Sarmila/GeoWiki-Features huggingface dataset:
Her first contact was a sighting of Japanese submarine &quot;I-165&quot;, but she was too far away for an attack. On 11 March 1944 she sank her first victim, a 500-ton coaster, with gunfire. In April she patrolled to the Andaman Islands in the Bay of Bengal south of Rangoon and on 14 April claimed her first sinking by torpedo, a 3,500-ton merchant vessel - although she did not see her sink.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Canaday has set 6 Fastest Known Time running records, including the speed record for the 28-mile Maroon Bells 4 Passes Loop in 2013. In January 2014, Canaday announced a new primary sponsor, Hoka One One, a French running shoe company known for its &quot;maximalist,&quot; highly cushioned shoes.

Geographic entities mentioned:
surface_form: Maroon Bells
instance_of: Mountain
countries: United States
coordinates: lat: 39.0708
lon: -106.989
Buffalo Ridge Wind Farm. Buffalo Ridge Wind Farm is a large wind farm on Buffalo Ridge near Lake Benton, Minnesota, United States. History. In 1994, a Minnesota legislative mandate increased the demand for wind power in Minnesota. Buffalo Ridge's geography is well suited for wind power and it has been heavily developed for this purpose.

Geographic entities mentioned:
surface_form: Buffalo Ridge
instance_of: Landform
countries: United States
coordinates: lat: 43.9802
lon: -96.0106
In 1994, the first wind farm cluster was built on Buffalo Ridge, northwest of the town of Lake Benton. This first cluster was built by the Kenetech Corporation and runs northwest to Lake Shaokatan; it consists of seventy-three wind turbines. The second phase occurred in 1998 when Zond Energy Systems built the next wind farm cluster near Hendricks, Minnesota.

Geographic entities mentioned:
surface_form: Lake Shaokatan
instance_of: Lake
countries: United States
coordinates: lat: 44.40472222
lon: -96.35805556
Gumihorn. The Gumihorn is a mountain of the Bernese Alps, the highest point of the Schynige Platte ridge, located at the western end of the Schwarzhorn group. It forms a limestone tower, overlooking the valley of the Lütschine. At, it is the highest summit lying west of the Loucherhorn. The Gumihorn lies between the municipalities of Gsteigwiler and Gündlischwand, in the canton of Bern.

Geographic entities mentioned:
surface_form: Schynige Platte
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.656111111111
lon: 7.9069444444444
surface_form: schwarzhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.38425
lon: 7.58008333
surface_form: schwarzhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6861
lon: 8.07556
surface_form: schwarzhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.7358
lon: 9.9417
surface_form: schwarzhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.60766667
lon: 9.10652778
surface_form: gumihorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6553
lon: 7.90806
surface_form: schwarzhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6772
lon: 9.0225
surface_form: schwarzhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.21694444
lon: 7.75666667
Gumihorn. The Gumihorn is a mountain of the Bernese Alps, the highest point of the Schynige Platte ridge, located at the western end of the Schwarzhorn group. It forms a limestone tower, overlooking the valley of the Lütschine. At, it is the highest summit lying west of the Loucherhorn. The Gumihorn lies between the municipalities of Gsteigwiler and Gündlischwand, in the canton of Bern.

Geographic entities mentioned:
surface_form: Loucherhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.666444444444
lon: 7.9348888888889
At, it is the highest summit lying west of the Loucherhorn. The Gumihorn lies between the municipalities of Gsteigwiler and Gündlischwand, in the canton of Bern. Although its summit cannot be easily climbed, two other slightly lower summits on both sides of the peak can be easily reached from the Schynige Platte railway station, hence allowing a 360-degree view of the region.

Geographic entities mentioned:
surface_form: schynige platte
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.656111111111
lon: 7.9069444444444
Gumihorn. The Gumihorn is a mountain of the Bernese Alps, the highest point of the Schynige Platte ridge, located at the western end of the Schwarzhorn group. It forms a limestone tower, overlooking the valley of the Lütschine. At, it is the highest summit lying west of the Loucherhorn. The Gumihorn lies between the municipalities of Gsteigwiler and Gündlischwand, in the canton of Bern.

Geographic entities mentioned:
surface_form: gumihorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6553
lon: 7.90806
At, it is the highest summit lying west of the Loucherhorn. The Gumihorn lies between the municipalities of Gsteigwiler and Gündlischwand, in the canton of Bern. Although its summit cannot be easily climbed, two other slightly lower summits on both sides of the peak can be easily reached from the Schynige Platte railway station, hence allowing a 360-degree view of the region.

Geographic entities mentioned:
surface_form: gumihorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6553
lon: 7.90806
Cougar Canyon. Cougar Canyon is a canyon near Kalamalka Lake Provincial Park, in the district municipality of Coldstream, British Columbia. It is a long canyon running along the eastern side of Kalamalka Lake. The Canyon is very popular with the local rock climbing community. The area contains over 200 bolted routes, with plenty of room for more.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: kalamalka lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.173611111111
lon: -119.33
surface_form: cougar canyon
instance_of: Valley
countries: Canada
coordinates: lat: 50.15
lon: -119.317
It is a long canyon running along the eastern side of Kalamalka Lake. The Canyon is very popular with the local rock climbing community. The area contains over 200 bolted routes, with plenty of room for more. Part of Cougar Canyon is an ecological preserve maintained by the British Columbia Ministry of Environment.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: cougar canyon
instance_of: Valley
countries: Canada
coordinates: lat: 50.15
lon: -119.317
Cougar Canyon. Cougar Canyon is a canyon near Kalamalka Lake Provincial Park, in the district municipality of Coldstream, British Columbia. It is a long canyon running along the eastern side of Kalamalka Lake. The Canyon is very popular with the local rock climbing community. The area contains over 200 bolted routes, with plenty of room for more.

