Sarmila/GeoWiki-Features huggingface dataset:
The hill is the source for the Manzanares and El Chuscal creeks that flow westwards onto the Bogotá savanna. Historically, Guadalupe Hill was an important sacred site for the indigenous Muisca, who inhabited the Bogotá savanna and surrounding regions before the Spanish conquest.

Geographic entities mentioned:
surface_form: guadalupe hill
instance_of: Mountain
countries: Colombia
coordinates: lat: 4.59194
lon: -74.0544
surface_form: bogotá
instance_of: Watercourse
countries: Colombia
coordinates: lat: 5.25
lon: -73.666666666667
Historically, Guadalupe Hill was an important sacred site for the indigenous Muisca, who inhabited the Bogotá savanna and surrounding regions before the Spanish conquest. During the colonial period, Guadalupe Hill contained a cross and the hermitage that was destroyed by various earthquakes in the eighteenth, nineteenth and twentieth centuries.

Geographic entities mentioned:
surface_form: guadalupe hill
instance_of: Mountain
countries: Colombia
coordinates: lat: 4.59194
lon: -74.0544
During the colonial period, Guadalupe Hill contained a cross and the hermitage that was destroyed by various earthquakes in the eighteenth, nineteenth and twentieth centuries. On Sundays, Guadalupe Hill and its chapel and statue are visited by tourists and pilgrims from Bogotá, accessing the hill either by road and public transport or via a walking trail to the hilltop. Etymology.

Geographic entities mentioned:
surface_form: guadalupe hill
instance_of: Mountain
countries: Colombia
coordinates: lat: 4.59194
lon: -74.0544
surface_form: bogotá
instance_of: Watercourse
countries: Colombia
coordinates: lat: 5.25
lon: -73.666666666667
On Sundays, Guadalupe Hill and its chapel and statue are visited by tourists and pilgrims from Bogotá, accessing the hill either by road and public transport or via a walking trail to the hilltop. Etymology. Guadalupe Hill is named after Our Lady of Guadalupe of Badajoz, not -as is commonly believed- after the famous Our Lady of Guadalupe in Mexico. Geology.

Geographic entities mentioned:
surface_form: guadalupe hill
instance_of: Mountain
countries: Colombia
coordinates: lat: 4.59194
lon: -74.0544
Geology. The Guadalupe Hill is the type locality for the Campanian-Maastrichtian Guadalupe Group, a sequence of three formations of sandstones and shales; Arenisca Dura, Plaeners, Arenisca de Labor and Arenisca Tierna. The thickness of the Guadalupe Group, defined as formation by some authors, at Guadalupe Hill is. Approximately 53% of the Eastern Hills consists of the Guadalupe Group.

Geographic entities mentioned:
surface_form: guadalupe hill
instance_of: Mountain
countries: Colombia
coordinates: lat: 4.59194
lon: -74.0544
Approximately 53% of the Eastern Hills consists of the Guadalupe Group. The Guadalupe Group is thrusted on top of the younger Guaduas, Bogotá and Cacho Formations by the Bogotá Fault. The NNW-SSE trending eastward dipping thrust fault forms a barrier for aquifers. The creeks (&quot;quebradas&quot;) Manzanares and El Chuscal originate from Guadalupe Hill. History.

Geographic entities mentioned:
surface_form: guadalupe hill
instance_of: Mountain
countries: Colombia
coordinates: lat: 4.59194
lon: -74.0544
At the time of the conquest, the Eastern Hills were a forested natural boundary of the Bogotá savanna. During the early colonial period, the Spanish constructed a cross on Guadalupe Hill as a symbol to protect the capital of the New Kingdom of Granada. The wood of the trees of the Eastern Hills were used for construction and heating in the city that grew steadily until the 19th century.

Geographic entities mentioned:
surface_form: guadalupe hill
instance_of: Mountain
countries: Colombia
coordinates: lat: 4.59194
lon: -74.0544
The first replanting of trees took place in 1855, and a second phase of reforestation happened in 1940. In 1801, Francisco José de Caldas recalculated the height of Guadalupe Hill. Hermitage and statue. The first hermitage on Guadalupe Hill was built in 1656 and blessed during a pilgrimage on September 8 of that year. The hermitage was destroyed by the earthquakes of 1743, 1785 and 1827.

Geographic entities mentioned:
surface_form: guadalupe hill
instance_of: Mountain
countries: Colombia
coordinates: lat: 4.59194
lon: -74.0544
The hermitage was rebuilt in 1945 by Jorge Murcia Riaño and blessed by archbishop Ismael Perdomo. In 1946, the high statue of the Virgin of Guadalupe, sculpted by Gustavo Arcila Uribe, was constructed on top of Guadalupe Hill. In 1967, the chapel and road leading up to it were constructed. Tourism.

Geographic entities mentioned:
surface_form: guadalupe hill
instance_of: Mountain
countries: Colombia
coordinates: lat: 4.59194
lon: -74.0544
The hill can be accessed via a walking trail, used by pilgrims since colonial times, or by the road to Choachí via the Avenida Circunvalar. Public transport to Guadalupe Hill leaves on Sundays from Carrera 10 with Calle 6. Since 1997, a running contest is held to ascend the Guadalupe Hill. Every Sunday, the chapel on the hill receives tourists between 7:00 in the morning and 4:00 in the afternoon.

