Sarmila/GeoWiki-Features huggingface dataset:
It is located 6.1 km SW of Deoban and 19 km SSE lies Hathi Parbat. Climbing history. An Indian team from West Bengal led by Sisir Ghosh attempted Mandir Parbat in 1978 and reached a high point 19, 960 ft. A 10-member team of West Bengal led by Shankar Biswas reached the summit on September 20, 1989. Summit was reached by Shyamal Sarkar and three HAPs Nataraj, Tendi and Tharchen.

Geographic entities mentioned:
surface_form: mandir parbat
instance_of: Mountain
countries: India
coordinates: lat: 30.82777777777778
lon: 79.60388888888889
Summit was reached by Shyamal Sarkar and three HAPs Nataraj, Tendi and Tharchen. The team consisted of Subrata Banerjee, Debashish Biswas, Sanjoy Das, Dr. Sujit Guha, Ajoy Mondai, Bhaskar Mukherjee, Soumajit Roy, Shyamal Sarkar and Nishi Kanta Sen. Glaciers and rivers. Bank kund Glacier lies on the eastern side of Mandir Parbat. On the western side lies an unnamed glacier.

Geographic entities mentioned:
surface_form: mandir parbat
instance_of: Mountain
countries: India
coordinates: lat: 30.82777777777778
lon: 79.60388888888889
The route is a circuit of roughly 58 miles (93 kilometres), taking in 24 summits with a total climb of around 28,500 feet (8,700 metres). Ben Nevis, Great Britain's highest peak, is included in the route along with 22 other Munros. Originally, all 24 summits on the Ramsay Round were Munros, but Sgurr an Iubhair was declassified as a Munro in 1997.

Geographic entities mentioned:
surface_form: Ben Nevis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.796891
lon: -5.003675
Sphingomonas desiccabilis. &quot;Sphingomonas desiccabilis&quot; is a Gram-negative and non-motile bacterium from the genus of Sphingomonas which has been isolated from biological soil crusts in the Colorado Plateau in the United States. It has been sent on the International Space Station in 2019 and 2020 for the BioRock and BioAsteroid experiments, respectively.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
Samdobong. Samdobong is a mountain of South Korea. It has an elevation of 1,176 metres.

Geographic entities mentioned:
surface_form: samdobong
instance_of: Mountain
countries: South Korea
Blåbergi. Blåbergi is a mountain in the municipality of Hol in Buskerud county, Norway. It is south of Fossedalen, southeast of Fossebrea and southwest of Nuten.

Geographic entities mentioned:
surface_form: fossebrea
instance_of: Mountain
countries: Norway
coordinates: lat: 60.77888889
lon: 8.42111111
Blåbergi. Blåbergi is a mountain in the municipality of Hol in Buskerud county, Norway. It is south of Fossedalen, southeast of Fossebrea and southwest of Nuten.

Geographic entities mentioned:
surface_form: blåbergi
instance_of: Mountain
countries: Norway
coordinates: lat: 60.73333333
lon: 7.81666667
Leaders of the protest rejected this view, indicating that the Proclamation did not call for punishment, but rather for accurate representation. After the controversial intervention of Romanian Police forces, and retaliation from the protesters, the newly-elected president made a public appeal which resulted in a violent intervention by groups of miners arriving from the Jiu Valley. Legacy.

Geographic entities mentioned:
surface_form: Jiu Valley
instance_of: Valley
countries: Romania
coordinates: lat: 43.77805556
lon: 23.81333333
Ozark Venture Base. Established in 1995, the Ozark Venture Base includes COPE, a mountain man living history program, a sea kayaking program on Lake Ouachita, and a trek program. Several of the programs take place off of the Reservation and Scouts only stay in the Base on the first and last days in the program.

Geographic entities mentioned:
surface_form: Lake Ouachita
instance_of: Lake
countries: United States
coordinates: lat: 34.6
lon: -93.3333
Kostal Cone. Kostal Cone, also called Kostal Volcano and Fire Mountain, is a young cinder cone in Wells Gray Provincial Park in east-central British Columbia, Canada. It rises from the northeast shore of Kostal Lake in the Cariboo Mountains. With an elevation of, Kostal Cone is one of the lowest volcanoes in the Wells Gray-Clearwater volcanic field.

Geographic entities mentioned:
surface_form: Kostal Lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.164
lon: -119.976
Lava flows from Kostal's 400 BP eruption are basaltic in composition and forms a lava bed. It is an example of volcanic activity that has occurred in the Wells Gray-Clearwater volcanic field since the last glacial period; others include the Dragon's Tongue lava flow from Dragon Cone just north of Kostal Cone and the Flourmill Volcanoes north of Mahood Lake.

Geographic entities mentioned:
surface_form: Dragon Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 52.25
lon: -120.05
surface_form: Mahood Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.910443
lon: -120.399196
surface_form: kostal cone
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1667
lon: -119.95
Kostal Cone. Kostal Cone, also called Kostal Volcano and Fire Mountain, is a young cinder cone in Wells Gray Provincial Park in east-central British Columbia, Canada. It rises from the northeast shore of Kostal Lake in the Cariboo Mountains. With an elevation of, Kostal Cone is one of the lowest volcanoes in the Wells Gray-Clearwater volcanic field.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: kostal cone
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1667
lon: -119.95
surface_form: cinder cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9717
lon: -123.007
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Kostal Cone. Kostal Cone, also called Kostal Volcano and Fire Mountain, is a young cinder cone in Wells Gray Provincial Park in east-central British Columbia, Canada. It rises from the northeast shore of Kostal Lake in the Cariboo Mountains. With an elevation of, Kostal Cone is one of the lowest volcanoes in the Wells Gray-Clearwater volcanic field.

