Sarmila/GeoWiki-Features huggingface dataset:
Two attempts were made to mine mineral veins in the rocks of Great Dodd, but neither attempt was successful. Topography. Three ridges lead from the rounded summit of Great Dodd. The west ridge leads over the shoulder called Little Dodd, and then turns north-west to the rocky pinnacle of Calfhow Pike and to the col separating Great Dodd from Clough Head.

Geographic entities mentioned:
surface_form: Clough Head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.593261111111
lon: -3.0337888888889
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: clough head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.593261111111
lon: -3.0337888888889
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
The more southerly ridge heads over High Brow (), fringed by Dowthwaite Crag which broods over the road-end settlement of Dowthwaitehead. The further tops of Low How () and Cockley Moor () are passed before this branch of the ridge peters out in extensive conifer plantations, and then the ground climbs again to Great Mell Fell.

Geographic entities mentioned:
surface_form: Great Mell Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.62
lon: -2.933
surface_form: great mell fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.62
lon: -2.933
There are no tarns on Great Dodd, and very few exposures of rock. Small crags do line the lower western slopes above St John's in the Vale. Lad Knott is the most prominent of these, and the deep ravine of Mill Gill also exposes the rock. On the north-east ridge Randerside, Wolf Crags and Dowthwaite Crag all display the rocks. Routes.

Geographic entities mentioned:
surface_form: St John's in the Vale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.593
lon: -3.06
surface_form: st john's in the vale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.593
lon: -3.06
Great Dodd (meaning: &quot;big round hill&quot;) is a mountain or fell in the English Lake District. It stands on the main ridge of the Helvellyn range, a line of mountains which runs in a north–south direction between the lakes of Thirlmere and Ullswater in the east of the Lake District. Great Dodd, with a height of is the highest of the fells in this range to the north of Sticks Pass.

Geographic entities mentioned:
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Alternative routes begin by following the Old Coach Road, either to the path alongside Groove Beck and up Randerside, or into Mosedale from near the Mariel Bridge and up to Calfhow Pike. This unsurfaced road provides a fine walking route from Dockray around the northern end of the Helvellyn range to the Vale of St John. The close up view of Wolf Crags is particularly good.

Geographic entities mentioned:
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
The close up view of Wolf Crags is particularly good. Great Dodd may also be included in a circular walk around Deepdale known as The Dodds. Or it may be included in a ridge walk, along the main Helvellyn ridge. The ridge path in either direction is broad and clear, with a shortcut contouring to the west of Great Dodd's summit which suggests that many ridge walkers bypass the summit. Summit.

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 what is now Helvellyn.

Geographic entities mentioned:
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
Together, these three are sometimes called ‘The Three Dodds’. These three are made of volcanic rocks of the Borrowdale Volcanic Group, and the tops of all three are covered by the same sheet of rock, which was formed in a series of huge volcanic explosions accompanying the formation of a volcanic caldera about 450 million years ago.

Geographic entities mentioned:
surface_form: borrowdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.42
lon: -2.665
Geology. The rocks of Great 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
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
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, and probably underlie much of the other volcanic rocks.

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
Great Dodd. Great Dodd (meaning: &quot;big round hill&quot;) is a mountain or fell in the English Lake District. It stands on the main ridge of the Helvellyn range, a line of mountains which runs in a north–south direction between the lakes of Thirlmere and Ullswater in the east of the Lake District.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
Great Dodd, with a height of is the highest of the fells in this range to the north of Sticks Pass. Walkers may approach Great Dodd from either High Row near Dockray to the east, or from Legburthwaite to the west – or along the main ridge track from either north or south. Scramblers with climbing skills may be attracted to three gill climbs on the western side of the mountain.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
These three are made of volcanic rocks of the Borrowdale Volcanic Group, and the tops of all three are covered by the same sheet of rock, which was formed in a series of huge volcanic explosions accompanying the formation of a volcanic caldera about 450 million years ago. Two attempts were made to mine mineral veins in the rocks of Great Dodd, but neither attempt was successful. Topography.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
Two attempts were made to mine mineral veins in the rocks of Great Dodd, but neither attempt was successful. Topography. Three ridges lead from the rounded summit of Great Dodd. The west ridge leads over the shoulder called Little Dodd, and then turns north-west to the rocky pinnacle of Calfhow Pike and to the col separating Great Dodd from Clough Head.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
Although it has little prominence, it is a pleasant top giving good views of the surrounding grassy slopes and the valleys below. A short south-west ridge leads to Watson's Dodd, where it merges with the north-west ridge of Stybarrow Dodd to drop into the valley at Legburthwaite. To the north-east a long ridge leads to the subsidiary stony top of Randerside ().

