Sarmila/GeoWiki-Features huggingface dataset:
Range. The Congo blind barb is found only in the Thysville Cave system, a part of the lower Congo River basin (notably Kwilu and Inkisi tributaries) in the Democratic Republic of the Congo. The area where it is found covers about, and is located at an altitude around above sea level.

Geographic entities mentioned:
surface_form: Inkisi
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: -8.52882
lon: 22.52485
At that same regatta she won a silver medal in a coxless pair with Natalie Bale. Six years later she won a bronze medal in a coxless pair with Kate Hornsey at the 2011 World Rowing Championships in Lake Bled. Tait was picked as captain of the Australian women's rowing team at the 2008 and 2012 Olympic Games, and at the 2010 and 2011 World Rowing Championships.

Geographic entities mentioned:
surface_form: Lake Bled
instance_of: Lake
countries: Slovenia
coordinates: lat: 46.364444444444
lon: 14.094722222222
Lakenenland. Lakenenland is a sculpture park located in Chocolay Township, Michigan. The park was founded in 2003, when artist Tom Lakenen moved his collection of scrap iron sculptures from his yard to a plot of land near the Lake Superior coast. Lakenenland contains more than 80 sculptures in the creator's &quot;junkyard art&quot; style. Description.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
He was born on 5 November 1912 in Lubongo Village, Nkokonjeru, Buikwe District, in southeast Uganda. His parents, Matayo Nandibijjo Lulume and Alistera Mbakolere hailed from the Buvuma Islands in Lake Victoria, but had relocated to the mainland during the sleeping sickness epidemic at the beginning of the 20th century. He was baptized in the Catholic faith on 5 December 2012.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
He first starts gambling to make money to buy her a sewing machine, and even encourages her remarriage with local photographer Dae-ho (Lee Ki-young). What Goni doesn't know, however, is that his stepfather used to be Jirisan's notorious swindler and that Goni's best friend Young-min (Kim Min-jun) is actually plotting against Dae-ho.

Geographic entities mentioned:
surface_form: Jirisan
instance_of: Mountain
countries: South Korea
coordinates: lat: 35.336944444444
lon: 127.73055555556
Across 48th is the territorial visitors' centre, with the entrance roads of the Prince of Wales Northern Heritage Centre and Northwest Territories Legislative Building to their west, set amongst more taiga, and Frame Lake to the south. A paved driveway leads north into an unpaved parking lot from 49th. On a slope at the north end of the lot stands inuksuk.

Geographic entities mentioned:
surface_form: Frame Lake
instance_of: Lake
countries: Canada
coordinates: lat: 62.454
lon: -114.39
After a brief pause during the years of World War II, the growth continued in the 1950s, with the New Town being built to augment the Old Town, the original, more rustic city, on the peninsula leading into Great Slave Lake.

Geographic entities mentioned:
surface_form: Great Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 61.666666666667
lon: -114
Russian frigate Oryol (1668). &quot;Oryol&quot; () was a frigate that served in the Russian Navy. It was commissioned by Tsar Alexis I to protect Russian trading ships on the Caspian Sea and became the first Russian-built warship. The ship was built between 1667 and 1669 by the developing shipyard in Dedinovo on the Oka River.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Construction. During the 17th century, Russia and Persia developed closer commercial ties, exchanging extravagant embassies and trading in cloth, silk, and other goods. Shipping was conducted across the Caspian Sea and through the Volga River, with Astrakhan as commercial center.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
The lake shrank in size, and the dried-up area was converted into farmland. The &quot;Jiajing Pei County Annals&quot; (嘉靖 沛县志) described it during this period as only 10 &quot;li&quot; long; it said the lake's beauty was comparable to that of Little West Lake and that it was considered one of the &quot;eight scenic spots&quot; of Pei County.

Geographic entities mentioned:
surface_form: Little West Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 28.145
lon: 106.858
surface_form: west lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 30.2375
lon: 120.14083333333
surface_form: little west lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 28.145
lon: 106.858
surface_form: west lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 23.67277778
lon: 116.63861111
surface_form: west lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 32.404051
lon: 119.420786
surface_form: west lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 23.09444444
lon: 114.39722222
Nansi Lake. Nansi Lake (), or Weishan Lake, administrated by Weishan County and located in Shandong Province in China, is the largest freshwater lake in the north of the country. It consists of four connected lakes: Weishan (), Zhaoyang (), Nanyang (), Dushan (). It is 120 km long and 1266 square km in area. Early records: Zhaoyang Lake alone.

Geographic entities mentioned:
surface_form: dushan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 33.070277777778
lon: 112.58638888889
It was also used to store water for canal transportation. Confusingly, contemporary sources also refer to Dushan Lake as Nanyang Lake, after the nearby town of Nanyang (20 km northeast of present-day Yutai County), although according to Han Zhaoqing, the contemporary descriptions of this lake's location match today's Dushan Lake rather than today's Nanyang Lake.

