Sarmila/GeoWiki-Features huggingface dataset:
Loki and Thor later meet under unknown circumstances and become best friends. In 2011, Loki attends Thor's intergalactic party on Earth alongside his fellow Frost Giants, who vandalize Mount Rushmore. Loki accidentally prevents Jane Foster from contacting Thor when, due to his large Frost Giant fingers, he drops and breaks Thor's cell phone.

Geographic entities mentioned:
surface_form: Mount Rushmore
instance_of: Mountain
countries: United States
coordinates: lat: 43.878947222222
lon: -103.459825
During a Constituent Assembly debate, Singh rebuked the Nagas for seeking Independence. He pointed out that the situation in the Naga Hills might become very serious and dangerous soon. Along with others in the Interim Government, he had received a few telegraphs on the intention of the Nagas declaring independence.

Geographic entities mentioned:
surface_form: Naga Hills
instance_of: Mountain
countries: Myanmar
India
coordinates: lat: 26
lon: 95
Geography. Geologically, Faganeanea offers insights into the volcanic history of American Samoa. While no trachytic fragments have been identified in the Matafao breccia at Matafao Peak, whitish trachyte fragments are found in breccia blocks along Faganeanea's shore, suggesting material that may have slid down from the steep slopes of the Matafao volcanic cone.

Geographic entities mentioned:
surface_form: Matafao Peak
instance_of: Mountain
countries: United States
coordinates: lat: -14.29972
lon: -170.7025
Secondary inflows are: Loughborough Lake Creek, at the east, which flows into Hart Lake and then into Opinicon Lake; and Rock Lake Creek, at the southeast, arriving from Lower Rock Lake. The primary outflow, at the northeast, is over the control structures and lock at Davis Lock to Sand Lake. The canal eventually flows via the Cataraqui River to Lake Ontario. Recreation.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Secondary inflows are: Loughborough Lake Creek, at the east, which flows into Hart Lake and then into Opinicon Lake; and Rock Lake Creek, at the southeast, arriving from Lower Rock Lake. The primary outflow, at the northeast, is over the control structures and lock at Davis Lock to Sand Lake. The canal eventually flows via the Cataraqui River to Lake Ontario. Recreation.

Geographic entities mentioned:
surface_form: sand lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.56833
lon: -76.26139
surface_form: sand lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.625
lon: -79.1681
surface_form: sand lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.1
lon: -79.6833
The primary inflow is the Rideau Canal arriving, at the northwest, from Indian Lake over the control structures and lock at Chaffey's Lock, which gives its name to the tourist and cottage community located there. Secondary inflows are: Loughborough Lake Creek, at the east, which flows into Hart Lake and then into Opinicon Lake; and Rock Lake Creek, at the southeast, arriving from Lower Rock Lake.

Geographic entities mentioned:
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.4597
lon: -118.263
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.4597
lon: -118.263
surface_form: opinicon lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.559
lon: -76.328
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.833333333333336
lon: -78.66666666666667
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.833333333333336
lon: -78.66666666666667
surface_form: loughborough lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.44722222222222
lon: -76.4113888888889
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.16916667
lon: -99.24694444
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.16916667
lon: -99.24694444
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.77775
lon: -94.41457
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.77775
lon: -94.41457
Opinicon Lake. Opinicon Lake is a lake in South Frontenac, Frontenac County and Rideau Lakes, United Counties of Leeds and Grenville in Eastern Ontario, Canada. This shallow lake was formed when Colonel John By built the Rideau Canal. It also is part of the Great Lakes Basin. Hydrology.

Geographic entities mentioned:
surface_form: opinicon lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.559
lon: -76.328
The canal eventually flows via the Cataraqui River to Lake Ontario. Recreation. This lake is a popular fishing spot and location for cottagers., a restaurant and former historical resort, is located at Chaffey's Locks. is located at the west end of Opinicon Lake. Since 1958 Skycroft has been a sought after campground hosting visitors from all over the world wishing to explore the area. History.

Geographic entities mentioned:
surface_form: opinicon lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.559
lon: -76.328
is located at the west end of Opinicon Lake. Since 1958 Skycroft has been a sought after campground hosting visitors from all over the world wishing to explore the area. History. The Queen's University Biological Station, built in 1945, is on the lake. In 2010, the James H. Fullard Nature Reserve was created, situated on Sugarbush Island.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
In 2018, Woods scored what he described as &quot;the best result of my career&quot; by finishing second in the Liège–Bastogne–Liège race. In September 2018, Woods won Stage 17 of the Vuelta a España, which finished up a steep climb to Balcón de Bizkaia. On 30 September, Woods finished third in the road race at the UCI Road World Championships in Innsbruck, Austria.

Geographic entities mentioned:
surface_form: Balcón de Bizkaia
instance_of: Mountain
countries: Spain
coordinates: lat: 43.228669444444
lon: -2.5900361111111
In August 2020, it was announced that Woods was to join from the 2021 season, on a three-year contract. He represented Canada at the 2020 Summer Olympics and finished in fifth place in the men's individual road race. In 2023, Woods won stage 9 of the Tour de France with a climb on the Puy de Dôme, making up over 1 minute in the last few kilometres to win the race.

