Sarmila/GeoWiki-Features huggingface dataset:
Lac de Creno. The Lac de Creno () is a small lake in the Monte Rotondo massif in the Corse-du-Sud department of France. Location. The Lac de Creno is in the Monte Rotondo massif at an altitude of. It is in the Orto commune of Corse-du-Sud to the north of the Monte Sant Eliseo. It is drained by the Ruisseau de Creno, which flows south to join the Fiume Grosso, a tributary of the Liamone river.

Geographic entities mentioned:
surface_form: monte rotondo
instance_of: Mountain
countries: France
coordinates: lat: 42.21611111111111
lon: 9.058055555555555
surface_form: lac de creno
instance_of: Lake
countries: France
coordinates: lat: 42.2047
lon: 8.94611
Lac de Creno. The Lac de Creno () is a small lake in the Monte Rotondo massif in the Corse-du-Sud department of France. Location. The Lac de Creno is in the Monte Rotondo massif at an altitude of. It is in the Orto commune of Corse-du-Sud to the north of the Monte Sant Eliseo. It is drained by the Ruisseau de Creno, which flows south to join the Fiume Grosso, a tributary of the Liamone river.

Geographic entities mentioned:
surface_form: lac de creno
instance_of: Lake
countries: France
coordinates: lat: 42.2047
lon: 8.94611
Pilot Knob (Austin, Texas). Pilot Knob is the eroded core of an extinct volcano located in Austin, Texas, United States. It is near Austin–Bergstrom International Airport and McKinney Falls State Park. Introduction. Pilot Knob is one of around 75 late-Cretaceous Period volcanoes scattered around Central Texas from Waco to Austin, San Antonio, and Del Rio.

