Sarmila/GeoWiki-Features huggingface dataset:
Church sent a small force ashore near present-day St. Stephen, New Brunswick, where they destroyed a house and raided a nearby Maliseet encampment, killing one Indian. Church then separated the warships, sending them to blockade the Digby Gut in the hopes of capturing a French supply ship, while the bulk of the expedition sailed for Grand Pré.

Geographic entities mentioned:
surface_form: Digby Gut
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.67652778
lon: -65.75888889
The lake covers an area of over 35 hectares, is surrounded by diverse floral vegetation, and provides a natural habitat for 26 species of water birds, fish, and various wildlife, including wolves, domestic cats, and hedgehogs. The lake is entirely man-made, created during the 1940s, and fed by the flow of the Sig River and Sarno Valley.

Geographic entities mentioned:
surface_form: Sig River
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 35.319166666667
lon: -0.41638888888889
The lake is entirely man-made, created during the 1940s, and fed by the flow of the Sig River and Sarno Valley. It was constructed to manage the floodwaters of the Mekerra River, thus mitigating the risk of destructive floods that used to threaten the city of Sidi Bel Abbès. The lake occupies a natural basin carved into sedimentary terrain, which is sealed downstream by an earthen dam.

Geographic entities mentioned:
surface_form: mekerra river
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 35.319166666667
lon: -0.41638888888889
Lake Sidi Mohamed Benali. Lake Sidi Mohamed Benali is a lake located in western Algeria, within the Sidi Bel Abbès Province, specifically on the lands of Ain Thrid municipality, approximately 1.7 kilometers from the city of Sidi Bel Abbès and near the East–West Highway.

Geographic entities mentioned:
surface_form: lake sidi mohamed benali
instance_of: Lake
countries: Algeria
France
coordinates: lat: 35.2425
lon: -0.6475000000000001
HMS Loch Morlich. HMS &quot;Loch Morlich&quot; was a Loch-class frigate that never saw service with the Royal Navy. Ordered during World War II, she saw service instead with the Royal Canadian Navy in the Battle of the Atlantic. She was named for Loch Morlich in Scotland. After the war she was returned to the Royal Navy and she was sold to the Royal New Zealand Navy and renamed &quot;Tutira&quot;.

Geographic entities mentioned:
surface_form: Loch Morlich
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.1631
lon: -3.7129
As Darryle Marble, a speaker at the Flat Earth Conference, told his audience, after watching hours of YouTube conspiracy videos on Sandy Hook, 11, false flags, the Bilderbergers, Rothschilds, Illuminati – &quot;Each thing started to make that much more sense.

Geographic entities mentioned:
surface_form: Sandy Hook
instance_of: Landform
countries: United States
coordinates: lat: 40.452891
lon: -73.995237
Army of West Virginia. The Army of West Virginia served in the Union Army during the American Civil War and was the primary field army of the Department of West Virginia. It campaigned primarily in West Virginia, Southwest Virginia and in the Shenandoah Valley. It is noted for having two future U.S. presidents serve in its ranks: Rutherford B.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Thaw Hill. Thaw Hill is a cinder cone in northwestern British Columbia, Canada. It is one of the volcanoes in the central portion of the Mount Edziza volcanic complex and last erupted during the Pleistocene period.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
Hold Caldron Mill. Hold Caldron Mill is a historic building in Nawton, North Yorkshire, a village in England. A watermill was located at this location on the Hodge Beck in the 17th century, but it burned down in 1704. It was rebuilt in 1734 by Matthew Foord, the date inscribed on a stone in the current cornmill.

