Sarmila/GeoWiki-Features huggingface dataset:
Burmester, geologist, Western Washington State University, Bellingham, WA, who worked in the Forrestal Range, 1978–79. Huie Cliffs. Steep rock cliffs rising above May Valley and forming the northwest edge of Saratoga Table. Named by US-ACAN for Carl Huie, technician in Antarctica, 1976–77, and geologist with USGS in the Pensacola Mountains, 1978–79. Himmelberg Hills.

Geographic entities mentioned:
surface_form: saratoga table
instance_of: Mountain
coordinates: lat: -83.34517
lon: -50.59592
Named by US-ACAN for Carl Huie, technician in Antarctica, 1976–77, and geologist with USGS in the Pensacola Mountains, 1978–79. Himmelberg Hills. A linear group of hills with prominent rock outcrops, long, at the southwest end of Saratoga Table. Named features in the group include Haskill Nunatak, near the center, and Ray Nunatak and Beiszer Nunatak at the south end. Named after Glen R.

Geographic entities mentioned:
surface_form: saratoga table
instance_of: Mountain
coordinates: lat: -83.34517
lon: -50.59592
Himmelberg Hills. A linear group of hills with prominent rock outcrops, long, at the southwest end of Saratoga Table. Named features in the group include Haskill Nunatak, near the center, and Ray Nunatak and Beiszer Nunatak at the south end. Named after Glen R. Himmelberg, Department of Geology, University of Missouri-Columbia. His laboratory research and scientific reporting with A.B.

Geographic entities mentioned:
surface_form: glen
instance_of: Mountain
coordinates: lat: -66.7667
lon: -67.4
Features, clockwise from the north, include Sorna Bluff, Mount Hummer, Mount Hook, Ronald Rock, Skidmore Cliff, Vigen Cliffs, Gabbro Crest, Sheriff Cliffs, Fierle Peak, Dyrdal Peak, Mount Stephens, Magnetite Bluff, Mathis Spur, Burmester Dome and Huie Cliffs. Features in the snowfield to the southeast include Haskill Nunatak, Ray Nunatak, Beiszer Nunatak, Grob Ridge and Coal Rock. Features.

Geographic entities mentioned:
surface_form: coal
instance_of: Mountain
coordinates: lat: -72.1167
lon: -68.5333
Named by US-ACAN for Richard W. Grob, cook at Ellsworth Station, winter 1957. Coal Rock. A prominent nunatak lying southeast of Fierle Peak at the south end of Forrestal Range, Pensacola Mountains. Named by Dwight L. Schmidt, USGS geologist to these mountains, for the Permian coal that is well exposed on the nunatak.

Geographic entities mentioned:
surface_form: coal
instance_of: Mountain
coordinates: lat: -72.1167
lon: -68.5333
Location. The Saratoga Table is bounded by the Support Force Glacier to the east and the Median Snowfield to the southwest. It is separated from the Lexington Table to the north by May Valley, Kent Gap and Chambers Glacier.

Geographic entities mentioned:
surface_form: lexington table
instance_of: Mountain
coordinates: lat: -83.11885
lon: -49.87252
History. In 878 the East Frankish king Carloman of Bavaria dedicated the Treffen estates around Lake Ossiach to the Benedictine monastery of Ötting. In the late 10th century the lands passed to the Bishops of Passau and later to Emperor Henry II, who conferred them to a certain Count Ozi, affiliated with the Styrian Otakar dynasty and father of Patriarch Poppo of Aquileia.

Geographic entities mentioned:
surface_form: Lake Ossiach
instance_of: Lake
countries: Austria
coordinates: lat: 46.666666666667
lon: 13.966666666667
Koryaksky or Koryakskaya Sopka () is an active volcano on the Kamchatka Peninsula in the Russian Far East. It lies within sight of Kamchatka Krai's administrative center, Petropavlovsk-Kamchatsky. Together with neighbouring Avachinsky, it is considered a Decade Volcano, worthy of particular study in light of its history of explosive eruptions and proximity to populated areas. Geological history.

Geographic entities mentioned:
surface_form: Avachinsky
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 53.255555555556
lon: 158.83333333333
The eruption continued until June 1957. On 29 December 2008, Koryaksky erupted with a plume of ash, the first major eruption in 3,500 years. In light of its proximity to Petropavlovsk-Kamchatsky, Koryaksky was designated a Decade Volcano in 1996 as part of the United Nations' International Decade for Natural Disaster Reduction, together with the nearby Avachinsky volcano.

Geographic entities mentioned:
surface_form: Avachinsky
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 53.255555555556
lon: 158.83333333333
Its extreme southern end dips into the town of Nottingham in Rockingham County. The pond is located on the Little River, a tributary of the Lamprey River and part of the larger Piscataqua River watershed. Like nearby Pawtuckaway Lake, Mendums Pond was created to ensure a consistent water supply for the Newmarket Manufacturing Company, a water-powered cotton textile manufacturer founded in 1822.

Geographic entities mentioned:
surface_form: Pawtuckaway Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.0889
lon: -71.1386
surface_form: mendums pond
instance_of: Lake
countries: United States
coordinates: lat: 43.173333333333
lon: -71.064166666667
Mendum's Pond. Mendums Pond (occasionally spelled Mendum's Pond) is a reservoir located primarily in Strafford County in eastern New Hampshire, United States, in the town of Barrington. Its extreme southern end dips into the town of Nottingham in Rockingham County. The pond is located on the Little River, a tributary of the Lamprey River and part of the larger Piscataqua River watershed.

