Sarmila/GeoWiki-Features huggingface dataset:
The basement is formed by faulted granite and metamorphic rocks of the North Patagonian Batholith. The subduction of the Nazca Plate under the South American Plate gives rise to the volcanism of the Andes. In the southern sector between Yate and Cerro Hudson, where Huequi is located, the crust is thin and does not heavily influence the basaltic and basaltic andesite magmas.

Geographic entities mentioned:
surface_form: yate
instance_of: Mountain
countries: Chile
coordinates: lat: -41.754722222222
lon: -72.396388888889
surface_form: cerro hudson
instance_of: Mountain
countries: Chile
coordinates: lat: -45.92
lon: -72.95
surface_form: huequi
instance_of: Mountain
countries: Chile
coordinates: lat: -42.376666666667
lon: -72.578055555556
Huequi. Huequi () is a volcano in the Los Lagos Region of Chile. It is in the Southern Volcanic Zone, in the centre of Ayacara Peninsula and close to the Gulf of Ancud. It is made up of a lava dome complex situated in a depression of unclear origin, a postglacial lava dome Calle and a Pleistocene volcano with Holocene parasitic cones, with a sharp summit at.

Geographic entities mentioned:
surface_form: huequi
instance_of: Mountain
countries: Chile
coordinates: lat: -42.376666666667
lon: -72.578055555556
There are only a few villages along the coast, and little human modification of the environment. Huequi lies roughly at the centre of the Ayacara Peninsula east of the Gulf of Ancud. Huequi is part of the Southern Volcanic Zone (SVZ), lying in its southern sector between the volcanoes Hornopiren and Chaiten-Minchinmavida; Chaiten erupted in 2008.

Geographic entities mentioned:
surface_form: huequi
instance_of: Mountain
countries: Chile
coordinates: lat: -42.376666666667
lon: -72.578055555556
A partially collapsed dome forms the summit. A summit crater was reported as &quot;narrow&quot; in 1909 and as wide by the Global Volcanism Program. Debris avalanches, partly channelled by a northwestward trending valley in the edifice, have formed a fan on that side of Huequi. Pumice from the volcano has been carried to the sea by the Huequi River, which originates at the foot of Huequi.

Geographic entities mentioned:
surface_form: huequi
instance_of: Mountain
countries: Chile
coordinates: lat: -42.376666666667
lon: -72.578055555556
Debris avalanches, partly channelled by a northwestward trending valley in the edifice, have formed a fan on that side of Huequi. Pumice from the volcano has been carried to the sea by the Huequi River, which originates at the foot of Huequi. Two additional cones are named Porcelana and Barranes Colorado or Barranco Colorado; there is also the Calle postglacial lava dome.

Geographic entities mentioned:
surface_form: huequi
instance_of: Mountain
countries: Chile
coordinates: lat: -42.376666666667
lon: -72.578055555556
surface_form: huequi
instance_of: Mountain
countries: Chile
coordinates: lat: -42.376666666667
lon: -72.578055555556
The main phenocryst phase is plagioclase, followed by orthopyroxene and hornblende. The lava domes contain columnar forms exposed in cliffs and dense porphyries. Compared to other volcanoes in this sector of the Southern Volcanic Zone, Huequi's magmas are water-rich. This may explain some peculiarities about its eruptive activity, as the water escapes from the magma and leaves a viscous andesite.

Geographic entities mentioned:
surface_form: huequi
instance_of: Mountain
countries: Chile
coordinates: lat: -42.376666666667
lon: -72.578055555556
The summit dome may have formed during this sequence. The volcano was reportedly &quot;smoking&quot; in 1935. Porcelana geyser and Porcelana hot spring lie on the Ayacara Peninsula and are associated with Huequi. The Porcelana geysers have produced pinnacles of travertine reaching heights of; this extreme size in a highly erosive environment may be due to microbial chemical processes.

Geographic entities mentioned:
surface_form: huequi
instance_of: Mountain
countries: Chile
coordinates: lat: -42.376666666667
lon: -72.578055555556
Composition. Huequi has erupted andesite and basaltic andesite, which have grey and red colours and feature both layered and brecciated sequences. Dacite has also been reported. The volcanic rocks define a calc-alkaline suite that resembles the adakites of Nevado de Longavi. The main phenocryst phase is plagioclase, followed by orthopyroxene and hornblende.

Geographic entities mentioned:
surface_form: nevado de longavi
instance_of: Mountain
countries: Chile
coordinates: lat: -36.193055555556
lon: -71.160833333333
Berard Beach. Berard Beach is an unincorporated community on the eastern shore of Wakaw Lake in the RM of Hoodoo No. 401, Saskatchewan, Canada. The community is located about north of Highway 41 and approximately east of the town of Wakaw.

Geographic entities mentioned:
surface_form: Wakaw Lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.6667
lon: -105.583
Eching am Ammersee. Eching am Ammersee (,) is a municipality in the district of Landsberg in Bavaria in Germany. It has a size of 6.15km2. Situated at the northern shore of the Ammersee at an elevation of 541m, it borders the Naturschutzgebiet &quot;Ampermoos&quot; and the wooded recreation area &quot;Weingarten&quot;. History.

