Sarmila/GeoWiki-Features huggingface dataset:
The three-man dog sledge party continued south to a small plywood caravan left at Binders Base at 72°36' South by the 1960 Mawson party, in order to re-provision and sledge on to the Fisher Glacier. Crevasses slowed the party, but one day sufficed to cross the glacier, and after inspecting the formidable ice-falls on the south side on Mt.

Geographic entities mentioned:
surface_form: menzies
instance_of: Mountain
coordinates: lat: -73.5
lon: 61.833333333333
On moving to California in 1880, Irish immediately became editor of the &quot;Alta California&quot; newspaper and, after that paper's demise, became editor and &quot;principal owner&quot; of the &quot;Oakland Times.&quot;
After 1888, Irish was a contributor to &quot;the most comprehensive visual coverage of the Far West&quot; then available—a printed work called &quot;Picturesque California and the Region West of the Rocky Mountains from Alaska to Mexico.&quot; In the chapter about the Sacramento Valley, for which he was responsible, &quot;John P.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
Hutchinson, Joseph Nisbet LeConte and James K. Moffitt. They approached the area overland from south of the Palisades, and scouted possible routes from the summits of Marion Peak and Mount Sill. Armed with this intelligence, they planned to ascend the southwest chute of the U Notch, and find a way to bypass the rock face between the notch and the upper reaches of North Palisade.

Geographic entities mentioned:
surface_form: Marion Peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.9566
lon: -118.52288
surface_form: Mount Sill
instance_of: Mountain
countries: United States
coordinates: lat: 37.094377777778
lon: -118.50288333333
surface_form: mount sill
instance_of: Mountain
countries: United States
coordinates: lat: 37.094377777778
lon: -118.50288333333
surface_form: sill
instance_of: Mountain
countries: United States
coordinates: lat: 37.094377777778
lon: -118.50288333333
surface_form: marion peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.9566
lon: -118.52288
North Palisade. North Palisade is the third-highest mountain in the Sierra Nevada range of California, and one of the state's small number of peaks over 14,000 feet, known as fourteeners. It is the highest peak of the Palisades group of peaks in the central part of the Sierra range.

Geographic entities mentioned:
surface_form: north palisade
instance_of: Mountain
countries: United States
coordinates: lat: 37.0943
lon: -118.5145
It is the highest peak of the Palisades group of peaks in the central part of the Sierra range. It sports a small glacier (the Palisade Glacier) and several highly prized rock climbing routes on its northeast side. History. North Palisade has a collection of names from the 19th century. The Wheeler Survey referred to it as Northwest Palisade in 1878. The following year, Lilbourne A.

Geographic entities mentioned:
surface_form: north palisade
instance_of: Mountain
countries: United States
coordinates: lat: 37.0943
lon: -118.5145
Hutchinson, Joseph Nisbet LeConte and James K. Moffitt. They approached the area overland from south of the Palisades, and scouted possible routes from the summits of Marion Peak and Mount Sill. Armed with this intelligence, they planned to ascend the southwest chute of the U Notch, and find a way to bypass the rock face between the notch and the upper reaches of North Palisade.

Geographic entities mentioned:
surface_form: north palisade
instance_of: Mountain
countries: United States
coordinates: lat: 37.0943
lon: -118.5145
These gullies were blocked by a pair of chockstones, requiring class 4 moves to pass. Beyond these obstacles, they crested the southeast ridge, and climbed a series of granite blocks to the summit. After making this climb, LeConte is quoted as writing in a letter, &quot;I have called the peak merely the North Palisade.

Geographic entities mentioned:
surface_form: north palisade
instance_of: Mountain
countries: United States
coordinates: lat: 37.0943
lon: -118.5145
After making this climb, LeConte is quoted as writing in a letter, &quot;I have called the peak merely the North Palisade. Put Dusy's name on some less imposing mass, and give us a name to be handed down through all time.&quot;
The peak has been called North Palisade since that day, and received official recognition by the U.S. Board on Geographic Names. Climate.

Geographic entities mentioned:
surface_form: north palisade
instance_of: Mountain
countries: United States
coordinates: lat: 37.0943
lon: -118.5145
History. It was the first of the National Parks of Spain. When it was created 22 July 1918 with help from Pedro Pidal, 1st Marquess of Villaviciosa de Asturias, it covered the western part of today's national park, centered on the Lakes of Covadonga. The &quot;Parque Nacional de la Montaña de Covadonga&quot;, as it then was called, had an area of 169.25 km².

Geographic entities mentioned:
surface_form: Lakes of Covadonga
instance_of: Group of lakes
countries: Spain
coordinates: lat: 43.26829288409789
lon: -4.985873734085007
As mentioned above, except for these two alternatives, the other, in most cases are suitable only for special vehicles, and yet they can not access certain areas. Suspension bridges road was constructed and opened in 1918 linking the Valley Traslasierra with the city of Villa Carlos Paz in the Punilla Valley. Geology.

