Sarmila/GeoWiki-Features huggingface dataset:
Noel V. Ginnity. Noel V. Ginnity is an Irish stand-up comedian and former hairdresser. He has been described as Ireland's last vaudeville star. As a cabaret performer, he has long been associated with Taylor's pub in Three Rock Mountain in south county Dublin. As a comedy writer his material has been used by comedians such as Brendan Grace. Ginnity was the victim of a tiger kidnapping in 1994.

Geographic entities mentioned:
surface_form: Three Rock Mountain
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.245277777778
lon: -6.2391666666667
Bodom (film). &quot;Bodom&quot; (internationally &quot;Lake Bodom&quot;) is a 2016 Finnish slasher film directed by Taneli Mustonen. It is inspired by, but not based upon, the 1960 Lake Bodom murders, telling the story of a group of Finnish friends who decide to go camping by Lake Bodom to reconstruct the 1960 murders, but something goes wrong.

Geographic entities mentioned:
surface_form: Lake Bodom
instance_of: Lake
countries: Finland
coordinates: lat: 60.256388888889
lon: 24.666666666667
Plot. A group of friends, Nora, Elias, Atte and Ida, go to Lake Bodom to camp and reconstruct the 1960 murders there. Ida has been rejected at school for her nude pictures. Her fascination with Elias is because he is accused of taking the pictures. At night at Bodom, with Ida and Atte in the tent, someone grabs them through the tent. Atte goes out, and a mysterious figure stabs him.

Geographic entities mentioned:
surface_form: Lake Bodom
instance_of: Lake
countries: Finland
coordinates: lat: 60.256388888889
lon: 24.666666666667
Doi Ang Khang. Doi Ang Khang () is a mountain in Fang District, Chiang Mai Province, Thailand. It is part of the Daen Lao Range that straddles both sides of the Burmese-Thai border. It is the site of an agricultural station, the first research station set up by King Bhumibol Adulyadej in 1969.

Geographic entities mentioned:
surface_form: doi ang khang
instance_of: Mountain
countries: Thailand
coordinates: lat: 19.9003
lon: 99.0393
It is part of the Daen Lao Range that straddles both sides of the Burmese-Thai border. It is the site of an agricultural station, the first research station set up by King Bhumibol Adulyadej in 1969. The peak of Doi Ang Khang is above sea level, and the agricultural station covers an area of 1,989 &quot;rai&quot; (318 ha). Climate. The temperature average is 19.6 °C.

Geographic entities mentioned:
surface_form: doi ang khang
instance_of: Mountain
countries: Thailand
coordinates: lat: 19.9003
lon: 99.0393
Location and Regional Context. The valley is centered at in the northeastern Aeolis quadrangle of Mars and drains approximately of the northern rim of Gale Crater. While the stream was active, surface water and groundwater drained to the south into a low-lying plain in the northern interior of the crater (Aeolis Palus) where the stream valley debouched into a large alluvial fan (Peace Vallis fan).

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
surface_form: peace vallis
instance_of: Valley
coordinates: lat: -4.21
lon: 137.23
Gale Crater itself is a -diameter impact crater that straddles the martian hemispheric dichotomy between the heavily cratered southern highlands and the lower elevation plains (Elysium Planitia) to the north. Gale Crater is noteworthy for its enigmatic -high crescent-shaped central mound, Aeolis Mons (known informally as Mt. Sharp).

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
Peace Vallis. Peace Vallis is an ancient stream valley on the northern rim of Gale Crater on the planet Mars. It is notable for its associated alluvial fan which lies near the Mars Science Laboratory &quot;Curiosity&quot; landing site (Bradbury Landing). The valley and alluvial fan provide evidence for geologically recent (Amazonian-aged) fluvial activity and sustained water flow on Mars.

Geographic entities mentioned:
surface_form: peace vallis
instance_of: Valley
coordinates: lat: -4.21
lon: 137.23
The valley and alluvial fan provide evidence for geologically recent (Amazonian-aged) fluvial activity and sustained water flow on Mars. Recent high-resolution orbital images of Peace Vallis and its watershed also suggest that at least one glacial episode affected Gale crater. All of this evidence has implications for the history of water on Mars and the planet's long-term habitability.

Geographic entities mentioned:
surface_form: peace vallis
instance_of: Valley
coordinates: lat: -4.21
lon: 137.23
All of this evidence has implications for the history of water on Mars and the planet's long-term habitability. Understanding Peace Vallis and its fan also provides geologic context for the rocks observed on the ground by the &quot;Curiosity&quot; rover. Location and Regional Context.

Geographic entities mentioned:
surface_form: peace vallis
instance_of: Valley
coordinates: lat: -4.21
lon: 137.23
The northern rim of Gale Crater is heavily eroded and hosts a number of geomorphic features indicating the effects of flowing water. These include valleys, gullies, and canyons; sinuous ridges interpreted to be inverted channels; and alluvial fan-like mesas. Peace Vallis and its alluvial fan is the largest and best studied of these fluvial features in northern Gale Crater. Name.

