Sarmila/GeoWiki-Features huggingface dataset:
The Chok were a community assimilated by the Pokotozek, their traditions state that there 'always were two original Suk tribes living on the Elgeyo Escarpment'. They further state that 'while the Suk nation was being evolved in the mountains of the Elgeyo escarpment the Kerio Valley was occupied by the Sambur. Conflict with Oropom at Cherangani and Elgon.

Geographic entities mentioned:
surface_form: Kerio Valley
instance_of: Valley
countries: Kenya
coordinates: lat: 0.6401
lon: 35.6086
Conflict with Oropom at Cherangani and Elgon. The Pokotozek finding that they were no longer facing a formidable tribal grouping to the north and west of Baringo, themselves expanded in that direction, expelling other Oropom from the Cherangany mountains and further west right up to the slopes of Mt Elgon hence limiting Turkana southern movement.

Geographic entities mentioned:
surface_form: Cherangany mountains
instance_of: Mountain
countries: Kenya
coordinates: lat: 1.251655
lon: 35.450478
Establishment of the Sebei. At Mount Elgon, a section of the Pokotozek formed into the people today known as the Sebei. On arriving at Mt Elgon, the Sebei-Pokotozek found Tepes people who were originally from Mount Kadam in Karamoja residing at a place later known as Entepes (present-day Endebess).

Geographic entities mentioned:
surface_form: Mount Elgon
instance_of: Mountain
countries: Uganda
Kenya
coordinates: lat: 1.1185
lon: 34.5265
Establishment of the Sebei. At Mount Elgon, a section of the Pokotozek formed into the people today known as the Sebei. On arriving at Mt Elgon, the Sebei-Pokotozek found Tepes people who were originally from Mount Kadam in Karamoja residing at a place later known as Entepes (present-day Endebess).

Geographic entities mentioned:
surface_form: Mount Kadam
instance_of: Mountain
countries: Uganda
coordinates: lat: 1.7630555555556
lon: 34.709166666667
Ascuta monowai. &quot;Ascuta monowai&quot; is a species of Orsolobidae. The species is endemic to New Zealand. Taxonomy. This species was described in 1985 by Ray Forster and Norman Platnick from a single female specimen collected at Lake Monowai. The species name refers to the locality of the holotype. The holotype is stored at Otago Museum. Description. The female is recorded at in length.

Geographic entities mentioned:
surface_form: Lake Monowai
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.866666666667
lon: 167.45
Alban people. The Albans were Latins from the ancient city of Alba Longa, southeast of Rome. Some of Rome's prominent patrician families such as the Julii, Servilii, Quinctii, Geganii, Curiatii and Cloelii were of Alban descent. Origins. Based on limited archaeological evidence, experts say the Alban tribe inhabited the long ridge between the modern-day Lake Albano and Monte Cavo. Power in Latium.

Geographic entities mentioned:
surface_form: Monte Cavo
instance_of: Mountain
countries: Italy
coordinates: lat: 41.751666666667
lon: 12.71
Religious customs. However, Pliny and others generally agree that the communities of Latium gathered at Alba Longa for sacrificial rites. Every year in the spring, the tribes would congregate on &quot;Mons Albanus&quot; (Monte Cavo) to worship Iuppiter Latiaris. The festival was known as &quot;Feriae Latinae&quot;.

Geographic entities mentioned:
surface_form: Monte Cavo
instance_of: Mountain
countries: Italy
coordinates: lat: 41.751666666667
lon: 12.71
History. In 1516, Portuguese commander Dom Joao de Monoy entered the Mahim Creek and defeated the commander of Mahim fort. The fort was the site of frequent skirmishes between the Portuguese and a Gujarati ruler before the island of Mahim was appropriated from Bahadur Shah of Gujarat by the Portuguese in 1534. In 1661, the Portuguese ceded the island of Mahim as dowry to Charles II of England.

Geographic entities mentioned:
surface_form: Mahim Creek
instance_of: Watercourse
countries: India
coordinates: lat: 19.052601
lon: 72.8393824
Conical Hill (Sri Lanka). Conical Hill is a mountain situated in the Nuwara Eliya District of Sri Lanka. It is the 9th highest mountain in Sri Lanka.

Geographic entities mentioned:
surface_form: conical hill (sri lanka)
instance_of: Mountain
countries: Sri Lanka
coordinates: lat: 6.9125
lon: 80.77583333333334
Conical Hill (Sri Lanka). Conical Hill is a mountain situated in the Nuwara Eliya District of Sri Lanka. It is the 9th highest mountain in Sri Lanka.

Geographic entities mentioned:
surface_form: conical hill
instance_of: Mountain
countries: Sri Lanka
coordinates: lat: 6.9125
lon: 80.77583333333334
Her ashes were interred with Alexander's grave exactly one year, to the hour, after his burial. Today, they rest together near the top of their &quot;beautiful mountain&quot; of their estate overlooking Bras d'Or Lake, under a simple boulder of granite. Deaf to Bell's utterances. Hubbard was the indirect source of her husband's early commercial success after his creation of the telephone. The U.S.

