Sarmila/GeoWiki-Features huggingface dataset:
Precipitation runoff from the mountain drains into tributaries of the nearby Crowsnest River. Topographic relief is significant as the summit rises 1,300 meters (4,265 feet) above the river in 4.5 kilometers (2.8 miles). Sentry Mountain is to the northwest and the nearest higher neighbor is Andy Good Peak, to the southeast on the Continental Divide. History.

Geographic entities mentioned:
surface_form: Sentry Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.5984
lon: -114.6328
surface_form: Andy Good Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.56527777777778
lon: -114.58805555555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Chinook Peak (Alberta). Chinook Peak is a mountain summit located in the Canadian Rockies of Alberta, Canada. Description. Chinook Peak is situated 10 kilometers southwest of the town of Coleman in the Crowsnest Pass area and can be seen from Highway 3, the Crowsnest Highway. It is set on land managed by Castle Wildland Provincial Park.

Geographic entities mentioned:
surface_form: chinook peak (alberta)
instance_of: Mountain
countries: Canada
coordinates: lat: 49.58555555555556
lon: -114.61
Chinook Peak (Alberta). Chinook Peak is a mountain summit located in the Canadian Rockies of Alberta, Canada. Description. Chinook Peak is situated 10 kilometers southwest of the town of Coleman in the Crowsnest Pass area and can be seen from Highway 3, the Crowsnest Highway. It is set on land managed by Castle Wildland Provincial Park.

Geographic entities mentioned:
surface_form: chinook peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.58555555555556
lon: -114.61
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Chinook Peak (Alberta). Chinook Peak is a mountain summit located in the Canadian Rockies of Alberta, Canada. Description. Chinook Peak is situated 10 kilometers southwest of the town of Coleman in the Crowsnest Pass area and can be seen from Highway 3, the Crowsnest Highway. It is set on land managed by Castle Wildland Provincial Park.

Geographic entities mentioned:
surface_form: chinook peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.58555555555556
lon: -114.61
Sentry Mountain is to the northwest and the nearest higher neighbor is Andy Good Peak, to the southeast on the Continental Divide. History. Chinook Peak was named by Jim Kerr, a resident of the Crowsnest Pass. Jim knew that when snow started blowing from the top from the west, a chinook wind would soon follow. When mapping this area, Dr. Raymond A.

Geographic entities mentioned:
surface_form: chinook peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.58555555555556
lon: -114.61
The mountain's toponym was officially adopted in 1962 by the Geographical Names Board of Canada. Geology. Chinook Peak 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 Cretaceous period rock during the Laramide orogeny. Climate.

Geographic entities mentioned:
surface_form: chinook peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.58555555555556
lon: -114.61
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger Cretaceous period rock during the Laramide orogeny. Climate. Based on the Köppen climate classification, Chinook Peak has an alpine subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: chinook peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.58555555555556
lon: -114.61
It is set on land managed by Castle Wildland Provincial Park. Precipitation runoff from the mountain drains into tributaries of the nearby Crowsnest River. Topographic relief is significant as the summit rises 1,300 meters (4,265 feet) above the river in 4.5 kilometers (2.8 miles).

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
When mapping this area, Dr. Raymond A. Price of the Geological Survey of Canada mapping this area, used this name to identify the peak. The mountain's toponym was officially adopted in 1962 by the Geographical Names Board of Canada. Geology. Chinook Peak is composed of sedimentary rock laid down during the Precambrian to Jurassic periods.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Tin discoveries in 1880 on the banks of the Wild River led to the development of Herberton and from here fossickers fanned out reporting new finds every year. Discoveries were made at locations nearby throughout the 1880s, then Charles Ross discovered tin in 1885 at Mount Amos, south of Cooktown, and then at Mounts Hartley, Leswell and Romeo on the upper Annan River.

Geographic entities mentioned:
surface_form: Romeo
instance_of: Mountain
countries: Canada
coordinates: lat: 50.2594
lon: -126.208
In 1854, he became a partner of Ephrem Hudon in a grocery business. He was elected to the Legislative Assembly of the Province of Canada for Terrebonne in 1861 and 1863, supporting the parti rouge. He voted against Confederation. He retired from politics in 1867. He was involved in the development of iron mines in the Moisie River area. He died in Montreal in 1872.

Geographic entities mentioned:
surface_form: Moisie River
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.2
lon: -66.0675
Tintina Trench. The Tintina Trench is a roughly valley extending from southwestern Yukon, Canada to the Yukon Flats in the central portion of the U.S. state of Alaska. It is a prominent topographic lineament along the northern extension of the Northern Rocky Mountain Trench in British Columbia and it has its origin from the Tintina Fault. It was named by R.G.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Tintina Trench. The Tintina Trench is a roughly valley extending from southwestern Yukon, Canada to the Yukon Flats in the central portion of the U.S. state of Alaska. It is a prominent topographic lineament along the northern extension of the Northern Rocky Mountain Trench in British Columbia and it has its origin from the Tintina Fault. It was named by R.G.

Geographic entities mentioned:
surface_form: tintina trench
instance_of: Valley
countries: Canada
coordinates: lat: 63.41627
lon: -137.00409
It was named by R.G. McConnell of the Geological Survey of Canada in 1904 after an indigenous word for “chief.”
The Tintina Trench crosses the Continental Divide between the Pacific Ocean and the Arctic Ocean near Finlayson Lake, between Ross River and Watson Lake. The northwestern part of the valley is occupied by the Yukon River before it flows northwestward into Alaska.

