Sarmila/GeoWiki-Features huggingface dataset:
Many explorations were conducted in highland Papua during the early 20th century. One of these was the Second South New Guinea Expedition led by Lorentz and composed of the and Apo Kayan Dayak tribes in 1909–1910, which successfully met with representatives from the Pesegem tribesman in the south of Mount Trikora, although they failed to reach the Baliem Valley.

Geographic entities mentioned:
surface_form: Mount Trikora
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.35
lon: 138.65
Trantham Hollow. Trantham Hollow is a valley in Oregon County in the Ozarks of southern Missouri. The headwaters of the intermittent stream in Trantham Hollow are at and the confluence with the Warm Fork Spring River is at. Trantham Hollow has the name of Eli Trantham, a pioneer citizen.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
surface_form: trantham hollow
instance_of: Valley
countries: United States
coordinates: lat: 36.62166667
lon: -91.56
surface_form: the ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
Trantham Hollow. Trantham Hollow is a valley in Oregon County in the Ozarks of southern Missouri. The headwaters of the intermittent stream in Trantham Hollow are at and the confluence with the Warm Fork Spring River is at. Trantham Hollow has the name of Eli Trantham, a pioneer citizen.

Geographic entities mentioned:
surface_form: Warm Fork Spring River
instance_of: Watercourse
countries: United States
coordinates: lat: 36.49444444
lon: -91.53611111
surface_form: trantham hollow
instance_of: Valley
countries: United States
coordinates: lat: 36.62166667
lon: -91.56
surface_form: spring river
instance_of: Landform
countries: United States
coordinates: lat: 44.6893
lon: -68.0818
Trantham Hollow. Trantham Hollow is a valley in Oregon County in the Ozarks of southern Missouri. The headwaters of the intermittent stream in Trantham Hollow are at and the confluence with the Warm Fork Spring River is at. Trantham Hollow has the name of Eli Trantham, a pioneer citizen.

Geographic entities mentioned:
surface_form: trantham hollow
instance_of: Valley
countries: United States
coordinates: lat: 36.62166667
lon: -91.56
Wailoa River State Recreation Area. The Wailoa River State Recreation Area, also known as Wailoa River State Park, is a park in Hilo, on Hawaii Island in the US state of Hawaii. It was developed as a buffer zone following the devastating 1960 tsunami that wiped out the central bayfront district of Hilo. Description.

Geographic entities mentioned:
surface_form: wailoa river state recreation area
instance_of: Landform
countries: United States
coordinates: lat: 19.7186
lon: -155.075
HRA decided to permanently relocate Shinmachi rather than rebuild and initiated Project Kaikoo (&quot;rough seas&quot;), completing the acquisition of land and relocation of residents by 1965. Approximately of oceanfront land would be set aside as a green belt and buffer zone to absorb future tsunamis, including the Wailoa River State Recreation Area.

Geographic entities mentioned:
surface_form: wailoa river state recreation area
instance_of: Landform
countries: United States
coordinates: lat: 19.7186
lon: -155.075
Construction of a system of locks, dams, and chutes was begun by the Monongahela Navigation Company in 1817; the project was abandoned following damage by floods in 1824. south of Weston, the river is dammed by the U.S. Army Corps of Engineers to form Stonewall Jackson Lake.

Geographic entities mentioned:
surface_form: Stonewall Jackson Lake
instance_of: Lake
countries: United States
coordinates: lat: 39.0033
lon: -80.4739
Tyresån Lake System. c0dlvipcznvrx3wmy68ky13w4wm" xml:space="preserve">#REDIRECT Tyresån lake system

Geographic entities mentioned:
surface_form: tyresån
instance_of: Group of lakes
countries: Sweden
coordinates: lat: 59.2333
lon: 18.1667
Goodea. &quot;Goodea&quot; is a genus of splitfins that are endemic to Mexico. They are found in a wide range of habitats in several river basins that originate in the Central Plateau, such as Pánuco, Lerma–Chapala–Grande de Santiago and Balsas. Overall this genus is among the most widespread and successful splitfins, although they also have declined and the relatively restricted &quot;G.

