Sarmila/GeoWiki-Features huggingface dataset:
Bannock Mountain. Bannock Mountain is a summit in the North Cascades of Washington state. Description. Bannock Mountain is located east of Darrington, Washington, in the heart of the Glacier Peak Wilderness, on land managed by Mount Baker–Snoqualmie National Forest and Okanogan–Wenatchee National Forest.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: bannock mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.255833333333
lon: -120.99166666667
Description. Bannock Mountain is located east of Darrington, Washington, in the heart of the Glacier Peak Wilderness, on land managed by Mount Baker–Snoqualmie National Forest and Okanogan–Wenatchee National Forest. The mountain is situated on the crest of the Cascade Range, along the common border shared by Snohomish County and Chelan County.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.14972222
lon: -109.84944444
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.155013
lon: -117.293429
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: bannock mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.255833333333
lon: -120.99166666667
Glacier Peak, a stratovolcano that is south of Bannock Mountain, began forming in the mid-Pleistocene. Due to Glacier Peak's proximity to Bannock Mountain, volcanic ash is quite common in the area. Throughout the ice age, the North Cascades were mostly covered in thick glaciers, extending to near Puget Sound. Glaciation was most prevalent approximately, and most valleys were ice-free by.

Geographic entities mentioned:
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.14972222
lon: -109.84944444
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.155013
lon: -117.293429
surface_form: bannock mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.255833333333
lon: -120.99166666667
Description. Bannock Mountain is located east of Darrington, Washington, in the heart of the Glacier Peak Wilderness, on land managed by Mount Baker–Snoqualmie National Forest and Okanogan–Wenatchee National Forest. The mountain is situated on the crest of the Cascade Range, along the common border shared by Snohomish County and Chelan County.

Geographic entities mentioned:
surface_form: chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
Bannock Mountain. Bannock Mountain is a summit in the North Cascades of Washington state. Description. Bannock Mountain is located east of Darrington, Washington, in the heart of the Glacier Peak Wilderness, on land managed by Mount Baker–Snoqualmie National Forest and Okanogan–Wenatchee National Forest.

Geographic entities mentioned:
surface_form: bannock mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.255833333333
lon: -120.99166666667
Extensive volcanic activity began to take place in the oligocene, about. However, mountain building in the area did not begin until the miocene, approximately. Bannock Mountain is located in the Cloudy Pass batholith, an intrusive formation that was formed approximately, during the early miocene. Glacier Peak, a stratovolcano that is south of Bannock Mountain, began forming in the mid-Pleistocene.

Geographic entities mentioned:
surface_form: bannock mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.255833333333
lon: -120.99166666667
As a result, valleys in the area are deep and u-shaped, and mountains tend to be rocky, with steep slopes and narrow summits. Climate. Bannock Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originating in the Pacific Ocean travel northeast toward the Cascade Mountains.

Geographic entities mentioned:
surface_form: bannock mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.255833333333
lon: -120.99166666667
Gévora (river). The Gévora () or Xévora () is a tributary of the Guadiana, in the southwest of the Iberian Peninsula. It runs through both Portugal and Spain. It has its source in the Serra de São Mamede (Portugal), at 1,027 metres above sea level.

Geographic entities mentioned:
surface_form: xévora
instance_of: Watercourse
countries: Portugal
Spain
coordinates: lat: 39.19661
lon: -7.04567
surface_form: gévora
instance_of: Watercourse
countries: Portugal
Spain
coordinates: lat: 39.19661
lon: -7.04567
Gévora (river). The Gévora () or Xévora () is a tributary of the Guadiana, in the southwest of the Iberian Peninsula. It runs through both Portugal and Spain. It has its source in the Serra de São Mamede (Portugal), at 1,027 metres above sea level.

Geographic entities mentioned:
surface_form: gévora (river)
instance_of: Watercourse
countries: Portugal
Spain
coordinates: lat: 39.19661
lon: -7.04567
In 1997, H2M established its forensic services discipline. In 2006, H2M became the first firm in the country to develop techniques to remove perchlorate. The decade also saw the firm open a new office in Suffern, New York, to more efficiently serve the Hudson Valley.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Description. Epaulette Mountain is located in Banff National Park and is visible from the Icefields Parkway. It is part of the Waputik Mountains, a subrange of the Canadian Rockies. The nearest higher peak is Mount Sarbach, to the northwest. Epaulette Mountain is situated south of Saskatchewan Crossing, where the Icefields Parkway intersects with the David Thompson Highway.

