Sarmila/GeoWiki-Features huggingface dataset:
There are seven lakes in the region totaling with the three principal lakes of the group being Big Spirit Lake, West Okoboji Lake, and East Okoboji Lake. They are the largest natural lakes in the state of Iowa. The largest, Spirit Lake, is 5,684 acres (2,300 ha). The lake area extends to the north into Jackson County, Minnesota.

Geographic entities mentioned:
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 47.94
lon: -116.9
surface_form: spirit
instance_of: Lake
countries: United States
coordinates: lat: 46.273055555556
lon: -122.135
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4739
lon: -95.1018
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 45.38055556
lon: -90.13694444
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 44.49305556
lon: -97.60861111
History. The area around the Iowa Great Lakes was not known for permanent settlement by the Sioux but rather for recreation or hunting. When settlers arrived around 1856 it led to conflicts and eventually the Spirit Lake Massacre in 1857. After the massacre, European settlers slowly returned and by 1900 nearly 8,000 people were living in the area.

Geographic entities mentioned:
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 47.94
lon: -116.9
surface_form: spirit
instance_of: Lake
countries: United States
coordinates: lat: 46.273055555556
lon: -122.135
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4739
lon: -95.1018
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 45.38055556
lon: -90.13694444
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 44.49305556
lon: -97.60861111
Geography. The Iowa Great Lakes region was formed 13,500 years ago along the southwest edge of the Des Moines lobe ice sheet as it pressed south into Iowa. The deepest part of the lake is in West Okoboji Lake. The Iowa Great Lakes lie within the Spirit Lake Micropolitan Area and the towns of Spirit Lake and Milford are within the lake area.

Geographic entities mentioned:
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 47.94
lon: -116.9
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 47.94
lon: -116.9
surface_form: spirit
instance_of: Lake
countries: United States
coordinates: lat: 46.273055555556
lon: -122.135
surface_form: spirit
instance_of: Lake
countries: United States
coordinates: lat: 46.273055555556
lon: -122.135
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4739
lon: -95.1018
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4739
lon: -95.1018
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 45.38055556
lon: -90.13694444
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 45.38055556
lon: -90.13694444
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 44.49305556
lon: -97.60861111
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 44.49305556
lon: -97.60861111
Geography. The Iowa Great Lakes region was formed 13,500 years ago along the southwest edge of the Des Moines lobe ice sheet as it pressed south into Iowa. The deepest part of the lake is in West Okoboji Lake. The Iowa Great Lakes lie within the Spirit Lake Micropolitan Area and the towns of Spirit Lake and Milford are within the lake area.

Geographic entities mentioned:
surface_form: west okoboji lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3844
lon: -95.1594
Iowa Great Lakes. The Iowa Great Lakes, often referred to as &quot;Okoboji&quot;, is a group of natural lakes in northwestern Iowa in the United States. There are seven lakes in the region totaling with the three principal lakes of the group being Big Spirit Lake, West Okoboji Lake, and East Okoboji Lake. They are the largest natural lakes in the state of Iowa.

Geographic entities mentioned:
surface_form: iowa great lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 43.3851
lon: -95.108
The lake area extends to the north into Jackson County, Minnesota. The headwaters of Little Sioux River flow past the west side of the lake area. History. The area around the Iowa Great Lakes was not known for permanent settlement by the Sioux but rather for recreation or hunting. When settlers arrived around 1856 it led to conflicts and eventually the Spirit Lake Massacre in 1857.

Geographic entities mentioned:
surface_form: iowa great lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 43.3851
lon: -95.108
After the massacre, European settlers slowly returned and by 1900 nearly 8,000 people were living in the area. The Iowa Great Lakes Sanitary District was created in 1939 to protect the lakes from pollution and sanitary issues. Likewise, the Iowa Great Lakes Association was formed in 2008 when the waters were threatened by a large commercial agricultural development. Geography.

Geographic entities mentioned:
surface_form: iowa great lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 43.3851
lon: -95.108
From Gordonvale, the river flows east by south and then south, eventually emptying into the Coral Sea south at the southern extremity of the Yarrabah Hills range, where it meets the Russell River. The Trinity Inlet was once the river mouth of the Mulgrave River.

Geographic entities mentioned:
surface_form: Trinity Inlet
instance_of: Body of water
countries: Australia
coordinates: lat: -16.92
lon: 145.784
Language. &quot;Yidinji&quot; (also known as &quot;Yidinj&quot;, &quot;Yidiny&quot;, and &quot;Idindji&quot;) is an Australian Aboriginal language. Its traditional language region is within the local government areas of Cairns Region and Tablelands Region, in such localities as Cairns, Gordonvale, and the Mulgrave River, and the southern part of the Atherton Tableland including Atherton and Kairi.

Geographic entities mentioned:
surface_form: Atherton Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
MTV highlighted the lyrics; &quot;but this pimp is at the top of Mount Olympus / Ready for the world's games / This is my Olympics / We make 'em say 'ho' cause the game is so pimpish / Choke a 'South Park' writer with a fish stick.&quot; The last line is a reference to the &quot;South Park&quot; episode &quot;Fishsticks&quot; which parodied West.

Geographic entities mentioned:
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
Ringebu Stave Church. Ringebu Stave Church () is a parish church of the Church of Norway in Ringebu Municipality in Innlandet county, Norway. It is located in the village of Ringebu in the Gudbrandsdalen valley. It is the church for the Ringebu parish which is part of the Sør-Gudbrandsdal prosti (deanery) in the Diocese of Hamar.

