Sarmila/GeoWiki-Features huggingface dataset:
His feast day is celebrated on 24 August, the date of his martyrdom. Life. Kosmas was born in the Greek village of Mega Dendron near the town of Thermo in the region of Aetolia. He studied Greek and theology before becoming a monk after a trip to Mount Athos, where he also attended the local Theological Academy. After two years Kosmas left Athos. He studied rhetoric in Constantinople for a time.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Lepontic language. Lepontic is an ancient Alpine Celtic language that was spoken in parts of Rhaetia and Cisalpine Gaul (now Northern Italy) between 550 and 100 BC. Lepontic is attested in inscriptions found in an area centered on Lugano, Switzerland, and including the Lake Como and Lake Maggiore areas of Italy.

Geographic entities mentioned:
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
1922 Lupeni mine disaster. The 1922 Lupeni mine disaster was a coal mining explosion at the Lupeni Coal Mine district in the Jiu Valley of Greater Romania, on April 27, 1922. A total of 82 miners were killed. Accident. The U.S.

Geographic entities mentioned:
surface_form: Jiu Valley
instance_of: Valley
countries: Romania
coordinates: lat: 43.77805556
lon: 23.81333333
The final delay, as of May 2014, was negotiations with the borough of Gustavo A. Madero to install a transmitter on Cerro del Chiquihuite. The Congress eventually planned to sign on additional broadcast transmitters to extend Canal del Congreso's over-the-air reach; however, the primary avenue of broadcast expansion has since been changed to SPR transmitters.

Geographic entities mentioned:
surface_form: Cerro del Chiquihuite
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.5328
lon: -99.1306
Feats. Konyukhov is the only person to have reached such extreme points of the planet as the North Pole (three times), the South Pole, the Pole of Inaccessibility in the Arctic Ocean and the top of Mount Everest (twice) and also sailed around the world via Cape Horn 4 times. He is also the first Russian to have climbed the three highest peaks in the world. Mount Everest, K2 and Kangchenjunga.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Konyukhov is the only person to have reached such extreme points of the planet as the North Pole (three times), the South Pole, the Pole of Inaccessibility in the Arctic Ocean and the top of Mount Everest (twice) and also sailed around the world via Cape Horn 4 times. He is also the first Russian to have climbed the three highest peaks in the world. Mount Everest, K2 and Kangchenjunga. Sailing.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
surface_form: K2
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
surface_form: Kangchenjunga
instance_of: Mountain
countries: India
Nepal
coordinates: lat: 27.7
lon: 88.133333
Mount Kiev is the highest point in the Endicott Mountains which are a subrange of the Brooks Range. It is set west of the Dalton Highway on the northeast boundary of Gates of the Arctic National Park and Preserve. Precipitation runoff from the mountain drains east into tributaries of the Atigun River and west into tributaries of the Itikmalac River which in turn flows into the Itkillik River.

Geographic entities mentioned:
surface_form: Atigun River
instance_of: Watercourse
countries: United States
coordinates: lat: 68.1219444
lon: -149.4591667
Topographic relief is significant as the summit rises approximately above the Atigun Valley in and above the Itikmalac Valley in. Galbraith Lake is to the north-northeast, whereas the Continental Divide and Atigun Pass are to the south. The nearest community is Prudhoe Bay, to the north. The mountain's toponym has not been officially adopted by the United States Board on Geographic Names. Climate.

Geographic entities mentioned:
surface_form: Galbraith Lake
instance_of: Lake
countries: United States
coordinates: lat: 68.4584432
lon: -149.416606
&quot;Citrullus colocynthis&quot; is a desert viney plant that grows in sandy, arid soils. It is native to the Mediterranean Basin and Asia, and is distributed among the west coast of northern Africa, eastward through the Sahara, Egypt until India, and reaches also the north coast of the Mediterranean and the Caspian Seas. It grows also in Southern Europe and on the Aegean Islands.

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
Ancient Diocese of Stavanger. The former Catholic Diocese of Stavanger in Norway included the modern counties of Rogaland and Agder together with the regions of Valdres and Hallingdal and the parishes of Eidfjord and Røldal from Hordaland. It existed from the beginning of the 12th century to the Protestant Reformation. History.

Geographic entities mentioned:
surface_form: Valdres
instance_of: Valley
countries: Norway
coordinates: lat: 60.916666666667
lon: 9.1666666666667
surface_form: Hallingdal
instance_of: Valley
countries: Norway
coordinates: lat: 60.633333333333
lon: 9.05
It has since disappeared. Bishop Audum Eivindssön (1426 – 1455) built many churches and gave the episcopal tithes of Valdres to the Brigittines of Munkeliv Abbey near Bergen in 1441 in their hour of need. The last Catholic bishop was Hoskuld Hoskuldsson (1513 – 1537), who was taken prisoner by Thord Rod at Bergen and died there.

