Sarmila/GeoWiki-Features huggingface dataset:
Pogubie Wielkie. Pogubie Wielki is a lake located in the Masurian Plains, on the terrain of the Puszcza Piska, to the South-Western direction of Pisz, in Poland,
near the village of Pogobie Średnie (Gmina Pisz, Pisz County, Warmian-Masurian Voivodeship). The lake is polymictic with a round shape and a depth which does not have substantial difference. The lake's area is, with a maximum depth of.

Geographic entities mentioned:
surface_form: pogubie wielkie
instance_of: Lake
countries: Poland
coordinates: lat: 53.5825
lon: 21.746666666667
Chaîne de la Selle. Chaîne de la Selle () is a mountain range in Haiti, on the island of Hispaniola. The range's Pic la Selle is the highest point of Haiti, at a height of 2,680 meters (8,793 feet) above sea level.

Geographic entities mentioned:
surface_form: Pic la Selle
instance_of: Mountain
countries: Haiti
coordinates: lat: 18.366666666667
lon: -71.983333333333
Synanthedon loranthi. &quot;Synanthedon loranthi&quot; is a moth of the family Sesiidae. It is found in most of Europe (except Ireland, Great Britain, Fennoscandia, the Netherlands, Portugal, the Baltic region and Ukraine) and Asia Minor. The wingspan is 20–22 mm.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Around 40 percent of the populations (based on the overestimate of 170,000) occurs in protected areas, mainly in Okavango Delta and Linyanti and Chobe swamps (Botswana); Dja Faunal Reserve and Lobéké National Park (Cameroon); Bangassou (Central African Republic); Odzala National Park, Lake Télé Community Reserve, Likouala and Salonga National Park (The Democratic Republic of Congo); Monte Alén National Park (Equatorial Guinea); Saiwa Swamp National Park (Kenya); Akagera National Park (Rwanda); Moyowosi and Kigosi Game Reserves (Tanzania); Bangweulu and Busanga Swamps (Zambia).

Geographic entities mentioned:
surface_form: Okavango Delta
instance_of: Body of water
Watercourse
countries: Botswana
coordinates: lat: -19.4
lon: 22.9
Taegisan. Taegisan () is a mountain in the counties of Hoengseong and Pyeongchang, Gangwon Province, South Korea. It has an elevation of.

Geographic entities mentioned:
surface_form: taegisan
instance_of: Mountain
countries: South Korea
The River's flow. The Mara River basin covers a surface of, of which approximately 65% is located in Kenya and 35% in Tanzania. From its sources in the Kenyan highlands, the river flows for about and originates from the Mau Escarpment and drains into Lake Victoria. The basin can be roughly divided into four land use and/or administrative units. The Mara's regions.

Geographic entities mentioned:
surface_form: Mau Escarpment
instance_of: Mountain
countries: Kenya
coordinates: lat: 0.61
lon: 35.74
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
In this part of the basin human and livestock densities are high and small-scale subsistence agriculture is the main land use. The Mara River basin is one of the ten drainage basins that feed into Lake Victoria, and is therefore functionally and ecologically related to the socio-economic activities in Lake Victoria and along the River Nile. Altitudes and ranges.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Eburru. Eburru is a village in Kenya. Eburru is found in Kenya's countryside, along the Great Rift Valley. It is located approximately 7 hours outside Keyna's capital, Nairobi, near the Ol Doinyo Eburru volcano. Eburru is home to Primary and Secondary Schools. A high school was built in 2017–18 with the help of local missionary, Pastor Steve Njenga, and his family.

Geographic entities mentioned:
surface_form: Ol Doinyo Eburru
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.648866
lon: 36.187248
Occurrence and association. Ferrokentbrooksite was discovered in Mont Saint-Hilaire, Quebec, Canada – a site wealth in rare alkaline minerals. At the site ferrokentbrooksite coexists with aegirine, albite, ancylite-(Ce), calcite, catapleiite, fluorite, fluorapatite, gonnardite, microcline, natrolite, nepheline, rhodochrosite, and serandite. Notes on chemistry.

Geographic entities mentioned:
surface_form: Mont Saint-Hilaire
instance_of: Mountain
countries: Canada
coordinates: lat: 45.552222222222
lon: -73.163888888889
The Ruskin is home to The Ruskin Whitehouse Collection, the world's largest assemblage of works by artist, writer, environmentalist and social thinker John Ruskin (1819–1900), and his circle. The collection is on display in The Ruskin building at Lancaster University, designed for the collection by Sir Richard MacCormac, and Brantwood, Ruskin's house, garden and estate on Coniston Water.

Geographic entities mentioned:
surface_form: Coniston Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.35
lon: -3.0666666666667
A village on the foot of Aragats is named Alagyaz. Geography and geology. Mount Aragats has a topographic prominence of 2,143 meters, more than some higher mountains, such as Dykh-Tau (5,205 m high) in the Russian part of Great Caucasus Range. Situated northwest of the Armenian capital Yerevan, Aragats is a large volcano with numerous fissure vents and adventive cones.

