Sarmila/GeoWiki-Features huggingface dataset:
Aghaming, Manitoba. Aghaming is a community in the Canadian province of Manitoba. The community is on the Wanipigow River near the point where it flows into Lake Winnipeg. Across the river is the Hollow Water First Nation. It is administered under the &quot;Northern Affairs Act&quot; of Manitoba. Demographics.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Bouchette was discharged in 1784. By 1788 Bouchette had returned to private life in Quebec, but it was not to last long. In 1791 he returned to Lake Ontario reappointed as master and commander in the Provincial Marine and by 1802-04 was the senior officer on the lake.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
This name references iemisch, a mythological monster of native Patagonian folklore. Roth noted that the size of the fossils fit descriptions made by Tehuelche locals and by Argentine naturalist Florentino Ameghino in the 1880s. This led Roth to believe it could still be living, with a Tehuelche guide telling him that a living individual resided near Lake Buenos Aires.

Geographic entities mentioned:
surface_form: Lake Buenos Aires
instance_of: Lake
countries: Chile
Argentina
coordinates: lat: -46.4375
lon: -71.715
It is northwest of Jackson and is accessible only from the west, through Driggs, Idaho. The border with Idaho is less than five miles (8 km) due west. The resort has lodging, a spa, retail stores, and conference facilities. On the west side of the famous Teton Range, it is located northwest of the Grand Teton, and the majority of the slopes at Grand Targhee face west. Activities.

Geographic entities mentioned:
surface_form: Grand Teton
instance_of: Mountain
countries: United States
coordinates: lat: 43.7412
lon: -110.802
The reason for the abundant snowfall is twofold. First, the area is on the west slope or &quot;wet&quot; side of the Teton Range, topped by Grand Teton at and, second, because there is a moisture channel through the Rocky Mountains formed by the Snake River Plain in Idaho that channels moisture from the Pacific Ocean to the west slope of the Tetons.

Geographic entities mentioned:
surface_form: Grand Teton
instance_of: Mountain
countries: United States
coordinates: lat: 43.7412
lon: -110.802
The cartoon was released on August 8, 1953, and stars Bugs Bunny. Plot. Bugs Bunny finds himself inadvertently embroiled in a bullfighting spectacle while en route to the Coachella Valley for a carrot festival. Upon stumbling into a Spanish bullring, Bugs becomes the target of Toro the Bull, who is engaged in a confrontation with a matador.

Geographic entities mentioned:
surface_form: Coachella Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.72
lon: -116.2
Of the agricultural land, 9.3% is used for growing crops and 13.3% is pastures, while 16.8% is used for orchards or vine crops. All the water in the municipality is in lakes. The former municipality is located in the Boudry district, on a small hill above Lake Neuchâtel. Coat of arms.

Geographic entities mentioned:
surface_form: Lake Neuchâtel
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.9
lon: 6.85
It is part of the Cape Coral-Fort Myers, Florida Metropolitan Statistical Area. Located just offshore in the Gulf of Mexico, the island is just north of Sanibel Island. Captiva is accessed by a small bridge that crosses Blind Pass from Sanibel Island. There is a toll to use the causeway that goes from the mainland to Sanibel Island.

Geographic entities mentioned:
surface_form: Blind Pass
instance_of: Landform
countries: United States
coordinates: lat: 26.4758
lon: -82.1781
According to the United States Census Bureau, the Captiva CDP has a total area of, of which are land and, or 28.15%, are water. Originally part of neighboring Sanibel Island to the southeast, it was severed in 1926 when a hurricane's storm surge created a new channel, Blind Pass. The channel filled in over subsequent years, but was reopened by dredging in the summer of 2009.

Geographic entities mentioned:
surface_form: Blind Pass
instance_of: Landform
countries: United States
coordinates: lat: 26.4758
lon: -82.1781
The South Seas Island Resort entry gate is at the end of this road. Roosevelt Channel on the east side of the island, is named for Theodore Roosevelt who fished there. North Captiva Island or Upper Captiva is another island, in turn severed from Captiva in a 1921 hurricane, creating Redfish Pass. North Captiva has power from lines that originate on the north end of Captiva, and is privately owned.

Geographic entities mentioned:
surface_form: Redfish Pass
instance_of: Landform
countries: United States
coordinates: lat: 26.55316667
lon: -82.19866667
In April 1917, the Brigade &quot;Aosta&quot; was transferred to Asiago as reserve for the 20th Army Corps. In July the brigade arrived at the front and was deployed between Strigno and Cima della Caldiera, in front of Mount Ortigara. Following the Battle of Caporetto, the brigade retreated to the Col della Berretta.

Geographic entities mentioned:
surface_form: Mount Ortigara
instance_of: Mountain
countries: Italy
coordinates: lat: 46.00722222
lon: 11.50777778
Mount Rebun. is the highest point on Rebun Island in Rebun, Hokkaidō, Japan. The mountain consists of marine sedimentary rocks from the Early Cretaceous period, 149–97 million years ago. Climbing route. The trailhead for the Mount Rebun hike is in Nairo. It is a 3-hour hike with no water available.

