Sarmila/GeoWiki-Features huggingface dataset:
Big Island Lake (California). Big Island Lake is a lake in Yosemite National Park, United States. Big Island Lake was named from the large lake island it contains.

Geographic entities mentioned:
surface_form: island lake
instance_of: Lake
countries: United States
coordinates: lat: 44.38027778
lon: -96.00888889
surface_form: island lake
instance_of: Lake
countries: United States
coordinates: lat: 40.615
lon: -115.381
surface_form: big island lake
instance_of: Lake
countries: United States
coordinates: lat: 38.091
lon: -119.7
surface_form: island lake
instance_of: Lake
countries: United States
coordinates: lat: 46.73416667
lon: -93.19
surface_form: island lake
instance_of: Lake
countries: United States
coordinates: lat: 42.5181
lon: -122.238
surface_form: island lake
instance_of: Lake
countries: United States
coordinates: lat: 47.78027778
lon: -95.02888889
surface_form: island lake
instance_of: Lake
countries: United States
coordinates: lat: 47.6819019
lon: -122.6602552
East Cove National Wildlife Refuge. East Cove National Wildlife Refuge is located south of Lake Charles, Louisiana along the southeast shore of Calcasieu Lake in Cameron Parish. It is accessible only by boat. It is managed by the Cameron Prairie National Wildlife Refuge office as part of the Southwest Louisiana National Wildlife Refuge Complex. Wildlife and habitat.

Geographic entities mentioned:
surface_form: Calcasieu Lake
instance_of: Lake
countries: United States
coordinates: lat: 29.900277777778
lon: -93.282777777778
Little Island, County Cork, is a civil parish and mainly industrial area to the east of Cork city in Ireland. It is no longer an island since the northern channel separating it from the mainland has filled over. To the west and south is Lough Mahon, part of Cork Harbour; across a channel to the east is Fota Island. Little Island is within the Dáil constituency of Cork North-Central. History.

Geographic entities mentioned:
surface_form: Lough Mahon
instance_of: Lake
countries: Ireland
coordinates: lat: 51.8833
lon: -8.36667
Waughop Lake. Waughop Lake is a lake less than 1.6 km (1.0 mi) east of Steilacoom in Pierce County, Washington, United States. The lake lies within Fort Steilacoom Park, in the city of Lakewood, Washington. Waughop Lake has a surface area of approximately and a mean depth of. The lake is fed by groundwater and has no surface drainage channels. The lake is named after Dr.

Geographic entities mentioned:
surface_form: waughop lake
instance_of: Lake
countries: United States
coordinates: lat: 47.1704
lon: -122.565
Waughop Lake. Waughop Lake is a lake less than 1.6 km (1.0 mi) east of Steilacoom in Pierce County, Washington, United States. The lake lies within Fort Steilacoom Park, in the city of Lakewood, Washington. Waughop Lake has a surface area of approximately and a mean depth of. The lake is fed by groundwater and has no surface drainage channels. The lake is named after Dr.

Geographic entities mentioned:
surface_form: waughop lake
instance_of: Lake
countries: United States
coordinates: lat: 47.1704
lon: -122.565
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Remnants of part of the hospital are incorporated into the trail. The lake is circled by a 9/10-mile paved loop trail. Waughop Lake is refilled with trout that, unless caught, die within a few weeks. One of the primary researchers of this lake, Michele La Fontaine, has done studies on the algae and dissolved oxygen content.

Geographic entities mentioned:
surface_form: waughop lake
instance_of: Lake
countries: United States
coordinates: lat: 47.1704
lon: -122.565
The depth fluctuates about 2 feet a year, gaining 2 feet in winter and losing 2 feet due to evaporation. Life. Waughop Lake is home to many animals and plants, including mallards, deer, Canada geese, raccoons, robins, squirrels, and other small birds. Algae. Algae in Waughop Lake has affected the lake for a long time.

Geographic entities mentioned:
surface_form: waughop lake
instance_of: Lake
countries: United States
coordinates: lat: 47.1704
lon: -122.565
Life. Waughop Lake is home to many animals and plants, including mallards, deer, Canada geese, raccoons, robins, squirrels, and other small birds. Algae. Algae in Waughop Lake has affected the lake for a long time. The algae are fed by nitrogen, supplied by the duck droppings and sediment, which the lake has plenty of.

Geographic entities mentioned:
surface_form: waughop lake
instance_of: Lake
countries: United States
coordinates: lat: 47.1704
lon: -122.565
Algae in Waughop Lake has affected the lake for a long time. The algae are fed by nitrogen, supplied by the duck droppings and sediment, which the lake has plenty of. There are serious algae blooms, and it is not advisable to come into contact with the water. During algae blooms, the lake may be closed or restricted to visitors. For some of the year, fishing is restricted due to the algae problem.

