Sarmila/GeoWiki-Features huggingface dataset:
Salmon Lake Mountain. Salmon Lake Mountain is a summit located in Adirondack Mountains of New York. It is located west of the hamlet of Long Lake in Hamilton County. Around 1933, a Aermotor LX24 tower was built on the mountain. The tower was privately owned, but cooperated with the Conservation Commission for fire watching operations.

Geographic entities mentioned:
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 34.78779
lon: -111.210939
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9728
lon: -74.4211
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.718
lon: -85.748
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.1086787
lon: -75.1564925
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.1657291
lon: -98.7168782
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9334172
lon: -97.0073724
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9496317
lon: -95.9225667
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.8456754
lon: -99.2676497
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.127777777778
lon: -83.973055555556
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 46.235907
lon: -89.49916
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9348621
lon: -97.3996461
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.20461
lon: -83.47775
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.5597393
lon: -75.1515847
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.248184
lon: -85.075807
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 41.615555555556
lon: -87.210555555556
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.7281765
lon: -97.3795798
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 47.483055555556
lon: -122.58972222222
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.971666666667
lon: -70.611666666667
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.8387529
lon: -88.6755297
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 47.0191485
lon: -122.7747634
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.572222222222
lon: -85.298888888889
Salmon Lake Mountain. Salmon Lake Mountain is a summit located in Adirondack Mountains of New York. It is located west of the hamlet of Long Lake in Hamilton County. Around 1933, a Aermotor LX24 tower was built on the mountain. The tower was privately owned, but cooperated with the Conservation Commission for fire watching operations.

Geographic entities mentioned:
surface_form: salmon lake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.963055555556
lon: -74.646111111111
surface_form: salmon lake
instance_of: Lake
countries: United States
coordinates: lat: 43.946388888889
lon: -74.940277777778
surface_form: salmon lake
instance_of: Lake
countries: United States
coordinates: lat: 64.9028
lon: -165.009
The tower was privately owned, but cooperated with the Conservation Commission for fire watching operations. The tower still remains, but is in poor condition and is not open to the public. History. Around 1933, Whitney Park built a Aermotor LX24 tower on the mountain. The tower was privately owned, but cooperated with the Conservation Commission.

Geographic entities mentioned:
surface_form: whitney
instance_of: Mountain
countries: United States
coordinates: lat: 36.57861111111111
lon: -118.29194444444444
Penygraig. Penygraig is a village and community in the Rhondda Valley in the county borough of Rhondda Cynon Taf, Wales. As a community Penygraig contains the neighbouring districts of Dinas, Edmondstown, Penrhiwfer and Williamstown. Penygraig is within the historic county boundaries of Glamorgan. The name Penygraig is Welsh for 'head of the rock'. Early history.

Geographic entities mentioned:
surface_form: Rhondda Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
The KB-29Ms were scrapped soon after. Four SAC RB-29As of the 16th Photographic Reconnaissance Squadron visited RAF Scampton in October and November 1948. One crashed at Bleaklow in Derbyshire, killing all 13 on board. Twelve RB-29As of the 23rd Strategic Reconnaissance Squadron deployed to RAF Sculthorpe from December 1949 to March 1950.

Geographic entities mentioned:
surface_form: crashed at Bleaklow
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.46
lon: -1.8626
It was released on 7 January 2015 in France. Plot. The story, inspired by actual events, takes place in 1977 in the Swiss town of Vevey, on Lake Geneva. Eddy, a 40-year-old thug, has just been released from the prison. In order to stay in his friend Osman's trailer, Eddy will have to take care of Osman's 7-year-old daughter Samira as Osman's wife Noor is hospitalized.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
He was awarded the Acharius Medal in 1992 for his lifetime contributions to lichenology. Early life and education. Santesson was born in 1916 in Trollhättan, Sweden. He was already collecting lichens as a student, investigating the lichen flora of the table mountains of Halleberg and Hunneberg near his home. He entered the University of Uppsala in the 1930s to study botany.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
List of mountain peaks of Maharashtra. Maharashtra has an extensive mountain range running parallel to its 750 km long coastline. This range is geographically part of the Sahyadris or the Western Ghats which forms a crest along the western edge. of the Deccan plateau separating it from the coastal Konkan belt. Throughout its extent it bears some renowned peaks, hill stations and valleys.

Geographic entities mentioned:
surface_form: Deccan plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Baker Lake (Alpine Lakes Wilderness). Baker Lake is a small freshwater lake located within the Alpine Lakes Wilderness in a valley on the northern slope of Keechelus Ridge between Keechelus Lake and Kachess Lake in Kittitas County, Washington, United States. Big Creek, a tributary to the Taylor River, exits Baker Lake into a canyon that produces Big Creek Falls.

Geographic entities mentioned:
surface_form: Keechelus Lake
instance_of: Lake
countries: United States
coordinates: lat: 47.34777777777778
lon: -121.36888888888889
surface_form: Kachess Lake
instance_of: Lake
countries: United States
coordinates: lat: 47.307795
lon: -121.232403
surface_form: baker lake
instance_of: Lake
countries: United States
coordinates: lat: 47.3515175
lon: -121.3017165
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Baker Lake (Alpine Lakes Wilderness). Baker Lake is a small freshwater lake located within the Alpine Lakes Wilderness in a valley on the northern slope of Keechelus Ridge between Keechelus Lake and Kachess Lake in Kittitas County, Washington, United States. Big Creek, a tributary to the Taylor River, exits Baker Lake into a canyon that produces Big Creek Falls.

