Sarmila/GeoWiki-Features huggingface dataset:
Pinnacle Peak (Whatcom County, Washington). Pinnacle Peak is a mountain summit in the North Cascades Range of Washington, United States. It is located within North Cascades National Park, between Pyramid Peak and Paul Bunyans Stump, which is the nearest higher peak. It rises steeply from Diablo Lake, one of the reservoirs on the Skagit River.

Geographic entities mentioned:
surface_form: Paul Bunyans Stump
instance_of: Mountain
countries: United States
coordinates: lat: 48.66624
lon: -121.14984
surface_form: pyramid
instance_of: Lake
countries: United States
coordinates: lat: 40.033333333333
lon: -119.56666666667
surface_form: pyramid peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.845
lon: -120.158
surface_form: pyramid peak
instance_of: Mountain
countries: United States
coordinates: lat: 32.2378
lon: -108.719
surface_form: pyramid peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.67485
lon: -121.14568
surface_form: pyramid peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.7963
lon: -113.991
surface_form: pyramid peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.8733
lon: -113.831
surface_form: pyramid peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0717
lon: -106.95
surface_form: pyramid peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.3075
lon: -142.3317
surface_form: pyramid peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.11138889
lon: -121.405
surface_form: pyramid peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.9065
lon: -118.46211
surface_form: pyramid peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.8068426
lon: -121.8120695
It rises steeply from Diablo Lake, one of the reservoirs on the Skagit River. It is part of a group of peaks that form the northern end of a chain running south through climbing destinations such as Colonial Peak and Snowfield Peak. Like many North Cascade peaks, Pinnacle Peak is more notable for its large, steep rise above local terrain than for its absolute elevation.

Geographic entities mentioned:
surface_form: Colonial Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.6615
lon: -121.121
surface_form: Snowfield Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.6353
lon: -121.138
Like many North Cascade peaks, Pinnacle Peak is more notable for its large, steep rise above local terrain than for its absolute elevation. Precipitation runoff from the mountain drains into Diablo Lake and Skagit River. The approach is via the Pyramid Lake Trail, starting near Diablo Dam on the North Cascades Highway. From the lake, there is route-finding up Pyramid Arm to Colonial Glacier.

Geographic entities mentioned:
surface_form: pyramid lake
instance_of: Lake
countries: United States
coordinates: lat: 40.033333333333
lon: -119.56666666667
surface_form: pyramid lake
instance_of: Lake
countries: United States
coordinates: lat: 38.848
lon: -120.141
Precipitation runoff from the mountain drains into Diablo Lake and Skagit River. The approach is via the Pyramid Lake Trail, starting near Diablo Dam on the North Cascades Highway. From the lake, there is route-finding up Pyramid Arm to Colonial Glacier. Climate. Pinnacle Peak is located in the marine west coast climate zone of western North America.

Geographic entities mentioned:
surface_form: pyramid
instance_of: Lake
countries: United States
coordinates: lat: 40.033333333333
lon: -119.56666666667
Pinnacle Peak (Whatcom County, Washington). Pinnacle Peak is a mountain summit in the North Cascades Range of Washington, United States. It is located within North Cascades National Park, between Pyramid Peak and Paul Bunyans Stump, which is the nearest higher peak. It rises steeply from Diablo Lake, one of the reservoirs on the Skagit River.

Geographic entities mentioned:
surface_form: pinnacle peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.7577989
lon: -121.7325035
surface_form: pinnacle peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.173663
lon: -121.973412
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: pinnacle peak (whatcom county, washington)
instance_of: Mountain
countries: United States
coordinates: lat: 48.67124
lon: -121.14929
surface_form: pinnacle peak
instance_of: Mountain
countries: United States
coordinates: lat: 33.725583333333
lon: -111.87025
Pinnacle Peak (Whatcom County, Washington). Pinnacle Peak is a mountain summit in the North Cascades Range of Washington, United States. It is located within North Cascades National Park, between Pyramid Peak and Paul Bunyans Stump, which is the nearest higher peak. It rises steeply from Diablo Lake, one of the reservoirs on the Skagit River.

Geographic entities mentioned:
surface_form: pinnacle peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.7577989
lon: -121.7325035
surface_form: pinnacle peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.173663
lon: -121.973412
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: pinnacle peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.67124
lon: -121.14929
surface_form: pinnacle peak
instance_of: Mountain
countries: United States
coordinates: lat: 33.725583333333
lon: -111.87025
It is part of a group of peaks that form the northern end of a chain running south through climbing destinations such as Colonial Peak and Snowfield Peak. Like many North Cascade peaks, Pinnacle Peak is more notable for its large, steep rise above local terrain than for its absolute elevation. Precipitation runoff from the mountain drains into Diablo Lake and Skagit River.

Geographic entities mentioned:
surface_form: pinnacle peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.7577989
lon: -121.7325035
surface_form: pinnacle peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.173663
lon: -121.973412
surface_form: pinnacle peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.67124
lon: -121.14929
surface_form: pinnacle peak
instance_of: Mountain
countries: United States
coordinates: lat: 33.725583333333
lon: -111.87025
The approach is via the Pyramid Lake Trail, starting near Diablo Dam on the North Cascades Highway. From the lake, there is route-finding up Pyramid Arm to Colonial Glacier. Climate. Pinnacle Peak is located in the marine west coast climate zone of western North America. Most weather fronts originating in the Pacific Ocean move northeast toward the Cascade Mountains.