Geographic entities mentioned:
surface_form: mount rebun
instance_of: Mountain
countries: Japan
coordinates: lat: 45.3725
lon: 141.01583333333
is the highest point on Rebun Island in Rebun, Hokkaidō, Japan. The mountain consists of marine sedimentary rocks from the Early Cretaceous period, 149–97 million years ago. Climbing route. The trailhead for the Mount Rebun hike is in Nairo. It is a 3-hour hike with no water available. The trail first passes through fields of &quot;sasa-no-ha&quot; before entering a forest of pine and birch.

Geographic entities mentioned:
surface_form: mount rebun
instance_of: Mountain
countries: Japan
coordinates: lat: 45.3725
lon: 141.01583333333
Rivière du Cinq. The rivière du Cinq (&quot;in English: river of the five&quot;) is a tributary of the west bank of Bras Saint-Victor which flows into the Chaudière River; the latter flows northward to empty on the south shore of the St. Lawrence River. Geography.

Geographic entities mentioned:
surface_form: Bras Saint-Victor
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.25889
lon: -70.82556
surface_form: Chaudière River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.742777777777775
lon: -71.2786111111111
This lake is located north of the village of East Broughton, north of route 112 and south-east of Mont Sainte-Marguerite. The Rivière du Cinq flows on the west bank of the Bras Saint-Victor in the municipality of Saint-Victor. This last river flows into the Chaudière River in Beauceville.

Geographic entities mentioned:
surface_form: Bras Saint-Victor
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.25889
lon: -70.82556
The Rivière du Cinq flows on the west bank of the Bras Saint-Victor in the municipality of Saint-Victor. This last river flows into the Chaudière River in Beauceville. The confluence of the Rivière du Cinq is located upstream from the confluence of the Prévost-Gilbert River, at north-west of center of the village of Saint-Victor and north of route 108. Toponymy.

Geographic entities mentioned:
surface_form: Chaudière River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.742777777777775
lon: -71.2786111111111
Frazier Lake. Frazier Lake is a seasonal lake in Gallatin County, Montana in the Bridger Range in south central Montana. It is located near Fairy Lake in the Gallatin National Forest and sits at an elevation of.

Geographic entities mentioned:
surface_form: Fairy Lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9044
lon: -110.959
Frazier Lake. Frazier Lake is a seasonal lake in Gallatin County, Montana in the Bridger Range in south central Montana. It is located near Fairy Lake in the Gallatin National Forest and sits at an elevation of.

Geographic entities mentioned:
surface_form: frazier lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9246
lon: -110.9735
Often the gods are Horus and Set, or on occasion Horus and Thoth. There are several examples of Barque stands from the reigns of Amenhotep III (Hermopolis), Taharqa (Jebel Barkal), and Atlanersa (Jebel Barkal) that show two river gods performing the rite. This matches a scene from the Temple at Abu Simbel from the time of Ramesses II.

Geographic entities mentioned:
surface_form: Jebel Barkal
instance_of: Mountain
countries: Sudan
coordinates: lat: 18.5368
lon: 31.8276
The culture is felt to be severely threatened. In the summer of 2008, Indigenous leaders and researchers from the University of California, Berkeley issued a report detailing the deaths of 38 Warao in the Delta Amacuro state from a mysterious illness.

Geographic entities mentioned:
surface_form: Delta Amacuro
instance_of: Body of water
countries: Venezuela
coordinates: lat: 8.7
lon: -61.15
Bukovik (Gornji Milanovac). koku8v3uqgl9p9ahfk6pws2ens1" xml:space="preserve">#REDIRECT Bukovik (central Serbia)

Geographic entities mentioned:
surface_form: bukovik
instance_of: Mountain
countries: Serbia
coordinates: lat: 43.69166667
lon: 21.63555556
surface_form: bukovik (gornji milanovac)
instance_of: Mountain
countries: Serbia
coordinates: lat: 43.9539
lon: 20.5197
Career. Lieutenant William Hunter commissioned &quot;Gaspée&quot; in January 1773. In 1775, she arrived at Quebec to take on provisions. There Colonel Guy Carleton, Lieutenant-Governor of the province of Quebec, prevailed upon Hunter to take some his men to Lake Champlain and take command of a vessel that Carleton was having built at St Johns. Lieutenant Hunter took command of.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Vérignon (; Verinhon in Classical Provençal and Verignoun in Provençal of the mistralian norm) is a commune in the Var department in the Provence-Alpes-Côte d'Azur region in southeastern France. Géography. The town is situated at the foot of the Great Canjuers Plain, at the heart of a forest of oaks. 15 square kilometres of the commune were requisitioned for the Canjuers military camp in 1970.

Geographic entities mentioned:
surface_form: Canjuers
instance_of: Plateau
countries: France
coordinates: lat: 43.70833333
lon: 6.30833333
15 square kilometres of the commune were requisitioned for the Canjuers military camp in 1970. History. Canjuers is supposed to be derived from the Latin Campus Julii (the field of Julius), preserving a folk-memory of Julius Caesar's army passing across it during the Gallic Wars. On a mountain range between Aups and Vérignon is an oppidum of the Verrucini.

