Sarmila/GeoWiki-Features huggingface dataset:
Provincial park. The Kitsu Plateau lies at the southern end of Mount Edziza Provincial Park, a protected area founded in 1972 to showcase the volcanic landscape. This remote wilderness area of northwestern British Columbia is not accessible by motorized vehicles to help protect the very sensitive environment. Instead, access is mainly via aircraft or unmaintained hiking trails that cross creeks.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
From there, it enters Mount Edziza Provincial Park and continues another west along Bourgeaux Creek through Raspberry Pass. The telegraph trail then continues to the northwest through Raspberry Creek valley along the northern edge of the Kitsu Plateau for about to Mess Creek valley.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Only short segments of the Yukon Telegraph Trail are still passable, having been mostly overgrown since maintenance of the trail ended in 1936. The Kitsu Plateau can be accessed by float plane or helicopter, both of which are available for charter at the communities of Iskut and Dease Lake.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
The Kitsu Plateau can be accessed by float plane or helicopter, both of which are available for charter at the communities of Iskut and Dease Lake. Private aircraft are prohibited from landing on the Kitsu Plateau lava flows, but Mess Lake is large enough to be used by float-equipped aircraft.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
It means in the Tahltan language and was likely chosen due to the plateau's association with Kitsu Creek and Kitsu Peak, whose names were also adopted on January 2, 1980, on the National Topographic System maps 104G/10 and 104G/7, respectively. Provincial park.

Geographic entities mentioned:
surface_form: kitsu creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.51636
lon: -130.85398
Landforms. The Kitsu Plateau is dominated by the Mess Lake Lava Field, which extends from Raspberry Creek in the north to Nagha Creek in the south. It covers an area of around and contains three pyroclastic cones which were the sources of lava flows that travelled westward towards the Mess Creek Escarpment.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Raspberry Formation. The Raspberry Formation is exposed on the lower northern, western and southwestern sides of the Kitsu Plateau. It has an elevation of less than along the Mess Creek Escarpment and consists of flat-lying basaltic lava flows interbedded with scoria.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
More than of Raspberry lava flows are exposed in the Mess Creek Escarpment, most of which were erupted from a shield volcano that formed on a Late Miocene erosion surface. These lava flows travelled westward into the ancestral valley of Mess Creek and originated from vents north of Raspberry Pass which were subsequently buried under younger volcanic deposits.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Armadillo Formation. Basaltic lava flows of the 6.3-million-year-old Armadillo Formation are exposed on the northern side of the plateau and along the Mess Creek Escarpment on the western side of the plateau where they overlie basaltic lava flows of the Raspberry Formation. Armadillo basalt flows are interbedded with air-fall pumice and ash flows of trachytic and comenditic compositions.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Lava from the Swarm Peak eruptive centre is exposed along the Mess Creek Escarpment where it overlies till and glacial-fluvial gravel derived from the Armadillo Formation. Spectrum Formation.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Spectrum Formation. The Kounugu Member is overlain by the 3.1-million-year-old Spectrum Formation, which is exposed along the Mess Creek Escarpment on the western side of the plateau and at the southern and eastern ends of the plateau.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Alkali basalt flows from the two oldest pyroclastic cones in the Mess Lake Lava Field, ML-1 and ML-2, most likely cascaded over the Mess Creek Escarpment into Mess Creek valley, but no evidence of this phenomenon has been found on or below the escarpment.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
It was also the source of a hawaiitic lava flow that travelled to the northwest through Nagha Creek valley towards Mess Lake. Residual heat from The Ash Pit eruption may have resulted in the formation of the Mess Lake Hot Springs to the west in Mess Creek valley. Basement. As a part of the Mount Edziza volcanic complex, the Kitsu Plateau is underlain by the Stikinia terrane.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Provincial park. The Kitsu Plateau lies at the southern end of Mount Edziza Provincial Park, a protected area founded in 1972 to showcase the volcanic landscape. This remote wilderness area of northwestern British Columbia is not accessible by motorized vehicles to help protect the very sensitive environment. Instead, access is mainly via aircraft or unmaintained hiking trails that cross creeks.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Instead, access is mainly via aircraft or unmaintained hiking trails that cross creeks. Mount Edziza Provincial Park covers, making it one of the largest provincial parks in British Columbia. Hunting, camping, fishing, hiking, wildlife viewing and nature studying are some of the activities available in Mount Edziza Provincial Park.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Stratigraphy. The Kitsu Plateau is subdivided into at least five geological formations, each being the product of a distinct period of volcanic activity. These periods of volcanic activity occurred during three magmatic cycles of the Mount Edziza volcanic complex; each cycle began with the effusion of alkali basalt and culminated with the eruption of lesser volumes of felsic magma.

Geographic entities mentioned:
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
These volcanic rocks were deposited by eruptions during the Holocene and mainly comprise the Mess Lake Lava Field, one of the three Big Raven lava fields of the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
In some, such as the Pit River Tribe, they can signify good fortune in hunting. The Arapaho, originally settled in the Red River Valley, made extensive use of quillwork and continued to seek out quills through trade or long expeditions after forced migration to the Great Plains, where porcupines were scarce.

