Sarmila/GeoWiki-Features huggingface dataset:
With an area of 1,186 km2 and an average altitude of 550 m, Sofia Valley is the largest and contains the nation's capital, Sofia. The Rose Valley encompasses the valleys of Karlovo and Kazanlak and is renowned for its rose-growing industry, which has been thriving there for centuries, producing 85% of the world's rose oil.

Geographic entities mentioned:
surface_form: Rose Valley
instance_of: Valley
countries: Bulgaria
coordinates: lat: 42.616666666667
lon: 25.4
The Kazanlak Valley is also known as the Valley of the Thracian Kings due to the extremely high concentration and variety of monuments of the Thracian culture. Srednogorie region stretches between the Sub-Balkan valleys in the north and the Rilo-Rhodope Massif in the south and from west to east includes the mountains Zavalska Planina, Viskyar, Lyulin, Vitosha, Plana and Sredna Gora.

Geographic entities mentioned:
surface_form: Zavalska Planina
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.83
lon: 22.783
surface_form: Viskyar
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.761111111111
lon: 22.944166666667
Rilo-Rhodope region. The Rilo-Rhodope geomorphological region covers the south-western regions of Bulgaria and includes the Rhodope Mountains, Rila, Pirin, Osogovo, Vlahina, Maleshevo, Ograzhden, Slavyanka and Belasitsa, as well as the valleys of the rivers Struma and Mesta.

Geographic entities mentioned:
surface_form: Vlahina
instance_of: Mountain
countries: Bulgaria
North Macedonia
coordinates: lat: 41.856944444444
lon: 22.928888888889
surface_form: Maleshevo
instance_of: Mountain
countries: Bulgaria
North Macedonia
coordinates: lat: 41.666666666667
lon: 23
The other Bulgarian rivers flowing directly to the Aegean are the Struma and the Mesta. Bulgaria has around 400 natural lakes with a total area of 95 km2 and volume of 278 million km3. The limans and lagoons along the Black Sea coast include from north to south Lake Durankulak, Lake Shabla, Lake Varna, Lake Beloslav, Lake Pomorie, Lake Atanasovsko, Lake Burgas and Lake Mandrensko.

Geographic entities mentioned:
surface_form: Lake Shabla
instance_of: Lake
countries: Bulgaria
coordinates: lat: 43.57305556
lon: 28.56555556
surface_form: Lake Varna
instance_of: Lake
countries: Bulgaria
coordinates: lat: 43.190277777778
lon: 27.825
surface_form: Lake Beloslav
instance_of: Lake
countries: Bulgaria
coordinates: lat: 43.18777778
lon: 27.7
surface_form: Lake Pomorie
instance_of: Lake
countries: Bulgaria
coordinates: lat: 42.583
lon: 27.618
surface_form: Lake Burgas
instance_of: Lake
countries: Bulgaria
coordinates: lat: 42.5
lon: 27.4
There are 170 glacial lakes in Rila and 164 in Pirin. They are an important tourist asset. The most renown lakes include the Seven Rila Lakes, Popovo Lake, Banderishki Lakes, Vasilashki Lakes, Vlahini Lakes, etc. Swamps and marshes include Alepu, Arkutino, Aldomirovtsi Marsh, Dragoman Marsh, etc. There are around 2,200 reservoirs with a total volume of c. 7 billion km3.

Geographic entities mentioned:
surface_form: Seven Rila Lakes
instance_of: Group of lakes
countries: Bulgaria
coordinates: lat: 42.2025
lon: 23.315
surface_form: Banderishki Lakes
instance_of: Group of lakes
countries: Bulgaria
coordinates: lat: 41.7417
lon: 23.4125
surface_form: Vasilashki Lakes
instance_of: Group of lakes
countries: Bulgaria
coordinates: lat: 41.741388888889
lon: 23.451666666667
surface_form: Vlahini Lakes
instance_of: Group of lakes
countries: Bulgaria
The early town quickly became a profitable re-supply center/mercantile as one of the leading stop-overs for miners traveling the Willamette River to the California Gold Rush mines. The city was thought to have been originally named after early settler Mary Lloyd, but now the name is credited to early French fur trappers who camped near Marys Peak.

Geographic entities mentioned:
surface_form: Marys Peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.504355555556
lon: -123.55245555556
According to the United States Census Bureau, the city has a total area of, of which are land and is covered by water. Climate. Like the rest of the Willamette Valley, Corvallis lies in the Marine West Coast climate zone, with Mediterranean characteristics. Under the Köppen climate classification scheme, Corvallis has a warm-summer Mediterranean climate (Köppen: Csb).

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Continuing on OR 34 another 9–10 miles east of I-5 is the city of Lebanon, Oregon the 3rd largest city of the Albany-Corvallis-Lebanon CSA. Westward on OR 34 connects Corvallis to Philomath, Marys Peak, Alsea and Waldport on the Oregon Coast. US Route 20 is the main connector between the cities of Corvallis and Albany, Oregon, which is the 2nd largest city of the Albany-Corvallis-Lebanon CSA.

Geographic entities mentioned:
surface_form: Marys Peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.504355555556
lon: -123.55245555556
He subsequently became chief of artillery in the Army of West Virginia. Du Pont served in General Philip Sheridan's army in the Shenandoah Valley of northern Virginia. He received the Medal of Honor for his handling of a retreat at the Battle of Cedar Creek, allowing Sheridan to win a victory in the battle. During the war, du Pont received two brevets (honorary promotions).

