Sarmila/GeoWiki-Features huggingface dataset:
Bovegno (Brescian:) is a &quot;comune&quot; in the province of Brescia, in Lombardy. It borders the communes of Artogne, Berzo Inferiore, Bienno, Collio, Esine, Gianico, Irma, Marmentino and Pezzaze. It is located in the valley named Val Trompia. The Brescian poet Angelo Canossi spent the last years of his life here, mainly at &quot;Cà de le bachere&quot; (now a national monument) in Val Sorda.

Geographic entities mentioned:
surface_form: Val Trompia
instance_of: Valley
countries: Italy
coordinates: lat: 45.691944444444
lon: 10.186388888889
Kratka Ridge. Kratka Ridge or Snowcrest is a skiable area on Waterman Mountain in the San Gabriel Mountains of Los Angeles County, California. Located 36 miles northeast of La Cañada and Pasadena along the Angeles Crest Highway, it reaches a height of 7,515 feet (2,291 m). The area had two chair lifts and a rope tow and has a total of 13 runs with a vertical drop of approximately 750 feet (230 m).

Geographic entities mentioned:
surface_form: Waterman Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.3361
lon: -117.936
There are approximately 1,500 such peaks on Earth. Some well-known peaks, such as the Matterhorn and Eiger, are not ultras because they are connected to higher mountains by high cols and thus do not achieve enough topographic prominence. The term &quot;ultra&quot; originated with earth scientist Steve Fry, from his studies of the prominence of peaks in Washington in the 1980s.

Geographic entities mentioned:
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
surface_form: Eiger
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.577607529
lon: 8.005286822
Distribution. Currently, over 1,500 ultras have been identified above sea level: 654 in Asia, 357 in North America, 209 in South America, 119 in Europe (including 12 in the Caucasus), 84 in Africa, 54 in Oceania, and 39 in Antarctica. Many of the world's largest mountains are ultras, including Mount Everest, K2, Kanchenjunga, Kilimanjaro, Mont Blanc, and Mount Olympus.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
surface_form: K2
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
Many of the world's largest mountains are ultras, including Mount Everest, K2, Kanchenjunga, Kilimanjaro, Mont Blanc, and Mount Olympus. On the other hand, others such as the Eiger and the Matterhorn are not ultras.

Geographic entities mentioned:
surface_form: Eiger
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.577607529
lon: 8.005286822
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
In British Columbia, some of the mountains listed do not even have generally recognized names. Thirteen of the fourteen 8,000-metre summits are ultras (the exception being Lhotse), and there are a further 64 ultras over in height. There are 90 ultras with a prominence of over, but only 22 with more than prominence.

Geographic entities mentioned:
surface_form: Lhotse
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.961666666667
lon: 86.933333333333
There are 90 ultras with a prominence of over, but only 22 with more than prominence. A number of ultras have yet to be climbed, with Sauyr Zhotasy, (possibly) Mount Siple, and Gangkar Puensum being the most likely candidates for the most prominent unclimbed mountain in the world. All of the Seven Summits are ultras by virtue of the fact that they are the high points of large landmasses.

Geographic entities mentioned:
surface_form: Sauyr Zhotasy
instance_of: Mountain
countries: Kazakhstan
People's Republic of China
coordinates: lat: 47.049166666667
lon: 85.566666666667
surface_form: Mount Siple
instance_of: Mountain
coordinates: lat: -73.433333333333
lon: -126.66666666667
Its mostly bare summit plateau is highly dissected, presenting difficulties even for helicopter landings. In his 1978 book, &quot;La Vegetación del Mundo Perdido&quot;, Charles Brewer-Carías referred to a smaller lateral peak of Aparamán-tepui () as &quot;Murochiopán-tepui&quot;, though this name is now more commonly applied to the major peak immediately east of it.

Geographic entities mentioned:
surface_form: major peak immediately east of it
instance_of: Mountain
countries: Venezuela
coordinates: lat: 5.86972222
lon: -62.07555556
surface_form: aparamán
instance_of: Mountain
countries: Venezuela
coordinates: lat: 5.88694444
lon: -62.13111111
Aparamán-tepui. Aparamán-tepui is the westernmost of the four main tepuis of the Los Testigos chain in Bolívar, Venezuela. While the other three tepuis share a common slope area, Aparamán is derived from a separate basement. Aparamán-tepui has an elevation of around, a summit area of, and an estimated slope area of.

Geographic entities mentioned:
surface_form: bolívar
instance_of: Mountain
countries: Venezuela
coordinates: lat: 8.540861111111111
lon: -71.0465
surface_form: aparamán-tepui
instance_of: Mountain
countries: Venezuela
coordinates: lat: 5.88694444
lon: -62.13111111
Aparamán-tepui. Aparamán-tepui is the westernmost of the four main tepuis of the Los Testigos chain in Bolívar, Venezuela. While the other three tepuis share a common slope area, Aparamán is derived from a separate basement. Aparamán-tepui has an elevation of around, a summit area of, and an estimated slope area of.