Geographic entities mentioned:
surface_form: lake may
instance_of: Lake
countries: United States
coordinates: lat: 47.09055556
lon: -94.59333333
Waughop Lake. Waughop Lake is a lake less than 1.6 km (1.0 mi) east of Steilacoom in Pierce County, Washington, United States. The lake lies within Fort Steilacoom Park, in the city of Lakewood, Washington. Waughop Lake has a surface area of approximately and a mean depth of. The lake is fed by groundwater and has no surface drainage channels. The lake is named after Dr.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Waughop Lake has a surface area of approximately and a mean depth of. The lake is fed by groundwater and has no surface drainage channels. The lake is named after Dr. John Wesley Waughop, former superintendent of the Washington State Hospital for the Insane. The hospital, now known as Western State Hospital, lies across from the park on Steilacoom Boulevard SW.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
History. It was established in 1873 in Wilkes-Barre, Pennsylvania as the Malt Club. It rapidly became &quot;the center of all social activity&quot; in the Wyoming Valley. The club moved to South Main Street in 1879 and stayed there until 1889. In 1889 they changed the name to &quot;Westmoreland&quot;. The club was incorporated on February 9, 1899. They rented the Hunt House near St.

Geographic entities mentioned:
surface_form: Wyoming Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
Rakhine State. Rakhine State (;,;), formerly known as Arakan State, is a state in Myanmar (Burma). Situated on the western coast, it is bordered by Chin State to the north, Magway Region, Bago Region and Ayeyarwady Region to the east, the Bay of Bengal to the west and the Chattogram Division of Bangladesh to the northwest.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Hamren has an average literacy rate of 86 per cent, with male literacy at 90 per cent and female literacy at 82 per cent. Nationally, India's average literacy rate is 74 per cent. Geography. Hamren is a hillside town with the Kopili river passing through it. Towards the southern border are the hills of Meghalaya and the lake of Borapani. Transport.

Geographic entities mentioned:
surface_form: Kopili river
instance_of: Watercourse
countries: India
coordinates: lat: 26.16166667
lon: 92.27638889
Bernhard Pez. Bernhard Pez (22 February 1683, at Ybbs near Melk &ndash; 27 March 1735, at Melk, Lower Austria) was an Austrian Benedictine historian and librarian. Life. He studied at Vienna and Krems, and in 1699 entered Melk Abbey.

Geographic entities mentioned:
surface_form: Ybbs
instance_of: Watercourse
countries: Austria
coordinates: lat: 47.7603
lon: 15.2053
He also decorated the original Teatro Colón. He returned to Italy and installed himself near Lake Maggiore, and the landscape of that area proved a new source of inspiration for paintings that he then produced with his son Serafino (1875–1945). He died in Lesa, aged 67.

Geographic entities mentioned:
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
Bonnie Lake (Alberta). Bonnie Lake is a small lake in Alberta, Canada. It is located outside of Vilna, Alberta, north of Highway 28, and is part of the North Saskatchewan River basin. The lake has a surface of and reaches a maximum depth of, while the average depth is. Bonnie Lake drains a total area of.

Geographic entities mentioned:
surface_form: bonnie lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.1508
lon: -111.864
Bonnie Lake is a small lake in Alberta, Canada. It is located outside of Vilna, Alberta, north of Highway 28, and is part of the North Saskatchewan River basin. The lake has a surface of and reaches a maximum depth of, while the average depth is. Bonnie Lake drains a total area of. The lake drains through its south shore into Stony Creek which empties into the North Saskatchewan River.

Geographic entities mentioned:
surface_form: bonnie lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.1508
lon: -111.864
He rarely did individual portraits. However, he painted himself into a few interior tipi scenes, usually smoking a pipe. He commonly referred to the tipis as tents, such as in the title, &quot;Inside a Skin Tent&quot;. Biography. Rindisbacher was born on 12 April 1806 in Emmental, Switzerland. He emigrated from Switzerland to western Canada with his family when he was fifteen.

Geographic entities mentioned:
surface_form: Emmental
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.91922
lon: 7.77868
In the mid 1890s, Bohls returned to his hometown, where he maid acquaintance with the writer Hermann Allmers, who introduced him to the union of Männer vom Morgenstern. Together with Gustav von der Osten, he formed in 1898 a homeland association for the whole area between the mouths of the Elbe and Weser rivers.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Bonnie Judd. Bonnie Judd is a Canadian animal trainer known for training dogs to act in films and commercials. She founded and runs the company Canine Co-Stars, based in Aldergrove, British Columbia, Canada, in the Fraser Valley area. Through this company, she has trained dogs and a variety of other animals, including monkeys and turtles, to successfully act in films.

Geographic entities mentioned:
surface_form: Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
Coleman Pond. Coleman Pond is a lake in the U.S. state of Georgia. Coleman Pond was named after one Mr. Coleman, the original owner of the site.

Geographic entities mentioned:
surface_form: coleman pond
instance_of: Lake
countries: United States
coordinates: lat: 31.7188168
lon: -83.4453068
Pampero's main markets are Italy, Spain and Venezuela. Its main production plant is located at &quot;Complejo Licorero del Centro&quot;, in Ocumare, Miranda state, in the region of the Tuy river valleys, in the central plains. Name.

