Sarmila/GeoWiki-Features huggingface dataset:
The section that runs just below the summit of Kuwohi (formerly Clingmans Dome) in Great Smoky Mountains National Park is the highest point on the trail at. The trail enters Tennessee from North Carolina atop Doe Knob and exits Tennessee into Virginia atop Holston Mountain. The first of the A.T. in Tennessee follow the crest of the Smokies, and are largely shared with North Carolina.

Geographic entities mentioned:
surface_form: Kuwohi
instance_of: Mountain
countries: United States
coordinates: lat: 35.562777777778
lon: -83.498611111111
The section that runs just below the summit of Kuwohi (formerly Clingmans Dome) in Great Smoky Mountains National Park is the highest point on the trail at. The trail enters Tennessee from North Carolina atop Doe Knob and exits Tennessee into Virginia atop Holston Mountain. The first of the A.T. in Tennessee follow the crest of the Smokies, and are largely shared with North Carolina.

Geographic entities mentioned:
surface_form: Holston Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.433333333333
lon: -82.133333333333
The first of the A.T. in Tennessee follow the crest of the Smokies, and are largely shared with North Carolina. In the western Smokies, the trail traverses a young forest that replaced what was once a large highland pasture, most noticeable in areas such as Spence Field, Thunderhead Mountain, and Silers Bald.

Geographic entities mentioned:
surface_form: Spence Field
instance_of: Landform
countries: United States
coordinates: lat: 35.5633
lon: -83.7328
surface_form: Thunderhead Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.568611111111
lon: -83.706388888889
surface_form: Silers Bald
instance_of: Mountain
countries: United States
coordinates: lat: 35.565830555556
lon: -83.565280555556
The trail crosses U.S. Route 441 at Newfound Gap and traverses a series of rocky cliffs known as &quot;The Sawteeth&quot; en route to the high ridges of the Eastern Smokies. Here, the trail crosses Mount Chapman and Mount Guyot, and passes one of its most remote shelters at Tricorner Knob before gradually descending. Just beyond Mount Cammerer, the A.T.

Geographic entities mentioned:
surface_form: Mount Chapman
instance_of: Mountain
countries: United States
coordinates: lat: 35.6867
lon: -83.2711
surface_form: Tricorner Knob
instance_of: Mountain
countries: United States
coordinates: lat: 35.695561111111
lon: -83.254169444444
Here, the trail crosses Mount Chapman and Mount Guyot, and passes one of its most remote shelters at Tricorner Knob before gradually descending. Just beyond Mount Cammerer, the A.T. exits the Smokies, crossing Interstate 40 into the Cherokee National Forest.

Geographic entities mentioned:
surface_form: Mount Cammerer
instance_of: Mountain
countries: United States
coordinates: lat: 35.7635495
lon: -83.1610915
Just beyond Mount Cammerer, the A.T. exits the Smokies, crossing Interstate 40 into the Cherokee National Forest. After traversing Snowbird Mountain, Max Patch Bald, and Lemon Gap (just south of Del Rio), the trail exits Tennessee atop Bluff Mountain and re-enters again atop Rich Mountain (in Greene County), some to the northeast.

Geographic entities mentioned:
surface_form: Max Patch
instance_of: Mountain
countries: United States
coordinates: lat: 35.797044444444
lon: -82.956811111111
At Watauga Lake at the TVA Watauga Dam, the trail turns northeast, crossing Iron Mountain before turning briefly to the northwest at the Carter County-Johnson County line. After passing over Cross Mountain, the trail again turns northeast and ascends Holston Mountain en route to Virginia. Virginia.

Geographic entities mentioned:
surface_form: Holston Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.433333333333
lon: -82.133333333333
The Appalachian Trail Conservancy considers to be excellent for beginning hikers a well-maintained section of the trail that the Civilian Conservation Corps constructed in Shenandoah National Park and whose climbs rarely exceed. McAfee Knob is affectionately known as &quot;the most photographed spot on the A.T.&quot;. McAfee Knob is part of what is known as Virginia's Triple Crown.

Geographic entities mentioned:
surface_form: McAfee Knob
instance_of: Mountain
countries: United States
coordinates: lat: 37.392777777778
lon: -80.036666666667
It is currently in PGF State Park and marked by a &quot;Midpoint&quot; sign. These areas in south central Pennsylvania are the northernmost portions of the Blue Ridge Mountains, which are geologically distinct from the Ridge and Valley section further north. The two parts are separated by the broad Cumberland Valley, where the trail has a change of scenery, crossing many farms and large highways.

Geographic entities mentioned:
surface_form: Cumberland Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.93
lon: -77.72
(The state's true highest point, on the shoulder of Mount Frissell at the Massachusetts line, lies about west of the AT, just east of the junction of those two states with New York. Such a side-trip is on the order of long and entails about 1,300 vertical feet (400 m) of climbing.)
Massachusetts. County crossed: Berkshire County
Massachusetts has of trail.

