Sarmila/GeoWiki-Features huggingface dataset:
Location. Bokaro Thermal is located at. It has an average elevation of 234 metres (767 feet). It is situated on the banks of the Konar River. =Area overview=. Bokaro district consists of undulating uplands on the Chota Nagpur Plateau with the Damodar River cutting a valley right across. It has an average elevation of above mean sea level. The highest hill, Lugu Pahar, rises to a height of.

Geographic entities mentioned:
surface_form: Chota Nagpur Plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
El Greco left Crete when relatively young, but Michael Damaskinos returned after a brief period in Venice, and was able to switch between Italian and Greek styles. Even the traditionalist Theophanes the Cretan, working mainly on Mount Athos, nevertheless shows unmistakable Western influence.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
He had Pottawatomi heritage in addition to his British ancestry, as his great-aunt Mamie Echo Hawk served as the tribe’s chief lobbyist in Washington DC office for many years. Born in Salinas, California, Willoughby was raised and attended high school in the town of Gustine in San Joaquin Valley.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Kiewa Valley Highway. Kiewa Valley Highway is a rural highway which traverses the Kiewa Valley near the alpine regions of Victoria, Australia, connecting the eastern Wodonga suburb of Bandiana to Mount Beauty, at the foot of Mount Bogong in the Alpine National Park. Route.

Geographic entities mentioned:
surface_form: Mount Bogong
instance_of: Mountain
countries: Australia
coordinates: lat: -36.7325
lon: 147.30583333333334
government in the late 19th century. According to his 1887 history of the indigenous peoples of Michigan, the people of Mackinac Island had been a small independent tribe known as &quot;Mi-shi-ne-macki naw-go&quot;. They became affiliated with the larger tribe of Ottawa from Ottawa Island (now Manitoulin Island) situated north of Lake Huron.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
The City and the Commission work together on the many issues affecting both the City and the State Park, such as the longtime ban on motorized vehicles on the island. Access to the island is by ferries across Lake Huron. The city of Mackinac Island is one of seven municipalities in the state of Michigan to consist entirely of islands, including Grosse Ile, Drummond, Bois Blanc, St.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Lake Pillsbury. Lake Pillsbury is a lake in the Mendocino National Forest of Lake County, California, created from the Eel River and Hull Mountain watershed by Scott Dam. Elevation is with of shoreline and covering. Activities in the Lake Pillsbury Recreation Area include powerboating, fishing, swimming, sailing, picnicking, hiking and hang gliding. There are two main access roads to the lake.

Geographic entities mentioned:
surface_form: lake pillsbury
instance_of: Lake
countries: United States
coordinates: lat: 39.4072
lon: -122.9575
By 1908 water was being diverted to the power plant and then to the Russian River. Part two of the project was building the dam which created Lake Pillsbury, located upstream. Scott Dam was completed in 1921 as a concrete gravity structure, high, long at its crest, and impounding a maximum capacity of. It maintains water flow to the hydroelectric plant during times of low water runoff.

Geographic entities mentioned:
surface_form: lake pillsbury
instance_of: Lake
countries: United States
coordinates: lat: 39.4072
lon: -122.9575
Other fish include black bass, steelhead, and pikeminnow. The California Office of Environmental Health Hazard Assessment (OEHHA) has developed a safe eating advisory for Lake Pillsbury based on levels of mercury or PCBs found in fish caught from this water body. In 2022, Lake County health officials reported that testing found concerning levels of cyanobacteria in Lake Pillsbury.

Geographic entities mentioned:
surface_form: lake pillsbury
instance_of: Lake
countries: United States
coordinates: lat: 39.4072
lon: -122.9575
Those who plan to recreate in or on Lake Pillsbury should look for informational signs posted throughout the county and avoid contact with water that, looks like spilled green or blue-green paint; has surface scums, mats, or films; has a blue or green crust at the shoreline; is discolored or has green-colored streaks; or has greenish globs suspended in the water beneath the surface.

Geographic entities mentioned:
surface_form: lake pillsbury
instance_of: Lake
countries: United States
coordinates: lat: 39.4072
lon: -122.9575
Hiking trails at the lake include an interpretive nature trail at Sunset Campground and the Lake Shore Loop Trail. Other nearby recreational opportunities include the Snow Mountain Wilderness located east of Lake Pillsbury. The Bloody Rock historic area is located within the wildlife refuge north of the lake as well as the Eel River and the Wild and Scenic Black Butte River. Wildlife.

Geographic entities mentioned:
surface_form: lake pillsbury
instance_of: Lake
countries: United States
coordinates: lat: 39.4072
lon: -122.9575
surface_form: snow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.2915
lon: -70.7093
surface_form: snow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.763333333333
lon: -121.79722222222
surface_form: snow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.1692
lon: -70.8267
Wildlife. The tule elk is one of the largest land mammals native to California, with cows weighing up to, and the largest bulls weighing roughly. Hunted to near extinction during the California Gold Rush era, the animals were reintroduced to the Lake Pillsbury Basin in the late 1970s by the California Department of Fish and Game, and the herd has steadily grown, numbering around 80 in 2007.

