Sarmila/GeoWiki-Features huggingface dataset:
The mountain is the site of mining ruins from the late nineteenth century. Climate. According to the Köppen climate classification system, New York Mountain is located in an alpine subarctic climate zone with cold, snowy winters, and cool to warm summers. Due to its altitude, it receives precipitation all year, as snow in winter and as thunderstorms in summer, with a dry period in late spring.

Geographic entities mentioned:
surface_form: new york mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.50861111111111
lon: -106.61805555555554
It is also the northernmost point in the canton of Vaud above 2,300 metres and the most prominent summit of both cantons. The Vanil Noir is the culminating point of the range separating the regions of Gruyère and Pays-d'Enhaut, although it is followed by the almost equally high Vanil de l'Ecri and Pointe de Paray.

Geographic entities mentioned:
surface_form: Vanil de l'Ecri
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.5222
lon: 7.14361
surface_form: Pointe de Paray
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.5131
lon: 7.13694
surface_form: vanil noir
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.528472222222
lon: 7.1483611111111
surface_form: gruyère
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.65
lon: 7.1
Vanil Noir. The Vanil Noir (; local) is a mountain of the Fribourg Prealps, located on the border between the cantons of Fribourg and Vaud in western Switzerland. Reaching a height of 2,389 metres above sea level, the Vanil Noir is the highest summit of the canton of Fribourg and of the Alpine foothills lying north of the Saane and Simme (or northwest of the Saanenmöser Pass).

Geographic entities mentioned:
surface_form: vanil noir
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.528472222222
lon: 7.1483611111111
On the west side, it consists of a smaller cirque, overlooking the alp of Bounavau. On the northeast side it overlooks the valley of Les Morteys. All three valleys descending from the Vanil Noir are part of the Saane drainage basin. The closest localities are Grandvillard (Fribourg) and Château d'Oex (Vaud). Several vertiginous trails lead to the summit, and cross it from north to south.

Geographic entities mentioned:
surface_form: vanil noir
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.528472222222
lon: 7.1483611111111
On the northeast side it overlooks the valley of Les Morteys. All three valleys descending from the Vanil Noir are part of the Saane drainage basin. The closest localities are Grandvillard (Fribourg) and Château d'Oex (Vaud). Several vertiginous trails lead to the summit, and cross it from north to south. The Vanil Noir is part of a nature reserve since 1983.

Geographic entities mentioned:
surface_form: vanil noir
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.528472222222
lon: 7.1483611111111
This stretch of the river is designated a National Wild and Scenic Riverway. From Kindred, the river flows north-northeastward through the fertile plains of the Red River Valley. The character of the river changes as it leaves the sandy grasslands and picks up the fertile clay soil of the Red River Valley.

Geographic entities mentioned:
surface_form: Red River Valley
instance_of: Valley
countries: Canada
United States
coordinates: lat: 49
lon: -97.5
The character of the river changes as it leaves the sandy grasslands and picks up the fertile clay soil of the Red River Valley. Previously, the river posed a flooding hazard to cities such as West Fargo and Harwood, where it joins the Red River of the North, which flows north to Lake Winnipeg in Manitoba.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Overview. The map shows a hilly area with the Rajmahal hills running from the bank of the Ganges in the extreme north to the south, beyond the area covered by the map into Dumka district. ‘Farakka’ is marked on the map and that is where Farakka Barrage is, just inside West Bengal. Rajmahal coalfield is shown in the map.

Geographic entities mentioned:
surface_form: Rajmahal hills
instance_of: Mountain
countries: India
coordinates: lat: 25
lon: 87
The area is served by a number of public schools, including John Rogers Elementary, Jane Addams Middle School, and Nathan Hale High School. The site where Nathan Hale High School now sits was formerly Meadowbrook Golf Course. History. Meadowbrook, with Thornton Creek near Lake Washington, has been inhabited since the end of the last glacial period (c. 8,000 BCE&mdash;10,000 years ago).

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
From then onwards, push-pull trains each made up of an ABe 4/4, an intermediate car if required, and a control car served the Oberengadin branch line Samedan – Pontresina, until the opening of the Vereina line in 1999, and the associated introduction of the &quot;NEVA Retica&quot; timetable concept made them superfluous.

