Sarmila/GeoWiki-Features huggingface dataset:
Steve imposed strict rules on his son, got angry if he had other children in the house when he was not present, and particularly disliked young girls; Melissa said she never understood why her husband disliked girls. Eventually, Steve decided to relocate the family from Lehigh Valley, Pennsylvania to Florida, separating Phillips from his half-brothers Daniel and Benjie.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Pelican City, Oregon. Pelican City is an unincorporated community in Klamath County in the U.S. state of Oregon. It lies along U.S. Route 97 just north of the city of Klamath Falls near the south end of Upper Klamath Lake and the upstream end of the Link River. The community is named after the Pelican Bay Lumber Company, which had a mill here.

Geographic entities mentioned:
surface_form: Upper Klamath Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.392222222222
lon: -121.88027777778
The specific epithet (&quot;atrata&quot;) is a Latin word meaning &quot;dressed in black&quot;, referring to the dark bark. Distribution and habitat. Herberton ironbark grows in grassy woodland or forest in scattered locations on and near the Atherton Tableland in Queensland, especially in the area bounded by Herberton, Irvinebank and Mareeba. Conservation.

Geographic entities mentioned:
surface_form: Atherton Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
Reggello. Reggello is a &quot;comune&quot; (municipality) in the Metropolitan City of Florence in the Italian region of Tuscany, located about southeast of Florence, between the north-western side of Pratomagno and the Upper Valdarno. The municipality borders with Castel San Niccolò, Castelfranco Piandiscò, Figline e Incisa Valdarno, Montemignaio, Pelago, and Rignano sull'Arno. History.

Geographic entities mentioned:
surface_form: Pratomagno
instance_of: Mountain
countries: Italy
coordinates: lat: 43.65
lon: 11.65
surface_form: Valdarno
instance_of: Valley
countries: Italy
coordinates: lat: 43.566666666667
lon: 11.533333333333
By 1948, Hydro-Québec had started the expansion of the Beauharnois power station. It then set its eyes on the Bersimis near Forestville, on the North Shore of the Saint Lawrence River, located east of Montreal. The Bersimis-1 and Bersimis-2 generating stations were built between 1953 and 1959 and were widely considered to be a bench trial for the fledgling company.

Geographic entities mentioned:
surface_form: Bersimis
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.93333333
lon: -68.62222222
As &quot;Jerry&quot; Lane he also led a small dance band known as ' which toured the Midwest from the early 1920s into the 1940s. In the 1950s and 1960s he was a reporter and feature writer for a local newspaper in New York State's Mohawk Valley region. He also worked in sales for newspaper advertising.

Geographic entities mentioned:
surface_form: Mohawk Valley
instance_of: Valley
countries: United States
He knew there was a misunderstanding which could not be rectified, so he led his torpedo bombers into attack positions. At this point, Cmdr Fuchida's pilot, Lieutenant Mitsuo Matsuzaki, guided their bomber along with the remaining horizontal bombers in a formation sweep around Kaena Point and headed down the western coast of Oahu. At 07:53, Fuchida ordered Mizuki to send the code words &quot;Tora!

Geographic entities mentioned:
surface_form: Kaena Point
instance_of: Landform
countries: United States
coordinates: lat: 21.574392
lon: -158.2799327
Sambongsan (South Gyeongsang and South Jeolla). Sambongsan is a mountain of South Jeolla Province, southwestern South Korea. It has an elevation of 1,187 metres.

Geographic entities mentioned:
surface_form: sambongsan
instance_of: Mountain
countries: South Korea
surface_form: sambongsan (south gyeongsang and south jeolla)
instance_of: Mountain
countries: South Korea
surface_form: sambongsan
instance_of: Mountain
countries: South Korea
Sambongsan (South Gyeongsang and South Jeolla). Sambongsan is a mountain of South Jeolla Province, southwestern South Korea. It has an elevation of 1,187 metres.

Geographic entities mentioned:
surface_form: sambongsan
instance_of: Mountain
countries: South Korea
surface_form: sambongsan
instance_of: Mountain
countries: South Korea
surface_form: sambongsan
instance_of: Mountain
countries: South Korea
Blue Hills Ski Area. Blue Hills Ski Area is located on the western face of Great Blue Hill in Canton, Massachusetts. This land is part of the Blue Hills Reservation, a state park managed by the Massachusetts Department of Conservation and Recreation. Blue Hills has eight trails covering a vertical drop of.

Geographic entities mentioned:
surface_form: Great Blue Hill
instance_of: Mountain
countries: United States
coordinates: lat: 42.212044444444
lon: -71.115605555556
The 2006–07 season was the 6th year of a 6-year &quot;lease&quot; to the owners and operators of Ragged Mountain Resort in New Hampshire. In 2007, the management of Campgaw Mountain, located in northern New Jersey, started a 5-year lease. Currently, there is one double chairlift leading up the main slope and three beginner magic carpets
Operations. There are 12 trails: 6 green, 5 blue and 4 black.

