Sarmila/GeoWiki-Features huggingface dataset:
Big Sur and Monterey. Varda exhibited his work in London and Paris before leaving for New York in 1939, where his work was exhibited at the Neumann-Willard Gallery. In 1940 he moved to Anderson Creek, in Big Sur, California, and after that to Monterey, about forty miles north of Big Sur. In late 1943, he persuaded the writer Henry Miller to move to Big Sur.

Geographic entities mentioned:
surface_form: Anderson Creek
instance_of: Valley
countries: United States
coordinates: lat: 36.1567
lon: -121.6652
It was opened as mixed gauge in November 1867. An opening bridge across the River Parrett was commissioned in March 1871. A coal wharf had long existed at Dunball where coal was imported from South Wales and despatched to destinations in Devon. The B&ER extended the primitive wharf there and made a mixed gauge branch to it which opened in November 1869.

Geographic entities mentioned:
surface_form: River Parrett
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 51.2292
lon: -3.00861
It is a Listed Building grade II. The line then runs south across the Somerset Levels. At Bridgwater, a retractable or Telescopic Bridge was built in 1871 to the design of Sir Francis Fox. It carried a short industrial branch line over the River Parrett to the docks, but the bridge had to be movable, to allow boats to proceed upriver.

Geographic entities mentioned:
surface_form: River Parrett
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 51.2292
lon: -3.00861
Towns including Mangakino, Tūrangi, Twizel and Otematata were originally founded for workers constructing hydroelectric schemes, and their families. The hydroelectric reservoirs of Lake Ruataniwha and Lake Karapiro are world-class rowing venues, with the latter having hosted the 1978 and the 2010 World Rowing Championships. Other schemes have shaped political New Zealand.

Geographic entities mentioned:
surface_form: Lake Ruataniwha
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.281
lon: 170.071
surface_form: Lake Karapiro
instance_of: Lake
countries: New Zealand
coordinates: lat: -37.943167
lon: 175.560833
The HVDC Inter-Island scheme is New Zealand's only high voltage direct current (HVDC) system, and links the North and South Island grids together. The link connects the South Island converter station at the Benmore Dam in southern Canterbury with the North Island converter station at Haywards substation in the Hutt Valley via of overhead bipolar HVDC lines and submarine cables across Cook Strait.

Geographic entities mentioned:
surface_form: Hutt Valley
instance_of: Valley
countries: New Zealand
coordinates: lat: -41.1657
lon: 174.973
The Prussian Ministry of Justice tried to solve the rivalry by assigning to Schwietz the executions in the eastern part of Prussia, to Engelhardt the executions in the western part, divided by the Elbe river. Engelhardt soon went bankrupt, since the authorities in Hanover refused to employ him and he spent too much of his money for alcohol.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Biography. Mary Mead was born in Jackson, Wyoming to Clifford Hansen (1912–2009) and Martha Close (1914–2011). She grew up on her family's ranch in Jackson Hole. She graduated from the University of Wyoming with a bachelor of arts in history and a minor in mathematics in 1957. She was a teacher in Pinedale from 1957 to 1958.

Geographic entities mentioned:
surface_form: Jackson Hole
instance_of: Valley
countries: United States
coordinates: lat: 43.516666666667
lon: -110.83333333333
The municipal population was estimated at 134,000 in 2008. Geography. Bou-Saada is located in the southwest of the Hodna region in the Hauts Plateaux, at the feet of the Ouled Naïl Range of the Saharan Atlas. Bou-Saada has traditionally been an important market place producing and selling jewelry, metalwork, carpets and bousaadi knives. There is also a textile mill in town.

Geographic entities mentioned:
surface_form: Hauts Plateaux
instance_of: Plateau
countries: Algeria
coordinates: lat: 34.01861111
lon: 0.08527778
Sheriff Mountain. Sheriff Mountain is a summit in Beaverhead County, Montana, in the United States. With an elevation of, Sheriff Mountain is the 284th highest summit in the state of Montana.

Geographic entities mentioned:
surface_form: sheriff mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.610833333333
lon: -112.93361111111
The story also earned an Emmy Award nomination for &quot;Feature News Report - Serious Feature&quot; at the Northwest Emmy Awards in 2013. On September 15, 2013, KHQ aired his feature report on two brothers who climbed Sloan Peak 40 years after their father vanished from the same mountain, called &quot;The Climb for Closure&quot;.

Geographic entities mentioned:
surface_form: Sloan Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.0413767
lon: -121.3402434
The Kaljina is a river in the central-northeastern part of Bosnia and Herzegovina, municipality of Sokolac. The source of the river is on Ozren Sarajevski, in the area of &quot;Vrela&quot; near Ozren village, while the majority of its course runs across Nišići karst plateau, where the river passes through a village with a same name, Kaljina, which is the largest settlement on its course.

