Sarmila/GeoWiki-Features huggingface dataset:
They are aphanitic or vesicular in the older volcano stage. The composition implies that the magma originated from the deep mantle and ascended quickly through the crust, with no storage in a magma chamber. Eruption history. Melville Peak grew in two stages. The first stage crops out close to the sea and consists of alternating lava-pyroclastic layers; it is called the Hektor Icefall Formation.

Geographic entities mentioned:
surface_form: melville
instance_of: Mountain
coordinates: lat: -62.0167
lon: -57.6833
A volcanic ash layer similar in composition to Melville Peak has been identified away from the volcano and may indicate Melville Peak has been volcanically active in the last few thousand years. This peak, which was probably known to early sealers in the area, was charted by the French Antarctic Expedition under Jean-Baptiste Charcot, 1908–10, and takes its name from Cape Melville.

Geographic entities mentioned:
surface_form: melville
instance_of: Mountain
coordinates: lat: -62.0167
lon: -57.6833
Geography and geomorphology. Melville Peak lies at the eastern end of King George Island, in the South Shetland Islands of Antarctica. The mountain rises from the peninsula that leads to Cape Melville. The volcano is about wide, but almost entirely covered by the ice of the Arctowski Icefield and Danowski Glacier.

Geographic entities mentioned:
surface_form: melville
instance_of: Mountain
coordinates: lat: -62.0167
lon: -57.6833
Ladies Delight Light. The Ladies Delight Light is a small lighthouse on Cobbosseecontee Lake, in Winthrop, Maine, United States. It was constructed in 1908 and is believed to be the only active inland waters lighthouse in Maine. The tower is tall, and is equipped with a solar powered dual-level LED marine beacon. It operates every night of the year.

Geographic entities mentioned:
surface_form: Cobbosseecontee Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.25
lon: -69.933333333333
The ship took part in fall 1998 in assisting in the recovery of wreckage from the crash of Swissair Flight 111. &quot;Earl Grey&quot; and recovered wreckage from the plane, while transferring human remains to. On 7–8 December 1989, two cargo vessels, and, sank in the Cabot Strait. &quot;Earl Grey&quot; was among the units dispatched to search for survivors, but they failed to find any.

Geographic entities mentioned:
surface_form: Cabot Strait
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.233333333333
lon: -59.716666666667
1818–1893) was one of the principal headmen of the Diné people before, during and after the Long Walk Period. &quot;Manuelito&quot; translates to &quot;Little Immanuel&quot;. He was born to the &quot;Bit'ahnii&quot; or ″Folded Arms People Clan″, near the Bears Ears in southeastern Utah about 1818. As many Navajo, he was known by different names depending upon context.

Geographic entities mentioned:
surface_form: Bears Ears
instance_of: Landform
countries: United States
coordinates: lat: 37.628329
lon: -109.866365
Trinity Dam is an earthfill dam on the Trinity River located about northeast of Weaverville, California in the United States. The dam was completed in the early 1960s as part of the federal Central Valley Project to provide irrigation water to the arid San Joaquin Valley. Standing high, Trinity Dam forms Trinity Lake – California's third largest reservoir, with a capacity of more than.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Bracora. Bracora or Bracara is a settlement in Lochaber in the Highlands of Scotland. It lies on the north shore of Loch Morar.

Geographic entities mentioned:
surface_form: Loch Morar
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.95
lon: -5.6722222222222
In Norway and Iceland, the usage is closest to the Old Norse, with fjord used for both a firth and for a long, narrow inlet. In eastern Norway, the term is also applied to long narrow freshwater lakes (Randsfjorden and Tyrifjorden) and sometimes even to rivers (for instance in Flå Municipality in Hallingdal, the Hallingdal river is referred to as).

Geographic entities mentioned:
surface_form: Randsfjorden
instance_of: Lake
countries: Norway
coordinates: lat: 60.390277777778
lon: 10.394166666667
surface_form: Tyrifjorden
instance_of: Lake
countries: Norway
coordinates: lat: 60.033333333333
lon: 10.133333333333
surface_form: Hallingdal
instance_of: Valley
countries: Norway
coordinates: lat: 60.633333333333
lon: 9.05
Such deposits are valuable sources of high-quality building materials (sand and gravel) for houses and infrastructure. Eidfjord village sits on the &quot;eid&quot; or isthmus between Eidfjordvatnet lake and Eidfjorden branch of Hardangerfjord. Nordfjordeid is the isthmus with a village between Hornindalsvatnet lake and Nordfjord.

Geographic entities mentioned:
surface_form: Eidfjordvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 60.445
lon: 7.1133333333333
Nordfjordeid is the isthmus with a village between Hornindalsvatnet lake and Nordfjord. Such lakes are also denoted &quot;fjord valley lakes&quot; by geologists. One of Norway's largest is Tyrifjorden at above sea level and an average depth at most of the lake is under sea level. Norway's largest lake, Mjøsa, is also referred to as &quot;the fjord&quot; by locals.

Geographic entities mentioned:
surface_form: Tyrifjorden
instance_of: Lake
countries: Norway
coordinates: lat: 60.033333333333
lon: 10.133333333333
One of Norway's largest is Tyrifjorden at above sea level and an average depth at most of the lake is under sea level. Norway's largest lake, Mjøsa, is also referred to as &quot;the fjord&quot; by locals. Another example is the freshwater fjord Movatnet (Mo lake) that until 1743 was separated from Romarheimsfjorden by an isthmus and connected by a short river.

