Sarmila/GeoWiki-Features huggingface dataset:
It is bordered on the north, east and southeast by houses in a gated community. On the south is a grass field, beyond which is Eloise Loop Road, and on the west and southwest is a citrus grove. Round Lake is about east of the south cove of Lake Winterset. This lake is swampy on much of its shore and there are ten or so minuscule islets along the shore.

Geographic entities mentioned:
surface_form: Lake Winterset
instance_of: Lake
countries: United States
coordinates: lat: 27.9745
lon: -81.682
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9344286
lon: -96.9790408
surface_form: round lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.0648
lon: -75.1033
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 46.1508
lon: -86.7447
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.070277777778
lon: -74.584722222222
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 42.934604
lon: -73.7823057
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 27.9631
lon: -81.674
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 45.036388888889
lon: -97.773055555556
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 43.531388888889
lon: -75.180277777778
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.8685
lon: -93.4925
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 48.161666666667
lon: -116.63805555556
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 45.6020431
lon: -122.4032555
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 41.837095
lon: -86.418541
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.964444444444
lon: -96.827222222222
Round Lake (Florida lake). Round Lake is a natural freshwater lake on the south side of Winter Haven, Florida. It is almost round in shape and has a surface area of. It is bordered on the north, east and southeast by houses in a gated community. On the south is a grass field, beyond which is Eloise Loop Road, and on the west and southwest is a citrus grove.

Geographic entities mentioned:
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9344286
lon: -96.9790408
surface_form: round lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.0648
lon: -75.1033
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 46.1508
lon: -86.7447
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.070277777778
lon: -74.584722222222
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 42.934604
lon: -73.7823057
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 27.9631
lon: -81.674
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 45.036388888889
lon: -97.773055555556
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 43.531388888889
lon: -75.180277777778
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.8685
lon: -93.4925
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 48.161666666667
lon: -116.63805555556
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 45.6020431
lon: -122.4032555
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 41.837095
lon: -86.418541
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.964444444444
lon: -96.827222222222
Round Lake is about east of the south cove of Lake Winterset. This lake is swampy on much of its shore and there are ten or so minuscule islets along the shore. Round Lake is completely surrounded by private property, which means the public needs to obtain permission to access the lake for fishing. There are no swimming beaches on the lake and only private boat and fishing docks.

Geographic entities mentioned:
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9344286
lon: -96.9790408
surface_form: round lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.0648
lon: -75.1033
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 46.1508
lon: -86.7447
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.070277777778
lon: -74.584722222222
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 42.934604
lon: -73.7823057
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 27.9631
lon: -81.674
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 45.036388888889
lon: -97.773055555556
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 43.531388888889
lon: -75.180277777778
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.8685
lon: -93.4925
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 48.161666666667
lon: -116.63805555556
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 45.6020431
lon: -122.4032555
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 41.837095
lon: -86.418541
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.964444444444
lon: -96.827222222222
Qaleh Kharabeh (, also Romanized as Qal‘eh Kharābeh) is the archaeological site of a 5th-century fort in the Gorgan Plain, in Golestan Province in northeastern Iran. It lies one mile to the south of the Great Wall of Gorgan, which was a fortification built between the Caspian Sea and the Kopet Dag Mountains between 420 AD and 530s AD by the Sasanian Empire, on the northern edge of their empire.

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
Southern forest is used for a wide range of recreational activities such as horseback-riding, jogging and scouting. The four parks are &quot;Hovmarken&quot;, &quot;Indelukket&quot;, &quot;Æblehaven&quot; and &quot;Hedeskovparken&quot;. Egå Engsø lies south of the city and from it the river New Egå (Danish: Ny Egå) runs to the coast and bay. Churches.

Geographic entities mentioned:
surface_form: Egå Engsø
instance_of: Lake
countries: Denmark
coordinates: lat: 56.218
lon: 10.221
Camp Leroy Johnson. fcct7swuc3bkx68l7nqcc5ja8bctw" xml:space="preserve">Camp Leroy Johnson in New Orleans, Louisiana, was located on the south shore of Lake Pontchartrain in the area bounded west by Franklin Avenue, and east by Inner Harbor Navigation Canal. The camp was opened in 1942 as the New Orleans Army Air Base.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
Location. The power station is located across the Nyagak River in Nyapea Sub County, Okoro County, Zombo District, in the West Nile sub-region of the Northern Region of Uganda. This is approximately north of the town of Paidha, close to the border with the Democratic Republic of the Congo, in close proximity to, but downstream of, the existing Nyagak I Power Station. Overview.

Geographic entities mentioned:
surface_form: Nyagak River
instance_of: Watercourse
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: 2.64781
lon: 31.11112
Geography. The Tell Atlas runs parallel to the Mediterranean coast. Together with the Saharan Atlas to the south, it forms the northernmost of two more or less parallel ranges which approach one another towards the east, remaining quite distinct from one another in &quot;Western Algeria&quot; and merging in &quot;Eastern Algeria&quot;.

Geographic entities mentioned:
surface_form: east
instance_of: Mountain
countries: Algeria
France
Between them lies the valley of the Chelif and various lesser rivers. South of the Tell Atlas is the high plateau of the &quot;Hautes Plaines&quot; (~1000 m in elevation) with level terrain where water collects during the wet season, forming large shallow salt lakes which become salt flats as they dry.

