Sarmila/GeoWiki-Features huggingface dataset:
Turnpikes followed the route of Lenape trails through the gap. By the 1750s, the Great Valley was well-settled to the southern end of the Shenandoah Valley. Immigrants continued to travel from the Philadelphia area south through the Great Valley beyond Shenandoah, to the vicinity of present-day Roanoke, Virginia. There is a wide gap in the Blue Ridge near Roanoke.

Geographic entities mentioned:
surface_form: shenandoah valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Turnpikes followed the route of Lenape trails through the gap. By the 1750s, the Great Valley was well-settled to the southern end of the Shenandoah Valley. Immigrants continued to travel from the Philadelphia area south through the Great Valley beyond Shenandoah, to the vicinity of present-day Roanoke, Virginia. There is a wide gap in the Blue Ridge near Roanoke.

Geographic entities mentioned:
surface_form: shenandoah
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 40.0586
lon: -75.5306
Just south of the Catskills, the first folds of the Ridge-and-Valley Appalachians border the valley, in the form of a continuous ridge (heading south) and known as the Shawangunk Ridge in New York, Kittatinny Mountain in New Jersey, and Blue Mountain in Pennsylvania.

Geographic entities mentioned:
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.95481
lon: -123.25907
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: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.8725
lon: -74.401111111111
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.5456079
lon: -90.4940088
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.8482
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surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.8158
lon: -114.186
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1469
lon: -74.8489
Interstate highways. In the &quot;northern&quot; valley, the thoroughfares vary. Heading northeast from Harrisburg, I-81 traces the valley to Swatara Gap, then swings north across Blue Mountain and leaves the valley en route to Scranton. I-78 then continues the route through the valley parallel to the southern slopes of Blue Mountain, connecting Harrisburg with Lebanon, Kutztown, and Allentown.

Geographic entities mentioned:
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.95481
lon: -123.25907
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: 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: 61.3833
lon: -150.25
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.8725
lon: -74.401111111111
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.5456079
lon: -90.4940088
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.8482
lon: -120.198
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.8158
lon: -114.186
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1469
lon: -74.8489
Interstate highways. In the &quot;northern&quot; valley, the thoroughfares vary. Heading northeast from Harrisburg, I-81 traces the valley to Swatara Gap, then swings north across Blue Mountain and leaves the valley en route to Scranton. I-78 then continues the route through the valley parallel to the southern slopes of Blue Mountain, connecting Harrisburg with Lebanon, Kutztown, and Allentown.

Geographic entities mentioned:
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.95481
lon: -123.25907
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.8725
lon: -74.401111111111
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.5456079
lon: -90.4940088
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.8482
lon: -120.198
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.8158
lon: -114.186
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1469
lon: -74.8489
This upcountry population soon surpassed the older and more established lowcountry population near the Atlantic coast, causing serious geopolitical tensions in the Carolinas during the late 18th century (Meinig, 1986: 291–293). On the west side, the Cumberland Gap became the main route for migration west from the southern Great Valley to Kentucky and Tennessee.

Geographic entities mentioned:
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 40.0586
lon: -75.5306
American Civil War. The Great Valley, especially Shenandoah Valley, played an important role during the American Civil War, including its Blue Ridge gaps and nearby Piedmont area and its northward extension to Gettysburg, Pennsylvania, where the bloodiest and most influential Civil War battle was fought in the Battle of Gettysburg from July 1 to July 3, 1863.

Geographic entities mentioned:
surface_form: battle
instance_of: Watercourse
countries: United States
coordinates: lat: 44.9266
lon: -93.0291
surface_form: battle
instance_of: Watercourse
countries: United States
coordinates: lat: 44.9266
lon: -93.0291
surface_form: battle
instance_of: Watercourse
countries: United States
coordinates: lat: 44.9266
lon: -93.0291
surface_form: piedmont
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -80
Another series of mountains bounds the southern Great Valley to the west, including North Mountain and Great North Mountain, the Allegheny Front, Powell Mountain, the Cumberland Mountains, Walden Ridge, and the Cumberland Plateau. The Cumberland Gap connects the Great Valley region with Kentucky and Tennessee lands to the west.

