Sarmila/GeoWiki-Features huggingface dataset:
Later alternative waste disposal techniques became available, e.g. very wide sewer pipes that were laid at the bottom of the streams. In the 1920s the Doode Stroom was the first part of the Binnendieze that was filled up after a concrete sewer pipe had been installed. There was some regret, but there were no protests, because public health benefited.

Geographic entities mentioned:
surface_form: binnendieze
instance_of: Watercourse
countries: Netherlands
coordinates: lat: 51.68527777777778
lon: 5.308055555555556
Nevertheless, even before World War II the possibilities for tourism were somewhat understood, and in the mid 1930s the first boat trips for tourists were organized. The real threat for the Binnendieze would come from the growth of automobile traffic after World War II. In 's-Hertogenbosch it led to the Marktroom and old city moat getting filled up without much protest in 1962.

Geographic entities mentioned:
surface_form: binnendieze
instance_of: Watercourse
countries: Netherlands
coordinates: lat: 51.68527777777778
lon: 5.308055555555556
This plan entailed motorways that cut off corners of the city center, and 'breakthrough's'. All in all about 25% of all buildings in the center would be destroyed, the Binnenhaven would be filled up, and nothing much would be left of the Binnendieze. It was presented only 6 days before it would be treated in the municipal council.

Geographic entities mentioned:
surface_form: binnendieze
instance_of: Watercourse
countries: Netherlands
coordinates: lat: 51.68527777777778
lon: 5.308055555555556
This changed in September 1966, when Hein Bergé and Jan van der Eerden got elected to the municipal council for the new party Beter Bestuur (better government). Bergé and Van der Eerden struggled for the preservation of the city center, and in particular for preserving the Binnendieze. Almost immediately after getting elected they asked for a report that had been made about the Binnendieze.

Geographic entities mentioned:
surface_form: binnendieze
instance_of: Watercourse
countries: Netherlands
coordinates: lat: 51.68527777777778
lon: 5.308055555555556
Bergé and Van der Eerden struggled for the preservation of the city center, and in particular for preserving the Binnendieze. Almost immediately after getting elected they asked for a report that had been made about the Binnendieze. It took the municipal government 23 months to deliver this report to the council.

Geographic entities mentioned:
surface_form: binnendieze
instance_of: Watercourse
countries: Netherlands
coordinates: lat: 51.68527777777778
lon: 5.308055555555556
Later it was found that the existing report had been suppressed and a new report had been made. The new report combined the future of the Binnendieze and the construction of a sewer system, which the city center did not have yet. The report advised that the cheapest way to realize the sewer system was to use the Binnendieze as a location and then to fill it up.

Geographic entities mentioned:
surface_form: binnendieze
instance_of: Watercourse
countries: Netherlands
coordinates: lat: 51.68527777777778
lon: 5.308055555555556
The new report combined the future of the Binnendieze and the construction of a sewer system, which the city center did not have yet. The report advised that the cheapest way to realize the sewer system was to use the Binnendieze as a location and then to fill it up. It would also create room for roads, and parking space.

Geographic entities mentioned:
surface_form: binnendieze
instance_of: Watercourse
countries: Netherlands
coordinates: lat: 51.68527777777778
lon: 5.308055555555556
It would also create room for roads, and parking space. Only a segment of the Vughterstroom and two small fragments of the Groote Stroom would remain. In January 1969 the fate of the Binnendieze would be decided in a meeting of the municipal council. Meanwhile the Rijksdienst voor Monumentenzorg (national heritage service), informed by Beter Bestuur had a different opinion.

Geographic entities mentioned:
surface_form: binnendieze
instance_of: Watercourse
countries: Netherlands
coordinates: lat: 51.68527777777778
lon: 5.308055555555556
Meanwhile the Rijksdienst voor Monumentenzorg (national heritage service), informed by Beter Bestuur had a different opinion. On the third day of the debate, a sketch arrived from The Hague, designating large parts of the Binnendieze as protected cityscape. Despite heavy opposition the plan survived the debate with a big majority.

Geographic entities mentioned:
surface_form: binnendieze
instance_of: Watercourse
countries: Netherlands
coordinates: lat: 51.68527777777778
lon: 5.308055555555556
Taking advantage of this, three northern Chaulukya feudatories in the Marwar region formed an alliance and rebelled against the imperial rule. These included Udayasimha, Somasimha and Dharavarsha (the Paramara chief of Abu). In the ensuing battle, Udayasimha was wounded by the Chaulukya general Lavanaprasada, but the conflict appears to have ended with an advantage for Udayasimha.

Geographic entities mentioned:
surface_form: Abu
instance_of: Mountain
countries: India
coordinates: lat: 24.5925
lon: 72.708333333333
Skipperhuset. Skipperhuset refers to a small cluster of historic buildings including an 18th-century former royal boathouse located in Fredensborg Palace gardens on the southeastern shoreline of Lake Esrum at Fredensborg, Denmark. The buildings are now home to the Lake Esrum Boat Service and a restaurant. History. Frederick IV's new Fredensborg Palace was completed in 1722.

