Sarmila/GeoWiki-Features huggingface dataset:
There are five listed buildings in the dale: the bridge over Grisedale Beck, East Scale Farmhouse, Fea Fow Farmhouse, Reachey Farmhouse and West Scale Farmhouse, all of which are registered as being in &quot;Grisdale&quot; with Historic England. Walking is popular in the dale over Baugh Fell to Sedbergh, north-west to Uldale, and across Swarth Fell to Wild Boar Fell.

Geographic entities mentioned:
surface_form: Wild Boar Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.384111111111
lon: -2.3741194444444
Grisedale, Grisedale Beck, and Grisedale Pike in the Lake District, are spelled exactly the same as the places within Grisedale near Garsdale. All of these places are now in Cumbria, with Grisedale valley next to Garsdale in South Lakeland. Grisedale Pike is high, and has several cairns on its flank, which provide a viewpoint across to Upper Wensleydale.

Geographic entities mentioned:
surface_form: Upper Wensleydale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.3056
lon: -2.16667
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
Grisedale. Grisedale (sometimes Grisdale, or Grizedale [archaic]) is a south east facing Dale in Cumbria, England, east of Sedbergh, and west of Hawes. Grisedale Beck, which drains Baugh Fell, flows down the dale eastwards, and on reaching the valley floor at Garsdale, forms the River Clough before turning westwards towards the Irish Sea.

Geographic entities mentioned:
surface_form: grisdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
Dunham and Speight assert that this refers to wild boars, but others state young pigs, perhaps in a farmed sense. The name of the dale was first documented in the 13th century, and has been recorded variously as Grizedale, Grisdale, and in 1640 as Grysdale. In 1225, most of the land in the dale belonged to Jervaulx Abbey, with the rest apportioned to Easby Abbey.

Geographic entities mentioned:
surface_form: grisdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
There are five listed buildings in the dale: the bridge over Grisedale Beck, East Scale Farmhouse, Fea Fow Farmhouse, Reachey Farmhouse and West Scale Farmhouse, all of which are registered as being in &quot;Grisdale&quot; with Historic England. Walking is popular in the dale over Baugh Fell to Sedbergh, north-west to Uldale, and across Swarth Fell to Wild Boar Fell.

Geographic entities mentioned:
surface_form: grisdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
Grisedale. Grisedale (sometimes Grisdale, or Grizedale [archaic]) is a south east facing Dale in Cumbria, England, east of Sedbergh, and west of Hawes. Grisedale Beck, which drains Baugh Fell, flows down the dale eastwards, and on reaching the valley floor at Garsdale, forms the River Clough before turning westwards towards the Irish Sea.

Geographic entities mentioned:
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
Grisedale Beck, which drains Baugh Fell, flows down the dale eastwards, and on reaching the valley floor at Garsdale, forms the River Clough before turning westwards towards the Irish Sea. A small part of the north-eastern side of the dale is in North Yorkshire, however, until 1974, all of the area around, and including Grisedale, was part of the West Riding of Yorkshire.

Geographic entities mentioned:
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
The subject of the farm workers moving out prompted Yorkshire Television to commission a film about the last farmer in the dale (&quot;The Dale that Died&quot;), with its director, Barry Cockcroft, remarking that Grisedale was &quot;the most romantic dale in all of Yorkshire.&quot;
History. Grisedale is a south-east facing Dale in Cumbria, but part of the Yorkshire Dales National Park.

Geographic entities mentioned:
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
It is between long, sandwiched between Baugh Fell to the south-west, Holmes Moss to the west, Swarth Fell Pike to the north, and White Birks Common to the east. Grisedale Beck rises on the east side of Baugh Fell (), and flows south-eastwards through Grisedale, over Clough waterfall, before becoming the River Clough in Garsdale at, then turning westwards to head to the Irish Sea.

Geographic entities mentioned:
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
In ancient times, the beck joined the valley floor farther west at Hard Ing Bridge (), but the pre-glacial valley was blocked by boulder clay, so the waters formed a new meander over Clough Waterfall. In its lower reaches before it flows under the A684 road, Grisedale beck cuts through an incised valley created by melting glacial waters.

Geographic entities mentioned:
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
The riverbed also has fossils in its bedrock just upstream of Clough Waterfall. Attempts have been made to mine coal in the north-eastern side of the dale near Grisedale Common. A small seam was worked some below the main limestone beds, but with little success. The bedrock of the dale is composed of the Yoredale Series limestones, with the surrounding hills being Millstone Grit.

Geographic entities mentioned:
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
Even though 14-16 families lived spread out across Grisedale at the turn of the 20th century, the hardships of the 1930s and severe snow falls in 1947, caused many families to leave, with only two houses in the dale populated by the mid-1960s.

Geographic entities mentioned:
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
The director of the documentary, Barry Cockcroft, said that Grisedale was &quot;the most romantic dale in all of Yorkshire...complete in its unspoilt beauty, serenity and vivid history.&quot;
However, in 2019, The Yorkshire Post visited the area and found that most homes had been renovated and had people living in them.

