Sarmila/GeoWiki-Features huggingface dataset:
In their 1953 book &quot;Yorkshire Village&quot;, Marie Hartley and Joan Ingliby describe the view of Wether Fell from the north across Hawes as looking like &quot;...the limbs and loins of a beast stretched full length filling the horizon.&quot; The geology of the fell is mostly limestone with some small outcrops of millstone grit.

Geographic entities mentioned:
surface_form: wether fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.277
lon: -2.191
Cam High Road, an old Roman Road between Ingleton and Bainbridge, goes over Wether Fell, quite close to the summit at Drumaldrace, reaching at its highest point. This was the route taken by the Richmond to Lancaster Turnpike between 1751 and 1795, before the turnpike was diverted through Hawes, and then over Widdale to the Ribble Valley.

Geographic entities mentioned:
surface_form: wether fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.277
lon: -2.191
This was the route taken by the Richmond to Lancaster Turnpike between 1751 and 1795, before the turnpike was diverted through Hawes, and then over Widdale to the Ribble Valley. Several cairns are also to be found on the slopes of Wether Fell, some which date back as far as the Bronze Age. An ancient right was exercised by the people Bainbridge - the right to graze geese on Wether Fell.

Geographic entities mentioned:
surface_form: wether fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.277
lon: -2.191
Several cairns are also to be found on the slopes of Wether Fell, some which date back as far as the Bronze Age. An ancient right was exercised by the people Bainbridge - the right to graze geese on Wether Fell. The northern edge of Wether Fell is recognised as a good place for hang gliding and paragliding when the weather conditions are right.

Geographic entities mentioned:
surface_form: wether fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.277
lon: -2.191
The northern edge of Wether Fell is recognised as a good place for hang gliding and paragliding when the weather conditions are right. Water falling on the slopes of Wether Fell flows into just two main river systems: to the north and east, it flows into the River Ure (via the River Bain to the east), and to the south, it exits through the River Wharfe.

Geographic entities mentioned:
surface_form: wether fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.277
lon: -2.191
The Wether Fell stone flags, typically used for footpaths through fields around Hawes, Hardraw, Gayle and Sedbusk. These flags were quarried from around a point about high. Coal was also mined from at least three locations on the steep western slope of Wether Fell, with the most notable being Storth Colliery. The seam was known as &quot;Simonstone Coal&quot;, and stretched for towards Burtersett.

Geographic entities mentioned:
surface_form: wether fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.277
lon: -2.191
This show's indeed the Somali saying &quot;tol waa tolane&quot; (clan is something joined together)&quot; and the structure is not based on blood relationship, that is why you will find Garre is closely affiliated with Tunni and Jiido of the Lower Jubba Valley.

Geographic entities mentioned:
surface_form: Lower Jubba Valley.
instance_of: Valley
countries: Ethiopia
Somalia
Kenya
coordinates: lat: 4.1772222222222
lon: 42.079444444444
Geography. Friuli-Venezia Giulia is Italy's north-easternmost region. It covers an area of 7,858 km2 and is the fifth smallest region of the country. It borders Austria to the north and Slovenia to the east, the three countries meeting at the tripoint on the mountain of Dreiländereck, known as Monte Forno in Italian. To the south, it faces the Adriatic Sea and to the west the Veneto region.

Geographic entities mentioned:
surface_form: Dreiländereck
instance_of: Mountain
countries: Austria
Slovenia
Italy
coordinates: lat: 46.522986
lon: 13.714089
Morphologically the region can be subdivided into four main areas. The mountainous area in the north: this part of the region includes Carnia and the ending section of the Alps (Carnic Alps and Julian Alps), of which the highest peaks exceed 2,700 m above sea level (Jôf di Montasio 2,754 m). Its landscapes are characterised by vast pine forests and pastures, mountain lakes (e.g.

Geographic entities mentioned:
surface_form: Carnia
instance_of: Valley
countries: Italy
coordinates: lat: 46.39444444
lon: 12.77416667
surface_form: Jôf di Montasio
instance_of: Mountain
countries: Italy
coordinates: lat: 46.437777777778
lon: 13.433333333333
Sauris, Fusine, and Barcis), and numerous streams and small rivers descending from the mountains. The area is also known for its tourist destinations, especially during the winter season (Monte Zoncolan, Tarvisio, Sella Nevea, Forni di Sopra and Piancavallo). The hilly area is situated to the south of the mountains and along the central section of the border with Slovenia.

Geographic entities mentioned:
surface_form: Monte Zoncolan
instance_of: Mountain
countries: Italy
coordinates: lat: 46.5
lon: 12.916666666667
Its products are exported not only within the country and Europe (fruit and vegetables, cheese) but have become known worldwide for their acclaimed quality (cured ham and wines, especially white ones). Noteworthy is also the production of soy (third producer in Italy with more than 37,000 hectares cultivated in 2000) and timber production in Carnia.