Geographic entities mentioned:
surface_form: Tuy river valleys
instance_of: Valley
countries: Venezuela
coordinates: lat: 10.2333
lon: -66.85
When Snider saw the private detective again the following day, he tried to convince the man to buy him a machine gun for &quot;home protection&quot;, but the detective talked him out of the idea. The next day, August 11, Snider drove out into the San Fernando Valley to look at a gun he had found for sale in a newspaper.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Willamette Greenway. The Willamette River Greenway is a cooperative state and local government effort to maintain and enhance the scenic, recreational, historic, natural and agricultural qualities of the Willamette River and its adjacent lands. A number of trails exist along the greenway, but significant gaps still exist.

Geographic entities mentioned:
surface_form: adjacent lands
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
In India, the creeper occurs in the states of Himachal Pradesh, Punjab, Haryana, Uttar Pradesh, Bihar, Orissa, Madhya Pradesh, Andhra Pradesh, Maharashtra, Karnataka, Kerala, Tamil Nadu, West Bengal, Sikkim, Assam, Meghalaya, Arunachal Pradesh, Nagaland, Manipur and Tripura. The creeper is common in the Western Ghats, and the patches of adjoining forest of the Konkan coast and the Deccan plateau.

Geographic entities mentioned:
surface_form: Deccan plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Malaxa Mountain. ksb9vscywbhiml308mtbij18lf0m5" xml:space="preserve">Malaxa Mountain is a mountain at Malaxa on the island of Crete in the country of Greece. This mountain feature is situated in northwestern coastal Crete in the vicinity of the city of Chania. Trypali limestone is a dominant rock of Malaxa Mountain.

Geographic entities mentioned:
surface_form: malaxa mountain
instance_of: Mountain
countries: Greece
coordinates: lat: 35.465
lon: 24.072
This mountain feature is situated in northwestern coastal Crete in the vicinity of the city of Chania. Trypali limestone is a dominant rock of Malaxa Mountain. The ancient city of Kydonia held sway over lands to the south of it across the Chania Plain all the way to Malaxa Mountain.

Geographic entities mentioned:
surface_form: malaxa mountain
instance_of: Mountain
countries: Greece
coordinates: lat: 35.465
lon: 24.072
Benthophilus ctenolepidus. &quot;Benthophilus ctenolepidus&quot; is a species of goby widespread along the southern coasts of the Caspian Sea: in the Gorgansky Bay, also from Absheron to Astara at south.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Lower Lea Valley. The Lower Lea Valley is the southern end of the Lea Valley which surrounds the River Lea in eastern Greater London. It is part of the Thames Gateway redevelopment area and was the location of the 2012 Summer Olympics. Geography. The Lower Lea Valley can be described as the part to the south of the long chain of reservoirs which end with the East and West Warwick Reservoirs.

Geographic entities mentioned:
surface_form: Lea Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69
lon: -0.01
surface_form: lower lea valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.55
lon: -0.0166667
surface_form: lea valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69
lon: -0.01
Lower Lea Valley. The Lower Lea Valley is the southern end of the Lea Valley which surrounds the River Lea in eastern Greater London. It is part of the Thames Gateway redevelopment area and was the location of the 2012 Summer Olympics. Geography. The Lower Lea Valley can be described as the part to the south of the long chain of reservoirs which end with the East and West Warwick Reservoirs.

Geographic entities mentioned:
surface_form: lower lea valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.55
lon: -0.0166667
surface_form: lea valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69
lon: -0.01
Geography. The Lower Lea Valley can be described as the part to the south of the long chain of reservoirs which end with the East and West Warwick Reservoirs. The Lea changes course at this point, changing from a SSW to a SSE direction for the last before its confluence with the Thames at Leamouth and Canning Town.

Geographic entities mentioned:
surface_form: lower lea valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.55
lon: -0.0166667
surface_form: lea valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69
lon: -0.01
The project completes the 26-mile long Lee Valley Regional Park which connects Ware in Hertfordshire to the River Thames. In popular culture. The 2005 documentary &quot;What Have You Done Today, Mervyn Day?&quot; focuses on the history and landscape of the Lower Lea Valley. The film was made by Paul Kelly in conjunction with British pop group Saint Etienne.

Geographic entities mentioned:
surface_form: lower lea valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.55
lon: -0.0166667
surface_form: lea valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69
lon: -0.01
The redevelopment of the Lea River Park opens up of new space creating walkways and cycle paths. The project completes the 26-mile long Lee Valley Regional Park which connects Ware in Hertfordshire to the River Thames. In popular culture. The 2005 documentary &quot;What Have You Done Today, Mervyn Day?&quot; focuses on the history and landscape of the Lower Lea Valley.

Geographic entities mentioned:
surface_form: lee valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69
lon: -0.01
Today the canyon bearing the name Doubtful Canyon, is mostly in Cochise County, Arizona, United States, near the New Mexico border. It descends to the east into the Animas Valley past Steins Peak it is in Hidalgo County, New Mexico. The western canyon is now called West Doubtful Canyon and it descends into the San Simon Valley, in Cochise County, Arizona. History.