Geographic entities mentioned:
surface_form: guadalupe hill
instance_of: Mountain
countries: Colombia
coordinates: lat: 4.59194
lon: -74.0544
Guadalupe Hill is the type locality of the Guadalupe Group, a Late Cretaceous sedimentary sequence of sandstones and shales of thick. The formation is being thrust on top of younger strata by the reverse Bogotá Fault as a result of the ongoing Andean orogeny. The hill is the source for the Manzanares and El Chuscal creeks that flow westwards onto the Bogotá savanna.

Geographic entities mentioned:
surface_form: bogotá
instance_of: Watercourse
countries: Colombia
coordinates: lat: 5.25
lon: -73.666666666667
The thickness of the Guadalupe Group, defined as formation by some authors, at Guadalupe Hill is. Approximately 53% of the Eastern Hills consists of the Guadalupe Group. The Guadalupe Group is thrusted on top of the younger Guaduas, Bogotá and Cacho Formations by the Bogotá Fault. The NNW-SSE trending eastward dipping thrust fault forms a barrier for aquifers.

Geographic entities mentioned:
surface_form: bogotá
instance_of: Watercourse
countries: Colombia
coordinates: lat: 5.25
lon: -73.666666666667
surface_form: bogotá
instance_of: Watercourse
countries: Colombia
coordinates: lat: 5.25
lon: -73.666666666667
The creeks (&quot;quebradas&quot;) Manzanares and El Chuscal originate from Guadalupe Hill. History. Guadalupe Hill in the times before the Spanish conquest was one of the sacred hilltops in the religion of the Muisca, the indigenous inhabitants of the Bogotá savanna. They considered the hills sacred and buried their dead in the mountains.

Geographic entities mentioned:
surface_form: bogotá
instance_of: Watercourse
countries: Colombia
coordinates: lat: 5.25
lon: -73.666666666667
Seen from Bolívar Square, at the winter solstice of December, Sué rises exactly over Guadalupe Hill and at the equinoxes of March and September in the valley between Monserrate and Guadalupe. At the time of the conquest, the Eastern Hills were a forested natural boundary of the Bogotá savanna.

Geographic entities mentioned:
surface_form: bogotá
instance_of: Watercourse
countries: Colombia
coordinates: lat: 5.25
lon: -73.666666666667
The wood of the trees of the Eastern Hills were used for construction and heating in the city that grew steadily until the 19th century. This led to deforestation and erosion in the Eastern Hills and when Alexander von Humboldt visited Santa Fe de Bogotá in 1806, he noted &quot;that there was not a single tree left until the open area of Choachí&quot;.

Geographic entities mentioned:
surface_form: bogotá
instance_of: Watercourse
countries: Colombia
coordinates: lat: 5.25
lon: -73.666666666667
The hermitage was destroyed by the earthquakes of 1743, 1785 and 1827. During the presidency of Tomás Cipriano de Mosquera, the hermitage was reconstructed, but affected again by the 1917 Bogotá earthquake. The hermitage was rebuilt in 1945 by Jorge Murcia Riaño and blessed by archbishop Ismael Perdomo.

Geographic entities mentioned:
surface_form: bogotá
instance_of: Watercourse
countries: Colombia
coordinates: lat: 5.25
lon: -73.666666666667
In 1967, the chapel and road leading up to it were constructed. Tourism. The Guadalupe Hill and the statue of the Virgin of Guadalupe are among the main touristic attractions of Bogotá. The top of the hill offers a viewpoint (&quot;mirador&quot;) for the Colombian capital.

Geographic entities mentioned:
surface_form: bogotá
instance_of: Watercourse
countries: Colombia
coordinates: lat: 5.25
lon: -73.666666666667
After passing through about of forest, the highway passes Primrose Spur Road, and enters Primrose. For the next five or so miles (8 km), the route runs on a thin strip of land between the mountains and Kenai Lake. At the northern end of Kenai Lake, the route passes through Crown Point, and provides access to a large campground where Trail Creek empties into Kenai Lake.

Geographic entities mentioned:
surface_form: Kenai Lake
instance_of: Lake
countries: United States
coordinates: lat: 60.418333333333
lon: -149.66666666667
At the northern end of Kenai Lake, the route passes through Crown Point, and provides access to a large campground where Trail Creek empties into Kenai Lake. The highway runs alongside Trail Creek for about, before passing the settlement of Moose Pass. The road continues, passing along Upper Trail Lake for a few miles, before returning to the dense forest, and passing a large mountain range.

Geographic entities mentioned:
surface_form: Upper Trail Lake
instance_of: Group of lakes
countries: United States
coordinates: lat: 60.4917
lon: -149.367
The Seward Highway officially reaches its northern terminus at an intersection with 5th Avenue. AK-1 continues on for a short period as 5th Avenue, before becoming known as the Glenn Highway. History. An stretch of the Seward Highway, traveling from Seward to Kenai Lake was completed in 1923. Another segment of the highway, running between Moose Pass and Hope, was completed in 1928.

Geographic entities mentioned:
surface_form: Kenai Lake
instance_of: Lake
countries: United States
coordinates: lat: 60.418333333333
lon: -149.66666666667
Therefore, he sailed to the shore of Lagoa dos Patos, mistaken for the Rio Grande river, and arriving there on February 19, 1737, founded a prison and built the Fort Jesus, Mary, and Joseph, constituting the origin of the city of Rio Grande, the first center of government in the region.

