Sarmila/GeoWiki-Features huggingface dataset:
Rúrec. Rúrec, also spelled Rurec, (possibly from Quechua &quot;ruri&quot; interior; valley or little river, &quot;-q&quot; a suffix) is a mountain in the southern part of the Cordillera Blanca in the Andes of Peru. It is located in the Ancash Region, Huaraz Province, Olleros District, and in the Huari Province, Chavín de Huantar District. Rúrec is located south of Huantsán.

Geographic entities mentioned:
surface_form: rúrec
instance_of: Mountain
countries: Peru
coordinates: lat: -9.56583
lon: -77.3067
Rúrec. Rúrec, also spelled Rurec, (possibly from Quechua &quot;ruri&quot; interior; valley or little river, &quot;-q&quot; a suffix) is a mountain in the southern part of the Cordillera Blanca in the Andes of Peru. It is located in the Ancash Region, Huaraz Province, Olleros District, and in the Huari Province, Chavín de Huantar District. Rúrec is located south of Huantsán.

Geographic entities mentioned:
surface_form: rúrec
instance_of: Mountain
countries: Peru
coordinates: lat: -9.56583
lon: -77.3067
surface_form: rurec
instance_of: Mountain
countries: Peru
coordinates: lat: -9.56583
lon: -77.3067
I DOK: Warszawska Brygada Obrony Narodowej (Warsaw Brigade of National Defense)
II DOK: Wołyńska Półbrygada Obrony Narodowej (Volhynian Demi-Brigade of National Defense)
III DOK: Dziśnieńska Półbrygada Obrony Narodowej (Dzisna Half-Brigade of National Defense)
IV DOK: Sieradzka Brygada Obrony Narodowej (Sieradz Brigade of National Defense)
V DOK: Dąbrowska Brygada Obrony Narodowej, Górnośląska Brygada Obrony Narodowej, Podhalańska Brygada Obrony Narodowej, Śląsko-Cieszyńska Brygada Obrony Narodowej (Dąbrowa Górnicza Brigade of National Defense, Upper Silesian Brigade of National Defense, Podhale Brigade of National Defense, Cieszyn Silesia Brigade of National Defense)
VI DOK: Lwowska Brygada Obrony Narodowej, Tarnopolska Półbrygada Obrony Narodowej (Lwów Brigade of National Defense, Tarnopol Half-Brigade of National Defense)
VII DOK: Poznańska Brygada Obrony Narodowej, Kaliska Brygada Obrony Narodowej (Poznań Brigade of National Defense, Kalisz Brigade of National Defense)
VIII DOK: Chełmińska Brygada Obrony Narodowej, Morska Brygada Obrony Narodowej, Pomorska Brygada Obrony Narodowej (Chełmno Brigade of National Defense, Sea Brigade of National Defense, Pomorze Brigade of National Defense)
X DOK: Karpacka Brygada Obrony Narodowej, Podkarpacka Brygada Obrony Narodowej (Carpathian Brigade of National Defense, Subcarpathian Brigade of National Defense)
Chełmińska Brygada ON •
Cieszyńska Brygada ON •
Dąbrowska Brygada ON •
Kaliska Brygada ON •
Karpacka Brygada ON •
Lwowska Brygada ON •
Morska Brygada ON •
Podhalańska Brygada ON •
Podkarpacka Brygada ON •
Pomorska Brygada ON •
Poznańska Brygada ON •
Sieradzka Brygada ON •
Śląska Brygada ON •
Warszawska Brygada ON
Bielsko •
Brodnica •
Brzozów •
Bydgoszcz •
Chełm •
Chrzanów •
Cieszyn I •
Cieszyn II •
Czersk •
Dąbrowa Górnicza •
Gdynia I •
Gdynia II •
Gdynia III •
Grudziądz •
Huculski I •
Huculski II •
Jabłonowo •
Jarosław •
Jasło •
Kartuzy IV •
Kaszuby V •
Katowice •
Kcynia •
Kępno •
Kłobuck •
Koronowo •
Kościan •
Kościerzyna •
Kowel •
Koźmin •
Krosno •
Krotoszyn •
Leszno •
Limanowa •
Lubliniec •
Lwów I •
Lwów II •
Łuck •
Mazurski I •
Mazurski II •
Nakło •
Nowy Sącz •
Oborniki •
Olkusz •
Opalenica •
Ostrów •
Ostrzeszów •
Oświęcim •
Poznań I •
Poznań II •
Przemyśl •
Rawicz •
Rybnik •
Rzeszów •
Sambor •
Sanok •
Sosnowiec •
Stanisławów •
Starogard •
Stry •
Szamotuły •
Świecie •
Tarnowskie Góry •
Tuchola •
Turka •
Warszawski I •
Warszawski II •
Warszawski III •
Wągrowiec •
Wieluń I •
Wieluń II •
Zakopane •
Zawiercie •
Żnin •
Żywiec

Geographic entities mentioned:
surface_form: Podhale
instance_of: Valley
countries: Poland
coordinates: lat: 49.4793
lon: 20.0291
The specific epithet (&quot;hammersleyana&quot;) honours Brenda Hammersley, for her contribution to the knowledge of the flora of the Denmark area. Distribution and habitat. This species of &quot;Andersonia&quot; grows in open jarrah woodland near Mount Lindsey in the Jarrah Forest bioregion of south-western Western Australia. Conservation status.

