Sarmila/GeoWiki-Features huggingface dataset:
Chawpi Urqu (Yocalla). Chawpi Urqu (Quechua &quot;chawpi&quot; central, middle, &quot;urqu&quot; mountain, &quot;central mountain&quot;, also spelled &quot;Chaupi Orkho&quot;) is a mountain in the Bolivian Andes which reaches a height of approximately. It is located in the Potosí Department, Tomás Frías Province, Yocalla Municipality. It lies northeast of Wichhu Qullu.

Geographic entities mentioned:
surface_form: chawpi urqu (yocalla)
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.52138889
lon: -65.88111111
Chawpi Urqu (Yocalla). Chawpi Urqu (Quechua &quot;chawpi&quot; central, middle, &quot;urqu&quot; mountain, &quot;central mountain&quot;, also spelled &quot;Chaupi Orkho&quot;) is a mountain in the Bolivian Andes which reaches a height of approximately. It is located in the Potosí Department, Tomás Frías Province, Yocalla Municipality. It lies northeast of Wichhu Qullu.

Geographic entities mentioned:
surface_form: chawpi urqu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.52138889
lon: -65.88111111
As of 2010, the total population of Greater Pittston is 48,020. This region includes Avoca, Dupont, Duryea, Exeter Boro, Exeter Township, Hughestown, Jenkins Township, Laflin, Pittston Township, West Pittston, West Wyoming, Wyoming, and Yatesville. It is a subregion of Wyoming Valley. Geography. Greater Pittston is a region in Luzerne County, Pennsylvania, encompassing the Susquehanna River.

Geographic entities mentioned:
surface_form: Wyoming Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
It was established in 1975. It is part of the Talamanca Range-La Amistad Reserves/La Amistad National Park UNESCO World Heritage Site due to its unique environment and outstanding biological diversity. It is named for its most prominent feature, Cerro Chirripó, which at is the highest mountain in Costa Rica. Geography. Chirripó is the 38th most prominent peak in the world.

Geographic entities mentioned:
surface_form: Cerro Chirripó
instance_of: Mountain
countries: Costa Rica
coordinates: lat: 9.4840833333333
lon: -83.488666666667
High Crag. High Crag stands at the southern end of the High Stile ridge which divides the valleys of Ennerdale and Buttermere in the west of the English Lake District. It is often climbed as part of a popular ridge walk, from Black Sail youth hostel, or from Buttermere via Scarth Gap. Panoramas of Great Gable and the Scafells are visible. Topography.

Geographic entities mentioned:
surface_form: High Stile
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.521669444444
lon: -3.2838111111111
surface_form: Buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: high crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.514638888889
lon: -3.2681388888889
High Crag. High Crag stands at the southern end of the High Stile ridge which divides the valleys of Ennerdale and Buttermere in the west of the English Lake District. It is often climbed as part of a popular ridge walk, from Black Sail youth hostel, or from Buttermere via Scarth Gap. Panoramas of Great Gable and the Scafells are visible. Topography.

Geographic entities mentioned:
surface_form: Great Gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
It is often climbed as part of a popular ridge walk, from Black Sail youth hostel, or from Buttermere via Scarth Gap. Panoramas of Great Gable and the Scafells are visible. Topography. The Western Fells occupy a triangular sector of the Lake District, bordered by the River Cocker to the north east and Wasdale to the south east. Westwards the hills diminish toward the coastal plain of Cumberland.

Geographic entities mentioned:
surface_form: Wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
Westwards the hills diminish toward the coastal plain of Cumberland. At the central hub of the high country are Great Gable and its satellites, while two principal ridges fan out on either flank of Ennerdale, the western fells in effect being a great horseshoe around this long wild valley.

Geographic entities mentioned:
surface_form: Great Gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
surface_form: Ennerdale
instance_of: Valley
countries: United Kingdom
At the central hub of the high country are Great Gable and its satellites, while two principal ridges fan out on either flank of Ennerdale, the western fells in effect being a great horseshoe around this long wild valley. The highest section of the northern branch is formed by the trio of Buttermere fells, High Crag, High Stile and Red Pike.

Geographic entities mentioned:
surface_form: Buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: High Stile
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.521669444444
lon: -3.2838111111111
surface_form: high crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.514638888889
lon: -3.2681388888889
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
The highest section of the northern branch is formed by the trio of Buttermere fells, High Crag, High Stile and Red Pike. The Buttermere Fells, also known as Buttermere Edge, form the watershed between Buttermere and Upper Ennerdale. The Ennerdale flanks are steep and rough, put with only small areas of crag, the lower slopes being planted with a ribbon of conifers.

Geographic entities mentioned:
surface_form: Buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
Across the narrow ridge-top to the north are deep corries and dark walls of crag, glowering down over the lake. The ridge continues south east to Haystacks and the Great Gable group. Beyond Red Pike to the west are Starling Dodd, Great Borne and the Loweswater Fells.