Geographic entities mentioned:
surface_form: Ozren Sarajevski
instance_of: Mountain
Plateau
countries: Bosnia and Herzegovina
coordinates: lat: 43.933627777778
lon: 18.450547222222
After about 26 kilometers of scenic flow from source to confluence, through the pristine nature of the plateau, the Kaljina meets Bioštica near the town of Olovo. The Krivaja basin is known for an abundant fish fauna, rich in species, some of which are critically endangered, such as Danube Salmon (or Danube Taimen) &quot;(Hucho hucho)&quot;.

Geographic entities mentioned:
surface_form: Bioštica
instance_of: Watercourse
countries: Bosnia and Herzegovina
coordinates: lat: 43.9906137
lon: 18.7795338
The Kaljina, its parent the Bioštica, and the Stupčanica are the main source of the Krivaja waters, and all three are unspoiled in sense of water quality, their hydromorphology, natural surroundings and river biodiversity.

Geographic entities mentioned:
surface_form: Bioštica
instance_of: Watercourse
countries: Bosnia and Herzegovina
coordinates: lat: 43.9906137
lon: 18.7795338
North Holland is a broad peninsula for the most part, located between the North Sea, the Wadden Sea, the IJsselmeer, and the Markermeer. More than half of the province consists of reclaimed polder land situated below sea level. The West Frisian islands of Noorderhaaks and Texel are also part of the province.

Geographic entities mentioned:
surface_form: Markermeer
instance_of: Lake
countries: Netherlands
coordinates: lat: 52.566666666667
lon: 5.2166666666667
Skorvebradden. Skorvebradden () is a heavily crevassed ice slope extending about 13 miles east-southeast from Hamarskorvene Bluff, in the Muhlig-Hofmann Mountains, Queen Maud Land. Mapped by Norwegian cartographers from surveys and air photos by the Norwegian Antarctic Expedition (1956–60) and named Skorvebradden.

Geographic entities mentioned:
surface_form: hofmann
instance_of: Mountain
coordinates: lat: -82.6667
lon: 160.6
surface_form: skorvebradden
instance_of: Landform
coordinates: lat: -72.1167
lon: 5.55
Skorvebradden. Skorvebradden () is a heavily crevassed ice slope extending about 13 miles east-southeast from Hamarskorvene Bluff, in the Muhlig-Hofmann Mountains, Queen Maud Land. Mapped by Norwegian cartographers from surveys and air photos by the Norwegian Antarctic Expedition (1956–60) and named Skorvebradden.

Geographic entities mentioned:
surface_form: skorvebradden
instance_of: Landform
coordinates: lat: -72.1167
lon: 5.55
In 1653, when Prince Aurangzeb was appointed the viceroy of the Deccan for the second time, he made Fatehnagar his capital and called it Aurangabad and built the fort Killa Arrak near the mosque, upon which the mosque felt in the boundaries of the fort walls expanding from Delhi Gate to Mecca Gate.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
The Wari are noted for their stone architecture and sculpture accomplishments, but their greatest proficiency was ceramic. The Wari produced magnificent large ceramics, many of which depicted images of the Staff God, an important deity in the Andes which during the Wari period had become specifically associated with the Lake Titicaca region on the modern Peru-Bolivia border.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
On that same day the &quot;Sheadle&quot; met up with another downbound freighter, the Canadian steamer James Carruthers off the shores of Georgian Bay. The &quot;Carruthers&quot; entered Lake Huron with the &quot;Sheadle&quot; behind her. They could see the lights of the &quot;Carruthers&quot; until she made a port turn to keep her south of Great Duck Island and on a strait line to Georgian Bay.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Command at sea, 1892–1909. Purey-Cust's first command was, based in Australia from 1892. He was promoted to Commander in 1894. While surveying in the New Hebrides, now Vanuatu, there was a major volcanic eruption on the island of Ambrym. Survey work was interrupted, and Dart helped to provide assistance to the islanders. Purey-Cust published an account of his observations of the eruption.

Geographic entities mentioned:
surface_form: Ambrym
instance_of: Mountain
countries: Vanuatu
coordinates: lat: -16.333333333333
lon: 168.33333333333
Rönne (river). The Rönne (Swedish: &quot;Rönne å&quot;) is a river in Scania, Sweden with a length of 83 kilometers. The Rönne flows from Ringsjön and opens into Skälderviken in Ängelholm.

