Sarmila/GeoWiki-Features huggingface dataset:
The trail passes the Lac de l'Oriente. It passes through a pine forest, maquis shrubland and over bare rocks. The view from the summit gives a panorama of Corsica, including Cap Corse to the north, Monte Cinto and Paglia Orba just opposite, Monte d'Oro, Monte Renoso, and Monte Incudine to the south, with the sea on the east and west sides of the island.

Geographic entities mentioned:
surface_form: Monte Cinto
instance_of: Mountain
countries: France
coordinates: lat: 42.37972222222222
lon: 8.945833333333333
surface_form: Paglia Orba
instance_of: Mountain
countries: France
coordinates: lat: 42.3425
lon: 8.878611
surface_form: Monte d'Oro
instance_of: Mountain
countries: France
coordinates: lat: 42.1375
lon: 9.098611111111111
surface_form: Monte Renoso
instance_of: Mountain
countries: France
coordinates: lat: 42.0583
lon: 9.13361
surface_form: Monte Incudine
instance_of: Mountain
countries: France
coordinates: lat: 41.8494655
lon: 9.2073797
surface_form: monte cinto
instance_of: Mountain
countries: France
coordinates: lat: 42.37972222222222
lon: 8.945833333333333
Location. The peak of Monte Rotondo lies on the boundary between the commune of Corte to the north and east and Venaco to the south and west. It is east of the Punta Mufrena and northeast of Lac de Battomello. The mountain lies within and gives its name to the &quot;Réserve naturelle du Massif du Monte Ritondu&quot;. Physical. Monte Rotondo has an elevation of and clean prominence of.

Geographic entities mentioned:
surface_form: monte ritondu
instance_of: Mountain
countries: France
coordinates: lat: 42.21611111111111
lon: 9.058055555555555
Monte Rotondo. Monte Rotondo () is a mountain in the department of Haute-Corse on the island of Corsica, France. At it is the second highest in Corsica, after Monte Cinto. It is the highest point on the Monte Rotondo massif. Location. The peak of Monte Rotondo lies on the boundary between the commune of Corte to the north and east and Venaco to the south and west.

Geographic entities mentioned:
surface_form: monte rotondo
instance_of: Mountain
countries: France
coordinates: lat: 42.21611111111111
lon: 9.058055555555555
It is the highest point on the Monte Rotondo massif. Location. The peak of Monte Rotondo lies on the boundary between the commune of Corte to the north and east and Venaco to the south and west. It is east of the Punta Mufrena and northeast of Lac de Battomello. The mountain lies within and gives its name to the &quot;Réserve naturelle du Massif du Monte Ritondu&quot;. Physical.

Geographic entities mentioned:
surface_form: monte rotondo
instance_of: Mountain
countries: France
coordinates: lat: 42.21611111111111
lon: 9.058055555555555
Physical. Monte Rotondo has an elevation of and clean prominence of. It is isolated by from its nearest higher neighbor, Monte Cinto. Hiking. A hiking trail to Monte Rotondo from the D623 road is rated moderate, and is in best condition from April to October. The return trip is long, with an elevation gain of. The hike is easy but long, and requires good physical condition.

Geographic entities mentioned:
surface_form: monte rotondo
instance_of: Mountain
countries: France
coordinates: lat: 42.21611111111111
lon: 9.058055555555555
A steam driven pump returned the water to the higher reservoir. The steam engine was of the atmospheric type. An improvement devised by Joshua Wrigley, trialled in Chorlton-upon-Medlock used two Savery engines to supplement the river in driving on overshot waterwheel. In 1784, Edmund Cartwright invented the power loom, and produced a prototype in the following year.

Geographic entities mentioned:
surface_form: river
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 53.4741
lon: -2.25342
The farm in South Africa failed and Stephen's parents returned to Hampshire, where he was born. When Stephen was six, the family moved to Canada, where they settled on a farm near the village of Sutton, Ontario, and the shores of Lake Simcoe. Their farm in the township of Georgina was also unsuccessful, and the family was kept afloat by money sent from Leacock's paternal grandfather.

Geographic entities mentioned:
surface_form: Lake Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
He was puzzled as to why Leacock's work was no longer well known in the United States. During the summer months, Leacock lived at Old Brewery Bay, his summer estate in Orillia, across Lake Simcoe from where he was raised and also bordering Lake Couchiching. A working farm, Old Brewery Bay is now a museum and National Historic Site of Canada.

Geographic entities mentioned:
surface_form: Lake Couchiching
instance_of: Lake
countries: Canada
coordinates: lat: 44.6667
lon: -79.3833
Lili Marlene (aircraft). The &quot;Lili Marlene&quot;, also known as the &quot;Lily Marline&quot;, was a Douglas C-47 Skytrain that crashed at Mount Makaturing, near Dansalan, Lanao, Philippines. All 17 people on board were killed.

