Sarmila/GeoWiki-Features huggingface dataset:
Three overlapping stratovolcanoes were constructed sequentially along a NE-SW line, with the youngest cone, Tseno-Semyachik, at the southwest end. A hot, acidic crater lake fills the historically active Troitsky Crater, which formed during a large explosive eruption of Ceno-Semiachik about 400 years ago. The water in the lake has an unusual bright turquoise color.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
A hot, acidic crater lake fills the historically active Troitsky Crater, which formed during a large explosive eruption of Ceno-Semiachik about 400 years ago. The water in the lake has an unusual bright turquoise color. It's because the waters of the lake are poisonous due to the content of several types of acids and other chemical elements of the periodic table.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The water in the lake has an unusual bright turquoise color. It's because the waters of the lake are poisonous due to the content of several types of acids and other chemical elements of the periodic table. The water in the lake never freezes, even when everything is covered with a layer of ice and deep snow.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
It's because the waters of the lake are poisonous due to the content of several types of acids and other chemical elements of the periodic table. The water in the lake never freezes, even when everything is covered with a layer of ice and deep snow. The name &quot;Semyachik&quot; in translation from Itelmensky means &quot;Stone Earth&quot;.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The Forty Days of Musa Dagh (film). &quot;The Forty Days of Musa Dagh&quot; is a 1982 American film produced by John Kurkjian, written by Alex Hakobian, and directed by Sarky Mouradian. It is an adaptation of the novel &quot;The Forty Days of Musa Dagh&quot;, about the resistance to the Armenian genocide at Musa Dagh, at the time in Aleppo Vilayet, Ottoman Empire and now in Hatay Province, Turkey.

Geographic entities mentioned:
surface_form: Musa Dagh
instance_of: Mountain
countries: Turkey
coordinates: lat: 36.258333333333
lon: 35.903611111111
Maslenica. Maslenica is a village in the municipality of Jasenice in Zadar County, Dalmatia, Croatia. It is situated in Novigrad Sea. Waters are quite clear due to the Zrmanja river which flows into this gulf. History. The village was built 1000 years ago. Maslenica was damaged under the Croatian War of Independence in the 1990s.

Geographic entities mentioned:
surface_form: Novigrad Sea
instance_of: Lake
countries: Croatia
coordinates: lat: 44.201388888889
lon: 15.521111111111
He was elected to the Ontario legislature in an 1873 by-election held after John Coyne died. He was also a director of the Central Bank of Canada. He owned quarries in the Credit River valley which supplied stone used to build the Ontario Legislature in Toronto. In 1880, he invested in the local Haggert Foundry and became vice-president.

Geographic entities mentioned:
surface_form: Credit River
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.5478
lon: -79.5808
They met while studying at Weber State. Together, they had three children: Danni, Brodie, and Wesley. He resided close to Slocan Lake, British Columbia, during his later years, and maintained a winter home in St. George, Utah. In December 2004, Bauer was diagnosed with stage four throat cancer, even though he never smoked or chewed tobacco.

Geographic entities mentioned:
surface_form: Slocan Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.9472
lon: -117.378
There has been no similar consultation conducted, by either Venezuela or Guyana, with the indigenous people of the region. Venezuelan administrative laws. According to some interpretations of Venezuelan legislation, Guayana Esequiba is an integral part of the jurisdiction of the states of Bolívar and Delta Amacuro, whose common boundary runs along the cusp of the Imataka mountain range.

Geographic entities mentioned:
surface_form: Delta Amacuro
instance_of: Body of water
countries: Venezuela
coordinates: lat: 8.7
lon: -61.15
Tüzer See. Tüzer See is a lake in the Mecklenburgische Seenplatte district in Mecklenburg-Vorpommern, Germany. At an elevation of 51.5 m, its surface area is ca. 0.25 km2.

Geographic entities mentioned:
surface_form: tüzer see
instance_of: Lake
countries: Germany
coordinates: lat: 53.721944444444
lon: 13.035555555556
Along with the battle site, features in the park include Pilot Knob, which at is one of the highest points in West Tennessee, and the Tennessee River Folklife Center, which interprets life in the lower Tennessee Valley in the 19th and 20th centuries. Geographical setting.

Geographic entities mentioned:
surface_form: Tennessee Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.959166666667
lon: -83.850277777778
In October 1954, Hurricane Hazel caused Etobicoke Creek to flood Island Road and 43rd Street and a trailer park in Long Branch, washing trailers and homes into Lake Ontario, killing seven persons. 700 people were evacuated from the trailer park and streets.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
The Cheshire Sandstone Ridge was shortlisted for AONB designation in 2021. Geology. The hills are composed of a range of sandstones of Permian and Triassic age. North–south faulting is in part responsible for elevating harder-wearing strata above the general level of the Cheshire Plain. Typically the higher summits are formed from the Helsby Sandstone.

Geographic entities mentioned:
surface_form: Cheshire Plain
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.2
lon: -2.4666666666667
Montes Jura. Montes Jura is a mountain range in the northwest part of the near side of the Moon. The selenographic coordinates of this range are 47.1° N 34.0° W. It has a diameter of 422 km, with mountains rising to approximately 3800m above the level of Sinus Iridum. They were named after the Jura Mountains in eastern France / western Switzerland.

