Sarmila/GeoWiki-Features huggingface dataset:
The northern side of the mountain is heavily glaciated and is part of a ski area. The Theodulhorn is the easternmost summit of the range descending from the south-east ridge of Matterhorn, named &quot;Furgggrat&quot;. It is named for Theodul Pass, which is in turn named for Saint Theodul, patron saint of the Valais.

Geographic entities mentioned:
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
surface_form: theodulhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.949333333333
lon: 7.7084166666667
Theodulhorn. The Theodulhorn (- 3,469 m) is a mountain of the Pennine Alps, overlooking the Theodul Pass on the border between Switzerland and Italy. It lies south of Zermatt (in Valais) and east of Breuil-Cervinia (in the Aosta Valley). The northern side of the mountain is heavily glaciated and is part of a ski area.

Geographic entities mentioned:
surface_form: theodulhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.949333333333
lon: 7.7084166666667
Burberg. The Burberg, also called the Buerberg and Bürberg, is a hill, in the Eifel mountains in Germany. It rises near Schutz in the county of Vulkaneifel in the state of Rhineland-Palatinate. Location. The Burberg is located within the Volcanic Eifel Nature Park and the Hinterbüsch. At its southeastern foot is the village of Schutz on whose territory the hill is situated.

Geographic entities mentioned:
surface_form: burberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.1338
lon: 6.75133
It rises near Schutz in the county of Vulkaneifel in the state of Rhineland-Palatinate. Location. The Burberg is located within the Volcanic Eifel Nature Park and the Hinterbüsch. At its southeastern foot is the village of Schutz on whose territory the hill is situated. 3.1 km west-southwest of the summit is the village of Weidenbach.

Geographic entities mentioned:
surface_form: burberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.1338
lon: 6.75133
Rowe the date may go back even to 2100 BC. Early ceramics have been found on the central coast at the large settlement of Las Haldas, at Huarmey, as well as at some other sites in the Casma River region, and in Lima area. Chavín potters (900–200 BC) on the Peruvian coast created distinctive stirrup spout vessels, both incised and highly burnished.

Geographic entities mentioned:
surface_form: Casma River
instance_of: Watercourse
countries: Peru
coordinates: lat: -9.44944
lon: -78.38237
Vessels were often effigies portraying elaborate scenes. A fineline painting tradition emerged, which resembles Greek black-figure pottery. A 29,000-square-foot Moche ceramics workshop with numerous kilns was discovered in at the mountain Mayal in the Chicama Valley. The workshop specialized in female figurines.

Geographic entities mentioned:
surface_form: Chicama Valley
instance_of: Valley
countries: Peru
The workshop specialized in female figurines. The Tiwanaku and Wari cultures shared dominance of the Andes, roughly from 500 to 1000 BCE. The Tiwanaku civilizations originated in Lake Titicaca region of Bolivia, and a staff-bearing deity figured largely in their artwork. Tiwanaku artists continued the tradition of naturalistic, ceramic portrait vessels.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
Tuftonboro, New Hampshire. Tuftonboro is a town in Carroll County, New Hampshire, United States. The population was 2,467 at the 2020 census. Bounded on the southwest by Lake Winnipesaukee, Tuftonboro includes the villages of Tuftonboro Corner, Center Tuftonboro, Melvin Village and Mirror Lake. History.

Geographic entities mentioned:
surface_form: Lake Winnipesaukee
instance_of: Lake
countries: United States
coordinates: lat: 43.598888888889
lon: -71.323055555556
Geography. According to the United States Census Bureau, the town has a total area of, of which are land and are water, comprising 18.06% of the town. Tuftonboro is drained by the Melvin River and Beech River, tributaries of Lake Winnipesaukee. Mirror Lake is in the south, and Dan Hole Pond is in the north.

Geographic entities mentioned:
surface_form: Lake Winnipesaukee
instance_of: Lake
countries: United States
coordinates: lat: 43.598888888889
lon: -71.323055555556
Tuftonboro is drained by the Melvin River and Beech River, tributaries of Lake Winnipesaukee. Mirror Lake is in the south, and Dan Hole Pond is in the north. The highest point in Tuftonboro is the south peak of Mount Shaw, elevation above sea level, on the town's northwestern boundary. The northern portion of Tuftonboro is occupied by the Ossipee Mountains.

Geographic entities mentioned:
surface_form: Dan Hole Pond
instance_of: Lake
countries: United States
coordinates: lat: 43.725
lon: -71.223333333333
Tuftonboro is drained by the Melvin River and Beech River, tributaries of Lake Winnipesaukee. Mirror Lake is in the south, and Dan Hole Pond is in the north. The highest point in Tuftonboro is the south peak of Mount Shaw, elevation above sea level, on the town's northwestern boundary. The northern portion of Tuftonboro is occupied by the Ossipee Mountains.

Geographic entities mentioned:
surface_form: Mount Shaw
instance_of: Mountain
countries: United States
coordinates: lat: 43.743938888889
lon: -71.274111111111
The two had split in 1950. Saint-Gédéon-de-Beauce is a site of Canam, one of the largest steel joist factories in Canada. Geography. Saint-Gédéon-de-Beauce is the only municipality whose territory straddles the Chaudière River that does not have a bridge across it. Notable people. Novelist Jacques Poulin was born in Saint-Gédéon-de-Beauce.