Geographic entities mentioned:
surface_form: aparamán-tepui
instance_of: Mountain
countries: Venezuela
coordinates: lat: 5.88694444
lon: -62.13111111
Aparamán-tepui. Aparamán-tepui is the westernmost of the four main tepuis of the Los Testigos chain in Bolívar, Venezuela. While the other three tepuis share a common slope area, Aparamán is derived from a separate basement. Aparamán-tepui has an elevation of around, a summit area of, and an estimated slope area of.

Geographic entities mentioned:
surface_form: aparamán
instance_of: Mountain
countries: Venezuela
coordinates: lat: 5.88694444
lon: -62.13111111
While the other three tepuis share a common slope area, Aparamán is derived from a separate basement. Aparamán-tepui has an elevation of around, a summit area of, and an estimated slope area of. Its mostly bare summit plateau is highly dissected, presenting difficulties even for helicopter landings.

Geographic entities mentioned:
surface_form: aparamán-tepui
instance_of: Mountain
countries: Venezuela
coordinates: lat: 5.88694444
lon: -62.13111111
Avery Plateau. Avery Plateau () is an ice-covered plateau, about long and rising to about, midway between Loubet Coast and Foyn Coast in Graham Land, Antarctica. It borders the Hemimont Plateau on the south and the Bruce Plateau on the north. The first sighting of this plateau is still being determined.

Geographic entities mentioned:
surface_form: Bruce Plateau
instance_of: Plateau
coordinates: lat: -66
lon: -64
It borders the Hemimont Plateau on the south and the Bruce Plateau on the north. The first sighting of this plateau is still being determined. Still, it was presumably seen in January and February 1909 by members of the French Antarctic Expedition under Jean-Baptiste Charcot from various positions in the Matha Strait.

Geographic entities mentioned:
surface_form: Matha Strait
instance_of: Body of water
coordinates: lat: -66.5667
lon: -67.5
The New World district sits only about four miles from the Northeast entrance to Yellowstone National Park at the drainage divide between two creeks both of which eventually feed the Yellowstone River: Miller Creek, on the southwest side of Henderson Mountain, flows to Soda Butte Creek which goes into Yellowstone National Park where it joins the Lamar River then the Yellowstone River; Fisher Creek, on the northeast side of Henderson Mountain, flows into the Clark's Fork of the Yellowstone River which joins the Yellowstone River downstream and well northeast of Yellowstone National Park at Laurel, Montana.

Geographic entities mentioned:
surface_form: Henderson Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.05133
lon: -109.9449
KCYU-LD. KCYU-LD (channel 41) is a low-power television station in Yakima, Washington, United States, affiliated with Fox and Telemundo. The station is owned by Rincon Broadcasting Group, and maintains studios on West Lincoln Avenue in Yakima; its transmitter is located on Ahtanum Ridge.

Geographic entities mentioned:
surface_form: Ahtanum Ridge
instance_of: Landform
countries: United States
coordinates: lat: 46.5069
lon: -120.816
Dayton Ballet School. The company's dependent dance school, Dayton Ballet School, is the oldest dance school in Dayton and one of the oldest in the US. It is the only school in the Miami Valley that is linked to a professional dance company.

Geographic entities mentioned:
surface_form: Miami Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.768611
lon: -84.189676
Ji Hyeon-ok. Ji Hyeon-ok (; January 20, 1961 – April 29, 1999) was a South Korean mountaineer. Born in Nonsan, she climbed several of the tallest mountains in the world, including Denali (Mount McKinley) in 1988, Mount Everest, in 1993, becoming the first Korean woman to do so, Gasherbrum I, in 1997 and Gasherbrum II, in 1998.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
surface_form: Gasherbrum I
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.724444444444
lon: 76.696388888889
surface_form: Gasherbrum II
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.7575
lon: 76.652777777778
Born in Nonsan, she climbed several of the tallest mountains in the world, including Denali (Mount McKinley) in 1988, Mount Everest, in 1993, becoming the first Korean woman to do so, Gasherbrum I, in 1997 and Gasherbrum II, in 1998. On April 29, 1999, she went missing while climbing the Annapurna; Ji set foot on the peak but failed to return to the base camp.

