Sarmila/GeoWiki-Features huggingface dataset:
Its nearest higher peak is Napeequa Peak, to the south. The peak is set on Chiwawa Ridge with Napeequa, and other notable peaks on this ridge include Fortress Mountain, Buck Mountain, Brahma Peak, Mount Berge, and Chiwawa Mountain. Topographic relief is significant since the western aspect of the mountain rises 4,000 feet above the Suiattle Valley in approximately.

Geographic entities mentioned:
surface_form: Brahma Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.06777777777778
lon: -120.91333333333334
surface_form: Mount Berge
instance_of: Mountain
countries: United States
coordinates: lat: 48.103246
lon: -120.946243
surface_form: Chiwawa Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.163333333333
lon: -120.90722222222
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6081079
lon: -90.3926199
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.66388889
lon: -90.52972222
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.889722222222
lon: -74.404166666667
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.461944444444
lon: -105.43833333333
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6894
lon: -110.819
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9509
lon: -76.2074
surface_form: fortress mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.336944444444
lon: -109.79805555556
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6047712
lon: -90.7190122
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.052777777778
lon: -74.532777777778
surface_form: fortress mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.15916667
lon: -120.93388889
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.193333333333
lon: -78.563611111111
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.093611111111116
lon: -120.91222222222223
Subduction and tectonic activity in the area began during the late cretaceous period, about. Extensive volcanic activity began to take place in the oligocene, about 35 million years ago. Glacier Peak, a stratovolcano that is west of Cirque Mountain, began forming in the mid-Pleistocene. Due to Glacier Peak's proximity to Cirque Mountain, volcanic ash is common in the area. Climate.

Geographic entities mentioned:
surface_form: Glacier Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.14972222
lon: -109.84944444
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.155013
lon: -117.293429
surface_form: cirque mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.003888888889
lon: -107.77166666667
surface_form: cirque mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.108491
lon: -120.972701
Cirque Mountain (Washington). Cirque Mountain is a mountain summit located in the Glacier Peak Wilderness of the North Cascades in Washington state. The mountain is situated on the crest of the Cascade Range, on the shared border of Snohomish County and Chelan County, also straddling the boundary between the Mount Baker-Snoqualmie National Forest and the Wenatchee National Forest.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: cirque mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.003888888889
lon: -107.77166666667
surface_form: cirque mountain (washington)
instance_of: Mountain
countries: United States
coordinates: lat: 48.108491
lon: -120.972701
Cirque Mountain (Washington). Cirque Mountain is a mountain summit located in the Glacier Peak Wilderness of the North Cascades in Washington state. The mountain is situated on the crest of the Cascade Range, on the shared border of Snohomish County and Chelan County, also straddling the boundary between the Mount Baker-Snoqualmie National Forest and the Wenatchee National Forest.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.14972222
lon: -109.84944444
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.155013
lon: -117.293429
surface_form: cirque mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.003888888889
lon: -107.77166666667
surface_form: cirque mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.108491
lon: -120.972701
Extensive volcanic activity began to take place in the oligocene, about 35 million years ago. Glacier Peak, a stratovolcano that is west of Cirque Mountain, began forming in the mid-Pleistocene. Due to Glacier Peak's proximity to Cirque Mountain, volcanic ash is common in the area. Climate. Cirque Mountain is located in the marine west coast climate zone of western North America.

Geographic entities mentioned:
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.14972222
lon: -109.84944444
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.155013
lon: -117.293429
surface_form: cirque mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.003888888889
lon: -107.77166666667
surface_form: cirque mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.108491
lon: -120.972701
Cirque Mountain (Washington). Cirque Mountain is a mountain summit located in the Glacier Peak Wilderness of the North Cascades in Washington state. The mountain is situated on the crest of the Cascade Range, on the shared border of Snohomish County and Chelan County, also straddling the boundary between the Mount Baker-Snoqualmie National Forest and the Wenatchee National Forest.

Geographic entities mentioned:
surface_form: chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Glacier Peak, a stratovolcano that is west of Cirque Mountain, began forming in the mid-Pleistocene. Due to Glacier Peak's proximity to Cirque Mountain, volcanic ash is common in the area. Climate. Cirque Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains.

Geographic entities mentioned:
surface_form: cirque mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.003888888889
lon: -107.77166666667
surface_form: cirque mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.108491
lon: -120.972701
Interstate 89 passes just east of Swanton village, with access from Exit 21 (Vermont Route 78). I-89 leads north to the Canada–US border and south to the Burlington area. Vermont Route 78 passes through the village on First Street, Grand Avenue, Depot Street, and North River Street, leading east to Highgate Center and west to Alburgh on Grand Isle in Lake Champlain.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
He also had contact with other contemporary artists such as José Chávez Morado and Raúl Anguiano. Career. He was a painter, sketch artist, engraver and muralist and considered to be one of the best landscape artists of the 20th century. His works have included depictions of the immense ravines of the Sierra Tarahumara, the Mezquital Valley, and the remains of Lake Xochimilco.

