Sarmila/GeoWiki-Features huggingface dataset:
Mount Pleasant Caldera. The Mount Pleasant Caldera is a large eroded Late Devonian volcanic caldera complex, located in the northern Appalachian Mountains of southwestern New Brunswick, Canada. It is one of few noticeable pre-Cenozoic calderas, and its formation is associated to a period of crustal thinning that followed the Acadian orogeny in the northern Appalachian Mountains.

Geographic entities mentioned:
surface_form: mount pleasant caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 45.7378
lon: -67.3306
The volcanic necks are defined by magmatic-hydrothermal breccias. Eruptive history. The eruptive history of the Mount Pleasant Caldera can be divided into three stages of activity: the exocaldera sequence, the intracaldera sequence, and the late caldera-fill sequence. These can further be subdivided into strata based on their depth below the surrounding rock.

Geographic entities mentioned:
surface_form: mount pleasant caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 45.7378
lon: -67.3306
On September 25, 2005, the Society of Economic Geologists hosted a small field trip to the caldera and the nearby Mount Pleasant Mine and Clarence stream deposit. The trip was divided into three stages: the Mount Pleasant Caldera, the Mount Pleasant Mine, and the Clarence Stream deposits.

Geographic entities mentioned:
surface_form: mount pleasant caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 45.7378
lon: -67.3306
Carrick, County Westmeath. Carrick is a townland in County Westmeath, Ireland. It lies within a civil parish of the same name. The N52 road cuts through the middle of the townland and Lough Ennell borders it to the west. Carrick House, an 18th-century country house historically linked to the Fetherston-Haugh family, is in the area.

Geographic entities mentioned:
surface_form: Lough Ennell
instance_of: Lake
countries: Ireland
coordinates: lat: 53.45
lon: -7.4166666666667
Egg rolling has been a tradition at Avenham Park for hundreds of years, but in recent years chocolate eggs have been used. Other traditional egg rolling sites are the castle moat at Penrith, Bunkers Hill in Derby, Arthur's Seat in Edinburgh, Hill 60 on the Beverley Westwood and on Penshaw Hill in Tyne and Wear at Penshaw Monument.

Geographic entities mentioned:
surface_form: Arthur's Seat
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.944166666667
lon: -3.1619444444444
His Jesus painting resembles Pavias's painting &quot;Christ Pantocrator&quot;. All of his works are at Mount Athos in the Dionysiou Monastery. They decorate the iconostasis. Fragkos Katelanos and Theophanes the Cretan were also working at Mount Athos around the same period. History. Euphrosynos was born in Crete sometime in the 16th century. He was a priest.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
History. Euphrosynos was born in Crete sometime in the 16th century. He was a priest. The only information regarding his life remains in five icons. His icons are in the Dionysiou Monastery, Mount Athos, Greece. His style resembles Theophanes the Cretan. There are rumors within the historical community that he was a member of the Klontzas family.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
The type specimen was collected in the Cherangani Hills of Kenya's Rift Valley Province, growing on a tree near a rivulet in a densely wooded ravine at an elevation of approximately. Additional specimens have been collected from the slopes of Table Mountain in South Africa, particularly in Blinkwater Ravine where it was found growing on &quot;Eucalyptus&quot; trees.

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
The district also includes Big Diomede Island, sometimes called &quot;Tomorrow Island&quot; since it is twenty-one hours ahead of its partner Little Diomede, despite being only away across the sea. Lakes Koolen and Ioni are located in the district. History. For the indigenous peoples, life has been rather static for the last few millennia, judging from archaeological excavations.

Geographic entities mentioned:
surface_form: Ioni
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 65.9
lon: -173.65
Within Hamilton, the highway crossed a Canadian National Railway on an overpass before bisecting the community of Lynden and Copetown, intersecting Highway 52 in the latter. East of Copetown, the route descended the Niagara Escarpment, finally diverging from its otherwise straight path.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
He visits Minos father to express his desperation at the nearing end of the multi-ethnic Austrian Empire. Dressed in his parade uniform he leaves for the front on Monte Grappa as he does not want to survive the Empire. Mino and Nena arrive to find Freda leaving for Vienna. Mino quickly finds his father, as the Austrian guards already have deserted the prisoner of war camp.

Geographic entities mentioned:
surface_form: Monte Grappa
instance_of: Mountain
countries: Italy
coordinates: lat: 45.873333333333
lon: 11.799166666667
He has been injured while fighting with the 4 Alpini Regiment in the Battle of Monte Grappa. His right arm is amputated and when he regains consciousness he tells Mino about the last Austrian attacks on Monte Grappa: the Austrians led by a colonel in parade uniform attacked without ammunition and perished all. Mino understands thus that also Karl Stolz is dead.

Geographic entities mentioned:
surface_form: Monte Grappa
instance_of: Mountain
countries: Italy
coordinates: lat: 45.873333333333
lon: 11.799166666667
Ewell, and later commanded a corps. A key Confederate defender of the Shenandoah Valley, during the Valley campaigns of 1864, Early made daring raids to the outskirts of Washington, D.C., and as far as York, Pennsylvania, but was eventually pushed back by Union Army troops led by General Philip Sheridan, losing over half his forces.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Whitefoord House. Whitefoord House (or occasionally Whiteford House is an 18th-century former mansion on the Canongate section of the Royal Mile in Edinburgh. It stands on the north side of the Royal Mile obscured by more modern buildings, under a backdrop of Calton Hill. History.

