Sarmila/GeoWiki-Features huggingface dataset:
Bindja Airport. Bindja Airport is an airport serving Bindja, a hamlet on the Lukenie River in Mai-Ndombe Province, Democratic Republic of the Congo. The runway is north of Bindja.

Geographic entities mentioned:
surface_form: Lukenie River
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: -2.73089
lon: 18.15563
Hartley is perhaps best known by undergraduates for his book &quot;Rings, Modules and Linear Algebra&quot;, with Trevor Hawkes. Personal life. Hartley was a keen hill walker, and it was while descending Helvellyn in the English Lake District that he collapsed with a heart attack and died.

Geographic entities mentioned:
surface_form: Helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
Jasper explains that if Joe can stop the bleeding, he'll have about 12 hours to get his fingertip reattached and that he will keep the fingertip in a cooler as ransom. Will instructs Joe to go to a house party at San Fernando Valley in order to retrieve cash from a man named Rufus. Before heading to the party, Joe cancels his invite to Love's lunch gathering with her friends.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
The Tungabhadra River then flows east, joining the Krishna in Andhra Pradesh and Telangana border. From here the Krishna continues east to empty into the Bay of Bengal. The wedge of land between the Tungabhadra and the Krishna is known as the Raichur Doab. Cultural significance.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Distribution. The Indus river dolphin presently only occurs in the Indus River system. Its range once stretched over about of the Indus River and its tributaries, but today, it only occurs in about of the river, and its range has declined by 80% since 1870; it is not present anymore in the tributaries. A remnant population is present in the Beas River and Harike Wetland located in Punjab, India.

Geographic entities mentioned:
surface_form: Harike Wetland
instance_of: Lake
countries: India
coordinates: lat: 31.15
lon: 74.96666666666667
Malise V, Earl of Strathearn. Malise V, Earl of Strathearn and Caithness, Jarl of Orkney (; died) was the last of the native Gaelic Earls of Strathearn. Biography. He succeeded to the Earldom of Strathearn in 1329, on the death of his father Malise IV, Earl of Strathearn.

Geographic entities mentioned:
surface_form: Strathearn
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.3325
lon: -3.6825
River. Because the Volga River runs through Chuvashia, Cheboksary is a frequent stop on the many boat tours that travel along the major cities up and down the Volga. To the south, Volgograd, Rostov-on-Don, Astrakhan, the Caspian Sea, and Black Sea are directly reachable. To the west, the Volga River connects Cheboksary with Nizhny Novgorod, Yaroslavl, Moscow, and the northern regions of Russia.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
James River Gorge. The James River Gorge is a water gap created by the James River in Central Virginia. The Gorge is deep as measured from Highcock Knob to the James River and is approximately long.

Geographic entities mentioned:
surface_form: james river gorge
instance_of: Valley
countries: United States
coordinates: lat: 37.596
lon: -79.392
From Buchanan the river flows along the base of the Blue Ridge Mountains until it joins the Maury River near the town of Glasgow and then it turns southeast and begins its descent over the Balcony Falls rapids and through the James River Gorge. The rocks of the gorge are metamorphic in nature with the oldest exposed outcrops being from the Proterozoic Era.

Geographic entities mentioned:
surface_form: james river gorge
instance_of: Valley
countries: United States
coordinates: lat: 37.596
lon: -79.392
The rocks of the gorge are metamorphic in nature with the oldest exposed outcrops being from the Proterozoic Era. To the south of the river the peaks of the James River Face Wilderness dominate and to the north the peaks of Big Rocky Row and Little Rocky Row Mountains form a dramatic backdrop to the river far below.

Geographic entities mentioned:
surface_form: little rocky
instance_of: Mountain
countries: United States
coordinates: lat: 41.918611111111
lon: -74.332222222222
That same day, Angela takes her final vows in a solemn ceremony, dedicating her life to God. Giovanni's older brother, Professor Ugo Severi, breaks down after years of research trying to harness the power of Mount Vesuvius and is taken to the Santa Giovanna d'Aza hospital. Giovanni visits him, and by chance, meets Angela. After their initial shock, he embraces and tries to kiss her.

Geographic entities mentioned:
surface_form: Mount Vesuvius
instance_of: Mountain
countries: Italy
coordinates: lat: 40.821388888889
lon: 14.425555555556
It is part of the larger Central Coast AVA, and contains the greatest concentration of wineries in Santa Barbara County. The valley is formed by the Purisima Hills and San Rafael Mountains to the north and the Santa Ynez Mountains to the south creating a long, east-west corridor with very cool temperatures on the coast that become progressively warmer inland.

Geographic entities mentioned:
surface_form: valley
instance_of: Valley
countries: United States
coordinates: lat: 34.5473
lon: -119.858
His early research focused on indigenous groups, while his later research and work primarily focused on Cass County, Michigan. He conducted additional archaeological research around the U.S. states of Wisconsin and Michigan, including at Little Lake Butte des Morts and Isle Royale. Life. George R. Fox was born to John W. and Viola P. Fox on May 18, 1880 in Peabody, Kansas.

