Sarmila/GeoWiki-Features huggingface dataset:
Leonard Pond. Leonard Pond is a lake located in Sevey, New York, USA. The outlet creek flows into the Raquette River. Fish species present in the lake are white sucker, smallmouth bass, largemouth bass, yellow perch and black bullhead. Access is by a trail off State Route 56 on the west shore.

Geographic entities mentioned:
surface_form: leonard pond
instance_of: Lake
countries: United States
coordinates: lat: 44.33175
lon: -74.73751
Ian Calderon. Ian Charles Calderon (born October 19, 1985) is an American politician who served in the California State Assembly. He is a Democrat who represented the 57th Assembly District, which encompasses the Gateway Cities and portions of the San Gabriel Valley from 2012 to 2020. He served as the Assembly Majority Leader from 2016 to 2020.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
Level Creek. Level Creek is a stream in Gwinnett County in the U.S. state of Georgia. It is a tributary that rises at Sugar Hill and flows westerly into the Chattahoochee River. It sits on an elevation of. Level Creek was so named on account of the relatively level terrain along its course. There is an elementary school named after this creek named Level Creek Elementary that is two miles away.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Lauteraarhorn. The Lauteraarhorn is a peak (4,042 m) of the Bernese Alps, located in the canton of Bern. Together with the higher Schreckhorn, to which it is connected by a high ridge, it lies between the valleys of the Lower Grindelwald Glacier and the Unteraar Glacier, about 10 kilometres southeast of Grindelwald, the closest locality.

Geographic entities mentioned:
surface_form: Schreckhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.58993
lon: 8.11816
Only the main summit of the Lauteraarhorn (together with the adjoining Schreckhorn) is on the UIAA list of Alpine four-thousanders. The first ascent was on 8 August 1842 by Pierre Jean Édouard Desor, Christian Girard, Arnold Escher von der Linth with the guides Melchior Bannholzer and Jakob Leuthold.

Geographic entities mentioned:
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.50486111
lon: 7.64305556
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6608
lon: 8.05469
The Lauteraarhorn belongs to the Aaremassif and is surrounded by large glaciers: the Lauteraargletscher and the Strahlegg-Gletscher (both feeders of the Unteraar Glacier) and the Obers Ischmeer (tributary of the Grindelwald Glacier). Being off the main ridge of the Bernese Alps, all the glaciers surrounding the Lauteraarhorn and the Schreckhorn are part of the Aare basin.

Geographic entities mentioned:
surface_form: schreckhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.58993
lon: 8.11816
surface_form: lauteraarhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.583388888889
lon: 8.1284166666667
Being off the main ridge of the Bernese Alps, all the glaciers surrounding the Lauteraarhorn and the Schreckhorn are part of the Aare basin. The Lauteraarhorn is the second highest summit (after the Schreckhorn) lying wholly within the canton of Bern. Administratively, it is split between the municipalities of Grindelwald and Guttannen.

Geographic entities mentioned:
surface_form: schreckhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.58993
lon: 8.11816
surface_form: lauteraarhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.583388888889
lon: 8.1284166666667
The Lauteraarhorn includes two unnamed but noticeable subsidiary summits: the north summit (4,015 m) and the central summit (4,014 m), both having a topographic prominence of over 30 metres. The main summit is the southernmost one and has a modest topographic prominence of 128 metres, due to the high elevation of the ridge (the Schrecksattel) connecting it to the slightly higher Schreckhorn.

Geographic entities mentioned:
surface_form: schreckhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.58993
lon: 8.11816
The main summit is the southernmost one and has a modest topographic prominence of 128 metres, due to the high elevation of the ridge (the Schrecksattel) connecting it to the slightly higher Schreckhorn. Only the main summit of the Lauteraarhorn (together with the adjoining Schreckhorn) is on the UIAA list of Alpine four-thousanders.

Geographic entities mentioned:
surface_form: schreckhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.58993
lon: 8.11816
surface_form: lauteraarhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.583388888889
lon: 8.1284166666667
Lauteraarhorn. The Lauteraarhorn is a peak (4,042 m) of the Bernese Alps, located in the canton of Bern. Together with the higher Schreckhorn, to which it is connected by a high ridge, it lies between the valleys of the Lower Grindelwald Glacier and the Unteraar Glacier, about 10 kilometres southeast of Grindelwald, the closest locality.

Geographic entities mentioned:
surface_form: lauteraarhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.583388888889
lon: 8.1284166666667
The Lauteraarhorn belongs to the Aaremassif and is surrounded by large glaciers: the Lauteraargletscher and the Strahlegg-Gletscher (both feeders of the Unteraar Glacier) and the Obers Ischmeer (tributary of the Grindelwald Glacier). Being off the main ridge of the Bernese Alps, all the glaciers surrounding the Lauteraarhorn and the Schreckhorn are part of the Aare basin.

Geographic entities mentioned:
surface_form: lauteraarhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.583388888889
lon: 8.1284166666667
The Lauteraarhorn is the second highest summit (after the Schreckhorn) lying wholly within the canton of Bern. Administratively, it is split between the municipalities of Grindelwald and Guttannen. The Lauteraarhorn includes two unnamed but noticeable subsidiary summits: the north summit (4,015 m) and the central summit (4,014 m), both having a topographic prominence of over 30 metres.

