Sarmila/GeoWiki-Features huggingface dataset:
Carrizo Creek flows west then north northwest through Jacumba Valley then north through Carrizo Gorge and Carrizo Canyon, into Carrizo Valley where it is joined on the left by Vallecito Creek, as it turns east through the Carrizo Badlands where 3 miles east of the site of the old Carrizo Creek Station, at an elevation of, it becomes Carrizo Wash.

Geographic entities mentioned:
surface_form: Carrizo Gorge
instance_of: Valley
countries: United States
coordinates: lat: 32.74444444
lon: -116.19722222
surface_form: Carrizo Valley
instance_of: Valley
countries: United States
coordinates: lat: 32.86888889
lon: -116.19583333
surface_form: Carrizo Badlands
instance_of: Landform
countries: United States
coordinates: lat: 32.8517
lon: -116.137
History. Carrizo Creek, its wash and its tributary, Vallecito Creek, were the watercourses that carved the pathway from the Peninsular Ranges of Southern California through the Carrizo Badlands to the Colorado Desert. They provided a pathway and water for Native Americans travelers out into the desert and on to the Colorado River along the course of the distributary New or Alamo Rivers.

Geographic entities mentioned:
surface_form: Carrizo Badlands
instance_of: Landform
countries: United States
coordinates: lat: 32.8517
lon: -116.137
Both companies used Carrizo Creek Station at the lower end if the creek in the badlands. Carrizo Wash. Carrizo Wash is a wash with its head at the mouth of Carrizo Creek in the Carrizo Badlands located at, and its mouth at its confluence with San Felipe Creek, at an elevation of below sea level.

Geographic entities mentioned:
surface_form: Carrizo Badlands
instance_of: Landform
countries: United States
coordinates: lat: 32.8517
lon: -116.137
Foinikas (river). The river Foinikas (,) is a river in the northern Peloponnese, Greece. It is also known as Salmenikos River (Σαλμένικος). Its source is on the north-eastern slopes of Mount Panachaiko, near the village of Vounopirgos (Loubista). It empties into the Gulf of Corinth, between the villages of Longos and Kamares.

Geographic entities mentioned:
surface_form: Panachaiko
instance_of: Mountain
countries: Greece
coordinates: lat: 38.2025
lon: 21.868888888889
Linus Beach. Linus Beach (,) is the ice-free 2 km long beach on the east side of Cape Timblón, Snow Island in the South Shetland Islands, Antarctica. It is part of the south coast of Morton Strait. The area was visited by early 19th century sealers. The feature is named after the mythical musician and poet Linus of Thrace, brother of Orpheus. Location.

Geographic entities mentioned:
surface_form: Morton Strait
instance_of: Body of water
coordinates: lat: -62.6972
lon: -61.22
The Mane Street Historic District is listed on the National Register of Historic Places. The winding, drive northwest to Pioneertown from Yucca Valley has been designated a California Scenic Drive, and the area is now surrounded by both privately and federally protected lands. The Sawtooths are a small mountain range to the south, while Black Hill is to the north. History.

Geographic entities mentioned:
surface_form: Sawtooths
instance_of: Mountain
countries: United States
coordinates: lat: 34.143611111111
lon: -116.50861111111
Paruma. Paruma is a stratovolcano that lies on the border of Bolivia and Chile. It is part of a ridge that contains several stratovolcanos. Paruma lies at the eastern end of the ridge, with Olca to its west. The older volcano Paruma lies to east of Paruma. Paruma has clearly been active during the Holocene, with many morphologically young lava flows on its flanks. It also has persistent fumaroles.

Geographic entities mentioned:
surface_form: Olca
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -20.933333333333
lon: -68.483333333333
surface_form: paruma
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -20.933333333333
lon: -68.483333333333
Paruma. Paruma is a stratovolcano that lies on the border of Bolivia and Chile. It is part of a ridge that contains several stratovolcanos. Paruma lies at the eastern end of the ridge, with Olca to its west. The older volcano Paruma lies to east of Paruma. Paruma has clearly been active during the Holocene, with many morphologically young lava flows on its flanks. It also has persistent fumaroles.

Geographic entities mentioned:
surface_form: paruma
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -20.933333333333
lon: -68.483333333333
Paruma. Paruma is a stratovolcano that lies on the border of Bolivia and Chile. It is part of a ridge that contains several stratovolcanos. Paruma lies at the eastern end of the ridge, with Olca to its west. The older volcano Paruma lies to east of Paruma. Paruma has clearly been active during the Holocene, with many morphologically young lava flows on its flanks. It also has persistent fumaroles.

Geographic entities mentioned:
surface_form: paruma
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -20.933333333333
lon: -68.483333333333
surface_form: paruma
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -20.933333333333
lon: -68.483333333333
Paruma lies at the eastern end of the ridge, with Olca to its west. The older volcano Paruma lies to east of Paruma. Paruma has clearly been active during the Holocene, with many morphologically young lava flows on its flanks. It also has persistent fumaroles. One lava flow in particular extends for 7 kilometres to the south-east of the peak.

Geographic entities mentioned:
surface_form: paruma
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -20.933333333333
lon: -68.483333333333
Șureanu Mountains. The Șureanu Mountains (German: &quot;Mühlbacher Gebirge&quot;, Hungarian: &quot;Kudzsiri-havasok&quot;), belong to Romania's Parâng range in the Southern Carpathians, with peaks frequently exceeding. The mountains are located north of Romania's Jiu Valley, in the Hunedoara and Alba counties. They border the Cindrel Mountains to the east and the Lotru Mountains to the southeast.