Geographic entities mentioned:
surface_form: Central Plateau
instance_of: Plateau
countries: Mexico
coordinates: lat: 24
lon: -103
surface_form: Chapala
instance_of: Lake
countries: Mexico
coordinates: lat: 20.333333333333
lon: -103
Slate Creek (British Columbia). f3ichmrmo709hftsesshlhmuxioi" xml:space="preserve">Slate Creek is a creek located in the Omineca Country region of British Columbia. This creek is a tributary of the Manson River and flows into that river from the west. Slate Creek was discovered in 1871. The creek has been mined using wing-damming and hand-mining.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: slate creek (british columbia)
instance_of: Watercourse
countries: Canada
coordinates: lat: 55.66972222222222
lon: -124.48472222222222
Slate Creek (British Columbia). f3ichmrmo709hftsesshlhmuxioi" xml:space="preserve">Slate Creek is a creek located in the Omineca Country region of British Columbia. This creek is a tributary of the Manson River and flows into that river from the west. Slate Creek was discovered in 1871. The creek has been mined using wing-damming and hand-mining.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: slate creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 55.66972222222222
lon: -124.48472222222222
Slate Creek (British Columbia). f3ichmrmo709hftsesshlhmuxioi" xml:space="preserve">Slate Creek is a creek located in the Omineca Country region of British Columbia. This creek is a tributary of the Manson River and flows into that river from the west. Slate Creek was discovered in 1871. The creek has been mined using wing-damming and hand-mining.

Geographic entities mentioned:
surface_form: slate creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 55.66972222222222
lon: -124.48472222222222
Educated at the University of Tennessee and the University of Texas, he worked as an engineer. During World War II, he served in the Army Air Forces as a radioman and tail gunner, flying more than fifty bombing missions over Italy. He took part in the bombing of the Benedictine Abbey at Monte Cassino, which proved a traumatic experience for him.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
Sixteen days before the Yongle Emperor gave the banquet at Longjiang, Huang Fu had departed from Nanjing and spend a night at Longjiang, before sailing west on the Yangtze River. After eight days, he reached Poyang Lake; after another week, he reached Dongting Lake. Thereafter, Huang traveled through the Xiang River southwards, passing Xiangtan and Guilin, heading towards Nanning in Guangxi.

Geographic entities mentioned:
surface_form: Poyang Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 29.066666666667
lon: 116.38333333333
surface_form: Dongting Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 29.316666666667
lon: 112.95
Abu Zurayq. Abu Zurayq is a cluster of archaeological sites at a well-watered spot at the western edge of the Jezreel Valley and its transition to the Menashe Heights, next to Highway 66, between the modern kibbutzim of HaZore'a and Mishmar HaEmek.

Geographic entities mentioned:
surface_form: Jezreel Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
Location; palaeogeography. Abu Zurayq village was situated in the northern foothills of an area overlooking the Jezreel Valley called &quot;Bilad al-Rawha&quot; ('The Fragrant Country'). It depended on a number of water sources in its vicinity including the spring of Ein Abu Zurayq, the Wadi Abu Zurayq stream, and a well.

Geographic entities mentioned:
surface_form: Jezreel Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
The prehistoric site of Abu Zurayq was found south of the mound, on the sloping terrace east of the foothills of the Menashe Heights. During the Neolithic period there was a large lake next to the site covering part of what is today the Jezreel Valley. Archaeological exploration. The site was excavated by three different expeditions.

Geographic entities mentioned:
surface_form: Jezreel Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
In the later phases of this period, the pottery was lustrous, painted red and black and burnished. Interesting findings from this period are non-local pottery that was acquired by trade. These include pottery of the Yarmukian culture but also pottery that is originated in areas further to the north of the Mediterranean coast such as the Amuq Valley and Mersin, in Cilicia.

Geographic entities mentioned:
surface_form: Amuq Valley
instance_of: Valley
countries: Turkey
coordinates: lat: 36.354349
lon: 36.36153
They were part of the larger nomadic Turkmen community that lived in the Marj Ibn Amer plain (the Jezreel Valley) and in their transition to a sedentary lifestyle also founded the nearby villages of Abu Shusha, al-Mansi, Ayn al-Mansi, Khirbat Lid, and al-Ghubayya at around the same time Abu Zurayq was founded.

Geographic entities mentioned:
surface_form: Jezreel Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
He also plays Yamaha and Ovation Adamas series acoustic–electric guitars. Early life. Steven Lee Lukather was born on October 21, 1957, in the San Fernando Valley, California. His father was an assistant director and production manager at Paramount Studios, and worked on shows such as &quot;The Adventures of Ozzie and Harriet&quot; and &quot;I Dream of Jeannie&quot;.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Under the influence of Tendai Buddhism and Shugendō, the &quot;gongen&quot; concept was adapted, for example, to religious beliefs tied to Mount Iwaki, a volcano, so that female &quot;kami&quot; Kuniyasutamahime became associated with Jūichimen Kannon Bosatsu (eleven-faced Kannon), &quot;kami&quot; Ōkuninushi with Yakushi Nyorai, and Kunitokotachi no Mikoto with Amida Nyorai. Practice.

Geographic entities mentioned:
surface_form: Mount Iwaki
instance_of: Mountain
countries: Japan
coordinates: lat: 40.653333
lon: 140.306667
Wayra Wasi. Wayra Wasi (Quechua &quot;wayra&quot; wind, &quot;wasi&quot; house, &quot;wind house&quot;, Hispanicized spelling &quot;Huayra Huasi&quot;) is a mountain in the Bolivian Andes. It is situated in the Potosí Department, Tomás Frías Province, Potosí Municipality. Wayra Wasi lies west of Jatun Q'asa and the Ch'aki Mayu (Quechua for &quot;dry river&quot;, &quot;Chaqui Mayu&quot;).