Geographic entities mentioned:
surface_form: Carnia
instance_of: Valley
countries: Italy
coordinates: lat: 46.39444444
lon: 12.77416667
In late April the &quot;Michigan&quot; headed for Buffalo to resupply before her yearly patrol. After that Commander Bigelow sailed west across Lake Erie, passing north along Detroit on Thursday, May 5, 1853 and then entered Lake Huron via Saint Clair River. On the following morning, at about 2:15 am, a lookout sighted a light in the darkness ahead of the &quot;Michigan&quot;.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
But the illegal logging trade continued to as late as the 1870s. Beaver-Mackinac War. The &quot;Michigan&quot; was also involved in the Beaver-Mackinac War. In 1850 James Strang crowned himself the king of Beaver Island, at the head of Lake Michigan. Eventually he began forcing his radical beliefs on some of his mainstream Mormon followers, known as Strangites.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
A race riot took place in Detroit in 1863, also about labor and economic competition issues at bottom, and another in Buffalo, New York. The USS &quot;Michigan&quot; spent much of the war patrolling back and forth between those urban areas. By 1863 Johnson's Island in Lake Erie was used as a prisoner of war camp for Confederates. The Southern government knew of the camp.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Thus the plot to capture the &quot;Michigan&quot; and liberate the prisoners on Johnson's Island failed before it really began. Rebel activity in the North did not end. Confederate agents in Canada launched an expedition to the coastal town of St. Albans, Vermont across Lake Champlain, one month after the incident on Lake Erie. The rebels, under Lieutenant Bennett H.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Barnaby River. yhlbdcrw61nwbtgovayv6ugh8vtsk" xml:space="preserve">The Barnaby River is a tributary of the Miramichi River in New Brunswick, Canada. The Barnaby River rises in southern Northumberland County, close to the Kent County, New Brunswick boundary and flows north and west into the south side of the Southwest Miramichi River at the community of Kirkwood, New Brunswick.

Geographic entities mentioned:
surface_form: Southwest Miramichi River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.519346
lon: -67.151946
surface_form: barnaby river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.905336
lon: -65.616093
Barnaby River. yhlbdcrw61nwbtgovayv6ugh8vtsk" xml:space="preserve">The Barnaby River is a tributary of the Miramichi River in New Brunswick, Canada. The Barnaby River rises in southern Northumberland County, close to the Kent County, New Brunswick boundary and flows north and west into the south side of the Southwest Miramichi River at the community of Kirkwood, New Brunswick.

Geographic entities mentioned:
surface_form: barnaby river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.905336
lon: -65.616093
The Barnaby River watershed is entirely rural, dominated by forests and small farms in the communities of Lower Barnaby, Upper Barnaby, and the Community of Barnaby River.

Geographic entities mentioned:
surface_form: barnaby river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.905336
lon: -65.616093
surface_form: barnaby river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.905336
lon: -65.616093
Caniche Peak. Caniche Peak is located on the border of Alberta and British Columbia. It was named in 1922 by Arthur O. Wheeler. He suggested it be called Poodle Park as he thought it resembled the head of a poodle. The French word for poodle, &quot;Caniche&quot;, was adopted to give the name more class.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: caniche peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.7539
lon: -118.371
Caniche Peak. Caniche Peak is located on the border of Alberta and British Columbia. It was named in 1922 by Arthur O. Wheeler. He suggested it be called Poodle Park as he thought it resembled the head of a poodle. The French word for poodle, &quot;Caniche&quot;, was adopted to give the name more class.

Geographic entities mentioned:
surface_form: caniche peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.7539
lon: -118.371
Assabet River. The Assabet River is a small, long river located about west of Boston, Massachusetts, United States. The Assabet rises from a swampy area known as the Assabet Reservoir in Westborough, Massachusetts, and flows northeast before merging with the Sudbury River at Egg Rock in Concord, Massachusetts, to become the Concord River.

Geographic entities mentioned:
surface_form: Egg Rock
instance_of: Landform
countries: United States
coordinates: lat: 42.4651
lon: -71.3585
Streams located in the towns of Shrewsbury and Grafton feed the reservoir. From Westborough the river flows northeast, starting at an elevation of and descending through the towns of Northborough, Marlborough, Berlin, Hudson, Stow, Maynard, Acton, and finally Concord, where it merges with the Sudbury River at Egg Rock () at an elevation of to form the Concord River. The Assabet's watershed covers.

Geographic entities mentioned:
surface_form: Egg Rock
instance_of: Landform
countries: United States
coordinates: lat: 42.4651
lon: -71.3585
Later, Seguenza chose to study the geological and mineralogical sciences. Scientific research. At the age of 23, Giuseppe Seguenza discovered that all the products of the emanations of Vulcano (one of the Aeolian Islands) contained arsenic compounds. Afterward, he published other scientific works that earned him the attention of scholars in Europe and the silver medal at the Paris Exposition.

