Sarmila/GeoWiki-Features huggingface dataset:
Betws Garmon. Betws Garmon is a community and small hamlet outside Waunfawr and near Beddgelert in Gwynedd, Wales. It has a population of 249. The summit of Snowdon lies within the community boundaries. Bryn Gloch has the newly reopened narrow gauge Welsh Highland Railway passing alongside it. The hamlet of Rhyd-Ddu is in the community. Over the road from Bryn Gloch there is a parish church.

Geographic entities mentioned:
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
He was hanged on December 23 of that year, in front of his gathered brigade. By March 1862, the regiment had crossed the Potomac and reached Winchester, Virginia, beginning their part in what was to become the Valley Campaign. After a brief foray to Manassas, they were ordered back to Winchester and subsequently started a long march up the Shenandoah Valley, reaching as far south as Harrisonburg.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Cime di Val Loga. Cime di Val Loga is a mountain of Lombardy, Italy.

Geographic entities mentioned:
surface_form: cime di val loga
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 46.47472222
lon: 9.27611111
Black River Escarpment (Wisconsin). The Black River Escarpment is a geological feature in Eastern Wisconsin. The escarpment runs parallel to and between the Niagara Escarpment and the Magnesian Escarpment. The escarpment marks the boundary between bedrock from Lower Magnesian limestone bedrock and earlier Black River limestone. The escarpment emerges from Green Bay, on Lake Michigan.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
The escarpment runs parallel to and between the Niagara Escarpment and the Magnesian Escarpment. The escarpment marks the boundary between bedrock from Lower Magnesian limestone bedrock and earlier Black River limestone. The escarpment emerges from Green Bay, on Lake Michigan. The escarpment's boundaries are not always visible to the untrained eye, but are marked by cliffs in some regions.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Hessdalen lights. The Hessdalen lights are unidentified lights which have been observed in a stretch of the Hessdalen valley in rural central Norway periodically since at least the 1930s. Background. The Hessdalen lights appear both by day and by night, and seem to float through and above the valley. They are usually bright white, yellow or red and can appear above and below the horizon.

Geographic entities mentioned:
surface_form: Hessdalen
instance_of: Valley
countries: Norway
coordinates: lat: 62.793055555556
lon: 11.188055555556
Despite this, Robert Gunther states that his numerous connections in Wales made him a &quot;welcome enquirer everywhere.&quot;
Ireland and Scotland (1699–1700). From Wales, Lhuyd and his team reached Ireland in July or August 1699, landing in Dublin, then travelled to Antrim and visited Newgrange and the Giant's Causeway.

Geographic entities mentioned:
surface_form: Giant's Causeway
instance_of: Landform
countries: United Kingdom
coordinates: lat: 55.240833333333
lon: -6.5116666666667
Störner. Störner is a mountain of Hesse, Germany. They are in the Natural regions number 32.

Geographic entities mentioned:
surface_form: störner
instance_of: Mountain
countries: Germany
coordinates: lat: 50.8333
lon: 8.63333
Unalakleet River. The Unalakleet River (Iñupiaq: &quot;Uŋalaqłiit Kurgat&quot;) in the U.S. state of Alaska flows southwest from the Kaltag Mountains to near the town of Unalakleet, on Norton Sound of the Bering Sea. In 1980, the upper of the river was protected as &quot;wild&quot; as part of the National Wild and Scenic Rivers System.

Geographic entities mentioned:
surface_form: Norton Sound
instance_of: Landform
countries: United States
coordinates: lat: 63.849166666667
lon: -164.26888888889
Route description. From the California border, US 6 heads northeast through semidesert Queen Valley with Boundary Peak, Nevada's highest summit, and Montgomery Peak in California on the right. These twin peaks are the northernmost high summits of the White Mountains, both over. The highway then climbs into pinyon–juniper woodland and crosses Montgomery Pass.

Geographic entities mentioned:
surface_form: Montgomery Peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.838263888889
lon: -118.35678611111
These twin peaks are the northernmost high summits of the White Mountains, both over. The highway then climbs into pinyon–juniper woodland and crosses Montgomery Pass. From the pass, US 6 descends into barren shadscale desert, passing Columbus Marsh on the left, then merging with US 95 from Coaldale to Tonopah. The Nevada Test and Training Range begins about southeast of Tonopah.

Geographic entities mentioned:
surface_form: Columbus Marsh
instance_of: Valley
countries: United States
coordinates: lat: 38.0858
lon: -117.965
Rosebud Summit. Rosebud Summit is a peak that constitutes the northeasternmost point in the Rosebud Ridge of the White Mountains in central Alaska. The mountain is traversed by the trail of the annual Yukon Quest 1,000-mile sled dog race. It lends its name to nearby Rosebud Creek.

Geographic entities mentioned:
surface_form: rosebud summit
instance_of: Mountain
countries: United States
coordinates: lat: 65.239380555556
lon: -145.82733333333
He became to Deputy Minister of Justice of Canada and Deputy Attorney General in 1924, in succession to Edmund Leslie Newcombe, CMG, KC, who had been appointed as a puisne justice of the Supreme Court of Canada. Edwards retired in 1941 owing to ill health. He was succeeded by F. P. Varcoe. He died in 1944 at Blue Sea Lake, Quebec. He was a nephew of Senator William Cameron Edwards.

Geographic entities mentioned:
surface_form: Blue Sea Lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.2167
lon: -76.0556
However, the government soon reconsidered its decision in light of the June 1989 pogroms against minorities in the Fergana valley where Crimean Tatars were exiled to, resulting in the formation of the Yanayev commission to readdress the possibility of allowing Crimean Tatars to return to Crimea.

