Sarmila/GeoWiki-Features huggingface dataset:
Climate. Based on the Köppen climate classification, Silverhorn Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Silverhorn Mountain drains west into the Mistaya River, or east into Dolomite Creek which is a tributary of the Siffleur River.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mistaya
instance_of: Valley
countries: Canada
coordinates: lat: 51.9503
lon: -116.717
surface_form: silverhorn mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.7667
lon: -116.50221
The Simien Mountains National Park stands out for its peaks and deep valleys that attract hikers and nature lovers alike. Its renowned peak, Ras Dashen rising 4,550 meters (m) above sea level is not only Ethiopia's peak but also one of the tallest mountains in Africa. Etymology.

Geographic entities mentioned:
surface_form: Ras Dashen
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 13.236666666667
lon: 38.3725
Maria-Chapdelaine Regional County Municipality. Maria-Chapdelaine is a regional county municipality in the Saguenay–Lac-Saint-Jean region of Quebec, Canada. Its seat is in Dolbeau-Mistassini. It runs from Lac Saint-Jean in the south to the deep interior of northern Quebec in the north. Demographics.

Geographic entities mentioned:
surface_form: Lac Saint-Jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
Tibetan blue bear. The Tibetan brown bear (&quot;Ursus arctos pruinosus&quot;), also known as Tibetan blue bear'&quot;, is a subspecies of the brown bear (&quot;Ursus arctos&quot;) in the eastern Tibetan Plateau. One of the rarest subspecies of bear in the world, the blue bear is rarely sighted in the wild.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Chippewa Valley. The Chippewa Valley is a valley in Wisconsin, US. History. The valley was first inhabited by the Ojibwe and colonized by German and Scandinavian immigrants. The region also has a large Hmong community.

Geographic entities mentioned:
surface_form: chippewa valley
instance_of: Valley
countries: United States
coordinates: lat: 44.75
lon: -91.5
The region also has a large Hmong community. While the term &quot;Chippewa Valley&quot; technically refers to the drainage basin of the Chippewa River and its tributaries, the name is more often applied to the Eau Claire-Chippewa Falls metropolitan area and the surrounding area—including communities not located within the Chippewa River's watershed.

Geographic entities mentioned:
surface_form: chippewa valley
instance_of: Valley
countries: United States
coordinates: lat: 44.75
lon: -91.5
From the 1850s to the early 1910s, lumber baron Orrin Henry Ingram was largely responsible for the deforestation of the valley and the subsequent establishment of many small towns in the area. The population center of the Chippewa Valley is Eau Claire. Menards, an American home improvement retail company, is also headquartered there.

Geographic entities mentioned:
surface_form: chippewa valley
instance_of: Valley
countries: United States
coordinates: lat: 44.75
lon: -91.5
Chippewa Valley. The Chippewa Valley is a valley in Wisconsin, US. History. The valley was first inhabited by the Ojibwe and colonized by German and Scandinavian immigrants. The region also has a large Hmong community.

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
From the 1850s to the early 1910s, lumber baron Orrin Henry Ingram was largely responsible for the deforestation of the valley and the subsequent establishment of many small towns in the area. The population center of the Chippewa Valley is Eau Claire. Menards, an American home improvement retail company, is also headquartered there.

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
Gau Graig. Gau Graig is a subsidiary summit of Cadair Idris in the Snowdonia National Park, in Gwynedd, northwest Wales. It lies to the east of Mynydd Moel on a broad grassy plateau. It marks the eastern end of the Cadair Idris ridge. The summit is marked by a cairn. To the north are Y Garn and Diffwys, to the west Rhobell Fawr and Aran Fawddwy and to the south are Waun-oer and Cribin Fawr.

Geographic entities mentioned:
surface_form: Cadair Idris
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.699827777778
lon: -3.9086944444444
Gau Graig. Gau Graig is a subsidiary summit of Cadair Idris in the Snowdonia National Park, in Gwynedd, northwest Wales. It lies to the east of Mynydd Moel on a broad grassy plateau. It marks the eastern end of the Cadair Idris ridge. The summit is marked by a cairn. To the north are Y Garn and Diffwys, to the west Rhobell Fawr and Aran Fawddwy and to the south are Waun-oer and Cribin Fawr.

Geographic entities mentioned:
surface_form: Mynydd Moel
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.705782
lon: -3.884874
Gau Graig. Gau Graig is a subsidiary summit of Cadair Idris in the Snowdonia National Park, in Gwynedd, northwest Wales. It lies to the east of Mynydd Moel on a broad grassy plateau. It marks the eastern end of the Cadair Idris ridge. The summit is marked by a cairn. To the north are Y Garn and Diffwys, to the west Rhobell Fawr and Aran Fawddwy and to the south are Waun-oer and Cribin Fawr.

