Sarmila/GeoWiki-Features huggingface dataset:
Obří důl. Obří důl (;) is a valley in the Giant Mountains in the Hradec Králové Region of the Czech Republic. The valley lies in the municipal territory of Pec pod Sněžkou and within the Krkonoše National Park. It is a valley of the upper course of the Úpa River, stretching between the foots of the Sněžka and Studniční hora mountains.

Geographic entities mentioned:
surface_form: obří důl
instance_of: Valley
countries: Czech Republic
coordinates: lat: 50.71591667
lon: 15.72361111
The valley was formed by a Quaternary glacier that reached a thickness of up to. In the valley lie the ashes of botanist Karel Kavina (1890–1948), as well as the resting place of several unfortunate individuals who fell from the top of Sněžka. Úpská jáma and historical sites. Úpská jáma is a glacial cirque that forms the uppermost section of Obří důl. Its slopes rise up to in height.

Geographic entities mentioned:
surface_form: obří důl
instance_of: Valley
countries: Czech Republic
coordinates: lat: 50.71591667
lon: 15.72361111
Historically, Obří bouda Hut stood on Czech territory since the mid-17th century but was demolished in 1982. On the Polish side of the border, the Silesian House, built in 1847, remains in use today. Within Obří důl, there once stood Kovárna, a building constructed before 1568 as a mining forge. Over time, it was converted into a tourist restaurant and later into a nature conservation facility.

Geographic entities mentioned:
surface_form: obří důl
instance_of: Valley
countries: Czech Republic
coordinates: lat: 50.71591667
lon: 15.72361111
Lawrie Glacier. Lawrie Glacier () is a glacier flowing between Mount Genecand and Mezzo Buttress, and entering the head of Barilari Bay between Cherkovna Point and Prestoy Point on the west coast of Graham Land, Antarctica.

Geographic entities mentioned:
surface_form: Mount Genecand
instance_of: Mountain
coordinates: lat: -66.1
lon: -64.65
The park is an excellent site for bird watching with osprey nests and bird blinds set up. The Barnegat Inlet is located at the southern tip of the park, separating the Barnegat Peninsula from Long Beach Island. Swimming, kayaking, and fishing are permitted in some areas of the park. Four wheel drive vehicles are permitted onto the beach with a permit. Flora.

Geographic entities mentioned:
surface_form: Barnegat Inlet
instance_of: Landform
countries: United States
coordinates: lat: 39.76666667
lon: -74.10333333
&quot;Leofshema&quot; was an important settlement at the confluence of the rivers Quaggy (from Farnborough) and Ravensbourne (Caesar's Well, Keston), so the village expanded north into the wetter area as drainage techniques improved. King Alfred was Lord of the Manor of Lewisham, as is celebrated by a plaque in Lewisham Library.

Geographic entities mentioned:
surface_form: Ravensbourne
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 51.482
lon: -0.017061111111111
The following month, Blenker's brigade was moved into Maj. Gen. John C. Frémont's Mountain Department, necessitating a march to Winchester, Virginia, where the 68th and the rest of Frémont's army guarded the western part of the Shenandoah Valley against incursions by Confederate forces under Lt. Gen. Stonewall Jackson. Their long march had left the 68th bereft of supplies and low on rations.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Gen. James Shields to converge on Jackson south of Massanutten Mountain. Jackson was determined to attack the two Union columns separately and arranged half of his troops to block Shields on the right side of the mountain, while the other half, commanded by Maj. Gen. Richard S. Ewell, blocked the left side. Jackson's wish was realized when, on June 8, Frémont's army attacked.

Geographic entities mentioned:
surface_form: Massanutten Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.643
lon: -78.612
Nganha. Nganha is a commune in Cameroon. It has a population between 3,000 and 5,000. It is about northwest of the summit of Tchabal Nganha, a large stratovolcano on the Ngaoundere Plateau, a highland area in the Adamawa Region of Cameroon.

Geographic entities mentioned:
surface_form: Tchabal Nganha
instance_of: Mountain
countries: Cameroon
coordinates: lat: 7.353687
lon: 14.014683
surface_form: Ngaoundere Plateau
instance_of: Plateau
countries: Cameroon
coordinates: lat: 7.33333333
lon: 13.83333333
Qinyang is now located along the Zhan (, &quot;Zhànhé&quot;), a tributary of the Yellow River. A part of the Taihang Mountains called the Shennong Mountain is in the rural area of Qinyang City. The southeast of Qinyang City is 128 kilometers away from Zhengzhou, the provincial capital, 90 kilometers away from Luoyang in the east and 36 kilometers away from Jiaozuo in the east. Terrain.

