Sarmila/GeoWiki-Features huggingface dataset:
Covering the highest parts of the Polish Beskids, it crosses peaks such as Stożek Wielki (&quot;Velký Stožek&quot; in Czech), Barania Góra, Babia Góra, Polica, Turbacz, Lubań, Przehyba, Radziejowa, Jaworzyna Krynicka, Rotunda, Cergowa, Chryszczata, Smerek and Halicz as well as towns such as Ustroń, Węgierska Górka, Jordanów, Rabka-Zdrój, Krościenko nad Dunajcem, Rytro, Krynica-Zdrój, Iwonicz-Zdrój, Rymanów-Zdrój, Komańcza, Cisna and Ustrzyki Górne.

Geographic entities mentioned:
surface_form: Stożek Wielki
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 49.605277777778
lon: 18.823055555556
surface_form: Barania Góra
instance_of: Mountain
countries: Poland
coordinates: lat: 49.611388888889
lon: 19.010555555556
surface_form: Babia Góra
instance_of: Mountain
countries: Poland
Slovakia
coordinates: lat: 49.573055555556
lon: 19.530555555556
surface_form: Turbacz
instance_of: Mountain
countries: Poland
coordinates: lat: 49.5428
lon: 20.1039
Lovön. Lovön is an island in the Swedish Lake Mälaren in Ekerö Municipality of Stockholm County. It was a municipality of its own until 1952, when it was joined with Ekerö Municipality. Lovön's greatest attraction is Drottningholm Palace and its many public gardens, which were built on the island in 1580. History. There is much known about the history of this rather small island.

Geographic entities mentioned:
surface_form: Mälaren
instance_of: Lake
countries: Sweden
coordinates: lat: 59.5
lon: 17.2
lavaretus&quot;. Distribution and habitat. The gwyniad is endemic to Bala Lake (Llyn Tegid) in the upper drainage system of the River Dee in the county of Gwynedd in north Wales. This species is found in the benthopelagic zone in the deeper parts of the two lakes it now inhabits but it undertakes daily vertical migrations to forage nearer the surface in the warmer months of the year. Conservation.

Geographic entities mentioned:
surface_form: Bala Lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.883333333333
lon: -3.6333333333333
Central California Traction Company. The Central California Traction Company is a Class III short-line railroad operating in the northern San Joaquin Valley, in San Joaquin County, California. It is owned jointly by the Union Pacific and BNSF Railway. Service. The railroad operates between Stockton and Lodi. CCT also operates the Stockton Public Belt Railway around the Port of Stockton.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Mount Minami. is a volcano located on the Shiretoko Peninsula in Hokkaido, northeastern Japan.

Geographic entities mentioned:
surface_form: mount minami
instance_of: Mountain
countries: Japan
coordinates: lat: 44.11230556
lon: 145.16072222
Vaajakoski-Jyskä. Vaajakoski-Jyskä is a ward of Jyväskylä, Finland. It is located seven kilometres from the city centre on both sides of Vaajavirta river on the Northern end of lake Päijänne and on the Western end of Lake Leppävesi. As of July 2011 the population of Vaajakoski-Jyskä was 14.588. Before 2009 Vaajakoski-Jyskä belonged to Jyväskylän maalaiskunta.

Geographic entities mentioned:
surface_form: Leppävesi
instance_of: Lake
countries: Finland
coordinates: lat: 62.25
lon: 25.95
From 1970 to 1985, Tabacci served for the Christian Democracy (DC) party as city councillor for several municipalities in the province of Mantua, including Mantua itself. From 1985 to 1991, he was regional councillor of Lombardy and from 1987 to 1989 he also served as President of the Region, during which he dealt with the disastrous flood in Valtellina, from July to September 1987.

Geographic entities mentioned:
surface_form: Valtellina
instance_of: Valley
countries: Italy
coordinates: lat: 46.166666666667
lon: 9.8666666666667
Etymology. In pre-European times, the Ngarrindjeri people used the Marne Valley as a route up into the hills to trade with the Peramangk people in the Barossa Valley and to cut bark canoes from the River Red Gums in the hills which had thicker bark than those near the Murray. The original name of the Marne River was &quot;Taingappa&quot;, meaning footrack-trading road.

Geographic entities mentioned:
surface_form: Barossa Valley
instance_of: Valley
countries: Australia
coordinates: lat: -34.533333333333
lon: 138.95
Julussdalen. Julussdalen is a small valley in Innlandet county, Norway. The valley runs through Elverum Municipality and Åmot Municipality as it follows the river Julussa, about east of the village of Rena. There are scattered settlements in the valley, especially in the lower part in Elverum. Julussdalen has many historic farms with cabins, mills, and mountain pastures. Geography.

Geographic entities mentioned:
surface_form: julussdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.038
lon: 11.692
Geography. The river Julussa flows through the valley, starting from Bergesjøen which is at an elevation of above sea level, and ending as the Julussa flows into the large river Glomma. Julussdalen was very important for timber out of the big forests, dating from around the mid-16th century. Etymology. Julussdalen is named after the river Julussa.

Geographic entities mentioned:
surface_form: julussdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.038
lon: 11.692
Julussdalen was very important for timber out of the big forests, dating from around the mid-16th century. Etymology. Julussdalen is named after the river Julussa. The first part of the name &quot;Juluss&quot; is most likely derived from a Norwegian dialect word that means &quot;silent&quot;, and the last part &quot;dalen&quot; is the Norwegian word for &quot;valley&quot;.

