Sarmila/GeoWiki-Features huggingface dataset:
He was buried on July 15/27, 1832 by the church in Kamenica (Valjevo), his endowment. Legacy. In the villages beneath the Medvednik is still taught the tale of the &quot;Church built by knez Jovan Simić Bobovac, but burned down by the Turks after the failure of the First Serbian Uprising (1804)&quot;, when the local people fled to the mountain.

Geographic entities mentioned:
surface_form: Medvednik
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.20917
lon: 19.63972
Pirogov Glacier. Pirogov Glacier (,) is a 5 km long and 1.5 km wide glacier situated south of Djerassi Glacier, west of the head of Mackenzie Glacier and northwest of Balanstra Glacier on Brabant Island in the Palmer Archipelago, Antarctica. It drains the south-southwest slopes of Mount Parry and flows westwards to enter Dallmann Bay south of Minot Point.

Geographic entities mentioned:
surface_form: Mount Parry
instance_of: Mountain
coordinates: lat: -64.25549333
lon: -62.40698
Before U.S. Route 101 was built through the Gaviota Pass, SR 154 was the main throughway to Santa Barbara and the tri city area including use as a stagecoach route in early years. After being replaced by US 101 as the primary route between the Santa Ynez Valley and Santa Barbara, SR 154 now serves as a scenic bypass. Route description.

Geographic entities mentioned:
surface_form: Santa Ynez Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.5473
lon: -119.858
Allegheny Plateau. The Allegheny Plateau () is a large dissected plateau area of the Appalachian Mountains in western and central New York, northern and western Pennsylvania, northern and western West Virginia, and eastern Ohio. It is divided into the unglaciated Allegheny Plateau and the glaciated Allegheny Plateau.

Geographic entities mentioned:
surface_form: glaciated Allegheny Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 41
lon: -81
It is divided into the unglaciated Allegheny Plateau and the glaciated Allegheny Plateau. The plateau extends southward into western West Virginia, eastern Kentucky, and Tennessee, where it is instead called the Cumberland Plateau. The plateau terminates in the east at the Allegheny Mountains, which are the highest ridges just west of the Allegheny Front.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
Absolute highest elevations in this area are often in the range of. By the Allegheny Front, however, elevations may reach well over, with relief of up to. Geology and physiography. The Allegheny Plateau is a physiographic section of the larger Appalachian Plateau province, which in turn is part of the larger Appalachian physiographic division.

Geographic entities mentioned:
surface_form: Appalachian Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 40
lon: -78
The township is part of Thunder Bay's Census Metropolitan Area, and consists of the communities of Amethyst Harbour, Ancliff, Bowker, Ishkibibble, Loon, Mackenzie, Navilus, Pass Lake, Pearl, Silver Harbour and Wild Goose. Serving today primarily as a rural bedroom community to Thunder Bay, Shuniah is also a popular cottaging locale with 40 kilometres of Lake Superior's northern shoreline.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Once they reached Askim, the Swedes encountered another Norwegian entrenchment a distance away, at Langnes, where another battle took place. Vegesack then advanced as far as Trøgstad and there captured about 200 Norwegians soldiers (the rest withdrew over the Glomma), on 11 August; the Swedes had thus became masters of the eastern side of the Glomma, south of Øyeren.

Geographic entities mentioned:
surface_form: Øyeren
instance_of: Lake
countries: Norway
coordinates: lat: 59.857222222222
lon: 11.163333333333
Legacy. Mount Austin on Hong Kong Island, Austin Road and Austin Avenue in Kowloon were named after him. The Austin station of the MTR was so-named due to its proximity to Austin Road West, and the naming may be more influenced by geographical convenience rather than any direct link to Austin himself.

Geographic entities mentioned:
surface_form: Mount Austin
instance_of: Mountain
countries: People's Republic of China
British Hong Kong
coordinates: lat: 22.275469444444
lon: 114.14382777778
It is situated in the Cusco Region, Chumbivilcas Province, Santo Tomás District. Sullu Sullu lies south of Sara Sara and northeast of Ikma.

Geographic entities mentioned:
surface_form: ikma
instance_of: Mountain
countries: Peru
coordinates: lat: -14.5822
lon: -72.46
Sullu Sullu. Sullu Sullu (Aymara &quot;sullu&quot; miscarried (fetus), Quechua &quot;sullu&quot; miscarriage; unborn fetus; key for doors or boxes, the reduplication indicates that there is a group or a complex of something, also spelled &quot;Sullo Sullo&quot;) is a mountain in the Wansu mountain range in the Andes of Peru, about high.