Geographic entities mentioned:
surface_form: pilot knob (austin, texas)
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
Pilot Knob (Austin, Texas). Pilot Knob is the eroded core of an extinct volcano located in Austin, Texas, United States. It is near Austin–Bergstrom International Airport and McKinney Falls State Park. Introduction. Pilot Knob is one of around 75 late-Cretaceous Period volcanoes scattered around Central Texas from Waco to Austin, San Antonio, and Del Rio.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
Pilot Knob is the eroded core of an extinct volcano located in Austin, Texas, United States. It is near Austin–Bergstrom International Airport and McKinney Falls State Park. Introduction. Pilot Knob is one of around 75 late-Cretaceous Period volcanoes scattered around Central Texas from Waco to Austin, San Antonio, and Del Rio. All of these volcanoes have been extinct for millions of years.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
All of these volcanoes have been extinct for millions of years. The Pilot Knob volcanic complex consists of four small, rounded hills (including Pilot Knob proper) forming the volcano's core area in an area two miles in diameter. The hills are composed of trap rock which is an erosion-resistant, fine-grained mafic volcanic rock.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
The volcano formed when magma worked its way to the surface and encountered water-laden, unconsolidated sediments with the existing water rapidly vaporizing into steam resulting in an enormous explosion that formed an explosion crater. Explosive eruptions continued at Pilot Knob as new magma encountered more water in the volcanic ash. Gradually, an ash cone was built up over the explosion crater.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
Gradually, an ash cone was built up over the explosion crater. Eruptions of ash continued until the mound grew above the level of the shallow sea. Ash beds, now altered to clay, occur interbedded with limestone and marl of the Austin Group around Pilot Knob; these ash beds provide evidence for subaerial eruptions at Pilot Knob.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
The Pilot Knob ash cone eventually built an unstable slope on the sea bottom, resulting in mud flows of ash and carbonate mud which tore up the underlying carbonate mud in places and injected itself into the carbonate mud at other places. The subaerial Pilot Knob ash cone allowed the intrusion of magma into the mound without contact with sea water, resulting in quieter lava eruptions.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
Some of the trap rock bodies are the erosional remnants of lava flows, due to their apparent dip away from the central core area. Cooling joints exposed on a hill about west of Pilot Knob suggest a dip of that trap rock body towards the center of the core area, possibly indicating that it is the erosional remnant of a cone sheet injected outwards from a central, discordant intrusive body of magma.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
During the Tertiary era, the central Texas area was uplifted, exposing the volcano as younger sedimentary rocks were eroded from the Cretaceous volcanic rocks. Today the terrain at Pilot Knob reflects the relative resistance to erosion of the different rock types that appear around the volcanic complex. Dating the volcanic activity.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
Today the terrain at Pilot Knob reflects the relative resistance to erosion of the different rock types that appear around the volcanic complex. Dating the volcanic activity. Two different approaches have been used by geologists to date the volcanism at Pilot Knob. The first approach was through the stratigraphy of the rocks at and around Pilot Knob and the fossils they contain.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
Dating the volcanic activity. Two different approaches have been used by geologists to date the volcanism at Pilot Knob. The first approach was through the stratigraphy of the rocks at and around Pilot Knob and the fossils they contain. The second approach was by isotopic age dating of the igneous rocks. The two means are very different, but supplement each other nicely. Stratigraphy.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
The two means are very different, but supplement each other nicely. Stratigraphy. The volcano at Pilot Knob exerted a profound influence on the stratigraphy of the Upper Cretaceous sedimentary rocks of the Austin area. The volcanism occurred during the deposition of the upper part of the Dessau and the Burditt formations of the Austin Chalk.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
Stratigraphy. The volcano at Pilot Knob exerted a profound influence on the stratigraphy of the Upper Cretaceous sedimentary rocks of the Austin area. The volcanism occurred during the deposition of the upper part of the Dessau and the Burditt formations of the Austin Chalk. These strata are only about one-third as thick near Pilot Knob as they are in other localities around Austin.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
These strata are only about one-third as thick near Pilot Knob as they are in other localities around Austin. The faunal zones of the two formations, that is zones within the formations where certain fossils are particularly abundant, are also telescoped in the vicinity of Pilot Knob. Two beds of altered ash occur within the Dessau Formation on Rinard Creek near Pilot Knob.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
Two beds of altered ash occur within the Dessau Formation on Rinard Creek near Pilot Knob. The exact relationship of the beach rock of the northern flank of Pilot Knob with the normal Austin Chalk has been demonstrated to be part of the Exponderosa erraticosta zone, although it may extend down to an age equivalent to the upper part of the Dessau in some areas along Onion Creek.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
The beach rock is now known as the McKown Formation of the Austin Chalk. Because the volcanism at Pilot Knob occurred during the deposition of the Dessau and Burditt Formations, an age of Lower Campanian (83 to 79 million years BP) can be interpreted for the volcanism according to the ages of the formations in the Austin Chalk, correlated to radiometric dated sections in the Rocky Mountain Region.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
Isotopic age. The potassium-argon method was utilized to determine the age of volcanism at Pilot Knob. This method is based upon the decay of the radioactive isotope of potassium (potassium 40) to argon 40, an isotope of argon, an inert gas.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
The age of Pilot Knob volcanism dated through the potassium-argon method is 79.5 +/- 3 million years, and agrees with the age derived by correlation with fossils to other radiometrically dated deposits. Source of the magma. The igneous rocks of the Pilot Knob volcano have not, as yet, undergone rigorous petrological study, although such studies are in progress.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
Source of the magma. The igneous rocks of the Pilot Knob volcano have not, as yet, undergone rigorous petrological study, although such studies are in progress. Similar rocks near Uvalde, Texas, of about the same age, have been studied.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
Similar rocks near Uvalde, Texas, of about the same age, have been studied. The Uvalde rocks are of the same igneous province as the Pilot Knob rocks; both are centers in a chain of volcanic and intrusive complexes that parallel the buried Ouachita structural belt in central and south Texas.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
Most of the igneous rocks on the surface probably are not representative of the original magmas formed in the mantle; certain processes, such as separation of phenocrysts from the liquid from which they crystallized have altered their original chemical compositions at depths shallower than the mantle. By inference, the rocks at Pilot Knob crystallized from partial melts of the upper mantle.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
By inference, the rocks at Pilot Knob crystallized from partial melts of the upper mantle. Only rocks of the second series have been discovered at Pilot Knob; no basaltic rocks have been located. No mantle fragments have been located in Pilot Knob igneous rocks, but their presence is suspected, and some of the olivine phenocrysts in the rocks may be fragments derived from the upper mantle.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
Only rocks of the second series have been discovered at Pilot Knob; no basaltic rocks have been located. No mantle fragments have been located in Pilot Knob igneous rocks, but their presence is suspected, and some of the olivine phenocrysts in the rocks may be fragments derived from the upper mantle. Location.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
No mantle fragments have been located in Pilot Knob igneous rocks, but their presence is suspected, and some of the olivine phenocrysts in the rocks may be fragments derived from the upper mantle. Location. Pilot Knob can be reached by driving south of Austin on Highway 183 past Austin-Bergstrom International Airport. The hill is visible on the right after crossing Onion Creek.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
The lowland is drained by Cottonmouth Creek and underlain by soft, easily eroded volcanic ash and other pyroclastic deposits, and the central core area formed by the resistant trap rock are easily visible to the south of Dee Gabriel Collins. About 2/3 of a mile east of the intersection of Bluff Springs Road with McKinney Falls Parkway, the trap rock of south Pilot Knob crops out along the road.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
This rock is very similar to that which forms the center of the volcano, and may represent the eroded remnant of a lava flow erupted along the flanks of the volcano or having flowed down the south side from the apex. Except for the road margins, Pilot Knob volcano lies entirely on private land. In popular culture.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
Except for the road margins, Pilot Knob volcano lies entirely on private land. In popular culture. The second season of the American procedural drama television series ' featured a scenario where Pilot Knob reactivated, and the characters' attempts at saving lives as a result of the eruption.