Geographic entities mentioned:
surface_form: Diffwys
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.79165
lon: -3.98676
surface_form: Rhobell Fawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.814
lon: -3.802
surface_form: Aran Fawddwy
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.78702
lon: -3.68786
surface_form: Waun-oer
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.717037
lon: -3.799394
surface_form: Cribin Fawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.721757
lon: -3.786277
Geography. Anji County is located within the Yangtze Delta, where the Yangtze meets the East China Sea. The Tianmu Mountains run through southwest portion of the county, with the county's highest point, reaching in elevation. Xitiao River, the county's longest river, flows from the southwest mountains northeast, before eventually emptying into Lake Tai.

Geographic entities mentioned:
surface_form: Xitiao River
instance_of: Watercourse
countries: People's Republic of China
coordinates: lat: 30.5919
lon: 119.655
surface_form: Lake Tai
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 31.166666666667
lon: 120.15
The basic traditionalism of Serbian sculptures after World War II was enriched by the individual expressions of Jovan Soldatović and Nebojša Mitrić, but it was left to yet another generation to break away from figurative conceptions. In 1973, commemorating the dedication of the new Njegoš mausoleum on Mount Lovćen, he created and designed a series of silver and gold medals.

Geographic entities mentioned:
surface_form: Lovćen
instance_of: Mountain
countries: Montenegro
coordinates: lat: 42.4
lon: 18.833333333333
Boreal chorus frog. The boreal chorus frog'&quot;, (&quot;Pseudacris maculata&quot;) is a species of chorus frog native to Canada from the west of Lake Superior to western Alberta and north to the North West Territories. It occurs in the USA throughout Montana, northwestern Wisconsin, northeastern Arizona, northern New Mexico and southwestern Utah.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
The colossus is about high and is meant as a personification of the Apennine Mountains. It was the water source for the Pratolino, its fountains and secret water plays. The colossus has the appearance of an elderly man crouched at the shore of a lake and is surrounded by other sculptures depicting mythological themes from Ovid's &quot;Metamorphoses&quot; including Pegasus, Parnassus or Jupiter.

Geographic entities mentioned:
surface_form: Parnassus
instance_of: Mountain
countries: Greece
coordinates: lat: 38.533
lon: 22.6167
The population was 2,341 at the 2020 census. History. The Apalachicola Province, after whom the river and, ultimately the city, are named, was located along the lower part of the Chattahoochee River in Alabama and Georgia in the 17th century, when the Spanish included the Chattahoochee as part of the Apalachicola River.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
A British trading post called &quot;Cottonton&quot; was founded at this site on the mouth of the Apalachicola River. In 1783, British West Florida was transferred to Spain; however, the trading post (and its British inhabitants) remained and continued facilitating trade along the Apalachicola River (which was connected to the trading network along the Chattahoochee River).

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
98, is named for him. Before railroads reached the region in the later 19th century, Apalachicola was the third-busiest port on the Gulf of Mexico (behind New Orleans and Mobile). Scheduled boats transported passengers and goods up and down the Apalachicola, Chattahoochee, and Flint rivers to Albany and Columbus, Georgia.

Geographic entities mentioned:
surface_form: Chattahoochee
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Scholars today hold that al-Badhan is to be identified with the Badan () citied in the 2nd-century CE Mishnah and Tosefta, said to be a place then settled by Samaritans and renowned for its pomegranates. Badan is featured prominently in Samaritan tradition; According to one of these, the Israelites purified themselves at Badan after crossing the Jordan River and on their way to Mount Gerizim.

Geographic entities mentioned:
surface_form: Mount Gerizim
instance_of: Mountain
countries: State of Palestine
coordinates: lat: 32.199444444444
lon: 35.272777777778
Museum of the Shenandoah Valley. The Museum of the Shenandoah Valley (MSV) is located at 901 Amherst Street, Winchester, Virginia. Built to preserve and enrich the cultural life and heritage of the Valley, it is located on the largest green space in the city of Winchester.

Geographic entities mentioned:
surface_form: Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Rivière du Petit Portage. The rivière du Petit Portage (&quot;in English: Little Portage River&quot;) is a tributary of the west bank of the Chaudière River which flows northward to empty onto the south shore of the St. Lawrence River.

Geographic entities mentioned:
surface_form: Chaudière River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.742777777777775
lon: -71.2786111111111
This includes trackage rights over the Union Pacific Railroad between Lordsburg, New Mexico, and Bowie, Arizona. The railroad serves the copper mining region of southeastern Arizona, and the agricultural Gila River Valley. The railroad offers a transload location for lumber, building materials and other consumer commodities at Globe, Arizona, and can handle railcars weighing up to 286,000lbs.

Geographic entities mentioned:
surface_form: Gila River Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.18339
lon: -110.21731
Lower elevations are wooded with species of the northern hardwood forest type; small stands of coniferous red spruce cling to the upper slopes. A fire tower stands on the summit and a beef livestock farm occupies the east shoulder of the mountain. Pitcher Mountain is part of an extensive area of heath barrens and blueberry fields that continue north over Hubbard Hill and Jackson Hill.