Geographic entities mentioned:
surface_form: Oberengadin
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.5497
lon: 9.8959
After the old measurement system was abolished, &quot;Merchant&quot; was remeasured in Buffalo on April 25, 1865; under the new system, &quot;Merchant&quot; was or long, or wide and deep, while her gross tonnage was 861.18 tons. While travelling on Lake Michigan in May 1866, &quot;Merchant&quot; lost one of her crewmen overboard. In May 1867, &quot;Merchant&quot; became stuck in ice near Buffalo.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
on July 31. She was placed in dry dock at the Wolf & Davidson shipyard in Milwaukee, where it was discovered that she had sustained severe damage to her keel and bottom. Her hull sustained $9,500 (equivalent to $ in) worth of damage, while her cargo was a total loss, resulting in a loss of $25,000 (equivalent to $ in). &quot;Merchant&quot; ran aground on Peche Island in Lake St. Clair in November.

Geographic entities mentioned:
surface_form: Lake St. Clair
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.450265
lon: -82.67572
Arthur Purchas. Arthur Guyon Purchas (27 September 1821 &ndash; 28 May 1906) was a clergyman, missionary, surgeon, musician, engineer, inventor, pioneer, geologist and botanist born at St. Arvans in the Wye Valley, Monmouthshire, Wales, who lived most of his life in Auckland, New Zealand.

Geographic entities mentioned:
surface_form: Wye Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69255
lon: -2.66283
Many of these hill forests are threatened by granite quarrying, forest fires and grazing. It has vanished from many sites where it was earlier known. Some well-known locations include the Nandi Hills, Horsley Hills, Gingee, Yercaud and the Biligirirangans. The species is also seen in some parts of the Western Ghats including the Anamalais.

Geographic entities mentioned:
surface_form: Horsley Hills
instance_of: Mountain
countries: India
coordinates: lat: 13.6508702
lon: 78.3965255
While sailing from Tongatapu to the Marquesas, Wilson became the first European to visit Pukarua, which he found uninhabited and named Searle Island. On 24 May Wilson he sighted Mangareva in the Gambier Islands, which he named for James Gambier, then a Lord Commissioner of the Admiralty. The largest land feature on Mangareva is named Mount Duff. At Mangareva &quot;Duff&quot; stopped at Rikitea.

Geographic entities mentioned:
surface_form: Mount Duff
instance_of: Mountain
countries: France
coordinates: lat: -23.1286
lon: -134.974
Grahovsko Polje. Grahovsko Polje is a &quot;polje&quot; (karst field) in Bosnia and Herzegovina, on the territory of Bosansko Grahovo municipality. It is surrounded by mountains: Dinara, Uilica, Jadovnik, Šator and Staretina. It consists of several smaller spaces: Resenovačko Polje, Pašića, Crnoluško Polje and Ždralovac. It is located at an altitude of 708 - 873, average 782 meters a.s.l.

Geographic entities mentioned:
surface_form: Šator
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 44.157330555556
lon: 16.5897
surface_form: Staretina
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 44.0833
lon: 16.6833
surface_form: šator
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 44.157330555556
lon: 16.5897
surface_form: staretina
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 44.0833
lon: 16.6833
Grahovsko Polje. Grahovsko Polje is a &quot;polje&quot; (karst field) in Bosnia and Herzegovina, on the territory of Bosansko Grahovo municipality. It is surrounded by mountains: Dinara, Uilica, Jadovnik, Šator and Staretina. It consists of several smaller spaces: Resenovačko Polje, Pašića, Crnoluško Polje and Ždralovac. It is located at an altitude of 708 - 873, average 782 meters a.s.l.

Geographic entities mentioned:
surface_form: grahovsko polje
instance_of: Plateau
countries: Bosnia and Herzegovina
Tičevska plateau at 1098 meters a.s.l. is a passage to the east towards Glamoč and Glamočko Polje. From a hydrographic point of view, Grahovsko polje is divided into the basins of the Black and Adriatic seas. The watershed in Begovac is popularly known as Dijelovi. There is a natural Pečenačko lake in the field, and an artificial lake in Borovača.