Geographic entities mentioned:
surface_form: Ammersee
instance_of: Lake
countries: Germany
coordinates: lat: 48
lon: 11.116666666667
Tourism. There are many scenic spots in Mimaropa. Some of them are the Bathala Cave, Balanacan Bay, and Tres Reyes Islands in the province of Marinduque; White Island in Mindoro; Fort San Andres, Mount Guiting-Guiting, and Bonbon Beach in Romblon; and the Puerto Princesa Subterranean River National Park and El Nido Marine Reserve Park in Palawan. Provinces.

Geographic entities mentioned:
surface_form: Mount Guiting-Guiting
instance_of: Mountain
countries: Philippines
coordinates: lat: 12.413888888889
lon: 122.56777777778
On 24 and 25 October 1917 the I. Corps broke through the Italian front at Flitsch and reached the new front section at Feltre and Monte Grappa, where the new &quot;Belluno Corps Group&quot; was established. General Krauss took over the supreme command of the Austro-Hungarian Eastern Army on 16 May 1918, and was also in command of the occupied territories in Ukraine.

Geographic entities mentioned:
surface_form: Monte Grappa
instance_of: Mountain
countries: Italy
coordinates: lat: 45.873333333333
lon: 11.799166666667
Mount Denjō. is a 　mountain of Chushin Highland, located in Nagawa, Nagano. This mountain is a part of the Yatsugatake-Chūshin Kōgen Quasi-National Park. Leisure. On Mount Denjō, there is Echo Valley Ski Resort. Route. There are several routes to the top of the mountain. The easiest route is to climb from Himekidaira. Other routes are from Mount Kuruma or Mount Ōsasa.

Geographic entities mentioned:
surface_form: Mount Ōsasa
instance_of: Mountain
countries: Japan
coordinates: lat: 36.116666666667
lon: 138.18333333333
Mount Denjō. is a 　mountain of Chushin Highland, located in Nagawa, Nagano. This mountain is a part of the Yatsugatake-Chūshin Kōgen Quasi-National Park. Leisure. On Mount Denjō, there is Echo Valley Ski Resort. Route. There are several routes to the top of the mountain. The easiest route is to climb from Himekidaira. Other routes are from Mount Kuruma or Mount Ōsasa.

Geographic entities mentioned:
surface_form: mount denjō
instance_of: Mountain
countries: Japan
coordinates: lat: 36.114444444444445
lon: 138.20519444444443
At least several miles of the journey were undertaken under conditions of heavy snow. The Indian Powerplus motorcycle Steinhart rode was able to make better progress than a man leading a horse that he passed. On January 1, 1917 Steinhart finished first among ten riders in a 180-mile course twice around Lake Washington in a time of 3 hours, 20 minutes.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
It has a surface elevation of. Overview. The lake is located at the northern end of the endorheic Altiplano basin high in the Andes on the border of Peru and Bolivia. The western part of the lake lies within the Puno Region of Peru, and the eastern side is located in the Bolivian La Paz Department.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
The lake has 41 islands, some of which are densely populated. Having only a single season of free circulation, the lake is monomictic, and water passes through Lago Huiñaimarca and flows out the single outlet at the Río Desaguadero, which then flows south through Bolivia to Lake Poopó. This only accounts for about 10% of the lake's water balance.

Geographic entities mentioned:
surface_form: Lake Poopó
instance_of: Lake
countries: Bolivia
coordinates: lat: -18.781944444444
lon: -67.024722222222
That claim is generally considered to refer to commercial craft. Numerous smaller lakes around the world are at higher elevations, such as the crater lake of Ojos del Salado, which at an elevation of is the overall highest lake in the world, and the Lake Puma Yumco, which at an elevation of is the highest large lake in the world.

Geographic entities mentioned:
surface_form: Ojos del Salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
Within the northern Altiplano (Tinajani Basin), these prehistoric lakes were Lake Mataro at an elevation of, Lake Cabana at an elevation of, Lake Ballivián at an elevation of, Lake (North) Minchin at an elevation of, and Lake (North) Tauca at an elevation. The age of Lake Mataro is uncertain—it may date back to the Late Pliocene. Lake Cabana possibly dates to the Middle Pleistocene.

Geographic entities mentioned:
surface_form: Lake Ballivián
instance_of: Lake
countries: Bolivia
surface_form: Lake (North) Tauca
instance_of: Lake
countries: Peru
coordinates: lat: -20
lon: -68
Lake Ballivián existed between 120,000 and 98,000 BP. Two high lake stands, between 72,000 and 68,000 BP and 44,000–34,000 BP, have been discerned for Lake Minchin within the Altiplano. Another ancient lake in the area is Ouki. The high lake levels of Lake Tauca have been dated as having occurred between 18,100 and 14,100 BP. Underwater archaeology.

Geographic entities mentioned:
surface_form: Lake Tauca
instance_of: Lake
countries: Peru
coordinates: lat: -20
lon: -68
Lake Titicaca. Lake Titicaca (;; and) is a large freshwater lake in the Andes mountains on the border of Bolivia and Peru. It is often called the highest navigable lake in the world. Titicaca is the largest lake in South America, both in terms of the volume of water and surface area. It has a surface elevation of. Overview.

