Sarmila/GeoWiki-Features huggingface dataset:
Stony Cove Pike. Stony Cove Pike (alternatively known as Caudale Moor or John Bell's Banner) is a fell in the Far Eastern part of the English Lake District. It stands on the other side of the Kirkstone Pass from Red Screes, and is on the end of a ridge coming down from High Street.

Geographic entities mentioned:
surface_form: caudale moor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.481980555556
lon: -2.9013305555556
surface_form: stony cove pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.481980555556
lon: -2.9013305555556
Name. There is considerable variation over use of the alternative names for the fell. The Ordnance Survey maps name the main summit as 'Stony Cove Pike', the second top to the west as 'Caudale Moor' and 'John Bell's Banner' is reserved for the south west ridge descending to St Raven's Edge.

Geographic entities mentioned:
surface_form: caudale moor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.481980555556
lon: -2.9013305555556
surface_form: stony cove pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.481980555556
lon: -2.9013305555556
Alfred Wainwright in his &quot;Pictorial Guide to the Lakeland Fells&quot; uses Caudale Moor for the fell as a whole, John Bell's Banner as an alternative to this and Stony Cove Pike as a name for the (main) summit. Bill Birkett prefers the Ordnance Survey scheme, but with John Bell's Banner as a second name for the subsidiary top. Topography.

Geographic entities mentioned:
surface_form: caudale moor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.481980555556
lon: -2.9013305555556
surface_form: stony cove pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.481980555556
lon: -2.9013305555556
The extensive Caudale Quarry is hollowed out about halfway down the edge, reached by what was once believed to be the steepest working track in Lakeland. There is also evidence of deeper mining here. A broad ridge also descends south from the Caudale Moor top. This passes over Pike How before dividing around the head of Woundale.

Geographic entities mentioned:
surface_form: caudale moor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.481980555556
lon: -2.9013305555556
Summit. The summit area is grassy, with a number of small tarns between the two tops. Walls follow the ridges to Hartsop Dodd, St Raven's Edge and Threshthwaite Mouth, making navigation of the complex ridge system easier. Both tops have cairns and there is a further cairn topped by a wooden cross to the south west of Caudale Moor. This is named Mark Atkinson's monument by Wainwright.

Geographic entities mentioned:
surface_form: caudale moor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.481980555556
lon: -2.9013305555556
Stony Cove Pike. Stony Cove Pike (alternatively known as Caudale Moor or John Bell's Banner) is a fell in the Far Eastern part of the English Lake District. It stands on the other side of the Kirkstone Pass from Red Screes, and is on the end of a ridge coming down from High Street.

Geographic entities mentioned:
surface_form: stony cove pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.481980555556
lon: -2.9013305555556
Geography. The Scott Glacier originates on the Antarctic Plateau in the vicinity of D'Angelo Bluff and Mount Howe, and descends between the Nilsen Plateau and the mountains of the Watson Escarpment to enter Ross Ice Shelf just west of the Tapley Mountains.

Geographic entities mentioned:
surface_form: Antarctic Plateau
instance_of: Plateau
coordinates: lat: -90
lon: 0
surface_form: Mount Howe
instance_of: Mountain
coordinates: lat: -87.3667
lon: -149.5
surface_form: Nilsen Plateau
instance_of: Plateau
coordinates: lat: -86.3333
lon: -158
surface_form: Watson Escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
The Tapley Mountains, Watson Escarpment, Mount Blackburn, and the La Gorce Mountains bound the Scott Glacier on its eastern margin, while the Karo Hills, Hays Mountains, Faulkner Escarpment, and Rawson Mountains define the western edge of the Scott's drainage.

Geographic entities mentioned:
surface_form: Watson Escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
The Will Hays Mountains (85°57' S., 155°20' W.) also in the Queen Maud Range, surmount the divide between the lower ends of these two glaciers. Mount Thorne rises to 6,000 feet in the Will Hays Mountains. Mount Weaver (86°57' S, 152°20' W.), about 10,000 feet high, marks the southern portal of the glacier at the polar plateau.

Geographic entities mentioned:
surface_form: Mount Thorne
instance_of: Mountain
coordinates: lat: -85.6833
lon: -158.667
Mount Thorne rises to 6,000 feet in the Will Hays Mountains. Mount Weaver (86°57' S, 152°20' W.), about 10,000 feet high, marks the southern portal of the glacier at the polar plateau. Blackburn in 1934, found at Mount Weaver extensive
coal beds and fossil tree section up to 18 inches in diameter.

Geographic entities mentioned:
surface_form: Mount Weaver
instance_of: Mountain
coordinates: lat: -86.966666666667
lon: -153.83333333333
Course. The Scott Glacier forms on the Polar Plateau and flows north between Mount Wilbur and the Davis Hills. The Poulter Glacier enters from the left (west) to the north of Mount Innes-Taylor. The Klein Glacier enters from the right (east) to the north of the David Hills.

Geographic entities mentioned:
surface_form: Mount Innes-Taylor
instance_of: Mountain
coordinates: lat: -86.85
lon: -154.45
The Klein Glacier enters from the right (east) to the north of the David Hills. The Robison Glacier enters from the right to the south of Mount Bowlin and the VanReeth Glacier enters from the right to the north of Mount Bowlin. The Scott Glacier flows past the Watson Escarpment to the east, from which the Howe Glacier and Griffith Glacier join it from the right.

