Sarmila/GeoWiki-Features huggingface dataset:
The third-lowest lake level occurred on August 3, 1978, when the lake was 27.7% full. August 1978. Two days after recording its third-lowest level, the lake surged to its second-highest level ever. On August 5, 1978, the water in Lake Stamford was above the spillway. This represents an increase over in less than 48 hours, the lake's fastest-ever change in elevation. In fact, the rise was so fast.

Geographic entities mentioned:
surface_form: lake stamford
instance_of: Lake
countries: United States
coordinates: lat: 33.0444
lon: -99.6082
Most of the rain was concentrated during the aforementioned four days, with the city receiving on August 14, 2005, alone. On August 17, 2005, these rains put the lake overcapacity by with the surface elevation of and resulted in the record high water level for Lake Stamford. This caused extensive flooding to more than 340 homes, resulting in a disaster area declaration by Governor Perry.

Geographic entities mentioned:
surface_form: lake stamford
instance_of: Lake
countries: United States
coordinates: lat: 33.0444
lon: -99.6082
By April 21, lake levels crested at above capacity, having increased by. Additional rain events in June and September each moved the lake overcapacity again by less than. Water levels eventually dropped below the spillway on December 5, 2010, the last time Lake Stamford was full until July 10, 2015. Sale of water to Tenaska.

Geographic entities mentioned:
surface_form: lake stamford
instance_of: Lake
countries: United States
coordinates: lat: 33.0444
lon: -99.6082
Sale of water to Tenaska. On July 12, 2011, the Stamford city council approved the sale of all &quot;excess water&quot; from Lake Stamford for use in Tenaska Energy's Trailblazer Energy Center in Nolan County, Texas. No public debate was held before the decision was made.

Geographic entities mentioned:
surface_form: lake stamford
instance_of: Lake
countries: United States
coordinates: lat: 33.0444
lon: -99.6082
In addition to the, Stamford will sell Tenaska all of its effluent water of about 250,000 gallons/day (280 acre ft/year). The proposed coal-fired power plant would be located 37 miles southwest of Stamford and 47 miles southwest of Lake Stamford. On June 21, 2013, Tenaska cancelled their proposed Trailblazer coal-fired power plant.

Geographic entities mentioned:
surface_form: lake stamford
instance_of: Lake
countries: United States
coordinates: lat: 33.0444
lon: -99.6082
While Stamford would have provided the majority of the project's water, Tenaska was unable to find a secondary source of water. Power plant. AEP (formerly West Texas Utilities) owns a gas-fired electric generating power plant located at Lake Stamford. The plant has a generating capacity of 218 MW. When operating, water is pumped directly from the lake for industrial (cooling) purposes.

Geographic entities mentioned:
surface_form: lake stamford
instance_of: Lake
countries: United States
coordinates: lat: 33.0444
lon: -99.6082
The mixed form of the novel was commonly described as grotesque – see for instance Fielding's &quot;comic epic poem in prose&quot; (&quot;Joseph Andrews&quot; and &quot;Tom Jones&quot;). Grotesque ornament received a further impetus from new discoveries of original Roman frescoes and stucchi at Pompeii and the other buried sites round Mount Vesuvius from the middle of the century.

Geographic entities mentioned:
surface_form: Mount Vesuvius
instance_of: Mountain
countries: Italy
coordinates: lat: 40.821388888889
lon: 14.425555555556
Maurepas, Louisiana. Maurepas is an unincorporated community in the south/southwestern area of Livingston Parish, Louisiana, United States. Louisiana Highway 22 passes through the community and Whitehall lies two miles to the east. Lake Maurepas is six miles to the east and the Amite River lies approximately one half mile to the north. The ZIP Code for Maurepas is 70449.

Geographic entities mentioned:
surface_form: Lake Maurepas
instance_of: Lake
countries: United States
coordinates: lat: 30.258027777778
lon: -90.498677777778
Louisiana Highway 22 passes through the community and Whitehall lies two miles to the east. Lake Maurepas is six miles to the east and the Amite River lies approximately one half mile to the north. The ZIP Code for Maurepas is 70449. Lake Maurepas is located to the west of Lake Pontchartrain, Louisiana's largest lake.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
According to R. H. Charles, the text of the &quot;Greek Apocalypse of Ezra&quot; was influenced by the book of &quot;2 Esdras&quot;. The extant version of the &quot;Greek Apocalypse&quot; is thought to have undergone extensive reworking, if not having been totally written by, Christian editors, mentioning the Apostles Paul and John, King Herod, etc.

Geographic entities mentioned:
surface_form: Gehenna
instance_of: Valley
countries: Israel
coordinates: lat: 31.76916667
lon: 35.22805556
May Creek (British Columbia). May Creek is a creek located in the Boundary Country of British Columbia. The creek is a tributary of July Creek. May Creek flows into July Creek about five miles west of Grand Forks, British Columbia. The creek has been mined for gold.

Geographic entities mentioned:
surface_form: July Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.99979
lon: -118.5356
Bump Mountain. Bump Mountain is a mountain located in the Catskill Mountains of New York northeast of Ashland. Richtmyer Peak is located north-northeast, The Knob is located west, and Ashland Pinnacle is located west-southwest of Bump Mountain.

