Sarmila/GeoWiki-Features huggingface dataset:
It is located west of Harrisonburg, Virginia, in Rockingham County. Description. Mole Hill is an isolated, rounded, tree-covered &quot;monadnock&quot; in an otherwise relatively flat valley, surrounded by farmland. The peak of Mole Hill is approximately above sea level.

Geographic entities mentioned:
surface_form: mole hill
instance_of: Landform
countries: United States
coordinates: lat: 38.4486
lon: -78.9533
Description. Mole Hill is an isolated, rounded, tree-covered &quot;monadnock&quot; in an otherwise relatively flat valley, surrounded by farmland. The peak of Mole Hill is approximately above sea level. The basalt outcropping at the crest of the hill is &quot;dark greenish gray to grayish black, medium grained, and moderately porphyritic.

Geographic entities mentioned:
surface_form: mole hill
instance_of: Landform
countries: United States
coordinates: lat: 38.4486
lon: -78.9533
Mount Arthur (British Columbia). Mount Arthur is a mountain located at the Queen Reach arm of the Jervis Inlet within the Pacific Ranges of the Coast Mountains in British Columbia Canada. The mountain was named during the 1860 survey by who charted all of the area and named the mountain after Prince Arthur William Patrick who was the seventh son of Queen Victoria and Prince Albert of England.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount arthur
instance_of: Mountain
countries: Canada
coordinates: lat: 81.3333
lon: -74.75
surface_form: mount arthur
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1286
lon: -123.917
Mount Arthur (British Columbia). Mount Arthur is a mountain located at the Queen Reach arm of the Jervis Inlet within the Pacific Ranges of the Coast Mountains in British Columbia Canada. The mountain was named during the 1860 survey by who charted all of the area and named the mountain after Prince Arthur William Patrick who was the seventh son of Queen Victoria and Prince Albert of England.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount arthur
instance_of: Mountain
countries: Canada
coordinates: lat: 81.3333
lon: -74.75
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mount arthur
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1286
lon: -123.917
Mount Arthur (British Columbia). Mount Arthur is a mountain located at the Queen Reach arm of the Jervis Inlet within the Pacific Ranges of the Coast Mountains in British Columbia Canada. The mountain was named during the 1860 survey by who charted all of the area and named the mountain after Prince Arthur William Patrick who was the seventh son of Queen Victoria and Prince Albert of England.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The &quot;Sailors&quot; nickname corresponds to local history and geography. Sandusky is located on the Sandusky Bay and Lake Erie and has long been home to sailing. The Old Soldiers and Sailors Home was founded in Sandusky in 1886. Today, the Sandusky Sailing Club continues operation and memberships. Beginning play in the 1936 Ohio State League, the Sailors finished in second place.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Yanamauras. Yanamauras (possibly from Quechua &quot;Yana Mawras&quot;, &quot;yana&quot; black) is a volcano in the Andes of Peru, about high. It is situated in the &quot;Valley of the Volcanoes&quot; in the Arequipa Region, Castilla Province, Andagua District. Yanamauras lies southwest of the Puca Mauras volcano and east of the Ticsho volcano.

Geographic entities mentioned:
surface_form: Ticsho
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4847
lon: -72.3786
surface_form: puca mauras
instance_of: Mountain
countries: Peru
coordinates: lat: -15.45361111
lon: -72.23027778
surface_form: puca mauras
instance_of: Mountain
countries: Peru
coordinates: lat: -15.42583333
lon: -72.33861111
surface_form: ticsho
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4847
lon: -72.3786
Yanamauras. Yanamauras (possibly from Quechua &quot;Yana Mawras&quot;, &quot;yana&quot; black) is a volcano in the Andes of Peru, about high. It is situated in the &quot;Valley of the Volcanoes&quot; in the Arequipa Region, Castilla Province, Andagua District. Yanamauras lies southwest of the Puca Mauras volcano and east of the Ticsho volcano.

Geographic entities mentioned:
surface_form: yanamauras
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4839
lon: -72.3517
Yanamauras. Yanamauras (possibly from Quechua &quot;Yana Mawras&quot;, &quot;yana&quot; black) is a volcano in the Andes of Peru, about high. It is situated in the &quot;Valley of the Volcanoes&quot; in the Arequipa Region, Castilla Province, Andagua District. Yanamauras lies southwest of the Puca Mauras volcano and east of the Ticsho volcano.

Geographic entities mentioned:
surface_form: yanamauras
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4839
lon: -72.3517
surface_form: yana mawras
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4839
lon: -72.3517
Tradesmen and representatives of agriculture were very poorly represented – the latter were mostly represented by big landowners from east of the Elbe, accompanied by only three farmers. Craftsmen like Robert Blum or Wilhelm Wolff were associated almost exclusively with the radical democratic Left, as they knew the social problems of the underprivileged classes from personal observations.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
El Infiernito. &quot;El Infiernito&quot; (Spanish for &quot;The Little Hell&quot;), is a pre-Columbian archaeoastronomical site located on the Altiplano Cundiboyacense in the outskirts of Villa de Leyva, Boyacá, Colombia. It is composed of several earthworks surrounding a setting of menhirs (upright standing stones); several burial mounds are also present.

