Sarmila/GeoWiki-Features huggingface dataset:
and flanked by a huge ponor named &quot;Il Profondo&quot;. The main ridge continues with the Monte Rotondo, Bocchin dell'Aseo pass and Monte Mongioie. Just North of the Bric Conoia stands the tiny Raschera lake, from which originates one of the headwaters of the Corsaglia creek.

Geographic entities mentioned:
surface_form: Monte Mongioie
instance_of: Mountain
countries: Italy
coordinates: lat: 44.1758
lon: 7.785
surface_form: monte mongioie
instance_of: Mountain
countries: Italy
coordinates: lat: 44.1758
lon: 7.785
Geology. Bric di Conoia is mainly made of crystalline rocks and belongs to a series of Mesozoic origin. Tectonically they represent the easternmost strip of a syncline of the stratigraphyc complex which that constitutes the nearby Monte Mongioie. Summer. The summit can be reached following the main ridge both by the Bocchin del Bianco and Bocchin dell'Aseo.

Geographic entities mentioned:
surface_form: Monte Mongioie
instance_of: Mountain
countries: Italy
coordinates: lat: 44.1758
lon: 7.785
surface_form: monte mongioie
instance_of: Mountain
countries: Italy
coordinates: lat: 44.1758
lon: 7.785
Bric di Conoia. The Bric di Conoia (2.521 m) is a mountain of the &quot;Alpi del Marguareis&quot;, the western section of the Ligurian Alps. Etymology. The mountain was known in the past as &quot;Pizzo di Cornia&quot; or &quot;Pizzo Conolia&quot;, with the second toponym presumably derived from the first one. In the local dialect its name is &quot;Piz d'Cunùi&quot;. Features.

Geographic entities mentioned:
surface_form: bric di conoia
instance_of: Mountain
countries: Italy
coordinates: lat: 44.163324
lon: 7.8050554
Further downstream, before reaching the homonymous municipality, water diversions are made to supply irrigation for an area of approximately 2,360 hectares. Just before the town of La Sénia, the river marks the border between Catalonia and the Valencian Community. From this point until its mouth, the Cenia serves as a border between these two autonomous communities.

Geographic entities mentioned:
surface_form: sénia
instance_of: Watercourse
countries: Spain
coordinates: lat: 40.6709
lon: 0.2341
Cenia (river). The Cenia is a coastal river in Spain that flows through the eastern part of the Iberian Peninsula. Along a significant portion of its course, it acts as a border between the provinces of Castelló and Tarragona. It has a length of 50 km and it flows into the Mediterranean Sea. Route.

Geographic entities mentioned:
surface_form: cenia
instance_of: Watercourse
countries: Spain
coordinates: lat: 40.6709
lon: 0.2341
Just before the town of La Sénia, the river marks the border between Catalonia and the Valencian Community. From this point until its mouth, the Cenia serves as a border between these two autonomous communities. As it moves away from this point, the river practically receives no natural contributions, and the water quality deteriorates significantly.

Geographic entities mentioned:
surface_form: cenia
instance_of: Watercourse
countries: Spain
coordinates: lat: 40.6709
lon: 0.2341
The Pyrénées-Atlantiques departmental archives noted that: &quot;As Labourd borders Spain via the famous Mondarrain mountain at Itxassou, via Sare and the Urrugne pass, the inhabitants take their herds to graze on the Spanish mountains, which are not subject to flies like ours, and in turn, the Spaniards take their herds to our mountains where there is less snow.

Geographic entities mentioned:
surface_form: Mondarrain
instance_of: Mountain
countries: France
coordinates: lat: 43.30277778
lon: -1.43222222
The treaty bringing together the inhabitants of the Barétous valley and those of the Roncal valley are also worth mentioning, under the name of Tribute of the Three Cows, perpetuating to this day the pastoral dependence existing on both sides of the Pyrenees.

Geographic entities mentioned:
surface_form: Roncal valley
instance_of: Valley
countries: Spain
coordinates: lat: 42.83273891
lon: -0.8876911059
The treaty of La Vesiau, or Port of Astun, was established between the Aragonese commune of Jaca and the communes of Etsaut, Urdos and Cette-Eygun in the upper Aspe valley. Caroline Lugat likens these treaties, &quot;in spirit and content, to the treaties of lees and passeries signed between the Pyrenean valleys during the Franco-Spanish wars&quot;.

Geographic entities mentioned:
surface_form: Aspe valley
instance_of: Valley
countries: France
coordinates: lat: 42.95
lon: -0.6
Pinasca. Pinasca is a &quot;comune&quot; (municipality) in the Metropolitan City of Turin in the Italian region Piedmont, located about southwest of Turin in the Val Chisone. Pinasca borders the following municipalities: Giaveno, Perosa Argentina, Cumiana, Pinerolo, Frossasco, San Pietro Val Lemina, Inverso Pinasca, and Villar Perosa.

Geographic entities mentioned:
surface_form: Val Chisone
instance_of: Valley
countries: Italy
coordinates: lat: 45.033
lon: 7.05
Rivière du Moulin (Beauceville). The rivière du Moulin (&quot;in English: river of the Mill&quot;) is a tributary of the west bank of the Chaudière River which flows northward to empty onto the south bank of the St. Lawrence River.

