Sarmila/GeoWiki-Features huggingface dataset:
Nordend. Nordend (meaning &quot;north end&quot; in German) is a northern peak of the Monte Rosa Massif. Nordend is the fourth highest peak of the massif, after the Dufourspitze (4,634 m), the Dunantspitze (4,632 m) and the Grenzgipfel (4,618 m).

Geographic entities mentioned:
surface_form: Dufourspitze
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.936666666667
lon: 7.8666666666667
surface_form: Dunantspitze
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.936944444444
lon: 7.8677777777778
surface_form: Grenzgipfel
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.93675
lon: 7.868
surface_form: grenzgipfel
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.93675
lon: 7.868
Nordend. Nordend (meaning &quot;north end&quot; in German) is a northern peak of the Monte Rosa Massif. Nordend is the fourth highest peak of the massif, after the Dufourspitze (4,634 m), the Dunantspitze (4,632 m) and the Grenzgipfel (4,618 m).

Geographic entities mentioned:
surface_form: nordend
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.942222222222
lon: 7.87
Nordend. Nordend (meaning &quot;north end&quot; in German) is a northern peak of the Monte Rosa Massif. Nordend is the fourth highest peak of the massif, after the Dufourspitze (4,634 m), the Dunantspitze (4,632 m) and the Grenzgipfel (4,618 m).

Geographic entities mentioned:
surface_form: nordend
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.942222222222
lon: 7.87
surface_form: nordend
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.942222222222
lon: 7.87
Lake Novozero. Lake Novozero (Ozero Novozero,), is a lake in Belozersky District in Vologda Oblast, Russia. The lake has the island Ognenny Ostrov which now holds a high-security penal institution.

Geographic entities mentioned:
surface_form: ozero novozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 59.937222222222
lon: 37.256944444444
surface_form: novozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 59.937222222222
lon: 37.256944444444
surface_form: novozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 59.937222222222
lon: 37.256944444444
surface_form: lake novozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 59.937222222222
lon: 37.256944444444
Lake Novozero. Lake Novozero (Ozero Novozero,), is a lake in Belozersky District in Vologda Oblast, Russia. The lake has the island Ognenny Ostrov which now holds a high-security penal institution.

Geographic entities mentioned:
surface_form: novozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 59.937222222222
lon: 37.256944444444
surface_form: lake novozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 59.937222222222
lon: 37.256944444444
Bridal Falls, British Columbia. Bridal Falls is a community in the Fraser Valley of British Columbia, located east of Rosedale and immediately adjacent to the on-ramps for the Agassiz-Rosedale Bridge, which connects the Trans-Canada Highway (Highway 1) at Bridal Falls to Agassiz, on Highway 9. Bridal Falls is mostly a highway services community, with several truck stops and restaurants.

Geographic entities mentioned:
surface_form: Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
Among those killed was the leader of the group, Lassaad Sassi, a former Tunisian policeman who had spent time in Afghanistan and headed a terror network based in Milan, Italy. Sassi's group had reportedly established training camps in the mountains in Djebel Ressas and Boukornine south of the Tunisian capital.

Geographic entities mentioned:
surface_form: Djebel Ressas
instance_of: Mountain
countries: Tunisia
coordinates: lat: 36.6
lon: 10.33333333
Starting from mid-February, the division was part of the Soviet reserve force during the German Operation Frühlingserwachen, east of Lake Balaton, in which the 6th SS Panzer Army was trying to get through Soviet defenses. On March 16, 1945, the Wehrmacht's offensive was stopped, and an offensive on Vienna was launched immediately afterwards.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
Kovanoor. Kovanoor is a village in Thanjavur district, Tamil Nadu, India. This is a very small village situated between two tributaries of Kaveri Rivers (Aralaru & Thirumalairajan). This village is situated 3 km east of Nachiyar Koil near Kumbakonam. Nachiarkoil is one of the 108 Sri Vaishnava Divya Desams. Many Alwars have composed songs the ruling Deity of Nachiar Koil, Sri Sinivasa Perumal.

Geographic entities mentioned:
surface_form: Kaveri Rivers
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
Geography. According to the United States Census Bureau, the village has a total area of, all land. The village of Senecaville is located two miles west of Senecaville Lake. The lake is a man-made reservoir created in 1937 for flood control and water conservation, and is a popular fishing and recreation destination, the third largest lake in Ohio.