Geographic entities mentioned:
surface_form: Mount Frissell
instance_of: Mountain
countries: United States
coordinates: lat: 42.050555555556
lon: -73.482222222222
The A.T. climbs the highest peak in the southern Taconic Mountains, Mount Everett (), then descends to the Housatonic River Valley and skirts the towns of Egremont, Sheffield, and of Great Barrington. From there, it ascends into the Berkshires and passes through the towns of Tyringham, Dalton and Cheshire.

Geographic entities mentioned:
surface_form: Mount Everett
instance_of: Mountain
countries: United States
coordinates: lat: 42.1019
lon: -73.4325
From there, it ascends into the Berkshires and passes through the towns of Tyringham, Dalton and Cheshire. It ascends into the Taconic Mountains again, visiting Mount Greylock, the highest point in the state at. It then quickly descends to the valley of the Hoosic River within of North Adams and Williamstown, before ascending again to the Vermont state line.

Geographic entities mentioned:
surface_form: Mount Greylock
instance_of: Mountain
countries: United States
coordinates: lat: 42.6375
lon: -73.166666666667
It follows the ridge of the southern Green Mountains, summiting such notable peaks as Stratton Mountain, Glastenbury Mountain and Killington Peak. The trail traverses the Glastenbury, Lye Brook, and Peru Peak Wilderness areas of the Green Mountain National Forest.

Geographic entities mentioned:
surface_form: Glastenbury Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.978133333333
lon: -73.071216666667
surface_form: Killington Peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.604444444444
lon: -72.82
The AT then turns in a more eastward direction, crossing the White River, passing through Norwich, and entering Hanover, New Hampshire, as it crosses the Connecticut River. The Green Mountain Club maintains the entire portion of the AT in Vermont. The NPS challenged Killington and Pico ski resorts in Vermont over development of private land that crossed the AT. New Hampshire.

Geographic entities mentioned:
surface_form: Pico
instance_of: Mountain
countries: United States
coordinates: lat: 43.639333333333
lon: -72.836333333333
The New Hampshire AT is nearly all within the White Mountain National Forest. The easier southern portion of the trail, from Hanover to Glencliff, passes over Velvet Rocks, Moose Mountain, Smarts Mountain, and Mount Cube. It then ascends Mount Moosilauke and enters the high peaks region of the White Mountains.

Geographic entities mentioned:
surface_form: Smarts Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.825666666667
lon: -72.038666666667
The New Hampshire AT is nearly all within the White Mountain National Forest. The easier southern portion of the trail, from Hanover to Glencliff, passes over Velvet Rocks, Moose Mountain, Smarts Mountain, and Mount Cube. It then ascends Mount Moosilauke and enters the high peaks region of the White Mountains.

Geographic entities mentioned:
surface_form: Mount Moosilauke
instance_of: Mountain
countries: United States
coordinates: lat: 44.024511111111
lon: -71.830916666667
In the Presidential Range of the White Mountains, the trail runs completely above treeline from the summit of Mount Pierce to the north side of the cone of Mount Madison, a distance of about.

Geographic entities mentioned:
surface_form: Mount Madison
instance_of: Mountain
countries: United States
coordinates: lat: 44.328333333333
lon: -71.278333333333
The AT passes over the summits of 15 of the 48 four-thousand footers of New Hampshire: Moosilauke, South and North Kinsman, Lincoln, Lafayette, South Twin, Jackson, Pierce, Washington (the highest point of the AT north of Tennessee), Madison, Wildcats D and A, Carter Dome, South and Middle Carter.

Geographic entities mentioned:
surface_form: Moosilauke
instance_of: Mountain
countries: United States
coordinates: lat: 44.024511111111
lon: -71.830916666667
surface_form: South and North Kinsman
instance_of: Mountain
countries: United States
coordinates: lat: 44.123
lon: -71.7367
surface_form: Lafayette
instance_of: Mountain
countries: United States
coordinates: lat: 44.160705555556
lon: -71.644361111111
surface_form: Carter Dome
instance_of: Mountain
countries: United States
coordinates: lat: 44.266944444444
lon: -71.178888888889
surface_form: South
instance_of: Mountain
countries: United States
coordinates: lat: 44.289722222222
lon: -71.176111111111
surface_form: Middle Carter
instance_of: Mountain
countries: United States
coordinates: lat: 44.303119444444
lon: -71.167297222222
It comes close to the summits of 9 other of the 48 four-thousand footers: Liberty, Garfield (60 yards away over ledges), Galehead, Zealand, Eisenhower, Monroe, Jefferson, Adams, and Moriah. A series of comfortable huts are maintained along parts of the NH trail by the Appalachian Mountain Club.

Geographic entities mentioned:
surface_form: Galehead
instance_of: Mountain
countries: United States
coordinates: lat: 44.185
lon: -71.5735
surface_form: Zealand
instance_of: Mountain
countries: United States
coordinates: lat: 44.1797
lon: -71.5213
surface_form: Eisenhower
instance_of: Mountain
countries: United States
coordinates: lat: 44.240666666667
lon: -71.350333333333
surface_form: Monroe
instance_of: Mountain
countries: United States
coordinates: lat: 44.255561111111
lon: -71.3225
There he was sold a third time to the Qazi al-Qudat of Mecca and then to Mir Qasim al-Baghdadi. Qasim converted Chapu to Islam from his traditional religion, educated him, and gave him the name Ambar, after recognizing his superior intellectual qualities. He eventually took Ambar to the Deccan Plateau.