Geographic entities mentioned:
surface_form: lake pillsbury
instance_of: Lake
countries: United States
coordinates: lat: 39.4072
lon: -122.9575
The elk live on the north shore of the lake at the bottom of Hull Mountain, and consume wild clovers and grasses, along with the green summer and fall foliage around Lake Pillsbury's edges. Mendocino National Forest and Los Padres National Forest are the only two national forests in California to have tule elk, though 22 herds are found across the state.

Geographic entities mentioned:
surface_form: lake pillsbury
instance_of: Lake
countries: United States
coordinates: lat: 39.4072
lon: -122.9575
Hiking trails at the lake include an interpretive nature trail at Sunset Campground and the Lake Shore Loop Trail. Other nearby recreational opportunities include the Snow Mountain Wilderness located east of Lake Pillsbury. The Bloody Rock historic area is located within the wildlife refuge north of the lake as well as the Eel River and the Wild and Scenic Black Butte River. Wildlife.

Geographic entities mentioned:
surface_form: black butte
instance_of: Mountain
countries: United States
coordinates: lat: 44.9044
lon: -111.855
surface_form: black butte
instance_of: Mountain
countries: United States
coordinates: lat: 35.88222222
lon: -115.72083333
surface_form: black butte
instance_of: Mountain
countries: United States
coordinates: lat: 39.7267
lon: -122.872
surface_form: black butte
instance_of: Mountain
countries: United States
coordinates: lat: 41.3663
lon: -122.348
surface_form: black butte
instance_of: Mountain
countries: United States
coordinates: lat: 44.3997
lon: -121.635
A powerhouse was constructed in Potter Valley. It was called the Potter Valley Project or Eel River Project. Later that year, the Snow Mountain Water and Power Company incorporated and took over the project from Van Arsdale's company. By 1908 water was being diverted to the power plant and then to the Russian River.

Geographic entities mentioned:
surface_form: snow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.2915
lon: -70.7093
surface_form: snow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.763333333333
lon: -121.79722222222
surface_form: snow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.1692
lon: -70.8267
It maintains water flow to the hydroelectric plant during times of low water runoff. Pacific Gas and Electric Company (PG&E) acquired the project in 1933. The lake is named for one of the founders of Snow Mountain Water and Power Company. The Pillsbury hydroelectric plant is the only one in the north coast region of California operated by PG&E.

Geographic entities mentioned:
surface_form: snow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.2915
lon: -70.7093
surface_form: snow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.763333333333
lon: -121.79722222222
surface_form: snow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.1692
lon: -70.8267
Morita struggled for many years in comedy, until fellow performer—ventriloquist Hank Garcia—told him to try his luck in Los Angeles. Sally Marr, Lenny Bruce's mother, acted as his agent and manager after he moved to Los Angeles, and booked him in the San Fernando Valley and at the Horn nightclub in Santa Monica.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Not knowing what to do, he went again to ask help from the god of compassion. Then Avalokiteśvara went on the mount Meru, or Sumeru (believed to correspond to today's Mount Kailash), a sacred place for Buddhists, Hindus, Jains and Bönpo. Some say that at the top of the mountain he gathered a handful of barley, others that he extracted five cereals from his own body to offer to the monkey father.

Geographic entities mentioned:
surface_form: Mount Kailash
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 31.066944444444
lon: 81.312777777778
Most of the scattered American remnants made their way to rejoin St. Clair's army on its way toward the Hudson River. Background. General John Burgoyne began his 1777 campaign for control of the Hudson River valley by moving an army of 8,000 down Lake Champlain in late June, arriving near Fort Ticonderoga on July 1. On July 5, General Arthur St.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Mynydd Mawr (disambiguation). cq8dfkctaf9y9imwpk5mh2plmm5r" xml:space="preserve">Mynydd Mawr (Welsh for &quot;big mountain&quot;) is a mountain in North Wales.

Geographic entities mentioned:
surface_form: Mynydd Mawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.0686
lon: -4.182
The route was essentially the same as that used by the Hudson's Bay Company fur brigades, which traded with the local Salish Indians. It followed the Columbia River to the confluence of the Okanogan River, and then up that river's watercourse via Osoyoos, Skaha (Dog) and Okanagan lakes, then using a pass via Monte Creek to Fort Kamloops, at the confluence of the North and South Thompson rivers.

