Sarmila/GeoWiki-Features huggingface dataset:
Long Lake (Jerauld County, South Dakota). Long Lake is a natural lake in South Dakota, in the United States. Long Lake was descriptively named on account of the lake's relative long outline.

Geographic entities mentioned:
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 34.78779
lon: -111.210939
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9728
lon: -74.4211
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.718
lon: -85.748
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.1086787
lon: -75.1564925
surface_form: long lake (jerauld county, south dakota)
instance_of: Lake
countries: United States
coordinates: lat: 44.1657291
lon: -98.7168782
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9334172
lon: -97.0073724
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9496317
lon: -95.9225667
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.8456754
lon: -99.2676497
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.127777777778
lon: -83.973055555556
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 46.235907
lon: -89.49916
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9348621
lon: -97.3996461
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.20461
lon: -83.47775
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.5597393
lon: -75.1515847
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.248184
lon: -85.075807
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 41.615555555556
lon: -87.210555555556
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.7281765
lon: -97.3795798
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 47.483055555556
lon: -122.58972222222
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.971666666667
lon: -70.611666666667
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.8387529
lon: -88.6755297
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 47.0191485
lon: -122.7747634
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.572222222222
lon: -85.298888888889
Long Lake (Jerauld County, South Dakota). Long Lake is a natural lake in South Dakota, in the United States. Long Lake was descriptively named on account of the lake's relative long outline.

Geographic entities mentioned:
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 34.78779
lon: -111.210939
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9728
lon: -74.4211
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.718
lon: -85.748
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.1086787
lon: -75.1564925
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.1657291
lon: -98.7168782
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9334172
lon: -97.0073724
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9496317
lon: -95.9225667
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.8456754
lon: -99.2676497
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.127777777778
lon: -83.973055555556
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 46.235907
lon: -89.49916
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9348621
lon: -97.3996461
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.20461
lon: -83.47775
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.5597393
lon: -75.1515847
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.248184
lon: -85.075807
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 41.615555555556
lon: -87.210555555556
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.7281765
lon: -97.3795798
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 47.483055555556
lon: -122.58972222222
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.971666666667
lon: -70.611666666667
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.8387529
lon: -88.6755297
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 47.0191485
lon: -122.7747634
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.572222222222
lon: -85.298888888889
Reicholzheim. Reicholzheim is a district of Wertheim am Main in Germany. It is located in the Tauber valley at the foothills of the Odenwald and the quiet forests of the Spessart on the banks of the Tauber river near the mouth of the Tauber into the Main river. Reicholzheim had 1,450 inhabitants in 2003. Description and location.

Geographic entities mentioned:
surface_form: Tauber
instance_of: Watercourse
countries: Germany
coordinates: lat: 49.25
lon: 10.114861111111
Koshin River. The Koshin River is a tributary of the Nahlin River in northwest part of the province of British Columbia, Canada. It flows generally north about to join the Nahlin River, which forms the Inklin River, one of the main tributaries of the Taku River. The Koshin River flows through the Nahlin Plateau. It joins the Nahlin River at the boundary between the Nahlin and Kawdy plateaus.

Geographic entities mentioned:
surface_form: Nahlin Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.44972222222222
lon: -131.41833333333332
surface_form: koshin river
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.86621
lon: -131.80364
It flows generally north about to join the Nahlin River, which forms the Inklin River, one of the main tributaries of the Taku River. The Koshin River flows through the Nahlin Plateau. It joins the Nahlin River at the boundary between the Nahlin and Kawdy plateaus. Both plateaus are part of the larger Stikine Plateau region. The Koshin River's watershed covers, and its mean annual discharge is.

Geographic entities mentioned:
surface_form: Kawdy
instance_of: Plateau
countries: Canada
coordinates: lat: 59.24948
lon: -131.50356
The Koshin River flows through the Nahlin Plateau. It joins the Nahlin River at the boundary between the Nahlin and Kawdy plateaus. Both plateaus are part of the larger Stikine Plateau region. The Koshin River's watershed covers, and its mean annual discharge is. The mouth of the Koshin River is located about northeast of Juneau, Alaska and about north of Telegraph Creek, British Columbia.

Geographic entities mentioned:
surface_form: Stikine Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
The Koshin River is in the traditional territories of the Taku River Tlingit First Nation, part of the Tlingit people, and the Tahltan First Nation, of the Tahltan people. Geography. The Koshin River originates on the north side of Level Mountain on the Nahlin Plateau. From its source the river flows generally north for about.

Geographic entities mentioned:
surface_form: Nahlin Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.44972222222222
lon: -131.41833333333332
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: koshin river
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.86621
lon: -131.80364
The Koshin River originates on the north side of Level Mountain on the Nahlin Plateau. From its source the river flows generally north for about. From its source it first flows northwest to Hatin Lake, just west of Callison Ranch. This headwater reach of the Koshin River lies just north of Matsatu Creek. From Hatin Lake the Koshin River flows north along a meandering course with many wetlands.