Geographic entities mentioned:
surface_form: kostal cone
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1667
lon: -119.95
It rises from the northeast shore of Kostal Lake in the Cariboo Mountains. With an elevation of, Kostal Cone is one of the lowest volcanoes in the Wells Gray-Clearwater volcanic field. There has been activity at this site as recently as 7,600 years ago, though more likely less than 1,000 years ago.

Geographic entities mentioned:
surface_form: kostal cone
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1667
lon: -119.95
There has been activity at this site as recently as 7,600 years ago, though more likely less than 1,000 years ago. Kostal Cone is too young for the commonly used potassium-argon dating technique (usable on specimens over 100,000 years old), and no charred organic material for radiocarbon dating has been found.

Geographic entities mentioned:
surface_form: kostal cone
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1667
lon: -119.95
However, the uneroded structure of the cone with the existence of trees on its flanks and summit have it an area for dendrochronology studies, which reveals the growth of tree-ring patterns. Tree-growth data has revealed an age of 400 years for Kostal Cone, making it the youngest volcano in the Wells Gray-Clearwater volcanic field and one of the youngest volcanoes in Canada.

Geographic entities mentioned:
surface_form: kostal cone
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1667
lon: -119.95
Tree-growth data has revealed an age of 400 years for Kostal Cone, making it the youngest volcano in the Wells Gray-Clearwater volcanic field and one of the youngest volcanoes in Canada. Kostal Cone is made of fragmented and solidified lava called cinder and its summit contains a bowl-shaped crater.

Geographic entities mentioned:
surface_form: kostal cone
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1667
lon: -119.95
Stage 5. 11 June 2009 &ndash; Valence to Mont Ventoux,
The first of the 2009 Dauphiné's four straight mountain stages sees the peloton ascend to the peak colloquially known as &quot;Mount Baldy&quot;, some six weeks before the mountain hosts a critical stage finish in the 2009 Tour de France.

Geographic entities mentioned:
surface_form: Mont Ventoux
instance_of: Mountain
countries: France
coordinates: lat: 44.166666666667
lon: 5.2833333333333
After his death, his daughter Effie said her father was a professor of Latin at the University of Iowa when he came to Los Angeles for a visit and stayed. Shafer taught in the San Joaquin Valley and then moved to Los Angeles and worked at the first public school in Santa Monica. He was the only teacher at Cahuenga School, which served the areas later known as Hollywood and the Wilshire District.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Poggio Sommavilla. Poggio Sommavilla or Poggetto (Local dialect: &quot;Poggettu&quot;) is a &quot;frazione&quot; of Collevecchio, Lazio region at Tiber Valley in Italy. It is known for the discovery of archaeological finds from prehistory. History.

Geographic entities mentioned:
surface_form: Tiber Valley
instance_of: Valley
countries: Italy
coordinates: lat: 42.133333333333
lon: 12.583333333333
More studies and surveys are recommended to better understand its biology, population and conservation status. It is found in multiple protected areas such as Northern Sierra Madre Natural Park, Bulusan Volcano Natural Park, Mount Banahaw, Aurora Memorial National Park and Kalbario–Patapat Natural Park but despite this legal protection, deforestation and hunting continues even within these areas.

Geographic entities mentioned:
surface_form: Mount Banahaw
instance_of: Mountain
countries: Philippines
coordinates: lat: 14.066666666667
lon: 121.48333333333
The high outer rim of the Grand Canyon is absent at Toroweap, and the overlook can therefore be reached by a road which follows the Toroweap Valley to the brink of the Inner Gorge. Just west of the overlook the Lava Falls can be seen spilling over the rim and falling to the river. Nearby is Vulcan's Throne, a cinder cone from the period of volcanic activity. Access.

Geographic entities mentioned:
surface_form: Vulcan's Throne
instance_of: Mountain
countries: United States
coordinates: lat: 36.2189
lon: -113.077
's Philippe Gilbert claimed victory for the second successive year after making a decisive move in the race's closing stages, attacking the field on the final climb of the race – the 12% gradient Cauberg – and thus becoming the first rider to win two Amstel Gold Races since Rolf Järmann won the race in 1993 and 1998.

Geographic entities mentioned:
surface_form: Cauberg
instance_of: Mountain
countries: Netherlands
coordinates: lat: 50.860278
lon: 5.823333
The Francis Oats House, a hostel for pupils at the Kimberley Boys' High School, was built in 1920 and was still in use in 2016. Cornish investments. On a visit back to Cornwall, Oats bought shares in the Levant Mine. He also took shareholdings in the Cape Cornwall and Kenidjack mines. At the time of his death he was chairman of Basset Mines of Redruth.

Geographic entities mentioned:
surface_form: Kenidjack
instance_of: Valley
countries: United Kingdom
coordinates: lat: 50.13
lon: -5.703
Course. The Lathkill Dale starts just to the east of the small village of Monyash, to the west of Bakewell, and is dry initially. In times of high rainfall the source of the river is Lathkill Head Cave (), where water which has flowed underground from the Flagg area to the west of Monyash emerges, but in drier conditions the river rises from springs further down the valley.