Geographic entities mentioned:
surface_form: Red River Valley
instance_of: Valley
countries: Canada
United States
coordinates: lat: 49
lon: -97.5
It shares the park with memorials honoring fallen soldiers. History. In the late 18th and early 19th centuries, the Potawatomi controlled a large territory around the southern portion of Lake Michigan, including this area. Around the turn of the century, Wahbememe (White Pigeon) was the chief of a village located west of here, near the St.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Hauser Kaibling. Hauser Kaibling is a ski area located within the Schladming-Dachstein ski area in the Ennstal Alps. Hauser Kaibling is part of the Schladminger 4-Berge-Schaukel, four connected mountains. The other three are Planai, Hochwurzen and Reiteralm (Styria), and they form the four highest mountains in Styria. The village of Haus im Ennstal is at the foot of Hauser Kaibling. Ski Lifts.

Geographic entities mentioned:
surface_form: Planai
instance_of: Mountain
countries: Austria
coordinates: lat: 47.392
lon: 13.694
surface_form: Hochwurzen
instance_of: Mountain
countries: Austria
coordinates: lat: 47.359925
lon: 13.639535
Hauser Kaibling. Hauser Kaibling is a ski area located within the Schladming-Dachstein ski area in the Ennstal Alps. Hauser Kaibling is part of the Schladminger 4-Berge-Schaukel, four connected mountains. The other three are Planai, Hochwurzen and Reiteralm (Styria), and they form the four highest mountains in Styria. The village of Haus im Ennstal is at the foot of Hauser Kaibling. Ski Lifts.

Geographic entities mentioned:
surface_form: dachstein
instance_of: Mountain
countries: Austria
coordinates: lat: 47.475168
lon: 13.605735
surface_form: hauser kaibling
instance_of: Mountain
countries: Austria
coordinates: lat: 47.3736
lon: 13.7786
Hauser Kaibling. Hauser Kaibling is a ski area located within the Schladming-Dachstein ski area in the Ennstal Alps. Hauser Kaibling is part of the Schladminger 4-Berge-Schaukel, four connected mountains. The other three are Planai, Hochwurzen and Reiteralm (Styria), and they form the four highest mountains in Styria. The village of Haus im Ennstal is at the foot of Hauser Kaibling. Ski Lifts.

Geographic entities mentioned:
surface_form: hauser kaibling
instance_of: Mountain
countries: Austria
coordinates: lat: 47.3736
lon: 13.7786
Mount Lawson (Alberta). Mount Lawson is a mountain located in the Kananaskis Range of Alberta. It was named in 1922 by Walter Wilcox and H.G. Bryant after Major W.E. Lawson, an employee with the Geological Survey of Canada who was killed in France during World War I.

Geographic entities mentioned:
surface_form: mount lawson (alberta)
instance_of: Mountain
countries: Canada
coordinates: lat: 50.7667
lon: -115.19
Mount Lawson (Alberta). Mount Lawson is a mountain located in the Kananaskis Range of Alberta. It was named in 1922 by Walter Wilcox and H.G. Bryant after Major W.E. Lawson, an employee with the Geological Survey of Canada who was killed in France during World War I.

Geographic entities mentioned:
surface_form: mount lawson
instance_of: Mountain
countries: Canada
coordinates: lat: 50.7667
lon: -115.19
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
St Leonards Salt Lagoon. St Leonards Salt Lagoon is a former marine embayment, isolated by coastal deposition from Port Phillip Bay, at St Leonards, Victoria, Australia. It now forms a shallow and hypersaline lake, of about, which is often dry. It is a Victorian Nature Reserve.

Geographic entities mentioned:
surface_form: st leonards salt lagoon
instance_of: Lake
countries: Australia
coordinates: lat: -38.158888888889
lon: 144.71111111111
After the war he resumed preaching. Early life and education. Checote was born in 1819 to a Muscogee family in the Chattahoochee Valley, traditional Creek territory. It is in present-day eastern Alabama, near the Georgia state line. He started school at the Asbury Manual Labor School, established by Methodist missionaries near Fort Mitchell, Alabama.

Geographic entities mentioned:
surface_form: Chattahoochee Valley
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Tin Mountain, Missouri. Tin Mountain is an unincorporated community in Madison County, in the U.S. state of Missouri. The community took its name from nearby Tin Mine Mountain.

Geographic entities mentioned:
surface_form: Tin Mine Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.51666667
lon: -90.41777778
Taku Plateau. The Taku Plateau is a sub-plateau of the Stikine Plateau in the far northwestern Interior of British Columbia, Canada. It lies to the south of the Teslin Plateau, part of the Yukon Plateau and to the southeast of the Yukon Plateau's other major sub-area within British Columbia, the Tagish Highland.

Geographic entities mentioned:
surface_form: Stikine Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: taku plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.7
lon: -132.5
Taku Plateau. The Taku Plateau is a sub-plateau of the Stikine Plateau in the far northwestern Interior of British Columbia, Canada. It lies to the south of the Teslin Plateau, part of the Yukon Plateau and to the southeast of the Yukon Plateau's other major sub-area within British Columbia, the Tagish Highland.

