Sarmila/GeoWiki-Features huggingface dataset:
Bamileke people. The Bamiléké people are an ethnic group of Central Africa that inhabits the Western High Plateau colloquially known as the &quot;grassfields&quot; of Cameroon. According to Dr John Feyou de Hapy, Bamiléké means &quot;people of faith&quot;. Languages. The Bamileke languages are Grassfields languages that belong to the Southern Bantoid branch of the Niger-Congo language family.

Geographic entities mentioned:
surface_form: Western High Plateau
instance_of: Plateau
countries: Cameroon
coordinates: lat: 6.5
lon: 10.5
Akademia Nauk (- &quot;Academy of Sciences&quot;) is a volcano located in the southern part of Kamchatka Peninsula, Russia, next to the stratovolcano of Karymsky. The volcano is filled with a few calderas, and the most notable one is known as Karymsky Lake (named after Karyms). The volcano is named after the &quot;Росси́йская Акаде́мия Нау́к&quot;, the Russian (Soviet) Academy of Sciences.

Geographic entities mentioned:
surface_form: Karymsky Lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.983333333333
lon: 159.46166666667
surface_form: karymsky
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 54.047777777777775
lon: 159.44222222222223
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: karymsky lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.983333333333
lon: 159.46166666667
Akademia Nauk. Akademia Nauk (- &quot;Academy of Sciences&quot;) is a volcano located in the southern part of Kamchatka Peninsula, Russia, next to the stratovolcano of Karymsky. The volcano is filled with a few calderas, and the most notable one is known as Karymsky Lake (named after Karyms).

Geographic entities mentioned:
surface_form: akademia nauk
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.966666666667
lon: 159.45
Akademia Nauk. Akademia Nauk (- &quot;Academy of Sciences&quot;) is a volcano located in the southern part of Kamchatka Peninsula, Russia, next to the stratovolcano of Karymsky. The volcano is filled with a few calderas, and the most notable one is known as Karymsky Lake (named after Karyms).

Geographic entities mentioned:
surface_form: akademia nauk
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.966666666667
lon: 159.45
surface_form: karymsky
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 54.047777777777775
lon: 159.44222222222223
1996 eruption. On 2 January 1996, Akademia Nauk erupted. Eruptive pulses from the bottom of Karymsky Lake ejected steam and ash columns in the air every five to six hours for the 18 hours that followed, releasing approximately 30 to 40 million tons of highly acidic pyroclastic material in the air, tsunamis up to 20 meters (65 feet) also occurred.

Geographic entities mentioned:
surface_form: karymsky
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 54.047777777777775
lon: 159.44222222222223
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: karymsky lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.983333333333
lon: 159.46166666667
Much of the material, which was rich in sodium, sulfates, calcium, and magnesium, collapsed back into Lake Karymsky, changing its pH from 7.5 to 3.2 (moderately acidic).

Geographic entities mentioned:
surface_form: karymsky
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 54.047777777777775
lon: 159.44222222222223
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
After Ruth Boone's death in 1998 at the age of 94, the City expanded the memorial to include Ruth, in honor of her generosity to the people of San Ramon and in recognition of the contribution women made to agriculture in the San Ramon Valley. History. The farm is located at the base of the Dougherty Hills, and Oak Creek divides it in two almost equal parts.

Geographic entities mentioned:
surface_form: San Ramon Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.75
lon: -121.95
It is almost entirely wooded. The nearest settlement is the village of Mitterfirmiansreut in the municipality of Philippsreut. Neighbouring mountains are the Almberg (1,140 m) to the south and, in Czechia, the Strážný (1,115 m) to the northeast.

Geographic entities mentioned:
surface_form: Almberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.889722222222
lon: 13.643888888889
Alzenberg. The Alzenberg (1,100 m) is a mountain in the Bavarian Forest, northeast of the town of Freyung and lies in the Bavarian Forest National Park about two kilometres from the German-Czech border. It is almost entirely wooded. The nearest settlement is the village of Mitterfirmiansreut in the municipality of Philippsreut.

Geographic entities mentioned:
surface_form: alzenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.8955
lon: 13.6263
Ysgafell Wen North Top. Ysgafell Wen North Top is a peak on a ridge in Snowdonia, North Wales. It lies to the north of the highest summit on the ridge Ysgafell Wen. It is a subsidiary summit of Allt-fawr. The summit is located at the edge of Cwm Edno, an edge that falls steeply into the cwm. Small lakes surround the summit, known as Llynnau'r Cwn (the dog lakes).

Geographic entities mentioned:
surface_form: Ysgafell Wen
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.013561111111
lon: -3.9884
Ysgafell Wen North Top. Ysgafell Wen North Top is a peak on a ridge in Snowdonia, North Wales. It lies to the north of the highest summit on the ridge Ysgafell Wen. It is a subsidiary summit of Allt-fawr. The summit is located at the edge of Cwm Edno, an edge that falls steeply into the cwm. Small lakes surround the summit, known as Llynnau'r Cwn (the dog lakes).

Geographic entities mentioned:
surface_form: Allt-fawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.007619444444
lon: -3.9672611111111
It lies to the north of the highest summit on the ridge Ysgafell Wen. It is a subsidiary summit of Allt-fawr. The summit is located at the edge of Cwm Edno, an edge that falls steeply into the cwm. Small lakes surround the summit, known as Llynnau'r Cwn (the dog lakes). To the west lies the peak's top, known as Ysgafell Wen Far North Top.

Geographic entities mentioned:
surface_form: the peak
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -7.95
lon: -14.35
surface_form: ysgafell wen
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.013561111111
lon: -3.9884
Ysgafell Wen North Top. Ysgafell Wen North Top is a peak on a ridge in Snowdonia, North Wales. It lies to the north of the highest summit on the ridge Ysgafell Wen. It is a subsidiary summit of Allt-fawr. The summit is located at the edge of Cwm Edno, an edge that falls steeply into the cwm. Small lakes surround the summit, known as Llynnau'r Cwn (the dog lakes).

