Sarmila/GeoWiki-Features huggingface dataset:
The peak height of Catawissa Mountain is above sea level. However, numerous places on the mountain rise to over above sea level. The mountain is the fifth-highest mountain in Columbia County, behind Red Rock Mountain, Central Mountain, Chimneystack Rock, and Buck Mountain. The community of Catawissa is close to Catawissa Mountain.

Geographic entities mentioned:
surface_form: Red Rock Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.308630555556
lon: -76.309352777778
surface_form: Central Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.3
lon: -76.3463
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6081079
lon: -90.3926199
surface_form: buck mountain
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countries: United States
coordinates: lat: 37.66388889
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surface_form: buck mountain
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countries: United States
coordinates: lat: 43.889722222222
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surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.461944444444
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surface_form: buck mountain
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countries: United States
coordinates: lat: 43.6894
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surface_form: buck mountain
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countries: United States
coordinates: lat: 40.9509
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surface_form: rock mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.799444444444
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surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6047712
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surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.052777777778
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surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.193333333333
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surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.093611111111116
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Catawissa Mountain. Catawissa Mountain is a mountain in Columbia County, Pennsylvania, in the United States. Its peak height is above sea level, making it the fifth-highest mountain in Columbia County. Streams that flow near the mountain include Roaring Creek, Catawissa Creek, and some of their tributaries. The mountain is near Nescopeck Mountain and Little Mountain.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
From here, it runs northwest through Beaver Township and Roaring Creek Township to the community of Catawissa. A spur of the mountain can be said to cross the Susquehanna River and turn west into Montour County, where it ceases to be a mountain. The peak height of Catawissa Mountain is above sea level. However, numerous places on the mountain rise to over above sea level.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
Its peak height is above sea level, making it the fifth-highest mountain in Columbia County. Streams that flow near the mountain include Roaring Creek, Catawissa Creek, and some of their tributaries. The mountain is near Nescopeck Mountain and Little Mountain. Sandstones and rock formations such as the Pocono Formation occur on Catawissa Mountain.

Geographic entities mentioned:
surface_form: little mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.186944444444
lon: -81.413611111111
surface_form: little mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.57
lon: -85.2808
Sandstone of the Pocono Formation occurs on the summit of the mountain. Catawissa Mountain is part of a chain of mountains running from beyond Dauphin to Carbondale. The mountain is located near both Nescopeck Mountain and Little Mountain. The meeting point of Catawissa Mountain and Nescopeck Mountain is on the edge of a canoe valley. Hydrology.

Geographic entities mentioned:
surface_form: little mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.186944444444
lon: -81.413611111111
surface_form: little mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.57
lon: -85.2808
Historically, a road known as the climbed up Catawissa Mountain. In the past, a road led from the valley of the Schuylkill River to Catawissa via the southern part of the mountain. The also passed from Catawissa to Philadelphia via the mountain. Colliers in the 1800s used the forests of Catawissa Mountain to supply charcoal for local iron furnaces.

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
Catawissa Mountain. Catawissa Mountain is a mountain in Columbia County, Pennsylvania, in the United States. Its peak height is above sea level, making it the fifth-highest mountain in Columbia County. Streams that flow near the mountain include Roaring Creek, Catawissa Creek, and some of their tributaries. The mountain is near Nescopeck Mountain and Little Mountain.

Geographic entities mentioned:
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
Streams that flow near the mountain include Roaring Creek, Catawissa Creek, and some of their tributaries. The mountain is near Nescopeck Mountain and Little Mountain. Sandstones and rock formations such as the Pocono Formation occur on Catawissa Mountain. The community of Catawissa is near Catawissa Mountain. There have also been several roads on or near the mountain in the past.

Geographic entities mentioned:
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
The community of Catawissa is near Catawissa Mountain. There have also been several roads on or near the mountain in the past. In more recent times, Pennsylvania State Game Lands Number 58 was established in the area and includes some parts of Catawissa Mountain. There are vernal pools on the mountain, which are used as breeding grounds for amphibians.

Geographic entities mentioned:
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
There are vernal pools on the mountain, which are used as breeding grounds for amphibians. The mountain is part of a much larger tract of forest. Catawissa Mountain is located in southeastern Catawissa Township, southwestern Main Township, eastern Roaring Creek Township, among other places. Geography.

Geographic entities mentioned:
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
Catawissa Mountain is located in southeastern Catawissa Township, southwestern Main Township, eastern Roaring Creek Township, among other places. Geography. Catawissa Mountain's southeastern edge is at the border between Luzerne County and Columbia County. From here, it runs northwest through Beaver Township and Roaring Creek Township to the community of Catawissa.

Geographic entities mentioned:
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
From here, it runs northwest through Beaver Township and Roaring Creek Township to the community of Catawissa. A spur of the mountain can be said to cross the Susquehanna River and turn west into Montour County, where it ceases to be a mountain. The peak height of Catawissa Mountain is above sea level. However, numerous places on the mountain rise to over above sea level.