Geographic entities mentioned:
surface_form: mendums pond
instance_of: Lake
countries: United States
coordinates: lat: 43.173333333333
lon: -71.064166666667
surface_form: mendum's pond
instance_of: Lake
countries: United States
coordinates: lat: 43.173333333333
lon: -71.064166666667
Like nearby Pawtuckaway Lake, Mendums Pond was created to ensure a consistent water supply for the Newmarket Manufacturing Company, a water-powered cotton textile manufacturer founded in 1822. During drought, a regulated flow would be released from the dam to run mills downriver in Newmarket. The University of New Hampshire owns of forestland on Mendums Pond. Arthur W.

Geographic entities mentioned:
surface_form: mendums pond
instance_of: Lake
countries: United States
coordinates: lat: 43.173333333333
lon: -71.064166666667
Mendum's Pond. Mendums Pond (occasionally spelled Mendum's Pond) is a reservoir located primarily in Strafford County in eastern New Hampshire, United States, in the town of Barrington. Its extreme southern end dips into the town of Nottingham in Rockingham County. The pond is located on the Little River, a tributary of the Lamprey River and part of the larger Piscataqua River watershed.

Geographic entities mentioned:
surface_form: mendum's pond
instance_of: Lake
countries: United States
coordinates: lat: 43.173333333333
lon: -71.064166666667
Artifacts show evidence of Woodland period, Hopewellian, and Mississippian cultures. Several important Native American settlements were located close to Peoria Lake, like the main villages of the Kickapoo and Potawatomi tribes. Other tribes may have used it as a game preserve during the winter while living in the Kaskaskia village, as the area was known for its &quot;fat beasts&quot;.

Geographic entities mentioned:
surface_form: Peoria Lake
instance_of: Lake
countries: United States
coordinates: lat: 40.702222222222
lon: -89.554444444444
Known as &quot;canapa&quot; in Italian, the historical ubiquity of hemp is reflected in the different variations of the name given to the plant in the various regions, including &quot;canape&quot;, &quot;càneva&quot;, &quot;canava&quot;, and &quot;canva&quot; (or &quot;canavòn&quot; for female plants) in northern Italy; &quot;canapuccia&quot; and &quot;canapone&quot; in the Po Valley; &quot;cànnavo&quot; in Naples; &quot;cànnavu&quot; in Calabria; &quot;cannavusa&quot; and &quot;cànnavu&quot; in Sicily; &quot;cànnau&quot; and &quot;cagnu&quot; in Sardinia.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
These include three Middle Neolithic (i.e. 4500–4000 B.C.) sites in the areas of Piacenza, Parma, and Forlì in Emilia-Romagna; as well as other sites near the Annone and Alserio lakes in Lombardy, from 5000 B.C. onwards.

Geographic entities mentioned:
surface_form: Annone
instance_of: Lake
countries: Italy
coordinates: lat: 45.811944444444
lon: 9.3494444444444
In regard to woven fabrics, archaeological excavations at Pompeii, in &quot;Campania felix&quot; (i.e. part of what is now Campania), unearthed samples of hemp textiles that had been preserved by the eruption of Mount Vesuvius in 79 A.D., reportedly including cloth sandals made of hemp, although linen was generally preferred in Antiquity for the production of canvas, sails, and clothing.

Geographic entities mentioned:
surface_form: Mount Vesuvius
instance_of: Mountain
countries: Italy
coordinates: lat: 40.821388888889
lon: 14.425555555556
A notable example of the use of Italian hemp ropes in mountaineering is the first technical climb of the Devils Tower in Wyoming in 1937, led by the German American pioneer of free climbing Fritz Wiessner, during which each climber carried a long safety rope made of the best quality Italian hemp.

Geographic entities mentioned:
surface_form: Devils Tower
instance_of: Mountain
countries: United States
coordinates: lat: 44.590277777778
lon: -104.71527777778
The ropes were tested using weights up to, and they were estimated to stretch between and, which would correspond to an extension between 17.1% and 22.9%, thus acting as a cushion to the climbers in case of a fall. Italian hemp ropes were also used during Wiessner's ill-fated American Karakoram expedition of 1939, which unsuccessfully attempted the first ascent to the then unclimbed summit of K2.

Geographic entities mentioned:
surface_form: K2
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
Der Kaiser von Kalifornien. &quot;Der Kaiser von Kalifornien&quot; (English: &quot;The Emperor of California&quot;), is a 1936 film that was the first Western film made in Nazi Germany. Some exterior scenes were shot on location in the United States at Sedona, Arizona, the Grand Canyon, and Death Valley in California. Plot.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Båvrojávrre. Båvrojávrre is a lake that lies on the border between Norway and Sweden. Most of the lake lies in Norway in Narvik Municipality in Nordland county. Only of the lake lies in Sweden in Gällivare Municipality in Norrbotten County. The lake Baugevatnet lies just to the north. The ending &quot;-jávrre&quot; is the Lule Sami word for lake.

Geographic entities mentioned:
surface_form: Baugevatnet
instance_of: Lake
countries: Norway
coordinates: lat: 68.0913
lon: 17.0148
Båvrojávrre. Båvrojávrre is a lake that lies on the border between Norway and Sweden. Most of the lake lies in Norway in Narvik Municipality in Nordland county. Only of the lake lies in Sweden in Gällivare Municipality in Norrbotten County. The lake Baugevatnet lies just to the north. The ending &quot;-jávrre&quot; is the Lule Sami word for lake.

