Sarmila/GeoWiki-Features huggingface dataset:
&quot;A. stappersii&quot; is found in Burundi, the Democratic Republic of the Congo, Tanzania, and Zambia. It inhabits the drainage basin of Lake Tanganyika, except for the Malagarasi River region. Its natural habitats are slow-flowing rivers, swamps, small freshwater lakes and marshes, and inland deltas. It eats mainly aquatic insect larvae.

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
Overall, however, it is common and widespread, and not considered a threatened species by the IUCN. The specific name honours the Belgian physiologist and biologist Louis Stappers (1883-1916) who led an expedition to Lake Tanganyika on which he collected the type.

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
Middle Ages. Between 774 and 787 the Venafro plain was crossed by the troops of Charlemagne, which clashed with the Lombards of the Principality of Benevento. According to Monte Cassino chronicler Erchempertus, in 861, Venafro was occupied by Emir Sawdan of the Emirate of Bari.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
In 1970, it was incorporated into the newly formed province of Isernia, despite controversy and often violent protests that favored to remain part of the province of Caserta. In the spring of 1984, the city was severely damaged by the earthquake originating in the nearby Valle di Comino, in the province of Frosinone.

Geographic entities mentioned:
surface_form: Valle di Comino
instance_of: Valley
countries: Italy
coordinates: lat: 41.63
lon: 13.8
It is about southeast of Rome, close to the Rome-Naples A1 Motorway. The city is the main city of the Valle Latina (&quot;Latin Valley&quot;), an Italian geographical and historical region that extends from south of Rome to Cassino. Until the 19th century, it was a village with a rural vocation, while from the 20th century, it became an important industrial and commercial centre.

Geographic entities mentioned:
surface_form: Valle Latina
instance_of: Valley
countries: Italy
coordinates: lat: 41.5744
lon: 13.3511
It was subjugated by the Romans in 386 BC during their advance against the Volsci in Valle del Sacco, then transformed into a &quot;municipium&quot; under the Roman garrison.

Geographic entities mentioned:
surface_form: Valle del Sacco
instance_of: Valley
countries: Italy
coordinates: lat: 41.5744
lon: 13.3511
It was within this general framework that the industrialization process began. In 1962, the Industrialization Unit of the Sacco Valley was established and the Rome-Naples motorway section was constructed. The motorway artery, which crosses the entire valley longitudinally, was hugely important in ending the isolation of the capital and of the entire province.

Geographic entities mentioned:
surface_form: Sacco Valley
instance_of: Valley
countries: Italy
coordinates: lat: 41.5744
lon: 13.3511
Geography. Frosinone is in Latium and is the main city of the Valle Latina (&quot;Latin Valley&quot;). The town is surrounded by the Ernici and Lepini mountain ranges. Cathedral of Santa Maria Assunta. The Cathedral of Santa Maria Assunta is the most important church in Frosinone and is located on the highest point of the hill on which the historic center of the city stands (Upper Frosinone).

Geographic entities mentioned:
surface_form: Valle Latina
instance_of: Valley
countries: Italy
coordinates: lat: 41.5744
lon: 13.3511
Contributor to the Soviet Union's rocket and satellite programs (1946–1952). In 1946, he was one of the more than two thousand German specialists forcibly brought to the Soviet Union under Operation Osoaviakhim. He was then one of the more than 170 German specialists – headed by Helmut Gröttrup – brought to Branch 1 of NII-88 on Gorodomlya Island in Lake Seliger.

Geographic entities mentioned:
surface_form: Lake Seliger
instance_of: Lake
Group of lakes
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 57.189
lon: 33.083333333333
Economy. The local economy is based on agriculture and farming; the residents keep sheep and llama and grow vegetables. Tourism plays an important part in the local economy as many tourists come to see the nearby mountains, volcanoes and calderas, including Galán caldera and the Antofagasta de la Sierra volcanic field. The village holds an annual Festival of the dead.

Geographic entities mentioned:
surface_form: Galán caldera
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
surface_form: Antofagasta de la Sierra volcanic field
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.968055555556
lon: -67.535833333333
In Sydney, in 1850, she married Alfred Ludlam (1810–1877). Irish-born Ludlam was a leading New Zealand politician, horticulturist and farmer who owned land at Wellington and in the Hutt Valley. Ludlam was a member of three of New Zealand's four earliest parliaments, he was also a philanthropist and a founder of Wellington's Botanic Garden. Ludlam was a periodic visitor to NSW.

Geographic entities mentioned:
surface_form: Hutt Valley
instance_of: Valley
countries: New Zealand
coordinates: lat: -41.1657
lon: 174.973
Diplacus pictus. &quot;Diplacus pictus&quot; is a species of monkeyflower known by the common name calico monkeyflower. Distribution. The wildflower is endemic to California, found only above the southeastern San Joaquin Valley within Kern County and Tulare County. It is known only from the western Tehachapi Mountains and southernmost Sierra Nevada foothills, at elevations of.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Petites Chutes de la Lukaya. The Petites Chutes de la Lukaya (French; &quot;Small falls of the Lukaya&quot;) is a set of small waterfalls on the Lukaya River. They are just south of Kinshasa, the capital city of the Democratic Republic of the Congo. They are about high.

