Sarmila/GeoWiki-Features huggingface dataset:
Baegunsan (Ulsan). Baegunsan (lit. White Cloud Mountain) is a mountain located in Duseomyeon, Ulju County, Ulsan, South Korea. It was previously named Albaksan () during the Silla Dynsasy. It has an elevation of.

Geographic entities mentioned:
surface_form: baegunsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.07472222
lon: 127.44416667
surface_form: baegunsan
instance_of: Mountain
countries: South Korea
surface_form: baegunsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 37.838530555556
lon: 127.66387777778
surface_form: baegunsan
instance_of: Mountain
countries: South Korea
surface_form: baegunsan
instance_of: Mountain
countries: South Korea
surface_form: baegunsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 35.106388888889
lon: 127.62166666667
From 2003 to 2013 it comprised all of Northampton County, most of Lehigh County, and small parts of Berks and Montgomery counties. The district included the Lehigh Valley, Indian Valley and Upper Perkiomen Valley regions. In the mid-20th century, it included Tioga County.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
In 1892, he was appointed to assist Patrick Geddes with the teaching of botany at University College, Dundee. in 1892 he was made a Fellow of the Royal Geographical Society. He then moved in 1892 to Fort William, Scotland to work on a metereological observatory on Ben Nevis. In 1894 he moved to Manchester to become a lecturer in political and commercial geography in the University of Manchester.

Geographic entities mentioned:
surface_form: Ben Nevis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.796891
lon: -5.003675
Sandaldjian's creations included a carving of Mount Ararat on a grain of rice, a crucifix in which a minute golden figure of Jesus hangs upon a cross made from a bisected strand of Sandaldjian's own hair, and recreations of Disney figures (Snow White and the Seven Dwarfs or Mickey Mouse, for example) or historical figures (such as Napoleon or Pope John Paul II) presented in the eye or on the tip of a needle.

Geographic entities mentioned:
surface_form: Mount Ararat
instance_of: Mountain
countries: Turkey
coordinates: lat: 39.70194444444444
lon: 44.29833333333333
Wisconsin Governor's Mansion. The Executive Residence, known better as the Governor's Mansion, is located at 99 Cambridge Road in the Village of Maple Bluff, Wisconsin (a suburb of the state capital of Madison), on the eastern shore of Lake Mendota. It is currently the official residence of Wisconsin Governor Tony Evers.

Geographic entities mentioned:
surface_form: Lake Mendota
instance_of: Lake
countries: United States
coordinates: lat: 43.106666666667
lon: -89.424722222222
Xhuvani was born in 1934 in Pogradec. His father, Kostaq Xhuvani, was a respected teacher from Elbasan. In 1944, during World War II, his family fled from Pogradec and took refuge in Mokër, where they stayed until their country was liberated, after which they moved to Elbasan. After finishing medical high-school he worked in the rural hospitals of Librazhd, Peqin, Gramsh, and Cërrik.

Geographic entities mentioned:
surface_form: Mokër
instance_of: Mountain
countries: Albania
coordinates: lat: 40.983333333333
lon: 20.516666666667
Rolf Brem. Rolf Brem (12 February 1926 – 11 April 2014) was a Swiss sculptor, illustrator and graphic artist. He worked in Meggen close to Lake Lucerne. Childhood. Rolf Brem grew up in a quarter in Lucerne where most people had conventional professions. There were butchers, bakers, metalworkers or carpenters. His father, Adolf Brem, was a hairdresser.

Geographic entities mentioned:
surface_form: Lake Lucerne
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.0194
lon: 8.4011
Meal Fell. Meal Fell is a small fell in the northern region of the English Lake District, it is situated south-west of the village of Caldbeck and is one of the four main Uldale Fells (the others being Longlands Fell, Great Cockup and Great Sca Fell). Topography.

Geographic entities mentioned:
surface_form: Longlands Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.7075
lon: -3.12671
surface_form: Great Cockup
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6895
lon: -3.12931
surface_form: Great Sca Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6942
lon: -3.10152
surface_form: meal fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6932
lon: -3.11545
surface_form: sca fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
Could this be the remains of another hill fort along the lines of Carrock Fell?’
Meal Fell is linked to Great Cockup to the west by the pass of Trusmadoor, a place described by Alfred Wainwright as the ‘Piccadilly of sheep in that locality’ to the east Meal Fell is connected by a ridge to Great Sca Fell. Ascents.

