Sarmila/GeoWiki-Features huggingface dataset:
Mean temperature: January: -3 C, April: 3 C, July: 14 C and October: 5 C. Mean maximum temperature in July: 28 C. The valley is populated by several upland villages; these are Lata, Omarishara, Shkhara and Zemo Azhara. Administratively, it was de facto and de jure a part of Upper Abkhazia (prior to August 2008), but the Republic of Abkhazia claims it as part of the Gulripshi District.

Geographic entities mentioned:
surface_form: Shkhara
instance_of: Mountain
countries: Georgia
Russia
Russian Empire
Soviet Union
coordinates: lat: 42.999444444444
lon: 43.111666666667
Kodori Valley. The Kodori Valley, also known as the Kodori Gorge (,), is a river valley in Abkhazia, Georgia's breakaway autonomous republic. The valley's upper part, populated by Svans, was the only corner of the post-1993 Abkhazia directly controlled by the central Georgian government, which since 2006 officially styles the area as Upper Abkhazia (Geo. ზემო აფხაზეთი, &quot;Zemo Apkhazeti&quot;).

Geographic entities mentioned:
surface_form: kodori valley
instance_of: Valley
countries: Georgia
coordinates: lat: 43.1
lon: 41.8
The valley's upper part, populated by Svans, was the only corner of the post-1993 Abkhazia directly controlled by the central Georgian government, which since 2006 officially styles the area as Upper Abkhazia (Geo. ზემო აფხაზეთი, &quot;Zemo Apkhazeti&quot;). On August 12, 2008, Russo–Abkhazian forces gained control of the Upper Kodori Valley, previously controlled by Georgia. Description.

Geographic entities mentioned:
surface_form: kodori valley
instance_of: Valley
countries: Georgia
coordinates: lat: 43.1
lon: 41.8
Description. The Upper Kodori Valley lies in the upper reaches of the Kodori River in northeastern Abkhazia, about 65 km (40 miles) inside an official administrative boundary of the region with the rest of Georgia. It is about 30 km (20 miles) down the coast from Abkhazia's capital Sukhumi.

Geographic entities mentioned:
surface_form: kodori valley
instance_of: Valley
countries: Georgia
coordinates: lat: 43.1
lon: 41.8
According to the last Georgian census (2002), the population of the former Georgian-controlled part of the valley was 1,956, of which were 1,912 ethnic Georgians (Svans). The population of the Upper Kodori Valley in 2011 was 196, mostly ethnic Georgians (Svans).

Geographic entities mentioned:
surface_form: kodori valley
instance_of: Valley
countries: Georgia
coordinates: lat: 43.1
lon: 41.8
The residents of Azhara did not have Abkhazian passports. History. The Abkhazian historic regions of Dal and Tsebelda occupied most of the Kodori Valley before the incorporation of Abkhazia into Russian Empire from 1810 to 1864. Its highland communities were independent of the central authority of Shervashidze-Chachba princes.

Geographic entities mentioned:
surface_form: kodori valley
instance_of: Valley
countries: Georgia
coordinates: lat: 43.1
lon: 41.8
In the 1840s, Imperial Russian soldiers started a series of massacres and ethnic cleansing. In January 1841, Russian troops massacred the Svan and Georgian populations in Kodori valley, specifically in the village of Dali. It is estimated that 90 Svan surnames went extinct as families were killed and few deported.

Geographic entities mentioned:
surface_form: kodori valley
instance_of: Valley
countries: Georgia
coordinates: lat: 43.1
lon: 41.8
The village of Lata was taken by Abkhazian forces on March 24 and 25, 1994. According to the Moscow Agreement, signed in May 1994, the ceasefire line was drawn to the north-east of it so, so that the Upper Kodori Valley would remain outside of the control of Abkhazian authorities.

Geographic entities mentioned:
surface_form: kodori valley
instance_of: Valley
countries: Georgia
coordinates: lat: 43.1
lon: 41.8
Together with the Gali district, it is one of the two areas that remain populated by Georgians in the post-war Abkhazia. 1. Monitor the withdrawal of troops of Georgia from the Kodori Valley to places beyond the boundaries of Abkhazia.2. Patrol the Kodori Valley regularly.

Geographic entities mentioned:
surface_form: kodori valley
instance_of: Valley
countries: Georgia
coordinates: lat: 43.1
lon: 41.8
surface_form: kodori valley
instance_of: Valley
countries: Georgia
coordinates: lat: 43.1
lon: 41.8
From the viewing platform of the chapel tower there is an all-round view that reaches to the Siebengebirge hills, the basalt &quot;kuppen&quot; of the Hohe Acht, the Hochthürmerberg and Aremberg hills as well as the Schneifel and Rur Eifel regions. In good visibility even the towers on Cologne Cathedral, about 50 kilometres away, may be visible.

Geographic entities mentioned:
surface_form: Hochthürmerberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.52777778
lon: 6.90777778
Michelsberg (Eifel). The Michelsberg, at, is the highest point in the borough of Bad Münstereifel in the county of Euskirchen in the German state of North Rhine-Westphalia. The hill, which rises near the village of Mahlberg belongs to that part of the Eifel mountains known as the Ahr Hills &quot;(Ahreifel)&quot;, and is the second highest point in the range. Location.

