Sarmila/GeoWiki-Features huggingface dataset:
Cam Spout Crag is a rock climbing location, although not a particularly busy one, with 12 climbs including Cam Spout Buttress and Eskdale Grooves. Ascents. One possible ascent of Slight Side is from Eskdale and this is often completed in conjunction with Scafell, and possibly Scafell Pike as well. The ascent may be started at the hamlet of Boot.

Geographic entities mentioned:
surface_form: Scafell Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454166666667
lon: -3.2115277777778
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.478
lon: -0.786
surface_form: scafell pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454166666667
lon: -3.2115277777778
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.189
lon: -3.068
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
Slight Side is steep and craggy on all sides except to the north where the ridge runs to Scafell. The eastern flank falls to the valley of the infant River Esk while the slopes to the west descend across Eskdale Fell towards Burnmoor Tarn. Horn Crag stands to the south of the summit overlooking Eskdale.

Geographic entities mentioned:
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.478
lon: -0.786
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.189
lon: -3.068
surface_form: burnmoor tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.428617
lon: -3.259844
The eastern flank falls to the valley of the infant River Esk while the slopes to the west descend across Eskdale Fell towards Burnmoor Tarn. Horn Crag stands to the south of the summit overlooking Eskdale. Just under a kilometre to the north past the 748m col is Long Green which is the summit of Cam Spout crags.

Geographic entities mentioned:
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.478
lon: -0.786
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.189
lon: -3.068
Just under a kilometre to the north past the 748m col is Long Green which is the summit of Cam Spout crags. When viewed from a distance (see picture) or even when walking, Long Green can be mistaken for the summit of Slight Side. Cam Spout Crag is a rock climbing location, although not a particularly busy one, with 12 climbs including Cam Spout Buttress and Eskdale Grooves. Ascents.

Geographic entities mentioned:
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.478
lon: -0.786
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.189
lon: -3.068
The ascent may be started at the hamlet of Boot. It takes the path which passes Eel Tarn and Stony Tarn before crossing bouldery ground to climb the broad ridge to the summit. Scafell stands to the north and is reached by a vertical ascent of. The fell can be bagged with little effort while descending to Eskdale from Scafell by the southern ridge. Summit.

Geographic entities mentioned:
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.478
lon: -0.786
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.189
lon: -3.068
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
Summit. The summit of Slight Side is a fine rocky peak and is listed by Alfred Wainwright as one of the six best summits in the Lake District, calling it &quot;“rocky, shapely, well defined and can be attained only by a rough final scramble”&quot;. The highlight of the view from the summit is the vista westward towards the sea.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Slight Side. Slight Side is a fell in the English Lake District it stands east southeast of the town of Whitehaven and reaches a height of. Slight Side lies at the south western edge of the Scafell Massif, a crescent of high ground which includes the highest ground in England.

Geographic entities mentioned:
surface_form: slight side
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4342
lon: -3.22095
Slight Side. Slight Side is a fell in the English Lake District it stands east southeast of the town of Whitehaven and reaches a height of. Slight Side lies at the south western edge of the Scafell Massif, a crescent of high ground which includes the highest ground in England.

Geographic entities mentioned:
surface_form: slight side
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4342
lon: -3.22095
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
Topography. When viewed from the valley of Eskdale the fell is seen as a distinct peak but in reality it is just the terminal point on Scafell’s southern ridge before it descends steeply to Eskdale. It only has of topographic prominence between itself and Scafell (the col is at) and therefore Slight Side narrowly fails to qualify as a Nuttall hill or a Hewitt.

Geographic entities mentioned:
surface_form: slight side
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4342
lon: -3.22095
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
It only has of topographic prominence between itself and Scafell (the col is at) and therefore Slight Side narrowly fails to qualify as a Nuttall hill or a Hewitt. It was left to Alfred Wainwright to give Slight Side the status of a separate fell in his Pictorial Guide to the Lakeland Fells. Slight Side is steep and craggy on all sides except to the north where the ridge runs to Scafell.

Geographic entities mentioned:
surface_form: slight side
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4342
lon: -3.22095
surface_form: slight side
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4342
lon: -3.22095
Just under a kilometre to the north past the 748m col is Long Green which is the summit of Cam Spout crags. When viewed from a distance (see picture) or even when walking, Long Green can be mistaken for the summit of Slight Side. Cam Spout Crag is a rock climbing location, although not a particularly busy one, with 12 climbs including Cam Spout Buttress and Eskdale Grooves. Ascents.

Geographic entities mentioned:
surface_form: slight side
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4342
lon: -3.22095
It was left to Alfred Wainwright to give Slight Side the status of a separate fell in his Pictorial Guide to the Lakeland Fells. Slight Side is steep and craggy on all sides except to the north where the ridge runs to Scafell. The eastern flank falls to the valley of the infant River Esk while the slopes to the west descend across Eskdale Fell towards Burnmoor Tarn.

