Sarmila/GeoWiki-Features huggingface dataset:
Tabaristan. Tabaristan or Tabarestan (;; from,) was a mountainous region located on the Caspian coast of northern Iran. It corresponded to the present-day province of Mazandaran, which became the predominant name of the area from the 11th-century onwards. Pre-Islamic era. Tabaristan was named after the Tapurians, who had been deported there from Parthia by the Parthian king Phraates I ().

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
This made it China's deadliest earthquake since the 2014 Ludian earthquake. Tectonic setting. The Jishi Shan range lies in the easternmost segment of the Qilian Mountains that form part of the northern margin of the Tibetan Plateau. The plateau is a thickened zone of continental crust formed as a result of the ongoing collision between the Indian plate and the Eurasian plate.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
These two fault structures represents a transpression zone between the right-lateral Riyue Shan Fault in the north and the left-lateral Qinling Fault in the south. Two prehistoric earthquakes were identified along the fault zone including one that may have destroyed Lajia. GNSS velocity observations indicate the Laji Shan Fault produces insignificant thrust and strike-slip movements.

Geographic entities mentioned:
surface_form: Riyue Shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 36.56388889
lon: 100.99305556
Wildstrubel Glacier. The Wildstrubel Glacier () is a long glacier (2005) situated in the Bernese Alps in the canton of Valais, on the eastern slopes of the Wildstrubel. In 1973 it had an area of

Geographic entities mentioned:
surface_form: Wildstrubel
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.400277777778
lon: 7.5286111111111
Ilha dos Marinheiros. Ilha dos Marinheiros (&quot;Island of the Sailors&quot;) is an island located in the south part of a lagoon named Lagoa dos Patos, located in the municipality of Rio Grande, in the state of Rio Grande do Sul, Brazil. It is situated on the west bank of that lagoon.

Geographic entities mentioned:
surface_form: Lagoa dos Patos
instance_of: Lake
countries: Brazil
coordinates: lat: -31.15
lon: -51.39
Nastapoka arc. The Nastapoka arc is a curved segment of the southeastern shore of Hudson Bay in Quebec, Canada, that extends from the most northerly of the Hopewell Islands to Long Island near the junction with James Bay. It is a prominent, near-perfect circular arc, covering more than 160° of a circle.

Geographic entities mentioned:
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
surface_form: nastapoka arc
instance_of: Landform
countries: Canada
coordinates: lat: 56.83333333
lon: -78.33333333
Nastapoka arc. The Nastapoka arc is a curved segment of the southeastern shore of Hudson Bay in Quebec, Canada, that extends from the most northerly of the Hopewell Islands to Long Island near the junction with James Bay. It is a prominent, near-perfect circular arc, covering more than 160° of a circle.

Geographic entities mentioned:
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: nastapoka arc
instance_of: Landform
countries: Canada
coordinates: lat: 56.83333333
lon: -78.33333333
Geology. The bedrock that comprises the shoreline and landscape that lies inland of the Nastapoka arc largely consists of Archean-age rocks of the Superior craton. In areal distribution, these rocks consist of about 60% Archean granitic plutons and granitic gneiss.

Geographic entities mentioned:
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
surface_form: nastapoka arc
instance_of: Landform
countries: Canada
coordinates: lat: 56.83333333
lon: -78.33333333
A large triangular area surrounding Richmond Gulf, which includes a short segment of the Nastapoka arc, is underlain by about of undeformed, pink and red, mainly fluvial, feldspar-rich sandstone that is interbedded with minor beds of conglomerate and basaltic, subaerial lava flows.

Geographic entities mentioned:
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
surface_form: richmond gulf
instance_of: Lake
countries: Canada
coordinates: lat: 56.24944444444444
lon: -76.29416666666667
surface_form: nastapoka arc
instance_of: Landform
countries: Canada
coordinates: lat: 56.83333333
lon: -78.33333333
These strata, which are known as the &quot;Richmond Gulf Group&quot;, rest unconformably on Archean crystalline rocks of the Superior craton and are now preserved by downfaulting only within the Richmond Gulf Graben. The graben, its faults, and the Richmond Gulf Group are unconformably overlain by the strata of the Nastapoka Group.

Geographic entities mentioned:
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
surface_form: richmond gulf
instance_of: Lake
countries: Canada
coordinates: lat: 56.24944444444444
lon: -76.29416666666667
The graben, its faults, and the Richmond Gulf Group are unconformably overlain by the strata of the Nastapoka Group. The portion of Hudson Bay immediately offshore of and partially encircled by the Nastapoka arc is underlain by Early Proterozoic strata of the Nastapoka Group.

