Sarmila/GeoWiki-Features huggingface dataset:
Beatrice Peak. Beatrice Peak is a peak located on the Continental Divide on the border of Banff and Kootenay National Parks, between Stanley Peak and Mount Ball. The mountain was named in 1912 by the Alpine Club of Canada after Beatrice Shultz who climbed the mountain that year. The scrambling route to Mt. Ball includes the ascent of Beatrice Peak.

Geographic entities mentioned:
surface_form: beatrice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.16277777777778
lon: -116.025
Beatrice Peak. Beatrice Peak is a peak located on the Continental Divide on the border of Banff and Kootenay National Parks, between Stanley Peak and Mount Ball. The mountain was named in 1912 by the Alpine Club of Canada after Beatrice Shultz who climbed the mountain that year. The scrambling route to Mt. Ball includes the ascent of Beatrice Peak.

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
Ketelbrug. The Ketelbrug is bridge spanning the Ketel-lake between the Noordoostpolder and the Eastern Flevopolder in the Dutch province of Flevoland. The motorway A6 runs over it. A part of it is a Bascule bridge. The bridge was opened on 15 June 1970. The Ketelbrug had a lot of accidents. One of those was when the warning lights didn't flash and the bridge went up.

Geographic entities mentioned:
surface_form: Ketel-lake
instance_of: Lake
countries: Netherlands
coordinates: lat: 52.596666666667
lon: 5.7622222222222
Jacques Peaks. u9u3gmgxqrsc69v3g0cgicwce123" xml:space="preserve">#redirect Jacques Peaks

Geographic entities mentioned:
surface_form: jacques peaks
instance_of: Mountain
coordinates: lat: -64.516666666667
lon: -61.85
Economy. While Deloraine is a predominantly rural farming town, it is also aimed at pleasing tourists, who visit because of its culture and location also serving as a base to explore areas such as Cradle Mountain, the Great Western Tiers, Mole Creek and the Central Highlands. Farms in the area produce poppies, herbs, onions and potatoes; as is typical produce for the Tasmanian climate.

Geographic entities mentioned:
surface_form: Cradle Mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -41.684644444444
lon: 145.951275
Udren Zom. Udren Zom is a mountain in the Hindu Kush mountain range in Pakistan. Its summit has an elevation of and a topographic prominence of. It is one of the highest peaks in the world located outside of the Himalayan and Karakoram ranges. Udren Zom is located in the Khyber Pakhtunkhwa province of Pakistan. The main peak was first climbed in 1964 by an Austrian team.

Geographic entities mentioned:
surface_form: udren zom
instance_of: Mountain
countries: Pakistan
coordinates: lat: 36.53333333333333
lon: 71.98333333333333
Udren Zom. Udren Zom is a mountain in the Hindu Kush mountain range in Pakistan. Its summit has an elevation of and a topographic prominence of. It is one of the highest peaks in the world located outside of the Himalayan and Karakoram ranges. Udren Zom is located in the Khyber Pakhtunkhwa province of Pakistan. The main peak was first climbed in 1964 by an Austrian team.

Geographic entities mentioned:
surface_form: udren zom
instance_of: Mountain
countries: Pakistan
coordinates: lat: 36.53333333333333
lon: 71.98333333333333
surface_form: kush
instance_of: Mountain
countries: Pakistan
coordinates: lat: 28.8171
lon: 66.5674
Its summit has an elevation of and a topographic prominence of. It is one of the highest peaks in the world located outside of the Himalayan and Karakoram ranges. Udren Zom is located in the Khyber Pakhtunkhwa province of Pakistan. The main peak was first climbed in 1964 by an Austrian team. Gerald Gruber and Rudolf Pischinger completed the first ascent on August 19.

Geographic entities mentioned:
surface_form: udren zom
instance_of: Mountain
countries: Pakistan
coordinates: lat: 36.53333333333333
lon: 71.98333333333333
Wagensonnriegel. Wagensonnriegel is a mountain of Bavaria, Germany.

Geographic entities mentioned:
surface_form: wagensonnriegel
instance_of: Mountain
countries: Germany
coordinates: lat: 48.9494
lon: 13.2827
Kingston Peninsula. The Kingston Peninsula is a peninsula in southern New Brunswick, Canada, located between the Saint John River and the Kennebecasis River in Kings County. The peninsula was the site of the first United Empire Loyalist settlement in New Brunswick in 1783.

Geographic entities mentioned:
surface_form: Kennebecasis River
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.31666667
lon: -66.13333333
The station's studios and offices are co-located with formerly co-owned KPIX-TV on Battery Street in downtown San Francisco, and its transmitter is off Wolfback Ridge Road on Mount Beacon in the Marin Headlands near Sausalito, California. History. The 97.3 MHz frequency signed on the air as KWBR-FM, dedicated September 14, 1947.

Geographic entities mentioned:
surface_form: Marin Headlands
instance_of: Landform
countries: United States
coordinates: lat: 37.827777777778
lon: -122.50611111111
Lake Five (Michigan). Lake Five is a private fresh water lake in Kalkaska County, Michigan, United States. Lake Five has abundant water fauna including largemouth bass, bluegill, perch, painted turtle and snapping turtle.

