Sarmila/GeoWiki-Features huggingface dataset:
The viewing deck also has coin-operated telescopes that the visitors can use to enjoy the cityscape. The number of visitors led to the construction of two major leisure and shopping centres, the Peak Tower and the Peak Galleria, situated adjacent to each other. The Peak Tower incorporates the upper station of the Peak Tram, the funicular railway that brings passengers up from the St.

Geographic entities mentioned:
surface_form: the peak
instance_of: Mountain
countries: People's Republic of China
British Hong Kong
coordinates: lat: 22.275469444444
lon: 114.14382777778
surface_form: the peak
instance_of: Mountain
countries: People's Republic of China
British Hong Kong
coordinates: lat: 22.275469444444
lon: 114.14382777778
surface_form: the peak
instance_of: Mountain
countries: People's Republic of China
British Hong Kong
coordinates: lat: 22.275469444444
lon: 114.14382777778
The viewing deck also has coin-operated telescopes that the visitors can use to enjoy the cityscape. The number of visitors led to the construction of two major leisure and shopping centres, the Peak Tower and the Peak Galleria, situated adjacent to each other. The Peak Tower incorporates the upper station of the Peak Tram, the funicular railway that brings passengers up from the St.

Geographic entities mentioned:
surface_form: the peak
instance_of: Mountain
countries: People's Republic of China
British Hong Kong
coordinates: lat: 22.275469444444
lon: 114.14382777778
surface_form: the peak
instance_of: Mountain
countries: People's Republic of China
British Hong Kong
coordinates: lat: 22.275469444444
lon: 114.14382777778
surface_form: the peak
instance_of: Mountain
countries: People's Republic of China
British Hong Kong
coordinates: lat: 22.275469444444
lon: 114.14382777778
surface_form: the peak
instance_of: Mountain
countries: People's Republic of China
British Hong Kong
coordinates: lat: 22.275469444444
lon: 114.14382777778
It can be reached from Victoria Gap by walking up Mount Austin Road, a climb of about. Another popular walk is the level loop along Lugard and Harlech Roads, giving good views of the entire Hong Kong Harbour and Kowloon, as well as Lantau and Lamma Islands, encircling the summit at the level of the Peak Tower.

Geographic entities mentioned:
surface_form: the peak
instance_of: Mountain
countries: People's Republic of China
British Hong Kong
coordinates: lat: 22.275469444444
lon: 114.14382777778
There are several restaurants on Victoria Peak, most of which are located in the two shopping centres. However, the Peak Lookout Restaurant, is housed in an older and more traditional building which was originally a spacious house for engineers working on the Peak Tramway. It was rebuilt in 1901 as a stop area for sedan chairs, but was re-opened as a restaurant in 1947. Education.

Geographic entities mentioned:
surface_form: the peak
instance_of: Mountain
countries: People's Republic of China
British Hong Kong
coordinates: lat: 22.275469444444
lon: 114.14382777778
It has had notable success breeding seahorses and achieved the first captive breeding of the freshwater motoro stingray. Other notable fish include Epaulette Sharks, Mudskippers, tropical reef fish and various Lake Malawi cichlids. Invertebrates such as starfish, sea urchins and several species of coral and shrimps are housed with the fish.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
Fort Diggings Hollow. Fort Diggings Hollow is a valley in Crawford County in the U.S. state of Missouri. Fort Diggings Hollow derives its name from Pat Fort, a local prospector.

Geographic entities mentioned:
surface_form: fort diggings hollow
instance_of: Valley
countries: United States
coordinates: lat: 37.9797676
lon: -91.1606944
The river has its source at in Col d'Aneu, Pyrenees, not far from the Col du Pourtalet. It then flows in the Tena Valley through the municipalities of Sallent de Gállego, Panticosa and Biescas. Starting from Sabiñánigo it forms a wide elbow until Triste, from which it continues in its primitive north–south direction until flowing into the Ebro near Zaragoza.

Geographic entities mentioned:
surface_form: Tena Valley
instance_of: Valley
countries: Spain
coordinates: lat: 42.666666666667
lon: -0.31666666666667
The main tributaries of the Gállego in its upper basin are the Aguas Limpias, Caldarés, Escarra, Lana Mayor and Aurín. In the medium and lower basin, they include Guarga, Seco, Asabón and Sotón. The river's waters are subject to extensive regulation and derivation during its course, thus when it flows into the Ebro its discharge is just some 10 percent of its natural discharge.

Geographic entities mentioned:
surface_form: Sotón
instance_of: Watercourse
countries: Spain
coordinates: lat: 42.011111111111
lon: -0.76222222222222
Since its inception, the city has experienced several incidences of extreme weather resulting in significant damages and casualties. History. Aurora was an early settlement attempt near the mouth of Taylor Bayou on Sabine Lake, about long and wide. It is a saltwater estuary formed by the confluence of the Neches and Sabine Rivers.