Geographic entities mentioned:
surface_form: jackson hill
instance_of: Mountain
countries: United States
coordinates: lat: 37.154217
lon: -89.4734187
surface_form: hubbard hill
instance_of: Mountain
countries: United States
coordinates: lat: 42.448888888889
lon: -74.343888888889
surface_form: pitcher mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.093888888889
lon: -72.135
surface_form: jackson hill
instance_of: Mountain
countries: United States
coordinates: lat: 34.2664822
lon: -85.1632836
The east and north sides of Pitcher Mountain drain into the Beards Brook watershed, then into the Contoocook River, then the Merrimack River and the Atlantic Ocean. The west and south sides drain into Robinson Brook, thence Otter Brook, &quot;The Branch&quot;, the Ashuelot River, then the Connecticut River and Long Island Sound.

Geographic entities mentioned:
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
Pitcher Mountain. Pitcher Mountain is a 2,153 foot (656 m) monadnock located in southwest New Hampshire. The mountain is traversed by the 50 mile (80 km) Monadnock-Sunapee Greenway and offers 360 degree views from its open summit. Lower elevations are wooded with species of the northern hardwood forest type; small stands of coniferous red spruce cling to the upper slopes.

Geographic entities mentioned:
surface_form: pitcher mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.093888888889
lon: -72.135
Pitcher Mountain is part of an extensive area of heath barrens and blueberry fields that continue north over Hubbard Hill and Jackson Hill. The east and north sides of Pitcher Mountain drain into the Beards Brook watershed, then into the Contoocook River, then the Merrimack River and the Atlantic Ocean.

Geographic entities mentioned:
surface_form: pitcher mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.093888888889
lon: -72.135
The crater lies in a volcanic field at a base elevation of about, and prominence heights of about. The northwestern end of the crater is covered with lava flows, while the southern end is filled with low cinder cones. Several of the surrounding cones include the better known, taller and younger Sunset Crater in the adjacent Sunset Crater National Monument.

Geographic entities mentioned:
surface_form: Sunset Crater
instance_of: Mountain
countries: United States
coordinates: lat: 35.365
lon: -111.5
surface_form: sunset crater
instance_of: Mountain
countries: United States
coordinates: lat: 35.365
lon: -111.5
Strawberry Crater. Strawberry Crater is a cinder cone volcano, more than high, in the San Francisco volcanic field, north of Flagstaff, Arizona. It is along Forest Road 545 between the Wupatki National Monument and Sunset Crater National Monument in the Strawberry Crater Wilderness. The crater lies in a volcanic field at a base elevation of about, and prominence heights of about.

Geographic entities mentioned:
surface_form: sunset crater
instance_of: Mountain
countries: United States
coordinates: lat: 35.365
lon: -111.5
surface_form: strawberry crater
instance_of: Landform
countries: United States
coordinates: lat: 35.4472
lon: -111.469
Strawberry Crater. Strawberry Crater is a cinder cone volcano, more than high, in the San Francisco volcanic field, north of Flagstaff, Arizona. It is along Forest Road 545 between the Wupatki National Monument and Sunset Crater National Monument in the Strawberry Crater Wilderness. The crater lies in a volcanic field at a base elevation of about, and prominence heights of about.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
surface_form: strawberry crater
instance_of: Landform
countries: United States
coordinates: lat: 35.4472
lon: -111.469
Strawberry Crater. Strawberry Crater is a cinder cone volcano, more than high, in the San Francisco volcanic field, north of Flagstaff, Arizona. It is along Forest Road 545 between the Wupatki National Monument and Sunset Crater National Monument in the Strawberry Crater Wilderness. The crater lies in a volcanic field at a base elevation of about, and prominence heights of about.

Geographic entities mentioned:
surface_form: strawberry crater
instance_of: Landform
countries: United States
coordinates: lat: 35.4472
lon: -111.469
Several of the surrounding cones include the better known, taller and younger Sunset Crater in the adjacent Sunset Crater National Monument. The wilderness area that includes Strawberry Crater covers, consisting mainly of hills, cinder cones, and arid terrain ranging in elevation from. The surface landforms are about 50,000 to 100,000 years old. Name.

Geographic entities mentioned:
surface_form: strawberry crater
instance_of: Landform
countries: United States
coordinates: lat: 35.4472
lon: -111.469
Name. The cone shape and the reddish cinders that created the cone resemble a giant strawberry. Geology. Experts say that Strawberry Crater is relatively young compared to other craters in the United States. It was formed from volcanic eruptions around. There were several volcanic periods, during which multi-colored rocks were deposited on Earth's surface.

Geographic entities mentioned:
surface_form: strawberry crater
instance_of: Landform
countries: United States
coordinates: lat: 35.4472
lon: -111.469
From the top of the cinder cones there are views of the Kachina Peaks Wilderness, the Hopi Buttes, the Painted Desert, and the valley of the Little Colorado River. The geologic forms and twisted junipers make Strawberry Crater Wilderness a popular place for photography. Climate. Hiking and recreation at Strawberry Crater is open year-round.

