Sarmila/GeoWiki-Features huggingface dataset:
Dukono. Dukono is an active volcano located in the northern part of Halmahera island, the largest of the Maluku Islands in Indonesia. It has a broad profile and is capped by compound craters. During the major eruption in 1550, a lava flow filled in the strait between Halmahera and the north flank cone of Mount Mamuya. It was an eruption of scale 3 on VEI.

Geographic entities mentioned:
surface_form: dukono
instance_of: Mountain
countries: Indonesia
coordinates: lat: 1.699505
lon: 127.878105
It was an eruption of scale 3 on VEI. Deaths were reported but the figure is unknown. Smaller eruptions occurred in 1719, 1868, and 1901. Since 1933, Dukono has been erupting continuously until the present. Eruptions in 2014 increased since early spring. Ash clouds rose up to height and volcanic lightning were observed and photographed on June 11.

Geographic entities mentioned:
surface_form: dukono
instance_of: Mountain
countries: Indonesia
coordinates: lat: 1.699505
lon: 127.878105
Under the terms of the purchase agreement, they took title only when they had extinguished the Indian title. Later in 1788, they were able to extinguish Indian title to all lands &quot;east&quot; of the Genesee River between Lake Ontario and the Pennsylvania border, as well as a tract by paralleling the west bank of the Genesee River (&quot;The Mill Yard Tract&quot;), totalling some.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
The Kowloon Peninsula and Ngong Shuen Chau comprises the Old Kowloon. The Old Kowloon and the area of New Kowloon are collectively known as Kowloon. Geographically, the term &quot;Kowloon Peninsula&quot; may also refer to the area south of the mountain ranges of Beacon Hill, Lion Rock, Tate's Cairn, Kowloon Peak, etc. The peninsula covers five of the eighteen districts of Hong Kong.

Geographic entities mentioned:
surface_form: Lion Rock
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.3531
lon: 114.187
surface_form: Tate's Cairn
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.358
lon: 114.218
surface_form: Kowloon Peak
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.3414
lon: 114.223
Historically speaking, Kowloon Peninsula refers to the ceded territories of Kowloon in 1860 as part of the Convention of Peking, but geographically it covers the entire Kowloon south of the mountain ranges of Lion Rock, Kowloon Peak and other hills. Kowloon Peninsula had a population of 800 when it was ceded to the British Empire in 1860.

Geographic entities mentioned:
surface_form: Lion Rock
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.3531
lon: 114.187
surface_form: Kowloon Peak
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.3414
lon: 114.223
It also has a mighty, craggy, summit block made of limestone, four hundred metres high, that stands atop base of grauwacke and primary rock (&quot;Urgestein&quot; - quartz phyllite). The Rettenstein is the dominating peak of the Spertental valley. Its isolated location also makes the summit an outstanding viewing point and it is therefore a popular destination.

Geographic entities mentioned:
surface_form: Spertental
instance_of: Valley
countries: Austria
coordinates: lat: 47.4131
lon: 12.3097
Großer Rettenstein. The Großer Rettenstein is a mountain with multiple peaks in the Kitzbühel Alps in Austria. The main summit reaches a height of
Although not the highest mountain in the Kitzbühel Alps (that honour goes to the Kreuzjoch at), the Großer Rettenstein is the most striking in this range of otherwise gentle grass-covered mountains.

Geographic entities mentioned:
surface_form: großer rettenstein
instance_of: Mountain
countries: Austria
coordinates: lat: 47.33277777777778
lon: 12.296388888888888
states of Virginia and West Virginia. The river and its tributaries drain the central and lower Shenandoah Valley and the Page Valley in the Appalachians on the west side of the Blue Ridge Mountains, in northwestern Virginia and the eastern panhandle of West Virginia. There is a hydroelectric plant along the Shenandoah River constructed in 2014 by Dominion. Course.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
surface_form: Page Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.7497
lon: -78.3992
The confluence is on the West Virginia-Maryland border, and from the Virginia-West Virginia border. Geology. The Shenandoah Valley is underlaid by limestone. The fertile soil made it a favored place for early settlement. It remains a major agricultural area of Virginia and West Virginia. Some karst topography is evident, and the limestone is honeycombed with caves.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Some karst topography is evident, and the limestone is honeycombed with caves. Several have been developed as commercial tourist attractions, including Luray Caverns, Shenandoah Caverns, and Skyline Caverns. On the riverbank, a few miles above Harper's Ferry, is said to be a cave with an opening just large enough for a mounted rider to squeeze through.