Geographic entities mentioned:
surface_form: Senecaville Lake
instance_of: Lake
countries: United States
coordinates: lat: 39.925
lon: -81.435277777778
Kedron River. The Kedron River is a short river of New Zealand's Southern Alps, located some north of Lake Sumner. It flows northeast from Lake Man, close to the peak of Mount Lakeman. It reaches the Doubtful River after just. The river's entire length is within the Lake Sumner Forest Park. The river is one of the headwaters of the Waiau River.

Geographic entities mentioned:
surface_form: Lake Sumner
instance_of: Lake
countries: New Zealand
coordinates: lat: -42.7006
lon: 172.217
Geology. In southern Washington state, the Cascade Range, which sits south of the dacitic Garibaldi Volcanic Belt, spans from British Columbia in Canada to Lassen Peak in northern California in the United States. Volcanoes in the range have been produced by subduction of the Juan de Fuca tectonic plate under the North American Plate.

Geographic entities mentioned:
surface_form: Garibaldi Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5283
lon: -126.113
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Martin's Hot Springs. West Crater forms part of the Quaternary Marble Mountain-Trout Creek Hill volcanic field in southern Washington state, formed by small basaltic and basaltic andesite shield volcanoes and cinder cones. This field encompasses an area of, running from Marble Mountain to the area to the south of Trout Creek Hill. Located south of Mount St.

Geographic entities mentioned:
surface_form: Trout Creek Hill
instance_of: Mountain
countries: United States
coordinates: lat: 45.8365
lon: -121.995
surface_form: marble mountain
instance_of: Mountain
countries: United States
coordinates: lat: 58.64139
lon: -136.30333
surface_form: marble mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.7309
lon: -75.161
West Crater forms part of the Quaternary Marble Mountain-Trout Creek Hill volcanic field in southern Washington state, formed by small basaltic and basaltic andesite shield volcanoes and cinder cones. This field encompasses an area of, running from Marble Mountain to the area to the south of Trout Creek Hill. Located south of Mount St. Helens, it extends for and has a width of.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: st. helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
In addition to the lava flows, hornblende andesite can also be found near West Crater to the northwest of the Trout Creek Hill. Scientists think West Crater erupted during the Holocene epoch, about 8,000 years before present. Its lava flows intermix with tephra from an eruption of Mount St. Helens and tephra from the climactic eruption of Mount Mazama about 7,700 years ago.

Geographic entities mentioned:
surface_form: Mount Mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
surface_form: mount mazama
instance_of: Lake
countries: United States
coordinates: lat: 42.943611111111
lon: -122.10666666667
surface_form: mount st. helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: st. helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
Helens. A monogenetic volcanic field, it consists of 13 basaltic to andesitic volcanic edifices that vary from 360,000 years old to 2,000 years old. They appear as a series of isolated lava flows emplaced as single units, except for the deposits at Bare Mountain, South Soda Peaks, and West Crater where deposits are more complex.

Geographic entities mentioned:
surface_form: bare mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.675277777778
lon: -75.073888888889
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
surface_form: bare mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.3037
lon: -72.5314
Its lava flows intermix with tephra from an eruption of Mount St. Helens and tephra from the climactic eruption of Mount Mazama about 7,700 years ago. Within the Marble Mountain-Trout Creek Hill field, only two other volcanoes have erupted during the Holocene: the volcanic cone near Hackamore Creek and a phreatic crater at Bare Mountain's summit.

Geographic entities mentioned:
surface_form: bare mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.675277777778
lon: -75.073888888889
surface_form: marble mountain
instance_of: Mountain
countries: United States
coordinates: lat: 58.64139
lon: -136.30333
surface_form: marble mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.7309
lon: -75.161
surface_form: bare mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.3037
lon: -72.5314
surface_form: trout creek hill
instance_of: Mountain
countries: United States
coordinates: lat: 45.8365
lon: -121.995
It has a summit crater with a width of and a depth of. West Crater's lava dome formed on the floor of a glacial cirque, and has a similar size to the lava dome formed after the 1980 eruption of Mount St. Helens. West Crater has erupted at least two large lava flows within the Holocene epoch, about 8,000 years before present, each of which extend about from the volcano.

Geographic entities mentioned:
surface_form: mount st. helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: st. helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
It reaches an elevation of. The volcano was registered with the United States Geographic Names Information System in 1979. West Crater and the rest of the Marble Mountain-Trout Creek Hill field can be accessed by roads in the Gifford Pinchot National Forest and Mount St. Helens National Volcanic Monument. Washington Route 503 and Forest Service Route 90 lie to the east of Woodland.