Geographic entities mentioned:
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 30.1622
lon: -97.7061
surface_form: pilot knob
instance_of: Mountain
countries: United States
coordinates: lat: 32.7316
lon: -114.75
South Mountain is a mountain in Greene County, New York and partially in Schoharie County, New York. It is located in the Catskill Mountains southwest of West Durham. Ashland Pinnacle is located west-southwest, and Steenburg Mountain is located north of South Mountain. The 1,498-acre South Mountain State Forest is a popular destination in the area that offers hiking, camping, hunting and skiing.

Geographic entities mentioned:
surface_form: Steenburg Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.39453
lon: -74.27486
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.182222222222
lon: -74.477777777778
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.949166666667
lon: -74.293333333333
surface_form: south mountain
instance_of: Landform
countries: United States
coordinates: lat: 40.33
lon: -76.2
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5544
lon: -72.8236
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.40111111
lon: -109.26111111
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.189166666667
lon: -74.051666666667
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.361944444444
lon: -74.285277777778
South Mountain (Ashland, New York). South Mountain is a mountain in Greene County, New York and partially in Schoharie County, New York. It is located in the Catskill Mountains southwest of West Durham. Ashland Pinnacle is located west-southwest, and Steenburg Mountain is located north of South Mountain.

Geographic entities mentioned:
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.182222222222
lon: -74.477777777778
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.949166666667
lon: -74.293333333333
surface_form: south mountain
instance_of: Landform
countries: United States
coordinates: lat: 40.33
lon: -76.2
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5544
lon: -72.8236
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.40111111
lon: -109.26111111
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.189166666667
lon: -74.051666666667
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.361944444444
lon: -74.285277777778
South Mountain (Ashland, New York). South Mountain is a mountain in Greene County, New York and partially in Schoharie County, New York. It is located in the Catskill Mountains southwest of West Durham. Ashland Pinnacle is located west-southwest, and Steenburg Mountain is located north of South Mountain.

Geographic entities mentioned:
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.182222222222
lon: -74.477777777778
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.949166666667
lon: -74.293333333333
surface_form: south mountain
instance_of: Landform
countries: United States
coordinates: lat: 40.33
lon: -76.2
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5544
lon: -72.8236
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.40111111
lon: -109.26111111
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.189166666667
lon: -74.051666666667
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.361944444444
lon: -74.285277777778
South Mountain is a mountain in Greene County, New York and partially in Schoharie County, New York. It is located in the Catskill Mountains southwest of West Durham. Ashland Pinnacle is located west-southwest, and Steenburg Mountain is located north of South Mountain. The 1,498-acre South Mountain State Forest is a popular destination in the area that offers hiking, camping, hunting and skiing.