Geographic entities mentioned:
surface_form: Chaudière River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.742777777777775
lon: -71.2786111111111
One of the earliest figures involved in this effort was Sir Henry Wellcome, a British-American pharmaceutical entrepreneur and philanthropist. In the early 1900s, Wellcome financed several archaeological expeditions in Sudan, where he employed aerial photography using a box kite to document excavations in Jebel Moya, Sudan.

Geographic entities mentioned:
surface_form: Jebel Moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
They were separated by &quot;Hubs&quot;, Mountain Hub and River Hub. Mountain Hub sub-camps: Alp, Carpathian, Pyrenees, Snowdonia. River Hub sub-camps: Danube, Oder, Rhine, Tagus. There was also an adult sub-camp, Lake Geneva. The Plaza was the central area of the campsite, located in front of Hylands House. The Plaza was the location for all services that the participants needed during EuroJam.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
The flanks have white warts. The legs have dark bands. The dorsum sometimes has a unique pattern as shown in the image. Distribution and ecology. This species has only been observed on Mt. Kupe and Meked on the nearby Bakossi Mountains. They can be found in torrents with rocky beds, on rocks with algae, and on surrounding vegetation at a height of. Etymology. The name &quot;P.

Geographic entities mentioned:
surface_form: Mt. Kupe
instance_of: Mountain
countries: Cameroon
coordinates: lat: 4.801
lon: 9.707
It is bounded on the north-east by the Sound of Mull, which separates Mull from the mainland of Scotland. In the centre is the long Loch Frisa, the largest freshwater loch in Mull. The small Ledmore river takes its overflow, feeding into the Aros River, which flows into the Sound. The catchment area of Locha Frisa is about, only 7% of the parish.

Geographic entities mentioned:
surface_form: Loch Frisa
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.566666666667
lon: -6.0833333333333
The small Ledmore river takes its overflow, feeding into the Aros River, which flows into the Sound. The catchment area of Locha Frisa is about, only 7% of the parish. The main offshore islands are Ulva, Gometra, Little Colonsay, Staffa and Calve Island. Tobermory on the north-east coast, founded in 1788, is the capital of, and until 1973, the only burgh on the Isle of Mull. Demographics.

Geographic entities mentioned:
surface_form: Gometra
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.491111111111
lon: -6.2869444444444
Mount Brooker. Mount Brooker () is a mountain, high, standing at the head of Webb Glacier and forming the last major summit in the southeast part of the Allardyce Range of South Georgia. The feature was identified as &quot;Pic&quot; (meaning Peak) or &quot;Pikstock&quot; by the German group of the International Polar Year Investigations, 1882–83. It was first climbed in 1955 by Ian M.

Geographic entities mentioned:
surface_form: pikstock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -54.5
lon: -36.233333333333
Mount Brooker. Mount Brooker () is a mountain, high, standing at the head of Webb Glacier and forming the last major summit in the southeast part of the Allardyce Range of South Georgia. The feature was identified as &quot;Pic&quot; (meaning Peak) or &quot;Pikstock&quot; by the German group of the International Polar Year Investigations, 1882–83. It was first climbed in 1955 by Ian M.

Geographic entities mentioned:
surface_form: mount brooker
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -54.5
lon: -36.233333333333
The city was strongly fortified at that period. Walls lined both sides of the Mtkvari River, and three forts protected it. The main citadel, Armazi, on Mount Bagineti controlled the entrance from the south and east, Tsitsamuri, at the base of Mount Jvari from the north, and Sarkine from the west.

Geographic entities mentioned:
surface_form: Mount Bagineti
instance_of: Mountain
countries: Georgia
coordinates: lat: 41.837944444444446
lon: 44.72172222222222
In southern Scania, runestones can be tied to large estates that also had churches constructed on their land. In the Mälaren Valley, the runestones appear to be placed so that they mark essential parts of the domains of an estate, such as courtyard, grave field, and borders to neighbouring estates. Runestones usually appear as single monuments and more rarely as pairs.

Geographic entities mentioned:
surface_form: Mälaren Valley
instance_of: Valley
countries: Sweden
coordinates: lat: 59.5
lon: 16.75
Pontes is a historical place name formerly used in Roman Britain. Sabrina Valley. An ice-free valley between Pontes Ridge and Sabrina Ridge. Named in association with Sabrina Ridge. Sabrina Ridge. A bare rock ridge between Sabrina Valley and Tamarus Valley, south of Derrick Peak. Sabrina is a historical name formerly used in Roman Britain for the River Severn.

Geographic entities mentioned:
surface_form: Tamarus Valley
instance_of: Valley
coordinates: lat: -80.1667
lon: 156.333
surface_form: derrick peak
instance_of: Mountain
coordinates: lat: -80.0667
lon: 156.383
Named after Lee DeGalan, contractor employee in charge of U.S. Antarctic Project (USAP) cargo shipments out of Port Hueneme, CA, for more than 20 years. Metaris Valley. A small, rounded cirque valley with steep sides and residual névé, lying west of Derrick Peak. Named in association with Britannia by a University of Waikato (N.Z.) geological party, 1978-79, led by M.J. Selby.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: derrick peak
instance_of: Mountain
coordinates: lat: -80.0667
lon: 156.383
Magnis Valley. Broad ice-free valley, long, lying west of Derrick Peak. Magnis is a historical place name formerly used in Roman Britain. Magnis Ridge. A rock ridge west of Derrick Peak, forming the divide between Magnis Valley and Metaris Valley. Named in association with Magnis Valley. DeGalan Peak. A peak that rises to at the head of Magnis Valley.

