Sarmila/GeoWiki-Features huggingface dataset:
Raumberg (Saxon Switzerland). Raumberg (Sächsische Schweiz) is a mountain of Saxony, southeastern Germany.

Geographic entities mentioned:
surface_form: raumberg (saxon switzerland)
instance_of: Mountain
countries: Germany
coordinates: lat: 50.8992
lon: 14.3339
Distribution and ecology. &quot;Paeonia cambessedesii&quot; is an endemic of the Balearic Islands, at one time present on Mallorca, Menorca and Cabrera, but now limited to the mountainous Northeast of Mallorca, such as in the Parc Natural de Llevant, and Northwest, such as the slopes of the Puig Major, where it grows on rocky limestone slopes or below limestone cliffs.

Geographic entities mentioned:
surface_form: Puig Major
instance_of: Mountain
countries: Spain
coordinates: lat: 39.8075
lon: 2.793333
The defeat and exile of Napoleon gave the Germans some respite, but during the Rhine Crisis of 1840, French prime minister Adolphe Thiers advanced the claim that the Upper and Middle Rhine River should serve as his country's &quot;natural eastern border&quot;. The member states of the German Confederation feared that France was resuming her annexationist designs.

Geographic entities mentioned:
surface_form: Middle Rhine
instance_of: Valley
countries: Germany
coordinates: lat: 50.364166666667
lon: 7.6055555555556
Active Sound. 3uhog6f6fibd5iwotcbxabdp5rlk" xml:space="preserve">#redirect Active Sound

Geographic entities mentioned:
surface_form: active sound
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
Her original words were: &quot;Where else should they move to? It's hard for the school to make such arrangements&quot;. Professor Xue also &quot;consoled&quot; Zhu's aunt that it would be Labor Day holidays soon and Zhu's dorm mates will be traveling to Mount Tai and there won't be anyone in the room. Theft case.

Geographic entities mentioned:
surface_form: Mount Tai
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 36.266666666667
lon: 117.1
Tobin walked to Santa Fe. John David Albert later settled in the Taos Valley, marrying Juliana León, the daughter of Miguel Antonio León. He carried mail out of the Spanish Peaks post office at Cuchara station, trapped on the Purgatory and Cucharas rivers, and is credited with building the fort at La Plaza de la Leones.

Geographic entities mentioned:
surface_form: Taos Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.375025
lon: -105.67140277777779
Tobin walked to Santa Fe. John David Albert later settled in the Taos Valley, marrying Juliana León, the daughter of Miguel Antonio León. He carried mail out of the Spanish Peaks post office at Cuchara station, trapped on the Purgatory and Cucharas rivers, and is credited with building the fort at La Plaza de la Leones.

Geographic entities mentioned:
surface_form: Spanish Peaks
instance_of: Mountain
countries: United States
coordinates: lat: 37.38
lon: -105
There is significant evidence of Aboriginal occupation at Mount Drysdale and it has been declared as an Aboriginal place. It lies 40 km east-north-east of the Mount Grenfell rock art site, an important Ngiyampaa Wangaaypuwan Aboriginal place. Settlers took over the area now known as Mount Drysdale, as part of the 'Tindarey' (or 'Tindeyrey') pastoral leasehold that was notified in July 1885.

Geographic entities mentioned:
surface_form: Mount Grenfell
instance_of: Mountain
countries: Australia
coordinates: lat: -31.301111111111112
lon: 145.30944444444444
It is located about east of Suez. It is the monotonous ride through here and Nekhel, a wilderness that provides the shortest route between Nuweiba and Cairo. Buses carrying tourists to Mount Sinai, St. Catherine's Monastery, and Feiran Oasis travel through there. Wars between Israel and Egypt.

Geographic entities mentioned:
surface_form: Mount Sinai
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.5384
lon: 33.9752
Taos County owns and manages it. History. Located in Taos, New Mexico. Spanish settlers began colonization of the Taos Valley in 1616, but the Plaza dates to the late 18th century when the Don Fernando de Taos Land Grant was ceded to Spanish settlers from the Taos Pueblo in 1796 by Don Fernando de Chacon, Governor of New Mexico.

Geographic entities mentioned:
surface_form: Taos Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.375025
lon: -105.67140277777779
375. A law that built upon Presidential Decree No. 374 and was also signed in 1974. This law added the Basilica of Taal, Church of Santa Maria, Barasoin Church, Tirad Pass, Miagao Church, the battle site of the Battle of Mactan, San Sebastian Church, and the Church of Santo Niño to the list of National Cultural Treasures. Presidential Decree No. 1505.

Geographic entities mentioned:
surface_form: Tirad Pass
instance_of: Mountain
countries: Philippines
coordinates: lat: 17.157193
lon: 120.650482
Khaste lake. 06c3gztuiemzgsd41gkzt1ufory" xml:space="preserve">#REDIRECT Khaste Lake

Geographic entities mentioned:
surface_form: khaste lake
instance_of: Lake
countries: Nepal
coordinates: lat: 28.194444444444443
lon: 84.05
Sources say that, in the summer of 1551, a mistress of Bishop Jón Arason, hid in a tent in the hollow behind from soldiers that the Danish King had sent to Hólar. The Youth Association (), was named after the mountain and operated in Akrahreppur from the early 20th century until 1995. The local newspaper, &quot;Feykir&quot;, is also named after the mountain.