Geographic entities mentioned:
surface_form: tintina trench
instance_of: Valley
countries: Canada
coordinates: lat: 63.41627
lon: -137.00409
The central part of the valley is occupied by the Pelly River before its confluence with the Yukon River at Fort Selkirk. The southern Tintina Trench is drained by the Liard River which first flows south-eastward, then eastward and finally merges into the Mackenzie River at Fort Simpson, NWT where the combined waters turn back north for the Mackenzie's long flow to the Arctic Ocean. Geology.

Geographic entities mentioned:
surface_form: tintina trench
instance_of: Valley
countries: Canada
coordinates: lat: 63.41627
lon: -137.00409
Geology. The location of the Tintina Trench corresponds with recessive weathering rocks which have been deformed by 450 km of right lateral faulting along the Tintina Fault.

Geographic entities mentioned:
surface_form: tintina trench
instance_of: Valley
countries: Canada
coordinates: lat: 63.41627
lon: -137.00409
Technically Gipmochi is part of the Zompelri ridge, which is a curved semicircular formation on the southern side of the plateau. The Dongkya Range, on the northern side, forms the dividing line between Sikkim (part of India) and the Chumbi Valley (part of Tibet), with numerous passes such as Cho La, Nathu La and Jelep La. The Doklam plateau is to the east of all these passes.

Geographic entities mentioned:
surface_form: Chumbi Valley
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 27.4893046
lon: 88.9050579
&quot;The Imperial Gazetteer of India&quot; states that the Dongkya range (or Chola range) that divides Sikkim from the Chumbi Valley bifurcates at Gipmochi into two great spurs, one running to the south-east and the other to the south-west. Between the two spurs lies the valley of the Dichul (Jaldhaka) river.

Geographic entities mentioned:
surface_form: Chumbi Valley
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 27.4893046
lon: 88.9050579
surface_form: gipmochi
instance_of: Mountain
countries: India
Bhutan
coordinates: lat: 27.2739637
lon: 88.9000613
Gipmochi. Gipmochi (Gyemo Chen or Gamochen, 'The Great Queen') is a mountain in the Lower Himalayas in south central Asia. Rising to a height of, the mountain sits on the border between the northern Indian state of Sikkim and Bhutan. China claims Gipmochi as the China–India–Bhutan tri-junction point. Bhutan and India, however, claim that the tri-junction is 6.5 km to the north, at Batang La.

Geographic entities mentioned:
surface_form: gipmochi
instance_of: Mountain
countries: India
Bhutan
coordinates: lat: 27.2739637
lon: 88.9000613
Gipmochi (Gyemo Chen or Gamochen, 'The Great Queen') is a mountain in the Lower Himalayas in south central Asia. Rising to a height of, the mountain sits on the border between the northern Indian state of Sikkim and Bhutan. China claims Gipmochi as the China–India–Bhutan tri-junction point. Bhutan and India, however, claim that the tri-junction is 6.5 km to the north, at Batang La. Geography.

Geographic entities mentioned:
surface_form: gipmochi
instance_of: Mountain
countries: India
Bhutan
coordinates: lat: 27.2739637
lon: 88.9000613
Geography. Mount Gipmochi is a Himalayan peak rising to,
on the southwestern shoulder of the Doklam plateau. The plateau is at the intersection between India, Bhutan and Tibet, and is formed by the joining of two ridges, Dongkya Range in the north and Zompelri ridge (or Jampheri ridge) in the south, via a Doka La pass in the middle.

Geographic entities mentioned:
surface_form: gipmochi
instance_of: Mountain
countries: India
Bhutan
coordinates: lat: 27.2739637
lon: 88.9000613
The plateau is at the intersection between India, Bhutan and Tibet, and is formed by the joining of two ridges, Dongkya Range in the north and Zompelri ridge (or Jampheri ridge) in the south, via a Doka La pass in the middle. Technically Gipmochi is part of the Zompelri ridge, which is a curved semicircular formation on the southern side of the plateau.

Geographic entities mentioned:
surface_form: gipmochi
instance_of: Mountain
countries: India
Bhutan
coordinates: lat: 27.2739637
lon: 88.9000613
In the modern view, the Dongkya Range is seen to continue beyond Sikkim to the east, passing through the Batang La, Merug La and Sinche La peaks and gradually descending down to the plains. To the west of the Mount Gipmochi and the Doklam plateau lie the headwaters of the Dichu river (also called the Jaldhaka river).

Geographic entities mentioned:
surface_form: gipmochi
instance_of: Mountain
countries: India
Bhutan
coordinates: lat: 27.2739637
lon: 88.9000613
A lake called Bitang Tso (or Bidan Tso, also called the Kupup Lake), just to the east of Kupup, is traditionally regarded as the origin of the Dichu river. Dichu flows southeast towards the Mount Gipmochi and turns south, entering the Bhutanese territory. A tributary of Dichu called Asam Khola rises below Mount Gipmochi on its southern shoulder, and joins Dichu near the village of Khentong.

Geographic entities mentioned:
surface_form: gipmochi
instance_of: Mountain
countries: India
Bhutan
coordinates: lat: 27.2739637
lon: 88.9000613
Dichu flows southeast towards the Mount Gipmochi and turns south, entering the Bhutanese territory. A tributary of Dichu called Asam Khola rises below Mount Gipmochi on its southern shoulder, and joins Dichu near the village of Khentong. To the northeast of Gipmochi lies the basin of the Amo Chu river, which rises in the Chumbi Valley and flows into Bhutanese territory near Sinche La.

