Sarmila/GeoWiki-Features huggingface dataset:
selenopoides&quot; and &quot;H. theologus&quot;. They are found in the southern United States and Mexico: &quot;H. theologus&quot; is mostly found west of the Colorado River, while &quot;H. selenopoides&quot; is mostly found to the east, with some populations in Death Valley and near Mercury, Nevada. They do not build webs, and are typically found under rocks or dead vegetation.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Mount Baleen. Mount Baleen () is a prominent peak of 910 m and of pyramidal shape when viewed from Larsen Ice Shelf, standing in Padesh Ridge between Rachel and Starbuck Glaciers in Aristotle Mountains on the east coast of Graham Land. The naming by United Kingdom Antarctic Place-Names Committee (UK-APC) is one in a group in this vicinity that reflects a whaling theme.

Geographic entities mentioned:
surface_form: baleen
instance_of: Mountain
coordinates: lat: -65.6
lon: -62.2
surface_form: mount baleen
instance_of: Mountain
coordinates: lat: -65.6
lon: -62.2
The naming by United Kingdom Antarctic Place-Names Committee (UK-APC) is one in a group in this vicinity that reflects a whaling theme. Baleen whales are distinguished by the presence of a sieve of horny baleen (whalebone) plates suspended from the upper jaw, and by the absence of teeth.

Geographic entities mentioned:
surface_form: baleen
instance_of: Mountain
coordinates: lat: -65.6
lon: -62.2
surface_form: baleen
instance_of: Mountain
coordinates: lat: -65.6
lon: -62.2
A little over a week later on July 23, defenseman Dmitri Tertyshny, coming off his rookie season, was fatally injured in a boating accident. Tertyshny was on a boating trip to Okanagan Lake in British Columbia with two players from the Flyers' minor-league affiliate Philadelphia Phantoms, Francis Belanger and Mikhail Chernov, when a freak accident caused him to suffer fatal injuries.

Geographic entities mentioned:
surface_form: Okanagan Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.920833333333
lon: -119.5
Adelaide Island. Adelaide Island is a large, mainly ice-covered island, long and wide, lying at the north side of Marguerite Bay off the west coast of the Antarctic Peninsula. The Ginger Islands lie off the southern end. Mount Bodys is the easternmost mountain on Adelaide Island, rising to over 1,220 m. The island lies within the Argentine, British and Chilean Antarctic claims. History.

Geographic entities mentioned:
surface_form: Mount Bodys
instance_of: Mountain
coordinates: lat: -67.15
lon: -67.8
The point was named by the UK Antarctic Place-Names Committee (UK-APC) for Joseph K. Landauer, an American physicist. To the south is Mothes Point, southwest of The Gullet. It was mapped by FIDS from RARE photos, and FIDASE in 1956–57. It was named by UK-APC for German glaciologist Hans Mothes. Continuing south, is Mackay Point about to the north-northeast of Rothera Point.

Geographic entities mentioned:
surface_form: The Gullet
instance_of: Body of water
coordinates: lat: -67.1667
lon: -67.6333
Rothera. The point is protected as Antarctic Specially Protected Area (ASPA) No.129 so that it would serve as a biological research site and control area against which the environmental impact of the adjacent Rothera Research Station could be monitored in an Antarctic fellfield ecosystem. On the southeast coast of the island, east of Mount Gaudry, wide Ryder Bay indents the coast to a depth of.

Geographic entities mentioned:
surface_form: Mount Gaudry
instance_of: Mountain
coordinates: lat: -67.5333
lon: -68.6167
The bay is named for Lisle C.D. Ryder, second mate on the &quot;Penola&quot; during the BGLE, 1934–37. Ives Bank is a submarine bank in the Bellingshausen Sea on the southern approaches to Ryder Bay. The southeast extremity of the island is Cape Alexandra, named by Charcot for Alexandra of Denmark, then Queen consort of England.

Geographic entities mentioned:
surface_form: Ives Bank
instance_of: Landform
coordinates: lat: -67.6667
lon: -68.2
It is an important and well-known tourist destination in the Bernese Oberland region of the Swiss Alps, and the main transport gateway to the mountains and lakes of that region. The town is located on flat alluvial land called Bödeli between two lakes, Brienz to the east and Thun to the west, and alongside the river Aare, which flows between them.

Geographic entities mentioned:
surface_form: Brienz
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.716667
lon: 7.95
surface_form: Thun
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.683333333333
lon: 7.7166666666667
Transport routes to the east and west alongside the lakes are complemented by a route southwards into the near mountain resorts and high mountains, e.g. the famous high Alpine peaks of Eiger, Mönch and Jungfrau, following upwards the Lütschine. Interlaken is the central town of a small agglomeration with the same name of 23,300 inhabitants.

Geographic entities mentioned:
surface_form: Eiger
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.577607529
lon: 8.005286822
surface_form: Mönch
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.558333333333
lon: 7.9972222222222
surface_form: Jungfrau
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.536944444444
lon: 7.9625
By 1247, there were also women at the monastery. During the 13th century the monastery's influence spread throughout the neighboring area and into the Aare and Gürbe valleys. They eventually had authority over two dozen churches along with a number of villages and farms and became the largest religious landholder in the region.