Geographic entities mentioned:
surface_form: Sabine Lake
instance_of: Lake
countries: United States
coordinates: lat: 29.875
lon: -93.8475
A few species are found in brackish habitats, and one possibly extinct species (Potamacmaea fluviatilis) is known from estuaries and tributaries which drain into the Bay of Bengal. They attach themselves to the substrate using pedal mucus and a foot. They locomote using wave-like muscular contractions of the foot when conditions are suitable for them to graze.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
It is located west of Keswick in the north western part of the national park and is a smaller member of the Coledale group of fells with a height of. The fell is part of a ridge on the southern side of Coledale which descends from the higher fell of Scar Crags and continues over the neighbouring smaller fell of Barrow before reaching the valley at the village of Braithwaite. Topography.

Geographic entities mentioned:
surface_form: Scar Crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.574388888889
lon: -3.2266805555556
surface_form: coledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.65
lon: -3.23333
surface_form: barrow
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5858
lon: -3.19703
Two roads cross from east to west, dividing the fells into three convenient groups. The central sector, rising between Whinlatter Pass and Newlands Pass, includes Outerside. The highest ground in the North Western Fells is an east–west ridge in this central sector, beginning with Grasmoor above Crummock Water and then gradually descending eastwards over Crag Hill, Sail, Scar Crags and Causey Pike.

Geographic entities mentioned:
surface_form: Grasmoor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.57115
lon: -3.2791805555556
surface_form: Crummock Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.55
lon: -3.3
surface_form: Crag Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.572
lon: -3.25
surface_form: Causey Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.576338888889
lon: -3.2112694444444
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.2445
lon: -2.47413
surface_form: sail
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.571
lon: -3.242
surface_form: scar crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.574388888889
lon: -3.2266805555556
To the south is the little dale of Stonycroft Gill, havings its birth at High Moss. It flows east between Outerside and Causey Pike to join Newlands Beck at Stair. All of the waters of Outerside thus run to Bassenthwaite Lake. North east of Outerside the little ridge continues across Low Moss to the subsidiary top of Stile End.

Geographic entities mentioned:
surface_form: Bassenthwaite Lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.652
lon: -3.215
surface_form: outerside
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5816
lon: -3.22226
Beyond is Barrow, a shapely fell overlooking Braithwaite village. Geology. The rocks of Outerside are representative of the Kirkstile Formation, laminated mudstone and siltstone also typical of the Skiddaw group. At High and Low Moss this is overlain by peat. The fell has no history of mining, unlike many of the surrounding hills. Ascents.

Geographic entities mentioned:
surface_form: Skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
surface_form: outerside
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5816
lon: -3.22226
Ascents. The fell is ascended either from Braithwaite or Stair in the Newlands Valley; the ascent from Stair uses an old mine road up Stoneycroft Gill which crosses the shoulder of the fell at a height of from where the walker then strikes northerly to attain the summit. The direct route from Braithwaite follows Barrow Gill south westerly before going west to the highest point.

Geographic entities mentioned:
surface_form: Newlands Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.573011111111
lon: -3.1848694444444
Summit. The view from Outerside's summit cairn is restricted by the higher Coledale fells of Grisedale Pike, Crag Hill and Causey Pike in an arc to the west but there is a good prospect of the Helvellyn range to the east and the Skiddaw group to the north east, as well as a bird's-eye view directly down into Coledale with the Force Crag mine at its head.

Geographic entities mentioned:
surface_form: Grisedale Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.592
lon: -3.241
surface_form: Skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.2445
lon: -2.47413
surface_form: outerside
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5816
lon: -3.22226
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.572
lon: -3.25
surface_form: causey pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.576338888889
lon: -3.2112694444444
surface_form: coledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.65
lon: -3.23333
surface_form: coledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.65
lon: -3.23333
Outerside. Outerside is a fell in the Lake District in Cumbria, England. It is located west of Keswick in the north western part of the national park and is a smaller member of the Coledale group of fells with a height of.

Geographic entities mentioned:
surface_form: outerside
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5816
lon: -3.22226
Outerside. Outerside is a fell in the Lake District in Cumbria, England. It is located west of Keswick in the north western part of the national park and is a smaller member of the Coledale group of fells with a height of.

Geographic entities mentioned:
surface_form: outerside
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5816
lon: -3.22226
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Two roads cross from east to west, dividing the fells into three convenient groups. The central sector, rising between Whinlatter Pass and Newlands Pass, includes Outerside. The highest ground in the North Western Fells is an east–west ridge in this central sector, beginning with Grasmoor above Crummock Water and then gradually descending eastwards over Crag Hill, Sail, Scar Crags and Causey Pike.

Geographic entities mentioned:
surface_form: outerside
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5816
lon: -3.22226
surface_form: whinlatter
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.614
lon: -3.252
The highest ground in the North Western Fells is an east–west ridge in this central sector, beginning with Grasmoor above Crummock Water and then gradually descending eastwards over Crag Hill, Sail, Scar Crags and Causey Pike. Outerside is a satellite of Scar Crags, standing out to the north of the main ridge across the marshy depression of High Moss.

