Sarmila/GeoWiki-Features huggingface dataset:
Castro Valnera. Castro Valnera (Spanish) or Castru Valnera (Cantabrian) is a peak located in the central area of the Cantabrian Mountains, in the border between the province of Burgos and Cantabria, northern Spain. It is around it that the whole Pas valley revolves, and also the source of the Miera River, between the Portillo de Lunada and Estacas de Trueba passes.

Geographic entities mentioned:
surface_form: castro valnera
instance_of: Mountain
countries: Spain
coordinates: lat: 43.147755555556
lon: -3.6811416666667
Castro Valnera. Castro Valnera (Spanish) or Castru Valnera (Cantabrian) is a peak located in the central area of the Cantabrian Mountains, in the border between the province of Burgos and Cantabria, northern Spain. It is around it that the whole Pas valley revolves, and also the source of the Miera River, between the Portillo de Lunada and Estacas de Trueba passes.

Geographic entities mentioned:
surface_form: castro valnera
instance_of: Mountain
countries: Spain
coordinates: lat: 43.147755555556
lon: -3.6811416666667
surface_form: castru valnera
instance_of: Mountain
countries: Spain
coordinates: lat: 43.147755555556
lon: -3.6811416666667
In 1920, Isakov was transferred and assigned to the destroyer &quot;Deyatelni&quot;, which patrolled from the Volga River down to the Caspian Sea and later shelled the positions of Allied interventionist forces in the midst of the Russian Civil War. Noted for his distinction during the battles, he was made the gun battery commander of the destroyer &quot;Izyaslav&quot; in 1921.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
In January 1965, Isakov wrote in the newspaper &quot;Nedelya&quot; that &quot;for centuries foreign enemies have tried to close for the Russian people all exits to the sea.&quot; Then he recalled, how &quot;Astrakhan's kingdom has blocked the Caspian Sea. In the Baltic the role of &quot;Cerberus&quot; was played in turn by the Livonian Knights, the Hanseatic League and later Sweden&quot;.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Isakov concluded &quot;The fortress Oreshek or Schlüsselburg has remained in the mouth of the Neva to this very day as a reminder of how afraid they were of letting the Russians out of Lake Ilmen.&quot;
On the basis of this article, Ivan Dziuba, a Ukrainian-born Soviet philologist and a staunch Leninist, criticized Isakov strongly in his book &quot;Internationalism or Russification&quot; (1968) for repeating &quot;what was written by the propagandists of tsarist times and in their falsified history textbooks,&quot; an attitude &quot;which looked on the whole surrounding world whether it was in the way of Russia or not, whether it satisfied the appetites of tsarism or not.&quot; Dziuba used Isakov as an example of how tsarist Russia was identified completely with the contemporary USSR and how Great Russian chauvinism had surpassed &quot;the Communist class approach&quot; with &quot;a pitiable Shulgin-type interpretation of the grandiose class battle of the proletariat, of the grandiose drama of universal history!&quot;
Both the Soviet Union and Armenia have issued postage stamps dedicated to Isakov.

Geographic entities mentioned:
surface_form: Lake Ilmen
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 58.266666666667
lon: 31.283333333333
The mountain is named after the settlement of Sarnegor in Southern Bulgaria. Location. Mount Sarnegor is located at, which is 4.4 km southeast of Fleming Point, 2.77 km south of Veles Bastion, 6.32 km west of Mount Imhotep, 4.7 km north by east of Mount Aciar and 5.26 km east-northeast of Devene Point. British mapping in 1980 and 2008.

Geographic entities mentioned:
surface_form: Fleming Point
instance_of: Landform
countries: United States
coordinates: lat: 37.8858
lon: -122.314
surface_form: Mount Imhotep
instance_of: Mountain
coordinates: lat: -64.35
lon: -62.4
surface_form: mount sarnegor
instance_of: Mountain
coordinates: lat: -64.35944444
lon: -62.52416667
surface_form: imhotep
instance_of: Mountain
coordinates: lat: -64.35
lon: -62.4
Mount Sarnegor. Mount Sarnegor (,) is the mostly ice-covered mountain of elevation 1189 m in Solvay Mountains on Brabant Island in the Palmer Archipelago, Antarctica. It has steep and partly ice-free southwest and northwest slopes, and surmounts Zlatiya Glacier to the north, Rush Glacier to the south and Aluzore Gap to the east-northeast.

Geographic entities mentioned:
surface_form: solvay
instance_of: Mountain
coordinates: lat: -72.5667
lon: 31.3833
surface_form: mount sarnegor
instance_of: Mountain
coordinates: lat: -64.35944444
lon: -62.52416667
It has steep and partly ice-free southwest and northwest slopes, and surmounts Zlatiya Glacier to the north, Rush Glacier to the south and Aluzore Gap to the east-northeast. A westerly offshoot of the feature forms Sidell Spur, extending to the seashore. The mountain is named after the settlement of Sarnegor in Southern Bulgaria. Location.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
Mount Sarnegor. Mount Sarnegor (,) is the mostly ice-covered mountain of elevation 1189 m in Solvay Mountains on Brabant Island in the Palmer Archipelago, Antarctica. It has steep and partly ice-free southwest and northwest slopes, and surmounts Zlatiya Glacier to the north, Rush Glacier to the south and Aluzore Gap to the east-northeast.