Geographic entities mentioned:
surface_form: Gürbe valleys
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.836111111111
lon: 7.5063888888889
However, in 1893, the Lake Thun railway line opened alongside Lake Thun providing a direct rail connection to Thun, with onward connections to Bern and beyond. In 1888, the Brünig railway opened between Alpnachstad, on Lake Lucerne, and Brienz, on Lake Brienz, thus providing a through steamer and rail connection from Interlaken to Lucerne.

Geographic entities mentioned:
surface_form: Lake Lucerne
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.0194
lon: 8.4011
In 1890, the Berner Oberland railway connected Interlaken to the tourist destinations of Lauterbrunnen and Grindelwald. With the opening up of transport links, hotels developed along the route to the Jungfrau. In 1860–75 and 1890–1914 several luxury hotels were built with views of the Jungfrau and surrounding mountains. The current Kursaal was built in 1898-99 and remodeled in 1909–10.

Geographic entities mentioned:
surface_form: Jungfrau
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.536944444444
lon: 7.9625
Of the 562 who completed tertiary schooling, 62.3% were Swiss men, 21.4% were Swiss women, 8.4% were non-Swiss men and 8.0% were non-Swiss women. Tourism. The town is principally a base from which to explore the surrounding areas. Among the main attractions are the mountains of the Jungfrau region, including the Jungfrau, (), the Mönch () and the Eiger ().

Geographic entities mentioned:
surface_form: Jungfrau
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.536944444444
lon: 7.9625
surface_form: Mönch
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.558333333333
lon: 7.9972222222222
surface_form: Eiger
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.577607529
lon: 8.005286822
Closer to Interlaken, the Harderkulm (), just to the north of the town, and the Schynige Platte (), just to the south, are also accessible by railway and provide extensive views of the higher mountains. Lake Thun and Lake Brienz are both close to the town, and the Aare flows east to west through the town. Boat trips operate on both lakes, serving various lakeside towns.

Geographic entities mentioned:
surface_form: Harderkulm
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.697269444444
lon: 7.8516611111111
surface_form: Schynige Platte
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.656111111111
lon: 7.9069444444444
The Berner Oberland railway also operates from Ost station, providing the first stage of several mountain railway routes into the Jungfrau region and, most notably, to Europe's highest station at the Jungfraujoch. Boat services across Lake Brienz to Brienz and across Lake Thun to Spiez and Thun are operated by the BLS AG.

Geographic entities mentioned:
surface_form: Lake Brienz
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.716667
lon: 7.95
surface_form: Lake Thun
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.683333333333
lon: 7.7166666666667
Both Malay and English are used in the road signs that are located along the Pengerang Highway (Federal Route 92), which links Kota Tinggi to Sungai Rengit in Johor state and Genting Sempah-Genting Highlands Highway which links Genting Sempah to Genting Highlands, which also have Chinese and Tamil on signs.

Geographic entities mentioned:
surface_form: Genting Highlands
instance_of: Mountain
countries: Malaysia
coordinates: lat: 3.42368
lon: 101.79335
This raiding was likely the reason for their village's location deep inside Salmon Bay, rather than being directly on Puget Sound. They also used the nearby Bitter Lake () and Haller Lake () as places of refuge during these raids. They hunted and gathered in the area as well; their usage of the area being proven by artifacts discovered at Haller Lake.

Geographic entities mentioned:
surface_form: Haller Lake
instance_of: Lake
countries: United States
coordinates: lat: 47.719619
lon: -122.334688
Despite living on a saltwater estuary, they were one of the, the Lake Peoples, a traditional ethnic identity of the Lushootseed-speaking world, whose villages were primarily located around the freshwater lakes Washington and Union. This is due to their connection to the other Lake Peoples and their reliance on the resources of Lake Washington and Lake Union. Salmon Bay Charlie.

Geographic entities mentioned:
surface_form: Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: Union
instance_of: Lake
countries: United States
coordinates: lat: 47.6392
lon: -122.3337
Chattahoochee river. ovmm04nq2vq37xurbwif09dd00b" xml:space="preserve">#REDIRECT Chattahoochee River

Geographic entities mentioned:
surface_form: chattahoochee river
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Mount Cornwall. Mount Cornwall is a prominent summit located between the Elbow River valley and Little Elbow River valley of Kananaskis Country in the Canadian Rockies of Alberta, Canada. The peak is visible from Highway 66, weather permitting. Mount Cornwall's nearest higher peak is Tombstone Mountain, to the southwest. __NOTOC__
History.

Geographic entities mentioned:
surface_form: Tombstone Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.68336
lon: -115.0187
surface_form: mount cornwall
instance_of: Mountain
countries: Canada
coordinates: lat: 50.738
lon: -114.947
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: tombstone mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 64.4051
lon: -138.6817
__NOTOC__
History. Mount Cornwall was named in 1922 for, a British warship involved in the Battle of the Falkland Islands during the First World War in the South Atlantic. The first ascent of the peak was made in 1949 by Arnold Choquette. The mountain's name became official in 1951 by the Geographical Names Board of Canada. Geology.

