Sarmila/GeoWiki-Features huggingface dataset:
Skelghyll Beck. g3sdq16m2hehpe5bxtvjiossl786z" xml:space="preserve">Skelghyll Beck is a Site of Special Scientific Interest (SSSI) within Lake District National Park in Cumbria, England. It is located 2 km southeast of the town of Ambleside. The protected area is located 1 km east of Lake Windermere. Skelghyll Beck flows into Lake Windermere.

Geographic entities mentioned:
surface_form: Lake Windermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.358333333333
lon: -2.9361111111111
The townland of Slievenakilla is practically divided by the Yellow River which flows initially west, passes under the road between Ballinagleragh and Stralongford, turns north and follows an approximate WNW course until Sranagarvanagh townland where it turns towards the southwest. At Fahy the river discharges into Lough Allen, effectively becoming a tributary of the River Shannon. Wildlife.

Geographic entities mentioned:
surface_form: Lough Allen
instance_of: Lake
countries: Ireland
coordinates: lat: 54.106944444444
lon: -8.0391666666667
Wareham, Dorset. Wareham () is an historic market town and, under the name Wareham Town, a civil parish, in the English county of Dorset. The town is situated on the River Frome southwest of Poole. Situation and geography. The town is built on a strategic dry point between the River Frome and the River Piddle at the head of the Wareham Channel of Poole Harbour.

Geographic entities mentioned:
surface_form: River Frome
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 50.6958
lon: -1.98861
The town is situated on the River Frome southwest of Poole. Situation and geography. The town is built on a strategic dry point between the River Frome and the River Piddle at the head of the Wareham Channel of Poole Harbour. The Frome Valley runs through an area of unresistant sand, clay and gravel rocks, and much of its valley has wide flood plains and marsh land.

Geographic entities mentioned:
surface_form: River Frome
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 50.6958
lon: -1.98861
Harris Lake (Berrien County, Michigan). Harris Lake is a lake in Berrien County, in the U.S. state of Michigan. The lake is in size. Harris Lake was named after Benjamin Harris, a pioneer who settled at the lake in 1850.

Geographic entities mentioned:
surface_form: harris lake
instance_of: Lake
countries: United States
coordinates: lat: 42.222777777778
lon: -86.356388888889
There are a number of works dedicated to him or his rule, including the 1969 film &quot;Tsar Ivan Shishman&quot; by Yuri Arnaudov and the song &quot;Tsar Ivan Shishman&quot; by the heavy metal band Epizod in the 2004 album &quot;Saint Patriarch Evtimiy&quot;. Shishman Peak on Livingston Island in the South Shetland Islands, Antarctica is also named after him. Legends.

Geographic entities mentioned:
surface_form: Shishman Peak
instance_of: Mountain
countries: Argentina
coordinates: lat: -62.649861111111
lon: -59.991111111111
Early life. Aung Kyaw Moe was born in 1983 in Maungdaw in Rakhine State, Myanmar. This town lies on the shore of the Naf River near to the entry of the river into the Bay of Bengal. The Naf River forms part of the border between Bangladesh and Myanmar. In 2016 and 2017, the Burmese military committed genocide and crimes against humanity against the Rohingya people in Rakhine.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Early life. Dotson was born on March 22, 2000, in Newark, New Jersey, and grew up in nearby East Orange, before moving to Pennsylvania. He attended Nazareth Area High School in Nazareth, Pennsylvania in the Lehigh Valley He left for Peddie School in Hightstown, New Jersey, for his junior year but then returned to Nazareth High School for his senior year in 2017.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Tsitika Mountain. Tsitika Mountain is a mountain on Vancouver Island, British Columbia, Canada, located southeast of Telegraph Cove and northwest of Mount Abel.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
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: mount abel
instance_of: Mountain
countries: Canada
coordinates: lat: 50.2119
lon: -126.32
surface_form: tsitika mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.4267
lon: -126.652
Tsitika Mountain. Tsitika Mountain is a mountain on Vancouver Island, British Columbia, Canada, located southeast of Telegraph Cove and northwest of Mount Abel.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: tsitika mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.4267
lon: -126.652
Abernethy Forest. Abernethy Forest is a remnant of the Caledonian Forest in Strathspey, in the Highland council area of Scotland. It lies within the Cairngorms National Park, close to the villages of Nethy Bridge, Boat of Garten, and Aviemore. The forest is an RSPB reserve, close to Loch Garten Osprey Centre, which is also owned by the RSPB.

Geographic entities mentioned:
surface_form: Strathspey
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.45
lon: -3.3
The Dell Woods section was added 1988, forming a 375 hectare extension to the existing NNR. In 2007, the NNR was greatly extended, becoming the new Abernethy National Nature Reserve, which extends from Abernethy Forest itself up into high Cairngorms, taking in Loch A'an and the mountains of Bynack More, Beinn Mheadhoin and the southern side of Cairn Gorm.