Geographic entities mentioned:
surface_form: mount st. helens national volcanic monument
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: st. helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
surface_form: marble mountain
instance_of: Mountain
countries: United States
coordinates: lat: 58.64139
lon: -136.30333
surface_form: marble mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.7309
lon: -75.161
surface_form: trout creek hill
instance_of: Mountain
countries: United States
coordinates: lat: 45.8365
lon: -121.995
It consists of mostly monogenetic scoria cones, each of which produced three or four lava flows. There are at least 22 cones, and all volcanic landforms older than 12,000 years have been glaciated, the oldest the Soda Peaks basalt lava flows, dated to 0.36 million years old. The West Crater-Soda Peaks zone covers an area of, to the southeast of Mount St. Helens.

Geographic entities mentioned:
surface_form: mount st. helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: st. helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
West Crater's dome reaches an elevation of, with a diameter of. It has a summit crater with a width of and a depth of. The dome still possesses a lobe of lava at the bottom of this summit crater. West Crater's lava dome formed on the floor of a glacial cirque, and has a similar size to the lava dome formed after the 1980 eruption of Mount St. Helens. Eruptive history.

Geographic entities mentioned:
surface_form: mount st. helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: st. helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
West Crater. West Crater is a small lava dome with associated lava flows in southern Washington, United States. Located in Skamania County, it rises to an elevation of, and forms part of the Cascade Volcanic Arc. It is also part of the Marble Mountain-Trout Creek Hill volcanic field, a little-known Quaternary volcanic field in the southern Cascades of Washington state.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
Located in Skamania County, it rises to an elevation of, and forms part of the Cascade Volcanic Arc. It is also part of the Marble Mountain-Trout Creek Hill volcanic field, a little-known Quaternary volcanic field in the southern Cascades of Washington state. The area can be hiked, and can be accessed by roads in the Gifford Pinchot National Forest.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: marble mountain
instance_of: Mountain
countries: United States
coordinates: lat: 58.64139
lon: -136.30333
surface_form: marble mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.7309
lon: -75.161
surface_form: trout creek hill
instance_of: Mountain
countries: United States
coordinates: lat: 45.8365
lon: -121.995
Emplaced into canyons on the sides of the crater, the flows are being eroded by local streams. The lava dome likely formed before the lava flows erupted. Geography and access. West Crater lies in Skamania County, in the U.S. state of Washington. It reaches an elevation of. The volcano was registered with the United States Geographic Names Information System in 1979.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
West Crater and the rest of the Marble Mountain-Trout Creek Hill field can be accessed by roads in the Gifford Pinchot National Forest and Mount St. Helens National Volcanic Monument. Washington Route 503 and Forest Service Route 90 lie to the east of Woodland. West Crater can be accessed by traveling north on the Wind River highway and following Forest Service road 54. Geology.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
The Washington Cascades consist of Cenozoic era volcanic and intrusive rocks, and they can be divided into two segments based on age and rock type: the Western Cascades (formed between 50 and 5 million years ago) and the High Cascades (produced within the past 5 million years).

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
In the Wind River area, the Cascades sit atop Cenozoic era lava flows and volcaniclastic deposits, which have a calc-alkaline composition. Divided into the Ohanapecosh Formation, Eagle Creek Formation (Washington), Yakima Basalt, and Quaternary basalt flows, they show variable thickness and topographies.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Divided into the Ohanapecosh Formation, Eagle Creek Formation (Washington), Yakima Basalt, and Quaternary basalt flows, they show variable thickness and topographies. The Cascade Arc formed during the Oligocene epoch, and by the late Miocene epoch there was a low but broad gap between the Washington segment of the arc and Cascade volcanoes in Oregon.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Martin's Hot Springs. West Crater forms part of the Quaternary Marble Mountain-Trout Creek Hill volcanic field in southern Washington state, formed by small basaltic and basaltic andesite shield volcanoes and cinder cones. This field encompasses an area of, running from Marble Mountain to the area to the south of Trout Creek Hill. Located south of Mount St.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
surface_form: marble mountain
instance_of: Mountain
countries: United States
coordinates: lat: 58.64139
lon: -136.30333
surface_form: marble mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.7309
lon: -75.161
surface_form: trout creek hill
instance_of: Mountain
countries: United States
coordinates: lat: 45.8365
lon: -121.995
West Crater. West Crater is a small lava dome with associated lava flows in southern Washington, United States. Located in Skamania County, it rises to an elevation of, and forms part of the Cascade Volcanic Arc. It is also part of the Marble Mountain-Trout Creek Hill volcanic field, a little-known Quaternary volcanic field in the southern Cascades of Washington state.

