Sarmila/GeoWiki-Features huggingface dataset:
Bhomat. Bhomat (also referred to as Bhumat; Hindi: भोमट or भूमट) is a mountainous and forested area in southern Rajasthan, covering all or parts of the tehsils of Kotra, Jhadol and Kherwara in Udaipur district. During British rule, the region was also referred to as 'Hilly Tracts of Mewar'. Name.

Geographic entities mentioned:
surface_form: bhomat
instance_of: Valley
countries: India
coordinates: lat: 24.433333333333334
lon: 73.3
Bhomat. Bhomat (also referred to as Bhumat; Hindi: भोमट or भूमट) is a mountainous and forested area in southern Rajasthan, covering all or parts of the tehsils of Kotra, Jhadol and Kherwara in Udaipur district. During British rule, the region was also referred to as 'Hilly Tracts of Mewar'. Name.

Geographic entities mentioned:
surface_form: bhomat
instance_of: Valley
countries: India
coordinates: lat: 24.433333333333334
lon: 73.3
surface_form: भोमट
instance_of: Valley
countries: India
coordinates: lat: 24.433333333333334
lon: 73.3
During British rule, the region was also referred to as 'Hilly Tracts of Mewar'. Name. The name 'Bhomat' is based on the understanding that land tenures known as &quot;bhum&quot; were held by &quot;jagirdars&quot; in the region. But as per details provided by Mewar State, Govt. of India accepted that the Rajputs who held villages in Bhomat were not Bhumias, but Jagirdars. Geography.

Geographic entities mentioned:
surface_form: bhomat
instance_of: Valley
countries: India
coordinates: lat: 24.433333333333334
lon: 73.3
During British rule, the region was also referred to as 'Hilly Tracts of Mewar'. Name. The name 'Bhomat' is based on the understanding that land tenures known as &quot;bhum&quot; were held by &quot;jagirdars&quot; in the region. But as per details provided by Mewar State, Govt. of India accepted that the Rajputs who held villages in Bhomat were not Bhumias, but Jagirdars. Geography.

Geographic entities mentioned:
surface_form: bhomat
instance_of: Valley
countries: India
coordinates: lat: 24.433333333333334
lon: 73.3
surface_form: bhomat
instance_of: Valley
countries: India
coordinates: lat: 24.433333333333334
lon: 73.3
Geography. The Bhomat region is wide in the east-west direction and stretches approximately in the north-south axis. It covers approximately.Geographically, Bhomat is divided in three sub-regions: its western area is called Bhader (Hindi: भाडेर), the central area is called Wakal (after the Wakal River; Hindi: वाकल) and the eastern area is called Khadak (Hindi: खड़क).

Geographic entities mentioned:
surface_form: bhomat
instance_of: Valley
countries: India
coordinates: lat: 24.433333333333334
lon: 73.3
It covers approximately.Geographically, Bhomat is divided in three sub-regions: its western area is called Bhader (Hindi: भाडेर), the central area is called Wakal (after the Wakal River; Hindi: वाकल) and the eastern area is called Khadak (Hindi: खड़क). Primary rivers of the Bhomat are Sabarmati, Vakal, and Som. History.

Geographic entities mentioned:
surface_form: bhomat
instance_of: Valley
countries: India
coordinates: lat: 24.433333333333334
lon: 73.3
Primary rivers of the Bhomat are Sabarmati, Vakal, and Som. History. In the 15th century, Rana Kumbha is credited with building fortresses in the Bhomat region with the goal of containing revolts among the Bhils of the area. In the 16th century, the Bhomat region was the shelter for the Ranas of Mewar when times of military crises caused by the Mughals.

Geographic entities mentioned:
surface_form: bhomat
instance_of: Valley
countries: India
coordinates: lat: 24.433333333333334
lon: 73.3
These &quot;Jagirdars&quot; were known as &quot;bhumias&quot; (i.e., ones holding a &quot;bhum&quot; land tenure) and owed only nominal allegiance to the Mewar State. For approximately a century during British paramountcy over Mewar State, the Bhomat represented a political unit divided in two sub-divisions - Kherwara Bhomat to the east and Kotra Bhomat to the east. Population.

Geographic entities mentioned:
surface_form: bhomat
instance_of: Valley
countries: India
coordinates: lat: 24.433333333333334
lon: 73.3
surface_form: bhomat
instance_of: Valley
countries: India
coordinates: lat: 24.433333333333334
lon: 73.3
surface_form: bhomat
instance_of: Valley
countries: India
coordinates: lat: 24.433333333333334
lon: 73.3
Mount Synge. Mount Synge is located NE of the head of the Blaeberry River and straddles the Continental Divide marking the Alberta-British Columbia border. It was named in 1918 after Captain Millington Henry Synge (1823–1907), British Army officer and author. __NOTOC__
Climate. Based on the Köppen climate classification, Mt.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount synge
instance_of: Mountain
countries: Canada
coordinates: lat: 51.80555555555556
lon: -116.66222222222223
Mount Synge. Mount Synge is located NE of the head of the Blaeberry River and straddles the Continental Divide marking the Alberta-British Columbia border. It was named in 1918 after Captain Millington Henry Synge (1823–1907), British Army officer and author. __NOTOC__
Climate. Based on the Köppen climate classification, Mt.

