Sarmila/GeoWiki-Features huggingface dataset:
Red Mountain Town. Following sporadic settling of the region in the 1870s, a series of permanent mining towns were founded in what became known as the Red Mountain Mining District. Among these was Red Mountain Town, which was founded following discoveries of silver in 1882.

Geographic entities mentioned:
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.4867
lon: -86.8064
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.3918
lon: -121.145
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.60041
lon: -120.98678
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.5231
lon: -111.876
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.415277777778
lon: -121.46694444444
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.45588
lon: -121.3891607
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.064444444444
lon: -117.24638888889
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.2979
lon: -119.441
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.26751
lon: -74.54952
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.5356
lon: -113.424
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.1122
lon: -105.181
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.9036
lon: -107.702
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.9783
lon: -110.872
Description and history. The Follett House stands prominently overlooking Burlington's waterfront, at the southwest corner of college and South Champlain Streets. The house is oriented facing west toward Lake Champlain, with a terraced lawn extending westward to Battery Street. It is a -story brick structure, with a gabled roof, clapboarded exterior, and stone foundation.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
It lies approximately east of Słubice, south-west of Gorzów Wielkopolski, and north-west of Zielona Góra. History. The village is located in the historic Lubusz Land, which formed part of Poland since the establishment of the state by the Piast dynasty in the 10th century. In the 13th century, it passed to the Margraviate of Brandenburg.

Geographic entities mentioned:
surface_form: Lubusz Land
instance_of: Plateau
countries: Germany
Poland
Kingdom of Poland
Lands of the Bohemian Crown
To the west lies Port Talbot, at approximately, and Swansea at approximately. Geography. The area of sand dunes and the pool at Kenfig are managed by Bridgend County Borough Council as Kenfig Pool National Nature Reserve, the area designated a Site of Special Scientific Interest. The reserve has a visitor and interpretation centre, and a car park.

Geographic entities mentioned:
surface_form: Kenfig Pool
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.5194
lon: -3.7362
It was one of several towns whose people spoke the Hitchiti language. It was first known as part of the Apalachicola Province, an association of tribal towns along the Chattahoochee River. Shortly after 1690, the towns of Apalachicola Province moved to the central part of present-day Georgia, with Hitchiti joining most of those towns along Ochese Creek (now named the Ocmulgee River).

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
The monastery played an important socio-economic role in the development of the village and the area in general. The story of the monastery's foundation has not been recorded, however, according to tradition, two monks from Lapithos, called Dorotheos and Dositheos, left their monastery of St Panteleimon at Mount Athos and returned to Cyprus to start a new monastery.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Geography. Although most of the area is outside the National Park boundary, the town is in the western part of the Peak District. To the north and south lie the Dark Peak highlands, which are made up of millstone grit and are heather-covered moorlands, rugged and bleak. These include Chinley Churn and South Head with, a little further off, Kinder Scout, which looms above the whole area.

Geographic entities mentioned:
surface_form: Dark Peak
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 53.4
lon: -1.8
These include Chinley Churn and South Head with, a little further off, Kinder Scout, which looms above the whole area. To the east is the gentler and more pastoral White Peak, consisting largely of limestone grasslands, nevertheless with spectacular bluffs and the occasional gorge.

Geographic entities mentioned:
surface_form: White Peak
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 53.2
lon: -1.8
Crosland Moor begins at the junction of the Manchester Road A62 and Blackmoorfoot Road the main thoroughfare. The area rises up the hillside to overlook the areas of Milnsbridge and Golcar in the Colne Valley. The name is derived from the local landowners the Crosland family, who owned much of the area in 15th and 16th centuries.

Geographic entities mentioned:
surface_form: Colne Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.6272
lon: -1.8624
Sardis Lake (Oklahoma). Sardis Lake is a reservoir in Pushmataha and Latimer counties in Oklahoma, USA. It was created about 1980 as the result of a dam constructed on Jackfork Creek, a tributary of the Kiamichi River, by the United States Corps of Engineers under contract to the state.

Geographic entities mentioned:
surface_form: sardis lake (oklahoma)
instance_of: Lake
countries: United States
coordinates: lat: 34.6583
lon: -95.3789
Sardis Lake (Oklahoma). Sardis Lake is a reservoir in Pushmataha and Latimer counties in Oklahoma, USA. It was created about 1980 as the result of a dam constructed on Jackfork Creek, a tributary of the Kiamichi River, by the United States Corps of Engineers under contract to the state.

Geographic entities mentioned:
surface_form: sardis lake
instance_of: Lake
countries: United States
coordinates: lat: 34.6583
lon: -95.3789
In brief it provided for the state to have administration and regulatory authority over Sardis Lake, as well as preserving water rights for the Nations in their treaty territories, and allocating a major portion of water from Sardis Lake for the needs of Oklahoma City, dependent on it conducting conservation measures. Description. The lake covers with of shoreline.

