Sarmila/GeoWiki-Features huggingface dataset:
It is a tributary of the larger Red Deer River. History. The name Little Red Deer River appears in use since the Palliser Expedition from 1857 to 1860. In 1904, after the discovery of coal, the town Skunk Hollow sprung into being along the banks of the Little Red Deer about west of Water Valley. At its peak the town had close to 100 inhabitants, a post office, wash house, dance hall, and a school.

Geographic entities mentioned:
surface_form: little red deer river
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.06681
lon: -114.15201
The river has seen multiple floods of varying severity including in 1929, 1952, 2005, 2013, 2014, 2018, 2020, and 2022. Course. The Little Red Deer River starts as a very small stream flowing from Waiparous Creek. From here it flows in a northeastern direction, eventually growing in size to be in width along the Harold Creek Road.

Geographic entities mentioned:
surface_form: little red deer river
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.06681
lon: -114.15201
The river heads east for and then flows north past the unincorporated community of Oklahoma before continuing northeast, flowing into the Red Deer River. The river flows through the municipal districts of Mountain View County, Red Deer County, Rocky View County, and the MD of Bighorn No. 8. Fish species.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
8. Fish species. Native sport fish in the Little Red Deer are Mountain whitefish (by far the most abundant), Burbot, Northern pike, Walleye, and Bull trout. The Little Red Deer has seen many introductions in its history, the most successful being the Brown trout and Brook trout.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Rolland criticized the control Münzenberg assumed over the committee and was against it being based in Berlin. Rolland moved to Villeneuve, on the shores of Lake Geneva to devote himself to writing. His life was interrupted by health problems, and by travels to art exhibitions.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Pomroy Lake. Pomroy Lake is a lake in Kanabec County, in the U.S. state of Minnesota. Pomroy Lake was named for John Pomroy, a lumberman.

Geographic entities mentioned:
surface_form: pomroy lake
instance_of: Lake
countries: United States
coordinates: lat: 46.01138889
lon: -93.18638889
prominens&quot;. Distribution and habitat. This eucalypt grows in sand over limestone, often on low rises and occurs on the Giralia Range between the Exmouth Gulf and Lake MacLeod in the Carnarvon biogeographic region. Conservation. &quot;Eucalyptus baiophylla&quot; is classified as &quot;not threatened&quot; by the Western Australian Government Department of Parks and Wildlife.

Geographic entities mentioned:
surface_form: Lake MacLeod
instance_of: Lake
countries: Australia
coordinates: lat: -24.166666666667
lon: 113.66666666667
They are divided into the 36 Heavenly Spirits and 72 Earthly Fiends. Li Jun's story. The following persons are &quot;jianghu&quot; figures living around the Lake Tai area. They become sworn brothers with Li Jun and eventually follow him to Siam, where he becomes king. &quot;11 Star Generals&quot;.

Geographic entities mentioned:
surface_form: Lake Tai
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 31.166666666667
lon: 120.15
Battle of Lake Benacus. The Battle of Lake Benacus was fought along the banks of Lake Garda in northern Italy, which was known to the Romans as Benacus, in 268 or early 269, between the army under the command of the Roman Emperor Claudius II and the Germanic tribes of the Alamanni and Juthungi. Background.

Geographic entities mentioned:
surface_form: Lake Garda
instance_of: Lake
countries: Italy
coordinates: lat: 45.633333333333
lon: 10.666666666667
His original plan was to attack the Union right flank, north of the Chickahominy River, before McDowell's corps, marching south from Fredericksburg, could arrive. However, on May 27, the same day the Battle of Hanover Court House was fought northeast of Richmond, Johnston learned that McDowell's corps had been diverted to the Shenandoah Valley and would not be reinforcing the Army of the Potomac.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Ranked among the Berbers of Zenata, of the Beni Merine branch, they would be according to another version provided by the historiographer Adelouahab Benmansour, from the Sanhajian clan of Lemtouna, a descendant of the great chief Almoravid Yusuf ibn Tashfin. At the advent of the Almohades, one of their ancestors would have joined the Merinids in the Zab (southern Algeria and Tunisia).

Geographic entities mentioned:
surface_form: Zab
instance_of: Valley
countries: Algeria
coordinates: lat: 32.487222222222
lon: 3.6813888888889
Wila Qullu (Bolivia-Chile). Wila Qullu (Aymara &quot;wila&quot; red or blood, &quot;qullu&quot; mountain, &quot;red mountain&quot;, Hispanicized spelling &quot;Wila Kkollu&quot;), also Cerro Laguna (Spanish &quot;cerro&quot; hill, &quot;laguna&quot; lake, lagoon), is a mountain in the Andes located on the border of Bolivia and Chile in the Cordillera Occidental.

Geographic entities mentioned:
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.3833
lon: -68.9667
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.51361111
lon: -66.96194444
surface_form: wila qullu (bolivia-chile)
instance_of: Mountain
countries: Bolivia
coordinates: lat: -20.3333
lon: -68.65
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.37833333
lon: -66.68833333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.0833
lon: -66.3333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.9719
lon: -66.3703
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.12694444
lon: -68.27916667
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.7833
lon: -68.8333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -20.97472222
lon: -66.38083333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.67472222
lon: -68.625
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.2953
lon: -69.3989
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.065
lon: -66.3222
Wila Qullu (Bolivia-Chile). Wila Qullu (Aymara &quot;wila&quot; red or blood, &quot;qullu&quot; mountain, &quot;red mountain&quot;, Hispanicized spelling &quot;Wila Kkollu&quot;), also Cerro Laguna (Spanish &quot;cerro&quot; hill, &quot;laguna&quot; lake, lagoon), is a mountain in the Andes located on the border of Bolivia and Chile in the Cordillera Occidental.