Geographic entities mentioned:
surface_form: Jiu Valley
instance_of: Valley
countries: Romania
coordinates: lat: 43.77805556
lon: 23.81333333
Årefjellet. Årefjellet is a mountain in Oscar II Land on the island of Spitsbergen, Svalbard. It has a maximum elevation of 882 m, and is located at the northern part of the ridge Jämtlandryggen. It borders to the glaciers Sveabreen and Wahlenbergbreen.

Geographic entities mentioned:
surface_form: Jämtlandryggen
instance_of: Mountain
countries: Norway
coordinates: lat: 78.6113
lon: 13.8513
Årefjellet. Årefjellet is a mountain in Oscar II Land on the island of Spitsbergen, Svalbard. It has a maximum elevation of 882 m, and is located at the northern part of the ridge Jämtlandryggen. It borders to the glaciers Sveabreen and Wahlenbergbreen.

Geographic entities mentioned:
surface_form: årefjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 78.6656
lon: 13.5648
After the war, the bodies were reused on Peerless lorry chassis. Some of these were still in service at the start of the Second World War. Some cars were sent to the Caspian Sea region. Austins were also used by the British in the Irish War of Independence.

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
Thamankaduwa Divisional Secretariat. Thamankaduwa Divisional Secretariat is a Divisional Secretariat of Polonnaruwa District, of North Central Province, Sri Lanka. It contains Parakrama Samudra and the historic ruins of the Polonnaruwa period. Geography. Thamankaduwa DS division is in extent, with 55 Grama Niladhari divisions, 117 villages, and a population of 94,254.

Geographic entities mentioned:
surface_form: Parakrama Samudra
instance_of: Lake
countries: Sri Lanka
coordinates: lat: 7.9
lon: 80.966666666667
946) therefore scriptures of Rastrakuta and Chalukyas of Kalyana dynasties shows the existence of this village goes back to ninth and 10th century and it is also ruled by Maratha king Shivaji and Peshwas of 17th and 18th century. This village name may be derived from old name of ‘’(Deccan Plains) or which means region consisting of 300 villages and also means fertile land.

Geographic entities mentioned:
surface_form: Deccan Plains
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
The hardest part was to pass the smooth crag &quot;Mysosten&quot;, which Rubenson finger traversed along a tiny crack. After this passage there was an easy climb to the summit. The same three climbers continued their 1910 tour by making first ascents of the Lofoten summits Svolværgeita and Trakta. Arne Næss, Ralph Høibakk, and K.

Geographic entities mentioned:
surface_form: Svolværgeita
instance_of: Mountain
countries: Norway
coordinates: lat: 68.246111111111
lon: 14.588333333333
surface_form: svolværgeita
instance_of: Mountain
countries: Norway
coordinates: lat: 68.246111111111
lon: 14.588333333333
surface_form: trakta
instance_of: Mountain
countries: Norway
coordinates: lat: 68.3364
lon: 14.8842
Stetinden (Narvik). or is a mountain in Narvik Municipality in Nordland county, Norway. It is located about northeast of the village of Kjøpsvik. The mountain has very smooth sides reaching all the way to the fjord. Stetinden has an obelisk-shape which gives it a very distinct look. In 2002 it was voted to be the &quot;National Mountain&quot; of Norway by listeners of NRK.

Geographic entities mentioned:
surface_form: stetinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.55
lon: 8.19638889
surface_form: stetinden (narvik)
instance_of: Mountain
countries: Norway
coordinates: lat: 68.165
lon: 16.5925
It is located about northeast of the village of Kjøpsvik. The mountain has very smooth sides reaching all the way to the fjord. Stetinden has an obelisk-shape which gives it a very distinct look. In 2002 it was voted to be the &quot;National Mountain&quot; of Norway by listeners of NRK. The coat of arms of Narvik Municipality is based on the silhouette of this mountain. Climbing.

Geographic entities mentioned:
surface_form: stetinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.55
lon: 8.19638889
surface_form: stetinden
instance_of: Mountain
countries: Norway
coordinates: lat: 68.165
lon: 16.5925
That cairn is now called &quot;Halls fortopp&quot; (elevation). In 1904, William Cecil Slingsby also failed to reach the summit. It was not until 30 July 1910 that Ferdinand Schjelderup, Carl Wilhelm Rubenson, and Alf Bonnevie Bryn finally reached the summit of Stetind. The weather conditions were good. It was Rubenson's 25th birthday, and he was given the honor of being first in the rope.

Geographic entities mentioned:
surface_form: stetind
instance_of: Mountain
countries: Norway
coordinates: lat: 61.55
lon: 8.19638889
surface_form: stetind
instance_of: Mountain
countries: Norway
coordinates: lat: 68.165
lon: 16.5925
After this passage there was an easy climb to the summit. The same three climbers continued their 1910 tour by making first ascents of the Lofoten summits Svolværgeita and Trakta. Arne Næss, Ralph Høibakk, and K. Friis Baasted did the first winter climb of Stetind in 1963 on the eastern wall. In 1966, Arne Næss and four others were the first ones to summit via the west wall. Name.