Geographic entities mentioned:
surface_form: Richtmyer Peak
instance_of: Mountain
countries: United States
coordinates: lat: 42.37564
lon: -74.26348
surface_form: the knob
instance_of: Mountain
countries: United States
coordinates: lat: 42.346666666667
lon: -74.313055555556
surface_form: the knob
instance_of: Mountain
countries: United States
coordinates: lat: 41.6522
lon: -85.3542
surface_form: bump mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.34675
lon: -74.26709
surface_form: the knob
instance_of: Mountain
countries: United States
coordinates: lat: 41.5423308
lon: -70.6611414
Bump Mountain. Bump Mountain is a mountain located in the Catskill Mountains of New York northeast of Ashland. Richtmyer Peak is located north-northeast, The Knob is located west, and Ashland Pinnacle is located west-southwest of Bump Mountain.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: bump mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.34675
lon: -74.26709
Bump Mountain. Bump Mountain is a mountain located in the Catskill Mountains of New York northeast of Ashland. Richtmyer Peak is located north-northeast, The Knob is located west, and Ashland Pinnacle is located west-southwest of Bump Mountain.

Geographic entities mentioned:
surface_form: bump mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.34675
lon: -74.26709
The forests extend within the Jinsha (upper Yangtze) and Yalong River valleys from approximately 32°N to 27°N. In addition, a portion of the Anning River valley and Mianmian Mountains near Lugu Lake support the subalpine conifer forests. This region covers northern Yunnan Province, western Sichuan Province, and the extreme eastern edge of the Tibet Autonomous Region.

Geographic entities mentioned:
surface_form: Lugu Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 27.701388888889
lon: 100.7975
This region covers northern Yunnan Province, western Sichuan Province, and the extreme eastern edge of the Tibet Autonomous Region. The Hengduan Mountains subalpine conifer forests are one zone in a range of montane ecosystems that transition between tropical and temperate ecoregions along the southeastern fringe of the Tibetan Plateau.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
state of Michigan. The name of the lake is derived from early French explorers who named it for the indigenous people they knew as Huron (Wyandot) inhabiting the region. Hydrologically, Lake Huron comprises the eastern portion of Lake Michigan–Huron, having the same surface elevation as Lake Michigan, to which it is connected by the, Straits of Mackinac.

Geographic entities mentioned:
surface_form: Lake Michigan–Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 45.813888888889
lon: -84.753888888889
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
The Huronian glaciation was named from evidence collected from the Lake Huron region. The northern parts of the lake include the North Channel and Georgian Bay. Saginaw Bay is located in the southwest corner of the lake. The main inlet is the St. Marys River from Lake Superior, and the main outlet is through the St. Clair River toward Lake Erie.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Water flows through Lake Huron faster than the other Great Lakes with a retention time of only 22 years. Geography. By surface area, Lake Huron is the second-largest of the Great Lakes, with a surface area of —of which lies in Michigan and lies in Ontario—making it the third-largest fresh water lake on Earth (or the fourth-largest lake, if the Caspian Sea is counted as a lake).

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
By surface area, Lake Huron is the second-largest of the Great Lakes, with a surface area of —of which lies in Michigan and lies in Ontario—making it the third-largest fresh water lake on Earth (or the fourth-largest lake, if the Caspian Sea is counted as a lake). By volume however, Lake Huron is only the third largest of the Great Lakes, being surpassed by Lake Michigan and Lake Superior.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Marys River which then flows into Lake Huron. The water then flows south to the St. Clair River, at Port Huron, Michigan and Sarnia, Ontario. The Great Lakes Waterway continues thence to Lake St. Clair; the Detroit River and Detroit, Michigan; into Lake Erie and thence – via Lake Ontario and the St. Lawrence River – to the Atlantic Ocean.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Georgian Bay contains 212 sunken vessels. Purportedly the first European vessel to sail the Great Lakes, &quot;Le Griffon&quot; also became the first ship lost on the Great Lakes. It was built in 1679 on the eastern shore of Lake Erie near Buffalo, New York. Robert Cavalier, Sieur de la Salle navigated across Lake Erie, up the Detroit River, Lake St. Clair and the St.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Purportedly the first European vessel to sail the Great Lakes, &quot;Le Griffon&quot; also became the first ship lost on the Great Lakes. It was built in 1679 on the eastern shore of Lake Erie near Buffalo, New York. Robert Cavalier, Sieur de la Salle navigated across Lake Erie, up the Detroit River, Lake St. Clair and the St. Clair River out into Lake Huron.

Geographic entities mentioned:
surface_form: Lake St. Clair
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.450265
lon: -82.67572
By car 5 minutes from Zirc with its historical abbey, about 30 minutes from the city of Veszprém, 40 minutes from lake Lake Balaton, 45 minutes from Győr, the city of three streams, 1.5 hours from Budapest and Bratislava and 2 hours from Vienna. History. Porva has an ancient history and is mentioned among about 40 other villages and cities in the founding document of Hungary.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
Sabis Vallis. Sabis Vallis is an ancient river valley in the Memnonia quadrangle of Mars, located at 5.3° south latitude and 152.5° west longitude. It is 206 km long and was named after a classical name for the present Sambre River in France and Belgium.