Geographic entities mentioned:
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.3833
lon: -68.9667
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.3833
lon: -68.9667
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.51361111
lon: -66.96194444
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.51361111
lon: -66.96194444
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -20.3333
lon: -68.65
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -20.3333
lon: -68.65
surface_form: cerro laguna
instance_of: Mountain
countries: Bolivia
coordinates: lat: -20.3333
lon: -68.65
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.37833333
lon: -66.68833333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.37833333
lon: -66.68833333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.0833
lon: -66.3333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.0833
lon: -66.3333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.9719
lon: -66.3703
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.9719
lon: -66.3703
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.12694444
lon: -68.27916667
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.12694444
lon: -68.27916667
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.7833
lon: -68.8333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.7833
lon: -68.8333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -20.97472222
lon: -66.38083333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -20.97472222
lon: -66.38083333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.67472222
lon: -68.625
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.67472222
lon: -68.625
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.2953
lon: -69.3989
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.2953
lon: -69.3989
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.065
lon: -66.3222
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.065
lon: -66.3222
Cat Tail Brook. Cat Tail Brook is a tributary of Rock Brook in central New Jersey in the United States. Course. Cat Tail Brook originates in Sourland Mountain at. It flows southeast until it meets Rock Brook at the edge of Sourland Mountain at.

Geographic entities mentioned:
surface_form: Sourland Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.4792
lon: -74.711
surface_form: cat tail brook
instance_of: Landform
countries: United States
coordinates: lat: 40.43194444
lon: -74.72888889
Cat Tail Brook. Cat Tail Brook is a tributary of Rock Brook in central New Jersey in the United States. Course. Cat Tail Brook originates in Sourland Mountain at. It flows southeast until it meets Rock Brook at the edge of Sourland Mountain at.

Geographic entities mentioned:
surface_form: sourland mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.4792
lon: -74.711
Cat Tail Brook. Cat Tail Brook is a tributary of Rock Brook in central New Jersey in the United States. Course. Cat Tail Brook originates in Sourland Mountain at. It flows southeast until it meets Rock Brook at the edge of Sourland Mountain at.

Geographic entities mentioned:
surface_form: cat tail brook
instance_of: Landform
countries: United States
coordinates: lat: 40.43194444
lon: -74.72888889
OR 238 begins, at its western terminus, at an interchange with U.S. Route 199 and Oregon Route 99 in Grants Pass. The highway heads south from there, eventually turning to the southeast, skirting the southern edge of the Rogue Valley, and the foothills of the Siskiyou Mountains. It continues in a general southeasterly direction for quite a while, and then turns northeast towards Jacksonville.

Geographic entities mentioned:
surface_form: Rogue Valley
instance_of: Valley
countries: United States
coordinates: lat: 42.440122222222
lon: -122.92615277778
Although the crater's age was previously estimated to be 52,000 ± 6,000 years, newer studies suggest an age of 576,000 ± 47,000 years. Lonar Crater sits inside the Deccan Plateaua massive plain of volcanic basalt rock created by eruptions some 65 million years ago. Its location in this basalt field suggested to some geologists that it was a volcanic crater.

Geographic entities mentioned:
surface_form: deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
surface_form: lonar
instance_of: Lake
countries: India
coordinates: lat: 19.975
lon: 76.5075
Geological origin. Lonar Lake lies within the only known extraterrestrial impact crater found within the great Deccan Traps, a huge basaltic formation in India. The lake was initially believed to be of volcanic origin, but now it is recognized as an impact crater. Lonar Lake was created by the impact of either a comet or of an asteroid.

Geographic entities mentioned:
surface_form: deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Lonar Lake. Lonar Lake, also known as Lonar crater, is a saline, soda lake, located at Lonar, 79 km from Buldhana city in Buldhana district, Maharashtra, India. It is a notified National Geo-heritage Monument. Lonar Lake is in an impact crater created by a meteorite impact during the Pleistocene Epoch. It is one of only four known hyper-velocity impact craters in basaltic rock anywhere on Earth.

Geographic entities mentioned:
surface_form: lonar
instance_of: Lake
countries: India
coordinates: lat: 19.975
lon: 76.5075
surface_form: lonar lake
instance_of: Lake
countries: India
coordinates: lat: 19.975
lon: 76.5075
surface_form: lonar
instance_of: Lake
countries: India
coordinates: lat: 19.975
lon: 76.5075
Lonar Crater sits inside the Deccan Plateaua massive plain of volcanic basalt rock created by eruptions some 65 million years ago. Its location in this basalt field suggested to some geologists that it was a volcanic crater. Today, however, Lonar Crater is understood to be the result of a meteorite impact. The water in the lake is both saline and alkaline.

Geographic entities mentioned:
surface_form: lonar
instance_of: Lake
countries: India
coordinates: lat: 19.975
lon: 76.5075
Lonar Lake. Lonar Lake, also known as Lonar crater, is a saline, soda lake, located at Lonar, 79 km from Buldhana city in Buldhana district, Maharashtra, India. It is a notified National Geo-heritage Monument. Lonar Lake is in an impact crater created by a meteorite impact during the Pleistocene Epoch. It is one of only four known hyper-velocity impact craters in basaltic rock anywhere on Earth.

