Sarmila/GeoWiki-Features huggingface dataset:
Geography. The Snowshoe Lava Field is at the southern end of the Big Raven Plateau which is bounded by Mess Creek valley in the west, Kakiddi Creek valley in the east and the Klastline River valley in the north.

Geographic entities mentioned:
surface_form: Big Raven Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
surface_form: Mess Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: Kakiddi Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
This intermontane plateau is one of the principal physiographic features of the Mount Edziza volcanic complex, a group of overlapping shield volcanoes, stratovolcanoes, lava domes and cinder cones that have formed over the last 7.5 million years. The Snowshoe Lava Field reaches an elevation of on the plateau, but remnants of the lava field decrease in elevation to near Mess Creek.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
The Snowshoe Lava Field consists of more than of blocky lava flows that issued from 12 eruptive centres. Most of these eruptive centres are more than in elevation and are located on the southern and western flanks of Ice Peak, the prominent south peak of Mount Edziza. Cocoa Crater, Coffee Crater, Keda Cone, Tennena Cone and The Saucer are the only named eruptive centres in the Snowshoe Lava Field.

Geographic entities mentioned:
surface_form: Ice Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
The Snowshoe Lava Field consists of more than of blocky lava flows that issued from 12 eruptive centres. Most of these eruptive centres are more than in elevation and are located on the southern and western flanks of Ice Peak, the prominent south peak of Mount Edziza. Cocoa Crater, Coffee Crater, Keda Cone, Tennena Cone and The Saucer are the only named eruptive centres in the Snowshoe Lava Field.

Geographic entities mentioned:
surface_form: Cocoa Crater
instance_of: Mountain
countries: Canada
coordinates: lat: 57.65
lon: -130.7
surface_form: Coffee Crater
instance_of: Mountain
countries: Canada
coordinates: lat: 57.63
lon: -130.67
surface_form: Tennena Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.68416666666667
lon: -130.66222222222223
Cocoa Crater and Coffee Crater on the western and southern flanks of Ice Peak attain elevations of, respectively, and are so-named for their deep colours. Keda Cone, in elevation, is just south of Coffee Crater on the southern side of upper Taweh Creek. The Saucer is a low, circular mound of lava in elevation on the southern flank of Ice Peak bounded by concentric ridges of broken lava slabs.

Geographic entities mentioned:
surface_form: Taweh Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
Taweh Creek flows northwest along the southern edge of the lava field and is a tributary of Mess Creek. At the northwestern end of the Snowshoe Lava Field is Sezill Creek, a northwesterly flowing tributary of Taweh Creek. Shaman Creek at the southeastern end of the lava field flows east and north into Kakiddi Lake which is an expansion of Kakiddi Creek.

Geographic entities mentioned:
surface_form: Sezill Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.69967
lon: -130.88724
Taweh Creek flows northwest along the southern edge of the lava field and is a tributary of Mess Creek. At the northwestern end of the Snowshoe Lava Field is Sezill Creek, a northwesterly flowing tributary of Taweh Creek. Shaman Creek at the southeastern end of the lava field flows east and north into Kakiddi Lake which is an expansion of Kakiddi Creek.

Geographic entities mentioned:
surface_form: Shaman Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.61636
lon: -130.40395
surface_form: Kakiddi Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
As a part of the Mount Edziza volcanic complex, the Snowshoe Lava Field lies within a broad area of volcanoes and lava flows called the Northern Cordilleran Volcanic Province, which extends from northwestern British Columbia northwards through Yukon into easternmost Alaska.

Geographic entities mentioned:
surface_form: Northern Cordilleran Volcanic Province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
The Buckley Lake to Mowdade Lake Route traverses south from Buckley Lake along Buckley Creek and gradually climbs onto the northern end of the Big Raven Plateau where Tsekone Ridge and landforms of the Desolation Lava Field such as Eve Cone and Sidas Cone are visible along the route. Most of the Buckley Lake to Mowdade Lake Route is marked by a series of rock cairns from Tsekone Ridge onwards.

Geographic entities mentioned:
surface_form: Tsekone Ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 57.77
lon: -130.69
surface_form: Eve Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
surface_form: Sidas Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.8589
lon: -130.628
The structure of the world of tiers, with a central mountain or tower which the sun passes behind at night is equivalent to early Babylonian and Egyptian cosmological theories. The placement of the Lord's palace at the highest level of the world is reminiscent of the home of the gods atop Mount Olympus.

Geographic entities mentioned:
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
Dalton Iceberg Tongue. The Dalton Iceberg Tongue () is a large iceberg tongue that extends seaward from the eastern part of Moscow University Ice Shelf. The feature was partly delineated from air photos taken by U.S. Navy Operation Highjump (1946–47).

Geographic entities mentioned:
surface_form: dalton iceberg tongue
instance_of: Landform
coordinates: lat: -66.25
lon: 121.5
The station is owned by the Lincoln Broadcasting Company and maintains studios on Valley Drive in south suburban Brisbane. It shares a channel and transmitter with KDTV-DT (channel 14), owned by Univision, broadcasting from atop Mount Allison. Channel 26 was approved in 1965 but did not begin broadcasting until September 1976.

