Sarmila/GeoWiki-Features huggingface dataset:
First incorporated into Ethiopia by Emperor Menelik II in the 1880s, its capital was first at Chencha, then around 1965 the capital was moved to Arba Minch. This province was bordered on the west and north by Kaffa, on the north and east by Sidamo, on the southeast by Lake Chew Bahir, and on the south by Kenya and Lake Turkana.

Geographic entities mentioned:
surface_form: Lake Chew Bahir
instance_of: Lake
countries: Ethiopia
Kenya
coordinates: lat: 4.6866666666667
lon: 36.851666666667
Leonid Kolotilo. Leonid Grigorievich Kolotilo (; born December 16, 1958, Leningrad) is a Soviet and Russian geographer, researcher of Lake Baikal, a full member of Academic Senate Russian Geographical Society, Captain 3rd Rank (1989). Author of over 100 scientific publications. D-SELF.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Geography. The hilly setting is filled with agricultural lands and surrounding houses. Sporadic forest cover and several hills lie to the east. The total area is approximately 2 km², its length is 1 km from north to south, and from east to west. The mountains dominate the northern part. The Panachaiko mountains lies to the east.

Geographic entities mentioned:
surface_form: Panachaiko
instance_of: Mountain
countries: Greece
coordinates: lat: 38.2025
lon: 21.868888888889
She won two medals in the 1964 Winter Olympics at Innsbruck, Austria. After graduating from college, Saubert became an educator. Early life. Born in Roseburg, Oregon, Saubert grew up in Cascadia and graduated from Lakeview High School in 1960. She learned to ski at Hoodoo Butte and raced competitively at Mount Hood and Mount Bachelor. Racing career. In 1962, Saubert earned a spot on the U.S.

Geographic entities mentioned:
surface_form: Hoodoo Butte
instance_of: Mountain
countries: United States
coordinates: lat: 44.4
lon: -121.88333333333
Killinierin. Kilanerin or Killinierin () is a village in north County Wexford, Ireland, 4 kilometres west of the N11 road, near the village of Inch and approximately 12 kilometres from the town of Gorey. It lies in the foothills of Croghan Mountain, the site of a once-famous gold rush. History and architecture. The Roman Catholic church in the village, St.

Geographic entities mentioned:
surface_form: Croghan Mountain
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.8
lon: -6.3166666666667
Kasinoet. Kasinoet (The Casino) is a mountain on Prins Karls Forland, Svalbard. It has a height of 949 m.a.s.l. and is located on the ridge of Grampianfjella, between Phippsfjellet and Monacofjellet.

Geographic entities mentioned:
surface_form: Grampianfjella
instance_of: Mountain
countries: Norway
coordinates: lat: 78.6239
lon: 10.9408
surface_form: Phippsfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 78.6392
lon: 10.9464
surface_form: Monacofjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 78.6567
lon: 10.9176
Kasinoet. Kasinoet (The Casino) is a mountain on Prins Karls Forland, Svalbard. It has a height of 949 m.a.s.l. and is located on the ridge of Grampianfjella, between Phippsfjellet and Monacofjellet.

Geographic entities mentioned:
surface_form: kasinoet
instance_of: Mountain
countries: Norway
coordinates: lat: 78.6517
lon: 10.9491
Cyamops femoratus. &quot; Cyamops femoratus&quot; is a species of fly. It is known from Lake Balinsasayao (Negros Island, the Philippines). Adult males measure and adult females in length.

Geographic entities mentioned:
surface_form: Lake Balinsasayao
instance_of: Lake
countries: Philippines
coordinates: lat: 9.3530555555556
lon: 123.17916666667
The devil tried to destroy the church bell tower and threw it with a large rock. However, the rock flew over the church to Tiirinkallio on the shore of Lake Loppijärvi, from where the rock was combed into the lake. The stone in the lake brought a disaster: cattle fell ill and animals died. So the villagers crammed the rock up the cliff and the luck of the cattle was restored.

Geographic entities mentioned:
surface_form: Lake Loppijärvi
instance_of: Lake
countries: Finland
coordinates: lat: 60.68333333
lon: 24.43333333
Lake Hirvijärvi flows into the Vantaa River watershed in the southeast on the border of Loppi, Riihimäki and Hyvinkää and Lake Keihäsjärvi in the south in Läyliäinen. Lake Keritty and Lake Punelia in the southwestern part of Loppi belong to the Svartån River watershed, which flows through Lake Lohja.

Geographic entities mentioned:
surface_form: Lake Lohja
instance_of: Lake
countries: Finland
coordinates: lat: 60.25
lon: 23.91666667
Description. Several small creeks flow into the lake, including a short creek from neighbouring Marean Lake. The outflow for the lake is Greenwater Creek, which exits the lake at the north-east corner and flows in a north-easterly direction, crossing Highways 38 and 23 near Chelan. About 3 miles north of Chelan, the Greenwater Creek meets up with the Red Deer River.

Geographic entities mentioned:
surface_form: Marean Lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.51667
lon: -103.56715
About 3 miles north of Chelan, the Greenwater Creek meets up with the Red Deer River. The Red Deer River is a major river in east central Saskatchewan and west central Manitoba as it is a major tributary of Lake Winnipegosis. Other than park amenities, there are no communities on the lake. Porcupine Plain, the closest town, is about away from the lake's main public access. Parks and recreation.

