Sarmila/GeoWiki-Features huggingface dataset:
Hayesbreen is a glacier in Sabine Land at Spitsbergen, Svalbard. It is named after American politician and Arctic explorer Isaac Israel Hayes. The glacier has a length of about eighteen kilometers, and debouches into the bay of Mohnbukta. Surrounding mountains are Aagaardfjellet to the north, Jebensfjellet to the south, and Panofskyfjellet where Hayesbreen joins the glacier of Königsbergbreen.

Geographic entities mentioned:
surface_form: Aagaardfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 78.411
lon: 18.554
surface_form: Jebensfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 78.3527
lon: 18.4695
Pwo Karens in Burma. In 1836, she was sent to Mawlamyine, Burma, as a missionary, arriving in December of that year. Soon after her arrival, she was appointed to labor among the Pwo Karens, a people whose language had not been acquired by any foreigner, though a beginning had been made at Tavoy, and in the region of the Zwaigaben hills, where no missionary labor had been performed.

Geographic entities mentioned:
surface_form: Zwaigaben hills
instance_of: Mountain
countries: Myanmar
coordinates: lat: 16.82426
lon: 97.66841
Modestinus, Florentinus and Flavianus. Saints Modestinus, Florentinus and Flavianus are three Christian martyrs of Campania, Italy, martyred in 311. Their relics were re-discovered in 1167 by Gugliemo, bishop of Avellino. Like others, they had taken refuge on Monte Vergine. Holweck considers the &quot;acts of Modestinus&quot; as &quot;untrustworthy&quot;.

Geographic entities mentioned:
surface_form: Monte Vergine
instance_of: Mountain
countries: Italy
coordinates: lat: 40.9393747
lon: 14.7244325
According to oral history, the construction of the St. Francis of Assisi Parish was initiated by a priest in 1875. He oversaw the parish until 1909. On March 17, 1957, the Douglas C-47 which carried then-president Ramon Magsaysay crashed in Mount Manunggal. A monument was erected at the site which is now considered historical site ever since.

Geographic entities mentioned:
surface_form: Mount Manunggal
instance_of: Mountain
countries: Philippines
coordinates: lat: 10.453055555555556
lon: 123.815
Returning to the mainland, wanting to help Zero and instill trust in him for the civilian populace, Euphemia announces on live television her intent to form the Special Administrative Zone of Japan in the region under Mount Fuji, giving the Japanese people their name and country back, and govern it alongside Zero.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
In 2023, Uzbek officials held talks with the Taliban on the matter, though no official agreements were reached. Environmental concerns. Environmental experts have raised concern that the Qosh Tepa Canal will make the Aral Sea situation worse by diverting even more water from Amu River.

Geographic entities mentioned:
surface_form: Aral Sea
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
Madero. The Treaty of Guadalupe Hidalgo, which ended the Mexican–American War of 1846–1848, was signed in Gustavo A. Madero. Points of interest. The area houses the Basílica de Guadalupe, the shrine of Our Lady of Guadalupe at the foot of Tepeyac Hill, where Roman Catholics believe the Virgin Mary appeared to the indigenous Mexican Juan Diego Cuauhtlatoatzin in 1531.

Geographic entities mentioned:
surface_form: Tepeyac Hill
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.4868321
lon: -99.1157824
In his mid-forties he relocated to Cuckoo Hill, near Fordingbridge in Hampshire, England, and spent the rest of his life investigating and recording the archaeology, geology and folklore of the New Forest and Cranborne Chase regions. Personal life and family.

Geographic entities mentioned:
surface_form: Cranborne Chase
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 50.961419444444
lon: -2.0440888888889
The BPW also owns shares in Consumers Energy's JH Campbell Unit 3 and Detroit Edison's Belle River Power Plant; power generated at these two plants is used to supplement power produced at the BPW's own facilities. Water filtration. Water from Lake Michigan is filtered at a facility in Park Township on the city's northside. The plant has a capacity of 38.5 million gallons per day.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Expansion has been considered by building a new plant south of the city near Saugatuck Dunes State Park. Wastewater treatment. Wastewater is treated at a facility on Lake Macatawa near the BPW's James DeYoung power plant. The plant spans both sides of River Avenue. Over of pipe and 36 lift stations are used on pipes up to in diameter.

Geographic entities mentioned:
surface_form: Lake Macatawa
instance_of: Lake
countries: United States
coordinates: lat: 42.778955555555555
lon: -86.16151388888889
Pitt Meadows, in the Fraser Valley east of Vancouver, subbed for the Indonesian landscape the crew needed for the sequence of Whitney Fordman's ultimate demise during battle &quot;Visage&quot;.

Geographic entities mentioned:
surface_form: Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
Akullikassaq. Akullikassaq is a mountain of Greenland. It is located in the Upernavik Archipelago.

