Sarmila/GeoWiki-Features huggingface dataset:
Known as an important waterway since antiquity, the Shannon first appeared in maps by the Graeco-Egyptian geographer Ptolemy ( 100 –  170 AD). The river flows generally southwards from the Shannon Pot in County Cavan before turning west and emptying into the Atlantic Ocean through the long Shannon Estuary. Limerick city stands at the point where the river water meets the sea water of the estuary.

Geographic entities mentioned:
surface_form: Shannon Pot
instance_of: Lake
countries: Ireland
coordinates: lat: 54.23475
lon: -7.919
Course. By tradition the Shannon is said to rise in the Shannon Pot, a small pool in the townland of Derrylahan on the slopes of Cuilcagh Mountain in County Cavan, Republic of Ireland, from where the young river appears as a small trout stream. Surveys have defined a immediate pot catchment area covering the slopes of Cuilcagh.

Geographic entities mentioned:
surface_form: Shannon Pot
instance_of: Lake
countries: Ireland
coordinates: lat: 54.23475
lon: -7.919
surface_form: Cuilcagh Mountain
instance_of: Mountain
countries: United Kingdom
Ireland
coordinates: lat: 54.2
lon: -7.811
Further sinks that source the pot include Pollboy and, through Shannon Cave, Pollahune in Cavan and Polltullyard and Tullynakeeragh in County Fermanagh, Northern Ireland. The highest point in the catchment is a spring at Tiltinbane on the western end of the Cuilcagh mountain ridge. From the Shannon Pot, the river subsumes a number of tributaries before replenishing Lough Allen at its head.

Geographic entities mentioned:
surface_form: Lough Allen
instance_of: Lake
countries: Ireland
coordinates: lat: 54.106944444444
lon: -8.0391666666667
There are some tributaries within the Shannon River Basin which have headwaters that are further in length (from source to mouth) than the Shannon Pot source's length of, such as the Owenmore River, total length in County Cavan and the Boyle River, total length with its source in County Mayo. The River Shannon is a traditional freshwater river for about 45% of its total length.

Geographic entities mentioned:
surface_form: Shannon Pot
instance_of: Lake
countries: Ireland
coordinates: lat: 54.23475
lon: -7.919
Indeed, the Shannon is a major river by the time it leaves Lough Ree with an average flow rate (at Athlone weir) of, larger than any of the other Irish rivers' total flow (apart from the River Corrib at Galway). Distributaries. The main flow of the river is affected by some distributaries along its course, many of which rejoin it downstream.

Geographic entities mentioned:
surface_form: Lough Ree
instance_of: Lake
countries: Ireland
coordinates: lat: 53.5
lon: -7.9666666666667
The first serious attempt to improve navigability came in 1755 when the Commissioners of Inland Navigation ordered Thomas Omer, a new immigrant from England, possibly of Dutch origin, to commence work. He worked at four places between Lough Derg and Lough Ree where natural navigation was obstructed, by installing lateral canals and either pound locks or flash locks.

Geographic entities mentioned:
surface_form: Lough Ree
instance_of: Lake
countries: Ireland
coordinates: lat: 53.5
lon: -7.9666666666667
Improvements on the lower levels were also undertaken, being completed by 1814. When the Royal Canal was completed in 1817 there was pressure to improve the navigation above Lough Ree. The Jamestown Canal was repaired, harbours built and John Killaly designed a canal alongside the river from Battlebridge to Lough Allen, which was opened in 1820. 1820s to Independence.

Geographic entities mentioned:
surface_form: Lough Allen
instance_of: Lake
countries: Ireland
coordinates: lat: 54.106944444444
lon: -8.0391666666667
Canals. There are also many canals connecting with the River Shannon. The Royal Canal and the Grand Canal connect the Shannon to Dublin and the Irish Sea. It is linked to the River Erne and Lough Erne by the Shannon–Erne Waterway. Ballinasloe is linked to the Shannon via the River Suck and canal, while Boyle is connected via the Boyle canal, the river Boyle and Lough Key.

Geographic entities mentioned:
surface_form: Lough Erne
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.48262
lon: -7.80622
The Royal Canal and the Grand Canal connect the Shannon to Dublin and the Irish Sea. It is linked to the River Erne and Lough Erne by the Shannon–Erne Waterway. Ballinasloe is linked to the Shannon via the River Suck and canal, while Boyle is connected via the Boyle canal, the river Boyle and Lough Key. There is also the Ardnacrusha canal connected with the Ardnacrusha dam south of Lough Derg.

Geographic entities mentioned:
surface_form: Lough Key
instance_of: Lake
countries: Ireland
coordinates: lat: 54
lon: -8.25
Tseng Lan Shue. Tseng Lan Shue () is a village in Sai Kung District, New Territories, Hong Kong. Location. Tseng Lan Shue is located on Clear Water Bay Road, east of Kowloon Peak and southwest of Pik Uk. Administration. Tseng Lan Shue is a recognized village under the New Territories Small House Policy. History. At the time of the 1911 census, the population of Tseng Lan Shue was 276.

Geographic entities mentioned:
surface_form: Kowloon Peak
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.3414
lon: 114.223
Chandalar Lake. Chandalar Lake is a lake in Yukon-Koyukuk Census Area, Alaska, United States. The lake is approximately in length.