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Girl Guides and Girl Scouts World Camp. At the 15th World Conference of WAGGGS it was decided to mark the centenary of the birth of Lord Baden-Powell, the founder of Guiding, by holding a World Camp with four locations — Doe Lake, Ontario; Quezon City, Philippines; Lac de Conche, Switzerland; and Windsor Great Park, England, from January 19 to February 2, 1957.

Geographic entities mentioned:
surface_form: Lac de Conche
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.264722222222225
lon: 6.8625
surface_form: doe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.53388888888889
lon: -79.41416666666667
Doe Lake (Parry Sound District). Doe Lake is a lake in Parry Sound District, Ontario, Canada. The lake is composed of three sections and as such known locally for their size as &quot;Big Doe Lake&quot;, &quot;Middle Doe Lake&quot;, and &quot;Little Doe Lake&quot;. Doe Lake is the largest lake in the Almaguin Highlands area of the Magnetawan River system.

Geographic entities mentioned:
surface_form: doe lake (parry sound district)
instance_of: Lake
countries: Canada
coordinates: lat: 45.53388888888889
lon: -79.41416666666667
Doe Lake (Parry Sound District). Doe Lake is a lake in Parry Sound District, Ontario, Canada. The lake is composed of three sections and as such known locally for their size as &quot;Big Doe Lake&quot;, &quot;Middle Doe Lake&quot;, and &quot;Little Doe Lake&quot;. Doe Lake is the largest lake in the Almaguin Highlands area of the Magnetawan River system.

Geographic entities mentioned:
surface_form: doe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.53388888888889
lon: -79.41416666666667
Doe Lake (Parry Sound District). Doe Lake is a lake in Parry Sound District, Ontario, Canada. The lake is composed of three sections and as such known locally for their size as &quot;Big Doe Lake&quot;, &quot;Middle Doe Lake&quot;, and &quot;Little Doe Lake&quot;. Doe Lake is the largest lake in the Almaguin Highlands area of the Magnetawan River system.

Geographic entities mentioned:
surface_form: doe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.53388888888889
lon: -79.41416666666667
surface_form: doe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.53388888888889
lon: -79.41416666666667
surface_form: doe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.53388888888889
lon: -79.41416666666667
surface_form: doe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.53388888888889
lon: -79.41416666666667
Doe Lake is the largest lake in the Almaguin Highlands area of the Magnetawan River system. The communities of Katrine and Doe Lake can be found on the Lake. The community of &quot;Katrine&quot; has a small marina and is found on the &quot;Little Doe&quot; section of the lake. However &quot;Doe Lake&quot; is a classified as a dispersed rural community found in the area.

Geographic entities mentioned:
surface_form: doe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.53388888888889
lon: -79.41416666666667
Llyn-y-Foel. is a lake in Snowdonia, Wales. It is approximately 240 m across, 120 m wide and up to 2 m deep. It lies at 535m altitude at the foot of the main ridge of Moel Siabod at. The main outflow, at the south-east of the lake, forms one of the main tributaries of Afon Ystumiau, which eventually feeds into Afon Lledr and subsequently into Afon Conwy.

Geographic entities mentioned:
surface_form: Moel Siabod
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.073075
lon: -3.9324638888889
Although the lake bears the name &quot;Llyn y Foel&quot;, it does have another name - Llyn Llygad yr Ych, the Lake of the Ox's Eye - which recounts a tale about an ox that lost an eye under the strain of pulling the dreadful &quot;afanc&quot; from Betws y Coed to Glaslyn below Snowdon. See Perrin, Jim. &quot;Visions of Snowdonia&quot; (London: BBC Books, 1997).

Geographic entities mentioned:
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
surface_form: snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
surface_form: glaslyn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 53.070555555556
lon: -4.0661111111111
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: llyn y foel
instance_of: Lake
countries: United Kingdom
coordinates: lat: 53.073130555556
lon: -3.9194888888889
Llyn-y-Foel. is a lake in Snowdonia, Wales. It is approximately 240 m across, 120 m wide and up to 2 m deep. It lies at 535m altitude at the foot of the main ridge of Moel Siabod at. The main outflow, at the south-east of the lake, forms one of the main tributaries of Afon Ystumiau, which eventually feeds into Afon Lledr and subsequently into Afon Conwy.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Llyn-y-Foel. is a lake in Snowdonia, Wales. It is approximately 240 m across, 120 m wide and up to 2 m deep. It lies at 535m altitude at the foot of the main ridge of Moel Siabod at. The main outflow, at the south-east of the lake, forms one of the main tributaries of Afon Ystumiau, which eventually feeds into Afon Lledr and subsequently into Afon Conwy.

Geographic entities mentioned:
surface_form: llyn-y-foel
instance_of: Lake
countries: United Kingdom
coordinates: lat: 53.073130555556
lon: -3.9194888888889
The World Cup came into existence during the 2008–09 Season. The series includes boats that have competed in the Olympics and Paralympics. The world cup was from the beginning composed of the major regattas Sail Melbourne in Melbourne, US Sailings's Rolex Miami OCR in Miami, Trofeo SAR Princess Sofia in Palma de Majorca, Semaine Olympique Française in Hyères and Delta Lloyd Regatta in Medemblik.

