Sarmila/GeoWiki-Features huggingface dataset:
Mount Dangar. Mount Dangar is prominent basalt peak at the eastern edge of the Goulburn River National Park, north-west of Denman, New South Wales. It has an elevation of AHD, and the first man of European descent to report a sighting was the surveyor Henry Dangar in October 1824, following his exploration of the confluence of the Goulburn and Hunter Rivers.

Geographic entities mentioned:
surface_form: mount dangar
instance_of: Mountain
countries: Australia
coordinates: lat: -32.336666666666666
lon: 150.48694444444445
Dangar named the domed shaped mountain Mount Cupola. In April 1825, botanist and explorer, Allan Cunningham, renamed the mountain Mount Dangar, when he ascended the mountain during his second northwest expedition to the Liverpool Plains. &quot;Acacia dangarensis&quot; (Mount Dangar wattle) occurs within the Goulburn River National Park.

Geographic entities mentioned:
surface_form: mount dangar
instance_of: Mountain
countries: Australia
coordinates: lat: -32.336666666666666
lon: 150.48694444444445
Mount Dangar is prominent basalt peak at the eastern edge of the Goulburn River National Park, north-west of Denman, New South Wales. It has an elevation of AHD, and the first man of European descent to report a sighting was the surveyor Henry Dangar in October 1824, following his exploration of the confluence of the Goulburn and Hunter Rivers. Dangar named the domed shaped mountain Mount Cupola.

Geographic entities mentioned:
surface_form: hunter
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
He wrote, &quot;The Hare Indian or Mackenzie River Dog bears the same relation to the prairie wolf [coyote] as the Esquimeaux Dog [Malamute] does to the great grey wolf.&quot; The breed seemed to be kept exclusively by the Hare Indians and other neighboring tribes, such as the Bear, Mountain, Dogrib, Cree, Slavey and Chippewa tribes living in the northwestern territories of Canada and the United States around the Great Bear Lake, Southwest to Lake Winnipeg and Lake Superior and West to the Mackenzie River.

Geographic entities mentioned:
surface_form: Great Bear Lake
instance_of: Lake
countries: Canada
coordinates: lat: 66
lon: -121
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Balatonföldvár. Balatonföldvár (,) is a popular resort town in Somogy County, Hungary, on the southern side of Lake Balaton, approximately 120 km southwest from Budapest and about 23 km southwest from Siófok, the &quot;capital of Balaton&quot;.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
Etymology. The origin of the name &quot;Balatonföldvár&quot; is from Lake Balaton, the lake bordering the town, and the &quot;földvár&quot; (in English &quot;earth castle&quot;). The &quot;földvár&quot; was built in the late Iron Age, during the occupation of the Celts.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
History. In around the 4th century AD, the area was settled by Celts, who constructed the large Iron Age hill fort that gives Balatonföldvár its name, the remains of which are still visible today. The region around Lake Balaton was occupied in around 180 AD by the Romans and was situated on a military road from Aquincum (part of present-day Budapest) to the Italian peninsula.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
It then descends to cross the West Branch Susquehanna River. North-Central Pennsylvania. I-80 enters Centre County around milemarker 138. I-80 descends Allegheny Mountain into the Nittany Valley, intersecting Future I-99/U.S. Route 220 (US 220) at exit 161, the main connecting point to the Pennsylvania Turnpike (I-70/I-76), Pennsylvania State University, and State College.

Geographic entities mentioned:
surface_form: Nittany Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.9
lon: -77.7
US 220 is concurrent between exits 161 and 178 where it heads toward Lock Haven, home to Lock Haven University of Pennsylvania. I-80 then ascends Sugar Valley Mountain and then follows White Deer Creek down to the West Branch Susquehanna River, which I-80 crosses a second time.

Geographic entities mentioned:
surface_form: Sugar Valley Mountain
instance_of: Valley
countries: United States
coordinates: lat: 40.9794
lon: -77.4867
Mount Kemul. Mount Kemul (also Kemoel, Kemal, Kongkemul, Kong Kemul) () is a mountain in East Kalimantan. It is the type locality of the pitcher plant species &quot;Nepenthes fusca&quot; and &quot;Nepenthes mollis&quot;.

Geographic entities mentioned:
surface_form: mount kemul
instance_of: Mountain
countries: Indonesia
coordinates: lat: 1.8602777777778
lon: 116.17638888889
Mount Kemul. Mount Kemul (also Kemoel, Kemal, Kongkemul, Kong Kemul) () is a mountain in East Kalimantan. It is the type locality of the pitcher plant species &quot;Nepenthes fusca&quot; and &quot;Nepenthes mollis&quot;.