Geographic entities mentioned:
surface_form: Lagoa dos Patos
instance_of: Lake
countries: Brazil
coordinates: lat: -31.15
lon: -51.39
Problems of pollution, mismanagement, and depletion of water sources in all the major watersheds are becoming especially serious, with several water bodies of enormous importance in critical situations in almost their entire length, such as the Lagoa dos Patos, Lake Guaíba, and the Sinos River; the deforestation of the Atlantic Forest, which preserves only 7% of its original cover and is under constant pressure; the pollution of soils, water, and food by pesticides, using almost twice the national average in a country that is notorious in the use of these chemicals, and the desertification of the &quot;pampa&quot;, associated with the introduction of rice, pine, and eucalyptus monocultures and overexploitation of cattle.

Geographic entities mentioned:
surface_form: Lagoa dos Patos
instance_of: Lake
countries: Brazil
coordinates: lat: -31.15
lon: -51.39
Liard Plateau. ut0wiwudcto6mum2dsubt7k0x4fy" xml:space="preserve">The Liard Plateau is a plateau in far northern British Columbia, Canada, located between the Smith and Liard Rivers, and extending north into the Yukon.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: liard plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 59.6667
lon: -125.5
Liard Plateau. ut0wiwudcto6mum2dsubt7k0x4fy" xml:space="preserve">The Liard Plateau is a plateau in far northern British Columbia, Canada, located between the Smith and Liard Rivers, and extending north into the Yukon.

Geographic entities mentioned:
surface_form: liard plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 59.6667
lon: -125.5
It has been acknowledged as the toughest off-road competition in India. The terrain. The Palar River is a subterranean river that runs across South India. With its source in the Nandi Hills in Karnataka, the river traverses three different states over a distance of 350 km to meet the Bay of Bengal near Kalpakkam in Tamil Nadu.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
The journal covers all aspects of mountains and mountaineering, including expeditions, adventure, art, literature, geography, history, geology, medicine, ethics and the mountain environment, and the history of mountain exploration, from early ascents in the Alps, exploration of the Himalaya and the succession of attempts on Mount Everest, to present-day exploits. Online access.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
from &quot;*h₂wes-&quot; &quot;dwell, pass the night, stay&quot;). And so likely also related to the name of the Latin goddess of the hearth, Vesta, though this connection is questioned by Beekes. Probably related to Umbrian Vesune which should be a dative singular of a *Vesuna, presumed to be a name of a goddess. Perhaps also related to the name of Mount Vesuvius.

Geographic entities mentioned:
surface_form: Mount Vesuvius
instance_of: Mountain
countries: Italy
coordinates: lat: 40.821388888889
lon: 14.425555555556
Protected area. The Paletará Valley is located within the protected area of the Puracé National Natural Park whose main feature is the active stratovolcano Puracé, one of Colombia's most active volcanoes. Four of the country's most important rivers originate within the area: Magdalena River, Cauca River, Japurá River and Patía River. Weather. The average temperature is °C.

Geographic entities mentioned:
surface_form: Puracé
instance_of: Mountain
countries: Colombia
coordinates: lat: 2.3141666666667
lon: -76.394166666667
surface_form: puracé
instance_of: Mountain
countries: Colombia
coordinates: lat: 2.3141666666667
lon: -76.394166666667
The valley presents a flat morphology filled with fine sediments of effusive and pyroclastic material from the neighboring volcanic centers of the area, such as those of the Coconuco Volcanic Chain, the Sotará volcanic complex and a series of phreatomagmatic structures located within the Paletará Valley itself. Geology. The Paletara valley constitutes the inner SW sector of the Paletará Caldera.

Geographic entities mentioned:
surface_form: sotará
instance_of: Mountain
countries: Colombia
coordinates: lat: 2.1080555555556
lon: -76.591944444444
Valle de Paletará. Valle de Paletará is a valley in the Cauca Department on the Colombian Massif located at altitudes between 3000 and 3200 m.a.s.l. It is an almost flat area eroded by the Cauca River, adjacent to the Coconuco Volcanic Chain and other resurgent volcanic structures that exist in the vicinity such as the Yerbabuena Maar. Geography.

Geographic entities mentioned:
surface_form: valle de paletará
instance_of: Valley
countries: Colombia
coordinates: lat: 2.2127777777778
lon: -76.475277777778
Geography. The region called Valle de Paletará is limited by the foot of the Coconucos Volcanic Chain to the northeast and a series of low hills to the southeast called Cerros Cortaderal, Las Tusas, Loma del Apio, Cresta de Gallo and Loma de las Peñas, the which are raised with respect to the valley by a SE-NW fault.

Geographic entities mentioned:
surface_form: valle de paletará
instance_of: Valley
countries: Colombia
coordinates: lat: 2.2127777777778
lon: -76.475277777778
Tumling actually is part of Nepal although there is no restriction for Indians or foreigners with Indian visa. In fact the border between India and Nepal in this part is quite blurred and there is a free way for all. One is able to see the Kangchenjunga Range from here and going forward for about 15 minutes visitors can notice the Mount Everest.

Geographic entities mentioned:
surface_form: Kangchenjunga
instance_of: Mountain
countries: India
Nepal
coordinates: lat: 27.7
lon: 88.133333
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Shaikhdara. Shaikhdara or Shaikh Dara (,) is the most popular locality of Union Council Dubair Bala in Lower Kohistan District of Khyber-Pakhtunkhwa province of Pakistan. Language.

Geographic entities mentioned:
surface_form: shaikhdara
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.14739567
lon: 72.92439314
Shaikhdara. Shaikhdara or Shaikh Dara (,) is the most popular locality of Union Council Dubair Bala in Lower Kohistan District of Khyber-Pakhtunkhwa province of Pakistan. Language.

