Sarmila/GeoWiki-Features huggingface dataset:
Bull Lake (New Brunswick). Bull Lake is a lake in York County, New Brunswick. Description. The lake is marshy and is reputed to have a quicksand bottom.

Geographic entities mentioned:
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.6872
lon: -76.9758
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.5275
lon: -93.9981
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.3544
lon: -91.5747
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.105
lon: -67.383
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.55209
lon: -83.13404
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.4328
lon: -82.19
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.9103
lon: -87.3933
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.1031
lon: -80.5825
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.8981
lon: -80.5561
It separates Capitán Aracena Island from the westernmost portion of Isla Grande de Tierra del Fuego, and crosses Alberto de Agostini National Park. It is flanked by mountains, the chief of which is Monte Sarmiento. Like the Abra Channel and the Bárbara Channel farther west, it joins the western part of the Strait of Magellan directly to the Pacific Ocean.

Geographic entities mentioned:
surface_form: Monte Sarmiento
instance_of: Mountain
countries: Chile
coordinates: lat: -54.45
lon: -70.833333333333
The surrounding Guild Park and Gardens is notable for a sculpture garden consisting of the rescued facades and ruins of various demolished downtown Toronto buildings such as bank buildings, the old &quot;Toronto Star&quot; building and the Granite Club. The park is situated on the Scarborough Bluffs with views of Lake Ontario.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
The second (1862-1888) was Karl Fedorovich Kessler (1815–1881). The early marine collections are primarily from the Mediterranean due to associations with Stazione Zoologica in Naples and Villefranche Zoological Station in France. Later material is from the White Sea, Barents Sea, the Baltic Sea, the Caspian Sea, Black Sea and Red Sea as well as the oceans.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
The choice was based on the military and economic advantages given by the natural barrier represented by the Retezat Mountains in the south and Poiana Ruscă Mountains in the north. The territory of the metropolis extended from Tibiscum to Micia and to the Jiu valley, the city being protected by several &quot;castra&quot;: Tibiscum, Pons Augusti, Micia and those of Bumbești.

Geographic entities mentioned:
surface_form: Jiu valley
instance_of: Valley
countries: Romania
coordinates: lat: 43.77805556
lon: 23.81333333
Moore Creek is a short creek in the St. Lawrence River drainage basin in Temiskaming Shores, Timiskaming District, Ontario, Canada, between the communities of New Liskeard and Haileybury. Hydrology. Moore Creek travels from its source east to its mouth at Wabi Bay on Lake Timiskaming, at an elevation of, which flows via the Ottawa River into the St. Lawrence River.

Geographic entities mentioned:
surface_form: Lake Timiskaming
instance_of: Lake
countries: Canada
coordinates: lat: 47.333333333333
lon: -79.5
surface_form: moore creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.4689
lon: -79.6478
Moore Creek (Timiskaming District). Moore Creek is a short creek in the St. Lawrence River drainage basin in Temiskaming Shores, Timiskaming District, Ontario, Canada, between the communities of New Liskeard and Haileybury. Hydrology. Moore Creek travels from its source east to its mouth at Wabi Bay on Lake Timiskaming, at an elevation of, which flows via the Ottawa River into the St.

Geographic entities mentioned:
surface_form: moore creek (timiskaming district)
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.4689
lon: -79.6478
Moore Creek (Timiskaming District). Moore Creek is a short creek in the St. Lawrence River drainage basin in Temiskaming Shores, Timiskaming District, Ontario, Canada, between the communities of New Liskeard and Haileybury. Hydrology. Moore Creek travels from its source east to its mouth at Wabi Bay on Lake Timiskaming, at an elevation of, which flows via the Ottawa River into the St.

Geographic entities mentioned:
surface_form: moore creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.4689
lon: -79.6478
On the northern end of the loch, there is several small hills, that make a shallow cliff which follows the curve of the loch. Overlooking the southwest end of the loch, is Creag Rainich at 807metres and Meall Dubh at 748metres comprising two hills.

Geographic entities mentioned:
surface_form: Creag Rainich
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.725176
lon: -5.1989865
surface_form: Meall Dubh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.127504
lon: -4.9009686
Further east again, is Sgurr Breac, which forms the peak of the second fold, which creates the corrie, that is intersected by a long shallow valley that descends from 600metres down to the north-east end of the loch. On the northern end of the loch, there is several small hills, that make a shallow cliff which follows the curve of the loch.

Geographic entities mentioned:
surface_form: sgurr breac
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.692067
lon: -5.091724
surface_form: the peak
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -7.95
lon: -14.35
Loch a' Bhraoin. Loch a' Bhraoin, Loch Broom (), is a freshwater loch, located in Wester Ross, in Ross-shire, on the west coast of Scotland. Settlements. Due to the remoteness of the loch, there are very few settlements in the area. The main A832 road that is part of the Wester Ross Coastal Trail, leaves the main A835 road, at the Falls of Measach and passes the eastern end of the loch. Walking.

Geographic entities mentioned:
surface_form: loch broom
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.7
lon: -3.6166666666667
surface_form: loch a' bhraoin
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.71818
lon: -5.13748
Geography. Loch a' Bhraoin lies about 7 miles to the south of the head of Loch Broom, and is surrounded by high hills. At the west end of the loch, about 2 miles from the end of the loch is the plateau of a' Chailleach that rises to 998.52metres above sea level. The loch is orientated on a northeast to southwest direction and is over 4 km in length.

