Sarmila/GeoWiki-Features huggingface dataset:
It may also be found in Corsica, and in the Balkans. It has specifically found in several Departments of France including, Charente-Maritime, (near Ciré-d'Aunis and Rochefort) Hérault, Vendée, (near Saint-Denis-du-Payré,) Pyrénées-Orientales (near Argelès-sur-Mer,) and Var, (near Hyères.)
Also within Spain, near Madrid, Aragon and Navarra. Habitat.

Geographic entities mentioned:
surface_form: Hyères
instance_of: Mountain
countries: France
coordinates: lat: 43.118888888889
lon: 6.1286111111111
One may either scramble over them directly (including the crossing of Lord Berkley's Seat), or take the bypass path on the southwest side. This path is eroded in some places and should not be regarded as an easy option. The winter traverse of the ridge is probably more demanding than that of Liathach or the Aonach Eagach.

Geographic entities mentioned:
surface_form: Liathach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.564327777778
lon: -5.4621222222222
surface_form: Aonach Eagach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.679497
lon: -5.012554
surface_form: liathach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.564327777778
lon: -5.4621222222222
surface_form: aonach eagach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.679497
lon: -5.012554
An Teallach. An Teallach (Scottish Gaelic for 'the forge' or 'the anvil') is a mountain group in Wester Ross, in the Northwest Highlands of Scotland. It lies west of Dundonnell Forest, north of Loch na Sealga, and south of Little Loch Broom. Its highest peaks are the Munros of Bidean a' Ghlas Thuill at 1062 m (3484 ft), and Sgùrr Fiona at 1058 m (3473 ft).

Geographic entities mentioned:
surface_form: loch broom
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.7
lon: -3.6166666666667
An Teallach. An Teallach (Scottish Gaelic for 'the forge' or 'the anvil') is a mountain group in Wester Ross, in the Northwest Highlands of Scotland. It lies west of Dundonnell Forest, north of Loch na Sealga, and south of Little Loch Broom. Its highest peaks are the Munros of Bidean a' Ghlas Thuill at 1062 m (3484 ft), and Sgùrr Fiona at 1058 m (3473 ft).

Geographic entities mentioned:
surface_form: an teallach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.806530555556
lon: -5.2516611111111
The mountains are mostly made of Torridonian sandstone. Like the peaks around Torridon (for which the rock is named), An Teallach has terraced sides riven with steep gullies and a sharp rocky summit crest at Sgùrr Fiona. The steepest section, known as Corrag Bhuidhe, rises above Loch Toll an Lochain.

Geographic entities mentioned:
surface_form: an teallach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.806530555556
lon: -5.2516611111111
This route, some in length, climbs steeply up the headwall of the corrie of Glas Tholl to reach the main ridge just north of Bidein a' Ghlas Thuill. Both of the above routes, however, miss out the central section, for which An Teallach is best known. A route reaching the summits from the south starts from near Corrie Hallie. It then follows a track (later a path) southwest for about.

Geographic entities mentioned:
surface_form: an teallach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.806530555556
lon: -5.2516611111111
Shyganak (Sarysu District). Geography. The village lies on the lower course of the Chu river. It is located at the northern end of lake Ulken Kamkaly by the eastern shore of lake Kishi Kamkaly, to the northeast of Zhanatas, the district capital.

Geographic entities mentioned:
surface_form: Ulken Kamkaly
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 44.809166666667
lon: 70
Waldstätten () was a canton of the Helvetic Republic from 1798 to 1803, combining the territories of the founding cantons of the Old Swiss Confederacy, Uri (without the Leventina but with the Urseren), Schwyz (without March and Höfe) and both cantons of Unterwalden, which were collectively known as &quot;Waldstätten&quot; (German for &quot;forested settlements&quot;) since the 14th century, along with Zug, the Republic of Gersau, and Engelberg Abbey.

Geographic entities mentioned:
surface_form: Urseren
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.633333333333
lon: 8.5333333333333
In Bolivia, Gismondi's photographic record of the country was extensive; it included one of the first systematic records of the La Paz Department, documenting aspects of the urban city as well as the surrounding Altiplano and tropical Yungas regions.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Fed by the Amargosa River and some neighbouring washes, it eventually culminated to a surface area of around 186,000 years ago and left sediments. Afterwards, the Amargosa River cut a gorge out of the lake and into Death Valley with its Lake Manly, draining the lake. The present-day towns of Shoshone, California and Tecopa, California lie within the basin of the former lake. Hydrology.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
The present-day towns of Shoshone, California and Tecopa, California lie within the basin of the former lake. Hydrology. Lake Tecopa occupied the Tecopa Valley, a pear-shaped valley east of southern Death Valley, in Inyo County, California. The cities of Barstow, California and Las Vegas, Nevada lie close to the lake basin.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
The Amargosa River flowed into Lake Tecopa, which was the river's terminal lake. Most of the water in Lake Tecopa came from the Amargosa River and to a lesser degree from the washes that drain Chicago Valley and Greenwater Valley; the total size of its catchment was about and most of its water originated in Paiute Mesa, Shoshone Mountains, Timber Mountains and Yucca Mountains.