Geographic entities mentioned:
surface_form: Lake Xochimilco
instance_of: Lake
countries: Mexico
coordinates: lat: 19.285
lon: -99.102
As one of the only routes across the Santa Monica Mountains, SR 27 is heavily traveled by commuters from the western San Fernando Valley heading to Santa Monica or Interstate 10. Route description. SR 27 begins at SR 1 near the Pacific Ocean at Topanga County Beach, in an unincorporated area of Los Angeles County east of Malibu.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Upon exiting the park, SR 27 provides access to Fernwood, Topanga, Sylvia Park, and Glenview, all unincorporated. SR 27 continues winding into the San Fernando Valley, nearly entering Calabasas before entering the Los Angeles community of Woodland Hills. The route becomes a major city arterial through the valley, intersecting US 101 before entering Warner Center and Canoga Park.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Several other limestone members exist (Tomstown and New Oxford), no caves have been located within these members. Blue Ridge & the Great Valley – the Blue Ridge rises up from the Piedmont just west of Frederick in the first of its two mountains, Braddock/Catoctin.

Geographic entities mentioned:
surface_form: Catoctin
instance_of: Mountain
countries: United States
coordinates: lat: 39.6478
lon: -77.4664
South Mountain, which serves as a natural border between Frederick and Washington counties, is the western edge of Maryland's Blue Ridge, giving way to an area of relatively little relief, known as the Great Valley (or locally as Hagerstown/Cumberland).

Geographic entities mentioned:
surface_form: Cumberland
instance_of: Valley
countries: United States
coordinates: lat: 39.93
lon: -77.72
Here the harder metamorphosed rocks of the Blue Ridge are replaced by carbonates, sandstones, and shale that grow progressively younger moving west, entering the early Ordovician period. The highest concentration of Maryland caves lies within the Hagerstown Valley, where well-established waterways have cut into the underlying carbonate rocks.

Geographic entities mentioned:
surface_form: Hagerstown Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.4397
lon: -77.7547
These younger rocks have settled to a depth equal to that of the much older rocks of the Ordovician. This change in depth occurs along a fault just east of Dans Mountain. Moving west from outcrops of early Devonian limestone, the Helderbergian limestones pinch out and the formation consists of clastic rocks that bear no caves.

Geographic entities mentioned:
surface_form: Dans Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.5818
lon: -78.8972
Camp Fatima (New Hampshire). Camp Fatima is a Catholic overnight summer camp located in Gilmanton Iron Works, NH. The camp has a waterfront on the northern shore of Upper Suncook Lake. History. The camp was founded in 1949 by Richard O Boner, after the previous establishment, a Jewish camp named Camp Wingo, closed and relocated to Maine.

Geographic entities mentioned:
surface_form: Upper Suncook Lake
instance_of: Group of lakes
countries: United States
coordinates: lat: 43.381666666667
lon: -71.275277777778
Haliotis corrugata. The pink abalone, scientific name &quot;Haliotis corrugata&quot;, is a species of large edible sea snail, a marine gastropod mollusk in the family Haliotidae, the abalone. Distribution. Pink abalone can be found along the Pacific coast of North America from Point Conception, California to Bahia de Santa Maria, Baja California Sur, Mexico. Description.

Geographic entities mentioned:
surface_form: Point Conception
instance_of: Landform
countries: United States
coordinates: lat: 34.448113
lon: -120.471439
Pukara Punta. Pukara Punta (Quechua &quot;pukara&quot; fortress, &quot;punta&quot; peak; ridge, &quot;fortress peak (or ridge)&quot;, also spelled &quot;Pucará Punta&quot;) is a mountain in the Andes of Peru which reaches a height of approximately. It lies in the Junín Region, Tarma Province, on the border of the districts of Palcamayo and Cajas.

Geographic entities mentioned:
surface_form: pukara
instance_of: Mountain
countries: Peru
coordinates: lat: -14.9583
lon: -72.3039
surface_form: pukara
instance_of: Mountain
countries: Peru
coordinates: lat: -14.9583
lon: -72.3039
surface_form: pukara
instance_of: Mountain
countries: Peru
coordinates: lat: -16.3361
lon: -70.8508
surface_form: pukara
instance_of: Mountain
countries: Peru
coordinates: lat: -16.3361
lon: -70.8508
surface_form: pukara
instance_of: Mountain
countries: Peru
surface_form: pukara
instance_of: Mountain
countries: Peru
surface_form: pukara
instance_of: Mountain
countries: Peru
coordinates: lat: -13.2042
lon: -71.6544
surface_form: pukara
instance_of: Mountain
countries: Peru
coordinates: lat: -13.2042
lon: -71.6544
surface_form: pukara punta
instance_of: Mountain
countries: Peru
coordinates: lat: -11.22222222
lon: -75.8325
surface_form: pukara
instance_of: Mountain
countries: Peru
coordinates: lat: -16.4594
lon: -70.9789
surface_form: pukara
instance_of: Mountain
countries: Peru
coordinates: lat: -16.4594
lon: -70.9789
Pukara Punta. Pukara Punta (Quechua &quot;pukara&quot; fortress, &quot;punta&quot; peak; ridge, &quot;fortress peak (or ridge)&quot;, also spelled &quot;Pucará Punta&quot;) is a mountain in the Andes of Peru which reaches a height of approximately. It lies in the Junín Region, Tarma Province, on the border of the districts of Palcamayo and Cajas.