Geographic entities mentioned:
surface_form: gipmochi
instance_of: Mountain
countries: India
Bhutan
coordinates: lat: 27.2739637
lon: 88.9000613
It joins the Amo Chu river about 8 miles downstream. Initial survey. Mount Gipmochi received a prominent position in British geography of the region because it is one of the peaks visible from Darjeeling, which the British leased from the Chogyal of Sikkim in 1835 in return for an annual subsidy. They had free access to the tract around Darjeeling, but not to Sikkim proper.

Geographic entities mentioned:
surface_form: gipmochi
instance_of: Mountain
countries: India
Bhutan
coordinates: lat: 27.2739637
lon: 88.9000613
Despite the great distance from which the peaks were measured, the positions were said to be correct to within quarter of a second in latitude and half a second in longitude. Misplacement of Gipmochi. Mount Gipmochi started appearing British maps around 1850 in the process of illustrating the travels of the noted British botanist Joseph Dalton Hooker.

Geographic entities mentioned:
surface_form: gipmochi
instance_of: Mountain
countries: India
Bhutan
coordinates: lat: 27.2739637
lon: 88.9000613
Misplacement of Gipmochi. Mount Gipmochi started appearing British maps around 1850 in the process of illustrating the travels of the noted British botanist Joseph Dalton Hooker. Hooker toured the then independent state of Sikkim to explore and collect samples of Himalayan plants.

Geographic entities mentioned:
surface_form: gipmochi
instance_of: Mountain
countries: India
Bhutan
coordinates: lat: 27.2739637
lon: 88.9000613
The Sikkimese authorities prohibited them from entering Tibetan territory, and arrested them near the pass. Evidently, Mount Gipmochi was visible from their route, and Hooker remarked that the Dongkya Range gradually sinks into Bhutan near Gipmochi. Hooker placed Gipmochi directly on the Dongkya range, and attributed its position to Waugh.

Geographic entities mentioned:
surface_form: gipmochi
instance_of: Mountain
countries: India
Bhutan
coordinates: lat: 27.2739637
lon: 88.9000613
surface_form: gipmochi
instance_of: Mountain
countries: India
Bhutan
coordinates: lat: 27.2739637
lon: 88.9000613
Evidently, Mount Gipmochi was visible from their route, and Hooker remarked that the Dongkya Range gradually sinks into Bhutan near Gipmochi. Hooker placed Gipmochi directly on the Dongkya range, and attributed its position to Waugh. For several decades after this, the Mount Gipmochi continued to be shown on the Dongkya range despite other evidence to the contrary.

Geographic entities mentioned:
surface_form: gipmochi
instance_of: Mountain
countries: India
Bhutan
coordinates: lat: 27.2739637
lon: 88.9000613
Hooker placed Gipmochi directly on the Dongkya range, and attributed its position to Waugh. For several decades after this, the Mount Gipmochi continued to be shown on the Dongkya range despite other evidence to the contrary. After the Hooker episode, the British signed the Treaty of Tumlong (1861) with Sikkim, bringing the state under their protectorate.

Geographic entities mentioned:
surface_form: gipmochi
instance_of: Mountain
countries: India
Bhutan
coordinates: lat: 27.2739637
lon: 88.9000613
Temple explored the lake region of Sikkim and presented his findings at the Royal Geographical Society in 1881. One of his sketches showed Bitang Tso (or Kupup Lake) viewed from Kupup in Sikkim, with Mount Gipmochi in the background.

Geographic entities mentioned:
surface_form: gipmochi
instance_of: Mountain
countries: India
Bhutan
coordinates: lat: 27.2739637
lon: 88.9000613
One of his sketches showed Bitang Tso (or Kupup Lake) viewed from Kupup in Sikkim, with Mount Gipmochi in the background. His cartographer however continued to show Mount Gipmochi on the Dongkya range, in the tradition of Joseph Hooker, and placed the Bitang Tso to its south in Bhutanese territory.

Geographic entities mentioned:
surface_form: gipmochi
instance_of: Mountain
countries: India
Bhutan
coordinates: lat: 27.2739637
lon: 88.9000613
(Map 3)
Temple himself invoked the authority of Hooker, stating, &quot;In Sir Joseph Hooker's 'Himalayan Journals' the name Gipmochi is always applied to the mountain which terminates the Chola range [Dongkya range].&quot;
20th century.

Geographic entities mentioned:
surface_form: gipmochi
instance_of: Mountain
countries: India
Bhutan
coordinates: lat: 27.2739637
lon: 88.9000613
Between the two spurs lies the valley of the Dichul (Jaldhaka) river. The &quot;western shoulder&quot; of Gipmochi was said to contain the trijunction point of Sikkim, Bhutan and Tibet. The southwest spur mentioned in the Gazetteer forms part of the boundary between Sikkim and Bhutan.

Geographic entities mentioned:
surface_form: gipmochi
instance_of: Mountain
countries: India
Bhutan
coordinates: lat: 27.2739637
lon: 88.9000613
The area bounded by Gipmochi and Batang La, extending about 5 km to the southeast, forms a plateau called Dolam or Doklam plateau. Some British travel maps from the 19th century (prior to official surveys) mark this plateau as &quot;Gipmochi Pk&quot; and show its alignment with the Sinchela pass (on the northern ridge of the plateau). Bhutan did not have a map of its lands till 1961.

Geographic entities mentioned:
surface_form: gipmochi
instance_of: Mountain
countries: India
Bhutan
coordinates: lat: 27.2739637
lon: 88.9000613
Bhutan did not have a map of its lands till 1961. Chinese border claims. The Article mentions Gipmochi as being on Bhutan border, but no other details regarding Bhutan were given. Bhutan was not a signatory to the convention. Further, Gipmochi is not the highest point on the Doklam plateau.

