Sarmila/GeoWiki-Features huggingface dataset:
This park of has trails for hiking, cycling and horseback riding and is one of two parks named in honor of former mayor Helen Putnam who served from 1965 to 1979; the other is Putnam Plaza on Petaluma Boulevard. Lying above the city of Petaluma on the northwest flank of Sonoma Mountain is the Fairfield Osborn Preserve, a nature reserve with a diversity of native plants and animals.

Geographic entities mentioned:
surface_form: Sonoma Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.3231
lon: -122.575
Lying above the city of Petaluma on the northwest flank of Sonoma Mountain is the Fairfield Osborn Preserve, a nature reserve with a diversity of native plants and animals. Nearby to the southeast is Tolay Lake, the site of prehistoric seasonal settlement by Miwok and Pomo tribes. Government. The mayor of Petaluma is Kevin McDonnell. State and federal representation.

Geographic entities mentioned:
surface_form: Tolay Lake
instance_of: Lake
countries: United States
coordinates: lat: 38.209166666667
lon: -122.51388888889
Boggy Lake. Boggy Lake is a lake of Guysborough District, in Nova Scotia, Canada. It also extends into Halifax County. This natural area is characterized by well-defined drumlins with mature to immature old-growth sugar maple, yellow birch, and beech forests, that sit in a matrix of well-drained coniferous hummocky terrain.

Geographic entities mentioned:
surface_form: boggy lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.0988
lon: -62.3151
Ronas Hill. Ronas Hill (or Rönies Hill) is a hill in Shetland, Scotland. It is classed as a Marilyn, and is the highest point in the Shetland Islands at an elevation of. A Neolithic chambered cairn is located near the summit. Location. Ronas Hill (, meaning stony ground or scree) is on the Northmavine peninsula of Mainland, Shetland, at. The Norse name certainly describes the hilltop.

Geographic entities mentioned:
surface_form: rönies hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 60.533856
lon: -1.445935
surface_form: ronas hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 60.533856
lon: -1.445935
Ronas Hill. Ronas Hill (or Rönies Hill) is a hill in Shetland, Scotland. It is classed as a Marilyn, and is the highest point in the Shetland Islands at an elevation of. A Neolithic chambered cairn is located near the summit. Location. Ronas Hill (, meaning stony ground or scree) is on the Northmavine peninsula of Mainland, Shetland, at. The Norse name certainly describes the hilltop.

Geographic entities mentioned:
surface_form: ronas hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 60.533856
lon: -1.445935
It is classed as a Marilyn, and is the highest point in the Shetland Islands at an elevation of. A Neolithic chambered cairn is located near the summit. Location. Ronas Hill (, meaning stony ground or scree) is on the Northmavine peninsula of Mainland, Shetland, at. The Norse name certainly describes the hilltop. Ronas Hill also gives its name to Ronas Voe, which it sits adjacent to.

Geographic entities mentioned:
surface_form: ronas hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 60.533856
lon: -1.445935
Ronas Hill (, meaning stony ground or scree) is on the Northmavine peninsula of Mainland, Shetland, at. The Norse name certainly describes the hilltop. Ronas Hill also gives its name to Ronas Voe, which it sits adjacent to. On a clear day, much of Shetland can be seen from the summit. It looks over Yell Sound, the North Sea, across to the Atlantic Ocean and even the highest points of Fair Isle.

Geographic entities mentioned:
surface_form: ronas hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 60.533856
lon: -1.445935
It looks over Yell Sound, the North Sea, across to the Atlantic Ocean and even the highest points of Fair Isle. Flora and fauna. Ronas Hill is a Ramsar site, containing many rare Arctic plants. Peculiarly for Shetland, there are several species of woodland fungi, notably ceps and chanterelles, which normally grow on the roots of deciduous trees (notable by their absence on Ronas Hill).

Geographic entities mentioned:
surface_form: ronas hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 60.533856
lon: -1.445935
Flora and fauna. Ronas Hill is a Ramsar site, containing many rare Arctic plants. Peculiarly for Shetland, there are several species of woodland fungi, notably ceps and chanterelles, which normally grow on the roots of deciduous trees (notable by their absence on Ronas Hill). Here, they are associated with creeping willow, which grows extensively on the hill.

Geographic entities mentioned:
surface_form: ronas hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 60.533856
lon: -1.445935
Here, they are associated with creeping willow, which grows extensively on the hill. The hill forms part of the Ronas Hill – North Roe and Tingon Important Bird Area (IBA), designated as such by BirdLife International because it supports a suite of moorland-breeding birds, including red-throated loons, great skuas and merlins. Chambered cairn.