Geographic entities mentioned:
surface_form: feykir
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.572222222222
lon: -19.270833333333
Glóðafeykir. is a mountain in eastern Skagafjörður, Iceland in the middle of the Blönduhlíð mountain range, directly opposite Varmahlíð. Its shape is gabled and it is rather striking. The mountain is rocky towards the top, but is still fairly easy to hike., also often called or, is 910 meters tall.

Geographic entities mentioned:
surface_form: glóðafeykir
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.572222222222
lon: -19.270833333333
Agiou Pavlou Monastery. Agiou Pavlou Monastery (;) is an Eastern Orthodox monastery in the monastic state of Mount Athos, located on the easternmost peninsula of Chalkidiki, Greece. The founder of monastery was Paul of Xeropotamou, after whom it is named.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
The tall mountain lies inside Reinheimen National Park, about southwest of the village of Lesja. The mountain is surrounded by several other mountains including Trihøene which is about to the west, Horrungen which is about to the southwest, and Kjølen, Søre Kjølhaugen, and Knatthøin which are all about to the northeast.

Geographic entities mentioned:
surface_form: Trihøene
instance_of: Mountain
countries: Norway
coordinates: lat: 62.0172
lon: 8.47444
surface_form: Horrungen
instance_of: Mountain
countries: Norway
coordinates: lat: 61.93333333
lon: 8.46666667
surface_form: Søre Kjølhaugen
instance_of: Mountain
countries: Norway
coordinates: lat: 62.045003
lon: 8.809453
surface_form: Knatthøin
instance_of: Mountain
countries: Norway
coordinates: lat: 62.02927
lon: 8.85002
surface_form: kjølen
instance_of: Mountain
countries: Norway
coordinates: lat: 62.05005
lon: 8.71375
The mountain is surrounded by several other mountains including Trihøene which is about to the west, Horrungen which is about to the southwest, and Kjølen, Søre Kjølhaugen, and Knatthøin which are all about to the northeast. The mountain Ryggehøi lies about to the south and the mountain Rundkollan lies about to the southeast.

Geographic entities mentioned:
surface_form: Ryggehøi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.61916667
lon: 8.56027778
surface_form: Rundkollan
instance_of: Mountain
countries: Norway
coordinates: lat: 61.99388889
lon: 8.65805556
Skardtind. Skardtind is a mountain in Innlandet county, Norway. The mountain is a tripoint on the border between Skjåk Municipality, Lom Municipality, and Lesja Municipality. The tall mountain lies inside Reinheimen National Park, about southwest of the village of Lesja.

Geographic entities mentioned:
surface_form: skardtind
instance_of: Mountain
countries: Norway
coordinates: lat: 62.008055555556
lon: 8.5913888888889
The thickness of the castle town walls is about. Its position provides an excellent view at the plains below bordered by the mountains Romanija, Jahorina, Treskavica and Bjelašnica in the east and southeast, Bitovnja in the south, the mountain Zec and Vranica in the Southeast, Vlašić in the west, and Tajan and Zvijezda in the north. Historic importance.

Geographic entities mentioned:
surface_form: Treskavica
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.589722222222
lon: 18.355555555556
surface_form: Bitovnja
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.802
lon: 17.935
After spending some time of preparation, Hedin started his exploration by crossing the Pamir Mountains. In mid-March 1894, Hedin and his entourage arrived in the &quot;most distant outpost of the Russian Empire&quot;, Pamirsky Post, in today's Tajikistan. From there, Hedin's next aim was to climb to the peak of the Muztagh-Ata. The first attempt failed due to health issues on Hedin's side.

Geographic entities mentioned:
surface_form: Muztagh-Ata
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 38.278333333333
lon: 75.115833333333
Lukens also led California's first attempts at reforestation in the 1890s. For his efforts, Lukens was given the moniker &quot;Father of Forestry&quot;, and and Mount Lukens in California are named for him. The house was added to the National Register of Historic Places on March 29, 1984.

Geographic entities mentioned:
surface_form: Mount Lukens
instance_of: Mountain
countries: United States
coordinates: lat: 34.2689
lon: -118.239
The peak is not exceptionally steep and is a fault-block mountain. The north and south slopes are gentle, while the east and west slopes are steeper, with difficult rock faces. It is located in the southern region of Eravikulam National Park at the junction of the Cardamom Hills, the Anaimalai Hills and the Palani Hills in the Periyar River basin of Kerala at a distance of from Munnar. Geology.

Geographic entities mentioned:
surface_form: hills
instance_of: Mountain
countries: India
coordinates: lat: 23.166666666667
lon: 92.833333333333
surface_form: hills
instance_of: Mountain
countries: India
coordinates: lat: 23.166666666667
lon: 92.833333333333
surface_form: hills
instance_of: Mountain
countries: India
coordinates: lat: 23.166666666667
lon: 92.833333333333
Anamudi. Anamudi (&quot;Elephant head&quot;,) is a mountain located in Ernakulam district and Idukki district of the Indian state of Kerala. With an elevation of, it is the highest peak in the Western Ghats and in South India. With a topographic prominence of, it is the 26th most prominent peak in the world. Geography. Anamudi has an elevation of.