Geographic entities mentioned:
surface_form: Hautes Plaines
instance_of: Plateau
countries: Algeria
coordinates: lat: 34.01861111
lon: 0.08527778
In the summer a hot, dry wind, the Sirocco, blows north from the Sahara across the Tell Atlas, causing dusty, dry conditions along the northern coast of Africa. Despite the arid climate, some agriculture for barley and wheat farming is found in the Tell Atlas region.

Geographic entities mentioned:
surface_form: farming
instance_of: Mountain
countries: Algeria
France
coordinates: lat: 36.7325
lon: 4.04972
This peak was named after German geologist and paleontologist Emanuel Kayser. Geography. Kayser Mountain is located at the eastern end of the Haug Range in northern Hall Land, at the southern limit of the Polaris Foreland. It rises 6 km to the southwest of the shore of the Newman Bay fjord. With a height of, Kayser Mountain is the highest elevation of Hall Land and of the Haug Range.

Geographic entities mentioned:
surface_form: Newman Bay
instance_of: Body of water
countries: Greenland
coordinates: lat: 81.63333
lon: -58
Kayser Mountain. Kayser Mountain () is a mountain in Hall Land, NW Greenland. Administratively it is part of the Northeast Greenland National Park. This peak was named after German geologist and paleontologist Emanuel Kayser. Geography. Kayser Mountain is located at the eastern end of the Haug Range in northern Hall Land, at the southern limit of the Polaris Foreland.

Geographic entities mentioned:
surface_form: kayser mountain
instance_of: Mountain
countries: Greenland
coordinates: lat: 81.56667
lon: -58.3
This peak was named after German geologist and paleontologist Emanuel Kayser. Geography. Kayser Mountain is located at the eastern end of the Haug Range in northern Hall Land, at the southern limit of the Polaris Foreland. It rises 6 km to the southwest of the shore of the Newman Bay fjord. With a height of, Kayser Mountain is the highest elevation of Hall Land and of the Haug Range.

Geographic entities mentioned:
surface_form: kayser mountain
instance_of: Mountain
countries: Greenland
coordinates: lat: 81.56667
lon: -58.3
It rises 6 km to the southwest of the shore of the Newman Bay fjord. With a height of, Kayser Mountain is the highest elevation of Hall Land and of the Haug Range. Brachiopod fossils of genus &quot;Pentamerus&quot; dating back to the Lower Silurian have been found in this mountain.

Geographic entities mentioned:
surface_form: kayser mountain
instance_of: Mountain
countries: Greenland
coordinates: lat: 81.56667
lon: -58.3
Pen yr Helgi Du. is a mountain peak in the eastern part of the Carneddau in Snowdonia, North Wales. It lies on the south-eastern flanks of Carnedd Llewelyn, and is linked to Carnedd Llewelyn over the col of Bwlch Eryl Farchog, a knife-edge ridge over the cliffs of Craig Yr Ysfa. Cwm Eigiau lies to the east and the Ffynnon Llugwy reservoir to the south.

Geographic entities mentioned:
surface_form: Carneddau
instance_of: Landform
countries: United Kingdom
coordinates: lat: 53.18114
lon: -4.00297
Pen yr Helgi Du. is a mountain peak in the eastern part of the Carneddau in Snowdonia, North Wales. It lies on the south-eastern flanks of Carnedd Llewelyn, and is linked to Carnedd Llewelyn over the col of Bwlch Eryl Farchog, a knife-edge ridge over the cliffs of Craig Yr Ysfa. Cwm Eigiau lies to the east and the Ffynnon Llugwy reservoir to the south.

Geographic entities mentioned:
surface_form: Carnedd Llewelyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.160586111111
lon: -3.9693055555556
surface_form: carnedd llewelyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.160586111111
lon: -3.9693055555556
It lies on the south-eastern flanks of Carnedd Llewelyn, and is linked to Carnedd Llewelyn over the col of Bwlch Eryl Farchog, a knife-edge ridge over the cliffs of Craig Yr Ysfa. Cwm Eigiau lies to the east and the Ffynnon Llugwy reservoir to the south. To the east of Pen yr Helgi Du is Pen Llithrig y Wrach (the slippery peak of the witch).

Geographic entities mentioned:
surface_form: Pen Llithrig y Wrach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.142330555556
lon: -3.9210805555556
surface_form: pen yr helgi du
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.148180555556
lon: -3.9482611111111
Pen yr Helgi Du. is a mountain peak in the eastern part of the Carneddau in Snowdonia, North Wales. It lies on the south-eastern flanks of Carnedd Llewelyn, and is linked to Carnedd Llewelyn over the col of Bwlch Eryl Farchog, a knife-edge ridge over the cliffs of Craig Yr Ysfa. Cwm Eigiau lies to the east and the Ffynnon Llugwy reservoir to the south.

Geographic entities mentioned:
surface_form: pen yr helgi du
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.148180555556
lon: -3.9482611111111
Grūda (lake). Grūda is a lake located near Ašašninkai at the border between Lithuania and Belarus. The lake is spread across Varėna district in Lithuania and Grodno region of Belarus, and is shared by the two countries. Geography. Grūda lake located near Ašašninkai at the border between Lithuania and Belarus.

