Sarmila/GeoWiki-Features huggingface dataset:
Just to the north of Lake Winterset is Cypress Gardens Boulevard. About to the west is Lake Eloise; Dollar Lake and Round Lake are just to the southeast. Although this is a large lake there is no public access to the lake shore, since it is surrounded by private property. Therefore, Lake Winterset has no public swimming areas or boat ramps.

Geographic entities mentioned:
surface_form: Lake Eloise
instance_of: Lake
countries: United States
coordinates: lat: 27.9836
lon: -81.704
surface_form: dollar lake
instance_of: Lake
countries: United States
coordinates: lat: 45.1899
lon: -117.1877
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9344286
lon: -96.9790408
surface_form: round lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.0648
lon: -75.1033
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 46.1508
lon: -86.7447
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.070277777778
lon: -74.584722222222
surface_form: dollar lake
instance_of: Lake
countries: United States
coordinates: lat: 42.724409
lon: -83.423268
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 42.934604
lon: -73.7823057
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 27.9631
lon: -81.674
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 45.036388888889
lon: -97.773055555556
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 43.531388888889
lon: -75.180277777778
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.8685
lon: -93.4925
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 48.161666666667
lon: -116.63805555556
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 45.6020431
lon: -122.4032555
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 41.837095
lon: -86.418541
surface_form: dollar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.6882
lon: -114.419
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.964444444444
lon: -96.827222222222
Therefore, Lake Winterset has no public swimming areas or boat ramps. However, the Chain of Lakes canal system links Lake Winterset to many area lakes. A canal on the west side directly links the lake to Lake Eloise. Boats can use Lake Winterset and the public may fish from private boats entering the lake.

Geographic entities mentioned:
surface_form: lake eloise
instance_of: Lake
countries: United States
coordinates: lat: 27.9836
lon: -81.704
Lake Winterset. Lake Winterset is a large natural freshwater lake on the south side of Winter Haven, Florida. This lake has a surface area and is round with an oval-shaped cove on its south end. The cove is connected to the main part of the lake by a short, wide channel.

Geographic entities mentioned:
surface_form: lake winterset
instance_of: Lake
countries: United States
coordinates: lat: 27.9745
lon: -81.682
The cove is connected to the main part of the lake by a short, wide channel. This lake is almost entirely surrounded by private residences, most of them in subdivisions, the majority of them gated subdivisions. Just to the north of Lake Winterset is Cypress Gardens Boulevard. About to the west is Lake Eloise; Dollar Lake and Round Lake are just to the southeast.

Geographic entities mentioned:
surface_form: lake winterset
instance_of: Lake
countries: United States
coordinates: lat: 27.9745
lon: -81.682
About to the west is Lake Eloise; Dollar Lake and Round Lake are just to the southeast. Although this is a large lake there is no public access to the lake shore, since it is surrounded by private property. Therefore, Lake Winterset has no public swimming areas or boat ramps. However, the Chain of Lakes canal system links Lake Winterset to many area lakes.

Geographic entities mentioned:
surface_form: lake winterset
instance_of: Lake
countries: United States
coordinates: lat: 27.9745
lon: -81.682
Although this is a large lake there is no public access to the lake shore, since it is surrounded by private property. Therefore, Lake Winterset has no public swimming areas or boat ramps. However, the Chain of Lakes canal system links Lake Winterset to many area lakes. A canal on the west side directly links the lake to Lake Eloise.

Geographic entities mentioned:
surface_form: lake winterset
instance_of: Lake
countries: United States
coordinates: lat: 27.9745
lon: -81.682
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
However, the Chain of Lakes canal system links Lake Winterset to many area lakes. A canal on the west side directly links the lake to Lake Eloise. Boats can use Lake Winterset and the public may fish from private boats entering the lake. &quot;The Hook and Bullet&quot; website says this lake contains flathead catfish, bluegill and largemouth bass.

Geographic entities mentioned:
surface_form: lake winterset
instance_of: Lake
countries: United States
coordinates: lat: 27.9745
lon: -81.682
He worked from his studios at Amritsar, Lahore (1926) and Delhi (1931). In 1946, he went back to Lahore and opened his studio at Anarkali and was working as an art director for a film when he was forced to leave the city due to partition of the country. In 1949 he settled down in Andretta (near Palampur), a remote and then little-known place in the Kangra Valley, beginning his career as a painter.

Geographic entities mentioned:
surface_form: Kangra Valley
instance_of: Valley
countries: India
coordinates: lat: 32.08638888888889
lon: 76.25333333333333
Life. Abar, a Nubian queen of the Kingdom of Kush dated to the Twenty-fifth Dynasty of Egypt, is known from a stela (Stela V) found in Kawa, Sudan, recording that she was dedicated as a sistrum player at the temple by her father, as well in a similar scene at Jebel Barkal where she appears behind her son Taharqa and from a stela from Tanis, Egypt.

