Sarmila/GeoWiki-Features huggingface dataset:
Green Mountain) and Jelenia Góra (Eng. Deer Mountain). The top of the mountain is fairly flat but the slopes of the northeastern part are quite steep. District of Maślana Góra is a home to the nature reservoir called Jelenia Góra (pron. &quot;Yeahlenyah Goora&quot;), and Beskidzkie Morskie Oko (pron. Beskitskyeah Morskye Oko, meaning: Sea Eye), which is a landslide pond.

Geographic entities mentioned:
surface_form: maślana góra
instance_of: Mountain
countries: Poland
coordinates: lat: 49.6444
lon: 21.0583
Beskitskyeah Morskye Oko, meaning: Sea Eye), which is a landslide pond. The etymology of the Maślana Góra is probably associated with the tectonic instability, resulting multiple landslides in the past. The carphatian beech as well as &quot;Phyllitis scolopendrium&quot; are one of the rare plants, that are protected in this fragment of the ancient Carpathian forests. Tourism.

Geographic entities mentioned:
surface_form: maślana góra
instance_of: Mountain
countries: Poland
coordinates: lat: 49.6444
lon: 21.0583
The carphatian beech as well as &quot;Phyllitis scolopendrium&quot; are one of the rare plants, that are protected in this fragment of the ancient Carpathian forests. Tourism. There is a green trail leading from Stróże to Szymbark through Maślana Góra and Jelenia Góra Reservoir.

Geographic entities mentioned:
surface_form: maślana góra
instance_of: Mountain
countries: Poland
coordinates: lat: 49.6444
lon: 21.0583
Later biblical passages mention the fortunes of several of Eli's descendants. Eli occupies a prominent place in Samaritan religious tradition, as the Samaritans attribute the schism between their community and the Jews to Eli's establishment of a rival shrine at Shiloh, challenging what they regard as the original Israelite sacred site, Mount Gerizim. Biblical narrative.

Geographic entities mentioned:
surface_form: Mount Gerizim
instance_of: Mountain
countries: State of Palestine
coordinates: lat: 32.199444444444
lon: 35.272777777778
Rabbah died at age 40 and his nephew Abaye died at age 60. Samaritan sources. The Samaritans assert that Mount Gerizim was the original Holy Place of Israel from the time that Joshua conquered Israel and the ten tribes settled the land.

Geographic entities mentioned:
surface_form: Mount Gerizim
instance_of: Mountain
countries: State of Palestine
coordinates: lat: 32.199444444444
lon: 35.272777777778
According to the Bible, the story of Mount Gerizim takes us back to the story of the time when Moses ordered Joshua to take the Twelve Tribes of Israel to the mountains by Shechem and place half of the tribes, six in number, on the top of Mount Gerizim (Mount of the Blessing), and the other half in Mount Ebal (Mount of the Curse).

Geographic entities mentioned:
surface_form: Mount Ebal
instance_of: Mountain
countries: State of Palestine
coordinates: lat: 32.234
lon: 35.2733
The Fortress (Alberta). The Fortress () is a mountain located SE of Gusty Peak in the Kananaskis River Valley of Kananaskis Park of the Canadian Rockies. When viewed from Highway 40, the north face presents a fortress like appearance. The Fortress should not be confused with nearby Fortress Mountain.

Geographic entities mentioned:
surface_form: Gusty Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.83062
lon: -115.25879
surface_form: the fortress
instance_of: Mountain
countries: Canada
coordinates: lat: 50.827777777777776
lon: -115.24333333333334
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The mountain was originally named Tower Mountain but was changed in 1957 to its current name so as not to be confused with Tower Mountain. __NOTOC__
Climbing routes. The southwestern slopes can be scrambled from either the Chester Lake side or Headwall Lakes side. Both routes join at the Chester-Fortress col. From the col, a steep path ascends the remaining to the summit.

Geographic entities mentioned:
surface_form: Headwall Lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 50.8058
lon: -115.246
surface_form: chester lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.8117
lon: -115.275
__NOTOC__
Climbing routes. The southwestern slopes can be scrambled from either the Chester Lake side or Headwall Lakes side. Both routes join at the Chester-Fortress col. From the col, a steep path ascends the remaining to the summit. Only the final section of the summit block requires any real hands on scrambling.

Geographic entities mentioned:
surface_form: Chester
instance_of: Mountain
countries: Canada
coordinates: lat: 50.8067
lon: -115.263
The Fortress (Alberta). The Fortress () is a mountain located SE of Gusty Peak in the Kananaskis River Valley of Kananaskis Park of the Canadian Rockies. When viewed from Highway 40, the north face presents a fortress like appearance. The Fortress should not be confused with nearby Fortress Mountain.

Geographic entities mentioned:
surface_form: the fortress (alberta)
instance_of: Mountain
countries: Canada
coordinates: lat: 50.827777777777776
lon: -115.24333333333334
When viewed from Highway 40, the north face presents a fortress like appearance. The Fortress should not be confused with nearby Fortress Mountain. The mountain was originally named Tower Mountain but was changed in 1957 to its current name so as not to be confused with Tower Mountain. __NOTOC__
Climbing routes.

