Sarmila/GeoWiki-Features huggingface dataset:
Students are able to embark on mountaineering expeditions to the summits of Mount Kilimanjaro, Mount Meru, and Mount Hanang, as well as beach cleanup, deep sea diving, and coral reef restoration on the Indian Ocean coast near the town of Pangani, where the school runs a Field Study Center. Hiking, camping, and mountain biking in the surrounding countryside are also offered.

Geographic entities mentioned:
surface_form: Mount Hanang
instance_of: Mountain
countries: Tanzania
coordinates: lat: -4.435
lon: 35.4
The area around Sligo town has one of the highest densities of prehistoric archaeological sites in Ireland, and is the only place in which all classes of Irish megalithic monuments are to be found together. Knocknarea mountain, capped by the great cairn of Miosgan Maeve, dominates the skyline to the west of the town.

Geographic entities mentioned:
surface_form: Knocknarea
instance_of: Mountain
countries: Ireland
coordinates: lat: 54.25891
lon: -8.57463
Geography. Situated on a coastal plain facing the Atlantic Ocean, Sligo is located on low gravel hills on the banks of the Garavogue River between Lough Gill and the estuary of the Garavogue river leading to Sligo Bay. The town is surrounded on three sides by an arc of mountains, with the Ox Mountain ridges of Slieve Daeane and Killery Mountain to the southeast bordering Lough Gill.

Geographic entities mentioned:
surface_form: Lough Gill
instance_of: Lake
countries: Ireland
coordinates: lat: 54.2542
lon: -8.38362
The flat topped limestone plateaux of Cope's, Keelogyboy and Castlegal Mountains to the north and northeast and the singular hill of Knocknarea with its Neolithic cairn to the west and the distinctive high plateau of Benbulben to the north. Sligo is an important bridging point on the main north–south route between Ulster and Connacht.

Geographic entities mentioned:
surface_form: Knocknarea
instance_of: Mountain
countries: Ireland
coordinates: lat: 54.25891
lon: -8.57463
On average, the driest months are April to June while the wettest months are October to January. Rainfall averages 1303 mm (51.3 in) per year. The high rainfall means Sligo is in the temperate rainforest biome, examples of which exist around Lough Gill. The lowest temperature ever recorded in Ireland was −19.1 °C (−2.4 °F) at Markree Castle, County Sligo, on 16 January 1881. Demographics.

Geographic entities mentioned:
surface_form: Lough Gill
instance_of: Lake
countries: Ireland
coordinates: lat: 54.2542
lon: -8.38362
He was killed for a satire he wrote on the O'Haras. The annals record the death in 1561 of Naisse mac Cithruadh, the &quot;most eminent musician that was in Éireann&quot;, by drowning on Lough Gill. In the 17th century, two brothers from County Sligo, Thomas and William Connellan from Cloonamahon, were among the last of the great Irish bards and harpists.

Geographic entities mentioned:
surface_form: Lough Gill
instance_of: Lake
countries: Ireland
coordinates: lat: 54.2542
lon: -8.38362
states of Pennsylvania and Ohio. The line runs from Derby, New York southwest along the shore of Lake Erie to Cleveland, Ohio, along the former New York Central Railroad main line. At its east end (east of downtown Buffalo), the Erie West Subdivision becomes the Buffalo Terminal Subdivision; at its west end (east of downtown Cleveland), it becomes the Cleveland Terminal Subdivision.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
This region has been occupied for at least 11,500 years. Members of the Sahaptin language group, the Nimíipuu were the dominant people of the Columbia Plateau for much of that time, especially after acquiring the horses that led them to breed the Appaloosa horse in the 18th century.

Geographic entities mentioned:
surface_form: Columbia Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 45.999444444444
lon: -119.00138888889
It is the seat of Calamarca Municipality, the fourth municipal section of Aroma Province. It lies on the Altiplano on the east side of the main road between La Paz and Patacamaya, about 60 km south of La Paz. Calamarca has a late 16th-century church with a silver altar worked in a rococo style, and two rococo altar pieces.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Florida Heartland. The Florida Heartland (also known as South Central Florida) is a region of Florida located to the north and west of Lake Okeechobee, composed of six inland, predominantly rural counties—DeSoto, Glades, Hardee, Hendry, Highlands, and Okeechobee. In 2020, The US Census Bureau recorded the population of the Florida Heartland region at 251,927.

Geographic entities mentioned:
surface_form: Lake Okeechobee
instance_of: Lake
countries: United States
coordinates: lat: 26.933333333333
lon: -80.8
Many seasonal residents (sometimes referred to as &quot;snowbirds&quot;) live in the area during the winter months only, as temperatures in south Florida stay very moderate during that time of year. Lake Okeechobee and Lake Istokpoga in Highlands County attract fishers to the area. Area codes. Area code 863 is used throughout the region. Newspapers.

Geographic entities mentioned:
surface_form: Lake Istokpoga
instance_of: Lake
countries: United States
coordinates: lat: 27.366666666667
lon: -81.283333333333
After capturing various provincial forts, the prince compelled the ruler, Muhammad Shah, to submit. In 1397, he was named governor of the eastern province of Ferghana. With the idea of an eventual campaign against China in mind, Timur ordered his grandson to consolidate bases in the region, as well as develop soil cultivation along the route.

Geographic entities mentioned:
surface_form: Ferghana
instance_of: Valley
countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
lon: 71.757777777778
In 1397, he was named governor of the eastern province of Ferghana. With the idea of an eventual campaign against China in mind, Timur ordered his grandson to consolidate bases in the region, as well as develop soil cultivation along the route. Muhammad Sultan was given an army of forty thousand and had a fort built in the region of Ashapara, followed by another further east by the Issyk-Kul.