Geographic entities mentioned:
surface_form: Lake Winnipegosis
instance_of: Lake
countries: Canada
coordinates: lat: 52.5
lon: -100
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: winnipegosis
instance_of: Lake
countries: Canada
coordinates: lat: 52.5
lon: -100
Greenwater Lake. Greenwater Lake is a lake in the Canadian province of Saskatchewan. The lake is at the heart of Greenwater Lake Provincial Park in the Porcupine Provincial Forest on the Porcupine Hills. The RM of Bjorkdale No. 426 surrounds the lake and Highway 38 provides access to it.

Geographic entities mentioned:
surface_form: greenwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.516666666666666
lon: -103.50055555555555
Porcupine Plain, the closest town, is about away from the lake's main public access. Parks and recreation. The entirety of the lake is within the boundaries of Greenwater Lake Provincial Park. As such, there are a lot of activities and amenities in and around the lake, including Greenwater Lake Marina, Green Hills Golf Resort beaches, two boat launches, restaurants, camping, and fishing.

Geographic entities mentioned:
surface_form: greenwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.516666666666666
lon: -103.50055555555555
Parks and recreation. The entirety of the lake is within the boundaries of Greenwater Lake Provincial Park. As such, there are a lot of activities and amenities in and around the lake, including Greenwater Lake Marina, Green Hills Golf Resort beaches, two boat launches, restaurants, camping, and fishing. During the winter months, ice skating and snowmobiling are popular on the lake.

Geographic entities mentioned:
surface_form: greenwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.516666666666666
lon: -103.50055555555555
As such, there are a lot of activities and amenities in and around the lake, including Greenwater Lake Marina, Green Hills Golf Resort beaches, two boat launches, restaurants, camping, and fishing. During the winter months, ice skating and snowmobiling are popular on the lake. Greenwater Lake is part of the Greenwater Lake Provincial Park (SK 071) Important Bird Area (IBA) of Canada. Fish species.

Geographic entities mentioned:
surface_form: greenwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.516666666666666
lon: -103.50055555555555
surface_form: greenwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.516666666666666
lon: -103.50055555555555
During the winter months, ice skating and snowmobiling are popular on the lake. Greenwater Lake is part of the Greenwater Lake Provincial Park (SK 071) Important Bird Area (IBA) of Canada. Fish species. Fish commonly found in Greenwater Lake include northern pike, walleye, and yellow perch. Ice fishing is popular in the winter.

Geographic entities mentioned:
surface_form: greenwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.516666666666666
lon: -103.50055555555555
The battle was the last of the Swiss-Austrian conflicts that stretched through most of the 14th century. Background. A few weeks after the Battle of Sempach on 9 July 1386, the Swiss Confederation captured the Habsburg village of Weesen on the Walensee. The following year, Glarus rose up against the Habsburgs and destroyed Burg Windegg.

Geographic entities mentioned:
surface_form: Walensee
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.116666666667
lon: 9.2
It has about 1,900 inhabitants. Geography. Nový Šaldorf-Sedlešovice is urbanistically fused with neighbouring Znojmo and is located about southwest of Brno. It lies mostly in the Jevišovice Uplands, the southern part of the municipal territory lies in the Dyje–Svratka Valley. The highest point is the hill Kraví hora at above sea level.

Geographic entities mentioned:
surface_form: Dyje–Svratka Valley
instance_of: Valley
countries: Czech Republic
coordinates: lat: 49
lon: 16.5
Upper Canada. In 1832, Steele and his son John emigrated to Upper Canada, where as a British officer, Steele was entitled to a land grant. He settled on a large farm, 1,000 acres in size, in Medonte Township, north of Lake Simcoe. The rest of his family joined him the next year. In 1833, he was named a justice of the peace.

Geographic entities mentioned:
surface_form: Lake Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
Steele had a strong interest in local improvements. With others, he signed a petition in 1839 advocating the development of a water route connecting the Bay of Quinte to Lake Huron. They argued that it would improve internal trade from the upper Great Lakes to Upper Canada and to Lower Canada, and also provide an internal communications line in the event of another war with the United States.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
The county was established in 1836. The county seat is Front Royal. History. By 1672, the entire Shenandoah Valley was claimed for hunting by the Iroquois Confederation following the Beaver Wars. Some bands of the Shawnee settled in the area as client groups to the Iroquois and alternately to the Cherokee after 1721.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Over the next couple of days, the disturbance moved south-westwards and gradually developed further, before it was classified as a tropical depression by the FMS during April 7. The system subsequently continued to move south-westwards and passed near to or over the islands of Maewo, Ambae and Malakula in northern Vanuatu.

Geographic entities mentioned:
surface_form: Ambae
instance_of: Mountain
countries: Vanuatu
coordinates: lat: -15.4
lon: 167.83333333333
Towns found in the valley include Harrisville, Kalbar, Roadvale, Warril View and Aratula. Fassifern Valley is known as a carrot-producing area, as well as for growing potatoes, onions, pumpkins and melons. It is one of four vegetable-producing regions in southern Queensland, the others being the Lockyer Valley, the eastern Darling Downs and the Granite Belt.