Geographic entities mentioned:
surface_form: Chicago Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.86055556
lon: -116.13333333
surface_form: Yucca Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.9402
lon: -116.485
The catchment of the Amargosa River above Tecopa, California is presently about. Later, after Lake Tecopa had disappeared, the river reached Death Valley and its Lake Manly, dramatically increasing the supply of water to the latter. Presently, the river is largely ephemeral except where it is fed by springs. Geography.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
In 1903 he graduated Dr. med. In the course of his studies he travelled to Crete, Albania and Persia, made numerous excursions to the mountains, skiing on the Zugspitze and in the Bernese Oberland on his own home-made skis. After his final medical exams in 1903, Albert Tafel pursued further courses in geography under Profs.

Geographic entities mentioned:
surface_form: Zugspitze
instance_of: Mountain
countries: Germany
Austria
coordinates: lat: 47.421217
lon: 10.986314
Sammamish River. The Sammamish River (also known as Sammamish Slough) flows through north King County, Washington for about, draining Lake Sammamish into Lake Washington. Along its course, the Sammamish River flows through Redmond, Woodinville, Bothell, and Kenmore. The river is named after the native people who once lived along its entire length. Course.

Geographic entities mentioned:
surface_form: Lake Sammamish
instance_of: Lake
countries: United States
coordinates: lat: 47.61638888888889
lon: -122.08944444444444
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
The river is named after the native people who once lived along its entire length. Course. The Sammamish River begins as an outlet on the north shore of Lake Sammamish, which in turn is fed by several creeks that make up the headwaters of the Sammamish River basin. The most important of these is Issaquah Creek. The river flows north from the lake through the city of Redmond.

Geographic entities mentioned:
surface_form: Lake Sammamish
instance_of: Lake
countries: United States
coordinates: lat: 47.61638888888889
lon: -122.08944444444444
The river continues to bend in a generally westward direction, where it is joined from the north by North Creek in Bothell near the University of Washington, and Swamp Creek in Kenmore. The Sammamish River enters Lake Washington on the west side of Kenmore. The Sammamish River basin covers an area from Everett in the north to May Valley in the south.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Lemon Tree Passage, New South Wales. Lemon Tree Passage is a suburb of the Port Stephens Local Government Area in the Hunter Region of New South Wales, Australia, located at the end of the Tilligerry Peninsula and surrounded by the waters of Port Stephens. At the it had a population of. It is a haven for koalas due to it being densely wooded.

Geographic entities mentioned:
surface_form: Hunter Region
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Differences between the Nepalese settlers and the indigenous population during his reign led to the direct intervention of the British, who were the de facto rulers of the Himalayan nation. The British ruled in favour of the Nepalese much to the discontent of the chogyal, who then retreated to the Chumbi Valley and allied himself with the Tibetans.

Geographic entities mentioned:
surface_form: Chumbi Valley
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 27.4893046
lon: 88.9050579
Regional. The Altiplano is a basin of Cretaceous-Cenozoic age in Peru and Bolivia and embedded between the Western Cordillera, a Mesozoic-Cenozoic volcanic arc and the Eastern Cordillera which is a Paleozoic fold belt. The development of the Altiplano started during the Neocomian and continued during the Tertiary, with several tectonic episodes resulting in the folding of the rocks.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
He was a professor emeritus of UCLA's Neuropsychiatric Institute. Family life and education. Edward Ross Ritvo, son of Max Ritvo and Frances (née Davis) Ritvo, was born in Boston on June 1, 1930. As a young man he enjoyed rowing, skied on Harvard's ski team, and once climbed Mount Blanc. He earned a B.A. in Social Anthropology at Harvard University in 1951, an M.D.

Geographic entities mentioned:
surface_form: Mount Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
Rattlesnake Mountain is traversed by the Metacomet Trail. Geography. Roughly in diameter, Rattlesnake Mountain rises steeply above the Farmington River valley to the west. The mountain consists of an upper summit cone that descends into a series of tiered ridges which become contiguous with the Metacomet Ridge on Pinnacle Rock to the south and Farmington Mountain to the north.