Geographic entities mentioned:
surface_form: Puy de Dôme
instance_of: Mountain
countries: France
coordinates: lat: 45.772
lon: 2.9624
Mount Jervois. Mount Jervois is a mountain in New Zealand. Description. Mount Jervois is set on the crest or Main Divide of the Southern Alps and is situated on the boundary shared by the West Coast and Canterbury Regions of the South Island. This peak is located northeast of Mount Cook and set on the boundary shared by Mount Cook National Park and Westland Tai Poutini National Park.

Geographic entities mentioned:
surface_form: Mount Cook
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.595
lon: 170.14194444444445
surface_form: mount cook
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.595
lon: 170.14194444444445
Topographic relief is significant as the summit rises above the Rudolf Glacier in one kilometre, and above the Tasman Glacier in four kilometres. The Centennial Hut is perched on the northwest ridge of this peak. Mount Jervois was named by Robert von Lendenfeld to honour the then-Governor of New Zealand, William Jervois, who served in that role from 1883 to 1889. Climbing.

Geographic entities mentioned:
surface_form: lendenfeld
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.56
lon: 170.17
surface_form: mount jervois
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.513
lon: 170.238
Mount Jervois. Mount Jervois is a mountain in New Zealand. Description. Mount Jervois is set on the crest or Main Divide of the Southern Alps and is situated on the boundary shared by the West Coast and Canterbury Regions of the South Island. This peak is located northeast of Mount Cook and set on the boundary shared by Mount Cook National Park and Westland Tai Poutini National Park.

Geographic entities mentioned:
surface_form: mount jervois
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.513
lon: 170.238
Marsden. Climate. Based on the Köppen climate classification, Mount Jervois is located in a marine west coast (Cfb) climate zone, with a subpolar oceanic climate (Cfc) at the summit. Prevailing westerly winds blow moist air from the Tasman Sea onto the mountains, where the air is forced upwards by the mountains (orographic lift), causing moisture to drop in the form of rain or snow.

Geographic entities mentioned:
surface_form: mount jervois
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.513
lon: 170.238
Geology. Star Carr now lies under farmland at the eastern end of the Vale of Pickering. During the Mesolithic, the site was near the outflow at the western end of a palaeolake, known as Lake Flixton. At the end of the last ice age, a combination of glacial and post-glacial geomorphology caused the area to drain to the west (away from the shortest-distance to the North Sea at Filey).

Geographic entities mentioned:
surface_form: Vale of Pickering
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.2
lon: -0.7
Hailan River. The Hailan River (,) is a tributary of the Buerhatong River in east Jilin province of China. The source of river is located in Helong and flows generally from southwest to northeast across Longjing City and joins Buerhatong River at east of Yanji City.The river has a length of 145 km and drains an area of 2,934 square km.

Geographic entities mentioned:
surface_form: hailan river
instance_of: Watercourse
countries: People's Republic of China
coordinates: lat: 42.90861
lon: 129.61833
Ikongo. Ikongo (formerly: &quot;Fort Canot&quot;) is a town in the region of Fitovinany eastern Madagascar. It is approximately 90 km south-east of the provincial capital Fianarantsoa. It has a population of 36,684 inhabitants. Rivers. The town lies at the Sandrananta River. Roads. Ikongo is situated on the unpaved National Road 14 between Ifanadiana and Vohipeno.

Geographic entities mentioned:
surface_form: Sandrananta River
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -22.4315
lon: 47.9106
Area overview. Giridih district is a part of the Chota Nagpur plateau, with rocky soil and extensive forests. Most of the rivers in the district flow from the west to east, except in the northern portion where the rivers flow north and north west. The Pareshnath Hill rises to a height of. The district has coal and mica mines.

Geographic entities mentioned:
surface_form: Chota Nagpur plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
The stratigraphy of the formation was most recently revised in a 1971 study. A stratigraphic column at the Mount Bonnell location starts with the Lower Cretaceous Trinity Group overlain by the Edwards Group. Upper Cretaceous formations follow, starting with the Del Rio Clay, Buda Limestone, and then the Eagle Ford Group.

Geographic entities mentioned:
surface_form: Mount Bonnell
instance_of: Mountain
countries: United States
coordinates: lat: 30.321084
lon: -97.773566
Schönborn, Donnersbergkreis. Schönborn is a municipality in the Donnersbergkreis district, in Rhineland-Palatinate, Germany. Geography. The village is located in the North Palatine Uplands, west of the Donnersberg mountain. The nearest bigger cities are Bad Kreuznach and Kaiserslautern. History.

Geographic entities mentioned:
surface_form: Donnersberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.625280555556
lon: 7.9147194444444
Nicholl Head. 8zmyluvep5n2gvnp9iin5q11jwcp" xml:space="preserve">Nicholl Head () is a bold west extremity of the ridge separating Dogs Leg Fjord and Square Bay, on the west coast of Graham Land, Antarctica. First surveyed in 1936 by the British Graham Land Expedition (BGLE) under Rymill. Resurveyed in 1948 by the Falkland Islands Dependencies Survey (FIDS) and named for Timothy M.

