Sarmila/GeoWiki-Features huggingface dataset:
This formation is notable for the discovery of the holotype of the basilosaurid whale &quot;Tutcetus wadii&quot;, the smallest basilosaurid whale ever found. This fossil was located in an indurated limestone block near the Upper Lake in the Wadi El-Rayan area, approximately 40 km northeast of the Wadi El-Hitan World Heritage Site, several meters above the Midawara Formation.

Geographic entities mentioned:
surface_form: Wadi El-Rayan
instance_of: Valley
countries: Egypt
coordinates: lat: 29.179444444444
lon: 30.440555555556
The St. Thomas Moraine is an east-west glacial moraine considered one of the Horseshoe Moraines. It formed at the time of Lake Maumee II filled part of the basin of what is now Lake Erie. Other portions of the basin were filled by a lobe of the Laurentian icesheet, known as the Erie Lobe. The moraine is approximately long, and wide, running parallel to the shore of Lake Erie, about inshore.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
After he arrived in Naples, the 340th Bombardment Group moved to San Petrazio, where Slayton flew combat missions into the Balkan Peninsula. After six weeks, he moved to Foggia, where 48 aircraft were destroyed after an eruption of Mount Vesuvius. Afterwards, Slayton flew out of Salerno and Corsica, where he upgraded from copilot to pilot.

Geographic entities mentioned:
surface_form: Mount Vesuvius
instance_of: Mountain
countries: Italy
coordinates: lat: 40.821388888889
lon: 14.425555555556
The river flows entirely within the Civil Parish of Tullaghobegly (Irish: &quot;Tulacha Beigile&quot;). Course. The Clady River flows out of the western end of Lower Lough Nacung (Irish: &quot;Loch na Cuinge Íochtarach&quot;) in Gweedore. Lower Lough Nacung is immediately north-west of Upper Lough Nacung (Irish: &quot;Loch na Cuinge Uachtarach&quot;).

Geographic entities mentioned:
surface_form: Upper Lough Nacung
instance_of: Lake
countries: Ireland
coordinates: lat: 55.031956
lon: -8.166305
Couch's kingbird. Couch's kingbird (&quot;Tyrannus couchii&quot;) is a passerine tyrant flycatcher of the kingbird genus. It is found from southern Texas along the Gulf Coast to the Yucatán Peninsula in Mexico, Belize and northern Guatemala. It is also found in the lower stretches of the Rio Grande Valley. The species is named after soldier and naturalist Darius N. Couch. Description.

Geographic entities mentioned:
surface_form: Rio Grande Valley
instance_of: Valley
countries: United States
Mexico
coordinates: lat: 26.22
lon: -98.12
Now, Leitner-Poma has created an improved Omega carrier, along with the new LPA grip, and a new version of the Omega terminal. Leitner-Poma has good relationships with Breckenridge Ski Resort, Vail Ski Resort, Winter Park Resort, Snowmass, Aspen Mountain, Buttermilk, Aspen Highlands, Okemo, Mount Snow, Sugarbush Resort and many other ski resorts. Doppelmayr.

Geographic entities mentioned:
surface_form: Mount Snow
instance_of: Mountain
countries: United States
coordinates: lat: 42.95897
lon: -72.92371
Although Lewis Tappan was active within the business community of Colorado City and El Paso County, Tappan still found time to explore the surrounding area. In 1859, Tappan, Anthony Bott, George Bute, Melancthon S. Beach, A.D. Richardson, several people from Golden City, and several women hiked to the summit of Pikes Peak, taking several days.

Geographic entities mentioned:
surface_form: Pikes Peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.840555555556
lon: -105.04416666667
The earthquake triggered an avalanche on Mount Everest, killing 22 people, the deadliest incident on the mountain on record. The earthquake triggered another huge avalanche in the Langtang valley, where 250 people were reported missing. Hundreds of thousands of Nepalese were made homeless with entire villages flattened across many districts of the country.

Geographic entities mentioned:
surface_form: Langtang
instance_of: Valley
countries: Nepal
coordinates: lat: 28.25
lon: 85.5
Hundreds of thousands of Nepalese were made homeless with entire villages flattened across many districts of the country. Centuries-old buildings were destroyed at UNESCO World Heritage Sites in the Kathmandu Valley, including some at the Kathmandu Durbar Square, the Patan Durbar Square, the Bhaktapur Durbar Square, the Changu Narayan Temple, the Boudhanath stupa, and the Swayambhunath stupa.

Geographic entities mentioned:
surface_form: Kathmandu Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
12 May 2015 earthquake. A second major earthquake occurred on 12 May 2015 at 12:50 NST with a moment magnitude (Mw) of 7.3Mw 18 km (11 mi) southeast of Kodari. The epicenter was near the Chinese border between the capital city of Kathmandu and Mount Everest. It struck at a depth of 18.5 km (11.5 miles).