Geographic entities mentioned:
surface_form: baker lake
instance_of: Lake
countries: United States
coordinates: lat: 47.3515175
lon: -121.3017165
Because of its proximity to Rampart Ridge, Interstate 90 and the cirque of Keechelus Ridge a short distance to the south, the lake is a popular area for hiking, swimming, and fishing brook trout, golden trout and rainbow trout. Access to Baker Lake is provided through Keechelus Ridge off Forest Road 126.

Geographic entities mentioned:
surface_form: baker lake
instance_of: Lake
countries: United States
coordinates: lat: 47.3515175
lon: -121.3017165
She politely refused, but the persistent Lawa king threatened to conquer Hariphunchai by force. To avoid a direct war, Queen Camadevi proposed a series of challenges. The most famous of these was a contest of strength and skill: a competition to throw a spear from the peak of Doi Suthep, the mountain overlooking the Chiang Mai basin, to the city walls of Hariphunchai.

Geographic entities mentioned:
surface_form: Doi Suthep
instance_of: Mountain
countries: Thailand
coordinates: lat: 18.816388888889
lon: 98.893055555556
In the village of Ban Mueang Ka, it is believed that the Lawa people there are descendants of Khun Luang Wirangka. Furthermore, the villagers believe that the spirit of Khun Luang resides in three locations: on Doi Khwam Long, at the shrine in Ban Mueang Ka (Mae Rim district), and in the Doi Kham area (Mueang Chiang Mai district), which is located south of Doi Suthep.

Geographic entities mentioned:
surface_form: Doi Suthep
instance_of: Mountain
countries: Thailand
coordinates: lat: 18.816388888889
lon: 98.893055555556
The piling of rocks marked it. It was a reminder of peace where each would not go beyond these rocks to attack the other. In the incident of the Levite's concubine, the men of Gibeah raped a woman. The other Israelite tribes met at the Mizpah of Benjamin, where they decided to attack the Benjaminites for this grievous sin according to Judges 20:1–11.

Geographic entities mentioned:
surface_form: Gibeah
instance_of: Mountain
countries: State of Palestine
coordinates: lat: 31.823372222222
lon: 35.23115
Chaku River. Chaku River is a tributary of Bhotekoshi River. The river is located in Sindhupalchowk District of central Nepal. Infrastructures. The river has a large hydropower potential and a number of projects are under development such as

Geographic entities mentioned:
surface_form: Bhotekoshi River
instance_of: Watercourse
countries: Nepal
People's Republic of China
coordinates: lat: 27.712
lon: 85.765
In August 1943, the battalion deployed to New Guinea again for its second campaign against the Japanese. Staging out of Port Moresby, in early September the 7th Division was flown into Nadzab, and the 2/16th supported operations to capture Lae. After this, it was air transported to Kaiapit, where from late September it took part in the advance up the Markham Valley towards Dumpu.

Geographic entities mentioned:
surface_form: Markham Valley
instance_of: Valley
countries: Papua New Guinea
coordinates: lat: -6.7388888888889
lon: 146.96805555556
Scandian Phase. The Scandian phase involved a collision between eastern Greenland on the eastern margin of Laurentia and the margin of the Baltoscandian platform of the Fennoscandian peninsula of Baltica. It involved the Scandinavian Caledonides in what is now Norway and the Swedish areas by its border. It occurred from the Wenlock Epoch of the Silurian to the Mid Devonian (430–380 Ma). Gee et al.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
This orogenic event also affected Scotland and the outer Hebrides, causing thrusting in the Northern Highlands which culminated in the development of the Moine Thrust Belt, Ben Hope Thrust and Naver-Sgurr Beag Thrust (435–420 Ma) and led to igneous intrusion in Galloway and the Southern Uplands (c. 400 Ma) in Scotland and the enlargement of the Lake District batholith in northern England.

Geographic entities mentioned:
surface_form: Ben Hope
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.41355
lon: -4.6087388888889
The closure of this ocean involved the (early) Eo-Variscan collision of Gondwana-related terranes in which Eastern Avalonia was peripherally involved. Subduction of the Iapetus Ocean occurred beneath the Midland Valley terrane of Scotland.

Geographic entities mentioned:
surface_form: Midland Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.408
lon: -4.044
Thus they invoke a model of slab drop-off caused by lithospheric mantle delamination. Northern England, Lake District. The Lakesman terrane covers the north of England down to the Wensleydale in North Yorkshire and crosses the Irish Sea passing by the Island of Anglesey off Wales. Its continuation in eastern Ireland is the Leinster terrane. The combined terrane is termed Leinster-Lakesman terrane.

Geographic entities mentioned:
surface_form: Wensleydale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.3056
lon: -2.16667
It consists of a series of faults with no traces of subduction, such as ophiolite remnants or oceanic trench-derived rocks. The Iapetus Suture also extends along the margin of the Baltoscandian platform of the Fennoscandian Peninsula which collided with the eastern margin of Greenland along the eastern margin of Laurentia in the Scandian orogeny. Controversies.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Lehigh Valley Zoo. The Lehigh Valley Zoo is a zoo located in Schnecksville in the Lehigh Valley region of eastern Pennsylvania. It is located inside the Trexler Nature Preserve. The zoo is open year round. Lehigh Valley Zoo has been accredited by the Association of Zoos and Aquariums (AZA) since March 2006. History.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Parascutigera festiva. &quot;Parascutigera festiva&quot; is a species of centipede in the Scutigeridae family. It is endemic to New Caledonia, a French overseas territory in Melanesia. It was first described in 1923 by French entomologist Henri Ribaut. Distribution. The species occurs on the main island of Grande Terre. The type locality is Mont Panié.