Geographic entities mentioned:
surface_form: the divide
instance_of: Body of water
coordinates: lat: -60.73333
lon: -45.16667
surface_form: derrick peak
instance_of: Mountain
coordinates: lat: -80.0667
lon: 156.383
Location. Derrick Peak is in the north of the Britannia Range, overlooking the Hatherton Glacier to the north, which forms the boundary with the Darwin Mountains. It is east of a line of relatively ice-free valleys and ridges along the south side of Hatherton Glacier, north of Mount Henderson and west of Johnstone Ridge and Dusky Ridge.

Geographic entities mentioned:
surface_form: mount henderson
instance_of: Mountain
coordinates: lat: -67.7
lon: 63.0667
Derrick Peak. Derrick Peak () is a prominent ice-free peak, high, overlooking the south side of Hatherton Glacier, west of the north end of Johnstone Ridge. Name. Derrick Peak was named by the Advisory Committee on Antarctic Names for Robert O.

Geographic entities mentioned:
surface_form: derrick peak
instance_of: Mountain
coordinates: lat: -80.0667
lon: 156.383
Name. Derrick Peak was named by the Advisory Committee on Antarctic Names for Robert O. Derrick of the United States Weather Bureau, who served as assistant to the United States Antarctic Research Program Representative at Christchurch from 1960 until his death in 1966. Location.

Geographic entities mentioned:
surface_form: derrick peak
instance_of: Mountain
coordinates: lat: -80.0667
lon: 156.383
Location. Derrick Peak is in the north of the Britannia Range, overlooking the Hatherton Glacier to the north, which forms the boundary with the Darwin Mountains. It is east of a line of relatively ice-free valleys and ridges along the south side of Hatherton Glacier, north of Mount Henderson and west of Johnstone Ridge and Dusky Ridge.

Geographic entities mentioned:
surface_form: derrick peak
instance_of: Mountain
coordinates: lat: -80.0667
lon: 156.383
surface_form: britannia
instance_of: Mountain
coordinates: lat: -64.7167
lon: -62.6833
Most of the nearby features were named in association with Britannia by a University of Waikato (New Zealand) geological party, 1978-79, led by M.J. Selby. Lindum Valley. Ice-filled valley that opens northward to Hatherton Glacier, lying west-northwest of Derrick Peak. Lindum is an old Roman place name for present-day Lincoln. Magnis Valley. Broad ice-free valley, long, lying west of Derrick Peak.

Geographic entities mentioned:
surface_form: derrick peak
instance_of: Mountain
coordinates: lat: -80.0667
lon: 156.383
Selby. Lindum Valley. Ice-filled valley that opens northward to Hatherton Glacier, lying west-northwest of Derrick Peak. Lindum is an old Roman place name for present-day Lincoln. Magnis Valley. Broad ice-free valley, long, lying west of Derrick Peak. Magnis is a historical place name formerly used in Roman Britain. Magnis Ridge.

Geographic entities mentioned:
surface_form: derrick peak
instance_of: Mountain
coordinates: lat: -80.0667
lon: 156.383
Named in association with Britannia by a University of Waikato (N.Z.) geological party, 1978-79, led by M.J. Selby. Metaris is the historical name of a bay in Roman Britain, known today as The Wash. Onnum Valley. An ice-free valley between Derrick Peak and Onnum Ridge. Named in association with Onnum Ridge. Operose Peak. A peak above Onnum Valley to the southwest of Derrick Peak.

Geographic entities mentioned:
surface_form: derrick peak
instance_of: Mountain
coordinates: lat: -80.0667
lon: 156.383
An ice-free valley between Derrick Peak and Onnum Ridge. Named in association with Onnum Ridge. Operose Peak. A peak above Onnum Valley to the southwest of Derrick Peak. The steep lower slopes of the peak are of Beacon sandstone; the top, high, is made up of a thick dolerite sill. The Latin name means laborious or requiring great pain reflecting the steepness of the slopes. Onnum Ridge.

Geographic entities mentioned:
surface_form: derrick peak
instance_of: Mountain
coordinates: lat: -80.0667
lon: 156.383
The steep lower slopes of the peak are of Beacon sandstone; the top, high, is made up of a thick dolerite sill. The Latin name means laborious or requiring great pain reflecting the steepness of the slopes. Onnum Ridge. A mountain spur that descends northeast to McCraw Glacier, south of Derrick Peak. Onnum is a historical placename formerly used in Roman Britain. Pontes Ridge.

Geographic entities mentioned:
surface_form: derrick peak
instance_of: Mountain
coordinates: lat: -80.0667
lon: 156.383
Onnum Ridge. A mountain spur that descends northeast to McCraw Glacier, south of Derrick Peak. Onnum is a historical placename formerly used in Roman Britain. Pontes Ridge. A mountain spur that descends eastward to McCraw Glacier, south of Derrick Peak. Pontes is a historical place name formerly used in Roman Britain. Sabrina Valley. An ice-free valley between Pontes Ridge and Sabrina Ridge.

Geographic entities mentioned:
surface_form: derrick peak
instance_of: Mountain
coordinates: lat: -80.0667
lon: 156.383
It is east of a line of relatively ice-free valleys and ridges along the south side of Hatherton Glacier, north of Mount Henderson and west of Johnstone Ridge and Dusky Ridge. Most of the nearby features were named in association with Britannia by a University of Waikato (New Zealand) geological party, 1978-79, led by M.J. Selby. Lindum Valley.