Geographic entities mentioned:
surface_form: ysgafell wen
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.013561111111
lon: -3.9884
surface_form: ysgafell wen north top
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.01741
lon: -3.99382
armata&quot; changed to &quot;Banksia armata&quot;. Distribution and habitat. The species is widespread throughout most of the south-west. The main distribution is between Perth and Albany, but it also occurs near Mount Lesueur in the north, and between Esperance and Israelite Bay on the south coast. It grows on sandy loam or in rocky soils in tall shrubland or low woodland. Conservation status.

Geographic entities mentioned:
surface_form: Mount Lesueur
instance_of: Mountain
countries: Australia
coordinates: lat: -30.1755
lon: 115.19908333333
Another colleague was king's acquaintance Rehuankh. High Steward. Under king Sobekhotep IV he became high steward. In this position he went on expeditions to the Wadi Hammamat and Wadi el-Hudi. Other attestations. Nebankh is known from a high number of monuments, including rock inscriptions and several stelae and a statue, found at Abydos.

Geographic entities mentioned:
surface_form: Wadi el-Hudi
instance_of: Valley
countries: Egypt
coordinates: lat: 23.96152778
lon: 33.13133333
A significant portion of the locality is within Yurol State Forest, a legacy of days past when the town once was a centre of forestry activities. The forest is now preserved as koala habitat. Mount Cooroora is in the south-west of the locality (), rising to. It is a high intrusive volcanic plug within the Tuchekoi National Park. It is approximately south-west of the town.

Geographic entities mentioned:
surface_form: Mount Cooroora
instance_of: Mountain
countries: Australia
coordinates: lat: -26.3714
lon: 152.838
Disasters. The main streets of the town were devastated by two separate fires in 1939 and 1942. Many buildings were re-constructed with brick or in the &quot;Art Deco&quot; architectural style of the era. In 2014, a major bushfire resulted in Mount Cooroora and the surrounding Tuchekoi National Park burning for a week. The 2022 South East Queensland flood saw significant flooding around Pomona.

Geographic entities mentioned:
surface_form: Mount Cooroora
instance_of: Mountain
countries: Australia
coordinates: lat: -26.3714
lon: 152.838
Attractions. Pomona is notable for its relaxed streetscape of distinctive timber and art deco buildings, the heritage-listed Majestic Theatre and the walk to the top of its imposing mountain sentinel Mount Cooroora in the Tuchekoi National Park. The Majestic, built in 1921, is claimed to be the world's oldest continuously operating silent movie theatre built for that purpose.

Geographic entities mentioned:
surface_form: Mount Cooroora
instance_of: Mountain
countries: Australia
coordinates: lat: -26.3714
lon: 152.838
At the very top, it is cold and snowy all year long (&quot;EF&quot;). The lower slopes and valleys have scattered juniper and birch trees, as well as grass and desert thornplants, grading to shorter grass and then just moss higher up. Goats and Siberian ibex live in the high mountaintops, while snow leopards and small populations of brown and black bears live and hunt in the valleys.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: brown
instance_of: Mountain
coordinates: lat: -68.3
lon: 86.4167
surface_form: hunt
instance_of: Mountain
coordinates: lat: -67.1167
lon: 144.3
Geology. The Hindu Kush are made of metamorphic rock, formed about 115 million years ago, and are the product of the Eurasian-Indian collision starting around 50 million years ago. The area is seismically active and has many and frequent earthquakes. The Hindu Kush mountains contain granites from the Cenozoic as well as metamorphic rocks. The Heart Fault is to the south of Akher Chhish.

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
Akher Chhish. Akher Chhish is a -high mountain in the Hindu Kush range, Pakistan. It is covered in gigantic glaciers, typical for its altitude, and is a popular tourist site. It is one of the highest in its range, at over 7,000 meters. Acclimatization is required due to the extremely high altitude. Geology.

Geographic entities mentioned:
surface_form: akher chhish
instance_of: Mountain
The area is seismically active and has many and frequent earthquakes. The Hindu Kush mountains contain granites from the Cenozoic as well as metamorphic rocks. The Heart Fault is to the south of Akher Chhish. Geography and environment.

Geographic entities mentioned:
surface_form: akher chhish
instance_of: Mountain
The Heart Fault is to the south of Akher Chhish. Geography and environment. Akher Chhish is in the monsoon-influenced east-center of the range (&quot;Dwc&quot; or &quot;BSk&quot; climate), to the south of the cold desert (&quot;BWk&quot;) on the Afghan side, but to the west of the Greater Himalayas. The Hindu Kush are very varied in terms of climate.

Geographic entities mentioned:
surface_form: akher chhish
instance_of: Mountain
Curll. Company B served, through March 1863, independent of the battalion, mostly in West Virginia, western Maryland, and the northern part of the Shenandoah Valley. The company was present in action as South Branch Bridge, West Virginia (October 26, 1861) and at the Battle of Kernstown (March 22, 1862), and spent much of 1862 in the area of Romney, West Virginia, on duty as a scouting force.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
In August (26th) and September (12th-16th), the battalion sent scouts into Loudoun County, Virginia. The list of actions continues with Catoctin Mountain, September 14; Loudoun Valley, Va., September 25; Loudoun Valley and Summit Point, October 7; Charles Town, October 7 (Co.

Geographic entities mentioned:
surface_form: Catoctin Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6478
lon: -77.4664
surface_form: Loudoun Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.2329
lon: -77.735
After weeks of work by surveyors and others, his grave was finally located—all landmarks remembered by the survivors had been destroyed in the interim. His body was flown to Israel and after a funeral attended by all the Moetzes Gedolei HaTorah and tens of thousands of people, he was finally laid to rest on Har HaMenuchot. Works.