Geographic entities mentioned:
surface_form: Hyères
instance_of: Mountain
countries: France
coordinates: lat: 43.118888888889
lon: 6.1286111111111
About 100,000 military seamen fought on the Leningrad front. In 1941-1944 naval vessels of this base participated in carrying out of landing operations in areas Strelna, Peterhof, on Lake Ladoga, in the Vyborg and in the Narva gulfs. During the blockade of Leningrad the fleet provided communication of the besieged city with the country through Lake Ladoga.

Geographic entities mentioned:
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
Life and work. Barr grew up in Trenton, New Jersey. In 1972, as a student researcher from Rutgers University, he took a short-term job at the Rocky Mountain Biological Laboratory measuring water quality near Crested Butte in the West Elk Mountains, Colorado. After some time, he featured in a local newspaper as an eccentric mountain hermit.

Geographic entities mentioned:
surface_form: Crested Butte
instance_of: Mountain
countries: United States
coordinates: lat: 38.883333333333
lon: -106.94361111111
Among these, Stol Mountain and Crni Vrh, stands as a notable peak, offering panoramic views and outdoor recreational opportunities. Incorporating Bor Lake, Brestovac Spa, and the Carpathian Mountains, including Stol Mountain, Veliki Krš and Mali Krš as well, into its geographical narrative, Bor presents a diverse and captivating environment for residents and tourists to explore. Climate.

Geographic entities mentioned:
surface_form: Bor Lake
instance_of: Lake
countries: Serbia
coordinates: lat: 44.0929
lon: 22.0126
surface_form: Veliki Krš
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.1708
lon: 22.0878
surface_form: Mali Krš
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.28555556
lon: 22.01611111
Assisi, called &quot;Asisium&quot; by the Romans, was an ancient Umbrian site on a spur of Mount Subasio. Myth relates that the city was founded by Dardanus in 847 BC. Perugia and Orvieto are not considered of Umbrian but Etruscan origin. According to the geographical distribution of the Umbrian territory, they are located on the left side of the Tiber River, which is part of the ancient Etruria.

Geographic entities mentioned:
surface_form: Mount Subasio
instance_of: Mountain
countries: Italy
coordinates: lat: 43.064166666667
lon: 12.6625
Named by United States Advisory Committee on Antarctic Names (US-ACAN) for Clair C. Patterson, glaciologist at Byrd Station, summer 1965-66. Pegmatite Peak. A peak, high, along the westside of Koerwitz Glacier, about midway between the main summits of Medina Peaks and Mount Salisbury. First mapped by the USGS from surveys and USN air photos, 1960-64.

Geographic entities mentioned:
surface_form: Mount Salisbury
instance_of: Mountain
countries: United States
coordinates: lat: 58.8508
lon: -137.372
surface_form: medina
instance_of: Mountain
coordinates: lat: -68.45
lon: -66.25
surface_form: medina peaks
instance_of: Mountain
coordinates: lat: -85.6
lon: -155.9
Medina Peaks. The Medina Peaks () are rugged, mainly ice-free, peaks surmounting a ridge long, extending north along the east side of Goodale Glacier to the edge of the Ross Ice Shelf, Antarctica. Discovery and naming. Some of the peaks were first seen and roughly mapped by the Byrd Antarctic Expedition, 1928–30.

Geographic entities mentioned:
surface_form: medina
instance_of: Mountain
coordinates: lat: -68.45
lon: -66.25
surface_form: medina peaks
instance_of: Mountain
coordinates: lat: -85.6
lon: -155.9
Discovery and naming. Some of the peaks were first seen and roughly mapped by the Byrd Antarctic Expedition, 1928–30. They were named by the Advisory Committee on Antarctic Names (US-ACAN) for Guillermo Medina, Technical Director of the U.S. Navy Hydrographic Office, 1954–60, and of the Naval Oceanographic Office, 1960–64. Location.

Geographic entities mentioned:
surface_form: medina
instance_of: Mountain
coordinates: lat: -68.45
lon: -66.25
Navy Hydrographic Office, 1954–60, and of the Naval Oceanographic Office, 1960–64. Location. The Medina Peaks lie between the Goodale Glacier to the west and the Koerwitz Glacier to the east, and extend up to the Ross Ice Shelf. From the south, features include Patterson Peak, Pegmatite Peak, Feeney Peak, Feeney Col and Hidden Col.

Geographic entities mentioned:
surface_form: medina
instance_of: Mountain
coordinates: lat: -68.45
lon: -66.25
surface_form: medina peaks
instance_of: Mountain
coordinates: lat: -85.6
lon: -155.9
Along the Ross Ice Shelf, from east to west, are Marks Point, Coloured Peak, Marble Peak, O'Brien Peak, Paradise Ridge and the MacDonald Nunataks. Patterson Peak. A peak, high, standing at the south end of Medina Peaks, northwest of Anderson Ridge. Mapped by United States Geological Survey (USGS) from ground surveys and United States Navy (USN) air photos, 1960-64.

Geographic entities mentioned:
surface_form: medina
instance_of: Mountain
coordinates: lat: -68.45
lon: -66.25
surface_form: medina peaks
instance_of: Mountain
coordinates: lat: -85.6
lon: -155.9
surface_form: anderson
instance_of: Mountain
coordinates: lat: -78.15
lon: -86.217
So named by New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1969-70, because of the occurrence of large, whitish pegmatite dykes in a rock wall at the SE spur of the peak. Feeney Peak. A peak, high, near the center of Medina Peaks, standing north of Patterson Peak on the E side of Goodale Glacier. Mapped by the USGS from ground surveys and USN air photos, 1960-64.