Geographic entities mentioned:
surface_form: Teslin Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 59.66666667
lon: -132.91666667
surface_form: Yukon Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 62.25
lon: -137.25
surface_form: teslin
instance_of: Lake
countries: Canada
coordinates: lat: 59.983333333333
lon: -132.41666666667
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: tagish
instance_of: Lake
countries: Canada
coordinates: lat: 59.71666666666667
lon: -134.23333333333332
surface_form: yukon plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 62.25
lon: -137.25
It lies to the south of the Teslin Plateau, part of the Yukon Plateau and to the southeast of the Yukon Plateau's other major sub-area within British Columbia, the Tagish Highland. Immediately northeast is the Kawdy Plateau and to the northwest of the Nahlin Plateau (both also components of the Stikine Plateau).

Geographic entities mentioned:
surface_form: Kawdy Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 59.24948
lon: -131.50356
surface_form: Nahlin Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.44972222222222
lon: -131.41833333333332
surface_form: stikine plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
Immediately northeast is the Kawdy Plateau and to the northwest of the Nahlin Plateau (both also components of the Stikine Plateau). The Inklin River forms the plateau's southwestern boundary with the northwestern extremities of the Tahltan Highland, beyond which are the Boundary Ranges. Very mountainous, its highest summit is Nahlin Mountain.

Geographic entities mentioned:
surface_form: Nahlin Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 58.8572
lon: -132.088
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Taku Plateau. The Taku Plateau is a sub-plateau of the Stikine Plateau in the far northwestern Interior of British Columbia, Canada. It lies to the south of the Teslin Plateau, part of the Yukon Plateau and to the southeast of the Yukon Plateau's other major sub-area within British Columbia, the Tagish Highland.

Geographic entities mentioned:
surface_form: taku plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.7
lon: -132.5
Linacre Reservoirs. Linacre Reservoirs is a series of three reservoirs on the western outskirts of Chesterfield, Derbyshire. The village of Old Brampton lies 500m to the south of the reservoirs. Linacre Lower Reservoir (storage capacity of 140 million litres, 9m deep) was built in 1855 following an Act of Parliament granting permission for its construction to supply drinking water to Chesterfield.

Geographic entities mentioned:
surface_form: linacre reservoirs
instance_of: Group of lakes
countries: United Kingdom
coordinates: lat: 53.249
lon: -1.509
Among its members were Noel Sandwith, curator at Kew Gardens, who first discovered &quot;Scorzonera humilis&quot;, or viper's grass, growing in Britain, botanist Eleanor Vachell who discovered &quot;Limosella aquatica x subulata&quot; in Glamorgan, and Gertrude Foggitt who recorded &quot;Carex microglochin&quot; on Ben Lawers, along with the botanist Lady Joanna Charlotte Davy.

Geographic entities mentioned:
surface_form: Ben Lawers
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.544922
lon: -4.22086
The Gorongosa team has reintroduced species to the ecosystem, worked with the Mozambican government to extend the park's boundaries to include Mount Gorongosa and planted more than three million trees on the mountain, created an international restoration ecology science research center, established eco-tourism in the park, and provides health and education programs to the local communities living near the park's borders.

Geographic entities mentioned:
surface_form: Mount Gorongosa
instance_of: Mountain
countries: Mozambique
coordinates: lat: -18.403888888889
lon: 34.10875
The Indian Nation lived along the banks of the Pequonnock River in the Pequonnock River Valley and also around the natural lake first called Mischa Lake, after the Indian chief who resided there, and now known as Pinewood Lake.

Geographic entities mentioned:
surface_form: Pinewood Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.256
lon: -73.176
Pine Brook Country Club. Benjamin Plotkin purchased Pinewood Lake and the surrounding acreage and built forty cabins and an auditorium with a revolving stage and incorporated as the Pine Brook Country Club in 1930. Plotkin's dream was to market the club as a summer resort for people to stay and enjoy theatrical productions.

Geographic entities mentioned:
surface_form: Pinewood Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.256
lon: -73.176
Kiceniuk began building hang gliders in 1971 while still in high school. At first he flew his gliders near Palomar Mountain where his father was curator of Palomar Observatory but later began flying at Torrey Pines Gliderport in La Jolla. He soon moved from the traditional Rogallo wing design to a rigid flying wing biplane design he called Icarus.

Geographic entities mentioned:
surface_form: Palomar Mountain
instance_of: Mountain
countries: United States
Mexico
coordinates: lat: 33.363483333333
lon: -116.83639444444
Sarana Valley. l75bf3cr7v6hex0uqtdas4t37jbu4" xml:space="preserve">Sarana Valley is a valley in the mountains of northeastern Attu Island in the Aleutian Islands in Alaska. The v-shaped valley extends northwest from Sarana Bay on Attu's east coast before angling northeast to Chichagof Harbor. Sarana Pass connects the valley to Holz Bay.

Geographic entities mentioned:
surface_form: Chichagof Harbor
instance_of: Landform
countries: United States
coordinates: lat: 52.9319
lon: 173.242
The v-shaped valley extends northwest from Sarana Bay on Attu's east coast before angling northeast to Chichagof Harbor. Sarana Pass connects the valley to Holz Bay. Attu Island was attacked and taken by Japanese forces six months after the attack on Pearl Harbor. In the course of retaking the Island, U.S.