Geographic entities mentioned:
surface_form: lake five (michigan)
instance_of: Lake
countries: United States
coordinates: lat: 44.765279
lon: -85.060431
surface_form: lake five
instance_of: Lake
countries: United States
coordinates: lat: 48.464444444444446
lon: -114.02
Lake Five (Michigan). Lake Five is a private fresh water lake in Kalkaska County, Michigan, United States. Lake Five has abundant water fauna including largemouth bass, bluegill, perch, painted turtle and snapping turtle.

Geographic entities mentioned:
surface_form: lake five
instance_of: Lake
countries: United States
coordinates: lat: 44.765279
lon: -85.060431
surface_form: lake five
instance_of: Lake
countries: United States
coordinates: lat: 48.464444444444446
lon: -114.02
Lake Five is a private fresh water lake in Kalkaska County, Michigan, United States. Lake Five has abundant water fauna including largemouth bass, bluegill, perch, painted turtle and snapping turtle. Lake Five also has abundant land fauna including black bear, white-tailed deer, garter snake, midland brown snake (&quot;Storeria dekayi wrightorum&quot;), red fox, beaver and wild turkey.

Geographic entities mentioned:
surface_form: lake five
instance_of: Lake
countries: United States
coordinates: lat: 44.765279
lon: -85.060431
surface_form: lake five
instance_of: Lake
countries: United States
coordinates: lat: 48.464444444444446
lon: -114.02
It is believed that if certain acts are carried out, then it will allow the child for a healthier and happier future. One example of this is the belief in the Chillihuani that if a knife or scissors are used for cutting the umbilical cord, it will cause for the child to go through clothes very quickly. To prevent this, a jagged ceramic tile is used to cut the umbilical cord.

Geographic entities mentioned:
surface_form: Chillihuani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.40166667
lon: -66.61527778
In addition to the usual central north-south road (), which in Jerusalem headed straight up the western hill, a second major north-south road was added down the line of the Tyropoeon Valley; these two cardines converge near the Damascus Gate, close to the.

Geographic entities mentioned:
surface_form: Tyropoeon Valley
instance_of: Valley
countries: State of Palestine
Israel
coordinates: lat: 31.776947222222
lon: 35.234238888889
The first reports of a pilgrimage route corresponding to the Biblical events date from the Byzantine era; during that time, a Holy Thursday procession started from the top of the Mount of Olives, stopped in Gethsemane, entered the Old City at the Lions' Gate, and followed approximately the current route to the Church of the Holy Sepulchre; however, there were no actual stops during the route along the itself.

Geographic entities mentioned:
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
(Today's extends westward from the western portion of that street.) Near the ruined Antonia Fortress and north of the Templum Domini precinct, Jehoshaphat Street led eastward to the Jehoshaphat Gate (near or at Lions' Gate on Lions' Gate Street), with the Valley of Jehoshaphat (near or in the Kidron Valley) beyond the gate.

Geographic entities mentioned:
surface_form: Kidron Valley
instance_of: Valley
countries: State of Palestine
coordinates: lat: 31.776972222222224
lon: 35.23897222222222
Fort Phantom Hill. Fort Phantom Hill, also called the Camp on the Clear Fork, is a former United States Army installation located in Jones County, Texas. The fort was established in 1851 as part of a line of forts in Texas to protect migrants passing through the state on their way to California. The US Army abandoned the fort in 1854 and it was shortly thereafter mostly destroyed by fire.

Geographic entities mentioned:
surface_form: fort phantom hill
instance_of: Landform
countries: United States
coordinates: lat: 32.6433
lon: -99.6775
During the war, the fort was occupied by Confederate frontier troops until the Confederacy's defeat and surrender. Following the US Army's return to Texas after the Civil War, Fort Phantom Hill was used as a subpost of the larger, newer Fort Griffin until 1875. After its final abandonment in 1875, a town was established at Fort Phantom Hill that flourished in the 1870s and ceased to exist by 1900.

Geographic entities mentioned:
surface_form: fort phantom hill
instance_of: Landform
countries: United States
coordinates: lat: 32.6433
lon: -99.6775
Following the fort's purchase by John Guitar in 1928, there was renewed public interest in the fort that led to its opening to the public in 1972. In 1997, Fort Phantom Hill was transferred to the Fort Phantom Hill Foundation. The ruins of the fort were added to the National Register of Historic Places on September 14, 1972. Use as military outpost.

Geographic entities mentioned:
surface_form: fort phantom hill
instance_of: Landform
countries: United States
coordinates: lat: 32.6433
lon: -99.6775
surface_form: fort phantom hill
instance_of: Landform
countries: United States
coordinates: lat: 32.6433
lon: -99.6775
Use as military outpost. Fort Phantom Hill was established during the American colonization of Texas, a process that began in the 1820s with the immigration of Anglo-Americans into Spanish, later Mexican, Texas. After existing as an independent republic for a decade, Texas was annexed by the United States of America in 1845, which led to the start of the Mexican-American War the next year.

Geographic entities mentioned:
surface_form: fort phantom hill
instance_of: Landform
countries: United States
coordinates: lat: 32.6433
lon: -99.6775
On November 14, 1851, five companies of the 5th Infantry Regiment, commanded by Lieutenant Colonel John Joseph Abercrombie, arrived on Phantom Hill and established the Camp on the Clear Fork of the Brazos, better known as Fort Phantom Hill.