Geographic entities mentioned:
surface_form: strawberry crater
instance_of: Landform
countries: United States
coordinates: lat: 35.4472
lon: -111.469
The geologic forms and twisted junipers make Strawberry Crater Wilderness a popular place for photography. Climate. Hiking and recreation at Strawberry Crater is open year-round. Winters near the crater average to around 50 degrees, while summers tend to be very hot and dry.

Geographic entities mentioned:
surface_form: strawberry crater
instance_of: Landform
countries: United States
coordinates: lat: 35.4472
lon: -111.469
These walls are said to be Native American constructions. There are also remnants of ancient gardens where inhabitants used volcanic cinders for water-retaining mulch. Recreation. Strawberry Crater offers a variety of recreational activities such as day hiking and horseback riding. Information about these activities can be found on the Coconino National Forest recreational website.

Geographic entities mentioned:
surface_form: strawberry crater
instance_of: Landform
countries: United States
coordinates: lat: 35.4472
lon: -111.469
Surrounding the crater, there are rolling cinder-strewn hills with a variety of different plants from pinons to junipers. From the top of the cinder cones there are views of the Kachina Peaks Wilderness, the Hopi Buttes, the Painted Desert, and the valley of the Little Colorado River. The geologic forms and twisted junipers make Strawberry Crater Wilderness a popular place for photography.

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
Pig Island / Mātau. Pig Island / Mātau is an island located at the northern end of Lake Wakatipu in the South Island of New Zealand, near the township of Glenorchy. It is slightly smaller and much flatter than its more popular neighbour Pigeon Island. It is in size and supports a variety of regenerating native scrub as well as introduced weeds.

Geographic entities mentioned:
surface_form: Lake Wakatipu
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.085
lon: 168.561
It is slightly smaller and much flatter than its more popular neighbour Pigeon Island. It is in size and supports a variety of regenerating native scrub as well as introduced weeds. Buff weka are also present on Pig Island, having been transferred there from Stevensons Island in Lake Wānaka in 2006.

Geographic entities mentioned:
surface_form: Lake Wānaka
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.5
lon: 169.13333333333
On display in the gorge, a variety of unique geologic features and processes exemplify the geology of the Appalachian Plateau, including the exposure of over of sandstone and shale, house-sized boulders scattered from rim to river, plant and invertebrate fossils, and steep channel drop-offs. The river has exposed four seams of coal, considered among the best bituminous coal in the world.

Geographic entities mentioned:
surface_form: Appalachian Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 40
lon: -78
It is surmounting Kopsis Glacier to the west, lower Embree Glacier to the north, and Young Glacier to the south. The peak is named after the settlement of Mirovyane in Western Bulgaria. Location. Mirovyane Peak is located at, which is 3.46 km northeast of Zimornitsa Peak, 13.68 km southeast of Mount Schmid and 17.94 km north-northwest of Mount Besch. US mapping in 1961, updated in 1988.

Geographic entities mentioned:
surface_form: Zimornitsa Peak
instance_of: Mountain
coordinates: lat: -78.0931
lon: -85.2036
surface_form: Mount Schmid
instance_of: Mountain
coordinates: lat: -77.96666667
lon: -85.66666667
surface_form: Mount Besch
instance_of: Mountain
coordinates: lat: -78.1833
lon: -84.7167
surface_form: mirovyane peak
instance_of: Mountain
coordinates: lat: -78.075
lon: -85.0817
Mirovyane Peak. Mirovyane Peak (,) is a mountain rising to 1387 m in Maglenik Heights, north-central Sentinel Range in the Ellsworth Mountains of Antarctica. It is surmounting Kopsis Glacier to the west, lower Embree Glacier to the north, and Young Glacier to the south. The peak is named after the settlement of Mirovyane in Western Bulgaria. Location.

Geographic entities mentioned:
surface_form: mirovyane peak
instance_of: Mountain
coordinates: lat: -78.075
lon: -85.0817
Jakob Hutter. Jakob Hutter (;; also spelled Huter or Hueter; c. 1500 – 25 February 1536) was a Tyrolean Anabaptist leader and founder of the Hutterites. Biography. Hutter was born in the small hamlet of Moos near St. Lorenzen in the Puster Valley, in the County of Tyrol (present-day South Tyrol, Italy). He learned hat making in nearby Prags and became an itinerant craftsman.

Geographic entities mentioned:
surface_form: Puster Valley
instance_of: Valley
countries: Italy
Austria
coordinates: lat: 46.7405
lon: 12.369555555555555
The western part of Assynt has many distinctively shaped mountains, including Quinag, Canisp, Suilven and Ben More Assynt, that rise steeply from the surrounding &quot;cnoc and lochan&quot; scenery. These can often appear higher than their actual height would indicate due to their steep sides and the contrast with the moorland from which they rise.

Geographic entities mentioned:
surface_form: Quinag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.215061111111
lon: -5.0505305555556
surface_form: Canisp
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.12125
lon: -5.0521
surface_form: Suilven
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.115
lon: -5.1370694444444
surface_form: Ben More Assynt
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.138164
lon: -4.858208
Many of the most distinctive peaks such as Suilven were formed during the last Ice Age, when they were left exposed above the ice sheet as nunataks, and they now remain as inselbergs of highly eroded Torridonian sandstone sitting on a bedrock of much older Lewisian gneiss.

