Sarmila/GeoWiki-Features huggingface dataset:
Geography. Clunes lies northeast of Gairlochy and northeast of Spean Bridge. The B8005 road passes by Clunes on Loch Lochy, and heads west to Loch Arkaig. This section is known as the &quot;Mìle Dorcha&quot; (Gaelic for &quot;dark mile&quot;), as the road runs through a heavily tree-lined, steep sided valley.

Geographic entities mentioned:
surface_form: Loch Arkaig
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.971989
lon: -5.158376
The northernmost and easternmost points of Russia coincide with those of Eurasia (both for the mainland and including the islands). The extreme points of the Soviet Union were identical, except that the southernmost point of the Soviet Union was Kushka in Turkmenistan, and the extreme elevation was the Communism Peak in Tajikistan, at.

Geographic entities mentioned:
surface_form: Communism Peak
instance_of: Mountain
countries: Tajikistan
coordinates: lat: 38.942732
lon: 72.015347
Kushka in present-day Turkmenistan had been the southernmost point of the Empire since 1885. Again, until the Alaska Purchase, the peak of Bolshaya was the extreme point of elevation in the Empire, at 6,194 m above sea level. Extreme coordinates. 1according to the path of the International Date Line, although being located in the Western Hemisphere.

Geographic entities mentioned:
surface_form: Bolshaya
instance_of: Mountain
countries: United States
coordinates: lat: 63.06916666666667
lon: -151.0063888888889
Culture. Zhumadian has a rich cultural history and the birthplace of many great people in ancient times. There is an old site of Liang Shanbo and Zhu Yingtai who are the characters in &quot;the Butterfly Lovers&quot;, a famous Chinese story. Zhumadian is the location of Mount Chaya, a major geological site of interest and tourist attraction. Dams.

Geographic entities mentioned:
surface_form: Mount Chaya
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 33.134166666666665
lon: 113.72833333333334
In 1963, with Lama Karma Thinley Rinpoche and under the guidance of the Karmapa, she founded the Karma Drubgyu Thargay Ling nunnery for Tibetan women, now located in Tilokpur, Kangra Valley. While running the Young Lamas Home School at Dalhousie in north India, Bedi also spent time at Rumtek in Sikkim, the seat of the Karmapa in exile.

Geographic entities mentioned:
surface_form: Kangra Valley
instance_of: Valley
countries: India
coordinates: lat: 32.08638888888889
lon: 76.25333333333333
In 1175, Valdemar I also erected the Vordingborg Castle as a defensive fortress, and as a base from which to launch raids against the German coast. After the death of Absalon in 1201, Valdemar II (reign: 1202–1241) – the second son of Absalon's stepbrother Valdemar I – led a Danish expedition across the Elbe river to invade Holstein, the region between the rivers Elbe and Eider.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Course and hydrology. Johnny Creek flows east from the east end of Link Lake and runs under the Highway 11 Johnny Creek Bridge about to the east. It then flows adjacent to the Sherman Mine branch line for, eventually running under the Ontario Northland Railway main line where it flows another into Boot Bay of Net Lake. The total length of the creek is about and has an elevation of.

Geographic entities mentioned:
surface_form: Net Lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.113
lon: -79.804
The total length of the creek is about and has an elevation of. Johnny Creek is part of the Ottawa River drainage basin, a large area covering much of eastern Ontario and western Quebec where water drains into the Ottawa River. After Johnny Creek flows into Net Lake, the water drains through Net Creek, entering Cassels Lake. It then enters Rabbit Lake, which is drained by the Matabitchuan River.

Geographic entities mentioned:
surface_form: Net Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.08
lon: -79.7283
surface_form: Cassels Lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.0667
lon: -79.7167
surface_form: net lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.113
lon: -79.804
surface_form: johnny creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.0867
lon: -79.7567
After Johnny Creek flows into Net Lake, the water drains through Net Creek, entering Cassels Lake. It then enters Rabbit Lake, which is drained by the Matabitchuan River. The Matabitchuan River then flows into Lake Timiskaming where the water eventually enters the Ottawa River. Geology. The floodplain of Johnny Creek is in a low lying trend associated with the Link Lake Deformation Zone.

Geographic entities mentioned:
surface_form: Lake Timiskaming
instance_of: Lake
countries: Canada
coordinates: lat: 47.333333333333
lon: -79.5
After Johnny Creek flows into Net Lake, the water drains through Net Creek, entering Cassels Lake. It then enters Rabbit Lake, which is drained by the Matabitchuan River. The Matabitchuan River then flows into Lake Timiskaming where the water eventually enters the Ottawa River. Geology. The floodplain of Johnny Creek is in a low lying trend associated with the Link Lake Deformation Zone.

Geographic entities mentioned:
surface_form: rabbit lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.001
lon: -79.6385
Johnny Creek. Johnny Creek is one of many creeks running through the Temagami region of Northeastern Ontario, Canada. It is located about south of Temagami North in southeastern Strathy Township. The creek is entirely within the municipality of Temagami, flowing in a west–east direction. Course and hydrology.

