Sarmila/GeoWiki-Features huggingface dataset:
In 1961, the Vinson Massif was named by the Advisory Committee on Antarctic Names (US-ACAN), after Carl G. Vinson, United States congressman from the state of Georgia, for his support for Antarctic exploration. On 1 November 2006, US-ACAN declared Mount Vinson and Vinson Massif to be separate entities. Vinson Massif lies within the unrecognized Chilean claim under the Antarctic Treaty System.

Geographic entities mentioned:
surface_form: vinson
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
surface_form: vinson massif
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
surface_form: mount vinson
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
Vinson, United States congressman from the state of Georgia, for his support for Antarctic exploration. On 1 November 2006, US-ACAN declared Mount Vinson and Vinson Massif to be separate entities. Vinson Massif lies within the unrecognized Chilean claim under the Antarctic Treaty System. Mount Vinson is the highest peak in Antarctica, at.

Geographic entities mentioned:
surface_form: vinson massif
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
On 1 November 2006, US-ACAN declared Mount Vinson and Vinson Massif to be separate entities. Vinson Massif lies within the unrecognized Chilean claim under the Antarctic Treaty System. Mount Vinson is the highest peak in Antarctica, at. It lies in the north part of Vinson Massif's summit plateau in the south portion of the main ridge of the Sentinel Range about north of Hollister Peak.

Geographic entities mentioned:
surface_form: vinson
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
surface_form: mount vinson
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
It was first climbed in 1966 by an American team led by Nicholas Clinch. An expedition in 2001 was the first to climb via the Eastern route, and also took GPS measurements of the height of the peak. 1,400 climbers have attempted to reach the summit of Mount Vinson. Mount Vinson is ranked 6th by topographic isolation. Geography.

Geographic entities mentioned:
surface_form: vinson
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
surface_form: mount vinson
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
The massif comprises both the high central Vinson Plateau with its few peaks rising to over, and several side ridges mostly trending southwest or northeast from the plateau. The current height () of Mount Vinson was measured by a GPS survey that was conducted by the 2004 Omega Foundation team comprising Damien Gildea of Australia (leader) and Rodrigo Fica and Camilo Rada of Chile.

Geographic entities mentioned:
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instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
surface_form: mount vinson
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
From 1998 through at least 2007, the Omega Foundation kept a GPS receiver on the summit for a suitable period of time to obtain accurate satellite readings. Geology. Steeply inclined strata known as the Crashsite Group forms Vinson Massif. It consists of of shallow-water, mostly marine, tan, green, and red quartzose sandstones (quartzites) and argillites.

Geographic entities mentioned:
surface_form: vinson massif
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
Climate and glaciers. The climate on Mount Vinson is generally controlled by the polar ice cap's high-pressure system, creating predominantly stable conditions but, as in any polar climate, high winds and snowfall are a possibility. Though the annual snowfall on Mount Vinson is low, high winds can cause base camp accumulations up to in a year.

Geographic entities mentioned:
surface_form: vinson
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
surface_form: mount vinson
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
During the summer season, November through January, there are 24 hours of sunlight. While the average temperature during these months is, the intense sun will melt snow on dark objects. Over successive years, the limited amount of snow that falls on Vinson Massif compacts and is transformed into ice, forming glaciers. These glaciers follow the topography and flow down the mountain's valleys.

Geographic entities mentioned:
surface_form: vinson massif
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
The Crosswell Glacier flows into the Rutford Ice Stream via Ellen Glacier. The south face of Mount Vinson is drained by Roché Glacier, which flows westwards into Branscomb Glacier, with the latter leaving Vinson Massif to join Nimitz Glacier. History.

Geographic entities mentioned:
surface_form: vinson
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
surface_form: vinson massif
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
surface_form: mount vinson
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
History. A high mountain, provisionally known as &quot;Vinson&quot;, was long suspected to be in this part of West Antarctica, but it was not actually seen until January 1958, when it was spotted by US Navy aircraft from Byrd Station. It was named after Carl Vinson, a United States Representative from Georgia who was a key supporter of funding for Antarctic research.

Geographic entities mentioned:
surface_form: vinson
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
It was named after Carl Vinson, a United States Representative from Georgia who was a key supporter of funding for Antarctic research. The first measurement of the Vinson Massif was established in 1959 at the elevation of. First ascent. In 1963, two groups within the American Alpine Club (AAC), one led by Charles D. Hollister and Samuel C.

Geographic entities mentioned:
surface_form: vinson massif
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
Hollister and Samuel C. Silverstein, M.D., then in New York, and the other led by Peter Schoening of Seattle, Washington, began lobbying the National Science Foundation to support an expedition to climb Mount Vinson. The two groups merged in spring 1966 at the urging of the National Science Foundation and the AAC and Nicholas Clinch was recruited by the AAC to lead the merged expeditions.

Geographic entities mentioned:
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instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
surface_form: mount vinson
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
surface_form: peter
instance_of: Mountain
coordinates: lat: -70.1833
lon: 64.9333
State Department. In the end, the purported race did not materialize as Conrad had difficulties with his plane. According to press reports, he and Sayre were still in Buenos Aires on the day the first four members of AAME 1966/67 reached Mount Vinson's summit. In December 1966 the Navy transported the expedition and its supplies from Christchurch, New Zealand to the U.S.