Geographic entities mentioned:
surface_form: lake titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
In 2012, the GNF nominated the lake &quot;Threatened Lake of the Year&quot;. Name. Given the various Indigenous groups that occupied the Lake Titicaca region, it likely lacked a single, commonly accepted name in prehistoric times and at the time the Spaniards arrived. The terms &quot;titi&quot; and &quot;caca&quot; can be translated in several ways.

Geographic entities mentioned:
surface_form: lake titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
This name can be loosely translated as lance point. This name survives in modern usage in which the large lake is occasionally referred to as &quot;Lago Chucuito.&quot;
Stanish argues that the logical explanation for the origin of the name Titicaca is a corruption of the term &quot;thakhsi cala,&quot; which is the 15th- to the 16th-century name of the sacred rock on the Isla del Sol.

Geographic entities mentioned:
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
The Titicaca orestias has likely become extinct (last seen in 1938) due to competition and predation by the introduced rainbow trout and the silverside &quot;Odontesthes bonariensis&quot;. In addition to the Titicaca orestias, native fish species in the lake's basin are other species of &quot;Orestias&quot;, and the catfish &quot;Trichomycterus dispar&quot;, &quot;T.

Geographic entities mentioned:
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
Titicaca is home to 24 described species of freshwater snails (15 endemics, including several tiny &quot;Heleobia&quot; spp.) and less than half a dozen bivalves (all in family Sphaeriidae), but in general these are very poorly known and their taxonomy is in need of a review.

Geographic entities mentioned:
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
The lake also has an endemic species flock of amphipods consisting of 11 &quot;Hyalella&quot; (an additional Titicaca &quot;Hyalella&quot; species is nonendemic). Reeds and other aquatic vegetation are widespread in Lake Titicaca. Totora sedges grow in water shallower than, less frequently to, but macrophytes, notably &quot;Chara&quot; and &quot;Potamogeton&quot;, occur down to.

Geographic entities mentioned:
surface_form: lake titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
They lie upon an angular unconformity which cuts across pre-basin strata. Lacustrine sediments of the Lower Tinajani Formation, which are exposed within the Tinajani Basin, demonstrate the presence of a pre-Quaternary, ancestral Lake Titicaca within it between 18 and 14 million years ago (Mya).

Geographic entities mentioned:
surface_form: lake titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
surface_form: lake titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
surface_form: lake titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
Little is known about the prehistory of Lake Titicaca between 14 Mya and 370,000 BP because the lake sediments dating to this period lie buried beneath the bottom of Lake Titicaca and have not yet been sampled by continuous coring.

Geographic entities mentioned:
surface_form: lake titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
surface_form: lake titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
The Lake Titicaca drilling project recovered a 136-m-long drill core of sediments from the bottom of Lake Titicaca at a depth of and at a location just east of Isla del Sol. This core contains a continuous record of lake sedimentation and paleoenvironmental conditions for Lake Titicaca back to about 370,000 BP.

Geographic entities mentioned:
surface_form: lake titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
Uros. The &quot;Floating Islands&quot; are small, human-made islands constructed by the Uros (or Uru) people from layers of cut totora, a thick, buoyant sedge that grows abundantly in the shallows of Lake Titicaca. The Uros harvest the sedges that naturally grow on the lake's banks to make the islands by continuously adding sedges to the surface.

Geographic entities mentioned:
surface_form: lake titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
Historically, most of the Uros islands were located near the middle of the lake, about from the shore; however, in 1986, after a major storm devastated the islands, many Uros rebuilt closer to shore., about 1,200 Uros lived on an archipelago of 60 artificial islands, clustering in the western corner of the lake near Puno, Titicaca's major Peruvian port town.

Geographic entities mentioned:
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
Lake Titicaca. Lake Titicaca (;; and) is a large freshwater lake in the Andes mountains on the border of Bolivia and Peru. It is often called the highest navigable lake in the world. Titicaca is the largest lake in South America, both in terms of the volume of water and surface area. It has a surface elevation of. Overview.

Geographic entities mentioned:
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
The smaller subbasin, Wiñaymarka (also called &quot;Lago Pequeño&quot;, &quot;little lake&quot;), has an average depth of and a maximum depth of. The overall average depth of the lake is. Five major river systems feed into Lake Titicaca. In order of their relative flow volumes, these are Ramis, Coata, Ilave, Huancané, and Suchez. More than 20 other smaller streams empty into Titicaca.

Geographic entities mentioned:
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
The overall average depth of the lake is. Five major river systems feed into Lake Titicaca. In order of their relative flow volumes, these are Ramis, Coata, Ilave, Huancané, and Suchez. More than 20 other smaller streams empty into Titicaca. The lake has 41 islands, some of which are densely populated.

Geographic entities mentioned:
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
Between April and November 2009 alone, the water level dropped by, reaching the lowest level since 1949. This drop is caused by shortened rainy seasons and the melting of glaciers feeding the tributaries of the lake. Water pollution is also an increasing concern because cities in the Titicaca watershed grow, sometimes outpacing solid waste and sewage treatment infrastructure.

Geographic entities mentioned:
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
Water pollution is also an increasing concern because cities in the Titicaca watershed grow, sometimes outpacing solid waste and sewage treatment infrastructure. According to the Global Nature Fund (GNF), Titicaca's biodiversity is threatened by water pollution and the introduction of new species by humans.

