Sarmila/GeoWiki-Features huggingface dataset:
The town was founded in 1236, and is the largest in Busturialdea. Bermeo was the provincial capital of Biscay from 1476 to 1602. Tourist attractions include the island of Gaztelugatxe, the Ercilla Tower (a fishing museum), San Juan Gate and the port. Bermeo is connected by Euskotren Trena and BizkaiBus to Bilbao.

Geographic entities mentioned:
surface_form: Gaztelugatxe
instance_of: Mountain
countries: Spain
coordinates: lat: 43.447
lon: -2.785
Attractions. On the road to Bakio is the lighthouse of Matxitxako, on the cape of the same name. Further along is Akatz Island, next to Gaztelugatxe (an island with the San Juan de Gaztelugatxe monastery). During the 14th century a castle topped the island, which was replaced by the monastery. On 29 August a mass celebrates the feast of San Juan. The island is a protected area.

Geographic entities mentioned:
surface_form: Gaztelugatxe
instance_of: Mountain
countries: Spain
coordinates: lat: 43.447
lon: -2.785
This find was published in the Melbourne &quot;Argus&quot; on 8 September 1851, leading to a rush to the Mount Alexander or Forest Creek diggings, centred on present-day Castlemaine, claimed as the richest shallow alluvial goldfield in the world. These discoveries were soon surpassed by Ballarat and Bendigo.

Geographic entities mentioned:
surface_form: Mount Alexander
instance_of: Mountain
countries: Australia
coordinates: lat: -36.996944444444
lon: 144.305
Surface alluvial gold was the first to be exploited. It is reported that in 1851, when the first miners arrived on the Mount Alexander goldfield, near Castlemaine, nuggets could be picked up without digging. Then followed the exploitation of alluvial gold in creeks and rivers, or deposited in silt on river banks and flats.

Geographic entities mentioned:
surface_form: Mount Alexander
instance_of: Mountain
countries: Australia
coordinates: lat: -36.996944444444
lon: 144.305
The current Hintalo Wajirat woreda is the merger of Gabat Milash and Wajirat, and both Gabatmilash as well as Wajirat have been an integral part of Enderta province when Enderta was an independent province as well as an awraja as recent as the late 1990s,
Overview. High points in this woreda include Amba Aradam, an amba or mountain north of Hintalo.

Geographic entities mentioned:
surface_form: Amba Aradam
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 13.333333333333
lon: 39.516666666667
It was carved out from the Zuiderzee by the construction of the polders of Noordoostpolder and Flevoland, between which it lies. It is via Ketelmeer that the IJsselmeer connects to the Zwarte Meer and the Veluwemeer, the strip of water which separates Flevoland from the coast of the mainland.

Geographic entities mentioned:
surface_form: Veluwemeer
instance_of: Lake
countries: Netherlands
coordinates: lat: 52.4
lon: 5.7
surface_form: ketelmeer
instance_of: Lake
countries: Netherlands
coordinates: lat: 52.596666666667
lon: 5.7622222222222
Ketelmeer. The Ketelmeer is the tongue of the IJsselmeer into which the River IJssel drains, it is situated between the polders Noordoostpolder (North-east Polder) and Oostelijk Flevoland (East Flevoland), and connects the river IJssel to the IJsselmeer.

Geographic entities mentioned:
surface_form: ketelmeer
instance_of: Lake
countries: Netherlands
coordinates: lat: 52.596666666667
lon: 5.7622222222222
It is one of the bordering lakes, a continuous body of water which separate Flevoland from the Noordostpolder and the ancient lands of the provinces of Gelderland and Utrecht. The Ketelmeer covers an area of 3500 hectares, most of which is in the province of Flevoland, but the river delta of the IJssel is in province of Overijssel.

Geographic entities mentioned:
surface_form: ketelmeer
instance_of: Lake
countries: Netherlands
coordinates: lat: 52.596666666667
lon: 5.7622222222222
The Ketelmeer borders two &quot;buurtschappen&quot;, on the opposite sides of the lake: Ketelhaven on the south and Schokkerhaven on the north, both located roughly halfway the lake, though Ketelhaven is still located about one kilometer further to the east. Ketelhaven also has significantly more inhabitants.

Geographic entities mentioned:
surface_form: ketelmeer
instance_of: Lake
countries: Netherlands
coordinates: lat: 52.596666666667
lon: 5.7622222222222
Ketelhaven also has significantly more inhabitants. The Ketelmeer contains the IJsseloog, a kilometre-diameter circular pit in an artificial island, built to contain the toxic sludge dredged from the bed of the Ketelmeer. The Ketelbrug is a bascule bridge over the Ketelmeer connecting the Noordoostpolder and Oostelijk Flevoland.