Geographic entities mentioned:
surface_form: johnny creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.0867
lon: -79.7567
Course and hydrology. Johnny Creek flows east from the east end of Link Lake and runs under the Highway 11 Johnny Creek Bridge about to the east. It then flows adjacent to the Sherman Mine branch line for, eventually running under the Ontario Northland Railway main line where it flows another into Boot Bay of Net Lake. The total length of the creek is about and has an elevation of.

Geographic entities mentioned:
surface_form: johnny creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.0867
lon: -79.7567
surface_form: johnny creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.0867
lon: -79.7567
surface_form: link lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.0717
lon: -79.8178
The total length of the creek is about and has an elevation of. Johnny Creek is part of the Ottawa River drainage basin, a large area covering much of eastern Ontario and western Quebec where water drains into the Ottawa River. After Johnny Creek flows into Net Lake, the water drains through Net Creek, entering Cassels Lake. It then enters Rabbit Lake, which is drained by the Matabitchuan River.

Geographic entities mentioned:
surface_form: johnny creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.0867
lon: -79.7567
The Matabitchuan River then flows into Lake Timiskaming where the water eventually enters the Ottawa River. Geology. The floodplain of Johnny Creek is in a low lying trend associated with the Link Lake Deformation Zone. This zone of deformation is at least wide and over long, extending from Link Lake in the west to east of Highway 11.

Geographic entities mentioned:
surface_form: johnny creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.0867
lon: -79.7567
surface_form: link lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.0717
lon: -79.8178
This zone of deformation is at least wide and over long, extending from Link Lake in the west to east of Highway 11. Several small shear zones paralleling the Johnny Creek floodplain are probably related to the Link Lake Deformation Zone. A diorite dike, thought to have been associated with volcanic activity, is crosscut by these minor shear zones.

Geographic entities mentioned:
surface_form: johnny creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.0867
lon: -79.7567
surface_form: link lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.0717
lon: -79.8178
Geology. The floodplain of Johnny Creek is in a low lying trend associated with the Link Lake Deformation Zone. This zone of deformation is at least wide and over long, extending from Link Lake in the west to east of Highway 11. Several small shear zones paralleling the Johnny Creek floodplain are probably related to the Link Lake Deformation Zone.

Geographic entities mentioned:
surface_form: link lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.0717
lon: -79.8178
A diorite dike, thought to have been associated with volcanic activity, is crosscut by these minor shear zones. This indicates that the dike intruded into the surrounding country rock at least prior to the latest reactivation of the Link Lake Deformation Zone. However, the amount of displacement along the deformation zone is unknown.

Geographic entities mentioned:
surface_form: link lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.0717
lon: -79.8178
The band earned a devoted local following through outdoor shows held at Carswell's family land at Lake James, sometimes drawing crowds of 700, which were Carswell described as often being shut-down by local police due to noise complaints. After recording a demo with producer Ely Bail, the band was signed to an eight-album and $1,000,000 record deal by Mercury Records in early 1991.

Geographic entities mentioned:
surface_form: Lake James
instance_of: Lake
countries: United States
coordinates: lat: 35.7478
lon: -81.8785
2009 in Azerbaijan. The following outlines notable events in the year 2009 in Azerbaijan. The Republic of Azerbaijan is the largest country in the Caucasus region, situated at the crossroads of Western Asia and Eastern Europe. It is bordered by the Caspian Sea to the east, Russia to the north, Georgia to the northwest, Armenia to the west, and Iran to the south.

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
Because the exotic species is suddenly introduced to a community, it does not have any established predators or prey. The exotic species then have a survival advantage over endemic organisms. One such example is the destruction of the endemic cichlid population in Lake Victoria via the introduction of the predatory Nile perch (&quot;Lates niloticus&quot;).

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Moel Cynghorion. is a mountain in Snowdonia, North Wales. It lies two miles north-west of Snowdon, and forms part of the Moel Eilio Horseshoe walk. The summit is situated on a wide plateau, marked by a pile of stones. The southern slopes are gentle, while the northern aspect is precipitous. The summit has close views of Clogwyn Du'r Arddu and Snowdon (Yr Wyddfa).

Geographic entities mentioned:
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
surface_form: moel eilio
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.096880555556
lon: -4.1595305555556
The summit is situated on a wide plateau, marked by a pile of stones. The southern slopes are gentle, while the northern aspect is precipitous. The summit has close views of Clogwyn Du'r Arddu and Snowdon (Yr Wyddfa). Views from the summit can extend as far as Holyhead in Anglesey to nearby towns and villages in Gwynedd such as Caernarfon, Llanrug and Llanberis.

Geographic entities mentioned:
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
surface_form: yr wyddfa
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
surface_form: wyddfa
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
Moel Cynghorion. is a mountain in Snowdonia, North Wales. It lies two miles north-west of Snowdon, and forms part of the Moel Eilio Horseshoe walk. The summit is situated on a wide plateau, marked by a pile of stones. The southern slopes are gentle, while the northern aspect is precipitous. The summit has close views of Clogwyn Du'r Arddu and Snowdon (Yr Wyddfa).

