Sarmila/GeoWiki-Features huggingface dataset:
Controlling it was vital to the war effort against the Judaeans, which led Antiochus to rebuild the city's defenses in 228 SE (85/84 BC). Historian Aryeh Kasher suggested that Antiochus XII dug what the first-century historian Josephus called the &quot;trench of Antiochus&quot; (or valley of Antiochus) to protect Damascus from the Nabataeans; the trench was probably located in the Hula Valley.

Geographic entities mentioned:
surface_form: Hula Valley
instance_of: Valley
countries: Israel
coordinates: lat: 33.103333333333
lon: 35.609166666667
Zakura, also known as Zukura and Zukur, is a notified area and town in the Srinagar district of the union territory of Jammu and Kashmir, India. The town is the integral part of Hazratbal constituency. The area is located about 12 km from commercial center of the Kashmir Valley. The area provides at least two major road links which connects municipal committee of Ganderbal with Srinagar.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
Janq'u Willk'i (Luribay). Janq'u Willk'i (Aymara &quot;janq'u&quot; white, &quot;willk'i&quot; gap,&quot;white gap&quot;, also spelled &quot;Jankho Willkhi&quot;) is a mountain in the Bolivian Andes. It is located in the La Paz Department, Loayza Province, Luribay Municipality. Janq'u Willk'i lies west of Kuntur Jiwaña.

Geographic entities mentioned:
surface_form: janq'u willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.13944444
lon: -68.39611111
surface_form: janq'u willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.7722
lon: -67.5314
surface_form: willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.39861111
lon: -69.02222222
surface_form: janq'u willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.01111111
lon: -67.57416667
Janq'u Willk'i (Luribay). Janq'u Willk'i (Aymara &quot;janq'u&quot; white, &quot;willk'i&quot; gap,&quot;white gap&quot;, also spelled &quot;Jankho Willkhi&quot;) is a mountain in the Bolivian Andes. It is located in the La Paz Department, Loayza Province, Luribay Municipality. Janq'u Willk'i lies west of Kuntur Jiwaña.

Geographic entities mentioned:
surface_form: janq'u willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.13944444
lon: -68.39611111
surface_form: janq'u willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.7722
lon: -67.5314
surface_form: willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.39861111
lon: -69.02222222
surface_form: willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.39861111
lon: -69.02222222
surface_form: janq'u willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.01111111
lon: -67.57416667
Touzaline. Touzaline is a village in the Boumerdès Province in Kabylie, Algeria. Location. The village is surrounded by Isser River and the town of Beni Amrane in the &quot;Khachna&quot; mountain range.

Geographic entities mentioned:
surface_form: Isser River
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.8391
lon: 3.6679
The Flores Daniel Gang was hunted down and 52 gang members were arrested and 18 gang members were hanged for the murder of the four Lawmen. Juan Flores and the gang had taken refuge on the Flores Peak after killing James R. Barton and three of his Posse. Flores made a daring escape from encirclement by a Los Angeles posse led by General Andrés Pico.

Geographic entities mentioned:
surface_form: Flores Peak
instance_of: Mountain
countries: United States
coordinates: lat: 33.71333333
lon: -117.62138889
Hasanabad, Amol. Hasanabad (, also Romanized as Ḩasanābād) is a village in Dabuy-ye Jonubi Rural District, Dabudasht District, Amol County, Mazandaran Province, Iran. It is located on the Caspian Sea. At the 2006 census, its population was 133, in 37 families.

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
Yellow Mountain (Montana). Yellow Mountain () is located in the Lewis Range, Glacier National Park in the U.S. state of Montana. Yellow Mountain forms a high ridge and connects Sherburne Peak in the east to Seward Mountain to the west.

Geographic entities mentioned:
surface_form: Sherburne Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.8836
lon: -113.562
surface_form: yellow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.8817
lon: -113.637
surface_form: seward mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.1597
lon: -74.1997
surface_form: seward mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.8708
lon: -113.681
Yellow Mountain (Montana). Yellow Mountain () is located in the Lewis Range, Glacier National Park in the U.S. state of Montana. Yellow Mountain forms a high ridge and connects Sherburne Peak in the east to Seward Mountain to the west.

Geographic entities mentioned:
surface_form: yellow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.8817
lon: -113.637
It is believed to be the birthplace of three Jain Tirthankaras. There are many ancient Hindu temples including Pandeshwar Temple and Karna Temple, as well as Jain temples such as Shri Digamber, Jain Mandir, Jambudweep, Kailash Parvat, and Shwetambar Jain Temple. Digamber Jain Bada Mandir Hastinapur. Digamber Jain Bada Mandir Hastinapur is one of the oldest Jain temples in Hastinapur.