Geographic entities mentioned:
surface_form: Mjøsa
instance_of: Lake
countries: Norway
coordinates: lat: 60.666666666667
lon: 11
Norway's largest lake, Mjøsa, is also referred to as &quot;the fjord&quot; by locals. Another example is the freshwater fjord Movatnet (Mo lake) that until 1743 was separated from Romarheimsfjorden by an isthmus and connected by a short river. During a flood in November 1743, the river bed eroded and sea water could flow into the lake at high tide.

Geographic entities mentioned:
surface_form: Movatnet
instance_of: Lake
countries: Norway
coordinates: lat: 63.6251
lon: 11.1884
Eventually, Movatnet became a saltwater fjord and renamed Mofjorden (). Like fjords, freshwater lakes are often deep. For instance Hornindalsvatnet is at least deep and water takes an average of 16 years to flow through the lake. Such lakes created by glacial action are also called fjord lakes or moraine-dammed lakes.

Geographic entities mentioned:
surface_form: Hornindalsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 61.933333333333
lon: 6.35
After the ice age the ocean was about at Notodden. The ocean stretched like a fjord through Heddalsvatnet all the way to Hjartdal. Post-glacial rebound eventually separated Heddalsvatnet from the ocean and turned it into a freshwater lake. In Neolithic times Heddalsvatnet was still a saltwater fjord connected to the ocean, and was cut off from the ocean around 1500 BC.

Geographic entities mentioned:
surface_form: Heddalsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 59.55805556
lon: 9.2175
Some freshwater fjords such as Slidrefjord are above the marine limit. Like freshwater fjords, the continuation of fjords on land are in the same way denoted as &quot;fjord-valleys&quot;. For instance Flåmsdal (Flåm valley) and Måbødalen. Outside of Norway, the three western arms of New Zealand's Lake Te Anau are named North Fiord, Middle Fiord and South Fiord.

Geographic entities mentioned:
surface_form: Flåmsdal
instance_of: Valley
countries: Norway
coordinates: lat: 60.79972222
lon: 7.11083333
surface_form: Måbødalen
instance_of: Valley
countries: Norway
coordinates: lat: 60.416666666667
lon: 7.2
Some freshwater fjords such as Slidrefjord are above the marine limit. Like freshwater fjords, the continuation of fjords on land are in the same way denoted as &quot;fjord-valleys&quot;. For instance Flåmsdal (Flåm valley) and Måbødalen. Outside of Norway, the three western arms of New Zealand's Lake Te Anau are named North Fiord, Middle Fiord and South Fiord.

Geographic entities mentioned:
surface_form: Lake Te Anau
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.2
lon: 167.8
Outside of Norway, the three western arms of New Zealand's Lake Te Anau are named North Fiord, Middle Fiord and South Fiord. Another freshwater &quot;fjord&quot; in a larger lake is Western Brook Pond, in Newfoundland's Gros Morne National Park; it is also often described as a fjord, but is actually a freshwater lake cut off from the sea, so is not a fjord in the English sense of the term.

Geographic entities mentioned:
surface_form: Western Brook Pond
instance_of: Lake
countries: Canada
coordinates: lat: 49.733333333333
lon: -57.766666666667
Locally they refer to it as a &quot;landlocked fjord&quot;. Such lakes are sometimes called &quot;fjord lakes&quot;. Okanagan Lake was the first North American lake to be so described, in 1962. The bedrock there has been eroded up to &quot;below&quot; sea level, which is below the surrounding regional topography.

Geographic entities mentioned:
surface_form: Okanagan Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.920833333333
lon: -119.5
Okanagan Lake was the first North American lake to be so described, in 1962. The bedrock there has been eroded up to &quot;below&quot; sea level, which is below the surrounding regional topography. Fjord lakes are common on the inland lea of the Coast Mountains and Cascade Range; notable ones include Lake Chelan, Seton Lake, Chilko Lake, and Atlin Lake.

Geographic entities mentioned:
surface_form: Lake Chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
surface_form: Seton Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.7
lon: -122.167
surface_form: Atlin Lake
instance_of: Lake
countries: Canada
coordinates: lat: 60.0133333
lon: -133.8308333
Fjord lakes are common on the inland lea of the Coast Mountains and Cascade Range; notable ones include Lake Chelan, Seton Lake, Chilko Lake, and Atlin Lake. Kootenay Lake, Slocan Lake and others in the basin of the Columbia River are also fjord-like in nature, and created by glaciation in the same way.

Geographic entities mentioned:
surface_form: Kootenay Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
surface_form: Slocan Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.9472
lon: -117.378
Kootenay Lake, Slocan Lake and others in the basin of the Columbia River are also fjord-like in nature, and created by glaciation in the same way. Along the British Columbia Coast, a notable fjord-lake is Owikeno Lake, which is a freshwater extension of Rivers Inlet. Quesnel Lake, located in central British Columbia, is claimed to be the deepest fjord formed lake on Earth. Great Lakes.

Geographic entities mentioned:
surface_form: Owikeno Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.683333333333
lon: -126.91666666667
Quesnel Lake, located in central British Columbia, is claimed to be the deepest fjord formed lake on Earth. Great Lakes. A family of freshwater fjords are the embayments of the North American Great Lakes. Baie Fine is located on the northwestern coast of Georgian Bay of Lake Huron in Ontario, and Huron Bay is located on the southern shore of Lake Superior in Michigan. Locations.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Old Weir Bridge. The Old Weir Bridge is an ancient bridge located in Killarney National Park in County Kerry, Ireland. It is a twin arch bridge made of stone. The bridge is situated at the spot known as the &quot;Meeting of the Waters&quot;, where the three Killarney lakes meet. The waters from the Upper Lake flow into the Middle (or Muckross Lake) and Lough Leane. History.