Geographic entities mentioned:
surface_form: shaikhdara
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.14739567
lon: 72.92439314
surface_form: shaikh dara
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.14739567
lon: 72.92439314
The park has facilities and space for tennis, hiking, disc golf, snowmobiling, sledding and other outdoor activities. The Buffalo Philharmonic Orchestra has held summer concerts at the base of the sledding hill, which provides an amphitheater-like setting. On a clear day, the sledding hill offers views of Buffalo and Lake Erie. Toboggan chutes also operate on the sled hill during the winter.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Niagara Escarpment AVA. Niagara Escarpment is an American Viticultural Area (AVA) in Niagara County, New York along the Niagara Escarpment.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
It was established on September 7, 2005 by the Alcohol and Tobacco Tax and Trade Bureau (TTB), Treasury after reviewing the petition submitted by Michael Von Heckler of Warm Lake Estate Vineyard and Winery proposing an
American viticultural area to be called &quot;Niagara Escarpment.&quot;
The boundary area runs in a narrow Niagara escarpment landscape which is part of a free-draining limestone ridge that also stretches around Lake Ontario and the Canadian province it was named after.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Freyberg Mountains. The Freyberg Mountains () are a group of mountains in Victoria Land, Antarctica, bounded by the Rennick Glacier, Bowers Mountains, Black Glacier, and Evans Névé. They are west of the Victory Mountains and south of the Bowers Mountains. Name.

Geographic entities mentioned:
surface_form: Evans Névé
instance_of: Landform
coordinates: lat: -72.75
lon: 164.5
Location. The Freyberg Mountains lie to the east of the Rennick Glacier and to the south of the Bowers Mountains. The Canham Glacier defines their northwest limit. The Black Glacier defines their eastern limit, separating them from the Leitch Massif, Neall Massif and West Quartzite Range further east. They extend south to the Evans Névé.

Geographic entities mentioned:
surface_form: Evans Névé
instance_of: Landform
coordinates: lat: -72.75
lon: 164.5
Piz Denter. Piz Denter is a mountain of the Lepontine Alps, located on the border between the Swiss cantons of Graubünden and Ticino. On its northern side (Graubünden), it overlooks the valleys of Lake Curnera and Lake Nalps, both drained by tributaries of the Rhine.

Geographic entities mentioned:
surface_form: piz denter
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.57388889
lon: 8.72305556
Griffith Lake. Griffith Lake is a small lake and campsite located in the towns of Peru and Mount Tabor, Vermont, in the Green Mountain National Forest. The site lies on the Long Trail/Appalachian Trail. The area is maintained by the Green Mountain Club and has an on-site caretaker to maintain the tent sites, outhouse, composting toilets, and trails during the peak season.

Geographic entities mentioned:
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.9822
lon: -105.302
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.291666666667
lon: -121.23861111111
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.3053
lon: -105.3
surface_form: griffith lake
instance_of: Lake
countries: United States
coordinates: lat: 43.302777777778
lon: -72.959166666667
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.5175
lon: -121.67305555556
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.563333333333
lon: -122.80694444444
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.700833333333
lon: -105.17805555556
The site lies on the Long Trail/Appalachian Trail. The area is maintained by the Green Mountain Club and has an on-site caretaker to maintain the tent sites, outhouse, composting toilets, and trails during the peak season. During that time, there is a $5 charge for the overnight use of the tent platforms and nearby lean-to shelter.

Geographic entities mentioned:
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.9822
lon: -105.302
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.291666666667
lon: -121.23861111111
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.3053
lon: -105.3
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.5175
lon: -121.67305555556
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.563333333333
lon: -122.80694444444
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.700833333333
lon: -105.17805555556
Griffith Lake. Griffith Lake is a small lake and campsite located in the towns of Peru and Mount Tabor, Vermont, in the Green Mountain National Forest. The site lies on the Long Trail/Appalachian Trail. The area is maintained by the Green Mountain Club and has an on-site caretaker to maintain the tent sites, outhouse, composting toilets, and trails during the peak season.

Geographic entities mentioned:
surface_form: griffith lake
instance_of: Lake
countries: United States
coordinates: lat: 43.302777777778
lon: -72.959166666667
As there are no 'safe' water sources, hikers should be prepared to use a camping-grade water purification system, or to boil their water. Access to Griffith lake is through a combination walking/snowmobile trail. Horses, motorized vehicles, and mountain bikes are not permitted on the access trail.

Geographic entities mentioned:
surface_form: griffith lake
instance_of: Lake
countries: United States
coordinates: lat: 43.302777777778
lon: -72.959166666667
Destroyed in 1945, the gardens were reconstructed 1962‑1995, partly in their original Baroque style. Between 1892 and 1900, prince Leopold zu Salm-Salm created the &quot;Leopold Park&quot;, inspired by Lake Lucerne, with a miniature lake, artificial rocks and a Swiss chalet.

Geographic entities mentioned:
surface_form: Lake Lucerne
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.0194
lon: 8.4011
Engelberg (Leonberg). Engelberg (Leonberg) is a mountain of Baden-Württemberg, Germany. The mountain rises up over the town of Leonberg, Engelberg at a height of. Originally known as Endelberg, it has been called by its current name since the 16th century. The mountain served as a military post with a tall watchtower in the Middle Ages.

