Sarmila/GeoWiki-Features huggingface dataset:
Agria. Agria () is a town and a former municipality in Magnesia, Thessaly, Greece. Since the 2011 local government reform it is part of the municipality Volos, of which it is a municipal unit. The municipal unit has an area of 25.227 km2. It lies on the Pelion peninsula about 7 km from Volos. Name. There are some different opinions about the town's name.

Geographic entities mentioned:
surface_form: Pelion
instance_of: Mountain
countries: Greece
coordinates: lat: 39.433333333333
lon: 23.05
During the 1980s the section through Huajialing lost its importance as a new route was built. The town is at the center of a reforestation programme of Gansu's Loess Plateau region, which commenced in 1971. Climate. Huajialing has a subarctic climate (Köppen climate classification &quot;Dwc&quot;). The average annual temperature in Huajialing is.

Geographic entities mentioned:
surface_form: Loess Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Sherman Oaks Center for Enriched Studies. Sherman Oaks Center for Enriched Studies is a magnet public school in the San Fernando Valley, Los Angeles, California, United States. Despite the name, SOCES is located in the Tarzana section of Los Angeles on the former campus of Sequoia Junior High School.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Freeman Peak. Freeman Peak is a mountain summit located in Lemhi County, Idaho, United States. Description. Freeman Peak is part of the Beaverhead Mountains which are a subset of the Bitterroot Range. The peak is situated 12 miles northeast of Salmon, Idaho, in the Salmon–Challis National Forest. The summit lies less than one-half mile west of the Continental Divide and the Idaho–Montana border.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: freeman peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.274444444444
lon: -113.70083333333
Freeman Peak. Freeman Peak is a mountain summit located in Lemhi County, Idaho, United States. Description. Freeman Peak is part of the Beaverhead Mountains which are a subset of the Bitterroot Range. The peak is situated 12 miles northeast of Salmon, Idaho, in the Salmon–Challis National Forest. The summit lies less than one-half mile west of the Continental Divide and the Idaho–Montana border.

Geographic entities mentioned:
surface_form: freeman peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.274444444444
lon: -113.70083333333
Freeman Creek was also called Oro Cache Creek (Gold Cache) due to the mining in this area. Climate. Based on the Köppen climate classification, Freeman Peak is located in an alpine subarctic climate zone with long, cold, snowy winters, and cool to warm summers. Winter temperatures can drop below −10 °F with wind chill factors below −30 °F.

Geographic entities mentioned:
surface_form: freeman peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.274444444444
lon: -113.70083333333
Carrie Glacier. Carrie Glacier is located on Mount Carrie and Mount Fairchild in the Olympic Mountains of Olympic National Park. Starting at an elevation of about, the glacier descends northward, but the ice soon reaches a cliff.

Geographic entities mentioned:
surface_form: Mount Carrie
instance_of: Mountain
countries: United States
coordinates: lat: 47.89425
lon: -123.64908
surface_form: Mount Fairchild
instance_of: Mountain
countries: United States
coordinates: lat: 47.90009
lon: -123.63352
Part of the Carrie Glacier plunges over the steep rockwall, contributing ice to an adjacent glacier, while the other section flows north-northeast, avoiding the precipitous drop. This segment of ice is confined by an arête to the west and Mount Fairchild to the east in a chute. The glacier reaches as low as before terminating.

Geographic entities mentioned:
surface_form: Mount Fairchild
instance_of: Mountain
countries: United States
coordinates: lat: 47.90009
lon: -123.63352
Geography. The approximate coordinates for the Town of South Palm Beach is located at (26.591746, –80.037525). South Palm Beach is bordered to the north by the Town of Palm Beach; to the east by the Atlantic Ocean; to the west by the Intracoastal waterway (known locally as the Lake Worth Lagoon); and on the south by the town of Manalapan as well as Lantana's public beach.

Geographic entities mentioned:
surface_form: Lake Worth Lagoon
instance_of: Lake
countries: United States
coordinates: lat: 26.6814
lon: -80.0458
Creach Bheinn (Loch Creran). Creach Bheinn (810 m) is a mountain in the Grampian Mountains of Scotland. It rises above the head Loch Creran in Argyll. A large and sprawling peak, a bulldozed track leads the way up to the ridge from Loch Creran. Some steep sections lie near the top. The islands of Lismore and Mull are clearly visible from its summit, as are the mountains around Glen Coe.

Geographic entities mentioned:
surface_form: creach bheinn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.53012
lon: -5.216208
surface_form: creach bheinn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.661536
lon: -5.4771643
Wheeler, his rival and adversary in a bitter legal battle over one particularly rich silver lode, he made his statement with large buildings bearing his name. The Hyman Building was faced in the same peachblow sandstone as Wheeler's Opera House, brought to the city by the railroads that Hyman and Wheeler had briefly put aside their differences to bring up the Roaring Fork Valley in the late 1880s.

