Sarmila/GeoWiki-Features huggingface dataset:
Geography. Saudi Arabia has a range of mountains, the Sarawat or Sarat Mountains, which run parallel with the Red Sea coast. These are low at the northern end, have a gap in the middle between Medina and Ta'if, and are higher at the southern end, where Mount Soudah in the Asir Mountains, at just over is the highest point in Saudi Arabia.

Geographic entities mentioned:
surface_form: Mount Soudah
instance_of: Mountain
countries: Saudi Arabia
coordinates: lat: 18.267222222222
lon: 42.368055555556
The mountainous region of Asir in the southwest is wetter; it receives monsoon rains between May and October which may amount to. The northern Ha'il Region has the Shammar Mountains, further divisible into the Aja and Salma subranges. The Red Sea was formed when in the Eocene period, the Arabian Peninsula began to move away from the continent of Africa.

Geographic entities mentioned:
surface_form: Shammar Mountains
instance_of: Mountain
countries: Saudi Arabia
coordinates: lat: 27.5
lon: 41.6
surface_form: Salma
instance_of: Mountain
countries: Saudi Arabia
coordinates: lat: 27.09777777777778
lon: 42.12388888888889
But Zafeirakis quickly opposed Ali Pasha's authoritative administration. As a result, Ali Pasha turned against him and he was forced to abandon his place for Thessaloniki and later Mount Athos and Constantinople.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
the Mousterian industry is named after the site of Le Moustier). By contrast, Neolithic axeheads from the Langdale axe industry were recognised as a type well before the centre at Great Langdale was identified by finds of debitage and other remains of the production, and confirmed by petrography (geological analysis).

Geographic entities mentioned:
surface_form: Great Langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.449119444444
lon: -3.0733305555556
Teotihuacan. Teotihuacan (; Spanish: &quot;Teotihuacán&quot;,;) is an ancient Mesoamerican city located in a sub-valley of the Valley of Mexico, which is located in the State of Mexico, northeast of modern-day Mexico City.

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
The city may have lasted until sometime between the 7th and 8th centuries CE, but its major monuments were sacked and systematically burned around 550 CE. Its collapse might be related to the extreme weather events of 535–536. Teotihuacan began as a religious center in the Mexican Plateau around the first century CE. It became the largest and most populated center in the pre-Columbian Americas.

Geographic entities mentioned:
surface_form: Mexican Plateau
instance_of: Plateau
countries: Mexico
coordinates: lat: 24
lon: -103
It now seems clear that may be understood as a generic Nahua term applied to any large settlement. In the Mesoamerican concept of urbanism, and other language equivalents serve as a metaphor, linking the bundles of reeds and rushes that formed part of the lacustrine environment of the Valley of Mexico and the large gathering of people in a city.

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
In the Late Formative era, a number of urban centers arose in central Mexico. The most prominent of these appears to have been Cuicuilco, on the southern shore of Lake Texcoco. Scholars have speculated that the eruption of the Xitle volcano may have prompted a mass emigration out of the central valley and into the Teotihuacan valley.

Geographic entities mentioned:
surface_form: Lake Texcoco
instance_of: Lake
countries: Mexico
coordinates: lat: 19.5
lon: -98.99
The most prominent of these appears to have been Cuicuilco, on the southern shore of Lake Texcoco. Scholars have speculated that the eruption of the Xitle volcano may have prompted a mass emigration out of the central valley and into the Teotihuacan valley. These settlers may have founded or accelerated the growth of Teotihuacan.

Geographic entities mentioned:
surface_form: Xitle
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.245669
lon: -99.222706
No traces of foreign invasion are visible at the site. Evidence for population decline beginning around the 6th century lends some support to the internal unrest hypothesis. The decline of Teotihuacan has been correlated to lengthy droughts related to the climate changes of 535–536, possibly caused by the eruption of the Ilopango volcano in El Salvador.

Geographic entities mentioned:
surface_form: the Ilopango volcano
instance_of: Lake
countries: El Salvador
coordinates: lat: 13.66666667
lon: -89.05
The mountain is situated on the crest of the Cascade Range, on the shared border of Snohomish County and Chelan County, and also straddling the boundary between Mount Baker-Snoqualmie National Forest and Wenatchee National Forest. White Mountain is located to the west-southwest of Kololo Peaks, and immediately north of White Pass. The Pacific Crest Trail traverses the south slope of the peak.

Geographic entities mentioned:
surface_form: Kololo Peaks
instance_of: Mountain
countries: United States
coordinates: lat: 48.064166666666665
lon: -121.09722222222221
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.94687
lon: -119.3096
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.040555555556
lon: -121.15305555556
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5781
lon: -109.32
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.67648
lon: -123.32823
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.0030248
lon: -111.4687966
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.634166666667
lon: -118.25555555556
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.9555
lon: -110.735
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.57476
lon: -114.49565
With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted. Glacier Peak, a stratovolcano that is north-northeast of White Mountain, began forming in the mid-Pleistocene. Due to Glacier Peak's proximity to White Mountain, volcanic ash is common in the area and provides fertile soil for an abundance of wildflowers.