Geographic entities mentioned:
surface_form: Calton Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.955278
lon: -3.182222
The division then attacked rapidly eastward, crossed the Rhine on March 27, 1945, and captured Leipzig in mid-April. On April 25, 1945, during the Allies' rapid advance into Germany and towards the end of World War II in Europe, elements of the 69th Division reached the Elbe and became the first American unit to come into contact with the Soviet Red Army.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
The feature is named after the town and region of Devol in medieval Southwestern Bulgaria. Location. The mountain is located at, which is 10.24 km south by east of Mount Wilbye, 8.7 km southwest of Mount Kliment Ohridski in Sofia University Mountains, 8.77 km west of Rachenitsa Nunatak, 2.7 km north by west of Moriseni Peak and 9.5 km east by north of Faulkner Nunatak.

Geographic entities mentioned:
surface_form: Mount Wilbye
instance_of: Mountain
coordinates: lat: -69.5
lon: -71.5333
surface_form: Mount Kliment Ohridski
instance_of: Mountain
coordinates: lat: -69.517777777778
lon: -71.391666666667
surface_form: Moriseni Peak
instance_of: Mountain
coordinates: lat: -69.609166666667
lon: -71.470833333333
surface_form: Faulkner Nunatak
instance_of: Mountain
coordinates: lat: -69.6
lon: -71.7
Boundaries. The limits of the plateau are easily definable. The southern boundary is marked by the Berlin Valley, through which the River Spree flows. To the west, the boundary between Barnim and the Glien Plateau is marked by a north–south glacial valley. To the north and north east is the boundary with the Eberswald Valley, and in the east, Lubusz Land. Subdivision.

Geographic entities mentioned:
surface_form: Glien Plateau
instance_of: Plateau
countries: Germany
surface_form: barnim
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
Boundaries. The limits of the plateau are easily definable. The southern boundary is marked by the Berlin Valley, through which the River Spree flows. To the west, the boundary between Barnim and the Glien Plateau is marked by a north–south glacial valley. To the north and north east is the boundary with the Eberswald Valley, and in the east, Lubusz Land. Subdivision.

Geographic entities mentioned:
surface_form: Lubusz Land
instance_of: Plateau
countries: Germany
Poland
Kingdom of Poland
Lands of the Bohemian Crown
Watershed. The principal drainage divide between the North Sea and the Baltic Sea runs across the Barnim plateau from Northeast to Southwest. It also runs between the drainage basins of the Elbe and Oder rivers. Its course roughly follows that of the Frankfurt push moraine. The main features along the divide include the Wandlitzer See and the Liepnitzsee. Lakes.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
It also runs between the drainage basins of the Elbe and Oder rivers. Its course roughly follows that of the Frankfurt push moraine. The main features along the divide include the Wandlitzer See and the Liepnitzsee. Lakes. Despite being an area of Young Drift, Barnim has relatively few lakes.

Geographic entities mentioned:
surface_form: Wandlitzer See
instance_of: Lake
countries: Germany
coordinates: lat: 52.75
lon: 13.449722222222
surface_form: Liepnitzsee
instance_of: Lake
countries: Germany
coordinates: lat: 52.75
lon: 13.516666666667
The main features along the divide include the Wandlitzer See and the Liepnitzsee. Lakes. Despite being an area of Young Drift, Barnim has relatively few lakes. At the outwash plain, the deposition of glacio-fluvial sediment has led to a higher number of lakes, the most well-known of which are Wandlitzer See, Gamensee and Straussee. Climate.

Geographic entities mentioned:
surface_form: Wandlitzer See
instance_of: Lake
countries: Germany
coordinates: lat: 52.75
lon: 13.449722222222
surface_form: Straussee
instance_of: Lake
countries: Germany
coordinates: lat: 52.582608333333
lon: 13.875819444444
Due to the height of Barnim, the Oderbruch, which lies to the east and is on average 100 metres lower than Barnim, is in a rain shadow. This is compounded by the height of other surrounding areas such as Lubusz Land and Chorin. Whereas Barnim receives relatively high amounts of precipitation, the Oderbruch receives less than 500mm annually and is one of the driest regions in Germany.

Geographic entities mentioned:
surface_form: Lubusz Land
instance_of: Plateau
countries: Germany
Poland
Kingdom of Poland
Lands of the Bohemian Crown
Subdivision. Traditionally the plateau is divided into the Upper and Lower Barnim, separated by a line running between Strausberg and Eberswalde. Typically, Lower Barnim does not reach higher than 80 metres above mean sea level (AMSL) whereas Upper Barnim is generally more than 100 metres AMSL. The highest point of the plateau is Semmelberg which stands at 157 metres AMSL. Settlements.

Geographic entities mentioned:
surface_form: semmelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 52.7413
lon: 13.9621
Barnim Plateau. rag4pg9f5mukihaa94qn81sgv8j71n" xml:space="preserve">The Barnim Plateau is a plateau which is occupied by the northeastern parts of Berlin and the surrounding federal state of Brandenburg in Germany. Boundaries. The limits of the plateau are easily definable. The southern boundary is marked by the Berlin Valley, through which the River Spree flows.