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
Sarana Valley. l75bf3cr7v6hex0uqtdas4t37jbu4" xml:space="preserve">Sarana Valley is a valley in the mountains of northeastern Attu Island in the Aleutian Islands in Alaska. The v-shaped valley extends northwest from Sarana Bay on Attu's east coast before angling northeast to Chichagof Harbor. Sarana Pass connects the valley to Holz Bay.

Geographic entities mentioned:
surface_form: sarana valley
instance_of: Valley
countries: United States
coordinates: lat: 52.888
lon: 173.205
Sarana Pass connects the valley to Holz Bay. Attu Island was attacked and taken by Japanese forces six months after the attack on Pearl Harbor. In the course of retaking the Island, U.S. forces were surprised in the Sarana Valley by 800 Japanese soldiers in an unsuccessful offensive attempt. Retaking the island cost 1500 American lives and 4350 Japanese lives.

Geographic entities mentioned:
surface_form: sarana valley
instance_of: Valley
countries: United States
coordinates: lat: 52.888
lon: 173.205
Soil. The two important types of soils noticed in the district are black soils and lateritic soils. The entire district forms a part of the Deccan Plateau and is made up mostly of solidified lava. The northern part of the district is characterized by expanses of level and treeless surface punctuated here and there by flat and undulating hillocks, black soils and basaltic rocks.

Geographic entities mentioned:
surface_form: Deccan Plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Griffin Creek (Alberta). Griffin Creek is a stream in Alberta, Canada. Griffin Creek has the name of Thomas Griffin, a pioneer citizen.

Geographic entities mentioned:
surface_form: griffin creek (alberta)
instance_of: Watercourse
countries: Canada
coordinates: lat: 55.98337
lon: -117.8027
Griffin Creek (Alberta). Griffin Creek is a stream in Alberta, Canada. Griffin Creek has the name of Thomas Griffin, a pioneer citizen.

Geographic entities mentioned:
surface_form: griffin creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 55.98337
lon: -117.8027
Otherwise, Loudoun shares borders with the parishes of Avondale (east), Eaglesham (north), East Kilbride (north-east), Fenwick (north-west) and Kilmarnock (west). Within Loudoun can be found the towns of Darvel and Newmilns, alongside Loudoun Hill, Loudoun Castle, Loudoun Kirk and Loudoun Academy.

Geographic entities mentioned:
surface_form: Loudoun Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.614719444444
lon: -4.2116805555556
Etymology. Various theories have been put forward as to the origins of the name &quot;Loudoun&quot;. One such theory is that the name was originally used in reference to Loudoun Hill, being a combination of two Scots words &quot;law&quot; and &quot;dun&quot;, which roughly translates as &quot;Firehill&quot;.

Geographic entities mentioned:
surface_form: Loudoun Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.614719444444
lon: -4.2116805555556
The diet of the families included oysters and clams which were given to them from the Nisqually people. Support for the station also came from John McLoughlin, who ordered donations of peas and flour along with the loaning of milk cows. Richmond attended the celebration of the Fourth of July at American Lake held by the visiting United States Exploring Expedition in 1841.

Geographic entities mentioned:
surface_form: American Lake
instance_of: Lake
countries: United States
coordinates: lat: 47.13
lon: -122.567
Its natural habitat is freshwater lakes. It was previously listed as Endangered in 1996, in 2004 it was changed to Data Deficient, and in 2018 it was changed to Critically Endangered. It is threatened by fishing of Lake Malawi and by lakeside deforestation which may cause sedimentation through soil erosion. A small portion may be protected by one national park, in which fishing is not allowed.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
It is headquartered at Kohima, which is at an altitude of above sea level. Mount Japfü at elevation of, the highest peak in the district is located in the Southern Angami Region of the district. Flora and fauna. In 1980, Kohima District became home to the Pulie Badze Wildlife Sanctuary, which has an area of. It is a natural habitat for Blyth’s Tragopan. Administration.

Geographic entities mentioned:
surface_form: Mount Japfü
instance_of: Mountain
countries: India
coordinates: lat: 25.598205
lon: 94.068051
Sacramento Wash (California). The Sacramento Wash (California) is the drainage southward, then east from the Lanfair Valley of extreme eastern San Bernardino County, California. The drainage combines with the Piute Wash-(mostly of Nevada) at the south terminus of the Dead Mountains, and immediately enters the Colorado River, just north of Needles, California.

Geographic entities mentioned:
surface_form: Lanfair Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.2889
lon: -115.103
The Sacramento Wash turns eastward, combines with other bajada drainages from the west and south, and merges with the Piute Wash, to rapidly descend down from the foothills of the Dead Mountains to the western bank of the Colorado River. The approximate center of the Sacramento Wash drainage is the center of Lanfair Valley, the Lanfair Buttes.

Geographic entities mentioned:
surface_form: Lanfair Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.2889
lon: -115.103
surface_form: Lanfair Buttes
instance_of: Mountain
countries: United States
coordinates: lat: 35.1525
lon: -115.15222222
Together with Tour du Marboré, the Cascade Peaks, and Pic de Marboré, it forms the range above Cirque de Gavarnie (1,500 m above the bottom of the valley marking the border between the Pyrenees National Park (France) and the Ordesa y Monte Perdido National Park, Ordesa Valley), Spain.), The 422 m high &quot;Gavarnie falls&quot;, the biggest waterfall in Europe, descends from Casque du Marboré.

