Sarmila/GeoWiki-Features huggingface dataset:
Watershed. The Sheldrake River drains a watershed whose upstream portions cover parts of Scarsdale and New Rochelle. The river supplies both Sheldrake Lake, and the smaller Goodliffe Pond to its east. It then flows under Weaver Street, and through Mamaroneck Town before ultimately joining the larger Mamaroneck River which empties into Mamaroneck Harbor and Long Island Sound. Conservancy.

Geographic entities mentioned:
surface_form: sheldrake lake
instance_of: Lake
countries: United States
coordinates: lat: 40.9524277
lon: -73.7744633
Watershed. The Sheldrake River drains a watershed whose upstream portions cover parts of Scarsdale and New Rochelle. The river supplies both Sheldrake Lake, and the smaller Goodliffe Pond to its east. It then flows under Weaver Street, and through Mamaroneck Town before ultimately joining the larger Mamaroneck River which empties into Mamaroneck Harbor and Long Island Sound. Conservancy.

Geographic entities mentioned:
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
About to the south, beyond the A55 road lie the villages of Caergeiliog and Llanfihangel yn Nhowyn. The Valley Wetlands, an area of lakes and marshes and a RSPB bird sanctuary, lie between these two villages. Bodedern is the closest village to the island's largest natural lake, Llyn Llywenan, which lies to the north. Education.

Geographic entities mentioned:
surface_form: Llyn Llywenan
instance_of: Lake
countries: United Kingdom
coordinates: lat: 53.305555555556
lon: -4.4805555555556
Nearby communities are Gooderham, Irondale, and Kinmount; Haliburton is a 25–35 minute drive away. The primary inflow, at the southwest, is Salerno Creek from White Lake. The primary outflow, at the northwest, is also Salerno Creek, which flows over a dam to the Irondale River, then via the Burnt River, the Kawartha Lakes, the Otonabee River and the Trent River to Lake Ontario. History.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
surface_form: kawartha lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 44.4994
lon: -78.441
Salerno Lake. Salerno Lake, formerly Devil's Lake, is a lake in the municipalities of Highlands East and Minden Hills in Haliburton County in Central Ontario, Canada. The lake is part of the Kawartha Lakes, and lies in the Great Lakes Basin. It is part of cottage country approximately a -hour drive away from Toronto. Geography. Salerno Lake is about long.

Geographic entities mentioned:
surface_form: kawartha
instance_of: Group of lakes
countries: Canada
coordinates: lat: 44.4994
lon: -78.441
It is part of cottage country approximately a -hour drive away from Toronto. Geography. Salerno Lake is about long. It is a narrow lake, at most, that resembles a large river. The lake is in a big valley, and the water depth increases quickly. Most places in the lake are about deep, but there are two spots where it can get as deep as.

Geographic entities mentioned:
surface_form: narrow lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.6194
lon: -113.616
Nearby communities are Gooderham, Irondale, and Kinmount; Haliburton is a 25–35 minute drive away. The primary inflow, at the southwest, is Salerno Creek from White Lake. The primary outflow, at the northwest, is also Salerno Creek, which flows over a dam to the Irondale River, then via the Burnt River, the Kawartha Lakes, the Otonabee River and the Trent River to Lake Ontario. History.

Geographic entities mentioned:
surface_form: white lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.31
lon: -76.52
surface_form: white lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.819166
lon: -72.271666
Salerno Lake. Salerno Lake, formerly Devil's Lake, is a lake in the municipalities of Highlands East and Minden Hills in Haliburton County in Central Ontario, Canada. The lake is part of the Kawartha Lakes, and lies in the Great Lakes Basin. It is part of cottage country approximately a -hour drive away from Toronto. Geography. Salerno Lake is about long.

Geographic entities mentioned:
surface_form: salerno lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.8569
lon: -78.4833
The lake is part of the Kawartha Lakes, and lies in the Great Lakes Basin. It is part of cottage country approximately a -hour drive away from Toronto. Geography. Salerno Lake is about long. It is a narrow lake, at most, that resembles a large river. The lake is in a big valley, and the water depth increases quickly.

Geographic entities mentioned:
surface_form: salerno lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.8569
lon: -78.4833
Yosemite. At the age of 20, Tresidder took a trip with his sister to Southern California, but due to washed-out railroad tracks, they ended up visiting Yosemite Valley instead. During his time there, he had the opportunity to meet several faculty members from Stanford University, who convinced him to enroll at the university.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
Tresidder spent his summers working in Yosemite, taking on various jobs such as a porter, among others. However, he was briefly fired for taking his future wife rock climbing on the backside of Half Dome. Tresidder and Mary Curry got married on June 17, 1920. After graduating from Stanford, Tresidder became the president of Yosemite Park and Curry Company.

Geographic entities mentioned:
surface_form: Half Dome
instance_of: Mountain
countries: United States
coordinates: lat: 37.746
lon: -119.53316666667
Kuusvesi. Kuusvesi is a medium-sized lake of Central Finland, in Laukaa Municipality. It belongs to the Kymijoki main catchment area. The inflow to the lake Kuusvesi is Simunankoski rapids and the outflow is Tarvaalanvirta rapids, which are protected by the rapid protection program of Finland.

