Sarmila/GeoWiki-Features huggingface dataset:
Due to the high elevation, most of the precipitation that falls on the mountain is snow. The view from Mount Rose facing east is the Truckee Meadows, the second largest population center in Nevada. According to one tradition, the peak was named after Jacob S, Rose, an early settler, while another tradition states the mountain has the name of Rose Hickman, an early explorer.

Geographic entities mentioned:
surface_form: mount rose
instance_of: Mountain
countries: United States
coordinates: lat: 47.50537
lon: -123.28933
surface_form: mount rose
instance_of: Mountain
countries: United States
coordinates: lat: 40.3605
lon: -74.7475
surface_form: mount rose
instance_of: Mountain
countries: United States
coordinates: lat: 39.3438
lon: -119.918
According to one tradition, the peak was named after Jacob S, Rose, an early settler, while another tradition states the mountain has the name of Rose Hickman, an early explorer. Mount Rose Ski Tahoe is nearby, but is not on Mount Rose. Despite the name, the resort is actually on the slopes of Slide Mountain, which is on the other side of Nevada State Route 431.

Geographic entities mentioned:
surface_form: mount rose
instance_of: Mountain
countries: United States
coordinates: lat: 47.50537
lon: -123.28933
surface_form: mount rose
instance_of: Mountain
countries: United States
coordinates: lat: 47.50537
lon: -123.28933
surface_form: mount rose
instance_of: Mountain
countries: United States
coordinates: lat: 40.3605
lon: -74.7475
surface_form: mount rose
instance_of: Mountain
countries: United States
coordinates: lat: 40.3605
lon: -74.7475
surface_form: mount rose
instance_of: Mountain
countries: United States
coordinates: lat: 39.3438
lon: -119.918
surface_form: mount rose
instance_of: Mountain
countries: United States
coordinates: lat: 39.3438
lon: -119.918
The east slope of Slide Mountain, is the East Bowl of Mt. Rose. In 1964, the north side of Slide Mountain was named Mount Rose Ski Area and Reno Ski Bowl was renamed Slide Mountain Ski Area. In 1987, the two ski areas merged and began operation as one resort named Mt. Rose. Dr.

Geographic entities mentioned:
surface_form: mount rose
instance_of: Mountain
countries: United States
coordinates: lat: 47.50537
lon: -123.28933
surface_form: mount rose
instance_of: Mountain
countries: United States
coordinates: lat: 40.3605
lon: -74.7475
surface_form: mount rose
instance_of: Mountain
countries: United States
coordinates: lat: 39.3438
lon: -119.918
surface_form: slide mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9986
lon: -74.3864
surface_form: slide mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9986
lon: -74.3864
surface_form: slide mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.3127
lon: -119.884
surface_form: slide mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.3127
lon: -119.884
In 1987, the two ski areas merged and began operation as one resort named Mt. Rose. Dr. James Edward Church of the University of Nevada established the Mount Rose Weather Observatory, one of America's first high-altitude meteorological observatories, on June 29, 1905. Climate.

Geographic entities mentioned:
surface_form: mount rose
instance_of: Mountain
countries: United States
coordinates: lat: 47.50537
lon: -123.28933
surface_form: mount rose
instance_of: Mountain
countries: United States
coordinates: lat: 40.3605
lon: -74.7475
surface_form: mount rose
instance_of: Mountain
countries: United States
coordinates: lat: 39.3438
lon: -119.918
Climate. Being a three-thousander and a mountain at a considerably high latitude, Mount Rose has (köppen: dsc) subarctic climate with long snowy winters and short, dry tepid summers. On average, the summit experiences four months with tepid temperatures (that being its summer from June–September) while the remainder of the year remains cold and chilly with frequent subzero temperatures.

Geographic entities mentioned:
surface_form: mount rose
instance_of: Mountain
countries: United States
coordinates: lat: 47.50537
lon: -123.28933
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount rose
instance_of: Mountain
countries: United States
coordinates: lat: 40.3605
lon: -74.7475
surface_form: mount rose
instance_of: Mountain
countries: United States
coordinates: lat: 39.3438
lon: -119.918
On average, the summit experiences four months with tepid temperatures (that being its summer from June–September) while the remainder of the year remains cold and chilly with frequent subzero temperatures. In contrast to the rest of Nevada, Mount Rose is plentiful in precipitation, and thus stands out from the state's predominantly hot semi-arid/desert climate.

Geographic entities mentioned:
surface_form: mount rose
instance_of: Mountain
countries: United States
coordinates: lat: 47.50537
lon: -123.28933
surface_form: mount rose
instance_of: Mountain
countries: United States
coordinates: lat: 40.3605
lon: -74.7475
surface_form: mount rose
instance_of: Mountain
countries: United States
coordinates: lat: 39.3438
lon: -119.918
Mount Rose Ski Tahoe is nearby, but is not on Mount Rose. Despite the name, the resort is actually on the slopes of Slide Mountain, which is on the other side of Nevada State Route 431. The east slope of Slide Mountain, is the East Bowl of Mt. Rose. In 1964, the north side of Slide Mountain was named Mount Rose Ski Area and Reno Ski Bowl was renamed Slide Mountain Ski Area.