Geographic entities mentioned:
surface_form: montes jura
instance_of: Mountain
coordinates: lat: 47.49
lon: -36.11
A little farther to the west is Sharp, and to the northeast is the ruined crater Maupertuis. Peter Grego describes a figurine of &quot;The Moon Maiden&quot;, seeing her facial profile in Promontorium Heraclides, her hair in the hills to the west, and her body in Montes Jura. She appears upside down when viewed in binoculars from the Northern Hemisphere. History.

Geographic entities mentioned:
surface_form: montes jura
instance_of: Mountain
coordinates: lat: 47.49
lon: -36.11
surface_form: peter
instance_of: Mountain
coordinates: lat: -70.1833
lon: 64.9333
This range of mountains form a visually pleasing semi-circular ring around the Sinus Iridum, a bay along the northwestern edge of Mare Imbrium. The blunt, east-facing cape at the southwestern end of the range is named Promontorium Heraclides, while the east-facing wedge at the northeast end is called Promontorium Laplace.

Geographic entities mentioned:
surface_form: blunt
instance_of: Mountain
coordinates: lat: -68.8
lon: -65.8
According to the United States Census Bureau, the town has a total area of, of which is land and, or 0.65%, is water. The Long Trail passes through Bolton on its way from Camel's Hump to Mount Mansfield. Schools. Bolton has its own elementary school (Pre-K to 4th grade). The Ellen P. Smilie Memorial School's benefactor was Ellen Pinneo, born in 1849 in Pinneo Flats in Bolton.

Geographic entities mentioned:
surface_form: Camel's Hump
instance_of: Mountain
countries: United States
coordinates: lat: 44.319722222222225
lon: -72.8861111111111
surface_form: Mount Mansfield
instance_of: Mountain
countries: United States
coordinates: lat: 44.543611111111
lon: -72.814166666667
Porzhenka. The Porzhenka () is a river, long, within the Dvina–Pechora Watershed District in Russia. The river originates in the Bolshoye Porzhenskoye Lake and flows into Lake Kenozero, which is drained by the Kena towards the Onega. The Porzhensky Pogost is nearby.

Geographic entities mentioned:
surface_form: Lake Kenozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 62.063
lon: 38.238
Clarksville to Western Grove. Highway 123 begins in the Arkansas River Valley in Clarksville, but quickly becomes a winding mountain highway, spending most of its length in the Ozark Mountains. The route is one of the few north–south corridors in the dense and sparsely populated forest, and passes many campsites, rivers, and hiking trails for recreational use.

Geographic entities mentioned:
surface_form: Arkansas River Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
The U.S. Army Corps of Engineers and the Illinois Water Survey are studying ways to halt degradation of the lake and the USDA Forest Service is helping with a study of public interests in recreation at Wolf Lake. The Wolf Lake water level determines the drainage to Lake Michigan because the connecting Calumet River flows southward during elevated levels and northward during lowered levels.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Pennine Fault System. 9ao0vqvnqgxo751hhklxe8tn5wgjh" xml:space="preserve">The Pennine Fault System is a NW-SE trending zone of faulting that forms the southwestern boundary to the Pennines in Cumbria. It was formed as a normal fault during Permian rifting, bounding the Vale of Eden basin, which has a half-graben geometry. It links through to the Dent Fault at its southeastern end.

Geographic entities mentioned:
surface_form: Vale of Eden
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.388
lon: -2.294
It was formed as a normal fault during Permian rifting, bounding the Vale of Eden basin, which has a half-graben geometry. It links through to the Dent Fault at its southeastern end. Rocks of Ordovician and Silurian age outcrop between the two main strands of the fault, forming the Cross Fell inlier.

Geographic entities mentioned:
surface_form: Cross Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.702777777778
lon: -2.4872222222222
The northernmost part is called the Hodgekinson Fold Belt. North Queensland Highlands. The North Queensland Highlands is a physiographic region in northern Queensland. It includes the Chillagoe Belt, Normanby Platform, Atherton Tableland, Mount Emu Lava Plains and the Cairns Littoral. Bowen. The Bowen Basin is partly overlaid by the Surat Basin.

Geographic entities mentioned:
surface_form: Atherton Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
Cape Town Castle (Afrikaans:), known as Cape Town Hanover Street () in 1924, was a constituency in the Cape Province of South Africa, which existed from 1910 to 1958. Named after the Castle of Good Hope, it covered an area north of Table Mountain and east of the Cape Town CBD. Throughout its existence it elected one member to the House of Assembly and one to the Cape Provincial Council.

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
History. Cape Town Castle was one of the four constituencies created out of the multi-member Cape Town seat for the Cape Parliament. At the time, it extended from Adderley Street in the west to the then-city limit, now in the suburb of Woodstock, in the east and Table Mountain in the south.

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
Derrytresk. Derrytresk is a townland outside Coalisland, County Tyrone, Northern Ireland and is close to the shores of Lough Neagh. It is situated in the historic barony of Dungannon Middle and the civil parish of Clonoe and covers an area of 1020 acres. Derrytresk consists of sub-townlands: Derryvarne, Derrykiltena and Derrynahaskila.

