Sarmila/GeoWiki-Features huggingface dataset:
Kashkari's mother Sheila Kashkari, was a pathologist at Akron City Hospital, and father Chaman Kashkari, worked as a professor of electrical engineering at the University of Akron. Kashkari's parents are Kashmiri Pandits, who were both born and raised in Srinagar in the Kashmir Valley, within the Indian state of Jammu and Kashmir and immigrated to the United States in 1964.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
A site was selected at the south end of King's Forest, in the Red Hill Valley, and plans were drawn up in January 1963 by local architect Charles Lenz for a &quot;Proposed Royal Zoological Park in the King's Forest&quot;.

Geographic entities mentioned:
surface_form: Red Hill Valley
instance_of: Valley
countries: Canada
coordinates: lat: 43.2234
lon: -79.7981
From there, the river travels southwest, absorbing additional tributaries of the Little River, the Little Tennessee, and the Clinch, and further down, the Hiwassee and the Ocoee (both of which have sources in Georgia), before reaching Chattanooga. The river then enters the Tennessee River Gorge as it winds its way through the Cumberland Plateau, reaching the lower portion of the Sequatchie Valley.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
surface_form: Sequatchie Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.125
lon: -85.5289
After traversing North Alabama, the river veers northwestward. From the beginning of the Tennessee Valley to this point is roughly; as it runs through East Tennessee the Valley is bound on the east by the Appalachian Mountains (including the Great Smoky Mountains) and on the northwest by the Cumberland Plateau and Cumberland Mountains.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
surface_form: cumberland
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: tennessee valley
instance_of: Valley
countries: United States
coordinates: lat: 35.959166666667
lon: -83.850277777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: tennessee valley
instance_of: Valley
countries: United States
coordinates: lat: 37.8611
lon: -122.534
It empties into the Ohio River in western Kentucky, where it divides the region known as the Jackson Purchase from the rest of Kentucky. Geologically, the eastern portion of the Tennessee Valley consists of many small valleys and ridges within a great valley. The larger region is termed the Ridge and Valley Province and the great valley is termed the Great Appalachian Valley.

Geographic entities mentioned:
surface_form: Great Appalachian Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 40.0586
lon: -75.5306
It empties into the Ohio River in western Kentucky, where it divides the region known as the Jackson Purchase from the rest of Kentucky. Geologically, the eastern portion of the Tennessee Valley consists of many small valleys and ridges within a great valley. The larger region is termed the Ridge and Valley Province and the great valley is termed the Great Appalachian Valley.

Geographic entities mentioned:
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 40.0586
lon: -75.5306
surface_form: tennessee valley
instance_of: Valley
countries: United States
coordinates: lat: 35.959166666667
lon: -83.850277777778
surface_form: tennessee valley
instance_of: Valley
countries: United States
coordinates: lat: 37.8611
lon: -122.534
state of Tennessee. It stretches from southwest Kentucky to north Alabama and from northeast Mississippi to the mountains of Virginia and North Carolina. The border of the valley is known as the Tennessee Valley Divide. The Tennessee Valley contributes greatly to the formation of Tennessee's three legally recognized sectors (the Grand Divisions). Geography.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: tennessee valley
instance_of: Valley
countries: United States
coordinates: lat: 35.959166666667
lon: -83.850277777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: tennessee valley
instance_of: Valley
countries: United States
coordinates: lat: 37.8611
lon: -122.534
Tennessee Valley. The Tennessee Valley is the drainage basin of the Tennessee River and is largely within the U.S. state of Tennessee. It stretches from southwest Kentucky to north Alabama and from northeast Mississippi to the mountains of Virginia and North Carolina. The border of the valley is known as the Tennessee Valley Divide.

Geographic entities mentioned:
surface_form: tennessee valley
instance_of: Valley
countries: United States
coordinates: lat: 35.959166666667
lon: -83.850277777778
surface_form: tennessee valley
instance_of: Valley
countries: United States
coordinates: lat: 37.8611
lon: -122.534
state of Tennessee. It stretches from southwest Kentucky to north Alabama and from northeast Mississippi to the mountains of Virginia and North Carolina. The border of the valley is known as the Tennessee Valley Divide. The Tennessee Valley contributes greatly to the formation of Tennessee's three legally recognized sectors (the Grand Divisions). Geography.

Geographic entities mentioned:
surface_form: tennessee valley
instance_of: Valley
countries: United States
coordinates: lat: 35.959166666667
lon: -83.850277777778
surface_form: tennessee valley
instance_of: Valley
countries: United States
coordinates: lat: 37.8611
lon: -122.534
Geography. The Tennessee Valley begins in the upper head water portions of the Holston River, the Watauga River, and the Doe River in Northeast Tennessee and Southwest Virginia, as well as east of Asheville, North Carolina, with the headwaters of the French Broad and Pigeon rivers, all of which join at the confluence of the French Broad and the Holston to form the Tennessee River in Knoxville.

Geographic entities mentioned:
surface_form: tennessee valley
instance_of: Valley
countries: United States
coordinates: lat: 35.959166666667
lon: -83.850277777778
surface_form: tennessee valley
instance_of: Valley
countries: United States
coordinates: lat: 37.8611
lon: -122.534
Delaronde Lake. Delaronde Lake is a lake in the Canadian province of Saskatchewan. It is situated at the western edge of the Waskesiu Upland in the boreal forest ecozone of Canada. Delaronde Lake is within the Churchill River drainage basin of the Hudson Bay. Most of Delaronde Lake is in the Rural Municipality of Big River No.