Geographic entities mentioned:
surface_form: moel cynghorion
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.085138888889
lon: -4.11265
In 2017, one example was a virtual reality and immersive set based on the movie &quot;Blade Runner 2049&quot;. In 2018, these examples included a Taco Bell &quot;Demolition Man&quot; themed pop-up restaurant in the Gaslamp and a Shake Shack &quot;Bob's Burgers&quot; themed pop-up restaurant in Mission Valley. However, there are some official offsite events that require a badge.

Geographic entities mentioned:
surface_form: Mission Valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
McLeod Nunataks. The McLeod Nunataks () are an isolated group of nunataks southeast of the Tula Mountains in Enderby Land, Antarctica. They were photographed in 1956 by Australian National Antarctic Research Expeditions (ANARE) aircraft, and were first visited in December 1958 by an ANARE dog-sledge party, with the position fixed by G.A. Knuckey.

Geographic entities mentioned:
surface_form: mcleod nunataks
instance_of: Mountain
coordinates: lat: -67.4833
lon: 52.7
Tibidabo. Tibidabo () is a hill overlooking Barcelona, Catalonia, Spain. At, it is the tallest hill in the Serra de Collserola. Rising sharply to the north-west, it has views over the city and the surrounding coastline. The summit of the hill is occupied by the Sagrat Cor church and adjacent Tibidabo Amusement Park. The Torre de Collserola telecommunications tower is a short walk away.

Geographic entities mentioned:
surface_form: Serra de Collserola
instance_of: Mountain
countries: Spain
coordinates: lat: 41.412222
lon: 2.073889
surface_form: collserola
instance_of: Mountain
countries: Spain
coordinates: lat: 41.412222
lon: 2.073889
Tibidabo. Tibidabo () is a hill overlooking Barcelona, Catalonia, Spain. At, it is the tallest hill in the Serra de Collserola. Rising sharply to the north-west, it has views over the city and the surrounding coastline. The summit of the hill is occupied by the Sagrat Cor church and adjacent Tibidabo Amusement Park. The Torre de Collserola telecommunications tower is a short walk away.

Geographic entities mentioned:
surface_form: tibidabo
instance_of: Mountain
countries: Spain
coordinates: lat: 41.4225
lon: 2.118611111111111
At, it is the tallest hill in the Serra de Collserola. Rising sharply to the north-west, it has views over the city and the surrounding coastline. The summit of the hill is occupied by the Sagrat Cor church and adjacent Tibidabo Amusement Park. The Torre de Collserola telecommunications tower is a short walk away. All three are prominently visible from most of the city of Barcelona.

Geographic entities mentioned:
surface_form: tibidabo
instance_of: Mountain
countries: Spain
coordinates: lat: 41.4225
lon: 2.118611111111111
It is topped by a sculpture of the Sacred Heart of Jesus by Josep Miret Llopart. Tibidabo can be reached by road or via the Tibidabo Funicular, which was the first of its kind in Spain, and by the Tramvia Blau. Funicular operations recommenced in June 2021 after modernisation, however the tramway remains out of service. Replacement bus TC2 connects Tibidabo with Avinguda de Tibidabo Metro station.

Geographic entities mentioned:
surface_form: tibidabo
instance_of: Mountain
countries: Spain
coordinates: lat: 41.4225
lon: 2.118611111111111
surface_form: tibidabo
instance_of: Mountain
countries: Spain
coordinates: lat: 41.4225
lon: 2.118611111111111
Funicular operations recommenced in June 2021 after modernisation, however the tramway remains out of service. Replacement bus TC2 connects Tibidabo with Avinguda de Tibidabo Metro station. The Transports Metropolitans de Barcelona minibus service 111 connects it to Vallvidrera village and the upper station of the Vallvidrera funicular. Origin of the name.

Geographic entities mentioned:
surface_form: tibidabo
instance_of: Mountain
countries: Spain
coordinates: lat: 41.4225
lon: 2.118611111111111
surface_form: tibidabo
instance_of: Mountain
countries: Spain
coordinates: lat: 41.4225
lon: 2.118611111111111
At, it is the tallest hill in the Serra de Collserola. Rising sharply to the north-west, it has views over the city and the surrounding coastline. The summit of the hill is occupied by the Sagrat Cor church and adjacent Tibidabo Amusement Park. The Torre de Collserola telecommunications tower is a short walk away. All three are prominently visible from most of the city of Barcelona.

Geographic entities mentioned:
surface_form: collserola
instance_of: Mountain
countries: Spain
coordinates: lat: 41.412222
lon: 2.073889
Although much of the land has been incorporated into the city, it is mostly rural. Given the size of the area, it is likely that more neighborhoods will develop within Rio Bravo. A major attraction to the area is the Kern River County Park, a large recreation area which includes: Hart Park, Kern County Soccer Park, California Living Museum (CALM), Lake Ming, and the Kern River Golf Course.