Geographic entities mentioned:
surface_form: akullikassaq
instance_of: Mountain
countries: Greenland
Carr Hollow. Carr Hollow is a valley in Shannon County in the U.S. state of Missouri. The southeast flowing intermittent stream in the valley is a tributary to McHenry Hollow. The stream source is at and the confluence with McHenry Hollow is at at an elevation of 853 feet. Carr Hollow has the name of the local Carr family.

Geographic entities mentioned:
surface_form: McHenry Hollow
instance_of: Valley
countries: United States
coordinates: lat: 37.256991
lon: -91.462917
Carr Hollow. Carr Hollow is a valley in Shannon County in the U.S. state of Missouri. The southeast flowing intermittent stream in the valley is a tributary to McHenry Hollow. The stream source is at and the confluence with McHenry Hollow is at at an elevation of 853 feet. Carr Hollow has the name of the local Carr family.

Geographic entities mentioned:
surface_form: carr hollow
instance_of: Valley
countries: United States
coordinates: lat: 37.2689351
lon: -91.4818064
But we rather incline to the belief that the remains found at Fall River belonged to the crew of a Phoenician vessel. The spot where they were found is on the sea-coast, and in the immediate neighborhood of Dighton Rock, famed for its hieroglyphic inscriptions, of which no sufficient explanation has yet been given, alla near which rock brazen vessels have been found.

Geographic entities mentioned:
surface_form: Dighton Rock
instance_of: Landform
countries: United States
Portuguese Empire
coordinates: lat: 41.812756
lon: -71.110556
Distribution and habitat. This species has a restricted distribution in Victoria growing in heathland in the Natimuk district, but unknown in the area since 1962, and found near Lake Hindmarsh in 2014. In South Australia it is found in the southern Eyre Peninsula district.

Geographic entities mentioned:
surface_form: Lake Hindmarsh
instance_of: Lake
countries: Australia
coordinates: lat: -36.0667
lon: 141.917
Genesis 49:4) to kill all other Gideon's sons, a total 70 of them. Gideon's youngest son of the seventy, Jotham, survived the slaughter and went to the top of Mount Gerizim to deliver a &quot;mashal&quot; (&quot;parable&quot;) to the people about useful trees, which decline rulership as beneath them, allow the useless and prickly bramble to reign over them with disastrous ending.

Geographic entities mentioned:
surface_form: Mount Gerizim
instance_of: Mountain
countries: State of Palestine
coordinates: lat: 32.199444444444
lon: 35.272777777778
However, there soon emerged rumors – believed by prominent foreigners Jean Laborde and William Ellis – that Radama lived and was making plans to reclaim the throne. A strong case has since been made on the basis of significant evidence that Radama may indeed have revived after the strangling and lived to old age in anonymity near Lake Kinkony in the northwestern part of the island.

Geographic entities mentioned:
surface_form: Lake Kinkony
instance_of: Lake
countries: Madagascar
coordinates: lat: -16.15
lon: 45.833333333333
Stissing Mountain. Stissing Mountain, with an elevation of 1,403 feet (428 meters), lies in northern Dutchess County, New York, where it rises about 1,000 feet (305 meters) above its local footings. The mountain is steepest on its eastern slopes, which average 40 percent (or 21.8 degrees). This eastern escarpment is about 3 miles (4.8 km) long.

Geographic entities mentioned:
surface_form: stissing mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.956388888889
lon: -73.6925
Tenchen Creek. Tenchen Creek is a tributary of Kakiddi Creek, which in turn is a tributary of the Klastline River, part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. It flows generally flows northeast for about to join Kakiddi Creek about south of Kakiddi Creek's confluence with the Klastline River.

Geographic entities mentioned:
surface_form: Kakiddi Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: tenchen creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.76636
lon: -130.43724
Tenchen Creek is in Mount Edziza Provincial Park which lies within the traditional territory of the Tahltan people. Geography. Tenchen Creek originates with several small streams converging at the head of Tenchen Glacier on the east side of Mount Edziza. From its source, Tenchen Creek flows about east-northeast through conifer forest into the broad hummocky lowland of Kakiddi Valley.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: tenchen creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.76636
lon: -130.43724
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
It consists of thin, slaggy flows of basalt that ponded against stagnant ice of a valley glacier. The basalt is part of the Big Raven Formation, the youngest geological formation of the Mount Edziza volcanic complex. Tenchen Creek is the namesake of the Tenchen Member, the northern geological member of the Nido Formation.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Tenchen Creek's watershed covers and its mean annual discharge is estimated at. The mouth of Tenchen Creek is located about southeast of Telegraph Creek, about west-southwest of Iskut and about south-southwest of Dease Lake. Elwyn Creek's watershed's land cover is classified as 32.5% barren, 28.4% conifer forest, 27% snow/glacier, 8% shrubland, 3.3% herbaceous, and small amounts of other cover.

