Sarmila/GeoWiki-Features huggingface dataset:
Haukedalen. Haukedalen is a village in Sunnfjord Municipality in Vestland county, Norway. The village is located in the Haukedalen valley at the northwestern end of the lake Haukedalsvatnet. The village lies in a fairly remote valley surrounded by the Gaularfjellet mountains. The town of Førde lies about to the west. Haukedalen Church is located in the village.

Geographic entities mentioned:
surface_form: Gaularfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 61.33861111
lon: 6.40361111
Mount Gerizim Temple. The Mount Gerizim Temple was an ancient Samaritan center of worship located on Mount Gerizim originally constructed in the mid-5th century BCE, reconstructed in the early 2nd century BCE, and destroyed later in that same century.

Geographic entities mentioned:
surface_form: Mount Gerizim
instance_of: Mountain
countries: State of Palestine
coordinates: lat: 32.199444444444
lon: 35.272777777778
After the cyclone dissipated, showers and gusty winds continued to occur on Midway and Kure for a few more days. Tropical Depression Dolly. After making landfall along the Bay of Campeche coast north of Tuxpan, Veracruz, Hurricane Dolly managed to maintain its tropical characteristics while crossing the Mexican Plateau, and entered the eastern Pacific as a tropical depression late on August 24.

Geographic entities mentioned:
surface_form: Mexican Plateau
instance_of: Plateau
countries: Mexico
coordinates: lat: 24
lon: -103
Linzor. Volcán Linzor is a stratovolcano on the border between Bolivia and Chile. In its vicinity lie Laguna Colorada and Cerro del León. Regional. Since the late Oligocene, subduction of the Nazca Plate beneath the South America Plate has caused volcanism on the western edge of South America, including the formation of the Central Volcanic Zone.

Geographic entities mentioned:
surface_form: Laguna Colorada
instance_of: Lake
countries: Bolivia
coordinates: lat: -22.198611111111
lon: -67.781111111111
surface_form: Cerro del León
instance_of: Mountain
countries: Chile
coordinates: lat: -22.15
lon: -68.116666666667
Linzor. Volcán Linzor is a stratovolcano on the border between Bolivia and Chile. In its vicinity lie Laguna Colorada and Cerro del León. Regional. Since the late Oligocene, subduction of the Nazca Plate beneath the South America Plate has caused volcanism on the western edge of South America, including the formation of the Central Volcanic Zone.

Geographic entities mentioned:
surface_form: volcán linzor
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.15
lon: -67.966666666667
surface_form: linzor
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.15
lon: -67.966666666667
Linzor. Volcán Linzor is a stratovolcano on the border between Bolivia and Chile. In its vicinity lie Laguna Colorada and Cerro del León. Regional. Since the late Oligocene, subduction of the Nazca Plate beneath the South America Plate has caused volcanism on the western edge of South America, including the formation of the Central Volcanic Zone.

Geographic entities mentioned:
surface_form: linzor
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.15
lon: -67.966666666667
The most important two form the Arequipa-Antofalla crustal domain. Local. Linzor volcano is part of the Central Volcanic Zone. The Andean Central Volcanic Zone has erupted large ignimbrites and lava flows. Dominant rocks are andesite and dacite.

Geographic entities mentioned:
surface_form: linzor
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.15
lon: -67.966666666667
Dominant rocks are andesite and dacite. One part of the Central Volcanic Zone is the Altiplano-Puna volcanic complex, a system of ignimbrite sheets and lava domes that was active between 8.4 and 2.9 million years ago and is underpinned by a layer of partially molten crust. In the Linzor area, volcanism is represented by the 8.3 million years old Sifon ignimbrite, Cerro Chillahuita and Cerro Chao.

Geographic entities mentioned:
surface_form: linzor
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.15
lon: -67.966666666667
In the Linzor area, volcanism is represented by the 8.3 million years old Sifon ignimbrite, Cerro Chillahuita and Cerro Chao. Linzor and other volcanoes in the neighbourhood are constructed by breccia, lava domes, lava flows, pyroclastic flows and breccia. The volcanoes are formed by basaltic andesite, andesite and dacite. Pyroxene andesite is the dominant component.

Geographic entities mentioned:
surface_form: linzor
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.15
lon: -67.966666666667
Pyroxene andesite is the dominant component. The volcanoes are constructed on top of Miocene ignimbrites and are of Pleistocene-Holocene age. An Inca sanctuary has been found on Linzor. Linzor is part of a north-south trending volcanic chain with San Pedro volcano which was heavily glaciated in the past. This chain is parallel to several Paleozoic faults in the region.

Geographic entities mentioned:
surface_form: linzor
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.15
lon: -67.966666666667
An Inca sanctuary has been found on Linzor. Linzor is part of a north-south trending volcanic chain with San Pedro volcano which was heavily glaciated in the past. This chain is parallel to several Paleozoic faults in the region. The Rio Toconce, a tributary of the Rio Salado and ultimately of the Loa River, originates at the foot of Linzor.