Geographic entities mentioned:
surface_form: Mount Allison
instance_of: Mountain
countries: United States
coordinates: lat: 37.4989
lon: -121.871
Meanwhile, the channel lay fallow, and KTSF-TV continued to exist only on paper, holding rights to begin broadcasting from the new Sutro Tower. However, the new station was instead built on San Bruno Mountain; Howell had been pushed out in the process of setting up the new facility. Early years and subscription television. KTSF began broadcasting on September 4, 1976.

Geographic entities mentioned:
surface_form: San Bruno Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6874
lon: -122.436
This was the third-highest payment to any San Francisco–market TV station. In the wake of the auction, KTSF entered into a channel-sharing agreement with Univision-owned KDTV-DT (channel 14), which broadcasts from Mount Allison. KDTV began broadcasting KTSF's subchannels on May 7, 2018. The KDTV–KTSF multiplex was then repacked from physical channel 51 to channel 20 on April 29, 2020. Programming.

Geographic entities mentioned:
surface_form: Mount Allison
instance_of: Mountain
countries: United States
coordinates: lat: 37.4989
lon: -121.871
Location. The McMahon Glacier forms in the Anare Mountains to the west of Tiger Peak and flows north past Buskirk Bluffs to the west and Gregory Bluffs to the east to enter the Nielsen Fjord, which leads to the Pacific Ocean. Cape North is at the west of the fjord's mouth, and the mouth of the Kirkby Glacier is at the east. Buskirk Bluffs. A sheer rock bluff on the west side of McMahon Glacier.

Geographic entities mentioned:
surface_form: Tiger Peak
instance_of: Mountain
coordinates: lat: -70.8667
lon: 165.967
The Middlebury River flows west to Otter Creek out of the mountains. Chipman Hill, a hill of glacial till, rises above the village just to the northeast. Foothills of the Green Mountains border the town to the east, with the Champlain Valley to the west. According to the United States Census Bureau, the town has a total area of, of which is land and, or 1.00%, is water.

Geographic entities mentioned:
surface_form: Champlain Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.45868
lon: -73.42617
Scranton School District (Pennsylvania). The Scranton School District is a large, urban school district located in Scranton, Pennsylvania in the Wyoming Valley region of northeastern Pennsylvania. It serves all of the city of Scranton in Lackawanna County, Pennsylvania. The district encompasses approximately 26 square miles.

Geographic entities mentioned:
surface_form: Wyoming Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
The municipality offers a wide variety of activities. The surrounding mountains such as Plasa, Čvrsnica and Prenj offer both hunting grounds and a variety of hiking trails. One popular hiking destination is &quot;Hajdučka Vrata&quot;, a natural wonder, the product of wind erosion, located 2,000 meters above sea level on the mountain of Čvrsnica.

Geographic entities mentioned:
surface_form: Čvrsnica
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.616666666667
lon: 17.616666666667
surface_form: Prenj
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.53480621248335
lon: 17.90430346491326
It has a carved oak case, copperplate script on ivory drawstops and a radiating and concave pedalboard. It was renovated in 1992 by J.M. Spinks of Leeds. Dinah Cautley (d.1910) donated the two-manual organ, which in its time was one of the largest in Nidderdale. Memorial plaques. There is a brass plaque presented by Lady Ingilby in memory of churchwarden George Lewis (d.1932).

Geographic entities mentioned:
surface_form: Nidderdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.0867
lon: -1.75773
Skull Valley (Utah). Skull Valley is a long valley located in east Tooele County, Utah, United States at the southwest of the Great Salt Lake. The valley trends north–south, but turns slightly northeast to meet Stansbury Bay, (adjacent Stansbury Island). Skull Valley's south and southwest borders the southeast Great Salt Lake Desert at Dugway and at a ridgeline southeast from the Cedar Mountains.

Geographic entities mentioned:
surface_form: long valley
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6833
lon: -115.722
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2767785
lon: -98.6946248
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 37.3789
lon: -112.573
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 44.965
lon: -96.443611111111
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.635555555556
lon: -99.9175
Skull Valley (Utah). Skull Valley is a long valley located in east Tooele County, Utah, United States at the southwest of the Great Salt Lake. The valley trends north–south, but turns slightly northeast to meet Stansbury Bay, (adjacent Stansbury Island). Skull Valley's south and southwest borders the southeast Great Salt Lake Desert at Dugway and at a ridgeline southeast from the Cedar Mountains.

Geographic entities mentioned:
surface_form: skull valley (utah)
instance_of: Valley
countries: United States
coordinates: lat: 40.5372
lon: -112.744
Skull Valley (Utah). Skull Valley is a long valley located in east Tooele County, Utah, United States at the southwest of the Great Salt Lake. The valley trends north–south, but turns slightly northeast to meet Stansbury Bay, (adjacent Stansbury Island). Skull Valley's south and southwest borders the southeast Great Salt Lake Desert at Dugway and at a ridgeline southeast from the Cedar Mountains.