Geographic entities mentioned:
surface_form: dease lake
instance_of: Lake
countries: Canada
coordinates: lat: 58.63502
lon: -130.03761
Tenchen Creek. Tenchen Creek is a tributary of Kakiddi Creek, which in turn is a tributary of the Klastline River, part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. It flows generally flows northeast for about to join Kakiddi Creek about south of Kakiddi Creek's confluence with the Klastline River.

Geographic entities mentioned:
surface_form: tenchen creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.76636
lon: -130.43724
Tenchen is a combination of the Tahltan words &quot;ten&quot; and &quot;chen&quot;, which mean &quot;ice&quot; and &quot;dirty&quot; respectively. Tenchen Creek's watershed covers and its mean annual discharge is estimated at. The mouth of Tenchen Creek is located about southeast of Telegraph Creek, about west-southwest of Iskut and about south-southwest of Dease Lake.

Geographic entities mentioned:
surface_form: tenchen creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.76636
lon: -130.43724
Elwyn Creek's watershed's land cover is classified as 32.5% barren, 28.4% conifer forest, 27% snow/glacier, 8% shrubland, 3.3% herbaceous, and small amounts of other cover. Tenchen Creek is in Mount Edziza Provincial Park which lies within the traditional territory of the Tahltan people. Geography.

Geographic entities mentioned:
surface_form: tenchen creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.76636
lon: -130.43724
Geography. Tenchen Creek originates with several small streams converging at the head of Tenchen Glacier on the east side of Mount Edziza. From its source, Tenchen Creek flows about east-northeast through conifer forest into the broad hummocky lowland of Kakiddi Valley. Tenchen Creek then flows about southeast before flowing an additional northwest where it drains into Kakiddi Creek. Geology.

Geographic entities mentioned:
surface_form: tenchen creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.76636
lon: -130.43724
Geography. Tenchen Creek originates with several small streams converging at the head of Tenchen Glacier on the east side of Mount Edziza. From its source, Tenchen Creek flows about east-northeast through conifer forest into the broad hummocky lowland of Kakiddi Valley. Tenchen Creek then flows about southeast before flowing an additional northwest where it drains into Kakiddi Creek. Geology.

Geographic entities mentioned:
surface_form: tenchen creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.76636
lon: -130.43724
surface_form: kakiddi creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
Exposed in the cirque headwall are hydrothermally altered rocks of the central volcanic conduit, as well as lava lakes that once filled the crater. These rocks are part of the Edziza Formation which comprises the nearly symmetrical trachyte stratovolcano of Mount Edziza. In the north fork of Tenchen Creek valley is a barrier of volcanic rocks called Cinder Cliff.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
The basalt is part of the Big Raven Formation, the youngest geological formation of the Mount Edziza volcanic complex. Tenchen Creek is the namesake of the Tenchen Member, the northern geological member of the Nido Formation. Sideromelane tuff breccia of the Tenchen Member is exposed in cliffs on the northern side of Tenchen Creek.

Geographic entities mentioned:
surface_form: tenchen creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.76636
lon: -130.43724
Tenchen Creek then flows about southeast before flowing an additional northwest where it drains into Kakiddi Creek. Geology. At the head of Tenchen Creek is an active cirque that has breached the eastern side of Mount Edziza's ice-filled summit crater. Exposed in the cirque headwall are hydrothermally altered rocks of the central volcanic conduit, as well as lava lakes that once filled the crater.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
At the head of Tenchen Creek is an active cirque that has breached the eastern side of Mount Edziza's ice-filled summit crater. Exposed in the cirque headwall are hydrothermally altered rocks of the central volcanic conduit, as well as lava lakes that once filled the crater. These rocks are part of the Edziza Formation which comprises the nearly symmetrical trachyte stratovolcano of Mount Edziza.

Geographic entities mentioned:
surface_form: lava lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 56.4333
lon: -130.9
Tenchen Creek. Tenchen Creek is a tributary of Kakiddi Creek, which in turn is a tributary of the Klastline River, part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. It flows generally flows northeast for about to join Kakiddi Creek about south of Kakiddi Creek's confluence with the Klastline River.

Geographic entities mentioned:
surface_form: kakiddi creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
surface_form: kakiddi creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
Schiedea attenuata. &quot;Schiedea attenuata&quot; is a rare species of flowering plant in the family Caryophyllaceae known by the common name Kalalau schiedea. It is endemic to Hawaii, where it is known only from the Kalalau Valley on the island of Kauai. It is threatened by the degradation of its habitat. It was federally listed as an endangered species of the United States in 2010.