Geographic entities mentioned:
surface_form: wayra wasi
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.3925
lon: -65.6458
surface_form: wayra wasi
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.47666667
lon: -65.83055556
Kagera River. The Kagera River, also known as Akagera River, or Alexandra Nile, is an East African river, forming part of the upper headwaters of the Nile and carrying water from its most distant source. With a total length of from its source located in Lake Rweru in Rwanda. The section of river named Kagera begins in Burundi, flowing out from Lake Rweru.

Geographic entities mentioned:
surface_form: Lake Rweru
instance_of: Lake
countries: Rwanda
Burundi
coordinates: lat: -2.3777777777778
lon: 30.323611111111
From the confluence, the Kagera flows north along the Rwanda-Tanzania border, over Rusumo Falls and through Akagera National Park. It then takes a turn to the east, following the Tanzania-Uganda border and emptying into Lake Victoria in Uganda. In 1898, Richard Kandt was the first European to reach the source of the Kagera.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
It is the largest single inflow into the lake, contributing approximately 6.4 billion cubic metres of water a year (about 28 per cent of the lake's outflow). The Kagera is formed by the confluence of the Ruvuvu and the Nyabarongo, close to the northernmost point of Lake Tanganyika. It forms parts of the Burundi–Tanzania, Rwanda–Tanzania, Burundi–Rwanda, and Tanzania–Uganda borders.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
This reduced the elevation at which crops could be grown and shortened the growing season by up to two months in extreme years, as it did in the 1690s. The massive eruptions of volcanoes at Hekla in Iceland (1693) and Serua (1693) and Aboina (1694) in Indonesia may also have polluted the atmosphere and filtered out significant amounts of sunlight.

Geographic entities mentioned:
surface_form: Serua
instance_of: Mountain
countries: Indonesia
coordinates: lat: -6.3
lon: 130
Initially occupying the area between Manyanga and the Malebo Pool, the Teke were gradually pushed north by Kongolese raids and emigration, itself a product of the violence of the Atlantic slave trade, into the Batéké Plateau. The French first arrived in what is now the Republic of Congo in the 1880s, and occupied the Congo until 1960.

Geographic entities mentioned:
surface_form: Batéké Plateau
instance_of: Plateau
countries: Gabon
Republic of the Congo
coordinates: lat: -3.51
lon: 15.76
On the eastern side stands Dhansā Degah (धन्सा देग:) (alternative name: Dhunsar), a 17th-century pagoda-shaped building. Its carved wood windows provide a specimen of the art of woodworking which has been highly developed in the Kathmandu Valley since ancient times. The upper part was destroyed in the great earthquake of 1934, and its height was shortened when it was repaired.

Geographic entities mentioned:
surface_form: Kathmandu Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
Following the uplift, large volumes of sediments, rich in early Tertiary fossils, were deposited in the adjoining basins. The ice ages of the Pleistocene led to extensive glaciation. Though many cirques, U-shaped valleys and glacial lakes can be found in the mountain range, the only remaining active glacier is the Cloud Peak Glacier, which is on the east slope of Cloud Peak. Geologist N.H.

Geographic entities mentioned:
surface_form: Cloud Peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.382138888889
lon: -107.17391388889
Geography. The highest peaks within the Bighorns are located in Wyoming in the Bighorn National Forest. Two peaks rise to over 13,000 ft: Cloud Peak () and Black Tooth Mountain (). There are a dozen more that rise to over. From the east the mountains present a vertical relief of over, rising abruptly from the plains.

Geographic entities mentioned:
surface_form: Cloud Peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.382138888889
lon: -107.17391388889
surface_form: Black Tooth Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.403333333333
lon: -107.17944444444
He made many adventurous journeys in China and Tibet, frequently travelling thousands of miles on foot. He was the first European to walk from Peking to Lhasa, when he described the Amne Machin massif in eastern Tibet in 1921–2, sometimes reckoned among the great geographical discoveries of the twentieth century.

Geographic entities mentioned:
surface_form: Amne Machin
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 34.798333333333
lon: 99.4625
Colorado Plateau shrublands. The Colorado Plateau shrublands is an ecoregion of deserts and xeric shrublands in the Western United States. Geography. The Colorado Plateau shrublands occupy the Colorado Plateau. They lie mostly in the basin of the upper Colorado River, and reach into the upper basin of the Rio Grande. Flora.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
Gen. Jubal A. Early decided to withdraw his army across the Potomac River into Virginia and return to the Shenandoah Valley. The Confederates withdrew along the Georgetown Pike into Montgomery County, Maryland towards Poolesville. On the July 14 they reached Conrad's Ferry (present day White's Ferry) and crossed making camp at Big Springs just north of Leesburg, Virginia.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Gen. George Crook had crossed into Loudoun that morning by way of Berlin (present day Brunswick), briefly skirmished with Confederate cavalry near Waterford and retired to Hillsboro. Seeing that he could pin Early between himself and the force under Crook in the Loudoun Valley, Wright determined to cross the Potomac the following morning and ensnare Early in the Federal pincers.