Geographic entities mentioned:
surface_form: Hatin Lake
instance_of: Lake
countries: Canada
coordinates: lat: 58.64944
lon: -131.72222
From its source the river flows generally north for about. From its source it first flows northwest to Hatin Lake, just west of Callison Ranch. This headwater reach of the Koshin River lies just north of Matsatu Creek. From Hatin Lake the Koshin River flows north along a meandering course with many wetlands. Lost Creek joins the Koshin, flowing northwest from Level Mountain.

Geographic entities mentioned:
surface_form: Matsatu Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.58283
lon: -131.77035
surface_form: koshin river
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.86621
lon: -131.80364
Lost Creek joins the Koshin, flowing northwest from Level Mountain. A few kilometres downriver Kaha Creek joins the Koshin, also flowing northwest from Level Mountain. Continuing north the Koshin River passes by a number of lakes, including Tedideech Lake, before emptying into the Nahlin River at Nahlin Crossing.

Geographic entities mentioned:
surface_form: Kaha Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.68283
lon: -131.68693
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Koshin River. The Koshin River is a tributary of the Nahlin River in northwest part of the province of British Columbia, Canada. It flows generally north about to join the Nahlin River, which forms the Inklin River, one of the main tributaries of the Taku River. The Koshin River flows through the Nahlin Plateau. It joins the Nahlin River at the boundary between the Nahlin and Kawdy plateaus.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: koshin river
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.86621
lon: -131.80364
The Koshin River's watershed covers, and its mean annual discharge is. The mouth of the Koshin River is located about northeast of Juneau, Alaska and about north of Telegraph Creek, British Columbia. The Koshin River's watershed's land cover is classified as 43.0% conifer forest, 36.3% shrubland, 8.8% mixed forest, 5.4% barren, 2.5% wetland, and small amounts of other cover.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: koshin river
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.86621
lon: -131.80364
The Koshin River's watershed's land cover is classified as 43.0% conifer forest, 36.3% shrubland, 8.8% mixed forest, 5.4% barren, 2.5% wetland, and small amounts of other cover. The Koshin River is in the traditional territories of the Taku River Tlingit First Nation, part of the Tlingit people, and the Tahltan First Nation, of the Tahltan people. Geography.

Geographic entities mentioned:
surface_form: tlingit
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
surface_form: tlingit
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
surface_form: koshin river
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.86621
lon: -131.80364
This headwater reach of the Koshin River lies just north of Matsatu Creek. From Hatin Lake the Koshin River flows north along a meandering course with many wetlands. Lost Creek joins the Koshin, flowing northwest from Level Mountain. A few kilometres downriver Kaha Creek joins the Koshin, also flowing northwest from Level Mountain.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
From its source the river flows generally north for about. From its source it first flows northwest to Hatin Lake, just west of Callison Ranch. This headwater reach of the Koshin River lies just north of Matsatu Creek. From Hatin Lake the Koshin River flows north along a meandering course with many wetlands. Lost Creek joins the Koshin, flowing northwest from Level Mountain.

Geographic entities mentioned:
surface_form: hatin lake
instance_of: Lake
countries: Canada
coordinates: lat: 58.64944
lon: -131.72222
surface_form: koshin river
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.86621
lon: -131.80364
Koshin River. The Koshin River is a tributary of the Nahlin River in northwest part of the province of British Columbia, Canada. It flows generally north about to join the Nahlin River, which forms the Inklin River, one of the main tributaries of the Taku River. The Koshin River flows through the Nahlin Plateau. It joins the Nahlin River at the boundary between the Nahlin and Kawdy plateaus.

Geographic entities mentioned:
surface_form: koshin river
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.86621
lon: -131.80364
The Koshin River flows through the Nahlin Plateau. It joins the Nahlin River at the boundary between the Nahlin and Kawdy plateaus. Both plateaus are part of the larger Stikine Plateau region. The Koshin River's watershed covers, and its mean annual discharge is. The mouth of the Koshin River is located about northeast of Juneau, Alaska and about north of Telegraph Creek, British Columbia.

Geographic entities mentioned:
surface_form: koshin river
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.86621
lon: -131.80364
The Koshin River's watershed covers, and its mean annual discharge is. The mouth of the Koshin River is located about northeast of Juneau, Alaska and about north of Telegraph Creek, British Columbia. The Koshin River's watershed's land cover is classified as 43.0% conifer forest, 36.3% shrubland, 8.8% mixed forest, 5.4% barren, 2.5% wetland, and small amounts of other cover.

Geographic entities mentioned:
surface_form: koshin river
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.86621
lon: -131.80364
A few kilometres downriver Kaha Creek joins the Koshin, also flowing northwest from Level Mountain. Continuing north the Koshin River passes by a number of lakes, including Tedideech Lake, before emptying into the Nahlin River at Nahlin Crossing. The historic Yukon Telegraph Trail follows much of the Koshin River, passing through Callison Ranch and running north along the river to Nahlin Crossing.