Geographic entities mentioned:
surface_form: Kalalau Valley
instance_of: Valley
countries: United States
coordinates: lat: 22.18
lon: -159.65361111
During the Viking Age, of the areas around Finland, Denmark, Norway and Sweden (particularly the Mälaren area) started to form into monarchies, where power was consolidated into the hands of one nobleman.

Geographic entities mentioned:
surface_form: Mälaren
instance_of: Lake
countries: Sweden
coordinates: lat: 59.5
lon: 17.2
The investigation attributed the crash to pilot error. On 26 March 2001, two F-15Cs from the 493rd FS (&quot;86-0169&quot; and &quot;86-0180&quot;) crashed into Ben Macdui in the Cairngorms mountain range, both pilots died in the crash. Between 23 March and 10 April 2008, the 493rd participated in the Romanian-led Operation Noble Endeavor.

Geographic entities mentioned:
surface_form: Ben Macdui
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.070368
lon: -3.669099
It is also comparable to hydraulic engineering works designed and built by the Etruscans and Romans and used throughout the Mediterranean basin during antiquity, including at Albano and Fucino in Italy, at Faiyum in Egypt, and at Copais and Trichonida in Greece.

Geographic entities mentioned:
surface_form: Copais
instance_of: Lake
countries: Greece
coordinates: lat: 38.45
lon: 23.05
surface_form: Trichonida
instance_of: Lake
countries: Greece
coordinates: lat: 38.5725
lon: 21.5525
Taşeli. Taşeli (Turkish for 'stone land') is a karst plateau in southern Turkey, in the ancient Cilicia Trachea. Taşeli plateau roughly covers the districts of Ermenek, Başyayla, Sarıveliler (Karaman Province), Mut, Gülnar (Mersin Province), and Taşkent (Konya Province) as well as interior uplands of the coastal Anamur and Bozyazı districts in Mersin Province and Gazipaşa in Antalya Province.

Geographic entities mentioned:
surface_form: taşeli
instance_of: Plateau
countries: Turkey
coordinates: lat: 36.49607
lon: 32.62693
The river Göksu and its main tributary Ermenek Çayı flow on the plateau. The Taşeli Peninsula () on the Mediterranean Sea, bordering Silifke to the east and Alanya to the west, takes its name from the plateau.

Geographic entities mentioned:
surface_form: taşeli
instance_of: Plateau
countries: Turkey
coordinates: lat: 36.49607
lon: 32.62693
Royal Lochnagar distillery. Royal Lochnagar distillery is a single malt Scotch whisky distillery based on the Abergeldie Estate, near Balmoral Castle in Royal Deeside. It is close to the mountain Lochnagar. The distillery is in the Highland whisky-producing area of Scotland. The distillery holds a Royal Warrant. History.

Geographic entities mentioned:
surface_form: Royal Deeside
instance_of: Valley
countries: United Kingdom
Royal Lochnagar distillery. Royal Lochnagar distillery is a single malt Scotch whisky distillery based on the Abergeldie Estate, near Balmoral Castle in Royal Deeside. It is close to the mountain Lochnagar. The distillery is in the Highland whisky-producing area of Scotland. The distillery holds a Royal Warrant. History.

Geographic entities mentioned:
surface_form: Lochnagar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.959930555556
lon: -3.2447805555556
It was played from 2004 to 2008 and then restarted in 2016. The tournament was originally played at GC Venezia, near Venice, but has since been played at GC Arzaga on Lake Garda and GC Udine, Fagagna. Italy's most successful 20th century male golfer, Costantino Rocca, made his senior debut at the 2007 edition of his home senior open.

Geographic entities mentioned:
surface_form: Lake Garda
instance_of: Lake
countries: Italy
coordinates: lat: 45.633333333333
lon: 10.666666666667
He was the father of the poet Tom MacInnes. Life. McInnes was born in Lake Ainslie, Nova Scotia, to Scottish immigrant parents. He studied in the US, at Harvard University and elsewhere, earning a medical degree from Rush Medical College. McInnes served in the Union Army during the American Civil War before returning to Canada.

Geographic entities mentioned:
surface_form: Lake Ainslie
instance_of: Lake
countries: Canada
coordinates: lat: 46.126666666667
lon: -61.176111111111
The cordillera is paralleled on the east by the Cauca river. From this massif the range divides further to form the Serranías de Ayapel, San Jerónimo and Abibe. Only to recede into the Caribbean plain and the Sinú River valley. It is a direct continuation of Cordillera Occidental of Ecuador. Geography.

Geographic entities mentioned:
surface_form: Sinú River
instance_of: Watercourse
countries: Colombia
coordinates: lat: 8.75825
lon: -75.88811111111112
It is a direct continuation of Cordillera Occidental of Ecuador. Geography. The western part of the mountain range belongs to the Pacific region of Colombia, with the San Juan River being the main watershed, while the eastern part belongs to the Cauca River basin. The northern and northwestern parts belong to the Atlantic Slope, with the Atrato and Sinú Rivers being the main watersheds.