Geographic entities mentioned:
surface_form: outerside
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5816
lon: -3.22226
surface_form: scar crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.574388888889
lon: -3.2266805555556
Outerside is a satellite of Scar Crags, standing out to the north of the main ridge across the marshy depression of High Moss. Outerside has a conical profile in most views and its upper slopes are clad predominantly in heather. To the north of the fell runs the valley of Coledale, falling north eastwards to Braithwaite and the floodplain of the Derwent.

Geographic entities mentioned:
surface_form: outerside
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5816
lon: -3.22226
To the north of the fell runs the valley of Coledale, falling north eastwards to Braithwaite and the floodplain of the Derwent. To the south is the little dale of Stonycroft Gill, havings its birth at High Moss. It flows east between Outerside and Causey Pike to join Newlands Beck at Stair. All of the waters of Outerside thus run to Bassenthwaite Lake.

Geographic entities mentioned:
surface_form: outerside
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5816
lon: -3.22226
surface_form: causey pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.576338888889
lon: -3.2112694444444
It flows east between Outerside and Causey Pike to join Newlands Beck at Stair. All of the waters of Outerside thus run to Bassenthwaite Lake. North east of Outerside the little ridge continues across Low Moss to the subsidiary top of Stile End. This was not treated as a separate fell by Alfred Wainwright, although some later guidebooks take a different view.

Geographic entities mentioned:
surface_form: outerside
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5816
lon: -3.22226
Outerside. Outerside is a fell in the Lake District in Cumbria, England. It is located west of Keswick in the north western part of the national park and is a smaller member of the Coledale group of fells with a height of.

Geographic entities mentioned:
surface_form: coledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.65
lon: -3.23333
Outerside has a conical profile in most views and its upper slopes are clad predominantly in heather. To the north of the fell runs the valley of Coledale, falling north eastwards to Braithwaite and the floodplain of the Derwent. To the south is the little dale of Stonycroft Gill, havings its birth at High Moss. It flows east between Outerside and Causey Pike to join Newlands Beck at Stair.

Geographic entities mentioned:
surface_form: coledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.65
lon: -3.23333
All of the waters of Outerside thus run to Bassenthwaite Lake. North east of Outerside the little ridge continues across Low Moss to the subsidiary top of Stile End. This was not treated as a separate fell by Alfred Wainwright, although some later guidebooks take a different view. Beyond is Barrow, a shapely fell overlooking Braithwaite village. Geology.

Geographic entities mentioned:
surface_form: barrow
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5858
lon: -3.19703
Ascents. The fell is ascended either from Braithwaite or Stair in the Newlands Valley; the ascent from Stair uses an old mine road up Stoneycroft Gill which crosses the shoulder of the fell at a height of from where the walker then strikes northerly to attain the summit. The direct route from Braithwaite follows Barrow Gill south westerly before going west to the highest point.

Geographic entities mentioned:
surface_form: barrow
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5858
lon: -3.19703
The direct route from Braithwaite follows Barrow Gill south westerly before going west to the highest point. The fell is often climbed along with the adjoining fell of Barrow to which it is connected by a ridge. Summit.

Geographic entities mentioned:
surface_form: barrow
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5858
lon: -3.19703
Wardersee. Wardersee is a lake in Kreis Segeberg, Schleswig-Holstein, Germany. At its elevation, its surface area is 3.6 km². The federal highway 432 crosses the lake in a west-east direction near the village of Warder.

Geographic entities mentioned:
surface_form: wardersee
instance_of: Lake
countries: Germany
coordinates: lat: 53.9725
lon: 10.433611111111
Öxnadalsheiði. Öxnadalsheiði is a plateau (which includes a valley of the same name) in between Norðurárdalur in Skagafjörður and Öxnadalur in Eyjafjörður, Iceland. Route 1 between Skagafjörður and Akureyri goes through the plateau, which is quite snowy and used to be a difficult route to travel. Geography.

Geographic entities mentioned:
surface_form: Norðurárdalur
instance_of: Valley
countries: Iceland
coordinates: lat: 65.4325
lon: -19.04597
US 340, which is known for most of its length as Jefferson National Pike, connects Frederick with the communities of Jefferson, Brunswick, and Knoxville in the southern part of the Middletown Valley of western Frederick County and Weverton in far southern Washington County. The U.S. highway also links Frederick with Harpers Ferry and Charles Town in the Eastern Panhandle of West Virginia.

Geographic entities mentioned:
surface_form: Middletown Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.43
lon: -77.53
The routes pass by the historic estate Massanutton Heights, pass through Salem, and cross the South Fork Shenandoah River at Whitehouse Landing, the site of The White House. The two U.S. highways head northeast to bypass Luray where US 211 Business (Main Street) heads east into the town just south of Luray Caverns.

Geographic entities mentioned:
surface_form: Luray Caverns
instance_of: Landform
countries: United States
coordinates: lat: 38.6643
lon: -78.4838
US 340 expands to a four-lane freeway at the community of Sandy Hook, curves east through a trumpet interchange with MD 67 (Rohrersville Road), and crosses Israel Creek at Weverton. The highway, the canal, and the railroad parallel the Potomac River through the second ridge, which comprises South Mountain in Maryland and Short Hill Mountain in Virginia.