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
In Tangail, a woman died trying to escape a building. Another woman was crushed to death by a collapsed wall while a teacher died of a heart attack during the earthquake. Avalanches on Mount Everest. This earthquake caused avalanches on Mount Everest. At least 19 died, with at least 120 others injured or missing. Landslides in the Langtang Valley.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
This earthquake caused avalanches on Mount Everest. At least 19 died, with at least 120 others injured or missing. Landslides in the Langtang Valley. In the Langtang valley located in Langtang National Park, 329 people were reported missing after an avalanche hit the village of Ghodatabela and the village of Langtang. The avalanche was estimated to have been two to three kilometres wide.

Geographic entities mentioned:
surface_form: Langtang valley
instance_of: Valley
countries: Nepal
coordinates: lat: 28.25
lon: 85.5
Operating areas. MWTC is located in Pickel Meadows of the Sierra Nevada mountains south of Lake Tahoe on of mountainous terrain with elevations from  –  . Other areas utilized by MWTC: Sweetwater Airstrip, Mount Shasta, the eastern slopes of the Sierra Nevada (U.S.) and Hawthorne Army Depot for live fire exercises. Formal courses and training programs offered.

Geographic entities mentioned:
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
Amicus Mountain. Amicus Mountain is a glaciated summit in British Columbia, Canada. Description. Amicus Mountain is located in the Coast Mountains, west-southwest of Whistler and west-northwest of Icecap Peak, which is the nearest neighbor. Precipitation runoff and glacial meltwater from this mountain drain into tributaries of the Squamish River.

Geographic entities mentioned:
surface_form: Icecap Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.03297
lon: -123.43605
The districts of Mysore, Chamarajanagar, Mandya, Hassan and Chikmagalur are part of Old Mysore region, districts of Dakshina Kannada and Udupi are part of Tulu language speaking Coastal Karnataka region and Kodagu district was part of the erstwhile Part-C state of Coorg. Part of the region falls under the Malnad area of Karnataka while the other part falls under the Kaveri river basin. Economy.

Geographic entities mentioned:
surface_form: Kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
Borders. St. Gallenkirch - Ill river as far as Partenen - Zeinisjoch - Zeinisbach - Paznauntal as far as Ischgl - Fimbertal - Fimber Pass - Val Chöglias - Val Sinestra - Inn River from the mouth of the Branclabach to the mouth of the Susasca - Val Susasca - Flüela Pass - Davos - Wolfgang - Laretbach - Klosters - Schlappinbach - Schlappiner Joch - Valzifensbach - Gargellental - St. Gallenkirch.

Geographic entities mentioned:
surface_form: Paznaun
instance_of: Valley
countries: Austria
coordinates: lat: 47.05
lon: 10.333333333333
surface_form: Val Sinestra
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.850724
lon: 10.336659
It can relatively easily be ascended from north or south through glaciers and stretches of easy climbing. The Silvretta is famous for its skiing especially its many backcountry skiing possibilities. In the 1920s Ernest Hemingway was staying in the region for a winter (he lived at Schruns in Montafon, Austria). Later, he wrote a couple of short stories about his skiing experiences in the Silvretta.

Geographic entities mentioned:
surface_form: Montafon
instance_of: Valley
countries: Austria
coordinates: lat: 47.08
lon: 9.9
Torvikbukt. Torvikbukt is a village in Gjemnes Municipality in Møre og Romsdal county, Norway. The village is located at the junction of the Batnfjorden and Tingvollfjorden and just northwest of the tall mountain Reinsfjellet. The village of Øre lies about to the southwest and the village of Heggem lies about to the south. The village has a population (2024) of 269 and a population density of.

Geographic entities mentioned:
surface_form: Reinsfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 62.929722222222
lon: 7.9263888888889
Tourism. Torvikbukt's typical Norwegian surroundings of fjords and mountains make it an excellent starting point for mountain hiking, fishing, and boat-safari. This attracts both domestic and foreign tourists, which has led to the development of many vacation homes near fjord.Reinsfjellet is a mountain with a very good view and is frequently hiked by tourists. Education.

Geographic entities mentioned:
surface_form: Reinsfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 62.929722222222
lon: 7.9263888888889
Wetland protection. Via the Wistron Foundation and in cooperation with the Society of Wilderness NGO, Wistron contributes to conservation, revitalization and education for Shuanglianpi Wetland in Yilan County, Taiwan. The wetland is considered a &quot;paradise&quot; for aquatic plant life and holds several nationally threatened species of flora.

Geographic entities mentioned:
surface_form: Shuanglianpi Wetland
instance_of: Lake
countries: Taiwan
coordinates: lat: 24.749166666666667
lon: 121.63805555555555
In addition to his legal practice and civic duties, Rawlins Lowndes acquired plantations through marriage, which he farmed using enslaved labor. He acquired his first plantation along the Stono River in St. Paul Parish in 1748 (which qualified him for a seat in the lower house of the South Carolina Assembly), although that wife died in childbirth in 1750.

Geographic entities mentioned:
surface_form: Stono River
instance_of: Landform
countries: United States
coordinates: lat: 32.6368
lon: -80.0151
The lake is part of a chain of wetlands situated along major ancient drainage lines in the area that run from Dumbleyung in the north to south of Wagin. The Shire of Wagin contains many large lakes and wetlands, including western parts of Lake Dumbleyung, Lake Parkeyerring, Lake Little Parkeyerring, Lake Quarbing, Lake Norring, Lake Little Norring, Lake Gundaring and Wagin Lake.