Geographic entities mentioned:
surface_form: Mont Panié
instance_of: Mountain
countries: France
coordinates: lat: -20.588333333333
lon: 164.77055555556
MacLeod, a Canadian Pacific Railroad surveyor who investigated a potential route in the Maligne Valley in 1875. Geology. Like other mountains in Banff Park, the mountain is composed of sedimentary rock laid down during 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. Climate.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Henry MacLeod. Mount Henry MacLeod is a summit located in Jasper National Park, in the Canadian Rockies of Alberta, Canada. Mount Henry MacLeod was named for Henry A. MacLeod, a Canadian Pacific Railroad surveyor who investigated a potential route in the Maligne Valley in 1875. Geology.

Geographic entities mentioned:
surface_form: mount henry
instance_of: Mountain
countries: Canada
coordinates: lat: 52.93332
lon: -118.25239
surface_form: mount henry macleod
instance_of: Mountain
countries: Canada
coordinates: lat: 52.53333
lon: -117.35229
The full music video which aired on MTV's &quot;The Tom Green Show&quot; shows Green in a variety of costumes and settings, placing his bum on objects and doing stunts, such as grabbing onto a moving vehicle while riding a skateboard. He arrives at Lake Washington where he wades in to find a loon which is actually a duck decoy.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Geiseltalsee. Geiseltalsee, literally Geisel valley lake, is at about the largest artificial lake by area in Germany. Once flooding of the Cottbuser Ostsee is complete it will surpass Geiseltalsee in surface area, covering. Geiseltalsee lies in the Saalekreis district of the state Saxony-Anhalt.

Geographic entities mentioned:
surface_form: Cottbuser Ostsee
instance_of: Lake
countries: Germany
coordinates: lat: 51.7875
lon: 14.4322
surface_form: geiseltalsee
instance_of: Lake
countries: Germany
coordinates: lat: 51.308
lon: 11.8854
Geiseltalsee lies in the Saalekreis district of the state Saxony-Anhalt. The lake was created in 2003-11 by flooding a former opencast lignite mine in the Geiseltal (Geisel valley); the name of that valley had become widely known due to the notable fossil record which emerged from that coal mine. Dimensions.

Geographic entities mentioned:
surface_form: Geiseltal
instance_of: Valley
countries: Germany
coordinates: lat: 51.307777777778
lon: 11.869166666667
surface_form: geisel valley
instance_of: Valley
countries: Germany
coordinates: lat: 51.307777777778
lon: 11.869166666667
The lake was created in 2003-11 by flooding a former opencast lignite mine in the Geiseltal (Geisel valley); the name of that valley had become widely known due to the notable fossil record which emerged from that coal mine. Dimensions. At surface area it is the largest artificial lake in Germany by surface area until Cottbuser Ostsee reaches its planned final size of.

Geographic entities mentioned:
surface_form: Cottbuser Ostsee
instance_of: Lake
countries: Germany
coordinates: lat: 51.7875
lon: 14.4322
However, the depth of flooded former open pit mines tends to decrease in the first few decades after flooding, as evidenced by Senftenberger See which was flooded from 1967 to 1972 reaching a maximum depth of but which has no point exceeding a depth of according to more recent measurements. Location.

Geographic entities mentioned:
surface_form: senftenberger see
instance_of: Lake
countries: Germany
coordinates: lat: 51.5
lon: 14.016666666667
While there had been vague plans to flood the resulting &quot;holes&quot; left over from mining (even if all overburden were filled back into the former mine, the &quot;missing&quot; coal would mean the surface would still be below the natural water table) as had been done with what is now Senftenberger See, the plans for the deep and wide former mine were only seriously made after reunification.

Geographic entities mentioned:
surface_form: senftenberger see
instance_of: Lake
countries: Germany
coordinates: lat: 51.5
lon: 14.016666666667
Geiseltalsee. Geiseltalsee, literally Geisel valley lake, is at about the largest artificial lake by area in Germany. Once flooding of the Cottbuser Ostsee is complete it will surpass Geiseltalsee in surface area, covering. Geiseltalsee lies in the Saalekreis district of the state Saxony-Anhalt.

Geographic entities mentioned:
surface_form: geisel valley
instance_of: Valley
countries: Germany
coordinates: lat: 51.307777777778
lon: 11.869166666667
surface_form: geiseltalsee
instance_of: Lake
countries: Germany
coordinates: lat: 51.308
lon: 11.8854
Geiseltalsee. Geiseltalsee, literally Geisel valley lake, is at about the largest artificial lake by area in Germany. Once flooding of the Cottbuser Ostsee is complete it will surpass Geiseltalsee in surface area, covering. Geiseltalsee lies in the Saalekreis district of the state Saxony-Anhalt.