Geographic entities mentioned:
surface_form: Loch A'an
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.1
lon: -3.6333333333333
surface_form: Bynack More
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.13822
lon: -3.584716
surface_form: Cairn Gorm
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.116714
lon: -3.644477
Readfield was set off and incorporated in 1791. The surface of the town is uneven, but with good land that yielded hay, grain and apples. Winthrop became noted for its orchards and cattle. At the outlet of Maranacook Lake into Annabessacook Lake, John Chandler built a sawmill in 1768, and then added a gristmill. Other industries followed, including a fulling mill, tannery and blacksmith shop.

Geographic entities mentioned:
surface_form: Maranacook Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.343
lon: -69.951
surface_form: Annabessacook Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.26833333333333
lon: -69.98102777777778
Winthrop Lakes Region. Winthrop is at the center of the Winthrop Lakes Region, which is situated between Lewiston and Augusta, Maine, and centered around six major bodies of water: Androscoggin Lake, Annabessacook Lake, Cobbosseecontee Lake, Echo Lake, Maranacook Lake and Parker Pond, in addition to numerous smaller bodies of water.

Geographic entities mentioned:
surface_form: Androscoggin Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.3242
lon: -70.0844
surface_form: Annabessacook Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.26833333333333
lon: -69.98102777777778
surface_form: Cobbosseecontee Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.25
lon: -69.933333333333
surface_form: Maranacook Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.343
lon: -69.951
Since then, Largo do Paiçandu has remained poorly valued, maintaining its peripheral character with low occupancy. From the 1920s onwards, with the expansion of the city into the Anhangabaú Valley and the formation of the Centro Novo, the Paiçandu area began to receive proper attention. In 1922, the famous Ponto Chic snack bar, a place of cultural and political turmoil in São Paulo, was set up.

Geographic entities mentioned:
surface_form: Anhangabaú Valley
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
It is bordered to the north by the National Petroleum Reserve–Alaska. The lower valley of the Noatak is not part of the preserve, separating the preserve from Cape Krusenstern National Monument on the coast. The southeast corner of the preserve runs almost to the coastline at Hotham Inlet. The distance from the headwaters in Gates of the Arctic National Park to Noatak, Alaska is about.

Geographic entities mentioned:
surface_form: Hotham Inlet
instance_of: Landform
countries: United States
coordinates: lat: 66.819722222222
lon: -161.965
The original hotel building would be torn down in the 1970s, but the golf course remains. The Bermudiana. The Bermudiana hotel was constructed through 1923 and opened on January 28, 1924.It had 248 rooms located on Hamilton Harbor. The hotel would close in 1939 after the start of World War II, opening again in 1941 to house members of the Imperial Censorship.

Geographic entities mentioned:
surface_form: Hamilton Harbor
instance_of: Landform
countries: United Kingdom
coordinates: lat: 32.289164
lon: -64.784195
Lermontov (town). Lermontov () is a town in Stavropol Krai, Russia, located on the mountainside of Beshtau. Population: 16,500 (1973). History. It was named after Russian poet Mikhail Lermontov. It was granted town status in 1956. Uranium mining boosted its growth. It was a closed town during the Soviet era. Uranium is no longer mined. Administrative and municipal status.

Geographic entities mentioned:
surface_form: Beshtau
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 44.098055555556
lon: 43.022222222222
Glenariff. Glenariff or Glenariffe (or) is a valley in County Antrim, Northern Ireland. It is one of the Glens of Antrim. Like other glens in that area, it was shaped during the Ice Age by giant glaciers. It is sometimes called the 'Queen of the Glens', and is the biggest of the Glens of Antrim and visited by most tourists. The village of Waterfoot lies on the coast at the foot of the glen.

Geographic entities mentioned:
surface_form: Glens of Antrim
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.16
lon: -6.1
The subsequent king of Iar Connacht, Muireadhach Ua Flaithbheartaigh (died 1121), and his descendants, remained loyal to the Ó Conchobair's. Before the close of the 13th century, the Chiefs of Clan Ó Flaithbertaigh became Lords of Iar Connacht, extending from the western banks of Lough Corrib to the shores of the Atlantic. In the 1230s, the Hiberno-Normans came and took Galway.

Geographic entities mentioned:
surface_form: Lough Corrib
instance_of: Lake
countries: Ireland
coordinates: lat: 53.466666666667
lon: -9.2833333333333
Little Cedar Lake (Wisconsin). Little Cedar Lake is a lake in Southeastern Wisconsin; United States. It is located at the geographic center of Washington County, in the Town of West Bend, and Town of Polk. The lake covers an area of, has a shoreline of, and reaches a maximum depth of.

Geographic entities mentioned:
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 47.3869
lon: -121.7
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 29.1925638
lon: -95.082994
surface_form: little cedar lake (wisconsin)
instance_of: Lake
countries: United States
coordinates: lat: 43.3764
lon: -88.2272
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3743
lon: -74.3212
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 46.221
lon: -93.404
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.97777778
lon: -94.46138889
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 45.5275
lon: -68.801111111111
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.960277777778
lon: -93.321111111111
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.78972222
lon: -94.73388889
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2144
lon: -92.571
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 40.9111048
lon: -74.4729616
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.59
lon: -93.523333333333
Little Cedar Lake (Wisconsin). Little Cedar Lake is a lake in Southeastern Wisconsin; United States. It is located at the geographic center of Washington County, in the Town of West Bend, and Town of Polk. The lake covers an area of, has a shoreline of, and reaches a maximum depth of.