Geographic entities mentioned:
surface_form: Vulcano
instance_of: Mountain
countries: Italy
coordinates: lat: 38.4042
lon: 14.9658
Salloomt River. uoc7fd6jcw181buemiycf8w96rqe" xml:space="preserve">The Salloomt River is a river in the Bella Coola Valley of the Central Coast region of British Columbia, Canada. It is a tributary of the Bella Coola River, flowing southwest out of the southernmost Kitimat Ranges to meet that river just upstream from the community of Hagensborg.

Geographic entities mentioned:
surface_form: Bella Coola Valley
instance_of: Valley
countries: Canada
The Cotopaxi volcano (meaning 'smooth neck of the moon' in Quechua; Quechua &quot;q'oto&quot; 'throat' + Aymara &quot;phakhsi&quot; 'moon') that lends its name to the park is located within its boundaries, together with two others: the dormant Rumiñawi volcano to its north-west and the historical Sincholagua volcano (last major eruption: 1877) to the south-east.

Geographic entities mentioned:
surface_form: Cotopaxi volcano
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.68055555555556
lon: -78.437777777778
The lift was later demolished in 2004. The lift and its cabins were manufactured by a former Italian lift company: Carlevaro-Savio. One of the longest gondola rides in the world, Gondelbahn Grindelwald-Männlichen, is in the Bernese Oberland in Switzerland and connects Grindelwald with Männlichen. Urban transport. In recent years, gondola lifts are finding increased usage in urban environments.

Geographic entities mentioned:
surface_form: Männlichen
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.618056
lon: 7.938056
The system uses multiple lines and has five stations, and it connects Epcot and Disney's Hollywood Studios with one another and with several Disney-owned and -operated resort hotels. In terms of urban gondola systems for the future, TransLink in Metro Vancouver has proposed to build a gondola up Burnaby Mountain to Simon Fraser University in an announcement in September 2010.

Geographic entities mentioned:
surface_form: Burnaby Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.2792
lon: -122.909
History. The Eye of the Needle was an -high naturally occurring geographic formation shaped much like an inverted &quot;V&quot;. It was located along a section of the Upper Missouri National Wild and Scenic River, on land administered by the Bureau of Land Management (BLM), approximately downstream from Fort Benton and adjacent to LaBarge Rock, another notable rock formation.

Geographic entities mentioned:
surface_form: LaBarge Rock
instance_of: Mountain
countries: United States
coordinates: lat: 47.9111
lon: -110.062
Second and third respectively were Italian riders Fiorenzo Magni and Agostino Coletto. Gaul took the lead in the legendary stage up Monte Bondone, where under a snow storm he won with an 8-minute margin over runner up Alessandro Fantini. This edition is unique since there were two Mountains Classification winners.

Geographic entities mentioned:
surface_form: Monte Bondone
instance_of: Mountain
countries: Italy
coordinates: lat: 45.98805556
lon: 11.03083333
The planned tenth stage from Salerno to Frascati was deemed an &quot;electoral stage&quot; at the route's announcement and was chosen to be removed because it fell on the day of Italian municipal elections. Three new Dolomite mountains were climbed during this edition of the race: Monte Bondone (), San-Pellegrino (), and Vallès (meters).

Geographic entities mentioned:
surface_form: Monte Bondone
instance_of: Mountain
countries: Italy
coordinates: lat: 45.98805556
lon: 11.03083333
Geography. At Seefingan is the 11th highest summit in the Wicklow Mountains, the second highest point in South Dublin after Kippure and the 92nd highest summit in Ireland. It stands at the junction of three ridges, Corrig to the north, Seefin to the southwest and Kippure to the east, and straddles the border between County Wicklow and South Dublin.

Geographic entities mentioned:
surface_form: Kippure
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.169397
lon: -6.338322
surface_form: kippure
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.169397
lon: -6.338322
There is not a cairn on the summit, but there is a notice warning walkers of Kilbride Camp and the nearby military firing range. There are extensive views to the mountains of western Wicklow, Mullaghcleevaun and Poulaphouca Reservoir, the prominent communication masts on the top of Kippure and across the city of Dublin towards Howth.

Geographic entities mentioned:
surface_form: Mullaghcleevaun
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.103627777778
lon: -6.4067222222222
surface_form: kippure
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.169397
lon: -6.338322
surface_form: mullaghcleevaun
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.103627777778
lon: -6.4067222222222
Geography. At Seefingan is the 11th highest summit in the Wicklow Mountains, the second highest point in South Dublin after Kippure and the 92nd highest summit in Ireland. It stands at the junction of three ridges, Corrig to the north, Seefin to the southwest and Kippure to the east, and straddles the border between County Wicklow and South Dublin.

Geographic entities mentioned:
surface_form: kippure
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.169397
lon: -6.338322
surface_form: seefin
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.313
lon: -8.521
surface_form: seefin
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.1862
lon: -6.3948
It stands at the junction of three ridges, Corrig to the north, Seefin to the southwest and Kippure to the east, and straddles the border between County Wicklow and South Dublin. The headwaters of the River Dodder lie on the eastern slopes of Seefingan, Kippure and Seecawn. The summit is a smooth grassy area but the three ridges are boggy, and particularly difficult to negotiate after rain.