Geographic entities mentioned:
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
surface_form: nastapoka arc
instance_of: Landform
countries: Canada
coordinates: lat: 56.83333333
lon: -78.33333333
The portion of Hudson Bay immediately offshore of and partially encircled by the Nastapoka arc is underlain by Early Proterozoic strata of the Nastapoka Group. Adjacent to the Nastapoka arc, these strata form a homocline that dips gently westward and consists of unmetamorphosed to slightly metamorphosed sandstone, stromatolite-bearing dolomite, banded iron formation, and basalt.

Geographic entities mentioned:
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
surface_form: nastapoka arc
instance_of: Landform
countries: Canada
coordinates: lat: 56.83333333
lon: -78.33333333
Adjacent to the Nastapoka arc, these strata form a homocline that dips gently westward and consists of unmetamorphosed to slightly metamorphosed sandstone, stromatolite-bearing dolomite, banded iron formation, and basalt. Further west, exposed in the Ottawa and Belcher Islands, the strata of the Nastapoka Group become highly faulted and tightly, often isoclinally, folded.

Geographic entities mentioned:
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
These strata unconformably overlie Archean strata of the Superior craton and Proterozoic Richmond Group. The unconformity between the Early Proterozoic Nastapoka Group and the underlying Archean Superior craton lies just inland of Nastapoka arc as defined by the edge of arcuate eastern coastline of Hudson Bay.

Geographic entities mentioned:
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
surface_form: nastapoka arc
instance_of: Landform
countries: Canada
coordinates: lat: 56.83333333
lon: -78.33333333
The unconformity consists of undeformed stromatolite-bearing dolomites overlying either foliated Archean granodiorite or the tilted and eroded strata of the Richmond Gulf Group. A thin, conglomeratic quartz sandstone separates the dolomites from the underlying strata and forms the base of the Nastapoka Group. Origin.

Geographic entities mentioned:
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
A thin, conglomeratic quartz sandstone separates the dolomites from the underlying strata and forms the base of the Nastapoka Group. Origin. The origin of the Nastapoka arc has been a source of disagreement and discussion among geologists, other Earth scientists, and planetary geologists.

Geographic entities mentioned:
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
surface_form: nastapoka arc
instance_of: Landform
countries: Canada
coordinates: lat: 56.83333333
lon: -78.33333333
Noting the paucity of impact structures on Earth in relation to the Moon and Mars and remarkable curvature of the shoreline of this part of Hudson Bay, Beals proposes that the Nastapoka arc is possibly part of a Precambrian extraterrestrial meteorite impact structure that is comparable in size to the Mare Crisium on the Moon.

Geographic entities mentioned:
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
surface_form: nastapoka arc
instance_of: Landform
countries: Canada
coordinates: lat: 56.83333333
lon: -78.33333333
In the same volume, Wilson evaluates Beals's interpretation and proposes an alternative hypothesis that the Nastapoka arc formed as the result of a continental-scale collision of pre-existing Archean continents and closure of an ancient ocean basin. In August 1972, Robert S. Dietz and J.

Geographic entities mentioned:
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
surface_form: nastapoka arc
instance_of: Landform
countries: Canada
coordinates: lat: 56.83333333
lon: -78.33333333
In August 1972, Robert S. Dietz and J. Paul Barringer conducted an extensive search of much of the Nastapoka arc with First Nations and Inuit canoes and fishing boats in an investigation of its impact origin.

Geographic entities mentioned:
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
surface_form: nastapoka arc
instance_of: Landform
countries: Canada
coordinates: lat: 56.83333333
lon: -78.33333333
They examined the abundant and extensive rock exposures that occur within the region of the Nastapoka arc and found no shatter cones, suevite-type or other unusual melt rocks, pseudotachylite or mylonite, radial faults or fractures, unusual injection breccias, or any other evidence of shock metamorphism.

Geographic entities mentioned:
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
surface_form: nastapoka arc
instance_of: Landform
countries: Canada
coordinates: lat: 56.83333333
lon: -78.33333333
However, other Earth scientists have proposed that the preexisting structure of an older Archean impact structure might have been reactivated by and was modified by the Trans-Hudson orogeny to form the Nastapoka arc. The deformation accompanying the Trans-Hudson orogeny could have masked evidence of such an Archean impact.

Geographic entities mentioned:
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
surface_form: nastapoka arc
instance_of: Landform
countries: Canada
coordinates: lat: 56.83333333
lon: -78.33333333
These strata, which are known as the &quot;Richmond Gulf Group&quot;, rest unconformably on Archean crystalline rocks of the Superior craton and are now preserved by downfaulting only within the Richmond Gulf Graben. The graben, its faults, and the Richmond Gulf Group are unconformably overlain by the strata of the Nastapoka Group.