Geographic entities mentioned:
surface_form: sardis lake
instance_of: Lake
countries: United States
coordinates: lat: 34.6583
lon: -95.3789
surface_form: sardis lake
instance_of: Lake
countries: United States
coordinates: lat: 34.6583
lon: -95.3789
The lake covers with of shoreline. The lake is an impoundment of Jackfork Creek, a tributary of the Kiamichi River. Sardis Lake is surrounded by the Winding Stair Mountains on the north and east, the Kiamichi Mountains on the south, and the Jackfork Mountains to the west, all of which are subranges of the Ouachita Mountains. The lake is east of McAlester, Oklahoma. It drains an area of.

Geographic entities mentioned:
surface_form: sardis lake
instance_of: Lake
countries: United States
coordinates: lat: 34.6583
lon: -95.3789
United States, et al.&quot; The case wound its way through the courts. At the appeals level, the appeals court upheld the federal government's suit. Oklahoma lost the case when the Supreme Court declined to hear the case. As a result of the state's failure to pay off its debt, the Corps of Engineers legally owns Sardis Lake. Proposed transfer of water.

Geographic entities mentioned:
surface_form: sardis lake
instance_of: Lake
countries: United States
coordinates: lat: 34.6583
lon: -95.3789
As a result of the state's failure to pay off its debt, the Corps of Engineers legally owns Sardis Lake. Proposed transfer of water. Shortly after Sardis Lake was filled, Oklahoma City developed various plans seeking to gain control of much of the water. It presented proposals to the Oklahoma Water Resources Board (OWRB) for moving water from Sardis Lake closer to this major city.

Geographic entities mentioned:
surface_form: sardis lake
instance_of: Lake
countries: United States
coordinates: lat: 34.6583
lon: -95.3789
&quot;Chickasaw Nation and Choctaw Nation, et al. v. Fallin&quot;. Oklahoma City was seeking to purchase the lion's share of water from Sardis Lake. A state contract executed in 2011, reserved 136,000 acre-feet of water for the Oklahoma City Water Utilities Trust. (OUT)
The Chickasaw Nation and Choctaw Nation filed a federal lawsuit in a U.S.

Geographic entities mentioned:
surface_form: sardis lake
instance_of: Lake
countries: United States
coordinates: lat: 34.6583
lon: -95.3789
A state contract executed in 2011, reserved 136,000 acre-feet of water for the Oklahoma City Water Utilities Trust. (OUT)
The Chickasaw Nation and Choctaw Nation filed a federal lawsuit in a U.S. District Court in 2011, seeking an injunction that would prevent the state and Oklahoma City from transporting water from Sardis Lake to Oklahoma City.

Geographic entities mentioned:
surface_form: sardis lake
instance_of: Lake
countries: United States
coordinates: lat: 34.6583
lon: -95.3789
In 1249 the Silesian Duke Bolesław II Rogatka had sold Lubusz Land in the west to the Ascanian Margraves of Brandenburg, and the city of &quot;Landisberch Nova&quot; (named after Altlandsberg) was founded on the site in 1257. The city was at that time an eastern outpost of the newly established Neumark region of Brandenburg, close to the Greater Polish fortress of Santok.

Geographic entities mentioned:
surface_form: Lubusz Land
instance_of: Plateau
countries: Germany
Poland
Kingdom of Poland
Lands of the Bohemian Crown
The entire township is drained by various tributaries of the Coldwater River. The north and west is drained by the South Branch of Hog Creek; the north central by Bagley Creek, which flows into Hog Creek just north of the township; northeast by Cold Creek; and the south by the Sauk River. The Coldwater River flows north to the St. Joseph River, which flows to Lake Michigan.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Redwood Valley, California. Redwood Valley (formerly Basil) is a census-designated place (CDP) in Mendocino County, California, United States. It is located north of Ukiah, the county seat, at an elevation of, and comprises the northern portion of the Ukiah Valley. It is about southeast of Willits. Potter Valley is to the east and Calpella to the south.