Geographic entities mentioned:
surface_form: Har HaMenuchot
instance_of: Mountain
countries: Israel
coordinates: lat: 31.798133333333
lon: 35.177727777778
Blaue Lacke. Blaue Lacke (German for &quot;the Blue Puddle&quot;) is a lake in the Stubai Alps in Tyrol, Austria.

Geographic entities mentioned:
surface_form: blaue lacke
instance_of: Lake
countries: Austria
coordinates: lat: 46.9914
lon: 11.1761
Article 27 of her will stated, &quot;I have lately caused to be erected on a lot owned by me in Marion Lower Village, a building... to be known as 'The Tabor Academy'.&quot; It is rumored that she named the school after Mount Tabor, a mountain of biblical importance near the Sea of Galilee. From its creation, the academy was co-educational just as Mrs.

Geographic entities mentioned:
surface_form: Mount Tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
Sestra (Moscow Oblast). The Sestra () is a river in Moscow Oblast, Russia. It is a left tributary of the Dubna (Volga basin). Its source is the Senezh Lake. The length of the river is. The area of its basin is. The river freezes over in November to early January and stays icebound until late March or April. Its main tributary is the Yakhroma. The town of Klin is located on the Sestra.

Geographic entities mentioned:
surface_form: Senezh Lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 56.2
lon: 37
Sandy Valley, California. Sandy Valley is the southeasternmost unincorporated community, in Inyo County, California, located in the Mesquite Valley. The population in the 2020 for sandy valley is in census tract 8, Block 1330–1333 was of 4. History. In 2011, Sandy Valley was considered as an alternative site for the Hidden Hills Solar Electric Generation System. Economy.

Geographic entities mentioned:
surface_form: Mesquite Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.76833333
lon: -115.60388889
In 1909, Yamaoka met Abdurreshid Ibrahim. Ibrahim highly advised him to convert to Islam at a stay in Mumbai. He converted to Islam and accompanied him on a pilgrimage to Mecca, making himself the first ever Japanese pilgrim to Mecca. After Mecca, Yamaoka also visited Mount Ararat, Medina, Damascus, Jerusalem, Cairo, and Istanbul. He returned to Japan via Russia in 1910.

Geographic entities mentioned:
surface_form: Mount Ararat
instance_of: Mountain
countries: Turkey
coordinates: lat: 39.70194444444444
lon: 44.29833333333333
Taxonomy. &quot;Leucos panosi&quot; was first formally described as &quot;Rutilus panosi&quot; in 2010 by the Russian ichthyologist and the Greek ichthyologist Konstantina Iliadou with its type locality given as Trichinos Lake in Greece. It is now classified as a valid species in the genus &quot;Leucos&quot; within the subfamily Leuciscinae of the family Leuciscidae. Etymology.

Geographic entities mentioned:
surface_form: Trichinos Lake
instance_of: Lake
countries: Greece
coordinates: lat: 38.5725
lon: 21.5525
Distribution and habitat. &quot;Leucos panosi&quot; has a native range which is restricted to the upper drainage of the Achelous River in Western Greece, it has been recorded from Lakes Trichonida, Lysimachia, Ozeros and Amvrakia. It has been introduced to the lower Thyamis and lakes Pamvotida and Ziros in Epirus, as well as in Lake Taka in the Pelopponese.

Geographic entities mentioned:
surface_form: Lysimachia
instance_of: Lake
countries: Greece
coordinates: lat: 38.56666667
lon: 21.36388889
surface_form: Ozeros
instance_of: Lake
countries: Greece
coordinates: lat: 38.655833333333
lon: 21.224166666667
surface_form: Amvrakia
instance_of: Lake
countries: Greece
coordinates: lat: 38.751944444444
lon: 21.178055555556
Distribution and habitat. &quot;Leucos panosi&quot; has a native range which is restricted to the upper drainage of the Achelous River in Western Greece, it has been recorded from Lakes Trichonida, Lysimachia, Ozeros and Amvrakia. It has been introduced to the lower Thyamis and lakes Pamvotida and Ziros in Epirus, as well as in Lake Taka in the Pelopponese.

Geographic entities mentioned:
surface_form: Pamvotida
instance_of: Lake
countries: Greece
coordinates: lat: 39.6625
lon: 20.885
The language exhibits mutual intelligibility with the other languages of the region including Thadou, Hmar, Vaiphei, Simte, Kom, Gangte and other languages. Etymology. The term &quot;Paithe&quot; originated in the Lushai Hills region. The Lushais used terms &quot;Pai&quot; or &quot;Poi&quot; to refer to central and southern Chin tribes, who tie their hair up.

Geographic entities mentioned:
surface_form: Lushai Hills
instance_of: Mountain
countries: India
coordinates: lat: 23.166666666667
lon: 92.833333333333
The English translation of Mrouj is &quot;The Meadows&quot;
Location. Mrouj is one of the Lebanese villages of the Metn district in Mount Lebanon. Mrouj overlooks Mount Sannine, Beskenta and Kesrouan to the north, and Metn south to the south. Elevation is 1,220 meters above sea level and is about 32 km from the capital Beirut.

Geographic entities mentioned:
surface_form: Mount Sannine
instance_of: Mountain
countries: Lebanon
coordinates: lat: 33.95
lon: 35.866666666667
Aghnaskeagh Cairns. Aghnaskeagh Cairns is a chambered cairn and portal tomb forming a national monument in County Louth, Ireland. Location. Aghnaskeagh Cairns are located south of Slieve Foy, to the west of the N1. History and archaeology. The two cairns may have been connected by a gallery. Portal tomb. The northern cairn is a dolmen (portal tomb) with the capstone missing.