Geographic entities mentioned:
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
Given the lack of a common name for Lake Titicaca in the 16th century, the Spaniards are thought to have used the name of the site of the most important indigenous shrine in the region, &quot;thakhsi cala&quot; on the Isla del Sol, as the name for the lake. In time and with usage, this name developed into &quot;Titicaca.&quot;
Locally, the lake goes by several names.

Geographic entities mentioned:
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
It has also been designated an Important Bird Area (IBA), in both Bolivia and Peru, by BirdLife International because it supports significant populations of many bird species. Several threatened species such as the huge Titicaca water frog and the flightless Titicaca grebe are largely or entirely restricted to the lake.

Geographic entities mentioned:
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
In addition to the threatened Titicaca grebe, some of the birds associated with water at Titicaca are the white-tufted grebe, Puna ibis, Chilean flamingo, Andean gull, Andean lapwing, white-backed stilt, greater yellowlegs, snowy egret, black-crowned night-heron, Andean coot, common gallinule, plumbeous rail, various ducks, wren-like rushbird, many-colored rush-tyrant, and yellow-winged blackbird.

Geographic entities mentioned:
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
surface_form: titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
Khoton Lake. Khoton Lake (Mongolian: Хотон нуур [qotuŋ naɣur],) is a freshwater lake in Altai Tavan Bogd National Park in Tsengel District, Bayan-Ölgii Province, western Mongolia. Geography. It lies at the foot of the Altai Mountains near the Chinese border, at an elevation of about above sea level. It is fed by the Khuiten River from the east and other rivers from the north.

Geographic entities mentioned:
surface_form: хотон нуур
instance_of: Lake
countries: Mongolia
coordinates: lat: 48.65
lon: 88.3
surface_form: khoton lake
instance_of: Lake
countries: Mongolia
coordinates: lat: 48.65
lon: 88.3
Khoton Lake. Khoton Lake (Mongolian: Хотон нуур [qotuŋ naɣur],) is a freshwater lake in Altai Tavan Bogd National Park in Tsengel District, Bayan-Ölgii Province, western Mongolia. Geography. It lies at the foot of the Altai Mountains near the Chinese border, at an elevation of about above sea level. It is fed by the Khuiten River from the east and other rivers from the north.

Geographic entities mentioned:
surface_form: khoton lake
instance_of: Lake
countries: Mongolia
coordinates: lat: 48.65
lon: 88.3
History. Valders was settled in the 1850s by immigrants from the Valdres mountainous region of Norway. The largest town in Valdres is Fagernes, but many immigrants arriving in Wisconsin came from the valleys of Vestre Slidre and Øystre Slidre, when hunger (&quot;sult&quot;) in these rocky hillside farms was far from unheard of.

Geographic entities mentioned:
surface_form: Valdres
instance_of: Valley
countries: Norway
coordinates: lat: 60.916666666667
lon: 9.1666666666667
Geography. Valders is located on U.S. Route 151 two miles east of the Manitowoc River. The city of Manitowoc lies ten miles to the east on Lake Michigan. According to the United States Census Bureau, the village has a total area of, all of it land. 2010 census. As of the census of 2010, there were 962 people, 406 households, and 272 families living in the village. The population density was.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Monte San Primo. Monte San Primo is a mountain of Lombardy, Italy. It is high and belongs to the province of Como. The mountain offers scenic views and is a popular destination for hiking and outdoor activities.

Geographic entities mentioned:
surface_form: monte san primo
instance_of: Mountain
countries: Italy
coordinates: lat: 45.91666667
lon: 9.20888889
This means that the hills to the north of Helensburgh lie in the Highlands, whereas the land to the south of Helensburgh is in the Lowlands or Central Belt of Scotland. Consequently, there is a wide variety of landscape in the surrounding area – for example, Loch Lomond (part of Scotland's first National Park) is only over the hill to the north-east of Helensburgh.

Geographic entities mentioned:
surface_form: Loch Lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
In the town itself there are footpaths inside the Duchess Woods, Argyll & Bute's only local nature reserve. A longer footpath is the Three Lochs Way which connects Loch Lomond with Helensburgh, the Gareloch and Loch Long, and which runs for 34 miles (55 km). The longest by far of all the walks with a local start is the John Muir Way.

Geographic entities mentioned:
surface_form: Loch Lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
Le Monde writes, &quot;We follow him, recovering hidden memory, rediscovering the city of Poughkeepsie, in the Hudson Valley, where his father worked for IBM, attracted by the myth of America and the great computer utopia of the 1970s.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
It is part of the southern Chain of Lakes. With a surface area, it is one of the larger lakes in Polk County, Florida. Lake Eloise has a somewhat oval shape and has a large cove on its south side. It borders Lake Summit on its northeast and it almost borders Lake Lulu on its northwest. Lake Eloise is mostly surrounded by residential areas.