Geographic entities mentioned:
surface_form: kuusvesi
instance_of: Lake
countries: Finland
coordinates: lat: 62.41666667
lon: 26.06666667
The Monaro Highway defines the park's western boundary. Within the confines of the park, the Genoa River flows eastwards to the Tasman Sea. The highest peaks in the park are Mount Coopracambra, with an elevation of above sea level; Mount Kaye, with an elevation of, and Mount Denmarsh, with an elevation of.

Geographic entities mentioned:
surface_form: Mount Kaye
instance_of: Mountain
countries: Australia
coordinates: lat: -37.3944
lon: 149.247
They hoped to be free of American settlers, only to find colonists moving there as well, so they did not stay long. In late 1789 or early 1790, Tecumseh traveled south with Cheeseekau to live with the Chickamauga Cherokees near Lookout Mountain in what is now Tennessee. Some Shawnees already lived among the Chickamaugas, who were fierce opponents of U.S. expansion.

Geographic entities mentioned:
surface_form: Lookout Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.863713888889
lon: -85.392452777778
Pocksha Pond. Pocksha Pond is a lake/reservoir/pond within the towns of Lakeville and Middleboro, in southeastern Massachusetts. It shares its waters with Great Quittacas Pond and openly connected with Assawompset Pond. These lakes provides a source of drinking water to the city of New Bedford, the largest city in southeastern Massachusetts. Wildlife.

Geographic entities mentioned:
surface_form: Assawompset Pond
instance_of: Lake
countries: United States
coordinates: lat: 41.840277777778
lon: -70.919444444444
Pocksha Pond. Pocksha Pond is a lake/reservoir/pond within the towns of Lakeville and Middleboro, in southeastern Massachusetts. It shares its waters with Great Quittacas Pond and openly connected with Assawompset Pond. These lakes provides a source of drinking water to the city of New Bedford, the largest city in southeastern Massachusetts. Wildlife.

Geographic entities mentioned:
surface_form: pocksha pond
instance_of: Lake
countries: United States
coordinates: lat: 41.827777777778
lon: -70.894444444444
He retired in 1966, subsequently working for the Decca company. Honours. Irving was president of the Institute of Navigation from 1964 to 1967. He was president of the Royal Geographical Society (1969–71) and received their Patron's Medal in 1976. Mount Irving in the South Shetland Islands was named in his honour.

Geographic entities mentioned:
surface_form: Mount Irving
instance_of: Mountain
coordinates: lat: -61.283333333333
lon: -54.133333333333
Sir George Williams University in Montreal, which was founded by YMCA, was named in commemoration of Williams; it was later merged into Concordia University, with its former campus retaining the name Sir George Williams Campus. George Williams College, located on the shores of Geneva Lake in Wisconsin, USA, is a satellite of Aurora University, and is also named after Williams.

Geographic entities mentioned:
surface_form: Geneva Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.59
lon: -88.435
Some weak tornadoes, known as landspouts, have been shown to develop in a similar manner. More than one waterspout can occur simultaneously in the same vicinity. In 2012, as many as nine simultaneous waterspouts were reported on Lake Michigan in the United States. In May 2021, at least five simultaneous waterspouts were filmed near Taree, off the northern coast of New South Wales, Australia.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Laguna Miscanti. Laguna Miscanti is a brackish water lake located in the altiplano of the Antofagasta Region in northern Chile. Cerro Miñiques volcano and Cerro Miscanti tower over this lake. This large heart-shaped lake has a deep blue colour and developed in a basin formed by a fault.

Geographic entities mentioned:
surface_form: altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
surface_form: laguna miscanti
instance_of: Lake
countries: Chile
coordinates: lat: -23.725
lon: -67.765
Laguna Miscanti. Laguna Miscanti is a brackish water lake located in the altiplano of the Antofagasta Region in northern Chile. Cerro Miñiques volcano and Cerro Miscanti tower over this lake. This large heart-shaped lake has a deep blue colour and developed in a basin formed by a fault.

Geographic entities mentioned:
surface_form: Cerro Miscanti
instance_of: Mountain
countries: Chile
coordinates: lat: -23.67361111111111
lon: -67.7161111111111
Cerro Miñiques volcano and Cerro Miscanti tower over this lake. This large heart-shaped lake has a deep blue colour and developed in a basin formed by a fault. South of Miscanti lies Laguna Miñiques, another lake which is separated from Miscanti by a lava flow that was emplaced there during the Pleistocene. The lake is part of one of the seven sectors of Los Flamencos National Reserve.

Geographic entities mentioned:
surface_form: Laguna Miñiques
instance_of: Lake
countries: Chile
coordinates: lat: -23.765
lon: -67.7925
The lake is part of one of the seven sectors of Los Flamencos National Reserve. A number of birds and mammals live at the lake, which is a major tourist destination. Geography. Laguna Miscanti lies in the Central Andes of Chile, east-southeast of the Salar de Atacama. Administratively, it is part of the Antofagasta Region. The closest town is Socaire, away from the lake.

Geographic entities mentioned:
surface_form: Salar de Atacama
instance_of: Lake
Body of water
countries: Chile
coordinates: lat: -23.416666666666668
lon: -68.26666666666667
surface_form: laguna miscanti
instance_of: Lake
countries: Chile
coordinates: lat: -23.725
lon: -67.765
The inhabitants of Socaire used the area for grazing, and it bears spiritual and religious importance for them. In 2002, there were 5,000 tourists at Miscanti and the nearby lake Miñiques, and in 2015, one in three tourists who went to the Los Flamencos National Reserve visited Miscanti and Laguna Miñiques.