Geographic entities mentioned:
surface_form: Chaudière River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.742777777777775
lon: -71.2786111111111
This lake is located at south-east of the center of the village of Saint-Alfred, at west of the Chaudière River, at north of the center of the village of Saint-Benoît-Labre and at north of the municipal boundary of Saint-Benoît-Labre (MRC Beauce-Sartigan Regional County Municipality).

Geographic entities mentioned:
surface_form: Chaudière River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.742777777777775
lon: -71.2786111111111
Lake Fortin (length:; altitude of) is renowned for its vacation; this head lake is located southeast of the village of Saint-Victor. The Moulin river flows on the west bank of the Chaudière River in the municipality of Beauceville. The confluence of the Rivière du Moulin is located south of the town of Beauceville bridge and downstream from Île aux Oies. Toponymy.

Geographic entities mentioned:
surface_form: Chaudière River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.742777777777775
lon: -71.2786111111111
Shaver, California. Shaver is a former settlement in Fresno County, California. It was located at the north end of Shaver Lake, where a post office operated from 1896 to 1925. The site is now under the waters of Shaver Lake.

Geographic entities mentioned:
surface_form: Shaver Lake
instance_of: Lake
countries: United States
coordinates: lat: 37.125969444444
lon: -119.29075
The Falkenstein went to his son Henry as part of the new Barony of Wildenstein. He set up his seat of power in the castle at New Wildenstein. In addition to the surrounding villages and towns, the lordship also included other watchtowers, e.g. on the Rauschenstein and the Frienstein. From about 1425, Henry von der Duba was repeatedly feuding with the Lusatian League and the Saxon Electors.

Geographic entities mentioned:
surface_form: Frienstein
instance_of: Mountain
countries: Germany
coordinates: lat: 50.912055555556
lon: 14.245805555556
on the Rauschenstein and the Frienstein. From about 1425, Henry von der Duba was repeatedly feuding with the Lusatian League and the Saxon Electors. His nephews, who inherited the barony around 1435, continued the feuds and attacked villages and merchant trains as robber barons. However, with the exception of the Elbe, there were no trade routes in the immediate vicinity of the Falkenstein.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
surface_form: falkenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 50.9183
lon: 14.2011
surface_form: falkenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 49.084166666667
lon: 13.28
Falkenstein (Saxon Switzerland). The Falkenstein is one of the best-known climbing peaks in Saxon Switzerland. It is situated near the rocky Schrammsteine ridge southeast of the town of Bad Schandau. The Falkenstein is nearly 90 m high and consists of sandstone. In the Middle Ages there were fortifications on top of the rock. Even today, the steps carved into the rock are still visible. History.

Geographic entities mentioned:
surface_form: falkenstein (saxon switzerland)
instance_of: Mountain
countries: Germany
coordinates: lat: 50.9183
lon: 14.2011
surface_form: falkenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 49.084166666667
lon: 13.28
Falkenstein (Saxon Switzerland). The Falkenstein is one of the best-known climbing peaks in Saxon Switzerland. It is situated near the rocky Schrammsteine ridge southeast of the town of Bad Schandau. The Falkenstein is nearly 90 m high and consists of sandstone. In the Middle Ages there were fortifications on top of the rock. Even today, the steps carved into the rock are still visible. History.

Geographic entities mentioned:
surface_form: falkenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 50.9183
lon: 14.2011
surface_form: falkenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 49.084166666667
lon: 13.28
History. The Falkenstein was probably built on and used as a castle lookout from the middle of the 14th century. Like almost all of Saxon Switzerland on the right bank of the Elbe, it belonged to the Barony of Hohnstein with its seat at Hohnstein Castle, which was given to the Bohemian noble family of Berka von Dubá in 1353 by Emperor Charles IV as a Bohemian fiefdom.

Geographic entities mentioned:
surface_form: falkenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 50.9183
lon: 14.2011
surface_form: falkenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 49.084166666667
lon: 13.28
In 1409 Hinko von der Duba divided the territory among his five sons. The Falkenstein went to his son Henry as part of the new Barony of Wildenstein. He set up his seat of power in the castle at New Wildenstein. In addition to the surrounding villages and towns, the lordship also included other watchtowers, e.g. on the Rauschenstein and the Frienstein.

Geographic entities mentioned:
surface_form: falkenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 50.9183
lon: 14.2011
surface_form: falkenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 49.084166666667
lon: 13.28
It also secured access from the Elbe to Wildenstein Castle. Elector Frederick II of Saxony finally besieged the Berkas on the Wildenstein from autumn 1439 to put an end to the feuds. The watchtower on the Falkenstein was probably destroyed during this campaign. The Berkas finally agreed in 1451 to an exchange of the Barony of Wildenstein for part of the Barony of Schluckenau in Bohemia.

Geographic entities mentioned:
surface_form: falkenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 50.9183
lon: 14.2011
surface_form: falkenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 49.084166666667
lon: 13.28
The watchtower on the Falkenstein was probably destroyed during this campaign. The Berkas finally agreed in 1451 to an exchange of the Barony of Wildenstein for part of the Barony of Schluckenau in Bohemia. With this, the Falkenstein finally became Saxon property. In the list of castles created in 1456, the Falkenstein was already one of the watchtowers described as derelict.