Geographic entities mentioned:
surface_form: mahlberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.836
lon: 8.37699
Location. The Michelsberg rises on the northwestern edge of the Ahr Hills in the High Fens-Eifel Nature Park. Its summit lies 1.2 km east-northeast of the centre of Mahlberg, which extends to the southwestern flank of the hill, and 1.5 km west-northwest of Reckerscheid. Some distance away to the south is the village of Esch with its hamlet of Wasserscheide.

Geographic entities mentioned:
surface_form: mahlberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.836
lon: 8.37699
Michelsberg (Eifel). The Michelsberg, at, is the highest point in the borough of Bad Münstereifel in the county of Euskirchen in the German state of North Rhine-Westphalia. The hill, which rises near the village of Mahlberg belongs to that part of the Eifel mountains known as the Ahr Hills &quot;(Ahreifel)&quot;, and is the second highest point in the range. Location.

Geographic entities mentioned:
surface_form: michelsberg (eifel)
instance_of: Mountain
countries: Germany
coordinates: lat: 50.5125
lon: 6.82417
Michelsberg (Eifel). The Michelsberg, at, is the highest point in the borough of Bad Münstereifel in the county of Euskirchen in the German state of North Rhine-Westphalia. The hill, which rises near the village of Mahlberg belongs to that part of the Eifel mountains known as the Ahr Hills &quot;(Ahreifel)&quot;, and is the second highest point in the range. Location.

Geographic entities mentioned:
surface_form: michelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.5125
lon: 6.82417
Lai Lung. Lai Lung is a lake in Switzerland. It is located near Riom-Parsonz in the Canton of the Grisons. According to a 1922 travel guide, its altitude is 6070 feet.

Geographic entities mentioned:
surface_form: lai lung
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.5954
lon: 9.54694
Lake Manatee. Lake Manatee is an artificial reservoir located in Manatee County, Florida. State Road 64 crosses the eastern end of the lake, while the Lake Manatee State Park is found at the southwestern end. The Manatee River flows into the lake at the eastern end, then continues to the west, where it flows into Tampa Bay.

Geographic entities mentioned:
surface_form: lake manatee
instance_of: Lake
countries: United States
coordinates: lat: 27.4836
lon: -82.3288
The Manatee River flows into the lake at the eastern end, then continues to the west, where it flows into Tampa Bay. Lake Manatee is a major source of water for Bradenton and other cities in Manatee County, providing per day. Lake Manatee State Park is located on the south shore of the lake. History. Discussion of building a reservoir in Manatee County started in the 1950s.

Geographic entities mentioned:
surface_form: lake manatee
instance_of: Lake
countries: United States
coordinates: lat: 27.4836
lon: -82.3288
Discussion of building a reservoir in Manatee County started in the 1950s. In 1951, the Manatee County Commission passed a resolution indicating interest in building a dam at an existing deep ravine east of the Rye Road bridge. Construction of the Lake Manatee reservoir broke ground on October 23, 1965. The reservoir's dimensions consisted of about high and across, with a concrete spillway.

Geographic entities mentioned:
surface_form: lake manatee
instance_of: Lake
countries: United States
coordinates: lat: 27.4836
lon: -82.3288
It was set by the government in the 1960s to 1970s in which regular swimming facilities weren't common. It is on the brink of the Hong Kong Island, outlining the Victoria Road and Mount Davis. It functions as a hybrid of swimming lot and photo-taking spot for photography lovers, for its vantage point which helps visitors see the small island to the West of the shed, the beacon and the sunset.

Geographic entities mentioned:
surface_form: Mount Davis
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.277
lon: 114.125
The Waipawa's flow is generally greater than that of the Tukituki River, into which it flows. The Old Bed of Waipawa River flows roughly parallel with and north of the present Waipawa River to join the Tukituki through the Papanui Stream, south west of Lake Poukawa. The Waipawa changed its course during a flood in 1868.

Geographic entities mentioned:
surface_form: Lake Poukawa
instance_of: Lake
countries: New Zealand
coordinates: lat: -39.7838
lon: 176.701
Roederer Estate is a California winery founded in 1982 by Jean-Claude Rouzaud, then president of its parent company, Champagne Louis Roederer. It produces estate-bottled sparkling wines from Mendocino County's cool, fog-shrouded Anderson Valley. As the California outpost of Champagne Louis Roederer, Roederer Estate winery is considered one of the top sparkling wine producers in the United States.

Geographic entities mentioned:
surface_form: Anderson Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.06
lon: -123.43
Mountain rescue in Wales. Mountain rescue in Wales is the search and rescue activities that occur in the mountainous and other wilderness environments in Wales. Wales is largely mountainous with its higher peaks in the north and central areas, including Snowdon (), its highest summit. Mountain rescue teams are called out through the police, via the 999 system, to assist police, fire and ambulance.