Geographic entities mentioned:
surface_form: Annapurna
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.5958
lon: 83.82
Most of the ferries date to the early years of European-American settlement in the 1820s and 1830s, when parts of the region were still occupied by Cherokee and other Native American communities. During this time, a variety of privately owned and operated ferries carried travelers and loads across the Chattahoochee River and several other smaller rivers.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
&quot; -033-93 GEORGIA HISTORICAL COMMISSION 1963
Johnson Ferry Road is a major arterial road between Cobb County and Sandy Springs. From Columns Drive on the northwest riverbank of the Chattahoochee River, southeast to Abernathy Road, and continuing east on Abernathy to Roswell Road (SR 9), the roads have been temporarily designated by GDOT as SR 947.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Pace's Ferry. Pace's Ferry belonged to Hardy Pace, one of Atlanta's founders. Paces Ferry Rd. connects historic Vinings in the west, on the Chattahoochee River in Cobb County, to the western edge of Atlanta's Buckhead area in the east. From this end, West Paces Ferry Road, one of Atlanta's best-known streets, passes east through some of the oldest and wealthiest Buckhead neighborhoods.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Powers Ferry. The Powers Ferry (originally spelled &quot;Power's Ferry&quot;) was another route northwest from Atlanta, upstream from Pace's Ferry. It is named for James Power (1790–1870), a plantation owner, who established this Chattahoochee River ferry in 1835, before Atlanta was founded. The ferry remained in service for nearly 70 years, until a bridge was built in 1903.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Army maps of the area in 1864 do not show a ferry at the Shallow Ford. Vann's Ferry. Vann's Ferry was the first ferry across the Chattahoochee River, starting in 1804. It was operated by Cherokee leader James Vann (builder of the Vann House). It crossed the river between what are now Hall and Forsyth counties. This crossing area was flooded by the creation of Lake Lanier in the 1950s.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Poultney River. The Poultney River is a river in southwestern Vermont and eastern New York. In its 40-mile long course, the river drains approximately 263 square miles as it flows northwards into the southern end of Lake Champlain. Course. The Poultney River's origin is from a mountain spring in the town of Tinmouth, VT.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Tibidabo Funicular. The Tibidabo Funicular (;) is a funicular railway in the city of Barcelona, in Catalonia, Spain. The line connects &quot;Plaça del Doctor Andreu&quot;, the upper terminus of the &quot;Tramvia Blau&quot;, with the summit of Tibidabo, where there is an amusement park and a church, the Temple Expiatori del Sagrat Cor.

Geographic entities mentioned:
surface_form: Tibidabo
instance_of: Mountain
countries: Spain
coordinates: lat: 41.4225
lon: 2.118611111111111
During the period from 1750 to 1830, about 230 churches were constructed in Norway. Among these, 35 were octagonal, 62 were long churches (single nave hall church) and 110 were given a cruciform floor plan. During this period, 17 octagonal churches appeared in the Diocese of Nidaros (all of Norway north of the Dovrefjell mountains). Later, these church designs became popular in rural Agder.

Geographic entities mentioned:
surface_form: Dovrefjell
instance_of: Mountain
countries: Norway
coordinates: lat: 62.1
lon: 9.41666667
Peak 2266. Peak 2266 is the second highest point in Minnesota, after Eagle Mountain. It is rarely climbed and has no summit trail. Peak 2266 was surveyed in 1961, in the same survey which established Eagle Mountain as the state's high point. The survey found that 2266 was also higher than the previous record holder, point 2230 in the Misquah Hills.

Geographic entities mentioned:
surface_form: Misquah Hills
instance_of: Landform
countries: United States
coordinates: lat: 47.98
lon: -90.56
Peak 2266. Peak 2266 is the second highest point in Minnesota, after Eagle Mountain. It is rarely climbed and has no summit trail. Peak 2266 was surveyed in 1961, in the same survey which established Eagle Mountain as the state's high point. The survey found that 2266 was also higher than the previous record holder, point 2230 in the Misquah Hills.

Geographic entities mentioned:
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.924722222222
lon: -74.288055555556
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.3209
lon: -74.6616
surface_form: peak 2266
instance_of: Mountain
countries: United States
coordinates: lat: 47.9296
lon: -90.3708
surface_form: eagle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0618
lon: -74.5093
surface_form: eagle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.8974
lon: -90.5601
surface_form: eagle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.15166667
lon: -115.15277778
Peak 2266. Peak 2266 is the second highest point in Minnesota, after Eagle Mountain. It is rarely climbed and has no summit trail. Peak 2266 was surveyed in 1961, in the same survey which established Eagle Mountain as the state's high point. The survey found that 2266 was also higher than the previous record holder, point 2230 in the Misquah Hills.

Geographic entities mentioned:
surface_form: peak 2266
instance_of: Mountain
countries: United States
coordinates: lat: 47.9296
lon: -90.3708
Peak 2266. Peak 2266 is the second highest point in Minnesota, after Eagle Mountain. It is rarely climbed and has no summit trail. Peak 2266 was surveyed in 1961, in the same survey which established Eagle Mountain as the state's high point. The survey found that 2266 was also higher than the previous record holder, point 2230 in the Misquah Hills.

Geographic entities mentioned:
surface_form: peak 2266
instance_of: Mountain
countries: United States
coordinates: lat: 47.9296
lon: -90.3708
surface_form: eagle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0618
lon: -74.5093
surface_form: eagle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.8974
lon: -90.5601
surface_form: eagle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.15166667
lon: -115.15277778
These included an album with long-term collaborator Steve Nelson, a recording by trumpeter Donald Byrd, comeback albums from alto saxophonist Frank Morgan, and the first of a series of releases with tenor saxophonist Benny Golson. Miller and his family moved to Palmer Township in the Lehigh Valley region of eastern Pennsylvania in 1989.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
It is on the island's East Shore. Dongan Hills is bounded by Laconia Avenue to the southeast, Jefferson Avenue on the southwest, Richmond Road on the northwest, and Old Town Road to the north. It is adjacent to New Dorp and Grant City to the southwest, Todt Hill to the northwest, Old Town/Concord to the northeast, and South Beach and Midland Beach to the southeast.