Geographic entities mentioned:
surface_form: sullu sullu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.5647
lon: -72.4481
The formation of the road itself was as minimal as the terrain allowed, with low side-cuttings and embankments as necessary. The actual construction and completion of the road is recorded in Cox's Journal. The journal indicates that three areas in particular required extensive cutting through rocky outcrops; at Linden to Woodford, Wentworth Falls and the descent at Mount York.

Geographic entities mentioned:
surface_form: Mount York
instance_of: Mountain
countries: Australia
coordinates: lat: -33.553
lon: 150.22
He played at two world championships, winning bronze with the New Zealand team in 1966. Playing for the Railways club in the Hutt Valley, Massey pitched his team to six national interclub titles between 1958 and 1967. During the same period he won eight national interprovincial titles representing Hutt Valley.

Geographic entities mentioned:
surface_form: Hutt Valley
instance_of: Valley
countries: New Zealand
coordinates: lat: -41.1657
lon: 174.973
Geography. Ellerslie lies along Maryland Route 35, north of Cumberland and is next to the Pennsylvania-Maryland state line. To the north, Pennsylvania Route 96 extends to Hyndman and to Bedford. The town is situated in the valley of Wills Creek, between the parallel ridges of Little Allegheny Mountain to the west and Wills Mountain to the east.

Geographic entities mentioned:
surface_form: Wills Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.845555555556
lon: -78.681666666667
History. Independence Creek shares the name of Independence Lake, which was named on Independence Day of 1852 or 1853 my the actress Lola Montez, who lived in nearby Grass Valley and for whom Mount Lola is named, although Augustus Moore claims to have named the lake on July 4, 1862. Watershed and Course.

Geographic entities mentioned:
surface_form: Mount Lola
instance_of: Mountain
countries: United States
coordinates: lat: 39.4331
lon: -120.365
Jefferson commissioned the Pike Expedition through Wilkinson, which was also to seek the headwaters of the Red River and to explore the west of the Louisiana Territory, along the Arkansas River. Departing from St. Louis in July 1806, the expedition recorded the discovery in November of what became called Pikes Peak, in present-day Colorado.

Geographic entities mentioned:
surface_form: Pikes Peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.840555555556
lon: -105.04416666667
The Earl and Virginia Young House, also known as the Young-Sartorette House, stands as a historic residence in Campbell, California. Constructed in 1928, it served as the home for Earl Young, a successful orchard farmer in the Santa Clara Valley, and his family. The house is historically significant in the Tudor Revival architectural style, which gained popularity in the mid-twentieth century.

Geographic entities mentioned:
surface_form: Santa Clara Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.366944444444
lon: -121.98388888889
The CDP is in eastern Blair County, along the southwestern edge of Catharine Township. It is in the valley of Township Run, which forms the boundary between Catharine and Frankstown Township. The small, steep valley is between Short Mountain to the east and the south end of Canoe Mountain to the west, and drains south to the Frankstown Branch of the Juniata River.

Geographic entities mentioned:
surface_form: Canoe Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.5417
lon: -78.2083
On the other hand, she led multiple research studies in different parts of the world: at the Kitt Peak National Observatory in Arizona, at the Skalnaté Pleso Observatory, and in Lomnický štít, Slovakia, the South African Astronomical Observatory in Cape Town, the Spanish National Observatory in Madrid and the Teide Observatory in Tenerife.

Geographic entities mentioned:
surface_form: Lomnický štít
instance_of: Mountain
countries: Slovakia
coordinates: lat: 49.2
lon: 20.212777777778
Punta Tersiva. Punta Tersiva (French: &quot;Pointe Tersive&quot;) (3,512m) is a mountain of the Graian Alps in Aosta Valley, north-western Italy. It is described as an &quot;elegant, pyramid shaped mountain&quot;. The mountain is a tough climb, and most of the famous peaks of the Alps are visible from its summit on a clear day, with Gran Paradiso especially visible.

Geographic entities mentioned:
surface_form: Gran Paradiso
instance_of: Mountain
countries: Italy
coordinates: lat: 45.533333333333
lon: 7.2666666666667
Punta Tersiva. Punta Tersiva (French: &quot;Pointe Tersive&quot;) (3,512m) is a mountain of the Graian Alps in Aosta Valley, north-western Italy. It is described as an &quot;elegant, pyramid shaped mountain&quot;. The mountain is a tough climb, and most of the famous peaks of the Alps are visible from its summit on a clear day, with Gran Paradiso especially visible.

Geographic entities mentioned:
surface_form: punta tersiva
instance_of: Mountain
countries: Italy
coordinates: lat: 45.6217
lon: 7.47528
Punta Tersiva. Punta Tersiva (French: &quot;Pointe Tersive&quot;) (3,512m) is a mountain of the Graian Alps in Aosta Valley, north-western Italy. It is described as an &quot;elegant, pyramid shaped mountain&quot;. The mountain is a tough climb, and most of the famous peaks of the Alps are visible from its summit on a clear day, with Gran Paradiso especially visible.