Geographic entities mentioned:
surface_form: Lukaya River
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: -4.49472
lon: 15.2822
They are about high. During the colonial era, Jesuits who settled on the Ndjili River in June 1893 at Kimbangu, in what is now Masina, were the first Catholic missionaries in the area. Within a month of their arrival, they moved away from the unhealthy, swampy conditions that they found there to relocate to Kimwenza, near the Petites Chutes de la Lukaya.

Geographic entities mentioned:
surface_form: Ndjili River
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: -4.335499
lon: 15.376182
Berens River, Manitoba. Berens River is a community in Manitoba, Canada, along the eastern shore of Lake Winnipeg, at the mouth of the Berens River, which flows west from the Ontario headwaters. Together with the adjacent Berens River 13 reserve, it forms one a population centre collectively called Berens River. Both are served by the Berens River Airport.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Jangchungdan Park. Jangchungdan Park () is a park located in Jung District, Seoul, South Korea. It is to the northeast of the mountain Namsan. It contains the historic, which was built by Emperor Gojong in 1900 to memorialize Empress Myeongseong. The park has a children's baseball field, a tennis court, and a swimming pool. It is popular for walks and for exercise.

Geographic entities mentioned:
surface_form: Namsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 37.54968111
lon: 126.99191083
As an apprentice clerk he played a significant role in the negotiation of the Douglas Treaties in the Colony of Vancouver Island. During the Crimean War McKay was sent to Fort Simpson (Port Simpson, B.C.) to ensure that the HBC and the Russian American Company remained neutral. In the early 1850s Douglas sent McKay to scout the Cowichan and Comox Valleys.

Geographic entities mentioned:
surface_form: Comox Valleys
instance_of: Valley
countries: Canada
coordinates: lat: 49.6798337
lon: -124.9694395
Gulf Coast through the first years of the American Civil War. She was with Union ships,, and in the Mississippi River near Head of Passes when the Confederate ironclad ram &quot;Manassas&quot; – accompanied by steamers and – attacked on 12 October. During the action she ran aground, but the Southern ships did not press their advantage.

Geographic entities mentioned:
surface_form: Head of Passes
instance_of: Landform
countries: United States
coordinates: lat: 29.157
lon: -89.254
When an ice sheet pushed its way between the Pennines and the North York Moors, it bulldozed the soft earth away and carved the cliffs at Whitestone and in turn the mud left over stopped the water's egress and formed the glacial lake. Gormire Lake was a result of this process and is fourth largest of the natural lakes in Yorkshire (the other three being Hornsea Mere, Malham Tarn and Semerwater).

Geographic entities mentioned:
surface_form: Hornsea Mere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 53.905555555556
lon: -0.18611111111111
surface_form: Semerwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.280555555556
lon: -2.125
surface_form: gormire lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.24202778
lon: -1.22983333
Gormire Lake. Gormire Lake is a natural lowland lake that lies at the foot of Whitestone Cliff, a western escarpment of the Hambleton Hills in the North York Moors National Park. The lake is east of the village of Sutton-under-Whitestonecliffe in North Yorkshire, England. Gormire has no inflow or major outflow of water.

Geographic entities mentioned:
surface_form: gormire lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.24202778
lon: -1.22983333
The knight and the abbot rode on from an inn and as they did so, it turned into a race. The abbot then changed into the devil, which caused such panic in the knight that he couldn't stop the horse and himself plunging into Gormire Lake from the clifftop.

Geographic entities mentioned:
surface_form: gormire lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.24202778
lon: -1.22983333
Gormire Lake is popular with wild swimmers as it has no streams feeding it so there is very little current and the waters are described as being 'warm'. Swimmers have reported that it is &quot;seething with leeches.&quot; &quot;The Times&quot; named the lake as one of the 20 best lakes and rivers in Britain for wild swimming.

Geographic entities mentioned:
surface_form: gormire lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.24202778
lon: -1.22983333
Other myths are that the lake is bottomless, that the bottom of the lake is the entrance to hell, there is submerged village underneath the water and that a goose once disappeared in the lake to emerge in a well at Kirkbymoorside stripped of all its feathers.