Geographic entities mentioned:
surface_form: mount kemul
instance_of: Mountain
countries: Indonesia
coordinates: lat: 1.8602777777778
lon: 116.17638888889
surface_form: kemoel
instance_of: Mountain
countries: Indonesia
coordinates: lat: 1.8602777777778
lon: 116.17638888889
The airmail letter received a positive reply within a fortnight. Digby continued to enjoy the favour of the new Indian ruling class, she was a guest of President Rajendra Prasad at his Republic Day 'at home' on her return to India in 1958. Digby based herself on a houseboat on the Dal Lake during two long visits to India in 1952/3 and 1957/8.

Geographic entities mentioned:
surface_form: Dal Lake
instance_of: Lake
countries: India
coordinates: lat: 34.12
lon: 74.87
An RNZAF Radar Unit operated on the island as a navigational aid, and it became a stopover for aircraft travelling between Australia, New Caledonia, New Zealand and the Solomon Islands. The RNZAF left the airfield in July 1946. At the airfield was an air-sea rescue unit, a servicing section and a radar unit installation at Mount Bates. Light aircraft transit.

Geographic entities mentioned:
surface_form: Mount Bates
instance_of: Mountain
countries: Australia
coordinates: lat: -29.0112306
lon: 167.939961
Geography. The region shown in the map below is a part of the undulating uplands bustling with coalmines. The Damodar River, the most important river of the Chota Nagpur Plateau, flows along the southern border. The area beyond the Damodar was once a part of Dhanbad district but was transferred to Bokaro district in 2001.

Geographic entities mentioned:
surface_form: Chota Nagpur Plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
Unlike the Mount of Olives and Har HaMenuchot cemeteries that are located on the outer edges of the city, Sanhedria Cemetery is situated in the heart of western Jerusalem, in proximity to residential housing. It is operated under the jurisdiction of the Kehilat Yerushalayim &quot;chevra kadisha&quot; (burial society) and accepts Jews from all religious communities.

Geographic entities mentioned:
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
surface_form: Har HaMenuchot
instance_of: Mountain
countries: Israel
coordinates: lat: 31.798133333333
lon: 35.177727777778
As of the 2000s, the cemetery is nearly filled to capacity. History. Until 1948, Jewish burials in Jerusalem were conducted in the centuries-old Jewish cemetery on the Mount of Olives. In January 1948, the Arab siege of Jerusalem made the Mount of Olives inaccessible, as the route to the cemetery passed through hostile Arab villages.

Geographic entities mentioned:
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
Following this event, Brahma and Vishnu worshipped Shiva, who named the day Shivaratri; he also prescribed the veneration of the lingam as his phallic emblem towards the achievement of salvation. The &quot;Lingashtaka&quot; also references other legends of Shiva, such as the quelling of the pride of Ravana when the latter attempted to lift Mount Kailash, and the destruction of Daksha's yajna.

Geographic entities mentioned:
surface_form: Mount Kailash
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 31.066944444444
lon: 81.312777777778
From 2018 to 2021, Burnside was the national hockey writer for &quot;The Athletic&quot;. During this time, he wrote about the rise and fall of goaltender Ray Emery, who drowned in Lake Ontario at age 35. Burnside joined &quot;Daily Faceoff&quot; in October 2021 as a senior writer.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Pasjača (mountain). Pasjača (Serbian Cyrillic: Пасјача) is a mountain in southern Serbia, near the town of Žitorađa. Its highest peak has an elevation of 971 meters above sea level.

Geographic entities mentioned:
surface_form: пасјача
instance_of: Mountain
countries: Serbia
coordinates: lat: 43.165
lon: 21.62194444
surface_form: pasjača
instance_of: Mountain
countries: Serbia
coordinates: lat: 43.165
lon: 21.62194444
Pasjača (mountain). Pasjača (Serbian Cyrillic: Пасјача) is a mountain in southern Serbia, near the town of Žitorađa. Its highest peak has an elevation of 971 meters above sea level.

Geographic entities mentioned:
surface_form: pasjača (mountain)
instance_of: Mountain
countries: Serbia
coordinates: lat: 43.165
lon: 21.62194444
Twin Goat Mountain is located east of Pemberton in the Lillooet Ranges of the Coast Mountains. Precipitation runoff from this mountain drains into tributaries of the Lillooet River. Twin Goat Mountain is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 1,928 metres (6,325 ft) above Lillooet Lake in.

Geographic entities mentioned:
surface_form: Lillooet Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.25
lon: -122.5
surface_form: twin goat mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.28302
lon: -122.48598
surface_form: goat mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.4036
lon: -123.079
Twin Goat Mountain. Twin Goat Mountain is a summit in British Columbia, Canada. Description. Twin Goat Mountain is located east of Pemberton in the Lillooet Ranges of the Coast Mountains. Precipitation runoff from this mountain drains into tributaries of the Lillooet River.

Geographic entities mentioned:
surface_form: twin goat mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.28302
lon: -122.48598
surface_form: goat mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.4036
lon: -123.079
Twin Goat Mountain. Twin Goat Mountain is a summit in British Columbia, Canada. Description. Twin Goat Mountain is located east of Pemberton in the Lillooet Ranges of the Coast Mountains. Precipitation runoff from this mountain drains into tributaries of the Lillooet River.