Geographic entities mentioned:
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
However, numerous places on the mountain rise to over above sea level. The mountain is the fifth-highest mountain in Columbia County, behind Red Rock Mountain, Central Mountain, Chimneystack Rock, and Buck Mountain. The community of Catawissa is close to Catawissa Mountain. Main Township and Locust Township are also located near the mountain. Geology.

Geographic entities mentioned:
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
Main Township and Locust Township are also located near the mountain. Geology. Catawissa Mountain is relatively short and rounded, especially compared to nearby mountains such as Huntington Mountain, which are straight and narrow ridges. Catawissa Mountain has some rocky outcroppings. There are two zigzagging outcroppings of the Pocono Formation on Catawissa Mountain.

Geographic entities mentioned:
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
Geology. Catawissa Mountain is relatively short and rounded, especially compared to nearby mountains such as Huntington Mountain, which are straight and narrow ridges. Catawissa Mountain has some rocky outcroppings. There are two zigzagging outcroppings of the Pocono Formation on Catawissa Mountain. These outcroppings pass through the mountain and south into Schuylkill County.

Geographic entities mentioned:
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
They also have spurs and knobs at each point where they zigzag. The Northumberland Syncline passes through a spur of the mountain. The mountain also has an elbow which is part of a double synclinal that heads eastward to Nescopeck Mountain. A coarse and hard sandstone can be found on Catawissa Mountain. Sandstone of the Pocono Formation occurs on the summit of the mountain.

Geographic entities mentioned:
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
A coarse and hard sandstone can be found on Catawissa Mountain. Sandstone of the Pocono Formation occurs on the summit of the mountain. Catawissa Mountain is part of a chain of mountains running from beyond Dauphin to Carbondale. The mountain is located near both Nescopeck Mountain and Little Mountain. The meeting point of Catawissa Mountain and Nescopeck Mountain is on the edge of a canoe valley.

Geographic entities mentioned:
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
Catawissa Mountain is part of a chain of mountains running from beyond Dauphin to Carbondale. The mountain is located near both Nescopeck Mountain and Little Mountain. The meeting point of Catawissa Mountain and Nescopeck Mountain is on the edge of a canoe valley. Hydrology. Several tributaries of the lower reaches of Catawissa Creek originate on Catawissa Mountain.

Geographic entities mentioned:
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
The meeting point of Catawissa Mountain and Nescopeck Mountain is on the edge of a canoe valley. Hydrology. Several tributaries of the lower reaches of Catawissa Creek originate on Catawissa Mountain. Many of these tributaries are impaired from acid deposition from abandoned mine drainage. Roaring Creek is also close to the western side of the mountain.

Geographic entities mentioned:
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
Many of these tributaries are impaired from acid deposition from abandoned mine drainage. Roaring Creek is also close to the western side of the mountain. Catawissa Creek cuts a gap between Catawissa Mountain and Nescopeck Mountain at the community of Mainville. The creek also flows parallel to Catawissa Mountain downstream of this gap.

Geographic entities mentioned:
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
Roaring Creek is also close to the western side of the mountain. Catawissa Creek cuts a gap between Catawissa Mountain and Nescopeck Mountain at the community of Mainville. The creek also flows parallel to Catawissa Mountain downstream of this gap. There are vernal pools on Catawissa Mountain in Beaver Township and Roaring Creek Township. History and etymology.

Geographic entities mentioned:
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
History and etymology. The word &quot;Catawissa&quot; may come from the Delaware or Shawanese words meaning &quot;pure water.&quot;
There was at least one Native American village in Catawissa, near Catawissa Mountain, and possibly several villages during different time periods. Historically, a road known as the climbed up Catawissa Mountain.

Geographic entities mentioned:
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
In the past, a road led from the valley of the Schuylkill River to Catawissa via the southern part of the mountain. The also passed from Catawissa to Philadelphia via the mountain. Colliers in the 1800s used the forests of Catawissa Mountain to supply charcoal for local iron furnaces. Flat areas signifying former charcoal pits may still be found throughout the mountain. J.H.

Geographic entities mentioned:
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
Flat areas signifying former charcoal pits may still be found throughout the mountain. J.H. Beers stated in his 1915 book &quot;Historical and Biographical Annals of Columbia and Montour Counties, Pennsylvania&quot; that the height of Catawissa Mountain was estimated to be. The same author described the mountain as &quot;majestic&quot; and &quot;towering&quot; in his book.

Geographic entities mentioned:
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
J.H. Beers stated in his 1915 book &quot;Historical and Biographical Annals of Columbia and Montour Counties, Pennsylvania&quot; that the height of Catawissa Mountain was estimated to be. The same author described the mountain as &quot;majestic&quot; and &quot;towering&quot; in his book. Since at least 2001, the Columbia-Montour Amateur Radio Club has had a receiver on Catawissa Mountain. Biology.

Geographic entities mentioned:
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
Amphibians use the vernal pools on Catawissa Mountain as breeding grounds, including American toads, wood frogs, and spotted salamanders. In Pennsylvania State Game Lands Number 58, the forests on Catawissa Mountain are hardwood/heath forests. Trees in these forests include red maple, chestnut oak, scarlet oak, mountain laurel, black huckleberry, and lowbush blueberry.

