Sarmila/GeoWiki-Features huggingface dataset:
The project took inspiration from: Lake Maracaibo with its original “Palafitos” (stilt house) and its modern days oil rigs; the oil refineries; the Venezuelan land represented by the Tepui Guayanes; and the tropical vegetation (which was recreated throughout the park and building). Inside the museum's building, visitors would follow a path similar to that of oil as it is extracted.

Geographic entities mentioned:
surface_form: Lake Maracaibo
instance_of: Lake
countries: Venezuela
coordinates: lat: 9.8158333333333
lon: -71.556666666667
Battery D, 1st Missouri Light Artillery Regiment was an artillery battery that served in the Union Army during the American Civil War. Organized before February 1862, Battery D fought at Fort Henry, Fort Donelson, Shiloh, Corinth siege, Corinth, and Missionary Ridge. After serving in the Knoxville campaign, the battery garrisoned Huntsville, Alabama until April 1865.

Geographic entities mentioned:
surface_form: Missionary Ridge
instance_of: Landform
countries: United States
coordinates: lat: 34.986388888889
lon: -85.278611111111
Castle in the Clouds. Castle in the Clouds (or &quot;Lucknow&quot;) is a 16-room mansion and mountaintop estate in Moultonborough, New Hampshire, opened seasonally to the public by the Castle Preservation Society. It overlooks Lake Winnipesaukee and the Ossipee Mountains from a rocky outcropping of Lee Mountain formerly known as &quot;The Crow's Nest&quot;. History.

Geographic entities mentioned:
surface_form: Lake Winnipesaukee
instance_of: Lake
countries: United States
coordinates: lat: 43.598888888889
lon: -71.323055555556
Wanu Wanu. Wanu Wanu (Aymara and Quechua &quot;wanu&quot; dung, fertilizer, &quot;a lot of dung&quot;, hispanicized spelling &quot;Huanu Huanu&quot;) is a mountain in the Andes of Peru, about high. It is located in the Cusco Region, Espinar Province, on the border of the districts of Condoroma and Ocoruro. It lies northeast of Atawallpa and southeast of Hatun Chhuka.

Geographic entities mentioned:
surface_form: hatun chhuka
instance_of: Mountain
countries: Peru
coordinates: lat: -15.17638889
lon: -71.04916667
Wanu Wanu. Wanu Wanu (Aymara and Quechua &quot;wanu&quot; dung, fertilizer, &quot;a lot of dung&quot;, hispanicized spelling &quot;Huanu Huanu&quot;) is a mountain in the Andes of Peru, about high. It is located in the Cusco Region, Espinar Province, on the border of the districts of Condoroma and Ocoruro. It lies northeast of Atawallpa and southeast of Hatun Chhuka.

Geographic entities mentioned:
surface_form: wanu wanu
instance_of: Mountain
countries: Peru
coordinates: lat: -15.19277778
lon: -71.03638889
Led by long standing coaches and teachers Mr Marron and Mr Forsythe, along with great help from alumnus Mr Barr, a previous winner of the event in 2008, the club brought the cup back to the Lagan for the first time in 10 years on 9 June 2018, dethroning Enniskillen after their long string of wins, and beating crews from Bann Rowing Club, RBAI and Enniskillen Royal Grammar School.

Geographic entities mentioned:
surface_form: Lagan
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.535555555556
lon: -5.9788888888889
The Monolith (Antarctica). The Monolith is a pair of small islets located off the southern tip of Sabrina Island within the Ross Dependency of Antarctica. The smaller of the two islets rises at a steep incline to above sea level, and is uninhabited even by penguins which have colonized the other nearby islands.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: the monolith
instance_of: Mountain
coordinates: lat: -66.95
lon: 163.28333
surface_form: monolith
instance_of: Mountain
coordinates: lat: -66.95
lon: 163.28333
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
The Monolith (Antarctica). The Monolith is a pair of small islets located off the southern tip of Sabrina Island within the Ross Dependency of Antarctica. The smaller of the two islets rises at a steep incline to above sea level, and is uninhabited even by penguins which have colonized the other nearby islands.

Geographic entities mentioned:
surface_form: the monolith (antarctica)
instance_of: Mountain
coordinates: lat: -66.95
lon: 163.28333
surface_form: monolith
instance_of: Mountain
coordinates: lat: -66.95
lon: 163.28333
In 1950, Itote swore the Mau Mau oath, and subsequently became responsible for oathing and was an executioner of traitors. As the police began clamping down on Mau Mau activities in 1952, Itote moved to the forests of Mount Kenya with a band of followers to join the insurgency. From here Itote began a wave of attacks on white settler farms in Nyeri and targeted loyalists in nearby villages.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
In September and October KG 100 remained on anti-shipping duties. In October 1942 it began supporting the eastward-most advance. It began bombing operations against Astrakhan and bombed Soviet ships on the Caspian Sea. On 26 October Hansgeorg Bätcher sank a ship in the Caspian after six attacks against it in the same mission. A SC250 was seen to hit the forecastle and the vessel began to burn.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
He also has a street named for him near Chopin Airport in Warsaw, Poland. The &quot;Avenue Gordon Bennett&quot; in Paris, where the French Open's Stade de Roland Garros is sited is named after his father. Bennett, British Columbia, now a ghost town, as well as nearby Bennett Lake and Bennett Peak are named for him, as is Bennett Island, discovered during the &quot;Jeannette&quot; expedition.