Geographic entities mentioned:
surface_form: Ringsjön
instance_of: Group of lakes
countries: Sweden
coordinates: lat: 55.872222222222
lon: 13.518611111111
Shark Tooth Mountain (British Columbia). Shark Tooth Mountain, officially named in 1954, is also known as The Sharktooth or Sharp Tooth Mountain. It is a mountain in the East Kootenay region of southeastern British Columbia, Canada, southwest of Whiteswan Lake. Presumably, the name is related to the profile of the peak.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: shark tooth mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0736
lon: -115.58
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Shark Tooth Mountain (British Columbia). Shark Tooth Mountain, officially named in 1954, is also known as The Sharktooth or Sharp Tooth Mountain. It is a mountain in the East Kootenay region of southeastern British Columbia, Canada, southwest of Whiteswan Lake. Presumably, the name is related to the profile of the peak.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: kootenay
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Presumably, the name is related to the profile of the peak. It sits to the southwest of Whiteswan Lake Provincial Park, with Lussier Hot Springs and Ram Creek Hot Springs nearby, and is part of the Kootenay Ranges subdivision of the Canadian Rockies in Western Alberta and most of British Columbia.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: kootenay
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
Shark Tooth Mountain (British Columbia). Shark Tooth Mountain, officially named in 1954, is also known as The Sharktooth or Sharp Tooth Mountain. It is a mountain in the East Kootenay region of southeastern British Columbia, Canada, southwest of Whiteswan Lake. Presumably, the name is related to the profile of the peak.

Geographic entities mentioned:
surface_form: the sharktooth
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0736
lon: -115.58
surface_form: shark tooth mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0736
lon: -115.58
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
The land area is composed of Plum Island, Detroit Island, Washington Island, Hog Island, Pilot Island, Fish Island, and Rock Island. Washington Island is the largest in a chain of islands (which are collectively referred to as the Potawatomi Islands) extending across Lake Michigan between the Door Peninsula in Wisconsin and the Garden Peninsula in Delta County, Michigan.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Washington Island is the largest in a chain of islands (which are collectively referred to as the Potawatomi Islands) extending across Lake Michigan between the Door Peninsula in Wisconsin and the Garden Peninsula in Delta County, Michigan. These islands are outcroppings of the Niagara Escarpment. Demographics. The 2010 US Census lists 708 residents.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
Sorensen Beach. Sorensen Beach, previously referred to as Sorenson's Beach, is an organized hamlet in the Rural Municipality of McKillop No. 220, Saskatchewan, Canada that is recognized as a designated place by Statistics Canada. It is located on the eastern shore of Last Mountain Lake, approximately northwest of Regina. History.

Geographic entities mentioned:
surface_form: Last Mountain Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.1667
lon: -105.25
Ownership is administered by the Bureau of Land Management. It is situated southeast of Bottleneck Peak, south of Assembly Hall Peak, and the nearest higher neighbor is Cedar Mountain, to the north-northeast. Precipitation runoff from this feature drains north into the nearby San Rafael River.

Geographic entities mentioned:
surface_form: Bottleneck Peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0603
lon: -110.688
surface_form: Assembly Hall Peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.066944444444
lon: -110.65805555556
surface_form: cedar mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.228055555556
lon: -111.52944444444
surface_form: hall peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.060277777778
lon: -121.53972222222
surface_form: cedar mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.3694
lon: -78.0714
Geology. This major erosional remnant along the San Rafael River is composed of Wingate Sandstone, which is the remains of wind-borne sand dunes deposited approximately 200 million years ago in the Late Triassic, overlain by Kayenta Formation, and capped by Jurassic Navajo Sandstone. Lightly-colored slopes of Chinle Formation are exposed in places around the base of the mountain. Climate.

Geographic entities mentioned:
surface_form: navajo
instance_of: Mountain
countries: United States
coordinates: lat: 37.034169444444
lon: -110.86888888889
Window Blind Peak. Window Blind Peak is a summit located in the San Rafael Swell of Emery County, Utah, U.S. Towering 1,800 feet above its surrounding terrain, it is the highest point of the Mexican Mountain Wilderness Study Area. Ownership is administered by the Bureau of Land Management.

Geographic entities mentioned:
surface_form: window blind peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.044722222222
lon: -110.65638888889
Climate. Spring and fall are the most favorable seasons to visit Window Blind Peak. According to the Köppen climate classification system, it is located in a Cold semi-arid climate zone, which is defined by the coldest month having an average mean temperature below 32 °F (0 °C), and at least 50% of the total annual precipitation being received during the spring and summer.

Geographic entities mentioned:
surface_form: window blind peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.044722222222
lon: -110.65638888889
Gorno Dupeni. Gorno Dupeni () is a village in the Resen Municipality of North Macedonia, north of Lake Prespa. It is located roughly from the municipal centre of Resen. Demographics. Gorno Dupeni has 59 inhabitants as of the most recent census of 2002. Macedonians have historically made up almost all of the village population.

Geographic entities mentioned:
surface_form: Lake Prespa
instance_of: Lake
countries: North Macedonia
Albania
Greece
coordinates: lat: 40.9
lon: 21.05
There are 5 hairpins curves between Devimane Temple and Sampakhanda. After entering the Western Ghats, there are many sharp curves until Ekkambi. On the Deccan Plateau, three hairpin curves exist between Ekkambi and Sirsi. There are 12 bridges in this ghat section. At this point, the road becomes signed SH69/SH142 and is maintained by the Karnataka State Highway works department.