Geographic entities mentioned:
surface_form: Glacier Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.94687
lon: -119.3096
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.14972222
lon: -109.84944444
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.040555555556
lon: -121.15305555556
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.155013
lon: -117.293429
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5781
lon: -109.32
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.67648
lon: -123.32823
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.0030248
lon: -111.4687966
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.634166666667
lon: -118.25555555556
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.9555
lon: -110.735
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.57476
lon: -114.49565
White Mountain (Washington). White Mountain is a mountain located in the Glacier Peak Wilderness of the North Cascades in Washington state. The mountain is situated on the crest of the Cascade Range, on the shared border of Snohomish County and Chelan County, and also straddling the boundary between Mount Baker-Snoqualmie National Forest and Wenatchee National Forest.

Geographic entities mentioned:
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.94687
lon: -119.3096
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.040555555556
lon: -121.15305555556
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5781
lon: -109.32
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.67648
lon: -123.32823
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.0030248
lon: -111.4687966
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.634166666667
lon: -118.25555555556
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.9555
lon: -110.735
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.57476
lon: -114.49565
White Mountain (Washington). White Mountain is a mountain located in the Glacier Peak Wilderness of the North Cascades in Washington state. The mountain is situated on the crest of the Cascade Range, on the shared border of Snohomish County and Chelan County, and also straddling the boundary between Mount Baker-Snoqualmie National Forest and Wenatchee National Forest.

Geographic entities mentioned:
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.94687
lon: -119.3096
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.14972222
lon: -109.84944444
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.040555555556
lon: -121.15305555556
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.155013
lon: -117.293429
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5781
lon: -109.32
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.67648
lon: -123.32823
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.0030248
lon: -111.4687966
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.634166666667
lon: -118.25555555556
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.9555
lon: -110.735
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.57476
lon: -114.49565
With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted. Glacier Peak, a stratovolcano that is north-northeast of White Mountain, began forming in the mid-Pleistocene. Due to Glacier Peak's proximity to White Mountain, volcanic ash is common in the area and provides fertile soil for an abundance of wildflowers.

Geographic entities mentioned:
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.94687
lon: -119.3096
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.14972222
lon: -109.84944444
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.040555555556
lon: -121.15305555556
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.155013
lon: -117.293429
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5781
lon: -109.32
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.67648
lon: -123.32823
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.0030248
lon: -111.4687966
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.634166666667
lon: -118.25555555556
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.9555
lon: -110.735
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.57476
lon: -114.49565
Uplift and faulting in combination with glaciation have been the dominant processes which have created the tall peaks and deep valleys of the North Cascades area. Climate. White Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originating in the Pacific Ocean travel northeast toward the Cascade Mountains.

Geographic entities mentioned:
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.94687
lon: -119.3096
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.040555555556
lon: -121.15305555556
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5781
lon: -109.32
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.67648
lon: -123.32823
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.0030248
lon: -111.4687966
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.634166666667
lon: -118.25555555556
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.9555
lon: -110.735
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.57476
lon: -114.49565
White Mountain (Washington). White Mountain is a mountain located in the Glacier Peak Wilderness of the North Cascades in Washington state. The mountain is situated on the crest of the Cascade Range, on the shared border of Snohomish County and Chelan County, and also straddling the boundary between Mount Baker-Snoqualmie National Forest and Wenatchee National Forest.

Geographic entities mentioned:
surface_form: chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Astraea Nunatak. Astraea Nunatak () is a nunatak south of Staccato Peaks in southern Alexander Island.

Geographic entities mentioned:
surface_form: Staccato Peaks
instance_of: Mountain
coordinates: lat: -71.783333333333
lon: -70.65
Geology. According to the British Antarctic Survey's (BAS) aeromagnetic 1975 survey of Astraea Nunatak and nearby Ceres Nunataks, this geographical feature is rich in the igneous rocks Diorite and Tonalite as presumed by the rock samples which were observed by BAS during this survey. Aeromagnetic Survey of Astraea Nunatak and Ceres Nunataks.

Geographic entities mentioned:
surface_form: Ceres Nunataks
instance_of: Mountain
coordinates: lat: -72.05
lon: -70.4167
Kaisersee. Kaisersee is a lake in Augsburg, Schwaben, Bavaria, Germany. Its surface area is 4 ha.

Geographic entities mentioned:
surface_form: kaisersee
instance_of: Lake
countries: Germany
coordinates: lat: 48.419269444444
lon: 10.917513888889
Mount Dall. Mount Dall is a mountain in the Alaska Range, in Denali National Park and Preserve, southwest of Denali. Mount Dall was named in 1902 by A.H. Brooks of the U.S. Geological Survey after naturalist and Alaska explorer William Healey Dall.