Geographic entities mentioned:
surface_form: Bennett Lake
instance_of: Lake
countries: Canada
coordinates: lat: 60.09166666666667
lon: -134.86555555555555
Blue Lake (Italy). The Blue Lake (,) is a mountain lake of the Pennine Alps, located not far from the Breuil-Cervinia ski resort in Valtournenche, Aosta Valley, Italy. The lake is located at a height of 1,980 metres above sea level. Its pristine waters are known for reflecting the Matterhorn.

Geographic entities mentioned:
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
Blue Lake (Italy). The Blue Lake (,) is a mountain lake of the Pennine Alps, located not far from the Breuil-Cervinia ski resort in Valtournenche, Aosta Valley, Italy. The lake is located at a height of 1,980 metres above sea level. Its pristine waters are known for reflecting the Matterhorn.

Geographic entities mentioned:
surface_form: blue lake (italy)
instance_of: Lake
countries: Italy
coordinates: lat: 45.92268
lon: 7.61833
Neighboring districts are Bad Kreuznach, Alzey-Worms, Bad Dürkheim, Kaiserslautern, Kusel. History. The district was created in 1969 by merging the districts Kirchheimbolanden and Rockenhausen. Geography. The district is located around the highest mountain of the Palatinate, the &quot;Donnersberg&quot; with 687 m above sea level. Coat of arms.

Geographic entities mentioned:
surface_form: Donnersberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.625280555556
lon: 7.9147194444444
On the left is the red wheel of the Lords of Bolanden, taken from the Kirchheim coat of arms. The blue wheel on the right is the wheel of the Lords of Falkenstein, taken from the Rockenhausen coat of arms. The green field on the bottom with the peak symbolizes the Donnersberg, the highest elevation in the district, and the sun the importance of the sunny plains for viticulture.

Geographic entities mentioned:
surface_form: Donnersberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.625280555556
lon: 7.9147194444444
Winona (legend). Winona or Wenonah is a Dakota Sioux character in a &quot;Lover's Leap&quot; romantic legend set at Maiden Rock, which is on the Wisconsin side of Lake Pepin in the United States. Winona is said to have leaped to her death from this high precipice rather than marry a suitor she did not love.

Geographic entities mentioned:
surface_form: Lake Pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
Further east into Skokie, Dempster Street intersects Interstate 94 (Edens Expressway) as well as U.S. Route 41 (Skokie Boulevard). Illinois Route 58 ends at U.S. Route 41. While still in Skokie, the road intersects Crawford Avenue. The road then enters Evanston and intersects Ridge Avenue. Dempster Street finally ends at a cul-de-sac at the shores of Lake Michigan in Evanston.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
The city of Chita lies at the confluence of the Ingoda and the Chitinka. A major portion of the Trans-Siberian Railway lies along the Ingoda valley. The name derives from the Evenki word &quot;ingakta&quot; which means &quot;river with pebbly and sandy banks&quot;. Lake Kenon, located in the western outskirts of Chita, is part of the Ingoda river basin.

Geographic entities mentioned:
surface_form: Kenon
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 52.0375
lon: 113.38138888889
It lies mostly in Lady Evelyn-Smoothwater Provincial Park, and mostly within Timiskaming District, with the exception of a short portion of the South Branch at its most southern stretch, which lies in northeastern Sudbury District, and of the southernmost tip of Lady Evelyn Lake, which lies in northwestern Nipissing District.

Geographic entities mentioned:
surface_form: Lady Evelyn Lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.3667
lon: -80.1792
Brown Lake (Stradbroke Island). Brown Lake (Bummeria) is a perched lake on North Stradbroke Island, in South-East Queensland, Australia. The ecosystem is an example of a coastal non-floodplain sand lake and is characterised by acidic water, nutrient-poor and sandy soil, shrub-like vegetation and wet heathland. Brown Lake is of geographical significance, possessing ecological value.