Geographic entities mentioned:
surface_form: Jebel Barkal
instance_of: Mountain
countries: Sudan
coordinates: lat: 18.5368
lon: 31.8276
New Jersey Route 35 forms the western border of the CDP, leading north to Eatontown and south to Neptune City. According to the U.S. Census Bureau, the Wanamassa CDP has a total area of, including of land and of water (3.30%). Deal Lake lies along the southern edge of the community. 2010 census. The 2010 United States census counted 4,532 people, 1,648 households, and 1,229 families in the CDP.

Geographic entities mentioned:
surface_form: Deal Lake
instance_of: Lake
countries: United States
coordinates: lat: 40.2316
lon: -74.0073
Cima dell'Uomo. The Cima dell'Uomo (2,390 m) is a mountain of the Swiss Lepontine Alps, located north-west of Monte Carasso in the canton of Ticino. It lies east of the slightly higher Pizzo di Vogorno, near the southern end of the range separating the main valley of the Ticino from Valle Verzasca. The summit is accessible to hikers via several trails on the south-west side.

Geographic entities mentioned:
surface_form: Pizzo di Vogorno
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.239722222222
lon: 8.8930555555556
surface_form: Valle Verzasca
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.2582
lon: 8.8350694444444
surface_form: verzasca
instance_of: Watercourse
countries: Switzerland
coordinates: lat: 46.3908
lon: 8.74333
surface_form: verzasca
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.2582
lon: 8.8350694444444
Cima dell'Uomo. The Cima dell'Uomo (2,390 m) is a mountain of the Swiss Lepontine Alps, located north-west of Monte Carasso in the canton of Ticino. It lies east of the slightly higher Pizzo di Vogorno, near the southern end of the range separating the main valley of the Ticino from Valle Verzasca. The summit is accessible to hikers via several trails on the south-west side.

Geographic entities mentioned:
surface_form: cima dell'uomo
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.233076
lon: 8.938276
Darlington became a unitary authority in 1997; the five authorities formed a Local Enterprise Partnership in 2011, further collaboration between the five authorities lead to Tees Valley Combined Authority being created in 2016. Background. The River Tees' geographical valley is traditionally known as Teesdale. For centuries, north Tees was under the Prince-bishopric of Durham.

Geographic entities mentioned:
surface_form: Teesdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.545
lon: -1.927
Sgùrr nan Eugallt. Sgùrr nan Eugallt is the highest of a well defined group of mountains that lie south of Loch Hourn, stretching from Barrisdale to Loch Quoich. Although its summit is lower than many nearby neighbours, it is cut off from all its higher neighbours by a ring of deep glens.

Geographic entities mentioned:
surface_form: sgùrr nan eugallt
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.088219444444
lon: -5.4245805555556
Despite being in a very wild and remote area, it can be easily ascended from a ruined roadside cottage 4 km to the east of its summit, where there is limited parking space. But the road is single track and the cottage is 20 miles from the nearest main road. Due to its isolation and insufficient height to qualify for Munro's Tables, Sgùrr nan Eugallt is infrequently climbed. Ascents.

Geographic entities mentioned:
surface_form: sgùrr nan eugallt
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.088219444444
lon: -5.4245805555556
Barki Saraiya is a census town in the Sariya CD block in the Bagodar-Saria subdivision of the Giridih district in the Indian state of Jharkhand. Area overview. Giridih district is a part of the Chota Nagpur plateau, with rocky soil and extensive forests. Most of the rivers in the district flow from the west to east, except in the northern portion where the rivers flow north and north west.

Geographic entities mentioned:
surface_form: Chota Nagpur plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
Kraul Mountains. The Kraul Mountains () are a chain of mountains and nunataks that trend northeastward from Veststraumen Glacier for approximately in western Queen Maud Land, Antarctica. They were discovered by the Third German Antarctic Expedition (1938–1939), led by Captain Alfred Ritscher, and named for Captain Otto Kraul, ice pilot of the expedition.

Geographic entities mentioned:
surface_form: kraul mountains
instance_of: Mountain
coordinates: lat: -73.333333333333
lon: -14.166666666667
Kraul Mountains. The Kraul Mountains () are a chain of mountains and nunataks that trend northeastward from Veststraumen Glacier for approximately in western Queen Maud Land, Antarctica. They were discovered by the Third German Antarctic Expedition (1938–1939), led by Captain Alfred Ritscher, and named for Captain Otto Kraul, ice pilot of the expedition.

Geographic entities mentioned:
surface_form: alfred
instance_of: Mountain
coordinates: lat: -70.31133
lon: -69.23369
From 1696 onwards, records show that he was employed as a court architect in Vienna. As well as the Belvedere, Hildebrandt's most outstanding achievements include the Schloss Hof Palace, which was also commissioned by Prince Eugene, the Schwarzenberg Palace (formerly known as the Mansfeld–Fondi Palace), the Kinsky Palace, as well as the entire Göttweig Monastery estate in the Wachau Valley.