Geographic entities mentioned:
surface_form: Fergana valley
instance_of: Valley
countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
lon: 71.757777777778
One of Pema Lingpa's most renowned treasure discoveries took place in Bhutan at Mebartso [burning lake], where before a large crowd he leaped into deep water with a burning butter lamp in his hand, later emerging with a term in one hand and the still burning butter lamp in the other. His works are popular and have flourished in each and every corner of the Himalayas.

Geographic entities mentioned:
surface_form: Mebartso
instance_of: Lake
countries: Bhutan
coordinates: lat: 27.53950556
lon: 90.81234444
Bumthang Valley. Bumthang Valley is the main inhabited valley in the Bumthang district of Bhutan. History. Bumthang is one of the most beautiful and sacred valleys in Bhutan. The main town in the valley is Jakar. Bhutan's only brewery, brewing Red Panda wheat beer, is in Jakar. Bumthang is divided into four &quot;gewogs&quot;, namely Chhoekhor, Tang, Chhume and Ura.

Geographic entities mentioned:
surface_form: bumthang valley
instance_of: Valley
countries: Bhutan
coordinates: lat: 27.55
lon: 90.75
At low altitudes, there is a forest (mainly Tien Shan spruce), and then from there is a subalpine zone, even higher — glaciers. Here there are four of the most famous and visited lakes of the Almaty Region: three Kolsay lakes and Lake Kaindy in the gorges of the Kolsay and the Kaindy. The Kungey ridge is interesting in mountaineering terms, as a little &quot;conquered&quot; ridge.

Geographic entities mentioned:
surface_form: Lake Kaindy
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 42.984611111111
lon: 78.465686111111
Küngöy Ala-Too Range. The Kungey Alatau (, &quot;Küngöy Ala-Too&quot;;, &quot;Küngei Alataw&quot;), also spelled Kungoy Ala-Too, and Kungey Alataw, is a mountain range, which forms the northern Tien Shan with Zailiyskiy Alatau.

Geographic entities mentioned:
surface_form: kungey alatau
instance_of: Mountain
countries: Kyrgyzstan
coordinates: lat: 42.776166
lon: 76.690021
The Chilik-Kemin Bridge connecting the two ridges separates the Chon-Kemin and Chilik valleys. The border of Kazakhstan and Kyrgyzstan, which runs along the Zailiysky Alatau ridge in the west, passes over the Chiliko-Kemin Bridge to the Kungey Alatau ridge.

Geographic entities mentioned:
surface_form: kungey alatau
instance_of: Mountain
countries: Kyrgyzstan
coordinates: lat: 42.776166
lon: 76.690021
Here the Kumbel ridge leads off in a southeasterly direction. The largest river of the southern slope of the Kungey Alatau, Chon-Ak-Suu, which flows into Issyk-Kul, begins at this point and flows in an easterly direction, so that the northern slope of its valley is the main ridge of the Kungey Alatau, and the southern ridge of the Kumbel.

Geographic entities mentioned:
surface_form: kungey alatau
instance_of: Mountain
countries: Kyrgyzstan
coordinates: lat: 42.776166
lon: 76.690021
surface_form: issyk-kul
instance_of: Lake
countries: Kyrgyzstan
coordinates: lat: 42.416666666667
lon: 77.25
Küngöy Ala-Too Range. The Kungey Alatau (, &quot;Küngöy Ala-Too&quot;;, &quot;Küngei Alataw&quot;), also spelled Kungoy Ala-Too, and Kungey Alataw, is a mountain range, which forms the northern Tien Shan with Zailiyskiy Alatau.

Geographic entities mentioned:
surface_form: küngöy ala-too range
instance_of: Mountain
countries: Kyrgyzstan
coordinates: lat: 42.776166
lon: 76.690021
The meaning of &quot;Zymoetz&quot; is unclear. It may come from a Tsimshianic word meaning &quot;palm of the hand&quot;. Geography. The Zymoetz River originates in the Bulkley Ranges, a subrange of the Hazelton Mountains, on the west side of Hudson Bay Mountain, west of the town of Smithers. The upper Zymoetz River flows westward through Aldrich Lake, Dennis Lake, and McDonell Lake.

Geographic entities mentioned:
surface_form: Hudson Bay Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 54.8116
lon: -127.34
There are numerous high mountains over tall in and along the drainage divides of the Zymoetz watershed, including Howson Peak (2759 m), Hudson Bay Mountain (2589 m), Polemic Peak (2579 m), Mount Sir Robert (2375 m), Andesite Peak (2366 m), Mount Henderson (2325 m), Cumulus Mountain (2292 m), Pillar Peak (2146 m), Mountt Clore (2053 m), and others.

Geographic entities mentioned:
surface_form: Howson Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 54.418611111111
lon: -127.74388888889
surface_form: Hudson Bay Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 54.8116
lon: -127.34
Gunstock Mountain Resort. Gunstock Mountain Resort, originally known as Belknap Mountain Recreation Area, is an outdoor recreation complex located on Gunstock Mountain in Gilford, New Hampshire. Constructed by the Works Progress Administration, it was completed in 1937 and is owned by Belknap County.

Geographic entities mentioned:
surface_form: Gunstock Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.525633333333
lon: -71.378405555556
The resort had the first chairlift in the eastern United States. After the completion of the 60-meter ski jump, the first meet was held in February 1937. The original Gunstock chairlift development was located on Mount Rowe. This single-chairlift-serviced ski area was eventually phased out when two double chairlifts were installed to the Gunstock Mountain summit.

