Sarmila/GeoWiki-Features huggingface dataset:
The higher ground is rocky heathland, with frequent tarns, while the lower ground supports pasture and woodland. In the east there are two main chains of hills: one overlooking Windermere, with Latterbarrow (245 m) as its highest point, and the other, which reaches 300 m, overlooking Coniston Water. Between them is flat country and Esthwaite Water.

Geographic entities mentioned:
surface_form: Esthwaite Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.3589
lon: -2.9846
After 1601, it was rarely used for moving soldiers, but remained vital for trade, and went through areas essential to French security. At the start of 1635, France had a total of around 100,000 men under arms, including 27,000 men under Urbain de Maillé-Brézé in Picardy and additional armies in Champagne, Lorraine, the Sarre, and the Valtellina.

Geographic entities mentioned:
surface_form: Valtellina
instance_of: Valley
countries: Italy
coordinates: lat: 46.166666666667
lon: 9.8666666666667
Geography. According to the United States Census Bureau, the town has a total area of, of which are land and are water, comprising 1.94% of the town. Bennington is drained by the north-flowing Contoocook River, which forms Powder Mill Pond on the southern boundary. The highest point in Bennington is above sea level on Crotched Mountain, whose summit lies just east in Francestown.

Geographic entities mentioned:
surface_form: Powder Mill Pond
instance_of: Lake
countries: United States
coordinates: lat: 42.969444444444
lon: -71.9325
Bennington is drained by the north-flowing Contoocook River, which forms Powder Mill Pond on the southern boundary. The highest point in Bennington is above sea level on Crotched Mountain, whose summit lies just east in Francestown. Bennington lies fully within the Merrimack River watershed. Transportation. The town is crossed by U. S. Route 202 and state routes 31 and 47.

Geographic entities mentioned:
surface_form: Crotched Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.998294444444
lon: -71.873711111111
Ben Wyvis. Ben Wyvis () is a mountain in Easter Ross, in the northern Highlands of Scotland. It lies north-west of Dingwall, in the council area of Highland, and the county of Ross and Cromarty. Ben Wyvis is a large winding and undulating ridge running roughly north–south for about 5 km, the highest point of which is Glas Leathad Mòr at. Geologically, the ridge is composed of Moine pelitic gneiss.

Geographic entities mentioned:
surface_form: ben wyvis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.679119444444
lon: -4.5792194444444
The mountain is prominent in views of the area, presenting a whale-back shape above the farmland of Strathconon. Ben Wyvis is an important habitat for several species of plants and birds, and is designated as a National Nature Reserve (NNR), a Special Protection Area (SPA), a Special Area of Conservation (SAC), and a Site of Special Scientific Interest (SSSI).

Geographic entities mentioned:
surface_form: ben wyvis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.679119444444
lon: -4.5792194444444
Of particular importance is the woolly hair-moss that covers the summit plateau. This springy moss provides ideal nesting territory for dotterel that breed here each summer: Ben Wyvis represents at least 2.4% of the breeding population in Great Britain. Name.

Geographic entities mentioned:
surface_form: ben wyvis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.679119444444
lon: -4.5792194444444
Name. The name 'Ben Wyvis' is believed to come from, which probably means &quot;high or lofty mountain&quot;, from the same root as &quot;uasal&quot; (noble, lofty). Another suggestion is that it comes from &quot;Beinn Uabhas&quot;, &quot;mountain of terror&quot;. Landscape.

Geographic entities mentioned:
surface_form: ben wyvis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.679119444444
lon: -4.5792194444444
Landscape. Ben Wyvis is a large winding and undulating ridge running roughly north–south for about 5 km, the highest point of which is called Glas Leathad Mòr (&quot;the great green slope&quot;) at above sea level. To the south lies the Corbett of Little Wyvis, which is separated from Ben Wyvis by the Bealach Mòr.

Geographic entities mentioned:
surface_form: ben wyvis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.679119444444
lon: -4.5792194444444
During the Ice Age much of Scotland was periodically covered by ice sheets, with glaciers forming in corries and glens. During the final phase of this period, much of Ben Wyvis was covered by ice. The presence of glacial erratic boulders can be interpreted as marking the upper extent of the ice sheet, with the top of Ben Wyvis remaining free of ice. History.

Geographic entities mentioned:
surface_form: ben wyvis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.679119444444
lon: -4.5792194444444
surface_form: ben wyvis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.679119444444
lon: -4.5792194444444
This condition they could easily fulfil, as snow was to be found in some of the mountain corries of their property all year round. The Battle of Bealach nam Broig was fought between rival clans near the pass that separates Ben Wyvis from the lower summit of Carn Mòr, which lies to the northwest.

Geographic entities mentioned:
surface_form: ben wyvis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.679119444444
lon: -4.5792194444444
The actual date of the battle is debated, but is thought to be 1452. From the sixteenth century cattle-droving was one of the major economic activities in the highlands, and Ben Wyvis lay near to a major drove road between northwest Scotland and the cattle markets of the south.