Geographic entities mentioned:
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2767785
lon: -98.6946248
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 44.965
lon: -96.443611111111
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.635555555556
lon: -99.9175
Description. Skull Valley trends north-south but narrows slightly northeast towards Stansbury Bay; the Lakeside Mountains at Delle, and the northwest Stansbury Mountains at Timpie from the narrowing of the valley; Skull Valley and sections of the mountain ranges form the Great Salt Lake's southwest border. Skull Valley narrows southeastwards at the springs, as described.

Geographic entities mentioned:
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2767785
lon: -98.6946248
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: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 44.965
lon: -96.443611111111
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.635555555556
lon: -99.9175
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Skull Valley narrows southeastwards at the springs, as described. Bordering southwest here, is a southeast trending 16 mi long ridgeline from the west perimeter Cedar Mountains, which separates the Dugway Proving Grounds and the Great Salt Lake Desert region from the southwest Skull Valley. The valley's center is adjacent west of Iosepa.

Geographic entities mentioned:
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2767785
lon: -98.6946248
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 44.965
lon: -96.443611111111
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.635555555556
lon: -99.9175
The valley's center is adjacent west of Iosepa. A dissected region of sinks and flood land from neighboring washes and creeks form this valley center; this dissected flood land area is about four miles wide at its widest southwest of Iosepa, and extends seven miles northwards towards the beginning of areas of salt flats, associated with the Great Salt Lake.

Geographic entities mentioned:
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2767785
lon: -98.6946248
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 44.965
lon: -96.443611111111
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.635555555556
lon: -99.9175
Skull Valley (Utah). Skull Valley is a long valley located in east Tooele County, Utah, United States at the southwest of the Great Salt Lake. The valley trends north–south, but turns slightly northeast to meet Stansbury Bay, (adjacent Stansbury Island). Skull Valley's south and southwest borders the southeast Great Salt Lake Desert at Dugway and at a ridgeline southeast from the Cedar Mountains.

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
The Skull Valley Indian Reservation is located in the valley's south at the southwest foothills of the Stansbury Mountains; adjacent southeast, the valley narrows between the Stansbury Mountains and the Cedar Mountains at the west, a region of creeks from the Stansburys and valley springs, Willow Patch Springs and Scribner Spring.

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
Skull Valley narrows southeastwards at the springs, as described. Bordering southwest here, is a southeast trending 16 mi long ridgeline from the west perimeter Cedar Mountains, which separates the Dugway Proving Grounds and the Great Salt Lake Desert region from the southwest Skull Valley. The valley's center is adjacent west of Iosepa.

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
The two forces met in the Battle of Sarakhs, where Abu Sa'id emerged victorious. While Sultan Sanjar was captured and executed, Ala al-Dawla and his son escaped, though Ibrahim died only a few months later. Ala al-Dawla himself died in 1460, while in exile in the Caspian province of Rostamdar. He was buried in the Gawhar Shad Mausoleum complex in Herat.

Geographic entities mentioned:
surface_form: Caspian
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Similarly, Dr., who, as a judge and head of a delegation, contributed to keeping Morskie Oko within Poland's borders during a territorial dispute, donated over six morgs of land on the northern slope in 1910 to expand the park. The signing of the contract was announced on 12 May 1910. The annexed northern section was named after Fryderyk Chopin in 1910 to commemorate his centenary.

Geographic entities mentioned:
surface_form: Morskie Oko
instance_of: Lake
countries: Poland
coordinates: lat: 49.197222222222
lon: 20.070833333333
Kfar Monash objects were also dated, based on typological considerations, to EB IB, similarly to the axes from Tel Beth Shean. The study of Kfar Monash hoard indicated that some of them were made of unalloyed copper. The source of this unalloyed copper was found likely to be in Wadi Feynan, in southern Jordan. Such unalloyed copper was apparently mainly used for the production of tools.

Geographic entities mentioned:
surface_form: Wadi Feynan
instance_of: Valley
countries: Jordan
coordinates: lat: 30.62282
lon: 35.44775
Correspondingly his birth could have been between 590 and 615 if Somogyi's theory is correct. Legacy. Kubrat Knoll on Livingston Island in the South Shetland Islands, Antarctica is named after Kubrat of Great Bulgaria. Kubrat was portrayed by Vasil Mihaylov in the 1981 Bulgarian movie &quot;Aszparuh&quot;, directed by Ludmil Staikov.

Geographic entities mentioned:
surface_form: Kubrat Knoll
instance_of: Mountain
coordinates: lat: -62.5267
lon: -60.0181
Geographically, the Bosavi languages are situated to the east and south of the East Strickland group. They can be found around Mount Bosavi, located east of the Strickland River and southwest of the western edge of the central highlands of Papua New Guinea. Although no extensive subgrouping analysis has been conducted, Shaw's lexicostatistical study in 1986 provides some insights.

Geographic entities mentioned:
surface_form: Mount Bosavi
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -6.6141666666667
lon: 142.82666666667
Cause. The station is a U-shaped structure made of reinforced concrete. Half of its depth is embedded within the Musashino gravel stratum, underneath the Kantō loam on the surface. Within the Musashino gravel, the groundwater level varies greatly with rainfall. On the day of the flood, the groundwater had risen to less than 3m below the surface, its highest level in 75 years.