Geographic entities mentioned:
surface_form: linzor
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.15
lon: -67.966666666667
There's also abbess &quot;Čika's horologion&quot; (1066). In Vatican there is a &quot;Osor Evangeliary&quot;, also in Monte Cassino Benedictine style (initials of intertwined leaves, interlace and animal heads. The same style of illumination we can found in Breviars in Trogir, Šibenik and Dubrovnik but there are many that were recorded (like 28 books in only one church in monastery of St.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
Kuchmyn Yar Street. Kuchmyn Yar Street is a street located in the Batyieva Hora neighborhood of Solomianskyi District, Kyiv, Ukraine. It is located between Petra Krivonosa Square and Rozdilna street. The street was founded in the 19th century as Kuchmyn Yar Lane. In 1926, it was renamed to Markelova Lane in honor of a worker who died during the January Uprising of 1918.

Geographic entities mentioned:
surface_form: Batyieva Hora
instance_of: Mountain
countries: Ukraine
coordinates: lat: 50.42945
lon: 30.49480833
The uphill approach to the finish on Montjuïc did not suit some of the sprinters, but there was a group of about 60 at the head of the field when Millar was caught near the 1 km red flag, and with some GC contenders and climbers contesting the finish, Thor Hushovd emerged as stage winner.

Geographic entities mentioned:
surface_form: Montjuïc
instance_of: Mountain
countries: Spain
coordinates: lat: 41.364166666667
lon: 2.1580555555556
Golodass. Golodass&quot;Gol&quot; means Rivine and &quot;Das&quot; means Barren Land in Khowar Language, is a village situated In District Ghizer, Punial tehsil, Gilgit Baltistan. This village is at two hours distance from Gilgit City towards north west on inshkoman road. Golodass has an enriched culture with a diverse society.

Geographic entities mentioned:
surface_form: Punial
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.0852
lon: 74.041
Raja Mir Aman Khan came here in 1960 and started to run its first school as only teacher in the village. The Residents of the village are all migrants from different parts of Gilgit region including Yasin, Phander Valley, Hunza, Punial region, Gupis, Darel, Chilas, and other areas. Due to different backgrounds, there are a mixture of culture and languages in the village. History.

Geographic entities mentioned:
surface_form: Yasin
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.367777777777775
lon: 73.33777777777777
surface_form: Hunza
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.31666667
lon: 74.65
surface_form: Punial region
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.0852
lon: 74.041
Until the 14th century the abbey had possessions in the whole of Italy, making its cartulary significant beyond local level. However, it later declined due to impoverishment of the neighbouring area due to the retreat of the sea front and the increasing presence of malaria of the lower Po valley.

Geographic entities mentioned:
surface_form: Po valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
Záruby. Záruby is the highest hill of the Little Carpathians in Slovakia. It is located at an altitude of 767 m above sea level, near the village of Smolenice. It is a monoclinal crest.

Geographic entities mentioned:
surface_form: záruby
instance_of: Mountain
countries: Slovakia
coordinates: lat: 48.523569444444
lon: 17.391666666667
Geography. According to the United States Census Bureau, the town has a total area of, of which is land and (35.15%) is water. The town borders Oneida Lake and the western town line is the border of Oswego County. The Erie Canal is on the southern border, near Sylvan Beach. Fish Creek defines part of the eastern town line and joins the Erie Canal near Sylvan Beach. Demographics.

Geographic entities mentioned:
surface_form: Oneida Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.2
lon: -75.9
The Holy Synod established two new metropolises: a) The Holy Metropolis of Apollonia and Fier, which includes the district of Fier, the area of Patos and Libofsha, detached from the Metropolitanate of Berat, Kaninë and Vlora; b) The Holy Metropolis of Elbasan, which includes the areas of Elbasan, Shpat and Librazhd, separated from the Archdiocese of Tirana and Durrës.

Geographic entities mentioned:
surface_form: Shpat
instance_of: Mountain
countries: Albania
coordinates: lat: 41.02917
lon: 20.25806
They both spoke a northern Iranian dialect that was mostly unintelligible with Persian. The Cadusii, who had mixed with Gilaks, lived from the Caspian coast into the mountains. Mazandaran was populated by the Amardi and Tapur tribe, who had intermingled.

Geographic entities mentioned:
surface_form: Caspian coast
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Sargochromis. &quot;Sargochromis&quot; is a genus of haplochromine cichlids native to freshwater habitats in Southern Africa, where found in the upper and middle Zambezi basin, Okavango delta, Cunene basin, Cuvelai basin and southeastern Congo Basin. They are typically known as happies (a name also used for some other haplocromines) or smallmouths.

Geographic entities mentioned:
surface_form: Okavango delta
instance_of: Body of water
Watercourse
countries: Botswana
coordinates: lat: -19.4
lon: 22.9
Beinn Eilideach. Beinn Eilideach (mountain of hinds) is a mountain near Ullapool in Ross-shire in the Scottish Highlands. It is 559 metres high, and listed as a Marilyn. It has a triangulation pillar near the summit, though the highest point is actually 100 metre away to the west of this.