Geographic entities mentioned:
surface_form: Lake Ming
instance_of: Lake
countries: United States
coordinates: lat: 35.44
lon: -118.866
Indus Vallis. Indus Vallis is a vallis (valley) in the Arabia quadrangle of Mars, located at 19.3° North and 321.3° West. It is 307 km long and was named for the Indus River in Pakistan. The westernmost part of the valley is in the vicinity of Cassini Crater.

Geographic entities mentioned:
surface_form: indus vallis
instance_of: Valley
coordinates: lat: 18.95
lon: 38.88
Mount Tabor. Mount Tabor (;;), sometimes spelled Mount Thabor, is a large hill of biblical significance in the Lower Galilee, Israel, at the eastern end of the Jezreel Valley, west of the Sea of Galilee.

Geographic entities mentioned:
surface_form: Jezreel Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
surface_form: jezreel
instance_of: Mountain
countries: Israel
coordinates: lat: 32.557852777778
lon: 35.327952777778
surface_form: mount tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
surface_form: tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
surface_form: thabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
It was the namesake of Tabor Light in Christian theology, of the Czech sect of the Taborites, and of numerous other settlements and institutions. The Arabic form of the name is (,) or &quot;Mount Tur&quot; (, &quot;Jebel eṭ-Ṭūr&quot;). The name &quot;Jabal aṭ-Ṭūr&quot; is shared with Sinai and Mount Gerizim. Geography.

Geographic entities mentioned:
surface_form: Mount Gerizim
instance_of: Mountain
countries: State of Palestine
coordinates: lat: 32.199444444444
lon: 35.272777777778
It is part of the Israel National Trail. History. At the bottom of the mountain was an important road junction: Via Maris passed there from the Jezreel Valley northward towards Damascus. Its location on the road junction and its bulgy formation above its environment gave Mount Tabor a strategic value and wars were conducted in its area in different periods in history. Hebrew Bible.

Geographic entities mentioned:
surface_form: Jezreel Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
surface_form: jezreel
instance_of: Mountain
countries: Israel
coordinates: lat: 32.557852777778
lon: 35.327952777778
surface_form: jezreel
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
Ottoman period. In 1799, during the time of Napoleon Bonaparte's Syrian expedition, in the valley between Mount Tabor and the Hill of Moreh, the Battle of Mount Tabor was fought in which a French force of about 3,000 soldiers under the command of Napoleon and general Kléber won against an Ottoman force of about 35,000 soldiers.

Geographic entities mentioned:
surface_form: Moreh
instance_of: Mountain
countries: Israel
coordinates: lat: 32.615833333333
lon: 35.363611111111
surface_form: mount tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
surface_form: tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
Hebrew Bible. The mountain is mentioned for the first time in the Hebrew Bible, in, as border of three tribes: Zebulun, Issachar and Naphtali. The mountain's importance stems from its strategic control of the junction of the Galilee's north–south route with the east–west highway of the Jezreel Valley.

Geographic entities mentioned:
surface_form: jezreel
instance_of: Mountain
countries: Israel
coordinates: lat: 32.557852777778
lon: 35.327952777778
surface_form: jezreel valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
Geography. Mount Tabor is shaped almost like half a sphere, suddenly rising from rather flat surroundings and reaching a height of 575 metres (1,886 feet), thus dominating by a good 450 metres the town in the plain below, Kfar Tavor. At the top of the mountain are two Christian monasteries, one Catholic on the southeast side and one Greek Orthodox on the northeast side.

Geographic entities mentioned:
surface_form: tavor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
Etymology. The Hebrew name of the mountain, &quot;tabor&quot;, has long been connected with the name for &quot;navel&quot;, &quot;ṭabbur&quot;, but this is probably due to popular etymology. In the Greek Septuagint's translation of the Book of Jeremiah, the name Itabyrium (, &quot;Itabýrion&quot;) was used for Mount Tabor. Josephus used the same name in his Greek works.

Geographic entities mentioned:
surface_form: itabyrium
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
surface_form: mount tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
surface_form: tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
Mount Tabor. Mount Tabor (;;), sometimes spelled Mount Thabor, is a large hill of biblical significance in the Lower Galilee, Israel, at the eastern end of the Jezreel Valley, west of the Sea of Galilee.

Geographic entities mentioned:
surface_form: mount tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
surface_form: tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
In the Hebrew Bible (Joshua, Judges), Mount Tabor is the site of the battle of Mount Tabor between the Israelite army under the leadership of Barak and the army of the Canaanite king of Hazor, Jabin, commanded by Sisera. In Christian tradition, Mount Tabor is the site of the transfiguration of Jesus. Etymology.

Geographic entities mentioned:
surface_form: mount tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
surface_form: mount tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
surface_form: tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
surface_form: tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
In the Hebrew Bible (Joshua, Judges), Mount Tabor is the site of the battle of Mount Tabor between the Israelite army under the leadership of Barak and the army of the Canaanite king of Hazor, Jabin, commanded by Sisera. In Christian tradition, Mount Tabor is the site of the transfiguration of Jesus. Etymology.

