Sarmila/GeoWiki-Features huggingface dataset:
This suggests that it erupted less than 10,000 years ago when the regional Fraser Glaciation retreated. Cauldron Dome, a subglacial volcano north of Mount Cayley, lies west of the massive glacier covering much the region. Like Pali Dome, it is composed of two geological units. Upper Cauldron Dome is a flat-topped, oval-shaped pile of at least five andesite lava flows that resembles a tuya.

Geographic entities mentioned:
surface_form: pali dome
instance_of: Mountain
countries: Canada
coordinates: lat: 50.136944444444
lon: -123.30694444444
Happy Valley Forest is a large upland forest on steeply rolling topography with various wooded swamps and minor wetland areas. It is located on Ordovician bedrock over the Oak Ridges Moraine. Pottageville Swamp, which was originally contiguous with the Holland Marsh, is now isolated from it because of drainage in the 1920s to prepare the land for agricultural use.

Geographic entities mentioned:
surface_form: Oak Ridges Moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
One of his sons William de Spens was laird of Gylgyrstoun, Glespany and gets the lands of Dumbarnie and Bondiingtoune from William Douglas, 1st Earl of Douglas in 1358. His son William de Spens get married with Isabel Campbell of Glendouglas heiress and daughter of Sir Duncan Campbell of Glen Douglas and Strachur.

Geographic entities mentioned:
surface_form: Glen Douglas
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.15
lon: -4.72
The highway follows the route of A10 through eastern Amsterdam where it runs southwards under the Buiten-IJ using the Zeeburgertunnel, and then using the Zeeburgerbrug over the IJmeer, Nieuwe Diep and Amsterdam&ndash;Rhine Canal. After running across these waters, the road approaches the Watergraafsmeer interchange, where A1 / E 231 starts at its western terminus.

Geographic entities mentioned:
surface_form: IJmeer
instance_of: Lake
countries: Netherlands
coordinates: lat: 52.362778
lon: 5.051944
Tropheus. &quot;Tropheus&quot; is a small genus of at least six species of cichlids endemic to Lake Tanganyika in East Africa. The genus is widespread across all regions of Lake Tanganyika, from Burundi in the north to Zambia in the south. Males and females are relatively similar in color, with only subtle sexual dimorphism in the form of the male's larger size.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
In 2017, the Bank of Canada unveiled a commemorative Canadian ten-dollar note in honour of Canada 150, featuring Cartier's portrait alongside Sir John A. Macdonald, Agnes Macphail and James Gladstone. Mount Cartier near Revelstoke, British Columbia, is named in his honour. Archives. There is a George-Étienne Cartier fonds at Library and Archives Canada.

Geographic entities mentioned:
surface_form: Mount Cartier
instance_of: Mountain
countries: Canada
coordinates: lat: 50.9132
lon: -118.0573
Lac du Lachtelweiher. Lac du Lachtelweiher is a lake in Haut-Rhin, France. At an elevation of 740 m, its surface area is 0.015 km². The French name is a tautology as the German &quot;Weiher&quot; already means &quot;pond&quot;/&quot;lake&quot;.

Geographic entities mentioned:
surface_form: lachtelweiher
instance_of: Lake
countries: France
coordinates: lat: 47.777222222222
lon: 6.9311111111111
surface_form: lac du lachtelweiher
instance_of: Lake
countries: France
coordinates: lat: 47.777222222222
lon: 6.9311111111111
In 1927, before opening, Harder and Hall went bankrupt on the project; it was then purchased by a group including US Congressman Edgar Raymond Kiess, with Vincent Hall returning as resident manager. On January 21, 1928, the classic Spanish Style hotel and golf resort opened on the shore of Little Lake Jackson. Operation.

Geographic entities mentioned:
surface_form: Little Lake Jackson
instance_of: Lake
countries: United States
coordinates: lat: 27.4678
lon: -81.4636
Mount Hoffmann. Mount Hoffmann is a prominent peak in northeastern Mariposa County in the center of Yosemite National Park, California, United States. It rises above May Lake and is a day hike of (one-way) from Tioga Pass Road. The mountain is named for the cartographer Charles F. Hoffmann, who was part of the California Geological Survey of the Sierra Nevada.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: mount hoffmann
instance_of: Mountain
countries: United States
coordinates: lat: 37.8469
lon: -119.511
Mount Hoffmann. Mount Hoffmann is a prominent peak in northeastern Mariposa County in the center of Yosemite National Park, California, United States. It rises above May Lake and is a day hike of (one-way) from Tioga Pass Road. The mountain is named for the cartographer Charles F. Hoffmann, who was part of the California Geological Survey of the Sierra Nevada.

Geographic entities mentioned:
surface_form: may lake
instance_of: Lake
countries: United States
coordinates: lat: 37.847222222222
lon: -119.49361111111
Mount Hoffmann. Mount Hoffmann is a prominent peak in northeastern Mariposa County in the center of Yosemite National Park, California, United States. It rises above May Lake and is a day hike of (one-way) from Tioga Pass Road. The mountain is named for the cartographer Charles F. Hoffmann, who was part of the California Geological Survey of the Sierra Nevada.