Geographic entities mentioned:
surface_form: twin goat mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.28302
lon: -122.48598
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: goat mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.4036
lon: -123.079
Climate. Based on the Köppen climate classification, Twin Goat Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (orographic lift), causing them to drop their moisture in the form of rain or snowfall.

Geographic entities mentioned:
surface_form: twin goat mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.28302
lon: -122.48598
surface_form: goat mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.4036
lon: -123.079
USS Liberty (1775). USS &quot;Liberty&quot; was an 8-gun schooner of the Continental Navy. She was originally the civilian vessel &quot;Katherine&quot;, built at Skenesboro, New York on Lake Champlain, for wealthy landowner and former British Army Captain Philip Skene. It was captured on May 11, 1775, during a raid on Skenesboro led by Capt.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Pratt's vole. Pratt's vole (&quot;Eothenomys chinensis&quot;), also called the Sichuan red-backed vole, is a species of rodent in the family Cricetidae. It is endemic to Mount Emei, Sichuan, China. It was named in 1891 for Antwerp Edgar Pratt.

Geographic entities mentioned:
surface_form: Mount Emei
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 29.519722222222
lon: 103.3325
Tillamook Head towers over the southern edge of the city. The geography associated with the gradual slope of the broad sandy beaches of Clatsop Spit provide excellent conditions for the formation of beds of millions of Pacific razor clams annually. The razor clams attract thousands of visitors to Seaside Beach each year. Waves attract surfers all year round to the sandy shores. Climate.

Geographic entities mentioned:
surface_form: Clatsop Spit
instance_of: Landform
countries: United States
coordinates: lat: 46.2289
lon: -124.014
His father, along with 20 other family members, stayed in Srebrenica and would end up as some of the more than 8,000 victims of the Srebrenica massacre - his father's remains are yet to be discovered. Irvin, with his mother and siblings, was welcomed in Italy, as a war refugee, in the Val Camonica area. Irvin lived in Italy for more than 20 years, in a small village in the Alps.

Geographic entities mentioned:
surface_form: Val Camonica
instance_of: Valley
countries: Italy
coordinates: lat: 46.0075
lon: 10.3475
It also hosts several archaeological sites related to World War I, including British trench warfare sites. Geography. Monte Zovetto lies within the municipality of Roana (in the province of Vicenza), one of the seven municipalities that make up the Asiago Plateau, with a population of approximately 4,299 residents. The closest locality is Cesuna, in the municipality of Roana.

Geographic entities mentioned:
surface_form: Asiago Plateau
instance_of: Plateau
countries: Italy
coordinates: lat: 45.9
lon: 11.5
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
It was only after the defeat at Caporetto on 24 October 1917 and the retreat of the Italian army to the Altopiano–Grappa–Piave line, that the Allies provided substantial support to Italy (a British Expeditionary Force as well as six French divisions were sent to Italy), trying to stop the Austro-Hungarians from advancing into the Po Valley and possibly towards the southern French border.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
surface_form: po valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
surface_form: grappa
instance_of: Mountain
countries: Italy
coordinates: lat: 45.873333333333
lon: 11.799166666667
The main slope Zovetto 1 was 2.6 kilometers long, and it was classified as easy. In 2014 the &quot;Sette Comuni&quot; organized into the &quot;Comunità Montana dell'Altopiano dei Sette Comuni&quot; (&quot;Mountain Community of the Plateau of the Seven Municipalities&quot;) to serve as the administrative body for the Asiago Plateau.

Geographic entities mentioned:
surface_form: Sette Comuni
instance_of: Plateau
countries: Italy
coordinates: lat: 45.9
lon: 11.5
The Brigata Liguria also distinguished itself on. After more than a year in the Venetian Pre-alps, under the command of future General Achille Papa, the brigade was transferred in 1917 to Bainsizza, where they received another gold medal for military valor. Cippo Bignami. The Cippo Bignami is a monument at the base of Monte Zovetto.

Geographic entities mentioned:
surface_form: Bainsizza
instance_of: Plateau
countries: Slovenia
coordinates: lat: 46.04905
lon: 13.69995
In 1310, Monte Zovetto became part of the &quot;Spettabile Reggenza dei Sette Comuni&quot; (&quot;Esteemed Regency of the Seven Municipalities&quot;), an autonomous federal government established to safeguard the independence of the communities on the Asiago Plateau. During this period, Venice expanded inland, acquiring territories such as Vicenza, Bassano del Grappa, and the Altopiano.