Geographic entities mentioned:
surface_form: württemberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.7821
lon: 9.26867
surface_form: engelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.9301
lon: 8.60884
surface_form: engelberg (leonberg)
instance_of: Mountain
countries: Germany
coordinates: lat: 48.8019
lon: 9.02528
Engelberg (Leonberg). Engelberg (Leonberg) is a mountain of Baden-Württemberg, Germany. The mountain rises up over the town of Leonberg, Engelberg at a height of. Originally known as Endelberg, it has been called by its current name since the 16th century. The mountain served as a military post with a tall watchtower in the Middle Ages.

Geographic entities mentioned:
surface_form: engelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.9301
lon: 8.60884
surface_form: engelberg (leonberg)
instance_of: Mountain
countries: Germany
coordinates: lat: 48.8019
lon: 9.02528
Engelberg (Leonberg). Engelberg (Leonberg) is a mountain of Baden-Württemberg, Germany. The mountain rises up over the town of Leonberg, Engelberg at a height of. Originally known as Endelberg, it has been called by its current name since the 16th century. The mountain served as a military post with a tall watchtower in the Middle Ages.

Geographic entities mentioned:
surface_form: engelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.9301
lon: 8.60884
surface_form: engelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.8019
lon: 9.02528
Originally known as Endelberg, it has been called by its current name since the 16th century. The mountain served as a military post with a tall watchtower in the Middle Ages. During the 19th century, parts of Engelberg were allotted to local citizens for gardening, and a forest was planted in 1840. The old watchtower was renovated by the Leonberg municipal council in 1842.

Geographic entities mentioned:
surface_form: engelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.9301
lon: 8.60884
surface_form: engelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.8019
lon: 9.02528
The old watchtower was renovated by the Leonberg municipal council in 1842. The area became a popular destination for walkers. The current Engelberg tower was opened in 1928, originally as a water tower for a golf course on the nearby heath. Disused as a water tower since 1982, it is now a well known lookout tower for tourists.

Geographic entities mentioned:
surface_form: engelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.9301
lon: 8.60884
surface_form: engelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.8019
lon: 9.02528
Visitors climb 123 steps to reach the viewing platform, for a panoramic view of the mountains around Heilbronn; the Black Forest is also visible in the distance when the weather is clear. There is a concentration camp memorial near the old Engelberg tunnel, which was converted into a production facility where prisoners were forced to work during the Second World War.

Geographic entities mentioned:
surface_form: engelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.9301
lon: 8.60884
surface_form: engelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.8019
lon: 9.02528
Pir Khidir Zinda. The Pir Khidir Zinda (), also called Khidir Zunja and Beshbarmag-piri, is a mausoleum, pilgrimage site, and sacred place for Muslims, located on the slopes of Beşbarmaq rock, in the Siyazan rayon of Azerbaijan. The mausoleum site is located within the “Beshbarmag Mountain” State Historical Cultural and Nature Reserve, proclaimed in 2020.

Geographic entities mentioned:
surface_form: Beşbarmaq
instance_of: Mountain
countries: Azerbaijan
coordinates: lat: 40.958333333333
lon: 49.232222222222
Buskerud extended from Hurum at the Oslofjord to the Halling mountains and Hardanger. The county was conventionally divided into traditional districts. These were Hallingdal, Numedal, Ringerike, Lower Buskerud, which was originally part of Vestfold, and Western Vingulmark. Hallingdal consisted of Flå, Nes, Gol, Hemsedal, Ål and Hol. Numedal consisted of Flesberg, Rollag and Nore og Uvdal.

Geographic entities mentioned:
surface_form: Hallingdal
instance_of: Valley
countries: Norway
coordinates: lat: 60.633333333333
lon: 9.05
surface_form: Numedal
instance_of: Valley
countries: Norway
coordinates: lat: 60
lon: 9.2
These were Hallingdal, Numedal, Ringerike, Lower Buskerud, which was originally part of Vestfold, and Western Vingulmark. Hallingdal consisted of Flå, Nes, Gol, Hemsedal, Ål and Hol. Numedal consisted of Flesberg, Rollag and Nore og Uvdal. Ringerike consisted of Hole, Krødsherad, Modum, Ringerike and Sigdal. Western Vingulmark consisted of Hurum and Røyken.

Geographic entities mentioned:
surface_form: Numedal
instance_of: Valley
countries: Norway
coordinates: lat: 60
lon: 9.2
Buskerud's western part was a mountainous plateau with forested valleys and high, grassy pastures; its eastern part contains a lowland basin with many lakes and streams. Tyrifjorden and Krøderen were the biggest lakes. Numedalslågen, the third longest river in Norway, starting in Hordaland, ran through Buskerud unto Vestfold where it reached the sea, while river Begna sweeps into lake Sperillen.

Geographic entities mentioned:
surface_form: Tyrifjorden
instance_of: Lake
countries: Norway
coordinates: lat: 60.033333333333
lon: 10.133333333333
Tyrifjorden and Krøderen were the biggest lakes. Numedalslågen, the third longest river in Norway, starting in Hordaland, ran through Buskerud unto Vestfold where it reached the sea, while river Begna sweeps into lake Sperillen. History. Buskerud was separated from Akershus as an amt of its own in 1685, but the amt was smaller than today.

Geographic entities mentioned:
surface_form: Sperillen
instance_of: Lake
countries: Norway
coordinates: lat: 60.466666666667
lon: 10.05
History. Buskerud was separated from Akershus as an amt of its own in 1685, but the amt was smaller than today. It then consisted of the present districts Eiker, Hallingdal, and Ringerike. The area of the present municipalities of Flesberg, Hurum, Kongsberg, Lier, Nore og Uvdal, Rollag and Røyken were transferred from Akershus amt to Buskerud amt in 1760. The name ' was changed to ' in 1919.