Geographic entities mentioned:
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
Chott Tigri volcanic field. The Chott Tigri volcanic field is a volcanic field in Morocco, last known to have been volcanically active during the Pleistocene. It is in the Oriental region of Morocco.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: chott tigri volcanic field
instance_of: Mountain
coordinates: lat: 32.92
lon: -1.85
Chott Tigri volcanic field. The Chott Tigri volcanic field is a volcanic field in Morocco, last known to have been volcanically active during the Pleistocene. It is in the Oriental region of Morocco.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
surface_form: chott tigri volcanic field
instance_of: Mountain
coordinates: lat: 32.92
lon: -1.85
It is located 31 km south of Karpenisi and 53 km northeast of Agrinio, 2 km from the homonymous village and is a spiritual and pilgrimage center of the entire region. It is built in a steep, rocky area between the mountains of Helidona, Kaliakouda and the mountain range of Panaitoliko, which is overgrown with fir trees.

Geographic entities mentioned:
surface_form: Kaliakouda
instance_of: Mountain
countries: Greece
coordinates: lat: 38.79596
lon: 21.75887
The same summer, the Sea-king Hjörvard of the Ylfings arrived at &quot;Myrkva Fjord&quot; (Mörköfjärden, an inlet that is still used to pass between Mälaren and the Baltic Sea and divides Södermanland in two parts). Hjörvard was invited to a feast with Granmar and he agreed as he had never pillaged in the area before.

Geographic entities mentioned:
surface_form: Mälaren
instance_of: Lake
countries: Sweden
coordinates: lat: 59.5
lon: 17.2
Accuratamente restaurato per adibito a museo, è stato inaugurato nel giugno del 2001, parte di un circuito di centri espositivi della Valdelsa e di musei vicariali sorti nell'area fiorentina con il fine di aggregare beni culturali religiosi sparsi nel territorio che, per ragioni di sicurezza e custodia, non possono essere conservati nelle sedi di origine e che trovano perciò assetto museografico, visibilità scientifica e pubblica fruizione presso la chiesa più importante della circoscrizione ecclesiastica di riferimento.

Geographic entities mentioned:
surface_form: Valdelsa
instance_of: Valley
countries: Italy
coordinates: lat: 43.46666667
lon: 11.15
The situation worsened in 1988 as much of the United States also suffered from severe drought. In California, the six-year drought ended in late 1992 as a significant El Niño event in the Pacific Ocean (and the eruption of Mount Pinatubo in June 1991) most likely caused unusually persistent heavy rains.

Geographic entities mentioned:
surface_form: Mount Pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Benedictia. &quot;Benedictia&quot; is a genus of freshwater snails with an operculum, aquatic gastropod molluscs or micromolluscs in the family Lithoglyphidae. &quot;Benedictia&quot; is the type genus of the subfamily Benedictiinae. Distribution. The genus &quot;Benedictia&quot; is endemic to Lake Baikal.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Grande Pointe des Planereuses. The Grande Pointe des Planereuses is a mountain of the Mont Blanc massif, located west of Praz de Fort in the canton of Valais, Switzerland. It lies on the range south of the Saleina Glacier.

Geographic entities mentioned:
surface_form: grande pointe des planereuses
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.96825
lon: 7.0722777777778
In 1847 he issued in Paris &quot;Notes to J. Hardouin's &quot;Doutes proposées sur l'âge du Dante&quot;.&quot;
Family. Lyell married in 1796 a daughter of Thomas Smith of Maker Hall, Swaledale, Yorkshire, by whom he had three sons and seven daughters. His wife died in 1850. His eldest son was Sir Charles Lyell. A son Henry went into the army, and another, Thomas, into the navy.

Geographic entities mentioned:
surface_form: Swaledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.361
lon: -1.838
Alexander received the German surrender in Italy on 29 April 1945. As a reward for his leadership in North Africa and Italy, Alexander, along with a number of other prominent British Second World War military leaders, was elevated to the peerage on 1 March 1946 by King George VI; he was created Viscount Alexander of Tunis and of Errigal in the County of Donegal.

Geographic entities mentioned:
surface_form: Errigal
instance_of: Mountain
countries: Ireland
coordinates: lat: 55.033
lon: -8.112
Geography. The north wall is over high above Pavilion Lake and is the southernmost extent of the Marble Range; the south wall is c. 515 m (1500 ft) and is the northern extremity of the Clear Range. Higher peaks lie in behind the walls, increasing the depth if measured from their summits. Stromatolites. Within the canyon are a series of lakes draining towards the Fraser River via Pavilion Creek.

Geographic entities mentioned:
surface_form: Pavilion Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.8668
lon: -121.742
Cultural rights. These areas and Pavilion Lake, in addition to being provincial park, are also governed by special cultural rights and have important spiritual significance of the Pavilion Band.

Geographic entities mentioned:
surface_form: Pavilion Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.8668
lon: -121.742
Marble Canyon (British Columbia). Marble Canyon is in the south-central Interior of British Columbia, a few kilometres east of the Fraser River and the community of Pavilion, midway between the towns of Lillooet and Cache Creek. The canyon stems from a collapsed karst formation. Nomenclature. The canyon's name comes from the brilliant limestone of its walls.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: marble canyon
instance_of: Valley
countries: Canada
coordinates: lat: 51.185833333333335
lon: -116.12277777777778
surface_form: marble canyon
instance_of: Valley
countries: Canada
coordinates: lat: 50.833333333333336
lon: -121.68333333333334
Rock and ice climbing. Marble Canyon is popular with climbers, both for its clean rock walls and also for its ice climbs, including one waterfall that freezes solid in midwinter (officially Crown Lake Falls but to climbers, &quot;Icy BC&quot;), and which is immediately opposite the provincial park campground adjacent to Highway 99 from Lillooet to Cache Creek, British Columbia. Cultural rights.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
In addition to the steep walls rising from the lake's southeastern end, there is an eroded pinnacle known as Chimney Rock, or in a translation of &quot;K'lpalekw&quot;, the Secwepemc (Shuswap) name for it, Coyote's Penis. Geography. The north wall is over high above Pavilion Lake and is the southernmost extent of the Marble Range; the south wall is c.

