Sarmila/GeoWiki-Features huggingface dataset:
The northern corrie of Corrie na Glas-lic holds the aforementioned lochs of Loch Cnoc na Mointeich and Loch Coireag nan Mang. Moruisg received something a boost in 1981 when the adjoining mountain of Sgùrr nan Ceannaichean, 2.5 km to the south west, was elevated to Munro status thus making a more interesting circular walk for Munro baggers.

Geographic entities mentioned:
surface_form: Sgùrr nan Ceannaichean
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.481753
lon: -5.1926756
surface_form: sgùrr nan ceannaichean
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.481753
lon: -5.1926756
To the south west is a ridge that skirts Coire Toll nam Bian and connects to Sgurr nan Ceannaichean. The northern corries look out over featureless moorland which descends towards Achnasheen. To the east of the highest point the plateau undulates, going over several minor tops before culminating in the outlying top of Càrn Gorm (875 metres) which is marked by an OS trig point. Ascents.

Geographic entities mentioned:
surface_form: Càrn Gorm
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.6221
lon: -4.2253
surface_form: càrn gorm
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.6221
lon: -4.2253
Another path starts at Glenuaig Lodge and climbs the precipitous southern slopes direct to the mountains summit. View. The mountain is a fine viewpoint being surrounded by deep glens it has a sizeable topographic prominence of 594 metres. The highlights of the view from the summit are the remote mountains to the north of Loch Monar and the rest of the Glen Carron mountains to the west.

Geographic entities mentioned:
surface_form: Loch Monar
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.4171
lon: -5.0988
surface_form: loch monar
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.4171
lon: -5.0988
This walk goes along the rim of the fine corrie of Coire Toll nan Bian (see picture) which stands between the two mountains, although Sgùrr nan Ceannaichean has since been demoted to a Corbett. Mòruisg is a long, steep sided mountain with a flat extensive summit plateau, the level top has many minor bumps and cairns and it can be difficult to ascertain the highest point, especially in mist.

Geographic entities mentioned:
surface_form: sgùrr nan ceannaichean
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.481753
lon: -5.1926756
Almost all ascents of Mòruisg are combined with the neighbouring Munro of Sgurr nan Ceannaichean. Approaches are possible from the south using well graded stalkers' paths; one of these leaves the valley of the Allt a’ Chonais and climbs Sgùrr nan Ceannaichean first before continuing to Mòruisg.

Geographic entities mentioned:
surface_form: sgùrr nan ceannaichean
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.481753
lon: -5.1926756
surface_form: mòruisg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.499712
lon: -5.17063
Its north and western slopes descend steeply to Glen Carron, its southern flanks are precipitous as they fall the valley of the Allt a’ Chonais which contains the track to Glenuaig Lodge. To the south west is a ridge that skirts Coire Toll nam Bian and connects to Sgurr nan Ceannaichean. The northern corries look out over featureless moorland which descends towards Achnasheen.

Geographic entities mentioned:
surface_form: sgurr nan ceannaichean
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.481753
lon: -5.1926756
Ascents. The direct ascent of Mòruisg starts on the A890 road in Glen Carron at a parking spot one kilometre west of Loch Sgamhain at grid reference. After crossing the River Carron by the footbridge it is a steep climb of almost 800 metres to reach the summit through heather and scree. Almost all ascents of Mòruisg are combined with the neighbouring Munro of Sgurr nan Ceannaichean.

Geographic entities mentioned:
surface_form: sgurr nan ceannaichean
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.481753
lon: -5.1926756
surface_form: mòruisg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.499712
lon: -5.17063
Ascents. The direct ascent of Mòruisg starts on the A890 road in Glen Carron at a parking spot one kilometre west of Loch Sgamhain at grid reference. After crossing the River Carron by the footbridge it is a steep climb of almost 800 metres to reach the summit through heather and scree. Almost all ascents of Mòruisg are combined with the neighbouring Munro of Sgurr nan Ceannaichean.

Geographic entities mentioned:
surface_form: loch sgamhain
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.5263
lon: -5.1746
surface_form: mòruisg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.499712
lon: -5.17063
Mòruisg. Mòruisg is a Scottish mountain situated in the Glencarron and Glenuig Forest, 10 kilometres south west of the village of Achnasheen in the Highland council area. Overview. The hill reaches a height of 928 metres (3044 feet) and is the most easily accessible of the Glen Carron Munros, being situated just three kilometres from the A890 road which runs through the glen.

Geographic entities mentioned:
surface_form: mòruisg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.499712
lon: -5.17063
Geography. The lake is situated at. Yeşilova ilçe (district) of Burdur Province is to the west of the lake. It is in a closed basin of Turkey which is popularly called &quot;Göller Yöresi&quot; (&quot;the region of lakes&quot;). Lake Burdur is to the north east, Lake Salda is to the west and Lake Karataş is to the south of Lake Yarışlı. The area of the lake is. It is a salt lake.