Geographic entities mentioned:
surface_form: koshin river
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.86621
lon: -131.80364
When they arrive at a meeting point arranged by the kidnappers—on adjacent aerial lift cars above Sugarloaf Mountain—they find that Homer has developed Stockholm syndrome and made a scrapbook to remember his kidnapping. They throw the money across and Homer jumps to the family's car, only for the cables to break and send them tumbling down the mountainside.

Geographic entities mentioned:
surface_form: Sugarloaf Mountain
instance_of: Mountain
countries: Brazil
coordinates: lat: -22.949444444444445
lon: -43.156666666666666
It was intended for the burial of Ay, who later became Pharaoh, after the 18th Dynasty king Tutankhamun. The grave was never finished, and Ay was later interred in the Western Valley of the Valley of the Kings (tomb WV23), in Thebes. The tomb was only partially carved from the rock, with the first part of the pillared hall approaching completion.

Geographic entities mentioned:
surface_form: Valley of the Kings
instance_of: Valley
countries: Egypt
coordinates: lat: 25.74025
lon: 32.602358
It eventually lost importance to Antigua, in Guatemala. Lempira is a rugged department, and it is relatively isolated from the rest of the country. The highest mountain peak in Honduras, Cerro las Minas, is in Lempira. The department was named after Lempira, a local chieftain of the Lenca people who fought against the Spanish conquistadores in the early 16th century.

Geographic entities mentioned:
surface_form: Cerro las Minas
instance_of: Mountain
countries: Honduras
coordinates: lat: 14.534166666667
lon: -88.68
Named for a geologist in the party, M. Gregory. Panorama Point. Point surmounted by a small hill on the northwest side of Cotton Plateau, overlooking the junction of Marsh and Nimrod Glaciers. So named by the Holyoake, Cobham and Queen Elizabeth Ranges party of the NZGSAE (1964-65) because it affords an excellent view. The Palisades.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: cotton plateau
instance_of: Plateau
coordinates: lat: -82.9
lon: 159.667
Cotton Plateau. Cotton Plateau () is a snow-covered plateau just east of the mouth of Marsh Glacier, in the Queen Elizabeth Range. Name. Cotton Plateau was named by the northern party of the New Zealand Geological Survey Antarctic Expedition (NZGSAE; 1961–62) for Sir Charles Cotton, noted New Zealand geomorphologist and authority on glacial landforms. Location.

Geographic entities mentioned:
surface_form: elizabeth
instance_of: Mountain
coordinates: lat: -83.9
lon: 168.383
surface_form: cotton plateau
instance_of: Plateau
coordinates: lat: -82.9
lon: 159.667
Location. Cotton Plateau is in the west of the Queen Elizabeth Range, bounded by the Marsh Glacier to the west, the Prince of Wales Glacier and Hamilton Glacier to the east and the Princess Anne Glacier to the south. Features include, from north to south, Hochstein Ridge, Prince Edward Glacier, Panorama Point and The Palisades. Hochstein Ridge.

Geographic entities mentioned:
surface_form: elizabeth
instance_of: Mountain
coordinates: lat: -83.9
lon: 168.383
surface_form: cotton plateau
instance_of: Plateau
coordinates: lat: -82.9
lon: 159.667
Named by US-ACAN for Walter D. Komhyr, USARP meteorologist at McMurdo Station, 1963-64. Mount Gregory. A mountain high at the south end of Hochstein Ridge. It is the only large elevation rising from Cotton Plateau. The name was suggested by the Holyoake, Cobham and Queen Elizabeth Ranges Part of the NZGSAE, 1964-65. Named for a geologist in the party, M. Gregory. Panorama Point.

Geographic entities mentioned:
surface_form: elizabeth
instance_of: Mountain
coordinates: lat: -83.9
lon: 168.383
Named for a geologist in the party, M. Gregory. Panorama Point. Point surmounted by a small hill on the northwest side of Cotton Plateau, overlooking the junction of Marsh and Nimrod Glaciers. So named by the Holyoake, Cobham and Queen Elizabeth Ranges party of the NZGSAE (1964-65) because it affords an excellent view. The Palisades.

Geographic entities mentioned:
surface_form: elizabeth
instance_of: Mountain
coordinates: lat: -83.9
lon: 168.383
The Palisades. A steep escarpment at the west side of Cotton Plateau in the Queen Elizabeth Range, overlooking Marsh and Nimrod Glaciers. Seen by the northern party of the NZGSAE (1961-62) and so named because of the resemblance to a protective wall at the junction of two rivers.

