Sarmila/GeoWiki-Features huggingface dataset:
Hoggar Mountains. The Hoggar Mountains (; Berber: &quot;idurar n Ahaggar&quot;) are a highland region in the central Sahara in southern Algeria, along the Tropic of Cancer. The mountains cover an area of approximately 550,000 km2. The Hoggar Mountains are home to the Ahaggar National Park.

Geographic entities mentioned:
surface_form: hoggar
instance_of: Plateau
countries: Algeria
France
coordinates: lat: 23.288611
lon: 5.534167
surface_form: ahaggar
instance_of: Plateau
countries: Algeria
France
coordinates: lat: 23.288611
lon: 5.534167
Assekrem is a famous and often visited point where Charles de Foucauld built a hermitage in 1911. The highlands are believed to be one of the main sources of the Tamanrasset River, an ancient river that flowed during the African humid period, and named after the main city near the Hoggar Mountains, Tamanrasset, built in a desert valley or wadi that was part of the ancient watercourse. Environment.

Geographic entities mentioned:
surface_form: hoggar
instance_of: Plateau
countries: Algeria
France
coordinates: lat: 23.288611
lon: 5.534167
Other plants may include &quot;Citrullus colocynthis&quot; and &quot;Calotropis procera&quot;. Slightly to the west of the Hoggar range, a population of the endangered African wild dog (&quot;Lycaon pictus&quot;) remained viable into the 20th century, but is now thought to be extirpated within this entire region.

Geographic entities mentioned:
surface_form: hoggar
instance_of: Plateau
countries: Algeria
France
coordinates: lat: 23.288611
lon: 5.534167
The Hoggar Mountains (; Berber: &quot;idurar n Ahaggar&quot;) are a highland region in the central Sahara in southern Algeria, along the Tropic of Cancer. The mountains cover an area of approximately 550,000 km2. The Hoggar Mountains are home to the Ahaggar National Park. The tallest peak in the range and Algeria, Mount Tahat, is located in the park area, which covers approximately. Geography.

Geographic entities mentioned:
surface_form: ahaggar
instance_of: Plateau
countries: Algeria
France
coordinates: lat: 23.288611
lon: 5.534167
Madone di Càmedo. The Madone di Càmedo is a mountain of the Swiss Lepontine Alps, overlooking Cevio in the canton of Ticino.

Geographic entities mentioned:
surface_form: madone
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.23861
lon: 8.91683
surface_form: madone di càmedo
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.330638888889
lon: 8.5636388888889
The house also displays a very high degree of historic integrity on both the exterior and interior, with only minor alterations since its construction in 1910. Martin Hill (1869–1939) and his orchard property surrounding the house were prominent in the development of the apple industry in the Hood River Valley.

Geographic entities mentioned:
surface_form: Hood River Valley
instance_of: Valley
countries: United States
coordinates: lat: 45.6
lon: -121.6
Strong winds, high temperatures, low humidity and extremely dry conditions caused the Peachland fire to grow quickly. By around 7:00 pm, it had reached 200 hectares and burned a path towards Okanagan Lake. At least 1,550 residents were evacuated from the fire zone; four houses and three outbuildings were destroyed.

Geographic entities mentioned:
surface_form: Okanagan Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.920833333333
lon: -119.5
Consequently, the lakes have not been completely filled since 1975, and had drained again just two years later. Environment. In good years, the Wimmera River fills Lake Hindmarsh to the south of the park, which overflows along Outlet Creek and then fills Lake Albacutya to the immediate south of the park.

Geographic entities mentioned:
surface_form: Lake Hindmarsh
instance_of: Lake
countries: Australia
coordinates: lat: -36.0667
lon: 141.917
surface_form: Lake Albacutya
instance_of: Lake
countries: Australia
coordinates: lat: -35.75
lon: 141.967
In 1958 he was transferred to the Pskov bishopric as parish priest of Saint Nicholas' church on the island of Talabsk (Zalit) in Pskov (Chudskoye) lake where he spent the remaining 44 years of his life, 40 as a priest, retiring at a very old age and settling at a humble wooden house nearby afterwards.

Geographic entities mentioned:
surface_form: Pskov (Chudskoye) lake
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
Etymology. The gorge gets its name from the village of Astrakí (el). Location. Astrakiano gorge is part of a larger geological complex known as the Juktas ecopark. It starts near the village of Peza and runs for about towards the north and parallel to Kounaviano gorge. The two gorges meet at Kaki Rachi near the village of Skalani (el), forming the Karteros gorge.