Geographic entities mentioned:
surface_form: Roaring Fork Valley
instance_of: Valley
countries: United States
However, an earlier journey to Dudhope Castle in 1619 involving crossing the Forth is detailed in the account book. In July 1623 she travelled with the Viscount Lauderdale to Drummond Castle in Strathearn to stay for a month with her brother John Drummond, 2nd Earl of Perth. Royal Governess Again.

Geographic entities mentioned:
surface_form: Strathearn
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.3325
lon: -3.6825
The plain is made up smaller individual sand and clay plains alternated with rivers and peat bogs. It extends as a 100 km wide and 257 km long belt along the northwestern coast of Finland. The plain is extremely flat with height differences never exceeding 50 m. Geologically the plain is a continuation of the Sub-Cambrian peneplain found across much of Fennoscandia.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Municipality of Jesenice. The Municipality of Jesenice (;) is a municipality in northwest Slovenia. The seat of the municipality is the town of Jesenice. It has 21,895 inhabitants. Geography. The municipality lies in the Upper Carniola region, in the Upper Sava Valley. It is bordered by the Karawanks and Austria (Carinthia) to the north, and by Mount Mežakla to the south.

Geographic entities mentioned:
surface_form: Upper Sava Valley
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.471111111111
lon: 13.911666666667
Municipality of Jesenice. The Municipality of Jesenice (;) is a municipality in northwest Slovenia. The seat of the municipality is the town of Jesenice. It has 21,895 inhabitants. Geography. The municipality lies in the Upper Carniola region, in the Upper Sava Valley. It is bordered by the Karawanks and Austria (Carinthia) to the north, and by Mount Mežakla to the south.

Geographic entities mentioned:
surface_form: Mežakla
instance_of: Plateau
countries: Slovenia
coordinates: lat: 46.40166667
lon: 14.04083333
Gibbs Lake (New York). Gibbs Lake is a small lake northwest of Old Forge in Herkimer County, New York. It drains north via an unnamed creek which flows into Half Moon Pond.

Geographic entities mentioned:
surface_form: Half Moon Pond
instance_of: Lake
countries: United States
coordinates: lat: 43.734717
lon: -75.012822
surface_form: half moon
instance_of: Mountain
countries: United States
coordinates: lat: 48.509867
lon: -120.613489
Gibbs Lake (New York). Gibbs Lake is a small lake northwest of Old Forge in Herkimer County, New York. It drains north via an unnamed creek which flows into Half Moon Pond.

Geographic entities mentioned:
surface_form: gibbs lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7325
lon: -75.000833333333
surface_form: gibbs lake
instance_of: Lake
countries: United States
coordinates: lat: 42.7828
lon: -89.1804
Contemporary reports stated &quot;Myola&quot; sunk off Sydney Heads. However, the wreck of &quot;Myola&quot; was found in 1994, in 48 metres of water off Long Reef, lying on its port side. Damage to the propeller indicates that the engine was still running as the ship foundered, which is consistent with accounts given by the crew.

Geographic entities mentioned:
surface_form: Sydney Heads
instance_of: Landform
countries: Australia
coordinates: lat: -33.8368
lon: 151.281
The route heads up Victory Road as a two-lane undivided highway, forming the northern limit of urban development in the Marmalade District. The land north of Victory road is the fell-like slope leading up to Ensign Peak. As the road heads southeast, it reaches the top of Salt Lake's Capitol Hill, a foothill of Ensign Peak, where residential developments begin to appear on the north side.

Geographic entities mentioned:
surface_form: Ensign Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.794166666667
lon: -111.89055555556
Cedar Mountain, Virginia. Cedar Mountain, also known as Slaughter Mountain, is a piedmont monadnock in Culpeper County, Virginia. The ridge is south of the town of Culpeper and just to the northwest of the northern tip of the Southwest Mountains at Clark Mountain. The mountain was used as a signal mountain by confederate troops during the Civil War.

Geographic entities mentioned:
surface_form: cedar mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.228055555556
lon: -111.52944444444
surface_form: cedar mountain, virginia
instance_of: Mountain
countries: United States
coordinates: lat: 38.3694
lon: -78.0714
Cedar Mountain, Virginia. Cedar Mountain, also known as Slaughter Mountain, is a piedmont monadnock in Culpeper County, Virginia. The ridge is south of the town of Culpeper and just to the northwest of the northern tip of the Southwest Mountains at Clark Mountain. The mountain was used as a signal mountain by confederate troops during the Civil War.

