Sarmila/GeoWiki-Features huggingface dataset:
In September 2013 a government panel recommended that two mountains be renamed Hillary Peak and Tenzing Peak as part of a batch of summits that would be opened to climbers in 2014. The coordinates given by the government indicate that it is one of a clutch of peaks on the Nepal and Tibet border between Cho Oyu and Gyachung Kang, known variously as Ngojumba Kang, Ngozumpa Kang and Ngojumba Ri.

Geographic entities mentioned:
surface_form: Cho Oyu
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 28.094166666667
lon: 86.660833333333
surface_form: Gyachung Kang
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 28.098055555556
lon: 86.742222222222
These deposits reach thicknesses of and also occur on neighbouring volcanic centres. Purupuruni has formed on the rim of a depression, which is surrounded by eroded Quaternary volcanoes and appears to be a wide caldera southwest of the domes. The volcano lies east-southeast from Yucamane volcano and just south of the Mauri River; the Mauri River is part of the Lake Titicaca watershed.

Geographic entities mentioned:
surface_form: Yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: Mauri River
instance_of: Watercourse
countries: Bolivia
Peru
coordinates: lat: -17.140278
lon: -70.015278
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
Purupuruni and neighbouring volcanic centres have formed on the Cretaceous sedimentary basement. Volcanism in Peru occurs mainly in the southern part of the country, where there are about 300 separate volcanic systems including El Misti, Ubinas, Ticsani, Sabancaya and Huaynaputina.

Geographic entities mentioned:
surface_form: Ubinas
instance_of: Mountain
countries: Peru
coordinates: lat: -16.34861111111111
lon: -70.90222222222222
surface_form: Ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
surface_form: Huaynaputina
instance_of: Mountain
countries: Peru
coordinates: lat: -16.615555555555556
lon: -70.84972222222223
surface_form: misti
instance_of: Mountain
countries: Peru
coordinates: lat: -16.296388888888888
lon: -71.41055555555556
surface_form: el misti
instance_of: Mountain
countries: Peru
coordinates: lat: -16.296388888888888
lon: -71.41055555555556
surface_form: misti
instance_of: Mountain
countries: Peru
coordinates: lat: -15.525277777778
lon: -71.690833333333
surface_form: huaynaputina
instance_of: Mountain
countries: Peru
coordinates: lat: -16.615555555555556
lon: -70.84972222222223
surface_form: ubinas
instance_of: Mountain
countries: Peru
coordinates: lat: -16.34861111111111
lon: -70.90222222222222
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
Volcanism in Peru occurs mainly in the southern part of the country, where there are about 300 separate volcanic systems including El Misti, Ubinas, Ticsani, Sabancaya and Huaynaputina. In the Tacna Region of Peru alone there are over 60 separate volcanoes, two of which, Tutupaca and Yucamane, have been active in historical time.

Geographic entities mentioned:
surface_form: Tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
The domes cover an area of about, are up to - high and are isolated and little eroded. The domes are accompanied by intrusions and lava and pyroclastic flow deposits. The volcanism appears to come from fissure vents and the volcanoes have been affected by faulting, such as the Pacollo fault. These deposits reach thicknesses of and also occur on neighbouring volcanic centres.

Geographic entities mentioned:
surface_form: pacollo
instance_of: Mountain
countries: Peru
coordinates: lat: -17.4111
lon: -69.8492
Geological context. Rock formations in the region include the Mesozoic Yura Group sediments, the Toquepala intrusive rocks, the 30-24 million years old Tacaza volcanic rocks, the 24-10 million years old Huaylillas volcanic rocks and the 10-3 million years old Barroso volcanic rocks; Purupuruni is considered to be part of this Barroso formation.

Geographic entities mentioned:
surface_form: barroso
instance_of: Mountain
countries: Peru
coordinates: lat: -17.556308
lon: -69.5954717
surface_form: barroso
instance_of: Mountain
countries: Peru
coordinates: lat: -17.556308
lon: -69.5954717
surface_form: purupuruni
instance_of: Mountain
countries: Peru
coordinates: lat: -17.30916667
lon: -69.91472222
surface_form: purupuruni
instance_of: Mountain
countries: Peru
coordinates: lat: -17.30916667
lon: -69.91472222
Purupuruni. Purupuruni is a group of lava domes in southern Peru and a correlative geological formation. They are among the many volcanoes that exist in Peru and whose activity has been associated with the subduction of the Nazca Plate beneath the South America Plate. Purupuruni is associated with a geothermal field and a caldera.

Geographic entities mentioned:
surface_form: purupuruni
instance_of: Mountain
countries: Peru
coordinates: lat: -17.30916667
lon: -69.91472222
Geography and geomorphology. Purupuruni lies in the Cordillera Occidental north of the border with Chile, about away from Tacna and only about from the town of Tarata. The volcano is part of the geopark. The term means dung in Aymara. The Purupuruni volcano, also known as Purupurini, is a wide complex of four large lava domes at an elevation of or.

Geographic entities mentioned:
surface_form: purupuruni
instance_of: Mountain
countries: Peru
coordinates: lat: -17.30916667
lon: -69.91472222
The volcano is part of the geopark. The term means dung in Aymara. The Purupuruni volcano, also known as Purupurini, is a wide complex of four large lava domes at an elevation of or. The domes cover an area of about, are up to - high and are isolated and little eroded. The domes are accompanied by intrusions and lava and pyroclastic flow deposits.