Geographic entities mentioned:
surface_form: hell
instance_of: Landform
countries: United Kingdom
coordinates: lat: 19.37935
lon: -81.40678
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Gormire Lake. Gormire Lake is a natural lowland lake that lies at the foot of Whitestone Cliff, a western escarpment of the Hambleton Hills in the North York Moors National Park. The lake is east of the village of Sutton-under-Whitestonecliffe in North Yorkshire, England. Gormire has no inflow or major outflow of water.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
The lake is east of the village of Sutton-under-Whitestonecliffe in North Yorkshire, England. Gormire has no inflow or major outflow of water. It is thought to be fed by an underground spring and drained by a limestone channel so the water finds a way out through the base of the cliff face to the east of the lake. The lake is also known as the White Mere, Lake Gormire, or more simply, Gormire.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Gormire has no inflow or major outflow of water. It is thought to be fed by an underground spring and drained by a limestone channel so the water finds a way out through the base of the cliff face to the east of the lake. The lake is also known as the White Mere, Lake Gormire, or more simply, Gormire. The name Gormire translates as filthy swamp.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
The name Gormire translates as filthy swamp. The lake was formed over 20,000 years ago by glacial erosion. When an ice sheet pushed its way between the Pennines and the North York Moors, it bulldozed the soft earth away and carved the cliffs at Whitestone and in turn the mud left over stopped the water's egress and formed the glacial lake.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Gormire Lake was a result of this process and is fourth largest of the natural lakes in Yorkshire (the other three being Hornsea Mere, Malham Tarn and Semerwater). The lake was first designated as an Site of Special Scientific Interest (SSSI) in 1954; however, in 1985 the area surrounding the lake was incorporated into the SSSI status with the new area being.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
The new designation incorporates the broadleaf woodlands of Garbutt Wood which encroach right up to the water's edge. The lake is the setting of several myths; one being of a knight known as Sir Harry Scriven who conned the Abbot of Rievaulx Abbey into letting him ride his horse (a white mare, the so called derivation of White Mare Cliff (another name for Whitestonecliff)).

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
The abbot then changed into the devil, which caused such panic in the knight that he couldn't stop the horse and himself plunging into Gormire Lake from the clifftop. The 'devil' was then seen to jump into the lake after them and the boiling effect of the devil in the water is what is said to have caused the darkness of the lake to this day.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Gormire Lake is popular with wild swimmers as it has no streams feeding it so there is very little current and the waters are described as being 'warm'. Swimmers have reported that it is &quot;seething with leeches.&quot; &quot;The Times&quot; named the lake as one of the 20 best lakes and rivers in Britain for wild swimming.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
At Thakur Kuan village (3560m), the Parvati Valley meets the valley of Dibibokri Nal river which is a tributary of Parvati River, which climbs towards the Northeast to the Dibibokri Glacier and Dibibokri Pyramid mountain peak (6400m). The area is characterised by abundant alpine flowers and rocky outcrops glittering with mica.

Geographic entities mentioned:
surface_form: pyramid
instance_of: Mountain
countries: India
coordinates: lat: 27.82073
lon: 88.172922
surface_form: parvati valley
instance_of: Valley
countries: India
coordinates: lat: 31.992352777778
lon: 77.481766666667
Parvati Valley. Parvati Valley is a Himalayan valley situated in the northern Indian state of Himachal Pradesh. From the confluence of the Parvati River with the River Beas, the valley runs eastwards, through a steep-sided valley from the town of Bhuntar, in the Kullu district of Himachal Pradesh in Northern India. Overview.

Geographic entities mentioned:
surface_form: parvati valley
instance_of: Valley
countries: India
coordinates: lat: 31.992352777778
lon: 77.481766666667
From Kheerganga to the site of Tunda Bhuj village (3285m) the Parvati Valley cuts a steep-sided gorge through the mountains and as the altitude increases, the thick, coniferous forest gradually makes way for patches of meadowland scattered with boulders. Several tributaries join the main Parvati River and numerous waterfalls cascade down the steep valley sides.

Geographic entities mentioned:
surface_form: parvati valley
instance_of: Valley
countries: India
coordinates: lat: 31.992352777778
lon: 77.481766666667
The area is characterised by abundant alpine flowers and rocky outcrops glittering with mica. Beyond Thakur Kuan village, the Parvati Valley ascends gradually to Pandupul village (Pandu Pul) where two natural, rock bridges cross the Parvati River and a southern tributary. According to legend, these bridges were created by the massive strength of the Pandava brothers.

Geographic entities mentioned:
surface_form: parvati valley
instance_of: Valley
countries: India
coordinates: lat: 31.992352777778
lon: 77.481766666667
According to legend, these bridges were created by the massive strength of the Pandava brothers. From Pandupul, the wide valley of the upper Parvati valley climbs gradually through the wide, high-altitude meadowland of Odi Thatch to the sacred site of Mantalai Lake (4100m), the source of the Parvati River.

Geographic entities mentioned:
surface_form: parvati valley
instance_of: Valley
countries: India
coordinates: lat: 31.992352777778
lon: 77.481766666667
Continuing east from Mantalai lake, it is possible to cross the Pin Parvati Pass (5319m) into the Pin Valley National Park and on to the Mudh village in the Lahul and Spiti district of Himachal Pradesh. Parvati Valley's scenic trekking routes are a popular destination for trekkers and tourists. Disappearances.

Geographic entities mentioned:
surface_form: parvati valley
instance_of: Valley
countries: India
coordinates: lat: 31.992352777778
lon: 77.481766666667
Disappearances. According to journalist Harley Rustad’s 2022 non-fiction book &quot;Lost in the Valley of Death: Obsession and Danger in the Himalayas&quot;, dozens of tourists have mysteriously disappeared in the Parvati Valley. As Rustad writes &quot;...the Parvati Valley has earned its own nicknames: the Valley of shadows, the Valley of Death.