Geographic entities mentioned:
surface_form: nicholl head
instance_of: Landform
coordinates: lat: -67.7833
lon: -67.1
This river separates the range from the Gurans Himal to the south and the eastern Kumaon to the southwest. To the east, the pass known as Lapche La marks the dividing point between the Nalakankar Himal and the Chandi Himal. To the north and northwest, the range gradually transitions into the northern foothills of the Himalayas and the Tibetan Plateau.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
To the north and northwest, the range gradually transitions into the northern foothills of the Himalayas and the Tibetan Plateau. The range has only three named peaks, of which only one is over 7,000 meters (22,966 feet), namely Gurla Mandhata, or Naimona'nyi, which stands at 7,694 meters(25,242 feet).

Geographic entities mentioned:
surface_form: Gurla Mandhata
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 30.438333333333
lon: 81.299166666667
It is located on the River Boyle, between Boyle and Carrick-on-Shannon near Lough Key Forest Park in the north of the county. Cootehall lies 4 kilometres off the N4 road from Dublin to Sligo and between the R284 and R285 regional roads. The Boyle River, which flows through Cootehall, connects the village with Lough Key to the west and the River Shannon to the east. History.

Geographic entities mentioned:
surface_form: Lough Key
instance_of: Lake
countries: Ireland
coordinates: lat: 54
lon: -8.25
Houghton won gold medals in the 2004 World Rowing Cups at both Lake Malta Poznań, Poland and Rotsee Lucerne, Switzerland, partnered by Alison Mowbray, Debbie Flood and Rebecca Romero – the first British women's quad to beat the Germans in this event. At the Athens Olympic games she won a silver medal in the quadruple sculls, beaten by the German boat.

Geographic entities mentioned:
surface_form: Rotsee
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.069722222222
lon: 8.3141666666667
She retired in Dease Lake, at the boundary between Yukon and British Columbia. Ford's association with the Sherpas stemmed from a 1979 conversation with the New Zealand mountaineer Edmund Hillary who was the first to ascend Mount Everest with his climbing partner Tenzing Norgay.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
The river then turns sharply southwards to form the border between Shanxi and Shaanxi, turns eastwards at its confluence with the Wei River, and flows across the North China Plain before emptying into the Bohai Sea. The river is named for the yellow color of its water, which comes from the large amount of sediment discharged into the water as the river flows through the Loess Plateau.

Geographic entities mentioned:
surface_form: Loess Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Etymology. When the Yellow River was still somewhat clear, it was simply referred to as 'the river' (, Old Chinese:). Observations made at the Yumenkou gorge, where the river leaves the modern Loess Plateau, indicated the river changed to muddy sometime between 367 BC and 165 AD, according to chronicles' records.

Geographic entities mentioned:
surface_form: Loess Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
The Tibetan name is &quot;River of the Peacock&quot; (;). Geology. The Yellow River first formed sometime during the Late Miocene, Pliocene or Pleistocene, as a result of the Tibetan Plateau being uplifted. Dynamics. The river has long been critical to the development of northern China, and is regarded by scholars as a cradle of civilization.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
The cause of the floods is the large amount of fine-grained loess carried by the river from the Loess Plateau, which is continuously deposited along the bottom of its channel. The sedimentation causes natural dams to slowly accumulate. These subaqueous dams are unpredictable and generally undetectable.

Geographic entities mentioned:
surface_form: Loess Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
By 1194, the mouth of the Huai had been blocked. The buildup of silt deposits was such that even after the Yellow River later shifted its course, the Huai could no longer flow along its historic course, but instead, its water pools into Hongze Lake and then runs southward toward the Yangtze River. A flood in 1344 returned the Yellow River south of Shandong.

Geographic entities mentioned:
surface_form: Hongze Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 33.3075
lon: 118.71
Its total drainage area is about. According to the China Exploration and Research Society, the source of the Yellow River is at in the Bayan Har Mountains near the eastern edge of the Yushu Tibetan Autonomous Prefecture. The source tributaries drain into Gyaring Lake and Ngoring Lake on the western edge of Golog Prefecture high in the Bayan Har Mountains of Qinghai.

Geographic entities mentioned:
surface_form: Gyaring Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 34.91666667
lon: 97.26666667
surface_form: Ngoring Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 34.9
lon: 97.7
The current mouth of the Yellow River is located at Kenli County, Shandong. The river is commonly divided into three stages. These are roughly the northeast of the mountainous Tibetan Plateau, the Ordos Loop and Loess Plateau, and the North China Plain. However, different scholars have different opinions on how the three stages are divided.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
surface_form: Loess Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
This segment has a total length of and total basin area of, 51.4% of the total basin area. Along this length, the elevation of the Yellow River drops, with an average grade of 0.10%. The source section flows mainly through pastures, swamps, and knolls between the Bayan Har Mountains, and the Anemaqen (Amne Machin) Mountains in Qinghai. The river water is clear and flows steadily.

Geographic entities mentioned:
surface_form: Amne Machin
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 34.798333333333
lon: 99.4625
The middle reaches contribute 92% of the river's silts. The middle stream of the Yellow River passes through the Loess Plateau, where substantial erosion takes place. The large amount of mud and sand discharged into the river makes the Yellow River the most sediment-laden river in the world. The highest recorded annual level of silts discharged into the Yellow River is 3.91 billion tons in 1933.

Geographic entities mentioned:
surface_form: Loess Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Tributaries. The lower reaches of the Yellow River have no tributaries. Characteristics. The Yellow River is notable for the large amount of silt it carries—1.6 billion tons annually at the point where it descends from the Loess Plateau. If it is running to the sea with sufficient volume, 1.4 billion tons are carried to the sea per year.

