Sarmila/GeoWiki-Features huggingface dataset:
Rheinwald. The Rheinwald (from Latin &quot;Rheni vallis&quot; meaning &quot;Rhine Valley&quot;; Romansh: &quot;Valrain&quot;) is a valley in the Canton of Grisons in Switzerland, the first section of the Hinterrhein valley. The river Hinterrhein flows through three valleys in the Grisons, the Rheinwald, the Schams and the Domleschg. Geography.

Geographic entities mentioned:
surface_form: Schams
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.612
lon: 9.426
surface_form: rheinwald
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.551778
lon: 9.319788
surface_form: rheinwald
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.551778
lon: 9.319788
surface_form: domleschg
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.7507
lon: 9.43314
surface_form: schams
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.612
lon: 9.426
Geography. The Rheinwald is about 26 km long and mainly runs from East to West. It is lined on both sides with peaks of over 3000 m high. The highest peaks are the Rheinwaldhorn (3402 m) to the West and the Pizzo Tambo (3279 m) in the South. The Hinterrhein leaves the valley at the entrance to the Rofla Gorge, which separates the Rheinwald from the Schams valley.

Geographic entities mentioned:
surface_form: Rheinwaldhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.493611111111
lon: 9.04
The highest peaks are the Rheinwaldhorn (3402 m) to the West and the Pizzo Tambo (3279 m) in the South. The Hinterrhein leaves the valley at the entrance to the Rofla Gorge, which separates the Rheinwald from the Schams valley. Two mountain passes lead South from the Rheinwald: the San Bernardino Pass into Misox valley and the Splügen Pass into Val San Giacomo in Italy.

Geographic entities mentioned:
surface_form: Schams
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.612
lon: 9.426
surface_form: rheinwald
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.551778
lon: 9.319788
surface_form: schams
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.612
lon: 9.426
The San Bernardino Tunnel (Swiss Highway A13) was opened in 1967 and stays open all winter. Mule tracks on Mount Safierberg and Mount Valserberg connect the Rheinwald with its Northern neighbour Safien valley and Vals. Another trail leads through the Val Curciusa valley via Bocchetta di Curciusa Pass and then connects to the San Bernardino.

Geographic entities mentioned:
surface_form: Val Curciusa
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.5052
lon: 9.2599194444444
surface_form: val curciusa
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.5052
lon: 9.2599194444444
Rheinwald. The Rheinwald (from Latin &quot;Rheni vallis&quot; meaning &quot;Rhine Valley&quot;; Romansh: &quot;Valrain&quot;) is a valley in the Canton of Grisons in Switzerland, the first section of the Hinterrhein valley. The river Hinterrhein flows through three valleys in the Grisons, the Rheinwald, the Schams and the Domleschg. Geography.

Geographic entities mentioned:
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.50486111
lon: 7.64305556
surface_form: rheinwald
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.551778
lon: 9.319788
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6608
lon: 8.05469
Rheinwald. The Rheinwald (from Latin &quot;Rheni vallis&quot; meaning &quot;Rhine Valley&quot;; Romansh: &quot;Valrain&quot;) is a valley in the Canton of Grisons in Switzerland, the first section of the Hinterrhein valley. The river Hinterrhein flows through three valleys in the Grisons, the Rheinwald, the Schams and the Domleschg. Geography.

Geographic entities mentioned:
surface_form: rheinwald
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.551778
lon: 9.319788
The Hinterrhein leaves the valley at the entrance to the Rofla Gorge, which separates the Rheinwald from the Schams valley. Two mountain passes lead South from the Rheinwald: the San Bernardino Pass into Misox valley and the Splügen Pass into Val San Giacomo in Italy. The San Bernardino Tunnel (Swiss Highway A13) was opened in 1967 and stays open all winter.

Geographic entities mentioned:
surface_form: rheinwald
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.551778
lon: 9.319788
surface_form: misox
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.385
lon: 9.235
The San Bernardino Tunnel (Swiss Highway A13) was opened in 1967 and stays open all winter. Mule tracks on Mount Safierberg and Mount Valserberg connect the Rheinwald with its Northern neighbour Safien valley and Vals. Another trail leads through the Val Curciusa valley via Bocchetta di Curciusa Pass and then connects to the San Bernardino.

Geographic entities mentioned:
surface_form: rheinwald
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.551778
lon: 9.319788
surface_form: safien valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.696666666667
lon: 9.3244444444444
The Rheinwald Kreis is a sub-district of the Hinterrhein District. It includes the municipalities of Hinterrhein, Nufenen, Splügen and Sufers. The municipality of Val Curciusa belongs orographically to the Rheinwald, but administratively to the district of San Bernardino. History. The San Bernardino Pass and the route via Splügen have been used since at least the days of the Romans.