Geographic entities mentioned:
surface_form: Lough Neagh
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.618333333333
lon: -6.3952777777778
Relation to the Xiongnu and other peoples called Huns. Since Joseph de Guignes in the, modern historians have associated the Huns who appeared on the borders of Europe in the with the Xiongnu who had invaded numerous Central Plain polities from the Mongolian Plateau between the and the.

Geographic entities mentioned:
surface_form: Mongolian Plateau
instance_of: Plateau
countries: Mongolia
People's Republic of China
Russia
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 107
Tunía River. Tunía River is a river of Colombia. It is part of the Amazon River basin and one of the sources of Apaporis River.

Geographic entities mentioned:
surface_form: Apaporis River
instance_of: Watercourse
countries: Colombia
coordinates: lat: 1.1847222222222222
lon: -72.72694444444444
Dølafe. The Dølafe is a rare breed of cattle. The breed originates from the Gudbrand Valley, Østerdalen and Hedmarken in Norway. These areas offered good conditions for livestock with easy access to rich mountain pastures. Most Dølafe cattle today came from a single herd at Fåvang in the Gudbrand Valley.

Geographic entities mentioned:
surface_form: Østerdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.575916666666664
lon: 11.087111111111112
The original 1926 section of Route 66 still exists and was renamed North Overholser Drive. This includes the picturesque Lake Overholser Bridge. The alignment runs south of the Stonebridge Lake Estates and Ramsey Lake and is considered one of the most scenic sections of the original Route 66. Dam.

Geographic entities mentioned:
surface_form: ramsey lake
instance_of: Lake
countries: United States
coordinates: lat: 45.208333333333
lon: -93.996388888889
Lake Overholser. Lake Overholser is a reservoir within the city limits of Oklahoma City, Oklahoma. Lake Overholser is formed by Overholser Dam on the North Canadian River in Oklahoma County, Oklahoma. The lake is west of Bethany and from Yukon. Lake Overholser is named after Ed Overholser who was the 16th Mayor of the City of Oklahoma City.

Geographic entities mentioned:
surface_form: lake overholser
instance_of: Lake
countries: United States
coordinates: lat: 35.4977
lon: -97.6796
The lake is west of Bethany and from Yukon. Lake Overholser is named after Ed Overholser who was the 16th Mayor of the City of Oklahoma City. The lake was originally intended to assure an adequate supply of municipal water, since the city depended primarily on the North Canadian River as a source, supplemented by private wells.

Geographic entities mentioned:
surface_form: lake overholser
instance_of: Lake
countries: United States
coordinates: lat: 35.4977
lon: -97.6796
The lake was originally intended to assure an adequate supply of municipal water, since the city depended primarily on the North Canadian River as a source, supplemented by private wells. The need for flood control capability became obvious when the river flooded in 1923. It breached the Lake Overholser Dam and inundated much of the city. Lake.

Geographic entities mentioned:
surface_form: lake overholser
instance_of: Lake
countries: United States
coordinates: lat: 35.4977
lon: -97.6796
U.S. Route 66. &quot;The Mother Road&quot; was situated along the North shore of Lake Overholser from 1926 to 1958. A 1958 Route 66 improvement project created a new alignment for the highway that relocated the roadbed about 1/4 mile North of the lake. The original 1926 section of Route 66 still exists and was renamed North Overholser Drive. This includes the picturesque Lake Overholser Bridge.

Geographic entities mentioned:
surface_form: lake overholser
instance_of: Lake
countries: United States
coordinates: lat: 35.4977
lon: -97.6796
The original 1926 section of Route 66 still exists and was renamed North Overholser Drive. This includes the picturesque Lake Overholser Bridge. The alignment runs south of the Stonebridge Lake Estates and Ramsey Lake and is considered one of the most scenic sections of the original Route 66. Dam.

Geographic entities mentioned:
surface_form: lake overholser
instance_of: Lake
countries: United States
coordinates: lat: 35.4977
lon: -97.6796
It sits above four arched sluiceway openings. 1923 flood. On October 16, 1923, operators at the central telephone exchange of Oklahoma City began calling to notify subscribers living south of Grand Avenue (now Sheridan Avenue) of an impending flood caused by levee breakage at the recently built City Reservoir (now known as Lake Overholser).

Geographic entities mentioned:
surface_form: lake overholser
instance_of: Lake
countries: United States
coordinates: lat: 35.4977
lon: -97.6796
By the time the crisis had passed, Jones, Oklahoma and Spencer, Oklahoma, two towns downstream of Oklahoma City, had been surrounded by water. The official damage estimate was five people confirmed dead and property loss was $3,500,000. Recreational facilities. Lake Overholser is a popular fishing area for local residents. A covered fishing pier is on the southwest side of the lake.

Geographic entities mentioned:
surface_form: dead
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
Raheen-a-Cluig. Raheen-a-Cluig is a medieval church and National Monument in Bray, County Wicklow, Ireland. Location. Raheen-a-Cluig lies on the north face of Bray Head in Raheen Park, about south of the beach, with a commanding view over the coastline. History. Raheen-a-Cluig is believed to have been built in the 12th–13th century AD. The name derives from the Irish &quot;Ráithín an Chloig&quot;.