Geographic entities mentioned:
surface_form: Little Lake Butte des Morts
instance_of: Lake
countries: United States
coordinates: lat: 44.209444444444
lon: -88.464166666667
He spent his free time traveling and exploring archeological sites in the United States, Mexico, and the Galapagos Islands. During this time he conducted amateur anthropological work such as a survey of Little Lake Butte des Morts in search of a Sauk and Meskwaki village site.

Geographic entities mentioned:
surface_form: Little Lake Butte des Morts
instance_of: Lake
countries: United States
coordinates: lat: 44.209444444444
lon: -88.464166666667
Wadi al-Nasara. Wadi al-Nasara (/ ALA-LC: &quot;Wādī an-Naṣārá&quot; &quot;Valley of Christians&quot;) is an area in western Syria that administratively belongs to the governorate of Homs. Most people in the area are Greek Orthodox Christians. It is ecclesiastically under the Archdiocese of Akkar, which has its seat in Cheikh Taba, Lebanon.

Geographic entities mentioned:
surface_form: wadi al-nasara
instance_of: Valley
countries: Syria
coordinates: lat: 34.75
lon: 36.3167
Wadi al-Nasara. Wadi al-Nasara (/ ALA-LC: &quot;Wādī an-Naṣārá&quot; &quot;Valley of Christians&quot;) is an area in western Syria that administratively belongs to the governorate of Homs. Most people in the area are Greek Orthodox Christians. It is ecclesiastically under the Archdiocese of Akkar, which has its seat in Cheikh Taba, Lebanon.

Geographic entities mentioned:
surface_form: wadi al-nasara
instance_of: Valley
countries: Syria
coordinates: lat: 34.75
lon: 36.3167
surface_form: valley of christians
instance_of: Valley
countries: Syria
coordinates: lat: 34.75
lon: 36.3167
Most people in the area are Greek Orthodox Christians. It is ecclesiastically under the Archdiocese of Akkar, which has its seat in Cheikh Taba, Lebanon. The current Greek Orthodox Metropolitan of Akkar and Wadi al-Nasara and its dependencies (Safita and Tartus) is Basilius Mansour. Landmarks. Wadi al-Nasara was a popular tourist site before the outbreak of the Syrian civil war.

Geographic entities mentioned:
surface_form: wadi al-nasara
instance_of: Valley
countries: Syria
coordinates: lat: 34.75
lon: 36.3167
surface_form: wadi al-nasara
instance_of: Valley
countries: Syria
coordinates: lat: 34.75
lon: 36.3167
At first, Silver would take the commanders and LMPs from the prime and backup crews to geological sites in Arizona and New Mexico as if for a normal field geology lesson, but closer to launch, these trips became more realistic. Crews began to wear mock-ups of the backpacks they would carry while hiking near the Rio Grande Gorge, and communicate using walkie-talkies to a CAPCOM in a tent.

Geographic entities mentioned:
surface_form: Rio Grande Gorge
instance_of: Landform
countries: United States
coordinates: lat: 36.476519444444
lon: -105.7338
They were able to see Elbow crater, and they began to drive in that direction. Reaching Elbow, a known location, allowed Mission Control to backtrack and get closer to pinpointing the location of the lander. The astronauts took samples there, and then drove to another crater on the flank of Mons Hadley Delta, where they took more.

Geographic entities mentioned:
surface_form: Mons Hadley Delta
instance_of: Mountain
coordinates: lat: 25.72
lon: 3.71
Mbulu District, Manyara. Mbulu District is one of the six districts of the Manyara Region of Tanzania. It is bordered to the north by the Arusha Region and Lake Eyasi, to the east by the Babati Rural District, to the south by the Hanang District, and to the west by the Singida Region. According to the 2022 Tanzania National Census, the population of Mbulu District was 238,272.

Geographic entities mentioned:
surface_form: Lake Eyasi
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.66667
lon: 35.08333
The District is inhabited by people of different ethnic affiliations, especially the Iraqw people who are some of the earliest agro-pastoralists to migrate to what is now the Republic of Tanzania. Other native tribes are the Wahatzabeti living in Yaeda Chini, living a primitive life, and the Datooga people living in Mbulu Vijijini.

Geographic entities mentioned:
surface_form: Yaeda
instance_of: Valley
countries: Tanzania
coordinates: lat: -4.0003083333333
lon: 34.999916666667
People engage mainly in agriculture, keeping livestock and farming activities. There is plantation of onions in Bashay and wheat in many places. The Mbulu District is located in the Mbulu Highlands, with forested mountains like Mount Guwang which are attractive to tourists. There's also a hot spring in Hhaynu.

Geographic entities mentioned:
surface_form: Mbulu Highlands
instance_of: Plateau
countries: Tanzania
coordinates: lat: -3.8556
lon: 35.5444
Though most modern bangka in the Philippines have double-outriggers, single-outrigger dugout canoes also exist in the Philippines. Examples include canoes from Laguna de Bay, as well as boats from Lake Bulusan and Lake Buhi of the Bicol Region. A notable example is the &quot;armadahan&quot; of Laguna de Bay, which were dugouts typically long and. They were equipped with two masts.