Geographic entities mentioned:
surface_form: geiseltalsee
instance_of: Lake
countries: Germany
coordinates: lat: 51.308
lon: 11.8854
Location. Geiseltalsee is bordered by the village of Mücheln to the southwest, west, and northwest, the towns of Braunsbedra to the northeast, east, and southeast, and of Bad Lauchstädt for a small stretch to the northwest. The lake is a part of the Central German Lake District. History.

Geographic entities mentioned:
surface_form: geiseltalsee
instance_of: Lake
countries: Germany
coordinates: lat: 51.308
lon: 11.8854
In a 28 November 2019 article in &quot;The Economist&quot;, it was reported that President Trump's decision to place sanctions on Gertler, who is a close friend of then-President of the Congo, Joseph Kabila, had come as &quot;a shock to many companies operating in the Congo.&quot; Citing Tom Perriello, then the United States envoy to the African Great Lakes under Barack Obama, the sanctions &quot;probably helped push Mr.

Geographic entities mentioned:
surface_form: African Great Lakes
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
Snowdonia. Snowdonia, or (), is a mountainous region and national park in North Wales. It contains all 15 mountains in Wales over 3000 feet high, including the country's highest, Snowdon (), which is tall. These peaks are all part of the Snowdon, Glyderau, and Carneddau ranges in the north of the region. The shorter Moelwynion and Moel Hebog ranges lie immediately to the south.

Geographic entities mentioned:
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
Snowdonia. Snowdonia, or (), is a mountainous region and national park in North Wales. It contains all 15 mountains in Wales over 3000 feet high, including the country's highest, Snowdon (), which is tall. These peaks are all part of the Snowdon, Glyderau, and Carneddau ranges in the north of the region. The shorter Moelwynion and Moel Hebog ranges lie immediately to the south.

Geographic entities mentioned:
surface_form: Carneddau
instance_of: Landform
countries: United Kingdom
coordinates: lat: 53.18114
lon: -4.00297
These peaks are all part of the Snowdon, Glyderau, and Carneddau ranges in the north of the region. The shorter Moelwynion and Moel Hebog ranges lie immediately to the south. The national park has an area of (the fourth-largest in the UK), and covers most of central and southern Gwynedd and the western part of Conwy County Borough.

Geographic entities mentioned:
surface_form: Moel Hebog
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.000138888889
lon: -4.1398
The national park has an area of (the fourth-largest in the UK), and covers most of central and southern Gwynedd and the western part of Conwy County Borough. This is much larger than the area traditionally considered Snowdonia, and in addition to the five ranges above includes the Rhinogydd, Cadair Idris, and Aran ranges and the Dyfi Hills.

Geographic entities mentioned:
surface_form: Cadair Idris
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.699827777778
lon: -3.9086944444444
surface_form: Aran
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.78702
lon: -3.68786
Its boundaries were described as stretching from the Conwy valley to Fairy Glen gorge (near Betws-y-Coed), then from the Lledr Valley towards Dolwyddelan, and then across the hills to the valley of Ffestiniog and to Porthmadog (Portmadoc), before following the road to Caernarfon passing Dolbenmaen and Llanllyfni.

Geographic entities mentioned:
surface_form: Lledr Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.06
lon: -3.87
Which encompasses the masses of Snowdon, the Carneddau, Glyderau, Moel Hebog, as well as the mountains extending from Moel Siabod forming the Moelwynion which was in neighbouring Merionethshire. The Nant Ffrancon Pass, Llanberis Pass, the glen between Siabod, the Glyderau and Capel Curig, and the Gwynant valley to Beddgelert, separates those mountain groups.

Geographic entities mentioned:
surface_form: Carneddau
instance_of: Landform
countries: United Kingdom
coordinates: lat: 53.18114
lon: -4.00297
surface_form: Moel Hebog
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.000138888889
lon: -4.1398
surface_form: Moel Siabod
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.073075
lon: -3.9324638888889
Which encompasses the masses of Snowdon, the Carneddau, Glyderau, Moel Hebog, as well as the mountains extending from Moel Siabod forming the Moelwynion which was in neighbouring Merionethshire. The Nant Ffrancon Pass, Llanberis Pass, the glen between Siabod, the Glyderau and Capel Curig, and the Gwynant valley to Beddgelert, separates those mountain groups.

Geographic entities mentioned:
surface_form: Nant Ffrancon Pass
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.1484
lon: -4.0414
Snowdonia was also suggested to extend further south into Merionethshire, with this part bounded by the north by Afon Glaslyn, the glen between Dolgellau and Trawsfynydd to the east, Cadair Idris (overlooking the Mawddach estuary) to the south and the coast to the west. In &quot;Snowdonia: The National Park of North Wales&quot; (1949), F. J.

Geographic entities mentioned:
surface_form: Cadair Idris
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.699827777778
lon: -3.9086944444444
Mountains. The principal ranges of the traditional Snowdonia are the Snowdon massif itself, the Glyderau, the Carneddau, the Moelwynion and the Moel Hebog range. All of Wales' 3000ft mountains are to be found within the first three of these massifs and are most popular with visitors. To their south within the wider national park are the Rhinogydd and the Cadair Idris and Aran Fawddwy ranges.

Geographic entities mentioned:
surface_form: Carneddau
instance_of: Landform
countries: United Kingdom
coordinates: lat: 53.18114
lon: -4.00297
surface_form: Moel Hebog
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.000138888889
lon: -4.1398
Mountains. The principal ranges of the traditional Snowdonia are the Snowdon massif itself, the Glyderau, the Carneddau, the Moelwynion and the Moel Hebog range. All of Wales' 3000ft mountains are to be found within the first three of these massifs and are most popular with visitors. To their south within the wider national park are the Rhinogydd and the Cadair Idris and Aran Fawddwy ranges.