Geographic entities mentioned:
surface_form: mt. rose
instance_of: Mountain
countries: United States
coordinates: lat: 47.50537
lon: -123.28933
surface_form: mt. rose
instance_of: Mountain
countries: United States
coordinates: lat: 40.3605
lon: -74.7475
surface_form: slide mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9986
lon: -74.3864
surface_form: slide mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.3127
lon: -119.884
The east slope of Slide Mountain, is the East Bowl of Mt. Rose. In 1964, the north side of Slide Mountain was named Mount Rose Ski Area and Reno Ski Bowl was renamed Slide Mountain Ski Area. In 1987, the two ski areas merged and began operation as one resort named Mt. Rose. Dr.

Geographic entities mentioned:
surface_form: mt. rose
instance_of: Mountain
countries: United States
coordinates: lat: 47.50537
lon: -123.28933
surface_form: mt. rose
instance_of: Mountain
countries: United States
coordinates: lat: 40.3605
lon: -74.7475
Mount Rose Ski Tahoe is nearby, but is not on Mount Rose. Despite the name, the resort is actually on the slopes of Slide Mountain, which is on the other side of Nevada State Route 431. The east slope of Slide Mountain, is the East Bowl of Mt. Rose. In 1964, the north side of Slide Mountain was named Mount Rose Ski Area and Reno Ski Bowl was renamed Slide Mountain Ski Area.

Geographic entities mentioned:
surface_form: slide mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9986
lon: -74.3864
surface_form: slide mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.3127
lon: -119.884
The SeeBird Camera (or Gull Cam) is also available online during the summer months, although it is controlled by the visitors at the museum and not the online visitors. The museum also hosts a number of interactive activities, from fish-feeding on Tuesdays and Fridays to tours of the harbor on the Homer Spit on Fridays and Saturdays during the summer months.

Geographic entities mentioned:
surface_form: Homer Spit
instance_of: Landform
countries: United States
coordinates: lat: 59.62
lon: -151.455
It was in Città di Castello, in 1798, that happened the famous episode of the discussed donation of Raphael's painting &quot;The Marriage of the Virgin&quot; to Giuseppe Lechi by the City Council. In the spring of 1799 Giuseppe Lechi with his unit was engaged in a military campaign in Valtellina attempting to curb an anti-French revolt.

Geographic entities mentioned:
surface_form: Valtellina
instance_of: Valley
countries: Italy
coordinates: lat: 46.166666666667
lon: 9.8666666666667
Numerous birds and several amphibians and mammals are also found in the area. Geography and geology. Central Mountain has an official elevation of, making it the second-highest mountain in Columbia County, after Red Rock Mountain. It is the northernmost mountain in Columbia County. The mountain is on the Allegheny Front.

Geographic entities mentioned:
surface_form: Red Rock Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.308630555556
lon: -76.309352777778
surface_form: central mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.3
lon: -76.3463
surface_form: rock mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.799444444444
lon: -120.97444444444
Central Mountain. Central Mountain is a mountain in Columbia County, Sullivan County, and Luzerne County, in Pennsylvania, United States. Its elevation is above sea level. The mountain is part of the Allegheny Front. Rock formations on the mountain include the Pocono Formation and the Duncannon Member of the Catskill Formation.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: central mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.3
lon: -76.3463
Its elevation is above sea level. The mountain is part of the Allegheny Front. Rock formations on the mountain include the Pocono Formation and the Duncannon Member of the Catskill Formation. It was historically known as North Mountain, but it was renamed Central Mountain (after the village of Central) in the late 1800s.

Geographic entities mentioned:
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.4206
lon: -78.0889
surface_form: central mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.3
lon: -76.3463
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.2175
lon: -74.0492
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.31944444
lon: -76.55388889
The soils on Central Mountain are deep-muck soils that are saturated with water. History and etymology. Central Mountain was historically known as North Mountain due to the fact that it is the northernmost mountain in Columbia County. Between 1860 and 1900, it came to be known as Central Mountain, after the village of Central.

Geographic entities mentioned:
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.4206
lon: -78.0889
surface_form: central mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.3
lon: -76.3463
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.2175
lon: -74.0492
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.31944444
lon: -76.55388889
Central Mountain. Central Mountain is a mountain in Columbia County, Sullivan County, and Luzerne County, in Pennsylvania, United States. Its elevation is above sea level. The mountain is part of the Allegheny Front. Rock formations on the mountain include the Pocono Formation and the Duncannon Member of the Catskill Formation.

Geographic entities mentioned:
surface_form: central mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.3
lon: -76.3463
It is the northernmost mountain in Columbia County. The mountain is on the Allegheny Front. A creek known as East Branch Fishing Creek flows along the base of Central Mountain. Morainic topography consisting of knobs and kettles occurs on the lowest of the side of the mountain. Central Mountain's official coordinates are in the United States Geological Survey quadrangle of Red Rock.

Geographic entities mentioned:
surface_form: central mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.3
lon: -76.3463
Morainic topography consisting of knobs and kettles occurs on the lowest of the side of the mountain. Central Mountain's official coordinates are in the United States Geological Survey quadrangle of Red Rock. The mountain is located partially in northeastern Sugarloaf Township and partially in Sullivan County and Luzerne County.

Geographic entities mentioned:
surface_form: central mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.3
lon: -76.3463
Central Mountain's official coordinates are in the United States Geological Survey quadrangle of Red Rock. The mountain is located partially in northeastern Sugarloaf Township and partially in Sullivan County and Luzerne County. A rock formation known as the Duncannon Member of the Catskill Formation occurs on Central Mountain. It is thick at this location.