Geographic entities mentioned:
surface_form: Wagin Lake
instance_of: Lake
countries: Australia
coordinates: lat: -33.326389
lon: 117.347222
Parkeyerring Lake. Parkeyerring Lake is an ephemeral salt lake in the Wheatbelt region of Western Australia, approximately south of the town of Wagin and about southeast of Perth. Much of the lake is surrounded by the Parkeyerring Nature Reserve, which was gazetted in 1905 and expanded in 1957.

Geographic entities mentioned:
surface_form: parkeyerring lake
instance_of: Lake
countries: Australia
coordinates: lat: -33.36989
lon: 117.3454
Coke County, Texas. Coke County is a county located on the Edwards Plateau in the U.S. state of Texas. As of the 2020 census, its population was 3,285. Its county seat is Robert Lee. The county was founded in 1889 and is named for Richard Coke, the 15th governor of Texas and later a U.S. senator.

Geographic entities mentioned:
surface_form: Edwards Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 30.3
lon: -99.6
He authored and published two books, &quot;Nature's Way&quot; and &quot;Wildlife Falsehoods&quot;. Blackwater Draw Museum. The original Blackwater Draw Museum opened in 1969 to display artifacts uncovered at the Blackwater Locality No. 1 site and illustrate life at the Blackwater Draw site during the Clovis period (over 13,000 years ago) through the recent historic period. Miles Mineral Museum.

Geographic entities mentioned:
surface_form: Blackwater Draw Museum
instance_of: Valley
countries: United States
coordinates: lat: 34.277874
lon: -103.32458
Harthope Moss. Harthope Moss, also known as Chapel Fell (elevation) is a mountain pass in the English Pennines. The pass divides Weardale to the north and Teesdale to the south. The unclassified road over the pass connects the A689 at St John's Chapel, County Durham with the B6277 near Langdon Beck in Upper Teesdale, County Durham.

Geographic entities mentioned:
surface_form: Weardale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.716
lon: -1.925
surface_form: Teesdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.545
lon: -1.927
The pass divides Weardale to the north and Teesdale to the south. The unclassified road over the pass connects the A689 at St John's Chapel, County Durham with the B6277 near Langdon Beck in Upper Teesdale, County Durham. It is the equal highest paved pass in England with the Killhope Cross on the A689, approximately 10 miles to the north on the other side of Burnhope Seat ().

Geographic entities mentioned:
surface_form: Burnhope Seat
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.732019444444
lon: -2.3353888888889
These were seized on 31 July 1918. These ships were later captured in April 1920 and incorporated into the Soviet Caspian Flotilla. Background. The Imperial Russian Navy had established the Caspian Flotilla in 1722. Following the Treaty of Gulistan of 1813, this flotilla had been the only naval force on the Caspian Sea. From 1867 it had been based at Baku.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Rhaphiolepis balgooyi. &quot;Rhaphiolepis balgooyi&quot; is a species of flowering plant in the family Rosaceae. It is endemic to Borneo, where it is found on Mount Kinabalu and Mount Tambuyukon in Kinabalu Park of Sabah state in Malaysia. &quot;Rhaphiolepis balgooyi&quot; is a multi-branched shrub, growing 0.5 to 2 meters high.

Geographic entities mentioned:
surface_form: Mount Kinabalu
instance_of: Mountain
countries: Malaysia
coordinates: lat: 6.075
lon: 116.5586111111111
surface_form: Mount Tambuyukon
instance_of: Mountain
countries: Malaysia
coordinates: lat: 6.20861111
lon: 116.65805556
Her tonnages were and. She had three masts and was a full-rigged ship. Her owners registered &quot;Loch Ard&quot; in Glasgow. Her official number was 68061 and her code letters were WSGD. The ship was named after Loch Ard in Scotland, a loch west of Aberfoyle and east of Loch Lomond. It means &quot;high lake&quot; in Scottish Gaelic. She gave her name to Loch Ard Gorge on the Shipwreck Coast.

Geographic entities mentioned:
surface_form: Loch Ard
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1844
lon: -4.4728
surface_form: Loch Lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
Several of these dams were constructed to divert stream flows to Stanford's reservoirs, the Lagunita Diversion Dam diverted flows to Lake Lagunita, Searsville Reservoir Dam which diverts minor flows for the Stanford Golf Course, and the Los Trancos Creek Diversion Dam which diverts water to Felt Reservoir.

Geographic entities mentioned:
surface_form: Lake Lagunita
instance_of: Lake
countries: United States
coordinates: lat: 37.423272222222
lon: -122.17607777778
It was located just north of the east end of Happy Hollow Lane near Alpine Road and near the Stanford Weekend Acres neighborhood in unincorporated Menlo Park. This dam was originally constructed in 1899–1900 to divert winter flows to fill Stanford's Lake Lagunita.

