Sarmila/GeoWiki-Features huggingface dataset:
The lava fountains could be seen in the south of the island, and a lava flow destroyed three farms near the village of Reykjahlíð, although nobody was harmed. Between 1975 and 1984, a series of volcanic events known as the Krafla fires took place within the Krafla caldera. There were nine volcanic eruptions and fifteen uplift and subsidence events.

Geographic entities mentioned:
surface_form: krafla
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.733333333333
lon: -16.783333333333
surface_form: krafla
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.733333333333
lon: -16.783333333333
During these events a large magma chamber was identified at depth by analysing the seismic activity. Some of the lava fountaining during these eruptions was caught on film by Maurice and Katia Krafft, and features in the 2022 film, Fire of Love. Since 1977 the Krafla area has been the source of the geothermal energy used by a 60 MWe power station.

Geographic entities mentioned:
surface_form: krafla
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.733333333333
lon: -16.783333333333
A survey undertaken in 2006 indicated very high temperatures at depths of between, and these favourable conditions led to the development of the first well from the Iceland Deep Drilling Project, IDDP-1, that found molten rhyolite magma deep beneath the surface in 2009. The Krafla fires interrupted some of the geothermal drilling work in the area. Krafla magma testbed.

Geographic entities mentioned:
surface_form: krafla
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.733333333333
lon: -16.783333333333
Krafla magma testbed. Following on from the encounter with molten rock during the drilling of IDDP-1, the Krafla Magma Testbed (KMT) concept has been developed, which envisages the creation of an 'international magma observatory' and further scientific drilling at Krafla in order to deliberately drill into the magma body.

Geographic entities mentioned:
surface_form: krafla
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.733333333333
lon: -16.783333333333
surface_form: krafla
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.733333333333
lon: -16.783333333333
One room, the Douglas library, is restored as a period room. There are more mining artifacts outside along with a picnic area offering a panoramic view of the Verde Valley & River, and the red rocks of Sedona–Oak Creek Canyon region. History. In 1962 the sons of Jimmy Douglas donated the Douglas Mansion to the State of Arizona. The Jerome State Historic Park opened in 1965.

Geographic entities mentioned:
surface_form: Verde Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.753055555555555
lon: -112.02194444444444
surface_form: Oak Creek Canyon
instance_of: Landform
countries: United States
coordinates: lat: 34.9125
lon: -111.727
Starling Dodd. Starling Dodd is a fell in the western part of the English Lake District, located between the valleys of Ennerdale and Buttermere, on the ridge between Great Borne to its west and Red Pike to its east. Not visible from Buttermere and rounded in profile, Starling Dodd is a relatively unfrequented top. Topography.

Geographic entities mentioned:
surface_form: Ennerdale
instance_of: Valley
countries: United Kingdom
surface_form: Buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: Great Borne
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.53435
lon: -3.35685
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.526
lon: -3.3
surface_form: starling dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.530180555556
lon: -3.32735
Not visible from Buttermere and rounded in profile, Starling Dodd is a relatively unfrequented top. Topography. The Western Fells occupy a triangular sector of the Lake District, bordered by the River Cocker to the north east and Wasdale to the south east. Westwards the hills diminish toward the coastal plain of Cumberland.

Geographic entities mentioned:
surface_form: Wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Westwards the hills diminish toward the coastal plain of Cumberland. At the central hub of the high country are Great Gable and its satellites, while two principal ridges fan out on either flank of Ennerdale, the western fells in effect being a great horseshoe around this long wild valley. Starling Dodd stands on the northern branch, dividing Buttermere and Ennerdale.

Geographic entities mentioned:
surface_form: Great Gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
Starling Dodd stands on the northern branch, dividing Buttermere and Ennerdale. The Buttermere–Ennerdale watershed runs north-west from Haystacks, climbing over High Crag, High Stile and Red Pike, the three fells of Buttermere Edge. The ridge then loses its craggy character, swinging westerly over the grassy Starling Dodd to its terminus at Great Borne.

Geographic entities mentioned:
surface_form: High Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.514638888889
lon: -3.2681388888889
surface_form: High Stile
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.521669444444
lon: -3.2838111111111
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
surface_form: haystacks
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.508
lon: -3.248
surface_form: high crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.514
lon: -3.0158
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.526
lon: -3.3
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
Starling Dodd stands on the northern branch, dividing Buttermere and Ennerdale. The Buttermere–Ennerdale watershed runs north-west from Haystacks, climbing over High Crag, High Stile and Red Pike, the three fells of Buttermere Edge. The ridge then loses its craggy character, swinging westerly over the grassy Starling Dodd to its terminus at Great Borne.