Geographic entities mentioned:
surface_form: kippure
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.169397
lon: -6.338322
surface_form: seefingan
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.192034
lon: -6.3749
The summit is a smooth grassy area but the three ridges are boggy, and particularly difficult to negotiate after rain. There are footpaths but they can be difficult to follow through the boggy parts; a Seefin – Seefingan – Kippure circuit is one possible route. There is not a cairn on the summit, but there is a notice warning walkers of Kilbride Camp and the nearby military firing range.

Geographic entities mentioned:
surface_form: kippure
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.169397
lon: -6.338322
surface_form: seefin
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.313
lon: -8.521
surface_form: seefingan
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.192034
lon: -6.3749
surface_form: seefin
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.1862
lon: -6.3948
There is a very large and perfect cairn on the top of it, which, like that at Seeghane, does not appear to have been opened. It may contain a chamber, like that on Seefin, which is about a mile further on, and is the loftiest hill of the three.

Geographic entities mentioned:
surface_form: seefin
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.313
lon: -8.521
surface_form: seefin
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.1862
lon: -6.3948
Seefingan. Seefingan often spelt Seafingan (meaning &quot;Fingan's Seat&quot;) is a mountain that straddles two county boundaries from its summit in Wicklow eastwards down into South Dublin, in Ireland. There are extensive views from the summit and there is a large megalithic cairn nearby. Geography.

Geographic entities mentioned:
surface_form: seefingan
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.192034
lon: -6.3749
Puca Mauras (possibly from Quechua &quot;puka&quot; red) is a volcano in the Andes of Peru, about high. It is situated at the &quot;Valley of the Volcanoes&quot; in the Arequipa Region, Castilla Province, on the border of the districts of Andagua and Chilcaymarca. Puca Mauras lies in the western extensions of the Chila mountain range, northeast of the Ticsho and Yanamauras volcanoes.

Geographic entities mentioned:
surface_form: Ticsho
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4847
lon: -72.3786
surface_form: Yanamauras
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4839
lon: -72.3517
surface_form: ticsho
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4847
lon: -72.3786
surface_form: yanamauras
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4839
lon: -72.3517
Puca Mauras (Andagua-Chilcaymarca). Puca Mauras (possibly from Quechua &quot;puka&quot; red) is a volcano in the Andes of Peru, about high. It is situated at the &quot;Valley of the Volcanoes&quot; in the Arequipa Region, Castilla Province, on the border of the districts of Andagua and Chilcaymarca.

Geographic entities mentioned:
surface_form: puca mauras
instance_of: Mountain
countries: Peru
coordinates: lat: -15.45361111
lon: -72.23027778
surface_form: puca mauras
instance_of: Mountain
countries: Peru
coordinates: lat: -15.42583333
lon: -72.33861111
Puca Mauras (Andagua-Chilcaymarca). Puca Mauras (possibly from Quechua &quot;puka&quot; red) is a volcano in the Andes of Peru, about high. It is situated at the &quot;Valley of the Volcanoes&quot; in the Arequipa Region, Castilla Province, on the border of the districts of Andagua and Chilcaymarca.

Geographic entities mentioned:
surface_form: puca mauras
instance_of: Mountain
countries: Peru
coordinates: lat: -15.45361111
lon: -72.23027778
surface_form: puca mauras
instance_of: Mountain
countries: Peru
coordinates: lat: -15.42583333
lon: -72.33861111
surface_form: puka
instance_of: Mountain
countries: Peru
coordinates: lat: -12.6339
lon: -75.5692
Qarhan railway station. The Qarhan or Cha'erhan railway station is a station on the Qingzang Railway at Qarhan in Golmud County, Haixi Prefecture, Qinghai Province, China. Qarhan station is located in Qarhan Playa of the Qaidam Basin, near Dabusun Lake where major salt works are located. As of 2012, a private railway branch from this station to the nearby facilities of the Zangge Potash Co Ltd.

Geographic entities mentioned:
surface_form: Dabusun Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 37.024080555556
lon: 95.138925
Archbishopric of Magdeburg. The Archbishopric of Magdeburg was a Latin Catholic archdiocese (969–1552) and Prince-Archbishopric (1180–1680) of the Holy Roman Empire centered on the city of Magdeburg on the Elbe River.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Waun-oer. Waun-oer is a mountain in Snowdonia, North Wales, situated approximately four miles to the south-west of Aran Fawddwy. It is one of the peaks in the Dyfi hills, a subgroup of the Cadair Idris group. It is a top of Maesglase and the summit consists of a trig point that crowns an uneven grassy plateau. It is connected to Cribin Fawr to the east and Mynydd Ceiswyn to the south.