Geographic entities mentioned:
surface_form: Lockyer Valley
instance_of: Valley
countries: Australia
coordinates: lat: -27.558833333333
lon: 152.27816666667
The Moogerah Peaks are a series of mountain peaks in the southeast of the catchment. To the east lies the valleys of the Logan River. Further to the west is the dry catchment of Laidley Creek and Lockyer Creek in the Lockyer Valley while Amberley is located just to the north of the valley. History.

Geographic entities mentioned:
surface_form: lockyer valley
instance_of: Valley
countries: Australia
coordinates: lat: -27.558833333333
lon: 152.27816666667
There is some uncertainty over the status of Jagara as a language, dialect or perhaps a group or clan within the local government boundaries of Ipswich City Council, Lockyer Regional Council and the Somerset Regional Council. Captain Patrick Logan was the first European to explore the valley in 1827, during which he climbed Mount French.

Geographic entities mentioned:
surface_form: mount french
instance_of: Mountain
countries: Australia
coordinates: lat: -28
lon: 152.617
Fassifern Valley. Fassifern Valley is a valley of the Scenic Rim in South East Queensland. Towns found in the valley include Harrisville, Kalbar, Roadvale, Warril View and Aratula. Fassifern Valley is known as a carrot-producing area, as well as for growing potatoes, onions, pumpkins and melons.

Geographic entities mentioned:
surface_form: fassifern valley
instance_of: Valley
countries: Australia
coordinates: lat: -27.810944444444
lon: 152.66505555556
Towns found in the valley include Harrisville, Kalbar, Roadvale, Warril View and Aratula. Fassifern Valley is known as a carrot-producing area, as well as for growing potatoes, onions, pumpkins and melons. It is one of four vegetable-producing regions in southern Queensland, the others being the Lockyer Valley, the eastern Darling Downs and the Granite Belt.

Geographic entities mentioned:
surface_form: fassifern valley
instance_of: Valley
countries: Australia
coordinates: lat: -27.810944444444
lon: 152.66505555556
The pair had arrived on the Darling Downs only to find all the best land already taken up. They eventually established themselves in the Fassifern Valley where number of other pastoral runs were established in the following decades, nearly all with familial connections to John Cameron. Cameron named the valley Fassefern which was a Scottish name.

Geographic entities mentioned:
surface_form: fassifern valley
instance_of: Valley
countries: Australia
coordinates: lat: -27.810944444444
lon: 152.66505555556
Moogerah Dam. Lake Moogerah was built on Reynolds Creek which runs into Warril Creek a tributary of the Bremer River which drains the slopes to the west of Fassifern Valley. Irrigation allowed local farmers to diversify crops after dairy farming declined in the 1960s.

Geographic entities mentioned:
surface_form: fassifern valley
instance_of: Valley
countries: Australia
coordinates: lat: -27.810944444444
lon: 152.66505555556
In September 1887, the Dugandan railway line was opened connecting Dugandan to the main line in the north. Timber-cutting served at least five sawmills in the area. The Mount Edwards railway line, a branch line of the Dugandan railway, serviced a number of towns in the valley between 1922 and 1960. Agriculture. Warril Creek provides a reliable water source for irrigated crop vegetables.

Geographic entities mentioned:
surface_form: mount edwards
instance_of: Mountain
countries: Australia
coordinates: lat: -28.0164
lon: 152.55
It is one of four vegetable-producing regions in southern Queensland, the others being the Lockyer Valley, the eastern Darling Downs and the Granite Belt. The Cunningham Highway passes through the town of Aratula and along ridges in the upper valley towards Cunninghams Gap, Mount Mitchell and parts of the Main Range National Park.

Geographic entities mentioned:
surface_form: mount mitchell
instance_of: Mountain
countries: Australia
coordinates: lat: -28.066388888889
lon: 152.4
Kälberbuckel. Kälberbuckel is a mountain in Bavaria, Germany. It is located west of the village of Achslach in the Bavarian Forest. The mountain is almost entirely forested. The nearest neighboring mountains are Predigtstuhl (1024 m) to the northwest and Hirschenstein (1092 m) to the southeast, along the same ridge.

Geographic entities mentioned:
surface_form: predigtstuhl
instance_of: Mountain
countries: Germany
coordinates: lat: 47.6972
lon: 12.8786
surface_form: hirschenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 48.963888888889
lon: 12.879722222222
surface_form: predigtstuhl
instance_of: Mountain
countries: Germany
coordinates: lat: 49.002222
lon: 12.849167
surface_form: hirschenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 50.593
lon: 12.5725
Kälberbuckel. Kälberbuckel is a mountain in Bavaria, Germany. It is located west of the village of Achslach in the Bavarian Forest. The mountain is almost entirely forested. The nearest neighboring mountains are Predigtstuhl (1024 m) to the northwest and Hirschenstein (1092 m) to the southeast, along the same ridge.