Geographic entities mentioned:
surface_form: Miñiques
instance_of: Lake
countries: Chile
coordinates: lat: -23.765
lon: -67.7925
A lava flow separates the otherwise flat lake floor into two basins. In the Atacama Altiplano, Laguna Miscanti is among the biggest waterbodies. The mountains Cerro Miscanti () and Cerro Miñiques () lie northeast and south of the lake, respectively. south of the lake is another waterbody, Laguna Miñiques.

Geographic entities mentioned:
surface_form: Cerro Miscanti
instance_of: Mountain
countries: Chile
coordinates: lat: -23.67361111111111
lon: -67.7161111111111
Miscanti and Miñiques occupy fault-bound basins; the Quebrada Nacimiento fault is also known as the Miscanti Fault and is part of a detachment fault system east of the Salar de Atacama, which separates the Western Cordillera from the Cordillera Domeyko.

Geographic entities mentioned:
surface_form: Salar de Atacama
instance_of: Lake
Body of water
countries: Chile
coordinates: lat: -23.416666666666668
lon: -68.26666666666667
This fault extends from the Purico complex, Llano de Chajnantor to Miñiques and has formed a ridge, which has dammed lava flows from Cerro Miscanti and Cerro Miñiques. The basins developed during the Pliocene and Pleistocene; Laguna Lejia also developed along this fault and the fault segment there is also known as Miscanti-Callejon de Varela fault.

Geographic entities mentioned:
surface_form: Purico complex
instance_of: Mountain
countries: Chile
coordinates: lat: -23
lon: -67.75
surface_form: purico
instance_of: Mountain
countries: Chile
coordinates: lat: -23
lon: -67.75
In the late Pleistocene and early Holocene the climate was much wetter and lakes expanded, especially during the first stage of the Central Andean Pluvial Event. The late Pleistocene—early Holocene wet period was particularly noticeable in the Altiplano, where two separate phases of the Lake Tauca occurred.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
surface_form: Lake Tauca
instance_of: Lake
countries: Peru
coordinates: lat: -20
lon: -68
Laguna Miscanti. Laguna Miscanti is a brackish water lake located in the altiplano of the Antofagasta Region in northern Chile. Cerro Miñiques volcano and Cerro Miscanti tower over this lake. This large heart-shaped lake has a deep blue colour and developed in a basin formed by a fault.

Geographic entities mentioned:
surface_form: laguna miscanti
instance_of: Lake
countries: Chile
coordinates: lat: -23.725
lon: -67.765
A lava flow separates the otherwise flat lake floor into two basins. In the Atacama Altiplano, Laguna Miscanti is among the biggest waterbodies. The mountains Cerro Miscanti () and Cerro Miñiques () lie northeast and south of the lake, respectively. south of the lake is another waterbody, Laguna Miñiques.

Geographic entities mentioned:
surface_form: laguna miscanti
instance_of: Lake
countries: Chile
coordinates: lat: -23.725
lon: -67.765
The separation of the lakes probably occurred during the Pleistocene, when a lava flow erupted from Cerro Miñiques split the lake basin in two. A number of creeks enter into Laguna Miscanti from the north, east and south (Quebrada de Chaquisoqui), and there are two springs on its northern shores.

Geographic entities mentioned:
surface_form: laguna miscanti
instance_of: Lake
countries: Chile
coordinates: lat: -23.725
lon: -67.765
The Cordon de Puntas Negras is the principal source of water. Water reaches Laguna Miscanti principally as groundwater, which is directed there by the fault; this may explain why Laguna Miscanti is a permanent lake rather than a playa. The lake has no surface outflow.

Geographic entities mentioned:
surface_form: laguna miscanti
instance_of: Lake
countries: Chile
coordinates: lat: -23.725
lon: -67.765
surface_form: laguna miscanti
instance_of: Lake
countries: Chile
coordinates: lat: -23.725
lon: -67.765
The lake has no surface outflow. Presently, water seeps to Miñiques through a lava flow along the path of the Quebrada Nacimiento fault; during former lake highstands a combined lake overflowed into the Pampa Varela basin south-southwest of Miñiques. Most water, however, leaves Laguna Miscanti through evaporation. The town of Peine draws its water supply from the Miscanti basin. Climate.

Geographic entities mentioned:
surface_form: laguna miscanti
instance_of: Lake
countries: Chile
coordinates: lat: -23.725
lon: -67.765
Fishermans Bay, New South Wales. Fishermans Bay is a small suburb of the Port Stephens local government area in the Hunter Region of New South Wales, Australia. It is located on the coast of the Tasman Sea adjacent to Anna Bay. A large part of the eastern portion of the suburb is occupied by Tomaree National Park and only a very small portion of the south western corner of the suburb is populated.

Geographic entities mentioned:
surface_form: Hunter Region
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Gowlett Peaks. The Gowlett Peaks () are a small group of isolated peaks, consisting of tall, sharp twin peaks and two close outliers, about northeast of the Anare Nunataks in Mac. Robertson Land, Antarctica.