Geographic entities mentioned:
surface_form: Aran Fawddwy
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.78702
lon: -3.68786
surface_form: waun-oer
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.717037
lon: -3.799394
Waun-oer. Waun-oer is a mountain in Snowdonia, North Wales, situated approximately four miles to the south-west of Aran Fawddwy. It is one of the peaks in the Dyfi hills, a subgroup of the Cadair Idris group. It is a top of Maesglase and the summit consists of a trig point that crowns an uneven grassy plateau. It is connected to Cribin Fawr to the east and Mynydd Ceiswyn to the south.

Geographic entities mentioned:
surface_form: Cadair Idris
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.699827777778
lon: -3.9086944444444
Waun-oer. Waun-oer is a mountain in Snowdonia, North Wales, situated approximately four miles to the south-west of Aran Fawddwy. It is one of the peaks in the Dyfi hills, a subgroup of the Cadair Idris group. It is a top of Maesglase and the summit consists of a trig point that crowns an uneven grassy plateau. It is connected to Cribin Fawr to the east and Mynydd Ceiswyn to the south.

Geographic entities mentioned:
surface_form: Maesglase
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.719996
lon: -3.752504
It is one of the peaks in the Dyfi hills, a subgroup of the Cadair Idris group. It is a top of Maesglase and the summit consists of a trig point that crowns an uneven grassy plateau. It is connected to Cribin Fawr to the east and Mynydd Ceiswyn to the south. To the north lies Cadair Idris, while Tarren y Gesail lies to the west.

Geographic entities mentioned:
surface_form: Cribin Fawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.721757
lon: -3.786277
It is one of the peaks in the Dyfi hills, a subgroup of the Cadair Idris group. It is a top of Maesglase and the summit consists of a trig point that crowns an uneven grassy plateau. It is connected to Cribin Fawr to the east and Mynydd Ceiswyn to the south. To the north lies Cadair Idris, while Tarren y Gesail lies to the west.

Geographic entities mentioned:
surface_form: Tarren y Gesail
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.635397
lon: -3.906926
surface_form: cadair idris
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.699827777778
lon: -3.9086944444444
Waun-oer. Waun-oer is a mountain in Snowdonia, North Wales, situated approximately four miles to the south-west of Aran Fawddwy. It is one of the peaks in the Dyfi hills, a subgroup of the Cadair Idris group. It is a top of Maesglase and the summit consists of a trig point that crowns an uneven grassy plateau. It is connected to Cribin Fawr to the east and Mynydd Ceiswyn to the south.

Geographic entities mentioned:
surface_form: waun-oer
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.717037
lon: -3.799394
Ewaso Ng'iro. Ewaso Ng'iro, also called Ewaso Nyiro, is a river in Kenya which rises on the west side of Mount Kenya and flows north, then east and finally south-east, passing through Somalia where it joins the Jubba River. The river's name is derived from the local community's Maasai language, and means river of brown or muddy water.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
Downstream, the intermittent stream in Somalia is also called Lagh Dera. The upper basin of the Ewaso Ng'iro River is. The river has a continuous water supply due to the glaciers on Mount Kenya. Ewaso Ng'iro feeds into Lake Ol Bolossat, the only lake in Nyandarua County and the larger Central Kenya, and crosses seven arid to semi-arid landscapes.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
The curving walls, a form later seen at Hopetoun, were a new innovation if Bruce did carry them out, possibly inspired by the work of the Italian Gian Lorenzo Bernini. In the gardens he laid out parterres and stepped &quot;Italian&quot; terraces, with a vista leading the eye to the Bass Rock, all inspired by French baroque gardens such as Vaux-le-Vicomte.

Geographic entities mentioned:
surface_form: Bass Rock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.08
lon: -2.64
William Bruce's appointment as Surveyor General of the King's Works in Scotland was made chiefly for the purpose of rebuilding the palace of Holyroodhouse. Aside from this project, he only carried out minor repairs to Edinburgh and Stirling Castles, and to the fortifications on the Bass Rock. Charles I had intended to extend and rebuild Holyroodhouse, and plans had been drawn up in the 1630s.

Geographic entities mentioned:
surface_form: Bass Rock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.08
lon: -2.64
Wynola, California. Wynola is an unincorporated community located in the Spencer Valley in San Diego County, California. Wynola is the site of the Spencer Valley School, a one-room public elementary school with a student population of 30-35 children. It is the only school in the Spencer Valley School District, founded in 1876.

Geographic entities mentioned:
surface_form: Spencer Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.0878
lon: -116.645
Ferries were not a viable solution in the long term; a ferry trip across the Hudson River lasted 20 minutes in good weather. The rival New York Central Railroad (NYC)'s line transported passengers from the Hudson Valley in the city's north, ran along Park Avenue in Manhattan, and terminated at Grand Central Depot (later Grand Central Terminal) at 42nd Street and Park Avenue.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
In 1991 he published &quot;Motstandsmann og politiker. Fra XU til SF og Kings Bay&quot; with Bjørn Bjørnsen. He lived at Kolsås in his later life. He died in January 1996 in Bærum. Shortly after his death, the Lund Commission found that Løfsnes had been subject to widespread political surveillance by the Norwegian Police Surveillance Agency.