Geographic entities mentioned:
surface_form: lauteraarhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.583388888889
lon: 8.1284166666667
Climate. The Sankwala Mountains have a cool climate. This has attracted tourists to the mountains in recent years to the Obudu Plateau on the Sankwala Mountains. Tourist activities. The Sankwala Mountains record a high number of tourist activities every year. This has led to the development of the Obudu Mountain Resort on one of the ridges of the mountains, known as the Oshie Ridge.

Geographic entities mentioned:
surface_form: Oshie Ridge
instance_of: Mountain
countries: Nigeria
coordinates: lat: 6.35
lon: 9.33333333
Bremberg (Rothaar). The Bremberg is a mountain, high, in the Rothaar Mountains range in the district of Hochsauerland, in North Rhine-Westphalia, Germany. The mountain lies just under 3 km west-southwest of the ski resort of Winterberg, about 1 km west-southwest of the Poppenberg (745.5 m) and around 1.3 km (as the crow flies) north-northeast of the Kahler Asten (841.9 m).

Geographic entities mentioned:
surface_form: Kahler Asten
instance_of: Mountain
countries: Germany
coordinates: lat: 51.179444444444
lon: 8.4888888888889
Bremberg (Rothaar). The Bremberg is a mountain, high, in the Rothaar Mountains range in the district of Hochsauerland, in North Rhine-Westphalia, Germany. The mountain lies just under 3 km west-southwest of the ski resort of Winterberg, about 1 km west-southwest of the Poppenberg (745.5 m) and around 1.3 km (as the crow flies) north-northeast of the Kahler Asten (841.9 m).

Geographic entities mentioned:
surface_form: bremberg (rothaar)
instance_of: Mountain
countries: Germany
coordinates: lat: 51.1896
lon: 8.49515
Bremberg (Rothaar). The Bremberg is a mountain, high, in the Rothaar Mountains range in the district of Hochsauerland, in North Rhine-Westphalia, Germany. The mountain lies just under 3 km west-southwest of the ski resort of Winterberg, about 1 km west-southwest of the Poppenberg (745.5 m) and around 1.3 km (as the crow flies) north-northeast of the Kahler Asten (841.9 m).

Geographic entities mentioned:
surface_form: bremberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.1896
lon: 8.49515
The mountain lies just under 3 km west-southwest of the ski resort of Winterberg, about 1 km west-southwest of the Poppenberg (745.5 m) and around 1.3 km (as the crow flies) north-northeast of the Kahler Asten (841.9 m). Part of the Rhine-Weser watershed runs over the Bremberg.

Geographic entities mentioned:
surface_form: bremberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.1896
lon: 8.49515
Part of the Rhine-Weser watershed runs over the Bremberg. On and around the Bremberg is part of the ski area known as the Skiliftkarussell Winterberg with langlauf trails (&quot;Loipen&quot;), a langlauf stadium, which often hosts international competitions, ski lifts and their associated pistes and, on the eastern spur of the mountain, a toboggan run and a small ski jump.

Geographic entities mentioned:
surface_form: bremberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.1896
lon: 8.49515
Route 107 starts east of Nashwaak Bridge travelling south-west crossing Route 148 and into Nashwaak Bridge. From here, the route crosses the Nashwaak River before turning north-west and passing through Sutherland Siding. From here, the route is known as &quot;Irishtown Rd&quot; as it enters the community of Nashwaak. The route then turns north-east until Cross Creek, and northwest at Route 625.

Geographic entities mentioned:
surface_form: Nashwaak River
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.965694444444
lon: -66.586194444444
The route then turns north-east until Cross Creek, and northwest at Route 625. Through mostly uninhabited forest land, through Williamsburg then the railway siding of Napadogan as it passes Miramichi Lake then meets up and begins to follow the south bank of the Southwest Miramichi River as it passes Deersdale, to the community of Juniper.

Geographic entities mentioned:
surface_form: Southwest Miramichi River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.519346
lon: -67.151946
Trostian. Trostian () &ndash; mountain peak in an array of the Skole Beskids (Eastern Beskids), peak spine Stryiska-Sanskoyi Verhoviny and limited by valleys Opir River and Holovchanka River. Mountain Trostyan has a height of 1,232 metres (4,042 ft) and the steep (30-40 °) slopes at north-eastern. The top is flat.

Geographic entities mentioned:
surface_form: trostian
instance_of: Mountain
countries: Ukraine
coordinates: lat: 48.856666666667
lon: 23.392055555556
Hokke-ji (Gifu). is a Buddhist temple of the Shingon school located in Gifu, Gifu Prefecture, Japan. Though its formal name is Hokke-ji, it is more well known by its unofficial name, Mitahora Kōbō (三田洞弘法). It is located in the foothills of Mount Dodo, the largest mountain in the city of Gifu. Also, it is the fifteenth of the Mino Thirty-three Kannon. History.