Geographic entities mentioned:
surface_form: Anare Nunataks
instance_of: Mountain
coordinates: lat: -69.9667
lon: 64.6167
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: twin peaks
instance_of: Mountain
coordinates: lat: -63.4
lon: -57.1167
surface_form: gowlett peaks
instance_of: Mountain
coordinates: lat: -69.8833
lon: 64.9167
Robertson Land, Antarctica. They were sighted in November 1955 by an Australian National Antarctic Research Expeditions party led by John Béchervaise, and were named by the Antarctic Names Committee of Australia for Alan Gowlett, an engineer at Mawson Station in 1955.

Geographic entities mentioned:
surface_form: béchervaise
instance_of: Mountain
coordinates: lat: -70.1833
lon: 64.8
Gowlett Peaks. The Gowlett Peaks () are a small group of isolated peaks, consisting of tall, sharp twin peaks and two close outliers, about northeast of the Anare Nunataks in Mac. Robertson Land, Antarctica.

Geographic entities mentioned:
surface_form: gowlett peaks
instance_of: Mountain
coordinates: lat: -69.8833
lon: 64.9167
The interior is relatively featureless with a small floor, with mounds of material deposited along the edges of the sloping inner walls. To the north of the crater, along the edge of the highland peninsula between the two maria is a domed mountainous rise that is designated Mons Gruithuisen Gamma (γ). Just to the east of this feature is another mountainous rise named Mons Gruithuisen Delta (δ).

Geographic entities mentioned:
surface_form: Mons Gruithuisen Gamma
instance_of: Mountain
coordinates: lat: 36.56
lon: -40.72
The interior is relatively featureless with a small floor, with mounds of material deposited along the edges of the sloping inner walls. To the north of the crater, along the edge of the highland peninsula between the two maria is a domed mountainous rise that is designated Mons Gruithuisen Gamma (γ). Just to the east of this feature is another mountainous rise named Mons Gruithuisen Delta (δ).

Geographic entities mentioned:
surface_form: Mons Gruithuisen Delta
instance_of: Mountain
coordinates: lat: 36.07
lon: -39.59
Connections. The station is served by Antelope Valley Transit Authority route 790, the North County TRANSporter. The route allows Metrolink passengers on mid-day trains (that only go as far as Newhall station in the Santa Clarita Valley) to travel to the Palmdale station. Vincent Grade/Acton station is only served in the northbound direction, by request from passengers onboard the bus.

Geographic entities mentioned:
surface_form: Santa Clarita Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.398
lon: -118.522
Its current name comes from Ruesi Vasuthep, who practiced asceticism on this mountain over a thousand years ago. Geography. The Doi Suthep - Doi Pui mountain is part of the Thanon Thong Chai Range, the southernmost subrange of the Shan Highland system. Other high peaks of the same range are Doi Luang Chiang Dao (), Doi Pui (), and Doi Inthanon, the highest point in Thailand, at.

Geographic entities mentioned:
surface_form: Doi Inthanon
instance_of: Mountain
countries: Thailand
coordinates: lat: 18.592222222222
lon: 98.486666666667
surface_form: doi luang chiang dao
instance_of: Mountain
countries: Thailand
coordinates: lat: 19.39972222
lon: 98.87666667
Doi Suthep. Doi Suthep (ดอยสุเทพ), is a mountain (&quot;doi&quot;) west of Chiang Mai, Thailand. It is in elevation and is one of the twin peaks of a granite mountain. The other peak is known as Doi Pui and is slightly higher (). Doi Suthep is from Chiang Mai city center. The vegetation below is mostly deciduous forest, with evergreen forest above this elevation.

Geographic entities mentioned:
surface_form: ดอยสุเทพ
instance_of: Mountain
countries: Thailand
coordinates: lat: 18.816388888889
lon: 98.893055555556
surface_form: doi suthep
instance_of: Mountain
countries: Thailand
coordinates: lat: 18.816388888889
lon: 98.893055555556
Doi Suthep. Doi Suthep (ดอยสุเทพ), is a mountain (&quot;doi&quot;) west of Chiang Mai, Thailand. It is in elevation and is one of the twin peaks of a granite mountain. The other peak is known as Doi Pui and is slightly higher (). Doi Suthep is from Chiang Mai city center. The vegetation below is mostly deciduous forest, with evergreen forest above this elevation.

Geographic entities mentioned:
surface_form: doi suthep
instance_of: Mountain
countries: Thailand
coordinates: lat: 18.816388888889
lon: 98.893055555556
Doi Suthep is from Chiang Mai city center. The vegetation below is mostly deciduous forest, with evergreen forest above this elevation. Originally, before the Doi Suthep forest was declared a national park, a royal decree in 1949 designated it as a protected forest. Name. Doi Suthep has other names in legend, such as Ucchugiri, Doi Aoi Chang, or Doi Gala.

Geographic entities mentioned:
surface_form: doi suthep
instance_of: Mountain
countries: Thailand
coordinates: lat: 18.816388888889
lon: 98.893055555556
surface_form: doi suthep
instance_of: Mountain
countries: Thailand
coordinates: lat: 18.816388888889
lon: 98.893055555556
Other high peaks of the same range are Doi Luang Chiang Dao (), Doi Pui (), and Doi Inthanon, the highest point in Thailand, at. Creeks flowing eastward down from Doi Suthep include Huai Kaew (ห้วยแก้ว), Huai Kok Ma (ห้วยคอกม้า), Huai Pha Lat (ห้วยผาลาด), Huai Mae Nai (ห้วยแม่ใน), and others. The creeks all flow into the Ping River. Geology.