Geographic entities mentioned:
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.182222222222
lon: -74.477777777778
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.949166666667
lon: -74.293333333333
surface_form: south mountain
instance_of: Landform
countries: United States
coordinates: lat: 40.33
lon: -76.2
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5544
lon: -72.8236
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.40111111
lon: -109.26111111
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.189166666667
lon: -74.051666666667
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.361944444444
lon: -74.285277777778
He was running far behind schedule due to severe weather damage to a large area of New Jersey. He arrived late and delivered a truncated speech, causing many residents in this heavily Democratic area to feel he had slighted their city. In 2000, the Lower Naugatuck Valley, which includes Ansonia, was named an &quot;All America City&quot; by the National Civic League. Rubber plant fire.

Geographic entities mentioned:
surface_form: Lower Naugatuck Valley
instance_of: Valley
countries: United States
Geography. According to the United States Census Bureau, the city has a total area of, of which is land and, or 2.72%, is water. The city is bisected by the Naugatuck River and spreads out from the river's banks up the hills—some quite steep—of the river valley. On the west side of the river, the city abuts Derby and Seymour along Silver Hill.

Geographic entities mentioned:
surface_form: river valley
instance_of: Valley
countries: United States
Landmarks. In addition to the Farrel Corporation and Ansonia Copper & Brass facilities along the banks of the Naugatuck River in the center of the city, Ansonia's landmarks include its public library (Ansonia Library), the Anna Sewell Memorial Fountain (honoring the author of &quot;Black Beauty&quot;), in front of the Library YMCA, National Guard Armory and many Victorian and Queen Anne houses.

Geographic entities mentioned:
surface_form: Naugatuck River
instance_of: Valley
countries: United States
Octavian's forces prevailed in the war, however, and as a result the kingdom's throne was reverted to Iamblichus II (the son of Iamblichus I) after Alexander was executed for treason. It was in 32 that Heliopolis and the Beqaa Valley came under the kingdom's control. Relations with the Roman government grew closer when King Sohaemus inherited the kingship.

Geographic entities mentioned:
surface_form: Beqaa Valley
instance_of: Valley
countries: Lebanon
coordinates: lat: 34.008888888889
lon: 36.145277777778
The coming of the Ottomans brought administrative changes to Homs, as it became the capital city of &quot;sanjak&quot; (&quot;district&quot;) of Homs, attached to the &quot;eyalet&quot; (&quot;province&quot;) of Tripoli—its old rival. In the late 16th century the district was ruled by emir 'Ali Harfush of the famous Shiite Harfush dynasty of the nearby Beqaa valley.

Geographic entities mentioned:
surface_form: Beqaa valley
instance_of: Valley
countries: Lebanon
coordinates: lat: 34.008888888889
lon: 36.145277777778
Lagorai. The Lagorai is a mountain range in the Eastern Alps, in Trentino, northern Italy. It is located between the Monte Panarotta (16 km) from Trento and Rolle Pass, for a length of some 70 km. It is bounded southwards by the Valsugana, by the Val di Fiemme from the north, the Val di Cembra from the west and the Primiero and Vanoi eastwards. The chain is mostly made of porphyry rocks.

Geographic entities mentioned:
surface_form: Monte Panarotta
instance_of: Mountain
countries: Italy
coordinates: lat: 46.05001
lon: 11.33507
Lagorai. The Lagorai is a mountain range in the Eastern Alps, in Trentino, northern Italy. It is located between the Monte Panarotta (16 km) from Trento and Rolle Pass, for a length of some 70 km. It is bounded southwards by the Valsugana, by the Val di Fiemme from the north, the Val di Cembra from the west and the Primiero and Vanoi eastwards. The chain is mostly made of porphyry rocks.

