Sarmila/GeoWiki-Features huggingface dataset:
The Pamir River is in the south-west of the Pamirs. Mountain. The three highest mountains in the Pamirs core are Ismoil Somoni Peak (known from 1932 to 1962 as Stalin Peak, and from 1962 to 1998 as Communism Peak),; Ibn Sina Peak (still unofficially known as Lenin Peak),; and Peak Korzhenevskaya (, &quot;Pik Korzhenevskoi&quot;). In the Eastern Pamirs, China's Kongur Tagh is the highest at.

Geographic entities mentioned:
surface_form: Ismoil Somoni Peak
instance_of: Mountain
countries: Tajikistan
coordinates: lat: 38.942732
lon: 72.015347
surface_form: Ibn Sina Peak
instance_of: Mountain
countries: Kyrgyzstan
Tajikistan
Soviet Union
coordinates: lat: 39.343677
lon: 72.877897
surface_form: Peak Korzhenevskaya
instance_of: Mountain
countries: Tajikistan
coordinates: lat: 39.055855
lon: 72.011744
The Pamir River is in the south-west of the Pamirs. Mountain. The three highest mountains in the Pamirs core are Ismoil Somoni Peak (known from 1932 to 1962 as Stalin Peak, and from 1962 to 1998 as Communism Peak),; Ibn Sina Peak (still unofficially known as Lenin Peak),; and Peak Korzhenevskaya (, &quot;Pik Korzhenevskoi&quot;). In the Eastern Pamirs, China's Kongur Tagh is the highest at.

Geographic entities mentioned:
surface_form: Kongur Tagh
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 38.593888888889
lon: 75.313333333333
Exploration. The lapis lazuli found in Egyptian tombs is thought to come from the Pamir area in Badakhshan province of Afghanistan. About 138 BCE Zhang Qian reached the Fergana Valley northwest of the Pamirs. Ptolemy vaguely describes a trade route through the area. From about 600 CE, Buddhist pilgrims travelled on both sides of the Pamirs to reach India from China.

Geographic entities mentioned:
surface_form: Fergana Valley
instance_of: Valley
countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
lon: 71.757777777778
The Dieze Railway bridge is somewhat further downstream. Location. For practical purposes, one can consider the Dieze bridge to be at the confluence of the Dommel, Binnendieze, and Aa. If one wants to be very exact, one can say that the Dommel and Binnendieze meet 50 m south of the bridge, to form the Dieze. Therefore, the bridge is technically at the confluence of the Dieze and Aa.

Geographic entities mentioned:
surface_form: Binnendieze
instance_of: Watercourse
countries: Netherlands
coordinates: lat: 51.68527777777778
lon: 5.308055555555556
Elaphoglossum serpens. &quot;Elaphoglossum serpens&quot; is a rare species of fern that grows only on Cerro de Punta, the highest mountain in Puerto Rico. The fern grows at one location, where there are 22 known specimens. It was federally listed as an endangered species of the United States in 1993. The fern was described in 1947 from specimens found at Monte Jayuya.

Geographic entities mentioned:
surface_form: Cerro de Punta
instance_of: Mountain
countries: United States
coordinates: lat: 18.1725
lon: -66.591944444444
The fern grows at one location, where there are 22 known specimens. It was federally listed as an endangered species of the United States in 1993. The fern was described in 1947 from specimens found at Monte Jayuya. This habitat was cleared for construction and the plant was extirpated. It was later located on Cerro de Punta.

Geographic entities mentioned:
surface_form: Monte Jayuya
instance_of: Mountain
countries: United States
coordinates: lat: 18.167777777778
lon: -66.574722222222
Talcot Lake. Talcot Lake is a lake in the U.S. state of Minnesota. The lake was named for Andrew Talcott, a surveyor.

Geographic entities mentioned:
surface_form: talcot lake
instance_of: Lake
countries: United States
coordinates: lat: 43.87805556
lon: -95.45277778
The lake runs from South Rome to Peoria Heights, with Spring Bay and the Detweiller Marina area of Peoria near the middle. Just north of Peoria Heights, it empties through a narrow part of the Illinois River into the smaller Peoria Lake, sometimes called Lower Peoria Lake, at approximately river mile 166.5. Geology.

Geographic entities mentioned:
surface_form: Peoria Lake
instance_of: Lake
countries: United States
coordinates: lat: 40.702222222222
lon: -89.554444444444
surface_form: peoria lake
instance_of: Lake
countries: United States
coordinates: lat: 40.702222222222
lon: -89.554444444444
surface_form: lower peoria lake
instance_of: Lake
countries: United States
coordinates: lat: 40.702222222222
lon: -89.554444444444
Upper Peoria Lake. Upper Peoria Lake is a section of the Illinois River primarily between Peoria County and Woodford County, Illinois, United States. The lake runs from South Rome to Peoria Heights, with Spring Bay and the Detweiller Marina area of Peoria near the middle.