Geographic entities mentioned:
surface_form: Tour du Marboré
instance_of: Mountain
countries: Spain
France
coordinates: lat: 42.6856
lon: -0.01722
surface_form: Cascade Peaks
instance_of: Mountain
countries: France
Spain
coordinates: lat: 42.6867
lon: 0.00222222
surface_form: Pic de Marboré
instance_of: Mountain
countries: Spain
France
coordinates: lat: 42.6928
lon: 0.01167
surface_form: Ordesa Valley
instance_of: Valley
countries: Spain
coordinates: lat: 42.648611111111
lon: -0.058055555555556
surface_form: marboré
instance_of: Mountain
countries: Spain
France
coordinates: lat: 42.6928
lon: 0.01167
surface_form: marboré
instance_of: Mountain
countries: Spain
France
coordinates: lat: 42.6928
lon: 0.01167
surface_form: marboré
instance_of: Mountain
countries: Spain
France
coordinates: lat: 42.6928
lon: 0.01167
surface_form: pic de marboré
instance_of: Mountain
countries: Spain
France
coordinates: lat: 42.6928
lon: 0.01167
surface_form: casque du marboré
instance_of: Mountain
countries: Spain
France
coordinates: lat: 42.6881
lon: -0.02667
Access. Access from Spain is possible up until the prairies of Ordesa Valley, or up till Bujaruelo valley,From France, one needs to travel to Gavarnie-Gèdre skiing resort, the nearest area to the summit.

Geographic entities mentioned:
surface_form: Ordesa Valley
instance_of: Valley
countries: Spain
coordinates: lat: 42.648611111111
lon: -0.058055555555556
Casque du Marboré. The Casque du Marboré, or Casque de Gavarnie or simply le Casque, is a Pyrenean summit, culminating at, located on the crest of three-thousanders in the Monte Perdido Range above Cirque de Gavarnie on the Franco-Spanish border. Toponymy. The term &quot;casque&quot; (a helmet) was applied to the peak due to its particular shape.

Geographic entities mentioned:
surface_form: marboré
instance_of: Mountain
countries: Spain
France
coordinates: lat: 42.6928
lon: 0.01167
surface_form: casque du marboré
instance_of: Mountain
countries: Spain
France
coordinates: lat: 42.6881
lon: -0.02667
Toponymy. The term &quot;casque&quot; (a helmet) was applied to the peak due to its particular shape. The word &quot;marboré&quot; means marble, which is a metamorphic rock found in the area. Topography.

Geographic entities mentioned:
surface_form: marboré
instance_of: Mountain
countries: Spain
France
coordinates: lat: 42.6928
lon: 0.01167
From Ordesa, a 4 hour long upward journey is needed to reach the Goriz refuge (2,190 m ~ base camp needed to explore the area) and then follow the path which leads to la Brèche de Roland, before arriving at the pass located between la tour du Marboré and le Casque, from which one starts the final ascension.

Geographic entities mentioned:
surface_form: marboré
instance_of: Mountain
countries: Spain
France
coordinates: lat: 42.6928
lon: 0.01167
surface_form: tour du marboré
instance_of: Mountain
countries: Spain
France
coordinates: lat: 42.6856
lon: -0.01722
Allentown School District. The Allentown School District is a large, urban public school district located in Allentown, Pennsylvania in the Lehigh Valley region of eastern Pennsylvania. The district is the fourth-largest school district in Pennsylvania as of the 2016-17 school year. The district includes almost all of Allentown, the third-largest city in Pennsylvania.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Between Helmsdale and Kinbrace the road is in Strath Ullie (known also as Strath of Kildonan). The River Ullie (known also as the River Helmsdale) reaches the sea at Helmsdale. Between Forsinard and Halladale Bridge the road is in Strath Halladale. The River Halladale reaches the sea near Melvich. In 2016 the road was declared the quietest A road in Britain.

Geographic entities mentioned:
surface_form: Strath Halladale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 58.46667
lon: -3.88333
Being pro-British, Petrakogiorgis had close ties with EOK and SOE. He had the code-name Selfridge because, in Beevor's words, &quot;his olive mill was Crete's closest approximation to big business&quot;. Petrakogiorgis' group, named &quot;Psiloritis&quot;, was active in the regions of Mt. Ida, the Mesara Plain, Mt.

Geographic entities mentioned:
surface_form: Mt. Kedros
instance_of: Mountain
countries: Greece
coordinates: lat: 35.181666666667
lon: 24.6175
surface_form: Amari Valley
instance_of: Valley
countries: Greece
coordinates: lat: 35.22
lon: 24.64
Phippsfjellet. Phippsfjellet is a mountain on Prins Karls Forland, Svalbard. It has a height of 1,013 m.a.s.l. and is located on the ridge of Grampianfjella. The mountain is named after British Arctic explorer and naval officer Constantine Phipps, 2nd Baron Mulgrave. Further southeast on the ridge is the mountain of Phippsaksla.

Geographic entities mentioned:
surface_form: Grampianfjella
instance_of: Mountain
countries: Norway
coordinates: lat: 78.6239
lon: 10.9408
Phippsfjellet. Phippsfjellet is a mountain on Prins Karls Forland, Svalbard. It has a height of 1,013 m.a.s.l. and is located on the ridge of Grampianfjella. The mountain is named after British Arctic explorer and naval officer Constantine Phipps, 2nd Baron Mulgrave. Further southeast on the ridge is the mountain of Phippsaksla.