Geographic entities mentioned:
surface_form: Campgaw Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0543
lon: -74.1993
During the 1967 Six-Day War Drori served as deputy commander of Golani's 51st Battalion and took part in fighting on the Golan Heights. During the subsequent War of Attrition he commanded Golani's 13th Battlation, participating in fighting on the Golan Heights, Beit She'an Valley, the Jordan Valley and along the Suez Canal.

Geographic entities mentioned:
surface_form: Beit She'an Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.4794
lon: 35.5058
This operation failed due to weather or fire. In 1835 he returned to Mifflin County and built a factory in the narrows of Kishacoquillas Creek (now Mann Narrows), at the base of Jacks Mountain between Reedsville and Yeagertown. Around 1840 a second shop was acquired in Yeagertown, mainly devoted to finishing of axe heads and making of other edge tools.

Geographic entities mentioned:
surface_form: Jacks Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.628611111111
lon: -77.631388888889
Kaufmann Peaks. Kaufmann Peaks is a 3,110 and 3,094 metre double summit mountain located on a ridge between the Howse River valley and Mistaya River valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. The nearest higher neighbor is Mount Sarbach, to the northwest, with Epaulette Mountain immediately to the southeast.

Geographic entities mentioned:
surface_form: Mount Sarbach
instance_of: Mountain
countries: Canada
coordinates: lat: 51.8927778
lon: -116.7680556
surface_form: Epaulette Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.865833333333335
lon: -116.735
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Kaufmann Peaks. Kaufmann Peaks is a 3,110 and 3,094 metre double summit mountain located on a ridge between the Howse River valley and Mistaya River valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. The nearest higher neighbor is Mount Sarbach, to the northwest, with Epaulette Mountain immediately to the southeast.

Geographic entities mentioned:
surface_form: kaufmann peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 51.88333333333333
lon: -116.75
Kaufmann Peaks. Kaufmann Peaks is a 3,110 and 3,094 metre double summit mountain located on a ridge between the Howse River valley and Mistaya River valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. The nearest higher neighbor is Mount Sarbach, to the northwest, with Epaulette Mountain immediately to the southeast.

Geographic entities mentioned:
surface_form: kaufmann peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 51.88333333333333
lon: -116.75
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mistaya
instance_of: Valley
countries: Canada
coordinates: lat: 51.9503
lon: -116.717
The nearest higher neighbor is Mount Sarbach, to the northwest, with Epaulette Mountain immediately to the southeast. Kaufmann Peaks is situated south of Saskatchewan Crossing, where the Icefields Parkway intersects with the David Thompson Highway. History.

Geographic entities mentioned:
surface_form: kaufmann peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 51.88333333333333
lon: -116.75
The &quot;North Peak&quot; (3,094 m) honors Christian Kaufmann (1872–1939) who completed 36 first ascents in the Canadian Rockies by making fifteen of those in 1901 and ten more in 1902. The two were half-brothers to Peter Kaufmann. The first ascent of Kaufmann Peaks was made in 1927 by D. Duncan and guide Ernest Feuz.

Geographic entities mentioned:
surface_form: kaufmann peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 51.88333333333333
lon: -116.75
Geology. Like other mountains in Banff Park, Kaufmann Peaks 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. A glacier shared with Mount Sarbach resides in the northeast cirque. Climate.

Geographic entities mentioned:
surface_form: kaufmann peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 51.88333333333333
lon: -116.75
A glacier shared with Mount Sarbach resides in the northeast cirque. Climate. Based on the Köppen climate classification, Kaufmann Peaks is located in a subarctic climate with cold, snowy winters, and mild summers. Winter temperatures can drop below -20 °C with wind chill factors below -30 °C.

Geographic entities mentioned:
surface_form: kaufmann peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 51.88333333333333
lon: -116.75
Climate. Based on the Köppen climate classification, Kaufmann Peaks is located in a subarctic climate with cold, snowy winters, and mild summers. Winter temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Kaufmann Peaks drains into the Mistaya River and Howse River which are both tributaries of the North Saskatchewan River.

Geographic entities mentioned:
surface_form: kaufmann peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 51.88333333333333
lon: -116.75
surface_form: mistaya
instance_of: Valley
countries: Canada
coordinates: lat: 51.9503
lon: -116.717
Geology. Like other mountains in Banff Park, Kaufmann Peaks 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. A glacier shared with Mount Sarbach resides in the northeast cirque. Climate.

Geographic entities mentioned:
surface_form: mount sarbach
instance_of: Mountain
countries: Canada
coordinates: lat: 51.8927778
lon: -116.7680556
Kaufmann Peaks is situated south of Saskatchewan Crossing, where the Icefields Parkway intersects with the David Thompson Highway. History. The &quot;South Peak&quot; (3,110 m) is named for Hans Kaufmann (1874–1930), the younger of two Swiss brothers who were popular mountain guides. Hans Kaufmann completed twelve first ascents in the Rockies during the years 1901 to 1904.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The first ascent of Kaufmann Peaks was made in 1927 by D. Duncan and guide Ernest Feuz. Recommended by James Outram in 1903, the mountain's toponym was officially adopted in 1920 by the Geographical Names Board of Canada. Geology. Like other mountains in Banff Park, Kaufmann Peaks is composed of sedimentary rock laid down during the Precambrian to Jurassic periods.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Łabski Szczyt. Łabski Szczyt or Violík (in Polish and Czech) () is a mountain peak located in the western Giant Mountains on the Czech-Polish border. The source of the Elbe (Labe) River, one of Europe's major rivers, is situated on the southern (Czech) slopes of the mountain. Situation.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
The source of the Elbe (Labe) River, one of Europe's major rivers, is situated on the southern (Czech) slopes of the mountain. Situation. In the main range this very distinct peak is situated between Szrenica (separated from it by Mokra Pass) and Śnieżne Kotły, the next peak eastwards being Wielki Szyszak. The summit is entirely on the Polish side. Tourism.