Geographic entities mentioned:
surface_form: mount hoffmann
instance_of: Mountain
countries: United States
coordinates: lat: 37.8469
lon: -119.511
Read Creek. Read Creek is a river in Delaware County, New York. It drains Merrick Pond and flows east until it meets the unnamed creek that drains Trask Pond, then begins flowing south receiving its other tributaries before converging with the East Branch Delaware River northeast of Fishs Eddy.

Geographic entities mentioned:
surface_form: Merrick Pond
instance_of: Lake
countries: United States
coordinates: lat: 42.067417
lon: -75.218781
surface_form: Trask Pond
instance_of: Lake
countries: United States
coordinates: lat: 42.069514
lon: -75.204743
The species is a member of the family Plethodontidae, which is characterized by being lungless and reproductive direct development. &quot;P. yonahlossee&quot; was first described in 1917 by E.R Dunn on a collection site on Grandfather Mountain in North Carolina. The common and specific name is of Native American origin, meaning “trail of the bear”.

Geographic entities mentioned:
surface_form: Grandfather Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.111111111111
lon: -81.811388888889
Distribution. &quot;P. yonahlossee&quot; can be found in the southern Blue Ridge Mountains of northern Tennessee, western North Carolina, and small portions of southwest Virginia. Specifically, they have been located in Avery, Yancey, and Rutherford Counties in North Carolina; Rocky Fork State Park & Limestone Cove in Unicoi County, Tennessee, and Whitetop Mountain, Virginia.

Geographic entities mentioned:
surface_form: Whitetop Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.642777777778
lon: -81.607777777778
The couple never had any children. Campaigning for women's suffrage. Lockwood first became involved in public political work in around 1907, and for the next fifteen years she was a significant figure in local politics. She was originally converted to the suffrage cause after hearing Emmeline Pankhurst of the Women's Social and Political Union (WSPU) speak at the 1907 Colne Valley by-election.

Geographic entities mentioned:
surface_form: Colne Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.6272
lon: -1.8624
South Cascade Glacier. South Cascade Glacier is a large alpine glacier in the North Cascades of Washington, USA. It is bordered on the east by Sentinel Peak, and is about north of Glacier Peak in the Glacier Peak Wilderness. Meltwater from the glacier flows directly into South Cascade Lake, which feeds the South Fork Cascade River, which is a tributary of the Skagit River.

Geographic entities mentioned:
surface_form: Glacier Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
South Cascade Glacier. South Cascade Glacier is a large alpine glacier in the North Cascades of Washington, USA. It is bordered on the east by Sentinel Peak, and is about north of Glacier Peak in the Glacier Peak Wilderness. Meltwater from the glacier flows directly into South Cascade Lake, which feeds the South Fork Cascade River, which is a tributary of the Skagit River.

Geographic entities mentioned:
surface_form: South Cascade Lake
instance_of: Lake
countries: United States
coordinates: lat: 48.3711
lon: -121.068
Rio Mesa High School. Rio Mesa High School (RMHS) is a high school in Ventura County, California. Located northeast of Oxnard, the school is surrounded by strawberry fields and other crops growing on the Oxnard Plain. The school is part of the Oxnard Union High School District (OUHSD).

Geographic entities mentioned:
surface_form: Oxnard Plain
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
Paramushir. Paramushir (,) is a volcanic island in the northern portion of the Kuril Islands chain in the Sea of Okhotsk in the northwest Pacific Ocean. It is separated from Shumshu by the very narrow Second Kuril Strait in the northeast, from Antsiferov by the Luzhin Strait () to the southwest, from Atlasov in the northwest by, and from Onekotan in the south by the wide Fourth Kuril Strait.

Geographic entities mentioned:
surface_form: Antsiferov
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
Japan
coordinates: lat: 50.2
lon: 154.98333333333
Royal wet nurses are more likely than most to reach the historical record. In Ancient Egypt, Maia was the wet nurse of King Tutankhamun. Sitre In, the nurse of Hatshepsut, was not a member of the royal family but received the honour of a burial in the royal necropolis in the Valley of the Kings, in tomb KV60. Her coffin has the inscription, meaning &quot;Great Royal Wet Nurse In&quot;.

Geographic entities mentioned:
surface_form: Valley of the Kings
instance_of: Valley
countries: Egypt
coordinates: lat: 25.74025
lon: 32.602358
Geology and physical geography. Terceira island is an active volcanic island, that is composed of several older extinct volcanoes. The highest point of Terceira is 1021 m, formed by the summit of the dormant Santa Barbara volcano, known as the Serra de Santa Bárbara.

Geographic entities mentioned:
surface_form: Serra de Santa Bárbara
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.73333333
lon: -27.31666667
The northern coast is an area marked by evidence of volcanic activity with several mistérios (lava fields), the swimming pools of Biscoitos, while the centre of the island is highlighted by the Algar do Carvão and Furnas do Enxofre (dormant and active volcanic forms) that are popular with tourists and geologists.