Geographic entities mentioned:
surface_form: stetind
instance_of: Mountain
countries: Norway
coordinates: lat: 61.55
lon: 8.19638889
surface_form: stetind
instance_of: Mountain
countries: Norway
coordinates: lat: 68.165
lon: 16.5925
Name. The shape of the mountain has been compared with a &quot;ste&quot; which means &quot;anvil&quot; and the last element is the finite form of &quot;tind&quot; which means &quot;mountain peak&quot;. Slingsby characterized Stetind as the ugliest mountain he ever saw. Tourism. Stetind is not a particularly popular tourist destination, despite being Norway's national mountain.

Geographic entities mentioned:
surface_form: stetind
instance_of: Mountain
countries: Norway
coordinates: lat: 61.55
lon: 8.19638889
surface_form: stetind
instance_of: Mountain
countries: Norway
coordinates: lat: 68.165
lon: 16.5925
It is the most forested provincial-level administrative region in China, with a 62.96% forest coverage rate in 2009. Fujian's highest point is Mount Huanggang in the Wuyi Mountains, with an altitude of. Fujian faces East China Sea to the east, South China Sea to the south, and the Taiwan Strait to the southeast. The coastline is rugged and has many bays and islands.

Geographic entities mentioned:
surface_form: Mount Huanggang
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 27.8606
lon: 117.784
Around Meizhou Islands is the Matsu pilgrimage. Natural features. Mount Taimu is a mountain and a scenic resort in Fuding. It offers a grand view of mountains and sea and is famous for its natural scenery including granite caves, odd-shaped stones, cliffs, clear streams, cascading waterfalls, and cultural attractions such as ancient temples and cliff Inscriptions.

Geographic entities mentioned:
surface_form: Mount Taimu
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 27.1244
lon: 120.182
The Wuyi Mountains was the first location in Fujian to be listed by UNESCO as one of the World Heritage Sites in 1999. They are a mountain range in the prefecture of Nanping and contain the highest peak in Fujian, Mount Huanggang. It is famous as a natural landscape garden and a summer resort in China. Notable individuals.

Geographic entities mentioned:
surface_form: Mount Huanggang
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 27.8606
lon: 117.784
According to the Syrian Central Bureau of Statistics, it had a population of 3,956 in the 2004 census. The village sits by the confluence of the Allan and Ehreir streams, overlooking the deep gorge where the streams meet. It is near the approaches to the Yarmuk river, which represents the border between Syria and Jordan. Ottoman period.

Geographic entities mentioned:
surface_form: Allan
instance_of: Watercourse
countries: Syria
coordinates: lat: 32.729722222222
lon: 35.898055555556
Mount Pahia. Mount Pahia is a mountain located in the South Pacific, on the island of Bora Bora. With an elevation of 661 metres (2,169 ft) above sea level, it is the second-highest point of the island, after the neighboring Mount Otemanu. Mount Pahia is an extinct volcano forming two twin peaks. The mountain is in the center of the island next to Mount Otemanu.

Geographic entities mentioned:
surface_form: Mount Otemanu
instance_of: Mountain
countries: France
coordinates: lat: -16.5
lon: -151.73333
surface_form: otemanu
instance_of: Mountain
countries: France
coordinates: lat: -16.5
lon: -151.73333
With an elevation of 661 metres (2,169 ft) above sea level, it is the second-highest point of the island, after the neighboring Mount Otemanu. Mount Pahia is an extinct volcano forming two twin peaks. The mountain is in the center of the island next to Mount Otemanu. The city of Vaitape sits at the base of the mountain.

Geographic entities mentioned:
surface_form: mount otemanu
instance_of: Mountain
countries: France
coordinates: lat: -16.5
lon: -151.73333
surface_form: otemanu
instance_of: Mountain
countries: France
coordinates: lat: -16.5
lon: -151.73333
Mount Pahia. Mount Pahia is a mountain located in the South Pacific, on the island of Bora Bora. With an elevation of 661 metres (2,169 ft) above sea level, it is the second-highest point of the island, after the neighboring Mount Otemanu. Mount Pahia is an extinct volcano forming two twin peaks. The mountain is in the center of the island next to Mount Otemanu.

Geographic entities mentioned:
surface_form: mount pahia
instance_of: Mountain
countries: France
coordinates: lat: -16.5
lon: -151.75
Quicksilver Rush. bxq61zy59ox2sxi7vpmx93lwmrgoj" xml:space="preserve">The Quicksilver Rush (ca. early 1930s) was a mining rush for cinnabar in southwest Arkansas and the Ozarks, mostly in Pike and Clark counties, beginning around 1931, in the early days of the Great Depression when people were desperate for jobs.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
His decision was understandably received with mixed feelings.&quot; Newspaper articles and reports from the time show part of the congregation happy with his exit, but others especially in the council quite attached and sorry to lose their &quot;beloved pastor.&quot; One correspondent states that Krakeel should have been the capital and that the pastor-preferring residents of that area, the Langkloof valley, had grounds for their own congregation.

Geographic entities mentioned:
surface_form: Langkloof
instance_of: Valley
countries: South Africa
coordinates: lat: -33.825
lon: 23.857777777778
Badenoch and Strathspey wards. † Area Convener (or &quot;Area Chairman&quot;)
Inverness wards. The Inverness area includes Loch Ness, Strathglass and the City of Inverness. The city lacks clearly defined boundaries. In ward descriptions below &quot;the city&quot; means the urban area centred on the former burgh of Inverness. † Area Convener (or &quot;Provost and Area Convener&quot;)
Nairn wards.

Geographic entities mentioned:
surface_form: Loch Ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
surface_form: Strathglass
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.35
lon: -4.7166666666667
The recreation area is named for Glen Canyon, which was flooded by the Glen Canyon Dam, completed in 1966, and is now mostly submerged beneath the waters of Lake Powell.

