Sarmila/GeoWiki-Features huggingface dataset:
Grabovica valley. Grabovica valley with small Grabovica creek is a special reserve within park, squeezed deep into Čvrsnica, and form a deep canyon between steep and rugged cliffs of the mountain. Within the valley are two small villages Gornja Grabovica (Jablanica) and Donja Grabovica (Jablanica).

Geographic entities mentioned:
surface_form: grabovica
instance_of: Lake
countries: Bosnia and Herzegovina
coordinates: lat: 43.62277778
lon: 17.76194444
surface_form: grabovica
instance_of: Lake
countries: Bosnia and Herzegovina
coordinates: lat: 43.62277778
lon: 17.76194444
surface_form: grabovica
instance_of: Valley
countries: Bosnia and Herzegovina
coordinates: lat: 43.606051664495205
lon: 17.68825777993787
surface_form: grabovica
instance_of: Valley
countries: Bosnia and Herzegovina
coordinates: lat: 43.606051664495205
lon: 17.68825777993787
The closest town to the Blidinje Nature Park is Jablanica, which is 24.9 km away. Doljani valley. Doljani valley is the longest valley and a northern border of the Čvrsnica-Vran-Čabulja complex, with the Doljanka river running through. Dugo Polje.

Geographic entities mentioned:
surface_form: čabulja
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.4833
lon: 17.65
surface_form: vran
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.6683
lon: 17.5058
surface_form: čvrsnica
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.616666666667
lon: 17.616666666667
Other lakes and &quot;lokvas&quot;. Beside Blidinje, plateau hosts few other, smaller lakes and lokvas, such as Crepulja and Crvenjak. The Crvenjak Lake is a small glacial lake located in the Čvrsnica massive. The lake is oval-shaped, approximately 70 meters long and 50 meters wide. It has a depth of approximately 9 meters. Flora and fauna.

Geographic entities mentioned:
surface_form: čvrsnica
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.616666666667
lon: 17.616666666667
Blidinje plateau. Blidinje plateau () is a karst plateau in Bosnia and Herzegovina, situated at the heart of Dinaric Alps, between major mountains of the range, Čvrsnica, Čabulja and Vran, with characteristic karstic features such as Dugo Polje field, Blidinje Lake, Grabovica and Drežnica valleys, and others.

Geographic entities mentioned:
surface_form: blidinje
instance_of: Lake
countries: Bosnia and Herzegovina
coordinates: lat: 43.60805556
lon: 17.49361111
surface_form: blidinje
instance_of: Plateau
countries: Bosnia and Herzegovina
coordinates: lat: 43.61085
lon: 17.508775
Although geomorphologically one whole, plateau is divided in two geographically and topographic distinct features, first in lower southern part, areal around the lake Blidinje, and another in northern higher part of the plateau where a flat plain Dugopolje is situated, as well as administratively between four municipalities: Jablanica, Prozor-Rama, Posušje, Tomislavgrad, and Mostar.

Geographic entities mentioned:
surface_form: blidinje
instance_of: Lake
countries: Bosnia and Herzegovina
coordinates: lat: 43.60805556
lon: 17.49361111
surface_form: blidinje
instance_of: Plateau
countries: Bosnia and Herzegovina
coordinates: lat: 43.61085
lon: 17.508775
surface_form: rama
instance_of: Watercourse
countries: Bosnia and Herzegovina
coordinates: lat: 43.73333333
lon: 17.68333333
The closest town to the Blidinje Nature Park is Jablanica, which is 24.9 km away. Doljani valley. Doljani valley is the longest valley and a northern border of the Čvrsnica-Vran-Čabulja complex, with the Doljanka river running through. Dugo Polje.

Geographic entities mentioned:
surface_form: blidinje
instance_of: Lake
countries: Bosnia and Herzegovina
coordinates: lat: 43.60805556
lon: 17.49361111
surface_form: blidinje
instance_of: Plateau
countries: Bosnia and Herzegovina
coordinates: lat: 43.61085
lon: 17.508775
The stream of Drežanka runs between large and steep slopes of the valley, with two eponymous villages, Donja Drežnica (Lower Drežnica) and Gornja Drežnica (Upper Drežnica) being situated on its banks. Blidinje lake. The most important hydrogeological phenomena in the park is alpine lake, Blidinje Lake, largest of its kind in Bosnia and Herzegovina.

Geographic entities mentioned:
surface_form: blidinje lake
instance_of: Lake
countries: Bosnia and Herzegovina
coordinates: lat: 43.60805556
lon: 17.49361111
surface_form: blidinje
instance_of: Plateau
countries: Bosnia and Herzegovina
coordinates: lat: 43.61085
lon: 17.508775
Blidinje lake. The most important hydrogeological phenomena in the park is alpine lake, Blidinje Lake, largest of its kind in Bosnia and Herzegovina. Blidinje lake is the direct result of a glacial retreat, but according to the Poklečani Parishes office documents, lake is, also, a product of anthropogenic intervention and activities of human inhabitants.

Geographic entities mentioned:
surface_form: blidinje lake
instance_of: Lake
countries: Bosnia and Herzegovina
coordinates: lat: 43.60805556
lon: 17.49361111
surface_form: blidinje
instance_of: Plateau
countries: Bosnia and Herzegovina
coordinates: lat: 43.61085
lon: 17.508775
History, heritage and culture. All around the valley is dotted with the Bosnia and Herzegovina trademark &quot;stećci&quot; from medieval ages. It is not clear how long human settlements have existed here but research began when Blidinje recently received Nature park status. Traces of Illyrian graves and Roman roads indicate that Blidinje has been settled for at least 2,500 years.