Geographic entities mentioned:
surface_form: ketelmeer
instance_of: Lake
countries: Netherlands
coordinates: lat: 52.596666666667
lon: 5.7622222222222
Azov Upland. Azov Upland or Cisazov Upland is a plateau or range of hills in East Ukraine within the Donetsk and Zaporizhia oblasts. To the north it borders Dnieper Lowland, to northeast &ndash; Donets Ridge, southwest &ndash; Black Sea Lowland, south &ndash; Azov Lowland. Elevation varies between. Interesting features are mounds locally known as ' similar to Russian equivalent of kurgan.

Geographic entities mentioned:
surface_form: azov upland
instance_of: Plateau
countries: Ukraine
coordinates: lat: 47.3315
lon: 36.57908333
Its population is 7,761 (2020). Location. The Innere Neustadt is located in the administrative district of Neustadt, on the right bank across the Elbe and to the north of the Innere Altstadt (Inner Old City). The River Elbe forms an enclosing arc around the Innere Neustadt. Four bridges cross the Elbe, connecting the district with the southern bank of the Elbe.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Within this arc, Bazman is located at the edge between the actual subduction and the continental collision zone. Bazman is also considered part of a long volcanic belt named the Urumieh-Dokhtar or Sahand-Bazman belt that extends from northwest to southeast and is accompanied by Cenozoic volcanic rocks and plutons.

Geographic entities mentioned:
surface_form: Sahand
instance_of: Mountain
countries: Iran
coordinates: lat: 37.73
lon: 46.5
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
surface_form: sahand
instance_of: Mountain
countries: Iran
coordinates: lat: 37.73
lon: 46.5
Local setting. Bazman is one among about nine volcanic centres in Iran that have had Quaternary eruptions. Other volcanoes are Damavand which is also Asia's highest volcano, Taftan, Qal'eh Hasan Ali, Sabalan and Sahand volcanoes. Most of these volcanoes are part of a volcanic belt named Dokhtar-Urmiah.

Geographic entities mentioned:
surface_form: Qal'eh Hasan Ali
instance_of: Mountain
countries: Iran
coordinates: lat: 29.66666667
lon: 57.95
surface_form: Sabalan
instance_of: Mountain
countries: Iran
coordinates: lat: 38.266944444444
lon: 47.836944444444
surface_form: sabalan
instance_of: Mountain
countries: Iran
coordinates: lat: 38.266944444444
lon: 47.836944444444
surface_form: qal'eh hasan ali
instance_of: Mountain
countries: Iran
coordinates: lat: 29.66666667
lon: 57.95
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
surface_form: sahand
instance_of: Mountain
countries: Iran
coordinates: lat: 37.73
lon: 46.5
surface_form: damavand
instance_of: Mountain
countries: Iran
coordinates: lat: 35.955277777778
lon: 52.109166666667
Thus Bazman may be regarded as dormant, rather than extinct, volcano. Its satellite cones have been the source of basaltic lava flows. Bazman volcano is part of a volcanic arc in southeastern Iran, the Makran volcanic arc. At this arc, shallow subduction has generated an arc of volcanic activity which includes Bazman, Taftan and Koh-i-Sultan volcanoes. Bazman has been affected by heavy erosion.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
There is no evidence of a Wadati–Benioff zone beneath the Makran and subduction occurs at a shallow angle. Bazman has been grouped with Taftan volcano also in Iran and Koh-i-Sultan in Pakistan, of which only Taftan is considered active, Kuh-e-Nader is another volcanic field in this arc. This arc is over away from the trench, indicating that the subduction is very shallow.

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
Most of these volcanoes are part of a volcanic belt named Dokhtar-Urmiah. With the exception of reports of possible lava flows at Taftan, none of these volcanoes have been reportedly active during historical times. Older volcanic activity within this belt has generated a number of copper porphyry deposits. Bazman volcano is high, rising high above the surrounding terrain, and has steep slopes.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
Bazman is considered to be occasionally smoking. Hot springs containing iron and sulfur are other signs of ongoing volcanism; Bazman has been considered a potential site for development of geothermal energy, with a surface area of. In 1960, Bazman together with Taftan was considered a volcano with sporadic historic activity, while a different report in 1975 considered the volcano extinct.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
Petrological analysis at the monogenetic volcanoes around Bazman has indicated porphyritic basalts containing clinopyroxene, hornblende, olivine and plagioclase, and titanite and zircon as accessories. The rocks have medium potassium content, lower than that of Taftan and Koh-i-Sultan. This may reflect differences in the subduction beneath Bazman and the other two volcanoes.

Geographic entities mentioned:
surface_form: taftan
instance_of: Mountain
countries: Iran
coordinates: lat: 28.6
lon: 61.133333333333
Bazman. Bazman (, also known as Kuh-e Bazman) is a dormant stratovolcano in a remote desert region of Sistan and Baluchestan Province in southeastern Iran. A 500-m-wide crater caps the summit of the dominantly andesitic-dacitic volcano, the flanks of which are covered by monogenetic centres especially to the northwest.