Geographic entities mentioned:
surface_form: Bray Head
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.190527777778
lon: -6.0841666666667
Geography. Netarhat is located at a height of. It is a plateau covered with thick forest. Located in the Pat region of Chota Nagpur Plateau, Netarhat plateau is about long and broad. It consists of crystalline rocks and has a summit capped with sandstone trap or laterite. Region of Netarhat is covered with Sal, Kendu, Mahua and Eucalyptus. Education.

Geographic entities mentioned:
surface_form: Chota Nagpur Plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
Its headquarters is located in Columbia. Pocosin Lakes NWR was established in 1990. Originally, the southwestern portion of the refuge, now known as the Pungo Unit, was established in 1963 as the Pungo National Wildlife Refuge, but was merged in 1990 with Pocosin Lakes. The National Wildlife Refuge is, and approximately were donated.

Geographic entities mentioned:
surface_form: Pungo Unit
instance_of: Lake
countries: United States
coordinates: lat: 35.7140686
lon: -76.5507567
The McKelvey Valley was named by the Victoria University of Wellington Antarctic Expedition (VUWAE) (1958–59) for B.C. McKelvey, a geologist of the Victoria University of Wellington, who, with P.N. Webb, undertook the first geological exploration of this area (1957–58), and was again in Wright Valley with the VUWAE in 1958–59. Location. The McKelvey Valley is one of the McMurdo Dry Valleys.

Geographic entities mentioned:
surface_form: Wright Valley
instance_of: Valley
coordinates: lat: -77.166666666667
lon: 161.83333333333
McKelvey, a geologist of the Victoria University of Wellington, who, with P.N. Webb, undertook the first geological exploration of this area (1957–58), and was again in Wright Valley with the VUWAE in 1958–59. Location. The McKelvey Valley is one of the McMurdo Dry Valleys. It runs from the Balham Valley to the west to the Victoria Valley and Lake Vida to the east.

Geographic entities mentioned:
surface_form: McMurdo Dry Valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
surface_form: dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
surface_form: mckelvey valley
instance_of: Valley
coordinates: lat: -77.433333333333
lon: 161.55
Location. The McKelvey Valley is one of the McMurdo Dry Valleys. It runs from the Balham Valley to the west to the Victoria Valley and Lake Vida to the east. The Olympus Range forms the south side of the valley, with several smaller valleys running north from that range into the McKelvey Valley.

Geographic entities mentioned:
surface_form: Balham Valley
instance_of: Valley
coordinates: lat: -77.4167
lon: 161.017
surface_form: Victoria Valley
instance_of: Valley
coordinates: lat: -77.383333333333
lon: 161.93333333333
surface_form: Lake Vida
instance_of: Lake
coordinates: lat: -77.38888888888889
lon: 161.92777805555556
surface_form: vida
instance_of: Lake
coordinates: lat: -77.38888888888889
lon: 161.92777805555556
Bull Pass runs from the east of the valley through the Olympus Range, between Mount Jason and Mount Orestes to Wright Valley. The Insel Range forms its north side. Priscu Valley. An upland ice-free valley on the east side of Prentice Plateau in the Olympus Range. The valley opens north to the head of McKelvey Valley. Named by US-ACAN (2004) after John C.

Geographic entities mentioned:
surface_form: Prentice Plateau
instance_of: Plateau
coordinates: lat: -77.4833
lon: 160.617
Priscu, Department of Biological Sciences, Montana State University, Bozeman, MT; United States Antarctic Project (United States ArmyP) investigator in the McMurdo Dry Valleys, 1984-2002. Wall Valley. An upland valley next east of Priscu Valley in the Olympus Range. Minotaur Pass is at the head between Apollo Peak and Mount Electra. The valley opens north to McKelvey Valley.

Geographic entities mentioned:
surface_form: Apollo Peak
instance_of: Mountain
coordinates: lat: -77.5
lon: 160.8
surface_form: Mount Electra
instance_of: Mountain
coordinates: lat: -77.5
lon: 160.9
Virginia Valley. An upland valley east of Wall valley in the Olympus Range, located between the north part of Mount Electra on the west, and Mount Circe and Mount Dido on the east. The valley opens north to McKelvey Valley. Named by US-ACAN (2004) after Ross A.

Geographic entities mentioned:
surface_form: Mount Circe
instance_of: Mountain
coordinates: lat: -77.4833
lon: 160.967
surface_form: Mount Dido
instance_of: Mountain
coordinates: lat: -77.5
lon: 160.95
Virginia, Environmental Studies Program, Dartmouth College, Hanover, NH; United States Antarctic Project (United States ArmyP) soils biologist in the McMurdo Dry Valleys, 13 field seasons, 1989-2002. Kellogg Valley. A high hanging valley, for the most part free of ice, between Mount Boreas and Mount Aeolus in Olympus Range. The valley opens north to McKelvey Valley, below.