Geographic entities mentioned:
surface_form: pillar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.497
lon: -3.282
Beinn Eilideach. Beinn Eilideach (mountain of hinds) is a mountain near Ullapool in Ross-shire in the Scottish Highlands. It is 559 metres high, and listed as a Marilyn. It has a triangulation pillar near the summit, though the highest point is actually 100 metre away to the west of this.

Geographic entities mentioned:
surface_form: beinn eilideach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.885919
lon: -5.087314
Early life. Aleksandrs Laime was born on July 9, 1911, in Riga. He grew up in Grīziņkalns neighborhood, and since early childhood was interested in adventure stories and shipping. At the age of 15, he learned basic principles of sailing in Ķīšezers. Together with some friends, they stole a sailboat and traveled to Liepāja.

Geographic entities mentioned:
surface_form: Ķīšezers
instance_of: Lake
countries: Latvia
coordinates: lat: 57.0226
lon: 24.172
Etymology. The barony takes its name from the villages of Kilkea (&quot;Cill Cathaigh&quot;, &quot;Cathac's church&quot;) and Moone (&quot;Maen Colmcille&quot;, &quot;Colm Cille's property&quot;). Location. Kilkea and Moone is located in southern County Kildare, reaching from Mullaghmast to the southern tip of the county, east of the Barrow and west of Sherriff Hill. History.

Geographic entities mentioned:
surface_form: Mullaghmast
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.01685
lon: -6.81203889
The rift failed, then crustal movement reversed. A range formed then eroded, forming basins on either side of a horst. These rocks have been buried beneath sediment in many areas, but are exposed in some areas, especially around Lake Superior. Grenville Orogen. The Grenville Orogen developed during the Proterozoic along eastern and southern margin of the North American Craton.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Grenville Orogen. The Grenville Orogen developed during the Proterozoic along eastern and southern margin of the North American Craton. The largest outcrop of Grenville age rocks is an approximately wide band southeast of the Grenville Front which stretches from the central Labrador coast southwest across southern Quebec and southeastern Ontario to Georgian Bay on Lake Huron.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
The center of the range is a pair of provinces running north and south parallel to each other, the eastern Blue Ridge Province and the western Valley and Ridge provinces. These are surrounded by the Appalachian Plateau on the west, and the Piedmont Province to the east. Faulting extends throughout the region and is caused by numerous spatially and temporally varied sources.

Geographic entities mentioned:
surface_form: Appalachian Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 40
lon: -78
The lithology of the Rocky Mountains in western Canada includes a thin-skinned fold and thrust belt involving Neoproterozoic through Mississippian series of carbonates, shales, argillites and sandstones. The Colorado Plateau is a stable region dating back at least 600 million years. As a relative lowland, it had been a site of deposition for sediments eroded from surrounding mountain regions.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
Southern Cordillera. The Sierra Madre mountain ranges of Mexico are separated by the Mexican Plateau, and transected by the Trans-Mexican Volcanic Belt. The Southern extent of the American Cordillera makes up Western Mexico and northern Central America. This includes the Sierra Madre Occidental, the Sierra Madre del Sur, and the Trans-Mexican Volcanic Belt.

Geographic entities mentioned:
surface_form: Mexican Plateau
instance_of: Plateau
countries: Mexico
coordinates: lat: 24
lon: -103
Sites Reservoir. The Sites Reservoir is a proposed offstream reservoir project west of Colusa in the Sacramento Valley of northern California to be built and operated by the Sites Project Authority. The project would divert water from the Sacramento River upstream of the Sacramento–San Joaquin River Delta through existing canals to a new reservoir away.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
surface_form: sacramento valley
instance_of: Valley
countries: United States
coordinates: lat: 34.8147
lon: -114.161
surface_form: sites reservoir
instance_of: Body of water
countries: United States
coordinates: lat: 39.355
lon: -122.341
Sites Reservoir is funded by local, state, and federal public dollars. Participation in Sites is broad and diverse, including the Bureau of Reclamation, State of California, urban areas of Southern California and the Bay Area, as well as public irrigation districts in the Sacramento Valley and San Joaquin Valley.

Geographic entities mentioned:
surface_form: san joaquin valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
surface_form: sacramento valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
surface_form: sacramento valley
instance_of: Valley
countries: United States
coordinates: lat: 34.8147
lon: -114.161
Sites Reservoir. The Sites Reservoir is a proposed offstream reservoir project west of Colusa in the Sacramento Valley of northern California to be built and operated by the Sites Project Authority. The project would divert water from the Sacramento River upstream of the Sacramento–San Joaquin River Delta through existing canals to a new reservoir away.

Geographic entities mentioned:
surface_form: sites reservoir
instance_of: Body of water
countries: United States
coordinates: lat: 39.355
lon: -122.341
About 30 public water agencies, public irrigation districts, counties, and cities in California have tentatively committed funding based on a beneficiary pays principle. History. The Sites Reservoir was proposed in the 1950s. California had serious droughts in 1977–1978, 2006–2010, and 2011–2017, raising concern about water insecurity.