Geographic entities mentioned:
surface_form: richmond gulf
instance_of: Lake
countries: Canada
coordinates: lat: 56.24944444444444
lon: -76.29416666666667
surface_form: richmond gulf
instance_of: Lake
countries: Canada
coordinates: lat: 56.24944444444444
lon: -76.29416666666667
The unconformity between the Early Proterozoic Nastapoka Group and the underlying Archean Superior craton lies just inland of Nastapoka arc as defined by the edge of arcuate eastern coastline of Hudson Bay. The unconformity consists of undeformed stromatolite-bearing dolomites overlying either foliated Archean granodiorite or the tilted and eroded strata of the Richmond Gulf Group.

Geographic entities mentioned:
surface_form: richmond gulf
instance_of: Lake
countries: Canada
coordinates: lat: 56.24944444444444
lon: -76.29416666666667
Senjōjiki Cirque. Senjōjiki Cirque (千畳敷カール) is a cirque (glacial landform) that lies just under Mount Hōken, Kiso Mountains in Nagano prefecture, Japan. It is called &quot;Senjōjiki Kaaru&quot; in Japanese. &quot;Senjōjiki&quot; means the wideness of 1000 tatami mats. Access to the cirque is easy via the &quot;Komagatake Ropeway&quot; aerial lift which runs all year from the bottom of cirque.

Geographic entities mentioned:
surface_form: Mount Hōken
instance_of: Mountain
countries: Japan
coordinates: lat: 35.781389
lon: 137.809167
Andrew Currie (sculptor). Andrew Currie (1812&ndash;1891) was a Scottish sculptor and antiquarian. His most noted works are the statue of James Hogg at St Mary's Loch (1860) (sometimes called the Ettrick Shepherd), the statue of Robert the Bruce on the esplanade at Stirling Castle (1876), and the figures of Edie Ochiltree and Old Mortality on the Scott Monument. Life.

Geographic entities mentioned:
surface_form: St Mary's Loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.492256
lon: -3.191433
It is situated in the district of Mecklenburgische Seenplatte of the state of Mecklenburg-Vorpommern. The town of Wesenberg can be found at the south-west end of the lake. The lake has an elevation of and a surface area of. The navigable River Havel flows through the Woblitzsee, entering via a channel from the Großer Labussee. The river exits the lake at Wesenburg via a channel to the Wangnitzsee.

Geographic entities mentioned:
surface_form: Großer Labussee
instance_of: Lake
countries: Germany
coordinates: lat: 53.308055555556
lon: 12.953611111111
surface_form: woblitzsee
instance_of: Lake
countries: Germany
coordinates: lat: 53.296944444444
lon: 12.994166666667
surface_form: labussee
instance_of: Lake
countries: Germany
coordinates: lat: 53.205
lon: 12.891666666667
The lake has an elevation of and a surface area of. The navigable River Havel flows through the Woblitzsee, entering via a channel from the Großer Labussee. The river exits the lake at Wesenburg via a channel to the Wangnitzsee. The Kammer Canal also connects to the Woblitzsee, allowing vessels to reach the Zierker See and Neustrelitz.

Geographic entities mentioned:
surface_form: Wangnitzsee
instance_of: Lake
countries: Germany
coordinates: lat: 53.243611111111
lon: 13.066388888889
The river exits the lake at Wesenburg via a channel to the Wangnitzsee. The Kammer Canal also connects to the Woblitzsee, allowing vessels to reach the Zierker See and Neustrelitz. The lake is navigable between these three entrances, and navigation is administered as part of the Obere–Havel–Wasserstraße.

Geographic entities mentioned:
surface_form: Zierker See
instance_of: Lake
countries: Germany
coordinates: lat: 53.361513888889
lon: 13.035963888889
surface_form: woblitzsee
instance_of: Lake
countries: Germany
coordinates: lat: 53.296944444444
lon: 12.994166666667
Woblitzsee. Woblitzsee is a lake in the Mecklenburg Lake District, in Germany. It is situated in the district of Mecklenburgische Seenplatte of the state of Mecklenburg-Vorpommern. The town of Wesenberg can be found at the south-west end of the lake. The lake has an elevation of and a surface area of.

Geographic entities mentioned:
surface_form: woblitzsee
instance_of: Lake
countries: Germany
coordinates: lat: 53.296944444444
lon: 12.994166666667
It was based on the area south of Ipswich and stretched toward the New South Wales border, although in subsequent redistributions was reduced in size away from the growing Brisbane area. It was named after the Fassifern Valley. Fassifern was a safe National district for most of its existence.

Geographic entities mentioned:
surface_form: Fassifern Valley
instance_of: Valley
countries: Australia
coordinates: lat: -27.810944444444
lon: 152.66505555556
Tröndelsee. Tröndelsee is a lake in Kiel, Schleswig-Holstein, Germany. At an elevation of 30 m, its surface area is 24 ha.

Geographic entities mentioned:
surface_form: tröndelsee
instance_of: Lake
countries: Germany
coordinates: lat: 54.305
lon: 10.1725
Tröndelsee. Tröndelsee is a lake in Kiel, Schleswig-Holstein, Germany. At an elevation of 30 m, its surface area is 24 ha.