Geographic entities mentioned:
surface_form: Lake Lagunita
instance_of: Lake
countries: United States
coordinates: lat: 37.423272222222
lon: -122.17607777778
Mouaroa. Mouaroa (alternately spelled Mouaroa or Moua Roa), also known as the Shark’s Tooth, is a prominent peak near the center of Moorea, an island in French Polynesia in the central Pacific Ocean. It lies about south of the head of Opunohu Bay and about west of the highest point in Moorea, Mount Tohivea.

Geographic entities mentioned:
surface_form: Mount Tohivea.
instance_of: Mountain
countries: France
coordinates: lat: -17.5449
lon: -149.8127
Hellyer Gorge. The Hellyer Gorge is a gorge in Tasmania, located between Stanley and Cradle Mountain. The Hellyer River flows through the gorge, which is named after Henry Hellyer. Throughout the Hellyer Gorge is a rainforest with sassafras, giant myrtle, and large ferns. The gorge is the site of the Hellyer Gorge State Reserve.

Geographic entities mentioned:
surface_form: Cradle Mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -41.684644444444
lon: 145.951275
He conducted raids in Illyria at Oricum and Apollonia and seized the frontier town of Sintia in Dardania or perhaps Paionia. He then marched rapidly south through Pelagonia, Lyncestis and Bottiaea and on to Tempe which he garrisoned with 4,000 men. He turned north again into Thrace, attacking the Maedi and their chief city Iamphorynna before returning to Macedon.

Geographic entities mentioned:
surface_form: Tempe
instance_of: Valley
countries: Greece
coordinates: lat: 39.872778
lon: 22.546667
Far High House Meadows. Far High House Meadows is a Site of Special Scientific Interest in Upper Weardale in west County Durham, England. It consists of three fields, located just south of Burnhope Reservoir, some 3 km west of the village of Ireshopeburn.

Geographic entities mentioned:
surface_form: Upper Weardale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.716
lon: -1.925
It is part of the Basin and Range Province. It is bound by Hamlin Valley to the west, Snake Valley (part of this area known as Antelope Valley on some maps) to the north, Pine Valley to the east, and trends into the Indian Peak Range to the south. Collectively, the Mountain Home Range and Indian Peak Range are known as the Needle Mountains due to their jagged nature.

Geographic entities mentioned:
surface_form: Hamlin Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5138
lon: -114.177
Described as a &quot;pioneer of television in Australia&quot;, Newton-John was a host on the program &quot;Any Questions&quot; in 1958 and the presenter of &quot;Forum&quot; for a Newcastle TV station, NBN 3, in 1962. He appeared on an episode of &quot;The Valleys People&quot; (a chat show featuring residents of the Hunter Valley) in 1980.

Geographic entities mentioned:
surface_form: Hunter Valley
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Eynali. Eynali (), or On ibn Ali (), is a mountain range in north of Tabriz, Iran. The range has a couple of peaks including Eynali (1800 m), Halileh (1850 m), Pakeh-chin (1945 m), Bahlul (1985 m) and the highest one Dand (2378 m). There is a tomb at top of the mountain which is believed to be the grave of two clerics which the mountain's name is related to them.

Geographic entities mentioned:
surface_form: eynali
instance_of: Mountain
countries: Iran
coordinates: lat: 38.105555555556
lon: 46.322222222222
It is endemic to Bioko Island in Equatorial Guinea. Its natural habitats are subtropical or tropical moist montane forests and subtropical or tropical high-altitude shrubland. The species is wholly restricted to the higher elevations of Pico Basilé. It is threatened by habitat loss and is considered vulnerable under the IUCN Red List of threatened species.

Geographic entities mentioned:
surface_form: Pico Basilé
instance_of: Mountain
countries: Equatorial Guinea
coordinates: lat: 3.5833333333333
lon: 8.7666666666667
Location. The Sabine Glacier is on the Davis Coast on the west side of the Antarctic Peninsula. It drains north into the Orléans Strait to the west of Cape Kater. Lanchester Bay is to the west, Detroit Plateau to the south and Charcot Bay to the east. Name.

Geographic entities mentioned:
surface_form: Detroit Plateau
instance_of: Plateau
coordinates: lat: -64.1667
lon: -60
It has subsidiary summits The Benn and Castle Crag. Topography. The fell is the high point on a 2-mile-long spur running up the western shore of Thirlmere, branching off from the main ridge of the central fells just east of High Tove. Subsidiary tops include The Benn (also known as Benn Man,) and Castle Crag (), the site of an Iron Age settlement.

Geographic entities mentioned:
surface_form: High Tove
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5396
lon: -3.10199
Raven Crag is bordered to the west by the long valley of Shoulthwaite Gill, which is a tributary of the River Greta. To the north the ridge drops to a depression, crossed by the Keswick–Ambleside road, before climbing again onto High Rigg. Geology. Raven Crag and the Benn exhibit rock of the Birker Fell Formation, composed of plagioclase-phyric andesite lavas with subordinate sills.