Geographic entities mentioned:
surface_form: Carrock Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.693561111111
lon: -3.0231472222222
surface_form: great sca fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6942
lon: -3.10152
surface_form: great cockup
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6895
lon: -3.12931
surface_form: meal fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6932
lon: -3.11545
surface_form: meal fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6932
lon: -3.11545
surface_form: sca fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
Ascents. The fell is usually climbed directly from the minor road to the west of the Uldale Fells with the hamlets of Orthwaite and Longlands the favoured starting points. Both of these walks approach the fell through the valleys although most walkers will climb Great Cockup first before arriving at Meal Fell and then go on to other fells in the area. Summit.

Geographic entities mentioned:
surface_form: great cockup
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6895
lon: -3.12931
surface_form: meal fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6932
lon: -3.11545
Meal Fell. Meal Fell is a small fell in the northern region of the English Lake District, it is situated south-west of the village of Caldbeck and is one of the four main Uldale Fells (the others being Longlands Fell, Great Cockup and Great Sca Fell). Topography.

Geographic entities mentioned:
surface_form: meal fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6932
lon: -3.11545
WXIX-TV additionally includes Decatur County in Indiana and Lewis County in Kentucky. Dayton-area media outlets similarly refer to a Miami Valley area that includes Butler and Warren counties in Ohio and sometimes Clinton County, Ohio, and Union County, Indiana.

Geographic entities mentioned:
surface_form: Miami Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.768611
lon: -84.189676
The view from the summit is vast, enabling the onlooker to see much of the encompassing region of County Kilkenny. Freestone Hill is seen to lay within the large natural &quot;amphitheatre&quot; surrounded by the Wicklow Mountains to the north, the Blackstairs to the east, Slievnaman to the south-west, and the Galtees to the west. Description.

Geographic entities mentioned:
surface_form: Slievnaman
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.43
lon: -7.563
surface_form: Galtees
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.366
lon: -8.179
Geology. Mount Elden is one of five large peripheral silicic volcanic features within the greater San Francisco Peaks volcanic system (part of the San Francisco volcanic field) which include the nearby Dry Lake Hills, the Hochderffer and White Horse Hills to the northwest, and O'Leary Peak to the northeast.

Geographic entities mentioned:
surface_form: O'Leary Peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.401388888889
lon: -111.52666666667
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6282988
lon: -97.0561783
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 38.3360373
lon: -117.7898285
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 45.0425
lon: -97.31972222
surface_form: mount elden
instance_of: Mountain
countries: United States
coordinates: lat: 35.241111111111
lon: -111.59666666667
Mount Elden. Mount Elden or Elden Mountain (Hopi: Hovi'itstuyqa) is located in central Coconino County northeast of Flagstaff, Arizona. The mountain is named after John Elden, one of the region's earliest Anglo settlers, who established a homestead on its lower slopes and grazed sheep on the open grasslands below during the late 19th century.

Geographic entities mentioned:
surface_form: mount elden
instance_of: Mountain
countries: United States
coordinates: lat: 35.241111111111
lon: -111.59666666667
In 1977, the Radio Fire, a human-caused wildfire, destroyed much of the vegetation on the southern and southeastern slopes, burning 4,600 acres (1,900 hectares). Despite its rugged appearance, steep relief, and nearly of surface area, Mount Elden is easily accessible via an extensive, well-developed road and non-motorized trail system that is part of the Coconino National Forest.

Geographic entities mentioned:
surface_form: mount elden
instance_of: Mountain
countries: United States
coordinates: lat: 35.241111111111
lon: -111.59666666667
Despite its rugged appearance, steep relief, and nearly of surface area, Mount Elden is easily accessible via an extensive, well-developed road and non-motorized trail system that is part of the Coconino National Forest. Mount Elden is one of six hundred volcanoes that dot the San Francisco volcanic field in Northern Arizona.

Geographic entities mentioned:
surface_form: mount elden
instance_of: Mountain
countries: United States
coordinates: lat: 35.241111111111
lon: -111.59666666667
Because these features developed within close proximity of the San Francisco Mountain strato-volcano there is a strong likelihood that each is a geologic subsidiary of the larger mountain. Geologically, Mount Elden is a lava dome composed almost entirely of dacitic lava flows which emerged from several vents.

Geographic entities mentioned:
surface_form: mount elden
instance_of: Mountain
countries: United States
coordinates: lat: 35.241111111111
lon: -111.59666666667
The mountain's overlapping flows commonly take lobe-like shapes which display a variety of flow characteristics and features including concentric benches, spires, ramping shear fractures, longitudinal tension fractures, and conjugate shear fractures. Positioned within the central part of Mount Elden, on the mountain's eastern and northwestern flanks, are two sedimentary blocks.