Geographic entities mentioned:
surface_form: Denali
instance_of: Mountain
countries: United States
coordinates: lat: 63.06916666666667
lon: -151.0063888888889
surface_form: denali
instance_of: Mountain
countries: United States
coordinates: lat: 63.06916666666667
lon: -151.0063888888889
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount dall
instance_of: Mountain
countries: United States
coordinates: lat: 62.5792
lon: -152.294
Mount Dall. Mount Dall is a mountain in the Alaska Range, in Denali National Park and Preserve, southwest of Denali. Mount Dall was named in 1902 by A.H. Brooks of the U.S. Geological Survey after naturalist and Alaska explorer William Healey Dall.

Geographic entities mentioned:
surface_form: mount dall
instance_of: Mountain
countries: United States
coordinates: lat: 62.5792
lon: -152.294
Goulburn Valley. The Goulburn Valley is a sub-region, part of the Hume region of the Australian state of Victoria. The sub-region consists of those areas in the catchment of the Goulburn River and other nearby streams, and is part of the Murray-Darling Basin.

Geographic entities mentioned:
surface_form: goulburn valley
instance_of: Valley
countries: Australia
coordinates: lat: -36.3831
lon: 145.399
The Goulburn Valley is a sub-region, part of the Hume region of the Australian state of Victoria. The sub-region consists of those areas in the catchment of the Goulburn River and other nearby streams, and is part of the Murray-Darling Basin. The Goulburn Valley is bordered on the south by the Great Dividing Range and to the north by the Murray River, the state border with New South Wales.

Geographic entities mentioned:
surface_form: goulburn valley
instance_of: Valley
countries: Australia
coordinates: lat: -36.3831
lon: 145.399
The Goulburn Valley is bordered on the south by the Great Dividing Range and to the north by the Murray River, the state border with New South Wales. The sub-region is one of Australia's most productive and intensively farmed areas and is predominantly irrigated. Major regional centres of the Goulburn Valley are Shepparton, Seymour, Echuca, Benalla, Yarrawonga and Kyabram. History.

Geographic entities mentioned:
surface_form: goulburn valley
instance_of: Valley
countries: Australia
coordinates: lat: -36.3831
lon: 145.399
Major regional centres of the Goulburn Valley are Shepparton, Seymour, Echuca, Benalla, Yarrawonga and Kyabram. History. Aboriginal groups inhabited the Goulburn Valley region prior to European settlement. In the central Goulburn around Nagambie, the traditional owners were the Natrakboolok, Ngooraialum or Thagungwurung tribes.

Geographic entities mentioned:
surface_form: goulburn valley
instance_of: Valley
countries: Australia
coordinates: lat: -36.3831
lon: 145.399
Economy. Industries in the Goulburn Valley include agricultural activities such as fruit growing and dairying, which supply processing plants in Shepparton and outlying towns such as Strathmerton and Tongala. This food processing industry produces around 25% of Victoria's rural output. The SPC Ardmona plant, founded in 1917 in Shepparton, is one of the world's largest fruit canneries.

Geographic entities mentioned:
surface_form: goulburn valley
instance_of: Valley
countries: Australia
coordinates: lat: -36.3831
lon: 145.399
As well as Tahbilk, other major wineries include Michelton between Seymour and Nagambie, Wine by Sam, Fowles Wines and boutique vineyards Box Grove and Brave Goose vineyard in the south near Seymour and Monichino near Katunga in the north. Nagambie Lakes is a recognised and protected subregion of the Goulburn Valley wine region.

Geographic entities mentioned:
surface_form: goulburn valley
instance_of: Valley
countries: Australia
coordinates: lat: -36.3831
lon: 145.399
Nagambie Lakes is a recognised and protected subregion of the Goulburn Valley wine region. Each year &quot;Tastes of the Goulburn&quot; food and wine festival is hosted in Seymour, showcasing the best local produce from the Goulburn Valley. Seymour also hosts the Victorian Wine Show. Politics.

Geographic entities mentioned:
surface_form: goulburn valley
instance_of: Valley
countries: Australia
coordinates: lat: -36.3831
lon: 145.399
Transport. Major transport routes through the Goulburn Valley region include the Goulburn Valley Highway, Midland Highway and the Murray Valley Highway. Passenger rail services are provided from Melbourne to Seymour railway station the junction for they North East and Goulburn Valley lines which was opened in 1872 and then onto Shepparton and Echuca by Line.

