Sarmila/GeoWiki-Features huggingface dataset:
Winter season starts from Deepavali around mid-November to mid-February. Summers are generally hot and suffocating due to high humidity levels in the air being the coastal to the Bay of Bengal sea. Chinapulivarru average later May temperate are highest for the season resulting sun strokes for few who expose to it.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
In later period near the fall of Majapahit, the art and architecture of Majapahit witnessed the revival of indigenous native Austronesian megalithic architectural elements, such as Sukuh and Cetho temples on western slopes of Mount Lawu.

Geographic entities mentioned:
surface_form: Mount Lawu
instance_of: Mountain
countries: Indonesia
coordinates: lat: -7.625
lon: 111.19166666667
Also in Canto 14 are territories east of Java: Badahulu and Lo Gajah (part of today's Bali). Gurun and Sukun, Taliwang, Sapi (Sape town, east end of Sumbawa island, by the Sape Strait) and Dompo, Sang Hyang Api, Bima. Sheran and Hutan Kadali (Buru island). Gurun island, and Lombok Merah. Together with prosperous Sasak (central, north and east Lombok) are already ruled. Bantayan with Luwu.

Geographic entities mentioned:
surface_form: Sang Hyang Api
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.18
lon: 119.05
Bradley Tyrrell, a colleague of Pond's from Beloit College, Mr. Denny of &quot;The New York Times&quot;, a motion picture operator, an interpreter, two native guides and a native chef. Alonzo Pond is said to have found Prorok &quot;difficult&quot;. The expedition was launched from Algiers in October 1925 and using motor vehicles for transport headed south towards the Hoggar Mountains.

Geographic entities mentioned:
surface_form: Hoggar Mountains
instance_of: Plateau
countries: Algeria
France
coordinates: lat: 23.288611
lon: 5.534167
He hoped to encounter inhabitants of the Hoggar Mountains who were, he had come to believe, &quot;a mysterious people, tall, straight and slender, who regard themselves as the greatest of all races with similarity to the Egyptians as represented on the ancient tombs of the Pharaohs.&quot;
In October 1925 the expedition arrived in Touggourt and entered the Sahara at El Kantara and &quot;from here we began the long plunge of a thousand
miles of desert to the Hoggar, in whose valleys are white people of magnificent physique and classic features, whose origin is a mystery, and on which
they themselves have steadfastly refused to give any information.&quot;
Prorok writes much about the Tuareg people whom he describes as &quot;a strange people&quot; whose &quot;impetuosity in attack has made them dreaded throughout the Sahara&quot;.

Geographic entities mentioned:
surface_form: Hoggar Mountains
instance_of: Plateau
countries: Algeria
France
coordinates: lat: 23.288611
lon: 5.534167
Hadassah medical convoy massacre. The Hadassah convoy massacre took place on April 13, 1948, when a convoy, escorted by Haganah militia, bringing medical and military supplies and personnel to Hadassah Hospital on Mount Scopus, Jerusalem, was ambushed by Arab forces.

Geographic entities mentioned:
surface_form: Mount Scopus
instance_of: Mountain
countries: Israel
coordinates: lat: 31.7925
lon: 35.244166666667
Mount Scopus blockade. In 1948, following the UN Partition Plan and anticipating Israel's declaration of independence, Arab troops blocked access to Hadassah Hospital and the Hebrew University campus on Mount Scopus, Jerusalem.

Geographic entities mentioned:
surface_form: Mount Scopus
instance_of: Mountain
countries: Israel
coordinates: lat: 31.7925
lon: 35.244166666667
In a statement they claimed that the demonstration was broken up by the Haganah. British soldier Jack Churchill coordinated the evacuation of 700 Jewish doctors, students and patients from the Hadassah hospital on the Hebrew University campus on Mount Scopus in Jerusalem. Inquiry.

Geographic entities mentioned:
surface_form: Mount Scopus
instance_of: Mountain
countries: Israel
coordinates: lat: 31.7925
lon: 35.244166666667
The Underwater Society kept several volumes containing statistics, reports, diagrams, photographs and other pertinent information on the shipwrecks. The wrecks were discovered in the St. Lawrence River from Lake St. Francis to Kingston, Ontario, the Rideau Canal and the Ottawa River from Montreal, Quebec to Lake Timiskaming as well as two dozen inland tributaries and lakes.

Geographic entities mentioned:
surface_form: Lake Timiskaming
instance_of: Lake
countries: Canada
coordinates: lat: 47.333333333333
lon: -79.5
The risk of starting new fires is now very low due to the lowering of temperatures and the humid soil due to heavy rains. Sardinia. Starting on 24 July, the Montiferru area, in Oristano province, was hit by a wildfire, which broke out between Bonarcado and Santu Lussurgiu, forcing the inhabitants of the towns of Cuglieri and Scano di Montiferro to flee for safety.