Geographic entities mentioned:
surface_form: Waskesiu Upland
instance_of: Mountain
countries: Canada
coordinates: lat: 53.8398
lon: -106.4284
The north section is deep, with depths of up to, while the south section is shallow at only deep. The lake is situated at the western end of the Waskesiu Upland, and, as such, the upland's western slopes are within the lake's catchment. Prince Albert National Park encompasses much of the Waskesiu Upland. Delaronde Lake has two named islands — Zig Zag and Delaronde — and multiple bays.

Geographic entities mentioned:
surface_form: Waskesiu Upland
instance_of: Mountain
countries: Canada
coordinates: lat: 53.8398
lon: -106.4284
The outflow river is at Hall Bay at the northern end of the lake's southern section. This river flows a short distance north-west into Taggart Lake. Taggart Creek then flows out of Taggart Lake heading north where it meets the Cowan River near Highway 924. The Cowan River is a tributary of the Beaver River, which, in turn, is a tributary of the Churchill River.

Geographic entities mentioned:
surface_form: Cowan River
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.41687
lon: -107.85138
Taggart Creek then flows out of Taggart Lake heading north where it meets the Cowan River near Highway 924. The Cowan River is a tributary of the Beaver River, which, in turn, is a tributary of the Churchill River. Along the shores of Delaronde Lake are small communities, subdivisions, and campgrounds, all of which are at the southern end of the lake.

Geographic entities mentioned:
surface_form: cowan river
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.41687
lon: -107.85138
Along the shores of Delaronde Lake are small communities, subdivisions, and campgrounds, all of which are at the southern end of the lake. These include Phillips Grove, Lakeshore RV Properties, Stoney Bay Campground, Delaronde Resort, Big River Bible Camp, Island View Shores, and Delaronde Lake (Zig Zag Bay) Recreation Site. Delaronde Lake (Zig Zag Bay) Recreation Site.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: delaronde lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05006
lon: -107.05056
Access to the lake and its amenities is from Highway 922. At about to the south-west, Big River is the closest town. Description. Delaronde Lake is a long and narrow lake that is separated into two sections — north and south — by a narrow channel. The north section is deep, with depths of up to, while the south section is shallow at only deep.

Geographic entities mentioned:
surface_form: narrow lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.6194
lon: -113.616
surface_form: delaronde lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05006
lon: -107.05056
Delaronde Lake. Delaronde Lake is a lake in the Canadian province of Saskatchewan. It is situated at the western edge of the Waskesiu Upland in the boreal forest ecozone of Canada. Delaronde Lake is within the Churchill River drainage basin of the Hudson Bay. Most of Delaronde Lake is in the Rural Municipality of Big River No.

Geographic entities mentioned:
surface_form: delaronde lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05006
lon: -107.05056
It is situated at the western edge of the Waskesiu Upland in the boreal forest ecozone of Canada. Delaronde Lake is within the Churchill River drainage basin of the Hudson Bay. Most of Delaronde Lake is in the Rural Municipality of Big River No. 555 with only the northernmost part in the Northern Saskatchewan Administration District.

Geographic entities mentioned:
surface_form: delaronde lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05006
lon: -107.05056
The lake is situated at the western end of the Waskesiu Upland, and, as such, the upland's western slopes are within the lake's catchment. Prince Albert National Park encompasses much of the Waskesiu Upland. Delaronde Lake has two named islands — Zig Zag and Delaronde — and multiple bays. The outflow river is at Hall Bay at the northern end of the lake's southern section.

Geographic entities mentioned:
surface_form: delaronde lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05006
lon: -107.05056
Taggart Creek then flows out of Taggart Lake heading north where it meets the Cowan River near Highway 924. The Cowan River is a tributary of the Beaver River, which, in turn, is a tributary of the Churchill River. Along the shores of Delaronde Lake are small communities, subdivisions, and campgrounds, all of which are at the southern end of the lake.

Geographic entities mentioned:
surface_form: delaronde lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05006
lon: -107.05056
These include Phillips Grove, Lakeshore RV Properties, Stoney Bay Campground, Delaronde Resort, Big River Bible Camp, Island View Shores, and Delaronde Lake (Zig Zag Bay) Recreation Site. Delaronde Lake (Zig Zag Bay) Recreation Site. Delaronde Lake (Zig Zag Bay) Recreation Site () is a leased provincial campground at Zig Zag Bay on the east side of the south section of Delaronde Lake.

Geographic entities mentioned:
surface_form: delaronde lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05006
lon: -107.05056
Delaronde Lake (Zig Zag Bay) Recreation Site. Delaronde Lake (Zig Zag Bay) Recreation Site () is a leased provincial campground at Zig Zag Bay on the east side of the south section of Delaronde Lake. This heavily wooded, park has a campground, marina, sandy beach, and boat launch. Access is from Highway 922. Fish species.