Geographic entities mentioned:
surface_form: Mount Boreas
instance_of: Mountain
coordinates: lat: -77.4833
lon: 161.117
Parish Riegel. A riegel, or rock bar extending north from Parish Ledge in the Olympus Range, across McKelvey Valley toward the Insel Range. The riegel is long, wide, and is similar to Bonney Riegel in Taylor Valley. Named by the Advisory Committee on Antarctic Names (US-ACAN) (2004) in association with Parish Ledge (q.v.).

Geographic entities mentioned:
surface_form: Taylor Valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: bonney
instance_of: Lake
coordinates: lat: -77.71667
lon: 162.41667
Minotaur Pass is at the head between Apollo Peak and Mount Electra. The valley opens north to McKelvey Valley. Named by US-ACAN (2004) after Diana Wall, Natural Resources Ecology Laboratory, Colorado State University, Fort Collins, CO; United States Antarctic Project (United States ArmyP) soils biologist in the McMurdo Dry Valleys, 13 field seasons, 1989-2002. Virginia Valley.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
surface_form: mcmurdo dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
surface_form: diana
instance_of: Landform
coordinates: lat: -63.4333
lon: -56.1833
The valley opens north to McKelvey Valley. Named by US-ACAN (2004) after Ross A. Virginia, Environmental Studies Program, Dartmouth College, Hanover, NH; United States Antarctic Project (United States ArmyP) soils biologist in the McMurdo Dry Valleys, 13 field seasons, 1989-2002. Kellogg Valley.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: virginia
instance_of: Mountain
coordinates: lat: -79.25
lon: -84.033333333333
surface_form: dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
surface_form: mcmurdo dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
Kellogg and Davida E. Kellogg, Department of Geological Sciences and Institute of Quaternary Studies, University of Maine, who in several seasons, 1976-90, collaborated in study of the glacial history of the McMurdo Sound region, including field work on the McMurdo Ice Shelf, Ross Ice Shelf, in Ross Sea, and the McMurdo Dry Valleys, the location of this valley. Bratina Valley.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
surface_form: mcmurdo dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
Kellogg Valley. A high hanging valley, for the most part free of ice, between Mount Boreas and Mount Aeolus in Olympus Range. The valley opens north to McKelvey Valley, below. Named by US-ACAN (1997) after husband and wife glacial geologists Thomas B. Kellogg and Davida E.

Geographic entities mentioned:
surface_form: thomas
instance_of: Mountain
coordinates: lat: -71.01666667
lon: 64.6
Minotaur Pass is at the head between Apollo Peak and Mount Electra. The valley opens north to McKelvey Valley. Named by US-ACAN (2004) after Diana Wall, Natural Resources Ecology Laboratory, Colorado State University, Fort Collins, CO; United States Antarctic Project (United States ArmyP) soils biologist in the McMurdo Dry Valleys, 13 field seasons, 1989-2002. Virginia Valley.

Geographic entities mentioned:
surface_form: virginia
instance_of: Mountain
coordinates: lat: -79.25
lon: -84.033333333333
The valley opens north to the head of McKelvey Valley. Named by US-ACAN (2004) after John C. Priscu, Department of Biological Sciences, Montana State University, Bozeman, MT; United States Antarctic Project (United States ArmyP) investigator in the McMurdo Dry Valleys, 1984-2002. Wall Valley. An upland valley next east of Priscu Valley in the Olympus Range.

Geographic entities mentioned:
surface_form: dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
surface_form: mcmurdo dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
It runs from the Balham Valley to the west to the Victoria Valley and Lake Vida to the east. The Olympus Range forms the south side of the valley, with several smaller valleys running north from that range into the McKelvey Valley. Bull Pass runs from the east of the valley through the Olympus Range, between Mount Jason and Mount Orestes to Wright Valley. The Insel Range forms its north side.

Geographic entities mentioned:
surface_form: wright valley
instance_of: Valley
coordinates: lat: -77.166666666667
lon: 161.83333333333
surface_form: bull
instance_of: Mountain
coordinates: lat: -65.0833
lon: -60.3833
McKelvey Valley. McKelvey Valley () is a valley between the western part of the Olympus Range and the Insel Range, in Victoria Land, Antarctica. Exploration and naming. The McKelvey Valley was named by the Victoria University of Wellington Antarctic Expedition (VUWAE) (1958–59) for B.C. McKelvey, a geologist of the Victoria University of Wellington, who, with P.N.

Geographic entities mentioned:
surface_form: mckelvey valley
instance_of: Valley
coordinates: lat: -77.433333333333
lon: 161.55
It runs from the Balham Valley to the west to the Victoria Valley and Lake Vida to the east. The Olympus Range forms the south side of the valley, with several smaller valleys running north from that range into the McKelvey Valley. Bull Pass runs from the east of the valley through the Olympus Range, between Mount Jason and Mount Orestes to Wright Valley. The Insel Range forms its north side.

Geographic entities mentioned:
surface_form: mckelvey valley
instance_of: Valley
coordinates: lat: -77.433333333333
lon: 161.55
Priscu Valley. An upland ice-free valley on the east side of Prentice Plateau in the Olympus Range. The valley opens north to the head of McKelvey Valley. Named by US-ACAN (2004) after John C. Priscu, Department of Biological Sciences, Montana State University, Bozeman, MT; United States Antarctic Project (United States ArmyP) investigator in the McMurdo Dry Valleys, 1984-2002. Wall Valley.