Geographic entities mentioned:
surface_form: Bras d'Or Lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.860277777778
lon: -60.778888888889
Site overview. Camp Withycombe is state land under the responsibility of the Oregon Military Department (OMD), a state agency, and is home to several Oregon Army National Guard (ORARNG) military units under the jurisdiction of federal and state military authorities. Camp Withycombe is a 77+-acre site that is located at the foot of Mount Talbert southeast of Portland.

Geographic entities mentioned:
surface_form: Mount Talbert
instance_of: Mountain
countries: United States
coordinates: lat: 45.4268
lon: -122.552
In its early years, the museum contained numerous art collections, including several works by the painter Johan Christian Dahl, cultural artefacts, and craftwork items. In 1831, the museum moved from its location in the Seminarium Fredericianum building near Bergen Cathedral School (&quot;Bergen katedralskole&quot;), to a new building southwest of Lille Lungegårdsvannet.

Geographic entities mentioned:
surface_form: Lille Lungegårdsvannet
instance_of: Lake
countries: Norway
coordinates: lat: 60.3904
lon: 5.3284
It crossed the North Channel into Northeastern Ontario near Sault Ste. Marie, where it quickly developed into a derecho line. As it crossed Manitoulin Island just southeast of Sault Ste. Marie in Lake Huron, numerous trees were uprooted and some homes sustained heavy damage. An official wind gust of 128 km/h (80 mph) was recorded at the Killarney weather station on the north shore of Lake Huron.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Ottawa Valley, Eastern Ontario and Southwestern Quebec. Through the next two hours the storm entered the Upper Ottawa Valley affecting places in Renfrew County such as Barry's Bay, Deep River, Cobden, Petawawa and Pembroke. There were numerous reports of damage, particularly blown-off or damaged roofs. After crossing the Pembroke area, the derecho started to lose some steam.

Geographic entities mentioned:
surface_form: Ottawa Valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
German plans did call for re-making the strategically located city of Belgrade as a &quot;fortress-city of the Reich&quot; (&quot;Reichsfestung Belgrad&quot;) to ensure control over the Iron Gates, populated only by Germans. The city's possible renaming to &quot;Prinz-Eugen-Stadt&quot; was also discussed. War crimes against Jews and Roma. The region was ruled by the German army.

Geographic entities mentioned:
surface_form: Iron Gates
instance_of: Valley
countries: Serbia
Romania
coordinates: lat: 44.671111111111
lon: 22.529722222222
Valle Maggia. Valle Maggia (English, &quot;Maggia Valley&quot;) is an alpine valley in the Vallemaggia district of canton of Ticino, the Italian-speaking canton of Switzerland. The valley is formed by the river Maggia and is situated between the Centovalli and Lago Maggiore as well as the Valle Verzasca in the East. Geography.

Geographic entities mentioned:
surface_form: Valle Verzasca
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.2582
lon: 8.8350694444444
surface_form: verzasca
instance_of: Watercourse
countries: Switzerland
coordinates: lat: 46.3908
lon: 8.74333
surface_form: valle verzasca
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.2582
lon: 8.8350694444444
surface_form: verzasca
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.2582
lon: 8.8350694444444
Geography. The Maggia valley has a spatial extension of, equal to one-fifth of the canton of Ticino. It is the largest valley of the canton and one of the widest within the Alps' south side. The valley is formed by the river Maggia, whose source is the Cristallina peak in Val Sambuco (Lavizzara). The river runs through the valley down to Ascona, where it pours into the Lake Maggiore.

Geographic entities mentioned:
surface_form: Cristallina
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.464722222222
lon: 8.5369444444444
surface_form: cristallina
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.464722222222
lon: 8.5369444444444
Geography. The Maggia valley has a spatial extension of, equal to one-fifth of the canton of Ticino. It is the largest valley of the canton and one of the widest within the Alps' south side. The valley is formed by the river Maggia, whose source is the Cristallina peak in Val Sambuco (Lavizzara). The river runs through the valley down to Ascona, where it pours into the Lake Maggiore.

Geographic entities mentioned:
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
The next side valley is the short Valle di Lodano. The next tributary to the Maggia from the West is the Rovana which joins in Cevio. Upstream it forms the Val Rovana, which at Cerentino leads up into Valle di Bosco/Gurin and Valle di Campo. The upper Maggia valley beyond Bignasco splits into two dead ends, the two major glacial troughs of Val Bavona in the West and Val Lavizzara in the East.

Geographic entities mentioned:
surface_form: Valle di Campo
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.28536
lon: 8.50888
surface_form: valle di campo
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.28536
lon: 8.50888
The side valley West of Val Bavona is the Val Canegia. To the Southwest of the Maggia Valley are Valle Onsernone and Centovalli. Parallelling the Maggia Valley in the East is the Valle Verzasca. The geographical configuration of the Maggia valley's territory goes from above sea level of Ponte Brolla to above s.l. of the Basòdino peak, with a height difference equal to in just as the crow flies.

Geographic entities mentioned:
surface_form: Valle Verzasca
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.2582
lon: 8.8350694444444
surface_form: verzasca
instance_of: Watercourse
countries: Switzerland
coordinates: lat: 46.3908
lon: 8.74333
surface_form: valle verzasca
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.2582
lon: 8.8350694444444
surface_form: verzasca
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.2582
lon: 8.8350694444444
To the Southwest of the Maggia Valley are Valle Onsernone and Centovalli. Parallelling the Maggia Valley in the East is the Valle Verzasca. The geographical configuration of the Maggia valley's territory goes from above sea level of Ponte Brolla to above s.l. of the Basòdino peak, with a height difference equal to in just as the crow flies. Climate.