Geographic entities mentioned:
surface_form: purupuruni
instance_of: Mountain
countries: Peru
coordinates: lat: -17.30916667
lon: -69.91472222
These deposits reach thicknesses of and also occur on neighbouring volcanic centres. Purupuruni has formed on the rim of a depression, which is surrounded by eroded Quaternary volcanoes and appears to be a wide caldera southwest of the domes. The volcano lies east-southeast from Yucamane volcano and just south of the Mauri River; the Mauri River is part of the Lake Titicaca watershed.

Geographic entities mentioned:
surface_form: purupuruni
instance_of: Mountain
countries: Peru
coordinates: lat: -17.30916667
lon: -69.91472222
The volcano lies east-southeast from Yucamane volcano and just south of the Mauri River; the Mauri River is part of the Lake Titicaca watershed. The Borateras geothermal field with about 40 separate manifestations is associated with Purupuruni and neighbouring volcanoes such as Coverane and Jaruma across the Mauri River and west from Purupuruni respectively.

Geographic entities mentioned:
surface_form: purupuruni
instance_of: Mountain
countries: Peru
coordinates: lat: -17.30916667
lon: -69.91472222
surface_form: purupuruni
instance_of: Mountain
countries: Peru
coordinates: lat: -17.30916667
lon: -69.91472222
Geology. The volcanic rocks are mainly andesitic and dacitic, and contain amphibole, biotite, olivine, plagioclase and pyroxene and are among the most differentiated volcanics in the area. They are part of the wider &quot;Purupurini Volcanics&quot;, which are named after Purupuruni and also form other volcanoes in the region. Geological context.

Geographic entities mentioned:
surface_form: purupuruni
instance_of: Mountain
countries: Peru
coordinates: lat: -17.30916667
lon: -69.91472222
Volcanic and geothermal activity in the region is a consequence of the subduction of the Nazca Plate beneath the South America Plate at a rate of about. Geologic history. The volcanic centres in the area including Purupuruni are of Miocene to Pliocene age, and appear to be of Pleistocene age.

Geographic entities mentioned:
surface_form: purupuruni
instance_of: Mountain
countries: Peru
coordinates: lat: -17.30916667
lon: -69.91472222
surface_form: purupuruni
instance_of: Mountain
countries: Peru
coordinates: lat: -17.30916667
lon: -69.91472222
Purupuruni formed during the last 100,000 years and appears to have developed between two interglacials; fission-track dating on glasses from Purupuruni has yielded ages of 53,000 ± 8,000 years ago but more recent surface exposure dating has yielded an age of 5,300 ± 1,100 years before present on one of the southern domes.

Geographic entities mentioned:
surface_form: purupuruni
instance_of: Mountain
countries: Peru
coordinates: lat: -17.30916667
lon: -69.91472222
The volcano is considered to be a low-hazard system and in 2018 the Peruvian Geological Institute announced it would begin monitoring Purupuruni and nine other volcanoes. Earthquake swarms in 2020 and 2021 do not appear to have been caused by volcanism; they are instead linked to local fault activity. Purupuruni appears to be the heat source for the Kovire geothermal field.

Geographic entities mentioned:
surface_form: purupuruni
instance_of: Mountain
countries: Peru
coordinates: lat: -17.30916667
lon: -69.91472222
Purupuruni appears to be the heat source for the Kovire geothermal field. Glacial erosion took place on Purupuruni during the Pleistocene, leaving moraines on the domes although research published in 2019 has found that the domes have not been eroded by glaciers even though evidence of glaciation occurs in the wider area.

Geographic entities mentioned:
surface_form: purupuruni
instance_of: Mountain
countries: Peru
coordinates: lat: -17.30916667
lon: -69.91472222
In 2015, he discovered a significant 320-million year old shark tooth. In January 2018, he was recognised for his discovery, in the late 1980s in the Maam Valley area of County Galway, of a species of brittle star, now named &quot;Crepidosoma doyleii&quot; after him. Doyle identified a further new species in 2019, a crinoid columnal. Publications.

Geographic entities mentioned:
surface_form: Maam Valley
instance_of: Valley
countries: Ireland
coordinates: lat: 53.48702
lon: -9.55484
Middleton Dale. Middleton Dale is a steep-sided, carboniferous limestone valley in the Derbyshire Peak District of England. The village of Stoney Middleton lies at the eastern foot of the dale and the village of Eyam lies about to the north, through the side valley of Eyam Dale. The dale is cut into the surrounding gritstone uplands of Middleton Moor and Eyam Moor.

Geographic entities mentioned:
surface_form: middleton dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.2805
lon: -1.6998
The dale is cut into the surrounding gritstone uplands of Middleton Moor and Eyam Moor. Dale Brook stream runs down the dale into Stoke Brook and on into the River Derwent beyond Stoney Middleton. The Delf is a secluded, wooded side gorge with a stream between Eyam and Middleton Dale. Opposite The Delf, water gushes from Hawkenedge Well and flows into Dale Brook.

Geographic entities mentioned:
surface_form: middleton dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.2805
lon: -1.6998
Fingals Cave is a tall passage with the largest entrance in the dale and is an old mine. Ivy Green Cave is long and in 1989 a local boy from Eyam got lost in it and his body was only found a year later. Limestone has been quarried in Middleton Dale for hundreds of years, from Darlton Quarry, Furness Quarry (now known as Horseshoe Quarry) and Goddards Quarry.