Geographic entities mentioned:
surface_form: Issyk-Kul
instance_of: Lake
countries: Kyrgyzstan
coordinates: lat: 42.416666666667
lon: 77.25
Fort Saint Pierre. Fort Saint Pierre on Rainy Lake was the first French fort built west of Lake Superior. It was the first of eight forts built during the elder Vérendrye's expansion of trade and exploration westward from the Great Lakes. History. In 1688 Jacques de Noyon, the first European to reach the area, built a temporary post or camp possibly at the same location.

Geographic entities mentioned:
surface_form: Rainy Lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 48.636944444444
lon: -93.031388888889
La Jemeraye reached Rainy Lake before the freezeup and built a fort at its outlet. Next May he sent a small load of furs back eastward, Vérendrye arrived in July, and pushed west to Lake of the Woods where he built Fort Saint Charles which quickly overshadowed Fort St. Pierre.

Geographic entities mentioned:
surface_form: Lake of the Woods
instance_of: Lake
countries: Canada
United States
coordinates: lat: 49.09027777777778
lon: -95.2388888888889
Saint-Maurice-de-Rotherens is a former commune in the Savoie department in the Auvergne-Rhône-Alpes region in south-eastern France. On 1 January 2019, it was merged into the new commune Saint-Genix-les-Villages. In 2022, it had 225 residents. Geography. The commune is located on the ridge of Mont Tournier. Saint-Maurice-de-Rotherens is located from Gresin and from Gerbaix.

Geographic entities mentioned:
surface_form: Mont Tournier
instance_of: Mountain
countries: France
coordinates: lat: 45.64
lon: 5.70527778
Avalanche boulder tongue. An avalanche boulder tongue is an accumulation of debris produced by snow avalanches. Well-developed avalanche boulder tongues usually develop below avalanche gullies due to successive avalanches over a long time span. The avalanche boulder tongues were first intensively investigated by Anders Rapp in the areas of Abisko and Kebnekaise in Swedish Lappland.

Geographic entities mentioned:
surface_form: Kebnekaise
instance_of: Mountain
countries: Sweden
coordinates: lat: 67.883333333333
lon: 18.55
Ashuluk. Ashuluk () is a rural locality (a settlement) near the Caspian Sea in Tambovsky Selsoviet, Kharabalinsky District, Astrakhan Oblast, Russia. The population was 1,678 as of 2010. There are 3 streets. Geography. Ashuluk is located 18 km southeast of Kharabali (the district's administrative centre) by road. Tambovka is the nearest rural locality.

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
Geography. The headwaters are in Mount Aspiring National Park, on the eastern flanks of the Southern Alps near Haast Pass, which is the saddle between the Makarora and Haast River valleys. The Makarora River flows south into the northern end of Lake Wānaka after passing the small community of Makarora. The river attracts some recreational fishing, jetboating and kayaking.

Geographic entities mentioned:
surface_form: Lake Wānaka
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.5
lon: 169.13333333333
All the water in the municipality is flowing water. The municipality is located in the agglomeration of Bern. Bolligen lies northeast of Bern, its area connects the Worblental to the Emmental. The &quot;Lutzere&quot; mountains form the watershed boundary between the Emme and the Aare rivers.

Geographic entities mentioned:
surface_form: Emmental
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.91922
lon: 7.77868
It consists of the village of Bolligen and the hamlets of Bantigen, Ferenberg, Flugbrunnen, Geristein and Habstetten. In the municipality is the Bantiger mountain (). The transmission tower of Swisscom located there supplies the surrounding region with radio and television programs. The mountain also provides a panorama of the Jura mountains, the Swiss plateau, and the Alps.

Geographic entities mentioned:
surface_form: Bantiger
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.979166666667
lon: 7.5291666666667
In the municipality is the Bantiger mountain (). The transmission tower of Swisscom located there supplies the surrounding region with radio and television programs. The mountain also provides a panorama of the Jura mountains, the Swiss plateau, and the Alps. On 31 December 2009 Amtsbezirk Bern, the municipality's former district, was dissolved.

Geographic entities mentioned:
surface_form: Swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
Barnacullian. Barnacullian is a mountain in County Wicklow, Ireland, located just north of Wicklow Mountains National Park. At 703 metres (2,306 ft) it is the 14th highest mountain in the Wicklow Mountains. An eroding peat bog on the mountain is the focus of a pilot conservation effort.

Geographic entities mentioned:
surface_form: barnacullian
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.084
lon: -6.397
He became provincial geologist to Canterbury, a post that he held from 1861 to 1868. His work in this capacity saw Haast conducting numerous expeditions throughout Canterbury and Westland, making geological discoveries and topographical maps of the area. Late in 1861, he discovered a coal seam in Kowai and the following year searched for gold in the area around Mount Cook.

Geographic entities mentioned:
surface_form: Mount Cook
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.595
lon: 170.14194444444445
Hong Kong. EIA in Hong Kong is regulated by the &quot;Environmental Impact Assessment Ordinance 1997&quot;, which became effective in 1998. The original proposal to construct the Lok Ma Chau Spur Line overground across the Long Valley failed to get through EIA, and the Kowloon–Canton Railway Corporation had to change its plan and build the railway underground.

Geographic entities mentioned:
surface_form: Long Valley
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 22.5091
lon: 114.114
Born the son of an Essen merchant, into a Protestant family of Italian origin (his ancestors came from Valtellina, from which they fled due to religious persecutions), together with his brother, Wilhelm he took over his father's enterprise and expanded the range of trade, becoming an influential businessman.

