Sarmila/GeoWiki-Features huggingface dataset:
The law explicitly protects war monuments historically significant to the United States, the Confederacy of the United States, or the State of Georgia. Given this law, the removal of the carving on Stone Mountain has not been successful under current laws. In addition to its status as a historical monument, Stone Mountain has additional protection under Georgia state law.

Geographic entities mentioned:
surface_form: stone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.805944444444
lon: -84.145422222222
Given this law, the removal of the carving on Stone Mountain has not been successful under current laws. In addition to its status as a historical monument, Stone Mountain has additional protection under Georgia state law. Part 4 of Article 6 of Chapter 3 of Title 12 of the Official Code of Georgia still requires the SMMA to maintain Stone Mountain as a memorial to the confederacy.

Geographic entities mentioned:
surface_form: stone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.805944444444
lon: -84.145422222222
SMAC membership is a diverse coalition of concerned citizens, political leaders, community organizations, faith-based groups and businesses who are dedicated to supporting constructive solutions and ideas that reflect a new, shared vision for the Park.The coalition became active in 2020 with the objectives to create a more honest portrayal of the history of white supremacy associated with Stone Mountain, and to advance the offerings of the park to attract a broader range of visitors, improving the economic viability of the park.

Geographic entities mentioned:
surface_form: stone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.805944444444
lon: -84.145422222222
surface_form: stone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.805944444444
lon: -84.145422222222
Europeans first learned of the mountain in 1567, when Spanish explorers were told of a mountain farther inland which was &quot;very high, shining when the sun set like a fire.&quot; By this time, the Stone Mountain area was inhabited by the Creek and (to a lesser extent) Cherokee peoples. In the early 19th century, the area was known as Rock Mountain.

Geographic entities mentioned:
surface_form: stone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.805944444444
lon: -84.145422222222
Over the years, Stone Mountain granite was used in many buildings and structures, including the locks of the Panama Canal, the steps to the East Wing of the United States Capitol and the Imperial Hotel in Tokyo. In recent years, granite suppliers in Georgia sent stone samples cut from Stone Mountain to the group responsible for planning the Martin Luther King Jr.

Geographic entities mentioned:
surface_form: stone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.805944444444
lon: -84.145422222222
surface_form: stone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.805944444444
lon: -84.145422222222
In 1887, Stone Mountain was purchased for $45,000 by the Venable Brothers of Atlanta, who quarried the mountain for 24 more years, and descendants of the Venable family would retain ownership of the mountain until it was purchased by the State of Georgia in 1958. Martin Luther King Jr.

Geographic entities mentioned:
surface_form: stone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.805944444444
lon: -84.145422222222
The laser light show projects images of the Deep South as well as Georgia history onto the Confederate Memorial carving. During Memorial Day Weekend of 2011, Stone Mountain unveiled its overhaul of the laser show, dubbed Mountainvision, which incorporates digital projections, lasers, special effects, and pyrotechnics.

Geographic entities mentioned:
surface_form: stone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.805944444444
lon: -84.145422222222
Hawassa. Hawassa (; ʾäwasa, also spelled Awassa or Awasa) known historically as Adare is a city in Ethiopia, on the shores of Lake Hawassa in the Great Rift Valley. It is south of Addis Ababa via Bishoftu, east of Sodo, and north of Dilla. The town serves as the capital of the Sidama Region.

Geographic entities mentioned:
surface_form: Lake Hawassa
instance_of: Lake
countries: Ethiopia
coordinates: lat: 7.05
lon: 38.433333333333
It is a largely flat endorheic basin filled with mixed sand and clay deposits, as well as sandy alluvial sediments. There are numerous intermittent salt lakes and sors. The main lakes are Akzhaikyn and Ashchykol. In wet years the Chu river may reach lake Akzhaikyn at the eastern end and the Boktykaryn the Ashchykol lake. At the western end the Sarysu river usually ends in the Telikol lake.

Geographic entities mentioned:
surface_form: Ashchykol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 45.13828
lon: 67.28035
The main lakes are Akzhaikyn and Ashchykol. In wet years the Chu river may reach lake Akzhaikyn at the eastern end and the Boktykaryn the Ashchykol lake. At the western end the Sarysu river usually ends in the Telikol lake. The latter is located between the western limit of the Ashchykol Depression and the Daryaly takir plain further to the west. Flora.

Geographic entities mentioned:
surface_form: Telikol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 45.2
lon: 66.56666666666666
Parson, British Columbia. Parson is an unincorporated community on the east shore of the Columbia River, in the Columbia Valley region of southeastern British Columbia. The locality, on BC Highway 95, is by road about north of Cranbrook and southeast of Golden. Name origin. E.

Geographic entities mentioned:
surface_form: Columbia Valley
instance_of: Valley
countries: Canada
coordinates: lat: 51.0333
lon: -116.617
Kumano Sea. The Kumano Nada () is a body of water belonging to North Pacific Ocean (Philippine Sea) located off the coast of Kumano Region of the Kii Peninsula located in central Japan.