Geographic entities mentioned:
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
Silver Peak (El Dorado County, California). Silver Peak is a mountain in the Sierra Nevada mountain range at the north end of the Crystal Mountains, to the east of Lake Tahoe. It is located in the Desolation Wilderness in El Dorado County, California.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: silver peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.564166666667
lon: -119.76027777778
surface_form: silver peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.361111111111
lon: -121.46166666667
surface_form: silver peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.9346
lon: -120.23
surface_form: silver peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.470277777778
lon: -119.02083333333
surface_form: silver peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.845555555556
lon: -114.53777777778
Silver Peak (El Dorado County, California). Silver Peak is a mountain in the Sierra Nevada mountain range at the north end of the Crystal Mountains, to the east of Lake Tahoe. It is located in the Desolation Wilderness in El Dorado County, California.

Geographic entities mentioned:
surface_form: silver peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.564166666667
lon: -119.76027777778
surface_form: silver peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.361111111111
lon: -121.46166666667
surface_form: silver peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.9346
lon: -120.23
surface_form: silver peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.470277777778
lon: -119.02083333333
surface_form: silver peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.845555555556
lon: -114.53777777778
Roberts Ice Piedmont. Roberts Ice Piedmont () is a large ice piedmont, 20 nautical miles (37 km) long in a north–south direction and 15 nautical miles (28 km) wide, lying to the north and northwest of Mount Calais and occupying most of the northeast corner of Alexander Island, Antarctica.

Geographic entities mentioned:
surface_form: Mount Calais
instance_of: Mountain
coordinates: lat: -69.1833
lon: -70.25
Roberts (1912–78), a British ornithologist, polar specialist and leading figure in the development of Antarctic nomenclature; ornithologist, BGLE, 1934–37; Secretary, United Kingdom Antarctic Place-names Committee, 1945–74. About six nunataks are situated within the Roberts Ice Piedmont, these are Hengist Nunatak (a separate nunatak) and the Horsa Nunataks (a group of about five nunataks).

Geographic entities mentioned:
surface_form: Hengist Nunatak
instance_of: Mountain
coordinates: lat: -69
lon: -70.2333
surface_form: Horsa Nunataks
instance_of: Mountain
coordinates: lat: -68.9333
lon: -70.3
Manych Ship Canal. The Manych Ship Canal is a canal between the Black Sea lagoon the Sea of Azov and the Caspian Sea. , proposals were being considered to turn it into a larger canal known as the Eurasia Canal. If built, this would be a multipurpose water-resources system and a limb of international transport. A proposed design would deepen the canal to and widen it to.

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
The Volga–Don Canal, constructed in the 1950s, is approaching its traffic capacity limit of 14.8 million tons. The Eurasia concept is one of a few extra or expanded canals being considered between the basins of Azov–Black and Caspian Seas to improve ease and speed of commerce.

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
The Eurasia concept is one of a few extra or expanded canals being considered between the basins of Azov–Black and Caspian Seas to improve ease and speed of commerce. The -long Manych Ship Canal includes the existing Manych Waterway through Lake Manych-Gudilo and the Veselovskoe and Proletarskoe reservoirs and could be extended to the Caspian Sea via the sparsely populated steppes of Kalmykia.

Geographic entities mentioned:
surface_form: Lake Manych-Gudilo
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 46.316666666667
lon: 42.866666666667
On their journey, they used the ancient river routes of what is now northern Russia. Some of these peoples, who may have originally spoken the same western Uralic language, stopped and stayed in the regions between Karelia, Ladoga and Lake Ilmen, and even further to the east and to the southeast.

Geographic entities mentioned:
surface_form: Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
surface_form: Lake Ilmen
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 58.266666666667
lon: 31.283333333333
The groups of these peoples that ended up in the Finnish Lakeland from 1600 to 1500 BC later &quot;became&quot; the Sámi. The Sámi people arrived in their current homeland some time during the Bronze Age or early Iron Age. The Sámi language first developed on the southern side of Lake Onega and Lake Ladoga and spread from there.

Geographic entities mentioned:
surface_form: Lake Onega
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
For centuries, the Sámi and the Scandinavians had relatively little contact; the Sámi primarily lived in the inland of northern Fennoscandia, while Scandinavians lived in southern Scandinavia and gradually colonised the Norwegian coast; from the 18th and especially the 19th century, the governments of Norway and Sweden started to assert sovereignty more aggressively in the north, and targeted the Sámi with Scandinavization policies aimed at forced assimilation from the 19th century.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
This hypothesis is still accepted among many historians, but has been the subject of scholarly debate in the 21st century. In recent years, several archaeological finds indicate a Sámi presence in southern Norway in the Middle Ages, and in southern Sweden, including finds in Lesja Municipality, in Vang Municipality, in Valdres and in Hol Municipality and Ål Municipality in Hallingdal.