Geographic entities mentioned:
surface_form: arnold
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.455833333333
lon: -70.865277777778
Mount Cornwall. Mount Cornwall is a prominent summit located between the Elbow River valley and Little Elbow River valley of Kananaskis Country in the Canadian Rockies of Alberta, Canada. The peak is visible from Highway 66, weather permitting. Mount Cornwall's nearest higher peak is Tombstone Mountain, to the southwest. __NOTOC__
History.

Geographic entities mentioned:
surface_form: mount cornwall
instance_of: Mountain
countries: Canada
coordinates: lat: 50.738
lon: -114.947
The peak is visible from Highway 66, weather permitting. Mount Cornwall's nearest higher peak is Tombstone Mountain, to the southwest. __NOTOC__
History. Mount Cornwall was named in 1922 for, a British warship involved in the Battle of the Falkland Islands during the First World War in the South Atlantic. The first ascent of the peak was made in 1949 by Arnold Choquette.

Geographic entities mentioned:
surface_form: mount cornwall
instance_of: Mountain
countries: Canada
coordinates: lat: 50.738
lon: -114.947
The first ascent of the peak was made in 1949 by Arnold Choquette. The mountain's name became official in 1951 by the Geographical Names Board of Canada. Geology. Mount Cornwall is 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: mount cornwall
instance_of: Mountain
countries: Canada
coordinates: lat: 50.738
lon: -114.947
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, Mount Cornwall is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below.

Geographic entities mentioned:
surface_form: mount cornwall
instance_of: Mountain
countries: Canada
coordinates: lat: 50.738
lon: -114.947
__NOTOC__
History. Mount Cornwall was named in 1922 for, a British warship involved in the Battle of the Falkland Islands during the First World War in the South Atlantic. The first ascent of the peak was made in 1949 by Arnold Choquette. The mountain's name became official in 1951 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
Climate. Based on the Köppen climate classification, Mount Cornwall is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below. Precipitation runoff from the mountain drains into the Elbow River which is a tributary of the Bow River.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
New Jezreel Valley railway. The New Jezreel Valley Railway () is a railway of Israel Railways (IR), which connects Haifa with Beit She'an in the Jezreel Valley. The railway line was opened to the public on October 16, 2016. It is a successor to the 1905 Ottoman Jezreel Valley railway. History.

Geographic entities mentioned:
surface_form: Jezreel Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
The Scranton International Airport is located in Pittston Township. Establishment. Pittston Township was one of the five original townships formed under the Susquehanna Land Company of Connecticut (in the Wyoming Valley). It was originally known as Pittstown (named for Sir William Pitt, an English statesman). Each township was originally five square miles and divided amongst forty settlers.

Geographic entities mentioned:
surface_form: Wyoming Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
Geography. Its limits extend from the Fort of São Benedito until the eastern edge of Monte Brasil, along the second line of defensive walls that protected the mountain, for approximately. The depth at which the artefacts and ruins exist varies from (in an area of rocks) until (in an area of sand).

Geographic entities mentioned:
surface_form: Monte Brasil
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.643
lon: -27.2213
It is located in the Moquegua Region, Mariscal Nieto Province, Torata District, and in the Tacna Region, Candarave Province, Camilaca District. Apacheta Limani is situated south of the mountain Limani, northwest of the Tutupaca volcano, Chuquiananta and Huañuma, and northeast of Pomani. The Asana River originates near Apacheta Limani. It flows to the southwest.

Geographic entities mentioned:
surface_form: Tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
surface_form: Chuquiananta
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0814
lon: -70.4494
surface_form: Huañuma
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0658
lon: -70.4467
surface_form: Pomani
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0703
lon: -70.4717
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
surface_form: huañuma
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0658
lon: -70.4467
surface_form: pomani
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0703
lon: -70.4717
surface_form: chuquiananta
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0814
lon: -70.4494
Apacheta Limani. Apacheta Limani (possibly from Aymara &quot;apachita&quot; the place of transit of an important pass in the principal routes of the Andes; name in the Andes for a stone cairn, a little pile of rocks built along the trail in the high mountains, &quot;-ni&quot; a suffix to indicate ownership) is a mountain in the Andes of southern Peru, about high.

Geographic entities mentioned:
surface_form: apacheta limani
instance_of: Mountain
countries: Peru
coordinates: lat: -17.015
lon: -70.4603
surface_form: apacheta
instance_of: Mountain
countries: Peru
coordinates: lat: -15.3842
lon: -72.1789
It is located in the Moquegua Region, Mariscal Nieto Province, Torata District, and in the Tacna Region, Candarave Province, Camilaca District. Apacheta Limani is situated south of the mountain Limani, northwest of the Tutupaca volcano, Chuquiananta and Huañuma, and northeast of Pomani. The Asana River originates near Apacheta Limani. It flows to the southwest.

Geographic entities mentioned:
surface_form: apacheta limani
instance_of: Mountain
countries: Peru
coordinates: lat: -17.015
lon: -70.4603
surface_form: apacheta
instance_of: Mountain
countries: Peru
coordinates: lat: -15.3842
lon: -72.1789
Mont Granier. Mont Granier (1,933m) is a limestone mountain located between the départements of Savoie and Isère in France. It lies in the Chartreuse Mountains range of the French Prealps between the towns of Chapareillan and Entremont-le-Vieux. Its east face overlooks the valley of Grésivaudan and Combe de Savoie, and the north face overlooks Chambéry.