Geographic entities mentioned:
surface_form: doi suthep
instance_of: Mountain
countries: Thailand
coordinates: lat: 18.816388888889
lon: 98.893055555556
Mid-Ordovician shale, 475 million years old, is located south of the peak in the southern part of the national park. Temple. The temple Wat Phra That Doi Suthep is on top of a hill (around) partway up Doi Suthep. This Buddhist place of worship dates back to the 14th century. It is an important venue for the devout and a legend featuring a white elephant is connected to this revered site.

Geographic entities mentioned:
surface_form: doi suthep
instance_of: Mountain
countries: Thailand
coordinates: lat: 18.816388888889
lon: 98.893055555556
surface_form: doi suthep
instance_of: Mountain
countries: Thailand
coordinates: lat: 18.816388888889
lon: 98.893055555556
There are views of Chiang Mai city and its surroundings from the top of this mountain. On the slopes of Doi Suthep, above Chiang Mai, lies a temple called Wat Pha Lat. Founded by King Kuena of Lanna in the 14th century, Wat Pha Lat originally served as a resting place for pilgrims journeying up to Wat Phra That Doi Suthep
National park. This mountain is part of the Doi Suthep-Pui National Park.

Geographic entities mentioned:
surface_form: doi suthep
instance_of: Mountain
countries: Thailand
coordinates: lat: 18.816388888889
lon: 98.893055555556
Founded by King Kuena of Lanna in the 14th century, Wat Pha Lat originally served as a resting place for pilgrims journeying up to Wat Phra That Doi Suthep
National park. This mountain is part of the Doi Suthep-Pui National Park. The park was established in 1981 and has an area of that includes the Wat Phrathat Doi Suthep temple as well as Bhubing Rjanives Palace, further up the mountain.

Geographic entities mentioned:
surface_form: doi suthep
instance_of: Mountain
countries: Thailand
coordinates: lat: 18.816388888889
lon: 98.893055555556
This mountain is part of the Doi Suthep-Pui National Park. The park was established in 1981 and has an area of that includes the Wat Phrathat Doi Suthep temple as well as Bhubing Rjanives Palace, further up the mountain. Doi Pui, the other peak of the massif, is close by via a paved road as well as through forest paths. Hmong hill tribe people live in the surrounding area. Environment.

Geographic entities mentioned:
surface_form: doi suthep
instance_of: Mountain
countries: Thailand
coordinates: lat: 18.816388888889
lon: 98.893055555556
Environment. The chief of Doi Suthep-Pui National Park voiced his concerns in 2018 about the increasing amount of garbage produced by the large number of tourists visiting Doi Suthep temple, a must-see site for Chiang Mai tourists. Untreated water and garbage from more than 300 shops and a large number of tourists is damaging the area's natural environment.

Geographic entities mentioned:
surface_form: doi suthep
instance_of: Mountain
countries: Thailand
coordinates: lat: 18.816388888889
lon: 98.893055555556
surface_form: doi suthep
instance_of: Mountain
countries: Thailand
coordinates: lat: 18.816388888889
lon: 98.893055555556
Untreated water and garbage from more than 300 shops and a large number of tourists is damaging the area's natural environment. Untreated waste water flows directly into the Huai Rap Sadet Waterfall. The annual Visakha Bucha pilgrimage up Doi Suthep leaves more than 30 tonnes of garbage in its wake. Housing Project.

Geographic entities mentioned:
surface_form: doi suthep
instance_of: Mountain
countries: Thailand
coordinates: lat: 18.816388888889
lon: 98.893055555556
Greater Sudbury (Ontario, Canada) is considered a city of lakes containing 330 lakes, and the largest lake contained within a city, Lake Wanapitei with 13,257 hectares. The lakes drain into two main watersheds: to the east is the French River watershed which flows into Lake Huron via Georgian Bay, and to the west is the Spanish River watershed which flows into Lake Huron via the North Channel.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
In his free time he visited museums in Minneapolis, Chicago, Boston, and New York. Tsutakawa also visited friends and family in the internment camps. During a visit to the Tule Lake camp in California he met and fell in love with Ayame Iwasa, a friend of his sister Sadako. Although she was ten years younger than he, she was, like Tsutakawa, a Nisei who had been educated in Japan.

Geographic entities mentioned:
surface_form: Tule Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.909322222222
lon: -121.53304722222
In 1977 he traveled to Nepal, where he at last saw in person the stacked rocks of the obos whose forms had for so long influenced his work. He later described seeing more than twenty such piles against a backdrop of Mount Everest as the most exciting experience of his life. After an earlier heart attack left him weakened, Tsutakawa died at his home in Seattle on December 18, 1997.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Paul. In August 1927, world-renowned aviator Charles Lindbergh visited the Milwaukee airport. Kohler Aviation Corporation began providing passenger service across Lake Michigan on August 31, 1929. During the late depression years (1938–July 1940), a new two-story passenger terminal building was constructed by the Works Progress Administration.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Level Mountain. Level Mountain is a large volcanic complex in the Northern Interior of British Columbia, Canada. It is located north-northwest of Telegraph Creek and west of Dease Lake on the Nahlin Plateau. With a maximum elevation of, it is the second-highest of four large complexes in an extensive north–south trending volcanic region.