Geographic entities mentioned:
surface_form: Valdres
instance_of: Valley
countries: Norway
coordinates: lat: 60.916666666667
lon: 9.1666666666667
surface_form: Hallingdal
instance_of: Valley
countries: Norway
coordinates: lat: 60.633333333333
lon: 9.05
Cultural region. Sápmi is located in Northern Europe, includes the northern parts of Fennoscandia and spans four countries: Norway, Sweden, Finland, and Russia. Non-Sámi and many regional maps have often called this same region &quot;Lapland&quot; as there is considerable regional overlap between Sápmi and the provinces of Lappland in Sweden and Lapland in Finland.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Bridge Brook Pond. Bridge Brook Pond is located southeast of Mount Arab, New York. Fish species present in the lake are white sucker, brook trout, and black bullhead. There is trail access from the west shore of Tupper Lake.

Geographic entities mentioned:
surface_form: tupper lake
instance_of: Lake
countries: United States
coordinates: lat: 44.17
lon: -74.54
Bridge Brook Pond. Bridge Brook Pond is located southeast of Mount Arab, New York. Fish species present in the lake are white sucker, brook trout, and black bullhead. There is trail access from the west shore of Tupper Lake.

Geographic entities mentioned:
surface_form: bridge brook pond
instance_of: Lake
countries: United States
coordinates: lat: 44.16336
lon: -74.58359
Bridge Brook Pond. Bridge Brook Pond is located southeast of Mount Arab, New York. Fish species present in the lake are white sucker, brook trout, and black bullhead. There is trail access from the west shore of Tupper Lake.

Geographic entities mentioned:
surface_form: bridge brook pond
instance_of: Lake
countries: United States
coordinates: lat: 44.16336
lon: -74.58359
surface_form: mount arab
instance_of: Mountain
countries: United States
coordinates: lat: 44.204166666667
lon: -74.585277777778
It first appeared in a short story by J. K. Rowling in 2016, and was subsequently depicted in the film &quot;Fantastic Beasts and Where to Find Them&quot;. The school was founded in the seventeenth century by Isolt Sayre in Adams, Massachusetts. It is located on Mount Greylock and is concealed from Muggles with enchantments. Like Hogwarts, Ilvermorny is divided into four houses.

Geographic entities mentioned:
surface_form: Mount Greylock
instance_of: Mountain
countries: United States
coordinates: lat: 42.6375
lon: -73.166666666667
The conservation park consisted of land in section 535 in the cadastral unit of the Hundred of Onkaparinga, located to the east of the Mount Lofty Summit Road about south of the summit of Mount Lofty and bounded on its northern boundary by the Cleland Conservation Park. It was proclaimed under the &quot;National Parks and Wildlife Act 1972&quot; on 22 September 1977.

Geographic entities mentioned:
surface_form: Mount Lofty
instance_of: Mountain
countries: Australia
coordinates: lat: -34.966666666667
lon: 138.7
Martinsburg, Pennsylvania. Martinsburg is a borough in the Morrisons Cove section of Blair County, Pennsylvania, United States. The population was 1,874 at the 2020 census. It is part of the Altoona, PA Metropolitan Statistical Area. History. The community was named after John Martin, a pioneer citizen. Geography.

Geographic entities mentioned:
surface_form: Morrisons Cove
instance_of: Landform
countries: United States
coordinates: lat: 40.2492
lon: -78.3358
Cameron River. The Cameron River is a river of New Zealand. It flows southeast from the slopes of Mount Arrowsmith in the Kā Tiritiri o te Moana, reaching Lake Stream just to the north of the outflow from Lake Heron. The longer Hakatere flows roughly parallel to the Cameron River, some to the southwest.

Geographic entities mentioned:
surface_form: Lake Heron
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.479166666667
lon: 171.17194444444
It rises to an altitude of 1,167 meters. Geology. With its twin, the Puy de Lassolas, they form two monogenetic volcanoes, meaning they were born from a single eruptive episode of Strombolian type. They form two scoria cones, ranging in color from red (for those exposed to the heat of the crater, which favored their oxidation) to black.

Geographic entities mentioned:
surface_form: Puy de Lassolas
instance_of: Mountain
countries: France
coordinates: lat: 45.71166
lon: 2.95828
Puy de la Vache. The Puy de la Vache is a basaltic volcano in the Chaîne des Puys, in the Massif Central of France. Topography. The Puy de la Vache is located in the municipality of Saint-Genès-Champanelle, southwest of Clermont-Ferrand. It rises to an altitude of 1,167 meters. Geology.

