Sarmila/GeoWiki-Features huggingface dataset:
Scuol-Tarasp railway station. Scuol-Tarasp railway station is the northern terminus of the Bever–Scuol-Tarasp railway. It is located on the western edge of the village of Scuol at an altitude of 1287 m in the Lower Engadine. The station is named after the neighbouring village of Scuol and the small town of Tarasp. Scuol-Tarasp station was completely rebuilt and renovated in 2009.

Geographic entities mentioned:
surface_form: Lower Engadine
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.75
lon: 10.25
Scuol-Tarasp is the terminus or starting point for the Scuol-Tarasp–Zernez–Samedan–Pontresina regional service and for the Scuol-Tarasp–Landquart RegioExpress service, both running hourly. Regular bus routes to Ftan, Tarasp, Samnaun, Martina, Sent, S-charl and Val Sinestra start at the station. In addition, the local school bus stops at the station.

Geographic entities mentioned:
surface_form: Val Sinestra
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.850724
lon: 10.336659
West Road River. The West Road River or Blackwater River or Tiyakoh is an important tributary of the Fraser River, flowing generally north-eastward from the northern slopes of the Ilgachuz Range and across the Fraser Plateau in the Chilcotin region of central British Columbia, Canada.

Geographic entities mentioned:
surface_form: Fraser Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 52
lon: -123
With only one major tributary, the Nazko River (&quot;river flowing from the south&quot; in the Carrier language), its confluence with the Fraser is approximately 40 km northwest of Quesnel. It forms the division between the Chilcotin Plateau (S) and the Nechako Plateau (N), which are subdivisions of the Fraser Plateau.

Geographic entities mentioned:
surface_form: Chilcotin Plateau
instance_of: Mountain
countries: Canada
coordinates: lat: 52.166666666666664
lon: -123.41666666666667
surface_form: Nechako Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 54.49979
lon: -126.00334
He graduated from the University of Rochester in 1855, at age 20. He joined the Boston &quot;Journal&quot; and also became editor of the &quot;Traveller.&quot; He moved to New York City in 1858 and joined the &quot;New York Evening Post.&quot; In 1859, he went to the Red River Valley in the Midwest as &quot;The Evening Posts correspondent.

Geographic entities mentioned:
surface_form: Red River Valley
instance_of: Valley
countries: Canada
United States
coordinates: lat: 49
lon: -97.5
This is based on similarities with regard to their decorative programs. Tomb QV52. Tyti's tomb is designated QV52 in the Valley of the Queens and her titles were: &quot;King's Daughter; King's Sister; King's Wife; King's Mother; God's Wife,&quot; &quot;Lady of the Two Lands.&quot; The tomb had been described by Champollion (tomb 3), Lepsius (number 9), Wilkinson (number 12) and Hay (number 2).

Geographic entities mentioned:
surface_form: Valley of the Queens
instance_of: Valley
countries: Egypt
coordinates: lat: 25.7275
lon: 32.593055555556
Most of the inhabitants of Eastern Equatoria live by subsistence farming, and also raise cattle, sheep and goats. Some of the crops are sold, while most are consumed locally. The Didinga Hills in Budi county have rich and fertile soil that is used for cultivation of tobacco, potatoes, maize, and Dura. Government. The executive head of the State was the Governor, who was elected.

Geographic entities mentioned:
surface_form: Didinga Hills
instance_of: Mountain
countries: South Sudan
coordinates: lat: 4.33333
lon: 33.5833
Lake Virelles. Lake Virelles is an artificial lake in Wallonia near the city of Chimay in Belgium. The lake is an important nature reserve with a great number of birds. The lake covers 1,25 km².

Geographic entities mentioned:
surface_form: lake virelles
instance_of: Lake
countries: Belgium
coordinates: lat: 50.072222222222
lon: 4.3430555555556
Mount Cambria. Mount Cambria (also Sheep Hill or Taka-a-raro / Takararo) is one of the volcanoes in the Auckland volcanic field. Located in the suburb of Devonport north-east of Mt Victoria, its 30-metre scoria cone was quarried away. The site is now Cambria Reserve. History.

Geographic entities mentioned:
surface_form: mount cambria
instance_of: Mountain
countries: New Zealand
coordinates: lat: -36.824444
lon: 174.801933
Mount Cambria. Mount Cambria (also Sheep Hill or Taka-a-raro / Takararo) is one of the volcanoes in the Auckland volcanic field. Located in the suburb of Devonport north-east of Mt Victoria, its 30-metre scoria cone was quarried away. The site is now Cambria Reserve. History.

Geographic entities mentioned:
surface_form: mount cambria
instance_of: Mountain
countries: New Zealand
coordinates: lat: -36.824444
lon: 174.801933
surface_form: sheep hill
instance_of: Mountain
countries: New Zealand
coordinates: lat: -36.824444
lon: 174.801933
surface_form: taka-a-raro
instance_of: Mountain
countries: New Zealand
coordinates: lat: -36.824444
lon: 174.801933
surface_form: takararo
instance_of: Mountain
countries: New Zealand
coordinates: lat: -36.824444
lon: 174.801933
The site is now Cambria Reserve. History. The hill was traditionally known as Takararo (&quot;The Hill Standing Below&quot;), contrasting with the larger Mount Victoria (&quot;The Hill Standing Above&quot;). It was named Heaphy Hill after Charles Heaphy by Ferdinand von Hochstetter in 1859, but this name is not used. Cambria is the ancient name for Wales.