Geographic entities mentioned:
surface_form: Slieve Foy
instance_of: Mountain
countries: Ireland
coordinates: lat: 54.08055556
lon: -6.36194444
Geography. Ruhengeri lies near the twin lakes of Lake Burera and Lake Ruhondo and is the gateway city to Volcanoes National Park and the famous mountain gorillas in the north-western part of the country. The city's proximity to the Volcanoes National Park has made it a popular tourist destination with several restaurants and hotels mainly aimed at visitors to the national park.

Geographic entities mentioned:
surface_form: Lake Burera
instance_of: Lake
countries: Rwanda
coordinates: lat: -1.45
lon: 29.78
surface_form: Lake Ruhondo
instance_of: Lake
countries: Rwanda
coordinates: lat: -1.4863888888889
lon: 29.748888888889
Slovenes began to settle in large numbers around the Cleveland area in the 1880s, particularly in the area that would become known as Newburgh. Other sizeable communities grew in the Collinwood and Euclid neighborhoods. By the 1890s, a larger community formed along St. Clair Avenue, eventually building up along eastern Cleveland and Lake Erie.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
The name changed to the current one in 1930. In addition to advising the forestry industry, the RSFS manages its own woodland, Cashel Forest at Cashel, near Milarrochy Bay on the east shore of Loch Lomond. The RSFS purchased the site in 1996 and since then has been establishing a native woodland to demonstrate best practice in woodland management and growing timber.

Geographic entities mentioned:
surface_form: Loch Lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
Capovalle. Capovalle (before 1907 Hano;) is a town and &quot;comune&quot; in the Italian province of Brescia, in Lombardy in the upper Valle Sabbia.

Geographic entities mentioned:
surface_form: Valle Sabbia
instance_of: Valley
countries: Italy
coordinates: lat: 45.7158
lon: 10.4181
Moston Brook. Moston Brook is a stream in Greater Manchester in north-west England and a tributary of the River Irk. The brook is formed at the confluence of Bower Brook and Hole Bottom Brook. This occurs near the Rochdale Canal in Failsworth in the Metropolitan Borough of Oldham.

Geographic entities mentioned:
surface_form: River Irk
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 53.4869
lon: -2.24504
The remaining parts of the brook that avoided being culverted are used for recreation by the local community. Course. The brook flows approximately 3.7 miles (6.0 km) from its source (the confluence of Bower Brook and Hole Bottom Brook) to its confluence with the River Irk. It forms part of the River Irwell drainage basin. The source of Moston Brook is now hidden.

Geographic entities mentioned:
surface_form: River Irk
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 53.4869
lon: -2.24504
Peroz was avenged by his grandson Khosrow I (), who in collaboration with the First Turkic Khaganate destroyed the Hephthalites in 560. Since Bahram I (), the Sasanian monarchs had primarily resided in Gundeshapur in southern Iran, due to its convenient position between the Iranian plateau and the Mesopotamian plain.

Geographic entities mentioned:
surface_form: Iranian plateau
instance_of: Plateau
countries: Iran
coordinates: lat: 36.283333
lon: 59.05
Additional fortifications were later made to the wall, possibly as late as the reigns of Kavad I and Khosrow I. The wall, stretching from the Caspian coast to Pishkamar, was the largest of its time, and the biggest Iranian investment in military infrastructure in the late antique and medieval periods. Coinage and imperial ideology.

Geographic entities mentioned:
surface_form: Caspian
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
(&quot;Under construction.&quot;)
There are about 32 volcanic systems in Iceland. Volcanic system means a volcano-tectonic fissure system and – very often a bigger volcano, a so-called central volcano which in most cases is a stratovolcano and may contain a caldera. Askja. - Askja; An active volcano in the central highlands. A complex of nested calderas within the Dyngjufjöll mountains.

Geographic entities mentioned:
surface_form: central highlands
instance_of: Plateau
countries: Iceland
coordinates: lat: 64.84
lon: -18.11
Askja. - Askja; An active volcano in the central highlands. A complex of nested calderas within the Dyngjufjöll mountains. The Askja system includes, for example, the Herðubreið tabular volcano, the Herðubreiðartögl palagonite ridge and the shield volcanoes Kollóttadyngja, Flatadyngja and Svartadyngja. &quot;(Part of the North volcanic zone (NVZ))&quot;.

Geographic entities mentioned:
surface_form: Herðubreið
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.183333333333
lon: -16.35
Bárðarbunga. - Bárðarbunga; An active stratovolcano located under the Vatnajökull glacier. The second highest mountain in Iceland, above sea level, and part of a volcanic system that is approximately long and wide. Historically there are large eruptions every 250–600 years. &quot;Part of the East volcanic zone (EVZ)&quot;.

Geographic entities mentioned:
surface_form: Bárðarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.640833333333
lon: -17.527777777778
Brennisteinsfjöll. - Brennisteinsfjöll; A minor system on the Reykjanes Peninsula in the southwest. crater rows and small shield volcanoes. &quot;Part of the Reykjanes volcanic zone (RVZ)&quot;. See &quot;Chronology of Eruptions&quot; below: &quot;Brennisteinsfjöll 5200BP&quot;, &quot;Brennisteinsfjöll 1340&quot;, &quot;Brennisteinsfjöll 1341&quot;
Dyngjufjöll.

Geographic entities mentioned:
surface_form: Brennisteinsfjöll
instance_of: Mountain
Plateau
countries: Iceland
coordinates: lat: 63.916666666667
lon: -21.833333333333
There is not a central volcano. Eldfell. - Eldfell, a volcanic cone on the island of Heimaey. It formed in a volcanic eruption which began without warning on the eastern side of Heimaey, in the Westman Islands, on 23 January 1973. The eruption caused a major crisis for the island and led to its temporary evacuation.

