Sarmila/GeoWiki-Features huggingface dataset:
The southeast side of South Dix drains into West Mill Brook, thence into the Schroon River, the Hudson River, and into New York Bay. The west side of South Dix drains into Lillian Brook, thence into the East Inlet of Elk Lake, and into The Branch of the Schroon River. South Dix is within the High Peaks Wilderness Area of Adirondack State Park.

Geographic entities mentioned:
surface_form: south dix
instance_of: Mountain
countries: United States
coordinates: lat: 44.0601
lon: -73.7743
surface_form: south dix
instance_of: Mountain
countries: United States
coordinates: lat: 44.0601
lon: -73.7743
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9742
lon: -121.802
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 44.025277777778
lon: -115.07138888889
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 45.919166666667
lon: -95.521944444444
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 45.867222222222
lon: -95.804722222222
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 44.85
lon: -85.3833
South Dix. South Dix is a mountain located in Essex County, New York. The mountain is part of the Dix Range, named after John A. Dix (1798–1879), New York Secretary of State in 1837, and later Governor. The name is being changed to Carson Peak, after Russell M.L. Carson (1884–1961), author of &quot;Peaks and People of the Adirondacks&quot;.

Geographic entities mentioned:
surface_form: carson peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.7475
lon: -119.12388888889
surface_form: carson peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.8575
lon: -107.40194444444
The southeast side of South Dix drains into West Mill Brook, thence into the Schroon River, the Hudson River, and into New York Bay. The west side of South Dix drains into Lillian Brook, thence into the East Inlet of Elk Lake, and into The Branch of the Schroon River. South Dix is within the High Peaks Wilderness Area of Adirondack State Park.

Geographic entities mentioned:
surface_form: high peaks
instance_of: Mountain
countries: United States
coordinates: lat: 45
lon: -70.4
Howell Park (Seattle). Howell Park (also known as Howell Beach Park and Howell Street Park) is a public park in Seattle's Madrona neighborhood, in the U.S. state of Washington. The small beachfront park abuts Lake Washington. It is used for nude recreation and has &quot;historically been more for the boys&quot; (referring to gay men), according to &quot;The Stranger&quot;.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
He joined the American mountaineers that year for one year. The following year, he served as a guide for a wagon train of pioneers to the Willamette Valley from Fort Laramie, and in 1845 led the ill-fated group that followed him from the Oregon Trail on the Meek Cutoff. That party split at Fort Hall from the main party that included Joel Palmer and Sam Barlow.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
The annal-entries noting this man are the last sources to specifically note Clann Ruaidhrí gallowglasses in Ireland. Nevertheless, there is reason to suspect that a certain Eóghan—granted the thanage of Glen Tilt by Robert Stewart at some point before 1346—was an Irish-based brother of Raghnall and Áine, brought back to Scotland to serve the military forces of the expanding Steward.

Geographic entities mentioned:
surface_form: Glen Tilt
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.833
lon: -3.776
After the assassination of the Tsar, Alexander II, Jews were evicted from the Russian capital to the Pale of Settlement. Zakhar Shumyatsky pleaded to be allowed to continue living in a city, where he could continue working, and was deported Verkhneudinsk (now Ulan-Ude) in the vicinity of Lake Baikal in Russian Siberia, where Boris Zakharovich was born. The family was registered there as peasants.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
They were led by Forefather Čech and his brother, Lech. After a long time (perhaps years) of traveling, they arrived to busky land. Forefather Čech climbed Říp Mountain and looked around the land. Then he allegedly said: &quot;Oh, comrades, you've endured hardships along with me, when we wandered in impassable woods; finally we arrived at our homeland.

Geographic entities mentioned:
surface_form: Říp
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.38653
lon: 14.2896344
Crepinella acaropunctata. &quot;Crepinella acaropunctata&quot; is a flowering plant in the family Araliaceae. It is endemic to the tepuis Cerro Duida and Cerro Marahuaca in Duida–Marahuaca National Park of Amazonas state of southern Venezuela. It grows in montane forest from 1,600 to 2,700 meters elevation.

Geographic entities mentioned:
surface_form: Cerro Duida
instance_of: Mountain
countries: Venezuela
coordinates: lat: 3.51333333
lon: -65.62611111
Champlain Valley. The Champlain Valley is a region of the United States around Lake Champlain in Vermont and New York extending north slightly into Quebec, Canada. It is part of the St. Lawrence River drainage basin, drained northward by the Richelieu River into the St. Lawrence at Sorel-Tracy, Quebec (northeast of Montreal).