Geographic entities mentioned:
surface_form: delaronde lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05006
lon: -107.05056
surface_form: delaronde lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05006
lon: -107.05056
Delaronde Lake (Zig Zag Bay) Recreation Site () is a leased provincial campground at Zig Zag Bay on the east side of the south section of Delaronde Lake. This heavily wooded, park has a campground, marina, sandy beach, and boat launch. Access is from Highway 922. Fish species. Fish commonly found in Delaronde Lake include northern pike, whitefish, lake trout, and walleye.

Geographic entities mentioned:
surface_form: delaronde lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05006
lon: -107.05056
The north section is deep, with depths of up to, while the south section is shallow at only deep. The lake is situated at the western end of the Waskesiu Upland, and, as such, the upland's western slopes are within the lake's catchment. Prince Albert National Park encompasses much of the Waskesiu Upland. Delaronde Lake has two named islands — Zig Zag and Delaronde — and multiple bays.

Geographic entities mentioned:
surface_form: waskesiu upland
instance_of: Mountain
countries: Canada
coordinates: lat: 53.8398
lon: -106.4284
It is situated in the Kamet range. The elevation of Durpata is and its prominence is. It is 93rd highest located entirely within the Uttrakhand. Nanda Devi, is the highest mountain in this category. It lies 3.8 km east of Gauri Parbat its nearest higher neighbor. Hathi Parbat lies 4.8 km SW and it is 5.1 km SSE of Rataban. It lies 11.7 km SSE of Nilgiri Parbat. Climbing history.

Geographic entities mentioned:
surface_form: Nanda Devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
It is situated in the Kamet range. The elevation of Durpata is and its prominence is. It is 93rd highest located entirely within the Uttrakhand. Nanda Devi, is the highest mountain in this category. It lies 3.8 km east of Gauri Parbat its nearest higher neighbor. Hathi Parbat lies 4.8 km SW and it is 5.1 km SSE of Rataban. It lies 11.7 km SSE of Nilgiri Parbat. Climbing history.

Geographic entities mentioned:
surface_form: Gauri Parbat
instance_of: Mountain
countries: India
coordinates: lat: 30.71096111
lon: 79.70085278
It is 93rd highest located entirely within the Uttrakhand. Nanda Devi, is the highest mountain in this category. It lies 3.8 km east of Gauri Parbat its nearest higher neighbor. Hathi Parbat lies 4.8 km SW and it is 5.1 km SSE of Rataban. It lies 11.7 km SSE of Nilgiri Parbat. Climbing history. It was first climbed by Andre Roch and Sherpa Gombu in 1939 during a Swiss climbing party.

Geographic entities mentioned:
surface_form: Hathi Parbat
instance_of: Mountain
countries: India
coordinates: lat: 30.685
lon: 79.70583333
surface_form: Rataban
instance_of: Mountain
countries: India
coordinates: lat: 30.75
lon: 79.75
It is 93rd highest located entirely within the Uttrakhand. Nanda Devi, is the highest mountain in this category. It lies 3.8 km east of Gauri Parbat its nearest higher neighbor. Hathi Parbat lies 4.8 km SW and it is 5.1 km SSE of Rataban. It lies 11.7 km SSE of Nilgiri Parbat. Climbing history. It was first climbed by Andre Roch and Sherpa Gombu in 1939 during a Swiss climbing party.

Geographic entities mentioned:
surface_form: Nilgiri Parbat
instance_of: Mountain
countries: India
coordinates: lat: 30.78302222
lon: 79.64545
Durpata. Durpata is a mountain of the Garhwal Himalaya in Uttarakhand India. It is situated in the Kamet range. The elevation of Durpata is and its prominence is. It is 93rd highest located entirely within the Uttrakhand. Nanda Devi, is the highest mountain in this category. It lies 3.8 km east of Gauri Parbat its nearest higher neighbor.

Geographic entities mentioned:
surface_form: durpata
instance_of: Mountain
countries: India
coordinates: lat: 30.7175
lon: 79.73666666666666
Durpata. Durpata is a mountain of the Garhwal Himalaya in Uttarakhand India. It is situated in the Kamet range. The elevation of Durpata is and its prominence is. It is 93rd highest located entirely within the Uttrakhand. Nanda Devi, is the highest mountain in this category. It lies 3.8 km east of Gauri Parbat its nearest higher neighbor.

Geographic entities mentioned:
surface_form: kamet
instance_of: Mountain
countries: India
coordinates: lat: 30.92
lon: 79.593333333333
Afon Senni. The Afon Senni is a river in Powys, Wales which rises in the Fforest Fawr section of the Brecon Beacons National Park and flows northwards for to a confluence with the River Usk at Sennybridge. The river rises as Blaen Senni to the north of the peak of Fan Nedd and east of Fan Gyhirych occupying a deep glacial trough until it reaches the hamlet of Heol Senni.

Geographic entities mentioned:
surface_form: Fan Nedd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 51.8529
lon: -3.5792
surface_form: Fan Gyhirych
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 51.859
lon: -3.627
It flows mainly in the Sukabumi Regency. Hydrology. The river flows from east to west with a length of around 100 km. The upstream of Cimandiri is located on the Mount Pasir Caringin, Sukamanah village, district of Gegerbitung and discharges into Indian Ocean near Pelabuhan Ratu. The tributaries of Cimandiri also flow from Mount Gede, Mount Pangrango, Mount Salak and Mount Halimun.