Geographic entities mentioned:
surface_form: Juktas
instance_of: Mountain
countries: Greece
coordinates: lat: 35.23994444444445
lon: 25.14413888888889
Korgalzhyn (lake). Korgalzhyn (;) is a lake in Korgalzhyn District, Akmola Region, Kazakhstan. Korgalzhyn is the main body of water of the Korgalzhyn group of lakes, which includes Birtaban, Sholakshalkar, Shalkar, Zhanybekshalkar, Uialyshalkar and Zhandyshalkar. Korgalzhyn is one of the main lakes of the Tengiz-Korgalzhyn Depression.

Geographic entities mentioned:
surface_form: Sholakshalkar
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.54722222222222
lon: 69.83555555555554
surface_form: korgalzhyn
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.5
lon: 69.5
surface_form: korgalzhyn
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.5
lon: 69.5
surface_form: shalkar
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.55
lon: 51.68333333
It is also an Important Bird Area and Ramsar site with its wetlands and mostly muddy waterways which are the breeding site of 318 bird species, including 22 endangered birds. Geography. Korgalzhyn is a lake that lies at the bottom of the large Tengiz-Korgalzhyn Depression, close to the southeast of larger Lake Tengiz. Lake Sholakshalkar lies to the east.

Geographic entities mentioned:
surface_form: Lake Tengiz
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.439722222222
lon: 68.9
surface_form: tengiz
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.439722222222
lon: 68.9
surface_form: tengiz
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.439722222222
lon: 68.9
surface_form: korgalzhyn
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.5
lon: 69.5
surface_form: korgalzhyn
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.5
lon: 69.5
Geography. Korgalzhyn is a lake that lies at the bottom of the large Tengiz-Korgalzhyn Depression, close to the southeast of larger Lake Tengiz. Lake Sholakshalkar lies to the east. The lake is shallow, with a maximum depth of. Most of it is covered by reeds, except for a few lobes in the northwest and northeast, Kokai, Sultankeldy and Isey, where the surface is relatively free of vegetation.

Geographic entities mentioned:
surface_form: Sholakshalkar
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.54722222222222
lon: 69.83555555555554
The lake bottom is flat and clayey, covered with dark grey silt. The Nura river flows into the eastern lakeshore from the northeast. During spring floods the overflow discharges into lake Tengiz from the northwestern end. River Kulanotpes flows along the western edge of Korgalzhyn.

Geographic entities mentioned:
surface_form: lake tengiz
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.439722222222
lon: 68.9
surface_form: tengiz
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.439722222222
lon: 68.9
The reed thickets also provide a habitat for the wild boar. Unlike barren neighboring lake Tengiz, Korgalzhyn is abundant in fish fauna. The main species in the lake are crucian carp, mirror carp, tench, ide, pike and perch.

Geographic entities mentioned:
surface_form: lake tengiz
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.439722222222
lon: 68.9
surface_form: tengiz
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.439722222222
lon: 68.9
surface_form: korgalzhyn
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.5
lon: 69.5
Korgalzhyn (;) is a lake in Korgalzhyn District, Akmola Region, Kazakhstan. Korgalzhyn is the main body of water of the Korgalzhyn group of lakes, which includes Birtaban, Sholakshalkar, Shalkar, Zhanybekshalkar, Uialyshalkar and Zhandyshalkar. Korgalzhyn is one of the main lakes of the Tengiz-Korgalzhyn Depression. The lake is part of the Korgalzhyn Nature Reserve, a protected area.

Geographic entities mentioned:
surface_form: tengiz
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.439722222222
lon: 68.9
surface_form: korgalzhyn
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.5
lon: 69.5
surface_form: korgalzhyn
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.5
lon: 69.5
Korgalzhyn (lake). Korgalzhyn (;) is a lake in Korgalzhyn District, Akmola Region, Kazakhstan. Korgalzhyn is the main body of water of the Korgalzhyn group of lakes, which includes Birtaban, Sholakshalkar, Shalkar, Zhanybekshalkar, Uialyshalkar and Zhandyshalkar. Korgalzhyn is one of the main lakes of the Tengiz-Korgalzhyn Depression.

Geographic entities mentioned:
surface_form: korgalzhyn
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.5
lon: 69.5
Korgalzhyn (lake). Korgalzhyn (;) is a lake in Korgalzhyn District, Akmola Region, Kazakhstan. Korgalzhyn is the main body of water of the Korgalzhyn group of lakes, which includes Birtaban, Sholakshalkar, Shalkar, Zhanybekshalkar, Uialyshalkar and Zhandyshalkar. Korgalzhyn is one of the main lakes of the Tengiz-Korgalzhyn Depression.

Geographic entities mentioned:
surface_form: korgalzhyn
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.5
lon: 69.5
surface_form: korgalzhyn
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.5
lon: 69.5
Korgalzhyn is one of the main lakes of the Tengiz-Korgalzhyn Depression. The lake is part of the Korgalzhyn Nature Reserve, a protected area. It is also an Important Bird Area and Ramsar site with its wetlands and mostly muddy waterways which are the breeding site of 318 bird species, including 22 endangered birds. Geography.