Geographic entities mentioned:
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877
The column alignments have been the subject of a more detailed study by archaeoastronomer Juan Morales who has found that the main columns are aligned at an azimuth of 91° to the top of Morro Negro hill pointing to the rise of the sun in the equinox. The summer solstice sun will be seen from the columns rising above the sacred Lake Iguaque, birthplace of the Muisca. Other monuments.

Geographic entities mentioned:
surface_form: Lake Iguaque
instance_of: Lake
countries: Colombia
coordinates: lat: 5.6427777777778
lon: -73.564722222222
After the eruption of Mount Tambora and the Year Without a Summer (1816), which followed close on the devastation of the Napoleonic Wars, widespread crop failures and food shortages resulted in the deaths of tens of thousands of horses, which either starved to death or were killed to provide meat and hides.

Geographic entities mentioned:
surface_form: Mount Tambora
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.2452777777778
lon: 117.99277777778
The San Joaquin originates in the southern Sierra and flows northwards to meet the Sacramento in the inland Sacramento–San Joaquin Delta. Both are joined by tributaries flowing westward from the Sierra. In the southern Central Valley, the Kings and Kaweah River flowed from headwaters in southern Sierra to empty into shallow Tulare Lake, and the Kern River flowed into Buena Vista Lake.

Geographic entities mentioned:
surface_form: Buena Vista Lake
instance_of: Lake
countries: United States
coordinates: lat: 35.1919
lon: -119.295
A number of smaller rivers and creeks empty into San Francisco bay from origins in the hills and mountains ringing the bay. The Salinas River originates in the coast ranges of Central California, and flows northwards through the Salinas Valley to empty into Monterey Bay. The ecoregion also includes the Carrizo Plain, an endorheic basin in the Coast Ranges of Central California. Fauna.

Geographic entities mentioned:
surface_form: Salinas Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.7654
lon: -121.7918
World War Two. The area was the site of several hard-fought battles in the Spring of 1945, during the last phases of World War II in Europe. The Allied crossing of the River Senio was one of the last hurdles that needed to be overcome in order to capture the great Po Valley basin and so complete the campaign in Italy.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
Stolze Peak. xkvqintian4dnpc33eidw25ty6oi" xml:space="preserve">#redirect Stolze Peak

Geographic entities mentioned:
surface_form: stolze peak
instance_of: Mountain
coordinates: lat: -64.7167
lon: -62.4333
Geography. The Tannu-Ola mountains form the northern border of Ubsunur Hollow., the only freshwater lake of the basin, lies, like Uvs Lake, on the Russian-Mongolian border. The more eastern part of the Uvs Lake drainage basin extends, in the north, to the Sengilen ridge of the Sayan Mountains, and in the east, to the basin of Sangiin Dalai Lake.

Geographic entities mentioned:
surface_form: Sangiin Dalai Lake
instance_of: Lake
countries: Mongolia
coordinates: lat: 49.263611111111
lon: 98.985277777778
The more eastern part of the Uvs Lake drainage basin extends, in the north, to the Sengilen ridge of the Sayan Mountains, and in the east, to the basin of Sangiin Dalai Lake. The southern part of the hollow is bordered by the basin of Khyargas Lake, with the Khan Khökhii mountains separating both basins of the Great Lakes Depression.

Geographic entities mentioned:
surface_form: Khan Khökhii
instance_of: Mountain
countries: Mongolia
coordinates: lat: 49.37777778
lon: 94.68833333
The southern part of the hollow is bordered by the basin of Khyargas Lake, with the Khan Khökhii mountains separating both basins of the Great Lakes Depression. More to the east, the forms the southern border of Uvs Lake's drainage basin. West of the Uvs Lake Basin lies the endorheic basin of Üüreg Lake, bordered by the Altai Mountains. The separates, in part, the Uvs and Üüreg lake basins.

