Sarmila/GeoWiki-Features huggingface dataset:
Rhyolites associated with the Bella Bella dike swarm are distributed on Denny Island whereas rhyolites belonging to the Gale Passage dike swarm are found on the northern ends of Athlone Island and Dufferin Island. Exposed in high cliffs along the Dean and Burke channels is the King Island Pluton.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
This easterly trending intrusion has a length of over and a width of, cutting across the predominantly northwest structural trend of the Coast Plutonic Complex. Two distinct phases of magmatism created the King Island Pluton 10.3 to 13 million years ago. The first and principal phase formed the core of the pluton which comprises coarse-grained syenite.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
The first and principal phase formed the core of the pluton which comprises coarse-grained syenite. These rocks form most of the pluton exposures at sea level. The second phase resulted in the creation of a marginal zone of alkali granite at the extreme western end of the King Island Pluton, as well as satellite stocks west of the main pluton. Central segment.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
The abnormal thicknesses of the Anahim Peak hawaiite flows coupled with a significantly coarser-grained groundmass and higher percentage of phenocrysts than the upper portions of the flows suggest that they were ponded during eruption, possibly as lava lakes within a former cinder cone.

Geographic entities mentioned:
surface_form: anahim peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.7578
lon: -125.625
surface_form: cinder cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9717
lon: -123.007
surface_form: lava lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 56.4333
lon: -130.9
Anahim Volcanic Belt. The Anahim Volcanic Belt (AVB) is a west–east trending chain of volcanoes and related magmatic features in British Columbia, Canada. It extends from Athlone Island on the Central Coast, running eastward through the strongly uplifted and deeply dissected Coast Mountains to near the community of Nazko on the Interior Plateau.

Geographic entities mentioned:
surface_form: anahim volcanic belt
instance_of: Mountain
countries: Canada
coordinates: lat: 52.666666666666664
lon: -125.83333333333333
No volcanic eruption was likely as the number and size of the tremors were too small. Although these volcano tectonic earthquakes were too small to be felt, they generated substantial local interest as they represented a significant concentration of seismic activity within the Anahim Volcanic Belt.

Geographic entities mentioned:
surface_form: anahim volcanic belt
instance_of: Mountain
countries: Canada
coordinates: lat: 52.666666666666664
lon: -125.83333333333333
In some places the AVB lavas imperceptibly merge with the Chilcotin Group basalts as the two volcanic zones were active simultaneously from the Neogene to Quaternary. This west–east trending volcanic belt is about long, extending from the Central Coast through the Coast Mountains to near the community of Nazko on the Interior Plateau.

Geographic entities mentioned:
surface_form: interior plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 52
lon: -123
A basaltic lava flow near the head of Moore Creek has an age of 3.91 million years, similar to the oldest rocks known from the Itcha Range or the Chilcotin Group basalts of the surrounding plateau. The relation of this flow to the Baldface Mountain volcanic field is in question as its source and extent have not been identified. Eastern segment.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: baldface mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.7723
lon: -124.5422
surface_form: baldface mountain volcanic field
instance_of: Mountain
countries: Canada
coordinates: lat: 52.75972222
lon: -124.53138889
The second episode is constituted by a subglacial mound of hyaloclastite that formed under the Cordilleran Ice Sheet, perhaps during the Fraser Glaciation which took place between 25,000 and 10,000 years ago. It forms the western side of Nazko Cone and is dominated by blocks of highly vesicular, glassy basalt.

Geographic entities mentioned:
surface_form: nazko cone
instance_of: Mountain
countries: Canada
coordinates: lat: 52.9272
lon: -123.734
The third episode is defined by coalescing pyroclastic cones and associated lava flows that formed subaerially during the Holocene. Radiocarbon dating of bog peat above and below a tephra layer near Nazko Cone suggest that the latest eruption took place about 7,200 years ago. This is the only known Holocene eruption from Nazko Cone as no other tephra layers have been identified.

Geographic entities mentioned:
surface_form: nazko cone
instance_of: Mountain
countries: Canada
coordinates: lat: 52.9272
lon: -123.734
Radiocarbon dating of bog peat above and below a tephra layer near Nazko Cone suggest that the latest eruption took place about 7,200 years ago. This is the only known Holocene eruption from Nazko Cone as no other tephra layers have been identified. From 9 October 2007 to 15 May 2008, a series of earthquakes measuring up to 2.9 magnitude occurred in the Nechako Basin about west of Nazko Cone.

Geographic entities mentioned:
surface_form: nazko cone
instance_of: Mountain
countries: Canada
coordinates: lat: 52.9272
lon: -123.734
This is the only known Holocene eruption from Nazko Cone as no other tephra layers have been identified. From 9 October 2007 to 15 May 2008, a series of earthquakes measuring up to 2.9 magnitude occurred in the Nechako Basin about west of Nazko Cone. Most of them occurred below the surface, indicating they originated within the lowermost crust.

Geographic entities mentioned:
surface_form: nazko cone
instance_of: Mountain
countries: Canada
coordinates: lat: 52.9272
lon: -123.734
It consists of a 2.37 million year old cone of aphanitic phonolite and porphyritic trachyte with feldspar phenocrysts. A basaltic lava flow near the head of Moore Creek has an age of 3.91 million years, similar to the oldest rocks known from the Itcha Range or the Chilcotin Group basalts of the surrounding plateau.