Geographic entities mentioned:
surface_form: Punilla Valley
instance_of: Valley
countries: Argentina
coordinates: lat: -31.033333333333
lon: -64.5
Gunnerside Gill. Gunnerside Gill (or Ghyll) is a small valley in the Yorkshire Dales, England, which branches off Swaledale into moorland to the north of Gunnerside. The site of intensive lead mining in the 18th and 19th centuries, the valley still contains much evidence of its industrial past.

Geographic entities mentioned:
surface_form: Swaledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.361
lon: -1.838
surface_form: gunnerside gill
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.3994
lon: -2.09222
Gunnerside Gill. Gunnerside Gill (or Ghyll) is a small valley in the Yorkshire Dales, England, which branches off Swaledale into moorland to the north of Gunnerside. The site of intensive lead mining in the 18th and 19th centuries, the valley still contains much evidence of its industrial past.

Geographic entities mentioned:
surface_form: gunnerside gill
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.3994
lon: -2.09222
The transition was complete on 1 April 1999, when the OPP's Northwest Patrol was transferred to NAPS. The OPP still administers First Nations policing for Big Trout Lake, Weagamow, Muskrat Dam, and Pikangikum. Organization and operations.

Geographic entities mentioned:
surface_form: Big Trout Lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.78333333333333
lon: -90.00722222222223
Lake Hule. Lake Hule (), which translates to &quot;Lake of Rubber&quot;, due to the abundance of rubber trees nearby, is a fresh water crater lake located in the northern highlands of Costa Rica. It is part of a complex of lakes comprising Lake Hule, Lake Congo and Lake Bosque Alegre. The lakes are part of the Bosque Alegre Wildlife Refuge. Location.

Geographic entities mentioned:
surface_form: lake hule
instance_of: Lake
countries: Costa Rica
coordinates: lat: 10.295277777778
lon: -84.208888888889
Eckkopf. The Eckkopf is a hill in the Palatine Forest in the German state of Rhineland-Palatinate. It lies about 3 km west of the small Palatine town of Deidesheim in the Haardt, as the eastern edge of the Palatine Forest is called. It has a observation tower called the Eckkopf Tower (&quot;Eckkopfturm&quot;).

Geographic entities mentioned:
surface_form: eckkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 49.4158
lon: 8.13806
It lies about 3 km west of the small Palatine town of Deidesheim in the Haardt, as the eastern edge of the Palatine Forest is called. It has a observation tower called the Eckkopf Tower (&quot;Eckkopfturm&quot;). By the tower is an inn, which is open on most weekends during the year and on several public holidays.

Geographic entities mentioned:
surface_form: eckkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 49.4158
lon: 8.13806
Since 1976, UNESCO has designated it as a biosphere reserve. The park covers an area of, approximately 85% of which is forested. It includes the northern and part of the southern side of the Babia Góra massif. The massif's main peak (known as &quot;Diablak&quot;), is the highest point of the Orava Beskids mountain range at.

Geographic entities mentioned:
surface_form: Babia Góra
instance_of: Mountain
countries: Poland
Slovakia
coordinates: lat: 49.573055555556
lon: 19.530555555556
Arbroath has a successful cricket club. It won the CSL Eastern Premiership in 2013 and the Scottish Cup in 2015. Arbroath is a popular location for angling. Public services. Water is supplied by Scottish Water from Lintrathen and Backwater reservoirs in Glen Isla. Electricity distribution is by Scottish and Southern Electricity Networks. Waste management is handled by Angus Council.

Geographic entities mentioned:
surface_form: Lintrathen
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.666666666667
lon: -3.1833333333333
By the mid-1990s, poaching had rendered the species extinct there. In 1950, Chitwan’s forest and grasslands extended over more than and were home to about 800 rhinos. When poor farmers from the mid-hills moved to the Chitwan Valley in search of arable land, the area was subsequently opened for settlement, and poaching of wildlife became rampant.

Geographic entities mentioned:
surface_form: Chitwan
instance_of: Valley
countries: Nepal
This decline in populations is due to hunting to supply the demand for skins. Habitat degradation. One problem at Lake Baikal is the introduction of pollutants into the ecosystem. Pesticides such as DDT and hexachlorocyclohexane, as well as industrial waste, mainly from the Baykalsk Pulp and Paper Mill, are thought to have been the cause of several disease epidemics among Baikal seal populations.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Career. Jenny Enodd competed for the Budal IL club. She competed in her first international biathlon race as part of the 18 IBU Cup in Arber. In the 15 km individual race, she achieved a top 10 finish in ninth place with just one shooting miss. Totally Enodd has completed 91 races in her IBU Cup career. She has won once and made the podium six times in individual races.