Geographic entities mentioned:
surface_form: dushan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 33.070277777778
lon: 112.58638888889
surface_form: dushan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 33.070277777778
lon: 112.58638888889
Moreover, several contemporary sources also identify Dushan and Nanyang as alternate names for the same lake, with Dushan coming from the nearby Dushan hills. The first definite mention of today's Nanyang Lake is in 1746, when it and Dushan Lake are mentioned as separate lakes.

Geographic entities mentioned:
surface_form: dushan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 33.070277777778
lon: 112.58638888889
surface_form: dushan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 33.070277777778
lon: 112.58638888889
Moreover, several contemporary sources also identify Dushan and Nanyang as alternate names for the same lake, with Dushan coming from the nearby Dushan hills. The first definite mention of today's Nanyang Lake is in 1746, when it and Dushan Lake are mentioned as separate lakes.

Geographic entities mentioned:
surface_form: dushan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 33.070277777778
lon: 112.58638888889
Originally, Lümeng Lake appears to have been the most prominent. The first mention of the four lakes as they exist today (Nanyang, Zhaoyang, Dushan, and Weishan) is in 1746. The merging of Weishan, Chishan, and Lümeng into one lake had probably taken place by this point.

Geographic entities mentioned:
surface_form: dushan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 33.070277777778
lon: 112.58638888889
Nansi Lake. Nansi Lake (), or Weishan Lake, administrated by Weishan County and located in Shandong Province in China, is the largest freshwater lake in the north of the country. It consists of four connected lakes: Weishan (), Zhaoyang (), Nanyang (), Dushan (). It is 120 km long and 1266 square km in area. Early records: Zhaoyang Lake alone.

Geographic entities mentioned:
surface_form: nansi lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 34.6
lon: 117.2
The 1851–1855 Yellow River floods caused a major northward expansion of the united Lake Weishan-Zhaoyang-Nanyang. Another period of repeated flooding, in 1871-73, caused the united lake to merge with Dushan Lake, thus forming today's Nansi Lake. Prior to the merging of Nansi Lake, the area was swampy, with relatively shallow and slow-moving water.

Geographic entities mentioned:
surface_form: nansi lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 34.6
lon: 117.2
surface_form: nansi lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 34.6
lon: 117.2
Until the mid-1980s, Nansi Lake's water quality was generally within drinking standards; however, since the late 1980s, widespread dumping of untreated industrial and agricultural sewage into the lake's drainage basin caused a deterioration in water quality. Description. Nansi Lake is the largest freshwater lake in northern China, with a surface area of 1266 km2.

Geographic entities mentioned:
surface_form: nansi lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 34.6
lon: 117.2
Nanyang, Dushan, and most of Zhaoyang Lake comprise the lake's upper part, while Weishan Lake and a small part of Zhaoyang Lake make up the lower part. The upper and lower parts of Nansi Lake have similar surface area (602 km2 for the upper and 664 km2 for the lower lake), but almost 90% of the drainage basin flows to the upper part.

Geographic entities mentioned:
surface_form: nansi lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 34.6
lon: 117.2
Abtsdorfer See. Abtsdorfer See is a lake in the region of Rupertiwinkel in Bavaria, Germany. At an elevation of 426.20 m, its surface area is 0.84 km².

Geographic entities mentioned:
surface_form: abtsdorfer see
instance_of: Lake
countries: Germany
coordinates: lat: 47.910555555556
lon: 12.907777777778
Late war. On 31 July 2019, Suleiman and his son were arrested by Hayat Tahrir al-Sham's security force at a checkpoint at the Ghazawiya crossing near Darat Izza as they were driving from Afrin District to the northern Idlib Governorate. Suleiman was detained in HTS's Oqab Prison in Jabal Zawiya, and released two days later.

Geographic entities mentioned:
surface_form: Jabal Zawiya
instance_of: Mountain
countries: Syria
coordinates: lat: 35.73333333
lon: 36.7
Perry Lake (Minnesota). Perry Lake is a lake in Crow Wing County, in the U.S. state of Minnesota. According to Warren Upham, Perry Lake was probably named for a lumberman.

Geographic entities mentioned:
surface_form: perry lake
instance_of: Lake
countries: United States
coordinates: lat: 39.1676
lon: -95.452
surface_form: perry lake (minnesota)
instance_of: Lake
countries: United States
coordinates: lat: 46.61416667
lon: -93.95611111
Perry Lake (Minnesota). Perry Lake is a lake in Crow Wing County, in the U.S. state of Minnesota. According to Warren Upham, Perry Lake was probably named for a lumberman.