Geographic entities mentioned:
surface_form: sette comuni
instance_of: Plateau
countries: Italy
coordinates: lat: 45.9
lon: 11.5
In 1310, Monte Zovetto became part of the &quot;Spettabile Reggenza dei Sette Comuni&quot; (&quot;Esteemed Regency of the Seven Municipalities&quot;), an autonomous federal government established to safeguard the independence of the communities on the Asiago Plateau. During this period, Venice expanded inland, acquiring territories such as Vicenza, Bassano del Grappa, and the Altopiano.

Geographic entities mentioned:
surface_form: grappa
instance_of: Mountain
countries: Italy
coordinates: lat: 45.873333333333
lon: 11.799166666667
Monte Zovetto. Monte Zovetto (Mount Zovetto) (BrE: is a mountain in the Pre-Alps, more specifically within the Vicentine Alps, in the northern Italian region of Veneto. It has a summit elevation of 1,232 m (4,042 ft) above sea level. The area is known for various activities such as hiking and mountain biking.

Geographic entities mentioned:
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
Triassic Period (about 250–200 million years ago). The geological foundation of Monte Zovetto dates back to the Late Triassic, a period during which the first stages of sedimentary deposition occurred in the area. At this time, the region was submerged in a shallow sea, which facilitated the deposition of dolomites and limestone, forming the base of the mountain's geology.

Geographic entities mentioned:
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
At this time, the region was submerged in a shallow sea, which facilitated the deposition of dolomites and limestone, forming the base of the mountain's geology. The main lithological unit characterizing Monte Zovetto is the Main Dolomite, a resistant carbonate rock that forms a solid base for the mountain.

Geographic entities mentioned:
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
Jurassic Period (about 200–145 million years ago). During the Early Jurassic, the region underwent a phase of geological change, during which the dolomite sediments were covered by layers of gray limestone. This limestone, mainly consisting of fine-grained micritic limestone, less resistant to erosion compared to the dolomites, contribute to the composition of Monte Zovetto.

Geographic entities mentioned:
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
Alpine Orogeny (about 35–25 million years ago). The morphological evolution of Monte Zovetto underwent a significant transformation from the Late Cretaceous to the Tertiary, during the process of Alpine orogeny. This event was triggered by the collision between the African plate and the Eurasian plate, causing the uplift, folding, and fracturing of the pre-existing sedimentary formations.

Geographic entities mentioned:
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
The uplift of the pre-existing dolomites and limestone led to the creation of the mountain ranges that now form the Asiago Plateau. The tectonic movement also generated a series of faults and folds, which have shaped the geological structure of Monte Zovetto. Pleistocene and Holocene (about 3 million years ago).

Geographic entities mentioned:
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
Pleistocene and Holocene (about 3 million years ago). During the Pleistocene and Holocene, the region experienced further landscape modification, primarily due to glaciations. Although the area of Monte Zovetto was not directly covered by glaciers, the colder climate favored glacial erosion and the ablation of debris, contributing to the reorganization of the landscape.

Geographic entities mentioned:
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
The karst phenomenon, intensified by abundant precipitation and surface waters, continued to shape the land, creating sinkholes and caves. These are a distinctive element of Monte Zovetto's landscape, reflecting the continuous interaction between the local geology and chemical erosion processes. The underground karst cavities also provide a habitat for various animal species.

Geographic entities mentioned:
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
The underground karst cavities also provide a habitat for various animal species. The Monte Zovetto stromatolite horizon, referred to as the 'Zovetto Horizon', is a prominent geological feature characterized by a continuous layer of stromatolites. This horizon is believed to have formed in a shallow, warm marine or lacustrine setting, where conditions supported the growth of microbial mats.

Geographic entities mentioned:
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
These mats played a role in the stabilization of sediments and the development of the layered stromatolitic structures. Climate. At the elevation of Monte Zovetto, the climate exhibits a mountainous temperate regime, with cool summers and cold winters. Summer temperatures are mild, typically ranging from 15°C to 25°C (59°F to 77°F).

Geographic entities mentioned:
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
The plateau generally experiences an annual precipitation ranging from 1400 mm (55 in) to 2000 mm (78 in), with rainfall occurring fairly evenly throughout the year. Strong southern winds have caused significant environmental damage in the Asiago Plateau, including Monte Zovetto. These air currents have flattened extensive coniferous forests, altering the landscape. Air quality.

Geographic entities mentioned:
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
These air currents have flattened extensive coniferous forests, altering the landscape. Air quality. On Monte Zovetto, pollution sources are fewer compared to the plains below, resulting in good air quality. Local air pollution in general is attributed to activities such as fossil fuel production and use, industrial manufacturing, mineral extraction, waste incineration and agricultural practices.

Geographic entities mentioned:
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
The etymology of the name Zovetto may also have local or dialectal origins. Ancient history. Human presence in the area of Monte Zovetto dates back to prehistoric times in the Middle Paleolithic, when Neanderthals (50,000–40,000 years ago) inhabited the Roana region. Between 15,000 and 10,000 years ago this area became a site of human settlement.