Geographic entities mentioned:
surface_form: peace vallis
instance_of: Valley
coordinates: lat: -4.21
lon: 137.23
surface_form: best
instance_of: Mountain
coordinates: lat: -66.8167
lon: 51.3833
Erosion of the watershed surface has produced a mottled scoured appearance, suggesting mobilization and transport of sediments into topographic lows. Compared with most terrestrial valleys carved by rainfall, the drainage density (stream length per unit area) of Peace Vallis and its tributaries is very low.

Geographic entities mentioned:
surface_form: peace vallis
instance_of: Valley
coordinates: lat: -4.21
lon: 137.23
The valleys are U-shaped in topographic profile, with widths ranging from 80 to 900 meters (262 to 2,950 feet) and a mean of 300 meters (984 feet). The main or trunk valley is about 32 km (20 miles) long. &quot;Curiosity&quot; rover landed near the end of the Peace Vallis fan. Peace Vallis fan covers and obtained water from an area of. Peace Vallis enters Gale Crater through a gap in its rim.

Geographic entities mentioned:
surface_form: peace vallis
instance_of: Valley
coordinates: lat: -4.21
lon: 137.23
surface_form: peace vallis
instance_of: Valley
coordinates: lat: -4.21
lon: 137.23
The main or trunk valley is about 32 km (20 miles) long. &quot;Curiosity&quot; rover landed near the end of the Peace Vallis fan. Peace Vallis fan covers and obtained water from an area of. Peace Vallis enters Gale Crater through a gap in its rim. Calculations suggest that the fan has an average thickness of. Numerous inverted channels are visible on the western surface of the fan.

Geographic entities mentioned:
surface_form: peace vallis
instance_of: Valley
coordinates: lat: -4.21
lon: 137.23
Calculations suggest that the fan has an average thickness of. Numerous inverted channels are visible on the western surface of the fan. Runoff through Peace Vallis that made the fan is estimated to be between; therefore a hydrologic cycle probably lasted at least thousands of years. The water that flowed in Peace Vallis is believed to be from precipitation, possibly in the form of snow.

Geographic entities mentioned:
surface_form: peace vallis
instance_of: Valley
coordinates: lat: -4.21
lon: 137.23
Geography. Norco is located at (30.003753, -90.410824). The city is situated on the eastern edge of the large Bonnet Carré Spillway, which provides for an outlet from the Mississippi River to Lake Pontchartrain during flooding of the river. According to the United States Census Bureau, the CDP has a total area of, of which is land and (12.83%) is water.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
Yanaqucha (Bolognesi). Yanaqucha (Quechua &quot;yana&quot; black, &quot;qucha&quot; lake, &quot;black lake&quot;, also spelled &quot;Yanacocha&quot;) is a lake in the Andes of Peru. It is situated at a height of comprising an area of. Yanaqucha is located in Aquia District, Bolognesi Province, Ancash Region.

Geographic entities mentioned:
surface_form: yanaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -12.8997
lon: -74.1439
surface_form: yanaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -10.8611
lon: -75.9903
surface_form: yanaqucha (bolognesi)
instance_of: Lake
countries: Peru
coordinates: lat: -10.04233333
lon: -77.20836111
Yanaqucha (Bolognesi). Yanaqucha (Quechua &quot;yana&quot; black, &quot;qucha&quot; lake, &quot;black lake&quot;, also spelled &quot;Yanacocha&quot;) is a lake in the Andes of Peru. It is situated at a height of comprising an area of. Yanaqucha is located in Aquia District, Bolognesi Province, Ancash Region.

Geographic entities mentioned:
surface_form: yanaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -12.8997
lon: -74.1439
surface_form: yanacocha
instance_of: Lake
countries: Peru
coordinates: lat: -12.8997
lon: -74.1439
surface_form: yanaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -10.8611
lon: -75.9903
surface_form: yanaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -10.04233333
lon: -77.20836111
Yanaqucha (Quechua &quot;yana&quot; black, &quot;qucha&quot; lake, &quot;black lake&quot;, also spelled &quot;Yanacocha&quot;) is a lake in the Andes of Peru. It is situated at a height of comprising an area of. Yanaqucha is located in Aquia District, Bolognesi Province, Ancash Region. The lake receives water from the Yanaqucha brook which originates southwest of the peak of Rahu Kutaq.

Geographic entities mentioned:
surface_form: yanaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -12.8997
lon: -74.1439
surface_form: yanaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -10.8611
lon: -75.9903
surface_form: yanaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -10.04233333
lon: -77.20836111
Carter's classification of the Himalayas divides the Gurans Himal into two subsections. The Saipal Subsection lies east of the Seti River, and its highest peak is Api. The Yoka Pahar Subsection lies west of the Seti, and contains Api,; Jethi Bahurani,; Bobaye,; and Nampa, among other peaks.

Geographic entities mentioned:
surface_form: Bobaye
instance_of: Mountain
countries: Nepal
coordinates: lat: 29.958321
lon: 81.021302
Eyebrowed jungle flycatcher. The eyebrowed jungle flycatcher (&quot;Vauriella gularis&quot;) is a species of bird in the Old World flycatcher family Muscicapidae. It is endemic to the island of Borneo (elevated areas, including the Meratus Mountains). The natural habitat of the eyebrowed jungle flycatcher is subtropical or tropical moist montane forests.