Geographic entities mentioned:
surface_form: båvrojávrre
instance_of: Lake
countries: Sweden
Norway
coordinates: lat: 68.044027777778
lon: 16.968888888889
Description. The range is located on the administrative border between Ivano-Frankivsk and Zakarpattia oblasts. It is adjacent to the Gorgany range. The highest peak of Chornohora is Hoverla (2,061 m) with other high peaks including Pip Ivan (2,022 m) and Petros (2,020 m). The mountains are made of flysch rock. The major part of the range forms the watershed between the Prut and Tysa River.

Geographic entities mentioned:
surface_form: Hoverla
instance_of: Mountain
countries: Ukraine
Soviet Union
Austria-Hungary
coordinates: lat: 48.16027777777778
lon: 24.5
He supported his elder brother William, Essex's chief lieutenant, who was in command of a troop of a hundred horse which had been recruited by their father, then serving as Lord Lieutenant of Berkshire. William was the first of Essex's commanders to be ambushed by Irish forces and when his horse was killed under him, near Massereene, east of Lough Neagh, John saved his brother from being slain.

Geographic entities mentioned:
surface_form: Lough Neagh
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.618333333333
lon: -6.3952777777778
In September 1584 Norreys accompanied the Lord Deputy of Ireland, Sir John Perrot, and the earl of Ormonde into Ulster. The purpose, once again, was to dislodge the Highlander Scots of Clan MacDonald of Dunnyveg, who, led by Somhairle Buidhe MacDonnell, had migrated into both the Route and the Glens of Antrim.

Geographic entities mentioned:
surface_form: Glens of Antrim
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.16
lon: -6.1
During the period of heaviest rain, average rainfall across the entire island exceeded per hour. Rates along the Macoucherie River reached per hour. The heaviest rain was concentrated around the nation's tallest mountain, Morne Diablotins, where an estimated fell. Rainfall across Morne Diablotin National Park generally exceeded.

Geographic entities mentioned:
surface_form: Morne Diablotins
instance_of: Mountain
countries: Dominica
coordinates: lat: 15.503333333333
lon: -61.397222222222
__TOC__
Tectonic setting. Turkmenistan lies at the northern edge of the zone of complex tectonics caused by the continuing collision between the Arabian plate and the Eurasian plate. The main structure in the Caspian Sea is the Apsheron Sill, a zone of active subduction. Tsunami. Tsunami waves formed in the Caspian Sea after the earthquake.

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
Titan Nunatak. Titan Nunatak () is a broad, rather flat-topped nunatak, rising to about 460 m, standing between Coal Nunatak and Tethys Nunataks in the southeast corner of Alexander Island, Antarctica. The nunatak was first sighted and photographed from the air by Lincoln Ellsworth on November 23, 1935, and mapped from photos obtained on that flight by W.L.G. Joerg.

Geographic entities mentioned:
surface_form: Coal Nunatak
instance_of: Mountain
coordinates: lat: -72.1167
lon: -68.5333
surface_form: Tethys Nunataks
instance_of: Mountain
coordinates: lat: -72.1667
lon: -68.9833
surface_form: titan nunatak
instance_of: Mountain
coordinates: lat: -72.15
lon: -68.7167
surface_form: alexander
instance_of: Mountain
coordinates: lat: -63.3039
lon: -55.80564
Titan Nunatak. Titan Nunatak () is a broad, rather flat-topped nunatak, rising to about 460 m, standing between Coal Nunatak and Tethys Nunataks in the southeast corner of Alexander Island, Antarctica. The nunatak was first sighted and photographed from the air by Lincoln Ellsworth on November 23, 1935, and mapped from photos obtained on that flight by W.L.G. Joerg.

Geographic entities mentioned:
surface_form: titan nunatak
instance_of: Mountain
coordinates: lat: -72.15
lon: -68.7167
Joerg. Observed from the northwest (the direction from which Ellsworth photographed this nunatak), only the summit protrudes above the coastal ice, and it was uncertain whether this was a Peak on Alexander Island or an island in George VI Sound. Its true nature was determined by the Falkland Islands Dependencies Survey who surveyed this nunatak in 1949.

Geographic entities mentioned:
surface_form: george
instance_of: Mountain
coordinates: lat: -67.71667
lon: 50
surface_form: alexander
instance_of: Mountain
coordinates: lat: -63.3039
lon: -55.80564
It is the seat of the Comunità di Valle dell'Altopiano della Paganella. Geography. The town lies on the Paganella plateau, between the mountains Piz Galin, elevation, and Paganella, and its territory is part of the Adamello-Brenta natural park. History.

Geographic entities mentioned:
surface_form: Paganella
instance_of: Mountain
countries: Italy
coordinates: lat: 46.166666666667
lon: 11.066666666667
surface_form: Paganella
instance_of: Mountain
countries: Italy
coordinates: lat: 46.166666666667
lon: 11.066666666667
Cabia. Cabia (Friulian: &quot;Cjabie&quot;) is a &quot;frazione&quot; of the &quot;comune&quot; of Arta Terme, Friuli, north-eastern Italy, in the Carnia traditional region. It is a village located at 753 m across the Valle di Incarojo and the Val Bût, near the Monte Sernio, the Monte Amarana and the valley of Tolmezzo.

