Sarmila/GeoWiki-Features huggingface dataset:
Durreck. The Durreck (, also called the &quot;Durreckspitze&quot;,) is the highest mountain in the Durreck Group, a South Tyrolean range that divides the Ahrntal valley in the north from the Reintal valley in the south. Location. The Durreck lies on the main chain of the mountains that runs from northeast to southwest.

Geographic entities mentioned:
surface_form: durreck
instance_of: Mountain
countries: Italy
coordinates: lat: 46.961219
lon: 12.029186
Further along the main chain to the northwest is the &quot;Gamskarschneide&quot;, several peaks just under the 3000-metre mark and finally the Hirbernock (3,010 m). Northwest of the Durreck are the last remnants of glaciation in the Durreck Group, the &quot;Klausenkees&quot; glacier, that still descended as low as 2,300 metres in 1910. The whole area is part of the Rieserferner-Ahrn Nature Park.

Geographic entities mentioned:
surface_form: durreck
instance_of: Mountain
countries: Italy
coordinates: lat: 46.961219
lon: 12.029186
An able mountain climber, he travelled to Rolwaling Himal to study the Sherpa people native to Nepal and the Himalayas, and fascinated by their way of thinking, he converted to Buddhism. In the late 1970s he was engaged in the Alta controversy and in protests against construction of the Innerdalsvatnet dam in the Orkla River.

Geographic entities mentioned:
surface_form: Innerdalsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 62.576111111111
lon: 10.1275
They had portrait studios in San Jose, California and Palo Alto, California. In 1892, the two men exhibited photographs of Santa Clara County, California at the California State Fair in Sacramento, California, including views of the Santa Clara Valley region, Santa Cruz Mountains, and the Mission Church in Santa Cruz.

Geographic entities mentioned:
surface_form: Santa Clara Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.366944444444
lon: -121.98388888889
Although most of the route of the Tōkaidō in Sagami and Suruga Provinces was along the seashore as the name &quot;East Sea Route&quot; implied, at Hara-juku travelers walked away from the sea. Also, up until this point on the journey, Mount Fuji could always be seen to the right of the travelers coming from Edo.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
Early life and education. Hawkes was born in Bath, New Brunswick to a Baptist family. Hawkes earned Bachelor of Science (1972) and Bachelor of Education (1973) degrees from Mount Allison University, before working as a teacher in Nova Scotia's Annapolis Valley in the later 1970s.

Geographic entities mentioned:
surface_form: Annapolis Valley
instance_of: Valley
countries: Canada
coordinates: lat: 44.979166666666664
lon: -64.89222222222222
Geological Survey who performed pioneering geologic studies in southeast Alaska in 1909–1910. &quot;Adolph Knopf Mountain&quot; was originally applied in 1968 to the mountain that is now known as Mount Ernest Gruening. The &quot;Adolph Knopf Mountain&quot; toponym was officially changed in 1976 by the U.S.

Geographic entities mentioned:
surface_form: Mount Ernest Gruening
instance_of: Mountain
countries: United States
coordinates: lat: 58.5686
lon: -134.6544
surface_form: mount ernest gruening
instance_of: Mountain
countries: United States
coordinates: lat: 58.5686
lon: -134.6544
Mount Adolph Knopf. Mount Adolph Knopf is a glaciated mountain summit located in the Boundary Ranges of the Coast Mountains, in the U.S. state of Alaska. It is situated north-northwest of Juneau to the western side of the Juneau Icefield, on land managed by Tongass National Forest.

Geographic entities mentioned:
surface_form: mount adolph knopf
instance_of: Mountain
countries: United States
coordinates: lat: 58.6783
lon: -134.7044
Climate. Based on the Köppen climate classification, Mount Adolph Knopf is located in a subpolar oceanic climate zone, with long, cold, wet winters, and cool summers. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (orographic lift), causing them to drop their moisture in the form of rain or snowfall.

Geographic entities mentioned:
surface_form: mount adolph knopf
instance_of: Mountain
countries: United States
coordinates: lat: 58.6783
lon: -134.7044
This climate supports the Eagle and Thiel glaciers surrounding the peak. History. Mount Adolph Knopf's toponym and present location was officially adopted in 1976 by the U.S. Board on Geographic Names to honor Adolph Knopf (1882–1966), American geologist with the U.S. Geological Survey who performed pioneering geologic studies in southeast Alaska in 1909–1910.

Geographic entities mentioned:
surface_form: mount adolph knopf
instance_of: Mountain
countries: United States
coordinates: lat: 58.6783
lon: -134.7044
Board on Geographic Names to honor Ernest Gruening, known as &quot;the father of Alaska statehood&quot;, the Governor of the Alaska Territory from 1939 through 1953, and one of Alaska's inaugural pair of Senators when Alaska gained statehood in 1959. The Adolph Knopf toponym was concurrently moved to the present peak eight miles north of its previous location.