Geographic entities mentioned:
surface_form: julussdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.038
lon: 11.692
Area code 626. Area code 626 is a telephone area code in the North American Numbering Plan (NANP) for most of the San Gabriel Valley in the U.S. state of California. The numbering plan area (NPA) also comprises nearby areas in the northeastern portion of Los Angeles County, California, including Arcadia, Monrovia, El Monte, most of Pasadena and West Covina.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
Kalenica. Kalenica () is a mountain in the Owl Mountains, part of Central Sudetes. Its height is 964 meters. It lies in Owl Mountains Landscape Park. The mountain located in Dzierżoniów County, Lower Silesian Voivodeship, in south-western Poland.

Geographic entities mentioned:
surface_form: kalenica
instance_of: Mountain
countries: Poland
coordinates: lat: 50.643333333333
lon: 16.546666666667
Episodes. On 26 January 1965, &quot;Eye Opener&quot; was pre-empted by &quot;Wall of Ice&quot;, an hour-long documentary about a Canadian expedition to Denali. &quot;The Dutchman&quot;, a drama on racial relations by Leroi Jones, was planned for broadcast on &quot;Eye Opener&quot;, but there was no confirmation whether this production was cancelled or televised. Controversy.

Geographic entities mentioned:
surface_form: Denali
instance_of: Mountain
countries: United States
coordinates: lat: 63.06916666666667
lon: -151.0063888888889
Lost Corner Mountain. Lost Corner Mountain is a mountain summit in the Sierra Nevada mountain range to the west of Lake Tahoe on the border of the Desolation Wilderness in El Dorado County, California. The city closest to it is Meyers, California which is 4.4 miles away. The Pacific Crest Trail skirts the mountain on its west flank.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: lost corner mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.0135
lon: -120.204
Lost Corner Mountain. Lost Corner Mountain is a mountain summit in the Sierra Nevada mountain range to the west of Lake Tahoe on the border of the Desolation Wilderness in El Dorado County, California. The city closest to it is Meyers, California which is 4.4 miles away. The Pacific Crest Trail skirts the mountain on its west flank.

Geographic entities mentioned:
surface_form: lost corner mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.0135
lon: -120.204
Dease Lake (British Columbia). Dease Lake is a lake in the Stikine Plateau of the Northern Interior of British Columbia, Canada, located at the head of the Dease River, which flows north then northeast from the lake to join the Liard River.

Geographic entities mentioned:
surface_form: Stikine Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: dease lake
instance_of: Lake
countries: Canada
coordinates: lat: 58.63502
lon: -130.03761
The community of Dease Lake, British Columbia, formerly Dease Lake Post, is located at the south end of the lake, straddling a low pass which leads into the basin from the Tanzilla River, a tributary of the Stikine. The area around the lake was the focus of the Cassiar Gold Rush and numerous ghost towns and former settlement sites are scattered around its shores, including Laketon and Centre City.

Geographic entities mentioned:
surface_form: Tanzilla River
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.126944
lon: -130.669722
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: dease lake
instance_of: Lake
countries: Canada
coordinates: lat: 58.63502
lon: -130.03761
surface_form: dease lake
instance_of: Lake
countries: Canada
coordinates: lat: 58.63502
lon: -130.03761
Dease Lake (British Columbia). Dease Lake is a lake in the Stikine Plateau of the Northern Interior of British Columbia, Canada, located at the head of the Dease River, which flows north then northeast from the lake to join the Liard River.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: dease lake (british columbia)
instance_of: Lake
countries: Canada
coordinates: lat: 58.63502
lon: -130.03761
The area around the lake was the focus of the Cassiar Gold Rush and numerous ghost towns and former settlement sites are scattered around its shores, including Laketon and Centre City. Dease Lake is the burial site and has a monument to English travelogue writer Warburton Pike. Name origin.

Geographic entities mentioned:
surface_form: dease lake
instance_of: Lake
countries: Canada
coordinates: lat: 58.63502
lon: -130.03761
Name origin. The lake was named in 1834 by John McLeod, a Chief Trader for the Hudson's Bay Company at the former Dease Lake Post, for Peter Warren Dease, superintendent of the New Caledonia Fur District from 1830 to 1834, who had served with the Franklin Expedition of 1825-27 and later was senior officer of the Dease & Simpson Arctic Expedition in 1837–39.

Geographic entities mentioned:
surface_form: dease lake
instance_of: Lake
countries: Canada
coordinates: lat: 58.63502
lon: -130.03761
Saray Khumalo. Saray Khumalo (born 1972) is a Zambian-born, South African explorer and mountaineer. In May 2019, she became the first black African woman to reach the summit of Mount Everest. Personal life. With a Rwandan bloodline but now resident in South Africa, Khumalo was born in Zambia. She works as an e-commerce business executive. She is a mother of two children. Mountain climbing.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Saray has also completed the Seven Summits challenge, which involves climbing the highest peaks on each of the seven continents. It includes Mount Everest (Asia), Mount Kilimanjaro (Africa), Denali (North America), Aconcagua (South America), Vinson Massif (Antartica), Mount Elbrus (Europe), and Mount Kosciuszko (Australia) or Carstensz Pyramid (Australasia). Philanthropy.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
surface_form: Denali
instance_of: Mountain
countries: United States
coordinates: lat: 63.06916666666667
lon: -151.0063888888889
surface_form: Aconcagua
instance_of: Mountain
countries: Argentina
coordinates: lat: -32.653055555555554
lon: -70.01166666666667
surface_form: Vinson Massif
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
surface_form: Mount Elbrus
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 43.35254
lon: 42.437875
surface_form: Mount Kosciuszko
instance_of: Mountain
countries: Australia
coordinates: lat: -36.4558303
lon: 148.2635105
The economy of the region is based on agriculture, livestock and manufacturing. The population of the area as of the 2006 census was 23,861. The division contains all of the south basin of Lake Manitoba, and borders the west shore of the north basin (which is part of Division No. 19). It also contains Hecla-Grindstone Provincial Park at its northeast corner.