Geographic entities mentioned:
surface_form: Kantō loam
instance_of: Plateau
countries: Japan
McCaul's Pond. McCaul's Pond was located at the site of Hart House, on the University of Toronto campus. It was created by damming Taddle Creek in the early 1860s. Increased settlement and economic activity had already begun changing the creek from being the clear, free running watercourse that the early settlers had found.

Geographic entities mentioned:
surface_form: Taddle Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.67
lon: -79.3986
Hukkok (Hebrew חקק) is mentioned in the Hebrew Bible in. The International Standard Bible Encyclopaedia considers the identification of Hukkok with Yakuk as plausible, although it might be too far from Aznoth-tabor (possibly Khirbet el-Jebeil, c. 3 miles north of Mount Tabor) to fit the description. Bronze Age. The village site was inhabited in the Early and Middle Bronze Age.

Geographic entities mentioned:
surface_form: Mount Tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
It consisted of women who ran a form of early water taxi; rowing people between the islands of Stockholm, to and from the islands of the Stockholm archipelago, as well as to and from places around Lake Mälaren on the other side of Stockholm. History. The Stockholm rower women are mentioned in text from the 15th century, and in 1638 they formed a special group within the Swedish ferrymen guild.

Geographic entities mentioned:
surface_form: Lake Mälaren
instance_of: Lake
countries: Sweden
coordinates: lat: 59.5
lon: 17.2
History. The Stockholm rower women are mentioned in text from the 15th century, and in 1638 they formed a special group within the Swedish ferrymen guild. They handled most of the traffic over the waters of the capital, working in teams of two, taking passengers between its islands, into Lake Mälaren, and to and from islands in the Stockholm archipelago.

Geographic entities mentioned:
surface_form: Lake Mälaren
instance_of: Lake
countries: Sweden
coordinates: lat: 59.5
lon: 17.2
The Rheinradweg (Rhine Cycle Route) is an international cycle route, running from the source to the mouth of the Rhine, traversing four countries at a distance of. Another cycling tour runs towards Bingen and further to the Middle Rhine, a UNESCO World Heritage Site (2002). Air transportation.

Geographic entities mentioned:
surface_form: Middle Rhine
instance_of: Valley
countries: Germany
coordinates: lat: 50.364166666667
lon: 7.6055555555556
In this role, he conducted a number of expeditions to northern Queensland to collect native plants, including trips to Cape York Peninsula in 1862 and the north-east coast to Mossman and the Daintree River in 1873, climbing Mount Bellenden Ker.

Geographic entities mentioned:
surface_form: Mount Bellenden Ker
instance_of: Mountain
countries: Australia
coordinates: lat: -17.264166666667
lon: 145.85388888889
Morro das Pedras and Armação do Pântano do Sul lie in the southeast. The east contains the communities Barra da Lagoa, Lagoa da Conceição, Rio Tavares and Campeche. Other neighborhoods on the island include Carvoeira, Córrego Grande, Itacorubi, Pantanal, Parque São Jorge, and Santa Mônica. Conservation.

Geographic entities mentioned:
surface_form: Lagoa da Conceição
instance_of: Lake
countries: Brazil
coordinates: lat: -27.55
lon: -48.45
Peyote has also been used for several thousand years in the Rio Grande Valley in North America by native tribes as an entheogen. In the Andean region of South America, the San Pedro cactus (&quot;Trichocereus macrogonus&quot; var. &quot;pachanoi&quot;, syn. &quot;Echinopsis pachanoi&quot;) has a long history of use, possibly as a traditional medicine.

Geographic entities mentioned:
surface_form: Rio Grande Valley
instance_of: Valley
countries: United States
Mexico
coordinates: lat: 26.22
lon: -98.12
Mount Kineo. Mount Kineo is a prominent geological feature located on a peninsula that extends from the easterly shore of Moosehead Lake in the northern forest of Maine. With cliffs rising straight up from the water, it is the central feature of Mount Kineo State Park, a protected area of managed by the Maine Department of Agriculture, Conservation and Forestry. History.

Geographic entities mentioned:
surface_form: Moosehead Lake
instance_of: Lake
countries: United States
coordinates: lat: 45.633333333333
lon: -69.65
surface_form: mount kineo
instance_of: Mountain
countries: United States
coordinates: lat: 45.6997
lon: -69.7339
Mount Kineo. Mount Kineo is a prominent geological feature located on a peninsula that extends from the easterly shore of Moosehead Lake in the northern forest of Maine. With cliffs rising straight up from the water, it is the central feature of Mount Kineo State Park, a protected area of managed by the Maine Department of Agriculture, Conservation and Forestry. History.

Geographic entities mentioned:
surface_form: mount kineo
instance_of: Mountain
countries: United States
coordinates: lat: 45.6997
lon: -69.7339
The mechanical properties of the rhyolite on Mount Kineo exhibits the physical properties of flint and was used extensively by indigenous peoples to make arrowheads and implements and thus, has often been referred to as &quot;Kineo flint&quot; in literature; but this term misleads by implication that the rhyolite is a cryptocrystalline form of the mineral quartz derived from a sedimentary origin.