Geographic entities mentioned:
surface_form: Dykh-Tau
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 43.0525
lon: 43.131666666667
surface_form: aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
According to an ancient Armenian legend, Aragats and Mount Ararat were loving sisters who parted after a quarrel and separated permanently. Another legend tells that Gregory the Illuminator, who converted Armenia to Christianity in the early 4th century, &quot;used to pray on the peak of the mountain. At nighttime an icon lamp shone to give light to him, the lamp hanging from heaven using no rope.

Geographic entities mentioned:
surface_form: Mount Ararat
instance_of: Mountain
countries: Turkey
coordinates: lat: 39.70194444444444
lon: 44.29833333333333
A cross is added on an annual basis. Scientific institutions. The Aragats Cosmic Ray Research Station is a cosmic-ray observatory near Lake Kari, at around above sea level. It was founded in 1943 by the brothers Artem Alikhanian and Abram Alikhanov. The Nor-Amberd station, built in 1960, is located at.

Geographic entities mentioned:
surface_form: Lake Kari
instance_of: Lake
countries: Armenia
coordinates: lat: 40.47355
lon: 44.18108888888889
Numerous Armenian poets (e.g., Avetik Isahakyan) have written about Aragats. Marietta Shaginyan compared Aragats to a &quot;half-open bud of a giant pomegranate flower&quot;. In one short poem, Silva Kaputikyan compares Armenia to an &quot;ancient rock-carved fortress&quot;, the towers of which are Mount Aragats and Mount Ararat. In visual art. Numerous artists have painted Aragats.

Geographic entities mentioned:
surface_form: Mount Ararat
instance_of: Mountain
countries: Turkey
coordinates: lat: 39.70194444444444
lon: 44.29833333333333
surface_form: mount aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
surface_form: aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
surface_form: aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
surface_form: aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
Mount Aragats. Mount Aragats (,) is an isolated four-peaked volcano massif in Armenia. Its northern summit, at above sea level, is the highest point of the Lesser Caucasus and Armenia. It is also one of the highest points in the Armenian Highlands.

Geographic entities mentioned:
surface_form: mount aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
surface_form: aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
This term was widely used up until the mid-20th century in European, Tsarist Russian, and early Soviet sources. Another version, &quot;Alagyaz&quot; (), has been used in Armenian. A village on the foot of Aragats is named Alagyaz. Geography and geology.

Geographic entities mentioned:
surface_form: aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
On May 28, 2005—the anniversary of the establishment of the First Republic of Armenia—around 250,000 people participated in a Dance of Unity () around Mount Aragats in a mass display of national unity. The quarter million participants, among them then-President Robert Kocharyan and Defense Minister Serzh Sargsyan, formed a ring around the mountain after a blessing from Catholicos Karekin II.

Geographic entities mentioned:
surface_form: mount aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
surface_form: aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
It is also one of the highest points in the Armenian Highlands. The Aragats massif is surrounded by the Kasagh River on the east, the Akhurian River on the west, Ararat Plain on the south, and Shirak Plain on the north. The circumference of the massif is around, and covers an area of or around of Armenia's total area. of the massif is located above. Etymology and names.

Geographic entities mentioned:
surface_form: aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
The circumference of the massif is around, and covers an area of or around of Armenia's total area. of the massif is located above. Etymology and names. According to Armenian tradition, the name of Aragats originates from the words and, which translates to &quot;Ara's throne&quot;, in reference to the legendary hero Ara the Handsome.

Geographic entities mentioned:
surface_form: aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
surface_form: aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
Aragats was mentioned by the early medieval historian Movses Khorenatsi, who in his &quot;History of Armenia&quot; claims that the mountain is named after, the son of Hayk, the legendary patriarch of the Armenian people. Aramaneak called his possessions &quot;the foot of Aragats&quot; (or). The modern Aragatsotn Province, dominated by the mountain, was formed in 1995.

Geographic entities mentioned:
surface_form: aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
The glaciation has been retreating on account of insufficient snowfall and increasing temperatures. Glacial meltwater dominates the upper part of the rivers descending from Aragats but its importance decreases farther down the valleys. Traces of prehistorical glaciation also exist including thick moraines in the summit area at an altitude of 2,600–3,000 m. Geological.

Geographic entities mentioned:
surface_form: aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
At nighttime an icon lamp shone to give light to him, the lamp hanging from heaven using no rope. Some say that the icon lamp is still there, but only the worthy ones can see it.&quot;
In 1935, on the 15th anniversary of Armenia's Sovietization, around one thousand people climbed the summit of Aragats from five directions.

Geographic entities mentioned:
surface_form: aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
The quarter million participants, among them then-President Robert Kocharyan and Defense Minister Serzh Sargsyan, formed a ring around the mountain after a blessing from Catholicos Karekin II. The organizers hoped the event would be included in the &quot;Guinness World Records&quot;. Prior to the dance, some 110,000 trees were planted on the slopes of Aragats. Nearby settlements.

Geographic entities mentioned:
surface_form: aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
Prior to the dance, some 110,000 trees were planted on the slopes of Aragats. Nearby settlements. The following settlements are located on the slopes or foot of Aragats: Ashtarak, Artik, Aparan, Talin, Oshakan, Byurakan. Historic and cultural sites. Aragats has historically played a significant role in Armenian history and culture.