Geographic entities mentioned:
surface_form: brown lake (stradbroke island)
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
Brown Lake (Stradbroke Island). Brown Lake (Bummeria) is a perched lake on North Stradbroke Island, in South-East Queensland, Australia. The ecosystem is an example of a coastal non-floodplain sand lake and is characterised by acidic water, nutrient-poor and sandy soil, shrub-like vegetation and wet heathland. Brown Lake is of geographical significance, possessing ecological value.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
The ecosystem is an example of a coastal non-floodplain sand lake and is characterised by acidic water, nutrient-poor and sandy soil, shrub-like vegetation and wet heathland. Brown Lake is of geographical significance, possessing ecological value. The geomorphology of the ecosystem is representative of the unique parabolic dune ridge systems that formed during the Pleistocene epoch.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
Brown Lake is of geographical significance, possessing ecological value. The geomorphology of the ecosystem is representative of the unique parabolic dune ridge systems that formed during the Pleistocene epoch. As a perched lake, the hydrological operations of Brown Lake are highly diverse and complex.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
The indigenous population care for and protect the landscape, sharing traditional environmental management knowledge. Brown Lake’s cultural heritage and ecological value, along with the environmental damage associated with tourism, has led to increased conservation.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
Geography. Brown Lake is 1 km in length and is located 4 km east of Dunwich, a small town on North Stradbroke Island. Brown Lake is in a subtropical climatic region; experiencing a wet season in the winter and a dry season in the summer. The mean daily temperature for the area is &quot;15°–29°C in summer and 9°–20°C in winter&quot; and the average annual rainfall is 1668 mm.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
The mean daily temperature for the area is &quot;15°–29°C in summer and 9°–20°C in winter&quot; and the average annual rainfall is 1668 mm. Geologically, Brown Lake exists on a parabolic beach ridge system that formed during the Quaternary glacial and interglacial cycles of the Pleistocene epoch.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
The cold-climate interval of the epoch caused a periodic lower sea level, which exposed the sea-bed of the coastal heathland to strong south-easterly winds that carried and deposited sediment which eventually accumulated to form the dune ridges on which Brown Lake developed. Perched lakes are formed via geological processes.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
This cemented layer is known as 'coffee rock' and it prevents rainwater from escaping the depression, percolating through to the regional aquifer, forming a perched lake. The sand at Brown Lake is quartz sand and the yellow-brown colouring of the sand is caused by the sesquioxide coating on the quartz grains. Podzol soil supports the health and growth of the vegetation at Brown Lake.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
The sand at Brown Lake is quartz sand and the yellow-brown colouring of the sand is caused by the sesquioxide coating on the quartz grains. Podzol soil supports the health and growth of the vegetation at Brown Lake. Developed from quartz-rich sand, podzol soil is sandy in texture and is characterised as a well-aerated, well-drained and acidic soil.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
Developed from quartz-rich sand, podzol soil is sandy in texture and is characterised as a well-aerated, well-drained and acidic soil. The soil is also nutrient deficient, which is largely due to leaching. Localities around Brown Lake. Encompassing Brown Lake are three townships; Dunwich, Amity and Point Lookout. Hydrology.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
The soil is also nutrient deficient, which is largely due to leaching. Localities around Brown Lake. Encompassing Brown Lake are three townships; Dunwich, Amity and Point Lookout. Hydrology. As a perched lake, Brown Lake contains high levels of dissolved organic matter, resulting in the water system being acidic in nature; possessing a PH level less than 6.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
Hydrology. As a perched lake, Brown Lake contains high levels of dissolved organic matter, resulting in the water system being acidic in nature; possessing a PH level less than 6. The high level of dissolved organic content contributes to the water colour of Brown Lake; staining the lake a brownish tea colour; characterising the lake as dystrophic.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
The high level of dissolved organic content contributes to the water colour of Brown Lake; staining the lake a brownish tea colour; characterising the lake as dystrophic. Water systems receive nutrients from the sediment surrounding the ecosystem and at Brown Lake, the sand and soil that support the ecological community possess a low nutrient supply; characterising the lake as oligotrophic.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
Perched lakes are recharged and replenished via rainfall infiltration. Accordingly, pro-longed periods of low rainfall often lead to decreased water levels however, studies show that Brown Lake’s water level has been relatively stable; remaining at a normative level due to the large rainfall infiltration that occurred during the January 1975 cyclonic event.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
The small fluctuation in water level that does occur at Brown lake is most likely a result of water seeping through the lakebed. Aquatic fauna. Brown Lake supports a diverse population of aquatic fauna; inhabiting macroinvertebrates, fish and decapod crustacea.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
Flora. The vegetation surrounding Brown Lake is composed of riparian grass and small plant species; characterising the ecosystem as a coastal wet heathland and shrub-dominated area however, there is some presence of larger trees. Fish migration. Up until 10 years ago, Brown Lake was a fish-less wetland.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
Fish migration. Up until 10 years ago, Brown Lake was a fish-less wetland. Both natural and physical disruptions to the ecosystem have contributed to two fish species migrating to the lake; the &quot;Gambusia holbrooki&quot; and &quot;Hypseleotris galii&quot;. A natural disruption that has contributed to the migration of the fish species is Charles Darwin's (1882) 'duck feet theory'.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
The concept posits that eggs belonging to marine life can be transported from one ecosystem to another via plant material that has become attached to a waterbird's feet or mouth; depositing eggs as they roam between wetlands. Natural hydrological processes have also contributed to the fish migrating to Brown Lake.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
Natural hydrological processes have also contributed to the fish migrating to Brown Lake. Storm events and major flooding can often force egg dispersal, as bodies of water transport and deposit colonists. Physical disruptions that have contributed to the fish species migrating to Brown Lake are associated with human activity.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
The recreational boating that occurs at Brown Lake is a contributing factor to fish migration, as boats passing through the ecosystem that have visited other water systems on North Stradbroke Island either accidentally or deliberately transport eggs and live cargo into the lake.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
In 2014 a large bushfire occurred near Brown Lake and a fire-fighter helicopter landed at the ecosystem to suck up water; utilising the lake as a source for water bombs to extinguish the fire. It is theorised that this helicopter accidentally deposited live fish into Brown Lake from its last filling point. Invasive species.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
Contemporary research revealed that the species' mosquito-repelling ability was no greater than the native marine life that fed on the insect; classifying the fish as a pest. The introduction of this pest species is impacting the aquatic fauna at Brown Lake through competition and predation; threatening the biodiversity and equilibrium of the ecosystem. &quot;Lepironia articulata&quot;.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
The flower on the plant is reddish-brown in colour, cylindrical in shape and points sideways. The species plays a significant role in the functioning of the Brown Lake ecosystem, as the submerged parts of &quot;Lepironia articulata&quot; provide a habitat for the macroinvertebrates and fish present at Brown lake.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
The species plays a significant role in the functioning of the Brown Lake ecosystem, as the submerged parts of &quot;Lepironia articulata&quot; provide a habitat for the macroinvertebrates and fish present at Brown lake. Also, decaying &quot;Lepironia articulata&quot; is a valuable food source for Brown Lake's fauna. Aboriginal significance.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
The Aboriginal people of the Brown Lake area, the Quandamooka people, associate the area very strongly with women and children; only women can speak for Brown Lake and women are responsible by Law to care for manage the lake and its resources. Brown Lake is also a ceremonial place at which women-only, ritualistic activities take place.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
For example, the Rainbow Serpent, which is a symbol of water, fertility and well-being in aboriginal culture, is known to inhabit Brown Lake and &quot;as a sign of respect to this spirit and to the old ancestors watching over the lake, the Quandamooka women would ask permission before they would enter the lake.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
Ripples on the water meant permission was denied, while a smooth lake meant women and children were free to enter&quot;. Environmental threats. Brown Lake is a popular tourist destination at which a range of recreational activities take place, including picnics, barbecues, camping, boating and swimming.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
Consequently, mining is a frequent occurrence in the area encompassing Brown Lake, negatively impacting the environment through habitat degradation, pollution and excessive withdrawal of water, which can potentially lead to loss of lakes due to ruptures at the base of the groundwater aquifer.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
Bushfires and fire management practices, such as hazard reduction back burning, threaten Brown Lake’s ecosystem. The fauna and flora of Brown Lake can be heavily impacted through the raised temperatures, habitat destruction and siltation that occurs during fire processes.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
The Queensland Government and Quandamooka Yoolooburrabee Aboriginal Corporation (GYAC) have included Brown Lake in a protected area expansion strategy that will combine traditional and contemporary management strategies; acknowledging the value of the intimate knowledge indigenous populations possess of the land and sea.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
The introduction of traditional management practices is evident through the first planned cultural burn at Brown Lake. In 2020, in order &quot;reduce fuel and aid recovery of culturally significant plant species&quot; an all-women team from the Quandamooka Yoolooburrabee Aboriginal Corporation and Queensland Parks and Wildlife Service engaged in a cultural burn.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: Australia
coordinates: lat: -27.49
lon: 153.4325
Location. Hadley Upland is to the east of Marguerite Bay in Graham Land on the Fallières Coast of the Antarctic Peninsula. Godfrey Upland is to the south, Traffic Circle, Mercator Ice Piedmont and Mobiloil Inlet are to the east, Solberg Inlet and Joerg Peninsula are to the north east and Walton Peak is to the north. Gibbs Glacier flows along the northeast side of the upland.