Geographic entities mentioned:
surface_form: High Rigg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.588430555556
lon: -3.07235
Raven Crag is most commonly climbed from the dam, via a steep waymarked path through the forestry. This ends with made paths and some short sections of boardwalk. The ridge between Raven Crag and High Tove can also be gained from Armboth, or an ascent can be made from 'behind' via Shoulthwaite. This can include visits to The Benn and the earth ramparts of Castle Crag. Summit.

Geographic entities mentioned:
surface_form: high tove
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5396
lon: -3.10199
surface_form: raven crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5596
lon: -3.07778
Raven Crag. Raven Crag is a fell in the English Lake District that overlooks Thirlmere reservoir. It has subsidiary summits The Benn and Castle Crag. Topography. The fell is the high point on a 2-mile-long spur running up the western shore of Thirlmere, branching off from the main ridge of the central fells just east of High Tove.

Geographic entities mentioned:
surface_form: castle crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5328
lon: -3.16207
It has subsidiary summits The Benn and Castle Crag. Topography. The fell is the high point on a 2-mile-long spur running up the western shore of Thirlmere, branching off from the main ridge of the central fells just east of High Tove. Subsidiary tops include The Benn (also known as Benn Man,) and Castle Crag (), the site of an Iron Age settlement.

Geographic entities mentioned:
surface_form: castle crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5328
lon: -3.16207
To the north the ridge drops to a depression, crossed by the Keswick–Ambleside road, before climbing again onto High Rigg. Geology. Raven Crag and the Benn exhibit rock of the Birker Fell Formation, composed of plagioclase-phyric andesite lavas with subordinate sills. Between the two is an area of garnet bearing porphyritic andesite. Castle Crag Fort overlays volcaniclastic sandstone. Ascents.

Geographic entities mentioned:
surface_form: castle crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5328
lon: -3.16207
This ends with made paths and some short sections of boardwalk. The ridge between Raven Crag and High Tove can also be gained from Armboth, or an ascent can be made from 'behind' via Shoulthwaite. This can include visits to The Benn and the earth ramparts of Castle Crag. Summit. The highest point is an outcrop of rock with a small cairn, partially screened by conifers.

Geographic entities mentioned:
surface_form: castle crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5328
lon: -3.16207
Summit. The highest point is an outcrop of rock with a small cairn, partially screened by conifers. The view from the summit is limited by the trees, but the eastward panorama opens up from the brink of the crag itself and there is an aerial view of the Thirlmere dam. The reservoir is also seen end on to the south. The Benn and Castle Crag provide a close-up view of Raven Crag from the north.

Geographic entities mentioned:
surface_form: castle crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5328
lon: -3.16207
surface_form: raven crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5596
lon: -3.07778
Raven Crag. Raven Crag is a fell in the English Lake District that overlooks Thirlmere reservoir. It has subsidiary summits The Benn and Castle Crag. Topography. The fell is the high point on a 2-mile-long spur running up the western shore of Thirlmere, branching off from the main ridge of the central fells just east of High Tove.

Geographic entities mentioned:
surface_form: raven crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5596
lon: -3.07778
Subsidiary tops include The Benn (also known as Benn Man,) and Castle Crag (), the site of an Iron Age settlement. The ridge has been extensively planted with conifers as part of the Thirlmere Forest, the face of Raven Crag appearing as a lone oasis of naked rock amid the trees. Raven Crag is bordered to the west by the long valley of Shoulthwaite Gill, which is a tributary of the River Greta.

Geographic entities mentioned:
surface_form: raven crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5596
lon: -3.07778
To the north the ridge drops to a depression, crossed by the Keswick–Ambleside road, before climbing again onto High Rigg. Geology. Raven Crag and the Benn exhibit rock of the Birker Fell Formation, composed of plagioclase-phyric andesite lavas with subordinate sills. Between the two is an area of garnet bearing porphyritic andesite. Castle Crag Fort overlays volcaniclastic sandstone. Ascents.

Geographic entities mentioned:
surface_form: raven crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5596
lon: -3.07778
Castle Crag Fort overlays volcaniclastic sandstone. Ascents. The main face of the fell stands over Thirlmere Dam, and appears from there as a sheer crag, the higher fells behind being hidden by the ridge. Raven Crag is most commonly climbed from the dam, via a steep waymarked path through the forestry. This ends with made paths and some short sections of boardwalk.

Geographic entities mentioned:
surface_form: raven crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5596
lon: -3.07778
Army as an Indian scout for Lieutenant Colonel George Crook's campaign against renegades still active in Arizona following the surrender of Cochise earlier that year. Jim and the other scouts guided cavalry troopers in the Tonto Basin where the Western Apache and Yavapais had been successfully conducting raids and eluding troops for several years.