Geographic entities mentioned:
surface_form: Arber
instance_of: Mountain
countries: Germany
coordinates: lat: 49.1125
lon: 13.136111111111
Alder Lake (New York). Alder Lake is a body of water that is located in Hardenburgh, Ulster County in the lower Hudson Valley region of New York. It is located in the Balsam Lake State Forest Preserve, which is a part of the Catskill Forest Preserve. The lake was man made by the Coykendall family in the 1900s. It is most often used for recreational uses and family day trips. History.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
surface_form: alder lake
instance_of: Lake
countries: United States
coordinates: lat: 42.049166666667
lon: -74.676388888889
Alder Lake (New York). Alder Lake is a body of water that is located in Hardenburgh, Ulster County in the lower Hudson Valley region of New York. It is located in the Balsam Lake State Forest Preserve, which is a part of the Catskill Forest Preserve. The lake was man made by the Coykendall family in the 1900s. It is most often used for recreational uses and family day trips. History.

Geographic entities mentioned:
surface_form: balsam lake
instance_of: Lake
countries: United States
coordinates: lat: 45.465
lon: -92.4369
surface_form: balsam lake
instance_of: Lake
countries: United States
coordinates: lat: 47.53
lon: -93.414166666667
Hiking. There is a state maintained/marked trail around the entire lake. The &quot;Alder Lake Loop Trail&quot; is 1.5 miles long. On the east side of the lake, the loop trail connects to the &quot;Mill Brook Ridge Trail&quot; which can be taken east to Balsam Lake Mountain. Fishing. There are Brook trout in the lake, but there are special fishing regulations because it is a man-made lake.

Geographic entities mentioned:
surface_form: balsam lake
instance_of: Lake
countries: United States
coordinates: lat: 45.465
lon: -92.4369
surface_form: balsam lake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0457
lon: -74.5945
surface_form: balsam lake
instance_of: Lake
countries: United States
coordinates: lat: 47.53
lon: -93.414166666667
Alder Lake (New York). Alder Lake is a body of water that is located in Hardenburgh, Ulster County in the lower Hudson Valley region of New York. It is located in the Balsam Lake State Forest Preserve, which is a part of the Catskill Forest Preserve. The lake was man made by the Coykendall family in the 1900s. It is most often used for recreational uses and family day trips. History.

Geographic entities mentioned:
surface_form: alder lake (new york)
instance_of: Lake
countries: United States
coordinates: lat: 42.049166666667
lon: -74.676388888889
It is located in the Balsam Lake State Forest Preserve, which is a part of the Catskill Forest Preserve. The lake was man made by the Coykendall family in the 1900s. It is most often used for recreational uses and family day trips. History. Alder Lake was established in 1901 by Samuel D. Coykendall. Coykendall was a strong financer in the area. He owned some of the Delaware and Ulster railroad.

Geographic entities mentioned:
surface_form: alder lake
instance_of: Lake
countries: United States
coordinates: lat: 42.049166666667
lon: -74.676388888889
If we were able to catch it and find a use 30, 40 years ago when the state bought it, perhaps something could have been done.&quot;
Physical features. Alder Lake elevation is above sea level. The mean depth of Alder Lake is feet. The max depth of Alder Lake is feet. The lake covers a total of. Hiking. There is a state maintained/marked trail around the entire lake.

Geographic entities mentioned:
surface_form: alder lake
instance_of: Lake
countries: United States
coordinates: lat: 42.049166666667
lon: -74.676388888889
To keep these fish they have to be a minimum of 12 inches long. Swimming. Swimming is allowed in Alder Lake. There is no beach or lifeguard. Boating. Non-motorized boats are allowed on Alder Lake. Camping. Camping is available for people interested in staying overnight. There are 7-10 primitive camp sites. Camping is on a first-come, first-served basis.

Geographic entities mentioned:
surface_form: alder lake
instance_of: Lake
countries: United States
coordinates: lat: 42.049166666667
lon: -74.676388888889
It is situated between Palisade Basin and Dusy Basin in the Palisades area of northern Kings Canyon National Park. It is west of North Palisade, south of Bishop Pass, and immediately north of Knapsack Pass. This mountain's name has been officially adopted by the United States Board on Geographic Names. The first ascent of the summit was made prior to 1925 by persons unknown. Climate.

Geographic entities mentioned:
surface_form: North Palisade
instance_of: Mountain
countries: United States
coordinates: lat: 37.0943
lon: -118.5145
Columbine Peak. Columbine Peak is a mountain summit located west of the crest of the Sierra Nevada mountain range, in Fresno County of northern California, United States. It is situated between Palisade Basin and Dusy Basin in the Palisades area of northern Kings Canyon National Park. It is west of North Palisade, south of Bishop Pass, and immediately north of Knapsack Pass.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: columbine peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.08937
lon: -118.54148
Columbine Peak. Columbine Peak is a mountain summit located west of the crest of the Sierra Nevada mountain range, in Fresno County of northern California, United States. It is situated between Palisade Basin and Dusy Basin in the Palisades area of northern Kings Canyon National Park. It is west of North Palisade, south of Bishop Pass, and immediately north of Knapsack Pass.