Geographic entities mentioned:
surface_form: Todt Hill
instance_of: Mountain
countries: United States
coordinates: lat: 40.602222222222
lon: -74.112222222222
The &quot;hills&quot; alluded to in the name are the eastern ridge of Todt Hill, and much of what is colloquially referred to as &quot;Todt Hill&quot; by most island residents is reckoned as belonging to Dongan Hills by more authoritative sources such as the &quot;Staten Island Advance&quot;. However, there is a section of Dongan Hills that contains large hills.

Geographic entities mentioned:
surface_form: Todt Hill
instance_of: Mountain
countries: United States
coordinates: lat: 40.602222222222
lon: -74.112222222222
Ibn Athir's depiction of the Rūs is not primarily ethnological, and not dealing with particular customs or detailed geography. Rather, he accounts for the military significance of the Rūs as a people who raided the Caspian region and, importantly, who served the Byzantine Empire as mercenaries. Several references to the Rūs in the &quot;Kāmil&quot; are connected with Byzantine military operations.

Geographic entities mentioned:
surface_form: Caspian region
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Russell Island (Nunavut). Russell Island is an uninhabited island of the Arctic Archipelago in the Qikiqtaaluk Region of Nunavut, Canada. It is located in the Parry Channel, separated from the northern tip of Prince of Wales Island by the narrow Baring Channel. The western third of the island is separated from the other two thirds by a narrow lake and its outlet.

Geographic entities mentioned:
surface_form: Parry Channel
instance_of: Watercourse
countries: Canada
coordinates: lat: 74.33333333
lon: -93
Beneath them an allegorical figure of Fame flies across the heavens blowing her trumpet and carrying a banner proclaiming &quot;Canit inclyta caeseris arma&quot; (&quot;She proclaims the Emperor's illustrious arms&quot;). On the left sits Apollo surrounded by the nine Muses on Mount Parnassus and below them Pan leads a group celebrating a bacchanalia.

Geographic entities mentioned:
surface_form: Mount Parnassus
instance_of: Mountain
countries: Greece
coordinates: lat: 38.533
lon: 22.6167
The captain would make a low-level fly-pass over Runway 02, climb up and turn back, and repeat the fly-pass over the same runway in the reciprocal direction (Runway 20). This would be followed by a sightseeing trip south to Mont Blanc before the passengers would be returned to Basel–Mulhouse Airport. Finally, the aircraft would return to Paris.

Geographic entities mentioned:
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
History. The geographic township of Albanel was proclaimed in 1883, named after Jesuit missionary and explorer Charles Albanel (ca. 1616–1696). It had excellent land for farming, among the finest in the Lac Saint-Jean region at the time. Circa 1891, a mission was established in the township, served by pastors from Saint-Méthode and Normandin. In 1892, the Albanel post office opened.

Geographic entities mentioned:
surface_form: Lac Saint-Jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
Mývatn. Mývatn () is a shallow lake situated in an area of active volcanism in the north of Iceland, near Krafla volcano. It has a high amount of biological activity. The lake and the surrounding wetlands provide a habitat for a number of waterbirds, especially ducks.

Geographic entities mentioned:
surface_form: Krafla
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.733333333333
lon: -16.783333333333
surface_form: mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
This lava dammed up the first Mývatn, which was about as large as the present lake. The second volcanic cycle, the Hverfjall cycle, began 2500 years ago with a gigantic but brief eruption, which formed the explosion crater (tephra ring) Hverfjall (also named Hverfell). An eruption in Jarðbaðshólar followed, producing the lavafield between Reykjahlíð and Vogar.

Geographic entities mentioned:
surface_form: Hverfjall
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.6044691176
lon: -16.8719421252
surface_form: hverfell
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.6044691176
lon: -16.8719421252
surface_form: hverfjall
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.6044691176
lon: -16.8719421252
Later lava flowed from Leirhnjúkur down to the north end of Mývatn, destroying two farms. The Mývatnseldar eruptions are quite similar in character to the recent volcanic activity near Krafla in 1975&ndash;1984. The source of both is a central volcano lying between Krafla and Gæsafjöll.

Geographic entities mentioned:
surface_form: krafla
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.733333333333
lon: -16.783333333333
The Mývatnseldar eruptions are quite similar in character to the recent volcanic activity near Krafla in 1975&ndash;1984. The source of both is a central volcano lying between Krafla and Gæsafjöll. Inside the volcano resides a magma chamber from which molten magma periodically bursts into a swarm of fissures that cut through the volcano from north to south.

Geographic entities mentioned:
surface_form: krafla
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.733333333333
lon: -16.783333333333
This is an example of the process of continental drift in Iceland. A central volcano and its associated fissure swarm is called a volcanic system. The Krafla volcanic system is one of several such systems which together form the volcanic zone of Iceland. A few rhyolite mountains border the Krafla central volcano (Hlíðarfjall, Jörundur, Hrafntinnuhryggur).

Geographic entities mentioned:
surface_form: krafla
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.733333333333
lon: -16.783333333333
A central volcano and its associated fissure swarm is called a volcanic system. The Krafla volcanic system is one of several such systems which together form the volcanic zone of Iceland. A few rhyolite mountains border the Krafla central volcano (Hlíðarfjall, Jörundur, Hrafntinnuhryggur). Because of its volcanic origin, the lake was formerly mined for diatomite, but this ceased in 2004.

