Sarmila/GeoWiki-Features huggingface dataset:
Sweden Peak's toponym was officially adopted in 1977 by the United States Board on Geographic Names, along with Denmark Peak, Norway Peak, and Finland Peak to honor Alaskan settlers from Scandinavia. Sweden Peak is part of a cluster of peaks that surround the unofficially named Scandinavia Glacier, which is a tributary of the Matanuska Glacier.

Geographic entities mentioned:
surface_form: matanuska
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: sweden peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.574166666667
lon: -147.39722222222
Sweden Peak is part of a cluster of peaks that surround the unofficially named Scandinavia Glacier, which is a tributary of the Matanuska Glacier. Precipitation runoff from the mountain drains to the Matanuska River. Topographic relief is significant as the south face rises in one-half mile (0.80 km). Climate.

Geographic entities mentioned:
surface_form: matanuska
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
Sweden Peak. Sweden Peak is a mountain summit in Alaska, United States. Description. Sweden Peak is located in the Chugach Mountains approximately midway between Anchorage and Glennallen. It is situated southeast of Mount Wickersham near the head of Matanuska Glacier.

Geographic entities mentioned:
surface_form: sweden peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.574166666667
lon: -147.39722222222
Climate. Based on the Köppen climate classification, Sweden Peak is located in a tundra climate zone with long, cold, snowy winters, and mild summers. Weather systems coming off the Gulf of Alaska are forced upwards by the Chugach Mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall.

Geographic entities mentioned:
surface_form: sweden peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.574166666667
lon: -147.39722222222
Ballig. Ballig (, also known as Ballig Bridge) is a small hamlet of a few houses situated between the 8th and 9th Milestone road-side markers on the Snaefell Mountain Course between Ballacraine and Glen Helen.

Geographic entities mentioned:
surface_form: Glen Helen
instance_of: Valley
countries: Isle of Man
coordinates: lat: 54.22583333
lon: -4.61722222
Ontario Peninsula. The Ontario Peninsula is the southernmost part of the province of Ontario and of Canada as a whole. It is bounded by Lake Huron on the west, Lake Ontario on the east, and Lake Erie on the south. At its tip, it is separated from Michigan by the Detroit and St. Clair rivers, as well as Lake St. Clair.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Ontario Peninsula. The Ontario Peninsula is the southernmost part of the province of Ontario and of Canada as a whole. It is bounded by Lake Huron on the west, Lake Ontario on the east, and Lake Erie on the south. At its tip, it is separated from Michigan by the Detroit and St. Clair rivers, as well as Lake St. Clair.

Geographic entities mentioned:
surface_form: Lake St. Clair
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.450265
lon: -82.67572
The procedure was carried out by Moran, an underworld doctor. The operations were so painful that Fred asked one of his friends to shoot him to stop the pain, but his friend refused. Moran disappeared shortly thereafter. A badly decomposed body was discovered a year later washed up from Lake Erie on Crystal Beach, Ontario, Canada. Police identified it as Moran.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Hocomonco Pond. Hocomonco Pond is a recreational pond located in Westborough, Massachusetts near Route 9. Also called Hobomoc Pond, it was named for Hobomok, a Wamesit Indian evil spirit. The pond and adjacent land are a Superfund site. Superfund site. A wood treatment and preservation plant operated on a site near the pond during the 1930s and 1940s. The business saturated wood products (e.g.

Geographic entities mentioned:
surface_form: hocomonco pond
instance_of: Lake
countries: United States
coordinates: lat: 42.2725
lon: -71.649444444444
Hocomonco Pond. Hocomonco Pond is a recreational pond located in Westborough, Massachusetts near Route 9. Also called Hobomoc Pond, it was named for Hobomok, a Wamesit Indian evil spirit. The pond and adjacent land are a Superfund site. Superfund site. A wood treatment and preservation plant operated on a site near the pond during the 1930s and 1940s. The business saturated wood products (e.g.

Geographic entities mentioned:
surface_form: spirit
instance_of: Lake
countries: United States
coordinates: lat: 46.273055555556
lon: -122.135
Benito Juárez National Park. The Benito Juárez National Park is in the Valles Centrales Region of Oaxaca, Mexico, and includes parts of the municipalities of San Felipe Tejalapam and San Andres Huayapan. The southern boundary of the park is about five kilometers north of the City of Oaxaca.

Geographic entities mentioned:
surface_form: Valles Centrales Region
instance_of: Valley
countries: Mexico
coordinates: lat: 17.0833
lon: -96.75
Bilsdale. Bilsdale is a dale in the western part of the North York Moors in North Yorkshire, England. The head of the dale is at Hasty Bank, and the dale extends south to meet Rye Dale near Hawnby. The dale is the valley of the River Seph, formed where Raisdale Beck joins Bilsdale Beck at the small village of Chop Gate in the north of the dale.

Geographic entities mentioned:
surface_form: Rye Dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.25
lon: -1.12
Bilsdale. Bilsdale is a dale in the western part of the North York Moors in North Yorkshire, England. The head of the dale is at Hasty Bank, and the dale extends south to meet Rye Dale near Hawnby. The dale is the valley of the River Seph, formed where Raisdale Beck joins Bilsdale Beck at the small village of Chop Gate in the north of the dale.