Geographic entities mentioned:
surface_form: Sinú
instance_of: Watercourse
countries: Colombia
coordinates: lat: 8.75825
lon: -75.88811111111112
The state park encompasses more than 1200 heavily wooded acres that include six lakes and ponds (Lake Rico, Furnace Pond, King's Pond, Middle Pond, Little Bearhole Pond, and Big Bearhole Pond) and numerous cranberry bogs. Features. The park has an extensive trail system for walking, hiking, biking, cross-country skiing, and equestrian use.

Geographic entities mentioned:
surface_form: Lake Rico
instance_of: Lake
countries: United States
coordinates: lat: 41.8748487
lon: -70.997468
His elder brother Thomas Stone signed the Declaration of Independence, and his younger brother John Hoskins Stone was the ninth governor of Maryland. Career. As an adult, Michael lived at Haberdeventure, which was the plantation of his brother Thomas near Port Tobacco. Michael married Mary Briscoe and they had five children. Their grandson, Frederick Stone, represented Maryland in the U.S.

Geographic entities mentioned:
surface_form: Port Tobacco
instance_of: Landform
countries: United States
coordinates: lat: 38.457777777778
lon: -77.035
He was back in Beijing by the end of January 1224. From the narrative of his expedition, &quot;Travels to the West of Qiu Chang Chun&quot; written by his pupil Li Zhichang, we derive some of the most vivid pictures ever drawn of nature and man between the Great Wall of China and Kabul, between the Aral and Yellow Seas, peppered by poetic expressions.

Geographic entities mentioned:
surface_form: Aral
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
He began modeling at the age of five, and as a child, he also appeared in commercials for Cookie Crisp cereal and Smurf merchandise, later winning guest spots on television series. He spent his teenage years in the Santa Clarita Valley in Southern California, where he attended Hart High School. Gosselaar has said that his natural hair color is brown, but he was &quot;blondish&quot; as a kid.

Geographic entities mentioned:
surface_form: Santa Clarita Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.398
lon: -118.522
The South Leinster Way, a long-distance trail, meandering through the Barrow Valley and traverses Brandon Hill. The village of Graiguenamanagh and River Barrow are at the base of the hill. It is classified as a county high point, an Arderin, a Myrddyn Dewey, and a Marilyn. Classification. Brandon Hill has various classifications (). Brandon Hill (Gribbon No.

Geographic entities mentioned:
surface_form: arderin
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.03805556
lon: -7.65388889
Brandon Hill. Brandon Hill () is the highest mountain in County Kilkenny, Ireland, with an elevation of and prominence at. The South Leinster Way, a long-distance trail, meandering through the Barrow Valley and traverses Brandon Hill. The village of Graiguenamanagh and River Barrow are at the base of the hill. It is classified as a county high point, an Arderin, a Myrddyn Dewey, and a Marilyn.

Geographic entities mentioned:
surface_form: brandon
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.234
lon: -10.254
surface_form: brandon hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.509702777778
lon: -6.9742527777778
The village of Graiguenamanagh and River Barrow are at the base of the hill. It is classified as a county high point, an Arderin, a Myrddyn Dewey, and a Marilyn. Classification. Brandon Hill has various classifications (). Brandon Hill (Gribbon No. 071) is known as the county high point but are also sometimes referred to as county top and county peak.

Geographic entities mentioned:
surface_form: brandon
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.234
lon: -10.254
surface_form: brandon hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.509702777778
lon: -6.9742527777778
It is classified as a county high point, an Arderin, a Myrddyn Dewey, and a Marilyn. Classification. Brandon Hill has various classifications (). Brandon Hill (Gribbon No. 071) is known as the county high point but are also sometimes referred to as county top and county peak. It is listed as one of the 200 Myrddyn Deweys, which are the Irish equivalent of Deweys.

Geographic entities mentioned:
surface_form: brandon
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.234
lon: -10.254
surface_form: brandon hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.509702777778
lon: -6.9742527777778
It is listed as one of the 407 Arderins, which are the Irish equivalent of the Hewitt. Brandon Hill has a regional height rank of 151 of 454 Marilyns in Ireland (389 in the Republic of Ireland and 66 in Northern Ireland), and a regional prominence of 53. With a height rank of 1098 and prominence rank of 269 of the total for the British Isles of 2,011. Geography.

Geographic entities mentioned:
surface_form: brandon
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.234
lon: -10.254
surface_form: brandon hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.509702777778
lon: -6.9742527777778
With a height rank of 1098 and prominence rank of 269 of the total for the British Isles of 2,011. Geography. Brandon is 4-kilometres South-South West of Graiguenamanagh, 7-kilometres east of Inistioge and 11-kilometres east of Thomastown, in the south of County Kilkenny. Brandon Hill is in the barony of Gowran and in the province of Leinster.