Geographic entities mentioned:
surface_form: Loudoun Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.2329
lon: -77.735
Confederate withdrawal and Union reconnaissance. The morning of July 16, with the Federals closing in, General Early broke camp at Leesburg and set out for the Shenandoah Valley by way of Snickers Gap which lay some 20 miles across the Loudoun Valley via the Snickers Gap and Leesburg Pike. While his main army and wagon trains used that route to withdrawal, cavalry under Brig. Gen. Bradley T.

Geographic entities mentioned:
surface_form: Loudoun Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.2329
lon: -77.735
Cody Lake (Minnesota). Cody Lake is a lake in Rice County, in the U.S. state of Minnesota. Cody Lake was named for Patrick Cody, an early settler.

Geographic entities mentioned:
surface_form: cody lake
instance_of: Lake
countries: United States
coordinates: lat: 44.4625
lon: -93.49666667
E.A. Wallis Budge adds the tradition that Jin Asgad initiated the use of Amba Geshen as a royal prison for troublesome relatives of the Emperor, when he was forced to imprison his treacherous brother Saba Asgad; at the same time he imprisoned his other three brothers and his own sons in Amba Geshen. Whatever the succession situation truly was, it came to an end when Wedem Arad seized the throne.

Geographic entities mentioned:
surface_form: Amba Geshen
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 11.4986
lon: 39.3184
It is found in Italy, Slovenia and Switzerland. Its natural habitats are rivers and freshwater lakes. It is threatened by habitat loss and predation and competition from introduced species such as roach, wels catfish and the common nase. It has been extirpated from Slovenia and numbers are declining in the Italian and Swiss lakes of Lake Como, Lake Lugano, Lake Maggiore, Lake Iseo and Lake Garda.

Geographic entities mentioned:
surface_form: Lake Lugano
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46
lon: 9
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
surface_form: Lake Iseo
instance_of: Lake
countries: Italy
coordinates: lat: 45.711666666667
lon: 10.071944444444
surface_form: Lake Garda
instance_of: Lake
countries: Italy
coordinates: lat: 45.633333333333
lon: 10.666666666667
Jacques Nicolas Ernest Germain de Saint-Pierre. rbw5a22knitss458wenft2tecyil5" xml:space="preserve">Jacques Nicolas Ernest Germain de Saint-Pierre (1 December 1814, Saint-Pierre-le-Moûtier &ndash; 28 June 1882, Hyères) was a French botanist.

Geographic entities mentioned:
surface_form: Hyères
instance_of: Mountain
countries: France
coordinates: lat: 43.118888888889
lon: 6.1286111111111
Technical. BBC Radio York broadcasts from its studios in York and uses three FM transmitters. The station broadcasts on 95.5 (Oliver's Mount, Scarborough), 103.7 (Acklam Wold transmitter near Leavening, midway between York and Malton) which is for Ryedale and the Vale of York.

Geographic entities mentioned:
surface_form: Vale of York
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.95
lon: -1.0833333333333333
During the Battle of Missionary Ridge on 25 November, Gibson's was the right-most brigade in Stewart's defenses on the ridge. Missionary Ridge is an imposing natural feature, but overconfident Breckinridge and army commander General Braxton Bragg completely mismanaged the Confederate defenses. When the Federals attacked the ridge, the brigades to Gibson's right began to break up and scatter.

Geographic entities mentioned:
surface_form: Missionary Ridge
instance_of: Landform
countries: United States
coordinates: lat: 34.986388888889
lon: -85.278611111111
Geography. Williamsfield is situated in northeastern Ohio near the Pennsylvania state border. The region features gently rolling terrain, agricultural fields, and wooded areas. It lies within the Great Lakes Basin, approximately 20 miles south of Lake Erie. Small streams and creeks flow through the community, enhancing its scenic rural environment. Economy.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
She headed the Centre Party electoral list in Oppland for the 2021 election. In 2025, she announced that she wouldn't be seeking re-election at that year's election due to family reasons. Personal life. She and her family reside in Valdres. She has three children.