Geographic entities mentioned:
surface_form: Canjuers
instance_of: Plateau
countries: France
coordinates: lat: 43.70833333
lon: 6.30833333
Parks and open spaces. London is well known for its greenery and the Parks and open spaces in the London Borough of Camden make an important contribution to this. Hampstead Heath is well known for its view over London, notably from Parliament Hill, its wild nature and its Hampstead Heath Ponds. Camden shares Regents Park with Westminster and the views from Primrose Hill are famous. Education.

Geographic entities mentioned:
surface_form: Hampstead Heath Ponds
instance_of: Group of lakes
countries: United Kingdom
coordinates: lat: 51.563
lon: -0.157
Nadzikambia. &quot;Nadzikambia&quot; (derived from their name in Chichewa) is a genus of chameleons. It includes two species of small, plesiomorphic chameleons from the Ruo Gorge forest on Mount Mulanje in Malawi and Mount Mabu in Mozambique. Initially only a single species was recognized and placed in &quot;Chamaeleo&quot;.

Geographic entities mentioned:
surface_form: Mount Mabu
instance_of: Mountain
countries: Mozambique
coordinates: lat: -16.298888888889
lon: 36.395555555556
Adolphustown. Adolphustown is a geographic area located in Greater Napanee, Ontario, Canada, on the Adolphus Reach of the Bay of Quinte in Lake Ontario. Adolphustown is now part of the town of Greater Napanee.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Hellenistic and early Roman period. Ancient Greek mathematics reached its acme during the Hellenistic and early Roman periods. Alexander the Great's conquest of the Eastern Mediterranean, Egypt, Mesopotamia, the Iranian plateau, Central Asia, and parts of India led to the spread of the Greek culture and language across these regions.

Geographic entities mentioned:
surface_form: Iranian plateau
instance_of: Plateau
countries: Iran
coordinates: lat: 36.283333
lon: 59.05
Seitz Lake is a major source of flow to Rabbit Creek (formerly known as Seitz Creek), which after exiting the mountains passes near the community of Spring Creek, meanders down Lamoille Valley, and then merges with the main branch of the Humboldt River between Halleck and Elburz, NV. The lake was named after brothers George and Edward Seitz, who were early ranchers in Pleasant Valley.

Geographic entities mentioned:
surface_form: brothers
instance_of: Mountain
countries: United States
coordinates: lat: 47.6537193
lon: -123.140575
surface_form: pleasant valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6389
lon: -77.5472
surface_form: pleasant valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6409256
lon: -114.0184307
Seitz Lake (Nevada). Seitz Lake is a glacial tarn in the Ruby Mountains, in Elko County in the northeastern part of the state of Nevada. It is located near the head of Seitz Canyon at approximately, and at an elevation of. It has an area of approximately, and a depth of up to.

Geographic entities mentioned:
surface_form: seitz lake (nevada)
instance_of: Lake
countries: United States
coordinates: lat: 40.6367
lon: -115.457
Seitz Lake (Nevada). Seitz Lake is a glacial tarn in the Ruby Mountains, in Elko County in the northeastern part of the state of Nevada. It is located near the head of Seitz Canyon at approximately, and at an elevation of. It has an area of approximately, and a depth of up to.

Geographic entities mentioned:
surface_form: seitz lake
instance_of: Lake
countries: United States
coordinates: lat: 40.6367
lon: -115.457
It has an area of approximately, and a depth of up to. Seitz Lake is a major source of flow to Rabbit Creek (formerly known as Seitz Creek), which after exiting the mountains passes near the community of Spring Creek, meanders down Lamoille Valley, and then merges with the main branch of the Humboldt River between Halleck and Elburz, NV.

Geographic entities mentioned:
surface_form: seitz lake
instance_of: Lake
countries: United States
coordinates: lat: 40.6367
lon: -115.457
A' Chràlaig. A' Chralaig () is a mountain in the Northwest Highlands of Scotland, north of Loch Cluanie and south of Glen Affric. It is a Munro with a height of. It is the highest peak along Glen Shiel and can be easily climbed from the Cluanie Inn on the A87. The eastern slopes of the mountain, are owned by the Forestry Commission and are part of the Kintail National Scenic Area.

Geographic entities mentioned:
surface_form: Loch Cluanie
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.13961
lon: -5.088876
surface_form: Glen Affric
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.283333333333
lon: -4.9333333333333
surface_form: a' chralaig
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.184186
lon: -5.154837
A' Chràlaig. A' Chralaig () is a mountain in the Northwest Highlands of Scotland, north of Loch Cluanie and south of Glen Affric. It is a Munro with a height of. It is the highest peak along Glen Shiel and can be easily climbed from the Cluanie Inn on the A87. The eastern slopes of the mountain, are owned by the Forestry Commission and are part of the Kintail National Scenic Area.