Geographic entities mentioned:
surface_form: fort phantom hill
instance_of: Landform
countries: United States
coordinates: lat: 32.6433
lon: -99.6775
Construction of Fort Phantom Hill began immediately and lasted until June 1852, and it was followed by the creation of a crude road to Fort Chadbourne, to the southwest. Construction and basic life at the fort was complicated by a lack of usable wood, water, game, and fertile soil.

Geographic entities mentioned:
surface_form: fort phantom hill
instance_of: Landform
countries: United States
coordinates: lat: 32.6433
lon: -99.6775
Officers' quarters lined the north and east sides, opposite the enlisted men's barracks, while administrative structures stood on the west side. Additional buildings, such as the magazine and bakery, were located away from the parade ground and its surrounding structures. On April 27, 1852, Abercrombie was replaced as commander of Fort Phantom Hill by Lieutenant Colonel Carlos Waite.

Geographic entities mentioned:
surface_form: fort phantom hill
instance_of: Landform
countries: United States
coordinates: lat: 32.6433
lon: -99.6775
McCulloch passed the task to his brother, Colonel Henry Eustace McCulloch, who distributed his forces across the former US Army installations in Texas. One of McCulloch's officers, Major James Buckner Barry, stationed a portion of his command at Fort Phantom Hill.

Geographic entities mentioned:
surface_form: fort phantom hill
instance_of: Landform
countries: United States
coordinates: lat: 32.6433
lon: -99.6775
After a campaign against the Comanche in 1861 quieted the frontier, McCulloch's troops were sent to fight in the Trans-Mississippi theater as part of the 1st Texas Cavalry Regiment. They were replaced with the Frontier Regiment, who also encamped at Fort Phantom Hill and were also increasingly pulled away from the frontier as the war continued. Use as satellite post, 1871–1875.

Geographic entities mentioned:
surface_form: fort phantom hill
instance_of: Landform
countries: United States
coordinates: lat: 32.6433
lon: -99.6775
From 1869 until the end of the Red River War in 1875, Fort Phantom Hill's ruins were occupied several times by US Army troops as a subpost of Fort Griffin, established in 1867 along the Clear Fork of the Brazos. Civilian use.

Geographic entities mentioned:
surface_form: fort phantom hill
instance_of: Landform
countries: United States
coordinates: lat: 32.6433
lon: -99.6775
Civilian use. White settlement in what became Jones County, Texas, began in November 1851 with Fort Phantom Hill and an Indian agent named Jesse Stem, who operated a farmstead near the fort until he was killed by Tonkawa natives in February 1854.

Geographic entities mentioned:
surface_form: fort phantom hill
instance_of: Landform
countries: United States
coordinates: lat: 32.6433
lon: -99.6775
Jones County was established on February 1, 1858, and during the Civil War it suffered from raids by indigenous peoples that halted white settlement in the county for 15 years. After the Red River War, a settlement was formed on Fort Phantom Hill's grounds that primarily serviced buffalo hunters roaming the region.

Geographic entities mentioned:
surface_form: fort phantom hill
instance_of: Landform
countries: United States
coordinates: lat: 32.6433
lon: -99.6775
By 1900, the town had ceased to exist, though the fort continued to be inhabited until at least 1913. From July 1918 to August 1919, test wells were dug near the fort by the Fort Phantom Hill Oil Company following the discovery of oil to the south in 1915. Preservation.

Geographic entities mentioned:
surface_form: fort phantom hill
instance_of: Landform
countries: United States
coordinates: lat: 32.6433
lon: -99.6775
Preservation. In 1928, the grounds of Fort Phantom Hill were purchased by John Guitar, who then sold the land in 1969 to his grandson, Jim Alexander. Guitar's purchase of the fort attracted the attention of Carl Coke Rister, a historian, professor at Hardin-Simmons University, and secretary of the West Texas Historical Association, who wrote extensively about the fort to promote its preservation.

Geographic entities mentioned:
surface_form: fort phantom hill
instance_of: Landform
countries: United States
coordinates: lat: 32.6433
lon: -99.6775
, Fort Phantom Hill consists of three stone structures and 12 stone chimneys standing on a site. Four historical markers have been placed on the grounds of Fort Phantom Hill or its vicinity by the state of Texas. The first, placed in 1936, generally commemorated the fort and was replaced with another marker after the original disappeared in 2010.

Geographic entities mentioned:
surface_form: fort phantom hill
instance_of: Landform
countries: United States
coordinates: lat: 32.6433
lon: -99.6775
In 1851, General William G. Belknap, commander of the Seventh Military District—an area corresponding to the present states of Arkansas and Oklahoma—visited the Brazos River valley with Marcy to find locations for outposts. Belknap began construction of what became Fort Belknap, and identified a nearby tributary, Pecan Bayou, as ideal for a second post on the Brazos.

Geographic entities mentioned:
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
The commune is located in the northern part of Hunedoara County, about west of the town of Brad and northwest of the county seat, Deva, on the border with Arad County. It is traversed by the European route E79. Vața de Jos is situated in a hilly area northeast of the northeast of the, in the upper reaches of the Crișul Alb River.