Geographic entities mentioned:
surface_form: Valtellina
instance_of: Valley
countries: Italy
coordinates: lat: 46.166666666667
lon: 9.8666666666667
He was fluent in Hebrew, English, Russian, German, and Arabic. Personal life. Ehud married Dora Rosenfeld and they had two daughters, Eliezra and Hemda (a professor of political science at Bar-Ilan University), and a son, Eliezer (a rabbi in the US). He died in November 1982 and was buried in the Ben-Yehuda family plot on the Mount of Olives in Jerusalem.

Geographic entities mentioned:
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
Soda Lakes. The Soda Lakes are two lakes located northwest of Fallon, Nevada. They occupy two basaltic maar volcano craters which may have erupted in the last 1,500 years. The larger lake, called Soda Lake or Big Soda Lake, is somewhat elongated, stretching in length. The smaller one, Little Soda Lake, is across.

Geographic entities mentioned:
surface_form: soda lake
instance_of: Lake
countries: United States
coordinates: lat: 46.963055555556
lon: -119.23833333333
surface_form: soda lake
instance_of: Lake
countries: United States
coordinates: lat: 46.963055555556
lon: -119.23833333333
surface_form: soda lake
instance_of: Group of lakes
countries: United States
coordinates: lat: 39.525
lon: -118.87805555556
surface_form: soda lake
instance_of: Group of lakes
countries: United States
coordinates: lat: 39.525
lon: -118.87805555556
They occupy two basaltic maar volcano craters which may have erupted in the last 1,500 years. The larger lake, called Soda Lake or Big Soda Lake, is somewhat elongated, stretching in length. The smaller one, Little Soda Lake, is across. Considered to be a single volcano, the combined craters are young enough that future activity cannot be ruled out.

Geographic entities mentioned:
surface_form: soda lake
instance_of: Lake
countries: United States
coordinates: lat: 46.963055555556
lon: -119.23833333333
surface_form: soda lake
instance_of: Group of lakes
countries: United States
coordinates: lat: 39.525
lon: -118.87805555556
Considered to be a single volcano, the combined craters are young enough that future activity cannot be ruled out. A geothermal power plant is located on the northeast flank of the volcano. A significant increase in level of Big Soda Lake occurred in the early 20th century due to increased groundwater table. It became a meromictic lake where the deeper water no longer mixes with surface waters.

Geographic entities mentioned:
surface_form: soda lake
instance_of: Lake
countries: United States
coordinates: lat: 46.963055555556
lon: -119.23833333333
surface_form: soda lake
instance_of: Group of lakes
countries: United States
coordinates: lat: 39.525
lon: -118.87805555556
It is monitored by the USGS California Volcano Observatory, which includes Nevada in its region. Geothermal plant. Exploration of the geothermal field in the Carson Desert near Soda Lakes began in the 1970s. The Soda Lake I & II geothermal energy plants came online in 1987 and 1991 respectively, with continuing development by multiple owners. 19th-century exploration.

Geographic entities mentioned:
surface_form: soda lake
instance_of: Lake
countries: United States
coordinates: lat: 46.963055555556
lon: -119.23833333333
surface_form: soda lake
instance_of: Group of lakes
countries: United States
coordinates: lat: 39.525
lon: -118.87805555556
19th-century exploration. A spring at Big Soda Lake provided the first drinkable water for 1800s wagon travelers on the Carson Trail at the end of the Forty Mile Desert, 2 miles before reaching the Carson River. The lakes are classified as soda lakes, hence the name. In 1875, two commercial facilities were built for extraction of soda from the lake, for use by the Nevada mining industry.

Geographic entities mentioned:
surface_form: soda lake
instance_of: Lake
countries: United States
coordinates: lat: 46.963055555556
lon: -119.23833333333
surface_form: soda lake
instance_of: Group of lakes
countries: United States
coordinates: lat: 39.525
lon: -118.87805555556
Additional water for irrigation was brought to Lahontan Reservoir from the Truckee River via a canal from Derby Dam. Rising groundwater increased the depth of Big Soda Lake by from to, bringing the commercial soda operations to an abrupt end by submerging the machinery. The facility was eventually under a depth of of water when the lake level stabilized in 1930. Meromictic lake.

Geographic entities mentioned:
surface_form: soda lake
instance_of: Lake
countries: United States
coordinates: lat: 46.963055555556
lon: -119.23833333333
surface_form: soda lake
instance_of: Group of lakes
countries: United States
coordinates: lat: 39.525
lon: -118.87805555556
The facility was eventually under a depth of of water when the lake level stabilized in 1930. Meromictic lake. Due to the rise in water level, Big Soda Lake became a meromictic lake. The denser lower layer is colder and more saline, and no longer mixes with the surface layer at any time of year. It is anoxic, or completely depleted of oxygen, below the chemocline boundary.

Geographic entities mentioned:
surface_form: soda lake
instance_of: Lake
countries: United States
coordinates: lat: 46.963055555556
lon: -119.23833333333
surface_form: soda lake
instance_of: Group of lakes
countries: United States
coordinates: lat: 39.525
lon: -118.87805555556
It is anoxic, or completely depleted of oxygen, below the chemocline boundary. A 1978 paper on &quot;Recent changes in the meromictic status of Big Soda Lake&quot; reported the depth of the chemocline was first detected in 1933 as at. It had fallen to at the time of the paper, leading to speculation that the lake would fully mix and cease to be meromictic within a few decades.