Geographic entities mentioned:
surface_form: anamudi
instance_of: Mountain
countries: India
coordinates: lat: 10.166666666667
lon: 77.066666666667
Specifically, Anamudi is located within a geological sub-province of the SGT known as the Madurai Province. The mountain massif itself is composed of neoproterozoic A-type granite known as Munnar Granite, which was intruded deep into the thickened crust of the SGT during Orogenic collapse of the Pan-African highlands.

Geographic entities mentioned:
surface_form: anamudi
instance_of: Mountain
countries: India
coordinates: lat: 10.166666666667
lon: 77.066666666667
At age 13, Lillian started playing senior softball for the Nelson Red Sox, winning the city league batting title in 1941. In between, she played basketball, bowled for a local team that won the first inter-city ladies five pin tournament, and regularly swam across Kootenay Lake, winning several swimming competitions and diving events.

Geographic entities mentioned:
surface_form: Kootenay Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
Haplochromis degeni. &quot;Haplochromis degeni&quot; is a species of cichlid endemic to Lake Victoria. It is sometimes placed in the monotypic genus &quot;Platytaeniodus&quot;, but FishBase leaves it in &quot;Haplochromis&quot; pending a thorough review of that group. This species grows to a length of SL. Etymology.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
January is the coldest month with an average mean temperature of, with temperatures dropping to or below 5 days per year on average. Snowfall is lighter than in the snowbelt areas to the northeast, but is still somewhat influenced by Lake Erie, located north of the city. Snowfall averages per season.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Indo-European languages. The Indo-European languages are a language family native to the northern Indian subcontinent, most of Europe, and the Iranian plateau with additional native branches found in regions such as Sri Lanka, the Maldives, parts of Central Asia (e.g., Tajikistan and Afghanistan), and Armenia.

Geographic entities mentioned:
surface_form: Iranian plateau
instance_of: Plateau
countries: Iran
coordinates: lat: 36.283333
lon: 59.05
Carinthia Rinka. bujfhg55a16b5ljt88ce6hbskxx" xml:space="preserve">#REDIRECT Carinthia Mount Rinka

Geographic entities mentioned:
surface_form: carinthia rinka
instance_of: Mountain
countries: Slovenia
coordinates: lat: 46.36675
lon: 14.565
Unicorn Peak. Unicorn Peak is a mountain summit in Lewis County of Washington state, United States. It is the highest point in the Tatoosh Range which is a sub-range of the Cascade Range. It is located in Mount Rainier National Park, south of Mount Rainier. Precipitation runoff from the mountain's small glaciers, such as Unicorn Glacier, drains into tributaries of the Cowlitz River.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: mount rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
Unicorn Peak. Unicorn Peak is a mountain summit in Lewis County of Washington state, United States. It is the highest point in the Tatoosh Range which is a sub-range of the Cascade Range. It is located in Mount Rainier National Park, south of Mount Rainier. Precipitation runoff from the mountain's small glaciers, such as Unicorn Glacier, drains into tributaries of the Cowlitz River.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: unicorn peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.745
lon: -121.7
Unicorn Peak. Unicorn Peak is a mountain summit in Lewis County of Washington state, United States. It is the highest point in the Tatoosh Range which is a sub-range of the Cascade Range. It is located in Mount Rainier National Park, south of Mount Rainier. Precipitation runoff from the mountain's small glaciers, such as Unicorn Glacier, drains into tributaries of the Cowlitz River.

Geographic entities mentioned:
surface_form: unicorn peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.745
lon: -121.7
The descriptive name is for the mountain's resemblance to the head and horn of a unicorn. The toponym was officially adopted in 1913 by the U.S. Board on Geographic Names. Climate. Unicorn Peak is located in the marine west coast climate zone of western North America. Most weather fronts originating in the Pacific Ocean travel northeast toward the Cascade Mountains.

Geographic entities mentioned:
surface_form: unicorn peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.745
lon: -121.7
Aigle River (Doda Lake). Forestry is the main economic activity of the sector; recreational tourism activities, second. The valley of the Aigle River is served by the forest road R1053 (East-West direction) which passes on the north-west side and north of Hébert Lake. This road joins the road R1009 (North-South direction) which passes to the East of the river of Eagle.

Geographic entities mentioned:
surface_form: Hébert Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.20111111
lon: -75.29972222
Kalm, in Eeyou Istchee James Bay (municipality). Upper course of the Eagle River (segment of)
Intermediate course of the Eagle River (segment of)
Lower course of the Eagle River (segment of)
The Aigle River flows on the south shore of a bay stretching over south of Doda Lake. The northern part of this lake is crossed to the West by the Opawica River.

Geographic entities mentioned:
surface_form: Doda Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.40111111
lon: -75.19444444
From there, the current of this river generally descends to the West, crossing in particular Doda Lake, Françoise Lake (Opawica River), La Ronde Lake, Lessard Lake, Lichen Lake (Opawica River), then north across Wachigabau Lake and Opawica Lake to its confluence with the Chibougamau River; this confluence is the source of the Waswanipi River.

Geographic entities mentioned:
surface_form: Doda Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.40111111
lon: -75.19444444
surface_form: Wachigabau Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.553611111111
lon: -75.875555555556
surface_form: Opawica Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.579166666667
lon: -75.878888888889
The course runs westward through the northern portion of lake Waswanipi, Goéland Lake and Lake Olga, before pouring into the Matagami Lake; the latter in turn flows into the Nottaway River, a tributary of Rupert Bay (James Bay). Toponymy. At various times in history, this territory has been occupied by the Attikameks, the Algonquins and the Crees.