Geographic entities mentioned:
surface_form: Kailash Parvat
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 31.066944444444
lon: 81.312777777778
Pierbattista Pizzaballa. Pierbattista Pizzaballa (;; born 21 April 1965) is an Italian member of the Franciscan Order and a Roman Catholic cardinal who has been serving as the Latin Patriarch of Jerusalem since 6 November 2020. After being received into the Franciscan Order in 1984, he spent his novitiate at the Franciscan Shrine of La Verna in Arezzo, Italy.

Geographic entities mentioned:
surface_form: Franciscan Shrine of La Verna
instance_of: Mountain
countries: Italy
coordinates: lat: 43.707
lon: 11.931
The demolition of the wall to facilitate entry to the port created more space and helped the mobility of the ships. The opening of the Mehmet Sabri Pasha road (nowadays Venizelou Street) in 1867 created a small square as the road widened towards the wharfs. It was initially called (Wharf Square) and later (Olympus Square) on account of the views of Mount Olympus across the sea.

Geographic entities mentioned:
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
Life. Biographical details on Ioane-Zosime are scarce beyond the fact that he was one of the numerous expatriate Georgian clerics active at the monastery of Mar Saba in Palestine. In the early 970s he moved to Mount Sinai, probably fleeing the armies of the Fatimid Caliphate. His voluminous body of work dates from between 949 and 987.

Geographic entities mentioned:
surface_form: Mount Sinai
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.5384
lon: 33.9752
Rahul Pandita. Rahul Pandita () is an Indian author and journalist. Early life. Rahul Pandita is a Kashmiri Pandit born in the Kashmir Valley. In 1990, at the age of 14, he had to leave the Valley along with his family as part of the Exodus of Kashmiri Pandits. Career.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
The aqueduct was completed in 1913. The Aqueduct brought plentiful water to Los Angeles, which supplied its explosive population growth. It also diverted the Owens River and its tributaries, taking water away from the Owens Valley, eventually disabling the farms and communities there. Controversy.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
Controversy. During the time that Eaton was surveying the Owens Valley land for his personal water project, the federal government was also in the process of reclaiming land in that area for a large irrigation system in response to the newly signed Newlands Reclamation Act. Many local farmers willingly gave up their land to make this project possible.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
William Mulholland refused to authorize the purchase and explored other areas to build the reservoir. Eventually he settled on an area which he had considered for a potential dam site during the process of designing and building the Los Angeles Aqueduct, a section of San Francisquito Canyon located north of the present day Santa Clarita Valley, and built the St. Francis Dam.

Geographic entities mentioned:
surface_form: Santa Clarita Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.398
lon: -118.522
six books of traditions of Muhammad Ismail Bukhari, Muslim Nishapuri, Ibn Majah, Abu Daud, Abu Isa Tirmizi and Abu Abdul Rehman Nisai. Life in Aurangabad. He returned from Hijaz to India and lived in the city of Aurangabad, Deccan till his death. Nasir Jang and other nobles of the Nizam's state were his devotees but he avoided worldly favours and preferred a life of piety and poverty.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Extinguisher Tower. Extinguisher Tower is a mountain on the SE side of Robson Glacier, SE of Berg Lake at the northern end of Mount Robson Provincial Park in British Columbia, Canada. It is part of the Rainbow Range which is a sub-range of the Canadian Rockies.

Geographic entities mentioned:
surface_form: Berg Lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.145555555556
lon: -119.15777777778
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount robson
instance_of: Mountain
countries: Canada
coordinates: lat: 53.11055555555556
lon: -119.15666666666667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: extinguisher tower
instance_of: Mountain
countries: Canada
coordinates: lat: 53.11944444444445
lon: -119.09555555555555
Extinguisher Tower. Extinguisher Tower is a mountain on the SE side of Robson Glacier, SE of Berg Lake at the northern end of Mount Robson Provincial Park in British Columbia, Canada. It is part of the Rainbow Range which is a sub-range of the Canadian Rockies.

Geographic entities mentioned:
surface_form: extinguisher tower
instance_of: Mountain
countries: Canada
coordinates: lat: 53.11944444444445
lon: -119.09555555555555
Mount Underwood. Mount Underwood () is an elongated mountain 2 nautical miles (3.7 km) east of Mount Flett in the central Nye Mountains. It was plotted from air photos taken from ANARE (Australian National Antarctic Research Expeditions) aircraft in 1956 and 1957 and was named by the ANC for R. Underwood, a geophysicist at Wilkes Station in 1959.