Geographic entities mentioned:
surface_form: Eldfell
instance_of: Mountain
countries: Iceland
coordinates: lat: 63.4333008635
lon: -20.2487692886
&quot;Part of the East volcanic zone (EVZ)&quot;. See &quot;Chronology of Eruptions&quot; below: &quot;Eldgjá 934 or 939&quot;
Esja / Esjan. - Esja, (Esjan), a mountain situated in the south-west of Iceland, about ten kilometres north of Iceland's capital city Reykjavík. Esja is not a single mountain, but a volcanic mountain range, made from basalt and tuff.

Geographic entities mentioned:
surface_form: Esja
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.2599926025
lon: -21.651530003
&quot;Part of the East volcanic zone (EVZ)&quot;. See &quot;Chronology of Eruptions&quot; below: &quot;Eyjafjallajökull 1612&quot;, &quot;Eyjafjallajökull 1821-23&quot;, &quot;Eyjafjallajökull 2010 March&quot;, &quot;Eyjafjallajökull 2010 April&quot;
Fagradalsfjall. - Fagradalsfjall; is an active tuya volcano formed in the Last Glacial Period on the Reykjanes Peninsula, around from Reykjavík.

Geographic entities mentioned:
surface_form: Fagradalsfjall
instance_of: Mountain
Plateau
countries: Iceland
coordinates: lat: 63.905
lon: -22.2725
&quot;Part of the Reykjanes volcanic zone (RVZ)&quot;. See &quot;Chronology of Eruptions&quot; below: &quot;Fagradalsfjall 2021&quot;, &quot;Fagradalsfjall 2022&quot;, &quot;Fagradalsfjall 2023&quot;
Festarfjall. - Festarfjall, an exposed tuya mountain on the south coast of the Reykjanes Peninsula near the Fagradalsfjall volcanic system and Grindavík.

Geographic entities mentioned:
surface_form: Fagradalsfjall
instance_of: Mountain
Plateau
countries: Iceland
coordinates: lat: 63.905
lon: -22.2725
Gjálp. Gjálp is a hyaloclastite ridge (tindar) under the Vatnajökull glacier shield. It originated in an eruption series in 1996 which is probably part of the Grímsvötn volcanic system,
It was the first modern technical monitoring and analysis of a subglacial eruption under a thick ice cover with a resulting jökulhlaup. The volume of meltwater was around 4 km3.

Geographic entities mentioned:
surface_form: Grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
See &quot;Chronology of Eruptions&quot; below: &quot; Kerið 6,500 BP&quot;. Grímsvötn. - Grímsvötn; an active volcano with a (partially subglacial) fissure system located in Vatnajökull National Park. Including the Skaftá eruption of 1783, Grímsvötn is probably the most eruptive volcano system in Iceland. The Lakagígar lava field alone is estimated to have produced about of lava.

Geographic entities mentioned:
surface_form: Grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
&quot;Part of the East volcanic zone (EVZ)&quot;. See &quot;Chronology of Eruptions&quot; below: &quot;Stórhöfði peninsula 6,000 BP&quot;, &quot;Helgafell (on Heimaey) 3,000 BC&quot;
Hengill. - Hengill, A volcanic table mountain the southwest, to the south of Þingvellir. The volcano is still active, evidenced by its numerous hot springs and fumaroles.

Geographic entities mentioned:
surface_form: Hengill
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.085555555556
lon: -21.313611111111
The volcano is still active, evidenced by its numerous hot springs and fumaroles. &quot;Part of the Reykjanes volcanic zone (RVZ)&quot;. See &quot;Chronology of Eruptions&quot; below: &quot;Hengill 1130 BC&quot;
Herðubreið. - Herðubreið, is a tuya in northern part of Vatnajökull National Park, close to Askja volcano. It formed beneath the icesheet during the last glacial period. Hofsjökull.

Geographic entities mentioned:
surface_form: Herðubreið
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.183333333333
lon: -16.35
The largest active volcano in the country, situated in the west of the Highlands
See chronology below: &quot;Hofsjökull 2,500,000-11,000&quot;, &quot;Hofsjökull 2015&quot;
Holuhraun. - Holuhraun, A lava field just north of the Vatnajökull ice cap, in the Icelandic Highlands, in Suður-Þingeyjarsýsla, Northeastern Region. The lava field was created by fissure eruptions.

Geographic entities mentioned:
surface_form: Icelandic Highlands
instance_of: Plateau
countries: Iceland
coordinates: lat: 64.84
lon: -18.11
The lava field was created by fissure eruptions. &quot;(Part of the North volcanic zone (NVZ))&quot;. See &quot;Chronology of Eruptions&quot; below: &quot;Holuhraun 2014-15&quot;
Hrómundartindur. - Hrómundartindur, is a mountain north of Hveragerði. Hvalbakur. - Hvalbakur. a small, uninhabited island is the easternmost point of Iceland.

Geographic entities mentioned:
surface_form: Hrómundartindur
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.06666667
lon: -21.21666667
Located in the Austurland region, offshore, it is long and up to wide, with its highest point above sea level. It appears on maps from 1761
Hvannadalshnúkur. - Hvannadalshnúkur, a pyramidal peak on the northwestern rim of the summit crater of the Öræfajökull volcano in Vatnajökull National Park, Iceland. Its summit is the highest point in the country. Hveravellir.

Geographic entities mentioned:
surface_form: Öræfajökull volcano
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.025436111111
lon: -16.642063888889
&quot;Part of the West volcanic zone (WVZ)&quot;. See &quot;Chronology of Eruptions&quot; below: &quot;Hveravellir 5,800 BC&quot;, &quot;Hveravellir 1000 BC&quot;
Hverfjall. - Hverfjall, (Hverfell) is a tephra cone or Phreatomagmatic eruption in northern Iceland. The eruption was in the southern part of the Krafla fissure swarm. &quot;(Part of the North volcanic zone (NVZ))&quot;.