Geographic entities mentioned:
surface_form: kumano sea
instance_of: Body of water
countries: Japan
coordinates: lat: 33.7833
lon: 136.333
During this time, the bridges across the Pearl River were under construction due to the difficulty of the highway through the swamp. The proposed routing was planned to enter Louisiana just south of Picayune, follow the path of the Honey Island Swamp, and bypass Slidell to the east, while coming to Lake Pontchartrain.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
The northwest face of the Zwölferkogel falls around 500 metres into the &quot;Längental&quot; valley. To the east below the &quot;Finstertal&quot; is the &quot;Finstertalspeicher&quot;, a reservoir belonging to the Sellrain-Silz Power Station. To the south, along a sharp arête, are the &quot;Mittagsköpfe&quot; (), the &quot;Mittagsturm&quot; tower () and the Sulzkogel ().

Geographic entities mentioned:
surface_form: Sulzkogel
instance_of: Mountain
countries: Austria
coordinates: lat: 47.1821
lon: 11.0115
surface_form: sulzkogel
instance_of: Mountain
countries: Austria
coordinates: lat: 47.1821
lon: 11.0115
Zwölferkogel (Stubai Alps). The Zwölferkogel is a mountain, in the Stubai Alps in the Austrian state of Tyrol. Topography. The Zwölferkogel lies about 2.7 kilometres south of the winter sport resort of Kühtai. The northwest face of the Zwölferkogel falls around 500 metres into the &quot;Längental&quot; valley.

Geographic entities mentioned:
surface_form: stubai
instance_of: Valley
countries: Austria
coordinates: lat: 47.1667
lon: 11.3167
surface_form: zwölferkogel (stubai alps)
instance_of: Mountain
countries: Austria
coordinates: lat: 47.19028
lon: 11.01056
Zwölferkogel (Stubai Alps). The Zwölferkogel is a mountain, in the Stubai Alps in the Austrian state of Tyrol. Topography. The Zwölferkogel lies about 2.7 kilometres south of the winter sport resort of Kühtai. The northwest face of the Zwölferkogel falls around 500 metres into the &quot;Längental&quot; valley.

Geographic entities mentioned:
surface_form: stubai
instance_of: Valley
countries: Austria
coordinates: lat: 47.1667
lon: 11.3167
surface_form: zwölferkogel
instance_of: Mountain
countries: Austria
coordinates: lat: 47.19028
lon: 11.01056
Zwölferkogel (Stubai Alps). The Zwölferkogel is a mountain, in the Stubai Alps in the Austrian state of Tyrol. Topography. The Zwölferkogel lies about 2.7 kilometres south of the winter sport resort of Kühtai. The northwest face of the Zwölferkogel falls around 500 metres into the &quot;Längental&quot; valley.

Geographic entities mentioned:
surface_form: zwölferkogel
instance_of: Mountain
countries: Austria
coordinates: lat: 47.19028
lon: 11.01056
Topography. The Zwölferkogel lies about 2.7 kilometres south of the winter sport resort of Kühtai. The northwest face of the Zwölferkogel falls around 500 metres into the &quot;Längental&quot; valley. To the east below the &quot;Finstertal&quot; is the &quot;Finstertalspeicher&quot;, a reservoir belonging to the Sellrain-Silz Power Station.

Geographic entities mentioned:
surface_form: zwölferkogel
instance_of: Mountain
countries: Austria
coordinates: lat: 47.19028
lon: 11.01056
He was also director of the Vesuvius Observatory until the time of his death. Giuseppe Mercalli also observed eruptions of the volcanoes Stromboli and Vulcano in the Aeolian Islands. His descriptions of these eruptions became the basis for two indices of the volcanic explosivity index: 1 – Strombolian eruption, and 2 – Vulcanian eruption.

Geographic entities mentioned:
surface_form: Vulcano
instance_of: Mountain
countries: Italy
coordinates: lat: 38.4042
lon: 14.9658
In 2024, Back Asset Management AG and Back Beteiligungs AG were added. These companies are involved in investments in domestic and foreign companies, as well as providing advisory services to businesses. Personal life. Back and his family live in an apartment overlooking Lake Zurich, Switzerland, where they have been resident since 2007 and where he is legally domiciled.

Geographic entities mentioned:
surface_form: Lake Zurich
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2475
lon: 8.6775
Major General James Wilkinson's division of 8,000 was to concentrate at Sackett's Harbor on Lake Ontario, and proceed down the Saint Lawrence River in gunboats, batteaux and other small craft. At some point, they would rendezvous with a division of 4,000 under Major General Wade Hampton advancing north from Plattsburgh on Lake Champlain, to make the final attack on Montreal.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Major General James Wilkinson's division of 8,000 was to concentrate at Sackett's Harbor on Lake Ontario, and proceed down the Saint Lawrence River in gunboats, batteaux and other small craft. At some point, they would rendezvous with a division of 4,000 under Major General Wade Hampton advancing north from Plattsburgh on Lake Champlain, to make the final attack on Montreal.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Gray Peak (Yukon). Gray Peak is the unofficial name for the highest mountain of the Big Salmon Range in south-central Yukon, Canada, located north of Johnson's Crossing and south of Fox Mountain.