Geographic entities mentioned:
surface_form: Ukiah Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.1867
lon: -123.2052
Adamo Alenane Alimo Aliti Alumar Amade Amade Ametina Aneli Anli Apura Arufo Assane Assane Assane Atoto Bacar Bacar Antigo Banjira Biaque Bidjolo Borolia Camope Cantalia Cantia Cauo Cavano Chefe Afonso Chefe Ahonamoro Chefe Antonio Chefe Aquimo Chefe Cahura Chefe Caire Chefe Calialia Chefe Cantato Chefe Caroa Chefe Chinande Chefe Cobre Chefe Colete Chefe Coze Chefe Cunliala Chefe Giquina Chefe Iacuelane Chefe Ingori Chefe Inhatia Chefe Inripa Chefe Inteia Chefe Jalipa Chefe Julai Chefe Lave Chefe Lile Chefe Lopa Chefe Madondo Chefe Malepela Chefe Marraca Chefe Misere Chefe Muanenele Chefe Muansava Chefe Muatuca Chefe Muisse Chefe Muituva Chefe Nacibo Chefe Naioto Chefe Namione Chefe Nampuara Chefe Nancuto Chefe Nanhoma Chefe N Cumabai Chefe Necule Chefe Neparula Chefe Nicuto Chefe Nigoeleua Chefe Nivero Chefe Pilote Chefe Puelia Chefe Purremuere Chefe Purulia Chefe Quilevele Chefe Quimao Chefe Quitarubo Chefe Raide Chefe Sabao Chefe Sararia Chefe Sehane Chefe Selemane Chefe Sucuma Chefe Taiar Chefe Tico Chitima Chiure Colue Comala Costa Covaninha Cuvave Daxe Dhalman Giole Givarro Iamorra Incole Ingaua Inraba Insania Iupuro Jipala João Joio Juma Langima Limia Maaje Macaia Macaiamo Macassar Machepe Macota Magengo Maite Malapua Manocha Maon-o Mapia Marraparre Mataiolava Mauala Mbonge Mecete Mecueracuera Megama Megege Meia Mejacara Menhula Mepamei Mepengula Mepipo Mepoto Mequitaculo Merrapia Mesa Messalo Messiloca Metania Metito Metoma Metoro Metorro Metuaquene Meurra Mexilo Minhoene Mocoloje Mogido Moguia Moja Moloco Monunene Moquina Morruma Mpingo Mpita Muada Muaja Muaja Mualania Muania Muaria Mue Muepurra Mueraerie Muero Muerria Mugara Muguia Muguia Muicava Muigima Muipace Muiquite Muita Mussa Nacacane Nacololo Nacopa Nacote Nacuale Nacuale Nacuanha Nacuchupa Nacussa Nagimbue Naia Nalapia Nalile Namaaquitica Namachatua Namaica Namangoma Namarraco Namarro Namatubile Namatuca Namauco Namuela Namuela Namecala NametaNampacala Nampita Namuine NancoiNancuto Nanduli Nangana Nanjua Nanlia Nanoa Nanripo Nantoa Nantucia Nanzarro Naoia Naputa Narenga Narreva Ncole Ndala Nero Ngeue Ngura Niare Nicocoro Nicorombe Nicuata Niico Nimone Nina Nipatacua Niqueque Niquita Nita Nivico Nomapa Nonia Ntete Nucuncile Nuico Nuto Olocota Omar Regulo Mariri Regulo MedomaRegulo Mepima Regulo Mogabo Regulo Momola Regulo Namaluma Regulo Polubo Regulo Polupo Reia Retima Reva Rimo Roja Rupe Sabai Saide Sicoto Simbo Sirico Sitaa Sunate Talibo Talique TapararaTarade Tarato Tecua Terruma Teucha Titimare Tonhinto TuculeUadjireUapila Uarrussa Uatuncorra Zambezia
Economy.

Geographic entities mentioned:
surface_form: Simbo
instance_of: Mountain
countries: Solomon Islands
coordinates: lat: -8.2916666666667
lon: 156.51666666667
Mount Michael. Mount Michael is an active volcano with a height of 843 m. It is located on Saunders Island in the South Sandwich Islands, a British Overseas Territory in the southern Atlantic Ocean. It is one of the few volcanoes in an overseas territory of the United Kingdom.

Geographic entities mentioned:
surface_form: mount michael
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -57.78
lon: -26.45
Persistent lava lake. In 2019, it was discovered that Mount Michael had a persistent lava lake, a rare phenomenon which is known to occur at only eight volcanoes in the world. In November 2022, an expedition from University College London led by geologist Emma Nicholson reached the summit of the volcano and was able to confirm the existence of the lava lake.

Geographic entities mentioned:
surface_form: mount michael
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -57.78
lon: -26.45
Schongau, Lucerne. Schongau () is a municipality in the district of Hochdorf in the canton of Lucerne in Switzerland. Geography. Schongau is located in the Seetal valley. The municipality has an area of. Of this area, 70.4% is used for agricultural purposes, while 26.1% is forested.