Geographic entities mentioned:
surface_form: kälberbuckel
instance_of: Mountain
countries: Germany
coordinates: lat: 48.9753
lon: 12.8869
In 2010, Britain failed to send a diplomatic representative to the opening of the National Famine Commemoration at the Murrisk Millennium Peace Park, at the foot of Croagh Patrick, County Mayo. Representatives of 14 other nations were present including the United States and Australia as well as the European Parliament. The Irish government was represented by several ministers.

Geographic entities mentioned:
surface_form: Croagh Patrick
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.7595
lon: -9.6584
&quot;Crucán na bPáiste&quot; – 'the burial place of (unbaptised) children' – lies on a hilltop in Maumtrasna, County Mayo, overlooking Loch Na Fooey, and Lough Mask in Ireland. It is a lament by a mother for a child she buries there during &quot;Aimsir an Drochshaoil&quot; ('The Time of the Bad Life' – the Famine).

Geographic entities mentioned:
surface_form: Maumtrasna
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.612
lon: -9.57
surface_form: Loch Na Fooey
instance_of: Lake
countries: Ireland
coordinates: lat: 53.577777777778
lon: -9.5480555555556
surface_form: Lough Mask
instance_of: Lake
countries: Ireland
coordinates: lat: 53.621944444444
lon: -9.3822222222222
Mathiesenfjella. fn8c15pu1prh3qc1wt7x9z4a3yu1u" xml:space="preserve">Mathiesenfjella is a mountain group in Oscar II Land at Spitsbergen, Svalbard. The group is named after Norwegian businessman Haaken L. Mathiesen. The group includes the mountain of Haakentoppen, as well as the glacier of Haakenbreen.

Geographic entities mentioned:
surface_form: Haakentoppen
instance_of: Mountain
countries: Norway
coordinates: lat: 78.748
lon: 12.065
Mathiesenfjella. fn8c15pu1prh3qc1wt7x9z4a3yu1u" xml:space="preserve">Mathiesenfjella is a mountain group in Oscar II Land at Spitsbergen, Svalbard. The group is named after Norwegian businessman Haaken L. Mathiesen. The group includes the mountain of Haakentoppen, as well as the glacier of Haakenbreen.

Geographic entities mentioned:
surface_form: mathiesenfjella
instance_of: Mountain
countries: Norway
coordinates: lat: 78.742
lon: 12.037
Lussi was born in Stans, Switzerland. He himself was not a competitive skater but a ski jumper. He lost his nerve for that sport after a fall, and became interested in skating instead. His previous experience with the sport was only recreational skating on Lake Lucerne as a boy. In 1919, Lussi emigrated to the United States, landing in New York City. He became a U.S. citizen in 1927.

Geographic entities mentioned:
surface_form: Lake Lucerne
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.0194
lon: 8.4011
A. Mahood. Exploration and construction teams were divided into groups: one was in British Columbia, another worked around the Yukon River and Norton Sound with headquarters at St. Michael, Alaska, a third explored the area along the Amur River in Siberia, and a fourth group of about forty men was sent to Port Clarence to build the line that was to cross the Bering Strait to Siberia.

Geographic entities mentioned:
surface_form: Norton Sound
instance_of: Landform
countries: United States
coordinates: lat: 63.849166666667
lon: -164.26888888889
I found one of the old green glass insulators still attached to a galvanized wire. I kept it as a souvenir but lost it later with a camera and some clothing when a scow was nearly overturned on Lake Laberge. Books and memoirs written about the expedition. Several major works are available documenting the expedition. The scientific travelogue by Smithsonian scientist W. H.

Geographic entities mentioned:
surface_form: Lake Laberge
instance_of: Lake
countries: Canada
coordinates: lat: 61.169444444444
lon: -135.16944444444
Together with the neighbouring river Ilisos, it drains a catchment area of. The &quot;Bibliotheca&quot; (3.15.1) states that the legendary Erechtheus' wife Praxithea was the daughter of Phrasimus (otherwise unknown to us) by Diogenia (otherwise unknown to us) daughter of Cephissus. The source of the river is in the saddle depression between the Parnitha and Penteli mountains.

Geographic entities mentioned:
surface_form: Penteli
instance_of: Mountain
countries: Greece
coordinates: lat: 38.08144
lon: 23.8825
Brompton Regis. Brompton Regis (formerly known as Kingsbrompton) is a village and civil parish in Somerset, England about north-east of Dulverton. It is situated on the River Pulham in the Brendon Hills within the Exmoor National Park, close to Wimbleball Lake, a water supply reservoir constructed in the 1970s and completed in 1979. According to the 2011 census the village had a population of 449.

Geographic entities mentioned:
surface_form: Wimbleball Lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.066666666667
lon: -3.4666666666667
Kelachay. Kelachay () is a city in, and the capital of, Kelachay District of Rudsar County, Gilan province, Iran. It is on the Caspian Sea. Population. At the time of the 2006 National Census, the city's population was 11,304 in 3,338 households. The following census in 2011 counted 11,936 people in 3,831 households.

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
Geography. Lakhimpur is located at. It has an average elevation of. It shares its boundaries with –
Its main rivers are Sharda, Ghaghara, Koriyala, Ull, Sarayan, Chauka, Gomti, Kathana, Saryu and Mohana. Climate. The climate is hot throughout the year except the rainy seasons. In winter, nights are very cold. Fog is very common in this season. Demographics.