Geographic entities mentioned:
surface_form: ronas hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 60.533856
lon: -1.445935
Most surviving Neolithic British cairns are sited in prominent places, but not generally on the top of taller hills. According to local farmers, until the construction of Sullom Voe Terminal in the mid-1970s, the cairn contained a variety of &quot;sacrifice&quot; items, such as coins (some &quot;very old&quot;) and other items. Before that time, Ronas Hill would have been far off the beaten track.

Geographic entities mentioned:
surface_form: ronas hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 60.533856
lon: -1.445935
Vermont Lake. Vermont Lake is a lake in Douglas County, in the U.S. state of Minnesota. A number of the first settlers being natives of Vermont caused the name to be selected.

Geographic entities mentioned:
surface_form: vermont lake
instance_of: Lake
countries: United States
coordinates: lat: 46.08194444
lon: -95.37305556
Sri Lanka's irrigation network was extensively expanded during the reign of Parākramabāhu the Great. He built 1470 reservoirs – the highest number by any ruler in Sri Lanka's history – repaired 165 dams, 3910 canals, 163 major reservoirs, and 2376 mini-reservoirs. His most famous construction is the Parakrama Samudra, the largest irrigation project of medieval Sri Lanka.

Geographic entities mentioned:
surface_form: Parakrama Samudra
instance_of: Lake
countries: Sri Lanka
coordinates: lat: 7.9
lon: 80.966666666667
Agriculture. Mass tanks were built for this purpose. Some of his notable works are the Parakrama Samudra and the Giritale tank. These works surpassed what existed during the Anuradhapura period. Previously built dams were largely renovated during this period. Demographics. The Sinhalese accounted for the majority, and the Sinhalese language was the common language.

Geographic entities mentioned:
surface_form: Parakrama Samudra
instance_of: Lake
countries: Sri Lanka
coordinates: lat: 7.9
lon: 80.966666666667
Origin. The Waterloo Moraine was formed as the three ice lobes of the Laurentide Ice Sheet retreated across what is now Waterloo Region from Lake Huron in the west, Georgian Bay in the northeast, Lake Ontario in the east and Lake Erie in the southeast. As the glacier moved, it carried with it huge boulders, sand, gravel and debris.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Located in Blaine County, Saviers Peak is about north of the Camas County border. The peak is also located in Sawtooth National Recreation Area south of Galena Summit. It is about northeast of Camas County Highpoint and southeast of Bromaghin Peak. No trails lead near Saviers Peak, and it is most easily accessed from the north at the Titus Lake trailhead along Idaho State Highway 75.

Geographic entities mentioned:
surface_form: Camas County Highpoint
instance_of: Mountain
countries: United States
coordinates: lat: 43.8148
lon: -114.719
surface_form: Bromaghin Peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.8305
lon: -114.719
Saviers Peak. Saviers Peak, at above sea level is the highest peak in the Smoky Mountains of Idaho. Located in Blaine County, Saviers Peak is about north of the Camas County border. The peak is also located in Sawtooth National Recreation Area south of Galena Summit. It is about northeast of Camas County Highpoint and southeast of Bromaghin Peak.

Geographic entities mentioned:
surface_form: saviers peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.822
lon: -114.713
Located in Blaine County, Saviers Peak is about north of the Camas County border. The peak is also located in Sawtooth National Recreation Area south of Galena Summit. It is about northeast of Camas County Highpoint and southeast of Bromaghin Peak. No trails lead near Saviers Peak, and it is most easily accessed from the north at the Titus Lake trailhead along Idaho State Highway 75.

Geographic entities mentioned:
surface_form: saviers peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.822
lon: -114.713
She returned to Tanzania and graduated with a Postgraduate Diploma in Diplomatic Relations from the Centre for Foreign Relations in Dar es Salaam. She also holds a Master of Arts degree in Mass Communication, awarded by St. Augustine University of Tanzania (SAUT), in Mwanza, along the shores of Lake Victoria.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
48% of the student body was female, with 52% male. The school has a student-teacher ratio of 26:1. Sandy High School's student body is primarily made up of residents along the Mount Hood Corridor, a route connecting the Portland metropolitan area with the recreational facilities on Mount Hood, and in Kah-Nee-Ta and central Oregon. Academics. Sandy High School is unranked by &quot;U.S.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
Bradford Dale (Yorkshire). Bradford Dale (or Bradfordale), is a side valley of Airedale that feeds water from Bradford Beck across the City of Bradford into the River Aire at Shipley in West Yorkshire, England. Whilst it is in Yorkshire and a dale, it is not part of the Yorkshire Dales and has more in common with Lower Nidderdale and Lower Airedale for its industrialisation.