Geographic entities mentioned:
surface_form: Luray Caverns
instance_of: Landform
countries: United States
coordinates: lat: 38.6643
lon: -78.4838
surface_form: Shenandoah Caverns
instance_of: Landform
countries: United States
coordinates: lat: 38.7156
lon: -78.6693
South Fork Shenandoah River. The South Fork is formed at Port Republic in southern Rockingham County, by the confluence of the North River and South River. It flows northeast in a tight meandering course, past Elkton and Shenandoah, through Page Valley, with the Blue Ridge Mountains to the east and the Massanutten Mountain range to the west. North Fork Shenandoah River.

Geographic entities mentioned:
surface_form: Massanutten Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.643
lon: -78.612
North Fork Shenandoah River. The North Fork is long and rises in northern Rockingham County, along the eastern flank of Shenandoah Mountain in the George Washington National Forest. At its formation, the principal feeder on the North Fork is the German River.

Geographic entities mentioned:
surface_form: Shenandoah Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.5097
lon: -79.1842
At its formation, the principal feeder on the North Fork is the German River. The North Fork flows initially southeast, down from the mountains, then northeast through a valley across Shenandoah County, along the western side of Massanutten Mountain. It flows past Woodstock and Strasburg.

Geographic entities mentioned:
surface_form: Massanutten Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.643
lon: -78.612
She is a NIDA graduate. Early life. Gormley was born in Bradford, West Yorkshire, England and moved to the Barossa Valley in South Australia at age 3 and to a farm in Tasmania at the age of 12. She is a country girl at heart, Gormley immediately made herself at home spending her formative years on the property.

Geographic entities mentioned:
surface_form: Barossa Valley
instance_of: Valley
countries: Australia
coordinates: lat: -34.533333333333
lon: 138.95
USS Spitfire (1776 gunboat). USS &quot;Spitfire&quot; was a 3-gun gundalow of the Continental Navy that operated in 1776 on Lake Champlain. She was part of Benedict Arnold's small, hastily built fleet of ships whose purpose was to counter any British invasion forces passing through the lake from Canada.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
It is located in Fuji-Hakone-Izu National Park. Overview. It is the only wetland remaining at the western foothill of Mount Fuji, and has been designated as an &quot;Important wetland&quot; and an &quot;Important Satochi-Satoyama&quot; by the Ministry of the Environment. The altitude ranges from, with an area of.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
It is situated just north of the Canada–United States border, with the south footing of the mountain at Boundary Creek just within Glacier National Park of the United States. Its nearest higher peak is Mount Alderson, to the northwest. Bertha Lake and Bertha Peak are situated immediately to the north. History.

Geographic entities mentioned:
surface_form: Mount Alderson
instance_of: Mountain
countries: Canada
coordinates: lat: 49.024
lon: -113.97
It is situated just north of the Canada–United States border, with the south footing of the mountain at Boundary Creek just within Glacier National Park of the United States. Its nearest higher peak is Mount Alderson, to the northwest. Bertha Lake and Bertha Peak are situated immediately to the north. History.

Geographic entities mentioned:
surface_form: Bertha Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.0425
lon: -113.9411
Climate. Based on the Köppen climate classification, Mount Richards is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Mount Richards drains into Waterton Lake, thence Waterton River.

Geographic entities mentioned:
surface_form: Waterton Lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 49
lon: -113.9
surface_form: mount richards
instance_of: Mountain
countries: Canada
coordinates: lat: 49.01027777777778
lon: -113.94166666666668
Mount Richards. Mount Richards is a mountain summit located in Waterton Lakes National Park, in the Canadian Rockies of Alberta, Canada. It is situated just north of the Canada–United States border, with the south footing of the mountain at Boundary Creek just within Glacier National Park of the United States. Its nearest higher peak is Mount Alderson, to the northwest.

Geographic entities mentioned:
surface_form: mount richards
instance_of: Mountain
countries: Canada
coordinates: lat: 49.01027777777778
lon: -113.94166666666668
Mount Richards. Mount Richards is a mountain summit located in Waterton Lakes National Park, in the Canadian Rockies of Alberta, Canada. It is situated just north of the Canada–United States border, with the south footing of the mountain at Boundary Creek just within Glacier National Park of the United States. Its nearest higher peak is Mount Alderson, to the northwest.

Geographic entities mentioned:
surface_form: mount richards
instance_of: Mountain
countries: Canada
coordinates: lat: 49.01027777777778
lon: -113.94166666666668
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Bertha Lake and Bertha Peak are situated immediately to the north. History. Mount Richards was named in honor of Admiral Sir George Henry Richards (1820–1896), Hydrographer of the Navy who was the Second Commissioner of the British Boundary Commission which delineated the border from the Pacific to the Rockies. It has also been called Sleeping Indian Mountain.

Geographic entities mentioned:
surface_form: mount richards
instance_of: Mountain
countries: Canada
coordinates: lat: 49.01027777777778
lon: -113.94166666666668
Geology. Like other mountains in Waterton Lakes National Park, Mount Richards is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger Cretaceous period rock during the Laramide orogeny. Climate.