Geographic entities mentioned:
surface_form: Basòdino
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 46.411555555556
lon: 8.4684333333333
Within the Maggia valley there's only 1,8% of the Ticinese population, even if it occupies 20% of the cantonal territory. The demographic density is, thus, very low: 9 inhabitants per square kilometre. From 1814 to 1824 a road (via cantonale) was built from Locarno on the Lake Maggiore to Bignasco, which broke the valley's isolation. In 1907, a railway line Locarno-Ponte Brolla-Bignasco was built.

Geographic entities mentioned:
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
Over time, the river has flooded and eroded valuable areas of cultivation, partly due to extensive woodcutting, so the lower Maggia valley is broad, but it is flanked by steep granite walls. The Maggia valley in its strict sense extends from Ponte Brolla in the South to Bignasco in the North. Going North the first side valley is Northeast of the village of Maggia, the Valle del Salto.

Geographic entities mentioned:
surface_form: sense
instance_of: Watercourse
countries: Switzerland
coordinates: lat: 46.906
lon: 7.23389
The Maggia valley in its strict sense extends from Ponte Brolla in the South to Bignasco in the North. Going North the first side valley is Northeast of the village of Maggia, the Valle del Salto. The next side valley is the short Valle di Lodano. The next tributary to the Maggia from the West is the Rovana which joins in Cevio.

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
When the Helvetian Republic was founded in 1798, the Valle Maggia became part of the Canton Lugano; In 1803, Napoleon gave the Republic a federal structure and Ticino became its own autonomous canton with Vallemaggia as its own district and Cevio as the capital.

Geographic entities mentioned:
surface_form: vallemaggia
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.25
lon: 8.7
surface_form: valle maggia
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.25
lon: 8.7
From the Middle Ages onwards people had emigrated to Locarno and the Sottoceneri. Population probably reached its peak in the middle of the 18th century, after which a first wave of bricklayers, stonemasons, grooms, traders and artists emigrated on a seasonal basis and for longer periods of time. This mitigated population pressure and enabled relative prosperity.

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
In 1398, the Vallemaggia, the Verzasca Valley and Mergoscia refused to pay royalties to the Locarno nobility, who had fiefs in these regions; In 1403, the valleys formally separated from Locarno and founded an independent judicial district with a 42-member general council and own land law (statuti) centered in Cevio; various conflicts between the local valleys characterized their coexistence.

Geographic entities mentioned:
surface_form: verzasca
instance_of: Watercourse
countries: Switzerland
coordinates: lat: 46.3908
lon: 8.74333
surface_form: verzasca
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.2582
lon: 8.8350694444444
surface_form: vallemaggia
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.25
lon: 8.7
The largest municipality is Maggia, at 323 metres altitude. Cevio at 418 metres is the former administrative centre and Gurin at 1503 metres the only German speaking community in Ticino in the upper Valle di Bosco/Gurin. Bignasco at 443 metres is a village at the junction of Maggia and Bavona valley. From the Middle Ages onwards people had emigrated to Locarno and the Sottoceneri.

Geographic entities mentioned:
surface_form: bavona valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.3861
lon: 8.5266
The next side valley is the short Valle di Lodano. The next tributary to the Maggia from the West is the Rovana which joins in Cevio. Upstream it forms the Val Rovana, which at Cerentino leads up into Valle di Bosco/Gurin and Valle di Campo. The upper Maggia valley beyond Bignasco splits into two dead ends, the two major glacial troughs of Val Bavona in the West and Val Lavizzara in the East.

Geographic entities mentioned:
surface_form: val bavona
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.3861
lon: 8.5266
The latter is, in turn, divided in the side valleys of Valle di Peccia in the West, Val di Prato in the East as cul-de sacs, and Val Sambuco. The side valley West of Val Bavona is the Val Canegia. To the Southwest of the Maggia Valley are Valle Onsernone and Centovalli. Parallelling the Maggia Valley in the East is the Valle Verzasca.

Geographic entities mentioned:
surface_form: val bavona
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.3861
lon: 8.5266
At the beginning of the 21st century, the Val Rovana, where the population had declined by 75% between 1860 and 1980, seemed to become a holiday resort, similar to the Val Bavona. The Valle Lavizzara was a little less affected by the population decline. Within the Maggia valley there's only 1,8% of the Ticinese population, even if it occupies 20% of the cantonal territory.

Geographic entities mentioned:
surface_form: val bavona
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.3861
lon: 8.5266
The latter is, in turn, divided in the side valleys of Valle di Peccia in the West, Val di Prato in the East as cul-de sacs, and Val Sambuco. The side valley West of Val Bavona is the Val Canegia. To the Southwest of the Maggia Valley are Valle Onsernone and Centovalli. Parallelling the Maggia Valley in the East is the Valle Verzasca.