Geographic entities mentioned:
surface_form: Loess Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Sideridis reticulata. &quot;Sideridis reticulata&quot;, commonly known as the bordered Gothic, is a moth of the family Noctuidae. It is found in the Palearctic realm, from the Iberian Peninsula throughout Europe and the temperate regions of Central Asia and the Russian Far East. In the north it occurs in Fennoscandia south of the Arctic Circle. In the south it ranges to the Mediterranean.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Pok To Yan (, literally &quot;Thin Razor's Edge&quot;), is a mountain on Lantau Island, Hong Kong, with a height of above sea level. Geology. Pok To Yan is formed by Volcanic rocks, much like many of the tallest mountains on Lantau Island, such as Lantau Peak. Flora. Pok To Yan and neighbouring Por Kai Shan were designated together a &quot;Site of Special Scientific Interest&quot; in 1994.

Geographic entities mentioned:
surface_form: Lantau Peak
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.245
lon: 113.917
surface_form: pok to yan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.2813
lon: 113.9557
surface_form: lantau peak
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.245
lon: 113.917
surface_form: lantau
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.245
lon: 113.917
Flora. Pok To Yan and neighbouring Por Kai Shan were designated together a &quot;Site of Special Scientific Interest&quot; in 1994. According to the local government, Pok To Yan has &quot;over 200 species of native plants.&quot; and &quot;a number of rare and protected indigenous plants&quot;. Geography. To the northwest is Tung Chung, while to the south is Sunset Peak.

Geographic entities mentioned:
surface_form: Por Kai Shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.28656
lon: 113.96023
surface_form: por kai shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.28656
lon: 113.96023
surface_form: kai shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.45837
lon: 114.01626
Flora. Pok To Yan and neighbouring Por Kai Shan were designated together a &quot;Site of Special Scientific Interest&quot; in 1994. According to the local government, Pok To Yan has &quot;over 200 species of native plants.&quot; and &quot;a number of rare and protected indigenous plants&quot;. Geography. To the northwest is Tung Chung, while to the south is Sunset Peak.

Geographic entities mentioned:
surface_form: sunset peak
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.2583
lon: 113.956
Pok To Yan. Pok To Yan (, literally &quot;Thin Razor's Edge&quot;), is a mountain on Lantau Island, Hong Kong, with a height of above sea level. Geology. Pok To Yan is formed by Volcanic rocks, much like many of the tallest mountains on Lantau Island, such as Lantau Peak. Flora.

Geographic entities mentioned:
surface_form: pok to yan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.2813
lon: 113.9557
Pok To Yan. Pok To Yan (, literally &quot;Thin Razor's Edge&quot;), is a mountain on Lantau Island, Hong Kong, with a height of above sea level. Geology. Pok To Yan is formed by Volcanic rocks, much like many of the tallest mountains on Lantau Island, such as Lantau Peak. Flora.

Geographic entities mentioned:
surface_form: pok to yan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.2813
lon: 113.9557
surface_form: lantau
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.245
lon: 113.917
Flora. Pok To Yan and neighbouring Por Kai Shan were designated together a &quot;Site of Special Scientific Interest&quot; in 1994. According to the local government, Pok To Yan has &quot;over 200 species of native plants.&quot; and &quot;a number of rare and protected indigenous plants&quot;. Geography. To the northwest is Tung Chung, while to the south is Sunset Peak.

Geographic entities mentioned:
surface_form: pok to yan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.2813
lon: 113.9557
Lac St. Cyr (Alberta). Lac St. Cyr is a lake in the County of St. Paul No. 19, Alberta. The lake is near the town of St. Paul and since 1951 has been used as a source of water. In 1978, seasonal pumping of water from the North Saskatchewan River into the lake was begun to address a fall in the water level.

Geographic entities mentioned:
surface_form: lac st. cyr
instance_of: Lake
countries: Canada
coordinates: lat: 53.896
lon: -111.193
Llwynmawr. Llwynmawr () is a village in the Ceiriog Valley in North Wales, about halfway between the villages of Glyn Ceiriog and Pontfadog, in the community of Glyntraian. The name means &quot;big grove&quot;.

Geographic entities mentioned:
surface_form: Ceiriog Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 52.915
lon: -3.197
List of crossings of the Connecticut River. This is a list of bridges and other crossings of the Connecticut River from its mouth at Long Island Sound upstream to its source at the Connecticut Lakes. The list includes current road and rail crossings, as well as ferries carrying a state highway across the river. Some pedestrian bridges and abandoned bridges are also listed.

Geographic entities mentioned:
surface_form: Connecticut Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 45.0936
lon: -71.2478
Muqu Wasi. Muqu Wasi (Quechua &quot;muqu&quot; hill, &quot;wasi&quot; house, &quot;hill house&quot;, Hispanicized spelling &quot;Mojo Huasi&quot;) is a mountain in the Andes of Peru, about high. It is situated in the Ayacucho Region, Cangallo Province, Totos District, northeast of Totos. Muqu Wasi lies west of Kiswara, east of Huch'uy Puka Q'asa and southeast of Chawpi Urqu.