Geographic entities mentioned:
surface_form: gipmochi
instance_of: Mountain
countries: India
Bhutan
coordinates: lat: 27.2739637
lon: 88.9000613
Merug La, at 15,266 feet, and Sinchela, at 14,531 feet, are higher, making the Batang La–Merug La–Sinchela line the highest watershed in the region. Maps of Sikkim produced by Survey of India in 1923, 1933 and 1937 show Gipmochi as the tri-junction point,
On 30 June 2017, the Chinese government released a previously published Chinese map depicting their territory extending south to Gipmochi.

Geographic entities mentioned:
surface_form: gipmochi
instance_of: Mountain
countries: India
Bhutan
coordinates: lat: 27.2739637
lon: 88.9000613
surface_form: gipmochi
instance_of: Mountain
countries: India
Bhutan
coordinates: lat: 27.2739637
lon: 88.9000613
Andrews was the object of particular hatred among Arabs in the Galilee area for the repressive manner in which he carried out government measures after the outbreak of the general strike of 1936, and for his support for Zionist settlements in the Galilee where he actively assisted Yishuv efforts to purchase land in the Hula Valley. He openly advised Jews to form their own defense units.

Geographic entities mentioned:
surface_form: Hula Valley
instance_of: Valley
countries: Israel
coordinates: lat: 33.103333333333
lon: 35.609166666667
Geography. Grimstad is a coastal municipality in Agder county bordering on the Skagerrak. The municipality is bordered by Arendal in the east, Froland and Birkenes in the north, and Lillesand in the west. The lakes Syndle and Rore are found in the northern part of the municipality. Landviksvannet and Reddalsvannet lakes are found in the southern part of the municipality, near Reddal.

Geographic entities mentioned:
surface_form: Syndle
instance_of: Lake
countries: Norway
coordinates: lat: 58.3625
lon: 8.4663888888889
Componenta is listed on Nasdaq Helsinki. Componenta's production units locate in Finland. There are two foundries (in Pori and in Karkkila), four machining services units (in Jyväskylä, in Härmä, in Kurikka and in Sastamala), and material services units (plate cutting, hydraulic tube manufacturing, forge) in Jyväskylä and in Leppävesi. In 2020, the company employed about 590 people. History.

Geographic entities mentioned:
surface_form: Leppävesi
instance_of: Lake
countries: Finland
coordinates: lat: 62.25
lon: 25.95
The outdoor restaurant offers scenic views of the park. History. Lying between Lake Michigan to the east and the Loop to the west, Grant Park has been Chicago's front yard since the mid-19th century.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Torget, Hurdal. Torget is the administrative centre of Hurdal municipality, Norway. It is located at the northern end of the lake Hurdalsjøen. Its population (2005) is 513.

Geographic entities mentioned:
surface_form: Hurdalsjøen
instance_of: Lake
countries: Norway
coordinates: lat: 60.31
lon: 11.104444444444
Igiugig, Alaska. Igiugig () is a census-designated place (CDP) in Lake and Peninsula Borough, Alaska, United States. The population was 68 at the 2020 census, up from 54 in 2010. The village is at the source of the Kvichak River, at the outlet of Lake Iliamna. History. The word &quot;Igiugig&quot; means &quot;Like a throat that swallows water&quot;.

Geographic entities mentioned:
surface_form: Lake Iliamna
instance_of: Lake
countries: United States
coordinates: lat: 59.536
lon: -155.024
Stoneman Lake. Stoneman Lake is a small lake located in northern Arizona, about south of the city of Flagstaff. Like the nearby Mormon Lake, it is one of the few natural lakes in Arizona. Stoneman Lake is small and shallow, with an average surface area of less than and depth of less than.

Geographic entities mentioned:
surface_form: Mormon Lake
instance_of: Lake
countries: United States
coordinates: lat: 34.9475
lon: -111.455
The lake fills a nearly circular basin in a region with some historical volcanic activity, leading to the possibility that the lake is either a crater lake or a filled in sinkhole. Evidence exists to support both conclusions, as the lake lies in the middle of the Mormon volcanic field. In Stoneman Lake, there are some traces of fungal prions.

Geographic entities mentioned:
surface_form: Mormon volcanic field
instance_of: Mountain
countries: United States
coordinates: lat: 35
lon: -111.5
Of particular interest to geologists and of some minor debate is the origin of the lake. The lake fills a nearly circular basin in a region with some historical volcanic activity, leading to the possibility that the lake is either a crater lake or a filled in sinkhole. Evidence exists to support both conclusions, as the lake lies in the middle of the Mormon volcanic field.

Geographic entities mentioned:
surface_form: crater lake
instance_of: Lake
countries: United States
coordinates: lat: 42.943611111111
lon: -122.10666666667
surface_form: crater lake
instance_of: Lake
countries: United States
coordinates: lat: 46.9382689
lon: -121.8620654
surface_form: crater lake
instance_of: Lake
countries: United States
coordinates: lat: 39.0853
lon: -106.967
Stoneman Lake. Stoneman Lake is a small lake located in northern Arizona, about south of the city of Flagstaff. Like the nearby Mormon Lake, it is one of the few natural lakes in Arizona. Stoneman Lake is small and shallow, with an average surface area of less than and depth of less than.

