Sarmila/GeoWiki-Features huggingface dataset:
A lack of extant erosion shows that Mount Cleveland is likely a Holocene volcano, forming within the last 10,000 years. All known events have occurred at Mount Cleveland's summit vent, but there are at least five small andesite to dacite volcanic domes on the lower flanks. At times Cleveland has had a summit lava dome. The volcano has no caldera.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
At times Cleveland has had a summit lava dome. The volcano has no caldera. The eastern half of Chuginadak, to which Mount Cleveland is connected by a narrow isthmus, consists of several low-lying volcanic cones and two prominent peaks that have been heavily eroded, partly by glaciers. Known as the Tana volcanic complex, the two features measure and in elevation.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
Even today, not all possible events are confirmed as eruptions by the Alaska Volcano Observatory, and many are listed as &quot;possible.&quot; In observed history, Mount Cleveland may have first erupted in 1744; the first confirmed eruption occurred in 1828. The volcano erupted again in 1836 (possibly), 1893, 1897 (possibly), 1929 (possibly), 1932, and 1938 (possibly).

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
This eruption significantly disrupted air traffic in the area. On June 19, 2012, a pilot reported an ash-producing explosion on Mount Cleveland. Due to continuing seismic activity, the volcano was placed on the USGS Volcano Watch List in the orange or &quot;watch&quot; category the following day. AVO continues to keep Cleveland on the watch because of a persistent anomaly at the summit.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
The volcano erupted several times in 2014 and 2015, and a single explosion was detected by the AVO on April 16, 2016. In total the volcano has erupted at least 22 times in the last 230 years. Monitoring. Today, the Alaska Volcano Observatory monitors activity at Mount Cleveland using satellite imagery. Cloud cover often obscures the volcano, which makes many events difficult to follow.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
Overview. The map shows a hilly area with the Rajmahal hills running from the bank of the Ganges in the extreme north to south, beyond the area covered by the map into Dumka district. ‘Farakka’ is marked on the map and that is where Farakka Barrage is, just inside West Bengal. Rajmahal coalfield is shown in the map. The entire area is overwhelmingly rural with only small pockets of urbanisation.

Geographic entities mentioned:
surface_form: Rajmahal hills
instance_of: Mountain
countries: India
coordinates: lat: 25
lon: 87
Rodi Garganico. Rodi Garganico (; Garganico:) is a town and commune in the province of Foggia, Apulia, south-eastern Italy. Located on a promontory east of the Lago di Varano, it is part of the Gargano National Park and of the Mountain Community of Gargano.

Geographic entities mentioned:
surface_form: Lago di Varano
instance_of: Lake
countries: Italy
coordinates: lat: 41.879166666667
lon: 15.746111111111
Margaret Stewart was born in 1498. Her mother, Margaret Drummond was the daughter of Lord Drummond. The Spanish ambassador Pedro de Ayala reported that the king kept Margaret Drummond in great state in a castle, and afterwards had her married. There is no record of her marriage, but she was given the rents of land in Strathearn. Margaret Drummond died in 1502 and was buried at Dunblane Cathedral.

Geographic entities mentioned:
surface_form: Strathearn
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.3325
lon: -3.6825
La Carabassa. La Carabassa is a mountain in Catalonia, Spain. Located in the Pyrenees, it has an altitude of 2736 metres above sea level.

Geographic entities mentioned:
surface_form: la carabassa
instance_of: Mountain
countries: Spain
coordinates: lat: 42.4579797147
lon: 1.72717359885
Taschensee. Taschensee is a lake in Scharbeutz, Schleswig-Holstein, Germany. At an elevation of 22,18 m, its surface area is 0.4 km2.

Geographic entities mentioned:
surface_form: taschensee
instance_of: Lake
countries: Germany
coordinates: lat: 54.049166666667
lon: 10.706666666667
Plansee Group. The Plansee Group (named after Lake Plansee; company name: &quot;Plansee Holding AG)&quot; is an Austrian company based in Reutte that specialises in the powder metallurgical production of materials (molybdenum and tungsten) and in processing them into tools and moulded parts. The Plansee Group is a private company and is considered a global market leader. History.