Geographic entities mentioned:
surface_form: Mount Rowe
instance_of: Mountain
countries: United States
coordinates: lat: 43.545277777778
lon: -71.378055555556
zp6c7qz3ppzwpmdp7deckax5ttvs1" xml:space="preserve">Image:A-na-cam-e-gish-ca.jpg|thumb|right|225px|A-na-cam-e-gish-ca (&quot;Enakamigishkang&quot; / &quot;[Traces of] Foot Prints <a href="A%3E.">a>.</a>
Rainy Lake and River Bands of Saulteaux (Ojibwe language: &quot;Gojijiwininiwag&quot;) are Saulteaux (Ojibwe) group located in Northwestern Ontario and northern Minnesota, along and about the Rainy Lake and the Rainy River, known in Ojibwe as &quot;Gojijiing&quot;.

Geographic entities mentioned:
surface_form: Rainy Lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 48.636944444444
lon: -93.031388888889
Uddjaure. Uddjaure is a lake in Norrbotten County, Lappland, Sweden, adjacent to Lake Hornavan.

Geographic entities mentioned:
surface_form: Hornavan
instance_of: Lake
countries: Sweden
coordinates: lat: 66.233333333333
lon: 17.5
surface_form: uddjaure
instance_of: Lake
countries: Sweden
coordinates: lat: 65.966666666667
lon: 17.833333333333
Uddjaure. Uddjaure is a lake in Norrbotten County, Lappland, Sweden, adjacent to Lake Hornavan.

Geographic entities mentioned:
surface_form: uddjaure
instance_of: Lake
countries: Sweden
coordinates: lat: 65.966666666667
lon: 17.833333333333
Before and after becoming a widow, Longstreet devoted much time to ensure that General Longstreet was accurately portrayed by history. In 1905, she documented her husband's account of the Civil War by publishing the book &quot;Lee and Longstreet at High Tide&quot;. Another important cause that she took up about 1911 was the creation of a state park at Tallulah Gorge.

Geographic entities mentioned:
surface_form: Tallulah Gorge
instance_of: Valley
countries: United States
coordinates: lat: 34.725
lon: -83.370277777778
Ripley, New York. Ripley is a town on Lake Erie in the westernmost part of Chautauqua County, New York, United States. The population was 2,310 at the time of the 2020 census. The town was named after Eleazer Wheelock Ripley, a general in the War of 1812. There are no incorporated villages in the town, but there is one census-designated place: the hamlet of Ripley.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Pen-yr-Orsedd quarry. Pen-yr-Orsedd quarry was a slate quarry in the Nantlle Valley in North Wales. It was one of the last slate quarries operating in North Wales and the last operating in the Nantlle Valley area, finally closing in 1979. History.

Geographic entities mentioned:
surface_form: Nantlle Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.025
lon: -4.2833333333333
William Darbishire took over direct management of the quarry that year and by 1882 had raised production to almost 8,000 tons. Pen-yr-Orsedd was one of the major slate producers of the Nantlle Valley. It was the last of the Nantlle quarries to commercially produce slate, closing in 1979. Narrow-gauge railway museum.

Geographic entities mentioned:
surface_form: Nantlle Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.025
lon: -4.2833333333333
It extends at an altitude of 900 to 1.150 meters, built amphitheatrically on the northern slopes of mount Parnon, filled with fir, chestnut, platanus and cherry trees, surrounded by creeks and small waterfalls. The village is spread in two neighborhoods and overlooks the plateau of Tripoli, with the visual horizon reaching the mountains of Mainalo, Artemisio, Helmos and Erymanthos.

Geographic entities mentioned:
surface_form: Mainalo
instance_of: Mountain
countries: Greece
coordinates: lat: 37.6583
lon: 22.2517
surface_form: Erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
It is white in color, with a tone of light blue or blue. It is one of the highest quality marbles in the Peloponnese, showing similarities with the Pentelic marble of Attica, although it does not reach the qualitative characteristics of the latter. It was most primarily used as a building block in antiquity and rarer in sculpture. Greek revolution.

Geographic entities mentioned:
surface_form: Pentelic
instance_of: Mountain
countries: Greece
coordinates: lat: 38.08144
lon: 23.8825
Copper Mountain (Wyoming). Copper Mountain is a roughly 8,312 foot mountain in the Bridger Mountains, a small range that straddles the Fremont and Hot Springs County line. The range rises north of Shoshoni, and is split by Wind River Canyon. The Owl Creek Mountains are west of Wind River Canyon. Copper Mountain is also sometimes known as Bridger's Mountain.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: copper mountain
instance_of: Mountain
coordinates: lat: 43.45944444444445
lon: -107.94472222222223
Geology. Copper Mountain is features Archean rocks of the Wyoming Craton and is overlain in the southern part by Cenozoic sedimentary rocks. Lithium-bearing pegmatite (otherwise known as igneous rock containing crystals) has been found on Copper Mountain, including amblygonite, lepidolite, iron-manganese phosphates, columbite, tapiolite and beryl. Mining.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
surface_form: copper mountain
instance_of: Mountain
coordinates: lat: 43.45944444444445
lon: -107.94472222222223
Copper Mountain (Wyoming). Copper Mountain is a roughly 8,312 foot mountain in the Bridger Mountains, a small range that straddles the Fremont and Hot Springs County line. The range rises north of Shoshoni, and is split by Wind River Canyon. The Owl Creek Mountains are west of Wind River Canyon. Copper Mountain is also sometimes known as Bridger's Mountain.