Geographic entities mentioned:
surface_form: central mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.3
lon: -76.3463
It is thick at this location. Additionally, the Pocono Formation, a rock formation from the Mississippian Period, occurs on the mountain. The soils on Central Mountain are deep-muck soils that are saturated with water. History and etymology. Central Mountain was historically known as North Mountain due to the fact that it is the northernmost mountain in Columbia County.

Geographic entities mentioned:
surface_form: central mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.3
lon: -76.3463
History and etymology. Central Mountain was historically known as North Mountain due to the fact that it is the northernmost mountain in Columbia County. Between 1860 and 1900, it came to be known as Central Mountain, after the village of Central. Central Mountain became the most common name for the mountain by the 1890s, during the period where the lumber industry was prevalent in the area.

Geographic entities mentioned:
surface_form: central mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.3
lon: -76.3463
Between 1860 and 1900, it came to be known as Central Mountain, after the village of Central. Central Mountain became the most common name for the mountain by the 1890s, during the period where the lumber industry was prevalent in the area. A school district and geographical district named Central District existed in the 1800s in Sugarloaf Township.

Geographic entities mentioned:
surface_form: central mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.3
lon: -76.3463
A school district and geographical district named Central District existed in the 1800s in Sugarloaf Township. It was named after Central Mountain and the village of Central. In the 21st century, potential threats to the natural habitats on the mountain include logging and all terrain vehicle trails. Plants. Central Mountain is listed on the Columbia County Natural Areas Inventory.

Geographic entities mentioned:
surface_form: central mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.3
lon: -76.3463
In the 21st century, potential threats to the natural habitats on the mountain include logging and all terrain vehicle trails. Plants. Central Mountain is listed on the Columbia County Natural Areas Inventory. It is one of the most important sites on the inventory, with a priority rank of 1 on a scale of 1 to 5, with 1 being the most important.

Geographic entities mentioned:
surface_form: central mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.3
lon: -76.3463
The only other sites in Columbia County with a rank of 1 are South Branch Roaring Creek and the Susquehanna River. The entire northern part of Columbia County, including Central Mountain, is covered in northern hardwood forests. Ecosystems on the mountain include an Ephemeral/Fluctuating Pool Natural Community and a Hemlock Palustrine Forest Natural Community.

Geographic entities mentioned:
surface_form: central mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.3
lon: -76.3463
The mountain contains forested wetlands consisting mainly of hemlock trees. There are open sedge meadows in some places. Sphagnum mosses, sedges, and other herbaceous plants grow on Central Mountain. The federally endangered northeastern bulrush also grows on it. Numerous species use the mountain as a habitat.

Geographic entities mentioned:
surface_form: central mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.3
lon: -76.3463
Numerous species use the mountain as a habitat. In addition to hemlock, the main tree species on the mountain include yellow birch, black birch, black gum, sugar maple, red maple, white oak, chestnut oak, red oak, white pine, sassafras, basswood, tulip poplar, pignut hickory, mockernut hickory, shagbark hickory, and ash. Numerous shrub species inhabit Central Mountain.

Geographic entities mentioned:
surface_form: central mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.3
lon: -76.3463
Animals. Numerous bird species inhabit Central Mountain. These include four warbler species, three vireo species, the hermit thrush, the dark-eyed junco, the veery, the black-capped chickadee, the ovenbird, the gray catbird, the common yellowthroat, the scarlet tanager, the eastern towhee, and the eastern wood pewee.

Geographic entities mentioned:
surface_form: central mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.3
lon: -76.3463
The entire northern part of Columbia County, including Central Mountain, is covered in northern hardwood forests. Ecosystems on the mountain include an Ephemeral/Fluctuating Pool Natural Community and a Hemlock Palustrine Forest Natural Community. The mountain contains forested wetlands consisting mainly of hemlock trees. There are open sedge meadows in some places.

Geographic entities mentioned:
surface_form: hemlock
instance_of: Lake
countries: United States
coordinates: lat: 42.718611111111
lon: -77.608888888889
Numerous species use the mountain as a habitat. In addition to hemlock, the main tree species on the mountain include yellow birch, black birch, black gum, sugar maple, red maple, white oak, chestnut oak, red oak, white pine, sassafras, basswood, tulip poplar, pignut hickory, mockernut hickory, shagbark hickory, and ash. Numerous shrub species inhabit Central Mountain.

Geographic entities mentioned:
surface_form: hemlock
instance_of: Lake
countries: United States
coordinates: lat: 42.718611111111
lon: -77.608888888889
Central Mountain's official coordinates are in the United States Geological Survey quadrangle of Red Rock. The mountain is located partially in northeastern Sugarloaf Township and partially in Sullivan County and Luzerne County. A rock formation known as the Duncannon Member of the Catskill Formation occurs on Central Mountain. It is thick at this location.

Geographic entities mentioned:
surface_form: sugarloaf
instance_of: Mountain
countries: United States
coordinates: lat: 43.832777777778
lon: -74.822222222222
Central Mountain became the most common name for the mountain by the 1890s, during the period where the lumber industry was prevalent in the area. A school district and geographical district named Central District existed in the 1800s in Sugarloaf Township. It was named after Central Mountain and the village of Central.