Geographic entities mentioned:
surface_form: peoria lake
instance_of: Lake
countries: United States
coordinates: lat: 40.702222222222
lon: -89.554444444444
surface_form: upper peoria lake
instance_of: Lake
countries: United States
coordinates: lat: 40.806666666667
lon: -89.551111111111
Just north of Peoria Heights, it empties through a narrow part of the Illinois River into the smaller Peoria Lake, sometimes called Lower Peoria Lake, at approximately river mile 166.5. Geology. The Upper Peoria Lake originated during the Woodfordian substage of the Wisconsin glaciation. It is part of the Bloomington moraine.

Geographic entities mentioned:
surface_form: peoria lake
instance_of: Lake
countries: United States
coordinates: lat: 40.702222222222
lon: -89.554444444444
surface_form: upper peoria lake
instance_of: Lake
countries: United States
coordinates: lat: 40.806666666667
lon: -89.551111111111
Geology. The Upper Peoria Lake originated during the Woodfordian substage of the Wisconsin glaciation. It is part of the Bloomington moraine. Upper Peoria Lake is a remnant of old Glacial Lake Illinois, which formed behind the moraine. Due to the flat stream bed, the water moves slowly, allowing sediment to settle at the bottom. Restoration.

Geographic entities mentioned:
surface_form: peoria lake
instance_of: Lake
countries: United States
coordinates: lat: 40.702222222222
lon: -89.554444444444
surface_form: upper peoria lake
instance_of: Lake
countries: United States
coordinates: lat: 40.806666666667
lon: -89.551111111111
Sedimentation and the soft bottom of the lake are not conducive for aquatic plants, which attract waterfowl. Fauna. Pollution has been a significant factor in decreasing levels of wildlife. Fish. Several species of fish are listed by the Illinois Department of Natural Resources for Upper Peoria Lake. Waterfowl. Upper Peoria Lake is a notable wildlife refuge for migrating waterfowl. Recreation.

Geographic entities mentioned:
surface_form: peoria lake
instance_of: Lake
countries: United States
coordinates: lat: 40.702222222222
lon: -89.554444444444
surface_form: upper peoria lake
instance_of: Lake
countries: United States
coordinates: lat: 40.806666666667
lon: -89.551111111111
Fauna. Pollution has been a significant factor in decreasing levels of wildlife. Fish. Several species of fish are listed by the Illinois Department of Natural Resources for Upper Peoria Lake. Waterfowl. Upper Peoria Lake is a notable wildlife refuge for migrating waterfowl. Recreation. The lake is currently a regional tourist attraction and is used for practice of many watersports.

Geographic entities mentioned:
surface_form: peoria lake
instance_of: Lake
countries: United States
coordinates: lat: 40.702222222222
lon: -89.554444444444
surface_form: upper peoria lake
instance_of: Lake
countries: United States
coordinates: lat: 40.806666666667
lon: -89.551111111111
The event is organized by the NGO Jõgeva MC. History. The first event took place in 1992 by the lake Peipus, it was organized for the first time by a legendary local motorcycle enthusiast Igor Ellisson (&quot;10. VI 1954 – 11. VII 2021&quot;), Jõgeva county citizen of the year 2012, In 2009, he was awarded the Silver Cross of Jõgeva County () and in 2011 the Order of the White Star. Organization.

Geographic entities mentioned:
surface_form: Peipus
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
Civil War. With the advent of the American Civil War, De Forest returned to the United States. As a captain in the Union Army, he organized a company from New Haven, the 12th Connecticut Volunteers. He served constantly in the field until January 1865, taking an active part under Maj. Gen. Godfrey Weitzel's command in the southwestern states, and under Philip Sheridan in the Shenandoah Valley.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Castle Mountain () is a mountain located within Banff National Park in the Canadian Rockies, approximately halfway between Banff and Lake Louise. It is the easternmost mountain of the Main Ranges in the Bow Valley and sits astride the Castle Mountain Fault which has thrust older sedimentary and metamorphic rocks forming the upper part of the mountain over the younger rocks forming its base.

Geographic entities mentioned:
surface_form: Bow Valley
instance_of: Valley
countries: Canada
coordinates: lat: 51.1671
lon: -115.48
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.29972222222222
lon: -115.9225
surface_form: the castle
instance_of: Mountain
countries: Canada
coordinates: lat: 49.69
lon: -123.2
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.03944444444444
lon: -116.4486111111111
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Internees were held at the Cave & Basin site during the winter months. Construction began in 1910 at Castle Junction on a highway connecting British Columbia to Calgary that would, upon its completion in the early 1920s, make Castle Mountain more accessible to climbers, hikers and other tourists. At a meeting of the Ottawa Canadian Club in January 1946 at which World War II general Dwight D.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.29972222222222
lon: -115.9225
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.03944444444444
lon: -116.4486111111111
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Castle Mountain. Castle Mountain () is a mountain located within Banff National Park in the Canadian Rockies, approximately halfway between Banff and Lake Louise.