Geographic entities mentioned:
surface_form: Lake Manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
Chief engineer William E. Raby formulated its initial plans, which settled upon the production of alternating current to feed three phase motors, powered by waterfalls of the nearby Chivilingo River. Construction work began in 1896, with civil works and the aqueduct built by the mining company, and hydraulic and electric engineering performed by Consolidated Co.

Geographic entities mentioned:
surface_form: Chivilingo River
instance_of: Watercourse
countries: Chile
coordinates: lat: -37.141388888889
lon: -73.171111111111
Hills. The hills on the left-hand or northern side of the valley reach a maximum height above sea level of 514 metres in the &quot;Mückenberg&quot; and are clearly lower than those opposite. On the right hand, southern, side the Bloskülb (570 m) and the Brogberg (567 m) are the highest peaks.

Geographic entities mentioned:
surface_form: Bloskülb
instance_of: Mountain
countries: Germany
coordinates: lat: 49.3333
lon: 7.9
surface_form: Brogberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.3308
lon: 7.89611
surface_form: bloskülb
instance_of: Mountain
countries: Germany
coordinates: lat: 49.3333
lon: 7.9
surface_form: brogberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.3308
lon: 7.89611
Elmstein valley. The Elmstein valley () runs through the central Palatine Forest region between the villages of Frankeneck and Johanniskreuz in the German state of Rhineland-Palatinate. The Speyerbach stream, a left tributary of the Rhine, flows through the valley. Location.

Geographic entities mentioned:
surface_form: elmstein valley
instance_of: Valley
countries: Germany
coordinates: lat: 49.3467
lon: 7.94778
The Speyerbach stream, a left tributary of the Rhine, flows through the valley. Location. Most of the Elmstein valley lies within the county of Bad Dürkheim; two smaller segments belong to Neustadt an der Weinstraße and the county of Südliche Weinstraße. The valley is 24 kilometres long and descends from west to east from about 470 to 170 metres above sea level. Waterbodies.

Geographic entities mentioned:
surface_form: elmstein valley
instance_of: Valley
countries: Germany
coordinates: lat: 49.3467
lon: 7.94778
The valley is 24 kilometres long and descends from west to east from about 470 to 170 metres above sea level. Waterbodies. The Speyerbach stream flows through the Elmstein valley. Together with its tributary streams, the biggest of which are the Helmbach and the Breitenbach, the Speyerbach drains the winding valley and the heights surrounding it. Hills.

Geographic entities mentioned:
surface_form: elmstein valley
instance_of: Valley
countries: Germany
coordinates: lat: 49.3467
lon: 7.94778
Structures. The four medieval castles above the valley, namely Elmstein, Breitenstein, Erfenstein and Spangenberg, guarded the sovereignty of the local territorial lords here for centuries. Today their ruins are visited by tourists, not least because of the legend of the Leather Bridge that is supposed to have existed between Erfenstein and Spangenberg.

Geographic entities mentioned:
surface_form: breitenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 48.583
lon: 9.5015
surface_form: breitenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 47.7222
lon: 11.9892
On the right hand, southern, side the Bloskülb (570 m) and the Brogberg (567 m) are the highest peaks. The highest point in the west, also the start of the valley, lies on the watershed between the Rhine and Moselle rivers, separating here the catchment areas of the Speyerbach and Schwarzbach. In the east the valley ends at the confluence of the Hochspeyerbach with the Speyerbach. Structures.

Geographic entities mentioned:
surface_form: schwarzbach
instance_of: Watercourse
countries: Germany
coordinates: lat: 49.3141
lon: 8.82233
In male apex round, wings transparent. There is a silvery tint with a trace of eyespot on tornus in hindwing. Female has bluish dorsum and bands irrorated with silvery white with dark blue. Larval host plants are &quot;Embelia tsjeriam-cottam&quot; and &quot;Ardisia humilis&quot;. A new subspecies, N. s. ramaswamii, was discovered in Pothigai in 2021.

Geographic entities mentioned:
surface_form: Pothigai
instance_of: Mountain
countries: India
coordinates: lat: 8.6166916666667
lon: 77.24625
Cache Col. Cache Col is a gap in a high ridge between Magic Mountain and Mix-up Peak. It's located at the highest part of Cache Glacier, on the shared boundary of Skagit County and Chelan County in Washington state. Cache Col is situated south of Cascade Pass on the shared border of North Cascades National Park and Glacier Peak Wilderness.

Geographic entities mentioned:
surface_form: Mix-up Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.45401
lon: -121.06095
surface_form: cache col
instance_of: Mountain
countries: United States
coordinates: lat: 48.4484594
lon: -121.0528892
surface_form: magic mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.446
lon: -121.041379
Cache Col is situated south of Cascade Pass on the shared border of North Cascades National Park and Glacier Peak Wilderness. Cache Col and the Cache Glacier are at the northern end of the Ptarmigan Traverse which is mountaineering route that provides access to remote peaks such as Mount Formidable and Dome Peak.