Geographic entities mentioned:
surface_form: hlíðarfjall
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.6487
lon: -18.2659
Mývatn. Mývatn () is a shallow lake situated in an area of active volcanism in the north of Iceland, near Krafla volcano. It has a high amount of biological activity. The lake and the surrounding wetlands provide a habitat for a number of waterbirds, especially ducks.

Geographic entities mentioned:
surface_form: mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
The effluent river Laxá is known for its rich fishing for brown trout and Atlantic salmon. The name of the lake (Icelandic (&quot;midge&quot;) and (&quot;lake&quot;); &quot;the lake of midges&quot;) comes from the large numbers of midges present in the summer. The name Mývatn is sometimes used not only for the lake but the whole surrounding inhabited area.

Geographic entities mentioned:
surface_form: mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
The name Mývatn is sometimes used not only for the lake but the whole surrounding inhabited area. The river Laxá, the lake Mývatn and the surrounding wetlands are protected as a nature reserve (the Mývatn&ndash;Laxá Nature Conservation Area), which occupies. Since 2000, a marathon around the lake has taken place in the summer. Geography.

Geographic entities mentioned:
surface_form: mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
The northern shoveler and northern pintail also regularly breed at the lake, albeit in smaller numbers, whilst common pochard used to breed regularly, but they have not done so regularly since the 1950s. The outflowing Laxá river contains around 250 pairs of harlequin duck and there is a large colony of eider at the river mouth some 50 km away from Mývatn.

Geographic entities mentioned:
surface_form: mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
The Barrow's goldeneye and the harlequin duck are both nearctic duck species. The population of the Barrow's goldeneye (of about 2000 individuals) relies entirely on the habitat provided by the Mývatn Laxá water system and its surrounding lava fields.

Geographic entities mentioned:
surface_form: mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
Most of the Barrow's goldeneyes overwinter there, using ice-free areas kept open by emerging spring water (both warm and cold) and in the strong river current. This species is a hole-nester, in North America using tree-holes, but at Mývatn the birds use cavities in the lava for nesting. The other duck species nest abundantly in the numerous islands of the lake and the surrounding marshlands.

Geographic entities mentioned:
surface_form: mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
Other common waterbirds include the Slavonian grebe, red-necked phalarope, great northern diver, red-throated diver and whooper swan. The lake is included in an important bird area. Bird populations have been monitored annually since 1975 by the Mývatn Research Station. There is a long tradition of harvesting duck eggs for home use on the local farms.

Geographic entities mentioned:
surface_form: mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
The ecosystem is now improving and small marimo balls are forming again. Volcanism. Mývatn was created about 2300 years ago by a large fissure eruption of basaltic lava. The lava flowed down the valley Laxárdalur to the lowland plain of Aðaldalur where it entered the Arctic Ocean about 50 km away from Mývatn.

Geographic entities mentioned:
surface_form: mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
The crater row that formed along the eruptive fissure is called Þrengslaborgir (or Lúdentarborgir) and has often been used as a textbook example of this type of volcanic activity. There was a large lake in the area at the time, a precursor of the present-day Mývatn. When the lava encountered the lake some of the water-logged lake sediment was trapped underneath it, generating steam explosions.

Geographic entities mentioned:
surface_form: mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
When the lava encountered the lake some of the water-logged lake sediment was trapped underneath it, generating steam explosions. By repeated explosions in a number of locations, groups of craters built up and now dominate the landscape on the shore of Lake Mývatn and also form some of the islands in the lake. This type of lava formation is known as rootless cones or pseudocraters.

Geographic entities mentioned:
surface_form: mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
At the close of the Ice Age, about 10,000 years ago, the Mývatn basin was covered by a glacier which pushed up huge end moraines which can still be seen at the north end of the lake. After the glacier started melting, a glacial lake was dammed up in the Mývatn depression until the glacier retreated from the present course of Laxá river.

Geographic entities mentioned:
surface_form: mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
At the close of the Ice Age, about 10,000 years ago, the Mývatn basin was covered by a glacier which pushed up huge end moraines which can still be seen at the north end of the lake. After the glacier started melting, a glacial lake was dammed up in the Mývatn depression until the glacier retreated from the present course of Laxá river.

Geographic entities mentioned:
surface_form: mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
surface_form: mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
The explosion crater (tephra ring) Lúdent dates from this cycle. Its eruption was followed by a number of small fissure eruptions. About 3800 years ago the shield volcano Ketildyngja was formed about 25 km south-east of Mývatn, and from it a huge lava flow, the Older Laxá-lava, spread over the southern part of the district, plunged down the valley Laxárdalur and flowed almost to the sea.

Geographic entities mentioned:
surface_form: mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
surface_form: mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
surface_form: laxárdalur
instance_of: Valley
countries: Iceland
coordinates: lat: 65.848333333333
lon: -19.866388888889
Approximately 200 years later a vast lava flow, the Younger Laxá Lava, was erupted (see above). The lava dammed up the present lake Mývatn and also the lakes Sandvatn, Grænavatn and Arnarvatn. The third volcanic cycle began with the Mývatnseldar eruptions in 1724–1729 which commenced with an explosion that formed the crater lake Víti.