Geographic entities mentioned:
surface_form: pukara
instance_of: Mountain
countries: Peru
coordinates: lat: -14.9583
lon: -72.3039
surface_form: pukara
instance_of: Mountain
countries: Peru
coordinates: lat: -16.3361
lon: -70.8508
surface_form: pukara
instance_of: Mountain
countries: Peru
surface_form: pukara
instance_of: Mountain
countries: Peru
coordinates: lat: -13.2042
lon: -71.6544
surface_form: pukara punta
instance_of: Mountain
countries: Peru
coordinates: lat: -11.22222222
lon: -75.8325
surface_form: pukara
instance_of: Mountain
countries: Peru
coordinates: lat: -16.4594
lon: -70.9789
Satluj Valley. Satluj Valley (alternative spelling &quot;Sutlej&quot;) is a valley in the Kinnaur district of Himachal Pradesh, India. Sutlej river runs through it.

Geographic entities mentioned:
surface_form: satluj valley
instance_of: Valley
countries: India
coordinates: lat: 31.345
lon: 77.453
Lac Vert (Lesponne). Lac Vert is a small lake in Hautes-Pyrénées, France. At an elevation of, its surface area is.

Geographic entities mentioned:
surface_form: lac vert
instance_of: Lake
countries: France
coordinates: lat: 45.94996
lon: 6.75308
surface_form: lac vert
instance_of: Lake
countries: France
coordinates: lat: 42.93333333
lon: 0.08777778
The Silk Glacier is fed from this ridge just south of Mount Zinkovich and flows east to join Nursery Glacier. The Jorda Glacier is fed from the ridge between Pyramid Mountain and Mount Coley, and also flows east to join Nursery Glacier. To the west is the Byrd Névé, from which rise the Wallabies Nunataks and the All-Blacks Nunataks. Kilroy Bluff.

Geographic entities mentioned:
surface_form: All-Blacks Nunataks
instance_of: Mountain
coordinates: lat: -81.4833
lon: 155.75
An ice-covered bluff, high, on the west side of Nursery Glacier at the junction with Jorda Glacier. The east face of the feature is indented by twin cirques that resemble eyes. Under certain light conditions the appearance of the bluff is reminiscent of ubiquitous Kilroy graffiti of World War II: a caricature of a head peering over a wall and the message &quot;Kilroy was here&quot;. Mount Coley.

Geographic entities mentioned:
surface_form: light
instance_of: Mountain
coordinates: lat: -74.2667
lon: -61.9833
Location. Mount Zinkovich is on a ridge that extends from Pyramid Mountain to the south, through Mount Coley, Mount Frost, Mount Zinkovich and further north past Mount Wharton and Turk Peak. The Silk Glacier is fed from this ridge just south of Mount Zinkovich and flows east to join Nursery Glacier.

Geographic entities mentioned:
surface_form: pyramid mountain
instance_of: Mountain
coordinates: lat: -77.76667
lon: 160.66667
surface_form: mount wharton
instance_of: Mountain
coordinates: lat: -81.04916667
lon: 157.79250333
surface_form: wharton
instance_of: Mountain
coordinates: lat: -81.04916667
lon: 157.79250333
surface_form: zinkovich
instance_of: Mountain
coordinates: lat: -81.13333
lon: 158.23333
surface_form: zinkovich
instance_of: Mountain
coordinates: lat: -81.13333
lon: 158.23333
surface_form: mount zinkovich
instance_of: Mountain
coordinates: lat: -81.13333
lon: 158.23333
surface_form: mount zinkovich
instance_of: Mountain
coordinates: lat: -81.13333
lon: 158.23333
surface_form: pyramid
instance_of: Mountain
coordinates: lat: -78.35
lon: 163.5
The Silk Glacier is fed from this ridge just south of Mount Zinkovich and flows east to join Nursery Glacier. The Jorda Glacier is fed from the ridge between Pyramid Mountain and Mount Coley, and also flows east to join Nursery Glacier. To the west is the Byrd Névé, from which rise the Wallabies Nunataks and the All-Blacks Nunataks. Kilroy Bluff.

Geographic entities mentioned:
surface_form: pyramid mountain
instance_of: Mountain
coordinates: lat: -77.76667
lon: 160.66667
surface_form: pyramid
instance_of: Mountain
coordinates: lat: -78.35
lon: 163.5
Mount Wharton. A mountain over, standing west of Turk Peak in the Churchill Mountains. Discovered by the BrNAE (1901-04) and named for Sir William Wharton, Hydrographer to the Royal Navy, 1884-1904. Turk Peak. A large hump-shaped peak, high, being the central of three peaks on a ridge north of Mount Zinkovich, in the Churchill Mountains. Named by US-ACAN for Lt. Col.

Geographic entities mentioned:
surface_form: wharton
instance_of: Mountain
coordinates: lat: -81.04916667
lon: 157.79250333
surface_form: william
instance_of: Mountain
coordinates: lat: -64.7833
lon: -63.6833
Bradshaw Peak. A peak rising to, south east of Turk Peak. Situated on the south west side of McLay Glacier. Named in honor of Margaret Bradshaw, geological scientist, University of Canterbury. Margaret is an eminent geologist and in 1979 was the first woman to lead a deep field party in the Antarctic. Margaret is also the only New Zealand woman to be awarded a Polar medal.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
Turk Peak. A large hump-shaped peak, high, being the central of three peaks on a ridge north of Mount Zinkovich, in the Churchill Mountains. Named by US-ACAN for Lt. Col. Wilbert Turk, commander of the 61st Troop Carrier Squadron which initiated the flights of C-130 Hercules aircraft in Antarctica in January 1960. Bradshaw Peak. A peak rising to, south east of Turk Peak.