Geographic entities mentioned:
surface_form: takararo
instance_of: Mountain
countries: New Zealand
coordinates: lat: -36.824444
lon: 174.801933
Shaw Nunatak. Shaw Nunatak () is a nunatak rising to 500 m in Nichols Snowfield, northern Alexander Island, Antarctica. It is situated 5.3 km north-northeast of Rachenitsa Nunatak, 4.23 km east-southeast of Tipits Knoll and 7 km southeast of Mount Kliment Ohridski in Sofia University Mountains, 7.5 km southwest of Lizard Nunatak and 8.1 km northwest of Tegra Nunatak.

Geographic entities mentioned:
surface_form: Mount Kliment Ohridski
instance_of: Mountain
coordinates: lat: -69.517777777778
lon: -71.391666666667
surface_form: Lizard Nunatak
instance_of: Mountain
coordinates: lat: -69.5
lon: -71.05
Shaw Nunatak. Shaw Nunatak () is a nunatak rising to 500 m in Nichols Snowfield, northern Alexander Island, Antarctica. It is situated 5.3 km north-northeast of Rachenitsa Nunatak, 4.23 km east-southeast of Tipits Knoll and 7 km southeast of Mount Kliment Ohridski in Sofia University Mountains, 7.5 km southwest of Lizard Nunatak and 8.1 km northwest of Tegra Nunatak.

Geographic entities mentioned:
surface_form: shaw nunatak
instance_of: Mountain
coordinates: lat: -69.55
lon: -71.2
Shaw Nunatak. Shaw Nunatak () is a nunatak rising to 500 m in Nichols Snowfield, northern Alexander Island, Antarctica. It is situated 5.3 km north-northeast of Rachenitsa Nunatak, 4.23 km east-southeast of Tipits Knoll and 7 km southeast of Mount Kliment Ohridski in Sofia University Mountains, 7.5 km southwest of Lizard Nunatak and 8.1 km northwest of Tegra Nunatak.

Geographic entities mentioned:
surface_form: shaw nunatak
instance_of: Mountain
coordinates: lat: -69.55
lon: -71.2
surface_form: alexander
instance_of: Mountain
coordinates: lat: -63.3039
lon: -55.80564
It is situated 5.3 km north-northeast of Rachenitsa Nunatak, 4.23 km east-southeast of Tipits Knoll and 7 km southeast of Mount Kliment Ohridski in Sofia University Mountains, 7.5 km southwest of Lizard Nunatak and 8.1 km northwest of Tegra Nunatak. The feature was photographed from the air by Ronne Antarctic Research Expedition in 1947–48, and mapped from these photographs by D.

Geographic entities mentioned:
surface_form: searle
instance_of: Mountain
coordinates: lat: -67.81666667
lon: -67.25
The feature was photographed from the air by Ronne Antarctic Research Expedition in 1947–48, and mapped from these photographs by D. Searle of Falkland Islands Dependencies Survey, 1960. The nunatak was named by United Kingdom Antarctic Place-Names Committee in 1977 after Colin Shaw (1944–78), British Antarctic Survey surveyor who worked in Alexander Island, from 1975 to 1976.

Geographic entities mentioned:
surface_form: alexander
instance_of: Mountain
coordinates: lat: -63.3039
lon: -55.80564
Gugler. The Guglers (also Güglers) were a body of mostly English and French knights who as mercenaries invaded Alsace and the Swiss plateau under the leadership of Enguerrand VII de Coucy during the Gugler War of 1375. Origin of the term.

Geographic entities mentioned:
surface_form: Swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
April 15–16. A two-day tornado outbreak affected portions of the Midwestern United States, Mississippi and Tennessee Valleys on April 15–16, with the worst of the outbreak taking place on the second day. On that day, at least 10 tornadoes swept through Middle Tennessee—three of them touching down in Nashville, causing significant damage to the downtown and East Nashville areas.

Geographic entities mentioned:
surface_form: Tennessee Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.959166666667
lon: -83.850277777778
A Good Season. &quot;A Good Season&quot; () is a 2014 Italian family drama television miniseries. It aired on Rai 1 from 1 April to 6 May 2014. Plot. The series follows the Masci-Santangelo family, a family of esteemed winemakers from Trentino-Alto Adige. Production. The series was filmed in several parts of Trentino-Alto Adige, including Mezzocorona, the Lago di Toblino, and Madonna di Campiglio.

Geographic entities mentioned:
surface_form: Lago di Toblino
instance_of: Lake
countries: Italy
coordinates: lat: 46.05336111111111
lon: 10.965805555555555
Development. In its first year, the club had fourteen members. Its equipment included alpine rope which had been fixed to the Cobbler and the Salisbury Crags in Edinburgh where the members trained. To qualify, members had to ascend four peaks of at least 3,000 feet with two snow climbs and two rock climbs.

Geographic entities mentioned:
surface_form: the Cobbler
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.211944444444
lon: -4.8108333333333
To qualify, members had to ascend four peaks of at least 3,000 feet with two snow climbs and two rock climbs. They then went on bold climbs of mountains such as the Beuckle (&quot;Buachaille Etive Mòr&quot;) and Suilven. To be decent, they would start their climbs in long skirts but, when no men were around, would often discard these to climb in knickerbockers.

