Sarmila/GeoWiki-Features huggingface dataset:
It occurs within metamorphically altered limestone adjacent to igneous intrusive rocks or within xenoliths. It also occurs as weathering crusts on larnite in the Hatrurim Formation of Israel. It occurs associated with portlandite, afwillite and hydrocalumite at Scawt Hill, Ireland and with afwillite, hydrocalumite, mayenite and gypsum in the Hatrurim Formation.

Geographic entities mentioned:
surface_form: Scawt Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.9105
lon: -5.9154
Further X-ray studies ensued; namely Wellin (1956) which determined the crystal structure of thaumasite, and Besjak and Jelenic (1966) which gave confirmation of the structure nature of ettringite. An ettringite sample extracted from Scawt Hill was analysed by C. E.

Geographic entities mentioned:
surface_form: Scawt Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.9105
lon: -5.9154
Lafont River. The Lafont River (&quot;in French: rivière Lafont&quot;) is a tributary on the northeast shore of the Nicolet Southwest River. It crosses the municipalities of Saint-Léonard-d'Aston and Sainte-Perpétue, in the Nicolet-Yamaska Regional County Municipality (MRC), in the administrative region of Centre-du-Québec, in Quebec, in Canada. Geography.

Geographic entities mentioned:
surface_form: Nicolet Southwest River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.21666666666667
lon: -72.60138888888889
Geography. The Lafont River takes its source in an agricultural zone near the railway, at the limit of the municipalities of Saint-Léonard-d'Aston and Sainte-Perpétue. This area is located on the southwest shore of the Nicolet River, southwest of the village of Saint-Léonard-d'Aston and east of the village of Sainte-Perpétue.

Geographic entities mentioned:
surface_form: Nicolet River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.255
lon: -72.6525
This area is located on the southwest shore of the Nicolet River, southwest of the village of Saint-Léonard-d'Aston and east of the village of Sainte-Perpétue. The Lafont River empties on the north bank of the Nicolet Southwest River at upstream of the bridge in the village of Sainte-Brigitte-des-Saults and at downstream of the Mitchell hamlet railway bridge. Toponymy.

Geographic entities mentioned:
surface_form: Nicolet Southwest River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.21666666666667
lon: -72.60138888888889
South Sentinel Island. South Sentinel Island is one of the Andaman Islands in the Bay of Bengal. It is long northeast to southwest and up to wide. At only, it is much smaller than its counterpart North Sentinel Island and is currently uninhabited.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
for the Minnewaska and Mohonk visitors&quot;. President Chester A. Arthur visited the station with his daughter in 1884. He was welcomed by the railroad's director and brought to Lake Mohonk. President Rutherford B. Hayes occasionally attended conferences at the Mohonk Mountain House. In 1892, several townspeople held a reception for him at the station, giving him &quot;three rousing cheers&quot;.

Geographic entities mentioned:
surface_form: Lake Mohonk
instance_of: Lake
countries: United States
coordinates: lat: 41.766111111111
lon: -74.156944444444
Woodlake, California. Woodlake is a city in Tulare County, California, United States. It is situated in the San Joaquin Valley near the foothills of the Sierra Nevada. The population was 7,419 at the 2020 census, up from 7,279 at the 2010 census. In 1912, the city of Woodlake was founded by Gilbert F. Stevenson. Geography.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Cheongpyeong Lake. Cheongpyeong Lake () is a clear water artificial lake in Cheongpyeong, Gapyeong County, and Gyeonggi Province, South Korea. It was created with the construction of Cheongpyeong Dam in 1944 to block the Bukhangang River. It is located 50 kilometers (30 miles) away from Seoul, the capital of South Korea.

Geographic entities mentioned:
surface_form: cheongpyeong lake
instance_of: Lake
countries: South Korea
coordinates: lat: 37.708
lon: 127.457
The lake has an area of, a full water area of, and a water storage capacity of 180 million tons. In 1977, it was designated as a marine protected area but this was lifted in November 1984. The lake is surrounded by mountains. Near Cheongpyeong Lake is an amusement park as well as a number of summer homes. Nearby the lake there is water skiing and other recreational activities.

Geographic entities mentioned:
surface_form: cheongpyeong lake
instance_of: Lake
countries: South Korea
coordinates: lat: 37.708
lon: 127.457
Near Cheongpyeong Lake is an amusement park as well as a number of summer homes. Nearby the lake there is water skiing and other recreational activities. Around Cheongpyeong Lake, there are approximately 30 boating areas for water skiing, motorboats, Jet Skis, banana boats, fly fishing, and other water activities. The tourist season is from July to August, accounting for 64.5% of annual footfall.