Geographic entities mentioned:
surface_form: blidinje
instance_of: Lake
countries: Bosnia and Herzegovina
coordinates: lat: 43.60805556
lon: 17.49361111
surface_form: blidinje
instance_of: Plateau
countries: Bosnia and Herzegovina
coordinates: lat: 43.61085
lon: 17.508775
It is not clear how long human settlements have existed here but research began when Blidinje recently received Nature park status. Traces of Illyrian graves and Roman roads indicate that Blidinje has been settled for at least 2,500 years. The large necropolis at Dugo Polje indicates that the waves of Slavs that came in the 7th century also made this area their home.

Geographic entities mentioned:
surface_form: blidinje
instance_of: Lake
countries: Bosnia and Herzegovina
coordinates: lat: 43.60805556
lon: 17.49361111
surface_form: blidinje
instance_of: Plateau
countries: Bosnia and Herzegovina
coordinates: lat: 43.61085
lon: 17.508775
The legend of Diva Grabovčeva tells the story about legendary daughter of a local shepherd who, as story goes, was killed by local nobleman whom she rejected, so that she would not marry another. Drežnica valley. Further downstream much larger vale appears again, this time between Čvrsnica and Čabulja mountains, called Drežnica Valley.

Geographic entities mentioned:
surface_form: drežnica valley
instance_of: Valley
countries: Bosnia and Herzegovina
coordinates: lat: 43.529361
lon: 17.679476
Damodar Kund. Damodar Kund, located at the foothills of Girnar hills, near Junagadh in the Indian state of Gujarat, is considered a sacred lake as per Hindu beliefs. Many Hindus prefer to bathe here and immerse the ashes and the bones left after cremation of dead bodies, here at Damodar Kund due to a belief that the departed souls would get moksha here.

Geographic entities mentioned:
surface_form: Girnar
instance_of: Mountain
countries: India
coordinates: lat: 21.516962
lon: 70.53154
surface_form: damodar kund
instance_of: Lake
countries: India
coordinates: lat: 21.52555556
lon: 70.48611111
Damodar Kund. Damodar Kund, located at the foothills of Girnar hills, near Junagadh in the Indian state of Gujarat, is considered a sacred lake as per Hindu beliefs. Many Hindus prefer to bathe here and immerse the ashes and the bones left after cremation of dead bodies, here at Damodar Kund due to a belief that the departed souls would get moksha here.

Geographic entities mentioned:
surface_form: damodar kund
instance_of: Lake
countries: India
coordinates: lat: 21.52555556
lon: 70.48611111
The water of the lake has properties of dissolving the bones. The lake is long and broad and only deep. It is surrounded by a well built ghat. The steps for going up the Girnar hills start near Damodar Kund. At the foothills of Ashwatthama Hill in Girnar mountain range base, southerly to Damodara Kund is the Damodar Hari Temple.

Geographic entities mentioned:
surface_form: damodar kund
instance_of: Lake
countries: India
coordinates: lat: 21.52555556
lon: 70.48611111
There are other sub shrines dedicated to Lord Balarama, Sri Revati and Lord Ganesha. There are several other ancient temples nearby with on and outside temple complex. Devotees are seen taking a holy dip in the sacred bathing tank, Damodar Kund, before offering prayers at the temple. The sewa of Shri Damodarji is being performed here in the Samprant-Yug by Vaishnav tradition.

Geographic entities mentioned:
surface_form: damodar kund
instance_of: Lake
countries: India
coordinates: lat: 21.52555556
lon: 70.48611111
The Damodar Kund is closely attached to the life of Narsinh Mehta, the famous 15th century Gujarati poet and devotee of Krishna, who used to come to bathe at Damodar Kund and is said to have written many of his &quot;prabhatiyas&quot; (morning prayers), in the natural surrounding here at the Damodar lake, at picturesque foothills of Girnar.

Geographic entities mentioned:
surface_form: damodar kund
instance_of: Lake
countries: India
coordinates: lat: 21.52555556
lon: 70.48611111
At present, there is also a temple of Narsinh Mehta, which is built near temple of Damodar, to commemorate the association of this great saint-poet with Damodar Kund and ancient temple of Damodar here.

Geographic entities mentioned:
surface_form: damodar kund
instance_of: Lake
countries: India
coordinates: lat: 21.52555556
lon: 70.48611111
There is another holy lake, Mrigi Kund located nearby in Bhavnath temple premises. Hindus prefer to bathe in all these lakes to get rid of their sins. Damodar Kund is one of the monuments protected by the state government of Gujarat. It is a temporary check-dam reservoir, which are being made and shifted regularly, in order to maintain water levels throughout the year at Damodar Kund.

Geographic entities mentioned:
surface_form: damodar kund
instance_of: Lake
countries: India
coordinates: lat: 21.52555556
lon: 70.48611111
It is a temporary check-dam reservoir, which are being made and shifted regularly, in order to maintain water levels throughout the year at Damodar Kund. There are changing rooms, public toilet and other basic amenities provided by government, who have built permanent structure at Damodar Kund for facility of pilgrims.

Geographic entities mentioned:
surface_form: damodar kund
instance_of: Lake
countries: India
coordinates: lat: 21.52555556
lon: 70.48611111
Production. The film was produced by Catalan outfit Galápagos Media alongside Valencian Dacsa Produccions, with the participatión of TVC, À Punt, TVE and backing from IVC. It was shot in the provinces of Castellón (Benicarló,) and Tarragona (Ebro Delta, La Sénia, Ulldecona). Release. The film had its world premiere at the 39th Warsaw International Film Festival.