Geographic entities mentioned:
surface_form: Algar do Carvão
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.728817
lon: -27.214315
Most of the island is ringed by coastal cliffs about 20 m (60 ft) high, except on the south coast near Angra do Heroísmo. Here, an eruption of basaltic lava in shallow water formed the tuff cone of Monte Brasil, which protects and shelters the harbor of the island's capital. The cone is about in diameter and rises above the western side of the harbor. Ecoregions and protected zones.

Geographic entities mentioned:
surface_form: Monte Brasil
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.643
lon: -27.2213
Many other regions had large societies. Archaeological sites include, La Sierra, and El Curruste in the northwest (thought to have been populated by Western Jicaque speakers), Los Naranjos north of Lake Yojoa, Tenampúa and Yarumela in the Comayagua valley. Some were built by the ancestors of the Lenca people during the pre classic period almost 1000 years before the Mayan cities.

Geographic entities mentioned:
surface_form: Lake Yojoa
instance_of: Lake
Mountain
countries: Honduras
coordinates: lat: 14.877222
lon: -87.980556
Supay Punku. Supay Punku (Quechua &quot;supay&quot; devil, demon, &quot;punku&quot; door, &quot;devil door&quot;) or Supay P'unqu (Quechua &quot;p'unqu&quot; pond, dam, &quot;devil pond&quot; or &quot;devil dam&quot;) is a mountain east of the Apolobamba mountain range in Bolivia, about high.

Geographic entities mentioned:
surface_form: supay punku
instance_of: Mountain
countries: Bolivia
coordinates: lat: -14.88527778
lon: -68.92638889
A few high altitude plants, however, manage to grow in certain crevices of rocks sometimes at very high altitudes. A specimen of glacier buttercup was found at the top of the Finsteraarhorn at an altitude of more than In the glacial zone, the species distribution is very different between calcareous and siliceous rocks.

Geographic entities mentioned:
surface_form: Finsteraarhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.537472222222
lon: 8.1260277777778
Sickle Mountain. Sickle Mountain is a tall mountain standing on the south side of Clarke Glacier and 14 miles (22 km) east of Cape Berteaux, on the west coast of Graham Land. So named by Finn Ronne of the East Base of the United States Antarctic Service (USAS), 1939–41, because its peculiar shape was suggestive of that of a sickle.

Geographic entities mentioned:
surface_form: sickle mountain
instance_of: Mountain
coordinates: lat: -68.883333333333
lon: -66.783333333333
It is located in unorganized territory of the Regional County Municipality of Manicouagan. This ecological reserve protects boreal, montane, and alpine ecosystems in the Toulnustouc River ecological region (domain of the black spruce-fir and moss forest) and that of the Lac Marceau summits (domain of the black spruce fir forest).

Geographic entities mentioned:
surface_form: Toulnustouc River
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.59361111
lon: -68.39333333
It was named in 1932 for James Henry Dege (born 1868), a prominent Tacoma businessman and Captain of the First Regiment National Guard of Washington. The peak is a popular hiking destination with views of the Emmons Glacier, Winthrop Glacier, Inter Glacier, Fryingpan Glacier, Little Tahoma Peak, and views in all directions because the trail is above tree line.

Geographic entities mentioned:
surface_form: Little Tahoma Peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.8496
lon: -121.712
surface_form: tahoma
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
Dege Peak. Dege Peak is a 7,009-foot (2,136 m) summit located in Pierce County of Washington state. It is part of the Sourdough Mountains in Mount Rainier National Park. It was named in 1932 for James Henry Dege (born 1868), a prominent Tacoma businessman and Captain of the First Regiment National Guard of Washington.

Geographic entities mentioned:
surface_form: mount rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
Dege Peak. Dege Peak is a 7,009-foot (2,136 m) summit located in Pierce County of Washington state. It is part of the Sourdough Mountains in Mount Rainier National Park. It was named in 1932 for James Henry Dege (born 1868), a prominent Tacoma businessman and Captain of the First Regiment National Guard of Washington.

Geographic entities mentioned:
surface_form: tacoma
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Dege Peak. Dege Peak is a 7,009-foot (2,136 m) summit located in Pierce County of Washington state. It is part of the Sourdough Mountains in Mount Rainier National Park. It was named in 1932 for James Henry Dege (born 1868), a prominent Tacoma businessman and Captain of the First Regiment National Guard of Washington.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: dege peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.9183
lon: -121.61
Dege Peak. Dege Peak is a 7,009-foot (2,136 m) summit located in Pierce County of Washington state. It is part of the Sourdough Mountains in Mount Rainier National Park. It was named in 1932 for James Henry Dege (born 1868), a prominent Tacoma businessman and Captain of the First Regiment National Guard of Washington.

Geographic entities mentioned:
surface_form: dege peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.9183
lon: -121.61
Access is limited by snowpack closing the Sunrise Road much of the year. July, August, and September are the months when the Sunrise Road is seasonally open for vehicle traffic. Antler Peak is the nearest higher neighbor, to the west. Precipitation runoff from Dege Peak drains into the White River. Climate. Dege Peak is located in the marine west coast climate zone of western North America.