Geographic entities mentioned:
surface_form: moore creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.4689
lon: -79.6478
Cosquín Festival. The Cosquín Folk Festival is one of the most important folk music festivals of Argentina, and most important in Latin America. It lasts nine days and takes place in the second half of January in the city of Cosquín, a scenic, Punilla Valley location in Córdoba Province. The tradition used to refer to &quot;nine moons of Cosquín.&quot;
History.

Geographic entities mentioned:
surface_form: Punilla Valley
instance_of: Valley
countries: Argentina
coordinates: lat: -31.033333333333
lon: -64.5
260 bodies washed ashore and were buried in a common grave at the local churchyard. The survivors were sent on to Scotland by the local clan leader, Sorley Boy MacDonnell of Dunluce Castle, which was situated just to the west on the Giant's Causeway cliffs overlooking the coast. From there, MacDonnell is also believed to have conducted the first clandestine salvage efforts on the shipwreck.

Geographic entities mentioned:
surface_form: Giant's Causeway
instance_of: Landform
countries: United Kingdom
coordinates: lat: 55.240833333333
lon: -6.5116666666667
Sass de Stria. Sass de Stria is a mountain of the Veneto, Italy. It has an elevation of 2,477 meters. During the First World War, the mountain and surrounding area was the scene of fighting between Italy and Austria-Hungary.

Geographic entities mentioned:
surface_form: sass de stria
instance_of: Mountain
countries: Italy
coordinates: lat: 46.521111111111
lon: 11.996944444444
Yabakei Bridge. is a Taishō-era stone bridge over the Yamakuni River in Yabakei, Nakatsu, Ōita Prefecture, Japan. Construction work on the eight-arched bridge, built as part of a tourist road for the viewing of the nearby Aonodōmon, began in 1920 and was completed in 1923; repair and restoration work took place in 1999.

Geographic entities mentioned:
surface_form: Yabakei
instance_of: Valley
countries: Japan
coordinates: lat: 33.44055556
lon: 131.14111111
During the Spanish colonial period in the Philippines, merchants travelling in and out of Laguna de Bay via Napindan had issues with the formation of sandbars that blocked or clogged the waterway. The name was also meant &quot;being pierced through&quot;, which was attributed to the periodical action of the lake piercing through the land area where the barangay is presently located.

Geographic entities mentioned:
surface_form: Laguna de Bay
instance_of: Lake
countries: Philippines
coordinates: lat: 14.508888888889
lon: 121.11888888889
In the October of the latter year, King Edward conferred upon him the lands of Annandale in Scotland, as well as the earldom of Atholl; he later resigned the earldom to David Strathbogie, the son of the old Earl of Atholl, in exchange for the sum of 10,000 marks. In the winter he served as one of the king's three wardens in Scotland, and was besieged in Ayr Castle.

Geographic entities mentioned:
surface_form: Annandale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.2
lon: -3.4
The regiment was initially assigned to the IV Corps of the Army of Northeastern Virginia (later became the Army of the Potomac) and saw its first combat action at the First Battle of Bull Run. The IV Corps later became the VI Corps of the Army of the Shenandoah, and the 2nd Rhode Island participated in several fights in the Shenandoah Valley.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
The Sixth Army Corps, including the Second Rhode Island, and Batteries C, D and G, were hurried to the defense of the Capital, and reached there just in season to save the city, and to aid in driving the enemy, who had approached within shelling distance, back into the valley of the Shenandoah.

Geographic entities mentioned:
surface_form: valley of the Shenandoah
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Mount Willard (New Hampshire). Mount Willard, elevation, is a mountain located in Carroll County, New Hampshire, United States. The summit is located in the town of Hart's Location in Crawford Notch State Park. The summit provides excellent views and is accessible via the Mount Willard Trail.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount willard
instance_of: Mountain
countries: United States
coordinates: lat: 44.2042
lon: -71.4128
Mount Willard (New Hampshire). Mount Willard, elevation, is a mountain located in Carroll County, New Hampshire, United States. The summit is located in the town of Hart's Location in Crawford Notch State Park. The summit provides excellent views and is accessible via the Mount Willard Trail.

Geographic entities mentioned:
surface_form: mount willard (new hampshire)
instance_of: Mountain
countries: United States
coordinates: lat: 44.2042
lon: -71.4128
Mount Willard, elevation, is a mountain located in Carroll County, New Hampshire, United States. The summit is located in the town of Hart's Location in Crawford Notch State Park. The summit provides excellent views and is accessible via the Mount Willard Trail. The Mount Willard Trail, &quot;a relatively steep day hike,&quot; is a long out-and-back with an elevation gain of.

Geographic entities mentioned:
surface_form: mount willard
instance_of: Mountain
countries: United States
coordinates: lat: 44.2042
lon: -71.4128
The summit is located in the town of Hart's Location in Crawford Notch State Park. The summit provides excellent views and is accessible via the Mount Willard Trail. The Mount Willard Trail, &quot;a relatively steep day hike,&quot; is a long out-and-back with an elevation gain of. Dogs are able to use this trail, and it has been rated as child friendly.