Geographic entities mentioned:
surface_form: Mount Formidable
instance_of: Mountain
countries: United States
coordinates: lat: 48.4164
lon: -121.067
surface_form: Dome Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.3034
lon: -121.03
surface_form: cache col
instance_of: Mountain
countries: United States
coordinates: lat: 48.4484594
lon: -121.0528892
surface_form: dome peak
instance_of: Mountain
countries: United States
coordinates: lat: 42.1019
lon: -73.4325
surface_form: dome peak
instance_of: Mountain
countries: United States
coordinates: lat: 58.5044
lon: -135.2575
Cache Col. Cache Col is a gap in a high ridge between Magic Mountain and Mix-up Peak. It's located at the highest part of Cache Glacier, on the shared boundary of Skagit County and Chelan County in Washington state. Cache Col is situated south of Cascade Pass on the shared border of North Cascades National Park and Glacier Peak Wilderness.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
Cache Col. Cache Col is a gap in a high ridge between Magic Mountain and Mix-up Peak. It's located at the highest part of Cache Glacier, on the shared boundary of Skagit County and Chelan County in Washington state. Cache Col is situated south of Cascade Pass on the shared border of North Cascades National Park and Glacier Peak Wilderness.

Geographic entities mentioned:
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.14972222
lon: -109.84944444
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.155013
lon: -117.293429
surface_form: cache col
instance_of: Mountain
countries: United States
coordinates: lat: 48.4484594
lon: -121.0528892
Cache Col. Cache Col is a gap in a high ridge between Magic Mountain and Mix-up Peak. It's located at the highest part of Cache Glacier, on the shared boundary of Skagit County and Chelan County in Washington state. Cache Col is situated south of Cascade Pass on the shared border of North Cascades National Park and Glacier Peak Wilderness.

Geographic entities mentioned:
surface_form: cache col
instance_of: Mountain
countries: United States
coordinates: lat: 48.4484594
lon: -121.0528892
Precipitation runoff on the north side of the col drains into the Stehekin River, while precipitation drains into the Cascade River from the south side. Climate. Cache Col is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains.

Geographic entities mentioned:
surface_form: cache col
instance_of: Mountain
countries: United States
coordinates: lat: 48.4484594
lon: -121.0528892
Rancho Sespe. Rancho Sespe was a Mexican land grant in present-day Ventura County, California given in 1833 by Governor José Figueroa to Carlos Antonio Carrillo. The grant encompassed the Santa Clara River Valley between Piru Creek on the east and Santa Paula Creek on the west, and was bounded to the north and south by the mountains, and included present day Fillmore. History.

Geographic entities mentioned:
surface_form: Santa Clara River Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.3667
lon: -118.983
The area includes both Ronaldsway and Balthane industrial estates and the Isle of Man Airport. The parish is bordered on the east by Castletown and Santon Burn; on the north by the Granite Mountain and the South Barrule; by an irregular line from the South Barrule to Poyll Vaaish on the west; and by the sea on the south. It contains about.

Geographic entities mentioned:
surface_form: South Barrule
instance_of: Mountain
countries: Isle of Man
coordinates: lat: 54.149
lon: -4.67
It contains about. Most of the parish is low and undulating, forming much of the southern plain of the Island. The northern portion is more hilly, including the South Barrule, the highest point of the south of the Island at. The Silver Burn river rises near the South Barrule and flows under the Monks Bridge at Ballasalla, reaching the sea at Castletown harbour.

Geographic entities mentioned:
surface_form: South Barrule
instance_of: Mountain
countries: Isle of Man
coordinates: lat: 54.149
lon: -4.67
The seal's heraldic elements may be evidence that Gilecrist's family was related to the Bissetts. In 1267, Alexander III, King of Scots granted Gilchrist the custody of the castle on Fraoch Eilean, an island in the northern end of Loch Awe.

Geographic entities mentioned:
surface_form: Loch Awe
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.291475
lon: -5.231141
Heidal cheese. Heidal cheese (or simply &quot;heidal&quot;) is a Norwegian brunost. The cheese is named after the parish of Heidal in the northern part of the Gudbrand Valley. It is dark brown. Heidal cheese is a molded cheese that was first produced at one of the many farms in Heidal. The cheese is currently produced by the Tine company and by the local Heidal Cheese Factory in Heidal.

Geographic entities mentioned:
surface_form: Heidal
instance_of: Valley
countries: Norway
coordinates: lat: 61.71789
lon: 9.4512
Aside from skiing, Çarıkçıoğlu practices ballet. Sports career. At the age of eight, Çarıkçıoğlu made acquaintance with skiing during a winter camp at Uludağ in Bursa held by her primary school. She is a member of the AKUT Search and Rescue Association, and competed for the AKUT sports Club's Snow Sports Branch. She competed at the 2011 European Youth Olympic Winter Festival.

Geographic entities mentioned:
surface_form: Uludağ
instance_of: Mountain
countries: Turkey
coordinates: lat: 40.0705295
lon: 29.222009805555555
Lang Sound. bglgy1r7jwo5l4cfw7uolcemkban" xml:space="preserve">Lang Sound () is a sound wide at its narrowest point and long, lying between the group of islands that includes Broka Island and Havstein Island and Law Promontory. It was mapped by Norwegian cartographers from aerial photographs taken by the Lars Christensen Expedition in January–February 1937 and named Langsundet (the long sound).