Geographic entities mentioned:
surface_form: lake Waswanipi
instance_of: Lake
countries: Canada
coordinates: lat: 49.5519
lon: -76.45
Extensional cracking of the North American Plate in this part of North America has existed for millions of years. Continuation of this continental rifting has fed scores of volcanoes throughout the Northern Cordilleran Volcanic Province over at least the past 20 million years (see Geology of the Pacific Northwest) and occasionally continued into geologically recent times.

Geographic entities mentioned:
surface_form: Northern Cordilleran Volcanic Province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
In the past 15 million years, at least four large volcanoes have formed their way through dense igneous and metamorphic composed bedrock of this part of North America. This includes Hoodoo Mountain, the Mount Edziza volcanic complex, Level Mountain and Heart Peaks, which are primarily located in northwestern British Columbia.

Geographic entities mentioned:
surface_form: Hoodoo Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: Heart Peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
Mount Shasta, the largest stratovolcano in the Cascade Arc and Mount Veniaminof, one of the largest and most active volcanoes in the Aleutian Arc, have volumes of at least, less than half of that of the Level Mountain and Edziza shield complexes.

Geographic entities mentioned:
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: Mount Veniaminof
instance_of: Mountain
countries: United States
coordinates: lat: 56.198055555556
lon: -159.39083333333
Just west of Level Mountain lies Heart Peaks, the third most voluminous volcano of the Northern Cordilleran Volcanic Province with an area of. However, remains of a shield volcano that once covered an area of more than are present in the western Cassiar Mountains as Maitland Volcano.

Geographic entities mentioned:
surface_form: Maitland Volcano
instance_of: Mountain
countries: Canada
coordinates: lat: 57.04
lon: -129.07
All of the known most recent eruptions have occurred in British Columbia, although there is evidence for volcanic activity in Yukon in the past thousand years. The two most recent were lava flow eruptions at Tseax Cone in the 18th century and at The Volcano in 1904.

Geographic entities mentioned:
surface_form: Tseax Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
When the Mount Edziza volcanic complex began to form 7.5 million years ago, volcanism rates in the Northern Cordilleran Volcanic Province increased again. Early volcanic activity of the Mount Edziza volcanic complex seven million years ago constructed Armadillo Peak, the oldest and most central of the four central volcanoes comprising the complex.

Geographic entities mentioned:
surface_form: Armadillo Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5383
lon: -130.56
Glacial ice and streams have since dissected the stratovolcano into a series of valleys with intervening ridges, forming the so-named Level Mountain Range on the central summit of Level Mountain. More Miocene age volcanics of and years are present at the Anderson and Moose bays of Atlin Lake in northern British Columbia that represent remnants of columnar-jointed basalt lava flows.

Geographic entities mentioned:
surface_form: Atlin Lake
instance_of: Lake
countries: Canada
coordinates: lat: 60.0133333
lon: -133.8308333
Volcanism 5.3 to 1.6 million years ago. In northern British Columbia, remnants of a shield volcano are found throughout the western Cassiar Mountains. This prehistoric shield volcano, known as Maitland Volcano, was erupted from five to four million years ago on a mature eroded surface as thin hawaiite and basaltic lava flows engulfed the surrounding landscape.

Geographic entities mentioned:
surface_form: Maitland Volcano
instance_of: Mountain
countries: Canada
coordinates: lat: 57.04
lon: -129.07
This volcano-ice association can be recognized in three different physiographic settings, each displaying unique relationships between topography, volcanism and glacial ice. The first volcano-ice interaction is displayed as tuyas, including Tuya Butte, on the Tanzilla Plateau in the Northern Interior of British Columbia.

Geographic entities mentioned:
surface_form: Tanzilla Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.3667
lon: -130.367
The first volcano-ice interaction is displayed as tuyas, including Tuya Butte, on the Tanzilla Plateau in the Northern Interior of British Columbia. This sub-section of the Stikine Plateau consists of large flatlands with hills of low relief, and might have been one of the areas of ice accumulation for the Cordilleran Ice Sheet.

Geographic entities mentioned:
surface_form: Stikine Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
The Mount Edziza and Level Mountain complexes have shelves of older lava with elevations more than and have been zones of volcanic activity long enough that their geothermal activities might have had effects on movements of the Cordilleran Ice Sheet much like the Grímsvötn caldera in Iceland, which has been a significant heat source beneath the vast Vatnajökull icecap.

Geographic entities mentioned:
surface_form: Grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
Just northwest of Level Mountain, the Heart Peaks shield volcano rises with a topographic prominence of above the Nahlin Plateau with rhyolitic lava domes capping its summit. Heart Peaks is made of flat-lying basaltic and trachybasaltic lava flows and pyroclastic rocks. The most recent eruption at the shield is of dominantly Pleistocene age and late-stage Holocene activity is uncertain.

Geographic entities mentioned:
surface_form: Heart Peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
surface_form: Nahlin Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.44972222222222
lon: -131.41833333333332
More than 90% of Hoodoo Mountain was formed during this eruptive period and interlayed peralkaline phonolitic and trachytic lava flows and hyaloclastites are the main volcanics comprising the volcano. On the northern flank of Hoodoo Mountain lies the smaller Little Bear Mountain, a tuya which also formed in the Pleistocene epoch.