Geographic entities mentioned:
surface_form: perry lake
instance_of: Lake
countries: United States
coordinates: lat: 39.1676
lon: -95.452
surface_form: perry lake
instance_of: Lake
countries: United States
coordinates: lat: 46.61416667
lon: -93.95611111
Topography. Angletarn Pikes stands on the western arm of the long horseshoe ridge which surrounds the Martindale catchment, a system of valleys draining north into Ullswater. The adjacent fells on this ridge are Place Fell to the north and Brock Crags to the south. Beda Fell, a subsidiary ridge, also juts out into Martindale from Angletarn Pikes.

Geographic entities mentioned:
surface_form: Place Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.543838888889
lon: -2.9212388888889
surface_form: Brock Crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5153
lon: -2.89897
Angletarn Pikes stands on the western arm of the long horseshoe ridge which surrounds the Martindale catchment, a system of valleys draining north into Ullswater. The adjacent fells on this ridge are Place Fell to the north and Brock Crags to the south. Beda Fell, a subsidiary ridge, also juts out into Martindale from Angletarn Pikes. This separates the heads of Boredale and Bannerdale.

Geographic entities mentioned:
surface_form: Beda Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5459
lon: -2.88728
surface_form: angletarn pikes
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5251
lon: -2.90845
The adjacent fells on this ridge are Place Fell to the north and Brock Crags to the south. Beda Fell, a subsidiary ridge, also juts out into Martindale from Angletarn Pikes. This separates the heads of Boredale and Bannerdale. The western side above Goldrill Beck is steep and includes the faces of Dubhow and Fall Crags.

Geographic entities mentioned:
surface_form: Boredale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.5592
lon: -2.8865
The northern top is the true summit, the other being some six feet lower. The southern top is compensated by a clear view of Angle Tarn, described by Wainwright as &quot;among the best of Lakeland tarns&quot;. The wider view stretches from the Helvellyn range to the spine of the Far Eastern Fells across Martindale. Ascents.

Geographic entities mentioned:
surface_form: Helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
Boredale Hause carries the tiny ruin of a building named ‘Chapel in the Hause’ on OS maps. A mountain pass at seems a curious place to construct a church. From the Hause a good path carries on northwards up Steel Edge to Place Fell. The north-east ridge to Beda Fell is also well defined, a fair path traversing a series of rocky knolls before the final rise to the summit, named Beda Head.

Geographic entities mentioned:
surface_form: place fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.543838888889
lon: -2.9212388888889
Angletarn Pikes. Angletarn Pikes is a fell in the English Lake District near the village of Patterdale. Its most notable feature is Angle Tarn from which it derives its name. Topography. Angletarn Pikes stands on the western arm of the long horseshoe ridge which surrounds the Martindale catchment, a system of valleys draining north into Ullswater.

Geographic entities mentioned:
surface_form: angle tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.5197
lon: -2.90056
surface_form: angle tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.458638
lon: -3.167195
The north-east ridge to Beda Fell is also well defined, a fair path traversing a series of rocky knolls before the final rise to the summit, named Beda Head. Southward from Angletarn Pikes is Angle Tarn itself. This indented waterbody is about a quarter of a mile long with an island in the middle and forms a picturesque foreground for views of the Pikes.

Geographic entities mentioned:
surface_form: angle tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.5197
lon: -2.90056
surface_form: angle tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.458638
lon: -3.167195
surface_form: angletarn pikes
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5251
lon: -2.90845
The northern top is the true summit, the other being some six feet lower. The southern top is compensated by a clear view of Angle Tarn, described by Wainwright as &quot;among the best of Lakeland tarns&quot;. The wider view stretches from the Helvellyn range to the spine of the Far Eastern Fells across Martindale. Ascents.

Geographic entities mentioned:
surface_form: angle tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.5197
lon: -2.90056
surface_form: angle tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.458638
lon: -3.167195
Ascents. The fell can be climbed via Boredale Hause, making Patterdale, Bridgend, Hartsop and Boredale Head all possible starting points. An alternative is to climb from Martindale Old Church, ascending via the Beda Fell ridge or Angle Tarn. The route from Patterdale is often undertaken as the first section of the ascent of High Street.

Geographic entities mentioned:
surface_form: angle tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.5197
lon: -2.90056
surface_form: angle tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.458638
lon: -3.167195
surface_form: beda fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5459
lon: -2.88728
The long eastern flank above Bannerdale is also pock-marked with crags, Heck Crag being the principal feature. The narrow north eastern slopes above Boredale, although steep, are less rocky and are cut by the upper ravine of Freeze Beck. North from the summit a long ridge drops over Stony Rigg () to the walkers’ crossroads of Boredale Hause.