Geographic entities mentioned:
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
Bazman. Bazman (, also known as Kuh-e Bazman) is a dormant stratovolcano in a remote desert region of Sistan and Baluchestan Province in southeastern Iran. A 500-m-wide crater caps the summit of the dominantly andesitic-dacitic volcano, the flanks of which are covered by monogenetic centres especially to the northwest.

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
A 500-m-wide crater caps the summit of the dominantly andesitic-dacitic volcano, the flanks of which are covered by monogenetic centres especially to the northwest. Bazman is a geologically young volcano which formed mainly in the Quaternary, with the oldest dated rocks being 11.7 million years old and the youngest 0.6 million years.

Geographic entities mentioned:
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
Bazman is a geologically young volcano which formed mainly in the Quaternary, with the oldest dated rocks being 11.7 million years old and the youngest 0.6 million years. Although no historic eruptions have been reported from Bazman, it does contain fumaroles. Thus Bazman may be regarded as dormant, rather than extinct, volcano. Its satellite cones have been the source of basaltic lava flows.

Geographic entities mentioned:
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
Thus Bazman may be regarded as dormant, rather than extinct, volcano. Its satellite cones have been the source of basaltic lava flows. Bazman volcano is part of a volcanic arc in southeastern Iran, the Makran volcanic arc. At this arc, shallow subduction has generated an arc of volcanic activity which includes Bazman, Taftan and Koh-i-Sultan volcanoes. Bazman has been affected by heavy erosion.

Geographic entities mentioned:
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
Bazman volcano is part of a volcanic arc in southeastern Iran, the Makran volcanic arc. At this arc, shallow subduction has generated an arc of volcanic activity which includes Bazman, Taftan and Koh-i-Sultan volcanoes. Bazman has been affected by heavy erosion. The flanks of the volcano are covered with debris coming from the volcano.

Geographic entities mentioned:
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
Bazman has been affected by heavy erosion. The flanks of the volcano are covered with debris coming from the volcano. A Cretaceous pluton is also associated with Bazman and has been investigated for the possibility of mining. Geography and geology. Bazman is also known as Kuh-i-Zindeh (&quot;Mountain of the Living One&quot;), after a saint, Khizr-as-Sallam.

Geographic entities mentioned:
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
A Cretaceous pluton is also associated with Bazman and has been investigated for the possibility of mining. Geography and geology. Bazman is also known as Kuh-i-Zindeh (&quot;Mountain of the Living One&quot;), after a saint, Khizr-as-Sallam. Yet another name is Kuh-i-Naushada, although they are sometimes considered to be separate mountains.

Geographic entities mentioned:
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
Each range is associated with a major suture zone, the Alborz-Kopeh Dag and the Bitlis-Zagros sutures respectively. These mountain chains surround Central Iran, in whose southern part lies the Lut block and Bazman. Tectonically, southern central Iran does not follow the typical Alpide geological patterns insofar as faults are rare and the folds in the crust are broad.

Geographic entities mentioned:
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
The Bazman area is covered by volcanic rocks of Tertiary age. The foreland of the mountain massifs such as the Bazman massif are affected by tectonic subsidence. A major Tertiary volcanic belt, analogous to the Indonesian volcanic arc, crosses Iran behind the Zagros. South of Bazman volcano lies the broad Jaz Murian depression.

Geographic entities mentioned:
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
A phase of subduction commenced in the Cretaceous or Plio-Pleistocene, probably after earlier phases of subduction. This subduction has resulted in the formation of a volcanic complex including Bazman that stretches east-west and reaches a width of, and is known as the Makran-Chagai magmatic arc.

Geographic entities mentioned:
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
Bazman has been grouped with Taftan volcano also in Iran and Koh-i-Sultan in Pakistan, of which only Taftan is considered active, Kuh-e-Nader is another volcanic field in this arc. This arc is over away from the trench, indicating that the subduction is very shallow. Within this arc, Bazman is located at the edge between the actual subduction and the continental collision zone.

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
At the top of the volcano lies a summit crater. This crater is well conserved and it has a diameter of. On the north flank, a northbound lava flow with prominent levees that eventually splits into a northwestern and northeastern arm was discharged by a steep lava cone that is known as Bazman Bacheh (&quot;Bazman's Child&quot;) and lies northeast of the summit.

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
In total the volcano covers an area of about. The volcano is constructed on top of the Lut block, which reaches a thickness of. Quaternary sediments are buried beneath Bazman's eruption products. The Moho beneath Bazman is approximately deep. The area around Bazman is remote. A field of monogenetic volcanoes is found northwest of Bazman.

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
In total the volcano covers an area of about. The volcano is constructed on top of the Lut block, which reaches a thickness of. Quaternary sediments are buried beneath Bazman's eruption products. The Moho beneath Bazman is approximately deep. The area around Bazman is remote. A field of monogenetic volcanoes is found northwest of Bazman.

