Sarmila/GeoWiki-Features huggingface dataset:
The Sainte-Marguerite stream, the mouth of which is located southwest of that of the Millette river (i.e. south of the Laviolette bridge), should not therefore be confused with the authentic Rivière Sainte-Marguerite whose toponym was replaced by Rivière Millette. The toponym &quot;rivière Millette&quot; was formalized on August 17, 1978, at the Commission de toponymie du Québec.

Geographic entities mentioned:
surface_form: rivière millette
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.318333333333
lon: -72.561666666667
surface_form: rivière millette
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.318333333333
lon: -72.561666666667
surface_form: rivière sainte-marguerite
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.318333333333
lon: -72.561666666667
Millette River. The Millette River is a tributary of the north shore of the Saint Lawrence River, flowing in the city of Trois-Rivières, Quebec, Canada. The surface of the Millette River (except the rapids areas) is generally frozen from mid-December to mid-March, but safe circulation on the ice is generally made from the end of December to the beginning of March.

Geographic entities mentioned:
surface_form: millette river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.318333333333
lon: -72.561666666667
This source is southwest of the course of the Saint-Maurice River. The Millette River flows onto the northwest shore of the St. Lawrence River, north of the Lacerte stream, south of the confluence of the Saint-Maurice River and north of the Laviolette Bridge which spans the Saint-Laurent river. History.

Geographic entities mentioned:
surface_form: millette river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.318333333333
lon: -72.561666666667
This artificial pond formed by a dam is located on the grounds of UQTR. The Mon Repos villa was built in 1895 on the edge of a small artificial lake on the middle course of the Millette River. This villa was located on leased land, between boulevard des Chenaux and boulevard des Récollets, on the east side of the Rosemont coast.

Geographic entities mentioned:
surface_form: millette river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.318333333333
lon: -72.561666666667
In late August 2011, a flood of the Milette river invaded part of J.-E.-Janvier, Louis-Camirand and Louis-Julien streets, which are located on the northeast side of the lower course of this river which crosses Trois-Rivières. In 2013, the city of Trois-Rivières carried out stabilization work on the banks of the Millette River south of Notre-Dame-Ouest Street. Toponymy.

Geographic entities mentioned:
surface_form: millette river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.318333333333
lon: -72.561666666667
According to a 1926 county map of Saint-Maurice, the mouth of the Millette river corresponds to that of the Sainte-Marguerite river. In 1978, the Commission de toponymie du Québec replaced the toponymic designation &quot;Rivière Sainte-Marguerite&quot; by &quot;Rivière Millette&quot;.

Geographic entities mentioned:
surface_form: millette river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.318333333333
lon: -72.561666666667
Nevertheless, this river remained anonymous for a long time. The Sainte-Marguerite stream, the mouth of which is located southwest of that of the Millette river (i.e. south of the Laviolette bridge), should not therefore be confused with the authentic Rivière Sainte-Marguerite whose toponym was replaced by Rivière Millette.

Geographic entities mentioned:
surface_form: millette river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.318333333333
lon: -72.561666666667
The homestead is about from the North West Coastal Highway. The property shares boundaries with Marrilla, Bullara, and Yanrey Stations; it also has frontage onto Exmouth Gulf. The property occupies an area of, of which about half is sand plains and the rest made up of dunes, limestone plains and stony plains, all of which are suitable for grazing.

Geographic entities mentioned:
surface_form: Marrilla
instance_of: Mountain
countries: Australia
coordinates: lat: -22.972
lon: 114.46
Scum Lake is a lake on the Sibley Peninsula in geographic Sibley Township in the Unorganized Part of Thunder Bay District in Northwestern Ontario, Canada. It is part of the Great Lakes Basin and is located entirely in Sleeping Giant Provincial Park. The primary outflow is an unnamed creek at the north east that flows to Mary Louise Lake, which in turn flows via Sibley Creek to Lake Superior.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Scum Lake (Ontario). Scum Lake is a lake on the Sibley Peninsula in geographic Sibley Township in the Unorganized Part of Thunder Bay District in Northwestern Ontario, Canada. It is part of the Great Lakes Basin and is located entirely in Sleeping Giant Provincial Park.

Geographic entities mentioned:
surface_form: scum lake (ontario)
instance_of: Lake
countries: Canada
coordinates: lat: 48.3756
lon: -88.8292
Scum Lake (Ontario). Scum Lake is a lake on the Sibley Peninsula in geographic Sibley Township in the Unorganized Part of Thunder Bay District in Northwestern Ontario, Canada. It is part of the Great Lakes Basin and is located entirely in Sleeping Giant Provincial Park.

Geographic entities mentioned:
surface_form: scum lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.3756
lon: -88.8292
Scum Lake is a lake on the Sibley Peninsula in geographic Sibley Township in the Unorganized Part of Thunder Bay District in Northwestern Ontario, Canada. It is part of the Great Lakes Basin and is located entirely in Sleeping Giant Provincial Park. The primary outflow is an unnamed creek at the north east that flows to Mary Louise Lake, which in turn flows via Sibley Creek to Lake Superior.