Geographic entities mentioned:
surface_form: goulburn valley
instance_of: Valley
countries: Australia
coordinates: lat: -36.3831
lon: 145.399
surface_form: goulburn valley
instance_of: Valley
countries: Australia
coordinates: lat: -36.3831
lon: 145.399
Transport. Major transport routes through the Goulburn Valley region include the Goulburn Valley Highway, Midland Highway and the Murray Valley Highway. Passenger rail services are provided from Melbourne to Seymour railway station the junction for they North East and Goulburn Valley lines which was opened in 1872 and then onto Shepparton and Echuca by Line.

Geographic entities mentioned:
surface_form: goulburn valley
instance_of: Valley
countries: Australia
coordinates: lat: -36.3831
lon: 145.399
Food scholar Pushpesh Pant also challenges the Mughal-origin claim, stating that it originated in Iran and that &quot;there is no evidence that biryani first came to this land with the Mughals. It is far more probable that it travelled with pilgrims and soldier-statesmen of noble descent to the Deccan region in South India&quot;.

Geographic entities mentioned:
surface_form: Deccan region
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Hyderabadi biryani. Hyderabadi &quot;biryani&quot; is India's most famous &quot;biryani&quot;; some say &quot;biryani&quot; is synonymous with Hyderabad. Hyderabadi &quot;biryani&quot; developed in Hyderabad Subah under the rule of Asaf Jah I, who was first appointed as the governor of Deccan by the Mughal Emperor Aurangzeb. It is made with &quot;basmati&quot; rice, spices and goat meat.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Likewise, the precipitation record is incomplete, with some months having less than ten years of record. Prior names. Alternate prior names for the lake were &quot;Natravak Lake&quot; and &quot;Sagavanirktok Lake.&quot; &quot;Natravak&quot; is an Eskimo name for &quot;big lake&quot; and a common name in northern Alaska.

Geographic entities mentioned:
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 40.0725
lon: -95.345
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 45.1722398
lon: -67.6821052
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 45.819722222222
lon: -96.113055555556
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 31.1667
lon: -101.483
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 33.8847
lon: -109.415
Galbraith Lake. Galbraith Lake is a lake located in the North Slope Borough of Alaska, United States. The surrounding area is uninhabited except for seasonal residents. The lake is located on the west side of the Dalton Highway between miles 272-75 of the highway.

Geographic entities mentioned:
surface_form: galbraith lake
instance_of: Lake
countries: United States
coordinates: lat: 68.4584432
lon: -149.416606
A campground is also located near the lake. The lake was named in 1951 after Bart Galbraith, a bush pilot who died in a 1950 plane crash while flying from Barter Island to Barrow. Galbraith Lake Airport is located in the area, as well as Pump Station 4 of the Trans-Alaska Pipeline System. A work camp was located at Galbraith Lake during the construction of the pipeline.

Geographic entities mentioned:
surface_form: galbraith lake
instance_of: Lake
countries: United States
coordinates: lat: 68.4584432
lon: -149.416606
Galbraith Lake Airport is located in the area, as well as Pump Station 4 of the Trans-Alaska Pipeline System. A work camp was located at Galbraith Lake during the construction of the pipeline. An oil spill near the camp in 1975 caused some oil to enter the lake and a slick to appear on its surface. Clean up efforts were then conducted.

Geographic entities mentioned:
surface_form: galbraith lake
instance_of: Lake
countries: United States
coordinates: lat: 68.4584432
lon: -149.416606
The infrastructure of the pipeline construction project in the 1970s also permitted the conduct of archeological investigations in the area, which previously had not been explored, funded by the Alyeska Pipeline Service Company. Campground. The Galbraith Lake Bureau of Land Management Campground is 359 miles north of Fairbanks and 140 miles south of Deadhorse at the 275 mile mark. Climate.

Geographic entities mentioned:
surface_form: galbraith lake
instance_of: Lake
countries: United States
coordinates: lat: 68.4584432
lon: -149.416606
Campground. The Galbraith Lake Bureau of Land Management Campground is 359 miles north of Fairbanks and 140 miles south of Deadhorse at the 275 mile mark. Climate. Galbraith Lake has a cold subarctic climate, bordering on a true tundra climate. Snow has occurred in all three summer months. During the construction of the Alaska Pipeline a weather station was operated at the construction site.

Geographic entities mentioned:
surface_form: galbraith lake
instance_of: Lake
countries: United States
coordinates: lat: 68.4584432
lon: -149.416606
Owens River. The Owens River is a river in eastern California in the United States, approximately long. It drains into and through the Owens Valley, an arid basin between the eastern slope of the Sierra Nevada and the western faces of the Inyo and White Mountains. The river terminates at the endorheic Owens Lake south of Lone Pine, at the bottom of a watershed.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
Course. The river rises in the Sierra Nevada in southwestern Mono County, approximately south of Mono Lake and east of Yosemite Valley. It flows southeast across the Long Valley Caldera, through Lake Crowley reservoir, then descends through the Owens River Gorge, emerging at the north end of the Owens Valley northwest of Bishop.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
Course. The river rises in the Sierra Nevada in southwestern Mono County, approximately south of Mono Lake and east of Yosemite Valley. It flows southeast across the Long Valley Caldera, through Lake Crowley reservoir, then descends through the Owens River Gorge, emerging at the north end of the Owens Valley northwest of Bishop.