Geographic entities mentioned:
surface_form: tröndelsee
instance_of: Lake
countries: Germany
coordinates: lat: 54.305
lon: 10.1725
surface_form: kiel
instance_of: Mountain
countries: Germany
coordinates: lat: 50.4081
lon: 12.4697
Vuolep Sårjåsjávrre. Vuolep Sårjåsjávrre () is a lake which lies on the border between Norway and Sweden. The western part lies in Fauske Municipality in Nordland county, Norway, and the eastern part lies in Jokkmokk Municipality in Norrbotten County, Sweden. The lake lies just to the east of the large Blåmannsisen glacier and smaller neighboring lake Bajep Sårjåsjávrre ().

Geographic entities mentioned:
surface_form: Bajep Sårjåsjávrre
instance_of: Lake
countries: Norway
coordinates: lat: 67.2178
lon: 16.2662
surface_form: sårjåsjávrre
instance_of: Lake
countries: Sweden
Norway
coordinates: lat: 67.221111111111
lon: 16.356111111111
Vuolep Sårjåsjávrre. Vuolep Sårjåsjávrre () is a lake which lies on the border between Norway and Sweden. The western part lies in Fauske Municipality in Nordland county, Norway, and the eastern part lies in Jokkmokk Municipality in Norrbotten County, Sweden. The lake lies just to the east of the large Blåmannsisen glacier and smaller neighboring lake Bajep Sårjåsjávrre ().

Geographic entities mentioned:
surface_form: sårjåsjávrre
instance_of: Lake
countries: Sweden
Norway
coordinates: lat: 67.221111111111
lon: 16.356111111111
surface_form: vuolep sårjåsjávrre
instance_of: Lake
countries: Sweden
Norway
coordinates: lat: 67.221111111111
lon: 16.356111111111
Mount Lawson (Washington). Mount Lawson is a mountain summit in Jefferson County of Washington state. Description. Mount Lawson is part of the Olympic Mountains and set within Olympic National Park and the Daniel J. Evans Wilderness. It is located south-southeast of Mount Olympus and the nearest higher neighbor is Mount Zindorf, to the northwest.

Geographic entities mentioned:
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount lawson
instance_of: Mountain
countries: United States
coordinates: lat: 47.6562
lon: -123.58851
Mount Lawson (Washington). Mount Lawson is a mountain summit in Jefferson County of Washington state. Description. Mount Lawson is part of the Olympic Mountains and set within Olympic National Park and the Daniel J. Evans Wilderness. It is located south-southeast of Mount Olympus and the nearest higher neighbor is Mount Zindorf, to the northwest.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: mount lawson (washington)
instance_of: Mountain
countries: United States
coordinates: lat: 47.6562
lon: -123.58851
Mount Lawson is part of the Olympic Mountains and set within Olympic National Park and the Daniel J. Evans Wilderness. It is located south-southeast of Mount Olympus and the nearest higher neighbor is Mount Zindorf, to the northwest. Precipitation runoff from the mountain drains to the North Fork Quinault River and topographic relief is significant as the summit rises above the river in. History.

Geographic entities mentioned:
surface_form: mount olympus
instance_of: Mountain
countries: United States
coordinates: lat: 47.801305555556
lon: -123.71083333333
surface_form: mount olympus
instance_of: Mountain
countries: United States
coordinates: lat: 40.6566
lon: -111.771
Mount Lawson (Washington). Mount Lawson is a mountain summit in Jefferson County of Washington state. Description. Mount Lawson is part of the Olympic Mountains and set within Olympic National Park and the Daniel J. Evans Wilderness. It is located south-southeast of Mount Olympus and the nearest higher neighbor is Mount Zindorf, to the northwest.

Geographic entities mentioned:
surface_form: daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
surface_form: mount lawson
instance_of: Mountain
countries: United States
coordinates: lat: 47.6562
lon: -123.58851
History. This peak was originally named &quot;Mount Grady&quot; by the 1889-90 Seattle Press Expedition to honor Henry W. Grady, editor of the &quot;Atlanta Constitution&quot; newspaper, and the expedition applied the Mount Lawson toponym to the 4,810-foot peak which is southwest.

Geographic entities mentioned:
surface_form: mount lawson
instance_of: Mountain
countries: United States
coordinates: lat: 47.6562
lon: -123.58851
The mountain's toponym has been officially adopted by the United States Board on Geographic Names. Climate. Based on the Köppen climate classification, Mount Lawson is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Olympic Mountains.

Geographic entities mentioned:
surface_form: mount lawson
instance_of: Mountain
countries: United States
coordinates: lat: 47.6562
lon: -123.58851
Distribution and habitat. &quot;Trichoglottis biglandulosa&quot; is endemic to the island of Java. It grows at rather high elevations in montane forests. At the time of its publication, it was reported from Mount Gede and Mount Salak. Taxonomy and naming. &quot;Trichoglottis biglandulosa&quot; was first described by Carl Ludwig Blume in 1825 as &quot;Ceratochilus biglandulosus&quot;.