Geographic entities mentioned:
surface_form: vinson
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
surface_form: mount vinson
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
base at McMurdo Sound, Antarctica, and from there in a ski-equipped C-130 Hercules to the Sentinel Range. All members of the expedition reached the summit of Mount Vinson. The first group of four climbers summited on 18 December 1966, three more on 19 December, and the last three on 20 December.

Geographic entities mentioned:
surface_form: vinson
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
surface_form: mount vinson
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
Later ascents. The climb of Vinson offers little technical difficulty beyond the usual hazards of travel in Antarctica, and as one of the Seven Summits, it has received much attention from well-funded climbers in recent years. Multiple guide companies offer guided expeditions to Mount Vinson, at a typical cost of around US$45,000 per person, including transportation to Antarctica from Chile.

Geographic entities mentioned:
surface_form: vinson
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
surface_form: mount vinson
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
Multiple guide companies offer guided expeditions to Mount Vinson, at a typical cost of around US$45,000 per person, including transportation to Antarctica from Chile. The skyrunner Fernanda Maciel did the fastest ascent of Vinson in 6h40min and round trip in 9h41min from base camp.

Geographic entities mentioned:
surface_form: vinson
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
The skyrunner Fernanda Maciel did the fastest ascent of Vinson in 6h40min and round trip in 9h41min from base camp. In January 2008, four Alpini of the Italian Army — Ettore Taufer, Giovanni Amort, Elio Sganga, and Marco Farina — completed the first ascent of Mount Vinson via a new route after a 270 km overland traverse from Patriot Hills.

Geographic entities mentioned:
surface_form: vinson
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
surface_form: mount vinson
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
The route had never been attempted before and required 13 days of travel across Antarctic terrain to reach the base camp. The ascent from 2,125 m to the 4,897 m summit was completed over two days, with an intermediate camp at 3,940 m. This remains one of the longest unsupported approaches to Mount Vinson recorded. First ascent from east side.

Geographic entities mentioned:
surface_form: vinson
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
surface_form: mount vinson
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
Geology. Steeply inclined strata known as the Crashsite Group forms Vinson Massif. It consists of of shallow-water, mostly marine, tan, green, and red quartzose sandstones (quartzites) and argillites. In ascending order, the Crashsite Group is subdivided into the Howard Nunataks Formation (), the Mount Liptak Formation (), and the Mount Wyatt Earp Formation ().

Geographic entities mentioned:
surface_form: liptak
instance_of: Mountain
coordinates: lat: -78.75
lon: -84.9
surface_form: mount liptak
instance_of: Mountain
coordinates: lat: -78.75
lon: -84.9
surface_form: mount wyatt earp
instance_of: Mountain
coordinates: lat: -77.56666667
lon: -86.41666667
surface_form: wyatt earp
instance_of: Mountain
coordinates: lat: -77.56666667
lon: -86.41666667
The steeply inclined strata of the Crashsite Group are part of the western limb of a major syncline that forms the core of the Sentinel Range within the Ellsworth Mountains. The Mount Wyatt Earp Formation contains Devonian fossils. The transition beds at the base of the Crashsite Group contain Late Cambrian trilobites.

Geographic entities mentioned:
surface_form: mount wyatt earp
instance_of: Mountain
coordinates: lat: -77.56666667
lon: -86.41666667
surface_form: wyatt earp
instance_of: Mountain
coordinates: lat: -77.56666667
lon: -86.41666667
The first measurement of the Vinson Massif was established in 1959 at the elevation of. First ascent. In 1963, two groups within the American Alpine Club (AAC), one led by Charles D. Hollister and Samuel C. Silverstein, M.D., then in New York, and the other led by Peter Schoening of Seattle, Washington, began lobbying the National Science Foundation to support an expedition to climb Mount Vinson.

Geographic entities mentioned:
surface_form: charles
instance_of: Mountain
coordinates: lat: -67.38333
lon: 50
These glaciers follow the topography and flow down the mountain's valleys. The uppermost glacier occupies Jacobsen Valley on the north face of Mount Vinson, and flows either into Branscomb Glacier to the west or Crosswell Glacier to the east. The Crosswell Glacier flows into the Rutford Ice Stream via Ellen Glacier.

Geographic entities mentioned:
surface_form: rutford
instance_of: Mountain
coordinates: lat: -78.6
lon: -85.3
Oujé-Bougoumou Cree Nation. Oujé-Bougoumou Cree Nation is a Cree First Nation of Canada. It is headquartered in the Cree village of Oujé-Bougoumou, located on the shores of Opémisca Lake, in the Eeyou Istchee territory equivalent of Quebec. Oujé-Bougoumou is unique from the other First Nations of Eeyou Istchee in that it doesn't have an associated reserve. The village is due west of Chibougamau.

Geographic entities mentioned:
surface_form: Opémisca Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.9175
lon: -74.8675
It is situated on a hillside with views west towards the mountains of South Wales. Little now remains of the village's industrial history, but once it was a centre for iron-ore smelting furnaces, forges and coal mines. The Norman castle, now little more than a mound, commanded the shortest route from Gloucester Castle to the Welsh Marches and the Wye Valley. History.