Geographic entities mentioned:
surface_form: britannia
instance_of: Mountain
coordinates: lat: -64.7167
lon: -62.6833
Antarctic Project (USAP) cargo shipments out of Port Hueneme, CA, for more than 20 years. Metaris Valley. A small, rounded cirque valley with steep sides and residual névé, lying west of Derrick Peak. Named in association with Britannia by a University of Waikato (N.Z.) geological party, 1978-79, led by M.J. Selby. Metaris is the historical name of a bay in Roman Britain, known today as The Wash.

Geographic entities mentioned:
surface_form: britannia
instance_of: Mountain
coordinates: lat: -64.7167
lon: -62.6833
Okstindbreen comprises an ice field including Vestisen, Vestre Okstindbreen, Austre Okstindbreen, Bessedørbreen, Steikvassbreen, Vestre Svartfjellbreen, and Oksfjellbreen. The largest outlet glacier from Okstindbreen is Austre Okstindbreen, measured to be 14 km² in 1996. It drains towards the valley Oksfjelldalen, located northeast of Oksskolten, the highest mountain in Northern Norway.

Geographic entities mentioned:
surface_form: Oksskolten
instance_of: Mountain
countries: Norway
coordinates: lat: 66.012222222222
lon: 14.338611111111
The iron ore was quarried at two mountains in modern Austria still called &quot;Erzberg&quot; &quot;ore mountain&quot; today, one at Hüttenberg, Carinthia and the other at Eisenerz, Styria, separated by. The latter is the site of the modern Erzberg mine.

Geographic entities mentioned:
surface_form: Erzberg mine
instance_of: Mountain
countries: Austria
coordinates: lat: 47.525
lon: 14.911666666667
Vesyoloye, Altai Krai. Vesyoloye () is a rural locality (a selo) in Slavgorod, Altai Krai, Russia. The population was 36 as of 2013. There is 1 street. Geography. Vesyoloye lies in the Kulunda Steppe, to the west of lake Maloye Yarovoye and to the NNW of lake Belenkoye.

Geographic entities mentioned:
surface_form: Maloye Yarovoye
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.041855555556
lon: 79.128811111111
Petite rivière Savane. The Petite rivière Savane (&quot;English: Little Savannah River&quot;) is a tributary of the Sainte-Anne River, flowing on the north bank of the Saint Lawrence River, in the territory unorganized from Lac-Jacques-Cartier, in the La Côte-de-Beaupré Regional County Municipality, in the administrative region of Capitale-Nationale, in the province of Quebec, in Canada.

Geographic entities mentioned:
surface_form: rivière savane
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.319999
lon: -71.000833
surface_form: petite rivière savane
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.293888
lon: -70.751388
surface_form: petite rivière
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.226597
lon: -64.434607
Petite rivière Savane. The Petite rivière Savane (&quot;English: Little Savannah River&quot;) is a tributary of the Sainte-Anne River, flowing on the north bank of the Saint Lawrence River, in the territory unorganized from Lac-Jacques-Cartier, in the La Côte-de-Beaupré Regional County Municipality, in the administrative region of Capitale-Nationale, in the province of Quebec, in Canada.

Geographic entities mentioned:
surface_form: rivière savane
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.319999
lon: -71.000833
surface_form: jacques-cartier
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.671388888889
lon: -71.747222222222
surface_form: petite rivière savane
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.293888
lon: -70.751388
surface_form: petite rivière
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.226597
lon: -64.434607
The water level of the river varies with the seasons and the precipitation; the spring flood occurs in March or April. Geography. The Petite rivière Savane flows on the southwest shore of the Sainte-Anne River (Beaupré), in the unorganized territory of Lac-Jacques-Cartier, facing the northern limit of Saint-Tite-des-Caps. This confluence is located west of the northwest shore of the St.

Geographic entities mentioned:
surface_form: rivière savane
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.319999
lon: -71.000833
surface_form: jacques-cartier
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.671388888889
lon: -71.747222222222
From the confluence of the Petite Savane River, the current flows over generally towards the southwest by the course of the Sainte-Rivière Anne, which crosses downtown Beaupré, to the northwest shore of the Saint Lawrence River. Toponymy. The toponym &quot;Petite rivière Savane&quot; was formalized on March 25, 1997 at the Place Names Bank of the Commission de toponymie du Québec.

Geographic entities mentioned:
surface_form: rivière savane
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.319999
lon: -71.000833
surface_form: petite rivière savane
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.293888
lon: -70.751388
surface_form: petite rivière
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.226597
lon: -64.434607
Beinn an Òir. Beinn an Òir (Gaelic for &quot;mountain of gold&quot;) is the highest peak of the Paps of Jura on the island of Jura, Scotland. It is the highest peak on the island, standing at 785 metres, and is thereby a Corbett. Beinn an Òir is frequently climbed along with the other two peaks forming the Paps: Beinn Shiantaidh and Beinn a' Chaolais.

Geographic entities mentioned:
surface_form: Beinn Shiantaidh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.900969444444
lon: -5.9801111111111
surface_form: Beinn a' Chaolais
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.888019444444
lon: -6.0187888888889
surface_form: beinn shiantaidh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.900969444444
lon: -5.9801111111111
surface_form: beinn a' chaolais
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.888019444444
lon: -6.0187888888889
Beinn an Òir. Beinn an Òir (Gaelic for &quot;mountain of gold&quot;) is the highest peak of the Paps of Jura on the island of Jura, Scotland. It is the highest peak on the island, standing at 785 metres, and is thereby a Corbett. Beinn an Òir is frequently climbed along with the other two peaks forming the Paps: Beinn Shiantaidh and Beinn a' Chaolais.