Geographic entities mentioned:
surface_form: Laguna de Bay
instance_of: Lake
countries: Philippines
coordinates: lat: 14.508888888889
lon: 121.11888888889
surface_form: Lake Bulusan
instance_of: Lake
countries: Philippines
coordinates: lat: 12.753888888889
lon: 124.09305555556
surface_form: Lake Buhi
instance_of: Lake
countries: Philippines
coordinates: lat: 13.45
lon: 123.51666666667
Though most modern bangka in the Philippines have double-outriggers, single-outrigger dugout canoes also exist in the Philippines. Examples include canoes from Laguna de Bay, as well as boats from Lake Bulusan and Lake Buhi of the Bicol Region. A notable example is the &quot;armadahan&quot; of Laguna de Bay, which were dugouts typically long and. They were equipped with two masts.

Geographic entities mentioned:
surface_form: Laguna de Bay
instance_of: Lake
countries: Philippines
coordinates: lat: 14.508888888889
lon: 121.11888888889
Formed by the confluence of the Bettles and Dietrich rivers near Wiseman on the southern flank of the Brooks Range, the Middle Fork flows generally southwest to its confluence with the North Fork Koyukuk River, with which it forms the main stem of the Koyukuk. From its starting point slightly north of Sukakpak Mountain, the river flows generally south or southwest in its upper reaches.

Geographic entities mentioned:
surface_form: Sukakpak Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 67.60417
lon: -149.74194
The chateau was strategically located within a system of defense for the region. Indeed, in case of attack, the Chateau of Chambéry would send signals from the main tower to the Chateau de Monterminod, which would then signal another chateau, and so forth until the message reached the Maurienne valley. This system enabled the vassals from the area to prepare for any attack and provide help.

Geographic entities mentioned:
surface_form: Maurienne
instance_of: Valley
countries: France
coordinates: lat: 45.2
lon: 6.6666666666667
Mundal Lagoon. Mundal Lagoon (, Muntal) is a lagoon in Puttalam District, western Sri Lanka. The lagoon is sometimes referred to as Mundal Lake. The lagoon is linked to Puttalam Lagoon to the north by a channel. The lagoon's water is brackish. The lagoon is surrounded by a region containing rice paddies, coconut plantations and scrubland. The land is used for prawn fishing and rice cultivation.

Geographic entities mentioned:
surface_form: Puttalam Lagoon
instance_of: Lake
countries: Sri Lanka
coordinates: lat: 8.1
lon: 79.7667
Mundal Lagoon. Mundal Lagoon (, Muntal) is a lagoon in Puttalam District, western Sri Lanka. The lagoon is sometimes referred to as Mundal Lake. The lagoon is linked to Puttalam Lagoon to the north by a channel. The lagoon's water is brackish. The lagoon is surrounded by a region containing rice paddies, coconut plantations and scrubland. The land is used for prawn fishing and rice cultivation.

Geographic entities mentioned:
surface_form: mundal lake
instance_of: Lake
countries: Sri Lanka
coordinates: lat: 7.7833333333333
lon: 79.816666666667
Mundal Lagoon. Mundal Lagoon (, Muntal) is a lagoon in Puttalam District, western Sri Lanka. The lagoon is sometimes referred to as Mundal Lake. The lagoon is linked to Puttalam Lagoon to the north by a channel. The lagoon's water is brackish. The lagoon is surrounded by a region containing rice paddies, coconut plantations and scrubland. The land is used for prawn fishing and rice cultivation.

Geographic entities mentioned:
surface_form: mundal lagoon
instance_of: Lake
countries: Sri Lanka
coordinates: lat: 7.7833333333333
lon: 79.816666666667
The St. Marys River is a tributary of the Maumee River in northwestern Ohio and northeastern Indiana in the United States. Prior to development, it was part of the Great Black Swamp. Today, it drains a primarily rural farming region in the watershed of Lake Erie. It is formed in southern Auglaize County in western Ohio by the confluence of the short East Branch and Center Branch.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Redesdale. Redesdale is a valley in western Northumberland, England. It is formed by the River Rede, which rises in the Cheviots and flows down to join the North Tyne at Redesmouth. Redesdale is traversed by the A68 trunk road, which enters Scotland via Carter Bar at the head of the valley. Redesdale contains the settlements of Elsdon, Otterburn, Rochester, and Byrness.

Geographic entities mentioned:
surface_form: redesdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.229
lon: -2.186
It is formed by the River Rede, which rises in the Cheviots and flows down to join the North Tyne at Redesmouth. Redesdale is traversed by the A68 trunk road, which enters Scotland via Carter Bar at the head of the valley. Redesdale contains the settlements of Elsdon, Otterburn, Rochester, and Byrness. Otterburn is the site of a British Army installation, Otterburn Training Area.

Geographic entities mentioned:
surface_form: redesdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.229
lon: -2.186
Redesdale contains the settlements of Elsdon, Otterburn, Rochester, and Byrness. Otterburn is the site of a British Army installation, Otterburn Training Area. A portion of Redesdale to the west and north of Otterburn forms part of Northumberland National Park and includes the Redesdale Forest, the northernmost part of Kielder Forest. History.

Geographic entities mentioned:
surface_form: redesdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.229
lon: -2.186
surface_form: redesdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.229
lon: -2.186
History. This valley has historically served as an important route into Scotland, and has seen conflict since the time of the Roman Empire. After the Norman Conquest of 1066, the Norman noble family Umfraville gained lands in the area and were the first &quot;Lords of Redesdale&quot;.

