Sarmila/GeoWiki-Features huggingface dataset:
It is in a suburban area with residential areas bordering the lake on the northwest and eastern shores. Swampland borders much of the rest of the shore. On the southwest is a house surrounded by much land. Reeves Lake has no public access. There is, however, a private park that has a private fishing dock on Rutledge Court, on the north side of the lake.

Geographic entities mentioned:
surface_form: reeves lake
instance_of: Lake
countries: United States
coordinates: lat: 27.9567
lon: -81.6651
Nowadays, after many geographical changes to the city layout, Quán Thánh Temple is located on the corner of Quán Thánh Street and Thanh Niên Street, facing West Lake. It is a short walk from Trúc Bạch Lake where pilot (and future United States senator) John McCain was shot down in October 1967. Architecture.

Geographic entities mentioned:
surface_form: Trúc Bạch Lake
instance_of: Lake
countries: Vietnam
coordinates: lat: 21.045555555556
lon: 105.83805555556
Lac de l'Oriente. Lac de l'Oriente is a lake in Corsica, France. The Lac de l'Oriente (East Lake) is in a basin on the north slope of Monte Rotondo. Its outlet is the Ruisseau de Lomento. This is a tributary of the Ruisseau Timozzo, in turn a tributary of the Restonica river. It is in the watershed of the Tavignano river.

Geographic entities mentioned:
surface_form: Monte Rotondo
instance_of: Mountain
countries: France
coordinates: lat: 42.21611111111111
lon: 9.058055555555555
Dakar, the capital of Senegal, occupies parts including its southern tip. The peninsula marks the border between Grande Côte to the north and Petite Côte to the south. It is delimited by two capes, Pointe des Almadies to the northwest and cap Manuel to the southeast. The larger of the Deux Mamelles volcanic hills in Dakar is topped by Les Mamelles Lighthouse at its highest point. History.

Geographic entities mentioned:
surface_form: Deux Mamelles
instance_of: Mountain
countries: Senegal
coordinates: lat: 14.723694444444
lon: -17.502138888889
The couple had two sons. From 1983, Cassell lived in Victoria. He was a prominent member of the Save Albert Park movement, after it was first proposed the Australian Grand Prix would relocate to the area where Cassell would walk his dogs. In his later years, Cassell was diagnosed with dementia and lived in an aged care facility at Kyneton where he died on 30 August 2017 at the age of 85.

Geographic entities mentioned:
surface_form: area
instance_of: Lake
countries: Australia
coordinates: lat: -37.846
lon: 144.97
Ice Lake Rebels. &quot;Ice Lake Rebels&quot; is an American reality TV show about houseboat dwellers in Great Slave Lake. It aired on Animal Planet for two seasons, from 2014 to 2016. The show was produced by Critical Content of Los Angeles, and aired on Animal Planet. The producer was Kathryn Haydn Hays.

Geographic entities mentioned:
surface_form: Great Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 61.666666666667
lon: -114
In 1888 his father built a grand Victorian Italianate mansion on the corner of Glebe Point and Wigram Roads Glebe known as &quot;Ben Ledi&quot;. It was named after the mountain Ben Ledi in Scotland. The design of the family home is attributed to the Sydney architect Thomas Rowe who Kethel was articled to when he studied architecture at Sydney Technical College.

Geographic entities mentioned:
surface_form: Ben Ledi
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.258659
lon: -4.322375
Mahadevapura, Mandya. Mahadevapura is a village in Mandya district of Karnataka province in India. It is from Mysore city. The village and its surrounding places are known for film shooting. Transportation. The road from Mysore to Mahadevapura starts from Sathgully bus station in East Mysore. It goes through Ramanahalli village before reaching Mahadevapura bridge. The river Kaveri has a bund here.

Geographic entities mentioned:
surface_form: Kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
Many Hutus were also killed for a variety of reasons, including sympathy for moderate opposition parties, being a journalist or simply having a &quot;Tutsi appearance&quot;. Thousands of bodies were dumped into the Kagera River, which ran along the northern border between Rwanda and Uganda and flowed into Lake Victoria.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Kresna Gorge. Kresna Gorge () is a steep valley in south-western Bulgaria, stretching about. The gorge has been formed by the Struma River, which flows from the Vitosha mountains. Kresna gorge has a rich biodiversity, which has come under pressure from the Struma motorway construction project, a new leg of the Trans European Corridor No. 4.