Geographic entities mentioned:
surface_form: Hverfjall
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.6044691176
lon: -16.8719421252
&quot;Part of the West volcanic zone (WVZ)&quot;. See &quot;Chronology of Eruptions&quot; below: &quot;Hveravellir 5,800 BC&quot;, &quot;Hveravellir 1000 BC&quot;
Hverfjall. - Hverfjall, (Hverfell) is a tephra cone or Phreatomagmatic eruption in northern Iceland. The eruption was in the southern part of the Krafla fissure swarm. &quot;(Part of the North volcanic zone (NVZ))&quot;.

Geographic entities mentioned:
surface_form: Krafla
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.733333333333
lon: -16.783333333333
The presence of water in magma reduces the melting temperature, which may also play a role in enhancing Icelandic volcanism. Ingólfsfjall. - Ingólfsfjall; A tuya in the vicinity of Hveragerði originating from subglacial eruptions and consisting mostly of basalt and palagonite. &quot;Part of the South Iceland Seismic Zone (SISZ)&quot;.

Geographic entities mentioned:
surface_form: Ingólfsfjall
instance_of: Mountain
countries: Iceland
coordinates: lat: 63.99472222
lon: -21.02916667
&quot;Part of the Reykjanes volcanic zone (RVZ)&quot;. See &quot;Chronology of Eruptions&quot; below: &quot;Keilir 2,500,000-11,000&quot;
Kerlingarfjöll. - Kerlingarfjöll, a mountain range in the Highlands of Iceland near the Kjölur highland road. Part of a large tuya volcano system with hot springs and rivulets, as well as red volcanic rhyolite stone. Kolbeinsey.

Geographic entities mentioned:
surface_form: Highlands of Iceland
instance_of: Plateau
countries: Iceland
coordinates: lat: 64.84
lon: -18.11
surface_form: Kjölur
instance_of: Plateau
countries: Iceland
coordinates: lat: 64.7
lon: -19.4
&quot;Part of the North volcanic zone (NVZ)&quot;. Krafla. - Krafla, a volcanic caldera of about 10 km in diameter with a 90 km long fissure zone. It is located in the north of Iceland in the Mývatn region and is situated on the Iceland hotspot atop the Mid-Atlantic Ridge, which forms the divergent boundary between the North American Plate and the Eurasian Plate.

Geographic entities mentioned:
surface_form: Krafla
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.733333333333
lon: -16.783333333333
Krafla. - Krafla, a volcanic caldera of about 10 km in diameter with a 90 km long fissure zone. It is located in the north of Iceland in the Mývatn region and is situated on the Iceland hotspot atop the Mid-Atlantic Ridge, which forms the divergent boundary between the North American Plate and the Eurasian Plate. Its highest peak reaches up to 818 m and it is 2 km in depth.

Geographic entities mentioned:
surface_form: Mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
- Laki. Lakagigar is a volcanic fissure that bisects Laki mountain in the western part of Vatnajökull National Park. Lakagígar is part of the Grímsvötn volcanic system. The pollution from the 1783 eruption led to the deaths of over 50% of Iceland's livestock, and the destruction of the vast majority of crops.

Geographic entities mentioned:
surface_form: Grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
See &quot;Chronology of Eruptions&quot; below: &quot;Landmannalaugar 1477&quot;
Langjökull. - Langjökull, (&quot;long glacier&quot;) is the second largest ice cap in Iceland, (953 km2), after Vatnajökull. It is situated in the west of the interior or Highlands of Iceland and can be seen clearly from Haukadalur. The volume is 195 km3 and up to thick.

Geographic entities mentioned:
surface_form: Highlands of Iceland
instance_of: Plateau
countries: Iceland
coordinates: lat: 64.84
lon: -18.11
&quot;Part of the Snæfellsnes volcanic belt (SVB))&quot;. See &quot;Chronology of Eruptions&quot; below: &quot;Ljósufjöll 960&quot;
Loki-Fögrufjöll. - Loki-Fögrufjöll, a subglacial volcano under the Vatnajökull glacier, within the Bárðarbunga fissure system. It is independent of Bárðarbunga itself. &quot;Part of the East volcanic zone (EVZ)&quot;.

Geographic entities mentioned:
surface_form: Loki-Fögrufjöll
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.480277777778
lon: -17.832222222222
surface_form: Bárðarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.640833333333
lon: -17.527777777778
See &quot;Chronology of Eruptions&quot; below: &quot;Loki-Fögrufjöll 1910&quot;, &quot;Loki-Fögrufjöll 1986&quot;, &quot;Loki-Fögrufjöll 1991&quot;, &quot;Loki-Fögrufjöll 2006&quot;, &quot;Loki-Fögrufjöll 2008&quot;, &quot;Loki-Fögrufjöll 2011&quot;. Lýsuhóll. - Lýsuhóll?, (also known as Lysukard or Helgrindur), is the smallest volcano in Iceland. It is centrally located on Snaefellsnes Peninsula.

Geographic entities mentioned:
surface_form: Helgrindur
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.8876702451
lon: -23.3284568109
It is centrally located on Snaefellsnes Peninsula. It includes a chain of small, basaltic cinder cones. &quot;Part of the Snæfellsnes volcanic belt (SVB)&quot;. The last eruption of Lysuhóll is not dated. Mývatn (fires). - The Mývatn fires were a series of fires at Krafla that raged from 1724 to 1729. Lava flowed into Mývatn and the explosive crater Víti at Krafla was formed. Nýey.

Geographic entities mentioned:
surface_form: Mývatn fires
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
It disappeared within a year. Note: The tiny skerry called Eldeyjarboði may be its remnants&quot;. (Part of the Reykjanes volcanic zone (RVZ))&quot;. See &quot;Chronology of Eruptions&quot; below: &quot;Nýey 1783&quot;,
Öræfajökull. - Öræfajökull, An ice-covered active volcano, it lies within the Vatnajökull National Park. &quot;(Part of the Öræfajökull volcanic belt (OVB))&quot;.