Geographic entities mentioned:
surface_form: mount richards
instance_of: Mountain
countries: Canada
coordinates: lat: 49.01027777777778
lon: -113.94166666666668
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger Cretaceous period rock during the Laramide orogeny. Climate. Based on the Köppen climate classification, Mount Richards is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: mount richards
instance_of: Mountain
countries: Canada
coordinates: lat: 49.01027777777778
lon: -113.94166666666668
Mount Richards. Mount Richards is a mountain summit located in Waterton Lakes National Park, in the Canadian Rockies of Alberta, Canada. It is situated just north of the Canada–United States border, with the south footing of the mountain at Boundary Creek just within Glacier National Park of the United States. Its nearest higher peak is Mount Alderson, to the northwest.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: boundary creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.99978
lon: -118.769
History. Mount Richards was named in honor of Admiral Sir George Henry Richards (1820–1896), Hydrographer of the Navy who was the Second Commissioner of the British Boundary Commission which delineated the border from the Pacific to the Rockies. It has also been called Sleeping Indian Mountain. The mountain's toponym was officially adopted in 1943 by the Geographical Names Board of Canada.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Richards was named in honor of Admiral Sir George Henry Richards (1820–1896), Hydrographer of the Navy who was the Second Commissioner of the British Boundary Commission which delineated the border from the Pacific to the Rockies. It has also been called Sleeping Indian Mountain. The mountain's toponym was officially adopted in 1943 by the Geographical Names Board of Canada. Geology.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Adults can commonly be found resting on trunks of trees. Taxonomy. This species was first described by Edward Meyrick in 1888 using specimens collected from Wellington, Lake Wakatipu and Invercargill in December and January. In 1927 Alfred Philpott discussed and illustrated the male genitalia of this species.

Geographic entities mentioned:
surface_form: Lake Wakatipu
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.085
lon: 168.561
This system of trading was used in particular in ancient Ghana. It was also used among the Kushites and the Aksumites. The Greek historian Herodotus wrote about the gold trade with Ghana and Carthage: &quot;The Carthaginians also tell us that they trade with a race of men who live in a part of Libya beyond the Pillars of Hercules.

Geographic entities mentioned:
surface_form: Pillars of Hercules
instance_of: Landform
countries: Morocco
Spain
Gibraltar
coordinates: lat: 36
lon: -5.35
To finance his plan to dethrone Jalaluddin, Alauddin decided to raid the neighboring Hindu kingdoms. In 1293, he raided Bhilsa, a wealthy town in the Paramara kingdom of Malwa, which had been weakened by multiple invasions. At Bhilsa, he learned of the immense wealth of the southern Yadava kingdom in the Deccan region, as well as about the routes leading to their capital Devagiri.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
During the siege of Warangal, Malik Kafur had learned about the wealth of the Hoysala and Pandya kingdoms located further south. After returning to Delhi, he took Alauddin's permission to lead an expedition there. Kafur started his march from Delhi in November 1310, and crossed Deccan in early 1311, supported by Alauddin's tributaries Ramachandra and Prataparudra.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Lauenau. Lauenau is a small town in Lower Saxony, Germany, with about 4,200 inhabitants. It is situated in the east of the district of Schaumburg just off the A2 Autobahn at the foot of the Deister ridge in the Deister-Süntel valley. As well as Lauenau itself, the parish includes the village of Feggendorf, a former coal mining community on the slopes of the Deister which now has a mining museum.

Geographic entities mentioned:
surface_form: Deister-Süntel valley
instance_of: Valley
countries: Germany
coordinates: lat: 52.2
lon: 9.3
Cerro de la Sal. The Cerro de la Sal or Cerro de Sal'&quot;, (&quot;Mountain of Salt&quot;) is located in Villa Rica District of Oxapampa Province in Pasco Department, Peru. The Cerro de la Sal was an important source of salt for the pre-Columbian indigenous people of the Amazon Basin in Peru.

Geographic entities mentioned:
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
Cerro de la Sal. The Cerro de la Sal or Cerro de Sal'&quot;, (&quot;Mountain of Salt&quot;) is located in Villa Rica District of Oxapampa Province in Pasco Department, Peru. The Cerro de la Sal was an important source of salt for the pre-Columbian indigenous people of the Amazon Basin in Peru.

Geographic entities mentioned:
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
The Cerro de la Sal was an important source of salt for the pre-Columbian indigenous people of the Amazon Basin in Peru. Because of the seasonal concentration at the mountain by indigenous people (Indians), especially the Asháninka and Yanesha (Amuesha), Spanish missionaries, settlers, and soldiers were attracted to the Cerro de la Sal as early as 1635.