Geographic entities mentioned:
surface_form: grūda
instance_of: Lake
countries: Lithuania
Belarus
coordinates: lat: 53.92638889
lon: 24.30694444
The lake is spread across Varėna district in Lithuania and Grodno region of Belarus, and is shared by the two countries. Geography. Grūda lake located near Ašašninkai at the border between Lithuania and Belarus. The lake is spread across Varėna district in Lithuania and Grodno region of Belarus, and is shared by the two countries.

Geographic entities mentioned:
surface_form: grūda
instance_of: Lake
countries: Lithuania
Belarus
coordinates: lat: 53.92638889
lon: 24.30694444
Geography. Grūda lake located near Ašašninkai at the border between Lithuania and Belarus. The lake is spread across Varėna district in Lithuania and Grodno region of Belarus, and is shared by the two countries. It is the source of the Grūda river, which flows for before joining the Merkys river, about from its mouth. The lake is spread over an area of at an altitude of.

Geographic entities mentioned:
surface_form: grūda
instance_of: Lake
countries: Lithuania
Belarus
coordinates: lat: 53.92638889
lon: 24.30694444
She was accompanied on that swim by the famous &quot;Endeavour&quot; fishing boat. On 10 June 1925 Norman Derham had completed a one way swim across the Estuary. On 27 August 1960 White swam Windermere in 7 hours 26 minutes. It was a British Long Distance Swimming Association (BLDSA) race, and age 16, she came second, finding the lake quite a challenge.

Geographic entities mentioned:
surface_form: Windermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.358333333333
lon: -2.9361111111111
Pichaqani (Vinto). Pichaqani (Aymara &quot;pichaqa, phichaqa, piqacha&quot; a big needle, &quot;-ni&quot; a suffix, &quot;the one with a big needle&quot;, also spelled &quot;Pichacani&quot;) is a mountain in the Bolivian Andes. It is located in the Cochabamba Department, Quillacollo Province, Vinto Municipality. Pichaqani lies southwest of Tunari and southeast of Phullu Punchu.

Geographic entities mentioned:
surface_form: Phullu Punchu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.29722222
lon: -66.425
surface_form: phullu punchu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.29722222
lon: -66.425
Pichaqani (Vinto). Pichaqani (Aymara &quot;pichaqa, phichaqa, piqacha&quot; a big needle, &quot;-ni&quot; a suffix, &quot;the one with a big needle&quot;, also spelled &quot;Pichacani&quot;) is a mountain in the Bolivian Andes. It is located in the Cochabamba Department, Quillacollo Province, Vinto Municipality. Pichaqani lies southwest of Tunari and southeast of Phullu Punchu.

Geographic entities mentioned:
surface_form: pichaqani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.86527778
lon: -67.91333333
surface_form: pichaqani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.50694444
lon: -66.89083333
surface_form: pichaqani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.4725
lon: -66.47444444
surface_form: pichaqani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.20611111
lon: -68.28388889
surface_form: pichaqani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.87694444
lon: -66.71333333
surface_form: pichaqani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.30916667
lon: -66.40333333
Pichaqani (Vinto). Pichaqani (Aymara &quot;pichaqa, phichaqa, piqacha&quot; a big needle, &quot;-ni&quot; a suffix, &quot;the one with a big needle&quot;, also spelled &quot;Pichacani&quot;) is a mountain in the Bolivian Andes. It is located in the Cochabamba Department, Quillacollo Province, Vinto Municipality. Pichaqani lies southwest of Tunari and southeast of Phullu Punchu.

Geographic entities mentioned:
surface_form: pichaqani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.86527778
lon: -67.91333333
surface_form: pichaqani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.50694444
lon: -66.89083333
surface_form: pichaqani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.4725
lon: -66.47444444
surface_form: pichaqani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.20611111
lon: -68.28388889
surface_form: pichaqani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.87694444
lon: -66.71333333
surface_form: pichaqa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.8097
lon: -68.8589
surface_form: pichaqani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.30916667
lon: -66.40333333
Door Peninsula. The Door Peninsula is a peninsula in eastern Wisconsin, separating the southern part of the Green Bay from Lake Michigan. The peninsula includes northern Kewaunee County, northeastern Brown County, and the mainland portion of Door County. It is on the western side of the Niagara Escarpment.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
The Door Peninsula is a peninsula in eastern Wisconsin, separating the southern part of the Green Bay from Lake Michigan. The peninsula includes northern Kewaunee County, northeastern Brown County, and the mainland portion of Door County. It is on the western side of the Niagara Escarpment. Well known for its cherry and apple orchards, the Door Peninsula is a popular tourism destination.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
With the 1881 completion of the Sturgeon Bay Ship Canal, the northern half of the peninsula became an island. Limestone outcroppings of the Niagara Escarpment are visible on both shores of the peninsula, but are larger and more prominent on the Green Bay side as seen at the Bayshore Blufflands. Progressions of dunes have created much of the rest of the shoreline, especially on the east side.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
Humans, whether Native Americans, early explorers, or American ship captains, have been well aware of the dangerous water passage that lies between the Door Peninsula and Washington Island, connecting the bay to the rest of Lake Michigan. It was named by the Native Americans and translated into French as &quot;Porte des Morts&quot;: in English, &quot;Death's Door&quot;.