Geographic entities mentioned:
surface_form: peak eight
instance_of: Mountain
countries: United States
coordinates: lat: 41.5504
lon: -123.776
Crest. The &quot;Cumann Peile Seamus O'Maille Uachtar Árd&quot; crest was designed by local artist and former player John Thomas Gibbons. The crest consists of the bridge over the Owenriff river with the Catholic church behind it, a portrait of Seamus O'Maille and a salmon representing the Lough Corrib. The club colours of green and white are also in the crest.

Geographic entities mentioned:
surface_form: Lough Corrib
instance_of: Lake
countries: Ireland
coordinates: lat: 53.466666666667
lon: -9.2833333333333
Environmental assessments are currently underway for one site next to Bruce Power's Bruce Nuclear Generating Station in Tiverton and another next to Ontario Power Generation's Darlington Nuclear Generating Station. Bruce Power has applied for a license to generate nuclear power at Cardinal Lake in the province of Alberta. Medical radioisotopes.

Geographic entities mentioned:
surface_form: Cardinal Lake
instance_of: Lake
countries: Canada
coordinates: lat: 56.2356
lon: -117.726
Kitten Mountain. Kitten Mountain (also &quot;Mao'er Mountains&quot;;) is a mountain located on the border between Ziyuan County and Xing'an County, Guangxi Zhuang Autonomous Region (GZAR) in the People's Republic of China that lies about from the prefecture-level city of Guilin. Description.

Geographic entities mentioned:
surface_form: kitten
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 25.8664
lon: 110.4127
World War II plane crash. On August 31, 1944, a Consolidated B-24 Liberator aircraft of the United States Army Air Corps crashed on Kitten Mountain following a bombing raid on Japanese warships off the coast of Taiwan. The ten man crew were listed as missing in action for 52 years until the remains of the aircraft were discovered in 1996 by two local youths searching for

Geographic entities mentioned:
surface_form: kitten
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 25.8664
lon: 110.4127
It is believed to be the principle bridge vector of WNV between birds and humans in southern France and is thought to have played a role in WNV transmission in the Danube delta, Caspian and Azov sea deltas, and the Volga region in Russia. It has also been implicated in Tahyna virus and Lednice virus transmission in France and Slovakia, respectively. Distribution. &quot;Cx.

Geographic entities mentioned:
surface_form: Caspian
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Zograf Monastery. The Saint George the Zograf Monastery or Zograf Monastery (, &quot;Moní Zográphou&quot;;) is one of the twenty Eastern Orthodox monasteries in Mount Athos (the &quot;Holy Mountain&quot;) in Greece.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Two medieval Bulgarian royal charters, the Zograf Charter and the Rila Charter, were discovered in the monastery's library. Honours. Zograf Peak on Livingston Island in the South Shetland Islands, Antarctica is named after the Zograf Monastery. The monastery and its seal are depicted on the obverse of the Bulgarian 2 levs banknote, issued in 1999 and 2005.

Geographic entities mentioned:
surface_form: Zograf Peak
instance_of: Mountain
coordinates: lat: -62.6518
lon: -60.1483
The animal is found in several regions of California, including the Central Coast, Sacramento Valley, San Joaquin Valley, and southern Sierra Nevada foothills. The southeastern Sacramento Valley contains about 15% of the remaining vernal pool grassland habitat in the state, and it has about 35% of the known occurrences of &quot;L. packardi&quot;.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
His oldest son, Jubran, was physically attacked in December 2013 for supporting his father's activities. Naddaf has received the support of Israeli Prime Minister Benjamin Netanyahu, the Israeli Ministry of Defense, members of the Knesset, and other officials. In 2016, Naddaf was selected to light a torch at the Israel Independence Day ceremony on Mount Herzl. Biography.

Geographic entities mentioned:
surface_form: Mount Herzl
instance_of: Mountain
countries: Israel
coordinates: lat: 31.774117
lon: 35.180567
Topography. The fell is part of the long ridge that radiates easterly from Eel Crag and includes the adjoining fells of Sail and Causey Pike before dropping to the Newlands Valley. Scar Crags is characterised by steep craggy flanks on its southern side which fall away steeply to Rigg Beck, while the northern slopes are less steep and grassy as they drop to Stoneycroft Gill. Geology.

Geographic entities mentioned:
surface_form: Eel Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.572
lon: -3.25
surface_form: Causey Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.576338888889
lon: -3.2112694444444
surface_form: Newlands Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.573011111111
lon: -3.1848694444444
surface_form: sail
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.571
lon: -3.242
Scar Crags is more usually approached from the east along the ridge from Causey Pike or from the west from Sail. It is a busy fell as it is part of the Coledale Round, a walk starting and finishing at Braithwaite or Stair in the Newlands valley and including the other nearby fells of Grisedale Pike, Hopegill Head, Eel Crag, Sail, and Causey Pike with over of ascent. Summit.

Geographic entities mentioned:
surface_form: Grisedale Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.592
lon: -3.241
surface_form: Hopegill Head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5875
lon: -3.2626694444444
surface_form: Causey Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.576338888889
lon: -3.2112694444444
surface_form: newlands valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.573011111111
lon: -3.1848694444444
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
surface_form: sail
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.571
lon: -3.242
surface_form: coledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.65
lon: -3.23333
Mining. The northern slopes of Scar Crags, below Long Crag, contain the remains of the Lake District’s only cobalt mine. It was opened by the Keswick Mining Company in 1846, who invested £7,000 in the project. A road and an inclined tramway were built to convey the ore down to Stoneycroft in the Newlands valley. Four adits were driven into the hillside, the longest being about in length.

