Sarmila/GeoWiki-Features huggingface dataset:
Its chief geographical features are Cuilcagh mountain on whose eastern side it lies, reaching a height of 1,208 feet; Pollnagollum Cave (Irish derived place name &quot;Poll na gColmán&quot;, meaning 'The Hole of the Pigeons') on the boundary with Binkeeragh townland; mountain streams; mountain pools; river swallowholes; caverns; a wood; spring wells and a dug well.

Geographic entities mentioned:
surface_form: Cuilcagh
instance_of: Mountain
countries: United Kingdom
Ireland
coordinates: lat: 54.2
lon: -7.811
Aghaboy is traversed by minor public roads and rural lanes. The townland covers 287 statute acres. History. In the 1609 Plantation of Ulster, Aghaboy formed part of the mountain of Cuilcagh which were granted to John Sandford of Castle Doe, County Donegal (the father-in-law of Thomas Guyllym of Ballyconnell) by letters patent dated 7 July 1613 (Pat. 11 James I – LXXI – 38, &quot;‘Quilkagh’&quot;).

Geographic entities mentioned:
surface_form: Cuilcagh
instance_of: Mountain
countries: United Kingdom
Ireland
coordinates: lat: 54.2
lon: -7.811
Much of it is set up as a museum known as the Johnson Historical Museum of the Southwest. History. The San Bernardino Valley was originally home to Southern Athabaskan Native American tribes. Spanish missionaries, including the Jesuit missionary Father Eusebio Kino, were the first Europeans to visit the site, in 1694.

Geographic entities mentioned:
surface_form: San Bernardino Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.066666666667
lon: -117.28333333333
The tall mountain is located about south of the village of Vang i Valdres and about north of the village of Trøym. The mountain is surrounded by several other notable mountains including Rankonosi and Klanten to the north, Storebotteggi to the northwest, Veslebotnskarvet to the southeast, and Blåkampen to the east.

Geographic entities mentioned:
surface_form: Rankonosi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.05
lon: 8.48333333
surface_form: Klanten
instance_of: Mountain
countries: Norway
coordinates: lat: 61.038747
lon: 8.541556
surface_form: Storebotteggi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.028888888889
lon: 8.4247222222222
surface_form: Veslebotnskarvet
instance_of: Mountain
countries: Norway
coordinates: lat: 60.9296
lon: 8.616
surface_form: Blåkampen
instance_of: Mountain
countries: Norway
coordinates: lat: 60.979656
lon: 8.694764
Ranastongi. Ranastongi or Ranastøngji is a mountain on the border of Vang Municipality in Innlandet county and Hemsedal Municipality in Buskerud county, Norway. The tall mountain is located about south of the village of Vang i Valdres and about north of the village of Trøym.

Geographic entities mentioned:
surface_form: ranastongi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.018333333333
lon: 8.5094444444444
Ranastongi. Ranastongi or Ranastøngji is a mountain on the border of Vang Municipality in Innlandet county and Hemsedal Municipality in Buskerud county, Norway. The tall mountain is located about south of the village of Vang i Valdres and about north of the village of Trøym.

Geographic entities mentioned:
surface_form: ranastongi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.018333333333
lon: 8.5094444444444
surface_form: ranastøngji
instance_of: Mountain
countries: Norway
coordinates: lat: 61.018333333333
lon: 8.5094444444444
Ranastongi. Ranastongi or Ranastøngji is a mountain on the border of Vang Municipality in Innlandet county and Hemsedal Municipality in Buskerud county, Norway. The tall mountain is located about south of the village of Vang i Valdres and about north of the village of Trøym.

Geographic entities mentioned:
surface_form: valdres
instance_of: Valley
countries: Norway
coordinates: lat: 60.916666666667
lon: 9.1666666666667
Khirbat Nuqayb al-Asaymir. Khirbat Nuqayb al-Asaymir (In Arabic means &quot;Ruin of the Small Black Pass&quot;, abbreviated as KNA) is a Middle Islamic period (1000-1400 CE) archaeological site located at Faynan, southern Jordan. The site contains smelting workshops, dwellings, watchtowers, and administration areas.

Geographic entities mentioned:
surface_form: Faynan
instance_of: Valley
countries: Jordan
coordinates: lat: 30.62282
lon: 35.44775
Geography. Khirbat Nuqayb al-Asaymir is located in the northwest direction of the archaeological site Khirbat Faynan; they are both located in the area of Wadi Faynan. KNA is at the midway between Dead Sea and Red Sea. The climate at KNA is arid, and the site is surrounded by a desert. History.

Geographic entities mentioned:
surface_form: Wadi Faynan
instance_of: Valley
countries: Jordan
coordinates: lat: 30.62282
lon: 35.44775
Cheonseongsan. Cheonseongsan () is a mountain of Gyeongsang Province, southeastern South Korea. It has an elevation of 812 metres.