Geographic entities mentioned:
surface_form: Lake Plansee
instance_of: Lake
countries: Austria
coordinates: lat: 47.469444
lon: 10.805556
Indira Col. __NOTOC__
Indira Col West () is a mountain pass at altitude on the Indira Ridge of Siachen Muztagh in Karakoram Range. It is on the border between Indian-controlled Siachen Glacier and the Chinese-controlled Trans-Karakoram Tract (both in the disputed Kashmir region), close to the tripoint of India, Pakistan, and China.

Geographic entities mentioned:
surface_form: Trans-Karakoram Tract
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 36.109089
lon: 76.646805
It is more difficult to ascend or descend on the north side controlled by China, but easier to do so from the south side controlled by India. India Saddle (Coord), a geographical saddle, connects the Indira Col East and Indira Col West. Indira Ridge separates the Chinese-controlled Trans-Karakoram Tract, which lies north of Indira Ridge, from the Siachen Glacier, which lies south of Indira Ridge.

Geographic entities mentioned:
surface_form: Trans-Karakoram Tract
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 36.109089
lon: 76.646805
Exploration. In 1889, British raj army officer and explorer Francis Younghusband reached the base of Turkestan La (North) from north side, and he noted that this was a long glacier and a major Central Asian dividing range. Colonel Narendra &quot;Bull&quot; Kumar reached Indira Col (the western col) in 1981.

Geographic entities mentioned:
surface_form: north side
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 36.109089
lon: 76.646805
It belongs to hotel division of the Sandoz Family Foundation. History. It was first constructed by the Bishop of Lausanne as a tower on the banks of Lake Léman around 1170. A century later, it was rebuilt and transformed into a fortified residence for bishops, particularly for Guillaume de Varax. It was also used as prison. The castle was abandoned and its tower reduced to ashes in 1609.

Geographic entities mentioned:
surface_form: Lake Léman
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
However, this diet has not been confirmed since neither behavioral observation nor analysis of its stomach contents has been possible. It has been found only at two widely separated localities in Malawi, Thumbi Island West at Cape Maclear and Nkhata Bay. It occurs in the deeper, rocky habitats of Lake Malawi, and is unknown in the aquarium trade.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
Riley ordered the election of representatives to a state constitutional convention, and handed over all civil authority to a governor and elected delegates at the end of 1849; the following year, California joined the U.S. as a state. He participated in the War of 1812 on Lake Ontario. He also served in the United States Army during the Seminole War in Florida, and Mexican–American War.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Riley volunteered for service in the War of 1812, and on 19 January 1813, he was appointed Ensign of Rifles. In March of the same year, he became a third lieutenant and in April 1814 a second lieutenant in the First Rifles. He saw action at Sackets Harbor, New York, in second of two battles for control of the shipyards on Lake Ontario. He gained a promotion to first lieutenant in March 1817.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Mount Bell is a summit in Alberta, Canada. Geography. Mount Bell is set within Banff National Park, in the Bow Range of the Canadian Rockies. The hamlet of Lake Louise is situated to the north and the Continental Divide is to the west. The nearest higher neighbor is Bident Mountain, to the west. Bident Mountain forms the west buttress of Consolation Pass with Mount Bell forming the east buttress.

Geographic entities mentioned:
surface_form: Bident Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.2875
lon: -116.14111111111112
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The hamlet of Lake Louise is situated to the north and the Continental Divide is to the west. The nearest higher neighbor is Bident Mountain, to the west. Bident Mountain forms the west buttress of Consolation Pass with Mount Bell forming the east buttress. These two peaks rise above the head of Consolation Valley. Precipitation runoff from Mount Bell drains into tributaries of the Bow River.