Geographic entities mentioned:
surface_form: newlands valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.573011111111
lon: -3.1848694444444
Ascents. Scar Crags is very rarely climbed directly. The only feasible direct ascent follows an old mine road that starts from Stair and goes up Stoneycroft Gill to finish at Sail Pass, from where it is a short ascent to the fell summit. Scar Crags is more usually approached from the east along the ridge from Causey Pike or from the west from Sail.

Geographic entities mentioned:
surface_form: sail
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.571
lon: -3.242
Ascents. Scar Crags is very rarely climbed directly. The only feasible direct ascent follows an old mine road that starts from Stair and goes up Stoneycroft Gill to finish at Sail Pass, from where it is a short ascent to the fell summit. Scar Crags is more usually approached from the east along the ridge from Causey Pike or from the west from Sail.

Geographic entities mentioned:
surface_form: sail
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.571
lon: -3.242
surface_form: scar crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.574388888889
lon: -3.2266805555556
surface_form: causey pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.576338888889
lon: -3.2112694444444
Scar Crags. Scar Crags is a fell in the north western part of the English Lake District in the county of Cumbria. It is one of the Coledale group of fells situated south west of Keswick and reaches a height of. Topography. The fell is part of the long ridge that radiates easterly from Eel Crag and includes the adjoining fells of Sail and Causey Pike before dropping to the Newlands Valley.

Geographic entities mentioned:
surface_form: scar crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.574388888889
lon: -3.2266805555556
Topography. The fell is part of the long ridge that radiates easterly from Eel Crag and includes the adjoining fells of Sail and Causey Pike before dropping to the Newlands Valley. Scar Crags is characterised by steep craggy flanks on its southern side which fall away steeply to Rigg Beck, while the northern slopes are less steep and grassy as they drop to Stoneycroft Gill. Geology.

Geographic entities mentioned:
surface_form: scar crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.574388888889
lon: -3.2266805555556
Geology. The ridgeline is composed of the laminated mudstone and siltstone of the Kirkstile Formation. Ascents. Scar Crags is very rarely climbed directly. The only feasible direct ascent follows an old mine road that starts from Stair and goes up Stoneycroft Gill to finish at Sail Pass, from where it is a short ascent to the fell summit.

Geographic entities mentioned:
surface_form: scar crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.574388888889
lon: -3.2266805555556
Summit. The top of the fell is grassy and often muddy with a small cairn and gives a heady view down onto Rigg Beck and a good but not exceptional all round view of the district. Mining. The northern slopes of Scar Crags, below Long Crag, contain the remains of the Lake District’s only cobalt mine. It was opened by the Keswick Mining Company in 1846, who invested £7,000 in the project.

Geographic entities mentioned:
surface_form: scar crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.574388888889
lon: -3.2266805555556
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Scar Crags. Scar Crags is a fell in the north western part of the English Lake District in the county of Cumbria. It is one of the Coledale group of fells situated south west of Keswick and reaches a height of. Topography. The fell is part of the long ridge that radiates easterly from Eel Crag and includes the adjoining fells of Sail and Causey Pike before dropping to the Newlands Valley.

Geographic entities mentioned:
surface_form: coledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.65
lon: -3.23333
He had then buried her body in a shallow grave within a clearing near Raquette Lake, at a location in or near the town of Inlet, without ensuring she was dead as opposed to simply unconscious before he had buried her, adding he could still see his van from the location where he buried Sara. He agreed to draw a map of the location of her burial to assist investigators in the recovery of her body.

Geographic entities mentioned:
surface_form: Raquette Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.833333333333
lon: -74.65
Foul play is suspected in her case, with Arthur Mason Slaybaugh also named as a prime suspect. Aftermath. Following Sara's disappearance, her family founded the Sara Anne Wood Rescue Center; this center later amalgamated into the Mohawk Valley branch of the National Center for Missing & Exploited Children (NCMEC) and remains operational.

Geographic entities mentioned:
surface_form: Mohawk Valley
instance_of: Valley
countries: United States
By 1928, Long had gained such momentum, that he became one of the major talking points of his opponents; opposing political conventions chanted &quot;It won't be Long now.&quot;
Long was a fervent critic of a toll bridge being constructed across Lake Pontchartrain by incumbent Governor Oramel H. Simpson, instead promising a toll-free bridge.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
Fluchthorn (Pennine Alps). The Fluchthorn is a mountain of the Swiss Pennine Alps, located south of Saas-Almagell in the canton of Valais. It lies east of the Strahlhorn.

Geographic entities mentioned:
surface_form: Strahlhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.013222222222
lon: 7.90175
Fluchthorn (Pennine Alps). The Fluchthorn is a mountain of the Swiss Pennine Alps, located south of Saas-Almagell in the canton of Valais. It lies east of the Strahlhorn.