Geographic entities mentioned:
surface_form: rheinwald
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.551778
lon: 9.319788
Their language and culture shape the valley today. The 1286 &quot;Erblehensbrief&quot; (&quot;Letter of enfeoffment&quot;) documents the legal relations between the settlers and their ruler. In 1337, after the death of the last Baron of Vaz, the Rheinwald came was given as a dowry to the counts of Werdenberg-Sargans. They sold it in 1493 to the Trivulzio family of Milan.

Geographic entities mentioned:
surface_form: rheinwald
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.551778
lon: 9.319788
They sold it in 1493 to the Trivulzio family of Milan. In 1616, the umbrella contract with the Trivulzio was terminated, and after paying the last interest payment the inhabitants of the Rheinwald obtained full autonomy within the Grey League, to which they had belonged to since around 1400.

Geographic entities mentioned:
surface_form: rheinwald
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.551778
lon: 9.319788
History. The San Bernardino Pass and the route via Splügen have been used since at least the days of the Romans. The Rheinwald valley, however, was sparsely inhabited until well into the High Middle Ages. During the 13th Century, Walser settlers travelled into the valley, at the behest of the Barons of Sax-Misox and the Barons of Vaz. Their language and culture shape the valley today.

Geographic entities mentioned:
surface_form: misox
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.385
lon: 9.235
They broke away from Eswatini around the year 1540. From mainline Swazi, Batau settled at Wakkerstroom and then Seokodibeng around 1624, at a place that is now called Lake Chrissie. From Lake Chrissie (Seokodibeng) they went to Mokwena River (which today is called Crocodile River) settling there in the late 17th century.

Geographic entities mentioned:
surface_form: Lake Chrissie
instance_of: Lake
countries: South Africa
coordinates: lat: -26.3333
lon: 30.2167
The Pakistani government denied the allegation. Accidents. A few incidents have occurred when radioactive material was disposed of improperly, shielding during transport was defective, or when it was simply abandoned or even stolen from a waste store. In the Soviet Union, waste stored in Lake Karachay was blown over the area during a dust storm after the lake had partly dried out.

Geographic entities mentioned:
surface_form: Lake Karachay
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 55.677222222222
lon: 60.799444444444
Tanat Valley. The Tanat Valley (Welsh:) is a large valley in northern Powys, Wales, formed by the course of the River Tanat and its tributaries. Situated south of the Berwyn range, the valley forms from at Llangynog from the merger of two narrow valleys, the Cwm Pennant and Cwm Rhiwarth.

Geographic entities mentioned:
surface_form: tanat valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 52.811051
lon: -3.339272
A large waterfall, the Pistyll Rhaeadr, lies at the head of the valley. Prehistoric and ancient settlements. The earliest evidence of human presence in the Tanat Valley dates to the Upper Palaeolithic; a barbed point from indicates temporary hunting settlements in the area. Hunter-gatherer seasonal settlements likely existed in the Mesolithic and Neolithic.

Geographic entities mentioned:
surface_form: tanat valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 52.811051
lon: -3.339272
Mining operations at Llangynog led to large-scale heavy metal contamination across the whole of the valley. The Tanat Valley Light Railway was opened in 1904 to serve the communities in the region, continuing operations until 1964.

Geographic entities mentioned:
surface_form: tanat valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 52.811051
lon: -3.339272
Umfolozi River. The Umfolozi River (also uMfolozi, Imfolozi or Mfolozi'&quot;) is a river in KwaZulu-Natal, a province of South Africa. It is formed by the confluence of the Black (&quot;Imfolozi emnyama&quot;) and White Umfolozi (&quot;Imfolozi emhlope&quot;) Rivers near the southeastern boundary of the Hluhluwe-Umfolozi Game Reserve.

Geographic entities mentioned:
surface_form: Black
instance_of: Watercourse
countries: South Africa
coordinates: lat: -28.34944444
lon: 31.98083333
Lucia Estuary. This caused the estuary mouth to rapidly silt up. There had only been one record of this occurring until that time, during the sustained drought during the 1930s. At the Black Umfolozi River and the White Umfolozi River, join to form the Umfolozi. Characteristics. It is a meandering river, with a catchment area of 11,068 km3.

Geographic entities mentioned:
surface_form: Black Umfolozi River
instance_of: Watercourse
countries: South Africa
coordinates: lat: -28.34944444
lon: 31.98083333
Pickerel Lake (Hubbard County, Minnesota). Pickerel Lake is a lake in Hubbard County, in the U.S. state of Minnesota. Pickerel Lake was named for its stock of the pickerel fish.