Geographic entities mentioned:
surface_form: Carnia
instance_of: Valley
countries: Italy
coordinates: lat: 46.39444444
lon: 12.77416667
Cabia. Cabia (Friulian: &quot;Cjabie&quot;) is a &quot;frazione&quot; of the &quot;comune&quot; of Arta Terme, Friuli, north-eastern Italy, in the Carnia traditional region. It is a village located at 753 m across the Valle di Incarojo and the Val Bût, near the Monte Sernio, the Monte Amarana and the valley of Tolmezzo.

Geographic entities mentioned:
surface_form: Monte Sernio
instance_of: Mountain
countries: Italy
coordinates: lat: 46.475
lon: 13.13767
Pic de Salòria. Pic de Salòria is a mountain of Catalonia, Spain. Located in the Pyrenees, it has an elevation of above sea level.

Geographic entities mentioned:
surface_form: pic de salòria
instance_of: Mountain
countries: Spain
coordinates: lat: 42.5144490848
lon: 1.38513757735
Jelenia Góra valley. 4i1qfgqcza60gqzaayngthlblpq" xml:space="preserve">#REDIRECT Jelenia Góra Valley

Geographic entities mentioned:
surface_form: jelenia góra valley
instance_of: Valley
countries: Prussia
coordinates: lat: 50.916666666667
lon: 15.75
Crooked Lake Canal. The Crooked Lake Canal was a canal in western New York, United States. Built from 1830-1833, the canal linked two Finger Lakes: Keuka and Seneca. The name refers to the unusual shape of Keuka Lake, which was formerly called &quot;Crooked Lake&quot;. The Keuka Outlet Trail now follows much of the route of the former canal. History.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
surface_form: Keuka
instance_of: Lake
countries: United States
coordinates: lat: 42.496388888889
lon: -77.146111111111
Peekamoose Mountain is flanked to the north by Table Mountain. The name Peekamoose is possibly an anglicization of an Algonquin word meaning 'broken off smooth', cf. Poke-O-Moonshine Mountain. Peekamoose Mountain stands within the watershed of Rondout Creek, a tributary of the Hudson River, which drains into New York Bay. The east and southeast slopes of Peekamoose Mtn. drain into Rondout Creek.

Geographic entities mentioned:
surface_form: Poke-O-Moonshine Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.4017
lon: -73.5131
Peekamoose Mountain. Peekamoose Mountain is a mountain located in Ulster County, New York. The mountain is part of the Catskill Mountains. Peekamoose Mountain is flanked to the north by Table Mountain. The name Peekamoose is possibly an anglicization of an Algonquin word meaning 'broken off smooth', cf. Poke-O-Moonshine Mountain.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.742222222222
lon: -112.46194444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.541388888889
lon: -118.29944444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7467
lon: -110.852
surface_form: peekamoose mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.953
lon: -74.3982
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.6918989
lon: -121.9826782
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6604
lon: -118.474
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.983
lon: -120.434
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9587
lon: -74.4048
Peekamoose Mountain. Peekamoose Mountain is a mountain located in Ulster County, New York. The mountain is part of the Catskill Mountains. Peekamoose Mountain is flanked to the north by Table Mountain. The name Peekamoose is possibly an anglicization of an Algonquin word meaning 'broken off smooth', cf. Poke-O-Moonshine Mountain.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: peekamoose mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.953
lon: -74.3982
Peekamoose Mountain. Peekamoose Mountain is a mountain located in Ulster County, New York. The mountain is part of the Catskill Mountains. Peekamoose Mountain is flanked to the north by Table Mountain. The name Peekamoose is possibly an anglicization of an Algonquin word meaning 'broken off smooth', cf. Poke-O-Moonshine Mountain.

Geographic entities mentioned:
surface_form: peekamoose mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.953
lon: -74.3982
Peekamoose Mountain is flanked to the north by Table Mountain. The name Peekamoose is possibly an anglicization of an Algonquin word meaning 'broken off smooth', cf. Poke-O-Moonshine Mountain. Peekamoose Mountain stands within the watershed of Rondout Creek, a tributary of the Hudson River, which drains into New York Bay. The east and southeast slopes of Peekamoose Mtn. drain into Rondout Creek.

Geographic entities mentioned:
surface_form: peekamoose mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.953
lon: -74.3982
The southwest end of Peekamoose drains into Buttermilk Falls Brook, thence into Rondout Creek. The west side of Peekamoose drains into Bear Hole Brook, thence into Rondout Creek. Peekamoose Mountain is within the Slide Mountain Wilderness of New York's Catskill State Park. The Long Path, a long-distance hiking trail from New York City to Albany, crosses the summits of Peekamoose and Table.

Geographic entities mentioned:
surface_form: peekamoose mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.953
lon: -74.3982
surface_form: slide mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9986
lon: -74.3864
surface_form: slide mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.3127
lon: -119.884
River Eden, Cumbria. The River Eden is a river that flows through Cumbria, England. It rises on Black Fell Moss, near the village of Outhgill, and runs in a generally north-westerly direction through the Vale of Eden and Solway Plain before reaching the sea at the Solway Firth. Etymology.

Geographic entities mentioned:
surface_form: Vale of Eden
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.388
lon: -2.294
Thus, there is no relation to the biblical Garden of Eden. Course of river. The Eden rises in Black Fell Moss, Mallerstang, on the high ground between High Seat, Yorkshire Dales and Hugh Seat. Here it forms the boundary between the counties of Cumbria and North Yorkshire; the river gave its name to the former Eden district of Cumbria.