Geographic entities mentioned:
surface_form: punta tersiva
instance_of: Mountain
countries: Italy
coordinates: lat: 45.6217
lon: 7.47528
surface_form: pointe tersive
instance_of: Mountain
countries: Italy
coordinates: lat: 45.6217
lon: 7.47528
Lough Talt. Lough Talt () is a lake in the Ox Mountains of south County Sligo, Ireland. The lake is located between the villages of Tubbercurry and Bonniconlon on the R294 road. Lough Talt is part of the Lough Hoe Bog Special Area of Conservation, an area of montane bogland and oligotrophic lakes. Lough Talt is the largest of the lakes in the Lough Hoe Bog area.

Geographic entities mentioned:
surface_form: lough talt
instance_of: Lake
countries: Ireland
coordinates: lat: 54.08333333
lon: -8.925
The lake is located between the villages of Tubbercurry and Bonniconlon on the R294 road. Lough Talt is part of the Lough Hoe Bog Special Area of Conservation, an area of montane bogland and oligotrophic lakes. Lough Talt is the largest of the lakes in the Lough Hoe Bog area. It is a glacier lake and lies at above sea level and measures at its deepest point. Its area is about.

Geographic entities mentioned:
surface_form: lough talt
instance_of: Lake
countries: Ireland
coordinates: lat: 54.08333333
lon: -8.925
Lough Talt is the largest of the lakes in the Lough Hoe Bog area. It is a glacier lake and lies at above sea level and measures at its deepest point. Its area is about. The lake flows out to the Lough Talt River which eventually joins the River Moy. The lake has two crannogs (artificial islands). Natural history.

Geographic entities mentioned:
surface_form: lough talt
instance_of: Lake
countries: Ireland
coordinates: lat: 54.08333333
lon: -8.925
The lake has two crannogs (artificial islands). Natural history. Fish species in Lough Talt include brown trout, three-spined stickleback, perch, the threatened Arctic char and the critically endangered European eel. Brown trout are the dominant fish species. A population of the endangered white-clawed crayfish has also been reported.

Geographic entities mentioned:
surface_form: lough talt
instance_of: Lake
countries: Ireland
coordinates: lat: 54.08333333
lon: -8.925
Water supply. Lough Talt is the source of domestic treated water for a large percentage of the population in south County Sligo, including Tubbercurry and Ballymote., a multi-year project to upgrade the Lough Talt Water Treatment plant began. The objective is to regain a safe drinking water standard and end the boil water notices the communities had been subject to.

Geographic entities mentioned:
surface_form: lough talt
instance_of: Lake
countries: Ireland
coordinates: lat: 54.08333333
lon: -8.925
The first phase was a 1.5 mile section between the Mountain Top Historical Society property and DEC land at the end of Laurel House Road. In 2016, further improvements were completed allowing visitors to travel from Haines Falls Station to the South Lake Campground via the Rail Trail and the Escarpment Trail, with multiple views of Kaaterskill Falls accessible to the public.

Geographic entities mentioned:
surface_form: South Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.199130555556
lon: -74.041072222222
The village is between Dove Holes Quarry (to the north) and Tunstead Quarry (to the south), with other smaller quarries in the vicinity. It was built to house quarry workers and their families, but some of the original houses have now been demolished. The village has a club (Great Rocks Club), a playground and a primary school. Great Rocks Dale lies immediately south of the village. Railway.

Geographic entities mentioned:
surface_form: Great Rocks Dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.266
lon: -1.849
East Lake Sammamish Trail. The East Lake Sammamish Trail is an recreational rail trail in King County, Washington that runs along Lake Sammamish from Marymoor Park in Redmond, through Sammamish, to Gilman Boulevard in Issaquah. History. The trail had initially encountered fierce political resistance from nearby homeowners through whose property the former BNSF Railway right-of-way runs.

Geographic entities mentioned:
surface_form: Lake Sammamish
instance_of: Lake
countries: United States
coordinates: lat: 47.61638888888889
lon: -122.08944444444444
Mátraháza. Mátraháza is a resort area within the town of Gyöngyös in Heves County, Hungary, situated in the Mátra mountain range. Mátraháza has its own postal code, 3233, and is located 14.4 km from the center of Gyöngyös. The highest peak in Hungary, Kékes, is 3.7 km from Mátraháza. As of the 2022 census, the population of Mátraháza is 80. History.

Geographic entities mentioned:
surface_form: Kékes
instance_of: Mountain
countries: Hungary
coordinates: lat: 47.87222222222222
lon: 20.012777777777778
Between 1927 and 1930, the Mátra Association built the Kékesalja Hostel. The lung sanatorium and the road leading to Kékes were completed in 1932, and a ski slope was created from Kékes to the Kékesalja Hostel. The military resort was built in 1933. The Patrona Hungariae chapel was built in 1942, and its wooden relief door was created in 1999 by the sculptor István Hegedűs.