Geographic entities mentioned:
surface_form: Valdres
instance_of: Valley
countries: Norway
coordinates: lat: 60.916666666667
lon: 9.1666666666667
Taxonomy. The species was formally described as new to science in 2018 by the lichenologists André Aptroot and Marcela Eugenia da Silva Cáceres. The type specimen was collected by the authors from the Morro do Pai Inácio (in Chapada Diamantina National Park) at an elevation between; here the lichen was found growing on siliceous sandstone rock in a transitional forest. Description.

Geographic entities mentioned:
surface_form: Morro do Pai Inácio
instance_of: Mountain
countries: Brazil
coordinates: lat: -12.4575
lon: -41.47305556
William James Loudon. William James Loudon (June 25, 1860 – September 27, 1951) was a Canadian geologist and amateur photographer in Ontario. Mount Loudon (10, 568 ft./3,221 m) in Banff National Park, Alberta is named in his honour.

Geographic entities mentioned:
surface_form: Mount Loudon
instance_of: Mountain
countries: Canada
coordinates: lat: 51.91675
lon: -116.43546
17th Virginia Cavalry Regiment. The 17th Virginia Cavalry Regiment was a cavalry regiment raised in Virginia for service in the Confederate States Army during the American Civil War. It fought with the Army of Northern Virginia, in southwestern Virginia, and in the Shenandoah Valley.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Nansok Sallah (1966?- 19 January 2012) is a journalist who was killed in Nigeria preceding a major attack by the Boko Haram terrorist group. Personal. Nansok Sallah was 46 years old when he was killed. He was from Langtang, Nigeria. Career. Sallah, who worked at Plateau State Radio and Television and Cool FM in Abuja before joining Highland FM radio, which is a government-owned station Jos.

Geographic entities mentioned:
surface_form: Langtang
instance_of: Valley
countries: Nepal
coordinates: lat: 28.25
lon: 85.5
Several of these buildings may also be found at the Kiekeberg Open Air Museum (&quot;Freilichtmuseum am Kiekeberg&quot;) and the Volksdorf Museum Village (&quot;Museumsdorf Volksdorf&quot;) in Hamburg; Examples from the eastern part of the &quot;Hallenhaus&quot; region are displayed in the Schwerin-Mueß Open Air Museum (&quot;Freilichtmuseum Schwerin-Mueß&quot;).

Geographic entities mentioned:
surface_form: Kiekeberg
instance_of: Mountain
countries: Germany
coordinates: lat: 53.4369
lon: 9.89944
Six Nepalese youths went to World Youth Day 2005 in Cologne, Germany. In a display of inter-religious cooperation, the Olympic torch was brought to the top of the sacred mountain of Makalu, having been blessed by both Pope Benedict XVI and the Dalai Lama. On February 10, 2007, Pope Benedict XVI raised the status of the missionary jurisdiction to an apostolic vicariate.

Geographic entities mentioned:
surface_form: Makalu
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.889166666667
lon: 87.088611111111
Geography. The river begins at Outlet Bay on Pakashkan Lake about northeast of the community of Upsala. It flows north through Brightsand Lake and further to Wapakaimaski Lake. The river splits with one channel flowing west into Seseganaga Lake and further into Kawaweogama Lake; the other flows north through Antler Lake and McEwan Lake.

Geographic entities mentioned:
surface_form: Seseganaga Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.09
lon: -90.354
surface_form: Kawaweogama Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.1994
lon: -90.1861
Lockyer Valley. The Lockyer Valley is an area of rich farmlands that lies to the west of Brisbane, Queensland, Australia and east of Toowoomba. The Lockyer Valley is rated among the top ten most fertile farming areas in the world, and the intensively cultivated area grows the most diverse range of commercial fruit and vegetables of any area in Australia.

Geographic entities mentioned:
surface_form: lockyer valley
instance_of: Valley
countries: Australia
coordinates: lat: -27.558833333333
lon: 152.27816666667
Such measures largely confine future development to non-arable land on the slopes of the hills. Geography. The valley is enclosed on either side by the Great Dividing Range and lies within the Lockyer Valley Region local government area. The largest town in the Lockyer Valley is Gatton, followed by the towns of Laidley, Withcott, and Plainland.

Geographic entities mentioned:
surface_form: lockyer valley
instance_of: Valley
countries: Australia
coordinates: lat: -27.558833333333
lon: 152.27816666667
Geography. The valley is enclosed on either side by the Great Dividing Range and lies within the Lockyer Valley Region local government area. The largest town in the Lockyer Valley is Gatton, followed by the towns of Laidley, Withcott, and Plainland. Other notable centres include Hatton Vale, Helidon, Forest Hill, Grantham, and Murphys Creek.