Geographic entities mentioned:
surface_form: cheongpyeong lake
instance_of: Lake
countries: South Korea
coordinates: lat: 37.708
lon: 127.457
Around Cheongpyeong Lake, there are approximately 30 boating areas for water skiing, motorboats, Jet Skis, banana boats, fly fishing, and other water activities. The tourist season is from July to August, accounting for 64.5% of annual footfall. Cheongpyeong Lake is listed as part of the 'Eight Scenic Views of Gapyeong' (가평팔경; 加平八景), alongside Chungnyungsan's pine forest.

Geographic entities mentioned:
surface_form: cheongpyeong lake
instance_of: Lake
countries: South Korea
coordinates: lat: 37.708
lon: 127.457
surface_form: chungnyungsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 37.75277778
lon: 127.33305556
It includes numerous salt and fresh water bodies. The main rivers are the Nura and Kulanotpes, and the biggest lake is Lake Tengiz, followed by Korgalzhyn, after which the nature reserve is named. Other lakes of the protected area are Kerey, Kypshak, Asaubalyk, Zhamankol, Zhabay Tabankazy, Manat, Saumalkol and Toktamys. History.

Geographic entities mentioned:
surface_form: Lake Tengiz
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.439722222222
lon: 68.9
It includes numerous salt and fresh water bodies. The main rivers are the Nura and Kulanotpes, and the biggest lake is Lake Tengiz, followed by Korgalzhyn, after which the nature reserve is named. Other lakes of the protected area are Kerey, Kypshak, Asaubalyk, Zhamankol, Zhabay Tabankazy, Manat, Saumalkol and Toktamys. History.

Geographic entities mentioned:
surface_form: Kypshak
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.15
lon: 68.4
Lake Svetloyar. Lake Svetloyar (= &quot;lake of the bright bank/ravine&quot;) is a lake in the Voskresensky District of the Nizhny Novgorod Oblast in central Russia. It is located within Voskresenskoe Povetluzhye Nature Park. In 2015, the lake was included in the Register of Cultural Heritage Objects as an object of cultural heritage of local significance.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake svetloyar
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 56.819166666667
lon: 45.091666666667
Lake Svetloyar. Lake Svetloyar (= &quot;lake of the bright bank/ravine&quot;) is a lake in the Voskresensky District of the Nizhny Novgorod Oblast in central Russia. It is located within Voskresenskoe Povetluzhye Nature Park. In 2015, the lake was included in the Register of Cultural Heritage Objects as an object of cultural heritage of local significance.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake svetloyar
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 56.819166666667
lon: 45.091666666667
It is located within Voskresenskoe Povetluzhye Nature Park. In 2015, the lake was included in the Register of Cultural Heritage Objects as an object of cultural heritage of local significance. It is closely associated with the Legend of Kitezh, a sunken city. Description. The lake is situated between the Kerzhenets and Vetluga rivers, both tributaries of the Volga.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The lake is oval in shape (470 × 350 m) with the longer axis aligned north-south. It reaches a depth of 33.4 m. Its deepest point is in the southern part of the lake, which rises to a shallow platform ranging in depth from 22 to 24 m. In the northern, relatively shallow part of the lake, the depth change is smoother comparatively. The surface of the lake is 109 m above sea level.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
It reaches a depth of 33.4 m. Its deepest point is in the southern part of the lake, which rises to a shallow platform ranging in depth from 22 to 24 m. In the northern, relatively shallow part of the lake, the depth change is smoother comparatively. The surface of the lake is 109 m above sea level. Its shores are somewhat elevated and the lake itself lies in a small basin.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
In the northern, relatively shallow part of the lake, the depth change is smoother comparatively. The surface of the lake is 109 m above sea level. Its shores are somewhat elevated and the lake itself lies in a small basin. The hills that encircle it are most prominent to the south, where they form an arc.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Its shores are somewhat elevated and the lake itself lies in a small basin. The hills that encircle it are most prominent to the south, where they form an arc. The height of the hills reaches 122–124 m above sea level (13–15 m above the lake's water level) and are separated by deep (7–8 m) ravines. The lake's water is transparent to a depth of more than 5 m.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The hills that encircle it are most prominent to the south, where they form an arc. The height of the hills reaches 122–124 m above sea level (13–15 m above the lake's water level) and are separated by deep (7–8 m) ravines. The lake's water is transparent to a depth of more than 5 m. The lake is said to be relatively cold and its banks are somewhat swampy.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The lake's water is transparent to a depth of more than 5 m. The lake is said to be relatively cold and its banks are somewhat swampy. To the north-east is the small, shallow Lunda River, to which the lake is connected by a stream. The runoff from the lake through the stream was disturbed during the construction of a road during the Soviet era. As a result, the lake began to swamp.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The lake is said to be relatively cold and its banks are somewhat swampy. To the north-east is the small, shallow Lunda River, to which the lake is connected by a stream. The runoff from the lake through the stream was disturbed during the construction of a road during the Soviet era. As a result, the lake began to swamp. Restoration of natural lake flow occurred in the 1990s.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The runoff from the lake through the stream was disturbed during the construction of a road during the Soviet era. As a result, the lake began to swamp. Restoration of natural lake flow occurred in the 1990s. In the 2000s, a number of studies confirmed the meteorite hypothesis of the origin of Svetloyar and some neighboring lakes.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
In the 2000s, a number of studies confirmed the meteorite hypothesis of the origin of Svetloyar and some neighboring lakes. In 2009, the results of field studies were published, confirming the hypothesis of the meteoric origin of the lake 3.0-3.2 thousand years ago. The volume of the lake basin (not the lake itself) is about 1.5 km, and the area of the lake itself is 14.83 hectares.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
In 2009, the results of field studies were published, confirming the hypothesis of the meteoric origin of the lake 3.0-3.2 thousand years ago. The volume of the lake basin (not the lake itself) is about 1.5 km, and the area of the lake itself is 14.83 hectares. The thickness of the bottom sediments is about 8 m. Origin.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The thickness of the bottom sediments is about 8 m. Origin. Various researchers during different timeframes have hypothesized about the glacial, karstic, old, volcanic, neotectonic, salt-dome, and meteorite origin of the lake. The first explorer of the lake in the late 19th century was a Russian geologist, Vasily Dokuchaev, who suggested it was a meteorite crater.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The first explorer of the lake in the late 19th century was a Russian geologist, Vasily Dokuchaev, who suggested it was a meteorite crater. The volcanic origin of the lake was first suggested in the early 20th century by the writer Vladimir Korolenko. Amateur archaeologist A. P.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
In 1969, under the leadership of Mark M. Barinov, scuba divers using sonar bathymetry detailed the complex structure of the relief of the bottom of the lake. The central pit-hollow is fringed by a system of two underwater terraces, expanding in the northern and narrowing in the southern parts of the lake and having depths of 18-20 and 9–10 m, respectively.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Based on this, it was concluded that the central basin was formed a little more than a millennium (about 1100–1200 years) ago in the form of a small lake with a depth of 15–17 m, and the immersion of the lower terrace occurred approximately 700–800 years ago. 19/9/2009 the origin of Svetloyar and some neighboring lakes.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
19/9/2009 the origin of Svetloyar and some neighboring lakes. In 2009, bolstered the hypothesis of the meteoric origin of the lake, around 3,000 years ago.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
In 2009, bolstered the hypothesis of the meteoric origin of the lake, around 3,000 years ago. The correct form, depth, the geological structure of the surrounding hills, the stratigraphy of bottom sediments, numerous fragments of fused rocks, rounded teardrop formations ejected from a foamy, black, vitreous mass, analogous to impactites, attest to the meteorite origin of the lake.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Media coverage. In 1993, the creative association &quot;Ekran&quot; () released the film &quot;The Tale of the Great and Invisible City of Kitezh&quot; (writer and director V. Kukushkin), about &quot;the mythological roots and the search for the invisible&quot; City of Kitezh under Lake Svetloyar.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake svetloyar
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 56.819166666667
lon: 45.091666666667
The film was shown on the first channel of Central Television in Easter on April 17, 1993, before the first television broadcast of the Easter service from the Epiphany Cathedral in Moscow. In literature. The elders and reverend mothers of the skete (monastery) were scandalised... &quot;Why&quot;, said they, &quot;this nightly splashing in the waters of the lake?