Geographic entities mentioned:
surface_form: Kékes
instance_of: Mountain
countries: Hungary
coordinates: lat: 47.87222222222222
lon: 20.012777777777778
Šipkovica Partisan Hospital. The Partisan Hospital is a former hospital and WWII historical site located on the mountain of Plačkovica near the village of Šipkovica, North Macedonia. Here, the wounded partisans were treated, during the Axis Spring Offensive in 1944. History.

Geographic entities mentioned:
surface_form: Plačkovica
instance_of: Mountain
countries: North Macedonia
coordinates: lat: 41.766666666667
lon: 22.533333333333
Immediately after the units of the Operative Headquarters in the region of the mountain Plačkovica left, the units of the 17th Bulgarian division while searching the area discovered a segment of the hospital, where 11 badly wounded partisans were found and only one survived. The doctors Gjorgi Kamčev and Strahil Panov worked in the hospital.

Geographic entities mentioned:
surface_form: Plačkovica
instance_of: Mountain
countries: North Macedonia
coordinates: lat: 41.766666666667
lon: 22.533333333333
Vicos. Vicos or Paccharuri (possibly from Ancash Quechua &quot;paqtsa&quot; waterfall, &quot;ruri&quot; inside; valley or little river) is a high mountain in the Cordillera Blanca in the Andes of Peru. It is situated in the Ancash Region, Carhuaz Province, Marcara District. Paccharuri lies in the Huascarán National Park, southwest of Copa and southeast of Lake Lejiacocha.

Geographic entities mentioned:
surface_form: Lake Lejiacocha
instance_of: Lake
countries: Peru
coordinates: lat: -9.28583333
lon: -77.50555556
surface_form: copa
instance_of: Mountain
countries: Peru
coordinates: lat: -9.2666666666667
lon: -77.516666666667
surface_form: huascarán
instance_of: Mountain
countries: Peru
coordinates: lat: -9.1166666666667
lon: -77.6
surface_form: lejiacocha
instance_of: Lake
countries: Peru
coordinates: lat: -9.28583333
lon: -77.50555556
surface_form: lake lejiacocha
instance_of: Lake
countries: Peru
coordinates: lat: -9.28583333
lon: -77.50555556
Vicos. Vicos or Paccharuri (possibly from Ancash Quechua &quot;paqtsa&quot; waterfall, &quot;ruri&quot; inside; valley or little river) is a high mountain in the Cordillera Blanca in the Andes of Peru. It is situated in the Ancash Region, Carhuaz Province, Marcara District. Paccharuri lies in the Huascarán National Park, southwest of Copa and southeast of Lake Lejiacocha.

Geographic entities mentioned:
surface_form: vicos
instance_of: Mountain
countries: Peru
coordinates: lat: -9.29278
lon: -77.4869
Vicos. Vicos or Paccharuri (possibly from Ancash Quechua &quot;paqtsa&quot; waterfall, &quot;ruri&quot; inside; valley or little river) is a high mountain in the Cordillera Blanca in the Andes of Peru. It is situated in the Ancash Region, Carhuaz Province, Marcara District. Paccharuri lies in the Huascarán National Park, southwest of Copa and southeast of Lake Lejiacocha.

Geographic entities mentioned:
surface_form: vicos
instance_of: Mountain
countries: Peru
coordinates: lat: -9.29278
lon: -77.4869
surface_form: paccharuri
instance_of: Mountain
countries: Peru
coordinates: lat: -9.29278
lon: -77.4869
Den. The rancho stretched along the Gaviota Coast to the northwest of today's city of Santa Barbara, from Fairview Avenue in Goleta (at that time in the middle of Goleta Slough) to the southeastern boundary of today's El Capitan State Beach. A was bought by Colin Powys Campbell in 1919.

Geographic entities mentioned:
surface_form: Goleta Slough
instance_of: Landform
countries: United States
coordinates: lat: 34.4238
lon: -119.847
It occurs in the Amazon Basin, in the drainage basin of the Orinoco, in the entire river basin of the Río de la Plata, the Río Paraná and the Río Uruguay, in the coastal rivers of the Guyanas, on the islands of Trinidad and Tobago, in the coastal rivers of northeastern Brazil and in the lagoons Lagoa dos Patos and Lagoa Mirim in the south of Brazil. Characteristics.