Geographic entities mentioned:
surface_form: Lathkill Dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.1896
lon: -1.71446
It is native to western North America (British Columbia, Washington, Oregon, California, Nevada, Utah, Idaho, Montana, Wyoming, Colorado), where it grows in several types of mountain and plateau habitat, including sagebrush. It typically prefers rocky soil. The species name is from the Modoc Plateau, in the northeast California range. Description.

Geographic entities mentioned:
surface_form: Modoc Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 41.6
lon: -121.2
Description. The wingspan is about for males and about for females. Adults are on wing from September to December. There is one generation per year. Its nearest relative, &quot;Anthene minima&quot;, is found approximately to the east, in KwaZulu-Natal, Mpumalanga, and the Okavango Delta in Botswana. Habitat and behavior. The larvae possibly feed on &quot;Acacia erioloba&quot; species.

Geographic entities mentioned:
surface_form: Okavango Delta
instance_of: Body of water
Watercourse
countries: Botswana
coordinates: lat: -19.4
lon: 22.9
Ballyscullion House. Ballyscullion House refers to two country houses built for the Hervey family near Bellaghy in County Londonderry, Northern Ireland, close to Lough Beg at north-west corner of Lough Neagh. The first Ballyscullion House, sometimes called &quot;Bishop's Folly&quot;, was a large house intended for Frederick Hervey, 4th Earl of Bristol and Bishop of Derry.

Geographic entities mentioned:
surface_form: Lough Beg
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.797222222222
lon: -6.475
surface_form: Lough Neagh
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.618333333333
lon: -6.3952777777778
Barysh (Dniester tributary). Barysh () is a river in Ukraine, which flows within the Chortkiv Raion of Ternopil Oblast. Left tributary of the river Dniester from the Black Sea basin. Length 38 km, basin area 186 km2. It originates on the northern slopes of the Podolian Upland, near the village of Ozeriany, Chortkiv Raion.

Geographic entities mentioned:
surface_form: Podolian Upland
instance_of: Plateau
countries: Ukraine
Moldova
coordinates: lat: 49.0275
lon: 27.85619444
Fort Mohave. Fort Mohave was originally named Camp Colorado when it was established on April 19, 1859 by Lieutenant Colonel William Hoffman during the Mohave War. It was located on the east bank of the Colorado River, at Beale's Crossing, near the head of the Mohave Valley in Mohave County, Arizona by the recommendation of Lieutenant Edward Fitzgerald Beale.

Geographic entities mentioned:
surface_form: Mohave Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.9569
lon: -114.585
Mongo Twa. The 14,000 Twa (locally &quot;Cwa&quot;, approximately) of the swamp forest north and west of Lake Tumba and between Tumba and Lake Mai-Ndombe in the west of the Congo are one of several fishing and hunter-gatherer castes living in a patron–client relationship with farming Bantu peoples across central and southern Africa.

Geographic entities mentioned:
surface_form: Lake Tumba
instance_of: Lake
countries: Democratic Republic of the Congo
coordinates: lat: -0.83333333333333
lon: 18
surface_form: Lake Mai-Ndombe
instance_of: Lake
countries: Democratic Republic of the Congo
coordinates: lat: -2
lon: 18.33
Ch'alla Willk'i (Totora). Ch'alla Willk'i (Aymara &quot;ch'alla&quot; sand, &quot;willk'i&quot; gap, &quot;sand gap&quot;, also spelled &quot;Challa Willkhi&quot;) is a mountain in the Andes of Bolivia. It is located in the Oruro Department, San Pedro de Totora Province. The Luk'i Jawira &quot;(Lokhe Jahuira)&quot; originates north of Ch'alla Willk'i. It flows to the northwest.

Geographic entities mentioned:
surface_form: ch'alla willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.1842
lon: -68.1725
surface_form: willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.39861111
lon: -69.02222222
surface_form: ch'alla willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.1364
lon: -68.2678
surface_form: ch'alla willk'i (totora)
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.88888889
lon: -68.29583333
Ch'alla Willk'i (Totora). Ch'alla Willk'i (Aymara &quot;ch'alla&quot; sand, &quot;willk'i&quot; gap, &quot;sand gap&quot;, also spelled &quot;Challa Willkhi&quot;) is a mountain in the Andes of Bolivia. It is located in the Oruro Department, San Pedro de Totora Province. The Luk'i Jawira &quot;(Lokhe Jahuira)&quot; originates north of Ch'alla Willk'i. It flows to the northwest.

Geographic entities mentioned:
surface_form: ch'alla willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.1842
lon: -68.1725
surface_form: willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.39861111
lon: -69.02222222
surface_form: willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.39861111
lon: -69.02222222
surface_form: ch'alla willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.1364
lon: -68.2678
surface_form: ch'alla willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.88888889
lon: -68.29583333
Ch'alla Willk'i (Totora). Ch'alla Willk'i (Aymara &quot;ch'alla&quot; sand, &quot;willk'i&quot; gap, &quot;sand gap&quot;, also spelled &quot;Challa Willkhi&quot;) is a mountain in the Andes of Bolivia. It is located in the Oruro Department, San Pedro de Totora Province. The Luk'i Jawira &quot;(Lokhe Jahuira)&quot; originates north of Ch'alla Willk'i. It flows to the northwest.