Geographic entities mentioned:
surface_form: cheonseongsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 35.42027778
lon: 129.11222222
Sorcery Ridge. Sorcery Ridge is a mountain ridge extending east of Tencho Glacier on the southern flank of Mount Edziza in northwestern British Columbia, Canada. It is bounded on the north and south by valleys containing unnamed streams while to the east and northeast it is bounded by Tennaya Creek valley.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
surface_form: sorcery ridge
instance_of: Mountain
coordinates: lat: 57.65606944444444
lon: -130.61504166666666
Sorcery Ridge. Sorcery Ridge is a mountain ridge extending east of Tencho Glacier on the southern flank of Mount Edziza in northwestern British Columbia, Canada. It is bounded on the north and south by valleys containing unnamed streams while to the east and northeast it is bounded by Tennaya Creek valley.

Geographic entities mentioned:
surface_form: Tennaya Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.69966
lon: -130.42065
The highest point of Sorcery Ridge reaches an elevation of at its westernmost end. Sorcery Ridge is one of three ridges east of the Big Raven Plateau named by Canadian volcanologist Jack Souther, the other two being Cartoona Ridge to the south and Idiji Ridge to the north. Geology.

Geographic entities mentioned:
surface_form: Big Raven Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
surface_form: Cartoona Ridge
instance_of: Mountain
coordinates: lat: 57.60666666666667
lon: -130.6147222222222
surface_form: Idiji Ridge
instance_of: Mountain
coordinates: lat: 57.67653055555555
lon: -130.6231527777778
surface_form: sorcery ridge
instance_of: Mountain
coordinates: lat: 57.65606944444444
lon: -130.61504166666666
The Nido and Ice Peak formations are two geological formations comprising the Mount Edziza volcanic complex which has been the focus of volcanic activity since the Miocene. The northern side of Sorcery Ridge contains a volcanic plug called The Neck.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
The northern side of Sorcery Ridge contains a volcanic plug called The Neck. It consists mainly of trachyte of the Ice Peak Formation and is about in diameter, representing the eroded remains of a parasitic vent on the southeastern flank of the Ice Peak stratovolcano. Two distinctive flows of Edziza obsidian are present on Sorcery Ridge which are also part of the Ice Peak Formation.

Geographic entities mentioned:
surface_form: Ice Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
Sorcery Ridge. Sorcery Ridge is a mountain ridge extending east of Tencho Glacier on the southern flank of Mount Edziza in northwestern British Columbia, Canada. It is bounded on the north and south by valleys containing unnamed streams while to the east and northeast it is bounded by Tennaya Creek valley.

Geographic entities mentioned:
surface_form: sorcery ridge
instance_of: Mountain
coordinates: lat: 57.65606944444444
lon: -130.61504166666666
It is bounded on the north and south by valleys containing unnamed streams while to the east and northeast it is bounded by Tennaya Creek valley. Sorcery Ridge is the namesake of Sorcery Creek which flows adjacent to Tennaya Creek from another ridge just to the south. The highest point of Sorcery Ridge reaches an elevation of at its westernmost end.

Geographic entities mentioned:
surface_form: sorcery ridge
instance_of: Mountain
coordinates: lat: 57.65606944444444
lon: -130.61504166666666
Sorcery Ridge is the namesake of Sorcery Creek which flows adjacent to Tennaya Creek from another ridge just to the south. The highest point of Sorcery Ridge reaches an elevation of at its westernmost end. Sorcery Ridge is one of three ridges east of the Big Raven Plateau named by Canadian volcanologist Jack Souther, the other two being Cartoona Ridge to the south and Idiji Ridge to the north.

Geographic entities mentioned:
surface_form: sorcery ridge
instance_of: Mountain
coordinates: lat: 57.65606944444444
lon: -130.61504166666666
Geology. Sorcery Ridge consists largely of sedimentary, volcanic, granitic and metamorphic rocks of Mesozoic and Paleozoic age. These rocks are overlain by Pliocene alkali basalt flows of the Nido Formation which are in turn overlain by Pleistocene alkali basalt, hawaiite, tristanite, trachybasalt and mugearite flows and pyroclastic breccia of the Ice Peak Formation.

Geographic entities mentioned:
surface_form: sorcery ridge
instance_of: Mountain
coordinates: lat: 57.65606944444444
lon: -130.61504166666666
The Nido and Ice Peak formations are two geological formations comprising the Mount Edziza volcanic complex which has been the focus of volcanic activity since the Miocene. The northern side of Sorcery Ridge contains a volcanic plug called The Neck.

Geographic entities mentioned:
surface_form: sorcery ridge
instance_of: Mountain
coordinates: lat: 57.65606944444444
lon: -130.61504166666666
The northern side of Sorcery Ridge contains a volcanic plug called The Neck. It consists mainly of trachyte of the Ice Peak Formation and is about in diameter, representing the eroded remains of a parasitic vent on the southeastern flank of the Ice Peak stratovolcano. Two distinctive flows of Edziza obsidian are present on Sorcery Ridge which are also part of the Ice Peak Formation.

Geographic entities mentioned:
surface_form: sorcery ridge
instance_of: Mountain
coordinates: lat: 57.65606944444444
lon: -130.61504166666666
Until then, he rendered regimental service with his parent unit on the North-West Frontier. In March 1936, he was appointed as staff captain of the Deccan Area. In 1938, Cariappa was promoted to major and was appointed the deputy assistant adjutant and quarter master general (DAA & QMG). World War II.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
The first sequence shot was the baptism of Jesus. The Pyramid Lake in Nevada represented the Sea of Galilee, and Lake Moab in Utah was used to film the Sermon on the Mount. Death Valley in California was filmed for Jesus's 40-day journey into the wilderness. Sections of the film were also shot at Lake Powell, Canyonlands and Dead Horse Point in Utah.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Chelan, Washington. Chelan () is a city in Chelan County, Washington, United States. The estimated population was 4,222 at the 2020 census. It lies on the southeast tip of Lake Chelan, where the lake flows into the Chelan River. Chelan is part of the Wenatchee−East Wenatchee Metropolitan Statistical Area. History.