Geographic entities mentioned:
surface_form: Mount Bowlin
instance_of: Mountain
coordinates: lat: -86.4667
lon: -147.3
The Robison Glacier enters from the right to the south of Mount Bowlin and the VanReeth Glacier enters from the right to the north of Mount Bowlin. The Scott Glacier flows past the Watson Escarpment to the east, from which the Howe Glacier and Griffith Glacier join it from the right. To the north of Mount Ruth, to the west of the Scott Glacier, the Bartlett Glacier joins from the left.

Geographic entities mentioned:
surface_form: Watson Escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
The Scott Glacier flows past the Watson Escarpment to the east, from which the Howe Glacier and Griffith Glacier join it from the right. To the north of Mount Ruth, to the west of the Scott Glacier, the Bartlett Glacier joins from the left. Tributaries of the Bartlett Glacier include the Holdsworth Glacier and the Souchez Glacier.

Geographic entities mentioned:
surface_form: Mount Ruth
instance_of: Mountain
coordinates: lat: -86.3
lon: -151.75
Further north, the Scott Glacier flows past the Tapley Mountains to the east, from which it receives the Albanus Glacier and the Roe Glacier. From the Queen Maud Mountains to the west it receives the Vaughan Glacier. The Koerwitz Glacier flows beside the Scott Glacier then pulls away at Mount Salisbury in the Karo Hills. Head.

Geographic entities mentioned:
surface_form: Mount Salisbury
instance_of: Mountain
countries: United States
coordinates: lat: 58.8508
lon: -137.372
Neal E. Early, USA, a member of the aviation unit that supported the USGS Topo East survey of this area, 1962-63. Sunny Ridge. A partly snow-free ridge that trends southward for from the western extremity of Mount Weaver. It stands at the west side of and near the head of Scott Glacier. The ridge was scaled by the Ohio State University geological party in November 1962.

Geographic entities mentioned:
surface_form: Mount Weaver
instance_of: Mountain
coordinates: lat: -86.966666666667
lon: -153.83333333333
Poulter, second in command of the expedition. Bartlett Glacier. A tributary glacier, about long and wide at its terminus. It flows northeast from Nilsen Plateau and joins Scott Glacier close north of Mount Gardiner. Discovered in December 1934 by the ByrdAE geological party under Quin Blackburn, and named by Byrd for Capt. Robert A.

Geographic entities mentioned:
surface_form: Nilsen Plateau
instance_of: Plateau
coordinates: lat: -86.3333
lon: -158
Not: Bob Bartlett Glacier. Holdsworth Glacier. A tributary glacier about long, flowing northeast from Fuller Dome to enter the southeast side of Bartlett Glacier. Named by US-ACAN for Gerald Holdsworth, involved in geological studies at McMurdo Station, summer of 1965-66. Souchez Glacier.

Geographic entities mentioned:
surface_form: Fuller Dome
instance_of: Mountain
coordinates: lat: -86.6333
lon: -156.3
Named by US-ACAN for Gerald Holdsworth, involved in geological studies at McMurdo Station, summer of 1965-66. Souchez Glacier. A tributary glacier about long, flowing from Mount Crockett south along the east side of Faulkner Escarpment and then turning southeast to parallel the southwest side of Hays Mountains. It joins Bartlett Glacier just south of Mount Dietz. Named by US-ACAN for Roland A.

Geographic entities mentioned:
surface_form: Mount Crockett
instance_of: Mountain
coordinates: lat: -86.0167
lon: -155.067
Souchez Glacier. A tributary glacier about long, flowing from Mount Crockett south along the east side of Faulkner Escarpment and then turning southeast to parallel the southwest side of Hays Mountains. It joins Bartlett Glacier just south of Mount Dietz. Named by US-ACAN for Roland A. Souchez, involved in geological studies at McMurdo Station during the season of 1965-66. Vaughan Glacier.

Geographic entities mentioned:
surface_form: Mount Dietz
instance_of: Mountain
coordinates: lat: -86.2667
lon: -153.167
Named by US-ACAN for Roland A. Souchez, involved in geological studies at McMurdo Station during the season of 1965-66. Vaughan Glacier. A tributary glacier, long, draining eastward from Mount Vaughan to enter Scott Glacier just south of Taylor Ridge, in the Hays Mountains. Mapped by USGS from surveys and USN air photos, 1960-64. Named by US-ACAN in association with Mount Vaughan.

Geographic entities mentioned:
surface_form: Mount Vaughan
instance_of: Mountain
coordinates: lat: -85.916666666667
lon: -155.83333333333
Mapped by USGS from surveys and USN air photos, 1960-64. Named by US-ACAN in association with Mount Vaughan. Koerwitz Glacier. A low gradient glacier flowing northeast from Mount Griffith in the Hays Mountains to the Karo Hills. First seen and roughly mapped by the ByrdAE, 1928-30. Named by US-ACAN for Peter H. Koerwitz, biolab manager at McMurdo Station in 1965. Klein Glacier.

Geographic entities mentioned:
surface_form: Mount Griffith
instance_of: Mountain
coordinates: lat: -85.8833
lon: -155.5
Named by US-ACAN for Lt. Cdr. Layton E. Robison, pilot with USN Squadron VX-6 during Operation Deep Freeze 1964, 1965 and 1966. Van Reeth Glacier. A tributary glacier about long, draining westward to Scott Glacier between Mount Blackburn and Mount Bowlin. Discovered in December 1934 by the ByrdAE geological party under Quin Blackburn. Named by US-ACAN for Cdr. Eugene W.