Geographic entities mentioned:
surface_form: redesdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.229
lon: -2.186
During the Middle Ages, Elsdon was the economic centre of the area: it served as the market town and as the gathering place for the local graynes (extended Border families). In modern times, the village of Otterburn now holds that distinction. The British crown created the title Baron Redesdale in the 19th century.

Geographic entities mentioned:
surface_form: redesdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.229
lon: -2.186
Although there seems to be no written record of his Cape visit en route to Mauritius, the collection of Proteaceae he sent to Jean-Baptiste Lamarck makes it evident that he at least reached the upper Breede River Valley between Worcester and Tulbagh. Lamarck was the first to describe the silky-haired pincushion in 1792 and he named it &quot;Protea vestita&quot;.

Geographic entities mentioned:
surface_form: Breede River Valley
instance_of: Valley
countries: South Africa
coordinates: lat: -33.75
lon: 19.5
Distribution, habitat and ecology. The silky-haired pincushion can be found between Heerenlogementberg (halfway between Klawer and Graafwater) in the north, through the Clanwilliam, Ceres, Piketberg and Tulbagh districts to the Breede River Valley, several kilometers north of Worcester in the south.

Geographic entities mentioned:
surface_form: Breede River Valley
instance_of: Valley
countries: South Africa
coordinates: lat: -33.75
lon: 19.5
On 1 February 1943, &quot;Makigumo&quot; was on a troop evacuation run to Guadalcanal. While maneuvering to avoid a PT boat attack, she struck a mine. The destroyer removed 237 survivors, including Cdr Isamu Fujita, and scuttled &quot;Makigumo&quot; with a torpedo, south-southwest of Savo Island ().

Geographic entities mentioned:
surface_form: Savo Island
instance_of: Mountain
countries: Solomon Islands
coordinates: lat: -9.1333333333333
lon: 159.81666666667
Frome St Quintin is a village and civil parish in the county of Dorset, southern England, situated approximately northwest of the county town of Dorchester. It is located on an outcrop of greensand near the head of the Frome valley, among the chalk hills of the Dorset Downs. The area features naturally occurring springs, and the first habitation likely dates back to the Roman era.

Geographic entities mentioned:
surface_form: Frome valley
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 50.6958
lon: -1.98861
In the, Warenda had &quot;no people or a very low population&quot;. Geography. Warenda is in the Channel Country. All watercourses in this area are part of the Lake Eyre drainage basin, and most will dry up before their water reaches Lake Eyre. The predominant land use is grazing on native vegetation. Demographics. In the, Warenda had &quot;no people or a very low population&quot;.

Geographic entities mentioned:
surface_form: Lake Eyre
instance_of: Lake
countries: Australia
coordinates: lat: -28.406
lon: 137.2963
During reconstruction this was the site of a track materials depot and siding (now removed). Further south again, the halt at Snowdon Ranger marks the start of one of the paths to the summit of Snowdon. Tracklaying north from Rhyd Ddu station started in May 2001, with an engineering base established there.

Geographic entities mentioned:
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
Chuaña (Lari). Chuaña (possibly from Aymara for oozing of water and other liquids / melting of metals and other things) is a mountain in the Chila mountain range in the Andes of Peru, about high. It is situated in the Arequipa Region, Caylloma Province, Lari District. Chuaña lies north of Quehuisha and Mismi and west of Pucara.

Geographic entities mentioned:
surface_form: chuaña
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4117
lon: -71.7318
It is situated in the Arequipa Region, Caylloma Province, Lari District. Chuaña lies north of Quehuisha and Mismi and west of Pucara. The lake Carhuacocha (possibly from Quechua for &quot;yellowish lake&quot;) lies at its feet.

Geographic entities mentioned:
surface_form: chuaña
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4117
lon: -71.7318
During the Permian extinction, this volcanic activity created the Panjal Traps. In eastern Australia, the Hunter-Bowen orogeny and related magmatic activity was shutting down. The fold belts from this event, as well as the first phase of those at Cape Fold Belt in what is now the South African coast, were being degraded by the Gondwanide orogeny. Induan life.

Geographic entities mentioned:
surface_form: Cape Fold Belt
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
Oga Peninsula. The Oga Peninsula (男鹿半島 &quot;Oga-hantō&quot;) is a rugged peninsula which projects west into the Sea of Japan from the coast of Akita in northern Honshū, the main island of Japan. Politically it coincides with the city of Oga. At the base of the peninsula is Hachirōgata, formerly the second largest lake in Japan. Oga Peninsula is famous for the traditional festival of Namahage.

Geographic entities mentioned:
surface_form: Hachirōgata
instance_of: Lake
countries: Japan
coordinates: lat: 39.913888888889
lon: 140.02083333333
It is the parent, with the hybrid Seyval, of Cayuga White and its sister Horizon. It was created, along with many hybrid grapes designed for the climate of New York's Finger Lakes, at the New York State Agricultural Experiment Station located at Cornell University in Geneva, New York. It is very cold tolerant, down to -29 °C / -20 °F.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
Tuker also expressed his concern over Freyberg's apparent obsession with reducing the monastery on Monte Cassino, arguing that (supported by General Juin, commanding the French Expeditionary Corps) they were attempting to breach the strongest and most fortified point of the Gustav Line.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
Big Island 31F. Big Island 31F is a First Nations reserve on Big Island in Lake of the Woods, northwestern Ontario, Canada. It is one of the reserves of the Anishnaabeg of Naongashiing.