Geographic entities mentioned:
surface_form: mount sarnegor
instance_of: Mountain
coordinates: lat: -64.35944444
lon: -62.52416667
They prolonged the operations until 1983. After that the ownership was transferred to the private persons. The first name of the vessel was &quot;Tehi&quot; due to the one part of the southernmost Päijänne, Vesijärvi. Later the hydrofoils were taken off. Later M/S Tehi became M/S Suvi-Tuuli. M/S Tehi. M/S Tehi started its operations in 1962.

Geographic entities mentioned:
surface_form: Vesijärvi
instance_of: Lake
countries: Finland
coordinates: lat: 61.082777777778
lon: 25.538333333333
M/S Tehi. M/S Tehi started its operations in 1962. Later the M/S Tehi was renamed as M/S Suvi-Tuuli (without hydrofoils):Lake Päijänne cities of Lahti and Jyväskylä 1962–1983, Pyhäjärvi 2008, river Kokemäenjoki 2009-
M/S Rosetta. M/S Rosetta is Raketa 314, which was bought from Tartu of Estonia in 1993. From 1995 to 2005 it was operated under the name M/S Suvijet &quot;.

Geographic entities mentioned:
surface_form: Lake Päijänne
instance_of: Lake
countries: Finland
coordinates: lat: 61.583333333333
lon: 25.5
M/S Rosetta is Raketa 314, which was bought from Tartu of Estonia in 1993. From 1995 to 2005 it was operated under the name M/S Suvijet &quot;. It was bought from Estonia and has been operated in Lake Päijänne for Royal Cruises since 2005 after the second renaming as M/S Rosetta. Raketa-314 was built in Feodocija in 1963. It may not prolong the chartered trips on Lake Päijänne after its sale.

Geographic entities mentioned:
surface_form: Lake Päijänne
instance_of: Lake
countries: Finland
coordinates: lat: 61.583333333333
lon: 25.5
It was bought from Estonia and has been operated in Lake Päijänne for Royal Cruises since 2005 after the second renaming as M/S Rosetta. Raketa-314 was built in Feodocija in 1963. It may not prolong the chartered trips on Lake Päijänne after its sale. The home harbour of M/S Rosetta is in Lahti. The vessel does not have its original engine just like M/S Suvi-Tuuli does not have.

Geographic entities mentioned:
surface_form: Lake Päijänne
instance_of: Lake
countries: Finland
coordinates: lat: 61.583333333333
lon: 25.5
Initially, it was believed its lavas are not as evolved as in Compton–Belkovich Thorium Anomaly, but by 2004 the low thorium enrichment signal was attributed to small size of volcanic complex, making it composition compatible with highly processed silicic lavas. By 2013, a patchy deposits of magnesium spinel were detected in the central and western parts of the volcanic dome.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
By 2013, a patchy deposits of magnesium spinel were detected in the central and western parts of the volcanic dome. The spinel-rich areas are associated with boulder fields, and fringed by areas showing a sign of hydration, with 4-8% of mineral by weight been hydroxylated. The average bulk density of material in Mons Hansteen is extremely low, been equal only to 1500–2000 kg/m3.

Geographic entities mentioned:
surface_form: rich
instance_of: Mountain
coordinates: lat: -79.7833
lon: 158.8
Mons Hansteen. Mons Hansteen is a mountain on the Moon, also known as Hansteen Alpha (α), named after Christopher Hansteen. It is roughly triangular in shape and occupies an area about 30 km across on the western margin of Oceanus Procellarum, southeast of the crater Hansteen and north of the dark-floored crater Billy.

Geographic entities mentioned:
surface_form: mons hansteen
instance_of: Mountain
coordinates: lat: -12.19
lon: -50.21
It is thought to be an extrusion of volcanic material that is younger than the crater Hansteen, with most of surface volcanic ash been deposited 3.5-3.74 billion years ago. The Mons Hansteen belongs to rare class of non-mare moon volcanoes. Composition. The extruded material is significantly enriched in silica, and strongly depleted in iron and titanium oxides compared to surrounding mare terrain.

Geographic entities mentioned:
surface_form: mons hansteen
instance_of: Mountain
coordinates: lat: -12.19
lon: -50.21
By 2013, a patchy deposits of magnesium spinel were detected in the central and western parts of the volcanic dome. The spinel-rich areas are associated with boulder fields, and fringed by areas showing a sign of hydration, with 4-8% of mineral by weight been hydroxylated. The average bulk density of material in Mons Hansteen is extremely low, been equal only to 1500–2000 kg/m3.

Geographic entities mentioned:
surface_form: mons hansteen
instance_of: Mountain
coordinates: lat: -12.19
lon: -50.21
Egwine. Egwine was a 6th-century Celtic princess and saint, who is a patron saint of the village of Llanigon, east of Hay-on-Wye, in the Wye Valley of Wales. Very little is known of her life. She was the sister of saints Cadoc, Maches and Cyndr, who all built churches in the same area. She was also the daughter of Gwladys, and granddaughter of king Brychan of Brycheiniog.