Geographic entities mentioned:
surface_form: Hodge Beck
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 54.23333
lon: -0.91667
Cerro Negro. Cerro Negro is an active volcano in the Cordillera de los Maribios mountain range in Nicaragua, about from the village of Malpaisillo. It is a very new volcano, the youngest in Central America, having first appeared in April 1850.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
It consists of a gravelly basaltic cinder cone, which contrasts greatly with the surrounding verdant hillsides, and gives rise to its name, which means Black Hill. Cerro Negro has erupted frequently since its first eruption. One unusual aspect of several eruptions has been the emission of ash from the top of the cone, while lava erupts from fractures at the base.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
Cerro Negro has erupted frequently since its first eruption. One unusual aspect of several eruptions has been the emission of ash from the top of the cone, while lava erupts from fractures at the base. Cerro Negro is a polygenetic cinder cone that is part of the Central America Volcanic Arc, which formed as a result of the Cocos Plate subducting under the Caribbean Plate, at a rate of per year.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
It is the largest and southernmost of four cinder cones that have formed along a NW-SE trend line in the Cordillera de los Maribios mountain range. Despite its youth, Cerro Negro has been one of the most active volcanoes in Nicaragua, with its latest eruption occurring in 1999. Since its birth in 1850, it has erupted approximately 23 times. Eruptive history.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
Since its birth in 1850, it has erupted approximately 23 times. Eruptive history. The first recorded eruption of Cerro Negro occurred on April 13, 1850 and volcanic activity lasted until May 27. Central vent and explosive eruptions transpired, with lava flow and damage to land and property.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
Finally, the lava volume was recorded to be 5.4 x 10 and the tephra volume was 6.5 x 105 m3. Cerro Negro's second eruption took place on November 14, 1867 and volcanic activity lasted until November 30. Radial fissure and explosive eruptions occurred, with some lava flows, along the NE-SW trend line fissure.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
Radial fissure and explosive eruptions occurred, with some lava flows, along the NE-SW trend line fissure. The VEI was also recorded at 2 (Strombolian/Vulcanian), and the tephra volume was 8.6 x 106 m3. The third eruption of Cerro Negro occurred 32 years later and lasted from November 22 to November 29, 1899. Explosive eruptions resulted in damaged land, and the VEI was also recorded as a 2.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
Mudslides also resulted in increased damage to the land, but there were no fatalities because they did not flow over any villages or towns. Although the VEI was yet again 2, the tephra volume was a recorded 2.8 x 106 m3. Five years later, Cerro Negro erupted again from June 20–30, 1919, with explosive eruptions resulting in a VEI of 2. No tephra or lava volumes were recorded at this time.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
No tephra or lava volumes were recorded at this time. Just four years after that, from October 23 until December 11, 1923, Cerro Negro erupted along the summit and upper north flank. Central vent and radial fissure explosions erupted during this time, and lava flows were recorded in this VEI 3 sub-plinian eruption.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
It was the largest eruption in the history of the volcano, with the lava volume being 1.0 x 107 m3 and the tephra volume being 3.6 x 107 m3. Cerro Negro erupted next on February 10, 1929, and volcanic activity lasted until March. Flank (excentric) vent and radial fissures also explosively erupted, resulting in excessive lava flows.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
The volume of lava erupted was recorded at only 1.0 x 105 m3 in the VEI 2 eruption. Eruptions of 1947, 1948 and 1950. Another 18 years passed before Cerro Negro erupted again, but on July 9, 1947 the volcano had its largest eruption to date. The VEI was recorded at 3 along the summit and NE flank, with the eruptive characteristics including central vent eruption, flank venting, and lava flows.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
The recorded lava volume was 3.8 x 106 m3 and the recorded tephra volume was 3.1 x 107 m3. Less than one year later, on March 31, 1948, Cerro Negro recorded another Strombolian eruption (VEI 2) from its central vent. No lava or tephra volumes were recorded, however. A similar eruption occurred in June 1949, with the VEI 2 eruption exploding from the central vent.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
No lava or tephra volumes were recorded, however. A similar eruption occurred in June 1949, with the VEI 2 eruption exploding from the central vent. Another sub-plinian VEI 3 explosive vulcanian eruption occurred from Cerro Negro's central vent from November 21 to December 17, 1950. Lava flows resulted, but evacuation was unnecessary.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
The lava volume was 1.0 x 105 m3 and the tephra volume was 3.8 x 107 m3 for this particular eruption. 1954 eruption. In February 1954 another VEI 2 Strombolian eruption exploded out of Cerro Negro's central vent, but lava and tephra volumes were not recorded. Three years later from September 4–24, 1957, a VEI of 2 was recorded via the summit and east flank of Cerro Negro.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
This particular VEI was determined to be level 3 after radial fissure and central vent eruptions occurred. Land damage was caused to the surrounding land via lava flows, with the volume of the lava recorded at 5.2 x 106 m3 and the tephra volume recorded at 3.4 x 107 m3. Cerro Negro's NE-flank fissure erupted next on October 25, 1961.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