Geographic entities mentioned:
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
A document from the time of the Dissolution states that Jervaulx owned lands at &quot;Clough in Sedberglic&quot;, &quot;Grisendene&quot;, &quot;Grisedale&quot;, &quot;Sudeberge&quot;, and &quot;Ulnedale&quot;. Some of the earliest deeds to cover the valley date from the 1580s when Lord Wharton issued deeds to the tenant farmers in Grisedale.

Geographic entities mentioned:
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
However, the track used to go between the ranges to Uldale, where an inn was built in 1828, in anticipation that the track would be improved for travellers. The long-distance footpath &quot;Pennine Journey&quot; runs across Grisedale, and access can also be found from the North Yorkshire side of the dale at Lunds, via a small bridge over the Settle Carlisle Railway.

Geographic entities mentioned:
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
The long-distance footpath &quot;Pennine Journey&quot; runs across Grisedale, and access can also be found from the North Yorkshire side of the dale at Lunds, via a small bridge over the Settle Carlisle Railway. Grisedale, Grisedale Beck, and Grisedale Pike in the Lake District, are spelled exactly the same as the places within Grisedale near Garsdale.

Geographic entities mentioned:
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
Grisedale Pike is high, and has several cairns on its flank, which provide a viewpoint across to Upper Wensleydale. Whilst historically, cairns such as those on Grisedale Pike were markers for shepherds, they are near to the point where sandstone was quarried on Baugh Fell from 1690 to provide roofing materials for the farmhouses in the dale.

Geographic entities mentioned:
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
Previous to this, most of the houses had thatched roofs. Most of Grisedale is within the civil parish of Garsdale, and is represented at Westminster as part of the Westmorland and Lonsdale Constituency. Parts of the dale, notably Grisedale Common, are just within the civil parish of Hawes. Religious history.

Geographic entities mentioned:
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
Fox's own journal records that Previous to this, the tenant farmers in the dale were tied to the Anglican church of St John the Baptist in Garsdale, with many donating money from their wills to the vicar at St Johns. Initially, in 1703, a joint meeting house at Raygill () was built for the benefit of those from Garsdale and Grisedale.

Geographic entities mentioned:
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
Llwynypia. Llwynypia () is a village and community (and electoral ward) in Rhondda Cynon Taf, Wales, near Tonypandy in the Rhondda Fawr Valley. Before 1850 a lightly populated rural farming area, Llwynypia experienced a population boom between 1860 and 1920 with the sinking of several coal mines after the discovery of large coal deposits throughout the Rhondda Valleys.

Geographic entities mentioned:
surface_form: Rhondda
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
Llwynypia. Llwynypia () is a village and community (and electoral ward) in Rhondda Cynon Taf, Wales, near Tonypandy in the Rhondda Fawr Valley. Before 1850 a lightly populated rural farming area, Llwynypia experienced a population boom between 1860 and 1920 with the sinking of several coal mines after the discovery of large coal deposits throughout the Rhondda Valleys.

Geographic entities mentioned:
surface_form: Rhondda Valleys
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
School District 83 North Okanagan-Shuswap. School District 83 North Okanagan-Shuswap is a school district in British Columbia. This includes the major center of Salmon Arm and the area around Shuswap Lake as well as the northern Okanagan communities of Armstrong and Enderby. In 2024, the School District No.

Geographic entities mentioned:
surface_form: Shuswap Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.000693
lon: -119.01263
Val de Dagne. The Val de Dagne is a valley to the south east of Carcassonne in the department of Aude in southwest France. It forms a fiscal area of the Carcassonne arrondissement in Aude. Geography.

Geographic entities mentioned:
surface_form: aude
instance_of: Lake
countries: France
coordinates: lat: 42.569783333333
lon: 2.0245722222222
surface_form: val de dagne
instance_of: Valley
countries: France
coordinates: lat: 43.119
lon: 2.449
Val de Dagne. The Val de Dagne is a valley to the south east of Carcassonne in the department of Aude in southwest France. It forms a fiscal area of the Carcassonne arrondissement in Aude. Geography.

Geographic entities mentioned:
surface_form: aude
instance_of: Lake
countries: France
coordinates: lat: 42.569783333333
lon: 2.0245722222222
Val de Dagne. The Val de Dagne is a valley to the south east of Carcassonne in the department of Aude in southwest France. It forms a fiscal area of the Carcassonne arrondissement in Aude. Geography.

Geographic entities mentioned:
surface_form: val de dagne
instance_of: Valley
countries: France
coordinates: lat: 43.119
lon: 2.449
However the precise extent of the area known as the Val de Dagne is more vague than this, and villages and hamlets beyond this main valley, particularly across its western watershed towards Limoux, are said to lie in the Val. Approaching from the direction of Carcassonne the northern part of the valley spreads out from Monze, and includes the villages of Pradelles-en-Val and Montlaur.

