Sarmila/GeoWiki-Features huggingface dataset:
Mark Kitto. Mark Kitto is a British magazine publisher, writer and actor notable for living in the People's Republic of China. During his time in China he initially lived in Shanghai before relocating to Mount Mogan where he ran a coffee shop, restaurant and three guest houses. In 2013 he announced his intention to leave, citing the welfare of his children as the deciding factor.

Geographic entities mentioned:
surface_form: Mount Mogan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 30.63333333
lon: 119.83333333
Anabarilius polylepis. &quot;Anabarilius polylepis&quot; s a species of freshwater ray-finned fish belonging to the family Xenocyprididae, the East Asian minnows or sharpbellies. This species is endemic to Yunnan, China. It only occurs in Dian Lake and Songhuaba reservoir in Kunming. It was once a major commercial fish species, but it has not been confirmed in the lake since the 1970s.

Geographic entities mentioned:
surface_form: Dian Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 24.800555555556
lon: 102.67138888889
For her new assignment, she departed Sasebo on 22 July 1942 bound for Penang, making a stop at Cam Ranh Bay along the way. Fifth and sixth war patrols. &quot;I-162&quot; departed Penang on 23 August 1942 to conduct her fifth war patrol, targeting Allied shipping in the Bay of Bengal. The patrol was uneventful, and she returned to Penang on 12 September 1942.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
The highway then descends along the coast towards Squamish at the head of Howe Sound. It passes a ferry terminal at Darrell Bay and the viewpoint for Shannon Falls, the third-highest waterfall in the province at. Highway 99 passes under Stawamus Chief, a large mountain immediately outside of Squamish, and travels through the city's residential neighbourhoods.

Geographic entities mentioned:
surface_form: Stawamus Chief
instance_of: Mountain
countries: Canada
coordinates: lat: 49.6867
lon: -123.135
This section of road parallels several rivers and water bodies, including the Squamish River, the Cheakamus River, and Daisy Lake, which flow south toward Howe Sound. In Whistler, near Alta Lake, the road crosses a watershed, and north of this point, the road follows the Green River and Lillooet River which flow north and east toward Lillooet Lake, and ultimately towards the Fraser River.

Geographic entities mentioned:
surface_form: Lillooet Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.25
lon: -122.5
After passing Lillooet Lake, the highway climbs a steep grade to Joffre Lakes Provincial Park, and shortly after passes through Cayoosh Pass, the highest point on the highway at. East of the pass the road follows the course of Cayoosh Creek as it traverses the southern base of Mount Rohr and skirts Duffey Lake Provincial Park.

Geographic entities mentioned:
surface_form: Mount Rohr
instance_of: Mountain
countries: Canada
coordinates: lat: 50.3989
lon: -122.4085
King George Highway. The modern-day highways between the Peace Arch Border Crossing and New Westminster generally follow the Semiahmoo Trail, an overland route used by indigenous Coast Salish peoples that was later adopted by fur traders and early non-indigenous Fraser Valley settlers in the 1860s. The trail was replaced with a wagon road that was completed by the provincial government in 1879.

Geographic entities mentioned:
surface_form: Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
The existing route from Squamish to Lillooet was long and mostly unpaved, with some sections that required vehicles with four-wheel drive to negotiate the terrain. Construction of an all-season gravel road to Alta Lake at the base of Whistler Mountain was announced in March 1962 as part of a larger development plan for a ski area that could host the Winter Olympics.

Geographic entities mentioned:
surface_form: Whistler Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.059166666667
lon: -122.95694444444
The provincial government provided funding for maintenance for several years before formally taking control on April 1, 1979. Early concepts for an extension of Highway 99 to Lillooet in the 1960s included a ferry to cross Anderson and Seton lakes. Paving of Duffey Lake Road began in 1990 and was mostly completed by the end of the following year at a cost of $22.5 million.

Geographic entities mentioned:
surface_form: Seton
instance_of: Lake
countries: Canada
coordinates: lat: 50.7
lon: -122.167
A major reconstruction of the highway, including widening sections to four lanes between Horseshoe Bay and Squamish, was proposed by political leaders in 1981 following the death of nine people who had driven off a washed out wooden bridge over M Creek. At the time, the Sea to Sky Highway had five wooden bridges that had yet to be replaced.

Geographic entities mentioned:
surface_form: M Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.48
lon: -123.24472222
The bid also considered a new highway to bypass parts of the corridor, including a tunnel under Grouse Mountain or a toll road through Indian Arm, but they were not advanced for further planning. A large section had already been upgraded between Squamish and Whistler in 2002, prior to the Olympics being awarded, to improve upon work done during the 1980s.