Geographic entities mentioned:
surface_form: soda lake
instance_of: Lake
countries: United States
coordinates: lat: 46.963055555556
lon: -119.23833333333
surface_form: soda lake
instance_of: Group of lakes
countries: United States
coordinates: lat: 39.525
lon: -118.87805555556
Compared to other usually-slower geological processes, the rate of growth of the tufa surprised observers. Roads. Nevada State Route 723 is a 2 mile long state highway on part of Soda Lake Road since 1978. Its southern terminus is at US Route 50, which passes about south of Little Soda Lake.

Geographic entities mentioned:
surface_form: soda lake
instance_of: Lake
countries: United States
coordinates: lat: 46.963055555556
lon: -119.23833333333
surface_form: soda lake
instance_of: Group of lakes
countries: United States
coordinates: lat: 39.525
lon: -118.87805555556
Soda Lakes. The Soda Lakes are two lakes located northwest of Fallon, Nevada. They occupy two basaltic maar volcano craters which may have erupted in the last 1,500 years. The larger lake, called Soda Lake or Big Soda Lake, is somewhat elongated, stretching in length. The smaller one, Little Soda Lake, is across.

Geographic entities mentioned:
surface_form: soda lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 39.525
lon: -118.87805555556
New tufa formations have served as a rare research example of tufa's rate of growth within a century. Geology. Maar volcanoes such as at Soda Lakes are formed by explosive eruptions when magma comes into contact with groundwater. The Lahontan Valley floor around Soda Lakes consists of ancient Lake Lahontan sediments.

Geographic entities mentioned:
surface_form: soda lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 39.525
lon: -118.87805555556
Geology. Maar volcanoes such as at Soda Lakes are formed by explosive eruptions when magma comes into contact with groundwater. The Lahontan Valley floor around Soda Lakes consists of ancient Lake Lahontan sediments. The Soda Lakes volcano's age is inferred as less than 6,000 years because it is younger than the lake sediments. Fault lines in the Carson Valley trend to the northeast.

Geographic entities mentioned:
surface_form: soda lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 39.525
lon: -118.87805555556
Fault lines in the Carson Valley trend to the northeast. Other older volcanoes nearby include the Upsal Hogback basalt cone 7 miles northeast and Rattlesnake Hill in Fallon. Volcano monitoring. Soda Lakes is the only volcano in Nevada currently listed on the USGS Volcano Hazards Program. It was added in 2018 with an initial assessment as a moderate threat potential.

Geographic entities mentioned:
surface_form: soda lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 39.525
lon: -118.87805555556
It is monitored by the USGS California Volcano Observatory, which includes Nevada in its region. Geothermal plant. Exploration of the geothermal field in the Carson Desert near Soda Lakes began in the 1970s. The Soda Lake I & II geothermal energy plants came online in 1987 and 1991 respectively, with continuing development by multiple owners. 19th-century exploration.

Geographic entities mentioned:
surface_form: soda lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 39.525
lon: -118.87805555556
19th-century exploration. A spring at Big Soda Lake provided the first drinkable water for 1800s wagon travelers on the Carson Trail at the end of the Forty Mile Desert, 2 miles before reaching the Carson River. The lakes are classified as soda lakes, hence the name. In 1875, two commercial facilities were built for extraction of soda from the lake, for use by the Nevada mining industry.

Geographic entities mentioned:
surface_form: soda lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 39.525
lon: -118.87805555556
The Lahontan Valley floor around Soda Lakes consists of ancient Lake Lahontan sediments. The Soda Lakes volcano's age is inferred as less than 6,000 years because it is younger than the lake sediments. Fault lines in the Carson Valley trend to the northeast. Other older volcanoes nearby include the Upsal Hogback basalt cone 7 miles northeast and Rattlesnake Hill in Fallon. Volcano monitoring.

Geographic entities mentioned:
surface_form: hogback
instance_of: Mountain
countries: United States
coordinates: lat: 42.706388888889
lon: -74.465
It also has a short coastline on the Gulf of Euboea. It bordered on Megaris (now West Attica) in the south, Attica in the southeast, Euboea in the northeast, Opuntian Locris (now part of Phthiotis) in the north and Phocis in the west. The main mountain ranges of Boeotia are Mount Parnassus in the west, Mount Helicon in the southwest, Cithaeron in the south and Parnitha in the east.

Geographic entities mentioned:
surface_form: Mount Parnassus
instance_of: Mountain
countries: Greece
coordinates: lat: 38.533
lon: 22.6167
surface_form: Mount Helicon
instance_of: Mountain
countries: Greece
coordinates: lat: 38.352222222222
lon: 22.825
The main mountain ranges of Boeotia are Mount Parnassus in the west, Mount Helicon in the southwest, Cithaeron in the south and Parnitha in the east. Its longest river, the Cephissus, flows in the central part, where most of the low-lying areas of Boeotia are found. Lake Copais was a large lake in the center of Boeotia. It was drained in the 19th century. Lake Yliki is a large lake near Thebes.

Geographic entities mentioned:
surface_form: Lake Copais
instance_of: Lake
countries: Greece
coordinates: lat: 38.45
lon: 23.05
Its longest river, the Cephissus, flows in the central part, where most of the low-lying areas of Boeotia are found. Lake Copais was a large lake in the center of Boeotia. It was drained in the 19th century. Lake Yliki is a large lake near Thebes. Origins. The origin of the name &quot;Boeotians&quot; may lie in the mountain Boeon in Epirus.

Geographic entities mentioned:
surface_form: Lake Yliki
instance_of: Lake
countries: Greece
coordinates: lat: 38.4
lon: 23.26666667
The advance eastward eventually proceeded both to the north and to the south of Copais lake. On the north side it ultimately reached Anthedon, a town credited with once having been occupied by the Thracians. On the south side it came as far as Thebes and Thespiae.