Geographic entities mentioned:
surface_form: Hallingdal
instance_of: Valley
countries: Norway
coordinates: lat: 60.633333333333
lon: 9.05
During the 10th century, Norway's kings Olaf Tryggvason and Olaf Haraldsson grew up at Bønsnes in Ringerike. In the valley of Numedal, silver was mined in Kongsberg from the 17th century until discontinued in 1957. Weapons industry had been developed in Kongsberg from 1814, and various high tech industry companies now represent the town's major employers.

Geographic entities mentioned:
surface_form: Numedal
instance_of: Valley
countries: Norway
coordinates: lat: 60
lon: 9.2
The Algic urheimat is thought to have been located in the Northwestern United States somewhere between the suspected homeland of the Algonquian branch (to the west of Lake Superior according to Ives Goddard) and the earliest known location of the Wiyot and Yurok (along the middle Columbia River according to Whistler). Classification of Algic.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Kauaeranga Valley. Kauaeranga Valley is a valley created by the Kauaeranga River, which flows from the Coromandel Range southwest to the Firth of Thames at Thames, New Zealand in the North Island. It contains the settlement of Kauaeranga () on the Coromandel Peninsula. It is located near Thames, in the Thames-Coromandel District in the Waikato region. It covers a land area of 179.01 km2.

Geographic entities mentioned:
surface_form: kauaeranga valley
instance_of: Valley
countries: New Zealand
coordinates: lat: -37.122
lon: 175.63
It contains the settlement of Kauaeranga () on the Coromandel Peninsula. It is located near Thames, in the Thames-Coromandel District in the Waikato region. It covers a land area of 179.01 km2. Kauaeranga Valley Road is the only significant road in the valley. History.

Geographic entities mentioned:
surface_form: kauaeranga valley
instance_of: Valley
countries: New Zealand
coordinates: lat: -37.122
lon: 175.63
Lack of roads and severe weather made farming difficult, so land was allowed to revert to bush. There was little farmed land left by the late 1960s. Residents first requested that the Auckland Education Board establish a school in the valley in 1896, but the Kauaeranga Valley School did not open until 1903. The initial roll was 30 students.

Geographic entities mentioned:
surface_form: kauaeranga valley
instance_of: Valley
countries: New Zealand
coordinates: lat: -37.122
lon: 175.63
The Kauaeranga Valley Dairy Company opened a factory in November 1907 to produce milk and butter. It closed in September 1908 and moved to Parawai, where it was defunct by 1910. A road between Thames and Tairua was proposed in 1909, with the recommended route going through the Kauaeranga Valley, up the Piraunui Valley, across the Hihi saddle, and down the third branch of Tairua River.

Geographic entities mentioned:
surface_form: kauaeranga valley
instance_of: Valley
countries: New Zealand
coordinates: lat: -37.122
lon: 175.63
After the Second World War, a route further south along the Kirikiri Stream gained favour, and the road which is now was built from 1961, opening to traffic in March 1967. From 1957, an electric power line was built from Thames, through the Kauaeranga Valley and north to Coroglen. This was complete by 1959.

Geographic entities mentioned:
surface_form: kauaeranga valley
instance_of: Valley
countries: New Zealand
coordinates: lat: -37.122
lon: 175.63
Tourism. Kauaeranga Visitor Centre is an information centre run by the Department of Conservation. It accepts payment for camping at the numerous campsites further along the road, and organises accommodation at two cottages next to the centre. The centre is from Thames on Kauaeranga Valley Road. The road is sealed to this point, and gravel for the remaining.

Geographic entities mentioned:
surface_form: kauaeranga valley
instance_of: Valley
countries: New Zealand
coordinates: lat: -37.122
lon: 175.63
The centre is from Thames on Kauaeranga Valley Road. The road is sealed to this point, and gravel for the remaining. Short walks, day tramps and multi-day tramps start from the road beyond the centre. The Pinnacles Walk is a tramp from the end of Kauaeranga Valley Road to the summit of a volcanic plug, above sea level. The return tramp takes eight hours and is often done over two days.

Geographic entities mentioned:
surface_form: kauaeranga valley
instance_of: Valley
countries: New Zealand
coordinates: lat: -37.122
lon: 175.63
There are bacteria, for example, living in Lake Whillans, half a mile below the ice of Antarctica; in the absence of sunlight, they must rely on organic material from elsewhere, perhaps decaying matter from glacier melt water or minerals from the underlying rock.

Geographic entities mentioned:
surface_form: Lake Whillans
instance_of: Lake
coordinates: lat: -84.25
lon: -153.5
Municipal council. The municipal council () of Fedje is made up of 15 representatives that are elected to four year terms. The tables below show the current and historical composition of the council by political party. Geography. The highest point on Fedje is the high hill called Fedjebjørnen. The largest lake is Storevatnet. Islands.

Geographic entities mentioned:
surface_form: Fedjebjørnen
instance_of: Mountain
countries: Norway
coordinates: lat: 60.764652777778
lon: 4.7352
Lake County is one of the 36 counties in the U.S. state of Oregon. As of the 2020 census, the population was 8,160. Its county seat is Lakeview. The county is named after the many lakes found within its boundaries, including Lake Abert, Summer Lake, Hart Lake, and Goose Lake. Lake County is in the high desert region known as the Oregon Outback, on the northwestern edge of the Great Basin.