Geographic entities mentioned:
surface_form: Wye Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69255
lon: -2.66283
The railway line was supposed to have opened in 1848, but the first unfinished viaduct collapsed into the river and its replacement delayed the opening of the line through the town by three years. The viaduct spans the Nidd Gorge about 200 metres north of the ruins of Knaresborough Castle and is a well-known landmark in the town.

Geographic entities mentioned:
surface_form: Nidd Gorge
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.014
lon: -1.487
He completed an exploration of the Mesabi and Vermilion Iron Ranges for the Minnesota Iron Company in 1875, and his observations were published in the &quot;Eleventh Annual Report of the Minnesota Geological Survey&quot; in 1882. Honors. Chester Peak, a mountain in the Sawtooth Range of northeastern Minnesota, was named in his honor.

Geographic entities mentioned:
surface_form: Chester Peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.813805555556
lon: -92.215436111111
His speech and personality impressed Dienhart, who invited him to their Chicago headquarters. Hillary proposed a &quot;Yeti search&quot; plus a party of climbers who would winter for the first time at () and then attempt the summit of Makalu () without oxygen.

Geographic entities mentioned:
surface_form: Makalu
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.889166666667
lon: 87.088611111111
The expedition gathered in Kathmandu in September 1960, destined for the Rolwaling Valley. The valley was reputed to be a Yeti stronghold and was the location where mountaineers Eric Shipton and Michael Ward, along with the Sherpa Sen Tenzing, had photographed alleged Yeti footprints in 1951. At the end of October the expedition went via the Tashi Laptsa Pass to the Khumbu region.

Geographic entities mentioned:
surface_form: Khumbu
instance_of: Valley
countries: Nepal
coordinates: lat: 27.805
lon: 86.71
Hillary and Doig took the &quot;scalp&quot; to Chicago in December 1960. The Assault on Ama Dablam. A party of leaders Mike Ward and Barry Bishop, Mike Gill and Wally Romanes made the first ascent to the summit of Ama Dablam on 13 March, starting on 11 March.

Geographic entities mentioned:
surface_form: Ama Dablam
instance_of: Mountain
countries: Nepal
coordinates: lat: 27.861111111111
lon: 86.861388888889
Sir Edward (sic) Hillary and Mrs E. (sic) Hillary had been invited at the last minute. The Assault on Makalu. The third object of the expedition was to acclimatise a party of climbers who would summit Makalu () without oxygen. There were to be three scientific camps where the bicycle ergonometer would be used: Base Camp (), camp 3 on the neve () and Camp 5 (on Makalu Col.

Geographic entities mentioned:
surface_form: Makalu
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.889166666667
lon: 87.088611111111
Pike's Peak Country. Pike's Peak Country was the name given to the gold mining region of the western United States near Pikes Peak during the Pike's Peak Gold Rush of 1858–1861.

Geographic entities mentioned:
surface_form: Pikes Peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.840555555556
lon: -105.04416666667
The short, finished arm east of Kędzierzyn-Koźle is known as &quot;Kanal Kędzierzynski&quot; and serves to connect the nitrogen factory &quot;Azoty Kędzierzyn AG&quot; to the Oder. The waterway today is again part of plans for a European Danube–Oder–Elbe Canal project that would also connect the Elbe river. In 2023, the Czech government cancelled the project.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
From the Cosby Campground (specifically behind Campsite B51), the Snake Den Ridge Trail winds for to its junction with the Appalachian Trail at Inadu Knob. Chapman's main peak is approximately to the south of Inadu Knob, with the trail first crossing the slopes of Old Black, Mount Guyot, and Tricorner Knob. A short bushwhack is required to reach the summit.

Geographic entities mentioned:
surface_form: Tricorner Knob
instance_of: Mountain
countries: United States
coordinates: lat: 35.695561111111
lon: -83.254169444444
surface_form: tricorner knob
instance_of: Mountain
countries: United States
coordinates: lat: 35.695561111111
lon: -83.254169444444
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 39.4587
lon: -105.938
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 44.1681
lon: -71.534
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 35.705
lon: -83.2575
surface_form: old black
instance_of: Mountain
countries: United States
coordinates: lat: 35.7147
lon: -83.2553
Like its neighbor Mount Guyot, Chapman is a double peak, with the southern peak being the true summit. A gap divides Chapman from Dashoga Ridge (i.e., Mount Hardison and Marks Knob), just two miles (3 km) to the east. Its western slope, known as Chapman Lead, is more gradual, descending roughly over to its base along the headwaters of the Little Pigeon River.

Geographic entities mentioned:
surface_form: marks knob
instance_of: Landform
Mountain
countries: United States
coordinates: lat: 35.6798
lon: -83.2487
surface_form: mount hardison
instance_of: Mountain
countries: United States
coordinates: lat: 35.68843
lon: -83.24932
Mount Chapman is situated along the Tennessee-North Carolina border, with Sevier County to the north and Swain County to the south. Like its neighbor Mount Guyot, Chapman is a double peak, with the southern peak being the true summit. A gap divides Chapman from Dashoga Ridge (i.e., Mount Hardison and Marks Knob), just two miles (3 km) to the east.