Geographic entities mentioned:
surface_form: cumberland
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 40.0586
lon: -75.5306
In the Shenandoah Valley, the road was known as the Valley Pike. The Wilderness Road branched off from Great Wagon Road in present-day Roanoke, Virginia, crossed the Cumberland Gap and led to Kentucky and Tennessee, including the fertile Bluegrass region and Nashville Basin.

Geographic entities mentioned:
surface_form: cumberland
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
<section begin=&quot;weather box&quot; /><section end=&quot;weather box&quot; />
Native Americans. Routes through the valley were first used by Native Americans. In pre-colonial and the early colonial era, a major Indian pathway through the Great Valley was known as the Great Indian Warpath, Seneca Trail, and various other names. European colonialism.

Geographic entities mentioned:
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instance_of: Lake
countries: United States
coordinates: lat: 42.655555555556
lon: -76.8975
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 40.0586
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A gap in these mountains exists near Roanoke, Virginia. Other gaps of note in the Blue Ridge of Virginia, connecting the Piedmont region with the Great Valley, include Thornton Gap, Swift Run Gap, and Rockfish Gap.

Geographic entities mentioned:
surface_form: piedmont
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -80
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 40.0586
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Immigrants continued to travel from the Philadelphia area south through the Great Valley beyond Shenandoah, to the vicinity of present-day Roanoke, Virginia. There is a wide gap in the Blue Ridge near Roanoke. A branch of the Great Wagon Road began there, crossing through the gap east into the Piedmont region of North Carolina and South Carolina. This road became known as the Carolina Road.

Geographic entities mentioned:
surface_form: piedmont
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -80
This road became known as the Carolina Road. During the 1750s, the stream of migrants traveling south through the valley and into the Carolina Piedmont grew into a flood. At the time, the Carolina Piedmont region offered some of the best land at the lowest prices. A string of towns appeared, including Salisbury, Salem, and Charlotte in North Carolina.

Geographic entities mentioned:
surface_form: piedmont
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -80
surface_form: piedmont
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -80
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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surface_form: the valley
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countries: United States
coordinates: lat: 61.3833
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surface_form: the valley
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countries: United States
coordinates: lat: 47.7174
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The Wilderness Road branched off from Great Wagon Road in present-day Roanoke, Virginia, crossed the Cumberland Gap and led to Kentucky and Tennessee, including the fertile Bluegrass region and Nashville Basin. Another branch at Roanoke, called the Carolina Road, led into the Piedmont regions of North Carolina, South Carolina, and Georgia.

Geographic entities mentioned:
surface_form: piedmont
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -80
At the time, the Carolina Piedmont region offered some of the best land at the lowest prices. A string of towns appeared, including Salisbury, Salem, and Charlotte in North Carolina. In the decades before the American Revolution, the Piedmont &quot;upcountry&quot; of the Carolinas was quickly settled, mostly by recent immigrants who migrated from the north to the south via the Great Valley.

Geographic entities mentioned:
surface_form: piedmont
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -80
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 40.0586
lon: -75.5306
Great Appalachian Valley. The Great Appalachian Valley, also called The Great Valley or Great Valley Region, is one of the major landform features of eastern North America. It is a gigantic trough, including a chain of valley lowlands, and the central feature of the Appalachian Mountains system.

Geographic entities mentioned:
surface_form: great appalachian valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
Great Appalachian Valley. The Great Appalachian Valley, also called The Great Valley or Great Valley Region, is one of the major landform features of eastern North America. It is a gigantic trough, including a chain of valley lowlands, and the central feature of the Appalachian Mountains system.

Geographic entities mentioned:
surface_form: great appalachian valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 40.0586
lon: -75.5306
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 40.0586
lon: -75.5306
The trough stretches about from Quebec in the north to Alabama in the south and has been an important north–south route of travel since prehistoric times. Geography. The Great Valley marks the eastern edge of the Ridge and Valley physiographic province. There are many regional names of the Great Valley, such as the Shenandoah Valley.