Geographic entities mentioned:
surface_form: Mount Lindsey
instance_of: Mountain
countries: United States
coordinates: lat: 37.583611111111
lon: -105.445
In the spring and summer of 2003, Parks Canada performed a prescribed burn in selected areas of the range in order to reduce fire hazard, manage the pine beetle population and increase sheep habitat. In total, 5300 hectares of land were affected. List of mountains. Anûkathâ Îpa is the official name as of 2020 of a mountain that previously held a racist and offensive name.

Geographic entities mentioned:
surface_form: Anûkathâ Îpa
instance_of: Mountain
countries: Canada
coordinates: lat: 51.13611111111111
lon: -115.33777777777777
Beehive Mountain. The Beehive Mountain was named by George M. Dawson in 1886. It is located in the High Rock Range of the Canadian Rockies and is on the boundary between British Columbia and Alberta, which follows the Continental Divide in this area. The mountain was named for its fancied resemblance to a beehive.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Beehive Mountain. The Beehive Mountain was named by George M. Dawson in 1886. It is located in the High Rock Range of the Canadian Rockies and is on the boundary between British Columbia and Alberta, which follows the Continental Divide in this area. The mountain was named for its fancied resemblance to a beehive.

Geographic entities mentioned:
surface_form: the beehive
instance_of: Mountain
countries: Canada
coordinates: lat: 51.41416666666667
lon: -116.24388888888889
surface_form: beehive mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.065
lon: -114.66305555556
surface_form: the beehive
instance_of: Mountain
countries: Canada
coordinates: lat: 51.064166666666665
lon: -115.39972222222222
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Beehive Mountain. The Beehive Mountain was named by George M. Dawson in 1886. It is located in the High Rock Range of the Canadian Rockies and is on the boundary between British Columbia and Alberta, which follows the Continental Divide in this area. The mountain was named for its fancied resemblance to a beehive.

Geographic entities mentioned:
surface_form: beehive mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.065
lon: -114.66305555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Beehive Mountain. The Beehive Mountain was named by George M. Dawson in 1886. It is located in the High Rock Range of the Canadian Rockies and is on the boundary between British Columbia and Alberta, which follows the Continental Divide in this area. The mountain was named for its fancied resemblance to a beehive.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
South of Schwanden is the oldest &quot;Jagdbanngebiet&quot; (literally hunting-banned area) in Switzerland, the &quot;Freiberg Kärpf&quot;, which has been protected since 1548. Also to the south, the Niederenbäch stream descends from the slopes of the mountain of Kärpf (). This stream has been dammed to create the Garichtisee reservoir.

Geographic entities mentioned:
surface_form: Kärpf
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.91674
lon: 9.09323
Located in a relatively unpopulated area, the Glacier View reservoir would have flooded lower Camas Creek and would have raised the level of Logging Lake by, inundating much of the winter range for the park's white-tailed deer, elk, mule deer and moose. The proposed reservoir was to extend nearly to the Canada–US border, at an estimated cost of $94,962,000.

Geographic entities mentioned:
surface_form: Logging Lake
instance_of: Lake
countries: United States
coordinates: lat: 48.7531
lon: -114.089
The Bad Rock Canyon site would have been on the main stem of the Flathead and was also determined to have poor abutment rock, as well as alluvial deposits on the valley floor reaching up to deep. It would have flooded the Hungry Horse damsite, which was under construction, as well as Lake McDonald in the park. Present.

Geographic entities mentioned:
surface_form: Lake McDonald
instance_of: Lake
countries: United States
coordinates: lat: 48.5692
lon: -113.935
List of monuments in Lalitpur, Nepal. This is a list of monuments in Lalitpur District, Nepal as officially recognized by and available through the website of the Department of Archaeology, Nepal. Patan Durbar Square also known as Lalitpur Durbar Square, in the city of Lalitpur, is an ancient palace in Kathmandu Valley. There are numerous monuments in the square.

Geographic entities mentioned:
surface_form: Kathmandu Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
Prince Edward Island Route 24. Route 24, also known as Dover Road and Murray Harbour Road, is a, two-lane, uncontrolled-access, secondary highway in Prince Edward Island. Its southern terminus is at Route 4 in Murray River and its northern terminus is at Route 3 in Vernon River. The route is in Kings and Queens counties. Route description.

Geographic entities mentioned:
surface_form: Vernon River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.20611111111111
lon: -62.841944444444444
The purchase of Swan Island was proposed to Portland's city council in March 1920 as part of a $10,000,000 harbor development plan. Other features of this &quot;Swan Island project&quot; included the development of Mock's Bottom, a swampy area directly east of Swan Island, and the draining of Guild's Lake, located west of the island. Swan Island Airport.

Geographic entities mentioned:
surface_form: Mock's Bottom
instance_of: Landform
countries: United States
coordinates: lat: 45.570277777778
lon: -122.705
surface_form: Guild's Lake
instance_of: Lake
countries: United States
coordinates: lat: 45.546944444444
lon: -122.72055555556
Industrial park. Swan Island is currently the location of a industrial park managed by the Port of Portland. The industrial development extends into the adjacent Mock's Bottom area, a natural wetland that was filled in the 1960s. Vigor Marine Group is headquartered at Swan Island, where it operates a shipyard with three dry docks.