Geographic entities mentioned:
surface_form: Law Promontory
instance_of: Landform
coordinates: lat: -67.22
lon: 58.8
surface_form: lang sound
instance_of: Landform
Body of water
coordinates: lat: -67.15
lon: 58.6667
Lang Sound. bglgy1r7jwo5l4cfw7uolcemkban" xml:space="preserve">Lang Sound () is a sound wide at its narrowest point and long, lying between the group of islands that includes Broka Island and Havstein Island and Law Promontory. It was mapped by Norwegian cartographers from aerial photographs taken by the Lars Christensen Expedition in January–February 1937 and named Langsundet (the long sound).

Geographic entities mentioned:
surface_form: christensen
instance_of: Mountain
coordinates: lat: -65.1
lon: -59.5167
surface_form: langsundet
instance_of: Landform
Body of water
coordinates: lat: -67.15
lon: 58.6667
surface_form: long sound
instance_of: Landform
Body of water
coordinates: lat: -67.15
lon: 58.6667
Lang Sound. bglgy1r7jwo5l4cfw7uolcemkban" xml:space="preserve">Lang Sound () is a sound wide at its narrowest point and long, lying between the group of islands that includes Broka Island and Havstein Island and Law Promontory. It was mapped by Norwegian cartographers from aerial photographs taken by the Lars Christensen Expedition in January–February 1937 and named Langsundet (the long sound).

Geographic entities mentioned:
surface_form: lang sound
instance_of: Landform
Body of water
coordinates: lat: -67.15
lon: 58.6667
The album's crown jewel, &quot;Fancy Pants&quot;, is a paean to one of Clarke's musical heroes, David Bowie. But many of Clarke's songs are clearly the product by his local work with groups of children in the Lower Hudson Valley region of New York and Clarke has said at his live shows that &quot;Jack, Jack, Jackson and Jason&quot; are four actual boys from one of his music classes.

Geographic entities mentioned:
surface_form: Lower Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Midge Lake. Midge Lake is the largest among numerous freshwater lakes on the ice-free Byers Peninsula, Livingston Island in the South Shetland Islands, Antarctica. The feature is arcuate in shape, extending 575 m in southwest-northeast direction and 125 m wide, surmounted by Chester Cone on the southeast, and draining through a 2 km stream north-northeastwards into Baba Tonka Cove.

Geographic entities mentioned:
surface_form: Chester Cone
instance_of: Mountain
coordinates: lat: -62.6365
lon: -61.0849
Midge Lake. Midge Lake is the largest among numerous freshwater lakes on the ice-free Byers Peninsula, Livingston Island in the South Shetland Islands, Antarctica. The feature is arcuate in shape, extending 575 m in southwest-northeast direction and 125 m wide, surmounted by Chester Cone on the southeast, and draining through a 2 km stream north-northeastwards into Baba Tonka Cove.

Geographic entities mentioned:
surface_form: midge lake
instance_of: Lake
coordinates: lat: -62.6303
lon: -61.095
Rivière le Renne. The rivière le Renne (&quot;English: Reindeer River&quot;) is a tributary of the Yamaska River, which flows in the municipalities of Maricourt, Sainte-Christine, Acton Vale, Saint-Nazaire-d'Acton, of Saint-Théodore-d'Acton, in the Acton Regional County Municipality (MRC), on the South Shore of the Saint Lawrence River, in Estrie, in Quebec, Canada. Geography.

Geographic entities mentioned:
surface_form: rivière le renne
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.68111
lon: -72.64778
Geography. The Renne river has its source in the Rivard stream, whose mouth is located northwest of the village of Maricourt. Upper course of the river (segment of)
Lower course of the river (segment of)
The Renne river flows on the north bank of the Black River (Yamaska River). Toponymy. Formerly, this stream was known as the &quot;Moose River&quot;.

Geographic entities mentioned:
surface_form: black river
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.05011
lon: -65.21543
He became one of the leading gamblers in Chicago and was known for taking bets on everything from presidential candidates to changes in the weather. In 1904, O'Leary began operating illegal gambling on Lake Michigan aboard the steamship &quot;The City of Traverse&quot;. Without police protection, this venture had failed by 1907 because of police raids each time the ship docked.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Since 2022, it has been a member of the 4th tier of the US soccer pyramid. History. Allentown United FC was founded by the young Lehigh Valley native, Emmanuel Ntow-Mensah in 2018 with the goal of supporting the local soccer community with hopes to showcase the talent on a broader regional and national level. The club made its debut on field in 2019 by joining the United Premier Soccer League.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Natashquan stretches along the coast, on both sides of the Little Natashquan River, about 120 km east of Havre-Saint-Pierre, near Aguanish and the Natashkuan Indian reserve. Pointe-Parent. In addition to the village of Natashquan itself, the municipality also includes the hamlet of Pointe-Parent located on the Natashquan River shore, directly adjacent to the Natashquan Reserve.

Geographic entities mentioned:
surface_form: Natashquan River
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.118611
lon: -61.807222
Notre-Dame-de-Natashquan Mission. Between 1855 and 1860, the pioneers of Natashquan lived without a parish organization, the construction of the church began in July 1859, the pioneer families participated in cutting the necessary wood inland from the great Natashquan River. The Notre-Dame-de-Natashquan Mission was founded on the west bank of the Little Natashquan River.