Geographic entities mentioned:
surface_form: Öræfajökull
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.025436111111
lon: -16.642063888889
&quot;(Part of the Öræfajökull volcanic belt (OVB))&quot;. See &quot;Chronology of Eruptions&quot; below: &quot;Öræfajökull 1357&quot;, &quot;Öræfajökull 1727&quot;
Prestahnúkur. - Prestahnúkur, is a volcano in the Central Highlands, a part of the Langjökull glacier. It consists of rhyolite and has a small magma chamber. &quot;(Part of the North volcanic zone (NVZ)&quot;.

Geographic entities mentioned:
surface_form: Prestahnúkur
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.6
lon: -20.58
It is part of Reykjanes Volcanic Belt like the 3-6 (depending on author) other volcanic systems on Reykjanes Peninsula. No volcanic eruption had occurred for 815 years on the Peninsula until 19 March 2021 when a fissure vent appeared in Geldingadalir to the south of Fagradalsfjall mountain. &quot;Part of the Reykjanes volcanic zone (RVZ)&quot;. See &quot;Fagradalsfjall&quot; in index.

Geographic entities mentioned:
surface_form: Fagradalsfjall
instance_of: Mountain
Plateau
countries: Iceland
coordinates: lat: 63.905
lon: -22.2725
&quot;(Part of the Öræfajökull volcanic belt (OVB))&quot;. Snæfellsjökull. - Snæfellsjökull The 700,000-year-old stratovolcano, the only large central volcano on the Snæfellsnes Peninsula, has many pyroclastic cones on its flanks, plus upper-flank craters and lower-flank basaltic lava flows. Several holocene eruptions have originated from the summit crater and have produced felsic material.

Geographic entities mentioned:
surface_form: Snæfellsjökull
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.8071204861
lon: -23.7762279203
See &quot;Chronology of Eruptions&quot; below: &quot;Surtsey 1963&quot;
Theistareykjarbunga. - Theistareykjarbunga (Þeistareykjarbunga); &quot;Part of the North volcanic zone (EVZ)&quot;. See &quot;Chronology of Eruptions&quot; below: &quot;Theistareykjarbunga 9500 BC&quot;, &quot;Theistareykjarbunga 6800 BC&quot;, &quot;Theistareykjarbunga 900 BC&quot;
Þingvellir / Thingvellir.

Geographic entities mentioned:
surface_form: Theistareykjarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.88
lon: -16.84
It has an elevation of. &quot;Part of the Öræfajökull volcanic belt (ÖVB)&quot;. Thríhnúkagígur. - Thrihnukagigur (Thríhnákagígur), (&quot;Three Peaks Crater&quot;) is a dormant volcano in the volcanic system of Brennisteinsfjöll near Reykjavík, Iceland. Covering a area and a depth of, it has not erupted in the past 4000 years.

Geographic entities mentioned:
surface_form: Brennisteinsfjöll
instance_of: Mountain
Plateau
countries: Iceland
coordinates: lat: 63.916666666667
lon: -21.833333333333
See &quot;Chronology of Eruptions&quot; below: &quot;Torfajökull 870&quot;, &quot;Torfajökull 1477&quot;
Trölladyngja. - Trölladyngja, Situated in the Ódáðahraun lava field, it is the biggest Icelandic shield volcano, with a height of and rising almost 600 metres above the surrounding desert and lava fields. It is about 10 kilometres in diameter.

Geographic entities mentioned:
surface_form: Trölladyngja
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.893055555556
lon: -17.254722222222
It is not to be confused with the Krýsuvík-Trölladyngja volcanic system on the Reykjanes Peninsula. &quot;(Part of the North volcanic zone (NVZ))&quot;
See &quot;Chronology of Eruptions&quot; below: &quot;Trölladyngja 1961&quot;, (&quot;Note: there are claims (Trölladyngja) that the last eruption was 5,000 years ago.&quot;)
Tungnafellsjökull. - Tungnafellsjökull, a glacier and volcano in Iceland.

Geographic entities mentioned:
surface_form: Trölladyngja
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.893055555556
lon: -17.254722222222
- Vatnajökull; (&quot;Glacier of Lakes&quot;, &quot;Vatna Glacier&quot;) is the largest and most voluminous ice cap in Iceland. It is in the south-east of the island, covering approximately 10% of the country. The Vatnajökull glacier embraces seven identified subglacial volcanoes, of which the best-known are Grímsvötn, Bárðarbunga, and Öraefajökull.

Geographic entities mentioned:
surface_form: Grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
surface_form: Bárðarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.640833333333
lon: -17.527777777778
See &quot;Chronology of Eruptions&quot; below: &quot;Vatnaöldur 870;&quot;
Veiðivötn. - Veiðivötn; &quot;Part of the East volcanic zone (EVZ)&quot;. See &quot;Chronology of Eruptions&quot; below: &quot;Veiðivötn 6700BC;&quot;; &quot;Veiðivötn 1200BC&quot;; &quot;Veiðivötn 940&quot;, &quot;Veiðivötn 1477&quot;. See: Veiðivötn image in Gallery. Vestmannaeyjar.

Geographic entities mentioned:
surface_form: Veiðivötn
instance_of: Lake
countries: Iceland
coordinates: lat: 64.11613889
lon: -18.84797222
Includes: Bárðarbunga, Bláhnjúkur, Brennisteinsalda, Eldgjá, Eyjafjallajökull, Gjálp, Grímsvötn, central volcano Hágöngur (), Hekla, Katla, Lakagigar, Laki, Þjórsá Lava, Þórólfsfell, Surtsey, Thordarhyrna (Þórðarhyrna), Tindfjallajökull, Torfajökull, Vatnafjöll, several volcanoes in Vatnajökull, Vatnaöldur, Vestmannaeyjar (Westman Islands), central volcano Vonarskarð. Kolbeinsey Ridge (KR).