Geographic entities mentioned:
surface_form: hercules
instance_of: Mountain
coordinates: lat: -77.4833
lon: 161.433
Named by US-ACAN for Cdr. Vernon J. Coley, commanding officer of USN Squadron VX-6 in Antarctica, 1957-58. Young Peaks. Young Peaks is a group of peaks along a ridge running west–east, starting 5 km east of Mount Coley. The feature is 5 km long with summits rising above 1200 m. Flanked by Lee Glacier at north and Jorda Glacier at south.

Geographic entities mentioned:
surface_form: young
instance_of: Mountain
coordinates: lat: -84.45
lon: 179.8
surface_form: young peaks
instance_of: Mountain
coordinates: lat: -81.2333333
lon: 158.7
The feature is 5 km long with summits rising above 1200 m. Flanked by Lee Glacier at north and Jorda Glacier at south. Named in honor of Pamela Young who was the first female event member in the New Zealand Antarctic Research Program (NZARP). Mount Frost. Mountain, high, in the Churchill Mountains, standing south of Mount Zinkovich, at the south side of the head of Silk Glacier.

Geographic entities mentioned:
surface_form: young
instance_of: Mountain
coordinates: lat: -84.45
lon: 179.8
Mount Zinkovich. Mount Zinkovich () is a pointed mountain, high, standing north of Mount Frost at the north side of the head of Silk Glacier in the Churchill Mountains of Antarctica. Name. Mount Zinkovich was named by US-ACAN for Lt. Col.

Geographic entities mentioned:
surface_form: zinkovich
instance_of: Mountain
coordinates: lat: -81.13333
lon: 158.23333
surface_form: mount zinkovich
instance_of: Mountain
coordinates: lat: -81.13333
lon: 158.23333
Name. Mount Zinkovich was named by US-ACAN for Lt. Col. Michael Zinkovich, USAF, commanding officer of the 1710th Aerial Port Squadron, which furnished airlift support between New Zealand and Antarctica, and from McMurdo Sound inland to Byrd, Eights, and South Pole Stations during USN OpDFrz 1962. Location.

Geographic entities mentioned:
surface_form: zinkovich
instance_of: Mountain
coordinates: lat: -81.13333
lon: 158.23333
Location. Mount Zinkovich is on a ridge that extends from Pyramid Mountain to the south, through Mount Coley, Mount Frost, Mount Zinkovich and further north past Mount Wharton and Turk Peak. The Silk Glacier is fed from this ridge just south of Mount Zinkovich and flows east to join Nursery Glacier.

Geographic entities mentioned:
surface_form: zinkovich
instance_of: Mountain
coordinates: lat: -81.13333
lon: 158.23333
surface_form: mount zinkovich
instance_of: Mountain
coordinates: lat: -81.13333
lon: 158.23333
Flanked by Lee Glacier at north and Jorda Glacier at south. Named in honor of Pamela Young who was the first female event member in the New Zealand Antarctic Research Program (NZARP). Mount Frost. Mountain, high, in the Churchill Mountains, standing south of Mount Zinkovich, at the south side of the head of Silk Glacier. Named by US-ACAN for Lt. Col. Foy B.

Geographic entities mentioned:
surface_form: zinkovich
instance_of: Mountain
coordinates: lat: -81.13333
lon: 158.23333
surface_form: mount zinkovich
instance_of: Mountain
coordinates: lat: -81.13333
lon: 158.23333
Mount Wharton. A mountain over, standing west of Turk Peak in the Churchill Mountains. Discovered by the BrNAE (1901-04) and named for Sir William Wharton, Hydrographer to the Royal Navy, 1884-1904. Turk Peak. A large hump-shaped peak, high, being the central of three peaks on a ridge north of Mount Zinkovich, in the Churchill Mountains. Named by US-ACAN for Lt. Col.

Geographic entities mentioned:
surface_form: zinkovich
instance_of: Mountain
coordinates: lat: -81.13333
lon: 158.23333
surface_form: mount zinkovich
instance_of: Mountain
coordinates: lat: -81.13333
lon: 158.23333
The seismotectonics of Yunnan and the adjacent areas is driven by the collision of the Indian plate with the Eurasian plate. This has uplifted the Tibetan Plateau (and the Himalaya Mountains) and forced it eastwards, pushing the South China Block and Indochina towards the westward subducting Philippine Sea plate and creating various extensional structures.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
The festival returns in 2025 after a five year hiatus. Stages. The main festival grounds are located in Tarahne Park near Atlin Lake, one of the largest natural lakes in British Columbia. There are three main stages in Atlin that are in use during the festival: The Park Stage, The Lake Stage, and The Globe Theatre.

Geographic entities mentioned:
surface_form: Atlin Lake
instance_of: Lake
countries: Canada
coordinates: lat: 60.0133333
lon: -133.8308333
It is situated on the edge of the Òdena Basin at the entrance to the Capellades Gorge. The town
is dominated by Claramunt castle, on a hilltop some 150 m above the modern settlement: the castle was, with
Castellbell castle, one of the main points of control of access to the Llobregat valley and hence to Barcelona.