Geographic entities mentioned:
surface_form: parvati valley
instance_of: Valley
countries: India
coordinates: lat: 31.992352777778
lon: 77.481766666667
Since the early 1990s, dozens of international backpackers have vanished without a trace while traveling in and around the Parvati Valley, an average of one every year, earning this tiny, remote sliver of the subcontinent a dark reputation as India's backpacker Bermuda Triangle.

Geographic entities mentioned:
surface_form: parvati valley
instance_of: Valley
countries: India
coordinates: lat: 31.992352777778
lon: 77.481766666667
The period of kalbaisakhi formation generally begins in April and lasts until the monsoon establishes itself over Northeast India, although March kalbaisakhi are not unknown. Based on event descriptions and the meteorological environments involved, these storms can be classified as progressive derechos. Kalbaisakhi originate over the Chhotanagpur Plateau between the states of Bihar and Jharkhand.

Geographic entities mentioned:
surface_form: Chhotanagpur Plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
Borders: to the northwest - municipality of Mali Zvornik, to the north - municipality of Krupanj, to the northeastern - municipality of Osečina, to the east - municipality of Valjevo, and to the south - municipality of Bajina Bašta. The highest peak is Tornička Bobija 1272 meters high on the mountain Bobija. Several torrential rivers, flowing into the Drina, intersect Azbukovica.

Geographic entities mentioned:
surface_form: Bobija
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.1961
lon: 19.5544
Geography. Henan has a diverse landscape with floodplains in the east and mountains in the west. Much of the province forms part the densely populated North China Plain, an area known as the &quot;breadbasket of China&quot;. The Taihang Mountains intrude partially into Henan's northwestern borders from Shanxi, forming the eastern edge of Loess Plateau.

Geographic entities mentioned:
surface_form: Loess Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
To the west the Xionger and Funiu Mountains form an extensive network of mountain ranges and plateaus, supporting one of the few remaining temperate deciduous forests which once covered all of Henan. The renowned Mount Song and its Shaolin Temple is located in the far east of the region, near the capital city Zhengzhou. To the far south, the Dabie Mountains divides Hubei from Henan.

Geographic entities mentioned:
surface_form: Mount Song
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 34.484722222222
lon: 112.96027777778
From San Feliciano a ferry leaves for the Isola Polvese. It is a fishing village and centre for tourism in the Commune of Magione. Among its attractions is the Museo della Pesca, a joint venture between local authorities and fishermen’s cooperatives. The village lies 4 km south west of Magione and 18 km west of Perugia at the Lake Trasimeno. San Feliciano has around 580 inhabitants,

Geographic entities mentioned:
surface_form: Lake Trasimeno
instance_of: Lake
countries: Italy
coordinates: lat: 43.14
lon: 12.1
The concept of “socialized economics” - (socialized economics - new economic concept), world economy, industrial policy and infrastructure problems, national regional strategy of development (autonomous activity, Free Economic Zones, industrial parks, regional clusters, business incubators), energy security and national energy strategy, challenges of modernization of the fuel and energy complex, model of oligopoly in development of the Azerbaijan oil industry, alternativeness in transformation of hydrocarbonic resources into nuclear potential, high technologies, information economy, nanotechnologies, the problem of urban public transport, new environmental requirements of motorization, the improvement of the regional transport infrastructure: corridors East-West and North-South, TRACECA, railway line Baku-Tbilisi-Kars, the Caspian-Persian corridor - geo-economics foreshortening (economic purposes and efficiency of constructing of the water canal from the Caspian sea to the Persian gulf), condominium safety and new financial architecture in power engineering in the Near East, Evaluation of economic potential in the South Caucasus and Caspian Basin regions.

Geographic entities mentioned:
surface_form: Caspian sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Manda II. Manda II is a mountain of the Garhwal Himalaya in Uttarakhand India also called Manda south. The elevation of Manda II is and its prominence is. It is joint 71st highest located entirely within the Uttrakhand. Nanda Devi, is the highest mountain in this category. It lies south of Manda I and north of Manda III. It lies NE of Jogin II. Its nearest higher neighbor is Bhrigupanth.

Geographic entities mentioned:
surface_form: Nanda Devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
The elevation of Manda II is and its prominence is. It is joint 71st highest located entirely within the Uttrakhand. Nanda Devi, is the highest mountain in this category. It lies south of Manda I and north of Manda III. It lies NE of Jogin II. Its nearest higher neighbor is Bhrigupanth. It is located NW of Shivling (mountain) and west lies Gangotri I. Gangotri National Park.

Geographic entities mentioned:
surface_form: Manda I
instance_of: Mountain
countries: India
coordinates: lat: 30.940277777777776
lon: 78.99861111111112
surface_form: Manda III
instance_of: Mountain
countries: India
coordinates: lat: 30.905
lon: 79.00027777777778
Nanda Devi, is the highest mountain in this category. It lies south of Manda I and north of Manda III. It lies NE of Jogin II. Its nearest higher neighbor is Bhrigupanth. It is located NW of Shivling (mountain) and west lies Gangotri I. Gangotri National Park. The entire surrounding area are protected within the Gangotri National Park, one of the largest conservation area in India.