Geographic entities mentioned:
surface_form: Deccan Plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
In 2007, the square was symbolically renamed the &quot;Freedom for Jonathan Pollard Square&quot;. Gaza Street begins at the intersection of Paris Square, King George, Keren HaYesod and Rambam streets, and it spans until the intersection with Rabbi Yitzhak HaLevi Herzog Avenue next to the Valley of the Cross (&quot;Emeq HaMatzleva&quot;) and the Monastery of the Cross.

Geographic entities mentioned:
surface_form: Valley of the Cross
instance_of: Valley
countries: Israel
coordinates: lat: 31.7731
lon: 35.2075
However, following his patron's death in same year, Fazli's career trajectory is unclear. By 1639-40, he had relocated to the Deccan, Mughal India, where he completed the second volume of &quot;Afẓal al-Tavārīkh&quot;. The reasons for his emigration remain uncertain, but many Safavid elites sought patronage in Mughal India.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Axel Prahl and Jan Josef Liefers performed their roles, Thiel and professor Boerne, but kept their real names. They wandered through Mecklenburg-Vorpommern (east coast, Kühlungsborn, Usedom, Rügen, Fischland-Darß-Zingst, and Lake Schwerin), interacting with the locals while having their typical quarrels, well known from &quot;Tatort Münster&quot;.

Geographic entities mentioned:
surface_form: Lake Schwerin
instance_of: Lake
countries: Germany
coordinates: lat: 53.716666666667
lon: 11.466666666667
Ysgol Gyfun Cwm Rhymni. Ysgol Gyfun Cwm Rhymni is a Welsh-medium school situated in the village of Fleur-de-Lys in the Rhymney Valley. Cwm Rhymni was founded in 1981 with just over 150 pupils and has since grown to 1,684 pupils with 1,164 at the Gellihaf campus and 520 at Y Gwyndy (September 2018). The school's motto is “Tua'r Goleuni” (Towards the Light) and its badge is a dragon rampant.

Geographic entities mentioned:
surface_form: Rhymney Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.697777777778
lon: -3.2294444444444
The school has also fared very well down the years in the Urdd Eisteddfod. Cwm Rhymni has a very large catchment area stretching from Rhymney near the top of the valley to Caerphilly. The breadth of the catchment area is reflected by the names of the three main corridors at the Gellihaf campus; Ebwy, Sirhywi and Rhymni; three adjoining South Wales Valleys that all feed some pupils into Cwm Rhymni.

Geographic entities mentioned:
surface_form: Sirhywi
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.779
lon: -3.233
surface_form: Rhymni
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.697777777778
lon: -3.2294444444444
The Couronne de Bréona, is a mountain of the Pennine Alps, located east of Les Haudères in the canton of Valais. It lies north of the Tsa de l'Ano, on the range between the valleys of Hérens and Moiry. &quot;Bréona&quot; is the name of an extensive alpine pasture to the south-west of the peak, spanning elevations between some, making it one of the highest pastures in the Alps altogether.

Geographic entities mentioned:
surface_form: Tsa de l'Ano
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.078055555556
lon: 7.5730555555556
Couronne de Bréona. The Couronne de Bréona, is a mountain of the Pennine Alps, located east of Les Haudères in the canton of Valais. It lies north of the Tsa de l'Ano, on the range between the valleys of Hérens and Moiry.

Geographic entities mentioned:
surface_form: couronne de bréona
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.0917
lon: 7.57056
The &quot;Bréona&quot; pasture stretches from here to and above, with a well structure indicated at. From here, the path ascends to &quot;Col de Bréona&quot; at, separating the &quot;Serra Neire&quot; to the southwest from the &quot;Couronne de Bréona&quot; to the southeast, and via &quot;Col du Tsaté&quot; () traversing to &quot;Pinte du Bandon&quot; () to the northwest.

Geographic entities mentioned:
surface_form: couronne de bréona
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.0917
lon: 7.57056
surface_form: couronne de bréona
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.0917
lon: 7.57056
He was a member of the Young Poland movement. Life. Kazimierz Przerwa-Tetmajer was born in Ludźmierz in Podhale near the Tatra Mountains, then in the Austro-Hungarian Empire now in Poland, and died in Warsaw. His older half-brother was the painter Włodzimierz Tetmajer. Przerwa-Tetmajer studied classics and philosophy at the Jagiellonian University in 1884–1889.

Geographic entities mentioned:
surface_form: Podhale
instance_of: Valley
countries: Poland
coordinates: lat: 49.4793
lon: 20.0291
Geography. Located near the Maddalena Pass, it is joined to the nearby Enciastraia peak by a ridge. The name, meaning &quot;Rock of the Three Bishops&quot;, derives from the fact that the mount is on the intersection point of three Catholic dioceses, those of Cuneo, Nice and Digne.

Geographic entities mentioned:
surface_form: Enciastraia
instance_of: Mountain
countries: Italy
coordinates: lat: 44.36666667
lon: 6.89
surface_form: enciastraia
instance_of: Mountain
countries: Italy
coordinates: lat: 44.36666667
lon: 6.89
Rocca dei Tre Vescovi. Rocca dei Tre Vescovi (French: &quot;Rocher des Trois Évêques&quot;) is a mountain in the Maritime Alps, on the boundary between the province of Cuneo (Piedmont, northern Italy) and the French region of Provence-Alpes-Côte-d'Azur. Geography. Located near the Maddalena Pass, it is joined to the nearby Enciastraia peak by a ridge.

