Sarmila/GeoWiki-Features huggingface dataset:
Location. Cusco extends throughout the Huatanay (or Watanay) river valley. Located on the eastern end of the Knot of Cusco, its elevation is around. To its north is the Vilcabamba mountain range with mountains. The highest peak is Salcantay () about northwest of Cusco. Climate. Cusco has a subtropical highland climate (Köppen: &quot;Cwb&quot;, Trewartha: &quot;Cwll&quot;).

Geographic entities mentioned:
surface_form: Salcantay
instance_of: Mountain
countries: Peru
coordinates: lat: -13.333611111111
lon: -72.544444444444
Exile. For the remainder of the war, Prince Paul was kept, with his family, under house arrest by the British in Kenya. Paul and his family arrived at Oserian, the former home of Lord Erroll on the shores of Lake Naivasha on 28 April 1941. Oserian was in a state of disrepair as the earl had been murdered earlier in 1941 and Princess Olga called it &quot;a complete nightmare&quot;.

Geographic entities mentioned:
surface_form: Lake Naivasha
instance_of: Lake
countries: Kenya
coordinates: lat: -0.76852777777778
lon: 36.350644444444
Lake Eden. Lake Eden (also referred to as Eden Lake) is a small, recreational lake in Alberta, Canada. It lies west of Stony Plain, Alberta. It has an area of, and has a mean depth of only ~, with clear water. History. In the early 1950s it was named Lake Eden by the owners of the Lake Eden Fur Farm, whose farm sat adjacent to the lake.

Geographic entities mentioned:
surface_form: lake eden
instance_of: Lake
countries: Canada
coordinates: lat: 53.5811
lon: -114.155
Lake Eden. Lake Eden (also referred to as Eden Lake) is a small, recreational lake in Alberta, Canada. It lies west of Stony Plain, Alberta. It has an area of, and has a mean depth of only ~, with clear water. History. In the early 1950s it was named Lake Eden by the owners of the Lake Eden Fur Farm, whose farm sat adjacent to the lake.

Geographic entities mentioned:
surface_form: lake eden
instance_of: Lake
countries: Canada
coordinates: lat: 53.5811
lon: -114.155
surface_form: lake eden
instance_of: Lake
countries: Canada
coordinates: lat: 53.5811
lon: -114.155
At Lake Mungo, in Western New South Wales, burial sites have been excavated and burial materials, including ochre-painted bones, have been dated to the arrival of people in Australia; &quot;Mungo Man&quot; (LM3) was buried sprinkled with red ochre at least 30,000 BP, and possibly as early as 60,000 BP.

Geographic entities mentioned:
surface_form: Lake Mungo
instance_of: Lake
countries: Australia
coordinates: lat: -33.75
lon: 143.08333333333
On September 15, the NHC first issued a tropical storm watch for the entirety of New Jersey's coastline from the Delaware Bay to the New York Metro area. Early the next day, this was upgraded to a hurricane warning as far north as Manasquan Inlet, with a tropical storm warning extending northward to New York.

Geographic entities mentioned:
surface_form: Manasquan Inlet
instance_of: Landform
countries: United States
coordinates: lat: 40.1025
lon: -74.035
As early as 5,200 years before present, Native Americans built fish weirs here, evidence of which was discovered during subway construction in 1913 (&quot;see&quot; Ancient Fishweir Project and Boylston Street Fishweir). In 1814, the Boston and Roxbury Mill Corporation was chartered to construct a milldam, which would also serve as a toll road connecting Boston to Watertown, bypassing Boston Neck.

Geographic entities mentioned:
surface_form: Boston Neck
instance_of: Landform
countries: United States
coordinates: lat: 42.34394444
lon: -71.06597222
After that, he worked as an intern at a national library in 1939. In 1941, he joined the Directorate General of Antiquities and worked as a writer at the National Museum. In 1942, he moved to Baalbek to become the manager of Beqaa Valley Ruins. He was among the contributors of the Beirut-based literary magazine &quot;Al Adib&quot;.

Geographic entities mentioned:
surface_form: Beqaa Valley
instance_of: Valley
countries: Lebanon
coordinates: lat: 34.008888888889
lon: 36.145277777778
Prior to colonization, the center of Duwamish society was around the Black and Duwamish rivers in Washington. The modern Duwamish primarily descend from two separate groups: the, or Duwamish, and the, a group of peoples whose traditional territory extends around Lake Washington.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
However, beginning around 1855, the word &quot;Duwamish&quot; was used to also include the Green and White river peoples and the. The were composed of several related peoples whose villages were located along Lake Washington and the Sammamish River; the ', whose villages were located around Lake Union, and the Shilshole ('), whose village was located on Salmon Bay.