Geographic entities mentioned:
surface_form: beinn an òir
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.901980555556
lon: -6.0042305555556
Beinn an Òir is frequently climbed along with the other two peaks forming the Paps: Beinn Shiantaidh and Beinn a' Chaolais. The most usual route for this ascent starts from the bridge over the Corran River, and Beinn an Òir is invariably the second peak to be climbed, regardless of which order of peaks is chosen for the route.

Geographic entities mentioned:
surface_form: beinn an òir
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.901980555556
lon: -6.0042305555556
The most usual route for this ascent starts from the bridge over the Corran River, and Beinn an Òir is invariably the second peak to be climbed, regardless of which order of peaks is chosen for the route. Alternatively, it is possible to avoid the other two peaks and climb Beinn an Òir from either of the bealachs that separate it from its neighbours.

Geographic entities mentioned:
surface_form: beinn an òir
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.901980555556
lon: -6.0042305555556
Aralsor (;) is a bittern salt lake group in Bokey Orda District, West Kazakhstan Region, Kazakhstan. The lake lies about to the east of the Russian border, north of the R-97 Highway (Kazakhstan). The road connects Saykyn station of the Volga Railway near lake Botkul with the village of Taipak on the right bank of the Ural River. Salt extraction on an industrial scale is carried out at the lake.

Geographic entities mentioned:
surface_form: Botkul
instance_of: Lake
countries: Russia
Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 48.766666666667
lon: 46.666666666667
Flowing from the north, the Ashchyozek is the main river in the area. A short channel connects the end of the river with Aralsor. This channel is periodically dry. The Kamys-Samar Lakes lie to the east. Flora and fauna. There is desert and steppe vegetation in the terraced flat areas of the Aralsor lakeside cliff-like formations.

Geographic entities mentioned:
surface_form: Kamys-Samar Lakes
instance_of: Group of lakes
Lake
countries: Kazakhstan
coordinates: lat: 48.93916667
lon: 49.65666667
Aralsor. Aralsor (;) is a bittern salt lake group in Bokey Orda District, West Kazakhstan Region, Kazakhstan. The lake lies about to the east of the Russian border, north of the R-97 Highway (Kazakhstan). The road connects Saykyn station of the Volga Railway near lake Botkul with the village of Taipak on the right bank of the Ural River.

Geographic entities mentioned:
surface_form: aralsor
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 49.04
lon: 48.2347222
Salt extraction on an industrial scale is carried out at the lake. Geography. Lying at the northern edge of the Ryn Desert, east of the Russian border, Aralsor is an endorheic lake group. The main water body is colored pink and is surrounded by a string of smaller lakes and salt pans. The latter contain clay salt-mud deposits covered with a crust of halite reaching.

Geographic entities mentioned:
surface_form: aralsor
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 49.04
lon: 48.2347222
The main water body is colored pink and is surrounded by a string of smaller lakes and salt pans. The latter contain clay salt-mud deposits covered with a crust of halite reaching. The western and eastern banks of Aralsor are steep and cliff-like in places. Flowing from the north, the Ashchyozek is the main river in the area. A short channel connects the end of the river with Aralsor.

Geographic entities mentioned:
surface_form: aralsor
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 49.04
lon: 48.2347222
The latter contain clay salt-mud deposits covered with a crust of halite reaching. The western and eastern banks of Aralsor are steep and cliff-like in places. Flowing from the north, the Ashchyozek is the main river in the area. A short channel connects the end of the river with Aralsor. This channel is periodically dry. The Kamys-Samar Lakes lie to the east. Flora and fauna.

Geographic entities mentioned:
surface_form: aralsor
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 49.04
lon: 48.2347222
The Kamys-Samar Lakes lie to the east. Flora and fauna. There is desert and steppe vegetation in the terraced flat areas of the Aralsor lakeside cliff-like formations. In the ravines of the shoreline cliffs there are plants such as tamarisk, anabasis, &quot;Halocnemum&quot; and winterfat, providing a habitat and breeding ground for the local fauna of small mammals, birds and reptiles.

Geographic entities mentioned:
surface_form: aralsor
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 49.04
lon: 48.2347222
Supervised by the Department of Natural Resources, the Caspian forests produced 820,000 cubic meters of timber products in 2004, more than 90 percent of which was for industrial use. The largest and most valuable woodland areas are in the Caspian region and the northern slopes of the Elburz Mts., where many of the forests are commercially exploitable and include both hardwoods and softwoods.

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
Using two HX range trucks (a 340 hp 4×4 40M and a 440 hp 6×6 58) the expedition aimed to reach the highest point on earth accessible to motor vehicles – the 6890 m-tall Ojos del Salado, the world's highest active volcano, located on the border of Chile and Argentina. In order to set a new world record the vehicles would have to reach an altitude of at least 6,690 metres above sea level.

Geographic entities mentioned:
surface_form: Ojos del Salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
Mount Tabor, Indiana. Mount Tabor is an unincorporated community in Bean Blossom Township, Monroe County, in the U.S. state of Indiana. History. Mount Tabor was platted in 1828. The community was named directly or indirectly after Mount Tabor, in the Middle East. A post office was established at Mount Tabor in 1831, and remained in operation until it was discontinued in 1860.

Geographic entities mentioned:
surface_form: Mount Tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
Common Nubian origin of Bassar, Bassari and Bassa. There is a Bassa community around the Adamaoua mountain range and a Bassari community around the Fouta-Djalon mountain range with whom we have distant origins in Meroé precisely around the Djebel Barkal mountain. The Nataka clan of Bassar in Togo would be descendants of the Nubian pharaoh Natakamani.