Geographic entities mentioned:
surface_form: chimney rock
instance_of: Mountain
countries: Canada
coordinates: lat: 50.8783
lon: -121.72
Course. Opalescent River has its source on the west side of Little Marcy Mountain, at over in elevation. After nearly two miles, Feldspar Brook—which itself originates from Lake Tear of the Clouds—converges with the Opalescent. The river then passes through Flowed Lands, and 11 miles later reaches Calamity Brook, at which point the stream becomes cartographically known as the Hudson River.

Geographic entities mentioned:
surface_form: Lake Tear of the Clouds
instance_of: Lake
countries: United States
coordinates: lat: 44.1067
lon: -73.9358
Innerer Fisistock. The Innerer Fisistock is a mountain of the Bernese Alps, overlooking Kandersteg in the Bernese Oberland. It lies at the western end the Blüemlisalp chain.

Geographic entities mentioned:
surface_form: Blüemlisalp
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.488611111111
lon: 7.7716666666667
Innerer Fisistock. The Innerer Fisistock is a mountain of the Bernese Alps, overlooking Kandersteg in the Bernese Oberland. It lies at the western end the Blüemlisalp chain.

Geographic entities mentioned:
surface_form: innerer fisistock
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.469555555556
lon: 7.6906944444444
Gaylord Nunatak. tqbnbxzm93jadj77ovpsxs2k0ac" xml:space="preserve">#redirect Gaylord Nunatak

Geographic entities mentioned:
surface_form: gaylord nunatak
instance_of: Mountain
coordinates: lat: -74.9333
lon: -72.1333
This makes more sense, as the title derives from the line &quot;per fine Troy ounce&quot; or a variation of. A fine ounce is a Troy ounce of not quite pure gold. Jenkins' synopsis found by John Pearson in Fleming's papers featured gold bicycle chains, baobab tree coffins and the magical Lake Fundudzi&mdash;presumably, Jenkins used some or all of these elements in the book itself.

Geographic entities mentioned:
surface_form: Lake Fundudzi
instance_of: Lake
countries: South Africa
coordinates: lat: -22.855
lon: 30.30555556
It is located in the La Paz Department, Los Andes Province, Pucarani Municipality. Tira Qullu lies between the lakes Sura Quta and Taypi Chaka Quta in the west and Juri Quta in the east. It is situated south-west of the mountains Jach'a Jipiña and Milluni.

Geographic entities mentioned:
surface_form: Taypi Chaka Quta
instance_of: Lake
countries: Bolivia
coordinates: lat: -16.205833333333334
lon: -68.35083333333333
surface_form: juri quta
instance_of: Lake
countries: Bolivia
coordinates: lat: -16.19361111
lon: -68.27222222
surface_form: taypi chaka quta
instance_of: Lake
countries: Bolivia
coordinates: lat: -16.205833333333334
lon: -68.35083333333333
It is located in the La Paz Department, Los Andes Province, Pucarani Municipality. Tira Qullu lies between the lakes Sura Quta and Taypi Chaka Quta in the west and Juri Quta in the east. It is situated south-west of the mountains Jach'a Jipiña and Milluni.

Geographic entities mentioned:
surface_form: Jach'a Jipiña
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.1986
lon: -68.2892
surface_form: jach'a jipiña
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.1986
lon: -68.2892
surface_form: milluni
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.3864
lon: -65.5481
Tira Qullu. Tira Qullu (Aymara &quot;tira&quot; cradle, &quot;qullu&quot; mountain, &quot;cradle mountain&quot;, also spelled &quot;Tira Kkollu&quot;) is a mountain in the western extension of the Cordillera Real in the Andes of Bolivia. It is located in the La Paz Department, Los Andes Province, Pucarani Municipality.

Geographic entities mentioned:
surface_form: tira qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.2025
lon: -68.3147
Geography. Rapale is located near the province of Siena in Tuscany, Italy. The village is part of the municipality of Bucine in south-western Arezzo. The Pratomagno is a mountain range which has the Arno river on both sides: to the west is the upper Valdarno and to the east is the Casentino. It lies north-west of the city of Arezzo, in Tuscany, Italy.

Geographic entities mentioned:
surface_form: Pratomagno
instance_of: Mountain
countries: Italy
coordinates: lat: 43.65
lon: 11.65
surface_form: Valdarno
instance_of: Valley
countries: Italy
coordinates: lat: 43.566666666667
lon: 11.533333333333
surface_form: Casentino
instance_of: Valley
countries: Italy
coordinates: lat: 43.7
lon: 11.816666666667
The river gives its name to the Erewash Valley, which has a rich industrial history, and the local government district and borough of Erewash, which was named after the river when the former borough of Ilkeston and urban district of Long Eaton were united with some of the surrounding rural areas in 1974. History. The river has been used as a source of water power in the past.