Geographic entities mentioned:
surface_form: the fortress
instance_of: Mountain
countries: Canada
coordinates: lat: 50.827777777777776
lon: -115.24333333333334
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The Headwall Lakes approach takes longer but the scree slopes leading to the col are not as loose as the Chester Lake side, which serves as a better descent route. Climate. Based on the Köppen climate classification, The Fortress is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C.

Geographic entities mentioned:
surface_form: the fortress
instance_of: Mountain
countries: Canada
coordinates: lat: 50.827777777777776
lon: -115.24333333333334
Both routes join at the Chester-Fortress col. From the col, a steep path ascends the remaining to the summit. Only the final section of the summit block requires any real hands on scrambling. The Headwall Lakes approach takes longer but the scree slopes leading to the col are not as loose as the Chester Lake side, which serves as a better descent route. Climate.

Geographic entities mentioned:
surface_form: chester lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.8117
lon: -115.275
surface_form: headwall lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 50.8058
lon: -115.246
When viewed from Highway 40, the north face presents a fortress like appearance. The Fortress should not be confused with nearby Fortress Mountain. The mountain was originally named Tower Mountain but was changed in 1957 to its current name so as not to be confused with Tower Mountain. __NOTOC__
Climbing routes.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: tower mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 58.414722222222224
lon: -124.86361111111111
surface_form: tower mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 58.414722222222224
lon: -124.86361111111111
In 1800, the Reverend Jeremiah Moore, no longer confined to jail, was granted permission to preach in the courthouse; in 1801 blacks were forbidden to play fives or other games within the enclosure. As construction of turnpike roads linking Alexandria and Washington to the Shenandoah Valley took place, activity that centered in Fairfax County's courthouse square increased.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
It was formerly surrounded by a wall with four gates, and today is home to a university. Sidi Bel Abbès is 75 kilometers from the Mediterranean Sea. History. The present city, on the Wadi Sig River, developed around a French camp built in 1843. In 1849 a planned agricultural town was established around the existing military post.

Geographic entities mentioned:
surface_form: Sig River
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 35.319166666667
lon: -0.41638888888889
In the 1930s much of the old city walls were demolished. Wide boulevards and squares replaced the traditional quarters, causing the town to lose much of its former character. Geography. The city sits astride both banks of the Sig River, and lake &quot;Sidi Mohamed Benali&quot;. The lake provides a major water reserve for the area. Climate.

Geographic entities mentioned:
surface_form: Sig River
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 35.319166666667
lon: -0.41638888888889
Initially, the Cima Coppi was scheduled to be the Passo di Gavia on the sixteenth stage, but due to weather the climb was removed from the itinerary. The next highest climb was that to Serrù Lake, however the climb had already been ascended prior to the cancellation.

Geographic entities mentioned:
surface_form: Serrù Lake
instance_of: Lake
countries: Italy
coordinates: lat: 45.459202777778
lon: 7.1257944444444
She served there during most of the remainder of the Civil War towing and repairing the ships of the blockade, steaming along the Confederate coast gathering information about activity ashore, carrying messages between ships of the squadron, and providing countless other services which helped the Union Navy to strangle the South. On 8 December she was ordered to St.

Geographic entities mentioned:
surface_form: St. Simons Sound
instance_of: Landform
countries: United States
coordinates: lat: 31.1286
lon: -81.415
Practitioners are called or. The mountains where &quot;shugendo&quot; is practiced are all over Japan, and can span multiple mountains within one range such as the Ōmine mountain range with Mount Hakkyō and Mount Ōmine or the Ishizuchisan mountain range with Kamegamori and Tengudake.

Geographic entities mentioned:
surface_form: Mount Hakkyō
instance_of: Mountain
countries: Japan
coordinates: lat: 34.173611
lon: 135.9075
surface_form: Mount Ōmine
instance_of: Mountain
countries: Japan
coordinates: lat: 34.252777777778
lon: 135.94055555556
surface_form: Ishizuchisan
instance_of: Mountain
countries: Japan
coordinates: lat: 33.766666666667
lon: 133.11666666667
The highest peak of the Ōmine mountain range is Mount Hakkyō at an altitude of 1915 m, and there are 75 places for ascetic practices along the mountain trail, and Ōminesan-ji Temple at the top of Mount Ōmine at an altitude of 1719 m is considered to be the highest sacred site of &quot;Shugendō&quot;.

Geographic entities mentioned:
surface_form: Mount Hakkyō
instance_of: Mountain
countries: Japan
coordinates: lat: 34.173611
lon: 135.9075
surface_form: Mount Ōmine
instance_of: Mountain
countries: Japan
coordinates: lat: 34.252777777778
lon: 135.94055555556
Mount Thiassi. Mount Thiassi is a mountain summit located in the Thiassi Range of the Coast Mountains, in southwestern British Columbia, Canada. It is the third-highest point in the Thiassi Range. Mount Thiassi is situated northwest of Pemberton, and south-southwest of Mount Vayu, which is its nearest higher peak.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount thiassi
instance_of: Mountain
countries: Canada
coordinates: lat: 50.7147
lon: -123.1836
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Thiassi. Mount Thiassi is a mountain summit located in the Thiassi Range of the Coast Mountains, in southwestern British Columbia, Canada. It is the third-highest point in the Thiassi Range. Mount Thiassi is situated northwest of Pemberton, and south-southwest of Mount Vayu, which is its nearest higher peak.