Geographic entities mentioned:
surface_form: Lake Chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
As the unrest continued into the 1870s, Lt. Colonel Henry Clay Merriam of the United States Army established Camp Chelan at the foot of Lake Chelan to control and safeguard the Indian population on the Moses Columbia Reservation.

Geographic entities mentioned:
surface_form: Lake Chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
Geography. The Missisquoi North River originates west of Lake Stukely and south of North Stukely. Two streams (coming from the north and the northwest) flow into Parker Lake (altitude:).

Geographic entities mentioned:
surface_form: Lake Stukely
instance_of: Lake
countries: Canada
coordinates: lat: 45.3753
lon: -72.2519
Constructed by Baku Plaza Ltd. at a reported cost of about $41.5 million, the mall houses 99 businesses, including a supermarket, a cinema, a children's playground, and several restaurants that offer views of the Bay of Baku on the Caspian Sea. The opening of Park Bulvar in 2010 was attended by President Ilham Aliyev and his family.

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
The river catchment contains ecologically significant alpine wetlands. In 2004, ACTEW announced that the creation of a large reservoir by damming the Gudgenby River, below Mount Tennent, was one of three options being considered as part of the Future Water Options Project to provide improved reliability and increased supply of potable water for Canberra and the ACT.

Geographic entities mentioned:
surface_form: Mount Tennent
instance_of: Mountain
countries: Australia
coordinates: lat: -35.55
lon: 149.05
Kotsifos Gorge. The Kotsifos Gorge () is a gorge on the southern side of the western part of the island of Crete. It is situated west of the mountain of Kouroupa, north of the town of Plakias, and on the road between Sellia and Angouseliana. It is noted for the high number of Cretan endemic plant species that grow there.

Geographic entities mentioned:
surface_form: Kouroupa
instance_of: Mountain
countries: Greece
coordinates: lat: 35.216666666667
lon: 24.433333333333
Rit'ipata (Ayacucho). Rit'ipata (Quechua &quot;rit'i&quot; snow, &quot;pata&quot; elevated place / above, at the top / edge, bank (of a river), shore, also spelled &quot;Ritipata&quot;) is a mountain in the Andes of Peru, about high. It is situated in the Ayacucho Region, Cangallo Province, Paras District. Rit'ipata lies south-west of the mountain Saywa Q'asa and north of the mountain Waranwallqa.

Geographic entities mentioned:
surface_form: Saywa Q'asa
instance_of: Mountain
countries: Peru
coordinates: lat: -13.4181
lon: -74.6594
surface_form: Waranwallqa
instance_of: Mountain
countries: Peru
coordinates: lat: -13.4469
lon: -74.6886
surface_form: waranwallqa
instance_of: Mountain
countries: Peru
coordinates: lat: -13.4469
lon: -74.6886
surface_form: saywa q'asa
instance_of: Mountain
countries: Peru
coordinates: lat: -13.4181
lon: -74.6594
Rit'ipata (Ayacucho). Rit'ipata (Quechua &quot;rit'i&quot; snow, &quot;pata&quot; elevated place / above, at the top / edge, bank (of a river), shore, also spelled &quot;Ritipata&quot;) is a mountain in the Andes of Peru, about high. It is situated in the Ayacucho Region, Cangallo Province, Paras District. Rit'ipata lies south-west of the mountain Saywa Q'asa and north of the mountain Waranwallqa.

Geographic entities mentioned:
surface_form: ritipata
instance_of: Mountain
countries: Peru
coordinates: lat: -14.61972222
lon: -69.35944444
surface_form: rit'ipata
instance_of: Mountain
countries: Peru
coordinates: lat: -14.61972222
lon: -69.35944444
surface_form: ritipata
instance_of: Mountain
countries: Peru
coordinates: lat: -13.4292
lon: -74.6917
Rit'ipata (Ayacucho). Rit'ipata (Quechua &quot;rit'i&quot; snow, &quot;pata&quot; elevated place / above, at the top / edge, bank (of a river), shore, also spelled &quot;Ritipata&quot;) is a mountain in the Andes of Peru, about high. It is situated in the Ayacucho Region, Cangallo Province, Paras District. Rit'ipata lies south-west of the mountain Saywa Q'asa and north of the mountain Waranwallqa.

Geographic entities mentioned:
surface_form: rit'ipata
instance_of: Mountain
countries: Peru
coordinates: lat: -14.61972222
lon: -69.35944444
surface_form: rit'ipata (ayacucho)
instance_of: Mountain
countries: Peru
coordinates: lat: -13.4292
lon: -74.6917
Historical testing. DVB-T was repeatedly tested from RTÉ Network Limited's Three Rock Mountain transmitter, with relatively long tests in 1998 and 2001, and shorter tests in 2004, with a single multiplex carrying the four Irish analogue terrestrial channels, and Tara Television while it was in existence, on both UHF (channel 26) and VHF (channel D).