Geographic entities mentioned:
surface_form: Osoyoos
instance_of: Lake
countries: Canada
United States
coordinates: lat: 49.000322222222
lon: -119.44559166667
surface_form: Skaha
instance_of: Lake
countries: Canada
coordinates: lat: 49.416666666667
lon: -119.58333333333
surface_form: Okanagan
instance_of: Lake
countries: Canada
coordinates: lat: 49.920833333333
lon: -119.5
Arennest. Arennest is a hill in Hesse, Germany. It is located nearby Biedenkopf and is covered with forest. It is also a known point of interest for hikers and is featured in regional hiking routes. Hiking. Arennest is part of several regional hiking routes and is known for its forested trails and scenic views. It is featured as a recommended trail destination by local hiking platforms.

Geographic entities mentioned:
surface_form: arennest
instance_of: Mountain
countries: Germany
coordinates: lat: 50.91405
lon: 8.5875916666667
History of soccer in Newcastle, New South Wales. The sport of soccer (association football) has had a long history in the Newcastle, New South Wales and the wider Hunter Region. The area has had a number of teams involved in national competitions from 1978 through to the present day, being represented by the Newcastle Jets in the A-League.

Geographic entities mentioned:
surface_form: Hunter Region
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Distribution and habitat. The tree is endemic to Oaxaca state in southwestern Mexico. It grows in Sierra Madre de Oaxaca pine-oak forests habitat in the Sierra Juárez, a subrange of the Sierra Madre de Oaxaca. &quot;Quercus macdouglallii&quot; is found in high-elevation oak forests and in mixed oak-pine or pine-oak forests between 2,500 and 3000 meters elevation.

Geographic entities mentioned:
surface_form: Sierra Juárez
instance_of: Mountain
countries: Mexico
coordinates: lat: 17.58333333
lon: -96.66666667
Ghazaouet-Nedroma. Ghazaouet-Nedroma is a volcanic field in Algeria. It is in the Tlecmen province. Part of the larger Oranie volcanic field, it has erupted alkali basalts, with one eruption date being 2.1 million years ago.

Geographic entities mentioned:
surface_form: ghazaouet-nedroma
instance_of: Mountain
countries: Algeria
France
coordinates: lat: 35.07
lon: -2
History. First discovered in the sediment of a marine geothermal area near Vulcano, Italy, &quot;Thermotoga maritima&quot; resides in hot springs as well as hydrothermal vents. The ideal environment for the organism is a water temperature of, though it is capable of growing in waters of.

Geographic entities mentioned:
surface_form: Vulcano
instance_of: Mountain
countries: Italy
coordinates: lat: 38.4042
lon: 14.9658
1989 Soviet Air Force Il-76 crash. On October 18, 1989, a Soviet Air Force Ilyushin Il-76, flying from Nasosnaya Air Base in SSR Azerbaijan to Zhovtneve Air Base in SSR Ukraine, crashed into the Caspian Sea. All 57 people on board were killed. The aircraft was carrying paratroopers from the 98th Guards Airborne Division. It is the deadliest aviation accident to have occurred in Azerbaijan.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
It is the deadliest aviation accident to have occurred in Azerbaijan. Accident. On 18 October 1989, a Soviet Air Force Ilyushin Il-76, with the registration CCCP-76569, carrying paratroopers from the 98th Guards Airborne Division, crashed into the Caspian Sea, killing all 57 people on board. The incident is the deadliest aviation accident in Azerbaijan history.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
The incident is the deadliest aviation accident in Azerbaijan history. The flight was part of a routine training exercise taking place near the city of Sumgait, situated along the Caspian Sea coast. The aircraft, en route to carry out a training mission, faced unforeseen technical difficulties shortly after departing from Baku's Heydar Aliyev International Airport.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Lake Frederick (Oklahoma). Lake Frederick is a reservoir in Tillman County, Oklahoma. It is located about 15 miles northeast of the town of Frederick, which owns it. It was constructed in 1974 for flood control and to provide a water supply. It has a total surface area of 878 acres, and a total volume of 9,663 acre-feet. It has about 18 miles of shoreline.

Geographic entities mentioned:
surface_form: lake frederick
instance_of: Lake
countries: United States
coordinates: lat: 34.530555555556
lon: -98.882222222222
It has about 18 miles of shoreline. Anglers can expect to catch a variety of fish including Channel Catfish, Largemouth Bass and Walleye. Facilities around Lake Frederick include boat ramps, boat dock, fishing dock, RV and tent campsites, picnic areas, outdoor grills, showers, restrooms, playground, pavilion, volleyball court, and hiking/biking/ATV trails. Deep Red Creek.

Geographic entities mentioned:
surface_form: lake frederick
instance_of: Lake
countries: United States
coordinates: lat: 34.530555555556
lon: -98.882222222222
Deep Red Creek. The Lake Frederick watershed is located in the northern portion of Tillman County and is approximately 35,907 acres. The primary tributary and major outflow from the lake is Deep Red Creek.