Geographic entities mentioned:
surface_form: Mount Flett
instance_of: Mountain
coordinates: lat: -68.15
lon: 49.2
surface_form: flett
instance_of: Mountain
coordinates: lat: -68.15
lon: 49.2
surface_form: mount underwood
instance_of: Mountain
coordinates: lat: -68.1333
lon: 49.35
surface_form: underwood
instance_of: Mountain
coordinates: lat: -68.1333
lon: 49.35
Mount Underwood. Mount Underwood () is an elongated mountain 2 nautical miles (3.7 km) east of Mount Flett in the central Nye Mountains. It was plotted from air photos taken from ANARE (Australian National Antarctic Research Expeditions) aircraft in 1956 and 1957 and was named by the ANC for R. Underwood, a geophysicist at Wilkes Station in 1959.

Geographic entities mentioned:
surface_form: mount underwood
instance_of: Mountain
coordinates: lat: -68.1333
lon: 49.35
surface_form: underwood
instance_of: Mountain
coordinates: lat: -68.1333
lon: 49.35
Mount Underwood. Mount Underwood () is an elongated mountain 2 nautical miles (3.7 km) east of Mount Flett in the central Nye Mountains. It was plotted from air photos taken from ANARE (Australian National Antarctic Research Expeditions) aircraft in 1956 and 1957 and was named by the ANC for R. Underwood, a geophysicist at Wilkes Station in 1959.

Geographic entities mentioned:
surface_form: underwood
instance_of: Mountain
coordinates: lat: -68.1333
lon: 49.35
He helped liberate Rome, Siena, and Tuscany. During Operation Dragoon on 16 August 1944, he continued to act as an observer from an airplane. Between 20 and 25 August, he fulfilled many war missions between Hyères and Toulon. During the Battle of Alsace, he took part in the destruction of several tanks and spotted two batteries.

Geographic entities mentioned:
surface_form: Hyères
instance_of: Mountain
countries: France
coordinates: lat: 43.118888888889
lon: 6.1286111111111
This zone can be viewed up close by hiking or climbing into the high elevations of the Sierra. Eastern biotic zones. In the Owens Valley, the Foothill Woodland Zone is replaced by a
Pinyon-Juniper Woodland Zone, characterized by
single-leaf pinyon pines and sierra junipers. The underbrush contains big sagebrush (&quot;Artemisia tridentata&quot;) and blackbrush (&quot;Coleogyne ramosissima&quot;).

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
It is located in the Cochabamba Department, Ayopaya Province, Morochata Municipality. It lies east of the village of Paranani. The Chullpa Q'asa Mayu (&quot;chullpa&quot; pass river&quot;, &quot;Chullpa Khasa Mayu&quot;) which downstream is named Pukarani originates at the mountain. It flows to the northwest as an affluent of the Santa Rosa River.

Geographic entities mentioned:
surface_form: chullpa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.1556
lon: -66.6372
surface_form: pukarani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.03
lon: -67.51861111
surface_form: pukarani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.05055556
lon: -66.64527778
surface_form: pukarani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.77666667
lon: -66.02138889
surface_form: pukarani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.1414
lon: -68.4369
Liqiliqini (Cochabamba). Liqiliqini (Aymara &quot;liqiliqi, liqi liqi&quot; Southern lapwing or Andean lapwing, &quot;-ni&quot; a suffix to indicate ownership, &quot;the one with the Southern lapwing (or Andean lapwing)&quot;, also spelled &quot;Lekhe Lekheni&quot;) is a mountain in the Bolivian Andes which reaches a height of approximately.

Geographic entities mentioned:
surface_form: liqiliqini
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.16
lon: -66.49694444
surface_form: liqiliqini
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.87805556
lon: -67.5975
Midgard Peak. Midgard Peak is a mountain summit located in the Valhalla Ranges of the Selkirk Mountains in British Columbia, Canada. Midgard Peak is the third-highest point in the Valhalla Ranges, with the highest being Gladsheim Peak, to the east-northeast. The nearest higher neighbor is Asgard Peak, to the northeast.

Geographic entities mentioned:
surface_form: Gladsheim Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.78316
lon: -117.63555
surface_form: midgard peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.76656
lon: -117.66895
Midgard Peak is the third-highest point in the Valhalla Ranges, with the highest being Gladsheim Peak, to the east-northeast. The nearest higher neighbor is Asgard Peak, to the northeast. It is situated on the southern border of Valhalla Provincial Park, northwest of Gimli Peak, and west of Slocan and Slocan Lake. Etymology.