Geographic entities mentioned:
surface_form: cedar mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.228055555556
lon: -111.52944444444
surface_form: piedmont
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -80
surface_form: slaughter mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.747777777778
lon: -83.950277777778
surface_form: slaughter mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.3694
lon: -78.0714
surface_form: cedar mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.3694
lon: -78.0714
Cedar Mountain, also known as Slaughter Mountain, is a piedmont monadnock in Culpeper County, Virginia. The ridge is south of the town of Culpeper and just to the northwest of the northern tip of the Southwest Mountains at Clark Mountain. The mountain was used as a signal mountain by confederate troops during the Civil War. Remnants of that fortification are still visible today.

Geographic entities mentioned:
surface_form: signal mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2063
lon: -72.3252
surface_form: signal mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.8489
lon: -110.567
Cedar Mountain, Virginia. Cedar Mountain, also known as Slaughter Mountain, is a piedmont monadnock in Culpeper County, Virginia. The ridge is south of the town of Culpeper and just to the northwest of the northern tip of the Southwest Mountains at Clark Mountain. The mountain was used as a signal mountain by confederate troops during the Civil War.

Geographic entities mentioned:
surface_form: clark mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.05
lon: -120.969
surface_form: clark mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.21936
lon: -70.17756
surface_form: clark mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.5256
lon: -115.589
Trödelsteine (mountain). The Trödelsteine is the name of a mountain, in the Heller Upland near Emmerzhausen in the county of Altenkirchen in the German state of Rhineland-Palatinate and the county of Siegen-Wittgenstein in the state of North Rhine-Westphalia with its summit area in Rhineland-Palatinate. Location.

Geographic entities mentioned:
surface_form: trödelsteine (mountain)
instance_of: Mountain
countries: Germany
coordinates: lat: 50.72836111
lon: 8.03716667
Trödelsteine (mountain). The Trödelsteine is the name of a mountain, in the Heller Upland near Emmerzhausen in the county of Altenkirchen in the German state of Rhineland-Palatinate and the county of Siegen-Wittgenstein in the state of North Rhine-Westphalia with its summit area in Rhineland-Palatinate. Location.

Geographic entities mentioned:
surface_form: trödelsteine
instance_of: Mountain
countries: Germany
coordinates: lat: 50.72836111
lon: 8.03716667
Location. The Trödelsteine lies about 1.2 kilometres northeast of Emmerzhausen, 3.6 km southwest of Burbach and 2.6 km northwest of Lippe, which are both in the neighbouring county of Siegen-Wittgenstein. The state border between Rhineland-Palatinate and North Rhine-Westphalia runs about 50 metres northeast of the summit – roughly along the lower part of the eponymous rock formation.

Geographic entities mentioned:
surface_form: trödelsteine
instance_of: Mountain
countries: Germany
coordinates: lat: 50.72836111
lon: 8.03716667
Neighbouring mountains are: to the north, the Nenkersberg (610.3 m) and, to the south-southeast, the Lipper Nürr (616.9 m). According to the Deutsche Grundkarte, the summit of the Trödelsteine is 613.0 m; on the topographical maps a height of 612.8 m is given. Natural regions. The Trödelsteine belongs to the natural region major unit group of the Süder Uplands (no.

Geographic entities mentioned:
surface_form: trödelsteine
instance_of: Mountain
countries: Germany
coordinates: lat: 50.72836111
lon: 8.03716667
According to the Deutsche Grundkarte, the summit of the Trödelsteine is 613.0 m; on the topographical maps a height of 612.8 m is given. Natural regions. The Trödelsteine belongs to the natural region major unit group of the Süder Uplands (no. 33), to the major unit of the Siegerland (331), the subunit of the Heller Upland (331.3) and the natural region of the Southern Heller Upland (331.32).

Geographic entities mentioned:
surface_form: trödelsteine
instance_of: Mountain
countries: Germany
coordinates: lat: 50.72836111
lon: 8.03716667
33), to the major unit of the Siegerland (331), the subunit of the Heller Upland (331.3) and the natural region of the Southern Heller Upland (331.32). The Trödelsteine. In the summit region of the mountain are the rocks of the same name, the Trödelsteine, which comprise several basalt crags and, below them, a column and blockfield of feldspar basalt. The rocks are protected as a natural monument.

Geographic entities mentioned:
surface_form: trödelsteine
instance_of: Mountain
countries: Germany
coordinates: lat: 50.72836111
lon: 8.03716667
The rocks are protected as a natural monument. Transport and hiking. The axis of the Landesstraßen 280 and 911 runs south past the Trödelsteine from Emmerzhausen in Rhineland-Palatinate to Lippe in North Rhine-Westphalia. The E1 European long distance path runs over the mountain, crossing the road at the state border.