Geographic entities mentioned:
surface_form: Beuckle
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.647302777778
lon: -4.8977972222222
surface_form: Suilven
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.115
lon: -5.1370694444444
Nordrepollen. Nordrepollen is a village in the Mauranger area of Kvinnherad municipality in Vestland county, Norway. The village is located at the northern end of the Maurangsfjorden, about half-way between the villages of Gjetingsdalen and Austrepollen. The southeastern entrance to the Jondal Tunnel is located in Nordrepollen.

Geographic entities mentioned:
surface_form: Gjetingsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 60.134722222222
lon: 6.2319444444444
The village is located at the northern end of the Maurangsfjorden, about half-way between the villages of Gjetingsdalen and Austrepollen. The southeastern entrance to the Jondal Tunnel is located in Nordrepollen. The lake Juklavatnet lies high up in the mountains to the north of Nordrepollen. That lake has a dam at the end, and its water is used to hydroelectric power generation.

Geographic entities mentioned:
surface_form: Juklavatnet
instance_of: Lake
countries: Norway
coordinates: lat: 60.2125
lon: 6.3797222222222
Svartfjellet, Loppa. or is a mountain in Loppa Municipality in Finnmark county, Norway. It lies alongside the small glacier Svartfjelljøkelen, a few kilometers north of the larger glacier Øksfjordjøkelen. The village of Bergsfjord lies about straight west of the mountain. For many years, Svartfjellet was regarded as the highest mountain in Finnmark, but this was due to a measurement error.

Geographic entities mentioned:
surface_form: svartfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 70.232777777778
lon: 21.998611111111
surface_form: svartfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 70.584166666667
lon: 23.859166666667
The village of Bergsfjord lies about straight west of the mountain. For many years, Svartfjellet was regarded as the highest mountain in Finnmark, but this was due to a measurement error. The highest point in Finnmark actually lies on the glacier Øksfjordjøkelen on the mountain Loppatinden.

Geographic entities mentioned:
surface_form: svartfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 70.232777777778
lon: 21.998611111111
surface_form: svartfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 70.584166666667
lon: 23.859166666667
It opposed the 1979 Soviet invasion of Afghanistan and provided both indirect and direct support for the Afghan mujahideen fighters in their struggle against the Soviet Union which included arming, funding, training and supplying various factions covertly, most notably support for Ahmad Shah Massoud in the Panjshir Valley.

Geographic entities mentioned:
surface_form: Panjshir Valley
instance_of: Valley
countries: Afghanistan
coordinates: lat: 35.266666666667
lon: 69.466666666667
It is situated north of Gerila Glacier and south of the head of Embree Glacier. The glacier drains the northeast slopes of the northern summit of Long Gables Peak and the southeast slopes of Mount Anderson, flows northeastwards and joins upper Ellen Glacier southeast of Eyer Peak. The glacier is named after the Fonfon locality on Vitosha Mountain, Bulgaria. Location. Fonfon Glacier is centred at.

Geographic entities mentioned:
surface_form: Long Gables
instance_of: Mountain
coordinates: lat: -78.1833
lon: -86.2333
surface_form: Eyer Peak
instance_of: Mountain
coordinates: lat: -78.155
lon: -85.9958
It is situated north of Gerila Glacier and south of the head of Embree Glacier. The glacier drains the northeast slopes of the northern summit of Long Gables Peak and the southeast slopes of Mount Anderson, flows northeastwards and joins upper Ellen Glacier southeast of Eyer Peak. The glacier is named after the Fonfon locality on Vitosha Mountain, Bulgaria. Location. Fonfon Glacier is centred at.

Geographic entities mentioned:
surface_form: Vitosha Mountain
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.566666666667
lon: 23.283333333333
It initially flows southeast down a narrow valley between the Big Hill Range and the Wild Man's Brother Range. from source the river trends south, turning southeast again to cross the flat Hakatere Valley where the outflows of several small lakes (collectively known as the Ashburton Lakes) join it.

Geographic entities mentioned:
surface_form: Ashburton Lakes
instance_of: Group of lakes
countries: New Zealand
coordinates: lat: -43.572929
lon: 171.160126
Basilisk Peak. Basilisk Peak () () is, at, the highest peak marking the crater rim of Bellingshausen Island, South Sandwich Islands. The name as applied by the UK Antarctic Place-Names Committee in 1971 &quot;marks the aura of this savage cliff which falls abruptly into a deep and steaming crater where the basilisk of legend might properly have his den.&quot;

Geographic entities mentioned:
surface_form: basilisk peak
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -59.41666667
lon: -27.08333333
Cerro Blanco farther southwest produced ignimbrites, which cover the terrain southwest of Carachipampa, and is still active. Seismic tomography has identified a low-speed anomaly underneath Carachipampa, which connects to it and to several neighbouring volcanoes like Galán and Ojos del Salado.

Geographic entities mentioned:
surface_form: Galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
surface_form: Ojos del Salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
It is probable that in the past, the basin extended to Fiambalá, before it was separated by volcanic activity. Later, activity of the Antofagasta de la Sierra volcanoes farther north removed inflow from the north although it is possible that water still flows underground from Antofagasta to Carachipampa. Until 1905 years ago, the climate was wetter and a terrace formed at Laguna Carachipampa.