Geographic entities mentioned:
surface_form: Cadair Idris
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.699827777778
lon: -3.9086944444444
surface_form: Aran Fawddwy
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.78702
lon: -3.68786
Further west the and empty into the western end of the Menai Strait. Part of the east of the national park is within the upper Dee (Dyfrydwy) catchment and includes Bala Lake, the largest natural water body in Wales. A fuller list of the rivers and tributaries within the area is found at List of rivers of Wales.There are few natural bodies of water of any size in Wales; Snowdonia is home to most.

Geographic entities mentioned:
surface_form: Bala Lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.883333333333
lon: -3.6333333333333
Climate. Snowdonia is one of the wettest parts of the United Kingdom; Crib Goch in Snowdonia is the wettest spot in the United Kingdom, with an average rainfall of a year over the 30-year period prior to the mid-2000s. (There is a rainfall gauge at on the slopes below Crib Goch.)
History.

Geographic entities mentioned:
surface_form: Crib Goch
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.075541666667
lon: -4.0535138888889
However, there are also some spectacular walks in Snowdonia on the lower mountains, and they tend to be relatively unfrequented. Among hikers' favourites are Y Garn (east of Llanberis) along the ridge to Elidir Fawr; Mynydd Tal-y-Mignedd (west of Snowdon) along the Nantlle Ridge to Mynydd Drws-y-Coed; Moelwyn Mawr (west of Blaenau Ffestiniog); and Pen Llithrig y Wrach north of Capel Curig.

Geographic entities mentioned:
surface_form: Elidir Fawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.130738888889
lon: -4.0760305555556
surface_form: Moelwyn Mawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.983688888889
lon: -4.0004388888889
surface_form: Pen Llithrig y Wrach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.142330555556
lon: -3.9210805555556
Among hikers' favourites are Y Garn (east of Llanberis) along the ridge to Elidir Fawr; Mynydd Tal-y-Mignedd (west of Snowdon) along the Nantlle Ridge to Mynydd Drws-y-Coed; Moelwyn Mawr (west of Blaenau Ffestiniog); and Pen Llithrig y Wrach north of Capel Curig. Further south are Y Llethr in the Rhinogydd, and Cadair Idris near Dolgellau.

Geographic entities mentioned:
surface_form: Y Llethr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.81285
lon: -3.98763
surface_form: Cadair Idris
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.699827777778
lon: -3.9086944444444
Use of in English. There have been calls to use the Welsh name for the area, &quot;Eryri&quot;, in preference to &quot;Snowdonia&quot; in English-language contexts. In 2003, the pressure group Cymuned campaigned for such a change, inspired by other campaigns such as Ayers Rock being known as Uluru and Mount Everest as Qomolangma.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Mellona Rocks. Mellona Rocks is a group of scattered rocks lying at the north entrance to Nelson Strait in the South Shetland Islands, Antarctica and extending. The area was known to the early 19th-century sealers and sometimes included under the names 'Heywood Islands' or 'Powels Islands'.

Geographic entities mentioned:
surface_form: nelson strait
instance_of: Body of water
coordinates: lat: -62.35
lon: -59.2833
surface_form: mellona rocks
instance_of: Mountain
coordinates: lat: -62.29702778
lon: -59.49544444
Location. The rocks are centred at which is north-northeast of Newell Point, Robert Island, east-northeast of the midpoint of Opaka Rocks, west of Harmony Point, Nelson Island and northwest of Liberty Rocks (British mapping in 1822, 1962 and 1968, Chilean in 1961 and 1971, Argentine in 1980, and Bulgarian in 2009).

Geographic entities mentioned:
surface_form: nelson
instance_of: Body of water
coordinates: lat: -62.35
lon: -59.2833
The area was known to the early 19th-century sealers and sometimes included under the names 'Heywood Islands' or 'Powels Islands'. The feature is named after the British sealing ship &quot;Mellona&quot; under Captain Thomas Johnson that operated in the South Shetlands in 1821–22. Location.

Geographic entities mentioned:
surface_form: thomas
instance_of: Mountain
coordinates: lat: -71.01666667
lon: 64.6
Mellona Rocks. Mellona Rocks is a group of scattered rocks lying at the north entrance to Nelson Strait in the South Shetland Islands, Antarctica and extending. The area was known to the early 19th-century sealers and sometimes included under the names 'Heywood Islands' or 'Powels Islands'.

Geographic entities mentioned:
surface_form: mellona rocks
instance_of: Mountain
coordinates: lat: -62.29702778
lon: -59.49544444
The glacier lies at and above the source the river Mulkhra. The length of the Tsaneri Glacier is and its surface area is. Tsaneri consists of two branches that feed off of the adjacent glaciers that are located on the slopes of Mt. Tikhtengeni, Lalveri, Tetnuldi, and Gistola. Size.