Geographic entities mentioned:
surface_form: Suilven
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.115
lon: -5.1370694444444
Ownership. As is typical for the Scottish highlands, the Assynt area is divided into a number of large estates, which are in a mix of private, charitable and community ownership. The Assynt Estate, which includes Ben More Assynt and the lands around Lochinver, remains in the hands of the Vestey family, who also formerly owned the North Assynt Estate (see below).

Geographic entities mentioned:
surface_form: Ben More Assynt
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.138164
lon: -4.858208
The Assynt Estate, which includes Ben More Assynt and the lands around Lochinver, remains in the hands of the Vestey family, who also formerly owned the North Assynt Estate (see below). The Quinag estate belongs to the John Muir Trust, a charity that seeks to conserve wild land and wild places.

Geographic entities mentioned:
surface_form: Quinag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.215061111111
lon: -5.0505305555556
On Monday, 1 February 1993, Assynt Crofters' Trust became the owners of the North Lochinver Estate, which they renamed the &quot;North Assynt Estate&quot;. Glencanisp and Drumrunie Estate. In June 2005 the Glencanisp estate, including the mountains Suilven and Canisp and the neighbouring Drumrunie estate, with the mountains Cùl Mòr and Cùl Beag, were bought by the local community.

Geographic entities mentioned:
surface_form: Suilven
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.115
lon: -5.1370694444444
surface_form: Canisp
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.12125
lon: -5.0521
surface_form: Cùl Mòr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.057980555556
lon: -5.1168
surface_form: Cùl Beag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.0294
lon: -5.15091
The full roadway was paved by the mid-1950s, and the C-66 moniker was designated on the roadway in the early 1970s. Route description. The roadway starts at a junction with M-119 (Lake Shore Drive) and C-77 (State Road) in the community of Cross Village near Lake Michigan in Emmet County. C-66 travels southward for about concurrently along C-77 to the intersection with Levering Road.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Christoffelpark. Christoffelpark is a national park, protected nature area and tourist attraction at the north-western end of the island of Curaçao surrounding Christoffelberg (Mt Christoffel).

Geographic entities mentioned:
surface_form: Christoffelberg
instance_of: Mountain
countries: Curaçao
coordinates: lat: 12.336944444444
lon: -69.123333333333
Jim Jumper massacre. The Jim Jumper massacre, or Bluefields massacre, was an incident in 1889 at a Seminole Indian camp northeast of Lake Okeechobee, in St. Lucie County, Florida, United States, in which Jim Jumper, a biracial Seminole, killed several Seminoles, and was then killed by another Seminole. Background.

Geographic entities mentioned:
surface_form: Lake Okeechobee
instance_of: Lake
countries: United States
coordinates: lat: 26.933333333333
lon: -80.8
The Snake clan, along with other Seminole clans, had lived on Fisheating Creek west of Lake Okeechobee for many years after the Third Seminole War, but in the 1880s a white cattleman bought their herds on the condition that the Seminoles move away. The Snake clan then moved to an area northeast of Lake Okeechobee later called Bluefields.

Geographic entities mentioned:
surface_form: Lake Okeechobee
instance_of: Lake
countries: United States
coordinates: lat: 26.933333333333
lon: -80.8
&quot;The Charter of Integration between Egypt and Sudan:&quot;
Additional Egyptian projects. Along with the projects made between Sudan and Egypt; Egypt has considered storage projects in equatorial lakes: Lake Victoria, Lake Kyoga, Lake Albert. Egypt is in participation with Ethiopia and Uganda in some projects and establishing power generation stations.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
The above European Top 10 list excludes peaks on lands and islands that are part of European countries but are outside or on the limits of the European continent and its tectonic and geographic boundaries, like Teide (with prominence of), Tenerife Island, Spain; Belukha peak of the Altai Mountains in Russia (with prominence of); and Piton des Neiges (with prominence of), Réunion, France.

Geographic entities mentioned:
surface_form: Belukha peak
instance_of: Mountain
countries: Russia
Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 49.806944444444
lon: 86.589722222222
surface_form: Piton des Neiges
instance_of: Mountain
countries: France
coordinates: lat: -21.098888888889
lon: 55.478888888889
Mount Narodnaya, the highest peak in the Ural Mountains, is on the main watershed ridge, so on the limits of Europe, and cannot be considered a strictly European mountain and peak.

Geographic entities mentioned:
surface_form: Mount Narodnaya
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 65.033333333333
lon: 60.116666666667
Mount Elbrus is a dormant stratovolcano, forming part of the Caucasus Mountains, and geographically it is laying entirely in Europe and Russia, north of the main ridge and watershed of the Greater Caucasus, considered as the one that is forming the limits of Europe, that also forms great part of the length of the border between Russia and Georgia.