Geographic entities mentioned:
surface_form: Lagoa dos Patos
instance_of: Lake
countries: Brazil
coordinates: lat: -31.15
lon: -51.39
Just, with a Canadian woman whose identity is unknown. Just and Annie had three children: John H., Mary H. and Alvah L. In June 1902, Dr. Just purchased two building lots in Selkirk Beach (on the shore of Lake Ontario – not to be confused with the Selkirk near Albany) from Edmund Brown to build a summer cottage. No construction was done, and the lots were sold a short time later to Edwin M.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Weyerberg. The Weyerberg is a sandy geest island, high, in the Teufelsmoor (&quot;Devil's Bog&quot;) in Northern Germany. It is located near its main settlement of Worpswede in the district of Osterholz in Lower Saxony. Its name means something like 'wooded hill'. It probably emerged at the end of the ice age, when meltwaters deposited sand around its clay core.

Geographic entities mentioned:
surface_form: weyerberg
instance_of: Mountain
countries: Germany
coordinates: lat: 53.2161
lon: 8.92361
In 1218 Worpswede was first mentioned in the records because the eight farms there were tithing to Osterholz Abbey. Several landmarks are located on the Weyerberg, such as the Cheese Dome House after designs by Bruno Taut, the Lower Saxony Stone by Bernhard Hoetger, and the Zion's Church. Painters of Worpswede's artists' colony often chose the Weyerberg as their scene or subject.

Geographic entities mentioned:
surface_form: weyerberg
instance_of: Mountain
countries: Germany
coordinates: lat: 53.2161
lon: 8.92361
Painters of Worpswede's artists' colony often chose the Weyerberg as their scene or subject. In 1957 the &quot;Stiftung Worpswede&quot; was founded that sought through land purchase to prevent further sand quarrying on the Weyerberg.

Geographic entities mentioned:
surface_form: weyerberg
instance_of: Mountain
countries: Germany
coordinates: lat: 53.2161
lon: 8.92361
The Snow Towers is a glaciated mountain summit located in the Boundary Ranges of the Coast Mountains, in the U.S. state of Alaska. The two peaks, 0.1 mi apart, are situated at the apex of the Taku and Herbert Glaciers near the western edge of the Juneau Icefield, north of Juneau, southwest of Snowpatch Crag, and northeast of Mount Ernest Gruening, on land managed by Tongass National Forest.

Geographic entities mentioned:
surface_form: Mount Ernest Gruening
instance_of: Mountain
countries: United States
coordinates: lat: 58.5686
lon: -134.6544
Orco. The Orco (, that is lit. &quot;Water of gold&quot;;) is an Italian river. It originates in the Piedmontese slopes of Gran Paradiso and after about reaches the Po river near Chivasso, in the Metropolitan City of Turin.

Geographic entities mentioned:
surface_form: Gran Paradiso
instance_of: Mountain
countries: Italy
coordinates: lat: 45.533333333333
lon: 7.2666666666667
Hansenbreen. Hansenbreen () is a glacier long, flowing north along the west side of Mount Nils Larsen in the Sør Rondane Mountains of Antarctica. It was roughly mapped by Norwegian cartographers from air photos taken by the Lars Christensen Expedition, 1936–37, and remapped by them in greater detail in 1957 from air photos taken by U.S. Navy Operation Highjump, 1946–47.

Geographic entities mentioned:
surface_form: Mount Nils Larsen
instance_of: Mountain
coordinates: lat: -72.2333
lon: 23.1
The present fountain is not on the same location as the old ones and is not identical in terms of architecture, but kept many elements from the old projects. Today located in front of the &quot;Zora&quot; palace (which hosts the Servantes Institute), it was sculptured by Aleksandar Deroko from the white Venčac marble, and is described as the &quot;monument to the old fountain&quot;.

Geographic entities mentioned:
surface_form: white Venčac marble
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.262777777778
lon: 20.592777777778
In 1987 there was a major reconstruction of Knez Mihailova and its transformation into the pedestrian zone. After six months of construction works, the street was open on 20 October 1987. It was paved with the black granite slabs from Jablanica, while a drinking fountain, made of white marble from Venčac, was erected in memory of former Delijska fountain which was further down the street.

Geographic entities mentioned:
surface_form: Venčac
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.262777777778
lon: 20.592777777778
&quot;Ocotea pachypoda&quot; is a species of evergreen tree in the genus &quot;Ocotea&quot; of the family Lauraceae. It is endemic to Ecuador. Its natural habitat is subtropical or tropical moist montane forests. It is thought that this species is most threatened by colonization, deforestation, and mining. It is known from two collections, both of which were taken from the Cotacachi Volcano.

Geographic entities mentioned:
surface_form: Cotacachi Volcano
instance_of: Mountain
countries: Ecuador
coordinates: lat: 0.3608333333333333
lon: -78.34916666666666
After that major work, De Rosen continued with his religious art in Poland and abroad, among others he painted murals at the Kahlenberg's Chapel of Saint Joseph near Vienna, Austria, and at the request of Pius XI two murals at papal residence at Castel Gandolfo. During the 1930s, De Rosen taught at the Lwów Politechnic University (Lviv Polytechnic).