Geographic entities mentioned:
surface_form: Consolation Valley
instance_of: Valley
countries: Canada
coordinates: lat: 51.31669
lon: -116.15217
History. Originally called Mount Bellevue, the name was changed to honor Dr. Frederick Bell (1883–1971), a founding member of the Alpine Club of Canada and club president from 1926 through 1928. Mount Bell in British Columbia is also named after him. The mountain's toponym was officially adopted on April 3, 1952, by the Geographical Names Board of Canada.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount bell
instance_of: Mountain
countries: Canada
coordinates: lat: 51.284166666666664
lon: -116.10111111111111
Mount Bell (Alberta). Mount Bell is a summit in Alberta, Canada. Geography. Mount Bell is set within Banff National Park, in the Bow Range of the Canadian Rockies. The hamlet of Lake Louise is situated to the north and the Continental Divide is to the west. The nearest higher neighbor is Bident Mountain, to the west.

Geographic entities mentioned:
surface_form: mount bell (alberta)
instance_of: Mountain
countries: Canada
coordinates: lat: 51.284166666666664
lon: -116.10111111111111
Mount Bell (Alberta). Mount Bell is a summit in Alberta, Canada. Geography. Mount Bell is set within Banff National Park, in the Bow Range of the Canadian Rockies. The hamlet of Lake Louise is situated to the north and the Continental Divide is to the west. The nearest higher neighbor is Bident Mountain, to the west.

Geographic entities mentioned:
surface_form: mount bell
instance_of: Mountain
countries: Canada
coordinates: lat: 51.284166666666664
lon: -116.10111111111111
The hamlet of Lake Louise is situated to the north and the Continental Divide is to the west. The nearest higher neighbor is Bident Mountain, to the west. Bident Mountain forms the west buttress of Consolation Pass with Mount Bell forming the east buttress. These two peaks rise above the head of Consolation Valley. Precipitation runoff from Mount Bell drains into tributaries of the Bow River.

Geographic entities mentioned:
surface_form: mount bell
instance_of: Mountain
countries: Canada
coordinates: lat: 51.284166666666664
lon: -116.10111111111111
surface_form: bident mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.2875
lon: -116.14111111111112
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
These two peaks rise above the head of Consolation Valley. Precipitation runoff from Mount Bell drains into tributaries of the Bow River. Topographic relief is significant as the north aspect rises over above Taylor Lake in one kilometre (0.6 mile) and the south aspect rises above Boom Lake in two km (1.2 mile). The peak is visible from the Icefields Parkway to the east. History.

Geographic entities mentioned:
surface_form: mount bell
instance_of: Mountain
countries: Canada
coordinates: lat: 51.284166666666664
lon: -116.10111111111111
The first ascent of the summit was made in 1910 by an Alpine Club of Canada party including Nora Bell, sister of Frederick Bell. Geology. Like other mountains in Banff Park, Mount Bell 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.

Geographic entities mentioned:
surface_form: mount bell
instance_of: Mountain
countries: Canada
coordinates: lat: 51.284166666666664
lon: -116.10111111111111
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate. Based on the Köppen climate classification, Mount Bell is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below with wind chill factors below.

Geographic entities mentioned:
surface_form: mount bell
instance_of: Mountain
countries: Canada
coordinates: lat: 51.284166666666664
lon: -116.10111111111111
These two peaks rise above the head of Consolation Valley. Precipitation runoff from Mount Bell drains into tributaries of the Bow River. Topographic relief is significant as the north aspect rises over above Taylor Lake in one kilometre (0.6 mile) and the south aspect rises above Boom Lake in two km (1.2 mile). The peak is visible from the Icefields Parkway to the east. History.