Geographic entities mentioned:
surface_form: Porte des Morts
instance_of: Body of water
countries: United States
coordinates: lat: 45.2933
lon: -86.9586
The fact that most of the sediments of the Upper Laetolil Beds are volcanic tuffs suggests that ash falls would have occurred regularly at Laetoli, with the (currently extinct) Sadiman volcano being the likely source of the ash.

Geographic entities mentioned:
surface_form: Sadiman volcano
instance_of: Mountain
countries: Tanzania
coordinates: lat: -3.193821
lon: 35.41297
Øvervatnet. Øvervatnet is a meromictic lake (containing anoxic seawater at depth of and below) located in Fauske Municipality in Nordland county, Norway. The lake is situated about east of the town of Fauske. Its water is fresh down to depths of. From that level, the water becomes increasingly salty. Øvervatnet is also heavily polluted by mining industry operations upstream in earlier times.

Geographic entities mentioned:
surface_form: øvervatnet
instance_of: Lake
countries: Norway
coordinates: lat: 67.216666666667
lon: 15.666666666667
The lake is situated about east of the town of Fauske. Its water is fresh down to depths of. From that level, the water becomes increasingly salty. Øvervatnet is also heavily polluted by mining industry operations upstream in earlier times. The lake flows out into the neighboring lake Nedrevatnet, to the west.

Geographic entities mentioned:
surface_form: øvervatnet
instance_of: Lake
countries: Norway
coordinates: lat: 67.216666666667
lon: 15.666666666667
The effects of Quaternary glacial erosion are not as visible in Gotland as they are in mainland Sweden because of its sedimentary basement. Glaciation did however left thin blankets of fine-grained boulder-clay till. The boulder include rocks of Archean age transported from far-away regions of Fennoscandia. Where the till blanket is absent the bare rock surfaces are exposed.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Wetlands occur on the eastern shores, and the local flora and fauna depend on the water supply to the lake. The Cordón de Puntas Negras separates Tuyajto Lake from Lejía Lake. Six former shorelines occur at Tuyajto Lake, like other lakes in the region at about above the current lake levels; they are considered to be remnants of late glacial shorelines, during the Lake Tauca wet period.

Geographic entities mentioned:
surface_form: Cordón de Puntas Negras
instance_of: Mountain
countries: Chile
coordinates: lat: -23.742777777778
lon: -67.534166666667
surface_form: lejía lake
instance_of: Lake
countries: Chile
coordinates: lat: -23.5
lon: -67.6925
surface_form: tuyajto lake
instance_of: Lake
countries: Chile
coordinates: lat: -23.94271
lon: -67.59172
Wetlands occur on the eastern shores, and the local flora and fauna depend on the water supply to the lake. The Cordón de Puntas Negras separates Tuyajto Lake from Lejía Lake. Six former shorelines occur at Tuyajto Lake, like other lakes in the region at about above the current lake levels; they are considered to be remnants of late glacial shorelines, during the Lake Tauca wet period.

Geographic entities mentioned:
surface_form: Lake Tauca
instance_of: Lake
countries: Peru
coordinates: lat: -20
lon: -68
surface_form: tuyajto lake
instance_of: Lake
countries: Chile
coordinates: lat: -23.94271
lon: -67.59172
Climate. The climate is dry, with precipitation averaging and at above elevation. Moisture originates from the Atlantic Ocean, the equatorial Pacific and the Gran Chaco in Argentina; it falls mostly during winter unlike the rest of the Altiplano where summer precipitation dominates. Potential evaporation reaches.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
In general, groundwater in the region is salty to brackish, it originates as rain or snow and probably obtains salts from underground salt bodies. The lake does not overflow at its surface, evaporation and perhaps underground drainage towards Salar Aguas Calientes farther west are mainly responsible for removing water from the lake. Geology.

Geographic entities mentioned:
surface_form: aguas calientes
instance_of: Mountain
countries: Chile
coordinates: lat: -23.368333333333
lon: -67.685
Alluvial deposits and lake sediments occur in the whole region; the lake sediments in particular can be found south and east of Tuyajto Lake and form alluvial fans on its eastern side. Tuyajto Lake lies within a endorheic basin which spreads out east of the lake; west lies the Salar Aguas Calientes basin.

Geographic entities mentioned:
surface_form: aguas calientes
instance_of: Mountain
countries: Chile
coordinates: lat: -23.368333333333
lon: -67.685
surface_form: tuyajto lake
instance_of: Lake
countries: Chile
coordinates: lat: -23.94271
lon: -67.59172
Tuyajto Lake lies within a endorheic basin which spreads out east of the lake; west lies the Salar Aguas Calientes basin. Major mountains in the area are the high Tuyajto north of the lake, Incahuasi Sur southeast and high Medano Volcano south-southwest of Tuyajto lake.

Geographic entities mentioned:
surface_form: incahuasi
instance_of: Mountain
countries: Chile
coordinates: lat: -24.033333333333
lon: -67.55
surface_form: tuyajto lake
instance_of: Lake
countries: Chile
coordinates: lat: -23.94271
lon: -67.59172
Tuyajto Lake. Tuyajto Lake is a salt lake located in the Antofagasta Region, northern Chile. Located at an elevation of about, its surface area presently fluctuates between but in the past it was considerably larger; this led to humans going to the lake and creating archeological sites there. Presently, the lake is groundwater-fed and has no surface outlet but water might seep out underground.