Geographic entities mentioned:
surface_form: sabis vallis
instance_of: Valley
coordinates: lat: -5.01
lon: 207.49
Soummam River. The Soummam River is a river in northern Algeria, born from the confluence of the Sahel River and the Bou Sellam River near Akbou and flowing into the Mediterranean at Béjaïa. Description. The waters that reach the sea in this place have for their origins the Mounts of Ain Oulmane, south of Sétif, Mount Dirah, south of Bouïra, and the extreme west of Djurdjura.

Geographic entities mentioned:
surface_form: Sahel River
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.42831
lon: 4.54511
surface_form: Bou Sellam River
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.40293
lon: 4.59121
surface_form: soummam
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.7294
lon: 5.0764
Soummam River. The Soummam River is a river in northern Algeria, born from the confluence of the Sahel River and the Bou Sellam River near Akbou and flowing into the Mediterranean at Béjaïa. Description. The waters that reach the sea in this place have for their origins the Mounts of Ain Oulmane, south of Sétif, Mount Dirah, south of Bouïra, and the extreme west of Djurdjura.

Geographic entities mentioned:
surface_form: Mounts
instance_of: Mountain
countries: Algeria
France
River valley. The Soummam valley is named after the river which crosses it. It is located in Kabylia, a region of northern Algeria, occupying a wide corridor in the wilaya of Béjaïa. The Béni Mansour-Bejaïa line is a regional railway that closely follows this river valley and connects to the national rail network in the municipality of Boudjellil.

Geographic entities mentioned:
surface_form: corridor
instance_of: Mountain
countries: Algeria
France
Soummam River. The Soummam River is a river in northern Algeria, born from the confluence of the Sahel River and the Bou Sellam River near Akbou and flowing into the Mediterranean at Béjaïa. Description. The waters that reach the sea in this place have for their origins the Mounts of Ain Oulmane, south of Sétif, Mount Dirah, south of Bouïra, and the extreme west of Djurdjura.

Geographic entities mentioned:
surface_form: soummam river
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.7294
lon: 5.0764
It is in fact that the physical geography of the region places the southernmost sources of the Soummam at the limits of the semi-arid zone characterized by rigors linked to the continental climate, whereas the closest sources are located in the territories Humid to temperate climate.

Geographic entities mentioned:
surface_form: soummam
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.7294
lon: 5.0764
The Soummam constitutes a dense and well-supplied hydrographic network, particularly in its part situated in the Tellian Atlas: Djurdjura, Babors and Bibans. Its watershed covers an area of 9,200 km2 spread over four wilayas: Bouïra, Bordj Bou Arréridj, Sétif and Béjaïa. With the Cheliff, the Tafna and the Rhummel, the Soummam is one of the largest rivers of Algeria. River valley.

Geographic entities mentioned:
surface_form: soummam
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.7294
lon: 5.0764
surface_form: babors
instance_of: Mountain
countries: Algeria
France
coordinates: lat: 36.55
lon: 5.4666666666667
The Soummam constitutes a dense and well-supplied hydrographic network, particularly in its part situated in the Tellian Atlas: Djurdjura, Babors and Bibans. Its watershed covers an area of 9,200 km2 spread over four wilayas: Bouïra, Bordj Bou Arréridj, Sétif and Béjaïa. With the Cheliff, the Tafna and the Rhummel, the Soummam is one of the largest rivers of Algeria. River valley.

Geographic entities mentioned:
surface_form: soummam
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.7294
lon: 5.0764
surface_form: rhummel
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.87212817
lon: 6.08567476
Its watershed covers an area of 9,200 km2 spread over four wilayas: Bouïra, Bordj Bou Arréridj, Sétif and Béjaïa. With the Cheliff, the Tafna and the Rhummel, the Soummam is one of the largest rivers of Algeria. River valley. The Soummam valley is named after the river which crosses it. It is located in Kabylia, a region of northern Algeria, occupying a wide corridor in the wilaya of Béjaïa.

Geographic entities mentioned:
surface_form: soummam
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.7294
lon: 5.0764
Between the Akfadou-Gouraya set in the north, the Biban chain (the historic territory of the Ait Abbas) in the south-east and the Sahel-Djurdjura valley (Tazmalt commune) in the south-west. The Soummam valley, which extends from Akbou to Béjaia, appears as a narrow winding corridor 65 km long (inside the wilaya of Béjaïa) over a maximum width of 4 km at El Kseur.

Geographic entities mentioned:
surface_form: soummam
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.7294
lon: 5.0764
Hydrology. The Soummam valley is drained by a dense hydrographic network, composed of numerous permanent and intermittent rivers, of which the Oued Soummam represents the main collector. According to the hydrological data collected between 1961 and 1976, the average flow of the Soummam is 25 m3 / s.

Geographic entities mentioned:
surface_form: soummam
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.7294
lon: 5.0764
surface_form: soummam
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.7294
lon: 5.0764
surface_form: oued soummam
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.7294
lon: 5.0764
Hydrology. The Soummam valley is drained by a dense hydrographic network, composed of numerous permanent and intermittent rivers, of which the Oued Soummam represents the main collector. According to the hydrological data collected between 1961 and 1976, the average flow of the Soummam is 25 m3 / s.