Geographic entities mentioned:
surface_form: Crișul Alb River
instance_of: Watercourse
countries: Romania
Hungary
coordinates: lat: 46.700277777778
lon: 21.269166666667
Mount Ganos. Mount Ganos (), today known as Işıklar Dağı in Turkish, is a mountain in eastern Thrace, on the European side of modern-day Turkey. It rises up from the western shore of the Sea of Marmara. The mountain was home to Christian monks and ascetics during the Byzantine period.

Geographic entities mentioned:
surface_form: işıklar dağı
instance_of: Mountain
countries: Turkey
coordinates: lat: 40.83967
lon: 27.31832
surface_form: mount ganos
instance_of: Mountain
countries: Turkey
coordinates: lat: 40.83967
lon: 27.31832
Mount Ganos. Mount Ganos (), today known as Işıklar Dağı in Turkish, is a mountain in eastern Thrace, on the European side of modern-day Turkey. It rises up from the western shore of the Sea of Marmara. The mountain was home to Christian monks and ascetics during the Byzantine period.

Geographic entities mentioned:
surface_form: mount ganos
instance_of: Mountain
countries: Turkey
coordinates: lat: 40.83967
lon: 27.31832
Byzantine Christian monks and clergymen who lived on the mountain included Patriarch Athanasius I of Constantinople and Maximos of Kafsokalyvia. Geography. Mount Ganos is basically a small mountain range that runs northeast-southwest at an approximately 70° angle. Its length in this direction is about 35 km, its width ranges from about 8 to 11 km, and its summit is 924 m above sea level.

Geographic entities mentioned:
surface_form: mount ganos
instance_of: Mountain
countries: Turkey
coordinates: lat: 40.83967
lon: 27.31832
Its length in this direction is about 35 km, its width ranges from about 8 to 11 km, and its summit is 924 m above sea level. On the north side, Mount Ganos rises abruptly from the Thracian plain. To the east is the Sea of Marmara, where the northern edge of the undersea Tekirdağ Basin also rises up sharply to form Mount Ganos's eastern flank.

Geographic entities mentioned:
surface_form: mount ganos
instance_of: Mountain
countries: Turkey
coordinates: lat: 40.83967
lon: 27.31832
On the north side, Mount Ganos rises abruptly from the Thracian plain. To the east is the Sea of Marmara, where the northern edge of the undersea Tekirdağ Basin also rises up sharply to form Mount Ganos's eastern flank. The mountain's southwestern end falls away steeply toward the Gulf of Saros, with the slope in some places reaching up to 50°.

Geographic entities mentioned:
surface_form: mount ganos
instance_of: Mountain
countries: Turkey
coordinates: lat: 40.83967
lon: 27.31832
The mountain's southwestern end falls away steeply toward the Gulf of Saros, with the slope in some places reaching up to 50°. Ganos is a steep mountain — the average slope is 24%, and over half of the mountain's surface area has a slope between 10-40°. Two streams cut through Mount Ganos, flowing to the west. Climate. Generally, Mount Ganos has a semi-humid climate typical of the Marmara region.

Geographic entities mentioned:
surface_form: mount ganos
instance_of: Mountain
countries: Turkey
coordinates: lat: 40.83967
lon: 27.31832
Two streams cut through Mount Ganos, flowing to the west. Climate. Generally, Mount Ganos has a semi-humid climate typical of the Marmara region. Because of its altitude, the mountain experiences cooler temperatures and receives more rainfall than the plains below. Its average annual temperature is less than 10 °C and its average yearly rainfall is more than 1000 mm. Soil.

Geographic entities mentioned:
surface_form: mount ganos
instance_of: Mountain
countries: Turkey
coordinates: lat: 40.83967
lon: 27.31832
These conditions have led to the formation of various soil orders, including alfisols, andisols, entisols, inceptisols, and mollisols. Specific areas. To the northeast of Mount Ganos is the Naip Plain, a flat alluvial plain surrounding the Ana Dere river. The plain covers some 500 hectares. Geologically, this area was once a river estuary, and has now been filled in by river sedimentation.

Geographic entities mentioned:
surface_form: mount ganos
instance_of: Mountain
countries: Turkey
coordinates: lat: 40.83967
lon: 27.31832
Rapid erosion has taken place in one area in the upper Kavak River basin in the 21st century. Rills that formed around 2004 developed into gullies by 2011, and the rate of erosion has increased even more since then. Geology. Mount Ganos forms an area of &quot;anomalous&quot; uplift at the end of the Ganos Fault, which it runs parallel to. The mountain is primarily composed of sandstone and shale.

Geographic entities mentioned:
surface_form: mount ganos
instance_of: Mountain
countries: Turkey
coordinates: lat: 40.83967
lon: 27.31832
This process has been going on for at least the last 2 million years, and has resulted in the mountain being moved eastward by at least 40 km. Four major geological formations have been identified as making up Mount Ganos: the Gaziköy Formation (the oldest), the Keşan Formation, the Mezardere Formation, and then finally the Osmancık Formation (the youngest).