Geographic entities mentioned:
surface_form: Szrenica
instance_of: Mountain
countries: Poland
Czech Republic
coordinates: lat: 50.791388888889
lon: 15.514166666667
surface_form: Śnieżne Kotły
instance_of: Valley
countries: Poland
coordinates: lat: 50.7833
lon: 15.5667
surface_form: Wielki Szyszak
instance_of: Mountain
countries: Czech Republic
Poland
coordinates: lat: 50.7775
lon: 15.5675
Łabski Szczyt. Łabski Szczyt or Violík (in Polish and Czech) () is a mountain peak located in the western Giant Mountains on the Czech-Polish border. The source of the Elbe (Labe) River, one of Europe's major rivers, is situated on the southern (Czech) slopes of the mountain. Situation.

Geographic entities mentioned:
surface_form: łabski szczyt
instance_of: Mountain
countries: Czech Republic
Poland
coordinates: lat: 50.780556
lon: 15.545556
Łabski Szczyt. Łabski Szczyt or Violík (in Polish and Czech) () is a mountain peak located in the western Giant Mountains on the Czech-Polish border. The source of the Elbe (Labe) River, one of Europe's major rivers, is situated on the southern (Czech) slopes of the mountain. Situation.

Geographic entities mentioned:
surface_form: łabski szczyt
instance_of: Mountain
countries: Czech Republic
Poland
coordinates: lat: 50.780556
lon: 15.545556
surface_form: violík
instance_of: Mountain
countries: Czech Republic
Poland
coordinates: lat: 50.780556
lon: 15.545556
Several residents of East Kingston had petitioned Governor Belcher that its location was too distant from the Kingston school and place of worship. The town grew up around the saw and grist mill at the Trickling Falls on the edge of Powwow Pond. Farms prospered on the good soil, and ice-cutting in the Powwow River was a thriving winter business before the age of refrigeration.

Geographic entities mentioned:
surface_form: Powwow Pond
instance_of: Lake
countries: United States
coordinates: lat: 42.914166666667
lon: -71.035555555556
The southern half of East Kingston is drained by the Powwow River, a tributary of the Merrimack River, while the remainder is drained by Great Brook, a tributary of the Exeter River, which ultimately drains to the Atlantic Ocean via Great Bay. A very small portion of Powwow Pond on the Powwow River lies within the town.

Geographic entities mentioned:
surface_form: Powwow Pond
instance_of: Lake
countries: United States
coordinates: lat: 42.914166666667
lon: -71.035555555556
Jae Suh Park. Jae Suh Park (, born April 5, 1984) is an American actress who starred in the 2017 Netflix comedy series &quot;Friends from College&quot;. Personal life. Park grew up in Lodi, California. She is married to Randall Park, and they have one daughter. They live in the San Fernando Valley.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
&quot;The Washington Post&quot; noted that the &quot;no-name storm&quot; dumped three times as much rain on Louisiana as Hurricane Katrina. It dropped the equivalent of 7.1 trillion gallons of water or enough to fill Lake Pontchartrain about four times. Hurricane Katrina, by comparison, dumped about 2.3 trillion gallons of rainwater in the state (though more in other states).

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
On August 13, a flash flood emergency was issued for areas along the Amite and Comite rivers. By August 15, more than ten rivers (Amite, Vermilion, Calcasieu, Comite, Mermentau, Pearl, Tangipahoa, Tchefuncte, Tickfaw, and Bogue Chitto) and many more had reached a moderate, major, or record flood stage. Eight rivers reached record levels, including the Amite and Comite rivers.

Geographic entities mentioned:
surface_form: Tangipahoa
instance_of: Watercourse
countries: United States
coordinates: lat: 30.3367
lon: -90.2739
surface_form: Tchefuncte
instance_of: Watercourse
countries: United States
coordinates: lat: 30.3767
lon: -90.1606
In 2009, he appeared in the &quot;Red Riding&quot; trilogy as the malevolent John Dawson. He also appeared in ' (2010), playing the role of Zeus, the king of Mount Olympus and God of the sky, thunder, and lightning. Also, that year, Bean starred in &quot;Cash&quot;, playing the lead role of Pyke Kubic, a dangerous man determined to recover his wealth in a bad economy.