Geographic entities mentioned:
surface_form: bilsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.331
lon: -1.122
Bilsdale is a dale in the western part of the North York Moors in North Yorkshire, England. The head of the dale is at Hasty Bank, and the dale extends south to meet Rye Dale near Hawnby. The dale is the valley of the River Seph, formed where Raisdale Beck joins Bilsdale Beck at the small village of Chop Gate in the north of the dale. The river flows south to meet the River Rye at Seph Mouth.

Geographic entities mentioned:
surface_form: bilsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.331
lon: -1.122
The river flows south to meet the River Rye at Seph Mouth. The dale is divided between two civil parishes. The upper part of the dale comprises the civil parish of Bilsdale Midcable and the lower part of the dale is in the civil parish of Hawnby. History. The place-name is derived from an Old Norse personal name &quot;Bildr&quot;, and so means &quot;Bildr's valley&quot;.

Geographic entities mentioned:
surface_form: bilsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.331
lon: -1.122
Bilsdale Rievaulx was itself divided by the River Seph. The part to the west of the river became the township of Bilsdale Westside in the parish of Hawnby. The part to the east became part of the township of Bilsdale Midcable, which also included Bilsdale Kirkham, in the parish of Helmsley. An area above Laskill became a separate township of Helmsley parish, known as Laskill Pasture.

Geographic entities mentioned:
surface_form: bilsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.331
lon: -1.122
Bilsdale Rievaulx was itself divided by the River Seph. The part to the west of the river became the township of Bilsdale Westside in the parish of Hawnby. The part to the east became part of the township of Bilsdale Midcable, which also included Bilsdale Kirkham, in the parish of Helmsley. An area above Laskill became a separate township of Helmsley parish, known as Laskill Pasture.

Geographic entities mentioned:
surface_form: bilsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.331
lon: -1.122
surface_form: bilsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.331
lon: -1.122
An area above Laskill became a separate township of Helmsley parish, known as Laskill Pasture. At the Dissolution both Bilsdale Kirkham and Bilsdale Rievaulx were granted to Thomas Manners, Earl of Rutland. His successors sold the estate in 1687 to the Duncombe family. In the 19th century jet was extensively mined in the dale.

Geographic entities mentioned:
surface_form: bilsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.331
lon: -1.122
surface_form: bilsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.331
lon: -1.122
His successors sold the estate in 1687 to the Duncombe family. In the 19th century jet was extensively mined in the dale. The townships of Bilsdale Westside, Bilsdale Midcable and Laskill Pasture became separate civil parishes in 1866. Bilsdale Westside and Laskill Pasture became part of the new Ryedale District in 1974, and were subsequently absorbed into the civil parish of Hawnby.

Geographic entities mentioned:
surface_form: bilsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.331
lon: -1.122
surface_form: bilsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.331
lon: -1.122
Bilsdale Westside and Laskill Pasture became part of the new Ryedale District in 1974, and were subsequently absorbed into the civil parish of Hawnby. The main settlements in the dale are Chop Gate, Fangdale Beck and the ancient hamlet of Urra. In 1969, Bilsdale transmitting station was erected above the dale on Bilsdale West Moor.

Geographic entities mentioned:
surface_form: bilsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.331
lon: -1.122
The townships of Bilsdale Westside, Bilsdale Midcable and Laskill Pasture became separate civil parishes in 1866. Bilsdale Westside and Laskill Pasture became part of the new Ryedale District in 1974, and were subsequently absorbed into the civil parish of Hawnby. The main settlements in the dale are Chop Gate, Fangdale Beck and the ancient hamlet of Urra.

Geographic entities mentioned:
surface_form: ryedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.25
lon: -1.12
The lake is named for a jumbled rock slide that extends into the lake from the south side. Sliderock Lake is northeast of Merriam Peak and located in the lower section of the Boulder Chain Lakes Basin. The lake is accessed from Sawtooth National Forest trail 683.

Geographic entities mentioned:
surface_form: Boulder Chain Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 44.0704685
lon: -114.5835292
The use of Faial as a technical layover was also used by other companies, who used the waters between Faial and Pico on stopovers between North America and Europe. In April 1931, during the Azores Revolt, three small hydroplanes of the Portuguese Navy used Horta as a base to overfly Angra do Heroísmo and Monte Brasil.

Geographic entities mentioned:
surface_form: Monte Brasil
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.643
lon: -27.2213
Ichera village is located by the left bank of the Lena, a little upstream from the confluence. Course. The Ichera is a left tributary of the Lena. It is formed in the western part of the Lena Plateau. The river heads in a roughly southeastern direction across a taiga area. Finally it meets the Lena from its mouth, downstream from the mouth of the Pilyuda.

Geographic entities mentioned:
surface_form: Lena Plateau
instance_of: Plateau
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.75
lon: 125
Piz Prüna. Piz Prüna is a mountain of the Livigno Alps, located in Graubünden, Switzerland. Its summit overlooks the Val Prüna.

Geographic entities mentioned:
surface_form: piz prüna
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.48725
lon: 9.9872777777778
Ells River. Ells River is a stream in Alberta, Canada. Ells River has the name of S. C. Ells, a geologist.