Geographic entities mentioned:
surface_form: Üüreg Lake
instance_of: Lake
countries: Mongolia
coordinates: lat: 50.166666666667
lon: 91
Guerber Engineering. The Guerber Engineering Co. was a civil engineering firm that served most of the Lehigh Valley during the first half of the 20th century, erecting many of the steel elements of most notable buildings in the valley during this time period. History. The company was established in 1901 by Paul A. E.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Julidochromis. &quot;Julidochromis&quot; is a genus of cichlids in the subfamily Pseudocrenilabrinae. They are commonly called julies and are endemic to Lake Tanganyika in eastern Africa. This genus includes six formally described species, some with a number local variants of uncertain taxonomic status.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
&quot;Julidochromis&quot; in the aquarium. &quot;Julidochromis&quot; are small-growing dwarf cichlids and easy to spawn and care for if their basic needs are fulfilled. Like all Lake Tanganyika cichlids, they are best maintained in hard alkaline water, with a pH of 8.5–9.0 and a hardness of 12–14 kH, and in aquaria no smaller than.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
Williams Lake (Goffs). Williams Lake, Goffs is a lake of Halifax Regional Municipality, in Goffs, Nova Scotia, Canada.

Geographic entities mentioned:
surface_form: williams lake (goffs)
instance_of: Lake
countries: Canada
coordinates: lat: 44.8141
lon: -63.4492
surface_form: williams lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.7172
lon: -63.0503
surface_form: williams lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.7714
lon: -63.6689
surface_form: williams lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.11695
lon: -122.07195
Williams Lake (Goffs). Williams Lake, Goffs is a lake of Halifax Regional Municipality, in Goffs, Nova Scotia, Canada.

Geographic entities mentioned:
surface_form: williams lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.7172
lon: -63.0503
surface_form: williams lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.7714
lon: -63.6689
surface_form: williams lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.11695
lon: -122.07195
The museum is close to the Hallstättersee, below the salt mines on the mountainside. The museum, the salt mines, and the Dachstein Ice Cave are designated as an UNESCO World Heritage Site.

Geographic entities mentioned:
surface_form: Dachstein Ice Cave
instance_of: Mountain
countries: Austria
coordinates: lat: 47.475168
lon: 13.605735
Waukegan Station is located very near to downtown Waukegan, home to attractions such as the Genesee Theatre. Located at the bottom of the bluff that overlooks Lake Michigan, the station is immediately downhill from the historic Carnegie Library building. Other historic buildings in the area include the old houses of the Shimer College Historic District, site of that school's campus until 2006.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
On 19 January 1939 Nazi Germany reached the Martha Coast, as part of the German Antarctic Expedition. It is named in honour of Crown Princess Märtha of Norway. Troll is located in the eastern part, from the coast. Explora Escarpment is an undersea escarpment off the coast.

Geographic entities mentioned:
surface_form: Explora Escarpment
instance_of: Landform
coordinates: lat: -70.55
lon: -15
Puy Mary. The Puy Mary is a summit in the mounts of Cantal in Massif Central in France. It is classified as a &quot;Grand National Site&quot; in France. Nearly 500,000 visitors come to this site every year. Geography and geology. The mountain is an extinct volcano, about 6.5 million years old, which was formed by the accumulation of viscous lava (trachyte).

Geographic entities mentioned:
surface_form: puy mary
instance_of: Mountain
countries: France
coordinates: lat: 45.1093
lon: 2.676252777777778
Seven glacial valleys radiate from the summit. It is accessible starting from the Pas de Peyrol, which at 1,589 m above sea level, is the highest pass of the Massif Central. Climate. First mountain met by the oceanic disturbances coming from the Atlantic Ocean, the Puy Mary is among the wettest places in France. In winter, snow is abundant. Flora.

Geographic entities mentioned:
surface_form: puy mary
instance_of: Mountain
countries: France
coordinates: lat: 45.1093
lon: 2.676252777777778
&quot;Cappaert v. United States&quot;. Devils Hole cavern in Nevada became a detached part of Death Valley National Monument in 1952, by a proclamation of President Harry S. Truman made under the Antiquities Act. The cavern is home to a rare species of desert fish, the Devils Hole pupfish (&quot;Cyprinodon diabolis&quot;).

Geographic entities mentioned:
surface_form: Devils Hole
instance_of: Lake
countries: United States
coordinates: lat: 36.425233333333
lon: -116.29087222222
Magee Peak. Magee Peak is a stratovolcano in the Cascade Volcanic Arc north of Lassen Peak in Shasta County, California, United States. It was last active 1 to 2 million years ago. The peak is a destination for hikers, and marks the end of the Magee Trail hiking trail. There was once a watchtower at Magee Peak.

Geographic entities mentioned:
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
surface_form: magee peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.6893
lon: -121.6194
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
There was once a watchtower at Magee Peak. Magee Peak also has a number of smaller peaks and cliffs, such as Crater Peak, Red Cliff, Gray Cliff, and Fredonyer Peak. Magee Peak has a large cirque on its northeast side. Geography. Magee Peak is in Shasta County. It is located north of both Lassen Peak and its volcanic field and southeast of Mount Shasta.

Geographic entities mentioned:
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
It was last active 1 to 2 million years ago. The peak is a destination for hikers, and marks the end of the Magee Trail hiking trail. There was once a watchtower at Magee Peak. Magee Peak also has a number of smaller peaks and cliffs, such as Crater Peak, Red Cliff, Gray Cliff, and Fredonyer Peak. Magee Peak has a large cirque on its northeast side. Geography. Magee Peak is in Shasta County.