Geographic entities mentioned:
surface_form: Lake Summit
instance_of: Lake
countries: United States
coordinates: lat: 27.9988
lon: -81.6948
surface_form: Lake Lulu
instance_of: Lake
countries: United States
coordinates: lat: 27.9964
lon: -81.7209
There is no public access from the shore, as all shoreline is on private property. The public can access the lake by boat via the Chain of Lakes canal system. Lake Eloise is linked by canal directly to Lake Lulu, Lake Summit and Lake Winterset. The nearest public boat ramp is on Lake Summit and the canal system links Lake Eloise to a number of area lakes. Fishing is allowed from boats.

Geographic entities mentioned:
surface_form: Lake Lulu
instance_of: Lake
countries: United States
coordinates: lat: 27.9964
lon: -81.7209
surface_form: Lake Summit
instance_of: Lake
countries: United States
coordinates: lat: 27.9988
lon: -81.6948
surface_form: Lake Winterset
instance_of: Lake
countries: United States
coordinates: lat: 27.9745
lon: -81.682
surface_form: lake summit
instance_of: Lake
countries: United States
coordinates: lat: 27.9988
lon: -81.6948
surface_form: lake lulu
instance_of: Lake
countries: United States
coordinates: lat: 27.9964
lon: -81.7209
surface_form: lake winterset
instance_of: Lake
countries: United States
coordinates: lat: 27.9745
lon: -81.682
The public can access the lake by boat via the Chain of Lakes canal system. Lake Eloise is linked by canal directly to Lake Lulu, Lake Summit and Lake Winterset. The nearest public boat ramp is on Lake Summit and the canal system links Lake Eloise to a number of area lakes. Fishing is allowed from boats. As there is no shore access, there are no public swimming areas.

Geographic entities mentioned:
surface_form: lake summit
instance_of: Lake
countries: United States
coordinates: lat: 27.9988
lon: -81.6948
surface_form: lake eloise
instance_of: Lake
countries: United States
coordinates: lat: 27.9836
lon: -81.704
Lake Eloise. Lake Eloise is a large natural freshwater lake on the south side of Winter Haven, Florida. It is part of the southern Chain of Lakes. With a surface area, it is one of the larger lakes in Polk County, Florida. Lake Eloise has a somewhat oval shape and has a large cove on its south side. It borders Lake Summit on its northeast and it almost borders Lake Lulu on its northwest.

Geographic entities mentioned:
surface_form: lake eloise
instance_of: Lake
countries: United States
coordinates: lat: 27.9836
lon: -81.704
It is part of the southern Chain of Lakes. With a surface area, it is one of the larger lakes in Polk County, Florida. Lake Eloise has a somewhat oval shape and has a large cove on its south side. It borders Lake Summit on its northeast and it almost borders Lake Lulu on its northwest. Lake Eloise is mostly surrounded by residential areas.

Geographic entities mentioned:
surface_form: lake eloise
instance_of: Lake
countries: United States
coordinates: lat: 27.9836
lon: -81.704
Lake Eloise has a somewhat oval shape and has a large cove on its south side. It borders Lake Summit on its northeast and it almost borders Lake Lulu on its northwest. Lake Eloise is mostly surrounded by residential areas. However, the northern half of its eastern shore is occupied by Legoland Florida, which was once Cypress Gardens, a large area theme park.

Geographic entities mentioned:
surface_form: lake eloise
instance_of: Lake
countries: United States
coordinates: lat: 27.9836
lon: -81.704
Some citrus groves border the lake on its west side. Eloise Loop Road passes by the south end of the cove on the lake's south side. Lake Eloise was first surveyed in 1849, by Dr John Westcott. He named the lake after Eloise Moody, daughter of Polk County pioneer Benjamin F. Moody. The lake appears in the first U.S. Government survey of the area, published in 1950.

Geographic entities mentioned:
surface_form: lake eloise
instance_of: Lake
countries: United States
coordinates: lat: 27.9836
lon: -81.704
Moody. The lake appears in the first U.S. Government survey of the area, published in 1950. Cypress Gardens opened in 1936 and soon had various attractions, including ones that had a connection to Lake Eloise. In the 1930s the park had water shows with water ski performances. Two grandstands were constructed to allow spectators to see the shows.

Geographic entities mentioned:
surface_form: lake eloise
instance_of: Lake
countries: United States
coordinates: lat: 27.9836
lon: -81.704
A large decorative pool in the shape of Florida was constructed just on shore and in the western edge of the botanical garden. Also, a large paddle boat was refurbished and dubbed the &quot;Cypress Belle&quot;. The &quot;Cypress Belle&quot; allowed park visitors to cruise on Lake Eloise. Also, at times the &quot;Belle&quot; was used for dinner cruises.

Geographic entities mentioned:
surface_form: lake eloise
instance_of: Lake
countries: United States
coordinates: lat: 27.9836
lon: -81.704
The &quot;Cypress Belle&quot; allowed park visitors to cruise on Lake Eloise. Also, at times the &quot;Belle&quot; was used for dinner cruises. Through the years various television shows and movies filmed at Cypress Gardens and many times filming made use of Lake Eloise. After 2000 Cypress Gardens went through various major changes to maintain its visitor base and finally closed in fall 2009.

Geographic entities mentioned:
surface_form: lake eloise
instance_of: Lake
countries: United States
coordinates: lat: 27.9836
lon: -81.704
Although Lake Eloise is a large lake, there is very little public access to it. There is no public access from the shore, as all shoreline is on private property. The public can access the lake by boat via the Chain of Lakes canal system. Lake Eloise is linked by canal directly to Lake Lulu, Lake Summit and Lake Winterset.