Geographic entities mentioned:
surface_form: dege peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.9183
lon: -121.61
Antler Peak is the nearest higher neighbor, to the west. Precipitation runoff from Dege Peak drains into the White River. Climate. Dege Peak is located in the marine west coast climate zone of western North America. Most weather fronts originating in the Pacific Ocean travel northeast toward the Cascade Mountains.

Geographic entities mentioned:
surface_form: dege peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.9183
lon: -121.61
The trail starts at the Sunrise Historic District. Access is limited by snowpack closing the Sunrise Road much of the year. July, August, and September are the months when the Sunrise Road is seasonally open for vehicle traffic. Antler Peak is the nearest higher neighbor, to the west. Precipitation runoff from Dege Peak drains into the White River. Climate.

Geographic entities mentioned:
surface_form: antler peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.91983
lon: -121.63204
surface_form: antler peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.8686
lon: -110.836
The Ercall. The Ercall is a small hill in Shropshire, England, between The Wrekin and Wellington. It is an internationally important geological site, part of The Wrekin and The Ercall Site of Special Scientific Interest (SSSI). The hill is managed by Shropshire Wildlife Trust and includes 540 million year old ripple beds and ancient pre-Cambrian lava flows in exposed quarries.

Geographic entities mentioned:
surface_form: The Wrekin
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.66916666666667
lon: -2.551388888888889
The green woodpecker is also present in the woods. Access. The hill is accessed in much the same way as The Wrekin nearby; exit the M54 motorway at J7 (last exit) or the last junction of the A5 from Shrewsbury before it becomes the M54. From there The Wrekin is signposted; follow this road until you reach The Wrekin, then follow the sign for the Buckatree Hotel.

Geographic entities mentioned:
surface_form: The Wrekin
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.66916666666667
lon: -2.551388888888889
Geology. The Ercall Quarries are a SSSI and therefore care needs to be exercised when investigating this area. Upon entering the quarry from the main entrance near The Wrekin one encounters an old quarry with many distinctive geological features evident. This is the first quarry that is apparent in the Ercall, it comprises Uriconian Volcanic deposits of Precambrian age.

Geographic entities mentioned:
surface_form: The Wrekin
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.66916666666667
lon: -2.551388888888889
At Santa Ysabel, SR 79 comes to a T intersection with SR 78 running east&ndash;west. SR 79 continues northwest, meeting the eastern terminus of SR 76 near Lake Henshaw at the settlement of Morettis and passing through Warner Springs before crossing into Riverside County. SR 79 then meets the western terminus of SR 371 before going through Aguanga.

Geographic entities mentioned:
surface_form: Lake Henshaw
instance_of: Lake
countries: United States
coordinates: lat: 33.236703
lon: -116.7454423
SR 79 then meets the western terminus of SR 371 before going through Aguanga. It then passes Vail Lake and parallels Temecula Creek as it approaches the Temecula city limits, where it becomes a city-maintained road. It overlaps I-15 for about three miles through Temecula.

Geographic entities mentioned:
surface_form: Vail Lake
instance_of: Lake
countries: United States
coordinates: lat: 33.496111111111
lon: -116.97611111111
surface_form: Temecula Creek
instance_of: Watercourse
countries: United States
coordinates: lat: 33.4742
lon: -117.141
Future. Due to increased traffic congestion through the San Jacinto Valley, there are plans to realign SR 79 to a new four-lane (eventually six-lane) limited-access expressway, spanning approximately 12 miles from East Newport Road to the southern end of the current divided highway portion at Ramona Expressway.

Geographic entities mentioned:
surface_form: San Jacinto Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.7978
lon: -117.005
The area includes Bratislava Forest Park, which is popular with many Bratislavans and is part of the Little Carpathians Protected Landscape Area. The city's lowest point is at the Danube's surface, at above mean sea level, and the highest point is Devínska Kobyla at. The average altitude is. The Záhorie and Danubian Lowlands are partly situated in the city.

Geographic entities mentioned:
surface_form: Devínska Kobyla
instance_of: Mountain
countries: Slovakia
coordinates: lat: 48.190555555556
lon: 16.995833333333
Gallen. The canton of St. Gallen is partially located in the Alps and is one of the nine cantons having summits over 3,000 metres. Topographically, the two most important summits of the canton are those of the Ringelspitz (most elevated and isolated) and the Säntis (most prominent). This list only includes significant summits with a topographic prominence of at least.

Geographic entities mentioned:
surface_form: Ringelspitz
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.899722222222
lon: 9.3441666666667
surface_form: Säntis
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.249167
lon: 9.343333
Menengai. Menengai Crater is a massive shield volcano with one of the biggest calderas in the world, in the Great Rift Valley, Kenya. It is the largest volcano caldera in Kenya and the second largest volcano caldera in Africa. Volcanic formed rich loam soils enrich the adjacent farmland around its flanks. The crater is on the floor of the Rift Valley.

Geographic entities mentioned:
surface_form: kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
surface_form: menengai
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.2
lon: 36.066666666667
Menengai. Menengai Crater is a massive shield volcano with one of the biggest calderas in the world, in the Great Rift Valley, Kenya. It is the largest volcano caldera in Kenya and the second largest volcano caldera in Africa. Volcanic formed rich loam soils enrich the adjacent farmland around its flanks. The crater is on the floor of the Rift Valley.