Geographic entities mentioned:
surface_form: sleeping giant
instance_of: Mountain
countries: Canada
coordinates: lat: 48.337222222222
lon: -88.904444444444
It covered a surface area of and reached an altitude of at highstands, although poorly recognizable shorelines have been found at altitudes of. The lake was fed by increased runoff during the Pleistocene and overflowed into the Lake Mojave basin and from there to Lake Manly in Death Valley, or less likely into the Bristol Lake basin and from there to the Colorado River.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
surface_form: Bristol Lake
instance_of: Lake
countries: United States
coordinates: lat: 34.4622
lon: -115.6738
The Mojave River entered the lake from the west, probably forming a river delta. The most recent drainage from the lake was Afton Canyon, which drained the lake east towards Soda Lake, Silver Lake and eventually Death Valley. This draining cut deep into the sediments of Lake Manix, removing about of material and depositing it below Afton Canyon.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Changes in sea surface temperatures increasing moisture supply or increased supply from tropical regions may also have contributed to lake formation. Similar lakes included Lake Babicora, Lake Bonneville, Lake Estancia, Lake Lahontan, Lake Manly, Lake Owens, Lake Panamint, Lake Russell and Lake Searles. Some interglacials also featured the growth of lakes.

Geographic entities mentioned:
surface_form: Lake Panamint
instance_of: Valley
countries: United States
coordinates: lat: 36.0592
lon: -117.244
Whatever path overflow might have taken, Lake Mojave was nourished by such overflow. The Mojave River, together with the Amargosa River, formed Lake Manly in Death Valley; the disappearance of Lake Manix after the formation of Afton Canyon would have increased water supply to Death Valley as evaporation surfaces were reduced.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Another theory assumes that the Troy Lake basin of Lake Manix might have spilled into Bristol Lake and from there into the Colorado River; this theory is viewed as questionable seeing as there is no evidence that Bristol Lake (which Lake Manix waters would have flowed through on the way to the Colorado) contained an overflowing lake, although paleocurrent data obtained from Lake Manix deposits may support it.

Geographic entities mentioned:
surface_form: Bristol Lake
instance_of: Lake
countries: United States
coordinates: lat: 34.4622
lon: -115.6738
surface_form: Bristol Lake
instance_of: Lake
countries: United States
coordinates: lat: 34.4622
lon: -115.6738
On 31 July 2019, Col. Afif Suleiman, commander of the Free Idlib Army and member of the National Front for Liberation's command council, was arrested by Hayat Tahrir al-Sham's security force at a checkpoint near Darat Izza as he was driving from Afrin District to the northern Idlib Governorate. Suleiman was detained in HTS's Oqab Prison in Jabal Zawiya, and released two days later.

Geographic entities mentioned:
surface_form: Jabal Zawiya
instance_of: Mountain
countries: Syria
coordinates: lat: 35.73333333
lon: 36.7
2018 UCI Mountain Bike World Championships. The 2018 UCI Mountain Bike World Championships was the 29th edition of the UCI Mountain Bike World Championships. It was held from 5 to 9 September 2018 in Lenzerheide, Switzerland. The four-cross competitions were held in Val di Sole, Italy from 5 to 6 July 2018

Geographic entities mentioned:
surface_form: Val di Sole
instance_of: Valley
countries: Italy
coordinates: lat: 46.3
lon: 10.8
Here at the confluence of the Salzach and its Lammer tributary, the river leaves the Salzachöfen Gorge between the Berchtesgaden Alps and the Tennen Mountains ranges of the Northern Limestone Alps and flows northwards into the broad Salzburg basin. The Hoher Göll massif of the Berchtesgaden Alps in the west comprise the Schwarzbachfall Cave and the high Golling Waterfall, a natural monument.

Geographic entities mentioned:
surface_form: Hoher Göll
instance_of: Mountain
countries: Austria
Germany
coordinates: lat: 47.594166666667
lon: 13.066944444444
Ross Isles. The Ross Isles are two small islands in Loch Lomond, in west central Scotland. They lie opposite Luss, and are named after the promontory on the east shore (&quot;ros&quot; meaning the same in Scottish Gaelic), where Ross Priory is located. The &quot;Pilot&quot; sank off here in 1850.

Geographic entities mentioned:
surface_form: Loch Lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
At various times he acted as Crown Counsel in the Thunder Bay district. He was a persistent advocate of deep waterways on the Great Lakes, later known as the St Lawrence Seaway and was the Canadian government's watchdog on international water questions such as water levels on the Great Lakes and Lake of the Woods, and the Chicago River water diversion.

Geographic entities mentioned:
surface_form: Lake of the Woods
instance_of: Lake
countries: Canada
United States
coordinates: lat: 49.09027777777778
lon: -95.2388888888889
It has been protected by the central government as a National Historic Site since 1935. Background. Oda Castle is located 5 kilometers south of Mount Tsukuba, in southwestern Hitachi Province, overlooking the Sakura River which flows from the northern slope of Mount Tsukuba towards Lake Kasumigaura.

Geographic entities mentioned:
surface_form: Mount Tsukuba
instance_of: Mountain
countries: Japan
coordinates: lat: 36.22580555555555
lon: 140.105
surface_form: Lake Kasumigaura
instance_of: Lake
Group of lakes
countries: Japan
coordinates: lat: 36.040277777778
lon: 140.39416666667
Commercial fishing or harvesting is not allowed. Description. Salvador WMA is surrounded on three sides by water with Lake Cataouatche to the northeast, Bayou Couba to the east, and Lake Salvador to the south, all considered part of the Wetlands of Louisiana. The WMA is only accessible by boat with the more direct route from US 90 at the Pier 90 Marina down Bayou Verret to Lake Salvador.