Geographic entities mentioned:
surface_form: aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
Numerous historical and modern monuments are located on its slopes, some of which are listed below. The 4th-century mausoleum of the Arsacid (Arshakuni) dynasty is located in the village of Aghtsk, on the slopes of Aragats. The early medieval fortress of Amberd and the nearby 11th-century Vahramashen Church are located on the slopes of Aragats, at an altitude of.

Geographic entities mentioned:
surface_form: aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
The 4th-century mausoleum of the Arsacid (Arshakuni) dynasty is located in the village of Aghtsk, on the slopes of Aragats. The early medieval fortress of Amberd and the nearby 11th-century Vahramashen Church are located on the slopes of Aragats, at an altitude of. One source calls Amberd the &quot;biggest and the best preserved fortress&quot; in modern-day Armenia.

Geographic entities mentioned:
surface_form: aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
It was founded in 1943 by the brothers Artem Alikhanian and Abram Alikhanov. The Nor-Amberd station, built in 1960, is located at. The Byurakan Observatory, established in 1946 by Victor Ambartsumian, is located on the southern slopes of Aragats, near the village of Byurakan, at an altitude of. It made Armenia one of the world's centers for the study of astrophysics in the 20th century.

Geographic entities mentioned:
surface_form: aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
The Byurakan Observatory, established in 1946 by Victor Ambartsumian, is located on the southern slopes of Aragats, near the village of Byurakan, at an altitude of. It made Armenia one of the world's centers for the study of astrophysics in the 20th century. The 2.6, a radio telescope built in 1985 by the radiophysicist Paris Herouni in the village of Orgov, on the slopes of Aragats. Gravity hill.

Geographic entities mentioned:
surface_form: aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
The hiking trail is approximately 5 kilometers long, and it typically takes between 2.5 and 3 hours to complete. In culture. Mount Aragats plays a special role in Armenian history and culture. Along with Ararat, it is considered a sacred mountain for the Armenians. Aragats is a male first name in Armenia, used especially in areas surrounding the mountain. Mt.

Geographic entities mentioned:
surface_form: aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
The mountain is depicted on the coat of arms of Gyumri. It is also depicted on the obverse side of the 10,000 Armenian dram banknote (in use since 2003) in the background of Avetik Isahakyan, a poet born in Gyumri. Numerous Armenian poets (e.g., Avetik Isahakyan) have written about Aragats. Marietta Shaginyan compared Aragats to a &quot;half-open bud of a giant pomegranate flower&quot;.

Geographic entities mentioned:
surface_form: aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
Reedy Glacier. The Reedy Glacier () is a major glacier in Antarctica, over long and wide, descending from the polar plateau to the Ross Ice Shelf between the Michigan Plateau and Wisconsin Range in the Transantarctic Mountains. It marks the limits of the Queen Maud Mountains on the west and the Horlick Mountains on the east. Naming.

Geographic entities mentioned:
surface_form: Michigan Plateau
instance_of: Landform
coordinates: lat: -86.1333
lon: -133.5
Reedy, USN, Commander, U.S. Naval Support Force, Antarctica, from November 1962 until April 1965. Topography and ice flow. The Reedy Glacier is the most southern large glacier that drains ice through the Transantarctic mountains from the Antarctic Plateau. It drains about of the polar plateau, with its catchment extending from south of the South Pole.

Geographic entities mentioned:
surface_form: Antarctic Plateau
instance_of: Plateau
coordinates: lat: -90
lon: 0
Course. From the polar plateau the Reedy Glacier flows north past the Spear Nunatak, Strickland Nunatak and Savage Nunatak. It passes the Metavolcanic Mountain to the east and the Watson Escarpment to the west. Past the Gratton Nunatak it is joined from the east by the McCarthy Glacier and the Olentangy Glacier.

Geographic entities mentioned:
surface_form: Metavolcanic Mountain
instance_of: Mountain
coordinates: lat: -86.2167
lon: -126.25
surface_form: Watson Escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
Past the Gratton Nunatak it is joined from the east by the McCarthy Glacier and the Olentangy Glacier. It is joined from the west by the Wotkyns Glacier and the Gardiner Glacier flowing from the Watson Escarpment. It flows northwest past the Wisconsin Range to the east, from which it receives the Norfolk Glacier and the Hueneme Glacier.

Geographic entities mentioned:
surface_form: Watson Escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
It is joined from the west by the Wotkyns Glacier and the Gardiner Glacier flowing from the Watson Escarpment. It flows northwest past the Wisconsin Range to the east, from which it receives the Norfolk Glacier and the Hueneme Glacier. Past the Quartz Hills to the west it receives the Colorado Glacier. Below Blubaugh Nunatak the Reedy Glacier is joined from the west by the large Kansas Glacier.

Geographic entities mentioned:
surface_form: Quartz Hills
instance_of: Mountain
coordinates: lat: -85.9333
lon: -132.833
Below Blubaugh Nunatak the Reedy Glacier is joined from the west by the large Kansas Glacier. The Kansas Glacier originates on the Stanford Plateau and is fed by the Johns Glacier from the south and Alaska Canyon from the north. The Reedy Glacier continues north past the Ford Nunataks to the east and Abbey Nunatak and Penrod Nunatak to the west.