Geographic entities mentioned:
surface_form: Killarney lakes
instance_of: Group of lakes
countries: Ireland
coordinates: lat: 52.041666666667
lon: -9.55
It is a twin arch bridge made of stone. The bridge is situated at the spot known as the &quot;Meeting of the Waters&quot;, where the three Killarney lakes meet. The waters from the Upper Lake flow into the Middle (or Muckross Lake) and Lough Leane. History. The actual age of the bridge is unclear, but believed to date back to the sixteenth century.

Geographic entities mentioned:
surface_form: Lough Leane
instance_of: Lake
countries: Ireland
coordinates: lat: 52.041666666667
lon: -9.55
Daggoo Peak. Daggoo Peak () is a rocky peak, high, situated in southeastern Aristotle Mountains at the north side of the mouth of Flask Glacier, west-southwest of Tashtego Point on the east side of Graham Land.

Geographic entities mentioned:
surface_form: daggoo peak
instance_of: Mountain
coordinates: lat: -65.75
lon: -62.3333
It was surveyed and photographed by the Falkland Islands Dependencies Survey in 1947, and named by the UK Antarctic Place-Names Committee in 1956 after Flask's harpooner on the &quot;Pequod&quot; in Herman Melville's &quot;Moby-Dick; or, The White Whale&quot;.

Geographic entities mentioned:
surface_form: melville
instance_of: Mountain
coordinates: lat: -62.0167
lon: -57.6833
Portage la Prairie is approximately west of Winnipeg, along the Trans-Canada Highway (exactly halfway between the provincial boundaries of Saskatchewan and Ontario). It sits on the Assiniboine River, which flooded the town persistently until a diversion channel north to Lake Manitoba (the Portage Diversion) was built to divert the flood waters.

Geographic entities mentioned:
surface_form: Lake Manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
This particular &quot;portage&quot; route, used by Indigenous peoples even before the global Fur Trade, ran for 25 kilometres between the Assiniboine River and Lake Manitoba.

Geographic entities mentioned:
surface_form: Lake Manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
Most of the songs were written by Parsons and Hillman at a house in the San Fernando Valley dubbed &quot;Burrito Manor.&quot; &quot;Sin City&quot;, co-written by Hillman and Parsons and called a &quot;loping lament&quot; and a &quot;cautionary dirge&quot;, mentions The Byrds's manager Larry Spector (&quot;a gold plated door&quot;) and Robert F. Kennedy (&quot;tried to clean up this town&quot;).

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
In the United States, Vignoles is most commonly grown in New York state's Finger Lakes region, and in the Midwest including Missouri, Indiana, Ohio, Illinois, Iowa and Kentucky.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
It is situated in western Bosnia and Herzegovina, on the road between Bosansko Grahovo and Bosanski Petrovac, and also near Glamoč. Drvar lies in a vast valley, the southeastern part of Bosanska Krajina, between the Osječanica, Klekovača, Vijenca and Šator mountains of the Dinaric Alps.

Geographic entities mentioned:
surface_form: Klekovača
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 44.4302
lon: 16.5087
surface_form: Šator
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 44.157330555556
lon: 16.5897
History. Dallas–Fort Worth National Cemetery was established in 2000 on the eastern shore of Mountain Creek Lake north of Dallas Baptist University. It is the sixth National Cemetery created in Texas and was created to meet the future needs of American veterans, nearly 1.5 million of whom live in the state of Texas. It currently has space for over 280,000 interments.

Geographic entities mentioned:
surface_form: Mountain Creek Lake
instance_of: Lake
countries: United States
coordinates: lat: 32.719269444444
lon: -96.960894444444
Sugarloaf Community Wind Farm. The Sugarloaf Community Wind Farm is a wind power project in western Maine under development by Endless Energy Corporation. The wind farm is planned to be situated between the Sugarloaf and the Saddleback Maine ski resorts on Redington Pond Range and Black Nubble Mountains.

Geographic entities mentioned:
surface_form: Redington Pond Range
instance_of: Mountain
countries: United States
coordinates: lat: 45.025
lon: -70.3887
In 2007 a permit for this project was denied by the Land Use Regulation Commission although their staff had recommended approval. The developer proposed an alternative project cut down to being only on Black Nubble, which was rejected by LURC a year later. Public opinion. Some controversy has surrounded the possibility of a wind farm on the Mount Redington area.

Geographic entities mentioned:
surface_form: Mount Redington
instance_of: Mountain
countries: United States
coordinates: lat: 45.025
lon: -70.3887
Visitors can take the Seattle Underground Tour to see what remains of the old storefronts. Just before the fire, cable car service was instituted from Pioneer Square along Yesler Way to Lake Washington and the Leschi neighborhood. In 1891, German-born Frederick Trump, President Donald Trump's grandfather, owned the Dairy Restaurant on Washington Street. 20th century.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Bagua Plateau - Baguashan Tunnel - Baguazhang - Bahá'í Faith in Taiwan - Bai Chongxi - Baishatun Mazu Pilgrimage - Bai Wanxiang - Bajiquan - H. A.

Geographic entities mentioned:
surface_form: Bagua Plateau
instance_of: Mountain
countries: Taiwan
coordinates: lat: 23.9328
lon: 120.627
Y. Lee
D.