Geographic entities mentioned:
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 39.4587
lon: -105.938
surface_form: double peak
instance_of: Mountain
countries: United States
coordinates: lat: 60.7295951
lon: -152.5857568
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 44.1681
lon: -71.534
surface_form: double peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.828507
lon: -121.580047
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 35.705
lon: -83.2575
Mount Chapman. Mount Chapman is a mountain in the Great Smoky Mountains, located in the Southeastern United States. It has an elevation of 6,427 feet (1,956 m) above sea level. While the mountain is located deep within the Smokies, the Appalachian Trail crosses its eastern slope, coming to within of the summit.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount chapman
instance_of: Mountain
countries: United States
coordinates: lat: 35.6867
lon: -83.2711
Mount Chapman. Mount Chapman is a mountain in the Great Smoky Mountains, located in the Southeastern United States. It has an elevation of 6,427 feet (1,956 m) above sea level. While the mountain is located deep within the Smokies, the Appalachian Trail crosses its eastern slope, coming to within of the summit.

Geographic entities mentioned:
surface_form: mount chapman
instance_of: Mountain
countries: United States
coordinates: lat: 35.6867
lon: -83.2711
While the mountain is located deep within the Smokies, the Appalachian Trail crosses its eastern slope, coming to within of the summit. Mount Chapman is among the 10 highest mountains in the Appalachian range, if subpeaks are not included. Mount Chapman is situated along the Tennessee-North Carolina border, with Sevier County to the north and Swain County to the south.

Geographic entities mentioned:
surface_form: mount chapman
instance_of: Mountain
countries: United States
coordinates: lat: 35.6867
lon: -83.2711
Mount Chapman is among the 10 highest mountains in the Appalachian range, if subpeaks are not included. Mount Chapman is situated along the Tennessee-North Carolina border, with Sevier County to the north and Swain County to the south. Like its neighbor Mount Guyot, Chapman is a double peak, with the southern peak being the true summit.

Geographic entities mentioned:
surface_form: mount chapman
instance_of: Mountain
countries: United States
coordinates: lat: 35.6867
lon: -83.2711
Chapman Lead parallels Guyot Spur to the north, with Buck Fork between the two ridges. The summit is coated in a dense stand of Southern Appalachian spruce-fir forest. The remoteness of Mount Chapman has left it largely untouched by human history. The mountain is named after Colonel David C. Chapman, a Knoxville business leader who led efforts to establish a national park in the Smokies.

Geographic entities mentioned:
surface_form: mount chapman
instance_of: Mountain
countries: United States
coordinates: lat: 35.6867
lon: -83.2711
As head of the Tennessee Great Smoky Mountains Park Commission from 1927 to 1937, Chapman raised funds and negotiated hundreds of land purchases that helped make the park possible. Arnold Guyot crossed Mount Chapman in the late 1850s, measuring the mountain's summit at 6,447 feet (Guyot called it &quot;Mount Alexander&quot; after a Princeton colleague).

Geographic entities mentioned:
surface_form: mount chapman
instance_of: Mountain
countries: United States
coordinates: lat: 35.6867
lon: -83.2711
Chapman's main peak is approximately to the south of Inadu Knob, with the trail first crossing the slopes of Old Black, Mount Guyot, and Tricorner Knob. A short bushwhack is required to reach the summit. The Tricorner Knob Shelter is approximately to the northeast of Mount Chapman.

Geographic entities mentioned:
surface_form: mount chapman
instance_of: Mountain
countries: United States
coordinates: lat: 35.6867
lon: -83.2711
Charles Parish, Louisiana. The primary purpose of the canal is drainage; a series of pumps and feeder canals feed a portion of the rain and ground water of the East Bank of Jefferson into the canal which drains it into Lake Pontchartrain. The city of Kenner, Louisiana is on the Jefferson, or eastern, side. For most of the canal's distance, the area on the St.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
The Hunter–Bowen orogeny occurred in two main phases: The first being Permian accretion of passive-marginal Devonian- and Carboniferous-age sediments, occurring in the Hunter region, as well as the mid-west region of what is now New South Wales, followed by rifting, back-arc volcanism. The later Permian to Triassic event consisted of arc accretion and metamorphism related to ongoing subduction.

Geographic entities mentioned:
surface_form: Hunter region
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Handen has a station on the Stockholm commuter rail system and a large bus station serving great areas of Södertörn. Handen is where the municipality seat of Haninge is located. Haninge's major shopping center, Haninge Centrum, and the joint campus of KTH and Södertörns Högskola are also located here. The Övre Rudasjön lake is located just west of the commercial center.

Geographic entities mentioned:
surface_form: Övre Rudasjön
instance_of: Lake
countries: Sweden
coordinates: lat: 59.168333333333
lon: 18.133333333333
Piz Ault. Piz Ault is a mountain of the Glarus Alps, located south of the Oberalpstock in Switzerland. Three ridges lead to the peak with a fourth one not very distinct to the south. The frontier between the Canton of Uri and the Canton of Graubünden lies on the eastern and the northern ridge, making it a three-quarter Graubünden mountain.