Geographic entities mentioned:
surface_form: sites reservoir
instance_of: Body of water
countries: United States
coordinates: lat: 39.355
lon: -122.341
The primary purpose of the Authority, as stated in the agreement, is to pursue the development and construction of the Sites Reservoir Project, which has long been viewed as an ideal location for additional off-stream storage to provide direct and real benefits to instream flows, the Delta ecosystem, and water supply.

Geographic entities mentioned:
surface_form: sites reservoir
instance_of: Body of water
countries: United States
coordinates: lat: 39.355
lon: -122.341
The Authority is governed by a board of directors that collaborates with other groups in the region interested in the construction of Sites Reservoir Project. Sites Reservoir is funded by local, state, and federal public dollars.

Geographic entities mentioned:
surface_form: sites reservoir
instance_of: Body of water
countries: United States
coordinates: lat: 39.355
lon: -122.341
In 2021, following the Authority's submission of the State Feasibility Report, the California Water Commission deemed the project feasible, which led to a $20 million inflation adjustment to the Proposition 1 award, making Sites Reservoir eligible for a total of $875 million in state funding.

Geographic entities mentioned:
surface_form: sites reservoir
instance_of: Body of water
countries: United States
coordinates: lat: 39.355
lon: -122.341
Location and specifications. The project is located in a naturally occurring valley near Maxwell, California. Once constructed, Sites Reservoir would stretch 13 miles from north to south and 4 miles from east to west. When full, the reservoir would be around 260 feet deep from surface to floor at its lowest point.

Geographic entities mentioned:
surface_form: sites reservoir
instance_of: Body of water
countries: United States
coordinates: lat: 39.355
lon: -122.341
Once constructed, it would be the 8th largest reservoir in California. Two primary dams, Sites Dam and Golden Gate Dam, would be constructed to hold water in the reservoir where hills drop too low, but they would not block major waterways or rivers. Sites Reservoir would also include nine small dams and dikes to hold the water at the right level. Operations.

Geographic entities mentioned:
surface_form: sites reservoir
instance_of: Body of water
countries: United States
coordinates: lat: 39.355
lon: -122.341
Operations. Sites Reservoir would operate as a flexible water storage solution by diverting water from the Sacramento River during high flows, after all other water rights and regulatory requirements are met, and storing it until water is needed in drier years. Unlike other major reservoirs, Sites would not dam a major river or rely on snowmelt.

Geographic entities mentioned:
surface_form: sites reservoir
instance_of: Body of water
countries: United States
coordinates: lat: 39.355
lon: -122.341
It is a rain-fed reservoir that can capture and store runoff from extreme storms. Sites Reservoir is uniquely located in relation to other major components of state and federal water projects like Shasta Lake, Lake Oroville, and Folsom Lake. The project would complement and extend these projects' functions by creating flexibility to adapt to changing river and Delta management conditions.

Geographic entities mentioned:
surface_form: sites reservoir
instance_of: Body of water
countries: United States
coordinates: lat: 39.355
lon: -122.341
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
Sites would not compete for the water resources stored in these state and federal facilities but would increase the total amount of managed water in storage. Diversions  . Sites Reservoir diversions occur only when there are high river flows, any reduction to Delta flows would be minor and would not impact any of the beneficial uses of the water in the Delta.

Geographic entities mentioned:
surface_form: sites reservoir
instance_of: Body of water
countries: United States
coordinates: lat: 39.355
lon: -122.341
Storing water in Sites Reservoir during times when there is a lot of flow in the Sacramento River for use during times with the flows are low, including during drought periods, is part of the statewide strategy for adapting to changing climate conditions and to return much needed flexibility to the statewide water management system.

Geographic entities mentioned:
surface_form: sites reservoir
instance_of: Body of water
countries: United States
coordinates: lat: 39.355
lon: -122.341
Conveyance. Water for Sites Reservoir would come from two general sources: the Sacramento River and local creeks. Water from the Sacramento River is diverted at the existing Red Bluff Pumping Plant, owned by the United States Bureau of Reclamation and operated by the, and at the Hamilton City Pump Station, owned and operated by the.

Geographic entities mentioned:
surface_form: sites reservoir
instance_of: Body of water
countries: United States
coordinates: lat: 39.355
lon: -122.341
Both pumping facilities have state-of-the-art fish screens to protect fish during project operations. Water diverted at the Red Bluff Pumping Plant, would enter the Tehama-Colusa Canal and be conveyed down to Funks Reservoir. From there, the Sites Project Authority would pump the water up into Sites Reservoir through a series of pipelines and tunnels.

Geographic entities mentioned:
surface_form: sites reservoir
instance_of: Body of water
countries: United States
coordinates: lat: 39.355
lon: -122.341
After water is diverted at the Hamilton City Pump Station, it would enter Glenn-Colusa Irrigation District's Main Canal and be conveyed down to the new Terminal Regulating Reservoir. The Authority would then pump this water up into Sites Reservoir through a series of pipelines and a tunnel. The maximum combined diversion capacity for Sites is about.