Geographic entities mentioned:
surface_form: Mock's Bottom
instance_of: Landform
countries: United States
coordinates: lat: 45.570277777778
lon: -122.705
Lake Tenkiller, created by damming the Illinois River beginning in 1947 with completion in 1953, has attracted tourists and fishermen to this once sparsely settled area. Seventy miles of the river between Lake Tenkiller and the Arkansas border, flowing through the Cookson Hills, have been supervised by the Oklahoma Scenic Rivers Commission, currently headed by Ed Fite since 1970. Description.

Geographic entities mentioned:
surface_form: Cookson Hills
instance_of: Landform
countries: United States
coordinates: lat: 35.7
lon: -94.8
It was not until 1978 that the municipal incorporation was confirmed. On December 26, 1998, the municipality was renamed to Trois-Rives (French for &quot;Three shores&quot;) to better represent the geography of the municipality as it is crossed by three rivers: the Matawin, the Mékinac, and the Saint-Maurice River.

Geographic entities mentioned:
surface_form: Mékinac
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.854166666667
lon: -72.765555555556
Geography. It is bounded on the west by the Saint-Maurice River, and includes the communities of Grande-Anse, Olscamps, Rivière-Matawin, Saint-Joseph-de-Mékinac, and partially Rivière-aux-Rats. The territory also includes in the east portions of Mékinac Lake (in part), Missionary Lake (in part), aux Loutres, and Dumont Lakes.

Geographic entities mentioned:
surface_form: Mékinac Lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.054722222222225
lon: -72.67333333333333
surface_form: Missionary Lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.91666667
lon: -72.56027778
The territory also includes in the east portions of Mékinac Lake (in part), Missionary Lake (in part), aux Loutres, and Dumont Lakes. The toponym &quot;Trois-Rives&quot; (three banks) refers to the three rivers that drain the territory: the Matawin River, the Saint-Maurice River and the Mékinac River. Demographics. Private dwellings occupied by usual residents: 288 (total dwellings: 544)
Mayors.

Geographic entities mentioned:
surface_form: Mékinac River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.854166666667
lon: -72.765555555556
The Italian territory extends over about 10° of latitude, therefore, while remaining in the context of temperate climates without extremes of heat, cold or aridity, the climatic difference between the north and the south of the country is not at all negligible, going from the nival climates of the Alpine peaks, to the cool semi-continental temperate climate of the Po Valley, to the Mediterranean climate of the central-southern coasts and the islands.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
In most of the inland northern and central regions, the climate ranges from humid subtropical to humid continental and oceanic. In particular, the climate of the Po valley geographical region is mostly continental, with harsh winters and hot summers. The coastal areas of Liguria, Tuscany and most of the South generally fit the Mediterranean climate stereotype (Köppen climate classification).

Geographic entities mentioned:
surface_form: Po valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
The petals are mauve to deep bluish-purple and long. Flowering occurs in spring. This species is included in &quot;Prostanthera ovalifolia&quot; in Queensland. Taxonomy. &quot;Prostanthera lanceolata&quot; was first formally described in 1928 by Karel Domin in &quot;Bibliotheca Botanica&quot; from material he collected near the &quot;Tambourine Mountains&quot; in 1910. Distribution and habitat.

Geographic entities mentioned:
surface_form: &quot;Tambourine Mountains&quot;
instance_of: Mountain
countries: Australia
coordinates: lat: -27.927513888889
lon: 153.19430555556
Jotunheimen. Jotunheimen (; &quot;the home of the Jötunn&quot;) is a mountainous area of roughly in southern Norway and is part of the long range known as the Scandinavian Mountains. The 29 highest mountains in Norway are all located in the Jotunheimen mountains, including the tall mountain Galdhøpiggen (the highest point in Norway and Northern Europe).

Geographic entities mentioned:
surface_form: Galdhøpiggen
instance_of: Mountain
countries: Norway
coordinates: lat: 61.633333333333
lon: 8.3
The picture is taken from Gjendesheim, a starting point for hiking into the mountain range. There is a very popular trail along Besseggen that follows the edge of the mountainous range to the right, which it is named after. There is a National Tourist Route, the Sognefjell Road, from Skjolden to Lom, as well as another road, the RV 51, from Gol to Vågåmo through the special area of Valdresflya.

Geographic entities mentioned:
surface_form: Besseggen
instance_of: Mountain
countries: Norway
coordinates: lat: 61.504608333333
lon: 8.72685
Geology. Jotunheimen is a residual mountain area, which is a mass of rock that has remained in place as the surrounding relief has been eroded. The tops of Dovrefjell and Jotunheimen and other parts of southern Norway are the few remnants of a formerly flat surface that existed in Norway prior to uplift. This surface is now largely eroded and warped.