Geographic entities mentioned:
surface_form: mckelvey valley
instance_of: Valley
coordinates: lat: -77.433333333333
lon: 161.55
Minotaur Pass is at the head between Apollo Peak and Mount Electra. The valley opens north to McKelvey Valley. Named by US-ACAN (2004) after Diana Wall, Natural Resources Ecology Laboratory, Colorado State University, Fort Collins, CO; United States Antarctic Project (United States ArmyP) soils biologist in the McMurdo Dry Valleys, 13 field seasons, 1989-2002. Virginia Valley.

Geographic entities mentioned:
surface_form: mckelvey valley
instance_of: Valley
coordinates: lat: -77.433333333333
lon: 161.55
Virginia Valley. An upland valley east of Wall valley in the Olympus Range, located between the north part of Mount Electra on the west, and Mount Circe and Mount Dido on the east. The valley opens north to McKelvey Valley. Named by US-ACAN (2004) after Ross A.

Geographic entities mentioned:
surface_form: mckelvey valley
instance_of: Valley
coordinates: lat: -77.433333333333
lon: 161.55
Kellogg Valley. A high hanging valley, for the most part free of ice, between Mount Boreas and Mount Aeolus in Olympus Range. The valley opens north to McKelvey Valley, below. Named by US-ACAN (1997) after husband and wife glacial geologists Thomas B. Kellogg and Davida E.

Geographic entities mentioned:
surface_form: mckelvey valley
instance_of: Valley
coordinates: lat: -77.433333333333
lon: 161.55
Bratina Valley. An upland valley at the east side of Harris Ledge in the Olympus Range. The valley opens north to McKelvey Valley. Named by US-ACAN (2004) after Bonnie J. Bratina, Department of Microbiology, Michigan State University, East Lansing, MI; with United States Antarctic Project (United States ArmyP) for four seasons at Lake Vanda in the 1990s. Parish Riegel.

Geographic entities mentioned:
surface_form: mckelvey valley
instance_of: Valley
coordinates: lat: -77.433333333333
lon: 161.55
Parish Riegel. A riegel, or rock bar extending north from Parish Ledge in the Olympus Range, across McKelvey Valley toward the Insel Range. The riegel is long, wide, and is similar to Bonney Riegel in Taylor Valley. Named by the Advisory Committee on Antarctic Names (US-ACAN) (2004) in association with Parish Ledge (q.v.).

Geographic entities mentioned:
surface_form: mckelvey valley
instance_of: Valley
coordinates: lat: -77.433333333333
lon: 161.55
Other pseudonyms he used were Jakob Holst and Giorgio Focco. Life. Kinau was the eldest child of fisherman Heinrich Wilhelm Kinau and his wife, Metta Holst, on the Elbe island of Finkenwerder (now part of Hamburg). In 1895 he was apprenticed to his uncle, the merchant August Kinau in Geestemünde (today part of Bremerhaven), and from 1897 until 1898 he attended a commercial school in Bremerhaven.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
In that sense, Democratic Senators Dianne Feinstein and Barbara Boxer proposed a 31-page emergency drought legislation of $300 million aid, and to speed up environmental reviews of water projects, so state and federal officials have &quot;operational flexibility&quot; to move water from the delta to San Joaquin Valley farms.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Dingadee railway station. Dingadee railway station was a regional railway station located on the North Coast line, serving the Hunter Valley locality of Fosterton. It opened in 1913 when the North Coast line was extended from to and closed to passenger services in 1975. The only trace that remains is a signalling hut.

Geographic entities mentioned:
surface_form: Hunter Valley
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
By the 1950s, 38 states, including California, had established migrant ministry programs. Doug Still became the director of the CMM in 1957, and established a rural ministry in the San Joaquin and Imperial Valleys, offering services like camps for children, English classes, personal hygiene instruction, daycare centers, and food distribution.

Geographic entities mentioned:
surface_form: San Joaquin
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
surface_form: Imperial Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.1
lon: -115.5
The current Head of School is Paul McLellan (appointed 2016). Rothesay Netherwood School is an independent private school offering both the Canadian High School Diploma as well as the International Baccalaureate Diploma. The school is located on a campus overlooking the Kennebecasis River in Rothesay, New Brunswick. Introduction.

Geographic entities mentioned:
surface_form: Kennebecasis River
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.31666667
lon: -66.13333333
Antelope Valley (Lander County). The Antelope Valley of west Lander County is a small, 25 mile (40 km) long, mostly arid valley in central Nevada, USA. A fourth valley of the same name Antelope Valley lies in southern Eureka County, east of the Monitor Range.

Geographic entities mentioned:
surface_form: antelope valley
instance_of: Valley
countries: United States
coordinates: lat: 39.8858
lon: -117.328
The Antelope Valley of west Lander County is a small, 25 mile (40 km) long, mostly arid valley in central Nevada, USA. A fourth valley of the same name Antelope Valley lies in southern Eureka County, east of the Monitor Range. The Lander County valley lies south of the Humboldt River and with Antelope Creek, is a western tributary valley to the north-flowing Reese River.