Geographic entities mentioned:
surface_form: ells river
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.30022
lon: -111.66856
Willamette Valley AVA. Willamette Valley () is an American Viticultural Area (AVA) which lies in the Willamette Valley of Oregon. The AVA is the wine growing region which encompasses the drainage basin of the Willamette River.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
The AVA is the wine growing region which encompasses the drainage basin of the Willamette River. It stretches from the Columbia River in the north to just south of Eugene in the south, where the Willamette Valley ends; and from the Oregon Coast Range in the west to the Cascade Mountains in the east.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Chehalem Mountains AVA. The Chehalem Mountains AVA, established in 2006, stretches from Wilsonville in the southeast to Forest Grove in the northwest. The Chehalem Mountains includes Ribbon Ridge, Parrett Mountain, and Bald Peak. The petition process for the creation of the AVA began in 2001 and was led by David Adelsheim of.

Geographic entities mentioned:
surface_form: Bald Peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.396
lon: -123.056
The hills cover an area west of the Willamette River approximately long by wide. The Eola-Amity Hills area benefits from steady winds off the Pacific Ocean that reach the Willamette Valley through the Van Duzer corridor, a gap in the Oregon Coast Range, moderating the summer temperatures.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Lower Long Tom AVA. The Lower Long Tom AVA was established in 2021. It is located in the southern Willamette Valley in Lane and Benton Counties, near the towns of Junction City and Monroe. Its coverage is approximately and contains 12 wineries and 24 commercially-producing vineyards that plant approximately.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
He subdivided the vast governorship established over Iraq and the eastern Caliphate under Abd al-Malik's viceroy al-Hajjaj ibn Yusuf. Sulayman's appointee to this super-province, Yazid ibn al-Muhallab, was dismissed and imprisoned by Umar for failing to forward the spoils from his earlier conquest of Tabaristan along the southern Caspian coast to the caliphal treasury.

Geographic entities mentioned:
surface_form: Caspian
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Merrymeeting River. The Merrymeeting River is a river in the Lakes Region of central New Hampshire in the United States. It is a tributary of Lake Winnipesaukee, part of the Merrimack River watershed. The river begins at the outlet of Merrymeeting Lake in the town of New Durham. The river flows south through a chain of ponds to the village proper of New Durham.

Geographic entities mentioned:
surface_form: Lake Winnipesaukee
instance_of: Lake
countries: United States
coordinates: lat: 43.598888888889
lon: -71.323055555556
Merrymeeting River. The Merrymeeting River is a river in the Lakes Region of central New Hampshire in the United States. It is a tributary of Lake Winnipesaukee, part of the Merrimack River watershed. The river begins at the outlet of Merrymeeting Lake in the town of New Durham. The river flows south through a chain of ponds to the village proper of New Durham.

Geographic entities mentioned:
surface_form: Merrymeeting Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.490277777778
lon: -71.155277777778
Overview. At Busengo, Uganda the major road continues into the Democratic Republic of the Congo, through Busengo, DRC and it joins the N2 Road in Rutshuru. A smaller road travels north in the DR Congo from Busengo, Uganda, re-enters Uganda and loops back to Kisoro Town, passing to the east of Lake Mutanda. Busengo, Uganda is the location of &quot;Busengo Primary School&quot;.

Geographic entities mentioned:
surface_form: Lake Mutanda
instance_of: Lake
countries: Uganda
coordinates: lat: -1.235
lon: 29.67
The presence of many huge volcanoes on Mars shows that large areas were very hot in the past. Olympus Mons is the largest volcano in the Solar System; Ceraunius Tholus, one of its smaller volcanoes, nears the height of Earth's Mount Everest. There is strong evidence for much more widespread sources of heat in the form of dikes, which indicate that magma traveled under the ground.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Leco language. Leco, also written as Leko, is a language isolate that, though long reported to be extinct, is spoken by 20–40 individuals in areas east of Lake Titicaca, Bolivia. The Leco ethnic population was 13,527 in 2012. Classification.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
Classification. Although Leco is generally considered to be a language isolate, Kaufman (1994: 64) groups Leco together with the Sechura–Catacao languages as part of a proposed &quot;Macro-Lecoan&quot; family. It has also been suggested that Leco might be grouped with the extinct Puquina languages spoken in the south shore of Lake Titicaca. Language contact.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
Helgi Skúlason. Helgi Skúlason (4 September 1933 – 25 September 1996) was an Icelandic actor and stage director. Early life and education. Helgi was born in Keflavík and attended the district school at Laugarvatn; he trained as an actor at the National Theatre of Iceland school, finishing in 1954. Career. He began his career with the National Theatre.

Geographic entities mentioned:
surface_form: Laugarvatn
instance_of: Lake
countries: Iceland
coordinates: lat: 64.211111111111
lon: -20.711111111111
Between 3 and 4 million years ago, volcanic-derived mud flows called lahars streamed down several major mountains that included nearby but now extinct Mount Yana and Mount Maidu to become the Tuscan Formation. Basaltic and later andesitic to dacitic flows of lava covered increasingly larger areas of this formation to eventually form the lava plateau upon which the park is situated.