Geographic entities mentioned:
surface_form: Mount Blackburn
instance_of: Mountain
countries: United States
coordinates: lat: 61.73190833333334
lon: -143.43929722222222
surface_form: Mount Bowlin
instance_of: Mountain
coordinates: lat: -86.4667
lon: -147.3
Named by US-ACAN for Robert C. Howe of USN Squadron VX-6, photographer on Operation Deep Freeze 1966 and 1967. Griffith Glacier. A tributary glacier draining westward from the California Plateau and Watson Escarpment to enter Scott Glacier between Mount McKercher and Mount Meeks. Mapped by USGS from surveys and USN air photos, 1960-63. Named by US-ACAN for Lt. Cdr. Philip G.

Geographic entities mentioned:
surface_form: California Plateau
instance_of: Plateau
coordinates: lat: -86.0667
lon: -145.167
surface_form: Watson Escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
surface_form: Mount McKercher
instance_of: Mountain
coordinates: lat: -86.15
lon: -150.033
surface_form: Mount Meeks
instance_of: Mountain
coordinates: lat: -86.2167
lon: -148.85
Sanctuary Glacier. A glacier almost completely encircled by the Gothic Mountains. It drains west between Outlook Peak and Organ Pipe Peaks into Scott Glacier. Mapped by USGS from surveys and USN aerial photographs, 1960-64. The descriptive name was proposed by Edmund Stump, leader of a USARP-Arizona State University geological party which established a base camp on the glacier in January 1981.

Geographic entities mentioned:
surface_form: Outlook Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 79.74
lon: -91.4
surface_form: Organ Pipe Peaks
instance_of: Mountain
coordinates: lat: -86.05
lon: -150
Albanus Glacier. A glacier, long, flowing west along the south side of Tapley Mountains to enter Scott Glacier just north of Mount Zanuck. Discovered in December 1934 by the ByrdAE geological party under Quin Blackburn, and named by Byrd for Albanus Phillips, Jr., manufacturer of Cambridge, MD, a patron of the ByrdAE of 1928-30 and 1933-35. Not: Phillips Glacier. Roe Glacier.

Geographic entities mentioned:
surface_form: Mount Zanuck
instance_of: Mountain
coordinates: lat: -85.96667
lon: -151.16667
Not: Phillips Glacier. Roe Glacier. A tributary glacier, long, flowing northwest through the Tapley Mountains to enter Scott Glacier just south of Mount Durham. Mapped by USGS from surveys and USN air photos, 1960-64. Named by US-ACAN for Derrell M. Roe, a member of summer parties at McMurdo Station in 1963-64 and 1964–65 and station engineer with the McMurdo winter party in 1966.

Geographic entities mentioned:
surface_form: Mount Durham
instance_of: Mountain
coordinates: lat: -85.55
lon: -151.2
Tacoma is the economic and cultural center of the South Sound region, which has a population of about 1 million. Tacoma adopted its name after the nearby Mount Rainier, called in the Puget Sound Salish dialect, and &quot;Takhoma&quot; in an anglicized version.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
In 1924, Tacoma's first movie studio, H. C. Weaver Studio, was sited at present-day Titlow Beach. At the time, it was the third-largest freestanding film production space in America, with the two larger facilities being located in Hollywood.

Geographic entities mentioned:
surface_form: Titlow Beach
instance_of: Landform
countries: United States
coordinates: lat: 47.247
lon: -122.553
There are several beaches along Ruston Way with public access, some of which are also popular for scuba diving. Another large park in Tacoma is Wapato Park, which has a lake and walking trails that circle the lake. Wapato is in Tacoma's south end, at Sheridan and 72nd St. Titlow Beach, at the end of 6th Avenue, is also a scuba diving area.

Geographic entities mentioned:
surface_form: Titlow Beach
instance_of: Landform
countries: United States
coordinates: lat: 47.247
lon: -122.553
The city of Tacoma contributed $100,000 to the airport's construction, in return for it being constructed at Bow Lake. The other proposed location near Lake Sammamish is much further from Tacoma, while Bow Lake is halfway between Seattle and Tacoma. A seaplane service with tours of the Tacoma area is operated by Kenmore Air from a dock near Old Town.

Geographic entities mentioned:
surface_form: Lake Sammamish
instance_of: Lake
countries: United States
coordinates: lat: 47.61638888888889
lon: -122.08944444444444
The smaller of the two, the North Alouette flows from Jacobs Lake south to its confluence with the South Alouette. The river flows over a minor set of falls about halfway from its mouth. The South Alouette originates on the slopes of Mount Robie Reid and flows into Alouette Lake. After exiting the lake the river flows west before converging with the North Alouette.

Geographic entities mentioned:
surface_form: Mount Robie Reid
instance_of: Mountain
countries: Canada
coordinates: lat: 49.431944444444
lon: -122.35611111111
surface_form: Alouette Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.3333
lon: -122.417
Zhiyan Reservoir. Zhiyan Reservoir () is a reservoir located in the town of Huangdian, Lanxi, Zhejiang, China. It covers a total surface area of and has a storage capacity of some of water. It belongs to the first grade water source protection area () and is part of Lanxi's water supply network. It is adjacent to the city of Jiande. History.

Geographic entities mentioned:
surface_form: zhiyan reservoir
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 29.388503
lon: 119.372593
It covers a total surface area of and has a storage capacity of some of water. It belongs to the first grade water source protection area () and is part of Lanxi's water supply network. It is adjacent to the city of Jiande. History. Zhiyan Reservoir was built in April 1974 for irrigation, flood control, electricity generation and drinking water purposes.