Geographic entities mentioned:
surface_form: mount synge
instance_of: Mountain
countries: Canada
coordinates: lat: 51.80555555555556
lon: -116.66222222222223
Winter temperatures can drop below with wind chill factors below. Geology. Like other mountains in Banff Park, Mount Synge is composed of sedimentary rock laid down from the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.

Geographic entities mentioned:
surface_form: mount synge
instance_of: Mountain
countries: Canada
coordinates: lat: 51.80555555555556
lon: -116.66222222222223
Saadat Ali Khan I. Saadat Khan Nishapuri (born Mir Muhammad Amin; – 19 March 1739) was the first Nawab of the Kingdom of Awadh from 26 January 1722 to 1739 and the son of Muhammad Nasir. At age 25, he accompanied his father on the final campaign of the Mughal Emperor Aurangzeb against the Marathas in the Deccan, and the emperor awarded him the title of Khan Bahadur for his service. Early life.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Nizam-ul-Mulk killed Dilawar Khan (Syed Hussain Ali Khan's agent) at the Asirgarh Fort in June 1720 and killed Sayyid Alam Khan, a relative (nephew, brother's son) of the Sayyid brothers, in August. Hussain Ali Khan decided to march to the Deccan Plateau, and Hassan Ali Khan agreed to march towards Delhi. Mughal Emperor Muhammad Shah also started for the Deccan from Agra.

Geographic entities mentioned:
surface_form: Deccan Plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Invasion of Canada (1812). Hull was partly the victim of his government's poor preparation for war and poor communication. He had repeatedly urged his superiors while he was governor to build a naval fleet on Lake Erie in order to defend Detroit, Fort Mackinac, and Fort Dearborn, but his requests were ignored by General Henry Dearborn, the commander of the northeast.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
The defences of the fortress at that time consisted of a stone wall 28 feet high and 14 feet thick, with seven towers. Near the northeastern part of the fortress was a castle, which itself consisted of a stone wall and three towers. The main defence of the fortress was the Neva river itself, along with Lake Ladoga, which together encircled the entire fort.

Geographic entities mentioned:
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
Siege. then of about twelve thousand men, Peter the Great and his army advanced to lay siege to the fortress of Nöteborg. Nöteborg had originally been built by the people of Novgorod four centuries earlier, under the name of Orekhovo or Oreshek, on a small island of the river Neva, just where it flows out from Lake Ladoga.

Geographic entities mentioned:
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
They have been introduced to other parts of the world, including New Zealand and Patagonia. Introduced Chinook salmon are thriving in Lake Michigan and Michigan's western rivers. A large Chinook is a prized and sought-after catch for a sporting angler. The flesh of the salmon is also highly valued for its dietary nutritional content, which includes high levels of important omega-3 fatty acids.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Introduced populations. In 1967, the Michigan Department of Natural Resources introduced Chinook into Lake Michigan and Lake Huron to control the alewife, an invasive species of nuisance fish from the Atlantic Ocean. In the 1960s, alewives constituted 90% of the biota in these lakes. Coho salmon had been introduced the year before, and the program was successful.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
As of December 2022, the plan is in its monitoring phase, in which ODFW are studying 10,000 hatchery-born spring-run Chinook released in certain tributaries of Upper Klamath Lake. Lake Michigan. Introduced Chinook salmon in Lake Michigan are sought after by tourists enjoying chartered fishing trips.

Geographic entities mentioned:
surface_form: Upper Klamath Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.392222222222
lon: -121.88027777778
Gora Ulun. Gora Ulun (, &quot;Mount Ulun&quot;) is a mountain in Khabarovsk Krai (Eastern Siberia), Russia and officially the highest point of the Badzhal Range (Баджа́льский хребет) with an elevation of. Geography. The Badzhal Range where the peak rises is a mountain chain with a length of approximately 220 kilometers.

Geographic entities mentioned:
surface_form: gora ulun
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 50.508888888889
lon: 134.32638888889
surface_form: ulun
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 50.508888888889
lon: 134.32638888889
Gora Ulun. Gora Ulun (, &quot;Mount Ulun&quot;) is a mountain in Khabarovsk Krai (Eastern Siberia), Russia and officially the highest point of the Badzhal Range (Баджа́льский хребет) with an elevation of. Geography. The Badzhal Range where the peak rises is a mountain chain with a length of approximately 220 kilometers.

Geographic entities mentioned:
surface_form: gora ulun
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 50.508888888889
lon: 134.32638888889
surface_form: ulun
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 50.508888888889
lon: 134.32638888889
surface_form: ulun
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 50.508888888889
lon: 134.32638888889
Elevations. The third edition of the Great Soviet Encyclopedia (GSE) listed in 1979 the range with an elevation of, no name was mentioned for the highest mountain. The geographic volume of the GSE listed &quot;Mount Ulun&quot; with an elevation of. After the breakdown of the Soviet Union topographic maps reduced the elevation to 2,221 m.

Geographic entities mentioned:
surface_form: ulun
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 50.508888888889
lon: 134.32638888889
Raichur district ranks first in Mosambi /Sweet Lime production in the state. Geography. The doab, named after Raichur is formed by Krishna River in the North and Tungabhadra river in the South. It lies within the Deccan Plateau region of Bayalu Seeme. History. Raichur Doab is inhabited since the Prehistoric cultures.