Geographic entities mentioned:
surface_form: mount willard
instance_of: Mountain
countries: United States
coordinates: lat: 44.2042
lon: -71.4128
Dôme des Nants. Dôme des Nants is a mountain of Savoie, France. It lies in the Massif de la Vanoise range. It has an elevation of 3,570 metres above sea level.

Geographic entities mentioned:
surface_form: dôme des nants
instance_of: Mountain
countries: France
coordinates: lat: 45.326706
lon: 6.742047
He has climbed Mount Everest and four of the five 8000 m peaks in Pakistan, including the world's second highest mountain K2 making the first ascent of the West Ridge on Aug 7, 1981 along with Eiho Otani both as members of the Waseda University K2 Expedition, Gasherbrum II 8035m, Broad Peak 8050m in 1982, and Gasherbrum I (Hidden Peak) 8068m in 1992 as a liaison officer on the Japanese TV Asahi team He became the first from Pakistan to have climbed Everest on 17 May 2000 as a team member on the Mountain Madness Everest Expedition led by Christine Boskoff from the United States that also included famed Everest climber Peter Habeler of Austria and eight Canadians.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
surface_form: K2
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
surface_form: Gasherbrum II
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.7575
lon: 76.652777777778
surface_form: Broad Peak
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.810555555556
lon: 76.568055555556
surface_form: Gasherbrum I
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.724444444444
lon: 76.696388888889
Climbing career. Sabir began his Himalayan climbing career with a Japanese expedition to the 7284m Passu Peak in Hunza in 1974. In 1975 he was part of a German Expedition as a trainee that attempted Nanga Parbat (8125m) and only went to 6700m up the south west ridge.

Geographic entities mentioned:
surface_form: Nanga Parbat
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.239166666667
lon: 74.59
On 17 July 1976 he made the first ascent of 6660m virgin Paiyu followed by Colonel Manzoor Hussain and Major Bashir with the first Pakistani expedition organised by the Alpine Club of Pakistan. In 1977 Sabir joined the largest Japan/Pakistan joint expedition to K2, attempting the traditional South East Abruzzi Ridge.

Geographic entities mentioned:
surface_form: K2
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
Sabir and his team from the Waseda University created history by successfully climbing K2's West/South West Ridge for the first time. A documentary film of the climb, &quot;50 Day Struggle&quot; was shown all over Japan, and made Sabir a household name there. In 1982, Sabir along with Sher Khan and the famous Italian mountaineer Reinhold Messner climbed Gasherbrum II 8035m and Broad Peak 8047m.

Geographic entities mentioned:
surface_form: Gasherbrum II
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.7575
lon: 76.652777777778
surface_form: Broad Peak
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.810555555556
lon: 76.568055555556
Both Gasherbrum II and Broad Peak were done in alpine style in a period of just one week, the fastest ascent of two 8000m peaks at the time. Expeditions to Nanga Parbat. He made three attempts on Nanga Parbat. His first was in October 1981, two months after his big success on K2 when he joined his friends from the Sangaku Doshikai Club Tokyo led by M. Omiya.

Geographic entities mentioned:
surface_form: Nanga Parbat
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.239166666667
lon: 74.59
Death of brother. In July 1980, Sabir lost his elder brother Inayat Shah, who served in the Pakistan Army Special Services Group (SSG). This was Shah's second attempt on Diran on the SSG expedition. On their first trip in 1979 they had to return from merely 150 m from the summit due to Khalid Bashir who had developed pulmonary oedema and on the descent Bashir fell to his death.

Geographic entities mentioned:
surface_form: Diran
instance_of: Mountain
countries: Pakistan
coordinates: lat: 36.116666666667
lon: 74.666666666667
While waiting for Ben Webster of Canada and two other Sherpas he went on enjoying the most splendid moments of his life with his two Sherpa colleagues taking video shots of Ben and others climbing the last part of the summit ridge and the magical surroundings against the backdrop of the much blessed early morning sun approaching from behind 8462m Makalu, 5th highest mountain in the world.

Geographic entities mentioned:
surface_form: Makalu
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.889166666667
lon: 87.088611111111
Environmentalist. Sabir is currently working as an environmentalist on the conservation of wildlife in his native Hunza Valley and across Northern Pakistan including the Baltoro Glacier region. He is involved on the conservation of the 5000 years old world heritage of Juniper forests in Ziarat Balochistan in collaboration with Hayatullah Khan Durrani of Chiltan Adventurers Association Balochistan.

Geographic entities mentioned:
surface_form: Hunza Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.31666667
lon: 74.65
He also attended the International Congress on &quot;Future of Mountain Sports&quot; at Innsbruck (Austria) in 2002, centennial celebrations of American Alpine Club in Salt Lake City in 2002, Sagarmatha Golden Jubilee celebrations in Kathmandu, Nepal in 2003.