Geographic entities mentioned:
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
These include cranberry, cinnamon fern, royal fern, tussock sedge, pitch pine, and numerous others. Recreation. The Pennsylvania State Game Lands Number 58 are located on Catawissa Mountain. Portions of Catawissa Mountain lying in Pennsylvania State Game Lands Number 58 are heavily hunted for white-tailed deer. Large tracts of Catawissa Mountain are privately owned.

Geographic entities mentioned:
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
These include cranberry, cinnamon fern, royal fern, tussock sedge, pitch pine, and numerous others. Recreation. The Pennsylvania State Game Lands Number 58 are located on Catawissa Mountain. Portions of Catawissa Mountain lying in Pennsylvania State Game Lands Number 58 are heavily hunted for white-tailed deer. Large tracts of Catawissa Mountain are privately owned.

Geographic entities mentioned:
surface_form: catawissa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
Saugeen and Cape Croker Fishing Islands 1. Saugeen and Cape Croker Fishing Islands 1 is a First Nations reserve consisting of 89 islands in Lake Huron off the western coast of the Bruce Peninsula in Ontario. They extend north of Chief's Point 28 for up to Pike Bay. These islands are shared between the Chippewas of Nawash Unceded First Nation and Saugeen First Nation. History.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
A number of hiking trails are also in its vicinity. Geography. The main outflow of Lake Rose is an unnamed tributary of Kitchen Creek. One of its main inflows is the spillway from Lake Jean. The lake has an elevation of above sea level. Lake Rose is entirely within the United States Geological Survey quadrangle of Red Rock. It has an area of.

Geographic entities mentioned:
surface_form: Lake Jean
instance_of: Lake
countries: United States
coordinates: lat: 41.34111111
lon: -76.29083333
Lake Rose (Pennsylvania). Lake Rose is a dry lake in Luzerne County, Pennsylvania, in the United States. It has a surface area of approximately, and is situated in Fairmount Township. Lake Rose is mostly dry and closely resembles a swamp. Its main inflow is the spillway from Lake Jean. Lake Rose was originally constructed by a squatter named Jesse Dodson.

Geographic entities mentioned:
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6282988
lon: -97.0561783
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 38.3360373
lon: -117.7898285
surface_form: lake rose
instance_of: Lake
countries: United States
coordinates: lat: 41.329166666667
lon: -76.295
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 45.0425
lon: -97.31972222
Lake Rose (Pennsylvania). Lake Rose is a dry lake in Luzerne County, Pennsylvania, in the United States. It has a surface area of approximately, and is situated in Fairmount Township. Lake Rose is mostly dry and closely resembles a swamp. Its main inflow is the spillway from Lake Jean. Lake Rose was originally constructed by a squatter named Jesse Dodson.

Geographic entities mentioned:
surface_form: lake rose (pennsylvania)
instance_of: Lake
countries: United States
coordinates: lat: 41.329166666667
lon: -76.295
Lake Rose (Pennsylvania). Lake Rose is a dry lake in Luzerne County, Pennsylvania, in the United States. It has a surface area of approximately, and is situated in Fairmount Township. Lake Rose is mostly dry and closely resembles a swamp. Its main inflow is the spillway from Lake Jean. Lake Rose was originally constructed by a squatter named Jesse Dodson.

Geographic entities mentioned:
surface_form: lake rose
instance_of: Lake
countries: United States
coordinates: lat: 41.329166666667
lon: -76.295
It has a surface area of approximately, and is situated in Fairmount Township. Lake Rose is mostly dry and closely resembles a swamp. Its main inflow is the spillway from Lake Jean. Lake Rose was originally constructed by a squatter named Jesse Dodson. Wildlife, including birds, butterflies, and dragonflies, has been observed near the lake. A number of hiking trails are also in its vicinity.

Geographic entities mentioned:
surface_form: lake rose
instance_of: Lake
countries: United States
coordinates: lat: 41.329166666667
lon: -76.295
Lake Rose was originally constructed by a squatter named Jesse Dodson. Wildlife, including birds, butterflies, and dragonflies, has been observed near the lake. A number of hiking trails are also in its vicinity. Geography. The main outflow of Lake Rose is an unnamed tributary of Kitchen Creek. One of its main inflows is the spillway from Lake Jean. The lake has an elevation of above sea level.

Geographic entities mentioned:
surface_form: lake rose
instance_of: Lake
countries: United States
coordinates: lat: 41.329166666667
lon: -76.295
Geography. The main outflow of Lake Rose is an unnamed tributary of Kitchen Creek. One of its main inflows is the spillway from Lake Jean. The lake has an elevation of above sea level. Lake Rose is entirely within the United States Geological Survey quadrangle of Red Rock. It has an area of. Lake Rose is mostly dry, but there is a small pool of water in it.

Geographic entities mentioned:
surface_form: lake rose
instance_of: Lake
countries: United States
coordinates: lat: 41.329166666667
lon: -76.295
The lake has an elevation of above sea level. Lake Rose is entirely within the United States Geological Survey quadrangle of Red Rock. It has an area of. Lake Rose is mostly dry, but there is a small pool of water in it. It more closely resembles a swamp than it does a lake. In 1990, &quot;Northeastern Geology&quot; stated that Lake Rose &quot;appears on the map but not in reality&quot;.