Geographic entities mentioned:
surface_form: Kahlenberg
instance_of: Mountain
countries: Austria
coordinates: lat: 48.2761
lon: 16.3333
Mary Magdalene, Lviv. Work. Among his decorations and paintings are: chapel in the Theological Seminary of Lviv (1929–30), chapel of King Jan Sobieski at Kahlenberg near Vienna (1930); pictures in the art museums of Lviv, Lublin and Bydgoszcz. Pope Pius XI commissioned De Rosen to paint murals in his private chapel at Castel Gandolfo.

Geographic entities mentioned:
surface_form: Kahlenberg
instance_of: Mountain
countries: Austria
coordinates: lat: 48.2761
lon: 16.3333
Directed by Andy Keen and produced by Keen, Harmer, Bryan Bean and Patrick Sambrook, it was released theatrically in 2006. In June 2005, Harmer launched a tour, called I Love the Escarpment, across southern Ontario to promote Protecting Escarpment Rural Land (PERL), a conservation group she cofounded to battle a proposed quarry development on the Niagara Escarpment near her hometown of Burlington.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
For skillful organization of battle and control in battle, and also for displaying courage and valor, Colonel Parfyonov is deserving of the state award of the Order of the Red Banner. The division assisted in the breakthrough of fortified defenses between Lakes Velence and Balaton on 13 March, after which it pursued the retreating German troops.

Geographic entities mentioned:
surface_form: Lakes Velence
instance_of: Lake
countries: Hungary
coordinates: lat: 47.208333333333
lon: 18.6
surface_form: Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
Minimal impact was reported. The storm produced moderate to heavy rainfall over parts of the Florida Peninsula, peaking at near Deland. Minor road washouts were reported in Lee County. Rainfall along the lower Kissimmee River and the Lake Okeechobee basin caused some pastures and flood plain areas to be inundated by water. Lake Kissimmee rose in height due to precipitation.

Geographic entities mentioned:
surface_form: Lake Okeechobee
instance_of: Lake
countries: United States
coordinates: lat: 26.933333333333
lon: -80.8
Minor road washouts were reported in Lee County. Rainfall along the lower Kissimmee River and the Lake Okeechobee basin caused some pastures and flood plain areas to be inundated by water. Lake Kissimmee rose in height due to precipitation. Jenny's remnants later contributed to the development of heavy rains in southern Louisiana. Hurricane Kara.

Geographic entities mentioned:
surface_form: Lake Kissimmee
instance_of: Lake
countries: United States
coordinates: lat: 27.902777777778
lon: -81.272222222222
Vuontisjärvi. Vuontisjärvi (;) is a small lake and a village located in Finnish Lapland. It belongs to Kemijoki main catchment area. The area of the lake was reduced greatly in 1861. During the spring flood the waters escaped through a ditch dug by a local man, and a new river formed. The new water level is six metres below the original.

Geographic entities mentioned:
surface_form: vuontisjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 68.435267
lon: 23.9879782
Nine Peaks. Nine Peaks is a mountain featuring numerous peaks on Vancouver Island, British Columbia, Canada, located northeast of Tofino and southeast of Big Interior Mountain. History. Although there was significant mining activity in the area of Della Lake and Big Interior Mountain prior to the 1950s, no record was made of any ascent of Nine Peaks.

Geographic entities mentioned:
surface_form: Big Interior Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.4606
lon: -125.574
History. Although there was significant mining activity in the area of Della Lake and Big Interior Mountain prior to the 1950s, no record was made of any ascent of Nine Peaks. The first recorded ascent was by the Syd Watt's Alpine Club of Canada party in July 1955. Access. 1. From the base of Della Falls, follow a faint route with bits of flagging up the left (south) side of the falls.

Geographic entities mentioned:
surface_form: Big Interior Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.4606
lon: -125.574
Access. 1. From the base of Della Falls, follow a faint route with bits of flagging up the left (south) side of the falls. The route is steep and mossy, requiring bush and branch climbing. 2. From Bedwell Lake, ascend Big Interior Mountain, cross over to its south summit (Marjorie's Load), and descend to the pass west of Della Lake.

Geographic entities mentioned:
surface_form: Big Interior Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.4606
lon: -125.574
The western side of the glacier contains a small possibly drained ice-marginal lake. Twin Glacier surrounds the northwestern base of Hoodoo Mountain and is the largest of the two valley glaciers. It is the source of the Twin River which also flows south into the Iskut River. Several changes have taken place at this double-lobed glacier since the 1920s.