Geographic entities mentioned:
surface_form: tuyajto lake
instance_of: Lake
countries: Chile
coordinates: lat: -23.94271
lon: -67.59172
Lake levels also vary with the discharge of springs that feed it. At times Tuyajto Lake is almost empty, and salts such as gypsum and halite can be seen on the edges. Wetlands occur on the eastern shores, and the local flora and fauna depend on the water supply to the lake. The Cordón de Puntas Negras separates Tuyajto Lake from Lejía Lake.

Geographic entities mentioned:
surface_form: tuyajto lake
instance_of: Lake
countries: Chile
coordinates: lat: -23.94271
lon: -67.59172
At that time between 13,8009,100 calibrated radiocarbon years ago or 12,80010,300 years ago Tuyajto Lake was much larger, having an area of - and its uppermost shoreline reached elevation. The former lake levels may have reached above the present-day level perhaps to the point of overflowing, and still was about deep about 8,000 years ago.

Geographic entities mentioned:
surface_form: tuyajto lake
instance_of: Lake
countries: Chile
coordinates: lat: -23.94271
lon: -67.59172
Part of the water comes from Tuyajto volcano as well as Pampa Las Tecas and Pampa Colorada east and northeast from Tuyajto Lake and flows underground towards Tuyajto. In general, groundwater in the region is salty to brackish, it originates as rain or snow and probably obtains salts from underground salt bodies.

Geographic entities mentioned:
surface_form: tuyajto lake
instance_of: Lake
countries: Chile
coordinates: lat: -23.94271
lon: -67.59172
Alluvial deposits and lake sediments occur in the whole region; the lake sediments in particular can be found south and east of Tuyajto Lake and form alluvial fans on its eastern side. Tuyajto Lake lies within a endorheic basin which spreads out east of the lake; west lies the Salar Aguas Calientes basin.

Geographic entities mentioned:
surface_form: tuyajto lake
instance_of: Lake
countries: Chile
coordinates: lat: -23.94271
lon: -67.59172
Temperatures average about. Human use. An Early Archaic archeological site consisting of fireplaces has been found at Tuyajto Lake; it was constructed on a former shoreline and appears to relate to this shoreline. Such archeological sites close to then-shorelines are common for the &quot;Tambillo stage&quot; of early human population in the Atacama.

Geographic entities mentioned:
surface_form: tuyajto lake
instance_of: Lake
countries: Chile
coordinates: lat: -23.94271
lon: -67.59172
Mining and tourism are increasingly important activities in the region and together with growing agriculture and cities have resulted in increased demand for water, resulting in more research in existing water sources. Reportedly, BHP obtains water from the Tuyajto Lake basin. Tuyajto is part of the Los Flamencos Natural Reserve.

Geographic entities mentioned:
surface_form: tuyajto lake
instance_of: Lake
countries: Chile
coordinates: lat: -23.94271
lon: -67.59172
KNWA-TV. KNWA-TV (channel 51) is a television station licensed to Rogers, Arkansas, United States, serving as the NBC affiliate for Northwest Arkansas and the Arkansas River Valley. It is owned by Nexstar Media Group alongside Fort Smith–licensed Fox affiliate KFTA-TV (channel 24) and Eureka Springs–licensed MyNetworkTV affiliate KXNW (channel 34).

Geographic entities mentioned:
surface_form: Arkansas River Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
MBH has built over 2,225 units and designed more than 9,000 units. MBH's rehabilitation projects include the Hathaway Warehouse in Rincon Hill, San Francisco. Built in the 1850s—perhaps as early as 1856—the Hathaway Warehouse is one of the oldest remaining warehouses in the city and is designated as a historically Significant Building.

Geographic entities mentioned:
surface_form: Rincon Hill, San Francisco
instance_of: Mountain
countries: United States
coordinates: lat: 37.78555556
lon: -122.39194444
Dunbar Head. c05ilb021uhc1aezr4ajufp3yvvv9" xml:space="preserve">Dunbar Head () is a projecting rock headland at the south end of the Scott Coast, southeast of the summit of Mount Morning. The feature rises to over and overlooks the Ross Ice Shelf midway between Eastface Nunatak and Birthday Bluffs. It was named by the Advisory Committee on Antarctic Names (1999) after Nelia W.

Geographic entities mentioned:
surface_form: Mount Morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Dunbar Head. c05ilb021uhc1aezr4ajufp3yvvv9" xml:space="preserve">Dunbar Head () is a projecting rock headland at the south end of the Scott Coast, southeast of the summit of Mount Morning. The feature rises to over and overlooks the Ross Ice Shelf midway between Eastface Nunatak and Birthday Bluffs. It was named by the Advisory Committee on Antarctic Names (1999) after Nelia W.

Geographic entities mentioned:
surface_form: Eastface Nunatak
instance_of: Mountain
coordinates: lat: -78.7
lon: 163.633
The feature rises to over and overlooks the Ross Ice Shelf midway between Eastface Nunatak and Birthday Bluffs. It was named by the Advisory Committee on Antarctic Names (1999) after Nelia W. Dunbar, Department of Geoscience, New Mexico Institute of Mining and Technology, Socorro, who made geological investigations at nearby Mount Erebus, the Allan Hills, Mount Takahe, and the Crary Mountains.