Geographic entities mentioned:
surface_form: lake rose
instance_of: Lake
countries: United States
coordinates: lat: 41.329166666667
lon: -76.295
It has an area of. Lake Rose is mostly dry, but there is a small pool of water in it. It more closely resembles a swamp than it does a lake. In 1990, &quot;Northeastern Geology&quot; stated that Lake Rose &quot;appears on the map but not in reality&quot;. Lake Rose was undeveloped in the early 1960s. History and recreation.

Geographic entities mentioned:
surface_form: lake rose
instance_of: Lake
countries: United States
coordinates: lat: 41.329166666667
lon: -76.295
surface_form: lake rose
instance_of: Lake
countries: United States
coordinates: lat: 41.329166666667
lon: -76.295
Lake Rose was built by Jesse Dodson, a squatter who made bedsteads out of cherry trees, and built the lake as a log splash pond. In 1905, Colonel R. Bruce Ricketts reinforced the Lake Rose dam. However, due to the dam's poor construction, the lake could not be used for hydroelectric power. In the middle of the 20th century, the state of Pennsylvania condemned the dam and drained the lake.

Geographic entities mentioned:
surface_form: lake rose
instance_of: Lake
countries: United States
coordinates: lat: 41.329166666667
lon: -76.295
However, due to the dam's poor construction, the lake could not be used for hydroelectric power. In the middle of the 20th century, the state of Pennsylvania condemned the dam and drained the lake. In 1950, some studies were being done by the Division of Dams on dams or dam repairs at Lake Rose. The Ganoga Glen Trail in Ricketts Glen State Park passes near Lake Rose, as does the Highland Trail.

Geographic entities mentioned:
surface_form: lake rose
instance_of: Lake
countries: United States
coordinates: lat: 41.329166666667
lon: -76.295
In the middle of the 20th century, the state of Pennsylvania condemned the dam and drained the lake. In 1950, some studies were being done by the Division of Dams on dams or dam repairs at Lake Rose. The Ganoga Glen Trail in Ricketts Glen State Park passes near Lake Rose, as does the Highland Trail. Biology. A &quot;Menziesia pilosa&quot; shrub was once observed in the vicinity of Lake Rose.

Geographic entities mentioned:
surface_form: lake rose
instance_of: Lake
countries: United States
coordinates: lat: 41.329166666667
lon: -76.295
The Ganoga Glen Trail in Ricketts Glen State Park passes near Lake Rose, as does the Highland Trail. Biology. A &quot;Menziesia pilosa&quot; shrub was once observed in the vicinity of Lake Rose. Highbrush blueberry also occurs in the vicinity of the lake. Certain types of wildlife can occur in the vicinity of Lake Rose, depending on the time of year.

Geographic entities mentioned:
surface_form: lake rose
instance_of: Lake
countries: United States
coordinates: lat: 41.329166666667
lon: -76.295
Biology. A &quot;Menziesia pilosa&quot; shrub was once observed in the vicinity of Lake Rose. Highbrush blueberry also occurs in the vicinity of the lake. Certain types of wildlife can occur in the vicinity of Lake Rose, depending on the time of year. Birds in this area include white-throated sparrows, mallard ducks, and evening grosbeaks.

Geographic entities mentioned:
surface_form: lake rose
instance_of: Lake
countries: United States
coordinates: lat: 41.329166666667
lon: -76.295
It has a surface area of approximately, and is situated in Fairmount Township. Lake Rose is mostly dry and closely resembles a swamp. Its main inflow is the spillway from Lake Jean. Lake Rose was originally constructed by a squatter named Jesse Dodson. Wildlife, including birds, butterflies, and dragonflies, has been observed near the lake. A number of hiking trails are also in its vicinity.

Geographic entities mentioned:
surface_form: lake jean
instance_of: Lake
countries: United States
coordinates: lat: 41.34111111
lon: -76.29083333
&quot;The physical territory may have shrunk to this patch on top of a city building&quot;, but the spirit has its boundaries extend limitless to horizon beyond. &quot;Views that extend to a distant horizon, with Mount Macedon in one direction and the blue expanse of the bay in the other&quot;, delineate the full extent of this human domain we live in.

Geographic entities mentioned:
surface_form: Mount Macedon
instance_of: Mountain
countries: Australia
coordinates: lat: -37.38291
lon: 144.57625
At the time of the 1991 Nepal census it had a population of 3368 people living in 737 individual households. At the 2011 census, the population of Bung was 4520 inhabitants (2247 male) in 982 individual households. Bung lies in the Himalaya mountains, 54 km South of Mount Everest and is bordered by the Hunku Drangka (East). Gudel lies on the other side of the valley of Bung. Villages and Hamlets.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
High-Rise Invasion. is a Japanese manga series written by Tsuina Miura and illustrated by Takahiro Oba. The series was serialized online in DeNA's Manga Box app from December 2013 to April 2019, with Kodansha compiling it into twenty-one volumes. The manga is licensed in North America by Seven Seas Entertainment.