Geographic entities mentioned:
surface_form: falkenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 50.9183
lon: 14.2011
surface_form: falkenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 49.084166666667
lon: 13.28
The Berkas finally agreed in 1451 to an exchange of the Barony of Wildenstein for part of the Barony of Schluckenau in Bohemia. With this, the Falkenstein finally became Saxon property. In the list of castles created in 1456, the Falkenstein was already one of the watchtowers described as derelict. In 1543 and 1547 the rock is mentioned as part of the forests belonging to Hohnstein.

Geographic entities mentioned:
surface_form: falkenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 50.9183
lon: 14.2011
surface_form: falkenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 49.084166666667
lon: 13.28
In 1543 and 1547 the rock is mentioned as part of the forests belonging to Hohnstein. The map of the first Electoral Saxon state survey, created by Matthias Oeder in 1592 describes it as &quot;bare and high&quot;. During the Thirty Years' War, residents of the surrounding towns hid themselves on the Falkenstein, as weather-beaten inscriptions, including the year &quot;1631&quot;, bear witness to.

Geographic entities mentioned:
surface_form: falkenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 50.9183
lon: 14.2011
surface_form: falkenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 49.084166666667
lon: 13.28
Plans to create a more generally accessible ascent came up again, which also failed due to lack of funds. At the end of 1894, a weather vane in the form of a falcon was mounted on the Falkenstein as a summit mark. In 1903 the flag had to be repaired after being damaged. In 1929, the falcon, whose existence had been repeatedly criticized as a blight, disappeared from the summit.

Geographic entities mentioned:
surface_form: falkenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 50.9183
lon: 14.2011
surface_form: falkenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 49.084166666667
lon: 13.28
In 1892, while descending the &quot;Turnerweg&quot; after the first ascent of the &quot;Schusterweg&quot;, Oscar Schuster and Martin Klimmer discovered artificial steps under the vegetation that had been part of the ascent to the watchtower. In 1940, Dresden architect and local historian, Oskar Pusch, carried out a major investigation of the fortification at Falkenstein.

Geographic entities mentioned:
surface_form: falkenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 50.9183
lon: 14.2011
surface_form: falkenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 49.084166666667
lon: 13.28
Hammergraben. Hammergraben is a river of Brandenburg, Germany. It branches off the Spree in Cottbus, and flows into the Großes Fließ (a tributary of the Spree) in Schmogrow-Fehrow. It is used to flood Cottbuser Ostsee, a former open pit lignite mine, which is planned to become Germany's largest artificial lake by surface area.

Geographic entities mentioned:
surface_form: Cottbuser Ostsee
instance_of: Lake
countries: Germany
coordinates: lat: 51.7875
lon: 14.4322
The Great Lakes. New York borders Lake Ontario and Lake Erie to the west. &quot;The levels of Lake Erie and Lake Ontario are expected to drop due to increased evaporation and lower recharge rates caused by climate change.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
It is located on the boundary of the Waikato and Manawatū-Whanganui regions. Geology. Mount Pureora has a prominence above the surrounding countryside of about and a diameter of. It is to the south west of a smaller pleioscene stratovolcano, Mount Titiraupenga, and both are located to the south of the ancient Mangakino caldera on a basement of Waipapa composite terrane.

Geographic entities mentioned:
surface_form: Mount Titiraupenga
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.509892
lon: 175.691807
surface_form: titiraupenga
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.509892
lon: 175.691807
surface_form: mount titiraupenga
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.509892
lon: 175.691807
Access. The mountain top is accessed by several trails and has bike access. These include a portion of the Te Araroa trail which incorporates the Timber trail and a branch of this called the Toi Toi track accessible off State Highway 30 near the township of Pureora. The Mount Pureora track is accessible also from back roads off State Highway 32, which lies to the west of Lake Taupō.

Geographic entities mentioned:
surface_form: pureora
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.551056
lon: 175.628694
Mount Pureora. Pureora (known more usually as Mount Pureora to avoid confusion with the township, locality and Forest Park) is an extinct high basaltic andesite stratovolcano located in the Pureora Forest Park between Lake Taupō and Te Kūiti on the North Island Volcanic Plateau in New Zealand.

Geographic entities mentioned:
surface_form: pureora
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.551056
lon: 175.628694
surface_form: mount pureora
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.551056
lon: 175.628694
Mount Pureora. Pureora (known more usually as Mount Pureora to avoid confusion with the township, locality and Forest Park) is an extinct high basaltic andesite stratovolcano located in the Pureora Forest Park between Lake Taupō and Te Kūiti on the North Island Volcanic Plateau in New Zealand.

Geographic entities mentioned:
surface_form: pureora
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.551056
lon: 175.628694
surface_form: pureora
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.551056
lon: 175.628694
surface_form: pureora
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.551056
lon: 175.628694
surface_form: mount pureora
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.551056
lon: 175.628694
Highway serves as the primary highway of the Middle Peninsula. At Fredericksburg, US 17 leaves the Atlantic Plain; the highway passes through the Piedmont town of Warrenton and crosses the Blue Ridge Mountains on its way to Winchester in the Shenandoah Valley. The route from Tappahannock to Winchester roughly follows the Confederate march during the Civil War to Gettysburg.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
At Glenns, the highway has an intersection with SR 198 (Glenns Road) and SR 33 (Lewis Puller Memorial Highway). US 17 and SR 33 head north together and cross the Dragon Swamp, which becomes the Piankatank River, into Middlesex County and assume the name Tidewater Trail. The two highways diverge at Saluda, into which SR 33 and US 17 Bus. head north as Gloucester Road.