Geographic entities mentioned:
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
Description. Google Earth locates the Cerro de la Sal about north of the town of Villa Rica. José Amich, an 18th-century Franciscan missionary, described the Cerro (mountain or hill) as shaped like a loaf of bread, running for &quot;three leagues,&quot;, to the southwest and many more leagues to the northeast.

Geographic entities mentioned:
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
Below elevations of about the climate is tropical rainforest (Af in the Köppen Classification). Above that elevation the climate is sub-tropical (Cfb in the Köppen Classification). Indigenous people. In pre-Columbian times, the indigenous people living in the Cerro de la Sal area had commercial relationships with the Inca Empire, but retained their independence.

Geographic entities mentioned:
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
The salt was loaded onto balsa wood rafts and transported down the river to the peoples living in the low jungles of the Amazon Basin. As many as 600 rafts per season carried salt down the rivers. During the other nine months of the year the Cerro de la Sal was almost abandoned. A Spanish expedition in May 1691 found only 44 people there of whom a few were mining salt.

Geographic entities mentioned:
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
Reasons for the seasonality of people at the Cerro de la Sal include the difficulty of navigating the flooded highland rivers during the rainy season and the fact that the Cerro has an elevation above the maximum elevation for the cultivation of manioc, the principal food crop of the indigenous people of the low jungles. Catholic missionaries.

Geographic entities mentioned:
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
Catholic missionaries. The Spanish religious, military and secular authorities realized the strategic importance of the Cerro de la Sal early in the 17th century. Roman Catholic Franciscan missionaries were attracted to the Cerro de la Sal because of the seasonal congregation of large numbers of indigenous people there.

Geographic entities mentioned:
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
Roman Catholic Franciscan missionaries were attracted to the Cerro de la Sal because of the seasonal congregation of large numbers of indigenous people there. A large number of Christian missions collectively called the Cerro de la Sal missions would be established in the region.

Geographic entities mentioned:
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
The indigenous people were resistant. In 1637, the pioneering missionaries, Jerónimo Jimenez and Cristóbal Larrios, and five more Spaniards were killed by the indigenous. In 1641 and 1645, five additional Franciscans were killed and the Cerro de la Sal missions were abandoned.

Geographic entities mentioned:
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
In 1641 and 1645, five additional Franciscans were killed and the Cerro de la Sal missions were abandoned. From about 1645 to 1651 a Spanish adventurer known as Pedro Bohórquez led an expedition of 40 men to the Cerro de la Sal area in search of the fabled city of Paititi, reputed to be lost in the Amazon rain forests.

Geographic entities mentioned:
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
During a stay at Quimiri, Bohórquez and his men abused the local Asháninka people, some of whom had been converted to Christianity by the Franciscans. In 1673, the Franciscans returned again to the Cerro de la Sal area, but in 1674 a convert named Mangoré killed 5 missionaries with arrows. Mangoré opposed the Franciscan's attempt to abolish polygyny.

Geographic entities mentioned:
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
Mangoré opposed the Franciscan's attempt to abolish polygyny. Mangoré's attempts to wipe out the Christians ended when Christian converts killed him at Quimiri. The missions of Quimiri and Huancabamba survived that uprising, but were destroyed and three priests killed in 1694. In 1709, the Franciscans came back to the Cerro de la Sal area, this time with more resources and personnel.

Geographic entities mentioned:
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
In 1709, the Franciscans came back to the Cerro de la Sal area, this time with more resources and personnel. From a base at the Convent of Santa Rosa de Ocopa in the Andes, they reestablished missions at Cerro de la Sal and Quimiri, and along the salt trading route down the Perene River at Metraro, Eneno, Epillo, Pichana, and San Judas Tadeo.

Geographic entities mentioned:
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
To attract the indigenous people the missionaries distributed steel knives and fishhooks as well as religious materials. Once again the missions failed. An epidemic in 1722-1723 reduced the population of Eneno from 800 to 220 and the other Cerro de la Sal missions suffered similarly. The indigenous people avoided the missions, associating them with disease and death.

Geographic entities mentioned:
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
An epidemic in 1722-1723 reduced the population of Eneno from 800 to 220 and the other Cerro de la Sal missions suffered similarly. The indigenous people avoided the missions, associating them with disease and death. From 1742 to 1752, a messianic movement headed by Juan Santos Atahualpa destroyed the missions and the Spanish lost control of Cerro de la Sal and much of the region.

Geographic entities mentioned:
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
The indigenous people led by Juan Santos defeated Spanish military expeditions sent to the region and for the next 100 years were unmolested by the Spanish and their Peruvian successors. Eleven Franciscan missionaries in the Cerro de la Sal missions were killed by the indigenous people during the 18th century. Peru gains control.

Geographic entities mentioned:
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
Peru gains control. The Peruvian government, now independent from Spain, established a fortress in 1842 at what became the town of San Ramon along the Chanchamayo River south of the Cerro de la Sal. Thus, the government began the reconquest of the region lost during the Juan Santos Atahualpa rebellion.