Geographic entities mentioned:
surface_form: Gudbrandsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.1333
lon: 10.35
Jacob Mata. Jacob Mata Tangwata is a Vanuatuan politician and a member of the Parliament of Vanuatu from Ambae as a member of Nagriamel.

Geographic entities mentioned:
surface_form: Ambae
instance_of: Mountain
countries: Vanuatu
coordinates: lat: -15.4
lon: 167.83333333333
Bortolo Belotti. Bortolo Belotti (26 August 1877 – 24 July 1944) was an Italian politician of the first half of 20th century. Life. Born in Zogno, son of a wealthy family, he studied law at the University of Pavia and then became a lawyer. In 1907, he joined the Italian Liberal Party and in 1913 he was elected to the Chamber of Deputies for the constituency of his native Val Brembana.

Geographic entities mentioned:
surface_form: Val Brembana
instance_of: Valley
countries: Italy
coordinates: lat: 45.8725
lon: 9.651944444444444
Le Bouveret. Le Bouveret () is a village in the commune of Port-Valais in the Swiss canton of Valais. Situated at the southernmost end of Lake Geneva and close to the French border, Le Bouveret is very much tourism-oriented with several amusement attractions, including the Swiss Vapeur Parc and the waterpark Aquaparc. Le Bouveret is also the seat of Cesar Ritz Colleges, a.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Pryor Glacier. Pryor Glacier () is a glacier flowing northeastward, to the north of Mount Shields and Yermak Point, into Rennick Bay. The feature is about long and forms a physical separation between Wilson Hills and Usarp Mountains. Discovery and naming. Mapped by United States Geological Survey (USGS) from surveys and United States Navy aerial photographs, 1960–62.

Geographic entities mentioned:
surface_form: Mount Shields
instance_of: Mountain
coordinates: lat: -70.1833333
lon: 159.9333333
Exchange Scientist at the Soviet Mirny Station (1962). Location. The Pryor Glacier originates in the west between the Wilson Hills and the Usarp Mountains and flows north-northeast to enter Rennick Bay to the north of Yermak Point. It passes Wagner Spur and Mount Send to the north. Past Mount Shields it is joined from the southwest by Robilliard Glacier.

Geographic entities mentioned:
surface_form: Mount Send
instance_of: Mountain
coordinates: lat: -70.0333
lon: 159.817
It passes Wagner Spur and Mount Send to the north. Past Mount Shields it is joined from the southwest by Robilliard Glacier. Svendsen Glacier and Robilliard Glacier feed the Kooperatsiya Ice Piedmont, which joins Pryor Glacier from the south just before its mouth.

Geographic entities mentioned:
surface_form: Mount Shields
instance_of: Mountain
coordinates: lat: -70.1833333
lon: 159.9333333
Svendsen Glacier and Robilliard Glacier feed the Kooperatsiya Ice Piedmont, which joins Pryor Glacier from the south just before its mouth. Features along the Svendsen Glacier and Robilliard Glacier include Mount Simmonds, Mount Theaker, Mount Harrison, McCain Bluff, Mount Gillmor and Lenfant Bluff, all in the Usarp Mountains. Wagner Spur.

Geographic entities mentioned:
surface_form: Mount Simmonds
instance_of: Mountain
coordinates: lat: -70.33333
lon: 159.56667
surface_form: Mount Theaker
instance_of: Mountain
coordinates: lat: -70.3
lon: 159.63333
surface_form: Mount Gillmor
instance_of: Mountain
coordinates: lat: -70.466666666667
lon: 159.76666666667
After the British took control of the region, the name &quot;Assam&quot; was extended to the province that was then much larger than the Ahom kingdom. It then included, Garo Hills and Lushai Hills (Mizoram). Since that time, the boundaries of Assam have been repeatedly redrawn, though the name &quot;Assam&quot; remained.

Geographic entities mentioned:
surface_form: Garo Hills
instance_of: Mountain
countries: India
coordinates: lat: 25.5
lon: 90.33333333333333
surface_form: Lushai Hills
instance_of: Mountain
countries: India
coordinates: lat: 23.166666666667
lon: 92.833333333333
Nant Glas. Nant Glas (or Nant-glas) is a village in the Elan Valley near Rhayader and Llandrindod Wells in Powys, Wales. It is on a side road between the A44 to the northeast and the A470 to the southwest. There is a small chapel at the southern end of the village. The Willow Globe Theatre is close to the village, to the south just off the A470.

Geographic entities mentioned:
surface_form: Elan Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 52.262222222222
lon: -3.5886111111111
It is the third-highest peak in the Hayes Range, a subset of the Alaska Range. This remote peak is situated east-southeast of Mount Hayes, and southeast of Fairbanks. Mount Moffit, the nearest higher neighbor, is set to the northeast, and McGinnis Peak is positioned to the east. This rarely climbed mountain has three large sweeping faces, the East, West, and South.

Geographic entities mentioned:
surface_form: Mount Hayes
instance_of: Mountain
countries: United States
coordinates: lat: 63.6208
lon: -146.715
surface_form: hayes
instance_of: Mountain
countries: United States
coordinates: lat: 61.6403
lon: -152.411
It is the third-highest peak in the Hayes Range, a subset of the Alaska Range. This remote peak is situated east-southeast of Mount Hayes, and southeast of Fairbanks. Mount Moffit, the nearest higher neighbor, is set to the northeast, and McGinnis Peak is positioned to the east. This rarely climbed mountain has three large sweeping faces, the East, West, and South.