Geographic entities mentioned:
surface_form: antelope valley
instance_of: Valley
countries: United States
coordinates: lat: 39.8858
lon: -117.328
A third valley that shares the name, lies in Douglas County and extends into California. Description. Antelope Valley was so named on account of antelope which once roamed the area. Antelope Valley is short, about 25 mi long, north-to-south, but curves slightly northeast.

Geographic entities mentioned:
surface_form: antelope valley
instance_of: Valley
countries: United States
coordinates: lat: 39.8858
lon: -117.328
Description. Antelope Valley was so named on account of antelope which once roamed the area. Antelope Valley is short, about 25 mi long, north-to-south, but curves slightly northeast. Antelope Creek flows through the valley north, its origins in the south where two mountain ranges merge, the New Pass Range southwest, and Ravenswood Mountain (Range), southeast.

Geographic entities mentioned:
surface_form: antelope valley
instance_of: Valley
countries: United States
coordinates: lat: 39.8858
lon: -117.328
The center-east of the valley is adjacent Antelope Butte, on a small separated ridge in the foothills from the northwest of Ravenswood Mountain. Access. The shortest access to Antelope Valley is made from the south, Nevada Route 305, from Austin, Nevada. The route parallels the Reese River and the valley's north end lies about 40 mi north of Austin, then 10 mi west on unimproved roads.

Geographic entities mentioned:
surface_form: antelope valley
instance_of: Valley
countries: United States
coordinates: lat: 39.8858
lon: -117.328
The light plate, which includes no trees, represents the city's future with sun-loving perennials that thrive in the heat and the sun. General information. Lying between Lake Michigan to the east and the Loop to the west, Grant Park has been Chicago's front yard since the mid 19th century.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
The armature also provides a permanent pruning guide. In addition to the Carl Sandburg symbolism, the western hedge also forms a topiary referring to greek mythology. Lurie Garden is bisected by a diagonal boardwalk, which represents the natural Lake Michigan seawall that still bisects Grant Park.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
The travel connections by road and rail mean residents work in Glasgow, Edinburgh, Falkirk, Stirling and beyond. The town is located in close proximity to the new Seven Lochs Wetland Park, from which views to the Campsies and Loch Lomond can be enjoyed. History. The etymology of the name is uncertain, but may relate to stepping stones over boggy ground. Early maps give the name as Coshnocksteps.

Geographic entities mentioned:
surface_form: Loch Lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
The east side drains into Heath Brook, thence into the South Branch of the Wells River. The south side drains into the Waits River, another tributary of the Connecticut. The west side drains into Great Brook, thence into the Winooski River, Lake Champlain, and ultimately into the Gulf of Saint Lawrence in Canada.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Signal Mountain is a mountain located in Caledonia County, Vermont, in the Groton State Forest. Signal Mountain is flanked to the northwest by Spruce Mountain, and to the southwest by Butterfield Mountain. The north side of Signal Mountain drains into Noyes Pond, thence into the South Branch of the Wells River, the upper Connecticut River, and into Long Island Sound in Connecticut.

Geographic entities mentioned:
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.405555555556
lon: -74.198888888889
surface_form: signal mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2063
lon: -72.3252
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.75
lon: -79.48
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0175
lon: -74.45
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.5521
lon: -114.822
surface_form: signal mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.8489
lon: -110.567
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.33007
lon: -74.1154089
Signal Mountain (Vermont). Signal Mountain is a mountain located in Caledonia County, Vermont, in the Groton State Forest. Signal Mountain is flanked to the northwest by Spruce Mountain, and to the southwest by Butterfield Mountain.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: signal mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2063
lon: -72.3252
surface_form: signal mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.8489
lon: -110.567
Signal Mountain (Vermont). Signal Mountain is a mountain located in Caledonia County, Vermont, in the Groton State Forest. Signal Mountain is flanked to the northwest by Spruce Mountain, and to the southwest by Butterfield Mountain.

Geographic entities mentioned:
surface_form: signal mountain (vermont)
instance_of: Mountain
countries: United States
coordinates: lat: 44.2063
lon: -72.3252
surface_form: signal mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.8489
lon: -110.567
Signal Mountain is flanked to the northwest by Spruce Mountain, and to the southwest by Butterfield Mountain. The north side of Signal Mountain drains into Noyes Pond, thence into the South Branch of the Wells River, the upper Connecticut River, and into Long Island Sound in Connecticut. The east side drains into Heath Brook, thence into the South Branch of the Wells River.

Geographic entities mentioned:
surface_form: signal mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2063
lon: -72.3252
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
surface_form: signal mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.8489
lon: -110.567
Havu people. The Havu people (also known as the Bahavu) are a Bantu ethnic group primarily living in the eastern part of the Democratic Republic of the Congo, particularly on Idjwi Island in Lake Kivu and in parts of Kalehe Territory and Bukavu in South Kivu Province.