Geographic entities mentioned:
surface_form: Lake Cataouatche
instance_of: Lake
countries: United States
coordinates: lat: 29.8417
lon: -90.2328
surface_form: Lake Salvador
instance_of: Lake
countries: United States
coordinates: lat: 29.7238
lon: -90.2462
Ravenshoe, Queensland. Ravenshoe () is a rural town and locality in the Tablelands Region, Queensland, Australia. In the, the locality of Ravenshoe had a population of 1,332 people. Geography. Ravenshoe is on the Atherton Tableland in Far North Queensland. It is located south west of the regional centre, Cairns.

Geographic entities mentioned:
surface_form: Atherton Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
The city borders the province of Anhui to the north, the province of Zhejiang to the east, and the province of Fujian to the south. Also, the city's western reaches extend into Poyang Lake. Shangrao had a population of 6,491,088 as of 2020 census whom 1,293,399 lived in the built up (&quot;or metro&quot;) area made of Xinzhou and Guangxin districts, Guangfeng District not being conurbated yet.

Geographic entities mentioned:
surface_form: Poyang Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 29.066666666667
lon: 116.38333333333
Thanks to your muse, a foreign copper shines,
Turned into gold and coined in sterling lines. In 1773 he wrote a pamphlet called &quot;The Life of John Wilkes, Esq., in the manner of Plutarch&quot;, a Wilkite mob having broken his windows in Dean Street. In 1777 he published &quot;An Account of some of the most Romantic Parts of North Wales&quot;, having ascended Snowdon in 1774. Later life.

Geographic entities mentioned:
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
It is native to eastern North America, where it has an unusual distribution. It is nearly endemic to the Cumberland Plateau of Kentucky and Tennessee, but there are disjunct populations in the Blue Ridge Mountains in North Carolina and Virginia. Its preferred habitat is the deep shade of acidic forests, often growing under &quot;Kalmia latifolia&quot; and &quot;Rhododendron maximum&quot;.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
Foglia (Magliano Sabina). Foglia is a frazione of the Italian comune of Magliano Sabina, in the province of Rieti, Lazio. Geography. Foglia is located on a tuff plateau in the Tiber Valley, between the mouth of the to the north and the to the south, almost opposite the mouth of the river on the Tiber. Prehistory - archaic era.

Geographic entities mentioned:
surface_form: Tiber Valley
instance_of: Valley
countries: Italy
coordinates: lat: 42.133333333333
lon: 12.583333333333
Foglia is located on a tuff plateau in the Tiber Valley, between the mouth of the to the north and the to the south, almost opposite the mouth of the river on the Tiber. Prehistory - archaic era. The town sits close to an ancient ford of the Tiber where it joins the Tiber Valley between Treja and Aia valley an prehistory-archaic way to Archaeological area of Poggio Sommavilla and Falerii Veteres.

Geographic entities mentioned:
surface_form: Tiber Valley
instance_of: Valley
countries: Italy
coordinates: lat: 42.133333333333
lon: 12.583333333333
Upwind the difference is less noticeable but again the 29er XX has the advantage. In April 2007, at the Women's High Performance Dinghy Evaluation Event in Hyères, France, ISAF conducted extensive trials of the 29er XX as a possible choice for a women's high performance dinghy class at the 2016 Olympics.

Geographic entities mentioned:
surface_form: Hyères
instance_of: Mountain
countries: France
coordinates: lat: 43.118888888889
lon: 6.1286111111111
It is the seat of the &quot;Verbandsgemeinde&quot; (&quot;collective municipality&quot;) Elbe-Havel-Land. Geography. The village is situated on a terminal moraine, stretching along the eastern bank of the Elbe River. It is located about north of the state capital of Magdeburg, halfway between Stendal in the west and Rathenow in the east.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Lake Fork Peak. Lake Fork Peak is a mountain summit in Taos County, New Mexico, United States. Description. Lake Fork Peak is part of the Taos Mountains which are a subset of the Sangre de Cristo Mountains. It is the second-highest point in the Wheeler Peak Wilderness and ranks as the sixth-highest summit in New Mexico.

Geographic entities mentioned:
surface_form: lake fork peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.550277777778
lon: -105.44527777778
The peak has also been known as Fairview Mountain. Climate. According to the Köppen climate classification system, Lake Fork Peak has an alpine climate with cold, snowy winters, and cool to warm summers. Due to its altitude, it receives precipitation all year, as snow in winter and as thunderstorms in summer.

Geographic entities mentioned:
surface_form: lake fork peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.550277777778
lon: -105.44527777778
Due to its altitude, it receives precipitation all year, as snow in winter and as thunderstorms in summer. Climbers can expect afternoon rain, hail, and lightning from the seasonal monsoon in late July and August. This climate supports the Taos Ski Valley area immediately north of Lake Fork Peak.