Geographic entities mentioned:
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.29972222222222
lon: -115.9225
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.03944444444444
lon: -116.4486111111111
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Castle Mountain. Castle Mountain () is a mountain located within Banff National Park in the Canadian Rockies, approximately halfway between Banff and Lake Louise.

Geographic entities mentioned:
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.29972222222222
lon: -115.9225
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.03944444444444
lon: -116.4486111111111
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Eisenhower. Public pressure caused its original name to be restored, but a pinnacle on the southeastern side of the mountain was named Eisenhower Tower. Located nearby are the remains of Silver City, a 19th-century mining settlement, and the Castle Mountain Internment Camp in which persons deemed enemy aliens and suspected enemy sympathizers were confined during World War I.

Geographic entities mentioned:
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.29972222222222
lon: -115.9225
surface_form: the castle
instance_of: Mountain
countries: Canada
coordinates: lat: 49.69
lon: -123.2
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.03944444444444
lon: -116.4486111111111
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Technicians use a helicopter rather than hiking the long ascent to the top. Geology. Castle Mountain is the easternmost member of the Main Ranges in the Bow Valley. Passing through the mountain is the Castle Mountain Fault, a thrust fault which separates it and the other nearby peaks of the Main Ranges from the Sawback Range to the northeast, the westernmost of the Front Ranges in the region.

Geographic entities mentioned:
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.29972222222222
lon: -115.9225
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.03944444444444
lon: -116.4486111111111
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: bow valley
instance_of: Valley
countries: Canada
coordinates: lat: 51.1671
lon: -115.48
Technicians use a helicopter rather than hiking the long ascent to the top. Geology. Castle Mountain is the easternmost member of the Main Ranges in the Bow Valley. Passing through the mountain is the Castle Mountain Fault, a thrust fault which separates it and the other nearby peaks of the Main Ranges from the Sawback Range to the northeast, the westernmost of the Front Ranges in the region.

Geographic entities mentioned:
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.29972222222222
lon: -115.9225
surface_form: the castle
instance_of: Mountain
countries: Canada
coordinates: lat: 49.69
lon: -123.2
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.03944444444444
lon: -116.4486111111111
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Castle Mountain's upper sections, including its cliff faces, consist of late Pre-Cambrian and Cambrian age sedimentary rocks such as limestone and shale along with some metamorphic quartzite. Originally deposited in an ancient shallow sea, these deposits were later thrust over younger layers of late Paleozoic and Mesozoic age which now form the forested, gently sloping, base of Castle Mountain.

Geographic entities mentioned:
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.29972222222222
lon: -115.9225
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.03944444444444
lon: -116.4486111111111
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
First Nations land claim. On January 25, 2017, the Government of Canada and the Siksika Nation announced an agreement to settle a land claim in the region of Castle Mountain, known as &quot;Miistukskoowa&quot; to the Siksika.

Geographic entities mentioned:
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.29972222222222
lon: -115.9225
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.03944444444444
lon: -116.4486111111111
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
On January 25, 2017, the Government of Canada and the Siksika Nation announced an agreement to settle a land claim in the region of Castle Mountain, known as &quot;Miistukskoowa&quot; to the Siksika. The agreement ended an outstanding claim dating back to the 1880s when land located at Castle Mountain was set aside as a timber berth for the use and benefit of the First Nation.

Geographic entities mentioned:
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.29972222222222
lon: -115.9225
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.03944444444444
lon: -116.4486111111111
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The basis of the claim was that these lands were wrongfully taken from the First Nation in 1908 without their consent and without proper compensation. In 1911, these lands at Castle Mountain were added to Rocky Mountain Park, now known as Banff National Park.

Geographic entities mentioned:
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.29972222222222
lon: -115.9225
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.03944444444444
lon: -116.4486111111111
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
First Nation members voted to approve the settlement on March 4, 2016. Canada gave its final approval on August 15, 2016. History. The first known climber to reach the top of Castle Mountain was Arthur P. Coleman, a professor at the University of Toronto, in 1884. Lawrence Grassi and P. Cerutti, both from Canmore, were the first to climb Eisenhower Tower in 1926.

Geographic entities mentioned:
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.29972222222222
lon: -115.9225
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.03944444444444
lon: -116.4486111111111
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
In 1881, Joe Healy received some ore in trade from an Indigenous person which was discovered to contain a relatively high silver content. The following year he settled at Castle Mountain as a prospector. News of Healy's ore soon spread; others began to arrive and the settlement of Silver City, situated near Castle Mountain, quickly developed.