Geographic entities mentioned:
surface_form: Dovrefjell
instance_of: Mountain
countries: Norway
coordinates: lat: 62.1
lon: 9.41666667
Geomorphology. The characteristic mountain landforms in Jotunheimen have been sculptured by glacial geomorphology during the Pleistocene, especially during its last glacial period. Whereas the Scandinavian Ice Sheet covered most of Fennoscandia, some mountain peaks of Jotunheimen were not covered by glaciers and remained as Nunatak. Galdhopiggen, Glittertinden or Store Lauvhøi are examples.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Whereas the Scandinavian Ice Sheet covered most of Fennoscandia, some mountain peaks of Jotunheimen were not covered by glaciers and remained as Nunatak. Galdhopiggen, Glittertinden or Store Lauvhøi are examples. Towards the west, the Scandinavian Ice Sheet disintegrated in several glacier tongues and caused the formation of the Norwegian Fiords. Climate, glaciers and permafrost.

Geographic entities mentioned:
surface_form: Store Lauvhøi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.7397
lon: 8.54278
A first comprehensive study on mountain permafrost in Scandinavia was published in 1982. Today, these findings are confirmed at various places, and Juvvasshøi, Juvasshytta and Galdhøi are preferred areas for scientific periglacial research due to yearround good logistic conditions compared with arctic areas. Jotunheimen National Park.

Geographic entities mentioned:
surface_form: Juvvasshøi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.67749
lon: 8.36848
surface_form: Galdhøi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.64972222
lon: 8.31861111
Jotunheimen National Park. Jotunheimen contains Jotunheimen National Park, which was established in 1980 and covers an area of. The Hurrungane mountain range is also inside the national park with the sharpest peaks in Jotunheimen. Adjacent to the national park border is Utladalen Nature Reserve which covers the Utladalen valley and the mountain Falketind, amongst others.

Geographic entities mentioned:
surface_form: Falketind
instance_of: Mountain
countries: Norway
coordinates: lat: 61.384444444444
lon: 8.0969444444444
In the east, the road leads to Lom. A few small dirt roads lead to different parts of the edge of Jotunheimen National Park, although the area of the national park itself is practically roadless. A small exception, however, is a blind road in the Veodalen to Glitterheim, whose head is inside the national park area near the mountain Glittertind.

Geographic entities mentioned:
surface_form: Veodalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.63332
lon: 8.68416
surface_form: Glittertind
instance_of: Mountain
countries: Norway
coordinates: lat: 61.651944444444
lon: 8.5544444444444
It is the second-highest point of the Joffre Group, which is a subset of the Lillooet Ranges. It is situated east of Pemberton and northeast of Lillooet Lake. Joffre is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 1,500 meters (4,920 ft) above Cayoosh Creek in.

Geographic entities mentioned:
surface_form: Lillooet Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.25
lon: -122.5
surface_form: lillooet lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.3333
lon: -122.417
Joffre is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 1,500 meters (4,920 ft) above Cayoosh Creek in. The nearest higher peak is Mount Matier, to the south. The mountain's climate supports the Matier Glacier on the southwest slope, and the Anniversary Glacier on the southeast slope.

Geographic entities mentioned:
surface_form: Mount Matier
instance_of: Mountain
countries: Canada
coordinates: lat: 50.33303
lon: -122.43597
The mountain's toponym was officially adopted June 22, 1967, by the Geographical Names Board of Canada. Joffre Peak should not be confused with Mount Joffre in the Canadian Rockies which is also named for the same person. Climate. Based on the Köppen climate classification, Joffre Peak is located in a subarctic climate zone of western North America.

Geographic entities mentioned:
surface_form: Mount Joffre
instance_of: Mountain
countries: Canada
coordinates: lat: 50.528333333333336
lon: -115.20694444444445
surface_form: joffre peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.33303
lon: -122.45268
Joffre Peak. Joffre Peak is a mountain summit located in the Coast Mountains, in Joffre Lakes Provincial Park, in southwestern British Columbia, Canada. It is the second-highest point of the Joffre Group, which is a subset of the Lillooet Ranges. It is situated east of Pemberton and northeast of Lillooet Lake.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: joffre peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.33303
lon: -122.45268
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Precipitation runoff from the peak drains into Joffre Creek and Cayoosh Creek which are both within the Fraser River watershed. History. The first ascent of the mountain was made on July 19, 1957 by Dick Chambers and Paddy Sherman, who were members of the British Columbia Mountaineering Club. The first ascent party named this peak for its position at the head of Joffre Creek.

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
Joffre Peak. Joffre Peak is a mountain summit located in the Coast Mountains, in Joffre Lakes Provincial Park, in southwestern British Columbia, Canada. It is the second-highest point of the Joffre Group, which is a subset of the Lillooet Ranges. It is situated east of Pemberton and northeast of Lillooet Lake.

Geographic entities mentioned:
surface_form: joffre peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.33303
lon: -122.45268
Climate. Based on the Köppen climate classification, Joffre Peak is located in a subarctic 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: joffre peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.33303
lon: -122.45268
As a result, the Coast Mountains experience high precipitation, especially during the winter months in the form of snowfall. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. The months July through September offer the most favorable weather for climbing Joffre Peak.