Geographic entities mentioned:
surface_form: Montiferru
instance_of: Mountain
countries: Italy
coordinates: lat: 40.2167
lon: 8.58333
The decline in population size has been recorded in almost all of its natural habitat locations. Based on a collection of data and resident accounts, &quot;Amazona finschi&quot; population range has decreased by 20% due to habitat loss. An increasingly growing population of approximately 100 individuals is found in Southern California, especially in the San Gabriel Valley and Orange Country.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
Ashgrove Loch. Ashgrove Loch, also known as Stevenston Loch, is a mesotrophic lochan (small loch) in North Ayrshire, Scotland, approximately 2 km northeast of the town of Stevenston. Due to artificial drains, known as cunnels, approximately 90% of the lochan's surface is covered by floating vegetation and is classed as a fen.

Geographic entities mentioned:
surface_form: stevenston loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.662015
lon: -4.743673
surface_form: ashgrove loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.662015
lon: -4.743673
Ashgrove Loch. Ashgrove Loch, also known as Stevenston Loch, is a mesotrophic lochan (small loch) in North Ayrshire, Scotland, approximately 2 km northeast of the town of Stevenston. Due to artificial drains, known as cunnels, approximately 90% of the lochan's surface is covered by floating vegetation and is classed as a fen.

Geographic entities mentioned:
surface_form: ashgrove loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.662015
lon: -4.743673
Posavec (surname). lgvijbt6ffdx4jk48gpllbhmrl5i" xml:space="preserve">Posavec is a surname, which is derived from the region of Posavina. It is the third most common surname in Koprivnica-Križevci County and the fourth most common in Varaždin County of Croatia.

Geographic entities mentioned:
surface_form: Posavina
instance_of: Valley
countries: Croatia
Bosnia and Herzegovina
Serbia
coordinates: lat: 45.16667
lon: 17.33333
Geography. The lowland region lies to the east of the Caspian Sea and southeast of the Aral Sea in the vast Aral–Caspian Depression but extends to parts above sea level as well. It is one of the largest expanses of sand in the world, covering an area of around 3 million km2. On average, the region receives less than of rainfall per year.

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
surface_form: Aral Sea
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
Vpadina Akchanaya in Turkmenistan is below sea level. The Amu Darya River runs in a southeast–north-westerly direction through the lowlands. In the Pliocene and Pleistocene, the territory of the modern Turan depression was the bottom of the vast Turan Sea, which was divided into the modern Caspian and Aral seas about ten thousand years ago.

Geographic entities mentioned:
surface_form: Caspian
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
surface_form: Aral seas
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
James Rigby Beevor. James Rigby Beevor (1811–1849) was a pioneer colonist and pastoralist of South Australia and a murder victim of the Australian frontier wars. Mount Beevor in South Australia is named after him. Origins. Beevor was born 1811 at Norwich, Norfolk, England, into the family of James Beevor, a brewery proprietor at Norwich, and Mary Beevor (&quot;née&quot; Rigby).

Geographic entities mentioned:
surface_form: Mount Beevor
instance_of: Mountain
countries: Australia
coordinates: lat: -34.933330555556
lon: 139.03333055556
Beevor promptly pioneered a sheep station northeast of Mount Barker, near Dawesley, on the eastern flanks of the Mount Lofty Ranges. His sheep run and homestead, then at the frontier of European settlement, was at the base of a prominent peak first discovered in January 1838 by European explorers Dr George Imlay and John Hill. That peak was consequently named Mount Beevor (498m).

Geographic entities mentioned:
surface_form: Mount Beevor
instance_of: Mountain
countries: Australia
coordinates: lat: -34.933330555556
lon: 139.03333055556
The Commissioners and the Wardens of the Western Marches. Its use by the Marcher Lords or Wardens suggests that the Scots regarded the Lochmaben stone as being the southernmost limit of the Scottish realm. In 1398, an indenture was made at &quot;Clochmabenstane&quot; for the men of Tyndale and Redesdale to meet from Whitsunday to Michaelmas at Kershope Bridge.

Geographic entities mentioned:
surface_form: Redesdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.229
lon: -2.186
Kernen (hill). Kernen is a mountain of Baden-Württemberg, Germany.

Geographic entities mentioned:
surface_form: kernen
instance_of: Mountain
countries: Germany
coordinates: lat: 48.7828
lon: 9.31111
An indeterminate species has also been reported from Thailand, of uncertain but probably Late Miocene age. &quot;Zygolophodon&quot; entered North America during the latter part of the Early Miocene (during the late Hemingfordian faunal stage), with the oldest record being a partial tooth from Massacre Lake, Nevada, dating to 16.5-16.4 million years ago.

Geographic entities mentioned:
surface_form: Massacre Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.6534655
lon: -119.6048641
Rotspitz. Rotspitz (literally &quot;redpeak&quot;) is a mountain in Liechtenstein, located close to the Swiss border, due east of the Swiss town of Wartau. It is in the Rätikon range of the Eastern Alps, and reaches a height of.

Geographic entities mentioned:
surface_form: rotspitz
instance_of: Mountain
countries: Liechtenstein
Switzerland
coordinates: lat: 47.05788
lon: 9.55242
Beacon Reservoir supplies water to the city of Beacon, in Dutchess County, New York, United States. It is located at 1,285 feet (392 m) above sea level in a hollow between Beacon Mountain and Scofield Ridge, in the neighboring Town of Fishkill, very close to the Putnam County line. It was created in 1922 by damming Dry Brook, a tributary of Fishkill Creek. It holds.