Geographic entities mentioned:
surface_form: Sagarmatha
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
They baptized the valley and named it Rancho Cañada de Guadalupe la Visitación y Rodeo Viejo - this tract of land also included the Bayshore district of Daly City, the city of Brisbane, and San Bruno Mountain. The neighborhood came to be known as Visitacion Valley. The term &quot;Visitacion&quot; is Spanish and a reference to the Visitation in Luke 1:39 of the Bible.

Geographic entities mentioned:
surface_form: San Bruno Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6874
lon: -122.436
Mount Grace Land Conservation Trust, incorporated in 1986, is a non-profit organization whose mission is the conservation of woodland and agricultural land in north central and western Massachusetts. Based out of Athol, Massachusetts, the MGLCT is named after Mount Grace, a nearby monadnock. As of August 2016, the trust had protected 31,559 acres by completing 335 projects.&quot;

Geographic entities mentioned:
surface_form: Mount Grace
instance_of: Mountain
countries: United States
coordinates: lat: 42.691111111111
lon: -72.355
Geography. The Vediantii dwelled on the Mediterranean coast, between the river Var and the Mont Agel, around the Massaliote colony of Nikaea (modern Nice). Their territory was located east of the Deciates and Nerusii, west of the Intimilii, and south of the Vesubiani. Their chief town was the &quot;oppidum&quot; &quot;Vediantiorum&quot;, known as &quot;Cemenelum&quot; by the 2nd century AD.

Geographic entities mentioned:
surface_form: Mont Agel
instance_of: Mountain
countries: France
Monaco
coordinates: lat: 43.775277777778
lon: 7.4263888888889
Ireland had been uninhabited since the Muintir Partholóin died of plague. The Muintir Nemid set sail from the Caspian Sea in 44 ships, but after a year and a half of sailing, the only ship to reach Ireland is Nemed's. In one version, the fleet come upon a tower of gold in the sea. They try to take the tower, but all the ships except Nemed's are wrecked by the waves.

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
Two quite different dates are given for the arrival of Muintir Nemid: 2350 BCE, according to the &quot;Annals of the Four Masters&quot;; or 1731 BCE in Seathrún Céitinn's chronology. Four lakes burst from the ground in Nemed's time, including Loch Annind, which flowed up when Annind's grave was being dug.

Geographic entities mentioned:
surface_form: Loch Annind
instance_of: Lake
countries: Ireland
coordinates: lat: 53.45
lon: -7.4166666666667
Four lakes burst from the ground in Nemed's time, including Loch Annind, which flowed up when Annind's grave was being dug. The other three lakes are Loch Cál in Uí Nialláin, Loch Munremair in Luigne, and Loch Dairbrech in Mide.

Geographic entities mentioned:
surface_form: Loch Munremair
instance_of: Lake
countries: Ireland
coordinates: lat: 53.816666666667
lon: -7.0833333333333
surface_form: Loch Dairbrech
instance_of: Lake
countries: Ireland
coordinates: lat: 53.6526
lon: -7.3587
Cwm Rhondda is a popular hymn tune written by John Hughes (1873–1932) in 1907. The name is taken from the Welsh name for the Rhondda Valley. It is usually used in English as a setting for William Williams' text &quot;Guide Me, O Thou Great Redeemer&quot; (or, in some traditions, &quot;Guide Me, O Thou Great Jehovah&quot;), originally (&quot;Lord, lead me through the wilderness&quot;) in Welsh.

Geographic entities mentioned:
surface_form: Rhondda Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
Essex County is in the northeastern part of New York state, just west of Vermont along the eastern boundary of the state. The eastern boundary of Essex County is Lake Champlain, which serves as the New York – Vermont border at an elevation of just under. The highest natural point in New York, Mount Marcy at, is in the town of Keene.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
The Willow Prairie Cabin is located in a remote area of the Butte Falls Ranger District in the Rogue River-Siskiyou National Forest. It sits on the western slope of the Cascade Mountains, at about elevation. The cabin is surrounded by a mature conifer forest just southwest of Mount McLoughlin. It is adjacent to Willow Prairie meadow, a large high country wetland with several beaver ponds.

Geographic entities mentioned:
surface_form: Mount McLoughlin
instance_of: Mountain
countries: United States
coordinates: lat: 42.444472222222
lon: -122.31561111111
This is 72 days longer than Toronto's, and longer than any other major urban centre in Canada. Despite normally semi-mild winters (for its latitude) due to the onshore air flow over the North Pacific Current, occasional cold squamish or Arctic outflow (sinking cold continental air that flows down through the Fraser Valley coastward) in winter can sometimes last a week or more.

Geographic entities mentioned:
surface_form: Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
Rain. Vancouver is Canada's third most rainy city, with 169 rainy days per year. As measured at Vancouver Airport in Richmond, Vancouver receives of rain per year. In North Vancouver, about away from the Vancouver airport, the amount of rain received doubles to per year as measured at the base of Grouse Mountain. Since Vancouver lacks a hot summer, convective storms are uncommon.

Geographic entities mentioned:
surface_form: Grouse Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.38611111
lon: -123.07638889
Many other Julys have recorded less than of rain in Vancouver. Snow. Snow falls in the higher-lying areas of Greater Vancouver, such as Burnaby Mountain, Coquitlam, and North and West Vancouver, every winter. It is also common in places close to or at sea level, however in lesser amounts.