Geographic entities mentioned:
surface_form: mount thiassi
instance_of: Mountain
countries: Canada
coordinates: lat: 50.7147
lon: -123.1836
It is the third-highest point in the Thiassi Range. Mount Thiassi is situated northwest of Pemberton, and south-southwest of Mount Vayu, which is its nearest higher peak. Precipitation runoff from the peak and meltwater from unnamed glaciers on its slopes drain into tributaries of the Lillooet, Bridge, and Hurley Rivers.

Geographic entities mentioned:
surface_form: mount thiassi
instance_of: Mountain
countries: Canada
coordinates: lat: 50.7147
lon: -123.1836
Climate. Based on the Köppen climate classification, Mount Thiassi is located in a subarctic climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall.

Geographic entities mentioned:
surface_form: mount thiassi
instance_of: Mountain
countries: Canada
coordinates: lat: 50.7147
lon: -123.1836
Precipitation runoff from the peak and meltwater from unnamed glaciers on its slopes drain into tributaries of the Lillooet, Bridge, and Hurley Rivers. The first ascent of the mountain was made in 1965 by Dick Culbert and Alice Purdey. The mountain's name was submitted by this first ascent party to commemorate Thiassi, the god of storms according to Norse mythology.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The first ascent of the mountain was made in 1965 by Dick Culbert and Alice Purdey. The mountain's name was submitted by this first ascent party to commemorate Thiassi, the god of storms according to Norse mythology. The name was officially adopted June 22, 1967, 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
Mount Ball. Mount Ball is a mountain located on the Continental Divide, on the borders of Banff and Kootenay national parks in Western Canada. Mt. Ball is the highest peak of the Ball Range in the Canadian Rockies. The mountain was named in 1858 by James Hector after John Ball, a politician who helped secure funding for the Palliser expedition.

Geographic entities mentioned:
surface_form: mount ball
instance_of: Mountain
countries: Canada
coordinates: lat: 51.156388888889
lon: -116.00638888889
surface_form: kootenay
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mt. Ball can be ascended from a scrambling route by late summer but involves remote bushwhacking, which limits the number of attempts per year. The trailhead is located at the Marble Canyon Campground in Kootenay National Park. __NOTOC__
Geology. Mount Ball is composed of sedimentary rock laid down during the Precambrian to Jurassic periods.

Geographic entities mentioned:
surface_form: marble canyon
instance_of: Valley
countries: Canada
coordinates: lat: 51.185833333333335
lon: -116.12277777777778
surface_form: kootenay
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
surface_form: marble canyon
instance_of: Valley
countries: Canada
coordinates: lat: 50.833333333333336
lon: -121.68333333333334
Mount Ball. Mount Ball is a mountain located on the Continental Divide, on the borders of Banff and Kootenay national parks in Western Canada. Mt. Ball is the highest peak of the Ball Range in the Canadian Rockies. The mountain was named in 1858 by James Hector after John Ball, a politician who helped secure funding for the Palliser expedition.

Geographic entities mentioned:
surface_form: mount ball
instance_of: Mountain
countries: Canada
coordinates: lat: 51.156388888889
lon: -116.00638888889
The trailhead is located at the Marble Canyon Campground in Kootenay National Park. __NOTOC__
Geology. Mount Ball is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate.

Geographic entities mentioned:
surface_form: mount ball
instance_of: Mountain
countries: Canada
coordinates: lat: 51.156388888889
lon: -116.00638888889
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate. Based on the Köppen climate classification, Mount Ball is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports glaciers on its slopes.

Geographic entities mentioned:
surface_form: mount ball
instance_of: Mountain
countries: Canada
coordinates: lat: 51.156388888889
lon: -116.00638888889
Mt. Ball is the highest peak of the Ball Range in the Canadian Rockies. The mountain was named in 1858 by James Hector after John Ball, a politician who helped secure funding for the Palliser expedition. The name was officially adopted in 1924 based on Palliser's 1863 map of British North America. Mt.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
It is a dicot shrub or sub-shrub in the Hydrangeaceae family, native to the Pacific Coastal region of the United States. &quot;Whipplea&quot; appears to have been first recorded in 1853 by the Scottish botanical explorer John Jeffrey in the Umpqua Valley near Mount Shasta, California, and named for Lieutenant Amiel Weeks Whipple (1817–1863), American surveyor and engineer.