Geographic entities mentioned:
surface_form: Beacon Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.4812
lon: -73.9449
Highway runs from Interstate 81 (I-81) and Virginia State Route 211 (SR 211) in New Market east to US 15 Business, US 29 Business, and US 211 Business in Warrenton. US 211 connects the Shenandoah Valley with the Piedmont town of Warrenton via Luray and Sperryville, where the highway runs concurrently with US 340 and US 522, respectively. Route description.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
The U.S. Highway expands to a four-lane divided highway after leaving the town of New Market. US 211 becomes a three-lane road, with two lanes in the ascending direction and one on the descending side, for its curvaceous path over Massanutten Mountain, which summits at New Market Gap at the Shenandoah&ndash;Page county line.

Geographic entities mentioned:
surface_form: Massanutten Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.643
lon: -78.612
US 211 expands to a four-lane divided highway again just west of its junction with US 340 at the hamlet of Intersections. The two highways pass through the hamlets of Salem, Whitehouse Landing&mdash;where the highways cross the South Fork Shenandoah River&mdash;and pass Luray Caverns at the west end of the town of Luray.

Geographic entities mentioned:
surface_form: Luray Caverns
instance_of: Landform
countries: United States
coordinates: lat: 38.6643
lon: -78.4838
Lake Wollumboola. Lake Wollumboola is a coastal lake in the Shoalhaven region of New South Wales, Australia. It lies to the immediate south of the town of Culburra Beach and to the north of Jervis Bay. It forms part of Jervis Bay National Park. The lake is separated from the ocean by a berm about wide which breaches only when the lake fills to over above mean sea level. Birds.

Geographic entities mentioned:
surface_form: lake wollumboola
instance_of: Lake
countries: Australia
coordinates: lat: -34.9517
lon: 150.762
The district is home to Muktinath Temple ('lord of liberation or moksha') and is a sacred place for Hindus and Buddhists. The district is a part of Gandaki Province in northern Nepal, straddles the Himalayas and extends northward onto the Tibetan Plateau. The district is one of the remotest areas in Nepal and is second in terms of the sparsity of population.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
The district is a part of Gandaki Province in northern Nepal, straddles the Himalayas and extends northward onto the Tibetan Plateau. The district is one of the remotest areas in Nepal and is second in terms of the sparsity of population. The elevation ranges from 1,372 to 8,167 meters (Mount Dhaulagiri, the 7th highest mountain in the world), with several peaks above 7,000 meters.

Geographic entities mentioned:
surface_form: Dhaulagiri
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.696666666666665
lon: 83.49
The elevation ranges from 1,372 to 8,167 meters (Mount Dhaulagiri, the 7th highest mountain in the world), with several peaks above 7,000 meters. Mustang was an ancient forbidden kingdom, bordered by the Tibetan Plateau and sheltered by some of world's tallest peaks, including 8000-meter tall Annapurna and Dhaulagiri.

Geographic entities mentioned:
surface_form: Annapurna
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.5958
lon: 83.82
surface_form: Dhaulagiri
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.696666666666665
lon: 83.49
Geographically this cold high-altitude steppe is a part of the Tibetan highlands. This boot-shaped piece of land thrusts north into western Tibet is caught in the rain shadow of Dhaulagiri to the south and west and the Annapurna Massif to the north and east. Average elevation of Mustang is 13,200 ft (4,023m), coming to a peak at 8,167m — the summit of Dhaulagiri.

Geographic entities mentioned:
surface_form: Dhaulagiri
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.696666666666665
lon: 83.49
Only about 40.3 square kilometres, about 1 per cent of the total land area, is cultivated and 1,477 square kilometres, about 40%, is pasture land. Kora La at in elevation is considered the lowest drivable path between Tibetan Plateau and Indian subcontinent. The elevation of the district range from 1640m in nearby Kopchepani under Kunjo VDC to 7061m in Nilgiri North above from the sea level.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
The portion of the river directly between Dhaulagiri and Annapurna I (7 km downstream from Tukuche) is at an elevation of, lower than Annapurna I. Major peaks along the gorge include Dhaulagiri (8,167 m or 26,795 ft) and Tukuche (6,920 m or 22,703 ft) on the west and Nilgiri Central (6,940 m or 22,769 ft) and Annapurna (8,091 m or 26,545 ft) on the east. History.

Geographic entities mentioned:
surface_form: Dhaulagiri
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.696666666666665
lon: 83.49
surface_form: Nilgiri Central
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.689166666667
lon: 83.746666666667
surface_form: Annapurna
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.5958
lon: 83.82
According to theory, they may date back to 8–10,000 BCE when Mustang was much greener. In 2007, a shepherd discovered a collection of 55 cave paintings near the village depicting the life of the Buddha. A series of at least twelve caves were discovered north of Annapurna and near the village of Lo Manthang, decorated with ancient Buddhist paintings and set in sheer cliffs at elevation.