Geographic entities mentioned:
surface_form: Mount Erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: Allan Hills
instance_of: Landform
coordinates: lat: -76.7
lon: 159.7
surface_form: Mount Takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
Caesars Head. Caesars Head is a mountain within Caesars Head State Park in northern Greenville County, South Carolina. The summit has an elevation of. The radio tower for TV station WYFF is nearby. Housing developments on top of the mountain are part of the Caesars Head census-designated place. Climate.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: caesars head
instance_of: Mountain
countries: United States
coordinates: lat: 35.105555555556
lon: -82.6275
surface_form: caesars head
instance_of: Mountain
countries: United States
coordinates: lat: 35.105555555556
lon: -82.6275
Caesars Head. Caesars Head is a mountain within Caesars Head State Park in northern Greenville County, South Carolina. The summit has an elevation of. The radio tower for TV station WYFF is nearby. Housing developments on top of the mountain are part of the Caesars Head census-designated place. Climate.

Geographic entities mentioned:
surface_form: caesars head
instance_of: Mountain
countries: United States
coordinates: lat: 35.105555555556
lon: -82.6275
The summit has an elevation of. The radio tower for TV station WYFF is nearby. Housing developments on top of the mountain are part of the Caesars Head census-designated place. Climate. Caesars Head has an oceanic climate (Cfb), a rarity for South Carolina, due to its high elevation, with warm summers and mild winters.

Geographic entities mentioned:
surface_form: caesars head
instance_of: Mountain
countries: United States
coordinates: lat: 35.105555555556
lon: -82.6275
leporina major&quot; (or &quot;D. leporina&quot; var. &quot;major&quot;) to dental fossils from the French phosphorite deposits of Caylux. He also erected two species: &quot;D. nobilis&quot;, basing it off of a maxilla fragment with molars from the Swiss locality of Egerkingen; and &quot;D. spinifera&quot; using a partial maxilla from Mormont in the Natural History Museum of Basel.

Geographic entities mentioned:
surface_form: Mormont
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.65514
lon: 6.53367
It is connected to the fall of Great Moravia, already weakened by its own inner decline and under the attacks of the Hungarians. The exact location of the battle remains unknown, and some interpretations place it west of Lake Balaton.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
The Carpathian mountain range begins in city territory with the Little Carpathians (&quot;Malé Karpaty&quot;). The Záhorie and Danubian lowlands stretch into Bratislava. The city's lowest point is at the Danube's surface at above mean sea level, and the highest point is Devínska Kobyla at. The average altitude is. Climate.

Geographic entities mentioned:
surface_form: Devínska Kobyla
instance_of: Mountain
countries: Slovakia
coordinates: lat: 48.190555555556
lon: 16.995833333333
The city has a number of natural and human-made lakes, most of which are used for recreation. Examples include Štrkovec lake in Ružinov, Kuchajda in Nové Mesto, Zlaté Piesky and the Vajnory lakes in the north-east, and Rusovce lake in the south, which is popular with nudists. Demographics. From the city's origin until the 19th century, Germans were the dominant ethnic group.

Geographic entities mentioned:
surface_form: Zlaté Piesky
instance_of: Lake
countries: Slovakia
coordinates: lat: 48.18472222
lon: 17.18944444
Samuel Hearne. Samuel Hearne (February 1745 – November 1792) was an English explorer, fur-trader, author and naturalist. He was the first European to make an overland excursion across northern Canada to the Arctic Ocean, specifically to Coronation Gulf, via the Coppermine River.

Geographic entities mentioned:
surface_form: Coppermine River
instance_of: Watercourse
countries: Canada
coordinates: lat: 67.816666666667
lon: -115.06666666667
By June, the geese had flown further north and they were again threatened with famine. At one point, they killed three muskoxen and had to eat them raw because it was too wet to light a fire. They crossed the Kazan River above Yathkyed Lake where they found good hunting and fishing and then went west to Lake Dubawnt which is about northwest of Churchill.

Geographic entities mentioned:
surface_form: Yathkyed Lake
instance_of: Lake
countries: Canada
coordinates: lat: 62.666667
lon: -97.966667
The group included eight of Matonabbee's wives to act as beasts of burden in the sledge traces, camp servant and cooks. This third expedition set out in December 1770, to reach the Coppermine River in summer, by which he could descend to the Arctic in canoes. Matonabbee kept a fast pace, so fast they reached the great caribou traverse before provisions dwindled and in time for the spring hunt.

Geographic entities mentioned:
surface_form: Coppermine River
instance_of: Watercourse
countries: Canada
coordinates: lat: 67.816666666667
lon: -115.06666666667
This expedition also proved successful in its primary goal by discovering copper in the Coppermine River basin; however, an intensive search of the area yielded only one four-pound lump of copper and commercial mining was not considered viable. Matonabbee led Hearne back to Churchill by a wide westward circle past Bear Lake in Athabasca Country.

Geographic entities mentioned:
surface_form: Bear Lake
instance_of: Lake
countries: Canada
coordinates: lat: 66
lon: -121
Matonabbee led Hearne back to Churchill by a wide westward circle past Bear Lake in Athabasca Country. In midwinter he became the first European to see and cross Great Slave Lake. Hearne returned to Fort Prince of Wales on 30 June 1772, having walked some and explored more than. Later life.