Geographic entities mentioned:
surface_form: Mount Makaturing
instance_of: Mountain
countries: Philippines
coordinates: lat: 7.65
lon: 124.31666666667
Alunan (NLSA), Francisco Zulueta (NSLA), Alfredo Paredes (NSLA) and 4 other NSLA staff, Colonel Edwin Andrews and Officers and Soldiers of the Philippine Army Air Corps. However, mid-way through the first leg of the trip, the plane had been guided into the direct flight path of Mount Makaturing in Lanao, near Dansalan, at around 5300 feet.

Geographic entities mentioned:
surface_form: Mount Makaturing
instance_of: Mountain
countries: Philippines
coordinates: lat: 7.65
lon: 124.31666666667
However, a week later on June 5, 1947, members of the Macaso Party near Mount Makaturing found body parts and parts of a plane on the slopes of Mount Seriban. This then raised speculation on whether the plane had &quot;exploded in mid-air due to undetermined causes&quot;. Aftermath.

Geographic entities mentioned:
surface_form: Mount Makaturing
instance_of: Mountain
countries: Philippines
coordinates: lat: 7.65
lon: 124.31666666667
Olive Townships, an active rail line is still in service and operated by the Morristown and Erie Railway to Wharton. The trail connects to the New Jersey Transit Raritan Valley Line at High Bridge and connects to Patriots Path in Long Valley. A notable portion of the Columbia Trail is the Ken Lockwood Gorge, between Califon and High Bridge (miles north of High Bridge).

Geographic entities mentioned:
surface_form: Ken Lockwood Gorge
instance_of: Landform
countries: United States
coordinates: lat: 40.69583333333333
lon: -74.87194444444444
Ancient Caucasian Albania lay on the south-eastern part of the Greater Caucasus mountains. It was bounded by Caucasian Iberia (present-day Georgia) to the west, by Sarmatia to the north, by the Caspian Sea to the east, and by the provinces of Artsakh and Utik in Armenia to the west along the Kura river.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
The alphabet was titled: &quot;Ałuanicʿ girn ē&quot; (, meaning, &quot;These are Albanian letters&quot;). In 1996, Zaza Aleksidze of the Georgian Centre of Manuscripts discovered at Saint Catherine's Monastery at Mount Sinai, Egypt, a text written on parchment that had been reused in a Georgian palimpsest.

Geographic entities mentioned:
surface_form: Mount Sinai
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.5384
lon: 33.9752
Roman Empire. There was an enduring relation of Albania with Ancient Rome. The Latin rock inscription close to Boyukdash mountain in Gobustan, Baku, which mentions Legio XII Fulminata, is the world's easternmost Latin inscription known. In Albania, Romans reached the Caspian Sea for the first time. The Roman coins circulated in Caucasian Albania till the end of the 3rd century AD.

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
Leatherman Peak. Leatherman Peak, at above sea level is the second highest peak in Idaho and the Lost River Range. The peak is located in Salmon-Challis National Forest in Custer County. It is southeast of Borah Peak, its line parent. It is also about 4.5 mi (7.2 km) northeast from U.S. Route 92. The peak was named after Henry Leatherman.

Geographic entities mentioned:
surface_form: Borah Peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1373891
lon: -113.78110123
Leatherman Peak. Leatherman Peak, at above sea level is the second highest peak in Idaho and the Lost River Range. The peak is located in Salmon-Challis National Forest in Custer County. It is southeast of Borah Peak, its line parent. It is also about 4.5 mi (7.2 km) northeast from U.S. Route 92. The peak was named after Henry Leatherman.

Geographic entities mentioned:
surface_form: leatherman peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.0821
lon: -113.733
French Valley, California. French Valley is a census-designated place located in the French Valley of Riverside County, California. The 2020 United States census reported French Valley's population as 35,280, up from 23,067 at the 2010 census. It became the most populous CDP in Riverside County when Rubidoux was incorporated into Jurupa Valley. Geography. French Valley sits at an elevation of.

Geographic entities mentioned:
surface_form: French Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.5959
lon: -117.125
There are many synonyms of &quot;Gladiolus crassifolius&quot;. In tropical areas &quot;Gladiolus crassifolius&quot; is known as &quot;Gladiolus thomsonii&quot;. It is found in the Afro-alpine zone of Mount Kenya, up to around 3,300 m (11,000 ft). It has scarlet petals with yellow centres and a strong stem, and has been seen growing in a variety of habitats such as forest edges and open grassland.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
He attended two public schools, Schwartz’s Academy in Bethlehem, Pennsylvania, and an academy in Merchantville and Princeton, New Jersey. He became a civil and mining engineer and was identified with banking, coal, iron, and lumber industries. He moved from Mauch Chunk, Pennsylvania to Upper Lehigh, Pennsylvania, in 1885. Political career.