Geographic entities mentioned:
surface_form: Mount Sarbach
instance_of: Mountain
countries: Canada
coordinates: lat: 51.8927778
lon: -116.7680556
Epaulette Mountain. Epaulette Mountain is a mountain summit in Alberta, Canada. Description. Epaulette Mountain is located in Banff National Park and is visible from the Icefields Parkway. It is part of the Waputik Mountains, a subrange of the Canadian Rockies. The nearest higher peak is Mount Sarbach, to the northwest.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: epaulette mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.865833333333335
lon: -116.735
Epaulette Mountain. Epaulette Mountain is a mountain summit in Alberta, Canada. Description. Epaulette Mountain is located in Banff National Park and is visible from the Icefields Parkway. It is part of the Waputik Mountains, a subrange of the Canadian Rockies. The nearest higher peak is Mount Sarbach, to the northwest.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: epaulette mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.865833333333335
lon: -116.735
The nearest higher peak is Mount Sarbach, to the northwest. Epaulette Mountain is situated south of Saskatchewan Crossing, where the Icefields Parkway intersects with the David Thompson Highway. Precipitation runoff from Epaulette Mountain drains east into the Mistaya River and west into Howse River, which are both tributaries of the North Saskatchewan River.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: epaulette mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.865833333333335
lon: -116.735
The nearest higher peak is Mount Sarbach, to the northwest. Epaulette Mountain is situated south of Saskatchewan Crossing, where the Icefields Parkway intersects with the David Thompson Highway. Precipitation runoff from Epaulette Mountain drains east into the Mistaya River and west into Howse River, which are both tributaries of the North Saskatchewan River.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mistaya
instance_of: Valley
countries: Canada
coordinates: lat: 51.9503
lon: -116.717
surface_form: epaulette mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.865833333333335
lon: -116.735
History. The first ascent of Epaulette Mountain was made in 1924 by Frederick Vanderbilt Field, William Osgood Field, and guide Edward Feuz Jr. The mountain's toponym was officially adopted June 7, 1961, by the Geographical Names Board of Canada.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: epaulette mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.865833333333335
lon: -116.735
History. The first ascent of Epaulette Mountain was made in 1924 by Frederick Vanderbilt Field, William Osgood Field, and guide Edward Feuz Jr. The mountain's toponym was officially adopted June 7, 1961, by the Geographical Names Board of Canada.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Geology. Like other mountains in Banff Park, the Epaulette 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: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: epaulette mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.865833333333335
lon: -116.735
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, Epaulette 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: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: epaulette mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.865833333333335
lon: -116.735
Precipitation runoff from Epaulette Mountain drains east into the Mistaya River and west into Howse River, which are both tributaries of the North Saskatchewan River. Topographic relief is significant as the summit rises 1,600 meters (5,250 feet) above the Howse Valley in three kilometers (1.9 miles), and 1,400 meters (4,593 feet) above the Mistaya Valley in three kilometers. History.

Geographic entities mentioned:
surface_form: mistaya
instance_of: Valley
countries: Canada
coordinates: lat: 51.9503
lon: -116.717
Retirement and death. After leaving the Senate, MacEachen retired to Nova Scotia spending the rest of his life at his house on Lake Ainslie in Inverness County, Cape Breton and in Antigonish. In 2006, MacEachen endorsed Bob Rae's candidacy to lead the Liberal Party, and was appointed honorary campaign chair of Rae's campaign. MacEachen died at the age of 96 on September 12, 2017, at St.

Geographic entities mentioned:
surface_form: Lake Ainslie
instance_of: Lake
countries: Canada
coordinates: lat: 46.126666666667
lon: -61.176111111111
Rheingau Hills. The Rheingau Mountains or Rheingau Hills form the westernmost section of the High Taunus and extend for 20 kilometres in a south-west to north-east direction between the Rhine valley near Lorch and Assmannshausen in the west and the Walluf valley near Schlangenbad in the east. The highest point is the 619-metre-high mountain of Kalte Herberge.

Geographic entities mentioned:
surface_form: Kalte Herberge
instance_of: Mountain
countries: Germany
coordinates: lat: 50.0548
lon: 8.0025
Location and surroundings. The Rheingau Mountains are part of the Rheingau region and lie within the county of Rheingau-Taunus-Kreis. The centre of the Rheingau Mountains is formed by the ridge line from the Kalter Herberge to the 580p-metre-high Erbacher Kopf. There is no point in four kilometres that is lower than 560 metres.

Geographic entities mentioned:
surface_form: Erbacher Kopf
instance_of: Mountain
countries: Germany
coordinates: lat: 50.068377777778
lon: 8.0350388888889
There is no point in four kilometres that is lower than 560 metres. About one kilometre southeast of the Kalter Herberge, and thus in front of the ridge line, the Hallgarter Zange also reaches a height of 580 meters. Here is a highly visible observation tower, which has been accessible again since the opening of an adventure park in 2015.

Geographic entities mentioned:
surface_form: Hallgarter Zange
instance_of: Mountain
countries: Germany
coordinates: lat: 50.0491
lon: 8.0146
In 1921 he commanded the troops of the Vitebsk region, then he took over the chair of tactics at the Military Academy of the Red Army. Between March and September 1922, he was the commander of Soviet troops in the Central-Asian Bukhara-Fergana region, and participated in the liquidation of Basmachi gangs. He contracted malaria and returned to Moscow.