Geographic entities mentioned:
surface_form: mount tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
surface_form: tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
It is part of the Israel National Trail. History. At the bottom of the mountain was an important road junction: Via Maris passed there from the Jezreel Valley northward towards Damascus. Its location on the road junction and its bulgy formation above its environment gave Mount Tabor a strategic value and wars were conducted in its area in different periods in history. Hebrew Bible.

Geographic entities mentioned:
surface_form: mount tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
surface_form: tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
According to the Book of Judges, Hazor was the seat of Jabin, the king of Canaan, whose commander, Sisera, led a Canaanite army against the Israelites. Deborah the Jewish prophetess summoned Barak of the tribe of Naphtali and gave him God's command, &quot;Go and draw toward mount Tabor, and take with thee ten thousand men of the children of Naphtali and of the children of Zebulun&quot; (Judges).

Geographic entities mentioned:
surface_form: mount tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
surface_form: tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
Roman period. In 55 BCE, during a Hasmonean rebellion against the Roman proconsul of Syria, Aulus Gabinius, Alexander of Judaea and his army of 30,000 Judeans was defeated in battle at Mount Tabor. As many as 10,000 Jewish fighters were killed in the battle and Alexander was forced to flee, apparently to Syria.

Geographic entities mentioned:
surface_form: mount tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
surface_form: tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
Church of the Transfiguration. Between 1919 and 1924 a Catholic church of the Franciscan order named &quot;Church of the Transfiguration&quot; was built on the peak of Mount Tabor. The architect who designed the church was Antonio Barluzzi. The church was built upon the ruins of a Byzantine church from the fifth or sixth century and a Crusader church from the 12th century.

Geographic entities mentioned:
surface_form: mount tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
surface_form: tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
Etymology. The Hebrew name of the mountain, &quot;tabor&quot;, has long been connected with the name for &quot;navel&quot;, &quot;ṭabbur&quot;, but this is probably due to popular etymology. In the Greek Septuagint's translation of the Book of Jeremiah, the name Itabyrium (, &quot;Itabýrion&quot;) was used for Mount Tabor. Josephus used the same name in his Greek works.

Geographic entities mentioned:
surface_form: tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
Up to 400 plant species have been found on the Mount including large yellow crocuses (&quot;Sternbergia clusiana&quot;), the Persian lily (&quot;Fritillaria persica&quot;) rain-bells flowers (&quot;Muscari parviflorum&quot;), black-eyed red tulips (&quot;Tulipa agenensis&quot;), orchids, irises (including &quot;Iris haynei&quot;) and yellow asphodel (&quot;Asphodeline Lutea&quot;), spontaneous barley (&quot;Hordeum spontaneum&quot;), Mt.

Geographic entities mentioned:
surface_form: tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
July 1954. July 13, 1954 (Tuesday). The 1954 Lake of Two Mountains boating accident led to the drowning deaths of twelve children in Lake of Two Mountains, Montreal, Quebec.

Geographic entities mentioned:
surface_form: Lake of Two Mountains
instance_of: Lake
countries: Canada
coordinates: lat: 45.45
lon: -74.016666666667
Kisdon. Kisdon, also called Kisdon Hill, is a fell situated in upper Swaledale in the Yorkshire Dales National Park in North Yorkshire, England. Geography and history. Kisdon was named by early Norse settlers. Kisdon Farm is on the southern slopes above Straw Beck. The fell is unusual in that it is an isolated area of high ground with no ridges connecting it to other fells.

Geographic entities mentioned:
surface_form: Swaledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.361
lon: -1.838
surface_form: kisdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.393569444444
lon: -2.1585888888889
surface_form: kisdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.393569444444
lon: -2.1585888888889
The grass- and heather-covered summit gives a good all-round view, with the bulk of Rogan's Seat including the great gash of Swinner Gill dominating to the east while Great Shunner Fell and Lovely Seat, with the Buttertubs Pass in between, show well to the south-west.

Geographic entities mentioned:
surface_form: Rogan's Seat
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.422939
lon: -2.125914
surface_form: Great Shunner Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.3701
lon: -2.23546
surface_form: Lovely Seat
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.350388888889
lon: -2.1892
Kisdon. Kisdon, also called Kisdon Hill, is a fell situated in upper Swaledale in the Yorkshire Dales National Park in North Yorkshire, England. Geography and history. Kisdon was named by early Norse settlers. Kisdon Farm is on the southern slopes above Straw Beck. The fell is unusual in that it is an isolated area of high ground with no ridges connecting it to other fells.

Geographic entities mentioned:
surface_form: kisdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.393569444444
lon: -2.1585888888889
This came about at the end of the last ice age, when the moraine left by the retreating glacier blocked the original course of the River Swale on the west side of the fell and diverted it to its present course, forming a gorge to the east and leaving Kisdon isolated from other high ground.