Geographic entities mentioned:
surface_form: Shennong Mountain
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 35.20691944
lon: 112.81848333
History. Cairness House was commissioned by Charles Gordon of Cairness and Buthlaw, a descendant of the Barclays of Cairness through his mother. The house was part of a estate that included the village of St Comb's and the Loch of Strathbeg.

Geographic entities mentioned:
surface_form: Loch of Strathbeg
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.619805555556
lon: -1.8769444444444
She graduated from Stanford Phi Beta Kappa with a bachelor's degree in communication. While at KRCR, she met and married Larry Blackstock, a news director. They have a son, Alex. Career. Matsukawa worked at KRCR, a Redding, California, station, then KPTV in Portland, Oregon, followed by three years at Seattle's KOMO TV, where one of her first stories was the 1980 eruption of Mount St. Helens.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
Nago–Torbole. Nago–Torbole (&quot;Nach e Tùrbule&quot; in local dialect) is a &quot;comune&quot; (municipality) in Trentino in the northern Italian region Südtirol, located about southwest of Trento on the north shore of Lake Garda.

Geographic entities mentioned:
surface_form: Lake Garda
instance_of: Lake
countries: Italy
coordinates: lat: 45.633333333333
lon: 10.666666666667
The villages cling to the limestone rocks on the extreme north-west slope of Monte Baldo; it lies close to the mouth of the river Sarca and its houses are set as an amphitheater around the small bay, in front of Monte Rocchetta and the Ledro Alps. Nago–Torbole borders the following municipalities: Arco, Riva del Garda, Mori, Ledro, Brentonico, and Malcesine. Torbole.

Geographic entities mentioned:
surface_form: Monte Baldo
instance_of: Mountain
countries: Italy
coordinates: lat: 45.733
lon: 10.833
surface_form: Monte Rocchetta
instance_of: Mountain
countries: Italy
coordinates: lat: 45.88694444
lon: 10.81416667
Nago–Torbole borders the following municipalities: Arco, Riva del Garda, Mori, Ledro, Brentonico, and Malcesine. Torbole. Torbole, at above sea level, is situated on the extreme north-western appendix of the Baldo chain and it is set as an amphitheatre on Lake Garda.

Geographic entities mentioned:
surface_form: Lake Garda
instance_of: Lake
countries: Italy
coordinates: lat: 45.633333333333
lon: 10.666666666667
The lake, once only valuable to fishermen and traders, is still the most precious resource together with high Monte Baldo, which was once a seemingly inexhaustible mine of firewood and game though now it is a protected area for its rare flora, some of which are endemic to the area. Nago. Situated on the hills above Torbole sits Nago.

Geographic entities mentioned:
surface_form: Monte Baldo
instance_of: Mountain
countries: Italy
coordinates: lat: 45.733
lon: 10.833
Examples of varieties having the Canna hybrid Madame Crozy as a parent, are C. 'Austria' (1893), C. 'Italia' (1893), C. 'Alemania' (1894), C. 'Britannia' (1895), C. 'Heinrich Seidel'(1895). There is recorded knowledge of 57 cultivars originating from this prolific nursery, until its destruction by the eruption of the Mount Vesuvius volcano in the early 1900s. 1880s Victor Lemoine.

Geographic entities mentioned:
surface_form: Mount Vesuvius
instance_of: Mountain
countries: Italy
coordinates: lat: 40.821388888889
lon: 14.425555555556
According to Gyula Pauler, Atyusz was a descendant of Bulcsú, who settled down near the Lake Balaton in the 10th century. János Karácsonyi, in his namesake work (1900–1901), first discovered the separate genus of Atyusz and also systematized the family's three branches. Wertner questioned Karácsonyi's remarks in 1902, who also maintained his position.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
Dong Hua Sao National Park. Dong Hua Sao National Protected Area is a national park in Champasak Province in southern Laos. This forested park rises from the Mekong river lowlands eastwards into the Bolaven Plateau. It is an ecotourism destination. Geography.