Geographic entities mentioned:
surface_form: Deccan Plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Fully natural places below sea level require a dry climate; otherwise, rain would exceed evaporation and fill the area. Historic and ice-covered areas. Deeper and larger than any of the trenches in the list above is the Bentley Subglacial Trench in Antarctica, at a depth of. It is subglacial, covered permanently by the largest glacier in the world.

Geographic entities mentioned:
surface_form: Bentley Subglacial Trench
instance_of: Valley
coordinates: lat: -80
lon: -115
Kunar Valley. Kunar Valley is a valley in Afghanistan and Pakistan. In Afghanistan the length of the valley is almost entirely narrow with steep and rugged mountains on both sides. The center of the valley is occupied by the Kunar River flowing south where it joins the Kabul River.

Geographic entities mentioned:
surface_form: kunar valley
instance_of: Valley
countries: Pakistan
Afghanistan
There are limited and small forested areas in some side valleys but more than 95% of the valley has been deforested. In limited areas at higher elevations there are sustained grassy mountain meadows. Overwhelmingly though the Kunar Valley is an arid, rocky, steep landscape with a fast-moving muddy river as its primary geographic feature.

Geographic entities mentioned:
surface_form: kunar valley
instance_of: Valley
countries: Pakistan
Afghanistan
The Ancestral Puebloans lived in a range of structures that included small family pit houses, larger structures to house clans, grand pueblos, and cliff-sited dwellings for defense. They had a complex network linking hundreds of communities and population centers across the Colorado Plateau. They held a distinct knowledge of celestial sciences that found form in their architecture.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
Domesticated turkeys appeared. After around 1130, North America had significant climatic change in the form of a 300-year period of aridity called the Great Drought. This also led to the collapse of the Tiwanaku civilization around Lake Titicaca in present-day Bolivia. The contemporary Mississippian culture also collapsed during this period.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
Lake Lavine (Michigan). Lake Lavine is a small lake, in south central Michigan. Located in Kinderhook Township, Branch County, Michigan approximately from Kinderhook, Lake Lavine is situated approximately north of the Indiana state line: directly north of the Lake James chain of lakes located in Indiana. Lake Lavine is a deep lake (84 feet maximum) with steep drop-offs.

Geographic entities mentioned:
surface_form: lake james
instance_of: Lake
countries: United States
coordinates: lat: 41.7
lon: -85.03888889
surface_form: michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: lake lavine
instance_of: Lake
countries: United States
coordinates: lat: 41.768055555556
lon: -85.0375
surface_form: lake james
instance_of: Lake
countries: United States
coordinates: lat: 35.7478
lon: -81.8785
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
Located in Kinderhook Township, Branch County, Michigan approximately from Kinderhook, Lake Lavine is situated approximately north of the Indiana state line: directly north of the Lake James chain of lakes located in Indiana. Lake Lavine is a deep lake (84 feet maximum) with steep drop-offs. Speed boats are allowed during the hours of 10:00 am until 6:30 pm.

Geographic entities mentioned:
surface_form: deep lake
instance_of: Lake
countries: United States
coordinates: lat: 46.9075
lon: -122.9125
surface_form: deep lake
instance_of: Lake
countries: United States
coordinates: lat: 41.5699
lon: -123.113
surface_form: deep lake
instance_of: Lake
countries: United States
coordinates: lat: 26.0506
lon: -81.3425
surface_form: lake lavine
instance_of: Lake
countries: United States
coordinates: lat: 41.768055555556
lon: -85.0375
surface_form: deep lake
instance_of: Lake
countries: United States
coordinates: lat: 39.773
lon: -107.3
Lake Lavine (Michigan). Lake Lavine is a small lake, in south central Michigan. Located in Kinderhook Township, Branch County, Michigan approximately from Kinderhook, Lake Lavine is situated approximately north of the Indiana state line: directly north of the Lake James chain of lakes located in Indiana. Lake Lavine is a deep lake (84 feet maximum) with steep drop-offs.

Geographic entities mentioned:
surface_form: michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: lake lavine (michigan)
instance_of: Lake
countries: United States
coordinates: lat: 41.768055555556
lon: -85.0375
Lake Lavine (Michigan). Lake Lavine is a small lake, in south central Michigan. Located in Kinderhook Township, Branch County, Michigan approximately from Kinderhook, Lake Lavine is situated approximately north of the Indiana state line: directly north of the Lake James chain of lakes located in Indiana. Lake Lavine is a deep lake (84 feet maximum) with steep drop-offs.

Geographic entities mentioned:
surface_form: michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: lake lavine
instance_of: Lake
countries: United States
coordinates: lat: 41.768055555556
lon: -85.0375
The lake is primarily groundwater seepage fed, without any significant inlet and no outlet. Lake Lavine is within the headwaters of the Prairie River watershed. The Prairie River (Michigan) flows westerly, joining the St. Joseph River just south of the community of Three Rivers. Almost half of the lakeshore is privately owned wetlands with no immediate plans for development.