Geographic entities mentioned:
surface_form: loch broom
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.7
lon: -3.6166666666667
surface_form: loch a' bhraoin
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.71818
lon: -5.13748
The main route is from the A832 road, taking the path east to west along Destitution Road to Loch a’ Bhraoin from the East. Also travelling from Poolewe past the Fionn Loch in the NW, which is the longest route. Travelling from Incheril over the Heights of Kinlochewe and the Kinlochewe Forest in the SW, and from Corrie Hallie that directly north of the loch. Geography.

Geographic entities mentioned:
surface_form: fionn loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.1068
lon: -5.1747
surface_form: fionn loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.75602
lon: -5.453
Geography. Loch a' Bhraoin lies about 7 miles to the south of the head of Loch Broom, and is surrounded by high hills. At the west end of the loch, about 2 miles from the end of the loch is the plateau of a' Chailleach that rises to 998.52metres above sea level. The loch is orientated on a northeast to southwest direction and is over 4 km in length.

Geographic entities mentioned:
surface_form: a' chailleach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.6938
lon: -5.128715
surface_form: a' chailleach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.109564
lon: -4.179285
The loch is orientated on a northeast to southwest direction and is over 4 km in length. The maximum breadth of the loch is nearly 800metres wide. On a north by northeast direction from a' Chailleach, the mountains have been folded extensively. Two corries overlook Loch a' Bhraoin to the north.

Geographic entities mentioned:
surface_form: a' chailleach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.6938
lon: -5.128715
surface_form: a' chailleach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.109564
lon: -4.179285
Loch a' Bhraoin. Loch a' Bhraoin, Loch Broom (), is a freshwater loch, located in Wester Ross, in Ross-shire, on the west coast of Scotland. Settlements. Due to the remoteness of the loch, there are very few settlements in the area. The main A832 road that is part of the Wester Ross Coastal Trail, leaves the main A835 road, at the Falls of Measach and passes the eastern end of the loch. Walking.

Geographic entities mentioned:
surface_form: loch a' bhraoin
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.71818
lon: -5.13748
Due to the remoteness of the loch, there are very few settlements in the area. The main A832 road that is part of the Wester Ross Coastal Trail, leaves the main A835 road, at the Falls of Measach and passes the eastern end of the loch. Walking. Loch a' Bhraoin is considered an excellent location for walkers. There are essentially four routes into the mountains surrounding Loch a' Bhraoin.

Geographic entities mentioned:
surface_form: loch a' bhraoin
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.71818
lon: -5.13748
Walking. Loch a' Bhraoin is considered an excellent location for walkers. There are essentially four routes into the mountains surrounding Loch a' Bhraoin. The main route is from the A832 road, taking the path east to west along Destitution Road to Loch a’ Bhraoin from the East. Also travelling from Poolewe past the Fionn Loch in the NW, which is the longest route.

Geographic entities mentioned:
surface_form: loch a' bhraoin
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.71818
lon: -5.13748
On a north by northeast direction from a' Chailleach, the mountains have been folded extensively. Two corries overlook Loch a' Bhraoin to the north. The first of these is formed by the mountain Toman Còinnich at 935metres, which forms the corrie that contains Loch Toll an Lochain, where the direction of the corrie faces the northern end of the loch, similar to a giants seat.

Geographic entities mentioned:
surface_form: loch a' bhraoin
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.71818
lon: -5.13748
Tordsvatnet. Tordsvatnet is a lake in Skjåk Municipality in Innlandet county, Norway. The lake lies within the Tafjordfjella mountain range inside the Reinheimen National Park. The mountain lake lies about northwest of the village of Bismo. The lake lies in a low area surrounded by the mountains Benkehøa (to the east), Karitinden (to the northwest), and Vetldalseggi (to the west).

Geographic entities mentioned:
surface_form: Benkehøa
instance_of: Mountain
countries: Norway
coordinates: lat: 62.17138889
lon: 7.86277778
surface_form: Karitinden
instance_of: Mountain
countries: Norway
coordinates: lat: 62.185833333333
lon: 7.7322222222222
surface_form: vetldalseggi
instance_of: Mountain
countries: Norway
coordinates: lat: 62.1486
lon: 7.78306
Tordsvatnet. Tordsvatnet is a lake in Skjåk Municipality in Innlandet county, Norway. The lake lies within the Tafjordfjella mountain range inside the Reinheimen National Park. The mountain lake lies about northwest of the village of Bismo. The lake lies in a low area surrounded by the mountains Benkehøa (to the east), Karitinden (to the northwest), and Vetldalseggi (to the west).

Geographic entities mentioned:
surface_form: tordsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 62.148888888889
lon: 7.8230555555556
The southwest flank of Mount Oldeani, one of the Ngorongoro volcanos, drains directly into the northeast end of the lake. Flow from the Budahaya / Udahaya River, which drains into the Yaeda Swamp to the southeast of the lake, was once second, but has decreased due to water diversion in the Mbulu Highlands. Water flow from the Serengeti is minor; the largest stream is the Sayu.

Geographic entities mentioned:
surface_form: Mbulu Highlands
instance_of: Plateau
countries: Tanzania
coordinates: lat: -3.8556
lon: 35.5444
surface_form: mbulu highlands
instance_of: Plateau
countries: Tanzania
coordinates: lat: -3.8556
lon: 35.5444
Even during wet periods, lake depths typically remain less than one metre. The Hadza are the indigenous inhabitants of the lake. They are found along most of the perimeter, though camps are few along most of the Serengeti, which is Maasai territory. The Datooga inhabit the Yaeda Valley to the southeast, the Isanzu the south, and the Sukuma across the Sibiti River in the southwest.