Geographic entities mentioned:
surface_form: rocca dei tre vescovi
instance_of: Mountain
countries: Italy
coordinates: lat: 44.36305556
lon: 6.88666667
The stadium was used for the 2013 UEFA Super Cup. History. In the early 1950s, Slavia was forced to leave its stadium at Letná and a new stadium was built at Eden in the Vršovice district. Its capacity was about 50,000 (mostly for standing). The wooden western (main) stand was taken from the old stadium at Letná, the rest of the stands were made of concrete.

Geographic entities mentioned:
surface_form: Letná
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.0957
lon: 14.4165
The exact GNIS location of its summit is, and it has an official (USGS) elevation of above mean sea level. It is the second-highest point in the county behind Kennesaw Mountain, and second in the core metro Atlanta area, behind Kennesaw Mountain, which is also in Cobb County. It is fifth if the exurban counties further north are considered.

Geographic entities mentioned:
surface_form: Kennesaw Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.976213888889
lon: -84.579655555556
surface_form: Kennesaw Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.976213888889
lon: -84.579655555556
Sweat Mountain is also a part of the ridge that divides the Chattahoochee River basin to the south and southeast, from the Lake Allatoona (Etowah River) basin to the north and northwest. From Sweat Mountain, this runs west-southwest through Cobb to Kennesaw Mountain and Lost Mountain. History. At one time the entire mountain was owned by the Wigley family.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
surface_form: etowah river
instance_of: Watercourse
countries: United States
coordinates: lat: 32.4862464
lon: -86.2777475
surface_form: sweat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.0669
lon: -84.4556
It is fifth if the exurban counties further north are considered. This height has made the mountain very attractive for radio, having several transmitters, radio towers, and antennas, for pagers, cellphones, broadcasting, and amateur radio. The fact that Stone Mountain and Kennesaw Mountain are both protected as parks has led to a proliferation of technology at the top.

Geographic entities mentioned:
surface_form: stone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.805944444444
lon: -84.145422222222
surface_form: stone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.548611111111
lon: -77.842777777778
surface_form: stone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.3936
lon: -81.0433
surface_form: kennesaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.976213888889
lon: -84.579655555556
Sweat Mountain. Sweat Mountain is a mountain in far northeastern Cobb County, Georgia, in the suburbs north of Atlanta. The exact GNIS location of its summit is, and it has an official (USGS) elevation of above mean sea level. It is the second-highest point in the county behind Kennesaw Mountain, and second in the core metro Atlanta area, behind Kennesaw Mountain, which is also in Cobb County.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: sweat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.0669
lon: -84.4556
Sweat Mountain is also a part of the ridge that divides the Chattahoochee River basin to the south and southeast, from the Lake Allatoona (Etowah River) basin to the north and northwest. From Sweat Mountain, this runs west-southwest through Cobb to Kennesaw Mountain and Lost Mountain. History. At one time the entire mountain was owned by the Wigley family.

Geographic entities mentioned:
surface_form: lost mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.3772
lon: -95.5944
surface_form: kennesaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.976213888889
lon: -84.579655555556
surface_form: sweat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.0669
lon: -84.4556
The main road now turns off from itself (makes a 90-degree turn) and continues generally west as Jamerson Road. Following the remaining Wigley Road to the dead end, there is a barrow pit just past the barricades. There was a place where natural springs created a huge swampy mudbog in the middle of the Wigley Road, which led to its closing.

Geographic entities mentioned:
surface_form: dead
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
Sweat Mountain. Sweat Mountain is a mountain in far northeastern Cobb County, Georgia, in the suburbs north of Atlanta. The exact GNIS location of its summit is, and it has an official (USGS) elevation of above mean sea level. It is the second-highest point in the county behind Kennesaw Mountain, and second in the core metro Atlanta area, behind Kennesaw Mountain, which is also in Cobb County.

Geographic entities mentioned:
surface_form: sweat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.0669
lon: -84.4556
The presence of the mountain has inspired the naming of a variety of nearby establishments including: Sweat Mountain Park, Mountain View Regional Library, Mountain View Elementary School, and Mountain View United Methodist Church.

Geographic entities mentioned:
surface_form: sweat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.0669
lon: -84.4556
Radio. There are also long-standing applications (potentially moot) for broadcast translators by Calvary Chapel on 94.5 and 103.7 to serve Woodstock. Another application for a translator on 102.1 by Community Public Radio to serve &quot;Sweat Mountain&quot; (which is not a recognized community) is also listed by the Federal Communications Commission (FCC). Television.