Geographic entities mentioned:
surface_form: Glen Shiel
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.2103
lon: -5.4239
It is the highest peak along Glen Shiel and can be easily climbed from the Cluanie Inn on the A87. The eastern slopes of the mountain, are owned by the Forestry Commission and are part of the Kintail National Scenic Area. Despite being the highest peak on the ridge, it is considered less interesting than the route over &quot;Stob Coire na Cràlaig&quot; to the nearby Mullach Fraoch-choire.

Geographic entities mentioned:
surface_form: Mullach Fraoch-choire
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.205379
lon: -5.155652
surface_form: mullach fraoch-choire
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.205379
lon: -5.155652
Despite being the highest peak on the ridge, it is considered less interesting than the route over &quot;Stob Coire na Cràlaig&quot; to the nearby Mullach Fraoch-choire. These two peaks may be combined with the neighbouring peaks of Sgurr nan Conbhairean and Sail Chaorainn to make the so-called &quot;Cluanie Horseshoe&quot;, although no path connects A' Chràlaig with the peaks to the east.

Geographic entities mentioned:
surface_form: sgurr nan conbhairean
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.177622
lon: -5.095407
surface_form: sail
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.571
lon: -3.242
surface_form: a' chràlaig
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.184186
lon: -5.154837
A' Chràlaig. A' Chralaig () is a mountain in the Northwest Highlands of Scotland, north of Loch Cluanie and south of Glen Affric. It is a Munro with a height of. It is the highest peak along Glen Shiel and can be easily climbed from the Cluanie Inn on the A87. The eastern slopes of the mountain, are owned by the Forestry Commission and are part of the Kintail National Scenic Area.

Geographic entities mentioned:
surface_form: a' chràlaig
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.184186
lon: -5.154837
Consequently, the water supply project was postponed until 1912. In 1912, the Public Utilities Commissioner, at the request of the City of Winnipeg, caused an investigation to be made and obtained an engineering report that recommended Shoal Lake, Kenora District, Ontario—the western tributary of the Lake of the Woods watershed—as the source of water supply. Winnipeg Mayor Thomas R.

Geographic entities mentioned:
surface_form: Lake of the Woods
instance_of: Lake
countries: Canada
United States
coordinates: lat: 49.09027777777778
lon: -95.2388888888889
The plan was put to Winnipeg voters on 1 October 1913 and was approved by a vote of 2,951 in favour and 90 against. As Shoal Lake is connected with, and is part of, the trans-boundary Lake of the Woods watershed, approval was required from the International Joint Commission which administered the 1909 Boundary Waters Treaty between the United States and Canada.

Geographic entities mentioned:
surface_form: Lake of the Woods
instance_of: Lake
countries: Canada
United States
coordinates: lat: 49.09027777777778
lon: -95.2388888888889
District 32. The 32nd district is based in the San Gabriel Valley and includes El Monte and West Covina. Incumbent Democrat Grace Napolitano, who had represented the 32nd district since 2013 and previously represented the 38th district from 2003 to 2013 and the 34th district from 1999 to 2003, ran for re-election. Campaign.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
Location. The Campos de Manicoré Environmental Protection Area (APA) is in the municipality of Manicoré, Amazonas. It is some distance to the north of the stretch of the Trans-Amazonian Highway (BR-230) between Humaitá and Apuí in the region between the Madeira River and the Aripuanã River. The Manicoré River defines the east boundary of the APA. History.

Geographic entities mentioned:
surface_form: Manicoré River
instance_of: Watercourse
countries: Brazil
coordinates: lat: -5.858936
lon: -61.328736
Volcano Mountain is called Nelrúna in the Northern Tutchone language. Geology. Volcano Mountain is the youngest volcano in the Fort Selkirk Volcanic Field and one of the youngest in the northern section of the Northern Cordilleran Volcanic Province. The lava at Volcano Mountain is olivine nephelinite, which is an uncommon type of lava.