Geographic entities mentioned:
surface_form: Erewash Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.0045
lon: -1.3131
Baden-Powell Peak. Baden-Powell Scout Peak, formerly known as Urkema Peak, in Nepal is part of the Himalayas, the highest mountain range in the world. It is on the border with China about a hundred miles west of Mount Everest.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Baden-Powell Peak. Baden-Powell Scout Peak, formerly known as Urkema Peak, in Nepal is part of the Himalayas, the highest mountain range in the world. It is on the border with China about a hundred miles west of Mount Everest.

Geographic entities mentioned:
surface_form: baden-powell peak
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.16757
lon: 85.53337
First Ascent. The first ascent of Baden-Powell Peak was completed by an international team of Scouting members, including members from Australia, Korea, Taiwan, Singapore, Taipei, Hong Kong, Malaysia and Nepal. The first person to reach the summit was Australian climber Mark Mangles at around 12 o’clock on 12 September 2007. 14 climbers in total summited the peak during this expedition.

Geographic entities mentioned:
surface_form: baden-powell peak
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.16757
lon: 85.53337
Baden-Powell Peak. Baden-Powell Scout Peak, formerly known as Urkema Peak, in Nepal is part of the Himalayas, the highest mountain range in the world. It is on the border with China about a hundred miles west of Mount Everest.

Geographic entities mentioned:
surface_form: baden-powell scout peak
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.16757
lon: 85.53337
surface_form: urkema peak
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.16757
lon: 85.53337
It is on the border with China about a hundred miles west of Mount Everest. As part of the Scouting 2007 Centenary, the government of Nepal renamed Urkema Peak to Baden-Powell Scout Peak, to commemorate 100 years of Scouting in honor of British soldier Robert Baden-Powell, founder of the World Scouting movement. First Ascent.

Geographic entities mentioned:
surface_form: baden-powell scout peak
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.16757
lon: 85.53337
surface_form: urkema peak
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.16757
lon: 85.53337
Karaś Lake. Karaś is a lake in the Masurian Lake District of north-eastern Poland, from the town of Iława in Warmian-Masurian Voivodeship. The lake is the site of a nature reserve, established in 1958 and covering an area of. Since 1984 it has been protected under the Ramsar convention as an important breeding ground for water birds. It is currently one of 13 such sites in Poland.

Geographic entities mentioned:
surface_form: karaś lake
instance_of: Lake
countries: Poland
coordinates: lat: 53.555555555556
lon: 19.480555555556
Karaś Lake. Karaś is a lake in the Masurian Lake District of north-eastern Poland, from the town of Iława in Warmian-Masurian Voivodeship. The lake is the site of a nature reserve, established in 1958 and covering an area of. Since 1984 it has been protected under the Ramsar convention as an important breeding ground for water birds. It is currently one of 13 such sites in Poland.

Geographic entities mentioned:
surface_form: karaś
instance_of: Lake
countries: Poland
coordinates: lat: 53.555555555556
lon: 19.480555555556
Franklin Glacier Complex. The Franklin Glacier Complex is a deeply eroded volcano in the Waddington Range of southwestern British Columbia, Canada. Located about northeast of Kingcome, this little-known complex is adjacent to Franklin Glacier near Mount Waddington. It is over in elevation and due to its considerable overall altitude, a large proportion of the complex is covered by glacial ice.

Geographic entities mentioned:
surface_form: Mount Waddington
instance_of: Mountain
countries: Canada
coordinates: lat: 51.373611111111
lon: -125.26333333333
They intrude through fractured and hydrothermally altered Mesozoic to early Tertiary granitic and metamorphic rocks of the Coast Plutonic Complex. The complex lies on the overlapping trend of the Garibaldi and Pemberton volcanic belts, which were formed as a result of subduction zone magmatism along the Cascade Volcanic Arc in the last 29 million years.

Geographic entities mentioned:
surface_form: Garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5283
lon: -126.113
surface_form: Pemberton
instance_of: Mountain
countries: Canada
coordinates: lat: 50.58051944
lon: -122.93235278
A series of smaller intrusions were emplaced during the second magmatic stage 2.2 to 3.9 million years ago, at least some of which appear to have been feeders for the overlying volcanic pile. The Franklin Glacier Complex is substantially older than the neighbouring Silverthrone Caldera to the northwest.

Geographic entities mentioned:
surface_form: Silverthrone Caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
surface_form: franklin glacier complex
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3333
lon: -125.4
Onucki and J. R. Deighton for the purpose of locating reported high-grade silver mineralization. Franklin Glacier was skied by Canadian mountaineers Don and Phyllis Munday on July 22, 1930 while exploring and mapping glaciers of the Waddington Range. Don Munday named the glacier in 1927 for its association with the Franklin River which in turn was named after a Benjamin Franklin at Tatla Lake.