Geographic entities mentioned:
surface_form: joffre peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.33303
lon: -122.45268
The nearest higher peak is Mount Matier, to the south. The mountain's climate supports the Matier Glacier on the southwest slope, and the Anniversary Glacier on the southeast slope. Precipitation runoff from the peak drains into Joffre Creek and Cayoosh Creek which are both within the Fraser River watershed. History.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The first ascent party named this peak for its position at the head of Joffre Creek. The creek and mountain's name honors Marshal Joseph Jacques Césaire Joffre (1852–1931), a French general who served as Commander-in-Chief of French Armies in World War I. The mountain's toponym was officially adopted June 22, 1967, 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
The creek and mountain's name honors Marshal Joseph Jacques Césaire Joffre (1852–1931), a French general who served as Commander-in-Chief of French Armies in World War I. The mountain's toponym was officially adopted June 22, 1967, by the Geographical Names Board of Canada. Joffre Peak should not be confused with Mount Joffre in the Canadian Rockies which is also named for the same person.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Challwayuq. Challwayuq (Quechua &quot;challwa&quot; fish, &quot;-yuq&quot; a suffix, &quot;the one with fish&quot;, also spelled &quot;Chalhuayoc&quot;) is a mountain in the Andes of Peru whose summit reaches about above sea level. It is located in the Pasco Region, Daniel Alcides Carrión Province, Yanahuanca District. Challwayuq lies northwest of Yana Chaka.

Geographic entities mentioned:
surface_form: challwayuq
instance_of: Mountain
countries: Peru
coordinates: lat: -10.555
lon: -76.67527778
surface_form: challwayuq
instance_of: Mountain
countries: Peru
coordinates: lat: -12.10388889
lon: -75.59416667
Caundle Marsh. Caundle Marsh is a village and civil parish in northwest Dorset, England, situated in the Blackmore Vale, southeast of Sherborne. The parish includes the hamlet of Tut Hill and the Dorset County Council estimate that in 2013 the population of the parish was 70. History.

Geographic entities mentioned:
surface_form: Blackmore Vale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 50.94
lon: -2.31
Major General William W. Loring was ordered to clear the Kanawha Valley of Union soldiers, and then move northeast to form a junction with more Confederate soldiers in the Shenandoah Valley. Loring's campaign to accomplish this objective began September6 and ended September16, although an important raid that was part of Loring's plan began on August22. Confederate army. Major General William W.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
It then descends again to its large lower section, which includes an open forest of aspen and white fir trees, sagebrush flats, and the junction with the south branch of the canyon. Towering above are granite cliffs and pinnacles. Like its neighbor to the north, Lamoille Canyon, Seitz Canyon is branched. The southern fork begins at the highest point of the range, the north face of Ruby Dome.

Geographic entities mentioned:
surface_form: Lamoille Canyon
instance_of: Valley
countries: United States
coordinates: lat: 40.6916
lon: -115.474
Towering above are granite cliffs and pinnacles. Like its neighbor to the north, Lamoille Canyon, Seitz Canyon is branched. The southern fork begins at the highest point of the range, the north face of Ruby Dome. Nearby are two other tall peaks known locally as Ruby Pyramid and Seitz Peak. The canyon descends steeply in four steps before merging with the main branch of the canyon.

Geographic entities mentioned:
surface_form: Ruby Dome
instance_of: Mountain
countries: United States
coordinates: lat: 40.621872222222
lon: -115.47505555556
This cessation in the production of stelae was the most dramatic symptom of a general decline in the region at this time. This decline has been linked to the intrusion of peoples from the western highlands combined with the disastrous eruption of the Ilopango Volcano that severely affected the entire region. Early Classic.

Geographic entities mentioned:
surface_form: Ilopango Volcano
instance_of: Lake
countries: El Salvador
coordinates: lat: 13.66666667
lon: -89.05
At some Maya cities the first appearance of stelae corresponded with the foundation of dynastic rule. The standard form of the Maya stela incorporating art, calendrical dates and hieroglyphic text onto a royal monument only began to be erected in the Maya lowlands after 250 AD.

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
Rapper Lil Nas X released a music video for the Young Thug and Mason Ramsey remix of &quot;Old Town Road&quot; about the planned raid. Copycat events such as plans to storm a genealogical vault of the Church of Jesus Christ of Latter-day Saints, Loch Ness, the Bermuda Triangle, the US Capitol Building and the Vatican City's archives were also created.

Geographic entities mentioned:
surface_form: Loch Ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
For the only time in Farmer's career, Laurent Boutonnat directed the video and wrote its screenplay (usually, it is Farmer who composes the latter). It is a Requiem Publishing production which was shot for two days in August 1989 on the Lac de Grand-Lieu (Loire Atlantique, France), with a budget of about 30,000 euros. Moreover, it is the first of Farmer's videos to be in black and white.

Geographic entities mentioned:
surface_form: Lac de Grand-Lieu
instance_of: Lake
countries: France
coordinates: lat: 47.083333333333
lon: -1.6666666666667
Nipawin. Nipawin () is a town in Saskatchewan, Canada, on the Saskatchewan River portion of Tobin Lake. The town lies between Codette Lake, created by the Francois-Finlay Dam (built in 1986) and Tobin Lake, created by the E.B. Campbell Dam built in 1963, renamed from Squaw Rapids. The construction of Francois-Finlay Dam earned Nipawin the nickname the &quot;Town of Two Lakes&quot;.