Geographic entities mentioned:
surface_form: Lake Abert
instance_of: Lake
countries: United States
coordinates: lat: 42.641666666666666
lon: -120.225
Peter Skene Ogden led Hudson's Bay Company trappers to Goose Lake in 1827. In 1832, the Hudson Bay trappers under John Work were in the Goose Lake Valley and their journals mentioned Hunter's Hot Springs. Work's expedition visited Warner Lakes and Lake Abert and camped at Crooked Creek in the Chandler Park area. There they documented eating wild plums, which still grow in the area.

Geographic entities mentioned:
surface_form: Goose Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.6
lon: -120.4
Peter Skene Ogden led Hudson's Bay Company trappers to Goose Lake in 1827. In 1832, the Hudson Bay trappers under John Work were in the Goose Lake Valley and their journals mentioned Hunter's Hot Springs. Work's expedition visited Warner Lakes and Lake Abert and camped at Crooked Creek in the Chandler Park area. There they documented eating wild plums, which still grow in the area.

Geographic entities mentioned:
surface_form: Warner Lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 42.4499
lon: -119.851
surface_form: Lake Abert
instance_of: Lake
countries: United States
coordinates: lat: 42.641666666666666
lon: -120.225
Lake County was created from Jackson and Wasco Counties on October 24, 1874, by the State Legislature. It then included the present Klamath County and all of the present Lake County except Warner Valley. In 1882, land was assigned to create Klamath County, and in 1885 the Warner area from Grant County was added. Linkville, now Klamath Falls, was the first county seat. M.

Geographic entities mentioned:
surface_form: Warner Valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
It is the third-largest county in Oregon. Lake County ranges in elevation from. The highest point in Lake County is Crane Mountain. The mountain is located north of the California border. Lake County has six other peaks with elevations above, all located in the southern half of the county. Hager Mountain is the highest peak in the northern part of the county.

Geographic entities mentioned:
surface_form: Crane Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.06281835
lon: -120.24083202
The mountain is located north of the California border. Lake County has six other peaks with elevations above, all located in the southern half of the county. Hager Mountain is the highest peak in the northern part of the county. The area includes alkali lakes, high desert scrub, and forests of Western Juniper, Ponderosa Pine, and Lodgepole Pine in the hills and mountains.

Geographic entities mentioned:
surface_form: Hager Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.009444444444
lon: -121.03166666667
Fossil Lake is an area nearby where many fossils of prehistoric animals have been identified. Glass Buttes is an obsidian complex in the extreme northeast corner of the county. Crack in the Ground, northeast of Christmas Valley is a long fissure with ice in its floor year round. Big Hole, Hole-in-the-Ground, and Fort Rock are ancient maar craters in the northwestern part of the county.

Geographic entities mentioned:
surface_form: Glass Buttes
instance_of: Mountain
countries: United States
coordinates: lat: 43.5573646
lon: -120.0744166
Other sights in North Lake include the Lost Forest, Crack-in-the-ground, and Hole-in-the-ground
Oregon sunstones are found north of Plush. The Oregon sunstone is Oregon's state gemstone. Glass Buttes are high desert mountains in northeastern Lake County named for the large deposits of obsidian found on their slopes. This is a favorite collecting area for rockhounds.

Geographic entities mentioned:
surface_form: Glass Buttes
instance_of: Mountain
countries: United States
coordinates: lat: 43.5573646
lon: -120.0744166
Other areas of interest include, Abert Lake and Abert Rim, Goose Lake, Hunter's Hot Springs and its Old Perpetual Geyser, Lake County Museum, Schminck Memorial Museum, Lake County Round-Up Museum, Schmink Museum, Warner Canyon ski area, Gearhart Mountain Wilderness, Sheldon National Wildlife Refuge, Summer Lake Hot Springs, sunstones (Oregon's state gemstone) near Plush, Warner Wetlands, Summer Lake Wildlife Area and sections of the Fremont National Forest of the Fremont–Winema National Forests.

Geographic entities mentioned:
surface_form: Warner Wetlands
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 42.4499
lon: -119.851
Svartsjön, Hanveden. Svartsjön is a lake in Stockholm County, Södermanland, Sweden.

Geographic entities mentioned:
surface_form: svartsjön, hanveden
instance_of: Lake
countries: Sweden
coordinates: lat: 59.143472222222
lon: 18.041388888889
Svartsjön, Hanveden. Svartsjön is a lake in Stockholm County, Södermanland, Sweden.

Geographic entities mentioned:
surface_form: svartsjön
instance_of: Lake
countries: Sweden
coordinates: lat: 59.143472222222
lon: 18.041388888889
The route is a scenic highway, following the North Shore of Lake Superior, and is part of the Lake Superior Circle Tour designation that runs through Minnesota, Ontario, Michigan, and Wisconsin. This roadway was designated U.S. Highway 61 (US 61) until 1991.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
of MN 61 from Duluth to Two Harbors is a four-lane expressway officially designated the Arthur Rohweder Memorial Highway. There are no markers on the highway showing this designation, but there is a plaque at a wayside. The roadway is located close to and in many places next to Lake Superior. Sights include forests, wildlife, cliffs, state parks, and a national monument.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
After almost being imprisoned by Aeolus under Gaea's orders, the trio manages to escape and end up in San Francisco. They defeat the giant Enceladus at Mount Diablo and rescue Piper's father, who was being held captive. After saving Piper's dad, she gives him a potion given to her by Aphrodite and he forgets about the mythical world.

