Sarmila/GeoWiki-Features huggingface dataset:
A promenade was built on top of the embankment around the perimeter of the pool. Pipes were laid from the streams by the Museum Gardens, under Bird Street into Minster Pool then under Dam Street and Stowe Fields into Stowe Pool. The stored water in Stowe Pool could then be conveyed back towards Sandfields Pumping Station, where it was piped along the railway line to Walsall.

Geographic entities mentioned:
surface_form: minster pool
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.684293
lon: -1.829972
surface_form: stowe pool
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.688384
lon: -1.822799
surface_form: stowe pool
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.688384
lon: -1.822799
In 1853 the South Staffordshire Waterworks Co. was founded and it was immediately proposed by John Robinson McClean to tap Lichfield's plentiful water resources to supply the Black Country. In 1856 the mill was demolished, the silt was dredged and an embankment built around the pool to raise the water level bringing it up to its current size.

Geographic entities mentioned:
surface_form: robinson
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.54
lon: -3.236
Stowe Pool. Stowe Pool is a reservoir located in the city of Lichfield, Staffordshire. Formerly a fishery (along with nearby Bishop's Pool and Minister Pool), Stowe Pool was turned into a reservoir in 1856 by the South Staffordshire Waterworks Co. Before 1856, Stowe Pool existed as a mill pond, with Stowe mill located just to the west of St Chad's Church.

Geographic entities mentioned:
surface_form: stowe pool
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.688384
lon: -1.822799
Formerly a fishery (along with nearby Bishop's Pool and Minister Pool), Stowe Pool was turned into a reservoir in 1856 by the South Staffordshire Waterworks Co. Before 1856, Stowe Pool existed as a mill pond, with Stowe mill located just to the west of St Chad's Church. Since 1968 the reservoir has not been used for supply and is now a public amenity used for recreation purposes.

Geographic entities mentioned:
surface_form: stowe pool
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.688384
lon: -1.822799
Before 1856, Stowe Pool existed as a mill pond, with Stowe mill located just to the west of St Chad's Church. Since 1968 the reservoir has not been used for supply and is now a public amenity used for recreation purposes. Stowe Pool is a designated SSSI site as it is home to the native white-clawed crayfish. Hydrology.

Geographic entities mentioned:
surface_form: stowe pool
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.688384
lon: -1.822799
The streams are then carried under Bird Street into Minster Pool and then pass into a pipe under Dam Street, Stowe Fields and into Stowe Pool. The outflow from Stowe Pool flows north as Curborough Brook, eventually flowing into the River Trent. Stowe Pool has a capacity of 217,600m3 (47.8 million gallons) and a surface area of 55,000m2 (14 acres), with an average depth of 3.95m. Natural History.

Geographic entities mentioned:
surface_form: stowe pool
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.688384
lon: -1.822799
Natural History. The pool supports a large variety of fish including, carp, bream, tench, roach, perch, pike and eel. Stowe Pool also supports a large and healthy population of white-clawed crayfish. Due to the isolated nature of Stowe Pool the crayfish are not exposed to disease which has spread into many of their other habitats.

Geographic entities mentioned:
surface_form: stowe pool
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.688384
lon: -1.822799
Stowe Pool also supports a large and healthy population of white-clawed crayfish. Due to the isolated nature of Stowe Pool the crayfish are not exposed to disease which has spread into many of their other habitats. As a result of its crayfish population Stowe Pool was designated a SSSI site in 1998.

Geographic entities mentioned:
surface_form: stowe pool
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.688384
lon: -1.822799
Due to the isolated nature of Stowe Pool the crayfish are not exposed to disease which has spread into many of their other habitats. As a result of its crayfish population Stowe Pool was designated a SSSI site in 1998. Effective wildlife management of the pool has attracted various species of wildfowl, including mute swans, moorhens, coots and grebes.

Geographic entities mentioned:
surface_form: stowe pool
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.688384
lon: -1.822799
Effective wildlife management of the pool has attracted various species of wildfowl, including mute swans, moorhens, coots and grebes. Stowe Pool has limited marginal vegetation, but its water plants include &quot;Polygonum amphibium&quot; and spiked water-milfoil. The shallow margins of the pool are dominated by extensive low-growing blankets of the water plant &quot;Chara aspera&quot; var.

Geographic entities mentioned:
surface_form: stowe pool
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.688384
lon: -1.822799
Because of Johnson's interest in the tree, it became known as 'Johnson's Willow'; the current tree on the site is a descendant of the original. By the 19th century due to the slow flowing nature of the streams Stowe Pool silted up and only existed at its eastern end. The western portion was a bog known as ‘the moggs’.

Geographic entities mentioned:
surface_form: stowe pool
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.688384
lon: -1.822799
It is roughly a diamond in shape, with a long north–south axis of about, and an east–west axis of about. It towers above Lake Malawi (elevation), and the towns of Livingstonia and Chilumba. Its well-defined north-west escarpment rises about above the north-eastern extremity of the Luangwa Valley, and its similarly prominent south-east escarpment rises about above the South Rukuru River valley.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
Nyika Plateau. The Nyika Plateau lies in northern Malawi, with a small portion in north eastern Zambia. Most of it lies at elevations of between, the highest point being at Nganda Peak. It is roughly a diamond in shape, with a long north–south axis of about, and an east–west axis of about. It towers above Lake Malawi (elevation), and the towns of Livingstonia and Chilumba.