Geographic entities mentioned:
surface_form: mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
The third volcanic cycle began with the Mývatnseldar eruptions in 1724–1729 which commenced with an explosion that formed the crater lake Víti. Later lava flowed from Leirhnjúkur down to the north end of Mývatn, destroying two farms. The Mývatnseldar eruptions are quite similar in character to the recent volcanic activity near Krafla in 1975&ndash;1984.

Geographic entities mentioned:
surface_form: mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
Most of the mountains in the vicinity of the lake were formed by eruptions under the ice sheet in the glacial periods of the Ice Age. Eruptions that melted their way up through the ice formed table mountains (Bláfjall, Sellandafjall, Búrfell, Gæsafjöll), those which did not formed hyaloclastite ridges (Vindbelgjarfjall, Námafjall, Dalfjall, Hvannfell).

Geographic entities mentioned:
surface_form: búrfell
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.08694444
lon: -19.82777778
surface_form: búrfell
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.0325
lon: -21.83333333
This type of lava formation is known as rootless cones or pseudocraters. A group of such craters at Skútustaðir on the south shore of the lake is protected as a natural monument. Other rootless cone groups in this lava field are in the valley Laxárdalur and the plain Aðaldalur. The formation of rootless cones halted the advance of the lava in some places creating temporary lava lakes.

Geographic entities mentioned:
surface_form: laxárdalur
instance_of: Valley
countries: Iceland
coordinates: lat: 65.848333333333
lon: -19.866388888889
Zavala, Ravno. Zavala () is a village in the Ravno municipality, in Bosnia and Herzegovina. Geography. Zavala is situated in the south-western expanse of Popovo polje, within the southernmost reaches of Bosnia and Herzegovina. The village is also located approximately 400 meters away from the Vjetrenica cave.

Geographic entities mentioned:
surface_form: Popovo polje
instance_of: Valley
countries: Bosnia and Herzegovina
coordinates: lat: 42.75
lon: 18.2131
Habitat and conservation. &quot;Allobates undulatus&quot; is diurnal, terrestrial frog found in mossy gallery forest. Scientists know it exclusively from its type locality in Cerro Yutajé, at an elevation of about above sea level. Its range is within the Formaciones de Tepuyes Natural Monument protected area. Reproduction.

Geographic entities mentioned:
surface_form: Formaciones de Tepuyes Natural Monument
instance_of: Landform
countries: Venezuela
coordinates: lat: 5.51666667
lon: -66.03333333
Michael to Nome on the Seward Peninsula, construction crews completed the final overland connection south of Fairbanks on June 27, 1903. By the time WAMCATS was fully operational in 1904, the system included almost of overland telegraph cable, over of submarine communications cable, and a wireless telegraphy system crossing the Norton Sound to Nome.

Geographic entities mentioned:
surface_form: Norton Sound
instance_of: Landform
countries: United States
coordinates: lat: 63.849166666667
lon: -164.26888888889
surface_form: norton sound
instance_of: Landform
countries: United States
coordinates: lat: 63.849166666667
lon: -164.26888888889
Army outposts and civilian Gold Rush camps in Alaska by telegraph. Along with Captain George C. Brunnell, Lieutenant Mitchell oversaw the construction of what became known as the Washington-Alaska Military Cable and Telegraph System (WAMCATS). Construction of the WAMCATS system began in the summer of 1900.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
By the time WAMCATS was fully operational in 1904, the system included almost of overland telegraph cable, over of submarine communications cable, and a wireless telegraphy system crossing the Norton Sound to Nome. This telegraph line was the first to link American outposts in Eagle, Valdez and Nome with each other as well as to Washington, D.C. in the contiguous United States.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Mount Billy Mitchell (Chugach Mountains). Mount Billy Mitchell is a prominent peak located in the Chugach Mountains, east of Valdez and west of the Copper River in the U.S. state of Alaska.

Geographic entities mentioned:
surface_form: mount billy mitchell
instance_of: Mountain
countries: United States
coordinates: lat: 61.2033
lon: -145.274
Mount Billy Mitchell was named for William &quot;Billy&quot; Mitchell (18791936), a brigadier general of the United States Army Air Service who is often referred to as the &quot;father of the United States Air Force&quot;. Naming. In response to the Klondike Gold Rush, the United States Army established numerous military outposts throughout the District of Alaska.

Geographic entities mentioned:
surface_form: mount billy mitchell
instance_of: Mountain
countries: United States
coordinates: lat: 61.2033
lon: -145.274
More snow falls in the vicinity of Valdez—an average annual snowfall of —than in any other location in the United States. Over thousands of years, this snow has accumulated to form glaciers on Mount Billy Mitchell, especially on its north face, which is its leeward side.