Geographic entities mentioned:
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
Military expeditions in 1868 and 1869 were unsuccessful, but destroyed or confiscated much Ashásnika property. The government proposed stationing up to 200 soldiers at the Cerro de la Sal. This was never realized, but beginning in 1873, the Peruvian government promoted the settlement of people imported from Europe.

Geographic entities mentioned:
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
The government proposed stationing up to 200 soldiers at the Cerro de la Sal. This was never realized, but beginning in 1873, the Peruvian government promoted the settlement of people imported from Europe. Several thousand Italians were settled south of the Cerro de la Sal in Asháninka territory and Germans and Austrians were settled north of the Cerro in Amuesha territory.

Geographic entities mentioned:
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
Several thousand Italians were settled south of the Cerro de la Sal in Asháninka territory and Germans and Austrians were settled north of the Cerro in Amuesha territory. In the 1890s, a British company, the Peruvian Corporation, gained a concession along the rivers near the Cerro de la Sal and sold land to British and Dutch settlers.

Geographic entities mentioned:
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
Peruvians, including landless Peruvians displaced in the Andes, also began to migrate into the region to obtain land. In 1896 and 1897 a Catholic priest, Gabriel Sala, visited the Cerro de la Sal. He found that European settlers had been preventing the indigenous people from mining the salt for their use and instead enslaving them to exploit the salt for commerce.

Geographic entities mentioned:
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
The response of the Asháninka had been to destroy the farmsteads of British settlers. However, the advance of the European and Andean settlers (plus Chinese brought in as farm workers) during the rubber boom was inexorable and the indigenous were forced away from the Cerro de la Sal.

Geographic entities mentioned:
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
The nearby town of Villa Rica was founded in 1928 by settlers of German ancestry from Pozuzo and coffee became the principal cash crop of the region. Until the 1980s the indigenous people continued to visit Cerro de la Sal and extract salt to carry back to their homes in the more remote parts of the Amazon Basin.

Geographic entities mentioned:
surface_form: cerro de la sal
instance_of: Mountain
countries: Peru
coordinates: lat: -10.691
lon: -75.273
The Port of Redwood City is the only deepwater port in the South San Francisco Bay. Significant expanses of bay mud are present nearby: in Redwood Creek, Westpoint Slough and especially at the mouth of Redwood Creek, where bay muds extend almost two kilometers into San Francisco Bay.

Geographic entities mentioned:
surface_form: Westpoint Slough
instance_of: Landform
countries: United States
coordinates: lat: 37.517
lon: -122.202
Extensive areas of marshland and bay muds are found in the vicinity of the Port. Westpoint Slough joins Redwood Creek from the southeast about 600 meters north of the Port of Redwood City. Deepwater Slough is a U-shaped channel whose two ends join Redwood Creek both north and south of the Port, with both joins on the opposite site of Redwood Creek.

Geographic entities mentioned:
surface_form: Westpoint Slough
instance_of: Landform
countries: United States
coordinates: lat: 37.517
lon: -122.202
As the Iroquois were very often leading punitive expeditions on the New France territories and were continuously trying to steal away the French allies' hunting territories, Louis XIV decided to send the whole Carignan-Salières Regiment to build a series of forts along the Richelieu River and Lake Champlain, which explains why the area was later named the Vallée des Forts (literally: the Forts Valley), and to lead a punitive expedition against the Iroquois.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
It was a fort of two hundred feet by two hundred feet that had four bastions, two of which were made in stone. This fort was an important relay between Montreal and Fort St. Frédéric, which was located in the south of Lake Champlain, because a road linked Fort Saint-Jean to La Prairie and allowed the communications between Montreal and St. Frédéric to be considerably shorter.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Because of bad weather and the weakened state of the few remaining troops, the Americans failed to take Quebec City in their assault on December 31, 1775. After British reinforcements arrived from England the next Spring, the Americans abandoned and burnt the forts, including Fort Saint-Jean, that they had taken north of Lake Champlain.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
But, fearing a new American invasion, the British reconstructed a strengthened Fort in 1776, adding a series of new ramparts. They also built in Saint-Jean an important shipyard to assemble the shallow-draft boats needed to follow the Americans on Lake Champlain. These boats soon would take part in the Battle of Valcour Island. 19th-century fortifications.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Ross named the land Victoria Land, and the mountains the Admiralty Range. He followed the coast southwards and passed Weddell's Farthest South point of 74°15'S on 23 January. A few days later, as they moved further eastward to avoid shore ice, they were met by the sight of twin volcanoes (one of them active), which were named Mount Erebus and Mount Terror, in honour of the expedition's ships.