Geographic entities mentioned:
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 40.0586
lon: -75.5306
Geography. The Great Valley marks the eastern edge of the Ridge and Valley physiographic province. There are many regional names of the Great Valley, such as the Shenandoah Valley. From a large perspective the Great Valley can be divided into a northern section and a southern section. Northern section.

Geographic entities mentioned:
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 40.0586
lon: -75.5306
A series of mountains bounds the northern half of the Great Valley on both sides.

Geographic entities mentioned:
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 40.0586
lon: -75.5306
There is a wide gap between the Reading Prong and South Mountain at Harrisburg, through which the Susquehanna River passes, connecting the Great Valley with the Piedmont region of southeast Pennsylvania. This gap is often considered the dividing point between the northern and southern sections of the Great Valley.

Geographic entities mentioned:
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 40.0586
lon: -75.5306
This gap is often considered the dividing point between the northern and southern sections of the Great Valley. To the west or continental side, a series of more impenetrable mountain regions border the northern Great Valley. The northernmost is the Adirondack Mountains, a southern extension of the Canadian Shield, which reach the valley along the shores of Lake Champlain and Lake George.

Geographic entities mentioned:
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 40.0586
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The Valley of Virginia is a region of karst, with sinkholes and caverns. Climate. The climate of the Great Valley is generally Warm- or Hot-summer Humid continental in the northern third and Humid subtropical from Pennsylvania southward. The first weather box is from the temperate portion and the second subtropical portion of the valley.

Geographic entities mentioned:
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 40.0586
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Another branch at Roanoke, called the Carolina Road, led into the Piedmont regions of North Carolina, South Carolina, and Georgia. The various gaps connecting the Great Valley to lands to the east and west have played important roles in American history. On the east side, the wide gap in southeast Pennsylvania became the main route for colonization of the Great Valley.

Geographic entities mentioned:
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 40.0586
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The various gaps connecting the Great Valley to lands to the east and west have played important roles in American history. On the east side, the wide gap in southeast Pennsylvania became the main route for colonization of the Great Valley. By the 1730s, the Pennsylvanian Great Valley west of South Mountain was open to settlement after treaty cessions and purchases from the Indians.

Geographic entities mentioned:
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 40.0586
lon: -75.5306
The road from Philadelphia west to the valley and then south through it became very heavily used and known variously as the Great Wagon Road, the Philadelphia Wagon Road, and the Valley Road. The Conestoga wagon was developed around 1725 in the area of the wide opening between Philadelphia and the Great Valley.

Geographic entities mentioned:
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 40.0586
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The Conestoga wagon was developed around 1725 in the area of the wide opening between Philadelphia and the Great Valley. The Conestoga wagon became the main vehicle for transportation through the Great Valley until the railroad era. Culver Gap near Culver's Lake in Sussex County, New Jersey, was an important route through the Kittatinny Mountain from about 10,000 years ago to present.

Geographic entities mentioned:
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: great valley
instance_of: Valley
countries: United States
coordinates: lat: 40.0586
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It is a gigantic trough, including a chain of valley lowlands, and the central feature of the Appalachian Mountains system. The trough stretches about from Quebec in the north to Alabama in the south and has been an important north–south route of travel since prehistoric times. Geography. The Great Valley marks the eastern edge of the Ridge and Valley physiographic province.

Geographic entities mentioned:
surface_form: the trough
instance_of: Landform
countries: United States
coordinates: lat: 39.2236
lon: -78.8575
The Cumberland Gap connects the Great Valley region with Kentucky and Tennessee lands to the west. Massanutten Mountain lies in the middle of the Valley of Virginia portion of the Great Valley. The Valley of Virginia is a region of karst, with sinkholes and caverns. Climate.