Geographic entities mentioned:
surface_form: taylor lake
instance_of: Lake
countries: Canada
coordinates: lat: 56.05009
lon: -108.70073
Mount Bell in British Columbia is also named after him. The mountain's toponym was officially adopted on April 3, 1952, by the Geographical Names Board of Canada. The first ascent of the summit was made in 1910 by an Alpine Club of Canada party including Nora Bell, sister of Frederick Bell. Geology.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Black River Island. Black River Island is an island in Lake Huron. It is part of a series of shoals around the mouth of Black River and is northeast of it. The island is included within the unincorporated community of Black River in Alcona Township, Michigan. The uninhabited rocky island is about long. Its area is less than and varies with lake levels. The shoals in the area are a boating hazard.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Its name originates from the Slavic name &quot;Bukow&quot;. &quot;Buk&quot; means &quot;beech&quot; in Polish. Geography. Buckau lies directly on the river Elbe opposite the southern part of the Rotehorn Landscape Park. To the north, on the roads of Erich-Weinert-Straße and Schönebecker Straße towards Harnackstraße and Steubenallee is Magdeburg’s old town, the Altstadt.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
The so-called &quot;natural shopping center&quot; consists of the activities in the city center. Tourism. Near Avezzano there are parks, valleys, cities and the natural environment of the Abruzzi mountains: National Park of Abruzzo, Lazio and Molise, Sirente-Velino Regional Park, Fucino plain, Mount Velino, Ovindoli, Tagliacozzo, Giovenco valley, Roveto valley and Cavaliere plain. Sports.

Geographic entities mentioned:
surface_form: Mount Velino
instance_of: Mountain
countries: Italy
coordinates: lat: 42.15
lon: 13.366666666667
The field marshal never spared himself, bivouacking in the snow with his men, and Carlyle records that private soldiers made rough shelters over him as he slept. He actually reached the Elbe at Schandau, but as the Saxons were unable to break out, von Browne retired, having succeeded, however, in delaying the development of Frederick's operations for a whole campaign.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Mount Baker. Mount Baker (;), also known as Koma Kulshan or simply Kulshan, is a active glacier-covered andesitic stratovolcano in the Cascade Volcanic Arc and the North Cascades of Washington State in the United States. Mount Baker has the second-most thermally active crater in the Cascade Range after Mount St. Helens.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: st. helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Older volcanic edifices have mostly eroded away due to glaciation. After Mount Rainier, Mount Baker has the heaviest glacier cover of the Cascade Range volcanoes; the volume of snow and ice on Mount Baker, is greater than that of all the other Cascades volcanoes (except Rainier) combined.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
It is also one of the snowiest places in the world; in 1999, Mount Baker Ski Area, located to the northeast, set the world record for recorded snowfall in a single season—. Mount Baker is the third-highest mountain in Washington and the fifth-highest in the Cascade Range, if Little Tahoma Peak, a subpeak of Mount Rainier, and Shastina, a subpeak of Mount Shasta, are not counted.

Geographic entities mentioned:
surface_form: Little Tahoma Peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.8496
lon: -121.712
surface_form: Shastina
instance_of: Mountain
countries: United States
coordinates: lat: 41.409041666667
lon: -122.22362222222
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: mount rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: tahoma
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
Geology. The present-day cone of Mount Baker is relatively young, perhaps less than 100,000 years old. The volcano sits atop a similar older volcanic cone called Black Buttes, which was active between 500,000 and 300,000 years ago.

Geographic entities mentioned:
surface_form: Black Buttes
instance_of: Landform
countries: United States
coordinates: lat: 48.7693
lon: -121.853
Volcanic rocks of Mount Baker and Black Buttes rest on a foundation of non-volcanic rocks. Deposits recording the last 14,000 years at Mount Baker indicate that Mount Baker has not had highly explosive eruptions like those of other volcanoes in the Cascade Volcanic Arc, such as Mount St. Helens, Glacier Peak, or the Mount Meager massif, nor has it erupted frequently.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: Glacier Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: mount st. helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: st. helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.14972222
lon: -109.84944444
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.155013
lon: -117.293429
The pale-colored rocks northeast of the modern volcano mark the site of the ancient (1.15  million years old) Kulshan caldera that collapsed after an enormous ash eruption one million years ago. Subsequently, eruptions in the Mount Baker area have produced cones and lava flows of andesite, the rock that constitutes much of the other Cascade Range volcanoes such as Rainier, Adams, and Hood.

Geographic entities mentioned:
surface_form: Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
surface_form: rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: adams
instance_of: Mountain
countries: United States
coordinates: lat: 46.202411111111
lon: -121.49089444444
surface_form: hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
From about 900,000  years ago to the present, numerous andesitic volcanic centers in the area have come and disappeared through glacial erosion. The largest of these cones is the Black Buttes edifice, active between 500,000 and 300,000  years ago and formerly bigger than today's Mount Baker. Modern craters and cone.