Geographic entities mentioned:
surface_form: Great Borne
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.53435
lon: -3.35685
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: starling dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.530180555556
lon: -3.32735
North of the summit dome, Starling Dodd levels into a wide plateau before disappearing over a steep rim of minor crags. At the base of this fall is the tenuous topographical connection to Mellbreak, a low watershed dividing Starling Dodd's northern drainage into widely differing catchments.

Geographic entities mentioned:
surface_form: Mellbreak
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.555438888889
lon: -3.3188888888889
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: starling dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.530180555556
lon: -3.32735
At the base of this fall is the tenuous topographical connection to Mellbreak, a low watershed dividing Starling Dodd's northern drainage into widely differing catchments. That to the west of the summit flows into the marshy valley of Mosedale, travelling all around Mellbreak to enter Crummock Water via Park Beck.

Geographic entities mentioned:
surface_form: Crummock Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.55
lon: -3.3
surface_form: mellbreak
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.555438888889
lon: -3.3188888888889
In recent years the posts have been removed from the stone cairn and an entirely metal cairn, looking like something out of the Tate Modern, has been constructed beside the original cairn. Ennerdale Water is well seen from the summit, with parts of the lakes of Crummock Water and Loweswater also visible.

Geographic entities mentioned:
surface_form: Loweswater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.5825
lon: -3.355277777777778
surface_form: crummock water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.55
lon: -3.3
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
The ridge then loses its craggy character, swinging westerly over the grassy Starling Dodd to its terminus at Great Borne. The western ridge of Red Pike swings down, away from the craggy Buttermere front of Ling Cove, and then rises to the subsidiary top of Little Dodd. This is generally considered to be a part of Red Pike, the territory of Starling Dodd beginning at the next depression westward.

Geographic entities mentioned:
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.526
lon: -3.3
The western ridge of Red Pike swings down, away from the craggy Buttermere front of Ling Cove, and then rises to the subsidiary top of Little Dodd. This is generally considered to be a part of Red Pike, the territory of Starling Dodd beginning at the next depression westward. A short climb on grass then leads to the summit, a rounded, but quite shapely grassy dome sitting atop a broad ridge.

Geographic entities mentioned:
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.526
lon: -3.3
surface_form: starling dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.530180555556
lon: -3.32735
Ennerdale Water is well seen from the summit, with parts of the lakes of Crummock Water and Loweswater also visible. High Stile hides part of the arc of the Western Fells, but Pillar and its neighbours make a fine panorama. The North Western Fells are also seen across Crummock Water. Ascents. Loweswater village can be used as a base, although this then requires a full traverse of marshy Mosedale.

Geographic entities mentioned:
surface_form: crummock water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.55
lon: -3.3
The North Western Fells are also seen across Crummock Water. Ascents. Loweswater village can be used as a base, although this then requires a full traverse of marshy Mosedale. Red Gill can then be followed to reach the plateau. The same point can also be reached from Buttermere village or Ennerdale by using Floutern Pass. This is not without bogs either.

Geographic entities mentioned:
surface_form: loweswater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.5825
lon: -3.355277777777778
Ennerdale Water is well seen from the summit, with parts of the lakes of Crummock Water and Loweswater also visible. High Stile hides part of the arc of the Western Fells, but Pillar and its neighbours make a fine panorama. The North Western Fells are also seen across Crummock Water. Ascents. Loweswater village can be used as a base, although this then requires a full traverse of marshy Mosedale.

Geographic entities mentioned:
surface_form: pillar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.497
lon: -3.282
surface_form: high stile
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.521669444444
lon: -3.2838111111111
Gentle slopes fall westward along the watershed, interrupted only by the slight rise of Gale Fell, a trivial summit listed only by Birkett. Rough grass on the facing slope leads up to the rockier environs of Great Borne. The southern flanks of Starling Dodd are heavily wooded below, part of the extensive conifer plantations of the Ennerdale Forest.