Geographic entities mentioned:
surface_form: Mount Moffit
instance_of: Mountain
countries: United States
coordinates: lat: 63.5683
lon: -146.399
surface_form: mcginnis peak
instance_of: Mountain
countries: United States
coordinates: lat: 63.54472222222222
lon: -146.3038888888889
Mount Shand. Mount Shand is a elevation glaciated summit located at the head of the Trident Glacier in the eastern Alaska Range, in Alaska, United States. It is the third-highest peak in the Hayes Range, a subset of the Alaska Range. This remote peak is situated east-southeast of Mount Hayes, and southeast of Fairbanks.

Geographic entities mentioned:
surface_form: hayes
instance_of: Mountain
countries: United States
coordinates: lat: 61.6403
lon: -152.411
This mountain is named for William Shand Jr. (1918–1946), a mountaineer who made the first ascents of nearby Mount Moffit in August 1942, and Mount Hayes on August 1, 1941. Following Shand's untimely death in a tragic car crash, Bradford Washburn, also of the Hayes first ascent party, proposed this name in 1949 to be applied to what is now called Mount Moffit.

Geographic entities mentioned:
surface_form: hayes
instance_of: Mountain
countries: United States
coordinates: lat: 61.6403
lon: -152.411
surface_form: mount moffit
instance_of: Mountain
countries: United States
coordinates: lat: 63.5683
lon: -146.399
surface_form: mount hayes
instance_of: Mountain
countries: United States
coordinates: lat: 63.6208
lon: -146.715
(1918–1946), a mountaineer who made the first ascents of nearby Mount Moffit in August 1942, and Mount Hayes on August 1, 1941. Following Shand's untimely death in a tragic car crash, Bradford Washburn, also of the Hayes first ascent party, proposed this name in 1949 to be applied to what is now called Mount Moffit. The present application of the name was suggested in 1961 by the U.S.

Geographic entities mentioned:
surface_form: hayes
instance_of: Mountain
countries: United States
coordinates: lat: 61.6403
lon: -152.411
surface_form: mount moffit
instance_of: Mountain
countries: United States
coordinates: lat: 63.5683
lon: -146.399
Mount Shand. Mount Shand is a elevation glaciated summit located at the head of the Trident Glacier in the eastern Alaska Range, in Alaska, United States. It is the third-highest peak in the Hayes Range, a subset of the Alaska Range. This remote peak is situated east-southeast of Mount Hayes, and southeast of Fairbanks.

Geographic entities mentioned:
surface_form: mount shand
instance_of: Mountain
countries: United States
coordinates: lat: 63.54416666666666
lon: -146.45027777777776
Board on Geographic Names. Climate. Based on the Köppen climate classification, Mount Shand is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. This climate supports the Trident and Black Rapids Glaciers surrounding this peak. Temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: mount shand
instance_of: Mountain
countries: United States
coordinates: lat: 63.54416666666666
lon: -146.45027777777776
He may have immigrated to India from Tabriz, but it is also possible that he inherited his &quot;nisba&quot; from ancestors of his who had migrated from Tabriz to India in the past. He settled in the Deccan region of the Indian subcontinent and served in the court of Abdullah Qutb Shah for some time. Muhammad Husayn completed his dictionary in 1651–1652. Content.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Urubamba, Peru. Urubamba (possibly from in the Quechua spelling &quot;Urupampa&quot;, flat land of spiders) is a small town in Peru, located near the Urubamba River under the snow-capped mountain Chicón. It is the capital of the district of the same name. Located one hour from Cusco, Urubamba is the largest town in the Sacred Valley of the Incas.

Geographic entities mentioned:
surface_form: Chicón
instance_of: Mountain
countries: Peru
coordinates: lat: -13.23666667
lon: -72.05611111
It is the capital of the district of the same name. Located one hour from Cusco, Urubamba is the largest town in the Sacred Valley of the Incas. It is also located near a number of significant ruins of the Inca Empire, including Machu Picchu. The sparse remains of the Inca palace, Quispiguanca, are within the town. Tourists often come through the town on their way to visit these sites. Geography.

Geographic entities mentioned:
surface_form: Sacred Valley
instance_of: Valley
countries: Peru
coordinates: lat: -13.333333333333
lon: -72.083333333333
Today the resort manages Gibson Pass Ski Area. The resort was operated by the Provincial Government (along with other Ski Resorts in the Province) until 1986, when it and other then-provincially operated hills including Cypress Bowl and Mount Seymour transferred to private operation. A fifty year land use permit was granted for private operations.

Geographic entities mentioned:
surface_form: Mount Seymour
instance_of: Mountain
countries: Canada
coordinates: lat: 49.393333333333
lon: -122.94444444444
Recreation. The park has a wide range of walking and hiking trails which range anywhere from a 15-minute walk to a 5 or 6 day hike. Lightning Lake is often used for non-motorized watersports, such as canoeing, kayaking, and fishing. Rentals are available at the lake for canoes, rowboats, kayaks and stand-up paddle boards.