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
&quot;the bright bank&quot; or &quot;the ravine of light /of Yarilo(?)&quot;) and the hills above it to be &quot;holy places&quot;...&quot;Here&quot; said they, &quot;there is a beautiful city, home to God's saints, the city of Great Kitezh...But, because we humans are all sinners, it is invisible to us - we cannot see its beauty - and if you (lay-folk) persist in your devilish practices the place will be polluted by your foul deeds...&quot;
And the God-fearing elders and honorable mothers began to visit Lake Svetloyar, bearing holy books, crosses and icons to its shores...They began to read the psalter and sing canons on the shores of the lake, fabricated the &quot;Chronicle of Kitezh&quot; and began to read it to the people who came to the lake to celebrate the pagan rites of Yarilo.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake svetloyar
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 56.819166666667
lon: 45.091666666667
Rugby career. Although little is recorded about Jones, he is listed as originally playing rugby for Porth Scarlets a now defunct Rhondda club. By the time he was selected to represent Wales in 1902, he was playing club rugby for Penygraig RFC, a more successful valley club that had supplied several players to the international squad since 1896.

Geographic entities mentioned:
surface_form: Rhondda
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
His stunts for James Bond films included tobogganing down the Cresta Run in &quot;On Her Majesty's Secret Service,&quot; doubling for George Lazenby, and later for Roger Moore in a cable car fight scene 1,000 ft above ground on Sugarloaf Mountain, Brazil, in &quot;Moonraker.&quot; At in height, Graydon was shorter than Moore, but it was necessary to maintain the height difference with the stuntman doubling for the Richard Kiel, who played Jaws.