Geographic entities mentioned:
surface_form: Wye Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69255
lon: -2.66283
It reaches a height of 1,090 m. Its extent is about 7 km × 10 km. 20 km northwest of &quot;Heioab&quot; is Mount Höchster. Several parts of the mountain range are covered with sand which is blown there by sandstorms. The average yearly rainfall in this area of the Namib amounts to just a few millimetres.

Geographic entities mentioned:
surface_form: Höchster
instance_of: Mountain
countries: Namibia
coordinates: lat: -27.3067
lon: 15.8225
surface_form: höchster
instance_of: Mountain
countries: Namibia
coordinates: lat: -27.3067
lon: 15.8225
surface_form: heioab
instance_of: Mountain
countries: Namibia
coordinates: lat: -27.4142
lon: 15.9675
Heioab. Heioab is a mountain in the Diamond Restricted Aerea, also called &quot;Sperrgebiet&quot;, in the southwestern part of Namibia. It reaches a height of 1,090 m. Its extent is about 7 km × 10 km. 20 km northwest of &quot;Heioab&quot; is Mount Höchster. Several parts of the mountain range are covered with sand which is blown there by sandstorms.

Geographic entities mentioned:
surface_form: heioab
instance_of: Mountain
countries: Namibia
coordinates: lat: -27.4142
lon: 15.9675
Velykyi Kuialnyk. The Velykyi Kuialnyk () or Bolshoy Kuyalnik () is a river in Podilsk and Berezivka Raions of Odesa Oblast, Ukraine. It flows into the Kuialnyk Estuary of the Black Sea. The river spans, with a drainage basin covering. The urban-type settlements of Shyriaieve and Ivanivka are located along its banks.

Geographic entities mentioned:
surface_form: Kuialnyk Estuary
instance_of: Lake
countries: Ukraine
coordinates: lat: 46.664444444444
lon: 30.713055555556
Shell Lake (Becker County, Minnesota). Shell Lake is a lake in Becker County, Minnesota, in the United States. Shell Lake was likely named from the shells on the lakeshore. Its name in the Ojibwe is &quot;Gaa-jiigajiwegamaag-zaaga'igan&quot; meaning &quot;'lake lying near the mountain' lake&quot;, in reference to the lake's position along the Smoky Hills complex.

Geographic entities mentioned:
surface_form: shell lake
instance_of: Lake
countries: United States
coordinates: lat: 45.734
lon: -91.9
surface_form: shell lake (becker county, minnesota)
instance_of: Lake
countries: United States
coordinates: lat: 46.94736111
lon: -95.44722222
Shell Lake (Becker County, Minnesota). Shell Lake is a lake in Becker County, Minnesota, in the United States. Shell Lake was likely named from the shells on the lakeshore. Its name in the Ojibwe is &quot;Gaa-jiigajiwegamaag-zaaga'igan&quot; meaning &quot;'lake lying near the mountain' lake&quot;, in reference to the lake's position along the Smoky Hills complex.

Geographic entities mentioned:
surface_form: shell lake
instance_of: Lake
countries: United States
coordinates: lat: 45.734
lon: -91.9
surface_form: shell lake
instance_of: Lake
countries: United States
coordinates: lat: 46.94736111
lon: -95.44722222
Venue. The arena with the most finals is Stockholm Olympic Stadium in Stockholm (50 times), Söderstadion in Stockholm (23) and Studenternas IP (17). Other venues are Rocklunda IP in Västerås, Idrottsparken in Norrköping, the bay of Brunnsviken in Stockholm, Tunavallen in Eskilstuna, Strömvallen in Gävle and Tingvalla IP in Karlstad.

Geographic entities mentioned:
surface_form: Brunnsviken
instance_of: Lake
countries: Sweden
coordinates: lat: 59.36805556
lon: 18.04
Due to the very limited depression between the two, most guidebooks follow Wainwright in counting High Crag as a part of Nethermost Pike. To the south of Dollywaggon Pike is the complex depression containing Grisedale Tarn, with Seat Sandal and Fairfield rising beyond. In common with much of the Helvellyn range there is a marked contrast between the western and eastern slopes of Dollywaggon Pike.

Geographic entities mentioned:
surface_form: Seat Sandal
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.494561111111
lon: -3.01585
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
surface_form: fairfield
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4969
lon: -2.99059
surface_form: grisedale tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.5
lon: -3.0083333333333
surface_form: seat sandal
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.494561111111
lon: -3.01585
In common with much of the Helvellyn range there is a marked contrast between the western and eastern slopes of Dollywaggon Pike. In Wainwright’s words &quot;‘To the west, uninteresting grass slopes descend to Dunmail Raise almost unrelieved by rock and scarred only by the wide stony track gouged across the breast of the fell by the boots of generations of pilgrims to Helvellyn.

Geographic entities mentioned:
surface_form: Helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
Before this diversion, Dollywaggon Pike was distinctive in that its drainage reached the sea at more widely spread points than any other Lakeland Fell, with Raise Beck going through Grasmere and Windermere to reach Morecambe Bay, Birkside Gill going through Thirlmere and Derwent Water to reach the Irish Sea at Workington and Grisedale Beck draining into Ullswater and then to the sea at the Solway Firth.