Geographic entities mentioned:
surface_form: medina
instance_of: Mountain
coordinates: lat: -68.45
lon: -66.25
surface_form: medina peaks
instance_of: Mountain
coordinates: lat: -85.6
lon: -155.9
Named by US-ACAN for Robert E. Feeney, biologist at McMurdo Station for several summers, 1964-65 to 1968-69. Feeney Col. A col at the northeast side of Feeney Peak, near the center of Medina Peaks. Though steep on both sides and high, the col provides a good route through Medina Peaks. Mapped by the USGS from surveys and USN air photos, 1960-64.

Geographic entities mentioned:
surface_form: medina
instance_of: Mountain
coordinates: lat: -68.45
lon: -66.25
surface_form: medina peaks
instance_of: Mountain
coordinates: lat: -85.6
lon: -155.9
Feeney Col. A col at the northeast side of Feeney Peak, near the center of Medina Peaks. Though steep on both sides and high, the col provides a good route through Medina Peaks. Mapped by the USGS from surveys and USN air photos, 1960-64. The col was used by members of NZGSAE, 1969-70, who named it in association with Feeney Peak. Hidden Col.

Geographic entities mentioned:
surface_form: medina
instance_of: Mountain
coordinates: lat: -68.45
lon: -66.25
surface_form: medina peaks
instance_of: Mountain
coordinates: lat: -85.6
lon: -155.9
Mapped by the USGS from surveys and USN air photos, 1960-64. The col was used by members of NZGSAE, 1969-70, who named it in association with Feeney Peak. Hidden Col. A col in the north part of Medina Peaks, about southwest of Marks Point, that allows a quick sledging route between the lower Amundsen and Scott Glaciers. Mapped by the USGS from surveys and USN air photos, 1960-64.

Geographic entities mentioned:
surface_form: medina
instance_of: Mountain
coordinates: lat: -68.45
lon: -66.25
surface_form: amundsen
instance_of: Mountain
coordinates: lat: -67.233333333333
lon: 100.75
surface_form: medina peaks
instance_of: Mountain
coordinates: lat: -85.6
lon: -155.9
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
The col was explored by NZGSAE, 1969-70, and so named because it is hidden behind ridges and spurs of the peaks to the northeast and southwest of it. Marks Point. A rock point extending east from the north end of Medina Peaks, at the south edge of the Ross Ice Shelf. This feature and nearby area were first seen by members of the Byrd Antarctic Expedition, 1928-30. Named by US-ACAN for George R.

Geographic entities mentioned:
surface_form: medina
instance_of: Mountain
coordinates: lat: -68.45
lon: -66.25
surface_form: medina peaks
instance_of: Mountain
coordinates: lat: -85.6
lon: -155.9
The name was applied by NZGSAE, 1969-70, because there are light-colored, whitish bands of marble crossing straight over its summit. O'Brien Peak. A rock peak, high, standing west of the north extremity of Medina Peaks, along the edge of the Ross Ice Shelf. Discovered in December 1929 by the Byrd Antarctic Expedition geological party under Laurence Gould, and named by Byrd for John S.

Geographic entities mentioned:
surface_form: medina
instance_of: Mountain
coordinates: lat: -68.45
lon: -66.25
surface_form: medina peaks
instance_of: Mountain
coordinates: lat: -85.6
lon: -155.9
Coloured Peak. A peak, high, near the head of Ross Ice Shelf in the coastal foothills of the Queen Maud Mountains, about southeast of O'Brien Peak. Mapped by the USGS from surveys and U.S. Navy air photos, 1960-64. The peak was examined by members of NZGSAE, 1969-70, and so named because of the colorful yellow, pink and brown banded strata that mark the feature. Marble Peak.

Geographic entities mentioned:
surface_form: brown
instance_of: Mountain
coordinates: lat: -68.3
lon: 86.4167
The peak was mapped by USGS from surveys and U.S. Navy air photos, 1960-64. The name was applied by NZGSAE, 1969-70, because there are light-colored, whitish bands of marble crossing straight over its summit. O'Brien Peak. A rock peak, high, standing west of the north extremity of Medina Peaks, along the edge of the Ross Ice Shelf.

Geographic entities mentioned:
surface_form: light
instance_of: Mountain
coordinates: lat: -74.2667
lon: -61.9833
The peak was examined by members of NZGSAE, 1969-70, and so named because of the colorful yellow, pink and brown banded strata that mark the feature. Marble Peak. A coastal peak, the twin of O'Brien Peak to the southeast and almost the same height, overlooking the head of Ross Ice Shelf about midway between Amundsen and Scott Glaciers. The peak was mapped by USGS from surveys and U.S.

Geographic entities mentioned:
surface_form: amundsen
instance_of: Mountain
coordinates: lat: -67.233333333333
lon: 100.75
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
Discovered in December 1929 by the Byrd Antarctic Expedition geological party under Laurence Gould, and named by Byrd for John S. O'Brien, surveyor with that party. Paradise Ridge. A low ridge that parallels the coast at the head of Ross Ice Shelf, located east of Amundsen Glacier and midway between MacDonald Nunataks and O'Brien Peak. Mapped by USGS from surveys and U.S. Navy air photos, 1960-64.