Geographic entities mentioned:
surface_form: korgalzhyn
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.5
lon: 69.5
The Nura river flows into the eastern lakeshore from the northeast. During spring floods the overflow discharges into lake Tengiz from the northwestern end. River Kulanotpes flows along the western edge of Korgalzhyn. The water of the lake is fresh near the mouth of the Nura, becoming increasingly brackish towards the northern sector. Flora and fauna.

Geographic entities mentioned:
surface_form: korgalzhyn
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.5
lon: 69.5
Flora and fauna. There are large reed beds scattered on mud islands almost completely covering the southern part with a mesh of open channels and ponds in between. Owing to these mud islands Korgalzhyn is an important wetland site for migratory water birds, such as different species of gulls, terns, ducks and grebes, including the northernmost colony of greater flamingo.

Geographic entities mentioned:
surface_form: korgalzhyn
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.5
lon: 69.5
The music video was filmed in Iceland, with Surtshellir Cave on the first day, Hekla Mountain on the second day, and Hjörleifshöfði on the third and final day. Accompanying the music video is a game for mobile titled &quot;The Storm - Interactive&quot;, where one can play through the story of the video.

Geographic entities mentioned:
surface_form: Hjörleifshöfði
instance_of: Mountain
countries: Iceland
coordinates: lat: 63.41666667
lon: -18.76666667
Other activities are the Chimac 99 toast time (an event held at 9:09pm where all the participants toast together), Chimac Cooking Competition, Chimac Ice Pub and Chimac busking. Participants and visitors also visit the nearby attractions like Palgongsan Mountain cable car, Modern Cultural Street and Seomun market. Bonghwa Eun-uh (Sweetfish) Festival.

Geographic entities mentioned:
surface_form: Palgongsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 36.016944444444
lon: 128.695
Popular events include selecting ginseng seeds to harvesting ginseng, ginseng footbath to ginseng cooking contest, making medicine using ginseng to traditional massage and more. Visitors also go to the nearby tourist spot such as Garden of Sky and Daedunsan Provincial Park while returning from the festival. Songi Mushroom Festival.

Geographic entities mentioned:
surface_form: Daedunsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 36.12
lon: 127.32333333
Jinan Red Ginseng Festival. The festival is held in the beginning of October every year in the Northern area of Maisan in Jinan County, North Jeolla Province. Jinan in Korea is a designated special district for the production of Hangsam (Hangeul:홍삼), red ginseng. This festival is designed to spread awareness and knowledge about red ginseng.

Geographic entities mentioned:
surface_form: Maisan
instance_of: Mountain
countries: South Korea
coordinates: lat: 35.76111111
lon: 127.41222222
&quot;Rage and Discipline&quot; received a favorable review from Ronnie Scheib of &quot;Variety&quot; and an Honorable Mention at the African Diaspora Film Festival. Clyde went on to direct two more feature films for Roger Corman and then completed &quot;Growing&quot;, a feature-length documentary about small, sustainable farms in the Hudson Valley region of New York State.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
WDWN. WDWN (89.1 FM) is a college radio station broadcasting an Alternative format. Licensed to Auburn, New York, United States, the station serves the Finger Lakes area. The station is owned by Cayuga County Community College. The station is also broadcast on HD radio.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
Hotine Glacier. Hotine Glacier () is a glacier long which is divided at its mouth by Mount Cloos, flowing west into both Deloncle Bay and Girard Bay on Kyiv Peninsula, on the west coast of Graham Land, Antarctica.

Geographic entities mentioned:
surface_form: Mount Cloos
instance_of: Mountain
coordinates: lat: -65.1167
lon: -63.95
Southwest Waterfront is bounded by Interstate 395 to the north, Washington Channel to the west, the Anacostia River to the south, and South Capitol Street to the east. Politically, Southwest Waterfront lies in Ward 6. History. Southwest Waterfront is part of Pierre L'Enfant's original city plans.

Geographic entities mentioned:
surface_form: Washington Channel
instance_of: Watercourse
countries: United States
coordinates: lat: 38.8787232
lon: -77.0271988
Carrollsburg was completed in 1967 and developed as a companion piece to Tiber Island by the same architects. In 1968, the Titanic Memorial was moved to the Washington Channel, near Fort McNair in Southwest Waterfront. The Washington Metro built the Waterfront Metro station on its Green Line and opened it in 1991.

Geographic entities mentioned:
surface_form: Washington Channel
instance_of: Watercourse
countries: United States
coordinates: lat: 38.8787232
lon: -77.0271988
Vetrovala Peak. l3u03oejrkt999bjmxapb2v6inqo" xml:space="preserve">#redirect Mount Daynes

Geographic entities mentioned:
surface_form: vetrovala peak
instance_of: Mountain
coordinates: lat: -64.2019
lon: -59.1053
Royal Muskoka Hotel. The Royal Muskoka Hotel was a luxury summer resort hotel that operated from 1901 to 1952 on Lake Rosseau in Ontario's Muskoka region. The hotel was built by the Muskoka Lakes Navigation Company and was serviced by its steamers.