Geographic entities mentioned:
surface_form: brandon
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.234
lon: -10.254
Geography. Brandon is 4-kilometres South-South West of Graiguenamanagh, 7-kilometres east of Inistioge and 11-kilometres east of Thomastown, in the south of County Kilkenny. Brandon Hill is in the barony of Gowran and in the province of Leinster. The village of Graiguenamanagh is at the base of the hill. Geology.

Geographic entities mentioned:
surface_form: brandon
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.234
lon: -10.254
surface_form: brandon hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.509702777778
lon: -6.9742527777778
Geology. It is the termination of the chain of granitic mountains that raise from the shores of Dublin bay. The base of Brandon Hill on the side of the River Barrow and the hill running to Graigue is composed of schist rock. This blackish siliceous schistus, sometimes containing grains of quartz and when it is broken it has a shivery texture and is hard enough to scratch glass.

Geographic entities mentioned:
surface_form: brandon
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.234
lon: -10.254
surface_form: brandon hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.509702777778
lon: -6.9742527777778
There are a few beds of marble and limestone gravel near the foot of the mountain. Archaeology. Evidence regarding the early settlement of the Brandon Hill uplands came to light as a result of ground and aerial surveys directed by Michael Gibbons, an archaeologist with the Board of Works, in 1989.

Geographic entities mentioned:
surface_form: brandon
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.234
lon: -10.254
surface_form: brandon hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.509702777778
lon: -6.9742527777778
The survey indicated that the slopes of Brandon were settled in excess of four thousand years ago and that the cairns, house sites, field systems and a large ritual enclosure identified on its slopes are part of the prehistoric remains there.

Geographic entities mentioned:
surface_form: brandon
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.234
lon: -10.254
View Lake (Vancouver Island). View Lake is a lake located on Vancouver Island east of the west end of Great Central Lake.

Geographic entities mentioned:
surface_form: Great Central Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.366666666667
lon: -125.16666666667
surface_form: view lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.38361
lon: -125.35778
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
View Lake (Vancouver Island). View Lake is a lake located on Vancouver Island east of the west end of Great Central Lake.

Geographic entities mentioned:
surface_form: view lake (vancouver island)
instance_of: Lake
countries: Canada
coordinates: lat: 49.38361
lon: -125.35778
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
Glyn commanded the troops in the opening action of the war, at Sihayo's Kraal on 12 January 1879. On their way to the Zulu capital of Ulundi, No. 3 Column made camp at Isandlwana. On the morning of 22 January Glyn accompanied Chelmsford on a reconnaissance in force to Mangeni, leaving Lieutenant-Colonel Henry Pulleine of the 1st Battalion of the 24th Regiment, in command of the camp.

Geographic entities mentioned:
surface_form: Isandlwana
instance_of: Mountain
countries: South Africa
coordinates: lat: -28.3589
lon: 30.6528
The specific epithet &quot;megalosperma&quot; is derived from the Greek &quot;referring to the large seeds&quot;. Distribution and habitat. Lesueur hakea is a rare and endangered species growing on lateritic sand plains in low heathland from Jurien Bay to Mount Lesueur Western Australia.

Geographic entities mentioned:
surface_form: Mount Lesueur
instance_of: Mountain
countries: Australia
coordinates: lat: -30.1755
lon: 115.19908333333
Bays may also be nested within each other; for example, James Bay is an arm of Hudson Bay in northeastern Canada. Some bays are large enough to have varied marine geology, such as the Bay of Bengal () and Hudson Bay (). The land surrounding a bay often reduces the strength of winds and blocks waves. Bays may have as wide a variety of shoreline characteristics as other shorelines.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
The largest bays have developed through plate tectonics. As the Paleozoic/early Mesozoic era super-continent Pangaea broke up along curved and indented fault lines, the continents moved apart and left large bays; these include the Gulf of Guinea, the Gulf of Mexico, and the Bay of Bengal, which is the world's largest bay. Bays also form through coastal erosion by rivers and glaciers.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
By the 12th century a sept of the Ua Braoin (Breens) were in Lune, as well as Ó Cearnacháin (Kernaghans). After the Norman conquest of Ireland, it was granted by Hugh de Lacy to Robert Misset as an Irish feudal barony in 1172. Geography. Lune is in the west of the county, on the border with County Westmeath. The Stonyford River flows through it and it contains the Hill of Ward.