Geographic entities mentioned:
surface_form: Upper Lehigh, Pennsylvania
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Velachery Lake. Velachery Aeri (), or Velachery Lake, is one of the lakes inside Chennai, in the Indian state of Tamil Nadu, with a good stock of water all through the year. Since Velachery is a low-lying area, the monsoon rain water from the neighbouring areas are drained into this lake. The ambitious programme of the corporation was conceived three years ago.

Geographic entities mentioned:
surface_form: velachery lake
instance_of: Lake
countries: India
coordinates: lat: 12.988
lon: 80.213
The Litani River that winds through the Beqaa Valley in Lebanon is named after Lotan as the river was believed to be the personification of the god.

Geographic entities mentioned:
surface_form: Beqaa Valley
instance_of: Valley
countries: Lebanon
coordinates: lat: 34.008888888889
lon: 36.145277777778
It starts at Clifton Suspension Bridge on the Avon Gorge in Bristol, and continues across the Chew Valley with its lakes, over the Mendip Hills to Cheddar Gorge and Cheddar, along the Somerset Levels to Glastonbury and Street and on through Bridgwater and Goathurst to the Quantock Hills with a scenic ridge walk passing through the villages Crowcombe and Stogumber and around the Brendon Hills.

Geographic entities mentioned:
surface_form: Chew Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.337422222222
lon: -2.6151972222222
surface_form: Cheddar Gorge
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.282409
lon: -2.76546
Eventually, those boats would be sold through Tracker Marine Group, owned by Bass Pro Shops. In 1981, Morris opened the first Bass Pro Shops outdoor store in Springfield. A few years later in 1987, Morris bought an empty plot of land on Table Rock Lake in Missouri's Ozark Mountains. One year later, at that location, he opened Big Cedar Lodge resort.

Geographic entities mentioned:
surface_form: Missouri's Ozark Mountains
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
Eurocopter and its predecessor companies have established a wide range of helicopter firsts, including the first production turboshaft-powered helicopter (the Aérospatiale Alouette II of 1955); the introduction of the Fenestron shrouded tail rotor (on the Gazelle of 1968); the first helicopter certified for full flight in icing conditions (the AS332 Super Puma, in 1984); the first production helicopter with a Fly-by-wire control system (the NHIndustries NH90, first flown in full FBW mode in 2003); the first helicopter to use a Fly-by-light primary control system (an EC135 testbed, first flown in 2003); and the first ever landing of a helicopter on Mount Everest (achieved by an AS350 B3 in 2005).

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Rigole de la plaine. The critical feature of the Canal du Midi was to provide sufficient water to ensure that the lock system continued to function, even through the summer months. The first part of this endeavor was the &quot;rigole de la plaine&quot; (). It carried water from the Sor River, at Pontcrouzet, to the Bassin de Naurouze, where the water was to enter the canal. This was done in 1667.

Geographic entities mentioned:
surface_form: Bassin de Naurouze
instance_of: Lake
countries: France
coordinates: lat: 43.35255
lon: 1.820942
It carried water from the Sor River, at Pontcrouzet, to the Bassin de Naurouze, where the water was to enter the canal. This was done in 1667. In 1668 Riquet built a loading basin, near Revel, on the rigole de la plaine between Pont Crouzet, on the river Sor, and Naurouze, called Port Louis. The feeder between this point and Naurouze was expanded in order for boats to ferry stones.

Geographic entities mentioned:
surface_form: Naurouze
instance_of: Lake
countries: France
coordinates: lat: 43.35255
lon: 1.820942
This was done in 1667. In 1668 Riquet built a loading basin, near Revel, on the rigole de la plaine between Pont Crouzet, on the river Sor, and Naurouze, called Port Louis. The feeder between this point and Naurouze was expanded in order for boats to ferry stones. Fourteen locks were put in place. In 1669 Riquet widened the rigole de la plaine enough to support navigation.

Geographic entities mentioned:
surface_form: Naurouze
instance_of: Lake
countries: France
coordinates: lat: 43.35255
lon: 1.820942
The feeder between this point and Naurouze was expanded in order for boats to ferry stones. Fourteen locks were put in place. In 1669 Riquet widened the rigole de la plaine enough to support navigation. It was opened to traffic in 1670 from Revel, to Naurouze. Pierre Borel had the original idea for this feature.

Geographic entities mentioned:
surface_form: Naurouze
instance_of: Lake
countries: France
coordinates: lat: 43.35255
lon: 1.820942
As force seemed hopeless, the Peshwa offered Ramji to be pardon and gave him an important Subedar post, in which he did excellent service. Even after the establishment of the British rule in the Deccan, nearly twenty years passed before the warlike Kolis were brought to order.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Description. Pelister was the first national park in Yugoslavia, declared on November 30, 1948. It is the oldest and second largest national park in North Macedonia after Mavrovo. It is one of the leading tourist areas in the country, since it is a well-known ski resort, along with Ohrid, Prespa, Dojran, Popova Šapka, and Kruševo. Geography and geology.