Geographic entities mentioned:
surface_form: mount kineo
instance_of: Mountain
countries: United States
coordinates: lat: 45.6997
lon: -69.7339
Features. The state park offers various trails around the peninsula and to the mountain peak. The park can only be reached by water. The Mount Kineo Golf Course operates the seasonal water shuttle service from the public dock in Rockwood to Mount Kineo. The park is one of five Maine State Parks that was in the path of totality for the 2024 solar eclipse, with 3 minutes and 24 seconds of totality.

Geographic entities mentioned:
surface_form: mount kineo
instance_of: Mountain
countries: United States
coordinates: lat: 45.6997
lon: -69.7339
Kineo for centuries to obtain this material. In 1846, Henry David Thoreau visited the Moosehead Lake region, and the mountain's geological formation, Indian relics and traditions deeply interested him. The first Mt. Kineo House was built on the shores of Moosehead Lake in 1848, but burned in 1868. Rebuilt in 1870 and opened in 1871, the second Mt. Kineo House burned again in 1882.

Geographic entities mentioned:
surface_form: moosehead
instance_of: Lake
countries: United States
coordinates: lat: 45.633333333333
lon: -69.65
Bric Ghinivert. Bric Ghinivert or Eiminàl (3,037 m a.s.l.) is a mountain of the Cottian Alps located in Italy. Geography. The mountain is the highest elevation of the water divide between Val Troncea (West) and Valle Germanasca (East).

Geographic entities mentioned:
surface_form: Valle Germanasca
instance_of: Valley
countries: Italy
coordinates: lat: 44.937044444444
lon: 7.1219361111111
surface_form: germanasca
instance_of: Valley
countries: Italy
coordinates: lat: 44.937044444444
lon: 7.1219361111111
Access to the summit. Easy routes to Bric Ghinivert start either from Val Troncea or from Val Germanasca; in both cases they do not require alpinistic skills but some scrambling. In the Italian scale of hiking difficulty is rated &quot;EE&quot; (&quot;Escursionisti Esperti&quot;, namely suitable for &quot;expert hikers&quot;).

Geographic entities mentioned:
surface_form: germanasca
instance_of: Valley
countries: Italy
coordinates: lat: 44.937044444444
lon: 7.1219361111111
surface_form: val germanasca
instance_of: Valley
countries: Italy
coordinates: lat: 44.937044444444
lon: 7.1219361111111
Bric Ghinivert. Bric Ghinivert or Eiminàl (3,037 m a.s.l.) is a mountain of the Cottian Alps located in Italy. Geography. The mountain is the highest elevation of the water divide between Val Troncea (West) and Valle Germanasca (East).

Geographic entities mentioned:
surface_form: eiminàl
instance_of: Mountain
countries: Italy
coordinates: lat: 44.9513
lon: 6.99103
surface_form: ghinivert
instance_of: Mountain
countries: Italy
coordinates: lat: 44.9513
lon: 6.99103
surface_form: bric ghinivert
instance_of: Mountain
countries: Italy
coordinates: lat: 44.9513
lon: 6.99103
Bric Ghinivert. Bric Ghinivert or Eiminàl (3,037 m a.s.l.) is a mountain of the Cottian Alps located in Italy. Geography. The mountain is the highest elevation of the water divide between Val Troncea (West) and Valle Germanasca (East).

Geographic entities mentioned:
surface_form: ghinivert
instance_of: Mountain
countries: Italy
coordinates: lat: 44.9513
lon: 6.99103
surface_form: bric ghinivert
instance_of: Mountain
countries: Italy
coordinates: lat: 44.9513
lon: 6.99103
Following northwards the ridge &quot;Colle del Beth&quot; (&quot;Beth Pass&quot;, 2783 m a.s.l.) divides Bric Ghinivert from &quot;Bric di Mezzogiorno&quot; (2,986 m a.s.l.), while going South &quot;Colle di Ghinivert&quot; (2,831 m a.s.l.) separates it from &quot;Monte Peolioso&quot; (2,886 m a.s.l.).

Geographic entities mentioned:
surface_form: ghinivert
instance_of: Mountain
countries: Italy
coordinates: lat: 44.9513
lon: 6.99103
surface_form: ghinivert
instance_of: Mountain
countries: Italy
coordinates: lat: 44.9513
lon: 6.99103
surface_form: bric ghinivert
instance_of: Mountain
countries: Italy
coordinates: lat: 44.9513
lon: 6.99103
Rongbuk Glacier. The Rongbuk Glacier () is located in the Himalaya of southern Tibet. Two large tributary glaciers, the East Rongbuk Glacier and the West Rongbuk Glacier, flow into the main Rongbuk Glacier. It flows north and forms the Rongbuk Valley north of Mount Everest. The famous Rongbuk Monastery is located at the northern end of the Rongbuk valley.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Mount Everest is the source of the Rongbuk Glacier and East Rongbuk Glacier. Discovery. The English climber George Mallory first explored the main Rongbuk Valley and its glacier while searching for possible routes to the summit of Mount Everest, during the first British Everest reconnaissance expedition of 1921. On the same expedition, Oliver Wheeler first explored the East Rongbuk Glacier.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
See 1921 British Reconnaissance Expedition. Route to Everest. Climbing expeditions attempting the normal route from Tibet use this glacier to reach the Advanced Base Camp of Mount Everest at the upper end of the East Rongbuk Glacier. From there, climbing expeditions try to summit Everest by the North Col and the northeast ridge. Environmental.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
See 1921 British Reconnaissance Expedition. Route to Everest. Climbing expeditions attempting the normal route from Tibet use this glacier to reach the Advanced Base Camp of Mount Everest at the upper end of the East Rongbuk Glacier. From there, climbing expeditions try to summit Everest by the North Col and the northeast ridge. Environmental.