Geographic entities mentioned:
surface_form: Mount Dodo
instance_of: Mountain
countries: Japan
coordinates: lat: 35.463133333333
lon: 136.80009722222
There are three main fjords that cut into the municipality: Åsskardfjorden, Hamnesfjorden, and Surnadalsfjorden. The landscape is a combination of forests, fjords, and mountains. The highest mountain peak is Snota at above sea level. Other mountains include Vassnebba, Indre Sula and Ytre Sula, Neådalssnota, and Trollhetta.

Geographic entities mentioned:
surface_form: Snota
instance_of: Mountain
countries: Norway
coordinates: lat: 62.857777777778
lon: 9.0955555555556
The landscape is a combination of forests, fjords, and mountains. The highest mountain peak is Snota at above sea level. Other mountains include Vassnebba, Indre Sula and Ytre Sula, Neådalssnota, and Trollhetta. The river Surna runs through the valley from the east to the west, and forms a large delta where it enters the fjord near Surnadalsøra and Skei.

Geographic entities mentioned:
surface_form: Vassnebba
instance_of: Mountain
countries: Norway
coordinates: lat: 62.801944444444
lon: 8.6138888888889
surface_form: Indre Sula
instance_of: Mountain
countries: Norway
coordinates: lat: 62.853888888889
lon: 8.7491666666667
surface_form: Ytre Sula
instance_of: Mountain
countries: Norway
coordinates: lat: 62.855
lon: 8.7266666666667
surface_form: Neådalssnota
instance_of: Mountain
countries: Norway
coordinates: lat: 62.777777777778
lon: 9.0819444444444
This river is rich in salmon, which attract tourists from the rest of the country and abroad. The lakes Foldsjøen and Gråsjøen lie along the border with Rindal Municipality in the east. The Grønkjølen Nature Reserve lies in the extreme northeast of the municipality. Climate.

Geographic entities mentioned:
surface_form: Foldsjøen
instance_of: Lake
countries: Norway
coordinates: lat: 62.965833333333
lon: 9.1141666666667
Mick and his brother Danny were leaders of the 1933 expedition into the Western Highlands. He also made two pioneering airplane flights into the western highlands, discovering the Wahgi Valley, taking thousands of photographs and movie film. He was one of the first Europeans to reach and climb the country's second tallest mountain – Mount Giluwe (1934).

Geographic entities mentioned:
surface_form: Mount Giluwe
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -6.0388888888889
lon: 143.88611111111
Early history. The first permanent settlements were built in the Iron Age. The Giant's Ring, a 5,000-year-old henge, is located near the city, and evidence of Bronze and Iron Age occupation has been found in the surrounding hills. For example, McArt's Fort, an Iron Age hill fort, sits atop Cavehill north of the city.

Geographic entities mentioned:
surface_form: Cavehill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.647
lon: -5.951
Essex then had MacPhelim's retainers killed and took MacPhelim, his wife and his brother into custody, sending them to Dublin where they were later executed. In 1597, during the Nine Years' War, the English garrison posted at Belfast Castle was captured and killed by Ulster rebels. The castle, village and surrounding Lagan Valley were all devastated during the rebellion. Plantation of Ulster.

Geographic entities mentioned:
surface_form: Lagan Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.535555555556
lon: -5.9788888888889
This was the final version of Belfast Castle on the original site; the building was destroyed by fire on 25 April 1708. Instead of building yet another structure at this location, a new stone mansion was constructed on Cave Hill in north Belfast in 1870 and dubbed Belfast Castle. This modern, off-site version of the castle still stands today and is a popular tourist attraction.

Geographic entities mentioned:
surface_form: Cave Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.647
lon: -5.951
A-2 (Michigan county highway). A-2 is a county-designated highway in the US state of Michigan running about along the shores of Lake Michigan in the southwestern part of the Lower Peninsula. The county highway starts near the town of Lake Michigan Beach in Berrien County at an intersection with M-63 and follows Blue Star Highway through rural coastal areas.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Route description. A-2 starts at an intersection with M-63 about west of the I-196/US 31 freeway in Lake Michigan Beach. From this intersection, the county highway runs northward through forest between Lake Michigan and the freeway in northern Berrien County. A-2 crosses into Van Buren County about a mile (1.6 km) later and continues winding north-northeasterly.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
North of here, the freeway turns to the northeast and crosses under A-2. Blue Star Highway continues due north into Douglas. In the city, the county road is bounded by businesses as it S-curves northeasterly to cross a narrow spot of Kalamazoo Lake (part of the Kalamazoo River) into Saugatuck. A-2 bypasses downtown Saugatuck to its east and continues north and northeasterly out of town.

Geographic entities mentioned:
surface_form: Kalamazoo Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.650555555556
lon: -86.206944444444
History. When auto trails were being developed in the early 20th century, the path of the modern A-2 was used for part of two. The first in 1912 was the West Michigan Pike, which ran from the Indiana state line north to the Straits of Mackinac along Lake Michigan. The second was the Western Mainline of the Dixie Highway in 1915.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
For instance, a difference of several meters was discovered when comparing the performance of LV03 and GPS technology in the measurement of the distance between the westernmost and easternmost areas of Switzerland (Geneva and Lower Engadin).