Geographic entities mentioned:
surface_form: nyika plateau
instance_of: Plateau
countries: Malawi
Zambia
coordinates: lat: -10.35
lon: 33.6
The only settlement on the plateau is Chelinda, the headquarters and accommodation site for the Malawian park. Flora. A large area of the Nyika Plateau, around, makes up the Nyika National Park. Owing to its protected status, endemic flora continue to flourish in this part of the plateau. The flora of the plateau include gladioli, delphiniums, lobelia, and 'red hot pokers'.

Geographic entities mentioned:
surface_form: nyika plateau
instance_of: Plateau
countries: Malawi
Zambia
coordinates: lat: -10.35
lon: 33.6
Junik Mountains. The Junik Mountains (,), part of the Accursed Mountains, are on the border between Albania and Kosovo. They reach a height of. On the Kosovo side is the Dukagjin region, some to the north-west of the Junik commune. Moronica Park, in southwestern Kosovo, marks the beginning of the Junik Mountains.

Geographic entities mentioned:
surface_form: junik mountains
instance_of: Mountain
countries: Albania
Kosovo
coordinates: lat: 42.50230555555556
lon: 20.17913888888889
The Junik Mountains (,), part of the Accursed Mountains, are on the border between Albania and Kosovo. They reach a height of. On the Kosovo side is the Dukagjin region, some to the north-west of the Junik commune. Moronica Park, in southwestern Kosovo, marks the beginning of the Junik Mountains. The 1999 Battle of Košare was fought along the slopes of the Junik and Accursed Mountains.

Geographic entities mentioned:
surface_form: junik mountains
instance_of: Mountain
countries: Albania
Kosovo
coordinates: lat: 42.50230555555556
lon: 20.17913888888889
Nevertheless, X-rated movies and &quot;Playboy&quot; magazine were banned from his hotels. In October 1988, Keating opened his most extravagant real estate project ever, the, 600-room The Phoenician Resort at the base of Camelback Mountain.

Geographic entities mentioned:
surface_form: Camelback Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.5144875
lon: -111.9618124
Copap. Copap (possibly from Quechua &quot;qupa&quot; the mineral turquoise and the turquoise color, &quot;-p&quot; a suffix,) is a mountain in the Cordillera Blanca in the Andes of Peru whose summit reaches about or above sea level depending on the source. It is located in Chacas District, Asunción Province, Ancash; in the same massif as Perlilla which belongs to the glacial system of Copap.

Geographic entities mentioned:
surface_form: Perlilla
instance_of: Mountain
countries: Peru
coordinates: lat: -9.30444444
lon: -77.31861111
surface_form: copap
instance_of: Mountain
countries: Peru
coordinates: lat: -9.28333333
lon: -77.33333333
surface_form: perlilla
instance_of: Mountain
countries: Peru
coordinates: lat: -9.30444444
lon: -77.31861111
Copap. Copap (possibly from Quechua &quot;qupa&quot; the mineral turquoise and the turquoise color, &quot;-p&quot; a suffix,) is a mountain in the Cordillera Blanca in the Andes of Peru whose summit reaches about or above sea level depending on the source. It is located in Chacas District, Asunción Province, Ancash; in the same massif as Perlilla which belongs to the glacial system of Copap.

Geographic entities mentioned:
surface_form: copap
instance_of: Mountain
countries: Peru
coordinates: lat: -9.28333333
lon: -77.33333333
Gusti Adipati agrees to the condition, not realising that his sister has fallen for another. Sultan Mahmud then sends Tuah to lead a delegation to warn Majapahit's enemy. Gusti Putri, overcome with longing for her beloved, decides to leave Majapahit for Mount Ledang, where she will wait for Tuah. Gusti Adipati learns that his sister has fled, and chases her to Malacca.

Geographic entities mentioned:
surface_form: Mount Ledang
instance_of: Mountain
countries: Malaysia
coordinates: lat: 2.3741666666667
lon: 102.60777777778
It drains the Mackenzie Basin and runs south-east to enter the Pacific Ocean between Timaru and Oamaru on the east coast. It starts at the confluence of the Ōhau and Tekapo rivers, now at the head of the artificial Lake Benmore, these rivers being fed by three large glacial lakes, Pukaki, Tekapo, and Ōhau, at the base of the Southern Alps.

Geographic entities mentioned:
surface_form: Lake Benmore
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.415
lon: 170.22055555556
surface_form: Pukaki
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.116666666667
lon: 170.16666666667
surface_form: Tekapo
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.9
lon: 170.525
It starts at the confluence of the Ōhau and Tekapo rivers, now at the head of the artificial Lake Benmore, these rivers being fed by three large glacial lakes, Pukaki, Tekapo, and Ōhau, at the base of the Southern Alps. The Waitaki flows through Lake Benmore, Lake Aviemore and Lake Waitaki, these lakes being contained by the hydroelectric dams of Benmore Dam, Aviemore Dam and Waitaki Dam.

Geographic entities mentioned:
surface_form: Lake Waitaki
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.674722222222
lon: 170.39888888889
The river is the site of many hydroelectricity projects. The Waitaki Hydro Scheme, which includes several large dams, is one of the largest hydroelectric projects in the nation. The Waitaki dam was built first, between 1928 and 1934, and without earth-moving machinery, followed by the development of the Aviemore Dam, which created Lake Aviemore, and then Benmore Dam, which created Lake Benmore.