Geographic entities mentioned:
surface_form: North Col
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 28.015833333333
lon: 86.925
According to the Syria Central Bureau of Statistics (CBS), Tell Dahab had a population of 660 in the 2004 census. History. Tell Dahab is one of several villages on the al-A'la plateau to contain Byzantine-era ruins. Greek inscriptions found on basalt lintels in the village date to 470, 489, 570 and 589 CE. In 1838, Tell Dahab's inhabitants were noted to be predominantly Sunni Muslims.

Geographic entities mentioned:
surface_form: al-A'la plateau
instance_of: Plateau
countries: Syria
coordinates: lat: 35.12833333333333
lon: 36.93333333333333
Before take-off. Flight 130 was scheduled to take off at around 12:00 p.m., heading to the Russian capital of Moscow with 115 passengers and 9 crew members. Most of the passengers were tourists who were heading home after their holiday in Lake Baikal. The flight would be commanded by Captain Gennady Padukov, and his co-pilot would be First Officer A. Zhavoronkov.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Germany. From Celtic ', s.f., 'alder'. (Compare the modern German Erlenbach) and Old High German (OHG) &quot;aha&quot;, s.n., 'flowing water'. Switzerland. Switzerland, especially the Swiss Plateau, has many Celtic (Gaulish) toponyms. This old layer of names was overlaid with Latin names in the Gallo-Roman period, and, from the medieval period, with Alemannic German and Romance names.

Geographic entities mentioned:
surface_form: Swiss Plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
Zarjoob. Zarjoob or Zarjoub (), in Gilan province, northern Iran, is a 41 km river that passes through the city of Rasht and empties into the Anzali Lagoon near the city of Bandar-e Anzali on the Caspian Sea. Pollution. Despite its short length, the Zarjoob watershed is home to about 1 million people and the river is heavily polluted.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
The lagoon is sometimes referred to as Elephant Pass Lagoon. The lagoon is fed by a number of small rivers from the south, including Kanakarayan Aru, Netheli Aru and Theravil Aru. It used to be linked to Jaffna Lagoon but since the construction of the causeway at Elephant Pass the lagoon has in effect been a lake. The lagoon's water is brackish.

Geographic entities mentioned:
surface_form: Kanakarayan Aru
instance_of: Watercourse
countries: Sri Lanka
Chundikkulam Lagoon. Chundikkulam Lagoon (,) is a lagoon in Jaffna District and Kilinochchi District, north-east Sri Lanka. The town of Chundikkulam is located on a narrow piece of land between the lagoon and the Indian Ocean. The lagoon is sometimes referred to as Elephant Pass Lagoon.

Geographic entities mentioned:
surface_form: chundikkulam lagoon
instance_of: Lake
countries: Sri Lanka
coordinates: lat: 9.4833333333333
lon: 80.5
Chief Mountain. Chief Mountain () () is located in the U.S. state of Montana on the eastern border of Glacier National Park and the Blackfeet Indian Reservation. The mountain is one of the most prominent peaks and rock formations along the Rocky Mountain Front, a overthrust fault, known as the Lewis Overthrust, which extends from central Montana into southern Alberta, Canada. Geology.

Geographic entities mentioned:
surface_form: chief mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.933833
lon: -113.610047
The mountain is one of the most prominent peaks and rock formations along the Rocky Mountain Front, a overthrust fault, known as the Lewis Overthrust, which extends from central Montana into southern Alberta, Canada. Geology. Chief Mountain is an example of a klippe. It consists of a Precambrian block which rests directly above much younger Cretaceous gray shales.

Geographic entities mentioned:
surface_form: chief mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.933833
lon: -113.610047
The surrounding portion of the thrust sheet has been removed by erosion leaving behind this and a few other isolated blocks of Proterozoic rock. History and significance. Chief Mountain has been a sacred mountain to the tribes of Native Americans in the United States and First Nations in Canada for hundreds of years. The Blackfoot name for the mountain is Nínaiistáko.

Geographic entities mentioned:
surface_form: chief mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.933833
lon: -113.610047
Elders from Southern Alberta's Siksika Band (where the Great Chief Crowfoot hailed from) and other First Nation groups have an oral tradition that near the end of days, a &quot;Great White God&quot; would appear from the top of Chief Mountain and upon his departure, the mountain would crumble and be destroyed. Climbing.