Geographic entities mentioned:
surface_form: Lake Union
instance_of: Lake
countries: United States
coordinates: lat: 47.6392
lon: -122.3337
It is part of the Columbia River Basin, as the Snake River is a tributary of the Columbia River. Its canyon was carved out by a fork in the catastrophic Missoula Floods of the previous ice age, which spilled over the northern Columbia Plateau and flowed into the Snake River, eroding the river's present course in a few thousand years. Course.

Geographic entities mentioned:
surface_form: Columbia Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 45.999444444444
lon: -119.00138888889
Located entirely within British Columbia, Canada, they run northwest from the lower stretches of the Fraser River to Bella Coola and Burke Channel, north of which are the Kitimat Ranges. The Coast Mountains lie between the Interior Plateau and the Coast of British Columbia. The Pacific Ranges include four of the five major coastal icecaps in the southern Coast Mountains.

Geographic entities mentioned:
surface_form: Interior Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 52
lon: -123
These are the largest temperate-latitude icecaps in the world and fuel a number of very major rivers (by volume, not length). One of these contains Mount Waddington, the highest summit entirely within British Columbia. Also within this region is Hunlen Falls, among the highest in Canada, located in Tweedsmuir South Provincial Park.

Geographic entities mentioned:
surface_form: Mount Waddington
instance_of: Mountain
countries: Canada
coordinates: lat: 51.373611111111
lon: -125.26333333333
The Garibaldi Volcanic Belt is within the Pacific Ranges, which is a volcanic belt formed by the subduction of the Juan de Fuca Plate (a remnant of the much larger Farallon Plate) under the North American Plate along the Cascadia subduction zone. The belt is the northern extension of the Cascade Volcanic Arc in the United States (which includes the volcanoes Mount St.

Geographic entities mentioned:
surface_form: Garibaldi Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5283
lon: -126.113
The Garibaldi Volcanic Belt is within the Pacific Ranges, which is a volcanic belt formed by the subduction of the Juan de Fuca Plate (a remnant of the much larger Farallon Plate) under the North American Plate along the Cascadia subduction zone. The belt is the northern extension of the Cascade Volcanic Arc in the United States (which includes the volcanoes Mount St.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: Mount Baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
The most recent major catastrophic eruption in the Garibaldi Volcanic Belt was from the Mount Meager massif 2,350 BP, which is Canada's most recent major catastrophic eruption. The Garibaldi Volcanic Belt contains two extra volcanic fields, the Franklin Glacier Complex and the Silverthrone Caldera, which lie 140 and 190 km northwest of the main volcanic belt.

Geographic entities mentioned:
surface_form: Franklin Glacier Complex
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3333
lon: -125.4
surface_form: Silverthrone Caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
Warner Bros. and Miller wanted to start filming immediately, but production was pushed back three months. Originally, the majority of &quot;Justice League: Mortal&quot; would be shot at Fox Studios Australia in Sydney, with other locations scouted nearby at local colleges, and Sydney Heads doubling for Happy Harbor.

Geographic entities mentioned:
surface_form: Sydney Heads
instance_of: Landform
countries: Australia
coordinates: lat: -33.8368
lon: 151.281
&quot;African Sanctus&quot; is a 1972 choral Mass and is the best-known work of British composer and collector of world musics David Fanshawe. In &quot;African Sanctus&quot; the Latin Mass is juxtaposed with live recordings of traditional African music, which the composer had recorded himself between 1969 and 1973 during a journey up the Nile, from the Mediterranean Sea to Lake Victoria.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
He was ordained deacon and priest by Bishop Lugidius, either at Clonmacnoise or Connor. He lived for a while in Ulster on an island on Lough Erne, accompanied by a few friends who followed a severe form of monastic life. The regime was so austere that seven companions died of cold and hunger.

Geographic entities mentioned:
surface_form: Lough Erne
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.48262
lon: -7.80622
The topography includes broad open park-like basins at higher elevations. Elevations range from 3,000 feet (900 m) at the Greenwater River in the north to 6,856 foot (2090 m) Norse Peak in the west and 6900 foot (2100 m) Fifes Peaks, a prominent remnant volcanic cone in the east. The eastern portion is drained by tributaries of the Naches River.

Geographic entities mentioned:
surface_form: Fifes Peaks
instance_of: Landform
countries: United States
coordinates: lat: 46.9737
lon: -121.3229
Durban, Gers. Durban () (&quot;Durban&quot; in Gascon) is a commune in the Gers department in southwestern France in the Occitanie Region. Historically and culturally, the town is in the country of Astarac, a territory in the very hilly south of Gers, with clay soil, which runs along the Plateau de Lannemezan.

Geographic entities mentioned:
surface_form: Plateau de Lannemezan
instance_of: Plateau
countries: France
coordinates: lat: 43.16666667
lon: 0.38333333
Natri Lake. Natri Lake () is a lake in south-central Chiloé Island, Chile. It has an area of 7.8 km2. The lake's catchment basin is mostly made up of hilly terrain that is covered by native forest, and to a lesser extent natural prairies. Chile Route 5 passes next to the lake's eastern end.