Geographic entities mentioned:
surface_form: Great Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 61.666666666667
lon: -114
Peery Lake. Peery Lake is a fresh water lake on the Paroo River, north of Wilcannia, New South Wales, Far West New South Wales. Peery Lake is an ephemeral lake, in area and is a Ramsar site. Setting. The lake in North western New South Wales is between Paroo-Darling National Park and Nocoleche Nature Reserve.

Geographic entities mentioned:
surface_form: peery lake
instance_of: Lake
countries: Australia
coordinates: lat: -30.7318
lon: 143.5679
Lake Pantano d'Avio. The Lake Pantano d'Avio (or more briefly, &quot;Lake Pantano&quot;) is an artificial lake located in the upper, a lateral valley of the Val Camonica, in the Province of Brescia. Situated at 2,378 meters above sea level, it is the second largest lake in Val Camonica by surface area, after. Description.

Geographic entities mentioned:
surface_form: Val Camonica
instance_of: Valley
countries: Italy
coordinates: lat: 46.0075
lon: 10.3475
surface_form: val camonica
instance_of: Valley
countries: Italy
coordinates: lat: 46.0075
lon: 10.3475
surface_form: lake pantano d'avio
instance_of: Lake
countries: Italy
coordinates: lat: 46.165
lon: 10.47194
Lake Pantano is part of a significant hydroelectric system that powers the power plant in Edolo, operational since 1984 (previously, the waters of the valley’s lakes drove the turbines of the old Temù power plant, now decommissioned). This system comprises Lake Pantano and, the two reservoirs at the highest elevation, and the two lakes in the mid-valley (Lake d'Avio and Lake Benedetto).

Geographic entities mentioned:
surface_form: Lake Benedetto
instance_of: Lake
countries: Italy
coordinates: lat: 46.1856541
lon: 10.4703999
surface_form: lake benedetto
instance_of: Lake
countries: Italy
coordinates: lat: 46.1856541
lon: 10.4703999
Access. Attached to the dam, which is always staffed, are the caretaker’s residence and some service facilities (control cabins), including the station for the cableway that arrives from Dosso Lavedole, above the southern end of Lake Benedetto. This facility, owned by Enel, is not open to the public
The dam and the lake are thus reachable only on foot.

Geographic entities mentioned:
surface_form: Lake Benedetto
instance_of: Lake
countries: Italy
coordinates: lat: 46.1856541
lon: 10.4703999
surface_form: lake benedetto
instance_of: Lake
countries: Italy
coordinates: lat: 46.1856541
lon: 10.4703999
Lake Pantano d'Avio. The Lake Pantano d'Avio (or more briefly, &quot;Lake Pantano&quot;) is an artificial lake located in the upper, a lateral valley of the Val Camonica, in the Province of Brescia. Situated at 2,378 meters above sea level, it is the second largest lake in Val Camonica by surface area, after. Description.

Geographic entities mentioned:
surface_form: val camonica
instance_of: Valley
countries: Italy
coordinates: lat: 46.0075
lon: 10.3475
This facility, owned by Enel, is not open to the public
The dam and the lake are thus reachable only on foot. The most direct trail leading to it branches off from the former route number 11 of the CAI sections of Val Camonica (now part of route number 1,) near Malga Lavedole, and by following it, one reaches the base of the dam in about one hour of walking.

Geographic entities mentioned:
surface_form: val camonica
instance_of: Valley
countries: Italy
coordinates: lat: 46.0075
lon: 10.3475
This system comprises Lake Pantano and, the two reservoirs at the highest elevation, and the two lakes in the mid-valley (Lake d'Avio and Lake Benedetto). However, the waters of the two highest lakes also feed a small power plant located on the shores of Lake Benedetto. Access.

Geographic entities mentioned:
surface_form: lake benedetto
instance_of: Lake
countries: Italy
coordinates: lat: 46.1856541
lon: 10.4703999
Lake Pantano d'Avio. The Lake Pantano d'Avio (or more briefly, &quot;Lake Pantano&quot;) is an artificial lake located in the upper, a lateral valley of the Val Camonica, in the Province of Brescia. Situated at 2,378 meters above sea level, it is the second largest lake in Val Camonica by surface area, after. Description.

Geographic entities mentioned:
surface_form: lake pantano d'avio
instance_of: Lake
countries: Italy
coordinates: lat: 46.165
lon: 10.47194
Alternatively, it is possible to reach the opposite end of the dam starting from the and, by following a section of the Alta Via dell'Adamello, arrive at the lake in forty-five minutes. However, this route includes a challenging section, the ascent and descent of the Bocchetta del Pantano or Passo del Lunedì (2,650 m), making it suitable only for experienced hikers.

Geographic entities mentioned:
surface_form: adamello
instance_of: Mountain
countries: Italy
coordinates: lat: 46.156
lon: 10.496388888889
It is important as a breeding site for seabirds, especially penguins. Description. The bay lies on the southern coast of Grande Terre, west of Mont Ross and Gallieni Massif, and encompassing the mouth of Fjord Larose and the tilted monolith known as the &quot;Doigt de Sainte Anne&quot; (Saint Anne's Finger). Important Bird Area.

Geographic entities mentioned:
surface_form: Mont Ross
instance_of: Mountain
countries: France
coordinates: lat: -49.6
lon: 69.5
Piz Rots. Piz Rots (also known as &quot;Vesilspitze&quot;) is a mountain of the Samnaun Alps, located on the Austria–Switzerland border. It lies south-west of Samnaun.