Geographic entities mentioned:
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
General Francis A. Shoup. The remains are spread across a six to seven mile stretch along the northwest side of the Chattahoochee River from a point just north of where Nickajack Creek joins the Chattahoochee in Mableton to north of S. Atlanta Road in Smyrna/Vinings. It was added to the National Register of Historic Places on July 5, 1973.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Sherman had managed to out-maneuver Confederate General Joseph E. Johnston's Army of Tennessee throughout Northwest Georgia forcing them to fall back to a defensive position at Kennesaw Mountain in late June. Johnston saw the nearby Chattahoochee River as the largest natural boundary between his army and the city of Atlanta.

Geographic entities mentioned:
surface_form: Kennesaw Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.976213888889
lon: -84.579655555556
Although Federal troops constructed both trenches and battery positions opposing Johnston's River Line, General Sherman had no intention of a direct assault—especially following his underestimation of Johnston's defensive position at Kennesaw Mountain.

Geographic entities mentioned:
surface_form: Kennesaw Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.976213888889
lon: -84.579655555556
Mouchli. Mouchli () was a Byzantine town and castle in the Tegean plain in the Peloponnese in Greece. It was on the edge of the Partheni Basin, between the Tegean plain and the Argolid. In the early 14th century, after the the seat of the Bishopric of Morea was moved from Nikli to Mouchli.

Geographic entities mentioned:
surface_form: Partheni Basin
instance_of: Mountain
countries: Greece
coordinates: lat: 37.4864
lon: 22.5474
In &quot;Lost Land of the Volcano&quot;, BBC One 2009, he led the first western expedition into the crater of the extinct volcano, Mount Bosavi, in Papua New Guinea, where they discovered, among other things, one of the largest species of rats known anywhere in the world, provisionally called the Bosavi woolly rat while its scientific name is determined.

Geographic entities mentioned:
surface_form: Mount Bosavi
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -6.6141666666667
lon: 142.82666666667
Backshall is a rock climber and mountaineer, and does adventure races, fell runs and endurance sports. In 2014, he summitted the highly technical granite Mount Asgard in Arctic Baffin Island, in one single 27-hour summit push.

Geographic entities mentioned:
surface_form: Mount Asgard
instance_of: Mountain
countries: Canada
coordinates: lat: 66.672222222222
lon: -65.274444444444
In 2014, he summitted the highly technical granite Mount Asgard in Arctic Baffin Island, in one single 27-hour summit push. Ice and alpine climbing are described as being among his great passions, and he has climbed such peaks as Cho Oyu, the sixth highest mountain in the world at 8201 m, and Cholatse in the Himalayan Khumbu.

Geographic entities mentioned:
surface_form: Cho Oyu
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 28.094166666667
lon: 86.660833333333
surface_form: Cholatse
instance_of: Mountain
countries: Nepal
coordinates: lat: 27.92
lon: 86.76611111111112
surface_form: Khumbu
instance_of: Valley
countries: Nepal
coordinates: lat: 27.805
lon: 86.71
He qualified as an advanced Himalayan Expedition leader from India's Nehru Institute of Mountaineering. He partnered John Arran and Ivan Calderon up the first ascent of Upuigma-tepui in Venezuela, and led the first ascent of the North face of Mount Kuli in Borneo. In 2005, he ran the Marathon des Sables 243 km across the Sahara desert to raise money for the Wolftrust.

Geographic entities mentioned:
surface_form: Upuigma-tepui
instance_of: Mountain
countries: Venezuela
coordinates: lat: 5.0861111111111
lon: -61.956388888889
He has competed in numerous triathlons, adventure races and fell running events. His best finishes include winning the 'Extreme' and 'Last Man Standing' events at UK Tough Guy, finishing 9th overall at Tough Guy and 4th in the Welsh 1000m peak marathon. In July 2008, while attempting to climb a wet cliff face in the Wye Valley in the Forest of Dean, he fell onto rocks.

Geographic entities mentioned:
surface_form: Wye Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69255
lon: -2.66283
It is located between two hill ranges. Oscawana Creek merges into Peekskill Hollow Creek near the intersection of Peekskill Hollow Road and Oscawana Lake Road in Putnam Valley the hamlet of Lake Peekskill. The lake has a number of houses around its edges, several rock formations in the center of the lake, and small islands accessible by kayak or canoe.

Geographic entities mentioned:
surface_form: oscawana lake
instance_of: Lake
countries: United States
coordinates: lat: 41.396666666667
lon: -73.848333333333
surface_form: lake peekskill
instance_of: Lake
countries: United States
coordinates: lat: 41.339166666667
lon: -73.882222222222
The lake has had a thriving summer resort community surrounding it since the 1850s, around which time the area was accessible by an hour-and-a-half drive from the Peekskill train station. Taxi carriages to and from the region were pulled by mules; these carts were also used to carry coal to mills near Oregon Corners along Oscawana Lake Road.

Geographic entities mentioned:
surface_form: oscawana lake
instance_of: Lake
countries: United States
coordinates: lat: 41.396666666667
lon: -73.848333333333
Bus service to the lake started in the 1920s up until the 1940s. There was an icehouse on Lake Oscawana, which made up the only major industry on the lake. It supplied ice to summer visitors and the Oscawana Lake House, a summer resort built in 1856 by Abijah Lee. A gristmill was present on the eastern side of the lake, the location of which was noted as Abele Cove. Celebrity residences.