Geographic entities mentioned:
surface_form: pickerel lake
instance_of: Lake
countries: United States
coordinates: lat: 47.038611111111
lon: -94.995555555556
surface_form: pickerel lake
instance_of: Lake
countries: United States
coordinates: lat: 43.63
lon: -93.4075
surface_form: pickerel lake
instance_of: Lake
countries: United States
coordinates: lat: 45.5167
lon: -97.2833
surface_form: pickerel lake
instance_of: Lake
countries: United States
coordinates: lat: 44.91666667
lon: -93.12055556
After the restoration of civil rights to Confederate officers, John Barbour was elected as a Democrat to the 47th and two succeeding Congresses (March 4, 1881 - March 3, 1887). He succeeded Eppa Hunton II, a fellow Shenandoah Valley lawyer who declined to seek renomination. Barbour served as chairman of the Committee on the District of Columbia (48th and 49th Congresses).

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Apollonia (Athos). Apollonia (Greek:) was an ancient town in the peninsula of Acte, or Mount Athos in Macedonia, the inhabitants of which were called &quot;Macrobii&quot;.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Rubner Peak. Rubner Peak () is the highest point on the sharp ridge separating McCance and Widdowson Glaciers, just south of Darbel Bay on the northeast coast of Pernik Peninsula, Loubet Coast in Graham Land. Photographed by the Falkland Islands and Dependencies Aerial Survey Expedition (FIDASE) in 1956–57.

Geographic entities mentioned:
surface_form: rubner peak
instance_of: Mountain
coordinates: lat: -66.7333
lon: -65.85
The smallest known amphipods are less than long. The size of amphipods is limited by the availability of dissolved oxygen, such that the amphipods in Lake Titicaca at an altitude of can only grow up to, compared to lengths of in Lake Baikal at. Some amphipods exhibit sexual dimorphism.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Some 1,900 species, or 20% of the total amphipod diversity, live in fresh water or other non-marine waters. Notably rich endemic amphipod faunas are found in the ancient Lake Baikal and waters of the Caspian Sea basin, with over 350 species inhabitting Lake Baikal.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
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
In the Early Middle Ages the palace was an important place in the Holy Roman Empire, serving as an important base for the Ottonians in the 10th century in particular. Although it subsequently lost its political significance to the newly established Imperial Palace of Goslar at Rammelsberg, it developed into an independent settlement with a busy industrial quarter.

Geographic entities mentioned:
surface_form: Rammelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.8875
lon: 10.431666944444444
To the north an original bailey developed, which at first covered only three hectares, however. Settlement. Already under Henry II Werla had begun to lose its political importance on account of the newly established palace at Goslar, which controlled the rich vein of silver at Rammelsberg. However, Werla's palace status was not abolished as the Sachsenspiegel would later claim.

Geographic entities mentioned:
surface_form: Rammelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.8875
lon: 10.431666944444444
Nag Hammadi is about west of ancient Chenoboskion ()
The &quot;Nag Hammadi library&quot;, an important collection of 2nd-century Gnostic texts, was found at
Jabal al-Ṭārif near Nag Hammadi in 1945. The city was the site of the Nag Hammadi Massacre in January 2010, in which eight Coptic Christians were shot dead by three men. In total, nineteen Coptic Christians were attacked. Economy.

Geographic entities mentioned:
surface_form: Jabal al-Ṭārif
instance_of: Mountain
countries: Egypt
coordinates: lat: 26.1286
lon: 32.21599
It is situated in the Moquegua Region, Mariscal Nieto Province, Torata District. It lies southwest of the mountain Iruma and east of Achucallani. Surehuayco is also the name of an intermittent stream north of the mountain.

Geographic entities mentioned:
surface_form: Achucallani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.9386
lon: -70.6258
surface_form: achucallani
instance_of: Mountain
countries: Peru
coordinates: lat: -15.10777778
lon: -70.68194444
surface_form: achucallani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.9386
lon: -70.6258
Surehuayco. Surehuayco (possibly from Aymara &quot;suri&quot; rhea, &quot;wayku&quot; brook or gorge, &quot;rhea brook (or gorge)&quot;) and from Quechua &quot;Suri Wayq'u&quot;) is a mountain in the Andes of southern Peru, about high. It is situated in the Moquegua Region, Mariscal Nieto Province, Torata District. It lies southwest of the mountain Iruma and east of Achucallani.

Geographic entities mentioned:
surface_form: suri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0686
lon: -69.9925
surface_form: suri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0686
lon: -69.9925
surface_form: surehuayco
instance_of: Mountain
countries: Peru
coordinates: lat: -16.9303
lon: -70.5978
Surehuayco. Surehuayco (possibly from Aymara &quot;suri&quot; rhea, &quot;wayku&quot; brook or gorge, &quot;rhea brook (or gorge)&quot;) and from Quechua &quot;Suri Wayq'u&quot;) is a mountain in the Andes of southern Peru, about high. It is situated in the Moquegua Region, Mariscal Nieto Province, Torata District. It lies southwest of the mountain Iruma and east of Achucallani.

Geographic entities mentioned:
surface_form: surehuayco
instance_of: Mountain
countries: Peru
coordinates: lat: -16.9303
lon: -70.5978
There they scouted for the most suitable locations for the script's dramatic outdoor scenes once filming commenced. In addition to choosing sites at Niagara Falls, they also chose locations at nearby Three Sisters Islands and at Ausable Chasm much farther away in the Adirondack Mountains.