Geographic entities mentioned:
surface_form: Kolsås
instance_of: Mountain
countries: Norway
coordinates: lat: 59.933333333333
lon: 10.516666666667
He divided his army into two groups. The larger force would enter the Indus Valley through the Khyber Pass, just as Darius had done 200 years earlier, while a smaller force under the personal command of Alexander entered through a northern route, possibly through Broghol or Dorah Pass near Chitral.

Geographic entities mentioned:
surface_form: Chitral
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.85111111111111
lon: 71.78888888888889
Alexander was commanding a group of shield-bearing guards, foot-companions, archers, Agrianians, and horse-javelin-men and led them against the tribes of the former Gandhara satrapy. The first tribe they encountered were the Aspasioi tribe of the Kunar Valley, who initiated a fierce battle against Alexander, in which he himself was wounded in the shoulder by a dart.

Geographic entities mentioned:
surface_form: Kunar Valley
instance_of: Valley
countries: Pakistan
Afghanistan
Mughal Empire. In 1526, Babur, a Timurid descendant of Timur and Genghis Khan from Fergana Valley (modern-day Uzbekistan), swept across the Khyber Pass and founded the Mughal Empire, covering parts of modern-day eastern- Afghanistan, much of what is now Pakistan, parts of India and Bangladesh. The Mughals were descended from Central Asian Turks (with significant Mongol admixture).

Geographic entities mentioned:
surface_form: Fergana Valley
instance_of: Valley
countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
lon: 71.757777777778
Bethune's Gully is a notable geological feature of northern Dunedin, in the South Island of New Zealand. It is located close to the suburb of Normanby towards the northern end of North East Valley. It preserves a number of acres of very old-growth forest and a large stand of exotic Douglas fir, and is an ecosystem directly below the cloud forest on the upper slopes of Mount Cargill.

Geographic entities mentioned:
surface_form: Mount Cargill
instance_of: Mountain
countries: New Zealand
coordinates: lat: -45.813
lon: 170.555
Helianthus silphioides. &quot;Helianthus silphioides&quot; is a North American species of sunflower known by the common names rosinweed sunflower or Ozark sunflower. It is native to the central United States, primarily in the Ozarks and the Tennessee Valley with additional populations north into Kentucky and Illinois and south as far as Louisiana, Mississippi and Alabama.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
surface_form: Tennessee Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.959166666667
lon: -83.850277777778
Las Ánimas is a volcano of the Central Ranges of the Colombian Andes at the border of the departments of Cauca and Nariño. The volcano is high. As is the neighbouring Petacas, the volcano is part of the Doña Juana Volcanic Complex, and lies northeast of the main Doña Juana volcano and southeast of Petacas. The products of the volcanic activity of the volcano have been found in San Pablo, Nariño.

Geographic entities mentioned:
surface_form: Petacas
instance_of: Mountain
countries: Colombia
coordinates: lat: 1.6211
lon: -76.8425
surface_form: Doña Juana Volcanic Complex
instance_of: Mountain
countries: Colombia
coordinates: lat: 1.47075
lon: -76.924902777778
surface_form: petacas
instance_of: Mountain
countries: Colombia
coordinates: lat: 1.6211
lon: -76.8425
surface_form: doña juana
instance_of: Mountain
countries: Colombia
coordinates: lat: 1.47075
lon: -76.924902777778
Las Ánimas (volcano). Las Ánimas is a volcano of the Central Ranges of the Colombian Andes at the border of the departments of Cauca and Nariño. The volcano is high. As is the neighbouring Petacas, the volcano is part of the Doña Juana Volcanic Complex, and lies northeast of the main Doña Juana volcano and southeast of Petacas.

Geographic entities mentioned:
surface_form: las ánimas (volcano)
instance_of: Mountain
countries: Colombia
coordinates: lat: 1.564
lon: -76.85436111
Las Ánimas (volcano). Las Ánimas is a volcano of the Central Ranges of the Colombian Andes at the border of the departments of Cauca and Nariño. The volcano is high. As is the neighbouring Petacas, the volcano is part of the Doña Juana Volcanic Complex, and lies northeast of the main Doña Juana volcano and southeast of Petacas.