Geographic entities mentioned:
surface_form: Bolaven Plateau
instance_of: Mountain
countries: Laos
coordinates: lat: 15.11
lon: 106.44
In 1867 the May family traveled by covered wagon and on foot to Salt Lake City with Leonard Rice's company. She chiseled her name into Independence Rock in Wyoming during the journey. The Mays arrived in the Salt Lake Valley in August 1867. After settling in the Ogden area, Ruth attended John Morgan's College in Salt Lake City for four months.

Geographic entities mentioned:
surface_form: Salt Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.6839
lon: -111.978
Kirana Hills Site. The Kirana Hills Site is an extensive rocky mountain range and a reservation of the Ministry of Defense (MoD) and nuclear arsenal storage location of Pakistan army, located in the Sargodha District in Punjab, Pakistan. Known locally as &quot;Black Mountains&quot; due to its brownish landscape, it is expanded between the township of Rabwah and the metropolitan city of Sargodha.

Geographic entities mentioned:
surface_form: kirana hills site
instance_of: Mountain
countries: Pakistan
coordinates: lat: 31.95
lon: 72.7
Known locally as &quot;Black Mountains&quot; due to its brownish landscape, it is expanded between the township of Rabwah and the metropolitan city of Sargodha. The highest peak of the Kirana Hills is measured at with average peaks at highest peak is about. Etymology.

Geographic entities mentioned:
surface_form: kirana hills
instance_of: Mountain
countries: Pakistan
coordinates: lat: 31.95
lon: 72.7
Topography and geology. The Kirana Hills is an extensive rocky mountain range located in the Sargodha District, and about in distance from the Salt Range. In 1913, British geologists conducted extensive investigations on the rock formations in the Kirana Hills, which are different from the rest of its parent mountains ranges; the rocks are noticeably black in formation.

Geographic entities mentioned:
surface_form: kirana hills
instance_of: Mountain
countries: Pakistan
coordinates: lat: 31.95
lon: 72.7
In 1913, British geologists conducted extensive investigations on the rock formations in the Kirana Hills, which are different from the rest of its parent mountains ranges; the rocks are noticeably black in formation. The highest peak at the Kirana Hills is measured exactly at by the British surveyors from the level of the plain in 1913.

Geographic entities mentioned:
surface_form: kirana hills
instance_of: Mountain
countries: Pakistan
coordinates: lat: 31.95
lon: 72.7
The highest peak at the Kirana Hills is measured exactly at by the British surveyors from the level of the plain in 1913. The average height in the Kirana Hills are recorded at by the Geological Survey of Pakistan (GSP) in their studies of hydrology reports in 1967. The Kirana Hills are expanded and scattered over an area of about and about in length.

Geographic entities mentioned:
surface_form: kirana hills
instance_of: Mountain
countries: Pakistan
coordinates: lat: 31.95
lon: 72.7
surface_form: kirana hills
instance_of: Mountain
countries: Pakistan
coordinates: lat: 31.95
lon: 72.7
In 1970s, the Geological Survey of Pakistan conducted a survey to find uranium ores and began the mining of uranium after its geologists confirmed the deposits of uranium ores at the Kirana Hills. Climate and wildlife. The landform of the Kirana Hills is known to be a steppe with heavy grassland besides the Rocky Mountains.

Geographic entities mentioned:
surface_form: kirana hills
instance_of: Mountain
countries: Pakistan
coordinates: lat: 31.95
lon: 72.7
Climate and wildlife. The landform of the Kirana Hills is known to be a steppe with heavy grassland besides the Rocky Mountains. The Pakistan Meteorological Department reported its weather conditions to be extreme with the highest have been recorded to in the summer while the minimum temperature recorded is as low as freezing point in the winter.

Geographic entities mentioned:
surface_form: kirana hills
instance_of: Mountain
countries: Pakistan
coordinates: lat: 31.95
lon: 72.7
The army engineers also worked on relocating the wildlife, specifically the wild boars, to stay out of the weapon-testing tunnels before the diagnosticians housed the tunnels. The tunnels at the Kirana Hills are composed of multiple cables, line-of-sight screen boxes, oscillators, computers, and other diagnostics equipments were installed by the national laboratories' diagnostics teams.

Geographic entities mentioned:
surface_form: kirana hills
instance_of: Mountain
countries: Pakistan
coordinates: lat: 31.95
lon: 72.7
With the Clinton administration continuously monitoring the region, the Ministry of Defense (MoD) moved the subcritical experiments to unknown location in Kala Chitta Range, which is in Khyber-Pakhtunkhwa. The Pakistani government released a tender for the remediation works at the Kirana Hills opened the parts of the site for public tourism in 1995.

