Sarmila/GeoWiki-Features huggingface dataset:
Fighting continued throughout the day, the troops remaining in position during the night. Each advance of troops on the 16th was under heavy fire from the Modoc positions. That night the troops succeeded in cutting the Modoc off from their water supply at the shore of Tule Lake. By the morning of April 17 everything was in readiness for the final attack on the Stronghold.

Geographic entities mentioned:
surface_form: Tule Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.909322222222
lon: -121.53304722222
Mount Rexford is a prominent mountain summit located in the Cascade Mountains of southwestern British Columbia, Canada. It is situated north of the Canada–United States border, west of Chilliwack Lake, and east of Slesse Mountain, which is its nearest higher neighbor. Precipitation runoff from the peak drains into Nesakwatch and Centre Creeks, both tributaries of the Chilliwack River.

Geographic entities mentioned:
surface_form: Chilliwack Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.05694444444445
lon: -121.41388888888889
surface_form: Slesse Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.0256
lon: -121.592
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Geology. Mount Rexford is composed of granitic rock related to the Chilliwack batholith, which intruded the region 26 to 29 million years ago after the major orogenic episodes in the region. This is part of the Pemberton Volcanic Belt, an eroded volcanic belt that formed as a result of subduction of the Farallon Plate starting 29 million years ago.

Geographic entities mentioned:
surface_form: Pemberton Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 50.58051944
lon: -122.93235278
surface_form: pemberton volcanic belt
instance_of: Mountain
countries: Canada
coordinates: lat: 50.58051944
lon: -122.93235278
Mount Rexford. Mount Rexford is a prominent mountain summit located in the Cascade Mountains of southwestern British Columbia, Canada. It is situated north of the Canada–United States border, west of Chilliwack Lake, and east of Slesse Mountain, which is its nearest higher neighbor.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mount rexford
instance_of: Mountain
countries: Canada
coordinates: lat: 49.0363
lon: -121.53
Precipitation runoff from the peak drains into Nesakwatch and Centre Creeks, both tributaries of the Chilliwack River. Originally known as &quot;Ensawkwatch&quot;, the mountain was named for an early settler in the area, Rexford, who had a cabin near Slesse Creek and had trap lines in the vicinity. The mountain has two subsidiary peaks known as the Nesakwatch Spires.

Geographic entities mentioned:
surface_form: slesse
instance_of: Mountain
countries: Canada
coordinates: lat: 49.0256
lon: -121.592
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Originally known as &quot;Ensawkwatch&quot;, the mountain was named for an early settler in the area, Rexford, who had a cabin near Slesse Creek and had trap lines in the vicinity. The mountain has two subsidiary peaks known as the Nesakwatch Spires. The mountain's name was officially adopted on June 2, 1950, by the Geographical Names Board of Canada.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Rexford. Mount Rexford is a prominent mountain summit located in the Cascade Mountains of southwestern British Columbia, Canada. It is situated north of the Canada–United States border, west of Chilliwack Lake, and east of Slesse Mountain, which is its nearest higher neighbor.

Geographic entities mentioned:
surface_form: mount rexford
instance_of: Mountain
countries: Canada
coordinates: lat: 49.0363
lon: -121.53
Climate. Based on the Köppen climate classification, Mount Rexford is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Cascade Range where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall.

Geographic entities mentioned:
surface_form: mount rexford
instance_of: Mountain
countries: Canada
coordinates: lat: 49.0363
lon: -121.53
Sri Lanka. Sri Lanka, officially the Democratic Socialist Republic of Sri Lanka, also known historically as Ceylon, is an island country in South Asia. It lies in the Indian Ocean, southwest of the Bay of Bengal, separated from the Indian peninsula by the Gulf of Mannar and the Palk Strait.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Society underwent a major transformation during the reign of Devanampiya Tissa, with the arrival of Buddhism from India. In 250 BCE, Mahinda, a bhikkhu and the son of the Mauryan Emperor Ashoka arrived in Mihintale carrying the message of Buddhism. His mission won over the monarch, who embraced the faith and propagated it throughout the Sinhalese population.

Geographic entities mentioned:
surface_form: Mihintale
instance_of: Mountain
countries: Sri Lanka
coordinates: lat: 8.350594
lon: 80.516945
This period is considered as a time when Sri Lanka was at the height of its power. He built 1,470 reservoirs – the highest number by any ruler in Sri Lanka's history – repaired 165 dams, 3,910 canals, 163 major reservoirs, and 2,376 mini-reservoirs. His most famous construction is the Parakrama Samudra, the largest irrigation project of medieval Sri Lanka.