Geographic entities mentioned:
surface_form: Valsugana
instance_of: Valley
countries: Italy
coordinates: lat: 46
lon: 11.666666666667
surface_form: Primiero
instance_of: Valley
countries: Italy
coordinates: lat: 46.183333333333
lon: 11.833333333333
Still Brook Waterfall. Still Brook Waterfall is a waterfall at mouth of Still Brook, where the brook empties into Black Brook Cove, and so into the Cabot Strait and the Atlantic Ocean.

Geographic entities mentioned:
surface_form: Cabot Strait
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.233333333333
lon: -59.716666666667
Hystad Lake. Hystad Lake is a lake in Kandiyohi County, in the U.S. state of Minnesota. It was named for Andrew O. Hystad, a pioneer who settled there.

Geographic entities mentioned:
surface_form: hystad lake
instance_of: Lake
countries: United States
coordinates: lat: 45.38527778
lon: -95.12027778
Mill Peak. Mill Peak () is a prominent peak, high, rising above the Antarctic ice sheet south of Pearce Peak and south of Cape Simpson. it was discovered in February 1931 by the British Australian New Zealand Antarctic Research Expedition under Douglas Mawson, who named it for Dr. Hugh Robert Mill.

Geographic entities mentioned:
surface_form: Pearce Peak
instance_of: Mountain
coordinates: lat: -67.8
lon: 61.2
surface_form: mill
instance_of: Mountain
coordinates: lat: -65.25
lon: -64.05
surface_form: mill peak
instance_of: Mountain
coordinates: lat: -67.9667
lon: 61.1333
Mill Peak. Mill Peak () is a prominent peak, high, rising above the Antarctic ice sheet south of Pearce Peak and south of Cape Simpson. it was discovered in February 1931 by the British Australian New Zealand Antarctic Research Expedition under Douglas Mawson, who named it for Dr. Hugh Robert Mill.

Geographic entities mentioned:
surface_form: mill
instance_of: Mountain
coordinates: lat: -65.25
lon: -64.05
surface_form: mill peak
instance_of: Mountain
coordinates: lat: -67.9667
lon: 61.1333
Mill Peak. Mill Peak () is a prominent peak, high, rising above the Antarctic ice sheet south of Pearce Peak and south of Cape Simpson. it was discovered in February 1931 by the British Australian New Zealand Antarctic Research Expedition under Douglas Mawson, who named it for Dr. Hugh Robert Mill.

Geographic entities mentioned:
surface_form: mill
instance_of: Mountain
coordinates: lat: -65.25
lon: -64.05
Saline wetlands are dominated by &quot;Salicornia herbacea&quot; and &quot;Salicornia fruticosa&quot;. Fauna. Large mammals include wild boar (&quot;Sus scrofa&quot;), red deer (&quot;Cervus elaphus elaphus&quot;), roe deer (&quot;Capreolus capreolus&quot;) and Iberian wolf (&quot;Canis lupus signatus&quot;). The Camargue (Rhone Delta) and Ebro Delta are important habitats for water birds.

Geographic entities mentioned:
surface_form: Ebro Delta
instance_of: Body of water
countries: Spain
coordinates: lat: 40.73243
lon: 0.86964
Western Australia has considerable resources of uranium, but to date there has been no commercial mining in the state. Mining proposals. Two uranium mining projects in the state are closer to production, the 750 tonne U3O8 Lake Maitland project, pursued by Mega Uranium, and the 680 tonne U3O8 Centipede–Lake Way project undertaken by Toro Energy, located at Lake Way. Public opposition.

Geographic entities mentioned:
surface_form: Lake Way
instance_of: Lake
countries: Australia
coordinates: lat: -26.783333333333
lon: 120.33333333333
Hammam-Lif. Hammam-Lif () is a coastal town about 20 km south-east of Tunis, the capital of Tunisia. It has been known since antiquity for its thermal springs originating in Mount Bou Kornine. History. Naro, which means fire, was Hammam-Lif's Punic name.