Geographic entities mentioned:
surface_form: lockyer valley
instance_of: Valley
countries: Australia
coordinates: lat: -27.558833333333
lon: 152.27816666667
12 different land types have been identified in the valley. The banks of waterways in the Lockyer Valley have been identified as the source of silt, which caused problems for the Mount Crosby Pumping Station during Cyclone Oswald. In 2014, $8 million was allocated to prevent soil erosion within the Lockyer Valley. History.

Geographic entities mentioned:
surface_form: lockyer valley
instance_of: Valley
countries: Australia
coordinates: lat: -27.558833333333
lon: 152.27816666667
History. The valley was once home to the Kitabul people before the arrival of Europeans in the early 19th century. Today, the Jagera people are considered the traditional owners of the Lockyer Valley region. One of the first white people known to the Indigenous people in the area was said to be &quot;Boralcho&quot; Baker, who lived with the Jagera people from 1826 for 18 years.

Geographic entities mentioned:
surface_form: lockyer valley
instance_of: Valley
countries: Australia
coordinates: lat: -27.558833333333
lon: 152.27816666667
Climate. With an average annual rainfall of 780 mm, the Lockyer Valley is the driest part of South East Queensland. Rainfall is highly variable and droughts are experienced regularly. The Lockyer Valley typically experiences temperatures higher than the Brisbane region in summer, but colder in the winter.

Geographic entities mentioned:
surface_form: lockyer valley
instance_of: Valley
countries: Australia
coordinates: lat: -27.558833333333
lon: 152.27816666667
Many council-owned bridges in the valley were either completely gone or partially destroyed. To repair roads and drains the Lockyer Valley Region local government area initially estimated the repair bill to be A$176 million. In 2012, a solar powered, radar based, imaging system was installed to detect dramatic rises in creek water levels.

Geographic entities mentioned:
surface_form: lockyer valley
instance_of: Valley
countries: Australia
coordinates: lat: -27.558833333333
lon: 152.27816666667
A variable climate and all year cropping has placed significant strain on water supply from groundwater aquifers. The viability of agriculture in the Lockyer Valley has been questioned after unreliable rains during drought, pest outbreaks and crop damage during severe weather have led to a decrease in agricultural productivity.

Geographic entities mentioned:
surface_form: lockyer valley
instance_of: Valley
countries: Australia
coordinates: lat: -27.558833333333
lon: 152.27816666667
Recycled wastewater from the Western Corridor Recycled Water Scheme could be used for irrigation in the Lockyer. The infrastructure is in place however the cost is prohibitive. Nearly all the nation's processing beetroot is grown in the Lockyer Valley. In 2002, the number of beetroot farmers had reduced to just eight farms. Golden Circle sources vegetables from the Lockyer Valley.

Geographic entities mentioned:
surface_form: lockyer valley
instance_of: Valley
countries: Australia
coordinates: lat: -27.558833333333
lon: 152.27816666667
Kloshe Nanitch Lookout. Kloshe Nanitch Lookout was built in the 1920s as a look out to spot fires in the Lake Crescent area of the Olympic Peninsula, Washington. The current structure is a replica of this structure, providing views of Lake Crescent, Mount Olympus (Washington), Lake Pleasant (Washington), and the Sol Duc Valley. It is located within the Olympic National Forest.

Geographic entities mentioned:
surface_form: Lake Crescent
instance_of: Lake
countries: United States
coordinates: lat: 48.0595755
lon: -123.8291037
The founder of the dynasty, Gulab Singh, was an influential noble in the court of the Sikh emperor Maharaja Ranjit Singh, while his brother Dhian Singh served as the prime minister of the Sikh Empire. Appointed by Ranjit Singh as the hereditary Raja of the Jammu principality, Gulab Singh established his supremacy over all the hill states surrounding the Kashmir Valley.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
John Wiswall says war makes farming glebe difficult because of high price of labour (with so many men away) and other things (except grain)
Halifax emergency caused by &quot;immense quantities of Snow [in] few days&quot; cutting off food supplies is ended by citizen and army efforts
Resident aliens (&quot;not being natural born Subjects[...]or Denizens, nor Persons duly Naturalized&quot;) are required to get special permit from government
&quot;Hurricane&quot; strikes Halifax, driving ships on shore, dragging away wharves with ships moored to them, and destroying stores containing merchanise
Map: Halifax harbour, including approaches, Bedford Basin, and nearby communities (Note: north is at bottom of page)
Having built house, storehouse, shipyard and 5 wharves on Sissiboo River, petitioner requests land for grist and sawmill
Where 1792 freshet shifted Truro channel, 50 acres of marshland created could be secured &quot;with Proper Materials,&quot; to public's and petitioner's benefit
Castaways on Sable Island survive 3 winter months in hut with chimney that they cover and line with cloth from wreck, living on ship provisions
Lady Wentworth's departure leaves N.S.