Geographic entities mentioned:
surface_form: elizabeth
instance_of: Mountain
coordinates: lat: -83.9
lon: 168.383
surface_form: cotton plateau
instance_of: Plateau
coordinates: lat: -82.9
lon: 159.667
Cotton Plateau. Cotton Plateau () is a snow-covered plateau just east of the mouth of Marsh Glacier, in the Queen Elizabeth Range. Name. Cotton Plateau was named by the northern party of the New Zealand Geological Survey Antarctic Expedition (NZGSAE; 1961–62) for Sir Charles Cotton, noted New Zealand geomorphologist and authority on glacial landforms. Location.

Geographic entities mentioned:
surface_form: cotton plateau
instance_of: Plateau
coordinates: lat: -82.9
lon: 159.667
Cotton Plateau. Cotton Plateau () is a snow-covered plateau just east of the mouth of Marsh Glacier, in the Queen Elizabeth Range. Name. Cotton Plateau was named by the northern party of the New Zealand Geological Survey Antarctic Expedition (NZGSAE; 1961–62) for Sir Charles Cotton, noted New Zealand geomorphologist and authority on glacial landforms. Location.

Geographic entities mentioned:
surface_form: cotton plateau
instance_of: Plateau
coordinates: lat: -82.9
lon: 159.667
surface_form: charles
instance_of: Mountain
coordinates: lat: -67.38333
lon: 50
Features include, from north to south, Hochstein Ridge, Prince Edward Glacier, Panorama Point and The Palisades. Hochstein Ridge. A ridge long, extending north from Cotton Plateau between Prince Edward Glacier and Prince of Wales Glacie. Mapped by the United States Geological Survey (USGS) from tellurometer surveys and Navy air photos, 1960-62.

Geographic entities mentioned:
surface_form: cotton plateau
instance_of: Plateau
coordinates: lat: -82.9
lon: 159.667
Named by US-ACAN for Walter D. Komhyr, USARP meteorologist at McMurdo Station, 1963-64. Mount Gregory. A mountain high at the south end of Hochstein Ridge. It is the only large elevation rising from Cotton Plateau. The name was suggested by the Holyoake, Cobham and Queen Elizabeth Ranges Part of the NZGSAE, 1964-65. Named for a geologist in the party, M. Gregory. Panorama Point.

Geographic entities mentioned:
surface_form: cotton plateau
instance_of: Plateau
coordinates: lat: -82.9
lon: 159.667
Mathilda tells Woodville that her upbringing, while cold on the part of her aunt, was never neglectful; she learned to occupy her time with books and jaunts around her aunt's estate in Loch Lomond, Scotland. On Mathilda's sixteenth birthday her aunt received a letter from Mathilda's father expressing his desire to see his daughter.

Geographic entities mentioned:
surface_form: Loch Lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
Cheondeungsan (South Jeolla). Cheondeungsan () is a mountain of South Jeolla Province, in western South Korea. It has an elevation of 550 metres.

Geographic entities mentioned:
surface_form: cheondeungsan
instance_of: Mountain
countries: South Korea
surface_form: cheondeungsan
instance_of: Mountain
countries: South Korea
surface_form: cheondeungsan (south jeolla)
instance_of: Mountain
countries: South Korea
surface_form: cheondeungsan
instance_of: Mountain
countries: South Korea
Cheondeungsan (South Jeolla). Cheondeungsan () is a mountain of South Jeolla Province, in western South Korea. It has an elevation of 550 metres.

Geographic entities mentioned:
surface_form: cheondeungsan
instance_of: Mountain
countries: South Korea
surface_form: cheondeungsan
instance_of: Mountain
countries: South Korea
surface_form: cheondeungsan
instance_of: Mountain
countries: South Korea
surface_form: cheondeungsan
instance_of: Mountain
countries: South Korea
Eber-Nari. Eber-Nari (Akkadian), also called Abar-Nahara (Aramaic) or Aber Nahra (Syriac), was a region of the ancient Near East. Translated as &quot;Beyond the River&quot; or &quot;Across the River&quot; in both the Akkadian and Aramaic languages, it referred to the land on the opposite side of the Euphrates from the perspective of Mesopotamia and Persia.

Geographic entities mentioned:
surface_form: Persia
instance_of: Plateau
countries: Iran
coordinates: lat: 36.283333
lon: 59.05
Ark Hill. Ark Hill is a mountainous landform within the Sidlaw Hills in Angus, Scotland. This location has been proposed as a windfarm for generating renewable electrical power. Approximately two kilometres to the north is the village of Eassie noted for the presence of the Eassie Stone; this carved Pictish stone is dated prior to the Early Middle Ages.

Geographic entities mentioned:
surface_form: ark hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.570973
lon: -3.04805
Early life. Born 1927, Kennedy moved from Santa Cruz to Santa Clara Valley at the age of 15, earning a degree from Stanford University at the age of 19. Married, and with the first of her four children, Kathryn moved to her Saratoga property in 1949 where she later decided to plant a vineyard.