Geographic entities mentioned:
surface_form: chandalar lake
instance_of: Lake
countries: United States
coordinates: lat: 67.5075
lon: -148.5125
On May 2, 1862, General George Wright wrote to Colonel Ferris Foreman, the new commander of Camp Latham to send, two or three companies of the Second Cavalry with Lieutenant Colonel George S. Evans as commander to establish a post in the Owens Valley. He was Commander of the District of Southern California from May 15, 1862, to May 17, 1862, and from April 10, 1863, to July 7, 1863.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
Waterfall Way. Waterfall Way is a country road in the Northern Tablelands region of New South Wales, Australia, linking Raleigh on the state's North Coast to Armidale. The route passes through some of New South Wales' most scenic countryside and has become well known as its best and Australia's third most beautiful tourist drive.

Geographic entities mentioned:
surface_form: Northern Tablelands
instance_of: Plateau
countries: Australia
coordinates: lat: -30.595277777777778
lon: 151.5
Mushroom Lake (Swat). Mushroom Lake is a small alpine lake is located in the Gabral Valley of Kalam Swat. Mushroom Lake is called Mushroom because of its mushroom-shaped structure. It is Ten hours hike from Shahi Bagh Kalam. Mushroom lake located in upper shahi bagh valley of swat, this is high alpine lake around 13500 feet above sea level.

Geographic entities mentioned:
surface_form: Gabral Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.68
lon: 72.4
surface_form: Kalam
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.4801
lon: 72.5874
surface_form: mushroom lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.635983
lon: 72.296603
Mushroom Lake (Swat). Mushroom Lake is a small alpine lake is located in the Gabral Valley of Kalam Swat. Mushroom Lake is called Mushroom because of its mushroom-shaped structure. It is Ten hours hike from Shahi Bagh Kalam. Mushroom lake located in upper shahi bagh valley of swat, this is high alpine lake around 13500 feet above sea level.

Geographic entities mentioned:
surface_form: mushroom lake (swat)
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.635983
lon: 72.296603
Mushroom Lake (Swat). Mushroom Lake is a small alpine lake is located in the Gabral Valley of Kalam Swat. Mushroom Lake is called Mushroom because of its mushroom-shaped structure. It is Ten hours hike from Shahi Bagh Kalam. Mushroom lake located in upper shahi bagh valley of swat, this is high alpine lake around 13500 feet above sea level.

Geographic entities mentioned:
surface_form: mushroom lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.635983
lon: 72.296603
Mushroom Lake is called Mushroom because of its mushroom-shaped structure. It is Ten hours hike from Shahi Bagh Kalam. Mushroom lake located in upper shahi bagh valley of swat, this is high alpine lake around 13500 feet above sea level. The awe-inspiring lake is located about 31 kilometres away from Utror and 20 kilometres from Shahi Bagh.

Geographic entities mentioned:
surface_form: mushroom lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.635983
lon: 72.296603
Mushroom Lake (Swat). Mushroom Lake is a small alpine lake is located in the Gabral Valley of Kalam Swat. Mushroom Lake is called Mushroom because of its mushroom-shaped structure. It is Ten hours hike from Shahi Bagh Kalam. Mushroom lake located in upper shahi bagh valley of swat, this is high alpine lake around 13500 feet above sea level.

Geographic entities mentioned:
surface_form: kalam
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.4801
lon: 72.5874
Before construction of the Keban Dam the Karasu joined the Murat River 10 km above the dam site and 13 km above the town of Keban. History. It is thought likely that the river Harpasos mentioned by Xenophon in Anabasis 7.18 is the Kara Su, or the headwaters of the river Çoruh. In 1996, 15 Turkish soldiers were killed when their personnel carrier fell into the river during a routine crossing.

Geographic entities mentioned:
surface_form: Çoruh
instance_of: Watercourse
countries: Turkey
Georgia
coordinates: lat: 40.3074
lon: 40.9997
The easiest way to the top is the 6.7 mile Big Rock Trail, which opened in 2003 when George Lucas donated 800 acres of land to create the Lucas Valley Open Space Preserve. The views from Big Rock Ridge are sweeping, with views to Mt. St Helena and Mt. Diablo from the top. Geology.

Geographic entities mentioned:
surface_form: Mt. St Helena
instance_of: Mountain
countries: United States
coordinates: lat: 38.669333333333
lon: -122.63355
surface_form: Mt. Diablo
instance_of: Mountain
countries: United States
coordinates: lat: 37.881697781
lon: -121.914154997
Jagodnja. Jagodnja (Serbian Cyrillic: Јагодња) is a mountain in western Serbia, near the town of Krupanj. Its highest peak &quot;Košutnja stopa&quot; has an elevation of 939 meters above sea level. The peak of Mačkov kamen (923 m,) was the site of one of bloodiest battles in World War I between Serbian and Austro-Hungarian army, during the Battle of Drina.

Geographic entities mentioned:
surface_form: jagodnja
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.33
lon: 19.293
Jagodnja. Jagodnja (Serbian Cyrillic: Јагодња) is a mountain in western Serbia, near the town of Krupanj. Its highest peak &quot;Košutnja stopa&quot; has an elevation of 939 meters above sea level. The peak of Mačkov kamen (923 m,) was the site of one of bloodiest battles in World War I between Serbian and Austro-Hungarian army, during the Battle of Drina.