Geographic entities mentioned:
surface_form: Lightning Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.0621
lon: -120.829
It is threatened by habitat loss. It is locally common in primary montane rain forest, aka cloud forest or mossy forest, on exposed ridges from 1,000 to 2,200 meters elevation, including Mount Dulit, Bukit Lawi, Bukit Skelap, Gunung Mulu, and Gunung Murud. It appears to be confined to ultrabasic soils.

Geographic entities mentioned:
surface_form: Mount Dulit
instance_of: Mountain
countries: Malaysia
coordinates: lat: 3.33333333
lon: 114.15
Surrounding features. The snowfield is bordered by the Skinner Saddle to the east. Surrounding mountains clockwise from the southeast are Mount Liard, Mount Stewart, Mount Durnford, Mount Field, Mount Hubble. Mount Liard. A peak east of Mount Durnford. It rises to on the ridge south of Cooper Snowfield. The peak was named by the Advisory Committee on Antarctic Names after Theodore J. Liard, Jr.

Geographic entities mentioned:
surface_form: Skinner Saddle
instance_of: Landform
coordinates: lat: -80.9667
lon: 159.417
Cooper Snowfield. Cooper Snowfield () is a snowfield with an area of about in the Churchill Mountains of Antarctica. Location. The snowfield rises to over and is nearly encircled by ridges connecting Mount Field, Mount Durnford, and Mount Liard. It was named after Alan K.

Geographic entities mentioned:
surface_form: mount field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
Surrounding features. The snowfield is bordered by the Skinner Saddle to the east. Surrounding mountains clockwise from the southeast are Mount Liard, Mount Stewart, Mount Durnford, Mount Field, Mount Hubble. Mount Liard. A peak east of Mount Durnford. It rises to on the ridge south of Cooper Snowfield. The peak was named by the Advisory Committee on Antarctic Names after Theodore J. Liard, Jr.

Geographic entities mentioned:
surface_form: mount field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
Named in honor of Ian Stewart, a retired diplomat, who was also the Whaling Commissioner for 12 years before John Scott and Jim McLay, setting the groundwork in place. Mount Durnford. A mountain, high, standing southeast of Mount Field. Discovered and named &quot;Durnford Bluff by the BrNAE (1901-04), for Admiral Sir John Durnford, a Junior Naval Lord who was of assistance to the expedition.

Geographic entities mentioned:
surface_form: mount field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
Mount Hubble. A mountain rising to between Mount Field and Mount Dick. It was named after American astronomer Edwin Hubble of the Carnegie Institution of Washington's Mount Wilson Observatory, 1919–53; in 1923 he furnished the first certain evidence that extragalactic nebulae were situated far outside the boundaries of our own galaxy, in fact were independent stellar systems. Northern peaks.

Geographic entities mentioned:
surface_form: mount field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
Northern peaks. To the north of Mount Field and Mount Hubble are Mount Egerton, East Egerton, Mount Dick and Prior Cliff
Mount Egerton. A mountain, high, rising north-north-west of Mount Field. Discovered by the BrNAE (1901-04) and named for Admiral Sir George Le Clerc Egerton, a member of the Arctic Expedition of 1875-76, one of Scott's advisors for this expedition. East Egerton.

Geographic entities mentioned:
surface_form: mount field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: mount egerton
instance_of: Mountain
coordinates: lat: -80.83333
lon: 157.91667
surface_form: mount egerton
instance_of: Mountain
coordinates: lat: -80.83333
lon: 157.91667
surface_form: egerton
instance_of: Mountain
coordinates: lat: -80.83333
lon: 157.91667
surface_form: egerton
instance_of: Mountain
coordinates: lat: -80.83333
lon: 157.91667
surface_form: egerton
instance_of: Mountain
coordinates: lat: -80.83333
lon: 157.91667
Northern peaks. To the north of Mount Field and Mount Hubble are Mount Egerton, East Egerton, Mount Dick and Prior Cliff
Mount Egerton. A mountain, high, rising north-north-west of Mount Field. Discovered by the BrNAE (1901-04) and named for Admiral Sir George Le Clerc Egerton, a member of the Arctic Expedition of 1875-76, one of Scott's advisors for this expedition. East Egerton.

Geographic entities mentioned:
surface_form: mount field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
Discovered and named &quot;Durnford Bluff by the BrNAE (1901-04), for Admiral Sir John Durnford, a Junior Naval Lord who was of assistance to the expedition. The NZGSAE (1960-61) remapped the feature and amended the name to Mount Durnford. Not: Durnford Bluff. Mount Field. A mountain, high, standing south-south-east of Mount Egerton. Discovered and named by the BrNAE, 1901-04, under Scott.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
The NZGSAE (1960-61) remapped the feature and amended the name to Mount Durnford. Not: Durnford Bluff. Mount Field. A mountain, high, standing south-south-east of Mount Egerton. Discovered and named by the BrNAE, 1901-04, under Scott. Mount Hubble. A mountain rising to between Mount Field and Mount Dick.

Geographic entities mentioned:
surface_form: mount egerton
instance_of: Mountain
coordinates: lat: -80.83333
lon: 157.91667
surface_form: egerton
instance_of: Mountain
coordinates: lat: -80.83333
lon: 157.91667
A mountain, high, rising north-north-west of Mount Field. Discovered by the BrNAE (1901-04) and named for Admiral Sir George Le Clerc Egerton, a member of the Arctic Expedition of 1875-76, one of Scott's advisors for this expedition. East Egerton. A prominent peak, high, rising east of Mount Egerton. Mapped by the NZGSAE (1960-61) and named in association with Mount Egerton. Mount Dick.