Geographic entities mentioned:
surface_form: valle onsernone
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.200211
lon: 8.648815
Valle Maggia. Valle Maggia (English, &quot;Maggia Valley&quot;) is an alpine valley in the Vallemaggia district of canton of Ticino, the Italian-speaking canton of Switzerland. The valley is formed by the river Maggia and is situated between the Centovalli and Lago Maggiore as well as the Valle Verzasca in the East. Geography.

Geographic entities mentioned:
surface_form: vallemaggia
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.25
lon: 8.7
surface_form: valle maggia
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.25
lon: 8.7
They returned it to Milan in 1422 and finally to the Rusca family in 1439. Around 1430, the Lavizzaratal valley was legally separated from Valle Maggia. In 1513, the Helvetians occupied the valley, and for the next 300 years, from 1513 to 1798, Vallemaggia was one of the bailiwicks of the twelve Helvetian cantons; its German name was &quot;Meiental&quot; or &quot;Mainthal&quot;.

Geographic entities mentioned:
surface_form: vallemaggia
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.25
lon: 8.7
It was divided into the two valleys of Vallemaggia and Lavizzara, but only one fiscal head and one chief officiated and only for 2 years each; The latter chose his place of residence (in Cevio or Sornico) himself, but had to regularly reside in the other main town to assess the litigation, in difficult cases with the help of local judges.

Geographic entities mentioned:
surface_form: vallemaggia
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.25
lon: 8.7
The Valle Lavizzara defended its self-reliance against Vallemaggia. It sabotaged the attempts of some of the bailiffs and of the annual accounts statute to settle the court centrally in Cevio or to overturn the directors.

Geographic entities mentioned:
surface_form: vallemaggia
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.25
lon: 8.7
Valle Maggia. Valle Maggia (English, &quot;Maggia Valley&quot;) is an alpine valley in the Vallemaggia district of canton of Ticino, the Italian-speaking canton of Switzerland. The valley is formed by the river Maggia and is situated between the Centovalli and Lago Maggiore as well as the Valle Verzasca in the East. Geography.

Geographic entities mentioned:
surface_form: valle maggia
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.25
lon: 8.7
They returned it to Milan in 1422 and finally to the Rusca family in 1439. Around 1430, the Lavizzaratal valley was legally separated from Valle Maggia. In 1513, the Helvetians occupied the valley, and for the next 300 years, from 1513 to 1798, Vallemaggia was one of the bailiwicks of the twelve Helvetian cantons; its German name was &quot;Meiental&quot; or &quot;Mainthal&quot;.

Geographic entities mentioned:
surface_form: valle maggia
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.25
lon: 8.7
The creation of jobs slowed the rural exodus. Economy. Since the Middle Ages, the economy has been based on field (cereals, potatoes and linen) and viticulture and pasture management. For many centuries cheese was exported from Valle Maggia. Forests were often overused as a resource, which polluted the environment.

Geographic entities mentioned:
surface_form: valle maggia
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.25
lon: 8.7
It is situated in the Cusco Region, Canchis Province, Pitumarca District, and in the Quispicanchi Province, Marcapata District. Yayamari lies northeast of Sibinacocha, north of the lake named Amayuni and northwest of Huila Aje and Condoriquiña. Elevation. Other data from available digital elevation models: SRTM yields 6016 metres, ASTER 5984 metres, ALOS 6023 metres and TanDEM-X 6071 metres.

Geographic entities mentioned:
surface_form: Sibinacocha
instance_of: Lake
countries: Peru
coordinates: lat: -13.856666666667
lon: -71.025
surface_form: condoriquiña
instance_of: Mountain
countries: Peru
coordinates: lat: -13.825
lon: -70.91972222
surface_form: huila aje
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7853
lon: -70.9694
surface_form: yayamari
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7667
lon: -70.9817
The height of the nearest key col is 5327 meters, leading to a topographic prominence of 722 meters. Yayamari is considered a Mountain Subgroup according to the &quot;Dominance System&quot; and its dominance is 11.94%. Its parent peak is Alcamarinayoc and the Topographic isolation is 14.4 kilometers. First Ascent.

Geographic entities mentioned:
surface_form: Alcamarinayoc
instance_of: Mountain
countries: Peru
coordinates: lat: -13.69972222
lon: -71.09472222
surface_form: alcamarinayoc
instance_of: Mountain
countries: Peru
coordinates: lat: -13.69972222
lon: -71.09472222
Yayamari. Yayamari (other names: Ambrocca or Ambroja in Hispanicized spellings or Montura) is a mountain in the Vilcanota mountain range in the Andes of Peru, about high. It is situated in the Cusco Region, Canchis Province, Pitumarca District, and in the Quispicanchi Province, Marcapata District.

Geographic entities mentioned:
surface_form: ambroja
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7667
lon: -70.9817
surface_form: yayamari
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7667
lon: -70.9817
surface_form: montura
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7667
lon: -70.9817
Yayamari. Yayamari (other names: Ambrocca or Ambroja in Hispanicized spellings or Montura) is a mountain in the Vilcanota mountain range in the Andes of Peru, about high. It is situated in the Cusco Region, Canchis Province, Pitumarca District, and in the Quispicanchi Province, Marcapata District.