Geographic entities mentioned:
surface_form: lonar lake
instance_of: Lake
countries: India
coordinates: lat: 19.975
lon: 76.5075
Lonar Lake is in an impact crater created by a meteorite impact during the Pleistocene Epoch. It is one of only four known hyper-velocity impact craters in basaltic rock anywhere on Earth. The other three basaltic impact structures are in southern Brazil. Lonar Lake has a mean diameter of and is about below the crater rim. The meteor crater rim is about in diameter.

Geographic entities mentioned:
surface_form: lonar lake
instance_of: Lake
countries: India
coordinates: lat: 19.975
lon: 76.5075
It is believed that only shock metamorphism caused by a hypervelocity impact can transform plagioclase into maskelynite, or create planar deformation features. The presence of impact deformation of basalt layers comprising the rim, of shocked breccia inside the crater, of shatter cones, and of the non-volcanic ejecta blanket surrounding the crater all support the impact origin of Lonar Lake.

Geographic entities mentioned:
surface_form: lonar lake
instance_of: Lake
countries: India
coordinates: lat: 19.975
lon: 76.5075
The saline deposits obtained from the lake are rather of an exceptional nature. Compared with the most famous salt lake in India, the Sambhar Lake in Rajasthan (India), it will be seen that whereas at Lonar the carbonates of soda are the most important, in the case of the Sambhar Lake the deposits of sodium chloride or common salt give the lake its value.

Geographic entities mentioned:
surface_form: lonar
instance_of: Lake
countries: India
coordinates: lat: 19.975
lon: 76.5075
The modes of formation are also entirely different and it is practically certain that the Lonar salts are derived from an unknown source in the bed of the lake. It is true that water is continually flowing into the lake and that except by evaporation there is no loss.

Geographic entities mentioned:
surface_form: lonar
instance_of: Lake
countries: India
coordinates: lat: 19.975
lon: 76.5075
Their further purification is not considered difficult. Commercial exploitation of the salts from the lake is recorded from 1842, including the period of Government of Nizam, and until 1903. Presently, there is only a very small local demand for these Lonar Lake products. Gaylussite mineral. Gaylussite is the mineral has been recently reported from drill core in Lonar lake.

Geographic entities mentioned:
surface_form: lonar lake
instance_of: Lake
countries: India
coordinates: lat: 19.975
lon: 76.5075
Microbial diversity. While the Lonar Lake appears green for most of the year due to the presence of dense blooms of cyanobacteria such as &quot;Arthrospira&quot; spp., bacteria and archaea belonging to diverse functional groups such as methanogens, methanotrophs, phototrophs, denitrifiers, sulfur oxidizers, sulfate reducers, heterotrophs and syntrophs have been reported.

Geographic entities mentioned:
surface_form: lonar lake
instance_of: Lake
countries: India
coordinates: lat: 19.975
lon: 76.5075
This haloalkaliphilic bacterium synthesizes and intracellularly accumulates organic solutes such as ectoine that are of biotechnological interest. Methylotrophic methanogenesis has been reported in Lonar Lake sediments and the primary microorganism (archaeon) that is responsible was identified as being closely related to &quot;Methanolobus oregonensis&quot;. Endolithic microorganisms.

Geographic entities mentioned:
surface_form: lonar
instance_of: Lake
countries: India
coordinates: lat: 19.975
lon: 76.5075
The lake was declared a protected Ramsar site in November 2020. Geographical features. A series of small hills surround the basin, which has an oval shape, almost round, with a circumference at top of about 8 km (five miles). The sides of the basin rise abruptly at an angle of about 75°. At the base of the sides, the lake has a circumference of about 4.8 km (three miles).

Geographic entities mentioned:
surface_form: hills
instance_of: Mountain
countries: India
coordinates: lat: 23.166666666667
lon: 92.833333333333
Mardalsfossen. Mardalsfossen is a waterfall in Molde Municipality in Møre og Romsdal county, Norway. It is sometimes referred to as one of the tallest waterfalls in Europe. The falls are on the Mardøla river which flows out of a hanging valley into the lake Eikesdalsvatnet, about northwest of the village of Eikesdalen. The waterfall was depicted in the coat of arms of the old Nesset Municipality.

Geographic entities mentioned:
surface_form: Eikesdalsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 62.543055555556
lon: 8.1702777777778
surface_form: Eikesdalen
instance_of: Valley
countries: Norway
coordinates: lat: 62.47611111
lon: 8.17416667
It reportedly supported one of the largest wading bird rookeries in South Florida. The first documented inhabitant of Munyon Island in 1884, was a man named Rodgers who was known to be an eccentric &quot;Robinson Crusoe&quot; type who lived in a tent and made his living by selling green sea turtles which he caught in Lake Worth.

Geographic entities mentioned:
surface_form: Lake Worth
instance_of: Lake
countries: United States
coordinates: lat: 26.6814
lon: -80.0458
Lerma chub. The Lerma chub (&quot;Algansea barbata&quot;) is a species of freshwater fish in the family Leuciscidae, the shiners, daces and minnows. It is endemic to the uppermost Lerma River basin in the State of Mexico and Toluca Valley of central Mexico. This threatened species is up to about long.