Geographic entities mentioned:
surface_form: amundsen
instance_of: Mountain
coordinates: lat: -67.233333333333
lon: 100.75
Navy air photos, 1960-64. So named by NZGSAE, 1969-70, because the ridge is rather flat on top and provides easy traversing. MacDonald Nunataks. Two nunataks overlooking the head of the Ross Ice Shelf, standing just east of the terminus of Amundsen Glacier, west of O'Brien Peak. Mapped by USGS from surveys and USN air photos, 1960-64. Named by US-ACAN for John A.

Geographic entities mentioned:
surface_form: amundsen
instance_of: Mountain
coordinates: lat: -67.233333333333
lon: 100.75
Medina Peaks. The Medina Peaks () are rugged, mainly ice-free, peaks surmounting a ridge long, extending north along the east side of Goodale Glacier to the edge of the Ross Ice Shelf, Antarctica. Discovery and naming. Some of the peaks were first seen and roughly mapped by the Byrd Antarctic Expedition, 1928–30.

Geographic entities mentioned:
surface_form: discovery
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: discovery
instance_of: Body of water
coordinates: lat: -64.5167
lon: -63.0167
Marks Point. A rock point extending east from the north end of Medina Peaks, at the south edge of the Ross Ice Shelf. This feature and nearby area were first seen by members of the Byrd Antarctic Expedition, 1928-30. Named by US-ACAN for George R. Marks, logistics worker at McMurdo Station, winter party, 1962. Coloured Peak.

Geographic entities mentioned:
surface_form: george
instance_of: Mountain
coordinates: lat: -67.71667
lon: 50
Westwood Plateau. Westwood Plateau is a neighbourhood in the northern region of Coquitlam, British Columbia. It is named for Westwood Motorsport Park which existed on the plateau before the community was built, and was closed in 1990 to make way for real estate development. Hampton Park Elementary School was built on top of the actual raceway. History.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: westwood plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 49.3
lon: -122.783
Geography. Westwood Plateau is bounded by the city boundary with Port Moody to the west, David Avenue to the south, and Pipeline Road to the east. It lies on on the southern portion of Eagle Mountain. Although touted as a plateau, the area is actually sloped rising from between 60 and 100 metres above sea level to almost 400 metres.

Geographic entities mentioned:
surface_form: eagle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.3478
lon: -122.83
surface_form: eagle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.10001
lon: -115.75211
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Travel times on bus to Downtown Port Moody or Coquitlam Town Centre are 15–20 minutes. The West Coast Express commuter rail service to Downtown Vancouver leaves from Coquitlam and Port Moody during weekday peak, and frequent rapid transit on Vancouver's SkyTrain network can be accessed from Lafarge Lake–Douglas station, Lincoln station, and Coquitlam Central station. Recreation & Leisure.

Geographic entities mentioned:
surface_form: lafarge lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.287
lon: -122.789
Westwood Plateau. Westwood Plateau is a neighbourhood in the northern region of Coquitlam, British Columbia. It is named for Westwood Motorsport Park which existed on the plateau before the community was built, and was closed in 1990 to make way for real estate development. Hampton Park Elementary School was built on top of the actual raceway. History.

Geographic entities mentioned:
surface_form: westwood plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 49.3
lon: -122.783
Hampton Park Elementary School was built on top of the actual raceway. History. The area currently known as Westwood Plateau was crown land purchased by Wesbild Corp. in 1989, and between then and 2005 transformed the area into a residential community of 4525 homes and in 2010 is home to about 15,000 residents. Geography.

Geographic entities mentioned:
surface_form: westwood plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 49.3
lon: -122.783
in 1989, and between then and 2005 transformed the area into a residential community of 4525 homes and in 2010 is home to about 15,000 residents. Geography. Westwood Plateau is bounded by the city boundary with Port Moody to the west, David Avenue to the south, and Pipeline Road to the east. It lies on on the southern portion of Eagle Mountain.

Geographic entities mentioned:
surface_form: westwood plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 49.3
lon: -122.783
Recreation & Leisure. Westwood Plateau has approximately of hiking trails. There are many parks in the area such as Bramble Park, Ridge Park, Panorama Park, North Hoy Creek Park, and Hampton Park. There are also two golf courses, Westwood Plateau Golf & Country Club and Westwood Plateau Executive 12-Hole Course.

Geographic entities mentioned:
surface_form: westwood plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 49.3
lon: -122.783
Recreation & Leisure. Westwood Plateau has approximately of hiking trails. There are many parks in the area such as Bramble Park, Ridge Park, Panorama Park, North Hoy Creek Park, and Hampton Park. There are also two golf courses, Westwood Plateau Golf & Country Club and Westwood Plateau Executive 12-Hole Course.

Geographic entities mentioned:
surface_form: westwood plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 49.3
lon: -122.783
surface_form: westwood plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 49.3
lon: -122.783
It is one of the 324 fish species found in Tennessee, United States. Geographic distribution. The species is found in the Coosa River in Georgia and Tennessee, the upper reaches of the Conasauga River, and the Etowah River. Ecology. The Bridled darter is a small freshwater fish only found in southern states.