Geographic entities mentioned:
surface_form: Yaeda Valley
instance_of: Valley
countries: Tanzania
coordinates: lat: -4.0003083333333
lon: 34.999916666667
Lake Eyasi. Lake Eyasi (; formerly, &quot;Njarasa Lake&quot;, and &quot;Hohenlohesee&quot;, &quot;Hohenlohe Lake&quot;) is a lake located in Karatu District of Arusha Region in north Tanzania. Lake Eyasi is the largest body of water in Arusha region.

Geographic entities mentioned:
surface_form: lake eyasi
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.66667
lon: 35.08333
surface_form: eyasi
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.66667
lon: 35.08333
Lake Eyasi. Lake Eyasi (; formerly, &quot;Njarasa Lake&quot;, and &quot;Hohenlohesee&quot;, &quot;Hohenlohe Lake&quot;) is a lake located in Karatu District of Arusha Region in north Tanzania. Lake Eyasi is the largest body of water in Arusha region.

Geographic entities mentioned:
surface_form: lake eyasi
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.66667
lon: 35.08333
surface_form: lake eyasi
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.66667
lon: 35.08333
surface_form: eyasi
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.66667
lon: 35.08333
surface_form: eyasi
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.66667
lon: 35.08333
The Iraqw traditionally lived on the other side of Yaeda, but have come in increasing numbers to the Baray, which is now the primary onion-growing region of East Africa. Mumba Cave is an archaeological site that is located by the shores of Lake Eyasi. The site has yielded a number of Middle Stone Age and Late Stone Age artifacts.

Geographic entities mentioned:
surface_form: lake eyasi
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.66667
lon: 35.08333
surface_form: eyasi
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.66667
lon: 35.08333
It is a seasonal shallow endorheic salt lake on the floor of the Great Rift Valley at the base of the Serengeti Plateau, just south of the Serengeti National Park and immediately southwest of the Ngorongoro Crater in the Crater Highlands of Tanzania. The lake is elongated, orientated southwest to northeast, and lies in the Eyasi-Wembere branch of the Great Rift Valley.

Geographic entities mentioned:
surface_form: eyasi
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.66667
lon: 35.08333
Cannon Lake is a lake located in Rice County, Minnesota, United States. The lake has a surface area of 1,593.22 acres and a maximum depth of 15 feet. The lake is part of the Cannon River system that starts in Shields Lake, goes through Le Sueur and Rice counties and drains into the Mississippi River. A survey of the lake in August 2009 showed the most predominant species of fish was the walleye.

Geographic entities mentioned:
surface_form: Shields Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.37
lon: -93.44138889
Cannon Lake (Rice County, Minnesota). Cannon Lake is a lake located in Rice County, Minnesota, United States. The lake has a surface area of 1,593.22 acres and a maximum depth of 15 feet. The lake is part of the Cannon River system that starts in Shields Lake, goes through Le Sueur and Rice counties and drains into the Mississippi River.

Geographic entities mentioned:
surface_form: cannon lake (rice county, minnesota)
instance_of: Lake
countries: United States
coordinates: lat: 44.267
lon: -93.3553
Cannon Lake (Rice County, Minnesota). Cannon Lake is a lake located in Rice County, Minnesota, United States. The lake has a surface area of 1,593.22 acres and a maximum depth of 15 feet. The lake is part of the Cannon River system that starts in Shields Lake, goes through Le Sueur and Rice counties and drains into the Mississippi River.

Geographic entities mentioned:
surface_form: cannon lake
instance_of: Lake
countries: United States
coordinates: lat: 44.267
lon: -93.3553
The language spoken by the Suba of Tanzania is very close to the Kisuba language spoken by the Suna Girango(Abagirango) people of Migori County of Kenya and Kuria language spoken by the Kuria people. The language spoken by the Suba of Tanzania is distinct from the Olosuba language spoken by the Suba people of Homa Bay County of Kenya and some islands of Lake Victoria.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Chabinoche River. The Chabinoche River is a tributary of Evans Lake, in Eeyou Istchee Baie-James (municipality), in the administrative region of Nord-du-Québec, in the Canadian province of Quebec, in Canada. The northern part of this hydrographic slope is served by a forest road from the south.

Geographic entities mentioned:
surface_form: evans lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.8167
lon: -123.167
surface_form: chabinoche river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.693888888889
lon: -77.155555555556
Chabinoche River. The Chabinoche River is a tributary of Evans Lake, in Eeyou Istchee Baie-James (municipality), in the administrative region of Nord-du-Québec, in the Canadian province of Quebec, in Canada. The northern part of this hydrographic slope is served by a forest road from the south.

Geographic entities mentioned:
surface_form: chabinoche river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.693888888889
lon: -77.155555555556
The surface of the river is usually frozen from early November to mid-May, however, safe ice circulation is generally from mid-November to mid-April. Toponymy. The toponym &quot;Chabinoche River&quot; was formalized on December 5, 1968, at the Commission de toponymie du Quebec, i.e. at the creation of this commission

Geographic entities mentioned:
surface_form: chabinoche river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.693888888889
lon: -77.155555555556
Of the unproductive areas, 1.43% is unproductive standing water (ponds or lakes), 0.12% is unproductive flowing water (rivers) and 0.3% is other unproductive land. The municipality is located on the eastern edge of the &quot;Rottal&quot;. It consists of the village of Buttisholz and the hamlets of Luternau, Soppensee and St. Ottilien. Demographics.