Geographic entities mentioned:
surface_form: DeNA
instance_of: Mountain
countries: Iran
coordinates: lat: 30.951666666667
lon: 51.4375
Manga. The manga was serialized online in DeNA's Manga Box app from December 5, 2013 to April 4, 2019. Kodansha held the license to publish the series and compiled it into twenty-one volumes, while Seven Seas Entertainment published it in two-in-one omnibus volumes in North America from June 2018 to October 2021.

Geographic entities mentioned:
surface_form: DeNA
instance_of: Mountain
countries: Iran
coordinates: lat: 30.951666666667
lon: 51.4375
Buccament River. The Buccament River is a river in the south-west of Saint Vincent. It rises on the western slopes of Grand Bonhomme, flowing west to reach the Caribbean Sea close to the town of Layou. Important Bird Area.

Geographic entities mentioned:
surface_form: Grand Bonhomme
instance_of: Mountain
countries: Saint Vincent and the Grenadines
coordinates: lat: 13.233333333333
lon: -61.233333333333
Nicobi Lake. The Nicobi Lake is a freshwater body of the southern part of Eeyou Istchee James Bay (municipality), in the administrative region of Nord-du-Québec, in the province of Quebec, in Canada. Forestry is the main economic activity of the sector.

Geographic entities mentioned:
surface_form: nicobi lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.345277777778
lon: -75.996111111111
Forestry is the main economic activity of the sector. Further south, thanks to the creation of the Wetetnagami Lake Protected Biodiversity Reserve, recreational and tourism activities have been highlighted. The hydrographic slope of Lake Nicobi is accessible via the R1051 forest road which passes to south of the lake.

Geographic entities mentioned:
surface_form: wetetnagami lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.9111
lon: -76.25889
From the Yayoi pottery found in the excavation, the first burial dates from the end of the late Yayoi period. Pottery from many locations, including the Ikoma Mountains of Kawachi, the lower reaches of Sanuki and the Tokai region of Japanese were also excavated.

Geographic entities mentioned:
surface_form: Ikoma Mountains
instance_of: Mountain
countries: Japan
coordinates: lat: 34.678452777778
lon: 135.67896944444
Älpelekopf (Gerstruben). Älpelekopf is a mountain with an elevation of 1,606 m (5,269 ft) in the Alps. Älpelekopf has a secondary peak situated on a ridge which runs southwest from Riffenkopf to Schrofen at which point the ridge falls off steeply. The ridges connecting Riffenkopf, Hahnenkopf and Wannenkopf form a ring around the valley &quot;Gerstruber Älpeles&quot;.

Geographic entities mentioned:
surface_form: Riffenkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 47.37933
lon: 10.31732
Älpelekopf has a secondary peak situated on a ridge which runs southwest from Riffenkopf to Schrofen at which point the ridge falls off steeply. The ridges connecting Riffenkopf, Hahnenkopf and Wannenkopf form a ring around the valley &quot;Gerstruber Älpeles&quot;. This valley has a deserted cabin and was formerly used as a pastoral area.

Geographic entities mentioned:
surface_form: Riffenkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 47.37933
lon: 10.31732
Lake Charest. Lake Charest (Mékinac) is located in the area Montauban-les-Mines, in the municipality of Notre-Dame-de-Montauban, in the Mékinac Regional County Municipality (RCM), in the extreme east of the administrative region of Mauricie, in Québec, Canada. Geography. Lake Charest is located just east of the mining village of Montautan-les-Mines.

Geographic entities mentioned:
surface_form: lake charest
instance_of: Lake
countries: Canada
coordinates: lat: 46.8311
lon: -72.3253
Lake Charest (Mékinac) is located in the area Montauban-les-Mines, in the municipality of Notre-Dame-de-Montauban, in the Mékinac Regional County Municipality (RCM), in the extreme east of the administrative region of Mauricie, in Québec, Canada. Geography. Lake Charest is located just east of the mining village of Montautan-les-Mines. It is located close to the limit of Saint-Ubalde.

Geographic entities mentioned:
surface_form: lake charest
instance_of: Lake
countries: Canada
coordinates: lat: 46.8311
lon: -72.3253
Then the river flows south-east (almost in parallel to the Batiscan River) and through 16 lots in the row Price in the eastern section of Saint-Adelphe, where its course becomes very coil down to its mouth. The shape of the lake Charest resembles to a pear which is raising his hat, and the top facing north. Lake Charest has a length of 0.56 km and a maximum width of 0.27 km.

Geographic entities mentioned:
surface_form: lake charest
instance_of: Lake
countries: Canada
coordinates: lat: 46.8311
lon: -72.3253
surface_form: lake charest
instance_of: Lake
countries: Canada
coordinates: lat: 46.8311
lon: -72.3253
It follows the line Dubrovnik-Bijela gora (above Grahovo)-Cuce-Čevska planina-Ostrog-Razbijeni vrh (Bjelopavlići)-Donja Morača-Kom. Serbian poet Matija Bećković wrote a book of poems of the same name.