Geographic entities mentioned:
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.29972222222222
lon: -115.9225
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.03944444444444
lon: -116.4486111111111
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The following year he settled at Castle Mountain as a prospector. News of Healy's ore soon spread; others began to arrive and the settlement of Silver City, situated near Castle Mountain, quickly developed. It was already thriving when the Canadian Pacific transcontinental railroad was built through the area in 1884.

Geographic entities mentioned:
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.29972222222222
lon: -115.9225
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.03944444444444
lon: -116.4486111111111
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Over three thousand people lived there at its height, but it was almost entirely abandoned in 1885 because the mines failed to yield a significant profit. Situated nearby is Castle Mountain Internment Camp, a First World War internment camp where Ukrainian immigrants to Canada were confined.

Geographic entities mentioned:
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.29972222222222
lon: -115.9225
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.03944444444444
lon: -116.4486111111111
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Situated nearby is Castle Mountain Internment Camp, a First World War internment camp where Ukrainian immigrants to Canada were confined. Life in the camps was often described as 'grim'; with its isolated location far from the roads of the time, the Castle Mountain camp was an ideal place to confine 'enemy aliens' and 'suspected enemy sympathisers'.

Geographic entities mentioned:
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.29972222222222
lon: -115.9225
surface_form: the castle
instance_of: Mountain
countries: Canada
coordinates: lat: 49.69
lon: -123.2
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.03944444444444
lon: -116.4486111111111
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Internees were held at the Cave & Basin site during the winter months. Construction began in 1910 at Castle Junction on a highway connecting British Columbia to Calgary that would, upon its completion in the early 1920s, make Castle Mountain more accessible to climbers, hikers and other tourists. At a meeting of the Ottawa Canadian Club in January 1946 at which World War II general Dwight D.

Geographic entities mentioned:
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.29972222222222
lon: -115.9225
surface_form: castle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.03944444444444
lon: -116.4486111111111
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
we have a mountain named Castle and we have thought that to change the name to Mount Eisenhower we would pay a tribute in the form of permanency expressing our admiration years after the castle in Scotland has completely disappeared.&quot; Immediate reaction was mixed; many Banff residents approved, but a telegram sent to King in the name of &quot;members of the ski clubs and climbing clubs of the Rocky Mountains&quot; protested the &quot;inappropriate name of Eisenhower Peak&quot;.

Geographic entities mentioned:
surface_form: the castle
instance_of: Mountain
countries: Canada
coordinates: lat: 49.69
lon: -123.2
The trail to Rockbound Lake leads hikers around the eastern side. The massif contains several high points including Helena Ridge (), Stuart Knob () and Television Peak (), the latter being named for the TV repeater located on top. Technicians use a helicopter rather than hiking the long ascent to the top. Geology. Castle Mountain is the easternmost member of the Main Ranges in the Bow Valley.

Geographic entities mentioned:
surface_form: television peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3817
lon: -116.0169
The mountain's castellated, or castle-like, appearance is a result of erosive processes acting at different rates on the peak's alternating layers of softer shale and harder limestone, dolomite and quartzite. The mountain was named in 1858 by James Hector for its castle-like appearance. From 1946 to 1979 it was known as Mount Eisenhower in honour of the World War II general Dwight D. Eisenhower.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Eisenhower. Public pressure caused its original name to be restored, but a pinnacle on the southeastern side of the mountain was named Eisenhower Tower. Located nearby are the remains of Silver City, a 19th-century mining settlement, and the Castle Mountain Internment Camp in which persons deemed enemy aliens and suspected enemy sympathizers were confined during World War I.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
It is an example of a castellated mountain in which erosion has sculpted a series of flat or gently sloping terraces composed of softer shale and sharp cliffs which reveal alternating layers of shale interspersed by harder layers of quartzite, dolomite and limestone. First Nations land claim.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
At a meeting of the Ottawa Canadian Club in January 1946 at which World War II general Dwight D. Eisenhower was a guest speaker, Prime Minister Mackenzie King renamed Castle Mountain in his honour. Alluding to Scotland's recent gift to Eisenhower of a castle, King said, &quot;We haven't any ancient castles, but we have something more enduring, we have ancient mountains...

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
A change of name was already planned by 1976, but its implementation was delayed to avoid causing offense on account of the United States Bicentennial commemorations taking place that year. The mountain was officially renamed Castle Mountain in November 1979, but an isolated pinnacle at the southeastern end was designated Eisenhower Tower. Scramble route.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Scramble route. While the peak presents a formidable challenge to climb when viewed from the highway, the mountain can be ascended by first hiking to Rockbound Lake which is located on the easier backside. A break in a cliff band provides access to a route above the lake. The ascent is a very long day when undertaken from the trailhead and can easily require 12 hours for a return trip.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Fighting erupted on the streets of Beirut as a Muslim mob burned the US Information Service library down. Heightened tensions existed around the country, including in the Beqaa Valley, where Shia militants were receiving weapons from Syria. &quot;The New York Times&quot; dated the beginning of a formal armed rebellion to 10 May 1958.