Geographic entities mentioned:
surface_form: Wachau Valley
instance_of: Valley
countries: Austria
coordinates: lat: 48.36444
lon: 15.43417
Distribution and habitat. &quot;Melaleuca sciotostyla&quot; is confined to the Cadoux, Wongan Hills and Meckering districts in the Avon Wheatbelt and Jarrah Forest biogeographic regions growing in clayey sand and laterite on scree slopes. Conservation. &quot;Melaleuca sciotostyla&quot; is listed as &quot;endangered&quot; by the Australian Government Department of the Environment.

Geographic entities mentioned:
surface_form: Wongan Hills
instance_of: Mountain
countries: Australia
coordinates: lat: -30.8
lon: 116.617
The town's economy still relies heavily on those two influences, but the development of Kicking Horse Mountain Resort, along with other outdoor adventure companies, has allowed the town to diversify into tourism. Mount 7, which is just southeast of town, is also an outdoor activity destination. The town forms part of the Golden Triangle cycle route.

Geographic entities mentioned:
surface_form: Mount 7
instance_of: Mountain
countries: Canada
coordinates: lat: 51.255
lon: -116.853
Geography. Golden is nestled in the Rocky Mountain Trench, built around the confluence of the Columbia and Kicking Horse rivers, surrounded by three different mountain ranges (most notably the Purcell Mountains and Rocky Mountains) and five national parks: Yoho National Park, Banff National Park, Jasper National Park, Glacier National Park, and Kootenay National Park.

Geographic entities mentioned:
surface_form: Rocky Mountain Trench
instance_of: Landform
Valley
countries: Canada
United States
coordinates: lat: 54.5
lon: -122.5
Creigiau Gleision. Creigiau Gleision is a mountain in Snowdonia, Wales, near Capel Curig. It is the easternmost of the high Carneddau and is separated from the others by Llyn Cowlyd. Directly across this reservoir from Creigiau Gleision is Pen Llithrig y Wrach. To the north-east it runs into the broad ridge of Cefn Cyfarwydd.

Geographic entities mentioned:
surface_form: Carneddau
instance_of: Landform
countries: United Kingdom
coordinates: lat: 53.18114
lon: -4.00297
Creigiau Gleision. Creigiau Gleision is a mountain in Snowdonia, Wales, near Capel Curig. It is the easternmost of the high Carneddau and is separated from the others by Llyn Cowlyd. Directly across this reservoir from Creigiau Gleision is Pen Llithrig y Wrach. To the north-east it runs into the broad ridge of Cefn Cyfarwydd.

Geographic entities mentioned:
surface_form: Pen Llithrig y Wrach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.142330555556
lon: -3.9210805555556
surface_form: creigiau gleision
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.1359
lon: -3.9014
Directly across this reservoir from Creigiau Gleision is Pen Llithrig y Wrach. To the north-east it runs into the broad ridge of Cefn Cyfarwydd. Creigiau Gleision affords splendid views in all directions, including northwards to the coast, and down the Ogwen Valley and Dyffryn Mymbyr towards Snowdon. In fact the mountain has three peaks, hence perhaps its plural name.

Geographic entities mentioned:
surface_form: Ogwen Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.125
lon: -4
surface_form: Dyffryn Mymbyr
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.0877
lon: -3.96494
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
surface_form: creigiau gleision
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.1359
lon: -3.9014
Creigiau Gleision. Creigiau Gleision is a mountain in Snowdonia, Wales, near Capel Curig. It is the easternmost of the high Carneddau and is separated from the others by Llyn Cowlyd. Directly across this reservoir from Creigiau Gleision is Pen Llithrig y Wrach. To the north-east it runs into the broad ridge of Cefn Cyfarwydd.

Geographic entities mentioned:
surface_form: creigiau gleision
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.1359
lon: -3.9014
map. Colin Adams, author of &quot;The Mountain Walker's Guide to Wales&quot; (Gwasg Carreg Gwalch, 2002), has reached the summit of Creigiau Gleision over 450 times. He claims that on many occasions he encountered a ghost there who has spoken to him, and although he makes no reference to this in his book, he wrote about it in 1999.

Geographic entities mentioned:
surface_form: creigiau gleision
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.1359
lon: -3.9014
Radiometric dating has yielded ages of up to 300,000years for its rocks, and it reached its present height about 200,000years ago. Several tephra layers encountered in ice cores at Mount Waesche and Byrd Station have been attributed to Mount Takahe, although some of them were later linked to eruptions of Mount Berlin instead. The tephra layers were formed by explosive or phreatomagmatic eruptions.