Geographic entities mentioned:
surface_form: Sugarloaf Mountain
instance_of: Mountain
countries: Brazil
coordinates: lat: -22.949444444444445
lon: -43.156666666666666
Kelabit Highlands. The Kelabit Highlands are a mountain range located in the northernmost part of Sarawak, Malaysia in the Miri Division. It hosts the Bario village. The highest mountains in this range are Mount Murud at, Bukit Batu Buli at, and Bukit Batu Lawi at. The current population of the Kelabit people is about 6,800.

Geographic entities mentioned:
surface_form: Mount Murud
instance_of: Mountain
countries: Malaysia
coordinates: lat: 3.9166666666667
lon: 115.33333333333
The US Air Force and Arnold Engineering Development Center own and operate Woods Reservoir. The dam itself is just under 3,000 feet long and holds back 26 billion gallons of water on a reservoir. The water is used to help the Arnold Air Force Base with cooling of their wind-tunnel equipment. Water exiting from the dam flows along the Elk River into Tims Ford Lake.

Geographic entities mentioned:
surface_form: Tims Ford Lake
instance_of: Lake
countries: United States
coordinates: lat: 35.196944444444
lon: -86.278611111111
Steamboats of Lake Chelan. Lake Chelan is a long, glacially-carved lake in the central part of the North Cascades mountain range in northwestern Washington State. Via the short Chelan River, it is a tributary to the Okanogan River, a tributary of the Columbia. Access to points along the lake has been primarily by water, and in the early 1900s, this was done by steamboat.

Geographic entities mentioned:
surface_form: Lake Chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
River Slaney. The River Slaney (;) is a large river in the southeast of Ireland. It rises on Lugnaquilla Mountain in the western Wicklow Mountains and flows west and then south through counties Wicklow, Carlow and Wexford for 117.5 km (73 mi), before entering St George's Channel in the Irish Sea at Wexford town. The estuary of the Slaney is wide and shallow and is known as Wexford Harbour.

Geographic entities mentioned:
surface_form: Lugnaquilla Mountain
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.966
lon: -6.463
Boney Point. 847gapop0a0d27igt2uq90fanb19" xml:space="preserve">Boney Point () is a rock headland along the south side of the entrance to Tripp Bay in Victoria Land. It was named in association with nearby Brough Nunatak after Lieutenant Commander B.E. Boney, U.S. Navy, captain of USS &quot;Brough&quot; in Antarctic waters in Operation Deep Freeze IV, 1958–59.

Geographic entities mentioned:
surface_form: Brough Nunatak
instance_of: Mountain
coordinates: lat: -76.5167
lon: 162.45
Povlen. Povlen () is a mountain in western Serbia, located thirty kilometers west of Valjevo. It has several peaks, the three most important being Small Povlen (), Middle Povlen () and Big Povlen (), which is, ironically, the lowest. Geography. It belongs to the Valjevo mountain range, which form the highland west of Valjevo towards Mačva.

Geographic entities mentioned:
surface_form: valjevo
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.150278
lon: 19.691111
surface_form: povlen
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.132777777778
lon: 19.748888888889
It has several peaks, the three most important being Small Povlen (), Middle Povlen () and Big Povlen (), which is, ironically, the lowest. Geography. It belongs to the Valjevo mountain range, which form the highland west of Valjevo towards Mačva. The mountains are not very high, their highest point, Small Povlen, reaches to, but they are difficult to cross.

Geographic entities mentioned:
surface_form: valjevo
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.150278
lon: 19.691111
surface_form: valjevo
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.150278
lon: 19.691111
History. In November 2019 it was announced that the remains of the Byzantine church were discovered. The object was discovered close to the Taor Springs, some from Valjevo. Remains of the Early Byzantium-style church are part of the wider complex, with parts of small fortification and presumably a mining settlement being located for now.

Geographic entities mentioned:
surface_form: valjevo
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.150278
lon: 19.691111
In the surrounding area there are numerous traces of ancient mining activities, including mining of copper and iron. Also, this is the fourth such church discovered in the Valjevo region in the past several years. In the village of Brangović there are remains of the fortification, called Jerinin Grad, with the remains of the church quite similar to the one discovered in Taor.

Geographic entities mentioned:
surface_form: valjevo
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.150278
lon: 19.691111
Beautiful cascades were used in many touristic brochures in the Former Yugoslavia. They are located at the village of Taor's hamlet of Donji Taor. It is located in the southwestern section of the mountain, southeast of Valjevo and northwest of Kosjerić. Majority of the location is covered in beech forests and the location is especially known for bear's garlic, which is abundant.