Geographic entities mentioned:
surface_form: Dadu Plateau
instance_of: Mountain
countries: Taiwan
coordinates: lat: 24.14583333
lon: 120.57888889
Lilley - Lin (surname) - Lin Ben Yuan Family - Lin Family Ancestral Shrine - Lin Hwai-min - Lin Wang - Justin Yifu Lin - Lin Yü-chih - Lin Yutang - Linji Huguo Chan Temple - Lion dance - List of airlines of Taiwan - List of archaeological sites in Taiwan -List of assets owned by the Kuomintang - List of banks in Taiwan - List of bridges in Taiwan - List of Chinese language schools in Taiwan - List of Chinese Taipei Representatives to APEC - List of cinemas in Taiwan - List of Cold War pilot defections - List of companies of Taiwan - List of convention centers in Taiwan - List of earthquakes in Taiwan - List of Legislative Yuan elections - List of museums in Taiwan - List of national parks in Taiwan - List of national scenic areas in Taiwan - List of night markets in Taiwan - List of political parties in Taiwan - List of postal codes in the Republic of China - List of power stations in Taiwan - List of protected species in Taiwan - List of rivers in Taiwan - List of rulers of Taiwan - List of Shinto shrines in Taiwan - List of shopping malls in Taiwan - List of sister cities of Taipei - List of Taiwanese authors - List of Taiwanese automakers - List of Taiwanese people by net worth - List of Taiwanese submissions for the Academy Award for Best Foreign Language Film - List of Taiwanese television series - List of tallest buildings in Taiwan - List of temples in Taichung - List of temples in Taiwan - List of tourist attractions in Taipei - List of tourist attractions in Taiwan - List of universities in Taiwan - List of U.S.

Geographic entities mentioned:
surface_form: Longtan Lake
instance_of: Lake
countries: Taiwan
coordinates: lat: 24.85
lon: 121.18333333333
Smith (historian) - Smoking in Taiwan - Snake wine - Sockgate - Sogo - Songzhu Temple - James Soong - Soong Mei-ling - Southern Chinese wedding - Spanish expedition to Formosa - Spanish Formosa - Sport in Taiwan - Sports Affairs Council - Spring and Autumn Pavilions - Spring Scream - SS Bokhara - St.

Geographic entities mentioned:
surface_form: Sun Moon Lake
instance_of: Lake
countries: Taiwan
coordinates: lat: 23.866666666667
lon: 120.91666666667
Bersame Glacier. Bersame Glacier (,) is the 2.4 km long and 1.5 km wide glacier on the west side of Urda Ridge on Clarence Island in the South Shetland Islands, Antarctica situated northeast of Giridava Glacier. It drains the slopes of Mount Llana, flows northwestwards and enters the Southern Ocean northeast of the terminus of Giridava Glacier.

Geographic entities mentioned:
surface_form: Mount Llana
instance_of: Mountain
coordinates: lat: -61.2461
lon: -54.1214
Mount Yumiori. is a mountain located in the city of Takayama, Gifu, Japan. It is tall and part of the Hida Mountains.

Geographic entities mentioned:
surface_form: mount yumiori
instance_of: Mountain
countries: Japan
coordinates: lat: 36.349444444444
lon: 137.59666666667
The saga revolves around the lives and times of the residents of the Fljótsdalur region in Iceland, including Helge Åsbjørnsson (&quot;Helgi Ásbjarnarson&quot;) and of Grim (&quot;Grímr&quot;) and Helge (&quot;Helgi&quot;), two sons of the widow Droplaug, a pair of brothers who have their own saga, &quot;Droplaugarsona saga&quot;. Plot and Themes.

Geographic entities mentioned:
surface_form: Fljótsdalur
instance_of: Valley
countries: Iceland
coordinates: lat: 65.033333333333
lon: -15
Plot and Themes. Fljótsdæla saga primarily focuses on the lives of people in the Fljótsdalur region, with a significant portion dedicated to characters from Northeast Iceland who intermarry into local families. The most prominent characters are Grímr and Helgi Droplaugarson, sons of the widow Droplaug Spak-Bersadóttir. Their own saga, &quot;Droplaugarsona saga&quot;, tells a similar tale.

Geographic entities mentioned:
surface_form: Fljótsdalur
instance_of: Valley
countries: Iceland
coordinates: lat: 65.033333333333
lon: -15
Laaxersee. Laaxersee or Lag Grond is a lake in the village of Laax, Grisons, Switzerland. Its surface area is and maximum depth 5.5 m. Fishing season is from May 1 to September 15. In winter, the lake is generally frozen.

Geographic entities mentioned:
surface_form: lag grond
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.808055555556
lon: 9.2572222222222
surface_form: laaxersee
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.808055555556
lon: 9.2572222222222
Laaxersee. Laaxersee or Lag Grond is a lake in the village of Laax, Grisons, Switzerland. Its surface area is and maximum depth 5.5 m. Fishing season is from May 1 to September 15. In winter, the lake is generally frozen.

Geographic entities mentioned:
surface_form: laaxersee
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.808055555556
lon: 9.2572222222222
Fetisovo. Fetisovo is a village located in Kazakhstan on the coast of the Caspian Sea. The European route E121 passes by the area.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Borgarvirki. Borgarvirki lies between Vesturhóp and Víðidalur in the north of Iceland, and at 177m above sea level it dominates the surrounding region. Made out of basalt strata, it has been used as a fortress. Borgarvirki is a natural phenomenon, altered by humans in earlier centuries. In 1949, Borgarvirki was renovated by workers who installed a granite lintel at the main entrance.

Geographic entities mentioned:
surface_form: borgarvirki
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.465666666667
lon: -20.599
Made out of basalt strata, it has been used as a fortress. Borgarvirki is a natural phenomenon, altered by humans in earlier centuries. In 1949, Borgarvirki was renovated by workers who installed a granite lintel at the main entrance. Borgarvirki is a volcanic plug (gosstapi), and the Icelandic sagas mention that in earlier centuries it was used for military purposes.