Geographic entities mentioned:
surface_form: Parakrama Samudra
instance_of: Lake
countries: Sri Lanka
coordinates: lat: 7.9
lon: 80.966666666667
Geography. Sri Lanka, an island in South Asia shaped as a teardrop or a pear/mango, lies on the Indian Plate, a major tectonic plate that was formerly part of the Indo-Australian Plate. It is in the Indian Ocean southwest of the Bay of Bengal, between latitudes 5° and 10° N, and longitudes 79° and 82° E.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Sri Lanka is separated from the mainland portion of the Indian subcontinent by the Gulf of Mannar and Palk Strait. According to Hindu mythology, a land bridge existed between the Indian mainland and Sri Lanka. It now amounts to only a chain of limestone shoals remaining above sea level. Legends claim that it was passable on foot up to 1480 CE, until cyclones deepened the channel.

Geographic entities mentioned:
surface_form: chain of limestone shoals
instance_of: Landform
countries: India
Sri Lanka
coordinates: lat: 9.121
lon: 79.5217
Portions are still as shallow as, hindering navigation. The island consists mostly of flat to rolling coastal plains, with mountains rising only in the south-central part. The highest point is Pidurutalagala, reaching above sea level. Sri Lanka has 103 rivers. The longest of these is the Mahaweli River, extending. These waterways give rise to 51 natural waterfalls of or more.

Geographic entities mentioned:
surface_form: Pidurutalagala
instance_of: Mountain
countries: Sri Lanka
coordinates: lat: 7.0008333333333335
lon: 80.77388888888889
Of the 211 woody trees and lianas within the reserve, 139 (66%) are endemic. The total vegetation density, including trees, shrubs, herbs, and seedlings, has been estimated at 240,000 individuals per hectare. The Minneriya National Park borders the Minneriya Tank, which is an important source of water for elephants inhabiting the surrounding forests.

Geographic entities mentioned:
surface_form: Minneriya Tank
instance_of: Lake
countries: Sri Lanka
coordinates: lat: 8.03333
lon: 80.8833
It was directed by Thierry Vargnes who previously worked with Dion in 2007 on the music videos for &quot;Et s'il n'en restait qu'une (je serais celle-là)&quot; and &quot;Immensité&quot;. The video was filmed in Las Vegas on 16 July 2012 and in the Death Valley. Because of the temperature of in the Nevada desert, in some scenes the director used Dion's double.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Ozark, Arkansas. Ozark is a city in Franklin County, Arkansas, United States and one of the county's two seats of government. The community is located along the Arkansas River in the Arkansas River Valley on the southern edge of the Ozark Mountains. As of the 2020 census it had a population of 3,542.

Geographic entities mentioned:
surface_form: Arkansas River Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
surface_form: Ozark Mountains
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
Almo, Idaho. Almo is an unincorporated town in the Upper Raft River Valley in Cassia County, Idaho, United States. Description. Almo is just over east away from the City of Rocks National Reserve, a area with granite columns as much as high. The ZIP Code for Almo is 83312. Almo is part of the Burley, Idaho Micropolitan Statistical Area. History.

Geographic entities mentioned:
surface_form: Upper Raft River Valley
instance_of: Valley
countries: United States
coordinates: lat: 42.06019
lon: -113.48695
Cadusii. The Cadusii (also called Cadusians;, &quot;Kadoúsioi&quot;; Latin: &quot;Cadusii,&quot; Arabic:&quot;Qādūsīān&quot;) were an ancient Iranian tribe that lived in the mountains between Media and the shore of the Caspian Sea, an area bordering that of the Anariacae and Albani. The Dareitai and Pantimati people may have been part of the Cadusii.

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
San Pedro lake. k8afdhh9pbfxl468qjqf6jpjybmw" xml:space="preserve">#REDIRECT San Pedro Lake

Geographic entities mentioned:
surface_form: san pedro lake
instance_of: Lake
countries: Bolivia
coordinates: lat: -13.146113888889
lon: -62.955897222222
Knockmore, County Mayo. Knockmore () is a village in County Mayo, Ireland in the Parish of Backs. It is adjacent to Lough Conn between the towns of Castlebar and Ballina. Sport.

Geographic entities mentioned:
surface_form: Lough Conn
instance_of: Lake
countries: Ireland
coordinates: lat: 54.043333333333
lon: -9.245
It is composed of 28 member states. Most of these are in Western Europe, but the group also includes countries of North America, the Eastern Mediterranean, Fennoscandia and Oceania. The United States and Holy See (Vatican City) participate as observers. The Group is a non-binding dialogue group where subjects concerning regional and international matters are discussed.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Sites of interest in Bobo-Dioulasso include: the Grand Mosque, the mausoleum of Guimbi Ouattara, the Houet Provincial Museum, and the Guinguette. Banfora. Sites of interest in Banfora include: the Natural Waterfall of Banfora, Lake Tengrela, and the Peaks of Sindou. Diapaga. Sites of interest in Diapaga include the Arli National Park, the W National Park and the cliffs of Gobnangou. Djibo.