Geographic entities mentioned:
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 47.3869
lon: -121.7
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 29.1925638
lon: -95.082994
surface_form: little cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3764
lon: -88.2272
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3743
lon: -74.3212
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 46.221
lon: -93.404
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.97777778
lon: -94.46138889
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 45.5275
lon: -68.801111111111
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.960277777778
lon: -93.321111111111
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.78972222
lon: -94.73388889
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2144
lon: -92.571
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 40.9111048
lon: -74.4729616
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.59
lon: -93.523333333333
Spring, summer and autumn activities on the lake include boating, fishing, and water skiing. In winter the lake freezes over completely with ice up to 36 inches thick, Winter activities on the lake include ice fishing and snowmobiling. Many species of fish are found in Little Cedar Lake, including northern pike, walleye, rock bass, smallmouth bass, bluegills, carp, and bullheads.

Geographic entities mentioned:
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 47.3869
lon: -121.7
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 29.1925638
lon: -95.082994
surface_form: little cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3764
lon: -88.2272
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3743
lon: -74.3212
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 46.221
lon: -93.404
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.97777778
lon: -94.46138889
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 45.5275
lon: -68.801111111111
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.960277777778
lon: -93.321111111111
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.78972222
lon: -94.73388889
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2144
lon: -92.571
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 40.9111048
lon: -74.4729616
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.59
lon: -93.523333333333
Little Cedar Lake (Wisconsin). Little Cedar Lake is a lake in Southeastern Wisconsin; United States. It is located at the geographic center of Washington County, in the Town of West Bend, and Town of Polk. The lake covers an area of, has a shoreline of, and reaches a maximum depth of.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
However, over the next few days, the success of the Japanese bombing attack on Clark Field rendered the base at Basco redundant, and work was discontinued. On 10 December, the Batan Island invasion force was redeployed from Batan Island and invaded Camiguin Island in the Babuyan Islands to the south.

Geographic entities mentioned:
surface_form: Camiguin Island
instance_of: Mountain
countries: Philippines
coordinates: lat: 18.833611111111
lon: 121.86111111111
Møsnuken. Møsnuken is a mountain in Bjørnafjorden Municipality in Vestland county, Norway. The mountain lies about east of the village of Søfteland.

Geographic entities mentioned:
surface_form: møsnuken
instance_of: Mountain
countries: Norway
coordinates: lat: 60.2331
lon: 5.51972
Exhausted, he retired in the spring of 1895 and died on July 26, 1897. Long before his death, Macleay's interest in the Oregonian Railway Company, which had built a narrow-gauge railway in the eastern Willamette Valley, led him to donate money for a schoolhouse at a railroad station in Marion County. The community, formerly named Stipp, was renamed Macleay in 1882.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Nevada. Nevada has only a single thirteener that meets the threshold for inclusion, Wheeler Peak in Great Basin National Park with an impressive of prominence. However, the highest point in the state is Boundary Peak, which is a sub-peak of California's Montgomery Peak with only of prominence. Washington.

Geographic entities mentioned:
surface_form: Montgomery Peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.838263888889
lon: -118.35678611111
However, the highest point in the state is Boundary Peak, which is a sub-peak of California's Montgomery Peak with only of prominence. Washington. Mount Rainier is the only mountain in Washington state that exceeds, and it has two summits that meet the prominence criteria, both of which are included on the list of fourteeners.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
Temagami Magnetic Anomaly. The Temagami Magnetic Anomaly, also called the Temagami Anomaly or the Wanapitei Anomaly, is a magnetic anomaly resulting from a large buried geologic structure in the Canadian Shield near Temagami, Ontario, Canada. It stretches from Lake Wanapitei in the west to Bear Island in Lake Temagami.

Geographic entities mentioned:
surface_form: Lake Temagami
instance_of: Lake
countries: Canada
coordinates: lat: 46.95
lon: -80.0833
Some researchers do however dissent from this view suggesting there was never such a collision. Erosion of the Timanide Orogen have produced sediments that are now found in the East European Platform, including the Cambrian Sablino Formation near Lake Ladoga.

Geographic entities mentioned:
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
Mount Danum. Mount Danum () is a mountain located at the Tawau Division of Sabah, Malaysia. With a height of, it is the highest peak in the Danum Valley Conservation Area.

Geographic entities mentioned:
surface_form: mount danum
instance_of: Mountain
countries: Malaysia
coordinates: lat: 4.95
lon: 117.683333
M'zab. The M'zab, or Mzab (Mozabite: &quot;Aghlan&quot;,), is a natural region of the northern Sahara Desert in Ghardaïa Province, Algeria. It is located south of Algiers and has approximately 360,000 inhabitants (2005 estimate). Geology. The M'zab is a limestone plateau, centred on the Wad M'zab (&quot;Oued Mzab&quot;) valley. History.