Geographic entities mentioned:
surface_form: Asgard Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.784
lon: -117.6573
Midgard Peak is the third-highest point in the Valhalla Ranges, with the highest being Gladsheim Peak, to the east-northeast. The nearest higher neighbor is Asgard Peak, to the northeast. It is situated on the southern border of Valhalla Provincial Park, northwest of Gimli Peak, and west of Slocan and Slocan Lake. Etymology.

Geographic entities mentioned:
surface_form: Gimli Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.76656
lon: -117.64805
surface_form: Slocan Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.9472
lon: -117.378
surface_form: gimli
instance_of: Mountain
countries: Canada
coordinates: lat: 49.76656
lon: -117.61055
Midgard Peak. Midgard Peak is a mountain summit located in the Valhalla Ranges of the Selkirk Mountains in British Columbia, Canada. Midgard Peak is the third-highest point in the Valhalla Ranges, with the highest being Gladsheim Peak, to the east-northeast. The nearest higher neighbor is Asgard Peak, to the northeast.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: midgard peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.76656
lon: -117.66895
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Midgard Peak. Midgard Peak is a mountain summit located in the Valhalla Ranges of the Selkirk Mountains in British Columbia, Canada. Midgard Peak is the third-highest point in the Valhalla Ranges, with the highest being Gladsheim Peak, to the east-northeast. The nearest higher neighbor is Asgard Peak, to the northeast.

Geographic entities mentioned:
surface_form: midgard peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.76656
lon: -117.66895
According to Norse mythology, Midgard is the home of earth dwellers. Climate. Based on the Köppen climate classification, Midgard Peak has a subarctic climate with cold, snowy winters, and mild summers. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into tributaries of the Slocan River.

Geographic entities mentioned:
surface_form: midgard peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.76656
lon: -117.66895
It is situated on the southern border of Valhalla Provincial Park, northwest of Gimli Peak, and west of Slocan and Slocan Lake. Etymology. The name &quot;Valhalla Mountains&quot; first appeared in George Mercer Dawson's Geological Survey of Canada map published in 1890. Dawson applied names derived from Scandinavian mythology to several of the mountain ranges and peaks in Southern Kootenay.

Geographic entities mentioned:
surface_form: kootenay
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Dawson applied names derived from Scandinavian mythology to several of the mountain ranges and peaks in Southern Kootenay. In keeping with the Valhalla theme, this peak's name was submitted February 1970 by Robert Dean of the Kootenay Mountaineering Club for consideration, and the toponym was officially adopted March 3, 1971, by the Geographical Names Board of Canada.

Geographic entities mentioned:
surface_form: kootenay
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
According to Norse mythology, Midgard is the home of earth dwellers. Climate. Based on the Köppen climate classification, Midgard Peak has a subarctic climate with cold, snowy winters, and mild summers. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into tributaries of the Slocan River.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Lake Carabundup. Lake Carabundup is an ephemeral salt lake located in the Great Southern region of Western Australia, approximately south west of Cranbrook and north east of Rocky Gully. It is located in a watershed between the Kent River and Frankland River catchments. The lake has a length of approximately and a width of approximately; it has neither dried up nor overflowed in the past 20 years.

Geographic entities mentioned:
surface_form: lake carabundup
instance_of: Lake
countries: Australia
coordinates: lat: -34.465833333333
lon: 117.29527777778
Location. James Ross Island is separated from Trinity Peninsula, at the tip of the Antarctic Peninsula to the northwest, by the Prince Gustav Channel. Vega Island is to the north of the island, separated from James Ross Island by the Herbert Sound. Erebus and Terror Gulf is to the northeast. Seymour Island and Snow Hill Island are to the southeast. It is in the James Ross Island group.

Geographic entities mentioned:
surface_form: Herbert Sound
instance_of: Body of water
coordinates: lat: -63.9167
lon: -57.6667
The genus name refers to the site of El Morro on James Ross Island, where the remains of the species were found. The specific name refers to Antarctica. Flett Buttress. A rock crag rising to high northwest of Mount Haddington. It provides the highest exposure of volcanic rock on the island. Named by the UK Antarctic Place-Names Committee (UK-APC) in 1987 after William R.