Geographic entities mentioned:
surface_form: Ebro Delta
instance_of: Body of water
countries: Spain
coordinates: lat: 40.73243
lon: 0.86964
Biography. Jeff Jones was raised in the gang dominated streets of Los Angeles' Compton and South Central neighborhoods. He moved around Southern California from the San Fernando Valley to Palmdale and finally Riverside due to his mother's battle with drug addiction. Jones started rapping and performing at the age of ten, freestyling at school and performing with a local rap group.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
It is under the administration of the prefecture-level city of Baoji. Taibai County is located west of the Qin Mountains and southeast of downtown Baoji. It is named after nearby Mount Taibai, a major peak of the Qin Mountains. It has five towns and three townships, including 66 administrative villages, and covers an area of. It has a population of 52,000.

Geographic entities mentioned:
surface_form: Mount Taibai
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 33.95666667
lon: 107.765
Pseudotropheus crabro. &quot;Pseudotropheus crabro&quot;, also known as the bumblebee cichlid or hornet cichlid, is a species of cichlid endemic to Lake Malawi where it is found in different habitats but most frequently in large caves or in the vicinity of large boulders. This species can reach a length of SL.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
Warren Hill, Hooke, Dorset. Warren Hill is a prominent elevation, high, 1 kilometre southwest of the hamlet of Hooke, in the county of Dorset in southern England. Its prominence of means it is listed as one of the Tumps. It is located within the Dorset Downs. The summit is open, as is the hill's eastern flank, but much of the western side of the hill is covered by the woods of Hooke Park.

Geographic entities mentioned:
surface_form: warren hill, hooke, dorset
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 50.7929
lon: -2.6736
She had a house built for her family, and was active in the council of the church parish. Schönberg was the first woman elected to the Schruns municipal council, serving from 1975 to 1985, initiating the erection of museums in Montafon. From 1979 to 2000, she was museum director of the.

Geographic entities mentioned:
surface_form: Montafon
instance_of: Valley
countries: Austria
coordinates: lat: 47.08
lon: 9.9
Overview. The Mugello was presented at the Époqu'auto show in Lyon in November 2019. The Mugello is produced in the Devalliet workshops in Tullins in the Vercors regional park. The car is named after the Mugello Circuit located in the historic region of the same name northeast of Florence, Italy. Specifications.

Geographic entities mentioned:
surface_form: historic region of the same name
instance_of: Valley
countries: Italy
coordinates: lat: 43.95
lon: 11.3833
It belongs to the district of Tsaratanana, which is a part of Betsiboka Region. The population of the commune was estimated to be approximately 10,000 in 2001 commune census. The Mahajamba River flows to the northeast. Only primary schooling is available. The majority 59% of the population of the commune are farmers, while an additional 40% receives their livelihood from raising livestock.

Geographic entities mentioned:
surface_form: Mahajamba River
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -15.55
lon: 47.13333
Artist Lake. Artist Lake is a glacial kettle hole lake located in Middle Island, New York south of Middle Country Road (Route 25) in central Long Island. Artist Lake holds a diverse warm water fish community including largemouth bass and pickerel. It is also one of Long Island's better waters for crappie and perch.

Geographic entities mentioned:
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
surface_form: artist lake
instance_of: Lake
countries: United States
coordinates: lat: 40.883888888889
lon: -72.931388888889
Artist Lake is a glacial kettle hole lake located in Middle Island, New York south of Middle Country Road (Route 25) in central Long Island. Artist Lake holds a diverse warm water fish community including largemouth bass and pickerel. It is also one of Long Island's better waters for crappie and perch. Access is via Town of Brookhaven's park located directly off of Middle Country Road.

Geographic entities mentioned:
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
Artist Lake. Artist Lake is a glacial kettle hole lake located in Middle Island, New York south of Middle Country Road (Route 25) in central Long Island. Artist Lake holds a diverse warm water fish community including largemouth bass and pickerel. It is also one of Long Island's better waters for crappie and perch.

Geographic entities mentioned:
surface_form: artist lake
instance_of: Lake
countries: United States
coordinates: lat: 40.883888888889
lon: -72.931388888889
Directions: Take Route 25 to Middle Island; lake is on the south side of the road opposite of what used to be Kmart. Restrictions: Hand launched boats are allowed; shoreline access is available but limited. Artist Lake has an irregular shape that was formed by the melting of massive chunks of partially buried glacial ice. A lake formed this way is called a kettlehole.

Geographic entities mentioned:
surface_form: artist lake
instance_of: Lake
countries: United States
coordinates: lat: 40.883888888889
lon: -72.931388888889
Artist Lake has an irregular shape that was formed by the melting of massive chunks of partially buried glacial ice. A lake formed this way is called a kettlehole. Artist Lake has no inlet or outlet streams. Therefore, the water level is determined by groundwater that gradually changes during periods of dry or wet weather. Artist Lake has three connected basins with a total surface area of.

Geographic entities mentioned:
surface_form: artist lake
instance_of: Lake
countries: United States
coordinates: lat: 40.883888888889
lon: -72.931388888889
A lake formed this way is called a kettlehole. Artist Lake has no inlet or outlet streams. Therefore, the water level is determined by groundwater that gradually changes during periods of dry or wet weather. Artist Lake has three connected basins with a total surface area of. The largest and deepest basin is on the east basin which has a maximum depth of.