Geographic entities mentioned:
surface_form: Fergana
instance_of: Valley
countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
lon: 71.757777777778
His literary works, &quot;From Sava to Adria through Bosnia and Herzegovina&quot; (1898), &quot;Along the coast of Adria&quot; (1902), &quot;From Požega valley&quot; (1914), &quot;Around Psunj mountain&quot; (1924), &quot;Topusko spa&quot; (1929), and many others, bear witness that Kempf had systematically noted his travels.

Geographic entities mentioned:
surface_form: Psunj
instance_of: Mountain
countries: Croatia
coordinates: lat: 45.4
lon: 17.316666666667
They form an important group, unusual for their scale and ambition outside London's West End. The buildings close to the quay on the River Parrett were built for the merchants who managed trade through the port, with the first bridge having been constructed in 1200 AD. Quays were built in 1424; with another quay, the &quot;Langport slip&quot;, being built in 1488 upstream of the town bridge.

Geographic entities mentioned:
surface_form: River Parrett
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 51.2292
lon: -3.00861
South side. Number 1 on the corner with West Quay and very close to the River Parrett was built as the Harbour Master's house and is now used as offices. Number 3 and 5 were originally separate houses but have now been made into one building and are used as offices. Number 7 and 9 follow the same pattern. Numbers 11 and 13 have been used as Bridgwater Arts Centre since 1946.

Geographic entities mentioned:
surface_form: River Parrett
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 51.2292
lon: -3.00861
Toponymy. The term “Métascouac” would a priori have been attributed to the river into which Lac Métascouac discharges. Surveyor Frederic William Blaiklock explored in 1847 the territory between Stoneham, near Quebec (city), and Métabetchouan–Lac-à-la-Croix, at Lac-Saint-Jean, with a view to the possible construction of a road connecting these two points.

Geographic entities mentioned:
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
Métascouac Lake. The lac Métascouac is a fresh body of water crossed by the Métascouac River, in the unorganized territory of Lac-Jacques-Cartier, in the La Côte-de-Beaupré Regional County Municipality, in the administrative region of Capitale-Nationale, in the province of Quebec, in Canada. Lac Métascouac is part of the Laurentides Wildlife Reserve.

Geographic entities mentioned:
surface_form: jacques-cartier
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.671388888889
lon: -71.747222222222
surface_form: lac métascouac
instance_of: Lake
countries: Canada
coordinates: lat: 47.837499
lon: -71.838333
Métascouac Lake. The lac Métascouac is a fresh body of water crossed by the Métascouac River, in the unorganized territory of Lac-Jacques-Cartier, in the La Côte-de-Beaupré Regional County Municipality, in the administrative region of Capitale-Nationale, in the province of Quebec, in Canada. Lac Métascouac is part of the Laurentides Wildlife Reserve.

Geographic entities mentioned:
surface_form: métascouac lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.837499
lon: -71.838333
Métascouac Lake. The lac Métascouac is a fresh body of water crossed by the Métascouac River, in the unorganized territory of Lac-Jacques-Cartier, in the La Côte-de-Beaupré Regional County Municipality, in the administrative region of Capitale-Nationale, in the province of Quebec, in Canada. Lac Métascouac is part of the Laurentides Wildlife Reserve.

Geographic entities mentioned:
surface_form: lac métascouac
instance_of: Lake
countries: Canada
coordinates: lat: 47.837499
lon: -71.838333
A few secondary forest roads serve this area for the purposes of forestry and recreational tourism activities. Forestry is the main economic activity in the sector; recreational tourism, second. The surface of Lac Métascouac is usually frozen from the beginning of December to the end of March, however the safe circulation on the ice is generally made from mid-December to mid-March. Toponymy.

Geographic entities mentioned:
surface_form: lac métascouac
instance_of: Lake
countries: Canada
coordinates: lat: 47.837499
lon: -71.838333
Toponymy. The term “Métascouac” would a priori have been attributed to the river into which Lac Métascouac discharges. Surveyor Frederic William Blaiklock explored in 1847 the territory between Stoneham, near Quebec (city), and Métabetchouan–Lac-à-la-Croix, at Lac-Saint-Jean, with a view to the possible construction of a road connecting these two points.

Geographic entities mentioned:
surface_form: lac métascouac
instance_of: Lake
countries: Canada
coordinates: lat: 47.837499
lon: -71.838333
Polyalthia hispida. &quot;Polyalthia hispida&quot; is a species of plants in the custard apple family Annonaceae. It is endemic to the foothills of Mount Bartle Frere, in the catchments of the north and south arms of the Johnstone River, Queensland, Australia. It is shrub or small tree which may flower once it has reached about in height.