Geographic entities mentioned:
surface_form: lake fork peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.550277777778
lon: -105.44527777778
The San Diego River loosely divided the 'Iipay and the Tiipai historical homelands, while the Kamia lived in the eastern desert areas. The 'Iipai lived to the north, from Escondido to Lake Henshaw, while the Tiipai lived to the south, in lands including the Laguna Mountains, Ensenada, and Tecate. The Kamia lived to the east in an area that included Mexicali and bordered the Salton Sea. Name.

Geographic entities mentioned:
surface_form: Lake Henshaw
instance_of: Lake
countries: United States
coordinates: lat: 33.236703
lon: -116.7454423
The Mexican settlers became refugees on Point Loma as they waited for ships, hoping to evacuate from San Diego as Kumeyaay victories challenged their ability to hold the pueblo. Mexican-American War. During the Mexican–American War, the Kumeyaay were initially neutral. The Kumeyaay of the San Pasqual pueblo were evacuated as the Americans approached the town.

Geographic entities mentioned:
surface_form: Point Loma
instance_of: Landform
countries: United States
coordinates: lat: 32.67
lon: -117.24194444
He was on good terms with the Ethiopian Orthodox Church, in particular Abuna Theophilos, then the Archbishop of Harar (later to become Patriarch). He gained permission to undertake a cataloguing project of ancient manuscripts held on monasteries in the islands of Lake Tana, largely in classical Ge'ez (by then a liturgical language, as Amharic was used for everyday communication).

Geographic entities mentioned:
surface_form: Lake Tana
instance_of: Lake
countries: Ethiopia
coordinates: lat: 12
lon: 37.25
The NCA covers an area of and measures around 25 kilometres from west to east and 50 kilometres from north to south. To the west and southwest, the land ascends from the Severn Valley to the Shropshire Hills and Herefordshire Plateau. To the east it rises from the Stour Valley into the Black Country and Arden.

Geographic entities mentioned:
surface_form: Severn Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 52.5
lon: -2.33333
Mid Severn Sandstone Plateau. The Mid Severn Sandstone Plateau is a rural landscape and one of the natural regions of central England, straddling the border between the counties of Shropshire and Staffordshire. It stretches from the western fringes of the Birmingham conurbation to Telford in the north and Kidderminster in the south.

Geographic entities mentioned:
surface_form: mid severn sandstone plateau
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5092
lon: -2.30361
The community of Battlement Mesa along Interstate 70 takes its name from the mesa. The mesa is similar in geology to the nearby Grand Mesa to the south, and to the Roan Cliffs to the north. It consists largely of a layer of basalt atop underlying layers of sedimentary rock, including a layer of the Green River Formation.

Geographic entities mentioned:
surface_form: Grand Mesa
instance_of: Mountain
countries: United States
coordinates: lat: 39.1333
lon: -107.933
Battlement Mesa. Battlement Mesa is a large prominent mesa in western Colorado in the United States. It sits along the Garfield-Mesa county line, between the Colorado River to the north and Plateau Creek to the south. It is visible south of Interstate 70, visible between the towns of Rifle and Parachute, stretching for approximately 15 miles (24 km) east-west.

Geographic entities mentioned:
surface_form: battlement mesa
instance_of: Mountain
countries: United States
coordinates: lat: 39.358611111111
lon: -107.91472222222
It is visible south of Interstate 70, visible between the towns of Rifle and Parachute, stretching for approximately 15 miles (24 km) east-west. The community of Battlement Mesa along Interstate 70 takes its name from the mesa. The mesa is similar in geology to the nearby Grand Mesa to the south, and to the Roan Cliffs to the north.

Geographic entities mentioned:
surface_form: battlement mesa
instance_of: Mountain
countries: United States
coordinates: lat: 39.358611111111
lon: -107.91472222222
Mormont. &quot;Le Mormont&quot; is a hill in the Swiss canton of Vaud, rising to an elevation of 605 metres, with a prominence of about 115 metres. It is part of the Éclépens municipality between lakes Neuchatel and Geneva. The name is first recorded in AD 814, as &quot;Mauromonte&quot;. It is derived from the Roman-era personal name &quot;Maurus&quot;. Geography.

Geographic entities mentioned:
surface_form: Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
surface_form: neuchatel
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.9
lon: 6.85
Geography. Le Mormont is a hill in the Swiss canton of Vaud, part of the Éclépens municipality, about halfway between lakes Neuchatel and Geneva. It is rising to an elevation of 605 metres, with a prominence of about 115 metres, forming a watershed between the Rhine and the Rhone basins, separating the Venoge and the Orbe valleys to the south and north, respectively.

Geographic entities mentioned:
surface_form: Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
surface_form: neuchatel
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.9
lon: 6.85
Mormont. &quot;Le Mormont&quot; is a hill in the Swiss canton of Vaud, rising to an elevation of 605 metres, with a prominence of about 115 metres. It is part of the Éclépens municipality between lakes Neuchatel and Geneva. The name is first recorded in AD 814, as &quot;Mauromonte&quot;. It is derived from the Roman-era personal name &quot;Maurus&quot;. Geography.

Geographic entities mentioned:
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.50486111
lon: 7.64305556
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6608
lon: 8.05469
Mormont. &quot;Le Mormont&quot; is a hill in the Swiss canton of Vaud, rising to an elevation of 605 metres, with a prominence of about 115 metres. It is part of the Éclépens municipality between lakes Neuchatel and Geneva. The name is first recorded in AD 814, as &quot;Mauromonte&quot;. It is derived from the Roman-era personal name &quot;Maurus&quot;. Geography.