Geographic entities mentioned:
surface_form: Codette Lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.2667
lon: -104.2838
Russian forces were also to guarantee the roads connecting Azerbaijan and Nakhchivan. Armenia–Azerbaijan border crisis (2021–2025). On 12 May, Azerbaijani troops crossed into internationally recognized Armenian territory, claiming the area around Lake Sev. Armenian Prime Minister, Nikol Pashinyan, attempted to appeal to the CSTO about the incursion.

Geographic entities mentioned:
surface_form: Lake Sev
instance_of: Lake
countries: Armenia
Azerbaijan
coordinates: lat: 39.598055555555554
lon: 46.23166666666667
It is north of the village of Skjolden in Luster and southwest of Bismo in Skjåk. The mountain is surrounded by several other notable mountains including Tundradalskyrkja to the east, Holåtindan to the southeast, Røykeskardhøi to the west, and Syrtbyttnosi to the northwest. The tall main peak is also called &quot;Store Tverrådalskyrkja&quot;.

Geographic entities mentioned:
surface_form: Tundradalskyrkja
instance_of: Mountain
countries: Norway
coordinates: lat: 61.7547
lon: 7.7525
surface_form: Holåtindan
instance_of: Mountain
countries: Norway
coordinates: lat: 61.750056111111
lon: 7.8833769444444
surface_form: Røykeskardhøi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.74138889
lon: 7.62916667
surface_form: Syrtbyttnosi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.76202
lon: 7.58102
Tverrådalskyrkja. Tverrådalskyrkja is a mountain on the border of Skjåk Municipality in Innlandet county and Luster Municipality in Vestland county, Norway. The tall mountain is located in the Breheimen mountains and inside the Breheimen National Park, just north of the large Harbardsbreen glacier. It is north of the village of Skjolden in Luster and southwest of Bismo in Skjåk.

Geographic entities mentioned:
surface_form: tverrådalskyrkja
instance_of: Mountain
countries: Norway
coordinates: lat: 61.744433333333
lon: 7.6865944444444
The mountain is surrounded by several other notable mountains including Tundradalskyrkja to the east, Holåtindan to the southeast, Røykeskardhøi to the west, and Syrtbyttnosi to the northwest. The tall main peak is also called &quot;Store Tverrådalskyrkja&quot;. About southwest of the main peak, there is a second peak at a height of, called &quot;Søre Tverrådalskyrkja&quot;.

Geographic entities mentioned:
surface_form: tverrådalskyrkja
instance_of: Mountain
countries: Norway
coordinates: lat: 61.744433333333
lon: 7.6865944444444
surface_form: store tverrådalskyrkja
instance_of: Mountain
countries: Norway
coordinates: lat: 61.744433333333
lon: 7.6865944444444
The tall main peak is also called &quot;Store Tverrådalskyrkja&quot;. About southwest of the main peak, there is a second peak at a height of, called &quot;Søre Tverrådalskyrkja&quot;. Tverrådalskyrkja can be reached from the Norwegian Mountain Touring Association cabin &quot;Sotasæter&quot;. Usual access to the peak is over the Fortundalsbreen glacier, then along the eastern ridge. Name.

Geographic entities mentioned:
surface_form: tverrådalskyrkja
instance_of: Mountain
countries: Norway
coordinates: lat: 61.744433333333
lon: 7.6865944444444
surface_form: tverrådalskyrkja
instance_of: Mountain
countries: Norway
coordinates: lat: 61.744433333333
lon: 7.6865944444444
A car accident in late 2001 involving several members of Mofro slowed things down for the band and it was not until 2004 until they released their next album Lochloosa. This album continued to deliver songs about where Grey grew up and the industrial progress that continues to plague the natural beauty of the areas around Lochloosa Lake and Orange Lake.

Geographic entities mentioned:
surface_form: Lochloosa Lake
instance_of: Lake
countries: United States
coordinates: lat: 29.5167
lon: -82.1206
In late August 1923, Brown disappeared from his home in Subiaco and did not return. Police and residents mounted a search of the surrounding area, and even employed a black tracker to assist them. Brown's body was found four days later, in bushland near Herdsman Lake. His throat was a cut and a razor found next to the body, leading the coroner to return a verdict of suicide.

Geographic entities mentioned:
surface_form: Herdsman Lake
instance_of: Lake
countries: Australia
coordinates: lat: -31.92
lon: 115.80694444444
Much of the water supply for Central California and Southern California is also derived from the Delta, via pumps located at the southern end of the Delta. The pumps deliver water for irrigation in the San Joaquin Valley and municipal water supply for Southern California. Geography.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
These are all surrounded by of levees that border of waterways. The southwestern side of the Delta lies at the foothills of the California Coast Ranges, while to the northwest sit the lower Montezuma Hills. Most of the Delta lies within Contra Costa, Sacramento, San Joaquin, Solano and Yolo Counties. The total human population of the Delta was 515,264 as of 2000.

Geographic entities mentioned:
surface_form: Montezuma Hills
instance_of: Landform
countries: United States
coordinates: lat: 38.1174
lon: -121.804
Staple foods included tule roots and pollen, acorns, wild fruits and seeds, fish and game. Europeans first entered the Delta region in 1772, when Spanish explorer Don Pedro Fages and missionary Juan Crespí observed the Delta from the summit of nearby Mount Diablo. For decades, the Delta was little utilized by the Spanish colonists.