Geographic entities mentioned:
surface_form: sugarloaf
instance_of: Mountain
countries: United States
coordinates: lat: 43.832777777778
lon: -74.822222222222
Animals. Numerous bird species inhabit Central Mountain. These include four warbler species, three vireo species, the hermit thrush, the dark-eyed junco, the veery, the black-capped chickadee, the ovenbird, the gray catbird, the common yellowthroat, the scarlet tanager, the eastern towhee, and the eastern wood pewee.

Geographic entities mentioned:
surface_form: the hermit
instance_of: Mountain
countries: United States
coordinates: lat: 37.16289
lon: -118.71847
Lake Fifteen. Lake Fifteen is a lake in the U.S. state of Washington. Lake Fifteen has a surface area of and reaches a depth of. Lake Fifteen is located in Thurston County's &quot;Section 15&quot;, hence the name.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: lake fifteen
instance_of: Lake
countries: United States
coordinates: lat: 46.87277777777778
lon: -122.66833333333334
Lake Fifteen. Lake Fifteen is a lake in the U.S. state of Washington. Lake Fifteen has a surface area of and reaches a depth of. Lake Fifteen is located in Thurston County's &quot;Section 15&quot;, hence the name.

Geographic entities mentioned:
surface_form: lake fifteen
instance_of: Lake
countries: United States
coordinates: lat: 46.87277777777778
lon: -122.66833333333334
Aan River. The Aan River is a short river in the South Island of New Zealand. The river flows out of Lake Innes and into the sea on the southern coast of the South Island. The river may be reached on foot via the South Coast Track, which crosses it via a suspension bridge. It also has a tributary that drains the basin to the south of the 1189-metre high Mount Aitkin.

Geographic entities mentioned:
surface_form: Lake Innes
instance_of: Lake
countries: New Zealand
coordinates: lat: -46.177
lon: 166.96
Poggio Ballone. Poggio Ballone is a hilly massif in southern Tuscany, near the northern-central coast of the Maremma region. It forms the southwestern extension of the Colline Metallifere, separating the Pecora River plain from the Grosseto plain, crossed by the Bruna and Ombrone rivers.

Geographic entities mentioned:
surface_form: poggio ballone
instance_of: Mountain
countries: Italy
coordinates: lat: 42.8292
lon: 10.8803
At the highest peak, Poggio Ballone, the Italian Air Force operates a radar station (&quot;121ª Squadriglia radar remota&quot;) for monitoring air traffic over the Tyrrhenian Sea. Other notable peaks include Poggio Spada (540 m) and Poggio Serra Alta (547 m), located east of Tirli.

Geographic entities mentioned:
surface_form: poggio ballone
instance_of: Mountain
countries: Italy
coordinates: lat: 42.8292
lon: 10.8803
The northern and eastern slopes transition into the Maremma plain, featuring peaks like Monte d'Alma (559 m), Monte Calvo (468 m), Poggio Scodella (355 m), Poggio Bruno (368 m), and Poggio di Vetulonia (335 m), near the historic town and archaeological site of Vetulonia.

Geographic entities mentioned:
surface_form: monte calvo
instance_of: Mountain
countries: Italy
coordinates: lat: 40.40583333
lon: 15.06388889
Lavandevil. Lavandevil () is a city in, and the capital of, Lavandevil District of Astara County, Gilan province, Iran. It also serves as the administrative center for Lavandevil Rural District. The city lies between the coast of the Caspian Sea and the northeastern Alborz mountain range, located just south of Lavandevil Wildlife Refuge. Population.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
South Gippsland. South Gippsland, a region of Gippsland in Victoria, Australia, is a well-watered region consisting of low, rolling hills descending to the coast in the south and the Latrobe Valley in the north. It is part of the larger Gippsland Basin bioregion. Geography. Low granite hills continue into Wilsons Promontory, the southernmost point of Victoria and mainland Australia.

Geographic entities mentioned:
surface_form: Latrobe Valley
instance_of: Valley
countries: Australia
coordinates: lat: -38.1806
lon: 146.278
Orobica. The Orobica or Valgerola is an Italian breed of domestic goat from the Val Gerola in the province of Sondrio, in the Bergamo Alps of northern Italy. It is raised in the Val Gerola and the Valchiavenna in the province of Sondrio, in the Alto Lario Occidentale, the Valsassina and the Val Varrone in the province of Como, and in the upper Val Brembana in the Province of Bergamo.

Geographic entities mentioned:
surface_form: Valchiavenna
instance_of: Valley
countries: Italy
coordinates: lat: 46.25
lon: 9.4
surface_form: Valsassina
instance_of: Valley
countries: Italy
coordinates: lat: 45.983
lon: 9.4
surface_form: Val Brembana
instance_of: Valley
countries: Italy
coordinates: lat: 45.8725
lon: 9.651944444444444
The main road from Luanda to Lubumbashi traverses the province from west to east. The province is dominated by dry savannah land; only in the Kasai River valley are there remnants of tropical rainforest. The Kasai forms the eastern and southern frontier of Lunda Sul and is the main river of the province. The Kwango River is also a major river of the province.

Geographic entities mentioned:
surface_form: Kasai River
instance_of: Watercourse
countries: Angola
Democratic Republic of the Congo
coordinates: lat: -10.9603
lon: 19.3156
The province is dominated by dry savannah land; only in the Kasai River valley are there remnants of tropical rainforest. The Kasai forms the eastern and southern frontier of Lunda Sul and is the main river of the province. The Kwango River is also a major river of the province. The climate of the province is predominantly tropical. Economy and social issues.