Geographic entities mentioned:
surface_form: big salmon
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.4167
lon: -65.4
surface_form: gray peak
instance_of: Mountain
countries: Canada
coordinates: lat: 61.1787
lon: -133.617
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
Gray Peak (Yukon). Gray Peak is the unofficial name for the highest mountain of the Big Salmon Range in south-central Yukon, Canada, located north of Johnson's Crossing and south of Fox Mountain.

Geographic entities mentioned:
surface_form: gray peak (yukon)
instance_of: Mountain
countries: Canada
coordinates: lat: 61.1787
lon: -133.617
Overview. Casino is the seat of the Richmond Valley Council, a local government area. Settlement of the area began in 1840 when pastoral squatters George Robert Stapleton and his business partner, Mr. Clay, set up a cattle station which they initially called Cassino after Cassino (near Monte Cassino) in Italy. The town now has a sister city agreement with the Italian village.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
Monte Fantino. The Monte Fantino is a mountain of the Ligurian Alps located in the Piedmont region of northwestern Italy. Geography. The mountain stands on the ridge dividing the small valleys of Rio Sbornina and Rio Sotto Crosa, both tributary of the Corsaglia.

Geographic entities mentioned:
surface_form: monte fantino
instance_of: Mountain
countries: Italy
coordinates: lat: 44.219624
lon: 7.7940256
The ridge starts from Cima della Brignola, descends till to the &quot;Bocchino della Brignola&quot; (2.276 m), rises again up to Cima Ferlette and follows with the del Punta Lusco (2.277 m) and Monte Fantino, ending at the confluence between the two streams, close to the &quot;Stalle Buroch&quot; (&quot;Buroch's stables&quot;). Monte Fantino summit is marked by a cross; its prominence is 161 m.

Geographic entities mentioned:
surface_form: monte fantino
instance_of: Mountain
countries: Italy
coordinates: lat: 44.219624
lon: 7.7940256
surface_form: monte fantino
instance_of: Mountain
countries: Italy
coordinates: lat: 44.219624
lon: 7.7940256
She plays for the India women's national kho kho team as a Wazir. She was part of the Indian women's team that won the inaugural Kho Kho World Cup held at New Delhi in January 2025. Early life and education. Devi is from Kharahal valley, Kullu district, Himachal Pradesh. She did her schooling at Government Senior Secondary School, Kharahal, where started playing kho kho.

Geographic entities mentioned:
surface_form: Kharahal
instance_of: Valley
countries: India
ExxonMobil announced it would be fully pulling out of Sakhalin-I in March 2022, in response to the 2022 Russian invasion of Ukraine. New Jersey wetlands. In 2004, the New Jersey Department of Environmental Protection sued ExxonMobil for $8.9 billion for lost wetland resources at Constable Hook in Bayonne and Bayway Refinery in Linden.

Geographic entities mentioned:
surface_form: Constable Hook
instance_of: Landform
countries: United States
coordinates: lat: 40.6578
lon: -74.0994
Acinetobacter lanii. &quot;Acinetobacter lanii&quot; is a Gram-negative, non-haemolytic and non-motile bacterium from the genus of &quot;Acinetobacter&quot; which has been isolated from the faeces of a Kiang from the Tibetan Plateau.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Valjean Hills. The Valjean Hills are a low mountain range in the eastern Mojave Desert, in northern San Bernardino County, southern California. They are located east of the Salt Spring Hills and southeastern Death Valley National Park, and west of Mount Charleston in the Spring Mountains.

Geographic entities mentioned:
surface_form: Mount Charleston
instance_of: Mountain
countries: United States
coordinates: lat: 36.271597222222
lon: -115.69556944444
Location. The nunatak is located at which is 1 km east of Atlantic Club Ridge, 1.2 km southeast of Sinemorets Hill, 2.8 km west by north of Castillo Nunatak, and 1 km north by east of the highest point of Charrúa Ridge. Krum Rock is named for Krum Velchev, meteorologist at St. Kliment Ohridski Base for several seasons since 1993.

Geographic entities mentioned:
surface_form: Sinemorets Hill
instance_of: Mountain
coordinates: lat: -62.6403
lon: -60.3617
surface_form: Castillo Nunatak
instance_of: Mountain
coordinates: lat: -62.6546
lon: -60.2928
The present name is in honor of the local Minford family. Physical geography. Minford is situated in rolling hills of the Appalachian Plateau and the Unglaciated Allegheny Plateau. These Appalachian foothills of southeastern Ohio, especially in nearby Shawnee State Park and Forest, have been nicknamed the &quot;Little Smokies&quot;. Rivers.