Geographic entities mentioned:
surface_form: Lake of the Woods
instance_of: Lake
countries: Canada
United States
coordinates: lat: 49.09027777777778
lon: -95.2388888888889
Overflow. During highstands, Lake Russell overflowed through the Adobe Valley into Owens Valley. This outflow path formed a narrow inset into the south-eastern shorelines of Lake Russell, and proceeded through a fault-influenced zone with several basins first into Lake Adobe and then through a narrow valley in the Benton Mountains in the Benton Valley arm of Owens Valley.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
This overflow is biogeographically important, as it connected Lake Russell via the Owens River to Owens Lake, Searles Lake, Panamint Lake and Lake Manly in Death Valley.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
Overflow along this pathway however did not occur very frequently; it is further possible that the eruption of the Bishop Tuff of Long Valley Caldera prompted a catastrophic flood through the Adobe Valley overflow path into Owens Valley.

Geographic entities mentioned:
surface_form: Long Valley Caldera
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
surface_form: owens valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6833
lon: -115.722
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 37.3789
lon: -112.573
The northerly &quot;Mount Hicks spillway&quot; is presently higher than the Adobe Valley sill, and passes between the Bodie Hills and the Wassuk Range into Mud Spring Canyon, Rough Creek and eventually East Walker River. This change in spillways is biologically important, as it allowed animals to use Lake Russell as a &quot;transfer point&quot; between different drainages. Lake level history.

Geographic entities mentioned:
surface_form: Bodie Hills
instance_of: Landform
countries: United States
coordinates: lat: 38.2558
lon: -119.09
surface_form: sill
instance_of: Mountain
countries: United States
coordinates: lat: 37.094377777778
lon: -118.50288333333
surface_form: rough creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.857553
lon: -90.217063
surface_form: mount hicks
instance_of: Mountain
countries: United States
coordinates: lat: 38.280277777778
lon: -118.81722222222
surface_form: bodie hills
instance_of: Landform
countries: United States
coordinates: lat: 38.2558
lon: -119.09
The overflow channel was not always located at Adobe Valley, however; a more northerly spillway existed until faulting and volcanism shifted the overflow sill towards Adobe Valley.

Geographic entities mentioned:
surface_form: sill
instance_of: Mountain
countries: United States
coordinates: lat: 37.094377777778
lon: -118.50288333333
Tectonically, the Mono Lake basin started forming 4–3 million years ago mostly in response to subsidence along the Sierra Nevada Fault. Inflow. Lee Vining Creek, Mill Creek and Rush Creek originate in the Sierra Nevada and form the principal inflow of Mono Lake and former Lake Russell. At the time of Lake Russell, June Lake overflowed into the lake. Glaciers.

Geographic entities mentioned:
surface_form: mill creek
instance_of: Watercourse
countries: United States
coordinates: lat: 44.4599675
lon: -89.6412311
surface_form: mill creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.871442
lon: -90.093448
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
At the time of Lake Russell, June Lake overflowed into the lake. Glaciers. During glacial stages, glaciers along Lee Vining Creek, Mill Creek and Rush Creek extended farther down and into Lake Russell. Thus, their moraines were subject to wave erosion by the waters of Lake Russell. These moraines record various pulses of lake and glacier growth and shrinkage.

Geographic entities mentioned:
surface_form: mill creek
instance_of: Watercourse
countries: United States
coordinates: lat: 44.4599675
lon: -89.6412311
surface_form: mill creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.871442
lon: -90.093448
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
Overflow. During highstands, Lake Russell overflowed through the Adobe Valley into Owens Valley. This outflow path formed a narrow inset into the south-eastern shorelines of Lake Russell, and proceeded through a fault-influenced zone with several basins first into Lake Adobe and then through a narrow valley in the Benton Mountains in the Benton Valley arm of Owens Valley.

Geographic entities mentioned:
surface_form: owens valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
This change in spillways is biologically important, as it allowed animals to use Lake Russell as a &quot;transfer point&quot; between different drainages. Lake level history. During the Tahoe glaciation (150,000–130,000 years ago, oxygen isotope stage 6), Lake Russell reached a highstand and overflowed into Owens Valley. During such overflow, the lake levels stabilized at elevation.

Geographic entities mentioned:
surface_form: owens valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
Inflow. Lee Vining Creek, Mill Creek and Rush Creek originate in the Sierra Nevada and form the principal inflow of Mono Lake and former Lake Russell. At the time of Lake Russell, June Lake overflowed into the lake. Glaciers. During glacial stages, glaciers along Lee Vining Creek, Mill Creek and Rush Creek extended farther down and into Lake Russell.

Geographic entities mentioned:
surface_form: june lake
instance_of: Lake
countries: United States
coordinates: lat: 37.7885
lon: -119.075
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
Lake Russell (prehistoric). Lake Russell is a former lake stage of Mono Lake. It was named in honour of Israel Russell, but is also known as Lake Mono in contrast to the present-day lake. This lake was larger than present-day Mono Lake and occasionally overflowed first into the East Walker River and later into the Owens River.