Geographic entities mentioned:
surface_form: piz rots
instance_of: Mountain
countries: Switzerland
Austria
coordinates: lat: 46.925194444444
lon: 10.315972222222
Piz Rots. Piz Rots (also known as &quot;Vesilspitze&quot;) is a mountain of the Samnaun Alps, located on the Austria–Switzerland border. It lies south-west of Samnaun.

Geographic entities mentioned:
surface_form: piz rots
instance_of: Mountain
countries: Switzerland
Austria
coordinates: lat: 46.925194444444
lon: 10.315972222222
surface_form: vesilspitze
instance_of: Mountain
countries: Switzerland
Austria
coordinates: lat: 46.925194444444
lon: 10.315972222222
Location. The Category 1 hut is situated in the Allgäu Alps in southern Germany, a few kilometres south of Oberstdorf on a grassy terrace near the lakes of Little and Great Rappensee. The most important summits in the vicinity are the Biberkopf and Hohes Licht. The well known Heilbronn Way begins and ends to the east and above the Rappensee Hut. History. The Rappensee Hut was built in 1885.

Geographic entities mentioned:
surface_form: Biberkopf
instance_of: Mountain
countries: Germany
Austria
coordinates: lat: 47.270527777778
lon: 10.232361111111
surface_form: Hohes Licht
instance_of: Mountain
countries: Austria
coordinates: lat: 47.2801709
lon: 10.2760287
At a second meeting on 28 January a planning committee was appointed, with representatives from the various municipalities in the area. It proposed three alternative routes for a railway: a continuation of the proposed Vestfold Line from Larvik, a railway down the valley of Lågendalen from Kongsberg, or a link from the Kongsberg–Drammen Line via Siljan to Skien.

Geographic entities mentioned:
surface_form: Lågendalen
instance_of: Valley
countries: Norway
The 2011 Census of India recorded a total of 1,684 residents in the village. Panchanadi is 1,202 hectares in size. The meaning of &quot;Panchanadi&quot; in Sanskrit literally translates to &quot;Five Rivers&quot;. References. Presently the village has been connected to the Kothari River due to the construction of a long bridge near the Arabian Sea.

Geographic entities mentioned:
surface_form: Kothari River
instance_of: Watercourse
countries: India
coordinates: lat: 25.3333333
lon: 75.0666667
The canal was taken into use in 1639, aimed to transport iron from the Central Swedish Mining District to Stockholm and further abroad. Plans to extend the canal west of Örebro to Lake Vänern and further to Göta älv were never realized (hilly area). Instead Göta Canal, located further south and taken into use in 1832, fulfilled the aimed function of connecting the Baltic with the North Sea.

Geographic entities mentioned:
surface_form: Vänern
instance_of: Lake
countries: Sweden
coordinates: lat: 58.916666666667
lon: 13.5
Cattle were driven to summer pastures in May and returned to lowlands in November, suggesting the festival's pastoral origins. Some Neolithic passage tombs in Ireland are aligned with the sunrise around the times of Samhain and Imbolc. These include the Mound of the Hostages (&quot;Dumha na nGiall&quot;) at the Hill of Tara, and Cairn L at Slieve na Calliagh. In Irish mythology.

Geographic entities mentioned:
surface_form: Slieve na Calliagh
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.744519444444
lon: -7.1116694444444
One Samhain, the young Fionn mac Cumhaill, stays awake and slays Aillen with a magical spear, for which he is made leader of the fianna. In a similar tale, one Samhain, the Otherworld being Cúldubh emerges from the burial mound on Slievenamon and snatches a roast pig. Fionn kills Cúldubh with a spear throw as he re-enters the mound.

Geographic entities mentioned:
surface_form: Slievenamon
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.43
lon: -7.563
He is warned of his impending doom by three undead horsemen who are messengers of Donn, the god of the dead. &quot;The Boyhood Deeds of Fionn&quot; tells how each Samhain the men of Ireland went to woo a beautiful maiden who lives in the fairy mound on Brí Éile (Croghan Hill). It says that each year someone would be killed &quot;to mark the occasion&quot;, by persons unknown.

Geographic entities mentioned:
surface_form: Brí Éile
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.2
lon: -7.16
Each Samhain, a host of otherworldly beings was said to emerge from the Cave of Cruachan in County Roscommon. The Hill of Ward (or Tlachtga) in County Meath is thought to have been the site of a great Samhain gathering and bonfire; the Iron Age ringfort is said to have been where the goddess or druid Tlachtga gave birth to triplets and where she later died.

Geographic entities mentioned:
surface_form: Hill of Ward
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.624
lon: -6.886
Surface characteristics. Most of the central edifice of Alba Mons is mantled with a layer of dust approximately thick. The dust layer is visible in high resolution images of the summit (pictured right). In places, the dust has been carved into streamlined shapes by the wind and is cut by small landslides. However, some isolated patches of dust appear smooth and undisturbed by the wind.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
Heavy dust cover is also indicated by the high albedo (reflectivity) and low thermal inertia of the region. Martian dust is visually bright (albedo > 0.27) and has a low thermal inertia because of its small grain size (<). (See the Martian surface.) However, the thermal inertia is high and albedo lower on the northern flanks of the volcano and in the apron area farther to the north.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7