Geographic entities mentioned:
surface_form: Black Buttes
instance_of: Landform
countries: United States
coordinates: lat: 48.7693
lon: -121.853
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
The Nooksack, who live in the closest proximity to the north face of the mountain, have multiple names for different areas of the mountain. The name, meaning &quot;white mountain,&quot; refers to Mount Baker as a whole, and specifically, to the glacier-covered summit above 7,000 feet. The open slopes of Mt.

Geographic entities mentioned:
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.94687
lon: -119.3096
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.040555555556
lon: -121.15305555556
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5781
lon: -109.32
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.67648
lon: -123.32823
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.0030248
lon: -111.4687966
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.634166666667
lon: -118.25555555556
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.9555
lon: -110.735
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.57476
lon: -114.49565
Reports of flooding on the Skagit River from the eruption are, however, probably greatly exaggerated. A short time later, two collapses of the east side of Sherman Crater produced two lahars, the first and larger of which flowed into the natural Baker Lake, increasing its level by at least. The location of the 19th-century lake is now covered by waters of the modern dam-impounded Baker Lake.

Geographic entities mentioned:
surface_form: baker lake
instance_of: Lake
countries: United States
coordinates: lat: 47.3515175
lon: -121.3017165
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: baker lake
instance_of: Lake
countries: United States
coordinates: lat: 40.6481
lon: -121.376
All retreated during the first half of the century, advanced from 1950 to 1975 and have been retreating with increasing rapidity since 1980. Mount Baker is drained on the north by streams that flow into the North Fork Nooksack River, on the west by the Middle Fork Nooksack River, and on the southeast and east by tributaries of the Baker River.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Located in the Mount Baker Wilderness, it is visible from much of Greater Victoria, Nanaimo, and Greater Vancouver in British Columbia, and to the south, from Seattle (and on clear days Tacoma) in Washington. Indigenous peoples have known the mountain for thousands of years, but the first written record of the mountain is from Spanish explorer Gonzalo Lopez de Haro, who mapped it in 1790 as '.

Geographic entities mentioned:
surface_form: tacoma
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Mount Baker. Mount Baker (;), also known as Koma Kulshan or simply Kulshan, is a active glacier-covered andesitic stratovolcano in the Cascade Volcanic Arc and the North Cascades of Washington State in the United States. Mount Baker has the second-most thermally active crater in the Cascade Range after Mount St. Helens.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: kulshan
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: kulshan
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: koma kulshan
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
In the language of the unidentified &quot;Koma tribe,&quot; the name is &quot;Tukullum&quot; or &quot;Nahcullum.&quot;
The first Europeans to see and name the mountain were the Spanish. Gonzalo Lopez de Haro was the first European to record the mountain, calling it ', meaning &quot;Great Mount Carmel&quot;. The current English name for the mountain, Mount Baker, was chosen by George Vancouver.