Geographic entities mentioned:
surface_form: Mount Gede
instance_of: Mountain
countries: Indonesia
coordinates: lat: -6.7883333333333
lon: 106.98166666667
surface_form: Mount Pangrango
instance_of: Mountain
countries: Indonesia
coordinates: lat: -6.7666666666667
lon: 106.95
It is part of Ward No. 17 of Dhanbad Municipal Corporation. The neighborhood features undulating uplands bustling with coalmines in the lowest rung of the Chota Nagpur Plateau. The entire area shown in the map is under Dhanbad Municipal Corporation, except Belgaria which is under Baliapur (community development block). The places in the DMC area are marked as neighbourhoods.

Geographic entities mentioned:
surface_form: Chota Nagpur Plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
The mountain is set in the Hoover Wilderness on land managed by Humboldt–Toiyabe National Forest. The summit is situated one mile outside the boundary of Yosemite National Park, and less than one mile east of line parent Camiaca Peak. Topographic relief is significant as the east aspect rises above East Lake in one-quarter mile.

Geographic entities mentioned:
surface_form: Camiaca Peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.05992
lon: -119.3246
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
The summit is situated one mile outside the boundary of Yosemite National Park, and less than one mile east of line parent Camiaca Peak. Topographic relief is significant as the east aspect rises above East Lake in one-quarter mile. This landform's toponym, which commemorates a miner and prospector named Page, has been officially adopted by the United States Board on Geographic Names. Climate.

Geographic entities mentioned:
surface_form: east lake
instance_of: Lake
countries: United States
coordinates: lat: 29.252666666667
lon: -98.376333333333
Most weather fronts originate in the Pacific Ocean, and travel east toward the Sierra Nevada mountains. As fronts approach, they are forced upward by the peaks (orographic lift), causing moisture in the form of rain or snowfall to drop onto the range. Precipitation runoff from this mountain drains into East Lake, thence West Fork Green Creek, which is a tributary of the Walker River.

Geographic entities mentioned:
surface_form: east lake
instance_of: Lake
countries: United States
coordinates: lat: 29.252666666667
lon: -98.376333333333
Page Peaks. Page Peaks is a mountain summit located in the Sierra Nevada mountain range, in Mono County of northern California, United States. The mountain is set in the Hoover Wilderness on land managed by Humboldt–Toiyabe National Forest. The summit is situated one mile outside the boundary of Yosemite National Park, and less than one mile east of line parent Camiaca Peak.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: page peaks
instance_of: Mountain
countries: United States
coordinates: lat: 38.06659
lon: -119.31127
Page Peaks. Page Peaks is a mountain summit located in the Sierra Nevada mountain range, in Mono County of northern California, United States. The mountain is set in the Hoover Wilderness on land managed by Humboldt–Toiyabe National Forest. The summit is situated one mile outside the boundary of Yosemite National Park, and less than one mile east of line parent Camiaca Peak.

Geographic entities mentioned:
surface_form: page peaks
instance_of: Mountain
countries: United States
coordinates: lat: 38.06659
lon: -119.31127
This landform's toponym, which commemorates a miner and prospector named Page, has been officially adopted by the United States Board on Geographic Names. Climate. Page Peaks is located in an alpine climate zone. Most weather fronts originate in the Pacific Ocean, and travel east toward the Sierra Nevada mountains.

Geographic entities mentioned:
surface_form: page peaks
instance_of: Mountain
countries: United States
coordinates: lat: 38.06659
lon: -119.31127
The Fairbottom Branch Canal was a canal near Ashton-under-Lyne in Greater Manchester, England. Route. The canal left the Hollinwood Branch Canal at Fairbottom Junction immediately above lock 22. It was just over one mile long (1.82 km) and it was lock free. It terminated at Fenny Fields Bridge, Bardsley, which is situated in the Medlock Valley between Ashton-under-Lyne and Oldham. History.

Geographic entities mentioned:
surface_form: Medlock Valley
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 53.4741
lon: -2.25342
From the southern coast the species occurs as far north as Cape Naturaliste, Bridgetown, Lake Muir, the Stirling Range, Gairdner River (Calyerup) and the Ravensthorpe Range, and is present off the coast at Bald and Coffin Islands near the city of Albany., The eastern extent of the population at the Esperance Plains region occurs at Cape Arid National Park, and at offshore outcrops of the Recherche Archipelago, such as Middle and Woody Islands.

Geographic entities mentioned:
surface_form: Lake Muir
instance_of: Lake
countries: Australia
coordinates: lat: -34.446944444444
lon: 116.74833333333
The &quot;Records&quot; (1991) of the Western Australian Museum gave a northernmost location of Glen Forrest in the Darling Range to an area near North Bannister and Mount Saddleback, and confirmed their continued absence from the Swan Coastal plain. However, there are occasional reports of sightings in the largely cleared region, HANZAB notes two seen at Canning Mills in 1997.

Geographic entities mentioned:
surface_form: Mount Saddleback
instance_of: Mountain
countries: Australia
coordinates: lat: -32.97128
lon: 116.4609
The volcano went quiet on 13 December 2021, and on 25 December 2021, the local government declared the eruption to be over. Cumbre Vieja erupted twice in the 20th century, in 1949 (Volcán San Juan) and in 1971 (Volcán Teneguía). Volcanic history.