Geographic entities mentioned:
surface_form: ben wyvis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.679119444444
lon: -4.5792194444444
Drovers often took a shortcut across the southern flanks of the mountain, following the Allt á Bhealaich Mhòir before crossing the bealach between Ben Wyvis and Little Wyvis then rejoining the main route near Auchterneed. The drove road was still being used into the early twentieth century.

Geographic entities mentioned:
surface_form: ben wyvis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.679119444444
lon: -4.5792194444444
Modern ownership. The southern and western sides of Ben Wyvis are now owned by NatureScot, forming the Ben Wyvis NNR, whilst the northern and eastern flanks form part of a privately owned sporting estate, Wyvis Estate. The lower slopes to the west of the NNR are forested, and owned by Forestry and Land Scotland.

Geographic entities mentioned:
surface_form: ben wyvis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.679119444444
lon: -4.5792194444444
As with all land in Scotland, there is a right of responsible access to most of the land on and surrounding Ben Wyvis under the Scottish Outdoor Access Code for people wishing to undertake pursuits such as walking, cycling, horse-riding and wild camping: this applies regardless of whether the land is in public or private ownership. Nature and conservation.

Geographic entities mentioned:
surface_form: ben wyvis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.679119444444
lon: -4.5792194444444
surface_form: ben wyvis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.679119444444
lon: -4.5792194444444
Nature and conservation. Ben Wyvis is home to over 170 plant species, including the nationally scarce dwarf birch, as well as other rare species, such as alpine foxtail. The summit ridge of Ben Wyvis is carpeted moss-heath, forming one of the longest single tracts of this habitat anywhere in Britain.

Geographic entities mentioned:
surface_form: ben wyvis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.679119444444
lon: -4.5792194444444
The area is also home to several species of dragonfly including the large red damselfly and the golden-ringed dragonfly. The mountain is an important breeding ground for the dotterel, which use the moss-heath of the plateau to breed: Ben Wyvis represents at least 2.4% of the breeding population for dotterel in Great Britain.

Geographic entities mentioned:
surface_form: ben wyvis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.679119444444
lon: -4.5792194444444
Ptarmigan also breed on upland areas of the reserve, nesting in higher areas among the boulders and scree. Other birds at Ben Wyvis include golden plover, red grouse and ravens, as well as birds of prey such as peregrine falcon and golden eagle. Deer are common at Ben Wyvis, with red deer in particular being frequently seen.

Geographic entities mentioned:
surface_form: ben wyvis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.679119444444
lon: -4.5792194444444
Other mammals at Ben Wyvis include mountain hare on the open slopes, and pine marten in the woodland. Deer numbers are managed via an annual cull in order to reduce grazing pressures on vegetation. Culling at Ben Wyvis is undertaken by a leaseholder, who rents the deer stalking rights from NatureScot. Ben Wyvis National Nature Reserve.

Geographic entities mentioned:
surface_form: ben wyvis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.679119444444
lon: -4.5792194444444
surface_form: ben wyvis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.679119444444
lon: -4.5792194444444
Ben Wyvis National Nature Reserve. The Ben Wyvis National Nature Reserve encompasses the western and southern slopes of Ben Wyvis, and the summit plateau of Glas Leathad Mòr, which stands at 1,046 metres above sea level. Managed by NatureScot, the reserve contains a range of important habitats for wildlife, as well as important geological features.

Geographic entities mentioned:
surface_form: ben wyvis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.679119444444
lon: -4.5792194444444
In 1996 the boundary was altered again, excluding land that was not owned by NatureScot from the reserve. The NNR is classified as a Category II protected area by the International Union for Conservation of Nature. Ben Wyvis is also designated as a Special Protection Area (SPA), a Special Area of Conservation (SAC), and a Site of Special Scientific Interest (SSSI). Tourism.

Geographic entities mentioned:
surface_form: ben wyvis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.679119444444
lon: -4.5792194444444
On the summit plateau, however, NatureScot have trialled an alternative method, encouraging the use of a single route to allow bare areas to recover by removing loose stones and transplanting small sections of vegetation. During the 1980s there were proposals for the construction of downhill skiing infrastructure on Ben Wyvis.

Geographic entities mentioned:
surface_form: ben wyvis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.679119444444
lon: -4.5792194444444
Powwow Pond. Powwow Pond is a water body in Rockingham County in southeastern New Hampshire, United States. It is classified as an artificial impoundment. The outlet of the pond is located in the town of East Kingston, but most of the lake lies in the town of Kingston. The Powwow River, the outlet of the pond, flows to the Merrimack River in Amesbury, Massachusetts.