Geographic entities mentioned:
surface_form: borgarvirki
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.465666666667
lon: -20.599
Borgarvirki is a natural phenomenon, altered by humans in earlier centuries. In 1949, Borgarvirki was renovated by workers who installed a granite lintel at the main entrance. Borgarvirki is a volcanic plug (gosstapi), and the Icelandic sagas mention that in earlier centuries it was used for military purposes. There is a viewing dial inside.

Geographic entities mentioned:
surface_form: borgarvirki
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.465666666667
lon: -20.599
History. After the Gorkhali conquest of the Kathmandu valley, King Prithvi Narayan Shah expelled the Christian Capuchin missionaries from Patan and renamed Nepal as &quot;Asil Hindustan&quot; (pure land of Hindus). The Tagadharis enjoyed a privileged status in the Nepalese capital and greater access to the authorities following these events.

Geographic entities mentioned:
surface_form: Kathmandu valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
Ambitle. Ambitle is a volcanic island on the South Bismarck plate which, together with Babase, another volcanic island, makes up the Feni Islands in the Bismarck Archipelago. The island is located within the Papua New Guinea's New Ireland Province, to the east of the island of New Ireland. It is part of the Tanir Rural LLG local government area.

Geographic entities mentioned:
surface_form: ambitle
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -4.0833333333333
lon: 153.95
It is part of the Tanir Rural LLG local government area. Ambitle is a stratovolcano, reaching above sea level, located at the southeastern end of the NW-trending 250 km long Tabar-Lihir-Tanga-Feni (TLTF) volcanic island chain. It last erupted in about 350 BCE based on radiocarbon dating.

Geographic entities mentioned:
surface_form: ambitle
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -4.0833333333333
lon: 153.95
It last erupted in about 350 BCE based on radiocarbon dating. The rock types sampled from Ambitle include feldspathoid-bearing basalt, trachybasalt, phonotephrite, trachyandesite, and trachydacite or quartz-trachyte. Its caldera, wide, contains thermal areas on its western side. Venting of hydrothermal water also occurs in coral reefs to the west of this island.

Geographic entities mentioned:
surface_form: ambitle
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -4.0833333333333
lon: 153.95
History. In March 1643 the expedition to Oceania of Abel Tasman approached New Ireland. Tasman believed that he had already reached the mainland of New Guinea, while he was in fact sailing along the eastern coast of New Ireland. The expedition passed south of Ambitle, naming it St. Jan's Island.

Geographic entities mentioned:
surface_form: ambitle
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -4.0833333333333
lon: 153.95
The island is located within the Papua New Guinea's New Ireland Province, to the east of the island of New Ireland. It is part of the Tanir Rural LLG local government area. Ambitle is a stratovolcano, reaching above sea level, located at the southeastern end of the NW-trending 250 km long Tabar-Lihir-Tanga-Feni (TLTF) volcanic island chain.

Geographic entities mentioned:
surface_form: tanir rural
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -4.0833333333333
lon: 153.95
Mount Humble. Mount Humble () is, at, the highest mountain in the Raggatt Mountains of Antarctica, standing south of the isolated mountain Mount Sibiryakov. It was plotted from air photos taken by the Australian National Antarctic Research Expeditions in 1956, and was named by the Antarctic Names Committee of Australia for John Edmund Humble, a cosmic ray physicist at Mawson Station in 1960.

Geographic entities mentioned:
surface_form: Mount Sibiryakov
instance_of: Mountain
coordinates: lat: -67.933333333333
lon: 49.583333333333
surface_form: mount humble
instance_of: Mountain
coordinates: lat: -67.6667
lon: 49.4833
surface_form: humble
instance_of: Mountain
coordinates: lat: -67.6667
lon: 49.4833
surface_form: sibiryakov
instance_of: Mountain
coordinates: lat: -67.933333333333
lon: 49.583333333333
Mount Humble. Mount Humble () is, at, the highest mountain in the Raggatt Mountains of Antarctica, standing south of the isolated mountain Mount Sibiryakov. It was plotted from air photos taken by the Australian National Antarctic Research Expeditions in 1956, and was named by the Antarctic Names Committee of Australia for John Edmund Humble, a cosmic ray physicist at Mawson Station in 1960.

Geographic entities mentioned:
surface_form: mount humble
instance_of: Mountain
coordinates: lat: -67.6667
lon: 49.4833
surface_form: humble
instance_of: Mountain
coordinates: lat: -67.6667
lon: 49.4833
Mount Humble. Mount Humble () is, at, the highest mountain in the Raggatt Mountains of Antarctica, standing south of the isolated mountain Mount Sibiryakov. It was plotted from air photos taken by the Australian National Antarctic Research Expeditions in 1956, and was named by the Antarctic Names Committee of Australia for John Edmund Humble, a cosmic ray physicist at Mawson Station in 1960.

Geographic entities mentioned:
surface_form: humble
instance_of: Mountain
coordinates: lat: -67.6667
lon: 49.4833
Wibald was one of the most influential councillors of the Holy Roman Emperor Lothaire II and King Conrad III. Combining patriotism with a submissive devotion to the Holy See, he used his great influence to preserve harmony between the emperors and the popes. In 1137 he accompanied Lothair on a military expedition to Italy and through the emperor's influence was elected Abbot of Monte Cassino.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
Background. Preceding the Delano grape strike was another grape strike organized by Filipino farm workers that occurred in Coachella Valley, California, on May 3, 1965. Because the majority of strikers were over 50 years old and did not have families of their own due to anti-miscegenation laws (first overthrown in 1949), they were willing to risk what little they had to fight for higher wages.