Geographic entities mentioned:
surface_form: Tonto Basin
instance_of: Valley
countries: United States
coordinates: lat: 33.8317
lon: -111.295
Terminology. Jammu and Kashmir is named after the two regions it encompasses the Jammu region and the Kashmir Valley. India collectively refers to the parts of Kashmir under Pakistani administration as &quot;Pakistan-occupied Kashmir&quot; (POK), and considers the region corresponding to Azad Kashmir as part of Jammu and Kashmir.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
History. After the Indo-Pakistani war of 1947–1948, three distinct areas of the princely state of Jammu and Kashmir were under Indian control: Muslim-majority Kashmir Valley, Hindu-majority Jammu region, and Buddhist-dominated Ladakh district. These regions were constituted as Jammu and Kashmir state and accorded special status by Article 370 of the Constitution of India, adopted in 1950.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
The alliance of Jammu & Kashmir National Conference and Indian National Congress formed the first government of the residual union territory with Omar Abdullah as chief minister. Topography. Jammu and Kashmir is home to several valleys such as the Kashmir Valley, Tawi Valley, Chenab Valley, Poonch Valley, Sind Valley, and Lidder Valley. The Kashmir valley is wide and in area.

Geographic entities mentioned:
surface_form: Sind Valley
instance_of: Valley
countries: India
coordinates: lat: 34.2892
lon: 74.8125
surface_form: Lidder Valley
instance_of: Valley
countries: India
coordinates: lat: 33.7764
lon: 75.2133
The Kashmir valley is wide and in area. The Himalayas divide the Kashmir valley from the Tibetan plateau while the Pir Panjal range, which encloses the valley from the west and the south, separates it from the Punjab Plain of the Indo-Gangetic Plain. Along the northeastern flank of the Valley runs the main range of the Himalayas.

Geographic entities mentioned:
surface_form: Tibetan plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Institutions such as the Jawahar Institute of Mountaineering and Winter Sports provides mountaineering, skiing and adventure courses. The Royal Springs Golf Course, Srinagar, located on the banks of Dal lake, is considered one of the best golf courses in India. Jammu and Kashmir was also host to the first Khelo India Winter Games, held in 2020 in Gulmarg.

Geographic entities mentioned:
surface_form: Dal lake
instance_of: Lake
countries: India
coordinates: lat: 34.12
lon: 74.87
Dénériaz's surprise win was by a margin of 0.72 seconds, the largest in this event in 42 years. He had entered the Olympics tied for tenth in the World Cup downhill standings; his best finish was seventh at Val Gardena in mid-December. Held on the Kandahar Banchetta piste, the course started at an elevation of above sea level with a vertical drop of and a length of.

Geographic entities mentioned:
surface_form: Val Gardena
instance_of: Valley
countries: Italy
coordinates: lat: 46.56
lon: 11.704722
Mammy Johnsons River. Mammy Johnsons River, a mostly perennial river of the Mid-Coast Council system, is located in the Mid North Coast and Upper Hunter regions of New South Wales, Australia. Course and features.

Geographic entities mentioned:
surface_form: Upper Hunter
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
The Albertine Rift follows the western edge of the Kenyan dome. This runs from Lake Malawi in the south, up into Lake Rukwa, Lake Tanganyika and Lake Albert in the north, where it ends. The Kenyan dome has the eastern branch of the EARS (known as The Gregory Rift) running through its middle, and contains most of what we historically saw as the Great Rift valley.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
This runs from Lake Malawi in the south, up into Lake Rukwa, Lake Tanganyika and Lake Albert in the north, where it ends. The Kenyan dome has the eastern branch of the EARS (known as The Gregory Rift) running through its middle, and contains most of what we historically saw as the Great Rift valley. Lake Victoria lies in the middle of the dome, with the Gregory Rift to the east of it.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
The Ethiopian dome is split down the middle by the Eastern Rift, formed by the developing plate boundary, and has formed a valley running from Lake Chamo and Lake Abaya in the south, widening through Lake Shala, Lake Ziwa and Lake Koku, until it reaches its widest point some from Djibouti.

Geographic entities mentioned:
surface_form: Lake Chamo
instance_of: Lake
countries: Ethiopia
coordinates: lat: 5.8333333333333
lon: 37.55
surface_form: Lake Abaya
instance_of: Lake
countries: Ethiopia
coordinates: lat: 6.236
lon: 37.832
Historian Jere L. Bacharach accepts Theophanes' date. Although earlier materials were re-used, much of the city is built on virgin soil. After being abandoned in later years, Anjar was resettled in 1939 with several thousand Armenian refugees from the Musa Dagh area. Its neighborhoods are named after the six villages of Musa Dagh: Haji Habibli, Kebusiyeh, Vakif, Kheder Bek, Yoghunoluk and Bitias.

Geographic entities mentioned:
surface_form: Musa Dagh
instance_of: Mountain
countries: Turkey
coordinates: lat: 36.258333333333
lon: 35.903611111111
Its neighborhoods are named after the six villages of Musa Dagh: Haji Habibli, Kebusiyeh, Vakif, Kheder Bek, Yoghunoluk and Bitias. During the civil war, the Syrian Army chose Anjar as one of its main military bases in the Beqaa Valley and the headquarters of its intelligence services. Following the civil war, Anjar started to rebuild economically.

Geographic entities mentioned:
surface_form: Beqaa Valley
instance_of: Valley
countries: Lebanon
coordinates: lat: 34.008888888889
lon: 36.145277777778
The Grossglockner High Alpine Road (in German &quot;Großglockner Hochalpenstraße&quot;) is the highest surfaced mountain pass road in Austria. It connects Bruck in the state of Salzburg with Heiligenblut in Carinthia via Fuscher Törl at 2,428 m (7,966 ft) and Hochtor Pass at. The road is named after the Grossglockner, Austria's highest mountain. Built as a scenic route, a toll is charged. Course.