Geographic entities mentioned:
surface_form: Llobregat
instance_of: Watercourse
countries: Spain
coordinates: lat: 42.282412
lon: 2.012826
Nevados de Pastos Grandes. y3vb6jtldbh2c4bbt0uy6zw43x25vi" xml:space="preserve">Nevados de Pastos Grandes is a Miocene volcanic centre in the Puna, Salta province, Argentina. It is a volcanic complex with several centres named El Queva, Gordo and Azufre. Some minor Pleistocene glaciation has affected the volcanic complex.

Geographic entities mentioned:
surface_form: El Queva
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.3075
lon: -66.733333333333
He was arrested again for violating his bail conditions, and died of pneumonia in custody on January 12, 2024. Early life. Lira was born to Chilean parents in Burbank, California, and grew up in the San Fernando Valley of Los Angeles; Guayaquil, Ecuador; and Santiago, Chile, among other places. He graduated from Saint George's College, Santiago in 1985.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Between 1909 and 1912, he excavated dwelling sites Riukjärvi and Piiskunsalmi. He also researched shore displacement at Lake Ladoga, creating the first model of its history, a history late 19th-century geologists and archaeologists had already found unique for its deviation from the standard land uplift model. In 1909 and 1910, he with salvage excavated Häyrynmäki in Viipuri Province.

Geographic entities mentioned:
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
Vermillion Creek. Vermillion Creek is a tributary of the Green River. It flows south from Sweetwater County, Wyoming to a confluence with the Green River just north of the Gates of Lodore in Moffat County, Colorado.

Geographic entities mentioned:
surface_form: Gates of Lodore
instance_of: Landform
countries: United States
coordinates: lat: 40.7131
lon: -108.893
The border with England in the east largely follows the course of the River Wye and its tributary, the River Monnow. In the south east is the Wye Valley AONB, a hilly region which stretches into England. The county has a shoreline on the Severn Estuary, with crossings into England by the Severn Bridge and Prince of Wales Bridge.

Geographic entities mentioned:
surface_form: Wye Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69255
lon: -2.66283
To the east, it borders the English counties of Herefordshire and Gloucestershire. The centre of the county is the plain of Gwent, formed from the basin of the River Usk, while the River Wye forms part of its eastern border, running through the Wye Valley, one of the five Areas of Outstanding Natural Beauty in Wales and the only one in the county.

Geographic entities mentioned:
surface_form: Wye Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69255
lon: -2.66283
Both rivers flow south to the Severn Estuary. The River Monnow is a tributary of the River Wye and forms part of the border with Herefordshire and England, passing through the town of Monmouth. The highest point of the county is Chwarel y Fan in the Black Mountains, with a height of.

Geographic entities mentioned:
surface_form: Chwarel y Fan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 51.958231
lon: -3.080984
Geology. The centre of the principal area is dominated by the Usk Inlier, a large outcrop of Silurian rock. The inlier is surrounded by younger, Devonian, rock, including areas of Old Red Sandstone which forms a very common building material in the county. The Wye Gorge, in the extreme east of the county, has a bed of Carboniferous Limestone. Coastline and landscape.

Geographic entities mentioned:
surface_form: Wye Gorge
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69255
lon: -2.66283
Llandegfedd Reservoir, developed in the 1960s to provide a water supply to Cardiff, is an SSSI providing overwintering for wildfowl. The Wye Valley, the county's only National Landscape, has its largest population of deer and the UK's largest population of lesser horseshoe bats.

Geographic entities mentioned:
surface_form: Wye Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69255
lon: -2.66283
The contemporary writer, Gilli Davies, in her study of Welsh food, &quot;Tastes of Wales&quot;, writes of the &quot;rare and appealing quality to the food in Monmouthshire&quot;. The county has a small viniculture industry, with vineyards at Ancre Hill Estates, north of Monmouth; White Castle vineyard near Abergavenny, and the Tintern Parva vineyard in the Wye Valley.

Geographic entities mentioned:
surface_form: Wye Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69255
lon: -2.66283
From this peak, the border approaching south from the Fluchthorn departs east to intersect the neighboring valley in an Austrian lower (north) part named Fimbatal and an uninhabited Swiss upper (south) part, named Val Fenga. On the Austrian west site lies the also uninhabited Larein valley.

Geographic entities mentioned:
surface_form: Fluchthorn
instance_of: Mountain
countries: Switzerland
Austria
coordinates: lat: 46.893055555555556
lon: 10.226944444444445
surface_form: Fimbatal
instance_of: Valley
countries: Switzerland
Austria
coordinates: lat: 46.9633
lon: 10.2839
Paraid Naira. The Gamspleisspitze (German, also &quot;Gemspleisspitze&quot;) or Paraid Naira (Romansh) is a mountain of the Silvretta Alps, located on the border between Austria and Switzerland.