Geographic entities mentioned:
surface_form: Animas Valley
instance_of: Valley
countries: United States
Mexico
coordinates: lat: 31.9489
lon: -108.807
surface_form: Steins Peak
instance_of: Mountain
countries: United States
coordinates: lat: 32.3336
lon: -109.044
Today the canyon bearing the name Doubtful Canyon, is mostly in Cochise County, Arizona, United States, near the New Mexico border. It descends to the east into the Animas Valley past Steins Peak it is in Hidalgo County, New Mexico. The western canyon is now called West Doubtful Canyon and it descends into the San Simon Valley, in Cochise County, Arizona. History.

Geographic entities mentioned:
surface_form: San Simon Valley
instance_of: Valley
countries: United States
coordinates: lat: 32.8017
lon: -109.633
Settlers began using the springs in the 1840s. In 1873, a Willamette Valley farmer John Minto, a Willamette Valley statesman and farmer began developing a transportation route over the Cascade Mountains, wrote in a 1903 memoire, that Henry States, Frank Cooper, and himself had named hot springs after meeting a one-armed hunter named John Breitenbush, who was camping near the hot springs.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Geography. Galeville is located at (43.088816, -76.178631). According to the United States Census Bureau, the CDP has a total area of, all land. Galeville is north of Onondaga Lake and borders Ley Creek, which flows into the lake. Interstate 81 passes through the eastern side of the community and intersects the New York State Thruway (Interstate 90) north of Galeville. Demographics.

Geographic entities mentioned:
surface_form: Onondaga Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.088888888889
lon: -76.208333333333
Its embrace of the style contrasted with the more restrained use of it on older buildings nearby like the Presbyterian chapel and Church House. The front columns were tall, and the dome top twice that height. The cupola was once open to visitors, allowing for views to Lake Ontario to the north in clear weather.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
For this reason, it has retained more of its traditional colonial architecture than almost any other town in the &quot;eje cafetero&quot;, along with a quiet and relaxed way of life, and as a result, the town and nearby Cocora valley are among the most popular tourist destinations in Colombia.

Geographic entities mentioned:
surface_form: Cocora valley
instance_of: Valley
countries: Colombia
coordinates: lat: 4.6411111111111
lon: -75.541388888889
Its geography is varied, rising from around 1300 m in the fertile valleys of the west of the municipality to the permanently snow-capped summit of the Nevado del Quindío, which at 4750 m is the highest point of the department of Quindío. The town of Salento itself lies on a plateau above the Quindío river valley.

Geographic entities mentioned:
surface_form: Nevado del Quindío
instance_of: Mountain
countries: Colombia
coordinates: lat: 4.7155555555556
lon: -75.388333333333
Its geography is varied, rising from around 1300 m in the fertile valleys of the west of the municipality to the permanently snow-capped summit of the Nevado del Quindío, which at 4750 m is the highest point of the department of Quindío. The town of Salento itself lies on a plateau above the Quindío river valley.

Geographic entities mentioned:
surface_form: Quindío river
instance_of: Watercourse
countries: Colombia
coordinates: lat: 4.393803
lon: -75.798246
The town of Salento itself lies on a plateau above the Quindío river valley. The section of the river valley from Salento to the head of the river is known as the Cocora valley. The town is located at an average altitude of 1895 meters above sea level, with steep drops to the valley floor at its northern and western perimeters. Climate.

Geographic entities mentioned:
surface_form: Cocora valley
instance_of: Valley
countries: Colombia
coordinates: lat: 4.6411111111111
lon: -75.541388888889
&quot;Heretaunga&quot; as a Māori name combines &quot;here&quot;, meaning &quot;to tie up&quot;, and &quot;Tauranga&quot;, literally meaning &quot;to be at home&quot; - the name originated with a mooring place for canoes. The settlement, one of the older suburbs in the Hutt Valley, dates from the 1840s when European settlers sought country sections.

Geographic entities mentioned:
surface_form: Hutt Valley
instance_of: Valley
countries: New Zealand
coordinates: lat: -41.1657
lon: 174.973
2021 Uttarakhand flood. The 2021 Uttarakhand flood, also known as the Chamoli disaster, began on 7 February 2021 in the environs of the Nanda Devi National Park, a UNESCO World Heritage Site in the outer Garhwal Himalayas in Uttarakhand state, India (Maps 1 and 2). It was caused by a large rock and ice avalanche consisting of material dislodged from Ronti peak.

Geographic entities mentioned:
surface_form: Ronti
instance_of: Mountain
countries: India
coordinates: lat: 30.369062
lon: 79.7194
On 8 February 2021, &quot;The Times&quot;, London, reported that a flood was caused by a portion of glacier being torn away and causing a landslide. In satellite images, a scar is visible on the slopes of Nanda Ghunti, a peak on the southwestern rim of the Nanda Devi sanctuary, a wall of mountains surrounding the Nanda Devi massif (Maps 2, 3, and 4).