Geographic entities mentioned:
surface_form: Lake Esrum
instance_of: Lake
countries: Denmark
coordinates: lat: 56.00778
lon: 12.37917
Payukosap Lake. Payukosap Lake is a glacial lake above the confluence of Holt Lake and Mistik Creek, approximately northeast of Bakers Narrows. As a segment of the Mistik Creek, it is part of the Nelson River watershed, in the Hudson Bay drainage basin in the Northern Region of Manitoba, Canada.

Geographic entities mentioned:
surface_form: Mistik Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.6256
lon: -101.568
surface_form: payukosap lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.79583333
lon: -101.3827778
Payukosap Lake. Payukosap Lake is a glacial lake above the confluence of Holt Lake and Mistik Creek, approximately northeast of Bakers Narrows. As a segment of the Mistik Creek, it is part of the Nelson River watershed, in the Hudson Bay drainage basin in the Northern Region of Manitoba, Canada.

Geographic entities mentioned:
surface_form: payukosap lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.79583333
lon: -101.3827778
Payukosap Lake. Payukosap Lake is a glacial lake above the confluence of Holt Lake and Mistik Creek, approximately northeast of Bakers Narrows. As a segment of the Mistik Creek, it is part of the Nelson River watershed, in the Hudson Bay drainage basin in the Northern Region of Manitoba, Canada.

Geographic entities mentioned:
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: mistik creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.6256
lon: -101.568
The lake is situated on the well known &quot;Mistik Creek Loop&quot;, a remote canoe route in length which can be paddled in four days. &quot;Payukosap&quot; means 'eleven' in Cree, as all of the fourteen lakes on Mistik Creek are named in numeric order in Cree.

Geographic entities mentioned:
surface_form: mistik creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.6256
lon: -101.568
Historic structures include houses, farms, stores, and other typical buildings dating from the 19th and early 20th centuries. Prehistoric resources include ceremonial and settlement sites and feature Nacoochee Mound, an earthwork platform mound on the banks of the Chattahoochee River. This area is adjacent to the Nacoochee Valley Historic District.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Gobba di Rollin. Gobba di Rollin (Italian, French: &quot;Dos de Rollin&quot;; 3,898 m) is a mountain of the Pennine Alps, straddling the border between Switzerland and Italy. It is located south of the Breithorn and it is largely covered by ice, the summit area being particularly flat.

Geographic entities mentioned:
surface_form: Breithorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.941111111111
lon: 7.7472222222222
surface_form: breithorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.941111111111
lon: 7.7472222222222
Gobba di Rollin is notable as having the highest ski lift in Europe on its top, since it is the highest point of the ski area &quot;Matterhorn Glacier Paradise&quot; on the Theodul Glacier, between Zermatt and Breuil-Cervinia. It is connected to both the Klein Matterhorn and Testa Grigia by ski lifts.

Geographic entities mentioned:
surface_form: Klein Matterhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.938333333333
lon: 7.7297222222222
surface_form: Testa Grigia
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.9353
lon: 7.7075
surface_form: matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
surface_form: testa grigia
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.9353
lon: 7.7075
It is located south of the Breithorn and it is largely covered by ice, the summit area being particularly flat. On the north side is the Breithorn Plateau of the Theodul Glacier, on the east side is the Verraz Glacier and on the south is the Glacier d'Aventine.

Geographic entities mentioned:
surface_form: breithorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.941111111111
lon: 7.7472222222222
On the north side is the Breithorn Plateau of the Theodul Glacier, on the east side is the Verraz Glacier and on the south is the Glacier d'Aventine. Gobba di Rollin is notable as having the highest ski lift in Europe on its top, since it is the highest point of the ski area &quot;Matterhorn Glacier Paradise&quot; on the Theodul Glacier, between Zermatt and Breuil-Cervinia.

Geographic entities mentioned:
surface_form: matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
It is connected to both the Klein Matterhorn and Testa Grigia by ski lifts. The shortest access is from the Klein Matterhorn station (3,820 m), less than two kilometres away, from where it can be easily reached by a piste on the glacier. The summit has even been reached via the Theodul Pass by 4x4 vehicles, a European record.

Geographic entities mentioned:
surface_form: matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
Gobba di Rollin. Gobba di Rollin (Italian, French: &quot;Dos de Rollin&quot;; 3,898 m) is a mountain of the Pennine Alps, straddling the border between Switzerland and Italy. It is located south of the Breithorn and it is largely covered by ice, the summit area being particularly flat.

Geographic entities mentioned:
surface_form: dos de rollin
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.924166666667
lon: 7.7344444444444
surface_form: gobba di rollin
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.924166666667
lon: 7.7344444444444
Gobba di Rollin. Gobba di Rollin (Italian, French: &quot;Dos de Rollin&quot;; 3,898 m) is a mountain of the Pennine Alps, straddling the border between Switzerland and Italy. It is located south of the Breithorn and it is largely covered by ice, the summit area being particularly flat.

Geographic entities mentioned:
surface_form: gobba di rollin
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.924166666667
lon: 7.7344444444444
The river Figgjoelva empties into the North Sea in Klepp. The small island of Feistein lies off shore and is the site of the Feistein Lighthouse. There are two large lakes in Klepp: Orrevatnet and Frøylandsvatnet. Transportation. The Sørlandet railway line, historically called the Jæren Line, runs through Klepp along lake Frøylandsvatnet.