Geographic entities mentioned:
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
Manaca Iznaga Tower, Cuba. Iznaga Tower was the bell tower housing the slave bell of the Manaca sugar plantation in Valle de los Ingenios, in Trinidad, Cuba. It is an example of the bell towers that were a common feature on sugar plantations in Cuba, other notable examples are at Angerona and El Padre plantations located in present-day Cafetal del Padre in the Havana Province.

Geographic entities mentioned:
surface_form: Valle de los Ingenios
instance_of: Valley
countries: Cuba
coordinates: lat: 21.84138888888889
lon: -79.85805555555555
Kjelbotn Peak. 9qy3d6ysjtstygt1sh98wj1a1bh1" xml:space="preserve">#REDIRECT Sør Rondane Mountains

Geographic entities mentioned:
surface_form: kjelbotn peak
instance_of: Mountain
coordinates: lat: -72.2333
lon: 26.5667
Ccarhuarazo (Ayacucho). Ccarhuarazo (possibly from Quechua, &quot;qarwa&quot; leaf worm; larva of a beetle; pale, yellowish, golden, Ancash Quechua &quot;rasu&quot; snow, ice, mountain with snow, Hispanicized spellings &quot;Carhuaraso, Carhuarasu, Carhuarazo, Ccarhuaraso, Ccarhuarasu, Ccarhuarazo, Qarwarazo&quot;) is a volcano in the Andes of Peru, about 5,112 m (16,772 ft) high.

Geographic entities mentioned:
surface_form: ccarhuarazo (ayacucho)
instance_of: Mountain
countries: Peru
coordinates: lat: -14.33194444
lon: -73.75694444
Ccarhuarazo (Ayacucho). Ccarhuarazo (possibly from Quechua, &quot;qarwa&quot; leaf worm; larva of a beetle; pale, yellowish, golden, Ancash Quechua &quot;rasu&quot; snow, ice, mountain with snow, Hispanicized spellings &quot;Carhuaraso, Carhuarasu, Carhuarazo, Ccarhuaraso, Ccarhuarasu, Ccarhuarazo, Qarwarazo&quot;) is a volcano in the Andes of Peru, about 5,112 m (16,772 ft) high.

Geographic entities mentioned:
surface_form: ccarhuarazo
instance_of: Mountain
countries: Peru
coordinates: lat: -14.33194444
lon: -73.75694444
surface_form: ccarhuarazo
instance_of: Mountain
countries: Peru
coordinates: lat: -14.33194444
lon: -73.75694444
Personal life. In October 2003, Stearns married Mindy Burbano, who was an entertainment reporter for Entertainment Tonight and KTLA in Los Angeles. They live in Jackson Hole, Wyoming. In addition to Charlene, Stearns has three sons named Skyler, Colby, and Trevor and two daughters who often appear on Burbano's Instagram. Stearns also has two grandchildren.

Geographic entities mentioned:
surface_form: Jackson Hole
instance_of: Valley
countries: United States
coordinates: lat: 43.516666666667
lon: -110.83333333333
The schemes included aspects of the GWML including Cardiff to Swansea, the Midland Main Line from Kettering to Sheffield via Derby and Nottingham and Oxenholme to Windermere in the Lake District. In February 2018, the five-year plan was published by Network Rail with significant investment though much of this was for renewals and smaller projects rather than major projects.

Geographic entities mentioned:
surface_form: Windermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.358333333333
lon: -2.9361111111111
If this is so, &quot;Leopoldus Primus&quot; would have had a length of about and a width of almost. To get over the shoals in the river Elbe, the hull was probably built after the &quot;Rotterdam form&quot;. The ship was elaborately decorated with Baroque carvings and sculptures. The &quot;Leopoldus&quot; had 54 guns.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Operations and decommissioning. The success of &quot;Leopoldus Primus&quot; is supported by many reports. Captain Berend Jacobsen Karpfanger took her through a number of successful battles against pirates. One highlight is Karpfanger's defense against five French ships in the Elbe estuary on 11 September 1678. Fifty whaling ships were returning to Hamburg from Greenland when the frigates attacked.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
The name is derived from the Old English &quot;Tīges hōh&quot;, meaning &quot;spur of land belonging to the god Tiw&quot;, after whom Tuesday is named. Eilert Ekwall speculated: &quot;The etymology suggested is rendered likely by the fact that at Tysoe was a cut figure of a horse, after which the Vale of the Red Horse was named.

Geographic entities mentioned:
surface_form: Vale of the Red Horse
instance_of: Valley
countries: United Kingdom
coordinates: lat: 52.117
lon: -1.472
The Hornadays had one daughter, Helen. Hornaday died in Stamford, Connecticut and was buried at Putnam Cemetery in Greenwich, Connecticut. A year after his death, in 1938, at the suggestion of President Franklin Delano Roosevelt, the National Park Service named a peak, Mount Hornaday, in the Absaroka Range in Yellowstone National Park for him.

Geographic entities mentioned:
surface_form: Mount Hornaday
instance_of: Mountain
countries: United States
coordinates: lat: 44.945
lon: -110.146
Mic Mac AAC. Mic Mac Amateur Aquatic Club (MMAAC) is located on Lake Banook in Dartmouth, Nova Scotia, Canada. It provides structured recreational and competitive boating, and swimming programs to the local community, and summer day camp programs for children ages 6-12. The club is part of Canoe Kayak Canada and Rowing Canada.