Geographic entities mentioned:
surface_form: Antofagasta de la Sierra
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.968055555556
lon: -67.535833333333
Geography. The Southern Alps extend for 500 km, running northeast–southwest down the length of the South Island. Mount Cook (3,754 m), New Zealand's highest peak, is in the Southern Alps. Rainfall is high along the western slope of the mountains, while the eastern slopes are generally drier. Flora. Alpine grassland, also known as tussock herbfield, is the dominant plant community in the ecoregion.

Geographic entities mentioned:
surface_form: Mount Cook
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.595
lon: 170.14194444444445
Description. While relatively low in terms of elevation at compared to other peaks, Taum Sauk and the St. Francois range are true mountains, being the result of a volcanic orogeny. Whereas vertical relief in the rest of the Ozarks region is the result of erosion of sedimentary strata, the St. Francois are an ancient Precambrian igneous uplift several times older than the Appalachians.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
surface_form: the ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
These falls normally have water cascading over them only during times of wet weather. At other times they are reduced to a trickle or less. The Taum Sauk pumped storage plant, which failed on December 14, 2005 sending a flash flood 20 feet (6 m) deep down the Black River, is not actually on Taum Sauk Mountain. It is on Proffit Mountain, about five miles (8 km) southwest.

Geographic entities mentioned:
surface_form: proffit mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.568888888889
lon: -90.781111111111
Taum Sauk State Park is in a common jurisdiction with nearby Johnson's Shut-ins State Park, and together they comprise the second largest state park in Missouri with a total area of. These parks and the adjacent Bell Mountain Wilderness Area make up part of a large wilderness area that is very popular with hikers and backpackers.

Geographic entities mentioned:
surface_form: bell mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.780833333333
lon: -74.153611111111
surface_form: bell mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.236666666667
lon: -113.19527777778
surface_form: bell mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.5828
lon: -117.217
surface_form: bell mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.163333333333
lon: -118.08583333333
surface_form: bell mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.6589
lon: -117.152
Taum Sauk Mountain. Taum Sauk Mountain in the Saint Francois Mountains is the highest natural point in the U.S. state of Missouri at 1,772 feet (540 m). The topography of Taum Sauk is that of an elongated ridge with a NNW-SSE orientation rather than a peak. Description. While relatively low in terms of elevation at compared to other peaks, Taum Sauk and the St.

Geographic entities mentioned:
surface_form: sauk mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.52262
lon: -121.59986
surface_form: taum sauk mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.570327777778
lon: -90.7279
Weathering and erosion of these ancient peaks provided the clastic sediments of the surrounding rock layers. Taum Sauk is said to be named for a Piankeshaw chief named Sauk-Ton-Qua. Though Taum Sauk Mountain is the highest mountain in Missouri, it is not the most prominent. Taum Sauk rises from an already elevated base. Mudlick Mountain rises from a lower base to an elevation of.

Geographic entities mentioned:
surface_form: sauk mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.52262
lon: -121.59986
surface_form: taum sauk mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.570327777778
lon: -90.7279
State park. In 1991 Missouri created Taum Sauk Mountain State Park, a state park on the mountain: it has a rustic campground, a paved trail to the highpoint marked by a polished granite plaque, and a lookout tower from which a good view can be had; the dense forest on the mountain obscures the view from most other vantage points.

Geographic entities mentioned:
surface_form: sauk mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.52262
lon: -121.59986
surface_form: taum sauk mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.570327777778
lon: -90.7279
These falls normally have water cascading over them only during times of wet weather. At other times they are reduced to a trickle or less. The Taum Sauk pumped storage plant, which failed on December 14, 2005 sending a flash flood 20 feet (6 m) deep down the Black River, is not actually on Taum Sauk Mountain. It is on Proffit Mountain, about five miles (8 km) southwest.

Geographic entities mentioned:
surface_form: sauk mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.52262
lon: -121.59986
surface_form: taum sauk
instance_of: Mountain
countries: United States
coordinates: lat: 37.570327777778
lon: -90.7279
surface_form: taum sauk mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.570327777778
lon: -90.7279
These parks and the adjacent Bell Mountain Wilderness Area make up part of a large wilderness area that is very popular with hikers and backpackers. The Taum Sauk section of the Ozark Trail is considered by the Ozark Trail Association to be one of the finest trails in Missouri.

Geographic entities mentioned:
surface_form: ozark
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
surface_form: ozark
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
surface_form: taum sauk
instance_of: Mountain
countries: United States
coordinates: lat: 37.570327777778
lon: -90.7279
Geologists believe that Taum Sauk and its neighbors may be among the few areas in the US never to have been submerged in ancient seas. The peaks of the St. Francois range existed as islands in the shallow seaway throughout most of the Paleozoic Era as the sandstones, limestones, and shales typical of the Ozarks were deposited.

Geographic entities mentioned:
surface_form: ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
surface_form: the ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
Taum Sauk Mountain. Taum Sauk Mountain in the Saint Francois Mountains is the highest natural point in the U.S. state of Missouri at 1,772 feet (540 m). The topography of Taum Sauk is that of an elongated ridge with a NNW-SSE orientation rather than a peak. Description. While relatively low in terms of elevation at compared to other peaks, Taum Sauk and the St.