Geographic entities mentioned:
surface_form: Stanford Plateau
instance_of: Landform
coordinates: lat: -85.95
lon: -140
Below Blubaugh Nunatak the Reedy Glacier is joined from the west by the large Kansas Glacier. The Kansas Glacier originates on the Stanford Plateau and is fed by the Johns Glacier from the south and Alaska Canyon from the north. The Reedy Glacier continues north past the Ford Nunataks to the east and Abbey Nunatak and Penrod Nunatak to the west.

Geographic entities mentioned:
surface_form: Ford Nunataks
instance_of: Mountain
coordinates: lat: -85.5833
lon: -131.5
Named by US-ACAN for Grosenvar S. Wotkyns, hospital corpsman at Byrd Station in 1962. Gardiner Glacier. A glacier at the south side of Quartz Hills, flowing east from Watson Escarpment into Reedy Glacier. Named by US-ACAN for Richard D. Gardiner, construction electrician at Byrd Station in 1962. Colorado Glacier.

Geographic entities mentioned:
surface_form: Quartz Hills
instance_of: Mountain
coordinates: lat: -85.9333
lon: -132.833
Named by US-ACAN for Richard D. Gardiner, construction electrician at Byrd Station in 1962. Colorado Glacier. A tributary glacier, long, draining northeast from Michigan Plateau to enter Reedy Glacier between the Quartz Hills and Eblen Hills. Named by US-ACAN for the University of Colorado Boulder, which has sent a number of research personnel to Antarctica. Kansas Glacier.

Geographic entities mentioned:
surface_form: Michigan Plateau
instance_of: Landform
coordinates: lat: -86.1333
lon: -133.5
Named by US-ACAN for the University of Colorado Boulder, which has sent a number of research personnel to Antarctica. Kansas Glacier. A steep glacier, long, draining northeast from Stanford Plateau to enter Reedy Glacier just north of Blubaugh Nunatak. Named by US-ACAN for the University of Kansas, Lawrence, KS, which has sent a number of research personnel to Antarctica. Johns Glacier.

Geographic entities mentioned:
surface_form: Stanford Plateau
instance_of: Landform
coordinates: lat: -85.95
lon: -140
Named by US-ACAN for the University of Kansas, Lawrence, KS, which has sent a number of research personnel to Antarctica. Johns Glacier. An arc-shaped glacier long in the northern part of Watson Escarpment. It drains eastward around the northern side of Mount Doumani to join the Kansas Glacier. Named by US-ACAN for Lt. Ernest H.

Geographic entities mentioned:
surface_form: Watson Escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
Named by US-ACAN for the University of Kansas, Lawrence, KS, which has sent a number of research personnel to Antarctica. Johns Glacier. An arc-shaped glacier long in the northern part of Watson Escarpment. It drains eastward around the northern side of Mount Doumani to join the Kansas Glacier. Named by US-ACAN for Lt. Ernest H.

Geographic entities mentioned:
surface_form: Mount Doumani
instance_of: Mountain
coordinates: lat: -85.8167
lon: -137.633
Named by US-ACAN for Lt. Ernest H. Johns, USN, a participant in several deployments of Operation Deep Freeze, 1955-68. McCarthy Glacier. A broad glacier at the south side of Wisconsin Plateau, flowing west to merge with the lower part of Olentangy Glacier before entering Reedy Glacier just southwest of Mount McNaughton. Named by US-ACAN for Lt. Robert J.

Geographic entities mentioned:
surface_form: Wisconsin Plateau
instance_of: Plateau
coordinates: lat: -85.8
lon: -125.4
surface_form: Mount McNaughton
instance_of: Mountain
coordinates: lat: -85.9667
lon: -128.2
Olentangy Glacier. A glacier draining that portion of the Wisconsin Plateau of the Horlick Mountains that stands east-north-east of Sisco Mesa, flowing south to merge into McCarthy Glacier and the larger Reedy Glacier to the southwest of Mount McNaughton. The name was proposed by the Ohio State University geological party to the Horlick Mountains, 1964-65.

Geographic entities mentioned:
surface_form: Sisco Mesa
instance_of: Landform
coordinates: lat: -85.8333
lon: -127.8
The Olentangy River flows through the University campus. Norfolk Glacier. A glacier, long, draining westward from Wisconsin Range to enter Reedy Glacier between Mount Soyat and Mount Bolton. Named by US-ACAN after Norfolk, VA, location of Detachment Three, the Meteorological Support Unit of the U.S. Naval Support Force, Antarctica. Hueneme Glacier.

Geographic entities mentioned:
surface_form: Mount Soyat
instance_of: Mountain
coordinates: lat: -85.86667
lon: -130.76667
surface_form: Mount Bolton
instance_of: Mountain
countries: Canada
coordinates: lat: 50.33
lon: -114.801
Naval Support Force, Antarctica. Hueneme Glacier. A glacier, long, draining westward from Wisconsin Range to enter Reedy Glacier between Griffith Peak and Mickler Spur. Named by US-ACAN for Port Hueneme, CA, location of the Construction Battalion Center which handles west coast cargo for USN Deep Freeze Operations. Horlick Ice Stream.