Geographic entities mentioned:
surface_form: Grouse Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.38611111
lon: -123.07638889
Kings House Hotel. The Kings House Hotel is a remote inn at the eastern end of Glen Coe in the Scottish Highlands. The inn, which is in an isolated position about 2 km east of Glen Etive, stands on the edge of Rannoch Moor. It faces Buachaille Etive Mor which makes it a popular hostelry with rock climbers.

Geographic entities mentioned:
surface_form: Glen Etive
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.601111111111
lon: -5.0058333333333
The strategic military road crossed the River Etive at this point by the inn. The military route, built by the British army in the aftermath of the 1745 Jacobite rising, then headed towards Glen Coe before ascending the Devil's Staircase to Kinlochleven. Parts of the former military route are now used as the West Highland Way.

Geographic entities mentioned:
surface_form: Devil's Staircase
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.679497
lon: -5.012554
From Aklan to the destination, the team travels 4 hours by boat. The following day, the host explores Magdiwang's Sibuyan forest using mountain bike. On his way, he passes Mount Guiting-Guiting or G2. He also visits Lambingan Falls, a community-based eco-tourism. From Magdiwang, the host visits San Fernando's Ikaduha Fish Sanctuary where he tries snorkeling.

Geographic entities mentioned:
surface_form: Mount Guiting-Guiting
instance_of: Mountain
countries: Philippines
coordinates: lat: 12.413888888889
lon: 122.56777777778
It is located north east of the tourism capital, Livingstone, and from Kitwe on the Copperbelt, Zambia's second-largest city. Mpulungu, the most distant major Zambian town from Lusaka, lies away on the shores of Lake Tanganyika. The city of Lusaka is coterminous with Lusaka District, and is the capital of Lusaka Province, which is Zambia's smallest but most populated province.

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
Tectonic setting. Yunnan lies at the southeastern boundary of the Tibetan Plateau where strike-slip faults accommodate crustal rotation resulting from deformation caused by the ongoing collision between the Indian Plate and the Eurasian Plate which formed the Himalayas and the Tibetan Plateau. The presence of active faults make the region prone to moderate to large earthquakes.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
It was named after Edward Stanley, who was three times British prime minister in the 1850s and 1860s. It is bounded by the Logan River in the south, the Brisbane River at what is now Lake Wivenhoe in the west, the Stanley River at what is now Lake Somerset in the north-west, and Caboolture River in the north.

Geographic entities mentioned:
surface_form: Lake Wivenhoe
instance_of: Lake
countries: Australia
coordinates: lat: -27.25
lon: 152.51666666667
R. Atterbury, Edward Warren, James Morgan and Owen Turner. Some of these pioneers were unmarried, which was another reason they could only claim. An 1851 map of the Willamette Valley notes &quot;Gopher Hole&quot; at this location. There was an early attempt by Mrs. Charles Shortridge to change the name to Lebanon Valley, but the settlers had grown accustomed to Gopher.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
surface_form: willamette valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
The earliest school was about halfway up the valley, and while it was referred to as the Lebanon Valley School District 36 in the early 1880s, the &quot;Yamhill Reporter&quot; (published in McMinnville) called this the Gopher Valley school in an 1886 article. School District 42, known as Fremont and later as the McKinley school, was established at about the same time.

Geographic entities mentioned:
surface_form: mckinley
instance_of: Mountain
countries: United States
coordinates: lat: 63.06916666666667
lon: -151.0063888888889
Most of these early &quot;Gopherites&quot; claimed, while later settlers could only claim half that amount, due to changes in the Donation Land Claim Act after 1850. Among the earliest settlers were Stephen Hussey, Joseph Pearson, William Toney, Peter Carlisle, Edward Warren, Green P. R. Atterbury, Edward Warren, James Morgan and Owen Turner.

Geographic entities mentioned:
surface_form: carlisle
instance_of: Mountain
countries: United States
coordinates: lat: 52.8939
lon: -170.054
Gopher Valley. Gopher Valley is a valley in Yamhill County, Oregon, United States. Gopher, Oregon was an unincorporated locale in the valley. Gopher post office ran from April 6, 1899 to September 14, 1905, with Edward H. Taylor first postmaster. Geography. Gopher Valley is located on hills on the north side of Oregon Route 18 about two miles (3 km) east of Sheridan.

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
surface_form: gopher, oregon
instance_of: Valley
countries: United States
coordinates: lat: 45.1475
lon: -123.39
Geography. Gopher Valley is located on hills on the north side of Oregon Route 18 about two miles (3 km) east of Sheridan. Gopher Valley rises in elevation from at the south end to over at the peaks of the hills, encompassing fertile farmland and timber. The Gopher Valley is about in area. Deer Creek meanders through the valley on its way to the South Yamhill River. History.