Geographic entities mentioned:
surface_form: boredale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.5592
lon: -2.8865
The narrow north eastern slopes above Boredale, although steep, are less rocky and are cut by the upper ravine of Freeze Beck. North from the summit a long ridge drops over Stony Rigg () to the walkers’ crossroads of Boredale Hause. From here paths run down to Hartsop, Patterdale and Boredale, while a further bridleway cuts across Beda Fell to Bannerdale.

Geographic entities mentioned:
surface_form: boredale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.5592
lon: -2.8865
North from the summit a long ridge drops over Stony Rigg () to the walkers’ crossroads of Boredale Hause. From here paths run down to Hartsop, Patterdale and Boredale, while a further bridleway cuts across Beda Fell to Bannerdale. Boredale Hause carries the tiny ruin of a building named ‘Chapel in the Hause’ on OS maps. A mountain pass at seems a curious place to construct a church.

Geographic entities mentioned:
surface_form: boredale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.5592
lon: -2.8865
surface_form: beda fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5459
lon: -2.88728
North from the summit a long ridge drops over Stony Rigg () to the walkers’ crossroads of Boredale Hause. From here paths run down to Hartsop, Patterdale and Boredale, while a further bridleway cuts across Beda Fell to Bannerdale. Boredale Hause carries the tiny ruin of a building named ‘Chapel in the Hause’ on OS maps. A mountain pass at seems a curious place to construct a church.

Geographic entities mentioned:
surface_form: boredale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.5592
lon: -2.8865
The wider view stretches from the Helvellyn range to the spine of the Far Eastern Fells across Martindale. Ascents. The fell can be climbed via Boredale Hause, making Patterdale, Bridgend, Hartsop and Boredale Head all possible starting points. An alternative is to climb from Martindale Old Church, ascending via the Beda Fell ridge or Angle Tarn.

Geographic entities mentioned:
surface_form: boredale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.5592
lon: -2.8865
surface_form: boredale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.5592
lon: -2.8865
The ridge proper runs to the east of the tarn above the Bannerdale face, rising again to the unnamed top above Satura Crag. This overtops the summit of Brock Crags, but was made subservient to it by Wainwright in his &quot;Pictorial Guide to the Lakeland Fells&quot;. Summit and view.

Geographic entities mentioned:
surface_form: brock crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5153
lon: -2.89897
Ascents. The fell can be climbed via Boredale Hause, making Patterdale, Bridgend, Hartsop and Boredale Head all possible starting points. An alternative is to climb from Martindale Old Church, ascending via the Beda Fell ridge or Angle Tarn. The route from Patterdale is often undertaken as the first section of the ascent of High Street.

Geographic entities mentioned:
surface_form: high street
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.492
lon: -2.865
Angletarn Pikes. Angletarn Pikes is a fell in the English Lake District near the village of Patterdale. Its most notable feature is Angle Tarn from which it derives its name. Topography. Angletarn Pikes stands on the western arm of the long horseshoe ridge which surrounds the Martindale catchment, a system of valleys draining north into Ullswater.

Geographic entities mentioned:
surface_form: angletarn pikes
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5251
lon: -2.90845
Its most notable feature is Angle Tarn from which it derives its name. Topography. Angletarn Pikes stands on the western arm of the long horseshoe ridge which surrounds the Martindale catchment, a system of valleys draining north into Ullswater. The adjacent fells on this ridge are Place Fell to the north and Brock Crags to the south.

Geographic entities mentioned:
surface_form: angletarn pikes
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5251
lon: -2.90845
A mountain pass at seems a curious place to construct a church. From the Hause a good path carries on northwards up Steel Edge to Place Fell. The north-east ridge to Beda Fell is also well defined, a fair path traversing a series of rocky knolls before the final rise to the summit, named Beda Head. Southward from Angletarn Pikes is Angle Tarn itself.

Geographic entities mentioned:
surface_form: beda fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5459
lon: -2.88728
Anjuman Pass. The Anjuman Pass (&quot;Kotal-e Anjoman&quot;) (also written Anjoman Pass) (4,430 m) is a mountain pass in the Hindu Kush in Afghanistan. It connects the Panjshir Valley and beyond in the south-west with Badakhshan province and beyond to the north-east, which is the most north-easterly province of Afghanistan.

Geographic entities mentioned:
surface_form: Panjshir Valley
instance_of: Valley
countries: Afghanistan
coordinates: lat: 35.266666666667
lon: 69.466666666667
Kleiner Nickus. The Kleiner Nickus is a hill in Hesse, Germany.