Geographic entities mentioned:
surface_form: Airedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.017
lon: -1.465
surface_form: bradford dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.794
lon: -1.7632
Bradford Dale (Yorkshire). Bradford Dale (or Bradfordale), is a side valley of Airedale that feeds water from Bradford Beck across the City of Bradford into the River Aire at Shipley in West Yorkshire, England. Whilst it is in Yorkshire and a dale, it is not part of the Yorkshire Dales and has more in common with Lower Nidderdale and Lower Airedale for its industrialisation.

Geographic entities mentioned:
surface_form: Nidderdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.0867
lon: -1.75773
surface_form: airedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.017
lon: -1.465
The dale is notable for the lack of a main river (Bradford Beck being only a small watercourse in comparison to the rivers Wharfe, Aire, Calder and Don) and necessitated the importation of clean water into the dale from as afar afield as Nidderdale. Most of the becks in the city centre have now been culverted and have suffered with pollution from the heavy woollen industry in the dale. History.

Geographic entities mentioned:
surface_form: nidderdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.0867
lon: -1.75773
Bradford Dale is not one of the Yorkshire Dales, though it was surrounded by high ground on three sides with water flowing down the valley. Its industrialisation has led to it being compared with Nidderdale and Airedale as a &quot;partly industrialised Yorkshire Valley&quot;.

Geographic entities mentioned:
surface_form: nidderdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.0867
lon: -1.75773
surface_form: airedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.017
lon: -1.465
Previous to the industrial Revolution, the dale was the name that united the various communities that were situated within it, and also of some on the outer edges. Places such as Allerton, Bolton and Manningham were settlements in their own right; the Parish of Manningham stretched from Chellow Dean Beck in the west to the Bradford Beck in the east.

Geographic entities mentioned:
surface_form: dean
instance_of: Valley
countries: United Kingdom
Several streams feed into the city (Pitty Beck, Pinch Beck, Hole Bottom Beck, Clayton Beck, Horton Beck, Chellow Dean Beck and two smaller ones near to the city centre) and merge in the city centre leaving Bradford flowing northwards as Bradford Beck. These waters that feed Bradford Beck, along with the geological conditions, formed Bradford Dale. The catchment area for the dale covers over.

Geographic entities mentioned:
surface_form: dean
instance_of: Valley
countries: United Kingdom
Bradford Dale (Yorkshire). Bradford Dale (or Bradfordale), is a side valley of Airedale that feeds water from Bradford Beck across the City of Bradford into the River Aire at Shipley in West Yorkshire, England. Whilst it is in Yorkshire and a dale, it is not part of the Yorkshire Dales and has more in common with Lower Nidderdale and Lower Airedale for its industrialisation.

Geographic entities mentioned:
surface_form: bradford dale (yorkshire)
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.794
lon: -1.7632
Since most settlements became suburbs of the City of Bradford, the term Bradford Dale has become archaic and has fallen into disuse, though it is sometimes used to refer to the flat section of land northwards from Bradford City Centre towards Shipley. The woollen and worsted industries had a profound effect on the dale, the later City of Bradford and the wider region.

Geographic entities mentioned:
surface_form: bradford dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.794
lon: -1.7632
History. Bradford Dale was described as being The valley that the Bradford Beck flows through was known variously as Bradforddale, Bradford-dale, Bradfordale, Bradford Dale, Bradeffordale and Broadfordesdale. The City of Bradford, which takes its name through the derivation of Broad Ford (across the Bradford Beck) was not formalised as a city until 1897.

Geographic entities mentioned:
surface_form: bradford dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.794
lon: -1.7632
surface_form: bradford dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.794
lon: -1.7632
Places such as Allerton, Bolton and Manningham were settlements in their own right; the Parish of Manningham stretched from Chellow Dean Beck in the west to the Bradford Beck in the east. Only since the institution of Bradford as a city at the end of the 19th century did these settlements become suburbs of Bradford, and so were referred to as being in Bradford rather than Bradford Dale.

Geographic entities mentioned:
surface_form: bradford dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.794
lon: -1.7632
Only since the institution of Bradford as a city at the end of the 19th century did these settlements become suburbs of Bradford, and so were referred to as being in Bradford rather than Bradford Dale. Bradford Dale is not one of the Yorkshire Dales, though it was surrounded by high ground on three sides with water flowing down the valley.

Geographic entities mentioned:
surface_form: bradford dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.794
lon: -1.7632
The valley of the River Aire was covered in a huge lake named Lake Bradford towards the end of the last ice age. This lake was fed by the meltwaters running through Cottingley, Harden, Keighley and Bradford (which was combined of several becks). Backfilling of water also created lakes further up in Bradford Dale; one at Fairweather Green was estimated by Kendall to be at least deep.