Geographic entities mentioned:
surface_form: columbine peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.08937
lon: -118.54148
This mountain's name has been officially adopted by the United States Board on Geographic Names. The first ascent of the summit was made prior to 1925 by persons unknown. Climate. According to the Köppen climate classification system, Columbine Peak is located in an alpine climate zone. Most weather fronts originate in the Pacific Ocean, and travel east toward the Sierra Nevada mountains.

Geographic entities mentioned:
surface_form: columbine peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.08937
lon: -118.54148
Human samples from Nemrik 9 (9500-8000 BC), Boncuklu (9000-8500 BC), Çayönü (8300-7500 BC) were part of a recent genetic study, as members of a Mesopotamia_Neolithic cluster. In this study, the Mesopotamia_Neolithic cluster appeared as a major ancestry of several Levantine and Egyptian Bronze Age individuals, particularly from Ebla, Ashkalon, Baq'ah and Nuwayrat.

Geographic entities mentioned:
surface_form: Baq'ah
instance_of: Valley
countries: State of Palestine
Phelps gave the mountain its current name based on its appearance to a haystack, and later cut the first trail to the summit in 1873. The summit is an alpine zone above the treeline, which offers a view of nearby Mount Marcy and Panther Gorge. Two trails can be used to access the summit of Haystack.

Geographic entities mentioned:
surface_form: Mount Marcy
instance_of: Mountain
countries: United States
coordinates: lat: 44.112733333333
lon: -73.923727777778
Mount Haystack. Mount Haystack is a mountain in the Great Range of the Adirondack Mountains of New York. With an elevation of, it is the third-highest mountain in New York and one of the 46 High Peaks in Adirondack Park. It is located in the town of Keene in Essex County.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount haystack
instance_of: Mountain
countries: United States
coordinates: lat: 44.1056
lon: -73.9006
Mount Haystack. Mount Haystack is a mountain in the Great Range of the Adirondack Mountains of New York. With an elevation of, it is the third-highest mountain in New York and one of the 46 High Peaks in Adirondack Park. It is located in the town of Keene in Essex County.

Geographic entities mentioned:
surface_form: mount haystack
instance_of: Mountain
countries: United States
coordinates: lat: 44.1056
lon: -73.9006
Mount Haystack. Mount Haystack is a mountain in the Great Range of the Adirondack Mountains of New York. With an elevation of, it is the third-highest mountain in New York and one of the 46 High Peaks in Adirondack Park. It is located in the town of Keene in Essex County.

Geographic entities mentioned:
surface_form: high peaks
instance_of: Mountain
countries: United States
coordinates: lat: 45
lon: -70.4
He participated in an integrated Boy Scout troop and attended McKinley Technology High School, spending a period every summer at a camp on Lake Winnipesaukee in New Hampshire. In 1957–58, during his senior year in high school, Reason became interested in the Naval Reserve Officer Training Corps, but was not selected although he ranked second out of 300 applicants.

Geographic entities mentioned:
surface_form: Lake Winnipesaukee
instance_of: Lake
countries: United States
coordinates: lat: 43.598888888889
lon: -71.323055555556
The type site is Pandu Rajar Dhibi, where black and red ware and tools made from bone and copper were found alongside remains of human body. It extends from the foothills of the Chota Nagpur Plateau to the Bhāgirathi-Hooghly river basin, covering a considerable part of southwestern or Rarh and coastal regions of modern-day West Bengal; from Birbhum in the north to Purba Medinipur in the south.

Geographic entities mentioned:
surface_form: Chota Nagpur Plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
Geography. The Pandu culture flourished in the present-day eastern Indian state of West Bengal, which is the western part of the historical Bengal region. The culture thus spread in the lower Ganges valley, from the Bhagirathi-Hooghly River, one of the two main tributaries of the Ganges, in the east to the eastern fringes of the Chota Nagpur Plateau in the west.

Geographic entities mentioned:
surface_form: Chota Nagpur Plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
Its historical center or core lay around the confluence of the Ajay and Kunur rivers, the area where most of the archaeological sites have been discovered. The valleys of the rivers originating from the Chotanagpur plateau and the Rajmahal hills where the culture flourished, had fertile farmland and availability of water, which created favorable conditions for agriculture in the region.

Geographic entities mentioned:
surface_form: Rajmahal hills
instance_of: Mountain
countries: India
coordinates: lat: 25
lon: 87
Death. Macià died due to appendicitis on 25 December 1933 in Barcelona. His funeral caused a massive demonstration of grief. His remains rest in the &quot;Plaça de la Fe&quot;, the Montjuïc Cemetery, in Barcelona's Montjuïc hill. Documentation.

Geographic entities mentioned:
surface_form: Montjuïc
instance_of: Mountain
countries: Spain
coordinates: lat: 41.364166666667
lon: 2.1580555555556
He was a brother of physician Christian Magnus Sinding-Larsen, colonel Birger Fredrik Sinding-Larsen and painter Kristofer Sinding-Larsen. Sinding-Larsen began his education at Kristiania tekniske skole (now Oslo ingeniørhøgskole) from 1885 to 1889 and received training from Herman Major Schirmer during surveying in Gudbrandsdalen.