Geographic entities mentioned:
surface_form: Deccan Plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
By the early 20th century, he was a nationally known industrialist who served as director of the American Iron and Steel Institute, president of the Portage Silica Company, and a director of the Youngstown Sheet and Tube Company, Pennsylvania & Lake Erie Dock Company, Youngstown and Suburban Railway Company, Pennsylvania and Ohio Power & Light Company, and Commercial National Bank of Youngstown.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
In 2011 a Health Canada study found that 122 First Nation communities were under water advisories. The rising need for water preservation and clean water inspired a much larger water walk to take place in 2011. The 2011 Mother Earth Water Walk involved walks collecting water from the Pacific Ocean, the Atlantic Ocean, Lake Superior, Hudson River and the Gulf of Mexico.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Blind Sucker River. The Blind Sucker River is a river in northwestern Luce County on the Upper Peninsula of Michigan in the United States. It is a tributary of Lake Superior.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Footpaths of Mount Athos. hslikwdqdm8qh11vlj8rly0djjit9" xml:space="preserve">Mount Athos has an extensive network of footpaths, many of which date back to the Byzantine period. These paths are typically trails designed for human foot traffic and mules, and are not wide enough for motor vehicles.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Hesychast hermits have traditionally lived in this area. Way of the Bey. The Way of the Bey (&quot;or&quot;) primarily runs along the Athos peninsular ridge. It starts from Esphigmenou Monastery, reaches its highest point at the peak of Antiathonas (1042 m), and ends at Dionysiou Monastery.

Geographic entities mentioned:
surface_form: Antiathonas
instance_of: Mountain
countries: Greece
coordinates: lat: 40.183333333333
lon: 24.283333333333
Black Fell (Lake District). Black Fell is a fell in the English Lake District. It rises to the north of Tarn Hows, between Coniston and Hawkshead. Topography. Black Fell is the high point in the hilly area bounded by Windermere, Langdale and Coniston. It occupies an area of around one mile by two, clad mainly in fell grass with many small outcrops of rock.

Geographic entities mentioned:
surface_form: Windermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.358333333333
lon: -2.9361111111111
surface_form: black fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4056
lon: -3.01673
The fell has no obvious connecting ridges in the manner of higher mountains, but in fact has a pivotal position in this area of the district. To the west over Oxen Fell High Cross (518 ft) is Holme Fell and an onward link to Wetherlam and the Furness Fells (Coniston Fells). To the south east a broad highland runs out between Windermere and Esthwaite Water, terminating in Claife Heights.

Geographic entities mentioned:
surface_form: Holme Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.396
lon: -3.056
surface_form: Wetherlam
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.401
lon: -3.098
To the west over Oxen Fell High Cross (518 ft) is Holme Fell and an onward link to Wetherlam and the Furness Fells (Coniston Fells). To the south east a broad highland runs out between Windermere and Esthwaite Water, terminating in Claife Heights. Finally southward runs the 7 mile ridge of Grizedale Forest, capped by Carron Crag and Top o'Selside, Black Fell's topographical parent.

Geographic entities mentioned:
surface_form: Esthwaite Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.3589
lon: -2.9846
To the south east a broad highland runs out between Windermere and Esthwaite Water, terminating in Claife Heights. Finally southward runs the 7 mile ridge of Grizedale Forest, capped by Carron Crag and Top o'Selside, Black Fell's topographical parent. Black Fell's northern boundary is formed by Elter Water and the River Brathay.

Geographic entities mentioned:
surface_form: Top o'Selside
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.317988888889
lon: -3.0637694444444
surface_form: top o'selside
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.317988888889
lon: -3.0637694444444
surface_form: black fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4056
lon: -3.01673
surface_form: black fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4056
lon: -3.01673
Finally southward runs the 7 mile ridge of Grizedale Forest, capped by Carron Crag and Top o'Selside, Black Fell's topographical parent. Black Fell's northern boundary is formed by Elter Water and the River Brathay. The broadleaved woodland of Brow Coppice stands above the village of Skelwith Bridge in the valley.

Geographic entities mentioned:
surface_form: Elter Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.427469444444
lon: -3.025875
Beyond the eastern slopes is a mile of gently falling country, running through plantations to the head of Windermere. There are many tarns within this landscape, most of them artificial. The largest are Blelham Tarn and the pools near the Drunken Duck (Inn) crossroads. On the western side is the A593 road from Coniston to Ambleside, crossing the minor pass of Oxen Fell.

Geographic entities mentioned:
surface_form: Blelham Tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.396
lon: -2.97729
The panorama takes in both the high Coniston and Langdale Fells, and the lowlands and lakes to the south and west, a fine distillation of what Cumbria has to offer. Ascents. All ascents end via the short walk from the bridleway at Iron Keld to the summit, but starts can be made at Skelwith Bridge, High Park, Oxen Fell, Yew Tree Tarn, Tom Gill, Tarn Hows or Knipe Fold.

Geographic entities mentioned:
surface_form: Yew Tree Tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.395277777778
lon: -3.0461111111111
Black Fell (Lake District). Black Fell is a fell in the English Lake District. It rises to the north of Tarn Hows, between Coniston and Hawkshead. Topography. Black Fell is the high point in the hilly area bounded by Windermere, Langdale and Coniston. It occupies an area of around one mile by two, clad mainly in fell grass with many small outcrops of rock.