Geographic entities mentioned:
surface_form: Vitosha
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.566666666667
lon: 23.283333333333
Terrain and Climate. Kresna Gorge is situated near the villages of Palat, Drakata, and Krupnik while surrounded by the Pirin and Maleshevska Mountains. The gorge is a transitory Mediterranean climate, as it is located between the Central-European and Mediterranean climate zones. The Struma River cuts through the gorge and is a main geological feature.

Geographic entities mentioned:
surface_form: Maleshevska Mountains
instance_of: Mountain
countries: Bulgaria
North Macedonia
coordinates: lat: 41.666666666667
lon: 23
It extends along the border of Shizuoka, Yamanashi and Nagano Prefectures for a length of, and a maximum width of for a total area of. The Park is a very mountainous region, centering on the Akaishi Mountains with several noted peaks of over 3000 meters in height, including Senjō-ga-take, Kita-dake, Aino-dake, Shiomi-dake, Arakawa-take, Akaishi-dake and Hijiri-dake.

Geographic entities mentioned:
surface_form: Kita-dake
instance_of: Mountain
countries: Japan
coordinates: lat: 35.67432
lon: 138.23874
surface_form: Aino-dake
instance_of: Mountain
countries: Japan
coordinates: lat: 35.646111111111
lon: 138.22833333333
surface_form: Shiomi-dake
instance_of: Mountain
countries: Japan
coordinates: lat: 35.57388889
lon: 138.18305556
surface_form: Akaishi-dake
instance_of: Mountain
countries: Japan
coordinates: lat: 35.461111111111
lon: 138.15722222222
surface_form: Hijiri-dake
instance_of: Mountain
countries: Japan
coordinates: lat: 35.42277778
lon: 138.13972222
Lake Minnetonka Regional Park. Located in Minnetrista, Lake Minnetonka Regional Park is a relatively new park in the Three Rivers system. It offers a chlorinated sand-bottom swimming pond and a creative play area. It also provides boat access to Lake Minnetonka. Lake Rebecca Park Reserve. Lake Rebecca Park Reserve, in Greenfield and Independence, is a large park reserve with.

Geographic entities mentioned:
surface_form: Lake Minnetonka
instance_of: Lake
countries: United States
coordinates: lat: 44.933333333333
lon: -93.566666666667
The main road of the Lukmanier Pass runs along the eastern shore of the lake. The lake lies at a height of 1,908 metres above sea level and is surrounded by mountains over 3,000 metres on both sides. The highest peak overlooking Lai da Sontga Maria is the Scopi (3,190 m), on the east side. On the west side are Piz Gannaretsch (3,040 m) and Piz Rondadura (3,016 m).

Geographic entities mentioned:
surface_form: Scopi
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.571666666667
lon: 8.83
The lake lies at a height of 1,908 metres above sea level and is surrounded by mountains over 3,000 metres on both sides. The highest peak overlooking Lai da Sontga Maria is the Scopi (3,190 m), on the east side. On the west side are Piz Gannaretsch (3,040 m) and Piz Rondadura (3,016 m). On the south side (in Ticino), the lake is overlooked by Pizzo dell'Uomo (2,663 m).

Geographic entities mentioned:
surface_form: Piz Gannaretsch
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.612027777778
lon: 8.7864444444444
surface_form: Piz Rondadura
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.57625
lon: 8.75075
The highest peak overlooking Lai da Sontga Maria is the Scopi (3,190 m), on the east side. On the west side are Piz Gannaretsch (3,040 m) and Piz Rondadura (3,016 m). On the south side (in Ticino), the lake is overlooked by Pizzo dell'Uomo (2,663 m). The lake is drained by the Rein da Medel, a tributary of the Anterior Rhine. In the lake, there is an anchor pylon of Lukmanier Powerline.

Geographic entities mentioned:
surface_form: Pizzo dell'Uomo
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.544583333333
lon: 8.7771111111111
Volkhov (river). The Volkhov (;;) is a river in Novgorodsky and Chudovsky Districts of Novgorod Oblast and Kirishsky and Volkhovsky Districts of Leningrad Oblast in northwestern Russia. The Volkhov, which forms part of the basin of the Neva, is the only outflow of Lake Ilmen, and connects it with Lake Ladoga. The length of the Volkhov is, and the area of its drainage basin is.