Geographic entities mentioned:
surface_form: crater peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0397
lon: -107.663
surface_form: magee peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.6893
lon: -121.6194
surface_form: fredonyer peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.68806
lon: -120.59917
Magee Peak. Magee Peak is a stratovolcano in the Cascade Volcanic Arc north of Lassen Peak in Shasta County, California, United States. It was last active 1 to 2 million years ago. The peak is a destination for hikers, and marks the end of the Magee Trail hiking trail. There was once a watchtower at Magee Peak.

Geographic entities mentioned:
surface_form: magee peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.6893
lon: -121.6194
It was last active 1 to 2 million years ago. The peak is a destination for hikers, and marks the end of the Magee Trail hiking trail. There was once a watchtower at Magee Peak. Magee Peak also has a number of smaller peaks and cliffs, such as Crater Peak, Red Cliff, Gray Cliff, and Fredonyer Peak. Magee Peak has a large cirque on its northeast side. Geography. Magee Peak is in Shasta County.

Geographic entities mentioned:
surface_form: magee peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.6893
lon: -121.6194
There was once a watchtower at Magee Peak. Magee Peak also has a number of smaller peaks and cliffs, such as Crater Peak, Red Cliff, Gray Cliff, and Fredonyer Peak. Magee Peak has a large cirque on its northeast side. Geography. Magee Peak is in Shasta County. It is located north of both Lassen Peak and its volcanic field and southeast of Mount Shasta.

Geographic entities mentioned:
surface_form: magee peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.6893
lon: -121.6194
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
Lac au Lard. The lac au Lard is the main body of water on the slope of the ruisseau du Lac au Lard, located in Haute-Batiscanie, in the town of La Tuque, in the administrative region of Mauricie, in Quebec, in Canada. Forestry is the main economic activity in the sector; recreational activities, second.

Geographic entities mentioned:
surface_form: lac au lard
instance_of: Lake
countries: Canada
coordinates: lat: 47.32694444444444
lon: -72.3963888888889
Lac au Lard. The lac au Lard is the main body of water on the slope of the ruisseau du Lac au Lard, located in Haute-Batiscanie, in the town of La Tuque, in the administrative region of Mauricie, in Quebec, in Canada. Forestry is the main economic activity in the sector; recreational activities, second.

Geographic entities mentioned:
surface_form: lac au lard
instance_of: Lake
countries: Canada
coordinates: lat: 47.32694444444444
lon: -72.3963888888889
surface_form: lac au lard
instance_of: Lake
countries: Canada
coordinates: lat: 47.32694444444444
lon: -72.3963888888889
Forestry is the main economic activity in the sector; recreational activities, second. The surface of Lac au Lard is generally frozen from the beginning of December to the end of March; however, safe circulation on the ice is generally from late December to early March. Geography. Lac au Lard has a length of, a width of and an altitude of. This lake is made in length.

Geographic entities mentioned:
surface_form: lac au lard
instance_of: Lake
countries: Canada
coordinates: lat: 47.32694444444444
lon: -72.3963888888889
A road bridge over the forest road R0400 intersects the northern part of the lake, thus forming a bay stretching for to the northwest. Lac au Lard has several small bays. The mouth of Lac au Lard is located North-West of the mouth of the confluence of the Jeannotte River with the Batiscan River, near which passes the Canadian National railway, and east of Petit lac Wayagamac.

Geographic entities mentioned:
surface_form: lac au lard
instance_of: Lake
countries: Canada
coordinates: lat: 47.32694444444444
lon: -72.3963888888889
A road bridge over the forest road R0400 intersects the northern part of the lake, thus forming a bay stretching for to the northwest. Lac au Lard has several small bays. The mouth of Lac au Lard is located North-West of the mouth of the confluence of the Jeannotte River with the Batiscan River, near which passes the Canadian National railway, and east of Petit lac Wayagamac.

Geographic entities mentioned:
surface_form: lac au lard
instance_of: Lake
countries: Canada
coordinates: lat: 47.32694444444444
lon: -72.3963888888889
surface_form: lac wayagamac
instance_of: Lake
countries: Canada
coordinates: lat: 47.374719444444
lon: -72.64445
surface_form: petit lac wayagamac
instance_of: Lake
countries: Canada
coordinates: lat: 47.377780555556
lon: -72.527219444444
From the mouth of Lac au Lard, the current descends successively towards the northeast on, on first towards the south then towards the east following the course of the Jeannotte River, and on the course of the Batiscan river towards the south which flows on the northwest bank of the St. Lawrence river. Toponymy.