Geographic entities mentioned:
surface_form: Fort Selkirk Volcanic Field
instance_of: Mountain
countries: Canada
coordinates: lat: 62.93
lon: -137.38
surface_form: Northern Cordilleran Volcanic Province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: volcano mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 62.93
lon: -137.38
Volcano Mountain. Volcano Mountain is a cinder cone in central Yukon Territory, Canada, located a short distance north of Fort Selkirk, near the confluence of the Pelly and Yukon Rivers. Volcano Mountain is called Nelrúna in the Northern Tutchone language. Geology.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9717
lon: -123.007
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: volcano mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 62.93
lon: -137.38
The most recent of these is estimated to have occurred around 7300 years ago. Eruption deposits consist of lava flows and cinder cones. The upper of the volcano is made up of a cinder cone. The age of the summit cinder cone is unknown but it likely predates eruptions on the north and south flanks that led to landslides originating from the cone.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9717
lon: -123.007
Eruption deposits consist of lava flows and cinder cones. The upper of the volcano is made up of a cinder cone. The age of the summit cinder cone is unknown but it likely predates eruptions on the north and south flanks that led to landslides originating from the cone. The oldest known lava flow traveled to the north of its vent and had a landslide associated with it.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9717
lon: -123.007
Volcano Mountain. Volcano Mountain is a cinder cone in central Yukon Territory, Canada, located a short distance north of Fort Selkirk, near the confluence of the Pelly and Yukon Rivers. Volcano Mountain is called Nelrúna in the Northern Tutchone language. Geology.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: volcano mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 62.93
lon: -137.38
Geology. Volcano Mountain is the youngest volcano in the Fort Selkirk Volcanic Field and one of the youngest in the northern section of the Northern Cordilleran Volcanic Province. The lava at Volcano Mountain is olivine nephelinite, which is an uncommon type of lava. This type of lava is believed to have come from much deeper inside the Earth than basaltic lava.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: volcano mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 62.93
lon: -137.38
The lava at Volcano Mountain is olivine nephelinite, which is an uncommon type of lava. This type of lava is believed to have come from much deeper inside the Earth than basaltic lava. A hill to the west of Volcano Mountain has basaltic columns and has been interpreted to be an ancestral cone of the edifice. Volcanism in the Fort Selkirk Volcanic Field appears to follow the Tintina Fault.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: volcano mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 62.93
lon: -137.38
Volcanism in the Fort Selkirk Volcanic Field appears to follow the Tintina Fault. Over four million years of activity, this has migrated northward along the fault by about to reach the area where Volcano Mountain is today. This has been theorized to result from pressure in the asthenosphere changing over time under the weight of glaciers or to be movement of magma from an unknown cause.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: volcano mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 62.93
lon: -137.38
This has been theorized to result from pressure in the asthenosphere changing over time under the weight of glaciers or to be movement of magma from an unknown cause. Volcano Mountain and other eruptive centres in the Fort Selkirk Volcanic Field lie on top of glacial deposits.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: volcano mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 62.93
lon: -137.38
surface_form: fort selkirk volcanic field
instance_of: Mountain
countries: Canada
coordinates: lat: 62.93
lon: -137.38
Below that is volcanic material from the Carmacks Group, which was erupted in a subduction zone setting in the Late Tertiary. Eruptive history. Researchers have discovered evidence for seven individual eruptions at Volcano Mountain. The most recent of these is estimated to have occurred around 7300 years ago. Eruption deposits consist of lava flows and cinder cones.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: volcano mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 62.93
lon: -137.38
It dammed a stream to create Caitlin Pond. Sediment core data from the pond shows it was dammed sometime before 7300 years ago. The southwestern side of the mountain has at least five separate lava flows along with additional landslide debris. The youngest lava flows on the southwest side traveled from their vent and dammed Leech Lake.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Pyroclastic debris from this event have been found on the volcano's crater floor. Lava flows from Volcano Mountain exhibit features common in other lava flows, such as lava tubes. Vegetation has been slow to grow on the lava flows because of the climate and northerly latitude of the region. Volcanic hazards.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: volcano mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 62.93
lon: -137.38
Vegetation has been slow to grow on the lava flows because of the climate and northerly latitude of the region. Volcanic hazards. Future eruptions from Volcano Mountain would probably be lava flows, since there is a lack of pyroclastic material. The main hazards from Volcano Mountain are forest fires started by the lava flows and poisonous gases.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: volcano mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 62.93
lon: -137.38
Future eruptions from Volcano Mountain would probably be lava flows, since there is a lack of pyroclastic material. The main hazards from Volcano Mountain are forest fires started by the lava flows and poisonous gases. Older volcanic deposits south of Volcano Mountain indicate that lava flows may have once partly blocked or at least altered the course of the Yukon and Pelly Rivers.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: volcano mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 62.93
lon: -137.38
The main hazards from Volcano Mountain are forest fires started by the lava flows and poisonous gases. Older volcanic deposits south of Volcano Mountain indicate that lava flows may have once partly blocked or at least altered the course of the Yukon and Pelly Rivers. Specific hazards at Volcano Mountain and other volcanoes in Yukon are poorly understood.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: volcano mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 62.93
lon: -137.38
A hill to the west of Volcano Mountain has basaltic columns and has been interpreted to be an ancestral cone of the edifice. Volcanism in the Fort Selkirk Volcanic Field appears to follow the Tintina Fault. Over four million years of activity, this has migrated northward along the fault by about to reach the area where Volcano Mountain is today.

Geographic entities mentioned:
surface_form: fort selkirk volcanic field
instance_of: Mountain
countries: Canada
coordinates: lat: 62.93
lon: -137.38
Their remote location lead to a lack of detailed geologic maps, research to determine past eruption dates, and real-time monitoring infrastructure such as seismographs. A review of Canadian volcanoes published in 2024 assessed the entire Fort Selkirk Volcanic Field under the &quot;very low&quot; threat category because of the primary eruptive style and relative isolation from population centres.