Geographic entities mentioned:
surface_form: Lalveri
instance_of: Mountain
countries: Russia
Georgia
Russian Empire
Soviet Union
coordinates: lat: 43.070833333333
lon: 43.016111111111
surface_form: Tetnuldi
instance_of: Mountain
countries: Georgia
coordinates: lat: 43.031388888889
lon: 42.993055555556
surface_form: Gistola
instance_of: Mountain
countries: Georgia
Russia
Russian Empire
Soviet Union
coordinates: lat: 43.048055555556
lon: 43.025277777778
Naftali Mountains. Naftali Mountains () is a mountain range between Lebanon and Upper Galilee, Israel. The western side gradually changes into the highlands of southern Lebanon. The eastern side sharply descends into the Hula Valley of Israel. They are a part of the watershed between the basins of the Mediterranean Sea and the Jordan River.

Geographic entities mentioned:
surface_form: Hula Valley
instance_of: Valley
countries: Israel
coordinates: lat: 33.103333333333
lon: 35.609166666667
The area was the place of heavy fighting in 1948 during the 1948 Palestine war. Geography. The Israeli side of Naftali Mountains rises about 300 meters above the agricultural areas of Hula Valley. The southern part of the mountains is marked by the Dishon Stream. In the Lebanoni side, the northern border of the mountains is marked by the Litani River.

Geographic entities mentioned:
surface_form: Hula Valley
instance_of: Valley
countries: Israel
coordinates: lat: 33.103333333333
lon: 35.609166666667
They were also to verify, through observation and patrolling, that troops from either side did not remain in or re-enter the security zone, and that heavy military equipment did not remain or be re-introduced. UNOMIG was to oversee the withdrawal of Georgian troops from the Kodori Valley and thus, out of Abkhaz territory. Their patrols replaced those of Georgia in the valley.

Geographic entities mentioned:
surface_form: Kodori Valley
instance_of: Valley
countries: Georgia
coordinates: lat: 43.1
lon: 41.8
Barossa Valley Way. Barossa Valley Way is the main road linking most of the major towns of the Barossa Valley in South Australia, designated as route B19 for its entire length. It is 35 km long, roughly following the North Para River. Route.

Geographic entities mentioned:
surface_form: Barossa Valley
instance_of: Valley
countries: Australia
coordinates: lat: -34.533333333333
lon: 138.95
Oppheim Church. Oppheim Church () is a parish church of the Church of Norway in Voss Municipality in Vestland county, Norway. It is located in the village of Oppheim, located on the northern shore of the lake Oppheimsvatnet. It is the church for the Oppheim parish which is part of the Hardanger og Voss prosti (deanery) in the Diocese of Bjørgvin.

Geographic entities mentioned:
surface_form: Oppheimsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 60.798055555556
lon: 6.6111111111111
The church seats about 250 people. History. The earliest existing historical records of the church date back to the year 1329, but it was built before that time. The first church was a wooden stave church that was likely built during the 13th century. It was located about northwest of the present site by the lake Oppheimsvatnet. Little is known about that church and it was torn down in 1673.

Geographic entities mentioned:
surface_form: Oppheimsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 60.798055555556
lon: 6.6111111111111
Geography. It is roughly bounded on the north by NY 3, the old Haybridge Road, which runs from Cold Brook to Averyville, the Adirondak Loj property at Heart Lake, the Mount Van Hoevenberg area and NY 73 near the Cascade Lakes. Private land to the west of Route 73 forms the eastern boundary.

Geographic entities mentioned:
surface_form: Mount Van Hoevenberg
instance_of: Mountain
countries: United States
coordinates: lat: 44.21
lon: -73.9293
The area includes 112 bodies of water on 1,392 acres (5.6 km2), 238.4 miles (383.5 km) of foot trails, 52.3 miles (84.1 km) of horse trails, and 84 lean-tos. The area contains 42 of the 46 Adirondack High Peaks, including the tallest, Mount Marcy.

Geographic entities mentioned:
surface_form: Mount Marcy
instance_of: Mountain
countries: United States
coordinates: lat: 44.112733333333
lon: -73.923727777778
The area contains 42 of the 46 Adirondack High Peaks, including the tallest, Mount Marcy. The topography ranges from small areas of low-lying swampland (e.g., along the Raquette and Saranac Rivers) to the highest point in New York State at the top of Mount Marcy. Although there is a considerable variety of topography, it is predominantly high mountain country.

Geographic entities mentioned:
surface_form: Mount Marcy
instance_of: Mountain
countries: United States
coordinates: lat: 44.112733333333
lon: -73.923727777778
Such streams as the Opalescent River, Johns Brook, Klondike Brook, Marcy Brook, Cold River and Moose Creek are frequently photographed. Lake Tear of the Clouds, often considered the source of the Hudson River, lies at about 4,300 feet (1,311 m) elevation on a flank of Mount Marcy. Recreation. This wilderness area is the most popular destination in the park.

Geographic entities mentioned:
surface_form: Lake Tear of the Clouds
instance_of: Lake
countries: United States
coordinates: lat: 44.1067
lon: -73.9358
surface_form: Mount Marcy
instance_of: Mountain
countries: United States
coordinates: lat: 44.112733333333
lon: -73.923727777778
The Northville-Placid Trail crosses the High Peaks Wilderness Area from its southeastern corner at Long Lake to Lake Placid. The range trail, which traverses a series of mountain summits known as the Great Range from Mount Marcy to Keene Valley, is considered by many to be the most scenic and rugged trail in the state.