Geographic entities mentioned:
surface_form: Beqaa Valley
instance_of: Valley
countries: Lebanon
coordinates: lat: 34.008888888889
lon: 36.145277777778
Skoddevarre. Skoddevarre () is a mountain in Alta Municipality in Finnmark county, Norway. The mountain has several peaks, the tallest of which is located in the east, reaching above sea level. The &quot;Great Norwegian Encyclopedia&quot; states that the highest peak is and is located in the north.

Geographic entities mentioned:
surface_form: skoddevarre
instance_of: Mountain
countries: Norway
coordinates: lat: 69.93583333333333
lon: 23.145833333333332
Nearby settlements include the village of Kvenvik northwest of the mountain and the town of Alta to the northeast. The European route E6 runs north of the mountain between the settlements. The west wall at Skoddevarre is high and is used for rock climbing. The bedrock consists of sandstone and greenschist. The &quot;Gubben&quot; formation is a pinnacle in the middle of the rock.

Geographic entities mentioned:
surface_form: skoddevarre
instance_of: Mountain
countries: Norway
coordinates: lat: 69.93583333333333
lon: 23.145833333333332
By the time they exited the city, the history included Smith's story up until March 1, 1843. Henry Fairbanks and Thomas Bullock transported the manuscript across the Great Plains. Bullock brought them into the Salt Lake Valley under the direction of Willard Richards. No significant progress was made on the history thereafter until George A. Smith became church historian.

Geographic entities mentioned:
surface_form: Salt Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.6839
lon: -111.978
Buur Ecological and Archaeological Project (BEAP). The Buur Ecological and Archaeological Project (BEAP) is a long-term multidisciplinary study of Late Pleistocene and Holocene subsistence and settlement patterns in the inter-riverine region of southern Somalia, focusing primarily on the Jubba and Shebelle river valleys..

Geographic entities mentioned:
surface_form: Jubba
instance_of: Valley
countries: Ethiopia
Somalia
Kenya
coordinates: lat: 4.1772222222222
lon: 42.079444444444
surface_form: Shebelle
instance_of: Valley
countries: Ethiopia
Somalia
coordinates: lat: 4.7333333333333
lon: 45.2
Buur Heybe. Buur Heybe, which translates to &quot;The Hill of the Potter's Sand&quot;, is a late Pleistocene and Holocene archaeological complex located in the largest granite inselberg in the inter-riverine region of the southern Bay province of Somalia approximately 180 km northwest of the capital Mogadishu.

Geographic entities mentioned:
surface_form: buur heybe
instance_of: Mountain
countries: Somalia
coordinates: lat: 3
lon: 44.3
Buur Heybe. Buur Heybe, which translates to &quot;The Hill of the Potter's Sand&quot;, is a late Pleistocene and Holocene archaeological complex located in the largest granite inselberg in the inter-riverine region of the southern Bay province of Somalia approximately 180 km northwest of the capital Mogadishu.

Geographic entities mentioned:
surface_form: buur heybe
instance_of: Mountain
countries: Somalia
coordinates: lat: 3
lon: 44.3
surface_form: buur heybe
instance_of: Mountain
countries: Somalia
coordinates: lat: 3
lon: 44.3
Buur Heybe has a longstanding history of archaeological research dating back to the 1930s when Paolo Graziosi carried out the first professional archaeological excavation in Somalia in the rockshelter site of Gogoshiis Qabe in Buur Heybe. Further excavations by J.

Geographic entities mentioned:
surface_form: buur heybe
instance_of: Mountain
countries: Somalia
coordinates: lat: 3
lon: 44.3
Further excavations by J. Desmond Clark in the 1950s and later by the Buur Ecological and Archaeological Project (BEAP) led by Steven Brandt in the 1980s have made Buur Heybe one of the best dated and closely studied archaeological sites in Somalia.

Geographic entities mentioned:
surface_form: buur heybe
instance_of: Mountain
countries: Somalia
coordinates: lat: 3
lon: 44.3
Furthermore, as war consumed Mogadishu the Somali National Museum was looted resulting in the destruction of all BEAP archaeological collections which included soil samples, lithics, and human skeletons from Buur Heybe and Guli Waabayo.

Geographic entities mentioned:
surface_form: buur heybe
instance_of: Mountain
countries: Somalia
coordinates: lat: 3
lon: 44.3
At ~4.7 kmformula_1 in dimension and rising 610m above sea level (a.s.l) Buur Heybe stands out as the largest inselberg in the Buur Region creating a unique ecological environment that supports diverse ecosystems of different species of plants and animals, creating an ecologically-productive environment for small animals such as dik-dik and hyrax.