Geographic entities mentioned:
surface_form: Walton Peak
instance_of: Mountain
coordinates: lat: -68.15
lon: -66.8
Further surveys in 1948 by the FIDS have identified this ridge as the feature first sighted in 1909 and named &quot;Ile Pavie&quot; or &quot;Cap Pavie&quot; by the FrAE under Charcot, but the name Red Rock Ridge is now too firmly established to alter. The name Pavie Ridge has been assigned to the prominent rocky ridge at 68°34'S, 66°59'W. Safety Col.

Geographic entities mentioned:
surface_form: Pavie Ridge
instance_of: Mountain
coordinates: lat: -68.5666667
lon: -66.9833333
First roughly surveyed in 1936-37 by the BGLE under John Rymill, and resurveyed in 1948-49 by the FIDS. The name was apparently first used by members of the RARE, 1947-48, under Finn Ronne, and the FIDS, and derives from its location near Neny Fjord, and its resemblance to the Swiss Matterhorn. Black Thumb.

Geographic entities mentioned:
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
surface_form: matterhorn
instance_of: Mountain
coordinates: lat: -71.855
lon: 8.3297222222222
Bertrand Ice Piedmont, Rymill Bay and Neny Fjord are on the northwest side. Snowshoe Glacier and Remus Glacier flow into Neny Fjord. Romulus Glacier and Martin Glacier flow into Rymill Bay. Other features and nearby features, from north to south, include the Blackwall Mountains, Neny Matterhorn, Black Thumb, Mount Lupa, Mount Medina, Mount Cortes and Mount Ptolemy. Exploration and name.