Geographic entities mentioned:
surface_form: jagodnja
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.33
lon: 19.293
surface_form: јагодња
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.33
lon: 19.293
The resort complex continued to expand rapidly. In 1932, the Inn was sold to J.J. Smith, who moved his clientele from the Pine
Ridge Resort complex at Hamlin Lake near Ludington, after that resort burned. Smith owned the Inn until his death in 1960. The Inn continued to operate for a number of years, and experienced ups and downs.

Geographic entities mentioned:
surface_form: Hamlin Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.063
lon: -86.466
He was primarily known for his Norwegian landscapes. Background. Ben Blessum was born in Marstein in Romsdalen, Norway. He was the son of shoemaker Johan Blessum and Marit Trøen from Vaage Municipality in Gudbrandsdal. His family emigrated from Trondheim in 1888 to Menominee, Wisconsin when he was 11 years old. He also lived in Eau Claire, Wisconsin, where his father worked in the lumber mills.

Geographic entities mentioned:
surface_form: Romsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 62.447222222222
lon: 7.8333333333333
History. In 1911, the Government of Ontario announced that a new asylum would be built to replace a similar facility in Toronto, and a site on Lake Ontario in Whitby was selected the following year. Whitby was chosen due its relative proximity to Toronto and for cheap power and water provided by local utilities.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
In 1894, Capt. Charles F. Kraft (b. 1831) bought &quot;Quickstep&quot; and brought the vessel to Lake Washington. In 1896, Capt. John L. Anderson bought &quot;Quickstep&quot; for $1,600 as a replacement for his steamer &quot;Winnifred&quot;, which had burned in early 1896. Loss by fire. On 3 January 1897 &quot;Quickstep&quot; in turn was lost by fire.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
In 1938, the fair was moved to its current location at the Cloverdale Fairgrounds. The rodeo was first held in 1945 and proved so popular that it was taken over by the Lower Fraser Valley Agricultural Association in 1947. In 1962, the fair was taken over by the Fraser Valley Exhibition Society, and in 1994, the fair and rodeo were renamed the Cloverdale Rodeo & Exhibition Association.

Geographic entities mentioned:
surface_form: Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
The Carlist advance continued with the inconclusive battle of Mañeru, where both sides claimed victory over the other. One month later, government general Moriones attempted an assault on Estella, defended by the Carlist general Joaquin Elio, but was repulsed with heavy casualties in the nearby town of Montejurra. Although the battle was inconclusive, both sides claimed victory once again.

Geographic entities mentioned:
surface_form: Montejurra
instance_of: Mountain
countries: Spain
coordinates: lat: 42.631111111111
lon: -2.0447222222222
The final battle of the war would be fought near Estella. Government forces, under General Fernando Primo de Rivera, advanced with the intention to capture Estella in February 1876 in a final offensive to put an end to the Carlist uprising. Carlist forces, this time under General Carlos Calderón, fortified themselves at Montejurra, a nearby mountain, and built a powerful stronghold.

Geographic entities mentioned:
surface_form: Montejurra
instance_of: Mountain
countries: Spain
coordinates: lat: 42.631111111111
lon: -2.0447222222222
The lower incisors are unicuspid, procumbent, sharp and delicate. Its dental formula is. Distribution. &quot;Paucidentomys vermidax&quot; is known from Mount Gandangdewata and Mount Latimojong in Sulawesi, Indonesia. Etymology. The generic name combines the Latin &quot;paucus&quot; (few) with &quot;dentis&quot; (tooth) and the Greek &quot;mys&quot; (mouse) in reference to the lack of molars.

Geographic entities mentioned:
surface_form: Mount Latimojong
instance_of: Mountain
countries: Indonesia
coordinates: lat: -3.385
lon: 120.02416666667
Geography. The Sierra de Cogollos extends between the Vega de Granada valley to the west and the Axarquía in the east. To the north the narrow Blanco River valley separates it from the Sierra Arana and to the south, another narrow valley, carved by the Bermejo River marks the limit with the lower Sierra de la Yedra range. The northeastern sector of the Sierra de Cogollos merges with Sierra Arana.

Geographic entities mentioned:
surface_form: Sierra Arana
instance_of: Mountain
countries: Spain
coordinates: lat: 37.3333
lon: -3.5
Geography. The Sierra de Cogollos extends between the Vega de Granada valley to the west and the Axarquía in the east. To the north the narrow Blanco River valley separates it from the Sierra Arana and to the south, another narrow valley, carved by the Bermejo River marks the limit with the lower Sierra de la Yedra range. The northeastern sector of the Sierra de Cogollos merges with Sierra Arana.

Geographic entities mentioned:
surface_form: Sierra Arana
instance_of: Mountain
countries: Spain
coordinates: lat: 37.3333
lon: -3.5
surface_form: sierra de cogollos
instance_of: Mountain
countries: Spain
coordinates: lat: 37.29166667
lon: -3.52777778
Protected areas. The Sierra de Cogollos, along with the neighboring ranges of Sierra de la Alfaguara, Sierra de Huétor, Sierra de Diezma, Sierra de Beas, as well as the southern part of the Sierra de Arana, is a protected area under the name Sierra de Huétor and la Alfaguara Natural Park &quot;(Parque Natural de la Sierra de Huétor y la Alfaguara)&quot;. Geology.