Geographic entities mentioned:
surface_form: Bhrigupanth
instance_of: Mountain
countries: India
coordinates: lat: 30.880401
lon: 79.002682
The elevation of Manda II is and its prominence is. It is joint 71st highest located entirely within the Uttrakhand. Nanda Devi, is the highest mountain in this category. It lies south of Manda I and north of Manda III. It lies NE of Jogin II. Its nearest higher neighbor is Bhrigupanth. It is located NW of Shivling (mountain) and west lies Gangotri I. Gangotri National Park.

Geographic entities mentioned:
surface_form: jogin ii
instance_of: Mountain
countries: India
coordinates: lat: 30.895833333333332
lon: 78.93277777777777
Fixing a total of 760 meters rope below the summit ridge. This is only the second summit of this peak and first Indian summit. Glaciers and rivers. On the western side lies Kedar Bamak and on the eastern side lies Bhrigupanth Bamak. Kedar Ganga emerges from Kedar bamak and joins Bhagirathi River near Gangotri. Bhrigupanth Bamak drain down to Bhagirathi River near Bhojwas.

Geographic entities mentioned:
surface_form: bhrigupanth
instance_of: Mountain
countries: India
coordinates: lat: 30.880401
lon: 79.002682
Nanda Devi, is the highest mountain in this category. It lies south of Manda I and north of Manda III. It lies NE of Jogin II. Its nearest higher neighbor is Bhrigupanth. It is located NW of Shivling (mountain) and west lies Gangotri I. Gangotri National Park. The entire surrounding area are protected within the Gangotri National Park, one of the largest conservation area in India.

Geographic entities mentioned:
surface_form: shivling
instance_of: Mountain
countries: India
coordinates: lat: 30.876944444444
lon: 79.065555555556
Manda II. Manda II is a mountain of the Garhwal Himalaya in Uttarakhand India also called Manda south. The elevation of Manda II is and its prominence is. It is joint 71st highest located entirely within the Uttrakhand. Nanda Devi, is the highest mountain in this category. It lies south of Manda I and north of Manda III. It lies NE of Jogin II. Its nearest higher neighbor is Bhrigupanth.

Geographic entities mentioned:
surface_form: manda ii
instance_of: Mountain
countries: India
coordinates: lat: 30.926111111111112
lon: 78.99861111111112
Climbing history. In 1982 an American expedition, led by Mark Udall had the privilege of first ascent of Manda II through the South Ridge. A group of climbers from Junipers, a climbing club of Calcutta decided to attempt Manda II from the east. The team led by Avijit Das, comprised Arnab Banerjee, Arka Ghosh, Kaushik Pal, RK Gambhisana, Thapa (HAP), Dil (HAP), and Dharmi (cook).

Geographic entities mentioned:
surface_form: manda ii
instance_of: Mountain
countries: India
coordinates: lat: 30.926111111111112
lon: 78.99861111111112
In 1993 this forest became one of the first areas in Japan listed as a UNESCO World Heritage Site. Dewa mountains in culture. The range is the focal point for the &quot;Akinomine&quot; (秋の嶺 &quot;peak of autumn&quot;) ritual, which is observed by the Mount Haguro lineage of Shugendō.

Geographic entities mentioned:
surface_form: Mount Haguro
instance_of: Mountain
countries: Japan
coordinates: lat: 38.7008
lon: 139.9825
Anamorava (), or Kosovo Pomoravlje (/ &quot;Kosovsko Pomoravlje&quot;, &quot;Morava Valley of Kosovo&quot;), is a valley in Kosovo, in the southern part of the District of Gjilan surrounding the Morava e Binçës River. It stretches eastward to the Preševo Valley in southern Serbia. The mountains in this region, rising to an altitude of, border the Skopska Crna Gora region in north of Skopje.

Geographic entities mentioned:
surface_form: Preševo Valley
instance_of: Valley
countries: Serbia
coordinates: lat: 42.3
lon: 21.633333333333
It stretches eastward to the Preševo Valley in southern Serbia. The mountains in this region, rising to an altitude of, border the Skopska Crna Gora region in north of Skopje. Gjilan, Kamenica, Novo Brdo and Viti are municipalities located in the region. Name.

Geographic entities mentioned:
surface_form: Skopska Crna Gora
instance_of: Mountain
countries: Serbia
Kosovo
North Macedonia
coordinates: lat: 42.166666666667
lon: 21.416666666667
Geography. Anamorava is about long and wide. It is bordered by the Skopska Crna Gora mountains in the south, Gollak in the north, and Kosovo field in the west. On the east, it borders the Morava Valley. The region's largest city is Gjilan. The region can be divided into Lower Anamorava and Upper Anamorava, which is also part of the Skopska Crna Gora region.