Geographic entities mentioned:
surface_form: great borne
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.53435
lon: -3.35685
Starling Dodd. Starling Dodd is a fell in the western part of the English Lake District, located between the valleys of Ennerdale and Buttermere, on the ridge between Great Borne to its west and Red Pike to its east. Not visible from Buttermere and rounded in profile, Starling Dodd is a relatively unfrequented top. Topography.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: starling dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.530180555556
lon: -3.32735
Starling Dodd. Starling Dodd is a fell in the western part of the English Lake District, located between the valleys of Ennerdale and Buttermere, on the ridge between Great Borne to its west and Red Pike to its east. Not visible from Buttermere and rounded in profile, Starling Dodd is a relatively unfrequented top. Topography.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: starling dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.530180555556
lon: -3.32735
Westwards the hills diminish toward the coastal plain of Cumberland. At the central hub of the high country are Great Gable and its satellites, while two principal ridges fan out on either flank of Ennerdale, the western fells in effect being a great horseshoe around this long wild valley. Starling Dodd stands on the northern branch, dividing Buttermere and Ennerdale.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
surface_form: starling dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.530180555556
lon: -3.32735
Rough grass on the facing slope leads up to the rockier environs of Great Borne. The southern flanks of Starling Dodd are heavily wooded below, part of the extensive conifer plantations of the Ennerdale Forest. Within the forest is Latterbarrow, a parallel lower ridge which diverts some of Starling Dodd's streams further west than might be expected.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
surface_form: starling dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.530180555556
lon: -3.32735
The southern flanks of Starling Dodd are heavily wooded below, part of the extensive conifer plantations of the Ennerdale Forest. Within the forest is Latterbarrow, a parallel lower ridge which diverts some of Starling Dodd's streams further west than might be expected. North of the summit dome, Starling Dodd levels into a wide plateau before disappearing over a steep rim of minor crags.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: starling dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.530180555556
lon: -3.32735
This is believed to be the highest single waterfall in the District, dropping around down a narrow cleft. Geology. The summit of Starling Dodd is formed by rocks of the Buttermere Formation, an olistostrome of disrupted, sheared and folded mudstone, siltstone and sandstone. Surrounding it on almost all sides are the granophyric granites of the Ennerdale Intrusion.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: starling dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.530180555556
lon: -3.32735
Wainwright's Pictorial Guides. In his concluding notes in the seventh and final volume of the Pictorial Guides to the Lakeland Fells, Wainwright wrote that Starling Dodd was the final fell he climbed during his research for the books. As such, some Wainwright-baggers save Starling Dodd to be their last Wainwright fell in honour of this.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: starling dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.530180555556
lon: -3.32735
That to the west of the summit flows into the marshy valley of Mosedale, travelling all around Mellbreak to enter Crummock Water via Park Beck. The north-eastern quarter takes a direct line into the lake, dropping down the craggy face via Scale Force. This is believed to be the highest single waterfall in the District, dropping around down a narrow cleft. Geology.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Ascents. Loweswater village can be used as a base, although this then requires a full traverse of marshy Mosedale. Red Gill can then be followed to reach the plateau. The same point can also be reached from Buttermere village or Ennerdale by using Floutern Pass. This is not without bogs either. Indirect ascents along the ridge from either direction are probably more common.

Geographic entities mentioned:
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
Geology. The summit of Starling Dodd is formed by rocks of the Buttermere Formation, an olistostrome of disrupted, sheared and folded mudstone, siltstone and sandstone. Surrounding it on almost all sides are the granophyric granites of the Ennerdale Intrusion. The steep northern slopes were the site of iron mines, operated in the late nineteenth century.

Geographic entities mentioned:
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
All work had ceased by 1877. Summit. The smooth grassy top once featured a sizeable cairn, reinforced by many iron posts and fittings salvaged from the Ennerdale Fence. In recent years the posts have been removed from the stone cairn and an entirely metal cairn, looking like something out of the Tate Modern, has been constructed beside the original cairn.

Geographic entities mentioned:
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
Crazywell Pool. Crazywell Pool or Crazy Well Pool is a large pond situated about south of Princetown just off the path between Burrator and Whiteworks on the western side of Dartmoor, Devon, England at. It is about long and has a surface area of about. The pool is thought to be the result of excavations by tin miners, and is either a flooded mine shaft, or a reservoir.

Geographic entities mentioned:
surface_form: crazywell pool
instance_of: Lake
countries: United Kingdom
coordinates: lat: 50.517061
lon: -4.0015
Crazywell Pool. Crazywell Pool or Crazy Well Pool is a large pond situated about south of Princetown just off the path between Burrator and Whiteworks on the western side of Dartmoor, Devon, England at. It is about long and has a surface area of about. The pool is thought to be the result of excavations by tin miners, and is either a flooded mine shaft, or a reservoir.

Geographic entities mentioned:
surface_form: crazywell pool
instance_of: Lake
countries: United Kingdom
coordinates: lat: 50.517061
lon: -4.0015
surface_form: crazy well pool
instance_of: Lake
countries: United Kingdom
coordinates: lat: 50.517061
lon: -4.0015
Near to the pool is Crazywell Cross, one of the line of crosses that marked the ancient track between Buckfast Abbey and Tavistock Abbey. In 1998, Nathaniel Burton, a sixteen-year-old recruit in the Royal Marines, died in Crazywell Pool. He was taking part in a routine training exercise and drowned while crossing the icy waters of the pool. Legends.