Geographic entities mentioned:
surface_form: Short Hill Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.25
lon: -77.71
US 340's name changes to Jefferson National Pike as it enters Frederick County. The highway leaves the Potomac Water Gap and enters the Middletown Valley at its partial interchange with MD 180 (Jefferson Pike) at Knoxville; there is no access from westbound US 340 to eastbound MD 180 or from westbound MD 180 to eastbound US 340. The U.S.

Geographic entities mentioned:
surface_form: Middletown Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.43
lon: -77.53
On the western edge of Jefferson, westbound US 340 receives a ramp from MD 180. Full access to Jefferson is provided by a diamond interchange with Lander Road. The U.S. highway passes through a wide gap in Catoctin Mountain and has a partial interchange with US 15 (Catoctin Mountain Highway), which heads south toward Point of Rocks.

Geographic entities mentioned:
surface_form: Catoctin Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6478
lon: -77.4664
Dudipatsar Lake. Dudipatsar Lake (), also known as Dudipat Lake, is a lake encircled by snow-clad peaks in Lulusar-Dudipatsar National Park. The lake lies at the north end of the Kaghan Valley, in the Mansehra District, Khyber Pakhtunkhwa province, in northern Pakistan. Geography. The lake's water is a greenish blue hue and very cold, at an elevation of.

Geographic entities mentioned:
surface_form: Kaghan Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 34.833333
lon: 73.516667
The surrounding mountains, with snow patches in the shady dales, average around in elevation. Their natural habitat is in the Western Himalayan alpine shrub and meadows ecoregion. Lulusar Lake, also in the park, is the primary headwaters of the Kunhar River. Saiful Muluk National Park, with Saiful Maluk Lake, is adjacent in the long Kaghan Valley region and the two parks jointly protect. Travel.

Geographic entities mentioned:
surface_form: Lulusar Lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.079132
lon: 73.927127
Their natural habitat is in the Western Himalayan alpine shrub and meadows ecoregion. Lulusar Lake, also in the park, is the primary headwaters of the Kunhar River. Saiful Muluk National Park, with Saiful Maluk Lake, is adjacent in the long Kaghan Valley region and the two parks jointly protect. Travel. Besal, or Besar, a town just before the Lulusar Lake, is fifteen kilometers from the lake.

Geographic entities mentioned:
surface_form: Saiful Maluk Lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 34.876666666666665
lon: 73.69416666666666
Lulusar Lake, also in the park, is the primary headwaters of the Kunhar River. Saiful Muluk National Park, with Saiful Maluk Lake, is adjacent in the long Kaghan Valley region and the two parks jointly protect. Travel. Besal, or Besar, a town just before the Lulusar Lake, is fifteen kilometers from the lake. The trek can be a tough hike and not particularly suitable for unfit or new trekkers.

Geographic entities mentioned:
surface_form: Lulusar Lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.079132
lon: 73.927127
Dudipatsar Lake. Dudipatsar Lake (), also known as Dudipat Lake, is a lake encircled by snow-clad peaks in Lulusar-Dudipatsar National Park. The lake lies at the north end of the Kaghan Valley, in the Mansehra District, Khyber Pakhtunkhwa province, in northern Pakistan. Geography. The lake's water is a greenish blue hue and very cold, at an elevation of.

Geographic entities mentioned:
surface_form: dudipatsar lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.0185
lon: 74.0895
Dudipatsar Lake. Dudipatsar Lake (), also known as Dudipat Lake, is a lake encircled by snow-clad peaks in Lulusar-Dudipatsar National Park. The lake lies at the north end of the Kaghan Valley, in the Mansehra District, Khyber Pakhtunkhwa province, in northern Pakistan. Geography. The lake's water is a greenish blue hue and very cold, at an elevation of.

Geographic entities mentioned:
surface_form: dudipatsar lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.0185
lon: 74.0895
surface_form: dudipatsar
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.0185
lon: 74.0895
surface_form: dudipat
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.0185
lon: 74.0895
All convertibles, all automatics, the car delivered loaded with options for $5,782 – approaching double that of the Star Chief Custom Convertible ($3,105) with which it shared the chassis. Jenkins Peak was named in his honor in 1960. The mountain is located north of the Bonneville Speedway and is prominently visible from there. Awards.

Geographic entities mentioned:
surface_form: Jenkins Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.9066
lon: -113.8267
Great Camp Sagamore. Great Camp Sagamore is one of several historic Great Camps located in the Adirondack Mountains of northern New York State. History. Great Camp Sagamore was constructed by William West Durant on Sagamore Lake between 1895 and 1897. Prior to Sagamore, William Durant had constructed Camp Pine Knot (purchased by Collis P.

Geographic entities mentioned:
surface_form: Sagamore Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.768055555556
lon: -74.619166666667
History. Great Camp Sagamore was constructed by William West Durant on Sagamore Lake between 1895 and 1897. Prior to Sagamore, William Durant had constructed Camp Pine Knot (purchased by Collis P. Huntington and now the Huntington Memorial Outdoor Education Center) on nearby Raquette Lake and Camp Uncas (once owned by J. P. Morgan) on Lake Mohegan. All three camps are still in use today.