Geographic entities mentioned:
surface_form: phippsfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 78.6392
lon: 10.9464
Mweka, Democratic Republic of the Congo. Mweka is a town in southern-central Democratic Republic of the Congo, situated on the Kasai railway line between Kananga (250 km away) and the Kasai River port of Ilebo (172 km away).

Geographic entities mentioned:
surface_form: Kasai River
instance_of: Watercourse
countries: Angola
Democratic Republic of the Congo
coordinates: lat: -10.9603
lon: 19.3156
Bolmen. Bolmen () is a lake in Småland, Sweden. Covering 184 km2, and with a maximum depth of 37 m, it supplies a considerable part of Skåne with fresh water by means of an 82-km long tunnel, the Bolmen Water Tunnel, built during the 1970s and 80s. Bolmen is situated at the heart of Finnveden, one of the &quot;small lands&quot; of today's Småland. It is the tenth largest lake in Sweden.

Geographic entities mentioned:
surface_form: bolmen
instance_of: Lake
countries: Sweden
coordinates: lat: 56.916666666667
lon: 13.666666666667
Aster Glacier. Aster Glacier () is an Antarctic glacier descending the east slope of Craddock Massif and flowing between Elfring Peak and Willis Ridge to Thomas Glacier in the Sentinel Range, Ellsworth Mountains in Antarctica.

Geographic entities mentioned:
surface_form: Elfring Peak
instance_of: Mountain
coordinates: lat: -78.5833
lon: -84.9667
It was named by the Advisory Committee on Antarctic Names in 2006, after Richard Aster, Professor of Geophysics at Colorado State University, whose research in Antarctica includes volcanological studies at the Mount Erebus volcano observatory on Ross Island, glaciological, oceanic, and tectonic seismic source studies, seismic tomography, ice shelf studies, and the coupling of solid Earth geophysics and Antarctic ice sheet evolution.

Geographic entities mentioned:
surface_form: Mount Erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
The village needs to provide a safe way of landing fish and securing boats when they are not in use. Fishing villages may operate from a beach, particularly around lakes. For example, around parts of Lake Malawi, each fishing village has its own beach. If a fisherman from outside the village lands fish on the beach, he gives some of the fish to the village headman.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
Other fishing villages are built on floating islands, such as the Phumdi on Loktak Lake in India, and the Uros on Lake Titicaca which borders Peru and Bolivia. Apart from catching fish, fishing villages often support enterprises typically found in other types of village, such as village crafts, transport, schools and health clinics, housing and community water supplies.

Geographic entities mentioned:
surface_form: Loktak Lake
instance_of: Lake
countries: India
coordinates: lat: 24.55
lon: 93.783333333333
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
These peoples were settled on the shores around of Lake Titicaca. It is documented that these spinners and embroiderers had a presence in Puno, and that part of this community migrated to Lima: &quot;... the characteristic hat of that time had a rectangular shape, there was the Kullawa Achachi, later these embroiderers went to Lima and not I know more about them&quot;.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
The trout are continually being stocked biannually to supplement the naturalised population. Brook trout were first introduced to the Cub Hills in 1934 with the stocking of McDougal and Lost Echo Creeks. Since then, the fish have been introduced to 25 rivers in the hills with five of those rivers now supporting populations of naturalised, self-sustaining feral brook trout.

Geographic entities mentioned:
surface_form: McDougal
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.1738249
lon: -103.7801105
Since then, the fish have been introduced to 25 rivers in the hills with five of those rivers now supporting populations of naturalised, self-sustaining feral brook trout. The other rivers include Nipekamew Creek and Mossy River. All seven of Saskatchewan's trout species can be found in the Cub Hills.

Geographic entities mentioned:
surface_form: Mossy River
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.0166775
lon: -102.6459824
Flowering occurs from May to September and the fruit is a slightly flattened triangular pod long. Taxonomy. &quot;Daviesia nudiflora&quot; was first formally described in 1844 by Carl Meissner in Lehmann's &quot;Plantae Preissianae&quot; from specimens collected near Lake Monger in 1839. The specific epithet (&quot;nudiflora&quot;) means &quot;naked-flowered&quot;. Distribution and habitat.

Geographic entities mentioned:
surface_form: Lake Monger
instance_of: Lake
countries: Australia
coordinates: lat: -31.9294
lon: 115.8265
The excavations, between 1977 and 1988, were directed by the archaeologist Amnon Ben-Tor. Some of the digs were also headed by Renate Rosenthal and Yuval Portugali. Two other sites were studied in that project: Tel Qashish and Tel Qiri. Further excavations were conducted on the acropolis by Miriam Avissar in 1993. Today. there is an archaeological park and a visitor center on the mound.

Geographic entities mentioned:
surface_form: Tel Qashish
instance_of: Mountain
countries: Israel
coordinates: lat: 32.6845
lon: 35.109
surface_form: tel qashish
instance_of: Mountain
countries: Israel
coordinates: lat: 32.6845
lon: 35.109
The site name appears in 19th century sources as a variant, Tell Qamun, which was probably the local Arab name. Geography. Tel Yokneam is located in the western Jezreel Valley. The region's abundant water, moderate climate, and fertile soils allow inhabitants to grow a variety of crops in the valley and herd cattle on the slopes of the Menashe Heights and Mount Carmel.