Geographic entities mentioned:
surface_form: Soppensee
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.090277777778
lon: 8.0808333333333
It is currently operated with 13173/13174 train numbers on a four-days-a-week basis. It is named after the Kangchenjunga peak of the Himalayan Mountains of Sikkim which is visible from New Jalpaiguri, as previously when this train was introduced in the 1960s it was between and New Jalpaiguri (Siliguri). Accident.

Geographic entities mentioned:
surface_form: Kangchenjunga
instance_of: Mountain
countries: India
Nepal
coordinates: lat: 27.7
lon: 88.133333
Many of his depictions were of ruins of Christian churches in the Caucasus. He also painted &quot;Défilé du Darial&quot; (Darial Gorge), &quot;The Convent at Kutaisi&quot; (Gelati Monastery), and &quot;Mount Arafat&quot;.

Geographic entities mentioned:
surface_form: Mount Arafat
instance_of: Mountain
countries: Saudi Arabia
coordinates: lat: 21.354831
lon: 39.983886
Rock climbing is discouraged because the wilderness's sandstone cliffs are friable and crumbly. The wilderness also includes a waterfall, Rock River Falls, and a shallow lake, Ginpole Lake. Both waterways, the waterfall, and the lake are all part of the Lake Superior drainage basin. Large fauna within the Rock River Canyon Wilderness includes the black bear and the whitetail deer.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Campbell Peak. Campbell Peak () is a peak, high, standing northeast of Mawson Peak, the summit of Heard Island. It was surveyed in 1948 by the Australian National Antarctic Research Expeditions (ANARE), who named it for Group-Captain Stuart Campbell, Royal Australian Air Force.

Geographic entities mentioned:
surface_form: Mawson Peak
instance_of: Mountain
countries: Australia
coordinates: lat: -53.104166666667
lon: 73.516944444444
surface_form: campbell peak
instance_of: Mountain
countries: Australia
coordinates: lat: -53.1
lon: 73.5333
Campbell Peak. Campbell Peak () is a peak, high, standing northeast of Mawson Peak, the summit of Heard Island. It was surveyed in 1948 by the Australian National Antarctic Research Expeditions (ANARE), who named it for Group-Captain Stuart Campbell, Royal Australian Air Force.

Geographic entities mentioned:
surface_form: campbell peak
instance_of: Mountain
countries: Australia
coordinates: lat: -53.1
lon: 73.5333
Distribution and habitat. White-topped box grows in the slopes and edges on the eastern side of the Northern and Central Tablelands in New South Wales, between Dorrigo and Scone in the north to Bundanoon and Milton in the south. There is also a disjunct population near Cunninghams Gap in south-eastern Queensland.

Geographic entities mentioned:
surface_form: Northern
instance_of: Plateau
countries: Australia
coordinates: lat: -30.595277777777778
lon: 151.5
Bhim Tal. Bhim Tal is situated at a distance of 5 km from Naukuchia Tal at an altitude of 1,375 m above sea level. The main attraction in Bhimtal is the Bhimtal Lake which has a small island at its centre. Bhimtal is an ancient place named after the legendary Bhima of Mahabharata when Bhima visited during the exile period of Pandavas. Haldwani.

Geographic entities mentioned:
surface_form: bhimtal lake
instance_of: Lake
countries: India
coordinates: lat: 29.343055555556
lon: 79.559166666667
Naukuchiatal. Naukuchiatal or &quot;lake of nine corners&quot; is a small hill station and lake near Nainital Town in Nainital district of Kumaon, Uttarakhand, India. Its chairman is Devendra Singh Chanotiya. The lake is 175 feet deep and is situated at above sea level. It is the deepest lake in the Nainital region. The length of the lake is, its breadth is and it has a depth of.

Geographic entities mentioned:
surface_form: naukuchiatal
instance_of: Lake
countries: India
coordinates: lat: 29.322222222222223
lon: 79.58555555555556
According to locals anyone performing a parikarma of the lake will be blessed by Brahmaji. Climate. The temperatures in summer range from 11 C to 26 C and in winter from -2 C to 14 C. Hanuman Temple. Hanuman Temple is situated on the main road to Naukuchiatal. It has a 52 foot tall statue of Lord Hanuman. The Temple has an artificial cave design on the lines of the famous Vaishno Devi Shrine.

Geographic entities mentioned:
surface_form: naukuchiatal
instance_of: Lake
countries: India
coordinates: lat: 29.322222222222223
lon: 79.58555555555556
The temple also houses Vaishno Devi temple, Shani Mandir, and Ram Darbar temples and a reflection and place to sit back and rest for the visitors. Mukteshwar. Mukteshwar is a temple situated at a distance of 38 km from Naukuchiatal set at an elevation of 2,285 m above sea level. Mukteshwar is named after a 350-year-old temple called Mukteshwer Dham whose presiding deity is great Lord Shiva.

Geographic entities mentioned:
surface_form: naukuchiatal
instance_of: Lake
countries: India
coordinates: lat: 29.322222222222223
lon: 79.58555555555556
It is surrounded by Pithorgarh to the east, Garhwal to the west, Bageshwar to the north and Nainital to the south. The landscape of Almora attracts hundreds of tourists each year. It is situated 72 km from Naukuchiatal. Ranikhet. Ranikhet is situated 7 3 km from Naukuchiatal at an altitude of 1,869 m above sea level.