Geographic entities mentioned:
surface_form: black fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4056
lon: -3.01673
Topography. Black Fell is the high point in the hilly area bounded by Windermere, Langdale and Coniston. It occupies an area of around one mile by two, clad mainly in fell grass with many small outcrops of rock. Despite its modest altitude Alfred Wainwright accorded Black Fell a chapter in his &quot;Pictorial Guide to the Lakeland Fells&quot;, partly due to its excellence as a view point.

Geographic entities mentioned:
surface_form: black fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4056
lon: -3.01673
It represents the perimeter of the Lakeland Fells proper in his opinion, the land to the south falling within his supplementary volume, &quot;The Outlying Fells of Lakeland&quot;. Later guidebook writers have also included Black Fell within their remit. The fell has no obvious connecting ridges in the manner of higher mountains, but in fact has a pivotal position in this area of the district.

Geographic entities mentioned:
surface_form: black fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4056
lon: -3.01673
Tarn Hows is maintained by a dam at the south west corner and circumnavigated by a broad, level path, providing access to all. Few of the millions of visitors stray onto the slopes of Black Fell, or even know the name of the hill which provides the backdrop to so many photographs.

Geographic entities mentioned:
surface_form: black fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4056
lon: -3.01673
Banshee Peak. Banshee Peak is a mountain summit located in Mount Rainier National Park in Pierce County of Washington state, US. As part of the Cascade Range, Banshee Peak is situated west of the Cowlitz Chimneys and east of Panhandle Gap, with the Sarvant Glacier set below its north cliff. Precipitation runoff from Banshee Peak drains into tributaries of the White River and the Cowlitz River.

Geographic entities mentioned:
surface_form: Cowlitz Chimneys
instance_of: Landform
countries: United States
coordinates: lat: 46.848877
lon: -121.609409
Banshee Peak is a high remnant of bedded Ohanapecosh Formation lava flows. Access is from Panhandle Gap via the Wonderland Trail. The broad summit has alpine tundra similar to that found on Burroughs Mountain. The Sunrise Historic District provides a viewpoint from which to see Banshee Peak when weather permits.

Geographic entities mentioned:
surface_form: Burroughs Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.901644
lon: -121.713687
2007 German Skeleton Championship. The 41st German Skeleton Championship 2007 was organized on 3 March 2007 in Königssee.

Geographic entities mentioned:
surface_form: Königssee
instance_of: Lake
countries: Germany
coordinates: lat: 47.55
lon: 12.975
Isingsalen Saddle. u62kp3zigtud50tu68j3okp07m27" xml:space="preserve">Isingsalen Saddle () is an ice saddle between Isingen Mountain and Salknappen Peak in the Sverdrup Mountains of Queen Maud Land, Antarctica. It was photographed from the air by the Third German Antarctic Expedition (1938–39).

Geographic entities mentioned:
surface_form: Isingen Mountain
instance_of: Mountain
coordinates: lat: -72.3833
lon: 1.06667
surface_form: Salknappen Peak
instance_of: Mountain
coordinates: lat: -72.31666667
lon: 1.03333333
The Göktürks eventually collapsed due to a series of dynastic conflicts, but the name &quot;Turk&quot; was later taken by many states and peoples. Turkic peoples and related groups migrated west from Turkestan and what is now Mongolia towards Eastern Europe, Iranian plateau and Anatolia and modern Turkey in many waves. The date of the initial expansion remains unknown.

Geographic entities mentioned:
surface_form: Iranian plateau
instance_of: Plateau
countries: Iran
coordinates: lat: 36.283333
lon: 59.05
The Seljuq Turkmens created a medieval empire that controlled a vast area stretching from the Hindu Kush to eastern Anatolia and from Central Asia to the Persian Gulf. From their homelands near the Aral Sea, the Seljuqs advanced first into Khorasan and then into mainland Persia before eventually conquering eastern Anatolia. The Seljuq/Seljuk empire was founded by Tughril Beg (1016–1063) in 1037.

Geographic entities mentioned:
surface_form: Aral Sea
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
The Sotará and Puracé are the prominent volcanoes of the area, the latter being within the Puracé National Natural Park.

Geographic entities mentioned:
surface_form: Puracé
instance_of: Mountain
countries: Colombia
coordinates: lat: 2.3141666666667
lon: -76.394166666667
Mountains. Andrée Land is mountainous. The highest point is high Margaretatop, also known as Margarita Spids, located in the southern part. The Lacroix Mountains &quot;(Lacroix Bjerge)&quot; are a mountain range at the SW end rising above the Isfjord. Arnold Escher Land is a nunatak group to the NW of Andrée Land.

Geographic entities mentioned:
surface_form: Margaretatop
instance_of: Mountain
countries: Greenland
coordinates: lat: 73.385
lon: -26.221666666666668
Oeschinenhorn. The Oeschinenhorn is a mountain of the Bernese Alps, overlooking Lake Oeschinen in the Bernese Oberland. It is the westernmost summit of the Blüemlisalp-main-ridge.

Geographic entities mentioned:
surface_form: Lake Oeschinen
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.498333333333
lon: 7.7269444444444
surface_form: oeschinen
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.498333333333
lon: 7.7269444444444
surface_form: oeschinenhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.483888888889
lon: 7.7669444444444
Oeschinenhorn. The Oeschinenhorn is a mountain of the Bernese Alps, overlooking Lake Oeschinen in the Bernese Oberland. It is the westernmost summit of the Blüemlisalp-main-ridge.