Geographic entities mentioned:
surface_form: Santa Clara Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.366944444444
lon: -121.98388888889
Uyshu. Uyshu (Jaqaru for to liquify, melt, also spelled &quot;Uysho&quot;) is a mountain in the Andes of Peru. It is situated in the Lima Region, Huarochirí Province, Huanza District. Uyshu lies northeast of Qullqi and southwest of the lakes named P'itiqucha and Saqsaqucha.

Geographic entities mentioned:
surface_form: qullqi
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7139
lon: -70.905
surface_form: qullqi
instance_of: Mountain
countries: Peru
coordinates: lat: -11.5706
lon: -76.4847
surface_form: qullqi
instance_of: Mountain
countries: Peru
coordinates: lat: -15.1389
lon: -70.4978
surface_form: p'itiqucha
instance_of: Lake
countries: Peru
coordinates: lat: -11.545
lon: -76.434166666667
Uyshu. Uyshu (Jaqaru for to liquify, melt, also spelled &quot;Uysho&quot;) is a mountain in the Andes of Peru. It is situated in the Lima Region, Huarochirí Province, Huanza District. Uyshu lies northeast of Qullqi and southwest of the lakes named P'itiqucha and Saqsaqucha.

Geographic entities mentioned:
surface_form: uyshu
instance_of: Mountain
countries: Peru
coordinates: lat: -11.5556
lon: -76.4606
Cadair Berwyn. Cadair Berwyn, Cader Berwyn or Craig Uchaf is a mountain summit in north-east Wales with a height of above sea level. It is the highest point in the Berwyn range, the highest in North East Wales and the highest significant summit in Wales outside the National Parks. Cadair Berwyn and Foel Cedig to the west are the two Marilyns that form the Berwyn range.

Geographic entities mentioned:
surface_form: Foel Cedig
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.84281
lon: -3.51331
surface_form: cadair berwyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.8806
lon: -3.38099
Craig y Llyn forms the headwall of a cwm, and it is to this that the word &quot;cadair&quot; (&quot;chair&quot; in Welsh) presumably refers. Further north along the ridge is Cadair Bronwen, whilst to south the ridge continues to Moel Sych (, meaning 'dry hill').

Geographic entities mentioned:
surface_form: Cadair Bronwen
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.90146
lon: -3.3729
surface_form: Moel Sych
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.87608
lon: -3.38878
surface_form: moel sych
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.87608
lon: -3.38878
surface_form: cadair bronwen
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.90146
lon: -3.3729
Further north along the ridge is Cadair Bronwen, whilst to south the ridge continues to Moel Sych (, meaning 'dry hill'). It is often reported that Moel Sych, along the ridge, is of equal height, but Cadair Berwyn's spot height on the Ordnance Survey maps, where the trig point stands, is not the true summit. Cadair Berwyn's summit, south of the trig point, is taller than Moel Sych.

Geographic entities mentioned:
surface_form: Moel Sych
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.87608
lon: -3.38878
surface_form: moel sych
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.87608
lon: -3.38878
surface_form: cadair berwyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.8806
lon: -3.38099
surface_form: cadair berwyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.8806
lon: -3.38099
Phillips uses the name Craig Berwyn rather than Cadair Berwyn for this summit. Several other summits in the area are listed as Hewitts or Nuttalls, including Foel Wen (, Welsh for &quot;white hill&quot;) and Mynydd Tarw (, &quot;bull mountain&quot;). Cadair Berwyn is the highest point (county top) of the historic county of Denbighshire.

Geographic entities mentioned:
surface_form: Foel Wen
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.89057
lon: -3.34012
surface_form: Mynydd Tarw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.8821
lon: -3.32005
surface_form: mynydd tarw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.8821
lon: -3.32005
surface_form: foel wen
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.89057
lon: -3.34012
surface_form: white hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.0233
lon: -2.50062
Curiously, the historic county of Denbighshire lies on the eastern side on the main Berwyn ridge, but the modern council lies on the western side. The northern end of the main ridge (Craig Berwyn on the OS map, height, north of Cadair Berwyn North Top) is the highest point in Wrexham county borough. Cadair Berwyn stands between Snowdon and the Wrekin and blocks their line-of-sight.

Geographic entities mentioned:
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
surface_form: the Wrekin
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.66916666666667
lon: -2.551388888888889
surface_form: wrekin
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.66916666666667
lon: -2.551388888888889
surface_form: the wrekin
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.66916666666667
lon: -2.551388888888889
Cadair Berwyn stands between Snowdon and the Wrekin and blocks their line-of-sight. The view from the summit on a clear day is extensive and includes Snowdon, Cadair Idris, Brecon Beacons, Shropshire Hills, Peak District, Yorkshire Dales, Lake District and the Isle of Man.

Geographic entities mentioned:
surface_form: Cadair Idris
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.699827777778
lon: -3.9086944444444
surface_form: snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
surface_form: cadair idris
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.699827777778
lon: -3.9086944444444
On 11 August 1942, a United States Army Air Forces, Boeing B-17E Flying Fortress flying from RAF Polebrook to RAF Burtonwood crashed into the side of Cadair Berwyn resulting in the deaths of all eleven passengers and crew. It is the location, as well as Cadair Bronwen, of an alleged UFO landing in 1974, known as the Berwyn Mountain UFO incident.