Geographic entities mentioned:
surface_form: Toluca Valley
instance_of: Valley
countries: Mexico
coordinates: lat: 19.2865
lon: -99.5595
Other significant streams include Kellogg Creek and Rose Creek. The Allatoona Dam holding back the lake was completed in 1949 on the Etowah River, which in turn merges with the Oostanaula River at Rome, Georgia to form the Coosa River of Georgia and Alabama. Its basin upstream (mostly northeast) of Lake Allatoona covers about.

Geographic entities mentioned:
surface_form: Coosa River
instance_of: Watercourse
countries: United States
coordinates: lat: 32.4862464
lon: -86.2777475
Creation of the park. The area that is now the city of Cleveland Heights lies atop the Portage Escarpment, a major landform in North America which marks the boundary between the Till Plains and the Appalachian Plateau. The escarpment is cut by several large and small streams, including Dugway Brook, which have left numerous ravines and gorges.

Geographic entities mentioned:
surface_form: Appalachian Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 40
lon: -78
According to the U.S. Census Bureau, Fraser has a total area of, of which are land and, or 0.38%, are water. Harrington Drain and its tributary, Sweeny Drain, flow northward through the city, Harrington Drain joining the Clinton River, a tributary of Lake St. Clair, in Mount Clemens. Climate.

Geographic entities mentioned:
surface_form: Lake St. Clair
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.450265
lon: -82.67572
Historical Background. The O'odham (Pima) and Pipaash (Maricopa) peoples lived in villages along the Gila River when settlers began to arrive. Due to the settlers removing so much water from the upstream of the River, many O'odham migrated to the Salt River Valley where there was relatively more water.

Geographic entities mentioned:
surface_form: Salt River Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.38111111111111
lon: -112.31305555555555
Micropterix hyrcana. &quot;Micropterix hyrcana&quot; is a species of moth belonging to the family Micropterigidae. It was described by Zagulajev in 1993. It is only known from Hyrcanian woods along the southern coast of the Caspian Sea from Azerbaijan to the Iranian province Golestan. The habitat consists of edges of deciduous forests. Adults have been caught in June.

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
Centerville Township, Michigan. Centerville Township is a civil township of Leelanau County in the U.S. state of Michigan. The population was 1,243 at the 2020 census. The township is bounded to the east by Lake Leelanau. History. Centerville Township was organized in 1862 as one of Leelanau County's first five townships. Geography.

Geographic entities mentioned:
surface_form: Lake Leelanau
instance_of: Lake
countries: United States
coordinates: lat: 44.85
lon: -85.73187
Geography. According to the United States Census Bureau, the township has a total area of, of which is land and (8.87%) is water. Centerville Township contains shorelines on both Lake Michigan and Lake Leelanau. Demographics. As of the census of 2000, there were 1,095 people, 435 households, and 325 families residing in the township. The population density was.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: Lake Leelanau
instance_of: Lake
countries: United States
coordinates: lat: 44.85
lon: -85.73187
Fort Lesley J. McNair. Fort Lesley J. McNair, also historically known as the Washington Arsenal, is a United States Army post located on the tip of Buzzard Point, the peninsula that lies at the confluence of the Potomac River and the Anacostia River in Washington, D.C. To the peninsula's west is the Washington Channel, while the Anacostia River is on its south side.

Geographic entities mentioned:
surface_form: Washington Channel
instance_of: Watercourse
countries: United States
coordinates: lat: 38.8787232
lon: -77.0271988
Fort McNair has been the headquarters of the Military District of Washington since 1966. Proposed buffer zone. In 2020, the Department of Defense and Army Corps of Engineers proposed a permanent restricted area of about 250 feet to 500 feet into the Washington Channel along the fort's western bank outlined by buoys and warning signs. This proposal was met with resistance from D.C.

Geographic entities mentioned:
surface_form: Washington Channel
instance_of: Watercourse
countries: United States
coordinates: lat: 38.8787232
lon: -77.0271988
Distribution and habitat. The Gabon bushbaby is native to tropical western Central Africa. Its range extends from the Sanaga River in Cameroon, through the Congo Republic and Río Muni, in Equatorial Guinea to Gabon, where it is found between the Sanaga River and the Ogooué River. It is unclear whether it occurs to the south of the Ogooue River.

Geographic entities mentioned:
surface_form: Sanaga River
instance_of: Watercourse
countries: Cameroon
coordinates: lat: 3.5593388888889
lon: 9.652175
It is similar in appearance to &quot;Eucalyptus moderata&quot;. Distribution. This mallee grows in laterite, limestone or sand on dunes, flats and sandplains and has a range from just north of Geraldton to Dowerin and Wongan Hills in the Avon Wheatbelt, Geraldton Sandplains, Mallee and Yalgoo biogeographic regions. Conservation status.

Geographic entities mentioned:
surface_form: Wongan Hills
instance_of: Mountain
countries: Australia
coordinates: lat: -30.8
lon: 116.617
The population density is. The municipality is unilingually Finnish. The neighboring municipalities of Lapinlahti are Iisalmi, Kuopio, Rautavaara, Siilinjärvi and Sonkajärvi. The neighboring municipality of Varpaisjärvi was consolidated with Lapinlahti on 1 January 2011. There are a total of 229 lakes in the municipality of Lapinlahti, the largest of which include Lake Onkivesi.