Geographic entities mentioned:
surface_form: crazywell pool
instance_of: Lake
countries: United Kingdom
coordinates: lat: 50.517061
lon: -4.0015
Legends. There are no natural lakes on Dartmoor, which may be one reason why Crazywell Pool has attracted more than its share of local legends. It was once believed to be bottomless, and according to local legend the parishioners of Walkhampton (or Sheepstor) brought up the bell ropes from the parish church to test its depth.

Geographic entities mentioned:
surface_form: crazywell pool
instance_of: Lake
countries: United Kingdom
coordinates: lat: 50.517061
lon: -4.0015
The reality is that the pool is about deep at the western end and considerably less at the eastern end. Crazywell Pool is the subject of other Dartmoor superstitions.

Geographic entities mentioned:
surface_form: crazywell pool
instance_of: Lake
countries: United Kingdom
coordinates: lat: 50.517061
lon: -4.0015
Kivu Lacus. Kivu Lacus is a small Titanean hydrocarbon lake. It was discovered by the Cassini probe. The lake is near Titan's north pole and is named after Lake Kivu in the Democratic Republic of Congo and Rwanda. In 2012, Cassini spotted an Infrared glint off the lake. The aspects of it suggested waves.

Geographic entities mentioned:
surface_form: Lake Kivu
instance_of: Lake
countries: Democratic Republic of the Congo
Rwanda
coordinates: lat: -1.8530555555556
lon: 29.135277777778
Most of the housing developments in Bønestoppen date to the early 1990s, having been built following the construction of a new road connecting Bønes and Fyllingsdalen. Formerly having been part of Løvstakken borough, it became part of Fyllingsdalen borough after the reform of 2000.

Geographic entities mentioned:
surface_form: Løvstakken
instance_of: Mountain
countries: Norway
coordinates: lat: 60.36130278
lon: 5.31916111
It was formerly in the historic county of Caernarvonshire. At the 2001 census, it had a population of 1,200, increasing to 1,292 at the 2011 census. It includes a large part of the Carneddau range including the lakes of Llyn Eigiau, Llyn Dulyn and Llyn Melynllyn. Features. Surrounding the 14th-century parish church of St. Mary are the banks of the Roman fort of Canovium.

Geographic entities mentioned:
surface_form: Carneddau
instance_of: Landform
countries: United Kingdom
coordinates: lat: 53.18114
lon: -4.00297
The Rashtriya Swayamsevak Sangh was established in Jammu in 1939 with the efforts of Kishen Dev Joshi. Jagdish Abrol and later Balraj Madhok, who arrived in 1942, are credited with its expansion. Madhok moved to the Kashmir Valley in 1944 and established RSS there. Prem Nath Dogra was also the chairman (&quot;sanghchalak&quot;) of the RSS in Jammu.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
The city is the capital of both the Arica Province and the Arica and Parinacota Region. Arica is located at the bend of South America's western coast known as the Arica Bend or Arica Elbow. At the location of the city are two valleys that dissect the Atacama Desert converge: Azapa and Lluta. These valleys provide citrus and olives for export.

Geographic entities mentioned:
surface_form: Azapa
instance_of: Valley
countries: Chile
coordinates: lat: -18.51722222
lon: -70.19194444
At the time of the Spanish settlement the region around Arica was already multiethnic displaying a mix of local sedentary populations and mitma settlers from the Altiplano. The proportions of these are that the first made up about 66% of the population and the latter 25%. The remaining 9% were fishing-oreinted people known as Camanchacos.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
It was attacked and captured on 7 June 1880 by Chilean troops, as the final effort of their &quot;Campaña del Desierto&quot; (Desert Campaign) during the War of the Pacific. Near to the city center is the Azapa Valley, an oasis where vegetables and, famously, Azapa olives are grown. Economically, it is also an important port for Chilean ore.

Geographic entities mentioned:
surface_form: Azapa Valley
instance_of: Valley
countries: Chile
coordinates: lat: -18.51722222
lon: -70.19194444
Geography. The canyon is traversed via Coldwater Canyon Drive and Coldwater Canyon Avenue (linked by a short section of Mulholland Drive), which connects the city of Beverly Hills and the Westside, with the Studio City neighborhood and the San Fernando Valley. The canyon is drained Coldwater Canyon Creek, a tributary of Ballona Creek.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Cizanye River. The Cizanye River () is a river in Burundi, a tributary of the Rurubu River. Course. The Cizanye River flows northeast through Muyinga Province to the border with Tanzania. Near the border it is joined from the right by the Rugobe River. It then turns east and defines the border to its mouth on the Ruvubu River, which leaves Burundi at this point. Marshes.