Geographic entities mentioned:
surface_form: mount elden
instance_of: Mountain
countries: United States
coordinates: lat: 35.241111111111
lon: -111.59666666667
Contemporary history. John Elden, the settler for whom Mount Elden bears its name, settled at the base of what is today Mount Elden in 1877 to raise sheep near a natural spring, now referred to as Elden Springs. The home-site today lies within the Coconino National Forest and bears a National Forest historical marker just north of the City of Flagstaff, Arizona, pictured to the right.

Geographic entities mentioned:
surface_form: mount elden
instance_of: Mountain
countries: United States
coordinates: lat: 35.241111111111
lon: -111.59666666667
surface_form: mount elden
instance_of: Mountain
countries: United States
coordinates: lat: 35.241111111111
lon: -111.59666666667
P. J. Abdul Kalam became the first Indian head of state to sail in a submarine. He was given a demonstrative excursion, during which the submarine dived and sailed in the Bay of Bengal for a few hours. He was accompanied by the Chief of Naval Staff Arun Prakash. The submarine was commanded by Commander P S Bisht. Accident (2010).

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
St. Wendelin's Chapel. vr8yo7xaatb6s1j64mthfffr1lhqh" xml:space="preserve">The small St. Wendelin's Chapel is located about 750 metres east of St. Odile above the Musbach valley, Germany, on the Small Roßkopf, a spur of the Roßkopf, at a height of 540 m. It belongs to the parish of St. Hilarius in Freiburg's suburb Ebnet.

Geographic entities mentioned:
surface_form: Musbach valley
instance_of: Valley
countries: Germany
coordinates: lat: 48.0027
lon: 7.89917
Lisa Brodyaga. Elisabeth S. Brodyaga (September 21, 1940 – October 28, 2021) was an American human rights lawyer. She ran Proyecto Libertad, a pro bono legal initiative for Central American asylum seekers. In 1986, she founded a refugee camp, Refugio del Rio Grande, in the Rio Grande Valley which she ran until her death. Since 1981, she was certified by the Texas Board of Legal Specialization.

Geographic entities mentioned:
surface_form: Rio Grande Valley
instance_of: Valley
countries: United States
Mexico
coordinates: lat: 26.22
lon: -98.12
Rock Pile Peaks. n86zjjqmv0r4k729va6wq89l09qw" xml:space="preserve">#redirect Rock Pile Peaks

Geographic entities mentioned:
surface_form: rock pile peaks
instance_of: Mountain
coordinates: lat: -68.416666666667
lon: -65.15
Rotundu. twym4zalpo1dj9srd51wk6l8d8el" xml:space="preserve">Rotundu is a flat, heavily forested peak on the side of Mount Kenya. It's formed by a near-perpendicular wall raising from a height of approximately above sea level and finally flattening above the peak's base. The flat land on the peak also hosts Lake Rotundu (.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
The initial race, which was in the uphill direction, was held between 2010 and 2013. The uphill race started near the desert floor and ended at the village of Summerhaven near the top of Mount Lemmon. Between 2017 and 2019, the second iteration of the race ran in the downhill direction from Summerhaven down to the desert floor.

Geographic entities mentioned:
surface_form: Mount Lemmon
instance_of: Mountain
countries: United States
coordinates: lat: 32.443130555556
lon: -110.78843055556
The &quot;New York Times&quot; noted that there are other difficult marathons including the Antarctic Ice Marathon which is run on snow and ice south of the Antarctic Circle, the Everest Marathon which starts at the south Everest Base Camp at an altitude of, and the Pikes Peak Marathon which climbs over to the top of Pikes Peak.

Geographic entities mentioned:
surface_form: Pikes Peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.840555555556
lon: -105.04416666667
Another sister ship, had been launched for the G&SWR a few weeks previously. &quot;Minerva&quot; had detail differences from &quot;Glen Rosa&quot; and &quot;Slieve Donard&quot;. &quot;Glen Rosa&quot; was named after Glen Rosa on the Isle of Arran. She worked various G&SWR ferry routes in the Firth of Clyde including off-season crossings to Arran.

Geographic entities mentioned:
surface_form: Glen Rosa
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.607
lon: -5.205
It is stretched in a north-south direction and considered to be the core of the Pamir mountain system. Geography. The highest peak of the range is the Ismoil Somoni Peak. It was also the highest peak in the former Soviet Union. The length of the Academy of Sciences Range is about 110 km. The crest of the range has an Alpine-like relief with 24 summits more than 6,000 m in height.

Geographic entities mentioned:
surface_form: Ismoil Somoni Peak
instance_of: Mountain
countries: Tajikistan
coordinates: lat: 38.942732
lon: 72.015347
Pebble jewellery, featuring the stones agate or &quot;Scotch Pebbles&quot;, Cairngorm, jasper, jaspagate, and sometimes bloodstone, freshwater pearls, gold, silver and granite, is a style of jewellery that has a long history associated with Scotland. Queen Victoria helped make the style become fashionable and she collected cairngorm stones on her walks on Beinn a' Bhùird near Balmoral Castle.