Geographic entities mentioned:
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
Lake Eloise. Lake Eloise is a large natural freshwater lake on the south side of Winter Haven, Florida. It is part of the southern Chain of Lakes. With a surface area, it is one of the larger lakes in Polk County, Florida. Lake Eloise has a somewhat oval shape and has a large cove on its south side. It borders Lake Summit on its northeast and it almost borders Lake Lulu on its northwest.

Geographic entities mentioned:
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
Lilaea (ancient city). Lilaea or Lilaia (), also Lilaeum or Lilaion (Λίλαιον), was one of the most important ancient Phocian towns, and a polis (city-state), built on the north slopes of Mount Parnassus, and at the sources of the Cephissus. Description.

Geographic entities mentioned:
surface_form: Mount Parnassus
instance_of: Mountain
countries: Greece
coordinates: lat: 38.533
lon: 22.6167
It is part of the Hauran plains which extend from southern Syria to the north of Jordan. From Johfiyeh, one can see the disputed Jordanian, Syrian and Israeli triangle of borders (tripoint). In winter, Mount Hermon, which is located in Lebanon and Syria, can be seen clearly. Topography. Johfiyeh lies on a plateau elevated around 750 to 793 meters above sea level.

Geographic entities mentioned:
surface_form: Mount Hermon
instance_of: Mountain
countries: Lebanon
Israel
Syria
coordinates: lat: 33.4
lon: 35.85
It is popular among the tourists for its natural environment and scenery. The village is a base camp for trekkers to the Kolahoi Glacier, the Tarsar–Marsar lakes and the Katrinag valley. It is also a base for the treks to Lidderwat, the Vishansar–Kishansar lakes and Kangan. The Kolahoi is the largest glacier in the Kashmir Valley, and is located near Mt.

Geographic entities mentioned:
surface_form: Kishansar
instance_of: Lake
countries: India
coordinates: lat: 34.39694444444444
lon: 75.1025
The city of Anouvong district is Ban Muang Cha (pronounced Ja from Ja river). It is home to Chao Anouvong cave, which is part of Phou Houa Xang Village, as well as the Phou Bia peak tourist site
History. On December 13, 2013, Xaisomboun was proclaimed the 18th province of Laos by the Lao People's Democratic Republic government.

Geographic entities mentioned:
surface_form: Phou Bia
instance_of: Mountain
countries: Laos
coordinates: lat: 18.983333333333
lon: 103.13333333333
From there, the capital is therefore called in the name of King Anouvong. This city currently extends over the region of the village (Ban) of Muang Cha (Ja, Ja river) and other small villages in the surroundings. In 2021, the authorities of Xaisomboun province approved a budget estimated at approximately USA $500 million for the development of Phou Bia Mountain.

Geographic entities mentioned:
surface_form: Phou Bia
instance_of: Mountain
countries: Laos
coordinates: lat: 18.983333333333
lon: 103.13333333333
Joukamojärvi. Joukamojärvi is a medium-sized lake in the Koutajoki main catchment area. It is located in Kuusamo municipality, in the region Northern Ostrobothnia in Finland.

Geographic entities mentioned:
surface_form: joukamojärvi
instance_of: Lake
countries: Finland
coordinates: lat: 65.85
lon: 29.9
At this remote post they perform four times in front-line dugouts for the small groups of soldiers manning them. They return to Milan, and are next booked in Verona. Their contract with Ivaldi ends, and they detour to visit a friend in Porto Cannero on Lake Maggiore before returning to the United Kingdom. Their next gig is another Army Welfare tour with stops in Berlin, Hanover and Minden.

Geographic entities mentioned:
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
Father Clancy was enthusiastically involved in the life of the town, local committees and governing bodies. He was instrumental in the changing of Geraldton's name to Innisfail in 1910. He also advocated for forging a link to the Atherton Tableland and the use of Mourilyan Harbour by shipping. Mount Father Clancy Garreth McGonnell near the Beatrice River was named in his honour. Early life.

Geographic entities mentioned:
surface_form: Atherton Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
The following days, preliminary results from DNA testing came back with matches to Simpson but the District Attorney delayed filing charges until all the results had come back. Simpson spent the night between June 16 and 17 at the San Fernando Valley home of friend Robert Kardashian; Shapiro asked several doctors to attend to Simpson's purported fragile mental state.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
In late February 2018, URC finally took possession of the concession assets and resumed operating the metre-gauge railway system in Uganda. Train ferries. URC operated three international train ferries on Lake Victoria:, and. On 8 May 2005, however, &quot;Kabalega&quot; and &quot;Kaawa&quot; collided almost head-on.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Baiyu Mountain. Baiyu Mountain () is a mountain in the urban area of Lüshunkou District, Dalian, Liaoning, China. It is located near the center of the urban area, with an altitude of 130 meters. Name. Baiyu Mountain was formerly known as Xiguan Mountain (西官山).