Geographic entities mentioned:
surface_form: bradford dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.794
lon: -1.7632
Backfilling of water also created lakes further up in Bradford Dale; one at Fairweather Green was estimated by Kendall to be at least deep. Additionally, water would sometimes reach such heights as to escape naturally away from its traditional route northwards through Bradford Dale.

Geographic entities mentioned:
surface_form: bradford dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.794
lon: -1.7632
Kendall claims that this was a natural cutting carved by water spilling over to the south east from the glacial lakes across the area. When the waters receded, the valley of Bradford Dale was settled first by Palaeolithic then Mesolithic man, who became hunter-gatherers in the wooded valley.

Geographic entities mentioned:
surface_form: bradford dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.794
lon: -1.7632
This pushed the Celtic peoples to the edges of Bradford Dale (Eccleshill and Wilsden), but also brought Christianity to the area, and when the Church of St Peter was built in what is now Bradford city centre, it was sometimes referred to as St Peters in Bradfordale.

Geographic entities mentioned:
surface_form: bradford dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.794
lon: -1.7632
Several streams feed into the city (Pitty Beck, Pinch Beck, Hole Bottom Beck, Clayton Beck, Horton Beck, Chellow Dean Beck and two smaller ones near to the city centre) and merge in the city centre leaving Bradford flowing northwards as Bradford Beck. These waters that feed Bradford Beck, along with the geological conditions, formed Bradford Dale. The catchment area for the dale covers over.

Geographic entities mentioned:
surface_form: bradford dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.794
lon: -1.7632
These waters that feed Bradford Beck, along with the geological conditions, formed Bradford Dale. The catchment area for the dale covers over. As the industrialisation of Bradford was some time off from the Middle Ages, many locations and settlements were not listed as being in Bradford itself, which was quite small, but in Bradford Dale.

Geographic entities mentioned:
surface_form: bradford dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.794
lon: -1.7632
surface_form: bradford dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.794
lon: -1.7632
As the industrialisation of the valley progressed, so too did the pollution in the air. By 1847, a stipulation had been laid down in local bye-laws that all chimneys must be at least in height to help progress smoke out of Bradford Dale.

Geographic entities mentioned:
surface_form: bradford dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.794
lon: -1.7632
Even then &quot;these chimneys belched out large quantities of smoke, ash, sulphur and other irritants into the atmosphere of Bradford Dale...during still-air conditions, especially in winter, polluted air was trapped in the basin-shaped valley of the Bradford Beck, and killing 'pea-soup fogs' used to occur.&quot;
Modern Bradford Dale has many roads through it; the A647 and the B6145 travel on either side of the small valley that starts off Bradford Dale to the west with Pinch Beck (Thornton Viaduct straddles this small valley too).

Geographic entities mentioned:
surface_form: bradford dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.794
lon: -1.7632
surface_form: bradford dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.794
lon: -1.7632
surface_form: bradford dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.794
lon: -1.7632
surface_form: bradford dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.794
lon: -1.7632
Geology. Bradford Dale consists largely of coal measures (of the &quot;Pennine Lower Coal Measures Formation&quot;) with hard sandstone beds in certain areas. The hard millstone grit which is renowned across the north becomes more widespread further up the Aire Valley, but certain areas within Bradford Dale were good locations for sandstone flags, such as the quarries at Bolton Woods.

Geographic entities mentioned:
surface_form: bradford dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.794
lon: -1.7632
The reservoirs at Chellow Dean receive water from the Nidd Aqueduct, but also took water from Manywells Spring in Cullingworth. The corporation also installed a sewage plant at Frizinghall, but this proved not to be capable enough to deal with the wastewater needs of the woollen industry and so a pipe was installed from the Frizinghall works to a new plant at Esholt in Airedale.

Geographic entities mentioned:
surface_form: airedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.017
lon: -1.465
Quonochontaug Pond. Quonochontaug () is a coastal lagoon in the towns of Charlestown and Westerly, both in Washington County, Rhode Island, United States. It is the most saline of nine such lagoons (often referred to as &quot;salt ponds&quot;) in southern Rhode Island. Geography. Quonochontaug Pond is the deepest and most saline of the salt ponds.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Quonochontaug Pond. Quonochontaug () is a coastal lagoon in the towns of Charlestown and Westerly, both in Washington County, Rhode Island, United States. It is the most saline of nine such lagoons (often referred to as &quot;salt ponds&quot;) in southern Rhode Island. Geography. Quonochontaug Pond is the deepest and most saline of the salt ponds.