Geographic entities mentioned:
surface_form: Long Valley Caldera
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
The river flows mainly on the east side of the valley, because alluvial deposits from Sierra Nevada streams have forced the river channel in that direction. Vertical relief in the basin is immense – elevations range from at Mount Whitney, the highest peak in the continental United States, to on the bed of Owens Lake. The Owens River itself heads at an elevation of.

Geographic entities mentioned:
surface_form: Mount Whitney
instance_of: Mountain
countries: United States
coordinates: lat: 36.57861111111111
lon: -118.29194444444444
Further to the north, the Owens River basin encompasses predominantly igneous rocks and vast remnants of past volcanic activity. The upper of the river run through the Long Valley Caldera, an enormous -wide crater formed by a volcanic eruption some 760,000 years ago. The eruption's resulting ash cloud covered much of the southwestern United States, including parts of ten U.S. states.

Geographic entities mentioned:
surface_form: Long Valley Caldera
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
states. Mammoth Mountain, to the southwest (more popularly known as a major ski area) also formed from eruptions related to the Long Valley Caldera. To the north of the Caldera, extending to the Mono Lake area, lie the chain of Mono-Inyo Craters, which range in age from 400,000 to 500 years old.

Geographic entities mentioned:
surface_form: Mammoth Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6306
lon: -119.033
The increased river volume caused Owens Lake to rise as well, eventually spilling out the south side of the valley into the Mojave Desert. Ancient, now-abandoned river channels suggest that the extended Owens River ran south to China Lake, then east into Searles Lake, north into the Panamint Valley (where it formed Panamint Lake), and finally east into Death Valley and the ancient Lake Manly.

Geographic entities mentioned:
surface_form: Panamint Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.0592
lon: -117.244
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Walker, who also came into the area in the 1800s. Gradually, the river's surroundings were settled by farmers and ranchers. The valley never accumulated a very large population, but mining activities brought significant income to the new inhabitants of the area. Ore was shipped down the Owens River from the north, and also borax and silver from Death Valley to the east.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Although it is controversial whether beaver were once native to the Owens Valley, there is growing evidence that they were native to the eastern slope of the Sierra Nevada. In particular, the northern Paiute of Walker Lake, Honey Lake and Pyramid Lake have a word for beaver &quot;su-i'-tu-ti-kut'-teh&quot;.

Geographic entities mentioned:
surface_form: Honey Lake
instance_of: Lake
countries: United States
coordinates: lat: 40.25
lon: -120.35
This occurs slightly inland from the outer skerry guard. In the updated 1991-2020 normals, Gullfjellet in Bergen (345 m) has the highest annual precipitation with. Annual precipitation can exceed in mountain areas near the coast. Lurøy Municipality at the Arctic Circle gets annually, a remarkable amount for a polar location.

Geographic entities mentioned:
surface_form: Gullfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 60.38752777777778
lon: 5.5904444444444445
The differences of inland areas are larger, with a maximum difference of in Karasjok Municipality. Finnmarksvidda has the coldest winters in mainland Norway, but inland areas much further south can also experience severe cold. Røros Municipality has recorded. Bø Municipality is the most northerly location in the world where all winter months have mean temperatures above.

Geographic entities mentioned:
surface_form: Finnmarksvidda
instance_of: Plateau
countries: Norway
coordinates: lat: 69.31666667
lon: 23.81666667
Lake Marion (McLeod County, Minnesota). Lake Marion is a lake in McLeod County, in the U.S. state of Minnesota. Lake Marion was named for Marion Hoag, the daughter of settler Charles Hoag.

Geographic entities mentioned:
surface_form: lake marion (mcleod county, minnesota)
instance_of: Lake
countries: United States
coordinates: lat: 44.783333333333
lon: -94.384722222222
surface_form: lake marion
instance_of: Lake
countries: United States
coordinates: lat: 40.46
lon: -115.457
Lake Marion (McLeod County, Minnesota). Lake Marion is a lake in McLeod County, in the U.S. state of Minnesota. Lake Marion was named for Marion Hoag, the daughter of settler Charles Hoag.

Geographic entities mentioned:
surface_form: lake marion
instance_of: Lake
countries: United States
coordinates: lat: 44.783333333333
lon: -94.384722222222
surface_form: lake marion
instance_of: Lake
countries: United States
coordinates: lat: 40.46
lon: -115.457
Rattlesnake Point (United States). Rattlesnake Point is a summit located in the Brady Mountains in central Texas. It is located entirely in McCulloch County.