Geographic entities mentioned:
surface_form: Blüemlisalp
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.488611111111
lon: 7.7716666666667
Oeschinenhorn. The Oeschinenhorn is a mountain of the Bernese Alps, overlooking Lake Oeschinen in the Bernese Oberland. It is the westernmost summit of the Blüemlisalp-main-ridge.

Geographic entities mentioned:
surface_form: oeschinenhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.483888888889
lon: 7.7669444444444
Coyote Valley is flanked by rolling hills that rise about the valley floor to the west of Lake Mendocino and steeper Franciscan bedrock hills to the east. Elevations above mean sea level in the surrounding region range from about in the valleys near Ukiah to about on top of Cow Mountain to the east. The hills to the east of Lake Mendocino are very rugged and continue for many miles.

Geographic entities mentioned:
surface_form: Cow Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.093055555556
lon: -123.35388888889
The Potter Valley Project was begun in 1900 to exploit the hydroelectric potential. The concrete gravity and earth filled Cape Horn Dam was built to impound a reservoir called Lake Van Arsdale on the Eel River. A tunnel in diameter lined with redwood timbers was excavated for more than south to emerge above the northern end of Potter Valley.

Geographic entities mentioned:
surface_form: Lake Van Arsdale
instance_of: Lake
countries: United States
coordinates: lat: 39.3858
lon: -123.117
In 1920 work started on Scott Dam, a large concrete ogee gravity structure upstream from Van Arsdale which collects water from the upper 7.3% of the Eel River watershed. It was completed in 1922 and began to fill Lake Pillsbury, which has a storage capacity of and releases water for the powerhouse throughout the year. The Pacific Gas and Electric Company (PG&E) acquired the project in 1930.

Geographic entities mentioned:
surface_form: Lake Pillsbury
instance_of: Lake
countries: United States
coordinates: lat: 39.4072
lon: -122.9575
Ralph Cobbold was born in Ipswich, the second son of the Ipswich MP John Patteson Cobbold. He was commissioned a second lieutenant in the King's Royal Rifle Corps on 17 October 1888, and promoted to lieutenant on 1 October 1890. He explored the Pamirs in 1897–1898. His report on Russian plans to occupy Chitral was an important episode in the Great Game between the Russian and British empires.

Geographic entities mentioned:
surface_form: Chitral
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.85111111111111
lon: 71.78888888888889
A person from Odalen is commonly called an. Geography. The Glommadal (or Glåmdalen) valley is a designation for the valley formed by the river Glomma (or Glåma), which is the longest and largest river in Norway. From the lake Aursund in the north on southwards to Elverum, the valley is called the Østerdalen. From that point and further south until Kongsvinger, the valley is referred to as Solør.

Geographic entities mentioned:
surface_form: Glommadal
instance_of: Valley
countries: Norway
A person from Odalen is commonly called an. Geography. The Glommadal (or Glåmdalen) valley is a designation for the valley formed by the river Glomma (or Glåma), which is the longest and largest river in Norway. From the lake Aursund in the north on southwards to Elverum, the valley is called the Østerdalen. From that point and further south until Kongsvinger, the valley is referred to as Solør.

Geographic entities mentioned:
surface_form: Østerdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.575916666666664
lon: 11.087111111111112
surface_form: aursund
instance_of: Lake
countries: Norway
coordinates: lat: 62.6678
lon: 11.6448
Odal, Norway. Odal or Odalen is a valley and traditional district in Innlandet county, Norway. The district encompasses the area around the lake Storsjøen in the north and to the areas around the river Glåma in the south. The district is currently divided between Sør-Odal Municipality and Nord-Odal Municipality. A person from Odalen is commonly called an. Geography.

Geographic entities mentioned:
surface_form: storsjøen
instance_of: Lake
countries: Norway
coordinates: lat: 60.3725
lon: 11.625
surface_form: storsjøen
instance_of: Lake
countries: Norway
coordinates: lat: 61.45222222
lon: 11.30972222
Odal, Norway. Odal or Odalen is a valley and traditional district in Innlandet county, Norway. The district encompasses the area around the lake Storsjøen in the north and to the areas around the river Glåma in the south. The district is currently divided between Sør-Odal Municipality and Nord-Odal Municipality. A person from Odalen is commonly called an. Geography.

Geographic entities mentioned:
surface_form: odal, norway
instance_of: Valley
countries: Norway
coordinates: lat: 60.3295
lon: 11.6144
Odal, Norway. Odal or Odalen is a valley and traditional district in Innlandet county, Norway. The district encompasses the area around the lake Storsjøen in the north and to the areas around the river Glåma in the south. The district is currently divided between Sør-Odal Municipality and Nord-Odal Municipality. A person from Odalen is commonly called an. Geography.

Geographic entities mentioned:
surface_form: odal
instance_of: Valley
countries: Norway
coordinates: lat: 60.3295
lon: 11.6144
surface_form: odalen
instance_of: Valley
countries: Norway
coordinates: lat: 60.3295
lon: 11.6144
Odal, Norway. Odal or Odalen is a valley and traditional district in Innlandet county, Norway. The district encompasses the area around the lake Storsjøen in the north and to the areas around the river Glåma in the south. The district is currently divided between Sør-Odal Municipality and Nord-Odal Municipality. A person from Odalen is commonly called an. Geography.