Geographic entities mentioned:
surface_form: lake frederick
instance_of: Lake
countries: United States
coordinates: lat: 34.530555555556
lon: -98.882222222222
The primary tributary and major outflow from the lake is Deep Red Creek. That stream originates just east inside the Comanche County, Oklahoma line south of State Highway 49 and east of State Highway 54, before traveling generally southwest into Kiowa County and eventually Tillman County, joining Lake Frederick from the north.

Geographic entities mentioned:
surface_form: lake frederick
instance_of: Lake
countries: United States
coordinates: lat: 34.530555555556
lon: -98.882222222222
The arc has about forty volcanoes between Alaska and Kamchatka. In the central Aleutians these include from west to east Seguam, Amukta, Chagulak, Yunaska, Herbert, Carlisle, Cleveland, Uliaga, Kagamil, Vsevidof, Recheshnoi, Okmok, Bogoslof, Makushin, Mount Gilbert, Westdahl, Fisher, Shishaldin, Isanotski and Roundtop.

Geographic entities mentioned:
surface_form: Carlisle
instance_of: Mountain
countries: United States
coordinates: lat: 52.8939
lon: -170.054
surface_form: Vsevidof
instance_of: Mountain
countries: United States
coordinates: lat: 53.13
lon: -168.693
surface_form: Recheshnoi
instance_of: Mountain
countries: United States
coordinates: lat: 53.157
lon: -168.539
surface_form: Westdahl
instance_of: Mountain
countries: United States
coordinates: lat: 54.518
lon: -164.65
surface_form: Isanotski
instance_of: Mountain
countries: United States
coordinates: lat: 54.7686
lon: -163.729
surface_form: shishaldin
instance_of: Mountain
countries: United States
coordinates: lat: 54.75
lon: -163.96666666667
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: bogoslof
instance_of: Mountain
countries: United States
coordinates: lat: 53.935833333333
lon: -168.03888888889
surface_form: carlisle
instance_of: Mountain
countries: United States
coordinates: lat: 52.8939
lon: -170.054
surface_form: vsevidof
instance_of: Mountain
countries: United States
coordinates: lat: 53.13
lon: -168.693
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 61.1725
lon: -148.2717
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 40.6244
lon: -115.446
surface_form: roundtop
instance_of: Mountain
countries: United States
coordinates: lat: 42.293888888889
lon: -74.490555555556
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 54.2521
lon: -165.662
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 37.1363688
lon: -118.5982233
An algorithm that processes satellite-derived thermal images of the ground to identify anomalous areas, was developed after the 1996 Pavlof eruption and renamed &quot;Okmok Algorithm&quot; after the 1997 eruption of Okmok, to which it was first applied.

Geographic entities mentioned:
surface_form: Pavlof
instance_of: Mountain
countries: United States
coordinates: lat: 55.419444444444
lon: -161.895
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
Two large caldera-forming eruptions took place during the Holocene, with a volcanic explosivity index (VEI) of 6; the second of these occurred in 43 BCE and caused a volcanic winter that might have changed the history of Egypt. After this second caldera-forming eruption a crater lake formed in the caldera, and drained in one of the largest known floods of the Holocene.

Geographic entities mentioned:
surface_form: crater lake
instance_of: Lake
countries: United States
coordinates: lat: 42.943611111111
lon: -122.10666666667
surface_form: crater lake
instance_of: Lake
countries: United States
coordinates: lat: 46.9382689
lon: -121.8620654
surface_form: crater lake
instance_of: Lake
countries: United States
coordinates: lat: 39.0853
lon: -106.967
While a direct causal link to the Okmok eruption is not proven, and food production recovered in the following years, the longer-term effects on Egypt's food resources of both the famine and the increased interest of the Roman Republic (which was itself affected by a serious crisis), contributed to the final collapse of the Ptolemaic dynasty and the Roman Republic after the 31 BCE Battle of Actium, leading to the Roman Empire.

Geographic entities mentioned:
surface_form: battle
instance_of: Watercourse
countries: United States
coordinates: lat: 44.9266
lon: -93.0291
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
Umnak island is on Cretaceous seafloor; the submerged Umnak oceanic plateau might extend under the island. Southwest of Okmok, a ridge formed by Tertiary volcanic rocks joins the volcano to the rest of Umnak island and the volcanoes Recheshnoi and Vsevidof. Northeast of Okmok is the Idak plateau, an uplifted older volcano. There is no evidence of faulting at Okmok.