Geographic entities mentioned:
surface_form: lac au lard
instance_of: Lake
countries: Canada
coordinates: lat: 47.32694444444444
lon: -72.3963888888889
Lawrence river. Toponymy. The toponym &quot;lac au Lard&quot; was formalized on December 5, 1968, at the Place Names Bank of the Commission de toponymie du Québec.

Geographic entities mentioned:
surface_form: lac au lard
instance_of: Lake
countries: Canada
coordinates: lat: 47.32694444444444
lon: -72.3963888888889
Dovedale. Dovedale is a valley in the Peak District of England. The land is owned by the National Trust and attracts a million visitors annually. The valley was cut by the River Dove and runs for just over between Milldale in the north and a wooded ravine, near Thorpe Cloud and Bunster Hill, in the south.

Geographic entities mentioned:
surface_form: the peak
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -7.95
lon: -14.35
surface_form: dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
Dovedale. Dovedale is a valley in the Peak District of England. The land is owned by the National Trust and attracts a million visitors annually. The valley was cut by the River Dove and runs for just over between Milldale in the north and a wooded ravine, near Thorpe Cloud and Bunster Hill, in the south.

Geographic entities mentioned:
surface_form: dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
In the wooded ravine, a set of stepping stones cross the river and there are two caves known as the Dove Holes. Dovedale's other attractions include rock pillars such as Ilam Rock, Viator's Bridge and the limestone features Lovers' Leap and Reynard's Cave. Geology.

Geographic entities mentioned:
surface_form: dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
Dovedale's other attractions include rock pillars such as Ilam Rock, Viator's Bridge and the limestone features Lovers' Leap and Reynard's Cave. Geology. The limestone rock that forms the geology of Dovedale consists of the fossilised remains of sea creatures that lived in a shallow sea over the area during the Carboniferous period, about 350 million years ago.

Geographic entities mentioned:
surface_form: dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
During the two ice ages, the limestone rock (known as reef limestone) was cut into craggy shapes by glacial meltwater, and dry caves such as Dove Holes and Reynard's Kitchen Cave were eventually formed. History. The caves were used as shelters by hunters around 13,000 BCE, and Dovedale has seen continuous human activity since. Around 4,500 years ago Neolithic farmers used the caves as tombs.

Geographic entities mentioned:
surface_form: dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
These settlements became permanent, and Thorpe is mentioned in the Domesday Book of 1086. Viator's Bridge, a packhorse bridge in Milldale, has been in use since the medieval period when silks and flax were transported from nearby Wetton and Alstonefield. Tourism started in the 18th century, and Dovedale is now one of the most visited natural tourist sites in Britain.

Geographic entities mentioned:
surface_form: dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
River Dove. The River Dove is a famous trout stream, 45 miles in length. Charles Cotton's Fishing House, the inspiration for Izaak Walton's &quot;The Compleat Angler&quot;, stands in the woods by the river. From Hartington to its confluence with the River Manifold at Ilam the River Dove flows through the scenic limestone valley known as Dove Valley, or Dovedale.

Geographic entities mentioned:
surface_form: dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
From Hartington to its confluence with the River Manifold at Ilam the River Dove flows through the scenic limestone valley known as Dove Valley, or Dovedale. From Hartington south to Ilam, a distance of, the Dove flows through Beresford Dale, Wolfscote Dale, Milldale, and then Dovedale. National Trust. Much of the dale is in the ownership of the National Trust's South Peak Estate.

Geographic entities mentioned:
surface_form: dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
National Trust. Much of the dale is in the ownership of the National Trust's South Peak Estate. Dovedale was acquired in 1934, with successive properties added until 1938, and Wolfscote Dale in 1948. Dovedale became a national nature reserve in 2006 in recognition that it is &quot;one of England's finest wildlife sites&quot; with diverse plant life and interesting rock formations.

Geographic entities mentioned:
surface_form: dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
Dovedale became a national nature reserve in 2006 in recognition that it is &quot;one of England's finest wildlife sites&quot; with diverse plant life and interesting rock formations. The National Trust became embroiled in controversy in 2010, when in conjunction with Derbyshire County Council it oversaw the &quot;renovation&quot; of Dovedale's iconic stepping stones.

Geographic entities mentioned:
surface_form: dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
It is listed as an ancient monument. Limestone formations. Dovedale is notable for its numerous limestone formations. The most southerly named formation, Dovedale Castle, is a short distance along the river from the stepping stones at Thorpe Cloud. The limestone promontory called Lover's Leap is accessible from a set of steps.

Geographic entities mentioned:
surface_form: dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
Tourism. Gentry comprised most of the visitors to Dovedale during the 18th and 19th centuries. From 1899 the Ashbourne–Buxton railway line ran to Thorpe Cloud station, above the village of Thorpe, making Dovedale more widely accessible to walkers and hikers of all social classes. Improvements in road transport facilitated travel to the area as well.