Cerro Negro's NE-flank fissure erupted next on October 25, 1961. Although radial fissure eruption and lava flow was characteristic of this particular eruption, the VEI was only recorded as a 1, and no lava or tephra volumes were recorded. It was the smallest Cerro Negro eruption to date. Another eruption from the central vent occurred on March 21, 1962 and lasted until early April.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
It was the smallest Cerro Negro eruption to date. Another eruption from the central vent occurred on March 21, 1962 and lasted until early April. The VEI was recorded as 2, and lava flows were observed, although no land damage was witnessed. Exactly one year later, a VEI 1 eruption occurred from the central vent of Cerro Negro on March 21, 1963. 1968 eruption.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
Exactly one year later, a VEI 1 eruption occurred from the central vent of Cerro Negro on March 21, 1963. 1968 eruption. The volcanic activity from October 23 until December 10, 1968 marked the formation of the Cristo Rey crater, when the summit and south flank of Cerro Negro erupted with a sub-plinian VEI of 3. The new vent formed a lava flow 750m long and 600m wide and a thickness of 3m.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
Additional larger-scale evacuations Nicaragua's 2nd largest city, León, recorded ash falls of over 1 cm thick. Lava flows advanced at a rate of 23 m/day, and it caused additional land damage as the lava poured from three of Cerro Negro's craters, fountaining to heights of 30m into the air. The eruptive ash columns reached heights of 2.3 to 4.8 km.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
1969 eruption. Another small-scale VEI 1 eruption took place after the central vent exploded from December 19–29, 1969. But two years later from February 3–14, 1971, the towns surrounding Cerro Negro were again evacuated due to the sudden sub-plinian VEI 3 eruption of the summit and the formation and eruption of a new eastern flank.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
1992 eruption. Over 20 years passed, and the Cerro Negro volcano was at peace until one of the volcano's largest eruptions occurred on April 9, 1992. Volcanic activity lasted for a total of five days, with the main sub-plinian eruption (VEI 3) occurring over a two-day time period, producing an ash column that was roughly seven kilometers high.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
By July 19, all volcanic activity ceased for a period of 95 days. By mid-November, the hiatus ended and the second phase commenced. Eruptions continued for a period of thirteen days and lasted until December 3, 1995. During this time, the eruptions were larger, and volcanic bombs and blocks up to two meters in diameter were ejected from Cerro Negro.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
1999 eruption. The last volcanic activity at Cerro Negro occurred on August 5, 1999 and lasted for a total of two days. Three earthquakes (5.2) occurred in three hours, which triggered a small-scale eruption of the volcano. It was the first time in the history of Cerro Negro that large-magnitude earthquakes preceded the eruption.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
Additionally, the tephra volume was only in the 106m3 range. It was concluded that the volcanic activity of Cerro Negro in 1999 was tectonically-induced, and had three earthquakes not occurred, the eruption would have also not occurred. The most recent eruptions at Cerro Negro occurred in August 1999, although strong seismic activity was registered in early 2004.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
Following the 1999 eruption, the summit crater and fissures created from this eruption are currently the main source of volcanic gas flux today. It is estimated that the total CO2 output of Cerro Negro is conservatively estimated to be 2,800 t d-1.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
It is estimated that the total CO2 output of Cerro Negro is conservatively estimated to be 2,800 t d-1. Although the Cerro Negro volcano has only been around for a period of 159 years, it has erupted at least 23 times, which is highly active compared to most volcanoes. This historical growth of the volcano has allowed for documentation of the growth of this volcano over time.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
It was discovered that the timing of future eruptions is correlated with the volume of the previous significant eruption. Since there have been steady-state eruptions since 1900, a Cerro Negro Time-Volume Prediction Model was made. Although a small-scale eruption did occur in 1999, another larger-scale eruption is expected to occur in the immediate future.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
Since there have been steady-state eruptions since 1900, a Cerro Negro Time-Volume Prediction Model was made. Although a small-scale eruption did occur in 1999, another larger-scale eruption is expected to occur in the immediate future. Cerro Negro does not differ from most volcanoes, in that numerous hazards are associated with volcanic activity.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
Cerro Negro does not differ from most volcanoes, in that numerous hazards are associated with volcanic activity. These hazards include lava flows, mudslides, pyroclastic flows, and earthquakes, but the biggest hazard of Cerro Negro is the effects of the ash and tephra fallouts.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
These hazards include lava flows, mudslides, pyroclastic flows, and earthquakes, but the biggest hazard of Cerro Negro is the effects of the ash and tephra fallouts. Currently, Cerro Negro is being monitored by the Nicaraguan Seismic Network, which is affiliated with INETER (Instituto Nicaragüense de Estudios Territoriales).