Geographic entities mentioned:
surface_form: valjevo
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.150278
lon: 19.691111
In the canyon of Trešnjica under Povlen, there is a colony of griffon vultures. Eagles and hawks also live on the mountain. Successful program of brown bears protection was conducted on the Tara mountain in the 21st century, some southwest of the Povlen. As the number of bears grew, by the 2020s they re-appeared on the Povlen, too. History.

Geographic entities mentioned:
surface_form: tara
instance_of: Mountain
countries: Serbia
coordinates: lat: 43.84833334
lon: 19.45944445
surface_form: povlen
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.132777777778
lon: 19.748888888889
Povlen. Povlen () is a mountain in western Serbia, located thirty kilometers west of Valjevo. It has several peaks, the three most important being Small Povlen (), Middle Povlen () and Big Povlen (), which is, ironically, the lowest. Geography. It belongs to the Valjevo mountain range, which form the highland west of Valjevo towards Mačva.

Geographic entities mentioned:
surface_form: povlen
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.132777777778
lon: 19.748888888889
Povlen. Povlen () is a mountain in western Serbia, located thirty kilometers west of Valjevo. It has several peaks, the three most important being Small Povlen (), Middle Povlen () and Big Povlen (), which is, ironically, the lowest. Geography. It belongs to the Valjevo mountain range, which form the highland west of Valjevo towards Mačva.

Geographic entities mentioned:
surface_form: povlen
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.132777777778
lon: 19.748888888889
surface_form: povlen
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.132777777778
lon: 19.748888888889
surface_form: povlen
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.132777777778
lon: 19.748888888889
Geography. It belongs to the Valjevo mountain range, which form the highland west of Valjevo towards Mačva. The mountains are not very high, their highest point, Small Povlen, reaches to, but they are difficult to cross. Dense forests and deep river canyons hide narrow and winding roads that lead to small hamlets. In the canyon of Trešnjica under Povlen, there is a colony of griffon vultures.

Geographic entities mentioned:
surface_form: povlen
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.132777777778
lon: 19.748888888889
The mountains are not very high, their highest point, Small Povlen, reaches to, but they are difficult to cross. Dense forests and deep river canyons hide narrow and winding roads that lead to small hamlets. In the canyon of Trešnjica under Povlen, there is a colony of griffon vultures. Eagles and hawks also live on the mountain.

Geographic entities mentioned:
surface_form: povlen
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.132777777778
lon: 19.748888888889
Eagles and hawks also live on the mountain. Successful program of brown bears protection was conducted on the Tara mountain in the 21st century, some southwest of the Povlen. As the number of bears grew, by the 2020s they re-appeared on the Povlen, too. History. In November 2019 it was announced that the remains of the Byzantine church were discovered.

Geographic entities mentioned:
surface_form: povlen
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.132777777778
lon: 19.748888888889
Located in the village of Ovčinja, the concrete and wood plateau include benches, parking spots and kiosk with vending and coffee machines. Taor Springs. One of the attraction of the Povlen are the &quot;Taor Springs&quot; (&quot;Taorska vrela&quot;). Beautiful cascades were used in many touristic brochures in the Former Yugoslavia. They are located at the village of Taor's hamlet of Donji Taor.

Geographic entities mentioned:
surface_form: povlen
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.132777777778
lon: 19.748888888889
Mythology. Area of Povlen is known for its myths. Southern extension of the now extinct Pannonian Sea, which drained out some 600,000 years ago, reached Povlen. Hence, fossils of the sea snails are occasionally being found, which influenced the myth about the massive ring, which allegedly exists somewhere on the mountain, by which Noah moored his ark after the deluge.

Geographic entities mentioned:
surface_form: povlen
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.132777777778
lon: 19.748888888889
Career and travels. De Steuben in 1812 debuted at the Salon de Paris with his painting of Peter the Great in the storm on Lake Ladoga, which garnered attention in the professional world. Encouraged by this first success, Steuben continued with a number of historical paintings. In 1820 he married a portrait painter named Eleanor Trollé, whom he had met during his training.

Geographic entities mentioned:
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
Lake Profound. Profound Lake or Lake Profound () is a lake northwest of Jasper Point in northeast Fildes Peninsula, King George Island. The feature was named &quot;Ozero Glubokoye&quot; (deep lake) by the Soviet Antarctic Expedition working from Bellingshausen Station from 1968, but both forms of the name are already in use in the Antarctic.

Geographic entities mentioned:
surface_form: bellingshausen
instance_of: Mountain
coordinates: lat: -75.1167
lon: 162.1
surface_form: ozero glubokoye
instance_of: Lake
coordinates: lat: -67.6667
lon: 45.8667
surface_form: glubokoye
instance_of: Lake
coordinates: lat: -67.6667
lon: 45.8667
surface_form: deep lake
instance_of: Lake
coordinates: lat: -77.56667
lon: 166.21667
surface_form: deep lake
instance_of: Lake
coordinates: lat: -68.56
lon: 78.19583
Lake Profound. Profound Lake or Lake Profound () is a lake northwest of Jasper Point in northeast Fildes Peninsula, King George Island. The feature was named &quot;Ozero Glubokoye&quot; (deep lake) by the Soviet Antarctic Expedition working from Bellingshausen Station from 1968, but both forms of the name are already in use in the Antarctic.