Geographic entities mentioned:
surface_form: Sissiboo River
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.412388888889
lon: -66.005888888889
North Head Quarantine Station. The North Head Quarantine Station is a heritage-listed former quarantine station and associated buildings that is now a tourist attraction at North Head Scenic Drive, on the north side of Sydney Harbour at North Head, near Manly, in the Northern Beaches Council local government area of New South Wales, Australia.

Geographic entities mentioned:
surface_form: North Head
instance_of: Landform
countries: Australia
coordinates: lat: -33.8368
lon: 151.281
Early life. MacTavish was born around 1787 in Stratherrick, Invernesshire, Scotland into Clan MacTavish. He was the son of Alexander MacTavish (1753–1788) and Marjory (née Fraser) MacTavish (1758–1828), and a nephew of Scots-Quebecer entrepreneur Simon McTavish, who took him in to raise after his father's death.

Geographic entities mentioned:
surface_form: Stratherrick
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.25
lon: -4.42
Planina pod Golico. Planina pod Golico (;) is a mountain village in the Municipality of Jesenice, in the Upper Carniola region of Slovenia. It lies on the southern foot of Mount Golica in the Karawanks range, at an elevation of. Name.

Geographic entities mentioned:
surface_form: Golica
instance_of: Mountain
countries: Austria
Slovenia
coordinates: lat: 46.491465
lon: 14.054569
The plants have been protected by law since 1949 and picking them is strictly forbidden. A narcissus festival is held by the local tourist association in May. The chairlift for the &quot;Španov vrh&quot; ski slope also begins in Planina pod Golico. There is also a natural luge track beyond the village in the Sava Caves area and competitions are held by the Jesenice Luge Club here every winter.

Geographic entities mentioned:
surface_form: Španov vrh
instance_of: Mountain
countries: Slovenia
coordinates: lat: 46.45965
lon: 14.069602777778
It is on the east side of Beaver Dam Road in the valley of Canoe Creek, a southward-flowing tributary of the Frankstown Branch of the Juniata River, part of the Susquehanna River watershed. Canoe Creek State Park is to the west, across Beaver Dam Road, and Canoe Mountain rises above the valley to the east. Moores Mill is north of U.S.

Geographic entities mentioned:
surface_form: Canoe Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.5417
lon: -78.2083
It is an intermediate stop on the standard gauge Vevey–Chexbres line of Swiss Federal Railways. It is adjacent to the valley station of the Vevey–Chardonne–Mont Pèlerin funicular railway to Mont Pèlerin. Rail services at this station ended with the December 2024 timetable change and replaced with a rush-hour bus service number 218 between Vevey and Chexbres.

Geographic entities mentioned:
surface_form: Mont Pèlerin
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.496877777778
lon: 6.8192472222222
It is the worst recorded flood in Murcia history. The flood. The rainfall that caused the flood was extremely heavy. It is estimated that at the head of the Guadalentín, 600 mm fell in just one hour. This river reached a flow in Lorca of 1450 m³/s, overflowing and causing great damage throughout its basin. The flow of Mundo, Alhárabe, Argos, Quípar and Mula rivers also increased rapidly.

Geographic entities mentioned:
surface_form: Guadalentín
instance_of: Watercourse
countries: Spain
coordinates: lat: 37.9916
lon: -1.0729
Inongo Airport. Inongo Airport is an airstrip serving Inongo, a city on the eastern shore of Lake Mai-Ndombe in Mai-Ndombe Province, Democratic Republic of Congo. The Inongo non-directional beacon (Ident: INO) is west-southwest of the airstrip.

Geographic entities mentioned:
surface_form: Lake Mai-Ndombe
instance_of: Lake
countries: Democratic Republic of the Congo
coordinates: lat: -2
lon: 18.33
Flagstaff is the principal city of the Flagstaff metropolitan area, which includes all of Coconino County, and has a population of 145,101. Flagstaff lies near the southwestern edge of the Colorado Plateau and within the San Francisco volcanic field, along the western side of the largest contiguous ponderosa pine forest in the continental United States.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
Flagstaff lies near the southwestern edge of the Colorado Plateau and within the San Francisco volcanic field, along the western side of the largest contiguous ponderosa pine forest in the continental United States. The city sits at around and is next to Mount Elden, just south of the San Francisco Peaks, the highest mountain range in the state of Arizona.

Geographic entities mentioned:
surface_form: Mount Elden
instance_of: Mountain
countries: United States
coordinates: lat: 35.241111111111
lon: -111.59666666667
The city sits at around and is next to Mount Elden, just south of the San Francisco Peaks, the highest mountain range in the state of Arizona. Humphreys Peak, the highest point in Arizona at, is about north of Flagstaff in Kachina Peaks Wilderness.