Geographic entities mentioned:
surface_form: pinnacle peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.7577989
lon: -121.7325035
surface_form: pinnacle peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.173663
lon: -121.973412
surface_form: pinnacle peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.67124
lon: -121.14929
surface_form: pinnacle peak
instance_of: Mountain
countries: United States
coordinates: lat: 33.725583333333
lon: -111.87025
Brunia pentandra. &quot;Brunia pentandra&quot; is a shrub belonging to the genus &quot;Brunia&quot;. The species is endemic to the Western Cape and is part of the fynbos. The plant has a range of 1170 km². It occurs from the Cederberg and Kouebokkeveld Mountains to the Witsenberg Plains. (pages needed)

Geographic entities mentioned:
surface_form: Kouebokkeveld Mountains
instance_of: Plateau
countries: South Africa
coordinates: lat: -32.2
lon: 19.4167
Topography. The lake is situated in an altitude of 1725 m, an egg-shaped form stretching itself along a north–south axis in the valley of Gaube. This steep-sided valley is located at the foot of the Vignemale (3298M). The lake is surrounded by the peak Mayouret (2688 m) to the east, the big Peak of the Paloumères (2720 m) to the southeast, and the peak of Gaube (2377 m) to the northwest.

Geographic entities mentioned:
surface_form: Vignemale
instance_of: Mountain
countries: Spain
France
coordinates: lat: 42.773888888889
lon: -0.1475
Charlotte, Rochester, New York. Charlotte () is a neighborhood in Rochester, in the U.S. state of New York, located along the western bank of the mouth of the Genesee River along the southern shore of Lake Ontario. It is the home of the Port of Rochester and Charlotte High School. Early settlers.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
H. Moore, and James Gourley. (Miller Mountain is west-southwest of Henderson Mountain). Climate. Based on the Köppen climate classification, Henderson Mountain is located in a subarctic climate zone characterized by long, usually very cold winters, and mild summers. Winter temperatures can drop below 0 °F with wind chill factors below −10 °F.

Geographic entities mentioned:
surface_form: miller mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.489
lon: -75.9522
surface_form: henderson mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.05133
lon: -109.9449
surface_form: miller mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.0655
lon: -118.192
Henderson Mountain. Henderson Mountain is a summit in Park County, Montana, United States. Description. Henderson Mountain is located north of Cooke City, Montana, in the Beartooth Mountains which are a subrange of the Rocky Mountains. It is set within the New World Mining District and the Custer-Gallatin National Forest.

Geographic entities mentioned:
surface_form: henderson mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.05133
lon: -109.9449
The mountain is a laccolith composed of Cambrian limestone, breccia, and Eocene dacite porphyry. Gold was discovered on Henderson Mountain in 1888. In the mid-1990s, Henderson Mountain was the epicenter of legal fighting over plans to mine a billion dollars' worth of gold and silver from the mountain which would threaten nearby Yellowstone National Park.

Geographic entities mentioned:
surface_form: henderson mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.05133
lon: -109.9449
Gold was discovered on Henderson Mountain in 1888. In the mid-1990s, Henderson Mountain was the epicenter of legal fighting over plans to mine a billion dollars' worth of gold and silver from the mountain which would threaten nearby Yellowstone National Park. The environmental controversy ended when the US government bought out the mining claim.

Geographic entities mentioned:
surface_form: henderson mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.05133
lon: -109.9449
surface_form: yellowstone
instance_of: Lake
countries: United States
coordinates: lat: 44.466666666667
lon: -110.36666666667
H. Moore, and James Gourley. (Miller Mountain is west-southwest of Henderson Mountain). Climate. Based on the Köppen climate classification, Henderson Mountain is located in a subarctic climate zone characterized by long, usually very cold winters, and mild summers. Winter temperatures can drop below 0 °F with wind chill factors below −10 °F.

Geographic entities mentioned:
surface_form: henderson mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.05133
lon: -109.9449
It is set within the New World Mining District and the Custer-Gallatin National Forest. Precipitation runoff from the mountain's north slope drains into Fisher Creek which is a tributary of the Clarks Fork Yellowstone River, whereas the south slope drains into Miller Creek → Soda Butte Creek → Lamar River. Topographic relief is significant as the summit rises nearly above Fisher Creek in.

Geographic entities mentioned:
surface_form: yellowstone
instance_of: Lake
countries: United States
coordinates: lat: 44.466666666667
lon: -110.36666666667
Lotus Flower Tower. Lotus Flower Tower is a peak in the Cirque of the Unclimbables, Northwest Territories, Canada. The tower is on a ridge one kilometre to the southwest of Mount Sir James MacBrien, and though the tower is not prominent in relation to surrounding peaks, it is noted for its sheer rock walls which are home to classic multi-pitch climbing routes. Climbing history.

Geographic entities mentioned:
surface_form: Mount Sir James MacBrien
instance_of: Mountain
countries: Canada
coordinates: lat: 62.1231
lon: -127.68
surface_form: the tower
instance_of: Mountain
countries: Canada
coordinates: lat: 50.8567
lon: -115.29
surface_form: the tower
instance_of: Mountain
countries: Canada
coordinates: lat: 50.8567
lon: -115.29
Climbing history. The first ascent was made by William J. Buckingham and party on July 16, 1960, via a traverse from &quot;Tathagata Tower&quot; along the ridge which connects Lotus Flower Tower to Mount Sir James MacBrien. The peak's second ascent and first ascent of the sheer 2200 foot southeast face was made in 1968 by Harthon &quot;Sandy&quot; Bill, Tom Frost, and James McCarthy.