Geographic entities mentioned:
surface_form: copper mountain
instance_of: Mountain
coordinates: lat: 43.45944444444445
lon: -107.94472222222223
The range rises north of Shoshoni, and is split by Wind River Canyon. The Owl Creek Mountains are west of Wind River Canyon. Copper Mountain is also sometimes known as Bridger's Mountain. Copper Mountain is part of a larger BLM owned parcel known as The Copper Mountain Wildlife Study area, which encompasses 6,858 acres. Most of the mountain is scattered limber pine and juniper with rocky slopes.

Geographic entities mentioned:
surface_form: copper mountain
instance_of: Mountain
coordinates: lat: 43.45944444444445
lon: -107.94472222222223
The Owl Creek Mountains are west of Wind River Canyon. Copper Mountain is also sometimes known as Bridger's Mountain. Copper Mountain is part of a larger BLM owned parcel known as The Copper Mountain Wildlife Study area, which encompasses 6,858 acres. Most of the mountain is scattered limber pine and juniper with rocky slopes. Nearby Boysen Reservoir is visible from Copper Mountain.

Geographic entities mentioned:
surface_form: copper mountain
instance_of: Mountain
coordinates: lat: 43.45944444444445
lon: -107.94472222222223
surface_form: copper mountain
instance_of: Mountain
coordinates: lat: 43.45944444444445
lon: -107.94472222222223
Copper Mountain is part of a larger BLM owned parcel known as The Copper Mountain Wildlife Study area, which encompasses 6,858 acres. Most of the mountain is scattered limber pine and juniper with rocky slopes. Nearby Boysen Reservoir is visible from Copper Mountain. The area is popular for hikers, hunters, and rock climbers, which has caused conflicts with local ranchers. Geology.

Geographic entities mentioned:
surface_form: copper mountain
instance_of: Mountain
coordinates: lat: 43.45944444444445
lon: -107.94472222222223
Geology. Copper Mountain is features Archean rocks of the Wyoming Craton and is overlain in the southern part by Cenozoic sedimentary rocks. Lithium-bearing pegmatite (otherwise known as igneous rock containing crystals) has been found on Copper Mountain, including amblygonite, lepidolite, iron-manganese phosphates, columbite, tapiolite and beryl. Mining.

Geographic entities mentioned:
surface_form: copper mountain
instance_of: Mountain
coordinates: lat: 43.45944444444445
lon: -107.94472222222223
Lithium-bearing pegmatite (otherwise known as igneous rock containing crystals) has been found on Copper Mountain, including amblygonite, lepidolite, iron-manganese phosphates, columbite, tapiolite and beryl. Mining. Copper Mountain is home to several mines, including those for uranium. Three of the four uranium mines in Wyoming are still producing.

Geographic entities mentioned:
surface_form: copper mountain
instance_of: Mountain
coordinates: lat: 43.45944444444445
lon: -107.94472222222223
Mining. Copper Mountain is home to several mines, including those for uranium. Three of the four uranium mines in Wyoming are still producing. The Arrowhead Mine on Copper Mountain produced around 500,000 pounds of Uranium in the 1960s and 70s. Copper Mountain was also mined for iron, some of which were discovered in the 1950s. Radio/Television uses.

Geographic entities mentioned:
surface_form: copper mountain
instance_of: Mountain
coordinates: lat: 43.45944444444445
lon: -107.94472222222223
Three of the four uranium mines in Wyoming are still producing. The Arrowhead Mine on Copper Mountain produced around 500,000 pounds of Uranium in the 1960s and 70s. Copper Mountain was also mined for iron, some of which were discovered in the 1950s. Radio/Television uses. Edwards Communications, based in nearby Riverton, Wyoming, operates two radio stations from a tower on Copper Mountain.

Geographic entities mentioned:
surface_form: copper mountain
instance_of: Mountain
coordinates: lat: 43.45944444444445
lon: -107.94472222222223
Copper Mountain was also mined for iron, some of which were discovered in the 1950s. Radio/Television uses. Edwards Communications, based in nearby Riverton, Wyoming, operates two radio stations from a tower on Copper Mountain. KDNO 101.7 FM is licensed to Thermopolis, while KWYW 99.1 FM is licensed to Lost Cabin.

Geographic entities mentioned:
surface_form: copper mountain
instance_of: Mountain
coordinates: lat: 43.45944444444445
lon: -107.94472222222223
Wyoming Public Radio's KUWT 91.3 FM, licensed to Thermopolis, also broadcasts from the mountain. Wyoming Public Radio also has two other stations on Copper Mountain, KTWY 97.1 FM, carrying an adult alternative format known as &quot;Wyoming Sounds&quot;, and KWWY 106.5 FM, carrying a classical format.

Geographic entities mentioned:
surface_form: copper mountain
instance_of: Mountain
coordinates: lat: 43.45944444444445
lon: -107.94472222222223
The last station that shares a tower on Copper Mountain is known as KUDA (FM), on 89.9 FM, licensed to Bonneville, Wyoming That station is known as &quot;Wyoming's Hot Spot&quot; in reference to the nearby hot springs in Thermopolis. In addition to radio stations, Copper Mountain provides a large coverage area for television stations in central Wyoming.