Geographic entities mentioned:
surface_form: Waitaki
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.674722222222
lon: 170.39888888889
surface_form: Lake Benmore
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.415
lon: 170.22055555556
The Waitaki dam was built first, between 1928 and 1934, and without earth-moving machinery, followed by the development of the Aviemore Dam, which created Lake Aviemore, and then Benmore Dam, which created Lake Benmore. Lake Pukaki was initially dammed at this stage to provide storage and flow control.

Geographic entities mentioned:
surface_form: Lake Pukaki
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.116666666667
lon: 170.16666666667
Lake Pukaki was initially dammed at this stage to provide storage and flow control. A small station was also installed on Lake Tekapo, with water taken through a tunnel to a power station below the level of the lake. The original Waitaki power stations discharge water back into the Waitaki River, which then forms a storage lake for the next station in the chain.

Geographic entities mentioned:
surface_form: Lake Tekapo
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.9
lon: 170.525
The dam at Pukaki was increased in height. Water from Pukaki is then transferred into the Pukaki Canal, which meets the Ohau Canal from Lake Ōhau into Ōhau A station and Lake Ruataniwha. The Ohau Canal continues beyond Lake Ruataniwha to Ōhau B midway along, before emptying through Ōhau C into Lake Benmore. Later proposals.

Geographic entities mentioned:
surface_form: Lake Ruataniwha
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.281
lon: 170.071
The dam at Pukaki was increased in height. Water from Pukaki is then transferred into the Pukaki Canal, which meets the Ohau Canal from Lake Ōhau into Ōhau A station and Lake Ruataniwha. The Ohau Canal continues beyond Lake Ruataniwha to Ōhau B midway along, before emptying through Ōhau C into Lake Benmore. Later proposals.

Geographic entities mentioned:
surface_form: Ruataniwha
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.281
lon: 170.071
Devick Lake (British Columbia). Devick Lake is a lake near Heffley Creek, British Columbia. History. It is named for Henri Louis Devick who came from Switzerland in 1904 to settle west of Heffley Creek, British Columbia. It is the source of Devick Creek.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: devick lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.90361
lon: -120.08139
Devick Lake (British Columbia). Devick Lake is a lake near Heffley Creek, British Columbia. History. It is named for Henri Louis Devick who came from Switzerland in 1904 to settle west of Heffley Creek, British Columbia. It is the source of Devick Creek.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Nigoglia. The Nigoglia (or;) is a short Italian river whose source is at the northern end of Lake Orta, of which it is the sole outflow. Its course of less than 2 kilometres passes in a northerly direction through the town of Omegna and into the Strona.

Geographic entities mentioned:
surface_form: Lake Orta
instance_of: Lake
countries: Italy
coordinates: lat: 45.8098
lon: 8.3963
Temple Mountain (Idaho). Temple Mountain was a summit in Boundary County, Idaho, United States. Temple Mountain was so named because its massive outline had the shape of a temple.

Geographic entities mentioned:
surface_form: temple mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.8275
lon: -71.885277777778
surface_form: temple mountain (idaho)
instance_of: Mountain
countries: United States
coordinates: lat: 48.738888888889
lon: -116.72055555556
surface_form: temple mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.688611111111
lon: -110.68194444444
Temple Mountain (Idaho). Temple Mountain was a summit in Boundary County, Idaho, United States. Temple Mountain was so named because its massive outline had the shape of a temple.

Geographic entities mentioned:
surface_form: temple mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.8275
lon: -71.885277777778
surface_form: temple mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.738888888889
lon: -116.72055555556
surface_form: temple mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.688611111111
lon: -110.68194444444
Planica 1949. Planica 1949 was an International ski jumping week with two competitions on a new K80 hill, held on 20 and 27 March 1949 in Planica, PR Slovenia, FPR Yugoslavia. Over 20,000 people were gathered. Competitions. On 19 March 1949, International Ski Jumping Week has officially started with premiere jumps on the new Srednja Bloudkova K80 normal hill.

Geographic entities mentioned:
surface_form: Planica
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.476944444444
lon: 13.722222222222
Relationship with Switzerland. Due to multiple attempts by the Cisalpine government to annex the Italian-speaking Swiss territories south of the Alps, relations with the Swiss Confederacy were strained. The Cisalpine Republic ended up taking control of Valtellina from the Three Leagues and Campione d'Italia and annexing them. A Cisalpine attempt to conquer Lugano by surprise failed in 1797.

Geographic entities mentioned:
surface_form: Valtellina
instance_of: Valley
countries: Italy
coordinates: lat: 46.166666666667
lon: 9.8666666666667
Janhukut. Janhukut (Hindi: जन्हुकुट) is a mountain of Garhwal Himalaya in Uttarakhand India. Janhukut standing majestically at 6805 meter. It's the 31st highest located entirely within the uttrakhand India. Nanda Devi, is the highest mountain in this category. Janhukut is the 473rd highest peak in the world. Climbing history.

Geographic entities mentioned:
surface_form: Nanda Devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
Janhukut. Janhukut (Hindi: जन्हुकुट) is a mountain of Garhwal Himalaya in Uttarakhand India. Janhukut standing majestically at 6805 meter. It's the 31st highest located entirely within the uttrakhand India. Nanda Devi, is the highest mountain in this category. Janhukut is the 473rd highest peak in the world. Climbing history.