Geographic entities mentioned:
surface_form: Appalachian Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 40
lon: -78
Hatun K'irawniyuq. Hatun K'irawniyuq (Quechua &quot;hatun&quot; big, &quot;k'iraw&quot; cradle, bed of a child, &quot;-ni&quot;, &quot;-yuq&quot; suffixes, &quot;the one with a big cradle&quot; or &quot;the big one with a cradle&quot;, Hispanicized spelling &quot;Jatun Quirauniyoc&quot;) is a mountain in the Arequipa Region in the Andes of Peru, about high.

Geographic entities mentioned:
surface_form: hatun k'irawniyuq
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4433
lon: -72.7072
No. 2 Fighter Sector (2FS) was a Royal Australian Air Force (RAAF) unit formed at New Lambton, Newcastle, New South Wales on 25 February 1942. No. 2 Fighter Sector was responsible for fighter aircraft control and coordination for the Newcastle and Hunter Region. The RAAF commandeered New Lambton Public School at New Lambton for use as an operations and plotting facility on 9 March 1942.

Geographic entities mentioned:
surface_form: Hunter Region
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Pacific (1978 album). &quot;Pacific&quot; is a 1978 album featuring instrumental compositions by Japanese musicians Haruomi Hosono, Shigeru Suzuki and Tatsuro Yamashita. It is the first in the. The album shows a small island named Motu Fara that is part of the Avatoru Pass. Critical reception.

Geographic entities mentioned:
surface_form: Avatoru Pass
instance_of: Landform
countries: France
coordinates: lat: -14.943
lon: -147.712
Gravel Mountain. Gravel Mountain is a summit in Hinsdale County, Colorado, United States. It is located southeast of the community of Ouray, on land administered by the Bureau of Land Management. It is situated west of the Continental Divide in the San Juan Mountains which are a subrange of the Rocky Mountains.

Geographic entities mentioned:
surface_form: gravel mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.959722222222
lon: -107.54111111111
Climate. According to the Köppen climate classification system, Gravel Mountain is located in an alpine subarctic climate zone with cold, snowy winters, and cool to warm summers. Due to its altitude, it receives precipitation all year, as snow in winter, and as thunderstorms in summer, with a dry period in late spring.

Geographic entities mentioned:
surface_form: gravel mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.959722222222
lon: -107.54111111111
Mylna Cave. Mylna Cave () is a horizontal limestone karst cave located on the western slope of the Raptawicka Turnia massif, in the Kościeliska Valley of the Tatra Mountains, southern Poland, at an elevation of approximately 1,090 to 1,098 meters above sea level.

Geographic entities mentioned:
surface_form: Kościeliska Valley
instance_of: Valley
countries: Poland
coordinates: lat: 49.2539
lon: 19.8669
History. Immanuel College was founded by Pastor Georg Leidig in 1895 at Point Pass (north of Eudunda, east of the Clare Valley), before its subsequent move to North Adelaide in 1921. During WWII, the buildings were required by the air force, and the college was forced to temporarily move to North Walkerville for the period 1942–1946.

Geographic entities mentioned:
surface_form: Clare Valley
instance_of: Valley
countries: Australia
coordinates: lat: -33.83361111
lon: 138.61
However the town survived and was rebuilt. Falköping or Falbygden (when meaning the agricultural landscape in which Falköping is located) is widely known for its ancient remains of Stone Age, Bronze Age and Iron Age. The town is located between the two plateaus Mösseberg and Ålleberg. The location has been inhabited since the end of the ice age and cultivated by people for the last 6000 years.

Geographic entities mentioned:
surface_form: Ålleberg
instance_of: Mountain
countries: Sweden
coordinates: lat: 58.13350891461411
lon: 13.602797077392246
History. Los Baños Creek is reported to have taken its name from the pools, near its head, called &quot;Los Baños de Padre Arroyo&quot; for Padre Felipe Arroyo de la Cuesta, who was at Mission San Juan Bautista from 1808 to 1833 and conducted proselytizing missions into the San Joaquin Valley.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
El Arroyo de los Baños was a watering place on El Camino Viejo in the San Joaquin Valley between Arroyo de Quinto and Arroyo de San Luis Gonzaga. Los Baños de Padre Arroyo is registered as California Historical Landmark #550. Watershed. The Los Baños Creek mainstem has its source at the confluence of North Fork Los Banos Creek and South Fork Los Banos Creek.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Rivière-Nipissis. Rivière-Nipissis () is an unorganized territory in the Côte-Nord region of Quebec, Canada, part of the Sept-Rivières Regional County Municipality. The eponymous Nipissis River is a left tributary of the Moisie River, with its source north of Lake Siamois.

Geographic entities mentioned:
surface_form: Moisie River
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.2
lon: -66.0675
The river flows southeast through Huntingdon and continues to the small village of Ardenheim, where the Raystown Branch, the longest of the Juniata's tributaries, enters from the southwest. The Juniata continues southeast, through a gap in the Jacks Mountain ridge.