Geographic entities mentioned:
surface_form: Popova Šapka
instance_of: Mountain
countries: North Macedonia
coordinates: lat: 42.01416667
lon: 20.88
DeRuyter Reservoir (or Tioughnioga Lake) occupies the northwest corner of the town, and flows out at its north end into Limestone Creek, a tributary of Chittenango Creek and part of the Oneida Lake watershed leading eventually to Lake Ontario. Demographics. As of the census of 2000, there were 1,532 people, 592 households, and 412 families residing in the town. The population density was.

Geographic entities mentioned:
surface_form: Oneida Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.2
lon: -75.9
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
A mestizo descendant of the conquistador Gonzalo de Sandoval, Sandoval was a justice of the peace at the close of the colonial period in his native Granada, but he also worked in transporting goods on Lake Nicaragua and the Río San Juan.

Geographic entities mentioned:
surface_form: Lake Nicaragua
instance_of: Lake
countries: Nicaragua
coordinates: lat: 11.5742
lon: -85.3563
As an alternative, the Paleys built a summer home, &quot;Kiluna North,&quot; on Squam Lake in New Hampshire and spent the summers there for many years, routinely entertaining their many friends, including Lucille Ball, Grace Kelly, and David O. Selznick. The couple had two children, William and Kate. Other affairs. Paley was a notorious womanizer his entire life.

Geographic entities mentioned:
surface_form: Squam Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.745277777778
lon: -71.526111111111
He was aware that his placement of the specimen in &quot;Chrysophyllum&quot; may have to be changed when &quot;perfect flowers are available&quot;. In 1923, he and fellow Australian botanist William Douglas Francis published a new description after examining flowering specimens from the Atherton Tableland collected by G.

Geographic entities mentioned:
surface_form: Atherton Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
Lower House Stream Section. Lower House Stream Section is a Site of Special Scientific Interest in the Rhymney Valley, in Caerphilly County Borough, south Wales. The stream is just south of the Lower House Reservoir and is north of Rhymney. The geological interest of the site centres on the best exposure of the Middle Shales Formation, part of the South Wales Coalfield, in south Wales.

Geographic entities mentioned:
surface_form: Rhymney Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.697777777778
lon: -3.2294444444444
Medina River. The Medina River is located in south central Texas, United States, in the Medina Valley. It was also known as the Rio Mariano, Rio San Jose, or Rio de Bagres (Catfish river). Its source is in springs in the Edwards Plateau in northwest Bandera County, Texas, and it merges with the San Antonio River in southern Bexar County, Texas, for a course of 120 miles.

Geographic entities mentioned:
surface_form: Medina Valley
instance_of: Valley
countries: United States
coordinates: lat: 29.5406
lon: -98.9335
It was also known as the Rio Mariano, Rio San Jose, or Rio de Bagres (Catfish river). Its source is in springs in the Edwards Plateau in northwest Bandera County, Texas, and it merges with the San Antonio River in southern Bexar County, Texas, for a course of 120 miles. It contains the Medina Dam in NE Medina County, Texas which restrains Lake Medina.

Geographic entities mentioned:
surface_form: Edwards Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 30.3
lon: -99.6
Location. Fung Lok Wai is located south of the Inner Deep Bay, between Yuen Long Industrial Estate and Hong Kong Wetland Park. Immediately south of Fung Lok Wai are the villages of is Ng Uk Tsuen and Shing Uk Tsuen of Wang Chau. Kai Shan is located to the immediate southwest of Fung Lok Wai. History. In the early 20th century, and before the 1920s, the area was the site of swamp and marsh.

Geographic entities mentioned:
surface_form: Kai Shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.45837
lon: 114.01626
History of the site. The Morelos Valley was settled from about 2000 BC. During the Classic Period, Teopanzolco came under the influence of the great metropolis of Teotihuacan in the Valley of Mexico. By the Postclassic, various Nahua groups had moved into the &quot;Altiplano&quot;; the Tlahuicas founded nearby Cuauhnahuac (Cuernavaca) and Teopanzolco itself.

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
History of the site. The Morelos Valley was settled from about 2000 BC. During the Classic Period, Teopanzolco came under the influence of the great metropolis of Teotihuacan in the Valley of Mexico. By the Postclassic, various Nahua groups had moved into the &quot;Altiplano&quot;; the Tlahuicas founded nearby Cuauhnahuac (Cuernavaca) and Teopanzolco itself.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Mexico
coordinates: lat: 24
lon: -103
After the ice retreated the Skagit breached the moraine dam near Concrete, Washington, finding its present course. The Sauk River and Suiattle River continued to drain into the future North Fork Stillaguamish River until eruptions of Glacier Peak choked the rivers with debris, causing the formation of an alluvial fan near present-day Darrington, Washington.