Geographic entities mentioned:
surface_form: Sarayan
instance_of: Watercourse
countries: India
coordinates: lat: 27.7666666667
lon: 80.5333333333
History. The district was created in 1938, when the two former districts Bensheim and Heppenheim were merged. Geography. The Bergstraße district is situated along the western slopes of the Odenwald mountains in southern Hesse, Germany. Its highest point is the Melibokus, a 517-meter (1,696-foot) hill near Zwingenberg.

Geographic entities mentioned:
surface_form: Melibokus
instance_of: Mountain
countries: Germany
coordinates: lat: 49.725208333333
lon: 8.6368166666667
All
in the AVA are owned by the Diablo Grande Resort Community, and Isom Ranch Winery is the only winery producing wines that carry the Diablo Grande AVA designation on their labels. Vineyards in the AVA are planted between and above sea level. The region is named after nearby Mount Diablo, the highest peak in the Pacific Coast Range.

Geographic entities mentioned:
surface_form: Mount Diablo
instance_of: Mountain
countries: United States
coordinates: lat: 37.881697781
lon: -121.914154997
Primitive Baptist Church of Sweeten's Cove. Primitive Baptist Church of Sweeten's Cove is a historic Primitive Baptist church in Marion County, Tennessee, located in the Sweeten's Cove area in the Sequatchie Valley, about north of South Pittsburg.

Geographic entities mentioned:
surface_form: Sequatchie Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.125
lon: -85.5289
Like other volcanic provinces or &quot;traps&quot;, the Emeishan Traps are multiple layers of igneous rock laid down by large mantle plume volcanic eruptions. The Emeishan Traps eruptions were serious enough to have global ecological and paleontological impact. It is named for Emeishan, a mountain in Sichuan. Etymology.

Geographic entities mentioned:
surface_form: Emeishan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 29.519722222222
lon: 103.3325
Glidewell, Missouri. Glidewell is an unincorporated community in Greene County, Missouri, United States. Glidewell is located approximately four miles north of Springfield, just east of Missouri Route 13 on a county road that accesses McDaniel Lake on the Little Sac River.

Geographic entities mentioned:
surface_form: McDaniel Lake
instance_of: Lake
countries: United States
coordinates: lat: 37.3024618
lon: -93.3045031
Dromod. Dromod or Drumod () is a village in County Leitrim, Ireland. Dromod is a fishing village beside Bofin and Boderg, which are threaded by the River Shannon. Built along the River Shannon, this is a Tidy Towns winner with a modern harbour that is frequently used by cruiser traffic.

Geographic entities mentioned:
surface_form: Boderg
instance_of: Lake
countries: Ireland
coordinates: lat: 53.871264
lon: -7.978204
Snorri Sturlason’s &quot;Heimskringla&quot; recounts that Haakon the Good (935–961) took an active part in the assemblies at Gulen, and under his rule the regions of Rogaland, Agder and Sunnmøre were brought into the area covered by the thing, with Valdres and Hallingdal also being incorporated later. Special legislation, (the Gulating law), was drafted to aid the discussions.

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
Durley, Illinois. Durley is an unincorporated community in Bond County, Illinois, United States. Durley is northeast of Greenville near Governor Bond Lake. History. Durley was laid out in the 1880s. The community bears the name of Horatio Durley, a local pioneer. A post office was established at Durley in 1888, and remained in operation until 1903.

Geographic entities mentioned:
surface_form: Governor Bond Lake
instance_of: Lake
countries: United States
coordinates: lat: 38.9242
lon: -89.3987
Flagstaff Glacier. Flagstaff Glacier () is a very small glacier lying immediately north of Flagstaff Hill on Keller Peninsula, King George Island, in the South Shetland Islands. The name arose locally in about 1958 and derives from association with Flagstaff Hill.

Geographic entities mentioned:
surface_form: Keller Peninsula
instance_of: Mountain
coordinates: lat: -62.0833
lon: -58.4333
Povien Bluff. rwki82w835ukaif43ay9u1cvsvrk" xml:space="preserve">#redirect Povien Peak

Geographic entities mentioned:
surface_form: povien bluff
instance_of: Mountain
coordinates: lat: -63.9822
lon: -58.97
Distribution and habitat. This species grows in mountainous rainforest in the Ngalba Bulal National Park, the headwaters of the Daintree River, on Mount Bartle Frere and in the catchment of the South Johnstone River in far north Queensland.

Geographic entities mentioned:
surface_form: Mount Bartle Frere
instance_of: Mountain
countries: Australia
coordinates: lat: -17.383333333333
lon: 145.81666666667
3500 South MAX. 3500 South MAX was a bus rapid transit (BRT) line in northwestern Salt Lake County, Utah, United States, operated by the Utah Transit Authority (UTA) that ran between Magna, West Valley City, and South Salt Lake. It opened for service on July 14, 2008, and was the first of several BRT lines that UTA is planning in the Salt Lake Valley, Weber County, and Utah County.

