Sarmila/GeoWiki-Features huggingface dataset:
Summerour Mound site. The Summerour Mound site (9FO16) is an archaeological site located in Forsyth County, Georgia. It was formerly on a floodplain of the west bank of the Chattahoochee River in northern Georgia. It is now flooded under the Buford Reservoir, also known as Lake Lanier.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Description. Located on the west bank of the upper Chattahoochee River, where the valley is constricted, Summerour Mound was likely sited on an east-west indigenous trail. Nearby were remains of a village and sites associated with later historic Cherokee people and an early prehistoric scatter site.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Ophthalmotilapia ventralis. &quot;Ophthalmotilapia ventralis&quot; is a species of cichlid endemic to Lake Tanganyika where it is only known from the southern end of the lake. It can reach a length of TL. It can also be found in the aquarium trade.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
Arthroleptis francei. &quot;Arthroleptis francei&quot; is a species of frog in the family Arthroleptidae. It is found in Mount Mulanje in southern Malawi and in Mount Namuli and Mount Mabu in northern Mozambique. Records from the Zomba Massif (Malawi) require confirmation. Common names Ruo River screeching frog and France's squeaker have been coined for it. Etymology.

Geographic entities mentioned:
surface_form: Mount Namuli
instance_of: Mountain
countries: Mozambique
coordinates: lat: -15.366666666667
lon: 37.033333333333
surface_form: Mount Mabu
instance_of: Mountain
countries: Mozambique
coordinates: lat: -16.298888888889
lon: 36.395555555556
In 2005, Housing Developers proposed to The Inyo county Board of Supervisors to build 65,000 housing units in Charleston View. This development was greeted with backlash by residents from Neighboring Pahrump, NV, whose main concern was that such development would deplete the ground water in the Pahrump Valley.

Geographic entities mentioned:
surface_form: Pahrump Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.2086
lon: -116.012
Villapinzón. Villapinzón is a municipality and town of Colombia in the Almeidas Province, part of the department of Cundinamarca. The urban centre is situated at an elevation of on the Altiplano Cundiboyacense, at a distance of from the capital Bogotá.

Geographic entities mentioned:
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877
Villapinzón borders Ventaquemada (Boyacá) and Lenguazaque in the north, Chocontá, Tibiritá and La Capilla in the south, Chocontá and Lenguazaque in the west and Ventaquemada, Turmequé and Úmbita in the east. The municipality is located in the uppermost part of the Bogotá River Basin; the origin of the river is within the municipality Villapinzón at an elevation of. Etymology.

Geographic entities mentioned:
surface_form: Bogotá River Basin
instance_of: Watercourse
countries: Colombia
coordinates: lat: 5.25
lon: -73.666666666667
Široka Planina (mountain). Široka Planina () is a mountain in southern Serbia, near the Macedonian border. The nearest town is Trgovište. Its highest peak &quot;Kopljača&quot; has an elevation of 1,345 meters above sea level.

Geographic entities mentioned:
surface_form: široka planina (mountain)
instance_of: Mountain
countries: Serbia
coordinates: lat: 42.3242
lon: 22.0339
Široka Planina (mountain). Široka Planina () is a mountain in southern Serbia, near the Macedonian border. The nearest town is Trgovište. Its highest peak &quot;Kopljača&quot; has an elevation of 1,345 meters above sea level.

Geographic entities mentioned:
surface_form: široka planina
instance_of: Mountain
countries: Serbia
coordinates: lat: 42.3242
lon: 22.0339
The feature is named after the Bulgarian folk dance Rachenitsa, in connection with the settlement of Rachenitsa in Southeastern Bulgaria. Location. The south height of the ridge is located at, which is 5.3 km south-southwest of Shaw Nunatak, 8.3 km west of Tegra Nunatak and 8.05 km northwest of Nebush Nunatak in Elgar Uplands, and 8.4 km east-northeast of Moriseni Peak in Lassus Mountains.

Geographic entities mentioned:
surface_form: Shaw Nunatak
instance_of: Mountain
coordinates: lat: -69.55
lon: -71.2
surface_form: Elgar Uplands
instance_of: Landform
coordinates: lat: -69.65
lon: -70.7167
surface_form: Moriseni Peak
instance_of: Mountain
coordinates: lat: -69.609166666667
lon: -71.470833333333
The name &quot;macOS&quot; stems from the intention to unify the operating system's name with that of iOS, watchOS and tvOS. Sierra is named after the Sierra Nevada mountain range in California and Nevada. Specifically, Lone Pine Peak is the location for macOS Sierra's default wallpaper. Its major new features concern Continuity, iCloud, and windowing, as well as support for Apple Pay and Siri.

Geographic entities mentioned:
surface_form: Lone Pine Peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.5619
lon: -118.226
This requires using a patch to modify the install image. Default wallpaper. The default desktop picture is an image of Lone Pine Peak. Siri. The user can access the Siri intelligent assistant via the Dock, the menu bar or a keyboard shortcut and results are shown in a window in the upper-right corner. Siri can send messages, search the web, find files and adjust settings.

Geographic entities mentioned:
surface_form: Lone Pine Peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.5619
lon: -118.226
Hansine Lake is located in the far north. Bell Peninsula is located in the southeastern part of the island. Mathiassen Mountain, a member of the Porsild Mountains, is the island's highest peak. The island's shape is vaguely similar to that of Newfoundland. Climate. Southampton Island has a severe subarctic climate (Köppen &quot;Dfc&quot;) which transitions into a tundra climate (&quot;ET&quot;).