Geographic entities mentioned:
surface_form: naukuchiatal
instance_of: Lake
countries: India
coordinates: lat: 29.322222222222223
lon: 79.58555555555556
The landscape of Almora attracts hundreds of tourists each year. It is situated 72 km from Naukuchiatal. Ranikhet. Ranikhet is situated 7 3 km from Naukuchiatal at an altitude of 1,869 m above sea level. Ranikhet is a hill station in Almora District of Uttarakhand state and is maintained by Ranikhet Cantonment Board. Ranikhet is also the home for the Kumaon and Naga regiments of the Indian Army.

Geographic entities mentioned:
surface_form: naukuchiatal
instance_of: Lake
countries: India
coordinates: lat: 29.322222222222223
lon: 79.58555555555556
Mukteshwar was developed by the British as a research and education institute by setting up Indian Veterinary Research Institute (IVRI) in 1893. Sat Tal ('Seven Lakes'). Sat Tal is a cluster of mysteriously interconnected seven freshwater lakes (Purna Tal, Ram Tal, Sita tal, Laxman Tal, Nal Damyanti Tal, Sukh Tal and Garud Tal) situated 19 km away from Naukuchia Tal.

Geographic entities mentioned:
surface_form: sat tal
instance_of: Lake
countries: India
coordinates: lat: 29.348055555555554
lon: 79.53194444444445
Sat Tal ('Seven Lakes'). Sat Tal is a cluster of mysteriously interconnected seven freshwater lakes (Purna Tal, Ram Tal, Sita tal, Laxman Tal, Nal Damyanti Tal, Sukh Tal and Garud Tal) situated 19 km away from Naukuchia Tal. Sat Tal is set at an altitude of 1,370 m above sea level. The group of lakes is set amidst dense forests of oak and pine trees.

Geographic entities mentioned:
surface_form: sat tal
instance_of: Lake
countries: India
coordinates: lat: 29.348055555555554
lon: 79.53194444444445
The Kettleman Hills is named, and misspelled, after Dave Kettelman, a pioneer sheep and cattle rancher who grazed his animals there in the 1860s. The hills, which rise to an elevation of approximately, divide the San Joaquin Valley on the east from the much smaller Kettleman Plain to the west. They are discontinuous, as indicated by their name (&quot;hills&quot; rather than &quot;ridge&quot;).

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Geography. The region takes its name from the Sambirano River, which runs through the center of the region. The
Sambirano region extends from the Ifasy River in the north to the Ampasindava Peninsula in the south, in the southwestern portion of Diana Region. It extends from the coast to the slopes of the Tsaratanana Massif, which bounds the region on the east.

Geographic entities mentioned:
surface_form: Sambirano River
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -13.61722222
lon: 48.33361111
Stasiūnai, Kėdainiai. Stasiūnai is a village in Kėdainiai district municipality, in Kaunas County, in central Lithuania. It is located by the Smilgaitis river and Keleriškiai pond, nearby Josvainiai forest. According to the 2011 census, the village has a population of 19 people. There is a &quot;Ąžuolotas&quot; forestry in the village.

Geographic entities mentioned:
surface_form: Smilgaitis
instance_of: Watercourse
countries: Lithuania
coordinates: lat: 55.29171
lon: 23.894404
Charpeney Lake. Charpeney Lake is the main body of fresh water at the head of the Saint-Jean North-East River (slope of the Saint-Jean River), flowing in the unorganized territory of Lac-Jérôme, in the Minganie Regional County Municipality, in the administrative region of Côte-Nord, in the province of Quebec, in Canada. Geography.

Geographic entities mentioned:
surface_form: Saint-Jean North-East River
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.68344
lon: -64.04863
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: charpeney lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.06562
lon: -63.86179
surface_form: east river
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.5529
lon: -62.3032
Lake Charpeney flows into its northeastern part. From the mouth of Charpeney Lake, the current descends the course of the Saint-Jean North-East River over, then the course of the Saint-Jean River (Minganie) on, which empties on the north shore of Gulf of St. Lawrence. Toponymy. The term &quot;Charpeney&quot; and its variant &quot;Charpenay&quot; turn out to be a French family name.

Geographic entities mentioned:
surface_form: Saint-Jean North-East River
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.68344
lon: -64.04863
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: charpeney lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.06562
lon: -63.86179
surface_form: east river
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.5529
lon: -62.3032
Charpeney Lake. Charpeney Lake is the main body of fresh water at the head of the Saint-Jean North-East River (slope of the Saint-Jean River), flowing in the unorganized territory of Lac-Jérôme, in the Minganie Regional County Municipality, in the administrative region of Côte-Nord, in the province of Quebec, in Canada. Geography.

Geographic entities mentioned:
surface_form: charpeney lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.06562
lon: -63.86179
Lake Solai. Lake Solai is a saltwater lake in the Rift Valley Province of Kenya. It is located near the town of Solai, at an elevation of. Geological conditions at the lake during the Little Ice Age have been the object of a scientific study. In 2014 there was a major contamination event at the lake.

Geographic entities mentioned:
surface_form: lake solai
instance_of: Lake
countries: Kenya
coordinates: lat: 0.06
lon: 36.15
Lake Solai. Lake Solai is a saltwater lake in the Rift Valley Province of Kenya. It is located near the town of Solai, at an elevation of. Geological conditions at the lake during the Little Ice Age have been the object of a scientific study. In 2014 there was a major contamination event at the lake.