Geographic entities mentioned:
surface_form: Mount Gede
instance_of: Mountain
countries: Indonesia
coordinates: lat: -6.7883333333333
lon: 106.98166666667
Stroheim had long wanted to do a film version of the book. He originally intended it to be a highly detailed reproduction of the original, shot mostly at the locations described in the book in San Francisco and Death Valley. Von Stroheim shot in San Francisco with his actors in period dress and silent movie makeup while the city itself was represented in its modern form.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
The nearby cities of Tiruchirapalli and Chidambaram are connected daily to other major cities by the network of Indian Railways and Tamil Nadu bus services. The temple though inland, is near the Kollidam River, within the Kaveri (Cauvery) delta with access to the Bay of Bengal and through it to the Indian Ocean. Nomenclature.

Geographic entities mentioned:
surface_form: Kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
The temple though inland, is near the Kollidam River, within the Kaveri (Cauvery) delta with access to the Bay of Bengal and through it to the Indian Ocean. Nomenclature. The Airavatesvara Shiva temple has a water tank that has a connected channel that brings in water from the Cauveri River. Hindus gather annually to take a dip in the tank.

Geographic entities mentioned:
surface_form: Cauveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
Wesenberg, Mecklenburg-Vorpommern. Wesenberg () is a town in the Mecklenburgische Seenplatte district, in Mecklenburg-Western Pomerania, Germany. It is situated 11 km southwest of Neustrelitz, at the south-west end of the Woblitzsee. Wesenberg Castle is located just outside the town.

Geographic entities mentioned:
surface_form: Woblitzsee
instance_of: Lake
countries: Germany
coordinates: lat: 53.296944444444
lon: 12.994166666667
Years later, the film of &quot;800 Bullets&quot; was filmed in the same place. Large sections of &quot;Conan the Barbarian&quot; (1982), &quot;Indiana Jones and the Last Crusade&quot;, &quot;Lawrence of Arabia&quot; and &quot;Patton&quot; were shot there as well. The main rivers are the Andarax River and Almanzora River, which are located near Granada in the Alpujarras.

Geographic entities mentioned:
surface_form: Andarax River
instance_of: Watercourse
countries: Spain
coordinates: lat: 37.0153
lon: -2.88917
At the end of January 1953, the Soviet request for an extension of their expired concession was turned down. In a meeting between Keshavarz Sadr and a USSR envoy on a ship in the Caspian Sea, the Iranian fishing industries were officially nationalised. He became the governor of Isfahan (a key province for Mossadegh), one of his recent predecessors being Mohammad Sa'ed.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Career. Born in Glasgow, John Higgins grew up in the East Ayrshire town of Stewarton and subsequently immigrated to the Tamborine Mountain region in the southeastern part of Australian state of Queensland. Using the performing name John Harley Weston, he has been a professional musician since 1990.

Geographic entities mentioned:
surface_form: Tamborine Mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -27.927513888889
lon: 153.19430555556
Solo career. As a solo artist, John Harley Weston has supported Indigo Girls at King Tut's Wah Wah Hut in Glasgow, Duran Duran at Glasgow Barrowlands, John Swan (Swanee) at on Tamborine Mountain and Lighthouse Family also at King Tut's.

Geographic entities mentioned:
surface_form: Tamborine Mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -27.927513888889
lon: 153.19430555556
Geography. The highest point in the Lakeview Mountains is at elevation above mean sea level. Mount Rudolph, a prominent feature at the northerly end of the range, rises to an elevation of. Reinhardt Canyon, on the easterly side of the range, is the home of the prehistoric petroglyph known as the Hemet Maze Stone (California Historical Landmark No. 557). Flora.

Geographic entities mentioned:
surface_form: Reinhardt Canyon
instance_of: Valley
countries: United States
coordinates: lat: 33.783333333333
lon: -117.05
Local SPCA officials have advised Hong Kong residents to never allow their pets off a lead at any time in the area, and to always be cautious about letting their dogs sniff or eat in the area. Hong Kong police believe the elusive killer is at work again. On the 12 October 2008, the SPCA sent specialists to the Peak where a dog was poisoned. The reward has been upped from HK$30,000 to HK$150,000.

Geographic entities mentioned:
surface_form: the Peak
instance_of: Mountain
countries: People's Republic of China
British Hong Kong
coordinates: lat: 22.275469444444
lon: 114.14382777778
Yarimburgaz Cave () is a cave of significant archaeological and paleontological importance, located within Istanbul Province, Turkey. Location. Yarımburgaz Cave is approximately west of the city of Istanbul, and about north of Lake Küçükçekmece and south of Sazlıdere Dam. It is situated in a locality known today as Altınşehir, within the neighborhood of Güvercintepe in Başakşehir district.