Geographic entities mentioned:
surface_form: Nahlin Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.44972222222222
lon: -131.41833333333332
It is located north-northwest of Telegraph Creek and west of Dease Lake on the Nahlin Plateau. With a maximum elevation of, it is the second-highest of four large complexes in an extensive north–south trending volcanic region. Much of the mountain is gently sloping; when measured from its base, Level Mountain is about tall, slightly taller than its neighbour to the northwest, Heart Peaks.

Geographic entities mentioned:
surface_form: Heart Peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
These valleys serve as a radial drainage for several small streams that flow from the mountain. Meszah Peak is the only named peak in the Level Mountain Range. The mountain began forming about 15 million years ago and has experienced volcanism up until geologically recent times. There have been four stages of activity throughout the long volcanic history of Level Mountain.

Geographic entities mentioned:
surface_form: Meszah Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 58.4786
lon: -131.437
Because of its great extent Level Mountain can be seen from outer space. This, coupled with snow and elevation, helps define the geology of the region. Level Mountain dominates the Nahlin Plateau, a subdivision of the larger Stikine Plateau. Level Mountain comprises two principal components: a voluminous basal shield volcano and an overlying eroded stratovolcano.

Geographic entities mentioned:
surface_form: Stikine Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
The south and west sides of the plateau are marked by a well-defined, but dissected escarpment. In contrast, the north and east plateau boundaries are less clear. V-shaped stream canyons occur along the lava plateau margin, exposing a section of Tertiary basalts along the Grand Canyon of the Stikine. From an elevation of onwards the overlying stratovolcano is dominant.

Geographic entities mentioned:
surface_form: Grand Canyon of the Stikine
instance_of: Valley
countries: Canada
coordinates: lat: 58.08222222222222
lon: -130.735
Ridges and peaks prevail at an elevation of and comprise the Level Mountain Range. These rise more steeply to, eventually reaching the highest point of at Meszah Peak. Therefore, when viewed from a distance, Level Mountain appears unusually flat except for a number of black peaks on its summit which have the appearance of enormous volcanic cones. Biogeography.

Geographic entities mentioned:
surface_form: Meszah Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 58.4786
lon: -131.437
Middle Creek, the fourth tributary, flows to the south near Beatty Creek. It contains one named tributary, Riley Creek, which flows to the southwest. The fifth named Tahltan River tributary draining the southern side of Level Mountain is Hartz Creek which flows to the south. To the east, the Tuya River gathers two named tributaries draining the eastern side of Level Mountain.

Geographic entities mentioned:
surface_form: Hartz Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.04966
lon: -131.00386
The first tributary is the Little Tuya River which flows to the southeast. It contains one named tributary, Mansfield Creek, which flows to the east. The second named Tuya River tributary draining the eastern side of Level Mountain is Classy Creek which flows to the southeast. The northern and western sides of Level Mountain are drained by streams within the Nahlin River watershed.

Geographic entities mentioned:
surface_form: Classy Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.19962
lon: -130.7871
The second named Tuya River tributary draining the eastern side of Level Mountain is Classy Creek which flows to the southeast. The northern and western sides of Level Mountain are drained by streams within the Nahlin River watershed. To the west, the Dudidontu River flows to the northwest and gathers one named tributary draining the western side of Level Mountain.

Geographic entities mentioned:
surface_form: Dudidontu River
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.78281
lon: -131.98693
To the west, the Dudidontu River flows to the northwest and gathers one named tributary draining the western side of Level Mountain. This tributary, Kakuchuya Creek, flows to the north and gathers Matsatu Creek which flows to the northwest from the western side of Level Mountain where it has cut a large steep-sided gorge into the western escarpment.

Geographic entities mentioned:
surface_form: Kakuchuya Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.58283
lon: -131.78695
surface_form: Matsatu Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.58283
lon: -131.77035
This tributary, Kakuchuya Creek, flows to the north and gathers Matsatu Creek which flows to the northwest from the western side of Level Mountain where it has cut a large steep-sided gorge into the western escarpment. The Koshin River flows to the north from the western side of Level Mountain and gathers two named tributaries.

Geographic entities mentioned:
surface_form: Koshin River
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.86621
lon: -131.80364
The Koshin River flows to the north from the western side of Level Mountain and gathers two named tributaries. These two tributaries, Lost Creek and Kaha Creek, also drain the western side of Level Mountain and flow to the northwest and west, respectively. The only named stream draining the northern side of Level Mountain is Megatushon Creek which flows to the north.

Geographic entities mentioned:
surface_form: Kaha Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.68283
lon: -131.68693
These two tributaries, Lost Creek and Kaha Creek, also drain the western side of Level Mountain and flow to the northwest and west, respectively. The only named stream draining the northern side of Level Mountain is Megatushon Creek which flows to the north. The southwestern side of Level Mountain is drained by streams within the Sheslay River watershed.

Geographic entities mentioned:
surface_form: Megatushon Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.59934
lon: -131.08793
The only named stream draining the northern side of Level Mountain is Megatushon Creek which flows to the north. The southwestern side of Level Mountain is drained by streams within the Sheslay River watershed. Egnell Creek is the only named stream in this watershed draining Level Mountain. It flows southwest into the mouth of the Hackett River just above the junction with the Shesley River.