Geographic entities mentioned:
surface_form: Cadair Bronwen
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.90146
lon: -3.3729
Curiously, the historic county of Denbighshire lies on the eastern side on the main Berwyn ridge, but the modern council lies on the western side. The northern end of the main ridge (Craig Berwyn on the OS map, height, north of Cadair Berwyn North Top) is the highest point in Wrexham county borough. Cadair Berwyn stands between Snowdon and the Wrekin and blocks their line-of-sight.

Geographic entities mentioned:
surface_form: cadair berwyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.8806
lon: -3.38099
surface_form: cadair berwyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.8806
lon: -3.38099
It is often reported that Moel Sych, along the ridge, is of equal height, but Cadair Berwyn's spot height on the Ordnance Survey maps, where the trig point stands, is not the true summit. Cadair Berwyn's summit, south of the trig point, is taller than Moel Sych. This summit is listed as Cadair Berwyn New Top on the Nuttall list.

Geographic entities mentioned:
surface_form: moel sych
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.87608
lon: -3.38878
The view from the summit on a clear day is extensive and includes Snowdon, Cadair Idris, Brecon Beacons, Shropshire Hills, Peak District, Yorkshire Dales, Lake District and the Isle of Man. The peak is the nearest high mountain to a significant fraction of the population of the English Midlands but sees far fewer walkers than equivalent summits in the Lake District and Snowdonia.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
This was re-erected in June 2008 by High Sports. The standing stone can be found at SJ080337. Below the mountain is a small lake, Llyn Lluncaws set in a glacial cirque. On 11 August 1942, a United States Army Air Forces, Boeing B-17E Flying Fortress flying from RAF Polebrook to RAF Burtonwood crashed into the side of Cadair Berwyn resulting in the deaths of all eleven passengers and crew.

Geographic entities mentioned:
surface_form: cadair berwyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.8806
lon: -3.38099
Cadair Berwyn. Cadair Berwyn, Cader Berwyn or Craig Uchaf is a mountain summit in north-east Wales with a height of above sea level. It is the highest point in the Berwyn range, the highest in North East Wales and the highest significant summit in Wales outside the National Parks. Cadair Berwyn and Foel Cedig to the west are the two Marilyns that form the Berwyn range.

Geographic entities mentioned:
surface_form: cadair berwyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.8806
lon: -3.38099
Cadair Berwyn and Foel Cedig to the west are the two Marilyns that form the Berwyn range. The undulating plateau of the range also includes a large number of other summits above, including satellite summits of Cadair Berwyn and many which are classed as Nuttalls. The mountain lies on main ridge of the Berwyns which runs north–south.

Geographic entities mentioned:
surface_form: cadair berwyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.8806
lon: -3.38099
Cadair Berwyn's summit, south of the trig point, is taller than Moel Sych. This summit is listed as Cadair Berwyn New Top on the Nuttall list. However, the name given to it by its discoverer, Bernard Wright, was Craig Uchaf.

Geographic entities mentioned:
surface_form: cadair berwyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.8806
lon: -3.38099
This summit is listed as Cadair Berwyn New Top on the Nuttall list. However, the name given to it by its discoverer, Bernard Wright, was Craig Uchaf. In 1987 Bernard Wright, a rambler from Cheshire, was standing on Cadair Berwyn North Top (then said to be the highest mountain in Clwyd) when he noticed that a nearby peak appeared to be higher.

Geographic entities mentioned:
surface_form: cadair berwyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.8806
lon: -3.38099
Near the summit is a Bronze Age cairn. In 2014, accurate re-surveying using GPS by Myrddyn Phillips added an additional 2 metres to the height. Phillips uses the name Craig Berwyn rather than Cadair Berwyn for this summit. Several other summits in the area are listed as Hewitts or Nuttalls, including Foel Wen (, Welsh for &quot;white hill&quot;) and Mynydd Tarw (, &quot;bull mountain&quot;).

Geographic entities mentioned:
surface_form: cadair berwyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.8806
lon: -3.38099
The peak is the nearest high mountain to a significant fraction of the population of the English Midlands but sees far fewer walkers than equivalent summits in the Lake District and Snowdonia. There is a standing stone in the area, located near the summit between Cadair Berwyn and Tomle. This was re-erected in June 2008 by High Sports. The standing stone can be found at SJ080337.

Geographic entities mentioned:
surface_form: cadair berwyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.8806
lon: -3.38099
Location and features. The falls are situated at the foot of the southern face of Mount Bartle Frere in Wooroonooran National Park. They descend from the Atherton Tableland at an elevation of above sea level in the range of near a popular recreation site as the water flows over a large rock to form a natural waterslide on Josephine Creek, a tributary of the Russell River.