Geographic entities mentioned:
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
The area can be hiked, and can be accessed by roads in the Gifford Pinchot National Forest. One of 13 volcanic cones in the West Crater-Soda Peaks zone, which covers an area of, West Crater is part of a monogenetic volcanic field with basaltic to andesitic volcanic edifices that vary from 360,000 years old to 2,000 years old. It has a summit crater with a width of and a depth of.

Geographic entities mentioned:
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
Helens. West Crater has erupted at least two large lava flows within the Holocene epoch, about 8,000 years before present, each of which extend about from the volcano. Emplaced into canyons on the sides of the crater, the flows are being eroded by local streams. The lava dome likely formed before the lava flows erupted. Geography and access. West Crater lies in Skamania County, in the U.S.

Geographic entities mentioned:
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
West Crater and the rest of the Marble Mountain-Trout Creek Hill field can be accessed by roads in the Gifford Pinchot National Forest and Mount St. Helens National Volcanic Monument. Washington Route 503 and Forest Service Route 90 lie to the east of Woodland. West Crater can be accessed by traveling north on the Wind River highway and following Forest Service road 54. Geology.

Geographic entities mentioned:
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
The western slope of the Wind River valley is shaped like a fault scarp, and it seems to be aligned with Trout Creek Hill, suggesting a potential fault line there that trends to the northwest. West Crater may also be part of this fault, as both it and Trout Creek Hill appear to be aligned with the lower Wind River and St. Martin's Hot Springs.

Geographic entities mentioned:
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
surface_form: trout creek hill
instance_of: Mountain
countries: United States
coordinates: lat: 45.8365
lon: -121.995
They appear as a series of isolated lava flows emplaced as single units, except for the deposits at Bare Mountain, South Soda Peaks, and West Crater where deposits are more complex. West Crater is a small lava dome, made up of andesitic lava with two large lava flows. It is not highly prominent.

Geographic entities mentioned:
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
West Crater is a small lava dome, made up of andesitic lava with two large lava flows. It is not highly prominent. The volcanic edifice has a ridge of Tertiary volcanic and intrusive rock, which lies on the southern edge of West Crater. West Crater's dome reaches an elevation of, with a diameter of. It has a summit crater with a width of and a depth of.

Geographic entities mentioned:
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
It is not highly prominent. The volcanic edifice has a ridge of Tertiary volcanic and intrusive rock, which lies on the southern edge of West Crater. West Crater's dome reaches an elevation of, with a diameter of. It has a summit crater with a width of and a depth of. The dome still possesses a lobe of lava at the bottom of this summit crater.

Geographic entities mentioned:
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
Helens. Eruptive history. West Crater has erupted at least two large lava flows since Quaternary time, each of which extend about from the volcano. Emplaced into canyons on the sides of the crater, the flows have just started to be eroded by local streams. The flows have a gray color, and they consist of a platy, olivine basalt lava interspersed with olivine phenocrysts.

Geographic entities mentioned:
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
The eastern flow has at least ten subunits with a rough surface; it was more viscous than the western flow. Both deposits have impeded soil development. In addition to the lava flows, hornblende andesite can also be found near West Crater to the northwest of the Trout Creek Hill. Scientists think West Crater erupted during the Holocene epoch, about 8,000 years before present.

Geographic entities mentioned:
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
surface_form: trout creek hill
instance_of: Mountain
countries: United States
coordinates: lat: 45.8365
lon: -121.995
Both deposits have impeded soil development. In addition to the lava flows, hornblende andesite can also be found near West Crater to the northwest of the Trout Creek Hill. Scientists think West Crater erupted during the Holocene epoch, about 8,000 years before present. Its lava flows intermix with tephra from an eruption of Mount St.

Geographic entities mentioned:
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
Within the Marble Mountain-Trout Creek Hill field, only two other volcanoes have erupted during the Holocene: the volcanic cone near Hackamore Creek and a phreatic crater at Bare Mountain's summit. These cones were likely active simultaneously, as one of the lava flows from West Crater is embedded with an andesitic lava flow from the Hackamore Creek cone.

Geographic entities mentioned:
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
Potential hazards. The human population within of West Crater is slightly more than 500 people, but more than 14,000 people live within of the volcano, and more than 2 million live within. However, the United States Geological Survey lists the threat potential from West Crater as &quot;Low/Very Low&quot;. Recreation.

Geographic entities mentioned:
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
Recreation. West Crater can be reached by traveling northwest on Wind River Road to Stabler and then following Forest Road 54 to Forest Road 34 before traveling a mile to the left. The lightly used Trail #155 West Crater runs through the area for, though it can only be hiked; use of bicycles and motorized vehicles on the trail is prohibited.