Geographic entities mentioned:
surface_form: cizanye river
instance_of: Watercourse
countries: Burundi
coordinates: lat: -2.654
lon: 30.5274
Marshes. As of 2014 there was a rehabilitated managed marsh on the Cizanye near Kobero, Commune of Butihinda, Muyinga Province, and a unmanaged marsh in the Commune of Muyinga. In July 2018 Déo Guide Rurema, Burundian Minister of Agriculture, launched the &quot;C&quot; growing season in the Commune of Butihinda in the Cizanye marsh.

Geographic entities mentioned:
surface_form: cizanye
instance_of: Watercourse
countries: Burundi
coordinates: lat: -2.654
lon: 30.5274
Groundwater-related subsidence often results in major damage to urban areas. United States. In the San Joaquin Valley of the United States, groundwater pumping for crops has gone on for generations. This has resulted in the entire valley sinking an extraordinary amount, as shown in the figure. This has not come without consequences.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
The entire East Coast has been sinking.Damage from Hurricane Katrina was exacerbated due to coastal sinking, associated with groundwater withdrawal. Major areas affected include the San Joaquin Valley in California, Central Arizona, Kansas which uses irrigation to grow corn and Arkansas which produces 50% of US rice. Between the 1950s and 1990s, Phoenix had a sunsidence drop of. Mexico.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Very little information of his life is known that is not even accurate as to the people to whom he belonged. It is only known that Nabati graduated from high school, spent his youth in Arasbaran, later visited the tomb of Sheikh Shahabaddin in Ahar, after which he returned to his native Ushtibin, where he lived until his death.

Geographic entities mentioned:
surface_form: Arasbaran
instance_of: Mountain
countries: Iran
coordinates: lat: 38.74
lon: 46.7
Work on the dam and water network was complete in May 1931. A year after inauguration, the Boyati Tunnel was transferring per second of water treated at the Galatsi Water Treatment Plant to Athens. The dam would serve as the primary water supply for Athens until 1959, when water was pumped from Yliki lake. Seismicity.

Geographic entities mentioned:
surface_form: Yliki lake
instance_of: Lake
countries: Greece
coordinates: lat: 38.4
lon: 23.26666667
Wu River (Wei River tributary). Wu River (), originates in Xiangxiang City, is long, and drains a basin of. It is the fourth largest river in Ningxiang City and one of the largest tributaries of the Wei River. Wu River has 68 tributaries.

Geographic entities mentioned:
surface_form: wu river
instance_of: Watercourse
countries: People's Republic of China
coordinates: lat: 27.11806
lon: 110
surface_form: wu river (wei river tributary)
instance_of: Watercourse
countries: People's Republic of China
coordinates: lat: 28.1854
lon: 112.54
Wu River (Wei River tributary). Wu River (), originates in Xiangxiang City, is long, and drains a basin of. It is the fourth largest river in Ningxiang City and one of the largest tributaries of the Wei River. Wu River has 68 tributaries.

Geographic entities mentioned:
surface_form: wu river
instance_of: Watercourse
countries: People's Republic of China
coordinates: lat: 27.11806
lon: 110
Wu River (), originates in Xiangxiang City, is long, and drains a basin of. It is the fourth largest river in Ningxiang City and one of the largest tributaries of the Wei River. Wu River has 68 tributaries. The river passes places such as Huitang Town, Xieleqiao Town, Zifu Town, Nantianping Town, Batang Town, and Lijingpu Township, and empties into the Wei River in Nantai Lake ().

Geographic entities mentioned:
surface_form: wu river
instance_of: Watercourse
countries: People's Republic of China
coordinates: lat: 27.11806
lon: 110
In 1906, Huntington, Frank Miller (owner of the Mission Inn), and Charles M. Loring formed the &quot;Huntington Park Association&quot;. Their intention was to purchase Mount Rubidoux in Riverside, build a road to the summit, and develop the hill as a park to benefit the city of Riverside. The road was completed in February 1907.

Geographic entities mentioned:
surface_form: Mount Rubidoux
instance_of: Mountain
countries: United States
coordinates: lat: 33.9839
lon: -117.393
Huntington Middle School in San Marino, and Huntington Drive running eastbound from downtown Los Angeles. Riverside's city park on Mount Rubidoux was originally named Huntington Park, and the road to the top was named Huntington Drive. Frank Miller's heirs donated the property to the city; the city renamed the park the Frank A.