Geographic entities mentioned:
surface_form: Dragon Swamp
instance_of: Landform
countries: United States
coordinates: lat: 37.5678
lon: -76.575
Every morning, the cowboys would congregate at &quot;The Watering Hole&quot;, where the directors would send over their assistants to hire for the following day. The cowboys would then dress in their normal riding clothes (unless told otherwise, for which they were paid extra), and ride to the set, most of which were located to the north in the vicinity of the San Fernando Valley.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Khökh Serkh. Khökh Serkh (, &quot;blue buck&quot;) with a latitude of 48.05 (48° 3' 2 N) and a longitude of 90.87 (90° 51' 59 E), is a mountain located in west Mongolia. The highest peak is the Takhilt.

Geographic entities mentioned:
surface_form: khökh serkh
instance_of: Mountain
countries: Mongolia
coordinates: lat: 48.05055556
lon: 90.86638889
Climate change and other forces can cause sea levels and elevations to vary over time. Units and abbreviations. For elevations or altitudes, often just the abbreviation MSL is used, e.g., Mount Everest (8849 m MSL), or the reference to sea level is omitted completely, e.g., Mount Everest (8849 m). Methods of measurement. Accurate measurement of historical mean sea levels is complex.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Career. Prior to World War II, Eleanor Ireland worked for a philatelist. Ireland volunteered for the Women's Royal Naval Service (WRNS) in the spring of 1944, and received a letter on 2 August 1944, that she was accepted into the WRNS. Once accepted into the Women's Royal Naval Service, Ireland was kept at Tullichewan Castle, located near Loch Lomond, Scotland.

Geographic entities mentioned:
surface_form: Loch Lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
In a series of rapids and cascades, it descends the Valle di Comino, passing through Picinisco, Atina— where it receives the waters of the little Mollarino— Casalattico and Casalvieri. Below Casalvieri it passes for 15 km through a deep gorge in the foothills of Monte Cairo at the end of which it reaches the Liri, near Roccasecca.

Geographic entities mentioned:
surface_form: Monte Cairo
instance_of: Mountain
countries: Italy
coordinates: lat: 41.542
lon: 13.76
On the west side of the icefield is the valley of the Squamish River, while on its east is the Callaghan Valley, which is the setting for the Nordic facilities for the 2010 Winter Olympics. The icefield is studded by several volcanic formations, including active Mount Cayley. Other summits are Powder Mountain, Brandywine Mountain and Mount Fee.

Geographic entities mentioned:
surface_form: Callaghan Valley
instance_of: Valley
countries: Canada
coordinates: lat: 50.1369
lon: -123.152
The icefield is studded by several volcanic formations, including active Mount Cayley. Other summits are Powder Mountain, Brandywine Mountain and Mount Fee. Mount Callaghan, a dormant volcano, is just northeast of the icefield. Mount Brew is just to its south. Geology.

Geographic entities mentioned:
surface_form: Brandywine Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.114444444444
lon: -123.22111111111
surface_form: Mount Fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
The icefield is studded by several volcanic formations, including active Mount Cayley. Other summits are Powder Mountain, Brandywine Mountain and Mount Fee. Mount Callaghan, a dormant volcano, is just northeast of the icefield. Mount Brew is just to its south. Geology.

Geographic entities mentioned:
surface_form: Mount Callaghan
instance_of: Mountain
countries: Canada
coordinates: lat: 50.2278
lon: -123.266
Mount Callaghan, a dormant volcano, is just northeast of the icefield. Mount Brew is just to its south. Geology. Numerous subglacial eruptions beneath the Powder Mountain Icefield have formed many distinctive subglacial volcanoes in the Mount Cayley volcanic field and contain abundant glass and fine-scale jointing from rapid cooling of lava, such as Ember Ridge and Slag Hill.

Geographic entities mentioned:
surface_form: Mount Cayley volcanic field
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1203
lon: -123.291
surface_form: Slag Hill
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1834
lon: -123.3
Its preceding local improvement district was established in 1908. Geography. Wood River and Notukeu Creek are two natural features in the RM. The lake resort of Gaumond Bay is on Thomson Lake near Thomson Lake Regional Park. Communities and localities. The following urban municipalities are surrounded by the RM. The following unincorporated communities are within the RM. Historic sites.

Geographic entities mentioned:
surface_form: Thomson Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.75003
lon: -106.60061
Description. Graybeard Peak is part of the North Cascades Range. Graybeard Peak straddles the North Cascades National Park boundary line, and can be seen from the North Cascades Highway at the Easy Pass Trailhead. Graybeard Peak is situated on Ragged Ridge. Other peaks on Ragged Ridge include Mesahchie Peak, Kimtah Peak, and Katsuk Peak. The nearest higher peak is Fisher Peak, to the south.

