Sarmila/GeoWiki-Features huggingface dataset:
The rate of subsidence of the caldera was slower at about 5 cm per day and levels of toxic gasses in inhabited areas stayed within safety limits for consistent periods. On 27 February the eruption ended after 6 months of continuous activity. Nevertheless, air pollution continued, and the area north of Bárðarbunga, including volcanoes Askja and Herðubreið, still remained closed to visitors. March.

Geographic entities mentioned:
surface_form: Herðubreið
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.183333333333
lon: -16.35
Southern Fells. rect 23 372 252 419 Slight Side (762 m)
rect 173 794 560 834 Scafell East Buttress
rect 707 787 893 861 Esk Pike or Crag (885 m)
rect 245 303 409 358 Sca Fell (964 m)
rect 408 238 637 280 Mickledore (c.

Geographic entities mentioned:
surface_form: Slight Side (762 m)
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4342
lon: -3.22095
surface_form: Esk Pike or Crag (885 m)
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456219444444
lon: -3.17995
840 m)
rect 544 174 826 213 South Summit (<978 m)
rect 706 310 928 355 Scafell Pike (978 m)
rect 870 238 1108 286 Broad Crag (934 m)
rect 1043 308 1198 360 Ill Crag (935 m)
rect 1238 311 1446 351 Great End (910 m)
rect 0 0 1444 1085 Click hyperlink or button to expand
The Southern Fells are a part of the Cumbrian Mountains in the Lake District of England.

Geographic entities mentioned:
surface_form: South Summit (<978 m)
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454166666667
lon: -3.2115277777778
surface_form: Scafell Pike (978 m)
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454166666667
lon: -3.2115277777778
surface_form: Broad Crag (934 m)
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456838888889
lon: -3.2077388888889
surface_form: Great End (910 m)
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.464
lon: -3.194
Including Scafell Pike, the highest peak in England, they occupy a broad area to the south of Great Langdale, Borrowdale and Wasdale. High and rocky towards the centre of the Lake District, the Southern Fells progressively take on a moorland character toward the south-west. In the south-east are the well-known Furness Fells, their heavily quarried flanks rising above Coniston Water.

Geographic entities mentioned:
surface_form: Scafell Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454166666667
lon: -3.2115277777778
surface_form: Great Langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.449119444444
lon: -3.0733305555556
surface_form: Wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
High and rocky towards the centre of the Lake District, the Southern Fells progressively take on a moorland character toward the south-west. In the south-east are the well-known Furness Fells, their heavily quarried flanks rising above Coniston Water. Partition of the Lakeland fells.

Geographic entities mentioned:
surface_form: Coniston Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.35
lon: -3.0666666666667
The Southern Fells are one of these divisions, covered by volume 4 of Wainwright's work. Boundaries. Of all Wainwright's boundary decisions, the outer perimeter of the Southern Fells is the most often debated. Two ridges continue south west on either side of the Duddon Valley, the longer ending only at the Irish Sea in the terminal height of Black Combe.

Geographic entities mentioned:
surface_form: Black Combe
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.256930555556
lon: -3.3293
Two ridges continue south west on either side of the Duddon Valley, the longer ending only at the Irish Sea in the terminal height of Black Combe. Wainwright however chose to excise a wide area of fell from his guidebooks, declaring that &quot;south and west from Green Crag the scenery quickly deteriorates.

Geographic entities mentioned:
surface_form: Green Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.3739
lon: -3.2325
This summit has therefore been taken as the boundary of fellwalking country for the purposes of this book and the territory southwest omitted from the map&quot;. He makes similar statements regarding the fells to the south of Dow Crag on the parallel Coniston ridge.

Geographic entities mentioned:
surface_form: Dow Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.369438888889
lon: -3.1374388888889
Even Wainwright ultimately relented and included the southern extremities in an eighth guidebook, &quot;The Outlying fells of Lakeland&quot; (1974). The northern boundaries are clear, beginning on the west with Wastwater and rising up beyond the head of Wasdale to Sty Head Pass, the popular walkers' route to Borrowdale. Across the border on this side are Great Gable and the Western Fells.

Geographic entities mentioned:
surface_form: Great Gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
Across the border on this side are Great Gable and the Western Fells. The boundary continues north to Stonethwaite in Borrowdale, before turning sharply south-east along the Langstrath branch of that valley, including the long ridge of Glaramara within the Southern Fells.

Geographic entities mentioned:
surface_form: Glaramara
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483319444444
lon: -3.1653
Topography. The Southern Fells occupy a broad sector of the circular Lake District massif, trending a little to the west of centre and about across in either direction. In addition to the perimeter dales, Eskdale and the Duddon Valley provide further subdivision flowing out from the centre of the district. In the north, surrounding the head of Eskdale, are the Scafells.