Geographic entities mentioned:
surface_form: Meratus Mountains
instance_of: Mountain
countries: Indonesia
coordinates: lat: -2.75
lon: 115.66666666667
From here parking is only permitted at designated car parks and there is a reduced winter service (no salting). The High Rhön Road runs about 840 metres east past the 926-metrek-high Heidelstein. From the east it is joined by the road from Ginolfs. A central crossing point in the High Rhön is at the &quot;Schornhecke&quot;, on the northern slopes of the Heidelstein, at kilometre 10.

Geographic entities mentioned:
surface_form: Heidelstein
instance_of: Mountain
countries: Germany
coordinates: lat: 50.458611111111
lon: 10.006666666667
Here the road is joined by the St 2286 from Oberelsbach to the east, and by the Landstraße (L) 3395 Wüstensachsen in the state of Hesse. The road runs eastwards past the Steinkopf (888 m) and the Stirnberg (902 m) and continues to the Black Moor. On this section it is joined from the east by roads from the Thuringian Hut (&quot;Thüringer Hütte&quot;), from Roth, Hillenberg and Hausen.

Geographic entities mentioned:
surface_form: Stirnberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.492222222222
lon: 10.039722222222
It is a tributary of the Cutler River, part of the Saco River watershed flowing to the Atlantic Ocean in Maine. The river is within the townships of Sargent's Purchase and Pinkham's Grant in Coos County. The New River rises in the Gulf of Slides, a small glacial cirque at the foot of Boott Spur, a southern extension of Mount Washington.

Geographic entities mentioned:
surface_form: Boott Spur
instance_of: Mountain
countries: United States
coordinates: lat: 44.252222222222
lon: -71.295
Clark grew up watching National Basketball Association (NBA) players Steve Nash and Chris Paul. He played youth travel basketball for Kings Academy in the Conejo Valley where he was coached by Adam Mazarei, a future NBA assistant coach for the Memphis Grizzlies. In eighth grade, Clark attended the Buckley School, a K–12 private school in Sherman Oaks.

Geographic entities mentioned:
surface_form: Conejo Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
The shared trail is also available for walkers and recreational horseriding, however motorised vehicles are prohibited. The trail is long and passes through a variety of forest and farmland landscapes with occasional views of the Gippsland Lakes. Parts of the trail are accessible to any bicycle, but significant sections are suitable only for mountain bikes or sturdy hybrid bikes.

Geographic entities mentioned:
surface_form: Gippsland Lakes
instance_of: Group of lakes
countries: Australia
coordinates: lat: -38
lon: 147.65
The trail initially passes between industrial and retail properties leading out of Bairnsdale, then travels mainly through open farmland, predominantly for cattle and horse grazing, to the town of Nicholson. There are distant views of the Gippsland Lakes in some sections and a number of crossings of minor roads are required as well as an unsigned crossing of the Princes Highway.

Geographic entities mentioned:
surface_form: Gippsland Lakes
instance_of: Group of lakes
countries: Australia
coordinates: lat: -38
lon: 147.65
The Brunswick and Florida faced major setbacks due to funding problems. On December 25, 1847, the Savannah and Albany Railroad Company was chartered by the Georgia General Assembly to construct a rail line from a point along the Central of Georgia Railway near Savannah to Albany with the possibility of extending the railroad to the Chattahoochee River at any time.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
In 1993, he made an early descent of the Great Whale River in northern Quebec, Canada. In 2015, Kennedy took two of his sons to the Yukon to visit Mount Kennedy and run the Alsek River, a whitewater river fed by the Alsek Glacier. Mount Kennedy was Canada's highest unclimbed peak when the Canadian government named it for John F. Kennedy in 1964.

Geographic entities mentioned:
surface_form: Mount Kennedy
instance_of: Mountain
countries: Canada
coordinates: lat: 60.341166666667
lon: -138.96633333333
One was the Indian Gap Trail, which connected the Rutherford Indian Trace in the Balsam Mountains to the Great Indian Warpath in modern-day Sevier County. The other was a lower trail that crested at Ekaneetlee Gap, a col just east of Gregory Bald.

Geographic entities mentioned:
surface_form: Gregory Bald
instance_of: Mountain
countries: United States
coordinates: lat: 35.5206
lon: -83.8661
surface_form: gregory bald
instance_of: Mountain
countries: United States
coordinates: lat: 35.5206
lon: -83.8661
His son, Frederick, built the cove's first gristmill. Other early settlers built houses on the surrounding mountains, among them Russell Gregory (1795–1864), for whom Gregory Bald is named, and James Spence, for whom Spence Field is named. Between 1820 and 1850, the population of Cades Cove grew to 671, with the size of cove farms averaging between.

Geographic entities mentioned:
surface_form: Gregory Bald
instance_of: Mountain
countries: United States
coordinates: lat: 35.5206
lon: -83.8661
surface_form: Spence Field
instance_of: Landform
countries: United States
coordinates: lat: 35.5633
lon: -83.7328
surface_form: gregory bald
instance_of: Mountain
countries: United States
coordinates: lat: 35.5206
lon: -83.8661
surface_form: spence field
instance_of: Landform
countries: United States
coordinates: lat: 35.5633
lon: -83.7328
On most days, multiple deer can be seen in the meadows and woods throughout the cove. Popular hiking trails within the cove include the trails to Abrams Falls (a nearly round trip hike) and Gregory Bald, the latter named after Russell Gregory. In addition to hiking and general sightseeing, horseback and bicycle riding are popular activities.