Geographic entities mentioned:
surface_form: Mount Waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: Mount Berlin
instance_of: Mountain
coordinates: lat: -76.055
lon: -135.825
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: mount takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
Mount Takahe is at the Bakutis Coast, eastern Marie Byrd Land, Antarctica. Bear Peninsula and the Amundsen Sea coast are north of Mount Takahe. It is an isolated mountain, and the closest other volcanoes are Mount Murphy and Toney Mountain away. No major air routes or supply roads to Antarctic stations pass close to the mountain, and some parts of the cone are accessible only by helicopter.

Geographic entities mentioned:
surface_form: Mount Murphy
instance_of: Mountain
coordinates: lat: -75.3
lon: -110.7
surface_form: Toney Mountain
instance_of: Mountain
coordinates: lat: -75.8
lon: -115.81666666667
surface_form: toney mountain
instance_of: Mountain
coordinates: lat: -75.8
lon: -115.81666666667
About 18 central volcanoes were active in Marie Byrd Land from the Miocene to the Holocene. Among the volcanic areas in Marie Byrd Land are the Flood Range with Mount Berlin, the Ames Range, the Executive Committee Range with Mount Sidley and Mount Waesche, the Crary Mountains, Toney Mountain, Mount Takahe and Mount Murphy.

Geographic entities mentioned:
surface_form: Mount Berlin
instance_of: Mountain
coordinates: lat: -76.055
lon: -135.825
surface_form: Mount Sidley
instance_of: Mountain
coordinates: lat: -77.04
lon: -126.1
surface_form: Mount Waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: Toney Mountain
instance_of: Mountain
coordinates: lat: -75.8
lon: -115.81666666667
surface_form: Mount Murphy
instance_of: Mountain
coordinates: lat: -75.3
lon: -110.7
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: mount takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: toney mountain
instance_of: Mountain
coordinates: lat: -75.8
lon: -115.81666666667
A series of eruptions about 200 years long took place at Mount Takahe 17,700years ago. These eruptions have been recorded from ice cores at the WAIS Divide and at Taylor Glacier in the McMurdo Dry Valleys, where they constrain estimates of the rate of deglaciation.

Geographic entities mentioned:
surface_form: McMurdo Dry Valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
Another eruption reported by the Global Volcanism Program may have occurred in 7050 BC. At Siple Dome, a further eruption between 10,700 and 5,600years ago is recorded and one tephra layer around 1783 BC (accompanied by increased sulfate concentrations in ice) might also come from Mount Takahe. Glass shards at Law Dome emplaced in 1552 and 1623 AD may come from this volcano as well.