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
History. The first settlers did not take up claims in the valley until 1850, some seven years after the arrival of the first settlers in the nearby Yamhill Valley. Most of these early &quot;Gopherites&quot; claimed, while later settlers could only claim half that amount, due to changes in the Donation Land Claim Act after 1850.

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
Furthermore, the town of Lebanon in Linn County was already established. There has been some speculation that the name was based on the shape of the valley as seen from the air, but this hardly seems possible given the lack of topographic maps or aircraft to determine the actual shape (which does not resemble the shape of any animal).

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
The earliest school was about halfway up the valley, and while it was referred to as the Lebanon Valley School District 36 in the early 1880s, the &quot;Yamhill Reporter&quot; (published in McMinnville) called this the Gopher Valley school in an 1886 article. School District 42, known as Fremont and later as the McKinley school, was established at about the same time.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: lebanon valley
instance_of: Valley
countries: United States
coordinates: lat: 40.453
lon: -76.493
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
surface_form: gopher valley
instance_of: Valley
countries: United States
coordinates: lat: 45.1475
lon: -123.39
School District 42, known as Fremont and later as the McKinley school, was established at about the same time. This school was near the intersection of Grauer Road and Gopher Valley Road. A third valley school, originally known as Ryan’s Mill (District 82) was established in 1894 about up the valley. By 1933 this was called the Osman School, but after that it was known as the Deer Creek School.

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
One of the first was Ryan’s Mill, followed by Stowe’s Mill, and later by Thomson’s Mill, for which a road leading to the west, and connecting to the upper end of Rock Creek Road, is named. Most of these mills were in the north end of the valley, with one exception: at one time, a flume carried logs down the valley to a sawmill.

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: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
One of the old timers who left a lasting impression with everyone he met was Red Snyder. Red went to work at Stow’s Mill shortly after moving onto his place in the upper end of the valley in 1908 or 1910. He lived the rest of his life in the valley, except for a stint in the Army during World War I.

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
Red went to work at Stow’s Mill shortly after moving onto his place in the upper end of the valley in 1908 or 1910. He lived the rest of his life in the valley, except for a stint in the Army during World War I. Red was a colorful character, to say the least, and his memories of people and events up the valley were repeated often to any listener with time on their hands.

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
He lived the rest of his life in the valley, except for a stint in the Army during World War I. Red was a colorful character, to say the least, and his memories of people and events up the valley were repeated often to any listener with time on their hands. Red recalled deer and elk rampaging through the valley in the mid-1930s, as they tried to escape the Tillamook Burn.

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
Red was a colorful character, to say the least, and his memories of people and events up the valley were repeated often to any listener with time on their hands. Red recalled deer and elk rampaging through the valley in the mid-1930s, as they tried to escape the Tillamook Burn. There are at least two pioneer cemeteries up the valley, one on the Agee claim and the other on the Hussey claim.

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
Much of the clothing worn by the men was made from animal hides. Raising a family and getting food on the table were the first priorities. Electricity was brought into the upper end of the valley in the early 1940s. As recently as the 1960s, annual community potlucks were held at least one Sunday afternoon in the summer.

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
Some of these pioneers were unmarried, which was another reason they could only claim. An 1851 map of the Willamette Valley notes &quot;Gopher Hole&quot; at this location. There was an early attempt by Mrs. Charles Shortridge to change the name to Lebanon Valley, but the settlers had grown accustomed to Gopher. Furthermore, the town of Lebanon in Linn County was already established.

Geographic entities mentioned:
surface_form: lebanon valley
instance_of: Valley
countries: United States
coordinates: lat: 40.453
lon: -76.493
Gopher Valley. Gopher Valley is a valley in Yamhill County, Oregon, United States. Gopher, Oregon was an unincorporated locale in the valley. Gopher post office ran from April 6, 1899 to September 14, 1905, with Edward H. Taylor first postmaster. Geography. Gopher Valley is located on hills on the north side of Oregon Route 18 about two miles (3 km) east of Sheridan.

Geographic entities mentioned:
surface_form: gopher valley
instance_of: Valley
countries: United States
coordinates: lat: 45.1475
lon: -123.39
Gopher post office ran from April 6, 1899 to September 14, 1905, with Edward H. Taylor first postmaster. Geography. Gopher Valley is located on hills on the north side of Oregon Route 18 about two miles (3 km) east of Sheridan. Gopher Valley rises in elevation from at the south end to over at the peaks of the hills, encompassing fertile farmland and timber. The Gopher Valley is about in area.