Geographic entities mentioned:
surface_form: Mathiassen Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 64.83027777777778
lon: -83.60222222222221
Lake Saiful Muluk. Saiful Muluk () is a mountainous lake in northern Pakistan, located at the northern end of the Kaghan Valley, near the town of Naran in the Saiful Muluk National Park. At an elevation of 3,224 m (10,578 feet) above sea level, the lake is located above the tree line, and is one of the highest lakes in Pakistan. Location.

Geographic entities mentioned:
surface_form: Kaghan Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 34.833333
lon: 73.516667
At an elevation of 3,224 m (10,578 feet) above sea level, the lake is located above the tree line, and is one of the highest lakes in Pakistan. Location. Saiful Muluk is located in the Mansehra district of Khyber Pakhtunkhwa, about north of Naran, in the northern part of Kaghan Valley. Malika Parbat, the highest peak in the valley is near the lake.

Geographic entities mentioned:
surface_form: Kaghan Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 34.833333
lon: 73.516667
Saiful Muluk is located in the Mansehra district of Khyber Pakhtunkhwa, about north of Naran, in the northern part of Kaghan Valley. Malika Parbat, the highest peak in the valley is near the lake. The lake is accessible from the nearby town of Naran during the summer season but access during winter is limited, as heavy snowfall and landslides threaten to cutoff the lake from other regions.

Geographic entities mentioned:
surface_form: Malika Parbat
instance_of: Mountain
countries: Pakistan
coordinates: lat: 34.805902777778
lon: 73.724327777778
Physical features. Saiful Muluk was formed by glacial moraines that blocked the water of the stream passing through the valley. The Kaghan Valley was formed in the greater Pleistocene Period dating back almost 300,000 years when the area was covered with ice. Rising temperatures and receding glaciers left a large depression where glaciers once stood. Melting water collected into the lake. Ecology.

Geographic entities mentioned:
surface_form: Kaghan Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 34.833333
lon: 73.516667
Lake Saiful Muluk. Saiful Muluk () is a mountainous lake in northern Pakistan, located at the northern end of the Kaghan Valley, near the town of Naran in the Saiful Muluk National Park. At an elevation of 3,224 m (10,578 feet) above sea level, the lake is located above the tree line, and is one of the highest lakes in Pakistan. Location.

Geographic entities mentioned:
surface_form: lake saiful muluk
instance_of: Lake
countries: Pakistan
coordinates: lat: 34.876666666666665
lon: 73.69416666666666
Folklore. The Lake Saiful Muluk is named after a legendary prince from the tale titled &quot;Saiful Muluk&quot;, later on put into poem form by the Sufi poet Mian Muhammad Bakhsh. It tells the story of the Egyptian Prince Saiful Malook who fell in love with a fairy princess named Princess Badi ul-Jamal at the lake.

Geographic entities mentioned:
surface_form: lake saiful muluk
instance_of: Lake
countries: Pakistan
coordinates: lat: 34.876666666666665
lon: 73.69416666666666
Halcott is in the Catskill Mountains. The western and southern town lines are the border of Delaware County. The northern and eastern borders are the range of mountains from Bearpen Mountain to Halcott Mountain, beyond which lies the neighboring town of Lexington. The town of Halcott is basically the valley of Vly Creek, and ringed by mountains on three sides.

Geographic entities mentioned:
surface_form: Bearpen Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.2734
lon: -74.484
surface_form: Halcott Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.1801
lon: -74.4379
Most access to the town is from the south, via the Delaware County village of Fleischmanns. The pass between Bearpen and neighboring Vly Mountain is traversed by Halcott Mountain Road, an unimproved county highway which reaches at the col, making it the highest elevation free public through road in New York State. It is also the only route between Halcott and the rest of Greene County.

Geographic entities mentioned:
surface_form: Vly Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.2458
lon: -74.4483
Spitzhorn. The Spitzhorn is a mountain of the Bernese Alps, located on the border between the Swiss cantons of Bern and Valais. It lies east of Gsteig (Bern) and north of the Sanetsch lake (Valais). It belongs to the massif of the Wildhorn.

Geographic entities mentioned:
surface_form: Wildhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.354583333333
lon: 7.3608611111111
Spitzhorn. The Spitzhorn is a mountain of the Bernese Alps, located on the border between the Swiss cantons of Bern and Valais. It lies east of Gsteig (Bern) and north of the Sanetsch lake (Valais). It belongs to the massif of the Wildhorn.

Geographic entities mentioned:
surface_form: spitzhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.375027777778
lon: 7.3104444444444
Eungboksan. Eungboksan () is a mountain in the counties of Yangyang and Hongcheon, Gangwon Province, in South Korea. It has an elevation of.

Geographic entities mentioned:
surface_form: eungboksan
instance_of: Mountain
countries: South Korea
coordinates: lat: 37.8833
lon: 128.567
Description. The Sundial is situated in the &quot;Towers of the Virgin&quot;, west of Zion's park headquarters, towering above the floor of Zion Canyon and the Virgin River which drains precipitation runoff from this mountain. Its nearest higher neighbor is The West Temple, one half mile to the southeast, and Altar of Sacrifice is set approximately one mile to the north-northeast.