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
surface_form: champlain valley
instance_of: Valley
countries: United States
coordinates: lat: 44.45868
lon: -73.42617
Geology and physiography. The Champlain Valley is among the northernmost valleys considered part of the Great Appalachian Valley reaching from Canada to Alabama. The Champlain Valley is a physiographic section of the larger Saint Lawrence Valley province, which in turn is part of the larger Appalachian physiographic division.

Geographic entities mentioned:
surface_form: Great Appalachian Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: champlain valley
instance_of: Valley
countries: United States
coordinates: lat: 44.45868
lon: -73.42617
Champlain Valley. The Champlain Valley is a region of the United States around Lake Champlain in Vermont and New York extending north slightly into Quebec, Canada. It is part of the St. Lawrence River drainage basin, drained northward by the Richelieu River into the St. Lawrence at Sorel-Tracy, Quebec (northeast of Montreal).

Geographic entities mentioned:
surface_form: champlain valley
instance_of: Valley
countries: United States
coordinates: lat: 44.45868
lon: -73.42617
Lawrence River drainage basin, drained northward by the Richelieu River into the St. Lawrence at Sorel-Tracy, Quebec (northeast of Montreal). The Richelieu valley is not generally referred to as part of the Champlain Valley. The Champlain Lake Valley is the most heavily populated region in Vermont, broadly stretching eastward from the lake's shore to the base of the Green Mountains.

Geographic entities mentioned:
surface_form: champlain valley
instance_of: Valley
countries: United States
coordinates: lat: 44.45868
lon: -73.42617
The state's largest city, Burlington, is located on the lake, and the city's associated suburban communities encompass part of the central section of the valley. Beyond urbanized Chittenden County, however, the valley's landscape is primarily open pasture and row crops, making the Champlain Valley the most productive agricultural region of Vermont.

Geographic entities mentioned:
surface_form: champlain valley
instance_of: Valley
countries: United States
coordinates: lat: 44.45868
lon: -73.42617
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Beyond urbanized Chittenden County, however, the valley's landscape is primarily open pasture and row crops, making the Champlain Valley the most productive agricultural region of Vermont. The New York portion of the Champlain Valley includes the eastern portions of Clinton County and Essex County.

Geographic entities mentioned:
surface_form: champlain valley
instance_of: Valley
countries: United States
coordinates: lat: 44.45868
lon: -73.42617
The city of Plattsburgh is to the north, and the historic town of Ticonderoga is in the southern part of the region. The northern part of Lake George is located at, and near Ticonderoga, and therefore is a part of the Champlain Valley. Geology and physiography. The Champlain Valley is among the northernmost valleys considered part of the Great Appalachian Valley reaching from Canada to Alabama.

Geographic entities mentioned:
surface_form: champlain valley
instance_of: Valley
countries: United States
coordinates: lat: 44.45868
lon: -73.42617
surface_form: lake george
instance_of: Lake
countries: United States
coordinates: lat: 43.622222222222
lon: -73.546666666667
surface_form: lake george
instance_of: Lake
countries: United States
coordinates: lat: 46.88111111
lon: -94.02694444
surface_form: lake george
instance_of: Lake
countries: United States
coordinates: lat: 47.193333333333
lon: -94.975277777778
surface_form: lake george
instance_of: Lake
countries: United States
coordinates: lat: 41.669166666667
lon: -87.502777777778
surface_form: lake george
instance_of: Lake
countries: United States
coordinates: lat: 29.286666666667
lon: -81.598055555556
surface_form: lake george
instance_of: Lake
countries: United States
coordinates: lat: 45.3569
lon: -93.3361
surface_form: lake george
instance_of: Lake
countries: United States
coordinates: lat: 41.5248956
lon: -87.2758367
Geology and physiography. The Champlain Valley is among the northernmost valleys considered part of the Great Appalachian Valley reaching from Canada to Alabama. The Champlain Valley is a physiographic section of the larger Saint Lawrence Valley province, which in turn is part of the larger Appalachian physiographic division.

Geographic entities mentioned:
surface_form: champlain valley
instance_of: Valley
countries: United States
coordinates: lat: 44.45868
lon: -73.42617
The Champlain Valley is a physiographic section of the larger Saint Lawrence Valley province, which in turn is part of the larger Appalachian physiographic division. In Vermont, the Champlain Valley is equivalent to the Vermont Lowlands physiographic region, and extends southward into the Valley of Vermont.

Geographic entities mentioned:
surface_form: champlain valley
instance_of: Valley
countries: United States
coordinates: lat: 44.45868
lon: -73.42617
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The Vermont Lowlands are primarily underlain by sedimentary rocks, especially limestone and shale, though metamorphic rocks such as marble and slate are also present. Lake Champlain is situated in the Champlain Valley between the Green Mountains of Vermont and the Adirondack Mountains of New York, drained northward by the Richelieu River into the St.