Geographic entities mentioned:
surface_form: quonochontaug pond
instance_of: Lake
countries: United States
coordinates: lat: 41.3417
lon: -71.7217
Earlier it was believed to occur in Burundi also, but this is quite doubtful. This killifish's native range are the drainage basins of Lake Kyoga and Victoria, and the Aswa, Bubu and Malagarasi River. Its natural habitats are rivers, swamps, freshwater lakes and marshes, temporary pools, floodplains and inland deltas.

Geographic entities mentioned:
surface_form: Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Lake Otis (Florida). Lake Otis is a natural freshwater lake located on the east side of Winter Haven, Florida. The Polk County Water Atlas says the lake sometimes is known as Little Otis, but this is confirmed nowhere else. The main part of the lake is somewhat rectangular in shape and on the south side of the main section of the lake is a long tail-shaped cove. Lake Otis has a surface.

Geographic entities mentioned:
surface_form: lake otis (florida)
instance_of: Lake
countries: United States
coordinates: lat: 28.011
lon: -81.7106
Lake Otis (Florida). Lake Otis is a natural freshwater lake located on the east side of Winter Haven, Florida. The Polk County Water Atlas says the lake sometimes is known as Little Otis, but this is confirmed nowhere else. The main part of the lake is somewhat rectangular in shape and on the south side of the main section of the lake is a long tail-shaped cove. Lake Otis has a surface.

Geographic entities mentioned:
surface_form: lake otis
instance_of: Lake
countries: United States
coordinates: lat: 28.011
lon: -81.7106
The Polk County Water Atlas says the lake sometimes is known as Little Otis, but this is confirmed nowhere else. The main part of the lake is somewhat rectangular in shape and on the south side of the main section of the lake is a long tail-shaped cove. Lake Otis has a surface. It is connected on its northeast side to nearby Lake Link by a canal. This is the closest point between the two lakes.

Geographic entities mentioned:
surface_form: lake otis
instance_of: Lake
countries: United States
coordinates: lat: 28.011
lon: -81.7106
It is connected on its northeast side to nearby Lake Link by a canal. This is the closest point between the two lakes. Other than where the shore where the two lakes are very close, Lake Otis is completely surrounded by residences. Lakewood Causeway runs between the two lakes. To the south of this area is a gated community that can be accessed by the public during the daytime.

Geographic entities mentioned:
surface_form: lake otis
instance_of: Lake
countries: United States
coordinates: lat: 28.011
lon: -81.7106
To the south of this area is a gated community that can be accessed by the public during the daytime. Most of the south cove is surrounded by another gated community and the public is prevented from entering it by gates that are closed all the time. Lake Otis has no public boat ramps or swimming areas. In fact, there are no areas of the shore accessible to the public.

Geographic entities mentioned:
surface_form: lake otis
instance_of: Lake
countries: United States
coordinates: lat: 28.011
lon: -81.7106
Lake Otis has no public boat ramps or swimming areas. In fact, there are no areas of the shore accessible to the public. The entire shore of the lake, other than the area near Lake Link, has steep banks. The Hook and Bullet website, however, says Lake Otis contains largemouth bass, bluegill and crappie.

Geographic entities mentioned:
surface_form: lake otis
instance_of: Lake
countries: United States
coordinates: lat: 28.011
lon: -81.7106
The Moolah-Corinya fire was &quot;the largest fire ever contained by man in New South Wales without the help of the weather.&quot; It burned and its perimeter was over. Area burned:. The fire reached Barkly Tableland, Victoria River district, near Newcastle Waters. The bushfire season was defined as October 1974 to February 1975. Area burned:. 95 cattle, 6,850 sheep lost.

Geographic entities mentioned:
surface_form: Barkly Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -19
lon: 138
KV11. Tomb KV11 is the tomb of Pharaoh Ramesses III. It is located in the main valley of the Valley of the Kings. The tomb was originally started by Setnakhte, but abandoned when it unintentionally broke into the earlier tomb of Amenmesse (KV10). Setnakhte was buried in KV14. The tomb KV11 was later restarted and extended and on a different axis for Ramesses III.