Geographic entities mentioned:
surface_form: Farmington Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.713433333333
lon: -72.815652777778
surface_form: pinnacle rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.6897
lon: -72.8328
surface_form: farmington mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.713433333333
lon: -72.815652777778
Recreation and conservation. Rattlesnake Mountain is traversed by the Metacomet Trail, (maintained by the Connecticut Forest and Park Association), which extends from the Hanging Hills of Meriden, Connecticut, to the Massachusetts border. Rattlesnake Mountain offers a number of clifftop views west over the Pequabuck River valley toward the eastern escarpment of the Berkshire Mountains.

Geographic entities mentioned:
surface_form: Hanging Hills
instance_of: Mountain
countries: United States
coordinates: lat: 41.56
lon: -72.82
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.458333333333
lon: -121.80611111111
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.25243
lon: -115.60644
surface_form: hanging hills
instance_of: Mountain
countries: United States
coordinates: lat: 41.56
lon: -72.82
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1322
lon: -74.8634
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6997
lon: -72.8328
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.4056
lon: -119.611
Rattlesnake Mountain (Connecticut). Rattlesnake Mountain is a traprock mountain, above sea level, located southwest of Hartford, Connecticut, in the town of Farmington. It is part of the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border.

Geographic entities mentioned:
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.458333333333
lon: -121.80611111111
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.25243
lon: -115.60644
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1322
lon: -74.8634
surface_form: rattlesnake mountain (connecticut)
instance_of: Mountain
countries: United States
coordinates: lat: 41.6997
lon: -72.8328
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.4056
lon: -119.611
Rattlesnake Mountain (Connecticut). Rattlesnake Mountain is a traprock mountain, above sea level, located southwest of Hartford, Connecticut, in the town of Farmington. It is part of the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border.

Geographic entities mentioned:
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.458333333333
lon: -121.80611111111
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.25243
lon: -115.60644
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1322
lon: -74.8634
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6997
lon: -72.8328
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.4056
lon: -119.611
It is part of the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border. Rattlesnake Mountain, a popular outdoor recreation resource of the metropolitan Hartford area, is known for its cliff-top scenic vistas, unique microclimate ecosystems, and rare plant communities.

Geographic entities mentioned:
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.458333333333
lon: -121.80611111111
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.25243
lon: -115.60644
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1322
lon: -74.8634
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6997
lon: -72.8328
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.4056
lon: -119.611
Rattlesnake Mountain is traversed by the Metacomet Trail. Geography. Roughly in diameter, Rattlesnake Mountain rises steeply above the Farmington River valley to the west. The mountain consists of an upper summit cone that descends into a series of tiered ridges which become contiguous with the Metacomet Ridge on Pinnacle Rock to the south and Farmington Mountain to the north.

Geographic entities mentioned:
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.458333333333
lon: -121.80611111111
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.25243
lon: -115.60644
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1322
lon: -74.8634
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6997
lon: -72.8328
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.4056
lon: -119.611
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
Three broadcasting towers (WTIC-TV, WHPX-TV and WVIT-TV) stand on the summit. The east side of Rattlesnake Mountain drains into Trout Brook, then to the Park River, thence into the Connecticut River and Long Island Sound; the west side into the Pequabuck River, then to the Farmington River, thence to the Connecticut River.

Geographic entities mentioned:
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.458333333333
lon: -121.80611111111
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.25243
lon: -115.60644
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1322
lon: -74.8634
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6997
lon: -72.8328
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.4056
lon: -119.611
The mountain formed near the end of the Triassic Period with the rifting apart of the North American continent from Africa and Eurasia. Lava welled up from the rift and solidified into sheets of strata hundreds of feet thick. Subsequent faulting and earthquake activity tilted the strata, creating the cliffs and ridgeline of Rattlesnake Mountain.

Geographic entities mentioned:
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.458333333333
lon: -121.80611111111
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.25243
lon: -115.60644
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1322
lon: -74.8634
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6997
lon: -72.8328
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.4056
lon: -119.611
Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Connecticut. Rattlesnake Mountain is also an important raptor migration path. (See Metacomet Ridge for more information on the geology and ecosystem of Rattlesnake Mountain). Folklore.

Geographic entities mentioned:
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.458333333333
lon: -121.80611111111
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.25243
lon: -115.60644
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1322
lon: -74.8634
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6997
lon: -72.8328
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.4056
lon: -119.611
Suburban Farmington is visible below. The mountain is open to hiking, bird watching, picnicking, snowshoeing, and other passive pursuits. A number of rock climbing websites indicate several climbing routes on the mountain. The ecosystem of Rattlesnake Mountain is most threatened by development and quarrying.