Geographic entities mentioned:
surface_form: Egnell Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.26629
lon: -131.80375
Snow avalanches are limited only to the Level Mountain Range and the steepest slopes. Background. Level Mountain is part of the Northern Cordilleran Volcanic Province (NCVP), a broad area of shield volcanoes, lava domes, cinder cones and stratovolcanoes extending from northwestern British Columbia northwards through Yukon into easternmost Alaska.

Geographic entities mentioned:
surface_form: Northern Cordilleran Volcanic Province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
Level Mountain is part of a subdivision of the NCVP called the Stikine Subprovince. This subprovince, confined to the Stikine region of northwestern British Columbia, consists of three other volcanic complexes: Heart Peaks, Hoodoo Mountain and Mount Edziza. The four complexes differ petrologically and/or volumetrically from the rest of the NCVP.

Geographic entities mentioned:
surface_form: Hoodoo Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
It is possible that geothermal outputs at Level Mountain had an influence on dynamics of past ice sheets much like the modern Grímsvötn caldera is an important heat source beneath Vatnajökull in Iceland. However, like other large volcanic centres in the NCVP, much of Level Mountain was formed prior to glaciation.

Geographic entities mentioned:
surface_form: Grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
3, Upper Tahltan Indian Reserve No. 4 and Tahltan Forks Indian Reserve No. 5. The northwestern side of Level Mountain is home to the Callison Ranch, which lies just east of Hatin Lake. Southeast of Level Mountain is the Days Ranch near the junction of the Tahltan and Stikine rivers. It was established by Ira Day in or before 1929 as a stopping place on the road from Dease Lake to Telegraph Creek.

Geographic entities mentioned:
surface_form: Hatin Lake
instance_of: Lake
countries: Canada
coordinates: lat: 58.64944
lon: -131.72222
More definitive evidence as to their age was obtained by W. A. Johnston and F. A. Kerr of the Geological Survey of Canada who placed them in the Tertiary. Some of the most recent lava flows of the Stikine valley were assigned as probably belonging to the Pleistocene. Level Mountain was demonstrated in the 1920s as a possible source for the extensive lavas in the neighbouring Tuya volcanic field.

Geographic entities mentioned:
surface_form: Tuya volcanic field
instance_of: Mountain
countries: Canada
coordinates: lat: 59.2167
lon: -130.95
Puvirnituq. Puvirnituq () is a northern village (Inuit community) in Nunavik, on the Povungnituk River near its mouth on Hudson Bay in northern Quebec, Canada. Its population was 2,129 as of the 2021 Canadian census. Of all other northern villages in Nunavik (VN), only Puvirnituq has no Inuit reserved land (TI) of the same name associated with it.

Geographic entities mentioned:
surface_form: Povungnituk River
instance_of: Watercourse
countries: Canada
coordinates: lat: 60.06
lon: -77.22
At Anthela, Mount Oeta recedes a little from the sea, leaving a plain a little more than half a mile in breadth, but again contracts near Alpeni, the first town of the Locrians, where the space is again only sufficient for a single carriage. Modern scholars identify its location with the modern village of Anthili in the municipality of Lamia. Nomenclature.

Geographic entities mentioned:
surface_form: Mount Oeta
instance_of: Mountain
countries: Greece
coordinates: lat: 38.816666666667
lon: 22.283333333333
Dark River (New Zealand). The Dark River, New Zealand is a river of Fiordland, New Zealand. It rises west of Barrier Peak and flows westward through Fiordland National Park into Lake Grave, which drains into Sutherland Sound.

Geographic entities mentioned:
surface_form: Sutherland Sound
instance_of: Watercourse
countries: New Zealand
coordinates: lat: -44.73
lon: 167.57
Desert Valley League. The Desert Valley League is an American high school sports league primarily within the Coachella Valley of Riverside County, California, with some schools from surrounding areas. The league is affiliated with the CIF Southern Section.

Geographic entities mentioned:
surface_form: Coachella Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.72
lon: -116.2
Fornacher Redlbach. The Fornacher Redlbach is a river of Upper Austria. The Fornacher Redlbach has a length of approximately and a width of about. West of Vöcklamarkt it joins the Vöckla, which itself joins the Ager. The river is partly untreated, partly modulated with backwater area. Thanks to its excellent water quality it is rich in trout.

Geographic entities mentioned:
surface_form: redlbach
instance_of: Watercourse
countries: Austria
coordinates: lat: 48.083712
lon: 13.405307
surface_form: fornacher redlbach
instance_of: Watercourse
countries: Austria
coordinates: lat: 48.083712
lon: 13.405307
She taught fiction and poetry workshops, introductory and advanced (for upperclassmen and graduate students) as well as a course on fiction (lecture format, 45 students). In addition to writing, Alvarez holds the position of writer-in-residence at Middlebury College, where she teaches creative writing on a part-time basis. Alvarez currently resides in the Champlain Valley in Vermont.