Geographic entities mentioned:
surface_form: gopher valley
instance_of: Valley
countries: United States
coordinates: lat: 45.1475
lon: -123.39
Taylor first postmaster. Geography. Gopher Valley is located on hills on the north side of Oregon Route 18 about two miles (3 km) east of Sheridan. Gopher Valley rises in elevation from at the south end to over at the peaks of the hills, encompassing fertile farmland and timber. The Gopher Valley is about in area. Deer Creek meanders through the valley on its way to the South Yamhill River.

Geographic entities mentioned:
surface_form: gopher valley
instance_of: Valley
countries: United States
coordinates: lat: 45.1475
lon: -123.39
Geography. Gopher Valley is located on hills on the north side of Oregon Route 18 about two miles (3 km) east of Sheridan. Gopher Valley rises in elevation from at the south end to over at the peaks of the hills, encompassing fertile farmland and timber. The Gopher Valley is about in area. Deer Creek meanders through the valley on its way to the South Yamhill River. History.

Geographic entities mentioned:
surface_form: gopher valley
instance_of: Valley
countries: United States
coordinates: lat: 45.1475
lon: -123.39
School District 42, known as Fremont and later as the McKinley school, was established at about the same time. This school was near the intersection of Grauer Road and Gopher Valley Road. A third valley school, originally known as Ryan’s Mill (District 82) was established in 1894 about up the valley. By 1933 this was called the Osman School, but after that it was known as the Deer Creek School.

Geographic entities mentioned:
surface_form: gopher valley
instance_of: Valley
countries: United States
coordinates: lat: 45.1475
lon: -123.39
Edward H. Taylor was the only postmaster serving the community of Gopher, after having been appointed in 1895. In that year, area citizens could pick up their mail at his house, about six miles (10 km) from Sheridan, on the east side of Gopher Valley Road. He later moved to the Hussey home, relocating the office to a small room near the front entry.

Geographic entities mentioned:
surface_form: gopher valley
instance_of: Valley
countries: United States
coordinates: lat: 45.1475
lon: -123.39
A window and letter slots were cut into the wall. Different sources report receiving mail via stage three to seven times each week. Perhaps the delivery days had increased by the time the office was officially discontinued in 1905. The timber industry boomed in the later days of the 19th century into the 1900s, and a number of lumber mills were established in Gopher Valley over the decades.

Geographic entities mentioned:
surface_form: gopher valley
instance_of: Valley
countries: United States
coordinates: lat: 45.1475
lon: -123.39
There are at least two pioneer cemeteries up the valley, one on the Agee claim and the other on the Hussey claim. The Agee Cemetery is the larger of the two, taking up about an acre of land about a half-mile beyond the end of the pavement and west of Gopher Valley Road, near Deer Creek. Isaac Agee and his wife Cordilla (Thornton) Agee are buried there.

Geographic entities mentioned:
surface_form: gopher valley
instance_of: Valley
countries: United States
coordinates: lat: 45.1475
lon: -123.39
In that year, area citizens could pick up their mail at his house, about six miles (10 km) from Sheridan, on the east side of Gopher Valley Road. He later moved to the Hussey home, relocating the office to a small room near the front entry. A window and letter slots were cut into the wall. Different sources report receiving mail via stage three to seven times each week.

Geographic entities mentioned:
surface_form: the wall
instance_of: Mountain
countries: United States
coordinates: lat: 43.8831
lon: -110.838
Located in San Gabriel, California, the school primarily serves families living in the Pasadena, San Marino, Arcadia areas, but also draws many families from La Cañada Flintridge, Monterey Park, Glendale, Alhambra, Altadena, South Pasadena, and other cities in the San Gabriel Valley. Clairbourn is a member of The Pasadena Area Independent Schools consortium. Accreditations.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
R.J. Neutra Elementary School. The R. J. Neutra Elementary School is an elementary school on the Naval Air Station Lemoore Base located in the San Joaquin Valley, in Lemoore Station, Kings County, California. Design. The school was built in 1960 from an earlier 1929 International style architectural design created by modernist architect Richard Neutra.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Geography. The mountain is located at the tripoint between three valleys: Valstrona, Valle Anzasca and Valle Mastallone (the latter a side valley of Valsesia). The Sesia/Anzasca wayer divide goes on westwards with Monte Mora () and Cima Cresta.