Geographic entities mentioned:
surface_form: trödelsteine
instance_of: Mountain
countries: Germany
coordinates: lat: 50.72836111
lon: 8.03716667
The E1 European long distance path runs over the mountain, crossing the road at the state border. On the Trödelsteine is a narrow footpath, which is part of the Trödelstein Path (&quot;Trödelsteinpfad&quot;), a 10.2-kilometre-long branch of the Rothaarsteig.

Geographic entities mentioned:
surface_form: trödelsteine
instance_of: Mountain
countries: Germany
coordinates: lat: 50.72836111
lon: 8.03716667
Consequently, Mount Rainier is one of the Decade Volcanoes identified by the International Association of Volcanology and Chemistry of the Earth's Interior (IAVCEI) as being worthy of particular study, due to the danger it poses to Seattle and Tacoma.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
The Cascade Volcanoes are part of the Pacific Ring of Fire, the ring of volcanoes and associated mountains around the Pacific Ocean. The Cascade Volcanoes have erupted several times in recorded history. Two most recent were Lassen Peak in 1914 to 1921 and a major eruption of Mount St. Helens in 1980. It is also the site of Canada's most recent major eruption, in 410 BCE at the Mount Meager massif.

Geographic entities mentioned:
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
Volcanism in the arc began about 37 million years ago; however, most of the present-day Cascade Volcanoes are less than 2,000,000 years old, and the highest peaks are less than 100,000 years old. Twelve volcanoes in the arc are over in elevation, and the two highest, Mount Rainier and Mount Shasta, exceed.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
By volume, the two largest Cascade Volcanoes are the broad shields of Medicine Lake Volcano and Newberry Volcano, which are about respectively. Glacier Peak is the only Cascade Volcano that is made exclusively of dacite. The history of the Cascade Volcanoes can be separated into three major chapters which are discussed below. West Cascades period.

Geographic entities mentioned:
surface_form: Glacier Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
During this time the arc was situated a little farther west than it is today. One volcano that was active during this time was the Mount Aix Volcanic Complex, which erupted more than of tephra and pyroclastic debris over the span of just three eruptions.

Geographic entities mentioned:
surface_form: Mount Aix
instance_of: Mountain
countries: United States
coordinates: lat: 46.795
lon: -121.256
Many rugged peaks in the North Cascades owe their prominence to this baking. The rocks holding up many such North Cascade giants, as Mount Shuksan, Mount Redoubt, Mount Challenger, and Mount Hozomeen, are all partly recrystallized by plutons of the nearby and underlying Chilliwack batholith. Widespread dormancy period.

Geographic entities mentioned:
surface_form: Mount Shuksan
instance_of: Mountain
countries: United States
coordinates: lat: 48.8316
lon: -121.603
The volcanoes of the Cascade Arc share some general characteristics, but each has its own unique geological traits and history. Lassen Peak in California, which last erupted in 1917, is the southernmost historically active volcano in the arc, while the Mount Meager massif in British Columbia, which erupted about 2,350 years ago, is generally considered the northernmost member of the arc.

Geographic entities mentioned:
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
A few isolated volcanic centers northwest of the Mount Meager massif such as the Silverthrone Caldera, which is a circular wide, deeply dissected caldera complex, may also be the product of Cascadia subduction because the igneous rocks andesite, basaltic andesite, dacite and rhyolite can also be found at these volcanoes as they are elsewhere along the subduction zone.

Geographic entities mentioned:
surface_form: Silverthrone Caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
The Cascade Volcanic Arc appears to be segmented; the central portion of the arc is the most active and the northern end least active. The Garibaldi Volcanic Belt is the northern extension of the Cascade Arc. Volcanoes within the volcanic belt are mostly stratovolcanoes along with the rest of the arc, but also include calderas, cinder cones, and small isolated lava masses.

Geographic entities mentioned:
surface_form: Garibaldi Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5283
lon: -126.113
Due to repeated continental and alpine glaciations, many of the volcanic deposits in the belt reflect complex interactions between magma composition, topography, and changing ice configurations. Four volcanoes within the belt appear related to seismic activity since 1975, including: Mount Meager massif, Mount Garibaldi and Mount Cayley.

Geographic entities mentioned:
surface_form: Mount Garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Four volcanoes within the belt appear related to seismic activity since 1975, including: Mount Meager massif, Mount Garibaldi and Mount Cayley. The Pemberton Volcanic Belt is an eroded volcanic belt north of the Garibaldi Volcanic Belt, which appears to have formed during the Miocene before fracturing of the northern end of the Juan de Fuca Plate.

Geographic entities mentioned:
surface_form: Pemberton Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 50.58051944
lon: -122.93235278
The Pemberton Volcanic Belt is an eroded volcanic belt north of the Garibaldi Volcanic Belt, which appears to have formed during the Miocene before fracturing of the northern end of the Juan de Fuca Plate. The Silverthrone Caldera is the only volcano within the belt that appears related to seismic activity since 1975. The Mount Meager massif is the most unstable volcanic massif in Canada.