Geographic entities mentioned:
surface_form: artist lake
instance_of: Lake
countries: United States
coordinates: lat: 40.883888888889
lon: -72.931388888889
Artist Lake has three connected basins with a total surface area of. The largest and deepest basin is on the east basin which has a maximum depth of. The south and west basins are shallower, particularly the west basin which does not exceed two feet in depth. Most of the shoreline of Artist Lake is privately owned. Public access is available from Middle Country Road (Route 25).

Geographic entities mentioned:
surface_form: artist lake
instance_of: Lake
countries: United States
coordinates: lat: 40.883888888889
lon: -72.931388888889
Public access is available from Middle Country Road (Route 25). Canoes or other hand carried boats can be launched from a small Brookhaven town park on the south side of the road. Fishing from shore is also possible. There is room for five or six cars to pull off the highway. Artist Lake is located on NYS Route 25 in Middle Island just east of Suffolk County Route 21.

Geographic entities mentioned:
surface_form: artist lake
instance_of: Lake
countries: United States
coordinates: lat: 40.883888888889
lon: -72.931388888889
For example, Russia maintains sizable border zones. Natural disaster exclusion zones. Similarly, exclusion zones have been established due to natural disasters. There is an exclusion zone on the island of Montserrat, where the long-dormant Soufrière Hills volcano started erupting in 1995 and has continued erupting since.

Geographic entities mentioned:
surface_form: Soufrière Hills
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 16.716666666667
lon: -62.183333333333
Of the water in the municipality, 0.5% is in lakes and 2.6% is in rivers and streams. Of the unproductive areas, 3.8% is unproductive vegetation and 4.0% is too rocky for vegetation. The municipality is located in the Monthey district, at the mouth of the Rhone into Lake Geneva. It consists of the villages of Le Bouveret and Les Evouettes and the hamlet of Port-Valais. Coat of arms.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
There are several small rivers and creeks that flow away from the plateau, such as north flowing Montgomery Creek and east flowing Little Pipestone Creek. Both of those are tributaries of Pipestone Creek, which flows across provincial borders into Manitoba. Moose Mountain Creek originates in the north-west corner of the plateau and heads south, then south-east into the Souris River.

Geographic entities mentioned:
surface_form: Moose Mountain Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.21675
lon: -102.20089
Lakes and reservoirs. Moose Mountain is dotted with hundreds of small lakes and sloughs, most of which are closed basin, meaning they have no regular out-flow. The largest is Kenosee Lake, which, along with Little Kenosee Lake, is the centrepiece of Moose Mountain Provincial Park. White Bear (Carlyle) Lake, formally &quot;Carlyle Lake&quot;, is entirely within the White Bear First Nation.

Geographic entities mentioned:
surface_form: Kenosee Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.8167
lon: -102.283
surface_form: Little Kenosee Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.83334
lon: -102.33383
Little White Bear Lake is right beside it, just to the west. On the east side of the plateau is Cannington Lake with the small resort community of Cannington Lake on its shore. Moose Mountain Creek was dammed in 1937 on the west side of the upland to create Moose Mountain Lake. Flora, fauna, and forest preserve.

Geographic entities mentioned:
surface_form: Moose Mountain Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.8975
lon: -103.04
Wolves were hunted to extinction in the 1920s. Walleye and yellow perch can be found in the lakes. Communities. The village of Kenosee Lake is on Kenosee Lake, alongside Highway 9, and in the heart of Moose Mountain Provincial Park. Outside of the Indian reserves, it is the largest community in Moose Mountain with a 2016 population of 234 people.

Geographic entities mentioned:
surface_form: Kenosee Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.8167
lon: -102.283
The chalet and golf course were built in tandem with the idea of bringing wealthy people to the park. The largest lake on the plateau, Kenosee Lake, is found in the park. Kenosee Lake is stocked with fish, has a beach area, docks, miniature golf, and camping. Overlooking the lake is the Kenosee Inn & Cabins which features a conference room, 30 hotel rooms, and 23 cabins.

Geographic entities mentioned:
surface_form: Kenosee Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.8167
lon: -102.283
He wrote to the mayor and corporation of Cork in July ordering the abolition of the new heresy of Protestantism, at a time when he appears to have been taking instruction from Irish Jesuits. By September 1569, Sidney had broken the back of the rebellion and left Sir Humphrey Gilbert behind to suppress fitz Maurice, who sought refuge in the woods of Aherlow, south of Tipperary.

Geographic entities mentioned:
surface_form: Aherlow
instance_of: Valley
countries: Ireland
coordinates: lat: 52.419
lon: -8.193
Mjøllkvaevane Cirques. The Mjøllkvaevane Cirques () are a series of small snow-filled cirques that indent the east side of Kvaevefjellet Mountain in the Payer Mountains of Queen Maud Land, Antarctica. They were plotted from air photos and surveys by the Sixth Norwegian Antarctic Expedition, 1956–60.

Geographic entities mentioned:
surface_form: Kvaevefjellet Mountain
instance_of: Mountain
coordinates: lat: -71.866666666667
lon: 14.45
Haddada, Boumerdès. Haddada, also known as Ihaddadene, is a village in the Boumerdès Province in Kabylie, Algeria. Location. The village is situated near the Meraldene River, Isser River, and Boumerdès River. It is surrounded by the towns of Beni Amrane and Thénia in the Khachna mountain range.

Geographic entities mentioned:
surface_form: Meraldene River
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.6981116
lon: 3.5435504
surface_form: Isser River
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.8391
lon: 3.6679
To the south rises the Snegovoy Range and to the north, above the other bank of the Ukelayat river, the Pikas Range. The highest point is Ledyanaya, a high rocky peak topped by an ice cap, which is also the highest point of the Koryak Highlands. To the east, not far from the sea, rises high Mt Undyer (гора Ундер).