Geographic entities mentioned:
surface_form: Nanda Ghunti
instance_of: Mountain
countries: India
coordinates: lat: 30.349444444444
lon: 79.716111111111
surface_form: Nanda Devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
Monte Generoso Observatory. The Monte Generoso Observatory () was an astronomical observatory that used to be located near Generoso Vetta atop Monte Generoso in the canton of Ticino, Switzerland. It was initially opened in 1996 with Italian astrophysicist Margherita Hack as its patron.

Geographic entities mentioned:
surface_form: Monte Generoso
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.929444444444
lon: 9.0191666666667
Another, on the right, was engraved in December 220. Other stones in the external walls represent funerary dedications. Also on the western side of the church, the &quot;Pierre du Tauroble&quot; evokes the cult of Cybele and also the Great mother of the Gods of Mount Ida. A chapel in the cathedral has a mosaic by Marc Chagall, dated 1979. The rue des Portiques is a section of the old Roman road.

Geographic entities mentioned:
surface_form: Mount Ida
instance_of: Mountain
countries: Turkey
This opinion reflects the traditional Shinto association between death and pollution (&quot;kegare&quot;). Later Susanoo takes this position over. Christian uses. Some Japanese Christian texts use to refer to what is called Hell in the English versions. For example,
Sometimes means Hades or Sheol, whereas means Gehenna. However 陰府 (yomi) is used in some translations.

Geographic entities mentioned:
surface_form: Gehenna
instance_of: Valley
countries: Israel
coordinates: lat: 31.76916667
lon: 35.22805556
Mount Nirvana. Mount Nirvana, at is the unofficial name of the highest mountain in the Northwest Territories, Canada. The mountain is a part of Nahanni National Park Reserve, the largest national park in the Northwest Territories. History. Part of the Mackenzie Mountains, it was first climbed by Bill Buckingham and Lew Surdam in July 1965.

Geographic entities mentioned:
surface_form: mount nirvana
instance_of: Mountain
countries: Canada
coordinates: lat: 61.8747
lon: -127.68
History. Part of the Mackenzie Mountains, it was first climbed by Bill Buckingham and Lew Surdam in July 1965. Buckingham gave the mountain the moniker of &quot;Mount Nirvana&quot; at that time. Before 2016, only five successful ascent were recorded, all with the assistance of helicopters or floatplane. In June 2016, Nirvana was climbed without assistance for the first time.

Geographic entities mentioned:
surface_form: mount nirvana
instance_of: Mountain
countries: Canada
coordinates: lat: 61.8747
lon: -127.68
In the second half of the 18th century, Kashmir was part of the Durrani Empire, also known the Afghan empire. Its second ruler, Timur Shah Durrani, appointed Amir Khan Sher Jawan as governor. He was responsible for pulling down royal palaces and other buildings around the Dal Lake, which had taken the Mughals and its nobles 170 years to construct. However, he also constructed in Srinagar.

Geographic entities mentioned:
surface_form: Dal Lake
instance_of: Lake
countries: India
coordinates: lat: 34.12
lon: 74.87
The buildings in the complex were designed with a quadrangular layout, constructed primarily from stone, and featured intricate wooden doors, ceilings, and roofs. By the 1930s, Maharaja Hari Singh (1895–1961) commissioned the construction of the Gulab Bhavan palace as his new residence in eastern Srinagar, overlooking the Dal Lake.

Geographic entities mentioned:
surface_form: Dal Lake
instance_of: Lake
countries: India
coordinates: lat: 34.12
lon: 74.87
Activism. Manuel is well known for her activism against corporate development projects in British Columbia, Canada, both those directed to gain tourism, and industry. She has been opposed to such developments as Sun Peaks Resort and Imperial Metals, and protested the Mount Polley mine spill.

Geographic entities mentioned:
surface_form: Mount Polley
instance_of: Mountain
countries: Canada
coordinates: lat: 52.5567
lon: -121.636
Lake Clearwater (village). Lake Clearwater is a village in the Ashburton District of New Zealand between a lake of the same name and the nearby Lake Camp. The village lies within the Ashburton Lakes region.

Geographic entities mentioned:
surface_form: lake of the same name
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.6033
lon: 171.044
surface_form: Lake Camp
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.615
lon: 171.055
Lake Clearwater is a village in the Ashburton District of New Zealand between a lake of the same name and the nearby Lake Camp. The village lies within the Ashburton Lakes region. The area for the village was first laid out in 1920, and the land was gifted to the people of the Ashburton District by the run-holders of the Mount Possession Station, in a series of gifts in 1926, 1949 and 1964.

Geographic entities mentioned:
surface_form: Ashburton Lakes
instance_of: Group of lakes
countries: New Zealand
coordinates: lat: -43.572929
lon: 171.160126
El Capitan () is a peak in Culberson County, Texas, located within Guadalupe Mountains National Park. The 7th-highest peak in Texas at 8,085 ft (2,464 m), El Capitan is part of the Guadalupe Mountains, an exposed portion of a Permian period reef uplifted and exposed by tectonic activity during the late Cretaceous period. The southern terminus of the Guadalupe Mountains, El Capitan looms over U.S.