Geographic entities mentioned:
surface_form: copper mountain
instance_of: Mountain
coordinates: lat: 43.45944444444445
lon: -107.94472222222223
One repeater receives 146.805 MHz and transmits on 146.205 MHz. The other repeater receives at 446.825 MHz and transmits at 441.825 MHz. A third repeater with the call sign W0KGB receives on 444.375 MHz and transmits on 449.375 MHz
There is also a repeater on Copper Mountain used for Automatic Packet Reporting System, or APRS, known as W7BEQ. It uses 144.390 MHz.

Geographic entities mentioned:
surface_form: copper mountain
instance_of: Mountain
coordinates: lat: 43.45944444444445
lon: -107.94472222222223
In August 1953, the Irk Valley Junction rail crash occurred on the line near Manchester Victoria, resulting in ten deaths and 58 injuries. It was caused by an electric train overrunning a danger signal which collided with a steam train, resulting in the front carriage of the electric train crashing into the River Irk.

Geographic entities mentioned:
surface_form: River Irk
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 53.4869
lon: -2.24504
The sylph horseman of Bonlieu. The horseman sylph is described as a king holding a raised saber, mounted on a white, winged, and superbly harnessed horse. He travels the skies, caracoling in &quot;the mountains bristling with black fir trees&quot; near the lakes of the Haut- Jura, such as those of Bonlieu and Narlay.

Geographic entities mentioned:
surface_form: Bonlieu
instance_of: Lake
countries: France
coordinates: lat: 46.586111111111
lon: 5.8736111111111
surface_form: Narlay
instance_of: Lake
countries: France
coordinates: lat: 46.642222222222
lon: 5.9125
Greek Mythology. An origin evoked by Désiré Monnier for the winged and flying horses is that of Pegasus of Greek mythology, who would have &quot;left his footprints all over the Jura region&quot;. The castle of the Jura eagle could be likened to Mount Olympus and the top of a mountain near Foncine-le-Haut to the Greek Mount Parnassus.

Geographic entities mentioned:
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
surface_form: Mount Parnassus
instance_of: Mountain
countries: Greece
coordinates: lat: 38.533
lon: 22.6167
The origin of the image of the &quot;winged horse on top of a mountain&quot; is, according to him, clearly linked to the myth of Pegasus. The riding sylph of Bonlieu recalls the Greek hero Bellerophon, who rode Pegasus and fell while trying to reach Olympus, and then ended up wandering on foot in the deserts, racked with worries and avoiding encounters. Roman mythology.

Geographic entities mentioned:
surface_form: Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
Sometime later, Hashem wakes up on the shore of the Caspian Sea and sees Mohammad lying motionless a short distance away. He stumbles toward Mohammad's body and takes him in his arms. He weeps over Mohammad's body and looks to the sky. A woodpecker is heard, and the sun comes out. Mohammad's fingers slowly start to move.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Elsewhere in the city are parks for sports like rugby, such as Coronation Park, Bill Brown Park and Colquhoun Park (also used for softball/baseball); and football: Skoglund Park (home of the Central Football Federation) and Celaeno Park. The Hokowhitu Lagoon is also located nearby the Esplanade and is a popular site for recreational kayaking and canoeing.

Geographic entities mentioned:
surface_form: Hokowhitu Lagoon
instance_of: Body of water
countries: New Zealand
coordinates: lat: -40.367016
lon: 175.629373
Access Manawatu 999AM is a local community station and Kia Ora FM is the local Iwi station. The city's main television and FM radio transmitter is located atop Wharite Peak, northeast of the city centre. The first transmitter at the site was commissioned in 1963 to relay Wellington's WNTV1 channel (now part of TVNZ 1). The current main transmitter was built in 1966.

Geographic entities mentioned:
surface_form: Wharite Peak
instance_of: Mountain
countries: New Zealand
coordinates: lat: -40.255
lon: 175.8567
Ubehebe Craters. The Ubehebe Craters are a volcanic field in the northern Death Valley of California, consisting of 14–16 craters in a area. The largest of the craters is the wide and deep Ubehebe Crater. Many of the craters, though, are partially buried and thus hardly recognizable. Other volcanic features there include a remnant of a scoria cone and a tuff cone.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
surface_form: ubehebe craters
instance_of: Valley
countries: United States
coordinates: lat: 37.01
lon: -117.45083333333
The volcanoes were first identified in reconnaissance studies in 1932. Geomorphology and geography. The Ubehebe Craters lie in the northern Death Valley on the slopes of Tin Mountain in the Panamint Range/Cottonwood Mountains about from Furnace Creek and from Las Vegas. The area is characterized by hills known as the Ubehebe Hills. About from the main crater a wash flows northward.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
surface_form: Tin Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.8865356
lon: -117.4560605
surface_form: tin mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.8865356
lon: -117.4560605
Geology. Death Valley is part of the Basin and Range Province, which is characterized by parallel mountain ranges and valleys. Since about 10 million years ago, the region around Death Valley has been subject to volcanic activity that has given rise to Ubehebe Craters, Yucca Mountain and a 400,000 years old cinder cone in southern Death Valley.

Geographic entities mentioned:
surface_form: Yucca Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.9402
lon: -116.485
surface_form: ubehebe craters
instance_of: Valley
countries: United States
coordinates: lat: 37.01
lon: -117.45083333333
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
surface_form: death valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
surface_form: yucca mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.9402
lon: -116.485
Beyond this mostly Miocene formation are Paleozoic carbonates. The Cottonwood Mountains consist of Paleozoic, Mesozoic, and in part Tertiary sedimentary rocks; most of the terrain west and north of the Ubehebe Craters is covered by modern alluvium. The Ubehebe Craters are atop a fault that forms the edge of the Tin Mountain range; adjacent to the craters the fault has formed scarps.