Geographic entities mentioned:
surface_form: mont granier
instance_of: Mountain
countries: France
coordinates: lat: 45.46472222
lon: 5.92527778
surface_form: granier
instance_of: Mountain
countries: France
coordinates: lat: 45.46472222
lon: 5.92527778
It lies in the Chartreuse Mountains range of the French Prealps between the towns of Chapareillan and Entremont-le-Vieux. Its east face overlooks the valley of Grésivaudan and Combe de Savoie, and the north face overlooks Chambéry. At 900 meters tall, Mont Granier has one of the highest cliffs in France. Catastrophic 1248 Landslide.

Geographic entities mentioned:
surface_form: mont granier
instance_of: Mountain
countries: France
coordinates: lat: 45.46472222
lon: 5.92527778
surface_form: granier
instance_of: Mountain
countries: France
coordinates: lat: 45.46472222
lon: 5.92527778
Activities. It is a popular spot for hiking, caving, rock climbing, and BASE jumping. Around the base of Mont Granier are many vineyards that produce the Apremont and Abymes appellations. These wines are made from the white Jacquère grape, seldom used outside Savoie. The Col du Granier (1,134 m.) crosses the ridge to the north-west of the mountain. Caving.

Geographic entities mentioned:
surface_form: granier
instance_of: Mountain
countries: France
coordinates: lat: 45.46472222
lon: 5.92527778
Caving. 454 caves have been identified over an area of 2.8 km2, and form two networks under this small area. To the north, the trou des Auges, ressaut de 108 m, trou des Filous, grotte Arva, and Cuvée des Ours connect with the Granier system, located in the center of the plateau, to form a 55.725 km network over a depth of 635 meters.

Geographic entities mentioned:
surface_form: granier
instance_of: Mountain
countries: France
coordinates: lat: 45.46472222
lon: 5.92527778
The latter consists of the Gros trou Bib, trou des Panaches, gouffre des Myriades, Étoile du Berger, trou Lilou and trou Mathieu for its main cavities. To the south, the system Balme à Collomb-grotte des Pincherins of for of elevation gain, now well known for its cave bear deposit has to date not been connected to the Granier system.

Geographic entities mentioned:
surface_form: granier
instance_of: Mountain
countries: France
coordinates: lat: 45.46472222
lon: 5.92527778
When a department of archaeology and anthropology was established at the University of Kentucky in 1926, Webb became its first head. The two-member department wrote several books on Kentucky in prehistoric times. Beginning in 1933, Webb coordinated archaeological excavations in the Tennessee Valley.

Geographic entities mentioned:
surface_form: Tennessee Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.959166666667
lon: -83.850277777778
There is also a Rough Tor on Dartmoor in Devon, three miles west of Postbridge. The early colonial name for Mount Barrow, in Northern Tasmania, was 'Row Tor, - believed to be the homonym of 'Rough Tor': named by Matthew Flinders on his maritime survey. Popular culture. Rough Tor features in Daphne du Maurier's novel &quot;Jamaica Inn&quot;.

Geographic entities mentioned:
surface_form: Mount Barrow
instance_of: Mountain
countries: Australia
coordinates: lat: -41.377222222222
lon: 147.4175
Geography. Kattertooq is located north of the King Dan Peninsula &quot;(Kong Dan Halvø)&quot;. It is oriented in a NW/SE direction and has a tributary fjord branching eastwards 25 km from its mouth. To the east it opens into the North Atlantic Ocean with Uiivaq island on the northern and the entrance of Sehested Fjord (Uummannap Kangertiva) and Griffenfeld Island on the southern side of its mouth.

Geographic entities mentioned:
surface_form: Sehested Fjord
instance_of: Body of water
countries: Greenland
coordinates: lat: 63.05
lon: -42
The garden contains most of the typical vascular plants that grow in the mountain regions in Southern Norway. In addition, the garden contains a few uncommon plants, emphasizing the particular characteristics of the rich flora of Dovrefjell. The mountain garden was established in 1992 by Simen Bretten, who was then the leader of the Kongsvoll biological station.

Geographic entities mentioned:
surface_form: Dovrefjell
instance_of: Mountain
countries: Norway
coordinates: lat: 62.1
lon: 9.41666667
It was described by Hall and Clarke in 1888, and the type species is &quot;Coronura aspectans&quot;, which was originally described under the genus &quot;Asaphus&quot; by Conrad in 1841. The species was described from the Onondaga Formation. Fossils of &quot;Coronura&quot; have also been found in Indiana, and in the Emsian to Givetian Floresta Formation, Altiplano Cundiboyacense, Colombia.

Geographic entities mentioned:
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877
Helm (mountain). The Helm (;) is a mountain in the Puster Valley in South Tyrol, Italy.

Geographic entities mentioned:
surface_form: Puster Valley
instance_of: Valley
countries: Italy
Austria
coordinates: lat: 46.7405
lon: 12.369555555555555
surface_form: helm
instance_of: Mountain
countries: Austria
Italy
coordinates: lat: 46.715
lon: 12.3872
Helm (mountain). The Helm (;) is a mountain in the Puster Valley in South Tyrol, Italy.