Geographic entities mentioned:
surface_form: The West Temple
instance_of: Mountain
countries: United States
coordinates: lat: 37.210869
lon: -113.02071
surface_form: Altar of Sacrifice
instance_of: Mountain
countries: United States
coordinates: lat: 37.225934
lon: -113.019858
surface_form: altar of sacrifice
instance_of: Mountain
countries: United States
coordinates: lat: 37.225934
lon: -113.019858
surface_form: the west temple
instance_of: Mountain
countries: United States
coordinates: lat: 37.210869
lon: -113.02071
Its nearest higher neighbor is The West Temple, one half mile to the southeast, and Altar of Sacrifice is set approximately one mile to the north-northeast. Other neighbors include The Witch Head, Bee Hive, The Sentinel, Mount Spry, Bridge Mountain, and Mount Kinesava. This geographical feature was named by the park's third superintendent, Preston P.

Geographic entities mentioned:
surface_form: The Witch Head
instance_of: Mountain
countries: United States
coordinates: lat: 37.2198
lon: -113.019
surface_form: Mount Spry
instance_of: Mountain
countries: United States
coordinates: lat: 37.221
lon: -112.964
surface_form: Mount Kinesava
instance_of: Mountain
countries: United States
coordinates: lat: 37.19804
lon: -113.0305
surface_form: mount kinesava
instance_of: Mountain
countries: United States
coordinates: lat: 37.19804
lon: -113.0305
surface_form: bridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.1355235
lon: -115.4905643
surface_form: bridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.20554
lon: -112.96605
surface_form: mount spry
instance_of: Mountain
countries: United States
coordinates: lat: 37.221
lon: -112.964
surface_form: the sentinel
instance_of: Mountain
countries: United States
coordinates: lat: 37.23054
lon: -112.98133
surface_form: the witch head
instance_of: Mountain
countries: United States
coordinates: lat: 37.2198
lon: -113.019
surface_form: bee hive
instance_of: Mountain
countries: United States
coordinates: lat: 37.2244897
lon: -112.9874313
The Sundial (Zion National Park). The Sundial is a elevation white Navajo Sandstone summit located in Zion National Park, in Washington County of southwest Utah, United States. Description.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: navajo
instance_of: Mountain
countries: United States
coordinates: lat: 37.034169444444
lon: -110.86888888889
surface_form: sundial
instance_of: Mountain
countries: United States
coordinates: lat: 47.832961
lon: -123.227692
surface_form: the sundial
instance_of: Mountain
countries: United States
coordinates: lat: 37.21526
lon: -113.023
The Sundial (Zion National Park). The Sundial is a elevation white Navajo Sandstone summit located in Zion National Park, in Washington County of southwest Utah, United States. Description.

Geographic entities mentioned:
surface_form: sundial
instance_of: Mountain
countries: United States
coordinates: lat: 47.832961
lon: -123.227692
surface_form: the sundial (zion national park)
instance_of: Mountain
countries: United States
coordinates: lat: 37.21526
lon: -113.023
Description. The Sundial is situated in the &quot;Towers of the Virgin&quot;, west of Zion's park headquarters, towering above the floor of Zion Canyon and the Virgin River which drains precipitation runoff from this mountain. Its nearest higher neighbor is The West Temple, one half mile to the southeast, and Altar of Sacrifice is set approximately one mile to the north-northeast.

Geographic entities mentioned:
surface_form: sundial
instance_of: Mountain
countries: United States
coordinates: lat: 47.832961
lon: -123.227692
surface_form: the sundial
instance_of: Mountain
countries: United States
coordinates: lat: 37.21526
lon: -113.023
Other neighbors include The Witch Head, Bee Hive, The Sentinel, Mount Spry, Bridge Mountain, and Mount Kinesava. This geographical feature was named by the park's third superintendent, Preston P. Patraw, because it had long been used as a sundial to regulate clocks in the nearby town of Grafton. The Sundial's name was officially adopted in 1934 by the U.S. Board on Geographic Names. Climate.

Geographic entities mentioned:
surface_form: sundial
instance_of: Mountain
countries: United States
coordinates: lat: 47.832961
lon: -123.227692
surface_form: sundial
instance_of: Mountain
countries: United States
coordinates: lat: 47.832961
lon: -123.227692
Board on Geographic Names. Climate. Spring and fall are the most favorable seasons to visit The Sundial. According to the Köppen climate classification system, it is located in a Cold semi-arid climate zone, which is defined by the coldest month having an average mean temperature below, and at least 50% of the total annual precipitation being received during the spring and summer.

Geographic entities mentioned:
surface_form: sundial
instance_of: Mountain
countries: United States
coordinates: lat: 47.832961
lon: -123.227692
surface_form: the sundial
instance_of: Mountain
countries: United States
coordinates: lat: 37.21526
lon: -113.023
It lies at an altitude of 3016 m, and has an area of about 270 km2 and volume of 2.64 km3. The lake's maximum length is 29 km, breadth about 18 km at its widest, and the deepest point is 13.2 m. It is the second largest lake in Kyrgyzstan after Issyk-Kul, and the largest fresh water lake in the country. Geography. High altitude Song-Köl belongs to the Naryn river basin.

Geographic entities mentioned:
surface_form: Issyk-Kul
instance_of: Lake
countries: Kyrgyzstan
coordinates: lat: 42.416666666667
lon: 77.25
surface_form: issyk-kul
instance_of: Lake
countries: Kyrgyzstan
coordinates: lat: 42.416666666667
lon: 77.25
Geography. High altitude Song-Köl belongs to the Naryn river basin. The lake sits in the central part of Song-Köl Valley surrounded by Songköl Too ridge from the north, and Borbor Alabas and Moldo Too mountains from the south. Hydrologically, the Song-Köl basin is characterized by poorly developed surface stream flows, and substantial subsurface flow.