Geographic entities mentioned:
surface_form: Oberalpstock
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.7425
lon: 8.7694444444444
surface_form: piz ault
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.728361111111
lon: 8.7819722222222
Piz Ault. Piz Ault is a mountain of the Glarus Alps, located south of the Oberalpstock in Switzerland. Three ridges lead to the peak with a fourth one not very distinct to the south. The frontier between the Canton of Uri and the Canton of Graubünden lies on the eastern and the northern ridge, making it a three-quarter Graubünden mountain.

Geographic entities mentioned:
surface_form: piz ault
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.728361111111
lon: 8.7819722222222
The municipalities are Disentis and Sedrun on the south and Silenen to the northeast. There is no path leading onto the peak for hikers. In winter time the area is accessible by a T-Bar ski lift which reaches up to some under its peak in its southwestern face. The ski resort is accessible from Disentis, lying south of Piz Ault in the State (Canton) of Graubünden.

Geographic entities mentioned:
surface_form: piz ault
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.728361111111
lon: 8.7819722222222
This was first built with Soviet assistance in 1958, and rose to international prominence when the 2006 North Korean nuclear test, 2009 North Korean nuclear test, 2013 North Korean nuclear test, and 2017 North Korean nuclear test were reported to have been held at Punggye-ri Nuclear Test Site in the area of Mantapsan mountain, in the northernmost part of the county.

Geographic entities mentioned:
surface_form: Mantapsan
instance_of: Mountain
countries: North Korea
coordinates: lat: 41.29861111
lon: 129.08166667
Geervliet. Geervliet is a town in the Dutch province of South Holland. It is a part of the municipality of Nissewaard, and lies about northwest of Spijkenisse on the Brielse Meer. It received city rights in 1381. Geervliet was a separate municipality until 1980, when it became part of Bernisse. Demographics. In 2001, the town of Geervliet had 1670 inhabitants.

Geographic entities mentioned:
surface_form: Brielse Meer
instance_of: Lake
countries: Netherlands
coordinates: lat: 51.905555555556
lon: 4.1897222222222
Qullpa Hirka. Qullpa Hirka (Quechua &quot;qullpa&quot; salty, saltpeter, Ancash Quechua &quot;hirka&quot; mountain, &quot;salty (or saltpeter) mountain&quot;, also spelled &quot;Colpa Irca&quot;) is a mountain in the Cordillera Negra in the Andes of Peru which reaches a height of approximately. It lies in the Ancash Region, Recuay Province, in the northern part of the Cotaparaco District.

Geographic entities mentioned:
surface_form: qullpa hirka
instance_of: Mountain
countries: Peru
coordinates: lat: -9.88083333
lon: -77.52666667
Southern Uplands Fault. The Southern Uplands Fault (or occasionally Southern Upland Fault) is a fault in Scotland that runs from Girvan (or more specifically from the Rhins of Galloway) to Dunbar on the East coast. It marks the southern boundary of the Scottish Midland Valley and the northern margin of the Southern Uplands; indeed it is recognised as a boundary between these two terranes.

Geographic entities mentioned:
surface_form: Midland Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.408
lon: -4.044
clarki&quot; and &quot;K. arenula&quot;. Originally considered a crown lorisid, more comprehensive phylogenetic analyses suggest it is a more basal to crown lorisiformes. &quot;K. clarki&quot; was described in 2003 from isolated teeth and jaw fragments found in Late Middle Eocene (&quot;c.&quot; 40 million years ago) sediments of the Birket Qarun Formation in the Egyptian Faiyum.

Geographic entities mentioned:
surface_form: Birket Qarun Formation
instance_of: Lake
countries: Egypt
coordinates: lat: 29.472222222222
lon: 30.614166666667
Altopiano delle Murge. The Altopiano delle Murge (Italian for 'plateau of the Murge') is a karst topographic plateau of rectangular shape in southern Italy. Most of it lies within Puglia and corresponds with the sub-region known as Murgia or Le Murge.

Geographic entities mentioned:
surface_form: murgia
instance_of: Plateau
countries: Italy
coordinates: lat: 40.976
lon: 16.406
surface_form: murge
instance_of: Plateau
countries: Italy
coordinates: lat: 40.976
lon: 16.406
It is usually divided into Alta Murgia (High Murgia), the highest area, with poorer vegetation, and Bassa Murgia (Lower Murgia), with more fertile land, extensively planted with olive-trees for the production of olives.

Geographic entities mentioned:
surface_form: murgia
instance_of: Plateau
countries: Italy
coordinates: lat: 40.976
lon: 16.406
surface_form: murgia
instance_of: Plateau
countries: Italy
coordinates: lat: 40.976
lon: 16.406
surface_form: murgia
instance_of: Plateau
countries: Italy
coordinates: lat: 40.976
lon: 16.406
surface_form: murgia
instance_of: Plateau
countries: Italy
coordinates: lat: 40.976
lon: 16.406
Altopiano delle Murge. The Altopiano delle Murge (Italian for 'plateau of the Murge') is a karst topographic plateau of rectangular shape in southern Italy. Most of it lies within Puglia and corresponds with the sub-region known as Murgia or Le Murge.