Geographic entities mentioned:
surface_form: Lake Ilmen
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 58.266666666667
lon: 31.283333333333
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
Geography. The Volkhov flows out of Lake Ilmen north into Lake Ladoga, the largest lake in Europe. It is the second largest tributary of Lake Ladoga. It is navigable over its whole length. Discharge is highly variable depending primarily on the level of Lake Ilmen. The Volkhov is reported to reverse the direction of its flow in its upper section in exceptional circumstances.

Geographic entities mentioned:
surface_form: Lake Ilmen
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 58.266666666667
lon: 31.283333333333
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
Peters Hill (Massachusetts). Peters Hill is a hill in Barnstable County, Massachusetts. It is located south-southeast of North Truro in the Town of Truro. Green Hill is located southeast and Tom Hill is located south of Peters Hill.

Geographic entities mentioned:
surface_form: tom hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.9993119
lon: -70.0724165
surface_form: green hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.0975
lon: -74.185555555556
surface_form: peters hill
instance_of: Mountain
countries: United States
coordinates: lat: 42.0240658
lon: -70.0735439
surface_form: green hill
instance_of: Mountain
countries: United States
coordinates: lat: 42.0154043
lon: -70.039933
Peters Hill (Massachusetts). Peters Hill is a hill in Barnstable County, Massachusetts. It is located south-southeast of North Truro in the Town of Truro. Green Hill is located southeast and Tom Hill is located south of Peters Hill.

Geographic entities mentioned:
surface_form: peters hill (massachusetts)
instance_of: Mountain
countries: United States
coordinates: lat: 42.0240658
lon: -70.0735439
Peters Hill (Massachusetts). Peters Hill is a hill in Barnstable County, Massachusetts. It is located south-southeast of North Truro in the Town of Truro. Green Hill is located southeast and Tom Hill is located south of Peters Hill.

Geographic entities mentioned:
surface_form: peters hill
instance_of: Mountain
countries: United States
coordinates: lat: 42.0240658
lon: -70.0735439
The men's alpine ski races were held on Bjelašnica, the highest mountain at 2,067 meters located southwest of Sarajevo. The women's events were contested on Jahorina, at an altitude of 1,913 meters and located to the south-east of the city. The Nordic events took place on Igman, in an area near Mount Bjelašnica. Igman Olympic Jumps of 70 and 90 meters were built in Malo Polje.

Geographic entities mentioned:
surface_form: Igman
instance_of: Plateau
countries: Bosnia and Herzegovina
coordinates: lat: 43.783333333333
lon: 18.25
The Nordic events took place on Igman, in an area near Mount Bjelašnica. Igman Olympic Jumps of 70 and 90 meters were built in Malo Polje. The already existing cross-country ski and biathlon tracks in Veliko Polje were redeveloped and a new shooting range installed for the biathlon. A bobsleigh and luge track, the first in the country's history, was built on the Trebević south-east of Sarajevo.

Geographic entities mentioned:
surface_form: Malo Polje
instance_of: Plateau
countries: Bosnia and Herzegovina
coordinates: lat: 43.783333333333
lon: 18.25
The Nordic events took place on Igman, in an area near Mount Bjelašnica. Igman Olympic Jumps of 70 and 90 meters were built in Malo Polje. The already existing cross-country ski and biathlon tracks in Veliko Polje were redeveloped and a new shooting range installed for the biathlon. A bobsleigh and luge track, the first in the country's history, was built on the Trebević south-east of Sarajevo.

Geographic entities mentioned:
surface_form: Veliko Polje
instance_of: Plateau
countries: Bosnia and Herzegovina
coordinates: lat: 43.783333333333
lon: 18.25
Igman Olympic Jumps of 70 and 90 meters were built in Malo Polje. The already existing cross-country ski and biathlon tracks in Veliko Polje were redeveloped and a new shooting range installed for the biathlon. A bobsleigh and luge track, the first in the country's history, was built on the Trebević south-east of Sarajevo. The track has a length of 1300 meters and a drop of 126 meters.

Geographic entities mentioned:
surface_form: Trebević
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.823333333333
lon: 18.448888888889
Events. There were 39 events contested in 6 sports (10 disciplines). Biathlon. The biathlon events were held in Veliko Polje on Mount Igman. Biathlon races began with the individual 20 km sprint. The 19-year-old East German Frank-Peter Rötsch quickly took the lead, but it was ultimately the West German Peter Angerer who won with a time one minute faster.