Geographic entities mentioned:
surface_form: dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
Riverside paths make the valley accessible to walkers. Literary and cultural associations. Charles Cotton's Fishing House, the inspiration for Izaak Walton's &quot;The Compleat Angler&quot;, stands in the woods by the River Dove. Samuel Johnson, Lord Tennyson, John Ruskin and Lord Byron all praised Dovedale's scenery.

Geographic entities mentioned:
surface_form: dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
The last wrote of Dovedale to the poet Thomas Moore, &quot;I can assure you there are things in Derbyshire as noble as Greece or Switzerland.&quot;
Elizabeth Bennet and Mr Darcy talk about her travels in Derbyshire, including Dove Dale, after they meet unexpectedly at Pemberley in Jane Austen's &quot;Pride and Prejudice&quot;.

Geographic entities mentioned:
surface_form: dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
surface_form: dove dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
The stepping stones across the river figure prominently in Jorge Grau's 1974 film &quot;The Living Dead at the Manchester Morgue&quot;. The area along the river was used in Franco Zeffirelli's 1996 version and the BBC's 2006 version of &quot;Jane Eyre&quot;, and Dovedale also featured in the 2008 film &quot;The Other Boleyn Girl&quot;.

Geographic entities mentioned:
surface_form: dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
surface_form: dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
The area along the river was used in Franco Zeffirelli's 1996 version and the BBC's 2006 version of &quot;Jane Eyre&quot;, and Dovedale also featured in the 2008 film &quot;The Other Boleyn Girl&quot;. The Ridley Scott film &quot;Robin Hood&quot; also used Dovedale as a location, and it can be clearly seen in several scenes towards the end of the movie. Dovedale Dash.

Geographic entities mentioned:
surface_form: dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
surface_form: dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
India reacted favourably to this plan. According to the Indian commentator Raghavan, it was first Nehru who proposed a partition-cum-plebiscite plan: Jammu and Ladakh would go to India, Azad Kashmir and Northern Areas to Pakistan, and a plebiscite would be held in the Kashmir Valley. Dixon favoured the plan, which bears his name till this day.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
Taoyuan Plateau. The Taoyuan Plateau () is a plateau located in northern Taiwan. It borders the Linkou Plateau in the northeast, the Hsuehshan Range in the southeast, the Hsinchu Hills in the south, and the Taiwan Strait in the west. In order to irrigate this area, many artificial pools have been created across the plateau. It is high, dry, and is full of rice paddies and factories.

Geographic entities mentioned:
surface_form: Linkou Plateau
instance_of: Plateau
countries: Taiwan
coordinates: lat: 25.06638889
lon: 121.36444444
Taoyuan Plateau. The Taoyuan Plateau () is a plateau located in northern Taiwan. It borders the Linkou Plateau in the northeast, the Hsuehshan Range in the southeast, the Hsinchu Hills in the south, and the Taiwan Strait in the west. In order to irrigate this area, many artificial pools have been created across the plateau. It is high, dry, and is full of rice paddies and factories.

Geographic entities mentioned:
surface_form: taoyuan plateau
instance_of: Plateau
countries: Taiwan
Demographics. As per a 2018 report from the Pakistan Bureau of Statistics, Barakahu accommodates a population exceeding 119,034 individuals. Residents originate from various regions, including Murree, Kashmir, Chitral, Khyber Pakhtunkhwa, Sindh, Balochistan, and Hazara. The area also encompasses a range of minority communities residing within its boundaries. Economy.

Geographic entities mentioned:
surface_form: Chitral
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.85111111111111
lon: 71.78888888888889
Queen Maud Mountains. The Queen Maud Mountains () are a major group of mountains, ranges and subordinate features of the Transantarctic Mountains, lying between the Beardmore and Reedy Glaciers and including the area from the head of the Ross Ice Shelf to the Antarctic Plateau in Antarctica.

Geographic entities mentioned:
surface_form: Antarctic Plateau
instance_of: Plateau
coordinates: lat: -90
lon: 0
&quot;At this point the scarp appears broken by a transverse fault which displaces the horst northward to Mount Wade (Mount Bush), a beacon sandstone massif rising to at least 14,000 feet above sea level, dominating the eastern flank of this remarkable valley glacier. Eastward of Mount Wade stand the Fisher Mountains, which form the western flank of the Liv Glacier.

Geographic entities mentioned:
surface_form: Mount Wade
instance_of: Mountain
coordinates: lat: -84.85
lon: -174.31666666667
The mountains are in the southern portion of the Eastern Highlands, or Manica Highlands, a belt of highlands that extend north and south along the international border, between the Zambezi and Save rivers. The Chimanimani Mountains include Monte Binga (2,436 m), the highest peak in Mozambique and the second-highest in Zimbabwe.