Geographic entities mentioned:
surface_form: Annapurna
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.5958
lon: 83.82
Charron Lake (Normandin River). Charron Lake is a freshwater body of the Lac-Ashuapmushuan, Quebec unorganized territory in the northwestern part of the Regional County Municipality (RCM) Le Domaine-du-Roy, in the administrative region of Saguenay-Lac-Saint-Jean, in province of Quebec, in Canada. This lake extends entirely in the canton of Charron.

Geographic entities mentioned:
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: charron lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.40001
lon: -104.28384
The surface of Charron Lake is usually frozen from early November to mid-May, however, safe ice circulation is generally from mid-November to mid-April. Toponymy. Formerly, this lake was designated &quot;lac la Blanche&quot; because of its extension to the north of the current &quot;lac la Blanche&quot; (English: White Lake). The term &quot;Charron&quot; is a family name of French origin.

Geographic entities mentioned:
surface_form: lac la blanche
instance_of: Lake
countries: Canada
coordinates: lat: 45.7236
lon: -75.3194
surface_form: lac la blanche
instance_of: Lake
countries: Canada
coordinates: lat: 45.7236
lon: -75.3194
surface_form: white lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.31
lon: -76.52
surface_form: white lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.819166
lon: -72.271666
Charron Lake (Normandin River). Charron Lake is a freshwater body of the Lac-Ashuapmushuan, Quebec unorganized territory in the northwestern part of the Regional County Municipality (RCM) Le Domaine-du-Roy, in the administrative region of Saguenay-Lac-Saint-Jean, in province of Quebec, in Canada. This lake extends entirely in the canton of Charron.

Geographic entities mentioned:
surface_form: charron lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.40001
lon: -104.28384
surface_form: charron lake (normandin river)
instance_of: Lake
countries: Canada
coordinates: lat: 49.523888888889
lon: -74.156944444444
surface_form: normandin river
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.203333333333
lon: -73.7975
This lake extends entirely in the canton of Charron. Forestry is the main economic activity of the sector. Recreational tourism activities come second. The forest road route 167 linking Chibougamau to Saint-Félicien, Quebec passes on the west shore of Charron Lake. The Canadian National Railway runs along this road.

Geographic entities mentioned:
surface_form: charron lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.40001
lon: -104.28384
Recreational tourism activities come second. The forest road route 167 linking Chibougamau to Saint-Félicien, Quebec passes on the west shore of Charron Lake. The Canadian National Railway runs along this road. The surface of Charron Lake is usually frozen from early November to mid-May, however, safe ice circulation is generally from mid-November to mid-April. Toponymy.

Geographic entities mentioned:
surface_form: charron lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.40001
lon: -104.28384
Genre and historical painting was presented of &quot;A Youth&quot; by Irina Baldina, &quot;Fathers and Sons&quot;, &quot;In native House&quot; by Alexei Eriomin, &quot;A Holiday in the village of Pochinok&quot; by Kirill Ivanov, &quot;Return&quot; by Boris Korneev, &quot;She is doomed&quot; by Gely Korzhev, &quot;Oilers of Pechora&quot;, &quot;Works begin&quot; by Engels Kozlov, &quot;Assemblers&quot; by Yaroslav Krestovsky, &quot;Dawn&quot; by Anatoli Levitin, &quot;May 9&quot;, &quot;Boys&quot;, &quot;They are called by Youth&quot;, &quot;A Speech&quot; by Evsey Moiseenko, &quot;Farewell&quot; by Andrei Mylnikov, &quot;Died a heroic death&quot; by Dmitry Oboznenko, &quot;A Memory&quot; by Lia Ostrova, &quot;Paths - the roads&quot; by Vsevolod Petrov-Maslakov, &quot;September on Mezen River&quot; by Victor Popkov, &quot;Victory Day&quot; by Gleb Savinov, &quot;Liberation&quot; by Fyodor Savostianov, &quot;Swing&quot; by Boris Shamanov, &quot;In the name of Freedom!&quot; by Yuri Tulin, &quot;June of 1941&quot; by Boris Ugarov, &quot;On the fields close to Ladoga Lake&quot; by Vecheslav Zagonek, and some others.

Geographic entities mentioned:
surface_form: Ladoga Lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
Latschensee. Latschensee is a lake in the Bavarian Forest, Bavaria, Germany. It lies at an elevation of 1150 meters and has a surface area of 0.1 hectares. The lake is located in the Bavarian Forest National Park (Nationalpark Bayerischer Wald), which is Germany's first national park and part of the largest single forest area in Central Europe.

Geographic entities mentioned:
surface_form: latschensee
instance_of: Lake
countries: Germany
coordinates: lat: 49.025277777778
lon: 13.397777777778
It lies at an elevation of 1150 meters and has a surface area of 0.1 hectares. The lake is located in the Bavarian Forest National Park (Nationalpark Bayerischer Wald), which is Germany's first national park and part of the largest single forest area in Central Europe. Latschensee is a popular destination for hikers and outdoor enthusiasts, featuring a boardwalk that leads to a scenic overview.