Geographic entities mentioned:
surface_form: Mesahchie Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.5786
lon: -120.88
surface_form: Kimtah Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.585
lon: -120.91
surface_form: Katsuk Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.5783
lon: -120.888
Graybeard Peak. Graybeard Peak is a mountain summit located in Skagit County, Washington. Description. Graybeard Peak is part of the North Cascades Range. Graybeard Peak straddles the North Cascades National Park boundary line, and can be seen from the North Cascades Highway at the Easy Pass Trailhead. Graybeard Peak is situated on Ragged Ridge.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: graybeard peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.55866667
lon: -120.822
Graybeard Peak is situated on Ragged Ridge. Other peaks on Ragged Ridge include Mesahchie Peak, Kimtah Peak, and Katsuk Peak. The nearest higher peak is Fisher Peak, to the south. Precipitation runoff on the east side of the mountain drains into Ross Lake via Granite Creek, whereas the west side of the mountain drains into Diablo Lake via Fisher Creek. Climate.

Geographic entities mentioned:
surface_form: fisher peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.54541
lon: -120.82344
Graybeard Peak is situated on Ragged Ridge. Other peaks on Ragged Ridge include Mesahchie Peak, Kimtah Peak, and Katsuk Peak. The nearest higher peak is Fisher Peak, to the south. Precipitation runoff on the east side of the mountain drains into Ross Lake via Granite Creek, whereas the west side of the mountain drains into Diablo Lake via Fisher Creek. Climate.

Geographic entities mentioned:
surface_form: ross lake
instance_of: Lake
countries: United States
coordinates: lat: 46.66277778
lon: -93.83638889
Graybeard Peak. Graybeard Peak is a mountain summit located in Skagit County, Washington. Description. Graybeard Peak is part of the North Cascades Range. Graybeard Peak straddles the North Cascades National Park boundary line, and can be seen from the North Cascades Highway at the Easy Pass Trailhead. Graybeard Peak is situated on Ragged Ridge.

Geographic entities mentioned:
surface_form: graybeard peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.55866667
lon: -120.822
Description. Graybeard Peak is part of the North Cascades Range. Graybeard Peak straddles the North Cascades National Park boundary line, and can be seen from the North Cascades Highway at the Easy Pass Trailhead. Graybeard Peak is situated on Ragged Ridge. Other peaks on Ragged Ridge include Mesahchie Peak, Kimtah Peak, and Katsuk Peak. The nearest higher peak is Fisher Peak, to the south.

Geographic entities mentioned:
surface_form: graybeard peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.55866667
lon: -120.822
Precipitation runoff on the east side of the mountain drains into Ross Lake via Granite Creek, whereas the west side of the mountain drains into Diablo Lake via Fisher Creek. Climate. Graybeard Peak is located in the marine west coast climate zone of western North America. Most weather fronts originating in the Pacific Ocean travel northeast toward the Cascade Mountains.

Geographic entities mentioned:
surface_form: graybeard peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.55866667
lon: -120.822
Wuikinuxv Nation. The Wuikinuxv Nation, also known as the Oweekeno Nation, is a First Nations band government whose traditional territory is the shores of Rivers Inlet and Owikeno Lake in the Central Coast region of the Canadian province of British Columbia, in the area south of Bella Bella and north of Queen Charlotte Strait. The Wuikinuxv people a.k.a.

Geographic entities mentioned:
surface_form: Owikeno Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.683333333333
lon: -126.91666666667
The Wuikinuxv people a.k.a. the Oweekeno people reside in the area of Rivers Inlet and Owikeno Lake, primarily at a village on the Wannock River. Substantial numbers of Wuikinuxv also reside away from the traditional territory in Port Hardy on Vancouver Island and in larger BC communities such as Campbell River, Vancouver and Victoria.

Geographic entities mentioned:
surface_form: Owikeno Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.683333333333
lon: -126.91666666667
Weaver Peninsula. Weaver Peninsula () is a small man-made peninsula between Collins Harbor and Marian Cove, Maxwell Bay, King George Island, terminating in North Spit. It was named by the United Kingdom Antarctic Place-Names Committee (UK-APC) in 1977 after Stephen D. Weaver, geologist, University of Birmingham, with the British Antarctic Survey (BAS) party in this area in 1976.

Geographic entities mentioned:
surface_form: North Spit
instance_of: Landform
coordinates: lat: -62.2167
lon: -58.8167
Goslin initially had difficulties in publishing the book, which was rejected by publishing houses. The one publisher who expressed interest insisted that the cover illustration of the statue of Christ on Corcovado ogling a bikini-clad girl would have to be removed, which was unacceptable to her. As a result, she decided to self-publish and ordered 3000 copies from a printer.

Geographic entities mentioned:
surface_form: Corcovado
instance_of: Mountain
countries: Brazil
coordinates: lat: -22.9525
lon: -43.211666666667
The remainder of the beaches, including Depot Street, Glendon Rd, Haigis, Inman Rd., Raycroft, Sea Street, South Village and West Dennis, are located on the southern side of the Cape and Islands. Princess and Scargo, both on Scargo Lake, are the two fresh water ponds, and both are located on the northern side as well.

Geographic entities mentioned:
surface_form: Scargo Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.7425
lon: -70.182777777778
Aunt Julia Ann Road, and the beach by the same name, is found on the Bass River, across from the Bass River Golf Club. It is named for Julia Ann Baker, the third wife and widow of Levi Baker. West Dennis Beach was once known as Davis Beach, and the road that runs along the length of the beach is Davis Beach Road. Charles Henry Davis sold the beach to the Town in the early 1900s.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Dennis Beaches. The Dennis Beaches, are a series of beaches in Dennis, Massachusetts, on Cape Cod. There are a total of eighteen beaches; sixteen located on the ocean and two located on fresh water ponds. Eight of the ocean beaches, Mayflower, Corporation, Bayview, Howes Street, Chapin Memorial, Cold Storage and Harbor View, are located on the northern (bay side) of the Cape and Islands.