Geographic entities mentioned:
surface_form: janhukut
instance_of: Mountain
countries: India
coordinates: lat: 30.772222222222
lon: 79.241666666667
Glaciers and rivers. On the eastern side of the Janhukut is Satopanth Bamak (Glacier) and on the west, Maiandi Bamak (Glacier). The southern end is flanked by Gangotri glacier and the northern by Bhagirathi Kharak glacier.

Geographic entities mentioned:
surface_form: janhukut
instance_of: Mountain
countries: India
coordinates: lat: 30.772222222222
lon: 79.241666666667
surface_form: satopanth
instance_of: Mountain
countries: India
coordinates: lat: 30.845844
lon: 79.21323
The southern end is flanked by Gangotri glacier and the northern by Bhagirathi Kharak glacier. From the Maiandi Bamak and Gangotri glaciers emerges Bhagirathi river and on the other side Satopanth Bamak and Bhagirathi kharak glacier, emerges Alaknanda river two main tributaries of Ganga. These two rivers meet at Devpryag, and from that confluence the two rivers form the headwater of the Ganga.

Geographic entities mentioned:
surface_form: satopanth
instance_of: Mountain
countries: India
coordinates: lat: 30.845844
lon: 79.21323
The entire surrounding area are protected within the Gangotri National Park, the largest conservation area in India. The Gangotri National Park is home to several world-class treks, including Gangotri Gomukh Tapoban, Kerdarnath Vasuki tal trek, Har ki dun valley trek and Badrinath to Satopanth tal trek.

Geographic entities mentioned:
surface_form: satopanth
instance_of: Mountain
countries: India
coordinates: lat: 30.845844
lon: 79.21323
The Mexican authorities had several follow-ups on Guzmán's whereabouts since previous months; through phone taps, they concluded that the drug lord was residing in the Toluca Valley.

Geographic entities mentioned:
surface_form: Toluca Valley
instance_of: Valley
countries: Mexico
coordinates: lat: 19.2865
lon: -99.5595
Habitat and distribution. &quot;Sarcogyne brunnea&quot; thrives in high-altitude, arid areas of the Andes. Its known habitats include the type locality in Bolivia at an elevation exceeding and a slope of the Cotopaxi volcano in Ecuador at. The lichen is usually found in sunny, exposed locations, growing on volcanic rock and soil.

Geographic entities mentioned:
surface_form: Cotopaxi
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.68055555555556
lon: -78.437777777778
Pammene ignorata. &quot;Pammene ignorata&quot; is a moth of the family Tortricidae. In Europe it is found in Great Britain, the Benelux, Fennoscandia, Switzerland, Austria, the Czech Republic, Hungary, Poland and the Baltic region, east to the eastern parts of the Palearctic realm. The wingspan is. Adults are on wing from May to July.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Ziegenkopf (Habichtswald). Ziegenkopf (Habichtswald) is a mountain of Hesse, Germany.

Geographic entities mentioned:
surface_form: ziegenkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 51.3079
lon: 9.36903
Niuatoputapu language. The Niuatoputapu languague (Tongan: &quot;Lea Faka-Niuatoputapu&quot;) was a Polynesian language and the indigenous language of the people of Niuatoputapu, Tonga and possibly Tafahi, Tonga due to its close proximity.

Geographic entities mentioned:
surface_form: Tafahi, Tonga
instance_of: Mountain
countries: Tonga
coordinates: lat: -15.852777777777778
lon: -173.74583333333334
The company was a former component of FTSE Italia Mid Cap Index of the Borsa Italiana (Milan Stock Exchange), but was removed and added as a component of Index in May 2017; the bank was added back to the reserve list of FTSE Italia Mid Cap in August 2017. The bank was named after the area Valtellina.

Geographic entities mentioned:
surface_form: Valtellina
instance_of: Valley
countries: Italy
coordinates: lat: 46.166666666667
lon: 9.8666666666667
Catfish Mountain. Catfish Mountain is a peak of the Kittatinny Mountains in Warren County, New Jersey, United States. The mountain stands in height. It lies along the Appalachian Trail in the Delaware Water Gap National Recreation Area. Catfish Pond is to the southwest; it is drained by Yards Creek, which flows through Catfish Pond Gap.

Geographic entities mentioned:
surface_form: catfish mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0475
lon: -74.9725
It has a subsidiary peak, Vasuki south. Vasuki Parbat stands majestically at 6792 meter and the south peak 6702 at meter. Its the 35th highest located entirely within the uttrakhand India. Nanda Devi, is the highest mountain in this category. Climbing history. Indo-Tibet Border Police claimed The first recorded ascent that took place in 1973.

Geographic entities mentioned:
surface_form: Nanda Devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
An attempt by a three-man team of Nigel Cleaver, Mark Evans and Ian Johnson in 1980. In October 2010, the four member British-New Zealand team made an alpine style ascent from the unclimbed west face, traverse of the main summit and descent from the northwest ridge. After establishing their base camp near the junction of Chaturangi and Vasuki Bamak at 4820 m, the attempt started on 3 October.

Geographic entities mentioned:
surface_form: chaturangi
instance_of: Mountain
countries: India
coordinates: lat: 30.93083333
lon: 79.20694444
Geography. It is surrounded by Glaciers on both side on the eastern side of the Vasuki Parbat is Sundar Bamak (Glacier),on the western side its Vasuki Glacier both the glacier in this area fed Chaturangi Glacier on the northern side. The entire Vasuki Parbat and surrounding area are protected within the Gangotri National Park, the largest conservation area in India.