Geographic entities mentioned:
surface_form: Grossglockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.074528
lon: 12.69385
The popular overlook was named after a visit by Emperor Franz Joseph I of Austria and his consort Elisabeth in 1856. It offers a panoramic view over the Pasterze Glacier, the Grossglockner massif, the Glocknerwand, and the Johannisberg in the northwest. From here the road runs downhill to the southern toll booth near Heiligenblut. History.

Geographic entities mentioned:
surface_form: Glocknerwand
instance_of: Mountain
countries: Austria
coordinates: lat: 47.079722222222
lon: 12.686388888889
Miltiades Hatzopoulos has suggested that the Macedonian dialect of the 4th century BC, as attested in the Pella curse tablet, was a sort of Macedonian 'koine' resulting from the encounter of the idiom of the 'Aeolic'-speaking populations around Mount Olympus and the Pierian Mountains with the Northwest Greek-speaking Argead Macedonians hailing from Argos Orestikon, who founded the kingdom of Lower Macedonia.

Geographic entities mentioned:
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
Census Bureau, the borough has a total area of, of which is land and (1.31%) is water. Three streams pass through Tamaqua: The Little Schuylkill River runs through Tamaqua from the north through the gap separating the folds of Sharp Mountain on the west and Nesquehoning Mountain. Panther Creek flows southwest from Lansford, five miles away, and joins the Little Schuylkill River in Tamaqua.

Geographic entities mentioned:
surface_form: Sharp Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.86182
lon: -75.83966
surface_form: Nesquehoning Mountain
instance_of: Landform
countries: United States
coordinates: lat: 40.8333
lon: -75.9158
Other highways near Tamaqua include Pennsylvania Route 54, Pennsylvania Route 443, Pennsylvania Route 895, and Pennsylvania Route 902, most of which connect the Tamaqua area to the Poconos, the Lehigh Valley, and South Central Pennsylvania. In addition, Interstates 81, 80, 476, and 78 are near the town.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Recent lake level declines have not prevented the deposition of microbe-produced rocks. Stromatolites are visible just underneath the water surface. Geology. Peinado is part of the Central Volcanic Zone of the Andes, which in northern Argentina extends across the Cordillera Occidental and the Altiplano.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
Numerous volcanoes occur in the region, including Laguna Amarga, Sierra Nevada de Lagunas Bravas, Laguna Escondida, Cerro El Condor, Wheelwright caldera, Falso Azufre, Nevado Tres Cruces, Ojos del Salado, Incahuasi, Cerro Torta, Cerro Blanco, Cueros de Purulla and numerous other calderas with accompanying ignimbrites, and monogenetic volcanoes.

Geographic entities mentioned:
surface_form: Falso Azufre
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -26.8
lon: -68.37
surface_form: Nevado Tres Cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: Ojos del Salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
surface_form: Incahuasi
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.033333333333
lon: -68.3
surface_form: laguna escondida
instance_of: Lake
countries: Argentina
coordinates: lat: -54.65
lon: -67.78
surface_form: cerro blanco
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.77
lon: -67.72
On the eastern side, the volcano is bordered by the Sierra de Calalaste. To the north lies the Salar de Antofalla, which ends close to Peinado, and the Laguna Peinado lake. A field of monogenetic volcanoes, the Peinado volcanic field, lies around Peinado. They consist of lava flows, maars, scoria cones and tuff rings, with volumes reaching, and were emplaced between 600,000 and 150,000 years ago.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
Volcanic carbon dioxide outgassing appears to occur at the lake. The lake presently has no outflow, but it may have spilled northward into the Salar de Antofalla during periods of higher lake level. Directly north of Laguna Peinado lies another lake, Laguna Turquesa, with an average depth of and a surface area of; the lakes may have been connected before 2005.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
Peinado presumably developed on Miocene volcanic rocks and eruption products of the Laguna Amarga caldera. A major strike-slip fault zone, the Peinado fault, runs from the western side of Salar de Antofalla south along Laguna Peinado to Peinado volcano. Farther south, it may connect to the San Francisco lineament.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
Peinado. Peinado is a stratovolcano in Catamarca Province, Argentina. It consists of a volcanic cone with a summit crater, surrounded at its foot by lava flows erupted from flank vents. It began erupting about 100,000 years ago, with the last eruption about 36,800 years ago. Future eruptions are possible.

Geographic entities mentioned:
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
It began erupting about 100,000 years ago, with the last eruption about 36,800 years ago. Future eruptions are possible. The volcano is part of the Andean Central Volcanic Zone and located within a cluster of calderas and large volcanoes, including the Laguna Amarga caldera just west of Peinado. The climate of the region is cold and dry, but may have been moister in the recent past.