Geographic entities mentioned:
surface_form: Lake Rosseau
instance_of: Lake
countries: Canada
coordinates: lat: 45.18333333333333
lon: -79.6
Some of these buildings have disappeared and others have been covered by jungle for about 3,000 years, unexplored. Pijijiapan and Izapa are on the Pacific coast and were the most important pre Hispanic cities for about 1,000 years, as the most important commercial centers between the Mexican Plateau and Central America.

Geographic entities mentioned:
surface_form: Mexican Plateau
instance_of: Plateau
countries: Mexico
coordinates: lat: 24
lon: -103
Shuswap Country. The Shuswap Country, or simply the Shuswap (pronounced /ˈʃuːʃwɑːp/) and called Secwepemcúl̓ecw in Secwepemctsín, is a term used in the Canadian province of British Columbia to refer to the environs of Shuswap Lake.

Geographic entities mentioned:
surface_form: Shuswap Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.000693
lon: -119.01263
Roughly defined, the Shuswap Country begins on its west at the town of Chase, located on Little Shuswap Lake, west of which is the South Thompson area of the Thompson Country, and includes Adams Lake to the northwest of Shuswap Lake as well as communities in the Eagle River area as far as Craigellachie and/or Three Valley Gap, which is at the summit of Eagle Pass, beyond which eastwards is the Columbia Country.

Geographic entities mentioned:
surface_form: Little Shuswap Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.84861111111111
lon: -119.6438888888889
surface_form: Adams Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.169444444444444
lon: -119.57083333333334
Many small-holders are organized in cooperative societies. Large dairy processing plants are nearby in Nakuru Town and even export-grade cheese is being made by several firms in the area. Fishing is practiced in Lake Naivasha, a fresh-water lake of 145 km2. There are three landing beaches and over one hundred boats. Fishing is regulated to ensure sustainability.

Geographic entities mentioned:
surface_form: Lake Naivasha
instance_of: Lake
countries: Kenya
coordinates: lat: -0.76852777777778
lon: 36.350644444444
History of Oregon State University. Oregon State University was founded as a small secondary and college preparatory school in the center of Oregon's Willamette Valley in 1856. The early school was first known as Corvallis Academy and served as the first public college in the American Northwest - known then as the Oregon Territory.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
They nominally had an academic mission, to research the spread of animal species between islands, but in reality they intended to &quot;run away to the South Seas&quot; and never return home. The couple arrived at Fatu Hiva in 1937, in the valley of Omo‘a.

Geographic entities mentioned:
surface_form: Omo‘a
instance_of: Valley
countries: France
coordinates: lat: -10.512222222222
lon: -138.68277777778
Synopsis. In the Book of Mormon, Moroni is the son of Mormon. Moroni shares a name with Captain Moroni, a much earlier Book of Mormon figure, of whom Mormon wrote highly. Moroni works under his father, the commander in chief of a Nephite army, who battles against the Lamanites. Upon the Nephites' defeat at Cumorah, Moroni goes into hiding to avoid being killed by the Lamanites.

Geographic entities mentioned:
surface_form: Cumorah
instance_of: Mountain
countries: United States
coordinates: lat: 43.0062
lon: -77.224
Yangchenghu South station. Yangchenghu South station () is the North-Eastern terminus of Line 5 of the Suzhou Metro. The station is located in Suzhou Industrial Park, Suzhou, Jiangsu Province. It has been in use since June 29, 2021, when Line 5 opened to the public, and is located on the south bank of Yangcheng Lake.

Geographic entities mentioned:
surface_form: Yangcheng Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 31.066666666667
lon: 120.13333333333
Taurikura. Taurikura is a small, rural township in the Whangarei District, approximately south east of Whangārei city in Northland, New Zealand. The town is located on the shores of Calliope Bay at the base of Mount Manaia which, along with Bream Head and the Hen Island, collectively form the ancient remnants of a very large andesitic volcano.

Geographic entities mentioned:
surface_form: Mount Manaia
instance_of: Mountain
countries: New Zealand
coordinates: lat: -35.818309
lon: 174.516985
The Helmet (British Columbia). The Helmet is a subsidiary peak on the Mount Robson massif located within Mount Robson Provincial Park in British Columbia, Canada. It is part of the Rainbow Range which is a sub-range of the Canadian Rockies.