Geographic entities mentioned:
surface_form: mormont
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.65514
lon: 6.53367
As of 2013 with more than 900 species recorded on the site, the Mormont has been considered one of the botanical hotspots of the canton of Vaud, with as a definite advantage the fact that it is still very preserved from invasive plants.

Geographic entities mentioned:
surface_form: mormont
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.65514
lon: 6.53367
It gives access not only to Murray's Anchorage (named for Commander-in-Chief Vice-Admiral Sir George Murray, who led the fleet of the North American Station through the channel to anchor there for the first time in 1794) but to the entire northern lagoon, the Great Sound and Hamilton Harbour, making the channel vital to the success of the Town of Hamilton, which had been established in 1790, and the economic development of the central and western parishes of Bermuda.

Geographic entities mentioned:
surface_form: Hamilton Harbour
instance_of: Landform
countries: United Kingdom
coordinates: lat: 32.289164
lon: -64.784195
The Kuteb people are made of the following clans which is believed to be Children of Kuteb;
Lumbu, Ticwo, Rufu, Askaen, Bika (Zwika), Ticwo, Rubur, Tswaen, Acha, Likam, Cwumam, and the Rucwu. Traditionally they engaged in farming, hunting and fishing in the fertile lands of the Benue River basin.

Geographic entities mentioned:
surface_form: Benue River
instance_of: Watercourse
countries: Cameroon
Nigeria
coordinates: lat: 7.783333
lon: 6.766667
Geography. Mahanoy City is located at (40.812413, -76.140223), with PA 54 as a main thoroughfare and through road, serving as a main street named Centre Street. To the west it connects to Shenandoah thence to the Susquehanna Valley and to the east reaches through several unincorporated villages then passes through Barnesville as Pine Creek Dr.

Geographic entities mentioned:
surface_form: Susquehanna Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.96666666666667
lon: -75.75
Miette Hill. Miette Hill is located on the border of Alberta and British Columbia. It was named for Bonhomme Miette, a figure in French Canadian folklore.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: miette hill
instance_of: Mountain
countries: Canada
coordinates: lat: 52.8475
lon: -118.384
Miette Hill. Miette Hill is located on the border of Alberta and British Columbia. It was named for Bonhomme Miette, a figure in French Canadian folklore.

Geographic entities mentioned:
surface_form: miette hill
instance_of: Mountain
countries: Canada
coordinates: lat: 52.8475
lon: -118.384
It occurs in a some protected areas like Pasonanca Natural Park, Mount Kitanglad and Mount Apo and while these areas a protected on paper encroachment and deforestation continues to occur.

Geographic entities mentioned:
surface_form: Mount Kitanglad
instance_of: Mountain
countries: Philippines
coordinates: lat: 8.1427777777778
lon: 124.9125
Tadekho Hill. Tadekho Hill is an isolated hill in the Northern Interior of British Columbia, Canada, located southwest of Tatogga and southwest of Kitsu Peak. It lies at the southwestern end of Mount Edziza Provincial Park. History. Tadekho Hill was named on 2 January 1980 by the Geological Survey of Canada in association with Tadekho Creek. Geology.

Geographic entities mentioned:
surface_form: Kitsu Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.4246
lon: -130.6906
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: tadekho hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3503
lon: -130.785
It lies at the southwestern end of Mount Edziza Provincial Park. History. Tadekho Hill was named on 2 January 1980 by the Geological Survey of Canada in association with Tadekho Creek. Geology. Tadekho Hill is a volcanic feature associated with the Spectrum Range volcanic complex which in turn form part of the Northern Cordilleran Volcanic Province.

Geographic entities mentioned:
surface_form: Tadekho Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.43296
lon: -130.90399
surface_form: tadekho hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3503
lon: -130.785
History. Tadekho Hill was named on 2 January 1980 by the Geological Survey of Canada in association with Tadekho Creek. Geology. Tadekho Hill is a volcanic feature associated with the Spectrum Range volcanic complex which in turn form part of the Northern Cordilleran Volcanic Province. It is a subglacial mound that formed in the Pleistocene period.

Geographic entities mentioned:
surface_form: Northern Cordilleran Volcanic Province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
surface_form: tadekho hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3503
lon: -130.785
Tadekho Hill. Tadekho Hill is an isolated hill in the Northern Interior of British Columbia, Canada, located southwest of Tatogga and southwest of Kitsu Peak. It lies at the southwestern end of Mount Edziza Provincial Park. History. Tadekho Hill was named on 2 January 1980 by the Geological Survey of Canada in association with Tadekho Creek. Geology.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Tadekho Hill. Tadekho Hill is an isolated hill in the Northern Interior of British Columbia, Canada, located southwest of Tatogga and southwest of Kitsu Peak. It lies at the southwestern end of Mount Edziza Provincial Park. History. Tadekho Hill was named on 2 January 1980 by the Geological Survey of Canada in association with Tadekho Creek. Geology.