Geographic entities mentioned:
surface_form: oscawana lake
instance_of: Lake
countries: United States
coordinates: lat: 41.396666666667
lon: -73.848333333333
Lake Oscawana. Lake Oscawana is a body of water located in Putnam Valley, New York, United States. The lake has a depth that ranges from at its deepest. The lake is fed by a stream from its north end and it drains out into Oscawana Creek at the middle of its southeastern shore. It is located between two hill ranges.

Geographic entities mentioned:
surface_form: lake oscawana
instance_of: Lake
countries: United States
coordinates: lat: 41.396666666667
lon: -73.848333333333
The lake has a number of houses around its edges, several rock formations in the center of the lake, and small islands accessible by kayak or canoe. Lake Oscawana provides summer recreation, and some local residents use the lake for boating, swimming, and fishing from the lake's several private beaches.

Geographic entities mentioned:
surface_form: lake oscawana
instance_of: Lake
countries: United States
coordinates: lat: 41.396666666667
lon: -73.848333333333
In the winter, the lake freezes over and allows for ice skating and ice fishing. There are reports of people falling through the ice in warmer winters. History. Lake Oscawana was said to be named by members of the Wappinger Indian Confederation, specifically the Nochpeem tribe, and varying spellings of the lake's name were written on tracts of land sold to the Van Cortlandt family in the 1680s.

Geographic entities mentioned:
surface_form: lake oscawana
instance_of: Lake
countries: United States
coordinates: lat: 41.396666666667
lon: -73.848333333333
Bus service to the lake started in the 1920s up until the 1940s. There was an icehouse on Lake Oscawana, which made up the only major industry on the lake. It supplied ice to summer visitors and the Oscawana Lake House, a summer resort built in 1856 by Abijah Lee. A gristmill was present on the eastern side of the lake, the location of which was noted as Abele Cove. Celebrity residences.

Geographic entities mentioned:
surface_form: lake oscawana
instance_of: Lake
countries: United States
coordinates: lat: 41.396666666667
lon: -73.848333333333
Completed in 1972 as the upperclass dining hall for the Centennials and named after Monroe Jackson Rathbone, it is modern in appearance and seems to hang off the mountain, being built in a very steep section and having ground floor access to each of its floors. The main part of the building is one of Lehigh's dining halls, offering sweeping views of the Lehigh Valley from the dining room.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Built as Bethlehem Steel's Homer Research Labs, the Mountaintop Campus is and was acquired by Lehigh in 1986. It is home to the College of Education and facilities for the Civil Engineering, Chemical Engineering, and Biological Sciences departments. The campus offers some of the most comprehensive views of the Lehigh Valley that surrounds the university and Bethlehem. Iacocca Hall (1958).

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Puma Wayin (Huánuco). Puma Wayin (Quechua &quot;puma&quot; cougar, puma, Ancash Quechua &quot;wayi&quot; house, &quot;cougar house&quot;, &quot;-n&quot; a suffix, also spelled &quot;Puma Huain&quot;) is a mountain in the Andes of Peru which reaches a height of approximately. It is located in the Huánuco Region, Huamalíes Province, Singa District.

Geographic entities mentioned:
surface_form: puma wayin
instance_of: Mountain
countries: Peru
coordinates: lat: -9.84056
lon: -77.2808
surface_form: puma wayin
instance_of: Mountain
countries: Peru
coordinates: lat: -10.00166667
lon: -76.86166667
surface_form: puma wayin (huánuco)
instance_of: Mountain
countries: Peru
coordinates: lat: -9.34305556
lon: -76.84222222
surface_form: puma wayin
instance_of: Mountain
countries: Peru
coordinates: lat: -9.69833333
lon: -77.56527778
Puma Wayin (Huánuco). Puma Wayin (Quechua &quot;puma&quot; cougar, puma, Ancash Quechua &quot;wayi&quot; house, &quot;cougar house&quot;, &quot;-n&quot; a suffix, also spelled &quot;Puma Huain&quot;) is a mountain in the Andes of Peru which reaches a height of approximately. It is located in the Huánuco Region, Huamalíes Province, Singa District.

Geographic entities mentioned:
surface_form: puma wayin
instance_of: Mountain
countries: Peru
coordinates: lat: -9.84056
lon: -77.2808
surface_form: puma wayin
instance_of: Mountain
countries: Peru
coordinates: lat: -10.00166667
lon: -76.86166667
surface_form: puma wayin
instance_of: Mountain
countries: Peru
coordinates: lat: -9.34305556
lon: -76.84222222
surface_form: puma huain
instance_of: Mountain
countries: Peru
coordinates: lat: -9.34305556
lon: -76.84222222
surface_form: puma wayin
instance_of: Mountain
countries: Peru
coordinates: lat: -9.69833333
lon: -77.56527778
Mount Lumarku. Mount Lumarku or Lumaku () is a mountain located southeast of Sipitang in the Interior Division of Sabah, Malaysia, and is the highest point of the Sipitang District, with an elevation of above sea level. The mountain has prominent biodiversity, and is part of the Gunong Lumaku Forest Reserve, under the surveillance of the Sabah Forestry Department. Geology.