Geographic entities mentioned:
surface_form: lake mono
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
Lake Russell (prehistoric). Lake Russell is a former lake stage of Mono Lake. It was named in honour of Israel Russell, but is also known as Lake Mono in contrast to the present-day lake. This lake was larger than present-day Mono Lake and occasionally overflowed first into the East Walker River and later into the Owens River.

Geographic entities mentioned:
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
Glaciers. During glacial stages, glaciers along Lee Vining Creek, Mill Creek and Rush Creek extended farther down and into Lake Russell. Thus, their moraines were subject to wave erosion by the waters of Lake Russell. These moraines record various pulses of lake and glacier growth and shrinkage. Evidence indicates that at least the Tioga stage glaciation coincided with a lake highstand. Overflow.

Geographic entities mentioned:
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
The northerly &quot;Mount Hicks spillway&quot; is presently higher than the Adobe Valley sill, and passes between the Bodie Hills and the Wassuk Range into Mud Spring Canyon, Rough Creek and eventually East Walker River. This change in spillways is biologically important, as it allowed animals to use Lake Russell as a &quot;transfer point&quot; between different drainages. Lake level history.

Geographic entities mentioned:
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
After 10,000 years before present lake levels were low. Lake deposits. Sandy beach deposits, lacustrine deposits and ooliths and tufa were deposited by Lake Russell, many of these lacustrine formations are known as the Wilson Creek beds. Furthermore, as lake levels dropped thinolite was deposited in the lake, where calcium-rich groundwater emerged into the lake.

Geographic entities mentioned:
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
Pumice and tephra shards are also found within lake deposits and may originate in the Mono Craters. The Mono-Inyo Craters formed in part after the retreat of Lake Russell, thus their deposits are not heavily modified by lacustrine phenomena. Deltaic landforms also exist at Lake Russell and formed during times where the lake levels were stable; the town of Lee Vining is constructed on such a delta.

Geographic entities mentioned:
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
The Mono-Inyo Craters formed in part after the retreat of Lake Russell, thus their deposits are not heavily modified by lacustrine phenomena. Deltaic landforms also exist at Lake Russell and formed during times where the lake levels were stable; the town of Lee Vining is constructed on such a delta. Biology.

Geographic entities mentioned:
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
Fish of the &quot;Catostomus&quot;, &quot;Chasmistes&quot;, &quot;Oncorhynchus clarkii&quot;, &quot;Prosopium&quot; and &quot;Ptychocheilus&quot; genera and molluscs may have been propagated between the Owens River system and the Lake Lahontan system through Lake Russell.

Geographic entities mentioned:
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
Geological setting. Iran lies within the complex zone of collision between the Arabian plate and the Eurasian plate; near Qeshm the rate of convergence is about 25 millimeters annually. Part of this convergence is accommodated by crustal shortening and thickening within the Zagros fold and thrust belt, with the remainder occurring to the north of the Iranian Plateau.

Geographic entities mentioned:
surface_form: Iranian Plateau
instance_of: Plateau
countries: Iran
coordinates: lat: 36.283333
lon: 59.05
Dog Mountain (disambiguation). k0lkgpxs5xfrtly3sffov8xx9sr3" xml:space="preserve">Dog Mountain rises above the north side of the Columbia River Gorge in the U.S. state of Washington.

Geographic entities mentioned:
surface_form: Dog Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.7171
lon: -121.701
Dagsnäs Castle. Dagsnäs Castle is a castle in Sweden, located south of Skara at Lake Hornborga. Dagsnäs has very old origins and belonged to the Gumsehuvud family in the 15th century. It was then passed down through the Thott, Soop, Kafle and Uggla families before it was purchased in 1762 by the original antiquarian and patron Per Tham, in whose family it remained until 1864.

Geographic entities mentioned:
surface_form: Lake Hornborga
instance_of: Lake
countries: Sweden
coordinates: lat: 58.316666666667
lon: 13.55
Goat Mountain (Brewster County, Texas). Goat Mountain is a summit in Brewster County, Texas, United States. Description. Goat Mountain is part of the Chisos Mountains where it is set in Big Bend National Park and the Chihuahuan Desert. The top of the mountain is composed of Burro Mesa Rhyolite (volcanic rock) which formed 29 million years ago during the Oligocene period.

Geographic entities mentioned:
surface_form: goat mountain
instance_of: Mountain
coordinates: lat: 60.607108
lon: -144.6462468
surface_form: goat mountain
instance_of: Mountain
coordinates: lat: 29.1875846
lon: -103.4062832
Goat Mountain (Brewster County, Texas). Goat Mountain is a summit in Brewster County, Texas, United States. Description. Goat Mountain is part of the Chisos Mountains where it is set in Big Bend National Park and the Chihuahuan Desert. The top of the mountain is composed of Burro Mesa Rhyolite (volcanic rock) which formed 29 million years ago during the Oligocene period.