Geographic entities mentioned:
surface_form: odal
instance_of: Valley
countries: Norway
coordinates: lat: 60.3295
lon: 11.6144
surface_form: odal
instance_of: Valley
countries: Norway
coordinates: lat: 60.3295
lon: 11.6144
Odal, Norway. Odal or Odalen is a valley and traditional district in Innlandet county, Norway. The district encompasses the area around the lake Storsjøen in the north and to the areas around the river Glåma in the south. The district is currently divided between Sør-Odal Municipality and Nord-Odal Municipality. A person from Odalen is commonly called an. Geography.

Geographic entities mentioned:
surface_form: odalen
instance_of: Valley
countries: Norway
coordinates: lat: 60.3295
lon: 11.6144
From that point and further south until Kongsvinger, the valley is referred to as Solør. As the river turns and heads west from Kongsvinger all the way to the border with Nes Municipality, the valley is called the Odalen (Nes is part of the district of Romerike). These designations are traditional districts, reflecting the designations that the locals have historically used for their valleys.

Geographic entities mentioned:
surface_form: odalen
instance_of: Valley
countries: Norway
coordinates: lat: 60.3295
lon: 11.6144
These designations are traditional districts, reflecting the designations that the locals have historically used for their valleys. History. The name &quot;Odalen&quot; is derived from the Old Norse name. The first part of the name comes from the Old Norse word or, which means 'river' (here referring to the Glomma river). The last element is, which means 'valley' or 'dale'.

Geographic entities mentioned:
surface_form: odalen
instance_of: Valley
countries: Norway
coordinates: lat: 60.3295
lon: 11.6144
Settlement accelerated in the Viking Age, increasing the number of farms by as much as an order of magnitude. Increased mobility in the Norwegian population likely changed the character of the society in Odalen, and there is evidence the area was under the administration of the Thing in Eidsvoll.

Geographic entities mentioned:
surface_form: odalen
instance_of: Valley
countries: Norway
coordinates: lat: 60.3295
lon: 11.6144
Farms were abandoned and consolidated during this time, and it took at least 200 years for the population to reach its previous levels. During the 17th century, Odalen suffered economic setbacks as a result of taxation and general economic downturns. Forestry rose as a complementary source of income to agriculture.

Geographic entities mentioned:
surface_form: odalen
instance_of: Valley
countries: Norway
coordinates: lat: 60.3295
lon: 11.6144
The Knolls lived in Northern Virginia near his job in Washington, DC, and they often visited her longtime second home in Lily Dale, New York, famous for its psychics and healers. They kept additional retreat property that Wayne Knoll had bought years earlier on the western slope of Old Rag Mountain, near the Shenandoah National Park. Wayne Knoll died in 2013 at the age of 80.

Geographic entities mentioned:
surface_form: Old Rag Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.5517157
lon: -78.3160343
Early life. Barack Obama Sr. was born in 1934 in Rachuonyo District on the shores of Lake Victoria just outside Kendu Bay, Kenya, at the time a colony and protectorate of the British Empire. He was raised in the village of Nyang'oma Kogelo, Siaya District, Nyanza Province. His family were members of the Luo people. His father was Onyango Obama, and his mother was Habiba Akumu Nyanjango (c.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Sam Ohu Gon III. Samuel M. 'Ohukani'ōhi'a Gon III is an American scientist and Hawaiian cultural practitioner, currently serving as Senior Scientist and Cultural Advisor for The Nature Conservancy of Hawaiʻi. He was born and raised in Nuʻuanu on the island of Oʻahu. Gon studied Hawaiian culture under Kumu John Keolamala'āinana Lake.

Geographic entities mentioned:
surface_form: Nuʻuanu
instance_of: Landform
countries: United States
coordinates: lat: 21.370277777778
lon: -157.79694444444
At the time of his death he was President of the Port Henry Iron Company of Lake Champlain and senior member of the firm of Edward Bech & Co of New York City. Personal life. Bech died from tuberculosis on July 9, 1873, in Stuttgart, Baden-Württemberg.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
St. Anthony's Peak. St. Anthony's Peak is a peak on the island of Saint Kitts in Saint Kitts and Nevis. It is the highest point on the island's Southeast Peninsula, rising to 319 m (1047 ft) above the Great Salt Pond. It is a lava dome.

Geographic entities mentioned:
surface_form: Great Salt Pond
instance_of: Lake
countries: Saint Kitts and Nevis
coordinates: lat: 17.233333333333
lon: -62.65
St. Anthony's Peak. St. Anthony's Peak is a peak on the island of Saint Kitts in Saint Kitts and Nevis. It is the highest point on the island's Southeast Peninsula, rising to 319 m (1047 ft) above the Great Salt Pond. It is a lava dome.

Geographic entities mentioned:
surface_form: st. anthony's peak
instance_of: Mountain
countries: Saint Kitts and Nevis
coordinates: lat: 17.24527777777778
lon: -62.634166666666665
Etymology. The name of the village comes from the Slavic words &quot;Debeli Deo&quot; () which translated into English mean &quot;Thick Place&quot;
Geography. The village is located in the Karadak Mountain range, northwest of Kopilaq Mountain. It borders the village of Mjak in the west and Tanuševci in the south which is located in North Macedonia. History.