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
Currently, Cerro Negro is being monitored by the Nicaraguan Seismic Network, which is affiliated with INETER (Instituto Nicaragüense de Estudios Territoriales). These programs have a total of 36 stations throughout Nicaragua, and they each have a monitoring station on Cerro Negro.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
Seismic activity, gas concentrations, surface deformation, and temperature fluctuations are all carefully watched in order to mitigate the effects of a possible eruption. As Cerro Negro lies in a less-populated area of Nicaragua, there is less volcanic risk to human life compared to many of the other volcanoes in the world.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
As Cerro Negro lies in a less-populated area of Nicaragua, there is less volcanic risk to human life compared to many of the other volcanoes in the world. Mudslides and pyroclastic flows that come from Cerro Negro are not in the direct path of major cities or towns.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
Mudslides and pyroclastic flows that come from Cerro Negro are not in the direct path of major cities or towns. Nevertheless, the eruptions of Cerro Negro have been known to cause catastrophic damage to buildings and farmland, due to the widespread ash falls and tephra fallouts.

Geographic entities mentioned:
surface_form: cerro negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
It is operated by the Michigan Department of Natural Resources. Wagner Falls. Wagner Falls is a cascade created by Wagner Creek as it falls over a stratum of erosion-resistant dolomite. The creek drops into a shallow gorge containing the Anna River. The Anna River then flows northward into Lake Superior.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
The Maratha Military Landscapes of India are a group of 12 forts that were occupied and developed by the Maratha rulers between the 17th and 19th-century. These include Salher, Shivneri Fort, Lohagad, Khanderi, Raigad Fort, Rajgad Fort, Pratapgad, Suvarnadurg, Panhala Fort, Vijaydurg Fort, Sindhudurg Fort, all located in Maharashtra and Gingee Fort in Tamil Nadu.

Geographic entities mentioned:
surface_form: Salher
instance_of: Mountain
countries: India
coordinates: lat: 20.72472222
lon: 73.94277778
Maharashtra has more than 390 forts, out of which only 11 forts were selected for this list along with one fort in Tamil Nadu. These forts span across the diverse topographies of the Sahyadri Range, Deccan Plateau, Konkan Coast, and the Eastern Ghats.

Geographic entities mentioned:
surface_form: Deccan Plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Erebus hotspot. The Erebus hotspot is a volcanic hotspot responsible for the high volcanic activity on Ross Island in the western Ross Sea of Antarctica. Its current eruptive zone, Mount Erebus, has erupted continuously since its discovery in 1841. Magmas of the Erebus hotspot are similar to those erupted from hotspots at the active East African Rift in eastern Africa.

Geographic entities mentioned:
surface_form: Mount Erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
Magmas of the Erebus hotspot are similar to those erupted from hotspots at the active East African Rift in eastern Africa. Mount Bird at the northernmost end of Ross Island and Mount Terror at its eastern end are large basaltic shield volcanoes that have been potassium-argon dated 3.8&ndash;4.8 and 0.8&ndash;1.8 million years old. About.

Geographic entities mentioned:
surface_form: Mount Bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Some spectacular scenery can be found along the route, including Thor's Cave, Wetton Hill and Beeston Tor. Many consider that this section bears comparison with the better-known Dovedale a few miles to the east. (The National Trust own several of these sites, as part of their South Peak Estate.)
The Old Light Railway Hotel at Hulme End is now called the Manifold Inn.

Geographic entities mentioned:
surface_form: Dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
Because its drainage basin includes areas both north and south of the Equator, its flow is stable, as there is always at least one part of the river experiencing a rainy season. The sources of the Congo are in the highlands and mountains of the East African Rift, as well as Lake Tanganyika and Lake Mweru, which feed the Lualaba River, which then becomes the Congo below Boyoma Falls.

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
surface_form: Lake Mweru
instance_of: Lake
countries: Zambia
Democratic Republic of the Congo
coordinates: lat: -9.1666666666667
lon: 28.5
The Congo flows generally toward the northwest from Kisangani just below the Boyoma Falls, then gradually bends southwestward, passing by Mbandaka, joining with the Ubangi River and running into the Pool Malebo (Stanley Pool).

Geographic entities mentioned:
surface_form: Pool Malebo
instance_of: Lake
countries: Republic of the Congo
Democratic Republic of the Congo
coordinates: lat: -4.2819444444444
lon: 15.488611111111
The &quot;Kwilu River&quot; originates in the hills near the Angolan border and enters the Congo some 100 km upstream from Matadi. The other is the Inkisi River, that flows in a northerly direction from the Uíge Province in Angola to the confluence with the Congo at &quot;Zongo&quot; some downstream from the twin capitals.

Geographic entities mentioned:
surface_form: Inkisi River
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: -8.52882
lon: 22.52485
In terms of aquatic life, the Congo River Basin has a very high species richness and among the highest known densities of endemics., almost 800 fish species have been recorded from the Congo River Basin (not counting Lake Tanganyika, which is connected but ecologically very different), and large sections remain virtually unstudied.

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
In 1831, it had a population of 17,471. It was one of 12 wapentakes of the old North Riding of Yorkshire, and it contained the parishes of Arkengarthdale, Barningham, Bowes, Brignall, Easby, Forcett, Gilling, Hutton Magna, Kirby Ravensworth, Marrick, Marske, Melsonby, Romaldkirk, Stanwick, Wycliffe, Rokeby, and Startforth.

Geographic entities mentioned:
surface_form: Arkengarthdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.45
lon: -2.034
Architecture. The temple is located in Adiramapattinam, a small town in Thanjavur district of Tamil Nadu. The town faces the Bay of Bengal and since the shrine of Amman, faces west, the deity is called &quot;Kadal Partha Nayagi&quot; (the deity facing the sea). The temple complex covers around one acre and can be entered through a three-tiered gopuram, the main gateway.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
The unincorporated communities of Nichols Shore Acres, Plummer Point, Shangri La Point, and Winnebago are located within the town, as is part of the census-designated place of Butte des Morts. Geography. According to the United States Census Bureau, the town has a total area of, of which is land and, or 84.02%, is water, consisting of a portion of Lake Winnebago. History.

