Sarmila/GeoWiki-Features huggingface dataset:
West Africans, bearing the Benin sickle cell haplotype, may have migrated into the northern region of Iraq (69.5%), Jordan (80%), Lebanon (73%), Oman (52.1%), and Egypt (80.8%). Schistosomes. According to Steverding (2020), while not definite: Near the African Great Lakes, schistosomes (e.g., S. mansoni, S. haematobium) underwent evolution.

Geographic entities mentioned:
surface_form: African Great Lakes
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
Ray Lake, east of Mount Ray, and Ray Mineral Spring are also named for John Ray. Mount Ray is best viewed from a plane and its bright red color contrasts with the forest below. The west slopes can be seen from boats on Clearwater Lake. No trails go anywhere near the mountain. The Kostal Lake trail used to pass to the south, but this trail was permanently closed by BC Parks in 2013.

Geographic entities mentioned:
surface_form: Kostal Lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.164
lon: -119.976
Mount Ray was named for John Bunyan Ray, the first settler in the Clearwater Valley. He was born in 1878 in North Carolina and came to the Valley in 1909. He cleared land and established a farm in the wilderness south of Clearwater Lake. He married Alice Ludtke in 1932 and they raised three children, Nancy, Doug and Bob.

Geographic entities mentioned:
surface_form: clearwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.203
lon: -79.233
surface_form: clearwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.2667
lon: -120.233
surface_form: clearwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.8734
lon: -107.9301
surface_form: clearwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05
lon: -101.05
Ray Lake, east of Mount Ray, and Ray Mineral Spring are also named for John Ray. Mount Ray is best viewed from a plane and its bright red color contrasts with the forest below. The west slopes can be seen from boats on Clearwater Lake. No trails go anywhere near the mountain. The Kostal Lake trail used to pass to the south, but this trail was permanently closed by BC Parks in 2013.

Geographic entities mentioned:
surface_form: clearwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.203
lon: -79.233
surface_form: clearwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.2667
lon: -120.233
surface_form: clearwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.8734
lon: -107.9301
surface_form: clearwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05
lon: -101.05
Mount Ray (British Columbia). Mount Ray, also known as Ray Mountain, is a subglacial mound in Wells Gray Provincial Park, British Columbia, Canada. Mount Ray last erupted during the Pleistocene. It is part of the Wells Gray-Clearwater volcanic field.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount ray (british columbia)
instance_of: Mountain
countries: Canada
coordinates: lat: 52.3833
lon: -120.2
Mount Ray (British Columbia). Mount Ray, also known as Ray Mountain, is a subglacial mound in Wells Gray Provincial Park, British Columbia, Canada. Mount Ray last erupted during the Pleistocene. It is part of the Wells Gray-Clearwater volcanic field.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: ray mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.3833
lon: -120.2
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Ray Lake, east of Mount Ray, and Ray Mineral Spring are also named for John Ray. Mount Ray is best viewed from a plane and its bright red color contrasts with the forest below. The west slopes can be seen from boats on Clearwater Lake. No trails go anywhere near the mountain. The Kostal Lake trail used to pass to the south, but this trail was permanently closed by BC Parks in 2013.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
In December 1947, John Ray trekked into his old homestead and died there from a heart attack. Ray Lake, east of Mount Ray, and Ray Mineral Spring are also named for John Ray. Mount Ray is best viewed from a plane and its bright red color contrasts with the forest below. The west slopes can be seen from boats on Clearwater Lake. No trails go anywhere near the mountain.

Geographic entities mentioned:
surface_form: ray lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.233333333333
lon: -120.06666666667
Pulpudeva Glacier. Pulpudeva Glacier (,) is the long and wide glacier in Sullivan Heights, Sentinel Range in Ellsworth Mountains, Antarctica.

Geographic entities mentioned:
surface_form: Sullivan Heights
instance_of: Mountain
coordinates: lat: -78.3167
lon: -85.05
Pulpudeva Glacier (,) is the long and wide glacier in Sullivan Heights, Sentinel Range in Ellsworth Mountains, Antarctica. It is draining the area northeast of Nebeska Peak, north of Johnson Col and northwest of Mount Farrell, flowing northwards west of Mount Levack, and (together with Crosswell and Patton Glaciers) joining Ellen Glacier northwest of Mamarchev Peak and southeast of Mount Jumper.