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
Its western slopes used to drain into St John's Beck, a tributary of the River Greta, which in turn joins the River Derwent at Keswick. When Thirlmere Reservoir was constructed in the late 19th century, two of Great Dodd's western streams, Ladknott Gill and Mill Gill, were captured by a water leat and diverted into the new reservoir.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
When Thirlmere Reservoir was constructed in the late 19th century, two of Great Dodd's western streams, Ladknott Gill and Mill Gill, were captured by a water leat and diverted into the new reservoir. The northern slopes of Great Dodd drain either into Mosedale and Mosedale Beck or into Trout Beck. These also flow into the River Greta (via the River Glenderamackin) and then to the Derwent.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
The northern slopes of Great Dodd drain either into Mosedale and Mosedale Beck or into Trout Beck. These also flow into the River Greta (via the River Glenderamackin) and then to the Derwent. However, the eastern and southern slopes of Great Dodd drain into Deepdale and Aira Beck, which flows into Ullswater. The lake drains into the River Eamont, which then joins the River Eden near Penrith.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.264
lon: -2.432
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.54
lon: -1.99
This is the head stream for the famous waterfall of Aira Force, a popular tourist sight. Similarly, Groove Beck, which rises on Matterdale Common, the north-east ridge of Great Dodd, becomes Thornsgill Beck and then Trout Beck, before joining the River Glenderamackin. There are no tarns on Great Dodd, and very few exposures of rock.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
Similarly, Groove Beck, which rises on Matterdale Common, the north-east ridge of Great Dodd, becomes Thornsgill Beck and then Trout Beck, before joining the River Glenderamackin. There are no tarns on Great Dodd, and very few exposures of rock. Small crags do line the lower western slopes above St John's in the Vale.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
On the north-east ridge Randerside, Wolf Crags and Dowthwaite Crag all display the rocks. Routes. Nearly all of Great Dodd (above the intake walls in the valleys) is Open Access land. The north-east ridge is part of Matterdale Common, owned by the National Trust. Ascents of Great Dodd can begin either from Legburthwaite to the west, or from High Row (near Dockray) to the east.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
Routes. Nearly all of Great Dodd (above the intake walls in the valleys) is Open Access land. The north-east ridge is part of Matterdale Common, owned by the National Trust. Ascents of Great Dodd can begin either from Legburthwaite to the west, or from High Row (near Dockray) to the east. Parking is available at both places. From Legburthwaite several routes are possible.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
Parking is available at both places. From Legburthwaite several routes are possible. A path above the ravine of Mill Gill, on its north side, leads to the cairn on Little Dodd. Ladknott Gill can be followed upwards. Or the old shepherds’ path leads from above Fornside to Calfhow Pike.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
There is no public access to this from Fornside, but it can be reached by following the intake wall north from Mill Gill. For scramblers with climbing skills and a rope, three gills on the west side of Great Dodd are accessible: Mill Gill, Beckthorns Gill and the deeply recessed Sandbed Gill. Walkers should keep out of the gills themselves.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
The close up view of Wolf Crags is particularly good. Great Dodd may also be included in a circular walk around Deepdale known as The Dodds. Or it may be included in a ridge walk, along the main Helvellyn ridge. The ridge path in either direction is broad and clear, with a shortcut contouring to the west of Great Dodd's summit which suggests that many ridge walkers bypass the summit. Summit.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
Summit. The summit area of Great Dodd is a short rounded ridge, covered with grass but with many stones lying among it, and with the highest point at the north-west end where there is a cairn. This was not present in 1955 when Alfred Wainwright published his Pictorial Guide. The original cairn is a substantial affair, about south of the highest point, and it incorporates a wind shelter.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
Better views may be had by walking a short distance from the summit in any direction. Much of the Lake District, the hills of south-west Scotland, the Eden Valley and the Pennine Hills may be seen on a clear day. Another small cairn lies part way down the western slope on the path to Clough Head, marking the minor top of Little Dodd. Geology.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: clough head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.593261111111
lon: -3.0337888888889
Individual lava flows may be separated by beds of volcaniclastic sandstone, sedimentary deposits formed from the erosion of the volcanic rocks and deposited by streams, floods and possibly wind. The geological map shows a number of areas of volcaniclastic sandstone on the western slopes of Great Dodd, above Beckthorns and Fornside.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
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. Towards the end of, or after the cessation of the volcanic activity, a large granite batholith was emplaced beneath the volcanic rocks of the Lake District.