Geographic entities mentioned:
surface_form: Great Gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
The ridge continues south east to Haystacks and the Great Gable group. Beyond Red Pike to the west are Starling Dodd, Great Borne and the Loweswater Fells. High Crag forms the eastern terminus of the Buttermere Fells, its most arresting feature being the great scree slopes of Gamlin End where the high ground falls away. below, the ridge levels out once more and throws up the craggy top of Seat ().

Geographic entities mentioned:
surface_form: Starling Dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.530180555556
lon: -3.32735
surface_form: Great Borne
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.53435
lon: -3.35685
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
Birkness Comb, also called Burtness Comb on Ordnance Survey maps, lies between the truncated and unnamed northern ridges of High Crag and High Stile. Drained into Buttermere by Comb Beck, its headwall is rimmed by crags on all sides. Sheepbone Buttress flanks High Crag, which also has a share in Comb Crags, lining the onward ridge.

Geographic entities mentioned:
surface_form: Buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
Summit. The triangular summit has a cairn at the high point above Gamlin End. The view is restricted by High Stile, but the head of Ennerdale- backed by the Scafells- presents a fine picture. More distant glimpses of Skiddaw and the Helvellyn range are also granted. A short walk north west toward the top of the crags brings Buttermere and Crummock Water into sight. Ascents.

Geographic entities mentioned:
surface_form: High Stile
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.521669444444
lon: -3.2838111111111
Summit. The triangular summit has a cairn at the high point above Gamlin End. The view is restricted by High Stile, but the head of Ennerdale- backed by the Scafells- presents a fine picture. More distant glimpses of Skiddaw and the Helvellyn range are also granted. A short walk north west toward the top of the crags brings Buttermere and Crummock Water into sight. Ascents.

Geographic entities mentioned:
surface_form: Skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
Summit. The triangular summit has a cairn at the high point above Gamlin End. The view is restricted by High Stile, but the head of Ennerdale- backed by the Scafells- presents a fine picture. More distant glimpses of Skiddaw and the Helvellyn range are also granted. A short walk north west toward the top of the crags brings Buttermere and Crummock Water into sight. Ascents.

Geographic entities mentioned:
surface_form: Buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: Crummock Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.55
lon: -3.3
High Crag. High Crag stands at the southern end of the High Stile ridge which divides the valleys of Ennerdale and Buttermere in the west of the English Lake District. It is often climbed as part of a popular ridge walk, from Black Sail youth hostel, or from Buttermere via Scarth Gap. Panoramas of Great Gable and the Scafells are visible. Topography.

Geographic entities mentioned:
surface_form: high crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.514638888889
lon: -3.2681388888889
The ridge continues south east to Haystacks and the Great Gable group. Beyond Red Pike to the west are Starling Dodd, Great Borne and the Loweswater Fells. High Crag forms the eastern terminus of the Buttermere Fells, its most arresting feature being the great scree slopes of Gamlin End where the high ground falls away. below, the ridge levels out once more and throws up the craggy top of Seat ().

Geographic entities mentioned:
surface_form: high crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.514638888889
lon: -3.2681388888889
All three Buttermere Fells throw out a rocky spur toward the lake, these walls enclosing Birkness and Bleaberry Combs. Birkness Comb, also called Burtness Comb on Ordnance Survey maps, lies between the truncated and unnamed northern ridges of High Crag and High Stile. Drained into Buttermere by Comb Beck, its headwall is rimmed by crags on all sides.

Geographic entities mentioned:
surface_form: high crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.514638888889
lon: -3.2681388888889
Drained into Buttermere by Comb Beck, its headwall is rimmed by crags on all sides. Sheepbone Buttress flanks High Crag, which also has a share in Comb Crags, lining the onward ridge. It is the great scooped hollow of the Comb which results in the narrowness of Buttermere Edge. The northern spur also ends abruptly as High Crag Buttress, a further tier of rock lying just above the lakeshore.

Geographic entities mentioned:
surface_form: high crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.514638888889
lon: -3.2681388888889
Sheepbone Buttress flanks High Crag, which also has a share in Comb Crags, lining the onward ridge. It is the great scooped hollow of the Comb which results in the narrowness of Buttermere Edge. The northern spur also ends abruptly as High Crag Buttress, a further tier of rock lying just above the lakeshore. Geology.

Geographic entities mentioned:
surface_form: high crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.514638888889
lon: -3.2681388888889
Interbeds of volcaniclastic sandstone and lapilli tuff also appear. Seat is an outcrop of the flow banded andesite lavas of the Haystacks Member, shot through with quartz-feldspar phyric microgranite. There was small scale mining activity in the late nineteenth century beneath Low Wax Knott, adjacent to the Scarth Gap path. Two men worked the operation, living on the fellside in a hut.

Geographic entities mentioned:
surface_form: knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.686211111111
lon: -3.0935388888889
He was born in Wasserburg am Inn, Bavaria. Career. on 15 March 1936, he became the first man in history to stand to stand on feet a &quot;flight&quot; of more than one hundred meters at 101.5 m (333 ft) on Bloudkova velikanka hill in Planica, Kingdom of Yugoslavia.