Geographic entities mentioned:
surface_form: mount lumarku
instance_of: Mountain
countries: Malaysia
The mountain has prominent biodiversity, and is part of the Gunong Lumaku Forest Reserve, under the surveillance of the Sabah Forestry Department. Geology. Mount Lumarku rests on a discontinuous geological formation at the southern end of the Crocker Mountains and the northern part of the Meligan Range. Biodiversity.

Geographic entities mentioned:
surface_form: mount lumarku
instance_of: Mountain
countries: Malaysia
hurrelliana&quot;, and &quot;N. tentaculata&quot; are native to this mountain. Approximately 127 species of mosses were discovered in Mount Lumarku, equivalent to nearly one-fifth of Borneo's moss taxa. Borneo-specific fauna available include frog species, &quot;Philautus bunitus&quot;, and skink species &quot;Tytthoscincus aesculeticola&quot; and &quot;Sphenomorphus kinabaluensis&quot;.

Geographic entities mentioned:
surface_form: mount lumarku
instance_of: Mountain
countries: Malaysia
Threats and conservation. Mount Lumarku's rain forest is protected as the Gunong Lumaku Forest Reserve, established in 1992 under the surveillance of the Sabah Forestry Department, with an area of. Mount Lumarku's protected rain forest exhibit a degree of deforestation leakage 0.14% annual rate, with a much higher degree of deforestation in its surrounding buffer zone with 1.56%.

Geographic entities mentioned:
surface_form: mount lumarku
instance_of: Mountain
countries: Malaysia
This is the lone active coal mine in Bangladesh. History. In Pre-partition era of British India, coal from Garo hills of Meghalaya was transported and traded through East Bengal. Mining offices opened in Dhaka and trade was aided by British Rail network in India. In 1961 UN-Pak Mineral Survey Project started surveys in then East Pakistan (today Bangladesh) by Geological Survey of Pakistan.

Geographic entities mentioned:
surface_form: Garo hills
instance_of: Mountain
countries: India
coordinates: lat: 25.5
lon: 90.33333333333333
Saint John. The UNB Saint John campus (UNBSJ) is in Tucker Park in the Millidgeville neighbourhood, several kilometres north of the city's central business district, and has views of the Kennebecasis River and Grand Bay-Westfield. New Brunswick's largest health care facility, Saint John Regional Hospital, is adjacent to the UNBSJ campus.

Geographic entities mentioned:
surface_form: Kennebecasis River
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.31666667
lon: -66.13333333
In addition, export quotas on Chinese rare-earth exports have resulted in a generally shaky supply of those metals. A few non-Chinese sources such as the advanced Hoidas Lake project in northern Canada and Mt Weld in Australia were under development, however it is not known if these sources will be developed before a shortage hits. Legislation and incentives.

Geographic entities mentioned:
surface_form: Hoidas Lake
instance_of: Lake
countries: Canada
coordinates: lat: 59.9258
lon: -107.823
15th century: The Templo Mayor. During the 15th century, the Cerro del Chiquihuite was located on the shores of Lake Texcoco, some 9 to 12 kilometers from the heart of the Aztec Empire, Tenochtitlán. The Cerro del Chiquihuite was made principally of a pinkish and violet rock called andesita de lamprobolita, an extrusive igneous rock.

Geographic entities mentioned:
surface_form: Lake Texcoco
instance_of: Lake
countries: Mexico
coordinates: lat: 19.5
lon: -98.99
surface_form: cerro del chiquihuite
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.5328
lon: -99.1306
surface_form: cerro del chiquihuite
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.5328
lon: -99.1306
Cerro del Chiquihuite. Cerro del Chiquihuite (Chiquihuite Hill) is a hill located in the north of Mexico City, in the borough of Gustavo A. Madero and bordering the municipality of Tlalnepantla de Baz in the State of Mexico. The hill has a height of above sea level and forms part of the Sierra de Guadalupe mountain range.

Geographic entities mentioned:
surface_form: cerro del chiquihuite
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.5328
lon: -99.1306
For instance, in the borough of Lázaro Cárdenas, only the largest of these, known as &quot;El Pocito&quot;, still flows. The mountain is rather heavily developed and is prone to landslides; in 1987, 15 people were killed by mudslides off Cerro del Chiquihuite and La Presa hills after heavy rains hit Mexico City. 15th century: The Templo Mayor.

Geographic entities mentioned:
surface_form: cerro del chiquihuite
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.5328
lon: -99.1306
A road leads to the top of the mountain, where transmitters are located for five FM radio stations and eleven television stations, as well as other telecommunications equipment. Radio stations. Five stations owned by Grupo Radio Centro maintain backup facilities on Cerro del Chiquihuite. They were relocated to a new facility at Villa Alpina, Naucalpan, State of Mexico, in August 2012.

Geographic entities mentioned:
surface_form: cerro del chiquihuite
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.5328
lon: -99.1306
Kudžioniai. Kudžioniai (formerly,) is a village in Kėdainiai district municipality, in Kaunas County, in central Lithuania. According to the 2011 census, it had a population of 1 person. It is from Nociūnai, by the Šerkšnys river and the Jonava-Šeduva (KK144) road.