Geographic entities mentioned:
surface_form: Duddon Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.297688888889
lon: -3.2347888888889
Also standing above the valleys of Wasdale, Borrowdale and Great Langdale, this high cirque is open to the south and contains England's highest ground. The range begins on the west with Slight Side before rising to the summits of Scafell, Scafell Pike and Great End. Across the gap of Esk Hause and enclosing the eastern side of Eskdale are Esk Pike, Bowfell and Crinkle Crags.

Geographic entities mentioned:
surface_form: Slight Side
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4342
lon: -3.22095
surface_form: Scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
surface_form: Scafell Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454166666667
lon: -3.2115277777778
surface_form: Great End
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.464
lon: -3.194
The range begins on the west with Slight Side before rising to the summits of Scafell, Scafell Pike and Great End. Across the gap of Esk Hause and enclosing the eastern side of Eskdale are Esk Pike, Bowfell and Crinkle Crags. Satellites to this main ridge are Lingmell above Wasdale and the Allen Crags- Glaramara- Rosthwaite Fell ridge jutting deep into Borrowdale.

Geographic entities mentioned:
surface_form: Esk Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456219444444
lon: -3.17995
surface_form: Bowfell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.447369444444
lon: -3.1658194444444
Across the gap of Esk Hause and enclosing the eastern side of Eskdale are Esk Pike, Bowfell and Crinkle Crags. Satellites to this main ridge are Lingmell above Wasdale and the Allen Crags- Glaramara- Rosthwaite Fell ridge jutting deep into Borrowdale. East of Bowfell is Rossett Pike providing the link to the Central Fells.

Geographic entities mentioned:
surface_form: Lingmell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462088888889
lon: -3.2217805555556
surface_form: Allen Crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4661
lon: -3.1802388888889
surface_form: Glaramara
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483319444444
lon: -3.1653
surface_form: Rosthwaite Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.496
lon: -3.15176
Satellites to this main ridge are Lingmell above Wasdale and the Allen Crags- Glaramara- Rosthwaite Fell ridge jutting deep into Borrowdale. East of Bowfell is Rossett Pike providing the link to the Central Fells. More loosely connected are Illgill Head and Whin Rigg, the fells forming the famous Wastwater Screes.

Geographic entities mentioned:
surface_form: Rossett Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.458211111111
lon: -3.1599611111111
East of Bowfell is Rossett Pike providing the link to the Central Fells. More loosely connected are Illgill Head and Whin Rigg, the fells forming the famous Wastwater Screes. South from Crinkle Crags, between Eskdale and the Duddon, are Hard Knott, Harter Fell and Green Crag.

Geographic entities mentioned:
surface_form: Illgill Head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4327
lon: -3.2825694444444
surface_form: Whin Rigg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.41945780200143
lon: -3.3093011327319037
East of Bowfell is Rossett Pike providing the link to the Central Fells. More loosely connected are Illgill Head and Whin Rigg, the fells forming the famous Wastwater Screes. South from Crinkle Crags, between Eskdale and the Duddon, are Hard Knott, Harter Fell and Green Crag.

Geographic entities mentioned:
surface_form: Hard Knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.410539
lon: -3.186436
surface_form: Green Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.3739
lon: -3.2325
South from Crinkle Crags, between Eskdale and the Duddon, are Hard Knott, Harter Fell and Green Crag. A second ridge falls south easterly from Crinkles over Cold Pike and Pike O'Blisco, crosses the motor road of Wrynose Pass and then rises to Great Carrs, the first of the Coniston (or Furness) Fells.

Geographic entities mentioned:
surface_form: Cold Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.421
lon: -3.134
surface_form: Great Carrs
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.3983
lon: -3.12438
A second ridge falls south easterly from Crinkles over Cold Pike and Pike O'Blisco, crosses the motor road of Wrynose Pass and then rises to Great Carrs, the first of the Coniston (or Furness) Fells. The remainder of this group comprises Swirl How, Grey Friar, Wetherlam, Brim Fell, Coniston Old Man and Dow Crag, together forming the watershed between Coniston and the Duddon.

Geographic entities mentioned:
surface_form: Swirl How
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.395661111111
lon: -3.1212305555556
surface_form: Grey Friar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.392761111111
lon: -3.1427111111111
surface_form: Wetherlam
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.401
lon: -3.098
surface_form: Brim Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.3777
lon: -3.12381
surface_form: Dow Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.369438888889
lon: -3.1374388888889
The remainder of this group comprises Swirl How, Grey Friar, Wetherlam, Brim Fell, Coniston Old Man and Dow Crag, together forming the watershed between Coniston and the Duddon. To the east are the low outliers of Holme Fell and Black Fell. Access for walkers.

Geographic entities mentioned:
surface_form: Holme Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.396
lon: -3.056
Bashiqah. 0iccmuyrrtkwgut45dl2swdbx1t6q" xml:space="preserve">Bashiqah Mountain is a mountain located northeast of Mosul, Iraq, east of Khorsabad and nearby Bashiqa township and near Ain Sifni in northern Iraq. The mountain is located behind Bashiqa township, is 359 km north of Baghdad in Nineveh Governorate, and located at 36,4531n and 43,3478e. It is 326 above sea level.