Geographic entities mentioned:
surface_form: kleiner nickus
instance_of: Mountain
countries: Germany
coordinates: lat: 50.3418
lon: 9.69067
Pollution incidents. There have been a high number of river pollution incidents in recent years in China, such as drinking water source pollution by algae in the Lake Tai, Wuxi in May 2007. There was a &quot;bloom of blue-green algae that gave off a rotten smell&quot; shutting off the main source of drinking water supply to 5.8 million people.

Geographic entities mentioned:
surface_form: Lake Tai
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 31.166666666667
lon: 120.15
Civic history. By the nineteenth century the neighbouring townships of Middleton and Tonge formed a single town. The townships, separated by the River Irk, lay in different parishes and local administration was in the hands of constables appointed by the Lord of the Manor.

Geographic entities mentioned:
surface_form: River Irk
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 53.4869
lon: -2.24504
Nelson-Miramichi, New Brunswick. Nelson-Miramichi is a suburban neighbourhood in the city of Miramichi, New Brunswick, Canada. Prior to municipal amalgamation on January 1, 1995, Nelson-Miramichi was an incorporated village in Northumberland County and one of the oldest European settlements in the Miramichi Valley. Earl J.

Geographic entities mentioned:
surface_form: Miramichi Valley
instance_of: Valley
countries: Canada
coordinates: lat: 46.96
lon: -65.63
Slieve Rushen. Slieve Rushen is a mountain which straddles the border between County Cavan in the Republic of Ireland and County Fermanagh in Northern Ireland. It is also called Slieve Russell or Ligavegra (also Legavagra, Ligavagra). It has an elevation of 404 metres above sea level. OS 1/50k Mapsheet: 27A & 26. Grid Ref: H234 226.

Geographic entities mentioned:
surface_form: slieve rushen
instance_of: Mountain
countries: United Kingdom
Ireland
coordinates: lat: 54.151925
lon: -7.6426416666667
The surface is mostly covered with peat, conifer forests and grazing fields. The mountain contains several caves and swallow-holes including Pollnagollum (Slieve Rushen) and Tory Hole which are a popular destination for potholers, both situate in Legavreagra townland. It forms part of the Slieve Rushen Bog Natural Heritage Area.

Geographic entities mentioned:
surface_form: slieve rushen
instance_of: Mountain
countries: United Kingdom
Ireland
coordinates: lat: 54.151925
lon: -7.6426416666667
The mountain contains several caves and swallow-holes including Pollnagollum (Slieve Rushen) and Tory Hole which are a popular destination for potholers, both situate in Legavreagra townland. It forms part of the Slieve Rushen Bog Natural Heritage Area. A recent addition to the mountain is the Slieve Rushen Wind Farm for generating electricity. Etymology.

Geographic entities mentioned:
surface_form: slieve rushen
instance_of: Mountain
countries: United Kingdom
Ireland
coordinates: lat: 54.151925
lon: -7.6426416666667
It forms part of the Slieve Rushen Bog Natural Heritage Area. A recent addition to the mountain is the Slieve Rushen Wind Farm for generating electricity. Etymology. The name Slieve Rushen derives from the Irish, 'mountain of the little wood'.

Geographic entities mentioned:
surface_form: slieve rushen
instance_of: Mountain
countries: United Kingdom
Ireland
coordinates: lat: 54.151925
lon: -7.6426416666667
Concupair gur airg Termann Dabeoc. Creach ele les gur airg go Binn Eclapra & go Sliabh Rusen & go Loch Erne). A poem about the River Shannon, composed at the beginning of the 17th century by Tadg Óg Ó hUiginn (born 1582), states in stanza 4: (As thy mighty current awakens but a little space from Slieve Rushen, it is not after Brian Boru that it were right to christen thee). History.

Geographic entities mentioned:
surface_form: slieve rushen
instance_of: Mountain
countries: United Kingdom
Ireland
coordinates: lat: 54.151925
lon: -7.6426416666667
Evolution is taught in many Islamic countries, and some scholars have tried to reconcile the Quran and evolution. Samiri. Quran recounts a story of the golden calf, where it mentions that Samiri, a rebellious follower of Moses, created the calf while Moses was away for 40 days on Mount Sinai, receiving the Ten Commandments.

Geographic entities mentioned:
surface_form: Mount Sinai
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.5384
lon: 33.9752
It premiered at the 2002 Sundance Film Festival. &quot;Blindsight&quot; premiered at Toronto. It follows the journey of six blind Tibetan teenagers who climb up the north side of Mount Everest with blind American mountaineer Erik Weihenmayer and their teacher, Sabriye Tenberken, who founded the only school for the blind in Tibet, Braille Without Borders.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
She had attended a botany course at Wray Castle on the shores of Windermere in 1943 and observed that much of the phytoplankton that was collected had been infected by fungi. Canter noticed a saprophytic chytrid she was unable to identify and contacted Ingold to send him a sample that he described as &quot;Chytriomyces elegans&quot;.