Geographic entities mentioned:
surface_form: dennis beaches
instance_of: Landform
countries: United States
coordinates: lat: 41.677
lon: -70.1779
White River (Huron County, Michigan). The White River is a river in southern Huron County, Michigan. It is a tributary of Lake Huron.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
The thicker, deeper, denser &quot;South-western Cape forests&quot; are dominated by larger afromontane trees. These tall woodlands are typically found in sheltered gorges and mountainous areas in the Western Cape. They also include the Cape Peninsula Forests such as those at Newlands Forest, Kirstenbosch, and Orangekloof, which are all located around Table Mountain, within the city of Cape Town.

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
Route 20 (US 20). Route description. It passes through Bryan, Wauseon (where it briefly becomes a couplet), and enters greater Toledo west of its interchange with the Ohio Turnpike. It continues east from greater Toledo and soon parallels Lake Erie, becoming a freeway near Port Clinton. From Oregon to Sandusky SR 2 is part of of the highway designated the &quot;Lake Erie Coastal Ohio Trail&quot;.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
The Cleveland Memorial Shoreway, often shortened to &quot;the Shoreway&quot;, is a limited-access freeway in Cleveland and Bratenahl. It closely follows the shore of Lake Erie and connects the east and west sides of Cleveland via the Main Avenue Bridge over the Cuyahoga River. The entire length of the Shoreway is part of the Lake Erie Circle Tour and all of the Shoreway is part of SR 2.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
The village has a population (2019) of 3,117 and a population density of. Farnes Church is located in this village. The road &quot;Tindevegen&quot; goes from Øvre Årdal, through the Fardalen valley to the village of Turtagrø in Luster Municipality. It's one of the highest elevation roads in Norway.

Geographic entities mentioned:
surface_form: Fardalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.339166666667
lon: 7.7605555555556
It's one of the highest elevation roads in Norway. There is also a road which goes south past the lake Tyin to the European route E16 highway which goes through Valdres to Oslo. Øvre Årdal is the starting point for tours into the nearby Utladalen Landscape Protection Area and Jotunheimen National Park.

Geographic entities mentioned:
surface_form: Valdres
instance_of: Valley
countries: Norway
coordinates: lat: 60.916666666667
lon: 9.1666666666667
Øvre Årdal is the starting point for tours into the nearby Utladalen Landscape Protection Area and Jotunheimen National Park. There are trips to the Utladalen and Avdalen valleys, to the mountain Falketind, to the Vettisfossen waterfall, and to the historic farms of Vetti, Vettismorki, and Avdalen. Norsk Hydro has an aluminium smelting plant which is a major employer in the area.

Geographic entities mentioned:
surface_form: Utladalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.4
lon: 7.9708333333333
surface_form: Avdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.2275
lon: 7.7863888888889
surface_form: Falketind
instance_of: Mountain
countries: Norway
coordinates: lat: 61.384444444444
lon: 8.0969444444444
surface_form: Avdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.2275
lon: 7.7863888888889
Today, there are two routes that oil can take between Superior and Sarnia. A northern route passes through the upper and lower peninsulas of Michigan before crossing into Ontario, while the southern route circles south of Lake Michigan through Illinois and Indiana before reaching Michigan. There are 59 pumping stations in the pipeline system, and the actual pipes range in diameter from.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
It has a population of 1,313. The municipality consists of the following villages Nabran, Dalğalı, Turist, Meşəli, Günəşli, Samurçay, and Şimal. Nabran is the largest region within the Khachmaz Rayon. Nabran is a 3-hour drive from the capital of Azerbaijan, Baku, and is located on the Caspian seashore in a subtropical forestland. The settlement covers several kilometers. Tourism.

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
Nature. The forested area which is immediately intertwined with the sandy beach is rich with unique trees particular to this area. In the background, the forests merge with Mount Shahdagh of Greater Caucasus Mountain range. Due to absence of manufacturing industry and low population density, the sea water is clean compared to heavily industrialized Absheron Peninsula.

Geographic entities mentioned:
surface_form: Mount Shahdagh
instance_of: Mountain
countries: Azerbaijan
coordinates: lat: 41.2725
lon: 48.004444444444
He died in 1892 or 1893 in the Canadian Arctic. He was the nephew of Swedish mathematician Emanuel Björling (1808–1872). Expeditions. In the summer of 1889 as a 17‑year‑old, he led an expedition along with two companions to become the first to climb Kebnekaise, the highest mountain in Sweden. In 1890, he participated in an expedition to Greenland and Spitsbergen.

Geographic entities mentioned:
surface_form: Kebnekaise
instance_of: Mountain
countries: Sweden
coordinates: lat: 67.883333333333
lon: 18.55
The ship sailed and was never heard from again. The next time people heard about the company was through a telegram, sent in November 1893 by the whaler &quot;Aurora&quot;, which stated that the ship had passed the wrecks of &quot;Ripple&quot; on June 17 of that year at the mouth of Smith Sound. Notes found later revealed details of Björling's tragic expedition.