Geographic entities mentioned:
surface_form: Windermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.358333333333
lon: -2.9361111111111
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
surface_form: derwent water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.583333333333
lon: -3.15
surface_form: windermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.358333333333
lon: -2.9361111111111
surface_form: grasmere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.449383
lon: -3.021239
North of Dollywaggon Pike the ridge narrows and then steps up over High Crag to the plateau top of Nethermost Pike. In the other direction the high ground curves south-east around Cock Cove before a long slope falls to Grisedale Tarn at around. This sizeable tarn has a depth of around and holds brown trout, perch and eels.

Geographic entities mentioned:
surface_form: Grisedale Tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.5
lon: -3.0083333333333
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
surface_form: grisedale tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.5
lon: -3.0083333333333
Dollywaggon Pike is the southernmost fell of the ridge proper, with Nethermost Pike immediately to the north. There is a subsidiary top between Nethermost and Dollywaggon Pikes named High Crag (). Due to the very limited depression between the two, most guidebooks follow Wainwright in counting High Crag as a part of Nethermost Pike.

Geographic entities mentioned:
surface_form: high crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.514638888889
lon: -3.2681388888889
surface_form: high crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.514
lon: -3.0158
There is a subsidiary top between Nethermost and Dollywaggon Pikes named High Crag (). Due to the very limited depression between the two, most guidebooks follow Wainwright in counting High Crag as a part of Nethermost Pike. To the south of Dollywaggon Pike is the complex depression containing Grisedale Tarn, with Seat Sandal and Fairfield rising beyond.

Geographic entities mentioned:
surface_form: high crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.514638888889
lon: -3.2681388888889
surface_form: high crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.514
lon: -3.0158
On the east, the first impression is all of rock. The long strath of Grisedale runs north-eastward to Ullswater, cutting off a series of hanging valleys which fall from the Helvellyn range. To the north-east of Dollywaggon Pike, below the summit of High Crag, is Ruthwaite Cove, a corrie surrounded on three sides by crag. Ruthwaite Cove is now the site of Ruthwaite Lodge, a climbing hut.

Geographic entities mentioned:
surface_form: high crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.514638888889
lon: -3.2681388888889
surface_form: high crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.514
lon: -3.0158
At the bottom of The Tongue is Spout Crag, standing above Grisedale Beck and forcing walkers to take a detour from the ridgeline. North of Dollywaggon Pike the ridge narrows and then steps up over High Crag to the plateau top of Nethermost Pike. In the other direction the high ground curves south-east around Cock Cove before a long slope falls to Grisedale Tarn at around.

Geographic entities mentioned:
surface_form: high crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.514638888889
lon: -3.2681388888889
surface_form: high crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.514
lon: -3.0158
But the eastern side is a desolation of crag and boulder and scree.’&quot;
The western flank is named Willie Wife Moor for reasons lost to antiquity. It is bounded by Birkside Gill to the north and Raise Beck to the south, Reggle Knott being the only area of rough ground. At the base of the slope Raise Beck flows north to Thirlmere, having been diverted as a part of the 1884 reservoir project.

Geographic entities mentioned:
surface_form: knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.686211111111
lon: -3.0935388888889
Further leases were taken out in 1784 and 1862, the last-known operation being in 1880. To the east of Dollywaggon Pike is a second corrie, Cock Cove, with Falcon Crag and the deeply gullied Tarn Crag providing the impressive headwall. Between the two coves, Dollywaggon Pike sends out a fine rocky ridge, The Tongue. This arête ascends by a series of rocky steps making straight for the summit.

Geographic entities mentioned:
surface_form: tarn crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.463
lon: -2.787
surface_form: tarn crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.473
lon: -3.076
surface_form: dollywaggon pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.508069444444
lon: -3.0115611111111
This arête ascends by a series of rocky steps making straight for the summit. At the bottom of The Tongue is Spout Crag, standing above Grisedale Beck and forcing walkers to take a detour from the ridgeline. North of Dollywaggon Pike the ridge narrows and then steps up over High Crag to the plateau top of Nethermost Pike.

Geographic entities mentioned:
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
This sizeable tarn has a depth of around and holds brown trout, perch and eels. The outflow is to Ullswater to the north east, picking up all of the rainfall from the eastern face of Dollywaggon Pike. To the west of the tarn is the unnamed col between Dollywaggon Pike and Seat Sandal and immediately to the south is Grisedale Hause, the depression between Seat Sandal and Fairfield.

Geographic entities mentioned:
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
surface_form: fairfield
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4969
lon: -2.99059
surface_form: dollywaggon pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.508069444444
lon: -3.0115611111111
surface_form: seat sandal
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.494561111111
lon: -3.01585
surface_form: seat sandal
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.494561111111
lon: -3.01585
surface_form: seat sandal
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.494561111111
lon: -3.01585
It carries a small cairn with a larger one a few yards to the west. The view is extensive with the eastern foreground particularly fine
Ascents. The Tongue provides a fine route of ascent, though a long one, from Patterdale and the fell can also be reached from the Grasmere area via Grisedale Tarn. Ascents up the western slopes are unimpeded but uninteresting.

Geographic entities mentioned:
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
surface_form: grisedale tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.5
lon: -3.0083333333333
surface_form: grasmere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.449383
lon: -3.021239
Dollywaggon Pike. Dollywaggon Pike is a fell in the English Lake District. It stands on the main spine of the Helvellyn range in the Eastern Fells, between Thirlmere and the Ullswater catchment. Toponymy. The spelling ‘Dollywaggon’ is used on Ordnance Survey 1:25,000 maps but ‘Dollywagon’ on 1:50,000 maps.