Geographic entities mentioned:
surface_form: Glacier Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
Eventually, the Skagit gorge was so deep that even after the Cordilleran ice retreated for good, the river continued flowing south instead of north into Canada. The Skagit watershed is made up of high peaks and low valleys. The highest points in the basin are two volcanoes: Mount Baker, elevation, and Glacier Peak, elevation. Most of the basin lies above.

Geographic entities mentioned:
surface_form: Mount Baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Archaeological evidence indicates that ancestors of the Upper Skagit tribe lived in the area now called Ross Lake National Recreation Area at least 8,000 years ago. They quarried chert from Hozomeen Mountain to make blades, which were used across a wide trading area. Both tribes traditionally spoke dialects of the Lushootseed language, a branch of the Salishan family.

Geographic entities mentioned:
surface_form: Hozomeen Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.9822
lon: -121.012
In 1796, Byron suffered from scarlet fever, and his mother took him to the Scottish Highlands to stay in the mountains until his recovery. This experience affected Byron greatly, as he described in his poetry, especially his memory of the mountain of Lochnagar and a girl named Mary. He soon fell in love with another Mary, a cousin, and would still think of her until he was 27.

Geographic entities mentioned:
surface_form: Lochnagar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.959930555556
lon: -3.2447805555556
During 2008, the Montabliz viaduct, the highest one in Spain, was inaugurated and connected Cantabria and the Inner Plateau by road. A year later, Cintra was awarded the construction, maintenance, and operation of the North Tarrant Express Highway in Texas in the US.

Geographic entities mentioned:
surface_form: Inner Plateau
instance_of: Plateau
countries: Spain
coordinates: lat: 40.5
lon: -3.5
Hector McNeil was elected unopposed to succeed Robert Gibson. Background. Greenock is a town in the west central Lowlands of Scotland. The seat became vacant when the Labour Member of Parliament (MP) Robert Gibson resigned to take up the post of Chairman of the Scottish Land Court. Gibson had held the seat since a by-election in 1936. Result.

Geographic entities mentioned:
surface_form: central Lowlands
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.408
lon: -4.044
Acanthomintha duttonii. &quot;Acanthomintha duttonii&quot; is a species of annual plant endemic to San Mateo County, California in the family Lamiaceae. It is commonly called San Mateo thornmint and is found growing on serpentine soils near the Crystal Springs Reservoir in a six-mile (10 km) long strip on the east side of Montara Mountain at elevations of approximately 150 to 300 meters. Taxonomy.

Geographic entities mentioned:
surface_form: Montara Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.5285
lon: -122.427
Dornberk. Dornberk (;) is a village in western Slovenia in the Municipality of Nova Gorica. It is located in the Vipava Valley within the &quot;Goriška&quot; region of the Slovenian Littoral. Dornberk is the centre of a local community that includes the satellite settlements of Potok pri Dornberku, Saksid, Brdo, Tabor, Draga, Zalošče, and Budihni.

Geographic entities mentioned:
surface_form: Vipava Valley
instance_of: Valley
countries: Slovenia
coordinates: lat: 45.876147222222
lon: 13.907319444444
This phonetic difference is not perceived in the nominative case in standard Slovene, in which the final voiced velar stop /g/ is pronounced as voiceless /k/. However, in the local Karst dialect spoken in the lower Vipava Valley, /g/ has developed into the voiced glottal fricative /ɦ/, and often a voiceless glottal fricative at the end of words. Economy.

Geographic entities mentioned:
surface_form: Vipava Valley
instance_of: Valley
countries: Slovenia
coordinates: lat: 45.876147222222
lon: 13.907319444444
Mount Engelhard. Mount Engelhard is a mountain summit located between the Athabasca River valley and Sunwapta River valley of Jasper National Park, in the Canadian Rockies of Alberta, Canada. Engelhard lies one kilometre northwest of Mount Cromwell, and three km NNE of the east summit of Stutfield Peak.

Geographic entities mentioned:
surface_form: Mount Cromwell
instance_of: Mountain
countries: Canada
coordinates: lat: 52.26888888888889
lon: -117.39305555555555
surface_form: Stutfield Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.23833333333334
lon: -117.4075
Mount Engelhard. Mount Engelhard is a mountain summit located between the Athabasca River valley and Sunwapta River valley of Jasper National Park, in the Canadian Rockies of Alberta, Canada. Engelhard lies one kilometre northwest of Mount Cromwell, and three km NNE of the east summit of Stutfield Peak.