Geographic entities mentioned:
surface_form: Copais lake
instance_of: Lake
countries: Greece
coordinates: lat: 38.45
lon: 23.05
From the upper parking area (on the Massachusetts side), the trail is shorter, but goes more steeply down to the falls. Additionally, from the Massachusetts parking lot, a short trail leads up to a viewpoint from which one can se all the way across the Hudson Valley to the Catskill Mountains. Tourism and recreation.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Octherlony offered peace terms to the Nepalese demanding British suzerainty in the form of a British resident and the delimitation of Nepal's territories corresponding roughly to its present-day boundaries. The Nepalese refusal to accede to the terms led to another campaign the following year, targeting the Kathmandu Valley, after which the Nepalese capitulated. Geographic Context.

Geographic entities mentioned:
surface_form: Kathmandu Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
The canyon itself is one of the most dramatic in the Santa Ynez Mountains with the locally highest peak, La Cumbre Peak at the top of the watershed, flanked by Cathedral Peak and Arlington Peak to the west, &quot;Pine Lookout&quot; and &quot;Rock Garden&quot; to the east, and rugged sandstone formations partially covered with chaparral on both sides of the creek.

Geographic entities mentioned:
surface_form: La Cumbre Peak
instance_of: Mountain
countries: United States
coordinates: lat: 34.495
lon: -119.714
Douglas. Butler held that position for seven years. Oregon settler. In 1853, Butler decided to move his family west to the Oregon Territory. After selling his farm in Illinois, he was elected captain of a wagon train bound for Oregon. He led his company to Oregon's Willamette Valley. Butler settled in Polk County, where he filed a Donation Land Act claim for along the Luckiamute River.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
However, Peru wanted to mediate in the conflict instead of joining the war, and sent Special Mission headed Don José Antonio Lavalle to solve the crisis. On 18 February, in Chichilaya, on the shores of Lake Titicaca, Reyes Ortiz received a legalized copy of the Chilean ultimatum. In Puno, he took a train to Moliendo, hurrying to deliver the news to the government.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
Beardmore Glacier. The Beardmore Glacier in Antarctica is one of the largest valley glaciers in the world, being long and having a width of. It descends about from the Antarctic Plateau to the Ross Ice Shelf and is bordered by the Commonwealth Range of the Queen Maud Mountains on the eastern side and the Queen Alexandra Range of the Central Transantarctic Mountains on the western.

Geographic entities mentioned:
surface_form: Antarctic Plateau
instance_of: Plateau
coordinates: lat: -90
lon: 0
Wild Icefalls. The extensive icefalls at the head of Beardmore Glacier, between Mount Wild and Mount Buckley. Named by the New Zealand Geological Survey Antarctic Expedition (NZGSAE) (1961–62) in association with nearby Mount Wild. Left tributaries. Tributaries from the left (northwest, Queen Alexandra Range) from west to east include Table Bay and Swinford Glacier near the head.

Geographic entities mentioned:
surface_form: Mount Buckley
instance_of: Mountain
coordinates: lat: -84.96666667
lon: 163.93333333
In the lower section the left tributaries include Alice Glacier, Evans Glacier and Socks Glacier. Table Bay. A small glacier between Mount Augusta and Mount Holloway in the south part of Queen Alexandra Range draining eastward into Beardmore Glacier at Lizard Point. Evidently named by the Southern Polar Party of the BrAE (1910–13) because of its appearance.

Geographic entities mentioned:
surface_form: Mount Augusta
instance_of: Mountain
countries: United States
Canada
coordinates: lat: 60.305277777778
lon: -140.46027777778
surface_form: Mount Holloway
instance_of: Mountain
coordinates: lat: -84.75
lon: 163.6
Lizard Point. A low morainic point along the west side of upper Beardmore Glacier, marking the south side of the entrance to glacier-filled Table Bay. Swinford Glacier. A tributary glacier, long, flowing southeast between Mount Holloway and Marshall Mountains to enter Beardmore Glacier. Discovered by the BrAE (1907–09) and named by Shackleton for his eldest son, Raymond Swinford.

Geographic entities mentioned:
surface_form: Mount Holloway
instance_of: Mountain
coordinates: lat: -84.75
lon: 163.6
Moody, United States Navy, at McMurdo Station, winter 1963. Bingley Glacier. A glacier long in Queen Alexandra Range, draining south from the slopes of Mount Kirkpatrick, Mount Dickerson and Barnes Peak and entering Beardmore Glacier just north of Adams Mountains. Named by E.H. Shackleton (BrAE, 1907–09) after Bingley, England, the ancestral home of the Shackleton family. Cherry Icefall.

Geographic entities mentioned:
surface_form: Mount Kirkpatrick
instance_of: Mountain
coordinates: lat: -84.333333333333
lon: 166.41666666667
surface_form: Mount Dickerson
instance_of: Mountain
coordinates: lat: -84.333333333333
lon: 167.13333333333
surface_form: Barnes Peak
instance_of: Mountain
coordinates: lat: -84.3833
lon: 167.567
The name has been amended on the recommendation of the NZGSAE (1961–62) to be more descriptive of the feature. Not: Cherry Glacier. Hewson Glacier. A glacier in the Queen Alexandra Range, long, flowing northeast to enter Beardmore Glacier just north of The Cloudmaker. Named by the NZGSAE (1961–62) for Ronald Hewson, surveyor with the expedition. Garrard Glacier.

Geographic entities mentioned:
surface_form: The Cloudmaker
instance_of: Mountain
coordinates: lat: -84.2833
lon: 169.417
Garrard Glacier. A glacier in Queen Alexandra Range, draining eastward from the névé between Mount Lockwood and Mount Kirkpatrick and entering Beardmore Glacier south of Bell Bluff. It appears that BrAE (1910–13) applied the name &quot;Garrard Glacier&quot; to the feature which had been named Bingley Glacier by Shackleton in 1908.