Geographic entities mentioned:
surface_form: Engadin
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.5497
lon: 9.8959
21 of these 222 Corbetts have a prominence that exceeds the P600 threshold of, which would class them as &quot;Majors&quot;. The highest Corbett, Beinn a' Chlaidheimh, at is just below the threshold for a Munro, a status it held until it was demoted in 2012 based on new surveys; it ranks as the 478th highest mountain in the British Isles, on the Simms classification.

Geographic entities mentioned:
surface_form: Beinn a' Chlaidheimh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.745922
lon: -5.259066
The highest Corbett, Beinn a' Chlaidheimh, at is just below the threshold for a Munro, a status it held until it was demoted in 2012 based on new surveys; it ranks as the 478th highest mountain in the British Isles, on the Simms classification. The Corbett with the greatest prominence is Goat Fell at, which ranks it as the 16th most prominent mountain in the British Isles.

Geographic entities mentioned:
surface_form: Goat Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.626111111111
lon: -5.1905555555556
Mount Cayley volcanic field. The Mount Cayley volcanic field (MCVF) is a remote volcanic zone on the South Coast of British Columbia, Canada, stretching from the Pemberton Icefield to the Squamish River. It forms a segment of the Garibaldi Volcanic Belt, the Canadian portion of the Cascade Volcanic Arc, which extends from Northern California to southwestern British Columbia.

Geographic entities mentioned:
surface_form: Garibaldi Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5283
lon: -126.113
The 1700 Cascadia earthquake caused near-shore subsidence, submerging marshes and forests on the coast that were later buried under more recent debris. Subglacial volcanoes. Lying in the middle of the MCVF is a subglacial volcano named Slag Hill. At least two geological units compose the edifice. Slag Hill itself consists of andesite lava flows and small amounts of pyroclastic rock.

Geographic entities mentioned:
surface_form: Slag Hill
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1834
lon: -123.3
This small subglacial volcano possibly formed between 25,000 and 10,000 years ago throughout the waning stages of the Fraser Glaciation. Cauldron Dome, a subglacial volcano north of Mount Cayley, lies west of the Powder Mountain Icefield. Like Slag Hill, it is composed of two geological units.

Geographic entities mentioned:
surface_form: Cauldron Dome
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1556
lon: -123.319
Therefore, this minor lava flow was likely extruded after Ring Mountain formed but when glacial ice covered a broader area than it does to this day, and that the lava flowed beyond the region in which glacial ice existed at that time. To the north lies Little Ring Mountain, another flow-dominated tuya lying at the northern portion of the MCVF.

Geographic entities mentioned:
surface_form: Little Ring Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.279166666667
lon: -123.31555555556
With a summit elevation of, Little Ring Mountain had its last volcanic activity between 25,000 and 10,000 years ago when the Fraser Glaciation was close to its maximum. Ember Ridge, a mountain ridge between Tricouni Peak and Mount Fee, consists of at least eight lava domes composed of andesite.

Geographic entities mentioned:
surface_form: Tricouni Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.6317
lon: -123.504
This acts like a volcanic plug and composes the lava spines that form pinnacles on Cayley's rugged summit. After Mount Cayley was constructed, the second phase of volcanism commenced million years ago. This eruptive phase was characterized by the eruption of dacite lava, tephra and breccia, which resulted in the creation of a craggy volcanic ridge known as the Vulcan's Thumb.

Geographic entities mentioned:
surface_form: Vulcan's Thumb
instance_of: Mountain
countries: Canada
coordinates: lat: 50.11
lon: -123.29
None of the rocks comprising Mount Cayley show signs of interaction with glacial ice, which contracts with several of the smaller adjacent volcanoes. Immediately southeast of Mount Cayley lies Mount Fee, an extensively eroded volcano. It contains a north–south trending ridge and is one of the older MCVF features.

Geographic entities mentioned:
surface_form: Mount Fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
This volcanic phase was also followed by a period of extensive erosion and likely one or more glacial periods, which has created the rugged north–south trending ridge that forms a prominent landmark. Pali Dome, located north and northeast of Mount Cayley, is an eroded volcano in the central MCVF. Like Cauldron Dome, it consists of two geological units.

Geographic entities mentioned:
surface_form: Pali Dome
instance_of: Mountain
countries: Canada
coordinates: lat: 50.136944444444
lon: -123.30694444444
This suggests that it was produced by an eruption after the Fraser Glaciation, which ended about 10,000 years ago. Lava flows. At least two sequences of basaltic andesite lava flows are deposited south of Tricouni Peak. One of these sequences, known as Tricouni Southwest, creates a cliff on the eastern side of a north–south trending channel with a depth of adjacent to the High Falls Creek mouth.

Geographic entities mentioned:
surface_form: Tricouni Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.6317
lon: -123.504
Lava flows. At least two sequences of basaltic andesite lava flows are deposited south of Tricouni Peak. One of these sequences, known as Tricouni Southwest, creates a cliff on the eastern side of a north–south trending channel with a depth of adjacent to the High Falls Creek mouth. The eastern flank of the lava flow, outside the High Falls Creek channel, has a more constant structure.