Geographic entities mentioned:
surface_form: Gudbrandsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.1333
lon: 10.35
As a municipal division, the district is incorporated as Beloyarsky Municipal District, with the town of okrug significance of Beloyarsky being incorporated within it as Beloyarsky Urban Settlement. Geography. Lake Numto, a sacred place for the Khanty, is located in the district. The adjacent wetlands and the lake are part of an integrated protected area which was established in 1997. Sources.

Geographic entities mentioned:
surface_form: Numto
instance_of: Lake
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 63.516666666666666
lon: 71.45
Belemnite Point. Belemnite Point () is the eastern extremity of a mainly ice-free, hook-shaped ridge, midway between Lamina Peak and Ablation Point and inland from George VI Sound on the east coast of Alexander Island, Antarctica. It was first photographed from the air on November 23, 1935, by Lincoln Ellsworth and mapped from these photos by W.L.G. Joerg.

Geographic entities mentioned:
surface_form: Lamina Peak
instance_of: Mountain
coordinates: lat: -70.5333
lon: -68.75
Churen Himal. Churen Himal () is a mountain that is part of the Dhaulagiri massif. It has an elevation of. It was first climbed by Kozo Hasegawa and Ang Norbu Sherpa in 1970.

Geographic entities mentioned:
surface_form: churen himal
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.731595
lon: 83.21011
surface_form: churen himal
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.696666666666665
lon: 83.49
Churen Himal. Churen Himal () is a mountain that is part of the Dhaulagiri massif. It has an elevation of. It was first climbed by Kozo Hasegawa and Ang Norbu Sherpa in 1970.

Geographic entities mentioned:
surface_form: churen himal
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.731595
lon: 83.21011
surface_form: dhaulagiri
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.696666666666665
lon: 83.49
surface_form: churen himal
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.696666666666665
lon: 83.49
John Williams (goldsmith). John Williams was a Welsh-born goldsmith based in London who worked for the British royal family. Background. He was a son of William Coetmor, and is associated with the property Hafod Lwyfog in Nant Gwynant near Beddgelert. In 1610 he donated a silver chalice and paten-cover to the church in Beddgelert. Williams is said to have founded a chapel at Nanwhynen. Career.

Geographic entities mentioned:
surface_form: Nant Gwynant
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.0374
lon: -4.0471
Trento became a Roman &quot;municipium&quot; in the 40s BC. During the reign of Emperor Claudius (41-54 AD) Trentino was integrated into the Imperial road network with the construction of the Via Claudia Augusta Padana (from Ostiglia to the Resia Pass) and the Via Augusta Altinate (from Treviso to Trento, passing through the Valsugana).

Geographic entities mentioned:
surface_form: Valsugana
instance_of: Valley
countries: Italy
coordinates: lat: 46
lon: 11.666666666667
Porto Ceresio. Porto Ceresio (Varesino: &quot;Pòrt Cerési&quot;) is a &quot;comune&quot; (municipality) on Lake Lugano in the Province of Varese in the Italian region Lombardy, located about northwest of Milan and about northeast of Varese, on the border with Switzerland. As of 31 December 2004, it had a population of 3,080 and an area of.

Geographic entities mentioned:
surface_form: Lake Lugano
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46
lon: 9
Orvin Mountains. The Orvin Mountains () constitute a major group of mountain ranges, extending for about between the Wohlthat Mountains and the Mühlig-Hofmann Mountains in Queen Maud Land. With its summit at, the massive Sandeggtind Peak forms the highest point in the Conrad Mountains, a subrange of the Orvin Mountains. Discovery and naming.

Geographic entities mentioned:
surface_form: Sandeggtind Peak
instance_of: Mountain
coordinates: lat: -71.866666666667
lon: 9.75
La Pointe County, Wisconsin. La Pointe County was created on February 19, 1845, by the Territory of Wisconsin from the northern portion of the existing territorial St.

Geographic entities mentioned:
surface_form: Lac Courte Oreilles
instance_of: Lake
countries: United States
coordinates: lat: 45.883333333333
lon: -91.416666666667
In the Hood Canal depression, two significant lake stages existed, Lake Skokomish and Lake Hood. Early Lake Skokomish’s surface was at above sea level, draining across the divide at Shelton, Washington into early Glacial Lake Russell. As the glacier receded northward, this freshwater lake grew in size, until the ice was north of the Clifton channel.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
surface_form: lake skokomish
instance_of: Lake
countries: United States
coordinates: lat: 47.363322
lon: -123.127485
Here, the water level equalized to Glacial Lake Russell no longer having a separate identify. Lake Skokomish. Lake Skokomish formed in the depression of the Hood Canal and the Skokomish River. It drained across a southern divide at Shelton, Washington. When this outflow joined Lake Russell, it formed the Shelton Delta. This outlet was approximately above sea level.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
This longer and lower level lake is referred to as Lake Hood. The glacier continued to recede northward until it reached the Poulsbo channel. Here, the water level equalized to Glacial Lake Russell no longer having a separate identify. Lake Skokomish. Lake Skokomish formed in the depression of the Hood Canal and the Skokomish River. It drained across a southern divide at Shelton, Washington.