Geographic entities mentioned:
surface_form: Mount Haddington
instance_of: Mountain
coordinates: lat: -64.216666666667
lon: -57.633333333333
Named by UK-APC for John A. Coley of FIDS, meteorological assistant at Hope Bay in 1952 and 1953. Cape Gage. A rocky promontory forming the east extremity of James Ross Island and the west side of the north entrance to Admiralty Sound. Discovered by a British expedition 1839–43, under James Clark Ross, who named it for V. Admiral William Hall Gage, a Lord Commissioner of the Admiralty.

Geographic entities mentioned:
surface_form: Admiralty Sound
instance_of: Body of water
coordinates: lat: -64.3333
lon: -57.1667
First seen, roughly surveyed, and given the descriptive name &quot;The Watch Tower&quot; by Otto Nordenskjold of the SwedAE in March 1902. Howarth Glacier. A small glacier flowing south-southeast to Admiralty Sound along the west side of The Watchtower. Named by UK-APC in 1995 after Michael Kingsley Howarth (b.

Geographic entities mentioned:
surface_form: Admiralty Sound
instance_of: Body of water
coordinates: lat: -64.3333
lon: -57.1667
Missouri Route 106. Route 106 is a highway in the southern part of the US State of Missouri. Its eastern terminus is at Route 21 at Ellington; its western terminus is at Route 17 in Summersville. Route 106 runs through the eastern, mountainous Ozarks and through two sections of the Ozark National Scenic Riverways. Related route. Spur Route 106 connects the main highway with Deer Run State Forest.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
Of the agricultural land, 11.1% is used for growing crops and 27.2% is pastures, while 4.1% is used for orchards or vine crops. All the water in the municipality is flowing water. The municipality is located in the Thierstein district, on the eastern slope of the valley that runs to the Passwang Pass. It consists of the village of Büsserach and Neu-Thierstein Castle. Coat of arms.

Geographic entities mentioned:
surface_form: Passwang Pass
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.3583
lon: 7.65611
Eve Cone. Eve Cone, also known as Eve's Cone, is a cinder cone in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of and is one of several volcanic cones in the Desolation Lava Field at the northern end of the Big Raven Plateau.

Geographic entities mentioned:
surface_form: Big Raven Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
It branches out into much narrower channels, the largest extending to Buckley Lake. Eve Cone is part of the Mount Edziza volcanic complex, which consists of diverse landforms such as shield volcanoes, stratovolcanoes, lava domes and cinder cones. The cone contains a circular summit crater deep but most of the lava from the volcano appears to have issued from vents around the base of the wide cone.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
The cone contains a circular summit crater deep but most of the lava from the volcano appears to have issued from vents around the base of the wide cone. Eve Cone is surrounded by a number of other volcanic features, including Tsekone Ridge, Pillow Ridge, Sidas Cone and the Triplex Cones.

Geographic entities mentioned:
surface_form: Tsekone Ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 57.77
lon: -130.69
surface_form: Pillow Ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7594
lon: -130.652
surface_form: Sidas Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.8589
lon: -130.628
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
Name and etymology. Jack Souther, a geologist of the Geological Survey of Canada who studied the area in detail from 1965 to 1992, named the cone after Eve Brown Edzerza. Edzerza was a local indigenous woman who traversed Mount Edziza by dog sled with her husband, Johnny Edzerza, and a man named Hank Williams in or before 1974.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Johnny and Hank were killed in an avalanche on the mountain during a vicious snowstorm that had blown in from the north, but Eve survived, directing a rescue team to the site of the accident. Johnny was buried on Mount Edziza; both &quot;Edzerza&quot; and &quot;Edziza&quot; may be etymologically linked. Williams Cone on the northeastern side of the mountain was named in honour of Hank.

Geographic entities mentioned:
surface_form: Williams Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
Geography. Eve Cone is located in Cassiar Land District of northwestern British Columbia, Canada, about southeast of Buckley Lake at the northern end of the Big Raven Plateau. It has an elevation of and is one of several volcanic cones in the Desolation Lava Field, which is one of the largest areas of Holocene lava flows in the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: Big Raven Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
Geography. Eve Cone is located in Cassiar Land District of northwestern British Columbia, Canada, about southeast of Buckley Lake at the northern end of the Big Raven Plateau. It has an elevation of and is one of several volcanic cones in the Desolation Lava Field, which is one of the largest areas of Holocene lava flows in the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
Apart from the main edifice of Mount Edziza, which reaches an elevation of, Eve Cone is surrounded by a number of other volcanic features. About southwest of Eve Cone is Tsekone Ridge on the northwestern flank of Mount Edziza. Pillow Ridge, about south of Eve Cone, extends northwest from the northern flank of Mount Edziza.