Geographic entities mentioned:
surface_form: Beinn a' Bhùird
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.087581
lon: -3.499366
In 2002, however, a joint venture between the Columbia Power Corporation and the Columbia Basin Trust constructed the 185 MW Arrow Lakes Hydro project in parallel with the Keenleyside Dam near Castlegar, 35 years after the storage dam was originally completed. The Duncan Dam remains a storage project, and has no power generation facilities. The Canadian and U.S.

Geographic entities mentioned:
surface_form: Arrow Lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 50
lon: -118
BC Hydro had to relocate and compensate for people's loss of land and homes. In Arrow Lake, 3,144 properties had to be bought and 1,350 people had to be relocated. With the construction of the Duncan Dam 39 properties were bought and 30 people moved, subsequently at Mica Dam 25 properties including trap lines and other economic resourceful lands were bought.

Geographic entities mentioned:
surface_form: Arrow Lake
instance_of: Group of lakes
countries: Canada
coordinates: lat: 50
lon: -118
By 1974, treaty power had increased this production threefold, hurting BC's own aluminum production, effectively exporting thousands of jobs in this industry. Further negative impacts include the flooding of approximately 600 km2 of fertile and productive valley bottoms to fill the Arrow Lakes, Duncan, Kinbasket and Koocanusa reservoirs.

Geographic entities mentioned:
surface_form: Arrow Lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 50
lon: -118
citizen, and remained there until 1964. Goldmann died in Bad Reichenhall, Germany of pulmonary collapse. He was buried in Jerusalem's Mount Herzl National Cemetery in the section reserved for leaders of the World Zionist Organization.His funeral was not attended by then-Prime Minister Menachem Begin, and no official statement of grief was issued by the Israeli government.

Geographic entities mentioned:
surface_form: Mount Herzl
instance_of: Mountain
countries: Israel
coordinates: lat: 31.774117
lon: 35.180567
Margilan. Margilan (,;) is a city (2024 pop. 253,500) in eastern Uzbekistan's Fergana Region. Margilan is located in the south of the Fergana Valley, where trade caravans from China traveled westwards and vice versa during the days of the Silk Road. Margilan has been renowned for its silk goods as far back as the 10th century. According to legend, Margilan was founded by Alexander the Great.

Geographic entities mentioned:
surface_form: Fergana Valley
instance_of: Valley
countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
lon: 71.757777777778
On his way back, he tasted the dish again and then called the place &quot;Murjinon&quot;. Since then, the city has been named Margilan. Margilan is one of the ancient cities of the Fergana Valley. In 1994-2004, employees of the Institute of Archaeology of Uzbekistan worked in the city, which revealed the existence of irrigated agriculture in Margilan oasis since no later than IV-III centuries BC.

Geographic entities mentioned:
surface_form: Fergana Valley
instance_of: Valley
countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
lon: 71.757777777778
The mosque has two impressive minarets, each 26 meters high, and original carved wooden pillars made from cedar by master craftsmen in Margilan. Geography. Margilan is located in the south-east of the Fergana Valley, in the foothills of the Alay Range, 9 km north-west of the regional center - the city of Fergana. There is a railway station on the Andijan - Kokand line. Population.

Geographic entities mentioned:
surface_form: Fergana Valley
instance_of: Valley
countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
lon: 71.757777777778
The western slopes of the fell drop swiftly to Fusedale over a few outcrops of rock, Fusedale Beck flowing due north to Ullswater. North north west and north from Loadpot Hill, two short spurs fan out to the twin tops of Bonscale Pike and Arthur's Pike. These two fells, both with craggy faces overlooking Ullswater, are separated by Swarthbeck Gill.

Geographic entities mentioned:
surface_form: Bonscale Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5731
lon: -2.84765
surface_form: loadpot hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.555211111111
lon: -2.8410888888889
Loadpot Hill. Loadpot Hill is a fell in the English Lake District, between Haweswater and Ullswater. Topography. Although of moderate height, Loadpot Hill and its descending ridges cover an area of around. Standing to the north of Wether Hill, Loadpot Hill is the last principal height on the main ridge of the Far Eastern Fells, before the land falls away to Penrith and the River Eamont.

Geographic entities mentioned:
surface_form: loadpot hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.555211111111
lon: -2.8410888888889
Loadpot Hill. Loadpot Hill is a fell in the English Lake District, between Haweswater and Ullswater. Topography. Although of moderate height, Loadpot Hill and its descending ridges cover an area of around. Standing to the north of Wether Hill, Loadpot Hill is the last principal height on the main ridge of the Far Eastern Fells, before the land falls away to Penrith and the River Eamont.