Geographic entities mentioned:
surface_form: sweat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.0669
lon: -84.4556
(This is different from the worldwide DVB-SH standard, which is derived from the DVB-S standard that Dish Network has used for DBS since the 1990s.) The signal from Sweat Mountain was active, but no service to the public was ever announced.

Geographic entities mentioned:
surface_form: sweat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.0669
lon: -84.4556
The three volcanoes are coalesced. Puyehue is located in the southeast, Cordón Caulle in the center, and Cordillera Nevada, which owes its name to its often snowy appearance from the relatively densely populated Chilean Central Valley, is at the northwestern end. The massif is located between two lakes, Ranco Lake in the north and Puyehue Lake in the south.

Geographic entities mentioned:
surface_form: Chilean Central Valley
instance_of: Valley
countries: Chile
coordinates: lat: -35.5
lon: -71.5
surface_form: puyehue
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
The three volcanoes are coalesced. Puyehue is located in the southeast, Cordón Caulle in the center, and Cordillera Nevada, which owes its name to its often snowy appearance from the relatively densely populated Chilean Central Valley, is at the northwestern end. The massif is located between two lakes, Ranco Lake in the north and Puyehue Lake in the south.

Geographic entities mentioned:
surface_form: Puyehue Lake
instance_of: Lake
countries: Chile
coordinates: lat: -40.683333333333
lon: -72.45
surface_form: puyehue
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
The old Pliocene volcano Mencheca, currently exposed just northeast of Puyehue's cone, declined in activity. This decline was probably due a regional change in the location of the active front of the Southern Volcanic Zone that also affected other volcanoes such as Tronador and Lanín. The relocation of the active front gave rise to new volcanoes further westward or increased their activity.

Geographic entities mentioned:
surface_form: Tronador
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -41.160833333333
lon: -71.8875
surface_form: Lanín
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -39.632777777778
lon: -71.499722222222
It is estimated that some 100,000 years ago in the period between Río Llico and Llanquihue glaciation a large ignimbrite called San Pablo was produced. This ignimbrite covers an estimated area of immediately west of Cordillera Nevada, stretching across the Chilean Central Valley almost reaching the Chilean Coast Range.

Geographic entities mentioned:
surface_form: Chilean Central Valley
instance_of: Valley
countries: Chile
coordinates: lat: -35.5
lon: -71.5
The closest were Valdivia and the sporadic missions of Nahuel Huapi all of them out of sight of the volcano. In 1759 an eruption was noticed in the Cordillera, although this is mainly attributed to Mocho. By the end of the 19th century most of the Central Valley west of Cordón Caulle had been settled by Chileans and European immigrants and an eruption was reported in 1893.

Geographic entities mentioned:
surface_form: Mocho
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
In 1759 an eruption was noticed in the Cordillera, although this is mainly attributed to Mocho. By the end of the 19th century most of the Central Valley west of Cordón Caulle had been settled by Chileans and European immigrants and an eruption was reported in 1893. The next report came in 1905, but the eruption of 8 February 1914 is the first one certain to have occurred.

Geographic entities mentioned:
surface_form: Central Valley
instance_of: Valley
countries: Chile
coordinates: lat: -35.5
lon: -71.5
The Chilean emergency office ONEMI (Oficina Nacional de Emergencia del Ministerio del Interior) organized a flight over the area with two volcanologists aboard. Puyehue and Cordón Caulle as well the Carrán crater were found without activity. From accounts of local inhabitants of the area it is inferred that a small pumice cone was formed around 1990.

Geographic entities mentioned:
surface_form: Carrán crater
instance_of: Mountain
countries: Chile
coordinates: lat: -40.308
lon: -72.07
Puyehue-Cordón Caulle. Puyehue (;) and Cordón Caulle are two coalesced volcanic edifices that form a major mountain massif in Puyehue National Park in the Andes of Ranco Province, in the South of Chile. In volcanology this group is known as the Puyehue-Cordón Caulle Volcanic Complex (PCCVC).

Geographic entities mentioned:
surface_form: puyehue
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
Cordón Caulle erupted shortly after the Great Chilean Earthquake. With a magnitude of 9.5, it remains the largest recorded earthquake in history. Apart from this, the Puyehue-Cordón Caulle area is one of the main sites of exploration for geothermal power in Chile. Geothermal activity is manifested on the surface of Puyehue and Cordón Caulle as several boiling springs and fumaroles.

Geographic entities mentioned:
surface_form: puyehue
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
Geothermal activity is manifested on the surface of Puyehue and Cordón Caulle as several boiling springs and fumaroles. Most of the stone artifacts found in Pilauco Bajo (dated to c. 12.5 to 13.5 ka BP) are made of dacite, rhyodacite and rhyolite from the Puyehue-Cordón Caulle. Yet these rocks were imported by humans to the site as nearby rivers have not transported them. Geography.

Geographic entities mentioned:
surface_form: puyehue
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
Puyehue-Cordón Caulle. Puyehue (;) and Cordón Caulle are two coalesced volcanic edifices that form a major mountain massif in Puyehue National Park in the Andes of Ranco Province, in the South of Chile. In volcanology this group is known as the Puyehue-Cordón Caulle Volcanic Complex (PCCVC).