Geographic entities mentioned:
surface_form: Mount Rubidoux
instance_of: Mountain
countries: United States
coordinates: lat: 33.9839
lon: -117.393
With the Ripogenus Dam by Chesuncook Lake, the West Branch is able to sustain the large landlocked salmon found there, with twelve miles of heavy rapids, deep runs, large pools, and slower moving water in some sections. Baxter State Park is located to the north. Some of the river's rapids are class IV or even V, making this one of the roughest rivers in the area, and attracting whitewater rafters.

Geographic entities mentioned:
surface_form: Chesuncook Lake
instance_of: Lake
countries: United States
coordinates: lat: 45.987222222222
lon: -69.340833333333
Maloney also competed for the University of California, Los Angeles in the NCAA from 2001 until 2005. Early life. Maloney was born on March 10, 1981, in Hackettstown, New Jersey and attended Pen Argyl Area High School in Pen Argyl, Pennsylvania in the Lehigh Valley region of eastern Pennsylvania. Gymnastics career.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Cornell Road. Cornell Road is an east–west street and traffic corridor in the Portland metropolitan area, in Multnomah and Washington counties in the U.S. state of Oregon. It crosses the Tualatin Mountains (West Hills) between the Willamette Valley and the city of Portland on the east and the Tualatin Valley and the city of Hillsboro on the west.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
surface_form: Tualatin Valley
instance_of: Valley
countries: United States
coordinates: lat: 45.5106
lon: -122.989
General Ved Prakash Malik, the then Chief of Army Staff, called to congratulate him. All across the nation, his triumph was being played out on television screens. On 26 June, shortly after the capture of Point 5140, 13 JAK Rif was ordered to move from Dras to Ghumri to rest, refit, and recoup. The battalion then moved to Mushkoh Valley on 30 June. Capture of Point 4875.

Geographic entities mentioned:
surface_form: Mushkoh Valley
instance_of: Valley
countries: India
coordinates: lat: 34.43
lon: 75.66
Raikot, Pakistan. Raikot (,) is a village in Diamer district, Gilgit-Baltistan, Pakistan. It is famous for hosting the Raikot Bridge. It is situated along the Indus River. Tourism. There are many restaurants and hotels in Raikot and is a route to Nanga Parbat. One of the most famous hotels is &quot;Raikot Serai&quot;. It also in the Fairy Meadows area, a base camp for Nanga Parbat.

Geographic entities mentioned:
surface_form: Nanga Parbat
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.239166666667
lon: 74.59
It is a tilted, heavily eroded plateau, with a deep canyon in its central portion (Cañón Grande), drained by the Baria River. Most of the massif is in Venezuelan territory, but its southeastern ridge forms part of the Brazil–Venezuela border, and this ridge is where the highest point in the massif, Pico da Neblina, is located.

Geographic entities mentioned:
surface_form: Pico da Neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.80549444444444
lon: -66.005358333333
surface_form: pico da neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.80549444444444
lon: -66.005358333333
surface_form: neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.80549444444444
lon: -66.005358333333
surface_form: brazil–venezuela border
instance_of: Landform
countries: Brazil
Venezuela
coordinates: lat: 1.2277777777778
lon: -66.869444444444
Pico da Neblina is inside Brazilian territory, but only a few hundred metres from the Venezuelan border. The slightly lower Pico 31 de Março or Pico Phelps, a.s.l., lies next to Pico da Neblina, on the precise international border. Pico 31 de Março/Phelps is Brazil's second-highest mountain and the highest in Venezuela outside of the Andes.

Geographic entities mentioned:
surface_form: Pico 31 de Março or Pico Phelps
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.8
lon: -66
surface_form: pico da neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.80549444444444
lon: -66.005358333333
surface_form: neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.80549444444444
lon: -66.005358333333
surface_form: pico 31 de março
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.8
lon: -66
surface_form: pico 31 de março
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.8
lon: -66
surface_form: pico phelps
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.8
lon: -66
Pico 31 de Março/Phelps is Brazil's second-highest mountain and the highest in Venezuela outside of the Andes. The massif's other named peaks include Pico Cardona, Pico Maguire, and Pico Zuloaga. To the north of Cerro de la Neblina lie the smaller outcrops of Cerro Aracamuni and Cerro Avispa, both reaching approximately in elevation.

Geographic entities mentioned:
surface_form: Cerro Avispa
instance_of: Mountain
countries: Venezuela
coordinates: lat: 1.33611111
lon: -65.87888889
surface_form: la neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.80549444444444
lon: -66.005358333333
surface_form: cerro de la neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.80549444444444
lon: -66.005358333333
surface_form: neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.80549444444444
lon: -66.005358333333
surface_form: cerro de la neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.88638889
lon: -65.98944444
Most of the massif is in Venezuelan territory, but its southeastern ridge forms part of the Brazil–Venezuela border, and this ridge is where the highest point in the massif, Pico da Neblina, is located. At above sea level, Pico da Neblina is also the highest point in Brazil, the highest point in the Guiana Shield, and the highest South American mountain east of the Andes.