Geographic entities mentioned:
surface_form: Seetal valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 47.23166667
lon: 8.24361111
Balatonudvari. Balatonudvari is a village in Veszprém county. Location. Balatonudvari is situated by the shore of Lake Balaton, between Örvényes and Balatonakali, to the west of the Tihany Peninsula. History. After the founding of the state, it was the property of the Hungarian kings, but in a record from 1164, it is referred to as the possession of the Atyuz Clan.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
WVMT. WVMT (620 AM) is a commercial radio station licensed to Burlington, Vermont, and serving the Champlain Valley of Vermont and New York. WVMT is simulcast on FM translator station W242BK at 96.3 MHz. The translator's owner, Vox AM/FM, LLC, operates WVMT under a local marketing agreement (LMA). The radio studios and offices are within Fort Ethan Allen in Colchester, with Vox's other stations.

Geographic entities mentioned:
surface_form: Champlain Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.45868
lon: -73.42617
Its daytime signal covers most of Northern Vermont, Northeastern New York and part of Quebec, Canada. At night, the station adjusts its coverage to concentrate the signal around the Burlington and Plattsburgh, New York, areas. WVMT's easily identifiable three-tower array is shown on Lake Champlain navigation charts, located in Colchester, near Malletts Bay. Programming.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
River Dysynni. The River Dysynni () is a river in mid Wales. Its source is the Tal-y-llyn Lake () just south of the Cadair Idris massif and its mouth is in the Cardigan Bay area of the Irish Sea to the north of Tywyn. It measures about in length. Course.

Geographic entities mentioned:
surface_form: Tal-y-llyn Lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.6725
lon: -3.8974388888889
surface_form: Cadair Idris
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.699827777778
lon: -3.9086944444444
It measures about in length. Course. The River Dysynni flows from the western end of Tal-y-llyn Lake in a southwesterly direction to its confluence with the Nant Gwernol at Abergynolwyn. From here it flows in a northwesterly direction to its confluence with the Afon Cader, from where it resumes its southwesterly direction, meandering through a broad valley.

Geographic entities mentioned:
surface_form: Tal-y-llyn Lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.6725
lon: -3.8974388888889
It is joined here by its tributary, the Afon Fathew, which flows from near Dolgoch and joins it to the east of Tywyn, near Bryncrug. The river enters Cardigan Bay through the Broad Water lagoon to the north of Tywyn, near Tonfanau. The river is interesting geologically because it exhibits river capture. This is likely to be as a result of river damming during a glacial period.

Geographic entities mentioned:
surface_form: Broad Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.60253
lon: -4.09606
Walking. The Dysynni Valley is popular with walkers. It is a scenic valley, with the Cadair Idris massif to the north and the huge rock face of Craig yr Aderyn to the south. The valley contains the ruins of Castell y Bere near Llanfihangel-y-Pennant. There are several walking routes, one being a path from Bryncrug alongside the Afon Fathew to the Broad Water.

Geographic entities mentioned:
surface_form: Cadair Idris
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.699827777778
lon: -3.9086944444444
Walking. The Dysynni Valley is popular with walkers. It is a scenic valley, with the Cadair Idris massif to the north and the huge rock face of Craig yr Aderyn to the south. The valley contains the ruins of Castell y Bere near Llanfihangel-y-Pennant. There are several walking routes, one being a path from Bryncrug alongside the Afon Fathew to the Broad Water.

Geographic entities mentioned:
surface_form: Broad Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.60253
lon: -4.09606
Stage 20. In the twentieth stage, Thibaut Pinot, in his last Tour before retirement, attacked the breakaway and was solo leader at the top of the Petit Ballon, which was lined by thousands of fans cheering him on. He was overtaken and dropped by the race leaders on the ascent to the Col du Platzerwasel, and Pogačar won the stage ahead of Gall and his tour rival Vingegaard.

Geographic entities mentioned:
surface_form: Petit Ballon
instance_of: Mountain
countries: France
coordinates: lat: 47.98083333
lon: 7.12583333
Early years. Chelios was born in Chicago on January 25, 1962, to Gus and Susan Chelios. They lived in Evergreen Park, Illinois, just south of Chicago. Chris attended Mount Carmel High School not far from the shore of Lake Michigan until his family moved to Poway, California. Then he went to Mira Mesa High School in the north part of San Diego.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Wittenberg Mountain'&quot;, locally &quot;the Wittenberg&quot;, is a mountain in Shandaken, Ulster County, New York. It is part of the Burroughs Range of the Catskill Mountains. Wittenberg is flanked to the southwest by Cornell Mountain and to the northeast by Terrace Mountain. Wittenberg Mountain is within the watershed of Esopus Creek, which drains into the Hudson River and New York Bay.