Geographic entities mentioned:
surface_form: puy de la vache
instance_of: Mountain
countries: France
coordinates: lat: 45.7054
lon: 2.96335
Cat Law. Cat Law (671 m) is a hill in the southern Mounth of Scotland, north of Kirriemuir in Angus. A rounded peak, it lies above Strathmore in the south and offers excellent views across the Angus countryside from its summit. It is usually climbed from the nearby village of Balintore.

Geographic entities mentioned:
surface_form: strathmore
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.717
lon: -3.549
surface_form: strathmore
instance_of: Valley
countries: United Kingdom
coordinates: lat: 58.376388888889
lon: -4.64
Cat Law. Cat Law (671 m) is a hill in the southern Mounth of Scotland, north of Kirriemuir in Angus. A rounded peak, it lies above Strathmore in the south and offers excellent views across the Angus countryside from its summit. It is usually climbed from the nearby village of Balintore.

Geographic entities mentioned:
surface_form: cat law
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.716666666667
lon: -3.1
Shichirigahama. is a beach near Kamakura, Kanagawa Prefecture, Japan, which goes from Koyurugimisaki Cape, near Fujisawa, to Inamuragasaki Cape, west of Kamakura. Since from it one could enjoy a clear view of both Mount Fuji and Enoshima at the same time, during the Edo period it was popular as a subject for &quot;ukiyo-e&quot;.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
Eastern and northern Britain were settled by groups wearing cruciform brooches, of the style in fashion at the time in coastal Scandinavia, Denmark, and Schleswig-Holstein south to the lower Elbe and east to the Oder, as well as a pocket in coastal Friesland. Later history. After the Angles departed from Angeln, by the 8th century the region was occupied by Danes.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Rinker Peak. Rinker Peak is a mountain summit in Chaffee County, Colorado, United States. Description. Rinker Peak is set approximately east of the Continental Divide in the Collegiate Peaks which are a subrange of the Sawatch Range. The mountain is located southwest of Twin Lakes on land managed by San Isabel National Forest. It ranks as the 114th-highest summit in Colorado.

Geographic entities mentioned:
surface_form: Collegiate Peaks
instance_of: Landform
countries: United States
coordinates: lat: 38.9244
lon: -106.321
surface_form: rinker peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.036666666667
lon: -106.43972222222
Precipitation runoff from the mountain's slopes drains into Lake Creek which is a tributary of the Arkansas River. Topographic relief is significant as the summit rises above Lake Creek in. The highest peak in Colorado, Mount Elbert, is to the north of Rinker. An ascent of Rinker Peak involves eight miles of hiking with 4,700-feet of elevation gain. Etymology.

Geographic entities mentioned:
surface_form: Mount Elbert
instance_of: Mountain
countries: United States
coordinates: lat: 39.1175
lon: -106.44527777778
Rinker Peak. Rinker Peak is a mountain summit in Chaffee County, Colorado, United States. Description. Rinker Peak is set approximately east of the Continental Divide in the Collegiate Peaks which are a subrange of the Sawatch Range. The mountain is located southwest of Twin Lakes on land managed by San Isabel National Forest. It ranks as the 114th-highest summit in Colorado.

Geographic entities mentioned:
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 27.893888888889
lon: -81.594722222222
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 43.4834018
lon: -74.9490486
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 37.6181
lon: -119.008
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 44.8079
lon: -118.0867
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 40.7433
lon: -115.283
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.0183
lon: -73.3867
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 45.23888889
lon: -111.86472222
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 60.638888888889
lon: -153.86305555556
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 48.6494
lon: -113.718
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 45.7487796
lon: -84.4527626
surface_form: twin lakes
instance_of: Lake
countries: United States
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 44.6375
lon: -89.41583333333334
Rinker Peak. Rinker Peak is a mountain summit in Chaffee County, Colorado, United States. Description. Rinker Peak is set approximately east of the Continental Divide in the Collegiate Peaks which are a subrange of the Sawatch Range. The mountain is located southwest of Twin Lakes on land managed by San Isabel National Forest. It ranks as the 114th-highest summit in Colorado.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: rinker peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.036666666667
lon: -106.43972222222
Rinker Peak. Rinker Peak is a mountain summit in Chaffee County, Colorado, United States. Description. Rinker Peak is set approximately east of the Continental Divide in the Collegiate Peaks which are a subrange of the Sawatch Range. The mountain is located southwest of Twin Lakes on land managed by San Isabel National Forest. It ranks as the 114th-highest summit in Colorado.