Geographic entities mentioned:
surface_form: Mount Lockwood
instance_of: Mountain
coordinates: lat: -84.15
lon: 167.4
surface_form: Mount Kirkpatrick
instance_of: Mountain
coordinates: lat: -84.333333333333
lon: 166.41666666667
Discovered by the BrAE (1907–09) and named for Robert Calder Allen of the Franklin Relief Expedition to the Arctic. Lands End Nunataks. Two rock nunataks north-north-west of Airdrop Peak at the north end of Ebony Ridge. The nunataks lie at the E side of the terminus of Beardmore Glacier and mark the northern termination of the Commonwealth Range at Ross Ice Shelf.

Geographic entities mentioned:
surface_form: Airdrop Peak
instance_of: Mountain
coordinates: lat: -83.75
lon: 172.75
Inglis Falls. One of three waterfalls that surround the city of Owen Sound, Ontario, Canada, Inglis Falls is the largest and most impressive. It is also the most visited. Situated in the heart of the 200-hectare Inglis Falls Conservation Area, Inglis Falls is an cascade, created by the Sydenham River meeting the edge of the Niagara Escarpment. Swimming is prohibited in the entire area.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
The population was 108 at the 2020 census, slightly down from 109 in 2010. History. Iliamna was originally the name of an Athabaskan village at the point where the Iliamna River flows into Iliamna Lake, about east of present-day Iliamna. That site is now called Old Iliamna (Dena'ina: &quot;Nuch'ak'dalitnu’&quot;). In 1935, the residents of Old Iliamna moved to the present-day location.

Geographic entities mentioned:
surface_form: Iliamna Lake
instance_of: Lake
countries: United States
coordinates: lat: 59.536
lon: -155.024
Geography. Iliamna is located in southwest Alaska at (59.765135, -154.840312). It is bordered to the south by the city of Newhalen, to the west by the Newhalen River, and to the southeast by Iliamna Lake. According to the United States Census Bureau, the CDP has a total area of, of which are land and, or 1.23%, are water. Climate.

Geographic entities mentioned:
surface_form: Iliamna Lake
instance_of: Lake
countries: United States
coordinates: lat: 59.536
lon: -155.024
Potrero Chico. El Potrero Chico is an internationally renowned rock climbing, and big wall climbing, area in the Mexican state of Nuevo León, outside the town of Hidalgo, within Sierra del Fraile protected area. El Potrero Chico is a unique geological formation of limestone cliffs and spires, some as high as. Rock climbing.

Geographic entities mentioned:
surface_form: Sierra del Fraile
instance_of: Mountain
countries: Mexico
coordinates: lat: 25.89861
lon: -100.47639
Heavy rainfall brought by the hurricane caused landslides and flooding along the Harbourville Mountain which washed out numerous roads. In the Annapolis Valley, the rainfall fell so quickly that drainage ditches and small creeks overflowed. In Lakeville, flooding washed away a bridge, and fallen trees and other storm debris littered the streets and roads.

Geographic entities mentioned:
surface_form: Annapolis Valley
instance_of: Valley
countries: Canada
coordinates: lat: 44.979166666666664
lon: -64.89222222222222
She probably travelled to collect the flowers. They were mostly collected in the region around the Newcastle and Scottish Borders where she lived, but some were from North Wales and Upper Teesdale, while others came from Cirencester, Kent, Ireland and Devon. Comparisons of some of her records with later information has shown significant changes in land use.

Geographic entities mentioned:
surface_form: Teesdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.545
lon: -1.927
Neighboring districts are (from the southwest clockwise): Non Sa-at, Nong Saeng, Mueang Udon Thani, Prachaksinlapakhom, Ku Kaeo and Si That of Udon Thani Province; Tha Khantho of Kalasin province and Kranuan of Khon Kaen province. North of the central town is the shallow Nong Han Kumphawapi Lake. The lake is surrounded by marshland, one of the largest natural wetlands in northeast Thailand.

Geographic entities mentioned:
surface_form: Nong Han Kumphawapi Lake
instance_of: Lake
countries: Thailand
coordinates: lat: 17.166666666667
lon: 103.03333333333
Ambroz River. The Ambroz is a river for which Valle del Ambroz, an area in Spain north of Extremadura, near the border of Portugal, was named. The area is home to eight villages: Hervás, Baños de Montemayor, Abadía, Casas del Monte, La Garganta, Gargantilla, Aldeanueva del Camino and Segura de Toro. The total population of the area is about 8,000. The river is popular with tourists.

Geographic entities mentioned:
surface_form: ambroz
instance_of: Watercourse
countries: Spain
coordinates: lat: 40.16416667
lon: -6.15555556
Ambroz River. The Ambroz is a river for which Valle del Ambroz, an area in Spain north of Extremadura, near the border of Portugal, was named. The area is home to eight villages: Hervás, Baños de Montemayor, Abadía, Casas del Monte, La Garganta, Gargantilla, Aldeanueva del Camino and Segura de Toro. The total population of the area is about 8,000. The river is popular with tourists.

Geographic entities mentioned:
surface_form: ambroz
instance_of: Watercourse
countries: Spain
coordinates: lat: 40.16416667
lon: -6.15555556
surface_form: ambroz
instance_of: Watercourse
countries: Spain
coordinates: lat: 40.16416667
lon: -6.15555556
Ambroz River. The Ambroz is a river for which Valle del Ambroz, an area in Spain north of Extremadura, near the border of Portugal, was named. The area is home to eight villages: Hervás, Baños de Montemayor, Abadía, Casas del Monte, La Garganta, Gargantilla, Aldeanueva del Camino and Segura de Toro. The total population of the area is about 8,000. The river is popular with tourists.