Geographic entities mentioned:
surface_form: mount ganos
instance_of: Mountain
countries: Turkey
coordinates: lat: 40.83967
lon: 27.31832
These formations are primarily exposed on the south side of the mountain. Ecology. Due to the prevailing Mediterranean climate, the plant species that grow on Mount Ganos are characteristic of the Mediterranean region. Wetlands. There are some wetland areas along ponds and streams, mainly in the vicinity of Yeniköy, Yazır and Işıklar.

Geographic entities mentioned:
surface_form: mount ganos
instance_of: Mountain
countries: Turkey
coordinates: lat: 40.83967
lon: 27.31832
Mariposa Creek. Mariposa Creek, originally called the Mariposa River'&quot;, is a creek that has its source in Mariposa County, California. It flows through the town of Mariposa then southwest through the Sierra foothills, into and across the San Joaquin Valley in Merced County, and empties the sloughs of the San Joaquin River south of the city of Merced. History.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Hilandar. The Hilandar Monastery (,,) is one of the twenty Eastern Orthodox monasteries in Mount Athos in Greece and the only Serbian Orthodox monastery there. It was founded in 1198 by two Serbs from the Grand Principality of Serbia, Stefan Nemanja (Saint Symeon) and his son Saint Sava. St.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Upon its foundation, the monastery became a focal point of the Serbian religious and cultural life, as well as assumed the role of &quot;the first Serbian university&quot;. It is ranked fourth in the Athonite hierarchy of 20 sovereign monasteries. It is regarded as the historical Serbian monastery on Mount Athos, traditionally inhabited by Serbian Orthodox monks.

Geographic entities mentioned:
surface_form: Athonite
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
The monastery was founded in 1198; prompted by the Mount Athos monastic community, Byzantine Emperor Alexios III Angelos (1195–1203) issued a golden sealed chrysobull donating the ancient monastery &quot;Helandaris,&quot; &quot;to the Serbs as an eternal gift...,&quot; thereby designating it, &quot;to serve the purpose of accepting the people of Serbian descent, who seek to pursue the monastic way of life, as monasteries belonging to Iberia and Amalfi endure on the Mount, exempt from any authority, including the authority of Protos.&quot; Hilandar was thereby handed over to Saint Sava and Saint Symeon with the mission of establishing and endowing a new monastery, elevated to the imperial rank.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
surface_form: Mount
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
The Nemanjić period and late Byzantine Empire. After the Fourth Crusade and Crusaders' sack of Constantinople in 1204, the whole Athos came under the Latin Occupation which exposed the Athonite monasteries to an unprecedented pillage. As a result, Saint Sava travelled to Serbia to secure more resources and support for the monastery.

Geographic entities mentioned:
surface_form: Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
King Dragutin also expanded proceeds to the monastery and land or metochion income. He participated in improving and reinforcing defensive fortifications. Following the end of the Latin Occupation of this part of Byzantium, a new wave of raids hit the monastic republic.

Geographic entities mentioned:
surface_form: monastic republic
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Following the end of the Latin Occupation of this part of Byzantium, a new wave of raids hit the monastic republic. In the early 14th century, pirate mercenaries of the Catalan Grand Company repeatedly raided the Holy Mountain, while looting and sacking numerous monasteries, stealing treasures and Christian relics, and terrorizing monks.

Geographic entities mentioned:
surface_form: Holy Mountain
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
In the early 14th century, pirate mercenaries of the Catalan Grand Company repeatedly raided the Holy Mountain, while looting and sacking numerous monasteries, stealing treasures and Christian relics, and terrorizing monks. Of the 300 monasteries and monastic communities on Athos, Hilandar was among only 35 that survived the violence of the first decade of the 14th century.

Geographic entities mentioned:
surface_form: Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
This is the period of Hilandar's greatest prosperity. The Emperor significantly supported the monastery and bequeathed a number of land possessions in Serbia and Greece to it. Ever since his reign (14th century) and until today, Hilandar owns one fifth of the entire landmass on Athos. In addition to the Emperor himself, Dusan's aristocracy also supported the monastery.

Geographic entities mentioned:
surface_form: Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Wisk'achani (Inquisivi-Loayza). Wisk'achani (Aymara &quot;wisk'acha&quot; a rodent, &quot;-ni&quot; a suffix to indicate ownership, &quot;the one with the viscacha&quot;, Hispanicized spelling &quot;Viscachani&quot;) is a mountain in the Bolivian Andes. It is located in the La Paz Department, Inquisivi Province, Ichoca Municipality, and in the Loayza Province, Yaco Municipality.

Geographic entities mentioned:
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.0397
lon: -67.3411
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.24444444
lon: -67.69694444
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.28833333
lon: -66.52972222
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6408
lon: -67.7108
surface_form: wisk'achani (inquisivi-loayza)
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.1519
lon: -67.3114
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.2631
lon: -66.8253
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.09388889
lon: -67.69277778
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.48055556
lon: -66.41166667
Wisk'achani (Inquisivi-Loayza). Wisk'achani (Aymara &quot;wisk'acha&quot; a rodent, &quot;-ni&quot; a suffix to indicate ownership, &quot;the one with the viscacha&quot;, Hispanicized spelling &quot;Viscachani&quot;) is a mountain in the Bolivian Andes. It is located in the La Paz Department, Inquisivi Province, Ichoca Municipality, and in the Loayza Province, Yaco Municipality.