Geographic entities mentioned:
surface_form: lake solai
instance_of: Lake
countries: Kenya
coordinates: lat: 0.06
lon: 36.15
surface_form: kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
Cangyanshan. Cangyanshan (), named after Mount Cangyan which rises to its south, is a town of Jingxing County in the Taihang Mountains of southwestern Hebei province, China, located south of the county seat., it has 19 villages under its administration.

Geographic entities mentioned:
surface_form: Mount Cangyan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 37.829427777778
lon: 114.13655555556
Quetrupillán. Quetrupillán (&quot;blunted&quot;, &quot;mutilated&quot;; also known as Ketropillán; the name is sometimes applied to the neighbouring Lanín volcano.) is a stratovolcano located in Los Ríos Region of Chile. It is situated between Villarrica and Lanín volcanoes, within Villarrica National Park.

Geographic entities mentioned:
surface_form: Lanín
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -39.632777777778
lon: -71.499722222222
surface_form: quetrupillán
instance_of: Mountain
countries: Chile
coordinates: lat: -39.5
lon: -71.7
Quetrupillán. Quetrupillán (&quot;blunted&quot;, &quot;mutilated&quot;; also known as Ketropillán; the name is sometimes applied to the neighbouring Lanín volcano.) is a stratovolcano located in Los Ríos Region of Chile. It is situated between Villarrica and Lanín volcanoes, within Villarrica National Park.

Geographic entities mentioned:
surface_form: Lanín
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -39.632777777778
lon: -71.499722222222
surface_form: villarrica
instance_of: Mountain
countries: Chile
coordinates: lat: -39.42
lon: -71.939166666667
surface_form: villarrica
instance_of: Mountain
countries: Chile
coordinates: lat: -39.42
lon: -71.939166666667
surface_form: villarrica
instance_of: Lake
countries: Chile
coordinates: lat: -39.25
lon: -72.083333333333
surface_form: villarrica
instance_of: Lake
countries: Chile
coordinates: lat: -39.25
lon: -72.083333333333
Quetrupillán lies on the border between Los Ríos Region and Araucanía Region, in the Southern Volcanic Zone. Together with Villarrica and Lanín it forms a northwest-southeast alignment of volcanoes, which coincides with the Mocha-Villarrica transcurrent fault.

Geographic entities mentioned:
surface_form: Lanín
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -39.632777777778
lon: -71.499722222222
surface_form: villarrica
instance_of: Mountain
countries: Chile
coordinates: lat: -39.42
lon: -71.939166666667
surface_form: villarrica
instance_of: Lake
countries: Chile
coordinates: lat: -39.25
lon: -72.083333333333
The Cordillera El Mocho and Quinquilil volcanoes are likewise situated on this alignment, both are deeply eroded composite volcanoes of small dimensions. Other volcanoes in the Southern Volcanic Zone have similar alignments, such as Nevados de Chillán and Puyehue-Cordón Caulle.

Geographic entities mentioned:
surface_form: Nevados de Chillán
instance_of: Mountain
countries: Chile
coordinates: lat: -36.863333333333
lon: -71.376666666667
surface_form: Puyehue-Cordón Caulle
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
surface_form: puyehue-cordón caulle
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
surface_form: nevados de chillán
instance_of: Mountain
countries: Chile
coordinates: lat: -36.863333333333
lon: -71.376666666667
In addition, three tephras in neighbouring lakes dated to 16,748–16,189, 15,597–12,582 and 12,708–12,567 years Before Present may originate from Quetrupillán but they have also been attributed to Sollipulli. All these tephras are of rhyolitic to rhyodacitic composition and the eruptions that generated them have an estimated volcanic explosivity index of 3.

Geographic entities mentioned:
surface_form: Sollipulli
instance_of: Mountain
countries: Chile
coordinates: lat: -38.975
lon: -71.52
surface_form: sollipulli
instance_of: Mountain
countries: Chile
coordinates: lat: -38.975
lon: -71.52
surface_form: quetrupillán
instance_of: Mountain
countries: Chile
coordinates: lat: -39.5
lon: -71.7
Mythology. According to a tale from Mapuche mythology, originally there were just two volcanoes: Choshuenco and Lanín. Then the volcano (Villarrica) fought the other two volcanoes in a century-long conflict; eventually Ruka Pillan was victorious, coinciding with the beginning Spanish conquest. Climate and vegetation. Annual precipitation exceeds, with a mean annual temperature of.

Geographic entities mentioned:
surface_form: Choshuenco
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
surface_form: Lanín
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -39.632777777778
lon: -71.499722222222
surface_form: choshuenco
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
Other volcanoes in the Southern Volcanic Zone have similar alignments, such as Nevados de Chillán and Puyehue-Cordón Caulle. In comparison to Villarrica, Quetrupillán has been less active and its eruptions were also smaller than Villarrica's, with no large pyroclastic flows found at Quetrupillán. Local.

Geographic entities mentioned:
surface_form: villarrica
instance_of: Mountain
countries: Chile
coordinates: lat: -39.42
lon: -71.939166666667
surface_form: quetrupillán
instance_of: Mountain
countries: Chile
coordinates: lat: -39.5
lon: -71.7
surface_form: quetrupillán
instance_of: Mountain
countries: Chile
coordinates: lat: -39.5
lon: -71.7
surface_form: quetrupillán
instance_of: Mountain
countries: Chile
coordinates: lat: -39.5
lon: -71.7
surface_form: villarrica
instance_of: Lake
countries: Chile
coordinates: lat: -39.25
lon: -72.083333333333
Fissure vents of Pleistocene-Holocene age occur on the southern side of the volcano. The small volume of the main Quetrupillán edifice and the widespread vents may reflect the interaction between the volcano and the Liquiñe-Ofqui fault, which generated secondary vents whose location was controlled by the Liquiñe-Ofqui fault, the Mocha-Villarrica fault and local structures.