Geographic entities mentioned:
surface_form: Cornell Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.001480555556
lon: -74.356816666667
surface_form: cornell mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.001480555556
lon: -74.356816666667
surface_form: terrace mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.621666666667
lon: -121.19638888889
surface_form: terrace mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0275
lon: -74.336388888889
surface_form: terrace mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.9555
lon: -110.735
Wittenberg Mountain. Wittenberg Mountain'&quot;, locally &quot;the Wittenberg&quot;, is a mountain in Shandaken, Ulster County, New York. It is part of the Burroughs Range of the Catskill Mountains. Wittenberg is flanked to the southwest by Cornell Mountain and to the northeast by Terrace Mountain.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: wittenberg mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0081
lon: -74.3474
Wittenberg Mountain. Wittenberg Mountain'&quot;, locally &quot;the Wittenberg&quot;, is a mountain in Shandaken, Ulster County, New York. It is part of the Burroughs Range of the Catskill Mountains. Wittenberg is flanked to the southwest by Cornell Mountain and to the northeast by Terrace Mountain.

Geographic entities mentioned:
surface_form: wittenberg mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0081
lon: -74.3474
The northwest and northeast slopes of the mountain drain into Woodland Creek, thence into Esopus Creek. The southeast side of Wittenberg drains into Wittenberg Brook, thence into Maltby Hollow Brook, Bush Kill, and Esopus Creek at Ashokan Reservoir. Wittenberg Mountain is within the Slide Mountain Wilderness of New York's Catskill State Park.

Geographic entities mentioned:
surface_form: slide mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9986
lon: -74.3864
surface_form: slide mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.3127
lon: -119.884
Sean Williams and Benji Vaughan had recently signed to Raja Ram's record label, TIP.World. Imagery and themes. One of the album's themes is Mount Kailash, which is mentioned in the titles of two songs from the album: &quot;Under Mount Kailash&quot; by Process, and &quot;High on Mount Kailash&quot; by Doof. A photograph of the mountain appears on the album cover.

Geographic entities mentioned:
surface_form: Mount Kailash
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 31.066944444444
lon: 81.312777777778
Coldingham Loch. Coldingham Loch is a freshwater loch in the parish of Coldingham, in the Scottish Borders area of Scotland, in the former Berwickshire, between Coldingham Moor and St Abb's Head. The loch is a natural spring-fed loch, about from the sea and about above sea level; it is used for fly fishing for rainbow trout and brown and blue trout. The area is also used for pheasant shooting.

Geographic entities mentioned:
surface_form: coldingham loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.910512
lon: -2.170222
The area is also used for pheasant shooting. The Scottish Borders Council has described Coldingham Loch as &quot;eutrophic open water, with high levels of plant nutrient, turbid water caused by high plankton levels; coarse fish generally dominant; in natural state supports high levels of biodiversity; often important wildfowl sites&quot;.

Geographic entities mentioned:
surface_form: coldingham loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.910512
lon: -2.170222
Paatuup Qaqqaa. Paatuup Qaqqaa is a mountain of Greenland. It is located in the Upernavik Archipelago. The peak is 476 meters tall.

Geographic entities mentioned:
surface_form: paatuup qaqqaa
instance_of: Mountain
countries: Greenland
Gooseberry Falls State Park. Gooseberry Falls State Park is a state park of Minnesota, United States, on the North Shore of Lake Superior. The park is located in Silver Creek Township, about 13 miles (21 km) northeast of Two Harbors, Minnesota in Lake County on scenic Minnesota Highway 61. The park surrounds the mouth of the Gooseberry River and includes Upper, Middle, and Lower Falls.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
This peak is situated on the common boundary shared by Kings Canyon National Park with John Muir Wilderness, and it is the highest point on LeConte Divide. Reinstein ranks as the 260th-highest summit in California. It is set west of Scylla and southwest of Mount Goddard. Topographic relief is significant as the summit rises nearly above Martha Lake in less than one mile.

Geographic entities mentioned:
surface_form: Mount Goddard
instance_of: Mountain
countries: United States
coordinates: lat: 37.1031
lon: -118.72
surface_form: scylla
instance_of: Mountain
countries: United States
coordinates: lat: 37.07994
lon: -118.68955
Mount Reinstein. Mount Reinstein is a mountain summit located west of the crest of the Sierra Nevada mountain range, in Fresno County, California, United States. This peak is situated on the common boundary shared by Kings Canyon National Park with John Muir Wilderness, and it is the highest point on LeConte Divide. Reinstein ranks as the 260th-highest summit in California.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount reinstein
instance_of: Mountain
countries: United States
coordinates: lat: 37.07938
lon: -118.73844
Mount Reinstein. Mount Reinstein is a mountain summit located west of the crest of the Sierra Nevada mountain range, in Fresno County, California, United States. This peak is situated on the common boundary shared by Kings Canyon National Park with John Muir Wilderness, and it is the highest point on LeConte Divide. Reinstein ranks as the 260th-highest summit in California.