Geographic entities mentioned:
surface_form: Bou Kornine
instance_of: Mountain
countries: Tunisia
coordinates: lat: 36.705
lon: 10.33333333
She was inspired to take up climbing at the age of 12 after a counsellor said she did not have to do it on a camp course. Because there was no support for one-handed climbing, she devised a way of doing it herself. She accompanied Jim Ewing in a climb of the Lotus Flower Tower in the Cirque of the Unclimbables. The 2018 documentary &quot;Stumped&quot; centered on Beck and her climbing career.

Geographic entities mentioned:
surface_form: Lotus Flower Tower
instance_of: Mountain
countries: Canada
coordinates: lat: 62.1143
lon: -127.697
It is situated in the La Paz Department, Franz Tamayo Province, Pelechuco Municipality, north-west of Pelechuco. Rit'i Apachita lies northeast of the mountain Sural &quot;(Soral)&quot; and southeast of the mountain Apachita Pura Pura. There is a little lake east of the mountain named Q'illuqucha (Quechua for &quot;yellow lake&quot;, &quot;Quellucocha&quot;).

Geographic entities mentioned:
surface_form: Apachita Pura Pura
instance_of: Mountain
countries: Bolivia
coordinates: lat: -14.7244
lon: -69.1517
surface_form: apachita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.3061
lon: -69.4011
surface_form: apachita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -22.4442
lon: -67.7911
surface_form: apachita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.7631
lon: -68.5361
surface_form: apachita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.465
lon: -67.12388889
surface_form: apachita pura pura
instance_of: Mountain
countries: Bolivia
coordinates: lat: -14.7244
lon: -69.1517
Rit'i Apachita. Rit'i Apachita (Quechua, &quot;rit'i&quot; snow, Aymara and Quechua &quot;apachita&quot; the place of transit of an important pass in the principal routes of the Andes; name in the Andes for a stone cairn, a little pile of rocks built along the trail in the high mountains, Hispanicized spelling &quot;Riti Apacheta&quot;) is a mountain in the Apolobamba mountain range in Bolivia.

Geographic entities mentioned:
surface_form: apachita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.3061
lon: -69.4011
surface_form: rit'i apachita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -14.7442
lon: -69.1172
surface_form: apachita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -22.4442
lon: -67.7911
surface_form: apachita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.7631
lon: -68.5361
surface_form: apachita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.465
lon: -67.12388889
Rit'i Apachita. Rit'i Apachita (Quechua, &quot;rit'i&quot; snow, Aymara and Quechua &quot;apachita&quot; the place of transit of an important pass in the principal routes of the Andes; name in the Andes for a stone cairn, a little pile of rocks built along the trail in the high mountains, Hispanicized spelling &quot;Riti Apacheta&quot;) is a mountain in the Apolobamba mountain range in Bolivia.

Geographic entities mentioned:
surface_form: apachita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.3061
lon: -69.4011
surface_form: apachita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.3061
lon: -69.4011
surface_form: rit'i apachita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -14.7442
lon: -69.1172
surface_form: apachita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -22.4442
lon: -67.7911
surface_form: apachita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -22.4442
lon: -67.7911
surface_form: apachita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.7631
lon: -68.5361
surface_form: apachita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.7631
lon: -68.5361
surface_form: apachita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.465
lon: -67.12388889
surface_form: apachita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.465
lon: -67.12388889
Raymond Terrace in the Hunter Region of New South Wales, was chosen as a major location for producing the film. The film was released in Australian cinemas on 2 September 2010. Reception for the movie was mixed. Review aggregate website Rotten Tomatoes reports that 64% of critics have given the film a positive review, with an average score of 5.6 out of 10.

Geographic entities mentioned:
surface_form: Hunter Region
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Lake Ipala. Laguna de Ipala is a crater lake in Guatemala. The lake is located in the limits of the Departments of Jutiapa and Chiquimula, at the bottom of the wide crater of the Ipala Volcano. The lake has a surface area of and is situated at an altitude of 1,493 m (4,898 ft).

Geographic entities mentioned:
surface_form: ipala
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.55
lon: -89.63
surface_form: lake ipala
instance_of: Lake
countries: Guatemala
coordinates: lat: 14.55555556
lon: -89.63888889
Lake Ipala. Laguna de Ipala is a crater lake in Guatemala. The lake is located in the limits of the Departments of Jutiapa and Chiquimula, at the bottom of the wide crater of the Ipala Volcano. The lake has a surface area of and is situated at an altitude of 1,493 m (4,898 ft).