Geographic entities mentioned:
surface_form: Bijela gora
instance_of: Plateau
countries: Montenegro
Bosnia and Herzegovina
coordinates: lat: 42.585
lon: 18.57
Water features. The Linacre Reservoirs are a notable amenity to the centre east of the parish within Linacre Park, and was once used for providing water for Chesterfield, but became non-operational in 1995, instead reverting to a leisure and habitat destination owned by the local water board, Severn Trent.

Geographic entities mentioned:
surface_form: Linacre Reservoirs
instance_of: Group of lakes
countries: United Kingdom
coordinates: lat: 53.249
lon: -1.509
Williamstown, Rhondda Cynon Taf. Williamstown () is a village in the Rhondda Valley in the county borough of Rhondda Cynon Taf, within the historic county boundaries of Glamorgan, Wales. Williamstown was founded in the 1870s, is located at the foot of Mynydd Dinas and is a district of neighbouring village Penygraig. Early history.

Geographic entities mentioned:
surface_form: Rhondda Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
Indo-Aryan migration into the region, from Central Asia, is considered to have started after 2000 BCE as a slow diffusion during the Late Harappan period and led to a language shift in the northern Indian subcontinent. Several hundred years later, the Iranian languages were brought into the Iranian plateau by the Iranians, who were closely related to the Indo-Aryans.

Geographic entities mentioned:
surface_form: Iranian plateau
instance_of: Plateau
countries: Iran
coordinates: lat: 36.283333
lon: 59.05
Several hundred years later, the Iranian languages were brought into the Iranian plateau by the Iranians, who were closely related to the Indo-Aryans. The Proto-Indo-Iranian culture, which gave rise to the Indo-Aryans and Iranians, developed on the Central Asian steppes north of the Caspian Sea as the Sintashta culture (c.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
dated a chariot burial at Krivoye Lake to about 2000 BCE and a Bactria-Margiana burial that also contains a foal has recently been found, indicating further links with the steppes.

Geographic entities mentioned:
surface_form: Krivoye Lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.259166666667
lon: 59.228055555556
In the east, the Scythians occupied several areas in Xinjiang, from Khotan to Tumshuq. The Medes, Parthians and Persians begin to appear on the western Iranian Plateau from c. 800 BCE, after which they remained under Assyrian rule for several centuries, as it was with the rest of the peoples in the Near East. The Achaemenids replaced Median rule from 559 BCE.

Geographic entities mentioned:
surface_form: Iranian Plateau
instance_of: Plateau
countries: Iran
coordinates: lat: 36.283333
lon: 59.05
Witzel points to the central Afghan highlands. Humbach derives Vaējah from cognates of the Vedic root &quot;vij&quot;, suggesting the region of fast-flowing rivers. Gnoli considers Choresmia (Xvairizem), the lower Oxus region, south of the Aral Sea to be an outlying area in the Avestan world. However, according to, the probable homeland of Avestan is, in fact, the area south of the Aral Sea.

Geographic entities mentioned:
surface_form: Aral Sea
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
According to the family tradition Ban Borić of Bosnia, who ruled from 1154 until c.1167, was an ancestor of the family. Their royal title was Ban of Bosnia (&quot;Ban de Bosna&quot;), while noble titles were Lord of Posavina (&quot;Signor de Posava&quot;) and Perpetual Count of Dobor (&quot;Comes Perpetuus de Dobor&quot;). Stjepan was the elder son of Ivaniš Berislavić (d.

Geographic entities mentioned:
surface_form: Posavina
instance_of: Valley
countries: Croatia
Bosnia and Herzegovina
Serbia
coordinates: lat: 45.16667
lon: 17.33333
When Jelena remarried to Ivaniš Berislavić in 1504, he received the title, from king Vladislaus II (d. 1516), and held it until his death in 1514. Regnal ascensions. From 1529, he has controlled regions in Slavonian Posavina, centered in Brod. During 1532 and 1533, he negotiated with king Ferdinand Habsburg, but no agreement was reached. Serbia (titular).

Geographic entities mentioned:
surface_form: Posavina
instance_of: Valley
countries: Croatia
Bosnia and Herzegovina
Serbia
coordinates: lat: 45.16667
lon: 17.33333
Kochu Pamba Weir. Kochu Pamba Weir is a diversion dam constructed across Pamba river in Seethathode village of Pathanamthitta district in Kerala, India. It is one of the five dams which are parts of Sabarigiri Hydro Electric Project. These are Pamba dam, Kakki dam, Anathode dam, Gavi dam and Kochu Pamba weir.

Geographic entities mentioned:
surface_form: Pamba river
instance_of: Watercourse
countries: India
coordinates: lat: 9.5
lon: 76.416666666667
In 1032 Sancho of Pamplona forced a marriage between his son, Fernando of Castile, and Sancha of León, and those lands went to Castile as part of her dowry. In 1034, Sancho wrested the city of León itself from his son-in-law, Bermudo, who retreated into Galicia. By the time Sancho died in 1035, the &quot;meseta&quot; north of the Duero was dominated by the Pyrenean pocket kingdom of Navarre.