Geographic entities mentioned:
surface_form: High Falls Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.93298
lon: -123.31943
At least 16 geothermal sites have been identified in British Columbia, Mount Cayley being one of the six areas most capable for commercial development. Others include Meager Creek and Pebble Creek near Pemberton, Lakelse Hot Springs near Terrace, Mount Edziza on the Tahltan Highland and the Lillooet Fault Zone between Harrison Lake and the community of Lillooet.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: Harrison Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.55
lon: -121.83333333333
The rocks that make up Mount Cayley were said to have been burnt black by the Thunderbird's lightning. This mountain, like others in the area, is considered sacred because it plays an important part of their history. The Black Tusk, a pinnacle of black volcanic rock on the north shore of Garibaldi Lake to the southeast, sustains the same name.

Geographic entities mentioned:
surface_form: The Black Tusk
instance_of: Mountain
countries: Canada
coordinates: lat: 49.97527777777778
lon: -123.04277777777777
surface_form: Garibaldi Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.925
lon: -123.01
The Black Tusk, a pinnacle of black volcanic rock on the north shore of Garibaldi Lake to the southeast, sustains the same name. Cultural ceremonial use, hunting, trapping and plant gathering occur around the Mount Garibaldi area, but the most important resource was a lithic material called obsidian.

Geographic entities mentioned:
surface_form: Mount Garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Obsidian is a black volcanic glass used to make knives, chisels, adzes and other sharp tools in pre-contact times. Glassy rhyodacite was also collected from a number of minor outcrops on the flanks of Mount Fee, Mount Callaghan and Mount Cayley. This material appears in goat hunting sites and at the Elaho rockshelter, collectively dated from about 8,000 to 100 years old.

Geographic entities mentioned:
surface_form: Mount Callaghan
instance_of: Mountain
countries: Canada
coordinates: lat: 50.2278
lon: -123.266
Volcanic hazards. The MCVF is one of the largest volcanic zones in the Garibaldi Belt. Smaller zones include the Garibaldi Lake volcanic field surrounding Garibaldi Lake and the Bridge River Cones on the northern flank of the upper Bridge River. These areas are adjacent to Canada's populated southwest corner where the population of British Columbia is the greatest.

Geographic entities mentioned:
surface_form: Bridge River Cones
instance_of: Mountain
countries: Canada
coordinates: lat: 50.8
lon: -123.4
Goldney River. The Goldney River is a river in the Canterbury region of New Zealand. It arises on the southern slopes of the Craigieburn Range and flows south into Lake Coleridge. The Goldney family were early squatters in the area.

Geographic entities mentioned:
surface_form: Lake Coleridge
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.291
lon: 171.499
The &quot;uezd&quot; was located in northern part of the Baku Governorate, bordering Caspian Sea to the east, Elizavetpol Governorate to the west, Dagestan Oblast to the north, the Geokchay, Shemakha, and Baku &quot;uezds&quot; to the south. The administrative center of the &quot;uezd&quot; was the city of Kuba (present-day Quba). Geography.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
It retains many of its original internal features. Displays. The museum collection and displays reflect the growth and history of Chepstow as a trading port from medieval times and Marches town and its location within the Wye Valley, attracting many poets and painters. In 2010 the museum held an exhibition, 'The Wye Tour and its Artists', of period art from the Wye Tour.

Geographic entities mentioned:
surface_form: Wye Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69255
lon: -2.66283
Accessing the cave involves a hike from Sudagala, and an additional climb to reach the cave entrance. Approximately from the cave is another partially submerged cave, which is accessible after a swim. In Buddhism, it is believed to be the cave in which the Buddha spent the day after placing his footprint on Adam's Peak, from where he supposedly proceeded to Dighavapi.

Geographic entities mentioned:
surface_form: Adam's Peak
instance_of: Mountain
countries: Sri Lanka
coordinates: lat: 6.809444444444445
lon: 80.49972222222222
It started on 4 June in Sawahlunto and ended in the Padang on 10 June. Like previous edition, the international cyclists competed in 7 stages over 7 days, which the routes has been surveyed by Amaury Sport Organization which surveyed also Tour de France routes. Covering a distance of 854 kilometres with prize money total to IDR 1 billion. The route across Lake Singkarak on stage 2 and stage 5.

Geographic entities mentioned:
surface_form: Lake Singkarak
instance_of: Lake
countries: Indonesia
coordinates: lat: -0.6135
lon: 100.5393
Difference. Different from organization of the Tour de Singkarak in previous years which always start from the city of Padang, this year's Tour de Singkarak actually began in Sawahlunto, one of the best old city in Indonesia. While the city of Padang as the capital of West Sumatra, as a finish place Tour de Singkarak, after previously placed in Lake Singkarak.

Geographic entities mentioned:
surface_form: Lake Singkarak
instance_of: Lake
countries: Indonesia
coordinates: lat: -0.6135
lon: 100.5393
Mount Sheldon is a summit in Alaska, United States. Description. Mount Sheldon is located in the Alaska Range and in Denali National Park and Preserve. It is situated northwest of Polychrome Mountain. Precipitation runoff from the mountain drains into tributaries of the Toklat River. Topographic relief is significant as the summit rises nearly above the river in 1.7 mile (2.7 km). Climate.