Geographic entities mentioned:
surface_form: kisdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.393569444444
lon: -2.1585888888889
Kisdon's isolation gives it the status of a Marilyn, even though it has only a modest height of 499 metres (1636 feet). Another unusual feature of Kisdon is that it has no official footpath to the highest point, despite being crossed by two busy rights of way high up on the fell.

Geographic entities mentioned:
surface_form: kisdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.393569444444
lon: -2.1585888888889
Kisdon lies within a band of Yoredale limestone. It is on Kisdon that the band attains its maximum thickness of 40 metres. Ascent and summit. The fell is crossed by many high wire-topped dry-stone walls, which can make attaining the highest point of the fell awkward.

Geographic entities mentioned:
surface_form: kisdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.393569444444
lon: -2.1585888888889
To conclude the day walkers can descend eastwards to the Pennine Way and see the impressive waterfalls around Keld, namely Kisdon Force, East Gill Force, Catrake Force and Wain Wath Force. Scar Closes, Kisdon Side SSSI. The western side of Kisdon has been designated as a Site of Special Scientific Interest (SSSI) over an area of 3.7 hectares since 1988.

Geographic entities mentioned:
surface_form: kisdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.393569444444
lon: -2.1585888888889
Scar Closes, Kisdon Side SSSI. The western side of Kisdon has been designated as a Site of Special Scientific Interest (SSSI) over an area of 3.7 hectares since 1988. The SSSI takes the form of four grazed enclosures with the combination of Calcareous grassland growing on limestone rock supporting exceptional and varied botanical species.

Geographic entities mentioned:
surface_form: kisdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.393569444444
lon: -2.1585888888889
Puka Qallpa (Quechua &quot;puka&quot; red, &quot;qallpa&quot; terrain after the harvest, also spelled &quot;Puca Khallpa&quot;) is a mountain in the Bolivian Andes. It is located in the Cochabamba Department, Mizque Province, Alalay Municipality. It lies in the northwest of Kachi Q'asa and northeast of Inka Pirqa. The Puka Urqu Mayu (&quot;red mountain river&quot;) flows along its western slope.

Geographic entities mentioned:
surface_form: inka
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.4822
lon: -67.8303
surface_form: inka pirqa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.79027778
lon: -65.70722222
Puka Qallpa. Puka Qallpa (Quechua &quot;puka&quot; red, &quot;qallpa&quot; terrain after the harvest, also spelled &quot;Puca Khallpa&quot;) is a mountain in the Bolivian Andes. It is located in the Cochabamba Department, Mizque Province, Alalay Municipality. It lies in the northwest of Kachi Q'asa and northeast of Inka Pirqa.

Geographic entities mentioned:
surface_form: puka qallpa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.75638889
lon: -65.70166667
KLUJ-TV. KLUJ-TV (channel 44) is a religious television station licensed to Harlingen, Texas, United States, serving the Lower Rio Grande Valley. It is owned and operated by the Trinity Broadcasting Network through its Community Educational Television subsidiary, which manages stations in Texas and Florida on channels allocated for non-commercial educational broadcasting.

Geographic entities mentioned:
surface_form: Lower Rio Grande Valley
instance_of: Valley
countries: United States
Mexico
coordinates: lat: 26.22
lon: -98.12
To the west are First and Second Boulder Canyons, to the south is Pole Canyon and Secret Pass, and to the east is the South Fork of Steele Creek and Clover Valley. The summit is the end of a high crest running almost to the north, and the beginning of a slow descent to Ruby Valley to the southeast.

Geographic entities mentioned:
surface_form: Ruby Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.4
lon: -115.3
Humboldt Peak (Nevada). Humboldt Peak is the southernmost high summit in the East Humboldt Range of Elko County in northeastern Nevada. To the west are First and Second Boulder Canyons, to the south is Pole Canyon and Secret Pass, and to the east is the South Fork of Steele Creek and Clover Valley.

Geographic entities mentioned:
surface_form: humboldt peak (nevada)
instance_of: Mountain
countries: United States
coordinates: lat: 40.9013
lon: -115.12
Humboldt Peak (Nevada). Humboldt Peak is the southernmost high summit in the East Humboldt Range of Elko County in northeastern Nevada. To the west are First and Second Boulder Canyons, to the south is Pole Canyon and Secret Pass, and to the east is the South Fork of Steele Creek and Clover Valley.

Geographic entities mentioned:
surface_form: humboldt peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.9013
lon: -115.12
It is located in the Arequipa Region, Castilla Province, Chachas District. Ticlla lies southwest of Chila and Chila Pillune at a valley named Puncuhuaico (possibly from Quechua for &quot;p'unqu&quot; pond, dam, &quot;wayq'u&quot; valley or stream). Its intermittent stream flows to Chachas Lake.