Geographic entities mentioned:
surface_form: medina
instance_of: Mountain
coordinates: lat: -68.45
lon: -66.25
surface_form: mount medina
instance_of: Mountain
coordinates: lat: -68.45
lon: -66.25
surface_form: mount cortes
instance_of: Mountain
coordinates: lat: -68.4833
lon: -66.1
surface_form: matterhorn
instance_of: Mountain
coordinates: lat: -71.855
lon: 8.3297222222222
surface_form: neny matterhorn
instance_of: Mountain
coordinates: lat: -68.3333
lon: -66.85
surface_form: ptolemy
instance_of: Mountain
coordinates: lat: -68.55
lon: -65.9667
surface_form: mount ptolemy
instance_of: Mountain
coordinates: lat: -68.55
lon: -65.9667
surface_form: black thumb
instance_of: Mountain
coordinates: lat: -68.4167
lon: -66.8833
surface_form: lupa
instance_of: Mountain
coordinates: lat: -68.4333
lon: -66.7167
surface_form: mount lupa
instance_of: Mountain
coordinates: lat: -68.4333
lon: -66.7167
Photographed by RARE in November 1947 (trimetrogon air photography). Surveyed by FIDS, 1958. Named by UK-APC after Pedro de Medina (1493-1567), Spanish Cosmographer Royal, who wrote Arte de Navegar (Valladolid, 1545), an important manual of navigation. Mount Cortés. A mainly ice-covered mountain high on the southwest side of Gibbs Glacier in southern Graham Land.

Geographic entities mentioned:
surface_form: medina
instance_of: Mountain
coordinates: lat: -68.45
lon: -66.25
surface_form: pedro
instance_of: Mountain
coordinates: lat: -63.9667
lon: -61.8333
Photographed by RARE, November 1947 (trimetrogon air photography). Surveyed from the ground by FIDS, December 1958. Named by the UK Antarctic Place-Names Committee (UK-APC) for Martín Cortés de Albacar, Spanish author of &quot;Arte de Navegar&quot; (Sevilla, 1551), an important manual of navigation. Mount Ptolemy. An isolated block mountain with four main summits, the highest rising to.

Geographic entities mentioned:
surface_form: cortés
instance_of: Mountain
coordinates: lat: -68.4833
lon: -66.1
Hadley Upland. Hadley Upland () is a triangular shaped remnant plateau with an undulating surface, in southern Graham Land, Antarctica. It is bounded by Windy Valley and Martin Glacier, Gibbs Glacier and Lammers Glacier. Location. Hadley Upland is to the east of Marguerite Bay in Graham Land on the Fallières Coast of the Antarctic Peninsula.

Geographic entities mentioned:
surface_form: gibbs
instance_of: Mountain
coordinates: lat: -73.81667
lon: 162.93333
surface_form: windy valley
instance_of: Valley
coordinates: lat: -68.6167
lon: -66.8333
surface_form: martin
instance_of: Mountain
coordinates: lat: -69.6667
lon: -62.9833
Godfrey Upland is to the south, Traffic Circle, Mercator Ice Piedmont and Mobiloil Inlet are to the east, Solberg Inlet and Joerg Peninsula are to the north east and Walton Peak is to the north. Gibbs Glacier flows along the northeast side of the upland. Windy Valley and Lammers Glacier define the south side. Bertrand Ice Piedmont, Rymill Bay and Neny Fjord are on the northwest side.

Geographic entities mentioned:
surface_form: gibbs
instance_of: Mountain
coordinates: lat: -73.81667
lon: 162.93333
Exploration and name. The existence of this upland was known to the United States Antarctic Service (USAS), 1939–41, Finn Ronne and Carl R. Eklund having travelled along Lammer Glacier and Gibbs Glacier in January 1941. The upland was surveyed by the Falkland Islands Dependencies Survey (FIDS) in 1948–50 and 1958.

Geographic entities mentioned:
surface_form: gibbs
instance_of: Mountain
coordinates: lat: -73.81667
lon: 162.93333
Mount Medina. A prominent ice-covered mountain high which rises from the northeast part of Hadley Upland and overlooks the head of Gibbs Glacier. Photographed by RARE in November 1947 (trimetrogon air photography). Surveyed by FIDS, 1958. Named by UK-APC after Pedro de Medina (1493-1567), Spanish Cosmographer Royal, who wrote Arte de Navegar (Valladolid, 1545), an important manual of navigation.

Geographic entities mentioned:
surface_form: gibbs
instance_of: Mountain
coordinates: lat: -73.81667
lon: 162.93333
surface_form: hadley upland
instance_of: Landform
coordinates: lat: -68.4833
lon: -66.4
Named by UK-APC after Pedro de Medina (1493-1567), Spanish Cosmographer Royal, who wrote Arte de Navegar (Valladolid, 1545), an important manual of navigation. Mount Cortés. A mainly ice-covered mountain high on the southwest side of Gibbs Glacier in southern Graham Land. It is separated from Hadley Upland by a col high high. Photographed by RARE, November 1947 (trimetrogon air photography).