Geographic entities mentioned:
surface_form: Twin River
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.72361111
lon: -131.21166667
Background. Hoodoo Mountain is part of the Northern Cordilleran Volcanic Province (NCVP), a broad area of shield volcanoes, lava domes, cinder cones and stratovolcanoes extending from northwestern British Columbia northwards through Yukon into easternmost Alaska.

Geographic entities mentioned:
surface_form: Northern Cordilleran Volcanic Province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
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
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
Hoodoo Mountain is part of a subdivision of the NCVP called the Stikine Subprovince. This subprovince, confined to the Stikine region of northwestern British Columbia, includes three other volcanic centres: Heart Peaks, Level Mountain and Mount Edziza. The four volcanic centres differ petrologically and/or volumetrically from the rest of the NCVP.

Geographic entities mentioned:
surface_form: Heart Peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The highest of the four complexes is Mount Edziza at, followed by Level Mountain at, Heart Peaks at and Hoodoo Mountain at. Hoodoo Mountain is one of ten volcanoes composing the Iskut volcanic field. This is a group of NCVP volcanoes scattered along the Iskut River and its main tributaries.

Geographic entities mentioned:
surface_form: Iskut volcanic field
instance_of: Mountain
countries: Canada
coordinates: lat: 56.5833
lon: -130.55
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
All of these volcanoes were active in the last 150,000 years; the latest eruption occurred from The Volcano about 150 years ago. The remaining Iskut volcanoes are Cinder Mountain, Little Bear Mountain and the Cone Glacier, Iskut Canyon, Second Canyon, Snippaker Creek, King Creek and Tom MacKay Creek cones. Structure. Hoodoo Mountain is one of the largest peralkaline volcanoes in the NCVP.

Geographic entities mentioned:
surface_form: Cinder Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.57
lon: -130.61
surface_form: Little Bear Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.8
lon: -131.3
surface_form: Second Canyon
instance_of: Mountain
countries: Canada
coordinates: lat: 56.41
lon: -130.72
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: bear
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.2833
lon: -126.967
Hoodoo Mountain. Hoodoo Mountain, sometimes referred to as Hoodoo Volcano, is a potentially active stratovolcano in the Northern Interior of British Columbia, Canada. It is located northeast of the Alaska–British Columbia border on the north side of the Iskut River opposite of the mouth of the Craig River.

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
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
Hoodoo Mountain. Hoodoo Mountain, sometimes referred to as Hoodoo Volcano, is a potentially active stratovolcano in the Northern Interior of British Columbia, Canada. It is located northeast of the Alaska–British Columbia border on the north side of the Iskut River opposite of the mouth of the Craig River.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
As a result, a limited number of mammals live around Hoodoo Mountain. Trees of the pine and willow families form forests in the regional river valleys and on the lower slopes of the volcano. They compose one of many ecoregions that occur throughout British Columbia. Due to its remoteness, Hoodoo Mountain can only be accessed by air, by water or by trekking great distances on foot.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Biogeography. Hoodoo Mountain lies within the Boundary Ranges Ecoregion, a mountainous region of the Coast Mountains in southeastern Alaska and northwestern British Columbia characterized by rugged, largely ice-capped mountains of granitic and metamorphic rocks. Mountain hemlock, western hemlock and Sitka spruce form forests on valley bottoms and lower valley slopes.

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
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
Climate. Hoodoo Mountain has a maritime glacial climate that is intermediate between fully coastal maritime and continental climates. Moist air from the Pacific Ocean brings intense precipitation over the region while simultaneously allowing cold Arctic air to pass down through the Portland Canal into the Dixon Entrance where it flows into British Columbia's North Coast.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Intruding the basement rocks are 1.8-million-year-old trachyandesite dikes, which represent the earliest known manifestations of Quaternary magmatism in the Iskut region. Hoodoo Mountain has been described as &quot;one of the most magnificent and interesting mountains in northern British Columbia&quot;.

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
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
These magmas were phonolitic and trachytic in composition, having possibly evolved from differentiation of alkali basaltic melts in the mid-crust. Several tephra layers in the Bob Quinn Lake, Dease Lake and Finlay River areas of northern British Columbia may have originated from Hoodoo Mountain. Eruptive periods.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: dease lake
instance_of: Lake
countries: Canada
coordinates: lat: 58.63502
lon: -130.03761
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
Personnel involved in the 1997 expedition were Catherine Hickson and Mark Stasiuk of the GSC, Jim Nicholls of the University of Calgary, Jeff Schmok and Guy Cross of Golder Associates, Alison Rust, Ben Edwards and Kelly Russell of the University of British Columbia, and Trevor Page of Lancaster University. By 2002, Hoodoo Mountain was no longer the least studied volcano of the Stikine Subprovince.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
However, this eruptive period is not known to have produced any pyroclastic deposits or tephras. Therefore other possible sources have been considered, including Level Mountain, Heart Peaks and the Mount Edziza volcanic complex. A thick trachytic tephra layer of unknown origin occurs in sediments at Bob Quinn Lake northeast of Hoodoo Mountain.