Geographic entities mentioned:
surface_form: middleton dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.2805
lon: -1.6998
Corno dei Tre Signori. Corno dei Tre Signori is a mountain in Lombardy, Italy. The Oglio and Noce rivers originate there.

Geographic entities mentioned:
surface_form: corno dei tre signori
instance_of: Mountain
countries: Italy
coordinates: lat: 46.344166666667
lon: 10.515
On 1 October 1943, Hauptmann Pöschl became the Battalion Commander of I.Bataillon/Gebirgsjäger-Regiment 100. The Battle of Monte Cassino (1944). In November 1943, the 5.Gebirgs-Division was withdrawn from the Soviet Union and redeployed to Italy to defend Monte Cassino against the Western Allied forces as part of the Wehrmacht's defense strategy in Italy.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
Taxonomy and naming. &quot;Caladenia alpina&quot; was first formally described by Richard Sanders Rogers in 1927 and the description was published in &quot;Transactions and Proceedings of the Royal Society of South Australia&quot;. Rogers described the species from specimens collected on Mount Bogong and Mount Hotham in Victoria and from Mount Kosciuszko in New South Wales.

Geographic entities mentioned:
surface_form: Mount Bogong
instance_of: Mountain
countries: Australia
coordinates: lat: -36.7325
lon: 147.30583333333334
surface_form: Mount Hotham
instance_of: Mountain
countries: Australia
coordinates: lat: -36.983333333333
lon: 147.13333333333
surface_form: Mount Kosciuszko
instance_of: Mountain
countries: Australia
coordinates: lat: -36.4558303
lon: 148.2635105
It is an area of recently folded mountains formed from sedimentary rocks from the Paleozoic to Quaternary (539 million years ago to the present). There are many intrusions and broad areas of recent volcanic material including Mount Ararat at, but no volcanic activity at present. The area is geologically unstable and very prone to earthquakes.

Geographic entities mentioned:
surface_form: Mount Ararat
instance_of: Mountain
countries: Turkey
coordinates: lat: 39.70194444444444
lon: 44.29833333333333
Schneekopf. The Schneekopf () near Gehlberg in the Thuringian county of Ilm-Kreis is and thus the second highest peak in the Thuringian Forest after its western neighbour, the Großer Beerberg (). The &quot;Adler&quot; Saddle between them is only about 59.4 metres lower than the two summits.

Geographic entities mentioned:
surface_form: Großer Beerberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.659444444444
lon: 10.746111111111
surface_form: schneekopf
instance_of: Mountain
countries: Germany
coordinates: lat: 50.6658
lon: 10.7644
The &quot;Adler&quot; Saddle between them is only about 59.4 metres lower than the two summits. To the east some distance away is its subpeak, the &quot;Sachsenstein&quot; (), to the south are the &quot;Teufelskreise&quot; () and &quot;Fichtenkopf&quot; (). The &quot;Goldlauterberg&quot; () further south marks the transition to the mountain of Großer Finsterberg (). Description.

Geographic entities mentioned:
surface_form: Großer Finsterberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.63695
lon: 10.800138
surface_form: finsterberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.63695
lon: 10.800138
surface_form: großer finsterberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.63695
lon: 10.800138
In very good visibility, for example during winter inversion weather conditions, the view extends as far as the Brocken in the Harz Mountains, the Schneeberg and the western Ore Mountains. In addition, the Wilde Gera Viaduct (on the A 71), which has a span of 252 metres - the largest arch bridge in Germany, is also visible.

Geographic entities mentioned:
surface_form: Brocken
instance_of: Mountain
countries: Germany
Kingdom of Prussia
coordinates: lat: 51.800555555556
lon: 10.617222222222
The &quot;Adler&quot; Saddle between them is only about 59.4 metres lower than the two summits. To the east some distance away is its subpeak, the &quot;Sachsenstein&quot; (), to the south are the &quot;Teufelskreise&quot; () and &quot;Fichtenkopf&quot; (). The &quot;Goldlauterberg&quot; () further south marks the transition to the mountain of Großer Finsterberg (). Description.

Geographic entities mentioned:
surface_form: fichtenkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 50.6658
lon: 10.7644
Schneekopf. The Schneekopf () near Gehlberg in the Thuringian county of Ilm-Kreis is and thus the second highest peak in the Thuringian Forest after its western neighbour, the Großer Beerberg (). The &quot;Adler&quot; Saddle between them is only about 59.4 metres lower than the two summits.

Geographic entities mentioned:
surface_form: schneekopf
instance_of: Mountain
countries: Germany
coordinates: lat: 50.6658
lon: 10.7644
Kettle in December 1960 and this holotype specimen is held in the New Zealand Arthropod Collection. It was first described by Beverley Holloway in 2007. Its type location is Mount Tuhua summit, near Lake Kaniere on the West Coast of New Zealand. The name &quot;servandus&quot; is a Latin word meaning &quot;[something] to be preserved, conserved, looked after&quot;. Description.

Geographic entities mentioned:
surface_form: Lake Kaniere
instance_of: Lake
countries: New Zealand
coordinates: lat: -42.833333333333
lon: 171.15
Glastenbury Mountain. Glastenbury Mountain is a mountain located in Bennington County, Vermont, in the Green Mountain National Forest. The mountain is part of the Green Mountains. The northeast side of Glastenbury Mountain drains into Deer Lick Brook, thence into the Glastenbury River, the Deerfield River, the Connecticut River, and into Long Island Sound in Connecticut.