Geographic entities mentioned:
surface_form: michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Speed boats are allowed during the hours of 10:00 am until 6:30 pm. On the southeastern shore there is a state-operated public fishing site with a paved boat ramp. The terrain surrounding Lake Lavine is gently rolling woodlands, wetlands, farm fields, and vineyards. Approximately half of the shoreline is developed, with about 60 summer and permanent homes on the lake.

Geographic entities mentioned:
surface_form: lake lavine
instance_of: Lake
countries: United States
coordinates: lat: 41.768055555556
lon: -85.0375
The remaining shoreline is wetlands and undeveloped woodland. The lake is primarily groundwater seepage fed, without any significant inlet and no outlet. Lake Lavine is within the headwaters of the Prairie River watershed. The Prairie River (Michigan) flows westerly, joining the St. Joseph River just south of the community of Three Rivers.

Geographic entities mentioned:
surface_form: lake lavine
instance_of: Lake
countries: United States
coordinates: lat: 41.768055555556
lon: -85.0375
The Prairie River (Michigan) flows westerly, joining the St. Joseph River just south of the community of Three Rivers. Almost half of the lakeshore is privately owned wetlands with no immediate plans for development. Known for its exceptional fishing, Lake Lavine holds significant numbers of perch, bass, bluegill and crappie. It was formally stocked by MDNR with rainbow trout.

Geographic entities mentioned:
surface_form: lake lavine
instance_of: Lake
countries: United States
coordinates: lat: 41.768055555556
lon: -85.0375
Geography. Referred to before 1924 as West Elizabeth Lake, Lake Hughes is one of a series of sag ponds in the foothills of the Sierra Pelona Mountains, including Elizabeth Lake, and Munz Lakes, all created by the active motion of tectonic plates on the San Andreas Fault. They are part of the northern upper Santa Clara River watershed.

Geographic entities mentioned:
surface_form: Munz Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 34.672763888889
lon: -118.43230277778
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 34.6658
lon: -118.403
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 34.6658
lon: -118.403
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 42.630489
lon: -83.380641
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 42.630489
lon: -83.380641
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 48.886
lon: -113.726
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 48.886
lon: -113.726
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 42.50822
lon: -88.26902
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 42.50822
lon: -88.26902
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 37.845012
lon: -119.370406
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 37.845012
lon: -119.370406
Hughes Lake (California). Hughes Lake is a sag pond on the San Andreas Fault in the northern Sierra Pelona Mountains, in Los Angeles County, California. At times the lake goes completely dry for years, as its water supply depends on local winter rain and snowmelt. Neighboring Elizabeth Lake also has a history of going dry and refilling. Geography.

Geographic entities mentioned:
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 34.6658
lon: -118.403
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 42.630489
lon: -83.380641
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 48.886
lon: -113.726
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 42.50822
lon: -88.26902
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 37.845012
lon: -119.370406
Hughes Lake (California). Hughes Lake is a sag pond on the San Andreas Fault in the northern Sierra Pelona Mountains, in Los Angeles County, California. At times the lake goes completely dry for years, as its water supply depends on local winter rain and snowmelt. Neighboring Elizabeth Lake also has a history of going dry and refilling. Geography.

Geographic entities mentioned:
surface_form: hughes lake (california)
instance_of: Lake
countries: United States
coordinates: lat: 34.6758
lon: -118.446
Hughes Lake (California). Hughes Lake is a sag pond on the San Andreas Fault in the northern Sierra Pelona Mountains, in Los Angeles County, California. At times the lake goes completely dry for years, as its water supply depends on local winter rain and snowmelt. Neighboring Elizabeth Lake also has a history of going dry and refilling. Geography.

Geographic entities mentioned:
surface_form: hughes lake
instance_of: Lake
countries: United States
coordinates: lat: 34.6758
lon: -118.446
Writing process. Xu Xiake traveled 22 years after he married in 1607 until his death in 1640. He reached all 16 provinces of China. He traveled to Jinling (Nanjing) in 1611, visited Mount Huangshan, Wuyishan, Baiyue Nine-Bend stream, and West Lake in 1616. He went to Songshan, Huashan, Tai Shan, and Wudang Mountains. He traveled to Luoyang during 1625–1627 and Fujian in 1628.

Geographic entities mentioned:
surface_form: West Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 30.2375
lon: 120.14083333333
He reached all 16 provinces of China. He traveled to Jinling (Nanjing) in 1611, visited Mount Huangshan, Wuyishan, Baiyue Nine-Bend stream, and West Lake in 1616. He went to Songshan, Huashan, Tai Shan, and Wudang Mountains. He traveled to Luoyang during 1625–1627 and Fujian in 1628. During 1636–1640, he was away from his home. Description. &quot;Xu Xiake's Travels&quot; has 22 sections.