Geographic entities mentioned:
surface_form: helm
instance_of: Mountain
countries: Austria
Italy
coordinates: lat: 46.715
lon: 12.3872
Enoshima Island has many attractions, including a botanical gardens and the Enoshima Sea Candle which is open to visitors. Its height of 119.6 meters above sea level affords an excellent view of the area and, on a clear day, Mount Fuji. There are a number of famous Shinto shrines, some in caves on the south side of the island.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
Between 6 March and 6 April 1961, he succeeded in photographing two bright patches near the Lagrange point. During the observation time, the patches hardly appeared to move relative to. The observations were taken from the mountain Kasprowy Wierch. In 1967, J. Wesley Simpson made observations of the clouds using the Kuiper Airborne Observatory.

Geographic entities mentioned:
surface_form: Kasprowy Wierch
instance_of: Mountain
countries: Slovakia
Poland
coordinates: lat: 49.231666666667
lon: 19.981666666667
Ponto Lake. Ponto Lake is a lake located north and east of Backus, Minnesota. A public access is located on the southeast shore just north of State Highway 84. The Minnesota Department of Natural Resources (MNDNR) has classified Minnesota's lakes into 43 different classes based on physical, chemical and other characteristics.

Geographic entities mentioned:
surface_form: ponto lake
instance_of: Lake
countries: United States
coordinates: lat: 46.873888888889
lon: -94.341111111111
The Minnesota Department of Natural Resources (MNDNR) has classified Minnesota's lakes into 43 different classes based on physical, chemical and other characteristics. Ponto Lake is in Lake Class 23; lakes in this class generally have hard water, are very deep and clear, and have a low amount of lake area less than 15 feet deep.

Geographic entities mentioned:
surface_form: ponto lake
instance_of: Lake
countries: United States
coordinates: lat: 46.873888888889
lon: -94.341111111111
This lake is managed primarily for walleye and northern pike and secondarily for bluegill, black crappie, largemouth bass, and yellow perch. Ponto Lake has an abundant population of naturally reproducing walleye. The average length of these walleye was, and the largest sampled was. Northern pike were also abundant, averaged about long, and had a maximum length of.

Geographic entities mentioned:
surface_form: ponto lake
instance_of: Lake
countries: United States
coordinates: lat: 46.873888888889
lon: -94.341111111111
The average length of these walleye was, and the largest sampled was. Northern pike were also abundant, averaged about long, and had a maximum length of. Ponto Lake has a good population of largemouth bass, and fish up to were sampled. Bluegill, black crappie and yellow perch are available for anglers, however numbers sampled in the 2002 assessment were low.

Geographic entities mentioned:
surface_form: ponto lake
instance_of: Lake
countries: United States
coordinates: lat: 46.873888888889
lon: -94.341111111111
Alid Volcano. The Alid Volcano is a stratovolcano located in the Northern Red Sea region of Eritrea in the Danakil Depression. The peak elevation from its base is. The volcano's most recent activity was identified in 1928, when it emitted smoke. It is a large volcano located in the northern east coast.

Geographic entities mentioned:
surface_form: alid
instance_of: Mountain
countries: Eritrea
coordinates: lat: 14.89
lon: 39.925833333333
Naramata. Naramata is an unincorporated community in the Okanagan region of south central British Columbia, Canada. On the eastern shore of southern Okanagan Lake, the locality is by road about north of Penticton. Name origin. In November 1906, John Moore Robinson purchased land.

Geographic entities mentioned:
surface_form: Okanagan Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.920833333333
lon: -119.5
Based on Edward Bulwer-Lytton's 1834 novel of the same name, the film – one of two different adaptations of the same book in Italy that year – is set during the final days leading up to the Mount Vesuvius eruption in Pompeii in 79 AD. Plot. In Pompeii 79AD, Glaucus and Jone are in love with each other. Arbaces, the Egyptian High Priest, is determined to conquer her.

Geographic entities mentioned:
surface_form: Mount Vesuvius
instance_of: Mountain
countries: Italy
coordinates: lat: 40.821388888889
lon: 14.425555555556
He established a property which he named &quot;Gleeville&quot; near the current Dashwood Road – Sunnyside Road junction, and also took up pastoral runs north of Adelaide, near the Wakefield River. In 1840, he established the &quot;Inchiquin&quot; run in the Clare Valley area, and in 1842 laid out a plan for a town.

Geographic entities mentioned:
surface_form: Clare Valley
instance_of: Valley
countries: Australia
coordinates: lat: -33.83361111
lon: 138.61
Mount Williams (New Zealand). Mount Williams is a mountain in the Canterbury Region of New Zealand. Description. Mount Williams is located northwest of Christchurch and east-southeast of Arthur's Pass in Arthur's Pass National Park. It is set in the Southern Alps of the South Island.

Geographic entities mentioned:
surface_form: mount williams
instance_of: Mountain
countries: New Zealand
coordinates: lat: -42.961
lon: 171.627
Mount Williams is a mountain in the Canterbury Region of New Zealand. Description. Mount Williams is located northwest of Christchurch and east-southeast of Arthur's Pass in Arthur's Pass National Park. It is set in the Southern Alps of the South Island. Precipitation runoff from the mountain's west slope drains into the Mingha River, whereas the east slope drains into the Edwards River.