Geographic entities mentioned:
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
The Moho beneath Bazman is approximately deep. The area around Bazman is remote. A field of monogenetic volcanoes is found northwest of Bazman. These include broad and shallow craters with diameters of with pyroclastic rocks, cryptodomes with diameters of up to and heights of, scoria cones reaching a height of with lava flow fields and individual lava flows.

Geographic entities mentioned:
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
The varying state of erosion of these volcanoes indicates they formed over many millennia; some have been worn down to their feeding dykes. Bazman has no recorded historical eruptions but fumarolic activity has been reported, as well as ongoing surface deformation. Bazman is considered to be occasionally smoking.

Geographic entities mentioned:
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
Bazman is considered to be occasionally smoking. Hot springs containing iron and sulfur are other signs of ongoing volcanism; Bazman has been considered a potential site for development of geothermal energy, with a surface area of. In 1960, Bazman together with Taftan was considered a volcano with sporadic historic activity, while a different report in 1975 considered the volcano extinct.

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
Potassium-argon dating of basalts from the volcano has yielded ages of 4.6 and 0.6 million years ago. These dates were obtained on the monogenetic cones; zircons directly from Bazman rocks are dated 7.5 ± 0.1 and 5.9 ± 0.2 million years ago by uranium-lead dating, along with other ages of 8–6 million years ago from other zircons around Bazman. A third date is of 11.7 million years ago.

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
A third date is of 11.7 million years ago. Another report in 1981 suggested that isotopic ages also indicate historic activity. Latest research indicates that the main Bazman volcano formed between 1.4 and 0.63 million years ago, with a preceding stage of regional volcanism between 8.6 and 4.1 million years ago.

Geographic entities mentioned:
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
Later ignimbritic volcanism took place between 590,000 and 470,000 years ago; the final volcanic activity around the summit of the volcano continued until less than 41,000 years ago. An important geothermal field is associated with Bazman and hot springs occur south of the volcano; they might derive their heat source from it but the volcano features no fumaroles.

Geographic entities mentioned:
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
The mountain's flanks are covered by a layer of detritus, burying most of the flanks to over of altitude. Most of this detritus is erosional in nature, but pyroclastic rocks created by explosive activity and hot avalanches of extruded lava also contribute. thick olivine basalt found in the Jaz Murian depression may also come from Bazman. Basalt has also been found at one cryptodome.

Geographic entities mentioned:
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
thick olivine basalt found in the Jaz Murian depression may also come from Bazman. Basalt has also been found at one cryptodome. North of Bazman, andesites of Miocene-Eocene age are partly buried beneath the volcano and there are also andesitic to dacitic intrusions. Carboniferous and Permian metamorphic rocks form the oldest basement at Bazman.

Geographic entities mentioned:
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
Carboniferous and Permian metamorphic rocks form the oldest basement at Bazman. Petrological analysis at the monogenetic volcanoes around Bazman has indicated porphyritic basalts containing clinopyroxene, hornblende, olivine and plagioclase, and titanite and zircon as accessories. The rocks have medium potassium content, lower than that of Taftan and Koh-i-Sultan.

Geographic entities mentioned:
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
The rocks have medium potassium content, lower than that of Taftan and Koh-i-Sultan. This may reflect differences in the subduction beneath Bazman and the other two volcanoes. Composition data are typical of volcanic island arc rocks, with some samples have element ratios more akin to ocean island basalts.

Geographic entities mentioned:
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
The magmas ultimately originate through partial melting from a stable heat source. A mining area is associated with Bazman and more precisely with Paleozoic-Mesozoic rocks including a 70 million years old granite pluton. This late Cretaceous pluton is localized south of Bazman volcano. According to other reports its rocks are also exposed on the northern side of Bazman.

Geographic entities mentioned:
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
A mining area is associated with Bazman and more precisely with Paleozoic-Mesozoic rocks including a 70 million years old granite pluton. This late Cretaceous pluton is localized south of Bazman volcano. According to other reports its rocks are also exposed on the northern side of Bazman. The granite complex is partly buried by Bazman volcano.

Geographic entities mentioned:
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
According to other reports its rocks are also exposed on the northern side of Bazman. The granite complex is partly buried by Bazman volcano. Various hydrothermal and skarn alterations have generated mineral deposits that include silver, gold, copper, lead, magnesium, molybdenum, and zinc, and minor amounts of tungsten and possibly of vanadium.

Geographic entities mentioned:
surface_form: bazman
instance_of: Mountain
countries: Iran
coordinates: lat: 28.075833333333
lon: 60.011111111111
Sheet floods such as those that occurred in 1976 are principal agents. Together with other kinds of erosion such as frost and salt weathering, these have formed a pediplain terrain with inselbergs being left, especially where harder rocks are found. Pebbles eroded from Bazman have been transported to the terrains of the Jaz Murian depression south of Bazman.