Geographic entities mentioned:
surface_form: Lake Onkivesi
instance_of: Lake
countries: Finland
coordinates: lat: 63.3
lon: 27.33333333
Wemyss Bay. Wemyss Bay () is a village on the coast of the Firth of Clyde in Inverclyde in the west central Lowlands of Scotland. It is in the traditional county of Renfrewshire. It is adjacent to Skelmorlie, North Ayrshire. The town and villages have always been in separate counties, divided by the Kelly Burn. Wemyss Bay is the port for ferries on the Sea Road to Rothesay on the Isle of Bute.

Geographic entities mentioned:
surface_form: central Lowlands
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.408
lon: -4.044
Hoher Stoppelkopf. The Hohe Stoppelkopf, locally just called the Stoppelkopf, is a 566.2-metre-high hill in the Palatine Forest in the German state of Rhineland-Palatinate. It lies 3 km north of the small town of Lambrecht.

Geographic entities mentioned:
surface_form: hoher stoppelkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 49.3972
lon: 8.0737
It lies 3 km north of the small town of Lambrecht. Together with the Drachenfels (577 m) to the northwest and the Stabenberg (496 m) to the east, the Stoppelkopf lies on the watershed between the catchment areas of two Palatine Rhine tributaries, the Speyerbach (south) and the Isenach (north).

Geographic entities mentioned:
surface_form: drachenfels
instance_of: Mountain
countries: Germany
coordinates: lat: 50.665277777778
lon: 7.2097222222222
surface_form: drachenfels
instance_of: Mountain
countries: Germany
coordinates: lat: 49.425
lon: 8.05306
Khirbet Mazin. Khirbet Mazin (), Hebrew name: Metzad Kidron () is an archaeological site on the northwestern shore of the Dead Sea. It is situated on the inlet of Wadi Mazin north of Kidron stream by the northwest shore of the Dead Sea. Mazin is located in the southern part of Ein Feshkha nature reserve. Name.

Geographic entities mentioned:
surface_form: Kidron stream
instance_of: Valley
countries: State of Palestine
coordinates: lat: 31.776972222222224
lon: 35.23897222222222
The provisions will allow developers to bypass the protections in the &quot;Clean Water Act&quot;, and other acts which protect the Great Lakes, Lake Simcoe, the Ontario Greenbelt, and the Oak Ridges Moraine. It also bypasses the requirements in the &quot;Places to Grow Act&quot; which prohibits green-field development except in specific areas designated for future growth.

Geographic entities mentioned:
surface_form: Lake Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
surface_form: Oak Ridges Moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
Lough Key Forest Park. Lough Key Forest Park is an 800-hectare park on the southern shore of Lough Key, 40 km south east of Sligo town and 3 km east of Boyle, County Roscommon, Ireland. Formerly part of the Rockingham Estate laid out by the King family, it is open to the public. History. Rockingham House had burned down in a fire started by an electrical fault in 1957.

Geographic entities mentioned:
surface_form: Lough Key
instance_of: Lake
countries: Ireland
coordinates: lat: 54
lon: -8.25
Caspian Sea&quot; by Vladimir Ovchinnikov, &quot;Haymaking time&quot;, &quot;Blue Winter&quot;, &quot;Pskov Site&quot; by Sergei Osipov, &quot;Native open spaces&quot;, &quot;Lilac Silvery. On footbridge&quot; by Lia Ostrova, &quot;Hermitage.

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
Paterson River. Paterson River, a perennial river that is part of the Hunter River catchment, is located in the Hunter and Mid North Coast regions of New South Wales, Australia. Course and features.

Geographic entities mentioned:
surface_form: Hunter
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Course and features. Paterson River rises in the Barrington Tops National Park, west by north of Careys Peak, and flows generally south and southeast, joined by six minor tributaries including the Allyn River at Vacy, before reaching its confluence with the Hunter River between Hinton and Morpeth.

Geographic entities mentioned:
surface_form: Careys Peak
instance_of: Mountain
countries: Australia
coordinates: lat: -32.0507
lon: 151.459
After the law of Béla IV, a massive construction began. Béla IV began the construction of the new Royal headquarters, Buda. Although the Royal Centre had already been transferred to Óbuda, the site was considered to be warlike and construction began on the South Side of the Castle Hill. At that time, the construction of Buda was still at a modest level, the main aspect was of protection.

Geographic entities mentioned:
surface_form: Castle Hill
instance_of: Plateau
countries: Hungary
coordinates: lat: 47.5028
lon: 19.0317
Mount Futamata. is located in the Hidaka Mountains, Hokkaidō, Japan.

Geographic entities mentioned:
surface_form: mount futamata
instance_of: Mountain
countries: Japan
coordinates: lat: 42.687777777778
lon: 142.71777777778
Loch Ossian. Loch Ossian (Scottish Gaelic: &quot;Loch Oisein&quot;) is a narrow loch that is about long on the north eastern edge of Rannoch Moor, on The Corrour Estate, with its western corner east of Corrour railway station. It is drained by the River Ossian, flowing north into Loch Guilbinn and ultimately to the River Spean at Moy.

Geographic entities mentioned:
surface_form: loch ossian
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.777707
lon: -4.627669
Loch Ossian is remote from public roads, and the nearest access is from Corrour railway station. On its banks near the western end of the loch stands Loch Ossian youth hostel, which belongs to the Scottish Youth Hostels Association (SYHA). The hostel was recently restored as an 'eco-hostel', boasting wind and solar power, and grey water and dry toilet systems.