Geographic entities mentioned:
surface_form: athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
surface_form: athabasca
instance_of: Mountain
countries: Canada
coordinates: lat: 52.18055555555556
lon: -117.20166666666667
surface_form: mount engelhard
instance_of: Mountain
countries: Canada
coordinates: lat: 52.27527777777778
lon: -117.40694444444445
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The first ascent was made in 1930 by W. Hainsworth, J.F. Lehmann, M.M. Strumia, and N.D. Waffl. __NOTOC__
Climate. Based on the Köppen climate classification, Mount Engelhard is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below. Precipitation runoff from the mountain drains into tributaries of the Athabasca River.

Geographic entities mentioned:
surface_form: athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
surface_form: athabasca
instance_of: Mountain
countries: Canada
coordinates: lat: 52.18055555555556
lon: -117.20166666666667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Engelhard. Mount Engelhard is a mountain summit located between the Athabasca River valley and Sunwapta River valley of Jasper National Park, in the Canadian Rockies of Alberta, Canada. Engelhard lies one kilometre northwest of Mount Cromwell, and three km NNE of the east summit of Stutfield Peak.

Geographic entities mentioned:
surface_form: mount engelhard
instance_of: Mountain
countries: Canada
coordinates: lat: 52.27527777777778
lon: -117.40694444444445
The first ascent was made in 1930 by W. Hainsworth, J.F. Lehmann, M.M. Strumia, and N.D. Waffl. __NOTOC__
Climate. Based on the Köppen climate classification, Mount Engelhard is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below. Precipitation runoff from the mountain drains into tributaries of the Athabasca River.