Geographic entities mentioned:
surface_form: mount sir james macbrien
instance_of: Mountain
countries: Canada
coordinates: lat: 62.1231
lon: -127.68
surface_form: lotus flower tower
instance_of: Mountain
countries: Canada
coordinates: lat: 62.1143
lon: -127.697
Lotus Flower Tower. Lotus Flower Tower is a peak in the Cirque of the Unclimbables, Northwest Territories, Canada. The tower is on a ridge one kilometre to the southwest of Mount Sir James MacBrien, and though the tower is not prominent in relation to surrounding peaks, it is noted for its sheer rock walls which are home to classic multi-pitch climbing routes. Climbing history.

Geographic entities mentioned:
surface_form: lotus flower tower
instance_of: Mountain
countries: Canada
coordinates: lat: 62.1143
lon: -127.697
Royal Terrace, Edinburgh. Royal Terrace is a grand street in the city of Edinburgh, Scotland, on the north side of Calton Hill within the New Town and part of the UNESCO World Heritage Site inscribed in 1995, built on the south side of a setted street, facing the sloping banks of London Road Gardens, formerly Royal Terrace Gardens, with views looking north towards Leith and the Firth of Forth.

Geographic entities mentioned:
surface_form: Calton Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.955278
lon: -3.182222
Association with the Cruthin therefore places the roots of the tribe in north-east Ireland, which is compatible with other accounts that state their origin as being on the shores of Lough Neagh. Lough Neagh is said to have burst sometime around 65AD and this flooding or subsequent floods may have forced the tribes in the area to migrate.

Geographic entities mentioned:
surface_form: Lough Neagh
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.618333333333
lon: -6.3952777777778
Little Grassy Lake (Florida). Little Grassy Lake (occasionally considered to be a smaller part of Grassy Lake) is a nearly-round lake south of Lake Placid, Florida. It has residences on the north shore, U.S. Route 27 is on the east shore and the south and west shores are bordered by woods. It seems U.S.

Geographic entities mentioned:
surface_form: lake placid
instance_of: Lake
countries: United States
coordinates: lat: 27.2425
lon: -81.363611111111
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9344286
lon: -96.9790408
surface_form: round lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.0648
lon: -75.1033
surface_form: lake placid
instance_of: Lake
countries: United States
coordinates: lat: 44.312978
lon: -73.993864
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 46.1508
lon: -86.7447
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.070277777778
lon: -74.584722222222
surface_form: little grassy lake
instance_of: Lake
countries: United States
coordinates: lat: 37.6368
lon: -89.1455
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 42.934604
lon: -73.7823057
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 27.9631
lon: -81.674
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 45.036388888889
lon: -97.773055555556
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 43.531388888889
lon: -75.180277777778
surface_form: grassy lake
instance_of: Lake
countries: United States
coordinates: lat: 29.7779
lon: -91.1104
surface_form: grassy lake
instance_of: Lake
countries: United States
coordinates: lat: 29.7779
lon: -91.1104
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.8685
lon: -93.4925
surface_form: lake placid
instance_of: Lake
countries: United States
coordinates: lat: 29.5477
lon: -98.0082
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 48.161666666667
lon: -116.63805555556
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 45.6020431
lon: -122.4032555
surface_form: grassy lake
instance_of: Lake
countries: United States
coordinates: lat: 27.255
lon: -81.3343
surface_form: grassy lake
instance_of: Lake
countries: United States
coordinates: lat: 27.255
lon: -81.3343
surface_form: little grassy lake
instance_of: Lake
countries: United States
coordinates: lat: 27.252
lon: -81.3419
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 41.837095
lon: -86.418541
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.964444444444
lon: -96.827222222222
Little Grassy Lake (Florida). Little Grassy Lake (occasionally considered to be a smaller part of Grassy Lake) is a nearly-round lake south of Lake Placid, Florida. It has residences on the north shore, U.S. Route 27 is on the east shore and the south and west shores are bordered by woods. It seems U.S.

Geographic entities mentioned:
surface_form: little grassy lake
instance_of: Lake
countries: United States
coordinates: lat: 37.6368
lon: -89.1455
surface_form: grassy lake
instance_of: Lake
countries: United States
coordinates: lat: 29.7779
lon: -91.1104
surface_form: grassy lake (florida)
instance_of: Lake
countries: United States
coordinates: lat: 27.255
lon: -81.3343
surface_form: little grassy lake (florida)
instance_of: Lake
countries: United States
coordinates: lat: 27.252
lon: -81.3419
It has residences on the north shore, U.S. Route 27 is on the east shore and the south and west shores are bordered by woods. It seems U.S. 27 was built on land filled in and that Little Grassy lake was once a cove on Grassy Lake's west side. Little Grassy Lake only has public access along the public right of way along US 27. There are no public boat ramps or no public swimming areas.