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
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countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Climate. The climate of the Great Valley is generally Warm- or Hot-summer Humid continental in the northern third and Humid subtropical from Pennsylvania southward. The first weather box is from the temperate portion and the second subtropical portion of the valley. <section begin=&quot;weather box&quot; /><section end=&quot;weather box&quot; />
Native Americans.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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coordinates: lat: 61.3833
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coordinates: lat: 47.7174
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European colonialism. For European colonists, the Great Valley was a major route for settlement and commerce in the United States along the Great Wagon Road, which began in Philadelphia. In the Shenandoah Valley, the road was known as the Valley Pike.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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coordinates: lat: 61.3833
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countries: United States
coordinates: lat: 47.7174
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The entire region between southeast Pennsylvania and the Shenandoah Valley soon became famous as a breadbasket, the most productive mixed farming region in America (Meinig, 1986:134). The road from Philadelphia west to the valley and then south through it became very heavily used and known variously as the Great Wagon Road, the Philadelphia Wagon Road, and the Valley Road.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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countries: United States
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Civil War-era sites and events in this region include Harpers Ferry, West Virginia; Antietam, Maryland; Chambersburg, Pennsylvania; the Valley Campaign of Northern Virginia; the Valley Campaigns of 1864, also in Virginia; the Battles of Chattanooga in Tennessee; and the Gettysburg Battlefield and Gettysburg National Cemetery in Pennsylvania. Interstate highways.

Geographic entities mentioned:
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countries: United States
coordinates: lat: 34.155833333333334
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At Allentown, I-78 then swings away south into the hills of the Reading Prong en route to New York City. From Allentown into New Jersey and southern New York, the valley is not traced by an interstate highway, though it is traversed at length (and at oblique angles) by both I-80 and I-84, as well as by the Delaware River between Easton, Pennsylvania, and the Delaware Water Gap.

Geographic entities mentioned:
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countries: United States
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In New Jersey and New York, the valley gradually bends from the northeast to the north, and starting near Newburgh just beyond the Hudson Highlands, I-87 runs much of the valley's length into Canada, passing Poughkeepsie, Albany, and Glens Falls. In an east–west section of the valley, I-90 traverses the Mohawk Valley towards Utica.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
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In an east–west section of the valley, I-90 traverses the Mohawk Valley towards Utica. North of Glens Falls, I-87 runs west of the valley through the Adirondack Mountains, though it descends back into the valley near Plattsburgh. At the Canada–US border, I-87 becomes Autoroute 15 and continues north to Montreal.

Geographic entities mentioned:
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countries: United States
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The gap is more than below the top of the mountain. Lenape Native Americans used the gap to hunt and trade on both sides of the mountain. Early settlers from Pennsylvania used the water drop from Culvers Lake to Branchville for a wide assortment of mills. Turnpikes followed the route of Lenape trails through the gap.