Geographic entities mentioned:
surface_form: Mount Bartle Frere
instance_of: Mountain
countries: Australia
coordinates: lat: -17.383333333333
lon: 145.81666666667
Napeequa River. The Napeequa River is a long river in the U.S. state of Washington on the east side of the Cascade Range. It rises in northwest Chelan County and flows southwest into the White River near Twin Lakes. The White River flows into Lake Wenatchee. The Napeequa River and its valley are notable for their beauty and isolation, as well as their interesting geological history.

Geographic entities mentioned:
surface_form: Lake Wenatchee
instance_of: Lake
countries: United States
coordinates: lat: 47.82267
lon: -120.7772
Gaudenzio Ferrari. Gaudenzio Ferrari (– 11 January 1546) was an Italian painter and sculptor of the Renaissance. Biography. Gaudenzio was born to Franchino Ferrari at Valduggia in Valsesia in the Duchy of Milan. Valduggia is now in the province of Vercelli in Piedmont. He is said to have first learned the art of painting at Vercelli from Gerolamo Giovenone.

Geographic entities mentioned:
surface_form: Valsesia
instance_of: Valley
countries: Italy
coordinates: lat: 45.816666666667
lon: 8.1333333333333
It then meanders around Lower Kersal and Lower Broughton. It bisects Salford and Manchester, joining the rivers Irk and Medlock, and then turns west toward Irlam, as part of the Manchester Ship Canal. Its course ends just beyond Irlam Locks, where it empties into the Mersey near Flixton. Natural history.

Geographic entities mentioned:
surface_form: Irk
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 53.4869
lon: -2.24504
surface_form: Medlock
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 53.4741
lon: -2.25342
Cyclone Michaung. Severe Cyclonic Storm Michaung () was a moderate tropical cyclone which formed in the Bay of Bengal during the 2023 North Indian Ocean cyclone season. Michaung originated as a low-pressure area in the Gulf of Thailand which crossed into the Bay of Bengal and became a deep depression on December 2. It developed into a cyclonic storm thereafter and was named &quot;Michaung&quot;.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
They travelled along the coastal road with Haparanda and Tornio as their first destinations. By carriage and boat they travelled along the Tornio River to Jukkasjärvi and then out on Torneträsk (the sixth largest lake in Sweden). The three young men went farther north than any botanist since Olof Rudbeck the Younger's 1695 expedition.

Geographic entities mentioned:
surface_form: Torneträsk
instance_of: Lake
countries: Sweden
coordinates: lat: 68.366666666667
lon: 19.1
It was created to protect the wetlands of the Camaquã River lagoon delta, including the Banhado do Caipira, Rincão do Escuro and many islands. It covers the banks of the Lagoa dos Patos from the Banhado do Caipira to the pontal, and covers the Camaquã river valley up to the settlement of Pacheca. History. The Camaquã State Park was created by decree 23.798 of 12 March 1975.

Geographic entities mentioned:
surface_form: Lagoa dos Patos
instance_of: Lake
countries: Brazil
coordinates: lat: -31.15
lon: -51.39
Rutherford Ridge. hdtud9z6xyt7mtih1ukle95glpve" xml:space="preserve">#REDIRECT Rutherford Ridge

Geographic entities mentioned:
surface_form: rutherford ridge
instance_of: Mountain
coordinates: lat: -77.20722222
lon: 161.72916667
&quot;Clostera albosigma&quot;, the sigmoid prominent, is a moth of the family Notodontidae. The species was first described by Asa Fitch in 1856. It is found in North America from Newfoundland west to Vancouver Island, north to the Great Slave Lake and the Northwest Territories and south to at least Missouri. The wingspan is 28–38 mm. The moth flies from May to August depending on the location.

Geographic entities mentioned:
surface_form: Great Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 61.666666666667
lon: -114
The wavy lines represent waves and meadows. There are three white lines to represent the three large rivers in the municipality: Lygna, Audna, and Mandalselva. The two green wavy lines (between the white wavy lines represent the two valleys in the municipality: Lyngdalen and Audnedalen. The arms were designed by Richard Haugland. Churches.

Geographic entities mentioned:
surface_form: Lyngdalen
instance_of: Valley
countries: Norway
coordinates: lat: 58.31583333
lon: 7.21805556
surface_form: Audnedalen
instance_of: Valley
countries: Norway
coordinates: lat: 58.19867
lon: 7.33302
Geography. Lyngdal is a coastal municipality that and borders Lindesnes municipality to the east, Evje og Hornnes and Åseral to the north, Hægebostad and Kvinesdal and Farsund to the west. Lyngdal municipality includes the southern portion of the Lyngdalen valley which follows the river Lygna to the Lyngdalsfjorden in the west.

Geographic entities mentioned:
surface_form: Lyngdalen
instance_of: Valley
countries: Norway
coordinates: lat: 58.31583333
lon: 7.21805556
She emerged with an extensive knowledge of Marxist sociology and a degree in 1979. After that she taught history between 1979 and 1985 at the &quot;Wilhelm Pieck FDJ Youth Academy&quot; at Bogensee, near Bernau and just outside Berlin. From 1985 till 1989 she was a post-graduate student (&quot;Aspirantin&quot;) at the ruling party central committee's Academy for Social Sciences.