Geographic entities mentioned:
surface_form: kirana hills
instance_of: Mountain
countries: Pakistan
coordinates: lat: 31.95
lon: 72.7
The river is believed to be named for a Cherokee chief who once lived in the area. Course. The river rises at the base of the Cumberland Plateau, just southwest of Monterey in eastern Putnam County, with the convergence of several smaller streams that drop off the Plateau. Several of these headwater streams are impounded at the Plateau's edge, including one which forms Monterey Lake.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
Acatenango, Chimaltenango. Acatenango is a town and municipality in the Chimaltenango department of Guatemala. It is in this municipality that the Acatenango volcano is located. The town is in the valley of the Cocoyá River. Spanish colony.

Geographic entities mentioned:
surface_form: Acatenango volcano
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.5
lon: -90.875833333333
1974 Volcán de Fuego eruption. On 15 October 1974, tremors woke up people in the settlements surrounding the Volcán de Fuego at 2:00 AM, followed by rumbling and cinders and ashes falling from the sky, which submerged the town into darkness for a few days.

Geographic entities mentioned:
surface_form: Volcán de Fuego
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.474722222222
lon: -90.880833333333
It lies northeast of the lakes named Q'umir Qucha (&quot;green lake&quot;, &quot;Khomer Khocha&quot;), Yana Qucha (&quot;black lake&quot;, &quot;Yana Khocha&quot;), Parinani (&quot;the one with flamingos&quot;) and Wallatani (&quot;the one with Andean geese&quot;, &quot;Huallatani&quot;).

Geographic entities mentioned:
surface_form: wallatani
instance_of: Lake
countries: Bolivia
coordinates: lat: -17.008333333333333
lon: -67.34722222222223
Q'illu Q'illu (Bolivia). Q'illu Q'illu (Aymara and Quechua &quot;q'illu&quot; yellow, the reduplication indicates that there is a group or a complex of something, &quot;a complex of yellow&quot;, or &quot;q'illu q'illu&quot; a plant &quot;(Berberis bumaelifolia)&quot;, also spelled &quot;Khellu Khellu&quot;) is a mountain in the Bolivian Andes which reaches a height of approximately.

Geographic entities mentioned:
surface_form: q'illu q'illu (bolivia)
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.06388889
lon: -66.48944444
Q'illu Q'illu (Bolivia). Q'illu Q'illu (Aymara and Quechua &quot;q'illu&quot; yellow, the reduplication indicates that there is a group or a complex of something, &quot;a complex of yellow&quot;, or &quot;q'illu q'illu&quot; a plant &quot;(Berberis bumaelifolia)&quot;, also spelled &quot;Khellu Khellu&quot;) is a mountain in the Bolivian Andes which reaches a height of approximately.

Geographic entities mentioned:
surface_form: q'illu q'illu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.06388889
lon: -66.48944444
surface_form: q'illu q'illu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.06388889
lon: -66.48944444
Himex. Himex is a Mount Everest guiding company. It was founded in 1996 by New Zealander Russell Brice. The name is a truncated version of the full name &quot;Himalayan Experience&quot;. &quot;National Geographic&quot; said Himex was the &quot;largest and most sophisticated guiding operation on Everest&quot; in a 2013 article.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
A distinctive feature of Himex's Mount Everest base camp is the social tent, the &quot;Tiger Dome&quot;, about across, climate controlled and with a large window to look out of, offering espresso, wine and other drinks, and television, music, web-connected computers, and gaming devices.<ref
Timeline. In 2015 Himex attempted an expedition to K2 but had to turn back due to avalanche risk.

Geographic entities mentioned:
surface_form: K2
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
Church too was interested in the Arctic, and in science and geography. He was a member of the American Geographical and Statistical Society, where the Arctic explorer Isaac Israel Hayes had lectured, and in 1859 he journeyed to the Arctic himself. Hayes, a friend of Church, named an Arctic peak at the Kennedy Channel after Church in the summer of 1861. As Church scholar David C.