Geographic entities mentioned:
surface_form: little grassy lake
instance_of: Lake
countries: United States
coordinates: lat: 37.6368
lon: -89.1455
surface_form: grassy lake
instance_of: Lake
countries: United States
coordinates: lat: 29.7779
lon: -91.1104
surface_form: grassy lake
instance_of: Lake
countries: United States
coordinates: lat: 29.7779
lon: -91.1104
surface_form: grassy lake
instance_of: Lake
countries: United States
coordinates: lat: 27.255
lon: -81.3343
surface_form: grassy lake
instance_of: Lake
countries: United States
coordinates: lat: 27.255
lon: -81.3343
surface_form: little grassy lake
instance_of: Lake
countries: United States
coordinates: lat: 27.252
lon: -81.3419
It seems U.S. 27 was built on land filled in and that Little Grassy lake was once a cove on Grassy Lake's west side. Little Grassy Lake only has public access along the public right of way along US 27. There are no public boat ramps or no public swimming areas. No information is available about the types of fish in this lake.

Geographic entities mentioned:
surface_form: little grassy lake
instance_of: Lake
countries: United States
coordinates: lat: 37.6368
lon: -89.1455
surface_form: grassy lake
instance_of: Lake
countries: United States
coordinates: lat: 29.7779
lon: -91.1104
surface_form: grassy lake
instance_of: Lake
countries: United States
coordinates: lat: 27.255
lon: -81.3343
surface_form: little grassy lake
instance_of: Lake
countries: United States
coordinates: lat: 27.252
lon: -81.3419
The lake is a part of the Vembanad-Kol wetland system which extends from Alappuzha in the south to Azheekkode in the north, making it by far India's longest lake at just over 96.5 km in length. The lake is fed by 10 rivers flowing into it including the six major rivers of central Kerala namely the Achenkovil, Manimala, Meenachil river, Muvattupuzha river, Pamba and Periyar.

Geographic entities mentioned:
surface_form: Pamba
instance_of: Watercourse
countries: India
coordinates: lat: 9.5
lon: 76.416666666667
surface_form: pamba
instance_of: Watercourse
countries: India
coordinates: lat: 9.5
lon: 76.416666666667
Vembanad. Vembanad () is the longest lake in India, and the largest in the state of Kerala. The lake has an area of 2,033 square kilometers and a maximum length of 96.5 km. Spanning three districts in the state of Kerala, it is known as Vembanad Lake in Kottayam, Vaikom, Changanassery, Punnamada Lake in Alappuzha, Punnappra, Kuttanadu and Kochi Lake in Kochi.

Geographic entities mentioned:
surface_form: kochi lake
instance_of: Lake
countries: India
coordinates: lat: 9.85
lon: 76.35
surface_form: vembanad
instance_of: Lake
countries: India
coordinates: lat: 9.85
lon: 76.35
Spanning three districts in the state of Kerala, it is known as Vembanad Lake in Kottayam, Vaikom, Changanassery, Punnamada Lake in Alappuzha, Punnappra, Kuttanadu and Kochi Lake in Kochi. Several groups of small islands including Vypin, Mulavukad, Maradu, Udayamperoor, Vallarpadam, and Willingdon Island are located in the Kochi Lake portion.

Geographic entities mentioned:
surface_form: kochi lake
instance_of: Lake
countries: India
coordinates: lat: 9.85
lon: 76.35
Vembanad. Vembanad () is the longest lake in India, and the largest in the state of Kerala. The lake has an area of 2,033 square kilometers and a maximum length of 96.5 km. Spanning three districts in the state of Kerala, it is known as Vembanad Lake in Kottayam, Vaikom, Changanassery, Punnamada Lake in Alappuzha, Punnappra, Kuttanadu and Kochi Lake in Kochi.

Geographic entities mentioned:
surface_form: vembanad
instance_of: Lake
countries: India
coordinates: lat: 9.85
lon: 76.35
Kochi Port is built around Willingdon Island and Vallarpadam island. Kuttanad, also known as &quot;The Rice Bowl of Kerala&quot;, has the lowest altitude in India, and is also one of the few places in the world where cultivation takes place below sea level. Kuttanad lies on the southern portion of Vembanad. The Nehru Trophy Boat Race is conducted in a portion of the lake.

Geographic entities mentioned:
surface_form: vembanad
instance_of: Lake
countries: India
coordinates: lat: 9.85
lon: 76.35
Kuttanad lies on the southern portion of Vembanad. The Nehru Trophy Boat Race is conducted in a portion of the lake. High levels of pollution have been noticed at certain hotspots of the Vembanad backwaters. The Government of India has identified the Vembanad wetland under the National Wetlands Conservation Programme. Geography and hydrography.

Geographic entities mentioned:
surface_form: vembanad
instance_of: Lake
countries: India
coordinates: lat: 9.85
lon: 76.35
The Nehru Trophy Boat Race is conducted in a portion of the lake. High levels of pollution have been noticed at certain hotspots of the Vembanad backwaters. The Government of India has identified the Vembanad wetland under the National Wetlands Conservation Programme. Geography and hydrography. The Vembanad lake is 96.5 km long, making it the longest lake in India.

Geographic entities mentioned:
surface_form: vembanad
instance_of: Lake
countries: India
coordinates: lat: 9.85
lon: 76.35
The Government of India has identified the Vembanad wetland under the National Wetlands Conservation Programme. Geography and hydrography. The Vembanad lake is 96.5 km long, making it the longest lake in India. The Vembanad wetland system covers an area of over 2033.02 km² thereby making it the largest wetland system in India.