Geographic entities mentioned:
surface_form: taum sauk
instance_of: Mountain
countries: United States
coordinates: lat: 37.570327777778
lon: -90.7279
The topography of Taum Sauk is that of an elongated ridge with a NNW-SSE orientation rather than a peak. Description. While relatively low in terms of elevation at compared to other peaks, Taum Sauk and the St. Francois range are true mountains, being the result of a volcanic orogeny. Whereas vertical relief in the rest of the Ozarks region is the result of erosion of sedimentary strata, the St.

Geographic entities mentioned:
surface_form: taum sauk
instance_of: Mountain
countries: United States
coordinates: lat: 37.570327777778
lon: -90.7279
Whereas vertical relief in the rest of the Ozarks region is the result of erosion of sedimentary strata, the St. Francois are an ancient Precambrian igneous uplift several times older than the Appalachians. Geologists believe that Taum Sauk and its neighbors may be among the few areas in the US never to have been submerged in ancient seas. The peaks of the St.

Geographic entities mentioned:
surface_form: taum sauk
instance_of: Mountain
countries: United States
coordinates: lat: 37.570327777778
lon: -90.7279
Weathering and erosion of these ancient peaks provided the clastic sediments of the surrounding rock layers. Taum Sauk is said to be named for a Piankeshaw chief named Sauk-Ton-Qua. Though Taum Sauk Mountain is the highest mountain in Missouri, it is not the most prominent. Taum Sauk rises from an already elevated base. Mudlick Mountain rises from a lower base to an elevation of.

Geographic entities mentioned:
surface_form: taum sauk
instance_of: Mountain
countries: United States
coordinates: lat: 37.570327777778
lon: -90.7279
Taum Sauk is said to be named for a Piankeshaw chief named Sauk-Ton-Qua. Though Taum Sauk Mountain is the highest mountain in Missouri, it is not the most prominent. Taum Sauk rises from an already elevated base. Mudlick Mountain rises from a lower base to an elevation of. Black Mountain, in Madison County, has the highest rise in elevation in Missouri. From its base, along the St.

Geographic entities mentioned:
surface_form: taum sauk
instance_of: Mountain
countries: United States
coordinates: lat: 37.570327777778
lon: -90.7279
Taum Sauk State Park is in a common jurisdiction with nearby Johnson's Shut-ins State Park, and together they comprise the second largest state park in Missouri with a total area of. These parks and the adjacent Bell Mountain Wilderness Area make up part of a large wilderness area that is very popular with hikers and backpackers.

Geographic entities mentioned:
surface_form: taum sauk
instance_of: Mountain
countries: United States
coordinates: lat: 37.570327777778
lon: -90.7279
The Taum Sauk section of the Ozark Trail is considered by the Ozark Trail Association to be one of the finest trails in Missouri. Mina Sauk Falls, the highest waterfall in Missouri, is on Taum Sauk and can be visited by hiking a rugged trail that makes a loop from the highpoint parking area. These falls normally have water cascading over them only during times of wet weather.

Geographic entities mentioned:
surface_form: taum sauk
instance_of: Mountain
countries: United States
coordinates: lat: 37.570327777778
lon: -90.7279
Kleiner Wurzelnberg. The Kleiner Wurzelnberg hill rises to a height of in the Harz mountains of Germany, 3.7 km northeast of Sieber in the district of Göttingen in Lower Saxony. It forms a rounded summit (&quot;Kuppe&quot;) on one of the ridges running south of the Acker which acts as the watershed between the Verlorene Kulmke and the Kleine Kulmke.

Geographic entities mentioned:
surface_form: Acker
instance_of: Mountain
countries: Germany
coordinates: lat: 51.7488
lon: 10.4453
surface_form: kuppe
instance_of: Mountain
countries: Germany
coordinates: lat: 51.7267
lon: 10.5086
It forms a rounded summit (&quot;Kuppe&quot;) on one of the ridges running south of the Acker which acts as the watershed between the Verlorene Kulmke and the Kleine Kulmke. The Großer Wurzelnberg is located 750 metres further east on the other side of the valley of the Kleine Kulmke.

Geographic entities mentioned:
surface_form: Großer Wurzelnberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.727825
lon: 10.459222222222
Kleiner Wurzelnberg. The Kleiner Wurzelnberg hill rises to a height of in the Harz mountains of Germany, 3.7 km northeast of Sieber in the district of Göttingen in Lower Saxony. It forms a rounded summit (&quot;Kuppe&quot;) on one of the ridges running south of the Acker which acts as the watershed between the Verlorene Kulmke and the Kleine Kulmke.

Geographic entities mentioned:
surface_form: kleiner wurzelnberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.7289
lon: 10.4486
Mahoning Creek rises due south of the borough of Summit Hill on the opposite side of the divide in a saddle connecting its two flanking ridgelines, runs parallel to and along the south slopes of Pisgah Mountain, diverges from the Mahoning Hills to run along the north-side slopes of Mauch Chunk Mountain, passes through Mahoning Township, then joins the Lehigh River near the borough of Lehighton.