Geographic entities mentioned:
surface_form: puyehue
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
surface_form: puyehue
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
In volcanology this group is known as the Puyehue-Cordón Caulle Volcanic Complex (PCCVC). Four volcanoes constitute the volcanic group or complex, the Cordillera Nevada caldera, the Pliocene Mencheca volcano, Cordón Caulle fissure vents and the Puyehue stratovolcano.

Geographic entities mentioned:
surface_form: puyehue
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
Four volcanoes constitute the volcanic group or complex, the Cordillera Nevada caldera, the Pliocene Mencheca volcano, Cordón Caulle fissure vents and the Puyehue stratovolcano. Like most stratovolcanoes in the Southern Volcanic Zone of the Andean Volcanic Belt, Puyehue and Cordón Caulle are along the intersection of a traverse fracture with the larger north–south Liquiñe-Ofqui Fault.

Geographic entities mentioned:
surface_form: puyehue
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
With a magnitude of 9.5, it remains the largest recorded earthquake in history. Apart from this, the Puyehue-Cordón Caulle area is one of the main sites of exploration for geothermal power in Chile. Geothermal activity is manifested on the surface of Puyehue and Cordón Caulle as several boiling springs and fumaroles. Most of the stone artifacts found in Pilauco Bajo (dated to c.

Geographic entities mentioned:
surface_form: puyehue
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
12.5 to 13.5 ka BP) are made of dacite, rhyodacite and rhyolite from the Puyehue-Cordón Caulle. Yet these rocks were imported by humans to the site as nearby rivers have not transported them. Geography. Puyehue, Cordón del Caulle, and Cordillera Nevada form a northwest trending massif in the Ranco Province of the Andes. The three volcanoes are coalesced.

Geographic entities mentioned:
surface_form: puyehue
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
The massif is located between two lakes, Ranco Lake in the north and Puyehue Lake in the south. The fact that Puyehue volcano is named after Puyehue Lake reflects that it is better seen and more accessible from the south. Cordillera Nevada is a wide semicircular caldera and corresponds to the remnants of a collapsed volcano. Cordillera Nevada covers an area of.

Geographic entities mentioned:
surface_form: puyehue
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
surface_form: puyehue
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
surface_form: puyehue lake
instance_of: Lake
countries: Chile
coordinates: lat: -40.683333333333
lon: -72.45
Cordillera Nevada covers an area of. Cordón Caulle is a northwest trending ridge that hosts a volcanic-tectonic graben in which a fissure vent is developed. Puyehue Volcano is a stratovolcano located on the southeastern end of Cordón Caulle, just east of the main fault of the Liquiñe-Ofqui Fault Zone. Its cone hosts a wide crater, and products of Puyehue volcanism cover an approximate area of.

Geographic entities mentioned:
surface_form: puyehue
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
Cordón Caulle is a northwest trending ridge that hosts a volcanic-tectonic graben in which a fissure vent is developed. Puyehue Volcano is a stratovolcano located on the southeastern end of Cordón Caulle, just east of the main fault of the Liquiñe-Ofqui Fault Zone. Its cone hosts a wide crater, and products of Puyehue volcanism cover an approximate area of. Flora.

Geographic entities mentioned:
surface_form: puyehue
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
Ancestral volcanoes. Some 300,000 years ago, important changes occurred in the area of Puyehue. The old Pliocene volcano Mencheca, currently exposed just northeast of Puyehue's cone, declined in activity. This decline was probably due a regional change in the location of the active front of the Southern Volcanic Zone that also affected other volcanoes such as Tronador and Lanín.

Geographic entities mentioned:
surface_form: puyehue
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
Volcanism during the Llanquihue glaciation. During the Llanquihue glaciation volcanism occurred on all three vents, Cordillera Nevada, Cordón Caulle and Puyehue volcano. During most of this time the volcano was covered by the Patagonian Ice Sheet, leaving glacial striae on many lava outcrops and affecting the volcanic activity.

Geographic entities mentioned:
surface_form: puyehue
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
The onset of this change was marked by the eruption of rhyodacite mingled with basaltic andesite rich in magnesium oxide (MgO). The bimodal activity continued with a small hiatus around 30,000 years ago until around 19,000 years ago when Puyehues started to produce lava domes and flows of dacitic to rhyolitic composition, a trend that lasted until 12,000 years before present.

Geographic entities mentioned:
surface_form: puyehue
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
The bimodal activity continued with a small hiatus around 30,000 years ago until around 19,000 years ago when Puyehues started to produce lava domes and flows of dacitic to rhyolitic composition, a trend that lasted until 12,000 years before present. Between 15,000 and 12,000 years ago Puyehue also erupted basaltic andesite.