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
Pebbles eroded from Bazman have been transported to the terrains of the Jaz Murian depression south of Bazman. The effects of this erosion have mantled the volcano with debris locally known as &quot;dasht&quot;, reaching distances of over from the vent. With the exception of the Ziyarat valley on Bazman's southern flank, the area around Bazman is arid and uninhabited. Climate and environment.

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
San Giovanni Battista, Morbegno. The Chiesa di San Giovanni Battista (Church of San Giovanni Battista) is a Roman Catholic collegiate church dating back to the 17th and 18th centuries, located in Morbegno in the Valtellina in region of Lombardy, and consecrated to St. John the Baptist. History. In 1993, the church experienced a theft of 37 paintings.

Geographic entities mentioned:
surface_form: Valtellina
instance_of: Valley
countries: Italy
coordinates: lat: 46.166666666667
lon: 9.8666666666667
The parish hall since 1560, has a relic of the Holy Spine (of the crown of Christ) and the remains of Blessed Andrea Grego da Peschiera. The Collegiate also holds important relics: The Holy Spina, donated by the Morgid bishop Feliciano Ninguarda, the earthly remains of Blessed Andrea da Peschiera known as the apostle of Valtellina and the body of Santa Costanza.

Geographic entities mentioned:
surface_form: Valtellina
instance_of: Valley
countries: Italy
coordinates: lat: 46.166666666667
lon: 9.8666666666667
September 25: White House sources, in an exclusive to the &quot;Dallas Morning News&quot;, announce that the president will visit Texas November 21–22, 1963 and that the tour will include Dallas. September 26: The &quot;Dallas Morning News&quot; is the first newspaper to announce the Texas visit in an article covering the president's conservation tour in Jackson Hole, Wyoming.

Geographic entities mentioned:
surface_form: Jackson Hole
instance_of: Valley
countries: United States
coordinates: lat: 43.516666666667
lon: -110.83333333333
In the northwest arm the hills are high, including the Monte Nuestra Señora de la Victoria (890 m) and the Lecky Look Out (890 m) on the Contreras Island, and the Monte Lucía of 510 m on the Diego de Almagro Island. In the vicinity of its south arm is Monte Burney, which lie on Muñoz Gamero Peninsula in mainland. This imposing volcanic peak stands out from the mountains that surround it.

Geographic entities mentioned:
surface_form: Monte Burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
Willowbrook Shopping Centre. Willowbrook Shopping Centre (sometimes referred to as Willowbrook Mall) is a shopping centre in the Fraser Valley area of Metro Vancouver, Canada. Situated on Fraser Highway at Highway 10 (Langley By-Pass), Willowbrook is located half in the City of Langley and half in the Township of Langley in British Columbia. The mall is 40 minutes southeast of Vancouver.

Geographic entities mentioned:
surface_form: Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
The Dyke railway station. The Dyke railway station was a railway station near Devil's Dyke in West Sussex, England which opened in 1887 and closed in 1939. History. The Dyke Station opened as the terminus for the standard gauge railway line which ran from Dyke Junction Station (now known as Aldrington railway station) to below the summit of Devil's Dyke.

Geographic entities mentioned:
surface_form: Devil's Dyke
instance_of: Valley
countries: United Kingdom
coordinates: lat: 50.885
lon: -0.205
It is commonly associated with hematite, barite, pyrolusite, quartz and other manganese oxide minerals. It has been found in France, Germany, England, Brazil, Russia, India, and various parts of the United States, including Arizona, Virginia, Tennessee and Michigan, and sites throughout the Appalachian Valley and Ridge. It occurs also in ferromanganese nodules from Lake Baikal.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Half Moon is situated on Kangaroo Ridge which is approximately two miles east and within view of the North Cascades Highway at Washington Pass. The nearest higher neighbor is Wallaby Peak, to the south. Precipitation runoff from the peak drains into Early Winters Creek, and Cedar Creek, both of which are tributaries of the Methow River. Geology.