Geographic entities mentioned:
surface_form: mount billy mitchell
instance_of: Mountain
countries: United States
coordinates: lat: 61.2033
lon: -145.274
Until the 1970s, the wetland stretched over and permanently covered an area of that extended to about during seasonal floods. It was the largest in West Asia. The shallow eutrophic and slightly brackish Lake Hammar is the largest water body in the Hammar Marshes. Ethnic groups. The main ethnic group in the area is the Marsh Arabs. History. Massive drainage projects were started in the 1990s.

Geographic entities mentioned:
surface_form: Lake Hammar
instance_of: Lake
countries: Iraq
coordinates: lat: 30.77238
lon: 47.00155
Mittaghorn (Rawilpass). The Mittaghorn (also known as &quot;Tachaigne&quot;) is a mountain of the Bernese Alps, overlooking the Rawil Pass on the border between the cantons of Bern and Valais. It is located east of the Wildhorn.

Geographic entities mentioned:
surface_form: Wildhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.354583333333
lon: 7.3608611111111
surface_form: wildhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.354583333333
lon: 7.3608611111111
Mittaghorn (Rawilpass). The Mittaghorn (also known as &quot;Tachaigne&quot;) is a mountain of the Bernese Alps, overlooking the Rawil Pass on the border between the cantons of Bern and Valais. It is located east of the Wildhorn.

Geographic entities mentioned:
surface_form: mittaghorn (rawilpass)
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.38616667
lon: 7.43875
surface_form: mittaghorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.49825
lon: 7.9326111111111
Mittaghorn (Rawilpass). The Mittaghorn (also known as &quot;Tachaigne&quot;) is a mountain of the Bernese Alps, overlooking the Rawil Pass on the border between the cantons of Bern and Valais. It is located east of the Wildhorn.

Geographic entities mentioned:
surface_form: mittaghorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.38616667
lon: 7.43875
surface_form: tachaigne
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.38616667
lon: 7.43875
surface_form: mittaghorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.49825
lon: 7.9326111111111
Forbidden Rocks. n0tb9su3oz0inrb94hgodbg2smj" xml:space="preserve">#redirect Forbidden Rocks

Geographic entities mentioned:
surface_form: forbidden rocks
instance_of: Mountain
coordinates: lat: -73.6
lon: -94.2
Wararayuq. Wararayuq (Quechua &quot;warara&quot; horn, &quot;-yuq&quot; a suffix to indicate ownership, &quot;the one with a horn&quot;, Hispanicized spelling &quot;Huararayoc&quot;) is a mountain in the Paryaqaqa mountain range in the Andes of Peru. It is located in the Lima Region, Huarochirí Province, Quinti District. Wararayuq lies northwest of Qullqi P'ukru.

Geographic entities mentioned:
surface_form: wararayuq
instance_of: Mountain
countries: Peru
coordinates: lat: -11.9533
lon: -76.0875
Wararayuq. Wararayuq (Quechua &quot;warara&quot; horn, &quot;-yuq&quot; a suffix to indicate ownership, &quot;the one with a horn&quot;, Hispanicized spelling &quot;Huararayoc&quot;) is a mountain in the Paryaqaqa mountain range in the Andes of Peru. It is located in the Lima Region, Huarochirí Province, Quinti District. Wararayuq lies northwest of Qullqi P'ukru.

Geographic entities mentioned:
surface_form: wararayuq
instance_of: Mountain
countries: Peru
coordinates: lat: -11.9533
lon: -76.0875
surface_form: paryaqaqa
instance_of: Mountain
countries: Peru
coordinates: lat: -11.991666666666667
lon: -75.99166666666666
Piz Arlos. Piz Arlos is a mountain in the Oberhalbstein Range, located near Savognin in Graubünden, Switzerland.

Geographic entities mentioned:
surface_form: piz arlos
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.5588
lon: 9.5838
Cyprus Paragliding Club is one of the most active in improving the quality of flights, and finding new sites where paragliding could be possible. From time to time local competitions are organized. Noticeable sites are Curium, Stavrovouni, where is possible to fly above the Stavrovouni Monastery. Beach volleyball.

Geographic entities mentioned:
surface_form: Stavrovouni Monastery
instance_of: Mountain
countries: Cyprus
coordinates: lat: 34.885875
lon: 33.435497222222
Originally providing services to the Mount Cook region of the South Island, the company grew to take over many other New Zealand bus companies: &quot;H&H&quot; of Invercargill, &quot;Luxury Landlines&quot; and &quot;Hawkes Bay Motor Co&quot; of the North Island.

Geographic entities mentioned:
surface_form: Mount Cook
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.595
lon: 170.14194444444445
In August 1923 Wigley and two guides became the first to climb Mt Cook in winter. The first skifield in New Zealand was developed on Ball Glacier in Mount Cook National Park; the company opened another at Ōhau. Mount Cook Line Skifields developed and operated the Queenstown ski areas of Coronet Peak and The Remarkables, now owned by NZSki Ltd. Mount Cook Ski Planes.