Geographic entities mentioned:
surface_form: toro
instance_of: Mountain
countries: Spain
coordinates: lat: 39.985
lon: 4.11361111
Spåtind. Spåtind is a mountain in Innlandet county, Norway. The tall mountain is located on the border of Etnedal Municipality and Nordre Land Municipality about west of the town of Lillehammer and about northeast of the town of Fagernes. The mountain lies a few kilometers south of the border of Langsua National Park. Spåtind is the highest mountain in the mountain area known as Synnfjell.

Geographic entities mentioned:
surface_form: spåtind
instance_of: Mountain
countries: Norway
coordinates: lat: 61.076944444444
lon: 9.7894444444444
The mountain lies a few kilometers south of the border of Langsua National Park. Spåtind is the highest mountain in the mountain area known as Synnfjell. There are numerous cabins situated around the mountain, the largest cluster being Hugulia on the southern side. On the western side there is a facility for alpine skiing and a hotel. Name.

Geographic entities mentioned:
surface_form: spåtind
instance_of: Mountain
countries: Norway
coordinates: lat: 61.076944444444
lon: 9.7894444444444
Its approximate length is 185 km. It joins the Assiniboine River about west of Brandon. The watershed has an area of. The watershed includes numerous lakes and three man-made reservoirs (Minnedosa Lake, Rapid City Reservoir and Lake Wahtopanah. In 1911 the Geographic Board of Canada adopted the name Minnedosa River but restored the original name in 1978.

Geographic entities mentioned:
surface_form: Lake Wahtopanah
instance_of: Lake
countries: Canada
coordinates: lat: 50.0653
lon: -100.172
Past Tanauan Exit, STAR Tollway descends on a scenic curve before ascending on approach to Malvar. Entering Malvar, the road mostly passes rural areas, mostly containing large coconut plantations and small residential areas. Also, within Malvar, Mount Maculot can be seen on the west of the road and Mount Malarayat can be sighted on the east.

Geographic entities mentioned:
surface_form: Mount Maculot
instance_of: Mountain
countries: Philippines
coordinates: lat: 13.916666666667
lon: 121.05
Nonetheless, he had designated the same route as Almagro for his expedition—the Atacama Desert. Reaching the Copiapó Valley, he founded settlements which would later become major cities in Chile: Santiago del Nuevo Extremo (now known as Santiago de Chile, since the date of independence in 1810) in 1541 and La Serena in 1544.

Geographic entities mentioned:
surface_form: Copiapó Valley
instance_of: Valley
countries: Chile
South of Kleinburg, the highway dipped into the Humber River valley, connecting with Islington Avenue. North of the valley, it continued through King Township into the Oak Ridges Moraine, dividing the village of Nobleton and entering Schomberg immediately south of Highway 9, north of which the highway entered Simcoe County.

Geographic entities mentioned:
surface_form: Oak Ridges Moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
The Canary Islands are another notable Spanish producer of the fruit. Other minor cultivators include North America (in South Florida and the California Coachella Valley), Hawai'i, and Australia. Many commercial cultivars grown in Europe are grafted onto the cold-hardy rootstock of the &quot;Gomera-1&quot; mango cultivar, originally from Cuba.

Geographic entities mentioned:
surface_form: Coachella Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.72
lon: -116.2
The hilly area in the city of Semarang is known as the upper city (Semarang Dhuwur). This hilly region is also the upstream area of the big rivers that flow in the city of Semarang. The upper city area is also near Mount Ungaran. Climate. Semarang features a tropical monsoon climate (Köppen: &quot;Am&quot;).

Geographic entities mentioned:
surface_form: Mount Ungaran
instance_of: Mountain
countries: Indonesia
coordinates: lat: -7.18
lon: 110.33
The majority of Saint Peter's remains still reside in Rome, preserved under the high altar of St Peter's Basilica. Jerusalem ossuaries. In 1953, two Franciscan friar discovered hundreds of 1st century ossuaries stored in a cave on the Mount of Olives near Jerusalem.

Geographic entities mentioned:
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
There are also a few hundred speakers of this language in northern Jammu and Kashmir, India. In Pakistan, Burushaski is spoken by the people of the Hunza District, the Nagar District, the northern Gilgit District, the Yasin Valley in the Gupis-Yasin District, and the Ishkoman Valley of the northern Ghizer District. Their native region is northern Gilgit–Baltistan.

Geographic entities mentioned:
surface_form: Yasin
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.367777777777775
lon: 73.33777777777777
surface_form: Ishkoman
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.52972222222222
lon: 73.82944444444445
Varieties. Burushaski is spoken by about 120,000 speakers in Pakistan, and also by a few hundred in India. In Pakistan, it is spoken in three main valleys: Yasin, Hunza, and Nagar. The varieties of Hunza and Nagar diverge slightly, but are clearly dialects of a single language. The Yasin variety, also known by the Khowar exonym &quot;Werchikwar&quot;, is much more divergent.

Geographic entities mentioned:
surface_form: Yasin
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.367777777777775
lon: 73.33777777777777
surface_form: Hunza
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.31666667
lon: 74.65
surface_form: Nagar
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.4
lon: 73.8
Lakes of Killarney. The Lakes of Killarney are a scenic attraction located in Killarney National Park near Killarney, County Kerry, in Ireland. They consist of three lakes: Lough Leane, Muckross Lake (also called Middle Lake) and Upper Lake. Surroundings. The lakes sit in a low valley some above sea level. They are surrounded by the rugged slopes of MacGillycuddy's Reeks.