Geographic entities mentioned:
surface_form: Humphreys Peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.346341666667
lon: -111.67794722222
The city remains an important distribution hub for companies such as Nestlé Purina PetCare, and is home to the U.S. Naval Observatory Flagstaff Station, the U.S. Geological Survey, and Northern Arizona University. Flagstaff has a strong tourism sector, due to its proximity to Grand Canyon National Park, Oak Creek Canyon, the Arizona Snowbowl, Meteor Crater, and Historic Route 66. Etymology.

Geographic entities mentioned:
surface_form: Oak Creek Canyon
instance_of: Landform
countries: United States
coordinates: lat: 34.9125
lon: -111.727
The Northern Sinagua were living in the pine forests of northern Arizona before moving into the area that is now Flagstaff about 700 CE. The 1064 and 1066 eruptions of Sunset Crater covered the area in ash, which greatly enriched the soil for farming; this also caused a population growth in the area, with Ancestral Puebloans and Cohonina people also moving to the Wupatki site near the city.

Geographic entities mentioned:
surface_form: Sunset Crater
instance_of: Mountain
countries: United States
coordinates: lat: 35.365
lon: -111.5
The Yavapai land in the area saw overlap with the land of the Northern Tonto Apache that stretched across the San Francisco Peaks to the Little Colorado River. Of the Northern Tonto Apache, two tribes lived within the area of present-day Flagstaff: the Oak Creek band and the Mormon Lake band.

Geographic entities mentioned:
surface_form: Oak Creek
instance_of: Landform
countries: United States
coordinates: lat: 34.9125
lon: -111.727
surface_form: Mormon Lake
instance_of: Lake
countries: United States
coordinates: lat: 34.9475
lon: -111.455
Of the Northern Tonto Apache, two tribes lived within the area of present-day Flagstaff: the Oak Creek band and the Mormon Lake band. The Mormon Lake band were centered around Flagstaff and were exclusively hunter-gatherers, traveling around places like the foot of the San Francisco Peaks, at Mount Elden, Lake Mary, Stoneman Lake, and Padre Canyon. 19th century.

Geographic entities mentioned:
surface_form: Mount Elden
instance_of: Mountain
countries: United States
coordinates: lat: 35.241111111111
lon: -111.59666666667
Flagstaff saw its first tourism boom in the early years of the 1900s, becoming known as the City of Seven Wonders, as the &quot;Seven Wonders&quot; of the wider Flagstaff area – listed as the Coconino National Forest, Grand Canyon, Oak Creek Canyon, San Francisco Peaks, Sunset Crater, Walnut Canyon, and Wupatki National Monument – were more widely known. U.S. Route 66.

Geographic entities mentioned:
surface_form: Oak Creek Canyon
instance_of: Landform
countries: United States
coordinates: lat: 34.9125
lon: -111.727
surface_form: Sunset Crater
instance_of: Mountain
countries: United States
coordinates: lat: 35.365
lon: -111.5
It is in a mountainous area, and lies along the Rio de Flag watercourse. It is about north of the State capital, Phoenix. The geology of the area is in line with that of the Colorado Plateau on which it lies, with the Moenkopi red sandstone abundant in the city also used to build many of the distinctive buildings forming its cityscape.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
Flagstaff is one of the United States' sunniest and snowiest cities, with a variable &quot;semi-arid&quot; climate and a monsoon season in summer. The San Francisco Peaks are a main aspect of Flagstaff's local geography and can be seen from everywhere in the city. Humphreys Peak is the highest point in Arizona at. Several trails around the peaks provide views of the Grand Canyon.

Geographic entities mentioned:
surface_form: Humphreys Peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.346341666667
lon: -111.67794722222
Lake Armington. Lake Armington is a water body in the town of Piermont, in Grafton County, on the western edge of the White Mountains in New Hampshire, United States. Water from Lake Armington flows north for into Lake Tarleton, and then continues west via Eastman Brook to reach the Connecticut River. Camp Walt Whitman is located at the south end of the lake.

Geographic entities mentioned:
surface_form: Lake Tarleton
instance_of: Lake
countries: United States
coordinates: lat: 43.975555555556
lon: -71.963055555556
surface_form: lake armington
instance_of: Lake
countries: United States
coordinates: lat: 43.958333333333
lon: -71.968611111111
Lake Armington. Lake Armington is a water body in the town of Piermont, in Grafton County, on the western edge of the White Mountains in New Hampshire, United States. Water from Lake Armington flows north for into Lake Tarleton, and then continues west via Eastman Brook to reach the Connecticut River. Camp Walt Whitman is located at the south end of the lake.

Geographic entities mentioned:
surface_form: lake armington
instance_of: Lake
countries: United States
coordinates: lat: 43.958333333333
lon: -71.968611111111
Brooke Lifeboat Station. Brooke Lifeboat Station was located at Brook Chine, near the village of Brook, on the south west coast of the Isle of Wight. A lifeboat was first placed here in 1860 by the Royal National Lifeboat Institution (RNLI). After 77 years service, Brooke Lifeboat Station was closed in 1937. Appeal.