Geographic entities mentioned:
surface_form: Glen Canyon
instance_of: Valley
countries: United States
coordinates: lat: 36.86443
lon: -111.58794
She was 40; he was 29. He said that he was &quot;a mere complication of cough and bones, much fitter for an emblem of mortality than a bridegroom.&quot; He travelled with his new wife and her son Lloyd north of San Francisco to Napa Valley and spent a summer honeymoon at an abandoned mining camp on Mount Saint Helena (today designated Robert Louis Stevenson State Park).

Geographic entities mentioned:
surface_form: Mount Saint Helena
instance_of: Mountain
countries: United States
coordinates: lat: 38.669333333333
lon: -122.63355
The sculptor of the statue was Alan Herriot, and the money to erect it was raised by the Colinton Community Conservation Trust. Stevenson's house Skerryvore, at the head of Alum Chine, was severely damaged by bombs during a destructive and lethal raid in the Bournemouth Blitz. Despite a campaign to save it, the building was demolished.

Geographic entities mentioned:
surface_form: Alum Chine
instance_of: Valley
countries: United Kingdom
coordinates: lat: 50.712666666666664
lon: -1.8976944444444444
Samoa. Stevenson's former home in Vailima, Samoa, is now a museum dedicated to the later years of his life. The Robert Louis Stevenson Museum presents the house as it was at the time of his death along with two other buildings added to Stevenson's original one, tripling the museum in size. The path to Stevenson's grave at the top of Mount Vaea starts at the museum. France.

Geographic entities mentioned:
surface_form: Mount Vaea
instance_of: Mountain
countries: Samoa
coordinates: lat: -13.86666667
lon: -171.76666667
It flows generally eastward and southeastward, through Woodward, Major, Dewey, Blaine, Canadian, Oklahoma, Lincoln, Pottawatomie, Seminole, Hughes, Okfuskee, Okmulgee, and McIntosh counties, through the cities and towns of Woodward, Oklahoma City, and Shawnee. It is dammed near Canton to form Canton Lake in Blaine County, and in Oklahoma City to form Lake Overholser.

Geographic entities mentioned:
surface_form: Lake Overholser
instance_of: Lake
countries: United States
coordinates: lat: 35.4977
lon: -97.6796
Aftermath. Cree presumed that Osman had been wounded. Brooke, too, was unsure whether Osman was dead a day after the battle. In the Journal Mundy, he initially reported that Osman had been driven into the mountains. The newspaper Friend of China reported on September 17, 1845, that at the time of the report, ten Europeans and 30 men from Manila were still in Osman's captivity as slaves.

Geographic entities mentioned:
surface_form: mountains
instance_of: Mountain
countries: Malaysia
coordinates: lat: 6.075
lon: 116.5586111111111
Chrysoritis midas. &quot;Chrysoritis midas&quot;, the Midas opal, is a butterfly of the family Lycaenidae. It is found in South Africa, where it is found from the Roggeveld escarpment to Nuweveldberge in the Western Cape. The wingspan is 24–28 mm for males and 25–30 mm for females. Adults are on wing from September to November. There is one generation per year.

Geographic entities mentioned:
surface_form: Roggeveld
instance_of: Plateau
countries: South Africa
coordinates: lat: -32.2
lon: 20.71666667
By treaty dated September 26, 1833, ending the Black Hawk War, the Ojibwe, Ottawa and Potawatomi tribes ceded to the United States all lands from the west shore of Lake Michigan west to the area that the Winnebago tribe ceded in 1832, north to the area that the Menominees had previously ceded to the United States, and south to the area previously ceded by an 1829 treaty at Prairie du Chien, a total of approximately.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Distribution. Today, Guató is spoken in Guató Indigenous Territory and Baía dos Guató Indigenous Territory. Loukotka (1968) reported that in Mato Grosso do Sul, Brazil, Guató is spoken on the banks of the Paraguay River and up the São Lourenço River, along the Bolivian border. It is also spoken at Uberaba Lake in Santa Cruz Department (Bolivia). Phonology.

Geographic entities mentioned:
surface_form: Uberaba Lake
instance_of: Lake
countries: Bolivia
coordinates: lat: -17.505277777778
lon: -57.799444444444
Background. In 1872, John D. Rockefeller's Standard Oil bought 176 acres of land on Constable Hook in Bayonne and by 1885 there was a pipeline connecting it to the field of Texas. Standard Oil opened Bayway Refinery in Linden, New Jersey in 1909. The refinery is part of the iconic imagery of New Jersey, visible to all passing cars on the New Jersey Turnpike.

Geographic entities mentioned:
surface_form: Constable Hook
instance_of: Landform
countries: United States
coordinates: lat: 40.6578
lon: -74.0994
Background. The A Shau Special Forces Camp was located in the A Sầu Valley, about southwest of Huế and 2 km east of the Laos border in Thừa Thiên Province. The valley was strategically important for the PAVN as a major infiltration route because it served as a bridge from the Ho Chi Minh Trail in Laos into populated coastal areas of Thừa Thiên Province. The camp had been established in 1963.