Geographic entities mentioned:
surface_form: Sierra de la Alfaguara
instance_of: Mountain
countries: Spain
coordinates: lat: 37.26583333
lon: -3.53027778
surface_form: sierra de cogollos
instance_of: Mountain
countries: Spain
coordinates: lat: 37.29166667
lon: -3.52777778
Sierra de Cogollos. The Sierra de Cogollos is a mountain range of the Baetic System in Granada Province, Andalusia, Spain. The range is located to the northeast of Granada city. Its highest point is the 1,889 m high Peñón del Majalijar peak. Geography. The Sierra de Cogollos extends between the Vega de Granada valley to the west and the Axarquía in the east.

Geographic entities mentioned:
surface_form: sierra de cogollos
instance_of: Mountain
countries: Spain
coordinates: lat: 37.29166667
lon: -3.52777778
Its highest point is the 1,889 m high Peñón del Majalijar peak. Geography. The Sierra de Cogollos extends between the Vega de Granada valley to the west and the Axarquía in the east. To the north the narrow Blanco River valley separates it from the Sierra Arana and to the south, another narrow valley, carved by the Bermejo River marks the limit with the lower Sierra de la Yedra range.

Geographic entities mentioned:
surface_form: sierra de cogollos
instance_of: Mountain
countries: Spain
coordinates: lat: 37.29166667
lon: -3.52777778
Peñón del Majalijar, the ranges's highest summit is located at the other end of the range. The Sierra de Cogollos is mostly included within the municipal term of Cogollos Vega, with a little part within Huétor Santillán at its eastern end. Protected areas.

Geographic entities mentioned:
surface_form: sierra de cogollos
instance_of: Mountain
countries: Spain
coordinates: lat: 37.29166667
lon: -3.52777778
Geology. Geologically the Sierra de Cogollos belongs to the Baetic System and is made up mainly of sedimentary rocks from the Triassic, Jurassic and Cretaceous.

Geographic entities mentioned:
surface_form: sierra de cogollos
instance_of: Mountain
countries: Spain
coordinates: lat: 37.29166667
lon: -3.52777778
Matsqui First Nation. The Matsqui First Nation () is the band government of the Matsqui people, a Aboriginal group located in the Central Fraser Valley region, at Matsqui, in the northern part of Abbotsford, British Columbia, Canada. They are a member government of the tribal council. Its governance structure is a custom electoral system. The current chief is Alice McKay.

Geographic entities mentioned:
surface_form: Central Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
Sugarloaf mountain. 20rvmkm5criiof2ttb9n1ndiw9a" xml:space="preserve">#REDIRECT List of mountains named Sugarloaf

Geographic entities mentioned:
surface_form: sugarloaf mountain
instance_of: Mountain
countries: Brazil
coordinates: lat: -22.949444444444445
lon: -43.156666666666666
A -long promenade leads from the marina in the city center, to the beach in Redłowo. Most of Gdynia can be seen from Kamienna Góra (asl) or the viewing point near Chwaszczyno. There are also two viewing towers, one at Góra Donas, the other at Kolibki. In 2015 the Emigration Museum opened in the city.

Geographic entities mentioned:
surface_form: Donas
instance_of: Mountain
countries: Poland
coordinates: lat: 54.469444444444
lon: 18.437222222222
Schruns railway station. Schruns railway station () serves the city of Schruns in the Montafon Valley, located in the Bludenz district of the Austrian federal state of Vorarlberg. Opened in 1905 and owned by the &quot;Montafonerbahn&quot; (MBS), it is the terminal station of the Bludenz–Schruns railway.

Geographic entities mentioned:
surface_form: Montafon Valley
instance_of: Valley
countries: Austria
coordinates: lat: 47.08
lon: 9.9
Takla Landing Water Aerodrome. Takla Landing Water Aerodrome is located on Takla Lake in the Takla Lake Marine Provincial Park, British Columbia, Canada.

Geographic entities mentioned:
surface_form: Takla Lake
instance_of: Lake
countries: Canada
coordinates: lat: 55.31
lon: -125.77
Knewstubb Lake is named for F.W. Knewstubb of the British Columbia government's Water Rights Branch, who led exploration parties for power development in various regions of the Coast Mountains in the 1920s. Mount Knewstubb to the south of Franklyn Arm of Chilko Lake is also named for F.W. Knewstubb.

Geographic entities mentioned:
surface_form: chilko lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.25
lon: -124.08333333333
Knewstubb Lake. Knewstubb Lake is an arm or stretch of the Ootsa Lake Reservoir in the Nechako Country of the western Central Interior of British Columbia, Canada. It forms part of the south arm of the reservoir, which includes adjoining stretches such as Eutsuk Lake and Natalkuz Lake, which are &quot;upstream&quot; to the southwest.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: knewstubb lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.5167
lon: -124.817
Knewstubb Lake is named for F.W. Knewstubb of the British Columbia government's Water Rights Branch, who led exploration parties for power development in various regions of the Coast Mountains in the 1920s. Mount Knewstubb to the south of Franklyn Arm of Chilko Lake is also named for F.W. Knewstubb.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Knewstubb Lake. Knewstubb Lake is an arm or stretch of the Ootsa Lake Reservoir in the Nechako Country of the western Central Interior of British Columbia, Canada. It forms part of the south arm of the reservoir, which includes adjoining stretches such as Eutsuk Lake and Natalkuz Lake, which are &quot;upstream&quot; to the southwest.