Geographic entities mentioned:
surface_form: Orrevatnet
instance_of: Lake
countries: Norway
coordinates: lat: 58.749444444444
lon: 5.5383333333333
surface_form: Frøylandsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 58.749722222222
lon: 5.6758333333333
There are two large lakes in Klepp: Orrevatnet and Frøylandsvatnet. Transportation. The Sørlandet railway line, historically called the Jæren Line, runs through Klepp along lake Frøylandsvatnet. The village of Klepp stasjon, east of Kleppe, is built around the train station Klepp Station. The nearby Oksnevadporten Station is the other railway station in Klepp. Economy.

Geographic entities mentioned:
surface_form: Frøylandsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 58.749722222222
lon: 5.6758333333333
Geography. Vennanthur is located at 11.5206° N, 78.0872°E. It has an average elevation of 218 metres (726 ft). Vennandur lake is located west of the town. Vennandur is close to the Alavaimalai Hills, which are part of the Eastern Ghats. The closest river is the Thirumanimutharu River, which rises on Mount Yercaud. Namakkal, the district capital, is located around 39 km from Vennanthur.

Geographic entities mentioned:
surface_form: Alavaimalai
instance_of: Mountain
countries: India
coordinates: lat: 11.46963889
lon: 78.11952778
Initially the settlement was lower but due to a plague epidemic that broke out in the middle of the 17th century the surviving inhabitants left their original homes and settled in the livestock settlement located in the current location of the village. The village was included in the treaty that granted autonomy to the so-called Agrafa, a mountainous region in Central Greece during Ottoman times.

Geographic entities mentioned:
surface_form: Agrafa
instance_of: Mountain
countries: Greece
coordinates: lat: 39.13972222
lon: 21.64944444
When the Europeans first arrived, an estimated 500,000 tule elk roamed these regions, but by 1870 they were thought to be extirpated. In 1874–1875 a single breeding pair was discovered in the tule marshes of Buena Vista Lake in the southern San Joaquin Valley. Conservation measures were taken to protect the species in the 1970s. Today, the wild population exceeds 4,000.

Geographic entities mentioned:
surface_form: Buena Vista Lake
instance_of: Lake
countries: United States
coordinates: lat: 35.1919
lon: -119.295
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Today, the wild population exceeds 4,000. Tule elk can reliably be found in Carrizo Plain National Monument, Point Reyes National Seashore, portions of the Owens Valley from Lone Pine to Bishop, on Coyote Ridge in Santa Clara Valley, San Jose, California and in Pacheco State Park and areas surrounding San Luis Reservoir near Los Banos, California. Description.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
surface_form: Santa Clara Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.366944444444
lon: -121.98388888889
California Department of Fish and Wildlife records show recent tule elk bulls on Grizzly Island in Suisun Bay weigh up to. This is a similar size to Roosevelt elk bulls which weigh between and. Wildlife biologist Dale McCullough described an elk transplanted from Buttonwillow in the San Joaquin Valley to a golf course in Monterey that grew to the size of a Rocky Mountain elk. Also hunter H. C.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Unrestricted hunting further reduced the herds. By the time elk hunting was banned by the State Legislature in 1873, the tule elk was believed to be extinct. California cattle baron Henry Miller protected tule elk after a pair was discovered on his ranch in the tule marshes near Buena Vista Lake by game warden A. C. Tibbett in 1874.

Geographic entities mentioned:
surface_form: Buena Vista Lake
instance_of: Lake
countries: United States
coordinates: lat: 35.1919
lon: -119.295
By 1895, habitat loss and poaching had reduced the elk population to only 28. In the years that followed, the elk were transplanted 21 times, with each attempt failing to establish free-ranging herds. In 1933, rancher Walter Dow took a small group of penned elk from Yosemite to his ranch in Owens Valley, east of the Sierra Nevada. Although not native habitat for the elk, they thrived.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
Although not native habitat for the elk, they thrived. In the same year, the state put a small herd at Cache Creek. This herd has not fared well due to poor range conditions. This herd may have interbred with the Rocky Mountain elk which were introduced near Mount Shasta. In 1960, the state held a hearing in Owens Valley to determine how many elk should be allowed to live there.

Geographic entities mentioned:
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
A herd was established at the San Luis Wildlife Refuge in 1974, and elk were released at the Concord Naval Weapons Station in 1977. In 1978, herds were established at Mount Hamilton in Santa Clara County, Lake Pillsbury in Lake County, Jawbone Canyon in Kern County, Point Reyes National Seashore, Fort Hunter Liggett Military Reservation, and Camp Roberts. Historic range and current population.

Geographic entities mentioned:
surface_form: Lake Pillsbury
instance_of: Lake
countries: United States
coordinates: lat: 39.4072
lon: -122.9575
Personal. Teeter and his wife, Kristen, a dancer and teacher of jazz and contemporary dance classes, married at a Sonoma Valley winery in 1998. Cast members from the tour of &quot;The Wizard of Oz&quot; attended. They celebrated their 15th wedding anniversary in 2013. They have four children.