Geographic entities mentioned:
surface_form: loadpot hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.555211111111
lon: -2.8410888888889
surface_form: wether hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.542
lon: -2.839
These two fells, both with craggy faces overlooking Ullswater, are separated by Swarthbeck Gill. North east from Loadpot Hill the main ridge becomes broad and indistinct, falling gently in stages between the rivers Eamont and Lowther. These empty Ullswater and Haweswater respectively and converge from the summit, just south of Penrith.

Geographic entities mentioned:
surface_form: loadpot hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.555211111111
lon: -2.8410888888889
These empty Ullswater and Haweswater respectively and converge from the summit, just south of Penrith. In fellwalking terms the practical northern boundary of Loadpot Hill is the road from Pooley Bridge to Askham. This encloses broad slopes of heather and fell grass, with a wide depression at Moor Divock () and then a steeper rise to the independent top of Heughscar Hill ().

Geographic entities mentioned:
surface_form: loadpot hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.555211111111
lon: -2.8410888888889
There are also sink holes and old quarries. The north east ridge has Heltondale Beck to the south, a feeder of the Lowther. Beyond this an east ridge descends from Loadpot Hill between Heltondale and Cawdale, both of which are deeply cut. This ridge has a subsidiary top, The Pen, which bears a beacon (columnar cairn).

Geographic entities mentioned:
surface_form: loadpot hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.555211111111
lon: -2.8410888888889
This ridge has a subsidiary top, The Pen, which bears a beacon (columnar cairn). The Lowther valley and the Askham-Bampton road form the eastern boundary of the fell. South of Loadpot Hill a short ridge connects to Wether Hill, crossing a succession of peat hags. Summit. The broad top of Loadpot Hill has a trig point marking its highest point.

Geographic entities mentioned:
surface_form: loadpot hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.555211111111
lon: -2.8410888888889
surface_form: wether hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.542
lon: -2.839
South of Loadpot Hill a short ridge connects to Wether Hill, crossing a succession of peat hags. Summit. The broad top of Loadpot Hill has a trig point marking its highest point. A little to the south of the summit stood Lowther House, an old shooting lodge, but nothing now remains but a pile of stone from the chimney.

Geographic entities mentioned:
surface_form: loadpot hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.555211111111
lon: -2.8410888888889
The broad top of Loadpot Hill has a trig point marking its highest point. A little to the south of the summit stood Lowther House, an old shooting lodge, but nothing now remains but a pile of stone from the chimney. The Roman road (the High Street) which runs along the main ridge, makes a detour to the west around the summit of the fell before continuing north east via Moor Divock to Penrith.

Geographic entities mentioned:
surface_form: high street
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.492
lon: -2.865
Elisabetta Hut. The Elisabetta Hut (Italian: &quot;Rifugio Elisabetta&quot;; French: &quot;Refuge Élisabeth&quot;) is a refuge in the Italian Alps at an altitude of 2,195 m, on the Tour du Mont Blanc. It is located 3 km north-east of the Col de la Seigne, at the south-west end of the Mont Blanc massif, and provides good views of Mont Blanc and the Aiguille Noire de Peuterey.

Geographic entities mentioned:
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
surface_form: Aiguille Noire de Peuterey
instance_of: Mountain
countries: Italy
coordinates: lat: 45.815
lon: 6.8936111111111
Geography and geomorphology. Tocomar lies in northwestern Argentina, away from the town of San Antonio de los Cobres in the Jujuy Province and in proximity to the border with the Salta Province farther south. The area is part of the Puna, a high plateau of the Andes which formed starting in the Eocene and whose margins are formed by the Eastern Cordillera and the volcanic Western Cordillera.

Geographic entities mentioned:
surface_form: Puna
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
The area is part of the Puna, a high plateau of the Andes which formed starting in the Eocene and whose margins are formed by the Eastern Cordillera and the volcanic Western Cordillera. The Salta-Antofagasta railway and pass close to the volcanic field. Tocomar is located at elevation within a northwestward draining valley.