Geographic entities mentioned:
surface_form: vsevidof
instance_of: Mountain
countries: United States
coordinates: lat: 53.13
lon: -168.693
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
Large caldera-forming eruptions are unlikely in the near future. Scientific importance. The 1945 eruption threatened Fort Glenn, drawing attention to Okmok and Aleutian volcanoes in general. Interest in Okmok stagnated afterwards until the 1997 eruption renewed scientific attention, which made Okmok one of the best studied Aleutian volcanoes.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
Mount Okmok. Mount Okmok is a volcano on eastern Umnak Island, in the central-eastern Aleutian Islands of Alaska. Part of the Aleutian Volcanic Arc, it was formed by the subduction of the oceanic Pacific Plate under the North American Plate. Okmok is a large shield volcano capped by a wide caldera. The caldera contains numerous cinder cones, their lava flows, and a few lakes.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
surface_form: mount okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
Mount Okmok. Mount Okmok is a volcano on eastern Umnak Island, in the central-eastern Aleutian Islands of Alaska. Part of the Aleutian Volcanic Arc, it was formed by the subduction of the oceanic Pacific Plate under the North American Plate. Okmok is a large shield volcano capped by a wide caldera. The caldera contains numerous cinder cones, their lava flows, and a few lakes.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
Part of the Aleutian Volcanic Arc, it was formed by the subduction of the oceanic Pacific Plate under the North American Plate. Okmok is a large shield volcano capped by a wide caldera. The caldera contains numerous cinder cones, their lava flows, and a few lakes. Okmok erupts mainly basaltic lava, mostly from the cones within the caldera. Activity began in the Pleistocene.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
After this second caldera-forming eruption a crater lake formed in the caldera, and drained in one of the largest known floods of the Holocene. Okmok is one of the most active volcanoes of North America; numerous eruptions have produced lava flows within the caldera, and the 1817 eruption destroyed an Aleut village. The last eruption was in 2008 and produced several new vents in the caldera.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
The last eruption was in 2008 and produced several new vents in the caldera. This eruption, which occurred with little forewarning, yielded a volcanic cloud that produced volcanic ash fall around Okmok. The volcano is monitored by the Alaska Volcano Observatory (AVO). Geography and geomorphology.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
The volcano is monitored by the Alaska Volcano Observatory (AVO). Geography and geomorphology. Okmok is on northeastern Umnak Island, a remote location in the central Aleutian Islands, from Anchorage. The former Fort Glenn Army Air Base is on the eastern side of the volcano. Some unmaintained trails and dirt roads lead around the mountain.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
Umnak Island is largely uninhabited, but fishery vessels sail around it all year round and a major North Pacific aviation route passes in the area. Dutch Harbor on Unalaska Island, the most important production place of seafood in the United States, is from Okmok. The name &quot;Okmok&quot; was applied to the mountain by Dunn 1908, who had discovered the caldera two years before.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
Dutch Harbor on Unalaska Island, the most important production place of seafood in the United States, is from Okmok. The name &quot;Okmok&quot; was applied to the mountain by Dunn 1908, who had discovered the caldera two years before. The Aleut name of the caldera is; the second word means &quot;to be thick&quot;. An alternative name for the volcano is &quot;Zoomie&quot;.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
Its slopes are mostly covered by pyroclastic flow deposits from the second caldera-forming eruption. There are more than twenty Pleistocene-Holocene cones on the outer flank of Okmok, including the high Tulik (highest point of Okmok) on the southern and Jag Peak on the southwestern flank. Glacial valleys, gullies, and amphitheatre-shaped valleys with widths reaching cut into the slopes.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
Numerous creeks radially drain the edifice to the Bering Sea and Pacific Ocean: From north clockwise they include Crater Creek, Antler Creek, Kansas Creek, Missouri Creek, Ginger Creek, Colorado Creek and Delaware Creek. Crater Creek has formed a fan around Cape Tanak, as mudflows from Okmok are preferentially channeled through this creek. Caldera.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
Arc-shaped structures out from the northern and eastern margins indicate the caldera is actually two nested calderas. Lava flows, pyroclastic flows and scoria deposits crop out in the steep cliffs that form the inner wall of the caldera. The highest point on the caldera rim is the high &quot;Mount Okmok&quot; on the northern rim. The Global Volcanism Program reports a height of.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
surface_form: mount okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
Umnak island is on Cretaceous seafloor; the submerged Umnak oceanic plateau might extend under the island. Southwest of Okmok, a ridge formed by Tertiary volcanic rocks joins the volcano to the rest of Umnak island and the volcanoes Recheshnoi and Vsevidof. Northeast of Okmok is the Idak plateau, an uplifted older volcano. There is no evidence of faulting at Okmok.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