Geographic entities mentioned:
surface_form: Sonoma Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.3667
lon: -122.5
California's 3rd congressional district is a U.S. congressional district in California. It includes the northern Sierra Nevada and northeastern suburbs of Sacramento, stretching south to Death Valley. It encompasses Alpine, Inyo, Mono, Nevada, Placer (where the majority of the district’s population lives), Plumas, and Sierra counties, as well as parts of El Dorado, Sacramento, and Yuba counties.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
The district is represented in the House of Representatives by Republican Kevin Kiley. Prior to redistricting in 2020, the 3rd district encompassed most of the Sacramento Valley north and west of Sacramento. It covered all of Colusa, Sutter and Yuba counties, most of Glenn, Lake, Solano and Yolo counties and a portion of Sacramento County.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
The district was represented by John Garamendi, a Democrat. Recent history. The 3rd district once extended up the Sacramento Valley from Sacramento to take in rural territory up to Tehama County. Once a Democratic bastion, the district was pushed into more rural and Republican-leaning territory after the 1990 census, and finally elected a Republican in 1998.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
In March 2023, they announced that she was pregnant and expecting their first child. The couple got engaged later in the year, and Leotta gave birth to their first daughter, named Aria, on 16 August 2023. They were married on 22 June 2024, at a private ceremony on the island of Vulcano near Sicily in Leotta's native Italy.

Geographic entities mentioned:
surface_form: Vulcano
instance_of: Mountain
countries: Italy
coordinates: lat: 38.4042
lon: 14.9658
Fernando de Mendoza Mate de Luna. Fernando de Mendoza Mate de Luna (1610 – 1692) was born in Cadiz. He served multiple Governorships including; Governor of Isla Margarita (Venezuela) 1649-54, Governor of Tucuman (Argentina)1681-86. He founded the city of San Fernando Valley of Catamarca in 1683, and he authorized the transfer of Tucuman. He was later appointed mayor of Santiago de Chile.

Geographic entities mentioned:
surface_form: San Fernando
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
National Army detachments were also withdrawn from southern Xinjiang, leaving the strategic city of Aksu and opening the road from Ürümqi to the Kashgar region. That allowed the Kuomintang to send 70,000 troops from 1946 to 1947 and quell the rebellion in the Pamir Mountains. The rebellion was broken on 19 August 1945 in the Sariqol area of Taghdumbash Pamir.

Geographic entities mentioned:
surface_form: Taghdumbash Pamir
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 37.2
lon: 75.4
Allegheny Parkway. The Allegheny Parkway was a proposed scenic highway, intended to extend from Harpers Ferry, West Virginia, to the Cumberland Gap, to be managed by the National Park Service. It was seen as a complementary project to the Skyline Drive and Blue Ridge Parkway on the east side of the Shenandoah Valley.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Proceeding generally west through Morgan County in the Ridge-and-Valley Appalachians, the route would pass near Berkeley Springs, along the crest of Cacapon Mountain at Cacapon State Park, meeting the Allegheny Front just south of Keyser. From Keyser the route turned south to follow the Allegheny Front, passing Blackwater Falls and Canaan Valley.

Geographic entities mentioned:
surface_form: Cacapon Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.4436
lon: -78.3469
Proceeding generally west through Morgan County in the Ridge-and-Valley Appalachians, the route would pass near Berkeley Springs, along the crest of Cacapon Mountain at Cacapon State Park, meeting the Allegheny Front just south of Keyser. From Keyser the route turned south to follow the Allegheny Front, passing Blackwater Falls and Canaan Valley.

Geographic entities mentioned:
surface_form: Canaan Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.126666666667
lon: -79.378055555556
From Keyser the route turned south to follow the Allegheny Front, passing Blackwater Falls and Canaan Valley. Farther south, the parkway was to pass near Seneca Rocks, Spruce Knob, the Sinks of Gandy, Droop Mountain Battlefield, White Sulphur Springs, Bluestone Lake in the New River valley and Breaks Interstate Park before ending at Cumberland Gap National Historical Park.

Geographic entities mentioned:
surface_form: Seneca Rocks
instance_of: Landform
countries: United States
coordinates: lat: 38.8347
lon: -79.3661
surface_form: Spruce Knob
instance_of: Mountain
countries: United States
coordinates: lat: 38.6999
lon: -79.5328
Büyen. The Büyen (, &quot;Büien&quot;) is a river of Kazakhstan. Its source is in the Dzungarian Alatau. It flows to the north, parallel to the Aksu to its east, and vanishes in the Jalkum desert south of Lake Balkhash. The Bronze Age settlement Tasbas is located in the upper Büyen valley.

Geographic entities mentioned:
surface_form: Lake Balkhash
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 46.540833333333
lon: 74.878888888889
It then spread northwards, and was detected in Port Philip Bay, Victoria, where it was observed to reach up to 12 million individuals over a two-year span, and is now considered established there. It has also been seen in San Remo, Anderson Inlet, Waratah Bay, Tidal River and the Gippsland Lakes area, but measures are being taken to ensure that they do not get established in these areas.

Geographic entities mentioned:
surface_form: Gippsland Lakes
instance_of: Group of lakes
countries: Australia
coordinates: lat: -38
lon: 147.65
Donaldson Peak. Donaldson Peak, at above sea level is the eighth-highest peak in the U.S. state of Idaho and the seventh-highest in the Lost River Range. The peak is located in Salmon-Challis National Forest in Custer County. It is east of Mount Church, its line parent and west of Mount Breitenbach. Named for Charles R. Donaldson (1919-1987), former Chief Justice of the Idaho Supreme Court.