Geographic entities mentioned:
surface_form: mount engelhard
instance_of: Mountain
countries: Canada
coordinates: lat: 52.27527777777778
lon: -117.40694444444445
Engelhard lies one kilometre northwest of Mount Cromwell, and three km NNE of the east summit of Stutfield Peak. The mountain was named in 1966 after Georgia Engelhard, an American who climbed for 15 years in the Canadian Rockies. The first ascent was made in 1930 by W. Hainsworth, J.F. Lehmann, M.M. Strumia, and N.D. Waffl. __NOTOC__
Climate.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The Saranac River forms the northern town line, with the town of Plattsburgh on the opposite shore. The Salmon River runs through the southern part of the town, approximately north of the border with the town of Peru. Both rivers flow east into Lake Champlain. New York State Route 22B is a north-south highway in the town, beginning east-west in the hamlet of Morrisonville. Demographics.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Jebel Moya. Jebel Moya is an archaeological site in the southern Gezira Plain, Sudan, approximately 250 km (150 miles) south southeast of Khartoum. Dating between 5000 BCE-500 CE and roughly 104,000 m2 (25 acres) in area, the site is one of the largest pastoralist cemeteries in Africa with over 3,000 burials excavated thus far. The site was first excavated by Sir Henry Wellcome from 1911 to 1914.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
Dating between 5000 BCE-500 CE and roughly 104,000 m2 (25 acres) in area, the site is one of the largest pastoralist cemeteries in Africa with over 3,000 burials excavated thus far. The site was first excavated by Sir Henry Wellcome from 1911 to 1914. Artifacts found at the site suggest trade routes between Jebel Moya and its surrounding areas, even as far as Egypt. Environment.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
The environmental transition from swamp to savanna and semi-desert steppe was complete by 3000 BCE. By the early centuries CE, few swampy conditions remained; one notable wet site that remained is Jebel et Tomat, another early pastoralist site, northeast of Jebel Moya.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
Environmentally, the Southern Gezira can be separated into categories of swamp vegetation, riverine woodland, grassland, and jebel vegetation. This places the environment of Jebel Moya close to transitional belts, in both modern day, and likely the Classic and Meroitic periods.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
This places the environment of Jebel Moya close to transitional belts, in both modern day, and likely the Classic and Meroitic periods. Jebel Moya refers to a massif which includes a group of granite hills connected by ridges and valleys; the name has become associated with the archaeological site within the north-easternmost of these valleys.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
Jebel Moya refers to a massif which includes a group of granite hills connected by ridges and valleys; the name has become associated with the archaeological site within the north-easternmost of these valleys. The Jebel Moya massif is a geological granite outcrop of the Gezira Plain's underlying Basement Complex, which breaks through the above Sandstone Formation.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
The Jebel Moya massif is a geological granite outcrop of the Gezira Plain's underlying Basement Complex, which breaks through the above Sandstone Formation. The Basement Complex contains an underground aquifer, which results in fresh water rising to the surface/ground level around outcrops like Jebel Moya.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
The Basement Complex contains an underground aquifer, which results in fresh water rising to the surface/ground level around outcrops like Jebel Moya. This established Jebel Moya as a potential fresh water source, which is important in a plain without permanent surface water sources for maintaining animal herds. The aquifer is replenished by both the Blue and While Niles.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
This establishes that the ecological conditions in the region were suitable for pastoralism from 1000 BCE-1000 CE. Excavation history. Excavations at Jebel Moya began 29 January 1911 and continued until April 1914 when further plans were abandoned due to the onset of World War I. During those four seasons, approximately a fifth of the 10.4 hectare (25 acre) site was excavated.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
Some graves, devoid of burials, contained only pottery; others contained multiple inhumations. 25 of the graves contained animal burials. In total, 3137 individuals were excavated, which marks Jebel Moya as the largest burial complex yet found in sub-Saharan Africa. Season 1. Wellcome supervised the first field season, from 29 January - April 1911.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
Work did not resume after the war ended, and Wellcome passed away in 1936. Post-Excavation. Due to a variety of setbacks, including two world wars and Wellcome's death in 1936, the first official report on Jebel Moya was not published until 1949 by Frank Addison, who was appointed by the Wellcome Trust. The Trustees of the Wellcome Trust also appointed G.M.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
The Trustees of the Wellcome Trust also appointed G.M. Morant, assisted by Otto Samson, to examine the remains from Jebel Moya. Unable to continue after the Second World War, the project to complete osteological work was transferred to J.C. Trevor, who employed R. Mukherjee and C.R. Rao to conduct the majority of analyses. They published their analysis in 1955.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
Mukherjee and C.R. Rao to conduct the majority of analyses. They published their analysis in 1955. During the 41 years in between excavating and the 1955 study re-examining the remains from Jebel Moya, a significant amount of material was lost due to poor storage conditions. Materials from Jebel Moya had been shipped to a depot in Maryleborne, and a warehouse in Dartford, London.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
Despite the setbacks caused by these conditions, the 1955 report was groundbreaking for its use of the now common Mahalanobis D2 distance to craniometric data; according to the Mukherjee, “The result was a measure of group divergence between Jebel Moya and 19 other African samples.”
Frank Addison's dating.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
He later modified the dates to between 400 BCE-400 CE, coinciding with the Meroitic kingdom to the north. Rudolf Gerharz' dating. In 1994, Rudolf Gerharz’ reinterpretation of the dating of Jebel Moya, based on Addison's data, included three more accurate time phases for the site. Phase I (5000 BCE) included occasional occupations at the site, and Dotted Wavy Line pottery.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
Phase I (5000 BCE) included occasional occupations at the site, and Dotted Wavy Line pottery. Phase II (3000-800 BCE) included the majority of the graves at Jebel Moya, including burials in the western half, and many unspecified burials with no or few associated funerary objects from the eastern half.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
Phase III (800-100 BCE) is potentially the first to feature trade items from the north, particularly metals, ceramics and glass. Phase III encompassed the remainder of the graves in the eastern half of Jebel Moya.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
Phase III encompassed the remainder of the graves in the eastern half of Jebel Moya. Gerharz’ estimates for the second and third phases were incorrect; the absence of Meroitic wheel-made pottery at Jebel Moya does not indicate the site's abandonment by 100 BCE, given the appearance of locally manufactured wheel made pottery. Current dating.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
All surviving site features, including graves, date in Phase II (ca. 3000-800 BCE) and Phase III (800-100 BCE). The main occupation at Jebel Moya is dated to 2300 BCE. The first conclusive evidence for burials at Jebel Moya dates to the mid-first century BCE. Period 1, following Gerharz' Phase I, dates to the late sixth or early fifth millennium BCE. Period 2 dates between 2500 and 1500 BCE.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
Period 1, following Gerharz' Phase I, dates to the late sixth or early fifth millennium BCE. Period 2 dates between 2500 and 1500 BCE. It is inferred from surrounding economies to the north that during this period, the inhabitants of Jebel Moya were pastoral or agro-pastoral. Period 3 dates between 100 BCE and 500 CE, during which the majority of the burials were interred.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
Period 3 dates between 100 BCE and 500 CE, during which the majority of the burials were interred. Accelerator Mass Spectrometry dating of bone samples from Jebel Moya were unsuccessful due to lack of collagen. OSL dating of pottery is the first absolute date from Jebel Moya. Habitation.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
OSL dating of pottery is the first absolute date from Jebel Moya. Habitation. Because of the permanent source of water, there were multiple habitation sites as well as grave sites at Jebel Moya used by pastoralists in the area. During the Wellcome Excavations, evidence of habitation sites were found. Most field notes concerning the habitation sites did not survive.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
During the Wellcome Excavations, evidence of habitation sites were found. Most field notes concerning the habitation sites did not survive. Human-made features at Jebel Moya include three hearths, three hardened mud floors, one of which contained post-holes, and a second contained a hearth. These finds are consistent with habitation activity and possibly contemporary with Phase I (5000 BCE).