Geographic entities mentioned:
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.458333333333
lon: -121.80611111111
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.25243
lon: -115.60644
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1322
lon: -74.8634
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6997
lon: -72.8328
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.4056
lon: -119.611
The Farmington Land Trust is active in the conservation of Rattlesnake Mountain and its viewshed. Will Warren's Den (part of the William S. Wadsworth Memorial property) is among the many easements managed by the trust.

Geographic entities mentioned:
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.458333333333
lon: -121.80611111111
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.25243
lon: -115.60644
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1322
lon: -74.8634
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6997
lon: -72.8328
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.4056
lon: -119.611
Rattlesnake Mountain (Connecticut). Rattlesnake Mountain is a traprock mountain, above sea level, located southwest of Hartford, Connecticut, in the town of Farmington. It is part of the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border.

Geographic entities mentioned:
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
The east side of Rattlesnake Mountain drains into Trout Brook, then to the Park River, thence into the Connecticut River and Long Island Sound; the west side into the Pequabuck River, then to the Farmington River, thence to the Connecticut River. The south side of the mountain supports the headwaters of the Quinnipiac River, which flows directly into Long Island Sound. Geology and ecology.

Geographic entities mentioned:
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
Rattlesnake Mountain is traversed by the Metacomet Trail, (maintained by the Connecticut Forest and Park Association), which extends from the Hanging Hills of Meriden, Connecticut, to the Massachusetts border. Rattlesnake Mountain offers a number of clifftop views west over the Pequabuck River valley toward the eastern escarpment of the Berkshire Mountains. Suburban Farmington is visible below.

Geographic entities mentioned:
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
Geography. Cnoc na Péiste is the highest point in the &quot;Eastern Reeks&quot; section of the MacGillycuddy's Reeks range, which consists of a long narrow ridge that takes in several summits before ending at Cruach Mhór and descending into the Gap of Dunloe, to the &quot;Head of the Gap&quot;, only to rise up again towards the Purple Mountain Group.

Geographic entities mentioned:
surface_form: Cruach Mhór
instance_of: Mountain
countries: Ireland
coordinates: lat: 51.9858
lon: -9.6615
surface_form: purple mountain
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.007916666667
lon: -9.6224805555556
surface_form: cruach mhór
instance_of: Mountain
countries: Ireland
coordinates: lat: 51.9858
lon: -9.6615
surface_form: cnoc na péiste
instance_of: Mountain
countries: Ireland
coordinates: lat: 51.998152777778
lon: -9.6955166666667
To the southwest of Cnoc na Péiste is the peak of Maolán Buí () and a generally flat grassy ridge to the col at the &quot;Devil's Ladder&quot;. To the northeast is the narrow sharp rocky arête that joins with The Big Gun (), and Cruach Mhór (), which marks the end of the eastern ridge of the Reeks.

Geographic entities mentioned:
surface_form: Maolán Buí
instance_of: Mountain
countries: Ireland
coordinates: lat: 51.9946
lon: -9.7011
surface_form: devil's ladder
instance_of: Mountain
countries: Ireland
coordinates: lat: 51.989444444444
lon: -9.7316666666667
surface_form: maolán buí
instance_of: Mountain
countries: Ireland
coordinates: lat: 51.9946
lon: -9.7011
To the southwest of Cnoc na Péiste is the peak of Maolán Buí () and a generally flat grassy ridge to the col at the &quot;Devil's Ladder&quot;. To the northeast is the narrow sharp rocky arête that joins with The Big Gun (), and Cruach Mhór (), which marks the end of the eastern ridge of the Reeks.

Geographic entities mentioned:
surface_form: The Big Gun
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.0009
lon: -9.6888
surface_form: Cruach Mhór
instance_of: Mountain
countries: Ireland
coordinates: lat: 51.9858
lon: -9.6615
surface_form: cruach mhór
instance_of: Mountain
countries: Ireland
coordinates: lat: 51.9858
lon: -9.6615
surface_form: big gun
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.0009
lon: -9.6888
surface_form: big gun
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.0009
lon: -9.6888
surface_form: the big gun
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.0009
lon: -9.6888
surface_form: the big gun
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.0009
lon: -9.6888
&quot;sufficient separation&quot;), but which is outside of (or &quot;furth&quot;) Scotland; which is why Knocknapeasta is sometimes referred to as one of the 13 Irish Munros. Cnoc na Péiste's prominence qualifies it to meet the British Isles Marilyn classification, being the only other 3,000 foot Reek alongside Carrauntoohil to meet the 150 metre Marilyn prominence threshold.