Geographic entities mentioned:
surface_form: natri lake
instance_of: Lake
countries: Chile
coordinates: lat: -42.794166666667
lon: -73.817777777778
Career. He debuted competing in FIS events at the national championships in Krasiya in Ukraine in 2015. In 2016, he firstly competed at the FIS Snowboarding Junior World Championships, held in Rogla without reaching a qualification in parallel slalom and parallel giant slalom events. In 2017, he debuted competing at the World Cup event in Carezza, reaching 65th place.

Geographic entities mentioned:
surface_form: Rogla
instance_of: Mountain
countries: Slovenia
coordinates: lat: 46.4525
lon: 15.333611
In 2017, he debuted competing at the World Cup event in Carezza, reaching 65th place. The following years, Mykhailo became a world junior champion at the 2019 Snowboarding Junior World Championships, held in Rogla, in parallel slalom event. In 2020, Mykhailo won a silver medal at the European Cup stage in Gudauri, Georgia.

Geographic entities mentioned:
surface_form: Rogla
instance_of: Mountain
countries: Slovenia
coordinates: lat: 46.4525
lon: 15.333611
She had at least three brothers, Ramesses, Khaemwaset and Merneptah and a sister who was named Isetnofret after their mother. Bintanath had a daughter who appears on the paintings in her tomb in the Valley of the Queens. She is unnamed there and her father is unknown, but according to Joyce Tyldesley it is possible that her name was also Bintanath and she married the next pharaoh, Merneptah.

Geographic entities mentioned:
surface_form: Valley of the Queens
instance_of: Valley
countries: Egypt
coordinates: lat: 25.7275
lon: 32.593055555556
Death and burial. Despite her being Ramesses' first daughter, she was actually one of the few children who outlived their long-lived father. She was depicted on a statue usurped by Merenptah. She died during the reign of her brother Merneptah and was buried in the tomb QV71 in the Valley of the Queens. The tomb is described by Lepsius (number 4).

Geographic entities mentioned:
surface_form: Valley of the Queens
instance_of: Valley
countries: Egypt
coordinates: lat: 25.7275
lon: 32.593055555556
Coqên Town. Coqên is a town and seat of Coqên County in Ngari Prefecture of the Tibet Autonomous Region of China. It lies at an altitude of 4,718 metres (15,482 feet). It is on the main route between Lhasa and Kashgar, northwest of Lhaze. Lakes not too far away include Zhari Nanmu Lake, Dawa Lake and Taruo Lake.

Geographic entities mentioned:
surface_form: Dawa Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 31.24444444
lon: 84.95416667
surface_form: Taruo Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 31.1333
lon: 84.1167
The new autonomous community would consist of the provinces of Granada, Almería and Málaga. The conception has not yet found a response. Geography. The tallest mountain in the Iberian Peninsula, Mulhacén, is located in Granada. It measures. The next highest mountains in the province are Veleta () and Alcazaba ().

Geographic entities mentioned:
surface_form: Mulhacén
instance_of: Mountain
countries: Spain
coordinates: lat: 37.053333333333
lon: -3.3113888888889
Ontario communities served by Northern Access Network besides Pickle Lake and Longlac included Armstrong, Balmertown, Caramat, Cochenour, Dubreuilville, Ear Falls, Ignace, Mattabi Mines, Moosonee, Nakina, Sioux Lookout, South Bay Mine and Wawa. In early 1978, Manitoba stations were established at Gillam, Leaf Rapids and Lynn Lake, where the only existing television at the time was from CBC.

Geographic entities mentioned:
surface_form: Leaf Rapids
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.4627
lon: -100.0108
Etymology. The modern name of Mount Hasan is widely accepted to be in dedication to Ebu'l-Gazi (El-Hasan), brother of Ebu'l-Kasım during the reign of the Anatolian Seljuks. It is hypothesized that Mount Hasan’s name was “&quot;Argeos&quot;” or “&quot;Argaios&quot;”, but this name belongs to Mount Erciyes.

Geographic entities mentioned:
surface_form: Mount Erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
surface_form: erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
surface_form: mount erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
Another hypothesis is that it was simply called &quot;Árgos&quot;, (Ancient Greek: Ἄργος) as well as Argeiopolis Mons. The Hittites called it. Geography and geomorphology. Mount Hasan lies in the Anatolian plateau, between the Taurus Range and the Pontic Mountains, and its and Mount Erciyes's silhouettes dominate the landscape and rise high above the surrounding terrain.

Geographic entities mentioned:
surface_form: Mount Erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
surface_form: erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
surface_form: mount erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
The volcano has been prospected as a potential source for geothermal power. Mount Hasan is part of a larger volcanic province in Central Anatolia known as the Central Anatolian or Cappadocian Volcanic Province., which includes ignimbrites, monogenetic volcanic fields and stratovolcanoes such as Mount Erciyes, Mount Hasan, Karacadağ and Melendiz Dağ with an area of about -.