Geographic entities mentioned:
surface_form: Burnaby Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.2792
lon: -122.909
Bienaimétoppane. Bienaimétoppane are two mountain peaks in Wedel Jarlsberg Land at Spitsbergen, Svalbard. They reach the heights of 767 and 763 m.a.s.l. and are located in the Martinfjella mountain range. The summits are named after French naval officer Amédée Pierre Leonard Bienaimé.

Geographic entities mentioned:
surface_form: bienaimétoppane
instance_of: Mountain
countries: Norway
coordinates: lat: 77.4639
lon: 14.907
Seruvalsar Lake. Seruvalsar Lake (also spelled Sirolsar Lake or Serol Sar Lake,) is a high altitude lake in the Seraj Valley of the Kullu district, Himachal Pradesh, India. The lake is about above the sea level and is surrounded by thick forest cover. Seruvalsar Lake is accessible via Jalori pass. History.

Geographic entities mentioned:
surface_form: seruvalsar lake
instance_of: Lake
countries: India
coordinates: lat: 31.5375
lon: 77.41666666666667
Tehuacana Hills. qv3ioeko13k0cpbsneagcd39nebcw" xml:space="preserve">The Tehuacana Hills (;) are a series of hills in Limestone County, Texas. Location. The hills are located northwest of Tehuacana in Limestone County, Texas. They are &quot;650 feet above sea level and 150 feet higher than the surrounding area&quot;. History.

Geographic entities mentioned:
surface_form: tehuacana hills
instance_of: Mountain
countries: United States
coordinates: lat: 31.7444
lon: -96.5514
However, it is unknown if other members of the genus were gregarious or solitary. Paleoecology. &quot;Amphimachairodus hezhengensis&quot; lived in an open arid environment in Linxia Basin, caused by the uplifting of Tibetan Plateau.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
The Esk'etemc are a First Nations people in the Cariboo Regional District of the Canadian province of British Columbia. They are a subgroup of the Secwepemc people and reside around the community of Alkali Lake, an unincorporated settlement and Indian Reserve community on the Cariboo Plateau south of the city of Williams Lake. Their band government was formerly called the Alkali Lake Indian Band.

Geographic entities mentioned:
surface_form: Cariboo Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 50.81652
lon: -118.81904
However, nuances exist in the application of this term across different communities. For example, in the Ottawa Valley tradition, the preferred term is &quot;step-dancing&quot; rather than &quot;step dance&quot;. In Scotland, both &quot;step dance&quot; and &quot;step-dancing&quot; are recognized.

Geographic entities mentioned:
surface_form: Ottawa Valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
Abyssinia Creek. Abyssinia Creek is a small meander in The Pilbara, Western Australia. It flows through the Tambourah mining district from the Tambourah Creek.

Geographic entities mentioned:
surface_form: abyssinia creek
instance_of: Watercourse
countries: Australia
coordinates: lat: -21.7282
lon: 119.301
Roscoe Boulevard. Roscoe Boulevard is a major east–west arterial road that runs for across the San Fernando Valley in Los Angeles, California. Name. There are two theories as to how Roscoe Boulevard got its name. The first is that it is named after a Southern Pacific employee named Roscoe who regularly asked to get off near his girlfriend's house on the street.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Southern Pacific Railroad Co.. It is also possible that both theories are incorrect. Route. Roscoe Boulevard travels east–west across almost the entire San Fernando Valley. From west to east, the boulevard travels from West Hills, through Canoga Park, Winnetka, Northridge, Van Nuys, North Hills, Panorama City and into Sun Valley.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Shavano (train). The &quot;Shavano&quot;, named for nearby Mount Shavano, was operated by the Denver and Rio Grande Railroad. The passenger train ran between Salida and Gunnison, Colorado on the railroad's historic narrow gauge route over Marshall Pass. The &quot;Shavano&quot; operated as Train #315 westbound (to Gunnison), and #316 eastbound (to Salida). History.

Geographic entities mentioned:
surface_form: Mount Shavano
instance_of: Mountain
countries: United States
coordinates: lat: 38.619166666667
lon: -106.23944444444
&quot;Kokanee&quot; was ordered in October 1941 as part of the 1942–43 building program. Named after Kokanee Lake in southeastern British Columbia, she was laid down on 25 August 1943 at Yarrows Ltd., Esquimalt and launched on 27 November 1943. She was commissioned into the RCN with pennant number K419 on 6 June 1944 at the Esquimalt naval base.

Geographic entities mentioned:
surface_form: Kokanee Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.7481
lon: -117.176
John's in September where she was assigned to Escort Group C-3 as the Senior Officer's Ship. &quot;Kokanee&quot; and EG C-3 spent the remainder of the Battle of the Atlantic on convoy escort duty. She also earned battle honours in the Battle of the St. Lawrence between September–November 1944 when she escorted convoys from Quebec City to the Cabot Strait and Strait of Belle Isle.