Geographic entities mentioned:
surface_form: soummam
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.7294
lon: 5.0764
During the 1970 flood period, the maximum recorded flow was 115.9 m3 / s and the low flow (during the months of July and August) dropped to 0.6 m3 / s. Indeed, these flows show great irregularities inter-annual, and therefore seasonal. At its mouth, the Soummam has a contribution of 700,106 m3 / year of water which it diversifies in the Mediterranean Sea (Visiterv, 1987).

Geographic entities mentioned:
surface_form: soummam
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.7294
lon: 5.0764
The tributaries of the left bank are located on slopes that are more watered in rain and snow, enabling them to channel a greater surface flow than the slopes drained by the tributaries of the right bank. Name. The word Soummam is a distortion of the word kabyle &quot;assemmam&quot;, which means &quot;acid&quot;. Pliny the Elder had cited the Soummam as being called &quot;Nasava&quot; by Ptolemy.

Geographic entities mentioned:
surface_form: soummam
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.7294
lon: 5.0764
This is also the main prey species in the Italian Alps above the tree line, comprising 49.7% of a sample size of 79 from 12 nests. In the Caspian Sea area of Kazakhstan, yellow ground squirrels (&quot;Spermophilus fulvus&quot;) are the most important mammalian prey at 23.4% of a sampling of 468 from 36 nests.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Kit fox (&quot;Vulpes macrotis&quot;), swift fox (&quot;Vulpes velox&quot;), gray fox (&quot;Urocyon cinereoargenteus&quot;) and island fox (&quot;Urocyon littoralis&quot;) are readily predated in North America. In Fennoscandia, golden eagles prey on Arctic foxes (&quot;Vulpes lagopus&quot;).

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Glazypeau Mountain. Glazypeau Mountain is a summit in Garland County, in the U.S. state of Arkansas. Glazypeau is derived from the French &quot;glaise à Paul&quot;, referring to a nearby salt lick.

Geographic entities mentioned:
surface_form: glazypeau mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.59194444
lon: -93.09194444
Alma Gol Lake. Alma Gol Lake (), also called Lake Ulmagol'&quot;, is a freshwater lake in Golestān Province, Iran near the Turkmenistan border. The lake is located north of Gonbad-e Qabus. The population of catfish (&quot;Silurus glanis&quot;) in the lake has drastically decreased because of increasing population growth among the villagers. Alma Gol is a winter habitat for migratory birds.

Geographic entities mentioned:
surface_form: alma gol lake
instance_of: Lake
countries: Iran
coordinates: lat: 37.35
lon: 54.583055555556
This was designed so that looking from Capital Hill, the War Memorial stood directly at the foot of Mount Ainslie. At the southwestern end of the land axis was Bimberi Peak. The straight edge of the circular segment that formed the central basin was designated the water axis, and it extended northwest towards Black Mountain.

Geographic entities mentioned:
surface_form: Mount Ainslie
instance_of: Mountain
countries: Australia
coordinates: lat: -35.27
lon: 149.15833333333
This was designed so that looking from Capital Hill, the War Memorial stood directly at the foot of Mount Ainslie. At the southwestern end of the land axis was Bimberi Peak. The straight edge of the circular segment that formed the central basin was designated the water axis, and it extended northwest towards Black Mountain.

Geographic entities mentioned:
surface_form: Bimberi Peak
instance_of: Mountain
countries: Australia
coordinates: lat: -35.660833333333
lon: 148.78916666667
Furthermore, the obelisk was a recognisable form (having long-held associations with notions of glory, death and eternity). Although most memorials were an initiative of a community or organisation, a Dangarsleigh family, in the Northern Tablelands of NSW, sought to memorialise their private loss by designing and commissioning a memorial of their own.

Geographic entities mentioned:
surface_form: Northern Tablelands
instance_of: Plateau
countries: Australia
coordinates: lat: -30.595277777777778
lon: 151.5
Raging Neisse. The Raging Neisse (, or &quot;Jauersche Neiße&quot;) is a river in Poland. It has a length of about and flows into the Kaczawa (Katzbach), which in turn flows into the Oder. Its largest tributary is the Little Neisse. The Raging Neisse rises at a height of on the western side of a mountain called the Kokosz on the Waldenburg Heights.

Geographic entities mentioned:
surface_form: Little Neisse
instance_of: Watercourse
countries: Poland
coordinates: lat: 51.00393
lon: 16.20931
STAs have been implemented in key positions at the northern edge of the Everglades to help keep phosphorus laden water from reaching the park, but concerns remain that the already elevated phosphorus levels in both Lake Okeechobee and the Everglades Agricultural Area (both heavy contributors to nutrient laden runoff) are so high that phosphorus loads into the park could continue for many decades.

Geographic entities mentioned:
surface_form: Lake Okeechobee
instance_of: Lake
countries: United States
coordinates: lat: 26.933333333333
lon: -80.8
It then heads east via Blumberg, here visible at the Riedöschinger Travertin and the Blauer Stein, in the direction of Engen in the Hegau with the volcanic formations of Hohenstoffeln, Hohenkrähen, Hohentwiel, Höwenegg, Hohenhewen and Neuhewen, Mägdeberg, Hohenkrähen, Staufen and Rosenegg to Lake Constance.