Geographic entities mentioned:
surface_form: Little Bear Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.8
lon: -131.3
On the northern flank of Hoodoo Mountain lies the smaller Little Bear Mountain, a tuya which also formed in the Pleistocene epoch. Ice Peak, which overlaps the northern flank of Armadillo Peak, began to form when the regional Cordilleran Ice Sheet began retreating from the Mount Edziza volcanic complex 1,600,000 years ago.

Geographic entities mentioned:
surface_form: Ice Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
Mount Edziza, a steep-sided stratovolcano overlapping the northern flank of Ice Peak and the most northerly of the four central volcanoes comprising the Mount Edziza volcanic complex, began to form a million years ago when the Cordilleran Ice Sheet retreated from the upper flanks of the Edziza lava plateau.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
It is a small cinder cone made of basanite with a deep breached volcanic crater at its summit. Extending from Prindle's breached volcanic crater is a long basanite lava flow that flowed southeast of the cone then flowed southwest into a river valley. The Cassiar Mountains and Tanzilla Plateau in northern British Columbia are dominated by tuyas of the broad Tuya Volcanic Field.

Geographic entities mentioned:
surface_form: Tuya Volcanic Field
instance_of: Mountain
countries: Canada
coordinates: lat: 59.2167
lon: -130.95
These flat-topped, steep-sided subglacial volcanoes were formed when magma intruded into and melted a vertical pipe in the overlying Cordilleran Ice Sheet. At least six volcanoes formed beneath glacial ice close to Tuya Lake, including Ash Mountain, South Tuya, Tuya Butte, Mathews Tuya.

Geographic entities mentioned:
surface_form: Tuya Lake
instance_of: Lake
countries: Canada
coordinates: lat: 59.0825
lon: -130.575556
surface_form: South Tuya
instance_of: Mountain
countries: Canada
coordinates: lat: 59.20861111
lon: -130.50527778
surface_form: Mathews Tuya
instance_of: Mountain
countries: Canada
coordinates: lat: 59.1953
lon: -130.433
Ash Mountain at the head of Parallel Creek consists of pillow lava and hyaloclastite, South Tuya consists of loose volcanic debris with basaltic dikes intruding into the volcano and Tuya Butte and Mathews Tuya consist of pillow lava and hyaloclastite on its lower flanks with subaerially erupted lava flows at their flat-topped summits. Volcanism in the past 10,000 years.

Geographic entities mentioned:
surface_form: Parallel Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 59.51416666666667
lon: -130.79083333333332
The most recent eruption of the Iskut-Unuk River Cones at The Volcano (also called Lava Fork volcano) in 1904 is also the most recent volcanic eruption in Canada. Immediately north of the junction of the Pelly and Yukon rivers, Volcano Mountain in central Yukon consists of a cinder cone and a series of lava flows.

Geographic entities mentioned:
surface_form: Volcano Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 62.93
lon: -137.38
More than 20 eruptions have occurred at the Mount Edziza volcanic complex in the past 10,000 years, including Mess Lake Cone, Kana Cone, Cinder Cliff, Icefall Cone, Ridge Cone, Williams Cone, Walkout Creek Cone, Moraine Cone, Sidas Cone, Sleet Cone, Storm Cone, Triplex Cones, Twin Cone, Cache Hill, Camp Hill, Cocoa Crater, Coffee Crater, Nahta Cone, Tennena Cone, The Saucer and the well-preserved Eve Cone.

Geographic entities mentioned:
surface_form: Williams Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
surface_form: Sidas Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.8589
lon: -130.628
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: Nahta Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3083
lon: -130.821
surface_form: Tennena Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.68416666666667
lon: -130.66222222222223
surface_form: Eve Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
The cones were built on the basaltic fragments and blocky lava fields surrounding the cones. The Snowshoe Lava Field on the southern end of the Big Raven Plateau is one of the areas of young lava flows in the region while the Desolation Lava Field on the northern end of the Big Raven Plateau is the largest area of young lava flows, covering an area of. The longest lava flow is.

Geographic entities mentioned:
surface_form: Big Raven Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
The longest lava flow is. This volcanic activity was followed by at least two younger, but still undated eruptions. Two well-preserved reddish-brown basaltic cinder cones cap a small shield volcano of the Alligator Lake volcanic complex in southcentral Yukon. These cinder cones are likely younger than the adjacent Holocene glaciation and both cones were erupting at the same time.

Geographic entities mentioned:
surface_form: Alligator Lake volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 60.389722222222
lon: -135.42638888889
In the Pleistocene Tuya Volcanic Field, small subaerial shield volcanoes and postglacial cinder cones and lava flows can be recognized. At least one of these volcanoes is of Holocene age. Gabrielse Cone near the headwaters of Iverson Creek in the Stikine Ranges rises with an elevation of and a diameter of. It is mostly made of loose basaltic scoria with a volcanic crater deep at its summit.

Geographic entities mentioned:
surface_form: Gabrielse Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 59.4186
lon: -130.397
Edziza and Hoodoo Mountain are two of the three most hazardous volcanoes in Western Canada that have been active in the past 10,000 years, the other being the Mount Meager massif in the Garibaldi Volcanic Belt of southwestern British Columbia which produced a large-scale eruption 2,350 years ago that sent ash as far as central Alberta.