Geographic entities mentioned:
surface_form: Lake Winnebago
instance_of: Lake
countries: United States
coordinates: lat: 44.0169756
lon: -88.4095327
During the Cold War, the neutral Austrian government used it to hold conferences and to host international guests, among them US President Richard Nixon, who on his way to Moscow met there with Chancellor Bruno Kreisky on 20 May 1972. Since 1993 it has been the home of the Salzburg casino, which used to be situated on the Mönchsberg.

Geographic entities mentioned:
surface_form: Mönchsberg
instance_of: Mountain
countries: Austria
coordinates: lat: 47.796524
lon: 13.040397
Thanks to the greater power generation he brought about. In 1922, he succeeded in persuading Paul Schwarzkopf to found the Plansee metal works. He founded an oil plant to exploit natural resources and several wood processing companies to promote the natural abundance of wood. In 1923, Stern was the executive director of the Tiroler Oelwerke LLC.

Geographic entities mentioned:
surface_form: Plansee
instance_of: Lake
countries: Austria
coordinates: lat: 47.469444
lon: 10.805556
In 1922, he succeeded in persuading Paul Schwarzkopf to found the Plansee metal works. He founded an oil plant to exploit natural resources and several wood processing companies to promote the natural abundance of wood. In 1923, Stern was the executive director of the Tiroler Oelwerke LLC. His main economic project was the construction of a cable car up to the Zugspitze.

Geographic entities mentioned:
surface_form: Zugspitze
instance_of: Mountain
countries: Germany
Austria
coordinates: lat: 47.421217
lon: 10.986314
Personal life. In 1911, he married Anna Knittel, the daughter of a school inspector, Josef Knittel. They gave birth to five children. Exile and death. In 1926, he was made an honorary citizen of the municipality of Ehrwald for his services to the construction of the cable car up to the Zugspitze (). This honorary citizenship was withdrawn from him in 1940 because of his Jewish descent.

Geographic entities mentioned:
surface_form: Zugspitze
instance_of: Mountain
countries: Germany
Austria
coordinates: lat: 47.421217
lon: 10.986314
Lang Nunatak. 5oiq6zho84h2m2ub5lw37gei13b" xml:space="preserve">#redirect Lang Nunatak

Geographic entities mentioned:
surface_form: lang nunatak
instance_of: Mountain
coordinates: lat: -74.1667
lon: -66.4833
It was a casualty of erosion after the surrounding woods were deforested—exacerbated by the need for lumber to rebuild several Midwestern cities and towns ravaged by fires in 1871. Its ruins are now buried beneath the sand dunes of the Lake Michigan shoreline at the mouth of the Kalamazoo River in Saugatuck Township, near the cities of Saugatuck and Douglas in Allegan County.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
state of Alaska. Beginning on the flanks of Mount Kialagvik, it flows northwest through the Alaska Peninsula National Wildlife Refuge to meet the larger river southwest of Ugashik, at the head of Ugashik Bay, an arm of Bristol Bay. It descends to the upper reaches of the bay from an elevation of in a valley of the Aleutian Range between Mount Chiginagak and Mount Kialagvik.

Geographic entities mentioned:
surface_form: Mount Kialagvik
instance_of: Mountain
countries: United States
coordinates: lat: 57.203
lon: -156.745
It is shallow with many oxbow turns and is not navigable. The streambed is a mix of gravel and mud, with its milky glacier headwaters growing increasingly muddy as it progresses. There are many rivers in Alaska bearing the name Dog Salmon River and this river should not be confused with those located on the Yukon-Kuskokwim Delta or eastern Norton Sound.

Geographic entities mentioned:
surface_form: Norton Sound
instance_of: Landform
countries: United States
coordinates: lat: 63.849166666667
lon: -164.26888888889
The entire climb is exposed to any bad weather that may arrive quickly, while climbing the upper slopes in winter can be dangerous due to slick ice on the rocks and heavy snow covering holes and other hazards. From the summit, there are views of Dove Lake, Barn Bluff and Mount Ossa. Climate.