Geographic entities mentioned:
surface_form: chief mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.933833
lon: -113.610047
The Blackfoot name for the mountain is Nínaiistáko. The peak is easily seen from Montana and Alberta due to the rapid altitude gain over the Great Plains which are immediately east of the mountain. The mountain was seen by white explorers in the late 18th century and was known as &quot;Kings Peak&quot; on maps produced in the United Kingdom in 1795.

Geographic entities mentioned:
surface_form: kings peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.776388888889
lon: -110.37277777778
A 14-foot Christmas tree was also erected at the UST Grandstand where students placed their donations for the victims of the Mount Pinatubo eruption and Tropical Storm Uring (International name: Thelma) in Ormoc City. It was in 1993 that the celebration was formally named as Paskuhan. The celebration was a simple gathering spearheaded by the then UST Treasurer Fr. Tereso Campillo, O.P.

Geographic entities mentioned:
surface_form: Mount Pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
The highest point in the municipality is the tall mountain Helldalisen. Steigen has fertile lowlands in between the mountains and the sea. There are several archeological sites showing settlements from the Bronze Age, Iron Age, and Viking Age. Lakes in the region include Forsanvatnet, Hopvatnet, Makkvatnet, and Straumfjordvatnet. Climate.

Geographic entities mentioned:
surface_form: Hopvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 67.809444444444
lon: 15.728333333333
surface_form: Makkvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 67.83896
lon: 15.82501
surface_form: Straumfjordvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 67.887222222222
lon: 15.503333333333
Usually, a river or stream carves out such splits between mountains. Examples of mountain-type canyons are Provo Canyon in Utah or Yosemite Valley in California's Sierra Nevada. Canyons within mountains, or gorges that have an opening on only one side, are called box canyons. Slot canyons are very narrow canyons that often have smooth walls.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
It is slightly longer than Grand Canyon in the United States. Others consider the Kali Gandaki Gorge in midwest Nepal to be the deepest canyon, with a difference between the level of the river and the peaks surrounding it. Vying for the deepest canyon in the Americas is the Cotahuasi Canyon and Colca Canyon, in southern Peru. Both have been measured at over deep.

Geographic entities mentioned:
surface_form: Colca Canyon
instance_of: Valley
countries: Peru
coordinates: lat: -15.5972
lon: -72.0559
It is located under an ice sheet. At long, it is believed to be the longest canyon in the world. Despite not being quite as deep or long as Grand Canyon, the Capertee Valley in Australia is actually 1 km wider than Grand Canyon, making it the widest canyon in the world. Cultural significance. Some canyons have notable cultural significance.

Geographic entities mentioned:
surface_form: Capertee Valley
instance_of: Valley
countries: Australia
coordinates: lat: -33.0483
lon: 150.134
Attractions. The neighborhood is known as a shopping area for affordable, trendy clothes. It is also home to La Vega Central Market, a large marketplace principally known for selling fresh fruits and vegetables originating from the Chilean Central Valley. The neighborhood hosts a number of Arabic restaurants. as well as South Korean and Vietnamese cuisine.

Geographic entities mentioned:
surface_form: Chilean Central Valley
instance_of: Valley
countries: Chile
coordinates: lat: -35.5
lon: -71.5
Survival (manga). is a Japanese manga series written and illustrated by Takao Saito. It was serialized in Shogakukan's manga magazine &quot;Weekly Shōnen Sunday&quot; from September 1976 to December 1980, with its chapters collected in 22 volumes. A Remake titled, illustrated by Akira Miyagawa serialized in DeNA's manga app Manga Box from May 2015 to November 2016. Publication.

Geographic entities mentioned:
surface_form: DeNA
instance_of: Mountain
countries: Iran
coordinates: lat: 30.951666666667
lon: 51.4375
In France, &quot;Survival&quot; had been licensed by Editions Milan. A Remake of Ishinomori's manga titled &quot;Survival: Shōnen S no Kiroku&quot; illustrated by Akira Miyagawa began serialization in DeNA's manga app Manga Box on April 30, 2015. The first series finished serialization on November 21, 2018.

Geographic entities mentioned:
surface_form: DeNA
instance_of: Mountain
countries: Iran
coordinates: lat: 30.951666666667
lon: 51.4375
It is a side valley of the Dreisam valley and is heavily vegetated with mixed forest. It begins below the Rosskopf summit at an altitude of 463 m and ends in Freiburg's suburb Waldsee (forest lake) at an altitude of 320 m. There is also the Vogelsanghütte (birdsong hut). Pilgrimage.

Geographic entities mentioned:
surface_form: rosskopf
instance_of: Mountain
countries: Germany
coordinates: lat: 47.42599
lon: 10.43258
surface_form: rosskopf
instance_of: Mountain
countries: Germany
coordinates: lat: 48.0103
lon: 7.90167
Musbach valley. The Musbachtal is a small 2.6 km long steep and narrow carved valley with a creek at the bottom. Location and geography. The valley stretches from the Carthusian monastery in Freiburg im Breisgau (Baden-Württemberg, Germany) to below the summit of the Roßkopf (Black Forest). It is a side valley of the Dreisam valley and is heavily vegetated with mixed forest.