Geographic entities mentioned:
surface_form: Griffith Peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.232463888889
lon: -115.64612777778
Davisville Glacier. A glacier about long which drains the north slopes of the Wisconsin Range, between Lentz Buttress and Moran Buttress, and trends northwestward to merge with the lower portion of the Horlick Ice Stream. Named by US-ACAN for Davisville, Rhode Island, location of the Construction Battalion Center responsible for cargo matters for USN Operation Deep Freeze on the east coast.

Geographic entities mentioned:
surface_form: Lentz Buttress
instance_of: Mountain
coordinates: lat: -85.666667
lon: -127.6
Quonset Glacier. A glacier about long which drains the north slopes of Wisconsin Range between Mount LeSchack and Ruseski Buttress and trends west-northwest to enter the north side of Davisville Glacier. Named by US-ACAN after the Naval Air Station, Quonset Point, Rhode Island, home base of Antarctic Development Squadron Six (VXE-6). Spear Nunatak.

Geographic entities mentioned:
surface_form: Mount LeSchack
instance_of: Mountain
coordinates: lat: -85.41667
lon: -124
surface_form: Ruseski Buttress
instance_of: Mountain
coordinates: lat: -85.483333
lon: -124.383333
Named by US-ACAN for Lawrence G. Langford, Jr., a builder with the Byrd Station winter party, 1958. Racine Nunatak. Nunatak, located west of the lower part of Reedy Glacier and ESE of Berry Peaks. Named by US-ACAN for Edward J. Racine, a member of the crew of the icebreaker Eastwind in Operation Deep Freeze 1967. Cohen Nunatak.

Geographic entities mentioned:
surface_form: Berry Peaks
instance_of: Mountain
coordinates: lat: -85.4333
lon: -138.533
Hinchinbrooke, Quebec. Hinchinbrooke (or Hinchinbrook until 1993) is a rural community in southern Quebec, Canada, in the Châteauguay Valley, in the MRC de Le Haut-Saint-Laurent. The population as of the 2021 Canadian census was 2,187. History. Its first settlers were Irish who arrived around 1820. The parish was called Saint-Patrice-de-Hinchin(g)brook(e), or in English St.

Geographic entities mentioned:
surface_form: Châteauguay Valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.3611
lon: -73.75
The primary industries in Hinchinbrooke are agriculture, with dairy cattle and apple farming being the most prevalent sub-sectors. Attractions. The Powerscourt Covered Bridge over the Châteauguay River was originally built in 1861, and is now a National Historic Site of Canada. Notable people. Sir William Hales Hingston, physician and mayor of Montreal from 1875 to 1877, was born in Hinchinbrooke.

Geographic entities mentioned:
surface_form: Châteauguay River
instance_of: Watercourse
countries: United States
Canada
coordinates: lat: 45.401
lon: -73.752
It is located in the Oruro Department, Sabaya Province, Sabaya Municipality. P'iq'iñ Q'ara is situated south-west of the mountain Kimsa Chata, near the border with Chile. It lies at the confluence of the rivers Chullumpiri Jawira and &quot;Lliscaya&quot; Jawira.

Geographic entities mentioned:
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.1058
lon: -68.3858
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.1214
lon: -68.3297
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.71666667
lon: -68.7
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.10972222
lon: -67.66222222
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.88333333
lon: -68.85
P'iq'iñ Q'ara (Oruro). P'iq'iñ Q'ara (Aymara &quot;p'iq'iña&quot; head, &quot;q'ara&quot; bare, bald, &quot;p'iq'iña q'ara&quot; bald, &quot;baldheaded&quot;, Hispanicized spelling &quot;Pekheñ Khara&quot;) is a mountain in the Cordillera Occidental in the Andes of Bolivia. It is located in the Oruro Department, Sabaya Province, Sabaya Municipality.

Geographic entities mentioned:
surface_form: p'iq'iñ q'ara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6117
lon: -67.8239
surface_form: p'iq'iñ q'ara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.99555556
lon: -66.54
surface_form: p'iq'iñ q'ara (oruro)
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.97
lon: -68.8903
surface_form: p'iq'iñ q'ara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.00444444
lon: -67.44555556
surface_form: p'iq'iñ q'ara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.78083333
lon: -67.99694444
P'iq'iñ Q'ara (Oruro). P'iq'iñ Q'ara (Aymara &quot;p'iq'iña&quot; head, &quot;q'ara&quot; bare, bald, &quot;p'iq'iña q'ara&quot; bald, &quot;baldheaded&quot;, Hispanicized spelling &quot;Pekheñ Khara&quot;) is a mountain in the Cordillera Occidental in the Andes of Bolivia. It is located in the Oruro Department, Sabaya Province, Sabaya Municipality.