Geographic entities mentioned:
surface_form: mount reinstein
instance_of: Mountain
countries: United States
coordinates: lat: 37.07938
lon: -118.73844
Reinstein ranks as the 260th-highest summit in California. It is set west of Scylla and southwest of Mount Goddard. Topographic relief is significant as the summit rises nearly above Martha Lake in less than one mile. An ascent of the peak is non-technical, and inclusion on the Sierra Peaks Section peakbagging list generates climbing interest in this remote peak. History.

Geographic entities mentioned:
surface_form: martha lake
instance_of: Lake
countries: United States
coordinates: lat: 37.0944
lon: -118.738
Kunkush. Cuncush (Ancash Quechua for &quot;Puya raimondii&quot;) is a mountain in the southern part of the Cordillera Blanca in the Andes of Peru, about high. It is situated in the Ancash Region, Recuay Province, Catac District. Cuncush lies southwest of Mururaju and northwest of Pukarahu.

Geographic entities mentioned:
surface_form: Mururaju
instance_of: Mountain
countries: Peru
coordinates: lat: -9.8075
lon: -77.24388889
surface_form: pukarahu
instance_of: Mountain
countries: Peru
coordinates: lat: -8.93027778
lon: -77.54416667
surface_form: pukarahu
instance_of: Mountain
countries: Peru
coordinates: lat: -8.89429
lon: -77.7083
surface_form: pukarahu
instance_of: Mountain
countries: Peru
coordinates: lat: -9.8175
lon: -77.1014
surface_form: mururaju
instance_of: Mountain
countries: Peru
coordinates: lat: -9.8075
lon: -77.24388889
surface_form: pukarahu
instance_of: Mountain
countries: Peru
coordinates: lat: -9.85306
lon: -77.2564
surface_form: pukarahu
instance_of: Mountain
countries: Peru
coordinates: lat: -9.32722
lon: -77.2778
Kunkush. Cuncush (Ancash Quechua for &quot;Puya raimondii&quot;) is a mountain in the southern part of the Cordillera Blanca in the Andes of Peru, about high. It is situated in the Ancash Region, Recuay Province, Catac District. Cuncush lies southwest of Mururaju and northwest of Pukarahu.

Geographic entities mentioned:
surface_form: kunkush
instance_of: Mountain
countries: Peru
coordinates: lat: -10.64888889
lon: -76.72138889
surface_form: kunkush
instance_of: Mountain
countries: Peru
coordinates: lat: -9.9175
lon: -77.0092
surface_form: kunkush
instance_of: Mountain
countries: Peru
coordinates: lat: -9.82722
lon: -77.2686
surface_form: kunkush
instance_of: Mountain
countries: Peru
coordinates: lat: -9.18944444
lon: -76.87194444
Kunkush. Cuncush (Ancash Quechua for &quot;Puya raimondii&quot;) is a mountain in the southern part of the Cordillera Blanca in the Andes of Peru, about high. It is situated in the Ancash Region, Recuay Province, Catac District. Cuncush lies southwest of Mururaju and northwest of Pukarahu.

Geographic entities mentioned:
surface_form: cuncush
instance_of: Mountain
countries: Peru
coordinates: lat: -9.82722
lon: -77.2686
The manuscript has many gaps in the text, as well as containing handwritten notes (known as marginalia). Using the study of comparative writing styles (palaeography), the codex is dated to the 8th or 9th century. The codex is currently kept in the Great Lavra monastery (B' 52) on the Athos peninsula. Description.

Geographic entities mentioned:
surface_form: Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
The area has been increasingly accessible as a tourist attraction and contains Frying Pan Lake, which is the largest hot spring in the world, and the steaming and usually pale blue Inferno Crater Lake, the largest geyser-like feature in the world although the geyser itself cannot be seen since it plays at the bottom of the lake.

Geographic entities mentioned:
surface_form: Frying Pan Lake
instance_of: Lake
countries: New Zealand
coordinates: lat: -38.284613888889
lon: 176.39433888889
The lake's water is usually a brown colour, but can vary depending on the state of the plants growing in it. Red aquatic fern growth is sometimes present. A short distance northeast lies Echo Crater, the biggest crater of the area, filled with the steaming-hot Frying Pan Lake, which is the largest hot spring in the world. The lake has an average depth of and covers.

Geographic entities mentioned:
surface_form: Frying Pan Lake
instance_of: Lake
countries: New Zealand
coordinates: lat: -38.284613888889
lon: 176.39433888889
He was succeeded in 2000 by David Ellenson as the 8th president. The 9th president of HUC-JIR, elected in 2014, was Aaron D. Panken. A noted authority on rabbinic and Second Temple literature, with research interests in the historical development of legal concepts and terms, Panken was killed in a plane crash on May 5, 2018, while piloting a single-engine Aeronca 7AC over New York's Hudson Valley.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Warner Lakes. The Warner Lakes are a chain of shallow lakes and marshes in the Warner Valley of eastern Lake County, Oregon, United States. The lakes extend the length of the valley, covering approximately. The lakes are named in honor of Captain William H. Warner, a topographical engineer who explored Warner Valley before being killed by Native Americans in 1849.