Geographic entities mentioned:
surface_form: chaturangi
instance_of: Mountain
countries: India
coordinates: lat: 30.93083333
lon: 79.20694444
surface_form: vasuki parbat
instance_of: Mountain
countries: India
coordinates: lat: 30.875
lon: 79.175277777778
The Gangotri National Park is home to several world-class treks, including Gangotri Gomukh Tapoban, Kerdarnath Vasuki tal trek. Har ki dun valley trek
Glaciers and rivers. Vasuki Parbat is surrounded by the Vasuki Glacier on the west side and Sundar Bamak (Glacier) on the east side northern side is surrounded by Chaturangi Glacier both east and west merge with Chaturangi Glacier.

Geographic entities mentioned:
surface_form: chaturangi
instance_of: Mountain
countries: India
coordinates: lat: 30.93083333
lon: 79.20694444
surface_form: chaturangi
instance_of: Mountain
countries: India
coordinates: lat: 30.93083333
lon: 79.20694444
surface_form: vasuki parbat
instance_of: Mountain
countries: India
coordinates: lat: 30.875
lon: 79.175277777778
Vasuki Parbat is surrounded by the Vasuki Glacier on the west side and Sundar Bamak (Glacier) on the east side northern side is surrounded by Chaturangi Glacier both east and west merge with Chaturangi Glacier. Chaturangi Glacier merge with Gangotri Glacier from the snout of Gangotri Glacier emerges Bhagirathi river also called Ganga or Ganges after it meets Alaknanda at Devprayag.

Geographic entities mentioned:
surface_form: chaturangi
instance_of: Mountain
countries: India
coordinates: lat: 30.93083333
lon: 79.20694444
Vasuki Parbat. Vasuki Parbat or Vasuki Parvat (Hindi:वासुकी पर्वत) is a mountain range of Garhwal Himalaya in Vasuki Glacier Uttarakhand, India. It has a subsidiary peak, Vasuki south. Vasuki Parbat stands majestically at 6792 meter and the south peak 6702 at meter. Its the 35th highest located entirely within the uttrakhand India. Nanda Devi, is the highest mountain in this category.

Geographic entities mentioned:
surface_form: वासुकी पर्वत
instance_of: Mountain
countries: India
coordinates: lat: 30.875
lon: 79.175277777778
surface_form: vasuki parvat
instance_of: Mountain
countries: India
coordinates: lat: 30.875
lon: 79.175277777778
surface_form: vasuki parbat
instance_of: Mountain
countries: India
coordinates: lat: 30.875
lon: 79.175277777778
Vasuki Parbat. Vasuki Parbat or Vasuki Parvat (Hindi:वासुकी पर्वत) is a mountain range of Garhwal Himalaya in Vasuki Glacier Uttarakhand, India. It has a subsidiary peak, Vasuki south. Vasuki Parbat stands majestically at 6792 meter and the south peak 6702 at meter. Its the 35th highest located entirely within the uttrakhand India. Nanda Devi, is the highest mountain in this category.

Geographic entities mentioned:
surface_form: vasuki parbat
instance_of: Mountain
countries: India
coordinates: lat: 30.875
lon: 79.175277777778
However, the Indian Mountaineering Federation (IMF) does not recognize the ascent and the details of that climb have been kept secret. Vasuki Parbat was climbed by a Japanese team in 1980 summited for the second time via the east face, leading to the northeast ridge. An attempt by a two-man team of Mick Fowler and Paul Ramsden in 2008.

Geographic entities mentioned:
surface_form: vasuki parbat
instance_of: Mountain
countries: India
coordinates: lat: 30.875
lon: 79.175277777778
Geography. It is surrounded by Glaciers on both side on the eastern side of the Vasuki Parbat is Sundar Bamak (Glacier),on the western side its Vasuki Glacier both the glacier in this area fed Chaturangi Glacier on the northern side. The entire Vasuki Parbat and surrounding area are protected within the Gangotri National Park, the largest conservation area in India.

Geographic entities mentioned:
surface_form: vasuki parbat
instance_of: Mountain
countries: India
coordinates: lat: 30.875
lon: 79.175277777778
Lakisamni. The Lakisamni, or alternately Laquisimne, () are one of the divisions of the Yokuts people, indigenous to the Stanislaus River area in California. The Lakisamni probably inhabited the land in the San Joaquin Valley, from present-day Ripon in the west to Knights Ferry in the east.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Workers and hunters alike preferred the added mobility, especially in the steep slopes of the Eastern Alps. While the exact origin of this cut is uncertain, the first written account of its use was made by August Lewald during his tour of Tuxertal, Tyrol, Austria in 1835.

Geographic entities mentioned:
surface_form: Tuxertal
instance_of: Valley
countries: Austria
coordinates: lat: 47.1625
lon: 11.754166666667
Mount Kembar. Mount Kembar (, means: &quot;Twin Mountain&quot;) is a Pleistocene volcano, located in the northern Sumatra island, Indonesia. It contains a fumarole field, named Gayolesten. The volcanic complex is located in the junction of two geological fault systems and it is a shield volcano.