Geographic entities mentioned:
surface_form: powwow pond
instance_of: Lake
countries: United States
coordinates: lat: 42.914166666667
lon: -71.035555555556
Topography. Seen from the west, Watson's Dodd is a noticeable shoulder on the Helvellyn ridge, north of Sticks Pass. The summit stands on the main ridge of the Helvellyn range at the point where the south-west ridge of Great Dodd and the north-west ridge of Stybarrow Dodd meet and merge. From this point a shoulder drops into the valley of the How Beck at Legburthwaite.

Geographic entities mentioned:
surface_form: Great Dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
surface_form: Stybarrow Dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.56105
lon: -3.0175111111111
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
Its highest point, at the western apex of the triangle, is marked by a small cairn. The view from the summit is ‘sumptuous’. Standing to the west of the main ridge, the summit gives a panoramic view from Blencathra and Skiddaw in the north, round to the Coniston group in the south. The view extends over Thirlmere to the central fells, and is bounded by the western and northwestern fells.

Geographic entities mentioned:
surface_form: skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
surface_form: blencathra
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.63985
lon: -3.0504611111111
Thomas West in 1778 referred to the valley ‘nobly terminated by the castle-like rock of St. John’. Jonathan Otley in 1823 knew the rock as ‘the massive rock of Green Crag, sometimes called the Castle Rock of St. John's’. The Scottish lawyer and novelist Sir Walter Scott, wrote his romantic narrative-poem &quot;The Bridal of Triermain&quot; in 1812.

Geographic entities mentioned:
surface_form: green crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.3739
lon: -3.2325
surface_form: castle rock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.948611111111
lon: -3.2008333333333
Watson's Dodd. Watson's Dodd is a fell in the English Lake District, a minor rise on the main ridge of the Helvellyn range in the Eastern Fells, but a prominent shoulder on the west side of that range. At its foot is the imposing crag of Castle Rock, on which rock climbers have developed some 60 named routes. Topography.

Geographic entities mentioned:
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: watson's dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5672
lon: -3.02849
At its foot is the imposing crag of Castle Rock, on which rock climbers have developed some 60 named routes. Topography. Seen from the west, Watson's Dodd is a noticeable shoulder on the Helvellyn ridge, north of Sticks Pass. The summit stands on the main ridge of the Helvellyn range at the point where the south-west ridge of Great Dodd and the north-west ridge of Stybarrow Dodd meet and merge.

Geographic entities mentioned:
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: watson's dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5672
lon: -3.02849
There are no marked paths up the fellside. Keeping to the crest of the ridge (after avoiding the initial rocky crags, or after visiting Castle Rock if wished) leads unfailingly to the summit cairn. The summit may also be visited by following the well-used paths along the main Helvellyn ridge, though many ridge walkers appear to bypass the summit. Geology.

Geographic entities mentioned:
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
This formation must represent a series of eruptions of truly exceptional magnitude, accompanying the formation of a volcanic caldera, probably in the area around where Helvellyn stands today. On Watson's Dodd this formation is represented by two members. The Tarn Crags Member makes up Castle Rock, as well as a thin layer higher up the fellside at about the 650 m contour.

Geographic entities mentioned:
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
Geology. The rocks of Watson's Dodd are all part of the Borrowdale Volcanic Group, formed on the margin of an ancient continent during a period of intense volcanic activity, roughly 450 million years ago in the Ordovician Period. Within that group, the bulk of the rocks forming the fell belong to the Birker Fell Andesite Formation.

Geographic entities mentioned:
surface_form: borrowdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.42
lon: -2.665
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
Within that group, the bulk of the rocks forming the fell belong to the Birker Fell Andesite Formation. These rocks are among the earliest of the volcanic rocks of the Borrowdale Volcanic Group, and are part of a thick succession of andesite sheets which now outcrop in a wide band around the western and northern sides of the Lake District.