Geographic entities mentioned:
surface_form: knewstubb lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.5167
lon: -124.817
The exterior coloring is unchanged from the re-liveried E3 series, also designed by Ken Okuyama: white, evoking the snow of Mount Zaō; deep purple inspired by the Mandarin duck, the prefectural bird for Yamagata Prefecture; and yellow and red for the safflower, the prefectural flower of Yamagata Prefecture. All cars are equipped with full active suspension.

Geographic entities mentioned:
surface_form: Mount Zaō
instance_of: Mountain
countries: Japan
coordinates: lat: 38.141
lon: 140.443
Both the cabins and vestibules are equipped with security cameras. The green car has room for one wheelchair user, while each ordinary car has room for two. All seven cars are equipped to handle large baggage. The color scheme of the Green car seating is inspired by the blue waters of the Mogami River, combined with the lush greenery covering Mount Gassan.

Geographic entities mentioned:
surface_form: Mount Gassan
instance_of: Mountain
countries: Japan
coordinates: lat: 38.548888888889
lon: 140.02694444444
Geography. Tamtert lies at an elevation of on the left (northeast) bank of the Oued Saoura in the Saoura valley. The Grand Erg Occidental, a large area of continuous sand dunes lies to the east, while the rocky ridges of the Ougarta Range rise to the west, running from northwest to southeast along the opposite side of the river from the town beyond a barren, rocky plain. Climate.

Geographic entities mentioned:
surface_form: Saoura
instance_of: Valley
countries: Algeria
France
coordinates: lat: 29.45
lon: -1.4333333333333
The name comes from the word (nominative case). Two lakes in Norway had the name in Old Norse times (now called Øymark and Øyeren), and these names are derived from the word which means &quot;flat and fertile land along the edge of the water&quot;.

Geographic entities mentioned:
surface_form: Øyeren
instance_of: Lake
countries: Norway
coordinates: lat: 59.857222222222
lon: 11.163333333333
Merak, Ladakh. Merak is a village on the southern banks of Pangong Tso, near Spangmik on the south India-China border in the Leh District, Ladakh. Location. Merak is situated 176 kilometers east of Leh, on the southern banks of Pangong Tso. It is directly opposite to Finger 3 which is located on the northern bank of the lake. History.

Geographic entities mentioned:
surface_form: Pangong Tso
instance_of: Lake
countries: People's Republic of China
India
coordinates: lat: 33.70472222222222
lon: 78.75
Muisca language. Muisca or Muysca (* *), also known as Chibcha, Mosca and Muysca of Bogotá, was a language spoken by the Muisca people, one of the many indigenous cultures of the Americas, historically only in the Savanna of Bogotá. The Muisca inhabit the Altiplano Cundiboyacense of what today is the country of Colombia.

Geographic entities mentioned:
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877
state of Maine, which is part of the Appalachian Mountains; its altitude is. Geography. The mountain, located in the municipality of Frontenac, on the zec Louise-Gosford east of lac aux Araignées, is crossed by the Canada–United States border. Toponymy. The toponym &quot;Montagne Merrill&quot; was formalized on November 7, 1985, by the Commission de toponymie du Québec.

Geographic entities mentioned:
surface_form: lac aux Araignées
instance_of: Lake
countries: Canada
coordinates: lat: 45.4747
lon: -70.8128
state of Maine, which is part of the Appalachian Mountains; its altitude is. Geography. The mountain, located in the municipality of Frontenac, on the zec Louise-Gosford east of lac aux Araignées, is crossed by the Canada–United States border. Toponymy. The toponym &quot;Montagne Merrill&quot; was formalized on November 7, 1985, by the Commission de toponymie du Québec.

Geographic entities mentioned:
surface_form: montagne merrill
instance_of: Mountain
countries: Canada
United States
coordinates: lat: 45.47417
lon: -70.69222
Merrill Mountain. Merrill Mountain () is a mountain on the border between the Canadian province of Quebec, in the region of Estrie, and the U.S. state of Maine, which is part of the Appalachian Mountains; its altitude is. Geography. The mountain, located in the municipality of Frontenac, on the zec Louise-Gosford east of lac aux Araignées, is crossed by the Canada–United States border. Toponymy.

Geographic entities mentioned:
surface_form: merrill mountain
instance_of: Mountain
countries: Canada
United States
coordinates: lat: 45.47417
lon: -70.69222
There are 13 small uninhabited islands in the lake. Some of its banks, underwater at high tide, have been made into nature reserves, while others are popular for water sports, such as sailing. The Veerse Meer was created as a flood control measure to end storm surges through the Veerse Gat.

Geographic entities mentioned:
surface_form: Veerse Gat
instance_of: Lake
countries: Netherlands
coordinates: lat: 51.547
lon: 3.675
surface_form: veerse meer
instance_of: Lake
countries: Netherlands
coordinates: lat: 51.533333333333
lon: 3.7166666666667
Veerse Meer. The Veerse Meer (Lake Veere) is a lagoon in the southwest Netherlands in the province of Zeeland. Description. It is 22 km long, and 1,500 m wide in places. Lying between the old islands of Noord-Beveland, Zuid-Beveland and Walcheren, it is linked to the river Scheldt by the Zandkreekdam sluice, which allows this lagoon to have brackish water, slightly less salty than sea water.