Geographic entities mentioned:
surface_form: kalamalka lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.173611111111
lon: -119.33
Cougar Canyon. Cougar Canyon is a canyon near Kalamalka Lake Provincial Park, in the district municipality of Coldstream, British Columbia. It is a long canyon running along the eastern side of Kalamalka Lake. The Canyon is very popular with the local rock climbing community. The area contains over 200 bolted routes, with plenty of room for more.

Geographic entities mentioned:
surface_form: cougar canyon
instance_of: Valley
countries: Canada
coordinates: lat: 50.15
lon: -119.317
Ardennaise. The Ardennaise or is a French and Belgian breed of domestic chicken from the Ardennes plateau, in Belgium and eastern France. Its range extends from the Pays de Herve in Wallonia to the French département of Ardennes, and includes the Fagnes, the Famenne, and the valleys of the Amblève, the Ourthe and the Semois. History. The Ardennaise is a traditional breed of the Ardennes region.

Geographic entities mentioned:
surface_form: Pays de Herve
instance_of: Plateau
countries: Belgium
coordinates: lat: 50.65
lon: 5.83
surface_form: Fagnes
instance_of: Plateau
countries: Belgium
Germany
coordinates: lat: 50.521389
lon: 6.102778
Battle of Dürenstein. The Battle of Dürenstein (; also known as Dürrenstein, Dürnstein and Diernstein) or the Battle of Krems (), on 11 November 1805, was an engagement in the Napoleonic Wars during the War of the Third Coalition. Dürenstein (modern Dürnstein), Austria, is located in the Wachau valley, on the river Danube, upstream from Vienna, Austria.

Geographic entities mentioned:
surface_form: Wachau
instance_of: Valley
countries: Austria
coordinates: lat: 48.36444
lon: 15.43417
Kred, Kobarid. Kred () is a village in the Municipality of Kobarid in the Littoral region of Slovenia. It is located in the Breginj Combe. The parish church in the centre of the village is dedicated to Saint Nicholas.

Geographic entities mentioned:
surface_form: Breginj Combe
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.26583333333333
lon: 13.417777777777777
Ithaca Falls. Ithaca Falls is a waterfall located within the city of Ithaca, New York. It is the last of a series of waterfalls along the hanging valley formed where Fall Creek intersects the glacial trough of Cayuga Lake. The falls are in an amphitheater formed by freezing and thawing of the weak shale which makes up most of the gorge walls.

Geographic entities mentioned:
surface_form: Cayuga Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.68805555555556
lon: -76.70222222222222
He was a Fellow of the Royal Society of Edinburgh, a Fellow of the Royal Scottish Society of Arts and Vice-President of the Edinburgh Philosophical Institution. He employed William Peck to run a private observatory at Murrayfield and later donated his telescopes to the City Observatory on Calton Hill. In 1899, Cox was elected a Fellow of the Society of Antiquaries of Scotland.

Geographic entities mentioned:
surface_form: Calton Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.955278
lon: -3.182222
Tope de Coroa. Tope de Coroa is a mountain on the island of Santo Antão's, Cape Verde, Africa. At 1,979 m elevation, it is the highest point of the island. It is in the western part of the island, 25 km west of the island capital Porto Novo. The mountain is entirely of volcanic origin. The area is the source of several streams including Ribeira de Monte Trigo which flows westward to Monte Trigo.

Geographic entities mentioned:
surface_form: tope de coroa
instance_of: Mountain
countries: Cape Verde
coordinates: lat: 17.033333333333
lon: -25.295833333333
Geography. It is bounded on the north and east by Mucklagh townland, on the south by Doon (Tomregan) and Derryginny townlands and on the west by Snugborough townland. Its chief geographical features are some mountain streams, a pond on its border with Snugborough and Slieve Rushen mountain, on whose southern slope it lies, reaching an altitude of 900 feet above sea-level.

Geographic entities mentioned:
surface_form: Slieve Rushen
instance_of: Mountain
countries: United Kingdom
Ireland
coordinates: lat: 54.151925
lon: -7.6426416666667
It has also been found in the States of Sinaloa and Jalisco to the south. It is also present in the Sierra de la Laguna of Baja California Sur. This plant is a perennial herb with stems 25 to 35 centimeters long growing from a tuber-like rootstock. The leaves are divided deeply into 5 to 7 lobes, the blades dark green in color and 3 to 6 centimeters wide.

Geographic entities mentioned:
surface_form: Sierra de la Laguna
instance_of: Mountain
countries: Mexico
coordinates: lat: 23.566666666667
lon: -110
After six decades of waiting by the people, Palaniswami laid the foundation stone for the ₹1,652-crore &quot;Athikadavu–Avinashi Groundwater Recharge and Drinking Water Supply Scheme&quot; on 28 February 2019, and the project work commenced on 25 December that year. In February 2020, the Government of Tamil Nadu declared the Kaveri delta region as a protected special agriculture zone.