Geographic entities mentioned:
surface_form: Kiswara
instance_of: Mountain
countries: Peru
coordinates: lat: -13.5525
lon: -74.4558
surface_form: Huch'uy Puka Q'asa
instance_of: Mountain
countries: Peru
coordinates: lat: -13.555
lon: -74.4886
surface_form: puka q'asa
instance_of: Mountain
countries: Peru
coordinates: lat: -13.18805556
lon: -74.99861111
surface_form: chawpi urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -12.47166667
lon: -74.58277778
surface_form: puka q'asa
instance_of: Mountain
countries: Peru
coordinates: lat: -13.20805556
lon: -72.08361111
surface_form: puka q'asa
instance_of: Mountain
countries: Peru
coordinates: lat: -12.9575
lon: -75.1725
surface_form: chawpi urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.9356
lon: -74.5178
surface_form: puka q'asa
instance_of: Mountain
countries: Peru
coordinates: lat: -12.7947
lon: -75.1794
surface_form: chawpi urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.5408
lon: -74.4928
surface_form: huch'uy puka q'asa
instance_of: Mountain
countries: Peru
coordinates: lat: -13.555
lon: -74.4886
surface_form: puka q'asa
instance_of: Mountain
countries: Peru
coordinates: lat: -13.1242
lon: -74.7719
surface_form: puka
instance_of: Mountain
countries: Peru
coordinates: lat: -12.6339
lon: -75.5692
Muqu Wasi. Muqu Wasi (Quechua &quot;muqu&quot; hill, &quot;wasi&quot; house, &quot;hill house&quot;, Hispanicized spelling &quot;Mojo Huasi&quot;) is a mountain in the Andes of Peru, about high. It is situated in the Ayacucho Region, Cangallo Province, Totos District, northeast of Totos. Muqu Wasi lies west of Kiswara, east of Huch'uy Puka Q'asa and southeast of Chawpi Urqu.

Geographic entities mentioned:
surface_form: muqu wasi
instance_of: Mountain
countries: Peru
coordinates: lat: -13.5544
lon: -74.4725
Muqu Wasi. Muqu Wasi (Quechua &quot;muqu&quot; hill, &quot;wasi&quot; house, &quot;hill house&quot;, Hispanicized spelling &quot;Mojo Huasi&quot;) is a mountain in the Andes of Peru, about high. It is situated in the Ayacucho Region, Cangallo Province, Totos District, northeast of Totos. Muqu Wasi lies west of Kiswara, east of Huch'uy Puka Q'asa and southeast of Chawpi Urqu.

Geographic entities mentioned:
surface_form: muqu wasi
instance_of: Mountain
countries: Peru
coordinates: lat: -13.5544
lon: -74.4725
surface_form: mojo huasi
instance_of: Mountain
countries: Peru
coordinates: lat: -13.5544
lon: -74.4725
Life. Sady Zañartu was born in the town of Taltal, Chile, the younger of two sons. His parents, Víctor Zañartu de la Cruz and Edelmira Bustos Frías, were farmers in the Copiapó Valley who also worked for a good part of their lives as miners. When he was very young, he moved to Santiago to study at the Internado Nacional Barros Arana, the Instituto de Aplicación, and the Instituto Nacional.

Geographic entities mentioned:
surface_form: Copiapó Valley
instance_of: Valley
countries: Chile
M. King in command. The wooden stern-wheel steamer departed Cairo that day for patrol duty in the Tennessee River, supporting Union Army efforts and protecting Federal positions in the Tennessee Valley from Confederate Cavalry raids. Frequently, as she patrolled the river and escorted transports and supply ships, her guns engaged hit-and-run batteries and bands of riflemen.

Geographic entities mentioned:
surface_form: Tennessee Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.959166666667
lon: -83.850277777778
Viinijärvi. Viinijärvi is a lake in Northern Karelia region in Finland and the 36th largest lake in Finland. It is connected to the Vuoksi main catchment area. The municipalities of Polvijärvi, Outokumpu and Liperi are in the area.

Geographic entities mentioned:
surface_form: viinijärvi
instance_of: Lake
countries: Finland
coordinates: lat: 62.73333333
lon: 29.28333333
Anne Hov. Anne Hov (&ndash;) was a Norwegian farm wife from Gudbrandsdalen. She has been credited with developing the modern version of the cheese brunost. Biography. Anne Olsdatter, the daughter of Ola Kvålen and Kari Olsdatter, was raised on the Solbrå (&quot;Solbråsetra&quot;) farm in the parish of Nord-Fron in the valley of Gudbrandsdalen in Christians amt (county).

Geographic entities mentioned:
surface_form: Gudbrandsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.1333
lon: 10.35
Biography. Anne Olsdatter, the daughter of Ola Kvålen and Kari Olsdatter, was raised on the Solbrå (&quot;Solbråsetra&quot;) farm in the parish of Nord-Fron in the valley of Gudbrandsdalen in Christians amt (county). Traditionally brunost was made on farms throughout Norway by boiling whey without the addition of milk or cream. This became a sugar rich, lean product.

Geographic entities mentioned:
surface_form: Gudbrandsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.1333
lon: 10.35
Terfens. Terfens is a municipality in the Schwaz district with 2116 inhabitants in the Austrian state of Tyrol. It is located about 20 km northeast of Innsbruck in the Lower Inn Valley. Geography. Terfens lies in the Lower Inn Valley 20 km east of Innsbruck. The Inn forms the southern municipal boundary. On the north and east, the boundary is the brook of Vomperbach, which flows into the Inn.