Geographic entities mentioned:
surface_form: val de dagne
instance_of: Valley
countries: France
coordinates: lat: 43.119
lon: 2.449
The hamlets of Fajac-en-Val on the plateau above Arquettes, and Molières-sur-l'Alberte on the plateau above Villar, are also described by some commentators as being in the Val de Dagne. Architecture. This is an area which for centuries has depended for its livelihood mainly upon viticulture, and has remained for the most part relatively poor.

Geographic entities mentioned:
surface_form: val de dagne
instance_of: Valley
countries: France
coordinates: lat: 43.119
lon: 2.449
History. The camp was originally built in 1940 during World War II. Some 22,000 American servicemen were accommodated and trained at the camp prior to Operation Overlord. There is an extensive Training Area in the surrounding region that extends up Glen Fruin to the west bank of Loch Lomond and along Loch Long through Glen Mallan to DM Glen Douglas.

Geographic entities mentioned:
surface_form: Glen Fruin
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.053611111111
lon: -4.7436111111111
surface_form: Loch Lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
Monroe is the core city in the Monroe metropolitan area, which is coterminous with Monroe County and had a population of 154,809 in 2020. Located on the western shores of Lake Erie approximately northeast of Toledo, Ohio, and southwest of Detroit, the city is part of the Detroit–Ann Arbor–Flint combined statistical area.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Geography. Monroe is in eastern Monroe County, with its city limits extending southeast from the downtown to Lake Erie. The average elevation of the city is, decreasing to at Lake Erie, which sits at the lowest elevation in Michigan.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Popple Peak. Popple Peak () is a mountain in the Drakensberg range, South Africa. It is located on the border between South Africa and Lesotho, on the watershed that forms the border between the two countries. Popple peak is 3331 m above sea level and has an elevation of approximately 300 metres from the surrounding escarpment.

Geographic entities mentioned:
surface_form: popple peak
instance_of: Mountain
countries: South Africa
Lesotho
coordinates: lat: -29.23333333
lon: 29.4
It is located on the border between South Africa and Lesotho, on the watershed that forms the border between the two countries. Popple peak is 3331 m above sea level and has an elevation of approximately 300 metres from the surrounding escarpment. It is the 13th highest peak in South Africa and it is visible from as far away as Estcourt and Ladysmith in the KwaZulu-Natal Midlands.

Geographic entities mentioned:
surface_form: popple peak
instance_of: Mountain
countries: South Africa
Lesotho
coordinates: lat: -29.23333333
lon: 29.4
The peak was named by Barry Anderson in 1946 after John Poppleton (who climbed the peak with Barry Anderson and Des Watkins). On arrival at the summit a thunderstorm came up, and Poppleton was concerned for his safety, causing him to leave the summit. Anderson later sent the survey of the peak to the Surveyor General with the height and name &quot;Popple Peak&quot;.

Geographic entities mentioned:
surface_form: popple peak
instance_of: Mountain
countries: South Africa
Lesotho
coordinates: lat: -29.23333333
lon: 29.4
It is located in the Truso Gorge, on the left bank of the Tergi in the Kazbegi Municipality, Mtskheta-Mtianeti region, known as a &quot;mkhare&quot;, from Stepantsminda town. The name literally translates as &quot;a bath&quot;, a reference to the nearby hot springs, known as Abano Mineral Lake Natural Monument. The 17th-century combat towers survive in the village.

Geographic entities mentioned:
surface_form: Abano Mineral Lake Natural Monument
instance_of: Lake
countries: Georgia
coordinates: lat: 42.58819444444445
lon: 44.42202777777778
The stretch through Chattanooga also experiences severe congestion, due to an unusually high volume of truck traffic. The stretch of I-24 across the Cumberland Plateau, commonly known as &quot;Monteagle Mountain&quot;, is considered one of the most hazardous stretches of highway in the US, particularly for trucks, due to its steep descents, which measure a maximum of six-percent grade.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
The Interstate then travels over the next through a wide swath of mostly farmland, before entering Grundy County and reaching an interchange with US 64 and SR 50 near the town of Pelham, where it begins a concurrency with the former route that is largely unsigned. A short distance later, I-24 crosses the Elk River, before reaching the base of the Cumberland Plateau.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
Upon reentering Tennessee and Hamilton County, I-24 travels through Tiftonia for several miles and has an interchange with US 11/US 41/US 72 (Lee Highway) about later near the Tiftonia neighborhood. About later, the Interstate curves sharply to the east, traveling on a narrow artificial causeway between the Tennessee River to the north and the northern tip of Lookout Mountain to the south.

Geographic entities mentioned:
surface_form: Lookout Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.863713888889
lon: -85.392452777778
It then travels through the south side of Chattanooga before reaching a partial interchange with US 41/US 76. Here, I-24 reaches the &quot;Ridge Cut&quot;, a stretch where the Interstate ascends Missionary Ridge on a steep grade, first curving sharply to the north at the bottom of the ascent and then to the east again at the top.