Geographic entities mentioned:
surface_form: tadekho hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3503
lon: -130.785
Beinn a' Chreachain. Beinn a' Chreachain (lit. &quot;Mountain of Scallops&quot;) is a Scottish mountain, with a conical top, to the north-west of Loch Lyon.

Geographic entities mentioned:
surface_form: Loch Lyon
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.540449
lon: -4.580667
surface_form: loch lyon
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.540449
lon: -4.580667
Beinn a' Chreachain. Beinn a' Chreachain (lit. &quot;Mountain of Scallops&quot;) is a Scottish mountain, with a conical top, to the north-west of Loch Lyon.

Geographic entities mentioned:
surface_form: beinn a' chreachain
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.560386
lon: -4.647622
Christine Reid. Christine Lincoln Reid (May 8, 1906 - May 4, 1990) was a mountaineer and filmmaker, the first woman to climb Mount Columbia in Canada. Reid started mountain climbing in her early 20s. Her early ascents included Assiniboine and the Grand Teton. In 1936 she made many climbs in the Dolomites; discovering a new route on the Piz Popena south wall, which is named Via Christine for her.

Geographic entities mentioned:
surface_form: Grand Teton
instance_of: Mountain
countries: United States
coordinates: lat: 43.7412
lon: -110.802
Reid started mountain climbing in her early 20s. Her early ascents included Assiniboine and the Grand Teton. In 1936 she made many climbs in the Dolomites; discovering a new route on the Piz Popena south wall, which is named Via Christine for her. She was also an early film maker and documentarian.

Geographic entities mentioned:
surface_form: Piz Popena
instance_of: Mountain
countries: Italy
coordinates: lat: 46.5768
lon: 12.2078
History. When the Mormon pioneers began moving westward across the Great Plains began settling the Salt Lake Valley around the Great Salt Lake in 1847, they relied on existing institutions within the Church of Jesus Christ of Latter-day Saints (LDS Church) in lieu of secular civil government.

Geographic entities mentioned:
surface_form: Salt Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.6839
lon: -111.978
Cerro El Plomo. Cerro El Plomo is a mountain in the Andes near Santiago, Chile. With an elevation of 5,444 m (17,783 ft), it is the largest peak visible from Santiago on clear days. The adequate season to climb this mountain is between November and March. In spring (September to November), soil conditions have abundant snow on the approach.

Geographic entities mentioned:
surface_form: el plomo
instance_of: Mountain
countries: Chile
coordinates: lat: -33.232777777778
lon: -70.212222222222
surface_form: cerro el plomo
instance_of: Mountain
countries: Chile
coordinates: lat: -33.232777777778
lon: -70.212222222222
The Incas climbed to its summit periodically in the 15th century. The first European ascent of the mountain was by Gustav Brandt and Rudolph Lucke in 1896. During a flight from Santiago, Chile, to Mendoza, Argentina, on 16 July 1932, the Pan American-Grace Airways (Panagra) Ford Trimotor &quot;San José&quot; crashed on Cerro El Plomo during a severe snowstorm, killing all nine people on board.

Geographic entities mentioned:
surface_form: el plomo
instance_of: Mountain
countries: Chile
coordinates: lat: -33.232777777778
lon: -70.212222222222
surface_form: cerro el plomo
instance_of: Mountain
countries: Chile
coordinates: lat: -33.232777777778
lon: -70.212222222222
History. Mod Con is a three-piece based out of Melbourne who originally played together under the moniker &quot;Palm Springs&quot;. Having known each other for some time and playing with various solo and collaborative projects. Over Easter 2017, the trio recorded their debut album with Gareth Liddiard at his home in the Goulburn Valley.

Geographic entities mentioned:
surface_form: Goulburn Valley
instance_of: Valley
countries: Australia
coordinates: lat: -36.3831
lon: 145.399
The earliest structures were probably built sometime between the occupation of La Galgada (3000–2000 BCE) and the era of the Chavín culture (1200–300 BCE). The artistic production resembles many of those found at the Moxeke complex in the Casma Valley. Around 1873, the Italian explorer Antonio Raimondi described the location as a &quot;hill&quot;, partially destroyed, built with huge stone walls.

Geographic entities mentioned:
surface_form: Casma Valley
instance_of: Valley
countries: Peru
Diocese of Sigtuna. The Diocese of Sigtuna was a Catholic diocese founded in Sigtuna, Sweden, established in the mid 11th century. At the time, the town of Sigtuna, situated to the north of lake Mälaren and to the south of Uppsala in the Swedish province of Uppland, had been the centre of royal power for some decades, and existed until the middle of the 12th century.

Geographic entities mentioned:
surface_form: Mälaren
instance_of: Lake
countries: Sweden
coordinates: lat: 59.5
lon: 17.2
With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted. Glacier Peak, a stratovolcano that is north-northeast of Skykomish Peak, began forming in the mid-Pleistocene. Due to Glacier Peak's proximity to Skykomish Peak, volcanic ash is common in the area and provides fertile soil for an abundance of wildflowers in its meadow-covered slopes.