Geographic entities mentioned:
surface_form: Djebel Barkal
instance_of: Mountain
countries: Sudan
coordinates: lat: 18.5368
lon: 31.8276
Other lakes in the region, such as Izmis lake, are harder to enter and need to be done so through trekking. Mahodand Lake is a large lake in the Swat Valley, located approximately 40 km from Kalam, in the Usho Sub-valley, at the base of the Hindu Kush mountains. Another notable lake in the Kalam Valley is the Kundol Lake, located in the north of Utror region, 19 km away from Kalam.

Geographic entities mentioned:
surface_form: Mahodand Lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.70861111111111
lon: 72.65333333333334
surface_form: kalam
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.4801
lon: 72.5874
surface_form: kush
instance_of: Mountain
countries: Pakistan
coordinates: lat: 28.8171
lon: 66.5674
The coldest month, January, has an average temperature of. Lakes. Kalam has numerous alpine glacial lakes. Two notable lakes in the Kalam Valley are the Mahodand lake and Kandol lake, both of which are frequently visited due to their easy access routes. Other lakes in the region, such as Izmis lake, are harder to enter and need to be done so through trekking.

Geographic entities mentioned:
surface_form: mahodand lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.70861111111111
lon: 72.65333333333334
surface_form: kandol lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.41888888888889
lon: 72.43305555555555
surface_form: kalam valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.4801
lon: 72.5874
The coldest month, January, has an average temperature of. Lakes. Kalam has numerous alpine glacial lakes. Two notable lakes in the Kalam Valley are the Mahodand lake and Kandol lake, both of which are frequently visited due to their easy access routes. Other lakes in the region, such as Izmis lake, are harder to enter and need to be done so through trekking.

Geographic entities mentioned:
surface_form: izmis lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.4
lon: 72.37694444444445
Located north from Mingora and at an elevation of about above sea level, the valley itself provides a plateau that is located above the river and is used for farming. There are a number of visible mountains, also visible from Matiltan, a valley close to Kalam Valley, including Mount Falak Sar at, and another unnamed peak at high. Climate.

Geographic entities mentioned:
surface_form: falak sar
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.68277778
lon: 72.78527778
surface_form: kalam valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.4801
lon: 72.5874
Mahodand Lake is a large lake in the Swat Valley, located approximately 40 km from Kalam, in the Usho Sub-valley, at the base of the Hindu Kush mountains. Another notable lake in the Kalam Valley is the Kundol Lake, located in the north of Utror region, 19 km away from Kalam. It is located at the base of the Hindu Kush mountains.

Geographic entities mentioned:
surface_form: kundol lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.41888888888889
lon: 72.43305555555555
surface_form: kalam valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.4801
lon: 72.5874
surface_form: kalam
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.4801
lon: 72.5874
Kalam Valley. Kalam (Kalami, Pashto and) is a valley located in the Swat Kohistan region of Swat District in the Khyber Pakhtunkhwa province, Pakistan. It is the site where the Swat River forms as a result of the confluence of two major tributaries, the Gabral and Ushu rivers.

Geographic entities mentioned:
surface_form: kalam valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.4801
lon: 72.5874
Kalam Valley. Kalam (Kalami, Pashto and) is a valley located in the Swat Kohistan region of Swat District in the Khyber Pakhtunkhwa province, Pakistan. It is the site where the Swat River forms as a result of the confluence of two major tributaries, the Gabral and Ushu rivers.

Geographic entities mentioned:
surface_form: kalam
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.4801
lon: 72.5874
Climate. With a mild, generally warm and temperate climate, Kalam features a Humid continental climate (&quot;Dfa&quot;) under the Köppen climate classification. The average temperature in Kalam is, while the annual precipitation averages. November is the driest month with of precipitation, while April, the wettest month, has an average precipitation of.

Geographic entities mentioned:
surface_form: kalam
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.4801
lon: 72.5874
Mahodand Lake is a large lake in the Swat Valley, located approximately 40 km from Kalam, in the Usho Sub-valley, at the base of the Hindu Kush mountains. Another notable lake in the Kalam Valley is the Kundol Lake, located in the north of Utror region, 19 km away from Kalam. It is located at the base of the Hindu Kush mountains.

Geographic entities mentioned:
surface_form: kush
instance_of: Mountain
countries: Pakistan
coordinates: lat: 28.8171
lon: 66.5674
He participated in the Haganah's first rifle course and became an instructor. One of his students was Yigal Allon. He was then responsible for commanding the Afula area forces, and from 1939 the entire Jezreel Valley. During this time he worked with Orde Wingate. In 1942 he was tasked with curbing the activities of the Irgun and Lehi in his area under the nickname &quot;Saadya&quot;.

Geographic entities mentioned:
surface_form: Jezreel Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
Belleayre Mountain. Belleayre Mountain is a ski resort in Highmount, New York, United States, located on a mountain of the same name within Catskill Park. It is owned by the Olympic Regional Development Authority (ORDA). There are 62 trails served by 4 chairlifts and 1 gondola with a vertical drop of.

Geographic entities mentioned:
surface_form: a mountain of the same name
instance_of: Mountain
countries: United States
coordinates: lat: 42.11592
lon: -74.49793
Its name is derived from two words, Shiva(शिव) and Har(हर), these both are names of Lord Shiva, it is named so due to the large number of temples in the city. Agriculture is the mainstay. It is one of the most flood-affected districts in Bihar, due to over flooding of the Bagmati and Budhi Gandak rivers. Devkuli is a holy place popular for ancient temple of Lord Shiva.