Geographic entities mentioned:
surface_form: Warner Valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
surface_form: warner lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 42.4499
lon: -119.851
The bridge was constructed between May 16, 1867, and July 24, 1867. Known as the Stone Bridge, it was actually a quarter mile long causeway constructed by hauling basalt boulders and smaller rocks from nearby Hart Mountain and dumping them into the marsh. Today, the Stone Bridge across the Warner wetlands still exists. It is listed on the National Register of Historic Places. Lakes and wetlands.

Geographic entities mentioned:
surface_form: Hart Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.4597
lon: -119.741
Most of the water from Twentymile Creek flows into Greaser Reservoir or into irrigation canals in the South Warner Valley. As field drainage, some of its water eventually merges with Deep Creek and flow into Pelican Lake. In addition to the fresh-water creeks that flow into the Warner Lakes, there are a number of hot springs that drain into them.

Geographic entities mentioned:
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 46.57611111
lon: -94.17611111
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 45.5041
lon: -89.2035
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 37.95017
lon: -122.77537
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 46.6985
lon: -96.0198
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 48.0611
lon: -92.9
surface_form: deep creek
instance_of: Watercourse
countries: United States
coordinates: lat: 34.72138888888889
lon: -83.47777777777777
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 46.05777778
lon: -95.80222222
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 44.0925246
lon: -96.9136823
This highway crosses the summit of the Warner Mountains, passing the Warner Canyon Ski Area on the way. The road forks from Lakeview. The main highway continues east while County Road 3–13 departs to the northeast. Following the main highway for leads to Adel in South Warner Valley, near the south end of Pelican Lake. Following County Road 3–13 leads to the North Warner Valley.

Geographic entities mentioned:
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 46.57611111
lon: -94.17611111
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 45.5041
lon: -89.2035
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 37.95017
lon: -122.77537
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 46.6985
lon: -96.0198
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 48.0611
lon: -92.9
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 46.05777778
lon: -95.80222222
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 44.0925246
lon: -96.9136823
It is recommended any visitors contact the Bureau of Land Management's district office in Lakeview, Oregon, for information on the current lake levels before planning canoe trips in the northern lakes. There are no developed campgrounds in the Warner Valley. However, dispersed camping is allowed on land administered by the Bureau of Land Management.

Geographic entities mentioned:
surface_form: current lake
instance_of: Lake
countries: United States
coordinates: lat: 44.164444444444
lon: -95.946388888889
The valley has two regions commonly referred to as South Warner Valley and North Warner Valley. The two areas transition between Crump Lake and Hart Lake at a point where the valley narrows to about in width. Native Americans used the Warner Valley's lakes and wetland for thousands of years before the first white explorers arrived.

Geographic entities mentioned:
surface_form: crump lake
instance_of: Lake
countries: United States
coordinates: lat: 42.2946
lon: -119.8252
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
In 1867, General George Crook decided to build a fort in the Warner Valley to prevent Indian raiding parties from passing through the area. To get his wagons across the wetlands, he directed a bridge to be built across a narrow, marshy channel between Hart Lake and Crump Lake. Forty soldiers of the 23rd Infantry Regiment under the command of Captain James Henton were assigned the task.

Geographic entities mentioned:
surface_form: crump lake
instance_of: Lake
countries: United States
coordinates: lat: 42.2946
lon: -119.8252
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
The valley slopes toward the north. As a result, Crump Lake is elevated higher than Bluejoint Lake. The Warner Lakes are fed by Twentymile Creek and Deep Creek at the south end and Honey Creek which flows into Hart Lake. Most of the water from Twentymile Creek flows into Greaser Reservoir or into irrigation canals in the South Warner Valley.

Geographic entities mentioned:
surface_form: crump lake
instance_of: Lake
countries: United States
coordinates: lat: 42.2946
lon: -119.8252
There are 239 species of birds that live in the area or migrate through the Warner Valley. Species that nest in the areas around Crump Lake and Hart Lake include sandhill cranes, American white pelicans, double-crested cormorants, willets, Wilson's phalaropes, gadwalls, northern shovelers, black-crowned night herons, Canada geese, and numerous varieties of ducks and terns.