Geographic entities mentioned:
surface_form: Karadak Mountain range
instance_of: Mountain
countries: Serbia
Kosovo
North Macedonia
coordinates: lat: 42.166666666667
lon: 21.416666666667
The Bajraktar of the village was Halil Arifi. The village alongside Tanuševci became a strongholds of Balli Kombëtar during the Second World War and were the site of the Congress of Kopilaqa of Karadak Leaders such as Mulla Idriz Gjilani, Sulë Hotla, Jusuf Lipovica and others. During the Interwar period, two Albanian families from Dëbëlldeh moved into the village Beguncë.

Geographic entities mentioned:
surface_form: Karadak
instance_of: Mountain
countries: Serbia
Kosovo
North Macedonia
coordinates: lat: 42.166666666667
lon: 21.416666666667
The Shire is named after the major geographical feature in the region, Lake Hindmarsh, (which in turn was named after John Hindmarsh) located in the east of the LGA. Administration and governance. The council meets in the council chambers at the council headquarters in the Nhill Municipal Offices, which is also the location of the council's administrative activities.

Geographic entities mentioned:
surface_form: Lake Hindmarsh
instance_of: Lake
countries: Australia
coordinates: lat: -36.0667
lon: 141.917
City proposal of Mount Athos. Dinocrates is noted by Vitruvius, in the only surviving architectural treatise from Antiquity, for his plan to sculpt in the flank of Mount Athos a colossal image of a man, holding a small city in one hand and with the other, pouring from a gigantic pitcher a river into the sea.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Australia had also hosted an international tournament that predated the first Women's World Championship. In 1965, the first ISF Women's World Championship was held in Melbourne, with games being played at Albert Park. Five nations competed at the inaugural championships including the United States, Japan and Australia, which Australia won 1–0 in a final game against the United States.

Geographic entities mentioned:
surface_form: Albert Park
instance_of: Lake
countries: Australia
coordinates: lat: -37.846
lon: 144.97
It is a tributary of the Baker River, part of the Pemigewasset River and Merrimack River watersheds. The river rises in the town of Orange, New Hampshire, on high ground north of Mount Cardigan. It flows north through the southwest corner of the town of Groton and the eastern part of Dorchester, enters Wentworth, and drops rapidly to the Baker River.

Geographic entities mentioned:
surface_form: Mount Cardigan
instance_of: Mountain
countries: United States
coordinates: lat: 43.649794444444
lon: -71.914805555556
Pröller. Pröller is a mountain of Bavaria, Germany.

Geographic entities mentioned:
surface_form: pröller
instance_of: Mountain
countries: Germany
coordinates: lat: 49.023056
lon: 12.820556
Riddle received 578 votes (11.77%) in 1995, finishing third against New Democratic Party incumbent George Hickes. Rupertsland: Eric Kennedy. Kennedy was born in Princess Harbour on Lake Winnipeg. He began his political career at the municipal level, serving as Mayor of Long Body Creek and president of the Northern Association of Community Councils.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
In July 2008, ComfortDelGro Cabcharge planned to venture into the bus building industry, and entered a memorandum of understanding to acquire bus body builder Custom Coaches. CDC had also planned to open a bus building plant in Rutherford in New South Wales' Hunter Valley, and the plant would be used as one of its bases for its bus building operations.

Geographic entities mentioned:
surface_form: Hunter Valley
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Firebase Bastogne. Firebase Bastogne (also known as Firebase Phu Xuan) was a U.S. Army and Army of the Republic of Vietnam (ARVN) firebase, located along Highway 547 halfway between the city of Huế and the A Sầu Valley, a feeder route from the Ho Chi Minh Trail. Creation and early years.

Geographic entities mentioned:
surface_form: A Sầu Valley
instance_of: Valley
countries: Vietnam
coordinates: lat: 16.259305555556
lon: 107.2125
The U. S. military was ineffective in stopping Comanche raids into Texas and Mexico. Finally, the Texas Rangers and some Native American allies began a campaign in 1858 to eliminate the problem. The campaign culminated in the Battle of Little Robe Creek on May 12, 1858. After gold was discovered in California in 1848, the large number of people traveling west created a need for a wagon road.

Geographic entities mentioned:
surface_form: battle
instance_of: Watercourse
countries: United States
coordinates: lat: 44.9266
lon: -93.0291
Antelope Hills, Oklahoma. The Antelope Hills are a series of low hills in the bend of the Canadian River in northwest Roger Mills County, Oklahoma, near the border between western Oklahoma and the Texas panhandle. They were a major landmark for the Plains Indians and travelers on what is now the western plains of Oklahoma.

Geographic entities mentioned:
surface_form: antelope hills, oklahoma
instance_of: Landform
Mountain
countries: United States
coordinates: lat: 35.9
lon: -99.88
Antelope Hills, Oklahoma. The Antelope Hills are a series of low hills in the bend of the Canadian River in northwest Roger Mills County, Oklahoma, near the border between western Oklahoma and the Texas panhandle. They were a major landmark for the Plains Indians and travelers on what is now the western plains of Oklahoma.

Geographic entities mentioned:
surface_form: antelope hills
instance_of: Landform
Mountain
countries: United States
coordinates: lat: 35.9
lon: -99.88
Captain Randolph B. Marcy was commissioned to lead a party to survey the route for such a road from Fort Smith to California. This became known as the California Road. Marcy described the Antelope Hills as, &quot;... about one hundred and fifty feet high, of porous sandstone, and appear to be the result of volcanic action.