Geographic entities mentioned:
surface_form: Windermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.358333333333
lon: -2.9361111111111
Fish. Africa is the richest continent of freshwater fish, with about 3,000 species. The East African Great Lakes (Victoria, Malawi, and Tanganyika) are the center of biodiversity of many fish, especially cichlids (they harbor more than two-thirds of the estimated 2,000 species in the family).

Geographic entities mentioned:
surface_form: Victoria
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countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
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surface_form: Malawi
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countries: Malawi
Mozambique
Tanzania
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surface_form: Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
Precipitation in the valley varies from approximately 35 to 40 inches (90 to 100 cm) per year. The latter amount falls on Taylor Mountain, located immediately above Bennett Valley, in an outlier spur of the Sonoma Mountains sometimes called the Los Gullicos Range. Rainfall occurs primarily during winters (November to April), separated by warm dry summers.

Geographic entities mentioned:
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instance_of: Mountain
countries: United States
coordinates: lat: 47.454444444444
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surface_form: taylor mountain
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countries: United States
coordinates: lat: 38.4007
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surface_form: bennett valley
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countries: United States
coordinates: lat: 38.3231
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The dominant surface soil category of Bennett Valley is Clear Lake clay, a soil type occurring here on slopes ranging from zero to two percent gradient. Clear Lake clay is poorly drained and occurs on long smooth flood plains. Clear Lake clay is found on both sides of Matanzas Creek, which flows northwesterly along the axis of Bennett Valley.

Geographic entities mentioned:
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instance_of: Lake
countries: United States
coordinates: lat: 43.1256
lon: -93.4247
surface_form: lake clay
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countries: United States
coordinates: lat: 27.3098
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surface_form: clear lake
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countries: United States
coordinates: lat: 44.75388889
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surface_form: clear lake
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countries: United States
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countries: United States
coordinates: lat: 28.5219
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countries: United States
coordinates: lat: 39.0616
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surface_form: clear lake
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countries: United States
coordinates: lat: 44.3606
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surface_form: clear lake
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countries: United States
coordinates: lat: 44.1622
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countries: United States
coordinates: lat: 46.823611111111
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surface_form: clear lake
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countries: United States
coordinates: lat: 29.5594
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surface_form: clear lake
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countries: United States
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countries: United States
coordinates: lat: 44.7668323
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surface_form: clear lake
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countries: United States
coordinates: lat: 43.7612743
lon: -97.0121224
surface_form: clear lake
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countries: United States
coordinates: lat: 41.8325
lon: -86.421388888889
surface_form: clear lake
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countries: United States
coordinates: lat: 43.6437495
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surface_form: clear lake
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countries: United States
coordinates: lat: 45.1805262
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surface_form: clear lake
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countries: United States
coordinates: lat: 45.69361111
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surface_form: clear lake
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coordinates: lat: 43.988333333333
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surface_form: clear lake
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countries: United States
coordinates: lat: 43.900277777778
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Clear Lake clay is poorly drained and occurs on long smooth flood plains. Clear Lake clay is found on both sides of Matanzas Creek, which flows northwesterly along the axis of Bennett Valley. Clear Lake clay is dark gray in appearance and manifests a fine to medium granular structure, most commonly supporting hay production in the Bennett Valley.

Geographic entities mentioned:
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.1256
lon: -93.4247
surface_form: lake clay
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countries: United States
coordinates: lat: 27.3098
lon: -81.3484
surface_form: clear lake
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countries: United States
coordinates: lat: 44.75388889
lon: -96.6575
surface_form: clear lake
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countries: United States
coordinates: lat: 46.8675
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countries: United States
coordinates: lat: 28.5219
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surface_form: clear lake
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countries: United States
coordinates: lat: 39.0616
lon: -122.8272
surface_form: clear lake
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countries: United States
coordinates: lat: 44.3606
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surface_form: matanzas
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countries: United States
coordinates: lat: 29.9138577
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surface_form: clear lake
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countries: United States
coordinates: lat: 44.1622
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surface_form: clear lake
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countries: United States
coordinates: lat: 46.823611111111
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surface_form: bennett valley
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countries: United States
coordinates: lat: 38.4
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surface_form: clear lake
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countries: United States
coordinates: lat: 29.5594
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surface_form: clear lake
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countries: United States
coordinates: lat: 45.274722222222
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coordinates: lat: 44.7668323
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coordinates: lat: 43.6437495
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surface_form: clear lake
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countries: United States
coordinates: lat: 45.1805262
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surface_form: clear lake
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countries: United States
coordinates: lat: 45.69361111
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surface_form: clear lake
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countries: United States
coordinates: lat: 43.988333333333
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countries: United States
coordinates: lat: 43.900277777778
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Bennett Valley is drained by Matanzas Creek which is incised into the valley floor; an unnamed stream and Spring Creek drain into Matanzas Creek from the east side of Bennett Valley below the Matanzas Creek Reservoir. A flood-control reservoir on Matanzas Creek in the central portion of the valley collects water from the drainage of the upper portion of the valley.