Geographic entities mentioned:
surface_form: Garibaldi Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5283
lon: -126.113
Tabeguache Peak. Tabeguache Peak is one of the fourteeners of the US state of Colorado. It is a near neighbor of the higher peak Mount Shavano, which lies approximately 1/2 mile (approximately 1 km) to the southeast. According to William Bright an American Linguist specialized in Native American and South Asian languages and descriptive linguistics it is pronounced &quot;TAB-uh-wahch&quot; ().

Geographic entities mentioned:
surface_form: Mount Shavano
instance_of: Mountain
countries: United States
coordinates: lat: 38.619166666667
lon: -106.23944444444
It is located within the San Isabel National Forest and is in Chaffee County. The mountain is named for the Tabeguache band of the Utes. &quot;Tabaguache&quot; means 'People of Sun Mountain', from &quot;Tava&quot; meaning 'sun.'
Climbing. It is frequently climbed with its neighbor Mount Shavano. The standard route combining both peaks is rated Class 2.

Geographic entities mentioned:
surface_form: Mount Shavano
instance_of: Mountain
countries: United States
coordinates: lat: 38.619166666667
lon: -106.23944444444
Tabeguache Peak. Tabeguache Peak is one of the fourteeners of the US state of Colorado. It is a near neighbor of the higher peak Mount Shavano, which lies approximately 1/2 mile (approximately 1 km) to the southeast. According to William Bright an American Linguist specialized in Native American and South Asian languages and descriptive linguistics it is pronounced &quot;TAB-uh-wahch&quot; ().

Geographic entities mentioned:
surface_form: tabeguache peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.625555555556
lon: -106.25083333333
History. Eustis is one of several towns in Lake County that trace their origins to the 1870s, a post-Civil War era when settlers moved southward into the Florida frontier. The city is named after then Colonel Abraham Eustis, a U.S. Army officer who served during the Seminole Wars and skirmished along the south shore of what is now Lake Eustis, near Tavares.

Geographic entities mentioned:
surface_form: Lake Eustis
instance_of: Lake
countries: United States
coordinates: lat: 28.8489
lon: -81.7253
Geography. According to the United States Census Bureau, the city has a total area of, of which is land and (13.28%) is water. Eustis is located in central Florida on the eastern shore of Lake Eustis, one of the Harris Chain of Lakes Harris Chain of Lakes. The city’s terrain is relatively flat, approximately 79 feet (24 meters, with numerous lakes in the surrounding area.

Geographic entities mentioned:
surface_form: Lake Eustis
instance_of: Lake
countries: United States
coordinates: lat: 28.8489
lon: -81.7253
The floods damaged about 3,000 homes and 100 businesses. Overall monetary damage in the city was estimated at $225 million, with $520 million in the entire metropolitan area, making it the city's worst flood on record. Across the Shenandoah Valley, the flooding caused widespread damage, notably in Rockingham County where the floods damaged most of the roads, and entered 4,000 houses and 350 farms.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Moore, Jr. Maryland, Washington, D.C., and Pennsylvania. Flooding in Maryland largely occurred along the Potomac River, primarily along the north branch and downstream after draining floodwaters from Virginia and West Virginia. Two gauging stations recorded new discharge records, although the peak of at Paw Paw was slightly less than the record set in 1936.

Geographic entities mentioned:
surface_form: the north branch
instance_of: Watercourse
countries: United States
coordinates: lat: 39.5284255
lon: -78.5875141
Lake Pepin (Le Sueur County, Minnesota). Lake Pepin is a lake in Le Sueur County, in the U.S. state of Minnesota. The lake took its name from Lake Pepin on the Mississippi River.

Geographic entities mentioned:
surface_form: Lake Pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
surface_form: pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
surface_form: lake pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.473333333333
lon: -93.592222222222
Lake Pepin (Le Sueur County, Minnesota). Lake Pepin is a lake in Le Sueur County, in the U.S. state of Minnesota. The lake took its name from Lake Pepin on the Mississippi River.

Geographic entities mentioned:
surface_form: pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
surface_form: lake pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
surface_form: lake pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.473333333333
lon: -93.592222222222
China claims the village as part of its Zanda County, Tibet. Geography. Kaurik lies in the Zanskar Range on the bank of the Pare Chu river (or Parang River). Pare Chu originates in Spiti and takes a circuitous route through Ladakh and Ngari Khorsum, finally reentering Spiti at Kaurik. It joins the Spiti River at Sumdo about 20 km to the southwest. Demographics.

Geographic entities mentioned:
surface_form: Spiti
instance_of: Valley
countries: India
Qing dynasty
coordinates: lat: 32.246944444444445
lon: 78.05222222222223
They faced the emissaries of the governor of Gartok, who were sent there for the purpose of pointing out the &quot;ancient boundary between Ladakh and the Chinese territory&quot;. (Spiti was traditionally part of Ladakh.)
In December 1957, seven years after the Chinese annexation of Tibet, Chinese forces were said to have intruded at Kaurik, for which India lodged a protest.