Geographic entities mentioned:
surface_form: Lake Banook
instance_of: Lake
countries: Canada
coordinates: lat: 44.6809
lon: -63.5569
It is a dominant grass in a number of regions, such as shrubsteppe in Colorado and forest and woodland ecosystems in Arizona and New Mexico. In some areas, it is an indicator of climax status in sagebrush and pinyon-juniper woodland. It indicates true dry grassland in northern Alberta and pristine subalpine habitat on the Wasatch Plateau in Utah. In New Mexico it grows back quickly after wildfire.

Geographic entities mentioned:
surface_form: Wasatch Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 39.311666666667
lon: -111.33694444444
Other vernacular names include &quot;thunder pumper&quot;, &quot;bog bull&quot;, &quot;bog thumper&quot;, &quot;mire drum&quot;, and &quot;water belcher&quot;. Distribution and habitat. Its range includes much of North America. It breeds in southern Canada as far north as British Columbia, the Great Slave Lake and Hudson Bay, and in much of the United States and possibly central Mexico.

Geographic entities mentioned:
surface_form: Great Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 61.666666666667
lon: -114
They are also used in the printing trades to aid in setting movable type and in bookbinding. History. A small copper awl from a Tel Tsaf grave in Israel is currently the oldest metal object discovered in the Middle East. Awls were used by the Eastern and Middle Dakota (Sioux) and by the peoples of the Red River region, including the Red River Métis, Anishinabe, Plains Cree, and Salteaux.

Geographic entities mentioned:
surface_form: Red River region
instance_of: Valley
countries: Canada
United States
coordinates: lat: 49
lon: -97.5
Kutwal Lake. Kutwal Lake is a high-altitude lake located in the Haramosh valley of Gilgit district, in Gilgit-Baltistan, Pakistan. The valley of Haramosh is about 60 miles to the east of the district capital, Gilgit. The lake is surrounded by several high mountains, including Haramosh Peak, Laila Peak and Dobani Peak.

Geographic entities mentioned:
surface_form: Haramosh Peak
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.841388888889
lon: 74.897777777778
surface_form: Dobani Peak
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.95566
lon: 74.634205
surface_form: laila peak
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.10661944
lon: 74.46288333
surface_form: laila peak
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.59166666666667
lon: 76.41027777777778
surface_form: laila peak
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.95666667
lon: 74.9625
Kutwal Lake. Kutwal Lake is a high-altitude lake located in the Haramosh valley of Gilgit district, in Gilgit-Baltistan, Pakistan. The valley of Haramosh is about 60 miles to the east of the district capital, Gilgit. The lake is surrounded by several high mountains, including Haramosh Peak, Laila Peak and Dobani Peak.

Geographic entities mentioned:
surface_form: haramosh
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.841388888889
lon: 74.897777777778
surface_form: kutwal lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.89361111
lon: 74.88611111
Kutwal Lake. Kutwal Lake is a high-altitude lake located in the Haramosh valley of Gilgit district, in Gilgit-Baltistan, Pakistan. The valley of Haramosh is about 60 miles to the east of the district capital, Gilgit. The lake is surrounded by several high mountains, including Haramosh Peak, Laila Peak and Dobani Peak.

Geographic entities mentioned:
surface_form: haramosh
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.841388888889
lon: 74.897777777778
Kutwal Lake. Kutwal Lake is a high-altitude lake located in the Haramosh valley of Gilgit district, in Gilgit-Baltistan, Pakistan. The valley of Haramosh is about 60 miles to the east of the district capital, Gilgit. The lake is surrounded by several high mountains, including Haramosh Peak, Laila Peak and Dobani Peak.

Geographic entities mentioned:
surface_form: kutwal lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.89361111
lon: 74.88611111
Hollenfels Castle. Hollenfels Castle (Luxembourgish: &quot;Buerg Huelmes&quot;;; German: &quot;Burg Hollenfels&quot;), with a history dating back to the 11th century, is one of the castles located close to the River Eisch in the Valley of the Seven Castles in central Luxembourg. Today it is used as a centre for activities for young people, including a nearby youth hostel. Location.

Geographic entities mentioned:
surface_form: Valley of the Seven Castles
instance_of: Valley
countries: Luxembourg
coordinates: lat: 49.7
lon: 6.1
MacNaughton Mountain. MacNaughton Mountain is a mountain located in Essex County, New York, named after James MacNaughton (1851–1905), the grandson of Archibald McIntyre. The mountain is part of the Street Range of the Adirondack Mountains.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: macnaughton mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.1398
lon: -74.0643
MacNaughton Mountain. MacNaughton Mountain is a mountain located in Essex County, New York, named after James MacNaughton (1851–1905), the grandson of Archibald McIntyre. The mountain is part of the Street Range of the Adirondack Mountains.