Geographic entities mentioned:
surface_form: Brook Chine
instance_of: Valley
countries: United Kingdom
Cameron Lake (Alberta). Cameron Lake is at the end of the Akamina Parkway, Waterton Lakes National Park, Alberta, Canada. It is named after Donald Roderick Cameron (1834–1921) a British Royal Artillery captain. The 49th parallel north runs through the southern end of the lake making part of it technically in Glacier County, Montana.

Geographic entities mentioned:
surface_form: cameron lake (alberta)
instance_of: Lake
countries: Canada
United States
coordinates: lat: 49.0094
lon: -114.051
Cameron Lake (Alberta). Cameron Lake is at the end of the Akamina Parkway, Waterton Lakes National Park, Alberta, Canada. It is named after Donald Roderick Cameron (1834–1921) a British Royal Artillery captain. The 49th parallel north runs through the southern end of the lake making part of it technically in Glacier County, Montana.

Geographic entities mentioned:
surface_form: cameron lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 49.0094
lon: -114.051
At the time, Gnaeus Petreius Atinas was only the sixth Roman officer whose actions qualified for such a distinction. The Cimbri now descended into the Po Valley spreading out over the area. Catulus and his staff decided that this fertile area would gain the Germanic tribes' attention for some time, long enough to give the Roman army time to regroup and link up with Marius' army.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
Karalad Lake. Karlad Lake is located in Thariode, Wayanad. It is the third largest fresh water lake in Kerala and second largest lake in Wayanad after Pookode Lake. The lake is 3 km away from Banasura Sagar Dam. Attractions. Wayanad Adventure Camp on the lake is administered by D.T.P.C (District Tourism Promotion Council) Wayanad.

Geographic entities mentioned:
surface_form: Pookode Lake
instance_of: Lake
countries: India
coordinates: lat: 11.542455555556
lon: 76.027222222222
Karalad Lake. Karlad Lake is located in Thariode, Wayanad. It is the third largest fresh water lake in Kerala and second largest lake in Wayanad after Pookode Lake. The lake is 3 km away from Banasura Sagar Dam. Attractions. Wayanad Adventure Camp on the lake is administered by D.T.P.C (District Tourism Promotion Council) Wayanad.

Geographic entities mentioned:
surface_form: karalad lake
instance_of: Lake
countries: India
coordinates: lat: 11.650555555555556
lon: 75.98166666666667
Trout Beck (Glenderamackin). Trout Beck is a long stream or beck in the English Lake District, Cumbria. It rises on the northwestern slopes of Great Dodd, with tributaries including Groove Beck and Thornsgill Beck, and flows east then north to the hamlet of Troutbeck.

Geographic entities mentioned:
surface_form: Great Dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
Kitsu Plateau. The Kitsu Plateau is a small intermontane plateau in Cassiar Land District of northwestern British Columbia, Canada. It lies on the Tahltan Highland and is surrounded by several valleys, including those of Mess Creek, Nagha Creek and Raspberry Creek.

Geographic entities mentioned:
surface_form: Mess Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
The Kitsu Plateau is volcanic in origin, consisting of lava flows that are interbedded with volcanic ejecta. These lava flows and the associated ejecta originated from several volcanoes of the Mount Edziza volcanic complex which has been the focus of volcanic activity over the last 7.5 million years.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
Location. The Kitsu Plateau is on the Tahltan Highland east of the Boundary Ranges of the Coast Mountains and west of the Skeena Mountains in Cassiar Land District. Between the Boundary Ranges and the Kitsu Plateau is Mess Creek valley, which extends more than to the north where it separates the Zagoddetchino massif from the Big Raven Plateau in the east.

Geographic entities mentioned:
surface_form: Mess Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: Big Raven Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
Between the Boundary Ranges and the Kitsu Plateau is Mess Creek valley, which extends more than to the north where it separates the Zagoddetchino massif from the Big Raven Plateau in the east. The northern end of the plateau is bounded by Raspberry Pass which contains the east-flowing Bourgeaux Creek in the east and the northwest-flowing Raspberry Creek in the west.

Geographic entities mentioned:
surface_form: Bourgeaux Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.49966
lon: -130.45397
Between the Kitsu Plateau and the Skeena Mountains is Artifact Ridge and the Little Iskut River, the latter of which flows north in a north–south trending valley and then flows southeast towards the Skeena Mountains into the Iskut River. In the southeast, the Kitsu Plateau is surrounded by the Spectrum Range whereas in the south the plateau is separated from Yagi Ridge by Nagha Creek valley.