Geographic entities mentioned:
surface_form: Kaveri delta
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
It is said that Palden Lhamo, the female guardian spirit of the sacred lake, Lhamo La-tso, promised the First Dalai Lama in one of his visions &quot;that she would protect the reincarnation lineage of the Dalai Lamas.&quot; Since the time of Gendun Gyatso, who formalised the system, monks have gone to the lake to seek guidance on choosing the next reincarnation through visions while meditating there.

Geographic entities mentioned:
surface_form: Lhamo La-tso
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 29.516666666667
lon: 92.733333333333
The birds also have a soft, croaking call and a whistling call. The tail is often flicked up and down. Distribution. It breeds in the mountains of Central Asia and southern Siberia from the Tien Shan range to the Tarbagatay and Altay Mountains and near Lake Baikal. Some birds move downhill for the winter while others, especially in the north-east of the range, migrate longer distances.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Hannikel and his gang were then confined in Vaduz, where Schäffer collected them in September and brought them to Sulz. Hannikel and three of his gang were sentenced to death and hanged on July 17, 1787, in Sulz. The others were sentenced to life imprisonment at Hohenasperg and the Hohentwiel fortress.

Geographic entities mentioned:
surface_form: Hohentwiel
instance_of: Mountain
countries: Germany
coordinates: lat: 47.764722222222
lon: 8.8188888888889
Merritt became the head of its Raw Materials Section, a position he held until the Manhattan Project wound up at the end of 1946. Over the next five years, he traveled widely, usually in civilian clothes, to sites like the Eldorado Mine on the shore of Great Bear Lake in Canada, the Shinkolobwe mine in the Belgian Congo, and the vanadium mines of the Colorado Plateau.

Geographic entities mentioned:
surface_form: Great Bear Lake
instance_of: Lake
countries: Canada
coordinates: lat: 66
lon: -121
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
The city borders Changhua County, Nantou County, Hualien County, Yilan County, Hsinchu County and Miaoli County. The Central Mountain Range lies just east of the city. Rolling hills run to the north leading to Miaoli County, while flat coastal plains dominate the landscape to the south leading to Changhua County and the Taiwan Strait to the west. The Dadu Plateau lies to the northwest. Climate.

Geographic entities mentioned:
surface_form: Dadu Plateau
instance_of: Mountain
countries: Taiwan
coordinates: lat: 24.14583333
lon: 120.57888889
Neither the city nor the fort has survived. Many reasons have been offered for such a situation. One of these is exemplified by the idiosyncratic rule of Mohammed bin Tughlaq, who inexplicably decreed the capital to be moved to Daulatabad in the Deccan, only to return to Delhi soon after.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Cerros de Quimán. Cerros de Quimán is a forest-covered mountain group between Riñihue Lake and Ranco Lake in Chile. The mountain group runs east–west from Cordillera Negra and Mocho-Choshuenco Volcano in the east and forms part of the border between Futrono and Los Lagos municipalities of Los Ríos Region.

Geographic entities mentioned:
surface_form: Mocho-Choshuenco Volcano
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
Cerros de Quimán. Cerros de Quimán is a forest-covered mountain group between Riñihue Lake and Ranco Lake in Chile. The mountain group runs east–west from Cordillera Negra and Mocho-Choshuenco Volcano in the east and forms part of the border between Futrono and Los Lagos municipalities of Los Ríos Region.

Geographic entities mentioned:
surface_form: cerros de quimán
instance_of: Mountain
countries: Chile
coordinates: lat: -40.020277777778
lon: -72.276111111111
Below this point the canyon widens and the creek becomes a wide gravelly wash. It reaches the Santa Clara River Valley at the town of Piru, and crosses under State Route 126 to join the Santa Clara River. History. Thousands of years ago, Native Americans of the Chumash group lived in the area, but by 500 CE, their former territory along Piru Creek had been occupied by the Tataviam.

Geographic entities mentioned:
surface_form: Santa Clara River Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.3667
lon: -118.983
However, the mines closed soon afterward and the town went into decline, though it was not abandoned completely until 1942. The Russell Borate Mining Company also acquired land in the Piru Creek area in 1907. By 1912, the Russell mine was the only one left in operation. Ultimately, all the mines were abandoned because of competitions from borax operations in Death Valley. Recreation.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
It is very visible and recognizable from the road surrounding the summit area of Praděd mountain (visible to the right of the peak). Another notable viewpoint is from the road around the Dlouhé stráně peak, from where it is also very visible and recognizable, located to the right of the Vozka peak.

Geographic entities mentioned:
surface_form: Dlouhé stráně
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.07125
lon: 17.15675
Another notable viewpoint is from the road around the Dlouhé stráně peak, from where it is also very visible and recognizable, located to the right of the Vozka peak. Keprník is the fifth-highest peak in the Hrubý Jeseník range (following the peaks: Praděd, Vysoká hole, Vysoká hole–JZ, and Petrovy kameny). Slopes.