Geographic entities mentioned:
surface_form: Tatla Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.9667
lon: -124.417
Franklin Glacier Complex. The Franklin Glacier Complex is a deeply eroded volcano in the Waddington Range of southwestern British Columbia, Canada. Located about northeast of Kingcome, this little-known complex is adjacent to Franklin Glacier near Mount Waddington. It is over in elevation and due to its considerable overall altitude, a large proportion of the complex is covered by glacial ice.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: franklin glacier complex
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3333
lon: -125.4
It has therefore been of interest to geothermal exploration. Geography. The area lies in one of British Columbia's many territorial divisions called the Range 2 Coast Land District. Local relief exceeds with the long valley-filling Franklin Glacier originating from an icefield below the west face of Mount Waddington.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Geography. The area lies in one of British Columbia's many territorial divisions called the Range 2 Coast Land District. Local relief exceeds with the long valley-filling Franklin Glacier originating from an icefield below the west face of Mount Waddington. It is part of the Waddington Range, a subrange of the Pacific Ranges which in turn are a subdivision of the Coast Mountains.

Geographic entities mentioned:
surface_form: mount waddington
instance_of: Mountain
countries: Canada
coordinates: lat: 51.373611111111
lon: -125.26333333333
Franklin Glacier Complex. The Franklin Glacier Complex is a deeply eroded volcano in the Waddington Range of southwestern British Columbia, Canada. Located about northeast of Kingcome, this little-known complex is adjacent to Franklin Glacier near Mount Waddington. It is over in elevation and due to its considerable overall altitude, a large proportion of the complex is covered by glacial ice.

Geographic entities mentioned:
surface_form: franklin glacier complex
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3333
lon: -125.4
It is over in elevation and due to its considerable overall altitude, a large proportion of the complex is covered by glacial ice. Magmatic activity of the Franklin Glacier Complex spanned roughly four million years from the Late Miocene to the Early Pleistocene, with the most recently identified volcanic eruption having taken place around 2.2 million years ago.

Geographic entities mentioned:
surface_form: franklin glacier complex
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3333
lon: -125.4
It is part of the Waddington Range, a subrange of the Pacific Ranges which in turn are a subdivision of the Coast Mountains. The Franklin Glacier Complex was covered by the Cordilleran Ice Sheet until its retreat about 13,000 years ago. Franklin Glacier has since undergone glacial retreat and expansion throughout the Holocene.

Geographic entities mentioned:
surface_form: franklin glacier complex
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3333
lon: -125.4
The timing of expansions corresponded with cool summer temperatures, generally moist conditions and increased precipitation. Geology. Minimal geologic studies have been conducted at the Franklin Glacier Complex and its geology is therefore poorly known. It measures wide and long, covering a northwesterly elliptical area of.

Geographic entities mentioned:
surface_form: franklin glacier complex
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3333
lon: -125.4
It measures wide and long, covering a northwesterly elliptical area of. Volcanic rocks of the Franklin Glacier Complex consist predominantly of dacite breccia, minor dacite flows and a few hornblende andesite remnants. An absence of pumice, glassy blocks or bombs in the breccia suggests that it may be of epiclastic origin, possibly formed during collapse and infilling of a caldera.

Geographic entities mentioned:
surface_form: franklin glacier complex
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3333
lon: -125.4
The complex lies on the overlapping trend of the Garibaldi and Pemberton volcanic belts, which were formed as a result of subduction zone magmatism along the Cascade Volcanic Arc in the last 29 million years. Two separate stages of magmatic activity have been identified at the Franklin Glacier Complex.

Geographic entities mentioned:
surface_form: franklin glacier complex
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3333
lon: -125.4
The Franklin Glacier Complex is substantially older than the neighbouring Silverthrone Caldera to the northwest. Immediately west of the Franklin Glacier Complex are a series of hot springs confined in valleys. At Canyon Lake, a hot spring feeds a small stream that flows into the southeastern end of that lake.

Geographic entities mentioned:
surface_form: franklin glacier complex
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3333
lon: -125.4
A single temperature of has been obtained from this spring while the Hoodoo Creek and Pinter spring temperatures remain unknown. The existence of these hot springs has made the Franklin Glacier Complex a target for geothermal exploration but little work has been conducted due to its remote location. The only performed exploration has been moderate geological mapping.

Geographic entities mentioned:
surface_form: franklin glacier complex
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3333
lon: -125.4
A 50 megawatt binary plant has been proposed at Canyon Lake. History. Mineral exploration at the Franklin Glacier Complex has occurred sporadically since at least the 1960s. The earliest recorded work was done by Kennco Exploration Limited with the staking of claims in a zone of copper-molybdenum mineralization associated with the quartz monzonite stock.

Geographic entities mentioned:
surface_form: franklin glacier complex
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3333
lon: -125.4
The area was founded in the 12th century by King Mokwena II the first born son of King Matlebjane II of Batau. The Batau clan trace their origin from the Swazi.They moved north to Lake Chrissie (known in the local language as Seoko-seokodibeng) from Wakkerstroom. They went from there to Mokwena River (which today is called Crocodile River) and established themselves in the Mpumalanga Mountains.