Geographic entities mentioned:
surface_form: mount kembar
instance_of: Mountain
countries: Indonesia
coordinates: lat: 3.85
lon: 97.664
surface_form: kembar
instance_of: Mountain
countries: Indonesia
coordinates: lat: 3.85
lon: 97.664
Governor James B. Ray led the negotiations. It allowed for a ribbon of land wide to stretch from the Ohio River (at Madison) to Lake Michigan (Michigan City). The Pottawatomie left the region by that very road when the last of their tribe was forcibly removed in the 1838 Pottawatomie Trail of Death. A commission was selected in 1828 to route the road from Indianapolis to Lake Michigan.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
The job came with a &quot;service flat&quot;, and the family accordingly lived on the factory premises. After completing his compulsory schooling Norbert Kaiser transferred to the &quot;Humanistische Gymnasium&quot; (secondary school) at Bruneck, along the Puster Valley. His school career was badly disrupted by serious kidney illness.

Geographic entities mentioned:
surface_form: Puster Valley
instance_of: Valley
countries: Italy
Austria
coordinates: lat: 46.7405
lon: 12.369555555555555
In 1966 he sat for but failed the Matura (schooling completion exam) which would have opened the way to university-level education. He now left the Puster Valley, relocating to Laas (Vinschgau), a small remote town near the Swiss frontier, some fifty miles to the west. The principal industry in Laas involved marble quarrying: here, during 1966/67, he took a teaching job at the local middle school.

Geographic entities mentioned:
surface_form: Puster Valley
instance_of: Valley
countries: Italy
Austria
coordinates: lat: 46.7405
lon: 12.369555555555555
surface_form: Vinschgau
instance_of: Valley
countries: Italy
coordinates: lat: 46.615
lon: 10.705
It is a renowned elephant and tiger reserve. The protected area encompasses, of which of the main zone was declared as the Periyar National Park in 1982. The park is a repository of rare, endemic, and endangered flora and fauna and forms the major watershed of two important rivers of Kerala: the Periyar and the Pamba.

Geographic entities mentioned:
surface_form: Pamba
instance_of: Watercourse
countries: India
coordinates: lat: 9.5
lon: 76.416666666667
Toward the west it expands into a high plateau. From this level the altitude drops steeply to the deepest point of the reserve, the 100 metre valley of the Pamba River. The highest peak in the park is the high Kottamala, the southernmost peak in India higher than. The Periyar and Pamba Rivers originate in the forests of the reserve, both in Mlappara.

Geographic entities mentioned:
surface_form: Pamba River
instance_of: Watercourse
countries: India
coordinates: lat: 9.5
lon: 76.416666666667
Toward the west it expands into a high plateau. From this level the altitude drops steeply to the deepest point of the reserve, the 100 metre valley of the Pamba River. The highest peak in the park is the high Kottamala, the southernmost peak in India higher than. The Periyar and Pamba Rivers originate in the forests of the reserve, both in Mlappara.

Geographic entities mentioned:
surface_form: Kottamala
instance_of: Mountain
countries: India
coordinates: lat: 9.521
lon: 77.402
The highest peak in the park is the high Kottamala, the southernmost peak in India higher than. The Periyar and Pamba Rivers originate in the forests of the reserve, both in Mlappara. The other prominent peaks within the park are Pachayarmala, Vellimala, Sunderamala, Chokkampetti mala and Karimala. The topography consists of steep and rolling hills which are thickly wooded.

Geographic entities mentioned:
surface_form: Pamba River
instance_of: Watercourse
countries: India
coordinates: lat: 9.5
lon: 76.416666666667
Luzoniella signifrons. &quot;Luzoniella signifrons&quot; is a species of &quot;conehead&quot; bush crickets or katydids, endemic to the Philippines. It is the only species in the genus &quot;Luzoniella&quot;: which is named after the northern island where the type locality, Mount Makiling is situated.

Geographic entities mentioned:
surface_form: Mount Makiling
instance_of: Mountain
countries: Philippines
coordinates: lat: 14.13
lon: 121.2
Bostrychus expatria. &quot;Bostrychus expatria&quot; is a species of freshwater fish in the family Butidae endemic to Lake Manguao on the island of Palawan in the Philippines. Anatomy and morphology. &quot;Bostrychus expatria&quot; is a small fish reaching a length of. They appear as standard members of their family, with non-hydrodynamically-shaped bodies typical of bottom-dwelling fish.

Geographic entities mentioned:
surface_form: Lake Manguao
instance_of: Lake
countries: Philippines
coordinates: lat: 10.766666666667
lon: 119.55
Its eyes are located dorsally, another trait commonly seen in benthic fish. Range and distribution. &quot;Bostrychus expatria&quot; has a single known population that can be found only in Lake Manguao in the Philippines. Lake Manguao is a freshwater lake located in the hilly areas in the northern part of the Philippine island of Palawan.

Geographic entities mentioned:
surface_form: Lake Manguao
instance_of: Lake
countries: Philippines
coordinates: lat: 10.766666666667
lon: 119.55
Wadi al-Kheder. The Wadi al-Kheder is a river in Syria. It a tributary of the Balikh River.

Geographic entities mentioned:
surface_form: wadi al-kheder
instance_of: Watercourse
countries: Syria
Bracan mac Máine Mór probably resided at Rathbracken townland to the north of Granard. His descendants, the &quot;, were defeated by the Cenél Coirpri in AD 751. Cairpre Gabra. Between the fifth and seventh centuries, a branch of the Uí Néill called the Cairpre Gabhra (- descendants of Coirpre mac Néill) settled around Granard and Lough Sheelin in North Tethbae (approximately county Longford).