Geographic entities mentioned:
surface_form: Glacier Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.14972222
lon: -109.84944444
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.155013
lon: -117.293429
surface_form: skykomish peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.956666666667
lon: -121.16361111111
Skykomish Peak. Skykomish Peak is a mountain summit located in the Henry M. Jackson Wilderness in the North Cascades of Washington state. The mountain is situated on the crest of the Cascade Range, on the shared border of Snohomish County with Chelan County, and also straddling the boundary between Mount Baker-Snoqualmie National Forest and Okanogan-Wenatchee National Forest.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Skykomish Peak. Skykomish Peak is a mountain summit located in the Henry M. Jackson Wilderness in the North Cascades of Washington state. The mountain is situated on the crest of the Cascade Range, on the shared border of Snohomish County with Chelan County, and also straddling the boundary between Mount Baker-Snoqualmie National Forest and Okanogan-Wenatchee National Forest.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: skykomish peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.956666666667
lon: -121.16361111111
Skykomish Peak. Skykomish Peak is a mountain summit located in the Henry M. Jackson Wilderness in the North Cascades of Washington state. The mountain is situated on the crest of the Cascade Range, on the shared border of Snohomish County with Chelan County, and also straddling the boundary between Mount Baker-Snoqualmie National Forest and Okanogan-Wenatchee National Forest.

Geographic entities mentioned:
surface_form: chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Skykomish Peak. Skykomish Peak is a mountain summit located in the Henry M. Jackson Wilderness in the North Cascades of Washington state. The mountain is situated on the crest of the Cascade Range, on the shared border of Snohomish County with Chelan County, and also straddling the boundary between Mount Baker-Snoqualmie National Forest and Okanogan-Wenatchee National Forest.

Geographic entities mentioned:
surface_form: skykomish peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.956666666667
lon: -121.16361111111
The mountain is situated on the crest of the Cascade Range, on the shared border of Snohomish County with Chelan County, and also straddling the boundary between Mount Baker-Snoqualmie National Forest and Okanogan-Wenatchee National Forest. Skykomish Peak is located to the north of Stevens Pass, and the Pacific Crest Trail traverses the east slope of this peak.

Geographic entities mentioned:
surface_form: skykomish peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.956666666667
lon: -121.16361111111
With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted. Glacier Peak, a stratovolcano that is north-northeast of Skykomish Peak, began forming in the mid-Pleistocene. Due to Glacier Peak's proximity to Skykomish Peak, volcanic ash is common in the area and provides fertile soil for an abundance of wildflowers in its meadow-covered slopes.

Geographic entities mentioned:
surface_form: skykomish peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.956666666667
lon: -121.16361111111
At the time, Uttigen Castle was one of the largest fortifications in the Canton of Bern. Uttigen Castle controlled both a major road and a navigable river that connected the Bernese Oberland with the towns of the Swiss Plateau. In 1271 the Freiherr von Wädenswil owned the castle, along with expansive holdings as the governors of Unspunnen, Frutigen and Mülinen.

Geographic entities mentioned:
surface_form: Swiss Plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
In 1271 the Freiherr von Wädenswil owned the castle, along with expansive holdings as the governors of Unspunnen, Frutigen and Mülinen. In 1285 the castle church was mentioned in the Strättliger Chronicle as one of the twelve churches surrounding Lake Thun. In the 14th century the von Wädenswil family died out and the Freiherr von Kramburg inherited Uttigen Castle and village.

Geographic entities mentioned:
surface_form: Lake Thun
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.683333333333
lon: 7.7166666666667
Origins. The Lower Rusizi development program began in July 1964 with assistance from the European Development Fund to develop an irrigated area for rice production. Peasants were to be resettled in villages supplied with water from a dam on the Mpanda River. The project was the basis for the SRDI. The (SRDI) was created in 1973 by Ministerial Order No. 710/27. History.

Geographic entities mentioned:
surface_form: Mpanda River
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.31944
lon: 29.27917
A rice processing plant was installed in 1976. From 1984 to 1992 SRDI collaborated with AMSAR in a rural development project in East Mpanda led by Louis Berger International. The Mpanda East project run by the SRDI aimed to develop of land to the east of the Mpanda River. 5,000 farming families were to be installed to cultivate food crops and irrigated rice.

Geographic entities mentioned:
surface_form: Mpanda River
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.31944
lon: 29.27917
Sustut Peak. Sustut Peak, prominence:, is the highest summit in the drainage of the Sustut River in British Columbia, Canada. Located in the Hogem Ranges west of Sustut Lake, which is at the Sustut River's headwaters, it is southwest of the road to the Kemess Mine.

Geographic entities mentioned:
surface_form: Hogem Ranges
instance_of: Mountain
countries: Canada
coordinates: lat: 55.833333333333
lon: -126
surface_form: Sustut Lake
instance_of: Lake
countries: Canada
coordinates: lat: 56.5833
lon: -126.45
Sustut Peak. Sustut Peak, prominence:, is the highest summit in the drainage of the Sustut River in British Columbia, Canada. Located in the Hogem Ranges west of Sustut Lake, which is at the Sustut River's headwaters, it is southwest of the road to the Kemess Mine.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: sustut peak
instance_of: Mountain
countries: Canada
coordinates: lat: 56.5864
lon: -126.581
Sustut Peak. Sustut Peak, prominence:, is the highest summit in the drainage of the Sustut River in British Columbia, Canada. Located in the Hogem Ranges west of Sustut Lake, which is at the Sustut River's headwaters, it is southwest of the road to the Kemess Mine.