Geographic entities mentioned:
surface_form: Mount Breitenbach
instance_of: Mountain
countries: United States
coordinates: lat: 44.0666
lon: -113.673
surface_form: mount church
instance_of: Mountain
countries: United States
coordinates: lat: 44.0661
lon: -113.713
surface_form: mount church
instance_of: Mountain
countries: United States
coordinates: lat: 62.8792
lon: -150.683
Donaldson Peak. Donaldson Peak, at above sea level is the eighth-highest peak in the U.S. state of Idaho and the seventh-highest in the Lost River Range. The peak is located in Salmon-Challis National Forest in Custer County. It is east of Mount Church, its line parent and west of Mount Breitenbach. Named for Charles R. Donaldson (1919-1987), former Chief Justice of the Idaho Supreme Court.

Geographic entities mentioned:
surface_form: donaldson peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.0646
lon: -113.698
The Trombay Hills occupy a large portion of Trombay on the eastern part of the city. The highest hill is about above sea level. The Powai Hills are present north of the city. The Borivali National Park occupies most of the region. The Vihar and Tulsi Lakes are present within the hills. The highest point of the metropolis, at, is located in this region. Lakes. There are three lakes in the city.

Geographic entities mentioned:
surface_form: Tulsi Lake
instance_of: Lake
countries: India
coordinates: lat: 19.1901
lon: 72.9179
The Vihar and Tulsi Lakes are present within the hills. The highest point of the metropolis, at, is located in this region. Lakes. There are three lakes in the city. The Vihar Lake and the Tulsi Lake are present within the National Park and supply part of the city's drinking water. The Powai Lake is immediately south of these two. They are located in central Mumbai. Bays.

Geographic entities mentioned:
surface_form: Tulsi Lake
instance_of: Lake
countries: India
coordinates: lat: 19.1901
lon: 72.9179
The highest point of the metropolis, at, is located in this region. Lakes. There are three lakes in the city. The Vihar Lake and the Tulsi Lake are present within the National Park and supply part of the city's drinking water. The Powai Lake is immediately south of these two. They are located in central Mumbai. Bays. Back Bay is the largest bay in the city.

Geographic entities mentioned:
surface_form: Powai Lake
instance_of: Lake
countries: India
coordinates: lat: 19.13
lon: 72.91
In the centre of the bay is the tomb of Haji Ali, a 14th-century Muslim saint. The bay perimeter is about two kilometres in length. Mahim Bay is the second largest bay in the city. The Mithi River empties into the Mahim Creek which drains into the bay. The border between the city and its suburbs bisects the bay. To the north lies Bandra and to the south, Mahim. Creeks.

Geographic entities mentioned:
surface_form: Mahim Creek
instance_of: Watercourse
countries: India
coordinates: lat: 19.052601
lon: 72.8393824
Within the city the Malad (or Marve) Creek and the Gorai (or Manori) Creek inundate the suburban region. The Mahim Creek forms the border between the two districts. There are also the Mahul Creek and the Mahim Creek. Islands. Although the islands were merged in the 18th century, islands still dot Thane Creek.

Geographic entities mentioned:
surface_form: Mahim Creek
instance_of: Watercourse
countries: India
coordinates: lat: 19.052601
lon: 72.8393824
The reserve's Aboriginal cultural walk, a return track, runs along the granite slopes of the mountain to the cave painting site. The track passes through one of the few remnants of natural bushland on the western slopes of the New England Tablelands. The walking track is clear and easy to follow and, apart from one short section, is level and undemanding.

Geographic entities mentioned:
surface_form: Tablelands
instance_of: Plateau
countries: Australia
coordinates: lat: -30.595277777777778
lon: 151.5
Mount Peal. Mount Peal () is in the Beartooth Mountains in the U.S. state of Montana. The peak is one of the tallest in the Beatooth Mountains, the ninth tallest in Montana and is in the Absaroka-Beartooth Wilderness of Custer National Forest. The nearest taller mountain to Mount Peal is Tempest Mountain, WNW.

Geographic entities mentioned:
surface_form: Tempest Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.16694444
lon: -109.79194444
surface_form: mount peal
instance_of: Mountain
countries: United States
coordinates: lat: 45.16083333
lon: -109.77277778
Mount Peal. Mount Peal () is in the Beartooth Mountains in the U.S. state of Montana. The peak is one of the tallest in the Beatooth Mountains, the ninth tallest in Montana and is in the Absaroka-Beartooth Wilderness of Custer National Forest. The nearest taller mountain to Mount Peal is Tempest Mountain, WNW.

Geographic entities mentioned:
surface_form: mount peal
instance_of: Mountain
countries: United States
coordinates: lat: 45.16083333
lon: -109.77277778
Cartographic evidence. Robert Gordon's map of circa 1636-52 marks the loch lying close to Belston Loch and Auchencloigh Castle, slightly the larger loch and to the north on the same watercourse. Blaeu's map of circa 1654 taken from Timothy Pont's map of circa 1600 shows Plaid Loch and a Trinmaks River as the outflow. A location recorded as Lochhill lies to the north and East Plaid is nearby.