Geographic entities mentioned:
surface_form: Law Dome
instance_of: Landform
coordinates: lat: -66.7333
lon: 112.833
Mount Takahe. Mount Takahe is a snow-covered shield volcano in Marie Byrd Land, Antarctica, from the Amundsen Sea. It is a mountain with parasitic vents and a caldera up to wide. Most of the volcano is formed by trachytic lava flows, but hyaloclastite is also found. Snow, ice, and glaciers cover most of Mount Takahe.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: mount takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
Mount Takahe. Mount Takahe is a snow-covered shield volcano in Marie Byrd Land, Antarctica, from the Amundsen Sea. It is a mountain with parasitic vents and a caldera up to wide. Most of the volcano is formed by trachytic lava flows, but hyaloclastite is also found. Snow, ice, and glaciers cover most of Mount Takahe.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: mount takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: amundsen
instance_of: Mountain
coordinates: lat: -67.233333333333
lon: 100.75
It is a mountain with parasitic vents and a caldera up to wide. Most of the volcano is formed by trachytic lava flows, but hyaloclastite is also found. Snow, ice, and glaciers cover most of Mount Takahe. With a volume of, it is a massive volcano; the parts of the edifice that are buried underneath the West Antarctic Ice Sheet are probably even larger.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: mount takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
The tephra layers were formed by explosive or phreatomagmatic eruptions. Major eruptions took place around 17,700years ago—possibly forming an ozone hole over Antarctica—and in the early Holocene. Mount Takahe's last eruption occurred about 7,600 years ago, and there is no present-day activity. Geography and geomorphology.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: mount takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
Geography and geomorphology. The mountain's name refers to the takahē, a flightless nearly extinct bird from New Zealand; members of the 1957–1958 Marie Byrd Land Traverse party nicknamed an aircraft that had resupplied them &quot;takahe&quot;. It was first visited in 1957–1958 and again in 1968, 1984–1985 and 1998–1999. Mount Takahe is at the Bakutis Coast, eastern Marie Byrd Land, Antarctica.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
It was first visited in 1957–1958 and again in 1968, 1984–1985 and 1998–1999. Mount Takahe is at the Bakutis Coast, eastern Marie Byrd Land, Antarctica. Bear Peninsula and the Amundsen Sea coast are north of Mount Takahe. It is an isolated mountain, and the closest other volcanoes are Mount Murphy and Toney Mountain away.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: mount takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: amundsen
instance_of: Mountain
coordinates: lat: -67.233333333333
lon: 100.75
The volcano is largely uneroded, mostly hiding the internal structure which would clarify its history.Only twelve outcrops, with a total area of less than, emerge from the ice. Based on these outcrops, lava flows with a thickness of appear to be widespread on Mount Takahe, while pyroclastic rocks such as deposits of Strombolian eruptions, lapilli tuffs and lahar deposits are less common.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: mount takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
A magnetic anomaly has also been linked to the mountain. Composition. Trachyte is the most common rock on Mount Takahe, phonolite being less common. Basanite, hawaiite, and mugearite are uncommon, but the occurrence of benmoreite and pantellerite has been reported, and some rocks have been classified as andesites.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: mount takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
In his 1990 book &quot;Volcanoes of the Antarctic Plate and Southern Oceans&quot; LeMasurier gave 310,000±90,000years ago as the oldest date for samples tested, citing unpublished K-Ar dates, but in a 2016 review of dates for Mount Takahe LeMasurier reported that none were older than 192,000years.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: mount takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
Rocks aged 192,000±6,300years old are found at the summit caldera, implying that the volcano had reached its present-day height by then. Early research indicated that most of Mount Takahe formed underneath the ice, but more detailed field studies concluded that most of the volcano developed above the ice surface.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: mount takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
The ice surface has fluctuated over the life of Mount Takahe with an increased thickness during marine isotope stages 4 and 2, explaining why units originally emplaced under ice or water now lie above the ice surface and alternate with lava flow deposits.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: mount takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
These elevated deposits were emplaced about 29,000–12,000years ago while the lava delta-like deposits are between about 70,000and 15,000years old. After it grew out of the ice, Mount Takahe increased in size through the emission of lava flows with occasional pyroclastic eruptions. Outcrops in the summit region indicate that most eruptions were magmatic, but some hydromagmatic activity occurred.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: mount takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
Cinder cones and tuff cones formed during the late stage of activity. Tephra in ice cores. Tephra layers in ice cores drilled at Byrd Station have been attributed to Mount Takahe. The volcano reaches an altitude high enough that tephras erupted from it can readily penetrate the tropopause and spread over Antarctica through the stratosphere.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: mount takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
The occurrence of several volcanic eruptions in the region about 30,000years ago has been suggested to have caused a cooling of the climate of Antarctica, but it is also possible that the growth of the ice sheets at that time squeezed magma chambers at Mount Takahe and thus induced an increase of the eruptive activity.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: mount takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
Assuming that most tephra layers at Byrd come from Mount Takahe, it has been inferred that the volcano was very active between 60,000 and 7,500 years ago, with nine eruptive periods and two pulses between 60,000 and 57,000and 40,000–14,000years ago.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: mount takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
In the latter part of the latter period hydrovolcanic eruptions became dominant at Mount Takahe, with a maximum around the time when the Wisconsin glaciation ended. It is possible that between 18,000 and 15,000years ago, either a crater lake formed in the caldera or the vents were buried by snow and ice.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: mount takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
In particular, tephra layers between 30,000and 20,000years ago have been attributed to the latter volcano. Tephra layers from Mount Takahe have also been found at Dome C, Dome F, Mount Takahe itself, Mount Waesche, Siple Dome and elsewhere in Antarctica. Apart from ice cores, tephras attributed to Mount Takahe have been found in sediment cores taken from the sea.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: mount takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: siple
instance_of: Mountain
coordinates: lat: -73.433333333333
lon: -126.66666666667
Tephra layers from Mount Takahe have also been found at Dome C, Dome F, Mount Takahe itself, Mount Waesche, Siple Dome and elsewhere in Antarctica. Apart from ice cores, tephras attributed to Mount Takahe have been found in sediment cores taken from the sea. Volcanic eruptions at Mount Takahe lack the pyroclastic flow deposits observed in other large explosive eruptions.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: mount takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: mount takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
Volcanic eruptions at Mount Takahe lack the pyroclastic flow deposits observed in other large explosive eruptions. The thickness of the Byrd ice core tephras attributed to Mount Takahe suggested that the eruptions were not large, but later research has indicated that large Plinian eruptions also occurred. A series of eruptions about 200 years long took place at Mount Takahe 17,700years ago.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: mount takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
As is the case with the present-day ozone hole, the ozone hole created by the Takahe eruptions might have altered the Antarctic climate and sped up deglaciation, which was accelerating at that time, but later research has determined that the warming was most likely not volcanically forced. Holocene and recent activity.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
Holocene and recent activity. Activity waned after this point, two hydromagmatic eruptions being recorded 13,000and 9,000years ago and a magmatic eruption 7,500years ago. This last eruption is also known from the Byrd ice core and may correspond to an eruption 8,200±5,400years ago recorded at Mount Waesche and the Takahe edifice and to two 6217 and 6231 BC tephra layers at Siple Dome.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: siple
instance_of: Mountain
coordinates: lat: -73.433333333333
lon: -126.66666666667
Tephra from a 8,200before present eruption has been recorded at Siple Dome and Mount Waesche. A 7,900before present eruption at Mount Takahe is one of the strongest eruptions at Siple Dome and Byrd Station of the last 10,000years. Another eruption reported by the Global Volcanism Program may have occurred in 7050 BC.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: mount takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: siple
instance_of: Mountain
coordinates: lat: -73.433333333333
lon: -126.66666666667
Another eruption reported by the Global Volcanism Program may have occurred in 7050 BC. At Siple Dome, a further eruption between 10,700 and 5,600years ago is recorded and one tephra layer around 1783 BC (accompanied by increased sulfate concentrations in ice) might also come from Mount Takahe. Glass shards at Law Dome emplaced in 1552 and 1623 AD may come from this volcano as well.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: mount takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
This last eruption is also known from the Byrd ice core and may correspond to an eruption 8,200±5,400years ago recorded at Mount Waesche and the Takahe edifice and to two 6217 and 6231 BC tephra layers at Siple Dome. Tephra from a 8,200before present eruption has been recorded at Siple Dome and Mount Waesche.