Geographic entities mentioned:
surface_form: Three Rock Mountain
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.245277777778
lon: -6.2391666666667
Nickorick Beach. Nickorick Beach is a hamlet on the southern shore of Wakaw Lake in Rural Municipality of Hoodoo No. 401, Saskatchewan, Canada. The hamlet is located north of the intersections of Highway 41 and Range road 260 on Range road 260, approximately east of the town of Wakaw.

Geographic entities mentioned:
surface_form: Wakaw Lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.6667
lon: -105.583
The southern part of the lake is a strait 0.8 km long to the bottom of a bay which receives the discharge of Philippe Lake. The waters of Lake Fontaine pour the northwest at the end of a long bay in a small discharge of 0.5 km to the lake Nicolas that crosses North Mékinac River, which runs in the Lejeune Township of Sainte-Thècle to the south-west.

Geographic entities mentioned:
surface_form: mékinac river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.854166666667
lon: -72.765555555556
Lake Fontaine (Mékinac). The Lac Fontaine (Fountain Lake) is a lake located in the municipality of Grandes-Piles, in the Mékinac Regional County Municipality, in Mauricie, in Quebec, in Canada. Geography. The &quot;Lake Fontaine&quot; is located in forest and mountain areas. The north end of the lake is 0.3 km south-west of the boundary of Sainte-Thècle.

Geographic entities mentioned:
surface_form: lake fontaine (mékinac)
instance_of: Lake
countries: Canada
coordinates: lat: 46.8153
lon: -72.6617
Lake Fontaine (Mékinac). The Lac Fontaine (Fountain Lake) is a lake located in the municipality of Grandes-Piles, in the Mékinac Regional County Municipality, in Mauricie, in Quebec, in Canada. Geography. The &quot;Lake Fontaine&quot; is located in forest and mountain areas. The north end of the lake is 0.3 km south-west of the boundary of Sainte-Thècle.

Geographic entities mentioned:
surface_form: lac fontaine
instance_of: Lake
countries: Canada
coordinates: lat: 46.8153
lon: -72.6617
The &quot;chemin of lake Fontaine&quot; from the intersection of Route 159 at the north end of Lake Roberge (Grandes-Piles), and moves towards the northeast to cross the path &quot;Joseph-St-Amant&quot; that penetrates deep into the Lejeune Township of Sainte-Thècle. Toponymy.

Geographic entities mentioned:
surface_form: lake roberge (grandes-piles)
instance_of: Lake
countries: Canada
coordinates: lat: 46.7661
lon: -72.675
Geography. The &quot;Lake Fontaine&quot; is located in forest and mountain areas. The north end of the lake is 0.3 km south-west of the boundary of Sainte-Thècle. The southern end is located 0.4 km from the mouth of the &quot;Lac du Renard&quot; (Fox Lake), located in the southeast, which is a tributary of Lake Fontaine.

Geographic entities mentioned:
surface_form: fox lake
instance_of: Body of water
countries: Canada
coordinates: lat: 49.8714
lon: -83.8733
surface_form: fox lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.8069
lon: -63.5036
surface_form: fox lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.6794
lon: -63.7052
surface_form: fox lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.8491
lon: -63.3286
Two bays north then represent the dog's ears. A forest road (north-south) serving the owners of the lake passes on the west side of the lake. The &quot;Watchtower fire path&quot; passes near the lake (south side), this path leads to the ancient tower fender at the top of a mountain in southern of Archange Lake (Mékinac).

Geographic entities mentioned:
surface_form: archange lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.7994
lon: -72.627
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The waters of Lake Fontaine pour the northwest at the end of a long bay in a small discharge of 0.5 km to the lake Nicolas that crosses North Mékinac River, which runs in the Lejeune Township of Sainte-Thècle to the south-west. continues and in Grandes-Piles to reach the north end of Lake Roberge (Grandes-Piles)
The lake fontaine is made in length, in the north-south direction.

Geographic entities mentioned:
surface_form: lake roberge (grandes-piles)
instance_of: Lake
countries: Canada
coordinates: lat: 46.7661
lon: -72.675
Lake Fontaine (Mékinac). The Lac Fontaine (Fountain Lake) is a lake located in the municipality of Grandes-Piles, in the Mékinac Regional County Municipality, in Mauricie, in Quebec, in Canada. Geography. The &quot;Lake Fontaine&quot; is located in forest and mountain areas. The north end of the lake is 0.3 km south-west of the boundary of Sainte-Thècle.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
West Texas is often subdivided according to distinct physiographic features. The portion of West Texas that lies west of the Pecos River is often called &quot;Far West Texas&quot; or the &quot;Trans-Pecos&quot;, a term introduced in 1887 by geologist Robert T. Hill. The Trans-Pecos lies within the Chihuahuan Desert and is the aridest part of the state.

Geographic entities mentioned:
surface_form: Trans-Pecos
instance_of: Valley
countries: United States
coordinates: lat: 30.56
lon: -103.79
Another part of West Texas is the Llano Estacado, a vast region of high, level plains extending into Eastern New Mexico and the Texas Panhandle. East of the Llano Estacado lies the &quot;redbed country&quot; of the Rolling Plains, and south of the Llano Estacado lies the Edwards Plateau. The Rolling Plains and Edwards Plateau subregions act as transitional zones between eastern and western Texas.