Geographic entities mentioned:
surface_form: Mount Erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
surface_form: erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
surface_form: mount erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
This alignment is congruent with the tectonic patterns of Anatolia, where the collision between Africa and Eurasia follows the same trend. It and to some degree Mount Hasan are also surrounded by a large depression, and the volcanoes of this alignment are separated by faults. Additionally, Mount Hasan forms a volcanic lineament with and the Karapınar Field.

Geographic entities mentioned:
surface_form: Karapınar Field
instance_of: Mountain
countries: Turkey
coordinates: lat: 37.67
lon: 33.65
surface_form: karapınar field
instance_of: Mountain
countries: Turkey
coordinates: lat: 37.67
lon: 33.65
Mount Hasan. Mount Hasan () is a volcano in Anatolia, Turkey. It has two summits, the high eastern Small Hasan Dagi and the high Big Hasan Dagi, and rises about above the surrounding terrain. It consists of various volcanic deposits, including several calderas, and its activity has been related to the presence of several faults in the area and to regional tectonics.

Geographic entities mentioned:
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
Etymology. The modern name of Mount Hasan is widely accepted to be in dedication to Ebu'l-Gazi (El-Hasan), brother of Ebu'l-Kasım during the reign of the Anatolian Seljuks. It is hypothesized that Mount Hasan’s name was “&quot;Argeos&quot;” or “&quot;Argaios&quot;”, but this name belongs to Mount Erciyes.

Geographic entities mentioned:
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
Mount Hasan lies in the Anatolian plateau, between the Taurus Range and the Pontic Mountains, and its and Mount Erciyes's silhouettes dominate the landscape and rise high above the surrounding terrain. The city of Aksaray lies northwest from Mount Hasan, while the settlements of Helvadere, Uluören, Dikmen and Taşpınar lie clockwise from north to northwest around the volcano.

Geographic entities mentioned:
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
Big Hasan Dagi has two nested craters with an wide and high inner cone that is the source of a lava flow. Whether they are located within a caldera is unclear; rather than one large caldera encompassing the entire complex, there may be a smaller one underlying Mount Hasan specifically. There is periglacial activity on the summit, and fossil rock glaciers are found on the volcano.

Geographic entities mentioned:
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
Hasan ashes&quot; unit and into a lava unit. Cinder cones, maars and accompanying lava flows also occur around Mount Hasan, they are part of a basaltic volcano family that forms parasitic vents. These include the cone/maar and a lava flow field at which covers an area of and was produced by fissure vents.

Geographic entities mentioned:
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
Further, volcanism at Mount Hasan has been related to the Tuz Gölü Fault and its intersection with the Karaman-Aksaray faults; the former of these is one of two major fault systems in Central Anatolia which influence volcanism there, and volcanic products of Mount Hasan have been deformed by the fault.

Geographic entities mentioned:
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
The Hasandag fault branches off the Karaman-Aksaray fault and cuts between the two summits of Mount Hasan. It and the Karacaören fault influence the hydrothermal system of the volcano. The westerly Mount Hasan, central and easterly form the Niğde Volcanic Complex, a mountain range, which is surrounded by plains and whose summits reach heights of over.

Geographic entities mentioned:
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
This alignment is congruent with the tectonic patterns of Anatolia, where the collision between Africa and Eurasia follows the same trend. It and to some degree Mount Hasan are also surrounded by a large depression, and the volcanoes of this alignment are separated by faults. Additionally, Mount Hasan forms a volcanic lineament with and the Karapınar Field.

Geographic entities mentioned:
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
The basaltic family includes both basaltic andesite and alkali basalts with augite, clinopyroxene, garnet, hornblende, hypersthene, olivine, orthopyroxene, oxides and plagioclase. Magma mixing processes appear to be the most important mechanisms involved in the genesis of Mount Hasan magmas, which are derived from the mantle with participation of crustal components.

Geographic entities mentioned:
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
Between October/November and May, the mountain is frequently covered by snow due to the common precipitation at that time and when it melts the water mostly infiltrates into the permeable rocks, making the volcano a principal groundwater recharge area in the region. Additionally, volcanics of Mount Hasan form a major aquifer and the Melendiz River passes north and northeast of the volcano.

Geographic entities mentioned:
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
Additionally, volcanics of Mount Hasan form a major aquifer and the Melendiz River passes north and northeast of the volcano. Eruption history. Mount Hasan has been active for the last 13 million years, with the, Paleo-Hasan, Mesovolcano and Neovolcano stages during the Miocene, Miocene-Pliocene and Quaternary; the older two stages might actually not be part of Mount Hasan at all.

Geographic entities mentioned:
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
Aside from the felsic central vent volcanism, basaltic volcanism also took place at Mount Hasan throughout its activity; this activity has been dated to 120,000, 65,000 and the most recent event 34,000 years ago. This volcanism however is not part of the actual Mount Hasan system. The main edifice has produced about of magma every millennium, more than at Erciyes.