Geographic entities mentioned:
surface_form: Mauch Chunk Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.80984
lon: -76.71591
John Troyer. John Troyer (3 February 1753 – 28 February 1842) was a farmer, businessman, medical practitioner, and exorcist in the Norfolk County, Ontario region. Troyer and family emigrated from southeastern Pennsylvania in 1789 and settled in Ontario, Canada, near Long Point on Lake Erie on a farm. The farm is still known as Troyer's Flats.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Albanian Tower. The Albanian Tower (), also known as Arbanaski pirg is a historic structure located within the Hilandar Monastery on Mount Athos. History. The Tower was thought to be originally being dedicated to Saint George.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Etang de la Gruère. Etang de la Gruère is a small lake in the Jura range near Saignelégier, Canton of Jura, Switzerland. The lake and the surrounding bog is a nature preserve. The lake was formed in the 17th century, when a dam was built for a mill.

Geographic entities mentioned:
surface_form: etang de la gruère
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.238888888889
lon: 7.0466666666667
Heinrichs presented Finnish interest in Eastern Karelia, but Germany recommended a passive stance. The negotiations continued the next day in Berlin with OKH, and contrary to the negotiations of the previous day, Germany wanted Finland to form a strong attack formation ready to strike on the eastern or western side of Lake Ladoga.

Geographic entities mentioned:
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
Flowering occurs in most months and the fruit consists of up to four follicles long and fused at the base. Taxonomy. &quot;Melicope broadbentiana&quot; was first formally described in 1891 by Frederick Manson Bailey in the &quot;Botany Journal&quot; of the Department of Agriculture, Queensland from specimens collected at an altitude of on Mount Bellenden Ker. Distribution and habitat.

Geographic entities mentioned:
surface_form: Mount Bellenden Ker
instance_of: Mountain
countries: Australia
coordinates: lat: -17.264166666667
lon: 145.85388888889
There is a transmission mast about 600 metres away on the spur to the northeast at High Stoy. Writing in 1906, Sir Frederick Treves described High Stoy as &quot;the most engaging of all Dorset hills—a hill of 800 feet, made up of green slopes, a cliff, and a mantle of trees.&quot; Opposite High Stoy is Dogbury Hill, another bastion of the chalk escarpment.

Geographic entities mentioned:
surface_form: Dogbury Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 50.84473889
lon: -2.48013611
A Franciscan friary lies in the hamlet of Hilfield beneath the hill to the west. Films. The area of Minterne, Dogbury Hill and High Stoy was the setting for Thomas Hardy's novel, &quot;The Woodlanders&quot;, Minterne House being referred to as Great Hintock House. The 1990s TV film of Hardy's &quot;Tess of the d'Urbervilles&quot; was made on Dogbury Hill. Sport.

Geographic entities mentioned:
surface_form: Dogbury Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 50.84473889
lon: -2.48013611
With the collaboration of French, Italian and German archaeologists meeting at the Archaeological Congress of Stockholm in 1874, the timing of the Culture of Golasecca became clearer, divided into three periods from 900 to 380 BC. It ended with the Gallic invasion of the Po Valley in 388 BC.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
The site of Golasecca, where the Ticino exits from Lake Maggiore, flourished from particularly favourable geographical circumstances as it was quite suitable for long-distance exchanges, in which Golaseccans acted as intermediaries between Etruscans and the Hallstatt culture of Austria, on the all-important trade in salt.

Geographic entities mentioned:
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
At the site of Sesto Calende, south of Lake Maggiore, were two chariot burials dating to the 7th and 6th century BC accompanied with weapons, ornaments and a large situla while an earlier burial at Ca' Morta – Como (c. 700 BC) included a four-wheeled wagon in the tomb. In a Golasecca culture tomb in Pombia has been found the oldest known remains of common hop beer in the world.

Geographic entities mentioned:
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
It was in regular use for 70 years, from the 1920s into the 1990s, hauling freight and passenger trains all over Switzerland. History. In the 1920s stronger locomotives were needed for the Swiss plateau (which has grades up to 12‰). The existing locomotives with three driven axles were a bit weak for their services.

Geographic entities mentioned:
surface_form: Swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
Torgny Peak. Torgny Peak () is a bare rock peak 2 nautical miles (3.7 km) west of Fenriskjeften Mountain in the Drygalski Mountains of Queen Maud Land. Photographed from the air by the German Antarctic Expedition (1938–39). Mapped from surveys and air photos by Norwegian Antarctic Expedition (1956–60) and named for Torgny Vinje, meteorologist with Norwegian Antarctic Expedition (1956–60).

Geographic entities mentioned:
surface_form: Fenriskjeften Mountain
instance_of: Mountain
coordinates: lat: -71.8833
lon: 8.3
surface_form: torgny peak
instance_of: Mountain
coordinates: lat: -71.85
lon: 8.1
Torgny Peak. Torgny Peak () is a bare rock peak 2 nautical miles (3.7 km) west of Fenriskjeften Mountain in the Drygalski Mountains of Queen Maud Land. Photographed from the air by the German Antarctic Expedition (1938–39). Mapped from surveys and air photos by Norwegian Antarctic Expedition (1956–60) and named for Torgny Vinje, meteorologist with Norwegian Antarctic Expedition (1956–60).