Geographic entities mentioned:
surface_form: loch ossian
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.777707
lon: -4.627669
Old Baldy Mountain (Okanogan County, Washington). Old Baldy Mountain is a peak in the Okanogan-Wenatchee National Forest, in Okanogan County, Washington, 10 miles northwest of Conconully. The height is listed at modern sources as 7,844 ft or 7,849 ft or 7,854 ft. Older government maps showed 7,870 feet elevation. There is a geodetic survey benchmark at 7,848 ft near the summit.

Geographic entities mentioned:
surface_form: old baldy
instance_of: Mountain
countries: United States
coordinates: lat: 31.69612
lon: -110.8481
surface_form: baldy
instance_of: Mountain
countries: United States
coordinates: lat: 31.69612
lon: -110.8481
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: old baldy
instance_of: Mountain
countries: United States
coordinates: lat: 34.2889
lon: -117.647
surface_form: baldy
instance_of: Mountain
countries: United States
coordinates: lat: 42.2983
lon: -122.751
surface_form: old baldy mountain (okanogan county, washington)
instance_of: Mountain
countries: United States
coordinates: lat: 48.59
lon: -119.95611111111
surface_form: old baldy
instance_of: Mountain
countries: United States
coordinates: lat: 36.63
lon: -105.213
surface_form: baldy mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.63
lon: -105.213
surface_form: baldy mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.7856
lon: -105.44
Old Baldy Mountain (Okanogan County, Washington). Old Baldy Mountain is a peak in the Okanogan-Wenatchee National Forest, in Okanogan County, Washington, 10 miles northwest of Conconully. The height is listed at modern sources as 7,844 ft or 7,849 ft or 7,854 ft. Older government maps showed 7,870 feet elevation. There is a geodetic survey benchmark at 7,848 ft near the summit.

Geographic entities mentioned:
surface_form: old baldy
instance_of: Mountain
countries: United States
coordinates: lat: 31.69612
lon: -110.8481
surface_form: baldy
instance_of: Mountain
countries: United States
coordinates: lat: 31.69612
lon: -110.8481
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: old baldy
instance_of: Mountain
countries: United States
coordinates: lat: 34.2889
lon: -117.647
surface_form: baldy
instance_of: Mountain
countries: United States
coordinates: lat: 42.2983
lon: -122.751
surface_form: old baldy
instance_of: Mountain
countries: United States
coordinates: lat: 48.59
lon: -119.95611111111
surface_form: old baldy
instance_of: Mountain
countries: United States
coordinates: lat: 36.63
lon: -105.213
surface_form: baldy mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.63
lon: -105.213
surface_form: baldy mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.7856
lon: -105.44
Baldy Pass is a pass about one kilometer northeast of the peak, and is traversed by Forest Service Road 37. The Golden Stairway multipurpose motorcycle/biking/hiking trail (not to be confused with the Golden Stairs on Alaska's Chilkoot Trail) leads to Old Baldy. Government maps as of 1963 showed a fire lookout tower on the peak, but it was not mentioned in the National Geodetic Survey in 1956.

Geographic entities mentioned:
surface_form: old baldy
instance_of: Mountain
countries: United States
coordinates: lat: 31.69612
lon: -110.8481
surface_form: baldy
instance_of: Mountain
countries: United States
coordinates: lat: 31.69612
lon: -110.8481
surface_form: old baldy
instance_of: Mountain
countries: United States
coordinates: lat: 34.2889
lon: -117.647
surface_form: baldy
instance_of: Mountain
countries: United States
coordinates: lat: 42.2983
lon: -122.751
surface_form: old baldy
instance_of: Mountain
countries: United States
coordinates: lat: 48.59
lon: -119.95611111111
surface_form: old baldy
instance_of: Mountain
countries: United States
coordinates: lat: 36.63
lon: -105.213
Government maps as of 1963 showed a fire lookout tower on the peak, but it was not mentioned in the National Geodetic Survey in 1956. Part of the mountain was burned in the 2006 Tripod Complex Fire, and the area between Old Baldy and Tripod Peak burned in the Cub Creek 2 Fire in late July, 2021.

Geographic entities mentioned:
surface_form: old baldy
instance_of: Mountain
countries: United States
coordinates: lat: 31.69612
lon: -110.8481
surface_form: baldy
instance_of: Mountain
countries: United States
coordinates: lat: 31.69612
lon: -110.8481
surface_form: old baldy
instance_of: Mountain
countries: United States
coordinates: lat: 34.2889
lon: -117.647
surface_form: baldy
instance_of: Mountain
countries: United States
coordinates: lat: 42.2983
lon: -122.751
surface_form: old baldy
instance_of: Mountain
countries: United States
coordinates: lat: 48.59
lon: -119.95611111111
surface_form: old baldy
instance_of: Mountain
countries: United States
coordinates: lat: 36.63
lon: -105.213
Part of the mountain was burned in the 2006 Tripod Complex Fire, and the area between Old Baldy and Tripod Peak burned in the Cub Creek 2 Fire in late July, 2021. The name of the United States Geological Survey 7.5 minute series topographic quadrangle map containing Old Baldy Mountain is &quot;Old Baldy, WA&quot;.