Geographic entities mentioned:
surface_form: Natashquan River
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.118611
lon: -61.807222
In 1684, the explorer Louis Jolliet spelled other spellings appearing with time. Noutascoüan, Nontascouanne, Natasquan, Nataskwan, Natashkwan, Natosquan, Nataskouan. A trading post already existed in 1710 at the mouth of the Natashquan River, the settlement of Natashquan in the eponymous township was not founded until 1855 when the first settlers arrived.

Geographic entities mentioned:
surface_form: Natashquan River
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.118611
lon: -61.807222
Route 138. At the beginning of the 20th century, the first routes of what would become Route 138 (formerly Route 15) were laid in the vicinity of Sept-Îles. In 1961, a section was added from the Franquelin region to the tip of the Moisie River, some 20 kilometres east of Sept-Îles. On the north shore of the Gulf of St.

Geographic entities mentioned:
surface_form: Franquelin
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.290555555556
lon: -67.894722222222
surface_form: Moisie River
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.2
lon: -66.0675
At the north end of the village of Ihlara, there is a stairway with almost 400 steps, which descends over 100 m down into the canyon. From the 7th century AD, the valley was settled by Byzantine monks who dug their houses and churches out of the tuff stone, which had been deposited by the eruptions of Mount Hasan. Churches. The Christian churches in the valley fall into two groups.

Geographic entities mentioned:
surface_form: Mount Hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
Ihlara valley. The Ihlara Valley (or Peristrema Valley; Turkish &quot;Ihlara Vadisi&quot;) is a canyon which is 15 km long and up to 150 m deep in the southwest of the Turkish region of Cappadocia, in the municipality of Güzelyurt, Aksaray Province. The valley contains around 50 rock-hewn Christian churches and numerous rock-cut buildings. Etymology.

Geographic entities mentioned:
surface_form: ihlara valley
instance_of: Valley
countries: Turkey
coordinates: lat: 38.2575
lon: 34.295277777778
Ihlara valley. The Ihlara Valley (or Peristrema Valley; Turkish &quot;Ihlara Vadisi&quot;) is a canyon which is 15 km long and up to 150 m deep in the southwest of the Turkish region of Cappadocia, in the municipality of Güzelyurt, Aksaray Province. The valley contains around 50 rock-hewn Christian churches and numerous rock-cut buildings. Etymology.

Geographic entities mentioned:
surface_form: ihlara valley
instance_of: Valley
countries: Turkey
coordinates: lat: 38.2575
lon: 34.295277777778
surface_form: ihlara vadisi
instance_of: Valley
countries: Turkey
coordinates: lat: 38.2575
lon: 34.295277777778
In the Niğde Archaeological Museum, there is a display of the mummies of a woman and four children who were entombed in the Ihlara Valley in the 10th century AD. The Aksaray Museum also has mummies from the Ihlara valley.

Geographic entities mentioned:
surface_form: ihlara valley
instance_of: Valley
countries: Turkey
coordinates: lat: 38.2575
lon: 34.295277777778
surface_form: ihlara valley
instance_of: Valley
countries: Turkey
coordinates: lat: 38.2575
lon: 34.295277777778
Ose, Norway. Ose is a village in Bygland municipality in Agder county, Norway. The village is located along the river Otra, just north of the lake Åraksfjorden. The Norwegian National Road 9 runs through the village. Just across the river to the north lies the village of Austad, and about to the north along Highway 9 lies the village of Moi. The Reiårsfossen waterfall lies about to the south.

Geographic entities mentioned:
surface_form: Åraksfjorden
instance_of: Lake
countries: Norway
coordinates: lat: 58.925555555556
lon: 7.7116666666667
There is a traditionally-built log building in Ose called &quot;Storståga&quot;, which is used for various exhibitions. The is a wood-fuelled heritage steamboat that travels the route between Byglandsfjord-Bygland-Ose across the lake Byglandsfjorden and Åraksfjorden each summer.

Geographic entities mentioned:
surface_form: Byglandsfjorden
instance_of: Lake
countries: Norway
coordinates: lat: 58.708333333333
lon: 7.8069444444444
surface_form: Åraksfjorden
instance_of: Lake
countries: Norway
coordinates: lat: 58.925555555556
lon: 7.7116666666667
Sidi M'Cid Bridge. Sidi M'Cid Bridge is a suspension bridge across the Rhumel River in Constantine, Algeria. It was opened to traffic in April 1912 and until 1929 was the highest bridge in the world at. The bridge was designed by French engineer Ferdinand Arnodin and links the Casbah to Sidi M'Cid hill.

Geographic entities mentioned:
surface_form: Rhumel River
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.87212817
lon: 6.08567476
Four Mile Trail. Four Mile Trail is a moderate to strenuous trail leading from Yosemite Valley to Glacier Point. The trail begins at the valley floor west of the Swinging Bridge recreation area, and climbs the south side up to Glacier Point, an elevation change of. Four Mile Trail was originally constructed in 1872 and was in length.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
In the early 1900s the trail was reconstructed and lengthened to, yet the original name remained. This trail is remarkable because it offers views of most of the Yosemite Valley landmarks. The trail begins at the base of the Sentinel Rock. The first four miles are full of grand views of El Capitan and Yosemite Falls, as well as the Merced River as it runs through the valley.