Geographic entities mentioned:
surface_form: Kennedy Channel
instance_of: Watercourse
countries: Canada
Greenland
coordinates: lat: 80.9167
lon: -66.5
He led several expeditions to the Guyana Highlands, bringing back thousands of samples. In 1954 he discovered the botanically rich Cerro de la Neblina (&quot;Mountain of the Clouds&quot;). He retired in 1978. &quot;The Bassett Maguire Festschrift: A Tribute to the Man and His Deeds&quot;, edited by William R. Buck, Brian M. Boom, and Richard A. Howard (Memoirs of the New York Botanical Garden Vol.

Geographic entities mentioned:
surface_form: Cerro de la Neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.88638889
lon: -65.98944444
Southern Muya Range. The Southern Muya Range () is a mountain range in Buryatia and Zabaykalsky Krai, Russia, part of the Stanovoy Highlands. The highest point of the range is 3,067 m high Muisky Gigant; another important peak is 2363 m high Mount Shaman. Geography. The Southern Muya Range is located in the Baikal Rift Zone, in the southwestern part of the Baikal-Stanovoy Region.

Geographic entities mentioned:
surface_form: Muisky Gigant
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 55.977222222222
lon: 114.43916666667
surface_form: Mount Shaman
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 56.068611111111
lon: 115.86166666667
Hydrography. Rivers Pravaya Shurinda and Dyaltukta, right tributaries of the Muya originate from the northwestern slopes of the axial or main Southern Muya Range. Lake Dorong is located at the southwestern end. Flora. The slopes of the range are mainly covered with mountain taiga, with pre-alpine woodland and bare summits (golets) at higher elevations.

Geographic entities mentioned:
surface_form: Dorong
instance_of: Lake
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 55.291666666666664
lon: 112.27111111111111
Scafell. Scafell (or; also spelled Sca Fell, previously Scawfell) is a mountain in the Lake District region of Cumbria, England. It has a height of, making it the second-highest mountain in England after its neighbour, Scafell Pike, from which it is separated by Mickledore col. Topography. Scafell stands between Wasdale in the west and upper Eskdale to the east.

Geographic entities mentioned:
surface_form: Scafell Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454166666667
lon: -3.2115277777778
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
It has a height of, making it the second-highest mountain in England after its neighbour, Scafell Pike, from which it is separated by Mickledore col. Topography. Scafell stands between Wasdale in the west and upper Eskdale to the east. The highest part of the fell is a ridge running south from Mickledore as far as Slight Side, which is counted as a separate fell by most guidebooks.

Geographic entities mentioned:
surface_form: Wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.478
lon: -0.786
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.189
lon: -3.068
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
Topography. Scafell stands between Wasdale in the west and upper Eskdale to the east. The highest part of the fell is a ridge running south from Mickledore as far as Slight Side, which is counted as a separate fell by most guidebooks. Despite regarding Slight Side as a separate entity, Wainwright included the wide upland area beyond it to the south west as a part of Scafell.

Geographic entities mentioned:
surface_form: Slight Side
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4342
lon: -3.22095
(Interactive labels.)
rect 23 372 252 419 Slight Side (762 m)
rect 173 794 560 834 Scafell East Buttress
rect 707 787 893 861 Esk Crag or Buttress (750 m)
rect 245 303 409 358 Scafell (964 m)
rect 408 238 637 280 Mickledore (840 m)
rect 544 174 826 213 South Summit (950 m)
rect 706 310 928 355 Scafell Pike (978 m)
rect 870 238 1108 286 Broad Crag (934 m)
rect 1043 308 1198 360 Ill Crag (935 m)
rect 1238 311 1446 351 Great End (910 m)
rect 0 0 1444 1085 Click hyperlink or button to expand
From the narrow ridge of Mickledore the northern face of Scafell rises precipitously, an unusually complete barrier to progress along a Lakeland ridge, which frustrates many ridge walkers who find that this is a cliff for rock climbers only.

Geographic entities mentioned:
surface_form: Slight Side (762 m)
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4342
lon: -3.22095
surface_form: Scafell East Buttress
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
surface_form: Esk Crag or Buttress (750 m)
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454166666667
lon: -3.2115277777778
surface_form: South Summit (950 m)
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454166666667
lon: -3.2115277777778
surface_form: Scafell Pike (978 m)
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454166666667
lon: -3.2115277777778
surface_form: Broad Crag (934 m)
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456838888889
lon: -3.2077388888889
surface_form: Great End (910 m)
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.464
lon: -3.194
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
Northward is a saddle, marked by a large cross of stones and then the bouldery climb to Symonds Knott, the north top. This gives views straight down to Mickledore. Scafell gives a very different view to that from its higher neighbour with Wastwater and the coastal plain given great prominence. There is a fine vista of the Western Fells, together with Bowfell and the Coniston Fells. Wasdale.