Geographic entities mentioned:
surface_form: ch'alla willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.1842
lon: -68.1725
surface_form: willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.39861111
lon: -69.02222222
surface_form: ch'alla willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.1364
lon: -68.2678
surface_form: ch'alla willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.88888889
lon: -68.29583333
It is renowned for its walnuts and apricots. Lhamo La-tso is the name of a small oval lake in the area. It is also called &quot;Oracle Lake&quot;, as it is where senior Tibetan monks go for visions to assist in the discovery of reincarnations of the Dalai Lamas is located in Gyaca County. Administrative divisions. Gyaca County contains 2 towns and 5 townships.

Geographic entities mentioned:
surface_form: Lhamo La-tso
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 29.516666666667
lon: 92.733333333333
In 1984, Aïn Témouchent Province was carved out of its territory. Geographical features. Lake Sidi Mohamed Benali is located in Sidi Bel Abbès Province, within the commune of Aïn Tindamine. Administrative divisions. The province is divided into 15 districts (&quot;daïras&quot;), which are further divided into 52 &quot;communes&quot; or municipalities.

Geographic entities mentioned:
surface_form: Lake Sidi Mohamed Benali
instance_of: Lake
countries: Algeria
France
coordinates: lat: 35.2425
lon: -0.6475000000000001
Barrhorn. The Barrhorn is a mountain in the Pennine Alps. Access roads and normal climbing route. The only access road is from the north, from the Turtmann village in the Rhona valley. From there, take direction to Gruben, and after passing it drive up to Vorder Sänntum at 1900 m. You will come to the point where the public road ends up, there is a formal parking that costs 4 CHF per day.

Geographic entities mentioned:
surface_form: barrhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.155833333333
lon: 7.7341666666667
Between the First and Second World Wars the Clemenses visited Hebei and Shandong provinces in China as well as Indo-China, British North Borneo, Sarawak, Java and Singapore. Especially notable are their visits to Mount Kinabalu in northern Borneo in 1915, and again in 1931–1934, where they amassed the largest collections of plants ever made from that mountain.

Geographic entities mentioned:
surface_form: Mount Kinabalu
instance_of: Mountain
countries: Malaysia
coordinates: lat: 6.075
lon: 116.5586111111111
Gilbert Strait. Gilbert Strait () is a strait between Trinity Island and Tower Island in the Palmer Archipelago. The strait was named by a British expedition 1828–31, under Foster, for Davies Gilbert, President of the Royal Society from 1827–30, and of the committee which formulated the objectives of the expedition.

Geographic entities mentioned:
surface_form: foster
instance_of: Mountain
coordinates: lat: -62.996666666667
lon: -62.548611111111
surface_form: gilbert
instance_of: Mountain
coordinates: lat: -69.2667
lon: -66.2833
surface_form: gilbert
instance_of: Body of water
coordinates: lat: -63.6333
lon: -60.2667
Gilbert Strait. Gilbert Strait () is a strait between Trinity Island and Tower Island in the Palmer Archipelago. The strait was named by a British expedition 1828–31, under Foster, for Davies Gilbert, President of the Royal Society from 1827–30, and of the committee which formulated the objectives of the expedition.

Geographic entities mentioned:
surface_form: gilbert
instance_of: Mountain
coordinates: lat: -69.2667
lon: -66.2833
surface_form: gilbert
instance_of: Body of water
coordinates: lat: -63.6333
lon: -60.2667
The strait was mapped by the Swedish Antarctic Expedition (SAE) of 1901–04, under Otto Nordenskjöld. Within the Gilbert Strait, off the east coast of Cape Neumayer on Trinity Island, is a small group of rocks called the Oluf Rocks. Just south of them is Sven Rock, and to the east are the Ryge Rocks.

Geographic entities mentioned:
surface_form: gilbert
instance_of: Mountain
coordinates: lat: -69.2667
lon: -66.2833
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: gilbert
instance_of: Body of water
coordinates: lat: -63.6333
lon: -60.2667
surface_form: neumayer
instance_of: Body of water
coordinates: lat: -64.7906
lon: -63.1392
Honaz Tunnel. The Honaz Tunnel () is a road tunnel in Denizli Province, Turkey. It connects the state roads and, passing through Mount Honaz. The tunnel was opened to traffic on 28 January 2023 by Turkish president Recep Tayyip Erdoğan.

Geographic entities mentioned:
surface_form: Mount Honaz
instance_of: Mountain
countries: Turkey
coordinates: lat: 37.67861111111111
lon: 29.2845
Zaka Valley. The Zaka Valley () is a valley in the Julian Alps in northwestern Slovenia. Geography. The Zaka Valley lies at the west end of Lake Bled. The railway between Jesenice and Gorizia runs above it.

Geographic entities mentioned:
surface_form: Lake Bled
instance_of: Lake
countries: Slovenia
coordinates: lat: 46.364444444444
lon: 14.094722222222
surface_form: bled
instance_of: Lake
countries: Slovenia
coordinates: lat: 46.364444444444
lon: 14.094722222222
surface_form: zaka valley
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.3613
lon: 14.0761
Zaka Valley. The Zaka Valley () is a valley in the Julian Alps in northwestern Slovenia. Geography. The Zaka Valley lies at the west end of Lake Bled. The railway between Jesenice and Gorizia runs above it.