Geographic entities mentioned:
surface_form: barnim
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
Last Glacial Period. In the last glacial period, more commonly known as the last time the Earth experienced an ice age, glaciers reached 60 kilometres south of Barnim. Watershed. The principal drainage divide between the North Sea and the Baltic Sea runs across the Barnim plateau from Northeast to Southwest. It also runs between the drainage basins of the Elbe and Oder rivers.

Geographic entities mentioned:
surface_form: barnim
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
To the north and north east is the boundary with the Eberswald Valley, and in the east, Lubusz Land. Subdivision. Traditionally the plateau is divided into the Upper and Lower Barnim, separated by a line running between Strausberg and Eberswalde. Typically, Lower Barnim does not reach higher than 80 metres above mean sea level (AMSL) whereas Upper Barnim is generally more than 100 metres AMSL.

Geographic entities mentioned:
surface_form: barnim
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
Subdivision. Traditionally the plateau is divided into the Upper and Lower Barnim, separated by a line running between Strausberg and Eberswalde. Typically, Lower Barnim does not reach higher than 80 metres above mean sea level (AMSL) whereas Upper Barnim is generally more than 100 metres AMSL. The highest point of the plateau is Semmelberg which stands at 157 metres AMSL. Settlements.

Geographic entities mentioned:
surface_form: barnim
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
surface_form: barnim
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
The highest point of the plateau is Semmelberg which stands at 157 metres AMSL. Settlements. Until the growth of Berlin in the 19th century, Barnim was only sparsely populated; in the eastern portion this continues to be the case. Excluding Berlin, only Bernau and Strausberg are the only settlements with more than 10,000 inhabitants.

Geographic entities mentioned:
surface_form: barnim
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
Bedrock Deposits. The southern edge of Barnim in the vicinity of Rüdersdorf unusually contains widespread deposits of limestone, Buntsandstein and Muschelkalk. The relatively high position of the limestone in the bedrock is explained by the presence of a salt dome; the migrating salt pushed the overlying sedimentary rock closer to the surface.

Geographic entities mentioned:
surface_form: barnim
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
They are particularly prominent in tunnel valleys. Kansan sediment primarily consists of till and deposits in proglacial lakes. Thanks to superposition with Wolstonian Stage sediment, it is generally only found at the surface in isolation around the Oderbruchrand area. Generally, present-day Barnim there is very little surface evidence of the Kansan period remaining. Wolstonian Stage.

Geographic entities mentioned:
surface_form: barnim
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
Wolstonian Stage. Only the two primary glacial motions of the Wolstonian Stage allowed the plateau to clearly emerge. Geologically, Barnim is composed mostly of deposits from the more recent Warthe Motion which extends as far as Fläming Heath. The till associated with the Wolstonian stage can be found on the surface or within a few metres of it in many places.

Geographic entities mentioned:
surface_form: barnim
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
The main features along the divide include the Wandlitzer See and the Liepnitzsee. Lakes. Despite being an area of Young Drift, Barnim has relatively few lakes. At the outwash plain, the deposition of glacio-fluvial sediment has led to a higher number of lakes, the most well-known of which are Wandlitzer See, Gamensee and Straussee. Climate.

Geographic entities mentioned:
surface_form: barnim
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
Climate. As in the rest of the region, Barnim is located in the transition zone between the oceanic climate of Western Europe and the continental climate of Eastern Europe. Due to the relatively small height differential between Upper and Lower Barnim there is little difference between the climates of the two areas.

Geographic entities mentioned:
surface_form: barnim
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
The coldest month is January with an average temperature of -1 °C and the warmest is July, with an average temperature of 18 °C. The averages for Upper Barnim are marginally lower. The average annual precipitation for Lower Barnim is 550mm whereas in Upper Barnim it is 600mm.

Geographic entities mentioned:
surface_form: barnim
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
The averages for Upper Barnim are marginally lower. The average annual precipitation for Lower Barnim is 550mm whereas in Upper Barnim it is 600mm. Due to the height of Barnim, the Oderbruch, which lies to the east and is on average 100 metres lower than Barnim, is in a rain shadow. This is compounded by the height of other surrounding areas such as Lubusz Land and Chorin.

Geographic entities mentioned:
surface_form: barnim
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
surface_form: barnim
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
This is compounded by the height of other surrounding areas such as Lubusz Land and Chorin. Whereas Barnim receives relatively high amounts of precipitation, the Oderbruch receives less than 500mm annually and is one of the driest regions in Germany. Paleolithic Age. There is evidence of settlement in Barnim at the time of the Allerød oscillation.

Geographic entities mentioned:
surface_form: barnim
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
Whereas Barnim receives relatively high amounts of precipitation, the Oderbruch receives less than 500mm annually and is one of the driest regions in Germany. Paleolithic Age. There is evidence of settlement in Barnim at the time of the Allerød oscillation. Hunter-gatherers mainly followed the courses of rivers, confirmed by archaeological discoveries north of Berlin.

Geographic entities mentioned:
surface_form: barnim
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
Around 6000 years ago the first permanent agricultural settlements were established. Discoveries of sickles and troughs from the Bronze Age have been discovered in the west of Barnim. The Germanic Semnones tribe settled in Barnim, and after their migration the Slavic stem of the Sprevane tribe followed in the 6th and 7th centuries and settled near Biesenthal and Wandlitz. Settlement since 1230.