Geographic entities mentioned:
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.9822
lon: -105.302
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.291666666667
lon: -121.23861111111
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.3053
lon: -105.3
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: glastenbury mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.978133333333
lon: -73.071216666667
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.5175
lon: -121.67305555556
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.563333333333
lon: -122.80694444444
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.700833333333
lon: -105.17805555556
Glastenbury Mountain is a mountain located in Bennington County, Vermont, in the Green Mountain National Forest. The mountain is part of the Green Mountains. The northeast side of Glastenbury Mountain drains into Deer Lick Brook, thence into the Glastenbury River, the Deerfield River, the Connecticut River, and into Long Island Sound in Connecticut. The southeast side of Glastenbury Mtn.

Geographic entities mentioned:
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
surface_form: glastenbury mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.978133333333
lon: -73.071216666667
Glastenbury Mountain. Glastenbury Mountain is a mountain located in Bennington County, Vermont, in the Green Mountain National Forest. The mountain is part of the Green Mountains. The northeast side of Glastenbury Mountain drains into Deer Lick Brook, thence into the Glastenbury River, the Deerfield River, the Connecticut River, and into Long Island Sound in Connecticut.

Geographic entities mentioned:
surface_form: glastenbury mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.978133333333
lon: -73.071216666667
The northwest side of Glastenbury drains into the Fayville Branch of Warm Brook, thence into Batten Kill and the Hudson River. The Long Trail, a 272-mile (438-km) hiking trail running the length of Vermont, passes over the summit of Glastenbury Mountain. The summit of the mountain has an observation tower maintained by GMC, who also maintains the shelter three-tenths of a mile south of the summit.

Geographic entities mentioned:
surface_form: glastenbury mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.978133333333
lon: -73.071216666667
Mio-Pliocene sandstones and marl grade into epiclastics and andesitic volcanics of the Suva Group. The Group forms the Korotini Tableland in the middle of the island, it includes the peaks of Seseleka (), Ndelanathau (), Nararo (), Valili (), Mariko (), Mount Nasorolevu (), Ndikeva (), and Uluingala ().

Geographic entities mentioned:
surface_form: Mount Nasorolevu
instance_of: Mountain
countries: Fiji
coordinates: lat: -16.616666666667
lon: 179.4
The antimeridian passes through this island, just touching its northeastern tip. A rugged mountain range divides the island horizontally, forming much of the boundary between the Provinces of Cakaudrove and Macuata. The highest peaks are Mount Batini, also known as Nasorolevu, with an elevation of, and, further north-east, Dikeva, also known as Mount Thurston, with an elevation of.

Geographic entities mentioned:
surface_form: Nasorolevu
instance_of: Mountain
countries: Fiji
coordinates: lat: -16.616666666667
lon: 179.4
Herzl Museum. The Herzl Museum is a museum in Jerusalem, which deals with activities and vision of Theodor Herzl. The museum is located at the main entrance plaza to Mount Herzl. History.

Geographic entities mentioned:
surface_form: Mount Herzl
instance_of: Mountain
countries: Israel
coordinates: lat: 31.774117
lon: 35.180567
History. Shortly after Herzl's death, the Anglo–Palestine Bank acquired about in south-central Palestine, where the Hulda Forest is located today, for a farm and a large building that would house the farm's management and double as a museum dedicated to Herzl. However, the museum was not created and only in 1960s one was built on Mount Herzl in Jerusalem.

Geographic entities mentioned:
surface_form: Mount Herzl
instance_of: Mountain
countries: Israel
coordinates: lat: 31.774117
lon: 35.180567
One scene that was filmed in Madras depicts several buildings near Marina Beach that were under construction. While filming at Dal Lake, where the song &quot;Nilavum Malarum&quot; was filmed, Vyjayanthimala almost drowned but was rescued by the cameraman. The song &quot;Oho Endhan Baby&quot; was picturised on Ganesan and Vyjayanthimala water skiing; Vyjayanthimala refused to use a body double.

Geographic entities mentioned:
surface_form: Dal Lake
instance_of: Lake
countries: India
coordinates: lat: 34.12
lon: 74.87
It was also known that Sostene had a prayer room in his home and was a devoted Christian. 1994 genocide. During the genocide against the Tutsi in 1994, he had a boat in Lake Kivu. Many Tutsi went to him in search of help to cross to the Democratic Republic of the Congo (DRC). He first took his two Tutsi women and some of his neighbours among others Gatete and Forodo.

Geographic entities mentioned:
surface_form: Lake Kivu
instance_of: Lake
countries: Democratic Republic of the Congo
Rwanda
coordinates: lat: -1.8530555555556
lon: 29.135277777778
The Varangerfjorden runs along the northern part of the municipality and the Bøkfjorden runs north–south cutting into the municipality and flowing into the Varangerfjorden. The large island of Skogerøya lies on the west side of the Bøkfjorden. Skogerøytoppen is the tallest mountain on Skogerøya. The Bøkfjord Lighthouse lies along the mouth of the Bøkfjorden.