Geographic entities mentioned:
surface_form: Ausable Chasm
instance_of: Landform
countries: United States
coordinates: lat: 44.529166666667
lon: -73.461111111111
Rhododendron cumberlandense. &quot;Rhododendron cumberlandense&quot;, the Cumberland rhododendron or Cumberland azalea, is a species of flowering plant in the family Ericaceae. It is native to the southeastern United States. A deciduous shrub with red flowers reaching, it is typically found growing on the Cumberland Plateau.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
Arnold Power Station. The Arnold Power Station is a hydroelectric facility fed from Lake Brunner on the Arnold River in West Coast, New Zealand, owned and operated by TrustPower. Commissioned in 1932, the plant is rated at and has an average annual output of. History.

Geographic entities mentioned:
surface_form: Lake Brunner
instance_of: Lake
countries: New Zealand
coordinates: lat: -42.615
lon: 171.45
The Arnold station had two variable-pitch Kaplan turbines each driving generators rated at 1,500 kW. Connecting to the National Grid. The settlements of the West Coast did not finally receive a supply of electricity from the National Grid until October 1938, when a 66 kV transmission line was completed from Lake Coleridge across the Southern Alps through Arthur's Pass to the West Coast.

Geographic entities mentioned:
surface_form: Lake Coleridge
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.291
lon: 171.499
Goat Island Mountain. Goat Island Mountain is a ridge-like mountain located in Mount Rainier National Park, in Pierce County of Washington state. It is part of the Cascade Range, and lies east-northeast of the summit of Mount Rainier. This mountain is quite visible from the Sunrise Historic District and the many trails surrounding the Sunrise area.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
This mountain is quite visible from the Sunrise Historic District and the many trails surrounding the Sunrise area. The Wonderland Trail provides an approach to this mountain, and the summit offers views of Cowlitz Chimneys, Fryingpan Glacier, and Mount Rainier. Burroughs Mountain is its nearest higher neighbor, to the northwest.

Geographic entities mentioned:
surface_form: Cowlitz Chimneys
instance_of: Landform
countries: United States
coordinates: lat: 46.848877
lon: -121.609409
surface_form: mount rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
The Wonderland Trail provides an approach to this mountain, and the summit offers views of Cowlitz Chimneys, Fryingpan Glacier, and Mount Rainier. Burroughs Mountain is its nearest higher neighbor, to the northwest. Precipitation runoff from Goat Island Mountain drains into the White River. The mountain's descriptive name derives from mountain goats that were often seen on the peak.

Geographic entities mentioned:
surface_form: Burroughs Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.901644
lon: -121.713687
Goat Island Mountain. Goat Island Mountain is a ridge-like mountain located in Mount Rainier National Park, in Pierce County of Washington state. It is part of the Cascade Range, and lies east-northeast of the summit of Mount Rainier. This mountain is quite visible from the Sunrise Historic District and the many trails surrounding the Sunrise area.

Geographic entities mentioned:
surface_form: island mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.9632
lon: -123.492
surface_form: goat island mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.88011
lon: -121.66065
Goat Island Mountain. Goat Island Mountain is a ridge-like mountain located in Mount Rainier National Park, in Pierce County of Washington state. It is part of the Cascade Range, and lies east-northeast of the summit of Mount Rainier. This mountain is quite visible from the Sunrise Historic District and the many trails surrounding the Sunrise area.

Geographic entities mentioned:
surface_form: island mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.9632
lon: -123.492
surface_form: mount rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: goat island mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.88011
lon: -121.66065
The Wonderland Trail provides an approach to this mountain, and the summit offers views of Cowlitz Chimneys, Fryingpan Glacier, and Mount Rainier. Burroughs Mountain is its nearest higher neighbor, to the northwest. Precipitation runoff from Goat Island Mountain drains into the White River. The mountain's descriptive name derives from mountain goats that were often seen on the peak.

Geographic entities mentioned:
surface_form: island mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.9632
lon: -123.492
surface_form: goat island mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.88011
lon: -121.66065
The mountain's descriptive name derives from mountain goats that were often seen on the peak. The toponym was officially adopted in 1932 by the United States Board on Geographic Names. Climate. Goat Island Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originating in the Pacific Ocean travel northeast toward the Cascade Mountains.

Geographic entities mentioned:
surface_form: island mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.9632
lon: -123.492
surface_form: goat island mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.88011
lon: -121.66065
Inahamne. Inahamne is a lake in Lääne County Lääne-Nigula Parish on the island of Osmussaar. The lake lies in the southern part of Osmussaar, from Storhamne bay. The shoreline of the lake is long. Its area is and its drainage basin's size is.