Geographic entities mentioned:
surface_form: Carrauntoohil
instance_of: Mountain
countries: Ireland
coordinates: lat: 51.998888888889
lon: -9.7427777777778
surface_form: carrauntoohil
instance_of: Mountain
countries: Ireland
coordinates: lat: 51.998888888889
lon: -9.7427777777778
surface_form: cnoc na péiste
instance_of: Mountain
countries: Ireland
coordinates: lat: 51.998152777778
lon: -9.6955166666667
surface_form: cnoc na péiste
instance_of: Mountain
countries: Ireland
coordinates: lat: 51.998152777778
lon: -9.6955166666667
Cnoc na Péiste. Cnoc na Péiste (Irish for &quot;hill of the serpent&quot;), anglicised Knocknapeasta, at, is the fourth-highest peak in Ireland, on the Arderin and Vandeleur-Lynam lists. Cnoc na Péiste is part of the MacGillycuddy's Reeks range in County Kerry.

Geographic entities mentioned:
surface_form: arderin
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.03805556
lon: -7.65388889
surface_form: cnoc na péiste
instance_of: Mountain
countries: Ireland
coordinates: lat: 51.998152777778
lon: -9.6955166666667
surface_form: cnoc na péiste
instance_of: Mountain
countries: Ireland
coordinates: lat: 51.998152777778
lon: -9.6955166666667
surface_form: knocknapeasta
instance_of: Mountain
countries: Ireland
coordinates: lat: 51.998152777778
lon: -9.6955166666667
Cnoc na Péiste. Cnoc na Péiste (Irish for &quot;hill of the serpent&quot;), anglicised Knocknapeasta, at, is the fourth-highest peak in Ireland, on the Arderin and Vandeleur-Lynam lists. Cnoc na Péiste is part of the MacGillycuddy's Reeks range in County Kerry.

Geographic entities mentioned:
surface_form: cnoc na péiste
instance_of: Mountain
countries: Ireland
coordinates: lat: 51.998152777778
lon: -9.6955166666667
Aircraft crash. At about 7 am on 17 December 1943, during World War II, a United States Army Air Forces (USAAF) plane crashed into the northerly face of Cnoc na Péiste. The plane was a &quot;Douglas C-47&quot; or &quot;Dakota&quot; (serial number 43-30719) with five crewmen aboard. It struck the mountain just above Lough Cummeenapeasta at an altitude of about 2,000 ft—killing all five passengers.

Geographic entities mentioned:
surface_form: cnoc na péiste
instance_of: Mountain
countries: Ireland
coordinates: lat: 51.998152777778
lon: -9.6955166666667
On the other side of the ridge, a stream flows southwards from Lough Googh into the Derrycarna River. Because of its positioning, Cnoc na Péiste is usually climbed as part of a &quot;horseshoe&quot; of the eastern section of the Reeks, starting from the &quot;Hag's Glen&quot;, and taking in Maolan Bui and The Big Gun, or as part of the even longer &quot;MacGillycuddy's Reeks Ridge Walk&quot;.

Geographic entities mentioned:
surface_form: maolan bui
instance_of: Mountain
countries: Ireland
coordinates: lat: 51.9946
lon: -9.7011
surface_form: big gun
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.0009
lon: -9.6888
surface_form: the big gun
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.0009
lon: -9.6888
The CDP is bordered to the south by the village of Brockport and the town of Sweden. Route 19 (Lake Road) leads north to Hamlin and to its terminus at Lake Ontario, while to the south it leads through Brockport and continues to Bergen, away. Route 104 (Ridge Road) leads east to the northern part of Rochester and west to Lewiston at the Niagara River.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
State Route 260 (Sweden-Walker Road) forms the eastern border of the Clarkson CDP and leads north to Lake Ontario and south to Route 31 in Sweden. According to the U.S. Census Bureau, the Clarkson CDP has an area of, all land. The area is drained to the north by Brockport Creek, part of the Salmon Creek watershed flowing to Lake Ontario.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Ivory Island. Ivory Island Lightstation is located 14 miles northwest of Bella Bella on the junction of Seaforth Channel and Milbanke Sound on the Inside Passage of British Columbia.

Geographic entities mentioned:
surface_form: Seaforth Channel
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.24672
lon: -128.29954
Don Victoriano. Don Victoriano, officially the Municipality of Don Victoriano, unofficially as Don Victoriano Chiongbian (;), is a municipality in the province of Misamis Occidental, Philippines. According to the 2024 census, it has a population of 10,214 people. The municipality is home to the Mount Malindang National Park. History.

Geographic entities mentioned:
surface_form: Mount Malindang
instance_of: Mountain
countries: Philippines
coordinates: lat: 8.2175
lon: 123.63666666667
Parts of seven municipalities in the province had been detached to be constituted into a new, distinct municipality. Those separated were barangays in Tudela (3) including Tuno which was designated the seat of government, Jimenez (also 3), Bonifacio (2), Clarin and Sinacaban (one in each); as well as sitios in a barangay each in Panaon and Aloran, situated on the side of the Mount Malindang Range.