Geographic entities mentioned:
surface_form: zhiyan reservoir
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 29.388503
lon: 119.372593
The cemetery consists of 20 tombs dug out of stone, called sepulchers. There are also five stelas, acting as gravestones. Every object within the cemetery is carved from sandstone quarried in the Oiz Mountains. The individuals buried in these graves were likely from the upper class, as lower-class Pyrenean communities typically used simple open-earth burials. The sepulchers consist of two pieces.

Geographic entities mentioned:
surface_form: Oiz Mountains
instance_of: Mountain
countries: Spain
coordinates: lat: 43.228669444444
lon: -2.5900361111111
Christopher C. Burt, a weather historian writing for Weather Underground, believes that the 1913 Death Valley reading is &quot;a myth&quot;, and is at least too high. Burt proposes that the highest reliably recorded temperature on Earth could still be at Death Valley, but is instead recorded on 30 June 2013.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
The only open marine environment where modern stromatolites are known to prosper is the Exuma Cays in the Bahamas. Freshwater locations. Laguna de Bacalar in Mexico's southern Yucatán Peninsula has an extensive formation of living giant microbialites (that is, stromatolites or thrombolites). The microbialite bed is over long with a vertical rise of several meters in some areas.

Geographic entities mentioned:
surface_form: Laguna de Bacalar
instance_of: Lake
countries: Mexico
coordinates: lat: 18.75
lon: -88.315
Large microbialite towers up to 40 m high were discovered in the largest soda lake on Earth, Lake Van in eastern Turkey. They are composed of aragonite and grow by precipitation of calcite from sub-lacustrine karst-water. Freshwater stromatolites are found in Lake Salda in southern Turkey. The waters are rich in magnesium and the stromatolite structures are made of hydromagnesite.

Geographic entities mentioned:
surface_form: Lake Salda
instance_of: Lake
countries: Turkey
coordinates: lat: 37.5508
lon: 29.6833
They are composed of aragonite and grow by precipitation of calcite from sub-lacustrine karst-water. Freshwater stromatolites are found in Lake Salda in southern Turkey. The waters are rich in magnesium and the stromatolite structures are made of hydromagnesite. Two instances of freshwater stromatolites are found in Canada, at Pavilion Lake and Kelly Lake in British Columbia.

Geographic entities mentioned:
surface_form: Pavilion Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.8668
lon: -121.742
From then on, Savoy experienced a revival following the economic crisis of 1860-1890, which also contributed to a slowdown in mountain migration. This period saw the development of aluminum production by hot electrolysis in La Praz in the Arc Valley, the creation of special steels in Ugine in the Val d'Arly, and the extraction of cheddite in Chedde-Passy in the Haut-Faucigny.

Geographic entities mentioned:
surface_form: Arc Valley
instance_of: Valley
countries: France
coordinates: lat: 45.2
lon: 6.6666666666667
However, it becomes clear that there was not a single Savoyard identity immediately after the Annexation, but rather multiple identities corresponding more or less to one of the six historical provinces—, Maurienne, Tarentaise, Chablais, Genevois, and Faucigny—and, most importantly, to the commune, highlighting a local spirit.

Geographic entities mentioned:
surface_form: Maurienne
instance_of: Valley
countries: France
coordinates: lat: 45.2
lon: 6.6666666666667
Additionally, selected verses from the poem including the refrain were set to Byzantine musical notation by the Simonopetra Monastery of Mount Athos in Greece. The result was the hymn &quot;Virgin Pure&quot; in Byzantine Greek. The monastery published the work in a book titled Ψαλτήριον Τερπνὸν (&quot;Psaltirion Terpnon&quot;, &quot;The Pleasant Psaltery&quot;). Contemporary practice.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Nevelfjell. Nevelfjell is a mountain in Lillehammer Municipality in Innlandet county, Norway. The tall mountain is the highest point in the municipality. The mountain sits about northeast of the town of Lillehammer, about to the south of the municipal border with Øyer Municipality. Nevelfjell is a popular destination in the Lillehammer area both in winter and in summer.

Geographic entities mentioned:
surface_form: nevelfjell
instance_of: Mountain
countries: Norway
coordinates: lat: 61.2
lon: 10.58333333
The mountain sits about northeast of the town of Lillehammer, about to the south of the municipal border with Øyer Municipality. Nevelfjell is a popular destination in the Lillehammer area both in winter and in summer. On clear days there is a good panoramic view of a wide area, including peaks in the Jotunheimen and Rondane mountain ranges.

Geographic entities mentioned:
surface_form: nevelfjell
instance_of: Mountain
countries: Norway
coordinates: lat: 61.2
lon: 10.58333333
Nevelfjell is a popular destination in the Lillehammer area both in winter and in summer. On clear days there is a good panoramic view of a wide area, including peaks in the Jotunheimen and Rondane mountain ranges. There are hiking and ski trails to the top of Nevelfjell and a small hiking cabin named &quot;Nevelhytta&quot;.

Geographic entities mentioned:
surface_form: nevelfjell
instance_of: Mountain
countries: Norway
coordinates: lat: 61.2
lon: 10.58333333
He named it 'Parthenope', in honor of his onetime principality in Naples, Italy, which had been founded on the site of the ancient Greek colony of Parthenope (see History of Naples). Murat's Parthenope was located about south of St. Augustine, on the west side of the Matanzas River, at the mouth of Moses Creek.