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
Associated with the granite batholith was the creation of numerous mineral veins. There is evidence of historic mining activity in two locations on Great Dodd in efforts to exploit such mineral veins. Fornside Mine on the western slopes consisted of two levels, one of which shows signs of copper ore, the other was on a barren quartz vein.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
Names. Great Dodd may originally have been &quot;Dodd Fell&quot;, the name shown on Donald's map of 1771 and Ford's map of 1839, though it is not known in pre-18th century sources. It did not need to be distinguished from its neighbours since Stybarrow Dodd seems to have been known in earlier times simply as &quot;Stybarrow&quot;, and Watson's Dodd is probably only an 18th-century name.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: dodd fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.2564
lon: -2.24633
Names. Great Dodd may originally have been &quot;Dodd Fell&quot;, the name shown on Donald's map of 1771 and Ford's map of 1839, though it is not known in pre-18th century sources. It did not need to be distinguished from its neighbours since Stybarrow Dodd seems to have been known in earlier times simply as &quot;Stybarrow&quot;, and Watson's Dodd is probably only an 18th-century name.

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
The west ridge leads over the shoulder called Little Dodd, and then turns north-west to the rocky pinnacle of Calfhow Pike and to the col separating Great Dodd from Clough Head. Calfhow Pike would have little significance in more rugged areas of the Lake District, but here in the midst of smooth green slopes it is a conspicuous landmark visible for miles around.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
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 of densely welded ignimbrite, a rock formed from a pyroclastic flow 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
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. Towards the end of, or after the cessation of the volcanic activity, a large granite batholith was emplaced beneath the volcanic rocks of the Lake District.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Dod or dodd is a dialect word of unknown origin, but 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. Calfhow Pike was referred to as &quot;Calfhou&quot; in a 13th-century source, and &quot;pyke of Cauvey&quot; in the 16th century.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
The lake drains into the River Eamont, which then joins the River Eden near Penrith. The beck in Deepdale undergoes a number of name changes. Beginning as Browndale Beck as it flows through the hanging valley of Deepdale, it becomes Rush Gill as it drops to Dowthwaitehead, and is then called Aira Beck. This is the head stream for the famous waterfall of Aira Force, a popular tourist sight.

Geographic entities mentioned:
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
This unsurfaced road provides a fine walking route from Dockray around the northern end of the Helvellyn range to the Vale of St John. The close up view of Wolf Crags is particularly good. Great Dodd may also be included in a circular walk around Deepdale known as The Dodds. Or it may be included in a ridge walk, along the main Helvellyn ridge.

Geographic entities mentioned:
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
Maja e Shnikut. Maja e Shnikut is a mountain with a height of in northern Albania - it is a part of the Accursed Mountains range. It is just one of the many mountains of the Accursed Mountains range in Albania which are higher than. It is situated northwest of Maja Jezercë – the highest mountain of the Accursed Mountains, and east of the village Nikç.

Geographic entities mentioned:
surface_form: maja jezercë
instance_of: Mountain
countries: Albania
coordinates: lat: 42.44222222222222
lon: 19.81277777777778
surface_form: jezercë
instance_of: Mountain
countries: Albania
coordinates: lat: 42.44222222222222
lon: 19.81277777777778
Maja e Shnikut. Maja e Shnikut is a mountain with a height of in northern Albania - it is a part of the Accursed Mountains range. It is just one of the many mountains of the Accursed Mountains range in Albania which are higher than. It is situated northwest of Maja Jezercë – the highest mountain of the Accursed Mountains, and east of the village Nikç.