Geographic entities mentioned:
surface_form: Gregory Bald
instance_of: Mountain
countries: United States
coordinates: lat: 35.5206
lon: -83.8661
surface_form: gregory bald
instance_of: Mountain
countries: United States
coordinates: lat: 35.5206
lon: -83.8661
As with neighboring limestone windows such as Tuckaleechee to the north and Wear Cove to the east, the weathering of the limestone produced deep, fertile soil, making Cades Cove attractive to early farmers. The majority of the rocks that make up Cades Cove are unaltered sedimentary rock formed between 340 million and 570 million years ago during the Ordovician period.

Geographic entities mentioned:
surface_form: wear cove
instance_of: Valley
countries: United States
coordinates: lat: 35.7139
lon: -83.6532
surface_form: cades cove
instance_of: Valley
countries: United States
coordinates: lat: 35.594166666667
lon: -83.841944444444
Cades Cove. Cades Cove is an isolated valley located in the Tennessee section of the Great Smoky Mountains National Park. The valley was home to numerous settlers before the formation of the national park.

Geographic entities mentioned:
surface_form: cades cove
instance_of: Valley
countries: United States
coordinates: lat: 35.594166666667
lon: -83.841944444444
The valley was home to numerous settlers before the formation of the national park. Cades Cove, the single most popular destination for visitors to the park, attracts more than two million visitors annually because of its well preserved homesteads, scenic mountain views, and abundant display of wildlife. The Cades Cove Historic District is listed on the National Register of Historic Places.

Geographic entities mentioned:
surface_form: cades cove
instance_of: Valley
countries: United States
coordinates: lat: 35.594166666667
lon: -83.841944444444
Cades Cove, the single most popular destination for visitors to the park, attracts more than two million visitors annually because of its well preserved homesteads, scenic mountain views, and abundant display of wildlife. The Cades Cove Historic District is listed on the National Register of Historic Places. Geology.

Geographic entities mentioned:
surface_form: cades cove
instance_of: Valley
countries: United States
coordinates: lat: 35.594166666667
lon: -83.841944444444
The Cades Cove Historic District is listed on the National Register of Historic Places. Geology. Geologically, Cades Cove is a type of valley known as a &quot;limestone window&quot;, created by erosion that removed the older Precambrian sandstone, exposing the younger Paleozoic limestone beneath.

Geographic entities mentioned:
surface_form: cades cove
instance_of: Valley
countries: United States
coordinates: lat: 35.594166666667
lon: -83.841944444444
As with neighboring limestone windows such as Tuckaleechee to the north and Wear Cove to the east, the weathering of the limestone produced deep, fertile soil, making Cades Cove attractive to early farmers. The majority of the rocks that make up Cades Cove are unaltered sedimentary rock formed between 340 million and 570 million years ago during the Ordovician period.

Geographic entities mentioned:
surface_form: cades cove
instance_of: Valley
countries: United States
coordinates: lat: 35.594166666667
lon: -83.841944444444
Gregory's Cave. The fracturing and weathering of the limestone and sandstone in Cades Cove has led to the formation of several caves in the vicinity, the two largest of which are Gregory's Cave and Bull Cave. Bull Cave, at, is the deepest cave in Tennessee. Trilobite and brachiopod fossils have been found in Gregory's Cave. The entrance to Gregory's Cave is approximately wide and high.

Geographic entities mentioned:
surface_form: cades cove
instance_of: Valley
countries: United States
coordinates: lat: 35.594166666667
lon: -83.841944444444
surface_form: bull
instance_of: Watercourse
countries: United States
coordinates: lat: 49.46663
lon: -115.45205
surface_form: bull
instance_of: Watercourse
countries: United States
coordinates: lat: 49.46663
lon: -115.45205
The dirt on this side of the cave has been excavated and removed, and pickax marks are still visible in the dirt. Saltpeter mining occurred in the Smokies from the late 18th century through the Civil War, so this mining activity must have occurred sometime between 1818, when settlers arrived in Cades Cove and 1865, the end of the Civil War.

Geographic entities mentioned:
surface_form: cades cove
instance_of: Valley
countries: United States
coordinates: lat: 35.594166666667
lon: -83.841944444444
European traders were using these trails as early as 1740. By 1797 (and probably much earlier), the Cherokee had established a settlement in Cades Cove known as &quot;Tsiya'hi&quot;, or &quot;Otter Place&quot;. This village, which may have been little more than a seasonal hunting camp, was located somewhere along the flats of Cove Creek.

Geographic entities mentioned:
surface_form: cades cove
instance_of: Valley
countries: United States
coordinates: lat: 35.594166666667
lon: -83.841944444444
European settlement. John Oliver (1793–1863), a veteran of the War of 1812, and his wife Lurena Frazier (1795–1888) were the first permanent European settlers in Cades Cove. The Olivers, originally from Carter County, Tennessee, arrived in 1818, accompanied by Joshua Jobe, who had initially persuaded them to settle in the cove.