Geographic entities mentioned:
surface_form: las ánimas
instance_of: Mountain
countries: Colombia
coordinates: lat: 1.564
lon: -76.85436111
Welland Canal. The Welland Canal is a ship canal in Ontario, Canada, and part of the St. Lawrence Seaway and Great Lakes Waterway. The canal traverses the Niagara Peninsula between Port Weller on Lake Ontario, and Port Colborne on Lake Erie, and was erected because the Niagara River—the only natural waterway connecting the lakes—was unnavigable due to Niagara Falls.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
The canal traverses the Niagara Peninsula between Port Weller on Lake Ontario, and Port Colborne on Lake Erie, and was erected because the Niagara River—the only natural waterway connecting the lakes—was unnavigable due to Niagara Falls. The Welland Canal enables ships to ascend and descend the Niagara Escarpment, and has followed four different routes since it opened.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
It takes ships an average of about eleven hours to traverse the entire length of the Welland Canal. History. Before the digging of the Welland Canal, shipping traffic between Lake Ontario and Lake Erie used a portage road between Chippawa, Ontario, and Queenston, Ontario, which are both located on the Niagara River—above and below Niagara Falls, respectively. First Welland Canal.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Catharines. From there it took a winding route up the Niagara Escarpment through Merritton, Ontario, to Thorold, where it continued south via Allanburg to Port Robinson, Ontario, on the Welland River. Ships went east (downstream) on the Welland River to Chippawa, at the south (upper) end of the old portage road, where they made a sharp right turn into the Niagara River, upstream towards Lake Erie.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
surface_form: Welland River
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.0377
lon: -79.1798
The town sits on top of the Eastern Continental Divide, with Camp Creek, draining the northern half of town, flowing north to Hazel Creek and the Soquee River, a tributary of the Chattahoochee River, and ultimately the Gulf of Mexico, while the southern half of town drains to Nancy Town Creek, then the Middle Fork of the Broad River and eventually the Savannah River, which flows to the Atlantic Ocean.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Monbiot argued that Bolton was one of the instigators of the Iraq War, of which Monbiot was an opponent. Politics. After Monbiot visited the remote Baliem Valley and criticised the Indonesian government's transmigration program and other policies in occupied Western New Guinea, Indonesian authorities sentenced him in absentia to life imprisonment. Monbiot is a critic of neoliberalism.

Geographic entities mentioned:
surface_form: Baliem Valley
instance_of: Valley
countries: Indonesia
coordinates: lat: -4.0218083333333
lon: 138.89602777778
It is surrounded by muskeg and boreal forest. Its primary inflow is from a channel connected to Culdesac River, which is a tributary of the Carrot River. An outlet from the eastern end of Culdesac Lake connects it to the Pasquia River — a tributary of the Saskatchewan River. The lake falls within the Cumberland Marshes (SK 102) Important Bird Area of Canada.

Geographic entities mentioned:
surface_form: Pasquia River
instance_of: Watercourse
countries: Canada
coordinates: lat: 53.82539
lon: -101.25913
Lake City, Seattle. Lake City is a neighborhood and the northeast region of Seattle, centered along Lake City Way NE (SR-522), 7–8 miles (11–13 km) northeast of downtown Seattle. A broader definition of the Lake City area includes all the land between 15th Avenue NE and Lake Washington, and between NE 95th and 98th streets to the Seattle city limits at NE 145th Street.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
8,000 BCE&mdash;10,000 years ago). The &quot;hah-chu-ahbsh&quot; (Lake People), now of the Duwamish tribe, Lushootseed (Skagit-Nisqually) Coast Salish, lived in diffuse permanent settlements along the shore of Lake Washington, dispersing in the summer, and in the winter living in large cedar long houses, each home to a couple dozen or more members of extended family groups.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
The lake people lost their rights in 1854. The Lake City area was clearcut by crude wagon road or by using Lake Washington, from 1850 to around the start of the 20th century, more rapidly with the Seattle, Lake Shore and Eastern Railway (c. 1886) providing easy access along what is now the Burke–Gilman Trail adjacent to the lake. Wetlands were drained.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Purcell Knob. Purcell Knob is a spur of the Blue Ridge Mountain in Loudoun County, Virginia. The peak is just northeast of the main ridge at Keyes Gap and southeast of the village of Neersville. Purcell Knob is notable for exposure of the sericitic phyllite base of the Paleozoic Loudoun Formation in its antiformal syncline.

Geographic entities mentioned:
surface_form: Blue Ridge Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.08166667
lon: -77.86222222
surface_form: blue ridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.275833333333
lon: -74.403888888889
surface_form: purcell knob
instance_of: Mountain
countries: United States
coordinates: lat: 39.2582
lon: -77.7497
surface_form: blue ridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.60777778
lon: -76.09305556
Purcell Knob. Purcell Knob is a spur of the Blue Ridge Mountain in Loudoun County, Virginia. The peak is just northeast of the main ridge at Keyes Gap and southeast of the village of Neersville. Purcell Knob is notable for exposure of the sericitic phyllite base of the Paleozoic Loudoun Formation in its antiformal syncline.

Geographic entities mentioned:
surface_form: purcell knob
instance_of: Mountain
countries: United States
coordinates: lat: 39.2582
lon: -77.7497
Route. The entire route (Phase 2A and 2B) of the Foothill Extension follows the roadbed of the former Atchison, Topeka & Santa Fe Railway's Second Division through the Foothill Cities. These cities are in the foothills south of the San Gabriel Mountains, in the northern San Gabriel and Pomona valleys.