Geographic entities mentioned:
surface_form: inahamne
instance_of: Lake
countries: Estonia
coordinates: lat: 59.281388888889
lon: 23.41
2022 ICF Canoe Sprint World Championships – Men's C-1 1000 metres. The men's C-1 1000 metres competition at the 2022 ICF Canoe Sprint World Championships in Dartmouth took place on Lake Banook. Heats. The fastest boat in each heat advanced directly to the A final. The next six fastest boats in each heat advanced to the semifinals. Semifinals.

Geographic entities mentioned:
surface_form: Lake Banook
instance_of: Lake
countries: Canada
coordinates: lat: 44.6809
lon: -63.5569
However political boundaries and political debates have distorted the extent of the area in some sources. In Burma. It is used in Chin State, Tiddim, and the Chin Hills. Use of Burmese has increased in the Zo speaking Chin State since the 1950s. &quot;Ethnologue&quot; reports that Zou is spoken in the following townships of Myanmar. In Bangladesh. In Bangladesh it is used by the Bawm people.

Geographic entities mentioned:
surface_form: Chin Hills
instance_of: Mountain
countries: Myanmar
coordinates: lat: 22.5
lon: 93.5
The purificatory bath is believed to remove sins and after the dip, pilgrims offer charitable gifts in the hope of being rewarded in the current life and subsequent lives. The Hindus consider taking a pilgrimage and holy dip during the Theerthavari as sacred. The Theerthavari festivals in a given region also follow the upstream and downstream flow of river, like in the case of river Kaveri.

Geographic entities mentioned:
surface_form: Kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
2014 Mount Everest ice avalanche. On 18 April 2014, seracs on the western spur of Mount Everest failed, resulting in an ice avalanche that killed sixteen climbing Sherpas in the Khumbu Icefall. This was the same icefall where the 1970 Mount Everest disaster had taken place.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Conditions change regularly with the glacier's shifting ice, so climbing guides must find and maintain a new route through the icefall each season. Ice avalanche. At approximately 06:45 local time (01:00 UTC, 18 April 2014), an ice avalanche occurred on the southern side of Mount Everest, at an elevation of approximately. Twenty-five men, mostly Sherpas, were buried in the avalanche.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Aldegondabreen. Aldegondabreen is a glacier in Nordenskiöld Land at Spitsbergen, Svalbard, Norway. It is named after Infanta Adelgundes, Duchess of Guimarães. The glacier has a length of about 5.5 kilometers. It flows from Qvigstadfjellet, Christensenfjella and Hermod Petersenfjellet towards Grønfjorden.

Geographic entities mentioned:
surface_form: Qvigstadfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 77.956
lon: 14.054
surface_form: Christensenfjella
instance_of: Mountain
countries: Norway
coordinates: lat: 77.963
lon: 13.973
McDaniels, Kentucky. McDaniels is an unincorporated community in Breckinridge County, Kentucky, United States. McDaniels is located along Kentucky Route 259, due south of Hardinsburg. McDaniels is situated on Rough River Lake, which collects the North Fork Rough River, which flows for its entire length in Breckinridge County. McDaniels has a post office with ZIP code 40152. History.

Geographic entities mentioned:
surface_form: Rough River Lake
instance_of: Lake
countries: United States
coordinates: lat: 37.6116
lon: -86.484
The first zoned section was published on Sundays only for the San Gabriel Valley in April 1952 under the direction of Mike Straszer, who was in charge of all succeeding zoned editions until 1958. An editorial in the &quot;Times's&quot; San Gabriel Valley section explained that
...

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
The San Gabriel Valley Section is the first of these. The next zoned editions were opened in the San Fernando Valley and in the Glendale areas on March 4, 1956. A one-year anniversary layout listed the names of key people working on the San Fernando section as Straszer, Maurice Stoller, Mary Nogueras, Albert Markado, Norman Dash, Richard W. Degnon and Fred Baumberger.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Degnon and Fred Baumberger. By the end of April 1957, zoned editions were appearing in the San Gabriel Valley (since 1952), Southern Communities (around 1954), Orange County (1954), the San Fernando Valley (1956), Glendale-Verdugo Hills (1956), as well as the newest sections, the Westside (1957) and Centinela-South Bay (1957).

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
In 1995, the San Fernando Valley staff was reduced &quot;significantly.&quot;
By 1999, the suburban sections had been almost entirely supplanted by a new venture, &quot;Our Times,&quot; a &quot;Los Angeles Times&quot; subsidiary that published separate community-oriented newspapers in Brea, Conejo Valley, the Crenshaw District in Los Angeles, Montebello and Pico Rivera, Irvine, Laguna Hills, Mission Viejo, Santa Clarita, Santa Monica, Sherman Oaks, Simi Valley and Ventura.

Geographic entities mentioned:
surface_form: Conejo Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
History. The Unified Fire Authority got its start on November 21, 1921, when the Salt Lake County Fire Department was formed. Discussions for the formation of a unified department within the Salt Lake Valley began over half a century later in 1998. Salt Lake County Fire had been providing emergency services to several contract cities in addition to the Unincorporated Salt Lake County.