Geographic entities mentioned:
surface_form: vembanad
instance_of: Lake
countries: India
coordinates: lat: 9.85
lon: 76.35
The lake surrounds the islands of Pathiramanal, Perumbalam and Pallippuram. The Vembanad Lake is approximately 14 kilometers wide at its widest point. The lake is a part of the Vembanad-Kol wetland system which extends from Alappuzha in the south to Azheekkode in the north, making it by far India's longest lake at just over 96.5 km in length.

Geographic entities mentioned:
surface_form: vembanad
instance_of: Lake
countries: India
coordinates: lat: 9.85
lon: 76.35
This barrier has helped farmers in Kuttanad by freeing the area of salinity and allowing them an additional crop in the dry season. The Thanneermukkom barrier is located at one of the narrower parts of the Vembanad Lake. Only two-thirds of the original number of gates are opened in July to release flood flow. These gates remain closed until mid-November.

Geographic entities mentioned:
surface_form: vembanad
instance_of: Lake
countries: India
coordinates: lat: 9.85
lon: 76.35
The major rivers of Muvattupuzha, Meenachil, Pamba and Achencovil rivers, are all navigable up to distances of about 30 km upstream in the tidal reach. The Kottappuram–Kollam segment of the west coast canal system has a major chunk passing through the Vembanad Lake and spans a total of 209 km. It has been declared as a National Waterway. Ecological importance.

Geographic entities mentioned:
surface_form: vembanad
instance_of: Lake
countries: India
coordinates: lat: 9.85
lon: 76.35
Almost all villages in these areas can be accessed via water transport. The major rivers of Muvattupuzha, Meenachil, Pamba and Achencovil rivers, are all navigable up to distances of about 30 km upstream in the tidal reach. The Kottappuram–Kollam segment of the west coast canal system has a major chunk passing through the Vembanad Lake and spans a total of 209 km.

Geographic entities mentioned:
surface_form: pamba
instance_of: Watercourse
countries: India
coordinates: lat: 9.5
lon: 76.416666666667
Hōei eruption. The Hōei eruption of Mount Fuji started on December 16, 1707 (during the Hōei era, 23rd day of the 11th month of the 4th year) and ended on February 24, 1708. It was the last confirmed eruption of Mount Fuji, with three unconfirmed eruptions reported from 1708 to 1854. The eruption took place during the reign of Emperor Higashiyama and the Shogun was Tokugawa Tsunayoshi.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
It has been classified as an explosive eruption. Lahars soon followed the eruption because of heavy rainfall and flooding in the area. It is suggested that two types of magma, silicic and basaltic magma, mixed together as a result of the earthquake. The eruption happened on Mount Fuji's east-southeast flank and formed three new volcanic vents, named No. 1, No. 2, and No. 3 Hōei vents.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
In April 1904, he briefly worked at a military hospital and Lake Como, as well as in Baden-Baden. From 1904–1906, he served as an assistant physician in Dresden. In April 1905, he collected lichens at Lake Garda, in Bolzano and Merano, and in summer 1905 around Dresden and in Saxon Switzerland. From 1906 to 1910, Lettau established his first ophthalmological practice in Arnstadt (Thuringia).

Geographic entities mentioned:
surface_form: Lake Garda
instance_of: Lake
countries: Italy
coordinates: lat: 45.633333333333
lon: 10.666666666667
In the fall of 1907, Lettau collected during a trip through Montafon in Vorarlberg, St Anton in West Tyrol, and in the Sonnwend mountain group in North Tyrol; in July 1908, he collected again at Bludenz in Vorarlberg and at Hohentwiel; in June 1909, he collected on the Samland coast in East Prussia.

Geographic entities mentioned:
surface_form: Montafon
instance_of: Valley
countries: Austria
coordinates: lat: 47.08
lon: 9.9
surface_form: Hohentwiel
instance_of: Mountain
countries: Germany
coordinates: lat: 47.764722222222
lon: 8.8188888888889
With clear weather, the mountain can be seen by hikers from High Divide or Hurricane Hill. The nearest higher neighbor is Mount Carrie to the east-southeast, and Mount Olympus rises to the south. Precipitation runoff from the mountain drains north into Cat Creek which is a tributary of the Elwha River, and south into the Hoh River.

Geographic entities mentioned:
surface_form: Mount Carrie
instance_of: Mountain
countries: United States
coordinates: lat: 47.89425
lon: -123.64908
surface_form: mount olympus
instance_of: Mountain
countries: United States
coordinates: lat: 47.801305555556
lon: -123.71083333333
surface_form: mount olympus
instance_of: Mountain
countries: United States
coordinates: lat: 40.6566
lon: -111.771
Cat Peak. Cat Peak is a mountain summit within Olympic National Park in Clallam County of Washington state. Description. Set within the Daniel J. Evans Wilderness, Cat Peak is the westernmost peak of the Bailey Range, which is a subrange of the Olympic Mountains. With clear weather, the mountain can be seen by hikers from High Divide or Hurricane Hill.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: cat peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.90009
lon: -123.67991
Cat Peak. Cat Peak is a mountain summit within Olympic National Park in Clallam County of Washington state. Description. Set within the Daniel J. Evans Wilderness, Cat Peak is the westernmost peak of the Bailey Range, which is a subrange of the Olympic Mountains. With clear weather, the mountain can be seen by hikers from High Divide or Hurricane Hill.