Geographic entities mentioned:
surface_form: A Sầu Valley
instance_of: Valley
countries: Vietnam
coordinates: lat: 16.259305555556
lon: 107.2125
Niagara Escarpment. The property is located on the Niagara Escarpment and classified as Escarpment Protection Area by the Niagara Escarpment Commission, which limits use and development. In April 2004, an application was made for an amendment to rezone the property to Escarpment Recreation Area, and re-applied for in May 2008.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
Bedek Stream. Bedek Stream (,) is the 3.2 km long stream on eastern Byers Peninsula, Livingston Island in the South Shetland Islands, Antarctica draining the lakes of Oread and Montemno. It flows northwards along the west side of Urvich Wall and the east side of Tsamblak Hill, crosses Robbery Beaches and empties into Barclay Bay just east of Sparadok Point.

Geographic entities mentioned:
surface_form: Oread
instance_of: Lake
coordinates: lat: -62.646388888888886
lon: -60.97416666666667
surface_form: Montemno
instance_of: Lake
coordinates: lat: -62.64472222222222
lon: -60.97138888888889
Bedek Stream (,) is the 3.2 km long stream on eastern Byers Peninsula, Livingston Island in the South Shetland Islands, Antarctica draining the lakes of Oread and Montemno. It flows northwards along the west side of Urvich Wall and the east side of Tsamblak Hill, crosses Robbery Beaches and empties into Barclay Bay just east of Sparadok Point. The area was visited by early 19th century sealers.

Geographic entities mentioned:
surface_form: Tsamblak Hill
instance_of: Mountain
coordinates: lat: -62.6369
lon: -61.0019
He also competed in the 2010 World Series of Poker Main Event, but was eliminated on Day 2. Early life. Moon lived in the western Maryland town of Oakland, at the foot of Backbone Mountain. Prior to entering the World Series of Poker, Moon lived in a trailer with his wife, Wendy. Moon owned and operated a small logging company with other family members.

Geographic entities mentioned:
surface_form: Backbone Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.1472
lon: -79.57
In the 2018 New Zealand census, 1,734 people listed Ngāti Kauwhata as their iwi. Ancestors of the iwi came to New Zealand on the Tainui waka. They originally lived around Maungatautari in the Waikato. Large numbers of them migrated to the southern North Island in the 1820s. Mason Durie was a prominent leader in the 20th century.

Geographic entities mentioned:
surface_form: Maungatautari
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.019
lon: 175.576
Valley Connector. The Valley Connector Regional Shuttle and Commuter Bus was a public transportation service provided by S & W Tours, LLC and Valley Connector, Inc. that provided weekday commuter bus service in the United States from northern Shenandoah Valley to Northern Virginia and Washington, D.C. Commuter bus service was terminated on January 31, 2011.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Origination points in Frederick County, Clarke County and the City of Winchester area included the Waterloo Park-and-Ride and Berryville. Destination points in Northern Virginia and Washington, D.C. included Arlington County and Fairfax County. Other transit services in Northern Shenandoah Valley include Winchester Transit, Page County Transit, and Front Royal Area Transit.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
The historic Asia School is located in Decherd. Geography. Decherd is located at (35.215767, -86.079183). According to the United States Census Bureau, the city has a total area of, of which is land and 0.21% is water which is part of Tims Ford Lake. Decherd is immediately adjacent to the county seat of Winchester. 2020 census.

Geographic entities mentioned:
surface_form: Tims Ford Lake
instance_of: Lake
countries: United States
coordinates: lat: 35.196944444444
lon: -86.278611111111
He retired from practice at the age of 102. Biography. Uglov was born into a peasant family in Siberia near Lake Baikal. He was one of six children. Having matriculated from the Saratov State University in 1929, he later settled in Leningrad, where he saved lives of soldiers wounded during the Winter War.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Marandeh Valley. Marandeh Valley is a town and one of the beautiful valleys of Tehsil Torkhow, Khot, of Upper Chitral District in the province of Pakistan. Khot Valley is located 129 km from the main city of Chitral. The language of Chitral, Khowar, originated from this area.

Geographic entities mentioned:
surface_form: Chitral
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.85111111111111
lon: 71.78888888888889
Marandeh Valley. Marandeh Valley is a town and one of the beautiful valleys of Tehsil Torkhow, Khot, of Upper Chitral District in the province of Pakistan. Khot Valley is located 129 km from the main city of Chitral. The language of Chitral, Khowar, originated from this area.

Geographic entities mentioned:
surface_form: marandeh valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.17
lon: 72.31
Marandeh Valley. Marandeh Valley is a town and one of the beautiful valleys of Tehsil Torkhow, Khot, of Upper Chitral District in the province of Pakistan. Khot Valley is located 129 km from the main city of Chitral. The language of Chitral, Khowar, originated from this area.

Geographic entities mentioned:
surface_form: marandeh valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.17
lon: 72.31
surface_form: chitral
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.85111111111111
lon: 71.78888888888889
Marandeh Valley. Marandeh Valley is a town and one of the beautiful valleys of Tehsil Torkhow, Khot, of Upper Chitral District in the province of Pakistan. Khot Valley is located 129 km from the main city of Chitral. The language of Chitral, Khowar, originated from this area.

Geographic entities mentioned:
surface_form: chitral
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.85111111111111
lon: 71.78888888888889
surface_form: khot valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.88333333
lon: 71.8
A book entitled was written in 2012 by local historian Andrew Eccles and covers the entire history from 1837-2012. Upper Edge Baptist Church is located on Dewsbury Road. The church traces its history to &quot;Rossendale Church&quot;, which consisted of many Independent congregations located across the Rossendale Valley. Individual congregations became separate churches by about 1720.