Geographic entities mentioned:
surface_form: Valle Anzasca
instance_of: Valley
countries: Italy
coordinates: lat: 45.9667
lon: 7.96667
surface_form: Valsesia
instance_of: Valley
countries: Italy
coordinates: lat: 45.816666666667
lon: 8.1333333333333
surface_form: valle anzasca
instance_of: Valley
countries: Italy
coordinates: lat: 45.9667
lon: 7.96667
surface_form: valsesia
instance_of: Valley
countries: Italy
coordinates: lat: 45.816666666667
lon: 8.1333333333333
From the summit of Monte Capezzone starts the dividing range between Val Strona and Val Mastallone which, heading South, after the &quot;Colle della Crocetta&quot; and the &quot;Cima Lago&quot; () reaches the Altemberg (Alpi Cusiane). Estwards the water divide between the valleys of the Strona and the Anza heads towards the Monte Massone.

Geographic entities mentioned:
surface_form: Monte Massone
instance_of: Mountain
countries: Italy
coordinates: lat: 45.947
lon: 8.337
surface_form: monte massone
instance_of: Mountain
countries: Italy
coordinates: lat: 45.947
lon: 8.337
The &quot;Colle della Crocetta&quot; can also be reached from Rimella with an uneasy hiking itinerary. Nature conservation. The slopes of Monte Capezzone facing Valstrona and Valsesia are part of the regional park of Alta Val Sesia e dell'Alta Val Strona. The area is also preserved by the establishment of S.C.I.

Geographic entities mentioned:
surface_form: Valsesia
instance_of: Valley
countries: Italy
coordinates: lat: 45.816666666667
lon: 8.1333333333333
surface_form: val sesia
instance_of: Valley
countries: Italy
coordinates: lat: 45.816666666667
lon: 8.1333333333333
The Sesia/Anzasca wayer divide goes on westwards with Monte Mora () and Cima Cresta. From the summit of Monte Capezzone starts the dividing range between Val Strona and Val Mastallone which, heading South, after the &quot;Colle della Crocetta&quot; and the &quot;Cima Lago&quot; () reaches the Altemberg (Alpi Cusiane).

Geographic entities mentioned:
surface_form: altemberg
instance_of: Mountain
countries: Italy
coordinates: lat: 45.9364
lon: 8.20378
surface_form: monte capezzone
instance_of: Mountain
countries: Italy
coordinates: lat: 45.945
lon: 8.209
Monte Capezzone. The Monte Capezzone (in Titzschu &quot;Jungebärg&quot;) is a mountain in the Pennine Alps of north-western Italy; with an elevation of is the highest peak of the Strona Valley. Geography. The mountain is located at the tripoint between three valleys: Valstrona, Valle Anzasca and Valle Mastallone (the latter a side valley of Valsesia).

Geographic entities mentioned:
surface_form: monte capezzone
instance_of: Mountain
countries: Italy
coordinates: lat: 45.945
lon: 8.209
Estwards the water divide between the valleys of the Strona and the Anza heads towards the Monte Massone. Administratively the summit of Monte Capezzone is the tripoint where the borders of the comunes of Rimella (VC), Calasca-Castiglione (VB) and Valstrona (VB) meet. Close to the main elevation of the mountain stands a cross. Geology.

Geographic entities mentioned:
surface_form: monte capezzone
instance_of: Mountain
countries: Italy
coordinates: lat: 45.945
lon: 8.209
Course. The Manitou River has its origin in Lac Caobus in the unorganized territory of Lac-Jérôme, Minganie Regional County Municipality, and lower down flows through the municipality of Rivière-au-Tonnerre, Minganie. The river flows south, widening in two places to form Lake Manitou and Eudist Lake.

Geographic entities mentioned:
surface_form: Eudist Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.50284
lon: -65.24656
surface_form: lake manitou
instance_of: Lake
countries: Canada
coordinates: lat: 50.87361
lon: -65.28778
surface_form: manitou
instance_of: Lake
countries: Canada
coordinates: lat: 45.7775
lon: -81.98333333333333
surface_form: lake manitou
instance_of: Lake
countries: Canada
coordinates: lat: 45.7775
lon: -81.98333333333333
The river flows south, widening in two places to form Lake Manitou and Eudist Lake. It reaches the Saint Lawrence in the Canton de Coopman, near the community of Manitou halfway between Sept-Îles and Havre-Saint-Pierre. The river basin lies between that of the Tortue River to the west and the Chaloupe River to the east. The river is long, with an average flow of.