Geographic entities mentioned:
surface_form: champlain valley
instance_of: Valley
countries: United States
coordinates: lat: 44.45868
lon: -73.42617
Lawrence River at Sorel-Tracy, Quebec (northeast of Montreal). Major tributaries of Lake Champlain include Otter Creek and the Winooski, Missisquoi, and Lamoille rivers in Vermont, and the Ausable, Chazy, Boquet, and Saranac rivers in New York. Lake Champlain also receives water from Lake George via the La Chute River

Geographic entities mentioned:
surface_form: lake george
instance_of: Lake
countries: United States
coordinates: lat: 43.622222222222
lon: -73.546666666667
surface_form: lake george
instance_of: Lake
countries: United States
coordinates: lat: 46.88111111
lon: -94.02694444
surface_form: lake george
instance_of: Lake
countries: United States
coordinates: lat: 47.193333333333
lon: -94.975277777778
surface_form: lake george
instance_of: Lake
countries: United States
coordinates: lat: 41.669166666667
lon: -87.502777777778
surface_form: lake george
instance_of: Lake
countries: United States
coordinates: lat: 29.286666666667
lon: -81.598055555556
surface_form: lake george
instance_of: Lake
countries: United States
coordinates: lat: 45.3569
lon: -93.3361
surface_form: lake george
instance_of: Lake
countries: United States
coordinates: lat: 41.5248956
lon: -87.2758367
The Champlain Lake Valley is the most heavily populated region in Vermont, broadly stretching eastward from the lake's shore to the base of the Green Mountains. The state's largest city, Burlington, is located on the lake, and the city's associated suburban communities encompass part of the central section of the valley.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The New York portion of the Champlain Valley includes the eastern portions of Clinton County and Essex County. Most of this area is part of the Adirondack Park, offering tremendous views of the Adirondack High Peaks region and many recreational opportunities in the park and along the relatively undeveloped coast line of Lake Champlain.

Geographic entities mentioned:
surface_form: high peaks
instance_of: Mountain
countries: United States
coordinates: lat: 45
lon: -70.4
Lawrence River drainage basin, drained northward by the Richelieu River into the St. Lawrence at Sorel-Tracy, Quebec (northeast of Montreal). The Richelieu valley is not generally referred to as part of the Champlain Valley. The Champlain Lake Valley is the most heavily populated region in Vermont, broadly stretching eastward from the lake's shore to the base of the Green Mountains.

Geographic entities mentioned:
surface_form: lake valley
instance_of: Valley
countries: United States
coordinates: lat: 38.3189
lon: -114.607
For her achievements she has been awarded the Arjuna award and the Padma Shri. She has inspired other Indian women, such as Bachendri Pal, the first Indian woman to successfully climb Mount Everest. As a child, Pal began to aspire to national fame after seeing a newspaper photograph of Zutshi with Prime Minister Indira Gandhi. She was coached by Mohammad Ilyas Babar.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
To the east there is the Kenogami threshold which is characterized by having an altitude of. This threshold splits the graben into two physiographic regions; the Lac Saint-Jean region to the west and the Saguenay region to the east. The plateau around the Graben is between in altitude. The Saguenay River as well as the Lac Saint-Jean are both contained within the Saguenay Graben. Local geology.

Geographic entities mentioned:
surface_form: Lac Saint-Jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: saguenay graben
instance_of: Valley
countries: Canada
coordinates: lat: 48.5
lon: -71.3333
Present day geography. The lowlands within the graben have an altitude of between. To the east there is the Kenogami threshold which is characterized by having an altitude of. This threshold splits the graben into two physiographic regions; the Lac Saint-Jean region to the west and the Saguenay region to the east. The plateau around the Graben is between in altitude.

Geographic entities mentioned:
surface_form: lac saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
Saguenay Graben. The Saguenay Graben is a rift valley or graben in the geological Grenville Province of southern Quebec, Canada. It is an elongated flat-bottomed basin long and wide, bounded by normal faults running parallel to its length. Formation of the Saguenay Graben.

Geographic entities mentioned:
surface_form: saguenay graben
instance_of: Valley
countries: Canada
coordinates: lat: 48.5
lon: -71.3333
It is an elongated flat-bottomed basin long and wide, bounded by normal faults running parallel to its length. Formation of the Saguenay Graben. The time of formation of the faults related to the Saguenay Graben is still under debate because it is difficult to accurately measure the age of faulting.