Geographic entities mentioned:
surface_form: borrowdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.42
lon: -2.665
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Watson's Dodd. Watson's Dodd is a fell in the English Lake District, a minor rise on the main ridge of the Helvellyn range in the Eastern Fells, but a prominent shoulder on the west side of that range. At its foot is the imposing crag of Castle Rock, on which rock climbers have developed some 60 named routes. Topography.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: watson's dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5672
lon: -3.02849
Just before reaching the valley, part of this shoulder rises again to the high, precipitous crag known as Castle Rock. On the eastern side of the ridge the deep valley of Browndale Beck separates Great Dodd from Stybarrow Dodd, so that Watson's Dodd has no eastern flanks at all other than its triangular summit plateau.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: stybarrow dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.56105
lon: -3.0175111111111
surface_form: watson's dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5672
lon: -3.02849
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
On the eastern side of the ridge the deep valley of Browndale Beck separates Great Dodd from Stybarrow Dodd, so that Watson's Dodd has no eastern flanks at all other than its triangular summit plateau. The highest point on Watson's Dodd has an elevation of, a prominence of only above the slight depression separating it from Stybarrow Dodd.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: stybarrow dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.56105
lon: -3.0175111111111
surface_form: watson's dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5672
lon: -3.02849
The highest point on Watson's Dodd has an elevation of, a prominence of only above the slight depression separating it from Stybarrow Dodd. Watson's Dodd stands on the main watershed between the Derwent river system to the west, and Ullswater (and the Eden river system) to the east. Streams on the west are now captured by a water leat and diverted into Thirlmere reservoir. Castle Rock.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: watson's dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5672
lon: -3.02849
The summit of Castle Rock has an elevation of, with a prominence of from the fellside behind it. Summit. The summit of Watson's Dodd is a grassy triangular plateau which slopes gently to the east and is bounded by paths on all three sides. Its highest point, at the western apex of the triangle, is marked by a small cairn. The view from the summit is ‘sumptuous’.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
This rock weathers to a white or pink colour, but it is covered by the smooth grassy turf characteristic of Great Dodd, Watson's Dodd and Stybarrow Dodd, all of which are covered by the same sheet. Names. Watson's Dodd.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: stybarrow dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.56105
lon: -3.0175111111111
surface_form: watson's dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5672
lon: -3.02849
surface_form: watson's dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5672
lon: -3.02849
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
Names. Watson's Dodd. Dod or dodd is a dialect word of unknown origin, but is common in hill names in the Lake District and the Scottish Borders for bare rounded summits, either free standing or subsidiary shoulders to higher neighbours. The Watson whose name this fell commemorates is unknown. There may (or may not) be a connection with Watson's Park in the same parish of St John's.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
In the area to the north of Sticks Pass the Birker Fell andesites are overlain by the Lincomb Tarns Tuff Formation. This formation is one of the most widespread of the volcanic rocks of the Lake District; it seems that the whole district was buried beneath at least 150 m of densely welded ignimbrite, a rock formed from pyroclastic flows of very hot gas and rock.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Names. Watson's Dodd. Dod or dodd is a dialect word of unknown origin, but is common in hill names in the Lake District and the Scottish Borders for bare rounded summits, either free standing or subsidiary shoulders to higher neighbours. The Watson whose name this fell commemorates is unknown. There may (or may not) be a connection with Watson's Park in the same parish of St John's.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Watson's Dodd. Watson's Dodd is a fell in the English Lake District, a minor rise on the main ridge of the Helvellyn range in the Eastern Fells, but a prominent shoulder on the west side of that range. At its foot is the imposing crag of Castle Rock, on which rock climbers have developed some 60 named routes. Topography.

Geographic entities mentioned:
surface_form: castle rock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.948611111111
lon: -3.2008333333333
This shoulder, part of the High Fells of St John's Common, is sharply defined by the deep valleys of Mill Gill to its north and Stanah Gill to its south. It slopes gently to around the 500 m contour, and then drops more steeply into the valley over a number of rocky crags. Just before reaching the valley, part of this shoulder rises again to the high, precipitous crag known as Castle Rock.

Geographic entities mentioned:
surface_form: castle rock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.948611111111
lon: -3.2008333333333
Watson's Dodd stands on the main watershed between the Derwent river system to the west, and Ullswater (and the Eden river system) to the east. Streams on the west are now captured by a water leat and diverted into Thirlmere reservoir. Castle Rock. Standing at the top of the Vale of St John's, the nearly vertical Castle Rock juts out from the hillside with rock faces on three sides.

Geographic entities mentioned:
surface_form: castle rock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.948611111111
lon: -3.2008333333333
Streams on the west are now captured by a water leat and diverted into Thirlmere reservoir. Castle Rock. Standing at the top of the Vale of St John's, the nearly vertical Castle Rock juts out from the hillside with rock faces on three sides. The castle-like profile is made still more picturesque by a garland of mixed woodland around the lower slopes.

Geographic entities mentioned:
surface_form: castle rock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.948611111111
lon: -3.2008333333333
Triermain was the name of a fiefdom in the barony of Gilsland in north-east Cumberland; a pele-tower near Birdoswald still bears the name. The association with Walter Scott's poem has sometimes led Castle Rock to be called Castle Rock of Triermain, especially by rock climbers in order to distinguish it from another Castle Rock in Gloucestershire.

Geographic entities mentioned:
surface_form: castle rock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.948611111111
lon: -3.2008333333333
surface_form: castle rock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.948611111111
lon: -3.2008333333333
surface_form: castle rock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.948611111111
lon: -3.2008333333333
There are no marked paths up the fellside. Keeping to the crest of the ridge (after avoiding the initial rocky crags, or after visiting Castle Rock if wished) leads unfailingly to the summit cairn. The summit may also be visited by following the well-used paths along the main Helvellyn ridge, though many ridge walkers appear to bypass the summit. Geology.