Geographic entities mentioned:
surface_form: villarrica
instance_of: Mountain
countries: Chile
coordinates: lat: -39.42
lon: -71.939166666667
surface_form: quetrupillán
instance_of: Mountain
countries: Chile
coordinates: lat: -39.5
lon: -71.7
surface_form: villarrica
instance_of: Lake
countries: Chile
coordinates: lat: -39.25
lon: -72.083333333333
Magnetotelluric investigation of the area has found evidence of a possible deep-seated magma reservoir. Composition. Volcanic rocks at Quetrupillán have a bimodal composition, ranging from basalt to andesite with trachyte the main component, and overall more silicic than the rocks erupted by Villarrica and Lanín. Unusually for the region, trachydacite also occurs at the volcano.

Geographic entities mentioned:
surface_form: villarrica
instance_of: Mountain
countries: Chile
coordinates: lat: -39.42
lon: -71.939166666667
surface_form: villarrica
instance_of: Lake
countries: Chile
coordinates: lat: -39.25
lon: -72.083333333333
Quetrupillán. Quetrupillán (&quot;blunted&quot;, &quot;mutilated&quot;; also known as Ketropillán; the name is sometimes applied to the neighbouring Lanín volcano.) is a stratovolcano located in Los Ríos Region of Chile. It is situated between Villarrica and Lanín volcanoes, within Villarrica National Park.

Geographic entities mentioned:
surface_form: quetrupillán
instance_of: Mountain
countries: Chile
coordinates: lat: -39.5
lon: -71.7
The volcano contains a field of lava domes, maars and pyroclastic cones that occupy a surface of. These subsidiary vents include the scoria cone Huililco, the Volcanes de Llancahue and the Volcanoes de Reyehueico. There are in total 16 lateral vents, of which 12 are found in a volcanic field south of Quetrupillán. Fissure vents of Pleistocene-Holocene age occur on the southern side of the volcano.

Geographic entities mentioned:
surface_form: quetrupillán
instance_of: Mountain
countries: Chile
coordinates: lat: -39.5
lon: -71.7
A number of eruption products show traces of ice-lava interactions. Tuff rings and maars formed through the interaction of magma with groundwater. A geomagnetic anomaly at shallow depth south of the volcano may be a pluton associated with a resurgent dome. Huililco scoria cone has produced two lava flows and is considered to be also part of the Quetrupillán volcanic complex.

Geographic entities mentioned:
surface_form: quetrupillán
instance_of: Mountain
countries: Chile
coordinates: lat: -39.5
lon: -71.7
Huililco scoria cone has produced two lava flows and is considered to be also part of the Quetrupillán volcanic complex. Three different formations make up the basement of Quetrupillán: The Triassic Panguipulli, the possibly Cretaceous Currarehue and the Miocene Trápatrapa formations and plutonic rocks. These are plutonic and volcaniclastic rock units.

Geographic entities mentioned:
surface_form: quetrupillán
instance_of: Mountain
countries: Chile
coordinates: lat: -39.5
lon: -71.7
These contain phenocrysts of plagioclase and pyroxene, with additional microphenocrysts of ilmenite and magnetite. Based on the composition, it has been inferred that the magma reservoir of Quetrupillán contained a mush of crystals, from which magma was repeatedly mobilized following the injection of fresh magmas that reheated the mush.

Geographic entities mentioned:
surface_form: quetrupillán
instance_of: Mountain
countries: Chile
coordinates: lat: -39.5
lon: -71.7
A tectonic regime associated with the Liquiñe-Ofqui Fault which prevents magma from simply ascending to the surface may help the magma evolution processes. Eruptive history. Eruptive activity at Quetrupillán commenced before the ice ages. The first phase of activity involved the formation of calderas and stratovolcanoes; later during the ice ages lava flows and ignimbrites were emplaced.

Geographic entities mentioned:
surface_form: quetrupillán
instance_of: Mountain
countries: Chile
coordinates: lat: -39.5
lon: -71.7
Reports exist of eruptions during the 19th century, one eruption was reported in 1872. Explosive activity has a recurrence interval of about 1,200 years, which given the age of the last event carries significant implications with regards to the volcanic hazard of Quetrupillán. Mythology. According to a tale from Mapuche mythology, originally there were just two volcanoes: Choshuenco and Lanín.

Geographic entities mentioned:
surface_form: quetrupillán
instance_of: Mountain
countries: Chile
coordinates: lat: -39.5
lon: -71.7
Annual precipitation exceeds, with a mean annual temperature of. The slopes of Quetrupillán are covered by temperate forests, with &quot;Nothofagus&quot; trees being the most important species; other trees are the tepa and the maniú hembra., vegetation on Quetrupillán included &quot;Araucaria araucana&quot; and &quot;Nothofagus antarctica&quot; forests, as well as puna-like vegetation.

Geographic entities mentioned:
surface_form: quetrupillán
instance_of: Mountain
countries: Chile
coordinates: lat: -39.5
lon: -71.7
The population was 2,291 at the 2010 census. It is part of the Harrisonburg Metropolitan Statistical Area. Geography. Massanutten is located at (38.404566, &minus;78.740120). It lies within a valley at the southern end of Massanutten Mountain. According to the United States Census Bureau, the CDP has a total area of 14.3 square miles (37.1 km2), all land. Demographics.