Geographic entities mentioned:
surface_form: fluchthorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.02166667
lon: 7.91444444
Life. He attended schools in Maidstone and Herstmonceux. In 1830, he emigrated to the United States, and became a clerk in a tannery near Oneida Lake. In 1837, he married Mary Cramp (1812–1883), and they had nine children. The couple removed to Ottawa, Illinois, and engaged in farming.

Geographic entities mentioned:
surface_form: Oneida Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.2
lon: -75.9
Chicago Railroad Fair. The Chicago Railroad Fair was an event organized to celebrate and commemorate 100 years of railroad history west of Chicago, Illinois. It was held in Chicago in 1948 and 1949 along the shore of Lake Michigan and is often referred to as &quot;the last great railroad fair&quot; with 39 railroad companies participating.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Audnedalen. Audnedalen is the shortest of the six main north-south valleys in Agder county, Norway. The long river valley runs through the municipalities of Lyngdal and Lindesnes. The river Audna runs through the valley, ending in Snigsfjorden in the south. The valley floor is flat and the sides are relatively steep.

Geographic entities mentioned:
surface_form: audnedalen
instance_of: Valley
countries: Norway
coordinates: lat: 58.19867
lon: 7.33302
Route description. Highway 13 runs the width of the province from the Alberta border east to the Manitoba border. It traverses the Missouri Coteau and the Laurentian continental divide in a semi-arid region known as Palliser's Triangle. The terrain of the Missouri Coteau features low hummocky, undulating, rolling hills, potholes, and grasslands.

Geographic entities mentioned:
surface_form: Missouri Coteau
instance_of: Plateau
countries: Canada
United States
coordinates: lat: 50.8
lon: -109.2
surface_form: Laurentian continental divide
instance_of: Landform
countries: United States
Canada
South on 47 is Estevan and the U.S. border while north is Highway 1. Continuing east, 13 provides access to Forget, Kisbey, Arcola, and Carlyle and crosses Moose Mountain Creek. Through Carlyle, 13 shares a short long concurrency with the north–south Highway 9. North-bound on 9 travels through Moose Mountain Provincial Park en route to Whitewood and Highway 1 while south-bound heads to the U.S.

Geographic entities mentioned:
surface_form: Moose Mountain Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.21675
lon: -102.20089
At the time of carving the Klácelka, Levý was an untutored young man. He chiseled from sandstone rock a cave that is an allegorical Blaník - a hall of sleeping heroes. These include the leader of the soldiers of the mythological army Zdeněk Zásmucký, the Hussite leaders Jan Žižka and Prokop Holý, the sleeping Blaník army, and the dwarf figures wielding weapons for them.

Geographic entities mentioned:
surface_form: Blaník
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 49.642222222222
lon: 14.872777777778
1952 Mount Gannett C-124 crash. The 1952 Mount Gannett C-124 crash was an accident in which a Douglas C-124 Globemaster II military transport aircraft of the United States Air Force crashed into Mount Gannett, a peak in the Chugach Mountains in the American state of Alaska, on November 22, 1952. All of the 52 men on board were killed.

Geographic entities mentioned:
surface_form: Mount Gannett
instance_of: Mountain
countries: United States
coordinates: lat: 61.2422
lon: -148.193
Putaqa (Junín). Putaqa (Quechua for &quot;Rumex peruanus&quot;, also spelled &quot;Putaca&quot;) is a mountain in Peru which reaches a height of approximately. It is located in the Junín Region, Yauli Province, Marcapomacocha District. A small lake named Aququcha (Quechua for &quot;sand lake&quot;) lies at its feet.

Geographic entities mentioned:
surface_form: putaqa
instance_of: Mountain
countries: Peru
coordinates: lat: -10.72638889
lon: -75.74583333
surface_form: junín
instance_of: Lake
countries: Peru
coordinates: lat: -11.0201
lon: -76.1075
surface_form: putaqa
instance_of: Mountain
countries: Peru
coordinates: lat: -10.46305556
lon: -75.98111111
surface_form: putaqa
instance_of: Mountain
countries: Peru
coordinates: lat: -11.44666667
lon: -76.27861111
surface_form: putaqa
instance_of: Mountain
countries: Peru
coordinates: lat: -9.0775
lon: -77.93888889
Putaqa (Junín). Putaqa (Quechua for &quot;Rumex peruanus&quot;, also spelled &quot;Putaca&quot;) is a mountain in Peru which reaches a height of approximately. It is located in the Junín Region, Yauli Province, Marcapomacocha District. A small lake named Aququcha (Quechua for &quot;sand lake&quot;) lies at its feet.