Geographic entities mentioned:
surface_form: Mount Elbrus
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 43.35254
lon: 42.437875
Mount Bazardüzü, also in the Caucasus, has a prominence of, but is located on the boundary between Europe and Asia, on the border between Russia and Azerbaijan, so it cannot be considered a strictly European mountain and peak. Caucasus Mountains. The boundary between Asia and Europe is following the main ridge of the Caucasus Mountains, also forming most of the border between Georgia and Russia.

Geographic entities mentioned:
surface_form: Mount Bazardüzü
instance_of: Mountain
countries: Russia
Azerbaijan
Russian Empire
Soviet Union
coordinates: lat: 41.2204928
lon: 47.8583417
A sequel, ‘’Pets United’’, was released in 2019, which exclusively brought the sequel to Netflix. Plot. In the Okavango Delta, the annual flood has failed to arrive in the Delta. The water has become scarce and the native animals including a herd of rhinos and buffaloes, including Chino and Biggie, fiercely fight over it.

Geographic entities mentioned:
surface_form: Okavango Delta
instance_of: Body of water
Watercourse
countries: Botswana
coordinates: lat: -19.4
lon: 22.9
Maiden Pap, Caithness. The Maiden Pap is a hill located in Caithness, Scotland. It is an inselberg, formed of Devonian conglomerates, rising steeply out of the surrounding plain and visible from as far away as Hoy and the Moray Firth. The Pap is so named because its shape resembles that of a human breast.

Geographic entities mentioned:
surface_form: maiden pap
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.233333333333
lon: -3.6166666666667
The aqueduct is a scheduled ancient monument. The River Meese feeds the Aqualate Mere, which is a National Nature Reserve and the largest lake in the West Midlands region, covering. Soon afterwards, the route of the canal has been cut by the building of the A41 Newport bypass.

Geographic entities mentioned:
surface_form: Aqualate Mere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.7812
lon: -2.3392
Larvik Harbour. Larvik Harbor () is a small bay southwest of Lagrange Peak in southeastern Brabant Island, Palmer Archipelago, Antarctica. The bay was roughly charted by a British expedition, 1920–22, and so named after the town of Larvik in southern Norway, following the name usage of whalers (M.C. Lester's amendments to Captain Johans Johannessen's manuscript chart of about 1919–20).

Geographic entities mentioned:
surface_form: Lagrange Peak
instance_of: Mountain
coordinates: lat: -64.4667
lon: -62.4333
Kimsa Chata (Arequipa). Kimsa Chata (Aymara and Quechua &quot;kimsa&quot; three, Pukina &quot;chata&quot; mountain, &quot;three mountains&quot;, Hispanicized spelling &quot;Quimsachata&quot;) is a group of three mountains in the Wansu mountain range in the Andes of Peru. Its central peak reaches above sea level. It is situated in the Arequipa Region, La Unión Province, Huaynacotas District.

Geographic entities mentioned:
surface_form: kimsa chata
instance_of: Mountain
countries: Peru
coordinates: lat: -14.7042
lon: -72.7689
surface_form: kimsa chata
instance_of: Mountain
countries: Peru
coordinates: lat: -13.66
lon: -71.04638889
Kimsa Chata (Arequipa). Kimsa Chata (Aymara and Quechua &quot;kimsa&quot; three, Pukina &quot;chata&quot; mountain, &quot;three mountains&quot;, Hispanicized spelling &quot;Quimsachata&quot;) is a group of three mountains in the Wansu mountain range in the Andes of Peru. Its central peak reaches above sea level. It is situated in the Arequipa Region, La Unión Province, Huaynacotas District.

Geographic entities mentioned:
surface_form: kimsa chata
instance_of: Mountain
countries: Peru
coordinates: lat: -14.7042
lon: -72.7689
surface_form: quimsachata
instance_of: Mountain
countries: Peru
coordinates: lat: -13.66
lon: -71.04638889
surface_form: kimsa chata
instance_of: Mountain
countries: Peru
coordinates: lat: -13.66
lon: -71.04638889
Its central peak reaches above sea level. It is situated in the Arequipa Region, La Unión Province, Huaynacotas District. Kimsa Chata lies at the Yana Wanaku valley (&quot;black guanaco&quot;, &quot;Yanahuanaco&quot;) southeast of Hatun Pata.

Geographic entities mentioned:
surface_form: hatun pata
instance_of: Mountain
countries: Peru
coordinates: lat: -12.8583
lon: -75.2147
Furnace Creek Fault Zone. The Furnace Creek Fault Zone (FCFZ) is a geological fault that is located in Eastern California and southwestern Nevada. The right lateral-moving (dextral) fault extends for some between a connection with the Death Valley Fault Zone in the Amargosa Valley and northward to a termination in the Fish Lake Valley of southwest Nevada.

Geographic entities mentioned:
surface_form: Amargosa Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.6333
lon: -116.4
surface_form: Fish Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.6947
lon: -118.078
Oregon Route 6. Oregon Route 6 is a state highway in the U.S. state of Oregon that runs between the city of Tillamook on the Oregon Coast, to the Willamette Valley, near Banks. OR 6 traverses the Wilson River Highway No. 37 of the Oregon state highway system, named after the river paralleling the highway's western segment. Route description.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Before 1957, OR 6 included the entirety of today's Oregon Route 8, plus an additional stretch into downtown Portland. With the completion of the Sunset Highway (and the new alignment through Banks), the route through Gales Creek and the Tualatin Valley was renumbered as OR 8; and OR 6 was placed on the alignment it has today.