Geographic entities mentioned:
surface_form: Lough Sheelin
instance_of: Lake
countries: Ireland
coordinates: lat: 53.8
lon: -7.3166666666667
With the construction of the Kichi Sipi Bridge, parts of PR 374 were paved and re-aligned to replace the old ferry. Route description. PR 374 begins at an intersection with PR 373 and a local road which connects to Whiskey Jack Landing on the shores of Kiskittogisu Lake. A two-lane gravel road, PR 374 runs northeast from PR 373 and makes a wide bend past a dirt road to nearby Cross Lake.

Geographic entities mentioned:
surface_form: Kiskittogisu Lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.2644
lon: -98.225
September arrives and, as usual, the protests on the anniversary of the coup d'état of 11 September 1973 increase. One day Carlos leaves a suspicious metal pipe at the Queen's house, and then invites her for a walk to Cajón del Maipo, where Augusto Pinochet and his wife, Lucía Hiriart, usually go to rest, accompanied by a strict military contingent.

Geographic entities mentioned:
surface_form: Cajón del Maipo
instance_of: Valley
countries: Chile
coordinates: lat: -33.633333333333
lon: -70.35
Fisk Lake. Fisk Lake is a freshwater lake in East Grand Rapids, Michigan, United States. It was named for John Fisk. Now primarily valued for scenic purposes, it was originally used as a source of ice for Grand Rapids, Michigan and the Chicago meatpacking industries. It receives water from Reeds Lake, and drains to the Grand River by way of Coldbrook Creek.

Geographic entities mentioned:
surface_form: Reeds Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.95
lon: -85.6
Fisk Lake. Fisk Lake is a freshwater lake in East Grand Rapids, Michigan, United States. It was named for John Fisk. Now primarily valued for scenic purposes, it was originally used as a source of ice for Grand Rapids, Michigan and the Chicago meatpacking industries. It receives water from Reeds Lake, and drains to the Grand River by way of Coldbrook Creek.

Geographic entities mentioned:
surface_form: michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: fisk lake
instance_of: Lake
countries: United States
coordinates: lat: 42.956204
lon: -85.619941
Fisk Lake. Fisk Lake is a freshwater lake in East Grand Rapids, Michigan, United States. It was named for John Fisk. Now primarily valued for scenic purposes, it was originally used as a source of ice for Grand Rapids, Michigan and the Chicago meatpacking industries. It receives water from Reeds Lake, and drains to the Grand River by way of Coldbrook Creek.

Geographic entities mentioned:
surface_form: michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Fisk Lake. Fisk Lake is a freshwater lake in East Grand Rapids, Michigan, United States. It was named for John Fisk. Now primarily valued for scenic purposes, it was originally used as a source of ice for Grand Rapids, Michigan and the Chicago meatpacking industries. It receives water from Reeds Lake, and drains to the Grand River by way of Coldbrook Creek.

Geographic entities mentioned:
surface_form: fisk lake
instance_of: Lake
countries: United States
coordinates: lat: 42.956204
lon: -85.619941
Rhinotropis heterorhyncha. &quot;Rhinotropis heterorhyncha&quot;, synonym &quot;Polygala heterorhyncha&quot;, is a species of flowering plant in the milkwort family known by the common names beaked spiny polygala and notch-beaked milkwort. It is native to southern Nevada and it is known from a few occurrences just over the border in the Funeral Mountains of California above Death Valley.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Fredensborg Palace. Fredensborg Palace (;) is a palace located on the eastern shore of Lake Esrum (Danish, &quot;Esrum Sø&quot;) in Fredensborg on the island of Zealand (&quot;Sjælland&quot;) in Denmark. It is the Danish royal family’s spring and autumn residence, and is often the site of important state visits and events in the royal family. It is the most used of the royal family’s residences.

Geographic entities mentioned:
surface_form: Lake Esrum
instance_of: Lake
countries: Denmark
coordinates: lat: 56.00778
lon: 12.37917
Their population is estimated at 157,787, with substantial fluent speakers. They migrated to Kenya from Uganda and settled on the two Lake Victoria islands of Rusinga and Mfangano, others also settled on the mainland areas including Gembe, Gwassi, Kaksingri of Suba South and Migori and are believed to be the last tribe to have settled in Kenya.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
These also exhibit minute longitudinal striation under a lens, with the striae being close-set, fine, and flexuous. The aperture is oval and rather large, with a thickened and elongated peristome that bears four equidistant, relatively small, digitate processes. Distribution. This marine species occurs from the Gulf of Aden and East Africa to Sumatra, Indonesia; also in the Bay of Bengal.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Dream Unlimited. Dream Unlimited Corporation is a Canadian real estate development company that is developing the Waterfront Toronto property on Lake Ontario. It manages $15 billion of real estate assets. History. Dream Unlimited was founded in 1994. In 2021, Dream Unlimited had $15 billion of assets under management, $9 billion of which are fee earning.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Swirl How. Swirl How is a fell in the English Lake District. It stands between Coniston and the Duddon Valley in the southern part of the District. It rivals the Old Man of Coniston as the highest point within the traditional County Palatine of Lancashire (it has been administered since 1974 as part of Cumbria for local government purposes).