Geographic entities mentioned:
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
Between 15,000 and 10,000 years ago this area became a site of human settlement. In the 14th–13th centuries BC, during the Bronze Age, a fortified village was established on Mount Cornion in the municipality of Lusiana. The first evidence of permanent settlements close to Monte Zovetto, dates to the late Iron Age (between the end of the 5th and the early 1st century BC) at Castelletto di Rotzo.

Geographic entities mentioned:
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
Roman sites have been found in the Lusiana and Rotzo areas. Under the Romans, the area of the Asiago Plateau and the Monte Zovetto region was organized as public grazing lands. The evidence of transhumance and the lack of permanent settlements in the region suggest that the Romans utilized the land for collective purposes, including summer grazing and forest exploitation. Middle Ages.

Geographic entities mentioned:
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
These collective traditions persisted when the Franks gained control of the area. In the 9th century, the population of the area began to increase, as German-speaking communities established settlements on Monte Zovetto and the surrounding mountains. It was during this time that the Cimbrian language, a Germanic language still in use today in Roana, emerged on the mountain.

Geographic entities mentioned:
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
Historically, this language was widely spoken across the mountainous area between the Adige and Brenta rivers. The history of Monte Zovetto and its surrounding area was shaped by feudalism and ecclesiastical power. In 915, the bishop of Padua was granted dominion over the Brenta valley, restoring Padua's control over the plateau.

Geographic entities mentioned:
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
During this period, Venice expanded inland, acquiring territories such as Vicenza, Bassano del Grappa, and the Altopiano. The 1378–1381 War of Chioggia marked a turning point for Venice, and in 1405, the towns of the Plateau, including the Monte Zovetto area, formally pledged allegiance to Venice, becoming part of the Republic, though with special privileges.

Geographic entities mentioned:
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
The Republic of Venice aimed to maintain control of the region and secure its borders, but the ongoing European wars influenced this area. After the fall of the Republic of Venice in 1797, Monte Zovetto region fell under French domination as part of Napoleon's territorial reorganization of Italy. This marked the fall of Venetian rule in the region.

Geographic entities mentioned:
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
By 5 and 6 June the Liguria, Forli, Pescara and Catanzaro brigades, had retreated to defensive positions from Lemerle to Monte Zovetto, Val Magnaboschi and Mount Pau in the southern part of the Asiago Plateau. The 33rd Division, along with the Liguria brigade, had arrived in the Vicenza region as a reserve force in early June.

Geographic entities mentioned:
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
The Italian victory not only marked the conclusion of the war on the Italian Front but also resulted in the collapse of the Austro-Hungarian Empire. By that time, the area had been fortified, and these well-preserved defences remain visible on Monte Zovetto to this day.

Geographic entities mentioned:
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
After World War II. The area experienced a decline in living conditions after the collapse of Fascism, leading to a significant wave of emigration. The 1960s marked a turning point as the economy began to recover, driven by the growth of tourism: villas and apartments were built on Monte Zovetto and commercial activities expanded.

Geographic entities mentioned:
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
The 1960s marked a turning point as the economy began to recover, driven by the growth of tourism: villas and apartments were built on Monte Zovetto and commercial activities expanded. Until 2014 Monte Zovetto was the site of the Cesuna Ski Resort, at an altitude of 1,087 m to 1,232 m, with a vertical drop of 145 meters.

Geographic entities mentioned:
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
The first gold medal was awarded for events in 1916 during the Strafexpedition, when the brigade held out against Austrian attacks on the Asiago Plateau, along the line between Monte Zovetto and Mount Lemerle, near Cesuna, in the municipality of Roana. The brigade suffered over 3,000 casualties, later reinterred at the Asiago War Memorial at Leiten after the war.

Geographic entities mentioned:
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
surface_form: monte zovetto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.82585
lon: 11.4531
He studied the geodynamics of the extensional basins in North China and their connection to the 1976 Tangshan earthquake. In the 1990s, Zeng organized the first Sino-American joint project to investigate the crust and upper mantle of the Tibetan Plateau and the collision process of the Indian Plate with the Eurasian Plate.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Adding to the challenges facing the 1997 team, Michigan entered the season with the toughest schedule among the 112 NCAA Division I-A schools based on records from the previous year. Days before the season opener, Lloyd Carr compared the daunting schedule to an expedition to Mount Everest. Carr noted, &quot;It's a little akin to climbing Mount Everest. But Mount Everest has been climbed.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Taxonomy and naming. &quot;Prasophyllum suttonii&quot; was first formally described in 1912 by Richard Sanders Rogers and Bertha Rees and the description was published in &quot;Proceedings of the Royal Society of Victoria&quot; from a specimen collected on Mount Buffalo.