Geographic entities mentioned:
surface_form: altopiano delle murge
instance_of: Plateau
countries: Italy
coordinates: lat: 40.976
lon: 16.406
surface_form: murge
instance_of: Plateau
countries: Italy
coordinates: lat: 40.976
lon: 16.406
Altopiano delle Murge. The Altopiano delle Murge (Italian for 'plateau of the Murge') is a karst topographic plateau of rectangular shape in southern Italy. Most of it lies within Puglia and corresponds with the sub-region known as Murgia or Le Murge.

Geographic entities mentioned:
surface_form: altopiano delle murge
instance_of: Plateau
countries: Italy
coordinates: lat: 40.976
lon: 16.406
surface_form: murge
instance_of: Plateau
countries: Italy
coordinates: lat: 40.976
lon: 16.406
surface_form: murge
instance_of: Plateau
countries: Italy
coordinates: lat: 40.976
lon: 16.406
The name is believed to originate from the, meaning 'sharp stone'. Geography and geology. The Murge plateau covers a surface of some 4,000 km², bordered by the Ofanto river and the Tavoliere delle Puglie to the north, the Adriatic Sea to the northeast, and by the Messapic depression, which separates it from the Salento peninsula, to the south.

Geographic entities mentioned:
surface_form: murge
instance_of: Plateau
countries: Italy
coordinates: lat: 40.976
lon: 16.406
In summer, they rise up to 30 °C. Rain, unlike in the arid Salento nearby, has an annual average of ca. 950 mm. Economy. Historically, the Murge have been the seat of transhumance practice in animal husbandry, since at least the first millennium BC, with cattle being moved to Abruzzo in summer, and southwards during winter.

Geographic entities mentioned:
surface_form: murge
instance_of: Plateau
countries: Italy
coordinates: lat: 40.976
lon: 16.406
Cove Lake is an alpine lake in Custer County, Idaho, United States, located in the White Cloud Mountains in the Sawtooth National Recreation Area. The lake is accessed from Sawtooth National Forest trail 601. Cove Lake is east of D. O. Lee Peak and next to Hook Lake. It is also upstream of Walker Lake and downstream of Snow, Boulder, Gentian, Sapphire, and Cirque Lakes as well as The Kettles.

Geographic entities mentioned:
surface_form: The Kettles
instance_of: Group of lakes
countries: United States
coordinates: lat: 44.102134
lon: -114.62229
Opimihaw Creek. ul8isvelopl9w1nc2pdyvqlqhyyu" xml:space="preserve">#REDIRECT Opimihaw Creek

Geographic entities mentioned:
surface_form: opimihaw creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.21869
lon: -106.59431
Attercliffe Road railway station. Attercliffe Road railway station is a former railway station in Sheffield, South Yorkshire, England. The station served the communities of Attercliffe, Burngreave and workers in the Don Valley and was situated on the Midland Main Line near Attercliffe Road, lying between Sheffield railway station and Brightside railway station. History.

Geographic entities mentioned:
surface_form: Don Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.405
lon: -1.417
Duck Lake (Kalamazoo County). Duck Lake is a lake in Kalamazoo County, Michigan.

Geographic entities mentioned:
surface_form: duck lake
instance_of: Lake
countries: United States
coordinates: lat: 44.218055555556
lon: -93.815833333333
surface_form: duck lake
instance_of: Lake
countries: United States
coordinates: lat: 48.868888888889
lon: -113.33361111111
surface_form: duck lake (kalamazoo county)
instance_of: Lake
countries: United States
coordinates: lat: 42.40834
lon: -85.3818
surface_form: duck lake
instance_of: Lake
countries: United States
coordinates: lat: 43.1477189
lon: -76.6894205
surface_form: duck lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4751
lon: -91.2536
surface_form: duck lake
instance_of: Lake
countries: United States
coordinates: lat: 44.615277777778
lon: -85.741944444444
Duck Lake (Kalamazoo County). Duck Lake is a lake in Kalamazoo County, Michigan.

Geographic entities mentioned:
surface_form: duck lake
instance_of: Lake
countries: United States
coordinates: lat: 44.218055555556
lon: -93.815833333333
surface_form: duck lake
instance_of: Lake
countries: United States
coordinates: lat: 48.868888888889
lon: -113.33361111111
surface_form: michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: duck lake
instance_of: Lake
countries: United States
coordinates: lat: 42.40834
lon: -85.3818
surface_form: duck lake
instance_of: Lake
countries: United States
coordinates: lat: 43.1477189
lon: -76.6894205
surface_form: duck lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4751
lon: -91.2536
surface_form: duck lake
instance_of: Lake
countries: United States
coordinates: lat: 44.615277777778
lon: -85.741944444444
Board on Geographic Names. Chuar Butte and adjacent Temple Butte are the historical site of wreckage from the 1956 Grand Canyon mid-air collision, in which two commercial airliners collided, resulting in the deaths of all 128 on board both planes. This disaster was a catalyst that forced the government to overhaul airline regulation and to establish the Federal Aviation Administration.