Geographic entities mentioned:
surface_form: bashiqah
instance_of: Mountain
countries: Iraq
The mountain became a strategic point following the Fall of Mosul to ISIS in 2014 but was retaken with the recapture of Mosul in July 2017. The hill was heavily fortified by ISIS. The mountain has since been taken by Kurdish Peshmerga forces. Climate. The climate is Csa under the Köppen-Geiger system, average temperature in Bashiqah is 19.5°C and the average annual rainfall is 572 mm.

Geographic entities mentioned:
surface_form: bashiqah
instance_of: Mountain
countries: Iraq
Eldership was created from the Josvainiai &quot;selsovet&quot; in 1993. Geography. The territory of Josvainiai Eldership is located mostly in the Nevėžis Plain, but the western edges are in the East Samogitian Plateau. Relief is mostly flat, 2/3 of the territory is agriculture lands, about 1/3 is covered by forests.

Geographic entities mentioned:
surface_form: East Samogitian Plateau
instance_of: Plateau
countries: Lithuania
The First Army suddenly had to fight the German troops based in Romania, but was able to hold the Carpathian Mountains passes until Soviet reinforcements arrived. Macici remained at the head of the First Army and participated in the advance in Transylvania and joint Soviet–Romanian attack on Hungary and Slovakia. In the fall of 1944 he fought at battles on the Cerna, Mureș, and Crișul Alb rivers.

Geographic entities mentioned:
surface_form: Crișul Alb
instance_of: Watercourse
countries: Romania
Hungary
coordinates: lat: 46.700277777778
lon: 21.269166666667
Erie people. The Erie people were an Indigenous people of the Northeastern Woodlands historically living on the south shore of Lake Erie. An Iroquoian-speaking tribe, they lived in what is now western New York, northwestern Pennsylvania, and northern Ohio before 1658.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Consequently, in 1654 the whole Iroquois Confederacy went to war against the Erie and neighboring tribes such as the Neutral people along the northern shores of Lake Erie and across the Niagara River, the Tobacco people between the Erie and Iroquois, neighbors to all three groups.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
The mountain is a major andesite volcano, with the magma known for its high levels of Nickel and Chromium. Captain John Moresby named the mountain after the naval battle of Trafalgar. Hydrographers Range, Mount Lamington, and Mount Victory are three other large Quaternary stratovolcanoes in south-eastern New Guinea. Name.

Geographic entities mentioned:
surface_form: Mount Lamington
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -8.95
lon: 148.15
surface_form: victory
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -9.2
lon: 149.06666666667
surface_form: lamington
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -8.95
lon: 148.15
surface_form: mount victory
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -9.21666667
lon: 149.06666667
Mount Trafalgar. Mount Trafalgar is an extinct volcano on the north east coast of Oro Province, Papua New Guinea. The mountain is a major andesite volcano, with the magma known for its high levels of Nickel and Chromium. Captain John Moresby named the mountain after the naval battle of Trafalgar.

Geographic entities mentioned:
surface_form: mount trafalgar
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -9.15
lon: 149.16666667
Hydrographers Range, Mount Lamington, and Mount Victory are three other large Quaternary stratovolcanoes in south-eastern New Guinea. Name. Mount Trafalgar is named after the famous naval battle of Trafalgar, which was fought off the coast of Spain in 1805 between the British Royal Navy and the combined fleets of France and Spain.

Geographic entities mentioned:
surface_form: mount trafalgar
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -9.15
lon: 149.16666667
Burtnieki Castle. Burtnieki Castle (;) is a castle in Burtnieki Parish, Valmiera Municipality in the Vidzeme region of Latvia. It was built on the south shore of Lake Burtnieks for the Livonian Order around 1284.

Geographic entities mentioned:
surface_form: Lake Burtnieks
instance_of: Lake
countries: Latvia
coordinates: lat: 57.733333333333
lon: 25.233333333333
Castelli di Cannero. The Castelli di Cannero are three rocky islets of Lake Maggiore in northern Italy. They are located off the shoreline of Cannero Riviera while administratively forming part of the Comune of Cannobio. They are known as &quot;castelli&quot;, or castles, in recognition of the ruined ancient fortifications which are found on two of them.

Geographic entities mentioned:
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
This went on until the Viscontis laid siege to the fortress, starving the bandits into surrender. The old castle was razed to the ground, so that no trace of it remains. The Rocca Vitaliana was then built to defend the upper part of Lake Maggiore from incursions by the Swiss after the Duchy of Milan lost control of the Canton of Ticino.

Geographic entities mentioned:
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
Elements landed on 11 May 1943, spearheaded by the 17th Infantry Regiment, and fought an intense battle over the tundra against strong Japanese resistance. The fight for the island culminated in a battle at Chichagof Harbor, when the division destroyed all Japanese resistance on the island on 29 May, after a suicidal Japanese bayonet charge.