Geographic entities mentioned:
surface_form: saguenay graben
instance_of: Valley
countries: Canada
coordinates: lat: 48.5
lon: -71.3333
Formation of the Saguenay Graben. The time of formation of the faults related to the Saguenay Graben is still under debate because it is difficult to accurately measure the age of faulting. Evidence suggests it was either the opening of the Iapetus Ocean (600–400 Ma), or the opening of the Atlantic Ocean (195–170 Ma) that caused the faulting.

Geographic entities mentioned:
surface_form: saguenay graben
instance_of: Valley
countries: Canada
coordinates: lat: 48.5
lon: -71.3333
During the opening of one of these oceans, fragmentation of the landmass occurred creating two fault planes, one to the north and one to the south. The resulting bedrock between dropped down along the normal faults, creating the Saguenay Graben. The extent of these faults are only known at the surface and therefore their extension and shape at depth is unknown.

Geographic entities mentioned:
surface_form: saguenay graben
instance_of: Valley
countries: Canada
coordinates: lat: 48.5
lon: -71.3333
The resulting bedrock between dropped down along the normal faults, creating the Saguenay Graben. The extent of these faults are only known at the surface and therefore their extension and shape at depth is unknown. The faults associated with the Saguenay Graben have been the source for earthquakes, including the 1988 Saguenay earthquake. Glaciations.

Geographic entities mentioned:
surface_form: saguenay graben
instance_of: Valley
countries: Canada
coordinates: lat: 48.5
lon: -71.3333
The plateau around the Graben is between in altitude. The Saguenay River as well as the Lac Saint-Jean are both contained within the Saguenay Graben. Local geology. The Saguenay Graben is in the Grenville Province (but was created long after the Grenville Orogeny). The Saguenay Graben is characterized primarily by the rock types: gneiss, anorthosite and granite that are Proterozoic in age.

Geographic entities mentioned:
surface_form: saguenay graben
instance_of: Valley
countries: Canada
coordinates: lat: 48.5
lon: -71.3333
Local geology. The Saguenay Graben is in the Grenville Province (but was created long after the Grenville Orogeny). The Saguenay Graben is characterized primarily by the rock types: gneiss, anorthosite and granite that are Proterozoic in age. There are two outliers of limestone and shale of the Paleozoic that are found only in the graben due to its faulting.

Geographic entities mentioned:
surface_form: saguenay graben
instance_of: Valley
countries: Canada
coordinates: lat: 48.5
lon: -71.3333
It is the 34th-highest peak in the world (using a 500-metre prominence cutoff). It is also notable for being well within the interior of the Tibetan Plateau (most peaks of similar height – except notably Shishapangma, the world's 14th-highest peak – lie nearer to or outside the edge of the Plateau) and relatively far away from other peaks with heights greater than 7,500 metres.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
surface_form: Shishapangma
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 28.352222222222
lon: 85.779722222222
It is also notable for being well within the interior of the Tibetan Plateau (most peaks of similar height – except notably Shishapangma, the world's 14th-highest peak – lie nearer to or outside the edge of the Plateau) and relatively far away from other peaks with heights greater than 7,500 metres. It sits roughly across Lake Manasarovar from the sacred peak of Mount Kailash. Names.

Geographic entities mentioned:
surface_form: Lake Manasarovar
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 30.666666666667
lon: 81.5
surface_form: Mount Kailash
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 31.066944444444
lon: 81.312777777778
surface_form: kailash
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 31.066944444444
lon: 81.312777777778
surface_form: manasarovar
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 30.666666666667
lon: 81.5
Names. &quot;Gurla Mandhata&quot; is a romanization of the Hindi name. It supposedly derives from a pass near the mountain and the legendary prehistoric Indian king Mandhata of the Raghuvaṃśa branch of the Solar Dynasty, who supposedly conquered the earth and passed the mountain on his way to the sacred lake Manasarovar beside the axis mundi Mount Kailash.

Geographic entities mentioned:
surface_form: Manasarovar
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 30.666666666667
lon: 81.5
surface_form: Mount Kailash
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 31.066944444444
lon: 81.312777777778
surface_form: mount kailash
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 31.066944444444
lon: 81.312777777778
surface_form: kailash
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 31.066944444444
lon: 81.312777777778
surface_form: lake manasarovar
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 30.666666666667
lon: 81.5
surface_form: manasarovar
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 30.666666666667
lon: 81.5
This was a strong achievement for the time, especially for such a small group; at that time no summit of over 7,000 m had yet been climbed and Longstaff's height represented a world altitude record. In 1935, the Viennese student Herbert Tichy made a trip to the holy mountain Kailash while disguised as an Indian pilgrim. On the way, he attempted Gurla Mandhata with one of his porters, Kitar.