Geographic entities mentioned:
surface_form: mzab
instance_of: Valley
countries: Algeria
coordinates: lat: 32.487222222222
lon: 3.6813888888889
surface_form: m'zab
instance_of: Valley
countries: Algeria
coordinates: lat: 32.487222222222
lon: 3.6813888888889
surface_form: aghlan
instance_of: Valley
countries: Algeria
coordinates: lat: 32.487222222222
lon: 3.6813888888889
It is located south of Algiers and has approximately 360,000 inhabitants (2005 estimate). Geology. The M'zab is a limestone plateau, centred on the Wad M'zab (&quot;Oued Mzab&quot;) valley. History. The Mozabites (&quot;Ath Mzab&quot;) are a branch of a large Berber tribe, the Iznaten, which lived in large areas of middle southern Algeria.

Geographic entities mentioned:
surface_form: mzab
instance_of: Valley
countries: Algeria
coordinates: lat: 32.487222222222
lon: 3.6813888888889
surface_form: m'zab
instance_of: Valley
countries: Algeria
coordinates: lat: 32.487222222222
lon: 3.6813888888889
Geology. The M'zab is a limestone plateau, centred on the Wad M'zab (&quot;Oued Mzab&quot;) valley. History. The Mozabites (&quot;Ath Mzab&quot;) are a branch of a large Berber tribe, the Iznaten, which lived in large areas of middle southern Algeria. Many Tifinagh letters and symbols are engraved around the Mzab Valley.

Geographic entities mentioned:
surface_form: mzab
instance_of: Valley
countries: Algeria
coordinates: lat: 32.487222222222
lon: 3.6813888888889
History. The Mozabites (&quot;Ath Mzab&quot;) are a branch of a large Berber tribe, the Iznaten, which lived in large areas of middle southern Algeria. Many Tifinagh letters and symbols are engraved around the Mzab Valley. After the Muslim conquest of the Maghreb, the Mozabites became Muslims of the Mu'tazili school. The indigenous Christian population persisted until the 11th century.

Geographic entities mentioned:
surface_form: mzab valley
instance_of: Valley
countries: Algeria
coordinates: lat: 32.487222222222
lon: 3.6813888888889
The indigenous Christian population persisted until the 11th century. After the fall of the Rustamid state, the Rustamid royal family with some of their citizens chose the Mzab Valley as their refuge. However, the Rostemids were Ibadi and sent a preacher (Abu Bakr an-Nafusi) who successfully converted the indigenous Mozabites. France conquered Algeria in 1830.

Geographic entities mentioned:
surface_form: mzab valley
instance_of: Valley
countries: Algeria
coordinates: lat: 32.487222222222
lon: 3.6813888888889
Architecture. There are five &quot;qsur&quot; &quot;walled villages&quot; (&quot;ksour&quot;) located on rocky outcrops along the Wəd Mzab collectively known as &quot;the Pentapolis&quot;, founded between 1012 and 1350.

Geographic entities mentioned:
surface_form: mzab
instance_of: Valley
countries: Algeria
coordinates: lat: 32.487222222222
lon: 3.6813888888889
Society. The insular nature of the Ibāḍiyya has preserved the area, and Ibāḍī Sezzaba continue to dominate the social life of the area. A federal council, &quot;Majlis Ammi Said&quot;, unites representatives of the seven settlements as well as Ouargla, an ancient town located 200 km South-East of the Mzab valley.

Geographic entities mentioned:
surface_form: mzab valley
instance_of: Valley
countries: Algeria
coordinates: lat: 32.487222222222
lon: 3.6813888888889
M'zab. The M'zab, or Mzab (Mozabite: &quot;Aghlan&quot;,), is a natural region of the northern Sahara Desert in Ghardaïa Province, Algeria. It is located south of Algiers and has approximately 360,000 inhabitants (2005 estimate). Geology. The M'zab is a limestone plateau, centred on the Wad M'zab (&quot;Oued Mzab&quot;) valley. History.

Geographic entities mentioned:
surface_form: m'zab
instance_of: Valley
countries: Algeria
coordinates: lat: 32.487222222222
lon: 3.6813888888889
France conquered Algeria in 1830. The M'zab was annexed to France only in 1882 and reverted to Algerian indigenous rule in summer 1962 upon its national independence. Ghardaia (Taghardait) is the main town and capital of the M'zab, and El Atteuf (Tajnint) is the oldest settlement in the region. Beni Isguen (At Isgen) is the most sacred Berber Islamic town.

Geographic entities mentioned:
surface_form: m'zab
instance_of: Valley
countries: Algeria
coordinates: lat: 32.487222222222
lon: 3.6813888888889
Melika (At Mlichet) is populated by a kabily town named Mlikch which is until now located near Bouira, and it contains spacious cemeteries and a historical Mosque in the centre of the ksar, and Bounoura (At Bounour) is a historical ksar which contain Azwil palm grove, while El Guerrara (Igraren) and Berriane (Iberguen) have been part of the M'zab since the 17th century. Architecture.