Geographic entities mentioned:
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
Here, the water level equalized to Glacial Lake Russell no longer having a separate identify. Lake Skokomish. Lake Skokomish formed in the depression of the Hood Canal and the Skokomish River. It drained across a southern divide at Shelton, Washington. When this outflow joined Lake Russell, it formed the Shelton Delta. This outlet was approximately above sea level.

Geographic entities mentioned:
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
This outlet was approximately above sea level. As the glacier receded northward, a lower outlet at Clifton, opened into Lake Russell at Cases Inlet (North Bay)
The second and lower stage of this water body formed when the ice was far enough north to open the Clifton outlet. It continued until the glacier reached the Poulsbo Channel. Here, Lake Russell and Lake Hood equalized and became one lake.

Geographic entities mentioned:
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
It continued until the glacier reached the Poulsbo Channel. Here, Lake Russell and Lake Hood equalized and became one lake. The Clifton Channel: The Clifton outlet channel is a definite feature across the divide on which it lies. It is deep at Lake Deborah in the col, above tide. This lake now drains both to Cases Inlet and Hood Canal.

Geographic entities mentioned:
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
surface_form: hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
It is deep at Lake Deborah in the col, above tide. This lake now drains both to Cases Inlet and Hood Canal. Gravel terraces exist along the channel, and one terrace on the east side continues as a small channel directly eastward to Cases Inlet. The Clifton channel ends in the forest west of Allyn, above tide, corresponding with the dominant water plane of Lake Russell.

Geographic entities mentioned:
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
A swampy pass occurs midway of its length at an altitude of, and a stream terrace lies on the eastern side of the valley near the pass, at an altitude of. In the Poulsbo Valley, Lake Hood appears to have found an outlet lower than the Clifton channel, and to have entered Lake Russell at the head of Dogfish (Liberty) Bay. The Brinnon Delta is to be correlated with the level of Lake Russell.

Geographic entities mentioned:
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
surface_form: hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
In the Poulsbo Valley, Lake Hood appears to have found an outlet lower than the Clifton channel, and to have entered Lake Russell at the head of Dogfish (Liberty) Bay. The Brinnon Delta is to be correlated with the level of Lake Russell. The two lakes may be considered as one at this stage, Lake Hood sinking by erosion of the Poulsbo channel to the level of Lake Russell, and becoming an arm of it.

Geographic entities mentioned:
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
In the Poulsbo Valley, Lake Hood appears to have found an outlet lower than the Clifton channel, and to have entered Lake Russell at the head of Dogfish (Liberty) Bay. The Brinnon Delta is to be correlated with the level of Lake Russell. The two lakes may be considered as one at this stage, Lake Hood sinking by erosion of the Poulsbo channel to the level of Lake Russell, and becoming an arm of it.

Geographic entities mentioned:
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
surface_form: hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
If the ice dam causing Lake Russell remained effective during the next few miles of retreat, as there is good reason for believing, Lake Russell levels obtained in Hood Canal with broad connection across the low northern tip of Kitsap County peninsula, a few miles north of the Poulsbo channel.

Geographic entities mentioned:
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
surface_form: hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
Lack of Vashon Deltas of Olympic Rivers
The Olympic Mountains have several streams leading into Hood Canal, which have no valley deltas at the levels of the glacial lakes. The valley of Quilcene River has a long gravel slope gradually descending from levels above Lake Russell to tidewater. The Duckabush Valley, the Hama Hama and Skokomish rivers show no evidence of glacially derived deltas.

Geographic entities mentioned:
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
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
It appears the later erosion regraded the Pleistocene gravels of these valleys. Lake Hood. The second and lower stage of this water body formed when the ice was far enough north to open the Clifton outlet. It continued until the glacier reached the Poulsbo Channel. Here, Lake Russell and Lake Hood equalized and became one lake.

Geographic entities mentioned:
surface_form: lake russell
instance_of: Lake
countries: United States
coordinates: lat: 38
lon: -119
surface_form: hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
The Clifton channel ends in the forest west of Allyn, above tide, corresponding with the dominant water plane of Lake Russell. The Brinnon Delta: The only delta of Vashon age known in the valley of Hood Canal is at the mouth of the Dusewallips River, on the north side of the valley. At the seaward upper margin, it is above the Sound.

Geographic entities mentioned:
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: 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: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
A meridional trough of the pre-Vashon topography, styled the Poulsbo Valley in this paper (locally called Big Valley), crosses the peninsula here. A swampy pass occurs midway of its length at an altitude of, and a stream terrace lies on the eastern side of the valley near the pass, at an altitude of.