Geographic entities mentioned:
surface_form: Jacks Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.628611111111
lon: -77.631388888889
From Lewistown it flows southeast, in a winding course, receiving Tuscarora Creek from the south at the Port Royal river bridge and passing through a gap in the Tuscarora Mountain ridge. The Juniata River is joined by three creeks in Millerstown in northeast Perry County. It receives Cocolamus Creek southeast, Raccoon Creek southeast, and Wildcat Run southeast of Millerstown.

Geographic entities mentioned:
surface_form: Tuscarora Mountain
instance_of: Landform
countries: United States
coordinates: lat: 40.236666666667
lon: -77.738333333333
Hapush Mountain. Hapush Mountain is a long narrow mountain on Vancouver Island, British Columbia, Canada, located east of Woss and north of Mount Abel.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mount abel
instance_of: Mountain
countries: Canada
coordinates: lat: 50.2119
lon: -126.32
surface_form: hapush mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.2428
lon: -126.334
Hapush Mountain. Hapush Mountain is a long narrow mountain on Vancouver Island, British Columbia, Canada, located east of Woss and north of Mount Abel.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hapush mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.2428
lon: -126.334
After this, Ciccone was named in the startlist for the Tour de France. During the sixth stage to La Planche des Belles Filles, he was part of a breakaway which survived to the finish line. Ciccone managed to take over the race leader's yellow jersey from Julian Alaphilippe despite fading in the final metres of the climb.

Geographic entities mentioned:
surface_form: La Planche des Belles Filles
instance_of: Mountain
countries: France
coordinates: lat: 47.7672
lon: 6.77417
Lenne. The Lenne () is a tributary of the river Ruhr in the Sauerland hills, western Germany. It has caused flooding in recent years. Originating on top of the &quot;Kahler Asten&quot; near Winterberg in an intermittent spring at an elevation of, the Lenne ends after a course of 129 km flowing into the Ruhr river near the city of Hagen.

Geographic entities mentioned:
surface_form: Kahler Asten
instance_of: Mountain
countries: Germany
coordinates: lat: 51.179444444444
lon: 8.4888888888889
The summits are separated by a U-shaped crevice that gives them a prominent appearance. Geology. Mount Fee is one of the southernmost volcanoes in the Mount Cayley volcanic field. This volcanic zone forms the central portion of the larger Garibaldi Volcanic Belt, which extends from the Silverthrone Caldera in the north to the Watts Point volcano in the south.

Geographic entities mentioned:
surface_form: Mount Cayley volcanic field
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1203
lon: -123.291
surface_form: mount fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
The summits are separated by a U-shaped crevice that gives them a prominent appearance. Geology. Mount Fee is one of the southernmost volcanoes in the Mount Cayley volcanic field. This volcanic zone forms the central portion of the larger Garibaldi Volcanic Belt, which extends from the Silverthrone Caldera in the north to the Watts Point volcano in the south.

Geographic entities mentioned:
surface_form: Garibaldi Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5283
lon: -126.113
surface_form: Silverthrone Caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
surface_form: Watts Point volcano
instance_of: Mountain
countries: Canada
coordinates: lat: 49.65
lon: -123.21
The removal of the ejected volcanic material has exposed the dacite lava that forms the narrow north-south trending ridge of Mount Fee. The Black Tusk, a pinnacle of dark volcanic rock to the southeast, is also interpreted to be the remains of a deeply eroded volcano that was once covered with pyroclastic material.

Geographic entities mentioned:
surface_form: The Black Tusk
instance_of: Mountain
countries: Canada
coordinates: lat: 49.97527777777778
lon: -123.04277777777777
surface_form: black tusk
instance_of: Mountain
countries: Canada
coordinates: lat: 49.97527777777778
lon: -123.04277777777777
Habitation. Human habitation at Mount Fee extends from hundreds to thousands of years ago. Glassy volcanic rocks, such as rhyodacite, were widely used to make knives, chisels, adzes and other sharp tools before the arrival of Europeans in the 18th century. It was collected from a number of minor outcrops on the flanks of Mount Fee, as well as at Mount Cayley and Mount Callaghan.

Geographic entities mentioned:
surface_form: Mount Callaghan
instance_of: Mountain
countries: Canada
coordinates: lat: 50.2278
lon: -123.266
surface_form: mount fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
Subsequently, Mount Fee was one of the volcanoes in the Mount Cayley volcanic field illustrated by volcanologist Jack Souther in 1980. Others included Mount Cayley, Cauldron Dome, Slag Hill, Ember Ridge and Ring Mountain, which was titled &quot;Crucible Dome&quot; at the time.