Geographic entities mentioned:
surface_form: sustut peak
instance_of: Mountain
countries: Canada
coordinates: lat: 56.5864
lon: -126.581
In 1219, during the Fifth Crusade, he accompanied Francis on his mission to the court of al-Kāmil, sultan of Egypt. In 1224, he was the first to spot the stigmata on Francis at La Verna. He convinced Francis to publicize the miracle. He was living at Greccio in 1246. He is reported to have died either in 1260–1262 or in 1266.

Geographic entities mentioned:
surface_form: La Verna
instance_of: Mountain
countries: Italy
coordinates: lat: 43.707
lon: 11.931
Setting. The Lompoc field follows the line of the Purisima Hills, a northwest-to-southeast trending range dividing the Santa Ynez Valley on the south from the Los Alamos Valley to the north, and the field is about long by across. The hills are a part of the Burton Mesa region, much of which is an ecological reserve maintained by the California Department of Fish and Game.

Geographic entities mentioned:
surface_form: Santa Ynez Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.5473
lon: -119.858
Geography. Beljarica occupies the marshland between the left bank of the Danube and the curved embankment which protects the drained and arable land in Pančevački Rit and is geographically known as the Pančevači Rit's Cassette). Northern section is known as the bog of Široka Bara. It covers an area of and is locally also known as &quot;Crvenka&quot; or &quot;Balaton&quot;.

Geographic entities mentioned:
surface_form: Široka Bara
instance_of: Lake
countries: Serbia
coordinates: lat: 44.931944444444
lon: 20.345833333333
The British protectorate ended in December 1963. In Tanganyika, British explorers Richard Francis Burton and John Speke became the first Europeans to visit Lake Tanganyika in 1858. In 1919, the British gained control of most of Tanganyikan territory, following a League of Nations mandate that ended the period of German colonial administration that had started in 1884.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
The walkway leads through the canopy of mature native West Coast forest dominated by rimu at a height of around above ground. It passes close to the crowns of mature rimu trees and sits above smaller trees and tree ferns. The loop walk takes in views of the nearby Lake Mahinapua and includes a cantilever extending out into the forest canopy.

Geographic entities mentioned:
surface_form: Lake Mahinapua
instance_of: Lake
countries: New Zealand
coordinates: lat: -42.793
lon: 170.917
Hatun P'ukru. Hatun P'ukru (Quechua &quot;hatun&quot; big, &quot;p'ukru&quot; hole, pit, gap in a surface, &quot;big hole&quot;, Hispanicized spelling &quot;Jatun Pucro&quot;) is a mountain in the Andes of southern Peru, about high. It is situated in the Moquegua Region, General Sánchez Cerro Province, on the border of the districts of Chojata and Matalaque.

Geographic entities mentioned:
surface_form: hatun p'ukru
instance_of: Mountain
countries: Peru
coordinates: lat: -16.5178
lon: -70.7581
surface_form: p'ukru
instance_of: Mountain
countries: Peru
coordinates: lat: -10.61361111
lon: -76.86416667
Hatun P'ukru. Hatun P'ukru (Quechua &quot;hatun&quot; big, &quot;p'ukru&quot; hole, pit, gap in a surface, &quot;big hole&quot;, Hispanicized spelling &quot;Jatun Pucro&quot;) is a mountain in the Andes of southern Peru, about high. It is situated in the Moquegua Region, General Sánchez Cerro Province, on the border of the districts of Chojata and Matalaque.

Geographic entities mentioned:
surface_form: hatun p'ukru
instance_of: Mountain
countries: Peru
coordinates: lat: -16.5178
lon: -70.7581
surface_form: jatun pucro
instance_of: Mountain
countries: Peru
coordinates: lat: -16.5178
lon: -70.7581
surface_form: p'ukru
instance_of: Mountain
countries: Peru
coordinates: lat: -10.61361111
lon: -76.86416667
surface_form: p'ukru
instance_of: Mountain
countries: Peru
coordinates: lat: -10.61361111
lon: -76.86416667
It is claimed that the Butt of Lewis is one of the windiest locations in the United Kingdom. Name. The Gaelic name for the Butt of Lewis, &quot;Rubha Robhanais&quot;, means &quot;Robhanais Point&quot;. The name &quot;Robhanais&quot;, formerly anglicised as &quot;Rowaness&quot;, comes from the Norse &quot;Rófunes&quot;, meaning &quot;promontory of the tail&quot;. Lighthouse.

Geographic entities mentioned:
surface_form: rubha robhanais
instance_of: Landform
countries: United Kingdom
coordinates: lat: 58.5156
lon: -6.26119
surface_form: butt of lewis
instance_of: Landform
countries: United Kingdom
coordinates: lat: 58.5156
lon: -6.26119
Butt of Lewis. The Butt of Lewis () is the most northerly point on the Island of Lewis, in the Outer Hebrides, Scotland. The headland, which lies in the North Atlantic, is frequently battered by heavy swells and storms and is marked by the Butt of Lewis Lighthouse. The nearest populated area is the village of Eoropie, about to the south.

Geographic entities mentioned:
surface_form: butt of lewis
instance_of: Landform
countries: United Kingdom
coordinates: lat: 58.5156
lon: -6.26119