Geographic entities mentioned:
surface_form: Skogerøytoppen
instance_of: Mountain
countries: Norway
coordinates: lat: 69.87555
lon: 29.85929
The flora of the area is a part of the Russian and Siberian taiga, including a few hundred spruce trees of the Russian variety. Bears also inhabit the upper valley, notably in the Øvre Pasvik National Park, Øvre Pasvik Landscape Protection Area, and Pasvik Nature Reserve. Lakes include Ellenvatnet, Gardsjøen, Garsjøen, Klistervatnet, and Ødevatnet. The fjords include Korsfjorden. Climate.

Geographic entities mentioned:
surface_form: Ellenvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 69.10975
lon: 28.90534
surface_form: Garsjøen
instance_of: Lake
countries: Norway
coordinates: lat: 69.917925
lon: 28.936553
surface_form: Klistervatnet
instance_of: Lake
countries: Russia
Norway
Russian Empire
Soviet Union
coordinates: lat: 69.573833
lon: 30.181389
surface_form: Ødevatnet
instance_of: Lake
countries: Norway
coordinates: lat: 69.0646
lon: 28.9893
California State Route 45. State Route 45 (SR 45) is a state highway in the U.S. State of California that travels in a north&ndash;south direction in the Sacramento Valley from Route 113 in Knights Landing to Route 32 in Hamilton City. Route description. The route begins at SR 113 in Knights Landing in Yolo County.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
Hackensack River crossings, notably the Pulaski Skyway, were also built. Newark Airport was the first major airport in the New York Metropolitan Area, opening on October 1, 1928. At Houvenkopf Mountain crosses were burned by the Ku Klux Klan. Radburn was founded in 1929 as &quot;a town for the motor age&quot;.

Geographic entities mentioned:
surface_form: Houvenkopf Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1059
lon: -74.1751
Fuss Peak. Fuss Peak (;; &quot;Shiriyajiri-dake&quot;) is an active stratovolcano located on the southwest coast of Paramushir Island, Kuril Islands, Russia. History. The volcano was discovered in 1805 during the first Russian circumnavigation of the Earth and named in honor of a Swiss mathematician Nicolas Fuss, who served as the permanent secretary to the Academy of Sciences in St. Petersburg.

Geographic entities mentioned:
surface_form: fuss
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 50.269722222222
lon: 155.2475
Phusnu Pullawi. Phusnu Pullawi (Aymara &quot;phusnu&quot; chyme, &quot;pulla&quot; a kind of sheep, &quot;-wi&quot; a suffix, &quot;a place with the chyme of sheep&quot;, also spelled &quot;Pusnupullave&quot;) is a mountain in the north of the Barroso mountain range in the Andes of Peru which reaches a height of approximately. It is located in the Tacna Region, Tarata Province, Tarata District.

Geographic entities mentioned:
surface_form: phusnu pullawi
instance_of: Mountain
countries: Peru
coordinates: lat: -17.39861111
lon: -69.87416667
Phusnu Pullawi. Phusnu Pullawi (Aymara &quot;phusnu&quot; chyme, &quot;pulla&quot; a kind of sheep, &quot;-wi&quot; a suffix, &quot;a place with the chyme of sheep&quot;, also spelled &quot;Pusnupullave&quot;) is a mountain in the north of the Barroso mountain range in the Andes of Peru which reaches a height of approximately. It is located in the Tacna Region, Tarata Province, Tarata District.

Geographic entities mentioned:
surface_form: phusnu pullawi
instance_of: Mountain
countries: Peru
coordinates: lat: -17.39861111
lon: -69.87416667
surface_form: barroso
instance_of: Mountain
countries: Peru
coordinates: lat: -17.556308
lon: -69.5954717
It is located in the Tacna Region, Tarata Province, Tarata District. Phusnu Pullawi lies southwest of Ch'uxñuma and northwest of Chunta Qullu and Pä Qullu.

Geographic entities mentioned:
surface_form: pä qullu
instance_of: Mountain
countries: Peru
coordinates: lat: -17.4111
lon: -69.8492
surface_form: chunta
instance_of: Mountain
countries: Peru
coordinates: lat: -11.4964
lon: -76.3772
surface_form: chunta
instance_of: Mountain
countries: Peru
coordinates: lat: -14.7836
lon: -72.5717
surface_form: chunta
instance_of: Mountain
countries: Peru
coordinates: lat: -14.4222
lon: -73.8572
surface_form: chunta qullu
instance_of: Mountain
countries: Peru
coordinates: lat: -17.4361
lon: -69.8533
This is in contrast to the Santa Clara Valley/Silicon Valley and San Gabriel Valley in California where there are concentrated communities with larger proportions of people of Taiwanese heritage and where many Chinese shopping centers, restaurants, supermarkets, and other retail businesses tend to reflect more of the modern Taiwanese trends.

Geographic entities mentioned:
surface_form: Santa Clara Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.366944444444
lon: -121.98388888889
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
Gregory was liberated, but the people were incensed by the excesses of his Norman allies, and he was compelled to leave Rome. He withdrew to Monte Cassino, and later to the castle of Salerno by the sea, in 1084, where he died in the following year, 25 May 1085. The German episcopate stood divided.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
The people of Fort Munro are nomads, especially of the Leghari tribe. Fort Munro's altitude is 1800 meters. Yakbai top and Mubarki top are other major tourist spots, located near Fort Munro where elevation reaches above 2000 meters. It can also be reached either from Loralai, Balochistan or from Multan (Punjab).