Geographic entities mentioned:
surface_form: Mount Bartle Frere
instance_of: Mountain
countries: Australia
coordinates: lat: -17.383333333333
lon: 145.81666666667
Location and features. The falls are situated at the foot of the southern face of Mount Bartle Frere in Wooroonooran National Park. They descend from the Atherton Tableland at an elevation of above sea level in the range of near a popular recreation site as the water flows over a large rock to form a natural waterslide on Josephine Creek, a tributary of the Russell River.

Geographic entities mentioned:
surface_form: Atherton Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
Mutyalapalem. Mutyalapalem is a village in East Godavari district in the state of Andhra Pradesh, India. Geography. Mutyalapalem covers around 412 acres, and has approximately 210 houses. The total population of the village is around 1000. Mutyalapalem is about from the Bay of Bengal. It is part of the Konaseema delta, a triangle formed by the waters of the Godavari River and the delta.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
The Sioux bands in council have earnestly solicited that they might have permission to bestow upon the half-breeds of their nation the tract of land within the following limits, to wit: Beginning at the place called the Barn, below and near the village of the Red Wing chief, and running back fifteen miles; thence, in a parallel line with Lake Pepin and the Mississippi, about 32 miles, to a point opposite the river aforesaid; the United States agree to suffer said half-breeds to occupy said tract of country; they holding by the same title, and in the same manner that other Indian titles are held.

Geographic entities mentioned:
surface_form: Lake Pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
The Himalayas, which stretch over 2400 km between the Namcha Barwa syntaxis at the eastern end of the mountain range and the Nanga Parbat syntaxis at the western end, are the result of an ongoing orogeny — the collision of the continental crust of two tectonic plates, namely, the Indian Plate thrusting into the Eurasian Plate.

Geographic entities mentioned:
surface_form: Namcha Barwa
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 29.630555555556
lon: 95.055277777778
surface_form: Nanga Parbat
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.239166666667
lon: 74.59
4). While most of the oceanic crust was &quot;simply&quot; subducted below the Tibetan block during the northward motion of India, at least three major mechanisms have been put forward, either separately or jointly, to explain what happened, since collision, to the 2500 km of &quot;missing continental crust&quot;.

Geographic entities mentioned:
surface_form: Tibetan block
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
It is commonly separated into four zones. High Himalayan Crystalline Sequence (HHCS). Approximately 30 different names exist in the literature to describe this unit; the most frequently found equivalents are &quot;Greater Himalayan Sequence&quot;, &quot;Tibetan Slab&quot; and &quot;High Himalayan Crystalline&quot;.

Geographic entities mentioned:
surface_form: Tibetan Slab
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
22 Ma) age. Although most of the metasediments forming the HHCS are of late Proterozoic to early Cambrian age, much younger metasediments can also be found in several areas, e.g. Mesozoic in the Tandi syncline of Nepal and Warwan Valley of Kistwar in Kashmir, Permian in the &quot;Tschuldo slice&quot;, Ordovician to Carboniferous in the &quot;Sarchu area&quot; on Leh-Manali Highway.

Geographic entities mentioned:
surface_form: Warwan Valley
instance_of: Valley
countries: India
coordinates: lat: 33.86416666666667
lon: 75.53527777777778
Nyimaling-Tso Morari Metamorphic Dome (NTMD). &quot;Nyimaling-Tso Morari Metamorphic Dome&quot; in the Ladakh region, the &quot;Tethys Himalaya synclinorium&quot; passes gradually to the north in a large dome of greenschist to eclogitic metamorphic rocks. As with the HHCS, these metamorphic rocks represent the metamorphic equivalent of the sediments forming the base of the Tethys Himalaya.

Geographic entities mentioned:
surface_form: Tso Morari
instance_of: Lake
countries: India
coordinates: lat: 32.9
lon: 78.3
He has served as a parish priest and taught theology at schools in Kenya, Tanzania, and the United States. Early life and career. Magesa was born in 1946 in northern Tanzania, along the shores of Lake Victoria. He attended primary school in Musoma and then attended secondary and high school at St. Mary’s Seminary in Mwanza, Tanzania, graduating in 1968.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Shortly after Wood's birth, the family moved to Waterville, Washington. Wood became fond of outdoor activities such as hiking, fishing, river rafting and horseback riding during her childhood, and her family spent many summers at a cottage on Lake Chelan. As a teenager, she worked as a camp counselor and ranch tour guide.