Geographic entities mentioned:
surface_form: Raquette Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.833333333333
lon: -74.65
Ibón de Bachimaña Alto. Ibón de Bachimaña Alto and Ibón de Bachimaña Bajo are glacial lakes in the Tena Valley in the Province of Huesca, northeastern Spain, near the border with France. Ibón de Bachimaña Alto, the larger, lies at an elevation of above sea level. It covers an area of. Ibón de Bachimaña Bajo lies at above sea level and has a surface area of.

Geographic entities mentioned:
surface_form: Tena Valley
instance_of: Valley
countries: Spain
coordinates: lat: 42.666666666667
lon: -0.31666666666667
On the other hand, Laird asserted that in the 1940s Tibetan peasants were well off and immune to famine, whereas starvation was common in China. According to other sources, the so-called &quot;slaves&quot; were domestic servants and managers of estates in reality. In 1904, a British expeditionary force occupied the Chumbi Valley for four years, in the border region adjacent to Bhutan and India.

Geographic entities mentioned:
surface_form: Chumbi Valley
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 27.4893046
lon: 88.9050579
The South Mathias River, a tributary of the West Mathias River, is a long easterly-flowing river which meets the West Mathias from its confluence with the North Mathias. The combined waters flow a further southeast across a braided, shingle strath, which meets with the valley of the Rakaia River west of Lake Coleridge.

Geographic entities mentioned:
surface_form: Lake Coleridge
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.291
lon: 171.499
Shoshkakol. Shoshkakol (;) is a lake in Zhanaarka District, Ulytau Region, and Nura District, Karaganda Region, Kazakhstan. The border between Ulytau and Karaganda regions runs across the lake from northwest to southeast. Aynabulak village is located to the southeast of the lake. Geography. Shoshkakol is an endorheic lake.

Geographic entities mentioned:
surface_form: shoshkakol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 49.27
lon: 70.81028
Aynabulak village is located to the southeast of the lake. Geography. Shoshkakol is an endorheic lake. Two rivers of the Nura basin, the Kulanotpes and the Sonaly, flow northwards close to the lake basin. The lake is roughly square-shaped and has a fairly large island, —Araltobe with a length of and a width of, in the southern half. The lakeshores are flat and sandy, overgrown with grass.

Geographic entities mentioned:
surface_form: shoshkakol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 49.27
lon: 70.81028
The lakeshores are flat and sandy, overgrown with grass. Lake Sulukol lies to the east. Shoshkakol is a drying lake. Its water level has dropped significantly in recent decades and currently there are only two residual pools left. Most of the remaining surface of the lake is marshy, encumbered with aquatic vegetation. The lake water is saline and bitter. Flora and fauna.

Geographic entities mentioned:
surface_form: shoshkakol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 49.27
lon: 70.81028
Most of the remaining surface of the lake is marshy, encumbered with aquatic vegetation. The lake water is saline and bitter. Flora and fauna. Shoshkakol is surrounded by highland steppe. Reeds cover most of the shallow parts of the surface. Migratory birds, such as ducks, swans and geese, nest at the lake in the spring season.

Geographic entities mentioned:
surface_form: shoshkakol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 49.27
lon: 70.81028
Some national sub-divisions were simply referred to by their major clan component. An example of this would be the &quot;Maandawe-doodem&quot; ('Fisher-clan') of the &quot;Meshkwahkihaki&quot; peoples who live along the south shore of Lake Superior. More inland than the &quot;Maandawe-doodem&quot; were the &quot;Waagosh-doodem&quot; ('Fox clan') of the &quot;Meshkwahkihaki&quot; (Meskwaki).

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
In the 19th century it as was known as the Kalkoenkransrivier or Rhenosterpoortrivier. It is a tributary of the Wilge River in the Olifants River basin, and it lends its name to the town of Bronkhorstspruit, situated mainly on its right bank. Course. Its sources are located in the highveld grasslands of western Mpumalanga, about 30 km to the ESE of Springs, Gauteng.

Geographic entities mentioned:
surface_form: bronkhorstspruit
instance_of: Watercourse
countries: South Africa
coordinates: lat: -25.808333333333334
lon: 28.852777777777778
Course. Its sources are located in the highveld grasslands of western Mpumalanga, about 30 km to the ESE of Springs, Gauteng. It flows generally northwards and its main tributary, the Delmas River, joins its left bank. Further downstream it flows into the Bronkhorstspruit Dam, situated in eastern Gauteng. Then before it bends northeastwards it passes by the Bronkhorstspruit urban area.

Geographic entities mentioned:
surface_form: bronkhorstspruit
instance_of: Watercourse
countries: South Africa
coordinates: lat: -25.808333333333334
lon: 28.852777777777778
It flows generally northwards and its main tributary, the Delmas River, joins its left bank. Further downstream it flows into the Bronkhorstspruit Dam, situated in eastern Gauteng. Then before it bends northeastwards it passes by the Bronkhorstspruit urban area. It finally has a confluence with the Wilge River some 10 km east of the town, at Premiermyn Dam, Gauteng. History.