Geographic entities mentioned:
surface_form: torgny peak
instance_of: Mountain
coordinates: lat: -71.85
lon: 8.1
Butterwick is a village and former civil parish, now in the parish of Foxholes (to the east, near the village of Weaverthorpe (to the west), in North Yorkshire, England. The village lies in the Great Wold Valley and the course of the winterbourne stream the Gypsey Race passes through it. Until 1974 the village lay in the historic county boundaries of the East Riding of Yorkshire.

Geographic entities mentioned:
surface_form: Great Wold Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.1385
lon: -0.3835
Hell, Grand Cayman. Hell is an area within the district of West Bay, Grand Cayman. Its name comes from a group of short, black, limestone formations located in the area. Its eerie and rather sinister look is what gave it its infamous name. It is roughly the size of half a football field. Visitors are not permitted to walk on the limestone formations but viewing platforms are provided.

Geographic entities mentioned:
surface_form: hell, grand cayman
instance_of: Landform
countries: United Kingdom
coordinates: lat: 19.37935
lon: -81.40678
Hell, Grand Cayman. Hell is an area within the district of West Bay, Grand Cayman. Its name comes from a group of short, black, limestone formations located in the area. Its eerie and rather sinister look is what gave it its infamous name. It is roughly the size of half a football field. Visitors are not permitted to walk on the limestone formations but viewing platforms are provided.

Geographic entities mentioned:
surface_form: hell
instance_of: Landform
countries: United Kingdom
coordinates: lat: 19.37935
lon: -81.40678
There are numerous versions of how Hell received its name, but they are generally variations on &quot;a ministration exclaimed, 'This is what Hell must look like.'&quot;
It is also claimed that the name &quot;Hell&quot; is derived from the fact that if a pebble is thrown out into the formation, it echoes among the limestone peaks and valleys and sounds as if the pebble is falling all the way down to &quot;Hell.&quot;
Regardless of how it first came to be called Hell, the name stuck and the area has become a tourist attraction, featuring a fire-engine red hell-themed post office from which you can send &quot;postcards from hell&quot;, and a gift shop with &quot;Satan&quot; Ivan Farrington passing out souvenirs while greeting people with phrases like &quot;How the hell are you?&quot; and &quot;Where the hell are you from?&quot;
Some of the stores in the area feature prominent quotations from the Bible on their sides.

Geographic entities mentioned:
surface_form: hell
instance_of: Landform
countries: United Kingdom
coordinates: lat: 19.37935
lon: -81.40678
surface_form: hell
instance_of: Landform
countries: United Kingdom
coordinates: lat: 19.37935
lon: -81.40678
surface_form: hell
instance_of: Landform
countries: United Kingdom
coordinates: lat: 19.37935
lon: -81.40678
surface_form: hell
instance_of: Landform
countries: United Kingdom
coordinates: lat: 19.37935
lon: -81.40678
surface_form: hell
instance_of: Landform
countries: United Kingdom
coordinates: lat: 19.37935
lon: -81.40678
surface_form: hell
instance_of: Landform
countries: United Kingdom
coordinates: lat: 19.37935
lon: -81.40678
surface_form: hell
instance_of: Landform
countries: United Kingdom
coordinates: lat: 19.37935
lon: -81.40678
surface_form: hell
instance_of: Landform
countries: United Kingdom
coordinates: lat: 19.37935
lon: -81.40678
surface_form: hell
instance_of: Landform
countries: United Kingdom
coordinates: lat: 19.37935
lon: -81.40678
Tannenfels Castle (Palatinate). Tannenfels Castle () is a ruined hill castle of the motte and bailey type which stands at a height of above the village of Dannenfels on the Donnersberg hill in the county of Donnersbergkreis in the German state of Rhineland-Palatinate. History. Along with the Barony (&quot;Herrschaft&quot;) of Kirchheim, the castle belonged to the lords of Bolanden.

Geographic entities mentioned:
surface_form: Donnersberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.625280555556
lon: 7.9147194444444
Albert the Great Priory was a Roman Catholic monastery at 41A and 41B Stubbs Road (I.L. no. 3550) in Victoria City, on the mid-levels of Mount Nicholson near Wong Nai Chung Gap on Hong Kong Island, Hong Kong, inaugurated on 24 November 1935, which came to be known as Rosaryhill or Rosary Hill. It was a house of studies of the Dominican Order's Province of Our Lady of the Rosary in the Far East.

Geographic entities mentioned:
surface_form: Mount Nicholson
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.2595
lon: 114.186
Ruud is also the only ski jumper to have won Olympic medals before and after the war and furthermore the one with the longest time period between winning medals at the Olympics (twelve years). Twice he set ski jumping world records: 76.5 m (250.98 ft) in Odnesbakken in 1931, and 92 m (301.84 ft) in Planica in 1934.

Geographic entities mentioned:
surface_form: Planica
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.476944444444
lon: 13.722222222222
Los Altares Valley. Los Altares Valley (&quot;Valle de los Altares&quot;), also called Las Ruinas Valley (&quot;Valle de las Ruinas&quot;) is a valley in central Chubut Province in southern Argentina. It is accessed via National Route 25. Los Altares Valley is crossed by the middle Chubut River, located west of Rawson and east of Tecka.