Geographic entities mentioned:
surface_form: Mount Erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
The Flinn or O'Flinn were rulers within Gaelic Irelands medieval over-kingdom of Ulaid. The O'Flinn were the chiefs of the Ui Tuirtre, a people seated on the east side of the River Bann and Lough Neagh in what today is Northern Ireland's County Antrim. The Flinn claim descent from Fiachra Tort, the grandson of the Irish king Colla Uais, who seized territory of the Ulaid in the 4th century A.D.

Geographic entities mentioned:
surface_form: Lough Neagh
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.618333333333
lon: -6.3952777777778
Wampuru. Wampuru (Quechua for a big pumpkin, also spelled &quot;Huampuro&quot;) is a mountain in the Cordillera Central in the Andes of Peru which reaches a height of approximately. It is located in the Lima Region, Yauyos Province, Huantán District.

Geographic entities mentioned:
surface_form: wampuru
instance_of: Mountain
countries: Peru
coordinates: lat: -12.56833333
lon: -75.72388889
The river is named for the Ute chief Sanpitch, who also gives his name to the San Pitch Mountains and Sanpete County. Course. The upper San Pitch River begins north of Milburn near Oak Creek Ridge on the northern Wasatch Plateau and flows south to Moroni. The middle San Pitch River runs from Moroni, where it crosses Utah State Route 132 (SR‑132).

Geographic entities mentioned:
surface_form: Wasatch Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 39.311666666667
lon: -111.33694444444
La Désirade Passage. La Désirade Passage () is a strait in the Caribbean. It separates the island of la Désirade, from Grande-Terre (Guadeloupe). History. The waters of the La Désirade Passage have long been known to be very dangerous and the crossings were historically perilous, at least until the arrival of new ferry vessels.

Geographic entities mentioned:
surface_form: la désirade passage
instance_of: Body of water
countries: France
coordinates: lat: 16.16
lon: -61.08
History. The waters of the La Désirade Passage have long been known to be very dangerous and the crossings were historically perilous, at least until the arrival of new ferry vessels. But there is also, and perhaps above all, a historical reason related to the fact that in the eighteenth century, the island La Désirade was endowed with a leprosarium.

Geographic entities mentioned:
surface_form: la désirade passage
instance_of: Body of water
countries: France
coordinates: lat: 16.16
lon: -61.08
Cape D'Aguilar. Cape D'Aguilar () is a cape on Hong Kong Island, Hong Kong. The cape is on the southeastern end of D'Aguilar Peninsula. To its north are Shek O and D'Aguilar Peak. Name. It is named after Major-General George Charles d'Aguilar. History. The name Cape D'Aguilar appeared first on a map in 1845 surveyed by Lieutenant Collinson and Sir John Francis Davis.

Geographic entities mentioned:
surface_form: D'Aguilar Peak
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.21677
lon: 114.24893
Many of the books are set on or around the Long Mynd and Stiperstones hills in south Shropshire, England, but some are based in Sussex (centred on Rye), Dartmoor, the Goathland and Whitby area of Yorkshire and the Southwold and Walberswick area of the Suffolk coast. One book is set in London, the self-explanatory &quot;Lone Pine London&quot;.

Geographic entities mentioned:
surface_form: Long Mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
surface_form: Stiperstones
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.581944444444
lon: -2.935
A 2002 two-pound coin featured the flag of Northern Ireland to mark the 2002 Commonwealth Games. These coins are not unique to Northern Ireland and circulate through the entire United Kingdom and other sterling area countries. The Giant's Causeway appeared on two five-pound coins in 2012; these are commemorative coins and are rarely circulated.

Geographic entities mentioned:
surface_form: Giant's Causeway
instance_of: Landform
countries: United Kingdom
coordinates: lat: 55.240833333333
lon: -6.5116666666667
Vallorbe is also served by Swiss Federal Railways' hourly running suburban train &quot;S2&quot; on the Simplon Railway to Lausanne and further to Palézieux. CFF also runs hourly services on the Vallorbe–Le Brassus railway line into the Vallée de Joux to Le Brassus in the south-west end of the valley. From there a bus connection connects Le Brassus with Nyon at the Lake of Geneva.

Geographic entities mentioned:
surface_form: Vallée de Joux
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.583333333333
lon: 6.2166666666667
Poet Norman Nicholson described the Screes as ‘like the inverted arches of a Gothic Cathedral’. The title Wastwater Screes applies to the scree-covered north-western fellside which plunges dramatically down into Wastwater. This also includes Illgill Head's neighbour Whin Rigg, the continuation of the ridge to the south-west. The scree slope continues beneath the lake to a depth of.

Geographic entities mentioned:
surface_form: Whin Rigg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.41945780200143
lon: -3.3093011327319037
surface_form: illgill head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4327
lon: -3.2825694444444
Geologically, Illgill Head and Whin Rigg are part of the Borrowdale Volcanic Group, typical for the southern-western area of the Lake District. In marked contrast to the north-western slope, the opposite flank of the fell, which descends to Burnmoor Tarn and Miterdale, is much gentler and covered in heather and bracken. Geology.