Geographic entities mentioned:
surface_form: antelope hills
instance_of: Landform
Mountain
countries: United States
coordinates: lat: 35.9
lon: -99.88
They are near the 100th degree of longitude, and are sometimes called the Boundary mounds, as being near the line formerly claimed by Texas as her eastern boundary.&quot;
The Antelope Hills area was added to the National Register of Historic Places on December 14, 1978. This area is sparsely populated.

Geographic entities mentioned:
surface_form: antelope hills
instance_of: Landform
Mountain
countries: United States
coordinates: lat: 35.9
lon: -99.88
Teeters Nunatak. 2hegcajd67vhbpmhkjwoop4vecxw" xml:space="preserve">#redirect Teeters Nunatak

Geographic entities mentioned:
surface_form: teeters nunatak
instance_of: Mountain
coordinates: lat: -74.2
lon: -100.017
Red Willow Lake (Griggs County, North Dakota). Red Willow Lake is a naturally formed lake located in Griggs County, North Dakota. The nearest town is Binford. The lake covers, has of shoreline, and has an average depth of, with a maximum depth of. Red Willow Lake is an endorheic (closed) lake; it has no significant input or output of rivers or streams and is fed only by rain and natural springs.

Geographic entities mentioned:
surface_form: willow lake
instance_of: Lake
countries: United States
coordinates: lat: 37.99409
lon: -105.60856
surface_form: willow lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6508646
lon: -97.6398816
surface_form: red willow lake
instance_of: Lake
countries: United States
coordinates: lat: 47.647
lon: -98.373
The nearest town is Binford. The lake covers, has of shoreline, and has an average depth of, with a maximum depth of. Red Willow Lake is an endorheic (closed) lake; it has no significant input or output of rivers or streams and is fed only by rain and natural springs. Red Willow Lake first became recognized as a recreational resource in 1882.

Geographic entities mentioned:
surface_form: willow lake
instance_of: Lake
countries: United States
coordinates: lat: 37.99409
lon: -105.60856
surface_form: willow lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6508646
lon: -97.6398816
surface_form: red willow lake
instance_of: Lake
countries: United States
coordinates: lat: 47.647
lon: -98.373
Three memorial services were held: one at Young Israel in St. Louis, in keeping with the tradition that the funeral of the &quot;Gadol Ha’ir&quot; (the rabbinic leader of the city) take place inside a synagogue; a second at Yeshivah Torah Vodaath in New York, and the third in Jerusalem. Rivkin was buried next to his wife, parents and grandparents at the Mount of Olives Cemetery in Jerusalem.

Geographic entities mentioned:
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
Gleason, the Greenwood Spring Water Cure in Cuba, New York, in 1846–1847. As a result, he spent the second half of his life as an advocate for hydropathy, training to become a physician and opening a hydropathic institute at Glen Haven on Skaneateles Lake in Cortland County, New York, in 1847. In 1858, he took over the 'Our Home Hygienic Institute' at Dansville, Livingston County, New York.

Geographic entities mentioned:
surface_form: Skaneateles Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.8625
lon: -76.372777777778
The primary inflow is from Pigeon Lake through the Gannon Narrows at the west. Secondary inflows are from Chemong Lake through the Harrington Narrows to Harrington Bay at the south, and from Sandy Lake via Sandy Creek to Sandy Creek Bay at the south. A dam and lock 31 of the Trent–Severn Waterway at the community of Buckhorn control the outflow of the lake to Lower Buckhorn Lake at the northeast.

Geographic entities mentioned:
surface_form: Lower Buckhorn Lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.55
lon: -78.2583
surface_form: buckhorn lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.485555555556
lon: -78.391111111111
Buckhorn Lake (Ontario). Buckhorn Lake is a lake in the townships of Trent Lakes and Selwyn in Peterborough County, Ontario, Canada, and is one of the Kawartha lakes. The primary inflow is from Pigeon Lake through the Gannon Narrows at the west.

Geographic entities mentioned:
surface_form: kawartha
instance_of: Group of lakes
countries: Canada
coordinates: lat: 44.4994
lon: -78.441
surface_form: buckhorn lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.485555555556
lon: -78.391111111111
Buckhorn is also a small town surrounded by the lake. There are a few restaurants in the Buckhorn region and many summer cottages. Settlements on the lake include Buckhorn, the Curve Lake First Nation, Gannon Village, Gannon Beach, Kawartha Hideaway, Kimberley Park, Oak Orchard and Young's Cove.

Geographic entities mentioned:
surface_form: kawartha
instance_of: Group of lakes
countries: Canada
coordinates: lat: 44.4994
lon: -78.441
Buckhorn Lake is a lake in the townships of Trent Lakes and Selwyn in Peterborough County, Ontario, Canada, and is one of the Kawartha lakes. The primary inflow is from Pigeon Lake through the Gannon Narrows at the west. Secondary inflows are from Chemong Lake through the Harrington Narrows to Harrington Bay at the south, and from Sandy Lake via Sandy Creek to Sandy Creek Bay at the south.

Geographic entities mentioned:
surface_form: pigeon lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.471666666666664
lon: -78.495
surface_form: pigeon lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.030277777778
lon: -114.06333333333