Geographic entities mentioned:
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
is the oldest (13 million years) volcanic structure, it is among the oldest volcanoes of the Central Anatolian volcanic province. This volcano is a small sized volcano with a caldera which crops out on the southwestern side of Mount Hasan. It grew over sediments to a present-day elevation of; today it is eroded, partly buried by the younger Hasan volcanics and disrupted by strike-slip faulting.

Geographic entities mentioned:
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
It grew over sediments to a present-day elevation of; today it is eroded, partly buried by the younger Hasan volcanics and disrupted by strike-slip faulting. About 7 million years ago the Paleovolcano began to grow north of; it too is buried by more recent volcanics but part of its deposits crop out on the northwestern flank of Mount Hasan in the form of ignimbrites, lahars and lava flows.

Geographic entities mentioned:
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
The Paleovolcano also formed a caldera which produced the rhyolitic Dikmen-Taspinar Ignimbrites; formerly the Cappadocian tuffs were in general attributed to volcanism at Mount Hasan, Mount Erciyes and Göllü Dag. The Quaternary activity gave rise to the Mesovolcano and Neovolcano, with the former centered between the two present-day summits.

Geographic entities mentioned:
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
surface_form: göllü dag
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.254662
lon: 34.5446
surface_form: erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
surface_form: mount erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
Small Mount Hasan is probably older as it is more heavily eroded while the morphology of Big Hasan Dagi is fresher although its pyroclastic flow deposits are heavily incised. Dates of 33,000 and 29,000 years ago have been obtained on the summit domes and ages of 66,000±7,000 years on the most recent monogenetic volcano south of Mount Hasan.

Geographic entities mentioned:
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
Explosive eruptions took place 28,900 ± 1,500 and 13,500 ± 1,500 years ago. Tephras found in the Konya plain and in a lake of the Turkish Lakes Region have been attributed to Mount Hasan. The debris flow from Mount Hasan occurred 150,000-100,000 years ago and a number of lava flows were emplaced during the last 100,000 years. Holocene and present activity.

Geographic entities mentioned:
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
Holocene and present activity. Eruptions occurred 8,970 ± 640, 8,200, less than 6,000 years ago and 0 ± 3,000 years ago; the first emplaced pumice on the summit, the penultimate of these formed a lava dome on the northern flank while the last formed a lava flow on Mount Hasan's western foot. A shift in archeological sites around Mount Hasan may be linked to the older eruptions.

Geographic entities mentioned:
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
the volcano is not monitored. Possible portrayal of an eruption in a mural from Çatalhöyük. A mural discovered in Çatalhöyük has been interpreted as showing a volcanic eruption, commonly linked to Mount Hasan, and this mural has even been interpreted as being the oldest known map.

Geographic entities mentioned:
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
The depicted activity resembles Strombolian eruptions, and the event may not have been directly visible from Çatalhöyük. The discovery of this mural has drawn attention to the volcano and has led to efforts to date the eruptive activity of Mount Hasan. Importance during ancient history. Mount Hasan was used as a source for Obsidian. The Byzantine city of Mokissos was located on Mount Hasan.

Geographic entities mentioned:
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
The depicted activity resembles Strombolian eruptions, and the event may not have been directly visible from Çatalhöyük. The discovery of this mural has drawn attention to the volcano and has led to efforts to date the eruptive activity of Mount Hasan. Importance during ancient history. Mount Hasan was used as a source for Obsidian. The Byzantine city of Mokissos was located on Mount Hasan.

Geographic entities mentioned:
surface_form: mount hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
In general, various sources have been proposed for the magmas of the Central Anatolian province. The magmatic system of Mount Hasan appears to be more active than that of Mount Erciyes. The magmas formed at different depths, with basalts originating at about depth at the base of the crust, while the other volcanic rocks have shallower sources.

Geographic entities mentioned:
surface_form: erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
surface_form: mount erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
This volcanism however is not part of the actual Mount Hasan system. The main edifice has produced about of magma every millennium, more than at Erciyes. is the oldest (13 million years) volcanic structure, it is among the oldest volcanoes of the Central Anatolian volcanic province. This volcano is a small sized volcano with a caldera which crops out on the southwestern side of Mount Hasan.

Geographic entities mentioned:
surface_form: erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
However, it is difficult to be certain as potatoes do not preserve well compared to other crops. Potatoes dating to about 2000 BC were also found at Huaynuma, in the Casma Valley of Peru, and early potatoes dating to 800-500 BC were also uncovered at the Altiplano site of Chiripa on the east side of Lake Titicaca.