Geographic entities mentioned:
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.0397
lon: -67.3411
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.24444444
lon: -67.69694444
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.28833333
lon: -66.52972222
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6408
lon: -67.7108
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.2631
lon: -66.8253
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.09388889
lon: -67.69277778
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.48055556
lon: -66.41166667
The ballcourt is located north of the acropolis with several residential groups in between. It is united by two causeways. The site's geologic context is volcanic; it is located just south of an active stratovolcano, Fuego volcano. The site contains monumental architecture in its acropolis as well as a probable sweatbath and obsidian workshops.

Geographic entities mentioned:
surface_form: Fuego volcano
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.474722222222
lon: -90.880833333333
The country's largest dolomite quarry is mined in Pugalo. Tourist attractions. Alcoy's Nug-as forest is the last rainforest of Cebu. It borders the town of Argao and is connected to the town's Lantoy Mountain. It is the home of the Black Shama (Copsychus Cebuensis), a local species of song bird in the family Muscicapidae that is only found in Cebu, where it is known locally as &quot;Siloy&quot;.

Geographic entities mentioned:
surface_form: Lantoy Mountain
instance_of: Mountain
countries: Philippines
coordinates: lat: 9.9833333333333
lon: 123.55305555556
Bernadotte had been hit six times, killing him almost instantaneously. The car was driven at full speed to Hadassah Hospital on Mount Scopus, but doctors there were unable to do anything for Bernadotte, who was bleeding profusely from his wounds. French Army Colonel André Serot, who had been sitting in the back seat next to Bernadotte, was also killed.

Geographic entities mentioned:
surface_form: Mount Scopus
instance_of: Mountain
countries: Israel
coordinates: lat: 31.7925
lon: 35.244166666667
Golden Hill (New York). Golden Hill is a mountain located in the Catskill Mountains of New York south of Kingston. Fly Mountain is located south-southwest, and Pink Hill is located southwest of Golden Hill.

Geographic entities mentioned:
surface_form: Fly Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.89176
lon: -74.0382
surface_form: pink hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.901111111111
lon: -74.045833333333
surface_form: golden hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.916388888889
lon: -74.019444444444
Golden Hill (New York). Golden Hill is a mountain located in the Catskill Mountains of New York south of Kingston. Fly Mountain is located south-southwest, and Pink Hill is located southwest of Golden Hill.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: golden hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.916388888889
lon: -74.019444444444
Golden Hill (New York). Golden Hill is a mountain located in the Catskill Mountains of New York south of Kingston. Fly Mountain is located south-southwest, and Pink Hill is located southwest of Golden Hill.

Geographic entities mentioned:
surface_form: golden hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.916388888889
lon: -74.019444444444
Twenty-dollar view. The view of Moraine Lake in Banff National Park from the top of the moraine rockpile is one of the most photographed locations in all of Canada. That view of the mountains behind the lake in Valley of the Ten Peaks is known as the Twenty-Dollar View, as Moraine Lake is featured on the backs of the 1969 and 1979 issues of the Canadian $20 note.

Geographic entities mentioned:
surface_form: Moraine Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
Twenty-dollar view. The view of Moraine Lake in Banff National Park from the top of the moraine rockpile is one of the most photographed locations in all of Canada. That view of the mountains behind the lake in Valley of the Ten Peaks is known as the Twenty-Dollar View, as Moraine Lake is featured on the backs of the 1969 and 1979 issues of the Canadian $20 note.

Geographic entities mentioned:
surface_form: Valley of the Ten Peaks
instance_of: Valley
countries: Canada
coordinates: lat: 51.3494444
lon: -116.1597222
Camp 4 Peak. Camp 4 Peak (also known as Research Mountain) is a mountain in the city and borough of Juneau, Alaska, United States. It is a part of the Boundary Ranges of the Coast Mountains in western North America. On the divide between East and West Twin Glaciers, it is located 5 miles north-northwest of Twin Glacier Lake and 27 miles northeast of the city of Juneau.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: camp 4 peak
instance_of: Mountain
countries: United States
coordinates: lat: 58.6117
lon: -133.954
Camp 4 Peak. Camp 4 Peak (also known as Research Mountain) is a mountain in the city and borough of Juneau, Alaska, United States. It is a part of the Boundary Ranges of the Coast Mountains in western North America. On the divide between East and West Twin Glaciers, it is located 5 miles north-northwest of Twin Glacier Lake and 27 miles northeast of the city of Juneau.

Geographic entities mentioned:
surface_form: camp 4 peak
instance_of: Mountain
countries: United States
coordinates: lat: 58.6117
lon: -133.954
It is a part of the Boundary Ranges of the Coast Mountains in western North America. On the divide between East and West Twin Glaciers, it is located 5 miles north-northwest of Twin Glacier Lake and 27 miles northeast of the city of Juneau. The peak was named by Maynard Miller after its use by the Juneau Icefield Research Program in 1965.

Geographic entities mentioned:
surface_form: glacier lake
instance_of: Lake
countries: United States
coordinates: lat: 47.4675
lon: -121.29611111111
This species grows to a length of SL. It lives only in streams of 1,200 meters (3,937 ft) above sea level. It was first studied and described by American ichthyologist H.M. Smith from type specimen were taken from Doi Luang Ang Ka (present-day Doi Inthanon)'s stream by Karen in December 1928. Later it was found in many streams as a branch of the Ping River in Chiang Mai Province.