Geographic entities mentioned:
surface_form: Kwango River
instance_of: Watercourse
countries: Angola
Democratic Republic of the Congo
coordinates: lat: -3.3713888888889
lon: 17.358055555556
The Annals of Ulster () cover years from AD 431 to AD 1540 and were compiled in the territory of what is now Northern Ireland: entries up to AD 1489 were compiled in the late 15th century by the scribe Ruaidhrí Ó Luinín, under his patron Cathal Óg Mac Maghnusa on the island of Belle Isle on Lough Erne.

Geographic entities mentioned:
surface_form: Lough Erne
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.48262
lon: -7.80622
It is located in the Ancash Region, Bolognesi Province, Pacllon District, and in the Lima Region, Cajatambo Province, Copa District. Rajucollota lies on a sub-range west of Yerupaja, west of the mountain Huacrish, northwest of the mountain Auxilio and north of the lake Suerococha.

Geographic entities mentioned:
surface_form: Huacrish
instance_of: Mountain
countries: Peru
coordinates: lat: -10.2986
lon: -76.9639
surface_form: Auxilio
instance_of: Mountain
countries: Peru
coordinates: lat: -10.3056
lon: -76.9653
surface_form: suerococha
instance_of: Mountain
countries: Peru
coordinates: lat: -10.2864
lon: -76.9758
surface_form: suerococha
instance_of: Mountain
countries: Peru
coordinates: lat: -10.2972
lon: -76.9806
surface_form: huacrish
instance_of: Mountain
countries: Peru
coordinates: lat: -10.2986
lon: -76.9639
surface_form: suerococha
instance_of: Mountain
countries: Peru
coordinates: lat: -10.3861
lon: -76.8556
surface_form: auxilio
instance_of: Mountain
countries: Peru
coordinates: lat: -10.3056
lon: -76.9653
It is located in the Ancash Region, Bolognesi Province, Pacllon District, and in the Lima Region, Cajatambo Province, Copa District. Rajucollota lies on a sub-range west of Yerupaja, west of the mountain Huacrish, northwest of the mountain Auxilio and north of the lake Suerococha.

Geographic entities mentioned:
surface_form: copa
instance_of: Mountain
countries: Peru
coordinates: lat: -9.2666666666667
lon: -77.516666666667
Rajucollota (possibly from Quechua &quot;rahu&quot; snow, ice, mountain with snow, &quot;qulluta, kalluta&quot; mortar), Suerococha (possibly from Quechua &quot;suyru&quot; very long dress tracked after when worn, &quot;qucha&quot; lake,), named after the nearby lake, or Diablo Mudo (Spanish for &quot;dumb devil&quot;) is a mountain in the west of the Huayhuash mountain range in the Andes of Peru, about high.

Geographic entities mentioned:
surface_form: qulluta
instance_of: Mountain
countries: Peru
coordinates: lat: -13.2558
lon: -74.895
surface_form: suerococha
instance_of: Mountain
countries: Peru
coordinates: lat: -10.2864
lon: -76.9758
surface_form: qulluta
instance_of: Mountain
countries: Peru
coordinates: lat: -8.46666667
lon: -77.525
surface_form: qulluta
instance_of: Mountain
countries: Peru
coordinates: lat: -9.97694444
lon: -77.45583333
surface_form: rajucollota
instance_of: Mountain
countries: Peru
coordinates: lat: -10.2972
lon: -76.9806
surface_form: diablo mudo
instance_of: Mountain
countries: Peru
coordinates: lat: -10.2972
lon: -76.9806
surface_form: suerococha
instance_of: Mountain
countries: Peru
coordinates: lat: -10.2972
lon: -76.9806
surface_form: suerococha
instance_of: Mountain
countries: Peru
coordinates: lat: -10.3861
lon: -76.8556
surface_form: qulluta
instance_of: Mountain
countries: Peru
coordinates: lat: -8.80416667
lon: -77.64944444
Rajucollota.

Geographic entities mentioned:
surface_form: rajucollota
instance_of: Mountain
countries: Peru
coordinates: lat: -10.2972
lon: -76.9806
Limestone Run (North Branch Potomac River tributary). Limestone Run is a stream that lies to the east of New Creek Mountain in Mineral County, West Virginia. It is a tributary of the North Branch Potomac River.

Geographic entities mentioned:
surface_form: New Creek Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.228
lon: -79.1288
Limestone Run (North Branch Potomac River tributary). Limestone Run is a stream that lies to the east of New Creek Mountain in Mineral County, West Virginia. It is a tributary of the North Branch Potomac River.

Geographic entities mentioned:
surface_form: North Branch Potomac River
instance_of: Watercourse
countries: United States
coordinates: lat: 39.5284255
lon: -78.5875141
As everybody was curious of Khamba's physical prowess, his sister then kept him in hiding for a while. Thoibi is heart-brokened and pines after him. From the grace of God Thangching, the two meet again on the Loktak lake. Their love is steady until the recalcitrant behaviour and overzealous stance of Thoibi provokes her father to come in the way of the lovers in league with Nongban.