Geographic entities mentioned:
surface_form: zaka
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.3613
lon: 14.0761
Locally, a distinction is made between the Little Zaka Valley (), originally at the extreme southeast part of the lake, east of Little Osojnica Hill (,) where Jezernica Creek empties into the lake in the hamlet of Mlino, and the Big Zaka Valley (), which lies at the westernmost part of the lake between Little Osojnica Hill and Kuhovnica Hill (), through which Zaka Creek flows, emptying into Zaka Bay.

Geographic entities mentioned:
surface_form: zaka
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.3613
lon: 14.0761
surface_form: zaka
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.3613
lon: 14.0761
surface_form: zaka
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.3613
lon: 14.0761
surface_form: zaka
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.3613
lon: 14.0761
The name &quot;Mala Zaka&quot; is now applied to the area around the rowing club at the extreme northwest part of the lake. Swimming areas are also located in the bays below the Big Zaka Valley and Little Zaka Valley. Name. The name &quot;Zaka&quot; was first recorded in 1185 as &quot;Zake&quot;.

Geographic entities mentioned:
surface_form: zaka
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.3613
lon: 14.0761
surface_form: zaka
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.3613
lon: 14.0761
History. Archaeological finds from the Urnfield culture and Roman coins have been found in the Zaka Valley, and there is a prehistoric Celtic burial site between Upper and Lower Ak. During the Second World War, members of the Carinthian People's League () renovated two ski jumps in the Zaka Valley.

Geographic entities mentioned:
surface_form: zaka
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.3613
lon: 14.0761
The name &quot;Mala Zaka&quot; is now applied to the area around the rowing club at the extreme northwest part of the lake. Swimming areas are also located in the bays below the Big Zaka Valley and Little Zaka Valley. Name. The name &quot;Zaka&quot; was first recorded in 1185 as &quot;Zake&quot;.

Geographic entities mentioned:
surface_form: zaka
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.3613
lon: 14.0761
Swimming areas are also located in the bays below the Big Zaka Valley and Little Zaka Valley. Name. The name &quot;Zaka&quot; was first recorded in 1185 as &quot;Zake&quot;. France Bezlaj suggested that the name &quot;Zaka&quot; was a contraction of *&quot;zějaka&quot; 'opening between hills'.

Geographic entities mentioned:
surface_form: zaka
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.3613
lon: 14.0761
Name. The name &quot;Zaka&quot; was first recorded in 1185 as &quot;Zake&quot;. France Bezlaj suggested that the name &quot;Zaka&quot; was a contraction of *&quot;zějaka&quot; 'opening between hills'. However, Dušan Čop has proposed that the name &quot;Zaka&quot; is a fused prepositional phrase derived from &quot;za Ak-&quot; 'behind Ak'.

Geographic entities mentioned:
surface_form: zaka
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.3613
lon: 14.0761
surface_form: zaka
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.3613
lon: 14.0761
He was then under Colonel John Bradstreet in North America. For Bradstreet, who was marching along the southern shore of Lake Erie from Niagara to re-establish British control in Indiana, he undertook a chancy mission in 1764, just after the end of the French and Indian War (the Seven Years' War in the North American theatre).

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
The original stone house was built in 1740. It was added to the National Register of Historic Places in 1995, as a highly stylized version of a typical Hudson Valley Dutch Colonial house, the use of brick and gambrel roof in its construction reflecting the influence of migrants from New Jersey and New York City, where that was more common. House and grounds.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Willis Curdy. Willis Curdy (born October 30, 1947) is an American politician. He served as a Democratic member for the 98th district in the Montana House of Representatives from 2015 to 2023. Curdy was born in Bitterroot Valley in 1947 and currently resides in Missoula, Montana. He also attended the University of Montana, once from 1967 to 1971, and once in 1987.

Geographic entities mentioned:
surface_form: Bitterroot Valley
instance_of: Valley
countries: United States
coordinates: lat: 46.247
lon: -114.16
Pethia atra. &quot;Pethia atra&quot; is a species of cyprinid fish native to India where it is found in sluggish streams in the Imphal Valley, Manipur. This species can reach a length of SL.

Geographic entities mentioned:
surface_form: Imphal Valley
instance_of: Valley
countries: India
Suwannee Springs, Florida. Suwannee Springs (also spelled Suwanee Springs) is an unincorporated community located on the Suwannee River in Suwannee County, Florida, United States. At least six springs comprise Suwannee Springs, of which five spill directly into the south side of the Suwannee River.

Geographic entities mentioned:
surface_form: suwannee springs
instance_of: Landform
countries: United States
coordinates: lat: 30.3942
lon: -82.9372
The main spring flows inside a man-made wall fifteen feet high and three feet thick of limestone rock, this wall was built in the late 1890s. Suwannee Springs was a resort destination from the 1830s until the early 1900s. There was once a large hotel and many cabins here for guests to stay in. The hotel burned in the early 1900s and was never rebuilt.

Geographic entities mentioned:
surface_form: suwannee springs
instance_of: Landform
countries: United States
coordinates: lat: 30.3942
lon: -82.9372
There was once a large hotel and many cabins here for guests to stay in. The hotel burned in the early 1900s and was never rebuilt. Suwannee Springs is a second magnitude spring with an average flow of 23.4 cubic feet per second (cfs). The spring emerges from Oligocene age limestone and discharges hard, sulphur water. The water maintains a year-round temperature of 70 to 76 degrees.