Geographic entities mentioned:
surface_form: Lake Burdur
instance_of: Lake
countries: Turkey
coordinates: lat: 37.7337
lon: 30.1781
surface_form: Lake Salda
instance_of: Lake
countries: Turkey
coordinates: lat: 37.5508
lon: 29.6833
surface_form: Lake Karataş
instance_of: Lake
countries: Turkey
coordinates: lat: 37.38596
lon: 29.97174
With its summit reaching 1,510 meters high, Mount Nif was one of the mountains called Olympus in ancient times and is renowned today for its dense forests of oaks, oleasters, pines and other trees of the Aegean basin, cold springs and trout farms.

Geographic entities mentioned:
surface_form: Mount Nif
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.387872
lon: 27.356461
It is part of the vast Northern European Plain that stretches from northern France to western Russia. The Berlin–Warsaw &quot;Urstromtal&quot; (ice age glacial valley), between the low Barnim Plateau to the north and the Teltow Plateau to the south, was formed by meltwater flowing from ice sheets at the end of the last Weichselian glaciation. The Spree follows this valley now.

Geographic entities mentioned:
surface_form: Barnim Plateau
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
In Spandau, Berlin's westernmost borough, the Spree empties into the river Havel, which flows from north to south through western Berlin. The course of the Havel is more like a chain of lakes, the largest being the Tegeler See and Großer (Grosser) Wannsee. A series of lakes also feeds into the upper Spree, which flows through the Großer (Grosser) Müggelsee in eastern Berlin.

Geographic entities mentioned:
surface_form: Großer (Grosser) Wannsee
instance_of: Lake
countries: Germany
coordinates: lat: 52.4275
lon: 13.173055555556
The course of the Havel is more like a chain of lakes, the largest being the Tegeler See and Großer (Grosser) Wannsee. A series of lakes also feeds into the upper Spree, which flows through the Großer (Grosser) Müggelsee in eastern Berlin. Substantial parts of present-day Berlin extend onto the low plateaus on both sides of the Spree Valley.

Geographic entities mentioned:
surface_form: Großer (Grosser) Müggelsee
instance_of: Lake
countries: Germany
coordinates: lat: 52.433333333333
lon: 13.65
The borough of Spandau lies partly within the Berlin Glacial Valley and partly on the Nauen Plain, which stretches to the west of Berlin. The highest elevations in Berlin are the Teufelsberg and the Müggelberge in the city's outskirts, and the Kreuzberg is the highest elevation in the centre. While the latter measures above sea level, the former are both about above sea level.

Geographic entities mentioned:
surface_form: Müggelberge
instance_of: Mountain
countries: Germany
coordinates: lat: 52.416111111111
lon: 13.633333333333
&quot;De Haven&quot; was hit by three bombs and further damaged by a near miss. One bomb hit the superstructure squarely, killing the commanding officer instantly. All was lost after the first hit and the ship began to settle rapidly, sinking in Ironbottom Sound about east of Savo Island. One of the LCTs she had escorted rescued the survivors. &quot;De Haven&quot; lost 167 killed and 38 wounded.

Geographic entities mentioned:
surface_form: Savo Island
instance_of: Mountain
countries: Solomon Islands
coordinates: lat: -9.1333333333333
lon: 159.81666666667
The community is located northwest of Sacramento, southwest of Red Bluff, and northwest of Corning. Forty-three percent of the town's residents fall below the federal poverty level. The community lies amidst rolling hills of oak and pine trees with views of Mount Shasta and Lassen Peak. The area has a variety of wildlife with scattered domestic cattle grazing.

Geographic entities mentioned:
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
Smaller occurrences have been reported in the Red Feather Lakes, near Fort Collins, Colorado; Amethyst Mountain, Texas; Yellowstone National Park; Delaware County, Pennsylvania; Haywood County, North Carolina; Deer Hill and Stow, Maine, and in the Lake Superior region of Minnesota, Wisconsin, and Michigan. Amethyst is relatively common in the Canadian provinces of Ontario and Nova Scotia.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Personal life. Sammis married English professor Sterling Andrus Leonard in 1913. They had a daughter, Barbara Leonard Reynolds, who became a noted peace activist with her husband, Earle L. Reynolds. Sterling Leonard drowned while canoeing with I. A. Richards on Lake Mendota in 1931. She died in 1960, in Madison, at the age of 86.

Geographic entities mentioned:
surface_form: Lake Mendota
instance_of: Lake
countries: United States
coordinates: lat: 43.106666666667
lon: -89.424722222222
The county was created on 1 April 1974 from parts of north-east Cheshire, south-east Lancashire, and a small part of the West Riding of Yorkshire. The centre and south-west of Greater Manchester are lowlands, similar to the West Lancashire Coastal Plain to the north-west and the Cheshire Plain to the south-west.

Geographic entities mentioned:
surface_form: Cheshire Plain
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.2
lon: -2.4666666666667
The Pennines rise to the north and east of the county with the West Pennine Moors in the northwest, the South Pennines in the northeast and the Peak District in the east. Several coalfields (mainly sandstones and shales) lie in the west of the county while the Cheshire Plain fringes the south. The rivers Mersey, Irwell and Tame run through Greater Manchester, all of which rise in the Pennines.