Geographic entities mentioned:
surface_form: barnim
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
Settlement since 1230. While the Slavic peoples tended to settle in lowland parts of Barnim near the relatively few areas, subsequent settlement of the plateau began in the 1230s by the House of Ascania under the rules of John I, Margrave of Brandenburg and Otto III, Margrave of Brandenburg as part of the German eastward expansion.

Geographic entities mentioned:
surface_form: barnim
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
Further settlement was also carried out under the House of Wettin, part of the Margravate of Meissen. The Wettiners expanded from the south with castles in Mittenwalde and Köpenick in Lower Barnim, whereas the Ascaniers expanded over the northern parts of Upper Barnim from Oranienburg to Strausberg.

Geographic entities mentioned:
surface_form: barnim
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
surface_form: barnim
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
They are amongst the most significant medieval buildings in the region. Thirty Years' War. After the Thirty Years' War a migration wave, mainly of Dutch colonists, arrived on Barnim. As with medieval settlement this was mainly confined to the areas along the rivers of Barnim.

Geographic entities mentioned:
surface_form: barnim
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
Thirty Years' War. After the Thirty Years' War a migration wave, mainly of Dutch colonists, arrived on Barnim. As with medieval settlement this was mainly confined to the areas along the rivers of Barnim. At the end of the 19th century the industrial revolution in Germany resulted in strong population growth in Berlin, which expanded into the plateau.

Geographic entities mentioned:
surface_form: barnim
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
The Wettiners expanded from the south with castles in Mittenwalde and Köpenick in Lower Barnim, whereas the Ascaniers expanded over the northern parts of Upper Barnim from Oranienburg to Strausberg. Conflicts over the question of territorial sovereignty contributed to the Teltow and Magdeburg Wars between 1239 and 1245 which were won by the Ascaniers.

Geographic entities mentioned:
surface_form: teltow
instance_of: Plateau
countries: Germany
coordinates: lat: 52.3667
lon: 13.3333
on 15 February. The pillars glowed bright red and exploded; the outer walls shattered and nearly 6,000 tons of stone plunged to earth, penetrating the massive floor as it fell. The altar, a relief depiction of Jesus' Agony in the Garden of Gethsemane on the Mount of Olives by Johann Christian Feige, was only partially damaged during the bombing raid and fire that destroyed the church.

Geographic entities mentioned:
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
Potapoco. The Potapoco were a tribe of Native Americans living in southern Maryland at the time of English colonization in the 17th century. The Potapoca were among the Atlantic coastal tribes speaking Algonquian languages, and they inhabited the area along what the English colonists later called the Port Tobacco River. They called their settlement Potopaco.

Geographic entities mentioned:
surface_form: Port Tobacco River
instance_of: Landform
countries: United States
coordinates: lat: 38.457777777778
lon: -77.035
In his 1829 treatise &quot;Recherches sur le traitement du cancer&quot;, he coined the term &quot;metastasis&quot; as a definition for the spread of cancer. &quot;Récamier's operation&quot; is a term used for curettage of the uterus. Honors. Mont Docteur Récamier, the highest point of the Joffre Peninsula in Kerguelen was named by cartographer Raymond Rallier du Baty in his honor.

Geographic entities mentioned:
surface_form: Mont Docteur Récamier
instance_of: Mountain
countries: France
coordinates: lat: -49.0992
lon: 69.3928
Skilfonna. Skilfonna (&quot;The Divide Glacier&quot;) is a glacier in Sørkapp Land at Spitsbergen, Svalbard. It is located west of Russefjella, and separates the glacier of Hedgehogfonna from Vasil'evbreen. The mountains of Brendetoppane separate Skilfonna from Svalisbreen.

Geographic entities mentioned:
surface_form: Brendetoppane
instance_of: Mountain
countries: Norway
coordinates: lat: 76.9225
lon: 16.8273
Fence Lake (Wisconsin). Fence Lake is a 3,483 acre lake in Vilas County, Wisconsin. The communities of Marlands and Lac du Flambeau border the lake. The fish present in the lake are Muskellunge, Panfish, Largemouth Bass, Smallmouth Bass, Northern Pike, Trout and Walleye.

Geographic entities mentioned:
surface_form: fence lake (wisconsin)
instance_of: Lake
countries: United States
coordinates: lat: 45.950833333333
lon: -89.839444444444
Fence Lake (Wisconsin). Fence Lake is a 3,483 acre lake in Vilas County, Wisconsin. The communities of Marlands and Lac du Flambeau border the lake. The fish present in the lake are Muskellunge, Panfish, Largemouth Bass, Smallmouth Bass, Northern Pike, Trout and Walleye.

Geographic entities mentioned:
surface_form: fence lake
instance_of: Lake
countries: United States
coordinates: lat: 45.950833333333
lon: -89.839444444444
Lobsang Tshering. Lopsang Tshering Bhutia (1951/1952&ndash;10 May 1993) was an Indian Sherpa mountaineer who died on Mount Everest and the nephew of Tenzing Norgay. His death made international headlines because he died on the 40th anniversary expedition of his uncle's summiting. His uncle, Tenzing Norgay, had died at home of natural causes in 1986 at the age of 72.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Origin. According to Hans Dietrich Lang, a steep gorge with a tunnel mouth hole in the Peißenberg coal district, near Peißenberg, served as the set. Spitzweg often stayed in Peißenberg; it was during a spa stay in 1833, that he made the decision to become a painter. According to Erika Günter, this rock motif is the entrance to a shaft of Mt. Hoher Peißenberg. Description.