Geographic entities mentioned:
surface_form: Missionary Ridge
instance_of: Landform
countries: United States
coordinates: lat: 34.986388888889
lon: -85.278611111111
Pisquioc. Pisquioc (possibly from Aymara &quot;p'isqi&quot; white quinoa, Quechua &quot;p'isqi&quot; a stew or purée of quinoa, &quot;-yuq&quot; a suffix, &quot;the one with white quinoa&quot;) is a mountain in the Vilcanota mountain range in the Andes of Peru, about high. It is located in the Cusco Region, Quispicanchi Province, Marcapata District, south of Aquichua.

Geographic entities mentioned:
surface_form: Aquichua
instance_of: Mountain
countries: Peru
coordinates: lat: -13.67555556
lon: -70.98333333
surface_form: aquichua
instance_of: Mountain
countries: Peru
coordinates: lat: -13.67555556
lon: -70.98333333
Pisquioc. Pisquioc (possibly from Aymara &quot;p'isqi&quot; white quinoa, Quechua &quot;p'isqi&quot; a stew or purée of quinoa, &quot;-yuq&quot; a suffix, &quot;the one with white quinoa&quot;) is a mountain in the Vilcanota mountain range in the Andes of Peru, about high. It is located in the Cusco Region, Quispicanchi Province, Marcapata District, south of Aquichua.

Geographic entities mentioned:
surface_form: pisquioc
instance_of: Mountain
countries: Peru
coordinates: lat: -13.70194444
lon: -70.98805556
Byatta. Byatta (,) was a senior commander in the Royal Army of King Anawrahta. He was a seaman, who joined Anawrahta's service after having shipwrecked at Thaton. He fathered two sons by a floral ogress from Popa district. The sons Shwe Hpyin Gyi and Shwe Hpyin Nge later entered the pantheon of Burmese nats as Shwe Hpyin Brothers. Origin.

Geographic entities mentioned:
surface_form: Popa district
instance_of: Mountain
countries: Myanmar
coordinates: lat: 20.920277777778
lon: 95.253888888889
Byatta nevertheless, escaped and could flee to Bagan, where he served King Anawrahta, who later appointed him as his 'flower officer' for his superhuman strength. He rode his steed daily to get to Mount Popa over 30 miles south of Bagan, gather and offer flowers to the king when returned.

Geographic entities mentioned:
surface_form: Mount Popa
instance_of: Mountain
countries: Myanmar
coordinates: lat: 20.920277777778
lon: 95.253888888889
After defeating the Republic of Genoa in a series of wars, it became the most powerful Mediterranean maritime power, and at its height, extended its rule from large parts of the Po Valley to the coastal regions and islands of present-day Slovenia, Croatia, Bosnia and Herzegovina, Montenegro, Albania, and Greece. Venice was a leading power of the Western world in the 15th and 16th centuries.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
Enchanted Lake. Enchanted Lake is a lake of Halifax Regional Municipality, Nova Scotia, Canada, in the southeastern part of the country, 1,000 km east of the capital Ottawa. Enchanted Lake is 48 meters above sea level. The highest point nearby is 84 meters above sea level, 1.0 km east of Enchanted Lake. It is densely populated around Enchanted Lake, with 1,056 inhabitants per square kilometre.

Geographic entities mentioned:
surface_form: enchanted lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.7189
lon: -63.5925
Enchanted Lake is 48 meters above sea level. The highest point nearby is 84 meters above sea level, 1.0 km east of Enchanted Lake. It is densely populated around Enchanted Lake, with 1,056 inhabitants per square kilometre. Average annual temperature in the neighbourhood is 7 °C. The warmest month is August, when the average temperature is 20 °C, and the coldest is January, about -6 °C.

Geographic entities mentioned:
surface_form: enchanted lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.7189
lon: -63.5925
Malabar 2012. In April 2012, &quot;Shakti&quot; took part in the Indian Navy's annual maritime exercise with the US Navy, Malabar 2012, in the Bay of Bengal. During these exercises, the ship replenished, the flagship of the US Navy's Carrier Strike Group 1. South China Sea and the North-West Pacific.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Kulshan (disambiguation). Kulshan'&quot; is a name for Koma Kulshan, the volcano otherwise known as Mount Baker.

Geographic entities mentioned:
surface_form: Mount Baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Juno Temple (Grand Canyon). Juno Temple is a 6,896-elevation summit located in the eastern Grand Canyon, in Coconino County of northern Arizona, United States. It is located 1.5 miles east-northeast of the Cape Final overlook, and is about 1.0 mi north of Jupiter Temple, its nearest high neighbor.

Geographic entities mentioned:
surface_form: Jupiter Temple
instance_of: Landform
countries: United States
coordinates: lat: 36.13443
lon: -111.89016
Awards. Hodgson's work on the Oak Ridges Moraine was recognized by the Environmental Commissioner with the 2001-2002 ECO Award. Hodgson and his ministry were also awarded the 2001 Canadian Urban Institute Brownie Award for leadership in policy development for Ontario's Brownfields Statute Law Amendment Act, 2001.