Geographic entities mentioned:
surface_form: Tualatin Valley
instance_of: Valley
countries: United States
coordinates: lat: 45.5106
lon: -122.989
Grenelle Mountain is a mountain summit located in British Columbia, Canada. Description. Grenelle Mountain is a glaciated peak situated in the Waddington Range of the Coast Mountains, in a remote wilderness area that few visit. Grenelle Mountain is set north of the community of Campbell River and southeast of Mount Waddington, the highest peak of the entire Coast Mountains range.

Geographic entities mentioned:
surface_form: Mount Waddington
instance_of: Mountain
countries: Canada
coordinates: lat: 51.373611111111
lon: -125.26333333333
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: grenelle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.321111111111115
lon: -125.13861111111112
Grenelle Mountain is set north of the community of Campbell River and southeast of Mount Waddington, the highest peak of the entire Coast Mountains range. Other neighbors between Waddington and Grenelle include Spearman Peak, Mount Munday, Arabesque Peaks and Bravo Peak. Precipitation runoff and glacier meltwater from Grenelle Mountain drains to Bute Inlet via the Homathko River.

Geographic entities mentioned:
surface_form: Spearman Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3594
lon: -125.2434
surface_form: Mount Munday
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3286
lon: -125.216
surface_form: Bravo Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3664
lon: -125.2364
Grenelle Mountain. Grenelle Mountain is a mountain summit located in British Columbia, Canada. Description. Grenelle Mountain is a glaciated peak situated in the Waddington Range of the Coast Mountains, in a remote wilderness area that few visit.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: grenelle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.321111111111115
lon: -125.13861111111112
Grenelle Mountain. Grenelle Mountain is a mountain summit located in British Columbia, Canada. Description. Grenelle Mountain is a glaciated peak situated in the Waddington Range of the Coast Mountains, in a remote wilderness area that few visit.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: grenelle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.321111111111115
lon: -125.13861111111112
Grenelle Mountain is a mountain summit located in British Columbia, Canada. Description. Grenelle Mountain is a glaciated peak situated in the Waddington Range of the Coast Mountains, in a remote wilderness area that few visit. Grenelle Mountain is set north of the community of Campbell River and southeast of Mount Waddington, the highest peak of the entire Coast Mountains range.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: grenelle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.321111111111115
lon: -125.13861111111112
Other neighbors between Waddington and Grenelle include Spearman Peak, Mount Munday, Arabesque Peaks and Bravo Peak. Precipitation runoff and glacier meltwater from Grenelle Mountain drains to Bute Inlet via the Homathko River. Topographic relief is significant as the summit rises 1,500 meters (4,920 feet) above the Tiedemann Glacier in two kilometers (1.2 mile). History.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: grenelle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.321111111111115
lon: -125.13861111111112
Topographic relief is significant as the summit rises 1,500 meters (4,920 feet) above the Tiedemann Glacier in two kilometers (1.2 mile). History. The name &quot;Crenelle Mountain&quot; was originally submitted in January 1928 by mountaineer Don Munday and officially adopted 19 December 1968. Munday so-named it because of its likeness to crenelles and battlements.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Munday so-named it because of its likeness to crenelles and battlements. The spelling &quot;Grenelle&quot;, although misconstrued, is firmly entrenched in the mountaineering community, according to April 1978 advice from Dr. Glenn Woodsworth, Geological Survey of Canada and Alpine Club of Canada representative to the Geographical Names Board of Canada.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Climate. Based on the Köppen climate classification, Grenelle Mountain has an ice cap climate. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: grenelle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.321111111111115
lon: -125.13861111111112
As a result, the Coast Mountains experience high precipitation, especially during the winter months in the form of snowfall. Temperatures can drop below −20 °C with wind chill factors  below −30 °C. This climate supports the Waddington, Splendour and Tiedemann glaciers which cover the slopes of Grenelle Mountain.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: grenelle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.321111111111115
lon: -125.13861111111112
Nashornkalvane Rocks. zzt7r1k98foeqtw8jvugxphakiii" xml:space="preserve">Nashornkalvane Rocks () is a group of rocks 2 nautical miles (3.7 km) north of Nashornet Mountain, at the south side of the mouth of Viddalen Valley in Queen Maud Land.

Geographic entities mentioned:
surface_form: Nashornet Mountain
instance_of: Mountain
coordinates: lat: -72.3667
lon: -2
surface_form: Viddalen Valley
instance_of: Valley
coordinates: lat: -72.3333
lon: -2.75
surface_form: nashornkalvane
instance_of: Mountain
coordinates: lat: -72.3167
lon: -1.93333
Nashornkalvane Rocks. zzt7r1k98foeqtw8jvugxphakiii" xml:space="preserve">Nashornkalvane Rocks () is a group of rocks 2 nautical miles (3.7 km) north of Nashornet Mountain, at the south side of the mouth of Viddalen Valley in Queen Maud Land.