Geographic entities mentioned:
surface_form: Doi Inthanon
instance_of: Mountain
countries: Thailand
coordinates: lat: 18.592222222222
lon: 98.486666666667
Short-headed sculpin. The short-headed sculpin (&quot;Cottinella boulengeri&quot;) ray-finned fish belonging to the family Cottidae, the typical sculpins. This species is endemic to Lake Baikal in Russia. It lives at depths of from, and is not longer than TL. This species is the only known member of its genus.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Yet, its enchanted nature has prevented anyone from laying hands upon it. The vicinity of Kundol Lake boasts numerous stunning attractions, including the Spinkhor Waterfall, Loypanghalay Lake, Desan Meadows, Katora Lake, Jaaz Banda, and Gabeen Lake. Location and trail to the lake.

Geographic entities mentioned:
surface_form: Katora Lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.3666
lon: 72.3464
surface_form: katora lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.3666
lon: 72.3464
surface_form: kundol lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.41888888888889
lon: 72.43305555555555
Kundol Lake. Kundol Lake (), also known as &quot;Kundol Dand&quot; and Kundal, is a lake in the Swat Valley of Khyber Pakhtunkhwa, Pakistan. It is located in the north of the Utror Valley. It is away from the Kalam Valley. A popular folktale surrounds the lake, claiming that every month, a golden bowl materializes at its center, shimmering like the moon.

Geographic entities mentioned:
surface_form: kundol dand
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.41888888888889
lon: 72.43305555555555
surface_form: kundol lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.41888888888889
lon: 72.43305555555555
Kundol Lake. Kundol Lake (), also known as &quot;Kundol Dand&quot; and Kundal, is a lake in the Swat Valley of Khyber Pakhtunkhwa, Pakistan. It is located in the north of the Utror Valley. It is away from the Kalam Valley. A popular folktale surrounds the lake, claiming that every month, a golden bowl materializes at its center, shimmering like the moon.

Geographic entities mentioned:
surface_form: kundol lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.41888888888889
lon: 72.43305555555555
The trail follows the stream and passes by forests and waterfalls. The mountains around the lake are covered by a thick blanket of vegetation. The banks of Kundol Lake serve as a camping site during the summer season for the trekkers. Kundol Lake is fed by melting glaciers and springs of the Hindu Kush. It gives rise to utror Khwar, the major right tributary of the Swat River. Access.

Geographic entities mentioned:
surface_form: kundol lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.41888888888889
lon: 72.43305555555555
surface_form: kundol lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.41888888888889
lon: 72.43305555555555
Kundol Lake. Kundol Lake (), also known as &quot;Kundol Dand&quot; and Kundal, is a lake in the Swat Valley of Khyber Pakhtunkhwa, Pakistan. It is located in the north of the Utror Valley. It is away from the Kalam Valley. A popular folktale surrounds the lake, claiming that every month, a golden bowl materializes at its center, shimmering like the moon.

Geographic entities mentioned:
surface_form: kalam valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.4801
lon: 72.5874
Kundol Lake lies in the lap of Hindu Kush mountains at an elevation of (9,950 ft), in the north of Utror, encompassed by snow-clad mountains and towering trees. The trail to the lake from Ladu is easy to follow as a large stream flows downwards from the lake, which merges with River Swat in the Kalam Valley. The trail follows the stream and passes by forests and waterfalls.

Geographic entities mentioned:
surface_form: kalam valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.4801
lon: 72.5874
Access. Kundol Lake is accessible only during summer. During winter, the roads are closed due to heavy snowfall. It can be accessed by an unpaved road from Kalam up to Utror in a four-wheel automotive where a link road ends in a green valley called Ladu in the foothills of the mountain. From Ladu it takes almost four to six hours to reach the lake.

Geographic entities mentioned:
surface_form: kalam
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.4801
lon: 72.5874
Location and trail to the lake. Kundol Lake lies in the lap of Hindu Kush mountains at an elevation of (9,950 ft), in the north of Utror, encompassed by snow-clad mountains and towering trees. The trail to the lake from Ladu is easy to follow as a large stream flows downwards from the lake, which merges with River Swat in the Kalam Valley.

Geographic entities mentioned:
surface_form: kush
instance_of: Mountain
countries: Pakistan
coordinates: lat: 28.8171
lon: 66.5674
The trail follows the stream and passes by forests and waterfalls. The mountains around the lake are covered by a thick blanket of vegetation. The banks of Kundol Lake serve as a camping site during the summer season for the trekkers. Kundol Lake is fed by melting glaciers and springs of the Hindu Kush. It gives rise to utror Khwar, the major right tributary of the Swat River. Access.

Geographic entities mentioned:
surface_form: kush
instance_of: Mountain
countries: Pakistan
coordinates: lat: 28.8171
lon: 66.5674
The road is almost entirely above 2000 metres altitude and so is only open from June 1 to October 31. It runs along the ridge that separates the Val Chisone and Susa valley and passes several mountain passes between these valleys including Colle dell'Assietta (2,474 m), Colle Blegier (2,381 m), Colle Costa Piana (2,313 m), Colle Bourget (2,299 m) and Col Basset (2,424 m).