Geographic entities mentioned:
surface_form: m'zab
instance_of: Valley
countries: Algeria
coordinates: lat: 32.487222222222
lon: 3.6813888888889
On the northwest is a large island (Carghill Island) or peninsula that fills much of the torso. The Hayes Rivers enters from the southwest and exits from the 'head' southeast below the town and airport of Oxford House, Manitoba. The Carrot River enters on the northwest and allows a portage to Cross Lake, Manitoba on the Nelson River. Downstream is Knee Lake.

Geographic entities mentioned:
surface_form: Knee Lake
instance_of: Lake
countries: Canada
coordinates: lat: 55.053888888889
lon: -94.738333333333
The lake is in size and sits at a surface elevation of. Description. Oxford Lake is a vaguely man-shaped lake, with a 'head' on the east, a 'neck', a northwest—southeast shoulder line and a 'torso' that tapers to a point in the west. The head is about 7 by 5 miles, the neck one mile across, and the shoulder line 11 miles. The south side of the torso is 25 miles and its northwest side 18 miles.

Geographic entities mentioned:
surface_form: the neck
instance_of: Mountain
countries: Canada
coordinates: lat: 57.67
lon: -130.58
Oxford Lake. Oxford Lake is a lake on the Hayes River in Manitoba, Canada. The lake is in size and sits at a surface elevation of. Description. Oxford Lake is a vaguely man-shaped lake, with a 'head' on the east, a 'neck', a northwest—southeast shoulder line and a 'torso' that tapers to a point in the west. The head is about 7 by 5 miles, the neck one mile across, and the shoulder line 11 miles.

Geographic entities mentioned:
surface_form: oxford lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.833333333333
lon: -95.583333333333
Oxford Lake. Oxford Lake is a lake on the Hayes River in Manitoba, Canada. The lake is in size and sits at a surface elevation of. Description. Oxford Lake is a vaguely man-shaped lake, with a 'head' on the east, a 'neck', a northwest—southeast shoulder line and a 'torso' that tapers to a point in the west. The head is about 7 by 5 miles, the neck one mile across, and the shoulder line 11 miles.

Geographic entities mentioned:
surface_form: oxford lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.833333333333
lon: -95.583333333333
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
The lake is in size and sits at a surface elevation of. Description. Oxford Lake is a vaguely man-shaped lake, with a 'head' on the east, a 'neck', a northwest—southeast shoulder line and a 'torso' that tapers to a point in the west. The head is about 7 by 5 miles, the neck one mile across, and the shoulder line 11 miles. The south side of the torso is 25 miles and its northwest side 18 miles.

Geographic entities mentioned:
surface_form: oxford lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.833333333333
lon: -95.583333333333
On the northwest is a large island (Carghill Island) or peninsula that fills much of the torso. The Hayes Rivers enters from the southwest and exits from the 'head' southeast below the town and airport of Oxford House, Manitoba. The Carrot River enters on the northwest and allows a portage to Cross Lake, Manitoba on the Nelson River. Downstream is Knee Lake.

Geographic entities mentioned:
surface_form: cross lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.7483
lon: -97.5019
surface_form: cross lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.39666666666667
lon: -77.94333333333333
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: cross lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.8714
lon: -79.9661
The head is about 7 by 5 miles, the neck one mile across, and the shoulder line 11 miles. The south side of the torso is 25 miles and its northwest side 18 miles. On the northwest is a large island (Carghill Island) or peninsula that fills much of the torso. The Hayes Rivers enters from the southwest and exits from the 'head' southeast below the town and airport of Oxford House, Manitoba.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
On the northwest is a large island (Carghill Island) or peninsula that fills much of the torso. The Hayes Rivers enters from the southwest and exits from the 'head' southeast below the town and airport of Oxford House, Manitoba. The Carrot River enters on the northwest and allows a portage to Cross Lake, Manitoba on the Nelson River. Downstream is Knee Lake.

Geographic entities mentioned:
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
Caridina glaubrechti. &quot;Caridina glaubrechti&quot; is species of lacustrine fresh water shrimp endemic to western part of Lake Towuti on the Indonesian island of Sulawesi. It is named in honor of German Zoologist Matthias Glaubrecht. Habitat and Ecology. &quot;C. glaubrechti&quot; is mainly found in shallow regions where it dwells on rocks and hard substrate.

Geographic entities mentioned:
surface_form: Lake Towuti
instance_of: Lake
countries: Indonesia
coordinates: lat: -2.76258
lon: 121.52232
East Rapti River. The East Rapti River flows from east to west through the Chitwan Valley in Nepal, forming the northern border of the Chitwan National Park. It joins the Narayani River inside the protected area.

Geographic entities mentioned:
surface_form: Chitwan Valley
instance_of: Valley
countries: Nepal
The city itself is carved into the side of Cerro Casigana, the mountain that dominates the north end of the city. From Ambato, it is possible to see many snow-capped volcanoes including Cotopaxi, Tungurahua, Carihuairazo, and the largest mountain in Ecuador, Chimborazo. Tungurahua lies about 40 kilometers to the southeast. The threat of eruption from the volcano is constant.