Geographic entities mentioned:
surface_form: Songköl Too
instance_of: Mountain
countries: Kyrgyzstan
coordinates: lat: 41.877886
lon: 75.545176
surface_form: Moldo Too
instance_of: Mountain
countries: Kyrgyzstan
coordinates: lat: 41.58
lon: 74.67
surface_form: moldo too
instance_of: Mountain
countries: Kyrgyzstan
coordinates: lat: 41.58
lon: 74.67
surface_form: song-köl
instance_of: Lake
countries: Kyrgyzstan
coordinates: lat: 41.85
lon: 75.15
surface_form: songköl
instance_of: Lake
countries: Kyrgyzstan
coordinates: lat: 41.85
lon: 75.15
surface_form: songköl too
instance_of: Mountain
countries: Kyrgyzstan
coordinates: lat: 41.877886
lon: 75.545176
Song-Köl. Song-Köl (, literally &quot;following lake&quot;) is an alpine lake in northern Naryn Region, Kyrgyzstan. It lies at an altitude of 3016 m, and has an area of about 270 km2 and volume of 2.64 km3. The lake's maximum length is 29 km, breadth about 18 km at its widest, and the deepest point is 13.2 m.

Geographic entities mentioned:
surface_form: song-köl
instance_of: Lake
countries: Kyrgyzstan
coordinates: lat: 41.85
lon: 75.15
Song-Köl. Song-Köl (, literally &quot;following lake&quot;) is an alpine lake in northern Naryn Region, Kyrgyzstan. It lies at an altitude of 3016 m, and has an area of about 270 km2 and volume of 2.64 km3. The lake's maximum length is 29 km, breadth about 18 km at its widest, and the deepest point is 13.2 m.

Geographic entities mentioned:
surface_form: song-köl
instance_of: Lake
countries: Kyrgyzstan
coordinates: lat: 41.85
lon: 75.15
surface_form: naryn
instance_of: Mountain
countries: Kyrgyzstan
coordinates: lat: 41.359415
lon: 76.471226
It is the second largest lake in Kyrgyzstan after Issyk-Kul, and the largest fresh water lake in the country. Geography. High altitude Song-Köl belongs to the Naryn river basin. The lake sits in the central part of Song-Köl Valley surrounded by Songköl Too ridge from the north, and Borbor Alabas and Moldo Too mountains from the south.

Geographic entities mentioned:
surface_form: song-köl
instance_of: Lake
countries: Kyrgyzstan
coordinates: lat: 41.85
lon: 75.15
surface_form: naryn
instance_of: Mountain
countries: Kyrgyzstan
coordinates: lat: 41.359415
lon: 76.471226
The lake sits in the central part of Song-Köl Valley surrounded by Songköl Too ridge from the north, and Borbor Alabas and Moldo Too mountains from the south. Hydrologically, the Song-Köl basin is characterized by poorly developed surface stream flows, and substantial subsurface flow. Four perennial rivers - Kumbel, Aktash, Tashdöbö, and Karakeche - disgorge themselves into the lake.

Geographic entities mentioned:
surface_form: song-köl
instance_of: Lake
countries: Kyrgyzstan
coordinates: lat: 41.85
lon: 75.15
Hydrologically, the Song-Köl basin is characterized by poorly developed surface stream flows, and substantial subsurface flow. Four perennial rivers - Kumbel, Aktash, Tashdöbö, and Karakeche - disgorge themselves into the lake. In the south-east, the structural high is cut through by the river Kajyrty (in its upper course also called &quot;Song-Köl&quot;) that flows into the Naryn. Climate.

Geographic entities mentioned:
surface_form: song-köl
instance_of: Lake
countries: Kyrgyzstan
coordinates: lat: 41.85
lon: 75.15
surface_form: naryn
instance_of: Mountain
countries: Kyrgyzstan
coordinates: lat: 41.359415
lon: 76.471226
Snow cover in the lake basin persists for 180 to 200 days a year. In winter the lake surface freezes, the ice becoming as much as 1-1.2 m thick. The ice on Song-Köl begins to thaw in the middle or at the end of April, and completely disappears by late May. Ecology. In 2011, Song-Köl was designated by Kyrgyzstan as its third Wetland of International Importance for the Ramsar List.

Geographic entities mentioned:
surface_form: song-köl
instance_of: Lake
countries: Kyrgyzstan
coordinates: lat: 41.85
lon: 75.15
Afon Roe. The Afon Roe is a small river in Snowdonia in north-west Wales. Its tributary is the Afon Tafolog, which drains the eastern slopes of Drum, a mountain in the Carneddau range. The river flows through the village of Rowen before joining the River Conwy. Course. The river originates from several small streams on the southern slopes of Tal y Fan, to the east of Bwlch y Ddeufaen.

Geographic entities mentioned:
surface_form: Carneddau
instance_of: Landform
countries: United Kingdom
coordinates: lat: 53.18114
lon: -4.00297
The river flows through the village of Rowen before joining the River Conwy. Course. The river originates from several small streams on the southern slopes of Tal y Fan, to the east of Bwlch y Ddeufaen. The highest of these streams originates approximately 480 meters up just south of the western summit of Tal y Fan.