Geographic entities mentioned:
surface_form: Mount Buffalo
instance_of: Mountain
countries: Australia
coordinates: lat: -36.777
lon: 146.767
Tsiribihina River. The Tsiribihina is a river of western Madagascar. The main tributaries are the Mahajilo, Manandaza, Mania, and Sakeny rivers. Its basin has an area of 49,800 km2. 7,025 km2 is in the basin of the Sakeny River, 14,500 km2 in that of the Mahajilo River, and 18,565 km2 in that of the Mania River. The headwaters are on Madagascar's Central Highlands.

Geographic entities mentioned:
surface_form: tsiribihina river
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -19.8833
lon: 44.45
Tsiribihina River. The Tsiribihina is a river of western Madagascar. The main tributaries are the Mahajilo, Manandaza, Mania, and Sakeny rivers. Its basin has an area of 49,800 km2. 7,025 km2 is in the basin of the Sakeny River, 14,500 km2 in that of the Mahajilo River, and 18,565 km2 in that of the Mania River. The headwaters are on Madagascar's Central Highlands.

Geographic entities mentioned:
surface_form: tsiribihina
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -19.8833
lon: 44.45
The headwaters are on Madagascar's Central Highlands. The tributary streams flow generally westwards except for the Sakeny, which flows northwards. As they leave the highlands and enter the north–south running Betsiriry Plain, the tributary rivers converge to form the Tsiribihina - the Mahajilo and Manandaza from the north, and the Mania and Sakeny from the south.

Geographic entities mentioned:
surface_form: tsiribihina
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -19.8833
lon: 44.45
The plain's wetlands and lakes are important habitat for waterbirds. The Tsiribihina then flows westward, cutting a steep and winding gorge through the Bemaraha Plateau, a limestone formation that extends north and south along the western edge of the Betsiriry Plain. As the river emerges from the Bemaraha Plateau it widens and meanders.

Geographic entities mentioned:
surface_form: tsiribihina
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -19.8833
lon: 44.45
The saltflats often flood during the rainy season. The freshwater marshes and lakes of the lower Tsiribihina are dominated by the sedges &quot;Cyperus&quot; spp, the reed &quot;Phragmites&quot;, and non-native water-hyacinth &quot;Eichhornia&quot;. The mouth of the river is near Belon'i Tsiribihina, where it empties into the Mozambique Channel.

Geographic entities mentioned:
surface_form: tsiribihina
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -19.8833
lon: 44.45
surface_form: tsiribihina
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -19.8833
lon: 44.45
A few pairs of Madagascar fish eagle (&quot;Haliaeetus vociferoides&quot;) live along the river. The Menabe Antimena protected area covers the south bank of the lower Tsiribihina along with the delta and mangroves.

Geographic entities mentioned:
surface_form: tsiribihina
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -19.8833
lon: 44.45
The Menabe Antimena protected area covers the south bank of the lower Tsiribihina along with the delta and mangroves. The Tsiribihina Delta is designated a wetland of international importance under the Ramsar Convention, and the Tsiribihina River and its delta are designated an Important Bird Area by Birdlife International.

Geographic entities mentioned:
surface_form: tsiribihina river
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -19.8833
lon: 44.45
The depot was demolished around 1990. Just beyond the north end of the Magic Mountain parking lot is the site of the adobe ranch house for the historic Rancho San Francisco, a Mexican land grant that encompassed the Santa Clarita Valley from Piru to Canyon Country.

Geographic entities mentioned:
surface_form: Santa Clarita Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.398
lon: -118.522
The other ships arrived by the 26th. Vancouver sailed south along the coast of Alta California, visiting Chumash villages at Point Conception and near Mission San Buenaventura. Bodega y Quadra offered to facilitate another message via New Spain (Mexico) and the Atlantic route, however Vancouver sent Lt. Broughton.

Geographic entities mentioned:
surface_form: Point Conception
instance_of: Landform
countries: United States
coordinates: lat: 34.448113
lon: -120.471439
They reached Fitz Hugh Sound on 26 May, arriving at what Vancouver named Restoration Cove two days later. Vancouver, with two of the boats, explored Cascade, Cousins and Roscoe Inlets and Fisher and Dean Channels, while Johnstone explored Burke Channel and North and South Bentinck Arms. The former, in passing the north point of what he named King Island, proved its insular nature.

Geographic entities mentioned:
surface_form: Fisher
instance_of: Watercourse
countries: Canada
coordinates: lat: 52
lon: -127.925
He returned 3 July, having circumnavigated what was named &quot;Hawkesbury's Island&quot; (which was really four islands: Gribbell, Loretta, Hawkesbury, and Maitland Islands) and explored Gardner Canal, Ursula, Devastation and Douglas Channels and Kitimat and Kildala Arms. After dispatching Whidbey and Barrie to the north, the ships anchored off the north coast of Gil Island.