Geographic entities mentioned:
surface_form: goat mountain
instance_of: Mountain
coordinates: lat: 60.607108
lon: -144.6462468
surface_form: park
instance_of: Mountain
coordinates: lat: -67.2333
lon: 51
surface_form: goat mountain
instance_of: Mountain
coordinates: lat: 29.1875846
lon: -103.4062832
Description. Goat Mountain is part of the Chisos Mountains where it is set in Big Bend National Park and the Chihuahuan Desert. The top of the mountain is composed of Burro Mesa Rhyolite (volcanic rock) which formed 29 million years ago during the Oligocene period. Lower slopes are composed of Wasp Spring Tuff of the Burro Mesa Formation, trachyte, and Bee Mountain Basalt of the Chisos Formation.

Geographic entities mentioned:
surface_form: bee mountain
instance_of: Mountain
coordinates: lat: 29.3426173
lon: -103.5403676
state of Idaho in the western United States. It flows for through central Idaho, draining a rugged, thinly populated watershed of. The river drops more than from its headwaters, near Galena Summit above the Sawtooth Valley in the Sawtooth National Recreation Area, to its confluence with the Snake River. Measured at White Bird, its average discharge is.

Geographic entities mentioned:
surface_form: Sawtooth Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.163
lon: -114.884
Course. The Salmon River originates from and flows through the mountains of central and eastern Idaho (Lemhi Range, Sawtooth, Salmon River Mountains, Clearwater and Bitterroot Range). The main stem rises in the Sawtooth Range at over in elevation, several miles northwest of Norton Peak.

Geographic entities mentioned:
surface_form: Norton Peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.7618
lon: -114.653
The main stem rises in the Sawtooth Range at over in elevation, several miles northwest of Norton Peak. For the first, it flows north through the Sawtooth Valley, then turns east at Stanley, receiving the Yankee Fork shortly below that point and the East Fork further downstream.

Geographic entities mentioned:
surface_form: Sawtooth Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.163
lon: -114.884
Shanklin to Ventnor. From Shanklin the path passes the Fisherman's Cottage pub on the beach at the foot of Shanklin Chine, before climbing Appley Steps up the side of the cliff and then through the edge of Shanklin. It continues uphill on a minor road, passing Luccombe village, where there are magnificent views across Sandown Bay.

Geographic entities mentioned:
surface_form: Shanklin Chine
instance_of: Valley
countries: United Kingdom
coordinates: lat: 50.626111111111
lon: -1.1744444444444
Several hydrothermal vents spew hot gas from the edges and depths of the lake. The changing chemical composition of the lake means that it changes colors often, ranging from red, dark green, and even to dark blue. The lake is abutted on its sides by Mount Lokon and Mount Mahawu. The lake carries a fairly strong miasma of rotten eggs, due to the sulfur that is often in great quantities in the lake.

Geographic entities mentioned:
surface_form: Mount Lokon
instance_of: Mountain
countries: Indonesia
coordinates: lat: 1.3580555555556
lon: 124.79194444444
surface_form: lokon
instance_of: Mountain
countries: Indonesia
coordinates: lat: 1.3580555555556
lon: 124.79194444444
Located 30 km from Manado, Lake Linow can be reached by traveling 3 km west of Tomohon, which takes about an hour. The still-active Mount Lokon is also visible and adds to the beauty of the surrounding panorama. Visitors can take a walk around the lake’s edge, but swimming is not recommended due to the high sulfur content. Exposure to sulfur can cause serious injuries and have fatal consequences.

Geographic entities mentioned:
surface_form: lokon
instance_of: Mountain
countries: Indonesia
coordinates: lat: 1.3580555555556
lon: 124.79194444444
The word &quot;Linow&quot; derives from the Minahasa word for &quot;water gathering place&quot;. Located 30 km from Manado, Lake Linow can be reached by traveling 3 km west of Tomohon, which takes about an hour. The still-active Mount Lokon is also visible and adds to the beauty of the surrounding panorama.

Geographic entities mentioned:
surface_form: lake linow
instance_of: Lake
countries: Indonesia
coordinates: lat: 1.2708330555556
lon: 124.82638888889
Lake Linow. Lake Linow is a volcanic lake located outside Tomohon, near Manado, Indonesia. Several hydrothermal vents spew hot gas from the edges and depths of the lake. The changing chemical composition of the lake means that it changes colors often, ranging from red, dark green, and even to dark blue. The lake is abutted on its sides by Mount Lokon and Mount Mahawu.

Geographic entities mentioned:
surface_form: lake linow
instance_of: Lake
countries: Indonesia
coordinates: lat: 1.2708330555556
lon: 124.82638888889
Taxonomy. The lichen was described as new to science in 2011 by the Dutch lichenologist Harrie Sipman. The type specimen was collected from Cerro de la Asunción (Cerro de la Muerte, Cordillera de Talamanca, Cartago, Costa Rica) at an elevation of, where it was found growing on shrub branches in shrubland similar to páramo.

Geographic entities mentioned:
surface_form: Cerro de la Muerte
instance_of: Mountain
countries: Costa Rica
coordinates: lat: 9.56666667
lon: -83.75
Saint Catherine, Egypt. Saint Catherine (,;; also spelled Saint Katrine) is a town located in the South Sinai Governorate of Egypt, situated at the foot of Mount Sinai. The city is the site of Saint Catherine's Monastery. The city is above sea level and is from Nuweiba. In 1994, its population was 4,603 people. In 2002, the Saint Catherine area was declared a UNESCO World Heritage Site. History.