Geographic entities mentioned:
surface_form: bronkhorstspruit
instance_of: Watercourse
countries: South Africa
coordinates: lat: -25.808333333333334
lon: 28.852777777777778
In 1880 this river was the scene of the action at Bronkhorstspruit, a battle between a Boer commando under the command of Frans Joubert and British troops under Lieutenant-Colonel Anstruther. It was one of the first serious clashes in the early days of the First Boer War.

Geographic entities mentioned:
surface_form: bronkhorstspruit
instance_of: Watercourse
countries: South Africa
coordinates: lat: -25.808333333333334
lon: 28.852777777777778
Bronkhorst Spruit. The Bronkhorst Spruit, meaning &quot;watercress stream&quot; or &quot;creek&quot;, is a river in the Mpumalanga and Gauteng provinces of South Africa. In the 19th century it as was known as the Kalkoenkransrivier or Rhenosterpoortrivier.

Geographic entities mentioned:
surface_form: bronkhorst spruit
instance_of: Watercourse
countries: South Africa
coordinates: lat: -25.808333333333334
lon: 28.852777777777778
University Drive eventually connects to Memorial Parkway, where US-72 splits off and heads north with US 231/431. Going through the intersection, University Drive narrows to five lanes and intersects Church Street, where it becomes Pratt Ave. Pratt Ave continues east, directly connecting to Five Points and then runs up Monte Sano Mountain. Retail.

Geographic entities mentioned:
surface_form: Monte Sano Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.745
lon: -86.511666666667
Wallan. Wallan, traditionally known as Wallan Wallan (large circular place of water), is a town in Victoria, north of Melbourne's Central Business District. The town sits at the southern end of the large and diverse Shire of Mitchell which extends from the northern fringes of Melbourne into the farming country of north-central Victoria and the lower Goulburn Valley.

Geographic entities mentioned:
surface_form: Goulburn Valley
instance_of: Valley
countries: Australia
coordinates: lat: -36.3831
lon: 145.399
New Galloway. New Galloway () is a town in the historical county of Kirkcudbrightshire in Dumfries and Galloway. It lies on the west side of the valley of the Water of Ken, north of the end of Loch Ken. Before the local government reform of 1975, it was the smallest Royal Burgh in Scotland. History.

Geographic entities mentioned:
surface_form: Loch Ken
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.009
lon: -4.056
The first full biography of his life was published in 2021: Sir Herbert Baker: Architect to the British Empire, by John Stewart. South Africa. He embarked for South Africa in 1892 ostensibly to visit his brother, and was commissioned in 1893 by Cecil Rhodes to remodel Groote Schuur, Rhodes' house on the slopes of Table Mountain in Cape Town, and the residence of South African Prime Ministers.

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
Dower Lake. Dower Lake is a lake in Todd County, in the U.S. state of Minnesota. Dower Lake was named for Sampson Dower, an English settler.

Geographic entities mentioned:
surface_form: dower lake
instance_of: Lake
countries: United States
coordinates: lat: 46.35111111
lon: -94.8525
Early life. Marion (or Marrion) E. Knowlton was born in Geneva, Ashtabula County, Ohio, June 15, 1839. She was a lifelong resident of the Western Reserve of Ohio, near Lake Erie. For a time, her home was in Unionville, Lake County, Ohio. She was a lineal descendant of the original settlers of the Dutch colony of New Netherland and of those who participated in the American Revolutionary War.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
The island has many rivers, the longest being the Panay River at a length of, followed by the Jalaur, Aklan, Sibalom, Iloilo and Bugang rivers. Standing at about, the dormant Mount Madja-as (situated in Culasi, Antique) is the highest point of the island, with Mount Nangtud (located between Barbaza, Antique and Jamindan, Capiz) following next at.

Geographic entities mentioned:
surface_form: Mount Nangtud
instance_of: Mountain
countries: Philippines
coordinates: lat: 11.26762
lon: 122.20721
He fought in the Battle of Puerto de Carretas, being notable enough to be mentioned by Zuazua. After this action, with 500 riflemen, he participated in the assault on Bufa Hill and in the capture of Zacatecas by Julián Quiroga. He was entrusted with attacking Chacón, who had defeated Anacleto de la Rosa in Charcas.

Geographic entities mentioned:
surface_form: Bufa Hill
instance_of: Mountain
countries: Mexico
coordinates: lat: 22.7772
lon: -102.562
It now goes by the slogan of &quot;Notre belle vallée&quot;, since the recent re-branding of the village in May 2015. The village name is originally Mi'kmaq and means &quot;variegated&quot; referring to the many intricacies of the Memramcook River. The first mention of the area used the spelling Mémérancouque in 1757.

Geographic entities mentioned:
surface_form: Memramcook River
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.867
lon: -64.552
Neighbourhoods. Starting on Route 925 North-East border with Dieppe following the Petitcodiac River south, the first community is Dover (aka Pre-of-Surette) where the route is known as &quot;Rue Principale&quot; as it passes the &quot;Little Dover Road&quot;. From here you could continue from the west to Little Dover and La-Montagne.