Geographic entities mentioned:
surface_form: fort selkirk volcanic field
instance_of: Mountain
countries: Canada
coordinates: lat: 62.93
lon: -137.38
Geography. Taranto faces the Ionian Sea. It is above sea level. It was built on a plain running north/north-west–southeast, and surrounded by the Murgia plateau from the north-west to the east. Its territory extends for and is mostly underwater. It is characterised by three natural peninsulas and a man-made island, formed by digging a ditch during the construction of Aragon Castle.

Geographic entities mentioned:
surface_form: Murgia
instance_of: Plateau
countries: Italy
coordinates: lat: 40.976
lon: 16.406
Early life. Armstrong was born at Drayton. Armstrong owned a pastoral property called Adare, which was one of the Lockyer Valley's largest cattle properties of the 19th and 20th centuries, and had its homestead approximately seven kilometres north of Gatton on Adare Road. The modern locality of Adare takes its name from the property.

Geographic entities mentioned:
surface_form: Lockyer Valley's
instance_of: Valley
countries: Australia
coordinates: lat: -27.558833333333
lon: 152.27816666667
Cortez Lake. Cortez Lake is located in Cortez Park in northwest Phoenix, Arizona, United States, at the northeast corner of 35th Avenue and Dunlap Avenue.

Geographic entities mentioned:
surface_form: cortez lake
instance_of: Lake
countries: United States
coordinates: lat: 33.570222222222
lon: -112.131875
Tuddal. Tuddal is a village in Hjartdal Municipality in Telemark county, Norway. The village is located in the Tuddalsdalen valley, about to the north of the village of Sauland and about to the south of the town of Rjukan. County road 3430 runs from Sauland, through Tuddal, and further north along the mountain Gaustatoppen and to Rjukan. The highest point along the road reaches above sea level.

Geographic entities mentioned:
surface_form: Gaustatoppen
instance_of: Mountain
countries: Norway
coordinates: lat: 59.854138888889
lon: 8.6503333333333
Paril Saddle. Paril Saddle (Parilska Sedlovina \pa-'ril-ska se-dlo-vi-'na\) is a saddle of elevation in Friesland Ridge in Tangra Mountains on Livingston Island, Antarctica. Bounded by St. Boris Peak to the northeast, and Simeon Peak to the southwest. Overlooking Macy Glacier to the east and southeast, and Huntress Glacier to the west and northwest.

Geographic entities mentioned:
surface_form: Simeon Peak
instance_of: Mountain
coordinates: lat: -62.690833333333
lon: -60.206944444444
Of nut trees, she had English walnuts, almonds, butternut, beachnuts, chestnuts, chickpecans, and filberts. 19th-century. The tract was located in the San Gabriel Valley on the northeast corner of Colorado Street and Orange Grove Avenue. When the Carrs purchased the property, it was a barren land on which the sheep herd fed. It was thickly infested with rabbits, gophers, and squirrels.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
Lake of Bays (Muskoka lake). Lake of Bays is a large lake in the District Municipality of Muskoka in Central Ontario, Canada. It is located almost entirely in the Township municipality of Lake of Bays, which is named after the lake, with the exception of the southwest arm of the lake which is in the Town of Huntsville. Ontario Highway 35 runs north and east of the lake.

Geographic entities mentioned:
surface_form: lake of bays (muskoka lake)
instance_of: Lake
countries: Canada
coordinates: lat: 45.2402
lon: -79.0486
surface_form: lake of bays
instance_of: Lake
countries: Canada
coordinates: lat: 49.9842
lon: -91.2878
Lake of Bays (Muskoka lake). Lake of Bays is a large lake in the District Municipality of Muskoka in Central Ontario, Canada. It is located almost entirely in the Township municipality of Lake of Bays, which is named after the lake, with the exception of the southwest arm of the lake which is in the Town of Huntsville. Ontario Highway 35 runs north and east of the lake.

Geographic entities mentioned:
surface_form: lake of bays
instance_of: Lake
countries: Canada
coordinates: lat: 45.2402
lon: -79.0486
surface_form: lake of bays
instance_of: Lake
countries: Canada
coordinates: lat: 49.9842
lon: -91.2878
Lake characteristics. Lake of Bays is a deep, cold, infertile lake which forms an important part of the Muskoka watershed. Despite its size and basin shape, low fertility and a short residence time combine to make it only moderately productive. Lake of Bays water is clear, and the maximum secchi disc reading obtained was.

Geographic entities mentioned:
surface_form: lake of bays
instance_of: Lake
countries: Canada
coordinates: lat: 45.2402
lon: -79.0486
surface_form: lake of bays
instance_of: Lake
countries: Canada
coordinates: lat: 49.9842
lon: -91.2878
Lake of Bays is a deep, cold, infertile lake which forms an important part of the Muskoka watershed. Despite its size and basin shape, low fertility and a short residence time combine to make it only moderately productive. Lake of Bays water is clear, and the maximum secchi disc reading obtained was. The surface layer, which is in depth, varies in temperature throughout the year.