Geographic entities mentioned:
surface_form: Songshan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 34.484722222222
lon: 112.96027777778
surface_form: Tai Shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 36.266666666667
lon: 117.1
Crystal Lake (Henderson, Jefferson County, New York). Crystal Lake, also known as Sixtown Pond, is located near Butterville, New York. Fish species present in the lake are largemouth bass, walleye, northern pike, and yellow perch. There is a state owned carry down on Route 178, four miles east of Henderson. There is a 10 horsepower motor limit on Crystal Lake.

Geographic entities mentioned:
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 42.9511
lon: -71.4083
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 42.051666666667
lon: -75.360833333333
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 26.049722222222
lon: -80.193055555556
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 44.7227
lon: -93.2667
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 43.64416
lon: -98.56947
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 42.621645
lon: -83.303091
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 44.2745524
lon: -75.7991552
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 28.1603
lon: -81.6415
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 42.3272
lon: -71.2003
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4433
lon: -71.3114
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 41.163055555556
lon: -81.465277777778
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 28.02622
lon: -81.90986
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 44.661644
lon: -86.172576
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 43.829166666667
lon: -76.126944444444
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 27.952
lon: -81.6823
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 47.62777778
lon: -96.10277778
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 43.6006
lon: -72.0889
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 44.33361111
lon: -93.2125
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 46.615
lon: -95.950555555556
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 46.002
lon: -89.613
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 42.650347
lon: -75.201606
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 46.7998926
lon: -109.5141115
Crystal Lake (Henderson, Jefferson County, New York). Crystal Lake, also known as Sixtown Pond, is located near Butterville, New York. Fish species present in the lake are largemouth bass, walleye, northern pike, and yellow perch. There is a state owned carry down on Route 178, four miles east of Henderson. There is a 10 horsepower motor limit on Crystal Lake.

Geographic entities mentioned:
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 42.9511
lon: -71.4083
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 42.051666666667
lon: -75.360833333333
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 26.049722222222
lon: -80.193055555556
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 44.7227
lon: -93.2667
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 43.64416
lon: -98.56947
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 42.621645
lon: -83.303091
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 44.2745524
lon: -75.7991552
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 28.1603
lon: -81.6415
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 42.3272
lon: -71.2003
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4433
lon: -71.3114
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 41.163055555556
lon: -81.465277777778
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 28.02622
lon: -81.90986
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 44.661644
lon: -86.172576
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 43.829166666667
lon: -76.126944444444
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 27.952
lon: -81.6823
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 47.62777778
lon: -96.10277778
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 43.6006
lon: -72.0889
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 44.33361111
lon: -93.2125
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 46.615
lon: -95.950555555556
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 46.002
lon: -89.613
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 42.650347
lon: -75.201606
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 46.7998926
lon: -109.5141115
He graduated with a degree in law in 1880. From 1881, he worked as an attorney with the magistrate judge's office in Numedal and Sandsvær, and later for the Ministry of the Interior and at the Akershus County Office under County Governor Johan Christian Collett. He worked as a court prosecutor in Akershus county in 1889, and then worked as a prosecutor in Follo and Drøbak in 1890.

Geographic entities mentioned:
surface_form: Numedal
instance_of: Valley
countries: Norway
coordinates: lat: 60
lon: 9.2
Munn Lake. Munn Lake is a lake in the U.S. state of Washington. The Olympia Regional Airport lies to the southwest of the lake and the community of Bush is situated to the south. Two other bodies of water in the surrounding area, Susan Lake and Trails End Lake, are in near proximity to Munn Lake. The lake has a surface area of approximately and reaches a depth of.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: munn lake
instance_of: Lake
countries: United States
coordinates: lat: 46.985
lon: -122.87944444444
Munn Lake. Munn Lake is a lake in the U.S. state of Washington. The Olympia Regional Airport lies to the southwest of the lake and the community of Bush is situated to the south. Two other bodies of water in the surrounding area, Susan Lake and Trails End Lake, are in near proximity to Munn Lake. The lake has a surface area of approximately and reaches a depth of.

Geographic entities mentioned:
surface_form: munn lake
instance_of: Lake
countries: United States
coordinates: lat: 46.985
lon: -122.87944444444
Two other bodies of water in the surrounding area, Susan Lake and Trails End Lake, are in near proximity to Munn Lake. The lake has a surface area of approximately and reaches a depth of. Munn Lake was named after Edwin Munn, a dairy farmer who operated in the area in the early 20th century.

Geographic entities mentioned:
surface_form: munn lake
instance_of: Lake
countries: United States
coordinates: lat: 46.985
lon: -122.87944444444
It is situated nine miles northwest of Grand Canyon Village, and immediately northeast of Mescalero Point. Pollux Temple is one mile northwest, Marsh Butte one mile east-northeast, and Vesta Temple is one mile south. Topographic relief is significant as Diana Temple rises nearly above the Colorado River in less than two miles.