Geographic entities mentioned:
surface_form: Valdres
instance_of: Valley
countries: Norway
coordinates: lat: 60.916666666667
lon: 9.1666666666667
Chenoweth in an attempt to contact Friend. In 1916, Hyslop wrote that the whole case for Pearl Curran's mediumship was based on fraud. Hyslop in the &quot;Journal for the American Society for Psychical Research&quot; claimed that Curran had known people from the Ozarks who spoke a dialect reminiscent of Patience Worth and Curran's husband had studied Chaucer and educated her on the subject.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
Legend. According to Sri Vaishnava tradition, Tiruppan Alvar was once singing the praises of Vishnu along the ghats of the river Kaveri, in front of the Ranganathaswamy temple in Srirangam. He was immersed in his chants of ecstasy to such an extent that he fell unconscious, alongside his veena.

Geographic entities mentioned:
surface_form: Kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
Ethnonyms. Chin (ချင်း, MLCTS: khyang:) is a pseudo-exonym, a Burmese language adaptation of the Asho Chin word &quot;khlong&quot; or &quot;khlaung&quot;, which means &quot;man&quot; or &quot;person.&quot; Burmese speakers approximated the Asho Chin word, and began to apply the exonym to all nearby groups residing in the Arakan Mountains and Chin Hills.

Geographic entities mentioned:
surface_form: Chin Hills
instance_of: Mountain
countries: Myanmar
coordinates: lat: 22.5
lon: 93.5
Durochertoppen. Durochertoppen is a mountain peak in Wedel Jarlsberg Land at Spitsbergen, Svalbard. Location. It has a height of 782 m.a.s.l. and is located in the Martinfjella mountain range. The summit is named after French geologist Joseph Marie Elisabeth Durocher.

Geographic entities mentioned:
surface_form: durochertoppen
instance_of: Mountain
countries: Norway
coordinates: lat: 77.4788
lon: 14.8834
Kedron Creek. Kedron Creek is a stream in the U.S. state of Minnesota. The stream was named after the Kidron Valley near Jerusalem.

Geographic entities mentioned:
surface_form: Kidron Valley
instance_of: Valley
countries: State of Palestine
coordinates: lat: 31.776972222222224
lon: 35.23897222222222
Around 1850, the residents of Roaring Fork constructed a crude road connecting the area to White Oak Flats (this old road is now a stop along the Roaring Fork Motor Nature Trail). By 1900, the community had matured into a mountain hamlet with its own school, church, general store, and tub mills. In 1976, the Roaring Fork Historic District was listed on the National Register of Historic Places.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
Uppermost on Roaring Fork, near where the stream absorbs Surry Creek, were farms owned by the Clabo family, Gilbert Ogle, and Jasper Mellinger. Former homesteads can usually be identified by the preponderance of young tuliptrees (rather than the more common hemlock or oak), as tuliptrees are the quickest to reclaim previously cultivated land.

Geographic entities mentioned:
surface_form: hemlock
instance_of: Lake
countries: United States
coordinates: lat: 42.718611111111
lon: -77.608888888889
From its source, Roaring Fork drops over just, spilling over Grotto Falls and absorbing Surry Creek before steadying in a narrow valley between Mount Winnesoka and Piney Mountain. The mouth of Roaring Fork is located at the northern end of Gatlinburg, where it empties into the West Fork of the Little Pigeon River.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
Over thousands of years, erosional forces have carried boulders composed of this sandstone down from boulder fields located higher up along the mountain ridges. This process has left the streambed of Roaring Fork and the flats in the Roaring Fork valley virtually covered with sandstone rocks of all sizes.

Geographic entities mentioned:
surface_form: roaring fork valley
instance_of: Valley
countries: United States
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
The Roaring Fork valley is underlain by Precambrian sandstone of the Ocoee Supergroup, a rock formation formed from ancient ocean sediments nearly a billion years ago. Roaring Fork Sandstone is found throughout the mid-level elevations of the northern Smokies and is especially common in Greenbrier to the east and the Sugarlands to the west.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
This process has left the streambed of Roaring Fork and the flats in the Roaring Fork valley virtually covered with sandstone rocks of all sizes. Farmers who lived at Roaring Fork, the Sugarlands, and Greenbrier were continually moving and stacking these rocks, creating the characteristic rock walls that still criss-cross these areas today. Roaring Fork Historic District.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
Patches of young tuliptrees mark the former location of the Clabo and Ogle farms. Immediately after the road crosses Roaring Fork, the Jim Bales Place is visible on the right (east). The Grapeyard Ridge Trail, which connects Roaring Fork to Greenbrier, begins just behind the barn. Past the Jim Bales Place are the Ephraim Bales Place and Alfred Reagan Place.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
Roaring Fork (Great Smoky Mountains). Roaring Fork is a stream in the Great Smoky Mountains of Tennessee, located in the southeastern United States. Once the site of a small Appalachian community, today the stream's area is home to the Roaring Fork Motor Nature Trail and the Roaring Fork Historic District. Like many mountain streams, Roaring Fork is volatile.