Geographic entities mentioned:
surface_form: Silverthrone Caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
The Mount Meager massif is the most unstable volcanic massif in Canada. It has dumped clay and rock several meters deep into the Pemberton Valley at least three times during the past 7,300 years. Recent drilling into the Pemberton Valley bed encountered remnants of a debris flow that had traveled from the volcano shortly before it last erupted 2,350 years ago.

Geographic entities mentioned:
surface_form: Pemberton Valley
instance_of: Valley
countries: Canada
coordinates: lat: 50.5
lon: -123
There is no sign of volcanic activity with these events. However, scientists warn the volcano could release another massive debris flow over populated areas any time without warning. In the past, Mount Rainier has had large debris avalanches, and has also produced enormous lahars due to the large amount of glacial ice present. Its lahars have reached all the way to Puget Sound.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
About 530 to 550 years ago, the Electron Mudflow occurred, although this was not as large-scale as the Osceola Mudflow. While the Cascade volcanic arc (a geological term) includes volcanoes such as the Mount Meager massif and Mount Garibaldi, which lie north of the Fraser River, the Cascade Range (a geographic term) is considered to have its northern boundary at the Fraser. Largest eruptions.

Geographic entities mentioned:
surface_form: Mount Garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Largest eruptions. The table below lists some of the greatest eruptions to have occurred in the Cascade chain. Human history. Native Americans have inhabited the area for thousands of years and developed their own myths and legends concerning the Cascade volcanoes. According to some of these tales, Mounts Baker, Jefferson, Shasta and Garibaldi were used as refuge from a great flood.

Geographic entities mentioned:
surface_form: 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
surface_form: Garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
According to some of these tales, Mounts Baker, Jefferson, Shasta and Garibaldi were used as refuge from a great flood. Other stories, such as the Bridge of the Gods tale, had various High Cascades such as Hood and Adams, act as god-like chiefs who made war by throwing fire and stone at each other. St.

Geographic entities mentioned:
surface_form: Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
Other stories, such as the Bridge of the Gods tale, had various High Cascades such as Hood and Adams, act as god-like chiefs who made war by throwing fire and stone at each other. St. Helens with its pre-1980 graceful appearance, was regaled as a beautiful maiden for whom Hood and Adams feuded.

Geographic entities mentioned:
surface_form: St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
Then, because of a marital dispute, she picked herself up and marched north to her present position. Native tribes also developed their own names for the High Cascades and many of the smaller peaks, the most well known to non-natives being Tahoma, the Lushootseed name for Mount Rainier.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
Native tribes also developed their own names for the High Cascades and many of the smaller peaks, the most well known to non-natives being Tahoma, the Lushootseed name for Mount Rainier. Mount Cayley and The Black Tusk are known to the Squamish people who live nearby as &quot;the Landing Place of the Thunderbird&quot;.

Geographic entities mentioned:
surface_form: The Black Tusk
instance_of: Mountain
countries: Canada
coordinates: lat: 49.97527777777778
lon: -123.04277777777777
Stories of Tahoma – today Mount Rainier and the namesake of Tacoma, Washington – allude to great, hidden grottos with sleeping giants, apparitions and other marvels in the volcanoes of Washington, and Mount Shasta in California has long been well known for its associations with everything from Lemurians to aliens to elves and, as everywhere in the arc, Sasquatch or Bigfoot.

Geographic entities mentioned:
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
In the spring of 1792 British navigator George Vancouver entered Puget Sound and started to give English names to the high mountains he saw. Mount Baker was named for Vancouver's third lieutenant, the graceful Mount St.

Geographic entities mentioned:
surface_form: Mount Baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
As marine trade in the Strait of Georgia and Puget Sound proceeded in the 1790s and beyond, the summits of Rainier and Baker became familiar to captains and crews (mostly British and American). With the exception of the 1915 eruption of remote Lassen Peak in Northern California, the arc was quiet for more than a century. Then, on May 18, 1980, the dramatic eruption of little-known Mount St.

Geographic entities mentioned:
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
With the exception of the 1915 eruption of remote Lassen Peak in Northern California, the arc was quiet for more than a century. Then, on May 18, 1980, the dramatic eruption of little-known Mount St. Helens shattered the quiet and brought the world's attention to the arc. Geologists were also concerned that the St.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
The eruption sent an ash column approximately high into the stratosphere. This activity produced a diverse sequence of volcanic deposits, well exposed in the bluffs along the Lillooet River, which is defined as the Pebble Creek Formation. The eruption was episodic, occurring from a vent on the north-east side of Plinth Peak.