Geographic entities mentioned:
surface_form: maja e shnikut
instance_of: Mountain
countries: Albania
coordinates: lat: 42.4726
lon: 19.7369
Lions Head Mountain. Lions Head Mountain is a mountain summit located in the Boundary Ranges of the Coast Mountains, in the U.S. state of Alaska. The peak is situated in the Kakuhan Range, northwest of Juneau, and east of Lynn Canal, on land managed by Tongass National Forest.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: lions head mountain
instance_of: Mountain
countries: United States
coordinates: lat: 58.8775
lon: -135.0644
Lions Head Mountain. Lions Head Mountain is a mountain summit located in the Boundary Ranges of the Coast Mountains, in the U.S. state of Alaska. The peak is situated in the Kakuhan Range, northwest of Juneau, and east of Lynn Canal, on land managed by Tongass National Forest.

Geographic entities mentioned:
surface_form: lions head mountain
instance_of: Mountain
countries: United States
coordinates: lat: 58.8775
lon: -135.0644
state of Alaska. The peak is situated in the Kakuhan Range, northwest of Juneau, and east of Lynn Canal, on land managed by Tongass National Forest. Although modest in elevation, relief is significant since Lions Head Mountain rises 5,400 feet above the Berners River Valley in less than three miles.

Geographic entities mentioned:
surface_form: lions head mountain
instance_of: Mountain
countries: United States
coordinates: lat: 58.8775
lon: -135.0644
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
Board on Geographic Names. Climate. Based on the Köppen climate classification, Lions Head Mountain has a subarctic climate with cold, snowy winters, and cool summers. Weather systems coming off the Gulf of Alaska are forced upwards by the Coast Mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall.

Geographic entities mentioned:
surface_form: lions head mountain
instance_of: Mountain
countries: United States
coordinates: lat: 58.8775
lon: -135.0644
Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports glaciers on the north side of this mountain. The months May through July offer the most favorable weather for viewing or climbing Lions Head Mountain.

Geographic entities mentioned:
surface_form: lions head mountain
instance_of: Mountain
countries: United States
coordinates: lat: 58.8775
lon: -135.0644
Located on the volcano flanks are fumaroles and mudpots. On the southern flank of the volcano, two crater lakes are located, Lakes Danao and Malagsom. Hot Springs are located on the southern shore of Lake Danao (not to be confused with the other Lake Danao which is located near Ormoc City and part of Lake Danao Natural Park). Lake Malagsom is a crater lake with green acidic water.

Geographic entities mentioned:
surface_form: lake danao
instance_of: Lake
countries: Philippines
coordinates: lat: 11.071
lon: 124.694
surface_form: lake danao
instance_of: Lake
countries: Philippines
coordinates: lat: 11.071
lon: 124.694
surface_form: lake danao
instance_of: Lake
countries: Philippines
coordinates: lat: 11.071
lon: 124.694
surface_form: lake danao
instance_of: Lake
countries: Philippines
coordinates: lat: 10.66666667
lon: 124.33333333
surface_form: lake danao
instance_of: Lake
countries: Philippines
coordinates: lat: 10.66666667
lon: 124.33333333
surface_form: lake danao
instance_of: Lake
countries: Philippines
coordinates: lat: 10.66666667
lon: 124.33333333
surface_form: lake danao
instance_of: Lake
countries: Philippines
coordinates: lat: 9.350556
lon: 123.1833
surface_form: lake danao
instance_of: Lake
countries: Philippines
coordinates: lat: 9.350556
lon: 123.1833
surface_form: lake danao
instance_of: Lake
countries: Philippines
coordinates: lat: 9.350556
lon: 123.1833
Mahagnao Volcano. Mahagnao Volcano also known as part of (Mahagnao Volcano Natural Park) is a dormant stratovolcano located in the Barangay Mahagnao part of the municipality of Burauen province of Leyte, Philippines. It is also bounded by the municipalities of La Paz and MacArthur.

Geographic entities mentioned:
surface_form: mahagnao
instance_of: Mountain
countries: Philippines
coordinates: lat: 10.874444444444
lon: 124.85966388889
Mahagnao Volcano. Mahagnao Volcano also known as part of (Mahagnao Volcano Natural Park) is a dormant stratovolcano located in the Barangay Mahagnao part of the municipality of Burauen province of Leyte, Philippines. It is also bounded by the municipalities of La Paz and MacArthur.