Geographic entities mentioned:
surface_form: Valley of the Kings
instance_of: Valley
countries: Egypt
coordinates: lat: 25.74025
lon: 32.602358
Poor Valley. Poor Valley is a valley in Grainger County, Tennessee, Hawkins County, Tennessee, Hancock County, Tennessee, Scott County, Virginia, Washington County, Virginia, and Smyth County, Virginia, United States. A variant name is Big Poor Valley. Poor Valley was named from the poor soil found there.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: poor valley
instance_of: Valley
countries: United States
coordinates: lat: 36.185555555556
lon: -83.695555555556
A variant name is Big Poor Valley. Poor Valley was named from the poor soil found there. A 1,900-2,200 acre portion of the valley in western Hawkins County was proposed and planned as state park known as Poor Valley State Park in order to promote economic development efforts in the upper East Tennessee region, the plan would stall in the 1970s.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: poor valley
instance_of: Valley
countries: United States
coordinates: lat: 36.185555555556
lon: -83.695555555556
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Poor Valley. Poor Valley is a valley in Grainger County, Tennessee, Hawkins County, Tennessee, Hancock County, Tennessee, Scott County, Virginia, Washington County, Virginia, and Smyth County, Virginia, United States. A variant name is Big Poor Valley. Poor Valley was named from the poor soil found there.

Geographic entities mentioned:
surface_form: poor valley
instance_of: Valley
countries: United States
coordinates: lat: 36.185555555556
lon: -83.695555555556
A variant name is Big Poor Valley. Poor Valley was named from the poor soil found there. A 1,900-2,200 acre portion of the valley in western Hawkins County was proposed and planned as state park known as Poor Valley State Park in order to promote economic development efforts in the upper East Tennessee region, the plan would stall in the 1970s.

Geographic entities mentioned:
surface_form: poor valley
instance_of: Valley
countries: United States
coordinates: lat: 36.185555555556
lon: -83.695555555556
The division broke through German defenses on the Neisse during the Berlin Offensive and on 25 April made contact with the American 69th Infantry Division at Torgau on the Elbe River on 25 April 1945, splitting Germany into two separate parts, an event that became known as Elbe Day. The first contact was made between patrols near Strehla, when U.S.

Geographic entities mentioned:
surface_form: Elbe River
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Cathedral in the Desert. The Cathedral in the Desert is a natural formation, sometimes referred to as an amphitheater, buried under Lake Powell in Glen Canyon. Due to the Southwestern North American megadrought, the cathedral has been visible in 2005 and 2019. Lake Powell must drop to 3,605 feet for the cathedral floor to be visible.

Geographic entities mentioned:
surface_form: Glen Canyon
instance_of: Valley
countries: United States
coordinates: lat: 36.86443
lon: -111.58794
Walter Moberly had discovered Eagle Pass just to the west, and based on suggestions in Moberly's reports, Rogers started out from what is now Revelstoke, up the Illecillewaet River. On May 28, 1881, the party followed a branch of the river past &quot;Syndicate Peak&quot; (now Mount Sir Donald), discovering a large level opening between the mountains where the waters flowed east and west.

Geographic entities mentioned:
surface_form: Mount Sir Donald
instance_of: Mountain
countries: Canada
coordinates: lat: 51.2631
lon: -117.431
(Some secondary sources state that Rogers only saw the pass from a distance, but this is contradicted by first-hand reports.) To get a better view of the landscape, Rogers, his nephew A.L. Rogers and some of their Shuswap guides then climbed to the crest of a nearby mountain ridge, later identified as the ridge between Mount Macdonald and Avalanche Mountain.

Geographic entities mentioned:
surface_form: Mount Macdonald
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3083
lon: -117.472
surface_form: Avalanche Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.2881
lon: -117.469
Moberly advocated Howse Pass. During the time it took to determine a practicable Kicking Horse/Selkirks route, the railhead had advanced up the Bow Valley making it too late to use Howse, which required an access from the North Saskatchewan River Valley.

Geographic entities mentioned:
surface_form: Bow Valley
instance_of: Valley
countries: Canada
coordinates: lat: 51.1671
lon: -115.48
Shortly after exiting the lake, it drops over impressive Statlu Falls, which is difficult to view without putting yourself in real danger. People have died when they have slipped and fallen over the falls. After the falls, the river turns south, eventually flowing into Chehalis Lake. After it exits the lake it continues its journey south to the Harrison River.

Geographic entities mentioned:
surface_form: Chehalis Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.45
lon: -122.017
There is a small ski resort, Hemlock Valley, on the eastern side of the Chehalis River basin. A road penetrates the northeast rim of the range into the Harrison Lake basin and on to historic Port Douglas, at the head of that lake, and beyond up the Lillooet River via Skookumchuck Hot Springs to Pemberton&ndash;Mount Currie.

Geographic entities mentioned:
surface_form: Harrison Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.55
lon: -121.83333333333
Geography. Horní Moštěnice is located about south of Přerov and southeast of Olomouc. The western part of the municipality lies in the Upper Morava Valley, the eastern part lies in the Moravian-Silesian Foothills. The highest point is the hill Švédské šance at above sea level. The Moštěnka River flows through the municipality. History. The first written mention of Horní Moštěnice is from 1141.