Geographic entities mentioned:
surface_form: stoneman lake
instance_of: Lake
countries: United States
coordinates: lat: 34.783138888889
lon: -111.52144444444
Like the nearby Mormon Lake, it is one of the few natural lakes in Arizona. Stoneman Lake is small and shallow, with an average surface area of less than and depth of less than. As such, it is subject to considerable fluctuations due to local rainfall and snowmelt conditions, and may even dry up completely.

Geographic entities mentioned:
surface_form: stoneman lake
instance_of: Lake
countries: United States
coordinates: lat: 34.783138888889
lon: -111.52144444444
Evidence exists to support both conclusions, as the lake lies in the middle of the Mormon volcanic field. In Stoneman Lake, there are some traces of fungal prions. They aren't too harmful to the environment or to the tourists who go into the lake. The lake is named after George Stoneman, who was active in the erstwhile Arizona Territory during the 1870s.

Geographic entities mentioned:
surface_form: stoneman lake
instance_of: Lake
countries: United States
coordinates: lat: 34.783138888889
lon: -111.52144444444
Semi-Bantu. 1e4vyxeppm2rqmdnr3s2payy32y0v" xml:space="preserve">The Semi-Bantu or Semibantu are specific inhabitants of the Western grassfields of Cameroon (portions of the Adamawa, West, Northwest, and Southwest regions), who speak languages that have certain characteristics to the Bantu language family but are excluded from them.

Geographic entities mentioned:
surface_form: Western grassfields
instance_of: Plateau
countries: Cameroon
coordinates: lat: 6.5
lon: 10.5
Dønttinden. Dønttinden is a mountain in Rauma Municipality in Møre og Romsdal county, Norway. The tall mountain is located inside the Reinheimen National Park in the Romsdalen valley. The European route E136 highway passes just north of the mountain. The Troll Wall and mountains of Store Trolltinden lie about to the northwest.

Geographic entities mentioned:
surface_form: Romsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 62.447222222222
lon: 7.8333333333333
Dønttinden. Dønttinden is a mountain in Rauma Municipality in Møre og Romsdal county, Norway. The tall mountain is located inside the Reinheimen National Park in the Romsdalen valley. The European route E136 highway passes just north of the mountain. The Troll Wall and mountains of Store Trolltinden lie about to the northwest.

Geographic entities mentioned:
surface_form: Store Trolltinden
instance_of: Mountain
countries: Norway
coordinates: lat: 62.486388888889
lon: 7.7186111111111
surface_form: trolltinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.9206
lon: 9.70833
Dønttinden. Dønttinden is a mountain in Rauma Municipality in Møre og Romsdal county, Norway. The tall mountain is located inside the Reinheimen National Park in the Romsdalen valley. The European route E136 highway passes just north of the mountain. The Troll Wall and mountains of Store Trolltinden lie about to the northwest.

Geographic entities mentioned:
surface_form: romsdal
instance_of: Valley
countries: Norway
coordinates: lat: 62.447222222222
lon: 7.8333333333333
surface_form: dønttinden
instance_of: Mountain
countries: Norway
coordinates: lat: 62.39963889
lon: 7.894
Dønttinden. Dønttinden is a mountain in Rauma Municipality in Møre og Romsdal county, Norway. The tall mountain is located inside the Reinheimen National Park in the Romsdalen valley. The European route E136 highway passes just north of the mountain. The Troll Wall and mountains of Store Trolltinden lie about to the northwest.

Geographic entities mentioned:
surface_form: dønttinden
instance_of: Mountain
countries: Norway
coordinates: lat: 62.39963889
lon: 7.894
The Mississippian culture peoples built mounds and earthworks in the area. Later Native Americans created a portage between the headwaters of Bayou St. John (known to the natives as Bayouk Choupique) and the Mississippi River. The bayou flowed into Lake Pontchartrain. This became an important trade route. Archaeological evidence has shown settlement in New Orleans dating back to at least 400 C.E.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
After considering several alternatives, Bienville selected the site for several strategic reasons and practical considerations, including: it was relatively high ground, along a sharp bend of the flood-prone Mississippi River, which thus created a natural levee (previously chosen as the site of an abandoned Quinipissa village); it was adjacent to the trading route and portage between the Mississippi and Lake Pontchartrain via Bayou St.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
Two large lakes (in reality estuaries) in the vicinity, Lake Pontchartrain and Lake Maurepas, commemorate respectively Louis Phelypeaux, Count Pontchartrain, minister and chancellor of France, and Jean Frederic Phelypeaux, Count Maurepas, minister and secretary of state.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
surface_form: Lake Maurepas
instance_of: Lake
countries: United States
coordinates: lat: 30.258027777778
lon: -90.498677777778
This surge also filled the Industrial Canal which breached either from the surge or the effects of being hit by a loose barge (the ING 4727). The London Avenue Canal and the 17th Street Canal were breached by the elevated waters of Lake Pontchartrain. Some areas that initially seemed to suffer little from the storm found themselves flooded by rapidly rising water on August 30.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
Lake 226. Lake 226 is one lake in Canada's Experimental Lakes Area (ELA) in Ontario. The ELA is a freshwater and fisheries research facility that operated these experiments alongside Fisheries and Oceans Canada and Environment Canada. In 1968 this area in northwest Ontario was set aside for limnological research, aiming to study the watershed of the 58 small lakes in this area.

Geographic entities mentioned:
surface_form: lake 226
instance_of: Lake
countries: Canada
coordinates: lat: 49.6897
lon: -93.7449
The theory that carbon was the limiting agent was quickly debunked by the ELA Lake 227 experiment that began in 1969, which found that carbon could be drawn from the atmosphere to remain proportional to the input of phosphorus in the water. Experimental Lake 226 was then created to test phosphorus' impact on eutrophication by itself. Geography.