Geographic entities mentioned:
surface_form: cades cove
instance_of: Valley
countries: United States
coordinates: lat: 35.594166666667
lon: -83.841944444444
Jobe returned in the spring of 1819 with a herd of cattle in tow and gave the Olivers two milk cows. In 1821, William &quot;Fighting Billy&quot; Tipton (1761–1849), a veteran of the American Revolution and son of State of Franklin opponent John Tipton, bought up large tracts of Cades Cove which he in turn sold to his sons and relatives, and settlement began to boom.

Geographic entities mentioned:
surface_form: cades cove
instance_of: Valley
countries: United States
coordinates: lat: 35.594166666667
lon: -83.841944444444
The isolation often attributed to Cades Cove is probably exaggerated. A post office was established in the cove in 1833, and Sevierville post master Philip Seaton set up a weekly mail route to the cove in 1839. Cades Cove had telephone service as early as the 1890s, when Dan Lawson and several neighbors built a phone line to Maryville.

Geographic entities mentioned:
surface_form: cades cove
instance_of: Valley
countries: United States
coordinates: lat: 35.594166666667
lon: -83.841944444444
Cades Cove had telephone service as early as the 1890s, when Dan Lawson and several neighbors built a phone line to Maryville. By the 1850s, various roads connected Cades Cove with Tuckaleechee and Montvale Springs, some of which are still maintained as seasonal passes or hiking trails. Religion.

Geographic entities mentioned:
surface_form: cades cove
instance_of: Valley
countries: United States
coordinates: lat: 35.594166666667
lon: -83.841944444444
Religion. Religion was an important part of life in Cades Cove from its earliest days, a reflection of the efforts of John and Lucretia Oliver. The Olivers managed to organize a branch of the Miller's Cove Baptist Church for Cades Cove in 1825. After briefly realigning themselves with the Wear's Cove Baptist Church, the Cades Cove Baptist Church was pronounced an independent entity in 1829.

Geographic entities mentioned:
surface_form: cades cove
instance_of: Valley
countries: United States
coordinates: lat: 35.594166666667
lon: -83.841944444444
In 1863, Confederate bushwhackers from Hazel Creek and other parts of North Carolina began making systematic raids into Cades Cove, stealing livestock and killing any Union supporter they could find. Elijah Oliver (1829–1905), a son of John Oliver and a Union sympathizer, was forced to hide out on Rich Mountain for much of the war.

Geographic entities mentioned:
surface_form: cades cove
instance_of: Valley
countries: United States
coordinates: lat: 35.594166666667
lon: -83.841944444444
Calvin Post had also gone into hiding, and with the death of John Oliver in 1863, the cove had lost most of its original leaders. Although Union forces occupied Knoxville in 1863, Confederate raids into Cades Cove continued. A pivotal figure at this time was Russell Gregory, who had originally vowed to remain neutral after his son defected to the Confederate cause.

Geographic entities mentioned:
surface_form: cades cove
instance_of: Valley
countries: United States
coordinates: lat: 35.594166666667
lon: -83.841944444444
Despite these threats, Chapman initiated a condemnation suit against John W. Oliver in July 1929. The court, however, ruled in favor of Oliver, reasoning that the federal government had never said Cades Cove was essential to the national park. Shortly after the verdict, the Secretary of the Interior officially announced that the cove was necessary, and another condemnation suit was filed.

Geographic entities mentioned:
surface_form: cades cove
instance_of: Valley
countries: United States
coordinates: lat: 35.594166666667
lon: -83.841944444444
At first, the National Park Service planned to let the cove return to its natural forested state. It ultimately yielded to requests by the Great Smoky Mountain Conservation Association to maintain Cades Cove as a meadow.

Geographic entities mentioned:
surface_form: cades cove
instance_of: Valley
countries: United States
coordinates: lat: 35.594166666667
lon: -83.841944444444
Touring. Though geographically isolated, Cades Cove today is a popular tourist destination in the Great Smoky Mountains National Park. A one-way, paved loop around Cades Cove draws thousands of visitors daily. The 11 miles may take more than four hours to traverse and view the sites during tourist season.

Geographic entities mentioned:
surface_form: cades cove
instance_of: Valley
countries: United States
coordinates: lat: 35.594166666667
lon: -83.841944444444
Oliver were burned, destroying a large portion of the family's livestock and tools. Shortly thereafter, Gregory's son was assaulted by Asa and John Sparks after a prank-gone-wrong. In response, Gregory and his brother, Dana, hunted down and shot the Sparks brothers on Christmas night in 1921. Both of the Gregorys were convicted of barn burning and later convicted of felonious assault.

Geographic entities mentioned:
surface_form: brothers
instance_of: Mountain
countries: United States
coordinates: lat: 47.6537193
lon: -123.140575
Cades Cove. Cades Cove is an isolated valley located in the Tennessee section of the Great Smoky Mountains National Park. The valley was home to numerous settlers before the formation of the national park.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
For about 100 years before the creation of the national park, much farming and logging was done in the valley, as the main source of economic development for the people living in the cove, both leading to massive deforestation. At first, the National Park Service planned to let the cove return to its natural forested state.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
More weathering-resistant formations, such as the Cades sandstone which underlies Rich Mountain to the north and the Elkmont and Thunderhead sandstones which form the Great Smoky Mountains crest to the south surround the cove, leaving it relatively isolated within the Smokies.