Geographic entities mentioned:
surface_form: Spiti
instance_of: Valley
countries: India
Qing dynasty
coordinates: lat: 32.246944444444445
lon: 78.05222222222223
This range is closely affiliated with three other small ranges in the area: the Ekalaka Hills, which are also located in Carter County, the East Short Pine Hills, which are located southwest of Buffalo, South Dakota, and the West Short Pine Hills, which are located south of Camp Crook, South Dakota.

Geographic entities mentioned:
surface_form: Ekalaka Hills
instance_of: Landform
countries: United States
coordinates: lat: 45.8767
lon: -104.472
Long Pines. The Long Pines, elevation, is a small mountain range southeast of Ekalaka, Montana, in Carter County.

Geographic entities mentioned:
surface_form: long pines
instance_of: Landform
countries: United States
coordinates: lat: 45.6889
lon: -104.228
Long Pines is the current designation of the former Long Pine National Forest, which was eventually consolidated into the Custer Gallatin National Forest. The majority of this land unit’s current lies within Carter County, Montana; of that total extend east into Harding County, South Dakota.

Geographic entities mentioned:
surface_form: long pines
instance_of: Landform
countries: United States
coordinates: lat: 45.6889
lon: -104.228
The majority of this land unit’s current lies within Carter County, Montana; of that total extend east into Harding County, South Dakota. The Long Pines land unit is part of Custer Gallatin’s Sioux Ranger District, as are the aforementioned Ekalaka Hills, East Short Pine Hills, and West Short Pine Hills land units.

Geographic entities mentioned:
surface_form: long pines
instance_of: Landform
countries: United States
coordinates: lat: 45.6889
lon: -104.228
In 2015, Stanley and his son Jason again traveled to California to restore another Henry Hunt totem pole which preceded the Sunnylands' pole arrival in the Coachella Valley when it was installed in Palm Springs. The Palm Springs pole had been a gift to the city in 1968 through the sister city program and still resides in its original location on Racquet Club Road in Victoria Park.

Geographic entities mentioned:
surface_form: Coachella Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.72
lon: -116.2
Beaty Lake (Arkansas). Beaty Lake is a lake in St. Francis County, Arkansas.

Geographic entities mentioned:
surface_form: beaty lake (arkansas)
instance_of: Lake
countries: United States
coordinates: lat: 35.0723
lon: -90.7081
Beaty Lake (Arkansas). Beaty Lake is a lake in St. Francis County, Arkansas.

Geographic entities mentioned:
surface_form: beaty lake
instance_of: Lake
countries: United States
coordinates: lat: 35.0723
lon: -90.7081
The 1921 house with its 8+ bedrooms and 7+ bathrooms was on sale in 2009 for $3.4 million. Its carriage house (built later in 1941) at 10914 Greendale was also up for sale. It is located on Lake Steilacoom. According to the broker's website, it was built in memory of Edward Rhodes, &quot;who served and paid the ultimate sacrifice in World War I&quot;.

Geographic entities mentioned:
surface_form: Lake Steilacoom
instance_of: Lake
countries: United States
coordinates: lat: 47.16166666666667
lon: -122.5325
Manitoba Provincial Road 265. Provincial Road 265 (PR 265) is an east–west road in the Westman and Central Plains Regions of Manitoba. Mostly a gravel road, it connects the communities of Clanwilliam, Polonia, Eden, Plumas, and Langruth, as well as providing a connection between Riding Mountain National Park and Lake Manitoba. Route description.

Geographic entities mentioned:
surface_form: Lake Manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
PR 265 now traverses the swampy marshlands surrounding Jackfish Lake, where it crosses the Whitemud River, before entering the hamlet of Langruth, where it comes to and end at a junction with PTH 50 (Kinosota Road). The road continues east as Road 94N to the beaches of Lake Manitoba at Big Point.

Geographic entities mentioned:
surface_form: Lake Manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
Service. In 1803 Lieutenant Isaac William Scott took command of &quot;Princess Augusta&quot; for the North Sea. In the second week of September she delivered orders from Lord Keith to warships off Hellevoetsluis, Texel and the Elbe. &quot;Princess Augusta&quot; vs. Two Dutch privateers.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Having discovered that there was not enough game around Karge, being hunters, they moved across Zalan to the Jos Plateau, settling temporarily at the present abode of the Anaguta and Afizere (Jarawa) peoples, before proceeding through Rahama, Kauru and subsequently settling at Mashan in Atyap Chiefdom.

Geographic entities mentioned:
surface_form: Jos Plateau
instance_of: Plateau
countries: Nigeria
coordinates: lat: 9.5667
lon: 9.0833
Today, Kafanchan is a melting pot of many Nigerians from parts of southern Kaduna such as the Gwong and the Ham, and other parts of Nigeria. Landscape. The town lies within the Southern Guinea Zone, consisting of forests and savannah lands, and is located southwest of the Jos Plateau escarpment on the windward region.

Geographic entities mentioned:
surface_form: Jos Plateau
instance_of: Plateau
countries: Nigeria
coordinates: lat: 9.5667
lon: 9.0833
The relief consists of two main rivers, Sanga (same as the Kogum River) and Amere (same as the Mada River and River Wonderful), both sourced from the plateau, with the former merging with the latter close to the Kogum River Station and finally emptying into the Benue River. There lie in addition, numerous hills, valleys streams.