Geographic entities mentioned:
surface_form: culvers lake
instance_of: Lake
countries: United States
coordinates: lat: 41.17
lon: -74.776
Lake Manzherok. Lake Manzherok (Manzherok, Altay: Manјӱrek, &quot;Manĵürek&quot;) is a lake in the Altai Republic, located on the right bank of the Katun, at an altitude of 373 m above sea level. The Altai name of the lake is Doingol. The length of the lake is 1112 m, the maximum width is 400 m, the depth is 2.5-2.8 m, and the area is 37.6 ha.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake manzherok
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 51.821666666667
lon: 85.811666666667
Lake Manzherok. Lake Manzherok (Manzherok, Altay: Manјӱrek, &quot;Manĵürek&quot;) is a lake in the Altai Republic, located on the right bank of the Katun, at an altitude of 373 m above sea level. The Altai name of the lake is Doingol. The length of the lake is 1112 m, the maximum width is 400 m, the depth is 2.5-2.8 m, and the area is 37.6 ha.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake manzherok
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 51.821666666667
lon: 85.811666666667
Lake Manzherok. Lake Manzherok (Manzherok, Altay: Manјӱrek, &quot;Manĵürek&quot;) is a lake in the Altai Republic, located on the right bank of the Katun, at an altitude of 373 m above sea level. The Altai name of the lake is Doingol. The length of the lake is 1112 m, the maximum width is 400 m, the depth is 2.5-2.8 m, and the area is 37.6 ha.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The Altai name of the lake is Doingol. The length of the lake is 1112 m, the maximum width is 400 m, the depth is 2.5-2.8 m, and the area is 37.6 ha. The village of the same name is located 2 km from the lake, on the banks of the Katun River. Near the lake is the village of Ozernoye. The lake is a natural monument. The lake is fed by streams, atmospheric precipitation and groundwater.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The length of the lake is 1112 m, the maximum width is 400 m, the depth is 2.5-2.8 m, and the area is 37.6 ha. The village of the same name is located 2 km from the lake, on the banks of the Katun River. Near the lake is the village of Ozernoye. The lake is a natural monument. The lake is fed by streams, atmospheric precipitation and groundwater. The water is fresh and soft.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The lake is fed by streams, atmospheric precipitation and groundwater. The water is fresh and soft. The water has a dirty green color, low transparency (60–180 cm), temperature - 22 °C in summer. According to chemical analysis, the lake belongs to the chloride-carbonate type. The bottom of the lake is composed of dark gray lake silt. The lake can be called the oxbow of Katun.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The water is fresh and soft. The water has a dirty green color, low transparency (60–180 cm), temperature - 22 °C in summer. According to chemical analysis, the lake belongs to the chloride-carbonate type. The bottom of the lake is composed of dark gray lake silt. The lake can be called the oxbow of Katun. In summer, the lake warms up.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
According to chemical analysis, the lake belongs to the chloride-carbonate type. The bottom of the lake is composed of dark gray lake silt. The lake can be called the oxbow of Katun. In summer, the lake warms up. In 1966, the Soviet-Mongolian Friendship Festival was held on the lake. The lake is a popular tourist destination. Many camp sites organize excursions here.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The bottom of the lake is composed of dark gray lake silt. The lake can be called the oxbow of Katun. In summer, the lake warms up. In 1966, the Soviet-Mongolian Friendship Festival was held on the lake. The lake is a popular tourist destination. Many camp sites organize excursions here. Since 2008, a ski resort has been built near Lake Manzherok. Flora and fauna.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
In 1966, the Soviet-Mongolian Friendship Festival was held on the lake. The lake is a popular tourist destination. Many camp sites organize excursions here. Since 2008, a ski resort has been built near Lake Manzherok. Flora and fauna. The vegetation of the eastern and southeastern slopes is diverse: pine, spruce, fir, birch, honeysuckle, blackcurrant, crataegus, rhododendron, buckthorn, etc.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake manzherok
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 51.821666666667
lon: 85.811666666667
They might instead have been brothers, as an age difference of 16 years among even full siblings is far from unlikely. Still he has been described as the &quot;poorer cousin&quot;, and is believed to have emigrated to Beverwijck in the Hudson Valley circa 1650. The Pieter Bronck House is a registered historic place in Coxsackie, New York.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Valley of a Thousand Hills. The Valley of a Thousand Hills is a valley between Pietermaritzburg and Durban, South Africa. The Umgeni River meets the Msunduzi River (Duzi River) in the valley, and the Dusi Canoe Marathon is run through the area every year. Geography.

Geographic entities mentioned:
surface_form: valley of a thousand hills
instance_of: Valley
countries: South Africa
coordinates: lat: -29.77
lon: 30.71
Geography. The Valley of a Thousand Hills stretches from Cato Ridge in the west to Kloof in the east and coincides with borders of the Outer West Region of the Ethekwini Metropolitan Municipality. The valley includes areas such as Cato Ridge, Inchanga, Mpumalanga (Hammarsdale), Drummond, Peacevale, Botha's Hill, Assagay, Hillcrest, Waterfall, Ngcolosi, Gillitts, Everton and Kloof.

Geographic entities mentioned:
surface_form: valley of a thousand hills
instance_of: Valley
countries: South Africa
coordinates: lat: -29.77
lon: 30.71
For example, the Kazakhstan nature reserve protects many different species. Also, programs that protect pikas and other small mammals also help protect the weasel; Sanjiangyuan, Changtang and Kekexili nature reserves in China are in this category. Another approach to conserving this animal would be to review conservation strategies of other species in the same genus.