Geographic entities mentioned:
surface_form: Mount Robson
instance_of: Mountain
countries: Canada
coordinates: lat: 53.11055555555556
lon: -119.15666666666667
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: the helmet
instance_of: Mountain
countries: Canada
coordinates: lat: 53.115
lon: -119.14166666666667
surface_form: mount robson
instance_of: Mountain
countries: Canada
coordinates: lat: 53.11055555555556
lon: -119.15666666666667
The Helmet (British Columbia). The Helmet is a subsidiary peak on the Mount Robson massif located within Mount Robson Provincial Park in British Columbia, Canada. It is part of the Rainbow Range which is a sub-range of the Canadian Rockies.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: the helmet (british columbia)
instance_of: Mountain
countries: Canada
coordinates: lat: 53.115
lon: -119.14166666666667
Pyramid Mountain (Clallam County, Washington). Pyramid Mountain is located high above Lake Crescent's north shore. Once known as Sugarloaf Mountain, it received its present name in 1928. It has a restored Aircraft Warning Service lookout at the summit, which was used to watch for enemy aircraft during World War Two. It dominates the view from Barnes Point and Lake Crescent Lodge.

Geographic entities mentioned:
surface_form: Lake Crescent
instance_of: Lake
countries: United States
coordinates: lat: 48.0595755
lon: -123.8291037
surface_form: pyramid
instance_of: Lake
countries: United States
coordinates: lat: 40.033333333333
lon: -119.56666666667
surface_form: pyramid mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.0748
lon: -123.807
Pyramid Mountain is located high above Lake Crescent's north shore. Once known as Sugarloaf Mountain, it received its present name in 1928. It has a restored Aircraft Warning Service lookout at the summit, which was used to watch for enemy aircraft during World War Two. It dominates the view from Barnes Point and Lake Crescent Lodge. It is accessible by trail from the Spruce Railroad Trail.

Geographic entities mentioned:
surface_form: Barnes Point
instance_of: Landform
countries: United States
coordinates: lat: 48.0611
lon: -123.796
It dominates the view from Barnes Point and Lake Crescent Lodge. It is accessible by trail from the Spruce Railroad Trail. On a clear day, Mount Baker is visible in the Cascade Range across the Puget Sound. From the summit, it is easy to see the landslide that blocked Indian Creek and dammed Lake Crescent. Below the landslide is Lake Sutherland and the Indian Creek valley down to the Elwha River.

Geographic entities mentioned:
surface_form: Mount Baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
It is accessible by trail from the Spruce Railroad Trail. On a clear day, Mount Baker is visible in the Cascade Range across the Puget Sound. From the summit, it is easy to see the landslide that blocked Indian Creek and dammed Lake Crescent. Below the landslide is Lake Sutherland and the Indian Creek valley down to the Elwha River. Climate.

Geographic entities mentioned:
surface_form: Lake Sutherland
instance_of: Lake
countries: United States
coordinates: lat: 48.0779116
lon: -123.7085698
Pyramid Mountain (Clallam County, Washington). Pyramid Mountain is located high above Lake Crescent's north shore. Once known as Sugarloaf Mountain, it received its present name in 1928. It has a restored Aircraft Warning Service lookout at the summit, which was used to watch for enemy aircraft during World War Two. It dominates the view from Barnes Point and Lake Crescent Lodge.

Geographic entities mentioned:
surface_form: pyramid
instance_of: Lake
countries: United States
coordinates: lat: 40.033333333333
lon: -119.56666666667
surface_form: pyramid mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.0748
lon: -123.807
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Below the landslide is Lake Sutherland and the Indian Creek valley down to the Elwha River. Climate. Set in the north-west portion of the Olympic Mountains, Pyramid 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 Olympic Mountains.

Geographic entities mentioned:
surface_form: pyramid
instance_of: Lake
countries: United States
coordinates: lat: 40.033333333333
lon: -119.56666666667
surface_form: pyramid mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.0748
lon: -123.807
Pyramid Mountain (Clallam County, Washington). Pyramid Mountain is located high above Lake Crescent's north shore. Once known as Sugarloaf Mountain, it received its present name in 1928. It has a restored Aircraft Warning Service lookout at the summit, which was used to watch for enemy aircraft during World War Two. It dominates the view from Barnes Point and Lake Crescent Lodge.

Geographic entities mentioned:
surface_form: sugarloaf mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.0748
lon: -123.807
surface_form: sugarloaf mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.6781
lon: -113.051
surface_form: sugarloaf mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.068611111111
lon: -74.926944444444
She then became a children's illustrator for Whitman Publishing as well worked as a greetings card designer for &quot;MacMillan's Readers&quot; and Chryston Limited Edition. During the 1950s, she purchased three and a half acres within the San Fernando Valley in which she constructed two houses and an office on Ventura Boulevard.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Orson Pratt, a member of the Quorum of the Twelve Apostles and contemporary of Smith, expressed his belief that more prophecies from Zenock were contained in additional ancient plates hidden in the hill Cumorah to someday be recovered and revealed by what he believed would be the will of God.