Geographic entities mentioned:
surface_form: Cotopaxi
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.68055555555556
lon: -78.437777777778
surface_form: Tungurahua
instance_of: Mountain
countries: Ecuador
coordinates: lat: -1.4669444444444
lon: -78.441666666667
surface_form: Carihuairazo
instance_of: Mountain
countries: Ecuador
coordinates: lat: -1.4069444444444
lon: -78.75
The city itself is carved into the side of Cerro Casigana, the mountain that dominates the north end of the city. From Ambato, it is possible to see many snow-capped volcanoes including Cotopaxi, Tungurahua, Carihuairazo, and the largest mountain in Ecuador, Chimborazo. Tungurahua lies about 40 kilometers to the southeast. The threat of eruption from the volcano is constant.

Geographic entities mentioned:
surface_form: Tungurahua
instance_of: Mountain
countries: Ecuador
coordinates: lat: -1.4669444444444
lon: -78.441666666667
In addition to walking paths, there are open fields, basketball and volley courts, as well as a large garden features an impressive amount of native species. On clear days, the park also affords the visitor excellent views of the city of Ambato and the constantly smoking Tungurahua volcano. Ficoa.

Geographic entities mentioned:
surface_form: Tungurahua
instance_of: Mountain
countries: Ecuador
coordinates: lat: -1.4669444444444
lon: -78.441666666667
Panamint City, California. Panamint City is a ghost town in the Panamint Range, near Death Valley, in Inyo County, California, US. It is also known by the official Board of Geographic Names as Panamint. Panamint was a boom town founded after silver and copper were found there in 1872. By 1874, the town had a population of about 2,000. Its main street was one mile (1.6 km) long.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Don Brownrigg. Don Brownrigg is a Canadian singer-songwriter from Codroy Valley, Newfoundland and Labrador. and has spent much of his career based in Halifax, Nova Scotia. He has released 3 full length albums, several singles, many collaborations, and has worked in theatre and puppetry. The Coast, Halifax's alt-weekly, said Brownrigg is &quot;instrumental to the Haligonian arts community&quot;.

Geographic entities mentioned:
surface_form: Codroy Valley
instance_of: Valley
countries: Canada
The Coast, Halifax's alt-weekly, said Brownrigg is &quot;instrumental to the Haligonian arts community&quot;. Early life. Brownrigg was raised in Upper Ferry in Codroy Valley. He is part of the MacArthur Family who settled in the area in the 19th century. His paternal great-grandfather is Henry J. Brownrigg. Career.

Geographic entities mentioned:
surface_form: Codroy Valley
instance_of: Valley
countries: Canada
Pulicat. Pulicat or Pazhaverkadu is a historic seashore town in Chennai Metropolitan Area at Thiruvallur District, of Tamil Nadu state, India. It is about north of Chennai and from Elavur, on the southern periphery of the Pulicat Lake. Pulicat lake is a shallow salt water lagoon which stretches about along the coast.

Geographic entities mentioned:
surface_form: Pulicat Lake
instance_of: Lake
countries: India
coordinates: lat: 13.565833333333
lon: 80.174722222222
McCollum Peak. McCollum Peak () is a peak, high, standing south of Beascochea Bay southeast of Mount Waugh, on the west coast of Graham Land, Antarctica. It was first charted by the Fourth French Antarctic Expedition under Jean-Baptiste Charcot, 1908–10, and was named by the UK Antarctic Place-Names Committee in 1959 for Elmer V.

Geographic entities mentioned:
surface_form: Mount Waugh
instance_of: Mountain
coordinates: lat: -65.52201
lon: -64.11144
surface_form: mccollum peak
instance_of: Mountain
coordinates: lat: -65.5333
lon: -64.0333
surface_form: waugh
instance_of: Mountain
coordinates: lat: -65.52201
lon: -64.11144
McCollum Peak. McCollum Peak () is a peak, high, standing south of Beascochea Bay southeast of Mount Waugh, on the west coast of Graham Land, Antarctica. It was first charted by the Fourth French Antarctic Expedition under Jean-Baptiste Charcot, 1908–10, and was named by the UK Antarctic Place-Names Committee in 1959 for Elmer V.

Geographic entities mentioned:
surface_form: mccollum peak
instance_of: Mountain
coordinates: lat: -65.5333
lon: -64.0333
The entire meltwater channel starts east of Nisku, wandering southeast through minor depressions and the chain of Saunders Lake, Ord Lake, three small unnamed lakes, Coal Lake and Driedmeat Lake. Coal Lake starts east of Kavanagh, Alberta, and ends at a dam built northwest of Gwynne, Alberta.

Geographic entities mentioned:
surface_form: driedmeat lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.8647
lon: -112.75
surface_form: coal lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.0747
lon: -113.271
Coal Lake (Alberta). Coal Lake is a long, sinuous lake located approximately southeast of the city of Edmonton, just northeast of the city of Wetaskiwin.