Geographic entities mentioned:
surface_form: Lake Chrissie
instance_of: Lake
countries: South Africa
coordinates: lat: -26.3333
lon: 30.2167
Llyn Dinas. Llyn Dinas is a lake near Beddgelert, Gwynedd in north Wales. It is formed by the River Glaslyn. Llyn Dinas lies on the valley floor a few miles north of Beddgelert at an altitude of about 55 metres above sea level. It has an area of and is fairly shallow, with the maximum depth only 10 metres. The lake offers good fishing for salmon and trout.

Geographic entities mentioned:
surface_form: llyn dinas
instance_of: Lake
countries: United Kingdom
coordinates: lat: 53.025521366132814
lon: -4.064557659479522
As of 2018-2019, the school board has 41 elementary and 9 secondary schools located in communities throughout Simcoe County and the District of Muskoka. Its boundaries are Highway 9 in the south to Huntsville in the north, and from Collingwood in the west to Brechin on the east side of Lake Simcoe.

Geographic entities mentioned:
surface_form: Lake Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
Normally, Ural owls are not too shy and may be approached quite closely. Historically, European birdwatchers often consider the species to be rather elusive and hard to observe. However, as the species as acclimated to nest boxes closer to areas where humans frequent, especially in Fennoscandia, encounters have increased sharply. Territoriality and movements.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Birds usually compromise less than 10% of the dietary intake by number in studies from Europe. Exceptionally high numbers, relatively speaking, were reported in Fennoscandia, especially when vole numbers go down. In bad vole years in Finland, of 860 prey items, 32.2% by number and 40.25% by biomass were birds.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Thus, the Ural owl is frequently considered to be a competitor with sympatric owl species. Most especially, the Ural owl has often being compared and studied in areas of sympatry with its close cousin, the tawny owl. The tawny owl may co-exist with Ural owls today in many parts of the latter's European distribution, including southern Fennoscandia, eastern and central Europe and European Russia.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
field vole, water vole, &quot;Apodemus&quot; species, birds and frogs). On Mount Krim in Slovenia, both tawny and Ural owls took the same primary prey species but the tawny owl was shown to be adaptable to alternate prey during the low part of the vole population cycle while the Ural was less adaptive to alternate prey.

Geographic entities mentioned:
surface_form: Mount Krim
instance_of: Mountain
countries: Slovenia
coordinates: lat: 45.95
lon: 14.40833333
However, cases of interspecific killing between the species are fairly infrequent, and recent study indicates that the tawny owl's relatively checkered distribution in northerly areas such as Fennoscandia is not likely due to this competition but rather due to the regional habitat type favoring the Ural owl.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Warming average temperatures in Fennoscandia have appeared to effect many owl species negatively due to the limiting nature on vole cycles, but the tawny owl, being confined to the south, has had the most decreased effect locally due to the lowering vole numbers (and despite their general ability to adapt to different prey) while the Ural owl, in central Finland at least, is not yet showing as drastic a negative effect due to this.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Pair occupancy. The Ural owl generally pairs for life and maintains a territory for several years. Mate retention in Fennoscandia was found to have averaged 98–100% in males and 90-95% in females, making it amongst the most monogamous birds of prey of any order (or at least well-studied bird of prey species). Territories of Ural owls are on average about 3 times larger than those of tawny owls.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Breeding in Slovenia is at a mean elevation of, with altitude less important than habitat. Many forest types were used in Slovenia but fir-beech mixed forest were seen to be most often utilized. The highest Slovenian densities were around 2-3 pairs per for Mount Krim and around 4-5 pairs per for Snežnik. In 2016, it was estimated that Slovenia holds 400-700 pairs.

Geographic entities mentioned:
surface_form: Mount Krim
instance_of: Mountain
countries: Slovenia
coordinates: lat: 45.95
lon: 14.40833333
A low density population was found for Pieniny National Park, Poland with 0.9-1.3 per. The average density in the Polish Kraków-Częstochowa Upland was 1 pair per. In the northern part of Moravia, Czech Republic, 3-5 pairs were recorded around the turn of the 21st century, an almost certain population increase.

Geographic entities mentioned:
surface_form: Kraków-Częstochowa Upland
instance_of: Plateau
countries: Poland
coordinates: lat: 50.2067
lon: 19.8292
In one case in Norway, a Ural owl utilized a hole in a common aspen (&quot;Populus tremula&quot;) in the same tree where common mergansers (&quot;Mergus merganser&quot;) were using a different hole. In several parts of their range they may make use of nest boxes, with the trend of nest box placement beginning and being perhaps most persistently used in Fennoscandia.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Eggs and young. The clutch size is typically 3-4 (rarely from as few as 1 to as many as 6), with the eggs being pure white and quite rounded. The mean egg laying dates in Fennoscandia are between mid-March and late April. In montane Slovenia, somewhat surprisingly, it is slightly later at late March into early June. Mean clutch size was found to be 2.93 in Sweden.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Larger clutches seem to be an insurance behaviour since authors showed that broods of 4 or so were more likely to have younger sibling die sooner or later before independence. Productivity is largely associated with prey access, with the effect most studied in Fennoscandia because of the dramatic 3 year fluctuation of vole prey appears to cause great variations in productivity.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Awaza. Awaza (or Avaza) refers to both a tourist zone in and a borough (district headed by a presidentially appointed mayor) of the city of Türkmenbaşy, Turkmenistan. It is located on the eastern shore of the Caspian Sea, 12 km west of downtown Türkmenbaşy. Awaza has grown from a small village to one of the largest resort destinations along the Caspian Sea coast.