Geographic entities mentioned:
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The four volcanic centres differ petrologically and/or volumetrically from the rest of the NCVP. Heart Peaks, Level Mountain and Mount Edziza are the largest NCVP centres by volume, the latter two of which have experienced volcanism for a much longer timespan than any other NCVP centre.

Geographic entities mentioned:
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Hoodoo Mountain, Level Mountain and Mount Edziza are the only NCVP centres that contain volcanic rocks of both mafic and intermediate to felsic composition. The highest of the four complexes is Mount Edziza at, followed by Level Mountain at, Heart Peaks at and Hoodoo Mountain at. Hoodoo Mountain is one of ten volcanoes composing the Iskut volcanic field.

Geographic entities mentioned:
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
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surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
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surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
Tephra layers. Hoodoo Mountain is a possible source of the Finlay tephras. These are two thick phonolitic to trachytic tephra layers in the Dease Lake and Finlay River areas. Radiocarbon dating of terrestrial plant macrofossils directly overlying the youngest tephra layer suggest an early Holocene age for this volcanic material.

Geographic entities mentioned:
surface_form: dease lake
instance_of: Lake
countries: Canada
coordinates: lat: 58.63502
lon: -130.03761
Several changes have taken place at this double-lobed glacier since the 1920s. Its terminus has retreated about, having formerly flowed around both sides of a north–south trending ridge. A small moraine-dammed lake lies along the southwestern margin of Twin Glacier. Hoodoo Glacier and Twin Glacier are separated by a ridgeline extending north of Hoodoo Mountain.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: twin
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.72361111
lon: -131.21166667
These rocks were deposited by volcanic eruptions from 20 million years ago to as recently as a few hundred years ago. The cause of volcanic activity in the Northern Cordilleran Volcanic Province is thought to be due to rifting of the North American Cordillera driven by changes in relative plate motion between the North American and Pacific plates.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
Extending from the northwestern side of Hoodoo Mountain is the Northwest Flow, a lava flow with well-preserved levees. Lava channels up to wide occur throughout the flow. The Southwest Flow is a large lava flow on the southwestern side of Hoodoo Mountain that appears to have issued from a poorly formed cinder cone. Volcanic history.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9717
lon: -123.007
surface_form: mountain
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countries: Canada
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countries: Canada
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instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
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Heart Peaks, Level Mountain and Mount Edziza are the largest NCVP centres by volume, the latter two of which have experienced volcanism for a much longer timespan than any other NCVP centre. Hoodoo Mountain, Level Mountain and Mount Edziza are the only NCVP centres that contain volcanic rocks of both mafic and intermediate to felsic composition.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
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countries: Canada
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countries: Canada
coordinates: lat: 51.4677778
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countries: Canada
coordinates: lat: 51.4677778
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instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
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Hoodoo Mountain. Hoodoo Mountain, sometimes referred to as Hoodoo Volcano, is a potentially active stratovolcano in the Northern Interior of British Columbia, Canada. It is located northeast of the Alaska–British Columbia border on the north side of the Iskut River opposite of the mouth of the Craig River.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
It is located northeast of the Alaska–British Columbia border on the north side of the Iskut River opposite of the mouth of the Craig River. With a summit elevation of and a topographic prominence of, Hoodoo Mountain is one of many prominent peaks within the Boundary Ranges of the Coast Mountains. Its flat-topped summit is covered by an ice cap more than thick and at least in diameter.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
Its flat-topped summit is covered by an ice cap more than thick and at least in diameter. Two valley glaciers surrounding the northwestern and northeastern sides of the mountain have retreated significantly over the last hundred years. They both originate from a large icefield to the north and are the sources of two meltwater streams.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
They both originate from a large icefield to the north and are the sources of two meltwater streams. These streams flow along the western and eastern sides of the volcano before draining into the Iskut River. Much of Hoodoo Mountain was formed beneath glacial ice and it has been overlain by glaciers or an ice cap throughout much of its history.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
Most of these eruptive periods were characterized by steady flows of lava, but at least one period of explosive activity occurred as indicated by the presence of pyroclastic rocks. The latest eruptive period began about 10,000 years ago with the eruption of extensive lava flows that cover the north–central, northwestern and southeastern mountain slopes.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
A lava flow covering the southwestern slope may have been produced by a more recent eruption within the last couple of hundred years. Although no historical eruptions are known at Hoodoo Mountain, there have been periods of seismic activity since at least the mid-1980s, indicating possible future eruptions and volcanic hazards.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444