Geographic entities mentioned:
surface_form: Planica
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.476944444444
lon: 13.722222222222
On 15 March 1938, exactly two years later after historic jump, he set another world record at 107 m (351 ft), this time again on Bloudkova velikanka hill in Planica, Kingdom of Yugoslavia. He won the ski jumping gold medal at the 1939 FIS Nordic World Ski Championships in Zakopane while competing under Nazi Germany in the wake of Austria being annexed in late 1938.

Geographic entities mentioned:
surface_form: Planica
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.476944444444
lon: 13.722222222222
A company called Zakłady Budowy Nadwozi Samochodowych (Automobile Chassis Works) was established. After the factory was rebuilt, the company started to develop and build bus bodies for Lublin and Star trucks, including buses such as the Jelcz PR110D. In 1974, the Polish expedition to Lhotse used a Jelcz 316 car to travel from Warsaw to Nepal.

Geographic entities mentioned:
surface_form: Lhotse
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.961666666667
lon: 86.933333333333
In 1974, the Polish expedition to Lhotse used a Jelcz 316 car to travel from Warsaw to Nepal. In 1975, the expedition of the Wrocław Mountain Club to Broad Peak Central, in Pakistan, used a Jelcz 315-M car to travel from Wrocław to Islamabad, driving up to 9,000 km between 2 and 21 May. Since 2004, Jelcz Sp. z o.o.

Geographic entities mentioned:
surface_form: Broad Peak
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.810555555556
lon: 76.568055555556
Lulonga River. The Lulonga (,) is a river in the Equateur province of Democratic Republic of the Congo. It is about 200 km long from its beginning at the town of Basankusu. The Lopori and the Maringa join to form the Lulonga there. The Lulonga River flows into the Congo River at the village of Lolanga.

Geographic entities mentioned:
surface_form: Lopori
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: 1.236166
lon: 19.811654
surface_form: Maringa
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: 1.228572
lon: 19.817963
The sites of Lal Chatto, Mashak Lohri and Lakhiyo situated along the bank of Lake Manchar are the most ancient sites, which date from the Harappan culture. The lake was formed when a branch of the Indus River flowed from Kashmore. In 1921, it was connected to Hamal Lake via the Main Nara Valley Drain. In 1958, the lake completely evaporated due to drought.

Geographic entities mentioned:
surface_form: Hamal Lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 27.449
lon: 67.632
Officials had hoped the ploy would protect up to 500,000 people from flooding. Geography. Lake Manchar is directly south of Hamal Lake, and the two are connected by the Main Nara Valley Drain built in 1921. Manchar lake's surface area fluctuates with the seasons - from as little as 200 km2 to as much as 500 km2 during monsoon rains. The average depth is only 2.5 to 3.75 metres.

Geographic entities mentioned:
surface_form: Hamal Lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 27.449
lon: 67.632
surface_form: lake manchar
instance_of: Lake
countries: Pakistan
coordinates: lat: 26.41
lon: 67.68
Lake Manchar. Lake Manchar (,), also spelled Manchhar, is the largest natural freshwater lake in Pakistan, and one of the largest in South Asia. It is located west of the Indus River, in Jamshoro and Dadu districts of Sindh, away from Sehwan. Lake Manchar collects water from numerous small streams in the Kirthar Mountains, and then empties into the Indus River.

Geographic entities mentioned:
surface_form: lake manchar
instance_of: Lake
countries: Pakistan
coordinates: lat: 26.41
lon: 67.68
It is located west of the Indus River, in Jamshoro and Dadu districts of Sindh, away from Sehwan. Lake Manchar collects water from numerous small streams in the Kirthar Mountains, and then empties into the Indus River. The lake's surface area fluctuates with the seasons, from as little as 36 km2, to as much as 500 km2 during monsoon rains. History.

Geographic entities mentioned:
surface_form: lake manchar
instance_of: Lake
countries: Pakistan
coordinates: lat: 26.41
lon: 67.68
History. The lake's banks and vicinity are home to ancient archaeological sites Ghazi Shah, Wahi Pandhi and Ali Murad Mound. The sites of Lal Chatto, Mashak Lohri and Lakhiyo situated along the bank of Lake Manchar are the most ancient sites, which date from the Harappan culture. The lake was formed when a branch of the Indus River flowed from Kashmore.

Geographic entities mentioned:
surface_form: lake manchar
instance_of: Lake
countries: Pakistan
coordinates: lat: 26.41
lon: 67.68
The diversion of water from the Indus and a diminished storm runoff from the Kirthar mountains have contributed to the reduction in fresh water supplies, resulting in the water becoming saline, and killing off fish. At the same time, saline drainage water from agricultural fields of Balochistan and surrounding areas flows into Lake Manchar.

Geographic entities mentioned:
surface_form: lake manchar
instance_of: Lake
countries: Pakistan
coordinates: lat: 26.41
lon: 67.68
Population. Lake Manchar is populated by the Mohana tribe, who are sometimes referred to as the &quot;Boat People.&quot; The lake supports thousands of fisherfolk, who depend on the freshwater fish in the lake.