Geographic entities mentioned:
surface_form: Salt Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.6839
lon: -111.978
Lake Malone. Lake Malone is a reservoir in Logan, Muhlenberg, and Todd counties in Kentucky. It was impounded from Rocky Creek, a tributary of the Mud River, in 1961, and named for Mr. and Mrs. Wallace C. Malone who donated a large tract of land for the lake.

Geographic entities mentioned:
surface_form: lake malone
instance_of: Lake
countries: United States
coordinates: lat: 37.0713
lon: -87.0399
Lake Malone. Lake Malone is a reservoir in Logan, Muhlenberg, and Todd counties in Kentucky. It was impounded from Rocky Creek, a tributary of the Mud River, in 1961, and named for Mr. and Mrs. Wallace C. Malone who donated a large tract of land for the lake.

Geographic entities mentioned:
surface_form: rocky creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.12638889
lon: -91.17166667
Water skiing at the 2009 World Games. The water skiing events at the 2009 World Games in Kaohsiung was played between 22 and 26 July. 81 athletes, from 29 nations, participated in the tournament. The water skiing competition took place at Lotus Pond.

Geographic entities mentioned:
surface_form: Lotus Pond
instance_of: Lake
countries: Taiwan
coordinates: lat: 22.685061111111
lon: 120.29739722222
It ranks as the second-highest summit in the Oquirrh Mountains, and sixth-highest in Tooele County. Precipitation runoff from the mountain's west slope drains to Rush Valley via Ophir Creek, whereas the east slope drains to Utah Lake via West Canyon Wash. Topographic relief is significant as the summit rises above Left Fork West Canyon in two miles (3.2 km).

Geographic entities mentioned:
surface_form: Rush Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.184166666667
lon: -112.39194444444
Lowe Peak (Utah). Lowe Peak is a mountain summit located on the common boundary that Tooele County shares with Utah County in Utah, United States. Description. Lowe Peak is located southwest of downtown Salt Lake City and west of Lehi in the Oquirrh Mountains which are part of the Great Basin Ranges.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: lowe peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.425555555556
lon: -112.19916666667
Lowe Peak (Utah). Lowe Peak is a mountain summit located on the common boundary that Tooele County shares with Utah County in Utah, United States. Description. Lowe Peak is located southwest of downtown Salt Lake City and west of Lehi in the Oquirrh Mountains which are part of the Great Basin Ranges.

Geographic entities mentioned:
surface_form: lowe peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.425555555556
lon: -112.19916666667
Lowe Peak is a mountain summit located on the common boundary that Tooele County shares with Utah County in Utah, United States. Description. Lowe Peak is located southwest of downtown Salt Lake City and west of Lehi in the Oquirrh Mountains which are part of the Great Basin Ranges. It ranks as the second-highest summit in the Oquirrh Mountains, and sixth-highest in Tooele County.

Geographic entities mentioned:
surface_form: lowe peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.425555555556
lon: -112.19916666667
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2767785
lon: -98.6946248
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 44.965
lon: -96.443611111111
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.635555555556
lon: -99.9175
This mountain's toponym has been officially adopted by the United States Board on Geographic Names. Climate. Lowe Peak is set within the Great Basin Desert which has hot summers and cold winters. The desert is an example of a cold desert climate as the desert's elevation makes temperatures cooler than lower elevation deserts.

Geographic entities mentioned:
surface_form: lowe peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.425555555556
lon: -112.19916666667
The railway opened on 13 May 1885 and it closed on 10 June 1949. The line branched off of the Main Line in Parattah outside the Tudor style Parattah Hotel and followed parallel to the Main Line for approximately before branching off in a north west direction towards Lake Dulverton.

Geographic entities mentioned:
surface_form: Lake Dulverton
instance_of: Lake
countries: Australia
coordinates: lat: -42.3
lon: 147.383
Rogers, Arkansas. Rogers is a city in Benton County, Arkansas, United States. Located in the Ozarks, it is part of the Northwest Arkansas region, one of the fastest growing metro areas in the country. Rogers was the location of the first Walmart store, whose corporate headquarters is located in neighboring Bentonville.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
Farrenberg. Farrenberg is a mountain of Baden-Württemberg, Germany.

Geographic entities mentioned:
surface_form: farrenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.389166666667
lon: 9.0708333333333
History. It is believed that Nabha House was built by Maharaja Hira Singh. It was built as residence for kings who would come to Sannhit Sarovar to take bath during solar eclipses. After independence, the Nabha House was used as space for government school and then for an Ayurveda college. Nabha House was also used as classrooms and office space by Kurukshetra University in 1957 to 1959.