Geographic entities mentioned:
surface_form: sites reservoir
instance_of: Body of water
countries: United States
coordinates: lat: 39.355
lon: -122.341
The water supply could fall short of projections. Environmental water. In alignment with the project's Proposition 1 funding, Sites Reservoir is planned to be the first and only reservoir in California that captures and stores a large portion of water specifically for the environment to support freshwater ecosystems.

Geographic entities mentioned:
surface_form: sites reservoir
instance_of: Body of water
countries: United States
coordinates: lat: 39.355
lon: -122.341
The environment is to be the single largest user of water stored in Sites Reservoir, managed and distributed by federal and state natural resource agencies. Fisheries. The additional water supply provided by Sites Reservoir may provide opportunities for improved management of salmonid habitat, particularly in the Sacramento River above Red Bluff.

Geographic entities mentioned:
surface_form: sites reservoir
instance_of: Body of water
countries: United States
coordinates: lat: 39.355
lon: -122.341
Fisheries. The additional water supply provided by Sites Reservoir may provide opportunities for improved management of salmonid habitat, particularly in the Sacramento River above Red Bluff. By delivering water to CVP contractors from Sites Reservoir, Reclamation may maintain supply in Shasta Lake to support habitat for salmonid spawning, incubation, rearing, and migration.

Geographic entities mentioned:
surface_form: sites reservoir
instance_of: Body of water
countries: United States
coordinates: lat: 39.355
lon: -122.341
Fisheries. The additional water supply provided by Sites Reservoir may provide opportunities for improved management of salmonid habitat, particularly in the Sacramento River above Red Bluff. By delivering water to CVP contractors from Sites Reservoir, Reclamation may maintain supply in Shasta Lake to support habitat for salmonid spawning, incubation, rearing, and migration.

Geographic entities mentioned:
surface_form: sites reservoir
instance_of: Body of water
countries: United States
coordinates: lat: 39.355
lon: -122.341
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
For example, Sites can be operated in coordination with Shasta Lake to preserve and enhance cold water for endangered salmon in the Sacramento River or to increase fresh-water flow into the Delta during drier periods to assist with salinity management.

Geographic entities mentioned:
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
According to &quot;Final Feasibility Report&quot; submitted by the Bureau of Reclamation in December 2020: &quot;A substantial portion of the project’s water would be specifically dedicated to environmental uses, helping to improve conditions for Delta smelt, preserving the cold-water pool in Lake Shasta to support salmon development, spawning and rearing, and providing a reliable water supply to improve the habitat for migratory birds and other native species&quot;.

Geographic entities mentioned:
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
To protect fisheries, the pumping stations along the Sacramento River are to have fish screens. There are potential modifications upstream at Shasta Dam that could increase the supply of cold water. The intakes at the Tehama-Colusa and Glenn-Colusa Canals are to be modified.

Geographic entities mentioned:
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
The possible additional water supply in Shasta Lake can then be allocated during real-time management scenarios for several uses (e.g., coldwater pool maintenance, spring pulse or fall pulse flow events, increased stability in fall flows) that may provide enhanced anadromous fish benefits. Water quality.

Geographic entities mentioned:
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
Flowing through a rugged and isolated coastal region, it descends rapidly from about to sea level at the Pacific Ocean. Except for the lowermost, the river is located entirely within the Rogue River – Siskiyou National Forest. The river rises in the Kalmiopsis Wilderness, northwest of Chetco Peak at the junction of the Oregon Coast Range and the Klamath Mountains.

Geographic entities mentioned:
surface_form: Chetco Peak
instance_of: Mountain
countries: United States
coordinates: lat: 42.135972222222
lon: -123.94241666667
Course. The Chetco River begins about east of Chetco Peak, approximately above sea level. It flows north, gathering small tributaries such as the Little Chetco River and Babyfoot Creek. The river turns west near the Pearsoll Peak, the highest point in the watershed. It receives Box Canyon Creek on the left bank, Tincup Creek on the right bank, and Boulder Creek on the left.

Geographic entities mentioned:
surface_form: Pearsoll Peak
instance_of: Mountain
countries: United States
coordinates: lat: 42.29875
lon: -123.84641666667
It then flows south, gathering the South Fork Chetco River. A few miles farther south, the river passes through a Redwood grove. It flows between Bosley Butte to the north and Mount Emily to the south; the latter is the impact site of one of only four bombs known to have been dropped in the continental United States by an enemy aircraft. This occurred during the Lookout Air Raids of 1942.

Geographic entities mentioned:
surface_form: Bosley Butte
instance_of: Mountain
countries: United States
coordinates: lat: 42.20910972222222
lon: -124.22522422222222
surface_form: Mount Emily
instance_of: Mountain
countries: United States
coordinates: lat: 42.078333
lon: -124.111111
Lake Arapuni. Lake Arapuni is one of several artificial lakes formed as part of a hydroelectricity scheme on the Waikato River in the North Island of New Zealand. It is southeast of Hamilton, to the north of Mangakino. The dam, at the small settlement of Arapuni at the lake's northern end, was the first constructed on the Waikato, and was commissioned in 1929. The lake occupies an area of.