Geographic entities mentioned:
surface_form: p'iq'iñ q'ara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6117
lon: -67.8239
surface_form: p'iq'iñ q'ara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.99555556
lon: -66.54
surface_form: p'iq'iñ q'ara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.97
lon: -68.8903
surface_form: p'iq'iñ q'ara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.00444444
lon: -67.44555556
surface_form: p'iq'iñ q'ara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.78083333
lon: -67.99694444
Materials from all over China were used throughout the building: granite from Sichuan province, porcelain plates from Guangdong province, pine trees from Yan'an in Shaanxi province, saw-wort seeds from the Tian Shan mountains in the Xinjiang Autonomous Region, soil from quake-stricken Tangshan, colored pebbles from Nanjing, milky quartz from the Kunlun Mountains, pine logs from Jiangxi province, and rock samples from Mount Everest.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Nothing particular is known about his visit. Adam Johann von Krusenstern's expedition visited India on his way to China in 1797–1798 during the first Russian circumnavigation. He stayed for short whiles in Madras and Calcutta, acquainted with the commercial and administrative activity of the East India Company and made a two-month journey on board HMS Orpheus in the Bay of Bengal.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Gibralfaro. Mount Gibralfaro () is a hill located in Málaga in southeast Spain. It is a 130 m high foothill of the Montes de Málaga, part of the Cordillera Penibética. At the top of the hill stands the Castle of Gibralfaro overlooking Málaga city and the Mediterranean Sea, and connected by a walled corridor to the Alcazaba of Málaga. History.

Geographic entities mentioned:
surface_form: alcazaba
instance_of: Mountain
countries: Spain
coordinates: lat: 37.067276
lon: -3.30127
surface_form: gibralfaro
instance_of: Mountain
countries: Spain
coordinates: lat: 36.72333333
lon: -4.41083333
History. Gibralfaro has been the site of fortifications since the Phoenician foundation of Málaga city, circa 770 BC. The location was fortified by Caliph Abd-al-Rahman III in 929 CE. At the beginning of the 14th century, Yusuf I of the Kingdom of Granada expanded the fortifications within the Phoenician lighthouse enclosure and erected a double wall to the Alcazaba.

Geographic entities mentioned:
surface_form: alcazaba
instance_of: Mountain
countries: Spain
coordinates: lat: 37.067276
lon: -3.30127
The castle was used as a military base until 1925. At the end of 2005, a thick forest of pines and eucalyptus trees were planted on the hill. On its outskirts are the historical buildings of the seminary and the Alcazaba, the &quot;Jardines de Puerta Oscura&quot; (Dark Gate Gardens), as well as a Parador.

Geographic entities mentioned:
surface_form: alcazaba
instance_of: Mountain
countries: Spain
coordinates: lat: 37.067276
lon: -3.30127
Gibralfaro. Mount Gibralfaro () is a hill located in Málaga in southeast Spain. It is a 130 m high foothill of the Montes de Málaga, part of the Cordillera Penibética. At the top of the hill stands the Castle of Gibralfaro overlooking Málaga city and the Mediterranean Sea, and connected by a walled corridor to the Alcazaba of Málaga. History.

Geographic entities mentioned:
surface_form: gibralfaro
instance_of: Mountain
countries: Spain
coordinates: lat: 36.72333333
lon: -4.41083333
At the top of the hill stands the Castle of Gibralfaro overlooking Málaga city and the Mediterranean Sea, and connected by a walled corridor to the Alcazaba of Málaga. History. Gibralfaro has been the site of fortifications since the Phoenician foundation of Málaga city, circa 770 BC. The location was fortified by Caliph Abd-al-Rahman III in 929 CE.

Geographic entities mentioned:
surface_form: gibralfaro
instance_of: Mountain
countries: Spain
coordinates: lat: 36.72333333
lon: -4.41083333
The most visible remains of the Castle today are the solid ramparts rising above the pines In the &quot;Centro de Interpretación de Gibralfaro&quot; (Gibralfaro Interpretation Center) in the former gunpowder arsenal of the Castle is a little museum that shows the castle’s history over the centuries since the Reconquest. The castle was used as a military base until 1925.

Geographic entities mentioned:
surface_form: gibralfaro
instance_of: Mountain
countries: Spain
coordinates: lat: 36.72333333
lon: -4.41083333
surface_form: gibralfaro
instance_of: Mountain
countries: Spain
coordinates: lat: 36.72333333
lon: -4.41083333
Currently pending approval is a project intended to safeguard the mount and its surroundings from any urban intervention and promote it as a space for public recreation. Another project is planned to build a cable car linking the city center with the Gibralfaro castle. Geology.

Geographic entities mentioned:
surface_form: gibralfaro
instance_of: Mountain
countries: Spain
coordinates: lat: 36.72333333
lon: -4.41083333
surface_form: gibralfaro
instance_of: Mountain
countries: Spain
coordinates: lat: 36.72333333
lon: -4.41083333
The aggregation of many individuals in one area increases the chances of fertilisation taking place and the buoyancy of the eggs should aid in their dispersal. Taxonomy. The species was first described in 1872 by Charles Wyville Thomson, from a specimen dredged from a depth of 500 fathoms of the Butt of Lews, and from fragments taken in deep waters of the Rockall Channel.

Geographic entities mentioned:
surface_form: Butt of Lews
instance_of: Landform
countries: United Kingdom
coordinates: lat: 58.5156
lon: -6.26119
Patterson Township is a geographic township in central Ontario, Canada. As it is unincorporated, it is located in the Central Unorganized portion of Parry Sound District. The township is located where the French River flows from Lake Nipissing, and then stretches south until it meets Pringle Township in the south. It is bordered by Nipissing Township on the east, and by Hardy Township on the west.