Geographic entities mentioned:
surface_form: Tortue River
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.300830555556
lon: -65.374169444444
surface_form: Chaloupe River
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.293056
lon: -65.121944
It contains massifs with undulating reliefs and altitudes of. Mount Manitou, which also contains part of the Tortue River watershed, has an elevation of. The bedrock includes eight types of magmatic or metamorphosed rock complexes: mixed paragneiss, granite and pegmatite, anorthosite, granitoid rocks, granodiorite and charnockite gneisses, gabbro and migmatite.

Geographic entities mentioned:
surface_form: Tortue River
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.300830555556
lon: -65.374169444444
Aigle Lake in the north covers, with an irregular shape. The Lake Manitou in the center-south of the basin is almost long but only wide, formed by flooding an old glacial valley with steep sides that rise to over in places. Eudist Lake in the south covers. Environment. The coastal plain extends up to from the river mouth and contains a large number of peat bogs, although only three are more than.

Geographic entities mentioned:
surface_form: Eudist Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.50284
lon: -65.24656
The river does not have the status of a salmon river, although the fish may enter the river estuary below the falls. It is estimated that up to 139 species of birds may nest in the watershed, taking advantage of the vast peat bogs of the coastal plain and the stretches of still water. Cliffs near the Eudistes, and Manitou lakes also provide potential habitat for birds of prey.

Geographic entities mentioned:
surface_form: manitou
instance_of: Lake
countries: Canada
coordinates: lat: 45.7775
lon: -81.98333333333333
Manitou River (Quebec). The Manitou River () is a river flowing in the unorganized territory of Lac-Jérôme and in the municipality of Rivière-au-Tonnerre, in the Minganie Regional County Municipality, in the Côte-Nord region in the province of Quebec, Canada. It flows through largely unspoiled wilderness, and has spectacular falls nears its mouth.

Geographic entities mentioned:
surface_form: manitou river (quebec)
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.297777777777775
lon: -65.24138888888889
surface_form: manitou
instance_of: Lake
countries: Canada
coordinates: lat: 45.7775
lon: -81.98333333333333
Manitou River (Quebec). The Manitou River () is a river flowing in the unorganized territory of Lac-Jérôme and in the municipality of Rivière-au-Tonnerre, in the Minganie Regional County Municipality, in the Côte-Nord region in the province of Quebec, Canada. It flows through largely unspoiled wilderness, and has spectacular falls nears its mouth.

Geographic entities mentioned:
surface_form: manitou
instance_of: Lake
countries: Canada
coordinates: lat: 45.7775
lon: -81.98333333333333
Course. The Manitou River has its origin in Lac Caobus in the unorganized territory of Lac-Jérôme, Minganie Regional County Municipality, and lower down flows through the municipality of Rivière-au-Tonnerre, Minganie. The river flows south, widening in two places to form Lake Manitou and Eudist Lake.

Geographic entities mentioned:
surface_form: manitou
instance_of: Lake
countries: Canada
coordinates: lat: 45.7775
lon: -81.98333333333333
The river flows south, widening in two places to form Lake Manitou and Eudist Lake. It reaches the Saint Lawrence in the Canton de Coopman, near the community of Manitou halfway between Sept-Îles and Havre-Saint-Pierre. The river basin lies between that of the Tortue River to the west and the Chaloupe River to the east. The river is long, with an average flow of.

Geographic entities mentioned:
surface_form: manitou
instance_of: Lake
countries: Canada
coordinates: lat: 45.7775
lon: -81.98333333333333
The river is long, with an average flow of. Three falls with heights of, and have hydroelectric potential of 40, 30 and 20 megawatts respectively. There was a proposal in May 2001 to build 36 small (less than 50 MW) hydroelectric power stations on rivers throughout Quebec, including the Manitou. Due to popular pressure, most of the projects were abandoned.

Geographic entities mentioned:
surface_form: manitou
instance_of: Lake
countries: Canada
coordinates: lat: 45.7775
lon: -81.98333333333333
Name. The name is based on the belief among several indigenous people that the manitou represents the powers of life, and is the great spirit, and that the manitou is in the waterfall. The phrase &quot;Tché-Manitou&quot; means &quot;good spirit&quot; while &quot;Matchi-Manitou&quot; means &quot;bad spirit&quot; or &quot;devil&quot;.

Geographic entities mentioned:
surface_form: manitou
instance_of: Lake
countries: Canada
coordinates: lat: 45.7775
lon: -81.98333333333333
surface_form: manitou
instance_of: Lake
countries: Canada
coordinates: lat: 45.7775
lon: -81.98333333333333
Name. The name is based on the belief among several indigenous people that the manitou represents the powers of life, and is the great spirit, and that the manitou is in the waterfall. The phrase &quot;Tché-Manitou&quot; means &quot;good spirit&quot; while &quot;Matchi-Manitou&quot; means &quot;bad spirit&quot; or &quot;devil&quot;.