Geographic entities mentioned:
surface_form: lake arapuni
instance_of: Lake
countries: New Zealand
coordinates: lat: -38.136111111111
lon: 175.63611111111
surface_form: arapuni
instance_of: Lake
countries: New Zealand
coordinates: lat: -38.136111111111
lon: 175.63611111111
Lake Arapuni. Lake Arapuni is one of several artificial lakes formed as part of a hydroelectricity scheme on the Waikato River in the North Island of New Zealand. It is southeast of Hamilton, to the north of Mangakino. The dam, at the small settlement of Arapuni at the lake's northern end, was the first constructed on the Waikato, and was commissioned in 1929. The lake occupies an area of.

Geographic entities mentioned:
surface_form: arapuni
instance_of: Lake
countries: New Zealand
coordinates: lat: -38.136111111111
lon: 175.63611111111
This is especially common during the months of August and September, the rainiest months that the surrounding villages seem to experience during the last months of Summer. With such a large density, this also proves to be beneficial to the surrounding organisms which live near the lake such as the Lake Patzcuaro Garter Snake, which thrives near the cattail closest to the lake.

Geographic entities mentioned:
surface_form: Lake Patzcuaro
instance_of: Lake
countries: Mexico
coordinates: lat: 19.615
lon: -101.65
Cox, who is described by BC historians G.P.V. and Helen B. Akrigg as &quot;friendly, genial and easy-going&quot;, encamped at Puntzi Lake on June 12, 1864, four days after leaving Alexandria, and did not very much in advance of the arrival of Seymour's and Brew's contingent other than build minor fortifications.

Geographic entities mentioned:
surface_form: Puntzi Lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.2
lon: -124
As the Akriggs comment, &quot;One can imagine the blistering contempt Sir James Douglas would have expressed if Cox had given such a report to him&quot; (had Douglas still been Governor). Governor Seymour, nonplussed by Cox's excuse, sent him and his troops to Tatla Lake to search for the warring members of the Tsilhqot'in.

Geographic entities mentioned:
surface_form: Tatla Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.9667
lon: -124.417
above the Roaring Fork Valley to the north. The highest peaks in the range are its fourteeners, Castle Peak (14,265 ft), Maroon Peak (14,156 ft), Capitol Peak (14,130 ft), Snowmass Mountain (14,092 ft), Pyramid Peak (14,018 ft), and North Maroon Peak (14,014 ft). Maroon Peak and North Maroon Peak are collectively known as the Maroon Bells, a popular destination for recreation alpinism.

Geographic entities mentioned:
surface_form: Maroon Peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0708
lon: -106.989
surface_form: Snowmass Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.118755555556
lon: -107.06645833333
surface_form: North Maroon Peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0708
lon: -106.989
above the Roaring Fork Valley to the north. The highest peaks in the range are its fourteeners, Castle Peak (14,265 ft), Maroon Peak (14,156 ft), Capitol Peak (14,130 ft), Snowmass Mountain (14,092 ft), Pyramid Peak (14,018 ft), and North Maroon Peak (14,014 ft). Maroon Peak and North Maroon Peak are collectively known as the Maroon Bells, a popular destination for recreation alpinism.

Geographic entities mentioned:
surface_form: Maroon Bells
instance_of: Mountain
countries: United States
coordinates: lat: 39.0708
lon: -106.989
Maroon Peak and North Maroon Peak are collectively known as the Maroon Bells, a popular destination for recreation alpinism. Mount Sopris (12,953 ft) sits at the northwest end of the range and dominates the skyline of the lower Roaring Fork Valley and the town of Carbondale, Colorado, serving as an unofficial symbol of the area.

Geographic entities mentioned:
surface_form: Mount Sopris
instance_of: Mountain
countries: United States
coordinates: lat: 39.2632
lon: -107.176
Davis Lake (British Columbia). Davis Lake is a lake in the Interior of British Columbia. It lies at the head of Davis Creek, just north of the town of Kettle Valley, British Columbia. Nearby is Mount Davis.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: davis lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.1072
lon: -118.871
Davis Lake (British Columbia). Davis Lake is a lake in the Interior of British Columbia. It lies at the head of Davis Creek, just north of the town of Kettle Valley, British Columbia. Nearby is Mount Davis.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Davis Lake (British Columbia). Davis Lake is a lake in the Interior of British Columbia. It lies at the head of Davis Creek, just north of the town of Kettle Valley, British Columbia. Nearby is Mount Davis.

Geographic entities mentioned:
surface_form: mount davis
instance_of: Mountain
countries: Canada
coordinates: lat: 50.11355556
lon: -117.08466667
Råna. Råna is a mountain in Møre og Romsdal county, Norway. The mountain sits on the municipal border between Ørsta Municipality and Sykkylven Municipality. It is part of Hjelledalstindane mountains in the Sunnmørsalpene range. The tall mountain is located about east of the village of Store-Standal in Ørsta Municipality and about south of the village of Straumgjerde in Sykkylven Municipality.