Geographic entities mentioned:
surface_form: baiyu mountain
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 38.81083333
lon: 121.25719444
Baiyu Mountain () is a mountain in the urban area of Lüshunkou District, Dalian, Liaoning, China. It is located near the center of the urban area, with an altitude of 130 meters. Name. Baiyu Mountain was formerly known as Xiguan Mountain (西官山). During the Self-Strengthening Movement in the late Qing Dynasty was built the Beiyang Fleet's Lüshun Naval Base in the bay at the foot of this mountain.

Geographic entities mentioned:
surface_form: baiyu mountain
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 38.81083333
lon: 121.25719444
In 1880, Li Hongzhang (李鴻章) inspected Lüshun Port and climbed to the top of the mountain with Yixuan, Prince Chun, the father of Emperor Guangxu. When they learned that the opposite mountain was called Gold Mountain, they said that, where there is gold, there must be white jade, so it was renamed Baiyu Mountain.

Geographic entities mentioned:
surface_form: baiyu mountain
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 38.81083333
lon: 121.25719444
When they learned that the opposite mountain was called Gold Mountain, they said that, where there is gold, there must be white jade, so it was renamed Baiyu Mountain. There is another saying that the mountain got its name from the white terrain like jade in the early years. In 1995, Baiyu Mountain was named as Dalian City's Patriotic Education Base. Baiyu Mountain Tower.

Geographic entities mentioned:
surface_form: baiyu mountain
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 38.81083333
lon: 121.25719444
There is another saying that the mountain got its name from the white terrain like jade in the early years. In 1995, Baiyu Mountain was named as Dalian City's Patriotic Education Base. Baiyu Mountain Tower. The Baiyu Mountain Tower is located on the top of Baiyu Mountain.

Geographic entities mentioned:
surface_form: baiyu mountain
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 38.81083333
lon: 121.25719444
In 1995, Baiyu Mountain was named as Dalian City's Patriotic Education Base. Baiyu Mountain Tower. The Baiyu Mountain Tower is located on the top of Baiyu Mountain. It was built in 1909 by the Japanese after the Russo-Japanese War to commemorate the Japanese officers and soldiers who had died in Lüshun.

Geographic entities mentioned:
surface_form: baiyu mountain
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 38.81083333
lon: 121.25719444
surface_form: baiyu mountain
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 38.81083333
lon: 121.25719444
He opened and designed Island Company stores in Nantucket, Naples Florida, Palm Beach, FL, Grand Cayman, Harbour Island, Bahamas, Martha’s Vineyard, a concept store inside the Ritz Carlton Ft Lauderdale, East Hampton, NY,
In March, 2013 he launched Island Company's first concept store, &quot;Escape Travel Live&quot; at Atlantis Paradise Island, Bahamas.

Geographic entities mentioned:
surface_form: Lauderdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.73
lon: -2.74889
Geography. Shivajinagar is situated on the West bank of the Mutha river with the older parts of Pune on the east side of the river. The area is surrounded on its Western side by the Vetal and Hanuman Hills. The village deity (Gramdaivat) is the temple of Rokdoba (God Hanuman) in Shivajinagar Gaothan. The Gaothan also has a temple of God Shri Ram. Transport.

Geographic entities mentioned:
surface_form: Vetal
instance_of: Mountain
countries: India
coordinates: lat: 18.5253
lon: 73.8153
Bjørnøy (Larvik). Bjørnøya is an island in Larvik Municipality in Vestfold county, Norway. The island lies within the large lake Farris. It is the largest island on the lake. It is located just east of the village of Kjose. The island's highest peak, in the center of the island, rises to the altitude of. A few other peaks on the island have a height of over.

Geographic entities mentioned:
surface_form: Farris
instance_of: Lake
countries: Norway
coordinates: lat: 59.166388888889
lon: 9.8766666666667
This war ended with the Peace of Požarevac on 21 June 1718. With this peace, the Venetians received Grbalj, Maine, Pobore and Brajići in Boka Kotorska, as well as Krivošije, Ledenice and Uble, which had previously belonged to Montenegro. The Montenegrins were reluctant to see this, and Metropolitan Danilo constantly tried to undermine Venetian rule in these places.

Geographic entities mentioned:
surface_form: Krivošije
instance_of: Landform
countries: Montenegro
coordinates: lat: 42.55
lon: 18.65
Under this model, the rocks dating to 3.8 Ga solidified only after much of the crust was destroyed by the LHB. Collectively, the Acasta Gneiss in the North American cratonic shield and the gneisses within the Jack Hills portion of the Narryer Gneiss Terrane in Western Australia are the oldest continental fragments on Earth, yet they appear to post-date the LHB.

Geographic entities mentioned:
surface_form: Jack Hills
instance_of: Mountain
countries: Australia
coordinates: lat: -26.1167
lon: 117.15
A dry valley continues in the same direction beyond the sinks and, as it crosses the Millstone Grit outcrop, gradually acquires a stream which is joined by others to become the lower Giedd. This separate river flows for about 6 km / 4 miles, passing the small village of Cwmgiedd, to its confluence with the River Tawe at Ystradgynlais in the Swansea Valley.

Geographic entities mentioned:
surface_form: Swansea Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.7593
lon: -3.7898
The middle of the lake has a maximum depth of a little over. The water of the lake is salty and bitter. Although it is not much smaller, the lake is also known as &quot;Little Kak&quot; in order to differentiate it from Kak (Ulken Kak) lake located to the WSW in the same district. The Sergeyev Dam lies to the east and lake Zhaltyr to the northeast. Fauna.