Geographic entities mentioned:
surface_form: lake of bays
instance_of: Lake
countries: Canada
coordinates: lat: 45.2402
lon: -79.0486
surface_form: lake of bays
instance_of: Lake
countries: Canada
coordinates: lat: 49.9842
lon: -91.2878
On September 5, 1837, Thompson mentioned catching lake trout in the lake. Thomas Moffatt, an agent for the Hudson's Bay Company (Moffatt reported an outpost on Bigwin Island) referred to it as Trading Lake. In 1853, a geological survey by Alexander Murray of the Geological Survey of Canada referred to the lake as Lake of Bays. Amenities.

Geographic entities mentioned:
surface_form: lake of bays
instance_of: Lake
countries: Canada
coordinates: lat: 45.2402
lon: -79.0486
surface_form: lake of bays
instance_of: Lake
countries: Canada
coordinates: lat: 49.9842
lon: -91.2878
Mary Creek). Bigwin Island is the largest island in the lake; other islands include Burnt Island, Fairview Island, Langmaids Island, Pancake Island, Raynor Island, Rock Island, Haystack Island, Millichamp Island, Reuben Island, Crown Island and Peanut Island.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
The irregular shape of the lake is defined by many bays such as Rabbit's Bay, Burnt Island Bay, Whitehouse Bay, Montgomery Bay, Portage Bay, Haystack Bay, Ten Mile Bay, Dwight Bay, Trading Bay and Murky Bay. Lake characteristics. Lake of Bays is a deep, cold, infertile lake which forms an important part of the Muskoka watershed.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
On September 5, 1837, Thompson mentioned catching lake trout in the lake. Thomas Moffatt, an agent for the Hudson's Bay Company (Moffatt reported an outpost on Bigwin Island) referred to it as Trading Lake. In 1853, a geological survey by Alexander Murray of the Geological Survey of Canada referred to the lake as Lake of Bays. Amenities.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
Port Cunnington is a community established on a peninsula reaching out deep inside the lake. Other settlements on the lake shore include Dwight, South Portage, Baysville and Dorset. Geography. The lake is fed by Oxtongue River, as well as other rivers and creeks flowing from the north-east (Boyne River and its tributary Sixteen Mile Creek, Ten Mile Creek, Hollow River, St. Mary Creek).

Geographic entities mentioned:
surface_form: boyne river
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.32972222222222
lon: -79.01666666666667
Origin of name. The First Nations apparently called the lake &quot;Num g e low e nee g go mark lak a hagan&quot; which means Lake of Forks. It was also known as Baptiste Lake, Forked Lake and Lake of Two Bays. In 1837, David Thompson traversed the lake and drew a map of the lake that refers to it as Forked Lake. On September 5, 1837, Thompson mentioned catching lake trout in the lake.

Geographic entities mentioned:
surface_form: baptiste lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.7567
lon: -113.561
His contributions have been recognized in several awards from US and Argentine government agencies. Mount Giovinetto is a 4090 m/13,419 ft mountain named after him in the Antarctic Ellsworth Mountains Sentinel Range.

Geographic entities mentioned:
surface_form: Mount Giovinetto
instance_of: Mountain
coordinates: lat: -78.26666667
lon: -86.16666667
It is located in the Ganderbal district of Jammu and Kashmir and the Kargil district of Ladakh, both union territories of India. This pass connects the Kashmir Valley to its west with the Dras and Suru valleys to its northeast and the Indus valley further east. 1 between Srinagar and Leh in the western section of the Himalayan mountain range, traverses the pass.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
surface_form: Suru valley
instance_of: Valley
countries: India
coordinates: lat: 34.566666666667
lon: 76.1
Weissenstein Tunnel. The Weissenstein Tunnel is a long, single-track railway tunnel on the Solothurn–Moutier railway line, built by the former. It passes under the 1,395-meter-high Weissenstein as a Jura crossing. Location and construction. The north portal is located at Gänsbrunnen at an elevation of 722 meters above sea level, and the south portal is at 659 meters above sea level at Oberdorf.

Geographic entities mentioned:
surface_form: Weissenstein
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.25399
lon: 7.50855
Thanks to the missionaries Nicolás Mascardi, Van der Meeren (Laguna), Zúñiga, Guglielmo and Elguea, the Todos los Santos Lake, the Vuriloche Pass and the Nahuelhuapi Lake, where there was a Catholic temple, were discovered. Father Mascardi spent four years as a missionary among the indigenous people of the area, who were not only Poyas, but also Pehuenches and Puelches.

Geographic entities mentioned:
surface_form: Todos los Santos Lake
instance_of: Lake
countries: Chile
coordinates: lat: -41.133333333333
lon: -72.2
The royal decrees spoke of the administration of the &quot;province of Nahuelhuapi&quot; by the kingdom of Chile. The southern boundary of the territories transferred to the new viceroyalty is the Diamante River, according to the founding act of the city of Mendoza and with the map of Juan de la Cruz Cano y Olmedilla of 1775, which was used by the king to create the new viceroyalty.