Geographic entities mentioned:
surface_form: Tin Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.8865356
lon: -117.4560605
surface_form: tin mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.8865356
lon: -117.4560605
The name has been mistakenly attributed to the native Shoshone tribes, which actually call it &quot;, which translates as &quot;basket in the rock&quot; or &quot;coyote's basket&quot;, referencing the form of the crater. The volcanoes were first identified in reconnaissance studies in 1932. Geomorphology and geography.

Geographic entities mentioned:
surface_form: shoshone
instance_of: Lake
countries: United States
coordinates: lat: 44.3722
lon: -110.713
The risk of renewed volcanic activity is low. Name and research history. &quot;Ubehebe&quot; is pronounced as &quot;YOU-bee-HEE-bee&quot; and its etymology is unclear; it may mean &quot;woman's breast&quot; () in Owens Valley Paiute but is often mistakenly translated as &quot;big basket&quot;.

Geographic entities mentioned:
surface_form: owens valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
Ubehebe Craters. The Ubehebe Craters are a volcanic field in the northern Death Valley of California, consisting of 14–16 craters in a area. The largest of the craters is the wide and deep Ubehebe Crater. Many of the craters, though, are partially buried and thus hardly recognizable. Other volcanic features there include a remnant of a scoria cone and a tuff cone.

Geographic entities mentioned:
surface_form: ubehebe craters
instance_of: Valley
countries: United States
coordinates: lat: 37.01
lon: -117.45083333333
Many of the craters, though, are partially buried and thus hardly recognizable. Other volcanic features there include a remnant of a scoria cone and a tuff cone. The Ubehebe Craters are associated with a fault system that runs across them. The region has been affected by volcanism for the last 10 million years. The volcanic field is in the Death Valley National Park and is accessible to tourists.

Geographic entities mentioned:
surface_form: ubehebe craters
instance_of: Valley
countries: United States
coordinates: lat: 37.01
lon: -117.45083333333
Various estimates have been put forward for the age of the craters. Recent research has shown that the Ubehebe Craters all formed in a single phreatomagmatic eruption episode about 2,100 years ago, making it one of the most recent volcanic events in southern California. The risk of renewed volcanic activity is low. Name and research history.

Geographic entities mentioned:
surface_form: ubehebe craters
instance_of: Valley
countries: United States
coordinates: lat: 37.01
lon: -117.45083333333
This volcanic activity is of transitional alkaline character and has decreased in volume over time. Ubehebe Craters is fairly isolated from the other volcanic fields in the region. The Ubehebe Craters formed within sedimentary rocks, which crop out in the craters. Conglomerates and sandstones form a sequence under Ubehebe Crater; they are part of the so-called Navadu Formation.

Geographic entities mentioned:
surface_form: ubehebe craters
instance_of: Valley
countries: United States
coordinates: lat: 37.01
lon: -117.45083333333
Beyond this mostly Miocene formation are Paleozoic carbonates. The Cottonwood Mountains consist of Paleozoic, Mesozoic, and in part Tertiary sedimentary rocks; most of the terrain west and north of the Ubehebe Craters is covered by modern alluvium. The Ubehebe Craters are atop a fault that forms the edge of the Tin Mountain range; adjacent to the craters the fault has formed scarps.

Geographic entities mentioned:
surface_form: ubehebe craters
instance_of: Valley
countries: United States
coordinates: lat: 37.01
lon: -117.45083333333
surface_form: ubehebe craters
instance_of: Valley
countries: United States
coordinates: lat: 37.01
lon: -117.45083333333
This fault is also known as the Tin Mountain fault, which cuts through Ubehebe Crater and branches out in a diffuse set of faults. This fault intersects the nearby Northern Death Valley fault close to the Ubehebe Craters; the latter fault may have ruptured at the same time or soon after an eruption in the volcanic field. Composition. The Ubehebe Craters have erupted alkali basalt and sideromelane.

Geographic entities mentioned:
surface_form: ubehebe craters
instance_of: Valley
countries: United States
coordinates: lat: 37.01
lon: -117.45083333333
Climate. Summer temperatures at the Ubehebe Craters can be quite high while winter temperatures often fall below freezing. During the Little Ice Age, temperatures were low enough to allow the development of snow patches in the Ubehebe Craters, which then left nivation landforms.

Geographic entities mentioned:
surface_form: ubehebe craters
instance_of: Valley
countries: United States
coordinates: lat: 37.01
lon: -117.45083333333
The volcanic eruptions at Ubehebe Craters involved significant amounts of water, perhaps implying that they took place under wetter than present climates, but later it was found that the Ubehebe Craters formed during the relatively dry Medieval Warm Period and that the phreatomagmatic activity can explained by the presence of only small amounts of groundwater. Eruption history.

Geographic entities mentioned:
surface_form: ubehebe craters
instance_of: Valley
countries: United States
coordinates: lat: 37.01
lon: -117.45083333333
surface_form: ubehebe craters
instance_of: Valley
countries: United States
coordinates: lat: 37.01
lon: -117.45083333333
They formed in a single episode about 2,100 years ago around 150 BCE. The timing of eruptive activity was determined with the help of archeomagnetic dating, beryllium-10 radiometric dating, and tephrochronology. This makes Ubehebe Craters the most recent basaltic eruption in the continental United States and, together with the Salton Buttes, one of the youngest in southern California.