Geographic entities mentioned:
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: siple
instance_of: Mountain
coordinates: lat: -73.433333333333
lon: -126.66666666667
Mount Takahe is almost entirely covered by ice of the West Antarctic Ice Sheet, which rises about above sea level. A tributary of the Thwaites Glacier passes close by. There are two small glaciers on the volcano itself, on the southwestern and northern flanks. They are eroding eruption products from the summit area, and moraines have been mapped both on the western flank and in the summit caldera.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
In the latter part of the latter period hydrovolcanic eruptions became dominant at Mount Takahe, with a maximum around the time when the Wisconsin glaciation ended. It is possible that between 18,000 and 15,000years ago, either a crater lake formed in the caldera or the vents were buried by snow and ice.

Geographic entities mentioned:
surface_form: crater lake
instance_of: Lake
coordinates: lat: -62.98333333
lon: -60.66666667
Volcanic activity in Marie Byrd Land commenced about 34million years ago, but high activity began 14million years ago. A major uplifted dome, in width, is centred on the Amundsen Sea coast and is associated with the Rift. About 18 central volcanoes were active in Marie Byrd Land from the Miocene to the Holocene.

Geographic entities mentioned:
surface_form: amundsen
instance_of: Mountain
coordinates: lat: -67.233333333333
lon: 100.75
It is part of the West Antarctic Rift System along with 18 other known volcanoes. The volcano was active in the Quaternary period. Radiometric dating has yielded ages of up to 300,000years for its rocks, and it reached its present height about 200,000years ago.

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
Geology. The West Antarctic Rift System is a basin and range province similar to the Great Basin in North America; it cuts across Antarctica from the Ross Sea to the Bellingshausen Sea. The Rift became active during the Mesozoic. Owing to thick ice cover it is not clear whether it is currently active, and there is no seismic activity. Most of the Rift lies below sea level.

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
Volcanic activity in Marie Byrd Land commenced about 34million years ago, but high activity began 14million years ago. A major uplifted dome, in width, is centred on the Amundsen Sea coast and is associated with the Rift. About 18 central volcanoes were active in Marie Byrd Land from the Miocene to the Holocene.

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
Most of these volcanoes are large, capped off by a summit caldera and appear to have begun as fast-growing shield volcanoes. Later, calderas formed. Eventually, late in the history of the volcanoes parasitic vents were active. The volcanoes are all surmounted by rocks composed of trachyte, phonolite, pantellerite, or comendite.

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
A lava dome may crop out inside the caldera. Radial fissure vents are found around the volcano, and vents also occur around the caldera rim. There are at least three parasitic vents with basaltic composition on its lower flanks, with three cinder cones found on the western and southern slopes. One of these cinder cones has been described as a subdued vent.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
One of these cinder cones has been described as a subdued vent. The Jaron Cliffs are found on the southern slope. The volcano is largely uneroded, mostly hiding the internal structure which would clarify its history.Only twelve outcrops, with a total area of less than, emerge from the ice.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
As many as 25 pikas have been found in a single bear's stomach and in Changtang, 60% of the diet consisted of pikas. Where plateau pikas are absent, as in the Mustang region of Nepal, Himalayan marmots (&quot;Marmota himalayana&quot;) become the dietary staple of the bear, occurring in about half of nearly 1,000 scats.