Geographic entities mentioned:
surface_form: lake manchar
instance_of: Lake
countries: Pakistan
coordinates: lat: 26.41
lon: 67.68
Officials had hoped the ploy would protect up to 500,000 people from flooding. Geography. Lake Manchar is directly south of Hamal Lake, and the two are connected by the Main Nara Valley Drain built in 1921. Manchar lake's surface area fluctuates with the seasons - from as little as 200 km2 to as much as 500 km2 during monsoon rains. The average depth is only 2.5 to 3.75 metres.

Geographic entities mentioned:
surface_form: manchar lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 26.41
lon: 67.68
Since then, the IES has organised and sponsored some of the most important archaeological projects carried out in the country including Tel Hazor, Masada, the excavations in Jerusalem near the Temple Mount, in the Jewish Quarter, and at the City of David, the Judean Desert Expeditions, En-Gedi, Tel Arad, Lachish, Aphek, Jericho, Herodium, Yoqneam, Dor and Tel Megiddo.

Geographic entities mentioned:
surface_form: Yoqneam
instance_of: Mountain
countries: Israel
coordinates: lat: 32.6640988
lon: 35.1082661
Its highest peak, Great Giewont (&quot;Wielki Giewont&quot;), is above sea level and one of the highest peaks of the Western Tatras (Polish: &quot;Tatry Zachodnie&quot;) located entirely within Poland's borders. The mountain is regarded as the symbol of Zakopane, the Polish Tatras and Podhale, which throughout history has been the subject of many legends, poems and works of art. Geography.

Geographic entities mentioned:
surface_form: Podhale
instance_of: Valley
countries: Poland
coordinates: lat: 49.4793
lon: 20.0291
surface_form: podhale
instance_of: Valley
countries: Poland
coordinates: lat: 49.4793
lon: 20.0291
Giewont. Giewont () is a mountain massif in the Tatra Mountains of Poland. Its highest peak, Great Giewont (&quot;Wielki Giewont&quot;), is above sea level and one of the highest peaks of the Western Tatras (Polish: &quot;Tatry Zachodnie&quot;) located entirely within Poland's borders.

Geographic entities mentioned:
surface_form: giewont
instance_of: Mountain
countries: Poland
coordinates: lat: 49.250556
lon: 19.933889
Giewont. Giewont () is a mountain massif in the Tatra Mountains of Poland. Its highest peak, Great Giewont (&quot;Wielki Giewont&quot;), is above sea level and one of the highest peaks of the Western Tatras (Polish: &quot;Tatry Zachodnie&quot;) located entirely within Poland's borders.

Geographic entities mentioned:
surface_form: giewont
instance_of: Mountain
countries: Poland
coordinates: lat: 49.250556
lon: 19.933889
surface_form: giewont
instance_of: Mountain
countries: Poland
coordinates: lat: 49.250556
lon: 19.933889
Geography. Giewont lies in the area of the Polish Tatra National Park (&quot;Tatrzański Park Narodowy&quot;). It encompasses three peaks: Small Giewont (Polish: &quot;Mały Giewont&quot;,), Great Giewont (&quot;Wielki Giewont&quot;,) and Long Giewont (&quot;Długi Giewont&quot;,). There is a mountain pass located between Great and Long Giewont, known as Szczerba ().

Geographic entities mentioned:
surface_form: giewont
instance_of: Mountain
countries: Poland
coordinates: lat: 49.250556
lon: 19.933889
surface_form: giewont
instance_of: Mountain
countries: Poland
coordinates: lat: 49.250556
lon: 19.933889
surface_form: giewont
instance_of: Mountain
countries: Poland
coordinates: lat: 49.250556
lon: 19.933889
surface_form: giewont
instance_of: Mountain
countries: Poland
coordinates: lat: 49.250556
lon: 19.933889
surface_form: giewont
instance_of: Mountain
countries: Poland
coordinates: lat: 49.250556
lon: 19.933889
surface_form: giewont
instance_of: Mountain
countries: Poland
coordinates: lat: 49.250556
lon: 19.933889
surface_form: giewont
instance_of: Mountain
countries: Poland
coordinates: lat: 49.250556
lon: 19.933889
It is located between the valleys of Kondratowa, Małej Łąki and Strążyska. The high northern face of Great Giewont is clearly visible from the nearby town of Zakopane and remains one of the most characteristic features of the panorama of the Polish Tatras. Geologically, Giewont is composed of dolomite and limestone caves, as well as gneiss and granite in the southern section.

Geographic entities mentioned:
surface_form: giewont
instance_of: Mountain
countries: Poland
coordinates: lat: 49.250556
lon: 19.933889
It might originate from the German word &quot;Gewand&quot; (rock formation); however, according to Mariusz Zaruski, the name has its roots like many other names in the Tatras in a family name of Goral people considering the fact that families bearing this name, which, however, could also derive from the German word, still lived in the area
The first recorded ascent to Giewont's summit was undertaken in 1830 by Franciszek Herbich and Aleksander Zawadzki.

Geographic entities mentioned:
surface_form: giewont
instance_of: Mountain
countries: Poland
coordinates: lat: 49.250556
lon: 19.933889
Cultural significance. In Polish folklore, the mountain is associated with several legends about sleeping knights who will awake when Poland is in danger. The profile of the mountain resembles a lying knight, wherein the Long Giewont is the knight's torso, and the Great Giewont is the knight's face as viewed from the side (the three 'peaks' representing the chin, the nose, and the eyebrow).