Geographic entities mentioned:
surface_form: puyehue
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
Between 15,000 and 12,000 years ago Puyehue also erupted basaltic andesite. During the Llanquihue glaciation Puyehue volcano produced some of the most primitive basalts of the Southern Volcanic Zone with a magnesium oxide mass percentage of 14.32, which is in equilibrium with melt from mantle peridotite. Postglacial volcanism.

Geographic entities mentioned:
surface_form: puyehue
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
Postglacial volcanism. Only Puyehue and Cordón Caulle have erupted during the Holocene, and until 2011 only Cordón Caulle had recorded historical eruptions. In the interval between 7,000 and 5,000 years ago Puyehue had rhyolitic eruptions that produced lava domes. The lava domes were later destroyed after a sequence of strong eruptions that were part of an explosive eruptive cycle.

Geographic entities mentioned:
surface_form: puyehue
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
From accounts of local inhabitants of the area it is inferred that a small pumice cone was formed around 1990. In 1994 a temporarily emplaced seismic network registered tremors north of Puyehue's cone which reached IV and V degrees on the Mercalli intensity scale. This prompted ONEMI to invoke an emergency action committee, however soon afterward unrest ceased.

Geographic entities mentioned:
surface_form: puyehue
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
Airports as far away as Buenos Aires and Melbourne, Australia, had to be closed temporarily due to volcanic ash. By 15 June a dense column of ash was still erupting 10 km into the air, with the ash cloud spreading across the Southern Hemisphere; scientists expected intensifying eruptions of Puyehue in the following days, and said the volcano showed no signs of slowing down.

Geographic entities mentioned:
surface_form: puyehue
instance_of: Mountain
countries: Chile
coordinates: lat: -40.59027777777778
lon: -72.11722222222222
Gwangdeoksan (South Chungcheong). Gwangdeoksan is a mountain of South Chungcheong Province, western South Korea. It has an elevation of 699 metres.

Geographic entities mentioned:
surface_form: gwangdeoksan (south chungcheong)
instance_of: Mountain
countries: South Korea
Gwangdeoksan (South Chungcheong). Gwangdeoksan is a mountain of South Chungcheong Province, western South Korea. It has an elevation of 699 metres.

Geographic entities mentioned:
surface_form: gwangdeoksan
instance_of: Mountain
countries: South Korea
Confluentibacter citreus. &quot;Confluentibacter citreus&quot; is a Gram-negative, aerobic and rod-shaped bacterium from the genus of &quot;Confluentibacter&quot; which has been isolated from the Sayram Lake in China.

Geographic entities mentioned:
surface_form: Sayram Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 44.598055555556
lon: 81.164722222222
French migration into Canada West/Ontario did not accelerate until the second half of the 19th century, farmers from Canada East/Quebec began to migrate in search of fertile land in Eastern Ontario, and along the Canadian Pacific Railway north of Lake Nipissing and Lake Huron.

Geographic entities mentioned:
surface_form: Lake Nipissing
instance_of: Lake
countries: Canada
coordinates: lat: 46.283333333333
lon: -80
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
He was subsequently given command of the frigate in 1812, but she was later wrecked in the Bahamas, although he was acquitted of blame for its loss. Yeo was then given command of the British squadron on Lake Ontario and commanded it in several engagements on Lake Ontario with American forces. He died off the African coast in 1818. Early life and career.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Yeo was sent to Canada in 1813 aboard to command the British naval forces in the Great Lakes. He was appointed commodore of the fleet on Lake Ontario. Yeo's use of his small navy was always determined and skillful, but he was hampered by a lack of cooperation from the British army.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
The commander of these forces, Sir George Prevost, failed to follow up key advances made by Yeo at Sackett's Harbour and elsewhere that might have resulted in major British victories. On the whole, historians regard the war on Lake Ontario as having been a draw. During 1814 both Yeo and Isaac Chauncey, the American commander, tried to out build the other.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Sefid-Rud. The Sepid-Rud (;; also known as Sefid-Rud) is a river, approximately long, rising in the Alborz mountain range of northwestern Iran and flowing generally northeast to empty into the Caspian Sea at Rasht. Names. Other names and transcriptions include Sepīd-Rūd, Sefidrud, Sefidrood, Sepidrood, and Sepidrud. Above Manjil, &quot;Long Red River&quot;.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
It then widens the valley between the Talesh Hills and the main Alborz range. The gap provides a major route between Tehran and Gīlān Province with its Caspian lowlands. In the wide valley before the Sefid-Rud enters the Caspian Sea, a number of transportation and irrigation canals have been cut; the two biggest are the Khomam and the Now. Dam and reservoir.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Wainwright's route leaves Bowness along the path of the Dales Way, makes an anticlockwise loop over the viewpoint of Post Knott to the summit, and either returns along the Dales Way or follows a woodland path to Helm Road from where another viewpoint, Biskey Howe, is only a slight detour before continuing down Helm Road to Bowness. He commends its &quot;fine prospect of Windermere&quot;.

Geographic entities mentioned:
surface_form: Windermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.358333333333
lon: -2.9361111111111