Geographic entities mentioned:
surface_form: mount egerton
instance_of: Mountain
coordinates: lat: -80.83333
lon: 157.91667
surface_form: egerton
instance_of: Mountain
coordinates: lat: -80.83333
lon: 157.91667
Discovered by the BrNAE (1901-04) and named for Admiral Sir George Le Clerc Egerton, a member of the Arctic Expedition of 1875-76, one of Scott's advisors for this expedition. East Egerton. A prominent peak, high, rising east of Mount Egerton. Mapped by the NZGSAE (1960-61) and named in association with Mount Egerton. Mount Dick. A prominent peak, high, standing east of Mount Egerton.

Geographic entities mentioned:
surface_form: mount egerton
instance_of: Mountain
coordinates: lat: -80.83333
lon: 157.91667
surface_form: egerton
instance_of: Mountain
coordinates: lat: -80.83333
lon: 157.91667
East Egerton. A prominent peak, high, rising east of Mount Egerton. Mapped by the NZGSAE (1960-61) and named in association with Mount Egerton. Mount Dick. A prominent peak, high, standing east of Mount Egerton. Named by the NZGSAE (1960-61) for R.G. Dick, Surveyor General of New Zealand. Prior Cliff. A cliff between extending east north east from Mount Dick.

Geographic entities mentioned:
surface_form: mount egerton
instance_of: Mountain
coordinates: lat: -80.83333
lon: 157.91667
surface_form: egerton
instance_of: Mountain
coordinates: lat: -80.83333
lon: 157.91667
Northern peaks. To the north of Mount Field and Mount Hubble are Mount Egerton, East Egerton, Mount Dick and Prior Cliff
Mount Egerton. A mountain, high, rising north-north-west of Mount Field. Discovered by the BrNAE (1901-04) and named for Admiral Sir George Le Clerc Egerton, a member of the Arctic Expedition of 1875-76, one of Scott's advisors for this expedition. East Egerton.

Geographic entities mentioned:
surface_form: egerton
instance_of: Mountain
coordinates: lat: -80.83333
lon: 157.91667
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
surface_form: george
instance_of: Mountain
coordinates: lat: -67.71667
lon: 50
A mountain, high, rising north-north-west of Mount Field. Discovered by the BrNAE (1901-04) and named for Admiral Sir George Le Clerc Egerton, a member of the Arctic Expedition of 1875-76, one of Scott's advisors for this expedition. East Egerton. A prominent peak, high, rising east of Mount Egerton. Mapped by the NZGSAE (1960-61) and named in association with Mount Egerton. Mount Dick.

Geographic entities mentioned:
surface_form: egerton
instance_of: Mountain
coordinates: lat: -80.83333
lon: 157.91667
Mount Hubble. A mountain rising to between Mount Field and Mount Dick. It was named after American astronomer Edwin Hubble of the Carnegie Institution of Washington's Mount Wilson Observatory, 1919–53; in 1923 he furnished the first certain evidence that extragalactic nebulae were situated far outside the boundaries of our own galaxy, in fact were independent stellar systems. Northern peaks.

Geographic entities mentioned:
surface_form: wilson
instance_of: Mountain
coordinates: lat: -68.45
lon: -65.55
surface_form: mount wilson
instance_of: Mountain
coordinates: lat: -68.45
lon: -65.55
It was named after Alan K. Cooper, a marine geophysicist with the United States Geological Survey, Menlo Park, California, who was involved in drilling and seismic studies of the Antarctic continental margin for deriving paleoenvironments and ice sheet history, 1984–2002. Surrounding features. The snowfield is bordered by the Skinner Saddle to the east.

Geographic entities mentioned:
surface_form: park
instance_of: Mountain
coordinates: lat: -67.2333
lon: 51
Mount Stewart. A mountain rising to, located mid way between Mount Durnford and Mount Liard. Named in honor of Ian Stewart, a retired diplomat, who was also the Whaling Commissioner for 12 years before John Scott and Jim McLay, setting the groundwork in place. Mount Durnford. A mountain, high, standing southeast of Mount Field.

Geographic entities mentioned:
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
The NZGSAE (1960-61) remapped the feature and amended the name to Mount Durnford. Not: Durnford Bluff. Mount Field. A mountain, high, standing south-south-east of Mount Egerton. Discovered and named by the BrNAE, 1901-04, under Scott. Mount Hubble. A mountain rising to between Mount Field and Mount Dick.

Geographic entities mentioned:
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
Cooper Snowfield. Cooper Snowfield () is a snowfield with an area of about in the Churchill Mountains of Antarctica. Location. The snowfield rises to over and is nearly encircled by ridges connecting Mount Field, Mount Durnford, and Mount Liard. It was named after Alan K.

Geographic entities mentioned:
surface_form: cooper snowfield
instance_of: Landform
coordinates: lat: -80.9333
lon: 158.667
Surrounding features. The snowfield is bordered by the Skinner Saddle to the east. Surrounding mountains clockwise from the southeast are Mount Liard, Mount Stewart, Mount Durnford, Mount Field, Mount Hubble. Mount Liard. A peak east of Mount Durnford. It rises to on the ridge south of Cooper Snowfield. The peak was named by the Advisory Committee on Antarctic Names after Theodore J. Liard, Jr.