Geographic entities mentioned:
surface_form: Ledyanaya
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 62.06666667
lon: 171.3666667
The WACC quickly replaced the Japanese contractors as principal contractors to the Oxnard Plain and even forced some of them to subcontract through the WACC. This process also adversely affected farmworkers as the WACC charged a fee for subcontracting beneath them.

Geographic entities mentioned:
surface_form: Oxnard Plain
instance_of: Valley
countries: United States
coordinates: lat: 34.36
lon: -119.15
Caribou Tuya. Caribou Tuya is a basaltic subglacial mound in far northwestern British Columbia that began eruptive activity under glacial ice during the Fraser glaciation (25 to 10 ka). Like Ash Mountain and South Tuya, sections of the subglacial mound reveal a consistent stratigraphic progression from pillow lavas to hyaloclastite deposits from the base upward.

Geographic entities mentioned:
surface_form: South Tuya
instance_of: Mountain
countries: Canada
coordinates: lat: 59.20861111
lon: -130.50527778
surface_form: ash mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 59.2744
lon: -130.509
Caribou Tuya. Caribou Tuya is a basaltic subglacial mound in far northwestern British Columbia that began eruptive activity under glacial ice during the Fraser glaciation (25 to 10 ka). Like Ash Mountain and South Tuya, sections of the subglacial mound reveal a consistent stratigraphic progression from pillow lavas to hyaloclastite deposits from the base upward.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: caribou tuya
instance_of: Mountain
countries: Canada
coordinates: lat: 59.2364
lon: -130.562
Caribou Tuya. Caribou Tuya is a basaltic subglacial mound in far northwestern British Columbia that began eruptive activity under glacial ice during the Fraser glaciation (25 to 10 ka). Like Ash Mountain and South Tuya, sections of the subglacial mound reveal a consistent stratigraphic progression from pillow lavas to hyaloclastite deposits from the base upward.

Geographic entities mentioned:
surface_form: caribou tuya
instance_of: Mountain
countries: Canada
coordinates: lat: 59.2364
lon: -130.562
Locally the sections are capped by subaerial basaltic lava flows. Samples of the glassy pillow basalts and hyaloclastites along with crystalline basalt flows were collected at Caribou Tuya. The volcano is believed to have formed and last erupted during the Pleistocene Epoch.

Geographic entities mentioned:
surface_form: caribou tuya
instance_of: Mountain
countries: Canada
coordinates: lat: 59.2364
lon: -130.562
Much of the border follows the Southern Turkish stretch of the Baghdad Railway, roughly along the 37th parallel between the 37th and 42nd eastern meridians. In the west, it almost surrounds the Turkish Hatay Province, partly following the course of the Orontes River and reaching the Mediterranean coast at the foot of Jebel Aqra. Description.

Geographic entities mentioned:
surface_form: Jebel Aqra
instance_of: Mountain
countries: Syria
Turkey
coordinates: lat: 35.9525
lon: 35.969305555556
Mazzafegato. &quot;Mazzafegato&quot; or &quot;mazafegghito&quot; is a sausage produced in central Italy. It comes from the upper Tiber Valley, Valtiberina (where it is also called &quot;sambudello&quot;), in Tuscany and Umbria, and from Marche. Etymology. The name means 'killing/butchering liver' (&quot;ammazza fegato&quot;). Production.

Geographic entities mentioned:
surface_form: Tiber Valley
instance_of: Valley
countries: Italy
coordinates: lat: 42.133333333333
lon: 12.583333333333
surface_form: Valtiberina
instance_of: Valley
countries: Italy
coordinates: lat: 43.56666667
lon: 12.11666667
The nearest town is Moab, Utah about to the southwest. The area is generally accessed from Fisher Towers Road off of Route 128 which runs along the Colorado River between I-70 and Route 191. Castleton Tower is visible approximately to the southwest from different parts of the Fisher Tower's area. The Towers lie just south of a larger mesa which they are emerging from on a geological time scale.

Geographic entities mentioned:
surface_form: Castleton Tower
instance_of: Mountain
countries: United States
coordinates: lat: 38.6514
lon: -109.3686
The ridge line of the fin drops considerable before reaching the western formation called &quot;Ancient Art&quot;. &quot;Ancient Art&quot; is composed of four separate summits the most striking of which is the &quot;cork screw summit.&quot; The Middle fin is split into two very distinct towers known as &quot;Echo Tower&quot; in the east and &quot;Cottontail&quot; in the west.

Geographic entities mentioned:
surface_form: Echo Tower
instance_of: Mountain
coordinates: lat: 38.72027
lon: -109.30084
Fisher Towers. Fisher Towers are a series of towers made of Cutler sandstone capped with Moenkopi sandstone and caked with a stucco of red mud located near Moab, Utah (). The Towers are named for a miner who lived near them in the 1880s. The Towers are world-renowned as a subject for photography and for its classic rock climbing routes. Location.

Geographic entities mentioned:
surface_form: fisher towers
instance_of: Mountain
countries: United States
coordinates: lat: 38.724
lon: -109.308
Location. The nearest town is Moab, Utah about to the southwest. The area is generally accessed from Fisher Towers Road off of Route 128 which runs along the Colorado River between I-70 and Route 191. Castleton Tower is visible approximately to the southwest from different parts of the Fisher Tower's area.