Geographic entities mentioned:
surface_form: Budhi Gandak
instance_of: Watercourse
countries: India
coordinates: lat: 25.43388889
lon: 86.60694444
Abraham of Galich. Abraham of Galich (; also Chukhlomsky or Gorodetsky; died 20 July 1375) was an abbot of the Russian Orthodox Church. He was a disciple of Sergius of Radonezh, and later went on to found four monasteries on Lake Chukhloma, in the region of Galich in present-day Kostroma Oblast. His feast day is on 20 July. Life and devotion. The birthplace and secular name of Abraham is unknown.

Geographic entities mentioned:
surface_form: Lake Chukhloma
instance_of: Lake
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 58.783333333333
lon: 42.616666666667
After some time, with the blessing of Sergius of Radonezh, Abraham went to the Galich princedom, where he founded the first monastery in the Galich region, named &quot;Avraamiyev Novozaozersky&quot; () in honor of the Dormition of the Most Holy Theotokos on the north-east shore of Galich Lake.

Geographic entities mentioned:
surface_form: Galich Lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 58.4065
lon: 42.2985
In the legend of Abraham, it is said that he settled in the domain of Prince Dimitry of Galich, who possessed Galich in the years 1360–1363. Later, Abraham founded another three monasteries; one of them is the Gorodets Monastery in honor of the &quot;Protection of the Holy Virgin&quot; located on the northern shore of Lake Chukhloma. Death.

Geographic entities mentioned:
surface_form: Lake Chukhloma
instance_of: Lake
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 58.783333333333
lon: 42.616666666667
Salen Mountain. 9qy3d6ysjtstygt1sh98wj1a1bh1" xml:space="preserve">#REDIRECT Sør Rondane Mountains

Geographic entities mentioned:
surface_form: salen
instance_of: Mountain
coordinates: lat: -72.0833
lon: 25.45
The third hall, in a separate impressive presentation, contains a large diorama which provides a sweeping view of the overall area of Sangiran, with volcanoes such as Mount Lawu in the background and humans and animals in the foreground, as it is imagined to have been around 1 million years ago.

Geographic entities mentioned:
surface_form: Mount Lawu
instance_of: Mountain
countries: Indonesia
coordinates: lat: -7.625
lon: 111.19166666667
In 1775 he made the first ascent of the Buet (3096 m) by the now usual route from the Pierre à Bérard, on which the great flat rock known as the Table au Chantre still preserves his memory. In 1784–1785 he was the first traveller to attempt the ascent of Mont Blanc (not conquered till 1786), but neither then nor later (1788) did he succeed in reaching its summit.

Geographic entities mentioned:
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
In total, 158 canoeists from 19 nations took part in the canoe races. All these countries had sent in entries before the deadline; the only late entry came from Latvia, which was as a result excluded from participating in the canoeing competitions. The competitions were held on August 7 and 8, 1936. They were held on a regatta course at Grünau on the Langer See.

Geographic entities mentioned:
surface_form: Langer See
instance_of: Lake
countries: Germany
coordinates: lat: 52.4052
lon: 13.6271
Distribution and habitat. This subspecies of &quot;A. moschatum&quot; grows in rainforest, often with &quot;Nothofagus moorei&quot;, at altitudes between between Barrington Tops and the Blue Mountains. Historical uses. The 1889 book &quot;The Useful Native Plants of Australia&quot; records that &quot;The fragrant bark of this tree has been used as tea in Tasmania.

Geographic entities mentioned:
surface_form: Barrington Tops
instance_of: Landform
countries: Australia
coordinates: lat: -31.94998
lon: 151.52687
The town sheltered thousands of refugees from nearby occupied areas. The Nehaj Fortress was completed in 1558 on the hill Nehaj, which at the time was outside of town (today it is wholly within the town's borders.)
Some of the Senj's towers; names were listed as Radomerić (east); Lipica and Pope Leo's (north); Ladarska, Gatska, and Šabac (west); and Zvancić, and Tulac (south).

Geographic entities mentioned:
surface_form: Nehaj
instance_of: Mountain
countries: Croatia
coordinates: lat: 44.98677778
lon: 14.90330556
Gen. John E. Smith. With the arrival of Sherman's force, Grant was prepared to take the offensive and break Bragg's siege. He assigned Sherman to assault the right flank of Bragg's army, at the north end of Missionary Ridge, with three of his four divisions and other troops; this attack was intended to play the major role for the Union.

Geographic entities mentioned:
surface_form: Missionary Ridge
instance_of: Landform
countries: United States
coordinates: lat: 34.986388888889
lon: -85.278611111111
Assabaska. Assabaska is a Saulteaux First Nation reserve in northwestern Ontario on Lake of the Woods. It is shared between the Big Grassy First Nation and the Ojibways of Onigaming First Nation. The Assabaska reserve was created in 1999 as a part of a land claim settlement in 1999. History. The lands that are now part of the Assabaska reserve were originally intended to become Reserve No.

Geographic entities mentioned:
surface_form: Lake of the Woods
instance_of: Lake
countries: Canada
United States
coordinates: lat: 49.09027777777778
lon: -95.2388888888889
At 09:07, &quot;Steregushchiy&quot; sank southeast of Mount Laoteshan and from the Lushun Lighthouse with the loss of 49 members of her crew. &quot;Shinonome&quot; later participated in the Battle of the Yellow Sea in August 1904 and the Battle of Tsushima in May 1905, among other actions. During the Battle of Tsushima, she served as flagship of the 3rd Destroyer Division.