Geographic entities mentioned:
surface_form: Lower Inn Valley
instance_of: Valley
countries: Austria
coordinates: lat: 47.45777778
lon: 11.94555556
Geography. Terfens lies in the Lower Inn Valley 20 km east of Innsbruck. The Inn forms the southern municipal boundary. On the north and east, the boundary is the brook of Vomperbach, which flows into the Inn. Between the two is the small lake Weißlahnsee. Heraldry. The arms were granted on September 3, 1974. The name is derived from a Celtic word for oak or acorn.

Geographic entities mentioned:
surface_form: Weißlahnsee
instance_of: Lake
countries: Austria
coordinates: lat: 47.322
lon: 11.6564
Lhatu Dhura is a mountain of the Garhwal Himalaya in Uttarakhand, India. It is situated in the eastern rim of the Nanda Devi Sanctuary, on the watershed of the Milam Glacier and the Nanda Devi basin. The elevation of Lhatu Dhura is and its prominence is. It is joint 103rd highest mountain located entirely within Uttrakhand (Nanda Devi is the highest mountain). It lies 4.6 km south of Sakram.

Geographic entities mentioned:
surface_form: Nanda Devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
The elevation of Lhatu Dhura is and its prominence is. It is joint 103rd highest mountain located entirely within Uttrakhand (Nanda Devi is the highest mountain). It lies 4.6 km south of Sakram. Its nearest higher neighbor Nanda Devi East () lies 4.5 km to the south west, and Deo Damla () lies 7.7 km to the north; it is 6.1 km east-north-east of Nanda Devi (), and 9.5 km south of Mangraon ().

Geographic entities mentioned:
surface_form: Sakram
instance_of: Mountain
countries: India
coordinates: lat: 30.432777777777776
lon: 80.03416666666666
It is joint 103rd highest mountain located entirely within Uttrakhand (Nanda Devi is the highest mountain). It lies 4.6 km south of Sakram. Its nearest higher neighbor Nanda Devi East () lies 4.5 km to the south west, and Deo Damla () lies 7.7 km to the north; it is 6.1 km east-north-east of Nanda Devi (), and 9.5 km south of Mangraon (). Glaciers and rivers.

Geographic entities mentioned:
surface_form: Deo Damla
instance_of: Mountain
countries: India
coordinates: lat: 30.46
lon: 80.01916666666666
surface_form: Nanda Devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
surface_form: Mangraon
instance_of: Mountain
countries: India
coordinates: lat: 30.475277777777777
lon: 80.0111111111111
surface_form: nanda devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
Lhatu Dhura. Lhatu Dhura is a mountain of the Garhwal Himalaya in Uttarakhand, India. It is situated in the eastern rim of the Nanda Devi Sanctuary, on the watershed of the Milam Glacier and the Nanda Devi basin. The elevation of Lhatu Dhura is and its prominence is. It is joint 103rd highest mountain located entirely within Uttrakhand (Nanda Devi is the highest mountain).

Geographic entities mentioned:
surface_form: nanda devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
surface_form: nanda devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
Goriganga River emerges from the snout of Milam glacier that later joins the Kali River at Jauljibi. On the western side Uttari Nanda Devi Glacier flows down north and joins Uttari Rishi Glacier from the snout of Uttari Rishi Glacier emerges Rish Ganga. Rishi Ganga met with Dhauliganga River near Rini. Later Dhauli ganga met with Alaknanda at Vishnuprayag.

Geographic entities mentioned:
surface_form: nanda devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
Lhatu Dhura. Lhatu Dhura is a mountain of the Garhwal Himalaya in Uttarakhand, India. It is situated in the eastern rim of the Nanda Devi Sanctuary, on the watershed of the Milam Glacier and the Nanda Devi basin. The elevation of Lhatu Dhura is and its prominence is. It is joint 103rd highest mountain located entirely within Uttrakhand (Nanda Devi is the highest mountain).

Geographic entities mentioned:
surface_form: lhatu dhura
instance_of: Mountain
countries: India
coordinates: lat: 30.39138888888889
lon: 80.03027777777778
Lhatu Dhura is a mountain of the Garhwal Himalaya in Uttarakhand, India. It is situated in the eastern rim of the Nanda Devi Sanctuary, on the watershed of the Milam Glacier and the Nanda Devi basin. The elevation of Lhatu Dhura is and its prominence is. It is joint 103rd highest mountain located entirely within Uttrakhand (Nanda Devi is the highest mountain). It lies 4.6 km south of Sakram.

Geographic entities mentioned:
surface_form: lhatu dhura
instance_of: Mountain
countries: India
coordinates: lat: 30.39138888888889
lon: 80.03027777777778
Glaciers and rivers. Lhatu Dhura stands at the head of the western side of Timphu Glacier and between Timphu glacier and Pachhu Glacier. Both the glacier flows down from west to east and the streams emerges from these glacier Timphu Gad and Pachhu Gad joins Goriganga River. Goriganga River emerges from the snout of Milam glacier that later joins the Kali River at Jauljibi.