Geographic entities mentioned:
surface_form: Volcán Teneguía
instance_of: Mountain
countries: Spain
coordinates: lat: 28.47333333
lon: -17.85166667
Research is continuing. Due to the lack of seismic monitoring equipment on the island, any claims about seismic activity are based upon personal observation and may not be reliable. 1971 eruption. The 1971 eruption occurred at the southern end of the Cumbre Vieja at the Teneguía vent. The eruption was mainly strombolian in style. Lava was erupted.

Geographic entities mentioned:
surface_form: Teneguía
instance_of: Mountain
countries: Spain
coordinates: lat: 28.47333333
lon: -17.85166667
Cumbre Vieja. The Cumbre Vieja (; meaning &quot;Old Summit&quot;) is an active volcanic ridge on the island of La Palma in the Canary Islands, Spain. The spine of Cumbre Vieja trends in an approximate north–south direction, comprising the southern half of La Palma, with both summit ridge and flanks pockmarked by dozens of craters and cones.

Geographic entities mentioned:
surface_form: cumbre vieja
instance_of: Mountain
countries: Spain
coordinates: lat: 28.566666666667
lon: -17.833333333333
Volcanic history. La Palma is a volcanic ocean island located on the African Plate and is currently—along with Tenerife—one of the most volcanically active of the Canary Islands. Since about 125,000 years ago (~125 ka), all subaerial eruptions on La Palma have been associated with the Cumbre Vieja, with eruptions ranging over the whole 25-kilometre-long ridge.

Geographic entities mentioned:
surface_form: cumbre vieja
instance_of: Mountain
countries: Spain
coordinates: lat: 28.566666666667
lon: -17.833333333333
Since about 125,000 years ago (~125 ka), all subaerial eruptions on La Palma have been associated with the Cumbre Vieja, with eruptions ranging over the whole 25-kilometre-long ridge. Submarine surveys show that the Cumbre Vieja continues south of (the &quot;Point of the Hot Source&quot;), but no volcanic activity connected with the submarine extension has yet been observed.

Geographic entities mentioned:
surface_form: cumbre vieja
instance_of: Mountain
countries: Spain
coordinates: lat: 28.566666666667
lon: -17.833333333333
Submarine surveys show that the Cumbre Vieja continues south of (the &quot;Point of the Hot Source&quot;), but no volcanic activity connected with the submarine extension has yet been observed. Historical eruptions on the Cumbre Vieja occurred in 1470, 1585, 1646, 1677, 1712, 1949, 1971, and 2021.

Geographic entities mentioned:
surface_form: cumbre vieja
instance_of: Mountain
countries: Spain
coordinates: lat: 28.566666666667
lon: -17.833333333333
It was traceable to the Hoyo Negro and Duraznero vents, making a total length of about two and half kilometres or about 1/10 of the exposed length of the Cumbre Vieja, and parts of the western half of the Cumbre Vieja ridge had apparently moved about 1 metre sideways and 2 metres downwards towards the Atlantic Ocean.

Geographic entities mentioned:
surface_form: cumbre vieja
instance_of: Mountain
countries: Spain
coordinates: lat: 28.566666666667
lon: -17.833333333333
surface_form: cumbre vieja
instance_of: Mountain
countries: Spain
coordinates: lat: 28.566666666667
lon: -17.833333333333
As a result, they postulated that the western flank may be in the initial stages of failure. In October 2000, the British Broadcasting Corporation (BBC) transmitted a &quot;Horizon&quot; programme called &quot;Mega-tsunami: Wave of Destruction&quot;, which suggested that a future failure of the western flank of Cumbre Vieja could cause a megatsunami.

Geographic entities mentioned:
surface_form: cumbre vieja
instance_of: Mountain
countries: Spain
coordinates: lat: 28.566666666667
lon: -17.833333333333
One scientist claimed, &quot;This is a true story—only it hasn't happened yet!&quot;
Day &quot;et al.&quot; (1999), Ward and Day (2001) and Ward and Day (2005) hypothesize that, during an eruption at some future date, the western half of the Cumbre Vieja—approximately 500 km3 (5 x 1011 m3) with an estimated mass of 1.5 trillion metric tons—will catastrophically fail in a massive gravitational landslide and enter the Atlantic Ocean, generating a so-called mega-tsunami.

Geographic entities mentioned:
surface_form: cumbre vieja
instance_of: Mountain
countries: Spain
coordinates: lat: 28.566666666667
lon: -17.833333333333
Murty &quot;et al.&quot; (2005) claim that it is almost impossible for a trans-oceanic tsunami to be generated in the basin of the Atlantic Ocean, which—if correct—supports the work by many other researchers that the failure of the western flank of the Cumbre Vieja would be unlikely to generate a &quot;mega-tsunami&quot;.

Geographic entities mentioned:
surface_form: cumbre vieja
instance_of: Mountain
countries: Spain
coordinates: lat: 28.566666666667
lon: -17.833333333333
Only residual fumarolic activity and thermal emissions then occurred until 30 July when the Duraznero vent and fissure re-activated. Lava then flowed from the Duraznero vent and fissure, filling the adjacent crater of El Fraile and created a lava lake. This subsequently overflowed and the lava flowed down the eastern flank towards the ocean.