Geographic entities mentioned:
surface_form: Matanzas River
instance_of: Landform
countries: United States
coordinates: lat: 29.9138577
lon: -81.2836827
Monte Caçador and Pico Forcado Protected Countryside. Monte Caçador and Pico Forcado Protected Countryside (Portuguese: &quot;Paisagem protegido de Monte Caçador e Pico Forcado&quot;) is a protected area covering of land in the eastern part of the island of Boa Vista in Cape Verde. It is the most important mountain formation on the island, but not the highest.

Geographic entities mentioned:
surface_form: monte caçador and pico forcado protected countryside
instance_of: Mountain
countries: Cape Verde
coordinates: lat: 16.11666667
lon: -22.76666667
Now immune to the sun and able to use Hamon, Kars's only desire is to kill Joseph. Joseph steals a Nazi plane and tries to crash it and Kars into the volcanic island of Vulcano. Joseph and Kars escape, but the shock of the plane crash causes a volcanic eruption.

Geographic entities mentioned:
surface_form: Vulcano
instance_of: Mountain
countries: Italy
coordinates: lat: 38.4042
lon: 14.9658
Quebrada Mamilla. tc8z6ao4p09nh0gauergmmbuio86v" xml:space="preserve">Quebrada Mamilla is a ravine in northern Chile's Antofagasta Region. The ravine is accessed from the Chile Route 1 that unites coastal cities of Iquique and Tocopilla. It is located about 10 km north of Tocopilla. Fourteen archaeological sites have been identified in Quebrada Mamilla.

Geographic entities mentioned:
surface_form: quebrada mamilla
instance_of: Watercourse
countries: Chile
coordinates: lat: -21.970833333333
lon: -70.179444444444
The ravine is accessed from the Chile Route 1 that unites coastal cities of Iquique and Tocopilla. It is located about 10 km north of Tocopilla. Fourteen archaeological sites have been identified in Quebrada Mamilla. It is thought to have an etymology based on &quot;milla&quot;, the Mapuche word for gold.

Geographic entities mentioned:
surface_form: quebrada mamilla
instance_of: Watercourse
countries: Chile
coordinates: lat: -21.970833333333
lon: -70.179444444444
Thomas and Bonner competed at the 1988 Summer Olympics in the coxless pair and came eighths. At the 1989 World Rowing Championships at Lake Bled near Bled in SR Slovenia, Yugoslavia, she teamed up with Catherine Miller in the women's pair and they came in eleventh (and last) place.

Geographic entities mentioned:
surface_form: Lake Bled
instance_of: Lake
countries: Slovenia
coordinates: lat: 46.364444444444
lon: 14.094722222222
Lievestuore. Lievestuore is an urban area (&quot;taajama&quot;) in Laukaa, Finland, located in the southeastern part of the municipality on the southern shore of lake Lievestuoreenjärvi. It is the third largest urban area and the most industrialized area in Laukaa. The Finnish national road 9 passes through Lievestuore and connects it to Jyväskylä, the distance between the two being.

Geographic entities mentioned:
surface_form: Lievestuoreenjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 62.31666667
lon: 26.15
Igala people. The Igala or Igara people are a West African ethnolinguistic group native to the region immediately south of the confluence of the Niger and Benue Rivers in central Nigeria.

Geographic entities mentioned:
surface_form: Benue
instance_of: Watercourse
countries: Cameroon
Nigeria
coordinates: lat: 7.783333
lon: 6.766667
Today, people of Igala descent are estimated to be at a population of over 2 million people. The Igala kingdom is ruled ceremonially and culturally by the Attah and has a long history of political warfare and campaigns with neighbouring groups along the Benue. Igala people traditionally worship the supreme being &quot;Ojo&quot;, as well as their divine ancestral spirits.

Geographic entities mentioned:
surface_form: Benue
instance_of: Watercourse
countries: Cameroon
Nigeria
coordinates: lat: 7.783333
lon: 6.766667
Location. The Igala Kingdom expanded vastly beyond the present-day boundary. Their homeland, the former Igala Kingdom, is a triangular area of about in the angle formed by the Benue and Niger rivers. The area was formerly known as the Igala Division of Kabba province and is now part of Kogi State. Its capital was Idah, in Kogi state.

Geographic entities mentioned:
surface_form: Benue
instance_of: Watercourse
countries: Cameroon
Nigeria
coordinates: lat: 7.783333
lon: 6.766667
On October 20 Tsarskoye Selo fell into the hands of the White troops, who were now at the gates of Petrograd. They captured the Pulkovo Heights, the left flank of the Army entered Ligovo and advanced units engaged the enemy in skirmishes as far as the Ijorski factories.

Geographic entities mentioned:
surface_form: Pulkovo Heights
instance_of: Landform
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 59.771811
lon: 30.326047
For example, it was also suggested to divert the soldiers to the large Russian villages on the lake Peipus (Chudskoye) since &quot;...should Typhus spread there, it will not be that painful to see the number of Russians there to diminish&quot;. According to the accounts of an officer Kuzmin, his Talabsky regiment was disarmed and then pushed back into Narova river where it was shot by the Reds.

Geographic entities mentioned:
surface_form: Peipus
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
Butternut Lake (Meeker County, Minnesota). Butternut Lake is a lake in Meeker County, in the U.S. state of Minnesota. Butternut Lake was named for the butternut trees near the lake.

Geographic entities mentioned:
surface_form: butternut lake
instance_of: Lake
countries: United States
coordinates: lat: 45.05944444
lon: -94.30638889
These were all gathered in their current location in the Bella Coola Valley (Nuxalk) by a combination of negotiation with Chief Pootlass and through government pressure, settling together based on cultural and linguistic similarities, reinforced by a large number of marriages arranged to ease the transition.