Geographic entities mentioned:
surface_form: mount williams
instance_of: Mountain
countries: New Zealand
coordinates: lat: -42.961
lon: 171.627
It is set in the Southern Alps of the South Island. Precipitation runoff from the mountain's west slope drains into the Mingha River, whereas the east slope drains into the Edwards River. Like many peaks of the Southern Alps, Mount Williams is more notable for its large, steep rise above local terrain than for its absolute elevation.

Geographic entities mentioned:
surface_form: mount williams
instance_of: Mountain
countries: New Zealand
coordinates: lat: -42.961
lon: 171.627
The nearest higher peak is Dome, 3.5 kilometres to the southeast. Climate. Based on the Köppen climate classification, Mount Williams is located in a marine west coast (Cfb) climate zone. Prevailing westerly winds blow moist air from the Tasman Sea onto the mountains, where the air is forced upwards by the mountains (orographic lift), causing moisture to drop in the form of rain or snow.

Geographic entities mentioned:
surface_form: mount williams
instance_of: Mountain
countries: New Zealand
coordinates: lat: -42.961
lon: 171.627
The months of December through February offer the most favourable weather for viewing or climbing this peak. The Spike. The Spike is a subsummit on the southwest ridge of Mount Williams, with less than one kilometre between summits. The elevation of The Spike is 1,440 metres and there are climbing routes via Gunbarrel Scree and the Southwest Ridge.

Geographic entities mentioned:
surface_form: mount williams
instance_of: Mountain
countries: New Zealand
coordinates: lat: -42.961
lon: 171.627
They are endemic to all river systems of the Mobile River basin in Mississippi, Alabama, Tennessee, and Georgia. They are particularly widespread in the upper Cahaba and Coosa River systems. Populations of the Mobile logperch and gulf logperch (&quot;Percina suttkusi&quot;) occur together at certain locations in the Alabama, Black Warrior, and upper and lower Tombigbee River systems.

Geographic entities mentioned:
surface_form: Coosa River
instance_of: Watercourse
countries: United States
coordinates: lat: 32.4862464
lon: -86.2777475
Minnow Lake (Minnesota). Minnow Lake is a lake in Clearwater County, Minnesota, in the United States. Minnow Lake was named from its population of small minnows.

Geographic entities mentioned:
surface_form: minnow lake (minnesota)
instance_of: Lake
countries: United States
coordinates: lat: 47.531666666667
lon: -95.475
Minnow Lake (Minnesota). Minnow Lake is a lake in Clearwater County, Minnesota, in the United States. Minnow Lake was named from its population of small minnows.

Geographic entities mentioned:
surface_form: minnow lake
instance_of: Lake
countries: United States
coordinates: lat: 47.531666666667
lon: -95.475
It is the part of Kanalichhina development Block and Didihat Tehsil. The place is also famous for the Askot Musk Deer Sanctuary dedicated to the conservation of Musk deer. Askot lies midway between Pithoragarh to Dharchula road and located on a ridge. 'Kailash-Mansarovar Pilgrimage route from Delhi - Kathgodam - Didihat - Dharchula, passes through Askot.

Geographic entities mentioned:
surface_form: Kailash
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 31.066944444444
lon: 81.312777777778
surface_form: Mansarovar
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 30.666666666667
lon: 81.5
Giffnock. Giffnock (;;,) is a town and the administrative centre of East Renfrewshire in the Central Lowlands of Scotland. It lies east of Barrhead, east-southeast of Paisley and northwest of East Kilbride, at the southwest of the Greater Glasgow conurbation. Giffnock has frequently been named amongst the least deprived areas in Scotland.

Geographic entities mentioned:
surface_form: Central Lowlands
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.408
lon: -4.044
Before its creation in 2005, Giffnock was in the Eastwood Constituency. Geography. At (55.803°, −4.30°) Giffnock is situated in Scotland's Central Lowlands. The town lies east of Barrhead, northwest of East Kilbride and south-southwest of Glasgow. The territory of Giffnock is contiguous with Glasgow and forms part of Greater Glasgow, the United Kingdom's fifth largest conurbation.

Geographic entities mentioned:
surface_form: Central Lowlands
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.408
lon: -4.044
On 15 June, steamed from Danzig to Kiel, where she joined the reconnaissance forces of the High Seas Fleet, taking the place of the light cruiser. She thereafter was ordered to accompany Kaiser Wilhelm's yacht to a sailing regatta held in the mouth of the Elbe and then for a visit to Bergen and Balestrand, Norway.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
It was one of the largest theropods of the Early Jurassic, with the subadult, being estimated to have reached long and weighed. &quot;Cryolophosaurus&quot; was first excavated from Antarctica's Early Jurassic, Pliensbachian aged Hanson Formation, formerly the upper Falla Formation, by paleontologist Dr. William Hammer in 1991.

Geographic entities mentioned:
surface_form: Hanson Formation
instance_of: Mountain
coordinates: lat: -84.3
lon: 166.5
The brain of &quot;Cryolophosaurus&quot; was also more primitive than those of other theropods. Discovery and naming. &quot;Cryolophosaurus&quot; originally was collected during the 1990–91 austral summer on Mount Kirkpatrick in the Beardmore Glacier region of the Transantarctic Mountains. The discovery was made by Hammer, a professor at Augustana College, and his team.