Geographic entities mentioned:
surface_form: Yakbai
instance_of: Mountain
countries: Pakistan
Siegfried Glacier. Siegfried Glacier () is a glacier flowing east-southeast into Lazarev Bay, south of Mirnyy Peak on Rothschild Island. It was named by the UK Antarctic Place-names Committee in association with the Wagner Ice Piedmont after Siegfried, the third part of the four-part festival play Der Ring des Nibelungen (1826) by Wagner.

Geographic entities mentioned:
surface_form: Mirnyy Peak
instance_of: Mountain
coordinates: lat: -69.3333
lon: -72.5667
Dome Mountain. Round Mountain is a mountain in northwestern British Columbia, Canada, located east of Dease Lake. Round Mountain is a volcanic feature of the Northern Cordilleran Volcanic Province that formed in the past 1.6 million years of the Pleistocene

Geographic entities mentioned:
surface_form: Northern Cordilleran Volcanic Province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: round mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.7649
lon: -123.024
Dome Mountain. Round Mountain is a mountain in northwestern British Columbia, Canada, located east of Dease Lake. Round Mountain is a volcanic feature of the Northern Cordilleran Volcanic Province that formed in the past 1.6 million years of the Pleistocene

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: dease lake
instance_of: Lake
countries: Canada
coordinates: lat: 58.63502
lon: -130.03761
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: round mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.7649
lon: -123.024
Dome Mountain. Round Mountain is a mountain in northwestern British Columbia, Canada, located east of Dease Lake. Round Mountain is a volcanic feature of the Northern Cordilleran Volcanic Province that formed in the past 1.6 million years of the Pleistocene

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: dome mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 58.4535
lon: -129.63516666667
Rimini. Rimini (,; or;) is a city in the Emilia-Romagna region of Northern Italy. Sprawling along the Adriatic Sea, Rimini is situated at a strategically-important north-south passage along the coast at the southern tip of the Po Valley. It is one of the most notable seaside resorts in Europe, with a significant domestic and international tourist economy.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
The conurbation is a result of urban sprawl as the tourist economy developed along the. Natural features. Rimini's natural geography provides a strategically-important passage along the Adriatic Sea at the boundary between northern Italy, characterised by the plains of the Po Valley, and central Italy, characterised by more mountainous terrain.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
Precipitations are equally distributed during the year, with a peak in October and minimums in January and July. In spring, autumn, and winter, precipitations mainly come from oceanic fronts, while in summer, they are brought by thunderstorms, coming from the Apennines or the Po Valley.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
The city has always been a key gate to the Orient and the southern areas of the Mediterranean for the Po Valley, thanks to its geographical position and its harbour, and a meeting point between cultures of Northern and Central Italy.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
The city's oldest lyceum, the Classical Lyceum &quot;Giulio Cesare&quot;, founded in 1800, was attended by Amintore Galli, Giovanni Pascoli, and Federico Fellini. Transport. Rimini is an important road and railway junction due to its geographic position at the southern tip of the Po Valley, where Adriatic coastal routes meet those extending northwest along the plains. Roads.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
The municipality has a population of 2,317 (2006). It is situated in the centre of the Sierra de las Nieves Nature Park at the foot of the Sierra Blanca and the Sierra Parda. In addition to La Torrecilla peak (1,919 m.), there are ancient woodlands of Spanish Fir and gall oak. The municipality covers 94 km2, has a mean elevation of 285 m.

Geographic entities mentioned:
surface_form: La Torrecilla
instance_of: Mountain
countries: Spain
coordinates: lat: 36.675950833333
lon: -4.9962178333333
But much of the remaining land, some 867,000 acres (over 350,000 hectares) of estates, included a large proportion of the best arable lands in the Shire Highlands, which was the most densely populated part of the country and where Africans had relied on subsistence farming.

Geographic entities mentioned:
surface_form: Shire Highlands
instance_of: Plateau
countries: Malawi
coordinates: lat: -15.64684105
lon: 35.12557983
Transport. From the time of Livingstone's expedition in 1859, the Zambesi, Shire River, and Lake Nyasa waterways were seen as the most convenient method of transport for Nyasaland. The Zambesi-Lower Shire and Upper Shire-Lake Nyasa systems were separated by of impassable falls and rapids in the Middle Shire which prevented continuous navigation.

Geographic entities mentioned:
surface_form: Lake Nyasa
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
Several streams draining the eastern slopes of Fan Nedd and the western slopes of Fan Dringarth in the Fforest Fawr section of the national park meet to form the river, which then flows southwards for to its confluence with the Afon Dringarth, the combined waters continuing south as the Afon Mellte.

Geographic entities mentioned:
surface_form: Fan Nedd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 51.8529
lon: -3.5792
Loch Kinord. Loch Kinord is a small, freshwater loch at Muir of Dinnet, Aberdeenshire, Scotland just north of the River Dee and east of Ballater. The loch is also known as &quot;Loch Ceander&quot; and &quot;Loch Cannor&quot;. It is approximately in length and was formed from a glacial kettle hole.

Geographic entities mentioned:
surface_form: Muir of Dinnet
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.06833333
lon: -2.92472222
surface_form: loch kinord
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.082
lon: -2.9222
It is approximately in length and was formed from a glacial kettle hole. The loch sits within the &quot;Muir of Dinnet National Nature Reserve&quot; and is immediately south of Loch Davan. It contains several islets, as noted in a 19th-century book giving a brief description of the loch, and is forested with birch trees. Flora and fauna. Due to its shallowness, light penetrates to the loch floor.