Geographic entities mentioned:
surface_form: Bowfell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.447369444444
lon: -3.1658194444444
surface_form: bowfell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.447369444444
lon: -3.1658194444444
An alternative is to ascend from the Burnmoor track via Green How, but this misses the rock scenery of Scafell Crag. Eskdale. A pleasant but lengthy alternative begins from Boot in Eskdale, following the River Esk upstream, and scrambling up to the summit by way of Foxes Tarn. A gentler return can be made across moorland, by way of the Burnmoor Tarn.

Geographic entities mentioned:
surface_form: Foxes Tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.447152
lon: -3.221133
surface_form: foxes tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.447152
lon: -3.221133
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.478
lon: -0.786
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.189
lon: -3.068
However, when they restarted their work in England, given the status of Sca Fell as an essential surveying station (taking bearings of Slieve Donard and Snowdon, thereby helping to fix the relative positions of Ireland and England), the familiarity with this mountain probably meant that the &quot;Name Book&quot; procedures were overlooked.

Geographic entities mentioned:
surface_form: Slieve Donard
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.180277777778
lon: -5.9208333333333
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
surface_form: snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
surface_form: sca fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
surface_form: slieve donard
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.180277777778
lon: -5.9208333333333
Hence the correct enquiries were not made and the mistake of Donald was perpetuated. Wainwright stated that, originally, the name Scawfell/Scafell referred to the whole of the massif from Great End south to Slight Side; only more recently had the general term become applied solely to the part of the fell south of Mickledore.

Geographic entities mentioned:
surface_form: Slight Side
instance_of: Mountain
countries: United Kingdom
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Otley also comments that the Donald map of 1774 and the Ordnance Survey were incorrect in their naming. Scafell Pike and Scafell were referred to by the Ordnance Survey in their 1811 report as &quot;Sca-Fell Higher Top&quot; and &quot;Sca-Fell Lower Top&quot;. This can be confirmed from the 1811 account, a modern map and some elementary trigonometry..

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This can be confirmed from the 1811 account, a modern map and some elementary trigonometry.. Once Scafell Pike (which has its own convoluted name history) had been identified as England's highest mountain, that fact and the greater interest in climbing and fell-walking necessitated the Scafell Range being broken down into a number of individually named elements.

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It was once believed that Scafell was the highest mountain in this part of the Lake District &ndash; it is much more prominent in views from many directions than its higher neighbour &ndash; with the three apparently inferior peaks to the north (those now known as Scafell Pike, Ill Crag and Broad Crag) being known collectively as the &quot;Pikes of Scawfell&quot;.

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At the top of the rise from Mickledore is Symonds Knott (), the northern top. The wall of crags &ndash; Scafell Crag to the west and the East Buttress above the Eskdale side of Mickledore &ndash; has two main weaknesses. Running laterally across Scafell Crag is Lord's Rake, a scree-filled chute with several intermediate cols.

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The wall of crags &ndash; Scafell Crag to the west and the East Buttress above the Eskdale side of Mickledore &ndash; has two main weaknesses. Running laterally across Scafell Crag is Lord's Rake, a scree-filled chute with several intermediate cols. It has two upper entrances onto the saddle separating Symonds Knott from the main summit.

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The access to West Wall Traverse is clear of debris. The second breach in the crags is Broad Stand, a series of sloping steps which drop down from Symonds Knott almost to Mickledore; however, these steepen immediately above Mickledore and cannot be negotiated safely except by rock-climbers. The main summit stands a little to the south of the saddle, all around being a sea of stones.

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Summit. The main summit bears a large cairn on a short rocky ridge. Northward is a saddle, marked by a large cross of stones and then the bouldery climb to Symonds Knott, the north top. This gives views straight down to Mickledore. Scafell gives a very different view to that from its higher neighbour with Wastwater and the coastal plain given great prominence.

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Its dangers are more obvious travelling from Scafell Pike, but travelling from Scafell, the route loses a lot of height before the danger is seen. Instead there are two walking routes, but they entail some loss of altitude. The first is via Foxes Tarn to the East of Scafell summit, and the second is via Lord's Rake and the West Wall traverse. Rock Climbing.