Geographic entities mentioned:
surface_form: Blauer Stein
instance_of: Mountain
countries: Germany
coordinates: lat: 47.82701
lon: 8.59824
surface_form: Hegau
instance_of: Mountain
countries: Germany
coordinates: lat: 47.795
lon: 8.75
surface_form: Hohenstoffeln
instance_of: Mountain
countries: Germany
coordinates: lat: 47.796388888889
lon: 8.7497222222222
surface_form: Hohenkrähen
instance_of: Mountain
countries: Germany
coordinates: lat: 47.798888888889
lon: 8.8205555555556
surface_form: Hohentwiel
instance_of: Mountain
countries: Germany
coordinates: lat: 47.764722222222
lon: 8.8188888888889
surface_form: Höwenegg
instance_of: Mountain
countries: Germany
coordinates: lat: 47.91444444
lon: 8.74166667
surface_form: Hohenhewen
instance_of: Mountain
countries: Germany
coordinates: lat: 47.835819444444
lon: 8.7477972222222
surface_form: Neuhewen
instance_of: Mountain
countries: Germany
coordinates: lat: 47.8791
lon: 8.7174
surface_form: Mägdeberg
instance_of: Mountain
countries: Germany
coordinates: lat: 47.805277777778
lon: 8.7975
surface_form: Hohenkrähen
instance_of: Mountain
countries: Germany
coordinates: lat: 47.798888888889
lon: 8.8205555555556
Geography. The town has three reservoirs: Qiguan Reservoir (), Meihua Reservoir () and Tuanshan Reservoir (). Chu River is known as &quot;Liushahe&quot;, a tributary of the Wei River, it flows through the town. The Fusi Mountain is a scenic spot in the town. Economy. The mountains in the town contains a rich supply of granite. Citrus, peach, prunus mume and tobacco are important to the economy.

Geographic entities mentioned:
surface_form: Fusi Mountain
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 28.0324
lon: 112.137
Fan Island. Fan Island is a summit located in the Grand Canyon, in Coconino County of northern Arizona, US. It is situated two miles south of Dutton Point, 2.5 miles west-northwest of Dox Castle, and 1.6 miles south-southwest of Masonic Temple. Topographic relief is significant as it rises above the Colorado River in. Fan Island was so named because the flat top resembles an unfolded hand fan.

Geographic entities mentioned:
surface_form: grand canyon
instance_of: Valley
countries: United States
coordinates: lat: 38.65888889
lon: -91.10388889
surface_form: fan island
instance_of: Mountain
countries: United States
coordinates: lat: 36.25748
lon: -112.36407
Fan Island. Fan Island is a summit located in the Grand Canyon, in Coconino County of northern Arizona, US. It is situated two miles south of Dutton Point, 2.5 miles west-northwest of Dox Castle, and 1.6 miles south-southwest of Masonic Temple. Topographic relief is significant as it rises above the Colorado River in. Fan Island was so named because the flat top resembles an unfolded hand fan.

Geographic entities mentioned:
surface_form: flat top
instance_of: Mountain
countries: United States
coordinates: lat: 34.9511
lon: -83.3156
surface_form: fan island
instance_of: Mountain
countries: United States
coordinates: lat: 36.25748
lon: -112.36407
Fan Island. Fan Island is a summit located in the Grand Canyon, in Coconino County of northern Arizona, US. It is situated two miles south of Dutton Point, 2.5 miles west-northwest of Dox Castle, and 1.6 miles south-southwest of Masonic Temple. Topographic relief is significant as it rises above the Colorado River in. Fan Island was so named because the flat top resembles an unfolded hand fan.

Geographic entities mentioned:
surface_form: fan island
instance_of: Mountain
countries: United States
coordinates: lat: 36.25748
lon: -112.36407
Fan Island was so named because the flat top resembles an unfolded hand fan. According to the Köppen climate classification system, Fan Island is located in a cold semi-arid climate zone, with precipitation runoff draining south to the Colorado River via Hakatai Canyon from the west aspect, and Burro Canyon from the east aspect.

Geographic entities mentioned:
surface_form: fan island
instance_of: Mountain
countries: United States
coordinates: lat: 36.25748
lon: -112.36407
Fan Island. Fan Island is a summit located in the Grand Canyon, in Coconino County of northern Arizona, US. It is situated two miles south of Dutton Point, 2.5 miles west-northwest of Dox Castle, and 1.6 miles south-southwest of Masonic Temple. Topographic relief is significant as it rises above the Colorado River in. Fan Island was so named because the flat top resembles an unfolded hand fan.

Geographic entities mentioned:
surface_form: dutton
instance_of: Mountain
countries: United States
coordinates: lat: 55.168
lon: -162.272
At its inception, Barrie was an establishment of houses and warehouses at the foot of the Nine Mile Portage from Kempenfelt Bay to Fort Willow, an indigenous transportation route that existed centuries before Europeans arrived in Simcoe County. The portage linked Kempenfelt Bay through Willow Creek, connecting Lake Simcoe to the Nottawasaga River which flows into Georgian Bay off Lake Huron.