Geographic entities mentioned:
surface_form: Tsekone Ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 57.77
lon: -130.69
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
About southwest of Eve Cone is Tsekone Ridge on the northwestern flank of Mount Edziza. Pillow Ridge, about south of Eve Cone, extends northwest from the northern flank of Mount Edziza. About southeast of Eve Cone are the Triplex Cones, a southeast-trending line of three deeply eroded volcanic cones. Sidas Cone about northwest of Eve Cone is a composite of two overlapping cones.

Geographic entities mentioned:
surface_form: Pillow Ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7594
lon: -130.652
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
About southeast of Eve Cone are the Triplex Cones, a southeast-trending line of three deeply eroded volcanic cones. Sidas Cone about northwest of Eve Cone is a composite of two overlapping cones. Pillow Ridge and Tsekone Ridge are older volcanic features of Pleistocene age whereas Sidas Cone and the Triplex Cones are part of the younger Desolation Lava Field.

Geographic entities mentioned:
surface_form: Sidas Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.8589
lon: -130.628
It includes not only the Mount Edziza area but also the Spectrum Range to the south, which are separated by Raspberry Pass. Mount Edziza Provincial Park is in the Tahltan Highland, a southeast-trending upland area extending along the western side of the Stikine Plateau. Background.

Geographic entities mentioned:
surface_form: Stikine Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
Background. As a part of the Mount Edziza volcanic complex, Eve Cone lies within a broad area of volcanoes and lava flows called the Northern Cordilleran Volcanic Province, which extends from northwestern British Columbia northwards through Yukon into easternmost Alaska.

Geographic entities mentioned:
surface_form: Northern Cordilleran Volcanic Province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Extending from these roads are horse trails that provide access to the Mount Edziza volcanic complex. From Telegraph Creek, the Buckley Lake Trail extends about southeast along Mess Creek and Three Mile Lake.

Geographic entities mentioned:
surface_form: Mess Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Eve Cone. Eve Cone, also known as Eve's Cone, is a cinder cone in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of and is one of several volcanic cones in the Desolation Lava Field at the northern end of the Big Raven Plateau.

Geographic entities mentioned:
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
Eve Cone. Eve Cone, also known as Eve's Cone, is a cinder cone in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of and is one of several volcanic cones in the Desolation Lava Field at the northern end of the Big Raven Plateau.

Geographic entities mentioned:
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Situated southeast of the community of Telegraph Creek, it lies in Mount Edziza Provincial Park, one of the largest provincial parks in British Columbia. A roughly lava field issued from Eve Cone during the Holocene and travelled down the northern side of the Big Raven Plateau. It branches out into much narrower channels, the largest extending to Buckley Lake.

Geographic entities mentioned:
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
Eve Cone is surrounded by a number of other volcanic features, including Tsekone Ridge, Pillow Ridge, Sidas Cone and the Triplex Cones. Access is via horse trails from the communities of Telegraph Creek and Iskut, although landing on Buckley Lake with float-equipped aircraft is also promoted to reach Eve Cone. Name and etymology.

Geographic entities mentioned:
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
In his 1992 report &quot;The Late Cenozoic Mount Edziza Volcanic Complex, British Columbia&quot;, Jack Souther gave Eve Cone the numeronym &quot;DLF-9&quot;; &quot;DLF&quot; is an acronym for the Desolation Lava Field whereas &quot;9&quot; refers to Eve Cone being the ninth youngest eruptive centre in the Desolation Lava Field.

Geographic entities mentioned:
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
BC Parks refers to the cone as both &quot;Eve Cone&quot; and &quot;Eve's Cone&quot;. Geography. Eve Cone is located in Cassiar Land District of northwestern British Columbia, Canada, about southeast of Buckley Lake at the northern end of the Big Raven Plateau.

Geographic entities mentioned:
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
Lichen and pioneer vegetation sparsely grows on the base of the wide cone. The Smithsonian Institution's Global Volcanism Program lists Eve Cone as one of many satellitic cones of Mount Edziza due to its location on the northern flank of this stratovolcano. Apart from the main edifice of Mount Edziza, which reaches an elevation of, Eve Cone is surrounded by a number of other volcanic features.

Geographic entities mentioned:
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
About southwest of Eve Cone is Tsekone Ridge on the northwestern flank of Mount Edziza. Pillow Ridge, about south of Eve Cone, extends northwest from the northern flank of Mount Edziza. About southeast of Eve Cone are the Triplex Cones, a southeast-trending line of three deeply eroded volcanic cones. Sidas Cone about northwest of Eve Cone is a composite of two overlapping cones.