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This was used by, among others William Wordsworth who, in addition to poetry, wrote a popular guide book to the Lake District, Harriet Martineau (whose work replaced Wordsworth's as the definitive guidebook), Jonathan Otley (who was one of the first to measure the height of most of the Lakeland fells), John Dalton (who also estimated the elevation of many of the fells), the surveyor of the Wasdale Head Enclosure map of 30 January 1808 and the hotel keepers and tour operators who lived or operated in the area, as typified by the many adverts in M.

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J. B. Baddeley's guide of 1895 (versus the guide text which was consistent with the maps therein). This split between local usage and maps printed by national publishers is further illustrated by the Wasdale Hall Estate Plan and Sales Particulars, dated 30th Sept 1920.

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The opposing flanks of Scafell are entirely different in character. To the south, monotonous smooth slopes, stony and lacking vegetation at higher levels, run down toward Burnmoor and the head of Wastwater. But on the east side several large crags loom impressively over upper Eskdale. On the north side, the sheer faces of Scafell Crag provide some the finest rock scenery in the Lake District.

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At the top of the rise from Mickledore is Symonds Knott (), the northern top. The wall of crags &ndash; Scafell Crag to the west and the East Buttress above the Eskdale side of Mickledore &ndash; has two main weaknesses. Running laterally across Scafell Crag is Lord's Rake, a scree-filled chute with several intermediate cols.

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An easy ridge then steps down southward over Long Green to Slight Side. On the east are Cam Spout Crag and the fine high waterfall after which it is named. Beyond Slight Side is a rough upland with many craggy tops and a number of tarns, before the southward descent finally ends in Lower Eskdale. South West of Scafell, below the scarp of Great How, is Burnmoor Tarn, one of the largest in Lakeland.

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However one section of Lord's Rake is now threatened by unstable rocks following a rock fall in 2001. An alternative is to ascend from the Burnmoor track via Green How, but this misses the rock scenery of Scafell Crag. Eskdale. A pleasant but lengthy alternative begins from Boot in Eskdale, following the River Esk upstream, and scrambling up to the summit by way of Foxes Tarn.

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Eskdale. A pleasant but lengthy alternative begins from Boot in Eskdale, following the River Esk upstream, and scrambling up to the summit by way of Foxes Tarn. A gentler return can be made across moorland, by way of the Burnmoor Tarn. Also starting in Eskdale, the Terrace route can be followed from Wha House, first ascending Slight Side. From Scafell Pike.

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More modern guides have partitioned the plateau off as a further independent top, Great How. The opposing flanks of Scafell are entirely different in character. To the south, monotonous smooth slopes, stony and lacking vegetation at higher levels, run down toward Burnmoor and the head of Wastwater. But on the east side several large crags loom impressively over upper Eskdale.

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Northward is a saddle, marked by a large cross of stones and then the bouldery climb to Symonds Knott, the north top. This gives views straight down to Mickledore. Scafell gives a very different view to that from its higher neighbour with Wastwater and the coastal plain given great prominence. There is a fine vista of the Western Fells, together with Bowfell and the Coniston Fells. Wasdale.

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Wasdale. The classic ascent via Lord's Rake path from Wastwater follows the main Scafell Pike footpath to Hollow Stones, then up to Lord's Rake. Lord's Rake may be followed in its entirety, or near the top of the first col, a diversion may be made onto the West Wall Traverse, the exit of which lies closer to the summit.

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Scafell. Scafell (or; also spelled Sca Fell, previously Scawfell) is a mountain in the Lake District region of Cumbria, England. It has a height of, making it the second-highest mountain in England after its neighbour, Scafell Pike, from which it is separated by Mickledore col. Topography. Scafell stands between Wasdale in the west and upper Eskdale to the east.

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But on the east side several large crags loom impressively over upper Eskdale. On the north side, the sheer faces of Scafell Crag provide some the finest rock scenery in the Lake District. Image:Annotated Scafell range.jpg|thumb|right|300px|The Scafell range as seen looking west from Crinkle Crags.

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From Scafell Pike. The route from Scafell Pike to Scafell (or its reverse) is one of the most frustrating in the Lake District. What seems like a direct route is in fact very hazardous as it has to negotiate Broad Stand crag, which is a dangerous and exposed scramble that has caused many accidents and injuries. It is usually treated as a rock climb, with appropriate ropes and belay protection.