Geographic entities mentioned:
surface_form: Loch Davan
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.0944
lon: -2.92306
surface_form: muir of dinnet
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.06833333
lon: -2.92472222
surface_form: loch davan
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.0944
lon: -2.92306
Loch Kinord. Loch Kinord is a small, freshwater loch at Muir of Dinnet, Aberdeenshire, Scotland just north of the River Dee and east of Ballater. The loch is also known as &quot;Loch Ceander&quot; and &quot;Loch Cannor&quot;. It is approximately in length and was formed from a glacial kettle hole.

Geographic entities mentioned:
surface_form: loch kinord
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.082
lon: -2.9222
Loch Kinord. Loch Kinord is a small, freshwater loch at Muir of Dinnet, Aberdeenshire, Scotland just north of the River Dee and east of Ballater. The loch is also known as &quot;Loch Ceander&quot; and &quot;Loch Cannor&quot;. It is approximately in length and was formed from a glacial kettle hole.

Geographic entities mentioned:
surface_form: loch cannor
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.082
lon: -2.9222
surface_form: loch ceander
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.082
lon: -2.9222
Recreation. There is a circular walking route around the loch with vantage points for bird watching and wildlife spotting. The starting point for the walk is Burn O'Vat car park on the Ballater to Aboyne road. Since 2009 the Kinord Hall Committee has organised a 10 kilometre run around the loch. The first race was held on Saturday 24 October 2009.

Geographic entities mentioned:
surface_form: burn o'vat
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.084
lon: -2.951
By October, he listed his services as a photographer.&quot; Gentile was the first British Columbia photographer to specialize in portraits of First Nations people. Besides taking local pictures of Victoria and its citizenry, he traveled to the interior of Vancouver Island to photograph the Alberni Valley, Nanaimo, Cowichan Bay, and the short-lived Leech River gold rush.

Geographic entities mentioned:
surface_form: Alberni Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.25
lon: -124.8
Lake Kivijärvi (Central Finland). Kivijärvi is a rather large lake in Finland. The name Kivijärvi is rather common and there are 121 lakes with the same name. This is the biggest of them. The lake is located in the Central Finland region. It is 30th biggest lake in Finland. It is a good lake for fishing. For example, a lake trout was caught in Kivijärvi lake in summer 2001.

Geographic entities mentioned:
surface_form: kivijärvi
instance_of: Lake
countries: Finland
coordinates: lat: 63.11666667
lon: 25.18333333
surface_form: lake kivijärvi
instance_of: Lake
countries: Finland
coordinates: lat: 63.11666667
lon: 25.18333333
surface_form: kivijärvi
instance_of: Lake
countries: Finland
coordinates: lat: 60.96666667
lon: 27.66666667
surface_form: lake kivijärvi
instance_of: Lake
countries: Finland
coordinates: lat: 60.96666667
lon: 27.66666667
Lake Kivijärvi (Central Finland). Kivijärvi is a rather large lake in Finland. The name Kivijärvi is rather common and there are 121 lakes with the same name. This is the biggest of them. The lake is located in the Central Finland region. It is 30th biggest lake in Finland. It is a good lake for fishing. For example, a lake trout was caught in Kivijärvi lake in summer 2001.

Geographic entities mentioned:
surface_form: kivijärvi
instance_of: Lake
countries: Finland
coordinates: lat: 63.11666667
lon: 25.18333333
surface_form: kivijärvi
instance_of: Lake
countries: Finland
coordinates: lat: 60.96666667
lon: 27.66666667
Hayestown, Connecticut. Hayestown is an unincorporated area in Danbury, Connecticut. It is located in the eastern section of the city, along the southern shoreline of Candlewood Lake, west of Great Plain, northwest of Germantown, and east of Clapboard Ridge. History.

Geographic entities mentioned:
surface_form: Candlewood Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.5
lon: -73.46
History. C. R. Gregory dated the manuscript to the 10th century. Currently the manuscript is dated by the INTF to the 10th or 11th century. The manuscript was added to the list of New Testament manuscripts by Gregory (994e). C. R. Gregory saw it in 1886. Currently it is housed in the Iviron monastery (170 (19)), at Mount Athos.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Wild Horse Lake (Oklahoma). Wild Horse Lake is a playa lake located in Texas County, Oklahoma. The lake is west of Hooker, east of Hough, just south of the Oklahoma-Kansas border, off State Highway 136. The lake was the location of the infamous Hay Meadow Massacre (July 1888) in which one faction in the county seat fight in Stevens County, Kansas, killed four members of the opposing faction.

Geographic entities mentioned:
surface_form: wild horse lake (oklahoma)
instance_of: Lake
countries: United States
coordinates: lat: 36.9189
lon: -101.448
Wild Horse Lake (Oklahoma). Wild Horse Lake is a playa lake located in Texas County, Oklahoma. The lake is west of Hooker, east of Hough, just south of the Oklahoma-Kansas border, off State Highway 136. The lake was the location of the infamous Hay Meadow Massacre (July 1888) in which one faction in the county seat fight in Stevens County, Kansas, killed four members of the opposing faction.