Geographic entities mentioned:
surface_form: Lake Tengrela
instance_of: Lake
countries: Burkina Faso
coordinates: lat: 10.63333
lon: -4.85
U.S. Route 220 in Maryland. U.S. Route 220 (US 220) is a part of the U.S. Highway System that runs from Rockingham, North Carolina, to South Waverly, Pennsylvania. In Maryland, the federal highway runs from the West Virginia state line at the North Branch Potomac River in McCoole north to the Pennsylvania state line in Dickens.

Geographic entities mentioned:
surface_form: North Branch Potomac River
instance_of: Watercourse
countries: United States
coordinates: lat: 39.5284255
lon: -78.5875141
The highway passes through the hamlet of Dawson, where it passes a curve of its old alignment designated MD 830A and closely parallels CSX's Mountain Subdivision. US 220 splits away from the railroad tracks to follow the valley of Deep Hollow Creek between Fort Hill immediately to the east and Dans Mountain further to the west.

Geographic entities mentioned:
surface_form: Dans Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.5818
lon: -78.8972
This area had previously been administered by the Bureau of Land Management. It is located northwest of Death Valley proper, south of Eureka Valley, and east of the Owens Valley. The valley's lowest elevations are about and it lies in the rain shadow of the Sierra Nevada range, plus the Inyo Mountains bordering the valley on the west. Natural features.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
surface_form: eureka valley
instance_of: Valley
countries: United States
coordinates: lat: 37.227
lon: -117.762
Saline Valley is a closed or endorheic basin. If filled with water it would be over deep, form a lake with a surface area of roughly, and hold approximately of water. History. Saline Valley was inhabited by the Ko'ongkatün Band of Timbisha Shoshone (also known as Panamint or Koso).

Geographic entities mentioned:
surface_form: shoshone
instance_of: Lake
countries: United States
coordinates: lat: 44.3722
lon: -110.713
surface_form: saline valley
instance_of: Valley
countries: United States
coordinates: lat: 36.75
lon: -117.81
Saline Valley was inhabited by the Ko'ongkatün Band of Timbisha Shoshone (also known as Panamint or Koso). One of their principal villages was known as &quot;Ko'on&quot; and located in Saline Valley, therefore the valley was named after the village and known as Ko'ongkatün (&quot;Ko'on&quot; + &quot;kantün&quot; - &quot;possessing, characterized by&quot; the village Ko'on) or simply Ko'on.

Geographic entities mentioned:
surface_form: saline valley
instance_of: Valley
countries: United States
coordinates: lat: 36.75
lon: -117.81
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The valley's lowest elevations are about and it lies in the rain shadow of the Sierra Nevada range, plus the Inyo Mountains bordering the valley on the west. Natural features. A large dry lake occupies the center of the valley. The west end of the lake supports a salt marsh, which contains a variety of plant and animal life. The marsh is fed by a perennial stream from Hunter Canyon.

Geographic entities mentioned:
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6282988
lon: -97.0561783
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 38.3360373
lon: -117.7898285
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 45.0425
lon: -97.31972222
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The Saline Military operations area (MOA) covers the entire valley south to Hunter Mountain from 200' AGL up to FL180 with an ATCAA located over the same area extending from FL180 up to FL600. The airspace is used by military aircraft primarily from Nellis AFB, Edwards AFB, NAWS China Lake, and NAS Lemoore for high and low altitude mission training.

Geographic entities mentioned:
surface_form: china lake
instance_of: Lake
countries: United States
coordinates: lat: 44.433
lon: -69.547
Salt mining began in 1903 at the south end of the lake, and continued into the 1930s. An electric aerial tram was constructed in 1911 to carry the salt over the Inyo Mountains to a terminus northeast of Keeler, California in the Owens Valley. It operated sporadically from 1913 to 1936, but ultimately proved to be too expensive to run.

Geographic entities mentioned:
surface_form: owens valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
Saline Valley. Saline Valley is a large, deep, and arid graben, about in length, in the northern Mojave Desert of California, a narrow, northwest–southeast-trending tectonic sink defined by fault-block mountains. Most of it became a part of Death Valley National Park when the park was expanded in 1994. This area had previously been administered by the Bureau of Land Management.

Geographic entities mentioned:
surface_form: saline valley
instance_of: Valley
countries: United States
coordinates: lat: 36.75
lon: -117.81
There are a number of hot springs in the northeast corner of the valley. The water temperature at the source of these springs averages at. Saline Valley's three main warm springs are reached by a primary road known as the Warm Springs Road or Painted Rock Road. Lower Warm Springs is the largest, most developed, and most popular dispersed camping area.

Geographic entities mentioned:
surface_form: saline valley
instance_of: Valley
countries: United States
coordinates: lat: 36.75
lon: -117.81
Saline Valley's three main warm springs are reached by a primary road known as the Warm Springs Road or Painted Rock Road. Lower Warm Springs is the largest, most developed, and most popular dispersed camping area. Palm Spring is smaller and less crowded with great views of Saline Valley and the source feeds two tubs known as Wizard Pool and Volcano Pool.