Geographic entities mentioned:
surface_form: Mount Marcy
instance_of: Mountain
countries: United States
coordinates: lat: 44.112733333333
lon: -73.923727777778
Wanika Falls, Indian Falls, Indian Pass, the Duck Hole, Avalanche Pass, and Panther Gorge, are also popular hiking destinations. Climbing. The area contains many cliffs that are popular for rock climbing, including Cascade Lakes, Wallface Mountain, and Avalanche Pass. In the winter, Avalanche Pass and the trap dike on Mount Colden are popular destinations. Skiing.

Geographic entities mentioned:
surface_form: Wallface Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.138
lon: -74.0368
Lists of wards, 1999 to 2007. Wards are listed by management area to which linked for area committee purposes. Inverness wards. The management area included Loch Ness, Strathglass and the former royal burgh of Inverness. Inverness was granted city status in 2001 and the Highland Council then used the 'city' title in reference to the Inverness management area.

Geographic entities mentioned:
surface_form: Loch Ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
The Coast Mountains are approximately long and average in width. The range's southern and southeastern boundaries are surrounded by the Fraser River and the Interior Plateau while its far northwestern edge is delimited by the Kelsall and Tatshenshini Rivers at the north end of the Alaska Panhandle, beyond which are the Saint Elias Mountains, and by Champagne Pass in the Yukon Territory.

Geographic entities mentioned:
surface_form: Interior Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 52
lon: -123
Covered in dense temperate rainforest on its western exposures, the range rises to heavily glaciated peaks, including the largest temperate-latitude ice fields in the world. On its eastern flanks, the range tapers to the dry Interior Plateau and the subarctic boreal forests of the Skeena Mountains and Stikine Plateau.

Geographic entities mentioned:
surface_form: Stikine Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
The Coast Mountains are part of the Pacific Ring of Firethe ring of volcanoes and associated mountains around the Pacific Oceanand contain some of British Columbia's highest mountains. Mount Waddington is the highest mountain of the Coast Mountains and the highest that lies entirely within British Columbia, located northeast of the head of Knight Inlet with an elevation of. Geography.

Geographic entities mentioned:
surface_form: Mount Waddington
instance_of: Mountain
countries: Canada
coordinates: lat: 51.373611111111
lon: -125.26333333333
Other than logging and a large ski resort at the resort town of Whistler, most of the land in the range is completely undeveloped. Mount Waddington, the highest mountain of the Coast Mountains, lies in the Waddington Range of the Pacific Ranges. Just north of the Pacific Ranges lies the central subdivision known as the Kitimat Ranges.

Geographic entities mentioned:
surface_form: Mount Waddington
instance_of: Mountain
countries: Canada
coordinates: lat: 51.373611111111
lon: -125.26333333333
The Boundary Ranges include several large icefields, including the Juneau Icefield between Juneau, Alaska and Atlin Lake in British Columbia, and the Stikine Icecap, which lies between the lower Stikine River and the Whiting River.

Geographic entities mentioned:
surface_form: Atlin Lake
instance_of: Lake
countries: Canada
coordinates: lat: 60.0133333
lon: -133.8308333
This precipitation is among the heaviest in North America. The eastern slopes are relatively dry and less steep and protect the British Columbia Interior from the Pacific weather systems, resulting in dry warm summers and dry cold winters. Beyond the eastern slopes is a plateau occupying the southern and central portions of British Columbia called the Interior Plateau.

Geographic entities mentioned:
surface_form: Interior Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 52
lon: -123
In addition, oceanic crust under the Pacific Ocean is being subducted at the southern portion of the range to form a north–south line of volcanoes called the Garibaldi Volcanic Belt, a northern extension of the Cascade Volcanoes in the northwestern United States, and contains the most explosive young volcanoes in Canada.

Geographic entities mentioned:
surface_form: Garibaldi Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5283
lon: -126.113
Further north the northwesterly structural trend of the Coast Mountains lies partly in a large continental rift responsible for the creation of several volcanoes. These volcanoes form part of the Northern Cordilleran Volcanic Province, the most volcanically active area in Canada. Insular and Omineca Arc eruptive periods.

Geographic entities mentioned:
surface_form: Northern Cordilleran Volcanic Province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
Mount Barrington. Mount Barrington, a mountain that is part of the Mount Royal Range, is located on the Barrington Tops plateau in the Mid-Coast Council within New South Wales, Australia and has an elevation of above sea level. Now the remnants of a volcano, Mount Barrington, formerly the Barrington Volcano, erupted near its present peak between 44 and 54 million years ago.

Geographic entities mentioned:
surface_form: Barrington Tops
instance_of: Landform
countries: Australia
coordinates: lat: -31.94998
lon: 151.52687
surface_form: mount royal
instance_of: Mountain
countries: Australia
coordinates: lat: -32.1742
lon: 151.326
surface_form: mount barrington
instance_of: Mountain
countries: Australia
coordinates: lat: -32.0402
lon: 151.404
The lava was up to thick. The extensive rainforests in the area grow on much of the resultant red/brown soils. Gemstones such as zircon, sapphire, sapphirine and ruby were formed from the volcano. Nearby Careys Peak is considered a vent in this extinct shield volcano. The surrounding area is covered by sub alpine Snow Gum woodland, with rainforest on the escarpment edge and in fire free gullies.