Geographic entities mentioned:
surface_form: Cumorah
instance_of: Mountain
countries: United States
coordinates: lat: 43.0062
lon: -77.224
Overview. Ranchi district is a part of the Ranchi plateau, most of it at an average elevation of 2,140 feet above sea level. Only a small portion in the north-eastern part of the district is the lower Ranchi plateau, spread over Silli, Rahe, Sonahatu and Tamar CD blocks, at an elevation of 500 to 1,000 feet above sea level. There is a 16 km long ridge south-west of Ranchi.

Geographic entities mentioned:
surface_form: Ranchi plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
It marks the end of the festivities. Open air theater. Yenya is also the season of open air theatre productions. Performances depicting social themes, satire and comedy are held on dance platforms or makeshift stages at market squares all over the Kathmandu Valley on the sidelines of the sacred festival. The plays, known as Dabu Pyākhan (दबू प्याखं), have a history going back centuries.

Geographic entities mentioned:
surface_form: Kathmandu Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
Data published by the Unification Ministry of the Republic of Korea stated that since 1948, there has been a difference of opinion between North Korea and China due to the problem of taking over Paektu Mountain.

Geographic entities mentioned:
surface_form: Paektu Mountain
instance_of: Mountain
countries: North Korea
People's Republic of China
coordinates: lat: 41.992777777778
lon: 128.07722222222
Jacob's Creek. Jacob's Creek is an Australian wine brand that is exported to over 60 countries. It is produced by Pernod Ricard in the small township of Rowland Flat in the Barossa Valley. In 1847, Johann Gramp, the founder of Orlando Wines, planted some of the first grape vines in the Barossa Valley along the banks of Jacob's Creek.

Geographic entities mentioned:
surface_form: Barossa Valley
instance_of: Valley
countries: Australia
coordinates: lat: -34.533333333333
lon: 138.95
She was elected to the National Assembly in 2017. Miss Ecuador 2010. Galarza was a student of Psychology in the Pontificia Universidad Cátolica del Ecuador. She is also the first woman from Tungurahua to be crowned Miss World Ecuador. Miss Ecuador 2010 was broadcast live from CEMEXPO, in Quito. Miss World 2010.

Geographic entities mentioned:
surface_form: Tungurahua
instance_of: Mountain
countries: Ecuador
coordinates: lat: -1.4669444444444
lon: -78.441666666667
Since the 2011 local government reform it is part of the municipality Aigialeia, of which it is a municipal unit. The municipal unit has an area of 98.710 km2. Its seat of administration was in the village of Lampiri. Erineos stretches between the northeastern slopes of the Panachaiko mountain and the Gulf of Corinth. The river Foinikas (Phoenix) (or Salmenikos) flows through the municipality.

Geographic entities mentioned:
surface_form: Panachaiko
instance_of: Mountain
countries: Greece
coordinates: lat: 38.2025
lon: 21.868888888889
Career. Like many others men of this period, Morofuyu began his career in 1336, at the end of the Kenmu Restoration. He fought many battles all over the country, including 1336's attack to Mount Hiei. In 1338, together with cousin Moroyasu, he went to fight against Southern Court forces in Aonohara, Mino Province, to help contain Kitabatake Akiie, who was threatening Kyoto.

Geographic entities mentioned:
surface_form: Mount Hiei
instance_of: Mountain
countries: Japan
coordinates: lat: 35.066666666667
lon: 135.83833333333
The mountain is surrounded by several other notable mountains including Skarvflytindene to the northeast, Leirungstinden to the east, Leirungskampen to the southeast, Kvitskardtinden and Mesmogtinden to the southwest, Store Svartdalspiggen to the west, and Nordre Knutsholstinden and Store Knutsholstinden to the northwest. Name.

Geographic entities mentioned:
surface_form: Skarvflytindene
instance_of: Mountain
countries: Norway
coordinates: lat: 61.443742
lon: 8.586625
surface_form: Leirungstinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.42171
lon: 8.60059
surface_form: Leirungskampen
instance_of: Mountain
countries: Norway
coordinates: lat: 61.39573
lon: 8.60128
surface_form: Kvitskardtinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.39638889
lon: 8.55388889
surface_form: Mesmogtinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.40388889
lon: 8.53416667
surface_form: Store Svartdalspiggen
instance_of: Mountain
countries: Norway
coordinates: lat: 61.4169
lon: 8.51278
surface_form: Nordre Knutsholstinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.43625
lon: 8.55491
surface_form: Store Knutsholstinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.429444444444
lon: 8.5702777777778
surface_form: knutsholstinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.43625
lon: 8.55491
surface_form: knutsholstinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.43625
lon: 8.55491
surface_form: knutsholstinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.41841
lon: 8.57373
surface_form: knutsholstinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.41841
lon: 8.57373
surface_form: svartdalspiggen
instance_of: Mountain
countries: Norway
coordinates: lat: 61.4169
lon: 8.51278
Vesle Knutsholstinden. Vesle Knutsholstinden is a mountain in Vågå Municipality in Innlandet county, Norway. The tall mountain is located in the Jotunheimen mountains within Jotunheimen National Park. The mountain sits about southwest of the village of Vågåmo and about northwest of the village of Beitostølen.