Geographic entities mentioned:
surface_form: Cabot Strait
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.233333333333
lon: -59.716666666667
The technology of cast iron was transferred to the West from China. Al-Qazvini in the 13th century and other travellers subsequently noted an iron industry in the Alburz Mountains to the south of the Caspian Sea. This is close to the silk route, thus the use of cast-iron technology being derived from China is conceivable.

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
Geography. According to the U.S. Census Bureau, the township has a total area of, of which is land and (25.19%) is water. The township occupies water boundaries in Lake Charlevoix and Walloon Lake. Young State Park is in the southwest part of the township along Lake Charlevoix. Demographics. As of the census of 2000, there were 773 people, 298 households, and 225 families residing in the township.

Geographic entities mentioned:
surface_form: Lake Charlevoix
instance_of: Lake
countries: United States
coordinates: lat: 45.248184
lon: -85.075807
surface_form: Walloon Lake
instance_of: Lake
countries: United States
coordinates: lat: 45.285833333333
lon: -85.018333333333
Britton is an unincorporated community in north-western Ellis County, Texas, United States. History. Britton was settled in 1895 under the name Helland and later Hellandville, named after Texas and New Orleans Railroad passenger agent Joseph Helland, later being renamed Britton after conductor H.C. Britton. The community is located on the border of the city of Mansfield, and Joe Pool Lake.

Geographic entities mentioned:
surface_form: Joe Pool Lake
instance_of: Lake
countries: United States
coordinates: lat: 32.628611111111
lon: -97.005277777778
Bylong Valley. The Bylong Valley is a winding but relatively flat valley that crosses the Great Dividing Range between the Goulburn River National Park and Wollemi National Park, west of the upper Hunter Region in New South Wales, Australia. The picturesque countryside was the site of Aboriginal and early European settlements.

Geographic entities mentioned:
surface_form: Hunter Region
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
surface_form: bylong valley
instance_of: Valley
countries: Australia
Bylong Valley. The Bylong Valley is a winding but relatively flat valley that crosses the Great Dividing Range between the Goulburn River National Park and Wollemi National Park, west of the upper Hunter Region in New South Wales, Australia. The picturesque countryside was the site of Aboriginal and early European settlements.

Geographic entities mentioned:
surface_form: bylong valley
instance_of: Valley
countries: Australia
The headwaters start in the Great Dividing Range to the north-west on Nullo Mountain. The Bylong Valley carries the Sandy Hollow-Gulgong cross-country railway line, which passes under Cox's Gap with a tunnel, and the Bylong Valley Way, which climbs over the ridge through the gap. The path across this ridge is steep and winding.

Geographic entities mentioned:
surface_form: bylong valley
instance_of: Valley
countries: Australia
surface_form: bylong valley
instance_of: Valley
countries: Australia
Lady Peak. Lady Peak is a mountain located just southeast of Cheam Peak in the Cheam Range near Chilliwack, British Columbia. It is west of the four peaks in the eastern portion of the range known as the Lucky Four Group,
consisting of Knight, Foley, Stewart and Welch peaks.

Geographic entities mentioned:
surface_form: Cheam Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.1867
lon: -121.682
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: lady peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.1753
lon: -121.666
According to the &quot;Canadian Mountain Encyclopedia&quot; &quot;From the Chilliwack area, according to Nation culture, Lady Peak looks like the head of a dog. This dog is the companion of the Old Woman, Cheam&quot;
Lady Peak can be summited by a route that branches off the Cheam Peak Trail. The peak was named by Arthur S.

Geographic entities mentioned:
surface_form: Cheam
instance_of: Mountain
countries: Canada
coordinates: lat: 49.1867
lon: -121.682
surface_form: cheam peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.1867
lon: -121.682
surface_form: lady peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.1753
lon: -121.666
The peak was named by Arthur S. Williamson, superintendent of the nearby Lucky Four Mine, to honor Phyllis Munday, the well-known Canadian mountaineer. Williamson also named nearby Baby Munday Peak in honor of her daughter, Edith. Both toponyms were officially adopted in 1946 by the Geographical Names Board of Canada. Climate.

Geographic entities mentioned:
surface_form: Baby Munday Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.166667
lon: -121.628334
surface_form: baby munday peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.166667
lon: -121.628334
It is west of the four peaks in the eastern portion of the range known as the Lucky Four Group,
consisting of Knight, Foley, Stewart and Welch peaks. According to the &quot;Canadian Mountain Encyclopedia&quot; &quot;From the Chilliwack area, according to Nation culture, Lady Peak looks like the head of a dog.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: lady peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.1753
lon: -121.666
Lady Peak. Lady Peak is a mountain located just southeast of Cheam Peak in the Cheam Range near Chilliwack, British Columbia. It is west of the four peaks in the eastern portion of the range known as the Lucky Four Group,
consisting of Knight, Foley, Stewart and Welch peaks.

Geographic entities mentioned:
surface_form: lady peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.1753
lon: -121.666
The summit of Mount Lamborn is the highest point in Delta County. Together with nearby Landsend Peak to the southwest, it lies at the western edge of the West Elks, rising dramatically nearly 6,000 ft (1,800 m) above the valley of the North Fork Gunnison River to the west. Mountain. Mount Lamborn is an eroded igneous intrusion that geologists call a laccolith.