Geographic entities mentioned:
surface_form: Monte Binga
instance_of: Mountain
countries: Mozambique
coordinates: lat: -19.774166666667
lon: 33.060555555556
These two parks, together with a larger buffer zone, constitute the Chimanmani Transfrontier Conservation Area. Geography. Much of the range is composed of quartzite ridges running north and south, with Monte Binga (2,436 m) as the highest point. Other peaks include Mt. Peza (2152 m), Mt. Dombe (2188 m), and Mawenje or Turret Towers (2362 m) in Zimbabwe, and Mt. Nhamadimo (2144 m) in Mozambique.

Geographic entities mentioned:
surface_form: Monte Binga
instance_of: Mountain
countries: Mozambique
coordinates: lat: -19.774166666667
lon: 33.060555555556
Normandin River. The Normandin River is a tributary of the north shore of Ashuapmushuan Lake, flowing into the unorganized territory of Lac-Ashuapmushuan, Quebec, into the Regional County Municipality (RCM) of Le Domaine-du-Roy, in the administrative region of Saguenay-Lac-Saint-Jean, in Quebec, in Canada.

Geographic entities mentioned:
surface_form: Ashuapmushuan Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.159722222222
lon: -73.753333333333
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: normandin river
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.203333333333
lon: -73.7975
Forestry is the main economic activity of the sector; recreational tourism activities, second. The southern part of the Normandin River Valley is served by route 212 which connects Obedjiwan, Quebec to La Tuque and passes south of Dubois Lake and Normandin Lake (Normandin River). From there, the forest road R0212 (East-West direction) cuts the course of the Normandin River.

Geographic entities mentioned:
surface_form: normandin lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.960833333333
lon: -74.280277777778
surface_form: normandin river
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.203333333333
lon: -73.7975
surface_form: normandin river
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.203333333333
lon: -73.7975
Normandin River. The Normandin River is a tributary of the north shore of Ashuapmushuan Lake, flowing into the unorganized territory of Lac-Ashuapmushuan, Quebec, into the Regional County Municipality (RCM) of Le Domaine-du-Roy, in the administrative region of Saguenay-Lac-Saint-Jean, in Quebec, in Canada.

Geographic entities mentioned:
surface_form: normandin river
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.203333333333
lon: -73.7975
Forestry is the main economic activity of the sector; recreational tourism activities, second. The southern part of the Normandin River Valley is served by route 212 which connects Obedjiwan, Quebec to La Tuque and passes south of Dubois Lake and Normandin Lake (Normandin River). From there, the forest road R0212 (East-West direction) cuts the course of the Normandin River.

Geographic entities mentioned:
surface_form: normandin river
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.203333333333
lon: -73.7975
From there, the forest road R0212 (East-West direction) cuts the course of the Normandin River. The surface of the Normandin River is usually frozen from early November to mid-May, however, safe ice circulation is generally from mid-November to mid-April. Toponymy. The term &quot;Normandin&quot; is a family name of French origin.

Geographic entities mentioned:
surface_form: normandin river
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.203333333333
lon: -73.7975
The surface of the Normandin River is usually frozen from early November to mid-May, however, safe ice circulation is generally from mid-November to mid-April. Toponymy. The term &quot;Normandin&quot; is a family name of French origin. The toponym &quot;Normandin River&quot; was formalized on December 5, 1968, at the Commission de toponymie du Québec, when it was created.

Geographic entities mentioned:
surface_form: normandin river
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.203333333333
lon: -73.7975
Verney lake. uf5ug42me04sdrukyzpfbcjsrmaj" xml:space="preserve">#REDIRECT Verney Lake

Geographic entities mentioned:
surface_form: verney lake
instance_of: Lake
countries: Italy
coordinates: lat: 45.688183333333
lon: 6.8824416666667
It is long (including its source river the Tekes), of which is in Kazakhstan. The river originates from the Tekes and Künes rivers in Eastern Tian Shan. The Ili drains the basin between the Tian Shan and the Borohoro Mountains. Flowing into Lake Balkhash (in the endorheic Balkhash-Alakol Basin), the Ili forms a large delta with vast wetland regions of lakes, marshes and vegetation. Name.

Geographic entities mentioned:
surface_form: Lake Balkhash
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 46.540833333333
lon: 74.878888888889
The name in Kazakh means &quot;painted&quot; or &quot;marked place&quot;, and means &quot;stone&quot;. Ili Delta. The Ili River flows into the southeastern edge of Lake Balkhash, where it forms a large delta of about. The delta is situated between the Saryesik-Atyrau Desert and the Taukum Desert. An area of within the delta has been designated as a Ramsar Site.