Geographic entities mentioned:
surface_form: Cheshire Plain
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.2
lon: -2.4666666666667
The rivers Mersey, Irwell and Tame run through Greater Manchester, all of which rise in the Pennines. Other rivers traverse the region as tributaries to the major rivers, including the Douglas, the Irk, and the Roch. Black Chew Head is the highest point in Greater Manchester which forms part of the Peak District National Park, rising above sea-level, within the parish of Saddleworth.

Geographic entities mentioned:
surface_form: Irk
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 53.4869
lon: -2.24504
The rivers Mersey, Irwell and Tame run through Greater Manchester, all of which rise in the Pennines. Other rivers traverse the region as tributaries to the major rivers, including the Douglas, the Irk, and the Roch. Black Chew Head is the highest point in Greater Manchester which forms part of the Peak District National Park, rising above sea-level, within the parish of Saddleworth.

Geographic entities mentioned:
surface_form: Black Chew Head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.5161
lon: -1.9216
Clover, sorrel, nettle and thistle are common, and grow wild in Greater Manchester. Common heather (&quot;Calluna vulgaris&quot;) dominates the uplands, such as Saddleworth Moor, which lies within the South Pennines and Dark Peak area of the Peak District National Park. The Rochdale Canal harbours floating water-plantain (&quot;Luronium natams&quot;), a nationally endangered aquatic plant.

Geographic entities mentioned:
surface_form: Saddleworth Moor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.543333333333
lon: -1.9558333333333
surface_form: Dark Peak
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 53.4
lon: -1.8
Between the Hills. Between the Hills is a small valley in northwest Loudoun County, Virginia, distinct from, but associated with, the greater Loudoun Valley. Geography. The Between the Hills valley encompasses the area of Loudoun that lies west of Short Hill Mountain and east of the Blue Ridge Mountain. The area includes the communities of Neersville and Loudoun Heights.

Geographic entities mentioned:
surface_form: Loudoun Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.2329
lon: -77.735
surface_form: between the hills
instance_of: Valley
countries: United States
coordinates: lat: 39.25
lon: -77.7333
Between the Hills. Between the Hills is a small valley in northwest Loudoun County, Virginia, distinct from, but associated with, the greater Loudoun Valley. Geography. The Between the Hills valley encompasses the area of Loudoun that lies west of Short Hill Mountain and east of the Blue Ridge Mountain. The area includes the communities of Neersville and Loudoun Heights.

Geographic entities mentioned:
surface_form: Short Hill Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.25
lon: -77.71
surface_form: Blue Ridge Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.08166667
lon: -77.86222222
surface_form: blue ridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.275833333333
lon: -74.403888888889
surface_form: blue ridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.60777778
lon: -76.09305556
surface_form: between the hills
instance_of: Valley
countries: United States
coordinates: lat: 39.25
lon: -77.7333
Between the Hills can be divided into two sections; the upper and lower valley. The upper valley encompasses the area north of the Hillsboro Gap in the Short Hill, while the lower valley encompasses the area south of the gap. The valley ranges from wide at its largest, just south of the Hillsboro gap to wide at its smallest, east of Purcell Knob in the upper valley and is approximately long.

Geographic entities mentioned:
surface_form: Purcell Knob
instance_of: Mountain
countries: United States
coordinates: lat: 39.2582
lon: -77.7497
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The main waterways of Between the Hills are the North Fork of Catoctin Creek, which drains the lower valley before flowing through the Hillsboro gap into the Catoctin Valley, and Piney Run, which drains the upper valley and flows north through the valley directly into the Potomac River. Across the Potomac River, the valley continues as Pleasant Valley in Maryland. Transportation.

Geographic entities mentioned:
surface_form: Catoctin Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.23
lon: -77.64
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: between the hills
instance_of: Valley
countries: United States
coordinates: lat: 39.25
lon: -77.7333
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Transportation. State Route 671, Harpers Ferry Road, is the main road in the valley, running north–south through the upper valley from its southern terminus at Virginia State Route 9, Charles Town Pike, west of Hillsboro, to its northern terminus at U.S. Route 340, south of the Sandy Hook bridge over the Potomac River and east of Harpers Ferry.

Geographic entities mentioned:
surface_form: sandy hook
instance_of: Landform
countries: United States
coordinates: lat: 40.452891
lon: -73.995237
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
Confederate partisan John Mosby and his Rangers suffered their first defeat in the valley and along the eastern slopes of the Blue Ridge in the Battle of Loudoun Heights, fought on January 1, 1864. References. Scheel, Eugene M. &quot;Loudoun Discovered: Communities, Corners and Crossroads, Vol V.

Geographic entities mentioned:
surface_form: battle
instance_of: Watercourse
countries: United States
coordinates: lat: 44.9266
lon: -93.0291
surface_form: loudoun heights
instance_of: Mountain
countries: United States
coordinates: lat: 39.3078
lon: -77.7386
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
Geography. The Between the Hills valley encompasses the area of Loudoun that lies west of Short Hill Mountain and east of the Blue Ridge Mountain. The area includes the communities of Neersville and Loudoun Heights. Between the Hills can be divided into two sections; the upper and lower valley.