Geographic entities mentioned:
surface_form: Bogensee
instance_of: Lake
countries: Germany
coordinates: lat: 52.773
lon: 13.5308
Mount Oku. Mount Oku, or Kilum Mountain, is the largest volcano in the Oku Massif, in the Cameroon Volcanic Line, located in the Oku region of the Western High Plateau of Cameroon. It is the second highest mountain in mainland Central Africa. The stratovolcano rises to above sea level, and is cut by a large caldera. Geology.

Geographic entities mentioned:
surface_form: Western High Plateau
instance_of: Plateau
countries: Cameroon
coordinates: lat: 6.5
lon: 10.5
surface_form: mount oku
instance_of: Mountain
countries: Cameroon
coordinates: lat: 6.1997222222222
lon: 10.518888888889
Further trachytic lavas, tuffs and breccias were produced, and the most recent phase produced pyroclastic cones and explosion craters. One of these craters holds Lake Oku, from which flows of basalt issued in the north, and of rhyolitic and phonolitic lavas in the south. Ecology.

Geographic entities mentioned:
surface_form: Lake Oku
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.1927777777778
lon: 10.453888888889
Since then there has been steady recovery of the forest reserve, which is under the direct management of the Kilum-Ijim communities. Endangered endemic species found exclusively on Mount Oku include the Mount Oku hylomyscus, the Dieterlen's brush-furred mouse, the Lake Oku clawed frog, Crotaphatrema lamottei the Mount Oku caecilian and the toad &quot;Wolterstorffina chirioi&quot;.

Geographic entities mentioned:
surface_form: lake oku
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.1927777777778
lon: 10.453888888889
surface_form: mount oku
instance_of: Mountain
countries: Cameroon
coordinates: lat: 6.1997222222222
lon: 10.518888888889
surface_form: mount oku
instance_of: Mountain
countries: Cameroon
coordinates: lat: 6.1997222222222
lon: 10.518888888889
surface_form: mount oku
instance_of: Mountain
countries: Cameroon
coordinates: lat: 6.1997222222222
lon: 10.518888888889
Mount Oku. Mount Oku, or Kilum Mountain, is the largest volcano in the Oku Massif, in the Cameroon Volcanic Line, located in the Oku region of the Western High Plateau of Cameroon. It is the second highest mountain in mainland Central Africa. The stratovolcano rises to above sea level, and is cut by a large caldera. Geology.

Geographic entities mentioned:
surface_form: mount oku
instance_of: Mountain
countries: Cameroon
coordinates: lat: 6.1997222222222
lon: 10.518888888889
Cathedral Mountain (North Shore Mountains). Cathedral Mountain is a mountain summit located in British Columbia, Canada. Description. Cathedral Mountain is a peak situated north of Vancouver, in the North Shore Mountains which are a subrange of the Coast Mountains. Precipitation runoff from Cathedral Mountain drains east to the Seymour River, and west to the Capilano River via Eastcap Creek.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: cathedral mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.39666666666667
lon: -116.39027777777778
surface_form: cathedral mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.46666666666667
lon: -123.00861111111111
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
History. The first ascent of the summit was made 11 October 1908 by Basil S. Darling and H. Hewton. The landform was named for its cathedral-like appearance when viewed from the northeast by a British Columbia Mountaineering Club party who were climbing Mount Dickens in 1908. The mountain's toponym was officially adopted May 6, 1924, by the Geographical Names Board of Canada. Climate.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Cathedral Mountain (North Shore Mountains). Cathedral Mountain is a mountain summit located in British Columbia, Canada. Description. Cathedral Mountain is a peak situated north of Vancouver, in the North Shore Mountains which are a subrange of the Coast Mountains. Precipitation runoff from Cathedral Mountain drains east to the Seymour River, and west to the Capilano River via Eastcap Creek.

Geographic entities mentioned:
surface_form: cathedral mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.39666666666667
lon: -116.39027777777778
surface_form: cathedral mountain (north shore mountains)
instance_of: Mountain
countries: Canada
coordinates: lat: 49.46666666666667
lon: -123.00861111111111
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Cathedral Mountain (North Shore Mountains). Cathedral Mountain is a mountain summit located in British Columbia, Canada. Description. Cathedral Mountain is a peak situated north of Vancouver, in the North Shore Mountains which are a subrange of the Coast Mountains. Precipitation runoff from Cathedral Mountain drains east to the Seymour River, and west to the Capilano River via Eastcap Creek.

Geographic entities mentioned:
surface_form: cathedral mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.39666666666667
lon: -116.39027777777778
surface_form: cathedral mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.46666666666667
lon: -123.00861111111111
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Description. Cathedral Mountain is a peak situated north of Vancouver, in the North Shore Mountains which are a subrange of the Coast Mountains. Precipitation runoff from Cathedral Mountain drains east to the Seymour River, and west to the Capilano River via Eastcap Creek. Cathedral is more notable for its steep rise above local terrain than for its absolute elevation.