Geographic entities mentioned:
surface_form: putaqa
instance_of: Mountain
countries: Peru
coordinates: lat: -10.72638889
lon: -75.74583333
surface_form: putaqa
instance_of: Mountain
countries: Peru
coordinates: lat: -10.46305556
lon: -75.98111111
surface_form: putaqa
instance_of: Mountain
countries: Peru
coordinates: lat: -11.44666667
lon: -76.27861111
surface_form: putaqa
instance_of: Mountain
countries: Peru
coordinates: lat: -9.0775
lon: -77.93888889
Putaqa (Junín). Putaqa (Quechua for &quot;Rumex peruanus&quot;, also spelled &quot;Putaca&quot;) is a mountain in Peru which reaches a height of approximately. It is located in the Junín Region, Yauli Province, Marcapomacocha District. A small lake named Aququcha (Quechua for &quot;sand lake&quot;) lies at its feet.

Geographic entities mentioned:
surface_form: junín
instance_of: Lake
countries: Peru
coordinates: lat: -11.0201
lon: -76.1075
surface_form: marcapomacocha
instance_of: Lake
countries: Peru
coordinates: lat: -11.40205
lon: -76.3465
surface_form: yauli
instance_of: Mountain
countries: Peru
coordinates: lat: -11.4992
lon: -76.1297
Features. The district comprises the floodplain of the Ruamahanga River and the associated Lake Wairarapa, as well as the long southern stretch of Palliser Bay. To the west of the plains rise the eastern slopes of the Remutaka Range, the crest of which forms the western boundary of the district, while the Aorangi Range lies to the south-east.

Geographic entities mentioned:
surface_form: Lake Wairarapa
instance_of: Lake
countries: New Zealand
coordinates: lat: -41.216666666667
lon: 175.25
From the date plantations and salt basins of the Kaouar, huge caravans transported good south to Zinder and Kano. 20th century.

Geographic entities mentioned:
surface_form: Kaouar
instance_of: Valley
countries: Niger
coordinates: lat: 18.9
lon: 12.9
From 2014 to 2015, she, alongside Katie Couric, hosted Yahoo! Music/Live Nation's original interview series &quot;Backstage with Citi,&quot; which won a Bronze Cio Award in 2015. She has also acted in the Roger Corman films &quot;The Haunting of Morella&quot; and &quot;The Watchers 2.&quot;
Parker grew up in the San Fernando Valley and attended the University of California, Los Angeles.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Geography. Landu Leko is located in the northeast of the island Roti. To the south lies the district Rote Timur. The district contains the Tapuafu peninsula, the eastern islands of Usu, Nusa Manupui and Boti, and the northern island Nusa Bibi, which lies in the Strait of Roti. The capital is Daeurendale, in the south of Tapuafu. On Tapuafu are two inland lakes, including Lake Undun.

Geographic entities mentioned:
surface_form: Lake Undun
instance_of: Lake
countries: Indonesia
coordinates: lat: -10.515833333333
lon: 123.36722222222
The area is very remote and the most southern herd of woodland caribou can be found here. Further to the north is Atikaki Provincial Wilderness Park with no roads. Almost the entire east side of Lake Winnipeg is wilderness, with a few First Nation communities and very few small towns. Both Booster Lake and Springer Lake are located in Nopiming Provincial Park. Beresford Lake.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Further to the north is Atikaki Provincial Wilderness Park with no roads. Almost the entire east side of Lake Winnipeg is wilderness, with a few First Nation communities and very few small towns. Both Booster Lake and Springer Lake are located in Nopiming Provincial Park. Beresford Lake. Beresford Lake () is in the park.

Geographic entities mentioned:
surface_form: Booster Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.44524
lon: -95.26746
surface_form: Springer Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.5336
lon: -95.4556
Manuel Afonso de Carvalho, bishop of Angra. The parish was elevated to the status of civil parish two years later, in 1960, when it was de-annexed from the territory of Bretanha. Geography. It is located in the northwestern part of the island of São Miguel, and includes the flanks of the Sete Cidades Massif, covered in &quot;laurisilva&quot; and endemic plant species to the coastal cliffs.

Geographic entities mentioned:
surface_form: Sete Cidades Massif
instance_of: Mountain
countries: Portugal
coordinates: lat: 37.855194444444
lon: -25.786166666667
The route travels north into Anahuac before turning to the east. It passes the Chambers County Airport before an intersection with SH 65; SH 61 turns to the north, while SH 65 continues east. SH 61 crosses I-10 near the community of Turtle Bayou, northeast of Lake Anahuac. The route travels north into Liberty County before reaching its northern terminus in Devers at US 90. History.

Geographic entities mentioned:
surface_form: Lake Anahuac
instance_of: Lake
countries: United States
coordinates: lat: 29.8003
lon: -94.6836
List of beaches in Bangladesh. Bangladesh, with a sea border extending about 1320 kms, including all the islands and the estuary facing the Bay of Bengal, claims to have the world's longest sea beach at Cox's Bazar, measuring at 120 km (75 miles) of unbroken sea beach, with a view of sunrise and sunset and a unique coral sea beach. Below is a list of sea beaches located in Bangladesh.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Juval Castle. Juval Castle (German: &quot;Schloss Juval&quot;;) is a medieval castle located at the entrance of the Schnalstal, in the Vinschgau, above the village of Naturns in the comune of Kastelbell-Tschars at around 1000 meters above sea level, in South Tyrol, northern Italy. It derives its name from the Latin name of the mountain, &quot;Mons Jovis&quot; (mountain of Jupiter).