Geographic entities mentioned:
surface_form: giewont
instance_of: Mountain
countries: Poland
coordinates: lat: 49.250556
lon: 19.933889
surface_form: giewont
instance_of: Mountain
countries: Poland
coordinates: lat: 49.250556
lon: 19.933889
Phnom Dei. Phnom Dei () is a 272 m high hill close to Siem Reap, Cambodia. Location. Phnom Dei is located to the southeast of the Banteay Srei, one of the major Angkorian temples, and south of Phnom Kulen. It is part of the temple complex in Angkor, the area that was the capital of the Khmer Empire. Angkorian temple.

Geographic entities mentioned:
surface_form: Phnom Kulen
instance_of: Mountain
countries: Cambodia
coordinates: lat: 13.612777777778
lon: 104.1125
surface_form: phnom dei
instance_of: Mountain
countries: Cambodia
coordinates: lat: 13.59583333
lon: 103.98361111
It is part of the temple complex in Angkor, the area that was the capital of the Khmer Empire. Angkorian temple. There is a temple on top of the hill that was built during the reign of King Yasovarman I (889-910 AD). Phnom Dei is only one of the hilltop temples built during King Yasovarman I's reign, the others being Phnom Bakheng, Phnom Bok and Phnom Krom.

Geographic entities mentioned:
surface_form: Phnom Bok
instance_of: Mountain
countries: Cambodia
coordinates: lat: 13.466111111111
lon: 103.98194444444
surface_form: Phnom Krom
instance_of: Mountain
countries: Cambodia
coordinates: lat: 13.28573
lon: 103.81218
surface_form: phnom dei
instance_of: Mountain
countries: Cambodia
coordinates: lat: 13.59583333
lon: 103.98361111
Phnom Dei. Phnom Dei () is a 272 m high hill close to Siem Reap, Cambodia. Location. Phnom Dei is located to the southeast of the Banteay Srei, one of the major Angkorian temples, and south of Phnom Kulen. It is part of the temple complex in Angkor, the area that was the capital of the Khmer Empire. Angkorian temple.

Geographic entities mentioned:
surface_form: phnom dei
instance_of: Mountain
countries: Cambodia
coordinates: lat: 13.59583333
lon: 103.98361111
Shortly after taking the throne in 1510, Qasim Khan fought against his cousin Muhammad Shaybani for control of the Desht-i-Kipchak region. After Shaybani and the Uzbeks suffered severe losses in numerous battles near Lake Balkhash, the Uzbek Khanate agreed to give Qasim Khan and the Kazakhs all former Uzbek lands north of the Syr Darya.

Geographic entities mentioned:
surface_form: Lake Balkhash
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 46.540833333333
lon: 74.878888888889
Washington. There are around 880 glaciers in Washington state, with 186 named according to the Geographic Names Information System (GNIS). However, the 1980 eruption of Mount St. Helens eliminated nine of its eleven named glaciers and only the new glacier known as Crater Glacier has been reestablished since. Mount St.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
Geography. Megatushon Creek originates on the east side of the massive Level Mountain shield volcano, near the headwaters of the Little Tuya River, Kaha Creek, Lost Creek, and Beatty Creek, and about east of Meszah Peak, the highest peak of the Level Mountain Range, a cluster of bare peaks on the summit of Level Mountain.

Geographic entities mentioned:
surface_form: Kaha Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.68283
lon: -131.68693
surface_form: Meszah Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 58.4786
lon: -131.437
surface_form: megatushon creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.59934
lon: -131.08793
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Megatushon Creek. Megatushon Creek is a tributary of the Nahlin River, part of the Taku River watershed in northwest part of the province of British Columbia, Canada. It flows generally northeast and east for roughly to join the Nahlin River not far from the Nahlin's source south of Tachilta Lakes. Megatushon Creek's watershed covers, and its mean annual discharge is estimated at.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: megatushon creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.59934
lon: -131.08793
Megatushon Creek's watershed covers, and its mean annual discharge is estimated at. The mouth of Megatushon Creek is located about west of Dease Lake, British Columbia, about north of Telegraph Creek, British Columbia, and about east of Juneau, Alaska. Megatushon Creek's watershed's land cover is classified as 34.8% barren, 32.3% shrubland, 24.8% conifer forest, and small amounts of other cover.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: megatushon creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.59934
lon: -131.08793
surface_form: dease lake
instance_of: Lake
countries: Canada
coordinates: lat: 58.63502
lon: -130.03761
Megatushon Creek. Megatushon Creek is a tributary of the Nahlin River, part of the Taku River watershed in northwest part of the province of British Columbia, Canada. It flows generally northeast and east for roughly to join the Nahlin River not far from the Nahlin's source south of Tachilta Lakes. Megatushon Creek's watershed covers, and its mean annual discharge is estimated at.