Geographic entities mentioned:
surface_form: Changtang
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 30
lon: 90
Mount Daly (Gunnison County, Colorado). Mount Daly is a mountain summit in Gunnison County, Colorado, United States. __NOTOC__

Geographic entities mentioned:
surface_form: mount daly
instance_of: Mountain
countries: United States
coordinates: lat: 39.1075
lon: -107.15194444444
Mount Daly (Gunnison County, Colorado). Mount Daly is a mountain summit in Gunnison County, Colorado, United States. __NOTOC__

Geographic entities mentioned:
surface_form: mount daly
instance_of: Mountain
countries: United States
coordinates: lat: 39.1075
lon: -107.15194444444
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
Walker and again by Blairgowrie architect Lake Falconer in 1912. The school's catchment area currently incorporates Strathardle, Kirkmichael, Glenshee, Blacklunans, Bridge of Cally and Enochdhu. Until the latter part of the 20th century the catchment area also had schools at Straloch, Ballintuim, Strone of Cally, Blackwater and Glenshee but these are all closed with pupils bussed to Kirkmichael.

Geographic entities mentioned:
surface_form: Glenshee
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.8
lon: -3.4333333333333
Chiemsee Cauldron. The Chiemsee Cauldron () is a gold cauldron found at the bottom of Lake Chiemsee in Bavaria, Germany, in 2001. Initially thought to be around 2,000 years old due to its similarity to the Gundestrup cauldron, the Chiemsee cauldron was later attributed to the 20th century though its origins and meaning remain disputed.

Geographic entities mentioned:
surface_form: Lake Chiemsee
instance_of: Lake
countries: Germany
coordinates: lat: 47.89
lon: 12.47
Due to the modern attribution, attempts to sell the cauldron as an ancient artefact have been the subject of fraud trials. Discovery. The Chiemsee Cauldron was discovered in 2001 by Jens Essig, a local diver, at the bottom of Lake Chiemsee, about 200m from the shore near Arlaching, Chieming municipality. The cauldron has a diameter of and a height of, and is made from of 18 carat gold.

Geographic entities mentioned:
surface_form: Lake Chiemsee
instance_of: Lake
countries: Germany
coordinates: lat: 47.89
lon: 12.47
Pizzo Bianco. Pizzo Bianco is a mountain of the Pennine Alps, overlooking Macugnaga in the Italian region of Piedmont. It lies on the range north of the Punta Grober, between the Belvedere Glacier and the valley of Quarazza. Pizzo Bianco faces the east wall of Monte Rosa and is a popular vantage point.

Geographic entities mentioned:
surface_form: Punta Grober
instance_of: Mountain
countries: Italy
coordinates: lat: 45.916667
lon: 7.916667
Pizzo Bianco. Pizzo Bianco is a mountain of the Pennine Alps, overlooking Macugnaga in the Italian region of Piedmont. It lies on the range north of the Punta Grober, between the Belvedere Glacier and the valley of Quarazza. Pizzo Bianco faces the east wall of Monte Rosa and is a popular vantage point.

Geographic entities mentioned:
surface_form: pizzo bianco
instance_of: Mountain
countries: Italy
coordinates: lat: 45.93805556
lon: 7.94
Pizzo Bianco is a mountain of the Pennine Alps, overlooking Macugnaga in the Italian region of Piedmont. It lies on the range north of the Punta Grober, between the Belvedere Glacier and the valley of Quarazza. Pizzo Bianco faces the east wall of Monte Rosa and is a popular vantage point. In 1789 Horace-Bénédict de Saussure reached its summit in order to measure the height of Monte Rosa.

Geographic entities mentioned:
surface_form: pizzo bianco
instance_of: Mountain
countries: Italy
coordinates: lat: 45.93805556
lon: 7.94
After the bloody defeat of Donghak, Gang Il-sun wandered around Korea for three years, surveying public sentiment. In 1900, he returned home and, starting in the years that followed, gathered a sizable number of followers. According to these followers, during the Summer of 1901 he achieved enlightenment on the Moaksan mountain, after forty-nine days of ascetic practices and fasting.