Geographic entities mentioned:
surface_form: Skopska Crna Gora
instance_of: Mountain
countries: Serbia
Kosovo
North Macedonia
coordinates: lat: 42.166666666667
lon: 21.416666666667
surface_form: Gollak
instance_of: Mountain
countries: Serbia
Kosovo
coordinates: lat: 42.691666666667
lon: 21.689166666667
On the east, it borders the Morava Valley. The region's largest city is Gjilan. The region can be divided into Lower Anamorava and Upper Anamorava, which is also part of the Skopska Crna Gora region. The region includes part of the valley and the Skopska Crna Gora region and Koznik mountains. Gjilan has six municipalities and 287 smaller settlements.

Geographic entities mentioned:
surface_form: Skopska Crna Gora region
instance_of: Mountain
countries: Serbia
Kosovo
North Macedonia
coordinates: lat: 42.166666666667
lon: 21.416666666667
surface_form: anamorava
instance_of: Valley
countries: Kosovo
coordinates: lat: 42.46666667
lon: 21.46666667
The region's largest city is Gjilan. The region can be divided into Lower Anamorava and Upper Anamorava, which is also part of the Skopska Crna Gora region. The region includes part of the valley and the Skopska Crna Gora region and Koznik mountains. Gjilan has six municipalities and 287 smaller settlements. The spa in Klokot has several thermal springs valued for their medicinal qualities.

Geographic entities mentioned:
surface_form: Skopska Crna Gora
instance_of: Mountain
countries: Serbia
Kosovo
North Macedonia
coordinates: lat: 42.166666666667
lon: 21.416666666667
The region's average annual temperature is. January's average is, and July's is. Hydrography. Tributaries of the Morava river system include the Karadak and Llapushnica rivers. The Preševo Valley is a corridor between the Morava and Vardar valleys, and the Morava valley's wetlands are home to many species of birds.

Geographic entities mentioned:
surface_form: Preševo Valley
instance_of: Valley
countries: Serbia
coordinates: lat: 42.3
lon: 21.633333333333
Anamorava. Anamorava (), or Kosovo Pomoravlje (/ &quot;Kosovsko Pomoravlje&quot;, &quot;Morava Valley of Kosovo&quot;), is a valley in Kosovo, in the southern part of the District of Gjilan surrounding the Morava e Binçës River. It stretches eastward to the Preševo Valley in southern Serbia.

Geographic entities mentioned:
surface_form: kosovo pomoravlje
instance_of: Valley
countries: Kosovo
coordinates: lat: 42.46666667
lon: 21.46666667
surface_form: anamorava
instance_of: Valley
countries: Kosovo
coordinates: lat: 42.46666667
lon: 21.46666667
Anamorava. Anamorava (), or Kosovo Pomoravlje (/ &quot;Kosovsko Pomoravlje&quot;, &quot;Morava Valley of Kosovo&quot;), is a valley in Kosovo, in the southern part of the District of Gjilan surrounding the Morava e Binçës River. It stretches eastward to the Preševo Valley in southern Serbia.

Geographic entities mentioned:
surface_form: anamorava
instance_of: Valley
countries: Kosovo
coordinates: lat: 42.46666667
lon: 21.46666667
In 2011, the town had 216 residents. History. The first settlers made their homes along the shores of Long Lake (now known as Last Mountain Lake), at places close to McKillops's Landing, Arlington Beach, and Taylorboro. The original settlers used the waters of Last Mountain Lake, which is long, as a means of transportation.

Geographic entities mentioned:
surface_form: Last Mountain Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.1667
lon: -105.25
Attractions in the city include the Lamido Palace and the Lamido Grand Mosque. The town is named after a nearby mountain on its eponymous plateau; the mountain's name is the Mbum word for &quot;navel mountain&quot;. &quot;Ngaou&quot; mean mountain in Mbum, and &quot;Ndare&quot; mean navel in Mbum language. Because of this some people call the navel of Adamwa. Mount Ngaoundéré is rockey.

Geographic entities mentioned:
surface_form: eponymous plateau
instance_of: Plateau
countries: Cameroon
coordinates: lat: 7.33333333
lon: 13.83333333
Al-Makassed Islamic Charitable Society Hospital () is a Muslim Community founded teaching hospital and charitable hospital of the Palestinian Arab’s charitable founded by Makassed Islamic Charitable Society, There is one of district general hospital from part of six hospitals in the East Jerusalem Hospitals Network. It has 250 beds and is situated on Mount of Olives in East Jerusalem.

Geographic entities mentioned:
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
Lago dei Monaci. Lago dei Monaci is a lake in the Province of Latina, Lazio, Italy. At an elevation of 1 m, its surface area is 0.9 km².

Geographic entities mentioned:
surface_form: lago dei monaci
instance_of: Lake
countries: Italy
coordinates: lat: 41.3804
lon: 12.9296
Little Iskut River. The Little Iskut River is a tributary of the Iskut River in the northwest part of the province of British Columbia, Canada, in Cassiar Land District. From its source at Little Ball Lake in Mount Edziza Provincial Park, the Little Iskut River flows about, generally north to the vicinity of Mowdale Lake, then southeast and south to the Iskut River just below Cascade Falls.