Geographic entities mentioned:
surface_form: Pollux Temple
instance_of: Mountain
countries: United States
coordinates: lat: 36.12054
lon: -112.30267
surface_form: Marsh Butte
instance_of: Mountain
countries: United States
coordinates: lat: 36.12054
lon: -112.24517
surface_form: Vesta Temple
instance_of: Mountain
countries: United States
coordinates: lat: 36.09359
lon: -112.26878
Diana Temple (Grand Canyon). Diana Temple is a summit located in the Grand Canyon, in Coconino County of northern Arizona, US. It is situated nine miles northwest of Grand Canyon Village, and immediately northeast of Mescalero Point. Pollux Temple is one mile northwest, Marsh Butte one mile east-northeast, and Vesta Temple is one mile south.

Geographic entities mentioned:
surface_form: grand canyon
instance_of: Valley
countries: United States
coordinates: lat: 38.65888889
lon: -91.10388889
surface_form: diana temple (grand canyon)
instance_of: Landform
countries: United States
coordinates: lat: 36.1119
lon: -112.2738
Diana Temple (Grand Canyon). Diana Temple is a summit located in the Grand Canyon, in Coconino County of northern Arizona, US. It is situated nine miles northwest of Grand Canyon Village, and immediately northeast of Mescalero Point. Pollux Temple is one mile northwest, Marsh Butte one mile east-northeast, and Vesta Temple is one mile south.

Geographic entities mentioned:
surface_form: grand canyon
instance_of: Valley
countries: United States
coordinates: lat: 38.65888889
lon: -91.10388889
surface_form: diana temple
instance_of: Landform
countries: United States
coordinates: lat: 36.1119
lon: -112.2738
Diana Temple (Grand Canyon). Diana Temple is a summit located in the Grand Canyon, in Coconino County of northern Arizona, US. It is situated nine miles northwest of Grand Canyon Village, and immediately northeast of Mescalero Point. Pollux Temple is one mile northwest, Marsh Butte one mile east-northeast, and Vesta Temple is one mile south.

Geographic entities mentioned:
surface_form: grand canyon
instance_of: Valley
countries: United States
coordinates: lat: 38.65888889
lon: -91.10388889
Topographic relief is significant as Diana Temple rises nearly above the Colorado River in less than two miles. Diana Temple is named for Diana, the goddess of the hunt and the moon according to Roman mythology. Clarence Dutton began the practice of naming geographical features in the Grand Canyon after mythological deities. The U.S.

Geographic entities mentioned:
surface_form: grand canyon
instance_of: Valley
countries: United States
coordinates: lat: 38.65888889
lon: -91.10388889
surface_form: dutton
instance_of: Mountain
countries: United States
coordinates: lat: 55.168
lon: -162.272
According to the Köppen climate classification system, Diana Temple is located in a Cold semi-arid climate zone. Geology. The forested top of Diana Temple is composed of Permian Kaibab Limestone overlaying cream-colored, cliff-forming, Permian Coconino Sandstone. The sandstone, which is the third-youngest of the strata in the Grand Canyon, was deposited 265 million years ago as sand dunes.

Geographic entities mentioned:
surface_form: grand canyon
instance_of: Valley
countries: United States
coordinates: lat: 38.65888889
lon: -91.10388889
Pollux Temple is one mile northwest, Marsh Butte one mile east-northeast, and Vesta Temple is one mile south. Topographic relief is significant as Diana Temple rises nearly above the Colorado River in less than two miles. Diana Temple is named for Diana, the goddess of the hunt and the moon according to Roman mythology.

Geographic entities mentioned:
surface_form: diana temple
instance_of: Landform
countries: United States
coordinates: lat: 36.1119
lon: -112.2738
Topographic relief is significant as Diana Temple rises nearly above the Colorado River in less than two miles. Diana Temple is named for Diana, the goddess of the hunt and the moon according to Roman mythology. Clarence Dutton began the practice of naming geographical features in the Grand Canyon after mythological deities. The U.S.

Geographic entities mentioned:
surface_form: diana temple
instance_of: Landform
countries: United States
coordinates: lat: 36.1119
lon: -112.2738
Board on Geographic Names. In the early 1900s this mesa was sometimes called &quot;No Mans Land&quot;. According to the Köppen climate classification system, Diana Temple is located in a Cold semi-arid climate zone. Geology. The forested top of Diana Temple is composed of Permian Kaibab Limestone overlaying cream-colored, cliff-forming, Permian Coconino Sandstone.

Geographic entities mentioned:
surface_form: diana temple
instance_of: Landform
countries: United States
coordinates: lat: 36.1119
lon: -112.2738
According to the Köppen climate classification system, Diana Temple is located in a Cold semi-arid climate zone. Geology. The forested top of Diana Temple is composed of Permian Kaibab Limestone overlaying cream-colored, cliff-forming, Permian Coconino Sandstone. The sandstone, which is the third-youngest of the strata in the Grand Canyon, was deposited 265 million years ago as sand dunes.

Geographic entities mentioned:
surface_form: diana temple
instance_of: Landform
countries: United States
coordinates: lat: 36.1119
lon: -112.2738
Further down are strata of the conspicuous cliff-forming Mississippian Redwall Limestone, the Cambrian Tonto Group, and finally granite of the Paleoproterozoic Vishnu Basement Rocks at river level in Granite Gorge. Precipitation runoff from Diana Temple drains east to the Colorado River via Slate Creek on the north side of the mesa, and Topaz Canyon on the south side.