Geographic entities mentioned:
surface_form: gamspleisspitze
instance_of: Mountain
countries: Switzerland
Austria
coordinates: lat: 46.931611111111
lon: 10.241583333333
surface_form: gemspleisspitze
instance_of: Mountain
countries: Switzerland
Austria
coordinates: lat: 46.931611111111
lon: 10.241583333333
surface_form: paraid naira
instance_of: Mountain
countries: Switzerland
Austria
coordinates: lat: 46.931611111111
lon: 10.241583333333
Paraid Naira. The Gamspleisspitze (German, also &quot;Gemspleisspitze&quot;) or Paraid Naira (Romansh) is a mountain of the Silvretta Alps, located on the border between Austria and Switzerland.

Geographic entities mentioned:
surface_form: paraid naira
instance_of: Mountain
countries: Switzerland
Austria
coordinates: lat: 46.931611111111
lon: 10.241583333333
Paiju Peak. Paiju Peak, also known as Payu, is a mountain in northern Pakistan. Description. Paiju Peak is a glaciated summit in the Baltoro Muztagh subrange of the Karakoram. The remote mountain is situated immediately northwest of the terminus of the Baltoro Glacier and southwest of the Trango Towers in Central Karakoram National Park.

Geographic entities mentioned:
surface_form: muztagh
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.828333333333
lon: 76.360833333333
surface_form: paiju peak
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.71436
lon: 76.115961
Paiju Peak. Paiju Peak, also known as Payu, is a mountain in northern Pakistan. Description. Paiju Peak is a glaciated summit in the Baltoro Muztagh subrange of the Karakoram. The remote mountain is situated immediately northwest of the terminus of the Baltoro Glacier and southwest of the Trango Towers in Central Karakoram National Park.

Geographic entities mentioned:
surface_form: paiju peak
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.71436
lon: 76.115961
Technical assistance was provided by Allen Steck who stopped short of the summit to photograph the other climbers. Climate. Based on the Köppen climate classification, Paiju Peak is located in a tundra climate zone with cold, snowy winters, and cool summers. Weather systems are forced upwards by the mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall.

Geographic entities mentioned:
surface_form: paiju peak
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.71436
lon: 76.115961
Mount Whitecap. Mount Whitecap () is located in the northern Wind River Range in the U.S. state of Wyoming. Situated southwest of Gannett Peak, Mount Whitecap is in the Bridger Wilderness of Bridger-Teton National Forest. Baby Glacier lies just to the east of the peak and Split Mountain is southeast. Mount Whitecap is the 30th tallest peak in Wyoming. Hazards.

Geographic entities mentioned:
surface_form: Gannett Peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.184202777778
lon: -109.65423333333
surface_form: mount whitecap
instance_of: Mountain
countries: United States
coordinates: lat: 43.1686
lon: -109.692
Mount Whitecap. Mount Whitecap () is located in the northern Wind River Range in the U.S. state of Wyoming. Situated southwest of Gannett Peak, Mount Whitecap is in the Bridger Wilderness of Bridger-Teton National Forest. Baby Glacier lies just to the east of the peak and Split Mountain is southeast. Mount Whitecap is the 30th tallest peak in Wyoming. Hazards.

Geographic entities mentioned:
surface_form: split mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.164166666667
lon: -109.6725
surface_form: split mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.020833333333
lon: -118.42222222222
surface_form: split mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.483333333333
lon: -109.22055555556
surface_form: split mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.5981
lon: -113.539
Mount Whitecap. Mount Whitecap () is located in the northern Wind River Range in the U.S. state of Wyoming. Situated southwest of Gannett Peak, Mount Whitecap is in the Bridger Wilderness of Bridger-Teton National Forest. Baby Glacier lies just to the east of the peak and Split Mountain is southeast. Mount Whitecap is the 30th tallest peak in Wyoming. Hazards.

Geographic entities mentioned:
surface_form: mount whitecap
instance_of: Mountain
countries: United States
coordinates: lat: 43.1686
lon: -109.692
state of Wyoming. Situated southwest of Gannett Peak, Mount Whitecap is in the Bridger Wilderness of Bridger-Teton National Forest. Baby Glacier lies just to the east of the peak and Split Mountain is southeast. Mount Whitecap is the 30th tallest peak in Wyoming. Hazards. Encountering bears is a concern in the Wind River Range.

Geographic entities mentioned:
surface_form: mount whitecap
instance_of: Mountain
countries: United States
coordinates: lat: 43.1686
lon: -109.692
Laurel Mountain (Oregon). Laurel Mountain is the fourth highest peak in Oregon's Central Coast Range with an elevation of. The peak is located in Polk County west of the city of Dallas. In 1997 it was labeled the wettest place in Oregon, and in 1996 it set an all-time calendar year rainfall record for the contiguous United States with. Climate.

Geographic entities mentioned:
surface_form: laurel mountain (oregon)
instance_of: Mountain
countries: United States
coordinates: lat: 44.9235
lon: -123.573
surface_form: laurel mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.5803
lon: -118.891
Laurel Mountain (Oregon). Laurel Mountain is the fourth highest peak in Oregon's Central Coast Range with an elevation of. The peak is located in Polk County west of the city of Dallas. In 1997 it was labeled the wettest place in Oregon, and in 1996 it set an all-time calendar year rainfall record for the contiguous United States with. Climate.