Geographic entities mentioned:
surface_form: Chila Pillune
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4072
lon: -72.1878
surface_form: pillune
instance_of: Mountain
countries: Peru
coordinates: lat: -15.0756
lon: -72.0747
surface_form: ticlla
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4075
lon: -71.6114
It is located in the Arequipa Region, Castilla Province, Chachas District. Ticlla lies southwest of Chila and Chila Pillune at a valley named Puncuhuaico (possibly from Quechua for &quot;p'unqu&quot; pond, dam, &quot;wayq'u&quot; valley or stream). Its intermittent stream flows to Chachas Lake.

Geographic entities mentioned:
surface_form: Chachas Lake
instance_of: Lake
countries: Peru
coordinates: lat: -15.52111111
lon: -72.26
Ticlla (Castilla). Ticlla (possibly from Quechua for eyelash; two-colored, or for 'with alternating colors') is a mountain in the Chila mountain range in the Andes of Peru. It is located in the Arequipa Region, Castilla Province, Chachas District.

Geographic entities mentioned:
surface_form: ticlla
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4075
lon: -71.6114
surface_form: ticlla (castilla)
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4122
lon: -72.2089
Ticlla (Castilla). Ticlla (possibly from Quechua for eyelash; two-colored, or for 'with alternating colors') is a mountain in the Chila mountain range in the Andes of Peru. It is located in the Arequipa Region, Castilla Province, Chachas District.

Geographic entities mentioned:
surface_form: ticlla
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4075
lon: -71.6114
Swimming is not permitted. Boats used in the lake may not be used in any other body of water, to prevent the spread of zebra mussels. This raised some local concern in 2005, since many were left on shore during the offseason and the town of Carmel found them unsightly as it prepared to spend $2.3 million to spruce up the hamlet.

Geographic entities mentioned:
surface_form: lake may
instance_of: Lake
countries: United States
coordinates: lat: 47.09055556
lon: -94.59333333
There are no inlet brooks. A dam and spillway are located on its northwest end, with outflow draining into the New York City water supply system's West Branch Reservoir, where it joins with waters from the Delaware Aqueduct. Water in excess of New York City's needs there goes over its spillway and into the West Branch Croton River, which is captured downstream by the Croton Falls Reservoir.

Geographic entities mentioned:
surface_form: west branch
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
A dam and spillway are located on its northwest end, with outflow draining into the New York City water supply system's West Branch Reservoir, where it joins with waters from the Delaware Aqueduct. Water in excess of New York City's needs there goes over its spillway and into the West Branch Croton River, which is captured downstream by the Croton Falls Reservoir. History.

Geographic entities mentioned:
surface_form: west branch
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
Lake Gleneida. Lake Gleneida is a controlled lake in the hamlet of Carmel within the Town of Carmel in central Putnam County, New York. Originally a smaller natural water body, Shaw's Pond, it was dammed by New York City in 1870 and enlarged to for inclusion in its water supply system. It is part of the New York City water system's Croton Watershed. Geography.

Geographic entities mentioned:
surface_form: lake gleneida
instance_of: Lake
countries: United States
coordinates: lat: 41.42
lon: -73.683333333333
It quickly became a popular spot for boating and fishing. The name started appearing on maps around 1840. Not long after, residents became dissatisfied with the name and proposed grander names for it. In 1852, a committee of local residents finally settled on Lake Gleneida. New York City bought rights to the lake around 1895 and tore down what houses were built near it. Recreation.

Geographic entities mentioned:
surface_form: lake gleneida
instance_of: Lake
countries: United States
coordinates: lat: 41.42
lon: -73.683333333333
New York City bought rights to the lake around 1895 and tore down what houses were built near it. Recreation. The New York City Department of Environmental Protection (DEP) owns Lake Gleneida, considered one of three controlled lakes in the city's water system. This allows DEP to withdraw water as a right of ownership. Recreational use of the lake falls under DEP regulations.

Geographic entities mentioned:
surface_form: lake gleneida
instance_of: Lake
countries: United States
coordinates: lat: 41.42
lon: -73.683333333333
Grimface Mountain. Grimface Mountain is a mountain summit in British Columbia, Canada. Description. Grimface Mountain, elevation 2,635-metres (8,645-feet), is the highest point in Cathedral Provincial Park and Protected Area, as well as the highest point in the Similkameen Division Yale Land District, and the fourth-highest in the Okanogan Range which is a subrange of the North Cascades.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: grimface mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.03304
lon: -120.18573
Grimface Mountain. Grimface Mountain is a mountain summit in British Columbia, Canada. Description. Grimface Mountain, elevation 2,635-metres (8,645-feet), is the highest point in Cathedral Provincial Park and Protected Area, as well as the highest point in the Similkameen Division Yale Land District, and the fourth-highest in the Okanogan Range which is a subrange of the North Cascades.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: grimface mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.03304
lon: -120.18573
Description. Grimface Mountain, elevation 2,635-metres (8,645-feet), is the highest point in Cathedral Provincial Park and Protected Area, as well as the highest point in the Similkameen Division Yale Land District, and the fourth-highest in the Okanogan Range which is a subrange of the North Cascades. It is situated north of the Canada–United States border.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: grimface mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.03304
lon: -120.18573
It is situated north of the Canada–United States border. Precipitation runoff from the mountain's slopes drains into headwaters of Wall and Lakeview creeks which are both tributaries of the Ashnola River. Topographic relief is significant as the summit rises 735 metres (2,411 feet) above Wall Creek in two kilometres (1.2 mile).