Geographic entities mentioned:
surface_form: Wallaby Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.506773
lon: -120.615238
Half Moon (Washington). Half Moon is a summit located in Okanogan–Wenatchee National Forest, in Okanogan County, of Washington state. The mountain is part of the Methow Mountains, which are a subset of the Cascade Range. Half Moon is situated on Kangaroo Ridge which is approximately two miles east and within view of the North Cascades Highway at Washington Pass.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: half moon
instance_of: Mountain
countries: United States
coordinates: lat: 48.509867
lon: -120.613489
Half Moon is a summit located in Okanogan–Wenatchee National Forest, in Okanogan County, of Washington state. The mountain is part of the Methow Mountains, which are a subset of the Cascade Range. Half Moon is situated on Kangaroo Ridge which is approximately two miles east and within view of the North Cascades Highway at Washington Pass. The nearest higher neighbor is Wallaby Peak, to the south.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: half moon
instance_of: Mountain
countries: United States
coordinates: lat: 48.509867
lon: -120.613489
With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted. In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago. Half Moon is located in the Golden Horn batholith and composed of granite like many of the peaks in the Washington Pass area.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: golden horn
instance_of: Mountain
countries: United States
coordinates: lat: 37.804722222222
lon: -107.82472222222
surface_form: golden horn
instance_of: Mountain
countries: United States
coordinates: lat: 48.603333333333
lon: -120.73194444444
surface_form: half moon
instance_of: Mountain
countries: United States
coordinates: lat: 48.509867
lon: -120.613489
Its waters flow to the Vilcanota River. Chillcamayu originates in the Vilcanota mountain range between the mountains Jatunhuma in the north-west and Huayruro Punco in the south-east. It crosses the Pitumarca District from north-east to south-west along the villages of Jampa, Chillca and Pitumarca. One of its main tributaries from the left is Yanamayo (Quechua for &quot;black river&quot;).

Geographic entities mentioned:
surface_form: Jatunhuma
instance_of: Mountain
countries: Peru
coordinates: lat: -13.74722222
lon: -71.13666667
surface_form: Huayruro Punco
instance_of: Mountain
countries: Peru
coordinates: lat: -13.79194444
lon: -71.11527778
The Four Squatters is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising nearly 2,500 meters (8,200 ft) above Duncan Lake in. The nearest higher neighbor is line parent Howser Peak, to the northeast. History.

Geographic entities mentioned:
surface_form: Howser Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.813889
lon: -116.681111
The Four Squatters. The Four Squatters is a mountain in British Columbia, Canada. Description. The Four Squatters is located in the Purcell Mountains, southwest of Bugaboo Provincial Park, and southeast of the confluence of East Creek and Duncan River. Precipitation runoff from The Four Squatters drains into East and Howser creeks, which are both tributaries of the Duncan River.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: the four squatters
instance_of: Mountain
countries: Canada
coordinates: lat: 50.605167
lon: -116.903243
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The Four Squatters. The Four Squatters is a mountain in British Columbia, Canada. Description. The Four Squatters is located in the Purcell Mountains, southwest of Bugaboo Provincial Park, and southeast of the confluence of East Creek and Duncan River. Precipitation runoff from The Four Squatters drains into East and Howser creeks, which are both tributaries of the Duncan River.

Geographic entities mentioned:
surface_form: the four squatters
instance_of: Mountain
countries: Canada
coordinates: lat: 50.605167
lon: -116.903243
Precipitation runoff from The Four Squatters drains into East and Howser creeks, which are both tributaries of the Duncan River. The Four Squatters is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising nearly 2,500 meters (8,200 ft) above Duncan Lake in.

Geographic entities mentioned:
surface_form: the four squatters
instance_of: Mountain
countries: Canada
coordinates: lat: 50.605167
lon: -116.903243
The nearest higher neighbor is line parent Howser Peak, to the northeast. History. The landform's name was applied in 1910 by Canadian surveyor Arthur Oliver Wheeler, and the mountain's toponym was officially adopted on June 9, 1960, by the Geographical Names Board of Canada.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
have been traced to the Munda languages by linguists. There are many Munda pockets in Chota Nagpur Plateau, in which the remnants of Munda culture are strong. It is held that changes in the phonetics and vocabulary of the Vedic language can be explained as much on the basis of the Dravidian influence as that of the Munda. Mediaeval to modern history.

Geographic entities mentioned:
surface_form: Chota Nagpur Plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
Grant formed what became the largest Baptist congregation in the Gaelic-speaking Highlands, and was at the forefront of evangelism in the area. Early life. Grant was born in Ballentua, Strathspey, Scotland, in 1783. He was reared in a small-farming family but grew a considerable ministry as a Baptist pastor,poet, and songwriter.

Geographic entities mentioned:
surface_form: Strathspey
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.45
lon: -3.3
New York State Route 64. New York State Route 64 (NY 64) is a north–south state highway in the Finger Lakes region of New York in the United States. Its southern terminus is at an intersection with NY 21 in the hamlet of Bristol Springs within the town of South Bristol, Ontario County. The northern terminus is at a junction with NY 96 and NY 252 in the village of Pittsford, Monroe County.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
The northern terminus is at a junction with NY 96 and NY 252 in the village of Pittsford, Monroe County. NY 64 is a mostly two-lane highway that primarily serves as a connector between the southeastern suburbs of the city of Rochester and the Canandaigua Lake area, home to Bristol Mountain Ski Resort. Near the midpoint of the route, NY 64 has an overlap with U.S.