Geographic entities mentioned:
surface_form: Chichagof Harbor
instance_of: Landform
countries: United States
coordinates: lat: 52.9319
lon: 173.242
History. The group was formed first in the aftermath of a mountaineering accident occurred in 1994 on Bolkar Mountains, at which two local climbers were involved. In December 1995, a group of volunteer mountaineers conducted their first organized mission on Mt. Uludağ, and rescued people, who got lost in the fog, freezing in heavy snowfall.

Geographic entities mentioned:
surface_form: Mt. Uludağ
instance_of: Mountain
countries: Turkey
coordinates: lat: 40.0705295
lon: 29.222009805555555
Exmoor is more precisely defined as the area of the former ancient royal hunting forest, also called Exmoor, which was officially surveyed 1815–1818 as in extent. The moor has given its name to a National Park, which includes the Brendon Hills, the East Lyn Valley, the Vale of Porlock and of the Bristol Channel coast.

Geographic entities mentioned:
surface_form: East Lyn Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.2242
lon: -3.73
It has several tributaries which arise on Exmoor. The River Barle runs from northern Exmoor to join the River Exe at Exebridge, Devon. The river and the Barle Valley are both designated as biological Sites of Special Scientific Interest. Another tributary, the River Haddeo, flows from the Wimbleball Lake. Most other rivers arising on Exmoor flow north to the Bristol Channel.

Geographic entities mentioned:
surface_form: Wimbleball Lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.066666666667
lon: -3.4666666666667
The River Horner, which is also known as Horner Water, rises near Luccombe and flows into Porlock Bay near Hurlstone Point. The River Mole arises on the south-western flanks of Exmoor and is the major tributary of the River Taw, which itself flows northward from Dartmoor. Badgworthy Water is one of the small rivers running north to the coast and is associated with the Lorna Doone legends. Climate.

Geographic entities mentioned:
surface_form: River Mole
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 50.9417
lon: -3.90667
One year later he was part of the British team that topped the medal table at the 2015 World Rowing Championships at Lac d'Aiguebelette in France, where he won a gold medal as part of the eight with Matt Gotrel, Constantine Louloudis, Pete Reed, Paul Bennett, Moe Sbihi, George Nash, Will Satch and Phelan Hill. Honours.

Geographic entities mentioned:
surface_form: Lac d'Aiguebelette
instance_of: Lake
countries: France
coordinates: lat: 45.552777777778
lon: 5.7972222222222
The Molalas were called &quot;kúikni&quot; by the Klamath. Homeland. Molala territory once stretched across the Western Cascades; from Mount Hood and the Molalla River in the north to the Rogue headwaters in the south. Dense forests of western hemlock, Douglas fir, and western red cedar inundated the region.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
No one recalled stories of conflict with the Molala, or of their supposed eviction from Tygh Valley. One informant stated that after the fish runs ended in the Willamette Valley, certain Molala would travel to Sherars Falls to continue fishing. After a decade of work among the Wascos and Sahaptins of Warm Springs, David H.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
However, little is recorded of the linguistic and cultural diversity among the Molala peoples. The three reported groupings are the Southern Molala, the Upper Santiam Molala, and the Northern Molala. The Southern Molala inhabited the headwaters of the Rogue and Umpqua Rivers along the bases of Crater Lake and Mount McLoughlin.

Geographic entities mentioned:
surface_form: Crater Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.943611111111
lon: -122.10666666667
surface_form: Mount McLoughlin
instance_of: Mountain
countries: United States
coordinates: lat: 42.444472222222
lon: -122.31561111111
Mythology. Only a few Molala myths remain extant, recorded by ethnographers in the late 19th and early 20th centuries. Boas recounts a story told by the Molala of the world once being entirely covered in water. As the world ocean receded, Mount Hood became exposed first and latter the Willamette Valley. Tensions with settlers.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
It is the largest river on the planet that links two major river systems. Eastern Asia. The Huai River in China splits into three streams. The main stream passes through the Sanhe Sluice, goes out of the Sanhe river, and enters the Yangtze River through Baoying Lake and Gaoyou Lake.

Geographic entities mentioned:
surface_form: Gaoyou Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 32.83333333
lon: 119.33333333
The main stream passes through the Sanhe Sluice, goes out of the Sanhe river, and enters the Yangtze River through Baoying Lake and Gaoyou Lake. On the east bank of Hongze Lake, another stream goes out of Gaoliangjian Gate and enters the Yellow Sea at the port of Bidan through Subei Guan'gai Zongqu, the main irrigation channel of Northern Jiangsu); its total length is 168 kilometers.