Geographic entities mentioned:
surface_form: Val Chisone
instance_of: Valley
countries: Italy
coordinates: lat: 45.033
lon: 7.05
surface_form: Susa valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.133333333333
lon: 7.05
However, Leith later telegraphed his safe arrival in Cochrane, Ontario. Leith's early research focused on the geology of the Lake Superior region, including the ore deposits of the Mesabi range. He served as a consultant for the location and valuation of ore deposits for several mining companies and served as mineral adviser to the U.S.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Big Salmon River (New Brunswick). The Big Salmon River () is a small river in southern New Brunswick, Canada, that flows south into the Bay of Fundy. The river has its source to the southwest of Sussex, New Brunswick. The river flows into the Bay of Fundy near Fundy-St. Martins, and serves as the endpoint of the Fundy Trail. The 84m Big Salmon River Suspension Bridge crosses the river.

Geographic entities mentioned:
surface_form: big salmon river
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.4167
lon: -65.4
The river has its source to the southwest of Sussex, New Brunswick. The river flows into the Bay of Fundy near Fundy-St. Martins, and serves as the endpoint of the Fundy Trail. The 84m Big Salmon River Suspension Bridge crosses the river. It can be accessed by the Suspension Bridge Trail. This trail begins at the Fundy Trail Parkway parking area P8 near the Mitchell Franklin Bridge.

Geographic entities mentioned:
surface_form: big salmon river
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.4167
lon: -65.4
Active exploration began in 1951. In 1958, the Potash Company of America became the first potash producer in Canada with the commissioning of an underground potash mine at Patience Lake. As numerous potash producers in Canada developed, the Saskatchewan government became increasingly involved in the industry, leading to the creation of Canpotex in the 1970s.

Geographic entities mentioned:
surface_form: Patience Lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.1197
lon: -106.344
Devil's Thumb (Greenland). Devil's Thumb (,) is a pinnacle-shaped, mountain in the Avannaata municipality in northwestern Greenland. Geography. Devil's Thumb is located in the central part of Kullorsuaq Island, an island in the northern part of Upernavik Archipelago, in Melville Bay, approximately to the north of the Kullorsuaq settlement.

Geographic entities mentioned:
surface_form: devil's thumb
instance_of: Mountain
countries: Greenland
coordinates: lat: 74.5936
lon: -57.1411
Geography. Devil's Thumb is located in the central part of Kullorsuaq Island, an island in the northern part of Upernavik Archipelago, in Melville Bay, approximately to the north of the Kullorsuaq settlement. It is a familiar feature for Arctic navigators, similar to the Melville Monument further north, but bigger.

Geographic entities mentioned:
surface_form: devil's thumb
instance_of: Mountain
countries: Greenland
coordinates: lat: 74.5936
lon: -57.1411
In the 2016 Canadian Census, it recorded a population of 517 living in 173 of its 200 total private dwellings. In the same year, its Community Well-Being index was calculated at 56 of 100, compared to 58.4 for the average First Nations community and 77.5 for the average non-Indigenous community. The reserve is located on the south side of Pasqua Lake in the Qu'Appelle Valley. Land reductions.

Geographic entities mentioned:
surface_form: Pasqua Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.775
lon: -103.9925
Snæfell (Múlaþing). Snæfell (, &quot;snow mountain&quot;) at high, is an ice-capped stratovolcano located in the north-east part of Vatnajökull National Park, Iceland. While it has been dormant in the Holocene, it is now known to have had repose times of over 100,000 years between eruptions, so it cannot be assumed to be extinct. Geography.

Geographic entities mentioned:
surface_form: snæfell (múlaþing)
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.79716667
lon: -15.5755
surface_form: snæfell
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.8071204861
lon: -23.7762279203
Snæfell (Múlaþing). Snæfell (, &quot;snow mountain&quot;) at high, is an ice-capped stratovolcano located in the north-east part of Vatnajökull National Park, Iceland. While it has been dormant in the Holocene, it is now known to have had repose times of over 100,000 years between eruptions, so it cannot be assumed to be extinct. Geography.

Geographic entities mentioned:
surface_form: snæfell
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.79716667
lon: -15.5755
surface_form: snæfell
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.8071204861
lon: -23.7762279203
It is SW of Egilsstaðir by &quot;road&quot;. Geology. Snæfell is the northernmost central volcano in Iceland's off-rift Öræfi volcanic belt, which is regarded by some as an eastern flank zone to the northern volcanic zone. Mostly Snæfell was formed under ice cover.

Geographic entities mentioned:
surface_form: snæfell
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.79716667
lon: -15.5755
surface_form: snæfell
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.8071204861
lon: -23.7762279203
surface_form: öræfi
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.025436111111
lon: -16.642063888889
Mostly Snæfell was formed under ice cover. In addition to the main mountain, the Snæfell volcanic system has a series of fissures and smaller subglacial eruptive features, oriented in a south-west to north-east direction (27°), almost parallel to the active northern volcanic zone, which is to its west.

Geographic entities mentioned:
surface_form: snæfell
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.79716667
lon: -15.5755
surface_form: snæfell
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.8071204861
lon: -23.7762279203