Geographic entities mentioned:
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
On the east, the first impression is all of rock. The long strath of Grisedale runs north-eastward to Ullswater, cutting off a series of hanging valleys which fall from the Helvellyn range. To the north-east of Dollywaggon Pike, below the summit of High Crag, is Ruthwaite Cove, a corrie surrounded on three sides by crag. Ruthwaite Cove is now the site of Ruthwaite Lodge, a climbing hut.

Geographic entities mentioned:
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
Thus Seat Sandal stands topographically on the ridge between the two higher fells, but so out on a limb that many walkers proceed directly from Dollywaggon Pike to Fairfield. Geology. Geologically the summit of the fell forms part of the Deepdale Formation, (principally volcaniclastic sandstone) underlain by the dacitic lapilli tuff of the Helvellyn Formation. Summit.

Geographic entities mentioned:
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.264
lon: -2.432
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.54
lon: -1.99
To the west of the tarn is the unnamed col between Dollywaggon Pike and Seat Sandal and immediately to the south is Grisedale Hause, the depression between Seat Sandal and Fairfield. Thus Seat Sandal stands topographically on the ridge between the two higher fells, but so out on a limb that many walkers proceed directly from Dollywaggon Pike to Fairfield. Geology.

Geographic entities mentioned:
surface_form: fairfield
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4969
lon: -2.99059
surface_form: dollywaggon pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.508069444444
lon: -3.0115611111111
Dollywaggon Pike. Dollywaggon Pike is a fell in the English Lake District. It stands on the main spine of the Helvellyn range in the Eastern Fells, between Thirlmere and the Ullswater catchment. Toponymy. The spelling ‘Dollywaggon’ is used on Ordnance Survey 1:25,000 maps but ‘Dollywagon’ on 1:50,000 maps.

Geographic entities mentioned:
surface_form: dollywaggon pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.508069444444
lon: -3.0115611111111
Toponymy. The spelling ‘Dollywaggon’ is used on Ordnance Survey 1:25,000 maps but ‘Dollywagon’ on 1:50,000 maps. The Ordnance Survey gazetteer, nominally based on the 1:50,000 maps, lists only ‘Dollywaggon Pike’. As of 2005, the ‘Dollywagon’ spelling is slightly more common in online references.

Geographic entities mentioned:
surface_form: dollywaggon pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.508069444444
lon: -3.0115611111111
As of 2005, the ‘Dollywagon’ spelling is slightly more common in online references. Alfred Wainwright used ‘Dollywaggon Pike’ in his &quot;Pictorial Guide&quot;, a position supported by other writers. One meaning for the word &quot;Dollywaggon&quot; gives an Old Norse source formed by the combination of ' (‘fiend’ or ‘giant’) and &quot;veginn&quot; (‘lifted’). Topography.

Geographic entities mentioned:
surface_form: dollywaggon pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.508069444444
lon: -3.0115611111111
Due to the very limited depression between the two, most guidebooks follow Wainwright in counting High Crag as a part of Nethermost Pike. To the south of Dollywaggon Pike is the complex depression containing Grisedale Tarn, with Seat Sandal and Fairfield rising beyond. In common with much of the Helvellyn range there is a marked contrast between the western and eastern slopes of Dollywaggon Pike.

Geographic entities mentioned:
surface_form: dollywaggon pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.508069444444
lon: -3.0115611111111
It is bounded by Birkside Gill to the north and Raise Beck to the south, Reggle Knott being the only area of rough ground. At the base of the slope Raise Beck flows north to Thirlmere, having been diverted as a part of the 1884 reservoir project. It previously turned south down the other side of Dunmail Raise pass to feed Grasmere.

Geographic entities mentioned:
surface_form: grasmere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.449383
lon: -3.021239
This sizeable tarn has a depth of around and holds brown trout, perch and eels. The outflow is to Ullswater to the north east, picking up all of the rainfall from the eastern face of Dollywaggon Pike. To the west of the tarn is the unnamed col between Dollywaggon Pike and Seat Sandal and immediately to the south is Grisedale Hause, the depression between Seat Sandal and Fairfield.

Geographic entities mentioned:
surface_form: dollywaggon pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.508069444444
lon: -3.0115611111111
This is still the case today when there is enough water in Raise Beck for it to flow both north and south, but normally Seat Sandal now has this distinction. Birkside Gill contains the remains of a number of levels driven for copper between 1840 and 1866. On the east, the first impression is all of rock.

Geographic entities mentioned:
surface_form: seat sandal
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.494561111111
lon: -3.01585
Cerbat Mountains. The Cerbat Mountains () is a mountain range in Mohave County in northwest Arizona immediately north of Kingman. The Cerbat Mountains and the White Hills (Arizona) adjacent north, are the dividing ranges between the Detrital Valley west, and the Hualapai Valley east. It is a 23 mi long range trending slightly northwest–southeast.