Geographic entities mentioned:
surface_form: lake 226
instance_of: Lake
countries: Canada
coordinates: lat: 49.6897
lon: -93.7449
Geography. The ELA lakes were far from human activities, therefore allowing the study of environmental conditions without human interaction. Lake 226 was specifically studied over a four-year period, from 1973–1977 to test eutrophication. Lake 226 itself is a 16.2 ha double basin lake located on highly metamorphosed granite known as Precambrian granite.

Geographic entities mentioned:
surface_form: lake 226
instance_of: Lake
countries: Canada
coordinates: lat: 49.6897
lon: -93.7449
Lake 226 was specifically studied over a four-year period, from 1973–1977 to test eutrophication. Lake 226 itself is a 16.2 ha double basin lake located on highly metamorphosed granite known as Precambrian granite. The depth of the lake was measured in 1994 to be 14.7 m for the northeast basin and 11.6 m for the southeast basin.

Geographic entities mentioned:
surface_form: lake 226
instance_of: Lake
countries: Canada
coordinates: lat: 49.6897
lon: -93.7449
surface_form: basin lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.63336
lon: -105.28386
The depth of the lake was measured in 1994 to be 14.7 m for the northeast basin and 11.6 m for the southeast basin. Lake 226 had a total lake volume of 9.6 × 105 m3, prior to the lake being additionally studied for drawdown alongside other ELA lakes. Due to this relatively small fetch of Lake 226, wind action is minimized, preventing resuspension of epilimnetic sediments.

Geographic entities mentioned:
surface_form: lake 226
instance_of: Lake
countries: Canada
coordinates: lat: 49.6897
lon: -93.7449
Lake 226 had a total lake volume of 9.6 × 105 m3, prior to the lake being additionally studied for drawdown alongside other ELA lakes. Due to this relatively small fetch of Lake 226, wind action is minimized, preventing resuspension of epilimnetic sediments. Eutrophication experiment. To test the effects of fertilization on water quality and algae blooms, Lake 226 was split in half with a curtain.

Geographic entities mentioned:
surface_form: lake 226
instance_of: Lake
countries: Canada
coordinates: lat: 49.6897
lon: -93.7449
Due to this relatively small fetch of Lake 226, wind action is minimized, preventing resuspension of epilimnetic sediments. Eutrophication experiment. To test the effects of fertilization on water quality and algae blooms, Lake 226 was split in half with a curtain. This curtain divided the northeast basin (NE) from the southwest (SW) basin.

Geographic entities mentioned:
surface_form: lake 226
instance_of: Lake
countries: Canada
coordinates: lat: 49.6897
lon: -93.7449
This caused the fertilized side with phosphorus to be classified as eutrophic, making this experiment a study of eutrophication. The N:P ratio in Lake 226 had less nitrogen than required to balance the necessary phosphorus amount for successful algae production, which must have occurred to create a eutrophic water ecosystem.

Geographic entities mentioned:
surface_form: lake 226
instance_of: Lake
countries: Canada
coordinates: lat: 49.6897
lon: -93.7449
The N:P ratio in Lake 226 had less nitrogen than required to balance the necessary phosphorus amount for successful algae production, which must have occurred to create a eutrophic water ecosystem. By having less nitrogen in the lake it was hypothesized that Lake 226 was able to pull nitrogen from the atmosphere to cause this algal production.

Geographic entities mentioned:
surface_form: lake 226
instance_of: Lake
countries: Canada
coordinates: lat: 49.6897
lon: -93.7449
You then take the mean of these two values to record the secchi depth of a lake to note where the light attenuates. Prior to the beginning of the eutrophication experiment, lake 226 NE had an average secchi depth of 3.76 in 1971. During the experiment, when lake 226 NE was experiencing algal bloom production from the phosphorus application, the average secchi depth in 1974 was 1.94.

Geographic entities mentioned:
surface_form: lake 226
instance_of: Lake
countries: Canada
coordinates: lat: 49.6897
lon: -93.7449
Prior to the beginning of the eutrophication experiment, lake 226 NE had an average secchi depth of 3.76 in 1971. During the experiment, when lake 226 NE was experiencing algal bloom production from the phosphorus application, the average secchi depth in 1974 was 1.94. When only nitrogen and carbon were added to lake 226 in the SE basin, there was no decrease in secchi depth over the experiment.

Geographic entities mentioned:
surface_form: lake 226
instance_of: Lake
countries: Canada
coordinates: lat: 49.6897
lon: -93.7449
During the experiment, when lake 226 NE was experiencing algal bloom production from the phosphorus application, the average secchi depth in 1974 was 1.94. When only nitrogen and carbon were added to lake 226 in the SE basin, there was no decrease in secchi depth over the experiment. Results.

Geographic entities mentioned:
surface_form: lake 226
instance_of: Lake
countries: Canada
coordinates: lat: 49.6897
lon: -93.7449
Fish. There were reports of the survivability of fish between these basins that found that lake whitefish in the NE basin grew faster and produced more than in the SW basin of Lake 226. Annually there were no differences in the survivability of the fish, but at age 0 the fish survival rate was higher in the NE basin.

Geographic entities mentioned:
surface_form: lake 226
instance_of: Lake
countries: Canada
coordinates: lat: 49.6897
lon: -93.7449
The population of whitefish were also used in 2014 to run tests to test if the experiments on these Canadian lakes caused radioactivity in the fish. Lake 226 was of specific interest in this study since there were historical measurements of 137Cs and 226Ra concentrations that were available for comparison. Drawdown experiment.