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This was then perpetuated by the Ordnance Survey from 1867. The Donald map is the first to name many mountains in the Lake District - earlier maps concentrated on showing passes through the mountains. Until 1867 the two spellings are roughly equally split on maps, the shorter form being more common with London publishers. General usage at the time was predominantly &quot;Scawfell&quot;.

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It is usually treated as a rock climb, with appropriate ropes and belay protection. Wainwright warns against its dangers to walkers. Its dangers are more obvious travelling from Scafell Pike, but travelling from Scafell, the route loses a lot of height before the danger is seen. Instead there are two walking routes, but they entail some loss of altitude.

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The highest part of the fell is a ridge running south from Mickledore as far as Slight Side, which is counted as a separate fell by most guidebooks. Despite regarding Slight Side as a separate entity, Wainwright included the wide upland area beyond it to the south west as a part of Scafell. More modern guides have partitioned the plateau off as a further independent top, Great How.

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The main summit stands a little to the south of the saddle, all around being a sea of stones. An easy ridge then steps down southward over Long Green to Slight Side. On the east are Cam Spout Crag and the fine high waterfall after which it is named. Beyond Slight Side is a rough upland with many craggy tops and a number of tarns, before the southward descent finally ends in Lower Eskdale.

Geographic entities mentioned:
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Scafell. Scafell (or; also spelled Sca Fell, previously Scawfell) is a mountain in the Lake District region of Cumbria, England. It has a height of, making it the second-highest mountain in England after its neighbour, Scafell Pike, from which it is separated by Mickledore col. Topography. Scafell stands between Wasdale in the west and upper Eskdale to the east.

Geographic entities mentioned:
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More modern guides have partitioned the plateau off as a further independent top, Great How. The opposing flanks of Scafell are entirely different in character. To the south, monotonous smooth slopes, stony and lacking vegetation at higher levels, run down toward Burnmoor and the head of Wastwater. But on the east side several large crags loom impressively over upper Eskdale.

Geographic entities mentioned:
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instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
But on the east side several large crags loom impressively over upper Eskdale. On the north side, the sheer faces of Scafell Crag provide some the finest rock scenery in the Lake District. Image:Annotated Scafell range.jpg|thumb|right|300px|The Scafell range as seen looking west from Crinkle Crags.

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The wall of crags &ndash; Scafell Crag to the west and the East Buttress above the Eskdale side of Mickledore &ndash; has two main weaknesses. Running laterally across Scafell Crag is Lord's Rake, a scree-filled chute with several intermediate cols. It has two upper entrances onto the saddle separating Symonds Knott from the main summit.

Geographic entities mentioned:
surface_form: scafell
instance_of: Mountain
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coordinates: lat: 54.448
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On the east are Cam Spout Crag and the fine high waterfall after which it is named. Beyond Slight Side is a rough upland with many craggy tops and a number of tarns, before the southward descent finally ends in Lower Eskdale. South West of Scafell, below the scarp of Great How, is Burnmoor Tarn, one of the largest in Lakeland. Around deep, it holds trout, perch and pike.

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Rock Climbing. Scafell Crag, the massive north buttress of Scafell, and the overhanging East Buttress to the East of Mickledore Col, are the site of many famous historic and contemporary rock climbs. The history of climbing on these crags is documented by a book by The Fell and Rock Climbing Club called Nowt but a fleein' thing., Latitude Press. Name history.

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The access to West Wall Traverse is clear of debris. The second breach in the crags is Broad Stand, a series of sloping steps which drop down from Symonds Knott almost to Mickledore; however, these steepen immediately above Mickledore and cannot be negotiated safely except by rock-climbers. The main summit stands a little to the south of the saddle, all around being a sea of stones.

Geographic entities mentioned:
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Eskdale. A pleasant but lengthy alternative begins from Boot in Eskdale, following the River Esk upstream, and scrambling up to the summit by way of Foxes Tarn. A gentler return can be made across moorland, by way of the Burnmoor Tarn. Also starting in Eskdale, the Terrace route can be followed from Wha House, first ascending Slight Side. From Scafell Pike.

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White Cloud Peak 6. White Cloud Peak 6, also known as WCP 6, at above sea level is an unofficially named peak in the White Cloud Mountains of Idaho. The peak is located in Sawtooth National Recreation Area in Custer County north-northeast of White Cloud Peak 7, its line parent.

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