Geographic entities mentioned:
surface_form: buur heybe
instance_of: Mountain
countries: Somalia
coordinates: lat: 3
lon: 44.3
According to Brandt, Gogoshiis Qabe and Guli Waabayo are two of ~100 rockshelter sites found in Buur Heybe, most of which are believed to date back to the early/mid Holocene based on pottery and stone tools artifacts. Additionally, it's worth mentioning the Buur Hakaba inselberg, ~25km from Buur Heybe, as another important archaeological site in the Buur Region. Excavated by J.

Geographic entities mentioned:
surface_form: buur heybe
instance_of: Mountain
countries: Somalia
coordinates: lat: 3
lon: 44.3
Excavated by J. Desmond Clark and Steven Brandt, the Rifle Range Site contributes to our limited, but important understanding of Somali archaeology. Somalia's first archaeological excavation was carried out by Italian archaeologist Paolo Graziosi when he excavated the rockshelter site of Gogishiis Qabe at Buur Heybe in 1935.

Geographic entities mentioned:
surface_form: buur heybe
instance_of: Mountain
countries: Somalia
coordinates: lat: 3
lon: 44.3
Further excavations and analysis carried out by Brandt as a part of the Buur Ecological and Archaeological Project (BEAP) in the 1980s revealed that Clark's 'Doian' industry was identical to Graziosi's Eibian industry and argued that, &quot;most of the culture-histories units formulated by Clark (1954) more than 30 years ago are in need of revision.&quot; Brandt opted to prioritize the original framework of Graziosi's Eibian industry to describe the LSA/terminal Pleistocene industry of Buur Heybe and identified a new early/mid Holocene industry that lacked distinctive Eibian features which he named the Bardaale industry after the local village surrounding Buur Heybe.

Geographic entities mentioned:
surface_form: buur heybe
instance_of: Mountain
countries: Somalia
coordinates: lat: 3
lon: 44.3
surface_form: buur heybe
instance_of: Mountain
countries: Somalia
coordinates: lat: 3
lon: 44.3
A recent study of sixteen new and seven recently published radiocarbon dates of faunal remains (ostrich eggshell) from the Guli Waabayo rockshelter in Buur Heybe have provided evidence of the continuous use of the site for over a ~30,000 year period that covers most of the Marine Isotope Stage (MIS) 2 (~29-14.5ka) and the MIS 1 African Humid Period ~14.5-6 ka.) Using Bayesian analysis to determine the separate phases of occupation at the rockshelter site, researchers were able to discover two major periods of site occupation that align with the lithic evidence and human remains.

Geographic entities mentioned:
surface_form: buur heybe
instance_of: Mountain
countries: Somalia
coordinates: lat: 3
lon: 44.3
Shives, Arkansas. Shives (also Shrives) is an unincorporated community in Chicot County, Arkansas, United States. Shives is located on the southeast shore of Lake Chicot, approximately west of the Mississippi River. U.S. Route 278 passes through Shives, and Shives is the first settlement west of the Greenville Bridge.

Geographic entities mentioned:
surface_form: Lake Chicot
instance_of: Lake
countries: United States
coordinates: lat: 33.3225
lon: -91.278333333333
In late 252, Zhuge Ke gave orders to rebuild the dam at Dongxing (東興; in present-day Chaohu, Anhui), which was constructed earlier in 230 but had been destroyed in 241. His plan was to create a reservoir near the Chao Lake and use it as a defensive structure against potential invasions from Wei, as well as to construct two castles nearby to serve as forward attack mechanisms for Wu ships.

Geographic entities mentioned:
surface_form: Chao Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 31.5282
lon: 117.5227388888889
The range reaches a maximum elevation of at the southern summit of Mount Jefferson. From Hickison Summit on U.S. Route 50, the range runs for approximately to the south-southwest. To its west are Big Smoky Valley, scenic State Route 376, and the large Toiyabe Range. To the east are remote Monitor Valley and the Monitor Range. Lying to the south of the range are U.S.

Geographic entities mentioned:
surface_form: Big Smoky Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.6644
lon: -117.171
Electric River. The Electric River is a river of Fiordland, New Zealand. It arises around Lake Jaquiery in the Kaherekoau Mountains and flows eastward into Lake Monowai at June Bay.

Geographic entities mentioned:
surface_form: Lake Monowai
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.866666666667
lon: 167.45
Bezliudivka. Lake Nahorivske and Lake Pidborivske are located in the settlement. History. Bezlyudivka was first mentioned in 1677. It was a village in Kharkov uyezd of Kharkov Governorate of the Russian Empire. In 1938, it was classified as an urban-type settlement.

Geographic entities mentioned:
surface_form: Lake Nahorivske
instance_of: Lake
countries: Ukraine
coordinates: lat: 49.856388888889
lon: 36.278333333333
surface_form: Lake Pidborivske
instance_of: Lake
countries: Ukraine
coordinates: lat: 49.879444444444
lon: 36.260277777778
Agrour Amogjar. The Agrour Amogjar is a 690 m high peak near the Amogjar Pass, in the Adrar plateau of central Mauritania. Its small natural shelters house a rich collection of rock paintings in a damaged state. An enclosure protects some of the shelters and access is subject to a fee. Rock paintings. The set of rock paintings is heterogeneous.