Geographic entities mentioned:
surface_form: saline valley
instance_of: Valley
countries: United States
coordinates: lat: 36.75
lon: -117.81
Upper Warm Spring, the smallest and least disturbed of the main springs, is a deep pool of lukewarm azure water surrounded by cattail, arrow-weed, and grasses, in full view of the Saline Range. Saline Valley is a closed or endorheic basin. If filled with water it would be over deep, form a lake with a surface area of roughly, and hold approximately of water. History.

Geographic entities mentioned:
surface_form: saline valley
instance_of: Valley
countries: United States
coordinates: lat: 36.75
lon: -117.81
Saline Valley was a significant mineral source in the late 19th and early 20th centuries. The Conn and Trudo Borax Company mined borax from the salt marsh from 1874 to 1895. The remains of this site can be seen today as a few shallow pits near Saline Valley Road. Salt mining began in 1903 at the south end of the lake, and continued into the 1930s.

Geographic entities mentioned:
surface_form: saline valley
instance_of: Valley
countries: United States
coordinates: lat: 36.75
lon: -117.81
This area had previously been administered by the Bureau of Land Management. It is located northwest of Death Valley proper, south of Eureka Valley, and east of the Owens Valley. The valley's lowest elevations are about and it lies in the rain shadow of the Sierra Nevada range, plus the Inyo Mountains bordering the valley on the west. Natural features.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The marsh is fed by a perennial stream from Hunter Canyon. North of the lake is a large area of low and sweeping sand dunes. There are a number of hot springs in the northeast corner of the valley. The water temperature at the source of these springs averages at. Saline Valley's three main warm springs are reached by a primary road known as the Warm Springs Road or Painted Rock Road.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Saline Valley. Saline Valley is a large, deep, and arid graben, about in length, in the northern Mojave Desert of California, a narrow, northwest–southeast-trending tectonic sink defined by fault-block mountains. Most of it became a part of Death Valley National Park when the park was expanded in 1994. This area had previously been administered by the Bureau of Land Management.

Geographic entities mentioned:
surface_form: death valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Golden Empire Council. The Golden Empire Council (GEC-BSA) is a California-based 501(c)(3) nonprofit affiliated with the Boy Scouts of America and its Western Region, Area 4. The council serves a large section of Northern California, primarily the Sacramento Valley and the northern Sierra Nevada.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
It is located in the Ancash Region, Huari Province, Chavín de Huantar District. Puka Mach'ay lies east of Qishqi. One of the little lakes south of it is named Pukaqucha (Quechua for &quot;red lake&quot;).

Geographic entities mentioned:
surface_form: pukaqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -13.24222222
lon: -71.86527778
surface_form: pukaqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -9.32944444
lon: -77.88083333
surface_form: pukaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -11.530555555556
lon: -76.356388888889
surface_form: pukaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -13.6917
lon: -71.1444
surface_form: pukaqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -11.5614
lon: -76.2258
Puka Mach'ay. Puka Mach'ay (Quechua &quot;puka&quot; red, &quot;mach'ay&quot; cave, &quot;red cave&quot;, also spelled &quot;Pucamachay&quot;) is a mountain in the Cordillera Blanca in the Andes of Peru, about high. It is located in the Ancash Region, Huari Province, Chavín de Huantar District. Puka Mach'ay lies east of Qishqi.

Geographic entities mentioned:
surface_form: pucamachay
instance_of: Mountain
countries: Peru
coordinates: lat: -9.77167
lon: -77.2344
surface_form: puka mach'ay
instance_of: Mountain
countries: Peru
coordinates: lat: -9.77167
lon: -77.2344
surface_form: puka mach'ay
instance_of: Mountain
countries: Peru
coordinates: lat: -10.64111111
lon: -76.61194444
surface_form: puka
instance_of: Mountain
countries: Peru
coordinates: lat: -12.6339
lon: -75.5692
surface_form: puka
instance_of: Mountain
countries: Peru
coordinates: lat: -12.6339
lon: -75.5692
surface_form: puka mach'ay
instance_of: Mountain
countries: Peru
coordinates: lat: -11.49888889
lon: -76.08666667
surface_form: mach'ay
instance_of: Mountain
countries: Peru
coordinates: lat: -9.63722222
lon: -76.40027778
surface_form: mach'ay
instance_of: Mountain
countries: Peru
coordinates: lat: -9.63722222
lon: -76.40027778
Puka Mach'ay. Puka Mach'ay (Quechua &quot;puka&quot; red, &quot;mach'ay&quot; cave, &quot;red cave&quot;, also spelled &quot;Pucamachay&quot;) is a mountain in the Cordillera Blanca in the Andes of Peru, about high. It is located in the Ancash Region, Huari Province, Chavín de Huantar District. Puka Mach'ay lies east of Qishqi.