Geographic entities mentioned:
surface_form: mount carmel
instance_of: Mountain
countries: United States
coordinates: lat: 41.430636
lon: -72.890767
Mount Baker. Mount Baker (;), also known as Koma Kulshan or simply Kulshan, is a active glacier-covered andesitic stratovolcano in the Cascade Volcanic Arc and the North Cascades of Washington State in the United States. Mount Baker has the second-most thermally active crater in the Cascade Range after Mount St. Helens.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Helens. About due east of the city of Bellingham, Whatcom County, Mount Baker is the youngest volcano in the Mount Baker volcanic field. While volcanism has persisted here for some 1.5 million years, the current volcanic cone is likely no more than 140,000 years old, and possibly no older than 80–90,000 years. Older volcanic edifices have mostly eroded away due to glaciation.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
After Mount Rainier, Mount Baker has the heaviest glacier cover of the Cascade Range volcanoes; the volume of snow and ice on Mount Baker, is greater than that of all the other Cascades volcanoes (except Rainier) combined. It is also one of the snowiest places in the world; in 1999, Mount Baker Ski Area, located to the northeast, set the world record for recorded snowfall in a single season—.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Indigenous peoples have known the mountain for thousands of years, but the first written record of the mountain is from Spanish explorer Gonzalo Lopez de Haro, who mapped it in 1790 as '. The explorer George Vancouver later named the mountain for 3rd Lieutenant Joseph Baker of HMS &quot;Discovery&quot;, who saw it on April 30, 1792. Name and etymology.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
The name, meaning &quot;white mountain,&quot; refers to Mount Baker as a whole, and specifically, to the glacier-covered summit above 7,000 feet. The open slopes of Mt. Baker, between about 5,000 feet and 7,000 feet, are known as, meaning &quot;shooting place,&quot; referring to the act of going hunting up on the slopes.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Gonzalo Lopez de Haro was the first European to record the mountain, calling it ', meaning &quot;Great Mount Carmel&quot;. The current English name for the mountain, Mount Baker, was chosen by George Vancouver. Vancouver named the mountain for 3rd Lieutenant Joseph Baker of HMS &quot;Discovery&quot;, who saw it on April 30, 1792.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
The current English name for the mountain, Mount Baker, was chosen by George Vancouver. Vancouver named the mountain for 3rd Lieutenant Joseph Baker of HMS &quot;Discovery&quot;, who saw it on April 30, 1792. Mount Baker is sometimes also known by the alternative English name &quot;Kulshan&quot; which is the Anglicized form of the Nooksack name.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Accompanying Quimper was first-pilot Gonzalo Lopez de Haro, who drew detailed charts during the six-week expedition. Although Quimper's journal of the voyage does not refer to the mountain, one of Haro's manuscript charts includes a sketch of Mount Baker. The Spanish named the snowy volcano ', as it reminded them of the white-clad monks of the Carmelite Monastery. First European ascent.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Isolated ridges of lava and hydrothermally altered rock, especially in the area of Sherman Crater, are exposed between glaciers on the upper flanks of the volcano; the lower flanks are steep and heavily vegetated. Volcanic rocks of Mount Baker and Black Buttes rest on a foundation of non-volcanic rocks.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Many, if not most, of these were not related to magmatic eruptions, but may have been induced by magma intrusion, steam eruptions, earthquakes, gravitational instability, or possibly even heavy rainfall. Early history. Research beginning in the late 1990s shows that Mount Baker is the youngest of several volcanic centers in the area and one of the youngest volcanoes in the Cascade Range.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Next, a small hydrovolcanic eruption occurred at Sherman Crater, triggering a second collapse of the flank just east of the Roman Wall. That collapse also became a lahar that mainly followed the course of the first lahar for at least, and also spilled into tributaries of the Baker River. Finally, an eruption cloud deposited ash as far as downwind to the northeast and east. Historical activity.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Activity gradually declined over the next two years, but stabilized at a higher level than before 1975. The increased level of fumarolic activity has continued at Mount Baker since 1975, but no other changes suggest that magma movement is involved. Current research at Mount Baker.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Mapping of Carmelo and Sherman craters, and interpretations of the eruptive history, continue, as well. The Mount Baker Volcano Research Center maintains an online archive of abstracts of this work, and an extensive references list, as well as photos. Climate. Mount Baker has an alpine tundra climate (ET)
Glaciers and hydrology. Eleven named glaciers descend from Mount Baker.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Mount Baker is drained on the north by streams that flow into the North Fork Nooksack River, on the west by the Middle Fork Nooksack River, and on the southeast and east by tributaries of the Baker River. Lake Shannon and Baker Lake are the largest nearby bodies of water, formed by two dams on the Baker River. U.S. Navy.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
U.S. Navy. Two ammunition ships of the United States Navy (traditionally named for volcanoes) have been named after the mountain. The first was USS &quot;Mount Baker&quot; (AE-4), which was commissioned from 1941 to 1947 and from 1951 to 1969. In 1972, the Navy commissioned USS &quot;Mount Baker&quot; (AE-34).