Geographic entities mentioned:
surface_form: west crater
instance_of: Landform
countries: United States
coordinates: lat: 45.874
lon: -122.084
West Crater's dome reaches an elevation of, with a diameter of. It has a summit crater with a width of and a depth of. The dome still possesses a lobe of lava at the bottom of this summit crater. West Crater's lava dome formed on the floor of a glacial cirque, and has a similar size to the lava dome formed after the 1980 eruption of Mount St. Helens. Eruptive history.

Geographic entities mentioned:
surface_form: the dome
instance_of: Mountain
countries: United States
coordinates: lat: 46.307777777778
lon: -122.1575
Their similar ages and locations imply that they resulted from the same movement of magma and were possibly fed by the same magma chambers. The lava dome likely formed before the lava flows erupted, suggested by its steep western side and the appearance of rock from the dome on the western lava flow.

Geographic entities mentioned:
surface_form: the dome
instance_of: Mountain
countries: United States
coordinates: lat: 46.307777777778
lon: -122.1575
The lava dome likely formed before the lava flows erupted, suggested by its steep western side and the appearance of rock from the dome on the western lava flow. The dome's deep depression may have formed when the dome's top collapsed as lava moved out of the volcano during the eruption of the two flows. Potential hazards.

Geographic entities mentioned:
surface_form: the dome
instance_of: Mountain
countries: United States
coordinates: lat: 46.307777777778
lon: -122.1575
surface_form: the dome
instance_of: Mountain
countries: United States
coordinates: lat: 46.307777777778
lon: -122.1575
There are a number of faults, but they show relatively little displacement. The western slope of the Wind River valley is shaped like a fault scarp, and it seems to be aligned with Trout Creek Hill, suggesting a potential fault line there that trends to the northwest. West Crater may also be part of this fault, as both it and Trout Creek Hill appear to be aligned with the lower Wind River and St.

Geographic entities mentioned:
surface_form: trout creek hill
instance_of: Mountain
countries: United States
coordinates: lat: 45.8365
lon: -121.995
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
Monte Tambura. Monte Tambura is a mountain (1,891 m) in the Alpi Apuane, in Tuscany, central Italy. It is the second highest peak in the chain after Monte Pisanino. Located on the boundary between the province of Lucca and the province of Massa-Carrara, the Tambura is part of the Natural Regional Park of the Alpi Apuane.

Geographic entities mentioned:
surface_form: Monte Pisanino
instance_of: Mountain
countries: Italy
coordinates: lat: 44.133611111111
lon: 10.214444444444
surface_form: pisanino
instance_of: Mountain
countries: Italy
coordinates: lat: 44.133611111111
lon: 10.214444444444
Monte Tambura. Monte Tambura is a mountain (1,891 m) in the Alpi Apuane, in Tuscany, central Italy. It is the second highest peak in the chain after Monte Pisanino. Located on the boundary between the province of Lucca and the province of Massa-Carrara, the Tambura is part of the Natural Regional Park of the Alpi Apuane.

Geographic entities mentioned:
surface_form: monte tambura
instance_of: Mountain
countries: Italy
coordinates: lat: 44.1072
lon: 10.2282
He designed The Playhouse, Colchester, Essex, which opened in 1929, and has been a Wetherspoon's pub since 1984. The huge and iconic Green's Playhouse in Dundee dates from 1936 and survives as a bingo hall on the Nethergate. His Edinburgh Playhouse is perhaps his least ambitious work and presumably was restrained by the Edinburgh officials keen for it not to impact on views of Calton Hill. Family.

Geographic entities mentioned:
surface_form: Calton Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.955278
lon: -3.182222
Geography. Located on the north shore of the Saint Lawrence River, between the Sainte-Marguerite and Moisie rivers, Sept-Îles lies on the shore of a deep-water bay fronted by a seven-island archipelago, about east of Baie-Comeau. The bay constitutes a natural harbour. The archipelago is under provincial jurisdiction, with some parts administered by the federal government or by individuals.