Geographic entities mentioned:
surface_form: Hongze Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 33.3075
lon: 118.71
The copper was then used for military purposes in 1916 reconstructed later. The original purpose was to host troops to defend the ships entering and leaving the Elbe from sea and beach pirates. The tower was also refuge for the farmers on the island during storm surges and survivors of shipwrecks over the centuries.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
The finished goods were sent to Degesch, who forwarded the product to two companies that acted as distributors: Heerdt-Linger GmbH (Heli) of Frankfurt and Tesch & Stabenow (Testa) of Hamburg. Their territory was split along the Elbe river, with Heli handling clients to the west and south, and Testa those to the east.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Yanshan Temple. Yanshan Temple () is a preserved location of national historical and cultural relics. It used to be named Lingyan Temple (). It is located in Tianyan Village of north side of Mount Wutai, Yukou, south of Fanshi County, Shanxi Province of China. It was founded in Zhenglong 3rd year (1158), Jin dynasty, and renovated in Yuan, Ming, and Qing dynasties.

Geographic entities mentioned:
surface_form: Mount Wutai
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 39.081388888889
lon: 113.56694444444
Cat Nunatak. Cat Nunatak () is a nunatak in Antarctica, midway between Vince Nunatak and Hogback Hill in the southern part of Wilson Piedmont Glacier, Victoria Land. It was so named by the New Zealand Geographic Board in 1994, in recollection that ship's cats accompanied the &quot;Morning&quot; and the &quot;Terra Nova&quot; on R. F. Scott's 1901–04 and 1910–13 expeditions to McMurdo Sound.

Geographic entities mentioned:
surface_form: Vince Nunatak
instance_of: Mountain
coordinates: lat: -77.5
lon: 163.367
surface_form: Hogback Hill
instance_of: Mountain
coordinates: lat: -77.48333333
lon: 163.61666667
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
surface_form: cat nunatak
instance_of: Mountain
coordinates: lat: -77.4833
lon: 163.483
surface_form: wilson
instance_of: Mountain
coordinates: lat: -68.45
lon: -65.55
Cat Nunatak. Cat Nunatak () is a nunatak in Antarctica, midway between Vince Nunatak and Hogback Hill in the southern part of Wilson Piedmont Glacier, Victoria Land. It was so named by the New Zealand Geographic Board in 1994, in recollection that ship's cats accompanied the &quot;Morning&quot; and the &quot;Terra Nova&quot; on R. F. Scott's 1901–04 and 1910–13 expeditions to McMurdo Sound.

Geographic entities mentioned:
surface_form: terra nova
instance_of: Mountain
coordinates: lat: -77.5167
lon: 167.95
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Cat Nunatak. Cat Nunatak () is a nunatak in Antarctica, midway between Vince Nunatak and Hogback Hill in the southern part of Wilson Piedmont Glacier, Victoria Land. It was so named by the New Zealand Geographic Board in 1994, in recollection that ship's cats accompanied the &quot;Morning&quot; and the &quot;Terra Nova&quot; on R. F. Scott's 1901–04 and 1910–13 expeditions to McMurdo Sound.

Geographic entities mentioned:
surface_form: cat nunatak
instance_of: Mountain
coordinates: lat: -77.4833
lon: 163.483
Lake Hayes. Lake Hayes () is a small lake in the Wakatipu Basin in Central Otago, in New Zealand's South Island. It is located close to the towns of Arrowtown and Queenstown. The southern end of the lake is close to, while the western side is bordered by Slope Hill. The main area for access to the lake is the northern end which has a large grassed area for recreation activities.

Geographic entities mentioned:
surface_form: lake hayes
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.983333333333
lon: 168.8
Lake Hayes. Lake Hayes () is a small lake in the Wakatipu Basin in Central Otago, in New Zealand's South Island. It is located close to the towns of Arrowtown and Queenstown. The southern end of the lake is close to, while the western side is bordered by Slope Hill. The main area for access to the lake is the northern end which has a large grassed area for recreation activities.

Geographic entities mentioned:
surface_form: lake hayes
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.983333333333
lon: 168.8
surface_form: wakatipu
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.085
lon: 168.561
The main area for access to the lake is the northern end which has a large grassed area for recreation activities. The Lake Hayes Showgrounds which have a pavilion and parking area has an annual show called &quot;The Lake Hayes A&P Show&quot;. The nearby large residential sub-division of Lake Hayes Estate is just across the main highway and takes its name from Lake Hayes.

Geographic entities mentioned:
surface_form: lake hayes
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.983333333333
lon: 168.8
surface_form: lake hayes
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.983333333333
lon: 168.8
The nearby large residential sub-division of Lake Hayes Estate is just across the main highway and takes its name from Lake Hayes. A track called the Lake Hayes Circuit runs around the lake and forms part of The Queenstown Trail and is popular for use by walkers, runners and cyclists. History.

Geographic entities mentioned:
surface_form: lake hayes
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.983333333333
lon: 168.8
Settlers originally knew the lake as Hays Lake after D. Hay, an Australian who came to the district looking for sheep country in 1859. Its name gradually changed to Lake Hayes, as its discovery was credited erroneously to Captain &quot;Bully&quot; Hayes, an early local character of the district. Fauna.