Geographic entities mentioned:
surface_form: Canandaigua Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.756666666667
lon: -77.317777777778
Route description. NY 64 begins at an intersection with NY 21 on a ridge overlooking Canandaigua Lake in Bristol Springs, a hamlet of South Bristol. The route heads to the northwest as a two-lane highway, running in the base of the Bristol Valley, a lowland created by a pair of imposing mountain ranges to the east and west that is home to the Bristol Mountain Ski Resort.

Geographic entities mentioned:
surface_form: Canandaigua Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.756666666667
lon: -77.317777777778
At a dinner in their honour he proposed the &quot;founding of a New Zealand Alpine Club&quot;, which eventually occurred in 1891. In the late 1880s Green did survey work in the Rocky Mountains of British Columbia, including the first ascent of Mount Bonney in 1888. Mount Green in Glacier National Park of the Selkirk Mountains is named in his honour, as well as Mount Green in New Zealand.

Geographic entities mentioned:
surface_form: Mount Bonney
instance_of: Mountain
countries: Canada
coordinates: lat: 51.20472222222222
lon: -117.5411111111111
In the late 1880s Green did survey work in the Rocky Mountains of British Columbia, including the first ascent of Mount Bonney in 1888. Mount Green in Glacier National Park of the Selkirk Mountains is named in his honour, as well as Mount Green in New Zealand. He was appointed a Companion of the Order of the Bath (CB) in the 1907 Birthday Honours.

Geographic entities mentioned:
surface_form: Mount Green
instance_of: Mountain
countries: Canada
coordinates: lat: 51.229
lon: -117.5806
It is located in the Junín Region, Huancayo Province, Huancayo District. Kawituyuq lies south of the Waytapallana mountain range, southwest of Yana Uqsha.

Geographic entities mentioned:
surface_form: yana uqsha
instance_of: Mountain
countries: Peru
coordinates: lat: -10.53083333
lon: -76.91083333
surface_form: uqsha
instance_of: Mountain
countries: Peru
coordinates: lat: -12.0883
lon: -76.0617
surface_form: yana uqsha
instance_of: Mountain
countries: Peru
coordinates: lat: -11.08083333
lon: -76.52
surface_form: yana uqsha
instance_of: Mountain
countries: Peru
coordinates: lat: -11.9392
lon: -75.0528
Kawituyuq. Kawituyuq (Quechua &quot;kawitu&quot; camp bed; rocking chair; swing; barbecue, &quot;-yuq&quot; a suffix to indicate ownership, possibly &quot;the one with a camp bed&quot;, also spelled &quot;Cahuituyoc&quot;) is a mountain in the Andes of Peru. It is located in the Junín Region, Huancayo Province, Huancayo District.

Geographic entities mentioned:
surface_form: kawituyuq
instance_of: Mountain
countries: Peru
coordinates: lat: -12.13388889
lon: -75.57972222
surface_form: kawituyuq
instance_of: Mountain
countries: Peru
coordinates: lat: -11.9761
lon: -75.0567
Lindeman Lake (Chilkoot Trail). Lindeman Lake, also known as Lake Lindeman, is a lake on the Chilkoot Trail in far northwestern British Columbia, Canada. It is just south of Bennett Lake and northeast of the summit of the Chilkoot Pass. From the direction of the pass it is fed by Lindeman Creek (formerly known as One Mile River), which connects the two lakes.

Geographic entities mentioned:
surface_form: Bennett Lake
instance_of: Lake
countries: Canada
coordinates: lat: 60.09166666666667
lon: -134.86555555555555
Lindeman Lake (Chilkoot Trail). Lindeman Lake, also known as Lake Lindeman, is a lake on the Chilkoot Trail in far northwestern British Columbia, Canada. It is just south of Bennett Lake and northeast of the summit of the Chilkoot Pass. From the direction of the pass it is fed by Lindeman Creek (formerly known as One Mile River), which connects the two lakes.

Geographic entities mentioned:
surface_form: Lindeman Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 59.83267
lon: -135.00366
Lindeman Lake (Chilkoot Trail). Lindeman Lake, also known as Lake Lindeman, is a lake on the Chilkoot Trail in far northwestern British Columbia, Canada. It is just south of Bennett Lake and northeast of the summit of the Chilkoot Pass. From the direction of the pass it is fed by Lindeman Creek (formerly known as One Mile River), which connects the two lakes.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: lindeman lake
instance_of: Lake
countries: Canada
coordinates: lat: 59.8
lon: -135.0561111111111
surface_form: lindeman lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.11527777777778
lon: -121.45694444444445
From the direction of the pass it is fed by Lindeman Creek (formerly known as One Mile River), which connects the two lakes. Lake Lindeman and Lake Bennett were key components of the Chilkoot Trail during the Klondike Gold Rush, with both seeing hundreds of vessels built to transit their waters and camp-town &quot;tent cities&quot; established on their shores.