Geographic entities mentioned:
surface_form: grahovsko polje
instance_of: Plateau
countries: Bosnia and Herzegovina
L'Acadie, Quebec. L'Acadie () is a former municipality in the Montérégie region of Quebec, Canada, on the west side of the Richelieu River, across from Saint-Jean-sur-Richelieu, Quebec. It was about 30 miles (50 km) from Montreal, and about the same distance from the United States border at the head of Lake Champlain.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Fuerte de Lonquén. ms2qeeytaw1aafj0pl4mbq1hmi8w2" xml:space="preserve">Fuerte de Lonquén () was a fort built in 1602 by Governor Alonso de Ribera on the south bank of the Lonquén River nine kilometers from the Itata River. It was established to protect the grain fields and cattle of the local estancias that fed Ribera's Spanish army on La Frontera.

Geographic entities mentioned:
surface_form: Lonquén River
instance_of: Watercourse
countries: Chile
coordinates: lat: -36.4325
lon: -72.690277777778
Luray, Virginia. Luray is the county seat of Page County, Virginia, United States. It is in the Shenandoah Valley and found within the northwestern part of the Commonwealth. The population was 4,831 at the 2020 census. The town was founded by William Staige Marye in 1812, a descendant of a family native to Luray, France. Geography.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Recognition and influence. The Nicholls Building on King Street in Toronto, Ontario, Canada is named after him including the Nicholls Oval and Nicholls Lake in Ontario. He was also known as an early editor of the Toronto Star newspaper. Frederic Nicholls's speech of January 19, 1905, to the Empire Club in Toronto was published as Niagara's power: past, present, prospective...

Geographic entities mentioned:
surface_form: Nicholls Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.4189
lon: -88.7844
Zalla. Zalla is a town and municipality located in the province of Biscay, in the Autonomous Community of the Basque Country, northern Spain, 24 kilometers to the southwest of Bilbao. The river Cadagua runs through the city. According to the 2019 census, it has 8,447 inhabitants. Popular culture. The Zallense people are known for their popular culture and especially for their mythology.

Geographic entities mentioned:
surface_form: Cadagua
instance_of: Watercourse
countries: Spain
coordinates: lat: 43.092947
lon: -3.391657
The attack made the British realise the militarily strategic position of Imphal. Geography and climate. Imphal lies on the Imphal Valley surrounded by nine ranges of hills at in extreme eastern India, with an average elevation of. It has a humid subtropical climate (Köppen: &quot;Cwa&quot;) with cool, dry winters and a slightly hot monsoon season.

Geographic entities mentioned:
surface_form: Imphal Valley
instance_of: Valley
countries: India
Gros Cap Reefs Light. The Gros Cap Reefs Light is a lighthouse located at the entrance to St. Mary's River from Whitefish Bay of Lake Superior. The light was completed in 1953 and replaced a lightship stationed there since 1923. The lighthouse, owned by the Canadian Coast Guard, is located on the southwest edge of the Gros Cap Reef.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Around the same time, the boat was equipped with a quick firing (QF) deck gun. On 24 May, in the Gulf of Drin, &quot;U-4&quot; unsuccessfully attacked an Italian, but on 9 June, Singule spotted the British cruiser escorting a convoy along the Montenegrin coast. Despite a screen of six destroyers, &quot;U-4&quot; was able to torpedo &quot;Dublin&quot; off San Giovanni de Medua.

Geographic entities mentioned:
surface_form: Gulf of Drin
instance_of: Body of water
countries: Albania
coordinates: lat: 41.76666667
lon: 19.51666667
Rivière du Lac. The rivière du Lac (&quot;English: River of the lake&quot;) is a tributary of the west bank of the Montmorency River. This watercourse flows on the north shore of the St. Lawrence River, in the city of Quebec, in the administrative region of Capitale-Nationale, in the province of Quebec, in Canada.

Geographic entities mentioned:
surface_form: rivière du lac
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.934444
lon: -71.194444
Lawrence River. Toponymy. The toponym &quot;rivière du Lac&quot; derives from the fact that this watercourse crosses the &quot;Lac du Chemin de l'Aqueduc&quot;. A dam has been built at the mouth of this lake. The toponym &quot;Rivière du Lac&quot; was formalized on December 5, 1968 at the Place Names Bank of the Commission de toponymie du Québec.