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
Bates believed the structures, composed of small stones, were not associated with any specific burial, and were perhaps parts of shelters, or stone platforms for sacrificing or feasting. Nineteen ovens were found in the Southwest sector of Jebel Moya. The ovens were barrel shaped pits plastered in mud, 40–50 cm (16&quot; to 20&quot;) in depth,  70–80 cm (28&quot; to 32&quot;) in diameter.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
Addison posited that the stones were heated in an external area and then placed in the oven, with food placed over it, to slowly cook. The available data suggests that settlement at Jebel Moya during Phase I was likely episodic. The lack of data from the rest of the valley prevents a concrete answer pertaining to the potentiality of a permanent settlement or a seasonal one during Phase II.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
36 of the burials were crouched, 217 of the burials were prone, and 1695 burials were supine, with 355 on their left side, and 430 on their right side. The majority of the burials were facing somewhat north or west. Burials. All ages and sexes were represented in the burials at Jebel Moya. 2026 burials (64.7%) were buried without funerary objects; many had only a small number.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
No permanent grave markings appear, or at least none have survived. There is a strong uniformity in number and type of burial assemblages; a high level of androgyny, at least in a mortuary realm. Infant burials. There are 93 infant burials at Jebel Moya, 35 of which have associated grave foods. The largest percentage of oval burials occurs for infant burials (16.13%).

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
Juvenile burials. There are 199 juvenile burials at Jebel Moya, 67 of which have associated funerary objects. Like the infants, there are no exclusive categories for juveniles, however, a wider array of artifacts were found with juveniles than infants. Grave shapes are similar to that of adults.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
In front of the ram is an uraeus. Base: The name Men-Ka-Ra flanked by uraei” (Referring to Menkhepera, the first Napatan ruler of the 25th Dynasty, 747-716 BCE). The artifacts found at Jebel Moya reinforce the idea of two distinct habitation periods at Jebel Moya. Of the burials that did contain funerary objects, the majority had only a few, often ornaments that would have been worn in life.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
Of the 3135 human burials, 1108 (35.3%) have associated funerary objects, and 2026 (64.7%) do not. The raw materials for these artifacts came from sources along the Nile and further north, likely brought by the Meroitic trade routes. The presence of cattle figurines (not associated with burials) as well as cattle burials supports the conclusion that the inhabitants of Jebel Moya were pastoralists.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
The presence of cattle figurines (not associated with burials) as well as cattle burials supports the conclusion that the inhabitants of Jebel Moya were pastoralists. There are 55 occurrences of cattle bones among the burials at Jebel Moya, either in association with human burials, or in separate burials by themselves.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
There are 55 occurrences of cattle bones among the burials at Jebel Moya, either in association with human burials, or in separate burials by themselves. Like the human remains, only a fraction of the items found at Jebel Moya survived. Agriculture.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
Like the human remains, only a fraction of the items found at Jebel Moya survived. Agriculture. In previous studies, the lack of agricultural equipment at Jebel Moya, contrasting Jebel et Tomat's numerous grindstones and evidence of sorghum, furthered the idea that the population at Jebel Moya was primarily pastoralist. Yet newer research led scholars to revise that point of view.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
These were associated with the Butana Group pottery, and dated to 3500–3000 BC. This area is only about 300km (200 miles) northeast of Jebel Moya. Jujube (&quot;Ziziphus&quot; sp.), a savanna shrub, was the only other definite food plant attested at Jebel Moya. Pottery. Most of the pottery found at Jebel Moya was not directly inside burials, but found in burial contexts.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
These were associated with the Butana Group pottery, and dated to 3500–3000 BC. This area is only about 300km (200 miles) northeast of Jebel Moya. Jujube (&quot;Ziziphus&quot; sp.), a savanna shrub, was the only other definite food plant attested at Jebel Moya. Pottery. Most of the pottery found at Jebel Moya was not directly inside burials, but found in burial contexts.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
This area is only about 300km (200 miles) northeast of Jebel Moya. Jujube (&quot;Ziziphus&quot; sp.), a savanna shrub, was the only other definite food plant attested at Jebel Moya. Pottery. Most of the pottery found at Jebel Moya was not directly inside burials, but found in burial contexts. The pottery samples at Jebel Moya are categorized into assemblages by their types and dates.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333
Assemblage 3 has been OSL dated from 100 BCE to 500 CE. The majority of the graves at Jebel Moya date from this time. The later occupation of Jebel et Tomat also dates to this period, whose pottery is similar to Jebel Moya's during this period. Both are thin and burnished. Assemblage 3 pottery was also found at Abu Geili, an agro-pastoralist site 30 kilometers east of Jebel Moya.

Geographic entities mentioned:
surface_form: jebel moya
instance_of: Mountain
countries: Sudan
coordinates: lat: 13.5
lon: 33.333333