Geographic entities mentioned:
surface_form: coal lake (alberta)
instance_of: Lake
countries: Canada
coordinates: lat: 53.0747
lon: -113.271
Coal Lake (Alberta). Coal Lake is a long, sinuous lake located approximately southeast of the city of Edmonton, just northeast of the city of Wetaskiwin.

Geographic entities mentioned:
surface_form: coal lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.0747
lon: -113.271
The entire meltwater channel starts east of Nisku, wandering southeast through minor depressions and the chain of Saunders Lake, Ord Lake, three small unnamed lakes, Coal Lake and Driedmeat Lake. Coal Lake starts east of Kavanagh, Alberta, and ends at a dam built northwest of Gwynne, Alberta.

Geographic entities mentioned:
surface_form: coal lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.0747
lon: -113.271
Coal Lake starts east of Kavanagh, Alberta, and ends at a dam built northwest of Gwynne, Alberta. Since construction of the dam in 1972, Pipestone Creek flows through the southern end of Coal Lake, draining the lake into the Battle River, southeast of Coal Lake. Coal Lake was named in 1892 by J.D.A.

Geographic entities mentioned:
surface_form: coal lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.0747
lon: -113.271
surface_form: coal lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.0747
lon: -113.271
Since construction of the dam in 1972, Pipestone Creek flows through the southern end of Coal Lake, draining the lake into the Battle River, southeast of Coal Lake. Coal Lake was named in 1892 by J.D.A. Fitzpatrick, a Dominion Land Surveyor, for the coal beds present in many places along the northeast shore.

Geographic entities mentioned:
surface_form: coal lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.0747
lon: -113.271
Geography. The Monti Lattari are the western extension of the Monti Picentini in the Campanian Apennines, stretching into the Tyrrhenian Sea to form the Sorrentine peninsula. The name derives from the flocks of goats grazing in the area, which provide a good quality of milk (&quot;lactis&quot; in Latin).

Geographic entities mentioned:
surface_form: Monti Picentini
instance_of: Mountain
countries: Italy
coordinates: lat: 40.75
lon: 15
The range is bounded from north-west by the Gulf of Naples, from north by the Sarno river plain, from east by the Metelliana plain of Cava de' Tirreni, and from south by the Gulf of Salerno. The rocks are of limestone formation, reaching their highest altitude at 1,444 m with the Monte San Michele. To the north is the popular Monte Faito, reachable by cable car from Castellammare di Stabia.

Geographic entities mentioned:
surface_form: Monte Faito
instance_of: Mountain
countries: Italy
coordinates: lat: 40.646111111111
lon: 14.513611111111
The total number built is given variously from 'At least 200' to 'Some 600', with '660' given in Vanessa Bird's 'Classic Classes'. As standard, the class carries of sail, however a variant known as the Hocco is a class with the same hull but of sail, conceived for sailing on inland waters, specifically Lake Geneva.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Some people call this section the 'Jail Trail' because it also passes the Allegheny County Jail on its way to Oakland, the university center of the city. A branch that extends into Schenley Park in Oakland is called the 'Junction Hollow Trail'.

Geographic entities mentioned:
surface_form: Junction Hollow
instance_of: Valley
countries: United States
coordinates: lat: 40.4429
lon: -79.9475
The frontier between Argentina and Chile passes over the mountain. The Argentine portion is in the Los Andes Department of Salta Province and the Chilean in Chile's Antofagasta Region. About northeast of Llullaillaco, the Salta–Antofagasta railway crosses the Andes at Socompa. Humans first moved into the area about 8,000 BCE. The region was inhabited by hunters and shepherds in pre-Hispanic times.

Geographic entities mentioned:
surface_form: Socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
The volcano is an imposing mountain, rising by and above the Salar de Punta Negra and the Salar de Llullaillaco, and away, respectively. With a summit height of, (or) it is one of the highest mountains in the Andes (third highest in Chile and seventh highest in the Andes, according to John Biggar) and the second- or third-highest volcano in the world (Ojos del Salado is the highest).

Geographic entities mentioned:
surface_form: Ojos del Salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
In the early 20th century, Llullaillaco was thought to be the highest volcano in the world. The elevation is to a large degree consequence of the underlying terrain, which rises about above sea level. The height of the mountain and the clear air in the region make Llullaillaco visible from Cerro Paranal, away as measured through Google Earth.

Geographic entities mentioned:
surface_form: Cerro Paranal
instance_of: Mountain
countries: Chile
coordinates: lat: -24.627222222222
lon: -70.404722222222
The height of the mountain and the clear air in the region make Llullaillaco visible from Cerro Paranal, away as measured through Google Earth. The view from the mountain extends from Licancabur north over the Nevados de Cachi mountains east to Ojos del Salado south; mountains in between are visible as well. Llullaillaco is a composite volcano formed mostly by lava flows.