Geographic entities mentioned:
surface_form: Mount Yana
instance_of: Mountain
coordinates: lat: 40.2175
lon: -121.3863888888889
surface_form: Mount Maidu
instance_of: Mountain
coordinates: lat: 40.29888888888889
lon: -121.61694444444444
About 600,000 years ago, Mount Tehama started to rise as a stratovolcano in the southwestern corner of the park, eventually reaching an estimated in height. Roughly 27,000 years ago, a dacite lava dome quickly pushed its way through Tehama's former north-eastern flank, becoming the approximately shorter Lassen Peak.

Geographic entities mentioned:
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
Lassen's shape was significantly altered by glacial erosion from 25,000 to 18,000 years ago during the Wisconsin glaciation. Since then, smaller dacite domes such as the 1,100-year-old Chaos Crags have formed around Lassen. Phreatic (steam explosion) eruptions, dacite and andesite lava flows along with cinder cone formation have persisted into modern times.

Geographic entities mentioned:
surface_form: Chaos Crags
instance_of: Mountain
countries: United States
coordinates: lat: 40.524166666667
lon: -121.52111111111
Since then, smaller dacite domes such as the 1,100-year-old Chaos Crags have formed around Lassen. Phreatic (steam explosion) eruptions, dacite and andesite lava flows along with cinder cone formation have persisted into modern times. Most notable of these is the eruption and formation of Cinder Cone in the mid- to late 17th century and the eruption of Lassen Peak in the early 20th century.

Geographic entities mentioned:
surface_form: Cinder Cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
Current setting. The Lassen volcanic area lies at the southern extremity of the Cascade Range, which extends northward some from Lassen Peak within the park through Oregon and Washington and into British Columbia. Lassen Peak is one of the Cascade Volcanoes that form a segment of a ring of volcanoes that circle the Pacific Ocean known collectively as the 'Pacific Ring of Fire'.

Geographic entities mentioned:
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
Northwest of the park lies the Klamath Mountains (a collective term for the Siskiyou, Trinity, Salmon and Marble mountain ranges). To the west lies the Sacramento Valley. Just south of the park begins the Sierra Nevada mountain range, and to the east lie the Modoc Plateau and then the Great Basin. Geologic history of the region.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
Northwest of the park lies the Klamath Mountains (a collective term for the Siskiyou, Trinity, Salmon and Marble mountain ranges). To the west lies the Sacramento Valley. Just south of the park begins the Sierra Nevada mountain range, and to the east lie the Modoc Plateau and then the Great Basin. Geologic history of the region.

Geographic entities mentioned:
surface_form: Modoc Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 41.6
lon: -121.2
From innumerable cracks, floods of highly fluid basaltic lava spread to cover an area of over. Now known as the Columbia Plateau, this great lava bed of flood basalt covers much of Oregon and Washington and even parts of Idaho. Northern California's Modoc Plateau is a thinner basaltic flow which some geologists associate with the Columbia Plateau, but there are technical objections to this.

Geographic entities mentioned:
surface_form: Columbia Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 45.999444444444
lon: -119.00138888889
An overlying rhyolitic lava flow gives an age of 1.5 million years. Lassen is the fifth volcanic center to be active in the region. Latour, Yana, Maidu and Dittmar were the four preceding centers; Latour and Yana are only poorly known. One major source of the formation was Mount Yana; centered a few miles (5 km) southwest of Butt Mountain and south of the park.

Geographic entities mentioned:
surface_form: Yana
instance_of: Mountain
coordinates: lat: 40.2175
lon: -121.3863888888889
surface_form: Maidu
instance_of: Mountain
coordinates: lat: 40.29888888888889
lon: -121.61694444444444
surface_form: Dittmar
instance_of: Mountain
coordinates: lat: 40.45277777777778
lon: -121.34722222222221
A third source situated north of Latour Butte made a lesser contribution to the formation. Minor sources included an area near Hatchet Mountain Pass (northwest of Burney Mountain), dikes south and southwest of Inskip Hill and possibly Campbell Mound (north of Chico, California).

Geographic entities mentioned:
surface_form: Burney Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.806666666667
lon: -121.62777777778
These volcanoes are geologically related to the Basin and Range volcanic province. Development of Lassen Peak. Radiometric dating indicates that around 31,000 years ago a new vent opened up on the northeastern slope of Tehama, probably close to where Lassen Peak now stands. Streams of fluid dacite flowed chiefly toward the north, reaching a thickness of and covering perhaps.

Geographic entities mentioned:
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
The growth of the pile of lava shattered the rocks previously there, forming enormous banks of talus. When Lassen Peak formed, it looked much like the nearby Chaos Crags domes do today, with steep sides covered by angular rock talus. Lassen Peak's shape was significantly altered by glacial erosion from 25,000 to 18,000 years ago during the Wisconsin glaciation.

Geographic entities mentioned:
surface_form: Chaos Crags
instance_of: Mountain
countries: United States
coordinates: lat: 40.524166666667
lon: -121.52111111111
Crescent Crater, which at first glance appears as a parasite on Lassen's northeast flank, has been more heavily glaciated and thus is older. Other dacite domes which rose on Tehama's flanks are Bumpass Mountain, Helen Ridge, Eagle Peak and Vulcan's Castle. An upper limit of 10,000 years has been set for the domes next to Lost Creek (north domes).