Geographic entities mentioned:
surface_form: megatushon creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.59934
lon: -131.08793
It flows generally northeast and east for roughly to join the Nahlin River not far from the Nahlin's source south of Tachilta Lakes. Megatushon Creek's watershed covers, and its mean annual discharge is estimated at. The mouth of Megatushon Creek is located about west of Dease Lake, British Columbia, about north of Telegraph Creek, British Columbia, and about east of Juneau, Alaska.

Geographic entities mentioned:
surface_form: megatushon creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.59934
lon: -131.08793
Megatushon Creek's watershed covers, and its mean annual discharge is estimated at. The mouth of Megatushon Creek is located about west of Dease Lake, British Columbia, about north of Telegraph Creek, British Columbia, and about east of Juneau, Alaska. Megatushon Creek's watershed's land cover is classified as 34.8% barren, 32.3% shrubland, 24.8% conifer forest, and small amounts of other cover.

Geographic entities mentioned:
surface_form: megatushon creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.59934
lon: -131.08793
Megatushon Creek's watershed's land cover is classified as 34.8% barren, 32.3% shrubland, 24.8% conifer forest, and small amounts of other cover. Megatushon Creek is in the traditional territory of the Tlingit Taku River Tlingit First Nation and the Tahltan First Nation, of the Tahltan people. Geography.

Geographic entities mentioned:
surface_form: megatushon creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.59934
lon: -131.08793
surface_form: tlingit
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
surface_form: tlingit
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
The creek flows north, northwest, and east, first through Level Mountain's high and relatively barren lava plateau, then through rugged forested terrain, before emptying into the Nahlin River.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Val's first vocal is joined by a banjo that emphasizes the song's triple meter. Siegel compares the vocal to that of bluegrass musician Bill Monroe, in particular Monroe's rendition of the murder ballad &quot;Roane County Prison&quot;, a traditional song from the Upper Cumberland area of Tennessee sometimes known as &quot;In the Hills of Roane County&quot;. Release.

Geographic entities mentioned:
surface_form: Upper Cumberland
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
Anglican Church, at the Huron Diocese, Ontario, 1859. Sorby began designing for Canadian clients while still domiciled in the United Kingdom. He designed an Anglican church &quot;on the banks of Lake Huron&quot;, possibly at Collingwood, in the Huron Anglican Diocese in 1859, early in his career. The church was for a &quot;small and scattered congregation&quot;.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Mount Stephen House, Field, British Columbia, 1886. Mount Stephen House, a hotel in Field, British Columbia, was designed by Sorby for the CPR, and opened in 1886. It was built in chalet style, &quot;fifty miles west of Banff, Alberta, in Kicking Horse Canyon, at the base of Mount Stephen&quot;. It accommodated tourists including fishermen, climbers and artists.

Geographic entities mentioned:
surface_form: Mount Stephen
instance_of: Mountain
countries: Canada
coordinates: lat: 51.399166
lon: -116.436389
Although at that time any religious activity was punishable by law, followers of the Evangelical tradition continued practicing their faith and gathered secretly in basements to avoid deportation to Siberia. Particularly Armenians of Musa Dagh (Musa Ler) became pioneers of Evangelical faith and adherence to their traditions despite continuous threats by the police and the neighborhood watch.

Geographic entities mentioned:
surface_form: Musa Dagh
instance_of: Mountain
countries: Turkey
coordinates: lat: 36.258333333333
lon: 35.903611111111
We knew we would be budget-limited, but the audience should not feel these limits. And we do not want to complain, it forced us to be imaginative.&quot;
Locations. The scenes of the planet Mars were shot in Morocco. The other scenes were shot in France: in La Rochelle for the scenes inside the spacecraft, near Tours, in an open pit near Chartres and on the slopes of Mont Blanc. Series 1.

Geographic entities mentioned:
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
He is famed in the Catholic Church, the Eastern Orthodox Church, the Lutheran Churches, the Anglican Communion, and Old Catholic Churches. In 1964, Pope Paul VI declared Benedict a patron saint of Europe. Benedict founded twelve communities for monks at Subiaco in present-day Lazio, Italy (about to the east of Rome), before moving southeast to Monte Cassino in the mountains of central Italy.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
Having failed by sending him poisonous bread, Florentius tried to seduce his monks with some prostitutes. To avoid further temptations, in about 530 Benedict left Subiaco. He founded 12 monasteries in the vicinity of Subiaco, and, eventually, in 530 he founded the great Benedictine monastery of Monte Cassino, which lies on a hilltop between Rome and Naples. Veneration.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
He founded 12 monasteries in the vicinity of Subiaco, and, eventually, in 530 he founded the great Benedictine monastery of Monte Cassino, which lies on a hilltop between Rome and Naples. Veneration. Benedict died of a fever at Monte Cassino not long after his sister, Scholastica, and was buried in the same tomb. According to tradition, this occurred on 21 March 547.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
He was appointed president of the board of conciliation in 1894, but resigned some 15 months later. Late life and legacy. Bundey retired on a pension in 1903, was knighted in 1904, and died on 6 December 1909 at his home at Mount Lofty in South Australia. In 1865 he married Ellen Wardlaw, daughter of Sir William Milne, who survived him with a daughter, Ellen Milne Bundey.