Geographic entities mentioned:
surface_form: diana temple
instance_of: Landform
countries: United States
coordinates: lat: 36.1119
lon: -112.2738
The name is modified from a Lenape (Delaware) Native American word meaning &quot;broad bottom lands&quot;. Wyoming County was formed from Genesee County in 1841. Wyoming County is one of New York's mostly agricultural counties. With an estimated 47,500 dairy cows in the county, there are more cattle in Wyoming County than people. The county is part of the Finger Lakes region of the state. History.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
Geommasan. Geommasan () is a mountain of North Gyeongsang Province, eastern South Korea. It has an elevation of.

Geographic entities mentioned:
surface_form: geommasan
instance_of: Mountain
countries: South Korea
Gräbersberg. The Gräbersberg, at, the highest point in the western Westerwald, a low mountain range in central Germany whose western region extends from the Nister river in the east to the Rhine in the west. On the slopes of the Gräbersberg lies the village of Alpenrod, part of the collective municipality of Hachenburg.

Geographic entities mentioned:
surface_form: gräbersberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.6253
lon: 7.85083
South of the hill is the protected area of the Westerwald Lake District and village of Lochum. Viewing tower. In 1998, a 73-metre-high viewing tower, the Gräbersberg Tower, was erected at the summit by mobile telephone operator, E-Plus. At 33 metres above the ground there is a viewing platform which is 8.5 metres in diameter.

Geographic entities mentioned:
surface_form: gräbersberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.6253
lon: 7.85083
Charles Mound. Charles Mound is a gentle, high hill located in Scales Mound Township, Jo Daviess County, Illinois, United States. It is northeast of the small town of Scales Mound, and northeast of Galena. Despite its name, Charles Mound is a naturally occurring, erosional feature and is not to be confused with the intentional mounds created by native cultures.

Geographic entities mentioned:
surface_form: charles mound
instance_of: Mountain
countries: United States
coordinates: lat: 42.50416666666667
lon: -90.23972222222223
Charles Mound. Charles Mound is a gentle, high hill located in Scales Mound Township, Jo Daviess County, Illinois, United States. It is northeast of the small town of Scales Mound, and northeast of Galena. Despite its name, Charles Mound is a naturally occurring, erosional feature and is not to be confused with the intentional mounds created by native cultures.

Geographic entities mentioned:
surface_form: charles mound
instance_of: Mountain
countries: United States
coordinates: lat: 42.50416666666667
lon: -90.23972222222223
surface_form: high hill
instance_of: Landform
countries: United States
coordinates: lat: 30.7314
lon: -85.4853
It is northeast of the small town of Scales Mound, and northeast of Galena. Despite its name, Charles Mound is a naturally occurring, erosional feature and is not to be confused with the intentional mounds created by native cultures. It is the highest natural point in the state and is thus considered a state highpoint. It is the lowest state highpoint in the Midwestern region of the United States.

Geographic entities mentioned:
surface_form: charles mound
instance_of: Mountain
countries: United States
coordinates: lat: 42.50416666666667
lon: -90.23972222222223
It is the highest natural point in the state and is thus considered a state highpoint. It is the lowest state highpoint in the Midwestern region of the United States. Geography. Charles Mound is the highest natural point in Illinois. (The highest point is the Willis Tower, formerly known as the Sears Tower.) The top of the hill is about from the Wisconsin border.

Geographic entities mentioned:
surface_form: charles mound
instance_of: Mountain
countries: United States
coordinates: lat: 42.50416666666667
lon: -90.23972222222223
Geology. As mapped in the early 1960's by Mullens, Charles Mound is an outlier and erosional remnant of Silurian Edgewood Dolomite overlying strata of the Ordovician Maquoketa Formation. The Maquoketa Formation consists of dark-gray clayey siltstone and silty dolomite that occurs in beds that are to thick.

Geographic entities mentioned:
surface_form: charles mound
instance_of: Mountain
countries: United States
coordinates: lat: 42.50416666666667
lon: -90.23972222222223
Within the Formation, layers of dark grayish-orange silty dolomite that are up to thick separate the beds of siltstone and silty dolomite. A prominent grayish-orange and grayish-yellow granular dolomite bed that ranges from in thickness, which contains abundant fossil bryozoa fragments, locally outcrops near Charles Mound.

Geographic entities mentioned:
surface_form: charles mound
instance_of: Mountain
countries: United States
coordinates: lat: 42.50416666666667
lon: -90.23972222222223
A prominent grayish-orange and grayish-yellow granular dolomite bed that ranges from in thickness, which contains abundant fossil bryozoa fragments, locally outcrops near Charles Mound. The Edgewood Dolomite is unconformably overlying, and in erosional contact with, the Maquoketa Formation. The maximum thickness of Edgewood Dolomite preserved beneath Charles Mound is about.