Geographic entities mentioned:
surface_form: castle rock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.948611111111
lon: -3.2008333333333
On Watson's Dodd this formation is represented by two members. The Tarn Crags Member makes up Castle Rock, as well as a thin layer higher up the fellside at about the 650 m contour. It is a coarse-grained dacitic lapilli tuff. Above this thin layer are rocks of the Thirlmere Tuff Member, which covers the top of the fell.

Geographic entities mentioned:
surface_form: castle rock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.948611111111
lon: -3.2008333333333
Atigun Gorge. Atigun Gorge is a valley located along the Atigun River, 2 miles east of Galbraith Lake in northern Alaska. It was first named in 1971. It is an important travel corridor for wildlife within the Arctic National Wildlife Refuge, and is specifically valuable to Dall sheep. It is also a popular hiking destination.

Geographic entities mentioned:
surface_form: Atigun River
instance_of: Watercourse
countries: United States
coordinates: lat: 68.1219444
lon: -149.4591667
surface_form: Galbraith Lake
instance_of: Lake
countries: United States
coordinates: lat: 68.4584432
lon: -149.416606
surface_form: atigun gorge
instance_of: Valley
countries: United States
coordinates: lat: 68.521111111111
lon: -149.08972222222
Atigun Gorge. Atigun Gorge is a valley located along the Atigun River, 2 miles east of Galbraith Lake in northern Alaska. It was first named in 1971. It is an important travel corridor for wildlife within the Arctic National Wildlife Refuge, and is specifically valuable to Dall sheep. It is also a popular hiking destination.

Geographic entities mentioned:
surface_form: atigun gorge
instance_of: Valley
countries: United States
coordinates: lat: 68.521111111111
lon: -149.08972222222
The entire massif is contained within the canton of Bern, as it lies north of the main crest and water divide of the Bernese Alps. To the west, it is connected with the Doldenhorn group via the Fründenhorn; to the east, it is continued by the Gspaltenhorn. To the south, it is connected to the main crest by the Tschingel Pass.

Geographic entities mentioned:
surface_form: Doldenhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.468611111111
lon: 7.735
surface_form: Fründenhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.476944444444
lon: 7.7575
surface_form: Gspaltenhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.511388888889
lon: 7.8277777777778
To the west, it is connected with the Doldenhorn group via the Fründenhorn; to the east, it is continued by the Gspaltenhorn. To the south, it is connected to the main crest by the Tschingel Pass. Ascent is from the ' (2,840 m), over the glacier, past the Wildi Frau (3,274 m)
Geography.

Geographic entities mentioned:
surface_form: Wildi Frau
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.504166666667
lon: 7.78
Ascent is from the ' (2,840 m), over the glacier, past the Wildi Frau (3,274 m)
Geography. The Blüemlisalp forms a ridge of great height, cut away in precipices on the southeast side, surmounted by four principal peaks, in the following order, reckoning from east to west: Morgenhorn (3,620 m), Wyssi Frau (3,648 m), the Blüemlisalphorn (3,660 m) and the Oeschinenhorn (3,486 m).

Geographic entities mentioned:
surface_form: Oeschinenhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.483888888889
lon: 7.7669444444444
surface_form: wyssi frau
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.488611111111
lon: 7.7716666666667
surface_form: blüemlisalphorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.488611111111
lon: 7.7716666666667
surface_form: morgenhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.488611111111
lon: 7.7716666666667
surface_form: blüemlisalp
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.488611111111
lon: 7.7716666666667
To the southwest of the last peak, and between it and the Doldenhorn, is a minor summit — the Fründenhorn (3,368 m). In front of the main ridge, as seen from the northwest, e. g. from the Dündenhorn, are seen three minor peaks which project as steep islets of rock from the great glacier-fields that cover that side of the mountain.

Geographic entities mentioned:
surface_form: Doldenhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.468611111111
lon: 7.735
surface_form: Fründenhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.476944444444
lon: 7.7575
In front of the main ridge, as seen from the northwest, e. g. from the Dündenhorn, are seen three minor peaks which project as steep islets of rock from the great glacier-fields that cover that side of the mountain. These are the Wildi Frau (3,274 m), the Ufem Stock (3,222 m), and the Blümlisalp Rothhorn (3,297 m).

Geographic entities mentioned:
surface_form: Dündenhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.520138888889
lon: 7.7296666666667
In front of the main ridge, as seen from the northwest, e. g. from the Dündenhorn, are seen three minor peaks which project as steep islets of rock from the great glacier-fields that cover that side of the mountain. These are the Wildi Frau (3,274 m), the Ufem Stock (3,222 m), and the Blümlisalp Rothhorn (3,297 m).