Geographic entities mentioned:
surface_form: crump lake
instance_of: Lake
countries: United States
coordinates: lat: 42.2946
lon: -119.8252
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
The lakes extend the length of the valley, covering approximately. The lakes are named in honor of Captain William H. Warner, a topographical engineer who explored Warner Valley before being killed by Native Americans in 1849. The Warner Lakes and surrounding wetlands support a wide variety of birds and other wildlife.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
Much of the land surrounding the lakes is owned by the public and is administered by the Bureau of Land Management. These public lands provide recreational opportunities including hunting, fishing, bird watching, and camping. Warner Valley. The Warner Valley is in south-central Oregon. It is approximately long and wide.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
These public lands provide recreational opportunities including hunting, fishing, bird watching, and camping. Warner Valley. The Warner Valley is in south-central Oregon. It is approximately long and wide. Most of the valley is in Lake County, however the north end of the valley extends about into Harney County.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
Today, steep cliffs rise above a chain of endorheic lakes and interconnected wetlands, known collectively as Warner Lakes. The valley has two regions commonly referred to as South Warner Valley and North Warner Valley. The two areas transition between Crump Lake and Hart Lake at a point where the valley narrows to about in width.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The two areas transition between Crump Lake and Hart Lake at a point where the valley narrows to about in width. Native Americans used the Warner Valley's lakes and wetland for thousands of years before the first white explorers arrived. There are scores of petroglyphs near the lake shores, some are estimated to be 12,000 years old.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
Native Americans used the Warner Valley's lakes and wetland for thousands of years before the first white explorers arrived. There are scores of petroglyphs near the lake shores, some are estimated to be 12,000 years old. The Greaser Petroglyph Site, in the South Warner Valley, is listed on the National Register of Historic Places. In December 1843, Captain John C.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
Fremont and his party spent Christmas Day camped near Hart Lake. In honor of the date, Fremont named it Christmas Valley and the lake Christmas Lake. However, early mapmakers mistakenly plotted Christmas Valley northwest of the Warner Valley, leaving the valley and lake unnamed on early maps. In 1849, the valley was explored by Captain William Horace Warner, an Army topographical engineer.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
However, early mapmakers mistakenly plotted Christmas Valley northwest of the Warner Valley, leaving the valley and lake unnamed on early maps. In 1849, the valley was explored by Captain William Horace Warner, an Army topographical engineer. On September 26, 1849, Warner was ambushed and killed by Indians just south of the Warner Valley. In 1864, Lieutenant Colonel C. S.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
Drew named the valley in honor of Warner, who he believed had been killed there. In 1867, General George Crook decided to build a fort in the Warner Valley to prevent Indian raiding parties from passing through the area. To get his wagons across the wetlands, he directed a bridge to be built across a narrow, marshy channel between Hart Lake and Crump Lake.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
It is listed on the National Register of Historic Places. Lakes and wetlands. At one time, the entire Warner Valley was covered by a single vast lake. However, the water level gradually receded, leaving a chain of lakes at the low spots with marsh land between the lakes. Today, the valley floor is occupied by a chain of lakes and wetlands covering over.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
The Warner Lakes are fed by Twentymile Creek and Deep Creek at the south end and Honey Creek which flows into Hart Lake. Most of the water from Twentymile Creek flows into Greaser Reservoir or into irrigation canals in the South Warner Valley. As field drainage, some of its water eventually merges with Deep Creek and flow into Pelican Lake.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
There are forty-two mammal species that live in the areas around the Warner Lakes. These include pronghorn, bighorn sheep, elk, mule deer, cougar, bobcat, and coyotes. Smaller mammals include jackrabbits, ground squirrels, chipmunks, skunks, and muskrats. There are 239 species of birds that live in the area or migrate through the Warner Valley.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
The larger birds common to the Warner Lakes area include great horned owls, long-eared owls, prairie falcons, marsh hawks, golden eagles, and bald eagles. Recreation. Much of the Warner Valley is public lands, administered by the Bureau of Land Management. These public lands offer numerous recreational opportunities including hunting, fishing, bird watching, boating, and camping.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
It is recommended any visitors contact the Bureau of Land Management's district office in Lakeview, Oregon, for information on the current lake levels before planning canoe trips in the northern lakes. There are no developed campgrounds in the Warner Valley. However, dispersed camping is allowed on land administered by the Bureau of Land Management.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
The main highway continues east while County Road 3–13 departs to the northeast. Following the main highway for leads to Adel in South Warner Valley, near the south end of Pelican Lake. Following County Road 3–13 leads to the North Warner Valley. The pavement ends past the junction, at the small unincorporated community of Plush, approximately two miles west of Hart Lake.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
In December 1843, Captain John C. Fremont led a party through the valley. Fremont and his party spent Christmas Day camped near Hart Lake. In honor of the date, Fremont named it Christmas Valley and the lake Christmas Lake. However, early mapmakers mistakenly plotted Christmas Valley northwest of the Warner Valley, leaving the valley and lake unnamed on early maps.

Geographic entities mentioned:
surface_form: christmas lake
instance_of: Lake
countries: United States
coordinates: lat: 44.898055555556
lon: -93.541388888889