Geographic entities mentioned:
surface_form: Moaksan
instance_of: Mountain
countries: South Korea
coordinates: lat: 35.72916667
lon: 127.08527778
Climate. It has a hot and humid climate. The hottest part of the year is May to early June with maximum temperatures around 35-42 °C. The coolest part of the year is January with a minimum temperature of 19-25 °C. It gets most of its rain fall from seasonal monsoon winds from August to December. This place is also affected by Cyclones from the Bay of Bengal.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Of this area, 49.3% is used for agricultural purposes, while 25.5% is forested. Of the rest of the land, 0.2% is settled (buildings or roads) and the remainder (25%) is non-productive (rivers, glaciers or mountains). Alplersee is located on the slopes of Rophaien. Demographics. Riemenstalden has a population (as of) of., 2.4% of the population was made up of foreign nationals.

Geographic entities mentioned:
surface_form: Alplersee
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.935555555556
lon: 8.6538888888889
surface_form: Rophaien
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.92798
lon: 8.64649
Tissa donated a royal park in the city to the Buddhist community, which was the beginning of the Mahāvihāra tradition. Mahinda is associated with the site of Mihintale, one of the oldest Buddhist site in Sri Lanka. Mihintale includes numerous caves which may have been used by the early Sri Lankan sangha. According to S. D.

Geographic entities mentioned:
surface_form: Mihintale
instance_of: Mountain
countries: Sri Lanka
coordinates: lat: 8.350594
lon: 80.516945
The northern part spans the Orobian Alps with the highest point being Mount Coca at. Its rivers include the Serio, Dezzo, Cherio, Brembo, and Adda. Its valleys include the Seriana, Cavallina, and Brembana. Other, smaller but important valleys include the Valle Imagna, the Val di Scalve, the Val Brembilla, the Val Serina, and the Val Taleggio. The southern part is mainly made up of flatlands.

Geographic entities mentioned:
surface_form: Brembana
instance_of: Valley
countries: Italy
coordinates: lat: 45.8725
lon: 9.651944444444444
The northern part spans the Orobian Alps with the highest point being Mount Coca at. Its rivers include the Serio, Dezzo, Cherio, Brembo, and Adda. Its valleys include the Seriana, Cavallina, and Brembana. Other, smaller but important valleys include the Valle Imagna, the Val di Scalve, the Val Brembilla, the Val Serina, and the Val Taleggio. The southern part is mainly made up of flatlands.

Geographic entities mentioned:
surface_form: Val Taleggio
instance_of: Valley
countries: Italy
coordinates: lat: 45.8833
lon: 9.6
The southern part is mainly made up of flatlands. In the east, Lake Iseo forms its boundary which the Oglio from the Camonica Valley flows through. Minerals are found in the area of Trescore Balneario and San Pellegrino (the source of the mineral water of the same name) and other places. Economy.

Geographic entities mentioned:
surface_form: Lake Iseo
instance_of: Lake
countries: Italy
coordinates: lat: 45.711666666667
lon: 10.071944444444
Geography. Three Springs is in southern Huntingdon County, sitting at the base of the south end of Jacks Mountain. Spring Creek and North Spring Branch flow through the borough, joining just southeast of the borough limits to form Three Springs Creek, an east-flowing tributary of Aughwick Creek and part of the Juniata River watershed.