Geographic entities mentioned:
surface_form: Cauldron Dome
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1556
lon: -123.319
surface_form: Slag Hill
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1834
lon: -123.3
surface_form: ring mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.2214
lon: -123.299
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Fee. Mount Fee is a volcanic peak in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. It is located south of Callaghan Lake and west of the resort town of Whistler. With a summit elevation of and a topographic prominence of, it rises above the surrounding rugged landscape on an alpine mountain ridge.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
This volcanic zone forms the central portion of the larger Garibaldi Volcanic Belt, which extends from the Silverthrone Caldera in the north to the Watts Point volcano in the south. The volcanic belt has formed as a result of ongoing subduction of the Juan de Fuca Plate under the North American Plate at the Cascadia subduction zone along the British Columbia Coast.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
The volcanic belt has formed as a result of ongoing subduction of the Juan de Fuca Plate under the North American Plate at the Cascadia subduction zone along the British Columbia Coast. This is a north-south trending fault zone about long, extending off the Pacific Northwest from Northern California to southwestern British Columbia.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
This material appears in goat hunting sites and at the Elaho rockshelter, collectively dated from about 100 to 8,000 years ago. In September 1928, Mount Fee was named by British mountaineer Tom Fyles after Charles Fee (1865–1927), who was a member of the British Columbia Mountaineering Club in Vancouver at the time.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
It might detect activity only once the volcano has started erupting. A significant eruption at Mount Fee would probably have considerable effects, particularly in a region like southwestern British Columbia where the Garibaldi Belt is located in a highly populated area.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
Eruptive history. Volcanic activity at Mount Fee is among the oldest in the Mount Cayley volcanic field. Its volcanic rocks remain undated, but the large amount of dissection and evidence of glacial ice overriding the volcano indicates that it formed more than 75,000 years ago before the Wisconsinan Glaciation.

Geographic entities mentioned:
surface_form: mount cayley volcanic field
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1203
lon: -123.291
surface_form: mount fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
In September 1928, Mount Fee was named by British mountaineer Tom Fyles after Charles Fee (1865–1927), who was a member of the British Columbia Mountaineering Club in Vancouver at the time. Subsequently, Mount Fee was one of the volcanoes in the Mount Cayley volcanic field illustrated by volcanologist Jack Souther in 1980.

Geographic entities mentioned:
surface_form: mount cayley volcanic field
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1203
lon: -123.291
surface_form: mount fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
Mount Fee. Mount Fee is a volcanic peak in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. It is located south of Callaghan Lake and west of the resort town of Whistler. With a summit elevation of and a topographic prominence of, it rises above the surrounding rugged landscape on an alpine mountain ridge.

Geographic entities mentioned:
surface_form: mount fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
With a summit elevation of and a topographic prominence of, it rises above the surrounding rugged landscape on an alpine mountain ridge. This mountain ridge represents the base of a north-south trending volcanic field which Mount Fee occupies. The mountain consists of a narrow north-south trending ridge of fine-grained volcanic rock and small amounts of fragmental material.

Geographic entities mentioned:
surface_form: mount fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The mountain consists of a narrow north-south trending ridge of fine-grained volcanic rock and small amounts of fragmental material. It is long and wide with nearly vertical flanks. Mount Fee has two main summits, the southern tower of which is the highest. The summits are separated by a U-shaped crevice that gives them a prominent appearance. Geology.

Geographic entities mentioned:
surface_form: mount fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
The plates move at a relative rate of over per year at an oblique angle to the subduction zone. The edifice of Mount Fee is the remains of a volcanic feature that has been significantly eroded by glacial ice. It likely represents a dissected stratovolcano (also known as a composite volcano) that was larger in area and higher in elevation than its current form.

Geographic entities mentioned:
surface_form: mount fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
During the glacial periods, much of the volcano's original outer cone of pyroclastic material was eroded away by moving layers of ice and rock. The removal of the ejected volcanic material has exposed the dacite lava that forms the narrow north-south trending ridge of Mount Fee.

Geographic entities mentioned:
surface_form: mount fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
The Black Tusk, a pinnacle of dark volcanic rock to the southeast, is also interpreted to be the remains of a deeply eroded volcano that was once covered with pyroclastic material. The present day edifice of Mount Fee contains several lava spines that reach heights of to above the main ridge. Eruptive history. Volcanic activity at Mount Fee is among the oldest in the Mount Cayley volcanic field.

Geographic entities mentioned:
surface_form: mount fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
As a result, the rocks comprising Mount Fee do not display evidence of interaction with glacial ice; the duration of volcanic events is unknown, and the exact timing of eruptive events is unknown. However, a large variety of volcanoes formed subglacially between 25,000 and 10,000 years ago in the vicinity of Mount Fee, including the lava domes of Ember Ridge to the south.

Geographic entities mentioned:
surface_form: mount fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
However, a large variety of volcanoes formed subglacially between 25,000 and 10,000 years ago in the vicinity of Mount Fee, including the lava domes of Ember Ridge to the south. At least three phases of eruptive activity have been recognized at Mount Fee. The only exposed remnant of Fee's earliest volcanic activity is a minor outcrop of pyroclastic rock.

Geographic entities mentioned:
surface_form: mount fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
The second volcanic event produced a sequence of volcanic rocks on Fee's eastern flank. This volcanic material was likely deposited when a sequence of lava flows and broken lava fragments erupted from a volcanic vent and moved down the flanks during the construction of the ancestral Mount Fee.