Geographic entities mentioned:
surface_form: lake 226
instance_of: Lake
countries: Canada
coordinates: lat: 49.6897
lon: -93.7449
Drawdown experiment. A drawdown study was conducted on Lake 226 to compare the effect of the ELA lakes drawdown on the benthic and planktonic plant communities of a small oligotrophic lake. The ELA lakes included in this study were 224, 239, 240, and 373, to serve as a reference for lake 226.

Geographic entities mentioned:
surface_form: lake 226
instance_of: Lake
countries: Canada
coordinates: lat: 49.6897
lon: -93.7449
Phytoplankton. The phytoplankton communities were studied from 1992–1997 to assess the average biomass of phytoplankton in the different basins of lake 226. This study was done as a factor of the drawdown study conducted on Lake 226 following the eutrophication study, after the water chemistry and phytoplankton concentrations returned to their natural conditions.

Geographic entities mentioned:
surface_form: lake 226
instance_of: Lake
countries: Canada
coordinates: lat: 49.6897
lon: -93.7449
In comparison to three reference lakes, Lakes 224, 239 and 373, Lake 226 had a similar phytoplankton composition, however some algal groups were more abundant, therefore Lake 226 had a more abundant planktonic biomass and productivity than most lakes.

Geographic entities mentioned:
surface_form: lake 226
instance_of: Lake
countries: Canada
coordinates: lat: 49.6897
lon: -93.7449
surface_form: lake 226
instance_of: Lake
countries: Canada
coordinates: lat: 49.6897
lon: -93.7449
The theory that carbon was the limiting agent was quickly debunked by the ELA Lake 227 experiment that began in 1969, which found that carbon could be drawn from the atmosphere to remain proportional to the input of phosphorus in the water. Experimental Lake 226 was then created to test phosphorus' impact on eutrophication by itself. Geography.

Geographic entities mentioned:
surface_form: lake 227
instance_of: Lake
countries: Canada
coordinates: lat: 49.6875
lon: -93.6895
Hope River (Western Australia). Hope River is a river in central Western Australia. It is a tributary of the Yalgar River, which is in turn a tributary of the Murchison River. It rises as an overflow of Lake Anneen about 40 kilometres southwest of Meekatharra, and flows in a northwesterly direction for about 102 kilometres before discharging into the Yalgar.

Geographic entities mentioned:
surface_form: Lake Anneen
instance_of: Lake
countries: Australia
coordinates: lat: -26.933333333333
lon: 118.3
Alkali Lake is a geographic sink located in Lake County, Oregon, United States. It lies within the Alkali Subbasin of the Summer Lake Basin watershed in southeastern Oregon. The lake is situated 26 miles east of Christmas Valley, Oregon, northeast of Lake Abert, and directly west of Abert Rim and Highway 395. Alkali Lake is believed to have reached a prehistoric maximum depth of and covered about.

Geographic entities mentioned:
surface_form: Lake Abert
instance_of: Lake
countries: United States
coordinates: lat: 42.641666666666666
lon: -120.225
Alkali Lake (Oregon). Alkali Lake is a geographic sink located in Lake County, Oregon, United States. It lies within the Alkali Subbasin of the Summer Lake Basin watershed in southeastern Oregon. The lake is situated 26 miles east of Christmas Valley, Oregon, northeast of Lake Abert, and directly west of Abert Rim and Highway 395.

Geographic entities mentioned:
surface_form: alkali lake
instance_of: Lake
countries: United States
coordinates: lat: 41.89888889
lon: -118.72555556
surface_form: alkali lake
instance_of: Lake
countries: United States
coordinates: lat: 47.50039
lon: -119.51496527777778
surface_form: alkali lake (oregon)
instance_of: Lake
countries: United States
coordinates: lat: 42.9772
lon: -120.028
Alkali Lake (Oregon). Alkali Lake is a geographic sink located in Lake County, Oregon, United States. It lies within the Alkali Subbasin of the Summer Lake Basin watershed in southeastern Oregon. The lake is situated 26 miles east of Christmas Valley, Oregon, northeast of Lake Abert, and directly west of Abert Rim and Highway 395.

Geographic entities mentioned:
surface_form: alkali lake
instance_of: Lake
countries: United States
coordinates: lat: 41.89888889
lon: -118.72555556
surface_form: alkali lake
instance_of: Lake
countries: United States
coordinates: lat: 47.50039
lon: -119.51496527777778
surface_form: alkali lake
instance_of: Lake
countries: United States
coordinates: lat: 42.9772
lon: -120.028
The lake is situated 26 miles east of Christmas Valley, Oregon, northeast of Lake Abert, and directly west of Abert Rim and Highway 395. Alkali Lake is believed to have reached a prehistoric maximum depth of and covered about. Since then, its water level has fluctuated, with a general trend towards drying.

Geographic entities mentioned:
surface_form: alkali lake
instance_of: Lake
countries: United States
coordinates: lat: 41.89888889
lon: -118.72555556
surface_form: alkali lake
instance_of: Lake
countries: United States
coordinates: lat: 47.50039
lon: -119.51496527777778
surface_form: alkali lake
instance_of: Lake
countries: United States
coordinates: lat: 42.9772
lon: -120.028
Alkali Lake is believed to have reached a prehistoric maximum depth of and covered about. Since then, its water level has fluctuated, with a general trend towards drying. Notable features include dissolved alkaline salts averaging 10% of total brine weight in its seasonal waters and a nearby chemical disaster, Alkali Lake Chemical Waste Dump. Climate.