Geographic entities mentioned:
surface_form: Detrital Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.70472222
lon: -114.4775
surface_form: Hualapai Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.57472222
lon: -113.93611111
It is a 23 mi long range trending slightly northwest–southeast. It lies directly east of the 130-mile long Black Mountains range and is separated by the Sacramento Valley bordering southwest of Kingman through which Interstate 40 turns south and west to meet Needles, California; the long Detrital Valley and plains drains northwest of the mountains into southern Lake Mead.

Geographic entities mentioned:
surface_form: Detrital Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.70472222
lon: -114.4775
A series of peaks can be found towards the southern end of the range, including Packsaddle Mountain at, and Cherum Peak at. The northern section of the Cerbat Mountains is composed mostly of the Mount Tipton Wilderness, with Mount Tipton being its peak at. The Dolan Springs community is at the base of the wilderness on the northwestern side of the Cerbat Mountains.

Geographic entities mentioned:
surface_form: Mount Tipton
instance_of: Mountain
countries: United States
coordinates: lat: 35.538869444444
lon: -114.19274722222
He would later scale each of the remaining Seven Summits (the highest mountains on each continent) in the following 14 years. In 2011, he climbed Aconcagua in South America and the Carstensz Pyramid in Oceania. The following year, he reached the peaks of Denali in North America and Mount Elbrus in Europe. In 2015, he completed Vinson Massif in Antarctica.

Geographic entities mentioned:
surface_form: Aconcagua
instance_of: Mountain
countries: Argentina
coordinates: lat: -32.653055555555554
lon: -70.01166666666667
He would later scale each of the remaining Seven Summits (the highest mountains on each continent) in the following 14 years. In 2011, he climbed Aconcagua in South America and the Carstensz Pyramid in Oceania. The following year, he reached the peaks of Denali in North America and Mount Elbrus in Europe. In 2015, he completed Vinson Massif in Antarctica.

Geographic entities mentioned:
surface_form: Denali
instance_of: Mountain
countries: United States
coordinates: lat: 63.06916666666667
lon: -151.0063888888889
surface_form: Mount Elbrus
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 43.35254
lon: 42.437875
The following year, he reached the peaks of Denali in North America and Mount Elbrus in Europe. In 2015, he completed Vinson Massif in Antarctica. That year, he also made his first attempt to climb Mount Everest, but was forced to suspend the trip after surviving the 2015 Mount Everest avalanches caused by the 7.8-magnitude Gorkha earthquake.

Geographic entities mentioned:
surface_form: Vinson Massif
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
In 2015, he completed Vinson Massif in Antarctica. That year, he also made his first attempt to climb Mount Everest, but was forced to suspend the trip after surviving the 2015 Mount Everest avalanches caused by the 7.8-magnitude Gorkha earthquake. He also assisted in the treatment of injured climbers after the avalanche.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Astatotilapia sp. 'shovelmouth'. &quot;Astatotilapia&quot; sp. 'shovelmouth' is a putative, formally undescribed species of freshwater fish in the family Cichlidae. It is endemic to Lake Victoria in Uganda. It was previously included in the IUCN Red List of Threatened Species as an endangered species, but omitted from more recent lists.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
These storms were bolstered by an unusually strong temperature contrast of the sea surface across the Atlantic Ocean. Abnormally warm waters had been widespread off West Africa whereas relatively cold surface waters had stretched between western Europe and the southeastern United States. The storm was exacerbated by the eruption cloud of the Soufrière Hills volcano.

Geographic entities mentioned:
surface_form: Soufrière Hills
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 16.716666666667
lon: -62.183333333333
Upaunan River. The Upaunan River is a tributary of the Enistustikweyach River in Regional County Municipality (RCM) of Eeyou Istchee James Bay (municipality) in the administrative region of the Nord-du-Québec, in Canadian province of Quebec, in Canada.

Geographic entities mentioned:
surface_form: Enistustikweyach River
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.779722222222
lon: -77.294166666667
surface_form: upaunan river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.799166666667
lon: -77.247222222222
The Upaunan River is a tributary of the Enistustikweyach River in Regional County Municipality (RCM) of Eeyou Istchee James Bay (municipality) in the administrative region of the Nord-du-Québec, in Canadian province of Quebec, in Canada. The Upaunan River hydrographic slope has no access road nearby; however, the northern route from Matagami passes to west of the mouth of the Upaunan River.

Geographic entities mentioned:
surface_form: matagami
instance_of: Lake
countries: Canada
coordinates: lat: 49.8667
lon: -77.4464
surface_form: upaunan river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.799166666667
lon: -77.247222222222
surface_form: upaunan river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.799166666667
lon: -77.247222222222
Upaunan River. The Upaunan River is a tributary of the Enistustikweyach River in Regional County Municipality (RCM) of Eeyou Istchee James Bay (municipality) in the administrative region of the Nord-du-Québec, in Canadian province of Quebec, in Canada.

Geographic entities mentioned:
surface_form: upaunan river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.799166666667
lon: -77.247222222222
The surface of the river is usually frozen from early November to mid-May, however, safe ice circulation is generally from mid-November to mid-April. Toponymy. Of Cree origin, the toponym &quot;Upaunan River&quot; means: &quot;the river of the camp of the pass&quot;. The toponym &quot;Upaunan River&quot; was formalized on October 5, 1982 at the Commission de toponymie du Québec

Geographic entities mentioned:
surface_form: upaunan river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.799166666667
lon: -77.247222222222
surface_form: upaunan river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.799166666667
lon: -77.247222222222
Lakeside is immediately west of the City and County of Denver, the most populous municipality in the state. The Alcott Post Office (ZIP Code 80212) serves Lakeside. The town's namesake lake is Lake Rhoda, which covers 20% of its total area. A year after its incorporation on November 12, 1907, the Lakeside Amusement Park, nicknamed &quot;White City&quot;, opened on the eastern shores.