Geographic entities mentioned:
surface_form: Polychrome Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 63.5424736
lon: -149.9550688
Etymology. The mountain's name was shown on a 1916 U.S. Geological Survey document and the toponym has been officially adopted by the United States Board on Geographic Names. The name honors Charles Alexander Sheldon (1867–1928), naturalist and author of &quot;The Wilderness of Denali&quot;, who studied Dall sheep and other wildlife in the Mount McKinley (Denali) area in 1906–1908.

Geographic entities mentioned:
surface_form: Denali
instance_of: Mountain
countries: United States
coordinates: lat: 63.06916666666667
lon: -151.0063888888889
The east branch of the Rocky River enters Strongsville from North Royalton and exits into Berea. Valley Parkway parallels the river's northwesterly course. This portion of the Cleveland Metroparks, named Mill Stream Run, includes Bonnie Park and Ranger Lake. Abutting the Rocky River, the recreation area offers visitors a pavilion, picnicking facilities, two small ponds, and several sport fields.

Geographic entities mentioned:
surface_form: Ranger Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.336666666667
lon: -81.825277777778
Delvenau. Delvenau (incorrectly known today as: Stecknitz) is a river in Herzogtum Lauenburg in Schleswig-Holstein, Germany. It begins in Büchen, flows to the Elbe–Lübeck Canal near its confluence with the Elbe in Lauenburg. The lower section between Bröthen and Lauenburg forms the border between Schleswig-Holstein and Mecklenburg-Vorpommern.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
New York State Route 431. New York State Route 431 (NY 431) is a state highway in Essex County, New York, United States. The highway, also known as the Whiteface Mountain Veterans Memorial Highway, begins at an intersection with NY 86 in Wilmington and climbs Whiteface Mountain in the Adirondacks. The New York State Department of Environmental Conservation maintains the highway, which is long.

Geographic entities mentioned:
surface_form: Whiteface Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.3658
lon: -73.9028
The intersection is signed, but the highway itself is unsigned except for mileposts. The highway heads to the west, ascending in elevation as it approaches Whiteface Mountain. It heads through a pass between Morgan and Esther Mountains, two smaller mountains adjacent to Whiteface Mountain, on its way to an intersection with County Route 72 (CR 72), the last highway that NY 431 intersects.

Geographic entities mentioned:
surface_form: Whiteface Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.3658
lon: -73.9028
Just west of CR 72, NY 431 passes through a toll booth and becomes a toll road. The NY 431 designation continues along the highway to the Union Falls Overlook, a scenic view in elevation about one mile (1.6 km) into the scenic drive. Th
At this point, NY 431 curves to the south, climbing up the western side of both Esther Mountain and Whiteface Mountain.

Geographic entities mentioned:
surface_form: Esther Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.387
lon: -73.8899
History. The idea of constructing a road up Whiteface Mountain was first conceived in the late 19th and early 20th centuries by Marcellus Leonard, an entrepreneur from Saranac Lake. The plans for the highway began to take shape in the 1920s when the land for the road was given by its owner to the state of New York on the condition that it would be named after America's Great War veterans.

Geographic entities mentioned:
surface_form: Whiteface Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.3658
lon: -73.9028
Bersimis-1 generating station. The Bersimis-1 generating station is a dam and a hydroelectric power station built by Hydro-Québec in conjunction with Perini, Atlas and Cartier construction companies on the Betsiamites River, in Lac-au-Brochet, north of the town of Forestville, Quebec.

Geographic entities mentioned:
surface_form: Betsiamites River
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.93333333
lon: -68.62222222
Mount Manaia. Mount Manaia is a dominant landmark approximately southeast of Whangārei city on the Whangārei Heads peninsula. Standing 420 metres, the summit offers outstanding views of the Marsden Point Oil Refinery, Bream Bay and the Hauraki Gulf to the south, Whangārei Harbour to the west and the Poor Knights Islands and Northland coast to the north.

Geographic entities mentioned:
surface_form: mount manaia
instance_of: Mountain
countries: New Zealand
coordinates: lat: -35.818309
lon: 174.516985
surface_form: manaia
instance_of: Mountain
countries: New Zealand
coordinates: lat: -35.818309
lon: 174.516985
Mt Manaia - along with Mt Lion, Bream Head and the Hen and Chicken Islands, are the scattered remnants of andesite, volcanic intrusions that erupted with force 16 to 22 million years ago during the early Miocene. They are part of a stratovolcano that extended to the Hen and Chickens.

Geographic entities mentioned:
surface_form: manaia
instance_of: Mountain
countries: New Zealand
coordinates: lat: -35.818309
lon: 174.516985
They are part of a stratovolcano that extended to the Hen and Chickens. Its jagged outline is similar to that of its neighbours and other volcanic outcrops in Northland that erupted in a similar period. Today blanketed by native bush, Manaia's jagged peaks and steep bluffs are protected within a Department of Conservation reserve which features a well-maintained 1½ hour track to the summit.