Geographic entities mentioned:
surface_form: Coosa River
instance_of: Watercourse
countries: United States
coordinates: lat: 32.4862464
lon: -86.2777475
History. This area was settled by members of the three Algonquian-speaking tribes of the Council of Three Fires: the Potawatomi, Odawa, and Chippewa (known as Ojibwa in Canada). French explorers in a party led by Father Hennepin came upriver from Lake Michigan in 1679. A Jesuit mission was established near where the French later built Fort St. Joseph, and they named the waterway as the St.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Wye Valley Brewery. Wye Valley Brewery is a brewery in the village of Stoke Lacy, Herefordshire, England, in the Wye Valley. Founded in 1985 by Peter Amor, it has become &quot;one of Britain's leading independent breweries&quot;. In 2002 Peter Amor's son, Vernon Amor, became managing director. History and location.

Geographic entities mentioned:
surface_form: Wye Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69255
lon: -2.66283
Fletcher Bluff. lrk7e9s94ul915jn1vg7rpihqeq4" xml:space="preserve">Fletcher Bluff () is a rock-faced, snow-backed bluff, about high, located west-northwest of the summit of Mount Liotard on the eastern margin of Fuchs Ice Piedmont, Adelaide Island. It was named in 1983 by the UK Antarctic Place-Names Committee after David D.W.

Geographic entities mentioned:
surface_form: Mount Liotard
instance_of: Mountain
coordinates: lat: -67.6167
lon: -68.5667
surface_form: Fuchs Ice Piedmont
instance_of: Landform
coordinates: lat: -67.1667
lon: -68.6667
&quot;Mesogobius batrachocephalus&quot;, the knout goby or toad goby, is one of the species of gobiid fish native to the Black Sea and the Sea of Azov basins. It lives in estuaries and brackish water lagoons, occasionally in fresh waters, such as the coastal Lake Siutghiol in Romania. It prefers areas near cliffs with sandy, shelly or rocky substrates at depths of from, sometimes down to.

Geographic entities mentioned:
surface_form: Lake Siutghiol
instance_of: Lake
countries: Romania
coordinates: lat: 44.246388888889
lon: 28.6
But the image of Denali from the hills above the rapids of the Tokositna River became his trademark. It is this image more than any other which personifies Laurence for his many admirers and collectors in Alaska and beyond. Laurence forged a uniquely personal style by applying the tonalist techniques he had learned in New York and Europe to the wilderness of the North.

Geographic entities mentioned:
surface_form: Denali
instance_of: Mountain
countries: United States
coordinates: lat: 63.06916666666667
lon: -151.0063888888889
Others say that it was founded by Pal Parmar whose brother Jagdev founded nearby Jagana village. It seems probable that, falling waste about the time of the conquest (1303) of Abu and Chandravati by the Devra Chauhans, it may have been re-peopled by Palansi. The local legends give the city a much higher antiquity, placing its re-founding under its present name as far back as the fifth century.

Geographic entities mentioned:
surface_form: Abu
instance_of: Mountain
countries: India
coordinates: lat: 24.5925
lon: 72.708333333333
Geißhorn. Geißhorn () is a mountain in the Allgäu Alps of Bavaria, Germany.

Geographic entities mentioned:
surface_form: geißhorn
instance_of: Mountain
countries: Germany
Austria
coordinates: lat: 47.287777777778
lon: 10.175277777778
Fritaja. &quot;Fritaja&quot; (Croatian) or &quot;frtalja&quot; (Slovenian) is a Mediterranean Croatian and Slovenian dish. Both are specialties in Istria and north from Trieste in Goriška Brda and in Soča and Vipava Valleys.

Geographic entities mentioned:
surface_form: Vipava Valley
instance_of: Valley
countries: Slovenia
coordinates: lat: 45.876147222222
lon: 13.907319444444
The trail, which starts and begins in neighborhoods, can be reached from its trailheads at Highgate Road and Denver Springs Drive. Besides mountain and lake views, the ridgeline trail also offers views of the Conejo Valley and the Santa Monica Mountains. A variety of highpoints can be found along the trail, which has a total elevation gain of 500 ft.

Geographic entities mentioned:
surface_form: Conejo Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
The range is northwest-southeast trending, about in length. The range borders the Buenos Aires National Wildlife Refuge to the west; both are in the southeast of the Altar Valley. The southeast of the range abuts &quot;Cobre Ridge&quot;, with various peaks, and Cobre Ridge borders the western edge of the Pajarito Wilderness, at the west end of the Pajarito Mountains.

Geographic entities mentioned:
surface_form: Altar Valley
instance_of: Valley
countries: United States
coordinates: lat: 31.82
lon: -111.4
Owned and operated by the government-owned Canadian Broadcasting Corporation, CBM-FM is a Class C1 station. It transmits from the Mount Royal candelabra tower with an effective radiated power of 100,000 watts, using horizontal polarization. Its studios and offices, along with those of CBC Radio One sister station CBME-FM, are located at Maison Radio-Canada on René Lévesque Boulevard. History.

Geographic entities mentioned:
surface_form: Mount Royal
instance_of: Mountain
countries: Canada
coordinates: lat: 45.506388888889
lon: -73.588888888889
Toornaarsuttoq. Toornaarsuttoq is a mountain of Greenland. It is located in the Upernavik Archipelago.

Geographic entities mentioned:
surface_form: toornaarsuttoq
instance_of: Mountain
countries: Greenland
Newlands Church. Newlands Church is a 16th-century church situated less than 500 metres west of the hamlet of Little Town, Cumbria, England in the Newlands Valley of the Lake District. Its exact date of origin is unknown, but a map of 1576 shows a &quot;Newlande Chap.&quot; on the site.