Geographic entities mentioned:
surface_form: Mount Laoteshan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 36.191666666667
lon: 120.59166666667
Of the rest of the land, 5.2% is settled (buildings or roads), and the remainder (3.7%) is non-productive (rivers, glaciers or mountains). The former municipality is located in the Ilanz sub-district of the Surselva district. It is located on a terrace in the southern Vorderrhein valley. It consists of the village of Sevgein and the settlement of Isla near Ilanz.

Geographic entities mentioned:
surface_form: Vorderrhein
instance_of: Watercourse
countries: Switzerland
coordinates: lat: 46.6325
lon: 8.6744444444444
Most of its terrain consists of rolling downland, sometimes lightly wooded, lying at altitudes between 1,800&ndash;2,593 metres (6,560&ndash;7,544 feet). Mount Nyangani, the highest point in Zimbabwe, lies in the centre of the park and Mutarazi Falls, Zimbabwe's highest waterfall, is in the south of the park.

Geographic entities mentioned:
surface_form: Mount Nyangani
instance_of: Mountain
countries: Zimbabwe
coordinates: lat: -18.311111111111
lon: 32.850555555556
The rainbow trout is most widespread within the park's dams and streams but brown trout and American brook trout are also present. Geography and geology. The park is dominated by Mount Nyangani which lies in the centre and is the highest mountain in Zimbabwe. The park is well watered by numerous streams and rivers. The central and eastern parts of the park form part of the Zambezi Basin.

Geographic entities mentioned:
surface_form: Mount Nyangani
instance_of: Mountain
countries: Zimbabwe
coordinates: lat: -18.311111111111
lon: 32.850555555556
Archaeological, historical cultural sites. Fifteenth to seventeenth century ruins of the Ziwa people (upland culture) have been found throughout Nyanga. The ruins include homesteads, centred on pit structures thought to have been used as cattle-pens and larger hill-top settlements, referred to as Forts.

Geographic entities mentioned:
surface_form: Ziwa
instance_of: Mountain
countries: Zimbabwe
coordinates: lat: -18.1333
lon: 32.6333
Hiking. There are numerous hiking paths leading to most of the waterfalls and many of the ruins, and along the rivers and mountains in the park. The main route up Mount Nyangani is a hike, and has views across the park, much of Nyanga District and further into Mozambique. Horse riding.

Geographic entities mentioned:
surface_form: Mount Nyangani
instance_of: Mountain
countries: Zimbabwe
coordinates: lat: -18.311111111111
lon: 32.850555555556
In 1963, the &quot;Schweizerische Aktionskomitee pro Tödi-Greina-Bahn&quot; (Swiss Action Committee for the Tödi-Greina Railway), which had representatives from several cantonal governments, commissioned a study to examine the feasibility of a Tödi–Greina railway. These plans were not pursued.

Geographic entities mentioned:
surface_form: Tödi
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.811111111111
lon: 8.9147222222222
With only minor topographical prominence the peak is not naturally noticeable from a distance, although it is easily identifiable due to the large number of antennas near its summit. It is a subsidiary peak of nearby San Gabriel Peak. Quartz diorite is the dominant bedrock.

Geographic entities mentioned:
surface_form: San Gabriel Peak
instance_of: Mountain
countries: United States
coordinates: lat: 34.2433
lon: -118.098
These contributions led to an understanding that the universe is not static, but expanding. This concept is the basis of the Big Bang theory of cosmology. In 1926, Albert Abraham Michelson made what was then the most precise calculation of the speed of light at the time by measuring the round-trip travel time of light between Mount Wilson and Mount San Antonio away. Transmission.

Geographic entities mentioned:
surface_form: Mount San Antonio
instance_of: Mountain
countries: United States
coordinates: lat: 34.2889
lon: -117.647
surface_form: mount wilson
instance_of: Mountain
countries: United States
coordinates: lat: 34.2238
lon: -118.062
surface_form: mount wilson
instance_of: Mountain
countries: United States
coordinates: lat: 34.2238
lon: -118.062
surface_form: mount wilson
instance_of: Mountain
countries: United States
coordinates: lat: 37.8392
lon: -107.991
surface_form: mount wilson
instance_of: Mountain
countries: United States
coordinates: lat: 37.8392
lon: -107.991
Mount Wilson (California). Mount Wilson is at the peak of the San Gabriel Mountains, located within the San Gabriel Mountains National Monument and Angeles National Forest in Los Angeles County, California. With only minor topographical prominence the peak is not naturally noticeable from a distance, although it is easily identifiable due to the large number of antennas near its summit.

Geographic entities mentioned:
surface_form: mount wilson
instance_of: Mountain
countries: United States
coordinates: lat: 34.2238
lon: -118.062
surface_form: mount wilson
instance_of: Mountain
countries: United States
coordinates: lat: 37.8392
lon: -107.991
In 1891, Thaddeus S. C. Lowe incorporated the Pasadena & Mount Wilson Railroad with the plan of building a scenic mountain railroad to the summit of Mt. Wilson. At the same time, land and easement disputes between camp owners Steils and Strain were going on over the public and private use of the Mount Wilson Trail.

Geographic entities mentioned:
surface_form: mt. wilson
instance_of: Mountain
countries: United States
coordinates: lat: 34.2238
lon: -118.062
surface_form: mt. wilson
instance_of: Mountain
countries: United States
coordinates: lat: 37.8392
lon: -107.991