Geographic entities mentioned:
surface_form: zhaltyr
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 51.62861111111111
lon: 78.26083333333334
surface_form: zhaltyr
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 53.97938
lon: 67.266236
The middle of the lake has a maximum depth of a little over. The water of the lake is salty and bitter. Although it is not much smaller, the lake is also known as &quot;Little Kak&quot; in order to differentiate it from Kak (Ulken Kak) lake located to the WSW in the same district. The Sergeyev Dam lies to the east and lake Zhaltyr to the northeast. Fauna.

Geographic entities mentioned:
surface_form: kak (ulken kak)
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 53.582111111111
lon: 66.213
Kak (Kishi Kak). Kak (;), also known as Kishi Kak (), is a salt lake in Timiryazev District, North Kazakhstan Region, Kazakhstan. The lake lies to the WSW of Sergeyev town. Timiryazevo town, the administrative center of the district, lies to the west of the lake. Geography.

Geographic entities mentioned:
surface_form: kak (kishi kak)
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 53.7641
lon: 66.823
Mount Musgrave. Mount Musgrave is a mountain located in western Newfoundland, near the southern side of the Humber River valley at Steady Brook, approximately east of Corner Brook. The peak is named in honour of Sir Anthony Musgrave, a colonial governor of Newfoundland.

Geographic entities mentioned:
surface_form: mount musgrave
instance_of: Mountain
countries: Canada
coordinates: lat: 48.93
lon: -57.8339
Mount Musgrave. Mount Musgrave is a mountain located in western Newfoundland, near the southern side of the Humber River valley at Steady Brook, approximately east of Corner Brook. The peak is named in honour of Sir Anthony Musgrave, a colonial governor of Newfoundland.

Geographic entities mentioned:
surface_form: mount musgrave
instance_of: Mountain
countries: Canada
coordinates: lat: 48.93
lon: -57.8339
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The peak is named in honour of Sir Anthony Musgrave, a colonial governor of Newfoundland. The steep ridges that form part of the northern side of the mountain are the location of Marble Mountain Ski Resort, the largest alpine ski resort in Atlantic Canada.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The steep ridges that form part of the northern side of the mountain are the location of Marble Mountain Ski Resort, the largest alpine ski resort in Atlantic Canada. The summit of the mountain hosts Environment Canada's doppler weather radar station &quot;XME&quot;, part of the Canadian weather radar network.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
It is reported that each Hawaiian island has at least one leaping place. According to natives of the land, the entrance located in Waipio Valley has since been covered in sand and is now hidden from the sight of upper areas. Another documented area where souls enter the next world is Leina Kauhane. The spirits of the dead can watch what the living do and turn them to stone by staring at them.

Geographic entities mentioned:
surface_form: Waipio Valley
instance_of: Valley
countries: United States
coordinates: lat: 20.1197
lon: -155.593
Uchku Mach'ay. Uchku Mach'ay (Quechua &quot;uchku&quot; hole, &quot;mach'ay&quot; cave, &quot;hole cave&quot;, also spelled &quot;Uchcomachay&quot;) is a mountain in the Andes of Peru which reaches a height of approximately. It lies in the Junín Region, Tarma Province, Tarma District.

Geographic entities mentioned:
surface_form: uchku
instance_of: Mountain
countries: Peru
coordinates: lat: -12.38472222
lon: -75.70138889
surface_form: uchku
instance_of: Mountain
countries: Peru
coordinates: lat: -10.44888889
lon: -77.24972222
surface_form: uchku mach'ay
instance_of: Mountain
countries: Peru
coordinates: lat: -11.42166667
lon: -75.80277778
surface_form: mach'ay
instance_of: Mountain
countries: Peru
coordinates: lat: -9.63722222
lon: -76.40027778
Uchku Mach'ay. Uchku Mach'ay (Quechua &quot;uchku&quot; hole, &quot;mach'ay&quot; cave, &quot;hole cave&quot;, also spelled &quot;Uchcomachay&quot;) is a mountain in the Andes of Peru which reaches a height of approximately. It lies in the Junín Region, Tarma Province, Tarma District.

Geographic entities mentioned:
surface_form: uchku
instance_of: Mountain
countries: Peru
coordinates: lat: -12.38472222
lon: -75.70138889
surface_form: uchku
instance_of: Mountain
countries: Peru
coordinates: lat: -12.38472222
lon: -75.70138889
surface_form: uchku
instance_of: Mountain
countries: Peru
coordinates: lat: -10.44888889
lon: -77.24972222
surface_form: uchku
instance_of: Mountain
countries: Peru
coordinates: lat: -10.44888889
lon: -77.24972222
surface_form: uchku mach'ay
instance_of: Mountain
countries: Peru
coordinates: lat: -11.42166667
lon: -75.80277778
surface_form: mach'ay
instance_of: Mountain
countries: Peru
coordinates: lat: -9.63722222
lon: -76.40027778
surface_form: mach'ay
instance_of: Mountain
countries: Peru
coordinates: lat: -9.63722222
lon: -76.40027778