Geographic entities mentioned:
surface_form: antofagasta
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.968055555556
lon: -67.535833333333
Tocomar. Tocomar is a Pleistocene volcano in the Jujuy Province, Argentina. It is part of the Andean Volcanic Belt, more specifically to its sub-belt the Central Volcanic Zone. The Central Volcanic Zone consists of about 44 active volcanoes and large calderas of the Altiplano-Puna volcanic complex.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
The Central Volcanic Zone consists of about 44 active volcanoes and large calderas of the Altiplano-Puna volcanic complex. Volcanism there is caused by the subduction of the Nazca Plate beneath the South America Plate in the Peru-Chile Trench. At Tocomar, volcanism is further influenced by a large fault zone, the Calama-Olacapato-El Toro fault, which runs diagonally across the volcanic arc.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
At Tocomar, volcanism is further influenced by a large fault zone, the Calama-Olacapato-El Toro fault, which runs diagonally across the volcanic arc. Tocomar has generated several pyroclastic flows during the Pleistocene as well as phreatic-phreatomagmatic activity, and a magma chamber may still exist beneath the volcano.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
Tocomar has generated several pyroclastic flows during the Pleistocene as well as phreatic-phreatomagmatic activity, and a magma chamber may still exist beneath the volcano. Hot springs are found at the volcanic centre and have been prospected for the generation of geothermal power; the water discharged by the springs eventually forms the Tocomar river. Wetlands are found in the area.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
Hot springs are found at the volcanic centre and have been prospected for the generation of geothermal power; the water discharged by the springs eventually forms the Tocomar river. Wetlands are found in the area. Other than this, Tocomar was used as a source of obsidian in antiquity and more recently as a candidate site for a gamma ray observatory and as a mine. Geography and geomorphology.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
Geography and geomorphology. Tocomar lies in northwestern Argentina, away from the town of San Antonio de los Cobres in the Jujuy Province and in proximity to the border with the Salta Province farther south. The area is part of the Puna, a high plateau of the Andes which formed starting in the Eocene and whose margins are formed by the Eastern Cordillera and the volcanic Western Cordillera.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
The Salta-Antofagasta railway and pass close to the volcanic field. Tocomar is located at elevation within a northwestward draining valley. In this valley, pyroclastic flow and pyroclastic surge deposits crop out on the valley floor and parts of its slopes. In the northwestern and southeastern segments of the field, two vents can be recognized and are associated with springs.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
An obsidian lava dome marks one of the vents; aside from vents and dome the pyroclastic deposit forms most of this volcano. Hot springs are found at Tocomar and their activity has generated travertine deposits on the field, including at Baños de Tocomar where silica and sulfur accumulations can be found. The travertines have fibrous, filamentous, granular and lamellar appearances.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
Pits interpreted as having formed during hydrothermal explosions are also found. The springs are mostly found where the terrain has been incised by valleys. Electrical resistivity has been used to infer the structure of the geothermal reservoir beneath Tocomar, which is mostly located within an Ordovician basement; the temperatures of the reservoir have been estimated to be at depth.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
Electrical resistivity has been used to infer the structure of the geothermal reservoir beneath Tocomar, which is mostly located within an Ordovician basement; the temperatures of the reservoir have been estimated to be at depth. The water appears to be precipitation water that infiltrates terrain south of Tocomar, at elevations of.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
After being heated by the deep geothermal system, the water seems to interact with another shallower aquifer before emerging in the springs. Tocomar has been investigated for the potential to generate geothermal power. Exploration of the Tocomar-Cerro Tuzgle area ceased after a few wells were drilled and ended up being unproductive but has been reinitiated. Background.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
Background. Tocomar is part of the Andean Volcanic Belt's Central Volcanic Zone, which runs along the western margin of South America and lies in the countries of Peru, Bolivia, Chile and Argentina. The Central Volcanic Zone features about 44 active volcanoes as well as several large ignimbrite caldera systems; some of these are part of the Altiplano-Puna volcanic complex.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
About 200 of all volcanoes in the Andes have been active during the Holocene, 66 of these in historical times. The date of the last eruption of Tocomar is not known with certainty but was in the Pleistocene. Aside from the regular volcanic arc, volcanoes aligned along west-northwest to east-southeast lineaments are also part of the Central Volcanic Zone. Local.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
Aside from the regular volcanic arc, volcanoes aligned along west-northwest to east-southeast lineaments are also part of the Central Volcanic Zone. Local. At Tocomar, the Calama-Olacapato-El Toro fault is subdivided into two subsidiary faults called Incachule and Chorrillos, which in turn are connected by a number of normal faults that give the whole are a complex faulting scheme.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
These normal faults are associated with the Tocomar vents, and deformation of the eruption deposits indicates that some of the faults were active just as eruptions occurred; it is likely that eruptions were triggered by movement along these faults.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