Geographic entities mentioned:
surface_form: Hoher Peißenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 47.800961111111
lon: 11.013244444444
Hartshead Pike. Hartshead Pike is a hill in Tameside in Greater Manchester, England, and its name is associated with the monument on its summit. It overlooks Ashton-under-Lyne, Mossley, Saddleworth, Lees and Oldham. On a clear day you can get views of Manchester, Cheshire and Snowdonia in Wales. Hartshead Pike Tower has been a Grade II listed building since 1967. History.

Geographic entities mentioned:
surface_form: hartshead pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.5183
lon: -2.0609
It overlooks Ashton-under-Lyne, Mossley, Saddleworth, Lees and Oldham. On a clear day you can get views of Manchester, Cheshire and Snowdonia in Wales. Hartshead Pike Tower has been a Grade II listed building since 1967. History. During the Roman occupation of Britain, a warning beacon for local garrisons, possibly lit during times of unrest, may have been sited on Hartshead Pike.

Geographic entities mentioned:
surface_form: hartshead pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.5183
lon: -2.0609
Hartshead Pike Tower has been a Grade II listed building since 1967. History. During the Roman occupation of Britain, a warning beacon for local garrisons, possibly lit during times of unrest, may have been sited on Hartshead Pike. Local trackways were routes for the Romans to access the Roman road at Limeside. The name refers to the hill and the tower.

Geographic entities mentioned:
surface_form: hartshead pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.5183
lon: -2.0609
Flimspitz. Flimspitz (2,929 m) is a mountain of the Samnaun Alps, located on the border between Switzerland and Austria. It lies on the range between the Greitspitz and the Bürkelkopf. From the Flimjoch a trail leads to the summit of the mountain.

Geographic entities mentioned:
surface_form: Greitspitz
instance_of: Mountain
countries: Switzerland
Austria
coordinates: lat: 46.97027778
lon: 10.33416667
surface_form: Bürkelkopf
instance_of: Mountain
countries: Switzerland
Austria
coordinates: lat: 46.98947
lon: 10.34752
Flimspitz. Flimspitz (2,929 m) is a mountain of the Samnaun Alps, located on the border between Switzerland and Austria. It lies on the range between the Greitspitz and the Bürkelkopf. From the Flimjoch a trail leads to the summit of the mountain.

Geographic entities mentioned:
surface_form: flimspitz
instance_of: Mountain
countries: Switzerland
Austria
coordinates: lat: 46.98222222
lon: 10.34388889
Its actual summit is in Bavaria. Sometimes its main peak is also called Schwabenhimmel. On the Heidelstein are the Heidelstein Transmitter and a memorial of the Rhön Club. On the northwestern slopes is the source of the River Ulster and on the western mountainside is the Rotes Moor Cross Country Skiing Centre.

Geographic entities mentioned:
surface_form: schwabenhimmel
instance_of: Mountain
countries: Germany
coordinates: lat: 50.458611111111
lon: 10.006666666667
Heidelstein. The Heidelstein, between Bischofsheim an der Rhön in the Bavarian county of Rhön-Grabfeld and Wüstensachsen in the Hessian county of Fulda, is a mountain, high, on the state border in the mountains of the High Rhön, part of the German Central Upland range of Rhön. Its actual summit is in Bavaria. Sometimes its main peak is also called Schwabenhimmel.

Geographic entities mentioned:
surface_form: heidelstein
instance_of: Mountain
countries: Germany
coordinates: lat: 50.458611111111
lon: 10.006666666667
Its actual summit is in Bavaria. Sometimes its main peak is also called Schwabenhimmel. On the Heidelstein are the Heidelstein Transmitter and a memorial of the Rhön Club. On the northwestern slopes is the source of the River Ulster and on the western mountainside is the Rotes Moor Cross Country Skiing Centre.

Geographic entities mentioned:
surface_form: heidelstein
instance_of: Mountain
countries: Germany
coordinates: lat: 50.458611111111
lon: 10.006666666667
surface_form: heidelstein
instance_of: Mountain
countries: Germany
coordinates: lat: 50.458611111111
lon: 10.006666666667
Salmon Lake (Alaska). Salmon Lake (native name, Nahwazuk, meaning &quot;salmon&quot;) is a natural lake on the Seward Peninsula in the U.S. state of Alaska. Situated north of Cape Nome, it drains into Port Clarence through Kruzgamepa River. The lake lies at the foot of the Kigluaik Mountains at an elevation of about. It has a water surface area of and a drainage area of.

Geographic entities mentioned:
surface_form: salmon lake
instance_of: Lake
countries: United States
coordinates: lat: 43.946388888889
lon: -74.940277777778
surface_form: salmon lake
instance_of: Lake
countries: United States
coordinates: lat: 64.9028
lon: -165.009
The lake lies at the foot of the Kigluaik Mountains at an elevation of about. It has a water surface area of and a drainage area of. Its principal supply comes from Grand Central River, which enters it at its western end. A number of small streams also enter the lake from both the north and the south; Fox Creek and Jasper Creek are the most notable of these.