Geographic entities mentioned:
surface_form: loudoun heights
instance_of: Mountain
countries: United States
coordinates: lat: 39.3078
lon: -77.7386
The main waterways of Between the Hills are the North Fork of Catoctin Creek, which drains the lower valley before flowing through the Hillsboro gap into the Catoctin Valley, and Piney Run, which drains the upper valley and flows north through the valley directly into the Potomac River. Across the Potomac River, the valley continues as Pleasant Valley in Maryland. Transportation.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: pleasant valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6389
lon: -77.5472
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: pleasant valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6409256
lon: -114.0184307
Route 340, south of the Sandy Hook bridge over the Potomac River and east of Harpers Ferry. State Route 719, Stony Point-Woodgrove road runs north–south through the lower valley from Hillsboro to Woodgrove. The Charlestown pike bisects the valley, running southeast–northwest from the Hillsboro Gap to Keyes Gap in the Blue Ridge. Geology.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Between the Hills. Between the Hills is a small valley in northwest Loudoun County, Virginia, distinct from, but associated with, the greater Loudoun Valley. Geography. The Between the Hills valley encompasses the area of Loudoun that lies west of Short Hill Mountain and east of the Blue Ridge Mountain. The area includes the communities of Neersville and Loudoun Heights.

Geographic entities mentioned:
surface_form: between the hills
instance_of: Valley
countries: United States
coordinates: lat: 39.25
lon: -77.7333
The area includes the communities of Neersville and Loudoun Heights. Between the Hills can be divided into two sections; the upper and lower valley. The upper valley encompasses the area north of the Hillsboro Gap in the Short Hill, while the lower valley encompasses the area south of the gap.

Geographic entities mentioned:
surface_form: between the hills
instance_of: Valley
countries: United States
coordinates: lat: 39.25
lon: -77.7333
Geology. The Between the Hills Valley was formed by action along the Short Hill fault during the early Paleozoic era, which resulted in separation of the underlying rocks of the Blue Ridge and Short Hill mountains, which were deposited during the Catoctin Formation of the late Proterozoic period and uplifted during the Grenville Orogeny.

Geographic entities mentioned:
surface_form: between the hills
instance_of: Valley
countries: United States
coordinates: lat: 39.25
lon: -77.7333
History. During the American Civil War, a Between the Hills resident, John Mobberly, gained notoriety as a Confederate guerrilla. During the last two years of the war, he successfully disputed control of the area through his daring exploits, until his assassination outside of Neersville in April 1865.

Geographic entities mentioned:
surface_form: between the hills
instance_of: Valley
countries: United States
coordinates: lat: 39.25
lon: -77.7333
During the last two years of the war, he successfully disputed control of the area through his daring exploits, until his assassination outside of Neersville in April 1865. In late November-early December 1864 much of the Between the Hills valley was put to the torch by Union cavalry during The Burning Raid, including Potts Mill, the ruins of which can be seen from off Stony Point Road.

Geographic entities mentioned:
surface_form: between the hills
instance_of: Valley
countries: United States
coordinates: lat: 39.25
lon: -77.7333
References. Scheel, Eugene M. &quot;Loudoun Discovered: Communities, Corners and Crossroads, Vol V. Waterford, The German Settlement and Between the Hills.&quot; The Friends of the Thomas Balch Library; Leesburg, Virginia 2002.

Geographic entities mentioned:
surface_form: between the hills
instance_of: Valley
countries: United States
coordinates: lat: 39.25
lon: -77.7333
It has also campaigned against the development of incinerators at Belfast North Foreshore and Lough Neagh, and against proposals to extend the airport runway at George Best Belfast City Airport. The Green Party campaigns not just for more environmental protection but also for politics for the common good.

Geographic entities mentioned:
surface_form: Lough Neagh
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.618333333333
lon: -6.3952777777778
The proposed border was described as follows: As drawn, this border was observed in 1907 by attorney Grant Jackson to contain a fatal flaw: it cut off from Angelenos the potentially valuable water supply from the Owens River in the Owens Valley, leaving it in the hands of northern Californians. This would have threatened the viability of the Los Angeles Aqueduct water project. Ecotopia.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
The various former sites of the brass- and iron-making industries that are scheduled monuments are features of the Angidy Trail, an 8-kilometre (5-mile) circular walking route, included in the Wye Valley National Landscape, a designated Area of Outstanding Natural Beauty.

Geographic entities mentioned:
surface_form: Wye Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69255
lon: -2.66283
It lies in the Huancavelica Region, Castrovirreyna Province, on the border of the districts of Castrovirreyna and Santa Ana, and in the Huancavelica Province, Huancavelica District. Qarwa K'anti lies south of Wachu Intiyuq, southwest of Antarasu and north of Yawar Q'asa.