Geographic entities mentioned:
surface_form: veerse meer
instance_of: Lake
countries: Netherlands
coordinates: lat: 51.533333333333
lon: 3.7166666666667
History. Originally an outlet of the Scheldt called the Veerse Gat to the west which met with the Zandkreek to the east, it was first closed off from the Scheldt by the Zandkreekdam in 1960, and from the North Sea in 1961 by Veerse Gatdam, some of the first constructions of the Delta Works water management system. Water quality issues.

Geographic entities mentioned:
surface_form: veerse gat
instance_of: Lake
countries: Netherlands
coordinates: lat: 51.547
lon: 3.675
Having helped to pay for his studies by giving private lessons, he set up a college, which was to merge with the Institut Minerva, to tutor students for entry to the ETH. In 1925, Husmann bought the old Hotel Schönfels on the Zugerberg overlooking Lake Zug as a site where he could found a school.

Geographic entities mentioned:
surface_form: Zugerberg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.139166666667
lon: 8.5383333333333
The peak is named after the city of Kazanlak in central Bulgaria. Location. The peak is located at which is on the northern side ridge descending from Delchev Peak towards Rila Point, 1.06 km northwest of Peter Peak, and 650 m south-southeast of Ghiaurov Peak (Bulgarian topographic survey 05 and mapping in 2009).

Geographic entities mentioned:
surface_form: Peter Peak
instance_of: Mountain
coordinates: lat: -62.637861111111
lon: -59.938888888889
surface_form: Ghiaurov Peak
instance_of: Mountain
coordinates: lat: -62.62777778
lon: -59.96361111
surface_form: peter
instance_of: Mountain
coordinates: lat: -70.1833
lon: 64.9333
Kazanlak Peak. Kazanlak Peak (,) is a rocky peak rising to 430 m in Delchev Ridge of Tangra Mountains, Livingston Island in the South Shetland Islands, Antarctica. Surmounting Bruix Cove to the northwest, Iskar Glacier to the southwest and Sopot Ice Piedmont to the east. The peak is named after the city of Kazanlak in central Bulgaria. Location.

Geographic entities mentioned:
surface_form: kazanlak peak
instance_of: Mountain
coordinates: lat: -62.632333333333
lon: -59.955833333333
Whaleback Mountain is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 625 meters (2,050 ft) above Little Yoho River in. The peak is visible from Highway 1 (the Trans-Canada Highway). The nearest higher neighbor is Isolated Peak, to the northwest. History.

Geographic entities mentioned:
surface_form: Isolated Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.54361111111111
lon: -116.57638888888889
Whaleback Mountain. Whaleback Mountain is a summit in British Columbia, Canada. Description. Whaleback Mountain is located in Yoho National Park, in the Waputik Mountains of the Canadian Rockies. Precipitation runoff from Whaleback drains into tributaries of the Yoho River which in turn is a tributary of the Kicking Horse River.

Geographic entities mentioned:
surface_form: whaleback mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.53944444444444
lon: -116.56055555555555
Whaleback Mountain. Whaleback Mountain is a summit in British Columbia, Canada. Description. Whaleback Mountain is located in Yoho National Park, in the Waputik Mountains of the Canadian Rockies. Precipitation runoff from Whaleback drains into tributaries of the Yoho River which in turn is a tributary of the Kicking Horse River.

Geographic entities mentioned:
surface_form: whaleback mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.53944444444444
lon: -116.56055555555555
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Precipitation runoff from Whaleback drains into tributaries of the Yoho River which in turn is a tributary of the Kicking Horse River. Whaleback Mountain is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 625 meters (2,050 ft) above Little Yoho River in.

Geographic entities mentioned:
surface_form: whaleback mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.53944444444444
lon: -116.56055555555555
The mountain's toponym was officially adopted on March 31, 1924, by the Geographical Names Board of Canada. Geology. Whaleback Mountain is composed of sedimentary rock laid down during 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: whaleback mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.53944444444444
lon: -116.56055555555555
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, Whaleback Mountain 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: whaleback mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.53944444444444
lon: -116.56055555555555
History. The mountain was named in 1901 by mountaineer Edward Whymper because the mountain's profile resembles the back of a whale. The mountain's descriptive name was then applied in 1916 by members of the Alberta-British Columbia Boundary Survey. The mountain's toponym was officially adopted on March 31, 1924, by the Geographical Names Board of Canada. Geology.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
He was, a contemporary historian wrote, &quot;the single most powerful person in the area for the first two decades of the century.&quot; His decision to sell the land in small parcels rather than large blocks, despite the objections of the company's trustees who wanted the land sold quickly, resulted in settlement by small farmers rather than the establishment of quasi-feudal manors as had occurred in the Hudson Valley.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Administratively, it encompasses the metropolitan city of Turin and, more marginally, the province of Biella and the province of Vercelli. It dates back to the Quaternary period and was created by the transport of sediment to the Po Valley that took place during the glaciations by the great glacier that ran through the Dora Baltea valley.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
With an area of more than 500 km2, it is one of the best-preserved geomorphological units of this type in the world. As an extension, it is surpassed in Italy only by the similar formation surrounding Lake Garda. The name amphitheater, usually given to these geomorphological structures, refers to their characteristic elliptical shape that is noticeable when it is shown as a plan on a map.