Geographic entities mentioned:
surface_form: Nebeska Peak
instance_of: Mountain
coordinates: lat: -78.3836
lon: -85.1878
surface_form: Mount Levack
instance_of: Mountain
coordinates: lat: -78.3
lon: -85.08333333
surface_form: Mamarchev Peak
instance_of: Mountain
coordinates: lat: -78.3136
lon: -85.1483
surface_form: Mount Jumper
instance_of: Mountain
coordinates: lat: -78.2333
lon: -85.6
The Kings Ransom. The Kings Ransom were an American garage rock band from Allentown, Pennsylvania who were active from 1965 to 1968 and were a popular act in the Lehigh Valley area, as well as around Philadelphia. Their record &quot;Shame&quot; became a hit in Milton, Pennsylvania and received airplay in Michigan.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Etymology. The word &quot;diummeri&quot; is first attested in 965. „Dümmer“ ist probably derived from &quot;dummerig&quot;, meaning moist or shaded, and &quot;Meer“, meaning sea. In northwestern Germany, &quot;Meer&quot; is the traditional term for still waters surrounded by marshes (see: &quot;Steinhuder Meer&quot; and &quot;Zwischenahner Meer&quot;).

Geographic entities mentioned:
surface_form: Steinhuder Meer
instance_of: Lake
countries: Germany
coordinates: lat: 52.466666666667
lon: 9.3333333333333
surface_form: Zwischenahner Meer
instance_of: Lake
countries: Germany
coordinates: lat: 53.197632
lon: 8.016015
surface_form: zwischenahner meer
instance_of: Lake
countries: Germany
coordinates: lat: 53.197632
lon: 8.016015
surface_form: steinhuder meer
instance_of: Lake
countries: Germany
coordinates: lat: 52.466666666667
lon: 9.3333333333333
Hence it counts as part of Oldenburg Münsterland. Character. The Dümmer is, after the Steinhuder Meer, the second largest lake in Lower Saxony. With its water surface of 13.5 km ² - the area within the ring dyke including siltation zones is 16 km ² - and maximum water depth of just 1.50 m, it is good for swimming and water sports.

Geographic entities mentioned:
surface_form: Steinhuder Meer
instance_of: Lake
countries: Germany
coordinates: lat: 52.466666666667
lon: 9.3333333333333
Dümmer. The Dümmer () or officially Dümmer See is a large lake in southern Lower Saxony (Germany). It has a surface of 13.5 km2 and an average depth of one metre. Its elevation is 37 metres. Dümmer is a popular resort for water sports, but also an important biotope for water birds and located in a zone especially frequented by migratory birds.

Geographic entities mentioned:
surface_form: dümmer
instance_of: Lake
countries: Germany
coordinates: lat: 52.5
lon: 8.35
surface_form: dümmer
instance_of: Lake
countries: Germany
coordinates: lat: 52.5
lon: 8.35
surface_form: dümmer see
instance_of: Lake
countries: Germany
coordinates: lat: 53.581388888889
lon: 11.202777777778
Dümmer. The Dümmer () or officially Dümmer See is a large lake in southern Lower Saxony (Germany). It has a surface of 13.5 km2 and an average depth of one metre. Its elevation is 37 metres. Dümmer is a popular resort for water sports, but also an important biotope for water birds and located in a zone especially frequented by migratory birds.

Geographic entities mentioned:
surface_form: dümmer
instance_of: Lake
countries: Germany
coordinates: lat: 52.5
lon: 8.35
It has a surface of 13.5 km2 and an average depth of one metre. Its elevation is 37 metres. Dümmer is a popular resort for water sports, but also an important biotope for water birds and located in a zone especially frequented by migratory birds. A large section of its shore is protected by nature reserve areas. Etymology. The word &quot;diummeri&quot; is first attested in 965.

Geographic entities mentioned:
surface_form: dümmer
instance_of: Lake
countries: Germany
coordinates: lat: 52.5
lon: 8.35
In northwestern Germany, &quot;Meer&quot; is the traditional term for still waters surrounded by marshes (see: &quot;Steinhuder Meer&quot; and &quot;Zwischenahner Meer&quot;). Possibly, there is also a connection between &quot;Dümmer&quot; and the southern dutch word „doom“ (&quot;mist&quot;, &quot;broom&quot;). Location. The Dümmer is located in the Dümmer depression.