Geographic entities mentioned:
surface_form: macnaughton mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.1398
lon: -74.0643
The mountain is part of the Street Range of the Adirondack Mountains. The western slopes and north end of MacNaughton Mountain drain into Preston Ponds and Duck Hole pond, the source of the Cold River, which drains into the Raquette River, the Saint Lawrence River in Canada, and into the Gulf of Saint Lawrence. The eastern slopes and south end of MacNaughton Mtn.

Geographic entities mentioned:
surface_form: macnaughton mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.1398
lon: -74.0643
drain into the southern Indian Pass Brook, thence into Henderson Lake, the source of the Hudson River, and into New York Bay. MacNaughton Mountain is within the High Peaks Wilderness Area of New York's Adirondack Park. According to early surveys, MacNaughton Mountain's elevation was, short of the 4,000 ft needed to qualify it as one of the Adirondack High Peaks.

Geographic entities mentioned:
surface_form: macnaughton mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.1398
lon: -74.0643
surface_form: high peaks
instance_of: Mountain
countries: United States
coordinates: lat: 45
lon: -70.4
MacNaughton Mountain is within the High Peaks Wilderness Area of New York's Adirondack Park. According to early surveys, MacNaughton Mountain's elevation was, short of the 4,000 ft needed to qualify it as one of the Adirondack High Peaks. According to the 1953 survey, the mountain &quot;did&quot; reach that height, while four of the 46 peaks on the list fell short.

Geographic entities mentioned:
surface_form: macnaughton mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.1398
lon: -74.0643
surface_form: high peaks
instance_of: Mountain
countries: United States
coordinates: lat: 45
lon: -70.4
The eastern slopes and south end of MacNaughton Mtn. drain into the southern Indian Pass Brook, thence into Henderson Lake, the source of the Hudson River, and into New York Bay. MacNaughton Mountain is within the High Peaks Wilderness Area of New York's Adirondack Park.

Geographic entities mentioned:
surface_form: henderson lake
instance_of: Lake
countries: United States
coordinates: lat: 44.0917
lon: -74.0667
Since then, a survey has measured the elevation at exactly. Because it is not one of the officially recognized Adirondack High Peaks and it does not offer notable views, MacNaughton is not climbed as frequently as many other mountains. There is no maintained trail or clear herd path for most of the climb from the end of the nearest trail at Wallface Pond.

Geographic entities mentioned:
surface_form: high peaks
instance_of: Mountain
countries: United States
coordinates: lat: 45
lon: -70.4
Musson Nunatak. gp5xe8duzu63t07izxe8sllzjuw" xml:space="preserve">#redirect Musson Nunatak

Geographic entities mentioned:
surface_form: musson nunatak
instance_of: Mountain
coordinates: lat: -71.5167
lon: -63.45
The topography of the Sahel is mainly flat; most of the region lies between in elevation. Several isolated plateaus and mountain ranges rise from the Sahel (e.g. Marrah Mountains, Aïr Mountains, Ennedi Plateau), but are designated as separate ecoregions because their flora and fauna are distinct from the surrounding lowlands (e.g. East Saharan woodlands).

Geographic entities mentioned:
surface_form: Ennedi Plateau
instance_of: Plateau
countries: Chad
coordinates: lat: 17
lon: 23
The course of the river flows entirely in O'Sullivan Township and in Albanel, Mistassini and Waconichi Lakes Wildlife Sanctuary. The hydrographic slope of the river is served by route 167, which is going north along the right shore of the Waconichi Lake and the river of the same name.

Geographic entities mentioned:
surface_form: Waconichi Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.153055555556
lon: -74.004444444444
It has a surface area of, and is located in the Pachuca Mountains, Hidalgo. Orography. The highland zone is in the Pachuca Mountain range. It is of volcanic origin and its limits split it north of the Valley of Mexico. This range is a southwestern extension of the Sierra Madre Oriental where it meets the Trans-Mexican Volcanic Belt. Elevations range between above sea level.

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
Lake Kero. Lake Kero is a medium-sized lake in Finland. It is situated in Kuusamo municipality in the Northern Ostrobothnia region, and it belongs to the Iijoki main catchment area. The southern part of the lake is called &quot;Iso-Kero&quot; and the northern part is called &quot;Keski-Kero&quot;.

Geographic entities mentioned:
surface_form: kero
instance_of: Lake
countries: Finland
coordinates: lat: 65.667322
lon: 29.157284
surface_form: lake kero
instance_of: Lake
countries: Finland
coordinates: lat: 65.667322
lon: 29.157284
Lake Kero. Lake Kero is a medium-sized lake in Finland. It is situated in Kuusamo municipality in the Northern Ostrobothnia region, and it belongs to the Iijoki main catchment area. The southern part of the lake is called &quot;Iso-Kero&quot; and the northern part is called &quot;Keski-Kero&quot;.

Geographic entities mentioned:
surface_form: kero
instance_of: Lake
countries: Finland
coordinates: lat: 65.667322
lon: 29.157284
surface_form: kero
instance_of: Lake
countries: Finland
coordinates: lat: 65.667322
lon: 29.157284
surface_form: iso-kero
instance_of: Lake
countries: Finland
coordinates: lat: 65.667322
lon: 29.157284
The first church in Øye was a wooden stave church that was built in the late 12th century, likely around the years 1180–1200. This church was located on the flat land along the shore of the lake Vangsmjøse, about northwest of the present Øye Church. This location was problematic over the years.