Geographic entities mentioned:
surface_form: manitou
instance_of: Lake
countries: Canada
coordinates: lat: 45.7775
lon: -81.98333333333333
surface_form: manitou
instance_of: Lake
countries: Canada
coordinates: lat: 45.7775
lon: -81.98333333333333
surface_form: manitou
instance_of: Lake
countries: Canada
coordinates: lat: 45.7775
lon: -81.98333333333333
Manitou is the French form of the word, while the English used the forms &quot;manitto&quot;, &quot;manetto&quot; or &quot;manitoa&quot;. The name is common throughout Quebec except in the region south of the Saint Lawrence, and is even found in Inuit territories in the hybrid form &quot;Manitounuk&quot;.

Geographic entities mentioned:
surface_form: manitou
instance_of: Lake
countries: Canada
coordinates: lat: 45.7775
lon: -81.98333333333333
The name is common throughout Quebec except in the region south of the Saint Lawrence, and is even found in Inuit territories in the hybrid form &quot;Manitounuk&quot;. The toponym &quot;Manitou River&quot; was formalized on December 5, 1968 at the Commission de toponymie du Québec. Chute Manitou. The coastal plain in this area is about above sea level.

Geographic entities mentioned:
surface_form: manitou
instance_of: Lake
countries: Canada
coordinates: lat: 45.7775
lon: -81.98333333333333
There are three large falls in the lower section of the river: the high Grosse Chute, from the river mouth, and the Aubin and Wallace falls respectively and from the river mouth. Tributaries include the Lavaivre River, which drains the northwest of the watershed, the Lloyd and Trout rivers, which drain the west-central portion and the Little Manitou River, which drains the east-central portion.

Geographic entities mentioned:
surface_form: manitou
instance_of: Lake
countries: Canada
coordinates: lat: 45.7775
lon: -81.98333333333333
Navajo Sandstone. The Navajo Sandstone is a geological formation in the Glen Canyon Group that is spread across the U.S. states of southern Nevada, northern Arizona, northwest Colorado, and Utah as part of the Colorado Plateau province of the United States. Description.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
Prarostino. Prarostino is a &quot;comune&quot; (municipality) in the Metropolitan City of Turin in the Italian region Piedmont, located about southwest of Turin, at the confluence of Val Chisone and Val Pellice.

Geographic entities mentioned:
surface_form: Val Chisone
instance_of: Valley
countries: Italy
coordinates: lat: 45.033
lon: 7.05
For this season, all Division One teams endorsed a decision to split both Zone A and Zone B into two groups of 12 teams each, increasing the total number of teams in the league to 48. It was decided that the first group from Zone A comprise teams from the Nairobi, Aberdares and Mount Kenya regions while the second group comprise teams from the Eastern, North and South Coast regions.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
Archer is best remembered for his exploits of October 12, 1944. In the midst of a furious series of dogfights over German-occupied Hungary, he shot down three Hungarian Bf 109s over Lake Balaton, Hungary, in engagements that spanned only 10 minutes. When Archer returned home in 1945 as a recipient of the Distinguished Flying Cross, he found that nothing seemed to have changed in American society.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
The Long Mynd is a heath and moorland plateau that forms part of the Shropshire Hills in Shropshire, England. The high ground, which is common land and designated as an Area of Outstanding Natural Beauty, lies between the Stiperstones range to the west and the Stretton Hills and Wenlock Edge to the east. Much of it is owned by the National Trust, and is managed by the Longmynd Commoners.

Geographic entities mentioned:
surface_form: Stiperstones
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.581944444444
lon: -2.935
Highest points. The Long Mynd comprises many hills and moors. From the summit of nearly every hill, there are extensive views of the surrounding area and surrounding counties. North, one can see as far as Cheshire; west commands views over the Stiperstones, and into Wales; the Cambrian Mountains in Powys, notably the Berwyn range and as far as Snowdonia on clear days.

Geographic entities mentioned:
surface_form: Stiperstones
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.581944444444
lon: -2.935
North, one can see as far as Cheshire; west commands views over the Stiperstones, and into Wales; the Cambrian Mountains in Powys, notably the Berwyn range and as far as Snowdonia on clear days. The views east are obscured by other areas of the Shropshire Hills, Caer Caradoc, the Wrekin and the Clee Hills. From some locations there are views of the West Midlands.