Geographic entities mentioned:
surface_form: fox creek
instance_of: Watercourse
countries: United States
coordinates: lat: 36.5250649
lon: -93.0971222
Under the influence of Tendai Buddhism and Shugendō, the gongen concept was adapted to religious beliefs tied to Mount Iwaki, a volcano, so that female kami Kuniyasutamahime became associated with Avalokiteśvara &quot;ekadaśamukha&quot; (Jūichimen Kannon Bosatsu, &quot;Eleven-Faced Guanyin&quot;), Ōkuninushi with Bhaisajyaguru (Yakushi Nyōrai) and Kuninotokotachi with Amitābha (Amida Nyōrai).

Geographic entities mentioned:
surface_form: Mount Iwaki
instance_of: Mountain
countries: Japan
coordinates: lat: 40.653333
lon: 140.306667
The street was once important for both road and public transportation, but today sections of it form a pedestrian zone shared with Zurich's trams, effectively forming a northern extension of the &quot;Seeuferanlage&quot; promenades that ring the shores of Lake Zurich.

Geographic entities mentioned:
surface_form: Lake Zurich
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2475
lon: 8.6775
KFSQ. KFSQ (1270 AM) is a radio station broadcasting a sports talk format. Licensed to Thousand Palms, California, United States, it serves the Coachella Valley and is also streamed via TuneIn. The station is owned by KGAY PSP, a California Benefit Corporation with Bradley Fuhr as CEO. The station is managed by Brian Arrington. History.

Geographic entities mentioned:
surface_form: Coachella Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.72
lon: -116.2
He replaced Bougainville at the bureau des longitudes on 28 October 1811. Also in 1811 he was made president of the council on naval architecture and in 1813 he, Tarbé (inspector of bridges and roads) and Beautemps-Beaupré were commanded to choose the site for a new naval arsenal at the mouth of the Elbe.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
The village has a population of around 3,500 inhabitants, according to the 1998 census. Geography. Pakkora is connected to the Hunza Valley via the Naltar pass from its northeastern side while annexed to the Pamir mountain range to the northwest. The village is sandwiched between the Hindukush and the great Karakorum mountain ranges. It has a diverse weather pattern.

Geographic entities mentioned:
surface_form: Hunza Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.31666667
lon: 74.65
surface_form: Naltar
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.16531026078764
lon: 74.17856522268198
Nevertheless, Zoroastrianism continued to decline, and most Iranians had become Muslims by the 10th century, shifting the concentration of the religion's followers away from the Iranian plateau for the first time in recorded history.

Geographic entities mentioned:
surface_form: Iranian plateau
instance_of: Plateau
countries: Iran
coordinates: lat: 36.283333
lon: 59.05
According to adherents of the sect, they are followers of the Zoroastrian faith as preserved by a clan of 2000 individuals called the &quot;Saheb-e-Dilan&quot; ('Masters of the Heart') who are said to live in complete isolation in the mountainous recesses of the Caucasus (alternatively, in the Alborz range, around Mount Damavand).

Geographic entities mentioned:
surface_form: Mount Damavand
instance_of: Mountain
countries: Iran
coordinates: lat: 35.955277777778
lon: 52.109166666667
Fernhill railway station. Fernhill railway station serves the village of Fernhill in the Cynon Valley, Wales. It is located on the Aberdare branch of the Merthyr Line. Passenger services are provided by Transport for Wales. History. The station, along with the line to Aberdare, was opened by British Rail in 1988. Services.

Geographic entities mentioned:
surface_form: Cynon Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.657
lon: -3.461
Nance, Missouri. Nance is an extinct town in eastern Taney County, in the Ozarks of southwest Missouri. The GNIS classifies it as a populated place. The townsite sits above the east bank of the west fork of Big Creek about one mile north of U.S. Route 160 and about 1.7 miles west of the Taney - Ozark county line. The site is at an elevation of 876 feet. History.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
The northwest side drains into Ashley Hill Brook, thence Bash Bish Brook, the Roeliff Jansen Kill, the Hudson River, and Upper New York Bay. The northeast side drains into Sages Ravine, thence into Schenob Brook, the Hubbard Brook, the Housatonic River, and Long Island Sound. Mount Frissell is bordered by Round Mountain to the southeast, Mount Ashley to the north, and Brace Mountain to the west.

Geographic entities mentioned:
surface_form: Brace Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.044166666667
lon: -73.4925
surface_form: round mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0489
lon: -73.4764
surface_form: mount frissell
instance_of: Mountain
countries: United States
coordinates: lat: 42.050555555556
lon: -73.482222222222
Here the state line reaches to about. The high-point marker for Connecticut is on the border with Massachusetts at. (The highest mountain summit in Connecticut is Bear Mountain, about to the east-southeast of Mount Frissell. Mount Frissell is traversed by the Mount Frissell Trail, which connects with the South Taconic Trail to the west and the Appalachian Trail to the east.