Geographic entities mentioned:
surface_form: Little Ball Lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.34889
lon: -130.58917
surface_form: ball lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.7
lon: -125.317
surface_form: little iskut river
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.448889
lon: -130.268611
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
The Little Iskut River is in the asserted traditional territory of the Tahltan First Nation and Iskut First Nation, of the Tahltan people. Geography. The Little Iskut River originates at Little Ball Lake just south of Kounugu Mountain. It flows northeast through the southern part of Mount Edziza Provincial Park, then north, forming the southeastern boundary of the park.

Geographic entities mentioned:
surface_form: Kounugu Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3647
lon: -130.5973
surface_form: ball lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.7
lon: -125.317
surface_form: little ball lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.34889
lon: -130.58917
surface_form: little iskut river
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.448889
lon: -130.268611
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
It collects tributary streams flowing east from the Spectrum Range. Stewbomb Creek and its tributary Artifact Creek flow from Obsidian Ridge, Artifact Ridge, and high mountains including Yeda Peak and Kitsu Peak. Bourgeaux Creek and its tributary Gerlib Creek also flow east from the Spectrum Range, Artifact Ridge, and high peaks including Tadeda Peak and Armadillo Peak.

Geographic entities mentioned:
surface_form: Stewbomb Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.41635
lon: -130.50397
surface_form: Artifact Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.41635
lon: -130.53728
surface_form: Yeda Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3811
lon: -130.678
surface_form: Kitsu Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.4246
lon: -130.6906
It collects tributary streams flowing east from the Spectrum Range. Stewbomb Creek and its tributary Artifact Creek flow from Obsidian Ridge, Artifact Ridge, and high mountains including Yeda Peak and Kitsu Peak. Bourgeaux Creek and its tributary Gerlib Creek also flow east from the Spectrum Range, Artifact Ridge, and high peaks including Tadeda Peak and Armadillo Peak.

Geographic entities mentioned:
surface_form: Bourgeaux Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.49966
lon: -130.45397
surface_form: Tadeda Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5422
lon: -130.616
surface_form: Armadillo Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5383
lon: -130.56
Between Stewbomb Creek and Bourgeaux Creek the historic Yukon Telegraph Trail crosses the Little Iskut River, following Bourgeaux Creek over Raspberry Pass to Mess Creek, continuing north along the western side of the Mount Edziza volcanic complex to Telegraph Creek on the Stikine River. After Bourgeaux Creek, near Mowdade Lake, the Little Iskut turns sharply to flow southeast.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: little iskut river
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.448889
lon: -130.268611
surface_form: stewbomb creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.41635
lon: -130.50397
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: bourgeaux creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.49966
lon: -130.45397
surface_form: bourgeaux creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.49966
lon: -130.45397
Little Iskut River. The Little Iskut River is a tributary of the Iskut River in the northwest part of the province of British Columbia, Canada, in Cassiar Land District. From its source at Little Ball Lake in Mount Edziza Provincial Park, the Little Iskut River flows about, generally north to the vicinity of Mowdale Lake, then southeast and south to the Iskut River just below Cascade Falls.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: little iskut river
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.448889
lon: -130.268611
The river's watershed's land cover is classified as 36.8% conifer forest, 27.9% barren, 17.3% shrubland, 10.3% herbaceous, and small amounts of other cover. The mouth of the Little Iskut River is located about southeast of Telegraph Creek, British Columbia, about south of Dease Lake, and about northeast of Wrangell, Alaska.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: little iskut river
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.448889
lon: -130.268611
surface_form: dease lake
instance_of: Lake
countries: Canada
coordinates: lat: 58.63502
lon: -130.03761
The Little Iskut River is a major tributary of the Iskut River. About 5% of its watershed is glacier-covered. Much of the lower Little Iskut River is braided. Geology. During the Miocene epoch, a series of lava flows from the adjacent Mount Edziza volcanic complex travelled east into the Little Iskut River. Here, the flows formed a lava dam behind which water ponded to form Raspberry Lake.

Geographic entities mentioned:
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: little iskut river
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.448889
lon: -130.268611
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Little Iskut River. The Little Iskut River is a tributary of the Iskut River in the northwest part of the province of British Columbia, Canada, in Cassiar Land District. From its source at Little Ball Lake in Mount Edziza Provincial Park, the Little Iskut River flows about, generally north to the vicinity of Mowdale Lake, then southeast and south to the Iskut River just below Cascade Falls.

Geographic entities mentioned:
surface_form: little iskut river
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.448889
lon: -130.268611
From its source at Little Ball Lake in Mount Edziza Provincial Park, the Little Iskut River flows about, generally north to the vicinity of Mowdale Lake, then southeast and south to the Iskut River just below Cascade Falls. The Little Iskut River is part of the Stikine River drainage basin, as the Iskut River is a major tributary of the Stikine.