Geographic entities mentioned:
surface_form: romsdal
instance_of: Valley
countries: Norway
coordinates: lat: 62.447222222222
lon: 7.8333333333333
surface_form: råna
instance_of: Mountain
countries: Norway
coordinates: lat: 62.275
lon: 6.5741666666667
Råna. Råna is a mountain in Møre og Romsdal county, Norway. The mountain sits on the municipal border between Ørsta Municipality and Sykkylven Municipality. It is part of Hjelledalstindane mountains in the Sunnmørsalpene range. The tall mountain is located about east of the village of Store-Standal in Ørsta Municipality and about south of the village of Straumgjerde in Sykkylven Municipality.

Geographic entities mentioned:
surface_form: råna
instance_of: Mountain
countries: Norway
coordinates: lat: 62.275
lon: 6.5741666666667
The Central Valley is California's productive agricultural heartland. Divided in two by the Sacramento-San Joaquin River Delta, the northern portion, the Sacramento Valley serves as the watershed of the Sacramento River, while the southern portion, the San Joaquin Valley is the watershed for the San Joaquin River. Both valleys derive their names from the rivers that flow through them.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
The Channel Islands are located off the Southern coast, while the Farallon Islands lie west of San Francisco. The Sierra Nevada (Spanish for &quot;snowy range&quot;) includes the highest peak in the contiguous 48 states, Mount Whitney, at.

Geographic entities mentioned:
surface_form: Mount Whitney
instance_of: Mountain
countries: United States
coordinates: lat: 36.57861111111111
lon: -118.29194444444444
The Sierra Nevada (Spanish for &quot;snowy range&quot;) includes the highest peak in the contiguous 48 states, Mount Whitney, at. The range embraces Yosemite Valley, famous for its glacially carved domes, and Sequoia National Park, home to the giant sequoia trees, the largest living organisms on Earth, and the deep freshwater lake, Lake Tahoe, the largest lake in the state by volume.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
The range embraces Yosemite Valley, famous for its glacially carved domes, and Sequoia National Park, home to the giant sequoia trees, the largest living organisms on Earth, and the deep freshwater lake, Lake Tahoe, the largest lake in the state by volume. To the east of the Sierra Nevada are Owens Valley and Mono Lake, an essential migratory bird habitat.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
In the south is a large inland salt lake, the Salton Sea. The south-central desert is called the Mojave; to the northeast of the Mojave lies Death Valley, which contains the lowest and hottest place in North America, the Badwater Basin at. The horizontal distance from the bottom of Death Valley to the top of Mount Whitney is less than.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
The higher elevation deserts of eastern California have hot summers and cold winters, while the low deserts east of the Southern California mountains have hot summers and nearly frostless mild winters. Death Valley, a desert with large expanses below sea level, is considered the hottest location in the world; the highest temperature in the world, was recorded there on July 10, 1913.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
The table below lists average temperatures for January and August in a selection of places throughout the state; some highly populated and some not. This includes the relatively cool summers of the Humboldt Bay region around Eureka, the extreme heat of Death Valley, and the mountain climate of Mammoth in the Sierra Nevada. The wide range of climates leads to a high demand for water.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Per capita income varies widely by geographic region and profession. The Central Valley is the most impoverished, with migrant farm workers making less than minimum wage. According to a 2005 report by the Congressional Research Service, the San Joaquin Valley was characterized as one of the most economically depressed regions in the United States, on par with the region of Appalachia.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Manitoba Provincial Road 222. Provincial Road 222 (PR 222) is a provincial road in the Interlake Region of the Canadian province of Manitoba. Essentially a northerly continuation of Highway 9, the road extends for along the western shore of Lake Winnipeg between the communities of Gimli and Riverton. The road is the inspiration for and namesake of singer-songwriter John K.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
It heads north out of town along the coastline of Lake Winnipeg, travelling past several lakefront subdivisions and campgrounds to pass through Camp Morton, where it has an intersection with Camp Morton Road (PR 324), which provides access to Camp Morton Provincial Park, as well as making a sharp left hand turn across a railroad track before making an immediate right and heading north again.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Beyond Downtown Los Angeles, US 101 uses the Hollywood Freeway as it travels northwest through the eponymous neighborhood towards Cahuenga Pass, where it crosses the Hollywood Hills and passes Universal Studios Hollywood. The highway leaves the Hollywood Freeway to turn west onto the Ventura Freeway, which travels along the southern edge of the suburban San Fernando Valley and intersects I-405.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
The highway leaves the Hollywood Freeway to turn west onto the Ventura Freeway, which travels along the southern edge of the suburban San Fernando Valley and intersects I-405. US 101 continues into Ventura County, where it joins SR 1 and serves communities in the Conejo Valley and Oxnard Plain.

Geographic entities mentioned:
surface_form: Conejo Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
surface_form: Oxnard Plain
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
US 101 passes near Pinnacles National Park and travels through the city of Salinas, where it turns northeast to cross the Gabilan Range. From there, the highway descends into the Santa Clara Valley and Gilroy, the southernmost city in the San Francisco Bay Area.