Geographic entities mentioned:
surface_form: Kailash
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 31.066944444444
lon: 81.312777777778
Gurla Mandhata. Gurla Mandhata, also Naimona'nyi or Namu Nani, is the highest peak of the Nalakankar Himal, a small subrange of the Himalaya. It lies in Burang County of the Ngari Prefecture in the Tibet Autonomous Region of China, near the northwest corner of Nepal. It is the 34th-highest peak in the world (using a 500-metre prominence cutoff).

Geographic entities mentioned:
surface_form: gurla mandhata
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 30.438333333333
lon: 81.299166666667
Names. &quot;Gurla Mandhata&quot; is a romanization of the Hindi name. It supposedly derives from a pass near the mountain and the legendary prehistoric Indian king Mandhata of the Raghuvaṃśa branch of the Solar Dynasty, who supposedly conquered the earth and passed the mountain on his way to the sacred lake Manasarovar beside the axis mundi Mount Kailash.

Geographic entities mentioned:
surface_form: gurla mandhata
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 30.438333333333
lon: 81.299166666667
St. Peter's Church (Kajmakčalan). St. Peter and Paul (), known simply as St. Peter or by the name of the peak St. Elijah (), is an Eastern Orthodox church on Kajmakčalan peak of the Voras Mountains, near in North Macedonia, on the border with Greece. It is part of the of the Macedonian Orthodox Church. Background.

Geographic entities mentioned:
surface_form: Kajmakčalan
instance_of: Mountain
countries: Greece
North Macedonia
coordinates: lat: 40.930277777778
lon: 21.786111111111
In 1928, the monument was converted into a church-ossuary dedicated to Saint Peter. The next year, the heart of Archibald Reiss was placed in an urn at the church, at his own request; Reiss was a Swiss journalist in Serbian service who covered the battles on the Macedonian front (Salonika front), which spread across the mountain Kajmakčalan in Маcedonia.

Geographic entities mentioned:
surface_form: Kajmakčalan
instance_of: Mountain
countries: Greece
North Macedonia
coordinates: lat: 40.930277777778
lon: 21.786111111111
Biography. Vo was born in Peoria, Illinois, where she lived until attending college at the University of Illinois Urbana-Champaign. In 2007 she moved to Milwaukee, Wisconsin on the shores of Lake Michigan. She defines her sexuality as queer. Vo's first published short story was &quot;Gift of Flight&quot; in 2007, after which she published a number of short stories in various media.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Table Mountain (Tulare County, California). Table Mountain is located near the northern end of the Great Western Divide, a sub-range of the Sierra Nevada in California. The summit marks a point on the boundary between Sequoia and Kings Canyon national parks and is south of Thunder Mountain and northeast of Midway Mountain.

Geographic entities mentioned:
surface_form: Midway Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6433251
lon: -118.48371
surface_form: thunder mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.1716
lon: -113.614
surface_form: thunder mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6741
lon: -120.091
surface_form: thunder mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.604722222222
lon: -107.56055555556
surface_form: thunder mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.6555606
lon: -121.1316006
surface_form: thunder mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.886111111111
lon: -111.80694444444
surface_form: thunder mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6691
lon: -118.476
Table Mountain (Tulare County, California). Table Mountain is located near the northern end of the Great Western Divide, a sub-range of the Sierra Nevada in California. The summit marks a point on the boundary between Sequoia and Kings Canyon national parks and is south of Thunder Mountain and northeast of Midway Mountain.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.742222222222
lon: -112.46194444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.541388888889
lon: -118.29944444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7467
lon: -110.852
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.6918989
lon: -121.9826782
surface_form: table mountain (tulare county, california)
instance_of: Mountain
countries: United States
coordinates: lat: 36.6604
lon: -118.474
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.983
lon: -120.434
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9587
lon: -74.4048
Table Mountain (Tulare County, California). Table Mountain is located near the northern end of the Great Western Divide, a sub-range of the Sierra Nevada in California. The summit marks a point on the boundary between Sequoia and Kings Canyon national parks and is south of Thunder Mountain and northeast of Midway Mountain.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.742222222222
lon: -112.46194444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.541388888889
lon: -118.29944444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7467
lon: -110.852
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.6918989
lon: -121.9826782
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6604
lon: -118.474
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.983
lon: -120.434
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9587
lon: -74.4048
Hoffmann's map of 1873. In 1881 the mountain was named Mount Hazen in honor of General Hazen, the Chief Signal Officer of the U.S. Army. In 1905, the Board on Geographic Names recognized the name Table Mountain. This name appeared on both the &quot;Tehipite&quot; and the &quot;Mt. Whitney&quot; USGS 30' maps published in 1905 and 1907 respectively.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.742222222222
lon: -112.46194444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.541388888889
lon: -118.29944444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7467
lon: -110.852
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.6918989
lon: -121.9826782
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6604
lon: -118.474
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.983
lon: -120.434
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9587
lon: -74.4048
In 1881 the mountain was named Mount Hazen in honor of General Hazen, the Chief Signal Officer of the U.S. Army. In 1905, the Board on Geographic Names recognized the name Table Mountain. This name appeared on both the &quot;Tehipite&quot; and the &quot;Mt. Whitney&quot; USGS 30' maps published in 1905 and 1907 respectively. It is the tallest of the 21 peaks named Table Mountain in California.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.742222222222
lon: -112.46194444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.541388888889
lon: -118.29944444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7467
lon: -110.852
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.6918989
lon: -121.9826782
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6604
lon: -118.474
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.983
lon: -120.434
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9587
lon: -74.4048
In 1881 the mountain was named Mount Hazen in honor of General Hazen, the Chief Signal Officer of the U.S. Army. In 1905, the Board on Geographic Names recognized the name Table Mountain. This name appeared on both the &quot;Tehipite&quot; and the &quot;Mt. Whitney&quot; USGS 30' maps published in 1905 and 1907 respectively. It is the tallest of the 21 peaks named Table Mountain in California.