Geographic entities mentioned:
surface_form: Lake Rhoda
instance_of: Lake
countries: United States
coordinates: lat: 39.7808
lon: -105.0582
Victoria became another centre of Indo-Canadian business activity and members of the ethnic group also settled Coombs, Duncan, Fraser Mills, New Westminster, and Ocean Falls. As of 1923 rural areas that received Indo-Canadian settlement included those in the Fraser Valley and Vancouver Island.

Geographic entities mentioned:
surface_form: Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
Commerce. The initial Sikh Indo-Canadian population primarily worked in laborer trades, with about 75% of the total population working in the forestry industry as of 1967. Indo-Canadians worked in Okanagan Valley fruit farms and Fraser Valley dairy farms. Some Indo-Canadians also established retail operations and commercial fishing operations.

Geographic entities mentioned:
surface_form: Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
Many men worked at logging camps and sawmills. As of circa 1987 about 9,600 farm workers in the Fraser Valley/Lower Mainland region were immigrants of Punjabi origin, making up 80% of that region's farm workers. By the 1970s these farm workers operated under a contracting system which involved the contractors transporting their charges and taking cuts from their charges' paychecks.

Geographic entities mentioned:
surface_form: Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
The East Indian Women's Association made recreational events open to the wider public. Those events included dinners and fashion shows. The Fraser Valley Indo-Canadian Business Association represents Indo-Canadian businesses in the Abbotsford area. It was established in 1987. The India-Canada Cultural Association of Victoria (ICCA) is maintained by Victoria-based Indo-Canadians.

Geographic entities mentioned:
surface_form: Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
Lake Herăstrău. Lake Herăstrău is an anthropic lake located in the northern part of the city of Bucharest, developed on the Colentina River, in the area where it flows through the urban area of the city, situated between Lake Băneasa upstream and Lake Floreasca downstream. It is the biggest lake in Bucharest.

Geographic entities mentioned:
surface_form: Lake Floreasca
instance_of: Lake
countries: Romania
coordinates: lat: 44.47008
lon: 26.10158
surface_form: lake herăstrău
instance_of: Lake
countries: Romania
coordinates: lat: 44.47532
lon: 26.08207
This sawmill proved to be profitable for the estate by providing wood for construction in the capital city. Lock. The Herăstrău Lake Lock (Ecluza Lacului Herăstrău) was constructed between 1933 and 1936, replacing an old dam that had served a sawmill in the area. This lock is located on the left bank of Lake Herăstrău and connects it to Lake Floreasca.

Geographic entities mentioned:
surface_form: Lake Floreasca
instance_of: Lake
countries: Romania
coordinates: lat: 44.47008
lon: 26.10158
surface_form: lake floreasca
instance_of: Lake
countries: Romania
coordinates: lat: 44.47008
lon: 26.10158
surface_form: lake herăstrău
instance_of: Lake
countries: Romania
coordinates: lat: 44.47532
lon: 26.08207
This lock is located on the left bank of Lake Herăstrău and connects it to Lake Floreasca. Besides its recreational function, allowing boat travel between Lake Herăstrău and Lake Floreasca, the lock also serves as an additional drainage system for Lake Herăstrău into Lake Floreasca.

Geographic entities mentioned:
surface_form: lake floreasca
instance_of: Lake
countries: Romania
coordinates: lat: 44.47008
lon: 26.10158
surface_form: lake floreasca
instance_of: Lake
countries: Romania
coordinates: lat: 44.47008
lon: 26.10158
surface_form: lake herăstrău
instance_of: Lake
countries: Romania
coordinates: lat: 44.47532
lon: 26.08207
surface_form: lake herăstrău
instance_of: Lake
countries: Romania
coordinates: lat: 44.47532
lon: 26.08207
Lake Herăstrău. Lake Herăstrău is an anthropic lake located in the northern part of the city of Bucharest, developed on the Colentina River, in the area where it flows through the urban area of the city, situated between Lake Băneasa upstream and Lake Floreasca downstream. It is the biggest lake in Bucharest.

Geographic entities mentioned:
surface_form: lake herăstrău
instance_of: Lake
countries: Romania
coordinates: lat: 44.47532
lon: 26.08207
Besides its recreational function, allowing boat travel between Lake Herăstrău and Lake Floreasca, the lock also serves as an additional drainage system for Lake Herăstrău into Lake Floreasca. This is particularly important during heavy rains when there is a risk of excessive water level rise in Lake Herăstrău, which could potentially pose a threat to areas in Bucharest.

Geographic entities mentioned:
surface_form: lake herăstrău
instance_of: Lake
countries: Romania
coordinates: lat: 44.47532
lon: 26.08207
Dreschhoff Peak. Dreschhoff Peak () in Antarctica is named after Gisela A.M. Dreschhoff, a physicist at the Space Technology Center, University of Kansas, who conducted radioactivity surveys and other field work in various parts of Antarctica, including Victoria Land, for 11 field seasons, 1976–89.