Geographic entities mentioned:
surface_form: Mount Malindang
instance_of: Mountain
countries: Philippines
coordinates: lat: 8.2175
lon: 123.63666666667
The River Forth runs along its southern boundary, and the River Teith runs east-south-eastward through the centre. A flat tract of considerable breadth lies along the Forth Valley, flanked on each side by a hill-ridge. The valley is traversed by the Teith, and an upland tract, part of the Braes of Doune, ascends to the summit of Uamh Mhòr on the northern boundary.

Geographic entities mentioned:
surface_form: Uamh Mhòr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.2763
lon: -4.11876
The chosen subject was from the history of the Cornelii, specifically the arrival of the goddess Cybele's image in Rome during the Second Punic War, as told in Ovid, Appian and Livy. Scipio Africanus had consulted the Sibylline Books and ordered that the image be brought from Mount Ida.

Geographic entities mentioned:
surface_form: Mount Ida
instance_of: Mountain
countries: Turkey
Tiltill Valley. Tiltill Valley is a remote valley in northerwestern Yosemite National Park. It is accessible only to hikers and equestrians. The valley is most easily reached via trail heads in the vicinity of the Hetch Hetchy Valley and Lake Eleanor.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: tiltill valley
instance_of: Valley
countries: United States
coordinates: lat: 37.9748364
lon: -119.6983194
It is accessible only to hikers and equestrians. The valley is most easily reached via trail heads in the vicinity of the Hetch Hetchy Valley and Lake Eleanor. The valley provides access to many remote alpine lakes throughout the largely untamed wilderness that defines the northern portion of Yosemite National Park and the adjacent Emigrant Wilderness.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
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
It is accessible only to hikers and equestrians. The valley is most easily reached via trail heads in the vicinity of the Hetch Hetchy Valley and Lake Eleanor. The valley provides access to many remote alpine lakes throughout the largely untamed wilderness that defines the northern portion of Yosemite National Park and the adjacent Emigrant Wilderness.

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
surface_form: hetch hetchy valley
instance_of: Valley
countries: United States
coordinates: lat: 37.9475
lon: -119.78694444
Tiltill Valley. Tiltill Valley is a remote valley in northerwestern Yosemite National Park. It is accessible only to hikers and equestrians. The valley is most easily reached via trail heads in the vicinity of the Hetch Hetchy Valley and Lake Eleanor.

Geographic entities mentioned:
surface_form: tiltill valley
instance_of: Valley
countries: United States
coordinates: lat: 37.9748364
lon: -119.6983194
Geology and history. Geologically Zion Canyon is part of the Navajo sandstone Colorado Plateau, which contained many joints and cracks when first uplifted, one of which was cut by the North Fork of the Virgin River to become Zion Canyon. The river was the largest force in cutting the canyon, mostly by flash floods, as the average flow of the river is very light.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
Tossal de la Baltasana. Tossal de la Baltasana is a mountain of Catalonia, Spain. It has an elevation of 1,203 metres above sea level.

Geographic entities mentioned:
surface_form: tossal de la baltasana
instance_of: Mountain
countries: Spain
coordinates: lat: 41.3260040526
lon: 1.00419364629
Course. The Chu is formed by the confluence of the rivers Joon Aryk and Kochkor, in the Kochkor District of the Naryn Region. After approaching within a few kilometres of Lake Issyk-Kul (near Balykchy), without either flowing into the lake or draining it, it turns towards the northwest. In the 1950s an old riverbed called Ketmaldy (also Buugan) linked the Chu River and Issyk Kul.

Geographic entities mentioned:
surface_form: Issyk-Kul
instance_of: Lake
countries: Kyrgyzstan
coordinates: lat: 42.416666666667
lon: 77.25
During floods part of Chu water would reach the lake, but such outflow has not been seen since the construction of the Orto-Tokoy Reservoir. After passing through the narrow Boom Gorge (, &quot;Boomskoye ushchelye&quot;), the river enters the comparatively flat Chüy Valley, within which lie the Kyrgyz capital Bishkek and the Kazakh city of Shu.

Geographic entities mentioned:
surface_form: Chüy Valley
instance_of: Valley
countries: Kyrgyzstan
Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 42.8333
lon: 75.2833
As the Chu flows through the Chüy Valley, it forms the border between Kyrgyzstan and Kazakhstan for more than a hundred kilometres, but then it leaves Kyrgyzstan and flows into Kazakhstan, where it flows at the northern edge of the Moiynkum Desert, with lake Kokuydynkol close to its channel.