Geographic entities mentioned:
surface_form: Lake Nipissing
instance_of: Lake
countries: Canada
coordinates: lat: 46.283333333333
lon: -80
It is bordered by Nipissing Township on the east, and by Hardy Township on the west. Patterson only has one community, that of Restoule. Most of its settlement is found in the southern region where Restoule is, and along the two lakes of the south, Restoule Lake and Commanda Lake. It is part of the Almaguin Highlands region.

Geographic entities mentioned:
surface_form: Restoule Lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.05
lon: -79.7667
surface_form: Commanda Lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.0167
lon: -79.7
It is part of the Almaguin Highlands region. There are also some cottages located on the south shore of Lake Nipissing, but the area has no permanent residences. There are approximately 300 people living in the township (415 including nearby Farleys Corners and Carr).

Geographic entities mentioned:
surface_form: Lake Nipissing
instance_of: Lake
countries: Canada
coordinates: lat: 46.283333333333
lon: -80
Situated between the eponymous main subrange of &quot;Cordillera Central&quot; and the Sierra de Cayey subrange, it is notable for its untouched forests and the large population of kapok (&quot;Ceiba pentandra&quot;). Las Bocas, along with San Cristóbal Canyon, its larger neighbor to its immediate south, form part of the La Plata River basin. Protection.

Geographic entities mentioned:
surface_form: San Cristóbal Canyon
instance_of: Valley
countries: United States
coordinates: lat: 18.16913
lon: -66.29156
She attended Ohio State University between 1978 and 1985, where she earned both a Master of Science (MS) and a Doctor of Philosophy (PhD) in Geological and Earth Sciences/Geosciences. Her graduate research focused on the study of volcanic fallout in snow and polar ice cores from both Greenland and in samples from the Byrd ice core and from shallow ice cores near Mt.

Geographic entities mentioned:
surface_form: Mt. Erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
Paswegin. Paswegin is an unorganized area in Saskatchewan, Canada. It is located at kilometre 199 of highway 5, north of the Quill Lakes.

Geographic entities mentioned:
surface_form: Quill Lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 51.9167
lon: -104.333
art surmounts nature... and where he... gathered the labourers, the fishermen and the shepherds; we rolled giant stones, built up a fortification against the Nymphs (that is, the river in spate), we carved out an altar for the Muses; soon we could see the Helicon, Parnassus, the Hippocrene; and we planted the forest of the poets. The park as it was - the &quot;carnet de 1802&quot;.

Geographic entities mentioned:
surface_form: Parnassus
instance_of: Mountain
countries: Greece
coordinates: lat: 38.533
lon: 22.6167
It no longer exists. At the edge of the park there is a little hill or mound, surrounded by a large estate wall which is entered through a formal gated doorway. This was, according to the note on the drawing... Mount Parnassus, on which Mr de Pompignan the elder (i.e. Jean-Jacques, the first marquis) composed some of his poetry. The raised area still existed in 1911.

Geographic entities mentioned:
surface_form: Mount Parnassus
instance_of: Mountain
countries: Greece
coordinates: lat: 38.533
lon: 22.6167
Wyndcliff. The Wyndcliff or Wynd Cliff (historically sometimes spelt Wyndcliffe) is a steep limestone cliff rising above the western bank of the River Wye in Monmouthshire, Wales, some north-east of the village of St Arvans, south of Tintern, and north of the town of Chepstow, within the Wye Valley Area of Outstanding Natural Beauty.

Geographic entities mentioned:
surface_form: Wye Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69255
lon: -2.66283
Bow River (New South Wales). Bow River, a partly perennial stream of the Hunter River catchment, is located in the Hunter district of New South Wales, Australia. Course.

Geographic entities mentioned:
surface_form: Hunter
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Bo-Dzhausa Mountain. Bo-Dzhausa Mountain () is a volcanic mountain in Primorsky Krai, Russia, and a part of the Sikhote-Alin mountain range. The nearest inhabited place is the coastal village of Grossevichi. Bo-Dzhausa is accessible from the towns of Dalnegorsk and Sovetskaya Gavan. In December 1995, Khabarovsk United Air Group Flight 3949 crashed in the area.

Geographic entities mentioned:
surface_form: bo-dzhausa mountain
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 48.133333333333
lon: 138.65
Forger Peak. Forger Peak is a mountain summit in British Columbia, Canada. Description. Forger Peak is located southeast of Whistler in Garibaldi Provincial Park. It is part of the McBride Range which is a subrange of the Coast Mountains. Precipitation runoff and glacial meltwater from the mountain's slopes drains north to the Cheakamus River and south to the Pitt River.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: forger peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.93639
lon: -122.79083
Forger Peak. Forger Peak is a mountain summit in British Columbia, Canada. Description. Forger Peak is located southeast of Whistler in Garibaldi Provincial Park. It is part of the McBride Range which is a subrange of the Coast Mountains. Precipitation runoff and glacial meltwater from the mountain's slopes drains north to the Cheakamus River and south to the Pitt River.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Forger Peak is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the west slope rising 1,223 metres (4,012 ft) in. The mountain is named in association with the officially named Forger Glacier which is a descriptive name for the forging action of the glacier in shaping the local terrain.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Forger Peak. Forger Peak is a mountain summit in British Columbia, Canada. Description. Forger Peak is located southeast of Whistler in Garibaldi Provincial Park. It is part of the McBride Range which is a subrange of the Coast Mountains. Precipitation runoff and glacial meltwater from the mountain's slopes drains north to the Cheakamus River and south to the Pitt River.