Geographic entities mentioned:
surface_form: lake hayes
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.983333333333
lon: 168.8
History. The local Māori iwi (tribe) of Ngāi Tahu originally named the lake &quot;Te Whaka-ata&quot; or &quot;Te Whaka-ata a Haki-te-kura&quot; after an ancestress called Haki-te-kura whose image was said to be reflected in the lake. Settlers originally knew the lake as Hays Lake after D. Hay, an Australian who came to the district looking for sheep country in 1859.

Geographic entities mentioned:
surface_form: te whaka-ata a haki-te-kura
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.983333333333
lon: 168.8
Unnamed tributaries of the surrounding creeks run down narrow valleys on the mountain's slopes. The summit ridge continues northeast to an unnamed summit and then Carl Mountain, both higher than Tremper at and respectively. Most of the mountain is within the Town of Shandaken, whose largest population center, the hamlet of Phoenicia, is at the southwest foot of the mountain.

Geographic entities mentioned:
surface_form: Carl Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.40505
lon: -73.53236
It was reopened in spring 2001 and listed on the National Register in late 2001. A new extension of the Long Path along the ridge past Carl Mountain to Plateau Mountain was opened that year as well. Access. The Phoenicia Trail, part of the Long Path, the former bark road extended to the fire tower, is a widely used route to Tremper's summit.

Geographic entities mentioned:
surface_form: plateau mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.1378
lon: -74.1744
surface_form: carl mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.40505
lon: -73.53236
state of New York. It is located near the hamlet of Phoenicia, in the valley of Esopus Creek. At in elevation, it is well below the higher peaks of the region. Its slopes were a source of two major local products during the 19th century: hemlock bark, a source of tannin, and bluestone used in construction. Later it was the site of Tremper House, one of the Catskills' earliest railroad resorts.

Geographic entities mentioned:
surface_form: hemlock
instance_of: Lake
countries: United States
coordinates: lat: 42.718611111111
lon: -77.608888888889
Mount Tremper. Mount Tremper, officially known as Tremper Mountain and originally called Timothyberg, is one of the Catskill Mountains in the U.S. state of New York. It is located near the hamlet of Phoenicia, in the valley of Esopus Creek. At in elevation, it is well below the higher peaks of the region.

Geographic entities mentioned:
surface_form: mount tremper
instance_of: Mountain
countries: United States
coordinates: lat: 42.0742
lon: -74.2775
In the 20th century it was acquired by the state and became part of the Catskill Park Forest Preserve. Its location in the Esopus Valley between the northern and southern Catskills made it an ideal place for a fire lookout tower, which still stands on the mountain's summit. The Mount Tremper Fire Observation Station has been restored and listed on the National Register of Historic Places.

Geographic entities mentioned:
surface_form: mount tremper
instance_of: Mountain
countries: United States
coordinates: lat: 42.0742
lon: -74.2775
The latter three are closely paralleled by state highways 214, 28 and 212. Its summit dominates the view from westbound Route 28 at the small hamlet of Mount Tremper. The mountain's lower slopes are gentle, becoming steep around and then leveling off again at the summit ridge. Unnamed tributaries of the surrounding creeks run down narrow valleys on the mountain's slopes.

Geographic entities mentioned:
surface_form: mount tremper
instance_of: Mountain
countries: United States
coordinates: lat: 42.0742
lon: -74.2775
Its remains are still visible today from the old road to the fire tower, which passes it. Flora and fauna. Because of its low elevation, the forests on Mount Tremper are dominated by a forest type referred to in the Catskills as southern hardwoods. This is dominated by oak, hickory and pine species, with some basswood and poplar scattered in lower elevations.

Geographic entities mentioned:
surface_form: mount tremper
instance_of: Mountain
countries: United States
coordinates: lat: 42.0742
lon: -74.2775
The Timothyberg side of the mountain was regularly burned over by blueberry pickers every year through 1916, the year the state built the fire lookout tower on the mountain and extended the old board road to make it accessible for observers coming by vehicle. It replaced another tower that had briefly stood on Slide Mountain, the Catskills' highest peak, a few years earlier.

Geographic entities mentioned:
surface_form: slide mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9986
lon: -74.3864
surface_form: slide mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.3127
lon: -119.884
Mount Tremper. Mount Tremper, officially known as Tremper Mountain and originally called Timothyberg, is one of the Catskill Mountains in the U.S. state of New York. It is located near the hamlet of Phoenicia, in the valley of Esopus Creek. At in elevation, it is well below the higher peaks of the region.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The Kokshetau - Atbasar highway passes close to the western lakeside. There are archaeological sites of the Bronze and Iron Ages in the area near the lake. Geography. Aydabol is located in the Kokshetau Mountains, Kazakh Uplands, and is part of the Irtysh basin. It lies at an elevation of. The lake has a drop shape oriented in a north–south direction.