Geographic entities mentioned:
surface_form: pico da neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.80549444444444
lon: -66.005358333333
surface_form: pico da neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.80549444444444
lon: -66.005358333333
surface_form: neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.80549444444444
lon: -66.005358333333
surface_form: neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.80549444444444
lon: -66.005358333333
Cerro de la Neblina. Cerro de la Neblina (lit. &quot;Mountain of the Mist&quot;), also known as Serra da Neblina in Brazil and Sierra de la Neblina in Venezuela, is a sandstone massif located in the northern Amazon Basin. It is a tilted, heavily eroded plateau, with a deep canyon in its central portion (Cañón Grande), drained by the Baria River.

Geographic entities mentioned:
surface_form: la neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.80549444444444
lon: -66.005358333333
surface_form: cerro de la neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.80549444444444
lon: -66.005358333333
surface_form: neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.80549444444444
lon: -66.005358333333
surface_form: cerro de la neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.88638889
lon: -65.98944444
Cerro de la Neblina. Cerro de la Neblina (lit. &quot;Mountain of the Mist&quot;), also known as Serra da Neblina in Brazil and Sierra de la Neblina in Venezuela, is a sandstone massif located in the northern Amazon Basin. It is a tilted, heavily eroded plateau, with a deep canyon in its central portion (Cañón Grande), drained by the Baria River.

Geographic entities mentioned:
surface_form: la neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.80549444444444
lon: -66.005358333333
surface_form: neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.80549444444444
lon: -66.005358333333
surface_form: neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.80549444444444
lon: -66.005358333333
surface_form: serra da neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.88638889
lon: -65.98944444
surface_form: sierra de la neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.88638889
lon: -65.98944444
The massif was first explored in 1954 by an American expedition led by Bassett Maguire of the New York Botanical Garden that performed an aerial inspection and then climbed the massif's northwestern slopes. The Neblina–Aracamuni Massif has a total summit area of roughly and an estimated slope area of, of which Cerro de la Neblina accounts for and, respectively.

Geographic entities mentioned:
surface_form: la neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.80549444444444
lon: -66.005358333333
surface_form: cerro de la neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.80549444444444
lon: -66.005358333333
surface_form: neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.80549444444444
lon: -66.005358333333
surface_form: cerro de la neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.88638889
lon: -65.98944444
Hahnfjella. Hahnfjella is a mountain group in Sabine Land at Spitsbergen, Svalbard, west of the bay of Wichebukta. It is named after German geographer Friedrich Gustav Hahn. The highest mountain of the group reaches 537 m.a.s.l.

Geographic entities mentioned:
surface_form: hahnfjella
instance_of: Mountain
countries: Norway
coordinates: lat: 78.414
lon: 18.975
The project was one of the first to be developed by the Reclamation Service, which later became the Bureau of Reclamation. The two main water supply sources for the project are Upper Klamath Lake and the Klamath River. The main bodies of water in the Klamath Project are Clear Lake Reservoir, Klamath River, Link River, Lost River, Lower Klamath Lake, Tule Lake, and Upper Klamath Lake.

Geographic entities mentioned:
surface_form: Upper Klamath Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.392222222222
lon: -121.88027777778
The project was one of the first to be developed by the Reclamation Service, which later became the Bureau of Reclamation. The two main water supply sources for the project are Upper Klamath Lake and the Klamath River. The main bodies of water in the Klamath Project are Clear Lake Reservoir, Klamath River, Link River, Lost River, Lower Klamath Lake, Tule Lake, and Upper Klamath Lake.

Geographic entities mentioned:
surface_form: Lower Klamath Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.99083983333333
lon: -121.74309983333333
surface_form: Tule Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.909322222222
lon: -121.53304722222
The Provisional Government of Hawaii under Sanford B. Dole passes a law which would forcibly relocate lepers to the Leprosy Colony of Kalawao on the Kalaupapa peninsula. When Kaluaikoolau, a leper, resisted arrest by a deputy sheriff and killed the man, Dole reacted by sending armed militia against the lepers of Kalalau Valley. Kaluaikoolau reportedly foiled or killed some of his pursuers.