Geographic entities mentioned:
surface_form: Bella Coola Valley
instance_of: Valley
countries: Canada
For centuries, Nepal remained in self-imposed isolation. After the 1860 treaty with the East India Company, Prime Minister Jung Bahadur Rana of Nepal allowed Indians to purchase and sell land in Nepal's Terai. After the ascent of Mt. Everest by Edmund Hillary and Tenzing Norgay, Nepal completely lifted its ban on foreigners.

Geographic entities mentioned:
surface_form: Mt. Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Flagtail Mountain. Flagtail Mountain is a summit in Grant County, Oregon, in the United States with an elevation of. History. The first Flagtail Mountain Lookout, a fire lookout tower, was constructed on the mountain in the 1920s. Additional structures were built in 1933 and 1960, and in 2003, it was added to the National Historic Lookout Register.

Geographic entities mentioned:
surface_form: flagtail mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.1862604
lon: -119.2813486
Under his leadership, this formidable fortress, alongside other Baramahal forts, played a pivotal role in securing the region from invading armies, earning it the title 'Gateway of Tamil Nadu' and leaving an enduring imprint on the historical legacy of the Vijayanagara Empire. In the 1670s, the charismatic Maratha leader Shivaji I captured the Krishnagiri Fort during his Deccan expedition.

Geographic entities mentioned:
surface_form: deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
surface_form: krishnagiri fort
instance_of: Mountain
countries: India
coordinates: lat: 12.537721
lon: 78.214638
Krishnagiri Fort. Krishnagiri Fort, situated in the Krishnagiri district of Tamil Nadu, India, is a formidable historical stronghold that has witnessed the ebb and flow of various dynasties and colonial powers. This fortification, now preserved as a national monument under the auspices of the Archaeological Survey of India, holds a rich history dating back centuries. History.

Geographic entities mentioned:
surface_form: krishnagiri fort
instance_of: Mountain
countries: India
coordinates: lat: 12.537721
lon: 78.214638
History. The fort and its surroundings were commonly referred to as &quot;Baramahal,&quot; a term that linguistically translates to &quot;twelve forts.&quot; This nomenclature reflects the presence of twelve hilltop forts in the region, including Krishnagiri Fort. This majestic fort was built under the aegis of the Vijayanagara Empire.

Geographic entities mentioned:
surface_form: krishnagiri fort
instance_of: Mountain
countries: India
coordinates: lat: 12.537721
lon: 78.214638
Subsequently, Hyder Ali reclaimed control of the fort, culminating in the Treaty of Madras. In 1792 AD, following Tipu Sultan's defeat in the Third Anglo-Mysore War at the hands of the Presidency armies and the subsequent signing of the Treaty of Srirangapatna, the East India Company assumed control of Krishnagiri Fort.

Geographic entities mentioned:
surface_form: krishnagiri fort
instance_of: Mountain
countries: India
coordinates: lat: 12.537721
lon: 78.214638
Captain Alexander Reed was appointed as the first District Collector of the region under the Company's administration. The British strategically maintained Krishnagiri Fort as an arsenal, employing it as a pivotal defense structure to safeguard the region.

Geographic entities mentioned:
surface_form: krishnagiri fort
instance_of: Mountain
countries: India
coordinates: lat: 12.537721
lon: 78.214638
By 1900s, with the British rule firmly established in the region and no imminent threats, the fort fell into disuse. Finally, in the aftermath of India's independence in 1947 AD, Krishnagiri Fort came under the jurisdiction of the Indian government.

Geographic entities mentioned:
surface_form: krishnagiri fort
instance_of: Mountain
countries: India
coordinates: lat: 12.537721
lon: 78.214638
His paintings have also been exhibited at SUNY New Paltz. During his career, Fuechsel painted various landscapes of New York including the Hudson Valley, Lake George, the Adirondacks, and Kaaterskill Falls; but also the Rocky Mountains. Fuechsel died at the Isabella Heimath in New York City on September 30, 1915.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Truc y Flou. Truc y Flou is a card game originally from Aragon in Spain, which is nowadays played in the French Pyrenees in the Aure and Louron valleys in Hautes-Pyrénées and the Oueil valley near Luchonnais. It is part of the Put family and may be compared to the games of Aluette, Brisca and Mus.

Geographic entities mentioned:
surface_form: Aure
instance_of: Valley
countries: France
coordinates: lat: 42.83
lon: 0.33
Other high-profile property investments by to Reid and his companies include the Meridian Mall, Dunedin, Elliott Stables in Auckland, and Plasma House on Queenstown Hill, which was purchased from American billionaire Peter Thiel for $6.85 million in 2022.

Geographic entities mentioned:
surface_form: Queenstown Hill
instance_of: Mountain
countries: New Zealand
coordinates: lat: -45.0083
lon: 168.693
Etymology and definitions. The Nama assemblage is named after the Nama Group from the Tsaus Mountains of Namibia, which preserves a Late Ediacaran record of soft-bodied fossils. The biota of the Namibian sites clusters with similar biotas found in the Southwestern United States, South China and British Columbia, leading to a Nama assemblage being first defined by Gehling in 2001.

Geographic entities mentioned:
surface_form: Tsaus Mountains
instance_of: Mountain
countries: Namibia
coordinates: lat: -27.1267
lon: 16.2
Lake Waipu. Lake Waipu, just south of Rātana Pā, is a shallow coastal aeolian, or dune-dammed, lake. Horizons Regional Council has monitored water quality in the lake since 2015. The lake's catchment is mainly pasture and Rātana's treated sewage runs into a tributary of the lake, accounting for the trophic level index being eutrophic at 6.9.