These faults also control where geothermal spring activity occurs, but whether the faults themselves were active in the Quaternary is unclear; microseismic activity is still ongoing. The Tocomar volcano was constructed atop the ignimbrites from the Aguas Calientes caldera, as well as Pleistocene sediments which display traces of earthquake activity and form an alluvial cone.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
The area is a former basin now filled with volcanic and sedimentary rocks. The oldest outcropping basement in the region is the Precambrian Puncoviscana Formation east of Tocomar, in the San Antonio de los Cobres ridge.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
The oldest outcropping basement in the region is the Precambrian Puncoviscana Formation east of Tocomar, in the San Antonio de los Cobres ridge. Other volcanoes in the region are Cerro Tuzgle and two maars due north, Negro de Chorrillos and San Jéronimo due east and the Aguas Calientes caldera due south; the last two are located fairly close to Tocomar.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
These volcanoes were active roughly in reverse order, with Aguas Calientes active between 11 and 10 million years ago, while the other centers are of Quaternary age. Composition. The Tocomar centre has erupted rhyolitic ignimbrites, which belong to the potassium-rich peraluminous calc-alkaline magmatic series. It does not contain many crystals, which are formed by biotite, plagioclase and quartz.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
Climate, hydrology and vegetation. The region is sunny, dry, windy, cold and has a high difference between daytime and nighttime temperature. Average precipitation is less than mostly during summer; consequently Tocomar has an arid climate. The region was warmer and even drier in the past during the early Holocene, but Tocomar was paradoxically wetter.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
Average precipitation is less than mostly during summer; consequently Tocomar has an arid climate. The region was warmer and even drier in the past during the early Holocene, but Tocomar was paradoxically wetter. Springs give source to several permanent rivers in the region, which flow in deep valleys.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
The region was warmer and even drier in the past during the early Holocene, but Tocomar was paradoxically wetter. Springs give source to several permanent rivers in the region, which flow in deep valleys. Among these rivers is the, which after originating in a wetland receives the water from the Tocomar geothermal field and eventually ends in the. Much of the area around Tocomar has no vegetation.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
Springs give source to several permanent rivers in the region, which flow in deep valleys. Among these rivers is the, which after originating in a wetland receives the water from the Tocomar geothermal field and eventually ends in the. Much of the area around Tocomar has no vegetation. Of the plants that grow in the region, vegetation in the Puna occurs in the form of grass and shrub steppe.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
Because of the dry climate, wetlands are highly important for the regional biota and feature a characteristic biota. They have a different flora; 25 species have been identified in the Tocomar wetland. Green algae form mats close to the warm springs, which are also colonized by blue-green algae.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
Other animals found in the wetlands are amphipods such as &quot;Hyalella&quot; and leeches, among other aquatic macroinvertebrates. During the mid-Holocene dry period the wetlands of Tocomar may further have offered a refuge for local humans. Eruptive history. Between 1,150,000 ± 300,000 and 550,000 ± 100,000, the &quot;Tocomar ignimbrite&quot; was emplaced in the area.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
During the mid-Holocene dry period the wetlands of Tocomar may further have offered a refuge for local humans. Eruptive history. Between 1,150,000 ± 300,000 and 550,000 ± 100,000, the &quot;Tocomar ignimbrite&quot; was emplaced in the area. It consists of several different units of pyroclastic material, which cover a surface of about.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
It consists of several different units of pyroclastic material, which cover a surface of about. It is likely that geothermal activity was occurring at Tocomar prior to the emplacement of these ignimbrites; geothermally altered material was ejected during the eruptions. The eruption process has been reconstructed with the aid of the volcanic deposits.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
Travertine deposition took place during the Holocene and Pleistocene when the climate was wetter, in particular between 161,000 and 126,000 years ago. Some volcanic and neotectonic activity took place at the same time. Gravimetric anomalies, the presence of magmatic water in the springs and their high temperatures of about indicate that a magma chamber still exists beneath Tocomar. Human use.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
Gravimetric anomalies, the presence of magmatic water in the springs and their high temperatures of about indicate that a magma chamber still exists beneath Tocomar. Human use. Indigenous people of the region obtained obsidian at Tocomar and other sites of the region. Tocomar itself was not a major obsidian source however; other sites in the region were far more important.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
Human use. Indigenous people of the region obtained obsidian at Tocomar and other sites of the region. Tocomar itself was not a major obsidian source however; other sites in the region were far more important. In modern times, Tocomar has been investigated as a candidate site for a gamma ray observatory in Argentina. The existence of a kaolin mine in the area was reported in 1993.