Geographic entities mentioned:
surface_form: Igman
instance_of: Plateau
countries: Bosnia and Herzegovina
coordinates: lat: 43.783333333333
lon: 18.25
Norway finished second with 1:20 ahead of East Germany. Kvalfoss and Angerer therefore ended the Games with three medals in three different events. Bobsleigh. The bobsleigh races took place on the luge track built on the Trebević mountain. The East Germans dominated the discipline as they won the two gold medals and two silver medals. As of 2020, this performance has still not been matched.

Geographic entities mentioned:
surface_form: Trebević
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.823333333333
lon: 18.448888888889
Enke ended the Games with four medals and Ehring with three. Ski jumping. The ski jumping events took place on the Igman hills, southwest of Sarajevo in windy weather conditions. On the normal hill, 20-year-old Matti Nykänen of Finland led the standings after the first round by achieving a jump of 91 meters. The 19-year-old East German Jens Weissflog was second with a jump of 90 meters.

Geographic entities mentioned:
surface_form: Igman hills
instance_of: Plateau
countries: Bosnia and Herzegovina
coordinates: lat: 43.783333333333
lon: 18.25
Marie, Michigan. The rock punched a hole in her hull, after which she was beached to prevent her from sinking. Early in the morning of July 20, 1897, while travelling on Lake Huron, &quot;Ira H. Owen&quot; collided with the package freighter &quot;Susquehanna&quot; in thick fog off Presque Isle, Michigan. Both vessels were severely damaged; &quot;Ira H.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Cottonwood Lake (Sully County, South Dakota). Cottonwood Lake is a lake in South Dakota, in the United States. The lake was so named on account of the cottonwood trees which grew there.

Geographic entities mentioned:
surface_form: cottonwood lake
instance_of: Lake
countries: United States
coordinates: lat: 45.109357
lon: -97.2247008
surface_form: cottonwood lake
instance_of: Lake
countries: United States
coordinates: lat: 44.835574
lon: -99.9058888
Kearsarge, California. Kearsarge or Kearsarge City is a former mining settlement in Inyo County, eastern California. It was located high on the east slope of the Sierra Nevada, near Kearsage Pass, west of present-day town of Independence, California. The mining camp was in the Kearsarge Mining District, located just below the high granite Kearsarge Peak, and east of the Kearsarge Pass. History.

Geographic entities mentioned:
surface_form: Kearsarge Peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.7891
lon: -118.34732
Sgùrr a' Mhadaidh. is a mountain peak in the Black Cuillin range on the Isle of Skye, Scotland. It is a Munro with a height of. Like the rest of the range it is composed of gabbro, a rock with excellent grip for mountaineering. The simplest route ascends via the col of An Dorus (the Door), most easily reached from Glen Brittle.

Geographic entities mentioned:
surface_form: sgùrr a' mhadaidh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.230868
lon: -6.231947
The Bucktown Five also recorded with Bix Beiderbecke. The band's name is linked with New Orleans, as Bucktown is a Chicago neighborhood, but also the name of the settlement that grew up on the shore of Lake Pontchartrain after the close of Storyville. It became a smaller version of that district.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
On the return to England Abbott had a breakdown and was invalided out of the service for a time. Legacy. Mount Abbott, a 1,020m-high mountain on the coast of Victoria Land, and Abbott Peak, a foothill of Mount Erebus on Ross Island, are named in honour of Petty Officer George P. Abbott.

Geographic entities mentioned:
surface_form: Mount Erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
One of the most significant landforms in southern Ontario, the moraine gets its name from the rolling hills and river valleys extending east from the Niagara Escarpment to Rice Lake, formed 12,000 years ago by advancing and retreating glaciers (see &quot;geological origins&quot;, below) during the last glaciation period.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: rice lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.05004
lon: -107.1173
surface_form: rice lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.1833
lon: -78.1667
The Oak Ridges Moraine probably formed in the Late Wisconsin glacial period. Ice melt from the Niagara Escarpment flowed into the western boundaries of the moraine, wherein conduits beneath the ice expanded to form a west-to-east passage between the main Laurentide Ice Sheet and a mass of ice in the Lake Ontario basin. Stratified sediment was deposited rapidly on the high-relief erosional surface.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Softer metamorphic rocks of the Precambrian basement include marbles or metaturbidites, both from sedimentary origin. Ecology. The ecologically diverse moraine is the water source for many headwaters streams flowing south into rivers that drain into Lake Ontario and north into rivers that drain into Lake Scugog and Lake Simcoe.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
surface_form: Lake Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
The Rice Lake wedge is separated from the other wedges where the Oak Ridges Moraine intersects Rice Lake. As the moraine is a local topographic high, streams originating in the lower Oak Ridges Moraine sediment packages, by groundwater movement, either flow south into Lake Ontario or north toward Lake Simcoe or Georgian Bay through large river valleys carved during melting of glaciers.