Geographic entities mentioned:
surface_form: yayamari
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7667
lon: -70.9817
The height of the nearest key col is 5327 meters, leading to a topographic prominence of 722 meters. Yayamari is considered a Mountain Subgroup according to the &quot;Dominance System&quot; and its dominance is 11.94%. Its parent peak is Alcamarinayoc and the Topographic isolation is 14.4 kilometers. First Ascent.

Geographic entities mentioned:
surface_form: yayamari
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7667
lon: -70.9817
Soppulsan. Soppulsan is a mountain of South Korea. It has an elevation of 1,118 metres.

Geographic entities mentioned:
surface_form: soppulsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 37.9
lon: 128.133
The Little Camas Fire at, in the Cascades south of Leavenworth, Washington, started on July 5 and reached over 300 acres. It caused the evacuation of a bible camp. Over 440 firefighters and three helicopters were sent to contain it. The Vulcan Mountain Fire at Vulcan Mountain in Ferry County grew to over 20 acres around July 13, before being contained.

Geographic entities mentioned:
surface_form: Vulcan Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.989444444444
lon: -118.64888888889
Larama Quta. Larama Quta (Aymara &quot;larama&quot; blue, &quot;quta&quot; lake, &quot;blue lake&quot;, Hispanicized spelling &quot;Laramacota&quot;) is a mountain in the Andes of southern Peru. It is situated in the Moquegua Region, General Sánchez Cerro Province, Ichuña District, northeast of Jukumarini Lake.

Geographic entities mentioned:
surface_form: larama quta
instance_of: Mountain
countries: Peru
coordinates: lat: -16.3269
lon: -70.3628
Larama Quta. Larama Quta (Aymara &quot;larama&quot; blue, &quot;quta&quot; lake, &quot;blue lake&quot;, Hispanicized spelling &quot;Laramacota&quot;) is a mountain in the Andes of southern Peru. It is situated in the Moquegua Region, General Sánchez Cerro Province, Ichuña District, northeast of Jukumarini Lake.

Geographic entities mentioned:
surface_form: larama quta
instance_of: Mountain
countries: Peru
coordinates: lat: -16.3269
lon: -70.3628
surface_form: laramacota
instance_of: Mountain
countries: Peru
coordinates: lat: -16.3269
lon: -70.3628
History. The village of Antares began as a railroad siding. The Atlantic and Pacific Railroad was laying tracks through the area in 1883 and had to reroute around the Peacock Mountains, diverting south of the mountains to the easier gradient through nearby Hackberry; when continuing west, the gradient was lower in the Hualapai Valley to the north of Hackberry, where Antares now lies.

Geographic entities mentioned:
surface_form: Hualapai Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.57472222
lon: -113.93611111
It is located in the Puno Region, Carabaya Province, on the border of the districts Corani and Ollachea. Macho Ritti lies north-west of the lakes Mancacocha and Jomercocha and north of the mountain Ananta.

Geographic entities mentioned:
surface_form: mancacocha
instance_of: Lake
countries: Peru
coordinates: lat: -12.0281
lon: -75.7394
surface_form: ananta
instance_of: Mountain
countries: Peru
coordinates: lat: -13.81388889
lon: -70.62055556
surface_form: ananta
instance_of: Mountain
countries: Peru
coordinates: lat: -15.8128
lon: -71.6825
surface_form: ananta
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7678
lon: -70.8147
Macho Ritti. Macho Ritti (possibly from Quechua &quot;machu&quot; old, old person, &quot;rit'i&quot; snow, &quot;old snow (mountain)&quot;) is a mountain in the Vilcanota mountain range in the Andes of Peru, about high. It is located in the Puno Region, Carabaya Province, on the border of the districts Corani and Ollachea.

Geographic entities mentioned:
surface_form: macho ritti
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7944
lon: -70.6206
2011 Shoal Creek Valley–Ohatchee tornado. In the evening hours of April 27, 2011, a large and violent EF4 tornado devastated the northern portion of Ohatchee and the beachside homes on the Coosa River and many other communities in Eastern Alabama.

Geographic entities mentioned:
surface_form: Coosa River
instance_of: Watercourse
countries: United States
coordinates: lat: 32.4862464
lon: -86.2777475
Clair, northwestern Calhoun and southern Etowah counties. The tornado rapidly strengthened after it crossed County Road 26, producing EF4 damage to site-built homes, mobile homes and trees. As it approached the Coosa River, the tornado expanded to its maximum width, approximately one mile (1.6 km). Crossing the river, the tornado exited St.

Geographic entities mentioned:
surface_form: Coosa River
instance_of: Watercourse
countries: United States
coordinates: lat: 32.4862464
lon: -86.2777475
Fortifications protected at least a few Germanic settlements. Unlike the Romans, however, the Germanii did not use mortar for their construction at that time. Among the best-known hill settlements in Germany are the Runder Berg near Bad Urach and the Gelbe Burg near Dittenheim. Sweden. In Sweden, hillforts are fortifications from the Iron Age which may have had several functions.