Geographic entities mentioned:
surface_form: suwannee springs
instance_of: Landform
countries: United States
coordinates: lat: 30.3942
lon: -82.9372
Tønsberg grew up in Bekkelagshøgda, Nordstrand, in the eastern part of Oslo. He developed an early interest in nature, frequently visiting the nearby lake Østensjøvannet and the forests of Østmarka with his younger brother Knut. His systematic nature and passion for collecting began in childhood, where he organized a &quot;museum&quot; in the basement of his parents' house.

Geographic entities mentioned:
surface_form: Østensjøvannet
instance_of: Lake
countries: Norway
coordinates: lat: 59.888333333333
lon: 10.826944444444
India census, Perinad had a population of 32,864 with 16,032 males and 16,832 females. Perinad is a fast-growing village at the outskirts of Kollam city. National Highway 183 (India) connects Perinad region with Kollam, Kundara, Chengannur, etc. Perinad is situated on the shores of Ashtamudi lake. The Perinad panchayath office is about 13 km away from Kollam City center.

Geographic entities mentioned:
surface_form: Ashtamudi lake
instance_of: Lake
countries: India
coordinates: lat: 8.9833333333333
lon: 76.6
USS Asp (1812). The first &quot;Asp&quot; was a schooner in the United States Navy during the War of 1812. &quot;Asp&quot;, the former British merchant vessel &quot;Elizabeth&quot;, was captured on Lake Ontario in 1812 by the schooner, purchased by the Navy from the prize court: outfitted; and commissioned on 6 February 1813. Battle of York.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Battle of York. &quot;Asp&quot; got underway on 25 April 1813 as a unit of Commodore Isaac Chauncey's Lake Ontario squadron escorting General Henry Dearborn's 1,700 troops to York (now Toronto), Canada. The squadron arrived off York two days later. While Dearborn's troops hustled ashore, &quot;Asp&quot; and the other ships of the squadron supported them by bombarding the town's defenses.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Badwater Basin. Badwater Basin is an endorheic basin in Death Valley National Park, Death Valley, Inyo County, California, noted as the lowest point in North America and the United States, with a depth of below sea level. Mount Whitney, the highest point in the contiguous United States, is only to the northwest.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Badwater Basin. Badwater Basin is an endorheic basin in Death Valley National Park, Death Valley, Inyo County, California, noted as the lowest point in North America and the United States, with a depth of below sea level. Mount Whitney, the highest point in the contiguous United States, is only to the northwest.

Geographic entities mentioned:
surface_form: Mount Whitney
instance_of: Mountain
countries: United States
coordinates: lat: 36.57861111111111
lon: -118.29194444444444
The salt flats are hazardous to traverse (in many cases being only a thin white crust over mud), and so the sign marking the low point is at the pool instead. Despite Laguna del Carbón in Argentina having an elevation of −105 meters (−344 feet), Badwater Basin is often mistakenly described as the lowest elevation in the Western Hemisphere. Geography.

Geographic entities mentioned:
surface_form: Laguna del Carbón
instance_of: Lake
countries: Argentina
coordinates: lat: -49.5762
lon: -68.3514
Lake Ngozi. Lake Ngozi (or Lake Ngosi) is the second largest crater lake in Africa. It can be found near Tukuyu, a small town in the highland Rungwe District, Mbeya Region, of southern Tanzania in East Africa. It is part of the Poroto Mountains and the northern rim of the caldera is the highest point in the range. The caldera mostly composed from trachytic and phonolitic lavas.

Geographic entities mentioned:
surface_form: rungwe
instance_of: Mountain
countries: Tanzania
coordinates: lat: -9.135
lon: 33.668055555556
Lake Ngozi. Lake Ngozi (or Lake Ngosi) is the second largest crater lake in Africa. It can be found near Tukuyu, a small town in the highland Rungwe District, Mbeya Region, of southern Tanzania in East Africa. It is part of the Poroto Mountains and the northern rim of the caldera is the highest point in the range. The caldera mostly composed from trachytic and phonolitic lavas.

Geographic entities mentioned:
surface_form: ngozi
instance_of: Mountain
Lake
countries: Tanzania
coordinates: lat: -9.03333333
lon: 33.53333333
surface_form: lake ngozi
instance_of: Mountain
Lake
countries: Tanzania
coordinates: lat: -9.03333333
lon: 33.53333333
It is part of the Poroto Mountains and the northern rim of the caldera is the highest point in the range. The caldera mostly composed from trachytic and phonolitic lavas. Ngozi is a Holocene caldera that generated the Kitulo pumice 12,000 years ago during a Plinian eruption, most likely in the same eruption that generated the caldera.

Geographic entities mentioned:
surface_form: ngozi
instance_of: Mountain
Lake
countries: Tanzania
coordinates: lat: -9.03333333
lon: 33.53333333
Ngozi is a Holocene caldera that generated the Kitulo pumice 12,000 years ago during a Plinian eruption, most likely in the same eruption that generated the caldera. Other eruption deposits are the Ngozi Tuff (less than thousand years ago) and the Ituwa Surge base surge deposits of uncertain age, but intermediary to the Kitulo pumice and Ngozi Tuff.

Geographic entities mentioned:
surface_form: ngozi
instance_of: Mountain
Lake
countries: Tanzania
coordinates: lat: -9.03333333
lon: 33.53333333
surface_form: ngozi
instance_of: Mountain
Lake
countries: Tanzania
coordinates: lat: -9.03333333
lon: 33.53333333
Air temperatures above the lake are around 18 °C with only minor seasonal variations. Sporadically, the forests were occupied by Safwa hunters. Reports in 2013 stated that in the following year a geothermal project would commence in the vicinity of the volcano halfway between Ngozi and the town of Mbeya. Local Myths and Folk Tales.