Geographic entities mentioned:
surface_form: Sannhit Sarovar
instance_of: Lake
countries: India
coordinates: lat: 29.966666666666665
lon: 76.83583333333333
Mount Outram. Mount Outram is a mountain summit located in the Howse River Valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Forbes, to the southwest. Glacier Lake is situated to the north, and the Sir James Glacier lies below the south aspect of the peak.

Geographic entities mentioned:
surface_form: Mount Forbes
instance_of: Mountain
countries: Canada
coordinates: lat: 51.859722222222224
lon: -116.93166666666667
History. Mount Outram was named in 1920 for James Outram (1864-1925), a mountaineer who made numerous first ascents in the Canadian Rockies including Mount Assiniboine, Chancellor Peak, Cathedral Mountain, and Mount Wilson. The first ascent of the mountain was made in 1924 by F.V. Field, W.O. Field, and L. Harris, with guides Edward Feuz Jr. and J. Biner.

Geographic entities mentioned:
surface_form: Mount Assiniboine
instance_of: Mountain
countries: Canada
coordinates: lat: 50.86972222222222
lon: -115.6511111111111
surface_form: Chancellor Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.22416666666667
lon: -116.51027777777777
surface_form: assiniboine
instance_of: Mountain
countries: Canada
coordinates: lat: 50.86972222222222
lon: -115.6511111111111
surface_form: mount wilson
instance_of: Mountain
countries: Canada
coordinates: lat: 52.0184
lon: -116.8014
surface_form: cathedral mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.39666666666667
lon: -116.39027777777778
surface_form: mount outram
instance_of: Mountain
countries: Canada
coordinates: lat: 51.88166666666667
lon: -116.87527777777778
surface_form: cathedral mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.46666666666667
lon: -123.00861111111111
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mount outram
instance_of: Mountain
countries: Canada
coordinates: lat: 49.289722222222224
lon: -121.15833333333333
Its nearest higher peak is Mount Forbes, to the southwest. Glacier Lake is situated to the north, and the Sir James Glacier lies below the south aspect of the peak. Mount Outram can be seen from the Icefields Parkway southwest of Saskatchewan Crossing, with optimum photography conditions in morning light. History.

Geographic entities mentioned:
surface_form: glacier lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.92056
lon: -116.85889
Mount Outram. Mount Outram is a mountain summit located in the Howse River Valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Forbes, to the southwest. Glacier Lake is situated to the north, and the Sir James Glacier lies below the south aspect of the peak.

Geographic entities mentioned:
surface_form: mount outram
instance_of: Mountain
countries: Canada
coordinates: lat: 51.88166666666667
lon: -116.87527777777778
surface_form: mount outram
instance_of: Mountain
countries: Canada
coordinates: lat: 49.289722222222224
lon: -121.15833333333333
Mount Outram. Mount Outram is a mountain summit located in the Howse River Valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Forbes, to the southwest. Glacier Lake is situated to the north, and the Sir James Glacier lies below the south aspect of the peak.

Geographic entities mentioned:
surface_form: mount outram
instance_of: Mountain
countries: Canada
coordinates: lat: 51.88166666666667
lon: -116.87527777777778
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mount outram
instance_of: Mountain
countries: Canada
coordinates: lat: 49.289722222222224
lon: -121.15833333333333
Its nearest higher peak is Mount Forbes, to the southwest. Glacier Lake is situated to the north, and the Sir James Glacier lies below the south aspect of the peak. Mount Outram can be seen from the Icefields Parkway southwest of Saskatchewan Crossing, with optimum photography conditions in morning light. History.

Geographic entities mentioned:
surface_form: mount outram
instance_of: Mountain
countries: Canada
coordinates: lat: 51.88166666666667
lon: -116.87527777777778
surface_form: mount outram
instance_of: Mountain
countries: Canada
coordinates: lat: 49.289722222222224
lon: -121.15833333333333
and J. Biner. The mountain's name was officially adopted in 1924 by the Geographical Names Board of Canada. Geology. Like other mountains in Banff Park, Mount Outram is composed of sedimentary rock laid down from the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate.

Geographic entities mentioned:
surface_form: mount outram
instance_of: Mountain
countries: Canada
coordinates: lat: 51.88166666666667
lon: -116.87527777777778
surface_form: mount outram
instance_of: Mountain
countries: Canada
coordinates: lat: 49.289722222222224
lon: -121.15833333333333
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate. Based on the Köppen climate classification, Mount Outram is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below -20 °C with wind chill factors below -30 °C.

Geographic entities mentioned:
surface_form: mount outram
instance_of: Mountain
countries: Canada
coordinates: lat: 51.88166666666667
lon: -116.87527777777778
surface_form: mount outram
instance_of: Mountain
countries: Canada
coordinates: lat: 49.289722222222224
lon: -121.15833333333333
Climate. Based on the Köppen climate classification, Mount Outram is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below -20 °C with wind chill factors below -30 °C. In terms of favorable weather conditions, summer months are best for climbing. Precipitation runoff from Mount Outram drains into tributaries of the Howse River.