Geographic entities mentioned:
surface_form: Lake Küçükçekmece
instance_of: Lake
countries: Turkey
coordinates: lat: 41.0056
lon: 28.7469
Engelmann Peak. Engelmann Peak is a high mountain summit in the Front Range of the Rocky Mountains of North America. The thirteener is located in Arapaho National Forest, west by south (bearing 261°) of the Town of Empire in Clear Creek County, Colorado, United States. The mountain was named in honor of the botanist George Engelmann.

Geographic entities mentioned:
surface_form: engelmann peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.7456
lon: -105.801
Engelmann Peak. Engelmann Peak is a high mountain summit in the Front Range of the Rocky Mountains of North America. The thirteener is located in Arapaho National Forest, west by south (bearing 261°) of the Town of Empire in Clear Creek County, Colorado, United States. The mountain was named in honor of the botanist George Engelmann.

Geographic entities mentioned:
surface_form: engelmann peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.7456
lon: -105.801
surface_form: high mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0887
lon: -74.2351
Engelmann Peak. Engelmann Peak is a high mountain summit in the Front Range of the Rocky Mountains of North America. The thirteener is located in Arapaho National Forest, west by south (bearing 261°) of the Town of Empire in Clear Creek County, Colorado, United States. The mountain was named in honor of the botanist George Engelmann.

Geographic entities mentioned:
surface_form: clear creek
instance_of: Watercourse
countries: United States
coordinates: lat: 39.83537
lon: -91.94278
The most significant easterly fault described by Edward Hull throws the strata down to the east. It was worked from Fairbottom in Ashton-under-Lyne across the River Medlock to Oldham and onwards to the west of Rochdale. The Red Rock Fault skirts the north-west extremity of the North Staffordshire coalfield towards Macclesfield and Poynton Colliery in Cheshire.

Geographic entities mentioned:
surface_form: River Medlock
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 53.4741
lon: -2.25342
More companies emerged during the 19th century and included Richard Evans and Company of Haydock, which originated in 1830. Pearson and Knowles Coal and Iron Company was formed in 1874 in Ince. Colonel John Hargreaves began a company with pits in Burnley, and George Hargreaves owned pits in Accrington and Rossendale Valley. James Lees' Chamber Colliery Company owned pits in Oldham. Drainage.

Geographic entities mentioned:
surface_form: Rossendale Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.7031
lon: -2.2893
Other soughs were dug, including one in 1729 to drain the Worsley mines and another from Standish Colliery to the Leeds and Liverpool Canal at Crooke. A waterwheel was used from 1720 to lift water from the workings of the Plumbe Street Mine in Burnley using an endless chain of buckets, and James Brindley installed one at the Wet Earth Colliery in the Irwell Valley.

Geographic entities mentioned:
surface_form: Irwell Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.66
lon: -2.31
In 1937, he was 20 and traveling with six other students in Shanghai when war broke out between China and Japan. Drey began acquiring timberland in the Missouri Ozarks for reforestation and conservation in 1951. His holdings, much acquired for the price of back taxes, eventually grew to nearly, the largest private landholding in the state and larger than Missouri's entire state park system.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
Bale Mountains National Park. Bale Mountains National Park is a national park in Ethiopia. The park encompasses an area of approximately in the Bale Mountains and Sanetti Plateau of the Ethiopian Highlands. The park's Afromontane habitats have one of the highest incidences of animal endemicity of any terrestrial habitat in the world.

Geographic entities mentioned:
surface_form: Sanetti Plateau
instance_of: Mountain
countries: Ethiopia
Traveling to Ireland with Olcott's crew that included leading lady and principal screenwriter Gene Gauntier, George Hollister shot &quot;The Lad from Old Ireland&quot; and The Irish Honeymoon, a travelogue shot in Blarney Castle, Glengarriff and at the Lakes of Killarney. A Kalem crew returned to Ireland in each of the next two years and in 1912.

Geographic entities mentioned:
surface_form: Lakes of Killarney
instance_of: Group of lakes
countries: Ireland
coordinates: lat: 52.041666666667
lon: -9.55
In 2015, it was run counterclockwise. Today, the races consist of the following;
Route. The route follows the Tour du Mont Blanc hiking path that is usually completed in 7 to 9 days by hikers. This is a loop around Mont Blanc. It starts from Chamonix (1,035 m) and goes up to the Col de Voza (1,653 m) to reach Les Contamines (1,150 m), which is the first life base.