Geographic entities mentioned:
surface_form: lake simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
surface_form: simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
For this reason, environmentalists and researchers promote an aggressive protection strategy extending beyond the moraine, thus ensuring a contiguously protected hydrological system. Preservation of aquifers under the moraine is especially important, since they are used as a primary water source by some municipalities located on or near the moraine.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
Oak Ridges Moraine. The Oak Ridges Moraine is an ecologically important geological landform in the Mixedwood Plains of south-central Ontario, Canada. The moraine covers a geographic area of between Caledon and Rice Lake, near Peterborough.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: oak ridges moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
Oak Ridges Moraine. The Oak Ridges Moraine is an ecologically important geological landform in the Mixedwood Plains of south-central Ontario, Canada. The moraine covers a geographic area of between Caledon and Rice Lake, near Peterborough.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: rice lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.05004
lon: -107.1173
surface_form: rice lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.1833
lon: -78.1667
Below the approximately 200 metre thick glacial derived sediments of the moraine lies thick bedrock successions of Precambrian rocks and up to 200 metres of Ordovician aged rock (see &quot;geology&quot; below), capped by a regional unconformity of erosion and non-deposition to the Quaternary period.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
Rivers and lakes scatter the landscape and are important for creating habitat for the rich diversity of species of animals, trees and shrubbery (see &quot;ecology&quot;). These are also the supply of fresh water to aquifers in the moraine through complex subterranean connections (see &quot;hydrology&quot;).

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
These are also the supply of fresh water to aquifers in the moraine through complex subterranean connections (see &quot;hydrology&quot;). Construction development nearby, and with expansion of communities around the moraine in need of potable water, it is a contested site in Ontario, since it stands in the path of major urban development (see &quot;political action&quot;).

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
Conservation of the moraine is thus an important step for keeping aquifers in a safe drinkable condition while also protecting the natural ecosystems surrounding and within the moraine (see &quot;conservation&quot;). This region has been subject to multiple decades of scientific research to study the origins of formation, and how early communities used the land.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
A larger focus currently is how to source potable water without removing the aquifer entirely (see &quot;research&quot; section). Physiography. The Oak Ridges Moraine is a pair of large ridges composed of four elevated wedges. It is bounded to the west by the Niagara Escarpment, a cuesta which was critical to the formation of the moraine, and to the east by the Trent River and Rice Lake.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: rice lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.05004
lon: -107.1173
surface_form: rice lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.05004
lon: -107.1173
surface_form: rice lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.1833
lon: -78.1667
surface_form: rice lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.1833
lon: -78.1667
The four wedges (&quot;Albion&quot;, &quot;Uxbridge&quot;, &quot;Pontypool&quot; and &quot;Rice Lake&quot; from west to east) formed in stages, though some synchronous formation also occurred at an early period of formation. The moraine peaks at the Uxbridge wedge, generally rising from east to west, a result of the moraine's west-to-east formation.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
The moraine peaks at the Uxbridge wedge, generally rising from east to west, a result of the moraine's west-to-east formation. That is, the western portion of the moraine received earlier and more frequent sedimentary deposition than the eastern portion, as the ice lobes which controlled the moraine's eastern formation slowly retreated.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
That is, the western portion of the moraine received earlier and more frequent sedimentary deposition than the eastern portion, as the ice lobes which controlled the moraine's eastern formation slowly retreated. The Rice Lake wedge is separated from the other wedges where the Oak Ridges Moraine intersects Rice Lake.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: oak ridges moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
To the north are drumlinized uplands, referred to as the &quot;Peterborough drumlin field,&quot; which may continue south of Rice Lake and the Rice Lake wedge&quot;.&quot; Near the Rice Lake wedge and Peterborough drumlin field are a couple of low-lying terrain plains and small hills on bedrock basement. Geological origins.