Geographic entities mentioned:
surface_form: Smith Sound
instance_of: Watercourse
countries: Greenland
Canada
coordinates: lat: 78.4167
lon: -74
Early history. The Stampa trace their ancestry back to Carlo Lanfranco of the dukes of Étampes, later governor of Milan under Charles the Great. His descendants settled in Milan and Gravedona, and ruled over the Val Bregaglia. The best evidence for this is the city of Stampa, named so by the family in honour of its ancestors.

Geographic entities mentioned:
surface_form: Val Bregaglia
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.3324
lon: 9.514
It is situated in the Moquegua Region, General Sánchez Cerro Province, Ichuña District, northeast of Jukumarini Lake. Jaqhi Jaqhini lies southwest of the mountain Wallqani, northwest of Larama Quta and northeast of Salla Qullu &quot;(Sallacollo)&quot;.

Geographic entities mentioned:
surface_form: Wallqani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.2911
lon: -70.3475
surface_form: Larama Quta
instance_of: Mountain
countries: Peru
coordinates: lat: -16.3269
lon: -70.3628
surface_form: larama quta
instance_of: Mountain
countries: Peru
coordinates: lat: -16.3269
lon: -70.3628
surface_form: wallqani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.2911
lon: -70.3475
Jaqhi Jaqhini. Jaqhi Jaqhini (Aymara &quot;jaqhi&quot; cliff, the reduplication indicates that there is a group or a complex of something, &quot;-ni&quot; a suffix to indicate ownership, &quot;the one with many cliffs&quot;, Hispanicized spelling &quot;Jaque Aquine&quot;) is a mountain in the Andes of southern Peru.

Geographic entities mentioned:
surface_form: jaqhi jaqhini
instance_of: Mountain
countries: Peru
coordinates: lat: -16.3011
lon: -70.3753
Jaqhi Jaqhini. Jaqhi Jaqhini (Aymara &quot;jaqhi&quot; cliff, the reduplication indicates that there is a group or a complex of something, &quot;-ni&quot; a suffix to indicate ownership, &quot;the one with many cliffs&quot;, Hispanicized spelling &quot;Jaque Aquine&quot;) is a mountain in the Andes of southern Peru.

Geographic entities mentioned:
surface_form: jaqhi jaqhini
instance_of: Mountain
countries: Peru
coordinates: lat: -16.3011
lon: -70.3753
surface_form: jaque aquine
instance_of: Mountain
countries: Peru
coordinates: lat: -16.3011
lon: -70.3753
It is situated in the Moquegua Region, General Sánchez Cerro Province, Ichuña District, northeast of Jukumarini Lake. Jaqhi Jaqhini lies southwest of the mountain Wallqani, northwest of Larama Quta and northeast of Salla Qullu &quot;(Sallacollo)&quot;.

Geographic entities mentioned:
surface_form: jukumarini
instance_of: Lake
countries: Peru
coordinates: lat: -16.386111111111
lon: -70.403611111111
Foxholes, North Yorkshire. Foxholes is a village in North Yorkshire, England, part of the civil parish of Foxholes with Butterwick. It lies where the B1249 road crosses the Great Wold Valley, south from Scarborough, north-west from Bridlington, and north-east from Sledmere. The course of the winterbourne stream the Gypsey Race passes to the south of the village.

Geographic entities mentioned:
surface_form: Great Wold Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.1385
lon: -0.3835
Geography. The municipality of Nevesinje covers and is located in the south of Bosnia and Herzegovina. A large polje called Nevesinjsko polje dominates the municipality, and is encircled by the mountains of Crvanj to the north and northeast, Prenj to the northwest, and Velež to the south and southwest.

Geographic entities mentioned:
surface_form: Crvanj
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.391388888889
lon: 18.200277777778
surface_form: Prenj
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.53480621248335
lon: 17.90430346491326
Lodgepole pine can tolerate relatively hostile environments such as high-elevation volcanic rock in Central Oregon (e.g. Crater Lake) and thin soils on the eastern slope of the Cascades. Further south, the species can be found in higher elevations up to above sea level, particularly in southern Colorado. It is rare in lowland rain forests.

Geographic entities mentioned:
surface_form: Crater Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.943611111111
lon: -122.10666666667
Out of the 700 soldiers fighting on the British side, 14 were Canadian locals and the remainder were British regulars. Although Vincent accompanied the column, he placed Harvey in command. At this point, the story of Billy Green comes to light. Green was a 19-year-old local resident who had witnessed the advance of the Americans from the top of the Niagara Escarpment earlier in the day.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
They may have come down the canal as far as Maple Bay. They occupied all the White River and Meziadin Lake basins and one of their original headquarters, especially for salmon fishing, was at Meziadin Lake. They stretched across the head of the Skeena River above the Kuldo River over to Bear and Sustut lakes &quot;

Geographic entities mentioned:
surface_form: Sustut
instance_of: Lake
countries: Canada
coordinates: lat: 56.5833
lon: -126.45
Yuraq Urqu (Apurímac). Yuraq Urqu (Quechua &quot;yuraq&quot; white, &quot;urqu&quot; mountain, &quot;white mountain&quot;, Hispanicized spelling &quot;Yurac Orjo&quot;) is a mountain in the Wansu mountain range in the Andes of Peru, about high. It is situated in the Apurímac Region, Antabamba Province, Antabamba District. Yuraq Urqu lies to the northwest of Yawriwiri and Jalanta.