Geographic entities mentioned:
surface_form: old baldy
instance_of: Mountain
countries: United States
coordinates: lat: 31.69612
lon: -110.8481
surface_form: old baldy
instance_of: Mountain
countries: United States
coordinates: lat: 31.69612
lon: -110.8481
surface_form: baldy
instance_of: Mountain
countries: United States
coordinates: lat: 31.69612
lon: -110.8481
surface_form: baldy
instance_of: Mountain
countries: United States
coordinates: lat: 31.69612
lon: -110.8481
surface_form: old baldy
instance_of: Mountain
countries: United States
coordinates: lat: 34.2889
lon: -117.647
surface_form: old baldy
instance_of: Mountain
countries: United States
coordinates: lat: 34.2889
lon: -117.647
surface_form: baldy
instance_of: Mountain
countries: United States
coordinates: lat: 42.2983
lon: -122.751
surface_form: baldy
instance_of: Mountain
countries: United States
coordinates: lat: 42.2983
lon: -122.751
surface_form: old baldy
instance_of: Mountain
countries: United States
coordinates: lat: 48.59
lon: -119.95611111111
surface_form: old baldy
instance_of: Mountain
countries: United States
coordinates: lat: 48.59
lon: -119.95611111111
surface_form: old baldy
instance_of: Mountain
countries: United States
coordinates: lat: 36.63
lon: -105.213
surface_form: old baldy
instance_of: Mountain
countries: United States
coordinates: lat: 36.63
lon: -105.213
surface_form: baldy mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.63
lon: -105.213
surface_form: baldy mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.7856
lon: -105.44
There is a geodetic survey benchmark at 7,848 ft near the summit. Some sources show the mountain in the Okanogan Range. Baldy Pass is a pass about one kilometer northeast of the peak, and is traversed by Forest Service Road 37. The Golden Stairway multipurpose motorcycle/biking/hiking trail (not to be confused with the Golden Stairs on Alaska's Chilkoot Trail) leads to Old Baldy.

Geographic entities mentioned:
surface_form: baldy
instance_of: Mountain
countries: United States
coordinates: lat: 31.69612
lon: -110.8481
surface_form: baldy
instance_of: Mountain
countries: United States
coordinates: lat: 42.2983
lon: -122.751
Public Food distribution system in Mumbai. Suresh headed an Indian People's Tribunal that inquired into the public food distribution system in Mumbai, releasing a report on the subject in March 2010. The HRLN and ANHAD conducted a Tribunal in Srinagar on 20–21 February 2010 that investigated human rights violations in the Kashmir Valley. Suresh headed the jury.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
Personal life. Isabella Williams was born in 1854 in Chicago, Illinois, to John Marshall Williams and Elizabeth Caroline Smith of Evanston, Illinois. She married Charles D. Blaney (1854–1923) on September 6, 1877, in Evanston, and in 1883 they moved to a large ranch in the Santa Clara Valley of California. They had a child, Clarissa Butler Blaney, who died in 1901 of typhoid fever at age 17.

Geographic entities mentioned:
surface_form: Santa Clara Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.366944444444
lon: -121.98388888889
Beginnings. After a request of the &quot;Consell de Cent&quot; (ancient city rulers of Barcelona) in 1578, some Capuchins from Italy came to Barcelona, and they settled in the hermitage of &quot;Santa Madrona&quot; near Montjuïc.

Geographic entities mentioned:
surface_form: Montjuïc
instance_of: Mountain
countries: Spain
coordinates: lat: 41.364166666667
lon: 2.1580555555556
Tour du Marboré. Tour du Marboré () or Tour de Gavarnie is a Pyrenean summit, culminating at, located on the Franco-Spanish border crest in the Monte Perdido Range. Toponymy. see: Cilindro de Marboré
Topography. The Tour du Marboré is part of the range above Cirque de Gavarnie. It marks the border between the Pyrenees National Park of France and the Ordesa y Monte Perdido National Park of Spain.

Geographic entities mentioned:
surface_form: Cilindro de Marboré
instance_of: Mountain
countries: Spain
coordinates: lat: 42.684722
lon: 0.023889
surface_form: marboré
instance_of: Mountain
countries: Spain
France
coordinates: lat: 42.6928
lon: 0.01167
Tour du Marboré. Tour du Marboré () or Tour de Gavarnie is a Pyrenean summit, culminating at, located on the Franco-Spanish border crest in the Monte Perdido Range. Toponymy. see: Cilindro de Marboré
Topography. The Tour du Marboré is part of the range above Cirque de Gavarnie. It marks the border between the Pyrenees National Park of France and the Ordesa y Monte Perdido National Park of Spain.

Geographic entities mentioned:
surface_form: marboré
instance_of: Mountain
countries: Spain
France
coordinates: lat: 42.6928
lon: 0.01167
surface_form: tour du marboré
instance_of: Mountain
countries: Spain
France
coordinates: lat: 42.6856
lon: -0.01722
Tour du Marboré () or Tour de Gavarnie is a Pyrenean summit, culminating at, located on the Franco-Spanish border crest in the Monte Perdido Range. Toponymy. see: Cilindro de Marboré
Topography. The Tour du Marboré is part of the range above Cirque de Gavarnie. It marks the border between the Pyrenees National Park of France and the Ordesa y Monte Perdido National Park of Spain. Mountaineering.