Geographic entities mentioned:
surface_form: Bumpass Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.4613
lon: -121.499
Manzanita Lake was formed as a result of Manzanita Creek being dammed by the debris. Steam rose from the domes of Chaos Crags until 1857. Around the mid-18th century a series of eruptions produced Cinder Cone in the northeast corner of the park, mantling an area of with ejecta in the process. Ash falling on the streams of lava pouring from the cone's east flank formed the Painted Dunes.

Geographic entities mentioned:
surface_form: Cinder Cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
Recently erupted volcanic domes are unstable and can collapse, generating small to large rockfalls. Approximately 350 years ago, collapse of one of the Chaos Crags domes generated huge rockfalls, creating an area now called the Chaos Jumbles. The first and largest of these traveled downslope and was able to climb up the side of Table Mountain.

Geographic entities mentioned:
surface_form: Chaos Crags
instance_of: Mountain
countries: United States
coordinates: lat: 40.524166666667
lon: -121.52111111111
It is approximately 65 km from the state capital, Gangtok, and 120 km from Siliguri, West Bengal. The name is derived from the Sikkimese language. ‘Ra’ means wild sheep, 'vong' translates to a rearing place, and ‘la’ means a pass. Geography. Mt. Kanchenjunga, Mt. Pandim, Mt. Siniolchu, Mt. Kabru are some of the major peaks visible from Ravangla. Flora.

Geographic entities mentioned:
surface_form: Siniolchu
instance_of: Mountain
countries: India
coordinates: lat: 27.75
lon: 88.316666666667
surface_form: Kabru
instance_of: Mountain
countries: India
Nepal
coordinates: lat: 27.635
lon: 88.11833333
The beer was also sold as a Discworld tie-in beer under the name &quot;Bearhugger's Old Restorative&quot;. &quot;Fan Dance&quot; took its name from the exercise conducted by the British army on Pen y Fan and contained a blend of Progress and &quot;dwarf&quot; hops. Closure. In January 2014, the brewery closed, with the loss of 3 jobs.

Geographic entities mentioned:
surface_form: Pen y Fan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 51.884031
lon: -3.436765
For a bust of Hitler, he stayed for several days in 1936 at Hitler's Obersalzberg compound. Alfred Rosenberg arranged a solo exhibition for him in 1935. He became wealthy and in 1937 or 1938 bought near the Chiemsee in Bavaria; in 1943 he also acquired Schloss Prielau, which had been seized from the family of Hugo von Hofmannsthal because of their Jewish ancestry.

Geographic entities mentioned:
surface_form: Chiemsee
instance_of: Lake
countries: Germany
coordinates: lat: 47.89
lon: 12.47
Al-Shu'ba Mountain. Al-Shu'ba mountain located in east of Al-Shu'ba village at Al-Ahsa and to the north of Al-Eskan next to the road leading from eastern villages to the northern villages and to Al-Dammam. Also it extends from north to south with a length of 20 km on the eastern edge of the northern oasis and its width is 4 km. Description.

Geographic entities mentioned:
surface_form: al-shu'ba mountain
instance_of: Mountain
countries: Saudi Arabia
coordinates: lat: 25.409992
lon: 49.688549
It descends to the northwest of Al-Jarn village. The height of Al-Shu'ba mountain is about 246 above sea level. The two parts of the mountain are separated by a 600-metre-wide aperture, in addition, the mountain overlook to the oasis from the western side, and from the eastern side it overlooks the desert and the site of Jawatha Mosque.

Geographic entities mentioned:
surface_form: al-shu'ba mountain
instance_of: Mountain
countries: Saudi Arabia
coordinates: lat: 25.409992
lon: 49.688549
Pierikpakte. Pierikpakte is a mountain in the Äpar massif and centrally located in Sarek National Park. The mountain rises to 1789 m above sea level. The mountain has an easily recognizable profile as seen from Pielavalta, one of the highest situated large highland plains in Sweden, at 820 m.

Geographic entities mentioned:
surface_form: pierikpakte
instance_of: Mountain
countries: Sweden
on January 1. It occurred in the Western Quebec seismic zone. The main shock epicenter was located in Lake Kipawa about north of Témiscaming in southwestern Quebec and northeast of North Bay, Ontario. The shaking was strongest within of the epicenter. It was felt in Témiscaming, North Bay and as far away as Toronto, making it one of the most significant earthquakes in Canada in 2000.

Geographic entities mentioned:
surface_form: Lake Kipawa
instance_of: Lake
countries: Canada
coordinates: lat: 46.8847
lon: -78.9678
It was felt in Témiscaming, North Bay and as far away as Toronto, making it one of the most significant earthquakes in Canada in 2000. The earthquake was triggered by major thrust faults associated with the Ottawa-Bonnechere Graben. Minor damage was reported during this earthquake, including fallen light objects, a damaged ventilation pipe and fractures in plaster.