Geographic entities mentioned:
surface_form: rivière du lac
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.934444
lon: -71.194444
Spring Valley Creek (Current River tributary). Spring Valley Creek is a stream in Texas and Shannon counties of the Ozarks of southern Missouri. The stream is a tributary of the Current River. The stream headwaters arise in southeast Texas County at. The stream flows to the east-southeast passing into Shannon County south of Summersville.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
3700 to 2700 BC). The municipality was formerly known by its French name &quot;Locras&quot;, however, that name is no longer used. During the Neolithic era there were two villages pile-dwelling (or stilt house) settlements along the shore of Lake Biel. The two settlements are now part of the Prehistoric Pile dwellings around the Alps, a UNESCO World Heritage Site.

Geographic entities mentioned:
surface_form: Lake Biel
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.085555555556
lon: 7.1741666666667
Of the water in the municipality, 0.5% is in lakes and 0.2% is in rivers and streams. On 31 December 2009 Amtsbezirk Erlach, the municipality's former district, was dissolved. On the following day, 1 January 2010, it joined the newly created Verwaltungskreis Seeland. Lüscherz is located on the right side of Lake Biel and at the foot of Mt. Feiberg.

Geographic entities mentioned:
surface_form: Lake Biel
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.085555555556
lon: 7.1741666666667
Features and location. The central feature of Mungo National Park is Lake Mungo, the second largest of the ancient dry lakes. The Mungo National Park is noted for the archaeological remains discovered in the park the remains of Mungo Man, the oldest human remains discovered in Australia, and Mungo Lady, the oldest known human to have been ritually cremated.

Geographic entities mentioned:
surface_form: Lake Mungo
instance_of: Lake
countries: Australia
coordinates: lat: -33.75
lon: 143.08333333333
She arranged an interview with a commander at Kasumigaura Airfield of Imperial Japanese Navy Air Service, and he accepted her for exceptional ten days' probational trainee, and she obtained acrobatics license.

Geographic entities mentioned:
surface_form: Kasumigaura
instance_of: Lake
Group of lakes
countries: Japan
coordinates: lat: 36.040277777778
lon: 140.39416666667
Mount Tholus. r0w02wkvzgyzghju6c1elhdi66uf" xml:space="preserve">#redirect Mount Tholus

Geographic entities mentioned:
surface_form: mount tholus
instance_of: Mountain
coordinates: lat: -63.2667
lon: -56.0667
surface_form: tholus
instance_of: Mountain
coordinates: lat: -63.2667
lon: -56.0667
It is estimated to occupy less than 2,200 km2 and is found between 47 and 139 metres above sea level. It has been proposed that the natural northern and southern limits of the species's range are the Manambolo river and Tsiribihina river, respectively. However, this has not been tested empirically. Threats.

Geographic entities mentioned:
surface_form: Manambolo river
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -19.24025
lon: 44.33283333333333
surface_form: Tsiribihina river
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -19.8833
lon: 44.45
Spider Lake (Minnesota). Spider Lake is a lake in Chisago County, Minnesota, in the United States. The outline of Spider Lake branches like a spider, hence the name.

Geographic entities mentioned:
surface_form: spider lake
instance_of: Lake
countries: United States
coordinates: lat: 44.674444444444
lon: -85.4925
surface_form: spider lake
instance_of: Lake
countries: United States
coordinates: lat: 45.32472222
lon: -92.82166667
Lake Rototuna Lower. Lake Rototuna Lower is a lake in the Northland Region of New Zealand.

Geographic entities mentioned:
surface_form: lake rototuna
instance_of: Lake
countries: New Zealand
coordinates: lat: -36.251667
lon: 174.040139
surface_form: lake rototuna lower
instance_of: Lake
countries: New Zealand
coordinates: lat: -36.25726
lon: 174.052317
Mount Evan-Thomas is a mountain summit located in the Opal Range of the Canadian Rockies of Alberta, Canada. Mount Evan-Thomas is the highest point in the Opal Range. It is situated in the Kananaskis River Valley northeast of Lower Kananaskis Lake and east of Highway 40 in Peter Lougheed Provincial Park. Its nearest higher peak is Mount Rae, to the south-southeast. __NOTOC__
History.

Geographic entities mentioned:
surface_form: Lower Kananaskis Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.6561
lon: -115.137
Mount Evan-Thomas is a mountain summit located in the Opal Range of the Canadian Rockies of Alberta, Canada. Mount Evan-Thomas is the highest point in the Opal Range. It is situated in the Kananaskis River Valley northeast of Lower Kananaskis Lake and east of Highway 40 in Peter Lougheed Provincial Park. Its nearest higher peak is Mount Rae, to the south-southeast. __NOTOC__
History.