Geographic entities mentioned:
surface_form: rattlesnake point
instance_of: Mountain
countries: United States
coordinates: lat: 31.2664
lon: -99.5347
Hurricane Lane (2018). Hurricane Lane was a powerful tropical cyclone that brought torrential rainfall and strong winds to Hawaii during late August 2018. The storm was the wettest on record in Hawaii, with peak rainfall accumulations of 58 inches (1,473 mm) along the eastern slopes of Mauna Kea.

Geographic entities mentioned:
surface_form: Mauna Kea
instance_of: Mountain
countries: United States
coordinates: lat: 19.820555555555554
lon: -155.46805555555557
Big Island. Although Hurricane Lane remained west of the Big Island, tremendous amounts of rain battered eastern areas of the island from August 22 to 26. Accumulations were greatest along the eastern slopes of Mauna Kea with a maximum of at Kahūnā Falls in Akaka Falls State Park, as measured by a private weather station.

Geographic entities mentioned:
surface_form: Mauna Kea
instance_of: Mountain
countries: United States
coordinates: lat: 19.820555555555554
lon: -155.46805555555557
Personal life. Gaon married Sarah ben Binyamin Hakim, a native of İzmir. They had 4 children, two daughters: Kalila and Yigal, and two sons, businessmen Benny Gaon and Yehoram Gaon. He died on 8 October 1958 and is buried at Har HaMenuchot.

Geographic entities mentioned:
surface_form: Har HaMenuchot
instance_of: Mountain
countries: Israel
coordinates: lat: 31.798133333333
lon: 35.177727777778
Dennistoun Glacier. The Dennistoun Glacier () is a glacier, long, draining the northern slopes of Mount Black Prince, Mount Royalist and Mount Adam in the Admiralty Mountains of Victoria Land, Antarctica. It flows northwest between the Lyttelton Range and Dunedin Range, turning east on rounding the latter range to enter the sea south of Cape Scott. Exploration and naming.

Geographic entities mentioned:
surface_form: Mount Royalist
instance_of: Mountain
coordinates: lat: -71.78333333
lon: 168.5
The Anare Pass is to its west, forming a route to the Ebbe Glacier. The Dennistoun Glacier flows north and then east, fed by the Rowles Glacier and Lann Glacier from the southeast. It passes the Hedgpeth Heights and Quam Heights to the north in the Anare Mountains. It enters the sea to the southeast of Cape Scott and northwest of Ponting Cliff and Meares Cliff.

Geographic entities mentioned:
surface_form: Hedgpeth Heights
instance_of: Mountain
coordinates: lat: -71.11666667
lon: 167.5
surface_form: Quam Heights
instance_of: Mountain
coordinates: lat: -71.05
lon: 167.8
A tributary glacier, long, in the Admiralty Mountains. From a common head with Dennistoun Glacier, it flows northwest between Mount Ajax and Mount Faget, entering the main flow of the Dennistoun Glacier at the southeast base of the Lyttelton Range. Named after Walter Fowlie of the New Zealand Antarctic Division, field assistant with a NZARP geological party to this area, 1981-82, led by R.H.

Geographic entities mentioned:
surface_form: Mount Ajax
instance_of: Mountain
coordinates: lat: -71.8
lon: 168.45
surface_form: Mount Faget
instance_of: Mountain
coordinates: lat: -71.7333
lon: 168.433
Hundsheimer Berg. Hundsheimer Berg is a hill located in the Hundsheimer Berge hill range in Lower Austria, Austria close to the border with Slovakia. Its peak is above sea level which makes it the highest hill in the Hundsheimer Berge. The north slopes of the Hundsheimer Berg are covered with forests while the southern slopes have a steppe vegetation.

Geographic entities mentioned:
surface_form: hundsheimer berg
instance_of: Mountain
countries: Austria
coordinates: lat: 48.1322
lon: 16.9386
Its peak is above sea level which makes it the highest hill in the Hundsheimer Berge. The north slopes of the Hundsheimer Berg are covered with forests while the southern slopes have a steppe vegetation. Since 1965, a nature reserve with the same name, &quot;Hundsheimer Berg&quot;, is located on these southern slopes.

Geographic entities mentioned:
surface_form: hundsheimer berg
instance_of: Mountain
countries: Austria
coordinates: lat: 48.1322
lon: 16.9386
Cleft Peak. Cleft Peak is a mountain in South West Tasmania. It lies on the North West end of the Frankland Range jutting out toward the East from the range toward the impoundment, Lake Pedder. It is South East of Murpheys Bluff and North West of Greycap.