Geographic entities mentioned:
surface_form: rich mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.2356
lon: -81.7058
surface_form: rich mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.170833333333
lon: -81.709166666667
surface_form: rich mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.7436
lon: -84.3431
surface_form: thunderhead
instance_of: Mountain
countries: United States
coordinates: lat: 35.568611111111
lon: -83.706388888889
surface_form: rich mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.6743
lon: -94.3292
In 1863, Confederate bushwhackers from Hazel Creek and other parts of North Carolina began making systematic raids into Cades Cove, stealing livestock and killing any Union supporter they could find. Elijah Oliver (1829–1905), a son of John Oliver and a Union sympathizer, was forced to hide out on Rich Mountain for much of the war.

Geographic entities mentioned:
surface_form: rich mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.2356
lon: -81.7058
surface_form: rich mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.170833333333
lon: -81.709166666667
surface_form: rich mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.7436
lon: -84.3431
surface_form: rich mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.6743
lon: -94.3292
With such sentiment and influence, Cades Cove remained staunchly pro-Union, regardless of the destruction it suffered throughout the war (there were some exceptions, however, such as the cove's affluent entrepreneur and Confederate sympathizer, Daniel Foute).

Geographic entities mentioned:
surface_form: daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
A one-way, paved loop around Cades Cove draws thousands of visitors daily. The 11 miles may take more than four hours to traverse and view the sites during tourist season. The cove receives approximately 5 million visitors per year and is the most popular destination in the Great Smoky Mountain National Park.

Geographic entities mentioned:
surface_form: smoky mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0594
lon: -113.68
This passage is long, and a side passage to the right (south) is developed about from the entrance. This side passage ends after about. In the vicinity of this side passage are &quot;tally marks&quot; on the wall, which were typically left by saltpeter miners. The dirt on this side of the cave has been excavated and removed, and pickax marks are still visible in the dirt.

Geographic entities mentioned:
surface_form: the wall
instance_of: Mountain
countries: United States
coordinates: lat: 43.8831
lon: -110.838
Valley Plaza. Valley Plaza was a shopping center in North Hollywood, Los Angeles, one of the first in the San Fernando Valley, opened in 1951. In the mid-1950s, it was reported to be the largest shopping center on the West Coast of the United States and the third-largest in the country. It was located along Laurel Canyon Boulevard from Oxnard to Vanowen, and west along Victory Boulevard.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Location and visit. Located on the lakefront of Lake Michigan, the Milwaukee Art Museum is one of the largest art museums in the Midwestern United States. Aside from its galleries, the museum includes a cafe, named Cafe Calatrava, and a gift shop. Hours. Normal operating hours for MAM are Wednesday, Friday, Saturday, and Sunday 10:00 a.m. to 5:00 p.m., and Thursday 10:00 a.m. to 8:00 p.m.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
All the paintings are of Bermuda images, and the theme continues upstairs through the corridors and upstairs in The Royal Suite, and the private quarters of the governor which overlook the North Shore towards Hamilton Harbour, and the four guest bedrooms whose verandah offers views of Hamilton.

Geographic entities mentioned:
surface_form: Hamilton Harbour
instance_of: Landform
countries: United Kingdom
coordinates: lat: 32.289164
lon: -64.784195
Nyerere came up with the idea for the conference. History. PAFMECA was formed in the town of Mwanza on the shores of Lake Victoria in northern Tanganyika under the leadership of Julius Nyerere. Nyerere was the leader of the Tanganyika African National Union (TANU), the party that campaigned for the independence of Tanganyika.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Dream Lake (Washington). Dream Lake is a freshwater lake located on the southern slope of Dog Mountain in King County, Washington, United States. It is west of Otter Lake, part of the Alpine Lakes Wilderness. Big Creek, a tributary to the Taylor River, exits Dream Lake into a canyon that produces Big Creek Falls.

Geographic entities mentioned:
surface_form: Dog Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.7171
lon: -121.701
surface_form: dream lake
instance_of: Lake
countries: United States
coordinates: lat: 40.309444444444
lon: -105.65888888889
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: dream lake
instance_of: Lake
countries: United States
coordinates: lat: 47.6
lon: -121.4367
Access to Dream Lake is provided through an unmaintained access trail that splits off the Snoqualmie Lake Trail. A short distance west of Dream Lake is a short side trail that branches off Taylor River Trail, shortly after the crossing of Otter Creek, that leads to Otter Falls, a snow-driven waterfall which drops directly into Lipsy Lake. Marten Lake is further west past Otter Falls.

Geographic entities mentioned:
surface_form: Marten Lake
instance_of: Lake
countries: United States
coordinates: lat: 47.592777777778
lon: -121.51444444444
Dream Lake (Washington). Dream Lake is a freshwater lake located on the southern slope of Dog Mountain in King County, Washington, United States. It is west of Otter Lake, part of the Alpine Lakes Wilderness. Big Creek, a tributary to the Taylor River, exits Dream Lake into a canyon that produces Big Creek Falls.