Geographic entities mentioned:
surface_form: laurel mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.9235
lon: -123.573
surface_form: laurel mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.5803
lon: -118.891
Climate. Laurel Mountain has a hyperhumid maritime climate, on the border between Mediterranean (&quot;Csb&quot;), oceanic (&quot;Cfb&quot;) and subpolar oceanic (&quot;Cfc&quot;/&quot;Csc&quot;). Rainfall is extremely heavy between October and April, and even in the dry months of July and August fog is very frequent and prevents soils and vegetation from drying out appreciably.

Geographic entities mentioned:
surface_form: laurel mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.9235
lon: -123.573
surface_form: laurel mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.5803
lon: -118.891
In addition, a number of Rowing World Cup events have been won by New Zealanders. Rowing New Zealand is the governing body. Lake Karapiro in the Waikato and Lake Ruataniwha in the Mackenzie Basin are the two premier rowing venues in New Zealand. Karapiro hosted the 2010 World Rowing Championships. Sailing.

Geographic entities mentioned:
surface_form: Lake Karapiro
instance_of: Lake
countries: New Zealand
coordinates: lat: -37.943167
lon: 175.560833
surface_form: Lake Ruataniwha
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.281
lon: 170.071
Elbe-Saale. tdow3p8thhi5naqdrnwdm35tu9guz" xml:space="preserve">Elbe-Saale was a &quot;Verwaltungsgemeinschaft&quot; (&quot;collective municipality&quot;) in the district Salzlandkreis, in Saxony-Anhalt, Germany. It was situated on the left bank of the Elbe, around the confluence with the Saale. The seat of the &quot;Verwaltungsgemeinschaft&quot; was in Barby. It was disbanded on 1 January 2010.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
The trail starts at the western part of Gompers Park in Chicago (), and from there it continues north approximately to Glencoe (). The trail follows a path along the North Branch of the Chicago River, the Skokie River and the Skokie Lagoons. Along the path, trail users will find themselves passing through city streets and into quiet forests where the sounds of the city quickly fade away.

Geographic entities mentioned:
surface_form: Skokie Lagoons
instance_of: Lake
countries: United States
coordinates: lat: 42.101666666667
lon: -87.759166666667
A major construction push in 1976 resulted in a complete trail from Devon Ave to Winnetka Ave, and the completion of the Lake St overpass for $505,000. The abandoning of the Skokie Lagoons (Nike) missile base (constructed during the cold war) allowed the trail to be extended to Dundee Road. The stretch of trail north of Tower Rd follows the original service road to the launch complex.

Geographic entities mentioned:
surface_form: Skokie
instance_of: Lake
countries: United States
coordinates: lat: 42.101666666667
lon: -87.759166666667
Ray Cheney. Ray Cheney is a retired rugby union player and sportsman from Wales. Early years. Ray was born in Porth in the Rhondda. He showed exceptional all round sporting abilities and played football at Ton Pentre for Ton Pentre F.C. He also played Welsh Youth soccer, winning an international youth cap at centre forward and attracted the attention of Tottenham Hotspur FC.

Geographic entities mentioned:
surface_form: Rhondda
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
Upon his death in 1882, he left an endowment to support the kindergarten which later became the Hill Institute. Sojourner Truth, a former slave from the Hudson Valley in New York, moved to Florence in 1843 to become a member of the NAEI community. After the community dissolved in 1846, she bought a house on Park Street where she lived until 1857.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Becoming a shareholder, he attended two half-yearly meetings of the company in 1850, at each of which he moved that to the Sunday trains which were being regularly run passenger carriages should be attached. Cox took an active part in the Right of Way Association, and was one of the parties to the action against George Murray, 6th Duke of Atholl, by which Glen Tilt was reopened to the public.

Geographic entities mentioned:
surface_form: Glen Tilt
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.833
lon: -3.776
Early life. Adolph W. Schmidt was born in 1904 and raised in McKeesport, Pennsylvania. He was educated at Princeton University and Harvard Business School. He met his future wife, Helen &quot;Patsy&quot; Mellon (great-granddaughter of Thomas Mellon, founder of the Mellon Bank), during a fox hunt at the Rolling Rock Club in the Ligonier Valley. The two married in 1936. Military service.

Geographic entities mentioned:
surface_form: Ligonier Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.238
lon: -79.23
Filson Nunatak. Filson Nunatak () is a small nunatak east of Trost Peak in the eastern part of the Framnes Mountains, Mac. Robertson Land, Antarctica. It was photographed from Australian National Antarctic Research Expeditions (ANARE) aircraft in 1958 and seen by an ANARE party in December 1962. It was named by the Antarctic Names Committee of Australia for R.

Geographic entities mentioned:
surface_form: Trost Peak
instance_of: Mountain
coordinates: lat: -67.8667
lon: 62.8
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: filson nunatak
instance_of: Mountain
coordinates: lat: -67.8667
lon: 63.05
Filson Nunatak. Filson Nunatak () is a small nunatak east of Trost Peak in the eastern part of the Framnes Mountains, Mac. Robertson Land, Antarctica. It was photographed from Australian National Antarctic Research Expeditions (ANARE) aircraft in 1958 and seen by an ANARE party in December 1962. It was named by the Antarctic Names Committee of Australia for R.