Geographic entities mentioned:
surface_form: lake waipu
instance_of: Lake
countries: New Zealand
coordinates: lat: -40.044444
lon: 175.155556
Planting and other improvements it is planned to improve the lake's pollution. Lake Waipu usually drains through the sand, as does nearby Lake Oraekomiko, though in places, especially in wet weather, a stream runs to the Turakina River.

Geographic entities mentioned:
surface_form: lake waipu
instance_of: Lake
countries: New Zealand
coordinates: lat: -40.044444
lon: 175.155556
Guadaíra. The Guadaíra is a river that runs through the province of Seville, in Andalusia, southern Spain. Its name contains the same &quot;guad&quot; root as the much larger Río Guadalquivir, coming from the Arabic word &quot;wadi&quot; (), meaning &quot;river valley&quot;. The river runs through the town of Alcalá de Guadaíra in the Seville's metropolitan area.

Geographic entities mentioned:
surface_form: guadaíra
instance_of: Watercourse
countries: Spain
coordinates: lat: 37.173791666667
lon: -6.1023888888889
Cockscomb (Tuolumne Meadows). Cockscomb is a mountain, in the area of Tuolumne Meadows, Yosemite National Park, California. On Cockscomb's particulars. Cockscomb is aptly named, notably when viewed from the northwest. It is located in the Yosemite Wilderness, and is often forgotten, due to its proximity to Cathedral Peak, Matthes Crest, and Echo Peaks, but is deserves to be climbed.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: cockscomb
instance_of: Mountain
countries: United States
coordinates: lat: 37.83548
lon: -119.3846
On Cockscomb's particulars. Cockscomb is aptly named, notably when viewed from the northwest. It is located in the Yosemite Wilderness, and is often forgotten, due to its proximity to Cathedral Peak, Matthes Crest, and Echo Peaks, but is deserves to be climbed. The proximity of Cockscomb. Cockscomb is near Echo Peaks, Unicorn Peak, Cathedral Peak, Matthes Crest, Budd Lake, also Elizabeth Lake.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: cathedral peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.8689
lon: -113.866
surface_form: cathedral peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.8477
lon: -119.405
surface_form: cathedral peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0344
lon: -106.859
surface_form: cathedral peak
instance_of: Mountain
countries: United States
coordinates: lat: 42.8253
lon: -109.179
surface_form: cathedral peak
instance_of: Mountain
countries: United States
coordinates: lat: 58.6125
lon: -134.3664
surface_form: cathedral peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.98926
lon: -120.188954
surface_form: echo peaks
instance_of: Mountain
countries: United States
coordinates: lat: 37.83243
lon: -119.40294
It is located in the Yosemite Wilderness, and is often forgotten, due to its proximity to Cathedral Peak, Matthes Crest, and Echo Peaks, but is deserves to be climbed. The proximity of Cockscomb. Cockscomb is near Echo Peaks, Unicorn Peak, Cathedral Peak, Matthes Crest, Budd Lake, also Elizabeth Lake. Rock climbing on Cockscomb. None of Cockscomb's routes walk-ups, the easiest a Class 4.

Geographic entities mentioned:
surface_form: budd lake
instance_of: Lake
countries: United States
coordinates: lat: 44.0228
lon: -84.7967
surface_form: cathedral peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.8689
lon: -113.866
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 34.6658
lon: -118.403
surface_form: budd lake
instance_of: Lake
countries: United States
coordinates: lat: 37.8417
lon: -119.396
surface_form: unicorn peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.745
lon: -121.7
surface_form: cathedral peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.8477
lon: -119.405
surface_form: cathedral peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0344
lon: -106.859
surface_form: cathedral peak
instance_of: Mountain
countries: United States
coordinates: lat: 42.8253
lon: -109.179
surface_form: budd lake
instance_of: Lake
countries: United States
coordinates: lat: 43.64
lon: -94.46666667
surface_form: cathedral peak
instance_of: Mountain
countries: United States
coordinates: lat: 58.6125
lon: -134.3664
surface_form: cockscomb
instance_of: Mountain
countries: United States
coordinates: lat: 37.83548
lon: -119.3846
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 42.630489
lon: -83.380641
surface_form: cathedral peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.98926
lon: -120.188954
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 48.886
lon: -113.726
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 42.50822
lon: -88.26902
surface_form: budd lake
instance_of: Lake
countries: United States
coordinates: lat: 47.16666667
lon: -95.175
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 37.845012
lon: -119.370406
surface_form: echo peaks
instance_of: Mountain
countries: United States
coordinates: lat: 37.83243
lon: -119.40294
surface_form: unicorn peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.01092
lon: -123.52213
Cockscomb (Tuolumne Meadows). Cockscomb is a mountain, in the area of Tuolumne Meadows, Yosemite National Park, California. On Cockscomb's particulars. Cockscomb is aptly named, notably when viewed from the northwest. It is located in the Yosemite Wilderness, and is often forgotten, due to its proximity to Cathedral Peak, Matthes Crest, and Echo Peaks, but is deserves to be climbed.