Geographic entities mentioned:
surface_form: Oak Ridges Moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
On 6 December, the IV Army Corps was reorganized by Mannerheim into a Group commanded by Paavo Talvela. Aaro Pajari was immediately ordered by Talvela to defend the western shore of Lake Tolvajärvi, while Per Ole Ekholm was ordered to continue the defense of Ilomantsi. On 10 December, Talvela issued counteroffensive orders to both Pajari and Ekholm for the next day.

Geographic entities mentioned:
surface_form: Lake Tolvajärvi
instance_of: Lake
countries: Russia
Soviet Union
Finland
Russian Empire
coordinates: lat: 62.269988
lon: 31.501491
Chilliwack Mountain. Chilliwack Mountain is a small mountain rising from the floodplain of the Fraser River in the city of Chilliwack, British Columbia, Canada. Located on the south side of the Fraser opposite the north side community of Deroche, it lies just west of the downtown of Chilliwack and to the east of Greendale, a rural neighbourhood of Chilliwack near its western boundary.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: chilliwack mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.155
lon: -122.0175
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Chilliwack Mountain. Chilliwack Mountain is a small mountain rising from the floodplain of the Fraser River in the city of Chilliwack, British Columbia, Canada. Located on the south side of the Fraser opposite the north side community of Deroche, it lies just west of the downtown of Chilliwack and to the east of Greendale, a rural neighbourhood of Chilliwack near its western boundary.

Geographic entities mentioned:
surface_form: chilliwack mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.155
lon: -122.0175
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Twentieth century. Mostly forested, the mountain has become the site of upscale real estate development which was approved by the City of Chilliwack Council in the Chilliwack Mountain Comprehensive Development Plan of 1996 for the development of a suburban community scenario that would lead to a build-out population of 4,500, or 1,700 dwelling units.

Geographic entities mentioned:
surface_form: chilliwack mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.155
lon: -122.0175
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Eochy's Cairn. Eochy's Cairn is a cairn and National Monument located in County Mayo, Ireland. Location. Eochy's Cairn is atop a hill northwest of The Neale overlooking Lough Mask. History. Eochy's Cairn has never been excavated, but is believed to have been constructed in the Neolithic. With a height of 22 feet and a diameter of over 150 feet Eochy's Cairn might be the largest cairn in Connacht.

Geographic entities mentioned:
surface_form: Lough Mask
instance_of: Lake
countries: Ireland
coordinates: lat: 53.621944444444
lon: -9.3822222222222
It had been inhabited for 2,000 years, until its Syrian population fled and their homes were destroyed by Israel following the 1967 Six-Day War. It is located at the foot of Mount Hermon, north of the Golan Heights, the classical &quot;Gaulanitis&quot;, in the part occupied by Israel. The spring is the source of the Banias River, one of the main tributaries of the Jordan River.

Geographic entities mentioned:
surface_form: Mount Hermon
instance_of: Mountain
countries: Lebanon
Israel
Syria
coordinates: lat: 33.4
lon: 35.85
The once very large spring gushed from the limestone cave, but an earthquake moved it to the foot of the natural terrace where it now seeps quietly from the bedrock, with a greatly reduced flow. From here the stream, called Nahal Hermon in Hebrew, flows towards what once were the malaria-infested Hula marshes. Semitic deity of the spring.

Geographic entities mentioned:
surface_form: Hula marshes
instance_of: Valley
countries: Israel
coordinates: lat: 33.103333333333
lon: 35.609166666667
Al-Sa'id Hasan of Banias, released by Hulegu during the Mongol invasion of Syria, allied with him, and took part in the Battle of Ain Jalut. During the Mamluk period, Banias served as the provincial seat of a subdistrict ('amal) subordinate to Damascus. It controlled all of the northern part of the Golan, in addition to the southern parts of Mt. Hermon.

Geographic entities mentioned:
surface_form: Mt. Hermon.
instance_of: Mountain
countries: Lebanon
Israel
Syria
coordinates: lat: 33.4
lon: 35.85
In September 1953, Israel advanced plans for its National Water Carrier to help irrigate the coastal Sharon Plain and eventually the Negev desert by launching a diversion project on a nine-mile (14 km) channel midway between the Huleh Marshes and Sea of Galilee in the central DMZ to be rapidly constructed.

Geographic entities mentioned:
surface_form: Huleh Marshes
instance_of: Valley
countries: Israel
coordinates: lat: 33.103333333333
lon: 35.609166666667
Meta River. The Meta River is a major left tributary of the Orinoco River in eastern Colombia and southern Venezuela, South America. The Meta originates in the Eastern Ranges of the Andes and flows through the Meta Department, Colombia as the confluence of the Humea, Guatiquía and Guayuriba rivers.

Geographic entities mentioned:
surface_form: Guayuriba
instance_of: Watercourse
countries: Colombia
coordinates: lat: 3.9080555555555554
lon: -73.09472222222222
The major tributaries of the Meta are the Cravo Sur, the Casanare, the Cusiana, the Upía and the Manacacías rivers. History. In 1531, while exploring the Orinoco river, Diego de Ordáz became the first European to discover the estuarine delta of the Meta.