Geographic entities mentioned:
surface_form: Jezreel Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
This location, at the crossroads of significant trade routes, is the main reason for Yokneam's continuous settlement over some four millennia. Approximately north and south respectively are Tel Qashish and Tel Qiri, other village sites believed to have been dependencies of Yokneam. History and archaeology.

Geographic entities mentioned:
surface_form: Tel Qashish
instance_of: Mountain
countries: Israel
coordinates: lat: 32.6845
lon: 35.109
Finds include bowls, platters, cooking pots, and jars that date from the entire period (3300–2100 BCE). A cylinder seal with a geometric motif, and a stamped seal were also found. Most of the finds correspond to the Early Bronze Age layer of the nearby Tel Qashish. An Egyptian vessel made of diorite, was discovered on top of the mound in the 1930s.

Geographic entities mentioned:
surface_form: Tel Qashish
instance_of: Mountain
countries: Israel
coordinates: lat: 32.6845
lon: 35.109
The end of this period in the city's history came with the Assyrian invasion under king Tiglath-Pileser III, in 732 BCE. At the time of this occupation, Yokneam was one of the largest cities in the Jezreel Valley. After this phase only a small settlement remained, and the fortifications were no longer in use.

Geographic entities mentioned:
surface_form: Jezreel Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
The statue is dated to the 9th century BCE, the time of the northern Kingdom of Israel. It shows Phoenician influence, and is the only one of its kind found in Israel to date. Also exhibited is a ritual vessel from the nearby Tel Qashish, dating from the Late Bronze Age. The visitor center was opened during Passover, 2019.

Geographic entities mentioned:
surface_form: Tel Qashish
instance_of: Mountain
countries: Israel
coordinates: lat: 32.6845
lon: 35.109
In modern terms, the ridge road or &quot;Way of the Patriarchs&quot; largely corresponds to Highway 60, the ancient route connecting it via Ta'anakh, Megiddo, and Yokneam with the coast is now followed by the Jenin-Haifa road (Highway 66 for the first section), and the pass road entering the Jezreel Valley at Yokneam is now Highway 70.

Geographic entities mentioned:
surface_form: jezreel
instance_of: Mountain
countries: Israel
coordinates: lat: 32.557852777778
lon: 35.327952777778
surface_form: jezreel valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
Nothing is known of Balian's doings in Caymont, but as he was a prominent leader it is plausible that he made a significant contribution to the site. After the initial Crusader victory at Damietta, the Franks of Acre attempted to attack the Muslims, but were defeated near Caymont by the sultan of Damascus, Al-Mu'azzam Isa.

Geographic entities mentioned:
surface_form: caymont
instance_of: Mountain
countries: Israel
coordinates: lat: 32.6640988
lon: 35.1082661
Tel Yokneam. Tel Yokneam, also spelled Yoqne'am or Jokneam (), is an archaeological site located in the northern part of the modern city of Yokneam Illit, Israel. It is known in Arabic as Tell Qamun (), believed to be a corruption of the Hebrew name. The site is an elevated mound, or tell, spanning around 40 dunams (10 acres/4 ha) and rising steeply to a height of.

Geographic entities mentioned:
surface_form: tel yokneam
instance_of: Mountain
countries: Israel
coordinates: lat: 32.6640988
lon: 35.1082661
With a few brief interruptions, Yokneam was occupied for 4,000 years, from the Middle Bronze Age to the Ottoman period. The ancient settlement at Tel Yokneam is first mentioned in Egyptian sources as a city conquered by Pharaoh Thutmose III. It appears later in the Hebrew Bible as a city defeated by Israelite leader Joshua and settled by the Tribe of Levi. It is mentioned twice in Roman sources.

Geographic entities mentioned:
surface_form: tel yokneam
instance_of: Mountain
countries: Israel
coordinates: lat: 32.6640988
lon: 35.1082661
The city was protected at that time by a massive fortification system. During Persian rule (539–330 BC) Yokneam was a dense, unfortified, and cosmopolitan city, housing Jews, Phoenicians, and Persians. Very little has been found in Yokneam from the Hellenistic, Roman, and Byzantine periods (333 BCE–634 CE), because the settlement was probably located on a different hill, south of Tel Yokneam.

Geographic entities mentioned:
surface_form: tel yokneam
instance_of: Mountain
countries: Israel
coordinates: lat: 32.6640988
lon: 35.1082661
Conder understands the name &quot;Cain Mons&quot; (i.e.: Caymont) as a corruption of &quot;Keimûn&quot;. History of archaeological excavation. Tel Yokneam was first surveyed in 1878 by Claude Reignier Conder of the Palestine Exploration Fund. It was later surveyed by Avner Raban, in the 1970s.