Geographic entities mentioned:
surface_form: mount rae
instance_of: Mountain
countries: Canada
coordinates: lat: 50.62277777777778
lon: -114.97472222222223
Its nearest higher peak is Mount Rae, to the south-southeast. __NOTOC__
History. The mountain was named in honor of Rear Admiral Sir Hugh Evan-Thomas (1862–1928), Royal Navy commander of the 5th Battle Squadron of the Grand Fleet during the Battle of Jutland in World War I. The name of the mountain was initially approved as Mount Evans-Thomas in 1922.

Geographic entities mentioned:
surface_form: mount evans
instance_of: Mountain
countries: Canada
coordinates: lat: 52.444
lon: -118.129
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Evan-Thomas. Mount Evan-Thomas is a mountain summit located in the Opal Range of the Canadian Rockies of Alberta, Canada. Mount Evan-Thomas is the highest point in the Opal Range. It is situated in the Kananaskis River Valley northeast of Lower Kananaskis Lake and east of Highway 40 in Peter Lougheed Provincial Park. Its nearest higher peak is Mount Rae, to the south-southeast.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mount evan-thomas
instance_of: Mountain
countries: Canada
coordinates: lat: 50.7659
lon: -115.0953
Its nearest higher peak is Mount Rae, to the south-southeast. __NOTOC__
History. The mountain was named in honor of Rear Admiral Sir Hugh Evan-Thomas (1862–1928), Royal Navy commander of the 5th Battle Squadron of the Grand Fleet during the Battle of Jutland in World War I. The name of the mountain was initially approved as Mount Evans-Thomas in 1922.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The name of the mountain was initially approved as Mount Evans-Thomas in 1922. The spelling error was corrected when the mountain's present name was made official in 1972 by the Geographical Names Board of Canada. The first ascent of the peak was made in 1954 by M.S. Hicks, W. Lemmon, G. Ross, I. Spreat, and J.F. Tarrant. Geology.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Temperatures can drop below −20 °C with wind chill factors below −30 °C. In terms of favorable weather, June through September are the best months to climb Mount Evan-Thomas. Precipitation runoff from the mountain drains into tributaries of the Kananaskis River.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Evan-Thomas. Mount Evan-Thomas is a mountain summit located in the Opal Range of the Canadian Rockies of Alberta, Canada. Mount Evan-Thomas is the highest point in the Opal Range. It is situated in the Kananaskis River Valley northeast of Lower Kananaskis Lake and east of Highway 40 in Peter Lougheed Provincial Park. Its nearest higher peak is Mount Rae, to the south-southeast.

Geographic entities mentioned:
surface_form: mount evan-thomas
instance_of: Mountain
countries: Canada
coordinates: lat: 50.7659
lon: -115.0953
Hicks, W. Lemmon, G. Ross, I. Spreat, and J.F. Tarrant. Geology. Mount Evan-Thomas 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. Mount Evan-Thomas was created during the Lewis Overthrust.

Geographic entities mentioned:
surface_form: mount evan-thomas
instance_of: Mountain
countries: Canada
coordinates: lat: 50.7659
lon: -115.0953
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Mount Evan-Thomas was created during the Lewis Overthrust. The steeply tilted strata are virtually the same in each peak of the Opal Range, with softer layers sandwiched between harder layers. Climate.

Geographic entities mentioned:
surface_form: mount evan-thomas
instance_of: Mountain
countries: Canada
coordinates: lat: 50.7659
lon: -115.0953
The steeply tilted strata are virtually the same in each peak of the Opal Range, with softer layers sandwiched between harder layers. Climate. Based on the Köppen climate classification, Mount Evan-Thomas is located in a subarctic climate zone 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: mount evan-thomas
instance_of: Mountain
countries: Canada
coordinates: lat: 50.7659
lon: -115.0953
Temperatures can drop below −20 °C with wind chill factors below −30 °C. In terms of favorable weather, June through September are the best months to climb Mount Evan-Thomas. Precipitation runoff from the mountain drains into tributaries of the Kananaskis River.