Geographic entities mentioned:
surface_form: manaia
instance_of: Mountain
countries: New Zealand
coordinates: lat: -35.818309
lon: 174.516985
In the case of some rivers such as the Columbia, the length listed in the table below is solely that of the main stem. In the case of others such as the Mackenzie, it is the combined lengths of the main stem and one or more upstream tributaries, as noted. Excluded from the list are rivers such as the Dauphin, a short connecting link between lakes Manitoba and Winnipeg, with main stems of or less.

Geographic entities mentioned:
surface_form: Manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
The lake is also an integral part of Kumaoni folklore. Nainital Lake in Nainital Town of the Nainital district, often called the Lake District of India, is one of the four important lakes of Kumaon; the other three are Sattal Lake, Bhimtal Lake and Naukuchiyatal Lake. It's the 3rd biggest lake by surface area in Uttarakhand. History. Historical records confirm that in 1839, Mr. P.

Geographic entities mentioned:
surface_form: Bhimtal Lake
instance_of: Lake
countries: India
coordinates: lat: 29.343055555556
lon: 79.559166666667
surface_form: Naukuchiyatal
instance_of: Lake
countries: India
coordinates: lat: 29.322222222222223
lon: 79.58555555555556
surface_form: nainital lake
instance_of: Lake
countries: India
coordinates: lat: 29.3875
lon: 79.4575
surface_form: sattal
instance_of: Lake
countries: India
coordinates: lat: 29.348055555555554
lon: 79.53194444444445
Nainital Lake. Naini Tal, also known as Naini Lake, is a natural freshwater body, situated amidst the town of Nainital in Kumaon, Uttarakhand, India. It is tectonic in origin and was almost circular, until frequent landslides made it crescent shaped and has an outfall at the southeastern end. Nainital, along with other lakes of Kumaon, is integral to tourism and recreation in Kumaon.

Geographic entities mentioned:
surface_form: nainital lake
instance_of: Lake
countries: India
coordinates: lat: 29.3875
lon: 79.4575
Crêt du Midi. The Crêt du Midi is a mountain of the Pennine Alps, overlooking Vercorin in the canton of Valais. The summit is accessible by cable car from Chalais or Vercorin (near Sierre).

Geographic entities mentioned:
surface_form: crêt du midi
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.22944444
lon: 7.52916667
The residential area is generally located in the south and east parts of the community. The main streets are Rideau, Prescott, Clothier and Van Buren streets. A creek named Kemptville Creek divides Kemptville in the southeast, where the least part of Kemptville is found. The creek begins southwest of Kemptville and empties NE into the Rideau River.

Geographic entities mentioned:
surface_form: Kemptville Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.055833333333
lon: -75.654166666667
Kuks. Kuks () is a municipality and village in Trutnov District in the Hradec Králové Region of the Czech Republic. It has about 300 inhabitants. It lies on the Elbe river. Its main feature is a Baroque spa building with famous sculptures by Matthias Braun. The village with the Baroque complex is protected as a monument reservation. Etymology.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
It lies on the border of three geomorphological regions: the lowlands of East Elbe Table and Orlice Table, and the undulating landscape of the Jičín Uplands. The highest point is at above sea level. The Elbe River flows through the municipality. History. Before any settlement was established here, the area was used for gold panning. The Kuks village was founded after the spa was founded here.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
History. Before any settlement was established here, the area was used for gold panning. The Kuks village was founded after the spa was founded here. In 1684, the estate was acquired by Count Franz Anton von Sporck. On the slope of the Elbe in Kuks, there used to be mineral springs. In 1692–1696, Count Sporck directed three of them at one place and built a simple spa.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
For popular Himalayan climbing routes, extensive networks of fixed ropes may be put in place to last the entire climbing season (e.g. the Khumbu Icefall on Mount Everest). While storms can strip a mountain of fixed ropes that have been left behind, the existence of old—and often unreliable and dangerous—fixed ropes along popular climbing routes, is a concern in 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
For example, on the Hillary Step of Everest, networks of fixed ropes improve client safety, but then cause bottlenecks at altitudes in the death zone. The ethics on the use of extensive fixed rope networks by commercial adventure companies facilitating access to dangerous eight-thousander summits for weaker climbers is a source of debate in mountaineering.

Geographic entities mentioned:
surface_form: Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
1948 – The Jericho Institution became part of the National Health Service and was renamed Fairfield General Hospital. Cheesden Valley and the Lost Mills by Air. The Cheesden Valley runs on a north-south alignment between Bury and Rochdale. Cheesden Brook runs through the valley, joining with Naden Brook to eventually run into the River Roch near Heywood.

Geographic entities mentioned:
surface_form: Cheesden Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.622269444444
lon: -2.2602638888889
Pre-Industrial History. There are signs of human activity dating from about 8000 BC. Flints from the Mesolithic period have been found in the Cheesden Valley and areas. All were discovered on high ground close to a water source, and all are small and suitable for use as arrowheads and similar objects. Archives+. Archives+ has created an archive in Manchester.