Geographic entities mentioned:
surface_form: Landsend Peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.770833333333
lon: -107.55166666667
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Mount Lamborn. Mount Lamborn is a mountain summit in the West Elk Mountains range of the Rocky Mountains of North America. The peak is located in Gunnison National Forest, southeast by south (bearing 141°) of the Town of Paonia in Delta County, Colorado, United States. The summit of Mount Lamborn is the highest point in Delta County.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount lamborn
instance_of: Mountain
countries: United States
coordinates: lat: 38.803055555556
lon: -107.52277777778
Mount Lamborn. Mount Lamborn is a mountain summit in the West Elk Mountains range of the Rocky Mountains of North America. The peak is located in Gunnison National Forest, southeast by south (bearing 141°) of the Town of Paonia in Delta County, Colorado, United States. The summit of Mount Lamborn is the highest point in Delta County.

Geographic entities mentioned:
surface_form: mount lamborn
instance_of: Mountain
countries: United States
coordinates: lat: 38.803055555556
lon: -107.52277777778
The summit of Mount Lamborn is the highest point in Delta County. Together with nearby Landsend Peak to the southwest, it lies at the western edge of the West Elks, rising dramatically nearly 6,000 ft (1,800 m) above the valley of the North Fork Gunnison River to the west. Mountain. Mount Lamborn is an eroded igneous intrusion that geologists call a laccolith.

Geographic entities mentioned:
surface_form: mount lamborn
instance_of: Mountain
countries: United States
coordinates: lat: 38.803055555556
lon: -107.52277777778
Learned Pond. Learned Pond was formed during the last glaciation. It is next to Brigham Road and Union Ave in Framingham, Massachusetts next to MetroWest Medical Center at an elevation of 165 ft. The pond has a beach and is surrounded in parts by woods.

Geographic entities mentioned:
surface_form: learned pond
instance_of: Lake
countries: United States
coordinates: lat: 42.2875
lon: -71.4194
Mount Scott (New Zealand). Mount Scott is a mountain in the Canterbury Region of New Zealand. Description. Mount Scott is located northwest of Christchurch in Arthur's Pass National Park. It is set in the Polar Range of the Southern Alps in the South Island.

Geographic entities mentioned:
surface_form: mount scott
instance_of: Mountain
countries: New Zealand
coordinates: lat: -42.927
lon: 171.682
Mount Scott is a mountain in the Canterbury Region of New Zealand. Description. Mount Scott is located northwest of Christchurch in Arthur's Pass National Park. It is set in the Polar Range of the Southern Alps in the South Island. Precipitation runoff from the mountain's west slope drains into the Edwards River, whereas the east slope drains to the Hawdon River via Sudden Valley Stream.

Geographic entities mentioned:
surface_form: mount scott
instance_of: Mountain
countries: New Zealand
coordinates: lat: -42.927
lon: 171.682
Climate. Based on the Köppen climate classification, Mount Scott is located in a marine west coast (Cfb) climate zone, with a subpolar oceanic climate (Cfc) at the summit. Prevailing westerly winds blow moist air from the Tasman Sea onto the mountains, where the air is forced upwards by the mountains (orographic lift), causing moisture to drop in the form of rain or snow.

Geographic entities mentioned:
surface_form: mount scott
instance_of: Mountain
countries: New Zealand
coordinates: lat: -42.927
lon: 171.682
During King Philip's War in 1675, the governor of New York, Edmund Andros, ordered that all canoes east of Hell Gate be confiscated. This was done to prevent local indigenous people from helping their Native allies on the mainland, who were attacking New England settlers there. Notable sachems, such as Tackapousha of the Massapequa, saw their influence wane post-King Philip's War in 1675.

Geographic entities mentioned:
surface_form: Hell Gate
instance_of: Landform
countries: United States
coordinates: lat: 40.78102
lon: -73.92452
The North Shore beaches are rocky from the remaining glacial debris, while the South Shore's are crisp, clear, outwash sand. Jayne's Hill, at, within Suffolk County near its border with Nassau County, is the highest hill along either moraine; another well-known summit is Bald Hill in Brookhaven Town, not far from its geographical center at Middle Island.

Geographic entities mentioned:
surface_form: Jayne's Hill
instance_of: Mountain
countries: United States
coordinates: lat: 40.815
lon: -73.425
Glacial till plains (Ohio). The Glacial till plains are a till plain landform in Northern Ohio, located near the shore of Lake Erie and produced by the retreat of the Wisconsin glaciation. Since glacial till is highly fertile soil, agriculture on the glacial till plains is very productive.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Since glacial till is highly fertile soil, agriculture on the glacial till plains is very productive. The region has gently rolling moraine hills left over from the retreating glaciers, as well as small sandy ridges, which were formed as coastal dunes during periods in which Lake Erie was higher than it is today (14,000-12,000 years ago).

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Magdalena tinamou. The Magdalena tinamou, &quot;Crypturellus erythropus saltuarius&quot;, is a member of one of the most ancient bird families, the tinamous. It is endemic to the Magdalena River Valley in Colombia, and had been considered possibly extinct, because of an absence of confirmed records since the type specimen was collected in 1943.