Geographic entities mentioned:
surface_form: Wildi Frau
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.504166666667
lon: 7.78
surface_form: blümlisalp
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.488611111111
lon: 7.7716666666667
surface_form: ufem stock
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.488611111111
lon: 7.7716666666667
The two main feeders of the Blüemlisalp Glacier (German: &quot;Blüemlisalpgletscher&quot;) flow downwards through the openings between the three last-named summits, but a short branch from the ice-stream that descends between the Wildi Frau and the Ufem Stock turns to the north, and flows into the head of the Kiental.

Geographic entities mentioned:
surface_form: wildi frau
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.504166666667
lon: 7.78
surface_form: ufem stock
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.488611111111
lon: 7.7716666666667
surface_form: blüemlisalp
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.488611111111
lon: 7.7716666666667
To the west, it is connected with the Doldenhorn group via the Fründenhorn; to the east, it is continued by the Gspaltenhorn. To the south, it is connected to the main crest by the Tschingel Pass. Ascent is from the ' (2,840 m), over the glacier, past the Wildi Frau (3,274 m)
Geography.

Geographic entities mentioned:
surface_form: tschingel
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.703722222222
lon: 8.14075
Blüemlisalp. The Blüemlisalp is a massif of the Bernese Alps, in the territory of the municipalities of Kandersteg and Reichenbach im Kandertal. The entire massif is contained within the canton of Bern, as it lies north of the main crest and water divide of the Bernese Alps.

Geographic entities mentioned:
surface_form: blüemlisalp
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.488611111111
lon: 7.7716666666667
5 June 1976 — Varazze to Ozegna,
Stage 16. 6 June 1976 — Castellamonte to Arosio,
Stage 17. 7 June 1976 — Arosio to Verona,
Stage 18. 8 June 1976 — Verona to Longarone,
Stage 19. 9 June 1976 — Longarone to Vajolet Towers,
Stage 20. 10 June 1976 — Vigo di Fassa to Terme di Comano,
Stage 21. 11 June 1976 — Terme di Comano to Bergamo,
Stage 22a. 12 June 1976 — Arcore to Arcore, (ITT)
Stage 22b.

Geographic entities mentioned:
surface_form: Vajolet Towers
instance_of: Mountain
countries: Italy
coordinates: lat: 46.47
lon: 11.624722222222
Geography. The Seohocheon stream flows SSE through Jeongja-dong. Its source is on the south west slopes below Gwanggyo Helipad on the nearby mountain Gwanggyosan, and this stream joins the Hwanggujicheon further south, by Suwon Air Base. The Seohocheon is joined in Jeongja-dong by the Jeongjacheon (also sometimes known as the Yeonghwacheon), which flows SSW from Ilwang Reservoir in Manseok Park.

Geographic entities mentioned:
surface_form: Gwanggyosan
instance_of: Mountain
countries: South Korea
coordinates: lat: 37.344722222222
lon: 127.03388888889
The market price for the starch was (between 17¢ and 35¢ per kg), and the geography of the river and the good performance of his machinery—the output was close to —brought Cooley great prosperity. His good fortune allowed him to dedicate much of his time to exploration of the area as far north as Lake Okeechobee and brought him increasing political influence.

Geographic entities mentioned:
surface_form: Lake Okeechobee
instance_of: Lake
countries: United States
coordinates: lat: 26.933333333333
lon: -80.8
Tangier Grand Lake Wilderness Area. Tangier Grand Lake Wilderness Area is a relatively large wilderness area located within the province of Nova Scotia, Canada, centered on its namesake lake, Tangier Grand Lake, the largest lake in Nova Scotia which does not have direct road access. Description.

Geographic entities mentioned:
surface_form: Tangier Grand Lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.8884
lon: -62.8169
Sarriguren. Sarriguren is a locality located in the municipality of Valle de Egüés, in Navarre province, Spain, Spain. As of 2020, it has a population of 15,665. Sarriguren is the capital of the municipality of Valle de Egüés. Geography. Sarriguren is located east of Pamplona.

Geographic entities mentioned:
surface_form: Valle de Egüés
instance_of: Valley
countries: Spain
coordinates: lat: 42.823722222222
lon: -1.5573611111111
The town sits in a highland area atop a watershed divide. The Ashuelot River, part of the Connecticut River watershed, drains the western side of the town, including Ashuelot Pond in the southwest. Bog Brook drains the center of the town from north to south, flowing into Highland Lake near the southern border.

Geographic entities mentioned:
surface_form: Ashuelot Pond
instance_of: Lake
countries: United States
coordinates: lat: 43.151388888889
lon: -72.149166666667
The lake is part of the Contoocook River watershed, as are Beards Brook and Woodward Brook on the eastern side of town, and by the Contoocook River are therefore part of the Merrimack River watershed. Lovewell Mountain, located northeast of the town center and with an elevation of, is the highest point in town. As Edwin A.