Geographic entities mentioned:
surface_form: Schnalstal
instance_of: Valley
countries: Italy
coordinates: lat: 46.722222222222
lon: 10.860833333333
surface_form: Vinschgau
instance_of: Valley
countries: Italy
coordinates: lat: 46.615
lon: 10.705
After Eline began restrengthening and turned more to the southwest, officials on Réunion declared a red alert, but this was dropped when the cyclone passed the island. Ultimately, the storm brushed the island with gusts of along the coast, and in the mountainous peak of Maïdo. Rainfall was heaviest in the mountainous peaks, reaching at Bébourg. Significant wave heights remained below. Madagascar.

Geographic entities mentioned:
surface_form: Maïdo
instance_of: Mountain
countries: France
coordinates: lat: -21.068889
lon: 55.387778
Geography and geomorphology. The Vilama caldera lies on the border between Argentina and Bolivia in the Puna-Altiplano, a high plateau in the Central Andes. The volcano straddles the border between Bolivia and Argentina, northeast of Cerro Zapaleri which is the tripoint between Argentina, Bolivia and Chile there.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
The Central Volcanic Zone is home to more than a thousand volcanoes, of which 44 were active after glacial times. Many of these are part of the main volcanic arc, which consists of stratovolcanoes such as Coropuna, the Nevados de Payachata, Ojos del Salado and Ollagüe and frequently reach heights of above.

Geographic entities mentioned:
surface_form: Ojos del Salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
surface_form: Ollagüe
instance_of: Mountain
countries: Bolivia
Chile
coordinates: lat: -21.3
lon: -68.166666666667
The Central Volcanic Zone is also the site of a number of large calderas, such as Los Frailes, Kari-Kari, Pastos Grandes, Cerro Panizos, Cerro Guacha, Purico complex, Coranzulí, La Pacana, Aguas Calientes, Negra Muerta volcanic complex, Galán, Wheelwright caldera and Incapillo. The Vilama caldera is between and wide.

Geographic entities mentioned:
surface_form: Cerro Panizos
instance_of: Mountain
countries: Bolivia
coordinates: lat: -22.4375
lon: -66.7825
surface_form: Cerro Guacha
instance_of: Mountain
countries: Bolivia
coordinates: lat: -22.75
lon: -67.46666667
surface_form: Purico complex
instance_of: Mountain
countries: Chile
coordinates: lat: -23
lon: -67.75
surface_form: La Pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: Galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
These centres mainly erupted dacitic magmas. Among the Altiplano-Puna volcanic complex volcanoes are the Cerro Panizos northeast of Vilama and the Cerro Guacha southwest of Vilama; the Vilama, Coruto and Guacha calderas have been designed the &quot;Eduardo Avaroa caldera complex&quot; ().

Geographic entities mentioned:
surface_form: Cerro Panizos
instance_of: Mountain
countries: Bolivia
coordinates: lat: -22.4375
lon: -66.7825
surface_form: Cerro Guacha
instance_of: Mountain
countries: Bolivia
coordinates: lat: -22.75
lon: -67.46666667
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
Between 8-4 million years ago large scale eruptions occurred, such as these at Cerro Panizos, Coranzulí, Vilama, Cerro Guacha and La Pacana. Volcanic activity decreased by the Pleistocene, during which activity occurred within the La Pacana caldera and at Cerro Purico, with the most recent eruptions formed the Cerro Chao dome and the Cerro Chascon-Runtu Jarita complex.

Geographic entities mentioned:
surface_form: La Pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
Between 8-4 million years ago large scale eruptions occurred, such as these at Cerro Panizos, Coranzulí, Vilama, Cerro Guacha and La Pacana. Volcanic activity decreased by the Pleistocene, during which activity occurred within the La Pacana caldera and at Cerro Purico, with the most recent eruptions formed the Cerro Chao dome and the Cerro Chascon-Runtu Jarita complex.

Geographic entities mentioned:
surface_form: Cerro Purico
instance_of: Mountain
countries: Chile
coordinates: lat: -23
lon: -67.75
This theory also envisaged two later stages of activity, the first linked to the Cerro Morado mafic volcanics and the Salle and Ceja Grande ignimbrites, while the fourth produced the Bonanza ignimbrite from the Coruto caldera as well as additional volcanoes including Cerro Zapaleri.

Geographic entities mentioned:
surface_form: Cerro Morado
instance_of: Mountain
countries: Argentina
coordinates: lat: -37.0567
lon: -68.7525
Among the products of this volcanism are the 58.1 ± 0.6 million year old northerly Khastor domes and stratovolcano, the 68.4 ± 0.6 million year old eastern centres (Cerro Alcoak, Cerro Salle, Bayo dome and the Vilama and Toloma lavas) and the less than 8.4 million years old Mesada Negra lavas on the resurgent dome. The Vitichi domes are of Pliocene age.