Geographic entities mentioned:
surface_form: Changtang
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 30
lon: 90
Brown bears also co-exist with leopards (&quot;Panthera pardus&quot;) (in very small remnant wild parts of the Middle East, Jammu and Kashmir, northeastern China and the Primorsky Krai) and snow leopards (&quot;Panthera uncia&quot;) in several areas of northern central Asia and the Tibetan Plateau).

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Lough Aleck More. Lough Aleck More () is a freshwater lake in the northwest of Ireland. It is located in County Donegal in the Rosses fishery. Geography and natural history. Lough Aleck More is south of Dungloe. It measures about long north–south and wide. The lake is a trout fishing destination with resident brown trout and seasonal sea trout.

Geographic entities mentioned:
surface_form: lough aleck more
instance_of: Lake
countries: Ireland
coordinates: lat: 54.91666667
lon: -8.36555556
Operation Leap 1. Operation Leap 1 (also known as Operation Jump 1) (&quot;Operacija Skok 1&quot;) was designed to widen the salient and allow the Croatian forces to advance towards Bosansko Grahovo. By spring 1995, relatively small shifts of the line of control west of the Livanjsko field enabled the VRS and the ARSK to threaten the HV positions on Dinara and Staretina mountains.

Geographic entities mentioned:
surface_form: Staretina
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 44.0833
lon: 16.6833
In the first stage of the operation, the attacking forces were tasked with capturing the village of Crni Lug and the southern part of the pass, while the second stage was planned to capture the Mount Šator and the Crvena Zemlja ridge to the north, blocking the Bosansko Grahovo-Glamoč road and making Glamoč difficult to resupply.

Geographic entities mentioned:
surface_form: Mount Šator
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 44.157330555556
lon: 16.5897
Each year on August astrophotography hobbyists gather there due to the clear view of the night sky, a result of the villages high elevation. The municipal unit has an area of 47.306 km2. Ano Vrontou is situated in the northeastern part of the Vrontous mountains, at about 1060 m elevation. It borders on the Drama regional unit to the north and east.

Geographic entities mentioned:
surface_form: Vrontous
instance_of: Mountain
countries: Greece
coordinates: lat: 41.258
lon: 23.602
History. The finding of a Greek inscription of Roman (Imperial) times supports the conclusion that in the place of the present village there was an ancient settlement, whose residents were engaged in the exploitation of the iron mines of the mountain Vrontous.

Geographic entities mentioned:
surface_form: Vrontous
instance_of: Mountain
countries: Greece
coordinates: lat: 41.258
lon: 23.602
KLXD. KLXD is a non-commercial FM radio station that is licensed to Victorville and serves Victor Valley on the 89.5 MHz frequency. It is owned by Educational Media Foundation and broadcasts Contemporary Christian music via EMF's nationwide K-Love network. History. KLXD signed on in 1996 as KXRD, a simulcast of KLRD in Yucaipa, California, known as &quot;K-Lord&quot;.

Geographic entities mentioned:
surface_form: Victor Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.5
lon: -117.3
Alternative routes over the range included Gorman's Gap near the headwaters of Hodgson's Creek, and Hodgson's Gap via Drayton. Squatters in the Warwick district continued to search for a southern pass through the range, and in April 1847, Henry Alphen rediscovered the pass identified by Cunningham in 1827, between Mount Mitchell and Spicers Peak.

Geographic entities mentioned:
surface_form: Spicers Peak
instance_of: Mountain
countries: Australia
coordinates: lat: -28.083055555556
lon: 152.32888888889
Interest was revived after 1910 with the development of the motor car and recreational driving. Shire Councils were lobbied to repair the road, but it was not always passable.In 1925–27, communities from the Darling Downs and Fassifern Valley combined to build a road through Cunningham's Gap. Debate followed regarding whether the alternative route would go through Cunningham or Spicers Gaps.

Geographic entities mentioned:
surface_form: Fassifern Valley
instance_of: Valley
countries: Australia
coordinates: lat: -27.810944444444
lon: 152.66505555556
Course and features. The Tonalli River rises on the eastern alopes of Mount Marrup within the Tonalli Range in remote country within the Greater Blue Mountains Area World Heritage Site, and flows generally east southeast, east northeast, and then east southeast, before reaching its confluence with the Wollondilly River within Lake Burragorang in Yerranderie State Conservation Area.

Geographic entities mentioned:
surface_form: Lake Burragorang
instance_of: Lake
countries: Australia
coordinates: lat: -34
lon: 150.43333333333
The Ballantine's whisky distillery continues to operate in the estate. Transport. Alexandria sits on the former A82 main road between Glasgow and Loch Lomond. There are regular bus services on the route, and the town has a railway station on the rail line between Balloch and Glasgow Queen Street.