Geographic entities mentioned:
surface_form: Runder Berg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.489722222222
lon: 9.365
The Big Pine Band of Owens Valley Paiute Shoshone Indians of the Big Pine Reservation bases their tribal headquarters there. Geography. Big Pine is located in the Owens Valley of California between the Sierra Nevada and the White Mountains, just west of the Owens River upstream of its diversion into the Los Angeles Aqueduct. It lies on U.S.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
It lies on U.S. Route 395, the main north–south artery through the Owens Valley, connecting the Inland Empire to Reno, Nevada. US 395 also connects Big Pine to Los Angeles via State Route 14 through Palmdale. To the East, CA route 168 crosses the White Mountains over Westgard Pass to the basin and range province of Nevada, while Death Valley Road leads to Death Valley.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Penguin Point lies on the south-eastern coast of Seymour Island, in the James Ross Island group, near the north-eastern extremity of the Antarctic Peninsula. The Argentine Marambio Base is about 8 km to the north-east. A ridge of exposed dark rock named Blackrock Ridge runs west-southwest–east-northeast, 1.5 nautical miles (3 km) north of Penguin Point. Important Bird Area.

Geographic entities mentioned:
surface_form: Blackrock Ridge
instance_of: Mountain
coordinates: lat: -64.2833
lon: -56.7167
This defeat combined with the Chinese resistance in the Second Sino-Japanese War, together with the signing of the German-Soviet non-aggression pact (which deprived the Army of the basis of its war policy against the USSR), moved the Imperial General Staff in Tokyo away from the policy of the North Strike Group favored by the Army, which wanted to seize Siberia for its resources as far as Lake Baikal.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Deane Hawkins. The site is located at the extreme northeast portion of Camp Smith and now sits within a secured perimeter fence line. Originally used in the later part of the Second World War as an R&R location, the site contains a small stone cabin and overlooks the southern coast of Oahu, from Diamond Head to Barber's Point, Hawaii.

Geographic entities mentioned:
surface_form: Diamond Head
instance_of: Mountain
countries: United States
coordinates: lat: 21.259722222222
lon: -157.81175
Pack River. The Pack River is a medium-sized river located in Northern Idaho. It is about long and drains a high mountainous area of the Idaho Panhandle's Rocky Mountains and Selkirk Mountains. The river flows into Lake Pend Oreille and is part of the Columbia River watershed via the Pend Oreille River. Course.

Geographic entities mentioned:
surface_form: Lake Pend Oreille
instance_of: Lake
countries: United States
coordinates: lat: 48.166666666667
lon: -116.33333333333
The river flows into Lake Pend Oreille and is part of the Columbia River watershed via the Pend Oreille River. Course. Its headwaters originate in the Selkirk Mountains, and flow in a southerly direction to the river's mouth at the northern tip of Lake Pend Oreille. It is the second largest tributary to the lake, after the Clark Fork River. Watershed. The Pack River basin drains approximately.

Geographic entities mentioned:
surface_form: Lake Pend Oreille
instance_of: Lake
countries: United States
coordinates: lat: 48.166666666667
lon: -116.33333333333
U.S. Route 5 borders the east side of East Rock while Interstate 91 crosses below Snake Rock to the south. The Metacomet Ridge extends west from East Rock as series of smaller, unnoteworthy traprock outcrops to West Rock Ridge; it extends east over another series of traprock outcrops to Saltonstall Mountain and Peter's Rock.

Geographic entities mentioned:
surface_form: West Rock Ridge
instance_of: Mountain
countries: United States
coordinates: lat: 41.380841666667
lon: -72.978319444444
surface_form: Saltonstall Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.324
lon: -72.8
surface_form: Peter's Rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.341944444444
lon: -72.853055555556
surface_form: east rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
East Rock. East Rock of south-central Connecticut, United States, with a high point of, is a long trap rock ridge located primarily in the neighborhood of East Rock on the north side of the city of New Haven.

Geographic entities mentioned:
surface_form: east rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
East Rock. East Rock of south-central Connecticut, United States, with a high point of, is a long trap rock ridge located primarily in the neighborhood of East Rock on the north side of the city of New Haven.

Geographic entities mentioned:
surface_form: east rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
surface_form: east rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
A prominent landscape feature and a popular outdoor recreation area with cliffs that rise over the city below, East Rock is part of the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, north through the Connecticut River Valley of Massachusetts to the Vermont border.

Geographic entities mentioned:
surface_form: east rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
East Rock is the central feature of East Rock Park, a municipal park owned by the city of New Haven along the New Haven-Hamden town line. Geography. East Rock, located in New Haven and Hamden, Connecticut, is long by wide at its widest point, although steepness of the terrain make the actual land area much larger.

Geographic entities mentioned:
surface_form: east rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
surface_form: east rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
East Rock is the central feature of East Rock Park, a municipal park owned by the city of New Haven along the New Haven-Hamden town line. Geography. East Rock, located in New Haven and Hamden, Connecticut, is long by wide at its widest point, although steepness of the terrain make the actual land area much larger.

Geographic entities mentioned:
surface_form: east rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
East Rock, located in New Haven and Hamden, Connecticut, is long by wide at its widest point, although steepness of the terrain make the actual land area much larger. Beside the high point, East Rock has three other distinct peaks: Whitney Peak, a sharp-sided pinnacle on the north side of the ridge; Indian Head, just south of the high point; and Snake Rock, the southern buttress of the ridge.