Geographic entities mentioned:
surface_form: matanzas
instance_of: Landform
countries: United States
coordinates: lat: 29.9138577
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surface_form: matanzas
instance_of: Landform
countries: United States
coordinates: lat: 29.9138577
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surface_form: matanzas
instance_of: Landform
countries: United States
coordinates: lat: 29.9138577
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surface_form: the valley
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countries: United States
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surface_form: bennett valley
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countries: United States
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countries: United States
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countries: United States
coordinates: lat: 61.3833
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instance_of: Valley
countries: United States
coordinates: lat: 47.7174
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Bennett Valley is drained by Matanzas Creek which is incised into the valley floor; an unnamed stream and Spring Creek drain into Matanzas Creek from the east side of Bennett Valley below the Matanzas Creek Reservoir. A flood-control reservoir on Matanzas Creek in the central portion of the valley collects water from the drainage of the upper portion of the valley.

Geographic entities mentioned:
surface_form: matanzas
instance_of: Landform
countries: United States
coordinates: lat: 29.9138577
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surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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surface_form: the valley
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countries: United States
coordinates: lat: 61.3833
lon: -150.25
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countries: United States
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countries: United States
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These effects have led to a decrease in available natural habitat as well as decreased area available for hay farming and pasture usage. Some of the grapes are used locally for wine production such as in the case of the Matanzas Creek Winery, while some are sold to production facilities elsewhere in Sonoma County.

Geographic entities mentioned:
surface_form: matanzas
instance_of: Landform
countries: United States
coordinates: lat: 29.9138577
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surface_form: sonoma
instance_of: Mountain
countries: United States
coordinates: lat: 38.3231
lon: -122.575
The axis of the valley floor slopes 40 feet (12 m) per mile (a gradient of 0.008 or 7.6 m per km) from the pinched central portion of the valley, where knolls divide the northwestern from the southeastern segment of the valley.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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surface_form: the valley
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countries: United States
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countries: United States
coordinates: lat: 47.7174
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A flood-control reservoir on Matanzas Creek in the central portion of the valley collects water from the drainage of the upper portion of the valley. Precipitation in the valley varies from approximately 35 to 40 inches (90 to 100 cm) per year.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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surface_form: the valley
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countries: United States
coordinates: lat: 61.3833
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countries: United States
coordinates: lat: 47.7174
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Rainfall occurs primarily during winters (November to April), separated by warm dry summers. Bennett Valley is accessed chiefly via Bennett Valley Road, which traverses the valley floor to connect southeast Santa Rosa with Warm Springs Road in Glen Ellen. Ecology. Both the upper southwest and northeast sideslopes of Bennett Valley have significant oak woodland.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: bennett valley
instance_of: Valley
countries: United States
coordinates: lat: 38.4
lon: -122.64
surface_form: bennett valley
instance_of: Valley
countries: United States
coordinates: lat: 38.4
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countries: United States
coordinates: lat: 61.3833
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countries: United States
coordinates: lat: 47.7174
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Ecology. Both the upper southwest and northeast sideslopes of Bennett Valley have significant oak woodland. Both forested areas have dominant trees that include coast live oak. On the lower slopes and northern valley floor there are considerable numbers of valley oak in relict stands, from a previous dominant cover of these lower elevations prior to agricultural development of the valley floor.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
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instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
In addition, Zamora silty clay loam is found in several large patches on the valley floor; Zamora silty clay loam is a grayish brown firm, sticky and plastic soil type and is also characteristic of alluvial fans; it has a neutral pH and occurs at minimum depths of about two meters.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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countries: United States
coordinates: lat: 61.3833
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surface_form: the valley
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countries: United States
coordinates: lat: 47.7174
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Bennett Valley. Bennett Valley is a northwest- to southeast-trending valley in Sonoma County, California, US, approximately wide in its northwestern portion, where the southeast extremity of Santa Rosa, California is located.

Geographic entities mentioned:
surface_form: bennett valley
instance_of: Valley
countries: United States
coordinates: lat: 38.4
lon: -122.64
Bennett Valley. Bennett Valley is a northwest- to southeast-trending valley in Sonoma County, California, US, approximately wide in its northwestern portion, where the southeast extremity of Santa Rosa, California is located.