Geographic entities mentioned:
surface_form: ngozi
instance_of: Mountain
Lake
countries: Tanzania
coordinates: lat: -9.03333333
lon: 33.53333333
Local Myths and Folk Tales. There are a number of local myths and folk tales which surround the volcanic lake, and the surrounding area. The Nyakyusa People (ethnic group in this area of Southern Tanzania) say that a shaman called Lwembe was chased from his birth village (Ukwama in the Makete area) to the waters of Lake Ngozi after the people had become weary of the deceptive nature of his magic.

Geographic entities mentioned:
surface_form: ngozi
instance_of: Mountain
Lake
countries: Tanzania
coordinates: lat: -9.03333333
lon: 33.53333333
surface_form: lake ngozi
instance_of: Mountain
Lake
countries: Tanzania
coordinates: lat: -9.03333333
lon: 33.53333333
The park is a &quot;Cooperating Site&quot; of the Keweenaw National Historical Park. History. Copper Harbor is located at the northern tip of the Keweenaw Peninsula, bordering Lake Superior. It is one of the best natural harbors in Keweenaw County and was a quick focus of attention after copper was discovered on the peninsula in the 1830s.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
In 1844, Fort Wilkins was established at the direction of Secretary of War William Wilkins. Fort Wilkins. The U.S. Army occupied Fort Wilkins, located east of Copper Harbor, Michigan on the strait of land between Copper Harbor and northern shore of Lake Fanny Hooe, in 1844.

Geographic entities mentioned:
surface_form: Lake Fanny Hooe
instance_of: Lake
countries: United States
coordinates: lat: 47.464166666667
lon: -87.863055555556
The Zangué River, a major right tributary of the Zambezi, makes a border with Caia District. The rivers in the southeastern portion of the district drain into the Pungwe River. The central part of the district lies on the Cheringoma Plateau. The highest point on the plateau is 379 meters elevation, located near Inhaminga.

Geographic entities mentioned:
surface_form: Cheringoma Plateau
instance_of: Mountain
countries: Mozambique
coordinates: lat: -18.44008333
lon: 35.0805
Her parents were Constance (born Wolfer) and Edward &quot;Bong&quot; VeaVea. Her father had been born in Queensland but his father was called Sam Ambrym so he probably came from the Vanuatu volcanic island of Ambryn. Sam is thought to have had French ancestors too. She lived in a community that had historically been oppressed.

Geographic entities mentioned:
surface_form: Ambryn
instance_of: Mountain
countries: Vanuatu
coordinates: lat: -16.333333333333
lon: 168.33333333333
He is traditionally associated with Brecknockshire, and wrote a eulogy of Brecknock which reveals that he was well acquainted with the area and it held a place in his affections. He is also associated with the Archenfield area of west Herefordshire and the Ewias or Vale of Ewyas of eastern Monmouthshire.

Geographic entities mentioned:
surface_form: Vale of Ewyas
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.941
lon: -3.035
Trite Chuki. Trite Chuki (, &quot;the three outcrops&quot;) or Tri Čuke () is a rocky summit in the western Balkan Mountains, on the border ridge between Bulgaria and Serbia. Trite Chuki is high and belongs to the Chiprovtsi Mountain, one of the highest parts of the Balkan Mountains. The summit's name references its three-headed shape composed by rocky outcrops.

Geographic entities mentioned:
surface_form: trite chuki
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 41.83333
lon: 25.96667
Trite Chuki. Trite Chuki (, &quot;the three outcrops&quot;) or Tri Čuke () is a rocky summit in the western Balkan Mountains, on the border ridge between Bulgaria and Serbia. Trite Chuki is high and belongs to the Chiprovtsi Mountain, one of the highest parts of the Balkan Mountains. The summit's name references its three-headed shape composed by rocky outcrops.

Geographic entities mentioned:
surface_form: trite chuki
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 41.83333
lon: 25.96667
surface_form: trite chuki
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 41.83333
lon: 25.96667
The summit's name references its three-headed shape composed by rocky outcrops. Trite Chuki's northeast slopes are very steep and almost vertical. The valleys of the Androvitsa and Grafska rivers originate east of Trite Chuki; the latter feeds the Lanzhin Skok, Voden Skok and Durshin Skok waterfalls. The large Chiprovtsi Waterfall originates to the north of the peak.

Geographic entities mentioned:
surface_form: trite chuki
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 41.83333
lon: 25.96667
The large Chiprovtsi Waterfall originates to the north of the peak. The middle outcrop hosts the remains of a basic fortification, reportedly built by Angel Voyvoda and Panayot Hitov in August 1863. The most common trailheads for ascending Trite Chuki are Kopilovtsi and Chiprovtsi in Bulgaria and Topli Do and Dojkinci in Serbia.