Geographic entities mentioned:
surface_form: east rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
C. Gilbert, is located at the base of the dam. On the summit of East Rock, clearly visible for miles below, is the Soldiers and Sailors Monument. The monument honors the residents of New Haven who gave their lives in the American Revolutionary War, the War of 1812, the Mexican War, and the Civil War.

Geographic entities mentioned:
surface_form: east rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
East Rock is located entirely within the 425-acre (172 ha) East Rock Park, managed by the city of New Haven, which maintains a seasonal automobile road that climbs to the summit of the ridge, a network of trails, an environmental center, and a rose garden. A number of recreation facilities are located at the southwest base of the ridge; these are also managed by the city.

Geographic entities mentioned:
surface_form: east rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
surface_form: east rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
A number of recreation facilities are located at the southwest base of the ridge; these are also managed by the city. The ridge is completely surrounded by the urban neighborhoods of New Haven and its metropolitan extension into south Hamden. East Rock lends its name to the nearby upscale East Rock neighborhood of New Haven, known for its Queen Anne and Victorian architecture. U.S.

Geographic entities mentioned:
surface_form: east rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
surface_form: east rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
The ridge is completely surrounded by the urban neighborhoods of New Haven and its metropolitan extension into south Hamden. East Rock lends its name to the nearby upscale East Rock neighborhood of New Haven, known for its Queen Anne and Victorian architecture. U.S. Route 5 borders the east side of East Rock while Interstate 91 crosses below Snake Rock to the south.

Geographic entities mentioned:
surface_form: east rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
The west side of East Rock drains into the Mill River thence to New Haven Harbor and Long Island Sound; the east side into the Quinnipiac River, thence to New Haven Harbor and Long Island Sound. Both rivers abut the base of the mountain. Geology.

Geographic entities mentioned:
surface_form: east rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
Both rivers abut the base of the mountain. Geology. East Rock is a fault-block ridge formed 200 million years ago during the Triassic and Jurassic periods and is composed of trap rock, known as basalt, if extrusive, or diabase, if intrusive. East Rock, being intrusive, is diabase.

Geographic entities mentioned:
surface_form: east rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
Geology. East Rock is a fault-block ridge formed 200 million years ago during the Triassic and Jurassic periods and is composed of trap rock, known as basalt, if extrusive, or diabase, if intrusive. East Rock, being intrusive, is diabase. Diabase is a dark colored rock, but the iron within it weathers to a rusty brown when exposed to the air, lending the ledges a distinct reddish appearance.

Geographic entities mentioned:
surface_form: east rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
Diabase is a dark colored rock, but the iron within it weathers to a rusty brown when exposed to the air, lending the ledges a distinct reddish appearance. Diabase frequently breaks into octagonal and pentagonal columns, creating a unique &quot;postpile&quot; appearance. Huge slopes made of fractured diabase scree are visible beneath many of the ledges of East Rock.

Geographic entities mentioned:
surface_form: east rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
At the foot of the mountain are located football, baseball, and soccer fields, tennis courts, basketball courts, and playgrounds. The Trowbridge Environmental Center is open Thursdays and Fridays from 10:00 am to 5:00 pm, and at least one Saturday a month for public programs; it offers displays and information about the geology and ecosystem of East Rock.

Geographic entities mentioned:
surface_form: east rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
Erosion and glacial abrasion over the subsequent 200 million years wore away the weaker sedimentary layers, under which the sill had intruded, at a faster rate than the diabase, leaving the abruptly tilted edges of the diabase sheets exposed, creating the distinct linear ridge and dramatic cliff faces visible today. Ecosystem. East Rock hosts a combination of microclimates unusual in New England.

Geographic entities mentioned:
surface_form: sill
instance_of: Mountain
countries: United States
coordinates: lat: 37.094377777778
lon: -118.50288333333
Whitney Peak and Lake Whitney (located at the western base of the mountain behind the dammed Mill River) are named after Eli Whitney, the inventor of the cotton gin and a former New Haven resident. The Eli Whitney Museum, a museum and workshop with hands-on projects and exhibits on Eli Whitney and A. C. Gilbert, is located at the base of the dam.

Geographic entities mentioned:
surface_form: lake whitney
instance_of: Lake
countries: United States
coordinates: lat: 41.352
lon: -72.911
In the first verse, its north–south extension is described by the way of the Eisack source and the &quot;Salurner Klause&quot;, a bottleneck which used to mark the border between the German and Italian-speaking area. The West–East extension is characterized by the mountain Ortler and the Sexten Dolomites.

Geographic entities mentioned:
surface_form: Ortler
instance_of: Mountain
countries: Italy
coordinates: lat: 46.508888888889
lon: 10.545
The West–East extension is characterized by the mountain Ortler and the Sexten Dolomites. In the following verses, various landmarks of South Tyrol such as the Schlern and the Rosengarten group are celebrated.

Geographic entities mentioned:
surface_form: Schlern
instance_of: Mountain
countries: Italy
coordinates: lat: 46.515
lon: 11.575555555556
Range. The Tooth Cave pseudoscorpion is only confirmed in two caves: Tooth Cave and Amber Cave, in Travis County, Texas. The caves span the Balcones Canyonlands, ranging from eastern to southeastern Edwards Plateau. Generally keeping to the caves, the Tooth Cave pseudoscorpions have a range of approximately 1 km from the caves before the environment becomes unsuitable for them to live.