Geographic entities mentioned:
surface_form: dümmer
instance_of: Lake
countries: Germany
coordinates: lat: 52.5
lon: 8.35
surface_form: dümmer
instance_of: Lake
countries: Germany
coordinates: lat: 52.5
lon: 8.35
The low water level was caused by heavy silting, also a result of dyking the lake. With the help of several locks it was possible to control the high water levels artificially without greatly interfering with nature. Nevertheless, the Dümmer suffers from heavy nutrient pollution caused by intensive agriculture. The remains of New Stone Age settlements have been found on the shores of the Dümmer.

Geographic entities mentioned:
surface_form: dümmer
instance_of: Lake
countries: Germany
coordinates: lat: 52.5
lon: 8.35
Caw Fell. Caw Fell is a fell in the English Lake District, standing between Haycock the Lank Rigg group. It occupies a wide upland area with Ennerdale to the north and Blengdale to the south. Caw Fell is distant from any point of access by Lakeland standards, but can be climbed from Blengdale or Bowness Knott car-parks. Topography.

Geographic entities mentioned:
surface_form: Lank Rigg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.494
lon: -3.403
surface_form: haycock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4844
lon: -3.32278
surface_form: caw fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.486
lon: -3.343
Caw Fell is distant from any point of access by Lakeland standards, but can be climbed from Blengdale or Bowness Knott car-parks. Topography. The Western Fells occupy a triangular sector of the Lake District, bordered by the River Cocker to the north east and Wasdale to the south east. Westwards the hills diminish toward the coastal plain of Cumberland.

Geographic entities mentioned:
surface_form: Wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Westwards the hills diminish toward the coastal plain of Cumberland. At the central hub of the high country are Great Gable and its satellites, while two principal ridges fan out on either flank of Ennerdale, the western fells in effect being a great horseshoe around this long wild valley. Caw Fell stands on the southern arm.

Geographic entities mentioned:
surface_form: Great Gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
Caw Fell stands on the southern arm. The main watershed runs broadly westwards from Great Gable, dividing the headwaters of Ennerdale and Wasdale. The main fells in this section are Kirk Fell, Pillar, Scoat Fell, Haycock and Caw Fell. The surrounding valleys gradually diverge until at Caw Fell they are apart and other rivers spring up to drain the intervening country.

Geographic entities mentioned:
surface_form: Wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
surface_form: great gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
Caw Fell stands on the southern arm. The main watershed runs broadly westwards from Great Gable, dividing the headwaters of Ennerdale and Wasdale. The main fells in this section are Kirk Fell, Pillar, Scoat Fell, Haycock and Caw Fell. The surrounding valleys gradually diverge until at Caw Fell they are apart and other rivers spring up to drain the intervening country.

Geographic entities mentioned:
surface_form: Kirk Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.242
surface_form: Scoat Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.490038888889
lon: -3.2998
surface_form: haycock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4844
lon: -3.32278
surface_form: pillar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.497
lon: -3.282
surface_form: caw fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.486
lon: -3.343
The Bleng rises to the south of Caw Fell, while Worm Gill drains the western slopes. The fell is therefore the end of the westerly run of the ridge, and the watershed curves north around the head of Worm Gill, crossing the subsidiary top of Iron Crag on the transit to Crag Fell and Lank Rigg.

Geographic entities mentioned:
surface_form: Crag Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.517
lon: -3.397
surface_form: Lank Rigg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.494
lon: -3.403
surface_form: iron crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4951
lon: -3.35506
The heathery spur of Tongue End runs parallel to the east. West of the summit a broad ridge descends steeply to Worm Gill, a craggy bowl scooped out on the northern side above the tributary of Bleaberry Gill. Running due north between this corrie and Silver Cove is the ridge of Iron Crag, making the whole summit area resemble an inverted 'T' in plan.

Geographic entities mentioned:
surface_form: Iron Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4951
lon: -3.35506
The fell is therefore the end of the westerly run of the ridge, and the watershed curves north around the head of Worm Gill, crossing the subsidiary top of Iron Crag on the transit to Crag Fell and Lank Rigg. The unnamed col connecting Caw Fell to Haycock is flat topped and carries the Ennerdale Fence, in this section a substantial dry stone wall.