Geographic entities mentioned:
surface_form: lhatu dhura
instance_of: Mountain
countries: India
coordinates: lat: 30.39138888888889
lon: 80.03027777777778
All places marked in the map are linked in the larger full screen map. History. In Mahajanpada period, Probably the Chotanagpur was under sub-ordination of Mahapadma Nanda. In Maurya period, it is also said that the entire Chhotanagpur was under the subordination of Ashoka. There are symbolic relies of Buddha period in the temple of Gola. Probably in 8th Century B.C.

Geographic entities mentioned:
surface_form: Chotanagpur
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
Gilkey Memorial. The Gilkey Memorial is a memorial and cenotaph for those who have died while climbing K2. The memorial is named after Art Gilkey who died on the mountain in 1953. The memorial is a stone cairn covered with metal plaques. Each plaque is inscribed with details about the dead climber, such as when they went missing or were found dead.

Geographic entities mentioned:
surface_form: K2
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
Six Mile Creek (Ithaca). Six Mile Creek is a creek in Tompkins County, New York. It originates in the Town of Dryden near the intersection of Irish Settlement Road (Tompkins County Highway 162A) and Card Road and drains into Cayuga Inlet, which flows into Cayuga Lake. Its watershed is the principal source of drinking water for the City of Ithaca, New York, and the surrounding communities.

Geographic entities mentioned:
surface_form: Cayuga Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.68805555555556
lon: -76.70222222222222
Balsam Cap. Balsam Cap is a mountain located in Ulster County, New York. The mountain is part of the Catskill Mountains. Balsam Cap is flanked to the north by Friday Mountain, and to the southwest by Rocky Mountain. The northeast and southeast slopes of Balsam Cap drain into Maltby Hollow Brook, thence into Bush Kill, the Ashokan Reservoir, Esopus Creek, the Hudson River, and into New York Bay.

Geographic entities mentioned:
surface_form: Friday Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.987591666667
lon: -74.362094444444
surface_form: rocky mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9727
lon: -74.3732
surface_form: rocky mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.7955
lon: -79.1808
surface_form: rocky mountain
instance_of: Landform
countries: United States
coordinates: lat: 41.7958
lon: -71.055
surface_form: balsam cap
instance_of: Mountain
countries: United States
coordinates: lat: 41.977036111111
lon: -74.357372222222
surface_form: rocky mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0918
lon: -74.2151
Balsam Cap. Balsam Cap is a mountain located in Ulster County, New York. The mountain is part of the Catskill Mountains. Balsam Cap is flanked to the north by Friday Mountain, and to the southwest by Rocky Mountain. The northeast and southeast slopes of Balsam Cap drain into Maltby Hollow Brook, thence into Bush Kill, the Ashokan Reservoir, Esopus Creek, the Hudson River, and into New York Bay.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: balsam cap
instance_of: Mountain
countries: United States
coordinates: lat: 41.977036111111
lon: -74.357372222222
The southwest side of Balsam Cap drains into the headwaters of Rondout Creek, thence into the Hudson River. The northwest side of Balsam Cap drains into the East Branch of the Neversink River, the Delaware River, and into Delaware Bay. Balsam Cap is within the Slide Mountain Wilderness of New York's Catskill State Park.

Geographic entities mentioned:
surface_form: slide mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9986
lon: -74.3864
surface_form: slide mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.3127
lon: -119.884
surface_form: balsam cap
instance_of: Mountain
countries: United States
coordinates: lat: 41.977036111111
lon: -74.357372222222
Balsam Cap. Balsam Cap is a mountain located in Ulster County, New York. The mountain is part of the Catskill Mountains. Balsam Cap is flanked to the north by Friday Mountain, and to the southwest by Rocky Mountain. The northeast and southeast slopes of Balsam Cap drain into Maltby Hollow Brook, thence into Bush Kill, the Ashokan Reservoir, Esopus Creek, the Hudson River, and into New York Bay.

Geographic entities mentioned:
surface_form: balsam cap
instance_of: Mountain
countries: United States
coordinates: lat: 41.977036111111
lon: -74.357372222222
Balsam Cap is flanked to the north by Friday Mountain, and to the southwest by Rocky Mountain. The northeast and southeast slopes of Balsam Cap drain into Maltby Hollow Brook, thence into Bush Kill, the Ashokan Reservoir, Esopus Creek, the Hudson River, and into New York Bay. The southwest side of Balsam Cap drains into the headwaters of Rondout Creek, thence into the Hudson River.

Geographic entities mentioned:
surface_form: balsam cap
instance_of: Mountain
countries: United States
coordinates: lat: 41.977036111111
lon: -74.357372222222
The southwest side of Balsam Cap drains into the headwaters of Rondout Creek, thence into the Hudson River. The northwest side of Balsam Cap drains into the East Branch of the Neversink River, the Delaware River, and into Delaware Bay. Balsam Cap is within the Slide Mountain Wilderness of New York's Catskill State Park.

Geographic entities mentioned:
surface_form: balsam cap
instance_of: Mountain
countries: United States
coordinates: lat: 41.977036111111
lon: -74.357372222222
He succeeded his father Yekuno Amlak. Reign. Yagbe'u Seyon served as co-ruler with his father Yekuno Amlak for the last few years of his reign, which eased his succession. A Memorandum in the Four Gospels of Iyasus Mo'a of a gift of vestments and utensils to Istifanos Monastery in Lake Hayq states these gifts were in the name of both Yekuno Amlak and his son Yagbe'u Seyon.