Geographic entities mentioned:
surface_form: mahagnao
instance_of: Mountain
countries: Philippines
coordinates: lat: 10.874444444444
lon: 124.85966388889
surface_form: mahagnao
instance_of: Mountain
countries: Philippines
coordinates: lat: 10.874444444444
lon: 124.85966388889
surface_form: mahagnao
instance_of: Mountain
countries: Philippines
coordinates: lat: 10.874444444444
lon: 124.85966388889
Because of numerous streams, rivers and similar kind bodies of water, Burauen has been known with its nicked name as the Spring Capital of Leyte. Mahagnao Volcano Natural Park is about 65 kilometers south of Tacloban City and 18 kilometers away from the town center of Burauen. Physical Features.

Geographic entities mentioned:
surface_form: mahagnao
instance_of: Mountain
countries: Philippines
coordinates: lat: 10.874444444444
lon: 124.85966388889
Although the volcano has been inactive, it is classified as potentially active due to the active thermal features of the mountain. Mahagnao Volcano Natural Park. Mahagnao Volcano is the focal point of the &quot;Mahagnao Volcano National Park&quot; created on August 27, 1937 with &quot;Proclamation No. 184&quot; with an area encompassing.

Geographic entities mentioned:
surface_form: mahagnao
instance_of: Mountain
countries: Philippines
coordinates: lat: 10.874444444444
lon: 124.85966388889
Although the volcano has been inactive, it is classified as potentially active due to the active thermal features of the mountain. Mahagnao Volcano Natural Park. Mahagnao Volcano is the focal point of the &quot;Mahagnao Volcano National Park&quot; created on August 27, 1937 with &quot;Proclamation No. 184&quot; with an area encompassing.

Geographic entities mentioned:
surface_form: mahagnao
instance_of: Mountain
countries: Philippines
coordinates: lat: 10.874444444444
lon: 124.85966388889
surface_form: mahagnao
instance_of: Mountain
countries: Philippines
coordinates: lat: 10.874444444444
lon: 124.85966388889
184&quot; with an area encompassing. Under the &quot;National Integrated Protected Areas System&quot; (NIPAS) of the Department of Environment and Natural Resources, the park was renamed to Mahagnao Volcano Natural Park with &quot;Proclamation No. 1157&quot; on February 3, 1998.

Geographic entities mentioned:
surface_form: mahagnao
instance_of: Mountain
countries: Philippines
coordinates: lat: 10.874444444444
lon: 124.85966388889
Eruptions. An eruption was reported to have occurred in 1895. It is a preatic eruption
Listings. The Philippine Institute of Volcanology and Seismology (PHIVOLCS) classifies Mahagnao as Inactive volcano. Although the volcano has been inactive, it is classified as potentially active due to the active thermal features of the mountain. Mahagnao Volcano Natural Park.

Geographic entities mentioned:
surface_form: mahagnao
instance_of: Mountain
countries: Philippines
coordinates: lat: 10.874444444444
lon: 124.85966388889
Russia. The embassy crossed the Caspian Sea and arrived in Astrakhan, in 1599. Here, Shirley reportedly felt emboldened to act against Melo, believing that the Portuguese friar had less influence under Russian rule. Shirley had Melo imprisoned, confiscating his letters and possessions.

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
Templehouse Lough. Templehouse Lough (; also &quot;Templehouse Lake&quot;) is a freshwater lake in the northwest of Ireland. It is located in south County Sligo and forms part of the course of the Owenmore River. Geography. Templehouse Lough lies about south of Sligo and west of Ballymote. The lake covers in area and is about long from north to south.

Geographic entities mentioned:
surface_form: templehouse lough
instance_of: Lake
countries: Ireland
coordinates: lat: 54.10472222
lon: -8.58916667
The lake drains north into the continuation of the Owenmore River, which then flows north to join the Ballysadare River. Natural history. Fish present in Templehouse Lough include roach, perch, pike and the critically endangered European eel. A number of duck species winter at the lake including teal, wigeon, mallard, tufted duck and goldeneye.