Geographic entities mentioned:
surface_form: Wachu Intiyuq
instance_of: Mountain
countries: Peru
coordinates: lat: -12.9536
lon: -75.1558
surface_form: Antarasu
instance_of: Mountain
countries: Peru
coordinates: lat: -12.93722222
lon: -75.12972222
surface_form: Yawar Q'asa
instance_of: Mountain
countries: Peru
coordinates: lat: -12.9944
lon: -75.1464
surface_form: antarasu
instance_of: Mountain
countries: Peru
coordinates: lat: -12.93722222
lon: -75.12972222
surface_form: yawar q'asa
instance_of: Mountain
countries: Peru
coordinates: lat: -12.9944
lon: -75.1464
Qarwa K'anti. Qarwa K'anti (Quechua &quot;qarwa&quot; pale, yellowish, golden, &quot;k'anti&quot; a kind of distaff, &quot;yellowish distaff&quot;, Hispanicized spelling &quot;Jarhuacante&quot;) is a mountain in the Chunta mountain range in the Andes of Peru, about high.

Geographic entities mentioned:
surface_form: chunta
instance_of: Mountain
countries: Peru
coordinates: lat: -11.4964
lon: -76.3772
surface_form: chunta
instance_of: Mountain
countries: Peru
coordinates: lat: -14.7836
lon: -72.5717
surface_form: chunta
instance_of: Mountain
countries: Peru
coordinates: lat: -14.4222
lon: -73.8572
surface_form: qarwa k'anti
instance_of: Mountain
countries: Peru
coordinates: lat: -12.9783
lon: -75.1581
Qarwa K'anti. Qarwa K'anti (Quechua &quot;qarwa&quot; pale, yellowish, golden, &quot;k'anti&quot; a kind of distaff, &quot;yellowish distaff&quot;, Hispanicized spelling &quot;Jarhuacante&quot;) is a mountain in the Chunta mountain range in the Andes of Peru, about high.

Geographic entities mentioned:
surface_form: qarwa k'anti
instance_of: Mountain
countries: Peru
coordinates: lat: -12.9783
lon: -75.1581
Adenanthos labillardierei. &quot;Adenanthos labillardierei&quot; is a species of erect shrub endemic to the slopes of the Barren Ranges in the Fitzgerald River National Park in southwest Western Australia. Description. It grows as an erect shrub, usually less than  m in height.

Geographic entities mentioned:
surface_form: Barren Ranges
instance_of: Mountain
countries: Australia
coordinates: lat: -34.21638889
lon: 119.43277778
Lho La. The Lho La () is a col on the border between Nepal and Tibet north of the Western Cwm, near Mount Everest. It is at the lowest point of the West Ridge of the mountain at a height of. It is not exactly a Pass, but a part of Mt. Everest Range. There was once a proposal, which failed, to change its name to Khumbu La. History and name.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Following the 1952 Swiss Mount Everest expedition it was suggested that &quot;Lho La&quot; (South Pass) was an unsatisfactory name because it lies to the west of Everest and it would better be renamed &quot;Khumbu La&quot; because it led up from the Khumbu Glacier. This would allow the South Col to be called &quot;Lho La&quot; as it is the col south of Everest and between it and Lhotse.

Geographic entities mentioned:
surface_form: Lhotse
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.961666666667
lon: 86.933333333333
Lho La gave access to Everest's West Ridge and to its Western Cwm but they thought neither of these gave feasible ways of ascent. Lho La was also investigated by Bill Tilman and Edmund Wigram on the 1935 British Mount Everest reconnaissance expedition but, like the 1921 explorers, they also preferred the North Col route for a summit attempt. Approach from Nepal.

Geographic entities mentioned:
surface_form: North Col
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 28.015833333333
lon: 86.925
In 1989 five out of six climbers in a Polish team, attempting a descent that involved climbing Khumbutse from the West Rongbuk Glacier via Lho La, were swept to their deaths on the Lho La itself as they climbed above the col, with one survivor Andrzej Marciniak. External links.

Geographic entities mentioned:
surface_form: Khumbutse
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 28.020277777778
lon: 86.873055555556
Tawqani. Tawqani (Aymara &quot;tawqaña&quot; to pile up, &quot;-ni&quot; a suffix, also spelled &quot;Taucani&quot;) is a mountain in the Andes of Bolivia which reaches a height of approximately. It is located in the La Paz Department, Larecaja Province, Quiabaya Municipality, northwest of Tacacoma.

Geographic entities mentioned:
surface_form: tawqani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -15.56444444
lon: -68.7
Wind gusts reached in Stone Ridge. The high winds caused power outage across eastern New York, affecting 63,000 people in Dutchess and Ulster counties. The northeasterly winds also produced high waves along Lake George and Peck Lake, which damaged docks along their southern shores. The high winds caused a fatal traffic accident when a driver in Kerhonkson was struck by flying debris.