Geographic entities mentioned:
surface_form: Lake Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Barrie is located in a snowbelt, a region that experiences regular lake-effect snow every year. Snow squalls are a common occurrence between November and January when the water temperature is often higher than the cold air passing over Lake Huron and Georgian Bay. The city averages of snow annually, the brunt of which coming from lake-effect snow events.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Tosor. The Tosor () is a river in Tong District and Jeti-Ögüz District of Issyk-Kul Region of Kyrgyzstan. It takes its rise on the north slopes of Teskey Ala-Too and falls into the lake Issyk-Kul. It is long, and has a drainage basin of. The river is fed by mixed sources of snow and glacier ice meltwater (85%) and rainfall (15%).

Geographic entities mentioned:
surface_form: Issyk-Kul
instance_of: Lake
countries: Kyrgyzstan
coordinates: lat: 42.416666666667
lon: 77.25
During this time a bad attack of bursitis left her with no movement in her left arm for five years, and the rest of the family took up her chores. The couple spent summers at a cottage on the Canadian shore of Lake Huron. A slipped disk suffered there gave her further trouble, and that and the bursitis caused her to switch from golf to swimming as her main exercise.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Composition and lyrics. &quot;You All Over Me&quot; is 3 minutes and 40 seconds long. Swift produced the song with Aaron Dessner, who recorded it with Bella Blasko at Long Pond Studios in Hudson Valley. Christopher Rowe recorded Swift's vocals at Kitty Committee Studio in London and Greg Kurstin and Julian Burg recorded Morris' vocals at No Expectations Studios in Los Angeles.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
SS Pewabic. The SS &quot;Pewabic&quot; was a package freighter that served ports on the Upper Great Lakes. She was launched in October 1863, fitted out in the spring of 1864, and was in active service until she sank off Thunder Bay Island in Lake Huron on August 9, 1865, due to collision with her sister vessel.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
The 13 JAK Rifles was placed under the command of the 79 Mountain Brigade after their victory at point 5140. The next assignment for Lt Col YK Joshi's battalion was to capture Point 4875, a strategically important peak located in the Mushkoh Valley. Since the feature dominated the National Highway 1 completely from Dras to Matayan, it became imperative for the Indian Army to capture Point 4875.

Geographic entities mentioned:
surface_form: Mushkoh Valley
instance_of: Valley
countries: India
coordinates: lat: 34.43
lon: 75.66
Towards the end of &quot;Description of Greece&quot;, Pausanias touches on the fruits of nature and products, such as the date palms of ancient Aulis, the wild strawberries at Mount Helicon, the olive oil in Tithorea, as well as the &quot;white blackbirds&quot; of Mount Kyllini (Cyllene) and the tortoises of Arcadia.

Geographic entities mentioned:
surface_form: Mount Helicon
instance_of: Mountain
countries: Greece
coordinates: lat: 38.352222222222
lon: 22.825
surface_form: Mount Kyllini
instance_of: Mountain
countries: Greece
coordinates: lat: 37.939166666667
lon: 22.396666666667
Langvatnet () is a lake that lies in Fauske Municipality in Nordland county, Norway. The lake lies about east of the town of Fauske. The village of Sulitjelma lies on the northeastern edge of the lake. Water from the lakes Kjelvatnet and Låmivatnet flow into the lake from the south and east. The water from Langvatnet flows out through the Sjønstå River to the west towards the lake Øvrevatnet.

Geographic entities mentioned:
surface_form: kjelvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 68.1873
lon: 17.1764
surface_form: kjelvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 67.0645
lon: 16.0296
surface_form: låmivatnet
instance_of: Lake
countries: Norway
coordinates: lat: 67.111944444444
lon: 16.215277777778
Langvatnet (Fauske). Langvatnet () is a lake that lies in Fauske Municipality in Nordland county, Norway. The lake lies about east of the town of Fauske. The village of Sulitjelma lies on the northeastern edge of the lake. Water from the lakes Kjelvatnet and Låmivatnet flow into the lake from the south and east.

Geographic entities mentioned:
surface_form: langvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 66.36861111
lon: 14.0825
surface_form: langvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 67.531944444444
lon: 16.181944444444
surface_form: langvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 68.13316
lon: 17.04921
surface_form: langvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 61.96136
lon: 7.3982
surface_form: langvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 67.136111111111
lon: 16.030833333333
surface_form: langvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 66.89061
lon: 14.14796
Langvatnet () is a lake that lies in Fauske Municipality in Nordland county, Norway. The lake lies about east of the town of Fauske. The village of Sulitjelma lies on the northeastern edge of the lake. Water from the lakes Kjelvatnet and Låmivatnet flow into the lake from the south and east. The water from Langvatnet flows out through the Sjønstå River to the west towards the lake Øvrevatnet.