Geographic entities mentioned:
surface_form: Rossendale Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.7031
lon: -2.2893
Lying in a tectonic depression on the northern slope of the Karatau Mountains, it is part of the Talas basin. The Asa river flows through the lake entering it from the east and flowing out from the north. The shores of the lake are sandy in places. Lake Akkol lies to the north of the northern end of Bilikol. Flora and fauna. Reeds grow on the lakeshore.

Geographic entities mentioned:
surface_form: Lake Akkol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 43.40388889
lon: 70.68833333
surface_form: bilikol
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 43.04565
lon: 70.70916
Bilikol. Bilikol (;) is a freshwater lake in the Zhambyl Region, Kazakhstan. The lake lies northwest of the city of Taraz. Its waters are used by the surrounding communities to irrigate crops. Geography. Lake Bilikol has a shape that roughly reminds of an hourglass. Lying in a tectonic depression on the northern slope of the Karatau Mountains, it is part of the Talas basin.

Geographic entities mentioned:
surface_form: bilikol
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 43.04565
lon: 70.70916
The lake lies northwest of the city of Taraz. Its waters are used by the surrounding communities to irrigate crops. Geography. Lake Bilikol has a shape that roughly reminds of an hourglass. Lying in a tectonic depression on the northern slope of the Karatau Mountains, it is part of the Talas basin. The Asa river flows through the lake entering it from the east and flowing out from the north.

Geographic entities mentioned:
surface_form: bilikol
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 43.04565
lon: 70.70916
He was also a member of the American Association for the Advancement of Science. Silliman College, one of Yale's residential colleges, is named for him, as is the mineral Sillimanite. In Sequoia National Park, Mount Silliman is named for him, as is Silliman Pass, a creek and two lakes below the summit of Mount Silliman.

Geographic entities mentioned:
surface_form: Mount Silliman
instance_of: Mountain
countries: United States
coordinates: lat: 36.6432761
lon: -118.6964871
After a rival official assassinated his father in 1141, Hōnen was initiated into his uncle's monastery at the age of 9. From then on, Hōnen lived his life as a monk and eventually studied at the famous monastery of Mount Hiei. He practiced traditional Tendai Buddhism for some time, but eventually became dissatisfied with it.

Geographic entities mentioned:
surface_form: Mount Hiei
instance_of: Mountain
countries: Japan
coordinates: lat: 35.066666666667
lon: 135.83833333333
Risimina Glacier. Risimina Glacier (,) is the 10 km long and 4.5 km wide glacier in Lovech Heights on Nordenskjöld Coast in Graham Land, Antarctica situated south of Zlokuchene Glacier and north of the lower course of Rogosh Glacier. It is draining the southeast slopes of Mount Moriya, and flowing east-southeastwards to enter Weddell Sea west of Pedersen Nunatak.

Geographic entities mentioned:
surface_form: Mount Moriya
instance_of: Mountain
coordinates: lat: -64.86277778
lon: -61.12972222
surface_form: Pedersen Nunatak
instance_of: Mountain
coordinates: lat: -64.9333
lon: -60.7333
In 1989, Flood was able to use the discovery of a cremated female skeleton to explain what life might have been like at Lake Mungo. Flood used this information to deduce the role of women in this Aboriginal society. Awards and prizes. In 1991, Flood was elected a Fellow of the Australian Academy of the Humanities (FAHA).

Geographic entities mentioned:
surface_form: Lake Mungo
instance_of: Lake
countries: Australia
coordinates: lat: -33.75
lon: 143.08333333333
It is a well-known tourist hiking spot and it is also known for its copper mines. It was sometimes called the &quot;mine mountain&quot;. Blåberg was the site of copper mining starting in the 18th century when rich sources of copper were found, and mining began on the mountain and surrounding valleys around the Årdalsfjorden which is part of the Sognefjord.

Geographic entities mentioned:
surface_form: årdalsfjorden
instance_of: Lake
countries: Norway
coordinates: lat: 58.708333333333
lon: 7.8069444444444
Blåberg. Blåberg is a mountain on the west side of the village of Øvre Årdal in Årdal Municipality in Vestland county, Norway. It is a well-known tourist hiking spot and it is also known for its copper mines. It was sometimes called the &quot;mine mountain&quot;.

Geographic entities mentioned:
surface_form: blåberg
instance_of: Mountain
countries: Norway
coordinates: lat: 61.3138
lon: 7.7633
Lake Modoc. Lake Modoc is a former lake in California and Oregon, in the location of present-day Upper Klamath Lake, Lower Klamath Lake and Tule Lake. It existed during the Pliocene and Pleistocene epochs, its formation probably influenced by volcanism and faulting. The bed of the former lake had plentiful resources for early humans, and today it is used for agriculture. Background.

Geographic entities mentioned:
surface_form: Upper Klamath Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.392222222222
lon: -121.88027777778
surface_form: Lower Klamath Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.99083983333333
lon: -121.74309983333333
surface_form: Tule Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.909322222222
lon: -121.53304722222
surface_form: lake modoc
instance_of: Lake
countries: United States
surface_form: tule lake
instance_of: Lake
countries: United States
coordinates: lat: 39.160206
lon: -122.945159
Background. It has been known for over a century that large lakes previously existed in the Western United States, most notably Nevada's Lake Lahontan and Utah's Lake Bonneville. Such lakes also formed in eastern Oregon, where present-day Malheur Lake and Goose Lake are remnants of former pluvial lakes. Lake Modoc was so named by Samuel N.