Geographic entities mentioned:
surface_form: Vysoká hole
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.06263888888889
lon: 17.235611111111112
surface_form: praděd
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.083194444444445
lon: 17.23086111111111
surface_form: keprník
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.17086111111111
lon: 17.116444444444443
surface_form: vysoká
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 49.4039
lon: 18.3611
surface_form: vysoká
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 49.4039
lon: 18.3611
surface_form: vysoká hole
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.06263888888889
lon: 17.235611111111112
It appears to be the highest peak in this part of the Hrubý Jeseník range at first glance and is the main central peak of the Keprník Massif. It is very visible and recognizable from the road surrounding the summit area of Praděd mountain (visible to the right of the peak).

Geographic entities mentioned:
surface_form: praděd
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.083194444444445
lon: 17.23086111111111
No nature monuments have been established on the slopes. Along the red tourist trail, an educational path named &quot;With Koprníček on an excursion to the Keprník Mountains&quot; () has been created, with 13 observation points, running from Červenohorské sedlo to. Šerák-Keprník National Nature Reserve.

Geographic entities mentioned:
surface_form: keprník
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.17086111111111
lon: 17.116444444444443
surface_form: keprník
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.17086111111111
lon: 17.116444444444443
Červenohorské sedlo – Červená hora – spring – Sedlo pod Vřesovkou pass – Keprník-JV – &quot;Trojmezí&quot; – Keprník summit – Sedlo pod Keprníkem pass – Šerák mountain – – Černava mountain – Ramzová
Branná – Tři kameny – mountain – Volská louka pass – mountain – &quot;Trojmezí&quot;
Branná – Pekelec mountain – Pekelec-SV summit – Alojzovské louky pass – Troják-JZ mountain – Hučava stream valley – Troják mountain – Vozka summit – Sedlo pod Vřesovkou pass
Lipová-lázně – Sněhulák mountain – Strmý mountain – – Šerák Mountain – Sedlo pod Keprníkem pass – mountain – mountain – Filipovice
Cycling and skiing trails.

Geographic entities mentioned:
surface_form: šerák
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.18658333333333
lon: 17.106666666666666
surface_form: šerák
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.18658333333333
lon: 17.106666666666666
surface_form: keprník
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.17086111111111
lon: 17.116444444444443
surface_form: keprník
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.17086111111111
lon: 17.116444444444443
surface_form: černava
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.17938888888889
lon: 17.078805555555554
&quot;Spojená cesta&quot; – mountain – mountain – Šumná-JV – Šumná mountain – Nad Borovým mountain – Borový potok valley – Bělá pod Pradědem – mountain – Šumný mountain – Sedlo pod Keprníkem pass – Šerák mountain – Mračná hora – Černava mountain – Ostružná – Petříkov
During snowy periods, cross-country ski trails are marked along the hiking and cycling trails (except the green tourist trail), including a trail named &quot;Jesenická magistrála&quot;.

Geographic entities mentioned:
surface_form: šerák
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.18658333333333
lon: 17.106666666666666
surface_form: černava
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.17938888888889
lon: 17.078805555555554
Keprník. Keprník is a mountain in the Hrubý Jeseník mountain range in the Czech Republic. It has an elevation of above sea level. It is located in the municipality of Ostružná, on the historical border between Silesia and Moravia. Location.

Geographic entities mentioned:
surface_form: keprník
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.17086111111111
lon: 17.116444444444443
It has an elevation of above sea level. It is located in the municipality of Ostružná, on the historical border between Silesia and Moravia. Location. Keprník is located in the northwestern region of the entire Hrubý Jeseník range, lying almost centrally in the Hrubý Jeseník area, in a sub-region called the (). It sits on the main ridge that runs from pass to pass.

Geographic entities mentioned:
surface_form: keprník
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.17086111111111
lon: 17.116444444444443
It sits on the main ridge that runs from pass to pass. The peak is easily recognizable due to its characteristic summit rock formation, situated on a deforested summit area among high-altitude vegetation. It appears to be the highest peak in this part of the Hrubý Jeseník range at first glance and is the main central peak of the Keprník Massif.

Geographic entities mentioned:
surface_form: keprník
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.17086111111111
lon: 17.116444444444443
Main summit. There are no marked tourist trails leading directly to the main summit. The main ridge path crosses the summit area, along with a red tourist trail and a green educational path, which leads to the secondary peak Keprník–JV. Near this path is a tourist intersection named &quot;Keprník (vrchol)&quot; with an informational sign indicating an elevation of 1,423 m.

Geographic entities mentioned:
surface_form: keprník
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.17086111111111
lon: 17.116444444444443
The main ridge path crosses the summit area, along with a red tourist trail and a green educational path, which leads to the secondary peak Keprník–JV. Near this path is a tourist intersection named &quot;Keprník (vrchol)&quot; with an informational sign indicating an elevation of 1,423 m. On top of this monument, lines with the names of visible peaks are marked.

Geographic entities mentioned:
surface_form: keprník
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.17086111111111
lon: 17.116444444444443
The State Geodetic and Cadastral Office lists the highest point of the mountain – the summit – at an elevation of 1,423.3 m above sea level and geographical coordinates. Access to the summit is via the main path and the &quot;Keprník (vrchol)&quot; tourist intersection, from which a path about 30 m long with wooden railings on either side leads to the summit. Secondary summits.