Geographic entities mentioned:
surface_form: Cravo Sur
instance_of: Watercourse
countries: Colombia
coordinates: lat: 4.68936
lon: -71.5314
surface_form: Upía
instance_of: Watercourse
countries: Colombia
coordinates: lat: 4.3
lon: -72.733333333333
surface_form: Manacacías
instance_of: Watercourse
countries: Colombia
coordinates: lat: 4.3833333333333
lon: -72.066666666667
They are slow-growing canopy evergreen trees and have a valuable timber. The wood and bark are pleasantly scented. They are present in Peru, Ecuador, Colombia, and the Guiana Shield (in northeastern Brazil, Venezuela (Amazonas, Bolívar and Delta Amacuro states), Guyana, Suriname and French Guiana). The species are heavily used by the timber industry. This causes a shortage of mature trees.

Geographic entities mentioned:
surface_form: Delta Amacuro
instance_of: Body of water
countries: Venezuela
coordinates: lat: 8.7
lon: -61.15
He took over as Canada's First Chief Hydrographic Surveyor in 1893 and continued to survey in Georgian Bay and the North Channel until 1894. In 1891, he surveyed Burrard Inlet in British Columbia. In 1895-97, he with his ship Bayfield was in Lake St. Clair, Lake Erie and Lake Huron. In 1898, he was back at Parry Sound.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Clair, Lake Erie and Lake Huron. In 1898, he was back at Parry Sound. During 1901, he took part in the first year of the Lake Winnipeg survey, but for the next two years, he was in Lake Superior surveying with a new Bayfield. He obtained his Master's Certificate, Inland Waters in 1897, though he never commanded his own survey ship. He was a member of the International Waterways Commission in 1909.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Sinbad Rock. Sinbad Rock () is a low rock (approximately 10 feet high) lying 1.25 nautical miles (2.3 km) west-northwest of Square End Island, off the west end of King George Island, in the South Shetland Islands. The rock was charted in 1935 by DI personnel on the &quot;Discovery II&quot; but the name appears to be first used on a 1948 Admiralty chart based upon this survey.

Geographic entities mentioned:
surface_form: discovery
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: discovery
instance_of: Body of water
coordinates: lat: -64.5167
lon: -63.0167
Sinbad Rock. Sinbad Rock () is a low rock (approximately 10 feet high) lying 1.25 nautical miles (2.3 km) west-northwest of Square End Island, off the west end of King George Island, in the South Shetland Islands. The rock was charted in 1935 by DI personnel on the &quot;Discovery II&quot; but the name appears to be first used on a 1948 Admiralty chart based upon this survey.

Geographic entities mentioned:
surface_form: low rock
instance_of: Mountain
coordinates: lat: -62.2833
lon: -58.65
surface_form: sinbad rock
instance_of: Mountain
coordinates: lat: -62.1667
lon: -59.0333
surface_form: george
instance_of: Mountain
coordinates: lat: -67.71667
lon: 50
Sinbad Rock. Sinbad Rock () is a low rock (approximately 10 feet high) lying 1.25 nautical miles (2.3 km) west-northwest of Square End Island, off the west end of King George Island, in the South Shetland Islands. The rock was charted in 1935 by DI personnel on the &quot;Discovery II&quot; but the name appears to be first used on a 1948 Admiralty chart based upon this survey.

Geographic entities mentioned:
surface_form: sinbad rock
instance_of: Mountain
coordinates: lat: -62.1667
lon: -59.0333
Zenssee. Zenssee is a lake in Uckermark, Brandenburg, Germany. At an elevation of, its surface area is 1.1167 km2. It is located in the town of Lychen.

Geographic entities mentioned:
surface_form: zenssee
instance_of: Lake
countries: Germany
coordinates: lat: 53.196944444444
lon: 13.341111111111
From 1941 to 1942, he was president of the Royal Society of Canada. He also served as a member of the Historic Sites and Monuments Board of Canada, briefly serving as its interim chairman. In 1933, he was awarded an honorary Doctor of Laws from the University of British Columbia. Mount Judge Howay, north of Stave Lake, is named in his honour. He died in 1943 in New Westminster, British Columbia.

Geographic entities mentioned:
surface_form: Mount Judge Howay
instance_of: Mountain
countries: Canada
coordinates: lat: 49.5069
lon: -122.322
Maurice and Irma worked as a husband and wife team at the Sanctuary until 1966, and then moved to a farm one ridge to the west of Hawk Mountain in East Brunswick Township, Pennsylvania. Death. Broun died of cancer on October 2, 1979, at Lehigh Valley Hospital–Cedar Crest in Allentown, Pennsylvania.

Geographic entities mentioned:
surface_form: Hawk Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.645555555556
lon: -75.98
Malcham cave. Malcham cave () is the longest salt cave in the world, located in Mount Sodom, by the Dead Sea, Israel. History. In March 2019 it has been revealed, by an international team, led by the Israeli geologist professor Amos Frumkin, after a second measurement that its length is almost two times longer than was measured back in the 1980s. Structure.