Geographic entities mentioned:
surface_form: Loch Lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
Migas tuhoe. &quot;Migas tuhoe&quot; is a species of mygalomorph spider endemic to New Zealand. Taxonomy. This species was described in 1968 by Cecil Wilton from a single female specimen collected near Lake Waikaremoana. The holotype is stored in Te Papa Museum under registration number AS.000119. Description. The female is recorded at 7.9mm in length. The carapace and legs are orange brown.

Geographic entities mentioned:
surface_form: Lake Waikaremoana
instance_of: Lake
countries: New Zealand
coordinates: lat: -38.766666666667
lon: 177.08333333333
Nallah Mar. Nallah Mar or Mar Canal (also known as Mar Kol) was a navigational canal running through the old city of Srinagar in the Indian union territory of Jammu and Kashmir. It connected the Brari Nambal lagoon to the Khushal Sar lake and thus provided navigability between the Dal and Aanchar lakes. It was filled up and converted to a road in the 1970s.

Geographic entities mentioned:
surface_form: Brari Nambal
instance_of: Lake
countries: India
coordinates: lat: 34.0869
lon: 74.8139
surface_form: Khushal Sar
instance_of: Lake
countries: India
coordinates: lat: 34.1115
lon: 74.7994
surface_form: Dal
instance_of: Lake
countries: India
coordinates: lat: 34.12
lon: 74.87
surface_form: Aanchar
instance_of: Lake
countries: India
coordinates: lat: 34.15
lon: 74.78333333
History. The canal was built during the reign of Sultan Zain-ul-Abidin of the Shah Mir dynasty (popularly known in Kashmir as 'Budshah'). It was considered as a lifeline of the city even up to the early part of the 20th century. However, with the arrival of motor transport, it gradually lost its sheen. As such, it was filled up to pave way for a road through the old city.

Geographic entities mentioned:
surface_form: Kashmir
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
In the 1970s, Nallah Mar was filled in and converted into a road to accommodate increasing road traffic, reflecting urban infrastructure priorities of the time but resulting in loss of drainage function and worsened flood risk. The culverting of the canal severely disrupted the hydrology of Brari Nambal and the Dal-Anchar waterway system. Architecture.

Geographic entities mentioned:
surface_form: Brari Nambal
instance_of: Lake
countries: India
coordinates: lat: 34.0869
lon: 74.8139
The culverting of the canal severely disrupted the hydrology of Brari Nambal and the Dal-Anchar waterway system. Architecture. Nallah Mar, also known as Mar Kol, was a historic canal originally constructed to connect Brari Nambal lagoon with Khushal Sar and other water bodies serving both navigation and flood control purposes.

Geographic entities mentioned:
surface_form: Brari Nambal
instance_of: Lake
countries: India
coordinates: lat: 34.0869
lon: 74.8139
surface_form: Khushal Sar
instance_of: Lake
countries: India
coordinates: lat: 34.1115
lon: 74.7994
In the beginning it was locally known as &quot;Club dels Xiflats&quot; (&quot;Club of the Dim-witted&quot; in Catalan), for at that time no one in this harbor town understood why the club's first members would engage for pleasure in rowing and sailing, the arduous task of sailors and fishermen. The RCNT's first building was destroyed during a seasonal flood of the Francolí River in 1917.

Geographic entities mentioned:
surface_form: Francolí
instance_of: Watercourse
countries: Spain
coordinates: lat: 41.398944
lon: 1.052333
His son Walter F. Dillingham (1875–1963) would also become a businessman in Oahu. His wife Emma Louise Smith Dillingham wrote a book of poetry on Diamond Head. His daughter Mary Emma (known as May) Dillingham married Walter Francis Frear (1863–1948) who became Governor of the Territory of Hawaii 1907–1913.

Geographic entities mentioned:
surface_form: Diamond Head
instance_of: Mountain
countries: United States
coordinates: lat: 21.259722222222
lon: -157.81175
Skarø. Skarø () is a Danish island south of Funen. The island covers an area of and has 26 inhabitants. It is one of the smallest islands in the South Funen Archipelago. Skarø was historically located within the Parish of Drejø. Today it is part of Svendborg Municipality within the Region of Southern Denmark. The island can be reached by ferry from Svendborg and Drejø.

Geographic entities mentioned:
surface_form: South Funen Archipelago
instance_of: Body of water
countries: Denmark
coordinates: lat: 54.939
lon: 10.454
A large salt lake, Lake Amadeus, and the subsequently-named Amadeus Basin, where it lies in central Australia, is also named after Amadeo I by the explorer Ernest Giles, who was the first European to encounter the lake, in 1872.

Geographic entities mentioned:
surface_form: Lake Amadeus
instance_of: Lake
countries: Australia
coordinates: lat: -24.75
lon: 130.91666666667