Geographic entities mentioned:
surface_form: Kokshetau Mountains
instance_of: Mountain
countries: Kazakhstan
coordinates: lat: 53.081
lon: 70.1885
surface_form: aydabol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.74611
lon: 69.14639
surface_form: kokshetau
instance_of: Mountain
countries: Kazakhstan
coordinates: lat: 53.0801
lon: 70.1883
A tributary of the Zhabay flows southwestwards from the western shore. The Arshaly flows out from the southeastern shore. Among the lakes in Aydabol's vicinity, Karagaychik lies to the NNE, Zerendi to the north, Kumdykol to the west, and Karaungir to the ENE. Flora and fauna. Aydabol is surrounded by mountain steppe vegetation and patches of forest. Reeds grow on the shore.

Geographic entities mentioned:
surface_form: Karaungir
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.839444444444446
lon: 69.68305555555555
surface_form: aydabol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.74611
lon: 69.14639
Aydabol. Aydabol () is a lake in Zerendi and Burabay districts, Akmola Region, Kazakhstan. The village of Viktorovka lies by the western lakeshore, and Bogenbay Bi (until 2007 — Losevka) by the eastern. The Kokshetau - Atbasar highway passes close to the western lakeside. There are archaeological sites of the Bronze and Iron Ages in the area near the lake. Geography.

Geographic entities mentioned:
surface_form: aydabol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.74611
lon: 69.14639
The Arshaly flows out from the southeastern shore. Among the lakes in Aydabol's vicinity, Karagaychik lies to the NNE, Zerendi to the north, Kumdykol to the west, and Karaungir to the ENE. Flora and fauna. Aydabol is surrounded by mountain steppe vegetation and patches of forest. Reeds grow on the shore. The water is fresh and is used for agricultural purposes.

Geographic entities mentioned:
surface_form: aydabol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.74611
lon: 69.14639
Aydabol. Aydabol () is a lake in Zerendi and Burabay districts, Akmola Region, Kazakhstan. The village of Viktorovka lies by the western lakeshore, and Bogenbay Bi (until 2007 — Losevka) by the eastern. The Kokshetau - Atbasar highway passes close to the western lakeside. There are archaeological sites of the Bronze and Iron Ages in the area near the lake. Geography.

Geographic entities mentioned:
surface_form: kokshetau
instance_of: Mountain
countries: Kazakhstan
coordinates: lat: 53.0801
lon: 70.1883
Geography. According to the United States Census Bureau, the town has a total area of 49.0 square miles (126.8 km), of which 41.7 square miles (108.1 km) is land and 7.2 square miles (18.8 km) (14.81%) is water. The Dead Creek and the Hospital Creek run through Addison, and Lake Champlain is on the west border of Addison. The highest point is Snake Mountain, which is 1281 ft above Lake Champlain.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
The Dead Creek and the Hospital Creek run through Addison, and Lake Champlain is on the west border of Addison. The highest point is Snake Mountain, which is 1281 ft above Lake Champlain. Demographics. As of the census of 2000, there were 1,393 people, 494 households, and 402 families residing in the town. The population density was. There were 651 housing units at an average density of.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Description. Falcor Peak is located in Kings Canyon National Park and approximately one mile west of the crest of the Sierra Nevada mountain range. It is situated west of the community of Independence and east of Mount Rixford, which is the nearest higher peak. Access to the peak is possible via the John Muir Trail which crosses Glen Pass one mile to the west of the peak.

Geographic entities mentioned:
surface_form: Mount Rixford
instance_of: Mountain
countries: United States
coordinates: lat: 36.784981
lon: -118.3989207
It is situated west of the community of Independence and east of Mount Rixford, which is the nearest higher peak. Access to the peak is possible via the John Muir Trail which crosses Glen Pass one mile to the west of the peak. Precipitation runoff from the peak drains north into Rae Lakes and south to Bullfrog Lake. Topographic relief is significant as the summit rises above Bullfrog Lake in.

Geographic entities mentioned:
surface_form: Rae Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 36.8053
lon: -118.402
With week-day meetings and visitations, this made his life a busy one. In Urquhart. In July 1813, at the wishes of Duncan Forbes of Culloden, he was translated to Urquhart. In 1818 he was discussed by the General Assembly of the Church of Scotland regarding his apparent unwanted preaching in the parishes of Aberlour and Strathbogie. This case attracted much public interest. On St Kilda.

Geographic entities mentioned:
surface_form: Strathbogie
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.39
lon: -2.81
The section of the mainline between Trondheim and Dombås reaches an altitude of over the &quot;Dovrefjell&quot;, with gradients of 1 in 46 to 1 in 56 and curves of radius. At the time, the maximum axle load was limited to 15.5 tons. Great skill was displayed in the design of these locomotives, which were built specifically to operate 300 ton trains under these conditions.

Geographic entities mentioned:
surface_form: Dovrefjell
instance_of: Mountain
countries: Norway
coordinates: lat: 62.1
lon: 9.41666667
It is a classic plostglacial ribbon lake with a strongly developed shoreline. The banks of the lake, which are mostly steep, are largely surrounded by forests. It is one of several lakes known collectively as the heated Konin Lakes because the water temperature is abnormally high due to the inflow of water from the cooling systems of two power stations.