Geographic entities mentioned:
surface_form: fisher towers
instance_of: Mountain
countries: United States
coordinates: lat: 38.724
lon: -109.308
Photographs of the unusual cork screw summit have been extensively published in many settings including mainstream advertisements. In film. The Fisher Towers were featured in the opening scene of &quot;Austin Powers in Goldmember&quot;. Television commercials, advertisements, and even scenes from famous movies have been filmed in the area of Moab, Utah (where the Fisher Towers are located).

Geographic entities mentioned:
surface_form: fisher towers
instance_of: Mountain
countries: United States
coordinates: lat: 38.724
lon: -109.308
Mount Du. Mount Du (), which means Lonely Hill in Chinese, is a small mountain near Nanyang City, Henan province, China. Mine. The hill is rich in a jade substitute or simulant stone, saussurite. &quot;Dushan jade&quot; is a misnomer. It is not the true jade found in Xinjiang, China: nephrite, a CaMg silicate (Si), nor the true jade found in Burma: jadeite, a NaAl silicate (Si).

Geographic entities mentioned:
surface_form: mount du
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 33.070277777778
lon: 112.58638888889
Mine. The hill is rich in a jade substitute or simulant stone, saussurite. &quot;Dushan jade&quot; is a misnomer. It is not the true jade found in Xinjiang, China: nephrite, a CaMg silicate (Si), nor the true jade found in Burma: jadeite, a NaAl silicate (Si). It is a fine grained mixture of feldspar and epidote.

Geographic entities mentioned:
surface_form: dushan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 33.070277777778
lon: 112.58638888889
It is not the true jade found in Xinjiang, China: nephrite, a CaMg silicate (Si), nor the true jade found in Burma: jadeite, a NaAl silicate (Si). It is a fine grained mixture of feldspar and epidote. It is currently marketed under the names, Dushan jade, Swiss jade (1st identified by Swiss mineralogist), and Nanyang jade (Nanyang, Henan Province). Local culture.

Geographic entities mentioned:
surface_form: dushan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 33.070277777778
lon: 112.58638888889
Its studios are located at 5000 d'Iberville street in the Plateau Mont-Royal district of Montreal. It broadcasts on 91.3 MHz with an effective radiated power of 36,200 watts (class C1) using an omnidirectional antenna located atop Mount Royal. Radio Ville-Marie now stylized as Radio VM received CRTC approval in 1994 to operate a new religious French-language FM radio programming at Montreal.

Geographic entities mentioned:
surface_form: Mount Royal
instance_of: Mountain
countries: Canada
coordinates: lat: 45.506388888889
lon: -73.588888888889
The Lac de l'Oriente to the north of the Monte Rotondo, drains through the Ruisseau de Lamento or Timozzo, a tributary of the Restonica. The small Lac de Pozzolo to the east of Monte Rotondo drains through the Ruisseau de Pozzolo, a tributary of the Ruisseau de Rivesecco, another tributary of the Restonica. The D623 road follows the river for most of its course. Tourism.

Geographic entities mentioned:
surface_form: Monte Rotondo
instance_of: Mountain
countries: France
coordinates: lat: 42.21611111111111
lon: 9.058055555555555
Brûlé Lake (Lac-Jacques-Cartier). Lac Brûlé (&quot;English: Burnt Lake&quot;) is a body of fresh water located northeast of the city of Quebec, in the unorganized territory of Lac-Jacques-Cartier, in the La Côte-de-Beaupré Regional County Municipality, in the administrative region of Capitale-Nationale, in the province, in Quebec, in Canada.

Geographic entities mentioned:
surface_form: lac brûlé
instance_of: Lake
countries: Canada
coordinates: lat: 52.25
lon: -63.8
surface_form: lac brûlé
instance_of: Lake
countries: Canada
coordinates: lat: 52.25
lon: -63.8
surface_form: burnt lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.25
lon: -63.8
surface_form: lac brûlé
instance_of: Lake
countries: Canada
coordinates: lat: 47.305
lon: -70.896944
surface_form: lac brûlé
instance_of: Lake
countries: Canada
coordinates: lat: 47.305
lon: -70.896944
Forestry is the main economic activity in this valley; recreational tourism, second. Because of the altitude, the surface of Lac Brûlé is generally frozen from the end of November until the beginning of April; however, safe circulation on the ice is generally done from the beginning of December until the beginning of April. Geography. Lac Brûlé has a length of, a width of and an altitude of.

Geographic entities mentioned:
surface_form: lac brûlé
instance_of: Lake
countries: Canada
coordinates: lat: 52.25
lon: -63.8
surface_form: lac brûlé
instance_of: Lake
countries: Canada
coordinates: lat: 47.305
lon: -70.896944
Brûlé Lake (Lac-Jacques-Cartier). Lac Brûlé (&quot;English: Burnt Lake&quot;) is a body of fresh water located northeast of the city of Quebec, in the unorganized territory of Lac-Jacques-Cartier, in the La Côte-de-Beaupré Regional County Municipality, in the administrative region of Capitale-Nationale, in the province, in Quebec, in Canada.

Geographic entities mentioned:
surface_form: brûlé lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.25
lon: -63.8
surface_form: brûlé lake (lac-jacques-cartier)
instance_of: Lake
countries: Canada
coordinates: lat: 47.305
lon: -70.896944
From the dam at the mouth of Brûlé Lake, the current descends following the outlet of Brûlé Lake on, then the course of the Brûlé River on, then flows on first towards the south-east, then the south-west, following the course of the Sainte-Anne River, which crosses downtown Beaupré, to the northwest shore of the Saint Lawrence River. Toponymy.