Geographic entities mentioned:
surface_form: Belston Loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.4227
lon: -4.4102
Blaeu's map of circa 1654 taken from Timothy Pont's map of circa 1600 shows Plaid Loch and a Trinmaks River as the outflow. A location recorded as Lochhill lies to the north and East Plaid is nearby. The loch is roughly circular and slightly smaller than Belston Loch. Molls map of 1745 shows a single loch that could be either Belston or Plaid.

Geographic entities mentioned:
surface_form: belston loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.4227
lon: -4.4102
In 1832 Thomson's map shows a rounded 'Plaid' with substantial surrounding marshlands; Laigh and High Plaid are recorded. In 1880 the loch was situated amongst extensive marshland and scrub with an outflow passing the Rottenrow area into the Burnock Water and running eventually into the Lugar Water, with an inflow from Belston Loch. Barlosh Farm lies to the west and Laigh Plaid borders the site.

Geographic entities mentioned:
surface_form: belston loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.4227
lon: -4.4102
Plaid Loch. Plaid Loch (NS 485186) was a freshwater loch in East Ayrshire, now a remnant due to drainage, near Sinclairston and 2 miles (3 km) south-east of Drongan, lying in a glacial kettle hole. The loch. Plaid Loch is one of four small lochs recorded in the 1880s, two of them artificial, within the parish of Ochiltree. Barlosh Moss.

Geographic entities mentioned:
surface_form: plaid loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.4351
lon: -4.40083
The loch. Plaid Loch is one of four small lochs recorded in the 1880s, two of them artificial, within the parish of Ochiltree. Barlosh Moss. Barlosh Moss is a Site of Special Scientific Interest (SSSI) and possesses a significant moth population. Once part of Plaid Loch, it is now marshy land that is home to carex grass, heather, juncus, pine, birch and thorn. Cartographic evidence.

Geographic entities mentioned:
surface_form: plaid loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.4351
lon: -4.40083
Cartographic evidence. Robert Gordon's map of circa 1636-52 marks the loch lying close to Belston Loch and Auchencloigh Castle, slightly the larger loch and to the north on the same watercourse. Blaeu's map of circa 1654 taken from Timothy Pont's map of circa 1600 shows Plaid Loch and a Trinmaks River as the outflow. A location recorded as Lochhill lies to the north and East Plaid is nearby.

Geographic entities mentioned:
surface_form: plaid loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.4351
lon: -4.40083
In 1961, he was appointed as a &quot;moreh tzedek&quot; and two years later, in 1963, he was invited to serve as rabbi of the Great Synagogue of Zikhron Moshe. In 1974, he was made a member of the Badatz of the Edah HaChareidis. In 1996, he was appointed Av Beit Din of the Edah HaChareidis. He died in 2003 and is buried on Har HaMenuchot.

Geographic entities mentioned:
surface_form: Har HaMenuchot
instance_of: Mountain
countries: Israel
coordinates: lat: 31.798133333333
lon: 35.177727777778
Even though it is in the French-speaking part of the canton of Bern, there is a German public school. History. Around 1570 the Prince-Bishop of Basel allowed Anabaptist refugees from the Emmental to settle in the seigniory of Erguel, including in the area that would become Mont-Tramelan. The farms in the area were part of the parish of Tramelan, which adopted the Reformed faith in 1530.

Geographic entities mentioned:
surface_form: Emmental
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.91922
lon: 7.77868
Ōhau B. Ōhau B is a power station operated by Meridian Energy in the South Island of New Zealand. It is a twin station with Ōhau C and is part of the Waitaki hydro scheme which consists of eight power stations operated from a control centre near Twizel. Water from Lake Ruataniwha flows through Ōhau B, then Ōhau C and then through to Lake Benmore.

Geographic entities mentioned:
surface_form: Lake Ruataniwha
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.281
lon: 170.071
surface_form: Lake Benmore
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.415
lon: 170.22055555556
Tell Dibbine. Tell Dibbine is an archaeological site 2km north of Marjayoun in the plain of &quot;El Marj&quot; in the Nabatieh Governorate. It dates at least to the Neolithic. It was also known in the ancient world as Ijon. Many artifacts have been found including statues (currently lost), columns, and many more... The people of this settlement could be Hivites, or most possibly Phoenician.

Geographic entities mentioned:
surface_form: tell dibbine
instance_of: Mountain
countries: Lebanon
coordinates: lat: 33.345277777778
lon: 35.59
Maude's accomplishments were, according to the DNB, inconsiderable, but he was esteemed for his love of ‘letters and of man.’ His verses are mainly descriptive of the Yorkshire dales. He contributed to Francis Grose's &quot;Antiquities&quot; the information about Bolton Castle and Wensleydale. Grose, who was his friend, quotes from 'Wharfedale' in illustration of Aysgarth Bridge.

Geographic entities mentioned:
surface_form: Wensleydale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.3056
lon: -2.16667
Julia Schacht. Julia Elise Schacht (born 13 July 1982) is a Norwegian actress, born on the island of Helgøya in the lake Mjøsa. Biography. Schacht was educated at Oslo National Academy of the Arts and Nordic Institute of Stage and Studio. She had her début in Pål Sletaune's 2005 thriller &quot;Next Door&quot;, which was only the second Norwegian movie ever to receive an over-18 rating.