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
The current English name for the mountain, Mount Baker, was chosen by George Vancouver. Vancouver named the mountain for 3rd Lieutenant Joseph Baker of HMS &quot;Discovery&quot;, who saw it on April 30, 1792. Mount Baker is sometimes also known by the alternative English name &quot;Kulshan&quot; which is the Anglicized form of the Nooksack name.

Geographic entities mentioned:
surface_form: kulshan
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Geology. The present-day cone of Mount Baker is relatively young, perhaps less than 100,000 years old. The volcano sits atop a similar older volcanic cone called Black Buttes, which was active between 500,000 and 300,000 years ago.

Geographic entities mentioned:
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Four Mile Lake (Ontario). Four Mile Lake is a lake in the city of Kawartha Lakes in Central Ontario, Canada. The lake is northeast of Coboconk, Ontario and west of Burnt River. It is one of the Kawartha Lakes series of lakes and is in the Great Lakes Basin. Geography and Geology. Four Mile Lake is a relatively shallow warm water lake with a surface area of.

Geographic entities mentioned:
surface_form: kawartha
instance_of: Group of lakes
countries: Canada
coordinates: lat: 44.4994
lon: -78.441
surface_form: four mile lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.681666666667
lon: -78.737222222222
Four Mile Lake (Ontario). Four Mile Lake is a lake in the city of Kawartha Lakes in Central Ontario, Canada. The lake is northeast of Coboconk, Ontario and west of Burnt River. It is one of the Kawartha Lakes series of lakes and is in the Great Lakes Basin. Geography and Geology. Four Mile Lake is a relatively shallow warm water lake with a surface area of.

Geographic entities mentioned:
surface_form: kawartha
instance_of: Group of lakes
countries: Canada
coordinates: lat: 44.4994
lon: -78.441
It is one of the Kawartha Lakes series of lakes and is in the Great Lakes Basin. Geography and Geology. Four Mile Lake is a relatively shallow warm water lake with a surface area of. The lake is located in the sub watershed of Corben Creek and has a flushing rate of approximately five years. The lake is located on the boundary between two different geological land forms.

Geographic entities mentioned:
surface_form: corben creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.685833333333
lon: -78.746666666667
Four Mile Lake (Ontario). Four Mile Lake is a lake in the city of Kawartha Lakes in Central Ontario, Canada. The lake is northeast of Coboconk, Ontario and west of Burnt River. It is one of the Kawartha Lakes series of lakes and is in the Great Lakes Basin. Geography and Geology. Four Mile Lake is a relatively shallow warm water lake with a surface area of.

Geographic entities mentioned:
surface_form: four mile lake (ontario)
instance_of: Lake
countries: Canada
coordinates: lat: 44.681666666667
lon: -78.737222222222
It is one of the Kawartha Lakes series of lakes and is in the Great Lakes Basin. Geography and Geology. Four Mile Lake is a relatively shallow warm water lake with a surface area of. The lake is located in the sub watershed of Corben Creek and has a flushing rate of approximately five years. The lake is located on the boundary between two different geological land forms.

Geographic entities mentioned:
surface_form: four mile lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.681666666667
lon: -78.737222222222
The southern two-thirds of the lake is located on the Corden plain and is characterized by sedimentary limestone cliffs along the shoreline. Four Mile Lake is a closed lake system with no navigable access to other lakes. The lake provides a community to approximately 450 cottages and homes. Four Mile Lake is located near a rare biological environment phenomenon known as alvars. Roads and services.

Geographic entities mentioned:
surface_form: four mile lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.681666666667
lon: -78.737222222222
Four Mile Lake is a closed lake system with no navigable access to other lakes. The lake provides a community to approximately 450 cottages and homes. Four Mile Lake is located near a rare biological environment phenomenon known as alvars. Roads and services. Electricity is serviced to all properties on Four Mile Lake by Hydro One and telephone is serviced by Bell Canada.