Geographic entities mentioned:
surface_form: dreschhoff peak
instance_of: Mountain
coordinates: lat: -78.0167
lon: 161.083
Dreschhoff Peak. Dreschhoff Peak () in Antarctica is named after Gisela A.M. Dreschhoff, a physicist at the Space Technology Center, University of Kansas, who conducted radioactivity surveys and other field work in various parts of Antarctica, including Victoria Land, for 11 field seasons, 1976–89.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
Scott's Gulf. Scott's Gulf is a canyon situated along the Caney Fork River in White County, Tennessee, in the southeastern United States. The canyon stretches for approximately as the Caney Fork drops from the top of the Cumberland Plateau down to the eastern Highland Rim.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
Basaral. Basaral (, &quot;Basaral&quot;) is an island in Lake Balkhash in Kazakhstan. It is located in the southwestern portion of the lake. Geography. Basaral is located close to the shore, separated from it by a wide sound. It has a length of a little over and a maximum width of roughly. Ortaaral is a similar smaller island located to the southeast of Basaral's southern end.

Geographic entities mentioned:
surface_form: Lake Balkhash
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 46.540833333333
lon: 74.878888888889
Siege of Torgau. The siege of Torgau (18 October 1813 – 10 January 1814) was a siege in the War of the Sixth Coalition. The French-held fortress on the Elbe was besieged by Prussian troops and forced to surrender. Background. The fortified city of Torgau was built on both sides of the Elbe as a royal Saxon main arsenal based on a design by Ernst Ludwig von Aster.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
The French-held fortress on the Elbe was besieged by Prussian troops and forced to surrender. Background. The fortified city of Torgau was built on both sides of the Elbe as a royal Saxon main arsenal based on a design by Ernst Ludwig von Aster. Its defenses consisted of a strong outer wall, fosses, and external works. There were seven bastion fronts along the perimeter of the wall.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Lopevi. Lopevi (or Lopévi) is an uninhabited island in Malampa Province, Vanuatu. It lies to the southeast of Ambrym and east of Paama. Geography. Lopevi consists of the 7-km-wide cone of the active stratovolcano by the same name. It reaches a peak of 1413 m above sea level, the tallest point in central Vanuatu. It has erupted at least 22 times since 1862.

Geographic entities mentioned:
surface_form: Ambrym
instance_of: Mountain
countries: Vanuatu
coordinates: lat: -16.333333333333
lon: 168.33333333333
Lopevi. Lopevi (or Lopévi) is an uninhabited island in Malampa Province, Vanuatu. It lies to the southeast of Ambrym and east of Paama. Geography. Lopevi consists of the 7-km-wide cone of the active stratovolcano by the same name. It reaches a peak of 1413 m above sea level, the tallest point in central Vanuatu. It has erupted at least 22 times since 1862.

Geographic entities mentioned:
surface_form: lopévi
instance_of: Mountain
countries: Vanuatu
coordinates: lat: -16.833333333333
lon: 168.5
surface_form: lopevi
instance_of: Mountain
countries: Vanuatu
coordinates: lat: -16.833333333333
lon: 168.5
Lopevi. Lopevi (or Lopévi) is an uninhabited island in Malampa Province, Vanuatu. It lies to the southeast of Ambrym and east of Paama. Geography. Lopevi consists of the 7-km-wide cone of the active stratovolcano by the same name. It reaches a peak of 1413 m above sea level, the tallest point in central Vanuatu. It has erupted at least 22 times since 1862.

Geographic entities mentioned:
surface_form: lopevi
instance_of: Mountain
countries: Vanuatu
coordinates: lat: -16.833333333333
lon: 168.5
It reaches a peak of 1413 m above sea level, the tallest point in central Vanuatu. It has erupted at least 22 times since 1862. The island was formerly inhabited, but in 1960 the population moved to nearby Paama or Epi because of the recurrent danger. Lopevi is on the New Hebrides Plate, where it lies above the subducted Australian Plate to the west.

Geographic entities mentioned:
surface_form: lopevi
instance_of: Mountain
countries: Vanuatu
coordinates: lat: -16.833333333333
lon: 168.5
Urfjell Cliffs. Urfjell Cliffs () is a line of rock cliff and spurs trending southwest for 10 nautical miles (18 km) from Urfjelldokka Valley, forming a part of the Kirwan Escarpment in Queen Maud Land. Mapped by Norwegian cartographers from surveys and air photos by Norwegian-British-Swedish Antarctic Expedition (NBSAE) (1949–52) and additional air photos (1958–59).

Geographic entities mentioned:
surface_form: Urfjelldokka Valley
instance_of: Valley
coordinates: lat: -73.8333
lon: -4.75
surface_form: Kirwan Escarpment
instance_of: Landform
coordinates: lat: -73.4167
lon: -3.5
Niangua River. The Niangua River is a tributary of the Osage River in the Ozarks region of southern and central Missouri in the United States. Via the Osage and Missouri rivers it is part of the watershed of the Mississippi River. Niangua River has the name of Niangua (or Nehemgar), an Indian tribal leader. The name is said to mean &quot;bear&quot;. Course.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159