Geographic entities mentioned:
surface_form: dream lake
instance_of: Lake
countries: United States
coordinates: lat: 40.309444444444
lon: -105.65888888889
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: dream lake (washington)
instance_of: Lake
countries: United States
coordinates: lat: 47.6
lon: -121.4367
It is west of Otter Lake, part of the Alpine Lakes Wilderness. Big Creek, a tributary to the Taylor River, exits Dream Lake into a canyon that produces Big Creek Falls. Because of its proximity to Dog Mountain summit and the cirque of Rooster Mountain to the west, the lake is a popular area for hiking, swimming, and fishing and rainbow trout.

Geographic entities mentioned:
surface_form: dream lake
instance_of: Lake
countries: United States
coordinates: lat: 40.309444444444
lon: -105.65888888889
surface_form: dream lake
instance_of: Lake
countries: United States
coordinates: lat: 47.6
lon: -121.4367
surface_form: big creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.41361111
lon: -91.60583333
surface_form: big creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.41361111
lon: -91.60583333
Big Creek, a tributary to the Taylor River, exits Dream Lake into a canyon that produces Big Creek Falls. Because of its proximity to Dog Mountain summit and the cirque of Rooster Mountain to the west, the lake is a popular area for hiking, swimming, and fishing and rainbow trout. Access to Dream Lake is provided through an unmaintained access trail that splits off the Snoqualmie Lake Trail.

Geographic entities mentioned:
surface_form: dream lake
instance_of: Lake
countries: United States
coordinates: lat: 40.309444444444
lon: -105.65888888889
surface_form: snoqualmie lake
instance_of: Lake
countries: United States
coordinates: lat: 47.5665567
lon: -121.4128124
surface_form: dream lake
instance_of: Lake
countries: United States
coordinates: lat: 47.6
lon: -121.4367
Access to Dream Lake is provided through an unmaintained access trail that splits off the Snoqualmie Lake Trail. A short distance west of Dream Lake is a short side trail that branches off Taylor River Trail, shortly after the crossing of Otter Creek, that leads to Otter Falls, a snow-driven waterfall which drops directly into Lipsy Lake. Marten Lake is further west past Otter Falls.

Geographic entities mentioned:
surface_form: dream lake
instance_of: Lake
countries: United States
coordinates: lat: 40.309444444444
lon: -105.65888888889
surface_form: dream lake
instance_of: Lake
countries: United States
coordinates: lat: 47.6
lon: -121.4367
Dream Lake (Washington). Dream Lake is a freshwater lake located on the southern slope of Dog Mountain in King County, Washington, United States. It is west of Otter Lake, part of the Alpine Lakes Wilderness. Big Creek, a tributary to the Taylor River, exits Dream Lake into a canyon that produces Big Creek Falls.

Geographic entities mentioned:
surface_form: otter lake
instance_of: Lake
countries: United States
coordinates: lat: 43.1402191
lon: -76.5330206
surface_form: otter lake
instance_of: Lake
countries: United States
coordinates: lat: 45.443611111111
lon: -89.186388888889
surface_form: otter lake
instance_of: Lake
countries: United States
coordinates: lat: 39.4081
lon: -89.9117
surface_form: otter lake
instance_of: Lake
countries: United States
coordinates: lat: 43.545555555556
lon: -74.563333333333
surface_form: otter lake
instance_of: Lake
countries: United States
coordinates: lat: 42.628644
lon: -83.347714
surface_form: otter lake
instance_of: Lake
countries: United States
coordinates: lat: 43.591944444444
lon: -75.117777777778
surface_form: otter lake
instance_of: Lake
countries: United States
coordinates: lat: 47.577777777778
lon: -121.2875
Big Creek, a tributary to the Taylor River, exits Dream Lake into a canyon that produces Big Creek Falls. Because of its proximity to Dog Mountain summit and the cirque of Rooster Mountain to the west, the lake is a popular area for hiking, swimming, and fishing and rainbow trout. Access to Dream Lake is provided through an unmaintained access trail that splits off the Snoqualmie Lake Trail.

Geographic entities mentioned:
surface_form: dog mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.7171
lon: -121.701
The area is roughly coextensive with the Martis Creek Basin, which drains into the Truckee River. It includes Martis Creek, Donner Creek, and Prosser Creek, major tributaries to the Truckee River. There are several natural lakes, Dry Lake, and Gooseneck Lake, Donner Lake. The Prosser Creek Reservoir, a small manmade lake, was created in 1962.

Geographic entities mentioned:
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6282988
lon: -97.0561783
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 38.3360373
lon: -117.7898285
Martis Valley. Martis Valley is a geographic area of in the United States, extending northward from the North Shore of Lake Tahoe, California, to the west of the California-Nevada border. It is located in Placer and Nevada Counties and is bisected by Martis Creek which flows north to the Truckee River. Description.

Geographic entities mentioned:
surface_form: martis valley
instance_of: Valley
countries: United States
coordinates: lat: 39.3467
lon: -120.118
It is located in Placer and Nevada Counties and is bisected by Martis Creek which flows north to the Truckee River. Description. Located in the Sierra Nevada mountains north of Lake Tahoe, Martis Valley is largely rural and forested. Elevation ranges from approximately 5,800 to 8,600 feet above mean sea level.