Geographic entities mentioned:
surface_form: Edwards Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 30.3
lon: -99.6
Pope Francis accepted Scola's resignation on 7 July 2017 and appointed Bishop Mario Delpini as his successor. In retirement, Scola planned to live in Imberido, a village near Lake Annone. 2014 and 2015 Synod of Bishops.

Geographic entities mentioned:
surface_form: Lake Annone
instance_of: Lake
countries: Italy
coordinates: lat: 45.811944444444
lon: 9.3494444444444
The former governor of Ambon, Arnold de Vlamingh van Oudshoorn turned up in Maluku in 1651 to restore order. Manilha maintained his claim and kept his residence in Jailolo on the west coast of Halmahera. The other brother Kalamata, an able figure and an expert in Islamic law, joined him there in 1652, but then proclaimed himself sultan in defiance of Manilha and Mandar Syah.

Geographic entities mentioned:
surface_form: Jailolo
instance_of: Mountain
countries: Indonesia
coordinates: lat: 1.08
lon: 127.42
Sluŋkajávrre. (or the historic spelling,) is a lake in Hamarøy Municipality in Nordland county, Norway. The lake lies about southeast of the village of Tømmerneset. The large lake Rekvatnet lies just to the west of this lake. The ending &quot;-jávri&quot; or &quot;-jávrre&quot; is the Sami language word for &quot;lake&quot;.

Geographic entities mentioned:
surface_form: Rekvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 67.8088
lon: 16.0817
Sluŋkajávrre. (or the historic spelling,) is a lake in Hamarøy Municipality in Nordland county, Norway. The lake lies about southeast of the village of Tømmerneset. The large lake Rekvatnet lies just to the west of this lake. The ending &quot;-jávri&quot; or &quot;-jávrre&quot; is the Sami language word for &quot;lake&quot;.

Geographic entities mentioned:
surface_form: sluŋkajávrre
instance_of: Lake
countries: Norway
coordinates: lat: 67.7819
lon: 16.1454
Tati Jhariya is a community development block (CD block) that forms an administrative division in the Hazaribagh Sadar subdivision of the Hazaribagh district in the Indian state of Jharkhand. Overview. Hazaribagh district is spread over a part of the Chota Nagpur Plateau. The central plateau, averaging a height of, occupies the central part of the district.

Geographic entities mentioned:
surface_form: Chota Nagpur Plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
Days before Congress was due to convene to choose a winner, the army launched the bloody coup of 17 July 1980, which installed a reactionary (and cocaine-tainted) dictatorship of General Luis García Meza. Siles escaped to exile in Peru by crossing Lake Titicaca on a boat. He returned in 1982, when the military's experiment had run its course and the Bolivian economy was on the verge of collapse.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
Mount Pleasant (Ulster County, New York). Mount Pleasant is a mountain located in the Catskill Mountains of New York state, USA, northwest of Olivebridge. Cross Mountain is located southwest and Romer Mountain is located north-northwest of Mount Pleasant.

Geographic entities mentioned:
surface_form: Romer Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.05815
lon: -74.31876
surface_form: mount pleasant
instance_of: Mountain
countries: United States
coordinates: lat: 42.034166666667
lon: -74.308333333333
Mount Pleasant (Ulster County, New York). Mount Pleasant is a mountain located in the Catskill Mountains of New York state, USA, northwest of Olivebridge. Cross Mountain is located southwest and Romer Mountain is located north-northwest of Mount Pleasant.

Geographic entities mentioned:
surface_form: mount pleasant (ulster county, new york)
instance_of: Mountain
countries: United States
coordinates: lat: 42.034166666667
lon: -74.308333333333
Mount Pleasant (Ulster County, New York). Mount Pleasant is a mountain located in the Catskill Mountains of New York state, USA, northwest of Olivebridge. Cross Mountain is located southwest and Romer Mountain is located north-northwest of Mount Pleasant.

Geographic entities mentioned:
surface_form: mount pleasant
instance_of: Mountain
countries: United States
coordinates: lat: 42.034166666667
lon: -74.308333333333
Obsessed with adulation, Trujillo promoted an extravagant cult of personality. When a hurricane struck Santo Domingo in 1930, killing 8,000 people, he rebuilt the city and renamed it &quot;Ciudad Trujillo&quot;: &quot;Trujillo City&quot;; he also renamed the country's and the Caribbean's highest mountain, Pico Duarte (Duarte Peak), &quot;Pico Trujillo&quot;.

Geographic entities mentioned:
surface_form: Pico Duarte
instance_of: Mountain
countries: Dominican Republic
coordinates: lat: 19.033055555556
lon: -71.005277777778
Altogether, the project was initially expected to cost $86 million and be completed in late 2009. The lengthy construction time was largely due to the need to construct two bridges over the Zoar Valley gorge. As of March 2009, the projected cost of the extension had risen to $116 million.

Geographic entities mentioned:
surface_form: Zoar Valley
instance_of: Valley
countries: United States
coordinates: lat: 42.4397
lon: -78.8733