Geographic entities mentioned:
surface_form: Edwards Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 30.3
lon: -99.6
Silver River (Baraga County). The Silver River is a river in the U.S. state of Michigan. It rises from the outflow of Fisher Lake at and flows in an arc to the northwest, then bends to the northeast before emptying into Huron Bay of Lake Superior at. Silver Falls are located on the river at.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Fleischbank (Kaiser). The Fleischbank is a 2,187-metre-high mountain in the Wilder Kaiser range in the Northern Limestone Alps in Austria, east of Kufstein in the Tyrol. The mountain is one of the well-known climbs in the Northern Limestone Alps. The starting point for many easy to difficult climbing tours is the Stripsenjochhaus belonging to the ÖAV.

Geographic entities mentioned:
surface_form: fleischbank
instance_of: Mountain
countries: Austria
coordinates: lat: 47.569167
lon: 12.3175
Skowkale First Nation. u47mskigo626581hj56ipzvf4afs" xml:space="preserve">The Skowkale First Nation or Skowkale Band () is a band government of the people located in the Upper Fraser Valley region, near Sardis, part of Chilliwack, British Columbia, Canada. They are a member government of the tribal council.

Geographic entities mentioned:
surface_form: Upper Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
Seti II is only attested in Upper Egypt in Regnal Year 1, 2, 5 and 6 of his reign while the usurper Amenmesse likely seized control of Upper Egypt and the Valley of the Kings sometime between Year 2 until Year 5 of Seti II's reign when he was finally defeated.

Geographic entities mentioned:
surface_form: Valley of the Kings
instance_of: Valley
countries: Egypt
coordinates: lat: 25.74025
lon: 32.602358
Yurco. Reign. Seti II promoted Chancellor Bay to become his most important state official and built 3 tombs &ndash; KV13, KV14, and KV15 &ndash; for himself, his Senior Queen Tausert and Bay in the Valley of the Kings. This was an unprecedented act on his part for Bay, who was of Syrian descent and was not connected by marriage or blood ties to the royal family.

Geographic entities mentioned:
surface_form: Valley of the Kings
instance_of: Valley
countries: Egypt
coordinates: lat: 25.74025
lon: 32.602358
Evidently this 'Mose' must have been a person of the highest importance, perhaps the king Amenmesse himself or a senior ally of the king. Seti II also expanded the copper mining at Timna Valley in Edom, building an important temple to Hathor, the cow goddess, in the region.

Geographic entities mentioned:
surface_form: Timna Valley
instance_of: Valley
countries: Israel
coordinates: lat: 29.78777778
lon: 34.98888889
For several years he traveled throughout the country as well as parts of Central America. He was also for some time a resident of Saint Paul, Minnesota. He eventually settled in the Red River Valley in 1859 in the fledgling community of Georgetown, Minnesota. Probstfield returned to Germany in the fall of 1860 upon news of his father's death, but he came back to Georgetown in June 1861.

Geographic entities mentioned:
surface_form: Red River Valley
instance_of: Valley
countries: Canada
United States
coordinates: lat: 49
lon: -97.5
Lamborghini has used carbon fibre in the construction, and the back of the chassis contains high-strength aluminium alloys. Powertrain. The Revuelto features a new 6.5-liter V12 engine, complemented by three electric motors that produce a combined power of 746.5 kW. Opera Unica (2024). The Opera Unica is a one-off Revuelto unveiled in Cala di Volpe, Sardinia in August 2024.

Geographic entities mentioned:
surface_form: Cala di Volpe
instance_of: Body of water
countries: Italy
coordinates: lat: 41.094
lon: 9.539
The location is difficult to pin down given the much broader extent of the March of Istria in the 12th century, which included the Karst Plateau, Trieste, Duino and most of the area of later Inner Carniola, possibly even encompassing the upper Vipava Valley.

Geographic entities mentioned:
surface_form: Vipava Valley
instance_of: Valley
countries: Slovenia
coordinates: lat: 45.876147222222
lon: 13.907319444444
Grace and Bancroft are the only incorporated towns in Gem Valley. However, there are several unincorporated communities including Cleveland, Thatcher, Lago, Bench, Niter, Dugway, Turner, Stanley, Lund, Tenmile, and Chesterfield. Some of these were once pioneer-era towns and settlements, but the name now denotes a region of the valley, rather than a town with defined boundaries. Geology.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
By local definition, Gem Valley originates at the Chesterfield Reservoir to the north, and terminates at the Oneida Narrows Reservoir to the south. History. Gem Valley was once inhabited by Shoshone Indians. Artifacts such as arrowheads can still be found there. White settlement dates back to the mid-to-late 19th century.

Geographic entities mentioned:
surface_form: shoshone
instance_of: Lake
countries: United States
coordinates: lat: 44.3722
lon: -110.713
surface_form: gem valley
instance_of: Valley
countries: United States
coordinates: lat: 42.49631
lon: -111.75828
This is the result of several extinct volcanoes and lava domes within the area. Most of the local obsidian is black with low gas content. Some of the mineral contains light brown marbling that is unique to the area. Obsidian plays historical importance to Gem Valley as it was used by the Shoshone Indians that once inhabited for knives and arrowheads.