Geographic entities mentioned:
surface_form: cooper snowfield
instance_of: Landform
coordinates: lat: -80.9333
lon: 158.667
Mount Liard. A peak east of Mount Durnford. It rises to on the ridge south of Cooper Snowfield. The peak was named by the Advisory Committee on Antarctic Names after Theodore J. Liard, Jr. (1918–2002), a geographer with the Department of Interior and the Department of Defense in toponymic research for the U.S. Board on Geographic Names, 1949–80.

Geographic entities mentioned:
surface_form: theodore
instance_of: Mountain
coordinates: lat: -64.96666667
lon: -62.6
Berill Mountain. Berill (Russian: &quot;Берилл&quot;) is a peak in the Suntar-Khayata Range. The elevation above sea level of the mountain is 2,933 m. It is the highest point of Khabarovsk Krai.

Geographic entities mentioned:
surface_form: berill mountain
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 62.395833333333
lon: 141.32666666667
Berill Mountain. Berill (Russian: &quot;Берилл&quot;) is a peak in the Suntar-Khayata Range. The elevation above sea level of the mountain is 2,933 m. It is the highest point of Khabarovsk Krai.

Geographic entities mentioned:
surface_form: berill
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 62.395833333333
lon: 141.32666666667
surface_form: берилл
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 62.395833333333
lon: 141.32666666667
Free lunches are provided weekdays. The Sand Springs Cultural and Historical Museum is located in the historic art-deco Page Memorial Library Building, and promotes cultural heritage and the arts. Keystone State Park and Keystone Lake are immediately to the west of town. Skiatook Lake is immediately to the north of town. Transportation.

Geographic entities mentioned:
surface_form: Keystone Lake
instance_of: Lake
countries: United States
coordinates: lat: 36.2306
lon: -96.305
The Sand Springs Cultural and Historical Museum is located in the historic art-deco Page Memorial Library Building, and promotes cultural heritage and the arts. Keystone State Park and Keystone Lake are immediately to the west of town. Skiatook Lake is immediately to the north of town. Transportation. US Route 412 and Oklahoma State Highway 51 are the major east–west highways through town.

Geographic entities mentioned:
surface_form: Skiatook Lake
instance_of: Lake
countries: United States
coordinates: lat: 36.351388888889
lon: -96.091944444444
Topographic relief is significant as the summit rises above Parleys Canyon in 1.25 mile (2 km) and above Millcreek Canyon in one mile (1.6 km). The peak is prominent on the Wasatch skyline, and it is the most accessible as well as easiest climb of the major peaks rising above the Salt Lake Valley.

Geographic entities mentioned:
surface_form: Salt Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.6839
lon: -111.978
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2767785
lon: -98.6946248
surface_form: lake valley
instance_of: Valley
countries: United States
coordinates: lat: 38.3189
lon: -114.607
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 44.965
lon: -96.443611111111
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.635555555556
lon: -99.9175
The peak is part of the Wasatch Range, which is a subset of the Rocky Mountains. Precipitation runoff from the mountain's north slope drains to Parleys Creek, whereas the south slope drains to Mill Creek. Topographic relief is significant as the summit rises above Parleys Canyon in 1.25 mile (2 km) and above Millcreek Canyon in one mile (1.6 km).

Geographic entities mentioned:
surface_form: mill creek
instance_of: Watercourse
countries: United States
coordinates: lat: 44.4599675
lon: -89.6412311
surface_form: mill creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.871442
lon: -90.093448
Grandeur Peak. Grandeur Peak is an mountain summit in the Wasatch Range in Salt Lake County, Utah, United States. Description. Grandeur Peak is located southeast of downtown Salt Lake City on land managed by Uinta-Wasatch-Cache National Foreste. The peak is part of the Wasatch Range, which is a subset of the Rocky Mountains.

Geographic entities mentioned:
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2767785
lon: -98.6946248
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 44.965
lon: -96.443611111111
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.635555555556
lon: -99.9175
surface_form: grandeur peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.707222222222
lon: -111.75972222222
The peak is prominent on the Wasatch skyline, and it is the most accessible as well as easiest climb of the major peaks rising above the Salt Lake Valley. Reaching the top involves 3.4 miles of trail hiking with 2,300 feet of elevation gain, and the summit provides excellent views of Salt Lake City. This mountain's toponym has been officially adopted by the United States Board on Geographic Names.

Geographic entities mentioned:
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2767785
lon: -98.6946248
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 44.965
lon: -96.443611111111
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.635555555556
lon: -99.9175
Grandeur Peak. Grandeur Peak is an mountain summit in the Wasatch Range in Salt Lake County, Utah, United States. Description. Grandeur Peak is located southeast of downtown Salt Lake City on land managed by Uinta-Wasatch-Cache National Foreste. The peak is part of the Wasatch Range, which is a subset of the Rocky Mountains.

Geographic entities mentioned:
surface_form: grandeur peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.707222222222
lon: -111.75972222222
These rocks were formed about 960 million years ago at a depth of about as a molten mass within older metamorphosed sedimentary rocks. Glacial erratic boulders of light-colored granitic gneiss cover the lower slopes of Mount Henderson, the David Range and Mount Hordern, but are not found more than about above the present-day ice surface. Above this level the darker charnockite bedrock is exposed.