Geographic entities mentioned:
surface_form: rice lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.05004
lon: -107.1173
surface_form: rice lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.05004
lon: -107.1173
surface_form: rice lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.05004
lon: -107.1173
surface_form: rice lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.1833
lon: -78.1667
surface_form: rice lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.1833
lon: -78.1667
surface_form: rice lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.1833
lon: -78.1667
Geological origins. The Oak Ridges Moraine probably formed in the Late Wisconsin glacial period. Ice melt from the Niagara Escarpment flowed into the western boundaries of the moraine, wherein conduits beneath the ice expanded to form a west-to-east passage between the main Laurentide Ice Sheet and a mass of ice in the Lake Ontario basin.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
Up to in some areas, the deposits occurred on surfaces defined by highly eroded channels and drumlin uplands. The channel tunnels were primarily created by the erosion from glacial rivers, a typical process before moraine formation. Characteristic of this moraine is the transition of deposition layers from glaciofluvial to glaciolacustrine.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
The channel tunnels were primarily created by the erosion from glacial rivers, a typical process before moraine formation. Characteristic of this moraine is the transition of deposition layers from glaciofluvial to glaciolacustrine. Sedimentary glaciofluvial areas form the core of the Oak Ridges Moraine, though restricted to subglacial cavity fills of confined subaqueous fans.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
Sedimentary glaciofluvial areas form the core of the Oak Ridges Moraine, though restricted to subglacial cavity fills of confined subaqueous fans. Overlaying this core is a glaciolacustrine sedimentary layer that is younger and topographically lower, principally in the delta and basin areas of the moraine.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
The wedges may have formed in a relatively short period of time, perhaps no more than a few hundred years, as indicated by the annual deposition cycles in glacial lakes (known as varves) within the moraine sediments. However, the lowest beds in the moraine may have experienced synchronous sedimentation. Glacial sediments.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
Glacial sediments. In the area of the Oak Ridges Moraine, glacially derived sediments, mainly of Pleistocene age, may overlie a regional unconformity and lower Newmarket till, up to 200 metres thick in some places. Extensive research in the moraine area indicate there may be 6 different periods of sedimentation from the onset of glaciation.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
Varied landforms on the moraine, such as woodlands, wetlands, watercourses, kettle lakes and bogs, have provided an environment suitable for significant flora and fauna communities to develop and thrive. The moraine contains one of the last large contiguous forested spans in southern Ontario.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
The moraine contains one of the last large contiguous forested spans in southern Ontario. Some of the wide variety of plant and animal species found in the moraine are &quot;species at risk&quot; in Canada and Ontario, including the West Virginia white butterfly, Jefferson salamander, and red-shouldered hawk.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
Unique ecosystems in the moraine include wetlands similar to those of boreal forests in Northern Ontario, and remnants of tallgrass prairie and oak-pine savanna that are globally threatened ecosystems. A representative portion of the moraine may be found in the Happy Valley Forests, in York Region, north of Toronto. Hydrology.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
Hydrology. This hydrological system is inter-twined with a regional flow systems not bound by the morphological limits of the moraine. For this reason, environmentalists and researchers promote an aggressive protection strategy extending beyond the moraine, thus ensuring a contiguously protected hydrological system.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
The &quot;Oak Ridges Moraine Conservation Act&quot; stipulates that any development which targets the moraine or nearby areas must satisfy several conditions, most prominently that each development leave a buffer zone of between it and any hydrological feature; for a kettle lake, this measure is from the edge of the lake's catchment area.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: oak ridges moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
Research on the moraine. In 1829, John Bigsby conducted the first investigation of the moraine. He noted the elevation, and styled the area &quot;Oak Ridge&quot;, identifying the portion of moraine north of Toronto. The moraine's extent was not established until 1863 when William Logan conducted the Geological Survey of Canada.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
He noted the elevation, and styled the area &quot;Oak Ridge&quot;, identifying the portion of moraine north of Toronto. The moraine's extent was not established until 1863 when William Logan conducted the Geological Survey of Canada. Taylor formally defined the landform as the Oak Ridges Moraine in 1913. He described its extent to be from King and Maple in the west to the Trent River in the east.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
He described its extent to be from King and Maple in the west to the Trent River in the east. He also proposed that its origin was overlapping, interlobate glaciation retreat, between the Lake Ontario Lobe and the older Lake Simcoe Lobe. This has become the accepted explanation for the moraine's development, though research in the 1970s suggested the moraine may not be interlobate.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
Research conducted in the 1990s revealed that the moraine has multiple origins: its eastern area has subglacial depositions (Gorrell and McCrae, 1993); early parts of the moraine were deposited in an esker (Brennand and Shaw, 1994); and that the moraine is not continuous, but is composed of multiple depositional environments: subglacial, ice-marginal and proglacial lacustrine (Barnett et al., 1998).