Geographic entities mentioned:
surface_form: Sentinel Rock
instance_of: Mountain
countries: United States
coordinates: lat: 37.7288
lon: -119.594
This trail is remarkable because it offers views of most of the Yosemite Valley landmarks. The trail begins at the base of the Sentinel Rock. The first four miles are full of grand views of El Capitan and Yosemite Falls, as well as the Merced River as it runs through the valley. The second half of the trail provides several good views of Half Dome and Tenaya Canyon.

Geographic entities mentioned:
surface_form: Half Dome
instance_of: Mountain
countries: United States
coordinates: lat: 37.746
lon: -119.53316666667
Aguilera is part of the Andean Austral Volcanic Zone, which lies in the southernmost territory of Chile. It consists of six volcanoes, from north to south these are Lautaro, Viedma, Aguilera, Reclus, Monte Burney and Cook; only the first has clearly documented historical activity, in 1959–1960.

Geographic entities mentioned:
surface_form: Monte Burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
surface_form: Cook
instance_of: Mountain
countries: Chile
coordinates: lat: -54.95
lon: -70.25
surface_form: lautaro
instance_of: Mountain
countries: Chile
coordinates: lat: -49.019
lon: -73.504
surface_form: reclus
instance_of: Mountain
countries: Chile
coordinates: lat: -50.9639
lon: -73.5847
surface_form: aguilera
instance_of: Mountain
countries: Chile
coordinates: lat: -50.402222222222
lon: -73.788055555556
A tephra layer found at archeological sites around Lago Argentino and deposited there 4,091 - 4,566 years before present originated at Aguilera and probably disrupted local human communities. Farther away in Antarctica, a tephra found in Talos Dome and deposited there 4,420 years before present may have originated at this volcano as well.

Geographic entities mentioned:
surface_form: Talos Dome
instance_of: Landform
coordinates: lat: -73
lon: 158
On Isla Grande de Tierra del Fuego apparently the eruption did not substantially impact human populations. Chemicals derived from Aguilera tephra are found in cave deposits close to Monte Burney. Furthermore, a 3,600 years old sulfur dioxide-rich layer in ice cores from Talos Dome, Antarctica, may have been produced by the Aguilera eruption. First climb.

Geographic entities mentioned:
surface_form: Talos Dome
instance_of: Landform
coordinates: lat: -73
lon: 158
surface_form: aguilera
instance_of: Mountain
countries: Chile
coordinates: lat: -50.402222222222
lon: -73.788055555556
surface_form: aguilera
instance_of: Mountain
countries: Chile
coordinates: lat: -50.402222222222
lon: -73.788055555556
The first five are located on the South America Plate at increasing distances from the trench, while Cook is on the Scotia Plate and is a complex of lava domes unlike the other volcanoes which are stratovolcanoes. North of Lautaro lies a long gap without volcanism and then Cerro Hudson, the southernmost volcano of the Southern Volcanic Zone.

Geographic entities mentioned:
surface_form: lautaro
instance_of: Mountain
countries: Chile
coordinates: lat: -49.019
lon: -73.504
surface_form: cerro hudson
instance_of: Mountain
countries: Chile
coordinates: lat: -45.92
lon: -72.95
Melts of subducted sediment and from the subducting slab give rise to the magmas of Aguilera and other volcanoes of the northern Austral Volcanic Zone, but they are subsequently modified by interactions with the mantle wedge and in the case of Aguilera, Lautaro and Viedma, further interaction takes place with the Paleozoic crust. Climate and vegetation.

Geographic entities mentioned:
surface_form: lautaro
instance_of: Mountain
countries: Chile
coordinates: lat: -49.019
lon: -73.504
surface_form: aguilera
instance_of: Mountain
countries: Chile
coordinates: lat: -50.402222222222
lon: -73.788055555556
surface_form: aguilera
instance_of: Mountain
countries: Chile
coordinates: lat: -50.402222222222
lon: -73.788055555556
Eruption history. Aguilera erupted during the Holocene, depositing tephra in the region of Lago Argentino and Torres del Paine. The composition of rocks erupted by Aguilera are similar to these from Lautaro and Viedma, and the linkage of specific ash deposits to Aguilera is based mainly on geographical considerations.

Geographic entities mentioned:
surface_form: lautaro
instance_of: Mountain
countries: Chile
coordinates: lat: -49.019
lon: -73.504
surface_form: aguilera
instance_of: Mountain
countries: Chile
coordinates: lat: -50.402222222222
lon: -73.788055555556
The composition of rocks erupted by Aguilera are similar to these from Lautaro and Viedma, and the linkage of specific ash deposits to Aguilera is based mainly on geographical considerations. Other volcanoes have left tephra deposits in the wider region, including Cerro Hudson, Monte Burney and Reclus.

Geographic entities mentioned:
surface_form: reclus
instance_of: Mountain
countries: Chile
coordinates: lat: -50.9639
lon: -73.5847
surface_form: cerro hudson
instance_of: Mountain
countries: Chile
coordinates: lat: -45.92
lon: -72.95
surface_form: monte burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
A1 eruption. The major A1 eruption occurred at Aguilera or years ago. It deposited tephra east of the volcano as far south as the Strait of Magellan; other Aguilera tephras are less widespread. Its volume has been estimated to be between, larger than the 1991 eruption of Cerro Hudson, reaching level 5 on the volcanic explosivity index.