Geographic entities mentioned:
surface_form: Newlands Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.573011111111
lon: -3.1848694444444
Location. The whitewashed roughcast Church of Newlands lies in open countryside some west of the hamlet of Little Town, Cumbria, England near the confluence of Newlands Beck, Scope Beck, and Keskadale Beck in the Lake District National Park and by road from Keswick. It is situated in the Newlands Valley, separated from Derwent Water to the east by the summit of Catbells.

Geographic entities mentioned:
surface_form: Newlands Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.573011111111
lon: -3.1848694444444
Only primary schooling is available. The majority 98% of the population of the commune are farmers. The most important crop is rice, while other important products are bananas, coffee and cassava. Services provide employment for 1.5% of the population. Additionally fishing employs 0.5% of the population. Geography. Mahavelo lies on the Manampatrana River.

Geographic entities mentioned:
surface_form: Manampatrana River
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -22.81944444
lon: 47.81666667
This collision primarily happened during the Miocene and folded the entire rocks that had been deposited from the Carboniferous to the Miocene in the geosyncline in front of the Iranian plate. The process of collision continues to the present and as the Arabian plate is being pushed against the Iranian plate, the Zagros Mountains and the Iranian plateau are getting higher and higher.

Geographic entities mentioned:
surface_form: Iranian plateau
instance_of: Plateau
countries: Iran
coordinates: lat: 36.283333
lon: 59.05
The peak of this volcanism happened in the Eocene. The Sahand-Bazman volcanic belt is supposed to have resulted from the collision of the Arabian and Central Iranian continental plate margins. It is represented by sub-alkaline volcanics that vary in composition from basaltic through andesitic to rhyolitic composition. Central Iran.

Geographic entities mentioned:
surface_form: Sahand
instance_of: Mountain
countries: Iran
coordinates: lat: 37.73
lon: 46.5
surface_form: Bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
Alborz. The Alborz mountain range forms a barrier between the south Caspian and the Iranian plateau. This range is located in northern Iran, parallel to the southern margin of Caspian Sea. Alborz is characterized by the dominance of platform-type sediments, including limestone, dolomite, and clastic rocks.

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
They are mainly alkaline in nature and are more abundant in Sanandaj–Sirjan. In Jurassic–Cretaceous, intrusive rocks exceed volcanic rocks; a significant number of batholiths in Iran occurred at this time. Kolah Ghazi, Shir Kuh, and Shah Kuh were formed by Jurassic granite; and Mount Alvand was made by Upper Cretaceous-Paleocene granite. Cenozoic.

Geographic entities mentioned:
surface_form: Shir Kuh
instance_of: Mountain
countries: Iran
coordinates: lat: 31.60388888888889
lon: 54.06611111111111
Some of the more important regions in terms of the Tertiary magmatic activities include: Sahand-Bazman (or Urumiyeh-Dokhtar) volcanic-plutonic belt with a series of famous mountain ranges including the Karkas Mountains and Jebal Barez and important peaks such as Karkas, Marshenan, Hezar and Lalehzar.

Geographic entities mentioned:
surface_form: Sahand
instance_of: Mountain
countries: Iran
coordinates: lat: 37.73
lon: 46.5
surface_form: Bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
surface_form: Marshenan
instance_of: Mountain
countries: Iran
coordinates: lat: 37.728
lon: 46.501
surface_form: Lalehzar
instance_of: Mountain
countries: Iran
The Tertiary magmatism could also be observed in Azerbaijan, Tarom–Taleghan, Central Alborz and its southern margins, Kavir–Sabzevar, Kashmar–Torbat-e Jam, Lut and Kavir, Central Iran, Sistan, Bam, Bazman, Taftan, East Iran, and Southern Jazmurian–Sabzevaran. The Quaternary volcanism produced very high peaks such as Sahand, Sabalan, Damavand, Taftan, Bazman and many others.

Geographic entities mentioned:
surface_form: Sahand
instance_of: Mountain
countries: Iran
coordinates: lat: 37.73
lon: 46.5
surface_form: Sabalan
instance_of: Mountain
countries: Iran
coordinates: lat: 38.266944444444
lon: 47.836944444444
surface_form: Bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
This event was associated with compressional tectonics in the northern Iran and tensional tectonics in the south. There is evidence that the compressional phase was preceded by tension and rift development. The compressional phase, happening in the Late Triassic, finally led to the closure of the Paleotethys (e.g., southeast to southwest of Caspian Sea).

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
Alpine (Pyrenean and Styrian). With regards to the geological evidence, this event was of compressional nature. This tectonic phase is represented by significant changes in the sedimentary environments, plutonism, and metamorphism (e.g., west of Central Iran, south of Central Alborz, Lut). The Sahand-Bazman volcanic arc or belt was mainly formed during the Eocene volcanism of the Alpine orogeny.

Geographic entities mentioned:
surface_form: Sahand
instance_of: Mountain
countries: Iran
coordinates: lat: 37.73
lon: 46.5
surface_form: Bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
The Pasadenian orogeny is the most important phase in forging the current shape of Iran. Some younger orogenic events might be the continuation of this orogenic phase (e.g., Alborz–Azerbaijan axis, Zagros, Central Iran). Sahand, Sabalan, Damavand, Bazman and Taftan were mainly formed during the volcanism of this orogenic phase. With an elevation of, Mount Damavand is the highest peak in Iran.