Geographic entities mentioned:
surface_form: kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
The Menengai volcano is considered one of the best-preserved Krakatau-style calderas in the world. Menengai has very little sediment in the caldera which is a thick mass of lava boulders and inaccessible ridges. Volcanic activity continues and a current project under the GDC is at an advanced stage towards geothermal power generation. Menengai is north of Nakuru, the fourth-biggest city in Kenya.

Geographic entities mentioned:
surface_form: kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
surface_form: menengai
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.2
lon: 36.066666666667
Menengai. Menengai Crater is a massive shield volcano with one of the biggest calderas in the world, in the Great Rift Valley, Kenya. It is the largest volcano caldera in Kenya and the second largest volcano caldera in Africa. Volcanic formed rich loam soils enrich the adjacent farmland around its flanks. The crater is on the floor of the Rift Valley.

Geographic entities mentioned:
surface_form: menengai
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.2
lon: 36.066666666667
The volcano formed about 200,000 years ago and the prominent 12 x 8 km caldera formed about 8000 years ago. The caldera floor is covered with numerous post caldera lava flows. The Menengai volcano is considered one of the best-preserved Krakatau-style calderas in the world. Menengai has very little sediment in the caldera which is a thick mass of lava boulders and inaccessible ridges.

Geographic entities mentioned:
surface_form: menengai
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.2
lon: 36.066666666667
The Menengai volcano is considered one of the best-preserved Krakatau-style calderas in the world. Menengai has very little sediment in the caldera which is a thick mass of lava boulders and inaccessible ridges. Volcanic activity continues and a current project under the GDC is at an advanced stage towards geothermal power generation. Menengai is north of Nakuru, the fourth-biggest city in Kenya.

Geographic entities mentioned:
surface_form: menengai
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.2
lon: 36.066666666667
Wong Tai Sin Temple (Chinese: 黃大仙祠) is a well known shrine and tourist attraction in Hong Kong. It is dedicated to Wong Tai Sin, or the Great Immortal Wong. The Taoist temple is famed for the many prayers answered: &quot;What you request is what you get&quot; () via a practice called &quot;kau chim&quot;. The temple is located on the southern side of Lion Rock in the north of Kowloon. History.

Geographic entities mentioned:
surface_form: Lion Rock
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.3531
lon: 114.187
King Ogato Sana was 10th rulers of the Wolaita kingdom under the Tigre dynasty. King Ogato had erected his palace at top of the Damot hills, driven the Hadiya people out of the present-day Humbo and Abaya in the north, and captured other provinces. To protect himself from intruders, he erected a fortification around his castle on Damot hill, as well as a defense trench surrounding Sore Mashedo.

Geographic entities mentioned:
surface_form: Damot hills
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 6.903583333333334
lon: 37.77938888888889
Kathmandu. Kathmandu () is the capital and largest city of Nepal, situated in the central part of the country within the Kathmandu Valley. As per the 2021 Nepal census, it has a population of 845,767 residing in 105,649 households, with approximately 4 million people in the surrounding metropolitan area. The city stands at an elevation of 4,344 feet (1,324 metres) above sea level.

Geographic entities mentioned:
surface_form: Kathmandu Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
Local officials confirmed structural cracks in a police post but no major destruction. Geography. Kathmandu is in the northwestern part of the Kathmandu Valley to the north of the Bagmati River and covers an area of. The average elevation is above sea level.

Geographic entities mentioned:
surface_form: Kathmandu Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
However, the urban agglomeration extends well beyond the neighbouring municipalities, e.g. to Bhaktapur, and nearly covers the entire Kathmandu Valley. Kathmandu is dissected by eight rivers, the main river of the valley, the Bagmati and its tributaries, of which the Bishnumati, Dhobi Khola, Manohara Khola, Hanumante Khola, and Tukucha Khola are predominant.

Geographic entities mentioned:
surface_form: Kathmandu Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
Stawell School. Stawell School was a short-lived (1927–1940) private school for girls founded by Mabel Hardy and Patience Hawker near the summit of Mount Lofty. History. Mabel Phyllis Hardy (1890–1977) was born in Malvern, South Australia, a member of the once wealthy Hardy family.

Geographic entities mentioned:
surface_form: Mount Lofty
instance_of: Mountain
countries: Australia
coordinates: lat: -34.966666666667
lon: 138.7
From there, its waters reach the North Sea via the Humber Estuary. For almost its entire course it forms the boundary between the counties of Staffordshire (to the west) and Derbyshire (to the east). The river meanders past Longnor and Hartington and cuts through a set of deep limestone gorges, Beresford Dale, Wolfscote Dale, Milldale and Dovedale. The river is a famous trout stream.

Geographic entities mentioned:
surface_form: Dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
He was more interested in the study of Italian art, and in travelling Europe, always bringing home admirable water-colour drawings of buildings and scenery. He was an early and enthusiastic member of the Alpine Club, making several first ascents, notably that of the Lyskamm.