Geographic entities mentioned:
surface_form: george
instance_of: Mountain
coordinates: lat: -67.71667
lon: 50
surface_form: fildes
instance_of: Body of water
coordinates: lat: -62.2333
lon: -59
surface_form: lake profound
instance_of: Lake
coordinates: lat: -62.1833
lon: -58.9167
surface_form: profound lake
instance_of: Lake
coordinates: lat: -62.1833
lon: -58.9167
Lake Profound. Profound Lake or Lake Profound () is a lake northwest of Jasper Point in northeast Fildes Peninsula, King George Island. The feature was named &quot;Ozero Glubokoye&quot; (deep lake) by the Soviet Antarctic Expedition working from Bellingshausen Station from 1968, but both forms of the name are already in use in the Antarctic.

Geographic entities mentioned:
surface_form: lake profound
instance_of: Lake
coordinates: lat: -62.1833
lon: -58.9167
She made her maiden voyage as a cargo ship in 1896, transporting sugar from the West Indies, cocoa, and coffee from Brazil and French Guiana to Nantes, France. History. &quot;Belem&quot; escaped the eruption of Mount Pelée in Saint-Pierre, Martinique, on 8 May 1902. On arriving at Saint Pierre ahead of the eruption, Captain Julien Chauvelon found that roadsteads were full of vessels.

Geographic entities mentioned:
surface_form: Mount Pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
Then, from their base around Mount Lebanon and the Beqaa Valley, they expanded into the northern Golan and Mount Hermon, as part of the settlement shift that occurred as a result of the collapse of the Seleucid empire, though no evidence of Iturean settlement or &quot;phase&quot; of settlement appears in the Galilee, including Upper Galilee. Etymology.

Geographic entities mentioned:
surface_form: Beqaa Valley
instance_of: Valley
countries: Lebanon
coordinates: lat: 34.008888888889
lon: 36.145277777778
In these areas, the canker-resistant Arizona cypress is much more successful. In northern areas where heavy snows occur, this plant is also susceptible to broken branches and uprooting in wet, heavy snow. The tree has also been introduced in Kenya on parts of Mount Kenya. The sap can cause skin irritation in susceptible individuals. Commercialization.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
The trail began on Bellingham Bay, at Fairhaven (now a Bellingham neighbourhood), the route used went via a route known as the Columbia Valley, which is a lowland route connecting the mid-Nooksack River area with Cultus Lake and the lower Chilliwack River in the Upper Fraser Valley, about 80 km east of today's Vancouver. In 1858, T. G.

Geographic entities mentioned:
surface_form: Cultus Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.053333333333335
lon: -121.98694444444445
surface_form: Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
The name &quot;Whatcom&quot; comes from the Lummi place name &quot;x̣ʷátqʷəm&quot;, probably meaning &quot;noisy&quot; with reference to a waterfall. A more westerly route now in use for a major border crossing (at Sumas) was not usable due to the presence of Sumas Lake, a large shallow lake, now drained and turned into agricultural land.

Geographic entities mentioned:
surface_form: Sumas Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.07
lon: -122.09
Guasaule River. The Guasaule River () is a river in northern Nicaragua and southern Honduras.

Geographic entities mentioned:
surface_form: nicaragua
instance_of: Lake
countries: Nicaragua
coordinates: lat: 11.5742
lon: -85.3563
surface_form: guasaule river
instance_of: Watercourse
countries: Nicaragua
coordinates: lat: 13.0179384
lon: -86.9754751
Guasaule River. The Guasaule River () is a river in northern Nicaragua and southern Honduras.

Geographic entities mentioned:
surface_form: guasaule river
instance_of: Watercourse
countries: Nicaragua
coordinates: lat: 13.0179384
lon: -86.9754751
Topographic relief is significant as the summit rises above the Macaulay Valley in three kilometres, and above the Godley Valley in four kilometres. The nearest higher neighbour is Mount D'Archiac, nine kilometres to the north. The mountain's toponym honours Sea Captain William Sibbald, the first runholder at nearby Lilybank Station in 1868.

Geographic entities mentioned:
surface_form: Mount D'Archiac
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.465
lon: 170.582
Mount Sibbald. Mount Sibbald is a mountain in Canterbury, New Zealand. Description. Mount Sibbald is the highest point of the Sibbald Range which is a small subrange of the Southern Alps. It is located west of the city of Christchurch in the Canterbury Region of the South Island. Precipitation runoff from the mountain drains west into the Godley River and east to the Macaulay River.