Geographic entities mentioned:
surface_form: rinker peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.036666666667
lon: -106.43972222222
Precipitation runoff from the mountain's slopes drains into Lake Creek which is a tributary of the Arkansas River. Topographic relief is significant as the summit rises above Lake Creek in. The highest peak in Colorado, Mount Elbert, is to the north of Rinker. An ascent of Rinker Peak involves eight miles of hiking with 4,700-feet of elevation gain. Etymology.

Geographic entities mentioned:
surface_form: rinker peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.036666666667
lon: -106.43972222222
Climate. According to the Köppen climate classification system, Rinker Peak is located in an alpine subarctic climate zone with cold, snowy winters, and cool to warm summers. Due to its altitude, it receives precipitation all year, as snow in winter and as thunderstorms in summer, with a dry period in late spring.

Geographic entities mentioned:
surface_form: rinker peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.036666666667
lon: -106.43972222222
Grafton, Nova Scotia. Grafton is a small farming community in the Annapolis Valley area of Kings County, Nova Scotia, Canada. Located just north of the village of Waterville, it stretches from the Cornwallis River to the slopes of the North Mountain and includes the crossroads of Buckleys Corner. Route 221 crosses the north part of Grafton while Highway 101 crosses the south part of the community.

Geographic entities mentioned:
surface_form: Annapolis Valley
instance_of: Valley
countries: Canada
coordinates: lat: 44.979166666666664
lon: -64.89222222222222
The entire route is part of the National Highway System. History. When the Cache Valley was settled and developed in the 19th century, the north&ndash;south road through the eastern part of the valley connected all the towns, including Hyrum, Providence, Logan, Hyde Park, and Smithfield.

Geographic entities mentioned:
surface_form: Cache Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.816666666667
lon: -111.93416666667
Mount Carleton. Mount Carleton (), at, is the highest peak in the Canadian province of New Brunswick, and the Maritime Provinces. Located in Mount Carleton Provincial Park, it is one of the highlights of the Canadian portion of the International Appalachian Trail. Mount Carleton is also part of the eighth and final section of the Nepisiguit Mi'gmaq Trail.

Geographic entities mentioned:
surface_form: nepisiguit
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.5559
lon: -65.6652
surface_form: mount carleton
instance_of: Mountain
countries: Canada
coordinates: lat: 47.3833
lon: -66.8833
Mount Carleton. Mount Carleton (), at, is the highest peak in the Canadian province of New Brunswick, and the Maritime Provinces. Located in Mount Carleton Provincial Park, it is one of the highlights of the Canadian portion of the International Appalachian Trail. Mount Carleton is also part of the eighth and final section of the Nepisiguit Mi'gmaq Trail.

Geographic entities mentioned:
surface_form: mount carleton
instance_of: Mountain
countries: Canada
coordinates: lat: 47.3833
lon: -66.8833
Mount Carleton is a monadnock, an erosional remnant of resistant igneous rocks that remained after an ancient Mesozoic peneplain surface was uplifted in the Cenozoic to form a plateau, and subsequently dissected via millions of years of erosion by wind, water and glacial ice. It consists of 400 million-year-old rhyolitic and basaltic volcanics.

Geographic entities mentioned:
surface_form: mount carleton
instance_of: Mountain
countries: Canada
coordinates: lat: 47.3833
lon: -66.8833
Mount Carleton is also part of the eighth and final section of the Nepisiguit Mi'gmaq Trail. The mountain was named after Thomas Carleton, New Brunswick's first lieutenant governor, and forms part of the Notre Dame Mountains chain, which is visible on Map 24 of the NB Atlas.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Before aerial surveillance was extensively used, a hut was maintained on the summit for fire-spotting in the remote north-central part of the province. A very similar hut was maintained on Big Bald Mountain. Triangulation among these huts and other fire towers allowed the locations of wildfires to be determined quickly and easily.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: big bald mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 47.195
lon: -66.4228
Nodales Channel. Nodales Channel is a channel along the coast of British Columbia, Canada. It is located between East Thurlow Island and Sonora Island, in the Discovery Islands archipelago between Vancouver Island and the mainland coast, north of the Salish Sea.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: nodales channel
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.39883
lon: -125.33555
Nodales Channel. Nodales Channel is a channel along the coast of British Columbia, Canada. It is located between East Thurlow Island and Sonora Island, in the Discovery Islands archipelago between Vancouver Island and the mainland coast, north of the Salish Sea.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
Nodales Channel connects to Cordero Channel and Frederick Arm, to the northeast, and to the junction of Discovery Passage and Johnstone Strait, to the southwest. The channel features Hemming Bay on the northern East Thurlow Island side.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
The channel features Hemming Bay on the northern East Thurlow Island side. Thurston Bay is on the southern Sonora Island side, near a cluster of bays, Binnington Bay, Handfield Bay, and Cameleon Harbour, in a small inlet connected to Nodales Channel by Burgess Passage and Young Passage. Thurston Bay Marine Park is located on Davis Point, between Thurston Bay and Nodales Channel.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: nodales channel
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.39883
lon: -125.33555
Nodales Channel. Nodales Channel is a channel along the coast of British Columbia, Canada. It is located between East Thurlow Island and Sonora Island, in the Discovery Islands archipelago between Vancouver Island and the mainland coast, north of the Salish Sea.