Geographic entities mentioned:
surface_form: mt. whitney
instance_of: Mountain
countries: United States
coordinates: lat: 36.57861111111111
lon: -118.29194444444444
surface_form: whitney
instance_of: Mountain
countries: United States
coordinates: lat: 36.57861111111111
lon: -118.29194444444444
The summit marks a point on the boundary between Sequoia and Kings Canyon national parks and is south of Thunder Mountain and northeast of Midway Mountain. Clarence King of the Whitney Survey mentioned in his notes that &quot;At one place the ridge [Great Western Divide] forms a level table.&quot; The name Table appeared on Charles F. Hoffmann's map of 1873.

Geographic entities mentioned:
surface_form: whitney
instance_of: Mountain
countries: United States
coordinates: lat: 36.57861111111111
lon: -118.29194444444444
Features of the lake. Koskikeskinen is 650 meters long, 500 meters wide and covers an area of 14.0 hectares. It is located in the upper reaches of Jämsänjoki below the lake Kankarisvesi. The short river bed of the Jämsänjoki starts from the Kankarisvesi, which descends through two parallel rapids, Naiskoski and Rekolankoski, into the Koskikeskinen.

Geographic entities mentioned:
surface_form: Kankarisvesi
instance_of: Lake
countries: Finland
coordinates: lat: 61.9667
lon: 25.1333
It is located in the upper reaches of Jämsänjoki below the lake Kankarisvesi. The short river bed of the Jämsänjoki starts from the Kankarisvesi, which descends through two parallel rapids, Naiskoski and Rekolankoski, into the Koskikeskinen. The Rekolankoski power plant operates on the western route, while the Naiskoski is used as a spillway.

Geographic entities mentioned:
surface_form: kankarisvesi
instance_of: Lake
countries: Finland
coordinates: lat: 61.9667
lon: 25.1333
surface_form: koskikeskinen
instance_of: Lake
countries: Finland
coordinates: lat: 61.9204085
lon: 25.1612886
The Rekolankoski power plant operates on the western route, while the Naiskoski is used as a spillway. The Jämsänjoki continues south from Koskikeskinen for about 14 kilometers, discharging into the Päijänne. The surface of Koskikeskinen is 5.6 meters below Kankarisvesi and around 13 meters below Jämsänjoki. The river flows through a pipe under the Jämsänkoski paper mill.

Geographic entities mentioned:
surface_form: kankarisvesi
instance_of: Lake
countries: Finland
coordinates: lat: 61.9667
lon: 25.1333
surface_form: koskikeskinen
instance_of: Lake
countries: Finland
coordinates: lat: 61.9204085
lon: 25.1612886
Koskikeskinen. Koskikeskinen is a lake located in central Jämsänkoski, Central Finland. Koskikeskinen is a backwater between two rapids that belong to the Jämsänjoki route. The lake is surrounded by the urban area of Jämsänkoski. Koskikeskinen is 96 meters above sea level. The area is 14 hectares and the coast is 2.41 kilometers long. The lake is part of the Kymi River's drainage basin.

Geographic entities mentioned:
surface_form: koskikeskinen
instance_of: Lake
countries: Finland
coordinates: lat: 61.9204085
lon: 25.1612886
Koskikeskinen is a lake located in central Jämsänkoski, Central Finland. Koskikeskinen is a backwater between two rapids that belong to the Jämsänjoki route. The lake is surrounded by the urban area of Jämsänkoski. Koskikeskinen is 96 meters above sea level. The area is 14 hectares and the coast is 2.41 kilometers long. The lake is part of the Kymi River's drainage basin. Features of the lake.