Geographic entities mentioned:
surface_form: Lake Balkhash
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 46.540833333333
lon: 74.878888888889
HMS Coventry (1757). HMS &quot;Coventry&quot; was a 28-gun sixth-rate frigate of the Royal Navy, launched in 1757 and in active service as a privateer hunter during the Seven Years' War, and as part of the British fleet in India during the Anglo-French War. After seventeen years' in British service she was captured by the French in 1783, off Ganjam in the Bay of Bengal.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Yinnar South, Victoria. Yinnar South is a locality in the Latrobe Valley in Victoria, Australia. According to the 2021 census, Yinnar South had a population of 675. Previous higher figures were from Census 2006 and incorrectly combined both Yinnar and Yinnar South due to Census data compiled from postal area as opposed to geographical reference. The first school in Yinnar South, School No.

Geographic entities mentioned:
surface_form: Latrobe Valley
instance_of: Valley
countries: Australia
coordinates: lat: -38.1806
lon: 146.278
Whiteless Pike. Whiteless Pike, high, is a fell in the north-western English Lake District. It stands immediately east of Crummock Water and forms a pyramid shape when viewed from Rannerdale. In his celebrated guide to the Lakeland fells, A Wainwright called it &quot;the Weisshorn of Buttermere&quot;. There are good views of Great Gable and the Scafells from the summit. Topography.

Geographic entities mentioned:
surface_form: Crummock Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.55
lon: -3.3
Whiteless Pike. Whiteless Pike, high, is a fell in the north-western English Lake District. It stands immediately east of Crummock Water and forms a pyramid shape when viewed from Rannerdale. In his celebrated guide to the Lakeland fells, A Wainwright called it &quot;the Weisshorn of Buttermere&quot;. There are good views of Great Gable and the Scafells from the summit. Topography.

Geographic entities mentioned:
surface_form: Weisshorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.101666666667
lon: 7.7161111111111
surface_form: Buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
Whiteless Pike. Whiteless Pike, high, is a fell in the north-western English Lake District. It stands immediately east of Crummock Water and forms a pyramid shape when viewed from Rannerdale. In his celebrated guide to the Lakeland fells, A Wainwright called it &quot;the Weisshorn of Buttermere&quot;. There are good views of Great Gable and the Scafells from the summit. Topography.

Geographic entities mentioned:
surface_form: Great Gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
surface_form: great gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
The central sector, rising between Whinlatter Pass and Newlands Pass, includes Whiteless Pike. 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: Scar Crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.574388888889
lon: -3.2266805555556
surface_form: Causey Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.576338888889
lon: -3.2112694444444
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: 54.2445
lon: -2.47413
surface_form: sail
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.571
lon: -3.242
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.572
lon: -3.25
surface_form: scar crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.574388888889
lon: -3.2266805555556
surface_form: causey pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.576338888889
lon: -3.2112694444444
surface_form: grasmoor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.57115
lon: -3.2791805555556
surface_form: grasmoor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.57115
lon: -3.2791805555556
Grasmoor has the greatest elevation, but Crag Hill stands at the hub of the range. It sends out a subsidiary ridge to the south west, stepping down over Wandope and Whiteless Pike toward Buttermere village. From the broad plateau of Wandope, the fine and airy ridge of Whiteless Edge descends south west to the depression at Saddle Gate (). A short climb then leads to the summit of Whiteless Pike.

Geographic entities mentioned:
surface_form: Wandope
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.565980555556
lon: -3.2573611111111
surface_form: wandope
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.565980555556
lon: -3.2573611111111
surface_form: whiteless pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.558669444444
lon: -3.2695111111111
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
A short climb then leads to the summit of Whiteless Pike. The ridge now turns south and falls to the wide shoulder of Whiteless Breast (), from where the slope continues down to Buttermere village. This is not however the end of the ridge, which twists sharply north west to continue to Rannerdale Knotts. Both sides of the ridge are steep throughout.

Geographic entities mentioned:
surface_form: Rannerdale Knotts
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5522
lon: -3.28941
surface_form: rannerdale knotts
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5522
lon: -3.28941
The sharp elbow in the ridge, between Whiteless Pike and Rannerdale Knotts, forms the head of Squat Beck, a tributary of Rannerdale. Geology. The summit of the fell is a part of the Kirkstile Formation, Ordovician rocks of the Skiddaw group. This is primarily laminated mudstone and siltstone.

Geographic entities mentioned:
surface_form: Skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
surface_form: skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
The steep slopes add foreground to the view, which includes a fine prospect of the Scafells. The Helvellyn range and Western Fells are well seen, with the rather drab close-up of Grasmoor perhaps the only disappointment. Buttermere, Crummock and Loweswater complete the view. Ascents. Buttermere provides the obvious starting point, climbing on a good path up Whiteless Breast and onto the ridge.

Geographic entities mentioned:
surface_form: Loweswater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.5825
lon: -3.355277777777778
surface_form: loweswater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.5825
lon: -3.355277777777778