Geographic entities mentioned:
surface_form: Moisie
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.2
lon: -66.0675
Career. Kim started his career in 2003 as a field producer for NY1 News in New York City. While there, he covered several major political events, including the 2008 presidential campaigns of Hillary Clinton, Rudy Giuliani and Barack Obama. Kim later joined Hudson Valley in 2012, where he worked as a reporter. He most notably covered the deadly Metro-North crash in 2015.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
S.I. Paul et al. (2021) isolated and identified multiple strains of &quot;Bacillus subtilis&quot; (strains WS1A, YBS29, KSP163A, OA122, ISP161A, OI6, WS11, KSP151E, and S8,) from marine sponges of the Saint Martin's Island Area of the Bay of Bengal, Bangladesh. Based on their study, colony, morphological, physiological, and biochemical characteristics of &quot;Bacillus&quot; spp.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Nanchan Temple. Nanchan Temple () is a Buddhist temple located near the town of Doucun on Mount Wutai, Shanxi, China. Nanchan Temple was built in 782 during China's Tang dynasty, and its Great Buddha Hall is currently China's oldest preserved timber building extant, as wooden buildings are often prone to fire and various destruction.

Geographic entities mentioned:
surface_form: Mount Wutai
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 39.081388888889
lon: 113.56694444444
Durnesh Lough. Durnesh Lough is a sedimentary lagoon in the northwest of Ireland. It is located on the coast of south County Donegal. Geography. Durnesh Lough is located about north of Ballyshannon on the R231 road, just past the village of Rossnowlagh. It measures about long north–south and wide. Hydrology. Durnesh Lough is separated from the sea by drumlins and high sand dunes.

Geographic entities mentioned:
surface_form: durnesh lough
instance_of: Lake
countries: Ireland
coordinates: lat: 54.57083333
lon: -8.18444444
It measures about long north–south and wide. Hydrology. Durnesh Lough is separated from the sea by drumlins and high sand dunes. At one time there was a natural outflow, but that has been replaced by an artificial channel flowing to the sea, which admits some seawater. A small number of streams enter the lagoon, which has a salinity of up to 7 ppt. Natural history.

Geographic entities mentioned:
surface_form: durnesh lough
instance_of: Lake
countries: Ireland
coordinates: lat: 54.57083333
lon: -8.18444444
A small number of streams enter the lagoon, which has a salinity of up to 7 ppt. Natural history. The lagoon forms the main part of the Durnesh Lough Special Area of Conservation, other parts being the dunes, the beach, a cobble storm-beach, drumlins covered with sand and a small seawater lagoon. The margins of the lough have extensive reedbeds with common reed, bulrush and common clubrush.

Geographic entities mentioned:
surface_form: durnesh lough
instance_of: Lake
countries: Ireland
coordinates: lat: 54.57083333
lon: -8.18444444
Submerged vegetation includes tasselweed, beaked tasselweed, and the uncommon freshwater green alga &quot;Chara canescens&quot;. There are also some uncommon invertebrates among the 48 taxa recorded in the lough. Fish species in Durnesh Lough include sand goby, flounder, rudd, three-spined stickleback, sea trout and the critically endangered European eel. Otters are also present.

Geographic entities mentioned:
surface_form: durnesh lough
instance_of: Lake
countries: Ireland
coordinates: lat: 54.57083333
lon: -8.18444444
Otters are also present. Durnesh Lough is also part of the Durnesh Lough Important Bird Area. Significant species wintering here include mute swan, whooper swan, tundra swan, greater white-fronted goose and several species of duck which feed in the wet grassland adjacent to the lough.

Geographic entities mentioned:
surface_form: durnesh lough
instance_of: Lake
countries: Ireland
coordinates: lat: 54.57083333
lon: -8.18444444
Anavros. The river Anavros and Anaurus (,) is a torrent near the ancient city of Iolkos (modern-day Volos), flowing from Mount Pelion into the Pagasetic Gulf. The hero Jason was said to have lost a sandal in its waters, as he ferried the disguised goddess Hera across its stream.

Geographic entities mentioned:
surface_form: Mount Pelion
instance_of: Mountain
countries: Greece
coordinates: lat: 39.433333333333
lon: 23.05
The Dahae relied their strength completely on horseback, and thus possessed an extremely mobile force, which was able to retreat to the south of the Aral Sea when endangered. Because of this, other empires met complications in their efforts trying to control them.

Geographic entities mentioned:
surface_form: Aral Sea
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
They first migrated southeast to Bactria, but were driven away, and as a result changed their course to the west. They gradually started settling in Parthia, a region in the south-eastern part of the Caspian Sea, that almost corresponded to present-day Khorasan Province of Iran and southern Turkmenistan. The region was then under the rule of the Seleucids.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
John. Description. The lake is fed by dozens of small rivers, including the Ashuapmushuan, the Mistassini, the Peribonka, the Des Aulnaies, the Métabetchouane, and the Ouiatchouane. The towns on its shores include Alma, Dolbeau-Mistassini, Roberval, Normandin, and Saint-Félicien. Three Regional County Municipalities lie on its shores: Lac-Saint-Jean-Est, Le Domaine-du-Roy, and Maria-Chapdelaine.