Geographic entities mentioned:
surface_form: tel yokneam
instance_of: Mountain
countries: Israel
coordinates: lat: 32.6640988
lon: 35.1082661
It appears later in the Hebrew Bible as a city defeated by Israelite leader Joshua and settled by the Tribe of Levi. It is mentioned twice in Roman sources. During the Crusades, it was called Caymont, or Cain Mons, recalling a legend that Yokneam was the site of Cain's death. For a period, it was the center of the Lordship of Caymont, the smallest seigneurie of the Crusader kingdom of Jerusalem.

Geographic entities mentioned:
surface_form: caymont
instance_of: Mountain
countries: Israel
coordinates: lat: 32.6640988
lon: 35.1082661
It is mentioned twice in Roman sources. During the Crusades, it was called Caymont, or Cain Mons, recalling a legend that Yokneam was the site of Cain's death. For a period, it was the center of the Lordship of Caymont, the smallest seigneurie of the Crusader kingdom of Jerusalem. The earliest archaeological features of Yokneam date from the Chalcolithic period, in the fourth millennium BCE.

Geographic entities mentioned:
surface_form: caymont
instance_of: Mountain
countries: Israel
coordinates: lat: 32.6640988
lon: 35.1082661
Yokneam is mentioned again, as &quot;Caymont&quot;, in a charter issued by King Baldwin IV of Jerusalem on 24 February 1182 granting a fief consisting of a few shops in Acre and 480 acres of land in the territory of Caymont (&quot;territorio de Caimont&quot;) to Joscelin III. By that time, Caymont was probably a lordship. The territory did not exceed.

Geographic entities mentioned:
surface_form: caymont
instance_of: Mountain
countries: Israel
coordinates: lat: 32.6640988
lon: 35.1082661
surface_form: caymont
instance_of: Mountain
countries: Israel
coordinates: lat: 32.6640988
lon: 35.1082661
The city was notable enough to be mentioned in the two detailed accounts recorded. One of these states that the site, along with others in the region, was plundered by the conquerors. Imad ad-Din al-Isfahani, Saladin's secretary, wrote that upon the fall of La Fève, Caymont surrendered like other Frankish localities.

Geographic entities mentioned:
surface_form: caymont
instance_of: Mountain
countries: Israel
coordinates: lat: 32.6640988
lon: 35.1082661
The Treaty of Jaffa, which ended the Third Crusade when it was signed on 2 September 1192, gave Qaymun and its lands to Balian of Ibelin, a prominent Frankish leader. Nothing is known of Balian's doings in Caymont, but as he was a prominent leader it is plausible that he made a significant contribution to the site.

Geographic entities mentioned:
surface_form: caymont
instance_of: Mountain
countries: Israel
coordinates: lat: 32.6640988
lon: 35.1082661
surface_form: caymont
instance_of: Mountain
countries: Israel
coordinates: lat: 32.6640988
lon: 35.1082661
After the initial Crusader victory at Damietta, the Franks of Acre attempted to attack the Muslims, but were defeated near Caymont by the sultan of Damascus, Al-Mu'azzam Isa. In a treaty signed during the Seventh Crusade, Caymont is listed among the castles that remained in Frankish hands. A lord of Caymont mentioned in 1253, Aymarri, is its last known lord.

Geographic entities mentioned:
surface_form: caymont
instance_of: Mountain
countries: Israel
coordinates: lat: 32.6640988
lon: 35.1082661
A lord of Caymont mentioned in 1253, Aymarri, is its last known lord. In 1256, Pope Alexander IV gave the destroyed monastery of Tabor, which included Caymont, to the Knights Hospitaller. An ownership dispute between the Hospitallers and the Knights Templar was resolved in May 1262, the Templars winning the territory.

Geographic entities mentioned:
surface_form: caymont
instance_of: Mountain
countries: Israel
coordinates: lat: 32.6640988
lon: 35.1082661
Sabyndykol falls within the perimeter of the Bayanaul National Park, a protected area. Geography. Sabyndykol lies in a small tectonic depression of the Kazakh Uplands, just below the slopes of Bayanaul Range, to the south of the eastern part of the mountains. It is the largest of the lakes of the range area, but Tuzkol, located to the southwest, is the largest of the district.

Geographic entities mentioned:
surface_form: Bayanaul Range
instance_of: Mountain
countries: Kazakhstan
coordinates: lat: 50.8
lon: 75.617
surface_form: sabyndykol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.766666666666666
lon: 75.7
Sabyndykol. Sabyndykol () is a lake in Bayanaul District, Pavlodar Region, Kazakhstan. The lake lies by the town of Bayanaul, located on the northern shore. Sabyndykol falls within the perimeter of the Bayanaul National Park, a protected area. Geography.

Geographic entities mentioned:
surface_form: sabyndykol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.766666666666666
lon: 75.7
It is the largest of the lakes of the range area, but Tuzkol, located to the southwest, is the largest of the district. The water of Sabyndykol is fresh. There are no big rivers flowing into the lake, only intermittent streams, the largest of which has its mouth in the northwestern shore. The lake has a maximum depth of to in the deepest areas.

Geographic entities mentioned:
surface_form: sabyndykol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.766666666666666
lon: 75.7
Sturgeon Creek (Washington). Sturgeon Creek is a stream in the U.S. state of Washington. Sturgeon Creek's name is an accurate preservation of its Indian name.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: sturgeon creek
instance_of: Watercourse
countries: United States
coordinates: lat: 48.0542635
lon: -122.1956937