Southwest of Okmok, a ridge formed by Tertiary volcanic rocks joins the volcano to the rest of Umnak island and the volcanoes Recheshnoi and Vsevidof. Northeast of Okmok is the Idak plateau, an uplifted older volcano. There is no evidence of faulting at Okmok. There are two tectonic stress regimes at Okmok, a northwest-southeast regional regime and a radial local one.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
Shallower pools of basaltic andesite magma are rarely involved, but played a role during the 2008 eruption. With rare exceptions (the Cone D immediately after the Okmok II eruption and the 2008 eruption), the magma is deflected sideward before reaching the surface via ring faults, thus erupting at the margin of the caldera instead of at its center. Composition.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
Vents in the northwestern sector of the caldera produce more mafic magmas than those in the southeastern. Okmok is the principal source of prehistoric obsidians in the Aleutians, as far as the Alaska Peninsula more than from the volcano; the so-called &quot;Group I&quot; obsidian in Alaskan archaeological sites may come from there.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
Water and ice interaction has converted some of the basalts to palagonite. The rocks have a typical composition for volcanic arc magmas, with enrichment of elements presumably derived from subducted sediments and sediment-derived fluids. The subducting plate releases fluids into the overlying mantle, which ascends under Okmok and melts at temperatures of to form basaltic magmas.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
Mean annual temperatures are. There is frequent snow cover, except on recent lava flows. The mountain obstructs the airflow, thus on the eastern (lee) side cloud cover is less. The closest weather station is at Dutch Harbor, and may not reflect the climate at Okmok. During the ice ages >55,000 and 24,000–12,000 years ago, the mountain was covered by glaciers.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
The upper parts of the edifice above are bare. Animals include red foxes, reindeer and numerous birds, and marine life occurs in the seas surrounding Umnak. Eruption history. Volcanic activity on northeastern Umnak Island commenced about 2.1–1.7 million years ago, eventually giving rise to Okmok volcano. A single rhyolitic flow was emitted on the northern flank during the Pleistocene.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
Older volcanic features, such as the Pleistocene Tulik, either formed in ice or show traces of glacial erosion. Effusive eruptions characterize the activity of the volcano, except for the two large caldera-forming eruptions during the Holocene: &quot;Okmok I&quot; about 12,000 years ago and &quot;Okmok II&quot; in 43 BCE.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
After the 43 BCE eruption, the rate was about one eruption every 75 years. The magma supply rate since that eruption amounts to. More than 60 tephra layers were emplaced after the Okmok I eruption. Seismic swarms and increased seismicity occurred in 2001 and 2009. Okmok I eruption. The Okmok I eruption 12,000 years ago is poorly documented, but some general features can be established.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
Caldera collapse occurred only late in the sequence, and a debris avalanche formed on the northwestern flank. The eruption reached a VEI of 6. Its volume was probably twice as large as that of the Okmok II eruption, albeit with significant uncertainty. Before the caldera collapse, Okmok might have reached a height of.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
The fallout was emplaced in three distinct units, with a brief break between the first two that lasted days to months. The fallout deposits are up to a meter thick, with the first unit being emplaced north and the second and third units southeast of Okmok. Then, a change in magma composition from dacite to andesite heralded a dramatic increase of activity.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
The eruption was notable for its lack of forewarning; precursory activity lasted a very short time and activity commenced by surprise. The Alaska Volcano Observatory (AVO) was alerted by the US Coast Guard after the latter received requests for assistance from a family living on the eastern side of Okmok. Alerted by noises, the population of Umnak fled, first by helicopter then by boat.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
The 1958 eruption submerged them beneath a lake, during the 2008 eruption they were flooded completely although later some re-emerged. Additional hot springs were found in creeks entering the Cone D lake. A field of geysers and sinter deposits may be linked to Okmok, and the caldera has been evaluated as a site for the generation of geothermal power. Hazards and monitoring.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
A field of geysers and sinter deposits may be linked to Okmok, and the caldera has been evaluated as a site for the generation of geothermal power. Hazards and monitoring. Okmok has had large caldera-forming eruptions. Its eruptions constitute a threat to air travel, which despite the remoteness of the volcano is heavy in the region.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
The AVO operates seismometers and equipment measuring deformation of the edifice, which relay their information to the AVO laboratories in Fairbanks and Anchorage. AVO publishes a volcano alert level for Okmok. The volcano is also the site of an array of infrasound detectors, which can also record activity at other Aleutian volcanoes.