Geographic entities mentioned:
surface_form: puka mach'ay
instance_of: Mountain
countries: Peru
coordinates: lat: -9.77167
lon: -77.2344
surface_form: puka mach'ay
instance_of: Mountain
countries: Peru
coordinates: lat: -10.64111111
lon: -76.61194444
surface_form: puka
instance_of: Mountain
countries: Peru
coordinates: lat: -12.6339
lon: -75.5692
surface_form: puka mach'ay
instance_of: Mountain
countries: Peru
coordinates: lat: -11.49888889
lon: -76.08666667
surface_form: mach'ay
instance_of: Mountain
countries: Peru
coordinates: lat: -9.63722222
lon: -76.40027778
It is a dangerous area due to sinkholes and land mines, and the entrance there is prohibited. The banks of the Arava Stream (and the brine channel) had become eroded in the area, and the continued erosion endangers the stability of the evaporation ponds. Also the seasonal floods of the stream present danger to the chemical plants in the Mount Sodom area.

Geographic entities mentioned:
surface_form: Mount Sodom
instance_of: Mountain
countries: Israel
coordinates: lat: 31.092222222222
lon: 35.382777777778
Pedra da Gávea. Pedra da Gávea is a monolithic mountain in Tijuca Forest, Rio de Janeiro, Brazil. Composed of granite and gneiss, its elevation is, making it one of the highest mountains in the world that ends directly in the ocean.

Geographic entities mentioned:
surface_form: pedra da gávea
instance_of: Mountain
countries: Brazil
coordinates: lat: -22.998055555556
lon: -43.284444444444
It has been suggested that Pedra da Gávea &quot;correspond[s] to the bottom of a granitic magma chamber and the original thickness of the granitic body was much larger than the present exposure.&quot; The granitic body of the Pedra da Gávea could also correspond to the eastern extension of the nearby Pedra Branca Granite Massif, according to Akihisa Motoki et al.

Geographic entities mentioned:
surface_form: pedra da gávea
instance_of: Mountain
countries: Brazil
coordinates: lat: -22.998055555556
lon: -43.284444444444
Marine Police. The Special Center of Maritime Police (Núcleo Especial de Polícia Marítima – NEPOM) was created in twelve Brazilian cities in response to the high rate of crime in Brazilian ports, as well as the need to ostensibly patrol to prevent the occurrence of criminal offenses in Amazonian rivers and Brazilian borders (especially Itaipu Lake on the Brazil-Paraguay border).

Geographic entities mentioned:
surface_form: Itaipu Lake
instance_of: Lake
countries: Brazil
Paraguay
coordinates: lat: -25.04
lon: -54.45
The first known example of the name with the addition &quot;Great&quot;, distinguishing it from Little Mell Fell, is &quot;Great mele Fell&quot; from 1487; it is also found under the name &quot;Westermellfell&quot; in 1589, since it lies to the west of Little Mell Fell; likewise Greenwood's map of 1823 distinguishes them as &quot;West&quot; and &quot;East Mell Fell&quot;.

Geographic entities mentioned:
surface_form: Little Mell Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.60785
lon: -2.8948194444444
The isolated position of the fell makes it a splendid viewpoint. Blencathra and the Dodds dominate the view towards the west, while to the south is an impressive vista of both the Far Eastern and the Eastern Fells, as far as Red Screes and the Kirkstone Pass. To the east, beyond Little Mell Fell there is a clear view across the Eden Valley to the north Pennines. Ascents.

Geographic entities mentioned:
surface_form: Blencathra
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.63985
lon: -3.0504611111111
The isolated position of the fell makes it a splendid viewpoint. Blencathra and the Dodds dominate the view towards the west, while to the south is an impressive vista of both the Far Eastern and the Eastern Fells, as far as Red Screes and the Kirkstone Pass. To the east, beyond Little Mell Fell there is a clear view across the Eden Valley to the north Pennines. Ascents.

Geographic entities mentioned:
surface_form: Little Mell Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.60785
lon: -2.8948194444444
Great Mell Fell. Great Mell Fell (&quot;Bare hill&quot;, with the later additions of both &quot;Fell&quot; and &quot;Great&quot;) is an isolated hill or fell in the English Lake District, north of Ullswater and adjacent to the Eastern Fells. It rises from a level plain to a height of 537 m. Its top is a viewpoint for many of the surrounding higher fells.

Geographic entities mentioned:
surface_form: great mell fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.62
lon: -2.933
Great Mell Fell lies on the watershed between the Derwent river system to the west and the Eden system to the east. This watershed is formed by a low ridge, barely perceptible in places, which connects the Northern and Eastern Fells.

Geographic entities mentioned:
surface_form: great mell fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.62
lon: -2.933
Enteromius sensitivus. &quot;Enteromius sensitivus&quot; is a species of ray-finned fish in the genus &quot;Enteromius&quot; which is found only in the Sanaga River in Cameroon.