Geographic entities mentioned:
surface_form: Mount Sodom
instance_of: Mountain
countries: Israel
coordinates: lat: 31.092222222222
lon: 35.382777777778
Middle basin. The middle section runs from the confluence of the Aroostook and Tobique rivers, flowing southeast to Mactaquac Dam. Other tributaries in this section include the Meduxnekeag River. This area is the only place in Atlantic Canada where Appalachian Hardwood Forest is found.

Geographic entities mentioned:
surface_form: Aroostook
instance_of: Watercourse
countries: United States
Canada
coordinates: lat: 46.345043
lon: -68.802268
surface_form: Tobique
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.7667
lon: -67.7
Middle basin. The middle section runs from the confluence of the Aroostook and Tobique rivers, flowing southeast to Mactaquac Dam. Other tributaries in this section include the Meduxnekeag River. This area is the only place in Atlantic Canada where Appalachian Hardwood Forest is found.

Geographic entities mentioned:
surface_form: Meduxnekeag River
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 46.1478
lon: -67.5729
surface_form: meduxnekeag
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 46.1478
lon: -67.5729
Lower basin. The lower basin, to Saint John Harbour on the Bay of Fundy, consisting of lakes, islands, wetlands and a tidal estuary. Tributaries in this section include the Nashwaak and Nerepis rivers and Belleisle Bay. The final tributary, the Kennebecasis River, is a fjord with a sill, or rise in depth near the mouth of a fjord caused by a terminal moraine.

Geographic entities mentioned:
surface_form: Nashwaak
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.965694444444
lon: -66.586194444444
surface_form: Nerepis
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.366667
lon: -66.25
Lower basin. The lower basin, to Saint John Harbour on the Bay of Fundy, consisting of lakes, islands, wetlands and a tidal estuary. Tributaries in this section include the Nashwaak and Nerepis rivers and Belleisle Bay. The final tributary, the Kennebecasis River, is a fjord with a sill, or rise in depth near the mouth of a fjord caused by a terminal moraine.

Geographic entities mentioned:
surface_form: Kennebecasis River
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.31666667
lon: -66.13333333
Saint John River (Bay of Fundy). The Saint John River (; Maliseet-Passamaquoddy: &quot;Wolastoq&quot;) is a river flowing within the Dawnland region from headwaters in the Notre Dame Mountains near the Maine-Quebec border through western New Brunswick to the northwest shore of the Bay of Fundy. Eastern Canada's longest river, its drainage basin is one of the largest on the east coast at about.

Geographic entities mentioned:
surface_form: saint john river
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.266667
lon: -66.066667
Maine communities along the river include Fort Kent, Madawaska, and Van Buren. New Brunswick settlements through which it passes include, moving downstream, Edmundston, Fredericton, Oromocto, and Saint John. It is regulated by hydro-power dams at Mactaquac, Beechwood, and Grand Falls, New Brunswick. Hydronym.

Geographic entities mentioned:
surface_form: saint john
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.266667
lon: -66.066667
It is regulated by hydro-power dams at Mactaquac, Beechwood, and Grand Falls, New Brunswick. Hydronym. Samuel de Champlain visited the mouth of the river on the feast day of John the Baptist in 1604 and renamed it the Rivière Saint-Jean or Saint John River in English. Many waterways in the system retain their original pre-European names.

Geographic entities mentioned:
surface_form: saint john river
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.266667
lon: -66.066667
surface_form: saint-jean
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.266667
lon: -66.066667
Plants rare for the province include wild ginger, black raspberry, wild coffee, maidenhair fern, showy orchis and others. This forest type, also known as the Saint John River Valley Hardwood Forest, once spread of much of the area and has been reduced to less than one percent of the land area because of human activities.

Geographic entities mentioned:
surface_form: saint john river
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.266667
lon: -66.066667
Soils are fine, loamy, and well-drained glacial tills overlaying limestone and sandstone. The climate here is drier and warmer than surrounding regions. Lower basin. The lower basin, to Saint John Harbour on the Bay of Fundy, consisting of lakes, islands, wetlands and a tidal estuary. Tributaries in this section include the Nashwaak and Nerepis rivers and Belleisle Bay.

Geographic entities mentioned:
surface_form: saint john
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.266667
lon: -66.066667
Surface runoff from heavy rainfall is the main cause of flooding, and can be exacerbated by ice jams, high tides, and rapid snowmelt. Floods have been documented for more than 300 years. Flooding has occurred in Edmundston, Grand Falls, Perth-Andover, Hartland, Woodstock, and most severely around Fredericton and Saint John. Major flooding occurred in 1923, with water above normal winter low.

Geographic entities mentioned:
surface_form: saint john
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.266667
lon: -66.066667
The Passamaquoddy hunted sea mammals along the northwest shore of the Bay of Fundy while speaking a mutually intelligible dialect with the Wolastoqiyik who were inland hunters along the upper Saint John River and its tributaries.