Geographic entities mentioned:
surface_form: templehouse lough
instance_of: Lake
countries: Ireland
coordinates: lat: 54.10472222
lon: -8.58916667
Llamayuq Q'asa (Bolivia). Llamayuq Q'asa (Quechua &quot;llama&quot; llama, &quot;-yuq&quot; a suffix, &quot;q'asa&quot; mountain pass, &quot;mountain pass with llamas&quot;, also spelled &quot;Llamayoj Khasa&quot;) is a mountain in the Bolivian Andes which reaches a height of approximately. It is located in the Cochabamba Department, Ayopaya Province, Cocapata Municipality.

Geographic entities mentioned:
surface_form: llamayuq q'asa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.92
lon: -66.52861111
By the early 1840s, Diwan Hari Chand had become central to Gulab Singh’s military endeavors, often leading expeditions at the frontiers of the expanding Dogra domain. His responsibilities grew as the Dogra kingdom pushed its boundaries northwards into the Himalayas and westwards towards the Indus, reaching as far as Chilas and Yasin in Dardistan.

Geographic entities mentioned:
surface_form: Yasin
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.367777777777775
lon: 73.33777777777777
This bold incursion provoked a strong Tibetan (Qing Chinese) response. Zorawar Singh was met by superior forces near Mansarovar and was killed in battle on 12 December 1841, in the midst of a harsh winter storm. His death led to a dramatic reversal: the Dogra garrisons in Tibet and Ladakh were weakened, and a combined Tibetan-Ladakhi counterattack swiftly materialized.

Geographic entities mentioned:
surface_form: Mansarovar
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 30.666666666667
lon: 81.5
From there, he traveled with Raja Dhian Singh to Jammu. After five or six days, Hari Chand left Jammu and arrived at Mirpur, where he stayed for 15 days while the troops were being armed. He had a total of 6,000 soldiers. They departed from Mirpur and arrived at Uri in Kashmir valley, where they were hosted for 15 days by the &quot;Nazim&quot; of the area. Battle of Kargil Fort.

Geographic entities mentioned:
surface_form: Kashmir valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
The besiegers panicked, but they were reassured by the Diwan and resumed their siege. Four days later, the Diwan noticed a stream flowing into the camp and had it flooded. The new camp was located at Tangtse, on the western end of Pangong Lake. The Tibetans had 3,000 soldiers, but their camp and trenches had been flooded. The besieged soldiers abandoned their camp.

Geographic entities mentioned:
surface_form: Pangong Lake
instance_of: Lake
countries: People's Republic of China
India
coordinates: lat: 33.70472222222222
lon: 78.75
With the throne of the Western Empire vacant, the Alamanni invaded Italy. They moved from Raetia and managed to reach Lake Maggiore on the south side of the Alps. Majorian led his field army north to fight the Alamanni, and defeated them. Reaching an agreement with Ricimer, Majorian was proclaimed emperor on 1 April 457.

Geographic entities mentioned:
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
White River (Wisconsin). The White River is a freshwater tributary located in the counties of Racine and Walworth, Wisconsin, that flows for 19 miles out of Geneva Lake in Lake Geneva to the Fox River in Burlington. The river flows through the 200-acre White River Park, which is managed by the Geneva Lake Conservancy and Walworth County Park System.

Geographic entities mentioned:
surface_form: Geneva Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.59
lon: -88.435
It was forced out of all of Abkhazia in August 2008 during the Russo-Georgian war by the Abkhazian armed forces. Upper Abkhazia is a territory that has population of c. 2,000 (1–1.5% of Abkhazia's post-war population) and is centered on the upper Kodori Valley (roughly 17% of the territory of the former Abkhaz ASSR). History.

Geographic entities mentioned:
surface_form: Kodori Valley
instance_of: Valley
countries: Georgia
coordinates: lat: 43.1
lon: 41.8
Chacon Creek. Chacon Creek is a small stream of water located in Webb County, Texas, US, which runs through Laredo. The creek is formed 6 miles from Webb and runs southwest for 20 miles until it connects to the Rio Grande. Chacon was dammed in 1951 in east Laredo to form Lake Casa Blanca, a 1,680 acres (6.8 km2) lake. The terrain surrounding the creek is mostly clay.