Geographic entities mentioned:
surface_form: Santa Clara Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.366944444444
lon: -121.98388888889
US 101 travels through Gold Beach and crosses the Rogue River to continue north along the coast. The highway turns west to follow the base of Humbug Mountain, a mountain that rises from the Pacific Ocean, and northwest to reach Port Orford, where it leaves the coastline.

Geographic entities mentioned:
surface_form: Humbug Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.678722222222
lon: -124.43677222222
US 101 diverts northeast to cross the Umpqua River at Reedsport and passes through a meandering section near Tahkenitch Lake before it returns to the coastal dunes around Dunes City. The Oregon Coast Highway crosses the Siuslaw River into Florence and intersects Oregon Route 126 (OR 126), a major east–west route that traverses the Coast Range to Eugene.

Geographic entities mentioned:
surface_form: Tahkenitch Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.77911983333333
lon: -124.1323
The streets travel through western Aberdeen and neighboring Hoquiam, where the highway is split by the Hoquiam River, and rejoin north of downtown. The highway continues north along inland streams into the Quinault Indian Reservation, which it enters near Lake Quinault at the edge of Olympic National Park.

Geographic entities mentioned:
surface_form: Lake Quinault
instance_of: Lake
countries: United States
coordinates: lat: 47.476377777778
lon: -123.87016388889
It then travels north through Forks and follows the Sol Duc River east to re-enter the national park. US 101 travels along the southern shore of Lake Crescent, one of the deepest lakes in the state, and the foothills of the Olympic Mountains until it crosses the Elwha River near the site of the demolished Elwha Dam.

Geographic entities mentioned:
surface_form: Lake Crescent
instance_of: Lake
countries: United States
coordinates: lat: 48.0595755
lon: -123.8291037
Most residents and businesses in the area use postal zip codes from neighboring cities of Morgan Hill, San Martin, and Gilroy. The telephone area code is 408. Climate. The region lies in the southern part of Santa Clara Valley, and supports a relatively mild Mediterranean climate.

Geographic entities mentioned:
surface_form: Santa Clara Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.366944444444
lon: -121.98388888889
The sum is covered by hills and mountains, with 90% of the area lying at altitudes above. The highest point is the Besbogda Mountain (). The sum contains the Tsengel Khairkhan mountain, with an elevation of. The Khovd River flows through the district, flowing through the town of Bilüü. Landmarks.

Geographic entities mentioned:
surface_form: Tsengel Khairkhan
instance_of: Mountain
countries: Mongolia
coordinates: lat: 48.6475
lon: 89.1561
Ailã River. The Ailã River () is a river of Roraima state in northern Brazil. It is located in Monte Caburaí, in the municipality of Uiramutã. Its source is the northernmost point of Brazil.

Geographic entities mentioned:
surface_form: Monte Caburaí
instance_of: Mountain
countries: Brazil
Guyana
coordinates: lat: 5.272222
lon: -60.211944
Ejected preachers such as John Blackadder conducted religious ceremonies at conventicles. Many of the covenanting prisoners on the Bass Rock had been charged with attending conventicles. Scotland after the Revolution.

Geographic entities mentioned:
surface_form: Bass Rock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.08
lon: -2.64
Labeo kibimbi. &quot;Labeo kibimbi&quot; is fish in genus &quot;Labeo&quot; from the upper Lualaba and Lake Tanganyika in the Democratic Republic of the Congo.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
Box Lake (Nevada). Box Lake is a glacial tarn in the Ruby Mountains, in Elko County in the northeastern part of the state of Nevada. It is located on a shelf on the side wall of Box Canyon, and at an elevation of. Along with Snow Lake, it is one of the sources of the stream which flows down Box Canyon.

Geographic entities mentioned:
surface_form: box lake (nevada)
instance_of: Lake
countries: United States
coordinates: lat: 40.5967
lon: -115.42
Box Lake (Nevada). Box Lake is a glacial tarn in the Ruby Mountains, in Elko County in the northeastern part of the state of Nevada. It is located on a shelf on the side wall of Box Canyon, and at an elevation of. Along with Snow Lake, it is one of the sources of the stream which flows down Box Canyon.

Geographic entities mentioned:
surface_form: box lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5967
lon: -115.42
Box Lake is a glacial tarn in the Ruby Mountains, in Elko County in the northeastern part of the state of Nevada. It is located on a shelf on the side wall of Box Canyon, and at an elevation of. Along with Snow Lake, it is one of the sources of the stream which flows down Box Canyon. After exiting the mountains it merges with other streams to form the South Fork of the Humboldt River.

Geographic entities mentioned:
surface_form: snow lake
instance_of: Lake
countries: United States
coordinates: lat: 40.6017
lon: -115.4
surface_form: snow lake
instance_of: Lake
countries: United States
coordinates: lat: 46.7572
lon: -121.698
surface_form: snow lake
instance_of: Lake
countries: United States
coordinates: lat: 47.46694444
lon: -121.45555556
surface_form: snow lake
instance_of: Lake
countries: United States
coordinates: lat: 33.4226
lon: -108.496