Geographic entities mentioned:
surface_form: cat peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.90009
lon: -123.67991
Description. Set within the Daniel J. Evans Wilderness, Cat Peak is the westernmost peak of the Bailey Range, which is a subrange of the Olympic Mountains. With clear weather, the mountain can be seen by hikers from High Divide or Hurricane Hill. The nearest higher neighbor is Mount Carrie to the east-southeast, and Mount Olympus rises to the south.

Geographic entities mentioned:
surface_form: cat peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.90009
lon: -123.67991
Climate. Based on the Köppen climate classification, Cat Peak is located in the marine west coast climate zone of western North America. Weather fronts originating in the Pacific Ocean travel northeast toward the Olympic Mountains. As fronts approach, they are forced upward by the peaks (orographic lift), causing them to drop their moisture in the form of rain or snow.

Geographic entities mentioned:
surface_form: cat peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.90009
lon: -123.67991
Cat Peak. Cat Peak is a mountain summit within Olympic National Park in Clallam County of Washington state. Description. Set within the Daniel J. Evans Wilderness, Cat Peak is the westernmost peak of the Bailey Range, which is a subrange of the Olympic Mountains. With clear weather, the mountain can be seen by hikers from High Divide or Hurricane Hill.

Geographic entities mentioned:
surface_form: daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
20.7% of the total district population). Chhetris form the second largest demographic group after Newars in the Kathmandu Valley, together with Lalitpur (Patan) and Bhaktapur, with a population of 621,346. Other districts with more than 150,000 Chhetri population are Kailali, Kanchanpur, Dang, Jhapa and Morang.

Geographic entities mentioned:
surface_form: Kathmandu Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
Shire of Herberton. The Shire of Herberton was a local government area of Queensland. It was located on the Atherton Tableland, a plateau forming part of the Great Dividing Range west of the city of Cairns.

Geographic entities mentioned:
surface_form: Atherton Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
Credit Indian Village. The Credit Indian Village was a settlement on the banks of the Credit River in modern-day Mississauga, Ontario. The settlement was initially founded in 1826 by a band of Mississaugas of the Credit who had converted to Christianity. Notable figures in the early settlement include Peter Jones, the son of Ontario surveyor Augustus Jones and his wife, Tuhbenahneequay.

Geographic entities mentioned:
surface_form: Credit River
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.5478
lon: -79.5808
The population is seen to be reducing as a result. Sino-Indian disputes. As of 2005, the route from Demchok to Lake Manasarovar in Tibet was closed and local trade with China was prohibited, although local residents admit that clandestine trade with China had been ongoing for decades.

Geographic entities mentioned:
surface_form: Lake Manasarovar
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 30.666666666667
lon: 81.5
Traffic. Originally proposed as a secondary mainline, it mainly carried freight, including: Weardale limestone; West County Durham coal; and Cleveland ironstone to support the growing industrialisation on Teesside. Its secondary transport was the shipment of agricultural supplies in and produce/livestock out from the valleys farms. Decline and closure.

Geographic entities mentioned:
surface_form: Weardale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.716
lon: -1.925
They undertook similar developments in Australia, which became the city of Mildura, and the town of Renmark and Paringa. Biography. Chaffey was born in Brockville, Canada West and attended Kingston Grammar School on Lake Ontario. Chaffey's family was of Scottish heritage. Although not interested in schoolroom instruction, he read engineering books from the local library.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Chaffey along with the other pioneers believed this name would bring more people to this southeastern part of California. In 1905, Chaffey purchased the ranch of John Shepherd at Manzanar, California, located in California's Owens Valley. Chaffey subdivided the ranch, along with other adjacent ranches, and founded the town of Manzanar in 1910.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
Life. Born in the early 19th century in the village of Shalkote in the undivided princely state of Jammu and Kashmir, Naranjan Singh Bhalla was one of the most prominent Sikh faces of the Kashmir valley. He played an active role in the Indian freedom movement and many times evaded arrest.

Geographic entities mentioned:
surface_form: Kashmir valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
Elias National Park and Preserve, in the U.S. state of Alaska. The remote peak is situated northwest of Yakutat, and northwest of Mount Logan. Mount Chitina rises above the confluence of the Chitina Glacier and the Logan Glacier. Precipitation runoff from the mountain drains into the Chitina River, which in turn is part of the Copper River drainage basin.

Geographic entities mentioned:
surface_form: Mount Logan
instance_of: Mountain
countries: Canada
coordinates: lat: 60.567222222222
lon: -140.40277777778
surface_form: mount logan
instance_of: Mountain
countries: United States
coordinates: lat: 39.401666666667
lon: -108.18888888889
Mount Chitina. Mount Chitina is an 8,424-foot (2,568-meter) mountain summit located in the Saint Elias Mountains of Wrangell-St. Elias National Park and Preserve, in the U.S. state of Alaska. The remote peak is situated northwest of Yakutat, and northwest of Mount Logan. Mount Chitina rises above the confluence of the Chitina Glacier and the Logan Glacier.

Geographic entities mentioned:
surface_form: mount chitina
instance_of: Mountain
countries: United States
coordinates: lat: 60.9658
lon: -141.2625
Elias National Park and Preserve, in the U.S. state of Alaska. The remote peak is situated northwest of Yakutat, and northwest of Mount Logan. Mount Chitina rises above the confluence of the Chitina Glacier and the Logan Glacier. Precipitation runoff from the mountain drains into the Chitina River, which in turn is part of the Copper River drainage basin.