Geographic entities mentioned:
surface_form: langvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 66.36861111
lon: 14.0825
surface_form: langvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 67.531944444444
lon: 16.181944444444
surface_form: langvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 68.13316
lon: 17.04921
surface_form: langvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 61.96136
lon: 7.3982
surface_form: langvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 67.136111111111
lon: 16.030833333333
surface_form: langvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 66.89061
lon: 14.14796
surface_form: øvrevatnet
instance_of: Lake
countries: Norway
coordinates: lat: 67.216666666667
lon: 15.666666666667
In the following year he was sent on an expedition to study the natural history of the Russian Empire. He explored the rivers Don and Volga, and the western and eastern coasts of the Caspian Sea. Whilst travelling in the Caucasus he was taken hostage by Usmey Khan of Khaïtakes and died of ill treatment in captivity in Akhmedkent, Dagestan. He was only 30 years of age.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
He was enthusiastically received in Detroit and rapidly became one of its best-known citizens, with the young men of his acquaintance soon styling themselves &quot;the Houghton boys&quot;. Houghton quickly was selected by Henry Rowe Schoolcraft, US Indian Agent and geologist, to act as physician-naturalist on expeditions through Lake Superior and the upper Mississippi valley in 1831 and 1832.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
He convincingly beat Germany's Felix Neureuther by half a second and future World Cup champion Marcel Hirscher, who led by 0.57 seconds after the first run. Pinturault's third win was at the super-combined in Wengen, Switzerland, where his superior slalom skills were key. After placing 22nd in the downhill portion, he finished 1.15 seconds ahead of Ivica Kostelić of Croatia.

Geographic entities mentioned:
surface_form: Wengen
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.592472
lon: 7.947944
It has a drainage basin of, the largest in the country, which covers almost one-fifth of the total area of the island. The Mahaweli Ganga starts at Polwathura (in the Mahawila area), a remote village of Nuwara-Eliya District in bank Nawalapitiya of Kandy District by further joining of Hatton Oya and Kotmale Oya. The river reaches the Bay of Bengal on the southwestern side of Trincomalee Bay.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
One of the many sources of the river is the Kotmale Oya. There is a misconception in Sri Lanka that the Mahaweli starts at Sri Pada Mountain. The Mahaweli gets its source waters from Horton Plains in Kirigalpoththa and the Thotupola mountain range. Starting of Mahaweli. The Mahaweli River starts from Polwathura/Mahavila area with its water source starting from the Horton Plains National Park.

Geographic entities mentioned:
surface_form: Kirigalpoththa
instance_of: Mountain
countries: Sri Lanka
coordinates: lat: 6.79916667
lon: 80.76666667
When Ronen competed in the Olympics he was tall, and weighed. Sailing career. In 1991 Ronen came in 4th in 420 in the IYRU Youth Sailing World Championships, in Largs, Scotland. In 1993 he won the gold medal in Laser II in the IYRU Youth Sailing World Championships, in Lake Garda, Italy. In 1995 Ronen won the gold medal in the 470 Open Junior World Championship, in Warnemunde, Germany.

Geographic entities mentioned:
surface_form: Lake Garda
instance_of: Lake
countries: Italy
coordinates: lat: 45.633333333333
lon: 10.666666666667
This figure was one of several examples of the eye being presented as a geoglyph to promote the fourth series. Others included another hill figure, approximately half the size of that at Uffington, being placed next to Urquhart Castle, Loch Ness, Scotland, which appeared from 3–5 May, alongside a crop circle in a secret location in Southern England and as a depiction on a beach in Kidwelly, Wales.

Geographic entities mentioned:
surface_form: Loch Ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
Heliamphora hispida. &quot;Heliamphora hispida&quot; (Latin: &quot;hispidus&quot; = covered with stiff or rough hairs, bristly) is a species of Marsh Pitcher Plant endemic to Cerro Neblina, the southernmost tepui of the Guiana Highlands at the Brazil-Venezuela border.

Geographic entities mentioned:
surface_form: Cerro Neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.80549444444444
lon: -66.005358333333
&quot;You can't get less Indian than a talking book, and an American talking book, so it was great,&quot; he said. Filming took place in Ireland at Ardmore Studios and on location in Wicklow during August–December 2002. Locations included Luggala Estate, Killruddery House and Garden, and Kiltegan. Release. Miramax Films released the film on April 9, 2004. Box office.

Geographic entities mentioned:
surface_form: Luggala Estate
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.105833333333
lon: -6.2836111111111
Binnendieze. Binnendieze is the common name for the river and canal system within the city walls of 's-Hertogenbosch, the Netherlands. It is a tourist attraction. Near the north-west tip of the city walls, the confluence of the Binnendieze with the rivers Aa and Dommel forms the short river Dieze, tributary of the Meuse (). Dieze and Dommel.

Geographic entities mentioned:
surface_form: binnendieze
instance_of: Watercourse
countries: Netherlands
coordinates: lat: 51.68527777777778
lon: 5.308055555555556
The stretch between Halder and 's-Hertogenbosch was renamed Dommel. Within the gates of 's-Hertogenbosch however, the Dommel retained the name 'Dieze', later changed to 'Binnendieze'. When the fortifications of 's-Hertogenbosch were dismantled in the 1870s, the main stream bed of the Dommel was rerouted to the west of the city. It created the 'Nieuwe Dommel', which is now simply known as Dommel.

Geographic entities mentioned:
surface_form: binnendieze
instance_of: Watercourse
countries: Netherlands
coordinates: lat: 51.68527777777778
lon: 5.308055555555556
which was already flowing from the city harbor of 's-Hertogenbosch to the Meuse. The natural situation. The part of the Dieze inside 's-Hertogenbosch is known as Binnendieze, or inner Dieze. Before human intervention, the Dommel flowed to the east of the town and made a bend south and east of the Windmolenberg (a natural height). It then continued to where the Hinthamereinde now is.