Geographic entities mentioned:
surface_form: Hugh Seat
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.3875
lon: -2.2939
It starts life as Red Gill Beck, then becomes Hell Gill Beck, before turning north and joining with Ais Gill Beck to become the River Eden. (Hell Gill Force, just before it meets Ais Gill Beck, is the highest waterfall along its journey to the sea). The steep-sided dale of Mallerstang later opens out to become the Vale of Eden.

Geographic entities mentioned:
surface_form: Vale of Eden
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.388
lon: -2.294
It landed in the southwestern part of Saipan, not far from Chalan Kanoa village. The 8th Marines assaulted the beach fortifications and later helped seized the airstrip in Chalan Kanoa. The 8th Marines under Wallace's command later attacked the Japanese positions along the Lake Susupe and advanced towards the highest point of Saipan, Mount Tapochau. Wallace's marines conquered the summit of Mt.

Geographic entities mentioned:
surface_form: Mount Tapochau
instance_of: Mountain
countries: United States
coordinates: lat: 15.18888889
lon: 145.74305556
He has also commanded a battalion in Operation Rhino, targeted at infiltrators in Assam and Operation Falcon, along the Line of Actual control (LAC) in Arunachal Pradesh; an infantry brigade in the desert, a counter-insurgency force in the Kashmir valley, IV Corps (Tezpur) and GOC-C South Western Command (Jaipur).

Geographic entities mentioned:
surface_form: Kashmir valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
The town of Flims can be found at the line where the slip surface disappears under the debris. North of Flims the rock face of &quot;Flimserstein&quot; stands high whereas more westerly the slide surface is clearly visible.

Geographic entities mentioned:
surface_form: Flimserstein
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.878472222222
lon: 9.2801388888889
South of Flims is a huge hilly debris area that has been forest ever since, as this area is not suitable for farming, firstly for its shape and, even more for its lack of water. The river Rhine crosses this debris in a gorge called Ruinaulta. The Rhine still runs in debris, which shows that it has not yet reached the level it had before the incident.

Geographic entities mentioned:
surface_form: Ruinaulta
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.8081
lon: 9.31495
The highest hill in the debris area is almost higher than Flims at the end of the sliding surface. Landscape. The top of the slide surface can be found at above sea north of Flims at Fil de Cassons; the end of the slide surface is at about 1100. The pre-slide valley would have been at. The rock is Mesozoic limestone, including Mergel; the angle of slide is (only) 20° to 25°. Debris covers.

Geographic entities mentioned:
surface_form: Fil de Cassons
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.878472222222
lon: 9.2801388888889
Debris covers. Pressure baked the debris together to a somewhat stable rock. Given the river Rhine as a base of the valley, the debris is as high as. This debris dammed the Vorderrhein and created a lake in the Ilanz area. The level of the lake was found to have been at a maximum of above sea level, which results in a lake some long. Dating.

Geographic entities mentioned:
surface_form: Vorderrhein
instance_of: Watercourse
countries: Switzerland
coordinates: lat: 46.6325
lon: 8.6744444444444
Using carbon dating the limestone dust was found to be 10,055 years old (±195 years). A second source is wood that was found inside the debris in the region some upstream of the mouth of the river Rabiusa, which was covered by massive rock identified as being from the Fil de Cassons area, hence reaching this point during the event.

Geographic entities mentioned:
surface_form: Rabiusa
instance_of: Watercourse
countries: Switzerland
coordinates: lat: 46.8044
lon: 9.33028
surface_form: Fil de Cassons
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.878472222222
lon: 9.2801388888889
Flow system. After the slide most of the water escaped through the upper section of the debris. There are several examples of rivers disappearing in the Alps and also in Scotland. The lakes in the debris area, such as Caumasee, still behave in this way. The Ilanz lake existed some 1000 to 2000 years before the water cut through the debris, creating the gorge.

Geographic entities mentioned:
surface_form: Caumasee
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.820277777778
lon: 9.2958333333333
Lake Nicolet. Note: not to be confused with another &quot;Lake Nicolet&quot;, in Michigan (USA), on the St. Marys River (Michigan–Ontario) which links Lake Superior with Lake Huron.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: lake nicolet
instance_of: Lake
countries: Canada
coordinates: lat: 45.83
lon: -71.5603
surface_form: lake nicolet
instance_of: Lake
countries: Canada
coordinates: lat: 45.83
lon: -71.5603
surface_form: nicolet
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.255
lon: -72.6525
surface_form: nicolet
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.255
lon: -72.6525
Lake Nicolet (&quot;in French: lac Nicolet&quot;) is located 50 km south of Victoriaville, in the municipality of Saints-Martyrs-Canadiens, in Arthabaska Regional County Municipality (MRC), in administrative region of Centre-du-Québec, Canada. Lake Nicolet is the source of the Nicolet River which flows to the southeast shore of lake Saint-Pierre, in Nicolet.

Geographic entities mentioned:
surface_form: Nicolet River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.255
lon: -72.6525
surface_form: nicolet
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.255
lon: -72.6525
surface_form: nicolet
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.255
lon: -72.6525
Marys River (Michigan–Ontario) which links Lake Superior with Lake Huron. Lake Nicolet (&quot;in French: lac Nicolet&quot;) is located 50 km south of Victoriaville, in the municipality of Saints-Martyrs-Canadiens, in Arthabaska Regional County Municipality (MRC), in administrative region of Centre-du-Québec, Canada.