Geographic entities mentioned:
surface_form: shoshone
instance_of: Lake
countries: United States
coordinates: lat: 44.3722
lon: -110.713
surface_form: gem valley
instance_of: Valley
countries: United States
coordinates: lat: 42.49631
lon: -111.75828
Gem Valley. Gem Valley is a rural valley in Caribou County, Bannock, and Franklin counties in Idaho, United States, so named for its local gemstones which can be found throughout the valley. It is approximately wide at its widest point east to west, and long north to south.

Geographic entities mentioned:
surface_form: gem valley
instance_of: Valley
countries: United States
coordinates: lat: 42.49631
lon: -111.75828
Gem Valley. Gem Valley is a rural valley in Caribou County, Bannock, and Franklin counties in Idaho, United States, so named for its local gemstones which can be found throughout the valley. It is approximately wide at its widest point east to west, and long north to south.

Geographic entities mentioned:
surface_form: gem valley
instance_of: Valley
countries: United States
coordinates: lat: 42.49631
lon: -111.75828
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
It is approximately wide at its widest point east to west, and long north to south. By local definition, Gem Valley originates at the Chesterfield Reservoir to the north, and terminates at the Oneida Narrows Reservoir to the south. History. Gem Valley was once inhabited by Shoshone Indians. Artifacts such as arrowheads can still be found there.

Geographic entities mentioned:
surface_form: gem valley
instance_of: Valley
countries: United States
coordinates: lat: 42.49631
lon: -111.75828
surface_form: oneida
instance_of: Lake
countries: United States
coordinates: lat: 43.2
lon: -75.9
Geography. Gem Valley is one of the northernmost valleys along the Wasatch Range which extends approximately south. The valley floor has an elevation roughly, while the surrounding mountain peaks have an elevation ranging from about. It is accessed primarily by Idaho State Highway 34 from the south, and U.S. Route 30 from the east and west.

Geographic entities mentioned:
surface_form: gem valley
instance_of: Valley
countries: United States
coordinates: lat: 42.49631
lon: -111.75828
The Bear River runs through the valley as well as several small streams. Grace and Bancroft are the only incorporated towns in Gem Valley. However, there are several unincorporated communities including Cleveland, Thatcher, Lago, Bench, Niter, Dugway, Turner, Stanley, Lund, Tenmile, and Chesterfield.

Geographic entities mentioned:
surface_form: gem valley
instance_of: Valley
countries: United States
coordinates: lat: 42.49631
lon: -111.75828
Some of these were once pioneer-era towns and settlements, but the name now denotes a region of the valley, rather than a town with defined boundaries. Geology. The most common gemstone found in Gem Valley is obsidian. This is the result of several extinct volcanoes and lava domes within the area. Most of the local obsidian is black with low gas content.

Geographic entities mentioned:
surface_form: gem valley
instance_of: Valley
countries: United States
coordinates: lat: 42.49631
lon: -111.75828
Obsidian plays historical importance to Gem Valley as it was used by the Shoshone Indians that once inhabited for knives and arrowheads. Other local gemstones that are common to Gem Valley are geode, quartz, agate, and petrified wood
Solid basalt can be found beneath the soil throughout most of the valley and exposed outcrops are common.

Geographic entities mentioned:
surface_form: gem valley
instance_of: Valley
countries: United States
coordinates: lat: 42.49631
lon: -111.75828
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Trilobite fossils can often be found in local shale deposits. In the northern end of the valley, limestone is commercially mined and processed into lime which is used elsewhere in concrete and steel production. Much of the soil in Gem Valley is dark, nitrogen rich volcanic soil. This soil type is ideal for farming, particularly potatoes and grain. Clay sediment is also common.

Geographic entities mentioned:
surface_form: gem valley
instance_of: Valley
countries: United States
coordinates: lat: 42.49631
lon: -111.75828
History. Gem Valley was once inhabited by Shoshone Indians. Artifacts such as arrowheads can still be found there. White settlement dates back to the mid-to-late 19th century. The Oregon Trail passed through the northern part of the valley and several pioneer landmarks such as cemeteries and small settlements can be found throughout the valley. Geography.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Geography. Gem Valley is one of the northernmost valleys along the Wasatch Range which extends approximately south. The valley floor has an elevation roughly, while the surrounding mountain peaks have an elevation ranging from about. It is accessed primarily by Idaho State Highway 34 from the south, and U.S. Route 30 from the east and west.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
It is accessed primarily by Idaho State Highway 34 from the south, and U.S. Route 30 from the east and west. Most of the valley is in Caribou County, and portions extend into Franklin County to the south, and Bannock County to the north. The Bear River runs through the valley as well as several small streams. Grace and Bancroft are the only incorporated towns in Gem Valley.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Grace and Bancroft are the only incorporated towns in Gem Valley. However, there are several unincorporated communities including Cleveland, Thatcher, Lago, Bench, Niter, Dugway, Turner, Stanley, Lund, Tenmile, and Chesterfield. Some of these were once pioneer-era towns and settlements, but the name now denotes a region of the valley, rather than a town with defined boundaries. Geology.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Trilobite fossils can often be found in local shale deposits. In the northern end of the valley, limestone is commercially mined and processed into lime which is used elsewhere in concrete and steel production. Much of the soil in Gem Valley is dark, nitrogen rich volcanic soil. This soil type is ideal for farming, particularly potatoes and grain. Clay sediment is also common.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Much of the soil in Gem Valley is dark, nitrogen rich volcanic soil. This soil type is ideal for farming, particularly potatoes and grain. Clay sediment is also common. The Wasatch Fault is visible throughout many parts of the valley due to the sharp displacement that creates a small bench at the foot of the mountains. Mild to moderate earthquakes have been reported to originate at the fault.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Notable events. The arena was also venue to many types of concerts, including Nirvana who played there on the 30th October 1993, music festivals, trade shows and conventions, formerly including the annual Dayton Hamvention (which, starting in 2017, is held at the Greene County Fairgrounds and Expo Center). The Miami Valley Home Improvement Show was also held annually here.