Geographic entities mentioned:
surface_form: roßkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 47.42599
lon: 10.43258
surface_form: roßkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 48.0103
lon: 7.90167
surface_form: württemberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.7821
lon: 9.26867
surface_form: roßkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 47.6567
lon: 11.8633
surface_form: roßkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 50.2583
lon: 8.52917
The valley stretches from the Carthusian monastery in Freiburg im Breisgau (Baden-Württemberg, Germany) to below the summit of the Roßkopf (Black Forest). It is a side valley of the Dreisam valley and is heavily vegetated with mixed forest. It begins below the Rosskopf summit at an altitude of 463 m and ends in Freiburg's suburb Waldsee (forest lake) at an altitude of 320 m.

Geographic entities mentioned:
surface_form: dreisam valley
instance_of: Valley
countries: Germany
coordinates: lat: 47.980555555555554
lon: 7.921666666666667
Musbach valley. The Musbachtal is a small 2.6 km long steep and narrow carved valley with a creek at the bottom. Location and geography. The valley stretches from the Carthusian monastery in Freiburg im Breisgau (Baden-Württemberg, Germany) to below the summit of the Roßkopf (Black Forest). It is a side valley of the Dreisam valley and is heavily vegetated with mixed forest.

Geographic entities mentioned:
surface_form: musbachtal
instance_of: Valley
countries: Germany
coordinates: lat: 48.0027
lon: 7.89917
Musbach valley. The Musbachtal is a small 2.6 km long steep and narrow carved valley with a creek at the bottom. Location and geography. The valley stretches from the Carthusian monastery in Freiburg im Breisgau (Baden-Württemberg, Germany) to below the summit of the Roßkopf (Black Forest). It is a side valley of the Dreisam valley and is heavily vegetated with mixed forest.

Geographic entities mentioned:
surface_form: musbach valley
instance_of: Valley
countries: Germany
coordinates: lat: 48.0027
lon: 7.89917
There is also the Vogelsanghütte (birdsong hut). Pilgrimage. The beginnings of the pilgrimage through the Musbach valley were between the 7th and the 13th centuries and it had its heyday in the 16th century. Through the lower part of the valley runs a way of the cross which ends at the end of the valley at the St. Odile chapel.

Geographic entities mentioned:
surface_form: musbach valley
instance_of: Valley
countries: Germany
coordinates: lat: 48.0027
lon: 7.89917
Gary Feulner and Binish Roobas also consider that may live in the southern Zagros Mountains of Iran. The holotype was found near Wadi Maydaq in 2006. Other examples were found locally and on Jebel Hafeet. &quot;Rafalus arabicus&quot; lives in the sparse vegetation found around the wadis that lie within the otherwise barren slopes of the Hajar Mountains.

Geographic entities mentioned:
surface_form: Jebel Hafeet
instance_of: Mountain
countries: United Arab Emirates
Oman
coordinates: lat: 24.05796
lon: 55.78086
Pennsylvania narrowly voted for Kennedy over the Republican nominee, Vice President Richard Nixon. Kennedy won Pennsylvania by a slim margin of 2.32%, being aided rather than hindered by his Catholic faith owing to the numerical power of his co-religionists in urban Philadelphia, Lackawanna County, and in the industrial areas around Lake Erie.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Feldberg (Kaiser). The Feldberg () is a mountain, in the Kaiser range in the Austrian state of Tyrol. Its summit may be ascended on an easy mountain path either directly from Griesenau or via the Stripsenjochhaus hut and the Stripsenkopf.

Geographic entities mentioned:
surface_form: Stripsenkopf
instance_of: Mountain
countries: Austria
coordinates: lat: 47.581944444444
lon: 12.308333333333
Feldberg (Kaiser). The Feldberg () is a mountain, in the Kaiser range in the Austrian state of Tyrol. Its summit may be ascended on an easy mountain path either directly from Griesenau or via the Stripsenjochhaus hut and the Stripsenkopf.

Geographic entities mentioned:
surface_form: feldberg (kaiser)
instance_of: Mountain
countries: Austria
coordinates: lat: 47.5924
lon: 12.3245
Feldberg (Kaiser). The Feldberg () is a mountain, in the Kaiser range in the Austrian state of Tyrol. Its summit may be ascended on an easy mountain path either directly from Griesenau or via the Stripsenjochhaus hut and the Stripsenkopf.

Geographic entities mentioned:
surface_form: feldberg
instance_of: Mountain
countries: Austria
coordinates: lat: 47.5924
lon: 12.3245
Lake Sachavacayoc. Lake Sachavacayoc (possibly from Quechua &quot;sach'awaka&quot; tapir, &quot;-yuq&quot; a suffix) is a lake in Tambopata National Reserve in Peru. It is located in the Madre de Dios Region, Tambopata Province, Tambopata District. The lake lies in a remote area near the Tambopata River.

Geographic entities mentioned:
surface_form: lake sachavacayoc
instance_of: Lake
countries: Peru
coordinates: lat: -12.89548
lon: -69.36055
surface_form: sachavacayoc
instance_of: Lake
countries: Peru
coordinates: lat: -12.89548
lon: -69.36055