Geographic entities mentioned:
surface_form: roaring fork (great smoky mountains)
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
Roaring Fork (Great Smoky Mountains). Roaring Fork is a stream in the Great Smoky Mountains of Tennessee, located in the southeastern United States. Once the site of a small Appalachian community, today the stream's area is home to the Roaring Fork Motor Nature Trail and the Roaring Fork Historic District. Like many mountain streams, Roaring Fork is volatile.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
Roaring Fork (Great Smoky Mountains). Roaring Fork is a stream in the Great Smoky Mountains of Tennessee, located in the southeastern United States. Once the site of a small Appalachian community, today the stream's area is home to the Roaring Fork Motor Nature Trail and the Roaring Fork Historic District. Like many mountain streams, Roaring Fork is volatile.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
Once the site of a small Appalachian community, today the stream's area is home to the Roaring Fork Motor Nature Trail and the Roaring Fork Historic District. Like many mountain streams, Roaring Fork is volatile. While the stream presents as a peaceful trickle on any given day, it quickly becomes a raging whitewater rapid after a mild rain shower.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
The &quot;roar&quot; of the water is amplified by its echo on surrounding mountain ridges. Geography. The source of Roaring Fork is located nearly up along the northern slopes of Mount Le Conte, where several small springs converge. The highest of these springs, known as Basin Spring, provides the water source for LeConte Lodge.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
The highest of these springs, known as Basin Spring, provides the water source for LeConte Lodge. From its source, Roaring Fork drops over just, spilling over Grotto Falls and absorbing Surry Creek before steadying in a narrow valley between Mount Winnesoka and Piney Mountain.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
The mouth of Roaring Fork is located at the northern end of Gatlinburg, where it empties into the West Fork of the Little Pigeon River. The Roaring Fork valley is underlain by Precambrian sandstone of the Ocoee Supergroup, a rock formation formed from ancient ocean sediments nearly a billion years ago.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
Some of Reagan's children settled to the west in the Sugarlands, while some of them moved east to the hollow along Roaring Fork, which was then known as &quot;Spruce Flats.&quot; By 1900, three of Reagan's grandsons, Alfred Reagan (1856–1928), Aaron Reagan, and John H. Reagan were still farming along the stream, just above Gatlinburg.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
Reagan were still farming along the stream, just above Gatlinburg. The Bales family settled in the upper section of Roaring Fork sometime in the 1830s or earlier. Caleb Bales (1839–1913), apparently a son or nephew of the first Bales to settle on Roaring Fork, owned a farm just south of the Reagan lands.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
The Bales family settled in the upper section of Roaring Fork sometime in the 1830s or earlier. Caleb Bales (1839–1913), apparently a son or nephew of the first Bales to settle on Roaring Fork, owned a farm just south of the Reagan lands. Caleb's sons Jim Bales (1869–1939) and Ephraim Bales (1867–1936) would spend most of their lives on Roaring Fork farming land inherited from their father.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
Caleb Bales (1839–1913), apparently a son or nephew of the first Bales to settle on Roaring Fork, owned a farm just south of the Reagan lands. Caleb's sons Jim Bales (1869–1939) and Ephraim Bales (1867–1936) would spend most of their lives on Roaring Fork farming land inherited from their father. As the Bales and Reagan families lived on adjoining lands, the families intermarried.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
Former homesteads can usually be identified by the preponderance of young tuliptrees (rather than the more common hemlock or oak), as tuliptrees are the quickest to reclaim previously cultivated land. Around 1850, the residents of Roaring Fork constructed a crude road connecting the area to White Oak Flats (this old road is now a stop along the Roaring Fork Motor Nature Trail).