Geographic entities mentioned:
surface_form: Nevados de Cachi
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.933333333333
lon: -66.383333333333
The landslide deposit covers a surface of about. Its volume has been estimated at and the speed at. This speed range is comparable to that of the Colima, Lastarria, and Mount St. Helens debris avalanches. The landslide occurred no earlier than 156,000 to 148,000 ±5,000 years ago; it might coincide with the 48,000-year-old lava flow.

Geographic entities mentioned:
surface_form: Lastarria
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -25.166666666667
lon: -68.5
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
It is not usually known what triggers the collapse, although eruption-associated earthquakes are suspected to play a role. Other volcanoes in the region with sector collapses are: Lastarria, Ollague, San Pedro, Socompa, and Tata Sabaya. The Mellado and Cerro Rosado volcanoes close to Llullaillaco also display evidence of sector collapses. Regional setting.

Geographic entities mentioned:
surface_form: Tata Sabaya
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.133333333333
lon: -68.5
In addition, there are large calderas and monogenetic volcanoes. Llullaillaco is one of more than 1,000 volcanoes in the CVZ. At least 44 volcanic centres with historical activity and 18 large caldera-forming volcanoes have been identified in the Central Volcanic Zone; the most active is Lascar, and Guallatiri and San Pedro have had historical eruptions as well.

Geographic entities mentioned:
surface_form: Guallatiri
instance_of: Mountain
countries: Chile
coordinates: lat: -18.42361111111111
lon: -69.08972222222222
At least 44 volcanic centres with historical activity and 18 large caldera-forming volcanoes have been identified in the Central Volcanic Zone; the most active is Lascar, and Guallatiri and San Pedro have had historical eruptions as well. Volcanism in the Central Volcanic Zone takes place mostly on the Altiplano and the Cordillera Occidental, where high stratovolcanoes with heights of over occur.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
They extend diagonally across the volcanic arc and are accompanied by volcanic manifestations at substantial distances from the arc. The Archibarca lineament runs from the Escondida copper deposit, over Llullaillaco (where it crosses the volcanic arc), Corrida de Cori, Archibarca, Antofalla to the Galán caldera; it influenced the development of Llullaillaco.

Geographic entities mentioned:
surface_form: Corrida de Cori
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.9142
lon: -68.45
surface_form: Archibarca
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.2373
lon: -67.8653
surface_form: Antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
surface_form: Galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
surface_form: llullaillaco
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.719863
lon: -68.536852
surface_form: llullaillaco
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.719863
lon: -68.536852
The climate has not always been uniformly dry. Between 14,000 and 9,500 years ago during the late glacial, a wet period gave rise to lakes in the Altiplano (Lake Tauca pluvial). Water discharge from Llullaillaco and neighbouring mountains into Salar de Punta Negra increased, leading to the formation of standing water bodies. As glaciers retreated between 15,000 and 10,000 years ago, lakes shrank.

Geographic entities mentioned:
surface_form: Lake Tauca
instance_of: Lake
countries: Peru
coordinates: lat: -20
lon: -68
There are myths associated with Llullaillaco, and the mountain is still important to the inhabitants of Socaire east of the Salar de Atacama, from where it is visible. Some ascents are done for ritual reasons. Children of Llullaillaco.

Geographic entities mentioned:
surface_form: Salar de Atacama
instance_of: Lake
Body of water
countries: Chile
coordinates: lat: -23.416666666666668
lon: -68.26666666666667
Llullaillaco. Llullaillaco (,) is a dormant stratovolcano on the border between Argentina (Salta Province) and Chile (Antofagasta Region). It is part of the Llullaillaco National Park and lies in the Puna de Atacama, a region of tall volcanic peaks on a high plateau close to the Atacama Desert, one of the driest places in the world.

Geographic entities mentioned:
surface_form: llullaillaco
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.719863
lon: -68.536852
Between and elevation there is a sparse plant cover, while at lower altitudes the climate is too dry for plants to grow. A species of mouse on Llullaillaco is the vertebrate species living at the highest-known altitude. The volcano formed during the Pleistocene in two stages, named Llullaillaco I and Llullaillaco II. The oldest rocks are about 1.5 million years old.

Geographic entities mentioned:
surface_form: llullaillaco
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.719863
lon: -68.536852
Between and elevation there is a sparse plant cover, while at lower altitudes the climate is too dry for plants to grow. A species of mouse on Llullaillaco is the vertebrate species living at the highest-known altitude. The volcano formed during the Pleistocene in two stages, named Llullaillaco I and Llullaillaco II. The oldest rocks are about 1.5 million years old.

Geographic entities mentioned:
surface_form: llullaillaco
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.719863
lon: -68.536852
surface_form: llullaillaco
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.719863
lon: -68.536852
During the last stage, three conspicuous lava flows were emplaced on the summit. The youngest-dated rocks are 930 ±140 years old, but there are reports of activity from the 19th century. There are archaeological sites on the mountain and at its foot; Llullaillaco marks the highest archaeological site in the world. The first recorded ascent was in 1950.

Geographic entities mentioned:
surface_form: llullaillaco
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.719863
lon: -68.536852