Geographic entities mentioned:
surface_form: Upper Morava Valley
instance_of: Valley
countries: Czech Republic
coordinates: lat: 49.29417
lon: 17.45179
It's located in the city of Rio Grande, in the Brazilian state of Rio Grande do Sul. It's the third largest in the country. The land access system to the port is made up of BR-392, BR-471 and BR-116. It is on the right bank of the North Channel, which connects Lagoa dos Patos with the Atlantic Ocean. The port bar is kept open by two breakwaters built at the mouth of the access channel.

Geographic entities mentioned:
surface_form: Lagoa dos Patos
instance_of: Lake
countries: Brazil
coordinates: lat: -31.15
lon: -51.39
Visočica (hill). Visočica (; also known as &quot;Brdo Grad&quot;, &quot;Hill Town&quot;) is a 213-metre-high hill in Bosnia and Herzegovina which is the site of the Old town of Visoki. Since at least 2005, the hill has been the subject of a pseudoarchaeological belief that it is part of an ancient man-made pyramid complex. This notion is rejected by archaeologists and geologists.

Geographic entities mentioned:
surface_form: visočica (hill)
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.978333333333
lon: 18.177777777778
Visočica (hill). Visočica (; also known as &quot;Brdo Grad&quot;, &quot;Hill Town&quot;) is a 213-metre-high hill in Bosnia and Herzegovina which is the site of the Old town of Visoki. Since at least 2005, the hill has been the subject of a pseudoarchaeological belief that it is part of an ancient man-made pyramid complex. This notion is rejected by archaeologists and geologists.

Geographic entities mentioned:
surface_form: visočica
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.978333333333
lon: 18.177777777778
surface_form: brdo grad
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.978333333333
lon: 18.177777777778
surface_form: grad
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.978333333333
lon: 18.177777777778
This idea originated with Houston-based expatriate Bosnian author and businessman Semir Osmanagić who has since turned the site into a tourist destination. All scientific investigations have concluded that Visočica hill and the surrounding hills are natural geological formations known as a flatirons, and no scientific study has demonstrated the existence of man-made pyramids in Bosnia.

Geographic entities mentioned:
surface_form: visočica
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.978333333333
lon: 18.177777777778
Archaeologists have criticised the Bosnian authorities for supporting the pyramid claim saying, &quot;This scheme is a cruel hoax on an unsuspecting public and has no place in the world of genuine science.&quot;
As of 2017, Osmanagić continues to run his project at Visočica, and to link the hill to long-standing non-scientific notions such as free energy and ancient astronauts.

Geographic entities mentioned:
surface_form: visočica
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.978333333333
lon: 18.177777777778
Arrowhead Mountain (California). Arrowhead Mountain is a mountain between Sonoma and Napa Counties in California, United States. It is part of the Mayacamas Mountains, a subrange of the California Coast Ranges. Geography.

Geographic entities mentioned:
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.274166666667
lon: -122.40027777778
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.670555555556
lon: -73.12
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.578333333333
lon: -111.66
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.1075
lon: -113.18361111111
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.75761
lon: -120.96538
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.8825
lon: -111.4665
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.513055555556
lon: -105.69138888889
Arrowhead Mountain (California). Arrowhead Mountain is a mountain between Sonoma and Napa Counties in California, United States. It is part of the Mayacamas Mountains, a subrange of the California Coast Ranges. Geography.

Geographic entities mentioned:
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.274166666667
lon: -122.40027777778
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.670555555556
lon: -73.12
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.578333333333
lon: -111.66
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.1075
lon: -113.18361111111
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.75761
lon: -120.96538
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.8825
lon: -111.4665
surface_form: sonoma
instance_of: Mountain
countries: United States
coordinates: lat: 38.3231
lon: -122.575
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.513055555556
lon: -105.69138888889
Legend. According to local legend native american tribes believed that the Arrowhead symbol was placed there by the Great Spirit to guide them to their desrined homeland - similar in purpose to the Israiltes' Pillar of Fire. The arrow was said to mark sacred ground near the hot springs below, known for their healing properties. Over time, forest fires have contributed to erosion of the formation.

Geographic entities mentioned:
surface_form: spirit
instance_of: Lake
countries: United States
coordinates: lat: 46.273055555556
lon: -122.135
Arrowhead Mountain is a mountain between Sonoma and Napa Counties in California, United States. It is part of the Mayacamas Mountains, a subrange of the California Coast Ranges. Geography. The mountain lies near the boundary of the Moon Mountain District Sonoma County AVA, a federally recognized wine-growing region, and plays a minor role in the AVA’s boundary description. Legend.