Geographic entities mentioned:
surface_form: mount evan-thomas
instance_of: Mountain
countries: Canada
coordinates: lat: 50.7659
lon: -115.0953
The population as of the Canada 2021 Census was 7,253. The township completely encircles the city of Waterloo and the city of Warden. Demographics. In the 2021 Census of Population conducted by Statistics Canada, Shefford had a population of living in of its total private dwellings, a change of from its 2016 population of. With a land area of, it had a population density of in 2021. Mont Shefford

Geographic entities mentioned:
surface_form: Mont Shefford
instance_of: Mountain
countries: Canada
coordinates: lat: 45.3636
lon: -72.6258
Project location. The project was to be located in the central Kenyan Highlands situated on the Kinangop Plateau, at an altitude of approximately 2,600 m above sea level, in Karati, Magumu and Heni Sub-locations of Nyandarua County. History. The Kinangop Wind Park project was launched in 2004 as a joint venture between EcoGen Wind Farms and Kengen.

Geographic entities mentioned:
surface_form: Kinangop Plateau
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.549995
lon: 36.554947
Despite the low chance of future eruptions, many scientists still consider mudflows a major threat at Mount Jefferson. Geography. The second tallest mountain in the U.S. state of Oregon after Mount Hood, Mount Jefferson lies within Jefferson, Linn, and Marion counties, in the central part of the state. Reaching an elevation of, the volcano has a proximal relief of.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 45.3522
lon: -68.2828
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 42.4584
lon: -74.6196
The wilderness area covers, with more than 150 lakes. It also has of trails, including of the Pacific Crest National Scenic Trail. Mount Jefferson is the major feature of the wilderness, along with the nearby Three Fingered Jack volcano. Physical geography. Mount Jefferson lies in the temperate maritime climate of Western Oregon.

Geographic entities mentioned:
surface_form: Three Fingered Jack
instance_of: Mountain
countries: United States
coordinates: lat: 44.478965122
lon: -121.843058797
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 45.3522
lon: -68.2828
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 42.4584
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The strip may still be active, as monogenetic vents near Jefferson have produced basaltic andesite since the last glacial period. Jefferson — with Mount Hood, the Three Sisters-Broken Top area, and Crater Lake — represents one of four volcanic centers responsible for much of the Oregon Cascades' Quaternary andesite, dacite, and rhyolite deposits.

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Eruptions around the same time period yielded pyroclastic flows that coursed down the Whitewater River drainage of the eastern side of Mount Jefferson, and the Whitewater Creek on the volcano's western flank. Basaltic lava flows at Forked Butte and to the south of Bear Butte mark the newest lava flows in the Jefferson area, as both were produced after Mount Mazama erupted roughly 7,600 years ago.

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Other popular trails include the Firecamp Lakes Trail and Canyon Creek Meadows trails. In addition to the trails, some of the most popular areas around Mount Jefferson Wilderness include Eight Lakes Basin, Pamelia Lake, Jack Lake, Duffy Lake, Russell Lake, Santiam Lake and Wasco Lake. Mount Jefferson can be climbed, but the route is challenging, especially the pinnacle of the summit.

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Some of this andesite and dacite occurs in vents that underlie the Jefferson vicinity, which also erupted during the Quaternary. Quaternary volcanic production rates in the Cascade Range from Jefferson to Crater Lake have averaged per mile of arc length per million years.

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Mount Jefferson (Oregon). Mount Jefferson is a stratovolcano in the Cascade Volcanic Arc, part of the Cascade Range in the U.S. state of Oregon. The second highest mountain in Oregon, it is situated within Linn County, Jefferson County, and Marion County and forms part of the Mount Jefferson Wilderness.

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Mount Jefferson (Oregon). Mount Jefferson is a stratovolcano in the Cascade Volcanic Arc, part of the Cascade Range in the U.S. state of Oregon. The second highest mountain in Oregon, it is situated within Linn County, Jefferson County, and Marion County and forms part of the Mount Jefferson Wilderness.

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Mount Jefferson is a stratovolcano in the Cascade Volcanic Arc, part of the Cascade Range in the U.S. state of Oregon. The second highest mountain in Oregon, it is situated within Linn County, Jefferson County, and Marion County and forms part of the Mount Jefferson Wilderness. Due to the ruggedness of its surroundings, the mountain is one of the hardest volcanoes to reach in the Cascades.

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It is also a popular tourist destination despite its remoteness, with recreational activities including hiking, backpacking, mountaineering, and photography. Vegetation at Mount Jefferson is dominated by Douglas fir, silver fir, mountain hemlock, ponderosa pine, lodgepole pine, and several cedar species.