Geographic entities mentioned:
surface_form: lac nicolet
instance_of: Lake
countries: Canada
coordinates: lat: 45.83
lon: -71.5603
surface_form: lake nicolet
instance_of: Lake
countries: Canada
coordinates: lat: 45.83
lon: -71.5603
surface_form: nicolet
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.255
lon: -72.6525
surface_form: nicolet
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.255
lon: -72.6525
Lake Nicolet. Note: not to be confused with another &quot;Lake Nicolet&quot;, in Michigan (USA), on the St. Marys River (Michigan–Ontario) which links Lake Superior with Lake Huron.

Geographic entities mentioned:
surface_form: lake nicolet
instance_of: Lake
countries: Canada
coordinates: lat: 45.83
lon: -71.5603
surface_form: nicolet
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.255
lon: -72.6525
Lawrence River. This lake is surrounded by Chemin du Lac-Nicolet (north-west side) and Chemin Gosford-Sud (south-east side). The lake takes its name from Jean Nicolet (1598 - 1642), a French explorer at the time of New France who is known to have been the first European to explore Lake Michigan. Geography. Lake Nicolet is long and wide, resembling a misshapen crescent surrounded by mountains.

Geographic entities mentioned:
surface_form: nicolet
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.255
lon: -72.6525
surface_form: nicolet
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.255
lon: -72.6525
The latest is crossed through the North-East by the St. Lawrence River. This lake is surrounded by Chemin du Lac-Nicolet (north-west side) and Chemin Gosford-Sud (south-east side). The lake takes its name from Jean Nicolet (1598 - 1642), a French explorer at the time of New France who is known to have been the first European to explore Lake Michigan. Geography.

Geographic entities mentioned:
surface_form: nicolet
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.255
lon: -72.6525
Lake Nicolet is long and wide, resembling a misshapen crescent surrounded by mountains. It has seven islands: Boulanger, Baril, Linke, L'Heureux, à Michel-Rheault, Rolland and a little unnamed island. The main mountain peaks around the lake are: Brûlé Mountain () at on the south side of the bay leading to the mouth of the lake; a vertex on the west side and another on the southeast side ().

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
It has seven islands: Boulanger, Baril, Linke, L'Heureux, à Michel-Rheault, Rolland and a little unnamed island. The main mountain peaks around the lake are: Brûlé Mountain () at on the south side of the bay leading to the mouth of the lake; a vertex on the west side and another on the southeast side (). This lake has a hundred chalets all around. Toponymy.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Improvements include more realistic chipping, better Internet support, and additional options for customization. The game features seven courses, including the following four from the previous game: The Links, and Teeth of the Dog, both at Casa de Campo in the Dominican Republic; and Lake Michigan's Bay Harbor Golf Club, and The Preserve 9 at Bay Harbor.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Pilgrimage to this area was off-limits to Jews from 1948 to 1967, when East Jerusalem was under Jordanian control. There are numerous lesser Jewish pilgrimage destinations, mainly tombs of &quot;tzadikim&quot;, throughout Israel and Palestine and all over the world, including: Hebron; Bethlehem; Mount Meron; Netivot; Uman, Ukraine; Silistra, Bulgaria; Damanhur, Egypt; and many others.

Geographic entities mentioned:
surface_form: Mount Meron
instance_of: Mountain
countries: Mandatory Palestine
Israel
Ottoman Empire
coordinates: lat: 32.9975
lon: 35.41222222222222
When the exhibit left Philadelphia on September 30, 2007, it traveled to London. This exhibit was nearly twice the size of the original Tutankhamun exhibit of the 1970s, and contained 50 objects directly from Tut's tomb, as well as nearly 70 object from the tombs of his ancestors in The Valley of the Kings. The show also featured a CAT Scan that revealed what the Boy King may have looked like.

Geographic entities mentioned:
surface_form: Valley of the Kings
instance_of: Valley
countries: Egypt
coordinates: lat: 25.74025
lon: 32.602358
Despite the consensus of the major nobles of the Empire to support Salomon, &quot;Azaj&quot; Salassie Barya brought Tekle Giyorgis from the royal prison on Wehni as a pretender to the throne. Salomon responded by marching out from Gondar; Tekle Giyorgis then fled to Tigray, whence he emerged in the month of Sane at the head of an army which was rumored to be &quot;a large force&quot;.

Geographic entities mentioned:
surface_form: Wehni
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 12.148333333333
lon: 37.766388888889
Transcaspian Oblast. The Transcaspian Oblast, or simply Transcaspia, was an oblast of the Russian Empire and early Soviet Russia to the east of the Caspian Sea during the second half of the 19th century until 1924.

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
History. Transcaspia was conquered by Russia in 1879&ndash;1885, in a series of campaigns led by Generals Nikolai Lomakin, Mikhail Skobelev, and Mikhail Annenkov. The construction of the Transcaspian Railway was started from the shores of the Caspian in 1879 in order to secure Russian control over the region and provide a rapid military route to the Afghan border.

Geographic entities mentioned:
surface_form: Caspian
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Wannian Temple (Mount Emei). Wannian Temple () is a Buddhist temple located at the foot of Camel Mountain Range of Mount Emei, in Emeishan City, Sichuan, China. It is one of the six earliest Buddhist temples on Mount Emei. The temple is situated at the foot of Camel Mountain Range, facing the Daping Temple (), Niuxin Temple (), Shisun Summit () and Bomeng Summit () in the front.