Geographic entities mentioned:
surface_form: Peck Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.114444444444
lon: -74.411388888889
Muskegon County was organized in 1859. Its name is from the Muskegon River, which runs through it and empties into Muskegon Lake and subsequently flows into Lake Michigan. The word &quot;Muskegon&quot; comes from the Ojibwa/Chippewa word &quot;mashkig,&quot; meaning &quot;marsh&quot; or &quot;swamp&quot;. &quot;See&quot; List of Michigan county name etymologies. Geography. According to the U.S.

Geographic entities mentioned:
surface_form: Muskegon Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.236849
lon: -86.290199
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Muskegon Lake then empties into Lake Michigan via the Muskegon Channel. Muskegon Lake is Michigan's only deep water port on Lake Michigan. In the north the White River flows through the county into White Lake and then on to Lake Michigan. In the south, Black Creek flows into Mona Lake which also flows into Lake Michigan.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
As the series was to be published in a magazine targeted at adults, Fujiko Mine was created to add a female presence and to fulfill a &quot;Bond girl&quot; role. Her name was inspired by a picture of Mount Fuji, Monkey Punch added the -ko female suffix to create her first name, and chose &quot;Mine&quot; for her family name because of its meaning as &quot;summit&quot;.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
Gheo-shih. Gheo-shih (5000 BC – 3000 BC), which translates to “&quot;River of the Gourd Trees&quot;” in the Zapotec language, is an open-air site found in the Oaxaca Valley that holds what is considered as the earliest representation of civic-ceremonial architecture. Within this site is a cleared area lined by boulders that is thought to have been used for rituals, dances or athletic competitions.

Geographic entities mentioned:
surface_form: Oaxaca Valley
instance_of: Valley
countries: Mexico
coordinates: lat: 17.045
lon: -96.7669
The former Visigothic bishopric of Baeza remains a Latin Catholic titular see. Geography. The town lies perched on a cliff in the range (the) separating the Guadalquivir River to its south from the Guadalimar to its north. History. The town stands at a high elevation about from the right bank of the Guadalquivir in the Loma de Úbeda. Under the Romans, the town was known as 'Beatia'.

Geographic entities mentioned:
surface_form: Guadalimar
instance_of: Watercourse
countries: Spain
coordinates: lat: 37.98333333
lon: -3.73333333
This chain of highlands divides the drainage of the rivers that flow to the east into the Pacific Ocean from those that flow west into the drainage of the Murray–Darling Basin (and thence to the Southern Ocean) or into inland waters, such as Lake Eyre, which lie below sea level, or else evaporate rapidly.

Geographic entities mentioned:
surface_form: Lake Eyre
instance_of: Lake
countries: Australia
coordinates: lat: -28.406
lon: 137.2963
Instead, the Australian Alps consist of a high plateau, with significantly softer rolling hills spread across a long, wide plateau that was lifted thousands of feet up by the movement of magma when Gondwana began to break up between 130 and 160 million years ago. The highest peak in the Australian Alps is Mount Kosciuszko ().

Geographic entities mentioned:
surface_form: Mount Kosciuszko
instance_of: Mountain
countries: Australia
coordinates: lat: -36.4558303
lon: 148.2635105
The State of Victoria is the one with the largest number of skiing areas in Australia. Mount Bogong, with its peak at 1986 m above sea level, is the highest peak in Victoria. The surrounding Bogong High Plains is one of the largest areas of snow country in Australia. It includes the leading resorts of Falls Creek and Mount Hotham.

Geographic entities mentioned:
surface_form: Mount Bogong
instance_of: Mountain
countries: Australia
coordinates: lat: -36.7325
lon: 147.30583333333334
The surrounding Bogong High Plains is one of the largest areas of snow country in Australia. It includes the leading resorts of Falls Creek and Mount Hotham. Recreational and practical skiing was being practised in the Victorian Alps by the 1880s and 1890s with skis made from local timbers, and making use of single steering poles.

Geographic entities mentioned:
surface_form: Mount Hotham
instance_of: Mountain
countries: Australia
coordinates: lat: -36.983333333333
lon: 147.13333333333
It includes the leading resorts of Falls Creek and Mount Hotham. Recreational and practical skiing was being practised in the Victorian Alps by the 1880s and 1890s with skis made from local timbers, and making use of single steering poles. Skiing began at Mount Buffalo in the 1890s, and a chalet was constructed in 1910. Australia's first ski tow was constructed near Mount Buffalo in 1936.

Geographic entities mentioned:
surface_form: Mount Buffalo
instance_of: Mountain
countries: Australia
coordinates: lat: -36.777
lon: 146.767
Route. In the southerly direction, the journey starts from the quayside in front of Lucerne station, in the central Swiss city of Lucerne (canton of Lucerne), which sits at the north-western end of Lake Lucerne (). This end of the lake is surrounded by the famous peaks of the Rigi, Pilatus and Bürgenstock, and the route sails between these mountains.

Geographic entities mentioned:
surface_form: Lake Lucerne
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.0194
lon: 8.4011
Route. In the southerly direction, the journey starts from the quayside in front of Lucerne station, in the central Swiss city of Lucerne (canton of Lucerne), which sits at the north-western end of Lake Lucerne (). This end of the lake is surrounded by the famous peaks of the Rigi, Pilatus and Bürgenstock, and the route sails between these mountains.