Geographic entities mentioned:
surface_form: cathedral mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.39666666666667
lon: -116.39027777777778
surface_form: cathedral mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.46666666666667
lon: -123.00861111111111
surface_form: seymour river
instance_of: Watercourse
countries: Canada
coordinates: lat: 51.2386
lon: -118.958
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Climate. Based on the Köppen climate classification, Cathedral Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall.

Geographic entities mentioned:
surface_form: cathedral mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.39666666666667
lon: -116.39027777777778
surface_form: cathedral mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.46666666666667
lon: -123.00861111111111
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Cathedral is more notable for its steep rise above local terrain than for its absolute elevation. Topographic relief is significant as the summit rises above Seymour Valley in. Access to the peak is off-limits because the mountain lies within the Metro Vancouver watersheds which provide clean drinking water to the city. There are radio repeater towers on the summit. History.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
History. The first ascent of the summit was made 11 October 1908 by Basil S. Darling and H. Hewton. The landform was named for its cathedral-like appearance when viewed from the northeast by a British Columbia Mountaineering Club party who were climbing Mount Dickens in 1908. The mountain's toponym was officially adopted May 6, 1924, by the Geographical Names Board of Canada. Climate.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Rigg Beck is also the name of a famous dwelling – the Purple House – placed where the Beck crosses the Keskadale road, and which formed an excellent starting point for exploring the fells. Source and course. Rigg Beck arises at the top of the high pass between Ard Crags and Causey Pike, of the latter of which it forms one boundary. The beck flows eventually into Newlands Beck.

Geographic entities mentioned:
surface_form: Ard Crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5663
lon: -3.22953
surface_form: Causey Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.576338888889
lon: -3.2112694444444
Source and course. Rigg Beck arises at the top of the high pass between Ard Crags and Causey Pike, of the latter of which it forms one boundary. The beck flows eventually into Newlands Beck. The path alongside Rigg Beck forms an attractive pedestrian route between Newlands Valley and Buttermere.

Geographic entities mentioned:
surface_form: Newlands Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.573011111111
lon: -3.1848694444444
She received a bachelor's degree in English at the University of Maryland before moving back to Missouri, settling in the Lebanon area. She oversaw a class of high school sophomores, juniors, and seniors who produced &quot;Bittersweet, the Ozark Quarterly&quot; magazine. Massey also gave hundreds of talks about the Ozarks. Awards.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
Brunkollen. Brunkollen is a mountain on the border of Dovre Municipality in Innlandet county and Oppdal Municipality in Trøndelag county in Norway. The tall mountain is located in the Dovrefjell mountains and inside the Dovrefjell-Sunndalsfjella National Park, about north of the village of Dombås and about northwest of the village of Hjerkinn.

Geographic entities mentioned:
surface_form: Dovrefjell
instance_of: Mountain
countries: Norway
coordinates: lat: 62.1
lon: 9.41666667
surface_form: sunndalsfjella
instance_of: Mountain
countries: Norway
surface_form: dovrefjell
instance_of: Mountain
countries: Norway
coordinates: lat: 62.1
lon: 9.41666667
The tall mountain is located in the Dovrefjell mountains and inside the Dovrefjell-Sunndalsfjella National Park, about north of the village of Dombås and about northwest of the village of Hjerkinn. The mountain is surrounded by several other notable mountains including Tverrfjellet to the southeast, Einøvlingseggen and Skredahøin to the southwest, Snøhetta and Storstyggesvånåtinden to the west.

Geographic entities mentioned:
surface_form: Einøvlingseggen
instance_of: Mountain
countries: Norway
coordinates: lat: 62.23527778
lon: 9.305
surface_form: Skredahøin
instance_of: Mountain
countries: Norway
coordinates: lat: 62.25
lon: 9.18333333
surface_form: Snøhetta
instance_of: Mountain
countries: Norway
coordinates: lat: 62.32
lon: 9.2683333333333
surface_form: Storstyggesvånåtinden
instance_of: Mountain
countries: Norway
coordinates: lat: 62.28401
lon: 9.18821
surface_form: tverrfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 62.2258
lon: 9.49222
surface_form: tverrfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 62.413333333333
lon: 6.1655555555556
surface_form: tverrfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 61.10337
lon: 8.35782
surface_form: tverrfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 61.8424
lon: 8.1109
Brunkollen. Brunkollen is a mountain on the border of Dovre Municipality in Innlandet county and Oppdal Municipality in Trøndelag county in Norway. The tall mountain is located in the Dovrefjell mountains and inside the Dovrefjell-Sunndalsfjella National Park, about north of the village of Dombås and about northwest of the village of Hjerkinn.