Geographic entities mentioned:
surface_form: marboré
instance_of: Mountain
countries: Spain
France
coordinates: lat: 42.6928
lon: 0.01167
surface_form: tour du marboré
instance_of: Mountain
countries: Spain
France
coordinates: lat: 42.6856
lon: -0.01722
Some environmental organisations expressed regret as the original law project presented in 2018 sought the extablish a definitive ban on the harvest. Along Rubens River in Magallanes Region there are some historically important harvesting fields of peat in &quot;Sphagnum&quot; peatlands.

Geographic entities mentioned:
surface_form: Rubens River
instance_of: Watercourse
countries: Argentina
Chile
coordinates: lat: -51.9
lon: -71.583333333333
Mount Elliot (New Zealand). Mount Elliot is a mountain in Fiordland, New Zealand. Description. Mount Elliot is part of the Wick Mountains and is situated in the Southland Region of the South Island. It is set within Fiordland National Park which is part of the Te Wahipounamu UNESCO World Heritage Site.

Geographic entities mentioned:
surface_form: mount elliot
instance_of: Mountain
countries: New Zealand
coordinates: lat: -44.78
lon: 167.785
The mountain's Māori name is &quot;Te Mauiuio-Ruru&quot; which translates as &quot;the weariness of Ruru,&quot; wherein Ruru was a lesser god who assisted Tuterangiwhanoa in the formation of the fiord landscape. After attacking McKinnon Pass, he sat down and rested on Mount Elliot, forming the depression that created the Jervois Glacier. Climate.

Geographic entities mentioned:
surface_form: mount elliot
instance_of: Mountain
countries: New Zealand
coordinates: lat: -44.78
lon: 167.785
Climate. Based on the Köppen climate classification, Mount Elliot is located in a marine west coast climate zone. Prevailing westerly winds blow moist air from the Tasman Sea onto the mountains, where the air is forced upward by the mountains (orographic lift), causing moisture to drop in the form of rain or snow. This climate supports the Jervois Glacier on the south slope.

Geographic entities mentioned:
surface_form: mount elliot
instance_of: Mountain
countries: New Zealand
coordinates: lat: -44.78
lon: 167.785
The General (Idaho). The General is a mountain summit in Custer County, Idaho, United States. Description. The General is part of the Salmon River Mountains which are a subrange of the Rocky Mountains. The mountain is located 17 miles (27 km) north-northeast of Stanley, Idaho, on the boundary line of the Frank Church–River of No Return Wilderness on land managed by Salmon–Challis National Forest.

Geographic entities mentioned:
surface_form: the general
instance_of: Mountain
coordinates: lat: 44.483387
lon: -114.802816
Topographic relief is significant as the summit rises above Lightning Creek in 0.85 mile (1.37 km) and above Mystery Lake in 0.38 mile (0.61 km). Climate. Based on the Köppen climate classification, The General is located in an alpine subarctic climate zone with long, cold, snowy winters, and cool to warm summers. Winter temperatures can drop below −10 °F with wind chill factors below −30 °F.

Geographic entities mentioned:
surface_form: the general
instance_of: Mountain
coordinates: lat: 44.483387
lon: -114.802816
Route description. The highway begins at an intersection with WIS 35 east of Lake Winneshiek, a lake along the Mississippi River. From there, it runs eastward, following Copper Creek until it ends just west of Mount Sterling, where it intersects WIS 27.

Geographic entities mentioned:
surface_form: Lake Winneshiek
instance_of: Lake
countries: United States
coordinates: lat: 43.31
lon: -91.07
Analysis shows that the water is strikingly similar to the samples taken in 1782, the first year such analysis took place. In fact, doctors from Northern Italy in the 13th century used to suggest that their patients go to the Val Brembana spring for treatment.

Geographic entities mentioned:
surface_form: Val Brembana
instance_of: Valley
countries: Italy
coordinates: lat: 45.8725
lon: 9.651944444444444
The source is a little further north, just over the county border in West Yorkshire, close to the Pennine Way. The highest point of the catchment is Greater Manchester's highest point at Black Chew Head. The river flows generally south through Delph, Uppermill, Mossley, Stalybridge, Ashton-under-Lyne, Dukinfield, Haughton Green, Denton and Hyde.

Geographic entities mentioned:
surface_form: Black Chew Head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.5161
lon: -1.9216
It is located on the Bow River, in the Waputik Range of the Canadian Rockies. It is named after James Hector, a geologist and naturalist with the Palliser Expedition. The lake is formed in a valley of the Waputik Range, north of the Waputik Icefield, between Pulpit Peak, Mount Balfour, Crowfoot Mountain and Bow Peak. Hector Glacier and Mount Hector rise on the opposite side of the Bow River.

Geographic entities mentioned:
surface_form: Pulpit Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5684
lon: -116.3689
surface_form: Mount Balfour
instance_of: Mountain
countries: Canada
coordinates: lat: 51.565555555555555
lon: -116.46527777777777
surface_form: Bow Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.62638888888889
lon: -116.37916666666666
A contingent of 140 Finns arrived in 1664. The ship &quot;Mercurius&quot; sailed to the colony in 1665, and 92 of the 106 passengers were listed as Finns. Memory of the early Finnish settlement lived on in place names near the Delaware River such as Finland (Marcus Hook), Torne, Lapland, Finns Point, Mullica Hill, and Mullica River.

Geographic entities mentioned:
surface_form: Finns Point
instance_of: Landform
countries: United States
coordinates: lat: 39.60583333333334
lon: -75.56055555555555