Geographic entities mentioned:
surface_form: Trans-Pecos
instance_of: Valley
countries: United States
coordinates: lat: 30.56
lon: -103.79
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 36.826666666667
lon: -110.22555555556
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 31.8772
lon: -104.858
While no trail to the summit has been developed, hikers can climb up to the top of El Capitan by first climbing to near the summit of Guadalupe Peak on the developed 4.5-mile Guadalupe Peak Trail, scrambling down to the south onto the Guadalupe Peak-El Capitan saddle, and then hiking up the back of El Capitan to the summit.

Geographic entities mentioned:
surface_form: Guadalupe Peak
instance_of: Mountain
countries: United States
coordinates: lat: 31.891461111111
lon: -104.86071111111
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 36.826666666667
lon: -110.22555555556
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 36.826666666667
lon: -110.22555555556
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 36.826666666667
lon: -110.22555555556
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 31.8772
lon: -104.858
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 31.8772
lon: -104.858
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 31.8772
lon: -104.858
El Capitan (Texas). El Capitan () is a peak in Culberson County, Texas, located within Guadalupe Mountains National Park. The 7th-highest peak in Texas at 8,085 ft (2,464 m), El Capitan is part of the Guadalupe Mountains, an exposed portion of a Permian period reef uplifted and exposed by tectonic activity during the late Cretaceous period.

Geographic entities mentioned:
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 36.826666666667
lon: -110.22555555556
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 31.8772
lon: -104.858
El Capitan () is a peak in Culberson County, Texas, located within Guadalupe Mountains National Park. The 7th-highest peak in Texas at 8,085 ft (2,464 m), El Capitan is part of the Guadalupe Mountains, an exposed portion of a Permian period reef uplifted and exposed by tectonic activity during the late Cretaceous period. The southern terminus of the Guadalupe Mountains, El Capitan looms over U.S.

Geographic entities mentioned:
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 36.826666666667
lon: -110.22555555556
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 31.8772
lon: -104.858
Geology. El Capitan is the southernmost peak of the Guadalupe escarpment, an ancient limestone reef that forms the present-day Guadalupe Mountains. These mountains are an exposed portion of the Capitan Reef Barrier, a 350-mile long reef constructed primarily from calcareous sponges, encrusting algae, such as stromatolites, and lime-rich mud directly from the ocean.

Geographic entities mentioned:
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 36.826666666667
lon: -110.22555555556
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 31.8772
lon: -104.858
Exposing the Guadalupe Mountains area of the reef, the impact of this tectonic event can be clearly seen in the difference in height between the towering El Capitan and the adjacent salt flat graben, vertically driven 1,000 feet apart by the uplift.

Geographic entities mentioned:
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 36.826666666667
lon: -110.22555555556
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 31.8772
lon: -104.858
Human history. Deep in the Chihuahuan Desert, the area around El Capitan is composed of rugged mountains and wind-swept salt flats. As a result, most of the Native American presence in the vicinity was centered around 3 miles southeast of El Capitan in the area now called Pine Springs.

Geographic entities mentioned:
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 36.826666666667
lon: -110.22555555556
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 31.8772
lon: -104.858
While the occasional Spanish expedition, such as that of Antonio de Espejo in 1582, came close to the area around El Capitan, permanent Anglo-European presence in the area dates from the late 1840s, when the region officially became a part of the United States after the American victory in the Mexican–American War.

Geographic entities mentioned:
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 36.826666666667
lon: -110.22555555556
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 31.8772
lon: -104.858
This road, which became known as the &quot;upper&quot; road, to distinguish itself from the original &quot;lower&quot; road through Fort Davis and up the Rio Grande to El Paso, soon became popular among traders and emigrants, their long trains of wagons and mules passing near the brooding face of El Capitan.

Geographic entities mentioned:
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 36.826666666667
lon: -110.22555555556
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 31.8772
lon: -104.858
Taking advantage of the water and timber available, the stagecoach line constructed a station at the Pinery, later called Pine Springs, 3 miles southeast of El Capitan. Though this station only lasted a year before the route was moved south to come under the protection of Forts Stockton and Davis, the Pinery station continued to be used by soldiers, freighters, and emigrants long after.

Geographic entities mentioned:
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 36.826666666667
lon: -110.22555555556
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 31.8772
lon: -104.858
During this period, El Capitan also bore witness to the El Paso Salt War, a violent struggle between Mexican-American residents and Anglo businessmen over access to the salt flats extending west from the base of the mountain. Long known to the Apache, the salt flats were first identified by Europeans in 1692 by the expedition of Diego de Vargas.

Geographic entities mentioned:
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 36.826666666667
lon: -110.22555555556
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 31.8772
lon: -104.858
Quickly becoming an important local resource, generations of Mexicans, and later, Mexican-Americans, braved the hot, dangerous, four-day trail from San Elizario on the Rio Grande to the Hueco Mountains and then east towards El Capitan to fill their wagons with the precious salt. This all changed in the late 1840s, when the region began to have a larger Anglo presence.