Geographic entities mentioned:
surface_form: murpheys bluff
instance_of: Mountain
countries: Australia
coordinates: lat: -42.954444444444
lon: 146.08
surface_form: greycap
instance_of: Mountain
countries: Australia
coordinates: lat: -42.971111111111
lon: 146.10694444444
Cleft Peak. Cleft Peak is a mountain in South West Tasmania. It lies on the North West end of the Frankland Range jutting out toward the East from the range toward the impoundment, Lake Pedder. It is South East of Murpheys Bluff and North West of Greycap.

Geographic entities mentioned:
surface_form: cleft peak
instance_of: Mountain
countries: Australia
coordinates: lat: -42.9625
lon: 146.09166666667
North Schell Peak. North Schell Peak is the highest mountain in the Schell Creek Range of White Pine County, Nevada, United States. It is the ninth-highest mountain in the state, and also ranks as the fifth-most topographically prominent peak in the state. The summit is northeast of the community of Ely within the High Schells Wilderness of the Humboldt-Toiyabe National Forest.

Geographic entities mentioned:
surface_form: north schell peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.41325
lon: -114.59969444444
It stars Raphaël Personnaz. Plot. To satisfy a need for freedom, the French media-director Teddy decides to leave the noise of the world, and settles alone in a cabin on the frozen shores of Lake Baikal. One night, lost in the blizzard, he is rescued by Aleksei, a Russian murderer on the run, who has been hiding in the Siberian forest for several years.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
The average depth of the lake is about 3 m, and the maximum depth is 4.7 m. The average annual water level varies up to 60 cm due to the fact that the lake is flowing. Through the river Zhinishkesu water goes to Lake Koshkarkol and then flows into Lake Alakol. Since the water in the lake is fresh, its mineralization varies during the year from 0.27 to 2.16 g/L.

Geographic entities mentioned:
surface_form: Lake Alakol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 46.081111111111
lon: 81.764166666667
surface_form: lake alakol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 46.081111111111
lon: 81.764166666667
surface_form: alakol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 46.081111111111
lon: 81.764166666667
surface_form: alakol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 51.20556
lon: 69.70754
Water birds including the mute swan, whooper swan, and spoonbill can be found here. Description. Into the Sasykkol lake (translated from the Kazakh language &quot;Sasyk&quot; - rotten, fetid;&quot; Kol &quot; - lake), in the delta of the Alakol Biosphere Reserve, flows the Tentek river from the south. The average depth of the lake is about 3 m, and the maximum depth is 4.7 m.

Geographic entities mentioned:
surface_form: alakol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 46.081111111111
lon: 81.764166666667
surface_form: alakol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 51.20556
lon: 69.70754
Lake Sasykkol. Sasykkol (, &quot;Sasyqköl&quot;) is a lake in eastern Kazakhstan. It is located near. It has a surface area of 600 km2 (736 km2 when water level is high), average depth of 3.3 m, and maximum depth of 4.7 m. Fishery on the lake is common. Water birds including the mute swan, whooper swan, and spoonbill can be found here. Description.

Geographic entities mentioned:
surface_form: sasykkol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 46.575555555556
lon: 80.974722222222
surface_form: lake sasykkol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 46.575555555556
lon: 80.974722222222
Lake Sasykkol. Sasykkol (, &quot;Sasyqköl&quot;) is a lake in eastern Kazakhstan. It is located near. It has a surface area of 600 km2 (736 km2 when water level is high), average depth of 3.3 m, and maximum depth of 4.7 m. Fishery on the lake is common. Water birds including the mute swan, whooper swan, and spoonbill can be found here. Description.

Geographic entities mentioned:
surface_form: sasykkol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 46.575555555556
lon: 80.974722222222
surface_form: sasyqköl
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 46.575555555556
lon: 80.974722222222
One of Mahmud of Ghazni's notable military campaigns during this period was the Siege of Lohkot in A.D. 1015. Positioned strategically in the Kashmir Valley, Lohkot (Iron Fort) presented a formidable challenge to Mahmud's forces due to its impregnable defenses. Despite persistent efforts, harsh winter conditions and reinforced defences compelled Mahmud to abandon the siege and retreat to Ghazni.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
Despite Mahmud's initial efforts, the fortress's formidable defenses proved insurmountable, leading to a protracted siege. Throughout the summer, Mahmud's army faced escalating challenges compounded by harsh winter conditions and heavy snowfall of Kashmir Valley. Concurrently, the defenders of Lohkot fortified their positions with reinforcements, further complicating Mahmud's campaign.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
The main flow is from west-north-west to east-south-east, the northernmost section is part of the Unstrut watershed (German river index 564), which in turn is part of the Saale (German River Index 56) and this in turn is part of the Elbe (German River index 5) watershed.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
The western limit of the Helme catchment area forms the main Elbe-Weser watershed: in the Harz between the Stöberhai mountain and the village of Osterhagen, then through the village of Osterhagen, the Mackenröde Forest and eastern crests of the Silkerode hill country west of Limlingerode, Stöckey and Epschenrode.