Geographic entities mentioned:
surface_form: el fraile
instance_of: Mountain
countries: Spain
coordinates: lat: 36.7819
lon: -2.08163
The property was purchased by Blevins Davis in July 1950. His wife, Marguerite Davis, a railroad heiress, died in 1948 and wished to have her fortune used for charitable purposes. The Modern Woodmen Sanatorium property and a house in Broadmoor called Trianon were sold to the Poor Sisters of St. Francis (Sisters of St. Francis of Perpetual Adoration) for $1 in 1952.

Geographic entities mentioned:
surface_form: Broadmoor
instance_of: Landform
countries: United States
coordinates: lat: 38.7956
lon: -104.841
According to the U.S. Census Bureau, the town has a total area of, of which is land and, or 2.26%, is water. Tuscarora Lake is in the south-central part of the town, draining northwest toward Chittenango Creek, a north-flowing stream that leads to Oneida Lake, part of the Lake Ontario/St. Lawrence River watershed.

Geographic entities mentioned:
surface_form: Tuscarora Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.867222
lon: -75.756667
surface_form: Oneida Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.2
lon: -75.9
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Then-President of the Senate Milan Štěch urged the city not to organize such events, and his concern was echoed by senator Václav Láska. In February 2016, it was announced that Ortel would perform at the April Říp Pilgrimage, held under Říp hill, near Krabčice. A petition appeared, opposing this on the basis that the event was for families, not supporters of xenophobia and hatred.

Geographic entities mentioned:
surface_form: Říp hill
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.38653
lon: 14.2896344
Realising that rain could flood the country and isolate his starving party Landsborough struggled back to the Albert River depot, having found no trace of Burke and Wills. During this journey Landsborough named the Gregory and Herbert (later Georgina) rivers, Lake Frances, Lake Mary and the Barkly Tableland and on his return reported the area well-suited for sheep raising.

Geographic entities mentioned:
surface_form: Barkly Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -19
lon: 138
Career. Button became a member of the Virginia Bar in 1922 and practiced law for a decade before beginning his public career. During this initial time he first became active in his community and the Shenandoah Valley through the Rotary Club and other organizations.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Lago di Salarno. Lago di Salarno is a lake in the Province of Brescia, Lombardy, Italy.

Geographic entities mentioned:
surface_form: lago di salarno
instance_of: Lake
countries: Italy
coordinates: lat: 46.109722222222
lon: 10.476111111111
Geography and watershed. The elevation near the mouth of Little Green Creek is above sea level. The elevation of the creek's source is between and above sea level. A portion of the creek is near a densely forested and steep hillside that is high and is located on the northern edge of the Greenwood Valley. The August 19, 1890 Wilkes-Barre tornado began in the vicinity of this area.

Geographic entities mentioned:
surface_form: Greenwood Valley
instance_of: Valley
coordinates: lat: -77.3667
lon: 162.85
Adamson's grunter. Adamson's grunter (&quot;Hephaestus adamsoni&quot;) is a species of freshwater ray-finned fish, a grunter from the family Terapontidae which is endemic to Lake Kutubu in the Kikori River system, Papua New Guinea. Habitat and biology.

Geographic entities mentioned:
surface_form: Lake Kutubu
instance_of: Lake
countries: Papua New Guinea
coordinates: lat: -6.4
lon: 143.33333333333
Ciekoty. Ciekoty is a village in the administrative district of Gmina Masłów, within Kielce County, Świętokrzyskie Voivodeship, in south-central Poland. It lies approximately east of Masłów and east of the regional capital Kielce. Geographically, it lies near the base of Mount Radostowa in the Łysogóry range of the Świętokrzyskie Mountains.

Geographic entities mentioned:
surface_form: Radostowa
instance_of: Mountain
countries: Poland
coordinates: lat: 50.9
lon: 20.816666666667
When Consumers Power announced their intentions to build the Palisades Nuclear Generating Station on the shoreline of Lake Michigan in 1967, Mary Sinclair's background in nuclear fission technology prompted her to write a letter to the editor questioning the safety of several elements of their plan.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Mount Showers. z1pq3xbwkkuzgbnvcns1ch9j2dc" xml:space="preserve">#redirect Mount Showers

Geographic entities mentioned:
surface_form: mount showers
instance_of: Mountain
coordinates: lat: -71.75
lon: -61.466666666667
surface_form: showers
instance_of: Mountain
coordinates: lat: -71.75
lon: -61.466666666667
Geography. Except for the Danube Delta, a marshy region located in its northeastern corner, Dobruja is hilly, with an average altitude of about 200–300  metres. The highest point is the Țuțuiatu (Greci) Peak in the Măcin Mountains, having a height of 467 m. The Dobruja Plateau covers most of the Romanian part of Dobruja. The Ludogorie Plateau is found in Bulgaria.

Geographic entities mentioned:
surface_form: Dobruja Plateau
instance_of: Plateau
countries: Romania
coordinates: lat: 44
lon: 28.25
The Parrett Navigation Act. Despite the scheme not being finished, some traffic continued to use the river. The Parrett Navigation Act, which was obtained in 1836, authorised improvements to the River Parrett below Langport, the construction of a canal to Westport, and the rebuilding of the Great Bow Bridge, to allow larger boats to travel beyond Langport.