Geographic entities mentioned:
surface_form: Coronet Peak
instance_of: Mountain
countries: New Zealand
coordinates: lat: -44.926897222222
lon: 168.73605277778
Montreux Casino. Montreux Casino (Casino Barrière de Montreux) is a casino located in Montreux, Switzerland on the shoreline of Lake Geneva. It has served as the venue for the Montreux Jazz Festival and was rebuilt following a 1971 fire memorialized in the Deep Purple song &quot;Smoke on the Water&quot;. It is a property of Groupe Lucien Barrière.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
A long descent leads to Long Mountain Circle, where Seven Lakes Drive crosses and US 6 joins the Palisades Interstate Parkway, descending slowly through a very scenic through Bear Mountain State Park between Bear Mountain to the south and Popolopen Torne to the north into another roundabout, the busy Bear Mountain Circle, where the parkway ends and US 6 intersects US 9W and US 202.

Geographic entities mentioned:
surface_form: Popolopen
instance_of: Mountain
countries: United States
coordinates: lat: 41.3269
lon: -74.0103
US 6 and US 202 turn right and begin a descent via Bear Mountain Bridge Road along the edge of the mountain to Peekskill. Pulloffs along this winding stretch allow drivers to take in sweeping views of that city, Haverstraw Bay, and Dunderberg Mountain across the river at the southern end of the Hudson Highlands. The road finally reaches US 6's third traffic circle just north of the city limit.

Geographic entities mentioned:
surface_form: Dunderberg Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.2856
lon: -73.9863
Leaving Mahopac, US 6 curves past the south end of West Branch Reservoir and controlled Lake Gleneida to its next highway junction, the east end of NY 52 at Reed Memorial Library just south of the county seat, Carmel. The highway immediately turns toward the south again, curving around Middle Branch Reservoir at Tilly Foster to the west terminus of NY 312.

Geographic entities mentioned:
surface_form: Lake Gleneida
instance_of: Lake
countries: United States
coordinates: lat: 41.42
lon: -73.683333333333
It rises in the Cass County town of Belton and empties into the Missouri River just west of the town of Sibley. The Little Blue was named for its smaller size relative to nearby Blue River. At Lake City, Missouri, the river has a mean annual discharge of 167 cubic feet per second. Longview Lake is a freshwater reservoir that was created by damming the river.

Geographic entities mentioned:
surface_form: Longview Lake
instance_of: Lake
countries: United States
coordinates: lat: 38.9097
lon: -94.4696
Lindeman Lake (Chilliwack). Lindeman Lake is a small lake in Chilliwack Lake Provincial Park, British Columbia, Canada. Located at the end of a trail, it is a popular hiking destination. A variety of fish inhabit this lake, including brook trout, cutthroat trout, rainbow trout, steelhead. Lindeman lake can be found by driving 40.5 km from Vedder Crossing along Chilliwack Lake road.

Geographic entities mentioned:
surface_form: chilliwack lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.05694444444445
lon: -121.41388888888889
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: lindeman lake
instance_of: Lake
countries: Canada
coordinates: lat: 59.8
lon: -135.0561111111111
surface_form: lindeman lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.11527777777778
lon: -121.45694444444445
Located at the end of a trail, it is a popular hiking destination. A variety of fish inhabit this lake, including brook trout, cutthroat trout, rainbow trout, steelhead. Lindeman lake can be found by driving 40.5 km from Vedder Crossing along Chilliwack Lake road. Lindeman lake trail can be found on the left hand side of the road prior to Chilliwack Lake Provincial Park.

Geographic entities mentioned:
surface_form: chilliwack lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.05694444444445
lon: -121.41388888888889
surface_form: lindeman lake
instance_of: Lake
countries: Canada
coordinates: lat: 59.8
lon: -135.0561111111111
surface_form: lindeman lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.11527777777778
lon: -121.45694444444445
Lindeman Lake (Chilliwack). Lindeman Lake is a small lake in Chilliwack Lake Provincial Park, British Columbia, Canada. Located at the end of a trail, it is a popular hiking destination. A variety of fish inhabit this lake, including brook trout, cutthroat trout, rainbow trout, steelhead. Lindeman lake can be found by driving 40.5 km from Vedder Crossing along Chilliwack Lake road.

Geographic entities mentioned:
surface_form: lindeman lake
instance_of: Lake
countries: Canada
coordinates: lat: 59.8
lon: -135.0561111111111
surface_form: lindeman lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.11527777777778
lon: -121.45694444444445
The archeological value of this site is immense at it provides a record of the lives of ordinary Egyptians – a perspective that is lost when only sources from society elites are studied. This site can be compared to Deir el-Medina, which, located adjacent to the Valley of the Kings, served a similar role for those artisans responsible for the construction of the tombs and temples there.

Geographic entities mentioned:
surface_form: Valley of the Kings
instance_of: Valley
countries: Egypt
coordinates: lat: 25.74025
lon: 32.602358
McDull tries his best to make his mother proud of him and his mother tries hard to give McDull a happy childhood. McDull wanted to go to the Maldives. His mother could not afford a trip there but she tricks him by taking him to The Peak by tram. The tram has a sign &quot;Go to the Maldives&quot;. It made McDull very happy as he thought that he was really going to the Maldives.

Geographic entities mentioned:
surface_form: The Peak
instance_of: Mountain
countries: People's Republic of China
British Hong Kong
coordinates: lat: 22.275469444444
lon: 114.14382777778