Geographic entities mentioned:
surface_form: Loktak lake
instance_of: Lake
countries: India
coordinates: lat: 24.55
lon: 93.783333333333
However, the college was only open for two years before the grounds were commandeered by the Australian Army in 1942. The boarding students were evacuated to Eagle Heights on Tamborine Mountain, where several guest houses were rented for accommodation and a building was purchased for the new school.

Geographic entities mentioned:
surface_form: Tamborine Mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -27.927513888889
lon: 153.19430555556
Cyclone Midhili. Severe Cyclonic Storm Midhili () was a tropical cyclone which impacted Bangladesh and Northeast India in mid-November 2023. The fifth named storm of the annual North Indian Ocean cyclone season, Midhili formed as a low-pressure area in the southeastern Bay of Bengal on 14 November. The system tracked west-northwest but turned northward on the next day.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Its remnants moved into Tripura, brought rainfalls and caused crop damage, but no fatalities were reported in the state. Meteorological history. On 14 November, the Indian Meteorological Department (IMD) noted a low-pressure area formed over the southeastern Bay of Bengal, near the Andaman and Nicobar Islands and tracked west-northwest. Early on the next day, the IMD designated it as a depression.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
A girl in Mirsharai Upazila was killed by a fallen tree at her home. A businessperson died in Basail Upazila, also due to a fallen tree. 300 fishermen on 20 fishing trawlers were missing in the Bay of Bengal after going out to the deep sea to catch fish. The Bangladesh Navy rescued numerous fisherman, though 25 of them were still missing as of 8 December.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Lake Ann (Minnesota). Lake Ann is a lake in Carver County, Minnesota, in the United States. Fishing.

Geographic entities mentioned:
surface_form: lake ann (minnesota)
instance_of: Lake
countries: United States
coordinates: lat: 44.87111111
lon: -93.55972222
Lake Ann (Minnesota). Lake Ann is a lake in Carver County, Minnesota, in the United States. Fishing.

Geographic entities mentioned:
surface_form: lake ann
instance_of: Lake
countries: United States
coordinates: lat: 44.87111111
lon: -93.55972222
Fishing. Lake Ann contains various species of fish including black, brown and yellow bullheads, banded killifish, black crappie, blackchin shiner, bluegill, central mudminnow, largemouth bass, northern pike, pumpkinseed, walleye, white sucker, yellow perch, common carp, Bluntnose minnow, golden shiner, Johnny darter, Spottail shiner as well as two species of sunfish: green and hybrid.

Geographic entities mentioned:
surface_form: lake ann
instance_of: Lake
countries: United States
coordinates: lat: 44.87111111
lon: -93.55972222
Lake Ann has two invasive species: Brittle naiad and Eurasian watermilfoil
History. Native American tribes occupied the lake long before European settlers. French-Canadian trappers and fur traders arrived from the Hudson-Bay Company but soon were replaced by the American Fur Company. However, Lake Ann soon became a site for those interested in lumbering. During this time, towns and camps emerged.

Geographic entities mentioned:
surface_form: lake ann
instance_of: Lake
countries: United States
coordinates: lat: 44.87111111
lon: -93.55972222
Native American tribes occupied the lake long before European settlers. French-Canadian trappers and fur traders arrived from the Hudson-Bay Company but soon were replaced by the American Fur Company. However, Lake Ann soon became a site for those interested in lumbering. During this time, towns and camps emerged. Lake Ann got its name from the wife of William S. Judd, an early settler.

Geographic entities mentioned:
surface_form: lake ann
instance_of: Lake
countries: United States
coordinates: lat: 44.87111111
lon: -93.55972222
French-Canadian trappers and fur traders arrived from the Hudson-Bay Company but soon were replaced by the American Fur Company. However, Lake Ann soon became a site for those interested in lumbering. During this time, towns and camps emerged. Lake Ann got its name from the wife of William S. Judd, an early settler. Early settlements were known for their local legends.

Geographic entities mentioned:
surface_form: lake ann
instance_of: Lake
countries: United States
coordinates: lat: 44.87111111
lon: -93.55972222
Early settlements were known for their local legends. Present-day historical societies have collections of newspaper clippings and hand-written accounts describing celebrity trappers, lumberjacks, and river drovers. In the 1970s, Chanhassen developed its first city park on the south shore of the lake, known as Lake Ann Park. The park was built during a population growth spur.

Geographic entities mentioned:
surface_form: lake ann
instance_of: Lake
countries: United States
coordinates: lat: 44.87111111
lon: -93.55972222
In the 1970s, Chanhassen developed its first city park on the south shore of the lake, known as Lake Ann Park. The park was built during a population growth spur. The park was part of a redevelopment plan which included adding more companies to the area, which brought in more residents. Today, Lake Ann Park in one of many parks in the city.

Geographic entities mentioned:
surface_form: lake ann
instance_of: Lake
countries: United States
coordinates: lat: 44.87111111
lon: -93.55972222
Background. The three women grew up in the San Fernando Valley, listening to the 1970s classic rock and Americana records of their music-loving parents. While they were still at school their parents formed a family band called Rockinhaim to play cover versions at local charity fairs, with Israeli-born father Mordechai (&quot;Moti&quot;) on drums and mother Donna on guitar.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Overview. Meall Glas has Munro status with a height of. It is the highest point of the high rolling uplands between Glen Lochay and Glen Dochart, an area lacking distinctive mountainous character. Another Munro, Sgiath Chuil, lies 2 km to the east; the Corbett Beinn nan Imirean is 2 km to the south west. The three hills can be climbed together in the same walk.