Geographic entities mentioned:
surface_form: Lough Leane
instance_of: Lake
countries: Ireland
coordinates: lat: 52.041666666667
lon: -9.55
surface_form: Upper Lake
instance_of: Lake
countries: Ireland
coordinates: lat: 51.98038
lon: -9.592089
surface_form: lough leane
instance_of: Group of lakes
countries: Ireland
coordinates: lat: 52.041666666667
lon: -9.55
They are surrounded by the rugged slopes of MacGillycuddy's Reeks. Notable mountains in the range include Carrauntoohil, which, at is Ireland's highest mountain, Purple Mountain, at, Mangerton Mountain, at, and Torc Mountain, at. The N71 road from Killarney to Kenmare passes a viewpoint called Ladies View which offers a view of the lakes and valleys.

Geographic entities mentioned:
surface_form: Carrauntoohil
instance_of: Mountain
countries: Ireland
coordinates: lat: 51.998888888889
lon: -9.7427777777778
surface_form: Mangerton Mountain
instance_of: Mountain
countries: Ireland
coordinates: lat: 51.970308333333
lon: -9.4843944444444
surface_form: Torc Mountain
instance_of: Mountain
countries: Ireland
coordinates: lat: 52
lon: -9.51667
surface_form: purple mountain
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.007916666667
lon: -9.6224805555556
The two are separated by a small peninsula, crossed by a stone arched bridge called Brickeen Bridge. It is Ireland's deepest lake, reaching to in parts. A paved hiking trail of approximately circles the lake. Upper Lake. The Upper Lake is the smallest of the three lakes, and the southernmost. It is separated from the others by a winding channel some long. Folklore.

Geographic entities mentioned:
surface_form: upper lake
instance_of: Lake
countries: Ireland
coordinates: lat: 51.98038
lon: -9.592089
Lakes of Killarney. The Lakes of Killarney are a scenic attraction located in Killarney National Park near Killarney, County Kerry, in Ireland. They consist of three lakes: Lough Leane, Muckross Lake (also called Middle Lake) and Upper Lake. Surroundings. The lakes sit in a low valley some above sea level. They are surrounded by the rugged slopes of MacGillycuddy's Reeks.

Geographic entities mentioned:
surface_form: lakes of killarney
instance_of: Group of lakes
countries: Ireland
coordinates: lat: 52.041666666667
lon: -9.55
The N71 road from Killarney to Kenmare passes a viewpoint called Ladies View which offers a view of the lakes and valleys. On the occasion of Queen Victoria's visit in 1861, the point was apparently chosen by the queen's ladies-in-waiting as the finest in the land; hence the name. Lough Leane. Lough Leane () is the largest and northernmost of the three lakes, approximately in size.

Geographic entities mentioned:
surface_form: lough leane
instance_of: Group of lakes
countries: Ireland
coordinates: lat: 52.041666666667
lon: -9.55
surface_form: lough leane
instance_of: Lake
countries: Ireland
coordinates: lat: 52.041666666667
lon: -9.55
On the occasion of Queen Victoria's visit in 1861, the point was apparently chosen by the queen's ladies-in-waiting as the finest in the land; hence the name. Lough Leane. Lough Leane () is the largest and northernmost of the three lakes, approximately in size. It is also the largest body of fresh water in the region.

Geographic entities mentioned:
surface_form: lough leane
instance_of: Group of lakes
countries: Ireland
coordinates: lat: 52.041666666667
lon: -9.55
surface_form: lough leane
instance_of: Lake
countries: Ireland
coordinates: lat: 52.041666666667
lon: -9.55
Lough Leane. Lough Leane () is the largest and northernmost of the three lakes, approximately in size. It is also the largest body of fresh water in the region. The River Laune drains Lough Leane to the north-west towards Killorglin and into Dingle Bay. Leane is dotted with small forested islands, including Innisfallen, which holds the remains of the ruined Innisfallen Abbey.

Geographic entities mentioned:
surface_form: lough leane
instance_of: Group of lakes
countries: Ireland
coordinates: lat: 52.041666666667
lon: -9.55
surface_form: lough leane
instance_of: Lake
countries: Ireland
coordinates: lat: 52.041666666667
lon: -9.55
Ross Castle, a 15th-century keep, sits on the eastern shore of the lake, north of the Ross Island peninsula. Muckross Lake. Also known as Middle Lake or Torc Lake, Muckross is just south of Lough Leane. The two are separated by a small peninsula, crossed by a stone arched bridge called Brickeen Bridge. It is Ireland's deepest lake, reaching to in parts.

Geographic entities mentioned:
surface_form: lough leane
instance_of: Group of lakes
countries: Ireland
coordinates: lat: 52.041666666667
lon: -9.55
surface_form: lough leane
instance_of: Lake
countries: Ireland
coordinates: lat: 52.041666666667
lon: -9.55
They are dominated by the Kleiner Müggelberg (88.3 m) and Großer Müggelberg (114.7 m). The &quot;Müggelberge&quot; cover an area of around seven square kilometres. The ridge was formed during the ice age. A viewing tower called the Müggelturm has been erected on the hills with a view of the Müggelsee and the Berlin-Müggelberge TV Tower.

Geographic entities mentioned:
surface_form: Müggelsee
instance_of: Lake
countries: Germany
coordinates: lat: 52.433333333333
lon: 13.65
surface_form: müggelberge
instance_of: Mountain
countries: Germany
coordinates: lat: 52.416111111111
lon: 13.633333333333
surface_form: müggelsee
instance_of: Lake
countries: Germany
coordinates: lat: 52.433333333333
lon: 13.65