Geographic entities mentioned:
surface_form: Temple Butte
instance_of: Mountain
countries: United States
coordinates: lat: 36.1619
lon: -111.825
Balaton Sound. Balaton Sound (also known as Heineken Balaton Sound between 2007 and 2012 and as MasterCard Balaton Sound since 2013 for sponsorship reasons) is one of Europe's largest open air electronic music festivals. Held annually since 2007 on the southern bank of Lake Balaton, Hungary, it features live acts and DJs from all around the world, from established artists to new names.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
Mount Ebal site. The Iron Age I Structure on Mt. Ebal, also known as the Mount Ebal site, Mount Ebal's Altar, and Joshua's Altar, is an archeological site dated to the Iron Age I, located on Mount Ebal, West Bank. The Mount Ebal site was discovered by Israeli archaeologist Adam Zertal during the Manasseh Hill Country Survey in 1980.

Geographic entities mentioned:
surface_form: Mount Ebal
instance_of: Mountain
countries: State of Palestine
coordinates: lat: 32.234
lon: 35.2733
Reception of the theory. There are several issues with the association with Joshua's altar that stand in opposition to Zertal's theory. One is that the site is located on the north side of the mountain, and not the south side facing Mount Gerizim, making a curse and blessing ritual held there and on Gerizim somewhat difficult to hold antiphonally.

Geographic entities mentioned:
surface_form: Mount Gerizim
instance_of: Mountain
countries: State of Palestine
coordinates: lat: 32.199444444444
lon: 35.272777777778
Mount Lugg. yc9umwxly8c2anm5sz6fnklffeu" xml:space="preserve">#REDIRECT Prince Charles Mountains

Geographic entities mentioned:
surface_form: lugg
instance_of: Mountain
coordinates: lat: -71.2167
lon: 64.7167
surface_form: mount lugg
instance_of: Mountain
coordinates: lat: -71.2167
lon: 64.7167
About 450 athletes of 29 nations participated. Compared to the former world masterships a long distance race was added. Individual. Event held in Valerette on February 24, 2008
Relay. event held in Morgins on February 25, 2008
Team. event held in Pointe de l'Au on February 26, 2008
Vertical race. event held on February 28, 2008
Long distance. event held on February 29, 2008

Geographic entities mentioned:
surface_form: Pointe de l'Au
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.200277777778
lon: 6.8411111111111
Filming. Most of the filming was done at Studio Babelsberg in Potsdam, but locations also included Lake Kitkajärvi in Kuusamo, Finland, several German locations (including Bad Tölz, the water bridge at Magdeburg, Köhlbrandbrücke and Reeperbahn in Hamburg, and various sites in Berlin, such as Kottbusser Tor, Görlitzer Bahnhof and Spreepark), as well as Ouarzazate and Essaouira in Morocco.

Geographic entities mentioned:
surface_form: Kitkajärvi
instance_of: Lake
countries: Finland
coordinates: lat: 66.133333333333
lon: 28.533333333333
Early life. Oscar Woolverton Griswold was born on 22 October 1886 in Ruby Valley, Nevada, son of William Griswold, a prominent Elko County rancher. Raised in Arthur, Nevada, he attended the University of Nevada, Reno from 1905 to 1906, when he received an appointment to the United States Military Academy (USMA) at West Point, New York.

Geographic entities mentioned:
surface_form: Ruby Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.4
lon: -115.3
She instructed people in Indian dance, hatha yoga, mantra, and meditation. Within a few years Swami Sivananda Radha began looking for land outside of the city. In 1963 she established Yasodhara Ashram, a spiritual retreat center, on Kootenay Lake near Nelson, British Columbia. In July 1963 she began sending out a monthly newsletter to her associates and friends.

Geographic entities mentioned:
surface_form: Kootenay Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
Ransome was living in the Lake District and he drew on his experiences and memories of encounters over many years with the local farming community. Ransome had often climbed Old Man of Coniston and in the book this becomes the children's Kanchenjunga. Expeditions to Kanchenjunga in the Himalayas had been much in the news while Ransome was writing the book. Plot summary.

Geographic entities mentioned:
surface_form: Kanchenjunga
instance_of: Mountain
countries: India
Nepal
coordinates: lat: 27.7
lon: 88.133333
Eventually the Great Aunt leaves and the Swallows and Amazons mount an expedition to sleep under the stars on the summit of nearby commanding hill &quot;Kanchenjunga&quot; (in reality The Old Man of Coniston). While there, they discover a box with a small coin left by the Blackett's parents and uncle on climbing the &quot;Matterhorn&quot; thirty years earlier.

Geographic entities mentioned:
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
Cryptantha crinita. &quot;Cryptantha crinita&quot; is a rare species of flowering plant in the borage family known by the common names Sacramento cryptantha and silky cryptantha. It is endemic to California in the United States, where it occurs in the northern Sacramento Valley and the adjacent edges of the Cascade Range foothills. This annual herb grows up to 30 or 40 centimeters in height.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
East Blackdene. East Blackdene is a hamlet in the civil parish of Stanhope, in County Durham, England. It is situated to the north of the River Wear, on the opposite side of Weardale from St John's Chapel. The land would have originally been one farm owned by the Bishop of Durham, but was subdivided through the 15th-17th centuries, resulting in a small cluster-settlement.