Geographic entities mentioned:
surface_form: okmok
instance_of: Mountain
countries: United States
coordinates: lat: 53.396944444444
lon: -168.16611111111
These rivers follow a Cameroon regime, experiencing a period of high waters during the wet season and a period of low waters in the dry period. The rivers all form part of the Atlantic basin. The Mbam River runs along the border with the Centre and Southeast Provinces. The Nkam is the name for the headwaters of the Wouri River, which flow from the West's Bamboutos Mountains.

Geographic entities mentioned:
surface_form: Mbam River
instance_of: Watercourse
countries: Cameroon
coordinates: lat: 4.385436
lon: 11.271286
The rivers all form part of the Atlantic basin. The Mbam River runs along the border with the Centre and Southeast Provinces. The Nkam is the name for the headwaters of the Wouri River, which flow from the West's Bamboutos Mountains. The eastern branch through the area rises northwest of Bangangté, and the western branch forms the border with the Littoral Province southwest of Bafang.

Geographic entities mentioned:
surface_form: Nkam
instance_of: Watercourse
countries: Cameroon
coordinates: lat: 5.062218
lon: 10.029659
surface_form: Wouri River
instance_of: Watercourse
countries: Cameroon
coordinates: lat: 4.0833
lon: 9.7
These headwaters are subject to seasonal flooding. The Noun River, a tributary of the Sanaga, flows from the Centre Province, around Bafoussam, and to the Bamendjing Reservoir. This man-made lake is created by a dam on the Noun River, which helps regulate the Sanaga at Edéa in the Littoral Province and is thus an important component in Cameroon's supply of hydroelectric power.

Geographic entities mentioned:
surface_form: Sanaga
instance_of: Watercourse
countries: Cameroon
coordinates: lat: 3.5593388888889
lon: 9.652175
Most of the West's lakes are crater lakes formed from collapsed volcanoes. Such lakes exist at Balent, Banéfo, Doupé, and near Foumban. Many of these still have active volcanoes at their bottoms, particularly in the northwest on the Western High Plateau. One example is Lake Baleng, northeast of Bafoussam, and the twin lakes of Foumbot.

Geographic entities mentioned:
surface_form: Western High Plateau
instance_of: Plateau
countries: Cameroon
coordinates: lat: 6.5
lon: 10.5
West of the Cameroon Mountains lies the Western High Plateau, with elevations of 1,000-2,500 metres. South of the fault, the land descends in steps until levelling off at the South Cameroon Plateau. Here, terrain is gentler, with large hills separated by deep valleys. Climate. High elevations and moderate to high humidity give the West one of Cameroon's more pleasant climates.

Geographic entities mentioned:
surface_form: South Cameroon Plateau
instance_of: Plateau
countries: Cameroon
coordinates: lat: 5
lon: 12
Human beings have inhabited the West since prehistoric times, as evidenced by archaeological finds at Galima and Foumban. Bamileke groups likely entered the area from the Adamawa Plateau in the 17th century, probably fleeing Fulbe (Fula) slave raids. They originally settled in what is now Bamum territory, but the Bamum forced them across the Noun in a series of wars in the 18th century.

Geographic entities mentioned:
surface_form: Adamawa Plateau
instance_of: Plateau
countries: Cameroon
coordinates: lat: 9.8
lon: 14.08333333
Henry Dumaresq (colonial settler). Lieutenant-Colonel Henry Dumaresq (c. 1792-1838) was a military officer of the era of the Napoleonic Wars, colonial government official, and early colonial settler of New South Wales. He was associated with the Upper Hunter Valley and Port Stephens, and was one of the first to take up land around Armidale. Early life and military service.

Geographic entities mentioned:
surface_form: Upper Hunter Valley
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
According to witnesses, all of the rebels captured by the Burundian Army were summarily executed and buried in mass graves. All persons seeking shelter in the bush or bearing scarification were deemed &quot;rebels&quot; by the government and hunted down. This provoked an exodus of thousands of refugees towards Zaire and Tanzania, particularly those who had resided on the coast of Lake Tanganyika.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
The Ordus lived on the Kherlen River but later moved to the area now known as Ordos. After Dayan Khan, whose father was the Jinong, unified the Mongolian Plateau, his descendants assumed the position until 1949. During the Qing dynasty the Jinong also served as the chief of the Yeke Juu League () or a banner in it.

Geographic entities mentioned:
surface_form: Mongolian Plateau
instance_of: Plateau
countries: Mongolia
People's Republic of China
Russia
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 107
It is located in the La Paz Department, Pacajes Province, Calacoto Municipality. Pukara lies north of the Anallajsi volcano, north-west of the mountain Pichaqa and south-west of the mountains Urqipi and Churi Willk'i. It is situated at the Jalsuri River, a right affluent of the Achuta River. The village of Pukara &quot;(Pucara)&quot; lies at its feet, south-east of it.

Geographic entities mentioned:
surface_form: Pichaqa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.8097
lon: -68.8589
surface_form: Urqipi
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.7739
lon: -68.9222
surface_form: Churi Willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.7817
lon: -68.9206
Pukara (Pacajes). Pukara (Aymara for fortress, Hispanicized spelling &quot;Pucara&quot;) is a mountain in the Andes of Bolivia. It is located in the La Paz Department, Pacajes Province, Calacoto Municipality. Pukara lies north of the Anallajsi volcano, north-west of the mountain Pichaqa and south-west of the mountains Urqipi and Churi Willk'i.