Geographic entities mentioned:
surface_form: Mount Diablo
instance_of: Mountain
countries: United States
coordinates: lat: 37.881697781
lon: -121.914154997
Big Raven Formation. The Big Raven Formation is a stratigraphic unit of Quaternary age in northwestern British Columbia, Canada. It is the youngest and least voluminous geological formation of the Mount Edziza volcanic complex (MEVC); it overlies at least eight older formations of this volcanic complex.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
Alkali basalt and hawaiite are in the form of lava flows and small volcanic cones while trachyte of the Sheep Track Member is mainly in the form of volcanic ejecta which covers an area of about. The Big Raven Formation is widespread throughout the MEVC, occurring on or adjacent to the Arctic Lake, Big Raven and Kitsu plateaus.

Geographic entities mentioned:
surface_form: Arctic Lake
instance_of: Plateau
countries: Canada
coordinates: lat: 57.3
lon: -130.767
surface_form: Big Raven
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
surface_form: Kitsu
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
Two lava fields of the Big Raven Formation occur on the Big Raven Plateau which in total contain at least 22 separate vents that issued lava flows. At least four isolated Big Raven vents occur on the eastern flank of Mount Edziza and on the extreme northern slope of the Big Raven Plateau.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Another outlier of the Big Raven Formation overlies the Nido Formation east of Mount Edziza. Big Raven breccia on the plateau surface east of Mess Lake directly overlies trachyte of the Armadillo Formation. At the mouth of Tennaya Creek valley on the eastern side of the Mount Edziza volcanic complex, the Big Raven Formation overlies trachyte of the Kakiddi Formation. Age and lithology.

Geographic entities mentioned:
surface_form: Mess Lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.4667
lon: -130.883
Another outlier of the Big Raven Formation overlies the Nido Formation east of Mount Edziza. Big Raven breccia on the plateau surface east of Mess Lake directly overlies trachyte of the Armadillo Formation. At the mouth of Tennaya Creek valley on the eastern side of the Mount Edziza volcanic complex, the Big Raven Formation overlies trachyte of the Kakiddi Formation. Age and lithology.

Geographic entities mentioned:
surface_form: Tennaya Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.69966
lon: -130.42065
Alkali basalt and hawaiite are the main volcanic rocks comprising the Big Raven Formation, having erupted from at least 30 vents along the entire north–south trending axis of the MEVC. They are in the form of lava flows and pyroclastic cones which largely comprise two lava fields on the northern and western flanks of Mount Edziza and Ice Peak, respectively.

Geographic entities mentioned:
surface_form: Ice Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
The Triplex Cones issued lava that flowed to near the south shore of Buckley Lake more than to the northwest. Sidas Cone and Twin Cone are complex volcanic piles resulting from simultaneous, multi-vent lava fountaining. Both cones issued relatively thin clinkery-surfaced basalt flows that are sparsely porphyritic.

Geographic entities mentioned:
surface_form: Sidas Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.8589
lon: -130.628
Sidas Cone and Twin Cone are complex volcanic piles resulting from simultaneous, multi-vent lava fountaining. Both cones issued relatively thin clinkery-surfaced basalt flows that are sparsely porphyritic. Moraine Cone was the source of a lava flow that travelled northeast into Kakiddi Valley near its junction with the Klastline River.

Geographic entities mentioned:
surface_form: Kakiddi Valley
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
Moraine Cone was the source of a lava flow that travelled northeast into Kakiddi Valley near its junction with the Klastline River. The two youngest cinder cones in the Desolation Lava Field, Eve Cone and Williams Cone, produced basaltic lava that flowed to Buckley Lake and the Klastline River, respectively.

Geographic entities mentioned:
surface_form: Eve Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
surface_form: Williams Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
As a result, the surface details of most of the upper lava flows in this lava field remain obscured and the cones are mantled with Sheep Track pumice. The Snowshoe Lava Field contains three subglacial cones, Tennena Cone being the only one named. Tennena Cone consists of a pile of tuff breccia and pillow basalt and is one of the oldest cones in the Snowshoe Lava Field.

Geographic entities mentioned:
surface_form: Tennena Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.68416666666667
lon: -130.66222222222223
Their inner structures have been exposed by sufficient erosion, but they still retain their central craters and original conical form. One of these cones, Coffee Crater, was the source of a lava flow that extended to the southwest; the northern edge of the terminal lobe of this lava flow forms a prominent, escarpment. Three subaerial cones exist in the Snowshoe Lava Field, two of which are named.

Geographic entities mentioned:
surface_form: Coffee Crater
instance_of: Mountain
countries: Canada
coordinates: lat: 57.63
lon: -130.67
Three subaerial cones exist in the Snowshoe Lava Field, two of which are named. The largest subaerial cone, Cocoa Crater, produced a wide lava flow that travelled into upper Sezill Creek canyon. Keda Cone and an unnamed subaerial cone to the northeast issued the most voluminous lava in the Snowshoe Lava Field, having flowed westward where it engulfed an area more than wide and long.