Geographic entities mentioned:
surface_form: Mount Diablo
instance_of: Mountain
countries: United States
coordinates: lat: 37.881697781
lon: -121.914154997
It has been a popular retreat from the heat of Rajasthan and neighboring Gujarat for centuries. The mountain is home to several Hindu temples, including the Adhar Devi Temple (also known as Arbuda Devi Temple), carved out of the solid rock; the Shri Raghunathji Temple; and a shrine and temple to Dattatreya built atop the Guru Shikhar peak; and the Achaleshwar Mahadev Temple (1412).

Geographic entities mentioned:
surface_form: Guru Shikhar
instance_of: Mountain
countries: India
coordinates: lat: 24.665277777778
lon: 72.781944444444
surface_form: guru shikhar
instance_of: Mountain
countries: India
coordinates: lat: 24.665277777778
lon: 72.781944444444
The Achalgarh Fort, built in the 14th century by Kumbha of Mewar, is nearby and at its center is the popular visitor attraction of the Nakki Lake. The Toad Rock is on a hill near the lake. Close to the fort is the Achaleshwar Mahadev Temple, a popular Shiva temple. Also, Achal Fort Jain Temple, Shantinath Jain Temple (1513) is equally famous.

Geographic entities mentioned:
surface_form: Nakki Lake
instance_of: Lake
countries: India
coordinates: lat: 24.596138888889
lon: 72.703066666667
surface_form: nakki lake
instance_of: Lake
countries: India
coordinates: lat: 24.596138888889
lon: 72.703066666667
In answer to his prayer, a youth arose from the Agnikunda (fire-altar) — the first Agnivansha. Achalgarh Fort is one of more attractive place which was built by Parmar kings. The Dilwara Jain Temple is a pilgrimage centre for the Jain religion among the lush green hills of Aravali. The Dilwara Jain Temple is located at a distance of 2.5 km from Mount Abu. Vastupala designed the temple.

Geographic entities mentioned:
surface_form: hills
instance_of: Mountain
countries: India
coordinates: lat: 23.166666666667
lon: 92.833333333333
Mount Abu. Mount Abu (), known as Arbudgiri in Jain tradition, is a hill station in the Aravalli Range in the Sirohi district of the state of Rajasthan in western India. Here, the mountain forms a rocky plateau 22 km long by 9 km wide. It is referred to as 'an oasis in the desert' as its heights are home to rivers, lakes, waterfalls and evergreen forests.

Geographic entities mentioned:
surface_form: mount abu
instance_of: Mountain
countries: India
coordinates: lat: 24.5925
lon: 72.708333333333
It is also home to numerous Jain and Hindu temples. History. The ancient name of Mount Abu is Arbuda. In the Puranas, the region has been referred to as &quot;Arbudaranya&quot; (&quot;forest of &quot;Arbuda&quot;) and 'Abu' is a diminutive of this ancient name. It is believed that sage Vashistha retired to the southern spur at Mount Abu following his differences with sage Vishvamitra.

Geographic entities mentioned:
surface_form: mount abu
instance_of: Mountain
countries: India
coordinates: lat: 24.5925
lon: 72.708333333333
There is another history story according to which a serpent named &quot;Arbuda&quot; saved the life of Nandi (Lord Shiva's bull). The incident happened on the mountain that is currently known as Mount Abu and so the mountain is named &quot;Arbudaranya&quot; after that incident which gradually became Abu.

Geographic entities mentioned:
surface_form: mount abu
instance_of: Mountain
countries: India
coordinates: lat: 24.5925
lon: 72.708333333333
The incident happened on the mountain that is currently known as Mount Abu and so the mountain is named &quot;Arbudaranya&quot; after that incident which gradually became Abu. According to a legend, the sage Vashistha performed a yajna at the peak of Mount Abu, to seek from the gods a provision for the defense of righteousness on earth.

Geographic entities mentioned:
surface_form: mount abu
instance_of: Mountain
countries: India
coordinates: lat: 24.5925
lon: 72.708333333333
Achalgarh Fort is one of more attractive place which was built by Parmar kings. The Dilwara Jain Temple is a pilgrimage centre for the Jain religion among the lush green hills of Aravali. The Dilwara Jain Temple is located at a distance of 2.5 km from Mount Abu. Vastupala designed the temple. Vimal Shah built it between the 11th century and the 13th century.

Geographic entities mentioned:
surface_form: mount abu
instance_of: Mountain
countries: India
coordinates: lat: 24.5925
lon: 72.708333333333
Close to the fort is the Achaleshwar Mahadev Temple, a popular Shiva temple. Also, Achal Fort Jain Temple, Shantinath Jain Temple (1513) is equally famous. The Durga Ambika Mata Temple lies in a cleft of rock in Jagat, just outside Mount Abu town. The mountain is also the home to a number of Jain temples including Dilwara Temples, a complex of temples carved out of white marble.

Geographic entities mentioned:
surface_form: mount abu
instance_of: Mountain
countries: India
coordinates: lat: 24.5925
lon: 72.708333333333
Also, Achal Fort Jain Temple, Shantinath Jain Temple (1513) is equally famous. The Durga Ambika Mata Temple lies in a cleft of rock in Jagat, just outside Mount Abu town. The mountain is also the home to a number of Jain temples including Dilwara Temples, a complex of temples carved out of white marble. The Dilwara Temples or Delvada Temples are located about 2½ kilometers from the Mount Abu town.

Geographic entities mentioned:
surface_form: mount abu
instance_of: Mountain
countries: India
coordinates: lat: 24.5925
lon: 72.708333333333