Geographic entities mentioned:
surface_form: Burnmoor Tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.428617
lon: -3.259844
Summit. The summit is a flat sheepwalk, giving no clue to the drama of the Screes. North-west from the cairn the grassy plateau gradually tilts, until a few yards away it simply disappears over the brink. Illgill Head is a fine viewpoint for Wasdale Head, the surrounding fells all appearing as they soar up from the dalehead. Nearer views, with care, are possible down the Screes themselves. Ascent.

Geographic entities mentioned:
surface_form: wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
surface_form: illgill head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4327
lon: -3.2825694444444
Nearer views, with care, are possible down the Screes themselves. Ascent. Illgill Head is commonly ascended from Wasdale Head over the north-eastern shoulder of the fell, skirting the edge of the Screes. There is also an ascent from Boot in Eskdale either over Whin Rigg or direct via Burnmoor Tarn.

Geographic entities mentioned:
surface_form: wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
surface_form: illgill head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4327
lon: -3.2825694444444
Illgill Head is commonly ascended from Wasdale Head over the north-eastern shoulder of the fell, skirting the edge of the Screes. There is also an ascent from Boot in Eskdale either over Whin Rigg or direct via Burnmoor Tarn. A lakeside path along the south-eastern shore of Wastwater starts at Wasdale Head Hall and continues through the boulder field with exhilarating close-up views of the Screes.

Geographic entities mentioned:
surface_form: wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
surface_form: wastwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.441666666667
lon: -3.2916666666667
Illgill Head is commonly ascended from Wasdale Head over the north-eastern shoulder of the fell, skirting the edge of the Screes. There is also an ascent from Boot in Eskdale either over Whin Rigg or direct via Burnmoor Tarn. A lakeside path along the south-eastern shore of Wastwater starts at Wasdale Head Hall and continues through the boulder field with exhilarating close-up views of the Screes.

Geographic entities mentioned:
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.478
lon: -0.786
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.189
lon: -3.068
surface_form: whin rigg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.41945780200143
lon: -3.3093011327319037
surface_form: burnmoor tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.428617
lon: -3.259844
Illgill Head. Illgill Head is a fell in the English Lake District. It is known more commonly as the northern portion of the Wastwater Screes. The fell is high and stands along the south-east shore of Wastwater, the deepest lake in England. Topography. The panorama of the Wastwater Screes across Wastwater is one of the most famous and awe-inspiring views in England.

Geographic entities mentioned:
surface_form: illgill head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4327
lon: -3.2825694444444
The screes were formed as a result of ice and weathering erosion on the rocks. Geologically, Illgill Head and Whin Rigg are part of the Borrowdale Volcanic Group, typical for the southern-western area of the Lake District. In marked contrast to the north-western slope, the opposite flank of the fell, which descends to Burnmoor Tarn and Miterdale, is much gentler and covered in heather and bracken.

Geographic entities mentioned:
surface_form: illgill head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4327
lon: -3.2825694444444
surface_form: borrowdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.42
lon: -2.665
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: whin rigg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.41945780200143
lon: -3.3093011327319037
Illgill Head. Illgill Head is a fell in the English Lake District. It is known more commonly as the northern portion of the Wastwater Screes. The fell is high and stands along the south-east shore of Wastwater, the deepest lake in England. Topography. The panorama of the Wastwater Screes across Wastwater is one of the most famous and awe-inspiring views in England.

Geographic entities mentioned:
surface_form: wastwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.441666666667
lon: -3.2916666666667
It is known more commonly as the northern portion of the Wastwater Screes. The fell is high and stands along the south-east shore of Wastwater, the deepest lake in England. Topography. The panorama of the Wastwater Screes across Wastwater is one of the most famous and awe-inspiring views in England. Poet Norman Nicholson described the Screes as ‘like the inverted arches of a Gothic Cathedral’.

Geographic entities mentioned:
surface_form: wastwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.441666666667
lon: -3.2916666666667
surface_form: wastwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.441666666667
lon: -3.2916666666667
Poet Norman Nicholson described the Screes as ‘like the inverted arches of a Gothic Cathedral’. The title Wastwater Screes applies to the scree-covered north-western fellside which plunges dramatically down into Wastwater. This also includes Illgill Head's neighbour Whin Rigg, the continuation of the ridge to the south-west. The scree slope continues beneath the lake to a depth of.