Geographic entities mentioned:
surface_form: Lyskamm
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.9225
lon: 7.8355555555556
The specific epithet (&quot;crassa&quot;) means &quot;thick&quot;, referring to the leaves. Distribution and habitat. &quot;Sannantha crassa&quot; grows in rocky places on steep slopes on the eastern edge of the Northern Tablelands from near Armidale to southern Barrington Tops in eastern New South Wales.

Geographic entities mentioned:
surface_form: Northern Tablelands
instance_of: Plateau
countries: Australia
coordinates: lat: -30.595277777777778
lon: 151.5
surface_form: Barrington Tops
instance_of: Landform
countries: Australia
coordinates: lat: -31.94998
lon: 151.52687
The rich are known to have consumed an array of different meats, such as chicken, shellfish, fallow deer, hares, partridge, pheasant, francolin, quail, fox, badger, clam, crab, and many others. Local freshwater fish from the nearby lake and river were also caught and brought to market, while the West Lake provided geese and duck as well.

Geographic entities mentioned:
surface_form: West Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 30.2375
lon: 120.14083333333
The book also includes a photograph of &quot;Bliss&quot;, which Microsoft allowed O'Rear to include in the book. In 2017, O'Rear was hired by Lufthansa to work on the &quot;New Angles of America&quot; project. He captured the Maroon Bells, the White Pocket in Arizona, and the Peek-A-Boo Slot in Utah. The photographs were made available as free wallpapers for mobile phones.

Geographic entities mentioned:
surface_form: Maroon Bells
instance_of: Mountain
countries: United States
coordinates: lat: 39.0708
lon: -106.989
Heritage. Antiquities in the area include the Clonkeen stone. This is said to be 340 million years old and legend has it that the stone was thrown from Croghan Hill by Fionn MacCumhaill. Other sites includes the remains of a togher at Ballykilleen, the ruins of Cloncrane Church, a ring-barrow at Shean and a sheela-na-gig from Ballynowlart and Clonsast.

Geographic entities mentioned:
surface_form: Croghan Hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.2
lon: -7.16
From the 14th century onward, equal-length civil hours supplanted unequal ones, so civil time no longer varied by season. Unequal hours are still used in a few traditional settings, such as monasteries of Mount Athos and in Jewish ceremonies.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
state of Washington. It starts at the confluence of the Middle and North Forks of Ahtanum Creek near Tampico, flows along the north base of Ahtanum Ridge, ends at the Yakima River near Union Gap and forms a portion of the northern boundary of the Yakama Indian Reservation. The name &quot;Ahtanum&quot; originates from the Sahaptin language, which was spoken by Native Americans in the region.

Geographic entities mentioned:
surface_form: Ahtanum Ridge
instance_of: Landform
countries: United States
coordinates: lat: 46.5069
lon: -120.816
Piz Cavel. Piz Cavel is a mountain of the Lepontine Alps, situated between the Val Sumvitg and the Lumnezia in the canton of Graubünden. The closest locality is Vrin on the eastern side.

Geographic entities mentioned:
surface_form: piz cavel
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.656
lon: 9.0198333333333
It is recorded that &quot;Robert Gillespie, an irregular preacher &quot;at the horn&quot;, was taken after a conventicle at Falkland, and on 2nd April sent by the Privy Council to the Bass to be immured.&quot; He was imprisoned on the Bass Rock between 2 April 1673 and 8 January 1674. He was the first person imprisoned there for Presbyterian principles.

Geographic entities mentioned:
surface_form: Bass
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.08
lon: -2.64
surface_form: Bass Rock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.08
lon: -2.64
Gartow. Gartow is a municipality in the district Lüchow-Dannenberg, in Lower Saxony, Germany. It is situated in the easternmost tip of Lower Saxony, not far from the river Elbe, approx. 30 km northeast of Salzwedel, and 20 km west of Wittenberge. Gartow is also the seat of the &quot;Samtgemeinde&quot; (&quot;collective municipality&quot;) Gartow. Geography.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Mudeungsan National Park. Mudeungsan National Park (), previously Mudeungsan Provincial Park, is located in the city of Gwangju and the province of Jeollanam-do, South Korea. The park was designated a provincial park on 22 May 1972 and was upgraded to national park status in 2012, making it South Korea's 21st national park. The park has an area of and is named after the 1,187 m tall Mudeungsan.

Geographic entities mentioned:
surface_form: Mudeungsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 35.134166666667
lon: 126.98888888889
Pag Triangle. Pag triangle () is a pareidolia and land formation in the shape of an irregular quadrilateral located near the village Caska, adjacent to Novalja on the Croatian island Pag. It has been designated a natural landmark by the town of Novalja. It is often referred to as &quot;the Bermuda triangle of Croatia&quot;.

Geographic entities mentioned:
surface_form: pag triangle
instance_of: Landform
countries: Croatia
coordinates: lat: 44.562555555556
lon: 14.919083333333
In reality, the Gap is a dip in the Owen Stanley Range about wide, convenient for aircraft crossing the range to pass through. The track reaches a height of as it passes around the peak of Mount Bellamy. The terrain rises and falls with regularity, up to up and down over the full length of the track.