Geographic entities mentioned:
surface_form: latschensee
instance_of: Lake
countries: Germany
coordinates: lat: 49.025277777778
lon: 13.397777777778
Not all houses were destroyed but every single structure had some kind of damage to it that gives each house a historic-artistic value. Since the city was blockaded, nothing could move in or out of the city. The only time people could get food delivered was when Lake Ladoga froze over and soldiers could come in to help the civilians. Public utilities were completely cut off from Leningrad.

Geographic entities mentioned:
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
Barak Democratic Front. The Barak Democratic Front (BDF) is the first regional political party formed in the Barak Valley, in the Indian state of Assam. The main motive of the party is to secure the socio-economic and political rights of the people.

Geographic entities mentioned:
surface_form: Barak Valley
instance_of: Valley
countries: India
coordinates: lat: 24.833333333333332
lon: 92.8
Kentville. Kentville is an incorporated town in Nova Scotia. It is the most populous town in the Annapolis Valley. As of 2021, the town's population was 6,630. Its census agglomeration is 26,929. History. Kentville owes its location to the Cornwallis River which, downstream from Kentville, becomes a large tidal river at the Minas Basin.

Geographic entities mentioned:
surface_form: Annapolis Valley
instance_of: Valley
countries: Canada
coordinates: lat: 44.979166666666664
lon: -64.89222222222222
The area was first settled by Acadians, who built many dykes along the river to keep the high Bay of Fundy tides out of their farmland. These dykes created the ideal fertile soil that the Annapolis Valley is known for. The Acadians were expelled from the area in the Bay of Fundy Campaign (1755) by the British authorities because they would not swear allegiance to the British king.

Geographic entities mentioned:
surface_form: Annapolis Valley
instance_of: Valley
countries: Canada
coordinates: lat: 44.979166666666664
lon: -64.89222222222222
To learn more about important African Nova Scotians of the Town and surrounding areas follow this
Growth. When the Windsor and Annapolis Railway (later named Dominion Atlantic Railway) established its headquarters in Kentville in 1868 and began shipping Annapolis Valley apples to British markets, the community began to thrive.

Geographic entities mentioned:
surface_form: Annapolis Valley
instance_of: Valley
countries: Canada
coordinates: lat: 44.979166666666664
lon: -64.89222222222222
Industries. During the early part of the 20th century Kentville emerged as the business centre of Kings County and despite the post-war loss of commerce to other valley communities, it remains the professional centre of the Annapolis Valley. Kentville is home to numerous professional services such as lawyers offices, doctors, and investment firms.

Geographic entities mentioned:
surface_form: Annapolis Valley
instance_of: Valley
countries: Canada
coordinates: lat: 44.979166666666664
lon: -64.89222222222222
High Mountain (Ramapo Mountains). High Mountain is a mountain on the Bergen and Passaic county line, New Jersey. The peak rises to. It is part of the Ramapo Mountains, and is not to be confused with the like-named High Mountain in the Preakness Range of the Watchung Mountains. High Mountain is partially within Ringwood State Park.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: high mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0887
lon: -74.2351
High Mountain (Ramapo Mountains). High Mountain is a mountain on the Bergen and Passaic county line, New Jersey. The peak rises to. It is part of the Ramapo Mountains, and is not to be confused with the like-named High Mountain in the Preakness Range of the Watchung Mountains. High Mountain is partially within Ringwood State Park.

Geographic entities mentioned:
surface_form: high mountain (ramapo mountains)
instance_of: Mountain
countries: United States
coordinates: lat: 41.0887
lon: -74.2351
High Mountain (Ramapo Mountains). High Mountain is a mountain on the Bergen and Passaic county line, New Jersey. The peak rises to. It is part of the Ramapo Mountains, and is not to be confused with the like-named High Mountain in the Preakness Range of the Watchung Mountains. High Mountain is partially within Ringwood State Park.

Geographic entities mentioned:
surface_form: high mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0887
lon: -74.2351
The word &quot;Deshastha&quot; derives from the Sanskrit &quot;deśa&quot; (inland, country) and &quot;stha&quot; (resident), literally translating to &quot;residents of the country&quot;. The valleys of the Krishna and the Godavari rivers, and a part of Deccan plateau adjacent to the Western Ghats, are collectively termed the &quot;Desha&quot; – the original home of the Deshastha Brahmins.

Geographic entities mentioned:
surface_form: Deccan plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Along with the Karhade and Konkanastha Brahmins, the Marathi-speaking Deshastha Brahmins are referred to as Maharashtrian Brahmins, which denotes those Brahmin subcastes of the Deccan Plateau which have a regional significance in Maharashtra, while the Kannada-speaking Deshastha Brahmins from the Deccan Plateau region of Karnataka are referred to as Karnataka Brahmins or Carnatic Brahmins.

Geographic entities mentioned:
surface_form: Deccan Plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
surface_form: Deccan Plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Deshastha Rigvedi Brahmins are followers of Ashvalayana sutra and Shakala Shakha of Rigveda. Deshastha Rigvedi Brahmins are the most ancient sub-caste among Deshasthas and are found throughout the Deccan. According to Iravati Karve, Deshastha Rigvedi Brahmins are found in western and central Deccan along the banks of the Godavari and the Krishna rivers and are spread deep into Karnataka.