Geographic entities mentioned:
surface_form: Benue River
instance_of: Watercourse
countries: Cameroon
Nigeria
coordinates: lat: 7.783333
lon: 6.766667
According to the U.S. Census Bureau, the village of Hilton has a total area of, all of it recorded as land. Salmon Creek, a direct tributary of Lake Ontario, flows eastward through the south side of the village. Demographics. As of the census of 2000, there were 5,856 people, 2,041 households, and 1,512 families residing in the village. The population density was.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Waqwaqucha. Waqwaqucha (Quechua &quot;waqwa, waqu, mayu sunsu&quot; black-crowned night heron (&quot;Nycticorax nycticorax hoacli gmel&quot;), &quot;qucha&quot; lake, &quot;night heron lake&quot;, hispanicized spellings &quot;Huajhuacocha, Huaj Huacocha&quot;) is a lake in Peru located in the Cusco Region, Quispicanchi Province, Quiquijana District.

Geographic entities mentioned:
surface_form: waqwaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -13.8511
lon: -71.6178
Waqwaqucha. Waqwaqucha (Quechua &quot;waqwa, waqu, mayu sunsu&quot; black-crowned night heron (&quot;Nycticorax nycticorax hoacli gmel&quot;), &quot;qucha&quot; lake, &quot;night heron lake&quot;, hispanicized spellings &quot;Huajhuacocha, Huaj Huacocha&quot;) is a lake in Peru located in the Cusco Region, Quispicanchi Province, Quiquijana District.

Geographic entities mentioned:
surface_form: waqwaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -13.8511
lon: -71.6178
surface_form: waqwaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -13.8511
lon: -71.6178
Post-publication review of this paper suggests that at least some of these SLOs are anthropogenic. Another group of scientists reported evidence supporting a modified version of the hypothesis—involving a fragmented comet or asteroid—was found in lake bed cores dating to 12,900 YBP from Lake Cuitzeo in Guanajuato, Mexico.

Geographic entities mentioned:
surface_form: Lake Cuitzeo
instance_of: Lake
countries: Mexico
coordinates: lat: 19.933333333333
lon: -101.08333333333
It belongs to the &quot;Zahmer Kaiser&quot; group and its summit is covered in mountain pine. Location. The Stripsenkopf rises immediately north of the Stripsenjoch saddle, which separates the peak from the &quot;Wilder Kaiser&quot;. Its unique location makes the Stripsenkopf a very popular destination with its commanding view of the rock faces on the Karlspitzen and Totenkirchl.

Geographic entities mentioned:
surface_form: Karlspitzen
instance_of: Mountain
countries: Austria
coordinates: lat: 47.565555555556
lon: 12.315555555556
surface_form: Totenkirchl
instance_of: Mountain
countries: Austria
coordinates: lat: 47.57
lon: 12.311944444444
surface_form: stripsenkopf
instance_of: Mountain
countries: Austria
coordinates: lat: 47.581944444444
lon: 12.308333333333
surface_form: stripsenkopf
instance_of: Mountain
countries: Austria
coordinates: lat: 47.581944444444
lon: 12.308333333333
surface_form: totenkirchl
instance_of: Mountain
countries: Austria
coordinates: lat: 47.57
lon: 12.311944444444
surface_form: karlspitzen
instance_of: Mountain
countries: Austria
coordinates: lat: 47.565555555556
lon: 12.315555555556
From the Stripsenkopf a wide ridge runs northeast over to the &quot;Feldberg&quot; (1,814 m), a frequently used climbing path heading along it toward Griesenau. On the west side the Stripsenkopf falls away into the Kaisertal valley, its slopes covered in mountain pine and woods. To the southeast its steep flanks and gullies drop into the Kaiserbach valley. Routes.

Geographic entities mentioned:
surface_form: Kaisertal
instance_of: Valley
countries: Austria
coordinates: lat: 47.58416666666667
lon: 12.265833333333333
surface_form: kaisertal
instance_of: Valley
countries: Austria
coordinates: lat: 47.58416666666667
lon: 12.265833333333333
From the Stripsenkopf a wide ridge runs northeast over to the &quot;Feldberg&quot; (1,814 m), a frequently used climbing path heading along it toward Griesenau. On the west side the Stripsenkopf falls away into the Kaisertal valley, its slopes covered in mountain pine and woods. To the southeast its steep flanks and gullies drop into the Kaiserbach valley. Routes.

Geographic entities mentioned:
surface_form: Kaiserbach valley
instance_of: Valley
countries: Austria
coordinates: lat: 47.58166666666666
lon: 12.361666666666666
surface_form: kaiserbach valley
instance_of: Valley
countries: Austria
coordinates: lat: 47.58166666666666
lon: 12.361666666666666
Its unique location makes the Stripsenkopf a very popular destination with its commanding view of the rock faces on the Karlspitzen and Totenkirchl. From the Stripsenkopf a wide ridge runs northeast over to the &quot;Feldberg&quot; (1,814 m), a frequently used climbing path heading along it toward Griesenau.

Geographic entities mentioned:
surface_form: feldberg
instance_of: Mountain
countries: Austria
coordinates: lat: 47.5924
lon: 12.3245
surface_form: stripsenkopf
instance_of: Mountain
countries: Austria
coordinates: lat: 47.581944444444
lon: 12.308333333333