Geographic entities mentioned:
surface_form: Casma Valley
instance_of: Valley
countries: Peru
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
In the Incan period, potato and legume consumption decreased (although still commonly consumed) in favor of crops like maize. Aside from these remains, in the Peruvian archaeological record, the potato was uncovered as a design influence of ceramic pottery in the Altiplanos, often in the shape of vessels.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Uses in South American societies. In the Altiplano, potatoes provided the principal energy source for the Inca Empire, its predecessors, and its Spanish successor. Andean people prepared their potatoes in a variety of ways, such as boiled, mashed, baked, and stewed in ways similar to modern methods.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
In a report written during the 1820 Cass Expedition, James Duane Doty wrote of crops grown around Leech Lake, Sandy Lake, and Fond du Lac, in what is now Minnesota, which the Ojibwe called &quot;waub-es-see-pin,&quot; indicating a type of potato. Potatoes were planted in Idaho as early as 1838; by 1900 the state's production exceeded a million bushels (about 27,000 tonnes).

Geographic entities mentioned:
surface_form: Leech Lake
instance_of: Lake
countries: United States
coordinates: lat: 47.166666666667
lon: -94.366666666667
surface_form: Sandy Lake
instance_of: Lake
countries: United States
coordinates: lat: 46.768
lon: -93.274
Ozo Golf Club. Ozo Golf Club is a golf club and course on the west bank of the Ķīšezers lake in Riga, Latvia. It is the national training centre for Latvian golf teams – and host to both the national tournament and the Baltic tournament. The club opened in 2002 and is owned by the retired Latvian ice hockey player Sandis Ozoliņš.

Geographic entities mentioned:
surface_form: Ķīšezers lake
instance_of: Lake
countries: Latvia
coordinates: lat: 57.0226
lon: 24.172
Gorenja Žetina. Gorenja Žetina () is a small settlement in the Municipality of Gorenja Vas–Poljane in the Upper Carniola region of Slovenia. It lies at the foot of Mount Blegoš and is a somewhat popular starting point for hikes to its peak.

Geographic entities mentioned:
surface_form: Mount Blegoš
instance_of: Mountain
countries: Slovenia
coordinates: lat: 46.1649
lon: 14.11354
Brachypnoea texana. &quot;Brachypnoea texana&quot; is a species of leaf beetle. It is endemic to the Edwards Plateau in Texas. It was first described by the American entomologist Charles Frederic August Schaeffer in 1919.

Geographic entities mentioned:
surface_form: Edwards Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 30.3
lon: -99.6
He proceeded to perform consistently in the range of 20th–30th, except for an eight place in Naeba in February. Then, until 2007 he only raced once in the World Cup, with a ninth place in Kreischberg in January 2006. The 2006–07 and 2007–08 seasons were mediocre, but in January 2009 he finished fourth in two races. He represents the sports club WSV Walchsee.

Geographic entities mentioned:
surface_form: Kreischberg
instance_of: Mountain
countries: Austria
coordinates: lat: 47.0664
lon: 14.0417
Aulonocara nyassae. &quot;Aulonocara nyassae&quot;, known as the emperor cichlid, is a species of haplochromine Cichlid that is endemic to Lake Malawi in Africa. It has been recorded from the southeastern arm of the lake and may be present in the southwestern arm.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
Oscar Eckenstein. Oscar Johannes Ludwig Eckenstein (9 September 1859 – 8 April 1921) was an English rock climber and mountaineer, and a pioneer in the sport of bouldering. Inventor of the modern crampon, he was an innovator in climbing technique and mountaineering equipment, and the leader of the first serious expedition to attempt K2. Background.

Geographic entities mentioned:
surface_form: K2
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
Mountaineering in the Alps. Together with Matthias Zurbriggen he made the first ascent of the Stecknadelhorn (4,241 m) in the Pennine Alps on 8 August 1887; on 10 July 1906, together with Karl Blodig and Alexis Brocherel, he made the first ascent of Mont Brouillard. Friendship with Aleister Crowley. Eckenstein was one of the few people who readily climbed with mystic and magician Aleister Crowley.

Geographic entities mentioned:
surface_form: Stecknadelhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.111527777778
lon: 7.8596666666667
surface_form: Mont Brouillard
instance_of: Mountain
countries: Italy
coordinates: lat: 45.8175
lon: 6.865
In 1900 Eckenstein travelled to Mexico to climb there with Crowley, they also climbed together on the expedition led by Eckenstein to attempt K2 in 1902. The Baltoro and K2. Eckenstein was a member of an expedition led by Sir Martin Conway to the Baltoro Muztagh region in 1892.

Geographic entities mentioned:
surface_form: K2
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
The highway begins at KY 107 (Deer Lick Road) at Deer Lick. The highway follows Dunmor Deer Lick Road north to the community of Whispering Pines along Lake Malone, where the route meets the east end of KY 1785 (Lake Malone Road). KY 1293 continues northeast through Agnes to its terminus at US 431 (Lewisburg Road) at the Logan–Muhlenberg county line between Hollow Bill and Dunmor. KY 1307.