Geographic entities mentioned:
surface_form: bear mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.7962
lon: -123.672
surface_form: bear mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.93041
lon: -121.34152
surface_form: mount frissell
instance_of: Mountain
countries: United States
coordinates: lat: 42.050555555556
lon: -73.482222222222
surface_form: bear mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.3134
lon: -84.648
Mount Frissell, which straddles the border of southwest Massachusetts and northwest Connecticut, is part of the Taconic Range. Frissell's south slopes include the highest point in Connecticut, a popular destination for highpointers. Frissell's summit and the majority of its slopes are within Massachusetts' Mount Washington State Forest. Its southern slopes are in Salisbury, Connecticut.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 47.5311964
lon: -123.2459807
Mount Frissell. Mount Frissell, which straddles the border of southwest Massachusetts and northwest Connecticut, is part of the Taconic Range. Frissell's south slopes include the highest point in Connecticut, a popular destination for highpointers. Frissell's summit and the majority of its slopes are within Massachusetts' Mount Washington State Forest.

Geographic entities mentioned:
surface_form: mount frissell
instance_of: Mountain
countries: United States
coordinates: lat: 42.050555555556
lon: -73.482222222222
(The highest mountain summit in Connecticut is Bear Mountain, about to the east-southeast of Mount Frissell. Mount Frissell is traversed by the Mount Frissell Trail, which connects with the South Taconic Trail to the west and the Appalachian Trail to the east. It passes by the Connecticut–Massachusetts–New York tri-state marker.

Geographic entities mentioned:
surface_form: mount frissell
instance_of: Mountain
countries: United States
coordinates: lat: 42.050555555556
lon: -73.482222222222
surface_form: mount frissell
instance_of: Mountain
countries: United States
coordinates: lat: 42.050555555556
lon: -73.482222222222
It passes by the Connecticut–Massachusetts–New York tri-state marker. The south side of Mount Frissell drains into Riga Lake and South Pond, then into Wachocostinook Brook, Salmon Creek, the Housatonic River, and Long Island Sound. The northwest side drains into Ashley Hill Brook, thence Bash Bish Brook, the Roeliff Jansen Kill, the Hudson River, and Upper New York Bay.

Geographic entities mentioned:
surface_form: mount frissell
instance_of: Mountain
countries: United States
coordinates: lat: 42.050555555556
lon: -73.482222222222
There is a dam at the lake outlet on the eastern shore a short distance south of Ciss Stream. Discharge through the dam flows down Caucomgomoc Stream through Black Pond and Chesuncook Lake to the West Branch Penobscot River at Ripogenus Gorge. White perch and yellow perch have largely replaced historic trout populations in the lake.

Geographic entities mentioned:
surface_form: Chesuncook Lake
instance_of: Lake
countries: United States
coordinates: lat: 45.987222222222
lon: -69.340833333333
surface_form: Ripogenus Gorge
instance_of: Landform
countries: United States
coordinates: lat: 45.8759
lon: -69.15
surface_form: west branch
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
surface_form: black pond
instance_of: Lake
countries: United States
coordinates: lat: 43.1307
lon: -73.5616
Caucomgomoc Lake. Caucomgomoc Lake is in the North Maine Woods at the corner of townships 6 and 7 in ranges 14 and 15. Loon Stream flows into the southern end of the lake from Loon Lake, Bear Pond, Big Hurd Pond, Little Hurd Pond, Bear Brook Pond, McDougal Pond, and tributaries from the southwest.

Geographic entities mentioned:
surface_form: loon lake
instance_of: Lake
countries: United States
coordinates: lat: 42.681175
lon: -83.358048
surface_form: loon lake
instance_of: Lake
countries: United States
coordinates: lat: 42.492777777778
lon: -77.566944444444
surface_form: loon lake
instance_of: Lake
countries: United States
coordinates: lat: 43.6794
lon: -73.8581
surface_form: loon lake
instance_of: Lake
countries: United States
coordinates: lat: 43.5958
lon: -123.844
surface_form: loon lake
instance_of: Lake
countries: United States
coordinates: lat: 48.0476
lon: -117.624
surface_form: bear pond
instance_of: Lake
countries: United States
coordinates: lat: 43.9581948
lon: -75.0025228
surface_form: loon lake
instance_of: Lake
countries: United States
coordinates: lat: 46.2
lon: -89.3
surface_form: loon lake
instance_of: Lake
countries: United States
coordinates: lat: 48.076
lon: -90.689
surface_form: bear pond
instance_of: Lake
countries: United States
coordinates: lat: 43.9202573
lon: -75.117371
surface_form: loon lake
instance_of: Lake
countries: United States
coordinates: lat: 47.096111111111
lon: -93.870833333333
Loon Stream flows into the southern end of the lake from Loon Lake, Bear Pond, Big Hurd Pond, Little Hurd Pond, Bear Brook Pond, McDougal Pond, and tributaries from the southwest. Overflow from Little Shallow Lake through Shallow Lake, Daggett Pond, and Round Pond enters the east side of Caucomgomoc Lake through Ciss Stream.