Geographic entities mentioned:
surface_form: Magdalena River Valley
instance_of: Valley
countries: Colombia
coordinates: lat: 7.05969444
lon: -73.85308333
Ecology. The type specimen was taken in Ayacucho in the Cesar Department, and the only other known specimen (although its present whereabouts is unknown) was taken near Mariquita in the Tolima Department (often erroneously listed as being in the Neiva Department [&quot;sic&quot;]). Both are in the Magdalena River Valley of Colombia.

Geographic entities mentioned:
surface_form: Magdalena River Valley
instance_of: Valley
countries: Colombia
coordinates: lat: 7.05969444
lon: -73.85308333
Chew Valley hoard. The Chew Valley hoard is a hoard of 2,528 coins from the mid-11th century, very shortly after the Norman Conquest of England in 1066, that was found in the Chew Valley, Somerset, England, in 2019. It is one of the largest finds of Norman coins in the UK. Discovery.

Geographic entities mentioned:
surface_form: Chew Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.337422222222
lon: -2.6151972222222
The mountain sits about southwest of the village of Vågåmo and about northwest of the village of Beitostølen. The mountain is surrounded by several other notable mountains including Rasletinden to the east; Tjønnholstinden and Tjønnholsoksle to the north; Skarvflytindene, Leirungskampen, and Austre Leirungstinden to the northwest; and Torfinnstindene to the west.

Geographic entities mentioned:
surface_form: Tjønnholsoksle
instance_of: Mountain
countries: Norway
coordinates: lat: 61.432777777778
lon: 8.6372222222222
surface_form: Skarvflytindene
instance_of: Mountain
countries: Norway
coordinates: lat: 61.443742
lon: 8.586625
surface_form: Leirungskampen
instance_of: Mountain
countries: Norway
coordinates: lat: 61.39573
lon: 8.60128
surface_form: Torfinnstindene
instance_of: Mountain
countries: Norway
coordinates: lat: 61.372222222222
lon: 8.5805555555556
surface_form: leirungstinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.42171
lon: 8.60059
surface_form: austre leirungstinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.42171
lon: 8.60059
Kalvehøgde is a long massif in the southernmost part of the Jotunheimen mountain range. The northern part of the massif lies within Jotunheimen National Park. The massif rises quite slowly from lake Bygdin, and ends in an extremely steep wall to the north. The wall is about high. On the northern side of the massif, there are several glaciers, with Leirungsbrean as the greatest.

Geographic entities mentioned:
surface_form: Bygdin
instance_of: Lake
countries: Norway
coordinates: lat: 61.348475
lon: 8.518661
The southwestern summit of Nordre Kalveholotind and the northeastern summit of Munken branches off from the main massif, and they can be reached easily from the main massif. Mostly the massif is also easily accessible from lake Bygdin, but that constitutes a rather long hike along the lake.

Geographic entities mentioned:
surface_form: Bygdin
instance_of: Lake
countries: Norway
coordinates: lat: 61.348475
lon: 8.518661
Kalvehøgde. Kalvehøgde is a mountain group in Vågå Municipality and Vang Municipality in Innlandet county, Norway. The tall mountain is located in the Jotunheimen mountains. The mountain sits about southwest of the village of Vågåmo and about northwest of the village of Beitostølen.

Geographic entities mentioned:
surface_form: kalvehøgde
instance_of: Mountain
countries: Norway
coordinates: lat: 61.393055555556
lon: 8.6194444444444
The mountain is surrounded by several other notable mountains including Rasletinden to the east; Tjønnholstinden and Tjønnholsoksle to the north; Skarvflytindene, Leirungskampen, and Austre Leirungstinden to the northwest; and Torfinnstindene to the west. Kalvehøgde is a long massif in the southernmost part of the Jotunheimen mountain range.

Geographic entities mentioned:
surface_form: kalvehøgde
instance_of: Mountain
countries: Norway
coordinates: lat: 61.393055555556
lon: 8.6194444444444
Because of the number of summits, there has been a need for more distinct names for all the seven summits, and the National Map Institute has decided upon the name Munken (the Monk) for the northeastern plateau - seen in the lowermost picture, Mugna (probably meaning huge) for the two central summits, Kalvehøgde (reindeer calf mountain) for the three western summits, and lastly Nordre Kalveholotind (northern reindeer calf hole peak) for the southwestern summit, which is the only summit which has a prominent, steep wall on the southern side of the massif.

Geographic entities mentioned:
surface_form: kalvehøgde
instance_of: Mountain
countries: Norway
coordinates: lat: 61.393055555556
lon: 8.6194444444444
Snow sparrows and mountain grouses are frequent and reindeers can be seen, but they mostly prefer the grassy slopes down towards lake Bygdin. The Eastern Kalvehøgde and the Mugna summit were both climbed in 1820 by the two students Balthazar Mathias Keilhau and Peter Christian Bianco Boeck, both later prominent scientists at the university of Christiania.

Geographic entities mentioned:
surface_form: kalvehøgde
instance_of: Mountain
countries: Norway
coordinates: lat: 61.393055555556
lon: 8.6194444444444