Geographic entities mentioned:
surface_form: Kokuydynkol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 44.583333333333
lon: 72
In wet years it may reach the endorheic salt lake Akzhaykyn, located among the vast solonchaks of the Ashchykol Depression. History. The area of this river was originally home to the Iranian Sughds who spoke Soghdian, an Eastern Iranian language. During the Middle Ages, the area was strategically important.

Geographic entities mentioned:
surface_form: Akzhaykyn
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 44.907222222222
lon: 67.781944444444
Grand Canyon (Crimea). The Grand Canyon of Crimea (;) is a canyon located in southern Crimea, an area internationally recognised as part of Ukraine but currently controlled by Russia. The Grand Canyon separates the Ai-Petri and massifs, and the area of the Grand Canyon zakaznik (nature reserve) is. It has a depth of, and its bottom are several springs. Description.

Geographic entities mentioned:
surface_form: Ai-Petri
instance_of: Mountain
countries: Ukraine
Russia
Russian Empire
Soviet Union
coordinates: lat: 44.451111111111
lon: 34.052777777778
It is approximately long, and its walls, made of limestone, reach high. At the bottom of the canyon, widths reach as thin as. The canyon is located between the Ai-Petri and massifs. The walls of the canyon are home to a variety of different types of trees and herbs, but are prone to rock slides during dry weather and after rain.

Geographic entities mentioned:
surface_form: Ai-Petri
instance_of: Mountain
countries: Ukraine
Russia
Russian Empire
Soviet Union
coordinates: lat: 44.451111111111
lon: 34.052777777778
Bear Island (Lake Winnipesaukee). Bear Island is the second largest of the 264 islands in Lake Winnipesaukee in New Hampshire, United States. In the summer it is accessible only by boat because it is not connected to the mainland via a bridge. In the winter it can be reached by crossing the frozen lake, including by snowmobile.

Geographic entities mentioned:
surface_form: Lake Winnipesaukee
instance_of: Lake
countries: United States
coordinates: lat: 43.598888888889
lon: -71.323055555556
Clapton in Gordano. Clapton in Gordano is a village and civil parish in Somerset, England. It is situated within the unitary authority of North Somerset on the southern side of the Gordano Valley, immediately adjacent to the M5 motorway. The parish has a population of 348. There is a village football club, Clapton in Gordano FC.

Geographic entities mentioned:
surface_form: Gordano Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.45315
lon: -2.8145111111111
It originally extended from the modern city of Dunedin, New Zealand, to Aramoana, about 25 km away. Extensive erosion has occurred over the last 10 million years, and Otago Harbour now fills the oldest parts of the volcano. The remnants of the volcano form the hills around Otago Harbour (including Mount Cargill, Flagstaff, Saddle Hill, Signal Hill, and Otago Peninsula). Geology.

Geographic entities mentioned:
surface_form: Mount Cargill
instance_of: Mountain
countries: New Zealand
coordinates: lat: -45.813
lon: 170.555
The total volume of eruptives has been estimated to be, but there was a much larger intrusive component at. The final phase of eruptions are preserved as phonolite domes around Mount Cargill. Traces of the old Dunedin Volcano are best seen in the Dunedin Botanic Garden's geology walk, the cliffs at Aramoana, and the geomorphology of Mount Cargill, which has preserved lava domes.

Geographic entities mentioned:
surface_form: Mount Cargill
instance_of: Mountain
countries: New Zealand
coordinates: lat: -45.813
lon: 170.555
They spread from Voronezh and Tambov to Southern Russia and the Volga region in the 19th century. Tsarist settlements. In 1802 Tsar Alexander I ordered the resettlement of Russian sectarians to the Caucasus; regions like Lori, Lake Sevan, Dilijan, and Zangezur were chosen for their similar climate to Russia.

Geographic entities mentioned:
surface_form: Lake Sevan
instance_of: Lake
countries: Armenia
coordinates: lat: 40.310555555556
lon: 45.349166666667
Mosier Mounds Complex. The Mosier Mounds Complex (Smithsonian trinomial: 35WS274), also known locally as the Mosier Battlements, is an archaeological site near Mosier, Oregon, United States. This collection of stone walls, pits, and mounds amid a basalt talus slope is the largest and most complex of a number of similar Native American sites in the southern Columbia Plateau.

Geographic entities mentioned:
surface_form: Columbia Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 45.999444444444
lon: -119.00138888889
Examples of Burns' work is in the permanent collection of the National Galleries of Scotland. Later life. In 1947 Burns moved to Cowdenknowes farm and ran a riding school with her younger brother Charles. In 1958 she became joint Master of the Lauderdale Hunt alongside Mrs. J.L. Hogarth and retained this position for two years.