Geographic entities mentioned:
surface_form: Konin Lakes
instance_of: Group of lakes
countries: Poland
coordinates: lat: 52.33
lon: 18.31
Licheńskie Lake. Licheńskie Lake is a small lake in central Poland known as Jezioro Licheńskie in Polish. It is located in Konin County in Gmina Ślesin, near the town of Licheń Stary. It is a classic plostglacial ribbon lake with a strongly developed shoreline. The banks of the lake, which are mostly steep, are largely surrounded by forests.

Geographic entities mentioned:
surface_form: jezioro licheńskie
instance_of: Lake
countries: Poland
coordinates: lat: 52.3083
lon: 18.3386
surface_form: licheńskie lake
instance_of: Lake
countries: Poland
coordinates: lat: 52.3083
lon: 18.3386
Licheńskie Lake. Licheńskie Lake is a small lake in central Poland known as Jezioro Licheńskie in Polish. It is located in Konin County in Gmina Ślesin, near the town of Licheń Stary. It is a classic plostglacial ribbon lake with a strongly developed shoreline. The banks of the lake, which are mostly steep, are largely surrounded by forests.

Geographic entities mentioned:
surface_form: licheńskie lake
instance_of: Lake
countries: Poland
coordinates: lat: 52.3083
lon: 18.3386
East Peak (Elko County, Nevada). East Peak is a summit in Elko County in the U.S. state of Nevada. The elevation is. The peak rises above the Humboldt River valley and the community of Ryndon about two miles to the north and the main peak of Elko Mountain is about two miles to the west-southwest. East Peak was named for the fact is east of other nearby summits.

Geographic entities mentioned:
surface_form: Elko Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.8945
lon: -115.63
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
East Peak (Elko County, Nevada). East Peak is a summit in Elko County in the U.S. state of Nevada. The elevation is. The peak rises above the Humboldt River valley and the community of Ryndon about two miles to the north and the main peak of Elko Mountain is about two miles to the west-southwest. East Peak was named for the fact is east of other nearby summits.

Geographic entities mentioned:
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.9425
lon: -119.907
surface_form: east peak (elko county, nevada)
instance_of: Mountain
countries: United States
coordinates: lat: 40.912222222222
lon: -115.58277777778
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 41.5575
lon: -72.8372
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.15
lon: -146.045
East Peak (Elko County, Nevada). East Peak is a summit in Elko County in the U.S. state of Nevada. The elevation is. The peak rises above the Humboldt River valley and the community of Ryndon about two miles to the north and the main peak of Elko Mountain is about two miles to the west-southwest. East Peak was named for the fact is east of other nearby summits.

Geographic entities mentioned:
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.9425
lon: -119.907
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.912222222222
lon: -115.58277777778
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 41.5575
lon: -72.8372
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.15
lon: -146.045
The highest point in the Ruahines is Mangaweka, situated along the Hikurangi Range. At, Mangaweka is the second highest non-volcanic mountainous peak in the North Island after Mount Hikurangi (1754 metres/5755 feet) in the Raukumara Range. The other notable peak is Wharite (, which marks the southern end-point of the Ruahine Range.

Geographic entities mentioned:
surface_form: Wharite
instance_of: Mountain
countries: New Zealand
coordinates: lat: -40.255
lon: 175.8567
Aqu Suntu. Aqu Suntu (Quechua &quot;aqu&quot; sand, &quot;suntu&quot; heap, pile, &quot;sand heap&quot;, Hispanicized spelling &quot;Ajo Sunto&quot;) is a mountain in the Wansu mountain range in the Andes of Peru. It is located in the Arequipa Region, La Unión Province, in the central part of the Huaynacotas District. Aqu Suntu lies southwest of Qarwa Urqu.

Geographic entities mentioned:
surface_form: Qarwa Urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.7961
lon: -72.7511
Aqu Suntu. Aqu Suntu (Quechua &quot;aqu&quot; sand, &quot;suntu&quot; heap, pile, &quot;sand heap&quot;, Hispanicized spelling &quot;Ajo Sunto&quot;) is a mountain in the Wansu mountain range in the Andes of Peru. It is located in the Arequipa Region, La Unión Province, in the central part of the Huaynacotas District. Aqu Suntu lies southwest of Qarwa Urqu.

Geographic entities mentioned:
surface_form: aqu suntu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.7108
lon: -72.6519
surface_form: aqu suntu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.8178
lon: -72.7731
William Hallett Ray. William Hallett Ray (May 25, 1825 &ndash; May 7, 1909) was a Canadian politician, farmer, and merchant. Born in Clementsport, Annapolis Valley, where he worked as a farmer and a merchant, Ray was elected to the Nova Scotia House of Assembly for Annapolis County in an 1864 by-election held after James William Johnston was named to the bench.

Geographic entities mentioned:
surface_form: Annapolis Valley
instance_of: Valley
countries: Canada
coordinates: lat: 44.979166666666664
lon: -64.89222222222222