Geographic entities mentioned:
surface_form: Glen Lochay
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.48333
lon: -4.43333
surface_form: Glen Dochart
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.417
lon: -4.433
The south side of the mountain has a broad shelf at a height of around 450 metres, the result of lateral erosion by glaciers in the Ice Age. Rainfall on Meall Glas drains to the east coast of Scotland via the glens of Dochart (south) or Lochay (north) and then by Loch Tay and the River Tay. Ascents and view. Meall Glas can be climbed from either Glen Dochart or Glen Lochay.

Geographic entities mentioned:
surface_form: Loch Tay
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.515555555556
lon: -4.1461111111111
surface_form: meall glas
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.4559
lon: -4.547
Meall Glas. Meall Glas is a mountain situated in the southern highlands of Scotland. It stands on the northern border of the Loch Lomond and the Trossachs National Park, 8.5 kilometres north east of Crianlarich. Overview. Meall Glas has Munro status with a height of.

Geographic entities mentioned:
surface_form: meall glas
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.4559
lon: -4.547
Meall Glas is a mountain situated in the southern highlands of Scotland. It stands on the northern border of the Loch Lomond and the Trossachs National Park, 8.5 kilometres north east of Crianlarich. Overview. Meall Glas has Munro status with a height of. It is the highest point of the high rolling uplands between Glen Lochay and Glen Dochart, an area lacking distinctive mountainous character.

Geographic entities mentioned:
surface_form: meall glas
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.4559
lon: -4.547
Another Munro, Sgiath Chuil, lies 2 km to the east; the Corbett Beinn nan Imirean is 2 km to the south west. The three hills can be climbed together in the same walk. Meall Glas is overshadowed by the more impressive mountains around Crianlarich. Its name, which translates from the Gaelic as “Greenish-grey hill” suggests its topographic character.

Geographic entities mentioned:
surface_form: meall glas
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.4559
lon: -4.547
The hill is not well seen from Glen Dochart to the south, from where it is usually climbed, being observed as merely the top of rising moorland. Geography. Meall Glas comprises mainly rolling grassy slopes, with two main ridges. The north west ridge drops from the summit to Glen Lochay and can be used as an ascent route.

Geographic entities mentioned:
surface_form: meall glas
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.4559
lon: -4.547
The other ridge curves east round the lip of Coire Cheathaich, passing over an unnamed top at 908m before swinging north east to the Munro Top of Beinn Cheathaich (937 metres), 1.5 km from the main peak. In Sir Hugh Munro’s original tables of 1891, Beinn Cheathaich was listed as the Munro with Meall Glas as the “Top”, an error rectified in the 1921 revision.

Geographic entities mentioned:
surface_form: meall glas
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.4559
lon: -4.547
Rainfall on Meall Glas drains to the east coast of Scotland via the glens of Dochart (south) or Lochay (north) and then by Loch Tay and the River Tay. Ascents and view. Meall Glas can be climbed from either Glen Dochart or Glen Lochay. The southern approach from Glen Dochart is the most popular because of ease of access by car.

Geographic entities mentioned:
surface_form: meall glas
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.4559
lon: -4.547
surface_form: glen dochart
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.417
lon: -4.433
The route proceeds for 1.5 km west up the glen, crosses the River Lochay by a ford (the bridge no longer exists) and follows a track by the Lubchurran Burn which goes south and west and before reaching the summit via the Top of Beinn Cheathaich. The summit of Meall Glas is marked by a small cairn perched on a rocky outcrop.

Geographic entities mentioned:
surface_form: meall glas
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.4559
lon: -4.547
It was probably named by the inhabitants of Glen Lochay to which it shows its more impressive northern outline, with the summit ridge seen as a curving hollow. The hill is not well seen from Glen Dochart to the south, from where it is usually climbed, being observed as merely the top of rising moorland. Geography. Meall Glas comprises mainly rolling grassy slopes, with two main ridges.

Geographic entities mentioned:
surface_form: glen dochart
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.417
lon: -4.433
Ascents and view. Meall Glas can be climbed from either Glen Dochart or Glen Lochay. The southern approach from Glen Dochart is the most popular because of ease of access by car. The route starts at Auchessan (grid reference) on the A85 road and goes north across moorland to reach the summit ridge just to the east of the highest point.

Geographic entities mentioned:
surface_form: glen dochart
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.417
lon: -4.433
Their operation was expanded in 1836 with the construction of an iron furnace and further still in 1841 when a rolling mill was added to the complex. Iron ore was transported from Centre County down the West Branch Susquehanna Valley and up Lycoming Creek to the iron works. The McKinneys' effort was ultimately unsuccessful. The efforts of two more iron masters also failed.

Geographic entities mentioned:
surface_form: West Branch Susquehanna Valley
instance_of: Valley
countries: United States
Punta Lazoney. The Punta Lazoney is a peak in the Biellese Alps with an elevation of 2,579 m a.s.l. It lies between Valsesia, in the Province of Vercelli, and the Lys Valley, in Aosta Valley; at the summit, the municipal territories of the Piedmontese commune of Rassa and the Aosta Valley communes of Gressoney-Saint-Jean and Gaby converge. Toponym.