Geographic entities mentioned:
surface_form: knutsholstinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.43625
lon: 8.55491
surface_form: knutsholstinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.41841
lon: 8.57373
surface_form: vesle knutsholstinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.41841
lon: 8.57373
Loess Plateau. The Loess Plateau is a plateau in north-central China formed of loess, a clastic silt-like sediment formed by the accumulation of wind-blown dust. It is located southeast of the Gobi Desert and is surrounded by the Yellow River. It includes parts of the Chinese provinces of Qinghai, Gansu, Shaanxi and Shanxi.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
It includes parts of the Chinese provinces of Qinghai, Gansu, Shaanxi and Shanxi. The depositional setting of the Chinese Loess Plateau was shaped by the tectonic movement in the Neogene period, after which strong southeast winds caused by the East Asian Monsoon transported sediment to the plateau during the Quaternary period.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
The depositional setting of the Chinese Loess Plateau was shaped by the tectonic movement in the Neogene period, after which strong southeast winds caused by the East Asian Monsoon transported sediment to the plateau during the Quaternary period. The three main morphological types in the Loess Plateau are loess platforms, ridges and hills, formed by the deposition and erosion of loess.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Most of the loess comes from the Gobi Desert and other nearby deserts. The sediments were transported to the Loess Plateau during interglacial periods by southeasterly prevailing winds and winter monsoon winds. After the deposition of sediments on the plateau, they were gradually compacted to form loess under the arid climate.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
After the deposition of sediments on the plateau, they were gradually compacted to form loess under the arid climate. The Loess Plateau is one of the largest and thickest loess plateaus in the world. Its 635,000 km2 area corresponds to around 6.6% of the land area in China. Around 108 million people inhabit the Loess Plateau.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
The Loess Plateau is one of the largest and thickest loess plateaus in the world. Its 635,000 km2 area corresponds to around 6.6% of the land area in China. Around 108 million people inhabit the Loess Plateau. Because of the strong winds, erosion is also powerful across the plateau. Therefore, erosional features, including wind escarpments, loess vertical joints and gullies are present.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
These changes may relate to human development in the plateau; Chinese environmental officials are trying to find sustainable ways to manage the region. Geomorphology. There are three main types of morphology in the Loess Plateau. They are loess platform, loess ridges, and loess hills. Loess tableland is flat and with many loess strata. It is mostly located at south Loess Plateau.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Geomorphology. There are three main types of morphology in the Loess Plateau. They are loess platform, loess ridges, and loess hills. Loess tableland is flat and with many loess strata. It is mostly located at south Loess Plateau. Loess ridges are formed by erosion and are located at the central Loess Plateau. Loess Hills are conical dunes and are located at the north Loess Plateau.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
They are loess platform, loess ridges, and loess hills. Loess tableland is flat and with many loess strata. It is mostly located at south Loess Plateau. Loess ridges are formed by erosion and are located at the central Loess Plateau. Loess Hills are conical dunes and are located at the north Loess Plateau. The geomorphology of the Loess Plateau is formed by the erosion and deposition of loess.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Loess ridges are formed by erosion and are located at the central Loess Plateau. Loess Hills are conical dunes and are located at the north Loess Plateau. The geomorphology of the Loess Plateau is formed by the erosion and deposition of loess. In the Loess Plateau, the geomorphology usually changes from rocky mountains to Alluvial plain at piedmont to river valley belt.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Loess Hills are conical dunes and are located at the north Loess Plateau. The geomorphology of the Loess Plateau is formed by the erosion and deposition of loess. In the Loess Plateau, the geomorphology usually changes from rocky mountains to Alluvial plain at piedmont to river valley belt. This pattern keeps repeating from the Northwest to the Southeast of the Loess Plateau.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
The geomorphology of the Loess Plateau is formed by the erosion and deposition of loess. In the Loess Plateau, the geomorphology usually changes from rocky mountains to Alluvial plain at piedmont to river valley belt. This pattern keeps repeating from the Northwest to the Southeast of the Loess Plateau. The height of the rocky mountains is much higher than the loess deposit.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
The height of the rocky mountains is much higher than the loess deposit. The height and morphology of the mountains are different in different locations. One of the highest mountains in the Loess Plateau is called Mahan Mountain. The elevation of this mountain is around, which is higher than the loess line. It is a flat-topped mountain and has paleo-peneplain remnants on the mountain top.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