Geographic entities mentioned:
surface_form: Adrar plateau
instance_of: Plateau
countries: Mauritania
coordinates: lat: 20.405277777778
lon: -13.111111111111
surface_form: agrour amogjar
instance_of: Mountain
countries: Mauritania
coordinates: lat: 20.633888888889
lon: -12.724166666667
Agrour Amogjar. The Agrour Amogjar is a 690 m high peak near the Amogjar Pass, in the Adrar plateau of central Mauritania. Its small natural shelters house a rich collection of rock paintings in a damaged state. An enclosure protects some of the shelters and access is subject to a fee. Rock paintings. The set of rock paintings is heterogeneous.

Geographic entities mentioned:
surface_form: agrour amogjar
instance_of: Mountain
countries: Mauritania
coordinates: lat: 20.633888888889
lon: -12.724166666667
Yosemite Village Historic District. The Yosemite Village Historic District encompasses the primary built-up section of the Yosemite Valley as it was developed by the National Park Service for Yosemite National Park. The district includes visitor services areas, park personnel residences and administrative facilities. It is located to the north of the Merced River.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
Nelles Peak. Nelles Peak is a remote mountain summit located in the Coast Mountains of British Columbia, Canada. It is situated at the northeastern periphery of the Juneau Icefield, inside the BC-Alaska boundary, on the west side of Tulsequah Lake. Its nearest higher peak is Devils Paw, to the southeast. Nelles Peak is the second-highest summit of the icefield, after Devils Paw.

Geographic entities mentioned:
surface_form: Devils Paw
instance_of: Mountain
countries: Canada
United States
coordinates: lat: 58.730833333333
lon: -133.83972222222
Nelles Peak. Nelles Peak is a remote mountain summit located in the Coast Mountains of British Columbia, Canada. It is situated at the northeastern periphery of the Juneau Icefield, inside the BC-Alaska boundary, on the west side of Tulsequah Lake. Its nearest higher peak is Devils Paw, to the southeast. Nelles Peak is the second-highest summit of the icefield, after Devils Paw.

Geographic entities mentioned:
surface_form: nelles peak
instance_of: Mountain
countries: Canada
coordinates: lat: 58.8044
lon: -133.9154
Nelles Peak. Nelles Peak is a remote mountain summit located in the Coast Mountains of British Columbia, Canada. It is situated at the northeastern periphery of the Juneau Icefield, inside the BC-Alaska boundary, on the west side of Tulsequah Lake. Its nearest higher peak is Devils Paw, to the southeast. Nelles Peak is the second-highest summit of the icefield, after Devils Paw.

Geographic entities mentioned:
surface_form: nelles peak
instance_of: Mountain
countries: Canada
coordinates: lat: 58.8044
lon: -133.9154
surface_form: remote mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4664
lon: -125.51975
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
It is situated at the northeastern periphery of the Juneau Icefield, inside the BC-Alaska boundary, on the west side of Tulsequah Lake. Its nearest higher peak is Devils Paw, to the southeast. Nelles Peak is the second-highest summit of the icefield, after Devils Paw. The mountain was named in 1924 to honor Douglas H.

Geographic entities mentioned:
surface_form: nelles peak
instance_of: Mountain
countries: Canada
coordinates: lat: 58.8044
lon: -133.9154
Climate. Based on the Köppen climate classification, Nelles Peak has a subarctic climate with cold, snowy winters, and mild summers.. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall.

Geographic entities mentioned:
surface_form: nelles peak
instance_of: Mountain
countries: Canada
coordinates: lat: 58.8044
lon: -133.9154
As a result, the Coast Mountains experience high precipitation, especially during the winter months in the form of snowfall. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Nelles Peak drains into the Tulsequah River which in turn empties into Taku River. The month of July offers the most favorable weather for viewing and climbing Nelles.

Geographic entities mentioned:
surface_form: nelles peak
instance_of: Mountain
countries: Canada
coordinates: lat: 58.8044
lon: -133.9154
Veslehorn. Veslehorn, also written Veslehødn, is a mountain located in the Hemsedal municipality in Norway. It is a part of Hemsedal Top 20.

Geographic entities mentioned:
surface_form: veslehorn
instance_of: Mountain
countries: Norway
coordinates: lat: 60.816944444444
lon: 8.6169444444444
As with Gardner an instrument, possibly a branch, had been inserted into her vagina. She also had a large gash that ran from the inside of her thigh up to her mutilated breast. Some of her possessions were found at the beach huts at Alum Chine. Although Heath was charged with Doreen's murder, his subsequent trial and execution related only to his earlier murder of Gardner.