Geographic entities mentioned:
surface_form: Valsesia
instance_of: Valley
countries: Italy
coordinates: lat: 45.816666666667
lon: 8.1333333333333
Description. Punta Lazoney lies at the convergence of three ridges: the northern ridge descends to the Loo Pass and connects it to the nearby Monte Cossarello, while the southeastern ridge, also part of the Lys / Sesia watershed, is rugged and uneven, reaching the Bocchetta di Niel (2,430 m) after a series of rocky outcrops before ascending to the Punta Tre Vescovi.

Geographic entities mentioned:
surface_form: Punta Tre Vescovi
instance_of: Mountain
countries: Italy
coordinates: lat: 45.72527778
lon: 7.9375
surface_form: punta tre vescovi
instance_of: Mountain
countries: Italy
coordinates: lat: 45.72527778
lon: 7.9375
In both cases, the &quot;Guida dei Monti d'Italia&quot; rates the ascent as difficulty &quot;E,&quot; while others consider it to be of type &quot;EE&quot;. The ascent along the southeastern ridge from the Bocchetta di Niel is more challenging and includes several II-grade passages plus a IV-grade section known as &quot;del Dado&quot;, which can be bypassed on the Valsesia side. Winter access.

Geographic entities mentioned:
surface_form: Valsesia
instance_of: Valley
countries: Italy
coordinates: lat: 45.816666666667
lon: 8.1333333333333
surface_form: valsesia
instance_of: Valley
countries: Italy
coordinates: lat: 45.816666666667
lon: 8.1333333333333
Punta Lazoney. The Punta Lazoney is a peak in the Biellese Alps with an elevation of 2,579 m a.s.l. It lies between Valsesia, in the Province of Vercelli, and the Lys Valley, in Aosta Valley; at the summit, the municipal territories of the Piedmontese commune of Rassa and the Aosta Valley communes of Gressoney-Saint-Jean and Gaby converge. Toponym.

Geographic entities mentioned:
surface_form: punta lazoney
instance_of: Mountain
countries: Italy
coordinates: lat: 45.7347
lon: 7.9269
Toponym. In addition to &quot;Punta Lazoney,&quot; the mountain is also referred to in Italian publications as &quot;Punta Loozoney,&quot; using a different transcription of the name used by local inhabitants. The name in French is &quot;Pointe Lazouney&quot;, and in Walser it is &quot;Lasòneyspetz&quot; or &quot;Lazòneyhòre&quot;. Description.

Geographic entities mentioned:
surface_form: punta lazoney
instance_of: Mountain
countries: Italy
coordinates: lat: 45.7347
lon: 7.9269
At the mountain's highest point stands a cairn of stones; the panorama is extensive, offering an excellent view of the Monte Rosa group. The mountain's summit also corresponds to the geodetic trigonometric point of the IGM named &quot;Punta Lazoney&quot; (code 029071). Summer access. Punta Lazoney is accessible via the ridge from both the Loo and the Lazoney Passes.

Geographic entities mentioned:
surface_form: punta lazoney
instance_of: Mountain
countries: Italy
coordinates: lat: 45.7347
lon: 7.9269
surface_form: punta lazoney
instance_of: Mountain
countries: Italy
coordinates: lat: 45.7347
lon: 7.9269
Delaware Lake (New York). Delaware Lake is a small lake north of Long Eddy in Delaware County, New York. It drains south via an unnamed creek which flows into Hoolihan Brook. It was once referred to as Perch Pond

Geographic entities mentioned:
surface_form: delaware lake (new york)
instance_of: Lake
countries: United States
coordinates: lat: 41.8875
lon: -75.13
Delaware Lake (New York). Delaware Lake is a small lake north of Long Eddy in Delaware County, New York. It drains south via an unnamed creek which flows into Hoolihan Brook. It was once referred to as Perch Pond

Geographic entities mentioned:
surface_form: delaware lake
instance_of: Lake
countries: United States
coordinates: lat: 41.8875
lon: -75.13
Kremena Ice Piedmont. Kremena Ice Piedmont (,) is a 2.4 km long and 2.7 km wide glacier on Smith Island in the South Shetland Islands, Antarctica draining the southeast slopes of Imeon Range south of Organa Peak. Draining southeastwards to flow into Osmar Strait. The glacier is named after the settlements of Kremena in northeastern Bulgaria, and Upper and Lower Kremena in northwestern Bulgaria.

Geographic entities mentioned:
surface_form: Organa Peak
instance_of: Mountain
coordinates: lat: -63.050555555556
lon: -62.629722222222
Heddalsvatnet. Heddalsvatnet () is a lake in Notodden Municipality and Midt-Telemark Municipality in Telemark county, Norway. The lake is located just south of the town of Notodden. The village of Heddal and the Heddalen valley are located to the northwest of the lake. Geography. The main rivers that flow into the lake are the rivers Tinnelva and Heddøla.

Geographic entities mentioned:
surface_form: heddalsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 59.55805556
lon: 9.2175
The lake is part of the Skien watershed and is connected to the ocean by the Telemark Canal. Heddalsvatnet is only above sea level and only two locks at Skien were needed to allow ships to sail on the lake. The canal opened in 1861 and made Notodden into Norway's largest fresh water port. In the late 1800s, seafaring vessels were constructed at the shores of Heddalsvatnet. History.

Geographic entities mentioned:
surface_form: heddalsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 59.55805556
lon: 9.2175