Geographic entities mentioned:
surface_form: Mount Emei
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 29.519722222222
lon: 103.3325
Natasha Baig. Natasha Baig (), also spelled Nata-sha Baig is a Pakistani singer-songwriter from Hunza Valley. She sings in various genres including Sufi rock and had her latest hit with the Burushaski language song &quot;Ya Maula&quot; in collaboration with the designer Yousuf B. Qureshi. Early life. Natasha Baig was born and raised in Karachi, but her family home is in Hunza. Career.

Geographic entities mentioned:
surface_form: Hunza Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.31666667
lon: 74.65
Situated on the Gulf of Tunis, behind the Lake of Tunis and the port of La Goulette (Ḥalq il-Wād), the city extends along the coastal plain and the hills that surround it. At its core lies the Medina, a World Heritage Site.

Geographic entities mentioned:
surface_form: Lake of Tunis
instance_of: Lake
countries: Tunisia
coordinates: lat: 36.816666666667
lon: 10.25
Geography. Tunis is located in north-eastern Tunisia on the Lake of Tunis, and is connected to the Mediterranean sea's Gulf of Tunis by a canal which terminates at the port of La Goulette/Halq al Wadi. The ancient city of Carthage is located just north of Tunis along the coastal part. The city lies on a similar latitude as the southernmost points of Europe.

Geographic entities mentioned:
surface_form: Lake of Tunis
instance_of: Lake
countries: Tunisia
coordinates: lat: 36.816666666667
lon: 10.25
Urban landscape. The Medina, built on a gentle hill slope on the way down to the Lake of Tunis, is the historical heart of the city and home to many monuments, including palaces, such as the Dar Ben Abdallah and Dar Hussein, the mausoleum of Tourbet el Bey and many mosques such as the Al-Zaytuna Mosque.

Geographic entities mentioned:
surface_form: Lake of Tunis
instance_of: Lake
countries: Tunisia
coordinates: lat: 36.816666666667
lon: 10.25
Except for small areas, the Dresden Heath is considered part of the western Lusatian Highlands and, consequently, is one of the westernmost parts of the Sudetes. Though the rocky subsoil of the forest was raised during the tectonic formation of the Dresden Basin, the mixed woodland of the heath is largely characterized by dune-like sand deposits of the Wolstonian Stage and Elster glaciation.

Geographic entities mentioned:
surface_form: Dresden Basin
instance_of: Valley
countries: Germany
Smaller regions on the edge of the heath belong to the administrative districts of Neustadt and Klotzsche, as well as to the town of Radeburg. In the south, the main part of the heath stretches between Loschwitz and the Waldschlösschen district, to the slopes of the Elbe and to Radeberger Vorstadt. The southernmost offshoots even border on the heavily populated Äussere Neustadt.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Surrounding landscapes include Lößnitz in the West, the Friedewald and the Moritzburg pond region in the northwest. In the north, the Königsbrück-Ruhland Heaths and the Seifersdorf valley border the forest in the northeast. The landscape to the southeast is the Schönfeld Upland. On the southern border of the Heide, the forest segues into the park and garden landscape of the Dresden Elbe valley.

Geographic entities mentioned:
surface_form: Schönfeld Upland
instance_of: Plateau
countries: Germany
coordinates: lat: 51.0417
lon: 13.8958
According to the account of Dionysius of Halicarnassus, the city would have been founded by Aeneas' son Ascanius thirty years after the founding of Lavinium, &quot;near a mountain and a lake, occupying the space between the two.&quot; Although the archaeologist Antonio Nibby placed the site of the city on the eastern side of Lake Albano, between the localities of Costa Caselle near Marino and Pozzo Carpino in the municipality of Grottaferrata, at the foot of Monte Cavo, the most substantial archaeological remains have been found on the southern side of the lake, between the Colle dei Cappuccini and the convent of Santa Maria ad Nives of Palazzolo in the municipality of Rocca di Papa.

Geographic entities mentioned:
surface_form: Monte Cavo
instance_of: Mountain
countries: Italy
coordinates: lat: 41.751666666667
lon: 12.71
The Alban Hills still retained some religious importance, due to the existence of the important shrines of Latian Jupiter on Monte Cavo, Diana Aricina near present-day Nemi, and Juno Sospita in Lanuvio, as well as the permanence of the surviving Albano priestly congregations in Bovillae, which from then on boasted of having succeeded Alba Longa as the Latin religious capital.

Geographic entities mentioned:
surface_form: Monte Cavo
instance_of: Mountain
countries: Italy
coordinates: lat: 41.751666666667
lon: 12.71
During the war between Pope Eugene IV and the Colonna family, in October 1434 the papal commander Orsino Orsini pressed the rebel army led by the mercenary captain Antonio da Pontedera as far as below the Borghetto di Grottaferrata, Marino and Albano, the first and last castles hospitable to the rebel because they were owned by the Savelli family, allies of the Colonna family who instead ruled Marino: Cardinal Giovanni Maria Vitelleschi, commander-in-chief of the papal army, reconquered Rome (from which the pope had been driven out) on October 25, and on March 31, 1436 arrived at the Borghetto di Grottaferrata, which was destroyed: Then, the cardinal passed by Marino without assaulting it and raided the Savelli fiefdoms along the Appian Way, namely Castel Gandolfo, Albano and Castel Savello, razing them to the ground: passing through Rocca Priora he then broke the delay and attacked the Colonna family directly in the Valle Latina.