Geographic entities mentioned:
surface_form: Alum Chine
instance_of: Valley
countries: United Kingdom
coordinates: lat: 50.712666666666664
lon: -1.8976944444444444
Mummies Hall. The Royal Mummies’ Hall is designed to display the mummies of the ancient monarchs of Egypt. The design aims to give the visitor the feeling of strolling down the Valley of the Kings, where most of these mummies were originally resting. The hall includes 20 royal mummies, 18 kings, and 2 queens, from the 17th to the 20th dynasties. Textile Hall.

Geographic entities mentioned:
surface_form: Valley of the Kings
instance_of: Valley
countries: Egypt
coordinates: lat: 25.74025
lon: 32.602358
Blue Hill (New York). Blue Hill is a mountain in Sullivan County, New York. It is located west-southwest of Claryville. Denman Mountain is located east-southeast of Blue Hill.

Geographic entities mentioned:
surface_form: Denman Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.902777777778
lon: -74.539722222222
surface_form: blue hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.911666666667
lon: -74.619166666667
Blue Hill (New York). Blue Hill is a mountain in Sullivan County, New York. It is located west-southwest of Claryville. Denman Mountain is located east-southeast of Blue Hill.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: blue hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.911666666667
lon: -74.619166666667
Blue Hill (New York). Blue Hill is a mountain in Sullivan County, New York. It is located west-southwest of Claryville. Denman Mountain is located east-southeast of Blue Hill.

Geographic entities mentioned:
surface_form: blue hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.911666666667
lon: -74.619166666667
Elk Lake (Douglas County, Minnesota). Elk Lake is a lake in Douglas County, in the U.S. state of Minnesota. Elk Lake was named for the elk which frequented it.

Geographic entities mentioned:
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9742
lon: -121.802
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 44.025277777778
lon: -115.07138888889
surface_form: elk lake (douglas county, minnesota)
instance_of: Lake
countries: United States
coordinates: lat: 45.919166666667
lon: -95.521944444444
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 45.867222222222
lon: -95.804722222222
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 44.85
lon: -85.3833
Elk Lake (Douglas County, Minnesota). Elk Lake is a lake in Douglas County, in the U.S. state of Minnesota. Elk Lake was named for the elk which frequented it.

Geographic entities mentioned:
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9742
lon: -121.802
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 44.025277777778
lon: -115.07138888889
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 45.919166666667
lon: -95.521944444444
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 45.867222222222
lon: -95.804722222222
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 44.85
lon: -85.3833
Later, he became a powerful minister and military general of kingdom Magadha (Ancient Bengal, Ancient India) under the Solar dynasty. He was later awarded the title of King who then ruled a city named &quot;Visana&quot; or &quot;Alaka&quot; in North, possibly in Tibet, China located near Himalayan region (500-1000BC).

Geographic entities mentioned:
surface_form: Tibet
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Bois de Sioux River. The Bois de Sioux River () drains Lake Traverse, the southernmost body of water in the Hudson Bay watershed of North America. It is a tributary of the Red River of the North and defines part of the western border of the U.S. state of Minnesota, and the eastern borders of North Dakota and South Dakota. It is about in length.

Geographic entities mentioned:
surface_form: Lake Traverse
instance_of: Lake
countries: United States
coordinates: lat: 45.769166666667
lon: -96.638888888889
Bois de Sioux is a name derived from French meaning &quot;Woods of the Sioux&quot;. Course. The river flows northward from a Corps of Engineers dam at the north end of Lake Traverse and shortly enters Mud Lake. Downstream of Mud Lake it is a small stream, and its flow has been channelized and straightened in some places so that the watercourse diverges slightly from the historical state boundary.

Geographic entities mentioned:
surface_form: Lake Traverse
instance_of: Lake
countries: United States
coordinates: lat: 45.769166666667
lon: -96.638888888889
Blackstairs Mountains. The Blackstairs Mountains () run roughly north/south along the border between County Carlow and County Wexford in Ireland. The highest peak is Mount Leinster with a total height of. Blackstairs Mountain is the second highest peak at.

Geographic entities mentioned:
surface_form: Mount Leinster
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.617
lon: -6.778
Blackstairs Mountains. The Blackstairs Mountains () run roughly north/south along the border between County Carlow and County Wexford in Ireland. The highest peak is Mount Leinster with a total height of. Blackstairs Mountain is the second highest peak at.

Geographic entities mentioned:
surface_form: Blackstairs Mountain
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.549705555556
lon: -6.8061972222222
Kilmacolm. Kilmacolm () is a village and civil parish in the Inverclyde council area, and the historic county of Renfrewshire in the west central Lowlands of Scotland. It lies on the northern slope of the Gryffe Valley, southeast of Greenock and around west of the city of Glasgow.

Geographic entities mentioned:
surface_form: central Lowlands
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.408
lon: -4.044