Geographic entities mentioned:
surface_form: little iskut river
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.448889
lon: -130.268611
The Little Iskut River is part of the Stikine River drainage basin, as the Iskut River is a major tributary of the Stikine. The Little Iskut River's watershed covers and its mean annual discharge is an estimated. The river's watershed's land cover is classified as 36.8% conifer forest, 27.9% barren, 17.3% shrubland, 10.3% herbaceous, and small amounts of other cover.

Geographic entities mentioned:
surface_form: little iskut river
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.448889
lon: -130.268611
The mouth of the Little Iskut River is located about southeast of Telegraph Creek, British Columbia, about south of Dease Lake, and about northeast of Wrangell, Alaska. The Little Iskut River is in the asserted traditional territory of the Tahltan First Nation and Iskut First Nation, of the Tahltan people. Geography.

Geographic entities mentioned:
surface_form: little iskut river
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.448889
lon: -130.268611
After Bourgeaux Creek, near Mowdade Lake, the Little Iskut turns sharply to flow southeast. It empties into the Iskut River just downstream of Cascade Falls. The Little Iskut River is a major tributary of the Iskut River. About 5% of its watershed is glacier-covered. Much of the lower Little Iskut River is braided. Geology.

Geographic entities mentioned:
surface_form: little iskut river
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.448889
lon: -130.268611
It empties into the Iskut River just downstream of Cascade Falls. The Little Iskut River is a major tributary of the Iskut River. About 5% of its watershed is glacier-covered. Much of the lower Little Iskut River is braided. Geology. During the Miocene epoch, a series of lava flows from the adjacent Mount Edziza volcanic complex travelled east into the Little Iskut River.

Geographic entities mentioned:
surface_form: little iskut river
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.448889
lon: -130.268611
Geology. During the Miocene epoch, a series of lava flows from the adjacent Mount Edziza volcanic complex travelled east into the Little Iskut River. Here, the flows formed a lava dam behind which water ponded to form Raspberry Lake. Water discharging from this prehistoric lake eventually cut through the eastern edge of this dam to create a new course for the Little Iskut River.

Geographic entities mentioned:
surface_form: little iskut river
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.448889
lon: -130.268611
Geography. The Little Iskut River originates at Little Ball Lake just south of Kounugu Mountain. It flows northeast through the southern part of Mount Edziza Provincial Park, then north, forming the southeastern boundary of the park. It collects tributary streams flowing east from the Spectrum Range.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Between Stewbomb Creek and Bourgeaux Creek the historic Yukon Telegraph Trail crosses the Little Iskut River, following Bourgeaux Creek over Raspberry Pass to Mess Creek, continuing north along the western side of the Mount Edziza volcanic complex to Telegraph Creek on the Stikine River. After Bourgeaux Creek, near Mowdade Lake, the Little Iskut turns sharply to flow southeast.

Geographic entities mentioned:
surface_form: bourgeaux creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.49966
lon: -130.45397
El Turbón. El Turbón is a mountain massif of the Pre-Pyrenees, located in the province of Huesca, the most northerly province in the autonomous community of Aragon, Spain. This long mountain is aligned N - S. It is fairly easy to climb El Turbón, but it is better not to do so in mid summer when this great expanse of naked rock can reach very high temperatures. Geology.

Geographic entities mentioned:
surface_form: el turbón
instance_of: Mountain
countries: Spain
coordinates: lat: 42.418888888889
lon: 0.51388888888889
surface_form: turbón
instance_of: Mountain
countries: Spain
coordinates: lat: 42.418888888889
lon: 0.51388888888889
It is fairly easy to climb El Turbón, but it is better not to do so in mid summer when this great expanse of naked rock can reach very high temperatures. Geology. El Turbón has a massive rocky limestone outcrop at its centre made of Cretaceous marl. There are caves and shafts in the mountain. The Isábena River flows on the eastern side, separating El Turbón massif from the Mountains of Sis range.

Geographic entities mentioned:
surface_form: el turbón
instance_of: Mountain
countries: Spain
coordinates: lat: 42.418888888889
lon: 0.51388888888889
surface_form: turbón
instance_of: Mountain
countries: Spain
coordinates: lat: 42.418888888889
lon: 0.51388888888889
The Golden Fleece (painting). &quot;The Golden Fleece&quot;, originally known as &quot;Shearing at Newstead&quot;, is an 1894 painting by the Australian artist Tom Roberts. The painting depicts sheep shearers plying their trade in a timber shearing shed at &quot;Newstead North&quot;, a sheep station near Inverell on the Northern Tablelands of New South Wales.

Geographic entities mentioned:
surface_form: Northern Tablelands
instance_of: Plateau
countries: Australia
coordinates: lat: -30.595277777777778
lon: 151.5
These &quot;Bigfoot bogies&quot; were also used under the Class locomotives whenever they had to be exchanged for maintenance purposes, sometimes running under their own power, sometimes hauled dead. Over the years since the Class was commissioned, the demand for rail services declined steadily on both the ACR and the Langkloof lines.

Geographic entities mentioned:
surface_form: Langkloof
instance_of: Valley
countries: South Africa
coordinates: lat: -33.825
lon: 23.857777777778