Geographic entities mentioned:
surface_form: Douglas Channel
instance_of: Watercourse
countries: Canada
coordinates: lat: 53.666666666667
lon: -129.13333333333
While Vancouver explored to the heads of Portland Canal, Fillmore and Nakat Inlets, and Boca de Quadra and circumnavigated Revillagigedo Island (during which he was attacked by Tlingit near what was named Escape Point, having two of his men injured), Johnstone and Barrie explored the channels to the southeast, including Work Channel and Khutzeymateen and Quottoon Inlets.

Geographic entities mentioned:
surface_form: Nakat Inlet
instance_of: Landform
countries: United States
coordinates: lat: 54.89388889
lon: -130.74138889
On 6 September, a few days after his return, they weighed anchor, sailing to what was named Port Protection, on the northwest coast of Prince of Wales Island—which they reached a couple days later. The boats were once again sent out: Johnstone charted the south coast of Kupreanof Island, while Whidbey explored the southeast part of Kuiu Island, reaching the head of Affleck Canal.

Geographic entities mentioned:
surface_form: Affleck Canal
instance_of: Landform
countries: United States
coordinates: lat: 56.17833333
lon: -134.06972222
The armaments may have aided Kamehameha's decisive victory at Battle of Nu'uanu, allowing him to unify the islands. The expedition left Hawaii for the final time on 15 March 1794. They spent late April and early May charting the furthest reaches of what Vancouver renamed Cook Inlet; Vancouver himself reached the head of Knik Arm, while Whidbey reached the head of Turnagain Arm.

Geographic entities mentioned:
surface_form: Knik Arm
instance_of: Body of water
countries: United States
coordinates: lat: 61.2
lon: -150.217
Flowering plants in the north include yellow poppy, &quot;Pedicularis&quot;, and &quot;Pyrola&quot;. Plant life in southern Greenland is more abundant, and certain plants, such as the dwarf birch and willow, may grow several feet high. The only natural forest in Greenland is found in the Qinngua Valley.

Geographic entities mentioned:
surface_form: Qinngua Valley
instance_of: Valley
countries: Greenland
coordinates: lat: 60.301944444444
lon: -44.475
Kural inscriptions and other historical records are found across Tamil Nadu. The 15th-century Jain inscriptions in the Ponsorimalai near Mallur in Salem district bear couplet 251 from the &quot;Shunning meat&quot; chapter of the Kural text, indicating that the people of the Kongu Nadu region practiced ahimsa and non-killing as chief virtues.

Geographic entities mentioned:
surface_form: Ponsorimalai
instance_of: Mountain
countries: India
The tallest of these is the stone statue of Valluvar erected in 2000 atop a small islet in the town of Kanyakumari on the southernmost tip of the Indian peninsula, at the confluence of the Bay of Bengal, the Arabian Sea, and the Indian Ocean. This statue is currently India's 25th tallest.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
There is also daily Amtrak Thruway bus service (operated by Coach USA) at the station, operating between the Buffalo Metropolitan Transportation Center and Jamestown station in Jamestown, New York, via Dunkirk and Fredonia, and serving the communities along the southeast shore of Lake Erie.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Johore Wooden Railway. It was said that the history of Johor railway developments started in the 1869 where Sultan Abu Bakar (then still Maharaja) officiated construction of Johore Railway, which line are planned to be built northwards towards Gunung Pulai, 18 miles from the terminus here.

Geographic entities mentioned:
surface_form: Gunung Pulai
instance_of: Mountain
countries: Malaysia
coordinates: lat: 1.6
lon: 103.55
Inside this protected channel it is possible to navigate the entire 1,600 km length of the Norwegian coast from North Cape to Stavanger. Such coastlines, sometimes known as Leadsa rough English translation for the common Norwegian nautical term Ledene (shipping lane) are common around ScandinaviaSkjaergaard also exist along the Swedish and Finnish Baltic coasts and off Greenland.

Geographic entities mentioned:
surface_form: and off Greenland
instance_of: Mountain
countries: Greenland
coordinates: lat: 68.1683
lon: -31.7169
Sal Glacier. Sal Glacier () is a glacier, long, flowing north between Salen Mountain and Mount Bergersen in the Sor Rondane Mountains. It was mapped by Norwegian cartographers in 1957 from air photos taken by U.S. Navy Operation Highjump, 1946–47, and named Salbreen (the saddle glacier), probably for its association with Salen Mountain.

Geographic entities mentioned:
surface_form: Salen Mountain
instance_of: Mountain
coordinates: lat: -72.0833
lon: 25.45
surface_form: Mount Bergersen
instance_of: Mountain
coordinates: lat: -72.066666666667
lon: 25.8
Bravo Glacier. Bravo Glacier is a glacier on Greenwich Island in the South Shetland Islands, Antarctica extending 2.1 km in northwest-southeast direction and 2.3 km in southwest-northeast direction and draining the south slopes of Dryanovo Heights to flow southeastwards into Shopski Cove.