Geographic entities mentioned:
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 36.826666666667
lon: -110.22555555556
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 31.8772
lon: -104.858
Decades before the creation of Guadalupe Mountains National Park, travelers by car and bus were already stopping at roadside rest stops to marvel at the sheer sides of El Capitan, take pictures, and write quick messages on the backs of postcards emblazoned with the mountain’s imposing face.

Geographic entities mentioned:
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 36.826666666667
lon: -110.22555555556
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 31.8772
lon: -104.858
During this period, the land that included El Capitan was owned by James Adolphus Williams, whose Williams Ranch house is still extant on park land west of the mountain. After several economic setbacks, Williams sold the land in 1941 to Judge J.C.

Geographic entities mentioned:
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 36.826666666667
lon: -110.22555555556
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 31.8772
lon: -104.858
Forced to run a tortuous gauntlet of state and federal legislators, park officials, and road engineers, as well as property owners and local ranchers, the Hunter donation, which included El Capitan and Guadalupe Peak, was finally deeded over to the Park Service in 1969. Three years later, Guadalupe Mountains National Park was officially opened, allowing public access to the area. Access.

Geographic entities mentioned:
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 36.826666666667
lon: -110.22555555556
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 31.8772
lon: -104.858
Three years later, Guadalupe Mountains National Park was officially opened, allowing public access to the area. Access. As previously noted, El Capitan is located within the boundaries of Guadalupe Mountains National Park, a fee-area located on U.S. Highway 62/180 between Carlsbad and El Paso.

Geographic entities mentioned:
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 36.826666666667
lon: -110.22555555556
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 31.8772
lon: -104.858
Access. As previously noted, El Capitan is located within the boundaries of Guadalupe Mountains National Park, a fee-area located on U.S. Highway 62/180 between Carlsbad and El Paso. The southern terminus of the Guadalupe range, El Capitan is guarded by cliffs on three sides, and those faces are rarely climbed due to the unstable condition of the rock and the sheer nature of the peak.

Geographic entities mentioned:
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 36.826666666667
lon: -110.22555555556
surface_form: el capitan
instance_of: Mountain
countries: United States
coordinates: lat: 31.8772
lon: -104.858
This reef surrounded much of the Delaware Sea, an inland ocean that covered parts of modern southern New Mexico and Trans-Pecos Texas in the Permian period (about 290 million years ago). Near the end of the late Permian period, in the Ochoan epoch, the outlet that allowed sea water to enter the inland waters began to silt over, occasionally closing the inland sea from its source.

Geographic entities mentioned:
surface_form: trans-pecos
instance_of: Valley
countries: United States
coordinates: lat: 30.56
lon: -103.79
By the end of the Ochoan, these deposits had filled the roughly 1,800-ft-deep basin and covered the reef with dry land. Red silt and sand deposited by rivers crossing these new lands eventually formed the dolomitic Rustler Formation, and the Dewey Lake Formation, burying the reef even deeper.

Geographic entities mentioned:
surface_form: dewey lake
instance_of: Lake
countries: United States
coordinates: lat: 47.59166667
lon: -92.94333333
Forestry is the main economic activity of the sector. Recreational tourism activities come second with a navigable body of water of length, including Father Lake (South); Doda Lake (Southeast). This last lake is formed by an enlargement of the Opawica River.

Geographic entities mentioned:
surface_form: Doda Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.40111111
lon: -75.19444444
surface_form: father lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.311388888889
lon: -75.473888888889
The hydrographic slope of Lac Francoise is accessible via the forest road R1051 coming from the North and serving the large peninsula which stretches out on the east side for. This peninsula is surrounded to the north by Lake Du Guesclin and Lac Françoise; to the East and to the South by Doda Lake; Southwest, by Father Lake (Doda Lake tributary).

Geographic entities mentioned:
surface_form: Doda Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.40111111
lon: -75.19444444
surface_form: lac françoise
instance_of: Lake
countries: Canada
coordinates: lat: 49.458888888889
lon: -75.305277777778
surface_form: father lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.311388888889
lon: -75.473888888889
surface_form: doda lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.40111111
lon: -75.19444444
Françoise Lake. Françoise Lake is a freshwater body of the southern part of Eeyou Istchee James Bay (municipality), in the administrative region of Nord-du-Québec, in the province of Quebec, in Canada. The area of Lac Françoise extends into the townships of Grandis and du Guesclin, in the territory of the Eeyou Istchee James Bay (municipality), southwest of Chapais, Quebec.

Geographic entities mentioned:
surface_form: françoise lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.458888888889
lon: -75.305277777778
Françoise Lake. Françoise Lake is a freshwater body of the southern part of Eeyou Istchee James Bay (municipality), in the administrative region of Nord-du-Québec, in the province of Quebec, in Canada. The area of Lac Françoise extends into the townships of Grandis and du Guesclin, in the territory of the Eeyou Istchee James Bay (municipality), southwest of Chapais, Quebec.