Geographic entities mentioned:
surface_form: Mount Sinai
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.5384
lon: 33.9752
They include temples from the 12th Dynasty, dedicated to Hathor, goddess of love, music, and beauty, and from the New Kingdom dedicated to Sopdu, the god of the Eastern Desert. Saint Catherine’s City was established between 527 and 565 CE, when Saint Catherine's Monastery was constructed at the foot of Mount Sinai by the order of Emperor Justinian. Modern township and tourist attractions.

Geographic entities mentioned:
surface_form: Mount Sinai
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.5384
lon: 33.9752
Snow is the best source of water as it melts slowly, thus releasing water at a steady pace, replenishing the underwater catchment areas. Water from rain flows quickly in the barren mountains, which may cause flash floods. The highest mountain in Egypt is Mount Catherine, with many other peaks in the area over. Religion.

Geographic entities mentioned:
surface_form: Mount Catherine
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.510833333333
lon: 33.955277777778
Places of interest. In addition to Saint Catherine's Monastery and Mount Sinai, of prime historical interest is the palace of Abbas I, the Wali and self-declared Khedive of Egypt and Sudan between 1849 and 1854. The palace was built on a mountain at the time called Jebel Tinya, but later named after him and today called Jebel Abbas Basha.

Geographic entities mentioned:
surface_form: Mount Sinai
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.5384
lon: 33.9752
On the other hand, he liked a secluded lifestyle and had other remote palaces. According to tradition, he selected the place after placing meat on the top of Mount Sinai, Mount Catherine and Mount Tinya. Where the meat took longer to decay, suggested a better environment and cleaner air. Another account recalls that this story was actually made up by the monks to keep him away from the holy peaks.

Geographic entities mentioned:
surface_form: Mount Catherine
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.510833333333
lon: 33.955277777778
Beyond the many religious places found around the Monastery of Saint Catherine and on the top of Mount Sinai and Jebel Safsafa are many other churches, monasteries, and holy sites. The Chapel of Saint Catherine is on the summit of Mount Catherine, the mountain where the body of the saint from Alexandria was placed by angels, according to Christian beliefs.

Geographic entities mentioned:
surface_form: Mount Catherine
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.510833333333
lon: 33.955277777778
North Dell. North Dell () is a village on the Isle of Lewis in the community of Ness, in the Outer Hebrides, Scotland. North Dell is within the parish of Barvas. It lies 5 km south of the Butt of Lewis, between the settlements of South Dell and Cross and comprises 22 crofts. North Dell is reputed to be the best village for the growing of potatoes in Lewis – along with Garrabost in Point! History.

Geographic entities mentioned:
surface_form: Butt of Lewis
instance_of: Landform
countries: United Kingdom
coordinates: lat: 58.5156
lon: -6.26119
Until the late 18th century, the shrine held a now-lost companion text, presumed to be a small illuminated gospel book associated with Saint Laisrén mac Nad Froích (564 or 571), also known as Molaisse or &quot;Mo Laisse&quot;. In the 6th century, Molaisse founded a church on Devenish Island in the southern part of Lough Erne in County Fermanagh, with which the cumdach is associated.

Geographic entities mentioned:
surface_form: Lough Erne
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.48262
lon: -7.80622
Dating. The Soiscél Molaisse was constructed in three phases: the rather plain 8th-century wooden core has bronze casing that once held a small illuminated manuscript. This book is assumed to have been a Gospel and was traditionally associated with the 6th-century Laisrén mac Nad Froích, also known as St.

Geographic entities mentioned:
surface_form: Lough Erne
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.48262
lon: -7.80622
Other potential clerics are Scannlain Ua Dungalaín, abbot of Downpatrick, who was &quot;abducted and blinded in 1010&quot;, and Scanlan Mac Cathail, ri Eoganacht of Lough Leane, although neither are considered strong candidates by most art historians. Provenance. The shrine's hereditary keepers were the O'Meehan family of County Leitrim, who held it for some 500 years.

Geographic entities mentioned:
surface_form: Lough Leane
instance_of: Lake
countries: Ireland
coordinates: lat: 52.041666666667
lon: -9.55
Creeks and swimming pools were also dragged, divers also searched Lake Erie, and members of the public outside the designated search radius were encouraged to search vacant lots and empty buildings. All these avenues of investigation failed to yield results.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
He published a further three books in 1911, which were so successful that he gave up his Admiralty appointment that year to become a full-time author. He lived on board a houseboat – a converted Thames barge – on the River Frome at Wareham in Dorset, where he wrote the majority of his books. An early book, &quot;The Flying Submarine&quot; (published in 1912) may indicate Westerman's genre.

Geographic entities mentioned:
surface_form: River Frome
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 50.6958
lon: -1.98861
It consists of plains covered in grasses, low shrubs, and few widely scattered trees. It was originally found on the plains near the Kissimmee River and Fisheating Creek connected to Lake Okeechobee, but conversion to agriculture and pasture have reduced its range. Frequent fires are necessary to maintain this system. Geographic range.

Geographic entities mentioned:
surface_form: Lake Okeechobee
instance_of: Lake
countries: United States
coordinates: lat: 26.933333333333
lon: -80.8