Geographic entities mentioned:
surface_form: meseta
instance_of: Plateau
countries: Spain
coordinates: lat: 40.5
lon: -3.5
In 1893, Dutreuil de Rhins and Grenard, left Xinjiang in order to cross Tibet and reach Xining in Qinghai. In December, they reached Lake Namtso, the men and animals exhausted and their supplies run out after a journey that had taken them three months longer than anticipated.

Geographic entities mentioned:
surface_form: Lake Namtso
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 30.720833333333
lon: 90.468055555556
Hendy Hills. ous6c3243sjjkfedqvh9jox1p11p" xml:space="preserve">Hendy Hills () are mostly ice-free hills, long and elevation, located along the western margin of the Rhone Glacier where the glacier descends abruptly to Lake Bonney in Taylor Valley, Victoria Land. Named by the New Zealand Geographic Board in 1998 after Chris H.

Geographic entities mentioned:
surface_form: Taylor Valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
Life and career. Wang Bo was born in a rural village of Shandong Province, China on November 2, 1989. The family relocated to the Shaolin village on Mount Song in central Henan Province, home to the Shaolin Temple, a Chán Buddhist monastery built in 495 A.D., considered to be the birthplace of Shaolin Kung Fu and associated with many other Chinese Martial Arts.

Geographic entities mentioned:
surface_form: Mount Song
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 34.484722222222
lon: 112.96027777778
Pizzo delle Pecore. Pizzo delle Pecore (2,381 m) is a mountain of the Swiss Lepontine Alps, located east of Cevio in the canton of Ticino. It lies just south of the slightly higher Cima di Broglio, on the range between the Valle Maggia and the Valle Verzasca.

Geographic entities mentioned:
surface_form: Cima di Broglio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.330416666667
lon: 8.6836388888889
surface_form: Valle Maggia
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.25
lon: 8.7
surface_form: Valle Verzasca
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.2582
lon: 8.8350694444444
surface_form: verzasca
instance_of: Watercourse
countries: Switzerland
coordinates: lat: 46.3908
lon: 8.74333
Pizzo delle Pecore. Pizzo delle Pecore (2,381 m) is a mountain of the Swiss Lepontine Alps, located east of Cevio in the canton of Ticino. It lies just south of the slightly higher Cima di Broglio, on the range between the Valle Maggia and the Valle Verzasca.

Geographic entities mentioned:
surface_form: pizzo delle pecore
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.324888888889
lon: 8.6815277777778
Mount Berry (Antarctica). ioxvl6arjt9x6radlfemj0bb8nee" xml:space="preserve">#redirect Mount Berry

Geographic entities mentioned:
surface_form: mount berry
instance_of: Mountain
coordinates: lat: -64.4333
lon: -60.7167
surface_form: berry
instance_of: Mountain
coordinates: lat: -64.4333
lon: -60.7167
He played Harry Landers in the &quot;Hospital&quot; skit from &quot;Amazon Women on the Moon&quot; opposite wife Michelle Pfeiffer, whom he had previously directed in the ABC Afterschool Special &quot;One Too Many&quot; in 1985. Horton also appeared in the 1997 TV movie version of the Jon Krakauer book ', playing Scott Fischer, the leader of the disastrous 1996 climb on Mount Everest.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Río de la Plata. The Río de la Plata (;), also called the River Plate or La Plata River in English, is the estuary formed by the confluence of the Uruguay River and the Paraná River at Punta Gorda. It empties into the Atlantic Ocean and forms a funnel-shaped indentation on the southeastern coastline of South America.

Geographic entities mentioned:
surface_form: Punta Gorda
instance_of: Landform
countries: Uruguay
Spain
coordinates: lat: -33.91611111
lon: -58.41444444
Geography. The Río de la Plata begins at the confluence of the Uruguay and Paraná rivers at Punta Gorda and flows eastward into the South Atlantic Ocean. No clear physical boundary marks the river's eastern end; the International Hydrographic Organization defines the eastern boundary of the Río de la Plata as &quot;a line joining Punta del Este, Uruguay and Cabo San Antonio, Argentina&quot;.

Geographic entities mentioned:
surface_form: Punta Gorda
instance_of: Landform
countries: Uruguay
Spain
coordinates: lat: -33.91611111
lon: -58.41444444
The Río de la Plata region, particularly Buenos Aires, was a significant site of trade throughout the 17th century. The Crown initially intended Buenos Aires to be a military establishment for the protection of the Potosí mines, but it soon became evident that a settlement large enough to provide military defense would attract trade.

Geographic entities mentioned:
surface_form: Potosí mines
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.618901
lon: -65.749687
Ticonderoga campaign reforms. In 1758, in preparation for the attack on the French fort at Ticonderoga, which controlled access from Lake George to Lake Champlain, Lord Howe set about reforming General James Abercrombie's army for warfare in North America. He used his own 55th Regiment as an example for the rest of the army to follow.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
It is also known to roost in trees. Its range extends from the Senegal Basin and Guinea-Bissau Drainage in West Africa to the Ethiopian Highlands and South-West Rift Valley in East Africa. &quot;Balearica pavonina pavonina&quot; occupies the western part of this range, while &quot;Balearica pavonina ceciliae&quot; is found in the east with the greatest numbers in Sudan. Vocalization.