Geographic entities mentioned:
surface_form: martis valley
instance_of: Valley
countries: United States
coordinates: lat: 39.3467
lon: -120.118
History. In 2001 a forest fire burned of land. Development. In the 2000s Martis Valley faced development pressure due to its proximity to Truckee, California and Northstar at Tahoe, a popular ski resort. Developers initially obtained approval to build 6,000 homes on of subdivisions, which would have more than doubled the population of Truckee, California.

Geographic entities mentioned:
surface_form: martis valley
instance_of: Valley
countries: United States
coordinates: lat: 39.3467
lon: -120.118
In 2016, Mountainside Partners and Sierra Pacific Industries submitted a final application for entitlements for its proposed Martis Valley West Parcel Specific Plan, a plan that prompted the Attorney General of California to write a letter of concern to Placer County.

Geographic entities mentioned:
surface_form: martis valley
instance_of: Valley
countries: United States
coordinates: lat: 39.3467
lon: -120.118
Ruby Mountain (New York). Ruby Mountain is a mountain located in the Adirondack Mountains of New York, in the town of Indian Lake in Hamilton County, east-southeast of the hamlet of Indian Lake. The mountain has been the location of a garnet mine owned by Barton Mines since 1982.

Geographic entities mentioned:
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 42.2980198
lon: -71.8120781
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 42.2980198
lon: -71.8120781
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7
lon: -74.3167
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7
lon: -74.3167
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 45.81402
lon: -89.30162
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 45.81402
lon: -89.30162
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 41.4793
lon: -71.4684
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 41.4793
lon: -71.4684
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 41.9947
lon: -86.2042
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 41.9947
lon: -86.2042
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 44.114166666667
lon: -93.786666666667
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 44.114166666667
lon: -93.786666666667
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 43.5083
lon: -95.5028
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 43.5083
lon: -95.5028
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 45.988888888889
lon: -86.332222222222
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 45.988888888889
lon: -86.332222222222
surface_form: ruby mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.746944444444
lon: -74.104722222222
surface_form: ruby mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.69457
lon: -121.04262
Ruby Mountain (New York). Ruby Mountain is a mountain located in the Adirondack Mountains of New York, in the town of Indian Lake in Hamilton County, east-southeast of the hamlet of Indian Lake. The mountain has been the location of a garnet mine owned by Barton Mines since 1982.

Geographic entities mentioned:
surface_form: ruby mountain (new york)
instance_of: Mountain
countries: United States
coordinates: lat: 43.746944444444
lon: -74.104722222222
surface_form: ruby mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.69457
lon: -121.04262
This appears to be a misreading of several sources. The Royal Navy did detain an American vessel named &quot;Little William&quot; and send her into Portsmouth. &quot;Little William&quot; was suspected of having planned to run the British blockade of the rivers Elbe, Weser, and Ems. The High Court of Admiralty condemned &quot;Little William&quot;, Brown, master, on 23 November 1807.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Nova Scotia's remaining independent publications include the &quot;Halifax Examiner&quot;, based in Halifax; and &quot;The Laker&quot;, based in Enfield. The province's Acadian community is served by &quot;Le Courrier de la Nouvelle-Écosse&quot;, a French-language newspaper founded in 1937 in Meteghan River. Atlantic Book Awards.

Geographic entities mentioned:
surface_form: Meteghan River
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.2169
lon: -66.1421
Chongra Peak. Chongra Peak () is a peak in the Himalaya range of Asia. Located in Gilgit–Baltistan, Pakistan,
it is one of the many subsidiary summits of the Nanga Parbat massif. __NOTOC__
The peak lies just south of the Indus River, in Pakistan. Not far to the north is the western end of the Karakoram range. Layout of the mountain.

Geographic entities mentioned:
surface_form: Nanga Parbat
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.239166666667
lon: 74.59
__NOTOC__
The peak lies just south of the Indus River, in Pakistan. Not far to the north is the western end of the Karakoram range. Layout of the mountain. &quot;From the article: Nanga Parbat&quot;
The core of Nanga Parbat is a long ridge trending southwest–northeast. The southwestern portion of this main ridge is known as the Mazeno Ridge, and has a number of subsidiary peaks.

Geographic entities mentioned:
surface_form: Nanga Parbat
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.239166666667
lon: 74.59
surface_form: nanga parbat
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.239166666667
lon: 74.59
surface_form: nanga parbat
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.239166666667
lon: 74.59
It is split into the Diamir (west) face and the Rakhiot (north) face by a long ridge. There are a number of subsidiary summits, including the North Peak (7816m) some 3 km north of the main summit. Chongra Peak itself is located at the far east end of the massif, directly north of the village of Tarashing and the upper Astore Valley.

Geographic entities mentioned:
surface_form: Astore
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.03897222
lon: 75.11025278
surface_form: astore valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.03897222
lon: 75.11025278
Chongra Peak. Chongra Peak () is a peak in the Himalaya range of Asia. Located in Gilgit–Baltistan, Pakistan,
it is one of the many subsidiary summits of the Nanga Parbat massif. __NOTOC__
The peak lies just south of the Indus River, in Pakistan. Not far to the north is the western end of the Karakoram range. Layout of the mountain.

Geographic entities mentioned:
surface_form: chongra peak
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.326280555556
lon: 74.677627777778