Geographic entities mentioned:
surface_form: Salt Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.6839
lon: -111.978
The Green Line provides service from West Valley City to the Salt Lake City International Airport via Downtown Salt Lake City, the Blue Line provides service from Draper to Downtown Salt Lake City, and the Red Line provides service from the University of Utah to the Daybreak Community in South Jordan in southwest Salt Lake Valley.

Geographic entities mentioned:
surface_form: Salt Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.6839
lon: -111.978
Höfen. The oldest trace of a settlement in the area is a single Neolithic artifact which was found in the Hofallmend. During the Middle Ages a small hunting estate, known as the &quot;Turm zu Stocken&quot; or &quot;Friedberg&quot;, was built above the Amsoldingersee. Very little is known of its early history, but in 1308 the Duke of Austria granted it to the knightly Amsoldingen family.

Geographic entities mentioned:
surface_form: Amsoldingersee
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.723888888889
lon: 7.5769444444444
The name &quot;Satah&quot; is Chilcotin in origin, meaning &quot;Of the Sun and Moon&quot;. Merston made some land surveys in the Upper Chilcotin Valley and a triangulation and topographical survey over an area extending eastward from Anahim Peak to the 124th meridian. The topographical work extended over the Itcha Range, which lies north-northwest of Satah Mountain. Geology.

Geographic entities mentioned:
surface_form: Anahim Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.7578
lon: -125.625
surface_form: anahim peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.7578
lon: -125.625
Satah Mountain. Satah Mountain is a twin-peaked mountain in the West-Central Interior of British Columbia, Canada. It is southeast of Punkutlaenkut Lake and east of the community of Anahim Lake in Range 3 Coast Land District. History. The name of the mountain was adopted 13 March 1947 on topographic map 93/SW.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: satah mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.4758
lon: -124.69
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: twin
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.72361111
lon: -131.21166667
History. The name of the mountain was adopted 13 March 1947 on topographic map 93/SW. Prior to this, the mountain was given the name &quot;Mount Lion&quot; which appeared on 2T268, a plan drawn in 1923 by W. Merston who was a member of the Association of British Columbia Land Surveyors (BCLS). The name &quot;Satah&quot; is Chilcotin in origin, meaning &quot;Of the Sun and Moon&quot;.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Satah Mountain. Satah Mountain is a twin-peaked mountain in the West-Central Interior of British Columbia, Canada. It is southeast of Punkutlaenkut Lake and east of the community of Anahim Lake in Range 3 Coast Land District. History. The name of the mountain was adopted 13 March 1947 on topographic map 93/SW.

Geographic entities mentioned:
surface_form: satah mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.4758
lon: -124.69
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The name &quot;Satah&quot; is Chilcotin in origin, meaning &quot;Of the Sun and Moon&quot;. Merston made some land surveys in the Upper Chilcotin Valley and a triangulation and topographical survey over an area extending eastward from Anahim Peak to the 124th meridian. The topographical work extended over the Itcha Range, which lies north-northwest of Satah Mountain. Geology.

Geographic entities mentioned:
surface_form: satah mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.4758
lon: -124.69
surface_form: satah mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.4758
lon: -124.69
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The western summit is flat-topped and resembles a tuya whereas the eastern summit retains the morphology of a cone with its southwestern rim having been breached by a in diameter crater. A small breached scoria ring on the northern flank of Satah Mountain appears largely unmodified by glacial erosion, implying that it might be younger than the main edifice.

Geographic entities mentioned:
surface_form: satah mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.4758
lon: -124.69
surface_form: satah mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.4758
lon: -124.69
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
A small breached scoria ring on the northern flank of Satah Mountain appears largely unmodified by glacial erosion, implying that it might be younger than the main edifice. Satah Mountain is one of the largest volcanoes in the Satah Mountain volcanic field (SMVF). Polygenetic in nature, the volcano was sporadically active 1.83–1.77 million years ago during the Early Pleistocene.

Geographic entities mentioned:
surface_form: satah mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.4758
lon: -124.69
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Polygenetic in nature, the volcano was sporadically active 1.83–1.77 million years ago during the Early Pleistocene. This contrasts with most SMVF volcanoes, which are smaller in volume and likely had episodic and short-lived activity. The only other polygenetic volcano in the SMVF is Mount Punkutlaenkut, a volcanic cone west-northwest of Satah Mountain.

Geographic entities mentioned:
surface_form: satah mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.4758
lon: -124.69
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
History. The name of the mountain was adopted 13 March 1947 on topographic map 93/SW. Prior to this, the mountain was given the name &quot;Mount Lion&quot; which appeared on 2T268, a plan drawn in 1923 by W. Merston who was a member of the Association of British Columbia Land Surveyors (BCLS). The name &quot;Satah&quot; is Chilcotin in origin, meaning &quot;Of the Sun and Moon&quot;.

Geographic entities mentioned:
surface_form: mount lion
instance_of: Mountain
countries: Canada
coordinates: lat: 52.4758
lon: -124.69
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
It is southeast of Punkutlaenkut Lake and east of the community of Anahim Lake in Range 3 Coast Land District. History. The name of the mountain was adopted 13 March 1947 on topographic map 93/SW. Prior to this, the mountain was given the name &quot;Mount Lion&quot; which appeared on 2T268, a plan drawn in 1923 by W.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Harmer Glacier. Harmer Glacier () is a glacier long, flowing southwest from Starbuck Peak to the sea close north of Ranvik, on the south coast of South Georgia. It was surveyed by the South Georgia Survey in the period 1951–57, and named by the UK Antarctic Place-Names Committee for Sir Sidney F. Harmer.