Geographic entities mentioned:
surface_form: Duddon Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.297688888889
lon: -3.2347888888889
surface_form: duddon
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 54.4155
lon: -3.1156
Consequently, it also feeds the headwaters of four valleys. The ridge northward to Great Carrs is named Top of Broad Slack, Broad Slack being a ferociously steep grass slope climbing out of the Greenburn valley between neighbouring crags. The ridge is a grassy plateau with a pronounced downward tilt to the west. The eastern edge is precipitous, curving around the head of Greenburn.

Geographic entities mentioned:
surface_form: Great Carrs
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.3983
lon: -3.12438
An engine and propeller from the aircraft are preserved at the Ruskin Museum in Coniston. The tilted plateau of the north ridge is triangular in plan, narrowing to a point at Fairfield in the west. This is the col between Swirl How and the ridge's western outlier, Grey Friar. To the north of this ridge are long slopes leading down to the Duddon at Wrynose Bottom.

Geographic entities mentioned:
surface_form: Grey Friar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.392761111111
lon: -3.1427111111111
surface_form: grey friar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.392761111111
lon: -3.1427111111111
The main ridge continues southward, stepping down Great and Little How Crags to the depression of Levers Hawse. From here it rises again to Brim Fell with Dow Crag and The Old Man Of Coniston beyond. To the west of the Hawse is the valley of Tarn Head Beck, the main feeder of Seathwaite Tarn, a reservoir in a side valley of the Duddon system.

Geographic entities mentioned:
surface_form: Brim Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.3777
lon: -3.12381
surface_form: Dow Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.369438888889
lon: -3.1374388888889
surface_form: dow crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.369438888889
lon: -3.1374388888889
The dam is almost long and is concrete cored with slate buttresses, the resulting depth of the tarn being around. Water is not abstracted directly from the tarn, but flows some distance downriver to an off-take weir. To the east of Levers Hawse is Levers Water. This smaller tarn has also been raised by damming, but in this case the original user was the Coniston Copper Mines.

Geographic entities mentioned:
surface_form: Levers Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.384134
lon: -3.11098
The eastern arm of Swirl How leads down the stony slope of Prison Band to the depression at Swirl Hawse. From here it rises over the subsidiary top of Black Sails to the main summit of Wetherlam. Swirl Hawse Beck runs south from this ridge to feed Levers Water, whilst to the north of Wetherlam is Greenburn. Geology.

Geographic entities mentioned:
surface_form: Wetherlam
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.401
lon: -3.098
surface_form: wetherlam
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.401
lon: -3.098
Ascents. Direct ascents can be made via Levers Hawse to the south or Swirl Hawse to the east. Both can be gained from Coniston and Swirl Hawse is also a practicable objective from Little Langdale. The right of way shown up the western (Duddon) side of Levers Hawse does not exist as a path on the ground.

Geographic entities mentioned:
surface_form: Little Langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.419557
lon: -3.073825
surface_form: little langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.419557
lon: -3.073825
It stands between Coniston and the Duddon Valley in the southern part of the District. It rivals the Old Man of Coniston as the highest point within the traditional County Palatine of Lancashire (it has been administered since 1974 as part of Cumbria for local government purposes). The Coniston (or Furness) Fells form the watershed between Coniston Water and the Duddon valley to the west.

Geographic entities mentioned:
surface_form: duddon valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.297688888889
lon: -3.2347888888889
surface_form: coniston water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.35
lon: -3.0666666666667
surface_form: duddon
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 54.4155
lon: -3.1156
The Coniston (or Furness) Fells form the watershed between Coniston Water and the Duddon valley to the west. The range begins at Wrynose Pass and runs south for around before petering out at Broughton in Furness on the Duddon Estuary.

Geographic entities mentioned:
surface_form: duddon
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.297688888889
lon: -3.2347888888889
surface_form: duddon
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 54.4155
lon: -3.1156
The tilted plateau of the north ridge is triangular in plan, narrowing to a point at Fairfield in the west. This is the col between Swirl How and the ridge's western outlier, Grey Friar. To the north of this ridge are long slopes leading down to the Duddon at Wrynose Bottom. The main ridge continues southward, stepping down Great and Little How Crags to the depression of Levers Hawse.

Geographic entities mentioned:
surface_form: duddon
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.297688888889
lon: -3.2347888888889
surface_form: duddon
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 54.4155
lon: -3.1156
From here it rises again to Brim Fell with Dow Crag and The Old Man Of Coniston beyond. To the west of the Hawse is the valley of Tarn Head Beck, the main feeder of Seathwaite Tarn, a reservoir in a side valley of the Duddon system. This was originally a much smaller waterbody, but was dammed early in the 20th century to provide drinking water for the Barrow-in-Furness area.

Geographic entities mentioned:
surface_form: duddon
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.297688888889
lon: -3.2347888888889
surface_form: duddon
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 54.4155
lon: -3.1156
An engine and propeller from the aircraft are preserved at the Ruskin Museum in Coniston. The tilted plateau of the north ridge is triangular in plan, narrowing to a point at Fairfield in the west. This is the col between Swirl How and the ridge's western outlier, Grey Friar. To the north of this ridge are long slopes leading down to the Duddon at Wrynose Bottom.

Geographic entities mentioned:
surface_form: fairfield
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4969
lon: -2.99059