Geographic entities mentioned:
surface_form: gibbs
instance_of: Mountain
coordinates: lat: -73.81667
lon: 162.93333
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
Hadley Upland. Hadley Upland () is a triangular shaped remnant plateau with an undulating surface, in southern Graham Land, Antarctica. It is bounded by Windy Valley and Martin Glacier, Gibbs Glacier and Lammers Glacier. Location. Hadley Upland is to the east of Marguerite Bay in Graham Land on the Fallières Coast of the Antarctic Peninsula.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
surface_form: hadley upland
instance_of: Landform
coordinates: lat: -68.4833
lon: -66.4
Godfrey Upland is to the south, Traffic Circle, Mercator Ice Piedmont and Mobiloil Inlet are to the east, Solberg Inlet and Joerg Peninsula are to the north east and Walton Peak is to the north. Gibbs Glacier flows along the northeast side of the upland. Windy Valley and Lammers Glacier define the south side. Bertrand Ice Piedmont, Rymill Bay and Neny Fjord are on the northwest side.

Geographic entities mentioned:
surface_form: windy valley
instance_of: Valley
coordinates: lat: -68.6167
lon: -66.8333
First observed by Finn Ronne and Carl Eklund of the United States Antarctic Service, 1939-41, from their sledge route through the Traffic Circle. Named by UK-APC after Claudius Ptolemy (2nd century A.D.), Egyptian mathematician, astronomer and geographer, who introduced the system of coordinates of latitude and longitude for fixing positions on the earth's surface. Windy Valley.

Geographic entities mentioned:
surface_form: ptolemy
instance_of: Mountain
coordinates: lat: -68.55
lon: -65.9667
The upland was surveyed by the Falkland Islands Dependencies Survey (FIDS) in 1948–50 and 1958. It was named by the UK Antarctic Place-Names Committee (UK-ADC) after John Hadley, an English mathematician who, at the same time as Thomas Godfrey, independently invented the quadrant (the forerunner of the sextant), in 1730–31. Red Rock Ridge.

Geographic entities mentioned:
surface_form: thomas
instance_of: Mountain
coordinates: lat: -71.01666667
lon: 64.6
Resurveyed in 1948-49 by the FIDS, and so named by them because the black cliffs of the mountains facing Rymill Bay remain snow free throughout the year. Little Thumb. A small isolated rock tower, high, on the south side of Neny Fjord, standing close south of The Spire at the northwest end of the Blackwall Mountains. First surveyed in 1936 by the BGLE under John Rymill.

Geographic entities mentioned:
surface_form: the spire
instance_of: Mountain
coordinates: lat: -68.3
lon: -66.88333333
Windy Valley. A glacier-filled valley opening onto the north part of Mikkelsen Bay and providing access via its head to the plateau, Lammers Glacier and the Traffic Circle area. So named by the BGLE under John Rymill, 1934-37, because of the strong winds which descend from the high plateau and blow out of this valley with great force.

Geographic entities mentioned:
surface_form: strong
instance_of: Mountain
coordinates: lat: -70.583333333333
lon: -62.75
Hadley Upland. Hadley Upland () is a triangular shaped remnant plateau with an undulating surface, in southern Graham Land, Antarctica. It is bounded by Windy Valley and Martin Glacier, Gibbs Glacier and Lammers Glacier. Location. Hadley Upland is to the east of Marguerite Bay in Graham Land on the Fallières Coast of the Antarctic Peninsula.

Geographic entities mentioned:
surface_form: hadley upland
instance_of: Landform
coordinates: lat: -68.4833
lon: -66.4
Location. Hadley Upland is to the east of Marguerite Bay in Graham Land on the Fallières Coast of the Antarctic Peninsula. Godfrey Upland is to the south, Traffic Circle, Mercator Ice Piedmont and Mobiloil Inlet are to the east, Solberg Inlet and Joerg Peninsula are to the north east and Walton Peak is to the north. Gibbs Glacier flows along the northeast side of the upland.

Geographic entities mentioned:
surface_form: hadley upland
instance_of: Landform
coordinates: lat: -68.4833
lon: -66.4
Mount Cortés. A mainly ice-covered mountain high on the southwest side of Gibbs Glacier in southern Graham Land. It is separated from Hadley Upland by a col high high. Photographed by RARE, November 1947 (trimetrogon air photography). Surveyed from the ground by FIDS, December 1958.

Geographic entities mentioned:
surface_form: hadley upland
instance_of: Landform
coordinates: lat: -68.4833
lon: -66.4
Bertrand Ice Piedmont, Rymill Bay and Neny Fjord are on the northwest side. Snowshoe Glacier and Remus Glacier flow into Neny Fjord. Romulus Glacier and Martin Glacier flow into Rymill Bay. Other features and nearby features, from north to south, include the Blackwall Mountains, Neny Matterhorn, Black Thumb, Mount Lupa, Mount Medina, Mount Cortes and Mount Ptolemy. Exploration and name.

Geographic entities mentioned:
surface_form: martin
instance_of: Mountain
coordinates: lat: -69.6667
lon: -62.9833
Charted and named by the BGLE under Rymill, 1934-37. Mount Lupa. A flat- topped, ice-covered mountain over high, standing between Romulus Glacier and Martin Glacier close east-southeast of Black Thumb and east of the head of Rymill Bay. First roughly surveyed in 1936 by the BGE under Rymill. Resurveyed in 1948-49 by the FIDS who applied the name.