Geographic entities mentioned:
surface_form: Lauderdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.73
lon: -2.74889
The first people to settle were farmers; remains of their presence have been found in the area dating back to the Stone Age, mostly in the area around Gammalstorp, Siretorp and Istaby. The hill in the east, marking the border towards Karlshamn called Ryssberget, was a direct creation of the glacial movements.

Geographic entities mentioned:
surface_form: Ryssberget
instance_of: Mountain
countries: Sweden
coordinates: lat: 56.133333333333
lon: 14.575
On the western side of the hill, the different times of ice withdrawal are clearly noticeable. The old, now drained lake of Vesan was also a product of the ice age. The port town of Sölvesborg was founded in the 12th century, between the mountain Ryssberget and the bay to the east (Sölvesborgsviken), but the city itself has grown up around the church, the monastery and later on the castle.

Geographic entities mentioned:
surface_form: Vesan
instance_of: Lake
countries: Sweden
coordinates: lat: 56.105
lon: 14.640555555556
Even after a near total fire in 1801, when the entire city except the church burnt down, it was decided to retain it instead of adapting a grid pattern. Sights. Apart from the aforementioned Ryssberget, the countryside villages outside of Sölvesborg are very scenic. In July, the village of Krokås hosts the day of eel fishing (&quot;Ålafiskets dag&quot;).

Geographic entities mentioned:
surface_form: Ryssberget
instance_of: Mountain
countries: Sweden
coordinates: lat: 56.133333333333
lon: 14.575
During the summer period, a visit to one of the many beaches is well worth. Notable beaches are Sandviken, Tredenborg and Hällevik. Sölvesborg is the start of the Skåneleden's SL1 trail and its oldest section. The trail leads hikers from the town center up onto Ryssberget, where they can experience the tranquility of old-growth beech forests and panoramic views of Listerlandet.

Geographic entities mentioned:
surface_form: Ryssberget
instance_of: Mountain
countries: Sweden
coordinates: lat: 56.133333333333
lon: 14.575
The developers plan to soon publish a detailed environmental impact assessment. They aim to start construction in 2026, and hope to deliver first power to the national grid in 2030. Proposals. The scheme will use Loch Ness as the lower reservoir, and &quot;Loch nam Breac Dearga&quot; as the upper. Economics. The scheme will cost in the order of £3 billion.

Geographic entities mentioned:
surface_form: Loch Ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
From the Middle Paleolithic period, which coincides with the emergence of Neanderthals in Iran, also remains of interesting tools made of pyrite or remains of animal fossil fountains, found in caves in Zagros Mountains and central Iranian Plateau like the caves of Bisotun and Khorramabad which are put on display in the museum.

Geographic entities mentioned:
surface_form: Iranian Plateau
instance_of: Plateau
countries: Iran
coordinates: lat: 36.283333
lon: 59.05
The town of Machias straddles the border of the Mississippi River drainage basin, with the waters of Lime Lake flowing north and then west via Cattaraugus Creek to Lake Erie and eventually the Saint Lawrence Seaway to the Atlantic Ocean, while the waters of Ischua Creek, less than south of Lime Lake, flow south towards the Allegheny River and eventually the Mississippi and Gulf of Mexico.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Sabitawasis Beach 89 C-1. Sabitawasis Beach 89 C-1 is an Indian reserve of the Fishing Lake First Nation in Saskatchewan. It is on the northern shore of Fishing Lake.

Geographic entities mentioned:
surface_form: Fishing Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.8466
lon: -103.532
Mount William (Antarctica). Mount William is a prominent snowy mountain in Antarctica, standing tall, and located north-northeast of Cape Lancaster which is the south extremity of Anvers Island, in the Palmer Archipelago. This is the tallest mountain visible from Biscoe Bay, near the south end of the island's Osterrieth Range which also includes Mount Français (the tallest mountain on the island).

Geographic entities mentioned:
surface_form: Mount Français
instance_of: Mountain
coordinates: lat: -64.633333333333
lon: -63.45
surface_form: biscoe
instance_of: Mountain
coordinates: lat: -66.21667
lon: 51.36667
He named it for William IV, then King of the United Kingdom. Mountain climbers from the U.K. were the first to ascend this peak, in 1956. In 2003, after climbing this mountain, two Americans skied down. A rock ridge leading northwest from Mount William leads to Shewry Peak.

Geographic entities mentioned:
surface_form: Shewry Peak
instance_of: Mountain
coordinates: lat: -64.75
lon: -63.633333333333
surface_form: mount william
instance_of: Mountain
coordinates: lat: -64.7833
lon: -63.6833
surface_form: william
instance_of: Mountain
coordinates: lat: -64.7833
lon: -63.6833