Geographic entities mentioned:
surface_form: Mount Lofty
instance_of: Mountain
countries: Australia
coordinates: lat: -34.966666666667
lon: 138.7
Kambarangoh. is an area along the summit trail to Low's Peak on Mount Kinabalu in Sabah, Borneo. It lies between the Power Station and Layang-Layang at an altitude of about 7,000ft. It shares its name with the only telecommunications station on the mountain, which is owned by Kambarangoh Telecoms.

Geographic entities mentioned:
surface_form: Mount Kinabalu
instance_of: Mountain
countries: Malaysia
coordinates: lat: 6.075
lon: 116.5586111111111
2020: Debut single and other projects. In March 2020, she appeared with fellow runner up of &quot;HaKokhav HaBa&quot; Orr Amrami Brockman in an advertising to Israeli telecommunications company Bezeq, along with the presenter of the company commercials, Israeli singer Gidi Gov. In April she performed with Amrami Brockman in Israel Independence national ceremony, held in Mount Herzl.

Geographic entities mentioned:
surface_form: Mount Herzl
instance_of: Mountain
countries: Israel
coordinates: lat: 31.774117
lon: 35.180567
White Otter Lake. White Otter Lake is a lake in Kenora District in northwestern Ontario, Canada.

Geographic entities mentioned:
surface_form: otter lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.77111111111111
lon: -89.46138888888889
surface_form: otter lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.78375
lon: -76.1239
surface_form: white otter lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.0833
lon: -91.8667
surface_form: otter lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.27792
lon: -79.9676
surface_form: otter lake
instance_of: Lake
countries: Canada
coordinates: lat: 55.5833
lon: -104.667
Springerville volcanic field is a monogenetic volcanic field located in east-central Arizona between Springerville and Show Low. The field consists of 405 discrete vents covering approximately and is the third-largest such field in the continental United States; only the San Francisco volcanic field and Medicine Lake volcanic field are larger. The total erupted volume is estimated at.

Geographic entities mentioned:
surface_form: medicine lake
instance_of: Lake
countries: United States
coordinates: lat: 45.00644
lon: -93.41997
surface_form: medicine lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9841655
lon: -97.3519987
Springerville volcanic field. Springerville volcanic field is a monogenetic volcanic field located in east-central Arizona between Springerville and Show Low. The field consists of 405 discrete vents covering approximately and is the third-largest such field in the continental United States; only the San Francisco volcanic field and Medicine Lake volcanic field are larger.

Geographic entities mentioned:
surface_form: springerville volcanic field
instance_of: Mountain
countries: United States
coordinates: lat: 34.25
lon: -109.567
The total erupted volume is estimated at. The field is located towards the western end of the Jemez Lineament. Economic resources. The St. Johns carbon dioxide reservoir is located in the northwest part of the Springerville volcanic field and has estimated reserves of 445 billion cubic meters.

Geographic entities mentioned:
surface_form: springerville volcanic field
instance_of: Mountain
countries: United States
coordinates: lat: 34.25
lon: -109.567
Additionally, 4 agreements on development and production sharing for the Azerbaijani sector of the Caspian Sea were signed. After the visit, Aliyev issued an order on “Measures to expand partnership relations between the Republic of Azerbaijan and the United States” on 2 September 1997.

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
After a year-long series of negotiations in Baku, Istanbul and Houston, the “Agreement on the Joint Development and Production Sharing for the Azeri and Chirag Fields and the Deep Water Portion of the Gunashli Field in the Azerbaijan Sector of the Caspian Sea” was signed in Baku on 20 September 1994 by the Government of Azerbaijan and a consortium of 11 oil companies from 6 countries (US, UK, Russia, Norway, Turkey, Saudi Arabia) in the presence of Aliyev.

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
He turned the south side Lake Michigan lakefront area, especially the Hyde Park community area and neighboring Kenwood and Woodlawn neighborhoods, into a resort community that had its heyday from the 1850s through the early 20th century. He was also an urban planner who paved the way for and preserved many of the parks that are now in the Chicago Park District.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
He selected the name Hyde Park to associate the area with the elite high class neighborhoods of New York and London. At about the same time, he built the Hyde Park House a 4-story hotel at 53rd Street and Lake Michigan. The hotel became the focal point of the community and drew affluent guests with leisure time and discretionary income. This site is now occupied by the Hampton House.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
It is situated in the Arequipa Region, Condesuyos Province, Cayarani District, and in the La Unión Province, Puyca District. Yana Yana lies northeast of Janq'u Q'awa and southeast of Kunturi.

Geographic entities mentioned:
surface_form: kunturi
instance_of: Mountain
countries: Peru
coordinates: lat: -15.0178
lon: -72.4725
surface_form: kunturi
instance_of: Mountain
countries: Peru
coordinates: lat: -16.2133
lon: -71.1472
surface_form: kunturi
instance_of: Mountain
countries: Peru
coordinates: lat: -14.8858
lon: -72.4728
surface_form: kunturi
instance_of: Mountain
countries: Peru
coordinates: lat: -15.3097
lon: -71.0897
Yana Yana (Peru). Yana Yana (Aymara &quot;yana&quot; black,night, Quechua &quot;yana&quot; black, the reduplication indicates that there is a group or a complex of something, may be &quot;a complex of black color&quot;) is a mountain in the Wansu mountain range in the Andes of Peru.