Geographic entities mentioned:
surface_form: Barn Bluff
instance_of: Mountain
countries: Australia
coordinates: lat: -41.724061111111
lon: 145.92304166667
surface_form: ossa
instance_of: Mountain
countries: Australia
coordinates: lat: -41.871025
lon: 146.03334444444
surface_form: mount ossa
instance_of: Mountain
countries: Australia
coordinates: lat: -41.871025
lon: 146.03334444444
surface_form: barn bluff
instance_of: Mountain
countries: Australia
coordinates: lat: -41.724061111111
lon: 145.92304166667
surface_form: dove
instance_of: Lake
countries: Australia
coordinates: lat: -41.658055555556
lon: 145.96194444444
Cradle Mountain. Cradle Mountain is a locality and mountain in the Central Highlands region of the Australian state of Tasmania. The mountain is situated in the Cradle Mountain-Lake St Clair National Park. At above sea level, it is the sixth-highest mountain in Tasmania.

Geographic entities mentioned:
surface_form: lake st clair
instance_of: Lake
countries: Australia
coordinates: lat: -42.066666666667
lon: 146.16666666667
surface_form: cradle mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -41.684644444444
lon: 145.951275
Cradle Mountain was gazetted as a locality in 1966. Cradle Mountain (the mountain) occupies a small area in the north-west of the locality, which occupies the northern half of Cradle Mountain-Lake St Clair National Park. Route C132 (Cradle Mountain Road / Dove Lake Road) enters from the north and runs south to Dove Lake, where it ends. History.

Geographic entities mentioned:
surface_form: lake st clair
instance_of: Lake
countries: Australia
coordinates: lat: -42.066666666667
lon: 146.16666666667
surface_form: cradle mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -41.684644444444
lon: 145.951275
surface_form: cradle mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -41.684644444444
lon: 145.951275
It is magnificent, and people must know about it and enjoy it&quot;. They began campaigning for the area from Cradle Mountain to Lake St Clair to be a national park, and set up a popular chalet the next year. It was declared a scenic reserve in 1922, a wildlife reserve in 1927 and its current designation of national park from 1947.

Geographic entities mentioned:
surface_form: lake st clair
instance_of: Lake
countries: Australia
coordinates: lat: -42.066666666667
lon: 146.16666666667
surface_form: cradle mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -41.684644444444
lon: 145.951275
During this transition former trappers began building huts and guiding bushwalkers, including Paddy Hartnett, Weindorfer and Bob Quaile. In 1931 fur trapper Bert Nichols blazed the Overland Track starting from Cradle Mountain and heading south to Lake St Clair. By 1935 it was consolidated and used by independent walking parties. Geology.

Geographic entities mentioned:
surface_form: lake st clair
instance_of: Lake
countries: Australia
coordinates: lat: -42.066666666667
lon: 146.16666666667
surface_form: cradle mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -41.684644444444
lon: 145.951275
Access. The area around the mountain has a large number of day walks, as well as being one terminus of the Overland Track. The Overland Track winds through a variety of landscapes to its opposite end— to the south—at Lake St Clair, Australia's deepest lake. The mountain is climbed by walkers virtually year round.

Geographic entities mentioned:
surface_form: lake st clair
instance_of: Lake
countries: Australia
coordinates: lat: -42.066666666667
lon: 146.16666666667
Fungi. Fungi are also a part of the park's biodiversity. While the Management Plan from 1999 for Cradle Mountain-Lake St Clair National Park only mentions fungi in the context of their destructive effects (&quot;Phytophthora cinnamomi&quot; and &quot;Chalara australis&quot;), the park has a variety of fungi that perform beneficial ecological roles.

Geographic entities mentioned:
surface_form: lake st clair
instance_of: Lake
countries: Australia
coordinates: lat: -42.066666666667
lon: 146.16666666667
surface_form: cradle mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -41.684644444444
lon: 145.951275
Other fungi form symbiotic relationships with other organisms. Although rarely acknowledged, the great majority of plants in Cradle Mountain-Lake St Clair National Park (and, indeed, in the world) form mutually beneficial mycorrhizal relationships with fungi.

Geographic entities mentioned:
surface_form: lake st clair
instance_of: Lake
countries: Australia
coordinates: lat: -42.066666666667
lon: 146.16666666667
surface_form: cradle mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -41.684644444444
lon: 145.951275
Cradle Mountain. Cradle Mountain is a locality and mountain in the Central Highlands region of the Australian state of Tasmania. The mountain is situated in the Cradle Mountain-Lake St Clair National Park. At above sea level, it is the sixth-highest mountain in Tasmania.

Geographic entities mentioned:
surface_form: cradle mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -41.684644444444
lon: 145.951275
The mountain is situated in the Cradle Mountain-Lake St Clair National Park. At above sea level, it is the sixth-highest mountain in Tasmania. The locality of Cradle Mountain is a rural locality in the local government areas of Meander Valley, Kentish and West Coast in the Launceston and North-west and west local government regions of Tasmania. The locality is about west of the town of Westbury.