Geographic entities mentioned:
surface_form: Petitcodiac River
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.926944444444
lon: -65.188888888889
History. The altarpiece, intended for the parish center at the entrance of the Val Brembana valley, was commissioned from Lotto by the Scuolo del Corpo di Cristo, the patrons of the altar of the piece. It was not easy to commission works from Lotto at the time, while he was in Bergamo and his works in high demand.

Geographic entities mentioned:
surface_form: Val Brembana
instance_of: Valley
countries: Italy
coordinates: lat: 45.8725
lon: 9.651944444444444
The Aiguilles Rouges (, &quot;Red Needles&quot;) are a crystalline mountainous massif of the French Prealps, opposite the Mont Blanc Massif. The colour of the iron rich gneiss (metamorphique) mountains gives the range its name. The highest summit is the Aiguille du Belvédère at. At the southern end of the range, Le Brévent at is accessible by a cable car in the Planpraz and the Brévent sections.

Geographic entities mentioned:
surface_form: Aiguille du Belvédère
instance_of: Mountain
countries: France
coordinates: lat: 45.9875
lon: 6.87333333
West of here, across the Firth of Clyde, sits the Island communities of Arran and Cumbrae, which are covered by the constituency. Along the east of the constituency is the more working-class Garnock Valley which comprises Kilbirnie, Beith and Dalry, towns which once specialised in the production of steel and textiles before the industries collapse across the 20th Century.

Geographic entities mentioned:
surface_form: Garnock Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.732
lon: -4.69
Ultimately, limnoforming aims to accelerate the rate of ecological succession in distressed aquatic systems (e.g., lower Green Bay, Lake Michigan), so as to produce a biologically complex climax community in a comparatively short amount of time. The concept of limnoforming originated from the benthic ecology laboratory of Dr. Jerry L.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Monte San Salvatore funicular. The Monte San Salvatore funicular, or &quot;Funicolare Monte San Salvatore&quot;, is a funicular railway in the city of Lugano in the Swiss canton of Ticino. The line links a lower station in the Lugano suburb of Paradiso with an upper station at the summit of the Monte San Salvatore.

Geographic entities mentioned:
surface_form: Monte San Salvatore
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.976666666667
lon: 8.9480555555556
The line links a lower station in the Lugano suburb of Paradiso with an upper station at the summit of the Monte San Salvatore. The top yields a 360° panorama with views of the city, Lake Lugano, Monte Generoso and the Italian enclave of Campione. The line was built in 1890, and originally used an Abt rack rail for braking.

Geographic entities mentioned:
surface_form: Lake Lugano
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46
lon: 9
surface_form: Monte Generoso
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.929444444444
lon: 9.0191666666667
The funicular is owned and operated by &quot;Funicolare Lugano-Paradiso-Monte San Salvatore SA&quot;. The Monte San Salvatore funicular is one of three operational funiculars within the Lugano area. The other two are the Monte Brè funicular, which ascends Monte Brè on the opposite side of the city, and the Lugano Città–Stazione funicular, which links the city centre with the railway station.

Geographic entities mentioned:
surface_form: Monte Brè
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.008611111111
lon: 8.9863888888889
Little Jack. Little Jack is a mountain summit in the North Cascades of Washington, United States. It is located within the Pasayten Wilderness. It is situated one mile south of its namesake Jack Mountain, west of Crater Mountain, and east of Ross Lake. Like many North Cascade peaks, Little Jack is more notable for its large, steep rise above local terrain than for its absolute elevation.

Geographic entities mentioned:
surface_form: Jack Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.7728
lon: -120.956
surface_form: Crater Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.7393
lon: -120.919
surface_form: crater mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.92206
lon: -118.42091
surface_form: ross lake
instance_of: Lake
countries: United States
coordinates: lat: 46.66277778
lon: -93.83638889
It is situated one mile south of its namesake Jack Mountain, west of Crater Mountain, and east of Ross Lake. Like many North Cascade peaks, Little Jack is more notable for its large, steep rise above local terrain than for its absolute elevation. In the early 1900s, the Forest Service built the Little Jack Trail for the purpose of grazing pack animals on the meadows of Little Jack Mountain.

Geographic entities mentioned:
surface_form: jack mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.7728
lon: -120.956
surface_form: little jack
instance_of: Mountain
countries: United States
coordinates: lat: 48.74388888888889
lon: -120.9786111111111
surface_form: little jack
instance_of: Mountain
countries: United States
coordinates: lat: 48.74388888888889
lon: -120.9786111111111
Little Jack Mountain is part of the &quot;Little Jack terrane&quot;. Outcrops of granite and fine-grained mica schist can be found on the top of Little Jack Mountain. During the Pleistocene period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris.