Geographic entities mentioned:
surface_form: Ottawa-Bonnechere Graben
instance_of: Landform
countries: Canada
coordinates: lat: 45.5767
lon: -76.9162
Point Au Roche State Park. Point Au Roche State Park is an state park in Clinton County, New York. The park is in the eastern part of the Town of Beekmantown, on the shore of Lake Champlain. History. Prior to its designation as a state park, Point Au Roche was used as pasture or cropland, and as a military encampment for cadets during World War One.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
In addition, Adams George Archibald, the first Lieutenant Governor of Manitoba, wanted to establish a treaty that would secure the government with land around Lake Winnipeg and the western side of the Red River Valley in order to build up agriculture and extract resources.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
surface_form: Red River Valley
instance_of: Valley
countries: Canada
United States
coordinates: lat: 49
lon: -97.5
Articles and memorandum of &quot;Treaty 1&quot;. The final articles of &quot;Treaty 1&quot; were outlined as follows: the indigenous peoples were to hand over a large portion of land in the southeast and south-central current-day Manitoba to Governor Archibald and the Crown. These lands were to include areas around Lake Manitoba and Winnipeg as well as around the Red River Valley.

Geographic entities mentioned:
surface_form: Lake Manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: Red River Valley
instance_of: Valley
countries: Canada
United States
coordinates: lat: 49
lon: -97.5
Areas of expertise. Professor Wang specializes in the fossil evolution, systematics, and phylogeny of mammals of the Cenozoic. He has researched the biostratigraphy of Inner Mongolia and Asia as a whole, the geochronology of Asia, paleoenvironments of the Tibetan Plateau, and mammalian migrations between Eurasia and North America.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
The origin of the Godavari River, which Hindus consider sacred, is near Trimbak. It flows for, first eastwards across the Deccan Plateau then turns southeast, entering the West Godavari district and East Godavari district of Andhra Pradesh, until it splits into two watercourses that widen into a large river delta and flow into the Bay of Bengal. Location.

Geographic entities mentioned:
surface_form: Deccan Plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Brahmagiri (Maharashtra). Brahmagiri is a hill in the Western Ghats of Maharashtra. It is situated in Nashik District in the Indian state of Maharashtra. Trimbakeshwar Shiva Temple is located near this place. The origin of the Godavari River, which Hindus consider sacred, is near Trimbak.

Geographic entities mentioned:
surface_form: brahmagiri (maharashtra)
instance_of: Mountain
countries: India
Brahmagiri (Maharashtra). Brahmagiri is a hill in the Western Ghats of Maharashtra. It is situated in Nashik District in the Indian state of Maharashtra. Trimbakeshwar Shiva Temple is located near this place. The origin of the Godavari River, which Hindus consider sacred, is near Trimbak.

Geographic entities mentioned:
surface_form: brahmagiri
instance_of: Mountain
countries: India
Location. Brahmagiri, the hill (giri) of Lord Brahma, appear in many mythological and legendary documents. The Puranas state that the Gautama Maharishi and his wife Ahalya resided on this hill. Saint Gautam worshiped Shiva, one of the main deities in Hinduism, to bring Ganga in this hill. This river is known as River Gautami in the Brahmagiri hills.

Geographic entities mentioned:
surface_form: brahmagiri
instance_of: Mountain
countries: India
The Puranas state that the Gautama Maharishi and his wife Ahalya resided on this hill. Saint Gautam worshiped Shiva, one of the main deities in Hinduism, to bring Ganga in this hill. This river is known as River Gautami in the Brahmagiri hills. The undulated terrains of Brahmagiri are challenging spots for adventurous travels like nature walk and trekking.

Geographic entities mentioned:
surface_form: brahmagiri
instance_of: Mountain
countries: India
surface_form: hills
instance_of: Mountain
countries: India
coordinates: lat: 23.166666666667
lon: 92.833333333333
Saint Gautam worshiped Shiva, one of the main deities in Hinduism, to bring Ganga in this hill. This river is known as River Gautami in the Brahmagiri hills. The undulated terrains of Brahmagiri are challenging spots for adventurous travels like nature walk and trekking. There are many trekking trails nestled among the woody trees. The ranges are rich with natural attractions and scenic spots.

Geographic entities mentioned:
surface_form: brahmagiri
instance_of: Mountain
countries: India
There are many trekking trails nestled among the woody trees. The ranges are rich with natural attractions and scenic spots. Brahmagiri hill is considered as a huge form of Shiva and hence the mountain climbing was considered as a sin at that time. In the year 1908, Seth Lalchand Jashodanand Bhambhani of Karachi (now in Pakistan) and Seth Ganeshdas built 500 steps of stone at a cost of Rs. 40,000.

Geographic entities mentioned:
surface_form: brahmagiri
instance_of: Mountain
countries: India
Brahmagiri hill is considered as a huge form of Shiva and hence the mountain climbing was considered as a sin at that time. In the year 1908, Seth Lalchand Jashodanand Bhambhani of Karachi (now in Pakistan) and Seth Ganeshdas built 500 steps of stone at a cost of Rs. 40,000. This has facilitated easy access to Brahmagiri. The water flows in three directions on the mountain.

Geographic entities mentioned:
surface_form: brahmagiri
instance_of: Mountain
countries: India
Childless families worship at the Ahilya sangam and it is believed that they do get a child. The first peak of Sahyadri is called &quot;Brahmadri&quot;. The story associated with this is that Shankar was pleased with Brahmadev and said &quot;I shall be known by your name&quot;. Hence it is called as Brahmagiri. The mountain is 1800 feet high. Its height from sea level is 4248 feet.