Geographic entities mentioned:
surface_form: trite chuki
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 41.83333
lon: 25.96667
The city is organized in a grid pattern dating back to the plan laid out by Augustus Jones between 1793 and 1797. Most streets are aligned in the north–south or east–west direction, based on the shoreline of Lake Ontario. In other words, major north–south roads are generally perpendicular to the Lake Ontario shoreline and major east–west roads are generally parallel to the lake's shoreline.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Gardiner Expressway. The Frederick G. Gardiner Expressway, known locally as &quot;the Gardiner&quot;, is an expressway connecting downtown with the western suburbs. Running close to the shore of Lake Ontario, it now extends from the junction of Highway 427 and the Queen Elizabeth Way (QEW) in the west to the foot of the Don Valley Parkway in the east, just past the mouth of the Don River.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
The newly modified Queens Quay was completed in 2015 from Bathurst Street to Bay Street. Lake Shore Boulevard. Lake Shore Boulevard, often incorrectly compounded to Lakeshore Boulevard, is so named because of its course along the Lake Ontario shoreline.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Mill Street Brewery, owned by InBev, is named after this street and continues to maintain a brewery and restaurant on that street in the Distillery District. Front Street. Front Street is so named because it fronted the Lake Ontario shoreline at the time of the original layout of York. The early street was called Palace Street.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Rathburn Road. Rathburn Road is a street in Etobicoke and Mississauga, which roughly parallels Burnhamthorpe Road to its north between the Credit River and Islington Avenue, breaking at the Etobicoke Creek, which divides the two cities. Its street name was acquired in 1954 to avoid name duplication and before known as Rosethorn Road. St. Clair Avenue. St.

Geographic entities mentioned:
surface_form: Credit River
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.5478
lon: -79.5808
York Mills Road. York Mills Road meets Yonge Street, the road to York, in Hoggs Hollow. Between 1804 and 1926, many mills flourished in this valley, lending to both the name of the road and neighbourhood. York Mills is an eastward continuation of Wilson Avenue; this continuity did not exist until the opening of the Yonge Subway extension in 1973.

Geographic entities mentioned:
surface_form: Hoggs Hollow
instance_of: Valley
countries: Canada
coordinates: lat: 43.739
lon: -79.4
Distribution and habitat. The common ant orchid grows in moist places in forest between the Northern Tablelands and Nowra. There is a single historical record from Kaitaia in New Zealand.

Geographic entities mentioned:
surface_form: Northern Tablelands
instance_of: Plateau
countries: Australia
coordinates: lat: -30.595277777777778
lon: 151.5
A white variety lacks these hematite crystals. Sillar is found as pyroclastic flow deposits of tuff near volcanoes in southern Peru, for example the now-extinct Chachani volcano which erupted flows of sillar during the Pleistocene epoch. Sillar facies Orvieto-Bagnoregio Ignimbrite (black blocks of scoria in red tuff) occurs at Civita di Bagnoregio in the Vulsini volcanic district of central Italy.

Geographic entities mentioned:
surface_form: Chachani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.194166666667
lon: -71.531666666667
Sillar is found as pyroclastic flow deposits of tuff near volcanoes in southern Peru, for example the now-extinct Chachani volcano which erupted flows of sillar during the Pleistocene epoch. Sillar facies Orvieto-Bagnoregio Ignimbrite (black blocks of scoria in red tuff) occurs at Civita di Bagnoregio in the Vulsini volcanic district of central Italy. Building stone.

Geographic entities mentioned:
surface_form: Vulsini
instance_of: Mountain
countries: Italy
coordinates: lat: 42.6
lon: 11.933333333333
The southern end of the extensive McCullough Range converges with four valleys and three mountain ranges. West of the McCullough's lie the endorheic Roach and Ivanpah Dry Lakes of Ivanpah Valley; the valley extends north into Las Vegas' southwest, a tributary to the Las Vegas Wash. Ivanpah Valley turns southeast to meet the water divide point.

Geographic entities mentioned:
surface_form: Ivanpah Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.56666666666667
lon: -115.375
surface_form: ivanpah valley
instance_of: Valley
countries: United States
coordinates: lat: 35.56666666666667
lon: -115.375
surface_form: ivanpah valley
instance_of: Valley
countries: United States
coordinates: lat: 35.56666666666667
lon: -115.375
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The northeast preserve corner is anchored by the water divide point. The northeast borders of the New York and smaller Castle Mountains meet the north of the Piute Range; to the west of the Piute's, east of the New York Mountains is the southerly draining endorheic Lanfair Valley.

Geographic entities mentioned:
surface_form: Lanfair Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.2889
lon: -115.103
surface_form: lanfair valley
instance_of: Valley
countries: United States
coordinates: lat: 35.2889
lon: -115.103
The Piute Valley Watershed is the first major watershed southeast of Las Vegas to drain into the western side of the south-flowing Colorado River. Though Piute Wash drains Piute Valley, the entire watershed includes Sacramento Wash (California) which covers an equivalent area west of the north–south Piute Range, and drains the Lanfair Valley and surrounding mountain ranges.

Geographic entities mentioned:
surface_form: Lanfair Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.2889
lon: -115.103
surface_form: lanfair valley
instance_of: Valley
countries: United States
coordinates: lat: 35.2889
lon: -115.103
surface_form: piute valley
instance_of: Valley
countries: United States
coordinates: lat: 35.3033
lon: -114.881
The north of the valley is at Searchlight, with some of the valley extending northwest from Searchlight. At the center-north lies Cal-Nev-Ari, Nevada. The second valley southeast of Las Vegas borders to the north, the endorheic Eldorado Valley, with its dry lake. The next watershed north is the Las Vegas Wash Watershed.

Geographic entities mentioned:
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6282988
lon: -97.0561783
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 38.3360373
lon: -117.7898285
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 45.0425
lon: -97.31972222