Geographic entities mentioned:
surface_form: Lake Malone
instance_of: Lake
countries: United States
coordinates: lat: 37.0713
lon: -87.0399
Managua. Managua () is the capital and largest city of Nicaragua, and one of the largest cities in Central America. Located on the shores of Lake Managua, the city had an estimated population of 1,055,247 as of 2020, and a population of 1,401,687 in its metropolitan area. The city also serves as the seat of Managua Department. Founded in 1819, Managua became the national capital in 1852.

Geographic entities mentioned:
surface_form: Lake Managua
instance_of: Lake
countries: Nicaragua
coordinates: lat: 12.333333333333
lon: -86.416666666667
Today, the city is a major economic hub for both the country and Central America. Etymology. There are two possible origins for the name &quot;Managua&quot;. It may have originated from the term &quot;Mana-ahuac&quot;, which in the Nahuatl language translates to &quot;adjacent to the water&quot; or &quot;site surrounded by water&quot; (referring to Lake Managua.

Geographic entities mentioned:
surface_form: Lake Managua
instance_of: Lake
countries: Nicaragua
coordinates: lat: 12.333333333333
lon: -86.416666666667
Residents of the city are called &quot;managuas&quot;, &quot;managüenses&quot;, or &quot;capitalinos&quot;. Origins. Nicaragua was inhabited by Paleo-Indians as far back as 12,000 BC. The ancient footprints of Acahualinca are 2,100-year-old fossils discovered along the shores of Lake Managua.

Geographic entities mentioned:
surface_form: Lake Managua
instance_of: Lake
countries: Nicaragua
coordinates: lat: 12.333333333333
lon: -86.416666666667
Geography. Managua is located on the southern shores of Lake Managua, also known as Lake Xolotlán. Lake Managua contains the same fish species as larger Lake Cocibolca in southeastern Nicaragua, except for the freshwater sharks found exclusively in the latter. Once a Managuan scenic highlight, the lake has been polluted from the dumping of chemical and waste water since 1927.

Geographic entities mentioned:
surface_form: Lake Managua
instance_of: Lake
countries: Nicaragua
coordinates: lat: 12.333333333333
lon: -86.416666666667
Elenydd is generally interpreted to mean the upland area between Pumlumon in the north and Mynydd Epynt in the south. The term &quot;Desert of Wales&quot; is sometimes applied to this or a wider area. Much of Elenydd is open land with public access, following the Countryside and Rights of Way Act 2000, widely known as the &quot;CROW Act&quot;.

Geographic entities mentioned:
surface_form: Desert of Wales
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.310644
lon: -3.721662
Turbidite mudstones of the lower Silurian Cwmere Formation occur around Caban-coch and Carreg-ddu reservoirs. The Caban Conglomerate Formation forms such summits as Drygarn Fawr. To their north and west are the similar lithologies of the Derwenlas Formation which can be seen for example beside the dam of Claerwen Reservoir.

Geographic entities mentioned:
surface_form: Drygarn Fawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.21214
lon: -3.66571
Fleming, New York. Fleming is a town in Cayuga County, New York, United States. The population was 2,475 at the 2020 census. The name is that of General George Fleming, an early settler. Fleming is at the northern end of Owasco Lake, south of Auburn. History. The area of Fleming was first settled &quot;circa&quot; 1790. The town was formed in 1823 from part of the town of Aurelius. Geography.

Geographic entities mentioned:
surface_form: Owasco Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.815
lon: -76.508333333333
According to the United States Census Bureau, Fleming has a total area of, of which is land and, or 10.21%, is water. The eastern town line is defined by Owasco Lake, one of the Finger Lakes. New York State Route 34 and New York State Route 38 are north-south highways in Fleming.

Geographic entities mentioned:
surface_form: Owasco Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.815
lon: -76.508333333333
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
The specific epithet (&quot;coccina&quot;) is a Latin word meaning &quot;red like a berry&quot; or &quot;scarlet&quot;. Distribution and habitat. The scarlet greenhood grows in grassy forest on the higher areas of New South Wales south from Mount Kaputar to north-eastern Victoria.

Geographic entities mentioned:
surface_form: Mount Kaputar
instance_of: Mountain
countries: Australia
coordinates: lat: -30.214722222222
lon: 150.14527777778
Loch Maree. Loch Maree () is a loch in Wester Ross in the Northwest Highlands of Scotland. At long and with a maximum width of, it is the fourth-largest freshwater loch in Scotland; it is the largest north of Loch Ness. Its surface area is. Loch Maree contains five large wooded islands and over 60 smaller ones, many of which have their own lochans.

Geographic entities mentioned:
surface_form: Loch Ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
surface_form: ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
North of the islands lies a shallower area, separating the Slattadale Basin from the Ardlair Basin, the most irregularly shaped of the three. The most prominent mountain on the northern side of Loch Maree is Slioch, one of Scotland's Munros (a mountain over high), which dominates the eastern end of the loch above Kinlochewe.