Geographic entities mentioned:
surface_form: mount sibbald
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.552
lon: 170.555
Climate. Based on the Köppen climate classification, Mount Sibbald is located in a marine west coast (Cfb) climate zone, with a tundra climate at the summit. Prevailing westerly winds blow moist air from the Tasman Sea onto the mountains, where the air is forced upward by the mountains (orographic lift), causing moisture to drop in the form of rain or snow.

Geographic entities mentioned:
surface_form: mount sibbald
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.552
lon: 170.555
Description. The Witch Head is situated west of Zion's park headquarters, towering above the floor of Zion Canyon and the Virgin River, which drains precipitation runoff from this mountain. Its neighbors include The West Temple, The Sundial, Altar of Sacrifice, Meridian Tower, Bee Hive, and Three Marys.

Geographic entities mentioned:
surface_form: The West Temple
instance_of: Mountain
countries: United States
coordinates: lat: 37.210869
lon: -113.02071
surface_form: Altar of Sacrifice
instance_of: Mountain
countries: United States
coordinates: lat: 37.225934
lon: -113.019858
surface_form: three marys
instance_of: Mountain
countries: United States
coordinates: lat: 37.2083156
lon: -113.0118854
surface_form: meridian tower
instance_of: Mountain
countries: United States
coordinates: lat: 37.23109
lon: -113.00077
surface_form: sundial
instance_of: Mountain
countries: United States
coordinates: lat: 47.832961
lon: -123.227692
surface_form: the sundial
instance_of: Mountain
countries: United States
coordinates: lat: 37.21526
lon: -113.023
surface_form: bee hive
instance_of: Mountain
countries: United States
coordinates: lat: 37.2244897
lon: -112.9874313
The Witch Head. The Witch Head is a white Navajo Sandstone mountain in Zion National Park in Washington County, Utah, United States, that is part of the Towers of the Virgin. Description. The Witch Head is situated west of Zion's park headquarters, towering above the floor of Zion Canyon and the Virgin River, which drains precipitation runoff from this mountain.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: navajo
instance_of: Mountain
countries: United States
coordinates: lat: 37.034169444444
lon: -110.86888888889
surface_form: the witch head
instance_of: Mountain
countries: United States
coordinates: lat: 37.2198
lon: -113.019
The Witch Head. The Witch Head is a white Navajo Sandstone mountain in Zion National Park in Washington County, Utah, United States, that is part of the Towers of the Virgin. Description. The Witch Head is situated west of Zion's park headquarters, towering above the floor of Zion Canyon and the Virgin River, which drains precipitation runoff from this mountain.

Geographic entities mentioned:
surface_form: the witch head
instance_of: Mountain
countries: United States
coordinates: lat: 37.2198
lon: -113.019
Description. The Witch Head is situated west of Zion's park headquarters, towering above the floor of Zion Canyon and the Virgin River, which drains precipitation runoff from this mountain. Its neighbors include The West Temple, The Sundial, Altar of Sacrifice, Meridian Tower, Bee Hive, and Three Marys.

Geographic entities mentioned:
surface_form: the witch head
instance_of: Mountain
countries: United States
coordinates: lat: 37.2198
lon: -113.019
Climate. Spring and fall are the most favorable seasons to visit The Witch Head. 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: the witch head
instance_of: Mountain
countries: United States
coordinates: lat: 37.2198
lon: -113.019
In February 1896 he moved to the prestigious St Andrews Church in Edinburgh's New Town. He was then living at 13 Regent Terrace on Calton Hill in east Edinburgh. The University of Edinburgh gave him an honorary Doctor of Divinity (DD) in 1902. He lived his final years at 35 Great King Street in a large Georgian house in Edinburgh's New Town. Hunter died in Edinburgh on 26 December 1909.

Geographic entities mentioned:
surface_form: Calton Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.955278
lon: -3.182222
&quot;Ce&quot; refers to the territory of Cé, which is independently attested in three Irish sagas and in the name of the mountain Bennachie (), and so was probably located in the area of modern-day Aberdeenshire. &quot;Cirig&quot; is usually associated with the territory of Circin, which may have encompassed The Mearns or Strathearn or both.

Geographic entities mentioned:
surface_form: Bennachie
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.29275
lon: -2.56244
&quot;Ce&quot; refers to the territory of Cé, which is independently attested in three Irish sagas and in the name of the mountain Bennachie (), and so was probably located in the area of modern-day Aberdeenshire. &quot;Cirig&quot; is usually associated with the territory of Circin, which may have encompassed The Mearns or Strathearn or both.