Geographic entities mentioned:
surface_form: Weardale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.716
lon: -1.925
The covered tower has a triangular plan and consists of seven larch logs that are connected by metal strips. The whole structure is tension with steel cables. Its observation platform is 18 metres high and offers views far across the Eifel and to the Hunsrück. For example, Klausen and its pilgrimage church may be seen.

Geographic entities mentioned:
surface_form: hunsrück
instance_of: Mountain
countries: Germany
coordinates: lat: 51.026111111111
lon: 9.1008333333333
At the top is the Kellerberg Observation Tower. Location. The Kellerberg rises in the Meulenwald forest, part of the Moselle Eifel. Its summit lies 0.5 km south-southeast of Dierscheid and belongs to its municipality; it is 2.2 km west-northwest of Erlenbach, in the municipality of Hetzerath, and 1.7 km north-northeast of Naurath in the county of Trier-Saarburg.

Geographic entities mentioned:
surface_form: erlenbach
instance_of: Watercourse
countries: Germany
coordinates: lat: 48.945
lon: 8.84
surface_form: erlenbach
instance_of: Watercourse
countries: Germany
coordinates: lat: 49.3428
lon: 9.52782
Kellerberg (Meulenwald). The Kellerberg is a hill, and the highest point of the Eifel part of the Meulenwald and of the collective municipality of Wittlich-Land. It rises near Dierscheid in the county of Bernkastel-Wittlich in the German state of Rhineland-Palatinate. At the top is the Kellerberg Observation Tower. Location. The Kellerberg rises in the Meulenwald forest, part of the Moselle Eifel.

Geographic entities mentioned:
surface_form: kellerberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.8944
lon: 6.761
surface_form: kellerberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.7296
lon: 11.075
At the top is the Kellerberg Observation Tower. Location. The Kellerberg rises in the Meulenwald forest, part of the Moselle Eifel. Its summit lies 0.5 km south-southeast of Dierscheid and belongs to its municipality; it is 2.2 km west-northwest of Erlenbach, in the municipality of Hetzerath, and 1.7 km north-northeast of Naurath in the county of Trier-Saarburg.

Geographic entities mentioned:
surface_form: kellerberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.8944
lon: 6.761
surface_form: kellerberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.7296
lon: 11.075
On topographic maps a spot height of 448.7 m appears in the vicinity of the summit. On the Kellerberg are parts of the protected landscape of the Meulenwald and Trier Municipal Forest (&quot;Meulenwald und Stadtwald Trier&quot;), CDDA No. 322963; established 1990; 132.8046 km²). Kellerberg Observation Tower.

Geographic entities mentioned:
surface_form: kellerberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.8944
lon: 6.761
surface_form: kellerberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.7296
lon: 11.075
322963; established 1990; 132.8046 km²). Kellerberg Observation Tower. In 1999 the 21.7-metre-high Kellerberg Observation Tower was built in a modern wood and steel design. The covered tower has a triangular plan and consists of seven larch logs that are connected by metal strips. The whole structure is tension with steel cables.

Geographic entities mentioned:
surface_form: kellerberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.8944
lon: 6.761
surface_form: kellerberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.7296
lon: 11.075
Mujir al-Din died in 1522. He was buried at the base of the Mount of Olives just outside the walls of the Old City, a little to the north of the Church of Gethsemane and right in front of the Tomb of Mary. His tomb, with its open four-columned structure covered by a dome, lies next to the sidewalk on the main road and there are steps leading down from it on both sides to the Tomb of the Virgin.

Geographic entities mentioned:
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
The remainder of the Marine Division was deployed to Huế and was given responsibility for north and northwest Thừa Thiên Province, while the 1st Division was given responsibility for the area southwest and south of Huế blocking any further PAVN advance from the A Sầu Valley.

Geographic entities mentioned:
surface_form: A Sầu Valley
instance_of: Valley
countries: Vietnam
coordinates: lat: 16.259305555556
lon: 107.2125
Pizzo Pianca. Pizzo Pianca is a mountain of the Swiss Lepontine Alps, located north of Olivone in the canton of Ticino. On its southern side it overlooks the lake of Luzzone.

Geographic entities mentioned:
surface_form: pizzo pianca
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.57638889
lon: 8.96222222
Bob Jr.'s son, Randy Orton, is also a professional wrestler. Orton and André the Giant were good friends for many years. Death. Orton died in Las Vegas, Nevada on July 16, 2006, at the age of 80, five days short of his 81st birthday, following multiple heart attacks. He was cremated and had his ashes scattered on Mount Charleston, Nevada in April 2007.

Geographic entities mentioned:
surface_form: Mount Charleston
instance_of: Mountain
countries: United States
coordinates: lat: 36.271597222222
lon: -115.69556944444
Geological exploration. In 1843 he made a geological exploration of the upper Mississippi in connection with an expedition sent to that region, and in 1846 visited the Lake Superior district for persons interested in the industrial development of that country. He delivered an interesting series of lectures on his return, giving an account of his experiences.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
The disease continued westward in 1892, across the Punjab (with 75,000 cholera deaths), and raged on through Afghanistan and claimed 60,000 lives in Persia, and then reached Imperial Russia which suffered a staggering morbidity rate, exacerbated by the Russian famine of 1891–1892. Cholera's penetration in Russia began at Baku, a port on the Caspian Sea.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5