Geographic entities mentioned:
surface_form: nodales channel
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.39883
lon: -125.33555
It is located between East Thurlow Island and Sonora Island, in the Discovery Islands archipelago between Vancouver Island and the mainland coast, north of the Salish Sea. Nodales Channel connects to Cordero Channel and Frederick Arm, to the northeast, and to the junction of Discovery Passage and Johnstone Strait, to the southwest.

Geographic entities mentioned:
surface_form: nodales channel
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.39883
lon: -125.33555
The channel features Hemming Bay on the northern East Thurlow Island side. Thurston Bay is on the southern Sonora Island side, near a cluster of bays, Binnington Bay, Handfield Bay, and Cameleon Harbour, in a small inlet connected to Nodales Channel by Burgess Passage and Young Passage. Thurston Bay Marine Park is located on Davis Point, between Thurston Bay and Nodales Channel.

Geographic entities mentioned:
surface_form: nodales channel
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.39883
lon: -125.33555
He primarily worked as a cinematographer on Norwegian films, in addition to occasionally working as a director and producer. At the end of his career he established his own film production company. Ski jumping. In 1934, Per Jonson participated in an international competition at the Bloudek Giant in Planica, making a jump long. In another jump, outside the competition, he landed at with a fall.

Geographic entities mentioned:
surface_form: Planica
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.476944444444
lon: 13.722222222222
News on the conclusion of the preliminary peace treaty reached Vienna on 7 September, but it was too late for reversal. On 18 September, the final peace Treaty of Belgrade was signed, thus confirming Habsburg loss of Wallachia Minor (Oltenia), central Serbia with Belgrade, and the Bosnian section of Posavina.

Geographic entities mentioned:
surface_form: Posavina
instance_of: Valley
countries: Croatia
Bosnia and Herzegovina
Serbia
coordinates: lat: 45.16667
lon: 17.33333
Pukara culture. The Pucará culture was an archaeological culture which developed in Qullaw, along the north-western shore of Lake Titicaca. It was characterized by a hierarchy of smaller centers and villages scattered throughout the northern basin of the Titicaca. The name originates from the town of Pukara, one of the largest settlements in the region.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
The Karasor Basin includes a Important Bird Area. Geography. The Karasor Depression is an endorheic basin in the Kazakh Uplands. It extends roughly from east to west for a length of approximately to the southeast of the Ayr and Zheltau ranges, and north of the Karkaraly Range and the Kyzyltas. Fourteen rivers flow into the basin, the largest of which are the long Taldy and the long Zharly.

Geographic entities mentioned:
surface_form: Kyzyltas
instance_of: Mountain
countries: Kazakhstan
coordinates: lat: 49
lon: 74.733333333333
Most rivers and rivulets flow only following the melting of the snows, breaking up into disconnected pools or drying out completely during the summer. Karasor, the largest lake, lies in a central position at the bottom of the depression. There are three other major lakes in the basin, Saumalkol, Katynkol and Balyktykol, as well as numerous smaller lakes and sors.

Geographic entities mentioned:
surface_form: Karasor
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 49.84889
lon: 75.35222
Karasor, the largest lake, lies in a central position at the bottom of the depression. There are three other major lakes in the basin, Saumalkol, Katynkol and Balyktykol, as well as numerous smaller lakes and sors. The water of all the lakes is saline; Saumalkol in the west is a dead lake, having the highest salt concentration, while Balyktykol has the lowest.

Geographic entities mentioned:
surface_form: Katynkol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 49.73916666666667
lon: 75.15833333333335
She also lost her home. Following the destruction she ended at Oberlößnitz which by this time had been subsumed - formally in 1934 - into Radebeul, a short distance down-river from Dresden, where she made her home at Eduard-Bilz-Straße 42, and where she lived for the rest of her life, in a home that was large enough to incorporate the little studio in which she now worked.

Geographic entities mentioned:
surface_form: river
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
History. Construction started on the George side of the pass in 1908. Ten tons of explosives were used to break up the hard Table Mountain quartzite, seven tunnels were built into the rock, and a workforce of 2,500 worked on the project. The railway covered a 1:40 grade in some areas of the 34-km pass, completed in 1913. It shortened the route from Port Elizabeth to Cape Town by 267 km. The route.