Geographic entities mentioned:
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
Background and release. Haim was formed in 2006, in San Fernando Valley, California, after spending their childhood as part of family cover band Rockinhaim. The group toured during the years, until they broke into the scene after a successful show at Texas music festival South by Southwest.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Taftan appears to be part of a geothermal area; there are a number of hot springs around the volcano. Taftan is part of a volcanic arc in Iran, together with Bazman, also in Iran, and Koh-i-Sultan in Pakistan. This volcanic arc has formed on Cretaceous-Eocene sedimentary layers and has resulted from the subduction of the oceanic Arabian Plate beneath Iran at the Makran trench.

Geographic entities mentioned:
surface_form: Bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
Taftan (volcano). Taftan (, &quot;Taptân&quot;, &quot;Taftân&quot;, in Balochi and also Persian for &quot;blistering, smoldering, fuming&quot;) is an active stratovolcano in south-eastern Iran in the Sistan and Baluchestan province. With variable heights reported, all around 4,000 metres (13,000 ft) above sea level, it is the highest mountain in south-eastern Iran. The nearest city is Khash.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
Currently, the volcano features vigorous fumarolic activity that is visible from a great distance and involves numerous vents on Materkuh. Taftan appears to be part of a geothermal area; there are a number of hot springs around the volcano. Taftan is part of a volcanic arc in Iran, together with Bazman, also in Iran, and Koh-i-Sultan in Pakistan.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
Taftan is in Iran's Sistan and Balochistan province. Closest cities are Khash south and Zahedan north north-west. In 1844, Abdul-Nabi reported of the existence of the mountain, as well as its volcanic activity. In 1971, it was reported that some Beluch tribes camp on Taftan's slopes outside of winter. Regional setting. Volcanic activity has occurred in parts of Iran since the Cretaceous period.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
The convergence of the two blocks continued even after their collision, generating strike-slip faults. The Saravan fault east of Taftan is one such fault; the 2013 Saravan earthquake occurred on this fault. From some of these faults it has been inferred that the mass load from the Taftan edifice has measurable effects on tectonic stress within the region. Local setting.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
Local setting. Taftan is the highest mountain in southeast Iran. The topography is overall steep. Deep valleys with U and V shapes have developed on Taftan, and the volcano has a strongly eroded appearance. One of these valleys, Tamindan, may be the Damindan valley in the Avesta religious texts.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
One of these valleys, Tamindan, may be the Damindan valley in the Avesta religious texts. One series of ignimbrites surrounding Taftan which reaches thicknesses of and reaches distances of from the edifice may be 2 million years old. The basement of Taftan is formed by various sedimentary rocks, along with some mafic volcanic rocks and metamorphic rocks.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
One series of ignimbrites surrounding Taftan which reaches thicknesses of and reaches distances of from the edifice may be 2 million years old. The basement of Taftan is formed by various sedimentary rocks, along with some mafic volcanic rocks and metamorphic rocks. At Taftan, the Nehbandan-Khash flysch borders the Makran zone. The oldest rocks are limestones from the Cretaceous period.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
The main edifice is constructed on top of the Eocene flysch, although some Cretaceous sediments are also part of the basement. Much of these rocks is coloured pink by haematite. The 19 mya old Mirabad granite pluton may be associated with Taftan; it could be the remnant of a Miocene volcano. Volcanic rocks of Quaternary age are widespread in the area.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
These loose rocks formed by erosion, explosive activity and hot avalanches and are deposited in a large apron at the base of the volcano that extends over away from the central vents. Several fans of pyroclastic material, cemented by andesitic tuffs, surround the base of Taftan. Ignimbrites and pyroclastic flows are also present, including breccias, nuee ardentes and tuffs.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
Ignimbrites and pyroclastic flows are also present, including breccias, nuee ardentes and tuffs. Volcanic rocks cover a surface of. There is also evidence of southeastern migration of the craters of Taftan, with Anjerk and Sardarya being more westerly vents. These preceding centres have left andesitic lava flows that are partially dissected and agglomerates.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
These preceding centres have left andesitic lava flows that are partially dissected and agglomerates. The existence of a caldera at Taftan has been inferred. The table mountain Takht-i-Rostam south of Taftan may be the remnant of a basalt extrusion, but it doesn't appear to be related to Taftan. A magma chamber may lie beneath the volcano. Composition.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
The dominant rock is andesite, with content ranging from 49.8 to 63.5%. Grey andesites form the youngest rocks on the main summit and contain chlorite schist and biotite gneiss inclusions. The andesites are vesicular. The magma of Taftan volcano is very oxidized, as can be inferred from the composition of the surrounding ignimbrite and fumarole gases. The lavas of Taftan are porphyritic.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
Fumarolic activity affects surrounding rocks and pyroclastics. Carbonates, opal, and white covers of possibly aluminum sulfate and calcium sulfate have been formed. Gypsum formed from the sulfur of the volcano is found in the form of crystals in the upper valleys of Taftan. Sinter and hydrothermally altered rocks are found farther down.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
Sinter and hydrothermally altered rocks are found farther down. Minerals formed by alteration processes include alunite, calcite, cristobalite, illite, jarosite, kaolinite, pyrophyllite, quartz, smectite, sulfur and tridymite. Some epithermal mineralizations have been identified around Taftan. Other secondary factors at Taftan include lahars. Eruptive history.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
Some epithermal mineralizations have been identified around Taftan. Other secondary factors at Taftan include lahars. Eruptive history. About five different active eruption periods have been discovered at Taftan volcano. Activity first involved lava and pyroclastics of dacitic to rhyodacitic composition. Later, upper Pliocene lavas were erupted along with agglomerates.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
That the name &quot;Taftan&quot; may be derived from an ancient Iranian word &quot;taft&quot; for &quot;semi solid liquid material&quot; could indicate that effusive activity was witnessed by the people of that time period around the volcano. It is not certain that there were any Holocene eruptions at Taftan, as clear evidence of such activity is missing.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
The eruption in 1993 involved a long lava flow, but it may have been a flow of molten sulfur. The volcano is currently classified as a dormant volcano. Satellite imagery indicates, however, that ground deformation occurs at Taftan. Unofficial volcano hazard maps have been developed. Fumarolic and geothermal activity.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
A fumarole field was described on the west side of the southeast cone, the venting clearly visible from a refuge farther down the mountain and covering a surface area of. The name &quot;Taftan&quot; is derived from these exhalations, which make the mountain appear to be burning. The overall gas composition found at Taftan includes, and water.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
Temperatures in the hydrothermal system are estimated to be between and. The composition of the water in various springs around Taftan varies in terms of elemental composition, probably reflecting the mixing between volcanic and meteoric waters and interaction with host rocks and brines. The geothermal area of Taftan is among the largest in the Makran zone of Iran; it covers a surface area of.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
Hot springs and other geothermal manifestations are widespread in Iran and using them to gain geothermal energy has been studied; according to a report of 2002 hot springs at that time were mainly used for therapeutic purposes and bathing. A report in 2002 indicated that Taftan may be a feasible place to install a binary cycle power plant. Climate and vegetation.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
Climate and vegetation. The climate at Taftan features cold winters accompanied by snowfall when temperatures drop below freezing between December and February, and hot summers with temperatures during July and August exceeding. Taftan is located in an arid locale but has more precipitation than the surrounding area, thus providing water to the surrounding terrain.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
The climate at Taftan features cold winters accompanied by snowfall when temperatures drop below freezing between December and February, and hot summers with temperatures during July and August exceeding. Taftan is located in an arid locale but has more precipitation than the surrounding area, thus providing water to the surrounding terrain. Average precipitation is per year.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
Volcanic activity at Taftan itself appears to relate to the subduction of the Arabian Plate beneath the Central Iran Plate, occurring at a pace of or at the Makran trench. This subduction is also responsible for volcanism at Bazman in Iran and Koh-i-Sultan in Pakistan; this chain is known as the Baluchistan volcanic arc.