Geographic entities mentioned:
surface_form: keprník
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.17086111111111
lon: 17.116444444444443
surface_form: keprník
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.17086111111111
lon: 17.116444444444443
Geology. Geologically, the Keprník massif belongs to the unit known as the Keprník Dome and is composed of metamorphic rocks, mainly gneisses (biotite), orthogneisses, mylonites, blasto-mylonites, migmatites, schists, and igneous rocks, primarily meta-granites. The geological structure also contains admixtures of gemstones such as staurolite, andalusite, garnet, and sillimanite.

Geographic entities mentioned:
surface_form: keprník
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.17086111111111
lon: 17.116444444444443
Hoggs Hollow is named after the Hogg family. James Hogg (1797–1839), a Scotsman, settled in the area in 1824. He operated a whisky distillery and a grist mill, and he was viewed as the most successful of all the millers in the valley. The name of the neighbourhood is usually written without an apostrophe as Hoggs Hollow, but it sometimes appears with an apostrophe as Hogg's Hollow. History.

Geographic entities mentioned:
surface_form: hogg's hollow
instance_of: Valley
countries: Canada
coordinates: lat: 43.739
lon: -79.4
surface_form: hoggs hollow
instance_of: Valley
countries: Canada
coordinates: lat: 43.739
lon: -79.4
Hoggs Hollow. Hoggs Hollow is a residential neighbourhood in Toronto, Ontario, Canada. It is located to the south of York Mills Road, east of Yonge Street, and the western branch of the upper Don River flows through it. Hoggs Hollow is named after the Hogg family. James Hogg (1797–1839), a Scotsman, settled in the area in 1824.

Geographic entities mentioned:
surface_form: hoggs hollow
instance_of: Valley
countries: Canada
coordinates: lat: 43.739
lon: -79.4
The name of the neighbourhood is usually written without an apostrophe as Hoggs Hollow, but it sometimes appears with an apostrophe as Hogg's Hollow. History. In 1856, John and William Hogg, sons of James Hogg, subdivided their father's estate under the name &quot;Hoggs Hollow&quot;. The subdivision included one hundred and forty-one lots.

Geographic entities mentioned:
surface_form: hoggs hollow
instance_of: Valley
countries: Canada
coordinates: lat: 43.739
lon: -79.4
The subdivision included one hundred and forty-one lots. With the area full of quick sand, swamps and bogs, only a few houses were actually built at this time, however Sebastian and Carson were among the first settlers to arrive in Hoggs Hollow with the Hogg family. The subdivision stood in close proximity to the historic village of York Mills.

Geographic entities mentioned:
surface_form: hoggs hollow
instance_of: Valley
countries: Canada
coordinates: lat: 43.739
lon: -79.4
John's Anglican Church, where a large family monument is situated. The family went on to operate a grist mill and distillery. Development of the present-day Hoggs Hollow neighbourhood began during the 1920s with the creation of lots, layout of roads, and design of homes reflecting the aesthetic of the English countryside.

Geographic entities mentioned:
surface_form: hoggs hollow
instance_of: Valley
countries: Canada
coordinates: lat: 43.739
lon: -79.4
The school was demolished in 2004, and bricks from it were used to create a memorial. The Miller Tavern (formerly the Jolly Miller Tavern), c. 1857, located at the bottom of Hoggs Hollow Hill, 3885 Yonge Street, was closed for many years, but re-opened in 2004 after many battles between developers, the city and groups that wanted to preserve the historical landmark. The George S. Pratt House, c.

Geographic entities mentioned:
surface_form: hoggs hollow
instance_of: Valley
countries: Canada
coordinates: lat: 43.739
lon: -79.4
The George S. Pratt House, c. 1886, located at 17 Mill Street, is another historic landmark in Hoggs Hollow. In need of funds, The York Mills Public School building was sold by the school board and demolished. Many of the original estate homes and modern movement residences of the early to mid-20th century are being demolished in favour of large new homes.

Geographic entities mentioned:
surface_form: hoggs hollow
instance_of: Valley
countries: Canada
coordinates: lat: 43.739
lon: -79.4
Public transportation. In 1892, the Metropolitan Street Railway extended streetcar service along Yonge Street from Toronto (Summerhill) to the southern rim of Hoggs Hollow near today's Glen Echo Road, and then through the valley to Richmond Hill in 1897. This radial railway service through the valley ended in 1948.

Geographic entities mentioned:
surface_form: hoggs hollow
instance_of: Valley
countries: Canada
coordinates: lat: 43.739
lon: -79.4
This radial railway service through the valley ended in 1948. However, the Yonge streetcar line continued to operate service from Glen Echo Road to downtown Toronto until 1954. Since 1973, Hoggs Hollow has been served by York Mills subway station. Disasters.

Geographic entities mentioned:
surface_form: hoggs hollow
instance_of: Valley
countries: Canada
coordinates: lat: 43.739
lon: -79.4
A steel truss bridge carrying Yonge Street across the river was damaged and temporarily replaced by a Bailey bridge until a new bridge was built. On March 17, 1960, the incident popularly known as the &quot;Hoggs Hollow Disaster&quot; occurred. Five young Italian immigrant workers were killed while constructing a tunnel for a water main at Hoggs Hollow.

Geographic entities mentioned:
surface_form: hoggs hollow
instance_of: Valley
countries: Canada
coordinates: lat: 43.739
lon: -79.4
On March 17, 1960, the incident popularly known as the &quot;Hoggs Hollow Disaster&quot; occurred. Five young Italian immigrant workers were killed while constructing a tunnel for a water main at Hoggs Hollow. The details of the accident, where they were trapped 35 feet underground in a cramped, dimly lit tunnel, sparked a public outcry over the lack of safety standards in construction.