Geographic entities mentioned:
surface_form: Plinth Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.6452
lon: -123.511
The volume of magma erupted in this event is equal to 2 km3. 7700 BP (5783 BC) eruption of Mount Mazama. The 7,700 BP eruption of Mount Mazama was a large catastrophic eruption in the U.S. state of Oregon. It began with a large eruption column with pumice and ash that erupted from a single vent.

Geographic entities mentioned:
surface_form: Mount Mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
It began with a large eruption column with pumice and ash that erupted from a single vent. The eruption was so great that most of Mount Mazama collapsed to form a caldera and subsequent smaller eruptions occurred as water began to fill in the caldera to form Crater Lake. Volcanic ash from the eruption was carried across most of the Pacific Northwest as well as parts of western Canada.

Geographic entities mentioned:
surface_form: Crater Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.943611111111
lon: -122.10666666667
Volcanic ash from the eruption was carried across most of the Pacific Northwest as well as parts of western Canada. 13100 BP (11,150 BC) eruptions of Glacier Peak. About 13,000 years ago, Glacier Peak generated an unusually strong sequence of eruptions, with one of them being a staggering 5 times larger than the 1980 eruption of Mount St. Helens.

Geographic entities mentioned:
surface_form: Glacier Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
Silverthrone Caldera. Most of the Silverthrone Caldera's eruptions in the Pacific Range occurred during the Last Glacial Period and was episodically active during both Pemberton and Garibaldi Volcanic Belt stages of volcanism. The caldera is one of the largest of the few calderas in western Canada, measuring about long (north-south) and wide (east-west).

Geographic entities mentioned:
surface_form: Silverthrone Caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
surface_form: Pemberton
instance_of: Mountain
countries: Canada
coordinates: lat: 50.58051944
lon: -122.93235278
surface_form: Garibaldi Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5283
lon: -126.113
The lava was dammed by the ice and made a cliff with a waterfall up against it. The most recent activity was 1000 years ago. Mount Garibaldi. Mount Garibaldi in the Pacific Range was last active about 10,700 to 9,300 years ago from a cinder cone called Opal Cone. It produced a long broad dacite lava flow with prominent wrinkled ridges. The lava flow is unusually long for a silicic lava flow.

Geographic entities mentioned:
surface_form: Mount Garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
surface_form: Opal Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8272
lon: -122.971
The lava flow is unusually long for a silicic lava flow. Mount Baker. During the mid-19th century, Mount Baker erupted for the first time in several thousand years. Fumarole activity remains in Sherman Crater, just south of the volcano's summit, became more intense in 1975 and is still energetic. However, an eruption is not expected in the near future. Glacier Peak.

Geographic entities mentioned:
surface_form: Mount Baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
However, an eruption is not expected in the near future. Glacier Peak. Glacier Peak last erupted about 200–300 years ago and has erupted about six times in the past 4,000 years. Mount Rainier. Mount Rainier last erupted between 1824 and 1854, but many eyewitnesses reported eruptive activity in 1858, 1870, 1879, 1882, and in 1894 as well.

Geographic entities mentioned:
surface_form: Glacier Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
Glacier Peak. Glacier Peak last erupted about 200–300 years ago and has erupted about six times in the past 4,000 years. Mount Rainier. Mount Rainier last erupted between 1824 and 1854, but many eyewitnesses reported eruptive activity in 1858, 1870, 1879, 1882, and in 1894 as well. Mount Rainier has created at least four eruptions and many lahars in the past 4,000 years. Mount Adams.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
Thermal anomalies (hot spots) and gas emissions (including hydrogen sulfide) have occurred especially on the summit plateau since the Great Slide of 1921. Mount Hood. Mount Hood was last active about 200 years ago, creating pyroclastic flows, lahars, and a well-known lava dome close to its peak called Crater Rock. Between 1856 and 1865, a sequence of steam explosions took place at Mount Hood.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
Mount Shasta. Mount Shasta last erupted around 1250 and has been the most active volcano in California for about 4,000 years. Previous claims of a 1786 eruption have been discredited. Eruptions in the Cascade Range. Eleven of the thirteen volcanoes in the Cascade Range have erupted at least once in the past 4,000 years, and seven have done so in just the past 200 years.

Geographic entities mentioned:
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
All of the known historical eruptions have occurred in Washington, Oregon and in Northern California. The three most recent were Lassen Peak from 1914 to 1921, a major eruption of Mount St. Helens in 1980, and a minor eruption of Mount St. Helens from 2004 to 2008. In contrast, volcanoes in southern British Columbia, central and southern Oregon are currently dormant.