Geographic entities mentioned:
surface_form: Sanaga River
instance_of: Watercourse
countries: Cameroon
coordinates: lat: 3.5593388888889
lon: 9.652175
The guards forced a rapid pace on the journey, and one of the exiles, Mikhail Bestuzhev, was nearly killed when he was thrown off the coach and dragged by his chains. Chita. Lunin arrived in Chita at the end of June in 1828, two years after his sentence. Three hundred kilometers southeast of Lake Baikal, the settlement sat in a beautiful valley at the junction of the Chita and Ingoda rivers.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Cowside. Cowside is a side dale of Littondale in North Yorkshire, England. The valley, which faces in a north east direction, carries the waters of Cowside Beck to the River Skirfare at Arncliffe, draining an area of, and flowing for. Cowside is one of the few 'V'-shaped valleys in the Yorkshire Dales (as opposed to a 'U'-shaped valley) which had ice run across the valley, but not down it.

Geographic entities mentioned:
surface_form: Littondale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.134
lon: -2.08
surface_form: cowside
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.126
lon: -2.143
In the latter half of the 12th century, William de Percy [II] granted the rights of the pasture land between Malham Tarn and Arncliffe to the monks of Fountains Abbey. At the eastern end of the beck, where it spills into Littondale, the north-west facing stones are home to dryas octopetala, a now rare plant that exists at is southernmost in England at Cowside.

Geographic entities mentioned:
surface_form: Littondale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.134
lon: -2.08
surface_form: cowside
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.126
lon: -2.143
The beck has an average width of, and an average depth of. Cowside is surrounded by the hills of Parson's Pulpit () to the south, Knowle Fell () and Fountains Fell () to the west, and Darnbrook Fell () to the north. All of these feed water into Cowside Beck through Darnbrook Beck, Fountains Fell Tarn, and Thoragill Beck among others. Cowside Beck flows for and drains an area of.

Geographic entities mentioned:
surface_form: Fountains Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.139722222222
lon: -2.2094444444444
surface_form: fountains fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.139722222222
lon: -2.2094444444444
It was supposedly a path that the monks took to travel between their estates in the area. There is a Cowside Beck near to Stainforth in the Ribblesdale valley; this beck feeds water over Catrigg Force, and into the River Ribble. Another Cowside, also in the parish of Arncliffe, relates to an 18th century farmhouse in Langstrothdale near Beckermonds.

Geographic entities mentioned:
surface_form: Ribblesdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.144333333333336
lon: -2.296333333333333
surface_form: cowside
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.126
lon: -2.143
There is a Cowside Beck near to Stainforth in the Ribblesdale valley; this beck feeds water over Catrigg Force, and into the River Ribble. Another Cowside, also in the parish of Arncliffe, relates to an 18th century farmhouse in Langstrothdale near Beckermonds. The name Cowside is first recorded in 1571 as &quot;Cowesyde&quot;, and literally means &quot;cow hill side&quot;.

Geographic entities mentioned:
surface_form: Langstrothdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.204
lon: -2.134
surface_form: langstrothdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.204
lon: -2.134
surface_form: cowside
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.126
lon: -2.143
The only settlement in the valley is Darnbrook, a very small hamlet at the foot of Darnbrook Fell. Cowside is a common name in the Craven area of the Yorkshire Dales, and it is not to be confused with the Cowside in Upper Wharfedale near Buckden, nor the Cowside Beck near Stainforth.

Geographic entities mentioned:
surface_form: wharfedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.88333
lon: -1.45
surface_form: cowside
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.126
lon: -2.143
surface_form: cowside
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.126
lon: -2.143
surface_form: cowside
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.126
lon: -2.143
Cowside. Cowside is a side dale of Littondale in North Yorkshire, England. The valley, which faces in a north east direction, carries the waters of Cowside Beck to the River Skirfare at Arncliffe, draining an area of, and flowing for. Cowside is one of the few 'V'-shaped valleys in the Yorkshire Dales (as opposed to a 'U'-shaped valley) which had ice run across the valley, but not down it.

Geographic entities mentioned:
surface_form: cowside
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.126
lon: -2.143
Most of the valley is in the civil parish of Arncliffe, but the upper part of the valley, including the hamlet of Darnbrook, is in the civil parish of Malham Moor. Description. The Cowside valley was carved out by glacial action, but the ice flow ran across the valley southwards (transverse) rather than down the valley. This action created the deep incised V-shape.

Geographic entities mentioned:
surface_form: cowside
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.126
lon: -2.143
This action created the deep incised V-shape. The Devensian ice moved from the north-west to the south-east across Cowside Valley, but some ice may have been pushed up the valley (north-eastwards) towards Arncliffe. Evidence of human habitation in the area is evident from the Bronze Age. The remains of small pounds to keep cattle in can be found in the valley above Cowside Beck.

Geographic entities mentioned:
surface_form: cowside
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.126
lon: -2.143
Evidence of human habitation in the area is evident from the Bronze Age. The remains of small pounds to keep cattle in can be found in the valley above Cowside Beck. One such settlement is at Dew Bottoms (), which shows distinct outlines in the ground of huts, both circular and rectangular, and crude boulder walls for pens.