Geographic entities mentioned:
surface_form: Cheesden Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.622269444444
lon: -2.2602638888889
Little Skootamatta Creek. Little Skootamatta Creek is a creek in the Moira River and Lake Ontario drainage basins in Hastings and Lennox and Addington Counties in Ontario, Canada. The river's name is thought to come from Ojibwa words meaning &quot;burnt shoreline&quot;. Course.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
His father ran Bonded Messenger Service, a delivery company founded by his grandfather in 1955. Perlstein grew up in the Bayside and Fox Point neighborhoods of suburban Milwaukee, taking cross country trips with his parents and siblings to national landmarks like Mount Rushmore and Yellowstone National Park.

Geographic entities mentioned:
surface_form: Mount Rushmore
instance_of: Mountain
countries: United States
coordinates: lat: 43.878947222222
lon: -103.459825
A. F. Theriault Shipyard. A. F. Theriault & Son Ltd is a privately owned shipyard located in Meteghan River, Digby County, Nova Scotia, Canada. It was founded by Augustin Theriault in 1938. The shipyard has built a variety of marine vessels. Past projects include the Boston fireboat &quot;American United&quot;, built in 2011.

Geographic entities mentioned:
surface_form: Meteghan River
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.2169
lon: -66.1421
Lake Rhoda. Lake Rhoda is a natural lake in the town of Lakeside, Colorado, located between Interstate 70 and West 44th Avenue. Originally named &quot;West Berkeley Lake&quot;, it was renamed for Rhoda Krasner by her father, Ben Krasner, who rescued Lakeside Amusement Park from bankruptcy during the Great Depression.

Geographic entities mentioned:
surface_form: lake rhoda
instance_of: Lake
countries: United States
coordinates: lat: 39.7808
lon: -105.0582
Pseudotropheus elegans. &quot;Pseudotropheus elegans&quot; is a species of cichlid endemic to Lake Malawi. This species can reach a length of SL. It can also be found in the aquarium trade.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
The most important domestic operations in the 1960s were the North Sea storm flood in 1962 and the mining accident of Lengede in 1963. The largest disaster control action took place in August 2002 after the flooding of the Elbe river in eastern Germany. About 24,000 THW members participated in the operation, with up to 10,000 people helping simultaneously along the Elbe and its tributaries.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
In 2021, the THW provided relief during major flooding in southwestern Germany, particularly in the Ahr Valley. In February 2023, THW personnel deployed to Turkey in the aftermath of the 2023 Turkey–Syria earthquake. Organization. As a federal authority which is part of the Federal Ministry of the Interior, the THW is headed by a president and board.

Geographic entities mentioned:
surface_form: Ahr Valley
instance_of: Valley
countries: Germany
coordinates: lat: 50.53333333
lon: 7.06666667
South Ossetia covers an area of about, separated by the mountains from the more populous North Ossetia (which is a republic within Russia) and extending southwards almost to the Mtkvari river in Georgia. More than 89% of South Ossetia lies over above sea level, and its highest point is Mount Khalatsa at above sea level.

Geographic entities mentioned:
surface_form: Mount Khalatsa
instance_of: Mountain
countries: Georgia
Russia
Russian Empire
Soviet Union
coordinates: lat: 42.598888888889
lon: 43.836666666667
Linton graduated from the Winona Normal School in 1872, and went on to the University of Minnesota, from which she graduated with a Bachelor of Science in chemistry. Career in Chemistry. During her senior year of college, Linton analyzed mineral specimens from the northern shore of Lake Superior that were collected by her professors, Stephen Farnum Peckham and Christopher W. Hall.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
The layer is thick in Smooth Canyon. The stratum is fossiliferous and it has been shown to contain orthocone cephalopods and corals identified as &quot;Eofletcheria sp.&quot;. The thickness has been measured between thick in Tule Valley, Utah to thick in Desert Range Experiment Station, Utah; it is thick at Crystal Peak. It is classified as Middle Ordovician age.

Geographic entities mentioned:
surface_form: Tule Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.9569
lon: -113.376
Earth pyramids of South Tyrol. The earth pyramids in South Tyrol are a special natural phenomenon that comes about in particular terrain, usually after a landslide or an unhinging of the earth. The main cause of the formation of earth pyramids is the continuous alternation of periods of torrential rain and drought.

Geographic entities mentioned:
surface_form: earth pyramids of south tyrol
instance_of: Landform
countries: Italy
coordinates: lat: 46.8049519
lon: 12.0194615
Other noticeable cycling races that attract a large number of amateur cyclists include the in Weinfelden, the in Lenzerheide or the, which circumnavigates Lake Constance through Switzerland, Germany and Austria as well as the which circumnavigates Lake Geneva through Switzerland and France. The Marmotte Valais - organised by - features races with the highest one day height differences.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Buckley Petawabano. Buckley Petawabano (born 1950), a Cree from Mistassini reserve in northern Québec, is a First Nations actor, cinematographer, and founder of a production company. Biography. Petawabano was born in a Cree settlement near Lake Mistassini. As part of the Canadian Indian residential school system, he attended Bishop Horden Memorial School and Shingwauk Indian Residential School.

Geographic entities mentioned:
surface_form: Lake Mistassini
instance_of: Lake
countries: Canada
coordinates: lat: 51.00194444444445
lon: -73.61666666666666