Geographic entities mentioned:
surface_form: Lake Chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
The persistent border between these two cultures indicates different cultural, and perhaps ethnic, identities. The Knovíz culture expanded to Central Bohemia by the time of Ha A2, into the middle Elbe region, where it displaced the Lusatian culture. At the end of this period, border fortifications are constructed, probably due to hostility between the two cultures.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Economy. Livelihood was probably based on agriculture, which is evidenced by the expansion of this culture along the fertile soil of the Elbe river basin and some of its tributaries, and supplemented by pastoralism, probably in the form of cattle farming, particularly in hilly and rocky areas. The contribution from hunting was probably negligible.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Nagyvázsony. Nagyvázsony is a village in Veszprém, Hungary. It lies approximately 15 km (9 mi) north of the Lake Balaton. It houses Kinizsi Castle, a 14th-century fortification donated by Matthias I to Pál Kinizsi. Kinizsi's sarcophagus can be found in the castle chapel. Facing the castle is a baroque church which was commissioned by Kinizsi in 1470.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
It was designed by John G. Alden and built by Goudy & Stevens Shipyard in Boothbay, Maine. It was designed in 1950 and launched in 1952. She measures in length, in beam, and with her fixed keel has a draft of. She was moved to Buffalo in the mid-1980s after sailing on Lake Champlain. It was listed on the National Register of Historic Places in 2013.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
An account of the rebellion is vividly described in the &quot;Diary of Adam Tas&quot;. Dirk Coetzee/Coetsee established Coetsenburg, one of the oldest wine estates in South Africa, in 1682, on land granted to him by the Dutch Governor of the Cape Colony, Simon van der Stel, on the banks of the Eerste River at the foot of the Stellenbosch Mountain.

Geographic entities mentioned:
surface_form: Stellenbosch Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.9698
lon: 18.9008
Adderley Street was originally named the Herengracht, after the canal (&quot;gracht&quot;) which ran down its centre, and which had its origins in the rivers flowing down to the sea from Table Mountain, and the lords or patricians (&quot;heren&quot;) which established their townhouses in the street.

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
Dirk and Sara Coetsee lived in Huis Herengracht for four years.[14]
In 1682, the Dutch Governor of the Cape Colony, Simon van der Stel, granted Coetzee/Coetsee land at the foot of the Stellenbosch Mountain on the banks of the Eerste River which Coetsee named Coetsenburg.[4] After moving onto Coetsenburg, the Coetzee/Coetsees used Huis Herengracht as their townhouse. Coetzenburg/Coetsenburg Estate.

Geographic entities mentioned:
surface_form: Stellenbosch Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.9698
lon: 18.9008
Thus &quot;Coetsenburg&quot; can be interpreted either as &quot;Coetzee/Coetsee and his Mountain&quot; or &quot;Coetzee/Coetsee and his Fortress&quot;. The mountain referred to in the name is the Groteberg or Stellenbosch Mountain, part of which is on the estate. The Coetsenburg Estate lies on the banks of the Eerste River in the town of Stellenbosch in the Western Cape province of South Africa.

Geographic entities mentioned:
surface_form: Stellenbosch Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.9698
lon: 18.9008
The estate stretches up southwards from the Eerste River onto the slopes of the Stellenbosch Mountain, which is part of the Hottentots Holland mountain range, to the Blaauwklippen River (Blouklip River) which forms its southern boundary.

Geographic entities mentioned:
surface_form: Stellenbosch Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.9698
lon: 18.9008
In 1706, he became captain of the Stellenbosch Infantry. In 1682, he approached Commander Simon van der Stel and was in particular given a piece of land or place later called Coetsenburg, located close to Stellenbosch. He also has a piece of land in Jan Jonkershoek (the Jonkershoek Valley), under the big mountain (Stellenbosch Mountain), called Assegaaibosch.

Geographic entities mentioned:
surface_form: Stellenbosch Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.9698
lon: 18.9008
Final years. Though he lived in the city of Trivandrum for more than three decades, Thirunalloor chose to spend the rest of his life in his native village of Perinad on the banks of Ashtamudi lake, which had been a constant source of inspiration for his poetry. He died on 5 July 2006 at his residence in Quilon. He was buried without any customary religious rites or ceremonies, as he had wished.

Geographic entities mentioned:
surface_form: Ashtamudi lake
instance_of: Lake
countries: India
coordinates: lat: 8.9833333333333
lon: 76.6
During his final years, he was engaged in writing a long poem titled 'Seetha' (Sita), reinterpreting the Ramayana legend
A three-day-long cultural festival called 'Thirunalloor Kavyolsavam' is held every year from 1 May (International Workers' Day) on the banks of the Ashtamudi lake in Quilon to perpetuate his memory. Writings and philosophy.

Geographic entities mentioned:
surface_form: Ashtamudi lake
instance_of: Lake
countries: India
coordinates: lat: 8.9833333333333
lon: 76.6
The Ashtamudi lake and life on its shores was a key source of inspiration for his writings, and his poetry abounds with varied themes, characters, and imagery taken from this environment. He wrote also wrote short lyrics dealing with soft transitory feelings and moods, as well as long narrative poems that contain diverse characters and complex social situations.

Geographic entities mentioned:
surface_form: Ashtamudi lake
instance_of: Lake
countries: India
coordinates: lat: 8.9833333333333
lon: 76.6