Geographic entities mentioned:
surface_form: cowside
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.126
lon: -2.143
Rainfall over the catchment is an average of annually, and the mean annual temperature is. Cowside beck is known to be home to trout, bullheads, wandering snail (lymnaea peregra), the river limpet (ancylus fluviatilis) and gammarus pulex. The valley and Cowside Beck are within the Malham-Arncliffe SSSI, a upland protected area.

Geographic entities mentioned:
surface_form: cowside
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.126
lon: -2.143
The valley and Cowside Beck are within the Malham-Arncliffe SSSI, a upland protected area. The becks of Malham Tarn outflow, Gordale and Cowside Beck, are noted as being of &quot;high water quality which provide a range of aquatic conditions and associated flora and fauna.&quot;
In normal flow, Cowside Beck discharges water into the River Skirfare at a rate of.

Geographic entities mentioned:
surface_form: cowside
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.126
lon: -2.143
surface_form: cowside
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.126
lon: -2.143
The beck has an average width of, and an average depth of. Cowside is surrounded by the hills of Parson's Pulpit () to the south, Knowle Fell () and Fountains Fell () to the west, and Darnbrook Fell () to the north. All of these feed water into Cowside Beck through Darnbrook Beck, Fountains Fell Tarn, and Thoragill Beck among others. Cowside Beck flows for and drains an area of.

Geographic entities mentioned:
surface_form: cowside
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.126
lon: -2.143
surface_form: cowside
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.126
lon: -2.143
surface_form: fountains fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.139722222222
lon: -2.2094444444444
The valley floor near Falcon Cave is about above sea level, but the top of the valley at Dew Bottoms, is. Darnbrook itself, is a three-building hamlet where the watercourse coming off Darnbrook Fell (and from Fountains Fell Tarn) meets Cowside Beck. Eastwards from here is the Cowside Gorge, a long limestone gorge with steep walls on either side.

Geographic entities mentioned:
surface_form: cowside
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.126
lon: -2.143
surface_form: fountains fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.139722222222
lon: -2.2094444444444
The valley floor near Falcon Cave is about above sea level, but the top of the valley at Dew Bottoms, is. Darnbrook itself, is a three-building hamlet where the watercourse coming off Darnbrook Fell (and from Fountains Fell Tarn) meets Cowside Beck. Eastwards from here is the Cowside Gorge, a long limestone gorge with steep walls on either side.

Geographic entities mentioned:
surface_form: cowside
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.126
lon: -2.143
The underlying stone of the valley floor is Cove Limestone (Holkerian), but at the valley sides and tops, it consists of Gordale Limestone, with the surrounding hills of Darnbrook Fell and Fountains Fell belonging to the Yoredale Series, though the uppermost part of Fountains Fell is Millstone Grit.

Geographic entities mentioned:
surface_form: yoredale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.3056
lon: -2.16667
surface_form: fountains fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.139722222222
lon: -2.2094444444444
surface_form: fountains fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.139722222222
lon: -2.2094444444444
Cowside Beck flows for and drains an area of. At the northern end of the dale, the beck meanders before it flows into Arncliffe and the River Skirfare. One of the caves in the valley, Robinson's Pot, has a strange access point being located in a grate underneath the kitchen window of Darnbrook Farm. The farmhouse and farm are a National Trust tenancy which is about south west of Arncliffe.

Geographic entities mentioned:
surface_form: robinson
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.54
lon: -3.236
Conservation and restoration of Pompeian frescoes. The conservation and restoration of Pompeian frescoes describes the activities, methods, and techniques that have historically been and are currently being used to care for the preserved remains of the frescoes from the archeological site of Pompeii, Italy. The ancient city of Pompeii is famously known for its demise in A.D.

Geographic entities mentioned:
surface_form: Mount Vesuvius
instance_of: Mountain
countries: Italy
coordinates: lat: 40.821388888889
lon: 14.425555555556
In 1945, the widow of Rhoades sold approximately to Dr. Harold E. Thomas of the Strawberry Institute of Santa Clara Valley. The larger was sold to Sebastian and Luigia Borello, now recognized as Borello Farms.

Geographic entities mentioned:
surface_form: Santa Clara Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.366944444444
lon: -121.98388888889
Geography. According to the United States Census Bureau, the town has a total area of 69.4 square miles (179.6 km2), of which 67.4 square miles (174.6 km2) is land and 1.9 square miles (5.0 km2) (2.78%) is water. The northern border of Sodus is Lake Ontario. Sodus Bay, a bay of Lake Ontario is partly in the town.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Oakwood School (Los Angeles). Oakwood School is a K-12 co-educational independent day school located in the San Fernando Valley region of Los Angeles, California. The school consists of two campuses: the elementary school campus in Studio City, and the secondary school campus in North Hollywood.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Enryaku-ji. is a Tendai monastery located on Mount Hiei in Ōtsu, overlooking Kyoto. It was first founded in 788 during the early Heian period (794–1185) by Saichō (767&ndash;822), also known as Dengyō Daishi, who introduced the Tendai sect of Mahayana Buddhism to Japan from China.