Geographic entities mentioned:
surface_form: filson nunatak
instance_of: Mountain
coordinates: lat: -67.8667
lon: 63.05
Sétif offensive. The Sétif offensive was a two-week Algerian army offensive against the Salafist Group for Preaching and Combat (GSPC) near the Babor Mountains in Sétif province in September 2003. The armed forces at this time began a campaign to eliminate the remains of the Armed Islamic Group and the GSPC, which reportedly had 400 fighters.

Geographic entities mentioned:
surface_form: Babor Mountains
instance_of: Mountain
countries: Algeria
France
coordinates: lat: 36.55
lon: 5.4666666666667
In one of its most successful attacks in the Algerian Civil War, the Algerian People's National Army successfully killed 150 rebel militants of the GSPC. Algerian newspapers reported that 105 rebel corpses were found in caves near the Babor Mountains after an intense artillery bombardment.

Geographic entities mentioned:
surface_form: Babor Mountains
instance_of: Mountain
countries: Algeria
France
coordinates: lat: 36.55
lon: 5.4666666666667
Geography. The Rosenheim district is located in the foothills of the Alps, the Chiemgau. The landscape is dominated by moraines created by the Inn Glacier in the last glacial period, including many lakes. To the east of the district is the largest of these lakes, the Chiemsee. The main rivers in the district are the Inn and the Mangfall, which meet in the city of Rosenheim.

Geographic entities mentioned:
surface_form: Chiemsee
instance_of: Lake
countries: Germany
coordinates: lat: 47.89
lon: 12.47
Rabbit Lake (Temagami). Rabbit Lake (known as &quot; in Ojibway) is a lake in the Temagami region of Northeastern Ontario, Canada, and lies within the townships of Askin, Riddell, and Eldridge. The lake is the largest and southernmost in a chain of lakes including Cassels Lake, Snake Island Lake, and Obashkong Lake. Importance to First Nations.

Geographic entities mentioned:
surface_form: Cassels Lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.0667
lon: -79.7167
surface_form: Snake Island Lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.0642
lon: -79.7617
Rabbit Lake (Temagami). Rabbit Lake (known as &quot; in Ojibway) is a lake in the Temagami region of Northeastern Ontario, Canada, and lies within the townships of Askin, Riddell, and Eldridge. The lake is the largest and southernmost in a chain of lakes including Cassels Lake, Snake Island Lake, and Obashkong Lake. Importance to First Nations.

Geographic entities mentioned:
surface_form: rabbit lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.001
lon: -79.6385
This is most noticeable north of Rabbit Point, where the forest still has not fully grown back after nearly a century. On the western shore just north of Rabbit Point, lies a 491 hectare area that has never been touched by logging, and has become the Rabbit Lake West Conservation Reserve. The reserve is the least known and the most untouched of its kind in Ontario.

Geographic entities mentioned:
surface_form: rabbit lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.001
lon: -79.6385
This old growth stand is closer to the original Temagami Boreal forest than even the White Bear Forest to the north. Ecosystem. Like the other lakes in the region, Rabbit Lake is an oligotrophic ecosystem. While the fish population has steadily declined over the years, the lake is still home to pike, walleye, trout, whitefish, perch, bass, etc. Geology.

Geographic entities mentioned:
surface_form: rabbit lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.001
lon: -79.6385
Hollywood. Hollywood has also visited the lake when scenes from the James Cagney movie &quot;Captains of the Clouds&quot; were filmed at Matabitchuan Lodge, a wilderness lodge in the north-east bay, on Rabbit Lake. Props from the movie can be seen on display in the lodge. This movie was also the first Hollywood movie to be filmed entirely on location in Canada.

Geographic entities mentioned:
surface_form: rabbit lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.001
lon: -79.6385
Semizbughy (village). Geography. Semizbughy is located just below of the western slopes of Semizbughy mountain. to the east of the village lies Botakara, the district center.

Geographic entities mentioned:
surface_form: Semizbughy
instance_of: Mountain
countries: Kazakhstan
coordinates: lat: 50.196666666666665
lon: 74.8611111111111
Marla Glacier. Marla Glacier () is a glacier long and wide on the northeast side of Detroit Plateau on the southern Trinity Peninsula in Graham Land, Antarctica. Location. Marla Glacier is in Graham Land on the southeast coast of the Trinity Peninsula, which forms the tip of the Antarctic Peninsula. It is situated south of Aitkenhead Glacier and north of Diplock Glacier.

Geographic entities mentioned:
surface_form: Detroit Plateau
instance_of: Plateau
coordinates: lat: -64.1667
lon: -60
Kintla Glacier. Kintla Glacier is in Glacier National Park in the U.S. state of Montana. The glacier is situated on a plateau southwest of Kintla Peak at an elevation between and above sea level. The glacier has numerous crevasses and is actually two glaciers with a combined area of as of 2005, a 34 percent decrease in area from 1966.

Geographic entities mentioned:
surface_form: Kintla Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.9439
lon: -114.171
As such, along with the Aurès, it was one of the most affected areas because of the importance of the maquis (aided by the mountainous terrain) and the high levels of support and collaboration of its inhabitants for the nationalist cause. Several historic leaders of the FLN came from this region, including Hocine Aït Ahmed, Abane Ramdane, and Krim Belkacem.

Geographic entities mentioned:
surface_form: mountainous terrain
instance_of: Mountain
countries: Algeria
France
coordinates: lat: 36.7325
lon: 4.04972