Geographic entities mentioned:
surface_form: Dryanovo Heights
instance_of: Mountain
coordinates: lat: -62.480555555556
lon: -59.869444444444
It is the northernmost peak of the Selwyn Range, which is a subrange of the Canadian Rockies. Precipitation runoff from the peak drains north into the Fraser River. Topographic relief is significant as the summit rises 1,400 meters (4,600 ft) above the Robson Valley in. The Yellowhead Highway (Highway 16) and Canadian National Railway traverse the northern base of the mountain.

Geographic entities mentioned:
surface_form: Robson Valley
instance_of: Valley
countries: Canada
coordinates: lat: 53.25
lon: -120
Precipitation runoff from the peak drains north into the Fraser River. Topographic relief is significant as the summit rises 1,400 meters (4,600 ft) above the Robson Valley in. The Yellowhead Highway (Highway 16) and Canadian National Railway traverse the northern base of the mountain. The nearest neighbor is line parent Overlander Mountain, to the southeast. Etymology.

Geographic entities mentioned:
surface_form: Overlander Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.99138888888889
lon: -119.19472222222223
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Klapperhorn Mountain. Klapperhorn Mountain is a summit in British Columbia, Canada. Description. Klapperhorn Mountain, elevation 2,301-meters (7,549-feet), is located in Mount Robson Provincial Park, just south and within view of the park's visitor centre. It is the northernmost peak of the Selwyn Range, which is a subrange of the Canadian Rockies.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: klapperhorn mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 53.00138888888889
lon: -119.21833333333333
Klapperhorn Mountain is a summit in British Columbia, Canada. Description. Klapperhorn Mountain, elevation 2,301-meters (7,549-feet), is located in Mount Robson Provincial Park, just south and within view of the park's visitor centre. It is the northernmost peak of the Selwyn Range, which is a subrange of the Canadian Rockies. Precipitation runoff from the peak drains north into the Fraser River.

Geographic entities mentioned:
surface_form: mount robson
instance_of: Mountain
countries: Canada
coordinates: lat: 53.11055555555556
lon: -119.15666666666667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: klapperhorn mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 53.00138888888889
lon: -119.21833333333333
Klapperhorn Mountain. Klapperhorn Mountain is a summit in British Columbia, Canada. Description. Klapperhorn Mountain, elevation 2,301-meters (7,549-feet), is located in Mount Robson Provincial Park, just south and within view of the park's visitor centre. It is the northernmost peak of the Selwyn Range, which is a subrange of the Canadian Rockies.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: klapperhorn mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 53.00138888888889
lon: -119.21833333333333
Precipitation runoff from the peak drains north into the Fraser River. Topographic relief is significant as the summit rises 1,400 meters (4,600 ft) above the Robson Valley in. The Yellowhead Highway (Highway 16) and Canadian National Railway traverse the northern base of the mountain. The nearest neighbor is line parent Overlander Mountain, to the southeast. Etymology.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Etymology. The mountain was named by BC Parks on March 13, 1972, and the toponym was officially adopted December 19, 1978, by the Geographical Names Board of Canada. The mountain is a classic horn-shaped summit, which is notable for the frequency of its rockslides which are audible to campers and are a source of much curiosity and interest. Climate.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Climate. Based on the Köppen climate classification, Klapperhorn Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: klapperhorn mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 53.00138888888889
lon: -119.21833333333333
A short unnamed creek flows in at the north. The primary outflow, at the south, is an unnamed creek towards Lost Lake, which flows via Calcite Creek, Sydney Creek and the Montreal River to Lake Timiskaming on the Ottawa River. A second Crawford Lake in Timiskaming District and also in the same drainage basins, Crawford Lake (Milner Township), lies just southwest.

Geographic entities mentioned:
surface_form: Lake Timiskaming
instance_of: Lake
countries: Canada
coordinates: lat: 47.333333333333
lon: -79.5
Crawford Lake (Haultain Township). Crawford Lake is a lake in geographic Haultain Township in the Montreal River and Ottawa River drainage basins in Timiskaming District, Ontario, Canada. It is about long and wide, and lies at an elevation of about northeast of the community of Gowganda. A short unnamed creek flows in at the north.

Geographic entities mentioned:
surface_form: crawford lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.0908
lon: -91.2892
surface_form: crawford lake (haultain township)
instance_of: Lake
countries: Canada
coordinates: lat: 47.7008
lon: -80.6828
surface_form: crawford lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.1394
lon: -81.9683
Crawford Lake (Haultain Township). Crawford Lake is a lake in geographic Haultain Township in the Montreal River and Ottawa River drainage basins in Timiskaming District, Ontario, Canada. It is about long and wide, and lies at an elevation of about northeast of the community of Gowganda. A short unnamed creek flows in at the north.

Geographic entities mentioned:
surface_form: crawford lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.0908
lon: -91.2892
surface_form: crawford lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.7008
lon: -80.6828
surface_form: crawford lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.1394
lon: -81.9683