Geographic entities mentioned:
surface_form: Slioch
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.664688888889
lon: -5.3479611111111
surface_form: slioch
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.664688888889
lon: -5.3479611111111
surface_form: maree
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.689722222222
lon: -5.4575
surface_form: loch maree
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.689722222222
lon: -5.4575
The southwestern side of Loch Maree is also very mountainous, comprising the Torridon Forest. The most prominent peak is Beinn Eighe, which is capped with white quartzite. Three main landowners occupy the southwestern shore: from south to north these are NatureScot (the Beinn Eighe National Nature Reserve), the Grudie & Talladale Estate, and the Gairloch (Flowerdale & Shieldaig) & Conon Estate.

Geographic entities mentioned:
surface_form: Beinn Eighe
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.37
lon: -5.24
surface_form: beinn eighe
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.37
lon: -5.24
Conservation designations. The presence of black-throated divers on the loch has led to it being designated as Special Protection Area (SPA) under the EU Habitats Directive. The loch is also designated as a Special Area of Conservation (SAC), forming part of the Loch Maree Complex SAC, which extends to cover the surrounding hills including Beinn Eighe.

Geographic entities mentioned:
surface_form: Beinn Eighe
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.37
lon: -5.24
surface_form: beinn eighe
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.37
lon: -5.24
surface_form: maree
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.689722222222
lon: -5.4575
surface_form: maree
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.689722222222
lon: -5.4575
surface_form: loch maree
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.689722222222
lon: -5.4575
surface_form: loch maree
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.689722222222
lon: -5.4575
The loch is also designated as a Special Area of Conservation (SAC), forming part of the Loch Maree Complex SAC, which extends to cover the surrounding hills including Beinn Eighe. Over 60 islands within the loch are designated as the Loch Maree Islands National Nature Reserve (NNR), which has since 2014 been jointly managed with the neighbouring Beinn Eighe NNR as a single reserve.

Geographic entities mentioned:
surface_form: Beinn Eighe
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.37
lon: -5.24
surface_form: beinn eighe
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.37
lon: -5.24
surface_form: beinn eighe
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.37
lon: -5.24
surface_form: maree
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.689722222222
lon: -5.4575
surface_form: loch maree
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.689722222222
lon: -5.4575
This has led to speculation that the island was a place of pre-Christian pagan worship which was taken over by the saint. The same island contains ancient stands of oak and holly which have been linked with ancient Scottish druids. Like Loch Ness and Loch Morar, Loch Maree has its own monster in the form of the &quot;muc-sheilch&quot;.

Geographic entities mentioned:
surface_form: Loch Ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
surface_form: Loch Morar
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.95
lon: -5.6722222222222
It is popular for hill walking, scrambling and climbing. Other peaks on the northern side include Beinn Àirigh Charr and Beinn Làir, both of which are classified as Corbetts. The entire length of the northeastern shore of Loch Maree forms part of the Letterewe, Heights of Kinlochewe & Tournaig Estate, which extends north over an area known as the Fisherfield Forest.

Geographic entities mentioned:
surface_form: beinn àirigh charr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.726801
lon: -5.4780421
surface_form: beinn làir
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.7
lon: -5.3666666666667
The most prominent peak is Beinn Eighe, which is capped with white quartzite. Three main landowners occupy the southwestern shore: from south to north these are NatureScot (the Beinn Eighe National Nature Reserve), the Grudie & Talladale Estate, and the Gairloch (Flowerdale & Shieldaig) & Conon Estate. History.

Geographic entities mentioned:
surface_form: beinn eighe
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.37
lon: -5.24
Loch Maree. Loch Maree () is a loch in Wester Ross in the Northwest Highlands of Scotland. At long and with a maximum width of, it is the fourth-largest freshwater loch in Scotland; it is the largest north of Loch Ness. Its surface area is. Loch Maree contains five large wooded islands and over 60 smaller ones, many of which have their own lochans.

Geographic entities mentioned:
surface_form: maree
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.689722222222
lon: -5.4575
surface_form: loch maree
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.689722222222
lon: -5.4575
At long and with a maximum width of, it is the fourth-largest freshwater loch in Scotland; it is the largest north of Loch Ness. Its surface area is. Loch Maree contains five large wooded islands and over 60 smaller ones, many of which have their own lochans. The largest island, Eilean Sùbhainn, contains a loch that itself contains an island, a situation that occurs nowhere else in Great Britain.

Geographic entities mentioned:
surface_form: maree
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.689722222222
lon: -5.4575
surface_form: loch maree
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.689722222222
lon: -5.4575
The largest island, Eilean Sùbhainn, contains a loch that itself contains an island, a situation that occurs nowhere else in Great Britain. Isle Maree holds the remains of a Pre-Reformation chapel and Christian pilgrimage shrine believed to be the 8th century hermitage of Saint Máel Ruba (d.

Geographic entities mentioned:
surface_form: maree
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.689722222222
lon: -5.4575