Geographic entities mentioned:
surface_form: cradle mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -41.684644444444
lon: 145.951275
The locality of Cradle Mountain is a rural locality in the local government areas of Meander Valley, Kentish and West Coast in the Launceston and North-west and west local government regions of Tasmania. The locality is about west of the town of Westbury. The 2016 census has a population of 66 for the state suburb of Cradle Mountain. Cradle Mountain was gazetted as a locality in 1966.

Geographic entities mentioned:
surface_form: cradle mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -41.684644444444
lon: 145.951275
The locality is about west of the town of Westbury. The 2016 census has a population of 66 for the state suburb of Cradle Mountain. Cradle Mountain was gazetted as a locality in 1966. Cradle Mountain (the mountain) occupies a small area in the north-west of the locality, which occupies the northern half of Cradle Mountain-Lake St Clair National Park.

Geographic entities mentioned:
surface_form: cradle mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -41.684644444444
lon: 145.951275
Cradle Mountain was gazetted as a locality in 1966. Cradle Mountain (the mountain) occupies a small area in the north-west of the locality, which occupies the northern half of Cradle Mountain-Lake St Clair National Park. Route C132 (Cradle Mountain Road / Dove Lake Road) enters from the north and runs south to Dove Lake, where it ends. History.

Geographic entities mentioned:
surface_form: cradle mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -41.684644444444
lon: 145.951275
surface_form: dove lake
instance_of: Lake
countries: Australia
coordinates: lat: -41.658055555556
lon: 145.96194444444
surface_form: dove lake
instance_of: Lake
countries: Australia
coordinates: lat: -41.658055555556
lon: 145.96194444444
Route C132 (Cradle Mountain Road / Dove Lake Road) enters from the north and runs south to Dove Lake, where it ends. History. Cradle Mountain sits between the Big River and Northern Tasmanian Aboriginal people. Aboriginal Tasmanians were persecuted by the European settlers upon their arrival, and the last free Aboriginals in the area were seen just south of Cradle Mountain in 1836.

Geographic entities mentioned:
surface_form: cradle mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -41.684644444444
lon: 145.951275
History. Cradle Mountain sits between the Big River and Northern Tasmanian Aboriginal people. Aboriginal Tasmanians were persecuted by the European settlers upon their arrival, and the last free Aboriginals in the area were seen just south of Cradle Mountain in 1836. Early European development.

Geographic entities mentioned:
surface_form: cradle mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -41.684644444444
lon: 145.951275
Early European development. In 1827 and 1828, the first Europeans to explore and summit Cradle Mountain were Joseph Fossey and Henry Hellyer, who were surveying for the Van Diemen's Land Company. Trappers worked in the area from the 1860s until the collapse of the fur trade in the 1950s, although hunting in the park was declared illegal after 1927.

Geographic entities mentioned:
surface_form: cradle mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -41.684644444444
lon: 145.951275
Cattle and sheep grazed in Cradle Valley from 1910 to 1930. Environmental protection and tourism. In the 1910s Gustav and Kate Cowle climbed Cradle Mountain. They found the land beautiful and Gustav proclaimed &quot;This must be a national park for the people for all time. It is magnificent, and people must know about it and enjoy it&quot;.

Geographic entities mentioned:
surface_form: cradle mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -41.684644444444
lon: 145.951275
Geology. Cradle Mountain is formed by an igneous dolerite sill that intruded the Permian-Jurassic sedimentary layers, cooling to form a broad hard layer. Subsequent erosion from Pleistocene glaciation left caps of dolerite at Cradle Mountain, and surrounding peaks. Access. The area around the mountain has a large number of day walks, as well as being one terminus of the Overland Track.

Geographic entities mentioned:
surface_form: cradle mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -41.684644444444
lon: 145.951275
Features. The mountain rises above the glacially formed Dove Lake (), Lake Wilks and Crater Lake. The mountain has four named summits. In order of height they are Cradle Mountain (), Smithies Peak (), Weindorfers Tower () and Little Horn (). The mountain itself is named after its resemblance to a gold-mining cradle. Flora.

Geographic entities mentioned:
surface_form: cradle mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -41.684644444444
lon: 145.951275
surface_form: smithies peak
instance_of: Mountain
countries: Australia
coordinates: lat: -41.68
lon: 145.95
The mountain is climbed by walkers virtually year round. It is a strenuous return hike from the Dove Lake car park with a recommended allotted time of six-and-a-half hours. The climb up the rocky part of the mountain involves scrambling over large boulders for several hundred metres.

Geographic entities mentioned:
surface_form: dove lake
instance_of: Lake
countries: Australia
coordinates: lat: -41.658055555556
lon: 145.96194444444
It receives an average of 47.9 snowy days annually, which can occur in any month of the year. Features. The mountain rises above the glacially formed Dove Lake (), Lake Wilks and Crater Lake. The mountain has four named summits. In order of height they are Cradle Mountain (), Smithies Peak (), Weindorfers Tower () and Little Horn ().