Geographic entities mentioned:
surface_form: Peribonka
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.746944444444
lon: -72.103611111111
surface_form: mistassini
instance_of: Lake
countries: Canada
coordinates: lat: 51.00194444444445
lon: -73.61666666666666
Lac Saint-Jean lies within a elongated rift valley that is known as the &quot;Lac Saint-Jean Lowlands&quot;. These lowlands are an elongated flat-bottomed basin formed by the Saguenay Graben by the displacement of Grenville crystalline rocks. This basin is long and wide. This basin is bounded by normal faults running parallel to its length.

Geographic entities mentioned:
surface_form: Saguenay Graben
instance_of: Valley
countries: Canada
coordinates: lat: 48.5
lon: -71.3333
Industry was mainly forestry and agriculture. In the 20th century, pulp and paper mills and aluminum smelting rose to importance, encouraged by hydroelectric dams at Alma and on the Péribonka River. Lac Saint-Jean also has an important summer resort and sport-fishing industry.

Geographic entities mentioned:
surface_form: péribonka
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.746944444444
lon: -72.103611111111
Lac Saint-Jean. Lac Saint-Jean (,) is a large, relatively shallow lake in south-central Quebec, Canada, in the Laurentian Highlands. It is situated north of the Saint Lawrence River, into which it drains via the Saguenay River. It covers an area of, and is at its deepest point. Its name in the Innu language is Piekuakamu. Lac Saint-Jean has been also been mapped and known as Lake St. John.

Geographic entities mentioned:
surface_form: lac saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
Lac Saint-Jean (,) is a large, relatively shallow lake in south-central Quebec, Canada, in the Laurentian Highlands. It is situated north of the Saint Lawrence River, into which it drains via the Saguenay River. It covers an area of, and is at its deepest point. Its name in the Innu language is Piekuakamu. Lac Saint-Jean has been also been mapped and known as Lake St. John. Description.

Geographic entities mentioned:
surface_form: lac saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
In the 20th century, pulp and paper mills and aluminum smelting rose to importance, encouraged by hydroelectric dams at Alma and on the Péribonka River. Lac Saint-Jean also has an important summer resort and sport-fishing industry. The area is featured in the classic French-language novel Maria Chapdelaine by Louis Hémon published in 1914 and subsequently translated into twenty languages.

Geographic entities mentioned:
surface_form: lac saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
The area is featured in the classic French-language novel Maria Chapdelaine by Louis Hémon published in 1914 and subsequently translated into twenty languages. In the 1940s, during World War II, Lac Saint-Jean, along with various other regions within Canada, such as the Saguenay, Saint Helen's Island and Hull, Quebec, had prisoner-of-war camps.

Geographic entities mentioned:
surface_form: lac saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
In the 1940s, during World War II, Lac Saint-Jean, along with various other regions within Canada, such as the Saguenay, Saint Helen's Island and Hull, Quebec, had prisoner-of-war camps. Lac Saint-Jean's was numbered and remained unnamed just like most of Canada's other war prisons.

Geographic entities mentioned:
surface_form: lac saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
It consists of fragments of island arcs and continental crust accreted to the south-eastern edge of Precambrian North American, Laurentia. Lac Saint-Jean lies within a elongated rift valley that is known as the &quot;Lac Saint-Jean Lowlands&quot;. These lowlands are an elongated flat-bottomed basin formed by the Saguenay Graben by the displacement of Grenville crystalline rocks.

Geographic entities mentioned:
surface_form: lac saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
These lowlands are an elongated flat-bottomed basin formed by the Saguenay Graben by the displacement of Grenville crystalline rocks. This basin is long and wide. This basin is bounded by normal faults running parallel to its length. It extends from just west of Lac Saint-Jean along the Saguenay River to the Saint Lawrence Valley where is it truncated by St. Lawrence rift system.

Geographic entities mentioned:
surface_form: lac saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
Preserved within the down-faulted interior of the Saguenay Graben are two large eroded, isolated patches, known as &quot;outliers&quot;, of Paleozoic, Middle Ordovician, sedimentary rock composed of limestones and shales overlying Precambrian basement. The Lac-Saint-Jean outlier rests against the south wall of the graben south of Lac Saint-Jean and extends to the west of the lake.