Geographic entities mentioned:
surface_form: martin
instance_of: Mountain
coordinates: lat: -69.6667
lon: -62.9833
surface_form: black thumb
instance_of: Mountain
coordinates: lat: -68.4167
lon: -66.8833
Surveyed in 1936 by the BGLE under John Rymill, who so named it because of its color. Further surveys in 1948 by the FIDS have identified this ridge as the feature first sighted in 1909 and named &quot;Ile Pavie&quot; or &quot;Cap Pavie&quot; by the FrAE under Charcot, but the name Red Rock Ridge is now too firmly established to alter.

Geographic entities mentioned:
surface_form: pavie
instance_of: Mountain
coordinates: lat: -68.5666667
lon: -66.9833333
surface_form: pavie
instance_of: Mountain
coordinates: lat: -68.5666667
lon: -66.9833333
Rocktown (Georgia). Rocktown, Georgia is the colloquial name for an outcropping of sandstone boulders on the Appalachian Plateau in northwest Georgia. It consists of several acres of large sandstone boulders; the average size is high. Every boulder has its unique features, all with great foot and hand holds, and are very popular with climbers.

Geographic entities mentioned:
surface_form: Appalachian Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 40
lon: -78
It has about 2,700 inhabitants. Geography. Horka nad Moravou is located about north of Olomouc. It lies in a flat landscape in the Upper Morava Valley. The market town is situated on the right bank of the Morava River. A large part of the municipal territory lies within the Litovelské Pomoraví Protected Landscape Area. History. The first written mention of Horka nad Moravou is from 1250.

Geographic entities mentioned:
surface_form: Upper Morava Valley
instance_of: Valley
countries: Czech Republic
coordinates: lat: 49.29417
lon: 17.45179
Raspberry Formation. The Raspberry Formation is a stratigraphic unit of Miocene age in northwestern British Columbia, Canada. Name. The Raspberry Formation takes its name from Raspberry Pass, a mountain pass cutting through the central portion of the Mount Edziza volcanic complex. Geology.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
Geology. The Raspberry Formation has a volume of, making it the third most voluminous geological formation comprising the Mount Edziza volcanic complex. It varies in elevation from less than along the Mess Creek Escarpment to near Armadillo Peak. The Raspberry Formation is overlain conformably by the Little Iskut Formation.

Geographic entities mentioned:
surface_form: Armadillo Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5383
lon: -130.56
He is buried in Oakwood Cemetery, Niagara Falls, alongside Annie Edson Taylor. Early life. Graham was born in Wilmington, Delaware in December 1850, although much of his childhood was spent in Canada, near Hamilton on Lake Ontario shores where he learned to swim. At the age of 14, he moved to Philadelphia where he became a cooper.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Lemberg (Nahe). The Lemberg is a hill on the river Nahe between the villages of Niederhausen (Nahe), Oberhausen an der Nahe and Feilbingert. At 422 metres, it is the highest hill on the Nahe. Linguistic researchers believe the derivation of the name Lemberg is &quot;Lindberg&quot; (&quot;lime hill&quot;) and local poets call it the &quot;King of the Nahegau&quot; (&quot;König des Nahegaus&quot;).

Geographic entities mentioned:
surface_form: lemberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.1509
lon: 8.74888
surface_form: lemberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.817
lon: 9.13225
surface_form: lemberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.7817
lon: 7.7679
surface_form: lemberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.9181
lon: 9.30861
At 422 metres, it is the highest hill on the Nahe. Linguistic researchers believe the derivation of the name Lemberg is &quot;Lindberg&quot; (&quot;lime hill&quot;) and local poets call it the &quot;King of the Nahegau&quot; (&quot;König des Nahegaus&quot;). The magmatic rock, porphyry, which is found here points to its volcanic origin.

Geographic entities mentioned:
surface_form: lemberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.1509
lon: 8.74888
surface_form: lemberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.817
lon: 9.13225
surface_form: lemberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.7817
lon: 7.7679
surface_form: lemberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.9181
lon: 9.30861
As of the 2020 census, the city had a population of 58,874. History. Located along the shores of Lake St. Clair and inhabited by French settlers as early as 1710, during which time the area was referred to as &quot;L'anse Creuse&quot;, the future St. Clair Shores would remain mainly a rural farming area populated by largely French and German immigrant families into the early 20th century.

Geographic entities mentioned:
surface_form: Lake St. Clair
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.450265
lon: -82.67572
All that remained of the once grand amusement park was its large, ornate lakefront dance coliseum, which for years thereafter was relegated to use as a marina storage facility and marine supply store until it, too, was destroyed by fire. Geography. St. Clair Shores is in southern Macomb County, on the western side of Lake St. Clair.

Geographic entities mentioned:
surface_form: Lake St. Clair
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.450265
lon: -82.67572
Used for its modern meaning of &quot;gambrel-roofed house&quot;, the term does not reflect the fact that housing styles in Dutch-founded communities in New York evolved over time. In the Hudson Valley, for example, the use of brick, or brick and stone is perhaps more characteristic of Dutch Colonial houses than is their use of a gambrel roof.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Geumdangsan. Geumdangsan () is a mountain in Pyeongchang County, Gangwon Province, South Korea. It has an elevation of.