Geographic entities mentioned:
surface_form: Hill of Ward
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.624
lon: -6.886
It is bounded on the west by the Confusion Range, on the east by the House Range, to the north by the Middle Range and the Great Salt Lake Desert, and the south by Wah Wah Valley and the Wah Wah Mountains. The central part of the valley has several knolls, the largest of which is Coyote Knolls. The White Valley name comes from the abundance of white rocks noted by James H. Simpson in 1859.

Geographic entities mentioned:
surface_form: Wah Wah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.7222
lon: -113.26
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2767785
lon: -98.6946248
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 44.965
lon: -96.443611111111
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.635555555556
lon: -99.9175
Geographic features. Tule Valley's most prominent feature may be Coyote Springs, an important spring system for local wildlife and feral horses, which populate the valley. It is also used as a gateway to viewing and traveling toward the base of Notch Peak, a carbonate rock cliff (of which is pure vertical drop), the tallest carbonate cliff in North America.

Geographic entities mentioned:
surface_form: Notch Peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.143055555556
lon: -113.40972222222
Tule Valley. Tule Valley (also known as White Valley) is a valley in Millard County, Utah, United States. Description. The valley is a north-south trending endorheic valley within the Great Basin (geographically), Great Basin Desert (ecologically), and Basin and Range Province (tectonically) of west-central Utah.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
It is bounded on the west by the Confusion Range, on the east by the House Range, to the north by the Middle Range and the Great Salt Lake Desert, and the south by Wah Wah Valley and the Wah Wah Mountains. The central part of the valley has several knolls, the largest of which is Coyote Knolls. The White Valley name comes from the abundance of white rocks noted by James H. Simpson in 1859.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The White Valley name comes from the abundance of white rocks noted by James H. Simpson in 1859. These rocks are mostly Lake Bonneville marls in the valley floor. Geographic features. Tule Valley's most prominent feature may be Coyote Springs, an important spring system for local wildlife and feral horses, which populate the valley.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Geographic features. Tule Valley's most prominent feature may be Coyote Springs, an important spring system for local wildlife and feral horses, which populate the valley. It is also used as a gateway to viewing and traveling toward the base of Notch Peak, a carbonate rock cliff (of which is pure vertical drop), the tallest carbonate cliff in North America.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: tule valley
instance_of: Valley
countries: United States
coordinates: lat: 38.9569
lon: -113.376
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
It is also used as a gateway to viewing and traveling toward the base of Notch Peak, a carbonate rock cliff (of which is pure vertical drop), the tallest carbonate cliff in North America. The name &quot;Tule&quot; is a reference to a swamp plant that probably was found at Coyote Springs during the early exploration of the valley.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Route 6/U.S. Route 50. There are no permanent human residents of the valley, though shepherds are known to populate it in the spring. The center of the valley is a large playa, the place where all precipitation from the drainage basin collects, since it is an isolated basin and watershed. This is the location of the lowest point in Millard County, Utah.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
They are located on the eastern edge of the Great Basin. Geology. The geology of Tule Valley consists of Quaternary alluvial sediments punctuated by chalky white Pleistocene marls. The valley is a true graben in the sense that it is down-faulted by normal faults on both sides of the valley. The knolls in the valley are horsts of Silurian to Devonian carbonates. Tule Valley watershed.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Tule Valley. Tule Valley (also known as White Valley) is a valley in Millard County, Utah, United States. Description. The valley is a north-south trending endorheic valley within the Great Basin (geographically), Great Basin Desert (ecologically), and Basin and Range Province (tectonically) of west-central Utah.

Geographic entities mentioned:
surface_form: white valley
instance_of: Valley
countries: United States
coordinates: lat: 38.9569
lon: -113.376
surface_form: tule valley
instance_of: Valley
countries: United States
coordinates: lat: 38.9569
lon: -113.376
It is bounded on the west by the Confusion Range, on the east by the House Range, to the north by the Middle Range and the Great Salt Lake Desert, and the south by Wah Wah Valley and the Wah Wah Mountains. The central part of the valley has several knolls, the largest of which is Coyote Knolls. The White Valley name comes from the abundance of white rocks noted by James H. Simpson in 1859.

Geographic entities mentioned:
surface_form: white valley
instance_of: Valley
countries: United States
coordinates: lat: 38.9569
lon: -113.376
Tule Valley. Tule Valley (also known as White Valley) is a valley in Millard County, Utah, United States. Description. The valley is a north-south trending endorheic valley within the Great Basin (geographically), Great Basin Desert (ecologically), and Basin and Range Province (tectonically) of west-central Utah.

Geographic entities mentioned:
surface_form: tule valley
instance_of: Valley
countries: United States
coordinates: lat: 38.9569
lon: -113.376
The valley is a true graben in the sense that it is down-faulted by normal faults on both sides of the valley. The knolls in the valley are horsts of Silurian to Devonian carbonates. Tule Valley watershed. The Tule Valley hydrologic unit is an area of several Utah valleys and ridgelines of the Basin and Range Province. The endorheic watershed's volume of surface water averages.