Geographic entities mentioned:
surface_form: western and central Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
The difficulty of the climbs gradually increased, with some stylistic differences between Queensland and NSW climbers, with the former often climbing free solo and NSW climbers relying heavily on ropes. Some of the early bold ascents include &quot;Crater Bluff (9)&quot; by Eric Dark and Dorothy English in 1936, and &quot;Federation Peak (5)&quot; in 1949. Post-WWII.

Geographic entities mentioned:
surface_form: Federation Peak
instance_of: Mountain
countries: Australia
coordinates: lat: -43.271388888889
lon: 146.47555555556
Muanenguba Lakes. Muanenguba lakes are a pair of caldera lakes on Mount Manengouba found in Bangem subdivision in the Kupe-muanenguba Division of the Southwest region of Cameroon. Surrounded by a park of vegetation, it is bounded by the neighboring Littoral region in Cameroon. They sit at an elevation of.

Geographic entities mentioned:
surface_form: Mount Manengouba
instance_of: Mountain
countries: Cameroon
coordinates: lat: 5.03
lon: 9.83
surface_form: kupe
instance_of: Mountain
countries: Cameroon
coordinates: lat: 4.801
lon: 9.707
surface_form: cameroon
instance_of: Mountain
countries: Cameroon
coordinates: lat: 4.2166666666667
lon: 9.1725
surface_form: manengouba
instance_of: Mountain
countries: Cameroon
coordinates: lat: 5.03
lon: 9.83
surface_form: muanenguba lakes
instance_of: Lake
countries: Cameroon
coordinates: lat: 5.03472
lon: 9.82806
Muanenguba Lakes. Muanenguba lakes are a pair of caldera lakes on Mount Manengouba found in Bangem subdivision in the Kupe-muanenguba Division of the Southwest region of Cameroon. Surrounded by a park of vegetation, it is bounded by the neighboring Littoral region in Cameroon. They sit at an elevation of.

Geographic entities mentioned:
surface_form: cameroon
instance_of: Mountain
countries: Cameroon
coordinates: lat: 4.2166666666667
lon: 9.1725
Muanenguba Lakes. Muanenguba lakes are a pair of caldera lakes on Mount Manengouba found in Bangem subdivision in the Kupe-muanenguba Division of the Southwest region of Cameroon. Surrounded by a park of vegetation, it is bounded by the neighboring Littoral region in Cameroon. They sit at an elevation of.

Geographic entities mentioned:
surface_form: muanenguba lakes
instance_of: Lake
countries: Cameroon
coordinates: lat: 5.03472
lon: 9.82806
Lash Wa Juwayn District. Lash wa Juwayn (also transliterated Lash o Jawain) is a district in Farah Province, Afghanistan. The main town, also called Lash wa Juwayn, is situated at 508 m elevation by Daryache-ye Sistan lake.

Geographic entities mentioned:
surface_form: Daryache-ye Sistan
instance_of: Group of lakes
countries: Iran
Afghanistan
coordinates: lat: 30.7653
lon: 61.6372
Ebenezer Mission. Ebenezer Mission, also known as Wimmera mission, Hindmarsh mission and Dimboola mission, was a mission station for Aboriginal people established near Lake Hindmarsh in Victoria, Australia (near Jeparit) in 1859 by the Moravian Church on the land of the Wotjobaluk. The first missionaries were two Germans, Reverend Friedrich Hagenauer and Reverend F.W. Spieseke (c. 1821–1877).

Geographic entities mentioned:
surface_form: Lake Hindmarsh
instance_of: Lake
countries: Australia
coordinates: lat: -36.0667
lon: 141.917
Nordagutu. Nordagutu is a village in Midt-Telemark Municipality in Telemark county, Norway. The village is located along the river Sauarelva, just south of the southern end of the lake Heddalsvatnet. The village of lies about south of the village of Holtsås, about northeast of the village of Akkerhaugen, and just across the river from the village of Sauherad.

Geographic entities mentioned:
surface_form: Heddalsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 59.55805556
lon: 9.2175
Mount Price (British Columbia). Mount Price is a small stratovolcano in the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. It has an elevation of and rises above the surrounding landscape on the western side of Garibaldi Lake in New Westminster Land District.

Geographic entities mentioned:
surface_form: Garibaldi Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.925
lon: -123.01
Mount Price is associated with a small group of volcanoes called the Garibaldi Lake volcanic field. This forms part of the larger Garibaldi Volcanic Belt, a north−south trending volcanic zone that represents a portion of the Canadian Cascade Arc. Mount Price began its formation 1.2million years ago and continued intermittently until sometime in the last 15,000 years.

Geographic entities mentioned:
surface_form: Garibaldi Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5283
lon: -126.113
Geography. Mount Price is located south of Whistler on the western side of Garibaldi Lake in New Westminster Land District. It lies within the Pacific Ranges Ecoregion, a mountainous region of the southern Coast Mountains characterized by high, steep and rugged mountains made of granitic rocks.