Geographic entities mentioned:
surface_form: Vangsmjøse
instance_of: Lake
countries: Norway
coordinates: lat: 61.162777777778
lon: 8.4416666666667
Camberwell, New South Wales. Camberwell is a small village just off the New England Highway in the Hunter Region of New South Wales, Australia. It is 196 kilometres north of Sydney and 15 kilometres northwest of Singleton in Singleton Shire. The village has an historic Anglican church, St Clements, which was opened in 1844. The area also has numerous open-cut mining operations.

Geographic entities mentioned:
surface_form: Hunter Region
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
The Aghlabids of Ifriqiya was a base for Saracen attacks along the Spanish East coast as well as against Southern Italy from the early 9th century; they attacked Rome in 845, Comacchio in 875-876, Monte Cassino in 882-83, and established the Emirate of Bari (847–871), the Emirate of Sicily (831–1091) and a base in Garigliano (882-906), which became bases of slave trade.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
Marine Corps Air Station Miramar contributed several aircraft as well as fire fighting trucks to operations based in Ramona. One of the larger airtankers, the Martin Mars, sent through a private contract from its home in Port Alberni, British Columbia on October 25, landing on Lake Elsinore in Riverside County, California. It has a 7,000 gallon capacity.

Geographic entities mentioned:
surface_form: Lake Elsinore
instance_of: Lake
countries: United States
coordinates: lat: 33.660069444444
lon: -117.35183888889
Mount Banoy. Mount Banoy (also known as Banoi) is a mountain in Batangas and the Calabarzon region, in the central part of the country, 100 km south of the city of Manila, the capital of the country, and in the island of Luzon in the Philippines. Mount Banoy is 960 meters above sea level, or 799 meters above the surrounding terrain. Its foothills are about 23.6 kilometers wide. Details.

Geographic entities mentioned:
surface_form: mount banoy
instance_of: Mountain
countries: Philippines
coordinates: lat: 13.696944444444
lon: 121.165
This change in composition geographically coincided with the volcanic activity crossing a lineament known as the Trotuș line. Volcano. Ciomadul is located in the southeastern Carpathians, at the end of the Călimani (Kelemen) – Gurghiu (Görgényi) – Harghita (Hargita) volcanic chain, and is also known as Csomád in Hungarian. The gorge of the Olt River separates Ciomadul from the Harghita Mountains.

Geographic entities mentioned:
surface_form: csomád
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
Cetății (Vár-tető), Vf. Comloș (Komlós-tető), Vf. Surduc (Szurdok-tető) and Dealul Mare southeast from the main complex. The central cluster of domes is elliptical and tectonic faults influenced their growth. The highest point of the complex is Ciomadul Mare (Nagy-Csomád) with an altitude of. Some domes were later affected by erosion, explosive activity or fumarolic alteration.