Geographic entities mentioned:
surface_form: Mount Hiei
instance_of: Mountain
countries: Japan
coordinates: lat: 35.066666666667
lon: 135.83833333333
In 2007, all &quot;Dryandra&quot; species were transferred to &quot;Banksia&quot; by Austin Mast and Kevin Thiele and the change is accepted by the Australian Plant Census. Distribution and habitat. This variety is widespread in the south-west, mainly between Mount Lesueur, Walpole and the Cape Arid National Park. It grows amongst open woodland and kwongan, usually on rocky soils.

Geographic entities mentioned:
surface_form: Mount Lesueur
instance_of: Mountain
countries: Australia
coordinates: lat: -30.1755
lon: 115.19908333333
The following year, he accompanied the return of to the capital. In 1864, during the Mito Rebellion, he was ordered to pacify the Tengutō encamped on Mount Taiheizan under the command of Takeda Kōunsai. Yamakuni sympathized with the rebels, and advised them to relocate to a more defensible position on Mount Tsukuba. Upon his return, he was imprisoned once again for his disobedience.

Geographic entities mentioned:
surface_form: Mount Tsukuba
instance_of: Mountain
countries: Japan
coordinates: lat: 36.22580555555555
lon: 140.105
Deputy mayor candidate Sobha Shakya finished in second place in Lalitpur, and Nirupama Yadav finished third in Kathmandu. The party was not as successful outside the Kathmandu Valley with their candidates in Itahari getting less than 500 votes. Bibeksheel Sajha. On 26 July 2017 the party announced that it would merge with Bibeksheel Nepali Dal to form Bibeksheel Sajha Party.

Geographic entities mentioned:
surface_form: Kathmandu Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
Death. Koakanu died on March 2, 1885, at Nuʻuanu. His obituaries in the Hawaiian newspapers &quot;Ko Hawaii Paeaina&quot; and &quot;Ka Nupepa Kuokoa&quot; noted he was not ill at the time of his death.

Geographic entities mentioned:
surface_form: Nuʻuanu
instance_of: Landform
countries: United States
coordinates: lat: 21.370277777778
lon: -157.79694444444
In California, some areas received up to ≥20 inches (508 millimeters) of rain. Late November–early December lake-effect snow. Lake effect snow impacted portions of northeastern Ohio and Pennsylvania near Lake Erie, leaving accumulations of. In preparation of the storm, Interstate 90 shut down over of highway. Snow also resulted in portions of Interstate 94 and Pennsylvania State Route 5 closing.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Croaghanmoira is situated in the far south-east corner of the Wicklow Mountains range, and sits on its own small massif with several other lesser but well known peaks, separated from the nearby larger massif of Lugnaquilla by the Laragh to Aghavannagh road; the summit of Croaghanmoira has a distinctive &quot;pyramidal&quot; profile. Naming.

Geographic entities mentioned:
surface_form: Lugnaquilla
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.966
lon: -6.463
surface_form: croaghanmoira
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.913888888889
lon: -6.3683333333333
surface_form: croaghanmoira
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.913888888889
lon: -6.3683333333333
Croaghanmoira. Croaghanmoira () at, is the 136th–highest peak in Ireland on the Arderin scale, and the 165th–highest peak on the Vandeleur-Lynam scale.

Geographic entities mentioned:
surface_form: arderin
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.03805556
lon: -7.65388889
surface_form: croaghanmoira
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.913888888889
lon: -6.3683333333333
Croaghanmoira's massif includes the northern subsidiary summit of Croaghanmoira North Top, which has a prominence of, thus qualifying it an Arderin Beg. Immediately to the east of Croaghanmoira is the summit of Ballinacor Mountain, which has a prominence of, thus qualifying it an Arderin.

Geographic entities mentioned:
surface_form: arderin
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.03805556
lon: -7.65388889
surface_form: croaghanmoira
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.913888888889
lon: -6.3683333333333
surface_form: croaghanmoira
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.913888888889
lon: -6.3683333333333
Croaghanmoira's massif includes the northern subsidiary summit of Croaghanmoira North Top, which has a prominence of, thus qualifying it an Arderin Beg. Immediately to the east of Croaghanmoira is the summit of Ballinacor Mountain, which has a prominence of, thus qualifying it an Arderin.

Geographic entities mentioned:
surface_form: arderin
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.03805556
lon: -7.65388889
surface_form: croaghanmoira
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.913888888889
lon: -6.3683333333333
Immediately to the east of Croaghanmoira is the summit of Ballinacor Mountain, which has a prominence of, thus qualifying it an Arderin. To the west of Croaghanmoira is the summit of Carrickashane Mountain, which has a prominence of, and thus also qualifies as an Arderin.

Geographic entities mentioned:
surface_form: arderin
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.03805556
lon: -7.65388889