Geographic entities mentioned:
surface_form: Garibaldi Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.925
lon: -123.01
surface_form: mount price
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
During winter, cold Arctic air invades from the Central Interior, resulting in extreme cloud cover and snow. A number of other volcanoes are situated within the Eastern Pacific Ranges Ecosection. This includes Mount Meager, which lies near the headwaters of the Lillooet River, and Mount Garibaldi and Mount Cayley, which lie in the Squamish River watershed.

Geographic entities mentioned:
surface_form: Mount Garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Geology. Mount Price is one of the three principal volcanoes in the southern segment of the Garibaldi Volcanic Belt, the other two being Mount Garibaldi and The Black Tusk. Mount Price is also part of the Garibaldi Lake volcanic field. This consists of several volcanoes and lava flows that formed in the last 1.3million years; the oldest volcanic rocks are found at Mount Price and The Black Tusk.

Geographic entities mentioned:
surface_form: Garibaldi Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5283
lon: -126.113
surface_form: The Black Tusk
instance_of: Mountain
countries: Canada
coordinates: lat: 49.97527777777778
lon: -123.04277777777777
surface_form: mount price
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
This retains the Garibaldi Lake system and has been the source of two large landslides in the past. The most recent major landslide in 1855–1856 resulted from failure along vertical rock fractures. It travelled down Rubble Creek to the Cheakamus River valley, depositing of rock. The southwest lava flow is in the upper reaches of the Culliton Creek valley and forms Clinker Ridge.

Geographic entities mentioned:
surface_form: Rubble Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.9708
lon: -123.146
The catchment area for the Greater Vancouver watershed is downwind from Mount Price. An eruption producing floods and lahars could destroy parts of Highway 99, threaten communities such as Brackendale and endanger water supplies from Pitt Lake. Fisheries on the Pitt River would also be at risk.

Geographic entities mentioned:
surface_form: Pitt Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.4167
lon: -122.55
Dacite and rhyolite lavas are normally too viscous to flow away from a volcanic vent, resulting in the formation of lava domes. An exception is the long Ring Creek dacite lava flow from Opal Cone on the southeastern flank of Mount Garibaldi, a length that is normally attained by basaltic lava flows.

Geographic entities mentioned:
surface_form: Opal Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8272
lon: -122.971
Naming. Mount Price has had at least three names throughout its history. It was originally named &quot;Red Mountain&quot; for its red appearance, but the date of when this name was adopted has not been cited. Another peak west of Overlord Mountain was identified as &quot;Red Mountain&quot; on a 1923 sketch by Canadian mountaineer Neal M. Carter.

Geographic entities mentioned:
surface_form: Overlord Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0156
lon: -122.8211
surface_form: red mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
Another peak west of Overlord Mountain was identified as &quot;Red Mountain&quot; on a 1923 sketch by Canadian mountaineer Neal M. Carter. To avoid confusion, the name of that mountain was changed to Fissile Peak on September 2, 1930, for its fissility. In 1952, Canadian volcanologist William Henry Mathews identified Mount Price as &quot;Clinker Mountain&quot; in the American Journal of Science.

Geographic entities mentioned:
surface_form: Fissile Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0186
lon: -122.849
Wildlife such as grey jays, chipmunks, squirrels, flickers, deer, mountain goats, wolverines, cougars and grizzly and black bears are locally present. The communities of Whistler, Pemberton, Mount Currie, Hope and Yale are situated within the Eastern Pacific Ranges Ecosection, all of which are connected to the Lower Mainland by a network of highways. Geology.

Geographic entities mentioned:
surface_form: mount currie
instance_of: Mountain
countries: Canada
coordinates: lat: 50.24861111111111
lon: -122.78194444444445
Mount Price (British Columbia). Mount Price is a small stratovolcano in the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. It has an elevation of and rises above the surrounding landscape on the western side of Garibaldi Lake in New Westminster Land District.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount price (british columbia)
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
Mount Price (British Columbia). Mount Price is a small stratovolcano in the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. It has an elevation of and rises above the surrounding landscape on the western side of Garibaldi Lake in New Westminster Land District.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount price
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
Naming. Mount Price has had at least three names throughout its history. It was originally named &quot;Red Mountain&quot; for its red appearance, but the date of when this name was adopted has not been cited. Another peak west of Overlord Mountain was identified as &quot;Red Mountain&quot; on a 1923 sketch by Canadian mountaineer Neal M. Carter.

Geographic entities mentioned:
surface_form: red mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
These lava flows are structurally unstable, having produced large landslides as recently as the 1850s. A large provincial park surrounds Mount Price and other volcanoes in its vicinity. It lies within an ecological region that surrounds much of the Pacific Ranges. Mount Price is associated with a small group of volcanoes called the Garibaldi Lake volcanic field.

Geographic entities mentioned:
surface_form: mount price
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
It lies within an ecological region that surrounds much of the Pacific Ranges. Mount Price is associated with a small group of volcanoes called the Garibaldi Lake volcanic field. This forms part of the larger Garibaldi Volcanic Belt, a north−south trending volcanic zone that represents a portion of the Canadian Cascade Arc.