Geographic entities mentioned:
surface_form: Mjøsa
instance_of: Lake
countries: Norway
coordinates: lat: 60.666666666667
lon: 11
WXFL. WXFL (96.1 FM, &quot;KIX 96&quot;) is a country music-formatted radio station based in Florence, Alabama, United States and owned by Big River Broadcasting, a company established by legendary rock and roll music producer Sam Phillips. WXFL serves Florence and the Tennessee Valley with an ERP of 20,500 watts. This station has held the WXFL call sign since 1990.

Geographic entities mentioned:
surface_form: Tennessee Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.959166666667
lon: -83.850277777778
Galwan battlefield is part of the Bharat Ranbhoomi Darshan initiative of the Indian Military which will boost border tourism, patriotism, local infrastructure and economy while reversing civilian outward migration from these remote locations, it entails 77 battleground war memorials in border area including the &quot;Longewala War Memorial, Sadhewala War Memorial, Siachen base camp, Kargil, Pangong Tso, Rezang La, Doklam, Bum La, Cho La, Kibithu, etc.

Geographic entities mentioned:
surface_form: Pangong Tso
instance_of: Lake
countries: People's Republic of China
India
coordinates: lat: 33.70472222222222
lon: 78.75
Oldfield moved his family from Toppenish, WA to Seattle, WA in 1946. There he stayed until 1959 when he moved to Ashford, WA. Nearby is Mount Rainier, which became the central subject of Oldfield’s artwork. In the 1960s, Oldfield had a few acres at the west entrance to Mount Rainier National Park. He and his wife moved to Federal Way, WA in 1976.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
The work was funded by private property owners and public funds. Overview. During the 19th century, the elevation of the Chicago area was little higher than the shoreline of Lake Michigan. For two decades following the city's incorporation, drainage from the city surface was inadequate, resulting in large bodies of standing and pathogenic water.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Arikaree Glacier. Arikaree Glacier is an alpine glacier located in a cirque to the north of Arikaree Peak and south of Navajo Peak, in Roosevelt National Forest in the U.S. state of Colorado. The glacier is just east of the Continental Divide and south of Isabelle Glacier.

Geographic entities mentioned:
surface_form: Navajo Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.053611111111
lon: -105.64666666667
A year later, Zhao Xi was promoted to Grand Commandant (), received the title of a &quot;Secondary Marquis&quot; (), and was tasked with inspecting the border. In 56 CE, he accompanied Emperor Guangwu to attend a &quot;fengshan&quot; () ceremony at Mount Tai. Service under Emperor Ming. Emperor Guangwu died in 57 CE. In his final edict, he ordered Zhao Xi to assist his successor, Emperor Ming.

Geographic entities mentioned:
surface_form: Mount Tai
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 36.266666666667
lon: 117.1
Martin died on 7 March 2022, at the age of 87. Work. Martin was most famous for his discoveries of the tomb of Maya, Tutankhamun's treasurer, and the private tomb of Horemheb, but also more generally for his work in the Valley of the Kings and Saqqara. The discoveries in Saqqara include Tia, Ramesses the Great's sister and other dignitaries.

Geographic entities mentioned:
surface_form: Valley of the Kings
instance_of: Valley
countries: Egypt
coordinates: lat: 25.74025
lon: 32.602358
Independence Monument (Colorado). Independence Monument is a sandstone pillar located in Colorado National Monument, in Mesa County of western Colorado, United States. This iconic 450-foot-high landmark is situated one mile southeast of the monument's visitor center, and west of the community of Grand Junction, where it towers above the floor of Monument Canyon and Wedding Canyon.

Geographic entities mentioned:
surface_form: independence monument
instance_of: Mountain
countries: United States
coordinates: lat: 39.0958148
lon: -108.7234324
Otto is remembered as Colorado National Monument's founder, and its first custodian. A fervent patriot, he named the rock features after great heroes and historic events, with Independence Monument still bearing the name he bestowed. John Otto made the first ascent of Independence Monument on June 14, 1911, flying Old Glory from the summit for Flag Day.

Geographic entities mentioned:
surface_form: independence monument
instance_of: Mountain
countries: United States
coordinates: lat: 39.0958148
lon: -108.7234324
A fervent patriot, he named the rock features after great heroes and historic events, with Independence Monument still bearing the name he bestowed. John Otto made the first ascent of Independence Monument on June 14, 1911, flying Old Glory from the summit for Flag Day. That flag was presented to Otto by President William Howard Taft.

Geographic entities mentioned:
surface_form: independence monument
instance_of: Mountain
countries: United States
coordinates: lat: 39.0958148
lon: -108.7234324
The pipes Otto attached were removed in the mid-1950s by the Park Service, but handholds and steps which he carved into the sandstone remain. John Otto married Boston artist Beatrice Farnham on June 20, 1911, at the base of Independence Monument in Wedding Canyon. It has become an annual tradition among climbers to raise the flag on the summit on July 4 each year. Geology.

Geographic entities mentioned:
surface_form: independence monument
instance_of: Mountain
countries: United States
coordinates: lat: 39.0958148
lon: -108.7234324
The thin caprock at the summit consists of fluvial sandstones of the resistant Kayenta Formation. The slope around the base of the Independence Monument is Chinle Formation. The floor of the canyon is Precambrian basement rock consisting of gneiss, schist, and granites. Precipitation runoff from this geographical feature drains to the Colorado River, approximately two miles to the northeast.