Geographic entities mentioned:
surface_form: koskikeskinen
instance_of: Lake
countries: Finland
coordinates: lat: 61.9204085
lon: 25.1612886
Koskikeskinen is 96 meters above sea level. The area is 14 hectares and the coast is 2.41 kilometers long. The lake is part of the Kymi River's drainage basin. Features of the lake. Koskikeskinen is 650 meters long, 500 meters wide and covers an area of 14.0 hectares. It is located in the upper reaches of Jämsänjoki below the lake Kankarisvesi.

Geographic entities mentioned:
surface_form: koskikeskinen
instance_of: Lake
countries: Finland
coordinates: lat: 61.9204085
lon: 25.1612886
The Rekolankoski power plant operates on the western route, while the Naiskoski is used as a spillway. The Jämsänjoki continues south from Koskikeskinen for about 14 kilometers, discharging into the Päijänne. The surface of Koskikeskinen is 5.6 meters below Kankarisvesi and around 13 meters below Jämsänjoki. The river flows through a pipe under the Jämsänkoski paper mill.

Geographic entities mentioned:
surface_form: koskikeskinen
instance_of: Lake
countries: Finland
coordinates: lat: 61.9204085
lon: 25.1612886
It was once isolated by the factory line of the industrial area. Today, the former railway is a light traffic route and a wooden footbridge crosses the mouth of the bay. The southern and southwestern shores of Koskikeskinen are dominated by the industrial environment of Jämsänkoski. Right on the southern shore of Koskikeskinen is the factory company's old clubhouse and a red brick paper warehouse.

Geographic entities mentioned:
surface_form: koskikeskinen
instance_of: Lake
countries: Finland
coordinates: lat: 61.9204085
lon: 25.1612886
Today, the former railway is a light traffic route and a wooden footbridge crosses the mouth of the bay. The southern and southwestern shores of Koskikeskinen are dominated by the industrial environment of Jämsänkoski. Right on the southern shore of Koskikeskinen is the factory company's old clubhouse and a red brick paper warehouse. West bank.

Geographic entities mentioned:
surface_form: koskikeskinen
instance_of: Lake
countries: Finland
coordinates: lat: 61.9204085
lon: 25.1612886
Right on the southern shore of Koskikeskinen is the factory company's old clubhouse and a red brick paper warehouse. West bank. On the west bank of Koskikeskinen is Pässinmäki, where art exhibitions are organized. The historic industrial environment of Naiskoski and Rekolankoski, where power plants and old factories have been converted into restaurants, is located on the lake's northern shore.

Geographic entities mentioned:
surface_form: koskikeskinen
instance_of: Lake
countries: Finland
coordinates: lat: 61.9204085
lon: 25.1612886
In 1711 the Portuguese priest Francis Cardoso, and the Augustinian Guillaume Bonjour, the only non-Jesuit, joined the geographers. Régis and Cardoso drew the map of Shandong; Jartoux, Fridelli and Bonjour traversed Mongolia as far as Lake Baikal in the north and the Zunghar Khanate to the west.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Williams Bay, Wisconsin. Williams Bay is a village in Walworth County, Wisconsin, United States. It is one of three municipalities on Geneva Lake. The population was 2,953 at the 2020 census. On June 22, 2024 the town was hit by an EF-1 tornado, there were no injuries or fatalities, but the storm caused some areas of considerable damage. History.

Geographic entities mentioned:
surface_form: Geneva Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.59
lon: -88.435
Geography. Kyaukpyu is a district in the Arakan division of Lower Burma, on the eastern coast of the Bay of Bengal. It consists of, first, a strip of mainland along the Bay of Bengal, extending from the An pass, across the main range, to the Ma-ī River, and, secondly, the large islands of Ramree and Cheduba, with many others to the south, lying off the coast of Sandoway.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Pukaskwa River. The Pukaskwa River is a river in Thunder Bay District and Algoma District in Northern Ontario, Canada. It is in the Great Lakes Basin and is a tributary of Lake Superior, which it enters at the south end of Pukaskwa National Park. It is a remote, pristine, free-flowing, medium-sized Shield river, with lots of whitewater, best travelled in spring.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
They were armed with one 13 mm heavy machine gun or one 20 mm anti-aircraft gun, 6 depth charges and two 450 mm torpedoes. Another flotilla of four MAS, the XII Squadriglia MAS, was deployed to Lake Ladoga in April 1942 to support the siege of Leningrad. They claim the sinking of a Soviet gunboat of the Bira class, a 1,300-ton cargo ship and several barges.