Geographic entities mentioned:
surface_form: Kalalau Valley
instance_of: Valley
countries: United States
coordinates: lat: 22.18
lon: -159.65361111
The expedition descended into wanton violence against the local population and ended in sedition on the part of the commanders. In 1898, the Battle of Sugar Point takes place in the northeast shore of Leech Lake, Minnesota. &quot;Old Bug&quot; (Bugonaygeshig), a leading member of the Pillager Band of Chippewa Indians in Bear Island had been arrested in September 1898.

Geographic entities mentioned:
surface_form: Leech Lake
instance_of: Lake
countries: United States
coordinates: lat: 47.166666666667
lon: -94.366666666667
Lavender Mountain. Lavender Mountain is a summit in the U.S. state of Georgia. The elevation is. Lavender Mountain was named after George Michael Lavender, a local merchant.

Geographic entities mentioned:
surface_form: lavender mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.335277777778
lon: -85.244722222222
The school is now a boy's boarding school delivering the 8-4-4 syllabus which is tested nationwide by the Kenya National Examination Council. Location. The school is located about from Karatina, on the foot of Mount Kenya. The locality experiences a cool weather round the year. The terrain is a hilly one which makes the area suitable for tea growing. Curriculum.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
To the north, it faces Deer Leap Mountain across Sherburne Pass. Seen from the pass, the summit of Pico Peak resembles a cone. Pico Peak is the northernmost mountain of the Coolidge Range, and the second highest mountain in that range after Killington Peak. In 1927 the State Legislature named the Coolidge Range after Vermont native Calvin Coolidge.

Geographic entities mentioned:
surface_form: Killington Peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.604444444444
lon: -72.82
surface_form: pico peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.639333333333
lon: -72.836333333333
The southeast side of Pico drains into Roaring Brook, and thence into the Ottauquechee. The northwest side of Pico drains into Mendon Brook, thence into East Creek, Otter Creek, and Lake Champlain, which drains via the Saint Lawrence River into the Gulf of St. Lawrence in Quebec, Canada. The southwest side of Pico drains into Brewer's Brook, and thence into Mendon Brook.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Pico Peak. Pico Peak is a mountain in the Green Mountains in Rutland County, Vermont, United States. Pico Peak is flanked to the south by Ramshead Peak. To the north, it faces Deer Leap Mountain across Sherburne Pass. Seen from the pass, the summit of Pico Peak resembles a cone.

Geographic entities mentioned:
surface_form: pico peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.639333333333
lon: -72.836333333333
Pico Peak is a mountain in the Green Mountains in Rutland County, Vermont, United States. Pico Peak is flanked to the south by Ramshead Peak. To the north, it faces Deer Leap Mountain across Sherburne Pass. Seen from the pass, the summit of Pico Peak resembles a cone. Pico Peak is the northernmost mountain of the Coolidge Range, and the second highest mountain in that range after Killington Peak.

Geographic entities mentioned:
surface_form: pico peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.639333333333
lon: -72.836333333333
In 1927 the State Legislature named the Coolidge Range after Vermont native Calvin Coolidge. The range runs between Pico Peak and the town of Plymouth, where Coolidge grew up. The peak's name may stem from the Abenaki for &quot;the pass/opening&quot; or indeed from the Spanish or Portuguese word for &quot;peak&quot;, &quot;Pico&quot;.

Geographic entities mentioned:
surface_form: pico peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.639333333333
lon: -72.836333333333
The peak's name may stem from the Abenaki for &quot;the pass/opening&quot; or indeed from the Spanish or Portuguese word for &quot;peak&quot;, &quot;Pico&quot;. &quot;Pico Peak&quot; appears on the 1869 Beers Atlas of Rutland County, Walling's 1860 Map of the State of Vermont and Chace's 1854 Map of Rutland County (albeit reversed with Killington Peak).

Geographic entities mentioned:
surface_form: pico peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.639333333333
lon: -72.836333333333
Pico Peak and of forest were presented to Mortimer R. Proctor as a birthday present in 1910. He sold the mountain to Pico Ski Inc. in 1948. Pico Mountain ski area — part of Killington Ski Resort since December 1997 — is located on the northwest side of Pico Peak, with its base lodge on U.S. Route 4. Pico opened in 1937, and the first T-bar lift in the United States was installed there in 1940.

Geographic entities mentioned:
surface_form: pico peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.639333333333
lon: -72.836333333333
It has year-round road access. The reserve is located in the traditional territory of the people of &quot;Kwesawék Amlamkuk&quot;, which roughly translated from the Míkmaq language means &quot;the delta where the multicoloured rivers meet&quot;. That description is based on the original location of the Fort Folly reserve at Beaumont on the Petitcodiac River.

Geographic entities mentioned:
surface_form: Petitcodiac River
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.926944444444
lon: -65.188888888889