Geographic entities mentioned:
surface_form: Massanutten Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.643
lon: -78.612
Cherleria dirphya. &quot;Cherleria dirphya&quot; is a rare species of plant in the family Caryophyllaceae. It is endemic to Mt. Dirfi on Evvia in Greece. It is restricted to the higher peaks of this single mountain on an island with many endemic plant species. Its natural habitat is Mediterranean-type shrubby vegetation. It is threatened by habitat loss. Description.

Geographic entities mentioned:
surface_form: Mt. Dirfi
instance_of: Mountain
countries: Greece
coordinates: lat: 38.6268
lon: 23.8409
Taxonomy. &quot;Minuartia dirphya&quot; was validly published in 2005 based on material collected from the northern slopes of mount Dirfi, Euboea, Greece. It is placed in &quot;Minuartia&quot; sect. &quot;Spectabiles&quot;, subsect. &quot;Laricifoliae&quot;, ser. &quot;Laricifoliae&quot;.

Geographic entities mentioned:
surface_form: Dirfi
instance_of: Mountain
countries: Greece
coordinates: lat: 38.6268
lon: 23.8409
The majority of the residents of the municipality are in the city of George, which as of 2011 has a population of 157,394. Close to George are the coastal resorts of Herolds Bay (pop. 704) and Wilderness (pop. 6,164). Haarlem (pop. 2,376) and Uniondale (pop. 4,525) are in the interior of the municipality at the top of the Langkloof. History.

Geographic entities mentioned:
surface_form: Langkloof
instance_of: Valley
countries: South Africa
coordinates: lat: -33.825
lon: 23.857777777778
Vallvidrera, el Tibidabo i les Planes. Vallvidrera, el Tibidabo i les Planes is a neighborhood in the &quot;Sarrià-Sant Gervasi&quot; district of Barcelona, Catalonia, Spain. It is formed by three areas: Vallvidrera (that was a former municipality added to Sarrià), Tibidabo and.

Geographic entities mentioned:
surface_form: Tibidabo
instance_of: Mountain
countries: Spain
coordinates: lat: 41.4225
lon: 2.118611111111111
Governors Ridge. Governors Ridge is located in Mount Rainier National Park in Pierce County of Washington state. It is part of the Cascade Range and is situated west of Cayuse Pass and 1.09 mile east of Tamanos Mountain, which is the nearest higher peak. Precipitation runoff from Governors Ridge drains into tributaries of the White River and Cowlitz River.

Geographic entities mentioned:
surface_form: Tamanos Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.87205
lon: -121.59676
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The toponym honors all the governors who have served the state of Washington. The highest rocky crag on the ridge is known as &quot;Governors Peak&quot;. There is also a 40-foot leaning spire known as &quot;Governors Needle&quot;, and Barrier Peak is at the southern culmination of the ridge. The normal climbing access is from the Owyhigh Lakes Trail. Climate.

Geographic entities mentioned:
surface_form: Barrier Peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.85951
lon: -121.577048
Governors Ridge. Governors Ridge is located in Mount Rainier National Park in Pierce County of Washington state. It is part of the Cascade Range and is situated west of Cayuse Pass and 1.09 mile east of Tamanos Mountain, which is the nearest higher peak. Precipitation runoff from Governors Ridge drains into tributaries of the White River and Cowlitz River.

Geographic entities mentioned:
surface_form: governors ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 46.86472
lon: -121.573252
It is part of the Cascade Range and is situated west of Cayuse Pass and 1.09 mile east of Tamanos Mountain, which is the nearest higher peak. Precipitation runoff from Governors Ridge drains into tributaries of the White River and Cowlitz River. The toponym honors all the governors who have served the state of Washington. The highest rocky crag on the ridge is known as &quot;Governors Peak&quot;.

Geographic entities mentioned:
surface_form: governors ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 46.86472
lon: -121.573252
surface_form: white river
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.93055556
lon: -74.10138889
surface_form: white river
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.99639
lon: -71.46167
Beebe Lake (Ithaca, New York). Beebe Lake /bibi/ is a reservoir in Ithaca, New York, located on the campus of Cornell University. Formation. Beebe Lake was once a forested swamp. A pond was formed when Ezra Cornell constructed a dam on Fall Creek in 1838, above Triphammer Falls, to provide power to the mills owned by Jeremiah S. Beebe.

Geographic entities mentioned:
surface_form: beebe lake (ithaca, new york)
instance_of: Lake
countries: United States
coordinates: lat: 42.451111111111
lon: -76.476388888889
surface_form: beebe lake
instance_of: Lake
countries: United States
coordinates: lat: 45.174166666667
lon: -93.743611111111
Beebe Lake (Ithaca, New York). Beebe Lake /bibi/ is a reservoir in Ithaca, New York, located on the campus of Cornell University. Formation. Beebe Lake was once a forested swamp. A pond was formed when Ezra Cornell constructed a dam on Fall Creek in 1838, above Triphammer Falls, to provide power to the mills owned by Jeremiah S. Beebe.

Geographic entities mentioned:
surface_form: beebe lake
instance_of: Lake
countries: United States
coordinates: lat: 42.451111111111
lon: -76.476388888889
surface_form: beebe lake
instance_of: Lake
countries: United States
coordinates: lat: 45.174166666667
lon: -93.743611111111