Geographic entities mentioned:
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
Campbell Ridges. The Campbell Ridges () are an irregular complex of ridges between Creswick Gap and Mount Courtauld in Palmer Land. Two north–south ridges are linked by an east–west ridge, on which stand the highest peaks. They were named by the Advisory Committee on Antarctic Names for Lieutenant Commander Bruce H. Campbell, U.S.

Geographic entities mentioned:
surface_form: Mount Courtauld
instance_of: Mountain
coordinates: lat: -70.35
lon: -67.4667
Highest point claims. Mount Canobolas is not, as is sometimes claimed in tourism brochures, the highest point between Australia's Great Dividing Range and Africa, as Mount Zeil in Australia's Northern Territory and Ngarutjaranya in South Australia are further west and higher, and a number of peaks elsewhere on the Great Dividing Range and peaks on Madagascar and Réunion are higher.

Geographic entities mentioned:
surface_form: Mount Zeil
instance_of: Mountain
countries: Australia
coordinates: lat: -23.401666666666667
lon: 132.39583333333334
surface_form: Ngarutjaranya
instance_of: Mountain
countries: Australia
coordinates: lat: -26.316666666667
lon: 131.73333333333
surface_form: mount zeil
instance_of: Mountain
countries: Australia
coordinates: lat: -23.401666666666667
lon: 132.39583333333334
surface_form: ngarutjaranya
instance_of: Mountain
countries: Australia
coordinates: lat: -26.316666666667
lon: 131.73333333333
Mount Canobolas. Mount Canobolas, a mountain on a spur of the Great Dividing Range, is located in the Central Tablelands region of New South Wales, Australia. With an elevation of above sea level, Mount Canobolas, an extinct volcano, is the highest mountain in the region. Situated southwest of the city of Orange, it is about west of Sydney.

Geographic entities mentioned:
surface_form: mount canobolas
instance_of: Mountain
countries: Australia
coordinates: lat: -33.3442
lon: 148.982
Etymology. The name comes from two words in the Wiradjuri language (the local Aboriginal language), &quot;gaahna&quot; and &quot;bula&quot;. This means &quot;two shoulders&quot; which refers to the summits of Mount Canobolas itself and the subsidiary peak Young Man Canobolas. Description.

Geographic entities mentioned:
surface_form: mount canobolas
instance_of: Mountain
countries: Australia
coordinates: lat: -33.3442
lon: 148.982
surface_form: mount canobolas
instance_of: Mountain
countries: Australia
coordinates: lat: -33.3442
lon: 148.982
Later eruptions became more violent, and producing increasingly viscous lavas with less extensive coverage. The contemporary landscape of Mount Canobolas exhibits erosional features dominated by several remnant peaks. Additional volcanic features are present within the zone of volcanic influence, including vents, dykes, peaks, domes and plugs.

Geographic entities mentioned:
surface_form: mount canobolas
instance_of: Mountain
countries: Australia
coordinates: lat: -33.3442
lon: 148.982
The summit can be seen from up to 100 km away. The mountain is now part of the Mount Canobolas Conservation Area, managed by the NSW National Parks & Wildlife Service, which offers various walks: to Bald Hill; to Young Man Canobolas; Federal Falls to Mount Towac, and other locations. The volcanic peaks give wide views and there are some attractive waterfalls.

Geographic entities mentioned:
surface_form: mount canobolas
instance_of: Mountain
countries: Australia
coordinates: lat: -33.3442
lon: 148.982
surface_form: bald hill
instance_of: Mountain
countries: Australia
coordinates: lat: -34.2236
lon: 150.993
Each year the Orange community runs the Great Volcanic Mountain Challenge, an walk and fun run from the Pinnacle to the Summit of Mount Canobolas by the volcanic plugs of Mount Towac and Young Man Canobolas. The inaugural event was held in 2006. Fires on the mountain. A major bushfire in 1967 affected 415 ha in the northern section of the Mount Canobolas Conservation Area.

Geographic entities mentioned:
surface_form: mount canobolas
instance_of: Mountain
countries: Australia
coordinates: lat: -33.3442
lon: 148.982
The inaugural event was held in 2006. Fires on the mountain. A major bushfire in 1967 affected 415 ha in the northern section of the Mount Canobolas Conservation Area. Another bushfire in 1982 affected 414 ha in the western part of the conservation area and a further bushfire occurred in the southern part of the conservation area in 1985.

Geographic entities mentioned:
surface_form: mount canobolas
instance_of: Mountain
countries: Australia
coordinates: lat: -33.3442
lon: 148.982