Geographic entities mentioned:
surface_form: Mount Bellamy
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -9.05
lon: 147.68333333
St. Stephan railway station. St. Stephan railway station () is a railway station in the municipality of St. Stephan, in the Swiss canton of Bern. It is an intermediate stop on the Montreux–Lenk im Simmental line of the Montreux Oberland Bernois Railway. Services. During the ski season there is a connecting bus to the Lengebrand–Parwengesattel chairlift to the Rinderberg.

Geographic entities mentioned:
surface_form: Rinderberg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.505277777778
lon: 7.3568055555556
Folldal Municipality. Folldal is a municipality in Innlandet county, Norway. It is located in the traditional district of Østerdalen. The administrative centre of the municipality is the village of Folldal. The municipality was established in 1914 when it was separated from Alvdal Municipality.

Geographic entities mentioned:
surface_form: Østerdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.575916666666664
lon: 11.087111111111112
The rest of the surrounding municipalities are all in Innlandet county. Tynset Municipality lies to the northeast, Alvdal Municipality is to the east, Stor-Elvdal Municipality is to the southeast, Sør-Fron Municipality and Sel Municipality are to the south, and Dovre Municipality is to the west. The highest point in the municipality is the tall mountain Rondeslottet.

Geographic entities mentioned:
surface_form: Rondeslottet
instance_of: Mountain
countries: Norway
coordinates: lat: 61.914722222222
lon: 9.8511111111111
Folldal Municipality is notable because the village of Folldal, its administrative center, has the highest elevation (above sea level) of all administrative centres in Norway. The village has picturesque scenery with mountains and valleys. The village lies at the foot of Rondeslottet mountain and Snøhetta mountain. The area also has many interesting geologic features from the last Ice Age.

Geographic entities mentioned:
surface_form: Rondeslottet
instance_of: Mountain
countries: Norway
coordinates: lat: 61.914722222222
lon: 9.8511111111111
surface_form: Snøhetta
instance_of: Mountain
countries: Norway
coordinates: lat: 62.32
lon: 9.2683333333333
Climate. Folldal has a subarctic climate (Dfc) with short, cool summers and long, cold winters. Situated in a mountain valley on the southern, continental side of the Dovre mountain range at above sea level, it has the coldest winters in the southern half of Norway. Outdoors. Folldal Municipality offers a wide variety of outdoor activities.

Geographic entities mentioned:
surface_form: Dovre
instance_of: Mountain
countries: Norway
coordinates: lat: 62.1
lon: 9.41666667
It last erupted in the Pleistocene. Geography. Cappy Mountain lies on the northern border of the Mount Thielsen Wilderness. It is surrounded by other Cascade volcanoes, such as the Cinnamon Butte volcanic field to the southwest, Howlock Mountain and Mount Thielsen to the south, and Cowhorn Mountain and Sawtooth Mountain to the north and northwest respectively.

Geographic entities mentioned:
surface_form: Cinnamon Butte
instance_of: Mountain
countries: United States
coordinates: lat: 43.241
lon: -122.11
surface_form: Howlock Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.19235
lon: -122.03975
surface_form: Mount Thielsen
instance_of: Mountain
countries: United States
coordinates: lat: 43.152837292
lon: -122.066514283
surface_form: sawtooth mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.150277777778
lon: -113.39916666667
surface_form: sawtooth mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.0699611
lon: -121.772014
It last erupted in the Pleistocene. Geography. Cappy Mountain lies on the northern border of the Mount Thielsen Wilderness. It is surrounded by other Cascade volcanoes, such as the Cinnamon Butte volcanic field to the southwest, Howlock Mountain and Mount Thielsen to the south, and Cowhorn Mountain and Sawtooth Mountain to the north and northwest respectively.

Geographic entities mentioned:
surface_form: mount thielsen
instance_of: Mountain
countries: United States
coordinates: lat: 43.152837292
lon: -122.066514283
surface_form: cappy mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.310277777778
lon: -121.97888888889
Cappy Mountain. Cappy Mountain, located in Klamath County in the U.S. state of Oregon, is a stratovolcano in the Cascade Range. It last erupted in the Pleistocene. Geography. Cappy Mountain lies on the northern border of the Mount Thielsen Wilderness.

Geographic entities mentioned:
surface_form: cappy mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.310277777778
lon: -121.97888888889
Pharaoh Peaks. Pharaoh Peaks is a triple summit mountain located in Banff National Park in Alberta, Canada. Pharaoh Peaks are part of the Ball Range in the Canadian Rockies. The nearest higher peak is Scarab Peak, to the southwest.

Geographic entities mentioned:
surface_form: pharaoh peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1167
lon: -115.90213
Pharaoh Peaks. Pharaoh Peaks is a triple summit mountain located in Banff National Park in Alberta, Canada. Pharaoh Peaks are part of the Ball Range in the Canadian Rockies. The nearest higher peak is Scarab Peak, to the southwest.

Geographic entities mentioned:
surface_form: pharaoh peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1167
lon: -115.90213
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Geology. Like other mountains in Banff Park, Pharaoh Peaks are composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate.