Geographic entities mentioned:
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
The regions lacking new eruptions keep in touch to positions of fracture zones that offset the Gorda Ridge, Explorer Ridge and the Juan de Fuca Ridge. The volcanoes with historical eruptions include: Mount Rainier, Glacier Peak, Mount Baker, Mount Hood, Lassen Peak, and Mount Shasta. Renewed volcanic activity in the Cascade Arc, such as the 1980 eruption of Mount St.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: Glacier Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: Mount Baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
A vast piece on the north side of Mount St. Helens dropped and formed a jumbled landslide environment several kilometers away from the volcano. Pyroclastic flows and lahars moved across the countryside. Parallel episodes have also happened at Mount Shasta and other Cascade volcanoes in prehistoric times.

Geographic entities mentioned:
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
History. Aboriginally, speakers of Mohican lived along the upper Hudson River in New York State, extending as far north as Lake Champlain, east to the Green Mountains in Vermont, and west near Schoharie Creek in New York State.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
History. The Mt Kenya Game Ranch was founded in the 1960s by filmstar William Holden, Don and Iris Hunt, Julian McKeand and Deane Johnson after purchase of an game farm on the slopes of Mount Kenya. Over time, 37 species in breeding herds were captured and brought to the ranch to create the first game ranch of its kind in East Africa.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
Together with other leading international wildlife artists Mead has taken part in two Artists for Nature Foundation projects, which bring artists together to promote and raise funds for conservation projects around the world, including the Great Fen Project in Cambridgeshire, and the Hula Valley in Israel. Public art. Mead has produced two large-scale public art pieces.

Geographic entities mentioned:
surface_form: Hula Valley
instance_of: Valley
countries: Israel
coordinates: lat: 33.103333333333
lon: 35.609166666667
Dendrocoelidae. Dendrocoelidae is a family of freshwater tricladida flatworms that has a holarctic distribution. The largest freshwater triclad known belongs to this family, it's up to 40 cm in length and inhabits the Lake Baikal. Description. The family Dendrocoelidae is characterized by an unusual arrangement of the muscle layers of the pharynx.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Lake Evoron. Lake Evoron () is a large freshwater lake in Khabarovsk Krai, Russia. It is located in the Gorin River basin, part of the Amur basin. It has an area of 194 square kilometres, and is 30 km long and 12 km at its widest. Its average depth is about 2–3 m. The lake is used for fishing. The Evur and Shroki rivers flow into the lake.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: evoron
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 51.44
lon: 136.52638888889
surface_form: lake evoron
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 51.44
lon: 136.52638888889
Lake Evoron. Lake Evoron () is a large freshwater lake in Khabarovsk Krai, Russia. It is located in the Gorin River basin, part of the Amur basin. It has an area of 194 square kilometres, and is 30 km long and 12 km at its widest. Its average depth is about 2–3 m. The lake is used for fishing. The Evur and Shroki rivers flow into the lake.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: evoron
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 51.44
lon: 136.52638888889
surface_form: lake evoron
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 51.44
lon: 136.52638888889
Lake Evoron () is a large freshwater lake in Khabarovsk Krai, Russia. It is located in the Gorin River basin, part of the Amur basin. It has an area of 194 square kilometres, and is 30 km long and 12 km at its widest. Its average depth is about 2–3 m. The lake is used for fishing. The Evur and Shroki rivers flow into the lake. The outflow is the Devyatke River, a tributary of the Gorin.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
After camps were disbanded in 1948, most of the remaining Yugoslav Germans emigrated to Germany because of economic reasons in the next decades. After World War II, the village was colonized by settlers from Montenegro and Mt. Vlašić, Bosnia. The Montenegrins renamed the village in honor of Mt. Lovćen and account for the majority of the population. Ethnic groups.

Geographic entities mentioned:
surface_form: Mt. Lovćen
instance_of: Mountain
countries: Montenegro
coordinates: lat: 42.4
lon: 18.833333333333
Visaginas (lake). Lake Visaginas is located south of the town of Visaginas in eastern Lithuania.

Geographic entities mentioned:
surface_form: visaginas
instance_of: Lake
countries: Lithuania
coordinates: lat: 55.587777777778
lon: 26.424722222222
Visaginas (lake). Lake Visaginas is located south of the town of Visaginas in eastern Lithuania.

Geographic entities mentioned:
surface_form: visaginas
instance_of: Lake
countries: Lithuania
coordinates: lat: 55.587777777778
lon: 26.424722222222
surface_form: visaginas
instance_of: Lake
countries: Lithuania
coordinates: lat: 55.587777777778
lon: 26.424722222222
Temple Hill (Hong Kong). Temple Hill, also known as Tsz Wan Shan (), is a hill between New Kowloon and the New Territories, Hong Kong. It peaks at 488 m. Beneath its south side is the residential area of Tsz Wan Shan and Buddhist temples. Sha Tin Pass runs between the hill and Unicorn Ridge. The summit of the hill is located within Sha Tin District.