Geographic entities mentioned:
surface_form: ipala
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.55
lon: -89.63
surface_form: laguna de ipala
instance_of: Lake
countries: Guatemala
coordinates: lat: 14.55555556
lon: -89.63888889
Lake Ipala. Laguna de Ipala is a crater lake in Guatemala. The lake is located in the limits of the Departments of Jutiapa and Chiquimula, at the bottom of the wide crater of the Ipala Volcano. The lake has a surface area of and is situated at an altitude of 1,493 m (4,898 ft).

Geographic entities mentioned:
surface_form: ipala
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.55
lon: -89.63
surface_form: chiquimula
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.83
lon: -89.55
Description. Bear Claw Spire is a summit located in the John Muir Wilderness on the crest of the Sierra Nevada mountain range. It is situated on the common boundary shared by Fresno County with Inyo County, as well as the boundary that Sierra National Forest shares with Inyo National Forest. The peak is set northeast of Royce Peak, which is the nearest higher peak.

Geographic entities mentioned:
surface_form: Royce Peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.318055555556
lon: -118.77083333333
Lake Edward. Lake Edward (locally Rwitanzigye or Rweru) is one of the smaller African Great Lakes. It is located in the Albertine Rift, the western branch of the East African Rift, on the border between the Democratic Republic of the Congo (DRC) and Uganda, with its northern shore a few kilometres south of the equator. History.

Geographic entities mentioned:
surface_form: African Great Lakes
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
surface_form: edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
surface_form: lake edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
Topography and drainage. Lake Edward lies at an elevation of, is long by wide at its maximum points, and covers a total surface area of, making it the 15th-largest on the continent. The lake is fed by the Nyamugasani River, the Ishasha River, the Rutshuru River, the Ntungwe River, and the Rwindi River. Lake George to the northeast empties into it via the Kazinga Channel.

Geographic entities mentioned:
surface_form: Rutshuru River
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: -0.642515
lon: 29.4162
History. Welsh explorer Henry Morton Stanley first saw the lake in 1888, during the Emin Pasha Relief Expedition. The lake was named in honour of Albert Edward, Prince of Wales, son of then British monarch Queen Victoria, and later to become King Edward VII. In 1973, Uganda and Zaire (DRC) renamed it Lake Idi Amin after Ugandan dictator Idi Amin.

Geographic entities mentioned:
surface_form: albert
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: 1.6833333333333
lon: 30.916666666667
surface_form: edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
surface_form: edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
The lake is fed by the Nyamugasani River, the Ishasha River, the Rutshuru River, the Ntungwe River, and the Rwindi River. Lake George to the northeast empties into it via the Kazinga Channel. Lake Edward empties to the north via the Semliki River into Lake Albert. The western escarpment of the Great Rift Valley towers up to above the western shore of the lake.

Geographic entities mentioned:
surface_form: albert
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: 1.6833333333333
lon: 30.916666666667
surface_form: lake albert
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: 1.6833333333333
lon: 30.916666666667
surface_form: edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
surface_form: lake edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
Lake Edward. Lake Edward (locally Rwitanzigye or Rweru) is one of the smaller African Great Lakes. It is located in the Albertine Rift, the western branch of the East African Rift, on the border between the Democratic Republic of the Congo (DRC) and Uganda, with its northern shore a few kilometres south of the equator. History.

Geographic entities mentioned:
surface_form: edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
surface_form: lake edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
Topography and drainage. Lake Edward lies at an elevation of, is long by wide at its maximum points, and covers a total surface area of, making it the 15th-largest on the continent. The lake is fed by the Nyamugasani River, the Ishasha River, the Rutshuru River, the Ntungwe River, and the Rwindi River. Lake George to the northeast empties into it via the Kazinga Channel.