Geographic entities mentioned:
surface_form: jack mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.7728
lon: -120.956
surface_form: little jack
instance_of: Mountain
countries: United States
coordinates: lat: 48.74388888888889
lon: -120.9786111111111
Little Jack. Little Jack is a mountain summit in the North Cascades of Washington, United States. It is located within the Pasayten Wilderness. It is situated one mile south of its namesake Jack Mountain, west of Crater Mountain, and east of Ross Lake. Like many North Cascade peaks, Little Jack is more notable for its large, steep rise above local terrain than for its absolute elevation.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: little jack
instance_of: Mountain
countries: United States
coordinates: lat: 48.74388888888889
lon: -120.9786111111111
Little Jack. Little Jack is a mountain summit in the North Cascades of Washington, United States. It is located within the Pasayten Wilderness. It is situated one mile south of its namesake Jack Mountain, west of Crater Mountain, and east of Ross Lake. Like many North Cascade peaks, Little Jack is more notable for its large, steep rise above local terrain than for its absolute elevation.

Geographic entities mentioned:
surface_form: little jack
instance_of: Mountain
countries: United States
coordinates: lat: 48.74388888888889
lon: -120.9786111111111
It is situated one mile south of its namesake Jack Mountain, west of Crater Mountain, and east of Ross Lake. Like many North Cascade peaks, Little Jack is more notable for its large, steep rise above local terrain than for its absolute elevation. In the early 1900s, the Forest Service built the Little Jack Trail for the purpose of grazing pack animals on the meadows of Little Jack Mountain.

Geographic entities mentioned:
surface_form: little jack
instance_of: Mountain
countries: United States
coordinates: lat: 48.74388888888889
lon: -120.9786111111111
In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago. Little Jack Mountain is part of the &quot;Little Jack terrane&quot;. Outcrops of granite and fine-grained mica schist can be found on the top of Little Jack Mountain.

Geographic entities mentioned:
surface_form: little jack
instance_of: Mountain
countries: United States
coordinates: lat: 48.74388888888889
lon: -120.9786111111111
It rises on the southern slopes of Ben Wyvis, passes through Strath Sgitheach, passing Clare plantation, Swordale, the village of Evanton, and after about empties into the Cromarty Firth near the ruin of the old Kiltearn parish church. About a mile to the northeast, on the other side of Balconie Point, the Allt Graad also empties in the Firth.

Geographic entities mentioned:
surface_form: Ben Wyvis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.679119444444
lon: -4.5792194444444
&quot;At Twenty-One&quot; is the heartbreaking story of a poor young man who watches his sweetheart sail away after she gave her hand in marriage to a rich young man. Irvine learned it from the singing of Robert Cinnamond who lived on the banks of Lough Neagh, County Tyrone and who had many songs collected for the BBC by Sean Boyle in 1955. &quot;My Back Pages&quot; / &quot;Afterthoughts&quot;.

Geographic entities mentioned:
surface_form: Lough Neagh
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.618333333333
lon: -6.3952777777778
Voter turnout in the last 2004 mayoral election was 54.45%. Advance voting was available using an internet voting system. District 1: Eastern Shore - Musquodoboit Valley. &quot;2004 Election - Steve Streatch 2,366 (46.4%); Laurie Taylor 1,367 (26.9%); Martin Singh 740 (14.59%); Randy Carter 600 (11.83%) - Voter turnout: 54.58%&quot;
District 2: Waverley - Fall River - Beaver Bank.

Geographic entities mentioned:
surface_form: Musquodoboit Valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.0167
lon: -63.1833
The smoke from the pipe attracted dark clouds from which rain fell and filled the pond. Beaches. There are two public beaches on Scargo Lake: Princess Beach, which is sandy and Scargo Beach, which has sand dumped in the water, but no sandy area by the water. Fishing. Scargo Lake is stocked in spring and fall with brook, brown, and rainbow trout, all of which are allowed to be fished.

Geographic entities mentioned:
surface_form: beaches
instance_of: Landform
countries: United States
coordinates: lat: 41.677
lon: -70.1779
surface_form: scargo lake
instance_of: Lake
countries: United States
coordinates: lat: 41.7425
lon: -70.182777777778
He was gone so long that the fish began to outgrow the pumpkin. She then had the women of the village dig out the pond with clam shells so the fish could survive. The dirt the women dug out became Scargo Hill. Today it is the highest hill in the mid-Cape area. Another legend is very similar, but she dug a hole in the ground (considered by many to be fish-shaped).

Geographic entities mentioned:
surface_form: scargo hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.7398315
lon: -70.180853
Another legend is very similar, but she dug a hole in the ground (considered by many to be fish-shaped). The dirt from the hole was said to become the 160-foot Scargo Hill, and that the hole filled up with water from the heavy autumn rains, which also drowned the princess. She was seen as a sacrifice, and the reason the lake is well stocked with fish.

Geographic entities mentioned:
surface_form: scargo hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.7398315
lon: -70.180853
A wide shelf of shallow water makes for easy wading and access to deeper water. This shelf makes Scargo Lake a popular pond for fly fishing. Scargo Lake is located between Massachusetts Route 6A and Scargo Hill Road, and is easily reached off of route 6A. There are three town landings, all of which are suitable for launching light draft boats and canoes.

Geographic entities mentioned:
surface_form: scargo hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.7398315
lon: -70.180853
surface_form: scargo lake
instance_of: Lake
countries: United States
coordinates: lat: 41.7425
lon: -70.182777777778