Geographic entities mentioned:
surface_form: bennett valley
instance_of: Valley
countries: United States
coordinates: lat: 38.4
lon: -122.64
surface_form: sonoma
instance_of: Mountain
countries: United States
coordinates: lat: 38.3231
lon: -122.575
Bennett Valley is accessed chiefly via Bennett Valley Road, which traverses the valley floor to connect southeast Santa Rosa with Warm Springs Road in Glen Ellen. Ecology. Both the upper southwest and northeast sideslopes of Bennett Valley have significant oak woodland. Both forested areas have dominant trees that include coast live oak.

Geographic entities mentioned:
surface_form: bennett valley
instance_of: Valley
countries: United States
coordinates: lat: 38.4
lon: -122.64
On the lower slopes and northern valley floor there are considerable numbers of valley oak in relict stands, from a previous dominant cover of these lower elevations prior to agricultural development of the valley floor. According to the 1990 report of Earth Metrics, a large percentage of valley oaks near Bennett Valley Road at the northwest end of Bennett Valley were infested with oak apple gall.

Geographic entities mentioned:
surface_form: bennett valley
instance_of: Valley
countries: United States
coordinates: lat: 38.4
lon: -122.64
surface_form: bennett valley
instance_of: Valley
countries: United States
coordinates: lat: 38.4
lon: -122.64
surface_form: apple
instance_of: Watercourse
countries: United States
coordinates: lat: 37.5656
lon: -89.5269
Clear Lake clay is poorly drained and occurs on long smooth flood plains. Clear Lake clay is found on both sides of Matanzas Creek, which flows northwesterly along the axis of Bennett Valley. Clear Lake clay is dark gray in appearance and manifests a fine to medium granular structure, most commonly supporting hay production in the Bennett Valley.

Geographic entities mentioned:
surface_form: bennett valley
instance_of: Valley
countries: United States
coordinates: lat: 38.4
lon: -122.64
Due to the economic demand for wine grapes in this region, pressure began in the 1980s to develop some of the Bennett Valley soils for viticulture. Luxury residential and vineyard growth. Economic factors of land scarcity for upscale residential development and for premium wine grape cultivation led to an explosion of land values in Bennett Valley starting in the 1980s.

Geographic entities mentioned:
surface_form: bennett valley
instance_of: Valley
countries: United States
coordinates: lat: 38.4
lon: -122.64
Luxury residential and vineyard growth. Economic factors of land scarcity for upscale residential development and for premium wine grape cultivation led to an explosion of land values in Bennett Valley starting in the 1980s. This trend is shaped by policies of the County of Sonoma, which discourage small lot residential development in Bennett Valley.

Geographic entities mentioned:
surface_form: bennett valley
instance_of: Valley
countries: United States
coordinates: lat: 38.4
lon: -122.64
Luxury residential and vineyard growth. Economic factors of land scarcity for upscale residential development and for premium wine grape cultivation led to an explosion of land values in Bennett Valley starting in the 1980s. This trend is shaped by policies of the County of Sonoma, which discourage small lot residential development in Bennett Valley.

Geographic entities mentioned:
surface_form: bennett valley
instance_of: Valley
countries: United States
coordinates: lat: 38.4
lon: -122.64
surface_form: sonoma
instance_of: Mountain
countries: United States
coordinates: lat: 38.3231
lon: -122.575
Some of the grapes are used locally for wine production such as in the case of the Matanzas Creek Winery, while some are sold to production facilities elsewhere in Sonoma County. As a result of this recognition of the Bennett Valley viticulture as a premium wine-grape region, an American Viticultural Area named &quot;Bennett Valley AVA&quot; was proposed and established in 2003.

Geographic entities mentioned:
surface_form: bennett valley
instance_of: Valley
countries: United States
coordinates: lat: 38.4
lon: -122.64
surface_form: bennett valley
instance_of: Valley
countries: United States
coordinates: lat: 38.4
lon: -122.64
According to the 1990 report of Earth Metrics, a large percentage of valley oaks near Bennett Valley Road at the northwest end of Bennett Valley were infested with oak apple gall. Gall wasps of the family Cynipidae produce a single sexual generation within a structure that resembles an apple.

Geographic entities mentioned:
surface_form: apple
instance_of: Watercourse
countries: United States
coordinates: lat: 37.5656
lon: -89.5269
Gall wasps of the family Cynipidae produce a single sexual generation within a structure that resembles an apple. Some valley oaks on the site are infested with these &quot;fruits,&quot; and on first glance appear as apple trees. This infestation is considered mild, and should not affect the oaks' ability to survive.

Geographic entities mentioned:
surface_form: apple
instance_of: Watercourse
countries: United States
coordinates: lat: 37.5656
lon: -89.5269