Geographic entities mentioned:
surface_form: lac saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
These rocks have been preferentially eroded by repeated glaciations exhuming the Saguenay Graben. The Saguenay Graben that undelies Lac Saint-Jean Lowlands has controlled the deposition and the accumulation of Quaternary deposits (sand, gravel, silt, and clay), which can reach up to in thickness beneath the central lowlands.

Geographic entities mentioned:
surface_form: lac saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
As a result, as the Laurentide Ice Sheet retreated, the Saguenay Graben was flooded by marine waters to form the Laflamme Sea. As the land rose in response to considerable Post-glacial rebound, the bottom of the Saguenay Graben was blanketed by the Saguenay River with deltaic and terrestrial fluvial sediments to form the modern day Lac Saint-Jean Lowlands.

Geographic entities mentioned:
surface_form: lac saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
The lake is fed by dozens of small rivers, including the Ashuapmushuan, the Mistassini, the Peribonka, the Des Aulnaies, the Métabetchouane, and the Ouiatchouane. The towns on its shores include Alma, Dolbeau-Mistassini, Roberval, Normandin, and Saint-Félicien. Three Regional County Municipalities lie on its shores: Lac-Saint-Jean-Est, Le Domaine-du-Roy, and Maria-Chapdelaine. History.

Geographic entities mentioned:
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
It was given its French name by Jean de Quen, a Jesuit missionary who in 1647 was the first European to reach its shores. Industry on the lake was dominated by the fur trade until the 19th century. Colonization began in the Saguenay–Lac-Saint-Jean region in the early 19th century and continued intensively until the early 20th century. Industry was mainly forestry and agriculture.

Geographic entities mentioned:
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
Prisoners worked the land, including lumbering and assisting in the production of pulp and paper. Geology. The bedrock of the Saguenay-Lac-Saint-Jean region consists largely of Precambrian igneous and metamorphic rocks. They are mostly composed of high-grade metamorphic rocks, amphibolite to granulite gneiss, that are intruded by anorthosite, mangerite, charnockite, and granite plutonic rocks.

Geographic entities mentioned:
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
John. Description. The lake is fed by dozens of small rivers, including the Ashuapmushuan, the Mistassini, the Peribonka, the Des Aulnaies, the Métabetchouane, and the Ouiatchouane. The towns on its shores include Alma, Dolbeau-Mistassini, Roberval, Normandin, and Saint-Félicien. Three Regional County Municipalities lie on its shores: Lac-Saint-Jean-Est, Le Domaine-du-Roy, and Maria-Chapdelaine.

Geographic entities mentioned:
surface_form: mistassini
instance_of: Lake
countries: Canada
coordinates: lat: 51.00194444444445
lon: -73.61666666666666
The 18 African men and boys aboard swam safely ashore, but Maples was pulled down by the weight of his cassock. Legacy. In recognition of his role in East Africa, in 1901 the ship SS &quot;Chauncy Maples&quot;, the first steamship on Lake Nyasa (now Lake Malawi), was named after Maples. The ship continues to serve as a floating hospital.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
Anadia bitaeniata. &quot;Anadia bitaeniata&quot;, the two-banded anadia, is a species of lizard in the family Gymnophthalmidae. It is endemic to the Sierra de la Culata in the Andes of Venezuela.

Geographic entities mentioned:
surface_form: Sierra de la Culata
instance_of: Mountain
countries: Venezuela
coordinates: lat: 8.98694
lon: -71.25
Description. The district consists of a line of homestead complexes along the Jackson-Moran Road near the southeast corner of Grand Teton National Park, in the valley called Jackson Hole. The rural historic landscape's period of significance includes the construction of the Andy Chambers, T.A. Moulton and John Moulton farms from 1908 to the 1950s.

Geographic entities mentioned:
surface_form: Jackson Hole
instance_of: Valley
countries: United States
coordinates: lat: 43.516666666667
lon: -110.83333333333
It is a popular destination for tourists and photographers because of the historic buildings, the herds of bison, and the Teton Range rising in the background. The alluvial soil to the east of Blacktail Butte was more suitable than most locations in Jackson Hole for farming, somewhat hampered by a lack of readily available water.

Geographic entities mentioned:
surface_form: Blacktail Butte
instance_of: Mountain
countries: United States
coordinates: lat: 43.6353
lon: -110.693
Country and Spanish quadcasts (1996–2003). On December 7, 1996, the station became part of the Big City Radio trimulcast (and eventual quadcast) with other 107.1 stations in Briarcliff Manor, New York and northern New Jersey and later, the Lehigh Valley/Allentown, Pennsylvania area. WWHB and the other two multicast stations switched formats to country as &quot;Y-107&quot;.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5