Geographic entities mentioned:
surface_form: Little Iskut River
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.448889
lon: -130.268611
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
In the southeast, the Kitsu Plateau is surrounded by the Spectrum Range whereas in the south the plateau is separated from Yagi Ridge by Nagha Creek valley. Roughly long and wide, the plateau lies at the southern end of the Mount Edziza volcanic complex, which also includes the Big Raven Plateau to the north as well as the Spectrum Range and the Arctic Lake Plateau to the south.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: Arctic Lake Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.3
lon: -130.767
The volcanic complex consists of a group of overlapping shield volcanoes, stratovolcanoes, lava domes and cinder cones that have formed over the last 7.5 million years. It contains four central volcanoes along its north–south trending axis; from north to south they are Mount Edziza, Ice Peak, Armadillo Peak and the Spectrum Range. Drainage.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: Ice Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
surface_form: Armadillo Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5383
lon: -130.56
Drainage. As a part of the Mount Edziza volcanic complex, the Kitsu Plateau is drained entirely by streams within the Stikine River watershed. The only named stream on the plateau is Kitsu Creek, which originates on the northern flank of Kitsu Peak in the Spectrum Range and flows northwest then north into Mess Creek, a tributary of the Stikine River.

Geographic entities mentioned:
surface_form: Kitsu Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.51636
lon: -130.85398
surface_form: Kitsu Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.4246
lon: -130.6906
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Several small unnamed streams flow into Kitsu Creek and the neighbouring valleys of Mess Creek, Raspberry Creek and Nagha Creek; Raspberry Creek drains into Mess Creek whereas Nagha Creek drains into Kitsu Creek just northeast of Mess Lake. Structure.

Geographic entities mentioned:
surface_form: Mess Lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.4667
lon: -130.883
surface_form: kitsu creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.51636
lon: -130.85398
surface_form: kitsu creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.51636
lon: -130.85398
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Both cones are covered by tundra vegetation and have been slightly rounded by erosion, although their craters are still recognizable. The Ash Pit, sometimes referred to by the numeronym ML-3, is the youngest and southernmost eruptive centre of the Mess Lake Lava Field.