Geographic entities mentioned:
surface_form: lac françoise
instance_of: Lake
countries: Canada
coordinates: lat: 49.458888888889
lon: -75.305277777778
He was the Chinese representative of the Design Board which designed the United Nations headquarters in New York City. He, along with wife Lin Huiyin, Mo Zongjiang, and Ji Yutang, discovered and analyzed the first and second oldest timber structures still standing in China, located at Nanchan Temple and Foguang Temple at Mount Wutai.

Geographic entities mentioned:
surface_form: Mount Wutai
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 39.081388888889
lon: 113.56694444444
On February 1, 1954, the &quot;arrieros&quot; Luis Ríos Barrueto, Guillermo Chacón Carrasco, and Jaime Ríos Abarca found the Plomo Mummy (also known as the Boy of El Plomo or La Momia del Cerro El Plomo in Spanish) on Cerro El Plomo. The mummy is a well preserved Inca girl and was the first discovery of a frozen, high-altitude human sacrifice made by the Incas. Casa de Piedra.

Geographic entities mentioned:
surface_form: Cerro El Plomo
instance_of: Mountain
countries: Chile
coordinates: lat: -33.232777777778
lon: -70.212222222222
Yerba Loca Nature Sanctuary. Yerba Loca Nature Sanctuary (Spanish: &quot;Santuario Natural Yerba Loca&quot;) is a protected area that extends from the top of La Paloma Hill () to the top of Cerro El Plomo, dividing the valleys of the Blanco River and Olivares River.

Geographic entities mentioned:
surface_form: Cerro El Plomo
instance_of: Mountain
countries: Chile
coordinates: lat: -33.232777777778
lon: -70.212222222222
The Aucanquilcha complex is much smaller volumetrically than the APVC ignimbrites, but the duration of activity and the location indicate that Aucanquilcha is a subcomponent of the APVC complex. The long-term magma output of Aucanquilcha is comparable to the magma output of other long-term active volcanoes in the central Andes such as Ollagüe and Llullaillaco.

Geographic entities mentioned:
surface_form: Ollagüe
instance_of: Mountain
countries: Bolivia
Chile
coordinates: lat: -21.3
lon: -68.166666666667
surface_form: Llullaillaco
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.719863
lon: -68.536852
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
In all such cases, an early peak in magma output is followed by later lower-volume activity (, followed by). Unzen in Japan and Mount Duff and Lassen Peak in California have similar eruption histories. Such decreases may occur because of the lithostatic load imposed by the edifices on the magma chambers and the increased travel distance of the magma through the edifice. Local setting.

Geographic entities mentioned:
surface_form: Mount Duff
instance_of: Mountain
countries: France
coordinates: lat: -23.1286
lon: -134.974
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
Covering a surface area of, the cluster is surrounded on its northern, western and eastern sides by salt flats and alluvial deposits. On its southern side lies the Cerro Chela volcano. The cluster lies on a thick crust, and arid conditions since the Miocene have preserved its structures.

Geographic entities mentioned:
surface_form: Cerro Chela
instance_of: Mountain
countries: Chile
coordinates: lat: -21.4
lon: -68.5
Aucanquilcha underwent a northwestward flank collapse, generating a debris avalanche deposit. The debris avalanche descended and ran for with an azimuth of 211°, eventually covering an area of. The flow was channeled between Miño Volcano and Cerro Cumbre Negra (an eroded lava massif) towards the dry Rio Loa valley, favouring the preservation of the slide deposit.

Geographic entities mentioned:
surface_form: Miño Volcano
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -21.183333333333
lon: -68.6
surface_form: cumbre negra
instance_of: Mountain
countries: Chile
coordinates: lat: -31.766666666667
lon: -70.733333333333
Another landslide occurred during the Redondo stage on the eastern side of the main volcano into the Salar de Carcote. It has the classic hummocky topography of landslides and covers a length of and a surface area of, roughly half of the surface area of the Mount St Helens avalanche of 1980 and one-third of the surface area of the Ollagüe avalanche.

Geographic entities mentioned:
surface_form: Ollagüe
instance_of: Mountain
countries: Bolivia
Chile
coordinates: lat: -21.3
lon: -68.166666666667
The total volume of this group is, indicating a flux rate of. The 3.6–2.3 mya Polan group, with ten dispersed volcanoes including Miño Volcano, is the largest group in the cluster and includes Tres Monos, La Luna, Cerro Polan, Chaihuiri, Miño Volcano and the lavas of the Aucanquilcha platform.

Geographic entities mentioned:
surface_form: Miño Volcano
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -21.183333333333
lon: -68.6
surface_form: miño volcano
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -21.183333333333
lon: -68.6
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
Chaihuiri (2.39 mya) is a lava dome with moraines and two short lava flows; it is the youngest Polan group volcano. The total volume of this group is, indicating a flux rate of. After the four main phases, some scoria cones of basaltic composition, including Poruñita and Luna de Tierra, formed between Aucanquilcha and Ollagüe. Aucanquilcha proper.

Geographic entities mentioned:
surface_form: Ollagüe
instance_of: Mountain
countries: Bolivia
Chile
coordinates: lat: -21.3
lon: -68.166666666667
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333