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
Current research efforts on the moraine are quite extensive. Because of the political implications of development on the moraine, and because its aquifers are a source of potable water for numerous communities, both federal and provincial governments have invested resources towards research on the moraine.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
Political action. Although preservation of the moraine was first suggested in the 1940s, it was not until 1991 that the issue achieved prominence in political discourse. Part of the reason for its entry into political discourse, was due to the formation, in 1989, of the Save the Oak Ridges Moraine (STORM) Coalition.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
Part of the reason for its entry into political discourse, was due to the formation, in 1989, of the Save the Oak Ridges Moraine (STORM) Coalition. The Government of Ontario created the &quot;Oak Ridges Moraine Technical Working Committee&quot; in June 1991, with the aim of creating a regional planning strategy for the moraine.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
The plan was completed in 1994, but was subsequently dismissed in favour of local government administration of the affected lands. This led to intense development on some portions of the moraine. In early 1999, developers targeted Richmond Hill for large subdivisions on the moraine which would house over 100,000 people.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
A media campaign by environmental groups built on the public opposition of the developments, and the issue was transferred to the Ontario Municipal Board (OMB) in 2000. By May 2001, with the issue still unresolved, the provincial Conservative government announced a six-month moratorium on moraine development.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
A panel was formed to create a land-use plan consistent with the current &quot;smart growth&quot; policy. The plan was released in October 2001, and became the basis for Bill 122, the &quot;Oak Ridges Moraine Conservation Act, 2001&quot;, which divided the moraine into four zones with increasingly stringent controls on development in each.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
The Act prevented development of over 92% of the land mass of the moraine and only those development projects which had already received zoning and planning approval were allowed to be completed. During the provincial election of 2003, the Liberal Party of Ontario promised to terminate development on the moraine as part of their election campaign.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
The government, in its attempt to halt developments, proposed the &quot;North Pickering Land Exchange.&quot; This involved exchanging government-owned public lands in North Pickering (the Seaton lands) for privately owned lands on the Oak Ridges Moraine in Richmond Hill and Uxbridge.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: oak ridges moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
The exchange settled outstanding disputes being considered by the OMB involving moraine lands in Richmond Hill and Uxbridge. Despite all these efforts, including the government's creation of a permanently protected Greenbelt, the political struggle regarding the moraine continues.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
Unless approved prior to the Oak Ridges Moraine Conservation Act coming into force in 2001 or through orders of the Ontario Municipal Board to the contrary, development on the Oak Ridges Moraine is restricted to the Settlement Area. Smaller-scale development which improves the ecological integrity of the moraine is permitted in other areas (i.e., tree farm), but is otherwise restricted.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
Given that the land-subdivision process is lengthy and that Markham, Vaughan, Richmond Hill, Whitchurch-Stouffville and King Township are experiencing a shortage in servicing capacity, what often appears as &quot;new&quot; development in Markham, Vaughan, Richmond Hill, Whitchurch-Stouffville and King Township on the moraine is in the majority of cases development which has had approval for many years.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
Development pressures. The greatest threat to the function of the moraine is land development on and below its surface, particularly in the headwaters. The estimated current population on the moraine land itself is roughly 200,000 but this number continues to grow at a frantic pace, with large urban developments occurring in Stouffville, Vaughan, Richmond Hill, and Aurora.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
Another five million people live in close proximity. Use of the moraine is currently under dispute; environmental groups such as the Sierra Club maintain the area's delicate ecosystems are threatened by development pressures. Attractive forests and hilly relief typical of the moraine are a magnet for developers looking for building opportunities in the densely populated Greater Toronto Area.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
Attractive forests and hilly relief typical of the moraine are a magnet for developers looking for building opportunities in the densely populated Greater Toronto Area. However, many planners and residents see a need to preserve the moraine from the negative aspects of urban sprawl.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
Whereas the glacial river deposits were more substantial by volume, the diamicton deposits represent a greater portion of the moraine's exposed surface. Research suggests that sedimentation occurred in a west to east sequence along the four main sedimentary wedges: &quot;Albion&quot;, &quot;Uxbridge&quot;, &quot;Pontytool&quot; and &quot;Rice Lake&quot;.