Geographic entities mentioned:
surface_form: Jacks Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.628611111111
lon: -77.631388888889
Pennsylvania Route 222. Pennsylvania Route 222 (PA 222) is a -long state highway located in Allentown and its surrounding suburbs in the Lehigh Valley region in eastern Pennsylvania. Most of the route runs along Hamilton Boulevard. In Center City Allentown, the route is aligned along West Hamilton, West Linden, and West Walnut Streets.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Route description. PA 222 begins at an interchange with I-78/PA 309 in Dorneyville in South Whitehall Township in Lehigh County, which is in the Lehigh Valley, where the road continues southwest as US 222 toward the city of Reading. From this interchange, PA 222 heads northeast on four-lane divided Hamilton Boulevard.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
After passing the amusement park, the route splits into two carriageways, with PA 222 north remaining on Hamilton Boulevard and PA 222 south following the newer Hamilton Boulevard Bypass to the north; at the split, there is a pair of median U-turn ramps. To the east, the road intersects Cedar Crest Boulevard, a major north&ndash;south arterial in the Lehigh Valley area.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Rosedale, Ontario. Rosedale is a Dispersed Rural Community and unincorporated place located in the city of Kawartha Lakes, Ontario, Canada, north-west of Lindsay. It is partly in geographic Fenelon Township and partly in Somerville Township, and is on the Rosedale River, part of the Trent–Severn Waterway, where that river drains Balsam Lake on its way to Cameron Lake.

Geographic entities mentioned:
surface_form: Rosedale River
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.570277777778
lon: -78.765833333333
At its north end the lake is drained by the Luvua River, which flows in a northwesterly direction to join the Lualaba River and thence to the Congo. It is the second-largest lake in the Congo's drainage basin and is located west of the southern end of the largest, Lake Tanganyika. The Luapula forms a swampy delta almost as wide as the southern end of the lake.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
Its elevation is, quite a bit higher than Tanganyika (). It is a rift valley lake lying in the Lake Mweru-Luapula graben, which is a branch of the East African Rift. The western shore of the lake in DR Congo exhibits the steep escarpment typical of a rift valley lake, rising to the Kundelungu Mountains beyond, but the rift valley escarpment is less pronounced on the eastern shore.

Geographic entities mentioned:
surface_form: rift valley lake
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
surface_form: mweru
instance_of: Lake
countries: Zambia
Democratic Republic of the Congo
coordinates: lat: -9.1666666666667
lon: 28.5
surface_form: lake mweru
instance_of: Lake
countries: Zambia
Democratic Republic of the Congo
coordinates: lat: -9.1666666666667
lon: 28.5
Mweru is shallow in the south and deeper in the north, with two depressions in the north-eastern section with maximum depths of. A smaller very marshy lake called Mweru Wantipa (also known as the Mweru Marshes) lies about to its east, and north of the Kalungwishi.

Geographic entities mentioned:
surface_form: Mweru Wantipa
instance_of: Lake
countries: Zambia
coordinates: lat: -8.7
lon: 29.7667
surface_form: mweru
instance_of: Lake
countries: Zambia
Democratic Republic of the Congo
coordinates: lat: -9.1666666666667
lon: 28.5
surface_form: mweru
instance_of: Lake
countries: Zambia
Democratic Republic of the Congo
coordinates: lat: -9.1666666666667
lon: 28.5
Lake Mweru. Lake Mweru (also spelled &quot;Mwelu&quot;, &quot;Mwero&quot;) (,) is a freshwater lake on the longest arm of Africa's second-longest river, the Congo. Located on the border between Zambia and Democratic Republic of the Congo, it makes up of the total length of the Congo, lying between its Luapula River (upstream) and Luvua River (downstream) segments.

Geographic entities mentioned:
surface_form: mweru
instance_of: Lake
countries: Zambia
Democratic Republic of the Congo
coordinates: lat: -9.1666666666667
lon: 28.5
surface_form: lake mweru
instance_of: Lake
countries: Zambia
Democratic Republic of the Congo
coordinates: lat: -9.1666666666667
lon: 28.5
Located on the border between Zambia and Democratic Republic of the Congo, it makes up of the total length of the Congo, lying between its Luapula River (upstream) and Luvua River (downstream) segments. Mweru means 'lake' in a number of Bantu languages, so it is often referred to as just 'Mweru'. Physical geography.

Geographic entities mentioned:
surface_form: mweru
instance_of: Lake
countries: Zambia
Democratic Republic of the Congo
coordinates: lat: -9.1666666666667
lon: 28.5