Geographic entities mentioned:
surface_form: San Gabriel
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
surface_form: Pomona
instance_of: Valley
countries: United States
coordinates: lat: 34.076
lon: -117.657
In October 2018, the Southern California Association of Governments (SCAG), in cooperation with the SBCTA and the Los Angeles Metro, conducted a transit and rail planning study for the corridor connecting the eastern San Gabriel Valley in Los Angeles County with the western San Bernardino Valley in San Bernardino County.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
surface_form: San Bernardino Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.066666666667
lon: -117.28333333333
Canoe and tube rentals are available in nearby Caddo Valley, Arkansas. The Ouachita National Forest and Hot Springs National Park are located on the scenic byway, approximately north of Arkadelphia. To the west of Hot Springs is Lake Ouachita, which has more than of shoreline and more than of water. The lake is surrounded by Ouachita National Forest.

Geographic entities mentioned:
surface_form: Lake Ouachita
instance_of: Lake
countries: United States
coordinates: lat: 34.6
lon: -93.3333
Isabelle Glacier. Isabelle Glacier is an alpine glacier located northeast of Apache Peak and southwest of Shoshoni Peak, in Roosevelt National Forest in the US state of Colorado. The glacier is immediately east of the Continental Divide on the opposite side of the divide from Fair Glacier.

Geographic entities mentioned:
surface_form: Apache Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.058333333333
lon: -105.65111111111
It is situated on the eastern boundary of the John Muir Wilderness, on land managed by Inyo National Forest. It is 1.3 mile southeast of Tinemaha Lake, and 1.8 mile northeast of parent Split Mountain. Topographic relief is significant as the east aspect rises above Owens Valley in two miles. History. This mountain's name was officially adopted in 1937 by the U.S.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
Most weather fronts originate in the Pacific Ocean, and travel east toward the Sierra Nevada mountains. As fronts approach, they are forced upward by the peaks, causing them to drop their moisture in the form of rain or snowfall onto the range (orographic lift). Precipitation runoff from this mountain drains to Red Mountain Creek and Tinemaha Creek, thence Tinemaha Reservoir.

Geographic entities mentioned:
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.4867
lon: -86.8064
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.3918
lon: -121.145
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.60041
lon: -120.98678
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.5231
lon: -111.876
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.415277777778
lon: -121.46694444444
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.45588
lon: -121.3891607
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.064444444444
lon: -117.24638888889
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.2979
lon: -119.441
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.26751
lon: -74.54952
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.5356
lon: -113.424
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.1122
lon: -105.181
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.9036
lon: -107.702
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.9783
lon: -110.872
This mountain's name was officially adopted in 1937 by the U.S. Board on Geographic Names to honor the legendary Paiute chief, Tinemaha. The peak was known by this name to the early prospectors and cattlemen of Owens Valley. The first ascent of the summit was made July 1, 1937, by Chester Versteeg, a prominent Sierra Club member. Chester Versteeg submitted the name to the board for consideration.

Geographic entities mentioned:
surface_form: owens valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
It is situated on the eastern boundary of the John Muir Wilderness, on land managed by Inyo National Forest. It is 1.3 mile southeast of Tinemaha Lake, and 1.8 mile northeast of parent Split Mountain. Topographic relief is significant as the east aspect rises above Owens Valley in two miles. History. This mountain's name was officially adopted in 1937 by the U.S.

Geographic entities mentioned:
surface_form: split mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.164166666667
lon: -109.6725
surface_form: split mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.020833333333
lon: -118.42222222222
surface_form: split mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.483333333333
lon: -109.22055555556
surface_form: split mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.5981
lon: -113.539
Mount Tinemaha. Mount Tinemaha is a mountain summit located east of the crest of the Sierra Nevada mountain range, in Inyo County of northern California. It is situated on the eastern boundary of the John Muir Wilderness, on land managed by Inyo National Forest. It is 1.3 mile southeast of Tinemaha Lake, and 1.8 mile northeast of parent Split Mountain.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount tinemaha
instance_of: Mountain
countries: United States
coordinates: lat: 37.03605
lon: -118.39732
Mount Tinemaha. Mount Tinemaha is a mountain summit located east of the crest of the Sierra Nevada mountain range, in Inyo County of northern California. It is situated on the eastern boundary of the John Muir Wilderness, on land managed by Inyo National Forest. It is 1.3 mile southeast of Tinemaha Lake, and 1.8 mile northeast of parent Split Mountain.

Geographic entities mentioned:
surface_form: mount tinemaha
instance_of: Mountain
countries: United States
coordinates: lat: 37.03605
lon: -118.39732
The first ascent of the summit was made July 1, 1937, by Chester Versteeg, a prominent Sierra Club member. Chester Versteeg submitted the name to the board for consideration. Climate. According to the Köppen climate classification system, Mount Tinemaha has an alpine climate. Most weather fronts originate in the Pacific Ocean, and travel east toward the Sierra Nevada mountains.

Geographic entities mentioned:
surface_form: mount tinemaha
instance_of: Mountain
countries: United States
coordinates: lat: 37.03605
lon: -118.39732