Geographic entities mentioned:
surface_form: Valle Latina
instance_of: Valley
countries: Italy
coordinates: lat: 41.5744
lon: 13.3511
Pope Pius II wanted to visit the archaeological ruins visible in Albano in the properties of the Abbey of St. Paul during his trip to the Alban Hills in 1462: other stops were Genzano di Roma, the convent of Santa Maria ad Nives of Palazzolo and Monte Cavo.

Geographic entities mentioned:
surface_form: Monte Cavo
instance_of: Mountain
countries: Italy
coordinates: lat: 41.751666666667
lon: 12.71
Dyken Pond. Dyken Pond is a lake in the towns of Grafton and Berlin in Rensselaer County, New York. The pond gets water primarily from precipitation and outflows westward into the Poesten Kill, a tributary of the Hudson River. It is located in northwest Berlin, south of Grafton Lakes State Park. Dyken Pond is long with a shoreline length of; its maximum depth is with an average depth of.

Geographic entities mentioned:
surface_form: dyken pond
instance_of: Lake
countries: United States
coordinates: lat: 42.723333333333
lon: -73.425555555556
The pond gets water primarily from precipitation and outflows westward into the Poesten Kill, a tributary of the Hudson River. It is located in northwest Berlin, south of Grafton Lakes State Park. Dyken Pond is long with a shoreline length of; its maximum depth is with an average depth of. It sits at an elevation of.

Geographic entities mentioned:
surface_form: dyken pond
instance_of: Lake
countries: United States
coordinates: lat: 42.723333333333
lon: -73.425555555556
It sits at an elevation of. Formerly a small pond, Dyken Pond was enlarged to its current size in 1902 after a dam was built to regulate water power and reduce flooding. The dam was constructed by the Manning Paper Company, who later donated their land holdings in the vicinity of the pond to Rensselaer County in 1973.

Geographic entities mentioned:
surface_form: dyken pond
instance_of: Lake
countries: United States
coordinates: lat: 42.723333333333
lon: -73.425555555556
The dam was constructed by the Manning Paper Company, who later donated their land holdings in the vicinity of the pond to Rensselaer County in 1973. That land became part of the Dyken Pond Environmental Education Center, a property that is accessible to the public for the purpose of outdoor education and low-impact recreation.

Geographic entities mentioned:
surface_form: dyken pond
instance_of: Lake
countries: United States
coordinates: lat: 42.723333333333
lon: -73.425555555556
Majadita. Cumbre de la Majadita is a mountain peak in the province of San Juan in Argentina near the town of Rodeo. It was one of the last 6000m+ peaks in the Andes to be climbed, the first recorded ascent being in December 1996. The peak has some large but easy angled glaciers on its flanks.

Geographic entities mentioned:
surface_form: majadita
instance_of: Mountain
countries: Argentina
coordinates: lat: -30.41667
lon: -69.73333
The trip took at least three hours for the uninitiated, whether they were traveling from Kuala Belait or the capital. Provided with greenery along the journey in the form of forest trees of different sizes, and occasionally coming across little houses constructed by the people. The summit of Mount Mulu, which can be seen from Kampong Melilas as the car ascends the mountainous route.

Geographic entities mentioned:
surface_form: Mount Mulu
instance_of: Mountain
countries: Malaysia
coordinates: lat: 4.05
lon: 114.933
Battle of Vesuvius. The Battle of Vesuvius (also known as the Battle of the Veseris) was the first recorded battle of the Latin War. The battle was fought near Mount Vesuvius in 340 BC between the Romans, with their allies the Samnites, against a coalition of several peoples: Latins, Campanians, Volsci, Sidicini, and Aurunci.

Geographic entities mentioned:
surface_form: Mount Vesuvius
instance_of: Mountain
countries: Italy
coordinates: lat: 40.821388888889
lon: 14.425555555556
Store Kvitingskjølen. Store Kvitingskjølen is the highest peak on the mountain Kvitingskjølen located on the northern edge of Jotunheimen, in Lom municipality in Innlandet, Norway. It has a height of 2,064 meters. &quot;Vestre Kvitingskjølen&quot; is another peak with a height of 2,060 meters above sea level. Two peaks separated by a shallow saddle.

Geographic entities mentioned:
surface_form: Kvitingskjølen
instance_of: Mountain
countries: Norway
coordinates: lat: 61.76666667
lon: 8.8
surface_form: store kvitingskjølen
instance_of: Mountain
These ridges are separated by streams that have carved deep ravines on the lower slopes. Due to the fact that Kvitingskjølen is rounded, it is less popular among tourists. The valley that divides it from the rest of Jotunheimen, Smådalen, is rich in wildlife, including wolverine. The valleys that surround Kvitingskjølen are also rich with old seters, a summer farms in the high pastures.

Geographic entities mentioned:
surface_form: rich
instance_of: Mountain
coordinates: lat: -79.7833
lon: 158.8
Due to the fact that Kvitingskjølen is rounded, it is less popular among tourists. The valley that divides it from the rest of Jotunheimen, Smådalen, is rich in wildlife, including wolverine. The valleys that surround Kvitingskjølen are also rich with old seters, a summer farms in the high pastures. Many of these seters are still in use. Several hiking routes lead to the Store Kvitingskjølen.

Geographic entities mentioned:
surface_form: rich
instance_of: Mountain
coordinates: lat: -79.7833
lon: 158.8