Geographic entities mentioned:
surface_form: geumdangsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 35.11666667
lon: 126.88333333
Grove Lake (Clay and Otter Tail counties, Minnesota). Grove Lake is a lake in Clay and Otter Tail counties, in the U.S. state of Minnesota. Grove Lake was named for the grove on the lake island within the lake.

Geographic entities mentioned:
surface_form: grove lake
instance_of: Lake
countries: United States
coordinates: lat: 46.632222222222
lon: -96.16
surface_form: grove lake
instance_of: Lake
countries: United States
coordinates: lat: 45.6
lon: -95.1875
Whereas most of the former German and Czech settlements of Lower Silesia and the County of Kladsko were repopulated by Poles from regions east of the Curzon line and from war-devastated central Poland after World War II, Czarny Bór and nearby Borówno were settled by a group of Gorals. These Gorals from the Podhale region created a new home here as well as in the nearby village of Krajanów.

Geographic entities mentioned:
surface_form: Podhale
instance_of: Valley
countries: Poland
coordinates: lat: 49.4793
lon: 20.0291
Austurdalur. Austurdalur (&quot;east valley&quot;) is a valley in interior Skagafjörður, Iceland. The Austari-Jökulsá, one of the two sources of one of the Héraðsvötn's forks, runs through it. The only residence in the valley is at Bústaðir, and there is a church at Ábær. Geography.

Geographic entities mentioned:
surface_form: austurdalur
instance_of: Valley
countries: Iceland
coordinates: lat: 65.3213024251
lon: -18.9617686693
Geography. The is a notable feature of Austurdalur's landscape and it runs somewhat to the west along the middle of the valley, although the valley is rather narrow. Inside the valley, the river runs around sandbanks, but when it arrives in, it forms a very deep gorge, which it rushes through all the way down until it joins the Vestari-Jökulsá, and together they form the.

Geographic entities mentioned:
surface_form: austurdalur
instance_of: Valley
countries: Iceland
coordinates: lat: 65.3213024251
lon: -18.9617686693
Grüner See (Hundelshausen). Grüner See is a lake in Hundelshausen, Hesse, Germany. At an elevation of, its surface area is ca.. Origin. The Green Lake, which is partially surrounded by steep slopes, was formed in 1940 when an abandoned open-cast mining pit from a gypsum quarry filled with groundwater, precipitation, and surface water. Its green color is due to its abundance of phytoplankton.

Geographic entities mentioned:
surface_form: grüner see
instance_of: Lake
countries: Germany
coordinates: lat: 51.2956
lon: 9.85417
Memorial Hall. The hall was built in 1919 on land donated by Arthur Moon as a memorial to the 1914–18 war. Timber was felled on Mount Karioi, milled at Armstrong's mill at Te Mata, carted by Te Uku farmers and erected by J. Munro of Raglan. Dressing rooms were added later and used for a library, and Plunket room.

Geographic entities mentioned:
surface_form: Karioi
instance_of: Mountain
countries: New Zealand
coordinates: lat: -37.864806
lon: 174.801583
The name Sutatenza comes from Chibcha and means either &quot;Cloud behind the anchovy&quot; or &quot;Descending to the house of the &quot;cacique&quot;. History. In the time before the Spanish conquest, Sutatenza, situated in the Tenza Valley to the east of the Altiplano Cundiboyacense, was ruled by a &quot;cacique&quot; called Tenzuzucá or Tenzucá, loyal to the &quot;zaque&quot; of Hunza.

Geographic entities mentioned:
surface_form: Tenza Valley
instance_of: Valley
countries: Colombia
coordinates: lat: 5.08333333
lon: -73.41666667
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877
Father Santiago kept a journal in which he noted seeing &quot;Temecula... an Indian village&quot;. The trip included the Lake Elsinore area and the Temecula Valley. 1800–1900. Little is known about the early 1800s because Temecula records were destroyed in the fire that followed the 1906 San Francisco earthquake.

Geographic entities mentioned:
surface_form: Lake Elsinore
instance_of: Lake
countries: United States
coordinates: lat: 33.660069444444
lon: -117.35183888889
General Stephen W. Kearny's men. Subsequently, in January 1847, José Lugo with Cahuilla Indians came to the Temecula Valley in pursuit of the Luiseño Indians and killed an unknown number, about 40–100 of them, reportedly, in the canyon just west of the current Vail Lake Dam. As American settlers moved into the area after the war, conflict with the native tribes increased.

Geographic entities mentioned:
surface_form: Vail Lake
instance_of: Lake
countries: United States
coordinates: lat: 33.496111111111
lon: -116.97611111111
In 1915, the first paved, two-lane county road was built through Temecula. By 1947, the Vail Ranch contained over. In 1948, the Vail family built a dam to catch the Temecula Creek water and created Vail Lake. Through the mid-1960s, the economy of the Temecula Valley centered around the Vail Ranch; the cattle business and agriculture were the stimuli for most business ventures.

Geographic entities mentioned:
surface_form: Temecula Creek
instance_of: Watercourse
countries: United States
coordinates: lat: 33.4742
lon: -117.141
surface_form: Vail Lake
instance_of: Lake
countries: United States
coordinates: lat: 33.496111111111
lon: -116.97611111111