Geographic entities mentioned:
surface_form: Lake Casa Blanca
instance_of: Lake
countries: United States
coordinates: lat: 27.533611111111
lon: -99.448611111111
Mount Arthur (Antarctica). Mount Arthur () is a mountain, 1,290 m, just west of Mount Douglas at the west end of the Scott Mountains, Enderby Land in Antarctica. Plotted from air photos taken from ANARE (Australian National Antarctic Research Expeditions) aircraft in 1956. Named by Antarctic Names Committee of Australia (ANCA) for J. Arthur, electrical fitter at Mawson station in 1960.

Geographic entities mentioned:
surface_form: arthur
instance_of: Mountain
coordinates: lat: -67.65
lon: 49.86667
surface_form: mount arthur
instance_of: Mountain
coordinates: lat: -67.65
lon: 49.86667
Mount Arthur (Antarctica). Mount Arthur () is a mountain, 1,290 m, just west of Mount Douglas at the west end of the Scott Mountains, Enderby Land in Antarctica. Plotted from air photos taken from ANARE (Australian National Antarctic Research Expeditions) aircraft in 1956. Named by Antarctic Names Committee of Australia (ANCA) for J. Arthur, electrical fitter at Mawson station in 1960.

Geographic entities mentioned:
surface_form: arthur
instance_of: Mountain
coordinates: lat: -67.65
lon: 49.86667
surface_form: mount arthur
instance_of: Mountain
coordinates: lat: -67.65
lon: 49.86667
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
Mount Arthur (Antarctica). Mount Arthur () is a mountain, 1,290 m, just west of Mount Douglas at the west end of the Scott Mountains, Enderby Land in Antarctica. Plotted from air photos taken from ANARE (Australian National Antarctic Research Expeditions) aircraft in 1956. Named by Antarctic Names Committee of Australia (ANCA) for J. Arthur, electrical fitter at Mawson station in 1960.

Geographic entities mentioned:
surface_form: arthur
instance_of: Mountain
coordinates: lat: -67.65
lon: 49.86667
Bannock War of 1895. The Bannock War of 1895, or the Bannock Uprising, refers to a minor conflict centered in Jackson Hole, Wyoming, in the United States. During the early 1890s, Wyoming passed a state law prohibiting the killing of elk for their teeth, which led to the arrests of several Bannock hunters in 1895.

Geographic entities mentioned:
surface_form: Jackson Hole
instance_of: Valley
countries: United States
coordinates: lat: 43.516666666667
lon: -110.83333333333
state of Alaska. The Klehini River is about long from its source in British Columbia to its mouth at the Chilkat River, of which it is the largest tributary. The Klehini River is renowned for its salmon runs, its biannual congregation of bald eagles&mdash;the second largest in the Haines area after the Chilkat River's Council Grounds&mdash;and for the Klehini Falls.

Geographic entities mentioned:
surface_form: Chilkat River
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 59.204166666667
lon: -135.47972222222
surface_form: klehini
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 59.39857
lon: -135.92305
state of Alaska. The Klehini River is about long from its source in British Columbia to its mouth at the Chilkat River, of which it is the largest tributary. The Klehini River is renowned for its salmon runs, its biannual congregation of bald eagles&mdash;the second largest in the Haines area after the Chilkat River's Council Grounds&mdash;and for the Klehini Falls.

Geographic entities mentioned:
surface_form: chilkat
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 59.204166666667
lon: -135.47972222222
surface_form: klehini river
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 59.39857
lon: -135.92305
surface_form: klehini
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 59.39857
lon: -135.92305
surface_form: klehini
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 59.39857
lon: -135.92305
The Klehini River is renowned for its salmon runs, its biannual congregation of bald eagles&mdash;the second largest in the Haines area after the Chilkat River's Council Grounds&mdash;and for the Klehini Falls. The Klehini also delineates the northern boundary of the Chilkat Range.

Geographic entities mentioned:
surface_form: chilkat
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 59.204166666667
lon: -135.47972222222
surface_form: klehini
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 59.39857
lon: -135.92305
The name &quot;Klehini&quot; appears to be derived from the Tlingit phrase &quot;l’éiw héeni&quot;, which translates to &quot;river with sand or gravel in it&quot;. The Klehini River contains abundances of both sand and gravel. The lower Klehini is located within the Alaska Chilkat Bald Eagle Preserve. Walt Disney's 1991 rendition of &quot;White Fang&quot; was filmed along the Klehini River.