Geographic entities mentioned:
surface_form: River Parrett
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 51.2292
lon: -3.00861
Geography. Krems is located at the confluence of the Krems and Danube Rivers at the eastern end of Wachau valley, in the southern Waldviertel. Krems borders the following municipalities: Stratzing, Langenlois, Rohrendorf bei Krems, Gedersdorf, Traismauer, Nußdorf ob der Traisen, Paudorf, Furth bei Göttweig, Mautern an der Donau, Dürnstein, and Senftenberg. History.

Geographic entities mentioned:
surface_form: Wachau
instance_of: Valley
countries: Austria
coordinates: lat: 48.36444
lon: 15.43417
Gamchen. Gamchen () is a complex volcano located in the southeastern part of the Kamchatka Peninsula, Russia. It is composed of four stratovolcanoes.

Geographic entities mentioned:
surface_form: gamchen
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 54.973055555556
lon: 160.70083333333
He is a member of the United Methodist Church. Larson is also a quail hunter and bass fisherman. San Antonio International Ag Promotions, which he founded, hosts such trade expositions as the San Antonio International Farm and Ranch Show and the Texas Hunting and Outdoor Classic. He takes an annual fishing trip to Lake Michigan with friends from high school and college.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Brambilla. 5w4dopcpl51tljyv3aiekfofdlvi5" xml:space="preserve">Brambilla is an Italian surname derived from Val Brembana in Italy. In the 1700s the name travelled to a small town in the state of Jalisco Mexico and was modified to Brambila to retain pronunciation in Spanish. Geographical distribution.

Geographic entities mentioned:
surface_form: Val Brembana
instance_of: Valley
countries: Italy
coordinates: lat: 45.8725
lon: 9.651944444444444
Glen Ellen, California. Glen Ellen is a census-designated place (CDP) in Sonoma Valley, Sonoma County, California, United States. The population was 714 at the 2020 census, down from 784 at the 2010 census. Glen Ellen is the location of Jack London State Historic Park (including the Wolf House), Sonoma Valley Regional Park, and a former home of Hunter S. Thompson.

Geographic entities mentioned:
surface_form: Sonoma Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.3667
lon: -122.5
In October 2017, the area was badly affected by wildfire. Geography. Glen Ellen is about northwest of the city of Sonoma. The United States Census Bureau fixes the total area at, 99.95% of it land and 0.05% covered by water. Sonoma Creek, the principal river of the Sonoma Valley, flows through Glen Ellen. Demographics. Glen Ellen first appeared as a census designated place in the 1980 U.S. Census.

Geographic entities mentioned:
surface_form: Sonoma Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.3667
lon: -122.5
(&quot;The Valley of the Moon&quot; is a translation of Sonoma Valley's name given by the Pomo and Coast Miwok peoples.)
The site of his ranch is now Jack London State Historic Park, which contains the ruins of Wolf House, several ranch buildings, the grave of Jack and Charmian London, and a museum housed in Charmian London's &quot;House of Happy Walls&quot;.

Geographic entities mentioned:
surface_form: Sonoma Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.3667
lon: -122.5
Its predecessor, the California Home for the Care and Training of Feeble Minded Children, was the setting for Jack London's story &quot;Told in the Drooling Ward.&quot;
Glen Ellen is located in the Wine Country and is part of the Sonoma Mountain AVA. Like all the communities in Sonoma Valley, Glen Ellen is home to many vineyards and wineries including B.R.

Geographic entities mentioned:
surface_form: Sonoma Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.3667
lon: -122.5
Goat Mountain (Cordova). Goat Mountain is a summit in the U.S. state of Alaska. Description. Goat Mountain is located in the Chugach Mountains, east-northeast of Cordova on land managed by Chugach National Forest. Although modest in elevation, topographic relief is significant as the summit rises 4,300 feet (1,310 m) above Miles Lake in less than three miles (4.8 km).

Geographic entities mentioned:
surface_form: goat mountain (cordova)
instance_of: Mountain
coordinates: lat: 60.607108
lon: -144.6462468
Goat Mountain (Cordova). Goat Mountain is a summit in the U.S. state of Alaska. Description. Goat Mountain is located in the Chugach Mountains, east-northeast of Cordova on land managed by Chugach National Forest. Although modest in elevation, topographic relief is significant as the summit rises 4,300 feet (1,310 m) above Miles Lake in less than three miles (4.8 km).

Geographic entities mentioned:
surface_form: goat mountain
instance_of: Mountain
coordinates: lat: 60.607108
lon: -144.6462468
state of Alaska. Description. Goat Mountain is located in the Chugach Mountains, east-northeast of Cordova on land managed by Chugach National Forest. Although modest in elevation, topographic relief is significant as the summit rises 4,300 feet (1,310 m) above Miles Lake in less than three miles (4.8 km). The mountain can be seen from the Copper River Highway at the Miles Glacier Bridge.

Geographic entities mentioned:
surface_form: goat mountain
instance_of: Mountain
coordinates: lat: 60.607108
lon: -144.6462468
Board on Geographic Names. Climate. Based on the Köppen climate classification, Goat Mountain is located in a subpolar oceanic climate zone, with long, cold, snowy winters, and cool summers. Weather systems coming off the Gulf of Alaska are forced upwards by the Chugach Mountains (orographic lift), causing heavy rainfall. Winter temperatures can drop to 0 °F with wind chill factors below −10 °F.