Geographic entities mentioned:
surface_form: Šerkšnys
instance_of: Watercourse
countries: Lithuania
coordinates: lat: 55.257734
lon: 23.953286
The entire route is in Shelter Island. County Route 70. County Route 70 is Old West Lake Drive and formerly CR 77A. The road runs northwest from NY 27 along the southwest side of Montauk Lake before reaching CR 77. The entire route is in Montauk. County Route 71. County Route 71 is also Old Country Road, but strictly in Eastport and the western town of Southampton.

Geographic entities mentioned:
surface_form: Montauk Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.068675
lon: -71.928
County Route 75. County Route 75 is a short divided highway in Smith Point County Park that was intended to be part of the formerly proposed Ocean Parkway extension. The entire route is in Smith Point County Park.

Geographic entities mentioned:
surface_form: Smith Point County Park
instance_of: Landform
countries: United States
coordinates: lat: 40.7384
lon: -72.8444
Background. He moved to Alaska in 1976, working on the Alaskan pipeline and owning and running a lodge at Kenai Lake during the 1970s. Pezzenti then began working as an independent wildlife photographer and published three photography books during his life. Some of his photos hung in the Oval Office during the presidency of Ronald Reagan.

Geographic entities mentioned:
surface_form: Kenai Lake
instance_of: Lake
countries: United States
coordinates: lat: 60.418333333333
lon: -149.66666666667
As the typhoon moved through Japan, heavy rainfall fell throughout the Tokai and Kanto-Koshin regions, with 24-hour rainfall records in June being broken in Mie Prefecture, Shizuoka Prefecture and Ibaraki Prefecture. Total accumulated rainfall totals of were reported at Miyagawa in Ōdai, and at Mount Amagi in Izu, Shizuoka.

Geographic entities mentioned:
surface_form: Mount Amagi
instance_of: Mountain
countries: Japan
coordinates: lat: 34.862777777778
lon: 139.00166666667
Mattertal. The Matter Valley (German: Mattertal, or sometimes &quot;Nikolaital&quot;) is located in southwestern Switzerland, south of the Rhône valley in the canton of Valais. The village of Zermatt is the most important settlement of the valley, which is surrounded by many four-thousanders, including the Matterhorn. Geography.

Geographic entities mentioned:
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
Located in the Pennine Alps, the Matter Valley is drained by the Matter Vispa, a tributary of the Rhone. The valley itself ends at Stalden where it meets the Saas Valley. The resulting Visp Valley continues for a few kilometres until it reaches the town of Visp on the young river Rhone. The valley starts between the high summits south of Zermatt (Monte Rosa, Matterhorn) on the border with Italy.

Geographic entities mentioned:
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
surface_form: monte rosa
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.936666666667
lon: 7.8666666666667
The upper side is glaciated, the second largest glacier of the Alps, the Gorner Glacier lies at the foot of Monte Rosa (4,634 m), while the Zmutt Glacier lies at the foot of the Matterhorn (4,478 m). Around the village of Randa are located the Weisshorn (4,505 m) and the Dom (4,545 m). The difference of height between the talweg and the summits on both side reaches over 3 km.

Geographic entities mentioned:
surface_form: Weisshorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.101666666667
lon: 7.7161111111111
surface_form: weisshorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.789583333333
lon: 9.6382222222222
surface_form: weisshorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.101666666667
lon: 7.7161111111111
surface_form: weisshorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.3838
lon: 7.4736
The valley starts between the high summits south of Zermatt (Monte Rosa, Matterhorn) on the border with Italy. The upper side is glaciated, the second largest glacier of the Alps, the Gorner Glacier lies at the foot of Monte Rosa (4,634 m), while the Zmutt Glacier lies at the foot of the Matterhorn (4,478 m). Around the village of Randa are located the Weisshorn (4,505 m) and the Dom (4,545 m).

Geographic entities mentioned:
surface_form: monte rosa
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.936666666667
lon: 7.8666666666667
Mattertal. The Matter Valley (German: Mattertal, or sometimes &quot;Nikolaital&quot;) is located in southwestern Switzerland, south of the Rhône valley in the canton of Valais. The village of Zermatt is the most important settlement of the valley, which is surrounded by many four-thousanders, including the Matterhorn. Geography.

Geographic entities mentioned:
surface_form: mattertal
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.083333333333
lon: 7.8
Mattertal. The Matter Valley (German: Mattertal, or sometimes &quot;Nikolaital&quot;) is located in southwestern Switzerland, south of the Rhône valley in the canton of Valais. The village of Zermatt is the most important settlement of the valley, which is surrounded by many four-thousanders, including the Matterhorn. Geography.