Geographic entities mentioned:
surface_form: brunkollen
instance_of: Mountain
countries: Norway
coordinates: lat: 62.318
lon: 9.362
At the first town meeting on February 5, 1749, he was elected one of the town's five selectmen. French and Indian War. He was initially a lieutenant in the New Hampshire Provisional Regiment and spent the fall of 1755 scouting the area around Lake Champlain. Promoted to captain, he raised a company that was among the defenders at the siege of Fort William Henry in August 1757.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
The community of Haukedalen is on the high ground of the Gaula river watershed. The Haukedalen people have always belonged to the parish of Førde, even though they had to cross the high Rørvikfjellet pass in the Gaularfjellet mountains to reach the Holsen Church (until Haukedalen received its own church).

Geographic entities mentioned:
surface_form: Gaularfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 61.33861111
lon: 6.40361111
Aït Si Amar. Aït Si Amar is a village in the Boumerdès Province in Kabylie, Algeria. Location. The village is surrounded by Isser River and the town of Ammal in the &quot;Khachna&quot; mountain range.

Geographic entities mentioned:
surface_form: Isser River
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.8391
lon: 3.6679
Gurdial Singh (mountaineer). Gurdial Singh (1 January 1924 – 30 May 2023) was an Indian schoolteacher and mountaineer who led the first mountaineering expedition of independent India to Trisul (7,120 metres) in 1951. In 1958, he led the team that made the first ascent of Mrigthuni (6,855 metres). In 1965, he was a member of the first successful Indian expedition team to climb Mount Everest.

Geographic entities mentioned:
surface_form: Trisul
instance_of: Mountain
countries: India
coordinates: lat: 30.312777777778
lon: 79.777222222222
Gurdial Singh (mountaineer). Gurdial Singh (1 January 1924 – 30 May 2023) was an Indian schoolteacher and mountaineer who led the first mountaineering expedition of independent India to Trisul (7,120 metres) in 1951. In 1958, he led the team that made the first ascent of Mrigthuni (6,855 metres). In 1965, he was a member of the first successful Indian expedition team to climb Mount Everest.

Geographic entities mentioned:
surface_form: Mrigthuni
instance_of: Mountain
countries: India
coordinates: lat: 30.29
lon: 79.82972222222222
In 1958, he led the team that made the first ascent of Mrigthuni (6,855 metres). In 1965, he was a member of the first successful Indian expedition team to climb Mount Everest. Singh also led many expeditions at The Doon School, where he was a geography teacher, and along with other Doon masters and students was instrumental in establishing a mountaineering culture in post-Independence India.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Holdsworth and Jack Gibson to take up mountaineering. The first headmaster of Doon Arthur Foot was a member of the Alpine Club. Together, they scaled many peaks including Bandarpunch, Trisul, Kamet, Abi Gamin and Nanda Devi. He was the first Indian member of the famed Alpine Club, which was &quot;a club of English gentlemen devoted to mountaineering&quot;.

Geographic entities mentioned:
surface_form: Bandarpunch
instance_of: Mountain
countries: India
coordinates: lat: 30.99916667
lon: 78.54166667
surface_form: Trisul
instance_of: Mountain
countries: India
coordinates: lat: 30.312777777778
lon: 79.777222222222
surface_form: Kamet
instance_of: Mountain
countries: India
coordinates: lat: 30.92
lon: 79.593333333333
surface_form: Abi Gamin
instance_of: Mountain
countries: India
coordinates: lat: 30.93
lon: 79.6
surface_form: Nanda Devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
He was the first Indian member of the famed Alpine Club, which was &quot;a club of English gentlemen devoted to mountaineering&quot;. In 1965, Singh was a member of the first Indian expedition to successfully climb Mount Everest. The expedition was led by Mohan Singh Kohli and Singh reached the South Col with the first group to attempt the summit.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
The former alignments of NY 96 were subsequently repurposed as connectors between NY 22 and NY 96. Both roads, a combined in length, are now designated as NY 914A, an unsigned reference route. In 1942, the state of New York switched the alignments of NY 96 and NY 2, a highway extending from Owego to Rochester in the Finger Lakes region. The change placed NY 2 on the Troy–Massachusetts routing.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
The popular spread of &quot;Pao Chui&quot; was in early association with Shaolin and was one of the first styles implemented into the Shaolin monastery training regimen. The first Shaolin monks learned this style from local martial artists from Mount Emei. Local legends say that the style was created by the bonding of Heaven, Earth, and the three emperors.

Geographic entities mentioned:
surface_form: Mount Emei
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 29.519722222222
lon: 103.3325
Activities and sports. &quot;Brabrandstien&quot; (lit.: the Brabrand pathway), which runs along the Aarhus river from the inner city and around both Brabrand Sø and Årslev Engsø, was established by the City Council in 1956 as a labor project for the unemployed, to give the public better access to green space. The pathway is c. 26 km long, with 9.5 km for Brabrand Lake alone.