Geographic entities mentioned:
surface_form: tocomar
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.166666666666668
lon: -66.56666666666666
The market originated in the 12th century around Murnau Castle. Murnau is on the edge of the Bavarian Alps, about south of Munich. Directly to its west is the Staffelsee lake and to the south are the peaks and ridges of the Ammergau Alps beginning with the Hörnle and extending up to the Ettaler Manndl, southwest of the Wetterstein.

Geographic entities mentioned:
surface_form: Staffelsee
instance_of: Lake
countries: Germany
coordinates: lat: 47.6908
lon: 11.1608
This mountain range is formed by the Zugspitze and the Alpspitze in the south as well as the Estergebirge with their striking Kistenkar and the Walchensee mountains including Heimgarten and Herzogstand in the southeast. To the south, the Murnauer Moos is the largest continuous wetland of its kind in Central Europe. History. The area around Murnau was already settled in pre-Christian times.

Geographic entities mentioned:
surface_form: Zugspitze
instance_of: Mountain
countries: Germany
Austria
coordinates: lat: 47.421217
lon: 10.986314
surface_form: Alpspitze
instance_of: Mountain
countries: Germany
coordinates: lat: 47.429444444444
lon: 11.0475
It was founded by settlers of The Church of Jesus Christ of Latter-day Saints in January 1878, several months before the neighboring community of Snowflake. Taylor straddles Silver Creek, flowing from the nearby White Mountains to the Little Colorado River on Arizona's Colorado Plateau. According to the 2010 census, the population of the town is 4,112.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
The division had moved into the line around Cassino, replacing the U.S. 36th Infantry Division, which had been attacking the strongly defended German positions. The first attack by the New Zealanders on 17 February was unsuccessful despite the bombing of the Monte Cassino abbey, which Kippenberger supported. A second attack was planned for 20 February, but it was delayed by bad weather.

Geographic entities mentioned:
surface_form: Monte Cassino abbey
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
Ohrdorf. The village of Ohrdorf lies in the north German state of Lower Saxony in the district of Gifhorn and belongs to the town of Wittingen. The village takes its name from the river Ohre, which rises near the village and empties into the Elbe north of Magdeburg. In East German times the state border ran down the centre of the Ohre not far from the village.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
He has also investigated various biblical mysteries, again presenting some controversial theories, such as an alternative location for Mount Sinai at Petra in Jordan, an Egyptian staff in a British museum as the staff of Moses, and a grave on the British island of Anglesey as the tomb of the Virgin Mary. Documentaries and television appearances.

Geographic entities mentioned:
surface_form: Mount Sinai
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.5384
lon: 33.9752
They had two children – a son and a daughter. Career. In 1905, Finley and Herman T. Bohlman visited and photographed Lower Klamath Lake and Tule Lake. Their report in the November–December issue of &quot;Bird Lore&quot; helped prompt President Theodore Roosevelt to set the areas aside as federal bird reservations.

Geographic entities mentioned:
surface_form: Lower Klamath Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.99083983333333
lon: -121.74309983333333
surface_form: Tule Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.909322222222
lon: -121.53304722222
It is situated at a height of about south west of Laguna Hedionda and east of Mount Araral.

Geographic entities mentioned:
surface_form: Araral
instance_of: Mountain
countries: Bolivia
coordinates: lat: -21.6
lon: -68.183333333333
surface_form: laguna hedionda
instance_of: Lake
countries: Bolivia
coordinates: lat: -21.5696528
lon: -68.0487138
surface_form: laguna hedionda
instance_of: Lake
countries: Bolivia
coordinates: lat: -22.4594235
lon: -67.3869217
surface_form: araral
instance_of: Mountain
countries: Bolivia
coordinates: lat: -21.6
lon: -68.183333333333
Ch'iyar Quta (Nor Lípez). __NOTOC__
Ch'iyar Quta (Aymara &quot;ch'iyara&quot; black, &quot;quta&quot; lake, &quot;black lake&quot;, hispanicized spellings &quot;Chiar Kkota, Chiar Khota, Chiar Kota&quot;) is a Bolivian lake located in the San Pedro de Quemes Municipality, Nor Lípez Province of the Potosí Department near the border to Chile.

Geographic entities mentioned:
surface_form: chiar khota
instance_of: Lake
countries: Bolivia
coordinates: lat: -16.195
lon: -68.24388889
surface_form: ch'iyar quta
instance_of: Lake
countries: Bolivia
coordinates: lat: -16.195
lon: -68.24388889
surface_form: ch'iyar quta
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.10083333
lon: -67.56083333
surface_form: ch'iyar quta
instance_of: Lake
countries: Bolivia
coordinates: lat: -18.049722222222222
lon: -69.05083333333333
surface_form: chiar kkota
instance_of: Lake
countries: Bolivia
coordinates: lat: -18.049722222222222
lon: -69.05083333333333
surface_form: lípez
instance_of: Mountain
countries: Bolivia
coordinates: lat: -21.914166666666667
lon: -66.88472222222222