Geographic entities mentioned:
surface_form: shallow lake
instance_of: Lake
countries: United States
coordinates: lat: 43.49
lon: -74.444
surface_form: shallow lake
instance_of: Lake
countries: United States
coordinates: lat: 43.49
lon: -74.444
surface_form: round pond
instance_of: Lake
countries: United States
coordinates: lat: 43.6765673
lon: -74.2537829
surface_form: round pond
instance_of: Lake
countries: United States
coordinates: lat: 41.8525
lon: -70.6042
surface_form: caucomgomoc lake
instance_of: Lake
countries: United States
coordinates: lat: 46.2
lon: -69.56666667
surface_form: round pond
instance_of: Lake
countries: United States
coordinates: lat: 41.17
lon: -74.776
surface_form: round pond
instance_of: Lake
countries: United States
coordinates: lat: 41.303611111111
lon: -73.536666666667
surface_form: round pond
instance_of: Lake
countries: United States
coordinates: lat: 43.738153
lon: -74.972297
Caucomgomoc Lake. Caucomgomoc Lake is in the North Maine Woods at the corner of townships 6 and 7 in ranges 14 and 15. Loon Stream flows into the southern end of the lake from Loon Lake, Bear Pond, Big Hurd Pond, Little Hurd Pond, Bear Brook Pond, McDougal Pond, and tributaries from the southwest.

Geographic entities mentioned:
surface_form: caucomgomoc lake
instance_of: Lake
countries: United States
coordinates: lat: 46.2
lon: -69.56666667
Weeks in Classical Revival style, and was built in 1922. It was listed on the National Register of Historic Places in 1998. It is significant for association with &quot;economic and political development&quot; of the Owens Valley and for housing county government during 1921–1947. It is the only example of &quot;monumental, Neo-Classical Revival architecture&quot; in the Owens Valley area.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
Babu Chiri Sherpa. Babu Chiri Sherpa (June 22, 1965 – April 29, 2001) was a Sherpa mountaineer from Nepal. He reached the summit of Mount Everest ten times. He held two world records on Everest. He spent 21 hours on the summit of Everest without auxiliary oxygen, a record which still stands, and he made the fastest ascent of Everest in 16 hours and 56 minutes.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Mountaineering. He began his career as a climber at the age of 16 when he procured a job as a trekking porter. On his first portering assignment he scaled the Amphu Labtsa pass. He summited Mera Peak (6472 m) in four hours in 1985. Chiri eventually found work portering for Everest expeditions, and eventually reached the summit of Everest ten times.

Geographic entities mentioned:
surface_form: Mera Peak
instance_of: Mountain
countries: Nepal
coordinates: lat: 27.7
lon: 86.866666666667
He summited Mera Peak (6472 m) in four hours in 1985. Chiri eventually found work portering for Everest expeditions, and eventually reached the summit of Everest ten times. In May 1999, he spent a record 21 hours on the summit without supplementary oxygen, and without sleeping. He also went on some expeditions to Cho Oyu. Other. Babu Chiri spoke Sherpa, Nepali, English and Hindi.

Geographic entities mentioned:
surface_form: Cho Oyu
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 28.094166666667
lon: 86.660833333333
The &quot;Stomatepia&quot; species are all recognized as critically endangered by the IUCN because of pollution and sedimentation due to human activities. They are potentially also threatened by large emissions of carbon dioxide (CO2) from the lake's bottom (compare Lake Nyos), although studies indicate that Barombo Mbo lacks excess amounts of this gas.

Geographic entities mentioned:
surface_form: Lake Nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889
It is in size, located approximately from Altamont. The lake sits between the south skirt of Stukel Mountain and Olene Gap to the north. Hydrology. The Klamath area has a peculiar natural draining system. The larger portion of this area, including Poe, Langell and Yonna valleys, is drained by the Lost River and its tributaries, which flow into several small lakes before emptying into Tule Lake.

Geographic entities mentioned:
surface_form: Tule Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.909322222222
lon: -121.53304722222
The most common type of fish in the lake are largemouth bass, rainbow trout and bluegill. Geography. Approximately 66,500 people live in Klamath County, mainly in the Klamath Falls metropolitan area. Many small towns in South and Eastern Klamath Falls are centered on a rural agricultural base that takes advantage of the peculiar irrigation systems offered by the Upper Klamath Lake and Lost River.

Geographic entities mentioned:
surface_form: Upper Klamath Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.392222222222
lon: -121.88027777778
Nuss Lake. Nuss Lake is a small private lake in Klamath Falls, Oregon, United States. It is in size, located approximately from Altamont. The lake sits between the south skirt of Stukel Mountain and Olene Gap to the north. Hydrology. The Klamath area has a peculiar natural draining system.

Geographic entities mentioned:
surface_form: nuss lake
instance_of: Lake
countries: United States
coordinates: lat: 42.1478
lon: -121.635
The larger portion of this area, including Poe, Langell and Yonna valleys, is drained by the Lost River and its tributaries, which flow into several small lakes before emptying into Tule Lake. Even though there are not many springs in Klamath County, some of the identifiable perennial springs that appear at land surface issue from the bottom of Nuss Lake.

Geographic entities mentioned:
surface_form: nuss lake
instance_of: Lake
countries: United States
coordinates: lat: 42.1478
lon: -121.635
Even though there are not many springs in Klamath County, some of the identifiable perennial springs that appear at land surface issue from the bottom of Nuss Lake. Hydraulic heads in wells are above surface at several places in the area, indicating that the aquifer is confined at these places, extending around Nuss Lake and the valley south and west of Stukel Mountain along Lost River.

Geographic entities mentioned:
surface_form: nuss lake
instance_of: Lake
countries: United States
coordinates: lat: 42.1478
lon: -121.635