Geographic entities mentioned:
surface_form: pharaoh peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1167
lon: -115.90213
Pharaoh Peaks are part of the Ball Range in the Canadian Rockies. The nearest higher peak is Scarab Peak, to the southwest. The mountain's name Pharaoh was in keeping with the Egyptian theme of the immediate surrounding area, e.g., Egypt Lake, Pharaoh Lake, Mummy Lake, and Scarab Lake, which were applied in 1922 by Arthur O. Wheeler of the Interprovincial Boundary Survey.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
can safely say that outstanding among them for scenic charm and interest may be classed the group of peaks, lakes and alpine meadows of the Egypt Lake area.&quot; The mountain's name was officially adopted in 1956 when approved by the Geographical Names Board of Canada. Geology.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate. Based on the Köppen climate classification, the mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Climate. Based on the Köppen climate classification, the mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. In terms of favorable weather, June through September are the best months to climb the mountain. Precipitation runoff from the mountain drains into tributaries of the Bow River.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Pharaoh Peaks are part of the Ball Range in the Canadian Rockies. The nearest higher peak is Scarab Peak, to the southwest. The mountain's name Pharaoh was in keeping with the Egyptian theme of the immediate surrounding area, e.g., Egypt Lake, Pharaoh Lake, Mummy Lake, and Scarab Lake, which were applied in 1922 by Arthur O. Wheeler of the Interprovincial Boundary Survey.

Geographic entities mentioned:
surface_form: scarab peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.096111111111114
lon: -115.93277777777779
On, a holding dam burst at the Los Frailes mine, near Aznalcóllar, Seville, releasing of mine tailings. The acidic tailings, which contained dangerous levels of several heavy metals, quickly reached the nearby River Agrio, and then its parent river, the River Guadiamar, travelling about along these waterways and covering an area of before they could be stopped.

Geographic entities mentioned:
surface_form: Guadiamar
instance_of: Watercourse
countries: Spain
coordinates: lat: 36.90344
lon: -6.334784
Lumbering and fishing also play a role. Tourism. The region has long been a popular destination due to the proximity of Mount Kŭmgang and, in recent years, tourists from South Korea have passed through the area in great numbers. Transport. A highway runs along the coastline.

Geographic entities mentioned:
surface_form: Mount Kŭmgang
instance_of: Mountain
countries: North Korea
coordinates: lat: 38.656763888889
lon: 128.10490277778
Stage 7. The seventh stage took the riders from Tomblaine to La Super Planche des Belles Filles for the first summit finish of the race. The first half of the stage was mostly flat before the riders went on a false flat uphill to the intermediate sprint in Gérardmer with left.

Geographic entities mentioned:
surface_form: La Super Planche des Belles Filles
instance_of: Mountain
countries: France
coordinates: lat: 47.7672
lon: 6.77417
71gx4w4on6iizwpqh79mge9qtxv6s" xml:space="preserve">The Serbian Football Championship was the unofficial championship of Serbia organized by the Belgrade Football Subassociation (a Belgrade branch of the Football Association of Yugoslavia was covering territory of former Kingdom of Serbia, Vojvodina and eastern part of Bosnia and Herzegovina) and had two editions in 1920 and 1921, before Subotica Football Subassociation started its own championship in 1922 in Bačka region.

Geographic entities mentioned:
surface_form: eastern part of Bosnia and Herzegovina
instance_of: Landform
countries: Bosnia and Herzegovina
coordinates: lat: 44.80083333
lon: 19.21361111
The people who lived along the stream were called Grušované. Geography. Hrušovany u Brna is located about south of Brno. It lies in the Dyje–Svratka Valley. The highest point is at above sea level. The municipality is situated on the right bank of the Šatava River. History. The first written mention of Hrušovany is from 1252, when the village was donated to the monastery in Žďár nad Sázavou.

Geographic entities mentioned:
surface_form: Dyje–Svratka Valley
instance_of: Valley
countries: Czech Republic
coordinates: lat: 49
lon: 16.5
Geography. According to the United States Census Bureau, the township has a total area of, of which is land and, or 7.70%, is water. It is bordered on the north by Gilmore Township, on the east by Joyfield Township, on the south by Arcadia and Pleasanton townships in Manistee County, and on the west by Lake Michigan.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
It has been the seat of the district of Gmina Czorsztyn since 1993. Located on the southern slopes of the Gorce Mountains, new Maniowy was built in 1970-1980s after having been moved to a higher altitude, from an area upon which Lake Czorsztyn now stretches. The history of the old village reached back to at least 1326 when it was founded during the colonisation of the Podhale region.

Geographic entities mentioned:
surface_form: Lake Czorsztyn
instance_of: Lake
countries: Poland
coordinates: lat: 49.44
lon: 20.2625
It has been the seat of the district of Gmina Czorsztyn since 1993. Located on the southern slopes of the Gorce Mountains, new Maniowy was built in 1970-1980s after having been moved to a higher altitude, from an area upon which Lake Czorsztyn now stretches. The history of the old village reached back to at least 1326 when it was founded during the colonisation of the Podhale region.

Geographic entities mentioned:
surface_form: Podhale
instance_of: Valley
countries: Poland
coordinates: lat: 49.4793
lon: 20.0291