Geographic entities mentioned:
surface_form: Malheur Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.332777777778
lon: -118.79305555556
surface_form: goose lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9411888
lon: -121.7644477
surface_form: goose lake
instance_of: Lake
countries: United States
coordinates: lat: 44.8466112
lon: -97.2727864
surface_form: goose lake
instance_of: Lake
countries: United States
coordinates: lat: 41.967777777778
lon: -90.402222222222
surface_form: goose lake
instance_of: Lake
countries: United States
coordinates: lat: 47.0393356
lon: -122.7915002
surface_form: goose lake
instance_of: Lake
countries: United States
coordinates: lat: 61.1956
lon: -149.821
surface_form: goose lake
instance_of: Lake
countries: United States
coordinates: lat: 46.47021
lon: -87.52014
Several islands formed in the lake, such as the Klamath Hills, present-day Miller Hill close to Klamath Falls and Turkey Hill close to Malin. The shoreline of Lake Modoc is well visible close to Tule Lake. Hydrology. Unlike other pluvial lakes, Lake Modoc had a steady inflow of surface water, owing to its proximity to snow- and glacier-covered mountains of the Cascade Range.

Geographic entities mentioned:
surface_form: Tule Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.909322222222
lon: -121.53304722222
surface_form: lake modoc
instance_of: Lake
countries: United States
surface_form: tule lake
instance_of: Lake
countries: United States
coordinates: lat: 39.160206
lon: -122.945159
Water levels began to decrease as the Pleistocene ended, as the climate became drier and the outlet to the Klamath River lower. The former lake floor is nearly level, and the shoreline is almost unwarped. Today, Tule Lake, Upper Klamath Lake and Lower Klamath Lake remain from Lake Modoc; Upper Klamath Lake is the largest present-day lake in Oregon by surface area.

Geographic entities mentioned:
surface_form: Tule Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.909322222222
lon: -121.53304722222
surface_form: Upper Klamath Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.392222222222
lon: -121.88027777778
surface_form: Lower Klamath Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.99083983333333
lon: -121.74309983333333
surface_form: upper klamath lake
instance_of: Lake
countries: United States
coordinates: lat: 42.392222222222
lon: -121.88027777778
surface_form: lake modoc
instance_of: Lake
countries: United States
surface_form: tule lake
instance_of: Lake
countries: United States
coordinates: lat: 39.160206
lon: -122.945159
History. Lake Modoc was probably formed by geologic processes such as faulting or by the Medicine Lake Volcano blocking a former southward-draining outlet. The lake appears to have existed during the Pleistocene and late Pliocene, with some lake deposits estimated to be at least 3 million years old. During marine oxygen isotope stage 4, Lake Modoc was deep and cold.

Geographic entities mentioned:
surface_form: medicine lake
instance_of: Lake
countries: United States
coordinates: lat: 45.00644
lon: -93.41997
surface_form: lake modoc
instance_of: Lake
countries: United States
surface_form: medicine lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9841655
lon: -97.3519987
It covered a length of from south of Tule Lake in California to near present-day Fort Klamath in Oregon, its waters reaching an elevation of about above sea level and covering an area of about with a highly irregular shape. Several islands formed in the lake, such as the Klamath Hills, present-day Miller Hill close to Klamath Falls and Turkey Hill close to Malin.

Geographic entities mentioned:
surface_form: turkey hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.0178
lon: -76.4441
Lake Modoc. Lake Modoc is a former lake in California and Oregon, in the location of present-day Upper Klamath Lake, Lower Klamath Lake and Tule Lake. It existed during the Pliocene and Pleistocene epochs, its formation probably influenced by volcanism and faulting. The bed of the former lake had plentiful resources for early humans, and today it is used for agriculture. Background.

Geographic entities mentioned:
surface_form: lake modoc
instance_of: Lake
countries: United States
It has been known for over a century that large lakes previously existed in the Western United States, most notably Nevada's Lake Lahontan and Utah's Lake Bonneville. Such lakes also formed in eastern Oregon, where present-day Malheur Lake and Goose Lake are remnants of former pluvial lakes. Lake Modoc was so named by Samuel N. Dicken, professor of geography at the University of Oregon.

Geographic entities mentioned:
surface_form: lake modoc
instance_of: Lake
countries: United States
Lake Modoc was so named by Samuel N. Dicken, professor of geography at the University of Oregon. The region of Lake Modoc was first described during the early and mid-19th century. The lake. Lake Modoc was a pluvial lake that existed during the Pleistocene in basins formed by faulting and volcanism.

Geographic entities mentioned:
surface_form: lake modoc
instance_of: Lake
countries: United States
The lake. Lake Modoc was a pluvial lake that existed during the Pleistocene in basins formed by faulting and volcanism. It covered a length of from south of Tule Lake in California to near present-day Fort Klamath in Oregon, its waters reaching an elevation of about above sea level and covering an area of about with a highly irregular shape.

Geographic entities mentioned:
surface_form: lake modoc
instance_of: Lake
countries: United States
Hydrology. Unlike other pluvial lakes, Lake Modoc had a steady inflow of surface water, owing to its proximity to snow- and glacier-covered mountains of the Cascade Range. Its watershed extended over present-day Modoc and Siskiyou counties (both in California), and Jackson, Klamath and Lake counties (all in Oregon), including the Williamson River, Sprague River and Lost River.

Geographic entities mentioned:
surface_form: lake modoc
instance_of: Lake
countries: United States
Cinder, pumice and volcanic ash from the Cascades filled the lake. Lake Modoc also featured an outflow, at first to the south before a lava flow blocked it, although seepage continued from there to this day. Presently, the Klamath River drains the area.