Geographic entities mentioned:
surface_form: edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
surface_form: lake edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
The Katwe-Kikorongo and Bunyaruguru Volcanic Fields, with extensive cones and craters, lie either side of the Kazinga Channel on the northwest shore of the lake. It is thought that Lakes George and Edward used to be joined as one larger lake, but lava from these fields flowed in and divided it, leaving only the Kazinga Channel as the remnant of the past union.

Geographic entities mentioned:
surface_form: edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
To the south lies the May-ya-Moto thermally active volcano away, and the Nyamuragira volcano in the western Virunga Mountains lies south, but its lava flows have reached the lake in the past. The Katwe-Kikorongo field features dozens of large craters and cones covering an area of by between lakes Edward and George, and includes seven crater lakes.

Geographic entities mentioned:
surface_form: edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
The Katwe-Kikorongo field features dozens of large craters and cones covering an area of by between lakes Edward and George, and includes seven crater lakes. The largest of these, the long Lake Katwe, occupies a crater across and is separated from Lake Edward by just of land. The crater is about deep, and Lake Katwe's surface is about lower than Lake Edward's.

Geographic entities mentioned:
surface_form: edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
surface_form: lake edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
The largest of these, the long Lake Katwe, occupies a crater across and is separated from Lake Edward by just of land. The crater is about deep, and Lake Katwe's surface is about lower than Lake Edward's. It is remarkable that the volcanic origin of this area southeast of the Ruwenzoris was not known until it was reported by G. F. Scott Elliot in 1894.

Geographic entities mentioned:
surface_form: edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
surface_form: lake edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
High-resolution analyses of the elemental composition of calcite and biogenic silica (BSi) content in piston cores from Lake Edward, equatorial Africa, document complex interactions between climate variability and lacustrine geochemistry over the past 5400 years.

Geographic entities mentioned:
surface_form: edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
surface_form: lake edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
Settlements. Lake Edward lies completely within the Virunga National Park (Congo) and the Queen Elizabeth National Park (Uganda) and does not have extensive human habitation on its shores, except at Ishango (DRC) in the north, home to a park ranger training facility. About two-thirds of its waters are in the DRC and one third in Uganda.

Geographic entities mentioned:
surface_form: edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
surface_form: lake edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
Ecology. Lake Edward is home to many species of fish, including populations of &quot;Bagrus docmak&quot;, &quot;Oreochromis niloticus&quot;, &quot;Oreochromis leucostictus&quot;, and over 50 species of &quot;Haplochromis&quot; and other haplochromine species, of which only 25 are formally described. Fishing is an important activity among local residents.

Geographic entities mentioned:
surface_form: edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
surface_form: lake edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
The hippopotamus is often poached for its large amount of meat as well as the ivory found in its teeth. Fueled by the high prices that hippo meat and ivory fetch, poachers are consistently hunting for these animals, which is causing a negative impact not only on the hippopotamus population, but the Lake Edward ecosystem and the local fishermen that depend on the lake for survival.

Geographic entities mentioned:
surface_form: edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
surface_form: lake edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
Fueled by the high prices that hippo meat and ivory fetch, poachers are consistently hunting for these animals, which is causing a negative impact not only on the hippopotamus population, but the Lake Edward ecosystem and the local fishermen that depend on the lake for survival. The hippopotamus population is extremely important to the ecosystem of Lake Edward due to being a keystone species.

Geographic entities mentioned:
surface_form: edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
surface_form: lake edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
The hippopotamus population is extremely important to the ecosystem of Lake Edward due to being a keystone species. Hippos produce dung, which feed tilapia, a once abundant fish species found in Lake Edward. One hippo could produce around 25 kilograms or 55 pounds of dung per day, which could feed thousands of tilapia within the ecosystem.

Geographic entities mentioned:
surface_form: edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
surface_form: lake edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
This has caused an immense decline in the tilapia population, as the decreasing hippo population cannot support the same amount of the tilapia fish species as it did before, causing a growing problem not only for the ecosystem, but the fishermen within the villages that surround Lake Edward.

Geographic entities mentioned:
surface_form: edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
surface_form: edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
surface_form: lake edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
surface_form: lake edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6