Geographic entities mentioned:
surface_form: mattertal
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.083333333333
lon: 7.8
surface_form: nikolaital
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.083333333333
lon: 7.8
He was born in Rhode Island in 1762. Casey was a Quaker and was viewed with hostility because he would not join in the combat. His father Samuel had been killed during the American Revolution. He first settled near Lake Champlain in the belief that it was held by the British. After the boundary was established, he moved to Adolphustown Township around 1790.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
History. Cramer Tunnel opened in 1957 after LTV Steel blasted a tunnel to connect Hoyt Lakes taconite plant and the location of its ore dock at Taconite Harbor on Lake Superior, from which the taconite was shipped to eastern steel mills. The tunnel was used consistently from its opening to 2001, when LTV Steel went bankrupt and closed their ore dock in Taconite Harbor.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
There is one record of it from the Australian Thursday Island. Its range includes several very small islands such as Karkar Island and Sakar Island. It is unknown why the great flying fox does not occur on nearby larger islands, such as the Louisiade Archipelago and the D'Entrecasteaux Islands. It has been documented at a range of elevations from above sea level.

Geographic entities mentioned:
surface_form: Karkar Island
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -4.633333
lon: 145.966667
surface_form: Sakar Island
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -5.40900833
lon: 148.08140556
Buttercup Mountain. Buttercup Mountain is a peak in the Smoky Mountains of Idaho, United States. The peak is above sea level in Sawtooth National Forest on the border of Blaine and Camas counties. It is in the watersheds of Willow and Deer creeks. It is about northwest of Kelly Mountain and southeast of Dollarhide Mountain. No roads or trails go to the summit.

Geographic entities mentioned:
surface_form: Dollarhide Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.8363
lon: -114.711
surface_form: kelly mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.4925
lon: -114.46722222222
Buttercup Mountain. Buttercup Mountain is a peak in the Smoky Mountains of Idaho, United States. The peak is above sea level in Sawtooth National Forest on the border of Blaine and Camas counties. It is in the watersheds of Willow and Deer creeks. It is about northwest of Kelly Mountain and southeast of Dollarhide Mountain. No roads or trails go to the summit.

Geographic entities mentioned:
surface_form: buttercup mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.5155
lon: -114.577
This third one was built between the Plaça de Catalunya and la Bordeta to link the city centre with the Plaça d'Espanya and Montjuïc, the site of the 1929 Barcelona International Exposition.

Geographic entities mentioned:
surface_form: Montjuïc
instance_of: Mountain
countries: Spain
coordinates: lat: 41.364166666667
lon: 2.1580555555556
Although it is common to refer to the entire body of water as the Serpentine, the name refers in the strict sense only to the eastern half of the lake. Serpentine Bridge, which marks the boundary between Hyde Park and Kensington Gardens, also marks the Serpentine's western boundary; the long and narrow western half of the lake is known as the Long Water.

Geographic entities mentioned:
surface_form: the Long Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.5074
lon: -0.174444
surface_form: long water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.5074
lon: -0.174444
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: the serpentine
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.505277777778
lon: -0.16944444444444
surface_form: serpentine
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.505277777778
lon: -0.16944444444444
surface_form: serpentine
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.505277777778
lon: -0.16944444444444
Among the landmarks near the lake is the Diana, Princess of Wales Memorial Fountain. Geography of the lake. Originally the lake was fed by the River Westbourne entering at the Italian Garden at the north-western end of the Long Water. The Westbourne ceased to provide the water for the Serpentine in 1834, as it had become polluted so water was for some years pumped from the tidal Thames.

Geographic entities mentioned:
surface_form: long water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.5074
lon: -0.174444
surface_form: the long water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.5074
lon: -0.174444
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
The water is now supplied by three boreholes drilled into the Upper Chalk. The first borehole is at the Italian Gardens, the second at the Diana Memorial and the third, drilled in 2012 to a depth of, is within of there. The Long Water runs south-east from this point to Serpentine Bridge, where the lake curves to the east, following the natural contours of the land.

Geographic entities mentioned:
surface_form: long water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.5074
lon: -0.174444
surface_form: the long water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.5074
lon: -0.174444
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: serpentine
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.505277777778
lon: -0.16944444444444
In the 1820s, the park was extensively redesigned by Decimus Burton. At the same time, John Rennie the Younger designed and oversaw the Serpentine Bridge as part of newly built West Carriage Drive bounding Hyde Park against Kensington Gardens, dividing the lake into the Serpentine (east) and the Long Water (west).

Geographic entities mentioned:
surface_form: long water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.5074
lon: -0.174444
surface_form: the long water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.5074
lon: -0.174444
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: the serpentine
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.505277777778
lon: -0.16944444444444
surface_form: the serpentine
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.505277777778
lon: -0.16944444444444
surface_form: serpentine
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.505277777778
lon: -0.16944444444444
surface_form: serpentine
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.505277777778
lon: -0.16944444444444
The Serpentine. The Serpentine (also known as the Serpentine River) is a recreational lake in Hyde Park, London, England, created in 1730 at the behest of Queen Caroline. Although it is common to refer to the entire body of water as the Serpentine, the name refers in the strict sense only to the eastern half of the lake.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: the serpentine
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.505277777778
lon: -0.16944444444444
surface_form: serpentine
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.505277777778
lon: -0.16944444444444