Geographic entities mentioned:
surface_form: Mount Kirkpatrick
instance_of: Mountain
coordinates: lat: -84.333333333333
lon: 166.41666666667
The discovery was made by Hammer, a professor at Augustana College, and his team. The fossils were found in the siliceous siltstone of the Hanson Formation, formerly the upper Falla Formation, and dated back to the Pliensbachian Stage of the early Jurassic. &quot;Cryolophosaurus&quot; was the second dinosaur, and first theropod to be discovered in Antarctica.

Geographic entities mentioned:
surface_form: Hanson Formation
instance_of: Mountain
coordinates: lat: -84.3
lon: 166.5
Beyond vertebrates, Insects (Blattodea, Coleoptera), Ostracodans, Conchostracans and arthropod ichnofossils (&quot;Diplichnites, Planolites, Scoyenia&quot;) are know from other coeval localities, like Gair Mesa, Mount Carson or Shafer Peak. Plant remains are also very common, including large tree trunks (+50 cm) from Mount Carson to Palynomorphs at Shafer Peak.

Geographic entities mentioned:
surface_form: Gair Mesa
instance_of: Mountain
coordinates: lat: -73.466666666667
lon: 162.86666666667
surface_form: Shafer Peak
instance_of: Mountain
coordinates: lat: -74.01834
lon: 162.59333
Geography. The Métabetchouane Est River takes its source at the mouth of &quot;Lac des Hautes des Terres&quot; (length:; altitude:). Enclosed between mountains, this lake is linked on the north side by a small stream with the &quot;Lac de la Hauteur&quot; which turns out to be the head lake of the rivière aux Écorces du Milieu.

Geographic entities mentioned:
surface_form: rivière aux Écorces du Milieu
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.714722222222
lon: -71.659444444444
surface_form: head lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.0486
lon: -78.5161
surface_form: rivière aux écorces du milieu
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.714722222222
lon: -71.659444444444
surface_form: head lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.74027777777778
lon: -78.91277777777778
Enclosed between mountains, this lake is linked on the north side by a small stream with the &quot;Lac de la Hauteur&quot; which turns out to be the head lake of the rivière aux Écorces du Milieu. The mouth of &quot;Lac des Hauts des Terres&quot; is located: south of the source of the source of rivière aux Écorces du Milieu, at northwest of Lac Chagnon, northeast of Lac Tentant and northeast.

Geographic entities mentioned:
surface_form: rivière aux Écorces du Milieu
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.714722222222
lon: -71.659444444444
surface_form: rivière aux écorces du milieu
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.714722222222
lon: -71.659444444444
Upper course of the Métabetchouane East River (from its source) (segment of)
Intermediate course of the Métabetchouane East river (segment of)
Lower course of the Métabetchouane Est river (segment of)
From the confluence of the Métabetchouane East river, the current descends the Métabetchouane North River on to the south shore of lac Saint-Jean; from there, the current crosses the latter on towards the northeast, then borrows the course of the Saguenay River via La Petite Landfill on until Tadoussac where it merges with the Saint Lawrence estuary.

Geographic entities mentioned:
surface_form: lac Saint-Jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: lac saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: north river
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.50472222
lon: -77.83416667
surface_form: métabetchouane east river
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.601388888889
lon: -71.860555555556
surface_form: métabetchouane east river
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.601388888889
lon: -71.860555555556
surface_form: east river
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.5529
lon: -62.3032
surface_form: east river
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.5529
lon: -62.3032
surface_form: east river
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.5529
lon: -62.3032
Métabetchouane East River. The Métabetchouane East river is a tributary of the northeast shore of the Métabetchouane River, flowing in the Laurentides Wildlife Reserve, in the unorganized territory of Lac-Jacques-Cartier, in the La Côte-de-Beaupré Regional County Municipality, in the administrative region of Capitale-Nationale, in the province from Quebec, to Canada.

Geographic entities mentioned:
surface_form: jacques-cartier
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.671388888889
lon: -71.747222222222
surface_form: métabetchouane east river
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.601388888889
lon: -71.860555555556
surface_form: east river
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.5529
lon: -62.3032
Métabetchouane East River. The Métabetchouane East river is a tributary of the northeast shore of the Métabetchouane River, flowing in the Laurentides Wildlife Reserve, in the unorganized territory of Lac-Jacques-Cartier, in the La Côte-de-Beaupré Regional County Municipality, in the administrative region of Capitale-Nationale, in the province from Quebec, to Canada.

Geographic entities mentioned:
surface_form: métabetchouane east river
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.601388888889
lon: -71.860555555556
surface_form: east river
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.5529
lon: -62.3032
He died on 2 September 1916 during the Battle of Doiran, and was buried in the village of Čaušli, today in North Macedonia. Honours. In 1991, the Louis Eyer Bulgarian-Swiss Association was founded in Rousse. The stadium in Silistra is named after him, as are streets around the country. Eyer Peak in Sentinel Range, Antarctica is named after Louis-Emil Eyer.