Geographic entities mentioned:
surface_form: binnendieze
instance_of: Watercourse
countries: Netherlands
coordinates: lat: 51.68527777777778
lon: 5.308055555555556
It is named Groote Hekel, after the beams (Hekels) that blocked the water gates. From the Groote Hekel the main course Groote Stroom flows east, the smaller Verwerstroom flows west. Both became known as Binnendieze. However, the name was also applied to other streams in the city. Some of these were arms of the Dieze, others were artificially connected to it.

Geographic entities mentioned:
surface_form: binnendieze
instance_of: Watercourse
countries: Netherlands
coordinates: lat: 51.68527777777778
lon: 5.308055555555556
These are remains of a steam-powered pumping station built in the early 1880s, and broken up in 1965. Groote Stroom. The original main course of the Binnendieze is known as Groote Stroom. It starts at the Groote Hekel in the southern city wall, and then bends to the east, before flowing back to the west, where it joins the city harbor at Jan Heins street.

Geographic entities mentioned:
surface_form: binnendieze
instance_of: Watercourse
countries: Netherlands
coordinates: lat: 51.68527777777778
lon: 5.308055555555556
In 1300-1319 a large bend of the Groote Stroom was cut off. It led to the construction of the Geerlingse bridge in the Hinthamer street. The Groote Stroom has some of the most spectacular sights of the Binnendieze. The water gate in the first city wall is one of these. It is remarkable that such a gate, that was superseded by later buildings, survived.

Geographic entities mentioned:
surface_form: binnendieze
instance_of: Watercourse
countries: Netherlands
coordinates: lat: 51.68527777777778
lon: 5.308055555555556
The southern stretch gradually started to disappear from the maps in the eighteenth century. During the construction of the Zuid-Willemsvaart in the 1820s, the Kleine Hekel north of this canal, was demolished, and the stretch of the Binnendieze from the Kleine Hekel to the Groote Stroom was cut off from the Aa. Hence it became known as 'Doode Stroom' (dead stream).

Geographic entities mentioned:
surface_form: binnendieze
instance_of: Watercourse
countries: Netherlands
coordinates: lat: 51.68527777777778
lon: 5.308055555555556
In the Snellestraat it is only visible in two places. At Guardianenhof there is a view of the Verwerstroom that shows that it changes course by flowing under a bridge in the Postelstraat. Indeed the prime attraction of the Verwerstroom and other parts of the Binnendieze, is that houses were built over it. It means that the Verwerstroom can still be navigated, but is hardly visible from the street.

Geographic entities mentioned:
surface_form: binnendieze
instance_of: Watercourse
countries: Netherlands
coordinates: lat: 51.68527777777778
lon: 5.308055555555556
The natural part south of the junction with the Kleine Vughterstroom, including the water gate has been filled up. The Vughterstroom is now one of the most famous parts of the 'Binnendieze'. The street that runs alongside it is very quiet and has many views on the water. The northern part has many cafés, restaurants and terraces.

Geographic entities mentioned:
surface_form: binnendieze
instance_of: Watercourse
countries: Netherlands
coordinates: lat: 51.68527777777778
lon: 5.308055555555556
The Vughterstroom is now one of the most famous parts of the 'Binnendieze'. The street that runs alongside it is very quiet and has many views on the water. The northern part has many cafés, restaurants and terraces. This is also one of the starting points for the popular boat trips on the Binnendieze. Kerkstroom. The Kerkstroom is named for flowing under the choir of St. Catherine's Church.

Geographic entities mentioned:
surface_form: binnendieze
instance_of: Watercourse
countries: Netherlands
coordinates: lat: 51.68527777777778
lon: 5.308055555555556
On foot, the western stretch can also be observed from the Kruisbroedershof. After disappearing, the Kleine Vughterstroom surfaces again in a closed-off space, before diving under Vughterstraat. The Kleine Vughterstroom is probably the least known part of the Binnendieze. It is publicly visible on street level in two places only.

Geographic entities mentioned:
surface_form: binnendieze
instance_of: Watercourse
countries: Netherlands
coordinates: lat: 51.68527777777778
lon: 5.308055555555556
It is the only stretch of the city center of 's-Hertogenbosch that is reminiscent of the canals of cities in Holland, and this is no coincidence. On all other stretches of the Binnendieze, the (smaller) canals run through the backyards of the houses. In the Binnenhaven, and in the cities of Holland, the canals run in front of the houses.

Geographic entities mentioned:
surface_form: binnendieze
instance_of: Watercourse
countries: Netherlands
coordinates: lat: 51.68527777777778
lon: 5.308055555555556
However, its uniform style does allow visitors to get an impression of the sheer size of the former factory. The debate for conservation. After the Binnendieze lost its defensive and transport functions, it became something like an open sewer in the nineteenth and early twentieth century. Later alternative waste disposal techniques became available, e.g.

Geographic entities mentioned:
surface_form: binnendieze
instance_of: Watercourse
countries: Netherlands
coordinates: lat: 51.68527777777778
lon: 5.308055555555556