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
Tosc (mountain). Tosc (), formerly also known as Tolstec, is a mountain of the central Julian Alps, located in Upper Carniola, western Slovenia. The mountain stands south of Triglav, rising above the Voje Valley to the south and Big Field Pasture () to the west. There is a steep gorge in it facing the Krma Valley to the northeast. Recreation. Tosc is protected within Triglav National Park.

Geographic entities mentioned:
surface_form: Triglav
instance_of: Mountain
countries: Slovenia
coordinates: lat: 46.378333
lon: 13.836667
Tosc (mountain). Tosc (), formerly also known as Tolstec, is a mountain of the central Julian Alps, located in Upper Carniola, western Slovenia. The mountain stands south of Triglav, rising above the Voje Valley to the south and Big Field Pasture () to the west. There is a steep gorge in it facing the Krma Valley to the northeast. Recreation. Tosc is protected within Triglav National Park.

Geographic entities mentioned:
surface_form: Krma Valley
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.400552777778
lon: 13.923669444444
Tosc (mountain). Tosc (), formerly also known as Tolstec, is a mountain of the central Julian Alps, located in Upper Carniola, western Slovenia. The mountain stands south of Triglav, rising above the Voje Valley to the south and Big Field Pasture () to the west. There is a steep gorge in it facing the Krma Valley to the northeast. Recreation. Tosc is protected within Triglav National Park.

Geographic entities mentioned:
surface_form: tosc
instance_of: Mountain
countries: Slovenia
coordinates: lat: 46.3567
lon: 13.8684
Tosc (mountain). Tosc (), formerly also known as Tolstec, is a mountain of the central Julian Alps, located in Upper Carniola, western Slovenia. The mountain stands south of Triglav, rising above the Voje Valley to the south and Big Field Pasture () to the west. There is a steep gorge in it facing the Krma Valley to the northeast. Recreation. Tosc is protected within Triglav National Park.

Geographic entities mentioned:
surface_form: tosc
instance_of: Mountain
countries: Slovenia
coordinates: lat: 46.3567
lon: 13.8684
surface_form: tolstec
instance_of: Mountain
countries: Slovenia
coordinates: lat: 46.3567
lon: 13.8684
The mountain stands south of Triglav, rising above the Voje Valley to the south and Big Field Pasture () to the west. There is a steep gorge in it facing the Krma Valley to the northeast. Recreation. Tosc is protected within Triglav National Park. Its southern slope is frequently used by ski tourers.

Geographic entities mentioned:
surface_form: tosc
instance_of: Mountain
countries: Slovenia
coordinates: lat: 46.3567
lon: 13.8684
surface_form: triglav
instance_of: Mountain
countries: Slovenia
coordinates: lat: 46.378333
lon: 13.836667
Ross served another four years as factor at Fort Nez Percés after the merger. While working for the HBC, Ross explored various territories of the Pacific Northwest. In 1824, while searching the mountain wilderness of what is present day Idaho, known to them as Columbia District, for beaver, Ross came up the Wood River and discovered Galena Summit on September 18.

Geographic entities mentioned:
surface_form: Wood River
instance_of: Valley
countries: United States
coordinates: lat: 43.5147
lon: -114.306
Kennedy International Airport and Washington Dulles International Airport. History. The original Ithaca Municipal Airport was west of downtown Ithaca, near the inlet of Cayuga Lake. The site was identified as a likely flying field in 1914 by pilot Charles Niles, who considered relocating to Ithaca to establish a practice field. In December 1914, the Thomas Brothers Aeroplane Co.

Geographic entities mentioned:
surface_form: Cayuga Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.68805555555556
lon: -76.70222222222222
He later entered the Faculty of Medicine and Port-au-Prince Pharmacy, where he graduated as a Doctor of Medicine. He spent his first postgraduate year in the northwest of the country, then spent some time in Jean-Rabel and Bombardopolis, and eventually in the Artibonite Valley as medical director of ODVA (Development Agency of the Valley of Artibonite).

Geographic entities mentioned:
surface_form: Artibonite Valley
instance_of: Valley
countries: Haiti
coordinates: lat: 19.12505833
lon: -72.48298611
Grey Mare's Tail, Moffat Hills. Grey Mare's Tail is a hanging valley waterfall near to Moffat in southern Scotland. The fall is produced by the Tail Burn flowing from Loch Skeen cascading into the Moffat Water in the lower valley below. The surrounding area forms the Grey Mare's Tail Nature Reserve, owned by the National Trust for Scotland.

Geographic entities mentioned:
surface_form: Loch Skeen
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.4351
lon: -3.3115
Parking is also provided. Grey Mare's Tail Nature Reserve is situated along the Moffat Water Valley in the heart of the Southern Uplands. This National Trust for Scotland property extends over 922 hectares and is characterised by a dramatic waterfall (the 5th highest in the UK), an upland loch Loch Skeen and White Coomb which rises to 821m and is one of the highest hills in Southern Scotland.

Geographic entities mentioned:
surface_form: Loch Skeen
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.4351
lon: -3.3115
surface_form: White Coomb
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.422578
lon: -3.323634