Geographic entities mentioned:
surface_form: Mount Hordern
instance_of: Mountain
coordinates: lat: -67.9333
lon: 62.4833
The charnockite contains regions up to wide of the older metamorphosed sedimentary rock, one of which includes most of the Casey Range. Painted Peak in the North Masson Range is an example, composed of rocks that were metamorphosed and deformed 1200 to 1000 million years ago. They include interlayered, metamorphosed arkose, metapelite, calcsilicates and granitic gneiss.

Geographic entities mentioned:
surface_form: Painted Peak
instance_of: Mountain
coordinates: lat: -67.75
lon: 62.85
During the last glacial cycle the ice sheet thickened more near the coast, less further inland. This is shown by the upper limit of glacial erratic boulders, ranging from on Fang Peak near the sea in the north of David Range, to on Mount Hordern, which is about from the sea. The ice surface appears have lowered by several hundred meters during the present interglacial.

Geographic entities mentioned:
surface_form: Fang Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4644
lon: -125.987
surface_form: Mount Hordern
instance_of: Mountain
coordinates: lat: -67.9333
lon: 62.4833
The ice surface appears have lowered by several hundred meters during the present interglacial. ANARE conducted glaciological surveys in the late 1950s between Fischer Nunatak and the Casey Range, where they found that the ice was about thick, and flowed at a rate of per year.

Geographic entities mentioned:
surface_form: Fischer Nunatak
instance_of: Mountain
coordinates: lat: -67.7333
lon: 63.05
Features. The Framnes Mountains consist of Casey Range, Masson Range, David Range, and Brown Range, and adjacent peaks and mountains. The east of the Framnes Mountains, from north to south, contains the Mount Henderson massif, Masson Range, Trilling Peaks and Shark Peak. The central section from north to south holds the David Range, Butler Nunataks and Brown Range.

Geographic entities mentioned:
surface_form: Trilling Peaks
instance_of: Mountain
coordinates: lat: -67.9667
lon: 62.75
Not: Trillingnutane. Shark Peak. . An isolated nunatak south-southwest of Van Hulssen Nunatak in the Framnes Mountains. Mapped by Norwegian cartographers from air photos taken by the Lars Christensen Expedition, 1936–37, and named Hånuten (the shark peak). The translated form of the name recommended by ANCA has been adopted. David Range. .

Geographic entities mentioned:
surface_form: Van Hulssen Nunatak
instance_of: Mountain
coordinates: lat: -67.9833
lon: 62.75
Butler, senior diesel mechanic at Mawson Station in 1967. Sørtindane Peaks or Brown Range. . A group of peaks just south of Mount Twintop at the south end of the David Range, Framnes Mountains. Mapped by Norwegian cartographers from air photos taken by the Lars Christensen Expedition (1936–37) and named Sortindane (the southern peaks). Not: Brown Range, Gory Sørtindane. Casey Range. .

Geographic entities mentioned:
surface_form: Mount Twintop
instance_of: Mountain
coordinates: lat: -68.0833
lon: 62.3667
These verses are the earliest known artifacts to be found in the Hebrew Bible text. Numbers begins at Mount Sinai, where the Israelites have received their laws and covenant from God and God has taken up residence among them in the sanctuary. The task before them is to take possession of the Promised Land. The people are counted and preparations are made for resuming their march.

Geographic entities mentioned:
surface_form: Mount Sinai
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.5384
lon: 33.9752
Most commentators divide Numbers into three sections based on locale (Mount Sinai, Kadesh-Barnea and the plains of Moab), linked by two travel sections; an alternative is to see it as structured around the two generations of those condemned to die in the wilderness and the new generation who will enter Canaan, making a theological distinction between the disobedience of the first generation and the obedience of the second.

Geographic entities mentioned:
surface_form: Mount Sinai
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.5384
lon: 33.9752
The landform is attached at the southwest to the Vishnu Temple massif, about 1.0 mi distant. Krishna Shrine is about 3.0 mi south of the Cape Royal overlook, Walhalla Plateau (southeast Kaibab Plateau, North Rim). A twin landform occupies the southeast of Vishnu Temple, the Rama Shrine. Krishna Shrine towers about 4,000 ft above the Colorado River, about 2.0 miles south.

Geographic entities mentioned:
surface_form: Kaibab Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36.1267
lon: -112.009
First, his headquarters received reports that Soviet forces held a bridgehead over the Oder River, from Berlin. Since the Allied armies on the Rhine were more than from Berlin, with the Elbe River, ahead, still to be crossed it seemed clear that the Soviets would capture Berlin long before the Western Allies could reach it.

Geographic entities mentioned:
surface_form: Elbe River
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Discontinuous belts that contain pyrrhotite are present in the western United States along the Sierra Nevada mountain range and Cascade Range extending into the northwestern United States. Pyrrhotite may also be found west and south of Lake Superior. Etymology and history. Named in 1847 by Ours-Pierre-Armand Petit-Dufrénoy.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
After climbing Yorkshire's gritstone, MacIntyre travelled to Scotland to develop his ice climbing technique and understanding of winter climbing conditions. On 14 March 1975, he made a solo ascent of two of the test pieces on Ben Nevis – &quot;Zero Gully&quot; and &quot;Point Five&quot;.

Geographic entities mentioned:
surface_form: Ben Nevis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.796891
lon: -5.003675
During this period, MacIntyre and his climbing partners ascended the Grandes Jorasses giant ice sheet, &quot;The Shroud&quot;, in a single day, and also accomplished the first non-sieged ascent of the &quot;Harlin Direct&quot; on the Eiger North Face. Climbing in the Himalaya.