Geographic entities mentioned:
surface_form: cockscomb
instance_of: Mountain
countries: United States
coordinates: lat: 37.83548
lon: -119.3846
Cockscomb is a mountain, in the area of Tuolumne Meadows, Yosemite National Park, California. On Cockscomb's particulars. Cockscomb is aptly named, notably when viewed from the northwest. It is located in the Yosemite Wilderness, and is often forgotten, due to its proximity to Cathedral Peak, Matthes Crest, and Echo Peaks, but is deserves to be climbed. The proximity of Cockscomb.

Geographic entities mentioned:
surface_form: cockscomb
instance_of: Mountain
countries: United States
coordinates: lat: 37.83548
lon: -119.3846
Cockscomb is aptly named, notably when viewed from the northwest. It is located in the Yosemite Wilderness, and is often forgotten, due to its proximity to Cathedral Peak, Matthes Crest, and Echo Peaks, but is deserves to be climbed. The proximity of Cockscomb. Cockscomb is near Echo Peaks, Unicorn Peak, Cathedral Peak, Matthes Crest, Budd Lake, also Elizabeth Lake. Rock climbing on Cockscomb.

Geographic entities mentioned:
surface_form: cockscomb
instance_of: Mountain
countries: United States
coordinates: lat: 37.83548
lon: -119.3846
The proximity of Cockscomb. Cockscomb is near Echo Peaks, Unicorn Peak, Cathedral Peak, Matthes Crest, Budd Lake, also Elizabeth Lake. Rock climbing on Cockscomb. None of Cockscomb's routes walk-ups, the easiest a Class 4. Cockscomb has two summits, a west and an east, separated by about, with a sharp notch between.

Geographic entities mentioned:
surface_form: cockscomb
instance_of: Mountain
countries: United States
coordinates: lat: 37.83548
lon: -119.3846
Rock climbing on Cockscomb. None of Cockscomb's routes walk-ups, the easiest a Class 4. Cockscomb has two summits, a west and an east, separated by about, with a sharp notch between. The west summit is a small perch, which can barely hold two people, while the east summit is a knife-edge, a dangerous perch.

Geographic entities mentioned:
surface_form: cockscomb
instance_of: Mountain
countries: United States
coordinates: lat: 37.83548
lon: -119.3846
Lake Morat or more rarely Lake Murten () is a lake located in the cantons of Fribourg and Vaud in the west of Switzerland. It is named after the small bilingual town of Morat on its southern shore. It is the smallest of the three lakes in the Seeland or Pays des trois lacs area of the Swiss plateau located at the foot of the first chain of the Jura mountains. The main tributary is the river Broye.

Geographic entities mentioned:
surface_form: Swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
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 main tributary is the river Broye. Since the Jura water correction its water leaves the lake through the Broye Canal (&quot;Canal de la Broye&quot;) into nearby Lake Neuchâtel that is connected to Lake Biel through the Thielle canal.

Geographic entities mentioned:
surface_form: Lake Neuchâtel
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.9
lon: 6.85
surface_form: Lake Biel
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.085555555556
lon: 7.1741666666667
surface_form: neuchâtel
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.9
lon: 6.85
surface_form: lake neuchâtel
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.9
lon: 6.85
surface_form: lake biel
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.085555555556
lon: 7.1741666666667
Lake Morat. Lake Morat or more rarely Lake Murten () is a lake located in the cantons of Fribourg and Vaud in the west of Switzerland. It is named after the small bilingual town of Morat on its southern shore. It is the smallest of the three lakes in the Seeland or Pays des trois lacs area of the Swiss plateau located at the foot of the first chain of the Jura mountains.

Geographic entities mentioned:
surface_form: lake murten
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.933333333333
lon: 7.075
surface_form: lake morat
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.933333333333
lon: 7.075
Lake Morat. Lake Morat or more rarely Lake Murten () is a lake located in the cantons of Fribourg and Vaud in the west of Switzerland. It is named after the small bilingual town of Morat on its southern shore. It is the smallest of the three lakes in the Seeland or Pays des trois lacs area of the Swiss plateau located at the foot of the first chain of the Jura mountains.

Geographic entities mentioned:
surface_form: lake morat
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.933333333333
lon: 7.075
Thus all three lakes form a natural reservoir in order to retain overflow water from the river Aare that flows into Lake Bienne/Biel: in times of combined heavy rainfalls and glacier
melting in the Alps, the peculiar situation arises that the water flows backwards through the Thielle and Broye canals, preventing an overflow of the Grand Marais.

Geographic entities mentioned:
surface_form: lake bienne
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.085555555556
lon: 7.1741666666667
Today, its main income is tourism. The countryside is also based economically on agriculture and herding. The tallest mountains in the regional unit include Mt Psiloritis (Mt Ida) reaching 2,456 metres and Mt Kedros reaching 1,777 metres. Prefecture. The Rethymno prefecture () was created while Crete was still an autonomous state, and was preserved after the island joined Greece in 1913.

Geographic entities mentioned:
surface_form: Mt Kedros
instance_of: Mountain
countries: Greece
coordinates: lat: 35.181666666667
lon: 24.6175
It is a southwest to northeast running fault formed by volcanic activity and earth movements during the middle Ordovician period (about 460 million years ago), following the general structural direction common to the Caledonian mountain-building event in northern Britain. First documented in 1881, it forms part of a collapsed volcanic basin known as the Snowdon caldera.

Geographic entities mentioned:
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
Geological setting and characteristics. The Beddgelert Fault separates the Snowdon syncline to the west and northwest from the Gwynant–Glaslyn valley to the east and southeast. These areas represent different stratigraphical successions of Ordovician rocks.

Geographic entities mentioned:
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
surface_form: Gwynant
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.0374
lon: -4.0471