Geographic entities mentioned:
surface_form: saint john river
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.266667
lon: -66.066667
No pure blooded Wolastoqiyik or Passamquoddy survived the 20th century. European colonization. When the Europeans arrived into Wolastokuk, the homeland of the Maliseet Nation and Saint John River basin, they found the locals hunting, gathering, and farming near the banks of the river. Rivalry between English and French fur traders pre-dated colonization of North America.

Geographic entities mentioned:
surface_form: saint john river
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.266667
lon: -66.066667
European colonists may have used fields and town sites prepared by the natives. Colonization pressure was less severe along the Saint John River where the cold water eddy of the Gulf of Maine kept the growing season shorter than Massachusetts and the Nova Scotia peninsula nearer the warm Gulf Stream.

Geographic entities mentioned:
surface_form: saint john river
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.266667
lon: -66.066667
These Acadians maintained favorable relationships with the First Nations while King Philip's War encouraged the Wolastoqiyik to join the Wabanaki Confederacy in military action against New England. French colonists populated the lower river valley as part of Acadia, with Fort Nashwaak in present-day Fredericton, Fort Boishebert at the confluence of the Saint John and Nerepsis rivers.

Geographic entities mentioned:
surface_form: saint john
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.266667
lon: -66.066667
However, this was not practical given the seasonal flooding, and the Acadians moved to higher ground. The Wolastoqiyik became steadfast allies of the Acadians through the subsequent French and Indian Wars; and their Saint John River valley became the last holdout of Acadian refusal to declare allegiance to the British monarchy.

Geographic entities mentioned:
surface_form: saint john river
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.266667
lon: -66.066667
As the longest river between the Chesapeake Bay and the Gulf of Saint Lawrence, the Saint John offered one of the best transportation corridors for First Nations refugees to retreat from the English colonization of North America's Atlantic coast. About a thousand Wolastoqiyik sheltered a hundred Acadian families retreating up the Saint John to avoid the Acadian Expulsion as the St.

Geographic entities mentioned:
surface_form: saint john
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.266667
lon: -66.066667
As the longest river between the Chesapeake Bay and the Gulf of Saint Lawrence, the Saint John offered one of the best transportation corridors for First Nations refugees to retreat from the English colonization of North America's Atlantic coast. About a thousand Wolastoqiyik sheltered a hundred Acadian families retreating up the Saint John to avoid the Acadian Expulsion as the St.

Geographic entities mentioned:
surface_form: saint john
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.266667
lon: -66.066667
surface_form: st. john river
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.266667
lon: -66.066667
International boundary dispute. While the upstream Wolastoqiyik and their Acadian allies rejected both Canada and United States sovereignty after English victories in the French and Indian War, many Loyalist refugees from the American Revolutionary War resettled in Saint John at the mouth of the river and in Sainte-Anne des Pays-Bas which was renamed Fredericton.

Geographic entities mentioned:
surface_form: saint john
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.266667
lon: -66.066667
The Saint Croix River formed the Atlantic coastal boundary at the close of the war keeping the Saint John River in Canada while the Penobscot River was allocated to Massachusetts. The Treaty of Paris (1783) defined the eastern boundary of Massachusetts as a line drawn due north from the source of St. Croix River to the drainage divide of the Saint Lawrence River.

Geographic entities mentioned:
surface_form: saint john river
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.266667
lon: -66.066667
Persistent hostilities with the Wolastoqiyik had prevented the English treaty signatories from mapping the river headwaters. Aside from ambiguity as to which tributary might be considered the source of the Saint Croix River, the Saint John River does not flow directly south as might have been assumed from knowledge of the better mapped Hudson and Connecticut Rivers.

Geographic entities mentioned:
surface_form: saint john river
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.266667
lon: -66.066667
surface_form: saint croix
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.8231
lon: -67.7558
Canada chose to interpret the treaty's intention as keeping the entire Saint John drainage basin under Canadian control. Surviving Acadian and Wolastoqiyik refugees continued to resist British rule while moving upriver to the Acadian Landing Site west of the Saint Croix treaty boundary where they were joined by other Acadian refugees who had fled to Quebec.

Geographic entities mentioned:
surface_form: saint john
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.266667
lon: -66.066667
Large numbers of people began settling the area in the early 1800s, mostly Scottish and Irish, and by the end of the 1850s much of the central Saint John valley had been cleared of old-growth forest for farming. Before the advent of railways, the river was an important trade route, including timber rafting.

Geographic entities mentioned:
surface_form: saint john
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.266667
lon: -66.066667
After the state of Maine obtained independence from Massachusetts in 1820, Maine lumbermen encouraged Acadian refugees to form the independent Republic of Madawaska, and began diverting the Saint John headwaters into the Penobscot River so log driving could float timber harvested in the upper Saint John watershed to Bangor sawmills.

Geographic entities mentioned:
surface_form: saint john
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.266667
lon: -66.066667
surface_form: saint john
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.266667
lon: -66.066667