Geographic entities mentioned:
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
Future eruptions are possible. The volcano is part of the Andean Central Volcanic Zone and located within a cluster of calderas and large volcanoes, including the Laguna Amarga caldera just west of Peinado. The climate of the region is cold and dry, but may have been moister in the recent past. North of Peinado lies the salt lake Laguna Peinado. Geography and geomorphology.

Geographic entities mentioned:
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
North of Peinado lies the salt lake Laguna Peinado. Geography and geomorphology. Peinado lies in Argentina's Catamarca Province, close to the border with Chile and about from the Paso San Francisco. Geographically, it is in the Cordillera Occidental of the Central Andes. The region is largely uninhabited, due to the extreme climatic conditions.

Geographic entities mentioned:
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
Claims that the volcano overlies a caldera lack supporting evidence. Just west of Peinado lies the eastern margin of the Pliocene Laguna Amarga caldera; its ignimbrites underlie Peinado and lava flows from Peinado have spilled across its borders on to the caldera floor. On the eastern side, the volcano is bordered by the Sierra de Calalaste.

Geographic entities mentioned:
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
On the eastern side, the volcano is bordered by the Sierra de Calalaste. To the north lies the Salar de Antofalla, which ends close to Peinado, and the Laguna Peinado lake. A field of monogenetic volcanoes, the Peinado volcanic field, lies around Peinado. They consist of lava flows, maars, scoria cones and tuff rings, with volumes reaching, and were emplaced between 600,000 and 150,000 years ago.

Geographic entities mentioned:
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
A field of monogenetic volcanoes, the Peinado volcanic field, lies around Peinado. They consist of lava flows, maars, scoria cones and tuff rings, with volumes reaching, and were emplaced between 600,000 and 150,000 years ago. Lake. Laguna Peinado is a wide, long lake with a mean depth of -. Water covers an area of. It lies at elevation at about.

Geographic entities mentioned:
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
Volcanic carbon dioxide outgassing appears to occur at the lake. The lake presently has no outflow, but it may have spilled northward into the Salar de Antofalla during periods of higher lake level. Directly north of Laguna Peinado lies another lake, Laguna Turquesa, with an average depth of and a surface area of; the lakes may have been connected before 2005.

Geographic entities mentioned:
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
Their ages range from Miocene to Quaternary; volcanism there has been ongoing since the Eocene-Oligocene. Peinado presumably developed on Miocene volcanic rocks and eruption products of the Laguna Amarga caldera. A major strike-slip fault zone, the Peinado fault, runs from the western side of Salar de Antofalla south along Laguna Peinado to Peinado volcano.

Geographic entities mentioned:
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
Farther south, it may connect to the San Francisco lineament. Apart from volcanoes, tectonically-generated basins and ridges form a steep relief in the region; the Laguna Peinado occupies one of several north-south trending tectonic depressions in the area. Magma may be present in the crust. Volcanic rocks are mainly andesite and basaltic andesite, with dacite being erupted more recently.

Geographic entities mentioned:
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
The monogenetic volcanoes have erupted basaltic andesite. In the summit region, the rocks have been discoloured presumably by hydrothermal alteration. Eruption history. Peinado is one of the youngest volcanoes in the area. Radiometric dating has yielded ages ranging between 80,000 and 40,000 years ago for the central cone and between 60,000 and 30,000 for the flank vents.

Geographic entities mentioned:
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
Eruptions have been mostly effusive, but with recent explosive events. The monogenetic volcanoes just south and north of Peinado developed 210,000 ± 40,000 and 380,000 ± 20,000 years ago, respectively; the flank vent that formed a scoria cone may also be associated with the monogenetic activity rather than Peinado proper.

Geographic entities mentioned:
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
Presumably, Peinado began its growth as a monogenetic volcano but eruptions became concentrated at a single vent, producing a shallow magma chamber that intercepted ascending magma and a single cone. Eventually, the cone reached a size at which further eruptions from the summit were impeded, causing volcanism to shift to the flank vents, which then built up the bulk of Peinado.

Geographic entities mentioned:
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
There are reports of fumarolic activity. Volcanoes have been observed to remain inactive for ten thousands of years; thus future activity at Peinado is possible. The configuration of volcanic vents suggests that the occurrence of caldera collapse and of sector collapses is possible, and its activity has become more explosive over time.

Geographic entities mentioned:
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
The climate has not been stable during the Pleistocene, and may have been wetter during glacial times. What little vegetation there is, is mostly steppe grasses. Salt-loving vegetation and underwater plants grow around and in Laguna Peinado, which also features microbial mats. Name and human activity. The name (&quot;combed&quot; in Spanish) is a reference to its smooth appearance.

Geographic entities mentioned:
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15
The name (&quot;combed&quot; in Spanish) is a reference to its smooth appearance. The first known ascent was by in 1965, but the mountain features a pre-Hispanic mountain sanctuary and may have been used as a source for valuable rocks by pre-Hispanic people. A prehistoric copper and aragonite mine with well-preserved buildings lies at Tambería El Peinado, close to the volcano.

Geographic entities mentioned:
surface_form: peinado
instance_of: Mountain
countries: Argentina
coordinates: lat: -26.62
lon: -68.15