Geographic entities mentioned:
surface_form: chilkat
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 59.204166666667
lon: -135.47972222222
Klehini River. The Klehini River is a large, glacially fed stream in the vicinity of Haines in the U.S. state of Alaska. The Klehini River is about long from its source in British Columbia to its mouth at the Chilkat River, of which it is the largest tributary.

Geographic entities mentioned:
surface_form: klehini river
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 59.39857
lon: -135.92305
The Klehini also delineates the northern boundary of the Chilkat Range. The name &quot;Klehini&quot; appears to be derived from the Tlingit phrase &quot;l’éiw héeni&quot;, which translates to &quot;river with sand or gravel in it&quot;. The Klehini River contains abundances of both sand and gravel. The lower Klehini is located within the Alaska Chilkat Bald Eagle Preserve.

Geographic entities mentioned:
surface_form: klehini
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 59.39857
lon: -135.92305
The Klehini River contains abundances of both sand and gravel. The lower Klehini is located within the Alaska Chilkat Bald Eagle Preserve. Walt Disney's 1991 rendition of &quot;White Fang&quot; was filmed along the Klehini River. Klehini Falls. The Klehini Falls are a series of four cataracts in far northwestern British Columbia occurring in a narrow gorge near the headwaters of the Klehini River.

Geographic entities mentioned:
surface_form: klehini river
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 59.39857
lon: -135.92305
surface_form: klehini
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 59.39857
lon: -135.92305
surface_form: klehini
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 59.39857
lon: -135.92305
Klehini Falls. The Klehini Falls are a series of four cataracts in far northwestern British Columbia occurring in a narrow gorge near the headwaters of the Klehini River. The falls are separated from one another by a distance of approximately 300 feet (91 m), with an average plunge of 30 to 40 feet (9.1 to 12.2 m). The individual cataracts are currently unnamed. Threats.

Geographic entities mentioned:
surface_form: klehini river
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 59.39857
lon: -135.92305
Fort Ticonderoga Ferry. The Fort Ticonderoga Ferry is a cable ferry crossing Lake Champlain between Ticonderoga, New York, and Shoreham, Vermont. It connects the New York and Vermont segments of State Route 74 The ferry can carry up to 18 cars and has a weight limit of 15 tons. The ferry operates seasonally, from May to October.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
She operated out of Navy Island Royal Naval Shipyard. British service. The British schooner served as a training ship for Canadian seamen on Lake Erie through 1812, in preparation for a campaign to gain control of the Great Lakes and a subsequent invasion of the United States.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
American service. Taken prize at the surrender, the schooner was repaired and joined the American squadron on Lake Erie as USS &quot;Lady Prevost&quot;. In company with &quot;Niagara&quot;, and &quot;Trippe&quot; under command of Captain Jesse D. Elliott, she sailed into Lake St. Clair on 29 September to cut the supply lines of the British Army attempting to invade western New York.

Geographic entities mentioned:
surface_form: Lake St. Clair
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.450265
lon: -82.67572
It is also bordered by one municipality in Buskerud county: Hol to the south-east. Most of the area is composed of fjords and mountains with small populated areas concentrated in the lower river valleys, the largest of which is the Aurlandsdalen. The main village areas include Aurlandsvangen, Gudvangen, Undredal, Flåm, and Vassbygdi.

Geographic entities mentioned:
surface_form: Aurlandsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 60.87416667
lon: 7.38972222
Wild and beautiful nature dominate the community from the fjords to mountaintops that are above sea level. There are two permanent glaciers in Aurland: Storskavlen and Blåskavlen. The Aurlandsfjellet mountains separate Aurland from the neighboring municipality to the east, Lærdal. The Lærdal Tunnel, the longest in the world as of 2014, cuts through the mountains connecting the two municipalities.

Geographic entities mentioned:
surface_form: Aurlandsfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 61.05
lon: 7.34
The Nærøyfjord areas in this site stretch through the municipalities of Aurland, Lærdal, Vik, and Voss. Aurlandsdalen Valley. The Aurlandsdalen valley is a well known hiking trail in Norway with its fabulous nature and contrasting countryside. The valley is rich in history and packed with culture.

Geographic entities mentioned:
surface_form: Aurlandsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 60.87416667
lon: 7.38972222