Geographic entities mentioned:
surface_form: wastwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.441666666667
lon: -3.2916666666667
surface_form: wastwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.441666666667
lon: -3.2916666666667
The title Wastwater Screes applies to the scree-covered north-western fellside which plunges dramatically down into Wastwater. This also includes Illgill Head's neighbour Whin Rigg, the continuation of the ridge to the south-west. The scree slope continues beneath the lake to a depth of. The screes were formed as a result of ice and weathering erosion on the rocks.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Geology. The summit area has outcropping tuff, lapilli tuff and breccia of the Lingmell Formation amid the drift deposits. The crags atop the Screes reveal the plagioclase-phyric andesite lavas of the Birker Fell Formation. Summit. The summit is a flat sheepwalk, giving no clue to the drama of the Screes.

Geographic entities mentioned:
surface_form: lingmell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462088888889
lon: -3.2217805555556
It also has a summit crater, Tantalus Crater. The cinder cone formed after the demise of Koolau Volcano, during a time of rejuvenated-stage volcanism in southeastern Oahu that also formed Punchbowl Crater, Diamond Head and Koko Head as part of the Honolulu Volcanics. Tantalus overlooks the modern city of Honolulu, which is built on top of Tantalus cinders. History.

Geographic entities mentioned:
surface_form: Punchbowl Crater
instance_of: Mountain
countries: United States
coordinates: lat: 21.3125
lon: -157.84611111111
surface_form: Diamond Head
instance_of: Mountain
countries: United States
coordinates: lat: 21.259722222222
lon: -157.81175
Army's coastal artillery defense system, a fire-control station was built on Tantalus. In conjunction with the fire-control station at Diamond Head, the two positions were used to control coast artillery batteries: at Fort DeRussey and Fort Ruger. The southern slope of Tantalus was bombed in Operation K, Japan's unsuccessful second attack on Oahu, which took place March 4, 1942.

Geographic entities mentioned:
surface_form: Diamond Head
instance_of: Mountain
countries: United States
coordinates: lat: 21.259722222222
lon: -157.81175
Tantalus (Oahu). Mount Tantalus (Puʻu ʻōhiʻa) is an extinct cinder cone in the southern Koolau Range on the Hawaiian Island of Oahu. It also has a summit crater, Tantalus Crater. The cinder cone formed after the demise of Koolau Volcano, during a time of rejuvenated-stage volcanism in southeastern Oahu that also formed Punchbowl Crater, Diamond Head and Koko Head as part of the Honolulu Volcanics.

Geographic entities mentioned:
surface_form: tantalus
instance_of: Mountain
countries: United States
coordinates: lat: 21.3327
lon: -157.815
Tantalus (Oahu). Mount Tantalus (Puʻu ʻōhiʻa) is an extinct cinder cone in the southern Koolau Range on the Hawaiian Island of Oahu. It also has a summit crater, Tantalus Crater. The cinder cone formed after the demise of Koolau Volcano, during a time of rejuvenated-stage volcanism in southeastern Oahu that also formed Punchbowl Crater, Diamond Head and Koko Head as part of the Honolulu Volcanics.

Geographic entities mentioned:
surface_form: mount tantalus
instance_of: Mountain
countries: United States
coordinates: lat: 21.3327
lon: -157.815
surface_form: tantalus
instance_of: Mountain
countries: United States
coordinates: lat: 21.3327
lon: -157.815
It also has a summit crater, Tantalus Crater. The cinder cone formed after the demise of Koolau Volcano, during a time of rejuvenated-stage volcanism in southeastern Oahu that also formed Punchbowl Crater, Diamond Head and Koko Head as part of the Honolulu Volcanics. Tantalus overlooks the modern city of Honolulu, which is built on top of Tantalus cinders. History.

Geographic entities mentioned:
surface_form: tantalus
instance_of: Mountain
countries: United States
coordinates: lat: 21.3327
lon: -157.815
surface_form: tantalus
instance_of: Mountain
countries: United States
coordinates: lat: 21.3327
lon: -157.815
History. The Tantalus Loop was a popular wagon trail from the late 1800s for views and picnic parties. It had &quot;rugged canyons, wooded valleys, aromatic eucalyptus giants, stag-horn fern, pungent guava&quot;, monkeypod, shower cassias, and myrtle, with a two-room, corrugated-roofed &quot;Half-Way House&quot;, managed by 1900s forester David Haugh, offering a welcome stop for trekkers.

Geographic entities mentioned:
surface_form: tantalus
instance_of: Mountain
countries: United States
coordinates: lat: 21.3327
lon: -157.815
Many immigrant families of note settled there &quot;in cool picturesque seclusion&quot;, including the Waterhouses, Giffords, Wilders, Dickeys, Davies, Isenbergs, Browns, and Alexanders. A cliff of pitch-black volcanic sand was an attraction on Tantalus until it was mined for blacktopping paths and yards. As part of the U.S.

Geographic entities mentioned:
surface_form: tantalus
instance_of: Mountain
countries: United States
coordinates: lat: 21.3327
lon: -157.815