Geographic entities mentioned:
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
Vilama (caldera). Vilama is a Miocene caldera in Bolivia and Argentina. Straddling the border between the two countries, it is part of the Central Volcanic Zone, one of the four volcanic belts in the Andes.

Geographic entities mentioned:
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
Straddling the border between the two countries, it is part of the Central Volcanic Zone, one of the four volcanic belts in the Andes. Vilama is remote and forms part of the Altiplano-Puna volcanic complex, a province of large calderas and associated ignimbrites that were active since about 8 million years ago, sometimes in the form of supervolcanoes.

Geographic entities mentioned:
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
The Vilama caldera was originally estimated to have a size of but the size was later revised to be between and and is almost entirely buried beneath younger volcanoes that have grown along the margin of the caldera; volcanic activity on these volcanoes continued into the Pleistocene. Several lakes also developed on the floor of the caldera, which contains a resurgent dome.

Geographic entities mentioned:
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
Several lakes also developed on the floor of the caldera, which contains a resurgent dome. Vilama is the source of the enormous Vilama ignimbrite, which was emplaced during an eruption with a volcanic explosivity index of 8 about 8.4–8.5 million years ago.

Geographic entities mentioned:
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
Vilama is the source of the enormous Vilama ignimbrite, which was emplaced during an eruption with a volcanic explosivity index of 8 about 8.4–8.5 million years ago. A large amount of the Vilama ignimbrite is inside the caldera depression, while the part outside of the caldera covers a surface area exceeding. The total volume of the ignimbrite is about, possibly as much as.

Geographic entities mentioned:
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
A large amount of the Vilama ignimbrite is inside the caldera depression, while the part outside of the caldera covers a surface area exceeding. The total volume of the ignimbrite is about, possibly as much as. Another large ignimbrite, the Sifon ignimbrite, may also have been erupted by Vilama, while the Granada ignimbrite was later attributed to a separate volcano. Geography and geomorphology.

Geographic entities mentioned:
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
The volcano straddles the border between Bolivia and Argentina, northeast of Cerro Zapaleri which is the tripoint between Argentina, Bolivia and Chile there. The region is largely uninhabited owing to its harsh climate, however several archeological sites have been found and obsidian from Vilama has been found throughout northwestern Argentina.

Geographic entities mentioned:
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
The region is largely uninhabited owing to its harsh climate, however several archeological sites have been found and obsidian from Vilama has been found throughout northwestern Argentina. Vilama is part of the Central Volcanic Zone, which together with the Northern Volcanic Zone, Southern Volcanic Zone and Austral Volcanic Zone is one of the four volcanic belts along the Andes.

Geographic entities mentioned:
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
The Central Volcanic Zone is also the site of a number of large calderas, such as Los Frailes, Kari-Kari, Pastos Grandes, Cerro Panizos, Cerro Guacha, Purico complex, Coranzulí, La Pacana, Aguas Calientes, Negra Muerta volcanic complex, Galán, Wheelwright caldera and Incapillo. The Vilama caldera is between and wide.

Geographic entities mentioned:
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
Several younger volcanic centres are found around the caldera and may be located above its margin, such as the Khastor domes and stratovolcano, the and volcanoes, the Cerros Conventos-Niño-Coyamboy chain, Vitichi and Cerro Bayo domes and the high Vilama stratovolcano. These edifices are mostly dacitic centres that are considered to be the expression of post-collapse volcanism at the Vilama system.

Geographic entities mentioned:
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
These edifices are mostly dacitic centres that are considered to be the expression of post-collapse volcanism at the Vilama system. The caldera was at first considered to be in width with a centre around, coinciding with the Vilama depression.

Geographic entities mentioned:
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
Vents were localized on the eastern margin beneath the Cerro Caucani, Cerro Solterío, Campanario and Coyaguayma volcanoes, which in turn make up the Abra Granada volcanic complex. One nested caldera associated with the Bonanza ignimbrite was identified as well, the Coruto caldera which is situated southwest of the redefined extent of the Vilama caldera. Geology.

Geographic entities mentioned:
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
The pre-caldera terrain at Vilama is formed by various sedimentary and volcanic formations, such as the Paleozoic Acoite Formation and the Cretaceous Salta Group; Ordovician sediments are the most important component of the basement while later units only sporadically crop out.

Geographic entities mentioned:
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
Volcanic units of Oligocene-Miocene age predating the formation of the Vilama caldera include the 9.79.8 million years old Granada ignimbrite, the 10.25 ± 0.12 million years old Lagunillas ignimbrite, the 9.8 ± 0.7 million years old Ojo de Perico lavas and other volcanic units.

Geographic entities mentioned:
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
Later volcanic activity from other volcanoes in the region led to the emplacement of extraneous volcanic rocks in the Vilama caldera, such as the Bonanza, Cienago and Panizos ignimbrites and the Loromayu lavas. In terms of tectonics, during the Cenozoic the region was substantially uplifted, forming a high plateau with an average elevation of about. Composition.

Geographic entities mentioned:
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
It has been inferred that before the eruption the magma was hot. A mixing between mantle derived and crustal melts has been suggested to be the source of the magma for both Vilama and other Altiplano-Puna volcanic complex systems. Climate and vegetation. The region has a dry climate with irregular rainfall (), temperatures between and high diurnal temperature variations.