Geographic entities mentioned:
surface_form: valle de las ruinas
instance_of: Valley
countries: Argentina
coordinates: lat: -43.892
lon: -68.392
surface_form: valle de los altares
instance_of: Valley
countries: Argentina
coordinates: lat: -43.892
lon: -68.392
surface_form: los altares valley
instance_of: Valley
countries: Argentina
coordinates: lat: -43.892
lon: -68.392
Los Altares Valley. Los Altares Valley (&quot;Valle de los Altares&quot;), also called Las Ruinas Valley (&quot;Valle de las Ruinas&quot;) is a valley in central Chubut Province in southern Argentina. It is accessed via National Route 25. Los Altares Valley is crossed by the middle Chubut River, located west of Rawson and east of Tecka.

Geographic entities mentioned:
surface_form: los altares valley
instance_of: Valley
countries: Argentina
coordinates: lat: -43.892
lon: -68.392
Dyirbal people. The Dyirbal, also called Jirrbal, are an Aboriginal Australian people living in northern Queensland, both one tribe (the &quot;Dyirbalŋan&quot; or 'Tully River blacks') and a group of related contiguous peoples included under that label as the Dyirbal tribes. They live on the upper Murray river of the Atherton Tableland.

Geographic entities mentioned:
surface_form: Atherton Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
Description. Mica Mountain is situated southwest of Tête Jaune Cache, British Columbia, at the eastern edge of the Premier Range which is a subset of the Cariboo Mountains. The Southern Yellowhead Highway passes the eastern base of the mountain as it traverses Robson Valley. Precipitation runoff from Mica Mountain drains into Tête Creek and the McLennan River.

Geographic entities mentioned:
surface_form: Robson Valley
instance_of: Valley
countries: Canada
coordinates: lat: 53.25
lon: -120
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Precipitation runoff from Mica Mountain drains into Tête Creek and the McLennan River. Topographic relief is significant as the summit rises over above the creek in. In good weather the view from the summit includes Mount Robson, Canoe Mountain and Kinbasket Lake. The mountain's well-established local name was officially adopted 23 May 1962 by the Geographical Names Board of Canada.

Geographic entities mentioned:
surface_form: Mount Robson
instance_of: Mountain
countries: Canada
coordinates: lat: 53.11055555555556
lon: -119.15666666666667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: canoe mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.70388888888889
lon: -119.16305555555556
Mica Mountain (British Columbia). Mica Mountain is a mountain summit located in British Columbia, Canada. Description. Mica Mountain is situated southwest of Tête Jaune Cache, British Columbia, at the eastern edge of the Premier Range which is a subset of the Cariboo Mountains. The Southern Yellowhead Highway passes the eastern base of the mountain as it traverses Robson Valley.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mica mountain (british columbia)
instance_of: Mountain
countries: Canada
coordinates: lat: 52.88722222222222
lon: -119.52805555555555
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mica Mountain (British Columbia). Mica Mountain is a mountain summit located in British Columbia, Canada. Description. Mica Mountain is situated southwest of Tête Jaune Cache, British Columbia, at the eastern edge of the Premier Range which is a subset of the Cariboo Mountains. The Southern Yellowhead Highway passes the eastern base of the mountain as it traverses Robson Valley.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mica mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.88722222222222
lon: -119.52805555555555
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mica Mountain (British Columbia). Mica Mountain is a mountain summit located in British Columbia, Canada. Description. Mica Mountain is situated southwest of Tête Jaune Cache, British Columbia, at the eastern edge of the Premier Range which is a subset of the Cariboo Mountains. The Southern Yellowhead Highway passes the eastern base of the mountain as it traverses Robson Valley.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mica mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.88722222222222
lon: -119.52805555555555
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The Southern Yellowhead Highway passes the eastern base of the mountain as it traverses Robson Valley. Precipitation runoff from Mica Mountain drains into Tête Creek and the McLennan River. Topographic relief is significant as the summit rises over above the creek in. In good weather the view from the summit includes Mount Robson, Canoe Mountain and Kinbasket Lake.

Geographic entities mentioned:
surface_form: mica mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.88722222222222
lon: -119.52805555555555
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The name refers to the mineral mica which was mined from the higher slopes of the peak in the early 1900s. Climate. Based on the Köppen climate classification, Mica Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures in winter can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: mica mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.88722222222222
lon: -119.52805555555555
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
In good weather the view from the summit includes Mount Robson, Canoe Mountain and Kinbasket Lake. The mountain's well-established local name was officially adopted 23 May 1962 by the Geographical Names Board of Canada. The name refers to the mineral mica which was mined from the higher slopes of the peak in the early 1900s. Climate.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The Towers of the Virgin is a series of several lofty sandstone monoliths on the west side of Zion Canyon in Zion National Park in Washington County, Utah, United States. Description. The peaks of the Towers of the Virgin (from south to northeast) include: The Sundial, The Witch Head, Broken Tooth, Rotten Tooth, Altar of Sacrifice, Meridian Tower, Bee Hive, and The Sentinel.

Geographic entities mentioned:
surface_form: The Witch Head
instance_of: Mountain
countries: United States
coordinates: lat: 37.2198
lon: -113.019
surface_form: Altar of Sacrifice
instance_of: Mountain
countries: United States
coordinates: lat: 37.225934
lon: -113.019858