Geographic entities mentioned:
surface_form: ubehebe craters
instance_of: Valley
countries: United States
coordinates: lat: 37.01
lon: -117.45083333333
Hazards and monitoring. The discovery of recent Holocene activity, which was initially assumed to have been protracted over time, has led to the California Volcano Observatory commencing volcano monitoring at the Ubehebe Craters, including the installation of one seismometer. The volcano is classified as a &quot;Moderate Threat&quot; volcano in the USGS volcanic threat assessment.

Geographic entities mentioned:
surface_form: ubehebe craters
instance_of: Valley
countries: United States
coordinates: lat: 37.01
lon: -117.45083333333
The volcano is classified as a &quot;Moderate Threat&quot; volcano in the USGS volcanic threat assessment. An incomplete circular volcano hazard zone has been defined for the Ubehebe Craters, which reaches Scotty's Castle, within which pyroclastic surges and steam blasts could be expected in case of renewed eruptions.

Geographic entities mentioned:
surface_form: ubehebe craters
instance_of: Valley
countries: United States
coordinates: lat: 37.01
lon: -117.45083333333
Future eruptions of the Ubehebe Craters may impact the almost a million annual Death Valley National Park visitors and the about 100 people who live in the region; however, the apparently monogenetic nature of the Ubehebe Craters implies that the risk for renewed eruptions is low.

Geographic entities mentioned:
surface_form: ubehebe craters
instance_of: Valley
countries: United States
coordinates: lat: 37.01
lon: -117.45083333333
The Ubehebe Craters are associated with a fault system that runs across them. The region has been affected by volcanism for the last 10 million years. The volcanic field is in the Death Valley National Park and is accessible to tourists. The fault system is within the tectonically active Basin and Range Province physiographic region.

Geographic entities mentioned:
surface_form: death valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Geology. Death Valley is part of the Basin and Range Province, which is characterized by parallel mountain ranges and valleys. Since about 10 million years ago, the region around Death Valley has been subject to volcanic activity that has given rise to Ubehebe Craters, Yucca Mountain and a 400,000 years old cinder cone in southern Death Valley.

Geographic entities mentioned:
surface_form: death valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Saqsa Punta. Saqsa Punta (Quechua &quot;saqsa&quot; multi-colored, &quot;punta&quot; peak, ridge, &quot;multi-colored peak (or ridge)&quot;, also spelled &quot;Sacsa Punta&quot;) is a mountain in the Andes of Peru. It is located in the Huánuco Region, Huánuco Province, Churubamba District. Saqsa Punta lies north of Saqra Waqra.

Geographic entities mentioned:
surface_form: saqsa punta
instance_of: Mountain
countries: Peru
coordinates: lat: -9.64111111
lon: -76.38333333
surface_form: saqsa
instance_of: Mountain
countries: Peru
coordinates: lat: -12.12166667
lon: -75.98138889
surface_form: saqsa
instance_of: Mountain
countries: Peru
coordinates: lat: -11.5358
lon: -76.4417
Saqsa Punta. Saqsa Punta (Quechua &quot;saqsa&quot; multi-colored, &quot;punta&quot; peak, ridge, &quot;multi-colored peak (or ridge)&quot;, also spelled &quot;Sacsa Punta&quot;) is a mountain in the Andes of Peru. It is located in the Huánuco Region, Huánuco Province, Churubamba District. Saqsa Punta lies north of Saqra Waqra.

Geographic entities mentioned:
surface_form: saqsa punta
instance_of: Mountain
countries: Peru
coordinates: lat: -9.64111111
lon: -76.38333333
surface_form: saqsa
instance_of: Mountain
countries: Peru
coordinates: lat: -12.12166667
lon: -75.98138889
surface_form: saqsa
instance_of: Mountain
countries: Peru
coordinates: lat: -12.12166667
lon: -75.98138889
surface_form: saqsa
instance_of: Mountain
countries: Peru
coordinates: lat: -11.5358
lon: -76.4417
surface_form: saqsa
instance_of: Mountain
countries: Peru
coordinates: lat: -11.5358
lon: -76.4417
The primary agricultural use of the Cheshire Plain is dairy farming, creating the general appearance of enclosed hedgerow fields. Meteorologists use the term Cheshire Gap when referring to the lowlands of the Cheshire Plain, providing as they do a passage between the Clwydian Hills, in Wales on the one hand and the Peak District and South Pennines on the other.

Geographic entities mentioned:
surface_form: the peak
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -7.95
lon: -14.35
surface_form: cheshire plain
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.2
lon: -2.4666666666667
Cheshire Plain. The Cheshire Plain is a relatively flat expanse of lowland within the county of Cheshire in North West England but extending south into Shropshire. It extends from the Mersey Valley in the north to the Shropshire Hills in the south, bounded by the hills of North Wales to the west and the foothills of the Pennines to the north-east.

Geographic entities mentioned:
surface_form: cheshire plain
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.2
lon: -2.4666666666667
It assumed its current form as the ice-sheets of the last glacial period melted away between 20,000 and 15,000 years ago leaving behind a thick cover of glacial till and extensive tracts of glacio-fluvial sand and gravel. The primary agricultural use of the Cheshire Plain is dairy farming, creating the general appearance of enclosed hedgerow fields.

Geographic entities mentioned:
surface_form: cheshire plain
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.2
lon: -2.4666666666667
Yushkino. Yushkino () is the third largest village of Yushkinskaya Volost and its administrative center. It belongs to Gdovsky District of Pskov Oblast, Russia and is located 11 kilometers south of Gdov. Vetka River flows through the village and the large Lake Peipus is located in around 5 kilometers from its center. The population in 2002 was 52.