Geographic entities mentioned:
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
Wrangell Mountains. The Wrangell Mountains are a high mountain range of eastern Alaska in the United States. Much of the range is included in Wrangell-Saint Elias National Park and Preserve. The Wrangell Mountains are almost entirely volcanic in origin, and they include the second and third highest volcanoes in the United States, Mount Blackburn and Mount Sanford.

Geographic entities mentioned:
surface_form: Mount Blackburn
instance_of: Mountain
countries: United States
coordinates: lat: 61.73190833333334
lon: -143.43929722222222
The Wrangell Mountains are almost entirely volcanic in origin, and they include the second and third highest volcanoes in the United States, Mount Blackburn and Mount Sanford. The range takes its name from Mount Wrangell, which is one of the largest andesite shield volcanoes in the world, and also the only presently active volcano in the range.

Geographic entities mentioned:
surface_form: Mount Wrangell
instance_of: Mountain
countries: United States
coordinates: lat: 62.006944444444
lon: -144.01583333333
Fitzroy Bay is a bay close to the entrance of Wellington Harbour in New Zealand. It lies to the southeast of the entrance to the harbour, between Pencarrow Head (to the north) and Baring Head (to the south). Lake Kohangatera drains into the bay through Gollans Stream. The bay has been the site of several shipwrecks, predominantly caused by the strong winds and swells which run through Cook Strait.

Geographic entities mentioned:
surface_form: Lake Kohangatera
instance_of: Lake
countries: New Zealand
coordinates: lat: -41.3686
lon: 174.8668
Large transit agencies (defined as those operating more than 65 buses in the San Joaquin Valley Air Basin or South Coast Air Quality Management District, or those operating more than 100 buses elsewhere with populations greater than 200,000) are required to have 25% of new bus purchases as zero-emission buses (ZEBs) starting in 2023, 50% of new purchases as ZEBs starting in 2026, and 100% of new purchases as ZEBs starting in 2029.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185