Geographic entities mentioned:
surface_form: Tal y Fan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.235169444444
lon: -3.9057611111111
The Pleiades (volcano group). The Pleiades are a volcanic group in northern Victoria Land of Antarctica. It consists of youthful cones and domes with Mount Atlas/Mount Pleiones, a small stratovolcano formed by three overlapping cones, being the dominant volcano and rising above the Evans Névé plateau.

Geographic entities mentioned:
surface_form: Evans Névé
instance_of: Landform
coordinates: lat: -72.75
lon: 164.5
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
An aeromagnetic anomaly has been correlated to the volcano group. The cones form an arcuate alignment that might reflect the existence of a wide caldera to their southeast. Geology. The Pleiades belong to the McMurdo Volcanic Group and more specifically to the Melbourne volcanic province, which extends from Mount Melbourne to The Pleiades and Malta Plateau.

Geographic entities mentioned:
surface_form: Mount Melbourne
instance_of: Mountain
coordinates: lat: -74.333333333333
lon: 164.7
surface_form: Malta Plateau
instance_of: Plateau
coordinates: lat: -72.967
lon: 167.3
surface_form: the pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
surface_form: the pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
surface_form: pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
surface_form: pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
Among the volcanoes of the McMurdo Volcanic Group are the large volcanoes Mount Overlord, Mount Melbourne and in the area of The Pleiades the Malta Plateau. Volcanic activity began about 107 million years ago. Earlier volcanic activity began during the Cretaceous, when the West Antarctic Rift System became active. The crust under the volcanic field is about thick.

Geographic entities mentioned:
surface_form: Mount Melbourne
instance_of: Mountain
coordinates: lat: -74.333333333333
lon: 164.7
surface_form: Malta Plateau
instance_of: Plateau
coordinates: lat: -72.967
lon: 167.3
surface_form: malta plateau
instance_of: Plateau
coordinates: lat: -72.967
lon: 167.3
surface_form: mount melbourne
instance_of: Mountain
coordinates: lat: -74.333333333333
lon: 164.7
surface_form: the pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
surface_form: pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
The volcanic group is named after the Pleiades star cluster in the constellation Taurus; the name was assigned to them by the New Zealand Geological Survey Antarctic Expedition. The volcanic group is formed by at least 12 steep, small volcanic cones and lava domes that emerge from the ice of Evans Neve over a long area.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
It has two poorly defined craters and consists of lava flows covered with scree and volcanic bombs when not buried under snow. Taygete Cone north of Mount Atlas appears to be a lava dome bearing traces of hydrothermal alteration and of a small crater. Apart from the lava flows which make up most of Mount Atlas, pyroclastic rocks have been encountered at The Pleiades.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
Composition. Basanite, basalt, benmoreite, hawaiite, phonolite, trachyandesite, trachyte and tristanite have been recovered from The Pleiades. These volcanic rocks define two separate sodium and potassium-rich magma suites and may originate from separate levels of the same magma chamber, different depths or through fractional crystallization.

Geographic entities mentioned:
surface_form: rich
instance_of: Mountain
coordinates: lat: -79.7833
lon: 158.8
Volcanic activity began about 107 million years ago. Earlier volcanic activity began during the Cretaceous, when the West Antarctic Rift System became active. The crust under the volcanic field is about thick. The basement underneath the volcanoes consists of Precambrian and Paleozoic sedimentary and intrusive rocks.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
Eruption history. The oldest dated rocks are 847,000 ± 12,000 years old. Eruptions took place about 825,000 years ago and emplaced trachytes in the central part of the field; even older eruptions may have occurred but are now buried underneath of snow and ice. Three more eruptions occurred in the subsequent 700,000 years before activity began to increase after 100,000 years.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
Among the volcanoes of the McMurdo Volcanic Group are the large volcanoes Mount Overlord, Mount Melbourne and in the area of The Pleiades the Malta Plateau. Volcanic activity began about 107 million years ago. Earlier volcanic activity began during the Cretaceous, when the West Antarctic Rift System became active. The crust under the volcanic field is about thick.

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
Most are nameless with the exception of the central Taygete Cone, Alcyone Cone just south of Taygete and the pair of high Mount Pleiones and c. high Mount Atlas in the southern sector. Mount Atlas and Mount Pleiones form a compound stratovolcano which is the principal volcano of The Pleiades and rises about above the ice. Mount Atlas is formed by three separate cones that rise above the ice.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
Geography and geomorphology. The Pleiades are located at the crest of the Transantarctic Mountains, away from the coast of Lady Newnes Bay, Ross Sea. The volcanoes are located between Evans Neve and the beginning of Mariner Glacier, which drains Evans Neve southeastwards towards the Ross Sea.

Geographic entities mentioned:
surface_form: crest
instance_of: Mountain
coordinates: lat: -63.40636
lon: -56.99204
surface_form: the crest
instance_of: Mountain
coordinates: lat: -63.40636
lon: -56.99204
surface_form: the pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
surface_form: pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
The other cones are partly buried by snow and some have breached or otherwise eroded craters. The volcanoes have alternatively been described as eroded or uneroded. The young appearance of the edifices indicates a young age of The Pleiades volcanoes. The volcanoes have been prospected for the possibility to generate geothermal energy but the presence of a good heat source is unlikely.