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It is considered a low threat by the United States Geological Survey. Despite the low chance of future eruptions, many scientists still consider mudflows a major threat at Mount Jefferson. Geography. The second tallest mountain in the U.S. state of Oregon after Mount Hood, Mount Jefferson lies within Jefferson, Linn, and Marion counties, in the central part of the state.

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Wilderness. Mount Jefferson's eastern segment lies within the Warm Springs Indian Reservation, and its western portion within the Mount Jefferson Wilderness, of the Willamette National Forest and Deschutes National Forests. The wilderness area covers, with more than 150 lakes. It also has of trails, including of the Pacific Crest National Scenic Trail.

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It also has of trails, including of the Pacific Crest National Scenic Trail. Mount Jefferson is the major feature of the wilderness, along with the nearby Three Fingered Jack volcano. Physical geography. Mount Jefferson lies in the temperate maritime climate of Western Oregon. The Cascades absorb east-moving moisture, causing warm and dry summers.

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Moving east, annual precipitation levels decrease from to lower than. When Little Ice Age glaciers retreated during the 20th century, water filled in the spaces left behind, forming moraine-dammed lakes, which are more common in the Mount Jefferson Wilderness and the nearby Three Sisters Wilderness than anywhere else in the contiguous United States.

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The flood on August 21, 1934, at a lake formed near Whitewater Glacier, created a debris flow that reached the Whitewater River drainage and buried parts of Jefferson Park in of debris; another event took place in 1957, but was poorly documented. Mount Jefferson has 35 snow and ice features, including four named glaciers: Whitewater, Jefferson Park, Russell, and Waldo.

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Mount Jefferson has 35 snow and ice features, including four named glaciers: Whitewater, Jefferson Park, Russell, and Waldo. These features, for the most part on the northern, eastern, and southeastern parts of Mount Jefferson, span elevations from and cover an area of.

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Other geographic features at Jefferson include rock outcrops, steep talus slopes, conifer forests, and alpine meadows. Additionally, a number of rivers drain Mount Jefferson.

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Additionally, a number of rivers drain Mount Jefferson. The northern and northwestern slopes feed the South Fork Breitenbush River, which flows into Detroit Lake, and the eastern side of Detroit Lake also receives water from Whitewater Creek, Russell Creek, and Milk Creek, which flow from the western flank of Mount Jefferson.

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The Whitewater Glacier and the northeastern side of the volcano drain into the Whitewater River, and Shitike Creek flows between Mount Jefferson and Olallie Butte before reaching the Deschutes River. Both Jefferson and Parker Creeks receive water from Jefferson's southeastern slopes, then join the Metolius River. Wildfires occur within the wilderness area at Mount Jefferson.

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Both Jefferson and Parker Creeks receive water from Jefferson's southeastern slopes, then join the Metolius River. Wildfires occur within the wilderness area at Mount Jefferson. In the late summer to early fall of 2017, the Whitewater and Little Devil fires occurred.

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In the late summer to early fall of 2017, the Whitewater and Little Devil fires occurred. While the Little Devil fire covered, the Whitewater fire reached more than in area, provoking the use of amphibious aircraft and causing trail closures. As a result of the Whitewater fire, officials closed the Mount Jefferson Wilderness during the solar eclipse of August 21, 2017. Ecology.

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Ecology. Vegetation at Mount Jefferson is dominated by Douglas fir, silver fir, mountain hemlock, ponderosa pine, lodgepole pine, and several species of cedar. Vine maple, rhododendron, purple lupine, yellow lupine, Indian paintbrush, wild strawberries, and red huckleberries are also common around Mount Jefferson.

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Above the timber line at above sea level, mountain hemlock and whitebark pine predominate, though mountain hemlock has also invaded into subalpine meadows at Mount Jefferson, possibly as a result of fire control programs, grazing, the influence of adjacent forest areas, and climate change.

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Carnivorous animals at Mount Jefferson and its surroundings include American black bears, coyotes, cougars, red foxes, raccoons, American martens, stoats (also known as ermines), long-tailed weasels, American minks, North American river otters, and bobcats.

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Roughly half the lakes in the Jefferson area contain rainbow trout. Geology. Mount Jefferson shows normal magnetic polarity, suggesting that it formed less than 730,000 years ago.

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