Geographic entities mentioned:
surface_form: Rigi
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.05
lon: 8.4666666666667
surface_form: Bürgenstock
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.000305555556
lon: 8.3983888888889
Descending this valley, with the aid of several more spiral loops, the train eventually arrives at Bellinzona, the capital city of Ticino that is famous for its three World Heritage listed castles. Connections are available at Bellinzona station for at Lago Maggiore. The train continues from Bellinzona to Lugano station, in the southern Swiss city of Lugano on the lake of the same name.

Geographic entities mentioned:
surface_form: the lake of the same name
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46
lon: 9
Because of the surrounding shield, the valley is narrow at its western end and then becomes increasingly wide (mainly on the Ontario side of the river) as it progresses eastward. The underlying geophysical structure is the Ottawa-Bonnechere Graben. Approximately 1.3 million people reside in the valley (&quot;and along its tributaries&quot;), around 80% of whom reside in Ottawa.

Geographic entities mentioned:
surface_form: Ottawa-Bonnechere Graben
instance_of: Landform
countries: Canada
coordinates: lat: 45.5767
lon: -76.9162
After the arrival of European settlers in North America, the first major industry of the Ottawa Valley was fur trading. The valley was part of the major cross-country route for French-Canadian Voyageurs, who would paddle canoes up the Ottawa River as far as Mattawa and then portage west through various rivers and lakes to Georgian Bay on Lake Huron.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
From west to east, communities in the Ottawa Valley include Deep River (with nearby Chalk River, the site of Canada's first nuclear reactor program), Mattawa, Petawawa (a major Canadian military base), Pembroke (where Samuel de Champlain landed briefly), Fort Coulonge, Shawville, Renfrew, Quyon, Arnprior, Ottawa (the nation's capital), Rockland, L'Orignal, Hawkesbury, and Rigaud and Almonte, Round Lake Centre, Dacre, Douglas, Hyndford, Scotch Bush, Osceola and Barr Line.

Geographic entities mentioned:
surface_form: round lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.64083333333333
lon: -77.52888888888889
surface_form: ottawa valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
surface_form: ottawa valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
surface_form: round lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.5333
lon: -102.367
Ottawa Valley. The Ottawa Valley (Vallée d'Outaouais) is the valley of the Ottawa River (Rivière des Outaouais), along the boundary between Eastern Ontario and the Outaouais, Quebec, Canada. The valley is the transition between the Saint Lawrence Lowlands and the Canadian Shield.

Geographic entities mentioned:
surface_form: ottawa valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
The underlying geophysical structure is the Ottawa-Bonnechere Graben. Approximately 1.3 million people reside in the valley (&quot;and along its tributaries&quot;), around 80% of whom reside in Ottawa. The total area of the Ottawa Valley is 2.4 million ha (6 million ac). The National Capital Region area has just over 1.4 million inhabitants in both provinces.

Geographic entities mentioned:
surface_form: ottawa valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
The National Capital Region area has just over 1.4 million inhabitants in both provinces. Near the City of Ottawa, the Ottawa Valley merges with the St. Lawrence Valley to the south to create a delta of flat farmland stretching unbroken from the Ottawa River to the Saint Lawrence River as far east as the island of Montreal, where the two rivers meet.

Geographic entities mentioned:
surface_form: ottawa valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
The area is sometimes referred to as the &quot;Lower Ottawa Valley,&quot; in contrast with the &quot;Upper Ottawa Valley&quot; west of Ottawa, but the name is not common, and most people think of the Ottawa Valley as only the upper portion.

Geographic entities mentioned:
surface_form: ottawa valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
surface_form: ottawa valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
surface_form: ottawa valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
However, there are many Algonquin communities and individuals not recognized as such by the Government of Canada under the &quot;Indian Act&quot;. These individuals are referred to as &quot;non-status Indians&quot;. Ardoch Algonquin First Nation is one such community located in the Ottawa Valley fighting for the return of the land they lost to the Iroquois.

Geographic entities mentioned:
surface_form: ottawa valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
As a relatively recent adaptation resulting from the economic pressures of the encroachment of non-native settling of the valley, the Algonquin First Nation is unevenly distributed within their territory. After the arrival of European settlers in North America, the first major industry of the Ottawa Valley was fur trading.

Geographic entities mentioned:
surface_form: ottawa valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
Major settlements in the Upper Ottawa Valley. Petawawa is a town located in Renfrew County, in the Ottawa Valley. It was thought to have been first settled by the Algonquian peoples and the name comes from their language meaning &quot;where one hears the noise of the water&quot;. Samuel de Champlain passed through the area and it was used as an important location for the Hudson's Bay Company.

Geographic entities mentioned:
surface_form: ottawa valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
Language. English and French are both commonly spoken throughout the Ottawa Valley on both sides of the river. The Counties of Prescott and Russell County, in the Ottawa Valley, has the highest concentration of francophones in Canada west of Quebec. The variant of French spoken in this area of the province is also based on Quebec French, but distinctly different from that of the Outaouais region.