Geographic entities mentioned:
surface_form: Eyer Peak
instance_of: Mountain
coordinates: lat: -78.155
lon: -85.9958
However, the project was ultimately abandoned due to costs exceeding the capabilities of local governments and a lack of interest from the city of Karpacz. In 2009, a Czech team of architects developed a concept for a 4 km railway tunnel under Sněžka, intended to connect Pec pod Sněžkou with Karpacz.

Geographic entities mentioned:
surface_form: Sněžka
instance_of: Mountain
countries: Czech Republic
Poland
coordinates: lat: 50.736111111111
lon: 15.740277777778
Bastian and he revealed that he was already offered the role in 2017 but turned down due to scheduling conflicts. Filming. Principal photography began in April 2019 and took place in Semarang, Tegal, Sukabumi, Jakarta as well as the hometown of Hamka in Lake Maninjau, West Sumatra. The film was also shot in Cairo, Egypt, and involved Indonesian students. It concluded on 15 July 2019. Release.

Geographic entities mentioned:
surface_form: Lake Maninjau
instance_of: Lake
countries: Indonesia
coordinates: lat: -0.31666666666667
lon: 100.2
It was described by Philogène Auguste Joseph Duponchel in 1836. It is found in most of Europe (except Portugal, Ireland, Great Britain, Fennoscandia, the Benelux, Poland and the Baltic region), Algeria, the United Arab Emirates, Syria, Lebanon, the Palestinian territories, Iraq, Turkmenistan, Mongolia, as well as Georgia, Kazakhstan, Armenia, Turkey, Iran and Afghanistan. The wingspan is 19–24 mm.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
The first three of these are found where the Nazca Plate subducts beneath the South America Plate, while the last zone occurs at the subduction zone of the Antarctic Plate. The Andean Central Volcanic Zone runs along the Western Cordillera of the Andes and along the Altiplano.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Volcanic activity during this time was heavily influenced by local strike-slip faults which acted to channel the magma flows. About 7 million years ago, tectonics and volcanic activity changed in the region, probably in response to the delamination of the crust beneath the region: large scale ignimbrites erupted at Galán and small back-arc volcanoes erupted mafic basaltic andesite lavas.

Geographic entities mentioned:
surface_form: Galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
The eruptions probably lasted several weeks to several years. A lava flow at La Laguna cone has been dated to 340,000 ± 60,000 years before present, consistent with its older appearance. A large-scale research project in the Puna yielded a number of Ar-Ar and K-Ar dates, including 3.2 and 4.5 million years ago for Jote and 0.3 and 7.3 million years ago for Alumbrera and La Laguna.

Geographic entities mentioned:
surface_form: Puna
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Antofagasta de la Sierra. Antofagasta de la Sierra is a volcanic field in Argentina. The main type of volcanic edifice in the area are scoria cones, formed by the La Laguna, Jote and Alumbrera volcanoes. The first and last of these form a sub-group which is better researched.

Geographic entities mentioned:
surface_form: antofagasta de la sierra
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.968055555556
lon: -67.535833333333
These small volcanic centres consist of lava domes, lava flows, maars, scoria cones and tuff rings. Local. The Antofagasta de la Sierra volcanic field lies within the north–south trending tectonic depression of the same name, in the Catamarca Province. Of the individual vents, the La Laguna and Alumbrera cones are the best studied ones; they lie about south of Antofagasta de la Sierra.

Geographic entities mentioned:
surface_form: antofagasta de la sierra volcanic field
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.968055555556
lon: -67.535833333333
Local. The Antofagasta de la Sierra volcanic field lies within the north–south trending tectonic depression of the same name, in the Catamarca Province. Of the individual vents, the La Laguna and Alumbrera cones are the best studied ones; they lie about south of Antofagasta de la Sierra. These volcanoes are associated with black lava flow fields.

Geographic entities mentioned:
surface_form: antofagasta de la sierra
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.968055555556
lon: -67.535833333333
Of the individual vents, the La Laguna and Alumbrera cones are the best studied ones; they lie about south of Antofagasta de la Sierra. These volcanoes are associated with black lava flow fields. The Jote volcanoes consist of a cluster of cinder cones and lava flows and are located south of the Antofagasta de la Sierra lake. To their northwest lies Cachamani.

Geographic entities mentioned:
surface_form: antofagasta de la sierra
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.968055555556
lon: -67.535833333333
Renewed activity in the field could cause ash to fall over hundreds of square kilometres of adjoining land and generate dangerous pyroclastic density currents close to the vent. Other. Between the Antofagasta and Alumbrera volcanoes lies the Antofagasta lake. The vegetation in the area is shrub steppe, and fairly sunny and dry.

Geographic entities mentioned:
surface_form: antofagasta
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.968055555556
lon: -67.535833333333
surface_form: antofagasta
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.968055555556
lon: -67.535833333333
Other. Between the Antofagasta and Alumbrera volcanoes lies the Antofagasta lake. The vegetation in the area is shrub steppe, and fairly sunny and dry. The Antofagasta River coming from the north forms a large wetland before the relatively deep Antofagasta lake; the Alumbrera volcano borders the lake in the south. The lake in 1911 consisted of two halves, joined by a canal.

Geographic entities mentioned:
surface_form: antofagasta
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.968055555556
lon: -67.535833333333