Geographic entities mentioned:
surface_form: Lake Garda
instance_of: Lake
countries: Italy
coordinates: lat: 45.633333333333
lon: 10.666666666667
Of particular note among these is the left lateral moraine of the ancient glacier, known as the Serra di Ivrea: this is the largest formation of its kind existing in Europe. The Serra originates on the southern slopes of Mombarone (2371 m a.s.l.) and heads in an almost straight path southeastward for almost 20 km, then fraying into the heights surrounding Lake Viverone.

Geographic entities mentioned:
surface_form: Mombarone
instance_of: Mountain
countries: Italy
coordinates: lat: 45.586008
lon: 7.8930066
surface_form: Lake Viverone
instance_of: Lake
countries: Italy
coordinates: lat: 45.416666666667
lon: 8.0333333333333
The catchment area of Lake Viverone is also defined not only by the outer moraine circle of the AMI, but also by smaller internal deposits; the municipalities in this area have grouped into the hill community around the lake.

Geographic entities mentioned:
surface_form: Lake Viverone
instance_of: Lake
countries: Italy
coordinates: lat: 45.416666666667
lon: 8.0333333333333
Nestled among the various moraine cordons that make up the amphitheater are numerous lakes whose formation is closely related to the geological history of the AMI. While Lake Viverone is quite large (in terms of surface area it is the third largest body of water in Piedmont) the others are small to medium in size.

Geographic entities mentioned:
surface_form: Lake Viverone
instance_of: Lake
countries: Italy
coordinates: lat: 45.416666666667
lon: 8.0333333333333
Just north of Ivrea are located the 5 lakes, the largest of which is Sirio; the right side moraine, on the other hand, hosts Alice Lake and Meugliano Lake, while between the hills that make up the frontal moraine are Candia Lake and the smaller ones of Maglione and Moncrivello.

Geographic entities mentioned:
surface_form: Sirio
instance_of: Lake
countries: Italy
coordinates: lat: 45.487
lon: 7.884
surface_form: Candia Lake
instance_of: Lake
countries: Italy
coordinates: lat: 45.333333333333
lon: 7.8833333333333
In the AMI zone north of the Outer Canavese Line is the Sesia-Lanzo Zone, composed mainly of mica schists and, in general, rocks that underwent metamorphic processes at depth; it includes Mombarone on the hydrographic left and Mount Gregorio on the opposite side of the Dora River.

Geographic entities mentioned:
surface_form: Mombarone
instance_of: Mountain
countries: Italy
coordinates: lat: 45.586008
lon: 7.8930066
Glacial phases. According to geologists, in the final phase of the Pliocene, the geological period that preceded the formation of the morainic amphitheater, in the Canavese area the sea that occupied the Po River basin at that time and reached into the interior of the Aosta and Orco valleys was gradually filled in by sediments originating from the erosion of the Alpine range.

Geographic entities mentioned:
surface_form: Orco
instance_of: Valley
countries: Italy
coordinates: lat: 45.417
lon: 7.467
During this period the best preserved of the three moraine circles, the Serra d'Ivrea group, was deposited. In addition to the main body of the Serra this includes a large part of the frontal moraine observable today (the area roughly between Moncrivello and Torre Canavese) and part of the reliefs located at the outlet of the Valchiusella.

Geographic entities mentioned:
surface_form: Valchiusella
instance_of: Valley
countries: Italy
coordinates: lat: 45.517
lon: 7.75
Paleogeographical research (in particular by geologists Francesco Carraro and Franco Gianotti) shows, for example, that in ancient times the Cervo stream, after leaving the alpine valley of the same name, headed decisively southward and flowed into the Dora Baltea roughly where Verrone stands today.

Geographic entities mentioned:
surface_form: alpine valley of the same name
instance_of: Valley
countries: Italy
coordinates: lat: 45.61
lon: 8.058
Trapped between the moraine ridges, however, several smaller bodies of water remained for a long time, some of which still exist today. Among these the largest are Lake Viverone and Lake Candia. Other lake basins of various sizes were gradually filled in by the only partially decomposed remnants of riparian vegetation and formed the numerous peat bogs still visible in the area.

Geographic entities mentioned:
surface_form: Lake Viverone
instance_of: Lake
countries: Italy
coordinates: lat: 45.416666666667
lon: 8.0333333333333
surface_form: Lake Candia
instance_of: Lake
countries: Italy
coordinates: lat: 45.333333333333
lon: 7.8833333333333
The AMI area also had considerable commercial importance in the imperial period, being located along Gaul, which, via Augusta Praetoria (Aosta) and the passes of the Little and Great St. Bernard, connected the Po Valley with Gaul. Middle Ages and Renaissance.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
In particular, the Piedmont Region established the Lake Candia Natural Park of Provincial Interest in 1995. Also in the Province of Turin and in the AMI area are the following Sites of Community Importance: Pelati Mountains and Torre Cives (cod.IT1110013), Lake Viverone (cod.IT1110020), Ivrea Lakes (cod.IT1110021), Meugliano and Alice Lakes (cod.

Geographic entities mentioned:
surface_form: Lake Viverone
instance_of: Lake
countries: Italy
coordinates: lat: 45.416666666667
lon: 8.0333333333333
Tourism and sport. The area of the morainic amphitheater includes within it some popular tourist destinations such as Lake Viverone and Lake Sirio, around which a decent network of accommodation facilities such as campsites, hotels and restaurants of various kinds has long been developed.