Geographic entities mentioned:
surface_form: Miami Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.768611
lon: -84.189676
Location. Tukvar Tea Garden is located at. Area overview. The map alongside shows the northern portion of the Darjeeling Himalayan hill region. Kangchenjunga, which rises with an elevation of is located further north of the area shown. Sandakphu, rising to a height of, on the Singalila Ridge, is the highest point in West Bengal.

Geographic entities mentioned:
surface_form: Kangchenjunga
instance_of: Mountain
countries: India
Nepal
coordinates: lat: 27.7
lon: 88.133333
Kennedy Glacier (Antarctica). Kennedy Glacier () is a steep glacier, long, flowing east from Kottmeier Mesa into the upper Matterhorn Glacier, Victoria Land, Antarctica.

Geographic entities mentioned:
surface_form: Kottmeier Mesa
instance_of: Landform
coordinates: lat: -77.65
lon: 162.15
Menelik, realizing that resistance was futile, was forced to submit to Yohannes. Escaping influence from Yohannes, Menelik moved his capital south from Ankober to Mount Entoto in 1884. There, his wife Taytu Betul was attracted to a nearby spring known as Finfinne by the local Oromo inhabitants. In the spring of 1886, Menelik chose the site for Addis Ababa, his future capital.

Geographic entities mentioned:
surface_form: Mount Entoto
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 9.1155555555556
lon: 38.772222222222
Agriculture. In 2014 Toyama contributed approximately 2.5% of Japan's rice production and
makes use of abundant water sources originating from Mount Tate. It also has many fisheries along its Sea of Japan coastline. Manufacturing.

Geographic entities mentioned:
surface_form: Mount Tate
instance_of: Mountain
countries: Japan
coordinates: lat: 36.575833333333
lon: 137.61972222222
In Britain this period is called the
&quot;Windermere interstadial&quot; because continuous deposits around the (Lake) Windermere region show the changing environment at this time from an alpine, herbaceous, covering to one which included woody plants such as tree birch and juniper.

Geographic entities mentioned:
surface_form: Windermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.358333333333
lon: -2.9361111111111
Serra da Boa Vista, Ceará. The Serra da Boa Vista is a mountain located in the central interior of Ceará. It is located in the municipality of Itatira with a long-distance view and lush landscapes of the semi-arid region, thus named &quot;Serra da Boa Vista&quot;. Location.

Geographic entities mentioned:
surface_form: serra da boa vista
instance_of: Mountain
countries: Brazil
surface_form: serra da boa vista
instance_of: Mountain
countries: Brazil
coordinates: lat: -4.4101
lon: -39.3927
And saw that there was a water hole, a spring, which was the main reason of the first people to climb. From generation to generation, the Serra da Boa Vista was always seen as a great place to visit and even today, young and old climb even in as a mountain sport. Climate and vegetation. The climate is tropical, hot and semi-arid.

Geographic entities mentioned:
surface_form: serra da boa vista
instance_of: Mountain
countries: Brazil
surface_form: serra da boa vista
instance_of: Mountain
countries: Brazil
coordinates: lat: -4.4101
lon: -39.3927
The name of the river is based on the Evenk word &quot;tagin&quot; (тагин), meaning &quot;swamp&quot;. Course. The Tyugyuene is a left tributary of the Lena. It has its origin at the confluence of the long Ysyakh-Yuryage and Kupsuyu-Yuryakh streams, at an altitude of about in the northeastern part of the Lena Plateau, southwest of the abandoned village of Abaranda.

Geographic entities mentioned:
surface_form: Lena Plateau
instance_of: Plateau
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.75
lon: 125
Talla Castle. Talla Castle, also known as Inch Talla or Inchtalla Castle, was a 15th-century castle on Inchtalla upon Lake of Menteith, Scotland. The castle was built by Malise Graham, Earl of Mentieth starting in 1427.

Geographic entities mentioned:
surface_form: Lake of Menteith
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.176666666667
lon: -4.2941666666667
These specimens were discovered in the Grenzbitumenzone of Monte San Giorgio, a UNESCO World Heritage Site on the Swiss-Italian border. Also known as the Besano Formation in Italy, the Grenzbitumenzone has produced many well-preserved fossils from the Anisian-Ladinian boundary within the Middle Triassic. Description.