Geographic entities mentioned:
surface_form: Lake Peipus
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
The Green Line will link the two campuses of the Hebrew University of Jerusalem and continue south via Pat junction to Gilo. It will pass the terminus of the Tel Aviv–Jerusalem railway, then cross the existing Red Line tram route and run to Mount Scopus. There will be 35 stops, and ridership is predicted at 200,000 passengers/day.

Geographic entities mentioned:
surface_form: Mount Scopus
instance_of: Mountain
countries: Israel
coordinates: lat: 31.7925
lon: 35.244166666667
Haesselia roraimensis. &quot;Haesselia roraimensis&quot; is a species of liverwort in the family Cephaloziaceae. It is endemic to Guyana. Its natural habitat is on rotten logs in periodically flooded riverine forest from elevation, in the humid submontane tropical 'mossy' forests on the slopes of Mount Roraima, where the borders of Brazil, Venezuela, and Guyana meet. Taxonomy.

Geographic entities mentioned:
surface_form: Mount Roraima
instance_of: Mountain
countries: Venezuela
Brazil
coordinates: lat: 5.141944444444444
lon: -60.76416666666667
Root-like structures (rhizoids) are either absent or sparsely produced on the lower side of branches. Habitat, distribution, and ecology. &quot;Haesselia roraimensis&quot; is known only from Mount Roraima in Guyana, specifically from its northern slopes and foothills, where it grows at elevations between above sea level. The species appears to flourish particularly well at altitudes between.

Geographic entities mentioned:
surface_form: Mount Roraima
instance_of: Mountain
countries: Venezuela
Brazil
coordinates: lat: 5.141944444444444
lon: -60.76416666666667
Towns and villages in Wharfedale (downstream, from west to east) include Buckden, Kettlewell, Conistone, Grassington, Hebden, Bolton Abbey, Addingham, Ilkley, Burley-in-Wharfedale, Otley, Pool-in-Wharfedale, Arthington, Collingham and Wetherby. Beyond Wetherby, the valley opens out and becomes part of the Vale of York.

Geographic entities mentioned:
surface_form: Vale of York
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.95
lon: -1.0833333333333333
The section from the river's source to around Addingham is known as &quot;Upper Wharfedale&quot;. It lies in North Yorkshire and the Yorkshire Dales National Park. The first or so is known as Langstrothdale, including the settlements of Beckermonds, Yockenthwaite and Hubberholme, famous for its church, the resting place of the writer J. B. Priestley.

Geographic entities mentioned:
surface_form: Langstrothdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.204
lon: -2.134
surface_form: langstrothdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.204
lon: -2.134
The northern side of Lower Wharfedale, opposite Ilkley, Burley-in-Wharfedale and Otley, is in the Nidderdale Area of Outstanding Natural Beauty. The Yorkshire Dales Rivers Trust has a remit to conserve the ecological condition of Wharfedale, Wensleydale, Swaledale and Nidderdale catchments from their headwaters to the Humber Estuary. History.

Geographic entities mentioned:
surface_form: Wensleydale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.3056
lon: -2.16667
surface_form: Swaledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.361
lon: -1.838
surface_form: Nidderdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.0867
lon: -1.75773
surface_form: wharfedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.88333
lon: -1.45
The valley was transformed into its classic U-shaped state between 18,000 and 12,000 years ago by the Wharfedale Glacier, though this was cutting through a channel that had already had a river draining water away to the east through what is now Wharfedale, and also to the north through what is now Bishopdale and then Wensleydale.

Geographic entities mentioned:
surface_form: Bishopdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.25
lon: -2.01667
surface_form: Wensleydale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.3056
lon: -2.16667
surface_form: wharfedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.88333
lon: -1.45
surface_form: wharfedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.88333
lon: -1.45
The uppermost part of the valley is known as Langstrothdale. Below Beckermonds the river is known as the River Wharfe. Wetherby is traditionally seen as the foot of Wharfedale, even though the river continues on through the Vale of York. The valley has been used largely for agriculture, and is now criss-crossed with stone walls and stone barns that evidence its use down the centuries. Geology.

Geographic entities mentioned:
surface_form: Vale of York
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.95
lon: -1.0833333333333333
surface_form: wharfedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.88333
lon: -1.45
The valley roughly follows a south-easterly direction, providing a border between West Yorkshire (on the south side) and North Yorkshire. Between Oughtershaw Moss and Wetherby, the valley runs for. The uppermost part of the valley is known as Langstrothdale. Below Beckermonds the river is known as the River Wharfe.

Geographic entities mentioned:
surface_form: langstrothdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.204
lon: -2.134
Wharfedale. Wharfedale () is one of the Yorkshire Dales. It is situated at source in North Yorkshire and then flows into West Yorkshire and forms the upper valley of the River Wharfe.

Geographic entities mentioned:
surface_form: wharfedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.88333
lon: -1.45
It is situated at source in North Yorkshire and then flows into West Yorkshire and forms the upper valley of the River Wharfe. Towns and villages in Wharfedale (downstream, from west to east) include Buckden, Kettlewell, Conistone, Grassington, Hebden, Bolton Abbey, Addingham, Ilkley, Burley-in-Wharfedale, Otley, Pool-in-Wharfedale, Arthington, Collingham and Wetherby.

Geographic entities mentioned:
surface_form: wharfedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.88333
lon: -1.45
surface_form: wharfedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.88333
lon: -1.45
surface_form: wharfedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.88333
lon: -1.45