Geographic entities mentioned:
surface_form: brahmagiri
instance_of: Mountain
countries: India
Trimbakeshwar itself is a place of worship because it is one of the 12 Jyotirlingas of Lord Shiva. From Trimbakeshwar, through regular steps, Ganga dwar is reached and the Gorakshanath cave which is end of Trimbakeshwar. Now again while climbing down, there is a road going towards Brahmagiri towards right. Following this route one reaches the carved steps in the rocks.

Geographic entities mentioned:
surface_form: brahmagiri
instance_of: Mountain
countries: India
From the base village, Brahmagiri is around 450 to 500 meters elevated
From base village, it takes 45 minutes to see Ganga dwar, the Gorakshanath caves and 108 Swayambhu Mahadev caves and in the halfway while descending, the road towards Brahmagiri takes you till the top in around 45 minutes and almost 2 hours to see the fort completely.

Geographic entities mentioned:
surface_form: brahmagiri
instance_of: Mountain
countries: India
surface_form: brahmagiri
instance_of: Mountain
countries: India
Målselva. The Målselva is a river in Målselv Municipality in Troms county, Norway. The long river flows through the Målselvdalen valley and then empties into the Målselvfjorden, an arm of the Malangen fjord. The municipality and the valley through which the river runs are both named after the river. The river is common fishing grounds for locals.

Geographic entities mentioned:
surface_form: Målselvdalen
instance_of: Valley
countries: Norway
coordinates: lat: 69.027
lon: 18.788
The municipality and the valley through which the river runs are both named after the river. The river is common fishing grounds for locals. The smaller rivers Divielva, Tamokelva, and Rostaelva converge near the Lille Rostavatnet lake to form the Målselva river. Later, the river Barduelva joins it near Fossmoen and Bardufoss. The river drains a watershed of.

Geographic entities mentioned:
surface_form: Lille Rostavatnet
instance_of: Lake
countries: Norway
coordinates: lat: 68.989722222222
lon: 19.638611111111
Van Hoevenberg Trail. The Van Hoevenberg Trail is a hiking trail that leads southward from Adirondak Loj to the peak of Mount Marcy, the highest point in New York State. Located in the High Peaks Wilderness Area, it is the shortest and most frequently-used route to get to the peak of Mount Marcy. It spans 7.4 miles (11.2 km) to the summit, a lengthy 14.8-mile (22.4 km) roundtrip.

Geographic entities mentioned:
surface_form: Mount Marcy
instance_of: Mountain
countries: United States
coordinates: lat: 44.112733333333
lon: -73.923727777778
Early life. Wilhelmus Nicholaas Theodore Marie van der Zalm was born and raised in Noordwijkerhout, Netherlands. He emigrated to Canada after World War II, settling in the Fraser Valley in 1947. After completing high school, he sold tulip bulbs and ultimately established himself in the gardening business. He moved to Surrey after marrying Lillian Mihalic, and purchased a nursery.

Geographic entities mentioned:
surface_form: Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
Geography. According to the United States Census Bureau, the town has a total area of, of which is land and is water. Located along the western side of Penobscot Bay, Lincolnville is drained by the Ducktrap River. Principal bodies of water include Megunticook Lake, Norton Pond (123 acres), Coleman Pond (225 acres), Moody Pond (61 acres), and Levenseller Pond (34 acres). The town is served by U.S.

Geographic entities mentioned:
surface_form: Megunticook Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.257777777778
lon: -69.111111111111
Grape pie. Grape pie is a type of fruit pie made from Concord grape and is part of harvest time traditions in the Finger Lakes region of New York in the United States. It is particularly sought after at the Naples Grape Festival, and can be found at various shops around town. Concord grape pie.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
Alpine Theatre Project. Alpine Theatre Project is a 501(c)(3) nonprofit professional theatre company based in Whitefish, Montana. It presents musicals, plays, and concerts. It also provides education and outreach to students in Montana's Flathead Valley. History. ATP was formed in December 2004, by actors David Ackroyd, Betsi Morrison, and Luke Walrath.

Geographic entities mentioned:
surface_form: Flathead Valley
instance_of: Valley
countries: United States
coordinates: lat: 48
lon: -114
Donnayite-(Y). Donnayite-(Y) is a rare-earth carbonate mineral containing the rare-earth metal yttrium. It was first discovered in 1978 at Mont Saint-Hilaire, Quebec. Donnayite was subsequently identified and named after Joseph D. H. Donnay and his wife, Gabrielle Donnay. Both were prominent mineralogists and crystallographers, and J. D. H.

Geographic entities mentioned:
surface_form: Mont Saint-Hilaire
instance_of: Mountain
countries: Canada
coordinates: lat: 45.552222222222
lon: -73.163888888889
Vik, Buskerud. Vik is a village and the administrative center of Hole in Buskerud, Norway. Vik is situated on the northeastern arm of Steinsfjorden, a branch of the Tyrifjorden. It is located on E16 between Sundvollen and Kroksund. The administration buildings for Hole Municipality are located in Vik. The village of Vik was originally named for the Vik farm in an inlet of Steinsfjorden.