Geographic entities mentioned:
surface_form: lake modoc
instance_of: Lake
countries: United States
Lake Modoc also featured an outflow, at first to the south before a lava flow blocked it, although seepage continued from there to this day. Presently, the Klamath River drains the area. Given that the basin at present cannot hold a lake the size of Lake Modoc, it is likely that its formation and demise was influenced by the existence of outlets. History.

Geographic entities mentioned:
surface_form: lake modoc
instance_of: Lake
countries: United States
The lake appears to have existed during the Pleistocene and late Pliocene, with some lake deposits estimated to be at least 3 million years old. During marine oxygen isotope stage 4, Lake Modoc was deep and cold. Volcanic eruptions formed tuff cones in the lake, such as at The Peninsula.

Geographic entities mentioned:
surface_form: lake modoc
instance_of: Lake
countries: United States
The lake. Lake Modoc was a pluvial lake that existed during the Pleistocene in basins formed by faulting and volcanism. It covered a length of from south of Tule Lake in California to near present-day Fort Klamath in Oregon, its waters reaching an elevation of about above sea level and covering an area of about with a highly irregular shape.

Geographic entities mentioned:
surface_form: tule lake
instance_of: Lake
countries: United States
coordinates: lat: 41.909322222222
lon: -121.53304722222
surface_form: tule lake
instance_of: Lake
countries: United States
coordinates: lat: 39.160206
lon: -122.945159
The former lake bed is now used as cropland, and agriculture is the most prevalent human land use in the region. Part of the southern shoreline has been covered by lava flows, and geologic processes have continued into the Holocene; the Glass Mountain lava flow was emplaced about 1,000 years ago, and some Holocene lava flows have been faulted.

Geographic entities mentioned:
surface_form: glass mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.7749
lon: -118.709
It has been described as being a &quot;district of Bootjack&quot; or in Bootjack, but it is a separate town. The town consists almost entirely of the Dreamland Inn (sometimes called the Dreamland Bar & Restaurant, Dreamland Hotel or &quot;Dreamland Hotel and bar;&quot; it is often referred to as being in Lake Linden—due to that being its mailing address) and some docks on Torch Bay. History.

Geographic entities mentioned:
surface_form: Torch Bay
instance_of: Lake
countries: United States
coordinates: lat: 47.087024
lon: -88.443159
The producer had come across his shorts and offered Tatum $30,000 to shoot a feature. The pair previously attempted, unsuccessfully, to finance the project via gambling. The cabin in the film was in Frazier Mountain, California, where the production team broke a family heirloom of the owner, which mirrors the breaking of the Blueberry horse statue in the movie. Release.

Geographic entities mentioned:
surface_form: Frazier Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.775
lon: -118.969
Mexico City. Scott's force arrived in the Valley of Mexico in August 1847, by which time Santa Anna had formed an army of approximately 25,000 men. Because Mexico City lacked walls and was essentially indefensible, Santa Anna sought to defeat Scott in a pitched battle, choosing to mount a defense near the Churubusco River several miles south.

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
Blatné (lake). Blatné is a lake in Slovakia. It covers an area of.

Geographic entities mentioned:
surface_form: blatné
instance_of: Lake
countries: Slovakia
coordinates: lat: 49.00277778
lon: 19.1625
The heaviest impact occurred at the bay front, in Davis Shores, and along the San Sebastian River. At Slave Market Square, floodwaters were &quot;hip deep&quot;, while floodwaters outside the Monson Motor Lodge was described as &quot;hubcap deep&quot;. &quot;The St. Augustine Record&quot; office was submerged, while some motel lobbies along the Matanzas River were flooded with of water.

Geographic entities mentioned:
surface_form: Matanzas River
instance_of: Landform
countries: United States
coordinates: lat: 29.9138577
lon: -81.2836827
This will bypass the towns to the south, with a new crossing of the River Finn. The N15 runs for over in County Sligo, passing north of the Dartry Mountains and around Benbulbin before passing Drumcliff Bay to enter Sligo Town. A bypass of the entire route was planned, with dual carriageway for at least part of the route.

Geographic entities mentioned:
surface_form: Benbulbin
instance_of: Mountain
countries: Ireland
coordinates: lat: 54.366666666667
lon: -8.4666666666667
palustris&quot; in 1809. Karl Ludwig Philipp Zeyher collected a specimen in the Kleinrivier Mountains, that was described by Carl Meissner, in 1856, in the series Prodromus Systematis Naturalis Regni Vegetabilis by Alphonse Pyramus de Candolle. He called it &quot;M. decapitata&quot;. John Patrick Rourke in 1984 regarded the specimens as belonging to the same species. Distribution and habitat.

Geographic entities mentioned:
surface_form: Kleinrivier Mountains
instance_of: Mountain
countries: South Africa
coordinates: lat: -34.3833
lon: 19.4167
John Patrick Rourke in 1984 regarded the specimens as belonging to the same species. Distribution and habitat. &quot;Mimetes palustris&quot; is an endemic species restricted to the Kleinrivier Mountains, Western Cape province of South Africa, where it can be found between the Platberg in the Fernkloof Nature Reserve near Hermanus in the west and slightly east of the Rocklands Peak.

Geographic entities mentioned:
surface_form: Kleinrivier Mountains
instance_of: Mountain
countries: South Africa
coordinates: lat: -34.3833
lon: 19.4167