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
In 1976, the Roaring Fork Historic District was listed on the National Register of Historic Places. Jim Bales Place. The first historic stop along the Roaring Fork Motor Nature Trail is the Jim Bales Place, a farm which Jim Bales inherited from his father, Caleb. Jim, born James Wesley Bales in 1869, lived here for much of his life.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
Alfred Reagan Place. Alfred Reagan, a descendant of the area's first settlers, owned a small farm just below the Ephraim Bales Place. Reagan was a jack-of-all-trades, operating the Roaring Fork community's blacksmith shop, general store, and its most consistent grist mill. Reagan was also a part-time preacher at the Roaring Fork Church, for which he donated the land and helped build.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
Reagan was a jack-of-all-trades, operating the Roaring Fork community's blacksmith shop, general store, and its most consistent grist mill. Reagan was also a part-time preacher at the Roaring Fork Church, for which he donated the land and helped build. Of all the buildings on Reagan's farm, only his cabin and mill remain today.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
The cabin's design is known as a &quot;saddlebag&quot; design, which involves two cabins constructed around a single chimney. A kitchen area was added later. The Reagan mill is a standard tub mill, with a flume directing water from Roaring Fork to power a tub-wheel turbine. The turbine turns a grindstone which breaks down corn and wheat into cornmeal and flour.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
Alex Cole Cabin. The Alex Cole Cabin is the last surviving structure from the Sugarlands community proper. Built by mountain guide Albert Alexander Cole, it has been moved from its original site to the Jim Bales Place along the Roaring Fork Motor Nature Trail. Motor Nature Trail.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
Trillium Gap—the gap between Brushy Mountain and the main Le Conte massif—was named by Horace Albright, who observed the trillium-filled area in the 1920s. Past the Trillium Gap Trailhead, the road enters the upper reaches of the Roaring Fork hollow. Patches of young tuliptrees mark the former location of the Clabo and Ogle farms.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
Past the Trillium Gap Trailhead, the road enters the upper reaches of the Roaring Fork hollow. Patches of young tuliptrees mark the former location of the Clabo and Ogle farms. Immediately after the road crosses Roaring Fork, the Jim Bales Place is visible on the right (east). The Grapeyard Ridge Trail, which connects Roaring Fork to Greenbrier, begins just behind the barn.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
Past the Jim Bales Place are the Ephraim Bales Place and Alfred Reagan Place. The road continues to descend past the historic district, passing along the way a parking lot that allows for a view of Roaring Fork. A thin waterfall known as &quot;The Place of a Thousand Drips&quot; is the last stop along the motor trail before it re-enters Gatlinburg.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
Dundas became commanding officer under Lord Hood after O’Hara's capture in this action. He lost Fort Mulgrave and Mount Faron after a 3-day bombardment on 17 December 1793. Dundas commanded the initial expedition to Corsica in 1794, landing 7 February 1794 and capturing the Mortella Tower.

Geographic entities mentioned:
surface_form: Mount Faron
instance_of: Mountain
countries: France
coordinates: lat: 43.149444444444
lon: 5.9511111111111
In its early years, Arlington was a thriving farming community and had its own lettuce that was quite popular. Arlington had a large ice industry on Spy Pond from the mid-19th century until the last ice house burned down in 1930; much of its ice was sent to the Caribbean and India by &quot;Ice King&quot; Frederic Tudor. Arlington's population grew by over 90 percent during the 1920s.

Geographic entities mentioned:
surface_form: Spy Pond
instance_of: Lake
countries: United States
coordinates: lat: 42.407777777778
lon: -71.156111111111
There are 210.52 acres (0.9 km2) of parkland. Elevation ranges from 4 feet (1.2 m) above sea level (along Alewife Brook) to 377 feet (114.9 m) near Park Avenue and Eastern Avenue. Arlington borders on the Mystic Lakes, Mystic River, and Alewife Brook. Within its borders are Spy Pond, the Arlington Reservoir, Mill Brook, and Hills Pond. Adjacent municipalities.

Geographic entities mentioned:
surface_form: Spy Pond
instance_of: Lake
countries: United States
coordinates: lat: 42.407777777778
lon: -71.156111111111
It is found in north-west Madagascar. The male of this species has a wingspan of 33 mm. Head, front and are yellow, thorax straw yellow, antennae yellow and dark brown strongly pectinated, abdomen dirty yellow. The forewings are white, almost translucent, hindwings white, shaded grey. The holotype was found near Ambanja, Sambirano River, Ankarafantsika National Park at an altitude of 250 m.

Geographic entities mentioned:
surface_form: Sambirano River
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -13.61722222
lon: 48.33361111
Loch Arkaig treasure. The treasure of Loch Arkaig, sometimes known as the Jacobite gold, was a large amount of specie provided by Spain to finance the Jacobite rising in Scotland in 1745, and rumoured still to be hidden at Loch Arkaig in Lochaber. Background. In 1745, Prince Charles Edward Stuart (Bonnie Prince Charlie) arrived in Scotland from France.

Geographic entities mentioned:
surface_form: Loch Arkaig
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.971989
lon: -5.158376
Cluny was hiding in a cave at Ben Alder, which came to be known as &quot;the cage&quot;, and when Charles briefly joined him there, Cluny had control of the money, which was still hidden at Arkaig. Treasure hunt. Charles finally escaped Scotland in the French frigate &quot;L'Heureux&quot; and arrived back in France in September 1746. However, the fate of the money is not as clear.

Geographic entities mentioned:
surface_form: Ben Alder
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.813796
lon: -4.465089
In 1753, Archibald Cameron—Lochiel's brother, who was acting as secretary to the Old Pretender—was sent back to Scotland to locate the treasure. However, whilst staying secretly at Brenachyle by Loch Katrine, he was betrayed (apparently by the notorious &quot;Pickle&quot;, a Hanoverian spy) and arrested.