Geographic entities mentioned:
surface_form: mount chitina
instance_of: Mountain
countries: United States
coordinates: lat: 60.9658
lon: -141.2625
The mountain's name is derived from the Chitina Glacier located at the base of the north slope, and was first published on a Canadian topographic map in 1958 no
Climate. Based on the Köppen climate classification, Mount Chitina is located in a subarctic climate zone with long, cold, snowy winters, and cool summers.

Geographic entities mentioned:
surface_form: mount chitina
instance_of: Mountain
countries: United States
coordinates: lat: 60.9658
lon: -141.2625
Geography. The Taubenkopf, like the hills of Breitenberg (545.2 m), Wetterkreuzberg (400.7 m), Hüttenberg (591.2 m) and the Kanzel (531.7 m), is one of the outlying peaks on the Kalmit massif (672.6 m). Its summit lies from the &quot;Kalmitstraße&quot; road (L515) and ca. northeast of the summit of the Kalmit itself, the highest peak in the Palatine Forest region.

Geographic entities mentioned:
surface_form: Wetterkreuzberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.3126
lon: 8.10708
surface_form: Kalmit
instance_of: Mountain
countries: Germany
coordinates: lat: 49.318888888889
lon: 8.0827777777778
surface_form: hüttenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.315555555555555
lon: 8.070638888888888
surface_form: breitenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.309
lon: 8.09033
surface_form: breitenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 47.5486
lon: 10.55186
surface_form: kanzel
instance_of: Mountain
countries: Germany
coordinates: lat: 48.8877
lon: 13.5321
surface_form: taubenkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 49.3225
lon: 8.09
Its summit lies from the &quot;Kalmitstraße&quot; road (L515) and ca. northeast of the summit of the Kalmit itself, the highest peak in the Palatine Forest region. Before storm damage and the subsequent removal of wood, the summit dome was in the shape of a dove's head (&quot;Taubenkopf&quot;).

Geographic entities mentioned:
surface_form: Kalmit
instance_of: Mountain
countries: Germany
coordinates: lat: 49.318888888889
lon: 8.0827777777778
surface_form: kalmit
instance_of: Mountain
countries: Germany
coordinates: lat: 49.318888888889
lon: 8.0827777777778
Tourism. The Taubenkopf is an important hub for several walking routes, which converge 20 metres in height below the summit. These are the blue and white waymarked path from the Totenkopf via the Hahnenschritt, the white and green main trail from Maikammer and the unmarked Klausental to Diedesfeld footpath (the Hinkelstein Path).

Geographic entities mentioned:
surface_form: totenkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 51.4544
lon: 8.78472
surface_form: totenkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 48.0808
lon: 7.67056
Before storm damage and the subsequent removal of wood, the summit dome was in the shape of a dove's head (&quot;Taubenkopf&quot;). Following the deforestation there is a 270 degree outlook from west (into the Palatine Forest) through north (Hohe Loog) to east (Klausental, Sommerberg and the Rhine Plain). Few hilltops of this height so close to the Rhine Plain have been cleared of trees. Tourism.

Geographic entities mentioned:
surface_form: hohe loog
instance_of: Mountain
countries: Germany
coordinates: lat: 49.3336
lon: 8.09667
surface_form: sommerberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.2994
lon: 8.35178
Taubenkopf (Haardt). The Taubenkopf is a hill, in the German state of Rhineland-Palatinate. It is part of the mountain chain of the Haardt in the Palatine Forest and lies in the municipal territory of Diedesfeld in the borough of Neustadt an der Weinstraße. Geography.

Geographic entities mentioned:
surface_form: taubenkopf (haardt)
instance_of: Mountain
countries: Germany
coordinates: lat: 49.3225
lon: 8.09
Taubenkopf (Haardt). The Taubenkopf is a hill, in the German state of Rhineland-Palatinate. It is part of the mountain chain of the Haardt in the Palatine Forest and lies in the municipal territory of Diedesfeld in the borough of Neustadt an der Weinstraße. Geography.

Geographic entities mentioned:
surface_form: taubenkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 49.3225
lon: 8.09
northeast of the summit of the Kalmit itself, the highest peak in the Palatine Forest region. Before storm damage and the subsequent removal of wood, the summit dome was in the shape of a dove's head (&quot;Taubenkopf&quot;). Following the deforestation there is a 270 degree outlook from west (into the Palatine Forest) through north (Hohe Loog) to east (Klausental, Sommerberg and the Rhine Plain).

Geographic entities mentioned:
surface_form: taubenkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 49.3225
lon: 8.09
The protected area. Adjacent to the site of community interest of Monte Morello, the protected natural area of local interest (ANPIL) of Terzolle was proposed in 2004, on an area of 1,927 hectares in the municipalities of Florence, Vaglia and Sesto Fiorentino, on the east side of Monte Morello at about 500 m a.s.l.

Geographic entities mentioned:
surface_form: Monte Morello
instance_of: Mountain
countries: Italy
coordinates: lat: 43.8822
lon: 11.2314
surface_form: Monte Morello
instance_of: Mountain
countries: Italy
coordinates: lat: 43.8822
lon: 11.2314
Mount Yoshino. is the general name for the mountain ridge that stretches from the south bank of the Yoshino River in the town of Yoshino central Nara Prefecture, Japan, to the Ōmine Mountains, stretching for about eight kilometers from north-to-south, or the broader name of the area dotted with shrines and temples, centered around Kinpusen-ji Temple.