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
There are secondary schools in Sumiswald and Wasen as well as a retirement home. Geography. Sumiswald consists of three villages (Sumiswald, Grünen and Wasen), two hamlets (Gammenthal and Griesbach) and scattered farm houses and alpine meadows in the lower Emmental. It is one of the largest municipalities in the canton. Sumiswald has an area of.

Geographic entities mentioned:
surface_form: Emmental
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.91922
lon: 7.77868
Life. Nothing is known of Callistus' early life. He was a disciple of Gregory Palamas and Gregory of Sinai. He lived at Mount Athos for 28 years and was a monk at the Skete of Magoula near Philotheou Monastery at Mount Athos. In his &quot;Hagiography of Gregory of Sinai&quot;, he mentions two devotees, Jakov of Serres and Romylos of Vidin, then living and writing in Serbia.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
While Callistus I was Patriarch, he once passed through Mount Athos on his way to Serbia and met Maximos of Kafsokalyvia, who greeted the Patriarch in a humorous manner, &quot;This old man will never see his old lady again&quot;. This turned out to be a prophecy of how Callistus I would never see Constantinople (&quot;his old lady&quot;) again, since he would die before being able to return there.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Geography and geology. The &quot;Wiesbach&quot; along with the &quot;Appelbach&quot;, drains the northwestern area of Rhenish Hesse. Its source region lies in the North Palatine Uplands, the northern outliers of the precipitation-rich Donnersberg massif, west of Haide in the borough of Kirchheimbolanden.

Geographic entities mentioned:
surface_form: Donnersberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.625280555556
lon: 7.9147194444444
This side branch joins the main river just before Grolsheim. The stream flows through Oberwiesen, Nieder-Wiesen and Wendelsheim, passing there the Teufelsrutsch (&quot;Devil’s Slide&quot;) and unites with the &quot;Finkenbach&quot;. It subsequently flows through (a district of Flonheim), Flonheim, Armsheim, (a district of Armsheim) and Wallertheim, on the eastern edge of which it is joined by the.

Geographic entities mentioned:
surface_form: Teufelsrutsch
instance_of: Mountain
countries: Germany
coordinates: lat: 49.7485
lon: 7.97929
Grande Fourche. The Grande Fourche is a mountain in the Mont Blanc Massif, located on the Swiss-French border. It lies between the Glacier de Saleina (Valais) and the Glacier du Tour (Haute-Savoie).

Geographic entities mentioned:
surface_form: grande fourche
instance_of: Mountain
countries: Switzerland
France
coordinates: lat: 45.976305555556
lon: 7.0211388888889
Geographic scope. In the narrower sense, &quot;Svitjod&quot; referred specifically to the core territory of the Svear in the Mälaren Valley, primarily in what is now Uppland, and by extension parts of Södermanland and Västmanland.

Geographic entities mentioned:
surface_form: Mälaren Valley
instance_of: Valley
countries: Sweden
coordinates: lat: 59.5
lon: 16.75
The company announced in June that it is interested to acquire stakes in the Singapore Refining. In September 2002, Petronas discovered new oil and gas reserves in the Turkmen part of the Caspian Sea with a flow rate of 14,176 barrels of oil and 19.05 million standard cubic feet. The company buy out minority shareholders in oil group Energy Africa in December.

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
Pethia manipurensis. &quot;Pethia manipurensis&quot; is a species of cyprinid native to India where it is only known from Loktak Lake. This species can reach a length of SL.

Geographic entities mentioned:
surface_form: Loktak Lake
instance_of: Lake
countries: India
coordinates: lat: 24.55
lon: 93.783333333333
Around the 1950–1953 Korean War, the business began specializing in hiking boots. It based its design on British military boots and began selling them to the public. In 1977, mountaineer wore Songlim boots while climbing Annapurna. In 1995, explorer wore Songlim boots while traversing the south and north poles. South Korean president Kim Young-sam reportedly was a customer of the store.

Geographic entities mentioned:
surface_form: Annapurna
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.5958
lon: 83.82
However, in the early part of the 18th century, a shift towards developing the industrial capabilities of the Urals took place, more than doubling Russia's iron production. In 1828, a series of geological surveys began as part of an effort to determine the mineral make up of the Magnitnaya Mountain and create estimates of the possible amount of iron contained underneath it.

Geographic entities mentioned:
surface_form: Magnitnaya Mountain
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.435555555556
lon: 59.142222222222
Ambazari Lake. Ambazari lake (Marathi: अंबाझरी तलाव) is situated near the Southwest border of Nagpur, in the state of Maharashtra, India. It is one of the 11 lakes in Nagpur and is the largest lake in the city. The Nag River of Nagpur originates from this lake. This was built in the year 1870, under Bhonsle rule, for supplying water to the city.