Geographic entities mentioned:
surface_form: hoggs hollow
instance_of: Valley
countries: Canada
coordinates: lat: 43.739
lon: -79.4
Vang, Innlandet. Vang is a municipality in Innlandet county, Norway. It is located in the traditional district of Valdres. The administrative centre of the municipality is the village of Vang i Valdres. Other villages in Vang include Hænsgardane, Nystuen, Øye, Ryfoss, and Tyinkrysset. The municipality is the 55th largest by area out of the 356 municipalities in Norway.

Geographic entities mentioned:
surface_form: Valdres
instance_of: Valley
countries: Norway
coordinates: lat: 60.916666666667
lon: 9.1666666666667
He was named as one of the members of the delegation that followed King Håkon V Magnusson to Copenhagen in 1309. Later, he became the local governor of Valdres and Hallingdal (Vang is part of the Valdres region). He played a major role in the development of the region and the arms can be seen on different places, including in the local Vang Church. The arms were designed by Stein Davidsen.

Geographic entities mentioned:
surface_form: Valdres
instance_of: Valley
countries: Norway
coordinates: lat: 60.916666666667
lon: 9.1666666666667
surface_form: Hallingdal
instance_of: Valley
countries: Norway
coordinates: lat: 60.633333333333
lon: 9.05
It is part of the Valdres prosti (deanery) in the Diocese of Hamar. History. Vang, like the rest of Valdres, was originally populated by migrants from Vestlandet. In 1153, recognizing this, Cardinal Breakspear included these valleys in the Diocese of Stavanger. The ancient Vang Church was the site of a legal court &quot;(thing)&quot; held by King Haakon VI in 1368.

Geographic entities mentioned:
surface_form: Valdres
instance_of: Valley
countries: Norway
coordinates: lat: 60.916666666667
lon: 9.1666666666667
Geography. Vang is bordered to the north by the municipalities of Lom and Vågå, to the east by Øystre Slidre, to the southeast by Vestre Slidre, to the south by Hemsedal (in Buskerud county), and to the west by Lærdal and Årdal (in Vestland county). Vang is part of the Valdres region in central, southern Norway. This region is situated between the Gudbrandsdal and Hallingdal valleys.

Geographic entities mentioned:
surface_form: Valdres
instance_of: Valley
countries: Norway
coordinates: lat: 60.916666666667
lon: 9.1666666666667
Vang is part of the Valdres region in central, southern Norway. This region is situated between the Gudbrandsdal and Hallingdal valleys. Vang municipality is on a north–south axis and on an east–west axis. The highest point is Kalvehøgde with a height of above sea level. Three-quarters of the region is above.

Geographic entities mentioned:
surface_form: Hallingdal
instance_of: Valley
countries: Norway
coordinates: lat: 60.633333333333
lon: 9.05
This region is situated between the Gudbrandsdal and Hallingdal valleys. Vang municipality is on a north–south axis and on an east–west axis. The highest point is Kalvehøgde with a height of above sea level. Three-quarters of the region is above. About 13 percent of the municipality is covered by water, including Lakes Fleinsendin, Slettningen and Vangsmjøsa. The lowest point is above sea level.

Geographic entities mentioned:
surface_form: Kalvehøgde
instance_of: Mountain
countries: Norway
coordinates: lat: 61.393055555556
lon: 8.6194444444444
Vang municipality is on a north–south axis and on an east–west axis. The highest point is Kalvehøgde with a height of above sea level. Three-quarters of the region is above. About 13 percent of the municipality is covered by water, including Lakes Fleinsendin, Slettningen and Vangsmjøsa. The lowest point is above sea level. The river Begna has its headwaters in the Filefjell area of Vang. Trivia.

Geographic entities mentioned:
surface_form: Fleinsendin
instance_of: Lake
countries: Norway
coordinates: lat: 61.267777777778
lon: 8.7194444444444
surface_form: Slettningen
instance_of: Lake
countries: Norway
coordinates: lat: 61.206666666667
lon: 8.1147222222222
From there, the road makes a slight curve to the right to cross over the railroad line. Both the tracks and the road run along the east coast of Lochloosa Lake in Lochloosa. The interchange with SR 20 in Hawthorne, also includes the side road Southeast 221st Street / Johnson Street, as well as the previously mentioned railroad line in between that side road and US 301.

Geographic entities mentioned:
surface_form: Lochloosa Lake
instance_of: Lake
countries: United States
coordinates: lat: 29.5167
lon: -82.1206
Business career. Chandy had interests in the fields of education and hospitality among others. He was the Chairman of the United Indian School, an Indian public school, and Indian Central School in Kuwait. He also ran Al-Alia International Indian School in Riyadh, Saudi Arabia. Chandy also owned a controlling interest in the Lake Palace Resort, located on the Punamada Lake in Kerala. Allegations.

Geographic entities mentioned:
surface_form: Punamada Lake
instance_of: Lake
countries: India
coordinates: lat: 9.85
lon: 76.35
Meteorological history. A low-pressure area formed over west central & adjoining north Bay of Bengal off north Andhra Pradesh south Odisha coast in the morning of June 10. It concentrated into a well marked low-pressure area over northern parts of central Bay of Bengal & adjoining north Bay of Bay on 11th morning and into a depression over north Bay of Bengal in the evening of 11th.).