Geographic entities mentioned:
surface_form: mount price
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
Mount Price is associated with a small group of volcanoes called the Garibaldi Lake volcanic field. This forms part of the larger Garibaldi Volcanic Belt, a north−south trending volcanic zone that represents a portion of the Canadian Cascade Arc. Mount Price began its formation 1.2million years ago and continued intermittently until sometime in the last 15,000 years.

Geographic entities mentioned:
surface_form: mount price
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
Several coastal islands, channels and fjords occur along the western margin of the Pacific Ranges Ecoregion. The Pacific Ranges Ecoregion is part of the Coast and Mountains Ecoprovince which forms part of the Humid Maritime and Highlands Ecodivision. The Pacific Ranges Ecoregion is subdivided into seven ecosections, the Eastern Pacific Ranges Ecosection being the main ecosection at Mount Price.

Geographic entities mentioned:
surface_form: mount price
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
Geology. Mount Price is one of the three principal volcanoes in the southern segment of the Garibaldi Volcanic Belt, the other two being Mount Garibaldi and The Black Tusk. Mount Price is also part of the Garibaldi Lake volcanic field. This consists of several volcanoes and lava flows that formed in the last 1.3million years; the oldest volcanic rocks are found at Mount Price and The Black Tusk.

Geographic entities mentioned:
surface_form: mount price
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
Mount Price is also part of the Garibaldi Lake volcanic field. This consists of several volcanoes and lava flows that formed in the last 1.3million years; the oldest volcanic rocks are found at Mount Price and The Black Tusk. Several volcanic rocks with differing compositions are present in the Garibaldi Lake volcanic field. This includes andesite, dacite, basaltic andesite and basalt.

Geographic entities mentioned:
surface_form: mount price
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
It is unknown when the last eruption occurred but it may have been in the early Holocene. Although no hot springs are known in the Garibaldi area, there is evidence of anomalously high heat flow in Table Meadows just south of Mount Price and elsewhere. Like other volcanoes in the Garibaldi Volcanic Belt, Mount Price formed as a result of subduction zone volcanism.

Geographic entities mentioned:
surface_form: mount price
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
The best evidence for ongoing subduction is the existence of active volcanism in the Cascade Volcanic Arc. Structure. Mount Price attains an elevation of and is one of several Garibaldi Belt volcanoes that have been volcanically active throughout the Quaternary. In contrast to most stratovolcanoes in Canada, Mount Price has a nearly symmetrical structure.

Geographic entities mentioned:
surface_form: mount price
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
Structure. Mount Price attains an elevation of and is one of several Garibaldi Belt volcanoes that have been volcanically active throughout the Quaternary. In contrast to most stratovolcanoes in Canada, Mount Price has a nearly symmetrical structure. Its western slope is flanked by Clinker Peak, a high parasitic stratovolcano containing a breached volcanic crater.

Geographic entities mentioned:
surface_form: mount price
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
Its western slope is flanked by Clinker Peak, a high parasitic stratovolcano containing a breached volcanic crater. Oxidation of Mount Price's volcanic rocks has given the mountain a red colour. Mount Price stands within a cirque-like basin cut into the plateau on the south side of the valley of Garibaldi Lake.

Geographic entities mentioned:
surface_form: mount price
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
Oxidation of Mount Price's volcanic rocks has given the mountain a red colour. Mount Price stands within a cirque-like basin cut into the plateau on the south side of the valley of Garibaldi Lake. This basin consists of a wall of granite, inclosing the volcano on its west and southwest sides.

Geographic entities mentioned:
surface_form: mount price
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
This basin consists of a wall of granite, inclosing the volcano on its west and southwest sides. It is now almost completely filled up by Mount Price, but some small areas of its floor are exposed on the north side. The basin likely formed as a result of glacial action as its north side appears to have been almost certainly glaciated.

Geographic entities mentioned:
surface_form: mount price
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
Volcanic history. At least three phases of eruptive activity have been identified at Mount Price. The first eruptive phase 1.2million years ago deposited hornblende andesite lava and pyroclastic rocks on the floor of the cirque-like basin after an Early Pleistocene glacial event.

Geographic entities mentioned:
surface_form: mount price
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
The first eruptive phase 1.2million years ago deposited hornblende andesite lava and pyroclastic rocks on the floor of the cirque-like basin after an Early Pleistocene glacial event. During the Middle Pleistocene about 300,000 years ago, volcanism of the second phase shifted westward and constructed the nearly symmetrical stratovolcano of Mount Price.

Geographic entities mentioned:
surface_form: mount price
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
After the Cordilleran Ice Sheet retreated from higher elevations less than 15,000 years ago, andesite eruptions of the third eruptive phase occurred from a satellite vent at Price Bay. These eruptions resulted in the creation of a small lava dome or scoria cone on Mount Price's northern flank with an elevation of.

Geographic entities mentioned:
surface_form: mount price
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
Both lava flows form steep cliffs; the current face of The Barrier is a result of the mid-19th century landslide. Volcanic hazards. Mount Price is one of the four highest threat volcanoes in Canada situated within close proximity to major populations with critical civil and economic infrastructure, the other three being Mount Meager, Mount Garibaldi and Mount Cayley.

Geographic entities mentioned:
surface_form: mount price
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556