Geographic entities mentioned:
surface_form: Loch Katrine
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.254444444444445
lon: -4.515555555555555
The river originates in the Porcupine Hills and flows northward towards the town of Hudson Bay and into the Red Deer River. &quot;Etomami&quot; is a First Nations word that means &quot;a place that three rivers join&quot;. It is in reference to the spot along the Red Deer River where the mouths of the Etomami and Fir Rivers meet the Red Deer River. Description.

Geographic entities mentioned:
surface_form: Fir River
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.81876
lon: -102.37866
It is in reference to the spot along the Red Deer River where the mouths of the Etomami and Fir Rivers meet the Red Deer River. Description. The river's source is at the north end of the bifurcating Etomami Lake in the RM of Preeceville No. 334 and flows northward through a deep-cut valley into the RM of Hudson Bay No. 394 following the Canadian National Railway and Highway 9.

Geographic entities mentioned:
surface_form: Etomami Lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.24999
lon: -102.65048
surface_form: etomami lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.24999
lon: -102.65048
394 following the Canadian National Railway and Highway 9. The south end of the lake is the source of the Lilian River, which flows south into the Assiniboine River. In 1691, Hudson's Bay Company fur trader and explorer Henry Kelsey traversed the length of the Etomami River while in search of a route to the aspen parkland region.

Geographic entities mentioned:
surface_form: Lilian River
instance_of: Watercourse
countries: Canada
coordinates: lat: 51.93328
lon: -102.55095
surface_form: assiniboine
instance_of: Mountain
countries: Canada
coordinates: lat: 50.86972222222222
lon: -115.6511111111111
surface_form: lilian river
instance_of: Watercourse
countries: Canada
coordinates: lat: 51.93328
lon: -102.55095
In 1691, Hudson's Bay Company fur trader and explorer Henry Kelsey traversed the length of the Etomami River while in search of a route to the aspen parkland region. Following a trail known to be used by the local Indigenous peoples, at Etomami Lake, he crossed over to the Lilian River system.

Geographic entities mentioned:
surface_form: lilian river
instance_of: Watercourse
countries: Canada
coordinates: lat: 51.93328
lon: -102.55095
surface_form: etomami lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.24999
lon: -102.65048
Etomami River. Etomami River is a river in the Canadian province of Saskatchewan. The river originates in the Porcupine Hills and flows northward towards the town of Hudson Bay and into the Red Deer River. &quot;Etomami&quot; is a First Nations word that means &quot;a place that three rivers join&quot;.

Geographic entities mentioned:
surface_form: etomami river
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.32811
lon: -96.88732
394 following the Canadian National Railway and Highway 9. The south end of the lake is the source of the Lilian River, which flows south into the Assiniboine River. In 1691, Hudson's Bay Company fur trader and explorer Henry Kelsey traversed the length of the Etomami River while in search of a route to the aspen parkland region.

Geographic entities mentioned:
surface_form: etomami river
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.32811
lon: -96.88732
An attack by Native Americans on July 14 killed 15 of Smith's party. One man escaped by heading north to Tillamook and then Fort Vancouver. Smith and two others who were not in camp at the time of the attack fled east toward the Willamette Valley and survived. The Smith River in California is also named for Smith. Tributaries.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Bake Oven Knob. Bake Oven Knob is a high point on the Blue Mountain ridge of the Appalachian Mountains near Germansville, Pennsylvania. Due to its location on the Appalachian Trail and proximity to many towns in the Lehigh Valley metropolitan area, it has become a popular spot for hiking. Hiking. Bake Oven Knob is a relatively accessible location on the Appalachian Trail.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Bake Oven Knob. Bake Oven Knob is a high point on the Blue Mountain ridge of the Appalachian Mountains near Germansville, Pennsylvania. Due to its location on the Appalachian Trail and proximity to many towns in the Lehigh Valley metropolitan area, it has become a popular spot for hiking. Hiking. Bake Oven Knob is a relatively accessible location on the Appalachian Trail.

Geographic entities mentioned:
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.95481
lon: -123.25907
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.924722222222
lon: -74.288055555556
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.3209
lon: -74.6616
surface_form: bake oven knob
instance_of: Mountain
countries: United States
coordinates: lat: 40.748611111111
lon: -75.733888888889
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.8725
lon: -74.401111111111
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.5456079
lon: -90.4940088
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.8482
lon: -120.198
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.8158
lon: -114.186
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1469
lon: -74.8489
Bake Oven Knob. Bake Oven Knob is a high point on the Blue Mountain ridge of the Appalachian Mountains near Germansville, Pennsylvania. Due to its location on the Appalachian Trail and proximity to many towns in the Lehigh Valley metropolitan area, it has become a popular spot for hiking. Hiking. Bake Oven Knob is a relatively accessible location on the Appalachian Trail.

Geographic entities mentioned:
surface_form: bake oven knob
instance_of: Mountain
countries: United States
coordinates: lat: 40.748611111111
lon: -75.733888888889