Geographic entities mentioned:
surface_form: Careys Peak
instance_of: Mountain
countries: Australia
coordinates: lat: -32.0507
lon: 151.459
Mount Barrington. Mount Barrington, a mountain that is part of the Mount Royal Range, is located on the Barrington Tops plateau in the Mid-Coast Council within New South Wales, Australia and has an elevation of above sea level. Now the remnants of a volcano, Mount Barrington, formerly the Barrington Volcano, erupted near its present peak between 44 and 54 million years ago.

Geographic entities mentioned:
surface_form: barrington volcano
instance_of: Mountain
countries: Australia
coordinates: lat: -32.0402
lon: 151.404
surface_form: mount barrington
instance_of: Mountain
countries: Australia
coordinates: lat: -32.0402
lon: 151.404
Mount Barrington. Mount Barrington, a mountain that is part of the Mount Royal Range, is located on the Barrington Tops plateau in the Mid-Coast Council within New South Wales, Australia and has an elevation of above sea level. Now the remnants of a volcano, Mount Barrington, formerly the Barrington Volcano, erupted near its present peak between 44 and 54 million years ago.

Geographic entities mentioned:
surface_form: mount barrington
instance_of: Mountain
countries: Australia
coordinates: lat: -32.0402
lon: 151.404
Now the remnants of a volcano, Mount Barrington, formerly the Barrington Volcano, erupted near its present peak between 44 and 54 million years ago. The eruption caused a basalt flow, which covered much of the Barrington Tops plateau. The lava was up to thick. The extensive rainforests in the area grow on much of the resultant red/brown soils.

Geographic entities mentioned:
surface_form: barrington tops
instance_of: Landform
countries: Australia
coordinates: lat: -31.94998
lon: 151.52687
It is part of the Ryfylke prosti (deanery) in the Diocese of Stavanger. History. The area that is now Suldal municipality has a long history of trade connections to the nearby valley regions to the north and east. The main mountain plateau trade route led east from Suldal municipality over the plateau to the nearby Setesdal valley in Bykle municipality in Agder county.

Geographic entities mentioned:
surface_form: Setesdal
instance_of: Valley
countries: Norway
coordinates: lat: 58.92025
lon: 7.7206388888889
To the north, Suldal is bordered by Sauda and Ullensvang municipalities, in the east by Vinje and Bykle, in the south by Hjelmeland, and in the west by Vindafjord. Across the Jelsafjorden and Vindafjorden lie the municipalities of Stavanger and Tysvær. The mountain Kistenuten is located at the triple border point of Rogaland, Vestland and Telemark.

Geographic entities mentioned:
surface_form: Kistenuten
instance_of: Mountain
countries: Norway
coordinates: lat: 59.782778
lon: 7.096389
The mountain Kistenuten is located at the triple border point of Rogaland, Vestland and Telemark. Other mountains in Suldal are Vassdalseggi, the highest mountain in Rogaland, Trollaskeinuten, Snønuten, Mælen, Knoda, Fitjanuten, Leirnuten, Kaldafjellet, Simlenuten, Steinkilenuten, and Raudberga, all reaching above m.a.s.l.

Geographic entities mentioned:
surface_form: Vassdalseggi
instance_of: Mountain
countries: Norway
coordinates: lat: 59.763322
lon: 7.110413
surface_form: Trollaskeinuten
instance_of: Mountain
countries: Norway
coordinates: lat: 59.7319
lon: 6.99722
surface_form: Snønuten
instance_of: Mountain
countries: Norway
coordinates: lat: 59.519166666667
lon: 6.8647222222222
surface_form: Knoda
instance_of: Mountain
countries: Norway
coordinates: lat: 59.7711
lon: 6.97722
surface_form: Fitjanuten
instance_of: Mountain
countries: Norway
coordinates: lat: 59.71388889
lon: 7.11638889
surface_form: Leirnuten
instance_of: Mountain
countries: Norway
coordinates: lat: 59.4956
lon: 6.91694
surface_form: Kaldafjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 59.523333333333
lon: 6.9802777777778
surface_form: Simlenuten
instance_of: Mountain
countries: Norway
coordinates: lat: 59.7131
lon: 7.0639
surface_form: Steinkilenuten
instance_of: Mountain
countries: Norway
coordinates: lat: 59.5067
lon: 6.94639
surface_form: Raudberga
instance_of: Mountain
countries: Norway
coordinates: lat: 59.73375
lon: 7.06297
Other mountains in Suldal are Vassdalseggi, the highest mountain in Rogaland, Trollaskeinuten, Snønuten, Mælen, Knoda, Fitjanuten, Leirnuten, Kaldafjellet, Simlenuten, Steinkilenuten, and Raudberga, all reaching above m.a.s.l. The Sandsfjorden and Hylsfjorden lie within Suldal, as does lake Suldalsvatnet. The Saudafjorden lies partially within the boundary of Suldal.

Geographic entities mentioned:
surface_form: Suldalsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 59.495833333333
lon: 6.5377777777778
The Sandsfjorden and Hylsfjorden lie within Suldal, as does lake Suldalsvatnet. The Saudafjorden lies partially within the boundary of Suldal. The Erfjorden and the lakes Blåsjø, Holmavatnet, and Holmevatnet also lie on the boundary of Suldal. Economy. The Ulla-Førre project of building huge hydroelectric dams in the mountains was initiated in the 1960s.

Geographic entities mentioned:
surface_form: Holmevatnet
instance_of: Lake
countries: Norway
coordinates: lat: 59.492222222222
lon: 7.0063888888889