Geographic entities mentioned:
surface_form: Diamante River
instance_of: Watercourse
countries: Argentina
coordinates: lat: -34.511666666667
lon: -66.757777777778
Its limit was in the rivers Diamante River, Quinto River, and in the river Hueuque, and when being separated these three rivers by extensive territories, it also used three imaginary lines by fields, or natural by mountains (a line that passed over the Desaguadero River, another that went down by the chained lagoons of the west of Buenos Aires, and another by the mountains of Buenos Aires to the sea) that joined these points according to the official document of Cano y Olmedilla of 1775.

Geographic entities mentioned:
surface_form: Diamante River
instance_of: Watercourse
countries: Argentina
coordinates: lat: -34.511666666667
lon: -66.757777777778
To which Argentina did not protest. The Argentine president, Juan Manuel de Rosas, sent officials to tax Talca ranchers in the area in question in 1847 and 1848. By then he had already resolved to incorporate into his country the territory south of the Diamante River to the Río Negro, most of which he knew after his 1833 expeditions.

Geographic entities mentioned:
surface_form: Diamante River
instance_of: Watercourse
countries: Argentina
coordinates: lat: -34.511666666667
lon: -66.757777777778
Nymlal. Nymlal (also spelled Nyamlell) is a populated place in the Northern Bahr el Ghazal state in South Sudan, north-west of the town of Aweil on the banks of the Lol River. Nymlal, situated in Aweil West County, has a marketplace. Most of the people in and around Nymlal are Dinka. The name &quot;Nymlal&quot; has the meaning of &quot;the place where stones are eaten&quot;.

Geographic entities mentioned:
surface_form: Lol River
instance_of: Watercourse
countries: South Sudan
coordinates: lat: 9.19055556
lon: 29.19666667
The stony lithalsa (heaved mounds) found on the archipelago of Svalbard are an example. Frost heaves occur in alpine regions, even near the equator, as illustrated by palsas on Mount Kenya.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
Cryogenic earth hummocks are a small formation resulting from granular convection that appear in seasonally frozen ground and have many different names; in North America they are earth hummocks; thúfur in Greenland and Iceland; and pounus in Fennoscandia.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
The story shifts to 1972, ten years after the events of &quot;The Sandlot&quot;. A new crop of five kids now reside in San Fernando Valley in Los Angeles and play baseball at the Sandlot. Johnnie Smalls, the little brother of Scott Smalls, has heard the legend of a ferocious dog he calls &quot;The Great Fear&quot;, that is one of The Beast’s offspring and is owned by Mr.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
However, the person actually depicted in the photograph was Watkins, as was later clarified by bassist Stuart Richardson in 2005. At the time, Oliver was also an acclaimed artist with his work being displayed in several exhibitions depicting Rhondda life.

Geographic entities mentioned:
surface_form: Rhondda
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
The collinean zone extends up to approximately 500 meters in altitude. The montane zone is between 500 and 1,000 meters, with the subalpine zone extending beyond that. The latter's highest point is the Grand Ballon, which reaches 1,424 meters. The diverse environmental conditions, including altitude, climate, topography, and soil types, contribute to the formation of heterogeneous vegetation.

Geographic entities mentioned:
surface_form: Grand Ballon
instance_of: Mountain
countries: France
coordinates: lat: 47.900833333333
lon: 7.0980555555556
The mountain chain is primarily oriented along a north-south axis, with higher altitudes observed in the southern region. The surrounding hills include the Northern Vosges (or Low Vosges), the Vôge region to the west, which straddles the Vosges and Haute-Saône departments, the Alsatian under-Vosgian hills to the east, and the southern and western under-Vosgian hills.

Geographic entities mentioned:
surface_form: Vôge
instance_of: Plateau
countries: France
coordinates: lat: 48.05
lon: 6.25
The altitude of the region in question typically ranges between 300 and 700 meters. However, the elevation varies considerably across the entire region, ranging from approximately 200 meters in the north to 1,424 meters at the Grand Ballon in the Haut-Rhin. The rocks that comprise the massif exhibit a distinct geographical distribution.

Geographic entities mentioned:
surface_form: Grand Ballon
instance_of: Mountain
countries: France
coordinates: lat: 47.900833333333
lon: 7.0980555555556
These include downy birches (&quot;Betula pubescens&quot;), Scots pines (&quot;Pinus sylvestris&quot;), and Norway spruces (&quot;Picea abies&quot;).Some peatland sites have been identified within the Vosges massif, including three of particular significance and situated within the commune of La Bresse: Lake Lispach, Lake Blanchemer, and Machais Pond.

Geographic entities mentioned:
surface_form: Lake Lispach
instance_of: Lake
countries: France
coordinates: lat: 48.051666666667
lon: 6.9422222222222
These pastures are classified as secondary pastures. Nevertheless, the initial human impact on the pastures predates the 8th century. For instance, research indicates that the Rossberg massif experienced at least three deliberate fires between the 4th century BC and the 1st century AD, following the abandonment or under-exploitation of the pastures.

Geographic entities mentioned:
surface_form: Rossberg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.0845
lon: 8.577527777777778