Geographic entities mentioned:
surface_form: mount fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
Following extensive dissection, renewed volcanism produced a viscous series of lavas on its northern flank. The U-shaped crevice separating the two main summits of Mount Fee separates this lava flow from the main volcanic ridge. The conduit from which these lava flows originated was likely vertical in structure and intruded through older rocks deposited during Fee's earlier volcanic events.

Geographic entities mentioned:
surface_form: mount fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
This volcanic event was also followed by a period of erosion, and likely one or more glacial periods. Extensive erosion following the last volcanic event at Mount Fee has created the rugged north-south trending ridge that currently forms a prominent landmark. Petrography. The dacite and rhyodacite rocks comprising Mount Fee contain up to 70% brown volcanic glass and up to 15% vesicles.

Geographic entities mentioned:
surface_form: mount fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
Petrography. The dacite and rhyodacite rocks comprising Mount Fee contain up to 70% brown volcanic glass and up to 15% vesicles. About 25% of the rocks contain crystal content, including plagioclase, hornblende, orthopyroxene, orthoclase and sporadic quartz. The orthoclase crystals are interpreted to represent rock fragments that became enveloped during hardening of the dacitic lavas.

Geographic entities mentioned:
surface_form: mount fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
The orthoclase crystals are interpreted to represent rock fragments that became enveloped during hardening of the dacitic lavas. A portion of the southwestern flank of Mount Fee comprises no volcanic glass, but rather composed of an abnormal cryptocrystalline matrix. This indicates that it might have developed as part of a subvolcanic intrusion. Habitation.

Geographic entities mentioned:
surface_form: mount fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
This indicates that it might have developed as part of a subvolcanic intrusion. Habitation. Human habitation at Mount Fee extends from hundreds to thousands of years ago. Glassy volcanic rocks, such as rhyodacite, were widely used to make knives, chisels, adzes and other sharp tools before the arrival of Europeans in the 18th century.

Geographic entities mentioned:
surface_form: mount fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
Monitoring. Like other volcanoes in the Garibaldi Belt, Mount Fee is not monitored closely enough by the Geological Survey of Canada to ascertain how active its magma chamber is. This is partly because no major eruptions have taken place in Canada for over a hundred years and the volcano is located in a remote region.

Geographic entities mentioned:
surface_form: mount fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
As a result, volcano monitoring is less important than dealing with other natural processes, such as tsunamis, earthquakes and landslides. No recent earthquakes are known to have occurred at Mount Fee. If it were to erupt there would likely be weeks, months or years of warning signs, such as clusters of minor earthquakes that would likely originate less than below the surface.

Geographic entities mentioned:
surface_form: mount fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
It is located south of Callaghan Lake and west of the resort town of Whistler. With a summit elevation of and a topographic prominence of, it rises above the surrounding rugged landscape on an alpine mountain ridge. This mountain ridge represents the base of a north-south trending volcanic field which Mount Fee occupies.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
This mountain ridge represents the base of a north-south trending volcanic field which Mount Fee occupies. The mountain consists of a narrow north-south trending ridge of fine-grained volcanic rock and small amounts of fragmental material. It is long and wide with nearly vertical flanks. Mount Fee has two main summits, the southern tower of which is the highest.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
They are generally too small to be felt by people, but the existing network of seismographs has been established to monitor tectonic earthquakes. However, the seismograph network is too far away to provide a good indication of what is happening under the mountain.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Teesta Khangtse Glacier. Teesta Khangtse Glacier or Tista Khangtse Glacier is located in the north of Sikkim, India, in a region bordering Tibet. This valley glacier is the primary source of the Teesta River. Location. The glacier is situated in the west of Pauhunri at and has a length of 12.88 kilometre.

Geographic entities mentioned:
surface_form: Pauhunri
instance_of: Mountain
countries: People's Republic of China
India
coordinates: lat: 27.953333333333
lon: 88.8425
It has a route of 372 m and a gradient of 8 m. The entrance is 885 m in height. It is in the Llor canal on the eastern side of Montcau (1,056 m) and at a distance of almost 400 m from the summit. It is a hypogean talveg of karst origin formed by conglomerate. The cave is part of a set of five systems that correspond to the same karst system.

Geographic entities mentioned:
surface_form: Montcau
instance_of: Mountain
countries: Spain
coordinates: lat: 41.6750412662
lon: 2.00462687673
Vern Clevenger. Vern Clevenger (born 1955 in Oakland, California) is a noted climber and landscape photographer. He made the first ascent of Cholatse in 1982. He lives in Mammoth Lakes, California with his wife and two children, Dylan and Sabrina. On April 13, 1977, Clevenger was arrested looting the crashed wreckage of a drug-smuggling airplane in Yosemite National Park.