Geographic entities mentioned:
surface_form: mount outram
instance_of: Mountain
countries: Canada
coordinates: lat: 51.88166666666667
lon: -116.87527777777778
surface_form: mount outram
instance_of: Mountain
countries: Canada
coordinates: lat: 49.289722222222224
lon: -121.15833333333333
History. Mount Outram was named in 1920 for James Outram (1864-1925), a mountaineer who made numerous first ascents in the Canadian Rockies including Mount Assiniboine, Chancellor Peak, Cathedral Mountain, and Mount Wilson. The first ascent of the mountain was made in 1924 by F.V. Field, W.O. Field, and L. Harris, with guides Edward Feuz Jr. and J. Biner.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The first ascent of the mountain was made in 1924 by F.V. Field, W.O. Field, and L. Harris, with guides Edward Feuz Jr. and J. Biner. The mountain's name was officially adopted in 1924 by the Geographical Names Board of Canada. Geology. Like other mountains in Banff Park, Mount Outram is composed of sedimentary rock laid down from the Precambrian to Jurassic periods.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Steenburg Lake. Steenburg Lake is a lake in the Trent River and Lake Ontario drainage basins in the township of Limerick, Hastings County, Ontario, Canada, about west of Ontario Highway 62 and south of the town of Bancroft. Hydrology. The lake is about long and wide and lies at an elevation of.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
surface_form: steenburg lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.825833333333335
lon: -77.68111111111111
There are six inflows. Mud Creek from Paddy's Lake at the southwest is the only named one. The other five unnamed creek inflows are: two at the northwest, one at the north, one at the northeast and one at the east. The primary outflow is Bass Creek to Limerick Lake, which flows via Beaver Creek, the Crowe River and the Trent River to the Bay of Quinte on Lake Ontario at Trenton. Settlements.

Geographic entities mentioned:
surface_form: Limerick Lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.89277777777778
lon: -77.61722222222222
surface_form: beaver creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.64999
lon: -113.70189
Sunset Point from the east and The Headland from the west jut into the middle of the lake. There are six inflows. Mud Creek from Paddy's Lake at the southwest is the only named one. The other five unnamed creek inflows are: two at the northwest, one at the north, one at the northeast and one at the east.

Geographic entities mentioned:
surface_form: paddy's lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.8094
lon: -77.7014
Steenburg Lake. Steenburg Lake is a lake in the Trent River and Lake Ontario drainage basins in the township of Limerick, Hastings County, Ontario, Canada, about west of Ontario Highway 62 and south of the town of Bancroft. Hydrology. The lake is about long and wide and lies at an elevation of.

Geographic entities mentioned:
surface_form: steenburg lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.825833333333335
lon: -77.68111111111111
The other five unnamed creek inflows are: two at the northwest, one at the north, one at the northeast and one at the east. The primary outflow is Bass Creek to Limerick Lake, which flows via Beaver Creek, the Crowe River and the Trent River to the Bay of Quinte on Lake Ontario at Trenton. Settlements. Steenburg Lake is on the northwest bay.

Geographic entities mentioned:
surface_form: steenburg lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.825833333333335
lon: -77.68111111111111
Hydrology. The lake is about long and wide and lies at an elevation of. It has six named islands: Crab Island, Dewey's Island, Picket Island, Bateman's Island, Uncle Bob's Island and Powers Island; and two named bays: Adam's Bay and Austin's Bay. Sunset Point from the east and The Headland from the west jut into the middle of the lake. There are six inflows.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
There was formerly a railway station here. Barcaldine Castle is located a few kilometres to the west. The castle was built in the 15th century by Sir Douglas Campbell of Glenorchy (or Glen Orchy). There is also Barcaldine House Hotel. The town of Barcaldine in western Queensland, Australia is named (indirectly) after Barcaldine in Argyll.

Geographic entities mentioned:
surface_form: Glen Orchy
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.48
lon: -4.82
After the Relief of Kohima the British continued towards Imphal, still with 23 Brigade as flank guard on the Kharasom–Ukhrul axis, with the task of cutting Japanese communications back to the Chindwin River. On 22 April, 60 and 88 columns started out into the Naga Hills.

Geographic entities mentioned:
surface_form: Naga Hills
instance_of: Mountain
countries: Myanmar
India
coordinates: lat: 26
lon: 95
Death and burial. Amenhotep II was interred in his KV35 tomb in the Valley of the Kings; his mummy was found there within his original sarcophagus when the tomb was discovered in March 1898 by Victor Loret. The tomb also housed a mummy cache containing several New Kingdom pharaohs including Thutmose IV, Seti II, Ramesses III, Ramesses IV, and Ramesses VI.

Geographic entities mentioned:
surface_form: Valley of the Kings
instance_of: Valley
countries: Egypt
coordinates: lat: 25.74025
lon: 32.602358