Geographic entities mentioned:
surface_form: Unicorn Ridge
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.3561553
lon: 114.1945384
Temple Hill (Hong Kong). Temple Hill, also known as Tsz Wan Shan (), is a hill between New Kowloon and the New Territories, Hong Kong. It peaks at 488 m. Beneath its south side is the residential area of Tsz Wan Shan and Buddhist temples. Sha Tin Pass runs between the hill and Unicorn Ridge. The summit of the hill is located within Sha Tin District.

Geographic entities mentioned:
surface_form: temple hill
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.356094
lon: 114.206572
Temple Hill (Hong Kong). Temple Hill, also known as Tsz Wan Shan (), is a hill between New Kowloon and the New Territories, Hong Kong. It peaks at 488 m. Beneath its south side is the residential area of Tsz Wan Shan and Buddhist temples. Sha Tin Pass runs between the hill and Unicorn Ridge. The summit of the hill is located within Sha Tin District.

Geographic entities mentioned:
surface_form: temple hill
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.356094
lon: 114.206572
surface_form: tsz wan shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.356094
lon: 114.206572
Temple Hill (Hong Kong). Temple Hill, also known as Tsz Wan Shan (), is a hill between New Kowloon and the New Territories, Hong Kong. It peaks at 488 m. Beneath its south side is the residential area of Tsz Wan Shan and Buddhist temples. Sha Tin Pass runs between the hill and Unicorn Ridge. The summit of the hill is located within Sha Tin District.

Geographic entities mentioned:
surface_form: tsz wan shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.356094
lon: 114.206572
For their part, the Czechs were having difficulty fighting their way to Vladivostok on the Trans-Siberian railway. Although many had linked up with the forces at Chelyabinsk by early July 1918, the area surrounding Lake Baikal was an obstacle that needed to be overcome before the Legion could get to Vladivostok.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
state of Minnesota. As of the 2020 census, the population was 6,441, and was estimated to be 6,284 in 2024. The county seat and the largest city is Ada. The county is in Minnesota's Red River Valley region. History. Norwegians started settling in Norman County in the early 1870s and up until December 27, 1906 that also included what is now Mahnomen County (Ojibwe for &quot;wild rice&quot;).

Geographic entities mentioned:
surface_form: Red River Valley
instance_of: Valley
countries: Canada
United States
coordinates: lat: 49
lon: -97.5
Betty Higgins. Betty Higgins is an entrepreneur from Papua New Guinea (PNG) who developed and runs a trout farm and hotel in the Mount Wilhelm area. In 2009 she was awarded the overall &quot;Women in Business Award&quot; at the Westpac Outstanding Women Awards for PNG. Early life.

Geographic entities mentioned:
surface_form: Mount Wilhelm
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -5.8
lon: 145.03333333333
2007 World Championship were attended by 117,000 spectators, with peaks of 23,000 on Saturday 10 February. Venue. The arena is located at the end of Antholz Valley (side valley of Puster Valley) at an altitude of 1600 m above sea level, near the Lake of Antholz. Antholz is usually the highest biathlon venue of the World Cup because Soldier Hollow is typically not part of the World Cup.

Geographic entities mentioned:
surface_form: Puster Valley
instance_of: Valley
countries: Italy
Austria
coordinates: lat: 46.7405
lon: 12.369555555555555
surface_form: Lake of Antholz
instance_of: Lake
countries: Italy
coordinates: lat: 46.885833333333
lon: 12.166111111111
In 1801, 147 vessels sailed from English ports, bound for the trade in enslaved people; 122 of these vessels sailed from Liverpool. &quot;Barton&quot; started acquiring captives on 12 December 1812 in the area between Rio Nuñez and the Assini River. She arrived at St Thomas, Danish West Indies on 28 July 1802 with 166 captives.

Geographic entities mentioned:
surface_form: Rio Nuñez
instance_of: Watercourse
countries: Guinea
coordinates: lat: 10.594471
lon: -14.675102
The tree cover is mostly made up of common hazel stands, which are stunted due to the intense windy conditions. Location. Ballachuan Hazelwood is located on the eastern side of the remote island of Seil next to the small Ballachuan Loch. The closest settlement is named Cuan Ferry, found around a kilometer to the west. Trees.

Geographic entities mentioned:
surface_form: Ballachuan Loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.27715
lon: -5.61788
Abbot Pass hut. The Abbot Pass hut was an alpine hut located at an altitude of in Abbot Pass in the Rocky Mountains in Alberta, Canada. It was nestled between Mount Victoria and Mount Lefroy, straddling the Great Divide, which, in this region, defines the boundary between Banff National Park in Alberta and Yoho National Park in British Columbia.

Geographic entities mentioned:
surface_form: Mount Lefroy
instance_of: Mountain
countries: Canada
coordinates: lat: 51.36222222222222
lon: -116.27972222222222