Geographic entities mentioned:
surface_form: Lake Viverone
instance_of: Lake
countries: Italy
coordinates: lat: 45.416666666667
lon: 8.0333333333333
surface_form: Lake Sirio
instance_of: Lake
countries: Italy
coordinates: lat: 45.487
lon: 7.884
The waters of the two lakes are suitable for bathing and, in the case of Lake Viverone, a public boat line connects the main towns along the coast.

Geographic entities mentioned:
surface_form: Lake Viverone
instance_of: Lake
countries: Italy
coordinates: lat: 45.416666666667
lon: 8.0333333333333
Precipitation runoff from the mountain drains north to the Middle Fork Flathead River, and topographic relief is significant as the summit rises over above Schafer Creek in less than two miles. Union Mountain is set two miles to the east-northeast, and the nearest higher neighbor is Argosy Mountain, to the southeast.

Geographic entities mentioned:
surface_form: Union Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.055833333333
lon: -113.27805555556
surface_form: Argosy Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.003888888889
lon: -113.23944444444
state of Montana. Description. Capitol Mountain is located in the Flathead Range, a subset of the Rocky Mountains. It is situated in the Great Bear Wilderness, on land managed by Flathead National Forest. Precipitation runoff from the mountain drains north to the Middle Fork Flathead River, and topographic relief is significant as the summit rises over above Schafer Creek in less than two miles.

Geographic entities mentioned:
surface_form: the flathead
instance_of: Valley
countries: United States
coordinates: lat: 48
lon: -114
surface_form: capitol mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.046388888889
lon: -113.31583333333
Capitol Mountain. Capitol Mountain is a summit located in Flathead County of the U.S. state of Montana. Description. Capitol Mountain is located in the Flathead Range, a subset of the Rocky Mountains. It is situated in the Great Bear Wilderness, on land managed by Flathead National Forest.

Geographic entities mentioned:
surface_form: capitol mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.046388888889
lon: -113.31583333333
Climate. Based on the Köppen climate classification, Capitol Mountain is located in a subarctic climate zone characterized by long, usually very cold winters, and short, cool to mild summers. Winter temperatures can drop below −10 °F with wind chill factors below −30 °F. Geology. Capitol Mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods.

Geographic entities mentioned:
surface_form: capitol mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.046388888889
lon: -113.31583333333
Geology. Capitol Mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks thick, wide and long over younger rock of the cretaceous period.

Geographic entities mentioned:
surface_form: capitol mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.046388888889
lon: -113.31583333333
The summit of Landsend Peak has an elevation of rising dramatically about above the valley below. Together with nearby Mount Lamborn to the northeast (the highest point in Delta County), it delineates the western edge of the West Elk Mountains (and West Elk Wilderness), and the two massifs top out about higher than the adjacent North Fork Gunnison River.

Geographic entities mentioned:
surface_form: Mount Lamborn
instance_of: Mountain
countries: United States
coordinates: lat: 38.803055555556
lon: -107.52277777778
Together with nearby Mount Lamborn to the northeast (the highest point in Delta County), it delineates the western edge of the West Elk Mountains (and West Elk Wilderness), and the two massifs top out about higher than the adjacent North Fork Gunnison River. Both peaks lie within the Gunnison National Forest near the physiographic boundary of the Rocky Mountains and the Colorado Plateau provinces.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
Landsend Peak. Landsend Peak is a prominent wedge-shaped mountain located in the West Elk Mountains range northeast of Crawford, Colorado. The summit of Landsend Peak has an elevation of rising dramatically about above the valley below.

Geographic entities mentioned:
surface_form: landsend peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.770833333333
lon: -107.55166666667
Landsend Peak. Landsend Peak is a prominent wedge-shaped mountain located in the West Elk Mountains range northeast of Crawford, Colorado. The summit of Landsend Peak has an elevation of rising dramatically about above the valley below.

Geographic entities mentioned:
surface_form: landsend peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.770833333333
lon: -107.55166666667
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Both peaks lie within the Gunnison National Forest near the physiographic boundary of the Rocky Mountains and the Colorado Plateau provinces. Geologically, Landsend Peak and Mount Lamborn are exposed igneous intrusions that geologists call laccoliths.

Geographic entities mentioned:
surface_form: landsend peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.770833333333
lon: -107.55166666667
surface_form: mount lamborn
instance_of: Mountain
countries: United States
coordinates: lat: 38.803055555556
lon: -107.52277777778
Italy was the first country in the world to build controlled-access highways reserved for fast traffic and for motor vehicles only. The &quot;Autostrada dei Laghi&quot; (&quot;Lakes Motorway&quot;) connected Milan to Lake Como and Lake Maggiore, and is now parts of the A8 and A9 motorways. It was devised by Piero Puricelli and was inaugurated in 1924.

Geographic entities mentioned:
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
In Hungary, similar to Ireland, motorway numbers can be derived from the original national highway numbers (1–7), with an M prefix attached, e.g. M7 is on the route of the old Highway 7 from Budapest towards Lake Balaton and Croatia. New motorways not following the original Budapest-centred radial highway system get numbers M8, M9, etc., or M0 in the case of the ring road around Budapest.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72