Geographic entities mentioned:
surface_form: dove lake
instance_of: Lake
countries: Australia
coordinates: lat: -41.658055555556
lon: 145.96194444444
Pleven Saddle. Pleven Saddle (Plevenska Sedlovina \'ple-ven-ska se-dlo-vi-'na\) is a deep saddle of elevation 500 m in Friesland Ridge, Tangra Mountains, Livingston Island, Antarctica, bounded by MacKay Peak to the west-southwest and Tervel Peak to the east-northeast, with two conspicuous rocks rising on it.

Geographic entities mentioned:
surface_form: MacKay Peak
instance_of: Mountain
coordinates: lat: -62.7211
lon: -60.2993
surface_form: Tervel Peak
instance_of: Mountain
coordinates: lat: -62.717138888889
lon: -60.269444444444
Walking trails from the Nara side start from a car park at about 1,400 metres. The mountain is famous for wild deer, and also for wild birds, especially wrens and Japanese robins, as well as treecreepers and woodpeckers. In 1980, an area of 36,000 hectares in the region of Mount Ōdaigahara and Mount Ōmine was designated a UNESCO Man and the Biosphere Reserve.

Geographic entities mentioned:
surface_form: Mount Ōmine
instance_of: Mountain
countries: Japan
coordinates: lat: 34.252777777778
lon: 135.94055555556
surface_form: mount ōdaigahara
instance_of: Mountain
countries: Japan
coordinates: lat: 34.11
lon: 136.03
surface_form: ōdaigahara
instance_of: Mountain
countries: Japan
coordinates: lat: 34.11
lon: 136.03
Mount Ōdaigahara. , also is a mountain in the Daikō Mountain Range on the border between the prefectures of Mie and Nara, Japan. Its top is the highest point in Mie at. Walking trails from the Nara side start from a car park at about 1,400 metres. The mountain is famous for wild deer, and also for wild birds, especially wrens and Japanese robins, as well as treecreepers and woodpeckers.

Geographic entities mentioned:
surface_form: mount ōdaigahara
instance_of: Mountain
countries: Japan
coordinates: lat: 34.11
lon: 136.03
surface_form: ōdaigahara
instance_of: Mountain
countries: Japan
coordinates: lat: 34.11
lon: 136.03
In 1980, an area of 36,000 hectares in the region of Mount Ōdaigahara and Mount Ōmine was designated a UNESCO Man and the Biosphere Reserve. The mountain was also selected by the Tokyo Nichi Nichi Shimbun and Osaka Mainichi Shimbun newspapers as one of the 100 Landscapes of Japan in 1927. It was referenced on American indie folk band Fleet Foxes's 2017 song &quot;Ōdaigahara&quot;.

Geographic entities mentioned:
surface_form: ōdaigahara
instance_of: Mountain
countries: Japan
coordinates: lat: 34.11
lon: 136.03
The political freedom and cultural boom of western culture opened the way for the clubbing scene, with several venues starting all around the country, especially in Budapest and around Lake Balaton. The 1990s also marked the creation of several dance formations, notably Soho Party, Splash, Náksi & Brunner and also rave formations such as Emergency House and Kozmix.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
With a colorful mix of musical styles, and popularity increasing each year, is considered to be the &quot;cheaper version&quot; of Sziget. Also founded by the Sziget management, Balaton Sound is a festival of mainly electronic music, held yearly in Zamárdi, next to Lake Balaton. With prestigious performers and exclusive surroundings, it tries to position itself as a high-standard event.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
S.I. Paul et al. (2021) isolated and characterized two species of &quot;Halobacillus&quot; (&quot;Halobacillus kuroshimensis&quot; and &quot;Halobacillus karajensis&quot;) from marine sponges (phylum: porifera) of the Saint Martin's Island of the Bay of Bengal, Bangladesh. Single colonies are pin headed (very small) in sized and opaque in color. Phylogeny.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Bald Mountain (Schoharie County, New York). Bald Mountain is a mountain located in the Catskill Mountains of New York west-northwest of Gilboa. Mount Jefferson is located north-northwest, and Mine Hill is located north of Bald Mountain.

Geographic entities mentioned:
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.655
lon: -114.409
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.8827026
lon: -88.0390147
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.8822
lon: -123.866
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6611024
lon: -107.4103338
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.4291
lon: -75.7503
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.6988
lon: -110.902
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.021388888889
lon: -75.190833333333
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.5344
lon: -119.115
surface_form: bald mountain (schoharie county, new york)
instance_of: Mountain
countries: United States
coordinates: lat: 42.423611111111
lon: -74.593888888889
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1209
lon: -74.2001
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.902777777778
lon: -74.724444444444
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.4439
lon: -105.969
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7386
lon: -74.9129
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.294722222222
lon: -74.387777777778