Geographic entities mentioned:
surface_form: lake bennett
instance_of: Lake
countries: Canada
coordinates: lat: 60.09166666666667
lon: -134.86555555555555
Lake Lindeman and Lake Bennett were key components of the Chilkoot Trail during the Klondike Gold Rush, with both seeing hundreds of vessels built to transit their waters and camp-town &quot;tent cities&quot; established on their shores. Lindeman was located at the south end of Lindeman Lake, while Bennett, often known as Bennett City, was at the south end of Lake Bennett.

Geographic entities mentioned:
surface_form: lake bennett
instance_of: Lake
countries: Canada
coordinates: lat: 60.09166666666667
lon: -134.86555555555555
surface_form: lindeman lake
instance_of: Lake
countries: Canada
coordinates: lat: 59.8
lon: -135.0561111111111
surface_form: lindeman lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.11527777777778
lon: -121.45694444444445
Lindeman Lake (Chilkoot Trail). Lindeman Lake, also known as Lake Lindeman, is a lake on the Chilkoot Trail in far northwestern British Columbia, Canada. It is just south of Bennett Lake and northeast of the summit of the Chilkoot Pass. From the direction of the pass it is fed by Lindeman Creek (formerly known as One Mile River), which connects the two lakes.

Geographic entities mentioned:
surface_form: lindeman lake
instance_of: Lake
countries: Canada
coordinates: lat: 59.8
lon: -135.0561111111111
surface_form: lindeman lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.11527777777778
lon: -121.45694444444445
The three explorers and two of their servants would set out each day, leaving the other two men at their campsite, and mark out a trail, before turning back later in the day to cut a path for the horses and allow the rest of the party to progress. The group first saw the plains beyond the mountains from Mount York.

Geographic entities mentioned:
surface_form: Mount York
instance_of: Mountain
countries: Australia
coordinates: lat: -33.553
lon: 150.22
He died of strangury on 20 July 1819, and, although an eminent man, was buried in an unmarked grave in Old Calton Burial Ground, on Waterloo Place in Edinburgh. His, and his brother, James's graves were marked by a plaque unveiled in 2011 following a local campaign. The monument to his memory by William Henry Playfair, on Calton Hill, is visible from the spot. Critical bibliography.

Geographic entities mentioned:
surface_form: Calton Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.955278
lon: -3.182222
Jupiter orders Venus to bring love to Dis, in fulfillment of the prophecy. Ceres has already sought to conceal the innocent Proserpina by sending her to safety in Sicily, Ceres' earthly home and sanctuary; but Dis comes out from the volcano at Mount Etna in his chariot, seizes Proserpina at the Pergusa Lake near Enna, and takes her down into the underworld. The poem ends at this point.

Geographic entities mentioned:
surface_form: Pergusa Lake
instance_of: Lake
countries: Italy
coordinates: lat: 37.513888888889
lon: 14.305833333333
It is endemic to the Mojave Desert of the United States, where it is known only from the Funeral Mountains and Death Valley area in eastern California, and the Ash Meadows area just over the border in Nevada. It grows in wet, highly alkaline habitat, such as seeps and mineral springs. Description.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Pontastacus pachypus. &quot;Pontastacus pachypus&quot;, the Caspian crayfish is a species of crayfish found in the Caspian Sea, the Don river, and parts of the Black Sea and Sea of Azov, where it lives in salinities of up to 14‰. It is listed as Data Deficient in the IUCN Red List.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
The aforementioned episodes aired on BBC2 on 18–20 December 2017. The series was filmed mainly in Hadfield, Derbyshire; other locations include Bacup, Lancashire; Glossop, Gamesley, and Hope Valley in Derbyshire; Marsden, Todmorden, and Sowerby Bridge in West Yorkshire; and Mottram in Greater Manchester. History.

Geographic entities mentioned:
surface_form: Hope Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.34727
lon: -1.7455
Another town to feature prominently in the series was Bacup in Rossendale, and the West Yorkshire town of Todmorden was used for some later scenes. Other locations include Glossop, Gamesley, and Hope Valley in Derbyshire; Marsden and Sowerby Bridge in West Yorkshire; and Mottram in Greater Manchester. The &quot;Local Shop&quot; is a purpose-built building on nearby Marsden Moor. Characters.

Geographic entities mentioned:
surface_form: Hope Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.34727
lon: -1.7455
Dombrava. Dombrava () is a settlement in the lower Vipava Valley in the Municipality of Renče–Vogrsko in the Littoral region of Slovenia. Name. The name &quot;Dombrava&quot;, with an &quot;m&quot; reflecting the old nasal vowel *&quot;ǫ&quot;, shares its origin with the more frequent place name &quot;Dobrava&quot; (e.g., Dolenja Dobrava).

Geographic entities mentioned:
surface_form: Vipava Valley
instance_of: Valley
countries: Slovenia
coordinates: lat: 45.876147222222
lon: 13.907319444444