Geographic entities mentioned:
surface_form: The Ash Pit
instance_of: Mountain
countries: Canada
coordinates: lat: 57.45
lon: -130.78
Kitsu Plateau. The Kitsu Plateau is a small intermontane plateau in Cassiar Land District of northwestern British Columbia, Canada. It lies on the Tahltan Highland and is surrounded by several valleys, including those of Mess Creek, Nagha Creek and Raspberry Creek.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
Kitsu Plateau. The Kitsu Plateau is a small intermontane plateau in Cassiar Land District of northwestern British Columbia, Canada. It lies on the Tahltan Highland and is surrounded by several valleys, including those of Mess Creek, Nagha Creek and Raspberry Creek.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
The plateau is drained by many small streams that flow into these neighbouring valleys and, unlike the valleys, it is relatively barren of vegetation. Surrounding the Kitsu Plateau is Mount Edziza Provincial Park which is one of the largest provincial parks in British Columbia.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Surrounding the Kitsu Plateau is Mount Edziza Provincial Park which is one of the largest provincial parks in British Columbia. Access to this remote plateau is mainly by aircraft since motorized vehicles are prohibited from entering Mount Edziza Provincial Park. The Kitsu Plateau is volcanic in origin, consisting of lava flows that are interbedded with volcanic ejecta.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
Alkali basalt, hawaiite and trachyte are among some of the volcanic rocks comprising the Kitsu Plateau which is subdivided into five geological formations, each being the product of a distinct period of volcanic activity. Volcanism on the plateau continued into the current Holocene epoch and created the Mess Lake Lava Field which contains small volcanic cones. Location.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
Location. The Kitsu Plateau is on the Tahltan Highland east of the Boundary Ranges of the Coast Mountains and west of the Skeena Mountains in Cassiar Land District. Between the Boundary Ranges and the Kitsu Plateau is Mess Creek valley, which extends more than to the north where it separates the Zagoddetchino massif from the Big Raven Plateau in the east.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
Between the Kitsu Plateau and the Skeena Mountains is Artifact Ridge and the Little Iskut River, the latter of which flows north in a north–south trending valley and then flows southeast towards the Skeena Mountains into the Iskut River. In the southeast, the Kitsu Plateau is surrounded by the Spectrum Range whereas in the south the plateau is separated from Yagi Ridge by Nagha Creek valley.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
Drainage. As a part of the Mount Edziza volcanic complex, the Kitsu Plateau is drained entirely by streams within the Stikine River watershed. The only named stream on the plateau is Kitsu Creek, which originates on the northern flank of Kitsu Peak in the Spectrum Range and flows northwest then north into Mess Creek, a tributary of the Stikine River.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
Structure. The western, northern and southern edges of the Kitsu Plateau are marked by steep cliffs forming the Mess Creek Escarpment, the southern side of Raspberry Creek valley and the northern side of Nagha Creek valley, respectively.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
At the Mess Creek Escarpment, the Kitsu Plateau rises more than above Mess Lake in Mess Creek valley; Mess Lake has an elevation below whereas the Mess Creek Escarpment reaches an elevation of more than. The plateau surface is barren of vegetation, but at lower elevations the surrounding valleys contain white spruce, lodgepole pine and trembling aspen forests. Landforms.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Landforms. The Kitsu Plateau is dominated by the Mess Lake Lava Field, which extends from Raspberry Creek in the north to Nagha Creek in the south. It covers an area of around and contains three pyroclastic cones which were the sources of lava flows that travelled westward towards the Mess Creek Escarpment.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
The Ash Pit, sometimes referred to by the numeronym ML-3, is the youngest and southernmost eruptive centre of the Mess Lake Lava Field. It lies on the steep southern slope of the Kitsu Plateau inside Nagha Creek valley and has been described as a pyroclastic cone or a conical explosion crater. Stratigraphy.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
Stratigraphy. The Kitsu Plateau is subdivided into at least five geological formations, each being the product of a distinct period of volcanic activity. These periods of volcanic activity occurred during three magmatic cycles of the Mount Edziza volcanic complex; each cycle began with the effusion of alkali basalt and culminated with the eruption of lesser volumes of felsic magma.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
The two oldest geological formations comprising the Kitsu Plateau are the Raspberry and Armadillo formations, which were deposited by volcanic eruptions during the first magmatic cycle between 7.5 and 6 million years ago. Overlying these two geological formations are the Nido and Spectrum formations, which were deposited between 6 and 3 million years ago during the second magmatic cycle.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
Overlying these two geological formations are the Nido and Spectrum formations, which were deposited between 6 and 3 million years ago during the second magmatic cycle. The fifth oldest geological formation comprising the Kitsu Plateau is the Big Raven Formation, which was deposited during the fifth magmatic cycle in the last 20,000 years. Raspberry Formation.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
Raspberry Formation. The Raspberry Formation is exposed on the lower northern, western and southwestern sides of the Kitsu Plateau. It has an elevation of less than along the Mess Creek Escarpment and consists of flat-lying basaltic lava flows interbedded with scoria.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
The source of these flows was probably a cluster of vents further to the north called Sezill Volcano which may have been active prior to the onset of Armadillo volcanism. In contrast, the interbedded air-fall pumice and ash flows probably originated from the more than in diameter Armadillo Peak caldera northeast of the Kitsu Plateau. Nido Formation.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
surface_form: armadillo peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5383
lon: -130.56
In contrast, the interbedded air-fall pumice and ash flows probably originated from the more than in diameter Armadillo Peak caldera northeast of the Kitsu Plateau. Nido Formation. Overlying the Armadillo Formation is the Kounugu Member, which is the only stratigraphic unit of the Nido Formation comprising the Kitsu Plateau.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
At least some of the Kounugu lava flows comprising the Kitsu Plateau may have originated from Swarm Peak further to the east, which issued lava that travelled westward; remains of the Swarm Peak eruptive centre are in the form of north-trending fissure swarms.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
This geological formation largely consists of comendite, pantellerite and pantelleritic trachyte; all three volcanic rocks comprise lava domes, lava flows and minor breccia and ash flow deposits. Spectrum trachyte flows on the Kitsu Plateau are the most distal remnants of the main Spectrum Dome and are relatively thin compared to those forming the adjacent Spectrum Range.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
Spectrum trachyte flows on the Kitsu Plateau are the most distal remnants of the main Spectrum Dome and are relatively thin compared to those forming the adjacent Spectrum Range. These trachyte flows are overlain by alkali basalt of the Kitsu Member, which is mainly exposed at the southern end of the Kitsu Plateau and along the western edge of the plateau.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
This alkali basalt is in the form of lava flows and likely originated from vents of the Spectrum Dome which have since been destroyed by erosion. Big Raven Formation. The Big Raven Formation is the youngest and uppermost geological formation comprising the Kitsu Plateau, consisting of hawaiite and alkali basalt in the form of lava flows, lava bombs, agglutinate and air-fall tephra.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
The Ash Pit, which may be the youngest eruptive centre of the entire Mount Edziza volcanic complex, was the source of a long and wide hawaiitic air-fall tephra deposit that extends to the north-northeast on the Kitsu Plateau. It was also the source of a hawaiitic lava flow that travelled to the northwest through Nagha Creek valley towards Mess Lake.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
Basement. As a part of the Mount Edziza volcanic complex, the Kitsu Plateau is underlain by the Stikinia terrane. This is a Paleozoic and Mesozoic suite of volcanic, sedimentary and metamorphic rocks that accreted to the continental margin of North America during the Jurassic.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
Minor exposures of Cretaceous–Paleocene sedimentary rocks assigned to the Sustut Group are present in the mouth of Nagha Creek valley at the southwestern end of the Kitsu Plateau and are in the form of conglomerates, sandstones, arkoses, siltstones, shales or minor coal. Name and etymology.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75