Geographic entities mentioned:
surface_form: charles mound
instance_of: Mountain
countries: United States
coordinates: lat: 42.50416666666667
lon: -90.23972222222223
The maximum thickness of Edgewood Dolomite preserved beneath Charles Mound is about. The Edgewood Dolomite outcrops at the northwest and southeast ends of Charles Mound, and there presents as thin beds of grayish-orange and olive-gray medium-grained dolomite that contains light-gray chert nodules. The chert nodules are irregular in shape, thick and as much as long.

Geographic entities mentioned:
surface_form: charles mound
instance_of: Mountain
countries: United States
coordinates: lat: 42.50416666666667
lon: -90.23972222222223
The Edgewood Dolomite outcrops at the northwest and southeast ends of Charles Mound, and there presents as thin beds of grayish-orange and olive-gray medium-grained dolomite that contains light-gray chert nodules. The chert nodules are irregular in shape, thick and as much as long. Just southwest of Charles Mound is an abandoned prospecting shaft for lead-zinc ore. Settlement.

Geographic entities mentioned:
surface_form: charles mound
instance_of: Mountain
countries: United States
coordinates: lat: 42.50416666666667
lon: -90.23972222222223
Settlement. Elijah Charles, one of the region's first permanent settlers, arrived in 1828 and settled at the base of the mound and the hill assumed his name. Access. Charles Mound is located on rolling farmland that is privately owned. The landowners allow public access on the first full weekends of the months of June, July, August, and September as well as President's Day Weekend in February.

Geographic entities mentioned:
surface_form: charles mound
instance_of: Mountain
countries: United States
coordinates: lat: 42.50416666666667
lon: -90.23972222222223
The landowners allow public access on the first full weekends of the months of June, July, August, and September as well as President's Day Weekend in February. Public access to the property is at 688 West Charles Mound Road, where there is a gate and access to the highpoint by foot. Visitors should park along the road and not block access to the gate.

Geographic entities mentioned:
surface_form: charles mound
instance_of: Mountain
countries: United States
coordinates: lat: 42.50416666666667
lon: -90.23972222222223
Chivay. Chivay is a town in the Colca valley, capital of the Caylloma province in the Arequipa region, Peru. Located at about 3,600 m above sea level (12,000 ft), it lies upstream of the renowned Colca Canyon. It has a central town square and an active market. Ten km to the east, and 1,500 metres above the town of Chivay lies the Chivay obsidian source.

Geographic entities mentioned:
surface_form: Colca Canyon
instance_of: Valley
countries: Peru
coordinates: lat: -15.5972
lon: -72.0559
He was part of the literary circle that included Jenkin Morgan Edwards and Edward Prosser Rhys. He is mostly known for his cywydd &quot;Rhos Helyg&quot; (&quot;Moor Willows&quot;), which extols the agrarian life and Welsh culture of his region. There is a memorial to him and the other three poets of Mynydd Bach near Llyn Eiddwen.

Geographic entities mentioned:
surface_form: Llyn Eiddwen
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.283
lon: -4.044
The use of dragon boats for racing and dragon ceremonies is believed by scholars, sinologists, and anthropologists to have originated in southern central China more than 2500 years ago, in Dongting Lake and along the banks of the Chang Jiang (now called the Yangtze) during the same era when the games of ancient Greece were being established at Olympia.

Geographic entities mentioned:
surface_form: Dongting Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 29.316666666667
lon: 112.95
Filming. Principal photography began on May 17, 1993, and wrapped three months later, on August 20. Parts of the film were shot at Glen Canyon in Utah as well as Los Angeles County, California. Sets that resembled a complete street from Bedrock were constructed adjacent to Vasquez Rocks in California. Before they were totally demolished, visitors could tour the location.

Geographic entities mentioned:
surface_form: Glen Canyon
instance_of: Valley
countries: United States
coordinates: lat: 36.86443
lon: -111.58794
Brookeborough. Brookeborough (; Irish: &quot;Achadh Lon&quot;, meaning 'Field of the Blackbirds') is a village in County Fermanagh, Northern Ireland, at the westerly foot of Slieve Beagh. It lies about eleven miles east of Enniskillen, just off the A4 trunk road, and about five miles west of the County Tyrone boundary.

Geographic entities mentioned:
surface_form: Slieve Beagh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.319
lon: -7.253
Having explored Navarino, Methoni and Koroni, the members of the section went to the ancient city of Messene (founded in 369 BC by the Theban general Epaminondas after his victory over Sparta at Leuctra), located on the slopes of Mounts Ithome and Eva. They spent a full month there from April 10, 1829, where they were warmly welcomed by the inhabitants of the village of Mavrommati.

Geographic entities mentioned:
surface_form: Ithome
instance_of: Mountain
countries: Greece
coordinates: lat: 37.186111111111
lon: 21.925
Blouet, in his, gave very precise descriptions of the churches he saw, especially those of Navarino (Church of the Transfiguration of the Savior, inside the new fortress Néokastro), Osphino (destroyed village which no longer exists), Modon (Church of Saint Basil), Androusa (Church of St.

Geographic entities mentioned:
surface_form: Vourkano
instance_of: Mountain
countries: Greece
coordinates: lat: 37.186111111111
lon: 21.925