Geographic entities mentioned:
surface_form: young
instance_of: Mountain
coordinates: lat: -84.45
lon: 179.8
surface_form: young
instance_of: Mountain
coordinates: lat: -84.45
lon: 179.8
surface_form: the pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
surface_form: pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
When ice loads decreases, the evolved magmas rise to the surface. The youngest ages of 6,000 ± 6,000 and 3,000 ± 14,000 years ago have been obtained on Taygete, which together with the youthful texture of this dome indicates a young age for The Pleiades, despite the imprecise dates.

Geographic entities mentioned:
surface_form: young
instance_of: Mountain
coordinates: lat: -84.45
lon: 179.8
surface_form: the pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
surface_form: pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
The Pleiades (volcano group). The Pleiades are a volcanic group in northern Victoria Land of Antarctica. It consists of youthful cones and domes with Mount Atlas/Mount Pleiones, a small stratovolcano formed by three overlapping cones, being the dominant volcano and rising above the Evans Névé plateau.

Geographic entities mentioned:
surface_form: the pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
surface_form: pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
The volcanoes are located between Evans Neve and the beginning of Mariner Glacier, which drains Evans Neve southeastwards towards the Ross Sea. The volcanic group is named after the Pleiades star cluster in the constellation Taurus; the name was assigned to them by the New Zealand Geological Survey Antarctic Expedition.

Geographic entities mentioned:
surface_form: the pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
surface_form: pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
Most are nameless with the exception of the central Taygete Cone, Alcyone Cone just south of Taygete and the pair of high Mount Pleiones and c. high Mount Atlas in the southern sector. Mount Atlas and Mount Pleiones form a compound stratovolcano which is the principal volcano of The Pleiades and rises about above the ice. Mount Atlas is formed by three separate cones that rise above the ice.

Geographic entities mentioned:
surface_form: the pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
surface_form: pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
Taygete Cone north of Mount Atlas appears to be a lava dome bearing traces of hydrothermal alteration and of a small crater. Apart from the lava flows which make up most of Mount Atlas, pyroclastic rocks have been encountered at The Pleiades. The other cones are partly buried by snow and some have breached or otherwise eroded craters.

Geographic entities mentioned:
surface_form: the pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
surface_form: pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
A major local fault system passes northeast of the volcanoes and roughly follows the path of the Mariner Glacier, while the Lanternman Fault passes southwest of them. Some of these faults formed during the Ross Orogeny, when three terranes collided to form northern Victoria Land; The Pleiades are located on the Bowers Terrane. Faults may also govern the position of The Pleiades volcanoes.

Geographic entities mentioned:
surface_form: the pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
surface_form: pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
Some of these faults formed during the Ross Orogeny, when three terranes collided to form northern Victoria Land; The Pleiades are located on the Bowers Terrane. Faults may also govern the position of The Pleiades volcanoes. Composition. Basanite, basalt, benmoreite, hawaiite, phonolite, trachyandesite, trachyte and tristanite have been recovered from The Pleiades.

Geographic entities mentioned:
surface_form: the pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
surface_form: pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
Composition. Basanite, basalt, benmoreite, hawaiite, phonolite, trachyandesite, trachyte and tristanite have been recovered from The Pleiades. These volcanic rocks define two separate sodium and potassium-rich magma suites and may originate from separate levels of the same magma chamber, different depths or through fractional crystallization.

Geographic entities mentioned:
surface_form: the pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
surface_form: pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
The presence of pumice lapilli has been taken as evidence of very recent activity in the form of a moderate pumice eruption. Presently, only minor fumarolic activity has been reported. Future eruptions are possible and The Pleiades are not monitored, but they are also remote from any research station.

Geographic entities mentioned:
surface_form: the pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
surface_form: pleiades
instance_of: Mountain
coordinates: lat: -72.666666666667
lon: 165.5
It has a population of about 2700 people and its closest neighbours are Georgetown and Terra Cotta. Glen Williams is noted for its visual artists, artist's studios, heritage buildings, a restaurant and bakery, a community centre (Town Hall), parks, churches and homes. The Credit River flow through the hamlet, providing a habitat for animals. History.

Geographic entities mentioned:
surface_form: Credit River
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.5478
lon: -79.5808
It lies at the end of the south-eastern branch of Lake Como (the branch is named &quot;Branch of Lecco&quot; / &quot;Ramo di Lecco&quot;). The Bergamo Alps rise to the north and east, cut through by the Valsassina of which Lecco marks the southern end. The lake, narrows to form the River Adda, so bridges were built to improve road communications with Como and Milan.

Geographic entities mentioned:
surface_form: Valsassina
instance_of: Valley
countries: Italy
coordinates: lat: 45.983
lon: 9.4
Despite being in a parallel dominated by a humid continental climate (&quot;Dfb&quot;), the territory is well sheltered from the mountain ranges, and from the climatic point of view, enjoys the beneficial influences of the lake's waters and the breath of the Tivano that blows from the Valtellina from the northeast all year round in the early hours of the morning. Its absence indicates bad weather.

Geographic entities mentioned:
surface_form: Valtellina
instance_of: Valley
countries: Italy
coordinates: lat: 46.166666666667
lon: 9.8666666666667
The territory is crossed by three main streams: the Gerenzone, the Calderone and the Bione. The mountains that surround the natural, wide valley are: to the north Monte Coltignone and San Martino, to the east mount Due Mani, Pizzo d'Erna and Resegone, to the south the Magnodeno, to the west, on the right bank of the Adda River, is Mount Barro.