Geographic entities mentioned:
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
Such features are typically considered to erupt only once and to be short-lived; they can remain active from days to years but are fed by a relatively small amount of magma. Eve Cone consists of hawaiite of the Big Raven Formation and is one of the two youngest eruptive centres in the Desolation Lava Field, the other being Williams Cone about to the southeast.

Geographic entities mentioned:
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
Both cones are of Holocene age but Eve Cone was most likely formed by a towering, vertical lava fountain due to its symmetrical structure. Loosely aggregated volcanic ejecta such as bombs, cinders and ash cover the outer surface of Eve Cone.

Geographic entities mentioned:
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
In contrast to Williams Cone, whose surroundings are at least still partially covered with fine ash from its eruption, ash from the Eve Cone eruption has completely eroded away from the surrounding landscape; this suggests Eve Cone is older than Williams Cone. Lava field. Nearly all of the lava erupted from Eve Cone appears to have originated from vents around the base of the volcanic edifice.

Geographic entities mentioned:
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
The Buckley Lake to Mowdade Lake Route traverses south from Buckley Lake along Buckley Creek and gradually climbs onto the northern end of the Big Raven Plateau where Eve Cone and Sidas Cone are visible along the route. BC Parks recommends visitors ascend Eve Cone using the main trail on its southeastern flank to prevent foot scarring on its delicate surface.

Geographic entities mentioned:
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
A roughly lava field issued from Eve Cone during the Holocene and travelled down the northern side of the Big Raven Plateau. It branches out into much narrower channels, the largest extending to Buckley Lake. Eve Cone is part of the Mount Edziza volcanic complex, which consists of diverse landforms such as shield volcanoes, stratovolcanoes, lava domes and cinder cones.

Geographic entities mentioned:
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
It has a maximum width of about. The lava field overlies older lava flows from the Triplex Cones and abuts with older lava flows in the northeast from Sidas Cone. The lava flows comprising this field branch out into much narrower lava channels to the north and northwest, the largest of which is approximately long and reaches the northeastern end of Buckley Lake.

Geographic entities mentioned:
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
From Telegraph Creek, the Buckley Lake Trail extends about southeast along Mess Creek and Three Mile Lake. It then traverses about northeast along Dagaichess Creek and Stinking Lake to the northeastern end of Buckley Lake, where it meets with the Klastline River Trail and the Buckley Lake to Mowdade Lake Route.

Geographic entities mentioned:
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
After entering Mount Edziza Provincial Park, the Klastline River Trail traverses northwest along the Klastline River for about and then crosses the river north of the Big Raven Plateau. From there, the Klastline River Trail traverses west for about to the northeastern end of Buckley Lake, where it meets with the Buckley Lake Trail and Buckley Lake to Mowdade Lake Route.

Geographic entities mentioned:
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
It has an elevation of and is one of several volcanic cones in the Desolation Lava Field at the northern end of the Big Raven Plateau. Situated southeast of the community of Telegraph Creek, it lies in Mount Edziza Provincial Park, one of the largest provincial parks in British Columbia.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Eve Cone lies in Mount Edziza Provincial Park southeast of the community of Telegraph Creek. With an area of, Mount Edziza Provincial Park is one of the largest provincial parks in British Columbia and was established in 1972 to showcase the volcanic landscape. It includes not only the Mount Edziza area but also the Spectrum Range to the south, which are separated by Raspberry Pass.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Cefn Manmoel. Cefn Manmoel is the name given to the broad ridge of high ground between the Sirhowy Valley and Ebbw Vale in the Valleys region of South Wales. It straddles the boundary between the unitary areas of Caerphilly and Blaenau Gwent. The NNW-SSE aligned ridge reaches a height of above sea-level at OS grid ref SO 166072.

Geographic entities mentioned:
surface_form: Sirhowy Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.779
lon: -3.233
Valdera. Valdera is the name of an area in the Province of Pisa in Tuscany. The Valdera area usually also includes the following municipalities for social and economical reasons. They are all located near the lower part of the Arno river valley and near the Lucca plain.

Geographic entities mentioned:
surface_form: Arno river valley
instance_of: Valley
countries: Italy
coordinates: lat: 43.566666666667
lon: 11.533333333333
WSLQ. WSLQ (99.1 FM &quot;Q99&quot;) is a commercial radio station licensed to Roanoke, Virginia, serving the New River Valley and Southwest Virginia. The station airs an adult contemporary radio format, switching to Christmas music for much of November and December. It is owned and operated by Mel Wheeler, Inc., with studios and offices on Electric Road in Roanoke.