Geographic entities mentioned:
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
The Vilama ignimbrite also includes other ignimbrites that were formerly considered to be separate ignimbrites, such as the Capaderos ignimbrite, Ceja Grande ignimbrite, Tobas Coruto, Tobas Lagunillas 1, Tobas Lagunillas 2, Tobas Lagunillas 3, Tobas Loromayu 1, Tobas Lupi Gera and Toloma ignimbrite.

Geographic entities mentioned:
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
The inclusion of these volcanic products into the Vilama ignimbrite was based on the similarity between their characteristics and those of the actual Vilama ignimbrite, including paleomagnetic and petrologic traits, and together they establish an ignimbrite field elongated towards the south and northwest away from the caldera. The outcrops cover an area of.

Geographic entities mentioned:
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
Based on such sizes, the caldera-forming eruption is considered to be a supereruption with a volcanic explosivity index of 8 and Vilama caldera is thus a supervolcano. Fracchia &quot;et al.&quot; 2010 further proposed that the &quot;Pululus ignimbrite&quot; which forms the southeast of Vilama is actually a section of the Vilama ignimbrite, which was later uplifted by a dacitic intrusion.

Geographic entities mentioned:
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
Based on such sizes, the caldera-forming eruption is considered to be a supereruption with a volcanic explosivity index of 8 and Vilama caldera is thus a supervolcano. Fracchia &quot;et al.&quot; 2010 further proposed that the &quot;Pululus ignimbrite&quot; which forms the southeast of Vilama is actually a section of the Vilama ignimbrite, which was later uplifted by a dacitic intrusion.

Geographic entities mentioned:
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
Fracchia &quot;et al.&quot; 2010 further proposed that the &quot;Pululus ignimbrite&quot; which forms the southeast of Vilama is actually a section of the Vilama ignimbrite, which was later uplifted by a dacitic intrusion. Additionally, it has been proposed that the Sifon ignimbrite, which was erupted 8.33 ± 0.06 million years ago, may originate in the Vilama caldera.

Geographic entities mentioned:
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
Magnetotelluric imaging of the area has identified a low electrical conductivity anomaly beneath the caldera, which may be a solidified magma body. Originally, the Granada ignimbrite was also considered to be a product of an earlier eruption of the Vilama caldera; later research indicated that it has its own eruptive centre at Abra Granada that is unrelated to Vilama.

Geographic entities mentioned:
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
According to this older theory of caldera history, the Granada ignimbrite was the first stage of caldera formation, with the second stage generating the Vilama ignimbrite proper.

Geographic entities mentioned:
surface_form: vilama
instance_of: Mountain
countries: Argentina
Bolivia
coordinates: lat: -22.43
lon: -67
Balke was also a pupil of Johan Christian Dahl from 1843 to 1844. During the summer of 1830 he walked from Rjukan in the Vestfjorddalen valley, through Telemark county, Røldal Municipality, Kinsarvik Municipality all the way to the city of Bergen, and then back to Rjukan through Vossevangen to Gudvangen, further over Filefjell to Valdres and then across the mountains to Hallingdal.

Geographic entities mentioned:
surface_form: Vestfjorddalen
instance_of: Valley
countries: Norway
coordinates: lat: 59.89917
lon: 8.71973
surface_form: Valdres
instance_of: Valley
countries: Norway
coordinates: lat: 60.916666666667
lon: 9.1666666666667
surface_form: Hallingdal
instance_of: Valley
countries: Norway
coordinates: lat: 60.633333333333
lon: 9.05
Ravenna Bridge. The Ravenna Bridge is a high and long railway viaduct on the Höllental Railway line in the Black Forest, in Breitnau, Breisgau-Hochschwarzwald, Baden-Württemberg, Germany. The bridge crosses the Ravenna Gorge that ends in the upper Höllental valley, and has a grade of. The origin of the name most likely comes from the French &quot;ravin&quot; for gorge. History and construction.

Geographic entities mentioned:
surface_form: Ravenna Gorge
instance_of: Valley
countries: Germany
coordinates: lat: 47.91972222
lon: 8.085
Stack Bay. Stack Bay () is a small bay between West Stack and the mouth of Hoseason Glacier in Enderby Land. Mapped by Norwegian cartographers from air photos taken by the Lars Christensen Expedition (1936–37) and called &quot;Skotvika&quot; because of the proximity to West Stack, named by personnel of RRS William Scoresby in 1936.

Geographic entities mentioned:
surface_form: West Stack
instance_of: Mountain
coordinates: lat: -67.05
lon: 58.05
Gatherings of two or more people, except individuals in the same household, were banned, whilst pubs, restaurants (with exception for take-aways) and shops selling 'non-essential goods' were ordered to closed. On 26 March, Snowdon and other Welsh mountains were closed to the public, after a larger number of tourists had gathered on the mountains in the preceding days, causing traffic mayhem.

Geographic entities mentioned:
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889