Geographic entities mentioned:
surface_form: Strathearn
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.3325
lon: -3.6825
Grand Haven Golf Club. Grand Haven Golf Club is a public golf course located just south of Grand Haven, Michigan. Very close to the Lake Michigan shore, the golf course takes advantage of the thick hardwood forest and natural sand dunes of the southwest Michigan shoreline. Golf Digest magazine ranked the club as &quot;one of the nation's Top 50 public courses&quot; for over ten years.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Geography. As its name indicates, the city lies in the eastern portion of a lowland area that extends from the Ozark Highlands to the Mississippi River, covering much of the Bootheel. Missouri Route 80 connects East Prairie with Interstate 55 and Matthews to the west, and the rural areas near the Mississippi River to the east.

Geographic entities mentioned:
surface_form: Ozark Highlands
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
The park protects more than of rugged terrain boasting deep canyons, rivers, waterfalls, and scenic mountain peaks, including the Cerro de la Silla (&quot;Saddle Mountain&quot;), part of Monterrey's famous skyline. The park was created in 1939 under president Lázaro Cárdenas to protect the native flora and fauna against the spreading urbanization of the city of Monterrey.

Geographic entities mentioned:
surface_form: Cerro de la Silla
instance_of: Mountain
countries: Mexico
coordinates: lat: 25.627777777778
lon: -100.23905388889
Craignafeich Reservoirs. The Craignafeich Reservoirs (also “Craignafeoch”) are a pair of lochs in Archarossan Forest, 3 kilometres west of Tighnabruaich. The main concrete dam is 15.8 metres high, and was completed in 1972.

Geographic entities mentioned:
surface_form: craignafeich reservoirs
instance_of: Group of lakes
countries: United Kingdom
coordinates: lat: 55.915
lon: -5.2813
Mount Wakefield. Mount Wakefield is a mountain in Mount Cook National Park, South Island, New Zealand. It is high. The Mountain is named after Edward Gibbon Wakefield. Māori named the slopes and fans of debris of the mountain &quot;Kirikiri katata&quot;, kirikiri means stones or shingle; katata means split open. Aetherius Society.

Geographic entities mentioned:
surface_form: mount wakefield
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.693
lon: 170.124
Mount Wakefield. Mount Wakefield is a mountain in Mount Cook National Park, South Island, New Zealand. It is high. The Mountain is named after Edward Gibbon Wakefield. Māori named the slopes and fans of debris of the mountain &quot;Kirikiri katata&quot;, kirikiri means stones or shingle; katata means split open. Aetherius Society.

Geographic entities mentioned:
surface_form: mount wakefield
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.693
lon: 170.124
surface_form: mount cook
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.595
lon: 170.14194444444445
Aetherius Society. The Aetherius Society considers it to be one of its 19 holy mountains. According to the Aetherius Society, Mount Wakefield was charged with majestic spiritual powers by The Master Jesus, a Cosmic Master from the planet Venus. On Christmas Eve of 1960, George King climbed the mountain in order to act as a conduit for the power between The Master Jesus & Mount Wakefield.

Geographic entities mentioned:
surface_form: mount wakefield
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.693
lon: 170.124
MV Ilala. MV &quot;Ilala&quot;, formally &quot;Ilala II&quot;, is a ferry that has plied Lake Malawi in East Africa since 1951. Every week she crosses the lake all the way north to Chilumba, Malawi, near Tanzania (about from Monkey Bay) and then returns to Monkey Bay.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
History. The central part of the castle was built in the late 12th century, and the newer outer castle added onto at the start of the 13th century by Conrad de Landsberg to provide defence for the abbeys of Mont Sainte-Odile, Niedermunster, Truttenhausen and Andlau. More recent additions were made in the 15th century. Herrad of Landsberg was born here around 1130.

Geographic entities mentioned:
surface_form: Mont Sainte-Odile
instance_of: Mountain
countries: France
coordinates: lat: 48.437458
lon: 7.4044908
Rhine → Bijlands Kanaal → Pannerdens Kanaal → Nederrijn → Lek → Nieuwe Maas → Het Scheur → Nieuwe Waterweg. Since the Rhine contributes most of the water, the term &quot;Rhine Delta&quot; is commonly used, although this name is also used for the delta where the Alpine Rhine flows into Lake Constance. By some calculations, the Rhine–Meuse–Scheldt delta covers, making it the largest in Europe.

Geographic entities mentioned:
surface_form: Alpine Rhine
instance_of: Valley
countries: Switzerland
Austria
Liechtenstein
coordinates: lat: 47.07013888888889
lon: 9.483347222222223
It is also bounded by the Berliner localities of Köpenick and Rahnsdorf. The residential area is surrounded in north by a big portion of the &quot;Berliner Stadtforst&quot; (city forest), and in south by the river Müggelspree (tributary of the Spree), and by the western side of Müggelsee, the biggest lake in Berlin. Transport.

Geographic entities mentioned:
surface_form: Müggelsee
instance_of: Lake
countries: Germany
coordinates: lat: 52.433333333333
lon: 13.65