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Cause. The landslide was caused by an incessant downpour that began early morning of 12 June, dropping of rain in 24 hours. The monsoon and depression over Bay of Bengal towards Bangladesh resulted in heavy rain over different parts, including Dhaka and Chittagong.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Alpine skiing at the 2012 Winter Youth Olympics. Alpine Skiing at the 2012 Winter Youth Olympics was held at the Olympia Run Patscherkofel in Igls, Innsbruck, Austria from 14 to 22 January. The difference in the Youth Olympic program for alpine skiing compared to the Winter Olympics was that there were no downhill for both genders, and an inclusion of a team event. Multi-medalists.

Geographic entities mentioned:
surface_form: Olympia Run Patscherkofel
instance_of: Mountain
countries: Austria
coordinates: lat: 47.208611
lon: 11.460556
Limmattal light rail line. The Limmattal light rail line () is a metre gauge tram line in the Limmat Valley between Zürich Altstetten and Killwangen which started service in 2022. The line is 13.4 kilometres (8.3 mi) long and serves 27 stops. It is served by the lines 20 and 2 of the Zürich tram network. History.

Geographic entities mentioned:
surface_form: Limmat Valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 47.5
lon: 8.25
Construction commenced in August 2017, and phase 1 between Farbhof and Schlieren opened in September 2019, operated by Verkehrsbetriebe Zürich and served by an extension of the existing tram line 2 from Zürich Tiefenbrunnen railway station at the shore of Lake Zurich.

Geographic entities mentioned:
surface_form: Lake Zurich
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2475
lon: 8.6775
Preuschoff Range. Preuschoff Range () is a mountain range consisting of Mount Hochlin and associated features, lying just west of Kaye Crest in the Mühlig-Hofmann Mountains of Queen Maud Land. The name was applied in the general area by the Third German Antarctic Expedition (1938–1939), led by Capt.

Geographic entities mentioned:
surface_form: Mount Hochlin
instance_of: Mountain
coordinates: lat: -72.0833
lon: 4.05
Outcast Hill. Outcast Hill is an isolated hill in northern British Columbia, Canada, located southeast of Mess Lake. It lies at the southern end of Mount Edziza Provincial Park. History. Outcast Hill was named on 2 January 1980 by the Geological Survey of Canada after the Wetalth people, a group of people who lived here in times past, outcast or exiled from the Tahltans. Geology.

Geographic entities mentioned:
surface_form: Mess Lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.4667
lon: -130.883
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: outcast hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.39
lon: -130.774
Geology. Outcast Hill is a volcanic feature associated with the Spectrum Range volcanic complex which in turn form part of the Northern Cordilleran Volcanic Province. It is a cinder cone that formed in the Pleistocene period.

Geographic entities mentioned:
surface_form: Northern Cordilleran Volcanic Province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
surface_form: outcast hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.39
lon: -130.774
Outcast Hill. Outcast Hill is an isolated hill in northern British Columbia, Canada, located southeast of Mess Lake. It lies at the southern end of Mount Edziza Provincial Park. History. Outcast Hill was named on 2 January 1980 by the Geological Survey of Canada after the Wetalth people, a group of people who lived here in times past, outcast or exiled from the Tahltans. Geology.

Geographic entities mentioned:
surface_form: outcast hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.39
lon: -130.774
The cornerstone for the university was laid on 24 July 1918. Seven years later, on 1 April 1925, the Hebrew University campus on Mount Scopus was opened at a gala ceremony attended by the leaders of the Jewish world, distinguished scholars and public figures, and British dignitaries, including the Earl of Balfour, Viscount Allenby, Winston Churchill and Sir Herbert Samuel.

Geographic entities mentioned:
surface_form: Mount Scopus
instance_of: Mountain
countries: Israel
coordinates: lat: 31.7925
lon: 35.244166666667
Mount Scopus (Hebrew: Har HaTzofim הר הצופים), in the north-eastern part of Jerusalem, is home to the main campus, which contains the Faculties of Humanities, Social Sciences, Law, Jerusalem School of Business Administration, Seymour Fox School of Education, Baerwald School of Social Work, Harry S.

Geographic entities mentioned:
surface_form: Mount Scopus
instance_of: Mountain
countries: Israel
coordinates: lat: 31.7925
lon: 35.244166666667
Only two buildings of this original scheme were built: the David Wolffsohn University and National Library, and the Mathematics Institute, with the Physics Institute probably being built to the designs of their Jerusalem-based partner, Benjamin Chaikin. Housing for students at Hebrew University who live on Mount Scopus is located at the three dormitories located near the university.

Geographic entities mentioned:
surface_form: Mount Scopus
instance_of: Mountain
countries: Israel
coordinates: lat: 31.7925
lon: 35.244166666667
Lochinvar, New South Wales. Lochinvar is a village in the Hunter Region of New South Wales, Australia, eleven kilometres west of the regional centre of Maitland. Lochinvar is within the boundaries of the City of Maitland local government area and is named after Lochinvar, a loch in southern Scotland.