Geographic entities mentioned:
surface_form: New River Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.228888888889
lon: -80.382444444444
Rich Mountain (Moses Cone Park, North Carolina). Rich Mountain is roughly south-southwest of Boone, in Moses H. Cone Memorial Park. Its elevation reaches. Because it's within the Blue Ridge Parkway, it is protected from development.

Geographic entities mentioned:
surface_form: rich mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.2356
lon: -81.7058
surface_form: rich mountain (moses cone park, north carolina)
instance_of: Mountain
countries: United States
coordinates: lat: 36.170833333333
lon: -81.709166666667
surface_form: rich mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.7436
lon: -84.3431
surface_form: rich mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.6743
lon: -94.3292
Rich Mountain (Moses Cone Park, North Carolina). Rich Mountain is roughly south-southwest of Boone, in Moses H. Cone Memorial Park. Its elevation reaches. Because it's within the Blue Ridge Parkway, it is protected from development.

Geographic entities mentioned:
surface_form: rich mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.2356
lon: -81.7058
surface_form: rich mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.170833333333
lon: -81.709166666667
surface_form: rich mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.7436
lon: -84.3431
surface_form: rich mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.6743
lon: -94.3292
Location. The lime tree is situated in the centre of the village of Kaditz, a district of Dresden, on the right bank of the Elbe, where it stands on a plateau with no danger of flooding, about north-west of the historic centre of Dresden.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Bornean leafbird. The Bornean leafbird (&quot;Chloropsis kinabaluensis&quot;), also known as the Kinabalu leafbird'&quot;, is a species of bird in the family Chloropseidae. It is found in humid forest in Borneo, to which it is endemic (elevated areas, including the Meratus Mountains). It has traditionally been considered a subspecies of the blue-winged leafbird (&quot;C.

Geographic entities mentioned:
surface_form: Meratus Mountains
instance_of: Mountain
countries: Indonesia
coordinates: lat: -2.75
lon: 115.66666666667
It was designed by the architect Andreas Thejll with collaboration with Asger Ostenfeld. Ermelunden Waterworks, a second waterworks, opened in 1907. Sjælsø Waterworks was inaugurated in 1936. Decommissioning. Gentofte Municipality's population peaked in 1952 at 89,142 and Tuborg Breweries increased its production increased dramatically, leading to new capacity problems for its water supply system.

Geographic entities mentioned:
surface_form: Sjælsø Waterworks
instance_of: Lake
countries: Denmark
coordinates: lat: 55.8653
lon: 12.4439
Suavjärvi. Suavjärvi (in Karelian, Russian:) is a lake in the Republic of Karelia, Russia about 50 km north of the town of Medvezhyegorsk. The lake is approximately wide. Mashchak and Naumov argue that Suavjärvi lies at the center of a deeply eroded and highly metamorphosed impact structure, the Suavjärvi structure, which has a diameter of.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: suavjärvi
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 63.1245
lon: 33.3732
Suavjärvi. Suavjärvi (in Karelian, Russian:) is a lake in the Republic of Karelia, Russia about 50 km north of the town of Medvezhyegorsk. The lake is approximately wide. Mashchak and Naumov argue that Suavjärvi lies at the center of a deeply eroded and highly metamorphosed impact structure, the Suavjärvi structure, which has a diameter of.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
They also found an absence of evidence of shock metamorphism in samples from within the hypothesized impact structure and that the rocks associated with it do not substantially differ from the normal regional geology. This lake is more likely a glacial lake. The Suavjärvi structure's classification as an impact structure remains controversial and unsettled.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Younger regional metamorphism has significantly altered the rocks composing the structure and may have either obliterated or altered any shock metamorphic effects. The inferred age of the Suavjarvi structure lies within an age interval between 2.7 and 2.2 billion years.

Geographic entities mentioned:
surface_form: suavjarvi
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 63.1245
lon: 33.3732
Its older age limit of 2.7 billion years is set by the regional age of Late Lopian granitoids that occur as fragments within the megabreccias. The overlap of impact polymictic breccias by basal conglomerates of the Jatulian Group and presence of weathered breccia within its conglomerates indicates that the Suavjarvi structure predates it.

Geographic entities mentioned:
surface_form: suavjarvi
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 63.1245
lon: 33.3732