Geographic entities mentioned:
surface_form: independence monument
instance_of: Mountain
countries: United States
coordinates: lat: 39.0958148
lon: -108.7234324
Precipitation runoff from this geographical feature drains to the Colorado River, approximately two miles to the northeast. Climate. According to the Köppen climate classification system, Independence Monument is located in a semi-arid climate zone. Summers are hot and dry, while winters are cold with some snow.

Geographic entities mentioned:
surface_form: independence monument
instance_of: Mountain
countries: United States
coordinates: lat: 39.0958148
lon: -108.7234324
His parents moved to California in 1985. He grew up in the San Fernando Valley region of Los Angeles and attended both private and public schools. He spent the bulk of his childhood acting professionally, appearing in stage plays, national commercials and the Phil Collins music video &quot;Do you Remember?&quot; He has had a Screen Actors Guild Card since 1987.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
After 1926, the management of the farm was offered to Spiritual Christians from Russia living in north Kars Province who were noted for animal breeding (Malakan horse, Malakan cow) but who refused repatriation to the Soviet Union. They declined to move to Ankara, because the most zealous believed they must live close to Mount Ararat for the Second Coming of Christ.

Geographic entities mentioned:
surface_form: Mount Ararat
instance_of: Mountain
countries: Turkey
coordinates: lat: 39.70194444444444
lon: 44.29833333333333
West Sleeping River. The West Sleeping River is an river in Ontonagon County, Michigan, in the United States. It is a tributary of Lake Superior.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Lakes, large and small, can be found in almost all cantons and provide an important source of water, leisure opportunities, as well as suitable habitat for fish-eating birds. The two most extensive, Lake Geneva and Lake Constance, are amongst the largest in Europe and mark the border of the Swiss Plateau, along with the Alps and the Jura Mountains. The largest wholly Swiss lake is Lake Neuchâtel.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
surface_form: Swiss Plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
The two most extensive, Lake Geneva and Lake Constance, are amongst the largest in Europe and mark the border of the Swiss Plateau, along with the Alps and the Jura Mountains. The largest wholly Swiss lake is Lake Neuchâtel. The remaining lakes over are Lake Maggiore and Lake Lucerne. In total 103 lakes exist that are more than in surface area, and a considerable number of smaller lakes.

Geographic entities mentioned:
surface_form: Lake Neuchâtel
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.9
lon: 6.85
The two most extensive, Lake Geneva and Lake Constance, are amongst the largest in Europe and mark the border of the Swiss Plateau, along with the Alps and the Jura Mountains. The largest wholly Swiss lake is Lake Neuchâtel. The remaining lakes over are Lake Maggiore and Lake Lucerne. In total 103 lakes exist that are more than in surface area, and a considerable number of smaller lakes.

Geographic entities mentioned:
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
surface_form: Lake Lucerne
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.0194
lon: 8.4011
Koch. The Carlsberg Foundation () had been the most generous single contributor at the time of financing the venture. In May-June 2007 an expedition led by Russ Hore with Gerwyn Lloyd and Tim Radford climbed some of the peaks of the nunataks rising to the west, as well as in the Eventyrfjelde area to the south. Geography.

Geographic entities mentioned:
surface_form: Eventyrfjelde
instance_of: Mountain
coordinates: lat: 76.08333333333333
lon: -24.366666666666667
surface_form: eventyrfjelde
instance_of: Mountain
coordinates: lat: 76.08333333333333
lon: -24.366666666666667
Carlsbergfondet Land. Carlsbergfondet Land is a group of nunataks in Queen Louise Land, NE Greenland. Administratively it is part of the Northeast Greenland National Park zone. History. The area was named &quot;Carlsbergfondets Land&quot; during the 1912–13 Danish Expedition to Queen Louise Land led by J.P. Koch.

Geographic entities mentioned:
surface_form: park
instance_of: Mountain
coordinates: lat: -67.2333
lon: 51
Administratively it is part of the Northeast Greenland National Park zone. History. The area was named &quot;Carlsbergfondets Land&quot; during the 1912–13 Danish Expedition to Queen Louise Land led by J.P. Koch. The Carlsberg Foundation () had been the most generous single contributor at the time of financing the venture.

Geographic entities mentioned:
surface_form: carlsbergfondets land
instance_of: Mountain
coordinates: lat: 76.55
lon: -24
Carlsbergfondet Land. Carlsbergfondet Land is a group of nunataks in Queen Louise Land, NE Greenland. Administratively it is part of the Northeast Greenland National Park zone. History. The area was named &quot;Carlsbergfondets Land&quot; during the 1912–13 Danish Expedition to Queen Louise Land led by J.P. Koch.

Geographic entities mentioned:
surface_form: carlsbergfondet land
instance_of: Mountain
coordinates: lat: 76.55
lon: -24
Pilot Fire. The Pilot Fire was a wildfire that burned near Silverwood Lake in San Bernardino County, California. The fire started at about 12:10 pm on Sunday, August 7, 2016, near the Miller Canyon OHV area off California State Route 138.

Geographic entities mentioned:
surface_form: Silverwood Lake
instance_of: Lake
countries: United States
coordinates: lat: 34.303888888889
lon: -117.31805555556