Geographic entities mentioned:
surface_form: yana yana
instance_of: Mountain
countries: Peru
coordinates: lat: -11.71833333
lon: -76.33083333
surface_form: yana yana
instance_of: Mountain
countries: Peru
coordinates: lat: -14.9481
lon: -72.3678
In August, the margraves of Meissen, Lusatia, and the Nordmark joined with the troops of the Bishop of Halberstadt under the leadership of Gisilher and defeated the Slavs at Belkesheim, near Stendal. Nevertheless, the Germans were once again limited to the land west of the Elbe. In March 984, Gisilher hosted Henry II, Duke of Bavaria, in Magdeburg on Palm Sunday.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Early years. Born in Bronx, New York, Friedman spent her formative years in the San Fernando Valley, north of Los Angeles after her family moved to Southern California when she was 10. She started playing guitar at the age of eight while listening to Woody Guthrie, Pete Seeger and Josh White.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Lake Lewis was formed when the restricted flow of waters from periodic cataclysmic floods from Glacial Lake Missoula, pluvial Lake Bonneville, and perhaps from subglacial outbursts, backed up through the constriction formed by the Wallula Gap in the Horse Heaven Hills (southern Washington).

Geographic entities mentioned:
surface_form: Horse Heaven Hills
instance_of: Landform
countries: United States
coordinates: lat: 46.13
lon: -119.87
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: lake lewis
instance_of: Lake
countries: United States
coordinates: lat: 46.1667
lon: -119
Glacial erratics. The maximum elevation of the flood, as established by other indications, is confirmed by glacial erratics, which were stranded on the slopes of the Horse Heaven Hills and other elevated regions in the mid-Columbia at elevations of up to above sea level. There were several long ridges (Saddle Mountains, Frenchman Hills, and Rattlesnake Mountain) that were above flood level.

Geographic entities mentioned:
surface_form: Horse Heaven Hills
instance_of: Landform
countries: United States
coordinates: lat: 46.13
lon: -119.87
surface_form: horse heaven hills
instance_of: Landform
countries: United States
coordinates: lat: 46.13
lon: -119.87
Glacial erratics. The maximum elevation of the flood, as established by other indications, is confirmed by glacial erratics, which were stranded on the slopes of the Horse Heaven Hills and other elevated regions in the mid-Columbia at elevations of up to above sea level. There were several long ridges (Saddle Mountains, Frenchman Hills, and Rattlesnake Mountain) that were above flood level.

Geographic entities mentioned:
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.458333333333
lon: -121.80611111111
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.25243
lon: -115.60644
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1322
lon: -74.8634
surface_form: frenchman hills
instance_of: Landform
countries: United States
coordinates: lat: 47
lon: -120
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6997
lon: -72.8328
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.4056
lon: -119.611
Water also backed up further downstream on the Columbia River between Washington and Oregon, delaying the drainage of Lake Lewis. The water remained for a period of weeks before the flood waters drained through Wallula Gap, just southeast of the Tri-Cities area. Lake Lewis reached an elevation of about above sea level (today's sea level) before subsiding.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: lake lewis
instance_of: Lake
countries: United States
coordinates: lat: 46.1667
lon: -119
Lake Lewis. Lake Lewis was a large transient lake (lasting only days to weeks) in the Pacific Northwest region of North America, formed by periodic Missoula Floods along the Columbia River paleocourse between 21,000 and 16,000 years ago.

Geographic entities mentioned:
surface_form: lake lewis
instance_of: Lake
countries: United States
coordinates: lat: 46.1667
lon: -119
The water remained for a period of weeks before the flood waters drained through Wallula Gap, just southeast of the Tri-Cities area. Lake Lewis reached an elevation of about above sea level (today's sea level) before subsiding. Lake Lewis also flooded the Yakima, Walla Walla, Touchet and Tucannon river valleys. Wallula Gap.

Geographic entities mentioned:
surface_form: lake lewis
instance_of: Lake
countries: United States
coordinates: lat: 46.1667
lon: -119
The Wallula Gap constrained the flow such that less than 1/5 of the 800 km3 of water per day entering could be discharged. As a result, the floods filled the Pasco Basin and formed, for a short period, Lake Lewis.

Geographic entities mentioned:
surface_form: lake lewis
instance_of: Lake
countries: United States
coordinates: lat: 46.1667
lon: -119
Steiner Tor. Steiner Tor is a preserved gate, originally built in the late 15th century but refashioned in the Baroque style in the city of Krems an der Donau, in the Wachau valley of Austria. It is considered the symbol of the city. Until the last third of the 19th century, the city of Krems was surrounded by a wall. This was systematically razed, and three gates were also removed.

Geographic entities mentioned:
surface_form: Wachau
instance_of: Valley
countries: Austria
coordinates: lat: 48.36444
lon: 15.43417