Geographic entities mentioned:
surface_form: Coachella Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.72
lon: -116.2
After the end of the grape strike in 1970, a strike against lettuce growers began. This led to conflict with the Teamsters union, in the Salinas Valley. In June 1975, California passed a law allowing for secret ballot union representation elections for farm workers.

Geographic entities mentioned:
surface_form: Salinas Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.7654
lon: -121.7918
Baldwin Rocks. 9n57gesuiizjk1igy1145zl87g0j" xml:space="preserve">The Baldwin Rocks () are a group of rock outcrops about northwest of Watson Bluff on the north side of David Island. They were charted by the Australasian Antarctic Expedition, 1911–14, under Mawson, and named by him for Joseph M. Baldwin of the Melbourne Observatory.

Geographic entities mentioned:
surface_form: Watson Bluff
instance_of: Landform
coordinates: lat: -66.4167
lon: 98.95
Quzah. Quzaḥ () is a pre-Islamic Arab god of weather, worshiped by the people of Muzdalifah. The pre-Islamic rite of the Ifada celebrated after the September equinox was performed facing the direction of Quzah's sanctuary. A lasting reference to Quzah is the term &quot;qaws Quzaḥ&quot; (), &quot;Bow of Quzah&quot;, which became the Arabic term for rainbow.

Geographic entities mentioned:
surface_form: Muzdalifah
instance_of: Valley
countries: Saudi Arabia
coordinates: lat: 21.3925
lon: 39.937777777778
The station's studios and offices are located in West Valley City. KODJ has an effective radiated power of 21,500 watts. The transmitter site is located in Erda, Utah, on Farnsworth Peak in the Oquirrh Mountains. KODJ is also heard on about a dozen FM translator stations in small communities around Utah and Wyoming. KALL-FM (1968–1984). On December 1, 1968, the station signed on as KALL-FM.

Geographic entities mentioned:
surface_form: Farnsworth Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.659783333333
lon: -112.20234722222
It starred and was produced by Errol Flynn. It commenced filming in Italy in 1953 and was meant to be the directorial debut of Jack Cardiff. It was filmed in CinemaScope. A £10,000 model town set was built near Mont Blanc. Development. Flynn said after a fight with Jack Warner he decided &quot;The hell with them all. I will go to Italy and make my own pictures.

Geographic entities mentioned:
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
Known with certainty is that the property soon came into the hands of Peter Lansing, an Albany merchant, whose family were prominent land owners and fellow merchants in the upper Hudson Valley. However, local nineteenth-century accounts hold that the Lansings and others fled south upon the approach of the British army and its Indian allies in the summer of 1777.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Alto de Nique. Alto de Nique is a mountain in South and Central America. It is tall and sits on the international border between Colombia and Panama.

Geographic entities mentioned:
surface_form: alto de nique
instance_of: Mountain
countries: Panama
Colombia
coordinates: lat: 7.7016666666667
lon: -77.7275
Similarly, the revolving restaurant, located atop the Schilthorn near the village of Mürren used in &quot;On Her Majesty's Secret Service&quot; has retained the name Piz Gloria since filming took place there. Klaus Dodds has noted that there is a geopolitical aspect to the locations used, although this is often a pre-emption of an issue by the film. For example, in the first film, &quot;Dr.

Geographic entities mentioned:
surface_form: Schilthorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.557222222222
lon: 7.8352777777778
Aebi was First Vice President of the National Council for the 2019–2020 session under the presidency of Isabelle Moret. Biography. Aebi was born in Burgdorf, in the Emmental region of the Canton of Bern. He is a farmer by profession and also works as an auctioneer. From 1999 to 2020, he was on the board of the Arbeitsgemeinschaft Schweizerischer Rinderzüchter, the Association of Cattle Breeders.

Geographic entities mentioned:
surface_form: Emmental
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.91922
lon: 7.77868
As it is thought that one Arabian represented, they found the length of 1° of meridian to be, which differs from the true value by. Marwarrūdhī was chosen by the geometer Al-Abbās ibn Said al-Jawharī to organize a new observatory on Mount Qasioun.

Geographic entities mentioned:
surface_form: Mount Qasioun
instance_of: Mountain
countries: Syria
coordinates: lat: 33.545833333333
lon: 36.286388888889
Wear Cove is a type of valley known as a &quot;limestone window&quot;, created when erosion weathers through the older Precambrian sandstone and exposes the younger Paleozoic limestone beneath. The northern rim of the Smokies is dotted with limestone coves, the most well-known of which are Cades Cove and Tuckaleechee Cove. Limestone coves contain very fertile soil which lured early settlers.

Geographic entities mentioned:
surface_form: Cades Cove
instance_of: Valley
countries: United States
coordinates: lat: 35.594166666667
lon: -83.841944444444
Limestone coves contain very fertile soil which lured early settlers. Wear Cove is hemmed in by Cove Mountain to the southeast, Roundtop to the southwest, Davis Mountain to the northwest, and Hatcher Mountain to the northeast. Numerous hollows cut into the ridges throughout the cove, including Happy Hollow, Smith Hollow, and Little Cove. U.S.

Geographic entities mentioned:
surface_form: Davis Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.761388888889
lon: -74.106111111111
Wear Cove. Wear Cove is a valley in southwestern Sevier County, Tennessee. It runs parallel to the Great Smoky Mountains National Park just to its south. Like other park border regions, the history and economy of the valley are intertwined with that of the Smokies. The primary community is Wears Valley.