Geographic entities mentioned:
surface_form: Monte Coltignone
instance_of: Mountain
countries: Italy
coordinates: lat: 45.8857
lon: 9.38899
surface_form: mount Due Mani
instance_of: Mountain
countries: Italy
coordinates: lat: 45.8993607
lon: 9.4496774
surface_form: Resegone
instance_of: Mountain
countries: Italy
coordinates: lat: 45.858333333333
lon: 9.4688888888889
surface_form: Magnodeno
instance_of: Mountain
countries: Italy
coordinates: lat: 45.8392408
lon: 9.4400797
surface_form: Barro
instance_of: Mountain
countries: Italy
coordinates: lat: 45.8325
lon: 9.37916667
The city's main road is the State Road 36 of Lake Como and Spluga, which crosses the town via a dual-lane viaduct in each direction and a long tunnel of approximately 4,800 meters divided into two separate, overlapping tubes called San Martino, connecting the Lombardy capital to the Valtellina and Valchiavenna regions.

Geographic entities mentioned:
surface_form: Valtellina
instance_of: Valley
countries: Italy
coordinates: lat: 46.166666666667
lon: 9.8666666666667
surface_form: Valchiavenna
instance_of: Valley
countries: Italy
coordinates: lat: 46.25
lon: 9.4
It opened to traffic on October 25, 1999, after approximately twenty years of construction. The Lecco-Valsassina link road was opened in 2006; 11.7 km of road, almost entirely tunnel-based, connects the capital with the nearby town of Ballabio.

Geographic entities mentioned:
surface_form: Valsassina
instance_of: Valley
countries: Italy
coordinates: lat: 45.983
lon: 9.4
Mount Oakan. is a stratovolcano located in Akan National Park in Hokkaidō, Japan. Geography and geology. Mount Oakan sits in the Akan caldera northeast of Lake Akan. The volcano rises some above the surrounding terrain. The top of the volcano is above sea level. The volcanic cone is some in diameter. There are three explosion craters at the summit. At at about, there is a fumarole.

Geographic entities mentioned:
surface_form: Lake Akan
instance_of: Lake
countries: Japan
coordinates: lat: 43.451666666667
lon: 144.09861111111
surface_form: akan
instance_of: Lake
countries: Japan
coordinates: lat: 43.451666666667
lon: 144.09861111111
surface_form: akan
instance_of: Lake
countries: Japan
coordinates: lat: 43.451666666667
lon: 144.09861111111
surface_form: akan
instance_of: Mountain
countries: Japan
coordinates: lat: 43.386388888889
lon: 144.00888888889
surface_form: akan
instance_of: Mountain
countries: Japan
coordinates: lat: 43.386388888889
lon: 144.00888888889
surface_form: mount oakan
instance_of: Mountain
countries: Japan
coordinates: lat: 43.452777777778
lon: 144.16083333333
surface_form: oakan
instance_of: Mountain
countries: Japan
coordinates: lat: 43.452777777778
lon: 144.16083333333
History. Mount Oakan emerged in the Late Pleistocene dropping pumice on Minamishikata. After that, continuous lava flows formed the bulk of the volcano. In the final stages of its life, a parasitic volcano formed a lava dome at the summit. According to its name and local legend, Mount Oakan is the male counterpart to Mount Meakan on the other side of Lake Akan.

Geographic entities mentioned:
surface_form: Mount Meakan
instance_of: Mountain
countries: Japan
coordinates: lat: 43.386111111111
lon: 144.00888888889
surface_form: lake akan
instance_of: Lake
countries: Japan
coordinates: lat: 43.451666666667
lon: 144.09861111111
surface_form: akan
instance_of: Lake
countries: Japan
coordinates: lat: 43.451666666667
lon: 144.09861111111
surface_form: meakan
instance_of: Mountain
countries: Japan
coordinates: lat: 43.386111111111
lon: 144.00888888889
surface_form: akan
instance_of: Mountain
countries: Japan
coordinates: lat: 43.386388888889
lon: 144.00888888889
surface_form: mount oakan
instance_of: Mountain
countries: Japan
coordinates: lat: 43.452777777778
lon: 144.16083333333
surface_form: oakan
instance_of: Mountain
countries: Japan
coordinates: lat: 43.452777777778
lon: 144.16083333333
Mount Oakan. is a stratovolcano located in Akan National Park in Hokkaidō, Japan. Geography and geology. Mount Oakan sits in the Akan caldera northeast of Lake Akan. The volcano rises some above the surrounding terrain. The top of the volcano is above sea level. The volcanic cone is some in diameter. There are three explosion craters at the summit. At at about, there is a fumarole.

Geographic entities mentioned:
surface_form: akan
instance_of: Lake
countries: Japan
coordinates: lat: 43.451666666667
lon: 144.09861111111
surface_form: akan
instance_of: Mountain
countries: Japan
coordinates: lat: 43.386388888889
lon: 144.00888888889
Mount Oakan. is a stratovolcano located in Akan National Park in Hokkaidō, Japan. Geography and geology. Mount Oakan sits in the Akan caldera northeast of Lake Akan. The volcano rises some above the surrounding terrain. The top of the volcano is above sea level. The volcanic cone is some in diameter. There are three explosion craters at the summit. At at about, there is a fumarole.