Geographic entities mentioned:
surface_form: Champlain Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.45868
lon: -73.42617
Licking, Missouri. Licking is a city located in Texas County, Missouri, United States. The population was 3,124 at the 2010 census, making it the most populous city in Texas County. Geography. Licking is located in north central Texas County in the Ozarks of southern Missouri. The city is located at the intersection of U.S. Route 63 and Missouri Route 32.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
Sawmill Pass. Sawmill Pass, is a mountain pass in the southern Sierra Nevada, California on the border of the Inyo National Forest (John Muir Wilderness) to the east and Kings Canyon National Park to the west. The eastern approach via the Sawmill Pass Trail is steep and strenuous, climbing from the Owens Valley floor.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
Götzenstein. The Götzenstein is a hill in the Odenwald range in Hesse, Germany.

Geographic entities mentioned:
surface_form: götzenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 49.5531
lon: 8.7705
Plot. A young woman wanders barefoot in the lush Aokigahara (青木ヶ原), also known as the Sea of Trees (樹海 Jukai) region of Mount Fuji, and suddenly falls into a cavern, awakening in an icy cave full of large eggs. When one of the eggs start to hatch, she goes into hysterics and flees until she is discovered by a construction crew.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
Her story airs on a televised news report that is seen by geologist Takashi Ashizawa. Upon hearing about the fossilized egg, Takashi sets off to Mount Fuji to find it. When he arrives at the small village bordering Fuji's Saiko Lake, Takashi immediately heads into the heavily forested Jukai when a sudden earthquake occurs and he is knocked out.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
Production began in December 1975, the same month that &quot;Jaws&quot; was released nationwide in Japan. It also coincided with a resurgence of reports of Nessie in Loch Ness. With a view to the world market, the film was to include Mount Fuji (as a symbol of Japan) and the similar theme of a mysterious lake-dwelling monster.

Geographic entities mentioned:
surface_form: Loch Ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
It also coincided with a resurgence of reports of Nessie in Loch Ness. With a view to the world market, the film was to include Mount Fuji (as a symbol of Japan) and the similar theme of a mysterious lake-dwelling monster. The script incorporated other elements of Japanese culture such as dragon legends and myths.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
In the spring of 1976, an early title for the screenplay was “The Giant Monster Bird vs. The Giant Dragon God&quot; (大怪鳥対大竜神, Dai kaisho tai Dai ryujin).The final script was completed on September 3, 1976 with filming starting on October 12. Filming ended after six months, on March 21, 1977, between locations at Toei Studios and Mount Fuji.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
Yolanda González (artist). Yolanda González (born 1964) is a Chicana multimedia artist based in Los Angeles. She primarily works in ceramics, drawing, painting, and printmaking. Biography. Yolanda Gonzalez was born in 1964 in San Gabriel Valley after her parents came from Mexico. Gonzalez is one of five children. She is descended from a family of artists, whose early work can be dated to 1877.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
The Newars, lost to the Gorkhalis who were expanding their kingdom. Blockade. Kathmandu (alternative names: Yen Desa येँ देस, Kantipur) was one of the three capital cities in the Kathmandu Valley, the other two being Lalitpur and Bhaktapur. The kingdom of Kathmandu extended to a distance of 12–13 days journey north to the Tibetan border.

Geographic entities mentioned:
surface_form: Kathmandu Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
However, the local traders saw the British failure as a relief due to the detrimental effect of British on the trade of Bihar and Bengal. Thamel capture. King Prithvi Narayan Shah began to assure support to locals of the outer reaches of the Kathmandu valley. The local Newars of Kathmandu began to appreciate the liberal temperament and personality of Prithvi Narayan.

Geographic entities mentioned:
surface_form: Kathmandu valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
Tell Aswad is the oldest site of agriculture, with domesticated emmer wheat dated to 10,800 BP. Soon after came hulled, two-row barley – found domesticated earliest at Jericho in the Jordan valley and at Iraq ed-Dubb in Jordan. Other sites in the Levantine corridor that show early evidence of agriculture include Wadi Faynan 16 and Netiv Hagdud.

Geographic entities mentioned:
surface_form: Jordan valley
instance_of: Valley
countries: Jordan
Lebanon
Israel
Syria
State of Palestine
coordinates: lat: 32.317222222222
lon: 35.57
Career. Arpa worked in management at an Integration Service and the Wolfsburg State Welfare Association, before becoming managing director of the Lavanttal Women's Shelter in 2019. She also ran her own language learning company. Arpa has been involved in various committees of the Social Democratic Party of Austria.

Geographic entities mentioned:
surface_form: Lavanttal
instance_of: Valley
countries: Austria
coordinates: lat: 46.8333
lon: 14.8417
Such a border determination process was employed in the Carinthian Plebiscite to determine the Slovenian–Austrian border. Land dispute on Sveta Gera/Trdinov vrh. Sveta Gera (), the Gorjanci mountain range's highest peak, was disputed in the 1990s, but the issue is dormant. The summit is claimed by both Croatia and Slovenia and is recorded in the Croatian land registry.

Geographic entities mentioned:
surface_form: Sveta Gera
instance_of: Mountain
countries: Croatia
coordinates: lat: 45.75978333333333
lon: 15.318158333333333
In 1912, Mellon and Nora finally agreed on a divorce settlement, largely on Mellon's terms. Mellon did not remarry. Nora lived in Pittsburgh for several years before eventually settling in the Hudson Valley, and the two children alternated living with either parent. In 1923, Nora married Harvey Arthur Lee, a British-born antiques dealer 14 years her junior.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613