Geographic entities mentioned:
surface_form: Lake Hayq
instance_of: Lake
countries: Ethiopia
coordinates: lat: 11.333333333333
lon: 39.716666666667
He was a member of the New York State Assembly (Clinton Co.) in 1887 and 1888. He was Judge of the Clinton County Court from 1889 to 1890. He was appointed by President Grover Cleveland as Collector of the Port of Lake Champlain in 1895, and remained in office until 1898. He was Deputy New York Superintendent of State Prisons under John B. Riley, and was Acting Warden of Sing Sing in 1914.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
It is one of the largest lakes by volume in the province because of its great depth, and the largest above 1,000 m in elevation. It and Harrison Lake are the largest lakes in the southern Coast Mountains. On March 11, 2019, the Province of British Columbia, working with the Tŝilhqot’in National Government, officially changed the name of the lake from Chilko Lake to Tŝilhqox Biny. Geography.

Geographic entities mentioned:
surface_form: Harrison Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.55
lon: -121.83333333333
The mountains at the head of the lake are among the highest in the province, and two broad, deep glacial valleys connect east to the smaller Taseko Lakes, which drains northwards parallel to the Chilko River, both of them converging with the Chilcotin River which is a tributary of the Fraser.

Geographic entities mentioned:
surface_form: Taseko Lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 51.259166666667
lon: -123.59055555556
Tatlayoko Lake, to the west across another range, is not part of the Chilcotin-Fraser drainage, however, but is part of the Homathko River drainage to Bute Inlet.

Geographic entities mentioned:
surface_form: Tatlayoko Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.546388888889
lon: -124.41472222222
Tsi'lʔos is the Tsilhqot'in name for Mount Tatlow 3,063 m (10,049 ft), which stands in the ranges between Chilko and Taseko Lakes.

Geographic entities mentioned:
surface_form: Mount Tatlow
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3725
lon: -123.86361111111111
Higher still are the mountains at the head of Tŝilhqox Biny, crowned by 3,182 m (10,440 ft) Monmouth Mountain, and to the southwest of the lake, between the two arms, is Mount Good Hope 3,242 m (10,636 ft), with the range rising west from there towards Mount Queen Bess 3,298 m (10,820 ft), to the south of Tatlayoko Lake and higher still beyond to Mount Waddington. History.

Geographic entities mentioned:
surface_form: Monmouth Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.9925
lon: -123.79
surface_form: Mount Good Hope
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1425
lon: -124.17166666666667
surface_form: Mount Queen Bess
instance_of: Mountain
countries: Canada
coordinates: lat: 51.2717
lon: -124.568
surface_form: Mount Waddington
instance_of: Mountain
countries: Canada
coordinates: lat: 51.373611111111
lon: -125.26333333333
surface_form: tŝilhqox biny
instance_of: Lake
countries: Canada
coordinates: lat: 51.25
lon: -124.08333333333
Tŝilhqox Biny. Tŝilhqox Biny (Pronounced: Tsyle-koh Bee), known as Chilko Lake, is a 180 km2 lake in west-central British Columbia, at the head of the Chilko River on the Chilcotin Plateau. The lake is about 65 km long, with a southwest arm 10 km long. It is one of the largest lakes by volume in the province because of its great depth, and the largest above 1,000 m in elevation.

Geographic entities mentioned:
surface_form: chilko lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.25
lon: -124.08333333333
surface_form: tŝilhqox biny
instance_of: Lake
countries: Canada
coordinates: lat: 51.25
lon: -124.08333333333
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
It is one of the largest lakes by volume in the province because of its great depth, and the largest above 1,000 m in elevation. It and Harrison Lake are the largest lakes in the southern Coast Mountains. On March 11, 2019, the Province of British Columbia, working with the Tŝilhqot’in National Government, officially changed the name of the lake from Chilko Lake to Tŝilhqox Biny. Geography.

Geographic entities mentioned:
surface_form: chilko lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.25
lon: -124.08333333333
surface_form: tŝilhqox biny
instance_of: Lake
countries: Canada
coordinates: lat: 51.25
lon: -124.08333333333
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Tŝilhqox Biny. Tŝilhqox Biny (Pronounced: Tsyle-koh Bee), known as Chilko Lake, is a 180 km2 lake in west-central British Columbia, at the head of the Chilko River on the Chilcotin Plateau. The lake is about 65 km long, with a southwest arm 10 km long. It is one of the largest lakes by volume in the province because of its great depth, and the largest above 1,000 m in elevation.

Geographic entities mentioned:
surface_form: tŝilhqox biny
instance_of: Lake
countries: Canada
coordinates: lat: 51.25
lon: -124.08333333333
Geography. The inland equivalent of the many fjords which line the British Columbia Coast on the other side of the Coast Mountains, Tŝilhqox Biny's glacial valley opens not out onto the ocean, but onto a broad lava plateau that lies inland from the highest section of the main range.

Geographic entities mentioned:
surface_form: tŝilhqox biny
instance_of: Lake
countries: Canada
coordinates: lat: 51.25
lon: -124.08333333333
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556