Geographic entities mentioned:
surface_form: Yawriwiri
instance_of: Mountain
countries: Peru
coordinates: lat: -14.5419
lon: -72.7039
Yuraq Urqu (Apurímac). Yuraq Urqu (Quechua &quot;yuraq&quot; white, &quot;urqu&quot; mountain, &quot;white mountain&quot;, Hispanicized spelling &quot;Yurac Orjo&quot;) is a mountain in the Wansu mountain range in the Andes of Peru, about high. It is situated in the Apurímac Region, Antabamba Province, Antabamba District. Yuraq Urqu lies to the northwest of Yawriwiri and Jalanta.

Geographic entities mentioned:
surface_form: yuraq urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.5025
lon: -72.7253
Danville Mountain. Danville Mountain is a mountain in Warren County, New Jersey. The summit rises to, and is located in Liberty Township. It is part of the New York–New Jersey Highlands of the Appalachian Mountains, although somewhat isolated to the west of the main body of the Highlands.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: danville mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.8695
lon: -74.9371
Danville Mountain. Danville Mountain is a mountain in Warren County, New Jersey. The summit rises to, and is located in Liberty Township. It is part of the New York–New Jersey Highlands of the Appalachian Mountains, although somewhat isolated to the west of the main body of the Highlands.

Geographic entities mentioned:
surface_form: danville mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.8695
lon: -74.9371
Danville Mountain. Danville Mountain is a mountain in Warren County, New Jersey. The summit rises to, and is located in Liberty Township. It is part of the New York–New Jersey Highlands of the Appalachian Mountains, although somewhat isolated to the west of the main body of the Highlands.

Geographic entities mentioned:
surface_form: the highlands
instance_of: Mountain
countries: United States
coordinates: lat: 42.0393156
lon: -70.0604509
Kanianitis. The Kanianitis () is a river in Phocis, central Greece. It receives its water from the mountains Oeta and Giona. It flows through the villages Kastellia, Gravia and Mariolata, and flows into the Cephissus near the village Lilaia in the municipality of Parnassos. In antiquity, it was called Pindos or Pindus (). The Pindus was a river of ancient Phocis and Doris.

Geographic entities mentioned:
surface_form: Oeta
instance_of: Mountain
countries: Greece
coordinates: lat: 38.816666666667
lon: 22.283333333333
surface_form: Giona
instance_of: Mountain
countries: Greece
coordinates: lat: 38.613888888889
lon: 22.253055555556
Mecodema manaia. &quot;Mecodema manaia&quot; is a medium-sized ground beetle species found in the native forests of Bream Head and Mt Manaia, Northland, New Zealand. This species shares the forests of Bream Head with a large-bodied species, &quot;Mecodema tewhara&quot;, with both inhabiting slightly different forest type. Description. Length, pronotal width, elytral width.

Geographic entities mentioned:
surface_form: Mt Manaia
instance_of: Mountain
countries: New Zealand
coordinates: lat: -35.818309
lon: 174.516985
Jumbled Hills. The Jumbled Hills are a mountain range in Lincoln County, Nevada.

Geographic entities mentioned:
surface_form: jumbled hills
instance_of: Landform
countries: United States
coordinates: lat: 37.2083
lon: -115.628
Los Nevados National Park. The Nevado del Tolima is located within the Los Nevados National Natural Park, In addition to the Nevado del Tolima, seven other volcanoes are located in the park: Nevado del Ruiz, Santa Isabel, Nevado del Quindío, Paramillo de Santa Rosa, Cerro Bravo, Cerro Machín and Nevado El Cisne.

Geographic entities mentioned:
surface_form: Nevado del Quindío
instance_of: Mountain
countries: Colombia
coordinates: lat: 4.7155555555556
lon: -75.388333333333
surface_form: Nevado El Cisne
instance_of: Mountain
countries: Colombia
coordinates: lat: 4.8430555555556
lon: -75.352222222222
surface_form: nevado del tolima
instance_of: Mountain
countries: Colombia
coordinates: lat: 4.6666666666667
lon: -75.333333333333
surface_form: nevado del tolima
instance_of: Mountain
countries: Colombia
coordinates: lat: 4.6666666666667
lon: -75.333333333333
Nevado del Tolima. The Nevado del Tolima is a Late Pleistocene to recently active andesitic stratovolcano located in the Tolima department, Colombia. The volcano lies south of Nevado del Ruiz volcano and is situated within the Los Nevados National Natural Park.

Geographic entities mentioned:
surface_form: nevado del tolima
instance_of: Mountain
countries: Colombia
coordinates: lat: 4.6666666666667
lon: -75.333333333333
Geography and geology. The steep-sided, glacier-clad Nevado del Tolima volcano contrasts with the broad profile of Nevado del Ruiz to the north. The andesitic-dacitic younger Tolima formed during the past 40,000 years, rising above and largely obscuring a wide Late Pleistocene caldera.

Geographic entities mentioned:
surface_form: nevado del tolima
instance_of: Mountain
countries: Colombia
coordinates: lat: 4.6666666666667
lon: -75.333333333333