Geographic entities mentioned:
surface_form: wear cove
instance_of: Valley
countries: United States
coordinates: lat: 35.7139
lon: -83.6532
The primary community is Wears Valley. Wear Cove is a type of valley known as a &quot;limestone window&quot;, created when erosion weathers through the older Precambrian sandstone and exposes the younger Paleozoic limestone beneath. The northern rim of the Smokies is dotted with limestone coves, the most well-known of which are Cades Cove and Tuckaleechee Cove.

Geographic entities mentioned:
surface_form: wear cove
instance_of: Valley
countries: United States
coordinates: lat: 35.7139
lon: -83.6532
The valley was originally named “Crowson Cove” after Aaron Crowson who first settled in the area in 1792. By 1900, however, it was renamed “Wear Cove” after Samuel Wear (1753–1817), a Revolutionary War veteran who erected a fort near the entrance to the valley in what is now Pigeon Forge. Crowson arrived in Wear Cove from North Carolina in 1792 along with his friend, Peter Percefield.

Geographic entities mentioned:
surface_form: wear cove
instance_of: Valley
countries: United States
coordinates: lat: 35.7139
lon: -83.6532
Crowson rode to Wear's Fort to get help, but the Cherokee had fled by the time he returned. Several settlers marched onward to Great Tellico to the west, where they murdered four Cherokee while they slept. Percefield was buried on a hill in the eastern half of Wear Cove in what is now Crowson Cemetery. Later that year, Crowson received a land grant for this plot of land.

Geographic entities mentioned:
surface_form: wear cove
instance_of: Valley
countries: United States
coordinates: lat: 35.7139
lon: -83.6532
Like many other farms in the cove, the Brickey farm was ravaged by the U.S. Civil War. Isaac Trotter, who operated the iron forge at Pigeon Forge reported a Cherokee raid in Wear Cove in 1864. Earlier in the war, a Union army passed through the valley en route to dislodge the troops of Will Thomas who were entrenched in Gatlinburg.

Geographic entities mentioned:
surface_form: wear cove
instance_of: Valley
countries: United States
coordinates: lat: 35.7139
lon: -83.6532
Civil War. Isaac Trotter, who operated the iron forge at Pigeon Forge reported a Cherokee raid in Wear Cove in 1864. Earlier in the war, a Union army passed through the valley en route to dislodge the troops of Will Thomas who were entrenched in Gatlinburg. Sometime after the war, Alfred Line established a farm at the base of Roundtop Mountain, near the southern half of Wear Cove.

Geographic entities mentioned:
surface_form: wear cove
instance_of: Valley
countries: United States
coordinates: lat: 35.7139
lon: -83.6532
Limestone coves contain very fertile soil which lured early settlers. Wear Cove is hemmed in by Cove Mountain to the southeast, Roundtop to the southwest, Davis Mountain to the northwest, and Hatcher Mountain to the northeast. Numerous hollows cut into the ridges throughout the cove, including Happy Hollow, Smith Hollow, and Little Cove. U.S.

Geographic entities mentioned:
surface_form: smith hollow
instance_of: Valley
countries: United States
coordinates: lat: 36.679236
lon: -94.105763
Brickey operated a large farm and distillery in the valley until his death in 1856. The log home he built shortly after his arrival still stands in Smith Hollow (between Wears Valley and Townsend) and is listed on the National Register of Historic Places. Like many other farms in the cove, the Brickey farm was ravaged by the U.S. Civil War.

Geographic entities mentioned:
surface_form: smith hollow
instance_of: Valley
countries: United States
coordinates: lat: 36.679236
lon: -94.105763
Puula is above sea level, with a surface area of. It is deep at its deepest point, located near Porttisalmi at Simpiänselkä, which is the biggest open area of the lake. Two big lakes Suontee and Puula were one lake until year 1854, when the water level was lowered 2.5 meters. This brought geological stacks above the surface, which are formed by water.

Geographic entities mentioned:
surface_form: Suontee
instance_of: Lake
countries: Finland
coordinates: lat: 61.7461265
lon: 26.2597018
surface_form: puula
instance_of: Lake
countries: Finland
coordinates: lat: 61.8101122
lon: 26.6938146
Two big lakes Suontee and Puula were one lake until year 1854, when the water level was lowered 2.5 meters. This brought geological stacks above the surface, which are formed by water. Water from lake Puula runs down to Vahvajärvi through Kissakoski Canal. Puula is known as a body of water with lake trout and lake salmon and it is therefore popular among trollers.

Geographic entities mentioned:
surface_form: Vahvajärvi
instance_of: Lake
countries: Finland
coordinates: lat: 61.64478
lon: 26.65512
surface_form: puula
instance_of: Lake
countries: Finland
coordinates: lat: 61.8101122
lon: 26.6938146
Puula. Puula (or Puulavesi) is a lake in the Kymi River area in the Finnish municipalities of Hirvensalmi, Kangasniemi and Mikkeli. Puula is above sea level, with a surface area of. It is deep at its deepest point, located near Porttisalmi at Simpiänselkä, which is the biggest open area of the lake.

Geographic entities mentioned:
surface_form: puula
instance_of: Lake
countries: Finland
coordinates: lat: 61.8101122
lon: 26.6938146
Puula. Puula (or Puulavesi) is a lake in the Kymi River area in the Finnish municipalities of Hirvensalmi, Kangasniemi and Mikkeli. Puula is above sea level, with a surface area of. It is deep at its deepest point, located near Porttisalmi at Simpiänselkä, which is the biggest open area of the lake.