Geographic entities mentioned:
surface_form: Cholatse
instance_of: Mountain
countries: Nepal
coordinates: lat: 27.92
lon: 86.76611111111112
In 1914 d'Albert moved to Zurich and became a Swiss citizen. He died in 1932 at the age of 67 in Riga, Latvia, where he had travelled for a divorce from his sixth wife. In the weeks preceding his death, d'Albert was the subject of attacks by the press in Riga concerning his personal life. D'Albert was buried in the cemetery overlooking Lake Lugano in Morcote, Switzerland. Recordings.

Geographic entities mentioned:
surface_form: Lake Lugano
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46
lon: 9
It is part of a lake and river system that has become a popular cruising sailboat destination. The river begins at the point where it flows out of Lake Izabal. At the entrance to the river there is a small Spanish colonial fort, the Castillo de San Felipe de Lara, built to stop pirates entering the lake from the Caribbean when this part of Central America was an important shipping staging point.

Geographic entities mentioned:
surface_form: Lake Izabal
instance_of: Lake
countries: Guatemala
coordinates: lat: 15.5
lon: -89.166666666667
At the entrance to the river there is a small Spanish colonial fort, the Castillo de San Felipe de Lara, built to stop pirates entering the lake from the Caribbean when this part of Central America was an important shipping staging point. Just after the river flows from Lake Izabal it is spanned by one of the biggest bridges in Central America.

Geographic entities mentioned:
surface_form: Lake Izabal
instance_of: Lake
countries: Guatemala
coordinates: lat: 15.5
lon: -89.166666666667
Dorothy Lake State Natural Area. Dorothy Lake State Natural Area is a Wisconsin Department of Natural Resources-designated State Natural Area featuring forested end moraine topography, with many steep-sided ridges and depressions. This results in a diverse mosaic of natural communities, including forests, swamps, fens, lakes, and streams. Location and access.

Geographic entities mentioned:
surface_form: dorothy lake
instance_of: Lake
countries: United States
coordinates: lat: 47.5864756
lon: -121.384297
surface_form: dorothy lake state natural area
instance_of: Lake
countries: United States
coordinates: lat: 45.22388889
lon: -91.30222222
This results in a diverse mosaic of natural communities, including forests, swamps, fens, lakes, and streams. Location and access. Dorothy Lake State Natural Area is located in northern Chippewa County approximately west of Holcombe. Access is via a forest trail off of Deer Fly Trail, approximately south of County Highway M. Description.

Geographic entities mentioned:
surface_form: dorothy lake
instance_of: Lake
countries: United States
coordinates: lat: 47.5864756
lon: -121.384297
surface_form: dorothy lake state natural area
instance_of: Lake
countries: United States
coordinates: lat: 45.22388889
lon: -91.30222222
Description. The namesake of the natural area, Dorothy Lake, is a 5.2 acre soft-water seepage lake, and contains a large, diverse assemblage of invertebrates, as well as three rare plant species. Three smaller, unnamed lakes surround Dorothy Lake, one of which contains a high-quality floating poor fen border.

Geographic entities mentioned:
surface_form: dorothy lake
instance_of: Lake
countries: United States
coordinates: lat: 47.5864756
lon: -121.384297
Uileacu de Beiuș () is a commune in Bihor County, Crișana, Romania. It is composed of four villages: Forău (&quot;Belényesforró&quot;), Prisaca (&quot;Gyepüpataka&quot;), Vălanii de Beiuș (&quot;Belényesvalány&quot;), and Uileacu de Beiuș. The commune is situated amid rolling hills, at an altitude of, on the banks of the river Crișul Negru and its tributaries, the Arman and the Săliște.

Geographic entities mentioned:
surface_form: Crișul Negru
instance_of: Watercourse
countries: Romania
Hungary
coordinates: lat: 46.700277777778
lon: 21.269166666667
History. Wadi Ara is part of the ancient historical route Via Maris, connecting what is now the Israeli coastal plain with the Jezreel Valley and, in a wider sense, Egypt in the west with Syria and Mesopotamia in the east. Chalcolithic. The site of En Esur has a main occupational level from the Early Chalcolithic period, when a large village with a temple stood at the well-watered site.

Geographic entities mentioned:
surface_form: Jezreel Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
Hydrology. The Panchganga River originates in the Western Ghats. It has five tributaries which supply the city and surroundings – the Bhogavati, Tulsi, Kumbhi, Kasari and Dhamani rivers. Kolhapur has a number of lakes. The Rankala Lake was once a stone quarry. The Kalamba lake was built in 1873. These two lakes provide the city with domestic potable water. Governance.

Geographic entities mentioned:
surface_form: Rankala Lake
instance_of: Lake
countries: India
coordinates: lat: 16.688586111111
lon: 74.211016666667
Schneefernerhaus. The Schneefernerhaus is a former hotel in the Alps, that is now used as an environmental research station. It lies immediately below the summit of the Zugspitze at a height of 2,650 m and was opened on 20 January 1931. It used to house the top station of the Bavarian Zugspitze Railway as well as a tourist hotel.

Geographic entities mentioned:
surface_form: Zugspitze
instance_of: Mountain
countries: Germany
Austria
coordinates: lat: 47.421217
lon: 10.986314