Geographic entities mentioned:
surface_form: forger peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.93639
lon: -122.79083
Precipitation runoff and glacial meltwater from the mountain's slopes drains north to the Cheakamus River and south to the Pitt River. Forger Peak is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the west slope rising 1,223 metres (4,012 ft) in.

Geographic entities mentioned:
surface_form: forger peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.93639
lon: -122.79083
Samson. Climate. Based on the Köppen climate classification, Forger Peak is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (orographic lift), causing them to drop their moisture in the form of rain or snowfall.

Geographic entities mentioned:
surface_form: forger peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.93639
lon: -122.79083
Winter temperatures can drop below −10 °C with wind chill factors below −20 °C. This climate supports the Forger Glacier on the south slope of the peak, as well as the Snow Bowl Glacier on the north slope. The months of July and August offer the most favorable weather for viewing or climbing Forger Peak.

Geographic entities mentioned:
surface_form: forger peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.93639
lon: -122.79083
Nahshon, Israel. Nahshon () is a kibbutz in central Israel. Located in the Ayalon Valley to the south-west of Modi'in, it falls under the jurisdiction of Mateh Yehuda Regional Council. In it had a population of. History. The village was established in 1950 by immigrant members of Hashomer Hatzair.

Geographic entities mentioned:
surface_form: Ayalon Valley
instance_of: Valley
countries: Israel
coordinates: lat: 31.8675
lon: 34.959444444444
A number of other streams also flow into the dam directly from Ajodhya Hills. The dam is surrounded by hills, forests and a number of small islands within it. The place is situated at the north west end of Ajodhya Hills which is considered as an eastern extension of Chota Nagpur Plateau. People and economy. The area is mainly inhabited by tribal people, with Santal people predominant.

Geographic entities mentioned:
surface_form: Chota Nagpur Plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
The government is promoting this place as a tourist destination. This dam is a part of one of the key small irrigation projects in rural as well as arid areas of West Bengal having a considerable percentage of tribal population. It is one of the promising tourist spots of Eastern Chota Nagpur Plateau region. To date, no facility of boating offered.

Geographic entities mentioned:
surface_form: Chota Nagpur Plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
Most other roads are gravel-covered or dirt roads, requiring off-road-capable vehicles. There is semi-regular passenger transportation with aircraft. The obvious circular area in the central valley is the Klyuchevskaya Sopka, an isolated volcanic group southeast of the curve of the Kamchatka River. West of Kronotsky Point is the Kronotsky Biosphere Reserve with the Valley of Geysers.

Geographic entities mentioned:
surface_form: Klyuchevskaya Sopka
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 56.066666666667
lon: 160.63333333333
The obvious circular area in the central valley is the Klyuchevskaya Sopka, an isolated volcanic group southeast of the curve of the Kamchatka River. West of Kronotsky Point is the Kronotsky Biosphere Reserve with the Valley of Geysers. At the southern tip is the Southern Kamchatka Wildlife Refuge with Kurile Lake. There are several other protected areas on the peninsula. Climate.

Geographic entities mentioned:
surface_form: Kurile Lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 51.457222222222
lon: 157.09861111111
The Kamchatka Peninsula is also known as the &quot;land of fire and ice&quot;. The highest volcano is Klyuchevskaya Sopka (), the largest active volcano in the Northern Hemisphere. Many have highly symmetrical cones, and Kronotsky is viewed by volcanologists Robert and Barbara Decker as a prime candidate for the world's most beautiful volcano.

Geographic entities mentioned:
surface_form: Klyuchevskaya Sopka
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 56.066666666667
lon: 160.63333333333
The highest volcano is Klyuchevskaya Sopka (), the largest active volcano in the Northern Hemisphere. Many have highly symmetrical cones, and Kronotsky is viewed by volcanologists Robert and Barbara Decker as a prime candidate for the world's most beautiful volcano. Somewhat more accessible are the three volcanoes visible from Petropavlovsk-Kamchatsky: Koryaksky, Avachinsky, and Kozelsky.

Geographic entities mentioned:
surface_form: Avachinsky
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 53.255555555556
lon: 158.83333333333
Due to its uniquely suitable environment, biologists estimate that a fifth of all Pacific salmon originates in Kamchatka. Kurile Lake is recognized as the biggest spawning-ground for sockeye in Eurasia. In response to pressure from poaching and to worldwide decreases in salmon stocks, some along nine of the more productive salmon rivers are in the process of being set aside as a nature preserve.

Geographic entities mentioned:
surface_form: Kurile Lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 51.457222222222
lon: 157.09861111111
In October 2019, it was announced that Yoonessi is developing an original film with Walt Disney Animation Studios. Principal photography on her film &quot;Mother Wolf&quot;, starring Melissa Leo, took place in Hudson Valley in New York State in August 2024.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
The City of Caseville is within the township survey area on M-25 but is independent of the Township. The township is small and irregularly shaped, consisting of only eight full sections and twelve partial sections. The township is at the opening of Saginaw Bay into Lake Huron and includes Sand Point, which forms the northern shore of Wild Fowl Bay. Geography.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293