Geographic entities mentioned:
surface_form: four mile lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.681666666667
lon: -78.737222222222
Four Mile Lake is located near a rare biological environment phenomenon known as alvars. Roads and services. Electricity is serviced to all properties on Four Mile Lake by Hydro One and telephone is serviced by Bell Canada. Numerous cellular telephone services are also available. Both dial-up and wireless high speed internet services are available.

Geographic entities mentioned:
surface_form: four mile lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.681666666667
lon: -78.737222222222
Dawes (lunar crater). Dawes is a lunar impact crater located in the wide straight between Mare Serenitatis and Mare Tranquilitatis. To its southwest lies the larger crater Plinius, and to its northeast sits the Mons Argaeus mountain rise. It is named after British astronomer William Rutter Dawes. Description. Dawes is circular with a sharp rim that has a slightly flattened oval perimeter.

Geographic entities mentioned:
surface_form: Mons Argaeus
instance_of: Mountain
coordinates: lat: 19.33
lon: 29.01
Ostorfer See. Ostorfer See is a lake in Nordwestmecklenburg, Mecklenburg-Vorpommern, Germany. At an elevation of 39.5 m, its surface area is 2.089 km². Its average depth is 2.9 meters and maximum depth is 5.1 meters.

Geographic entities mentioned:
surface_form: ostorfer see
instance_of: Lake
countries: Germany
coordinates: lat: 53.613333333333
lon: 11.394166666667
In 1977, the Archaeological Research Center was established as an independent research center. Expeditions of the Old Stone Age Georgian Archaeology Department were organized in the mountains of southern Georgia, Tskaltsitela valley, Kodori valley and Terjola district. Studies on the problems of the Stone Age have been published by: Guram Grigolia, Medea Nioradze, L.

Geographic entities mentioned:
surface_form: Kodori valley
instance_of: Valley
countries: Georgia
coordinates: lat: 43.1
lon: 41.8
Ellison Provincial Park. Ellison Provincial Park is a provincial park in British Columbia, Canada, located on the east side of Okanagan Lake to the south of the city of Vernon. The park contains approximately of land, 200 ha. of it upland, 19 ha. of it foreshore. Name origin.

Geographic entities mentioned:
surface_form: Okanagan Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.920833333333
lon: -119.5
Mistatikamekw River. The Mistatikamekw River is a tributary of the Oskélanéo River which flows into the South Bay of Bureau Lake (Gouin Reservoir), flowing into the town of La Tuque, in the
administrative region of Mauricie, in Quebec, in Canada. The Mistatikamekw river flows successively into the townships of Tassé, Montpetit, Faucher and Achintre.

Geographic entities mentioned:
surface_form: Oskélanéo River
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.255555555556
lon: -75.136666666667
surface_form: mistatikamekw river
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.200555555556
lon: -75.125277777778
Mistatikamekw River. The Mistatikamekw River is a tributary of the Oskélanéo River which flows into the South Bay of Bureau Lake (Gouin Reservoir), flowing into the town of La Tuque, in the
administrative region of Mauricie, in Quebec, in Canada. The Mistatikamekw river flows successively into the townships of Tassé, Montpetit, Faucher and Achintre.

Geographic entities mentioned:
surface_form: mistatikamekw river
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.200555555556
lon: -75.125277777778
Some secondary forest roads are in use nearby for forestry and recreational tourism activities. The surface of the Mistatikamekw River is usually frozen from mid-November to the end of April, however, safe ice circulation is generally from early December to late March. Toponymy. The hydronym &quot;Mistatikamekw&quot; is of autochthonous origin.

Geographic entities mentioned:
surface_form: mistatikamekw river
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.200555555556
lon: -75.125277777778
The surface of the Mistatikamekw River is usually frozen from mid-November to the end of April, however, safe ice circulation is generally from early December to late March. Toponymy. The hydronym &quot;Mistatikamekw&quot; is of autochthonous origin. The toponym &quot;Mistatikamekw River&quot; was formalized on September 3, 1981, at the Commission de toponymie du Quebec.

Geographic entities mentioned:
surface_form: mistatikamekw river
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.200555555556
lon: -75.125277777778