Geographic entities mentioned:
surface_form: Sahand
instance_of: Mountain
countries: Iran
coordinates: lat: 37.73
lon: 46.5
surface_form: Sabalan
instance_of: Mountain
countries: Iran
coordinates: lat: 38.266944444444
lon: 47.836944444444
surface_form: Bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
Sahand, Sabalan, Damavand, Bazman and Taftan were mainly formed during the volcanism of this orogenic phase. With an elevation of, Mount Damavand is the highest peak in Iran. This volcano first erupted in the Pleistocene about 1.78 million years ago and after several known eruptions around 600,000 and 280,000 years ago, it finally erupted in the Holocene almost 7300 years ago.

Geographic entities mentioned:
surface_form: Mount Damavand
instance_of: Mountain
countries: Iran
coordinates: lat: 35.955277777778
lon: 52.109166666667
Piz Ner. Piz Ner is a mountain of the Glarus Alps, located north of Trun in the canton of Graubünden. It lies in the group south of Piz Urlaun.

Geographic entities mentioned:
surface_form: Piz Urlaun
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.796472222222
lon: 8.9281111111111
Piz Ner. Piz Ner is a mountain of the Glarus Alps, located north of Trun in the canton of Graubünden. It lies in the group south of Piz Urlaun.

Geographic entities mentioned:
surface_form: piz ner
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.768944444444
lon: 8.948
The manuscript was preserved in the Chudov Monastery, till it was discovered by church historian Nikolay Kedrov. In his road journal, later published under the title &quot;Travels through Siberia to the Chinese borders&quot;, Milescu correctly described the middle course of the Ob, Irtysh, and Angara rivers. He assumed the Ob to have its source in Lake Teletskoye in the Altai Mountains.

Geographic entities mentioned:
surface_form: Lake Teletskoye
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 51.529166666667
lon: 87.714722222222
He assumed the Ob to have its source in Lake Teletskoye in the Altai Mountains. He was also the first person to describe Lake Baikal and all the rivers feeding the lake, and the first to point out Baikal's unfathomable depth. His works became popular with Russian elites, being found in their collections for the next century.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Pelican Lake (California). Pelican Lake is a small lake in the southern portion of the Point Reyes National Seashore, northwest of Bolinas. The lake sits at an elevation of and has an outflow via the short Pelican Lake Creek southwest through a notch in the coastal cliffs onto Double Point's Bolsa Beach.

Geographic entities mentioned:
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 46.57611111
lon: -94.17611111
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 45.5041
lon: -89.2035
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 37.95017
lon: -122.77537
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 46.6985
lon: -96.0198
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 48.0611
lon: -92.9
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 46.05777778
lon: -95.80222222
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 44.0925246
lon: -96.9136823
Pelican Lake is a small lake in the southern portion of the Point Reyes National Seashore, northwest of Bolinas. The lake sits at an elevation of and has an outflow via the short Pelican Lake Creek southwest through a notch in the coastal cliffs onto Double Point's Bolsa Beach. Pelican Lake is one of the five Coast Trail Lakes, along with Bass Lake, Crystal Lake, Ocean Lake and Wildcat Lake.

Geographic entities mentioned:
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 46.57611111
lon: -94.17611111
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 45.5041
lon: -89.2035
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 37.95017
lon: -122.77537
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 46.6985
lon: -96.0198
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 48.0611
lon: -92.9
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 46.05777778
lon: -95.80222222
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 44.0925246
lon: -96.9136823
Geology. As with the other nearby lakes in the southeast portion of the Point Reyes peninsula, Pelican Lake occupies a natural synclinal depression formed behind blocks of rock displaced by landslides within the past 10,000 years. The depressions forming Crystal, Pelican and Bass lakes appear to have been caused by the Double Point Slide, which covers an area of about.

Geographic entities mentioned:
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 46.57611111
lon: -94.17611111
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 45.5041
lon: -89.2035
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 37.95017
lon: -122.77537
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 46.6985
lon: -96.0198
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 48.0611
lon: -92.9
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 46.05777778
lon: -95.80222222
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 44.0925246
lon: -96.9136823
The process that caused these slides is ongoing, with several nearby slides caused by the 1906 San Francisco earthquake and others as recently as 1956. Prior to geological research in the 1960s, the area was considered to be sufficiently stable for the United States Army to construct an underground artillery control facility within the North Point headland directly west of Pelican Lake in 1944.

Geographic entities mentioned:
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 46.57611111
lon: -94.17611111
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 45.5041
lon: -89.2035
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 37.95017
lon: -122.77537
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 46.6985
lon: -96.0198
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 48.0611
lon: -92.9
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 46.05777778
lon: -95.80222222
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 44.0925246
lon: -96.9136823
The timing of their movement has been attributed to a thrust into northern Syria by the Mongol &quot;noyan&quot; Yasa'ur. They numbered 10,000 troops, including the Kurdish contingent. Dividing into two groups, they advanced into Palestine through the Biqa' and the Ghuta. At their approach, the allied forces that had been arrayed against Egypt retreated.

Geographic entities mentioned:
surface_form: Biqa'
instance_of: Valley
countries: Lebanon
coordinates: lat: 34.008888888889
lon: 36.145277777778