Geographic entities mentioned:
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
Lake Skokomish. During the Vashon Glaciation a series of lakes formed along the southern margin of the Cordilleran Ice Cap. In the Hood Canal depression, two significant lake stages existed, Lake Skokomish and Lake Hood. Early Lake Skokomish’s surface was at above sea level, draining across the divide at Shelton, Washington into early Glacial Lake Russell.

Geographic entities mentioned:
surface_form: lake skokomish
instance_of: Lake
countries: United States
coordinates: lat: 47.363322
lon: -123.127485
Lake Skokomish. During the Vashon Glaciation a series of lakes formed along the southern margin of the Cordilleran Ice Cap. In the Hood Canal depression, two significant lake stages existed, Lake Skokomish and Lake Hood. Early Lake Skokomish’s surface was at above sea level, draining across the divide at Shelton, Washington into early Glacial Lake Russell.

Geographic entities mentioned:
surface_form: lake skokomish
instance_of: Lake
countries: United States
coordinates: lat: 47.363322
lon: -123.127485
surface_form: hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
surface_form: hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
This longer and lower level lake is referred to as Lake Hood. The glacier continued to recede northward until it reached the Poulsbo channel. Here, the water level equalized to Glacial Lake Russell no longer having a separate identify. Lake Skokomish. Lake Skokomish formed in the depression of the Hood Canal and the Skokomish River. It drained across a southern divide at Shelton, Washington.

Geographic entities mentioned:
surface_form: lake skokomish
instance_of: Lake
countries: United States
coordinates: lat: 47.363322
lon: -123.127485
The glacier continued to recede northward until it reached the Poulsbo channel. Here, the water level equalized to Glacial Lake Russell no longer having a separate identify. Lake Skokomish. Lake Skokomish formed in the depression of the Hood Canal and the Skokomish River. It drained across a southern divide at Shelton, Washington. When this outflow joined Lake Russell, it formed the Shelton Delta.

Geographic entities mentioned:
surface_form: lake skokomish
instance_of: Lake
countries: United States
coordinates: lat: 47.363322
lon: -123.127485
surface_form: hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
As the glacier receded northward, this freshwater lake grew in size, until the ice was north of the Clifton channel. With the opening of the Clifton channel, the water dropped to above sea level. This longer and lower level lake is referred to as Lake Hood. The glacier continued to recede northward until it reached the Poulsbo channel.

Geographic entities mentioned:
surface_form: hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
The Clifton Channel: The Clifton outlet channel is a definite feature across the divide on which it lies. It is deep at Lake Deborah in the col, above tide. This lake now drains both to Cases Inlet and Hood Canal. Gravel terraces exist along the channel, and one terrace on the east side continues as a small channel directly eastward to Cases Inlet.

Geographic entities mentioned:
surface_form: hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
At the seaward upper margin, it is above the Sound. Its altitude makes it obviously a feature produced subsequent to Lake Hood, whose waters were higher. The Poulsbo Channel: The Kitsap County peninsula between Hood Canal and Admiralty Inlet is sufficiently high to have confined Lake Hood as far north as Breidablik, northwest of Dogfish (Liberty) Bay.

Geographic entities mentioned:
surface_form: hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
At the seaward upper margin, it is above the Sound. Its altitude makes it obviously a feature produced subsequent to Lake Hood, whose waters were higher. The Poulsbo Channel: The Kitsap County peninsula between Hood Canal and Admiralty Inlet is sufficiently high to have confined Lake Hood as far north as Breidablik, northwest of Dogfish (Liberty) Bay.

Geographic entities mentioned:
surface_form: hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
surface_form: hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
Lack of Vashon Deltas of Olympic Rivers
The Olympic Mountains have several streams leading into Hood Canal, which have no valley deltas at the levels of the glacial lakes. The valley of Quilcene River has a long gravel slope gradually descending from levels above Lake Russell to tidewater. The Duckabush Valley, the Hama Hama and Skokomish rivers show no evidence of glacially derived deltas.

Geographic entities mentioned:
surface_form: hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
The Duckabush Valley, the Hama Hama and Skokomish rivers show no evidence of glacially derived deltas. It appears the later erosion regraded the Pleistocene gravels of these valleys. Lake Hood. The second and lower stage of this water body formed when the ice was far enough north to open the Clifton outlet. It continued until the glacier reached the Poulsbo Channel.

Geographic entities mentioned:
surface_form: hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
Tibetan independence ended with the Chinese invasion of 1950, which resulted in an exodus of Tibetans. In the 21st century, Tibetan Buddhism continues to have adherents on the Tibetan Plateau and in surrounding regions, while it has also attracted a considerable interest in the Western world. Pre 6th century.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
The Sakya Imperial Preceptors were active at the Yuan court and enjoyed special power. During this period Tibetan Buddhism was practiced not only within the capital Beijing and the Tibetan Plateau, but throughout the country.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
For instance, Hangzhou, capital of the former Southern Song dynasty and the largest city in the Yuan realm, became an important hub of the activities of Tibetan Buddhism, which took public or official precedence over Han Chinese Buddhism. Similarly, Mount Wutai, the sacred site of Bodhisattva Manjusri and the holy mountain of Chinese Buddhist pilgrims, was greatly influenced by Tibetan Buddhism.