Geographic entities mentioned:
surface_form: the Wrekin
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.66916666666667
lon: -2.551388888888889
Etymology. The name &quot;Long Mynd&quot; means &quot;long mountain&quot;, the second element being Brittonic in origin. In modern Welsh it is named &quot;Mynydd Hir&quot;, which has the same meaning, or &quot;Cefn Hirfynydd&quot;, meaning &quot;long mountain ridge&quot;. Commoning on Long Mynd.

Geographic entities mentioned:
surface_form: cefn hirfynydd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
Long Mynd. The Long Mynd is a heath and moorland plateau that forms part of the Shropshire Hills in Shropshire, England. The high ground, which is common land and designated as an Area of Outstanding Natural Beauty, lies between the Stiperstones range to the west and the Stretton Hills and Wenlock Edge to the east.

Geographic entities mentioned:
surface_form: the long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
surface_form: long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
Much of it is owned by the National Trust, and is managed by the Longmynd Commoners. The Long Mynd is approximately long by wide, and is broadly characterised by steep valleys on its eastern flanks, and a long slope to the western side rising in a steep escarpment.

Geographic entities mentioned:
surface_form: the long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
surface_form: long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
In its vicinity are the principal settlements of Church Stretton, Little Stretton and All Stretton, Pulverbatch, Smethcott, Woolstaston, Asterton, Myndtown, Wentnor and Ratlinghope. The highest point on the Long Mynd is Pole Bank (); this and the adjacent hill of Caer Caradoc () are classed as Marilyns. Etymology.

Geographic entities mentioned:
surface_form: the long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
surface_form: long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
Commoning on Long Mynd. There is pollen evidence to show that trees began to be replaced by grass on the plateau of the Long Mynd from the Bronze Age and written evidence of organised management as a grazed common from the 13th century. The Long Mynd commoners' ponies and sheep grazed here are hardy animals and are well adapted to the harsh conditions of life on the hill.

Geographic entities mentioned:
surface_form: the long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
surface_form: the long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
surface_form: long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
surface_form: long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
They graze selectively and very close to the ground, leaving patches of long vegetation which benefits insects and small mammals. This grazing pattern has resulted in a special ecology and the Long Mynd Common is therefore designated as a Site of Special Scientific Interest.

Geographic entities mentioned:
surface_form: the long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
surface_form: long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
Referred to collectively as the Longmyndian Supergroup, the rock sequence is divided into two groups; the older Stretton Group comprising five named formations and the younger Wentnor Group formed of two formations. The entire 7000m thick succession was folded into an NE-SW aligned syncline, the Long Mynd Syncline. The axis of the syncline lies to the west of Long Mynd itself.

Geographic entities mentioned:
surface_form: the long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
surface_form: long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
surface_form: long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
Like nearby Stiperstones and Long Mountain, the Long Mynd itself is not considered to have been over-ridden by ice during this ice age. The Onny Valley Glacier pushed around the southern margin of the Long Mynd; one of many lowland outlets for the Welsh Ice Sheet. A series of meltwater channels on the eastern side of the Long Mynd is associated with the wasting of the ice mass.

Geographic entities mentioned:
surface_form: the long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
surface_form: long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
The Onny Valley Glacier pushed around the southern margin of the Long Mynd; one of many lowland outlets for the Welsh Ice Sheet. A series of meltwater channels on the eastern side of the Long Mynd is associated with the wasting of the ice mass. After the retreat of the ice, downcutting of the batches and hollows continued during a prolonged period of wetter climate.

Geographic entities mentioned:
surface_form: the long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
surface_form: long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
Downcutting continues today at a much reduced rate. Today the steep and narrow valleys are covered in a thin layer of acidic soil, able to support only strong grasses, rushes and heathers. From 2006, University of Cambridge scientists monitored seismic activity in the Long Mynd. The broadband seismometer was connected to the internet, and real-time traces viewable online. Bronze Age.

Geographic entities mentioned:
surface_form: the long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
surface_form: long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
Bronze Age. Numerous sites are recorded from the Bronze Age on the Long Mynd including tumuli (also referred to as barrows), chambered tombs, dykes and cross-ridge dykes. Barristers Plain Cross-Ridge Dyke runs southwest to northeast, almost in a straight line for across the narrowest section of the ridge between Grindle Hill and Round Hill.

Geographic entities mentioned:
surface_form: the long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
surface_form: long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
Both ends of the dyke end on steep slopes. It was built with stone and earth, and is wide, and high, with shallow ditches either side. It is roughly 1,500 years old. It was probably built to control the access along the ancient east to west route, which still crosses the Long Mynd today by means of a modern road. At High Park Cross-Ridge Dyke is the longest on the Long Mynd.

Geographic entities mentioned:
surface_form: the long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
surface_form: the long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
surface_form: long mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389