Geographic entities mentioned:
surface_form: Bárðarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.640833333333
lon: -17.527777777778
surface_form: Bláhnjúkur
instance_of: Mountain
countries: Iceland
coordinates: lat: 63.9768
lon: -19.0681
surface_form: Brennisteinsalda
instance_of: Mountain
countries: Iceland
coordinates: lat: 63.980833
lon: -19.145833
surface_form: Grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
surface_form: Vatnaöldur
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.119533548
lon: -18.9128769387
North volcanic zone (NVZ). North of Iceland, the Mid-Atlantic Ridge is called Kolbeinsey Ridge (KR) and is connected to the North Volcanic Zone via the Tjörnes Fracture Zone (TFZ). Includes: Askja, Dimmuborgir, Fremrinámur, Herðubreið, Hverfjall, Kollóttadyngja, Krafla, Kverkfjöll, many volcanoes in the Mývatn district, Rauðhólar, Theistareykjarbunga, Trölladyngja
Öræfajökull volcanic belt (ÖVB).

Geographic entities mentioned:
surface_form: Herðubreið
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.183333333333
lon: -16.35
surface_form: Hverfjall
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.6044691176
lon: -16.8719421252
surface_form: Krafla
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.733333333333
lon: -16.783333333333
surface_form: Mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
surface_form: Theistareykjarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.88
lon: -16.84
surface_form: Trölladyngja
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.893055555556
lon: -17.254722222222
Includes: Askja, Dimmuborgir, Fremrinámur, Herðubreið, Hverfjall, Kollóttadyngja, Krafla, Kverkfjöll, many volcanoes in the Mývatn district, Rauðhólar, Theistareykjarbunga, Trölladyngja
Öræfajökull volcanic belt (ÖVB). The Öræfajökull volcanic belt (ÖVB, also Öræfi volcanic belt) is an intraplate volcanic belt, connected to the Eurasian plate. Reykjanes volcanic zone (RVZ).

Geographic entities mentioned:
surface_form: Öræfajökull
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.025436111111
lon: -16.642063888889
Includes: Bláfjöll, Brennisteinsfjöll, Búrfell (Hafnarfjörður), Eldborg í Bláfjöllum, Eldvörp–Svartsengi, Fagradalsfjall, Heiðin há, Helgafell (Hafnarfjörður), Hengill (also listed under WVZ), Keilir, Krýsuvík (volcanic system), Krýsuvík fires, Leitin, Rauðhólar (Reykjavík), Reykjanes volcanic system, Stóra-Eldborg undir Geitahlíð, Svartsengi Power Station, Sveifluháls, Vífilsfell, Þorbjörn (mountain)
Snæfellsnes volcanic belt (SVB).

Geographic entities mentioned:
surface_form: Brennisteinsfjöll
instance_of: Mountain
Plateau
countries: Iceland
coordinates: lat: 63.916666666667
lon: -21.833333333333
surface_form: Fagradalsfjall
instance_of: Mountain
Plateau
countries: Iceland
coordinates: lat: 63.905
lon: -22.2725
surface_form: Hengill
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.085555555556
lon: -21.313611111111
surface_form: Sveifluháls
instance_of: Mountain
countries: Iceland
coordinates: lat: 63.9365657828
lon: -22.0030412838
surface_form: Vífilsfell
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.0362705933
lon: -21.5566141304
The Snæfellsnes volcanic belt (SVB) is an intraplate volcanic belt, connected to the North American plate. It is proposed that the east–west line from the Grímsvötn volcano in the Mid-Iceland Belt (MIB) to the SVB shows the movement of the North American Plate over the Iceland hotspot. Includes: Snæfellsjökull and smaller volcanoes on Snæfellsnes, plus Helgafell. South Iceland Seismic Zone (SISZ).

Geographic entities mentioned:
surface_form: Snæfellsjökull
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.8071204861
lon: -23.7762279203
The Tjörnes and Reykjanes Fracture Zones are found striking about 75°N to 80°W. West volcanic zone (WVZ). Includes: Geitlandsjökull, Geysir, Hengill (also listed under RFZ), Hlöðufell, Hveravellir, Skjaldbreiður, Stóra-Björnsfell, Þórisjökull. Grímsvötn eruptivity. Grímsvötn, including the Skaftá eruption of 1783, is probably the most eruptive volcano system.

Geographic entities mentioned:
surface_form: Hengill
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.085555555556
lon: -21.313611111111
surface_form: Hlöðufell
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.4181882323
lon: -20.5436720066
surface_form: Stóra-Björnsfell
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.49666667
lon: -20.71138889
surface_form: Þórisjökull
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.541944444444
lon: -20.715555555556
West volcanic zone (WVZ). Includes: Geitlandsjökull, Geysir, Hengill (also listed under RFZ), Hlöðufell, Hveravellir, Skjaldbreiður, Stóra-Björnsfell, Þórisjökull. Grímsvötn eruptivity. Grímsvötn, including the Skaftá eruption of 1783, is probably the most eruptive volcano system. The Lakagígar lava field alone is estimated to have produced about of lava.

Geographic entities mentioned:
surface_form: Grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
As a member of the Supreme Council of the Republic of Karakalpakstan 8, 9, 10 and 12 convocations Ch Abdirov took an active part in political work, he headed the Committee on Environment and Nature Protection and participated in the drafting of legislation on the environment and addressing socio- environmental problems of the population of the Aral Sea coast.

Geographic entities mentioned:
surface_form: Aral Sea
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
Tofte, Minnesota. Tofte () is an unincorporated community in Tofte Township, Cook County, Minnesota, United States. Location. Tofte is on the North Shore of Lake Superior, within the Superior National Forest, 27 miles southwest of the city of Grand Marais and 56 miles northeast of the city of Two Harbors.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445