Geographic entities mentioned:
surface_form: Rift Valley
instance_of: Group of lakes
countries: Kenya
Tanzania
Ethiopia
Malawi
Mozambique
Democratic Republic of the Congo
Rwanda
Burundi
Uganda
Zambia
coordinates: lat: 3
lon: 36.333333333333336
From there it would have run along the Jersey Central's line to Constable Hook, and then pass through a tunnel under the Kill Van Kull and connect with the North Shore Branch in New Brighton. They proposed several stops in Bayonne and Jersey City and a stop on Richmond Terrace.

Geographic entities mentioned:
surface_form: Constable Hook
instance_of: Landform
countries: United States
coordinates: lat: 40.6578
lon: -74.0994
The mountain sits about southwest of the village of Fossbergom and about northeast of the village of Øvre Årdal. The mountain is surrounded by several other notable mountains including Svellnosbreahesten to the north; Store Tverråtinden to the west, Bukkehøe and Lindbergtinden to the southwest, Bukkeholstindene to the southwest, and Store Styggehøe and Bukkeholshøe to the southeast.

Geographic entities mentioned:
surface_form: Svellnosbreahesten
instance_of: Mountain
countries: Norway
coordinates: lat: 61.6214
lon: 8.3075
surface_form: Store Tverråtinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.615277777778
lon: 8.3019444444444
surface_form: Bukkehøe
instance_of: Mountain
countries: Norway
coordinates: lat: 61.604166666667
lon: 8.2661111111111
surface_form: Lindbergtinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.604336
lon: 8.280225
surface_form: Store Styggehøe
instance_of: Mountain
countries: Norway
coordinates: lat: 61.5911
lon: 8.33722
surface_form: bukkeholshøe
instance_of: Mountain
countries: Norway
coordinates: lat: 61.57972222
lon: 8.35583333
surface_form: tverråtinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.6142
lon: 8.30139
surface_form: styggehøe
instance_of: Mountain
countries: Norway
coordinates: lat: 61.5911
lon: 8.33722
surface_form: styggehøe
instance_of: Mountain
countries: Norway
coordinates: lat: 61.58853
lon: 8.61946
surface_form: styggehøe
instance_of: Mountain
countries: Norway
coordinates: lat: 61.46639
lon: 8.92042
Midtre Tverråtinden. Midtre Tverråtinden is a mountain in Lom Municipality in Innlandet county, Norway. The tall mountain is located in the Jotunheimen mountains within Jotunheimen National Park. The mountain sits about southwest of the village of Fossbergom and about northeast of the village of Øvre Årdal.

Geographic entities mentioned:
surface_form: tverråtinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.6142
lon: 8.30139
surface_form: midtre tverråtinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.614444444444
lon: 8.3152777777778
He left the post in 1894, when President Grover Cleveland took office, and was re-appointed to the office in 1903 by President Theodore Roosevelt. Snider grew up in the Goose Lake Valley, an area that straddles the Oregon-California border. He attended school in Lakeview, where he graduated from Lakeview High School in 1898.

Geographic entities mentioned:
surface_form: Goose Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.6
lon: -120.4
state of Arkansas. The route is split into three sections, all of which are located in western Arkansas. The first and longest section begins at AR 22 in Subiaco, and ends near Lake Dardanelle southwest of Tokalon. The second section begins at AR 22 in New Blaine, and ends just south of Shoal Bay. The third section begins at AR 10 in Booneville, and ends about south.

Geographic entities mentioned:
surface_form: Lake Dardanelle
instance_of: Lake
countries: United States
coordinates: lat: 35.2833
lon: -93.2333
The route heads towards the north, before taking a sharp turn towards the east near Wilkins, right at the intersection of AR 393. The route heads more in a northeasterly direction for about before entering the town of Scranton, and intersecting AR 109. The route continues east for about before reaching its northern terminus near Lake Dardanelle. The route is about long. Section 2.

Geographic entities mentioned:
surface_form: Lake Dardanelle
instance_of: Lake
countries: United States
coordinates: lat: 35.2833
lon: -93.2333
Wheeler Ridge, California. Wheeler Ridge is an unincorporated community in the southwestern San Joaquin Valley, within Kern County, California. It is at the junction of the valley floor and the Wheeler Ridge landform of the Tehachapi Mountains. Geography. The community is located at the Wheeler Ridge Interchange, the junction of State Route 99 and Interstate 5.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Nowadays many people park their cars on Sheriffmuir and take a longer but more gently sloping path to the summit, passing behind, i.e. slightly to the north of, the summit of Castle Law. The third route is via Menstrie Glen from the east, and is a somewhat gentle ascent in the beginning, which steepens satisfactorily for those who like a decent climb, as the summit is approached.

Geographic entities mentioned:
surface_form: Menstrie Glen
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.158
lon: -3.857
surface_form: menstrie glen
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.158
lon: -3.857