Geographic entities mentioned:
surface_form: Steinsfjorden
instance_of: Body of water
countries: Norway
coordinates: lat: 60.0833
lon: 10.3167
surface_form: Tyrifjorden
instance_of: Lake
countries: Norway
coordinates: lat: 60.033333333333
lon: 10.133333333333
The species occurs across diverse ecological settings: in Sierra Madrona and Montes de Toledo on &quot;Quercus faginea&quot; subsp. &quot;broteroi&quot; in narrow siliceous valleys; in Sierra de Segura and Sierra de Alcaraz on &quot;Q. faginea&quot; subsp. &quot;faginea&quot; and &quot;Q. ilex&quot; subsp. &quot;ballota&quot; in limestone valleys and ravines; and in Cádiz province on &quot;Q.

Geographic entities mentioned:
surface_form: Sierra Madrona
instance_of: Mountain
countries: Spain
coordinates: lat: 38.438333333333
lon: -4.1652777777778
The first Chinese in Oakland fished in the San Francisco Bay for shrimp similarly to the Chinese at China Camp near San Rafael. In 1868, Chinese laborers built the Temescal Dam in Oakland providing water for the East Bay as well as the Lake Chabot Dam in 1874–75. They worked in canneries, cotton mills and fuse and explosive factories as well as farms.

Geographic entities mentioned:
surface_form: Temescal
instance_of: Lake
countries: United States
coordinates: lat: 37.847777777778
lon: -122.23138888889
Raundalen. Raundalen () is a valley in Vestland county, Norway. The long valley stretches from Uppsetedalen in the northwest corner of Ulvik municipality all the way to Urdland in central Voss municipality.

Geographic entities mentioned:
surface_form: raundalen
instance_of: Valley
countries: Norway
coordinates: lat: 60.6789
lon: 6.56167
Xenotilapia caudofasciata. &quot;Xenotilapia caudofasciata&quot; is a species of cichlid endemic to Lake Tanganyika where it prefers areas with sandy substrates. This species can reach a length of TL. It can also be found in the aquarium trade.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
It is found in the Pyrenees, the Cantabrians, the Massif Central, the Black Forest, the Sudetes (1300–1400m), throughout the Carpathians (900–2500m in the Tatras), in the north of the Apennines, on the island of Corsica, and on the Balkan Peninsula: in the mountains of Bosnia and Herzegovina, Montenegro, North Macedonia, Albania, Kosovo (specifically in Žljeb and Accursed Mountains), northernmost Greece (2000–2500m in Varnous, Kajmakčalan and Tzena), in the east of Serbia (Suva Planina) and the west of Bulgaria (at elevations of 1600–2700m in western and central Stara Planina, Sredna Gora, Vitosha, Osogovo, Rila, Pirin, Slavyanka and the western Rhodopes).

Geographic entities mentioned:
surface_form: Žljeb
instance_of: Mountain
countries: Montenegro
Kosovo
Serbia
coordinates: lat: 42.77
lon: 20.253333333333
surface_form: Varnous
instance_of: Mountain
countries: Greece
coordinates: lat: 40.874
lon: 21.243
surface_form: Kajmakčalan
instance_of: Mountain
countries: Greece
North Macedonia
coordinates: lat: 40.930277777778
lon: 21.786111111111
surface_form: Vitosha
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.566666666667
lon: 23.283333333333
It is part of the municipality of Lokroi since 2010. It was an independent commune between the 1820s and 1907, and was part the municipality of Atalanti between 1907 and 2010. In 2021 its population was 348. It is situated at 480 m elevation on the southern slope of the Chlomo mountain. It is 8 km southeast of Atalanti and 12 km northeast of Orchomenos. Its main industry is agriculture.

Geographic entities mentioned:
surface_form: Chlomo
instance_of: Mountain
countries: Greece
coordinates: lat: 38.5987
lon: 23.0008
The main occupations of the inhabitants were agriculture, animal husbandry and pottery. In the 2nd century CE, Pausanias described Cyrtones, also Cyrtone, as a town of ancient Boeotia situated east of Lake Copais, on a mountain 20 stades from Hyettus. It had a temple and a grove of Apollo, and a spring with sanctuary to the nymphs. Its location is a little east of the modern day village.

Geographic entities mentioned:
surface_form: Lake Copais
instance_of: Lake
countries: Greece
coordinates: lat: 38.45
lon: 23.05
(An Associated Press story dated May 23, 1947, reported that a judge granted the divorce &quot;yesterday&quot;, which would have been May 22, 1947.)
Golf. In 1938, Andre set a then world golfing record for women by shooting 156 holes of golf in 11 hours and 56 minutes on the Lake Norconian, California course. Her best round was 91 for 18 holes and her worst was 115. Post-acting career.

Geographic entities mentioned:
surface_form: Lake Norconian, California
instance_of: Lake
countries: United States
coordinates: lat: 33.9242
lon: -117.571
Devils Couch. Devils Couch is a mountain summit located in the Valhalla Ranges of the Selkirk Mountains in southeast British Columbia, Canada. It is situated in Valhalla Provincial Park, north of Gladsheim Peak, west of Slocan Lake, and northwest of Slocan. The mountain's descriptive name refers to its shape.

Geographic entities mentioned:
surface_form: Gladsheim Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.78316
lon: -117.63555
surface_form: Slocan Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.9472
lon: -117.378