Geographic entities mentioned:
surface_form: Lovewell Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.203611111111
lon: -72.060833333333
Kitchener TFC rebranded from Kitchener SC, Hamilton TFC rebranded from Mount Hamilton Youth SC (Mount Hamilton is also part of the Hamilton United group that competes in League1 Ontario and Mount Hamilton is named after Hamilton Mountain) and DeRo TFC rebranded from DeRo United Futbol Academy, named after former Canadian Toronto FC forward and attacking midfielder Dwayne De Rosario. Broadcasting.

Geographic entities mentioned:
surface_form: Hamilton Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 43.21681
lon: -79.86633
Åraksbø. Åraksbø is a village in Bygland municipality in Agder county, Norway. The village is located on the eastern shore of the Åraksfjorden, about north of the village of Sandnes and about southeast of the village of Ose. The population (2001) of the Åraksbø area was 89. The lake Hovatn and its hydroelectric power plant are located about to the northeast, just north of the village of Litveit.

Geographic entities mentioned:
surface_form: Åraksfjorden
instance_of: Lake
countries: Norway
coordinates: lat: 58.925555555556
lon: 7.7116666666667
Its capital is Vercelli. , it has an area of and a total population of some 176,000. It is an area known for the cultivation of rice. Main sights. In 2003, UNESCO added the Sacred Mountain of Varallo to the World Heritage List. Other historical sights include the Basilica of Sant'Andrea in Vercelli. There are also numerous natural sights in the Valsesia area.

Geographic entities mentioned:
surface_form: Valsesia
instance_of: Valley
countries: Italy
coordinates: lat: 45.816666666667
lon: 8.1333333333333
km and contains the greatest concentration of some of the tallest mountains on Earth. It has four peaks over 8,000 m including K2 (8611 m), Gasherbrum-I (8068 m), Gasherbrum-II (8035 m) and Broad Peak (8051 m), and sixty peaks higher than 7,000 m. The park was placed on the World Heritage Site Tentative List in 2016. Features.

Geographic entities mentioned:
surface_form: K2
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
surface_form: Broad Peak
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.810555555556
lon: 76.568055555556
It covers about in the Central Karakoram mountain range. It varies in altitude from above sea level to the summit of Chogori K2, the world's second highest mountain at. There are three other mountains over, Gasherbrum I (), Gasherbrum II () and phalchanri Broad Peak (), and sixty mountains over.

Geographic entities mentioned:
surface_form: K2
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
It covers about in the Central Karakoram mountain range. It varies in altitude from above sea level to the summit of Chogori K2, the world's second highest mountain at. There are three other mountains over, Gasherbrum I (), Gasherbrum II () and phalchanri Broad Peak (), and sixty mountains over.

Geographic entities mentioned:
surface_form: Gasherbrum I
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.724444444444
lon: 76.696388888889
surface_form: Gasherbrum II
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.7575
lon: 76.652777777778
surface_form: Broad Peak
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.810555555556
lon: 76.568055555556
It may be climbed from the Crimea Pass via Moel Barlwyd, from Blaenau Ffestiniog or Cwm Penamnen to the north. A circular of Cwm Penamnen can be done taking in Y Ro Wen. It may also be combined with its parent peak Manod Mawr, however the pass between these peaks is extremely boggy and there are many mines, air shafts and open quarries in the area.

Geographic entities mentioned:
surface_form: Manod Mawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.9841
lon: -3.90156
surface_form: manod mawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.9948
lon: -3.89753
Moel Penamnen. Moel Penamnen is a mountain just north of Blaenau Ffestiniog, North Wales and forms part of the Moelwynion. It may be climbed from the Crimea Pass via Moel Barlwyd, from Blaenau Ffestiniog or Cwm Penamnen to the north. A circular of Cwm Penamnen can be done taking in Y Ro Wen.

Geographic entities mentioned:
surface_form: moel penamnen
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.01655
lon: -3.9154888888889
The Shu Capital Rhapsody described the city of Chengdu and the surrounding area. This work features the earliest surviving reference to Mount Emei. The work was so highly renowned and frequently copied upon its release that the price of paper in Luoyang is said to have risen as a result.

Geographic entities mentioned:
surface_form: Mount Emei
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 29.519722222222
lon: 103.3325
Training. During the Joseon era, the area of Namsan's Bokrok (present-day Yejang-dong and Jangchung-dong) was entirely military camps. The current Hanok Village was the headquarters of the Eoyeongcheong (어영청), and Jangchungdan Park was the headquarters of the Geumwiyeong (금위영), known as the &quot;18 Martial Arts Acres&quot; (십팔기터).

Geographic entities mentioned:
surface_form: Namsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 37.54968111
lon: 126.99191083
It is a volcanic field that takes the form of a large cinder cone field, with numerous shield volcanoes and maars. Pico de Tancítaro (3860 m) is the highest peak. The volcanic field is best known for the 18th-century eruption of Jorullo volcano, and 20th-century eruption of Parícutin volcano. Morphology.