Geographic entities mentioned:
surface_form: Monte San Giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
Paleoecology. &quot;A. italicus&quot; was found in the Middle Triassic of Switzerland and Italy, with most specimens recovered from sites on Monte San Giorgio. It lived alongside many other fish and marine reptiles, including two other genera of thalattosaurs: &quot;Clarazia&quot; and &quot;Hescheleria.&quot;

Geographic entities mentioned:
surface_form: Monte San Giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
Königsruhe. Königsruhe (also &quot;Gut Königsruhe&quot; i.e. Königsruhe Estate) is a small settlement in the Bode Gorge in the Harz Mountains of Germany, south of the town of Thale in Saxony-Anhalt. Location. Königsruhe lies in the &quot;Hirschgrund&quot; (&quot;Stag Bottom&quot;) immediately next to the River Bode, a mountain river that has cut deeply into the surrounding mountains at this point.

Geographic entities mentioned:
surface_form: Bode Gorge
instance_of: Valley
countries: Germany
coordinates: lat: 51.735555555556
lon: 11.009722222222
Puʻu Hawaiʻiloa. Puʻu Hawaiʻiloa is a cinder cone located in Honolulu County, Hawaii on the Mokapu Peninsula. Much like neighboring Ulupaʻu Crater. it formed as a vent of the Koʻolau Range during the Honolulu Volcanic Series. The material of the cone is nepheline basalt. Puʻu Hawaiʻiloa is used by Marine Corps Base Hawaii and the Wailuku Community Center is next to it.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
surface_form: puʻu hawaiʻiloa
instance_of: Mountain
countries: United States
coordinates: lat: 21.447777777778
lon: -157.75666666667
Puʻu Hawaiʻiloa. Puʻu Hawaiʻiloa is a cinder cone located in Honolulu County, Hawaii on the Mokapu Peninsula. Much like neighboring Ulupaʻu Crater. it formed as a vent of the Koʻolau Range during the Honolulu Volcanic Series. The material of the cone is nepheline basalt. Puʻu Hawaiʻiloa is used by Marine Corps Base Hawaii and the Wailuku Community Center is next to it.

Geographic entities mentioned:
surface_form: puʻu hawaiʻiloa
instance_of: Mountain
countries: United States
coordinates: lat: 21.447777777778
lon: -157.75666666667
It occurs only in China, with a wide range north to Shandong Province and south to Guangdong Province. The type locality is Jiangsu Province, Wuxi, Tai Lake and Gaoyou Lake. It has also been recorded from Fujian Province, Fuzhou, Minhou County, Shangan Town, Tao River; Shandong Province, Weishan Lake; Hubei Province, Wuhan, estuary of Han River; and Guangdong Province, Shenzhen River. Comparison.

Geographic entities mentioned:
surface_form: Tai Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 31.166666666667
lon: 120.15
surface_form: Gaoyou Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 32.83333333
lon: 119.33333333
The Hampton Roads Beltway extends on a long loop through the region, crossing the harbor on two toll-free bridge-tunnel facilities. These crossings are the Hampton Roads Bridge-Tunnel between Phoebus in Hampton and Willoughby Spit in Norfolk and the Monitor-Merrimac Memorial Bridge-Tunnel between Newport News and Suffolk. The Beltway connects with another Interstate highway and three arterial U.S.

Geographic entities mentioned:
surface_form: Willoughby Spit
instance_of: Landform
countries: United States
coordinates: lat: 36.967
lon: -76.282472222222
Knipowitschia mermere. &quot;Knipowitschia mermere&quot; is a species of fresh water goby endemic to Lake Marmara and the associated basin of the River Gediz in Turkey where it can be found in shallow, poorly oxygenated water with plentiful weed growth. This species can reach a length of TL. Mermere

Geographic entities mentioned:
surface_form: Lake Marmara
instance_of: Lake
countries: Turkey
coordinates: lat: 38.6166
lon: 28.0155
He built a tower on top of the hill and charged visitors to picnic and climb the tower. Originally known as Stoney Hill, the hill was later named Government Hill, after the government teams that used it for surveying. In 1870, the Army Signal Corps built a signal station to relay data about approaching storms from Pikes Peak, Colorado, to Great Lakes ports. Pioneering meteorologist Increase A.

Geographic entities mentioned:
surface_form: Pikes Peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.840555555556
lon: -105.04416666667
Definition. The term Bregenz Forest Mountains refers to the range according to the Alpine Club classification of the Eastern Alps (AVE); the term Bregenz Forest, by contrast, refers to a landscape or region which is part of the Bregenzer Ache basin area. As a result, the Bregenz Forest Mountains and the Bregenz Forest are not conterminous.

Geographic entities mentioned:
surface_form: Bregenz Forest
instance_of: Valley
countries: Austria
coordinates: lat: 47.3728
lon: 9.91278
Most of the area is shaped by a Mittelgebirge character with extended forests and Alpine pastures, except for small High Alpine region in the southeast. The Bregenzerwald mountain range is located in the far northwest of the Eastern Alps, east of the lower Alpine Rhine Valley and southeast of Lake Constance. It lies entirely within the Austrian state of Vorarlberg and dominates its northern half.

Geographic entities mentioned:
surface_form: Rhine Valley
instance_of: Valley
countries: Switzerland
Austria
Liechtenstein
coordinates: lat: 47.07013888888889
lon: 9.483347222222223