Geographic entities mentioned:
surface_form: tule valley
instance_of: Valley
countries: United States
coordinates: lat: 38.9569
lon: -113.376
Sheryl McFarlane. Sheryl McFarlane is a Canadian author of books for children and young adults. Career. McFarlane was born in the Ottawa Valley, grew up in Arizona and has lived on the West Coast of Canada since 1974. A former teacher, McFarlane often visits schools and speaks at seminars across Canada on topics related to children's literature.

Geographic entities mentioned:
surface_form: Ottawa Valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
Until the middle of the twentieth century, the Buša was the dominant cattle breed of the inhabitants of the wider area of the Balkans, and spread south of the Sava and Danube rivers, from Avala to Olympus and from the Rhodope to the Velebit. Buša cattle were raised together with sheep and goats in the mountainous regions in an extensive (primitive) way.

Geographic entities mentioned:
surface_form: Avala
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.690555555556
lon: 20.514166666667
surface_form: Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
Eimhjellen. Eimhjellen is a village in Gloppen Municipality in Vestland county, Norway. It is located in the Hyen area about south of Straume. The village lies on the eastern shore of the large lake Eimhjellevatnet. The villages of Hjorteset and Solheim lie about to the west (across the lake). Eimhjellen has a population of around 40 people living on 12 farms.

Geographic entities mentioned:
surface_form: Eimhjellevatnet
instance_of: Lake
countries: Norway
coordinates: lat: 61.6384
lon: 5.75
The confluence of the Bill Williams River with the Colorado is north of Parker, and south of Lake Havasu City. To the north of the river are the Artillery Mountains, the Rawhide Mountains and Bill Williams Mountain. To the south lie the Buckskin Mountains. The old mining camp of Swansea (now a ghost town) lies in the Buckskin Mountains about south of the river.

Geographic entities mentioned:
surface_form: Bill Williams Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.20013256
lon: -112.20521298
Bolmen Water Tunnel. The Bolmen Water Tunnel () is a water supply tunnel, long. It goes from the lake Bolmen in Kronoberg County to the province of Skåne, all in Sweden, and it serves around 700,000 people with drinking water. It has a cross section area of 9 m2, a diameter of more than 3 m. About 2 m³/s is transported through the tunnel, although the capacity is 6 m³/s.

Geographic entities mentioned:
surface_form: Bolmen
instance_of: Lake
countries: Sweden
coordinates: lat: 56.916666666667
lon: 13.666666666667
Background. The tunnel was built because of the foreseen lack of tap water because of the growth of the population in the province of Scania in the 1960s and the high calcium level of the local water. That water was groundwater or came from the lakes of Ringsjön and Vombsjön. The construction took more time and money than planned, partly because of unexpectedly bad rock quality.

Geographic entities mentioned:
surface_form: Ringsjön
instance_of: Group of lakes
countries: Sweden
coordinates: lat: 55.872222222222
lon: 13.518611111111
surface_form: Vombsjön
instance_of: Lake
countries: Sweden
coordinates: lat: 55.68083333
lon: 13.58861111
Nordhaug led Sky at the Tour of the Basque Country, where he came sixth overall. His promising early season form saw him take a prominent role in the team's Ardennes classics squad. Nordhaug was well placed in the closing stages of the Amstel Gold Race but crashed out in the final of the finishing climb, the Cauberg, after clashing wheels with 's Damiano Cunego.

Geographic entities mentioned:
surface_form: Cauberg
instance_of: Mountain
countries: Netherlands
coordinates: lat: 50.860278
lon: 5.823333
Tauber. The Tauber () is a river in Franconia (Baden-Württemberg and Bavaria), Germany. It is a left tributary of the Main and is in length. The name derives from the Celtic word for water (compare: Dover). Course. It flows through Rothenburg ob der Tauber, Creglingen, Weikersheim, Bad Mergentheim, Königshofen, Tauberbischofsheim, and flows into the river Main in Wertheim am Main.

Geographic entities mentioned:
surface_form: württemberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.7821
lon: 9.26867
surface_form: tauber
instance_of: Watercourse
countries: Germany
coordinates: lat: 49.25
lon: 10.114861111111
Tauber. The Tauber () is a river in Franconia (Baden-Württemberg and Bavaria), Germany. It is a left tributary of the Main and is in length. The name derives from the Celtic word for water (compare: Dover). Course. It flows through Rothenburg ob der Tauber, Creglingen, Weikersheim, Bad Mergentheim, Königshofen, Tauberbischofsheim, and flows into the river Main in Wertheim am Main.

Geographic entities mentioned:
surface_form: tauber
instance_of: Watercourse
countries: Germany
coordinates: lat: 49.25
lon: 10.114861111111