Geographic entities mentioned:
surface_form: Lake Kivu
instance_of: Lake
countries: Democratic Republic of the Congo
Rwanda
coordinates: lat: -1.8530555555556
lon: 29.135277777778
Most Havu people are also fluent in Swahili and, to a lesser extent, French. History. The Havu trace their origins to ancient Bantu migrations and have lived in the Lake Kivu region for centuries. The island of Idjwi has long been the cultural and political center of the Havu. Traditional monarchies ruled by kings (Bami) governed much of the region and still hold symbolic power today.

Geographic entities mentioned:
surface_form: Lake Kivu
instance_of: Lake
countries: Democratic Republic of the Congo
Rwanda
coordinates: lat: -1.8530555555556
lon: 29.135277777778
Background. Since the 14th century the Deccan had been divided in two entities: on the one side stood the Muslim Bahmani Sultanate, and on the other stood the native rajas rallied around the Vijayanagara Empire. Continuous wars demanded frequent resupplies of fresh horses, which were imported through sea routes from Persia and Arabia.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Ekur. Ekur (), also known as Duranki, is a Sumerian term meaning &quot;mountain house&quot;. It is the assembly of the gods in the Garden of the gods, parallel in Greek mythology to Mount Olympus and was the most revered and sacred building of ancient Sumer. Origin and meaning. There is a clear association of Ziggurats with mountain houses.

Geographic entities mentioned:
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
Warner sucker. The Warner sucker (&quot;Catostomus warnerensis&quot;) is a rare species of freshwater ray-finned fish in the family Catostomidae. Native to Oregon in the United States and found only in the Warner Basin, its distribution extends just into Nevada and California. It is a federally listed threatened species. Its other common name is redhorse'&quot;.

Geographic entities mentioned:
surface_form: Warner Basin
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 42.4499
lon: -119.851
It becomes sexually mature at three or four. Distribution. This fish is native to shallow lakes and associated marshes and intermittent lakes and creeks in the Warner Valley of Lake County, Oregon. It has been seen in Twelvemile Creek just over the border in Nevada and West Barrel Creek within California state lines. It was historically quite abundant in the valley.

Geographic entities mentioned:
surface_form: Warner Valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
Allenheads. Allenheads is a former mining village in the Pennines to the north of Weardale in Northumberland, England. Lead extraction was the settlement's industry until the mine closed in the late 19th century. Allenheads, which is above sea level, is situated further along the River East Allen from Allendale. History. The settlement was founded around lead mining.

Geographic entities mentioned:
surface_form: Weardale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.716
lon: -1.925
Lake Winfred. Lake Winfred is a natural lake in South Dakota, in the United States. Lake Winfred has the name of the daughter of a pioneer settler.

Geographic entities mentioned:
surface_form: lake winfred
instance_of: Lake
countries: United States
coordinates: lat: 44.000937
lon: -97.359296
Loch of Swannay. The Loch of Swannay is the most northerly loch on the mainland of Orkney and lies within the parish of Birsay in the north west of the island. It is an elliptically shaped, freshwater loch and is close to the lochs of Hundland and Boardhouse.

Geographic entities mentioned:
surface_form: Hundland
instance_of: Lake
countries: United Kingdom
coordinates: lat: 59.11611111
lon: -3.23416667
surface_form: Boardhouse
instance_of: Lake
countries: United Kingdom
coordinates: lat: 59.11166667
lon: -3.27638889
surface_form: the lochs
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.7673
lon: -4.58769
Loch of Swannay. The Loch of Swannay is the most northerly loch on the mainland of Orkney and lies within the parish of Birsay in the north west of the island. It is an elliptically shaped, freshwater loch and is close to the lochs of Hundland and Boardhouse.

Geographic entities mentioned:
surface_form: loch of swannay
instance_of: Lake
countries: United Kingdom
coordinates: lat: 59.1344
lon: -3.20493
Abraham Peak. Abraham Peak is a tall rock formation in Zion National Park in Washington County, Utah, United States. Access to Abraham Peak is from the main Park road through Sand Beach Trail. Abraham Peak is the tallest of the three peaks that make the Three Patriarchs. Across from Abraham Peak is prominent The Sentinel (,). Name.

Geographic entities mentioned:
surface_form: Three Patriarchs
instance_of: Mountain
countries: United States
coordinates: lat: 37.2372
lon: -112.965
surface_form: abraham peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.2451674
lon: -112.9814476
Abraham Peak. Abraham Peak is a tall rock formation in Zion National Park in Washington County, Utah, United States. Access to Abraham Peak is from the main Park road through Sand Beach Trail. Abraham Peak is the tallest of the three peaks that make the Three Patriarchs. Across from Abraham Peak is prominent The Sentinel (,). Name.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: abraham peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.2451674
lon: -112.9814476
Abraham Peak. Abraham Peak is a tall rock formation in Zion National Park in Washington County, Utah, United States. Access to Abraham Peak is from the main Park road through Sand Beach Trail. Abraham Peak is the tallest of the three peaks that make the Three Patriarchs. Across from Abraham Peak is prominent The Sentinel (,). Name.

Geographic entities mentioned:
surface_form: abraham peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.2451674
lon: -112.9814476