Geographic entities mentioned:
surface_form: Grandes Jorasses
instance_of: Mountain
countries: Italy
France
coordinates: lat: 45.866666666667
lon: 6.9833333333333
surface_form: Eiger
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.577607529
lon: 8.005286822
Climbing in the Himalaya. MacIntyre later climbed in the Himalaya where he was a proponent of 'Alpine Style' ethics, along with a number of other climbers, including Voytek Kurtyka. He climbed with a number of international groups, whose ascents included attempts on major objectives such as Dhaulagiri, Changabang, Shishapangma and Makalu. Death.

Geographic entities mentioned:
surface_form: Dhaulagiri
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.696666666666665
lon: 83.49
surface_form: Changabang
instance_of: Mountain
countries: India
coordinates: lat: 30.483333333333
lon: 80.016666666667
surface_form: Shishapangma
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 28.352222222222
lon: 85.779722222222
surface_form: Makalu
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.889166666667
lon: 87.088611111111
He climbed with a number of international groups, whose ascents included attempts on major objectives such as Dhaulagiri, Changabang, Shishapangma and Makalu. Death. In the autumn of 1982, at the age of 28, MacIntyre was killed by a single stone while setting up a new route on Annapurna's South Face with French alpinist René Ghilini.

Geographic entities mentioned:
surface_form: Annapurna
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.5958
lon: 83.82
It is the high point of a ring of mountains, known as the Cruachan Horseshoe, that surrounds the power station reservoir. The horseshoe includes a further Munro (Stob Diamh), a Corbett (Beinn a' Bhuiridh), and several subsidiary summits. &quot;Cruachan!&quot; is the battle cry of Highland clans Campbell and MacIntyre.

Geographic entities mentioned:
surface_form: Beinn a' Bhuiridh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.408357
lon: -5.0907986
Ben Cruachan. Ben Cruachan () is a mountain that rises to, the highest in Argyll and Bute, Scotland. It gives its name to the Cruachan Dam, a pumped-storage hydroelectric power station located in a cavern inside the mountain. It is the high point of a ring of mountains, known as the Cruachan Horseshoe, that surrounds the power station reservoir.

Geographic entities mentioned:
surface_form: ben cruachan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.42684
lon: -5.131834
In the speech one of Murong's generals, Yinalou, addressed him as &quot;kehan&quot; (, later); some sources suggests that Tuyuhun might also have used the title after settling at Qinghai Lake in the 3rd century. The Rouran Khaganate (330–555) was the first people to use the titles Khagan and Khan for their emperors, replacing the Chanyu of the Xiongnu, whom Grousset and others assume to be Turkic.

Geographic entities mentioned:
surface_form: Qinghai Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 37
lon: 100
After the breakdown of Mongol Empire and the fall of the Yuan dynasty in the mid-14th century, the Mongols turned into a political turmoil. Dayan Khan (1464–1517/1543) once revived the Emperor's authority and recovered its reputation on the Mongolian Plateau, but with the distribution of his empire among his sons and relatives as fiefs it again caused decentralized rule.

Geographic entities mentioned:
surface_form: Mongolian Plateau
instance_of: Plateau
countries: Mongolia
People's Republic of China
Russia
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 107
Towards the 15th century, Huarpe territory expanded into the current Argentinian provinces of San Luis, Mendoza and San Juan and even on the north of the Neuquen Province. They inhabited between the Jáchal River at north, to the Diamante River at south and between the Andes and Conlara Valley on San Luis.

Geographic entities mentioned:
surface_form: Jáchal River
instance_of: Watercourse
countries: Argentina
coordinates: lat: -30.22
lon: -68.756111111111
surface_form: Diamante River
instance_of: Watercourse
countries: Argentina
coordinates: lat: -34.511666666667
lon: -66.757777777778
Fagerfjell. Fagerfjell is a mountain in the municipality of Flesberg in Buskerud, Norway.

Geographic entities mentioned:
surface_form: fagerfjell
instance_of: Mountain
countries: Norway
coordinates: lat: 69.26666667
lon: 17.33333333
Chauvet Cave. The Chauvet-Pont-d'Arc Cave () in the Ardèche department of southeastern France is a cave that contains some of the best-preserved figurative cave paintings in the world, as well as other evidence of Upper Paleolithic life. It is located near the commune of Vallon-Pont-d'Arc on a limestone cliff above the former bed of the river Ardèche, in the Gorges de l'Ardèche.

Geographic entities mentioned:
surface_form: Gorges de l'Ardèche
instance_of: Valley
countries: France
coordinates: lat: 44.34444444
lon: 4.47694444
It is situated southwest of Invermere, and north-northeast of Kaslo, on the northern boundary of Purcell Wilderness Conservancy Provincial Park and Protected Area. Nearby peaks include Truce Mountain, to the west, Mount Earl Grey, to the northeast, and Jumbo Mountain, to the north. The first ascent of Redtop Mountain was made August 11, 1916, by Albert H.

Geographic entities mentioned:
surface_form: Truce Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.29992
lon: -116.68542
surface_form: Mount Earl Grey
instance_of: Mountain
countries: Canada
coordinates: lat: 50.33325
lon: -116.51878
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: jumbo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.403056
lon: -116.565