Geographic entities mentioned:
surface_form: Cocoa Crater
instance_of: Mountain
countries: Canada
coordinates: lat: 57.65
lon: -130.7
surface_form: Sezill Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.69967
lon: -130.88724
Keda Cone and an unnamed subaerial cone to the northeast issued the most voluminous lava in the Snowshoe Lava Field, having flowed westward where it engulfed an area more than wide and long. This lava then continued to flow westward into upper Taweh Valley where it transformed into a relatively narrow flow that formerly extended to near Mess Creek.

Geographic entities mentioned:
surface_form: Taweh Valley
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
East slope centres. The heavily eroded eastern flank of Mount Edziza contains at least three satellitic centres of the Big Raven Formation. Cinder Cliff consists of thin, slaggy basalt flows that ponded against an ice dam in the upper part of Tenchen Valley. Tuff breccia and ash, as well as glacial and fluvial gravel, form mixed deposits at the base of Cinder Cliff.

Geographic entities mentioned:
surface_form: Tenchen Valley
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.76636
lon: -130.43724
Arctic Lake Plateau. Two isolated occurrences of the Big Raven Formation occur on the Arctic Lake Plateau, Nahta Cone near its northern edge being the southernmost vent of Big Raven age. This cone overlies a glacially-scoured limestone hill and contains a crater that is breached to the east.

Geographic entities mentioned:
surface_form: Nahta Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3083
lon: -130.821
Extending north and west of Nahta Cone are two tephra deposits, suggesting it was active twice during different wind directions. Northeast of Nahta Cone on the south flank of Kuno Peak in the Spectrum Range are the remains of a Big Raven pyroclastic cone.

Geographic entities mentioned:
surface_form: Kuno Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3763
lon: -130.7398
Lava flows from both cones travelled westward to the edge of the Mess Creek Escarpment where they most likely cascaded into Mess Creek valley, but no evidence of this phenomenon has been found on or below the escarpment. At the southern end of the Mess Lake Lava Field on the steep, south-facing side of Nagha Creek is the third separate vent called The Ash Pit.

Geographic entities mentioned:
surface_form: The Ash Pit
instance_of: Mountain
countries: Canada
coordinates: lat: 57.45
lon: -130.78
It lies in the La Paz Department, Ingavi Province, Guaqui Municipality. Quta Willk'i is situated north-west of the mountain Wanq'uni, north-east of Tanqa Tanqani and south-east of Qala Waxrani.

Geographic entities mentioned:
surface_form: Qala Waxrani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6244
lon: -68.8281
surface_form: qala waxrani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6244
lon: -68.8281
surface_form: wanq'uni
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6547
lon: -68.7931
surface_form: wanq'uni
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.78277778
lon: -65.67194444
Quta Willk'i. Quta Willk'i (Aymara &quot;quta&quot; lake, &quot;willk'i&quot; gap, &quot;lake gap&quot;, also spelled &quot;Kkota Willkki&quot;) is a mountain in the Chilla-Kimsa Chata mountain range in the Andes of Bolivia. It lies in the La Paz Department, Ingavi Province, Guaqui Municipality.

Geographic entities mentioned:
surface_form: quta willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6411
lon: -68.8058
surface_form: willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.39861111
lon: -69.02222222
Quta Willk'i. Quta Willk'i (Aymara &quot;quta&quot; lake, &quot;willk'i&quot; gap, &quot;lake gap&quot;, also spelled &quot;Kkota Willkki&quot;) is a mountain in the Chilla-Kimsa Chata mountain range in the Andes of Bolivia. It lies in the La Paz Department, Ingavi Province, Guaqui Municipality.

Geographic entities mentioned:
surface_form: quta willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6411
lon: -68.8058
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.1058
lon: -68.3858
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.1214
lon: -68.3297
surface_form: willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.39861111
lon: -69.02222222
surface_form: willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.39861111
lon: -69.02222222
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.71666667
lon: -68.7
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.10972222
lon: -67.66222222
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.88333333
lon: -68.85
There are usually about 50 graduate students studying at the Solar System School. Two thirds are from abroad from over 30 different countries. About 30 percent are women. History. The institute was founded by Walter Dieminger, who was head of the Luftwaffe test center at Rechlin at the Müritz from 1934 onwards. Erich Regener was cofounder.

Geographic entities mentioned:
surface_form: Müritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.416666666667
lon: 12.683333333333
Ehle (river). The Ehle is a river in Saxony-Anhalt, Germany. It is a right tributary of the Elbe, and approximately long.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Apalachee River (Georgia). The Apalachee River is a tributary of the Oconee River in the U.S. state of Georgia. It rises north of Lawrenceville in eastern Gwinnett County and flows southeast to join the Oconee River in Lake Oconee west of Greensboro. It is spanned by the Kilgore Mill Covered Bridge.

Geographic entities mentioned:
surface_form: Lake Oconee
instance_of: Lake
countries: United States
coordinates: lat: 33.35
lon: -83.157
Lake Marian. Lake Marian is an alpine lake at the southern end of the Darran Mountains in the Fiordland National Park in the South Island of New Zealand. The lake is located just above the treeline in a hanging valley leading northwest from the Hollyford Valley near The Divide pass. The valley is sheltered by steep snow-covered peaks of over on all sides apart from the entrance.

Geographic entities mentioned:
surface_form: Hollyford Valley
instance_of: Valley
countries: New Zealand
coordinates: lat: -44.727222222222
lon: 168.12927222222