Geographic entities mentioned:
surface_form: Starbuck Peak
instance_of: Mountain
countries: South Georgia and the South Sandwich Islands
United Kingdom
coordinates: lat: -54.7333
lon: -36.2
It is situated in the Potosí Department, Antonio Quijarro Province, Tomave Municipality, Tomave Canton, east of the Uyuni salt flat and south-west of the Nuevo Mundo volcano (Jatun Mundo Quri Warani) and Kuntur Chukuña.

Geographic entities mentioned:
surface_form: Nuevo Mundo
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.774166666667
lon: -66.478333333333
surface_form: kuntur chukuña
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.91666667
lon: -66.51666667
surface_form: kuntur chukuña
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.39055556
lon: -66.59555556
surface_form: nuevo mundo volcano
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.774166666667
lon: -66.478333333333
surface_form: jatun mundo quri warani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.774166666667
lon: -66.478333333333
surface_form: kuntur chukuña
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.25
lon: -66.71666667
Mount Uyuni. Uyuni (Aymara, &quot;uyu&quot; pen (enclosure), yard, cemetery, &quot;-ni&quot; a suffix to indicate ownership, &quot;the one that has got a pen&quot;, &quot;the one with a pen&quot;) is a mountain in the Andes of Bolivia, about 5,084 metres (16,680 ft) high.

Geographic entities mentioned:
surface_form: mount uyuni
instance_of: Mountain
countries: Bolivia
coordinates: lat: -20
lon: -66.58333333
Tunupa. Tunupa is a dormant volcano in the Potosí Department of southwestern Bolivia. It stands on the northern side of the Salar de Uyuni at an elevation of on the Bolivian Altiplano. Tunupa was active in the Pleistocene, with most of the volcano constructed by lava flows that erupted between 1.36 and 1.56 million years ago. Later glaciers developed on the mountain.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Later glaciers developed on the mountain. There is a cave with several mummies about halfway up and an ancient village at the foot with a modest &quot;salt hotel&quot;. Geography and geomorphology. Tunupa is located in Bolivia, at the centre of the Altiplano about east of the main volcanic arc. It forms a peninsula in the Salar de Uyuni, which surrounds the volcano on its southern side.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Volcanism in the backarc of the Central Andes is represented by several types of volcanoes, including several monogenetic volcanoes, stratovolcanoes such as Cerro Tuzgle, Tunupa and Uturunku and large ignimbrites like Altiplano-Puna volcanic complex, Galán, Los Frailes volcanic field and Morococala.

Geographic entities mentioned:
surface_form: Galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
surface_form: tunupa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.83
lon: -67.64
Three separate stages of glaciation have been inferred at Tunupa, one dating proposal dates the first advance to about 160,000 before present, the second lasts until about 15,000 years/may coincide with the existence of Lake Tauca before present and the last one occurred during the Younger Dryas.

Geographic entities mentioned:
surface_form: Lake Tauca
instance_of: Lake
countries: Peru
coordinates: lat: -20
lon: -68
surface_form: tunupa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.83
lon: -67.64
The southern slopes of Tunupa are incised by the shorelines of former lakes that occupied the Altiplano, such as Lake Minchin and Lake Tauca. Crusts of algae, stromatolites and river deltas are also found at these former shorelines. Over seven separate shoreline stages have been identified at Tunupa, which was part of an island in Lake Tauca.

Geographic entities mentioned:
surface_form: Lake Tauca
instance_of: Lake
countries: Peru
coordinates: lat: -20
lon: -68
surface_form: tunupa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.83
lon: -67.64
Crusts of algae, stromatolites and river deltas are also found at these former shorelines. Over seven separate shoreline stages have been identified at Tunupa, which was part of an island in Lake Tauca. It is likely that evaporation from the lake increased precipitation at Tunupa and thus allowed glaciers to grow to larger sizes than they would have without such evaporation. Geology.

Geographic entities mentioned:
surface_form: Lake Tauca
instance_of: Lake
countries: Peru
coordinates: lat: -20
lon: -68
surface_form: tunupa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.83
lon: -67.64
Presently, the Nazca Plate is subducting eastward below South America. The subduction is responsible for the formation of the Altiplano high plateau; the Tibetan Plateau is the only other place in the world where oceanic subduction has generated a high plateau. Volcanism in the Andes occurs in a frontal volcanic arc, but also in the back-arc region.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
East of Tunupa lie the Huayrana lavas, which are much older (Potassium-argon dating has yielded an age of 11.1 ± 0.4 million years ago). Tunupa and Sillajhuay farther west form a chain of volcanoes known as the Serranía Intersalar, which lies within the so-called Pica gap where recent volcanism is rare. This chain of volcanoes was active starting from the Oligocene to the Quaternary. Composition.