Geographic entities mentioned:
surface_form: brûlé lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.25
lon: -63.8
surface_form: brûlé lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.25
lon: -63.8
Geography. Lac Brûlé has a length of, a width of and an altitude of. This misshapen body of water looks like a mushroom, the stem of which leans west. Lac Savane is mainly supplied by the outlet of Lac des Vases, an unidentified stream and the outlet of Lac à Chiens. Lac Brûlé is a body of water artificially enhanced by the construction of a dam at its mouth.

Geographic entities mentioned:
surface_form: mushroom
instance_of: Mountain
countries: Canada
coordinates: lat: 62.8
lon: -137.45
Lac de la Rivière aux Anglais. The lac de la Rivière aux Anglais (&quot;English: Lake of the English River&quot;) is a freshwater body of the watershed of rivière aux Anglais, flowing in the unorganized territory of Rivière-aux-Outardes, in the Manicouagan Regional County Municipality, in the administrative region of Côte-Nord, in the province from Quebec, to Canada.

Geographic entities mentioned:
surface_form: rivière aux Anglais
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.256666666667
lon: -68.133611111111
surface_form: rivière aux anglais
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.256666666667
lon: -68.133611111111
surface_form: rivière aux anglais
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.256666666667
lon: -68.133611111111
surface_form: lac de la rivière aux anglais
instance_of: Lake
countries: Canada
coordinates: lat: 49.28032
lon: -68.15558
Forestry and hydroelectricity are the main economic activity around the lake. Geography. The lac de la Rivière aux Anglais is located in the eastern part of the territory of the town of Baie-Comeau. This lake crossed to the southeast by the rivière aux Anglais, has a length of, a maximum width of and an altitude of. It has three islands. This lake is formed by the dam erected at its mouth.

Geographic entities mentioned:
surface_form: rivière aux Anglais
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.256666666667
lon: -68.133611111111
surface_form: rivière aux anglais
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.256666666667
lon: -68.133611111111
From the mouth of the lac de la Rivière aux Anglais, the current descends on generally towards the south-east, following the course of the rivière aux Anglais, in particular by passing at the end of the segment on the north side of an industrial sector in the eastern part of Baie-Comeau, to discharge onto the west shore of Baie aux Anglais, on the north shore of the estuary of Saint Lawrence.

Geographic entities mentioned:
surface_form: rivière aux Anglais
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.256666666667
lon: -68.133611111111
surface_form: rivière aux anglais
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.256666666667
lon: -68.133611111111
surface_form: rivière aux anglais
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.256666666667
lon: -68.133611111111
surface_form: lac de la rivière aux anglais
instance_of: Lake
countries: Canada
coordinates: lat: 49.28032
lon: -68.15558
Lac de la Rivière aux Anglais. The lac de la Rivière aux Anglais (&quot;English: Lake of the English River&quot;) is a freshwater body of the watershed of rivière aux Anglais, flowing in the unorganized territory of Rivière-aux-Outardes, in the Manicouagan Regional County Municipality, in the administrative region of Côte-Nord, in the province from Quebec, to Canada.

Geographic entities mentioned:
surface_form: rivière aux anglais
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.256666666667
lon: -68.133611111111
surface_form: lac de la rivière aux anglais
instance_of: Lake
countries: Canada
coordinates: lat: 49.28032
lon: -68.15558
The surroundings of Rivière aux Anglais lake are served by a few forest roads connecting from the south to the Rivière aux Anglais path. Forestry and hydroelectricity are the main economic activity around the lake. Geography. The lac de la Rivière aux Anglais is located in the eastern part of the territory of the town of Baie-Comeau.

Geographic entities mentioned:
surface_form: rivière aux anglais
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.256666666667
lon: -68.133611111111
surface_form: rivière aux anglais
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.256666666667
lon: -68.133611111111
Forestry and hydroelectricity are the main economic activity around the lake. Geography. The lac de la Rivière aux Anglais is located in the eastern part of the territory of the town of Baie-Comeau. This lake crossed to the southeast by the rivière aux Anglais, has a length of, a maximum width of and an altitude of. It has three islands. This lake is formed by the dam erected at its mouth.

Geographic entities mentioned:
surface_form: rivière aux anglais
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.256666666667
lon: -68.133611111111
Toponym. The toponym &quot;Lac de la Rivière aux Anglais&quot; derives from the name of the river. The toponym &quot;Lac de la Rivière aux Anglais&quot; was formalized on August 2, 1974, at the Place Names Bank of the Commission de toponymie du Québec.

Geographic entities mentioned:
surface_form: rivière aux anglais
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.256666666667
lon: -68.133611111111
surface_form: lac de la rivière aux anglais
instance_of: Lake
countries: Canada
coordinates: lat: 49.28032
lon: -68.15558
surface_form: lac de la rivière aux anglais
instance_of: Lake
countries: Canada
coordinates: lat: 49.28032
lon: -68.15558
Toponym. The toponym &quot;Lac de la Rivière aux Anglais&quot; derives from the name of the river. The toponym &quot;Lac de la Rivière aux Anglais&quot; was formalized on August 2, 1974, at the Place Names Bank of the Commission de toponymie du Québec.

Geographic entities mentioned:
surface_form: rivière aux anglais
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.256666666667
lon: -68.133611111111
Taxonomy and naming. &quot;Eremophila biserrata&quot; was first formally described by Robert Chinnock in 1979 and the description was published in &quot;Journal of the Adelaide Botanic Garden&quot;. Chinnock collected the type specimen north of the road between Hyden and Lake Cronin. The specific epithet (&quot;biserrata&quot;) refers to the unusually serrated leaf margins.