Geographic entities mentioned:
surface_form: ambazari lake
instance_of: Lake
countries: India
coordinates: lat: 21.12898
lon: 79.042768
Ambazari Lake. Ambazari lake (Marathi: अंबाझरी तलाव) is situated near the Southwest border of Nagpur, in the state of Maharashtra, India. It is one of the 11 lakes in Nagpur and is the largest lake in the city. The Nag River of Nagpur originates from this lake. This was built in the year 1870, under Bhonsle rule, for supplying water to the city.

Geographic entities mentioned:
surface_form: ambazari lake
instance_of: Lake
countries: India
coordinates: lat: 21.12898
lon: 79.042768
surface_form: अंबाझरी तलाव
instance_of: Lake
countries: India
coordinates: lat: 21.12898
lon: 79.042768
Early art advocacy. Their scenic paintings moved U.S. leaders in Washington, D.C., including President Abraham Lincoln. Their visual examples helped define how the United States managed and legislated the territory and then new U.S. state of California, especially represented by the preservation of Yosemite Valley and the Mariposa Grove.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
Laguna Verde (volcano). Cerro Laguna Verde is one of the many stratovolcanoes that integrate a -long chain east of the Gran Salar de Atacama in Chile's II Region. The mountain is located west of Acamarachi (also known as Cerro de Pili) and north of the Aguas Calientes (Simbad) and Lascar stratovolcanoes. The age of the volcano, which rises above the surrounding terrain is not known for certain.

Geographic entities mentioned:
surface_form: Salar de Atacama
instance_of: Lake
Body of water
countries: Chile
coordinates: lat: -23.416666666666668
lon: -68.26666666666667
surface_form: laguna verde
instance_of: Mountain
countries: Chile
coordinates: lat: -23.254
lon: -67.71266667
Laguna Verde (volcano). Cerro Laguna Verde is one of the many stratovolcanoes that integrate a -long chain east of the Gran Salar de Atacama in Chile's II Region. The mountain is located west of Acamarachi (also known as Cerro de Pili) and north of the Aguas Calientes (Simbad) and Lascar stratovolcanoes. The age of the volcano, which rises above the surrounding terrain is not known for certain.

Geographic entities mentioned:
surface_form: Acamarachi
instance_of: Mountain
countries: Chile
coordinates: lat: -23.295833333333
lon: -67.617222222222
surface_form: aguas calientes
instance_of: Mountain
countries: Chile
coordinates: lat: -23.368333333333
lon: -67.685
Laguna Verde (volcano). Cerro Laguna Verde is one of the many stratovolcanoes that integrate a -long chain east of the Gran Salar de Atacama in Chile's II Region. The mountain is located west of Acamarachi (also known as Cerro de Pili) and north of the Aguas Calientes (Simbad) and Lascar stratovolcanoes. The age of the volcano, which rises above the surrounding terrain is not known for certain.

Geographic entities mentioned:
surface_form: laguna verde
instance_of: Mountain
countries: Chile
coordinates: lat: -23.254
lon: -67.71266667
Geographic Range. The wood white is found in Europe and eastwards across the Caucasus, Asia Minor, the Middle East, Middle Asia, Kazakhstan and south Siberia to the Baikal region. Within Europe, the wood white is unevenly distributed across the Midlands and Southern England, as well as Northern Europe and Ireland.

Geographic entities mentioned:
surface_form: Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Clarias maclareni. &quot;Clarias maclareni&quot; is a critically endangered species of catfish in the family Clariidae. It is endemic to Lake Barombi Mbo in western Cameroon. It is currently threatened because of pollution and sedimentation due to human activities, and potentially also by large emissions of carbon dioxide (CO2) from the lake's bottom (compare Lake Nyos). It is known to grow to TL.

Geographic entities mentioned:
surface_form: Lake Nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889
Ostrozub. Ostrozub (Serbian Cyrillic: Острозуб) is a mountain in southern Serbia, near the town of Crna Trava. It forms a continuous range with Čemernik mountain. Its highest peak &quot;Ostrozupska čuka&quot; has an elevation of 1,546 meters above sea level. on the mountain is depopulated. According to the 2002 census, it had a population of 1.

Geographic entities mentioned:
surface_form: Čemernik
instance_of: Mountain
countries: Serbia
coordinates: lat: 42.73544
lon: 22.2775
Ostrozub. Ostrozub (Serbian Cyrillic: Острозуб) is a mountain in southern Serbia, near the town of Crna Trava. It forms a continuous range with Čemernik mountain. Its highest peak &quot;Ostrozupska čuka&quot; has an elevation of 1,546 meters above sea level. on the mountain is depopulated. According to the 2002 census, it had a population of 1.

Geographic entities mentioned:
surface_form: ostrozub
instance_of: Mountain
countries: Serbia
coordinates: lat: 42.8817
lon: 22.2397