These flat river basins, which include valley flat and lower terraces, are important for construction and agricultural activities. Wind escarpment and bedrock ridges. Mu Us Desert is located in the northwest of the Loess Plateau. Wind escarpment in the Loess Plateau marks a boundary between Mu Us Desert and the Loess Plateau.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Wind escarpment and bedrock ridges. Mu Us Desert is located in the northwest of the Loess Plateau. Wind escarpment in the Loess Plateau marks a boundary between Mu Us Desert and the Loess Plateau. It also represents a transition from loess accumulation to wind erosion in the Loess Plateau. Many linear bedrock ridges are formed behind the wind escarpment, which are parallel to the wind direction.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Wind escarpment and bedrock ridges. Mu Us Desert is located in the northwest of the Loess Plateau. Wind escarpment in the Loess Plateau marks a boundary between Mu Us Desert and the Loess Plateau. It also represents a transition from loess accumulation to wind erosion in the Loess Plateau. Many linear bedrock ridges are formed behind the wind escarpment, which are parallel to the wind direction.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
It also represents a transition from loess accumulation to wind erosion in the Loess Plateau. Many linear bedrock ridges are formed behind the wind escarpment, which are parallel to the wind direction. In the northern Loess Plateau, the bedrock ridges are pointing towards the northeast. However, the direction of the ridges slowly rotates to the North in the central Loess Plateau.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
In the northern Loess Plateau, the bedrock ridges are pointing towards the northeast. However, the direction of the ridges slowly rotates to the North in the central Loess Plateau. At North Loess Plateau, the ridges are oriented 118° ±14° while they are oriented 179° ± 11° at central Loess Plateau. This indicates the role of wind erosion.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Therefore, modern windstorms also contribute to shaping the eolian geomorphology. The Yellow River has provided sediments supply continuously which has been reworked by wind. Also, the wind erosion becomes stronger when it reaches the Loess Plateau wind escarpment. Because of the streamline compression of the wind escarpment, the wind speed is increased.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Also, the wind erosion becomes stronger when it reaches the Loess Plateau wind escarpment. Because of the streamline compression of the wind escarpment, the wind speed is increased. As a result, the Loess Plateau is not only a site of loess deposition but also a source of dust because of strong wind erosion. Wind erosion is very severe during the glacial period.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Vertical development features. Vertically, joints can be found in different loess strata, including late, middle and early Pleistocene loess layers. It is one of the most significant structures of the Loess Plateau. The development and size of the vertical loess joints depend on the vegetation coverage and slope. Steep slope and poor vegetation coverage favor the development of the joints.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
The water from rainfall and irrigation will infiltrate into the loess strata through the vertical joint surface and pore concentration zone. The joint systems in the loess strata are of different sizes, properties, periods, and origins. Loess Vertical Joints distribute all over the loess plateau. The joints in landslides can be categorized by their different features.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Gullies. Gully erosion acts as an important source for sediments. If an area has gully erosion, it means that the area has serious land degradation. In the Loess Plateau, the contribution of gully erosion on total sediment production in the hilly areas is about 60% to 90%. It is serious in the Loess Plateau. To know the contribution of gully erosion, we can measure the gully volume changes.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
It is serious in the Loess Plateau. To know the contribution of gully erosion, we can measure the gully volume changes. There are three types of gullies in the Loess Plateau, including floor gullies, hill slope gullies and valley bank gullies. Geological development. In conclusion, the geomorphic outline of the Loess Plateau was shaped by the tectonic movement since Neogene.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
There are three types of gullies in the Loess Plateau, including floor gullies, hill slope gullies and valley bank gullies. Geological development. In conclusion, the geomorphic outline of the Loess Plateau was shaped by the tectonic movement since Neogene. After that, because of the East Asia Monsoon in Quaternary, the loess and different erosional features started to form.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Geological development. In conclusion, the geomorphic outline of the Loess Plateau was shaped by the tectonic movement since Neogene. After that, because of the East Asia Monsoon in Quaternary, the loess and different erosional features started to form. However, because of human activities, many areas in the Loess Plateau turned into erosional environments. Formation of loess.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Around 6% of the land in the world is covered with loess. Loess record the past climate and environment. The Chinese Loess Plateau is one of the largest sinks of loess in the world. When the sediments are transported to the Loess Plateau, they are silt materials. After they deposit in arid areas and under strong chemical weathering and the process of carbonation, loess is formed.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Loess record the past climate and environment. The Chinese Loess Plateau is one of the largest sinks of loess in the world. When the sediments are transported to the Loess Plateau, they are silt materials. After they deposit in arid areas and under strong chemical weathering and the process of carbonation, loess is formed. Two types of loess are defined by their formation process.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667