Geographic entities mentioned:
surface_form: goat mountain
instance_of: Mountain
coordinates: lat: 60.607108
lon: -144.6462468
North of the Souris basin, an arm of this lake extended along the Assiniboine River from Griswold and Oak Lake to some distance above the mouth of the Qu'Appelle River in Saskatchewan; and the main body of the lake was deeply indented on the east by the high oval area of Turtle Mountain, and forms, with overlying drift deposits, the massive terrace of the Missouri Coteau on the west.

Geographic entities mentioned:
surface_form: Missouri Coteau
instance_of: Plateau
countries: Canada
United States
coordinates: lat: 50.8
lon: -109.2
The gold contained in the Lake Souris gravel deposits was apparently derived from rocks of the Canadian Shield to the north. The glaciers that transported the gold to north-central North Dakota flowed over what are today the Gods Lake, Flin Flon, and Lac La Ronge mining districts of northern Manitoba and Saskatchewan.

Geographic entities mentioned:
surface_form: Gods Lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.67388888888889
lon: -94.24666666666667
New York State Route 255 (now decommissioned) joined New York State Route 256 in Sparta. New York State Route 63 is a north-south highway in the western part of the town. Conesus Inlet, flowing toward Conesus Lake, is in the northwest part of the town. Demographics. As of the census of 2000, there were 1,627 people, 595 households, and 462 families residing in the town. The population density was.

Geographic entities mentioned:
surface_form: Conesus Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.779722222222
lon: -77.716666666667
Goose Pond (Washington). Goose Pond is a pond in the U.S. state of Washington. Goose Pond was named for the geese which congregate there.

Geographic entities mentioned:
surface_form: goose pond
instance_of: Lake
countries: United States
coordinates: lat: 47.0365614
lon: -122.7970914
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Goose Pond (Washington). Goose Pond is a pond in the U.S. state of Washington. Goose Pond was named for the geese which congregate there.

Geographic entities mentioned:
surface_form: goose pond
instance_of: Lake
countries: United States
coordinates: lat: 47.0365614
lon: -122.7970914
Ilan Halimi was initially buried in the Cimetière parisien de Pantin near Paris, and the funeral drew a large Jewish crowd. At the request of the family, his remains were reburied in Har HaMenuchot cemetery in Jerusalem on 9 February 2007. It was timed to allow his first Yartzeit, on Tu Bishvat, to pass before the reburial.

Geographic entities mentioned:
surface_form: Har HaMenuchot
instance_of: Mountain
countries: Israel
coordinates: lat: 31.798133333333
lon: 35.177727777778
What became known as the Tonypandy riots of 1910 and 1911 (sometimes collectively known as the Rhondda riots) were a series of violent confrontations between striking coal miners and police that took place at various locations in and around the Rhondda mines of the Cambrian Combine, a consortium of mining companies in South Wales.

Geographic entities mentioned:
surface_form: Rhondda
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
On 2 November 1910, the authorities in South Wales began enquiring about the procedures for requesting military aid in the event of disturbances caused by the striking miners. The Glamorgan Constabulary's resources were already stretched due to multiple industrial disputes, as there was a month-old strike ongoing in the neighbouring Cynon Valley in addition to the Cambrian Combine dispute.

Geographic entities mentioned:
surface_form: Cynon Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.657
lon: -3.461
Pacific Standard Time, March 17, 1998. The Change alters both the course of history and all physical laws when it causes all the electricity, firearms, explosives, internal combustion engines, steam power and most forms of high-energy-density technology on Earth to permanently no longer work. Most of the action in the series takes place in the Willamette Valley of Oregon in the United States.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Areas of China that survived came under attack by mounted hordes from the Mongolian steppe. India devolved to a fervently nationalistic northeastern state called Hinduraj, with smaller populations surviving south in the Deccan. Parts of South America apparently survived, given that Cardinals from there participated in the election of the new Pope.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Public life. During the late 1860s, Staub began working with a group called the Tennessee Clonisation Gesellschaft, which sought to establish colonies of Swiss immigrants atop the Cumberland Plateau west of Knoxville. Staub purchased a large tract of land along a remote section of the Plateau in Grundy County in 1869 that provided the core of the Swiss colony of Gruetli (now Gruetli-Laager).

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
The marbled lungfish is caught in large numbers throughout much of its range, including several hundred metric tonnes per year in Mwanza Region's Mwanza Gulf of Lake Victoria alone. It is mostly a food fish, although this varies depending on the exact community, with some recognizing it as a delicacy and others strongly disliking its taste or considering it as a taboo to eat it.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Distribution. &quot;Protopterus aethiopicus&quot; is found in the African countries of Angola, Burundi, Egypt, Ethiopia, the Democratic Republic of Congo, Kenya, Republic of the Congo, Rwanda, South Sudan, Sudan, Tanzania, Uganda and Zambia. Among others, it lives in the Nile and Congo River basins, including lakes such as Albert, Edward, Tanganyika, Victoria, Nabugabo, Turkana, No and Kyoga.

Geographic entities mentioned:
surface_form: Edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
surface_form: Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
surface_form: Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
surface_form: Nabugabo
instance_of: Lake
countries: Uganda
coordinates: lat: -0.37
lon: 31.9
surface_form: No
instance_of: Lake
countries: South Sudan
coordinates: lat: 9.4977777777778
lon: 30.465