Geographic entities mentioned:
surface_form: wild horse lake
instance_of: Lake
countries: United States
coordinates: lat: 36.9189
lon: -101.448
Its inhabitants were nicknamed manzañones. In November 1955, Forestry Heritage began, based on a 1927 Decree related to the construction of the Yesa Reservoir, the procedures for the voluntary purchase or subsequent expropriation of the land of Cenarbe and the Garcipollera Valley.

Geographic entities mentioned:
surface_form: Garcipollera Valley
instance_of: Valley
countries: Spain
coordinates: lat: 42.62
lon: -0.4855555555555556
It was also announced that the album would be titled &quot;Rainier Fog&quot;, with the release date scheduled for August 24, 2018. The album's artwork and the track listing were also revealed on the same day. Jerry Cantrell told &quot;Rolling Stone&quot; that the title &quot;Rainier Fog&quot; was inspired by the Mount Rainier in Seattle, and the title track is a tribute to the Seattle music scene.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
Kiryat Luza. Kiryat Luza (,) is a village situated on Mount Gerizim near the city of Nablus in the West Bank. It is within Area B of the West Bank, and as a result is under the joint control of Israel and the Palestinian National Authority, and is the only remaining site populated wholly by Samaritans.

Geographic entities mentioned:
surface_form: Mount Gerizim
instance_of: Mountain
countries: State of Palestine
coordinates: lat: 32.199444444444
lon: 35.272777777778
Azrieli College of Engineering Jerusalem. Azrieli College of Engineering Jerusalem () is an Israeli public academic college that trains engineers. It is located in the Ramat Beit HaKerem neighborhood of Jerusalem, between Jerusalem's two major high-tech industrial areas, Har Hotzvim and the Jerusalem Technology Park. Overview.

Geographic entities mentioned:
surface_form: Har Hotzvim
instance_of: Mountain
countries: Israel
coordinates: lat: 31.802527777778
lon: 35.209636111111
Fraser Lake (Minnesota). Fraser Lake is a lake in Lake County, in the U.S. state of Minnesota. Fraser Lake was named for John Fraser, a lumberman.

Geographic entities mentioned:
surface_form: fraser lake (minnesota)
instance_of: Lake
countries: United States
coordinates: lat: 48.012222222222
lon: -91.196388888889
Fraser Lake (Minnesota). Fraser Lake is a lake in Lake County, in the U.S. state of Minnesota. Fraser Lake was named for John Fraser, a lumberman.

Geographic entities mentioned:
surface_form: fraser lake
instance_of: Lake
countries: United States
coordinates: lat: 48.012222222222
lon: -91.196388888889
Mount Helen (Montana). Mount Helen () is located in the Lewis Range, Glacier National Park in the U.S. state of Montana. Mount Helen rises immediately to the northwest roughly above Upper Two Medicine Lake in the southeastern part of Glacier National Park. The Continental Divide of the Americas passes over the summit of Mount Helen. Geology. Like the mountains in Glacier National Park, Mt.

Geographic entities mentioned:
surface_form: Upper Two Medicine Lake
instance_of: Lake
countries: United States
coordinates: lat: 48.4639
lon: -113.462
surface_form: mount helen
instance_of: Mountain
countries: United States
coordinates: lat: 43.1511
lon: -109.631
surface_form: mount helen
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: medicine lake
instance_of: Lake
countries: United States
coordinates: lat: 45.00644
lon: -93.41997
surface_form: mount helen
instance_of: Mountain
countries: United States
coordinates: lat: 48.4747
lon: -113.467
surface_form: two medicine lake
instance_of: Lake
countries: United States
coordinates: lat: 48.4769
lon: -113.387
surface_form: medicine lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9841655
lon: -97.3519987
Mount Helen (Montana). Mount Helen () is located in the Lewis Range, Glacier National Park in the U.S. state of Montana. Mount Helen rises immediately to the northwest roughly above Upper Two Medicine Lake in the southeastern part of Glacier National Park. The Continental Divide of the Americas passes over the summit of Mount Helen. Geology. Like the mountains in Glacier National Park, Mt.

Geographic entities mentioned:
surface_form: mount helen
instance_of: Mountain
countries: United States
coordinates: lat: 43.1511
lon: -109.631
surface_form: mount helen
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: mount helen
instance_of: Mountain
countries: United States
coordinates: lat: 48.4747
lon: -113.467
state of Montana. Mount Helen rises immediately to the northwest roughly above Upper Two Medicine Lake in the southeastern part of Glacier National Park. The Continental Divide of the Americas passes over the summit of Mount Helen. Geology. Like the mountains in Glacier National Park, Mt. Helen is composed of sedimentary rock laid down during the Precambrian to Jurassic periods.

Geographic entities mentioned:
surface_form: mt. helen
instance_of: Mountain
countries: United States
coordinates: lat: 43.1511
lon: -109.631
surface_form: mt. helen
instance_of: Mountain
countries: United States
coordinates: lat: 48.4747
lon: -113.467
Climate. Based on the Köppen climate classification, Mt. Helen is located in an alpine subarctic climate zone characterized by long, usually very cold winters, and short, cool to mild summers. Temperatures can drop below −10 °F with wind chill factors below −30 °F.

Geographic entities mentioned:
surface_form: mt. helen
instance_of: Mountain
countries: United States
coordinates: lat: 43.1511
lon: -109.631
surface_form: mt. helen
instance_of: Mountain
countries: United States
coordinates: lat: 48.4747
lon: -113.467