Geographic entities mentioned:
surface_form: pukara (pacajes)
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.7944
lon: -68.9267
Pukara (Pacajes). Pukara (Aymara for fortress, Hispanicized spelling &quot;Pucara&quot;) is a mountain in the Andes of Bolivia. It is located in the La Paz Department, Pacajes Province, Calacoto Municipality. Pukara lies north of the Anallajsi volcano, north-west of the mountain Pichaqa and south-west of the mountains Urqipi and Churi Willk'i.

Geographic entities mentioned:
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.7944
lon: -68.9267
It is located in the La Paz Department, Pacajes Province, Calacoto Municipality. Pukara lies north of the Anallajsi volcano, north-west of the mountain Pichaqa and south-west of the mountains Urqipi and Churi Willk'i. It is situated at the Jalsuri River, a right affluent of the Achuta River. The village of Pukara &quot;(Pucara)&quot; lies at its feet, south-east of it.

Geographic entities mentioned:
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.7944
lon: -68.9267
Cando (river). The Cando is a river of eastern San Marino. It rises to the east of Monte San Cristoforo, flowing northeast to join with the Marano near the town of Faetano.

Geographic entities mentioned:
surface_form: Monte San Cristoforo
instance_of: Mountain
countries: San Marino
coordinates: lat: 43.906944444444
lon: 12.464722222222
Mont Abourasséin. Mont Abourasséin is a mountain in Central Africa. It is 1113 metres tall and stands on the international boundary between the Central African Republic and South Sudan. It is in the Haute-Kotto prefecture of the Central African Republic and the Western Bahr el Ghazal state of South Sudan.

Geographic entities mentioned:
surface_form: mont abourasséin
instance_of: Mountain
countries: South Sudan
Central African Republic
coordinates: lat: 8.60583333
lon: 24.27944444
History. In 1916 Ray K. Phillips established the Cedar Island Camp for girls on Fourth Lake, near Inlet, New York. In 1920 the Cedar Island Corporation, of which she was a member, purchased the Antlers Hotel on Raquette Lake and she moved the girls' camp to the Antlers property, changing the name to Raquette Lake Girls Camp. Construction on the present girls' camp site began in 1922.

Geographic entities mentioned:
surface_form: Raquette Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.833333333333
lon: -74.65
In addition, a few recreational excursions are scheduled to the Olympic Training Center in Lake Placid, the Adirondack Museum in Blue Mountain Lake, the Baseball Hall of Fame in Cooperstown, Six Flags Great Escape & Splashwater Kingdom in Queensbury and a local water park. Special trips for teens include excursions to Montreal, New Hampshire, the Berkshires, and deep-lake fishing in Lake Ontario.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Water course. The headwaters of the Chattooga River are located southwest of Cashiers, North Carolina, and it stretches to its confluence with the Tallulah River within Lake Tugalo, which was created by the Tugalo Dam. The Chattooga begins in southern Jackson County, North Carolina, and flows southwestward between northwestern Oconee County, South Carolina, and eastern Rabun County, Georgia.

Geographic entities mentioned:
surface_form: Lake Tugalo
instance_of: Lake
countries: United States
coordinates: lat: 34.73
lon: -83.352
The rock is mostly granite. Geologists believe that the Chattooga may have made one direction change during its life. Originally, it probably flowed southwesterly into the Chattahoochee River and on to the Gulf of Mexico. At some point, the Savannah River eroded its northern headland until it captured the Chattooga and diverted its waters to the Atlantic.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Bunda District. Bunda is one of the seven districts of Mara Region in the United Republic of Tanzania, East Africa. It is bordered to the north by the Musoma Rural District and Butiama District, to the east by Serengeti District, to the south by Bariadi District and Busega District, and to the west by Lake Victoria.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
A chalet called &quot;Chata M. R. Štefánika&quot; is situated under the summit (1,740 m). Ďumbier, as well as the nearby Chopok mountain, can be reached following the hiking trails either from the north (from the Demänovská dolina and Jánska dolina valleys) or from the south (from the bus stop Trangoška).

Geographic entities mentioned:
surface_form: Chopok
instance_of: Mountain
countries: Slovakia
coordinates: lat: 48.943055555556
lon: 19.593055555556
surface_form: chopok
instance_of: Mountain
countries: Slovakia
coordinates: lat: 48.943055555556
lon: 19.593055555556
Ďumbier. Ďumbier (2,043 m or 6,703 ft) is the highest mountain in the Low Tatra range, in central Slovakia. Despite the remains of medieval mines (gold, iron, antimony), the massif is now protected as a part of the Low Tatras National Park. The easily accessible summit offers a scenic view of High Tatra, Liptov and the valley of Hron. A chalet called &quot;Chata M. R.

Geographic entities mentioned:
surface_form: ďumbier
instance_of: Mountain
countries: Slovakia
coordinates: lat: 48.936611111111
lon: 19.640169444444