Geographic entities mentioned:
surface_form: Mount Wutai
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 39.081388888889
lon: 113.56694444444
21st century – exile and spread abroad. Today, Tibetan Buddhism continues to thrive both within and outside the Tibetan Plateau. It remains the predominant religion in Tibet, Bhutan, and Mongolia, and has significant followings in northern Nepal, the Indian regions of Sikkim, Ladakh, and Arunachal Pradesh, as well as in parts of Russia such as Kalmykia, Tuva, and Buryatia.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Moreover, Tamazight has a greater amount of internal diversity than Shilha. Tamazight's dialects are divided into three distinct subgroups and geographic regions: those spoken in the Middle Atlas mountains; those spoken in the High Atlas mountains; and those spoken in Jbel Saghro and its foothills.

Geographic entities mentioned:
surface_form: Jbel Saghro
instance_of: Mountain
countries: Morocco
coordinates: lat: 31.14318
lon: -5.64412
Although the characteristic spirantization of >; > or; >; > or; and >, or is apparent in Berber languages in central and northern Morocco and Algeria, as in many Middle Atlas dialects, it is more rare in High Atlas Tamazight speakers, and is absent in Tamazight speakers from the foothills of Jbel Saghro. Southern dialects (e.g.

Geographic entities mentioned:
surface_form: Jbel Saghro
instance_of: Mountain
countries: Morocco
coordinates: lat: 31.14318
lon: -5.64412
In his youth he learned to fly glider aircraft. He made his first flights at the glider school in Grunau in Silesia, present-day Jeżów Sudecki, Poland. Here, among others, he was taught to fly by Hanna Reitsch. He was also trained by Wolf Hirth on the Hornberg in the Black Forest, and by Heini Dittmar and Oskar Ursinus at the Wasserkuppe in the Rhön Mountains.

Geographic entities mentioned:
surface_form: Wasserkuppe
instance_of: Mountain
countries: Germany
coordinates: lat: 50.498055555556
lon: 9.9377777777778
National Bison Range herd. The National Bison Range herd of American bison in Flathead Valley of the U.S. state of Montana consisted of about 300-500 of these animals. The management was transferred from the U.S. Fish and Wildlife Service to the Confederated Salish and Kootenai Tribes in 2021.

Geographic entities mentioned:
surface_form: Flathead Valley
instance_of: Valley
countries: United States
coordinates: lat: 48
lon: -114
Geographic range. &quot;L. fabiani&quot; is endemic to the Salar de Atacama, the Atacama salt flat, in northern Chile. The species was first described by José L. Yáñez and Herman Núñez in 1983, from a sample collected at a high elevation, near San Pedro de Atacama in Llano de Vilama in September 1981 by the Chilean National Museum of Natural History. Habitat.

Geographic entities mentioned:
surface_form: Salar de Atacama
instance_of: Lake
Body of water
countries: Chile
coordinates: lat: -23.416666666666668
lon: -68.26666666666667
Mont Margériaz. Mont Margériaz is a mountain of Savoie, France. It lies in the Bauges range. It has an elevation of above sea level.

Geographic entities mentioned:
surface_form: mont margériaz
instance_of: Mountain
countries: France
coordinates: lat: 45.63583333
lon: 6.03444444
At that time, it was considered to be the most ambitious winter hauling enterprise ever undertaken in Canada. Power for construction was supplied by two small turbines at a temporary hydro-electric plant and dam at Spruce Falls on Swan River, about down river (east), where Chicken and Kipahigan Lakes drain into the Sisipuk Lake of the Churchill River.

Geographic entities mentioned:
surface_form: Chicken
instance_of: Lake
countries: Canada
coordinates: lat: 55.51907
lon: -101.96046
surface_form: Kipahigan Lake
instance_of: Lake
countries: Canada
coordinates: lat: 55.313333333333
lon: -101.84333333333
Rindge is located in a hilly upland lake region. Hubbard Pond is in the northeast, Contoocook Lake on the northern boundary, Pearly Lake is in the northwest, and Lake Monomonac is on the southern boundary. The town is located on a regional watershed divide and is the headwaters for two river systems.

Geographic entities mentioned:
surface_form: Contoocook Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.786666666667
lon: -72.0125
surface_form: Pearly Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.7753
lon: -72.0603
The Contoocook River flows north to the Merrimack River, thence to the Gulf of Maine, and the North Branch of the Millers River flows southwest to the Connecticut River, thence to Long Island Sound. Rindge's highest point is on its eastern border, on the lower slopes of Pratt Mountain, where the elevation reaches above sea level.

Geographic entities mentioned:
surface_form: Pratt Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.7325
lon: -71.919444444444