Geographic entities mentioned:
surface_form: mount oakan
instance_of: Mountain
countries: Japan
coordinates: lat: 43.452777777778
lon: 144.16083333333
surface_form: oakan
instance_of: Mountain
countries: Japan
coordinates: lat: 43.452777777778
lon: 144.16083333333
At at about, there is a fumarole. The volcano is made mostly from non-alkali mafic volcanic rock. The main rock type is andesite and dacite. History. Mount Oakan emerged in the Late Pleistocene dropping pumice on Minamishikata. After that, continuous lava flows formed the bulk of the volcano. In the final stages of its life, a parasitic volcano formed a lava dome at the summit.

Geographic entities mentioned:
surface_form: mount oakan
instance_of: Mountain
countries: Japan
coordinates: lat: 43.452777777778
lon: 144.16083333333
surface_form: oakan
instance_of: Mountain
countries: Japan
coordinates: lat: 43.452777777778
lon: 144.16083333333
History. The shopping center was constructed in 1970 on the southwest corner of the I-215 belt route and West 3500 South (Utah State Route 171 in the Salt Lake Valley. Valley Fair Mall hosts approximately 120 in-line shops, a 13-bay, 450-seat food court, 15-screen Megaplex movie theater. In 2005 Satterfield Helm Management, Inc.

Geographic entities mentioned:
surface_form: Salt Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.6839
lon: -111.978
Benara. Benara, or Mlima Bénara, is the highest peak of Grande-Terre, Mayotte, an overseas collectivity of France in the western Indian Ocean, with a height of. Description. Benara forms part of the massif that dominates south-central Mayotte. The upper slopes of the mountain rise steeply to a triangular peak.

Geographic entities mentioned:
surface_form: benara
instance_of: Mountain
countries: France
coordinates: lat: -12.879444444444
lon: 45.163055555556
Le Portalet. Le Portalet is a mountain of the Mont Blanc massif, located west of Praz de Fort in the canton of Valais. It lies on the range between the glaciers of Trient and Saleina. It has two important subsidiary summits: Grand Clocher du Portalet (2,983 m) and Petit Clocher du Portalet (2,823 m). The latter forms a needle and is particularly hard to climb.

Geographic entities mentioned:
surface_form: le portalet
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.990305555556
lon: 7.0562777777778
Crystal Cave (Ohio). The Crystal Cave is a limestone cave located in Put-in-Bay, Ohio, located on South Bass Island in Lake Erie. In 1887, Gustav Heineman emigrated from Baden-Baden, Germany, to Put-in-Bay, Ohio, where he established a winery. In 1897 he dug a well beneath his winery and discovered a large vug at a depth of.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Strandbad Wannsee. The Strandbad Wannsee is an open-air lido on the eastern shore of Großer Wannsee lake, a large bay of the Havel river in Berlin, Germany. Opened in 1907, it is one of the largest inland lidos in Europe, with a beach that is long and wide, replenished with sand from the Baltic coast.

Geographic entities mentioned:
surface_form: Großer Wannsee
instance_of: Lake
countries: Germany
coordinates: lat: 52.4275
lon: 13.173055555556
Endu Pahakol. Endu Pahakol, or simply Endu, is a village in the Malampa Province of Vanuatu. It is located on the southeastern portion of Ambrym. The houses in the village are mainly built up of thatch huts and traditional artifacts. The village chief is and has been Miles Moses for over 30 years.

Geographic entities mentioned:
surface_form: Ambrym
instance_of: Mountain
countries: Vanuatu
coordinates: lat: -16.333333333333
lon: 168.33333333333
Spring Brook (Susquehanna River tributary). Spring Brook is a river located in central Otsego County, New York. The creek drains Arnold Lake and flows south before converging with Goodyear Lake, which is an impoundment of the Susquehanna River, by Portlandville, New York.

Geographic entities mentioned:
surface_form: Arnold Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.611388888889
lon: -75.004444444444
surface_form: Goodyear Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.507777777778
lon: -74.981666666667
Fore, County Westmeath. Fore () is a village, next to the old Benedictine Abbey ruin of Fore Abbey, situated to the north of Lough Lene in County Westmeath, in Ireland. The village, (sister parish of nearby St. Mary's Collinstown) is situated within a valley between two hills: the Hill of Ben, the Hill of Houndslow, and the Ankerland rise area.

Geographic entities mentioned:
surface_form: Lough Lene
instance_of: Lake
countries: Ireland
coordinates: lat: 53.664722222222
lon: -7.2369444444444
It is a demersal fish that lives on saltwater bottoms at depths of between. Its natural habitat is the tropical waters of the western Indian Ocean, from KwaZulu-Natal and Mozambique in Southern Africa, to coastal Tanzania and Kenya in the African Great lakes region, to Somalia in the Horn of Africa, to Karnataka and Maharashtra in India. It can grow up to in length. Description.

Geographic entities mentioned:
surface_form: African Great lakes
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
Naples Grape Festival. The Naples Grape Festival is an annual festival in Naples, New York, United States, dedicated to grapes. The town of Naples is in the center of Finger Lakes American Viticultural Area (AVA), a region known for grape-growing and wine making in the Finger Lakes area of Upstate New York. Around 80,000 people attend the festival each year.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
South Bastion Mountain. South Bastion Mountain is a peak in British Columbia, Canada. Its line parent is Develin Peak, away. It is part of the Tower of London Range of the Muskwa Ranges, in the Canadian Rockies. South Bastion Mountain is named after the South Bastion of the Tower of London.

Geographic entities mentioned:
surface_form: Develin Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 58.304722222222225
lon: -124.76416666666667