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Precipitation runoff from the mountain's slopes drains into headwaters of Wall and Lakeview creeks which are both tributaries of the Ashnola River. Topographic relief is significant as the summit rises 735 metres (2,411 feet) above Wall Creek in two kilometres (1.2 mile). The mountain's toponym was officially adopted on September 24, 1979, by the Geographical Names Board of Canada. Climate.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Bald Hill (Oregon). Bald Hill is a hill in the Willamette Valley west of Corvallis, Oregon. With an elevation of and a top clear of tree cover, Bald Hill is a popular local hiking destination and lookout, with Corvallis, Mary's Peak, the Coastal Range, and the Cascade Range foothills all visible from atop the hill.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Geography. Bald Hill is located at the western edge of the Willamette Valley, where it meets the Oregon Coast Range. South of the Cardwell Hills, Bald Hill is separated from the foothills of the Coastal Range by Oak Creek and Mulkey Creek. History. The Bald Hill Natural Area was purchased by the Greenbelt Land Trust in 1990 and turned over to the City of Corvallis in 1993.

Geographic entities mentioned:
surface_form: Cardwell Hills
instance_of: Landform
countries: United States
coordinates: lat: 44.6429
lon: -123.373
Dog Bone Lake (Nevada). Dog Bone Lake is a dog bone-shaped topographic flat with two larger ends connected by a narrow body, which are two of the three eponymic features of their namesake, the Three Lakes Valley, Nevada.

Geographic entities mentioned:
surface_form: dog bone lake
instance_of: Lake
countries: United States
coordinates: lat: 36.71611111111111
lon: -115.448
From October 1935 on, he continued to do photographic work for the RA and later the Farm Security Administration (FSA), primarily in the Southern United States. In November 1935, he visited the industrial hub of the Lehigh Valley in eastern Pennsylvania, capturing photos of Bethlehem Steel. His photograph, &quot;Bethlehem Graveyard and Steel Mill&quot;, which captured Bethlehem's St.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
11133 Kumotori. 11133 Kumotori (provisional designation) is a background asteroid from the central regions of the asteroid belt, approximately in diameter. It was discovered on 2 December 1996, by Japanese amateur astronomer Takao Kobayashi at his Ōizumi Observatory. The asteroid was named after Mount Kumotori near Tokyo. It has a rotation period of 4.6 hours. Orbit and classification.

Geographic entities mentioned:
surface_form: Mount Kumotori
instance_of: Mountain
countries: Japan
coordinates: lat: 35.855277777778
lon: 138.94361111111
Naming. This minor planet was named after Mount Kumotori (雲取山 Kumotori-san). With an altitude of, it is the highest peak in the Tokyo metropolitan area, located at the boundary between Tokyo and Saitama and considered to be one of the 100 most celebrated mountains of Japan. The official naming citation was published by the Minor Planet Center on 9 November 2003 ().

Geographic entities mentioned:
surface_form: Mount Kumotori
instance_of: Mountain
countries: Japan
coordinates: lat: 35.855277777778
lon: 138.94361111111
Sirbaz Khan. Sirbaz Khan (born 1986.12.03) is a Pakistani mountaineer. He is the first Pakistani to summit all 14 eighth-thousander peaks in the world. Early life. Sirbaz was born in Aliabad, Hunza Valley in 1987. His father was a carpenter and his first expedition was as an assistant cook for the base camp of K2 when he was in 9th grade. Career.

Geographic entities mentioned:
surface_form: Hunza Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.31666667
lon: 74.65
Early life. Sirbaz was born in Aliabad, Hunza Valley in 1987. His father was a carpenter and his first expedition was as an assistant cook for the base camp of K2 when he was in 9th grade. Career. He initially started his climbing career working as a porter for foreign climbers but in 2016 he was sponsored by the Nepalese climber Mingma Sherpa for an expedition to climb K2.

Geographic entities mentioned:
surface_form: K2
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
Career. He initially started his climbing career working as a porter for foreign climbers but in 2016 he was sponsored by the Nepalese climber Mingma Sherpa for an expedition to climb K2. Although the duo failed in their attempt but in October 2017 Sirbaz successfully summited Nanga Parbat becoming the first to climb the mountain in autumn season.

Geographic entities mentioned:
surface_form: Nanga Parbat
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.239166666667
lon: 74.59
Although the duo failed in their attempt but in October 2017 Sirbaz successfully summited Nanga Parbat becoming the first to climb the mountain in autumn season. In July 2018, Sirbaz climbed the tall K2 — the second-tallest mountain in the world.

Geographic entities mentioned:
surface_form: K2
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333