Geographic entities mentioned:
surface_form: Hunter Region
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Lochinvar, New South Wales. Lochinvar is a village in the Hunter Region of New South Wales, Australia, eleven kilometres west of the regional centre of Maitland. Lochinvar is within the boundaries of the City of Maitland local government area and is named after Lochinvar, a loch in southern Scotland.

Geographic entities mentioned:
surface_form: Lochinvar
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.142777777778
lon: -4.1058333333333
History. The town was very important for the History of agriculture in the area. It is one of the oldest towns in the Hunter Region. The Windermere homestead (built around 1821-1823) by the Winder family (“Tom” i.e. Thomas White Melville Winder). It is the oldest homestead in the Hunter Region and likely built up by convicts and emancipated previously convict workers. See Windermere House, NSW.

Geographic entities mentioned:
surface_form: Hunter Region
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Brigadier General William Hull would attack Amherstburg from Detroit, Major General Van Rensselaer would attack across the Niagara River, another attack would cross Lake Ontario to take Kingston, and Major General Henry Dearborn, the commander-in-chief of the United States Army, would use the Lake Champlain route to capture Montreal.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Pontfadog. Pontfadog is a village in the Ceiriog Valley west of Chirk in Wrexham County Borough, Wales; it is part of the community of Glyntraian. Like the neighbouring village of Glyn Ceiriog, the growth of Pontfadog is connected to the area's former quarrying industry. The village's name translates as &quot;Bridge of Madoc&quot;, taking its name from a bridge over the River Ceiriog.

Geographic entities mentioned:
surface_form: Ceiriog Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 52.915
lon: -3.197
Principal photography began on July 17, 1967 in Philadelphia, where many scenes in the first half of the movie were filmed, including Market Street near 13th Street and City Hall, and a protest scene at the Philadelphia Museum of Art. Other scenes were filmed in the Lehigh Valley at Dorney Park and at St. Mary's Villa, a Catholic home for troubled youths on Bethlehem Pike in Ambler, Pennsylvania.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Iveland. Iveland is a municipality in Agder County, Norway. It is located in the traditional district of Setesdal. The administrative centre of the municipality is the village of Birketveit. Other villages in the municipality include Bakken, Skaiå, and Vatnestrøm. The municipality is the 279th largest by area out of the 356 municipalities in Norway.

Geographic entities mentioned:
surface_form: Setesdal
instance_of: Valley
countries: Norway
coordinates: lat: 58.92025
lon: 7.7206388888889
This resulted in better prices, since it provided competition with the floated timber. Geography. Iveland is the smallest municipality in Setesdal. The Otra river, which flows through Iveland, is the largest river in the Sørlandet district. Towards the east it borders on lake Oggevatn.

Geographic entities mentioned:
surface_form: Setesdal
instance_of: Valley
countries: Norway
coordinates: lat: 58.92025
lon: 7.7206388888889
Geography. Iveland is the smallest municipality in Setesdal. The Otra river, which flows through Iveland, is the largest river in the Sørlandet district. Towards the east it borders on lake Oggevatn. The municipality is bordered in the northwest by Evje og Hornnes, in the northeast and east by Birkenes, and in the south and west by Vennesla.

Geographic entities mentioned:
surface_form: Ogge
instance_of: Lake
countries: Norway
coordinates: lat: 58.39253
lon: 8.09991
The river, joined by Tidbinbilla River and Gibraltar Creek, flows generally north-west and to the west of the Canberra suburbs of Conder and Gordon, before reaching its confluence with Cotter River, near Mount Stromlo. The river descends over its course.

Geographic entities mentioned:
surface_form: Mount Stromlo
instance_of: Mountain
countries: Australia
coordinates: lat: -35.316666666667
lon: 149.01666666667
It is situated at a height of about, about 1.87 km long and 0.55 km at its widest point. Querquecocha lies south-east of Velille and north of the lake Orccococha.

Geographic entities mentioned:
surface_form: orccococha
instance_of: Lake
countries: Peru
coordinates: lat: -13.919444444444
lon: -72.725
Querquecocha. Querquecocha (possibly from Quechua &quot;khirki&quot; armadillo / very rough, &quot;qucha&quot; lake, &quot;armadillo lake&quot; or &quot;rough lake&quot;) is a lake in Peru located in the Cusco Region, Chumbivilcas Province, Velille District. It is situated at a height of about, about 1.87 km long and 0.55 km at its widest point.

Geographic entities mentioned:
surface_form: querquecocha
instance_of: Lake
countries: Peru
coordinates: lat: -14.630555555556
lon: -71.836944444444
Glückstadt. Glückstadt (;) is a town in the Steinburg district of Schleswig-Holstein, Germany. It is located on the right bank of the Lower Elbe at the confluence of the small Rhin river, about northwest of Altona. Glückstadt is part of the Hamburg Metropolitan Region (&quot;Metropolregion Hamburg&quot;). History.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Cookie Jar Butte lies between them on the north shore of the bay. At the southern mouth of the bay, north of Dominguez Butte on the south shore is Padres Butte, formerly an island, now with lower water in the lake the tip of Padre Point. Padres Butte marks the location of the Crossing of the Fathers, which is approximately a mile west of the butte.

Geographic entities mentioned:
surface_form: Padres Butte
instance_of: Mountain
countries: United States
coordinates: lat: 37.048611111111
lon: -111.28277777778