Geographic entities mentioned:
surface_form: csomád
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
Ciomadul. Ciomadul () is a dormant volcano in Romania. It is in the Eastern Carpathians, between the spa towns of Băile Tușnad and Balvanyos. Ciomadul lies at the southeastern end of the Carpathian volcanic chain and it is the youngest volcano of the Carpatho-Pannonian region.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
It is in the Eastern Carpathians, between the spa towns of Băile Tușnad and Balvanyos. Ciomadul lies at the southeastern end of the Carpathian volcanic chain and it is the youngest volcano of the Carpatho-Pannonian region. Ciomadul consists of several lava domes with two embedded explosion craters known as Mohoș and Sfânta Ana, the latter of which contains a crater lake, Lake Sfânta Ana.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
Ciomadul lies at the southeastern end of the Carpathian volcanic chain and it is the youngest volcano of the Carpatho-Pannonian region. Ciomadul consists of several lava domes with two embedded explosion craters known as Mohoș and Sfânta Ana, the latter of which contains a crater lake, Lake Sfânta Ana. The dominant volcanic rock at Ciomadul is potassium-rich dacite.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
Ciomadul consists of several lava domes with two embedded explosion craters known as Mohoș and Sfânta Ana, the latter of which contains a crater lake, Lake Sfânta Ana. The dominant volcanic rock at Ciomadul is potassium-rich dacite. Volcanic activity at Ciomadul commenced with effusive activity about one million years ago. Most of the volcano was constructed between 650,000 – 500,000 years ago.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
Most of the volcano was constructed between 650,000 – 500,000 years ago. Between 56,000 and 32,000 years ago explosive volcanic activity occurred at Ciomadul. Both the exact dates of the various eruptions and of the formation of the Sfânta Ana and Mohoș craters are unclear, partly because dates obtained by potassium-argon dating and other dating techniques deviate from each other.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
Some eruptions may have reached sub-Plinian strength, ejecting volcanic ash as far as the Black Sea. The last eruption took place between 32,600 and 27,500 years ago. Its date is likewise unclear. Ongoing seismic and geothermal activity, and exhalations of volcanic gas and evidence of a still existing magma chamber indicate that Ciomadul is a potentially active volcano. Regional setting.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
Volcanism in the region of Carpathia and Pannonia has been ongoing since 20 million years ago but has decreased during the Quaternary. No eruptions took place in the Holocene. The last volcanism occurred at Ciomadul in the last glacial age. Sparse basaltic volcanism has also taken place in the area, forming monogenetic volcanic fields. A volcanic arc lies in the Carpathians.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
This is part of the collision between the African Plate and the Eurasian Plate; subduction may still be underway in the area of the Carpathians. The, which is away from Ciomadul, features ongoing earthquake activity; deep earthquakes suggest that a remnant of a slab exists beneath the Vrancea Zone.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
The, which is away from Ciomadul, features ongoing earthquake activity; deep earthquakes suggest that a remnant of a slab exists beneath the Vrancea Zone. This tectonic setting may also be responsible for ongoing exhumation in the southeastern Carpathians, volcanism at Ciomadul and the Perșani volcanic field, south of Ciomad, which was concurrently active to the older Ciomadul activity.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
surface_form: ciomad
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
This tectonic setting may also be responsible for ongoing exhumation in the southeastern Carpathians, volcanism at Ciomadul and the Perșani volcanic field, south of Ciomad, which was concurrently active to the older Ciomadul activity. Other theories on Ciomadul's volcanic activity imply delamination of the lithosphere or roll-back of the subduction zone.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
This change in composition geographically coincided with the volcanic activity crossing a lineament known as the Trotuș line. Volcano. Ciomadul is located in the southeastern Carpathians, at the end of the Călimani (Kelemen) – Gurghiu (Görgényi) – Harghita (Hargita) volcanic chain, and is also known as Csomád in Hungarian. The gorge of the Olt River separates Ciomadul from the Harghita Mountains.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
The basement of the volcano is formed by flysch of Cretaceous age and by older volcanics; in some places volcanic rocks overlie fluvial deposits. Places around Ciomadul were first mentioned in 1349; the Saxon mineralogist Johann Ehrenwert Fichtel was the first to interpret it as a volcano, in 1780.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
Places around Ciomadul were first mentioned in 1349; the Saxon mineralogist Johann Ehrenwert Fichtel was the first to interpret it as a volcano, in 1780. The idea that Ciomadul could be a still active volcano was first proposed in the same year on the basis of its young appearance and the release of gas.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
These discoveries drew scholars and visitors to the volcano and the first scientific analysis of the volcano was published just eight years later. While a publication in 1964 postulated that the tuffs of Ciomadul were reworked Pliocene volcanites, the late Pleistocene age was established soon afterwards.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
The volcano is the youngest volcanic centre in the Carpathians and has a more rugged appearance than the surrounding mountains. Ciomadul is formed by a complex of lava domes and other volcanic material that form a south-tilting ridge that rises above the surrounding Lower Ciuk Basin. Individual lava domes form cone-shaped hills, which reach heights of and widths of.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
Both craters were formed by explosive eruptions and distinguishing between the deposits of both is difficult. The existence of an even larger crater with a diameter of has been suggested, encompassing both Sfânta Ana and Mohoș. Pyroclastic flow deposits generated by Ciomadul have been found on its northeastern, southern and western slopes. They reach a distance of as much as from the volcano.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
They reach a distance of as much as from the volcano. At Tușnad road, one of the flows has a thickness of. Tephra fall bed, lapilli, and surge deposits are also found, and the flow deposits contain pumice blocks. One lapilli layer, thick, from Ciomadul has been identified east of the volcano.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
Finally, volcanic erosion products and tephra occur all over the volcanic complex and up to east of it. Older volcanic centres extend northwest of Ciomadul. With increasing distance they are the 2.5—1.5 million-year-old Pilisca centre, the 2.8—2.2 million-year-old Cucu centre and the 4.3—3.6 million-year-old Luci-Lazu and Șumuleu-Ciuc volcanic centres.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
With increasing distance they are the 2.5—1.5 million-year-old Pilisca centre, the 2.8—2.2 million-year-old Cucu centre and the 4.3—3.6 million-year-old Luci-Lazu and Șumuleu-Ciuc volcanic centres. South of Ciomadul the Murgul shoshonites were erupted 2.3—1.5 million years ago; they represent cryptodomes. Andesite lava flows from Pilisca underlie the Ciomadul deposits in some places. Composition.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
Clots formed by various felsic crystals are common. The composition of Ciomadul's rocks has been fairly constant throughout its evolution albeit with two shifts 1 million and 650,000 years before present, and this diversity of its components indicate that the genesis of Ciomadul magmas involved mixing between felsic and mafic magma.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
These include amphibole, biotite, feldspar and zircon. The zircons formed almost continuously over hundred thousands of years within Ciomadul's magma chamber, indicating a steady crystallization of the chamber. Differences in magma temperature, crystal content and the participation of pre-existent crystal mushes determine whether an eruption will be effusive or explosive.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88