Geographic entities mentioned:
surface_form: Pico de Tancítaro
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.416333333333
lon: -102.3195
It is a volcanic field that takes the form of a large cinder cone field, with numerous shield volcanoes and maars. Pico de Tancítaro (3860 m) is the highest peak. The volcanic field is best known for the 18th-century eruption of Jorullo volcano, and 20th-century eruption of Parícutin volcano. Morphology.

Geographic entities mentioned:
surface_form: Parícutin
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.493
lon: -102.251
There are an average of 2.5 cinder cones every 2. El Jorullo — 1759−1774. El Jorullo volcano began on September 29, 1759. Earthquakes occurred prior to this first day of the eruption. Once the cinder cone started erupting, it continued for 15 years, eventually stopping in 1774. El Jorullo destroyed what had been a rich agricultural area.

Geographic entities mentioned:
surface_form: El Jorullo
instance_of: Mountain
countries: Mexico
coordinates: lat: 18.972
lon: -101.718
El Parícutin — 1943−1952. The Parícutin volcano began as a fissure in a cornfield owned by a Purépecha farmer, Dionisio Pulido, on February 20, 1943. Pulido, his wife, and their son all witnessed the initial eruption of ash and stones first-hand as they ploughed the field. El Parícutin grew quickly, reaching five stories tall in just a week, and it could be seen from afar in a month.

Geographic entities mentioned:
surface_form: Parícutin
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.493
lon: -102.251
Ukko (island). Ukko () is an island in Lake Inari, Finnish Lapland. The area of the lake is called Ukonselkä. Ukko was considered by the local Inari Sámi to be an extremely important &quot;sieidi&quot; (,), or sacred natural formation, and was used as a sacrificial site, perhaps as recently as in the 19th century.

Geographic entities mentioned:
surface_form: Lake Inari
instance_of: Lake
countries: Finland
coordinates: lat: 68.9596511
lon: 27.6017069
Mount Mangin (Antarctica). Mount Mangin is a mountain, high, standing northeast of Mount Barre on Adelaide Island, Antarctica. It was discovered by the French Antarctic Expedition, 1908–10, and named by Jean-Baptiste Charcot for the noted French botanist Louis A. Mangin.

Geographic entities mentioned:
surface_form: Mount Barre
instance_of: Mountain
coordinates: lat: -67.5
lon: -68.55
surface_form: mangin
instance_of: Mountain
coordinates: lat: -67.4167
lon: -68.4333
surface_form: mount mangin
instance_of: Mountain
coordinates: lat: -67.4167
lon: -68.4333
Mount Mangin (Antarctica). Mount Mangin is a mountain, high, standing northeast of Mount Barre on Adelaide Island, Antarctica. It was discovered by the French Antarctic Expedition, 1908–10, and named by Jean-Baptiste Charcot for the noted French botanist Louis A. Mangin.

Geographic entities mentioned:
surface_form: mount mangin
instance_of: Mountain
coordinates: lat: -67.4167
lon: -68.4333
surface_form: mangin
instance_of: Mountain
coordinates: lat: -67.4167
lon: -68.4333
Mount Mangin (Antarctica). Mount Mangin is a mountain, high, standing northeast of Mount Barre on Adelaide Island, Antarctica. It was discovered by the French Antarctic Expedition, 1908–10, and named by Jean-Baptiste Charcot for the noted French botanist Louis A. Mangin.

Geographic entities mentioned:
surface_form: mangin
instance_of: Mountain
coordinates: lat: -67.4167
lon: -68.4333
Fore (County Westmeath barony). Fore () is a barony in northern County Westmeath, Ireland. It was formed by 1672. Geography. Fore has an area of 49,056 acres, making it the largest barony in Westmeath but placing it among the smaller baronies in Ireland. Mullaghmeen, the highest point in Westmeath is located in Fore and at 261 metres (856 ft) is the lowest county high point in Ireland.

Geographic entities mentioned:
surface_form: Mullaghmeen
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.761388888889
lon: -7.2875
Mullaghmeen, the highest point in Westmeath is located in Fore and at 261 metres (856 ft) is the lowest county high point in Ireland. The barony contains three large lakes, Lough Derravaragh, Lough Sheelin and Lough Lene and the River Inny flows through the barony before it connects to the River Shannon. The barony borders the counties of Cavan, Longford and Meath. Civil parishes of the barony.

Geographic entities mentioned:
surface_form: Lough Derravaragh
instance_of: Lake
countries: Ireland
coordinates: lat: 53.6526
lon: -7.3587
surface_form: Lough Sheelin
instance_of: Lake
countries: Ireland
coordinates: lat: 53.8
lon: -7.3166666666667
surface_form: Lough Lene
instance_of: Lake
countries: Ireland
coordinates: lat: 53.664722222222
lon: -7.2369444444444