Geographic entities mentioned:
surface_form: ottawa valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
Valley twang. Regional English accents are rare west of Québec, but because of its isolation before the arrival of the railways and also by the mixture of the dominant French, Irish and Scottish populations, the valley at one time developed a distinctive dialect, referred to as the Ottawa Valley Twang.

Geographic entities mentioned:
surface_form: ottawa valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
Traditions continued in the Valley's festivals and hotels. Of these, Lennox Gavan's Hotel in Quyon, Quebec and Fred Meilleur's Chapeau Hotel on L'Ile aux Allumettes (now burned down), Quebec were particularly influential. Legendary performer and songwriter Mac Beattie and the Melodiers were also large influences on keeping the Ottawa Valley's musical culture vibrant and living.

Geographic entities mentioned:
surface_form: ottawa valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
There are also three road bridges to the west of the city and one to the east, all along Country Road 17 and Route 148. There are also a number of ferries at various points along the river which can transport people and vehicles across. Part of the Trans Canada Railway passes through the Ottawa Valley. Via Rail operates passenger trains to and from Ottawa and other towns in the Ottawa Valley.

Geographic entities mentioned:
surface_form: ottawa valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
With the Senators' arena Canadian Tire Centre (CTC), originally named the &quot;Palladium&quot;, located in Kanata, Ontario, which links Ottawa with the Valley, residents of the Upper Ottawa Valley can easily access the games. The CTC is the home of the &quot;Ottawa Sports Hall of Fame&quot;, several restaurants, a fitness complex and several businesses.

Geographic entities mentioned:
surface_form: ottawa valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
Uña Paka. Uña Paka (Quechua &quot;uña&quot; little animal, &quot;paka&quot; eagle, &quot;little eagle&quot;, Hispanicized spelling &quot;Uñapaca&quot;) is a mountain in the Huancavelica Region in Peru, about high. It is located in the Huancavelica Province, Huachocolpa District, and in the Huaytará Province, Pilpichaca District.

Geographic entities mentioned:
surface_form: uña paka
instance_of: Mountain
countries: Peru
coordinates: lat: -13.193055555556
lon: -74.931111111111
surface_form: paka
instance_of: Mountain
countries: Peru
coordinates: lat: -11.89583333
lon: -76.06611111
Uña Paka. Uña Paka (Quechua &quot;uña&quot; little animal, &quot;paka&quot; eagle, &quot;little eagle&quot;, Hispanicized spelling &quot;Uñapaca&quot;) is a mountain in the Huancavelica Region in Peru, about high. It is located in the Huancavelica Province, Huachocolpa District, and in the Huaytará Province, Pilpichaca District.

Geographic entities mentioned:
surface_form: uña paka
instance_of: Mountain
countries: Peru
coordinates: lat: -13.193055555556
lon: -74.931111111111
surface_form: uñapaca
instance_of: Mountain
countries: Peru
coordinates: lat: -13.193055555556
lon: -74.931111111111
surface_form: paka
instance_of: Mountain
countries: Peru
coordinates: lat: -11.89583333
lon: -76.06611111
surface_form: paka
instance_of: Mountain
countries: Peru
coordinates: lat: -11.89583333
lon: -76.06611111
Geography. Ashville is located in the Scioto River Valley and has an elevation of 715 feet (218 m) above sea level. The village is located in the till plain-area of Western Ohio and borders the Appalachian Plateau. The area is generally viewed to be a fertile region with gently rolling hills created by moraines.

Geographic entities mentioned:
surface_form: Appalachian Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 40
lon: -78
it is generally uncommon but has a large range across West Visayas and Luzon. More surveys and understanding of its biology are needed and it is highly possible that this species be uplisted due to habitat destruction. It is found in multiple protected areas such as Mount Banahaw, Mount Makiling, Mount Isarog, Bataan National Park and Northern Sierra Madre Natural Park, Mt.

Geographic entities mentioned:
surface_form: Mount Banahaw
instance_of: Mountain
countries: Philippines
coordinates: lat: 14.066666666667
lon: 121.48333333333
surface_form: Mount Makiling
instance_of: Mountain
countries: Philippines
coordinates: lat: 14.13
lon: 121.2
surface_form: Mount Isarog
instance_of: Mountain
countries: Philippines
coordinates: lat: 13.659166666667
lon: 123.37333333333
surface_form: Mt. Kanlaon Natural Park
instance_of: Mountain
countries: Philippines
coordinates: lat: 10.411944444444
lon: 123.13194444444
La Vereda del Monte was the upper part of La Vereda Caballo, (Spanish for &quot;The Horse Trail&quot;), used by mesteñeros from the early 1840s to drive Alta California horses to Sonora for sale. From its northern beginning at Point of Timber on the Sacramento River Delta near modern-day Brentwood, the trail traveled south to the Livermore Valley.

Geographic entities mentioned:
surface_form: Livermore Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.6886
lon: -121.736