Geographic entities mentioned:
surface_form: Stöberhai
instance_of: Mountain
countries: Germany
coordinates: lat: 51.6563
lon: 10.5545
Lecanvey. Lecanvey () or Leckanvy () is a seaside village in County Mayo, Ireland, between Westport and Louisburgh, about 2 km west of Murrisk. It has a small beach with Lecanvey Pier. To the south is Croagh Patrick. To the west is Clare Island.

Geographic entities mentioned:
surface_form: Croagh Patrick
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.7595
lon: -9.6584
Early archaeological career. Sandars took part in her first archaeological excavation in the 1930s after her sister had introduced her to Kathleen Kenyon. In 1939, Nancy joined Kenyon to work at her excavation of an Iron Age hill fort at The Wrekin, Shropshire. She had also been planning to join an excavation in Normandy run by Mortimer Wheeler, but was stopped by the outbreak of World War II.

Geographic entities mentioned:
surface_form: The Wrekin
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.66916666666667
lon: -2.551388888888889
Smith Volcano. Smith Volcano, also known as Mount Babuyan, is a cinder cone on Babuyan Island, the northernmost of the Babuyan group of islands on Luzon Strait, north of the main island of Luzon in the Philippines. The mountain is one of the active volcanoes in the Philippines, which last erupted in 1924.

Geographic entities mentioned:
surface_form: mount babuyan
instance_of: Mountain
countries: Philippines
coordinates: lat: 19.536622222222
lon: 121.91284444444
surface_form: smith
instance_of: Mountain
countries: Philippines
coordinates: lat: 19.536622222222
lon: 121.91284444444
Smith Volcano. Smith Volcano, also known as Mount Babuyan, is a cinder cone on Babuyan Island, the northernmost of the Babuyan group of islands on Luzon Strait, north of the main island of Luzon in the Philippines. The mountain is one of the active volcanoes in the Philippines, which last erupted in 1924.

Geographic entities mentioned:
surface_form: smith
instance_of: Mountain
countries: Philippines
coordinates: lat: 19.536622222222
lon: 121.91284444444
The sparsely-vegetated cinder cone is high with a base diameter of. Layers of basaltic lava flows are evident south of the volcano. Smith Volcano is one of the probably five Pleistocene-to-Holocene volcanic centers on Babuyan Island (also known as Babuyan de Claro Island) with Smith, the youngest volcano on the island. The largest on the island is Babuyan Claro (also known as &quot;Mt.

Geographic entities mentioned:
surface_form: smith
instance_of: Mountain
countries: Philippines
coordinates: lat: 19.536622222222
lon: 121.91284444444
surface_form: smith
instance_of: Mountain
countries: Philippines
coordinates: lat: 19.536622222222
lon: 121.91284444444
The largest on the island is Babuyan Claro (also known as &quot;Mt. Pangasun&quot;), an active stratovolcano with two well-preserved summit craters in diameter, located in the center of the island. Babuyan Claro is about peak-to-peak southeast of Smith Volcano, which is the north-westernmost summit on the triangular-shaped island. Eruptions.

Geographic entities mentioned:
surface_form: smith
instance_of: Mountain
countries: Philippines
coordinates: lat: 19.536622222222
lon: 121.91284444444
Emergency investigation of 1993. A team of volcanologists from the Philippine Institute of Volcanology and Seismology (PHIVOLCS) Quick Response Team conducted an investigation on July 8, 1993 following reports of unusual volcanic activity at Babuyan Island. Results of the survey showed that Smith Volcano was quiet with no volcanic earthquakes recorded during the survey.

Geographic entities mentioned:
surface_form: smith
instance_of: Mountain
countries: Philippines
coordinates: lat: 19.536622222222
lon: 121.91284444444
Smith Volcano is one of the probably five Pleistocene-to-Holocene volcanic centers on Babuyan Island (also known as Babuyan de Claro Island) with Smith, the youngest volcano on the island. The largest on the island is Babuyan Claro (also known as &quot;Mt. Pangasun&quot;), an active stratovolcano with two well-preserved summit craters in diameter, located in the center of the island.

Geographic entities mentioned:
surface_form: babuyan claro
instance_of: Mountain
countries: Philippines
coordinates: lat: 19.523333333333
lon: 121.94
surface_form: babuyan claro
instance_of: Mountain
countries: Philippines
coordinates: lat: 19.523333333333
lon: 121.94
There are three camp sites in the park, one of which can only be reached by canoeing or biking. The park contains seven hiking trails totaling, including one that is long with an elevation gain. On these trails, hikers can reach the top of the Montagne des Érables, the highest summit in the park, at an elevation of.

Geographic entities mentioned:
surface_form: Montagne des Érables
instance_of: Mountain
countries: Canada
coordinates: lat: 47.885
lon: -70.4555