Geographic entities mentioned:
surface_form: Lake Cronin
instance_of: Lake
countries: Australia
coordinates: lat: -32.385555555556
lon: 119.765
Ereta Peak. A peak rising to high at the north extremity of Bastien Range. It is situated 12.88 km northwest of Ichev Nunatak, 19.63 km southwest of Mount Gardner and 22.5 km west of Mount Vinson in Sentinel Range. It has steep and partly ice-free north and southwest slopes. Erata Peak surmounts upper Nimitz Glacier to the southeast.

Geographic entities mentioned:
surface_form: Mount Gardner
instance_of: Mountain
coordinates: lat: -78.405
lon: -85.965
Mount Michener. Mount Michener is a mountain on the eastern border of the Canadian Rockies in Alberta, Canada. It forms the northerly part of the Ram Range. The mountain sits on the shore of Abraham Lake and its north, west and south face are all visible from the David Thompson Highway.

Geographic entities mentioned:
surface_form: mount michener
instance_of: Mountain
countries: Canada
coordinates: lat: 52.20666666666666
lon: -116.39055555555555
Mount Michener. Mount Michener is a mountain on the eastern border of the Canadian Rockies in Alberta, Canada. It forms the northerly part of the Ram Range. The mountain sits on the shore of Abraham Lake and its north, west and south face are all visible from the David Thompson Highway.

Geographic entities mentioned:
surface_form: mount michener
instance_of: Mountain
countries: Canada
coordinates: lat: 52.20666666666666
lon: -116.39055555555555
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The pressure on the fault line caused thousands of metres of rock to thrust upward. The contorted beds near the summit of Mount Michener are visible evidence of the tremendous force that caused its formation. A system of limestone caves does exist within the mountain, but they remain undocumented.

Geographic entities mentioned:
surface_form: mount michener
instance_of: Mountain
countries: Canada
coordinates: lat: 52.20666666666666
lon: -116.39055555555555
Mount Michener is a mountain on the eastern border of the Canadian Rockies in Alberta, Canada. It forms the northerly part of the Ram Range. The mountain sits on the shore of Abraham Lake and its north, west and south face are all visible from the David Thompson Highway. The mountain was named in 1982 after Daniel Roland Michener who was the Governor General of Canada from 1967 - 1974.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The mountain was named in 1982 after Daniel Roland Michener who was the Governor General of Canada from 1967 - 1974. Its previous names were Eye Opener Mountain and Phoebe's Teat, reportedly after a woman from Rocky Mountain House who would periodically visit the Nordegg miners in the 1930s. Geography.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The pressure on the fault line caused thousands of metres of rock to thrust upward. The contorted beds near the summit of Mount Michener are visible evidence of the tremendous force that caused its formation. A system of limestone caves does exist within the mountain, but they remain undocumented.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Santorini caldera is a large, mostly submerged caldera, located in the southern Aegean Sea, 120 kilometers north of Crete in Greece. Visible above water is the circular Santorini island group, consisting of Santorini (known as Thera in antiquity), the main island, Therasia and Aspronisi at the periphery, and the Kameni islands at the center. It has been designated a Decade Volcano. Geography.

Geographic entities mentioned:
surface_form: thera
instance_of: Mountain
countries: Greece
coordinates: lat: 36.403611
lon: 25.396389
surface_form: santorini
instance_of: Mountain
countries: Greece
coordinates: lat: 36.403611
lon: 25.396389
surface_form: santorini
instance_of: Mountain
countries: Greece
coordinates: lat: 36.403611
lon: 25.396389
Santorini caldera. Santorini caldera is a large, mostly submerged caldera, located in the southern Aegean Sea, 120 kilometers north of Crete in Greece. Visible above water is the circular Santorini island group, consisting of Santorini (known as Thera in antiquity), the main island, Therasia and Aspronisi at the periphery, and the Kameni islands at the center.

Geographic entities mentioned:
surface_form: santorini caldera
instance_of: Mountain
countries: Greece
coordinates: lat: 36.403611
lon: 25.396389
It has been designated a Decade Volcano. Geography. The caldera measures about, with high steep cliffs on three sides, and a maximum depth of. There are two small volcanic islands at the center of the caldera, Nea (&quot;New&quot;) Kameni and Palea (&quot;Old&quot;) Kameni. The main island, Santorini has an area of, Therasia, and the uninhabited islands of Nea Kameni, Palea Kameni and Aspronisi.

Geographic entities mentioned:
surface_form: santorini
instance_of: Mountain
countries: Greece
coordinates: lat: 36.403611
lon: 25.396389
Geology. The volcanic complex of Santorini is the most active part of the South Aegean Volcanic Arc, which includes the active volcanoes of Methana on the mainland of Greece, Milos, Santorini and Nisyros.

Geographic entities mentioned:
surface_form: santorini
instance_of: Mountain
countries: Greece
coordinates: lat: 36.403611
lon: 25.396389
surface_form: santorini
instance_of: Mountain
countries: Greece
coordinates: lat: 36.403611
lon: 25.396389
This subduction causes earthquakes at depths of 150–170 km. Non-volcanic rocks are exposed on Santorini at Mikro Profititis Ilias, Mesa Vouno, the Gavrillos ridge, Pirgos, Monolithos and the inner side of the caldera wall between Cape Plaka and Athinios. The Kameni islands at the center of the caldera are made of lava rocks. Volcanology.

Geographic entities mentioned:
surface_form: santorini
instance_of: Mountain
countries: Greece
coordinates: lat: 36.403611
lon: 25.396389