Geographic entities mentioned:
surface_form: Ōmine Mountains
instance_of: Mountain
countries: Japan
coordinates: lat: 34.252777777778
lon: 135.94055555556
Mount Yoshino. is the general name for the mountain ridge that stretches from the south bank of the Yoshino River in the town of Yoshino central Nara Prefecture, Japan, to the Ōmine Mountains, stretching for about eight kilometers from north-to-south, or the broader name of the area dotted with shrines and temples, centered around Kinpusen-ji Temple.

Geographic entities mentioned:
surface_form: mount yoshino
instance_of: Mountain
countries: Japan
coordinates: lat: 34.356433333333
lon: 135.87061666667
It was designated a National Place of Scenic Beauty and National Historic Site in 1924 and became part of Yoshino-Kumano National Park in 1936. In 2004, Mount Yoshino was designated as part of a UNESCO World Heritage Site under the name &quot;Sacred Sites and Pilgrimage Routes in the Kii Mountain Range&quot;. In 1990, it was selected as one of Japan's 100 Best Cherry Blossom Spots.

Geographic entities mentioned:
surface_form: mount yoshino
instance_of: Mountain
countries: Japan
coordinates: lat: 34.356433333333
lon: 135.87061666667
In 2004, Mount Yoshino was designated as part of a UNESCO World Heritage Site under the name &quot;Sacred Sites and Pilgrimage Routes in the Kii Mountain Range&quot;. In 1990, it was selected as one of Japan's 100 Best Cherry Blossom Spots. Mount Yoshino and Cherry Blossoms. Mount Yoshino has been planted with cherry blossoms since the Heian period.

Geographic entities mentioned:
surface_form: mount yoshino
instance_of: Mountain
countries: Japan
coordinates: lat: 34.356433333333
lon: 135.87061666667
Yoshino is also the subject of several poems in the &quot;Ogura Hyakunin Isshu&quot;. The 12th century CE Japanese Buddhist poet Saigyō writes of Mount Yoshino's cherry blossoms. During this period, the extent of the cherry forests was much greater, and large portions have been replaced by more economically valuable Hinoki cypress or Cryptomeria forests before and during World War II.

Geographic entities mentioned:
surface_form: mount yoshino
instance_of: Mountain
countries: Japan
coordinates: lat: 34.356433333333
lon: 135.87061666667
In the 21st century, efforts have been made to restore the cherry forests to their former extent. The reason why such a large number of cherry tree exist on Mount Yoshino is subject to controversy, but a prevalent belief is that the cherry tree is the sacred tree of Zao Gongen, the central deity of Shugendo, a mountain cult centered in this area.

Geographic entities mentioned:
surface_form: mount yoshino
instance_of: Mountain
countries: Japan
coordinates: lat: 34.356433333333
lon: 135.87061666667
Mount Yoshino as a sacred mountain. Several important religious and pilgrimage destinations are located around Mount Yoshino, including Yoshino Mikumari Shrine, Kimpu Shrine and Kimpusen-ji. The Ōmine Okugakemichi trail was established by the 7th century ascetic En no Gyōja. It connects Kimpusen-ji in Yoshino district, Nara Prefecture with the Kumano Sanzan in southern Wakayama Prefecture.

Geographic entities mentioned:
surface_form: mount yoshino
instance_of: Mountain
countries: Japan
coordinates: lat: 34.356433333333
lon: 135.87061666667
It has about 1,600 inhabitants. Geography. Nedakonice is located about southwest of Uherské Hradiště and southwest of Zlín. It lies in the Lower Morava Valley. The municipality is situated on the right bank of the Morava River, which forms the eastern municipal border. The stream Dlouhá řeka flows through the village. History. The first written mention of Nedakonice is from 1220.

Geographic entities mentioned:
surface_form: Lower Morava Valley
instance_of: Valley
countries: Czech Republic
coordinates: lat: 48.9430014
lon: 17.3295197
Beulah, Alabama. Beulah is an unincorporated community in the northeast corner of Lee County, Alabama, United States, just south of Valley. It is part of the Columbus, Georgia-Alabama Metropolitan Area. It is bounded by Chambers County on the north, the Chattahoochee River on the east, and the Halawaka Embayment of Lake Harding on the south. History.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Allana Beltran. Allana Beltran is an Australian performance artist and environmental activist. She is known as the &quot;Weld Angel&quot; for her protests on behalf of old growth forest in the Weld Valley. Early life. Beltran grew up on the Central Coast of New South Wales and completed her degree in Contemporary Fine Art at Sydney College of the Arts.

Geographic entities mentioned:
surface_form: Weld Valley
instance_of: Valley
countries: Australia
coordinates: lat: -42.95
lon: 146.6
Weld Angel incident. In November 2006, Beltran participated in a long-term protest against logging of old growth forest in the Weld Valley Activists had for some time accused Forestry Tasmania of allowing illegal logging practices to occur in World Heritage-valued forests. By March, most of her fellow protesters had been arrested.

Geographic entities mentioned:
surface_form: Weld Valley
instance_of: Valley
countries: Australia
coordinates: lat: -42.95
lon: 146.6