Geographic entities mentioned:
surface_form: alkali lake
instance_of: Lake
countries: United States
coordinates: lat: 41.89888889
lon: -118.72555556
surface_form: alkali lake
instance_of: Lake
countries: United States
coordinates: lat: 47.50039
lon: -119.51496527777778
surface_form: alkali lake
instance_of: Lake
countries: United States
coordinates: lat: 42.9772
lon: -120.028
Since then, its water level has fluctuated, with a general trend towards drying. Notable features include dissolved alkaline salts averaging 10% of total brine weight in its seasonal waters and a nearby chemical disaster, Alkali Lake Chemical Waste Dump. Climate. According to the Köppen Climate Classification system, Alkali Lake has a steppe climate, abbreviated &quot;BSk&quot; on climate maps.

Geographic entities mentioned:
surface_form: alkali lake
instance_of: Lake
countries: United States
coordinates: lat: 41.89888889
lon: -118.72555556
surface_form: alkali lake
instance_of: Lake
countries: United States
coordinates: lat: 47.50039
lon: -119.51496527777778
surface_form: alkali lake
instance_of: Lake
countries: United States
coordinates: lat: 42.9772
lon: -120.028
Alkali Lake (Oregon). Alkali Lake is a geographic sink located in Lake County, Oregon, United States. It lies within the Alkali Subbasin of the Summer Lake Basin watershed in southeastern Oregon. The lake is situated 26 miles east of Christmas Valley, Oregon, northeast of Lake Abert, and directly west of Abert Rim and Highway 395.

Geographic entities mentioned:
surface_form: summer lake
instance_of: Lake
countries: United States
coordinates: lat: 42.83
lon: -120.75
Legend. The temple's name is derived from the words &quot;kapala&quot; (head) and &quot;Ishvara&quot;, an epithet of Shiva. According to the &quot;Puranas&quot;, during the meeting of the deities Brahma and Shiva at top of Mount Kailash, Brahma failed to show the due respect to Shiva. Due to this, Shiva plucked off one of the five heads (&quot;kapala&quot;) of Brahma.

Geographic entities mentioned:
surface_form: Mount Kailash
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 31.066944444444
lon: 81.312777777778
Eyebrow Lake. Eyebrow Lake is a man-made, marshy lake that parallels the Qu'Appelle River in the southern region of the Canadian province of Saskatchewan. Located in the RM of Huron No. 223, it is the first lake in a series of lakes along the Qu'Appelle River after Qu'Appelle River Dam and Lake Diefenbaker. The next lake downstream is Buffalo Pound Lake.

Geographic entities mentioned:
surface_form: eyebrow lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.93336
lon: -106.1506
Eyebrow Lake. Eyebrow Lake is a man-made, marshy lake that parallels the Qu'Appelle River in the southern region of the Canadian province of Saskatchewan. Located in the RM of Huron No. 223, it is the first lake in a series of lakes along the Qu'Appelle River after Qu'Appelle River Dam and Lake Diefenbaker. The next lake downstream is Buffalo Pound Lake.

Geographic entities mentioned:
surface_form: eyebrow lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.93336
lon: -106.1506
surface_form: marshy lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.3167
lon: -124.733
The entire lake and much of the surrounding landscape is an Important Bird Area of Canada while the lower half is part of the provincial Nisku Wildlife Refuge (). Description. Eyebrow Lake is set in the Upper Qu'Appelle Valley, which was created about 14,000 years ago during the melting of the last ice age. The valley is noted for its steep sides, flat bottom, and multiple coulees.

Geographic entities mentioned:
surface_form: eyebrow lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.93336
lon: -106.1506
The valley is noted for its steep sides, flat bottom, and multiple coulees. As such, inflows for Eyebrow Lake include the Qu'Appelle River and multiple streams coming down through the coulees, including Deer Run Creek at the north-western corner. Eyebrow Lake is about wide, long, and covers an area of.

Geographic entities mentioned:
surface_form: eyebrow lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.93336
lon: -106.1506
As such, inflows for Eyebrow Lake include the Qu'Appelle River and multiple streams coming down through the coulees, including Deer Run Creek at the north-western corner. Eyebrow Lake is about wide, long, and covers an area of. In 1968, a major water management project was begun to offset the effects of periodic droughts in the region.

Geographic entities mentioned:
surface_form: eyebrow lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.93336
lon: -106.1506
In 1968, a major water management project was begun to offset the effects of periodic droughts in the region. Prior to the project, at the location of Eyebrow Lake was a large marsh in the Qu'Appelle River's floodplain. A series of dykes were built creating five basins allowing water levels to be controlled, which resulted in a permanent lake and marshland.

Geographic entities mentioned:
surface_form: eyebrow lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.93336
lon: -106.1506
The Qu'Appelle River runs along the north and eastern edge of the lake in a canal. Important Bird Area. In 1969, the Nisku Project was initiated at Eyebrow Lake by Ducks Unlimited Canada. The project was designed to help re-establish Canada geese into Saskatchewan. Goslings were raised at the lake and then distributed throughout the province into marshes, lakes, and ponds.

Geographic entities mentioned:
surface_form: eyebrow lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.93336
lon: -106.1506
Goslings were raised at the lake and then distributed throughout the province into marshes, lakes, and ponds. In the 1980s, after the geese were well established throughout the southern prairies, the project ended. The lake is now an Important Bird Area (IBA) of Canada designated as Eyebrow Lake SK 058 and is operated by Ducks Unlimited Canada. The IBA covers an area of. Flora and fauna.

Geographic entities mentioned:
surface_form: eyebrow lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.93336
lon: -106.1506