Geographic entities mentioned:
surface_form: sonoma
instance_of: Mountain
countries: United States
coordinates: lat: 38.3231
lon: -122.575
It forms the border between Belgium and Luxembourg for north of Martelange. West of Esch-sur-Sûre it flows into an artificial lake, the Upper Sûre Lake created by the Esch-sur-Sûre Dam, which gives its (French) name to the Luxembourgish commune of Lac de la Haute-Sûre.

Geographic entities mentioned:
surface_form: Upper Sûre Lake
instance_of: Lake
countries: Luxembourg
coordinates: lat: 49.9
lon: 5.866666666666667
Ol Doinyo Lengai. Ol Doinyo Lengai is an active volcano in northern Tanzania. It consists of a volcanic cone with two craters, the northern of which has erupted during historical time. Uniquely for volcanoes on Earth, it has erupted natrocarbonatite, an unusually low temperature and highly fluid type of magma. Eruptions in 2007–2008 affected the surrounding region. Name.

Geographic entities mentioned:
surface_form: doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: ol doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
The southern crater is inactive and sometimes filled with water. White volcanic ash deposits cover the slopes of the volcano, which have large fractures on the western flank. There are parasitic vents on Ol Doinyo Lengai's flanks, such as Kirurum Crater on the western, the Nasira cones on the northern, Dorobo crater on the northeastern, and Oltatwa Crater on the eastern flank.

Geographic entities mentioned:
surface_form: doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: ol doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
The Natron Fault, the western boundary of the Gregory Rift in the area, passes just southwest of the volcano. The volcano is part of the Ngorongoro volcanic highland, a system of volcanoes that were active from the Miocene to present, and which includes the Ngorongoro and other volcanoes. Over time, volcanic activity shifted northeastward to the present-day Ol Doinyo Lengai.

Geographic entities mentioned:
surface_form: doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: ol doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
Over time, volcanic activity shifted northeastward to the present-day Ol Doinyo Lengai. Other volcanoes in the area are Gelai to the northeast and Ketumbeine southeast of Ol Doinyo Lengai; further away are the Olduvai Gorge to the west and Kilimanjaro mountain east of the volcano. Composition. Most of the volcanic cone is formed by melilite, nephelinite, and phonolite.

Geographic entities mentioned:
surface_form: doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: ol doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
The properties of Ol Doinyo Lengai's magmas have been used as an analogue for the conditions on carbon planets; these are planets which are rich in carbon.

Geographic entities mentioned:
surface_form: doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: ol doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
There appear to be two magma reservoirs under the volcano, and its plumbing system is complex, involving regional tectonic structures. Volcanic gases. Volcanic gas sampled at Ol Doinyo Lengai consists mostly of water vapor and carbon dioxide and originates in the mantle. The volcano is a major source of volcanic carbon dioxide, producing about of. Eruption history.

Geographic entities mentioned:
surface_form: doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: ol doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
Volcanic gases. Volcanic gas sampled at Ol Doinyo Lengai consists mostly of water vapor and carbon dioxide and originates in the mantle. The volcano is a major source of volcanic carbon dioxide, producing about of. Eruption history. Radiometric dates obtained by geologists for the start of volcanic eruptions at Ol Doinyo Lengai range from more than 500,000 to 22,000 years ago.

Geographic entities mentioned:
surface_form: doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: ol doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
It formed in two stages, Lengai I consisting of phonolite that forms about 60% of the volume of Ol Doinyo Lengai and crops out in its southern part, and Lengai II formed by nephelinitic rocks; growth of the volcanic cone was complete about 15,000 years ago, when the Naisiusiu Beds were emplaced in the Olduvai Gorge.

Geographic entities mentioned:
surface_form: doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: ol doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
The oldest natrocarbonatite lavas date to 1,250 years before present. An eruption 3,000-2,500 years before present produced a tephra fallout west of Ol Doinyo Lengai, that is presently being eroded by wind and forming dunes including the Shifting Sands of the Olduvai Gorge.

Geographic entities mentioned:
surface_form: doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: ol doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
Steam jets have also been observed. There is evidence of underground magma intrusions. Satellite observations have shown deformation of the volcano during eruptions, and ground-based observations have identified movement in neighboring fault systems such as the Natron Fault caused by magma originating at Ol Doinyo Lengai. Recent eruptive period: 1983 and subsequent.

Geographic entities mentioned:
surface_form: doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: ol doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333