Geographic entities mentioned:
surface_form: Sillajhuay
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -19.75
lon: -68.7
Tunupa. Tunupa is a dormant volcano in the Potosí Department of southwestern Bolivia. It stands on the northern side of the Salar de Uyuni at an elevation of on the Bolivian Altiplano. Tunupa was active in the Pleistocene, with most of the volcano constructed by lava flows that erupted between 1.36 and 1.56 million years ago. Later glaciers developed on the mountain.

Geographic entities mentioned:
surface_form: tunupa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.83
lon: -67.64
The volcano rises about above the surrounding terrain, the summit of the volcano is heavily hydrothermally altered and its summit crater degraded by erosion, with crags representing remnants of the old lava conduit. Several lava domes were emplaced on top of lava flows from Tunupa on its eastern flank. Pyroclastic flows are found on the northern flank.

Geographic entities mentioned:
surface_form: tunupa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.83
lon: -67.64
Pyroclastic flows are found on the northern flank. Erosion and glaciation have generated a deposit of eroded material that surrounds much of the volcano. There is no present-day permanent ice on Tunupa as the region is too dry but the mountain was glaciated in the past, and large valley glaciers descended to elevations of when they reached their largest extent.

Geographic entities mentioned:
surface_form: tunupa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.83
lon: -67.64
Crusts of algae, stromatolites and river deltas are also found at these former shorelines. Over seven separate shoreline stages have been identified at Tunupa, which was part of an island in Lake Tauca. It is likely that evaporation from the lake increased precipitation at Tunupa and thus allowed glaciers to grow to larger sizes than they would have without such evaporation. Geology.

Geographic entities mentioned:
surface_form: tunupa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.83
lon: -67.64
Volcanism in the Andes occurs in a frontal volcanic arc, but also in the back-arc region. This back-arc volcanism that Tunupa is part of has an uncertain origin; one proposed process is delamination, whereby the lowermost mafic section of the crust and lithosphere underneath separates itself from the above lying layers.

Geographic entities mentioned:
surface_form: tunupa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.83
lon: -67.64
Back-arc volcanism in the region started about 25-30 million years ago. East of Tunupa lie the Huayrana lavas, which are much older (Potassium-argon dating has yielded an age of 11.1 ± 0.4 million years ago). Tunupa and Sillajhuay farther west form a chain of volcanoes known as the Serranía Intersalar, which lies within the so-called Pica gap where recent volcanism is rare.

Geographic entities mentioned:
surface_form: tunupa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.83
lon: -67.64
The lava domes are more silicic than the main volcanic edifice. An average magma output of has been estimated, which is comparable to Lascar and Parinacota. Delamination of the crust, hydration-induced melting and magma mixing processes have been used to explain the magma chemistry at Tunupa.

Geographic entities mentioned:
surface_form: tunupa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.83
lon: -67.64
Eruption history. Initial Potassium-argon dating has yielded ages of 2.5 ± 0.5 and 1.8 ± 0.2 million years ago on samples from Tunupa. Later performed argon-argon dating produced ages between 1.55 ± 0.01 and 1.40 ± 0.04 million years ago, with even younger dates of 440,000 ± 40,000 years before present. The main edifice developed first, the lava domes were emplaced later.

Geographic entities mentioned:
surface_form: tunupa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.83
lon: -67.64
The main edifice developed first, the lava domes were emplaced later. The volcano is considered to be extinct. Mythology. In Aymara legends, Tunupa is personified as a deity with varying attributes and often linked to legends about the origin of the Salar de Uyuni.

Geographic entities mentioned:
surface_form: tunupa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.83
lon: -67.64
Monson Lake State Park is located west of Sunburg and west of the junction of  9 and MN 104. The park entrance is located off MN 9 via County Road 95 (CR 95). A portion of the route passes through the Red River Valley region in northwest Minnesota. East–west section. The eastern terminus for MN 9 is its intersection with MN 23 in New London in west-central Minnesota.

Geographic entities mentioned:
surface_form: Red River Valley
instance_of: Valley
countries: Canada
United States
coordinates: lat: 49
lon: -97.5
The eastern two-thirds of Meriwether County, going east from just west of U.S. Route 27 Alternate, is located in the Upper Flint River sub-basin of the ACF River Basin (Apalachicola-Chattahoochee-Flint River Basin). The western third of the county is located in the Middle Chattahoochee River-Lake Harding sub-basin of the same ACF River Basin. Demographics.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Janke Nunatak. xd6cjwn8rmuof0nmgqt1h8dq577" xml:space="preserve">#redirect Janke Nunatak

Geographic entities mentioned:
surface_form: janke nunatak
instance_of: Mountain
coordinates: lat: -75.8833
lon: -70.45
There are important historical monuments in Tsalka: Kldekari Fortress (ninth century) and the church of St. George in Dashbashi (tenth-eleventh centuries). Dashbashi Canyon and its new bridge are also interesting tourist attractions. Geography. The town and municipality center of Tsalka is located south of the Tsalka Plateau in the Trialeti region, about 60 km southwest of the capital Tbilisi.

Geographic entities mentioned:
surface_form: Tsalka Plateau
instance_of: Plateau
countries: Georgia
coordinates: lat: 41.61666666666667
lon: 44