Geographic entities mentioned:
surface_form: puula
instance_of: Lake
countries: Finland
coordinates: lat: 61.8101122
lon: 26.6938146
surface_form: puulavesi
instance_of: Lake
countries: Finland
coordinates: lat: 61.8101122
lon: 26.6938146
This brought geological stacks above the surface, which are formed by water. Water from lake Puula runs down to Vahvajärvi through Kissakoski Canal. Puula is known as a body of water with lake trout and lake salmon and it is therefore popular among trollers. The largest lake salmon in Finland in the 21st century, which weighed 12.4 kg, came from Puula.

Geographic entities mentioned:
surface_form: puula
instance_of: Lake
countries: Finland
coordinates: lat: 61.8101122
lon: 26.6938146
Water from lake Puula runs down to Vahvajärvi through Kissakoski Canal. Puula is known as a body of water with lake trout and lake salmon and it is therefore popular among trollers. The largest lake salmon in Finland in the 21st century, which weighed 12.4 kg, came from Puula. Multi-kilo trout are a typical catch from Puula.

Geographic entities mentioned:
surface_form: puula
instance_of: Lake
countries: Finland
coordinates: lat: 61.8101122
lon: 26.6938146
The Vestmannaeyjar Airport and the Westman Islands Golf Club taken together cover a good portion of the island. In January 1973, lava flow from nearby Eldfell destroyed half the town and threatened to close its harbour, its main income source. An operation to cool the advancing lava with sea water saved the harbour. First settlers.

Geographic entities mentioned:
surface_form: Eldfell
instance_of: Mountain
countries: Iceland
coordinates: lat: 63.4333008635
lon: -20.2487692886
The Hallgrímskirkja Lutheran church in Reykjavík is named in his honour. Eldfell. At 01:00 on 23 January 1973, a volcanic eruption of the mountain Eldfell began on Heimaey. The ground on Heimaey started to quake and fissures formed. The fissures grew to in length, and lava began to erupt. Lava sprayed into the air from the fissures. Volcanic ash was blown to sea. Later, the situation deteriorated.

Geographic entities mentioned:
surface_form: Eldfell
instance_of: Mountain
countries: Iceland
coordinates: lat: 63.4333008635
lon: -20.2487692886
Hominina footprints from site G. The principal discovery, made by Mary Leakey and her team in 1976 (and fully excavated by 1978), is a 75-foot (24-meter) line of Hominina fossil footprints, preserved in powdery volcanic ash originally thought to have been from an eruption of the nearby (20 km) Sadiman volcano.

Geographic entities mentioned:
surface_form: Sadiman volcano
instance_of: Mountain
countries: Tanzania
coordinates: lat: -3.193821
lon: 35.41297
The temple is the third LDS temple built in Arizona and the first temple announced by Thomas S. Monson after being sustained as President of the Church in 2008. Monson dedicated the temple on May 23, 2010. Geography. From its location just south of the Gila River within the Upper Gila Valley, Mount Graham of the Pinaleño Mountains dominates the southern skyline.

Geographic entities mentioned:
surface_form: Mount Graham
instance_of: Mountain
countries: United States
coordinates: lat: 32.70166666666667
lon: -109.87138888888889
He has brothers Allan, James, and Robert. He graduated from Darien High School in Darien, Connecticut. While living in a Hill City, South Dakota motel, his mother and stepfather did an oral history project for the University of South Dakota, interviewing the men who worked to create Mount Rushmore. Karl later credited that project for sparking his interest in journalism.

Geographic entities mentioned:
surface_form: Mount Rushmore
instance_of: Mountain
countries: United States
coordinates: lat: 43.878947222222
lon: -103.459825
Bader Glacier. Bader Glacier () is a small glacier draining the west slopes of Rudozem Heights and flowing to Bourgeois Fjord just south of Thomson Head on German Peninsula, Fallières Coast on the west side of Graham Land, Antarctica. History.

Geographic entities mentioned:
surface_form: Rudozem Heights
instance_of: Mountain
coordinates: lat: -67.65
lon: -66.7
But as the Delano grape strike seemed to be ending, an attempt by the International Brotherhood of Teamsters to organize farm laborers in the Salinas Valley in California led to the costly &quot;Salad Bowl strike.&quot; Six thousand drivers and packing workers represented by the Teamsters struck on July 17, 1970, winning a contract on July 23 under which growers gave the Teamsters, not the UFW, access to farms and the right to organize workers into unions.

Geographic entities mentioned:
surface_form: Salinas Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.7654
lon: -121.7918
Soon organizing battles between the two unions became violent. &quot;Flying squads&quot; of Teamsters began attacking UFW supporters in broad daylight in the Coachella Valley. The violence worsened when the dispute moved into the Delano vineyards.

Geographic entities mentioned:
surface_form: Coachella Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.72
lon: -116.2
The dike has been partially eroded, leaving a prominent gorge up to wide deep that extends from near the summit down to Avalanche Lake. Landslides in the mountain's past have scarred the western slopes with large slides and were responsible for separating Avalanche Lake from nearby Lake Colden. Recent landslides were observed in 1869, 1942, 1990, 1999, and 2011. History.

Geographic entities mentioned:
surface_form: Lake Colden
instance_of: Lake
countries: United States
coordinates: lat: 44.1225
lon: -73.979166666667
surface_form: avalanche lake
instance_of: Lake
countries: United States
coordinates: lat: 48.6564
lon: -113.786
surface_form: avalanche lake
instance_of: Lake
countries: United States
coordinates: lat: 44.1331
lon: -73.9678
surface_form: avalanche lake
instance_of: Lake
countries: United States
coordinates: lat: 47.4948614
lon: -121.3172495