Geographic entities mentioned:
surface_form: brabrand sø
instance_of: Lake
countries: Denmark
coordinates: lat: 56.1458
lon: 10.1125
Brabrand Lake. Brabrand Lake () is a lake in the district of Brabrand (Gellerup), west of Aarhus city, Denmark. The Aarhus River passes through Brabrand Lake and it is possible to canoe all the way to the inner city from here. The lake is oblong-shaped. Since 2003, Brabrand Lake has been steadily extended 3–4 km further west, with the new lake of Årslev Engsø (lit.: Årslev meadow-lake).

Geographic entities mentioned:
surface_form: brabrand lake
instance_of: Lake
countries: Denmark
coordinates: lat: 56.1458
lon: 10.1125
The lake is oblong-shaped. Since 2003, Brabrand Lake has been steadily extended 3–4 km further west, with the new lake of Årslev Engsø (lit.: Årslev meadow-lake). In 2001–2, it was politically decided to abandon the artificial draining of the meadows and as of 2013, Årslev meadow lake has a surface area of around. The total area including adjoining meadows and reed beds totals.

Geographic entities mentioned:
surface_form: brabrand lake
instance_of: Lake
countries: Denmark
coordinates: lat: 56.1458
lon: 10.1125
The total area including adjoining meadows and reed beds totals. It is hoped that Eurasian bittern and otter will find themselves a new home here with time. In everyday parlance, &quot;Brabrand Lake&quot; is a general term including the surroundings as well, indicating a total area of around with for the lake alone.

Geographic entities mentioned:
surface_form: brabrand lake
instance_of: Lake
countries: Denmark
coordinates: lat: 56.1458
lon: 10.1125
In everyday parlance, &quot;Brabrand Lake&quot; is a general term including the surroundings as well, indicating a total area of around with for the lake alone. A special Natura2000 protected area under the European Union, Brabrand Lake is home to a large variety of birds and an important resting place for migrating birds, with several towers built to facilitate bird-watching.

Geographic entities mentioned:
surface_form: brabrand lake
instance_of: Lake
countries: Denmark
coordinates: lat: 56.1458
lon: 10.1125
A public hiking trail surrounds the lake, whose landscape varies from wide meadows and reed beds to dense woods. Privately owned pastures almost completely surround the lake and are not publicly accessible, but public paths leading to the lake are scattered in between. There are several garden allotments (&quot;kolonihaver&quot; in Danish) near Brabrand Lake and it is a popular recreational spot.

Geographic entities mentioned:
surface_form: brabrand lake
instance_of: Lake
countries: Denmark
coordinates: lat: 56.1458
lon: 10.1125
Acting partly on this fact, the lake water was also included in a large water treatment project led by &quot;Aarhus Vand A/S&quot; from 2006 to 2013. The project involved the Brabrand Lake, the Aarhus River and the Aarhus harbour, budgeted at € 45 million. As a result, the waters in Brabrand Lake and the Aarhus River attained bathing quality in September 2012. Special flora and fauna.

Geographic entities mentioned:
surface_form: brabrand lake
instance_of: Lake
countries: Denmark
coordinates: lat: 56.1458
lon: 10.1125
As a result, the waters in Brabrand Lake and the Aarhus River attained bathing quality in September 2012. Special flora and fauna. Apart from these rarer species, the Brabrand Lake area is characterized by many common species living here, mostly birds, insects and aquatic plants. Archaeological finds. The area around Brabrand Lake has been populated for at least 6,000 years.

Geographic entities mentioned:
surface_form: brabrand lake
instance_of: Lake
countries: Denmark
coordinates: lat: 56.1458
lon: 10.1125
Special flora and fauna. Apart from these rarer species, the Brabrand Lake area is characterized by many common species living here, mostly birds, insects and aquatic plants. Archaeological finds. The area around Brabrand Lake has been populated for at least 6,000 years. In prehistoric times, Brabrand Lake was part of a deep brackish water fjord, offering natural protection and food in abundance.

Geographic entities mentioned:
surface_form: brabrand lake
instance_of: Lake
countries: Denmark
coordinates: lat: 56.1458
lon: 10.1125
The third district, La Pointe-aux-Prairies, is a typical suburb composed of townhouses, condos and single-family dwellings, which makes it a destination of choice for young families that wish to remain on the island of Montréal. The Saint Lawrence River flows at the southern border of Montreal, while the Rivière des Prairies River forms Montreal Island's northern boundary with Laval. Demographics.

Geographic entities mentioned:
surface_form: Rivière des Prairies
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.708333333333
lon: -73.479166666667
Description. Ghenge Liru is a glaciated summit in the Nepali Himalayas. It is situated north of Kathmandu above the Langtang Valley in Langtang National Park. Precipitation runoff from the mountain's slopes drains into tributaries of the Trishuli River. Topographic relief is significant as the summit rises 3,400 metres (11,155 ft) above the Langtang Valley in.

Geographic entities mentioned:
surface_form: Langtang Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 28.25
lon: 85.5