Geographic entities mentioned:
surface_form: nashornkalvane rocks
instance_of: Mountain
coordinates: lat: -72.3167
lon: -1.93333
Mapped by Norwegian cartographers from surveys and air photos by Norwegian-British-Swedish Antarctic Expedition (NBSAE) (1949–52) and air photos by the Norwegian expedition (1958–59) and named Nashornkalvane (the rhinoceros' calves).

Geographic entities mentioned:
surface_form: nashornkalvane
instance_of: Mountain
coordinates: lat: -72.3167
lon: -1.93333
Geography. Located in Kyrgyzstan's eastern corner, the district borders in the north with the Almaty Region of Kazakhstan, and in the east, with the Aksu Prefecture of China's Xinjiang Uyghur Autonomous Region. Two of Kyrgyzstan's highest mountains, Jengish Chokusu (Victory Peak, or Pobeda Peak in Russian) and Khan Tengri, are located on these borders.

Geographic entities mentioned:
surface_form: Jengish Chokusu
instance_of: Mountain
countries: Kyrgyzstan
People's Republic of China
coordinates: lat: 42.034662
lon: 80.128713
surface_form: Khan Tengri
instance_of: Mountain
countries: Kyrgyzstan
Kazakhstan
People's Republic of China
Russian Empire
Soviet Union
coordinates: lat: 42.210833333333
lon: 80.175
The maximum expected wind speed (once in 20-year period) is 34 m/s. Tourism. The Ak-Suu district is an important hub for Kyrgyzstan's adventure tourism industry centred on Karakol, most notably trekking to lake Ala-Köl and the newly-established Ak-Suu Traverse, a multi-day trek which typically takes between seven and nine days to complete. Demographics.

Geographic entities mentioned:
surface_form: Ala-Köl
instance_of: Lake
countries: Kyrgyzstan
coordinates: lat: 42.3175
lon: 78.535555555556
Le Cheval Blanc (mountain). Le Cheval Blanc is a mountain in the Chablais Alps on the Swiss-French border. It overlooks the lake of Vieux Emosson on its eastern side.

Geographic entities mentioned:
surface_form: cheval blanc
instance_of: Mountain
countries: Switzerland
France
coordinates: lat: 46.0519
lon: 6.87278
surface_form: le cheval blanc
instance_of: Mountain
countries: Switzerland
France
coordinates: lat: 46.0519
lon: 6.87278
It has been promoted particularly in academic contexts, such as at Makerere University. However, a fully unified orthography for Runyakitara has yet to be developed and widely adopted. In south-central Uganda, the Bantu languages of Luganda and Lusoga are largely interintelligible as well. This dialectic similarity also extends to the Lussese language spoken in the Ssese Islands of Lake Victoria.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
She moved permanently to London in her career as an artist. Her associates included Edith Anna Somerville, Violet Florence Martin, Lady Gregory, W.B. and Jack Yeats, Frances Perkins, Ethel Smyth. Her brother Francis died in a tragic drowning accident on Lough Corrib in August 1887. Her surviving brother, Captain Richard Kinkead, R.A.M.C., was killed in action at Ypres on 30 October 1914.

Geographic entities mentioned:
surface_form: Lough Corrib
instance_of: Lake
countries: Ireland
coordinates: lat: 53.466666666667
lon: -9.2833333333333
Rajmahal hills. The Rajmahal Hills are located in the Santhal Pargana division of Jharkhand, India. They were located on the northern margin of the Gondwana supercontinent, and its hills are today inhabited by the Sauria Paharia people whilst its valleys are dominated by the Santhal people. The hills span over an area of.

Geographic entities mentioned:
surface_form: hills
instance_of: Mountain
countries: India
coordinates: lat: 23.166666666667
lon: 92.833333333333
surface_form: rajmahal hills
instance_of: Mountain
countries: India
coordinates: lat: 25
lon: 87
Rajmahal hills. The Rajmahal Hills are located in the Santhal Pargana division of Jharkhand, India. They were located on the northern margin of the Gondwana supercontinent, and its hills are today inhabited by the Sauria Paharia people whilst its valleys are dominated by the Santhal people. The hills span over an area of.

Geographic entities mentioned:
surface_form: hills
instance_of: Mountain
countries: India
coordinates: lat: 23.166666666667
lon: 92.833333333333
The Rajmahal Hills are located in the Santhal Pargana division of Jharkhand, India. They were located on the northern margin of the Gondwana supercontinent, and its hills are today inhabited by the Sauria Paharia people whilst its valleys are dominated by the Santhal people. The hills span over an area of. Volcanic activity during the Jurassic resulted in the formation of the Rajmahal Traps.

Geographic entities mentioned:
surface_form: hills
instance_of: Mountain
countries: India
coordinates: lat: 23.166666666667
lon: 92.833333333333