Geographic entities mentioned:
surface_form: rice lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.05004
lon: -107.1173
surface_form: rice lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.1833
lon: -78.1667
He taught here as professor of pharmaceutical chemistry (1923–48) and Systematic Botany (1925–48), as well as directing the Botany Seminar (1935–1948). The wild potato species, &quot;S. neoweberbaueri&quot;, collected by Weberbauer on Morro Solar, was named by Ludwig Wittmack in 1914. He taught at the Deutsche Schule Lima Alexander von Humboldt.

Geographic entities mentioned:
surface_form: Morro Solar
instance_of: Mountain
countries: Peru
coordinates: lat: -12.18345
lon: -77.031872222222
No concrete archaeological evidence was found to substantiate a human presence in Egypt throughout this millennium, according to Egyptologists. The time gap has been filled, at least, with comparable discoveries made at Tushka in Egypt during this millennium, showing continuity of human presence in the area from this antiquity all the way down to the start of history. Technology and agriculture.

Geographic entities mentioned:
surface_form: Tushka
instance_of: Group of lakes
countries: Egypt
coordinates: lat: 23.422052777778
lon: 30.597697222222
Lake Alice (Southland). Lake Alice is a small lake at the eastern end of George Sound approximately 52 km north west of Te Anau in the Southland region of the South Island. The lake is fed by the Edith River and flows into George Sound via Alice Falls.

Geographic entities mentioned:
surface_form: te anau
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.2
lon: 167.8
surface_form: lake alice
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.973333333333336
lon: 167.46472222222224
surface_form: lake alice
instance_of: Lake
countries: New Zealand
coordinates: lat: -40.134166666666665
lon: 175.33194444444445
Lake Alice (Southland). Lake Alice is a small lake at the eastern end of George Sound approximately 52 km north west of Te Anau in the Southland region of the South Island. The lake is fed by the Edith River and flows into George Sound via Alice Falls.

Geographic entities mentioned:
surface_form: lake alice
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.973333333333336
lon: 167.46472222222224
surface_form: lake alice
instance_of: Lake
countries: New Zealand
coordinates: lat: -40.134166666666665
lon: 175.33194444444445
Sellaronda. The Sellaronda is the ski circuit around the Sella group in the Dolomites mountains of Northern Italy. The Sella massif lies between the four Ladin valleys of Badia, Gardena, Fascia, and Fodom and is divided between the provinces of South Tyrol, Trentino and Belluno in the regions of Trentino-Alto Adige and Veneto.

Geographic entities mentioned:
surface_form: Badia
instance_of: Valley
countries: Italy
coordinates: lat: 46.683333333333
lon: 11.9
surface_form: Gardena
instance_of: Valley
countries: Italy
coordinates: lat: 46.56
lon: 11.704722
Mount Giona. Mount Giona (, also transliterated as &quot;Gkiona&quot;,) is a mountain in Phocis, Central Greece. It is located between the mountains of Parnassus to the east, Vardousia to the west, and Oeta to the north. Known in classical antiquity as the &quot;Aselinon Oros&quot; (, 'moonless mountain'), it is the highest mountain south of Olympus and the fifth overall in Greece.

Geographic entities mentioned:
surface_form: Parnassus
instance_of: Mountain
countries: Greece
coordinates: lat: 38.533
lon: 22.6167
surface_form: Vardousia
instance_of: Mountain
countries: Greece
coordinates: lat: 38.679831
lon: 22.142922
surface_form: Oeta
instance_of: Mountain
countries: Greece
coordinates: lat: 38.816666666667
lon: 22.283333333333
It is located between the mountains of Parnassus to the east, Vardousia to the west, and Oeta to the north. Known in classical antiquity as the &quot;Aselinon Oros&quot; (, 'moonless mountain'), it is the highest mountain south of Olympus and the fifth overall in Greece. Pyramida is its highest peak at.

Geographic entities mentioned:
surface_form: Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
Mount Giona. Mount Giona (, also transliterated as &quot;Gkiona&quot;,) is a mountain in Phocis, Central Greece. It is located between the mountains of Parnassus to the east, Vardousia to the west, and Oeta to the north. Known in classical antiquity as the &quot;Aselinon Oros&quot; (, 'moonless mountain'), it is the highest mountain south of Olympus and the fifth overall in Greece.

Geographic entities mentioned:
surface_form: giona
instance_of: Mountain
countries: Greece
coordinates: lat: 38.613888888889
lon: 22.253055555556
surface_form: mount giona
instance_of: Mountain
countries: Greece
coordinates: lat: 38.613888888889
lon: 22.253055555556