Geographic entities mentioned:
surface_form: cerro hudson
instance_of: Mountain
countries: Chile
coordinates: lat: -45.92
lon: -72.95
On Isla Grande de Tierra del Fuego apparently the eruption did not substantially impact human populations. Chemicals derived from Aguilera tephra are found in cave deposits close to Monte Burney. Furthermore, a 3,600 years old sulfur dioxide-rich layer in ice cores from Talos Dome, Antarctica, may have been produced by the Aguilera eruption. First climb.

Geographic entities mentioned:
surface_form: monte burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
Aguilera (volcano). Aguilera () is a stratovolcano in southern Chile. The volcano rises above the edge of the Southern Patagonian Ice Field. It is a remote volcano that was identified as such in 1985. The first ascent only occurred in 2014, making it the last unclimbed major Andean volcano.

Geographic entities mentioned:
surface_form: aguilera
instance_of: Mountain
countries: Chile
coordinates: lat: -50.402222222222
lon: -73.788055555556
The first ascent only occurred in 2014, making it the last unclimbed major Andean volcano. Aguilera is located west of Lake Argentino and northeast of Peel Fjord in the southern Andes and erupted mainly dacites and pyroclastic tephra. It has erupted several times in the Holocene, with a major eruption taking place 3,000 ± 1,000 years before present.

Geographic entities mentioned:
surface_form: aguilera
instance_of: Mountain
countries: Chile
coordinates: lat: -50.402222222222
lon: -73.788055555556
Its eruptions have spread ashfalls over Patagonia. Geography and geomorphology. Aguilera lies west of the city of Calafate, northwest of Peel Fjord and within the commune of Natales. There is not much knowledge on volcanism in southernmost Chile/Patagonia as the volcanoes are poorly mapped, difficult to access and the weather conditions hostile.

Geographic entities mentioned:
surface_form: aguilera
instance_of: Mountain
countries: Chile
coordinates: lat: -50.402222222222
lon: -73.788055555556
There is not much knowledge on volcanism in southernmost Chile/Patagonia as the volcanoes are poorly mapped, difficult to access and the weather conditions hostile. Aguilera was named in 1933 by Alberto Maria de Agostini, so its volcanic nature was first established in 1985. Aguilera is part of the Andean Austral Volcanic Zone, which lies in the southernmost territory of Chile.

Geographic entities mentioned:
surface_form: aguilera
instance_of: Mountain
countries: Chile
coordinates: lat: -50.402222222222
lon: -73.788055555556
This subduction is responsible for the volcanism in the Austral Volcanic Zone, whereas earthquake activity is low; this is possibly because the subducting plate is too hot and too slow moving. The basement below Aguilera is of Paleozoic-early Mesozoic age and consists of metamorphic rocks.

Geographic entities mentioned:
surface_form: aguilera
instance_of: Mountain
countries: Chile
coordinates: lat: -50.402222222222
lon: -73.788055555556
The Austral Volcanic Zone was once considered part of the Southern Volcanic Zone. Composition. Aguilera has erupted dacites with intermediate contents of potassium, defining a calc-alkaline suite with adakitic characteristics. Phenocrysts include amphibole, biotite, clinopyroxene, hornblende and plagioclase; plagioclase and also orthoclase and pyroxene often occur as xenoliths.

Geographic entities mentioned:
surface_form: aguilera
instance_of: Mountain
countries: Chile
coordinates: lat: -50.402222222222
lon: -73.788055555556
Climate and vegetation. Aguilera lies within the Southern Hemisphere Westerlies belt and the average temperature of the region is about.

Geographic entities mentioned:
surface_form: aguilera
instance_of: Mountain
countries: Chile
coordinates: lat: -50.402222222222
lon: -73.788055555556
Eruption history. Aguilera erupted during the Holocene, depositing tephra in the region of Lago Argentino and Torres del Paine. The composition of rocks erupted by Aguilera are similar to these from Lautaro and Viedma, and the linkage of specific ash deposits to Aguilera is based mainly on geographical considerations.

Geographic entities mentioned:
surface_form: aguilera
instance_of: Mountain
countries: Chile
coordinates: lat: -50.402222222222
lon: -73.788055555556
A tephra layer found at archeological sites around Lago Argentino and deposited there 4,091 - 4,566 years before present originated at Aguilera and probably disrupted local human communities. Farther away in Antarctica, a tephra found in Talos Dome and deposited there 4,420 years before present may have originated at this volcano as well.

Geographic entities mentioned:
surface_form: aguilera
instance_of: Mountain
countries: Chile
coordinates: lat: -50.402222222222
lon: -73.788055555556
Another smaller eruption occurred at Aguilera after the A1 event and deposited ash in the Lago Argentino area; the date of its eruption is unknown. There are no known historical eruptions although an eruption reported in 1886 in the area may have occurred at Aguilera. A1 eruption. The major A1 eruption occurred at Aguilera or years ago.

Geographic entities mentioned:
surface_form: aguilera
instance_of: Mountain
countries: Chile
coordinates: lat: -50.402222222222
lon: -73.788055555556
A1 eruption. The major A1 eruption occurred at Aguilera or years ago. It deposited tephra east of the volcano as far south as the Strait of Magellan; other Aguilera tephras are less widespread. Its volume has been estimated to be between, larger than the 1991 eruption of Cerro Hudson, reaching level 5 on the volcanic explosivity index.

Geographic entities mentioned:
surface_form: aguilera
instance_of: Mountain
countries: Chile
coordinates: lat: -50.402222222222
lon: -73.788055555556