Geographic entities mentioned:
surface_form: haycock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4844
lon: -3.32278
surface_form: caw fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.486
lon: -3.343
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
Caw Fell. Caw Fell is a fell in the English Lake District, standing between Haycock the Lank Rigg group. It occupies a wide upland area with Ennerdale to the north and Blengdale to the south. Caw Fell is distant from any point of access by Lakeland standards, but can be climbed from Blengdale or Bowness Knott car-parks. Topography.

Geographic entities mentioned:
surface_form: knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.686211111111
lon: -3.0935388888889
surface_form: caw fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.486
lon: -3.343
From this top the ridge swings west again, the rough northern flanks running above the shore of Ennerdale Water. The main features here are Mart Knott, Stair Knott and Boat How. The ridge now meets the headwaters of the River Calder and divides to embrace the valley, Crag Fell to the north and Lank Rigg to the south.

Geographic entities mentioned:
surface_form: knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.686211111111
lon: -3.0935388888889
surface_form: knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.686211111111
lon: -3.0935388888889
It is necessary to cross the wall to take in the full view. Ascents. The south west ridge over Stockdale Moor can be followed from the car park at Bleng Bridge, this being over each way. From Bowness Knott in Ennerdale, Caw Fell can be reached in a similar distance via the Tongue End spur. Indirect ascents can be made via Grike and Crag Fell from the Kinniside Stone Circle.

Geographic entities mentioned:
surface_form: knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.686211111111
lon: -3.0935388888889
surface_form: caw fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.486
lon: -3.343
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
Caw Fell. Caw Fell is a fell in the English Lake District, standing between Haycock the Lank Rigg group. It occupies a wide upland area with Ennerdale to the north and Blengdale to the south. Caw Fell is distant from any point of access by Lakeland standards, but can be climbed from Blengdale or Bowness Knott car-parks. Topography.

Geographic entities mentioned:
surface_form: caw fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.486
lon: -3.343
At the central hub of the high country are Great Gable and its satellites, while two principal ridges fan out on either flank of Ennerdale, the western fells in effect being a great horseshoe around this long wild valley. Caw Fell stands on the southern arm. The main watershed runs broadly westwards from Great Gable, dividing the headwaters of Ennerdale and Wasdale.

Geographic entities mentioned:
surface_form: caw fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.486
lon: -3.343
The main fells in this section are Kirk Fell, Pillar, Scoat Fell, Haycock and Caw Fell. The surrounding valleys gradually diverge until at Caw Fell they are apart and other rivers spring up to drain the intervening country. The Bleng rises to the south of Caw Fell, while Worm Gill drains the western slopes.

Geographic entities mentioned:
surface_form: caw fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.486
lon: -3.343
The ridge now meets the headwaters of the River Calder and divides to embrace the valley, Crag Fell to the north and Lank Rigg to the south. Caw Fell also has a lower level south west ridge, running down between the River Bleng and Worm Gill. This descends first to Stockdale Moor, a site littered with tumuli, hut circles, enclosures and other remnants of ancient habitation.

Geographic entities mentioned:
surface_form: caw fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.486
lon: -3.343
The main features here are Mart Knott, Stair Knott and Boat How. The ridge now meets the headwaters of the River Calder and divides to embrace the valley, Crag Fell to the north and Lank Rigg to the south. Caw Fell also has a lower level south west ridge, running down between the River Bleng and Worm Gill.

Geographic entities mentioned:
surface_form: crag fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.517
lon: -3.397
surface_form: lank rigg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.494
lon: -3.403
It is necessary to cross the wall to take in the full view. Ascents. The south west ridge over Stockdale Moor can be followed from the car park at Bleng Bridge, this being over each way. From Bowness Knott in Ennerdale, Caw Fell can be reached in a similar distance via the Tongue End spur. Indirect ascents can be made via Grike and Crag Fell from the Kinniside Stone Circle.

Geographic entities mentioned:
surface_form: crag fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.517
lon: -3.397
surface_form: grike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.513
lon: -3.415
Running due north between this corrie and Silver Cove is the ridge of Iron Crag, making the whole summit area resemble an inverted 'T' in plan. A narrow and steep sided col at provides Iron Crag with considerably more prominence than its parent, a small tarn lying on the northern slope. The rock face giving Iron Crag its name overlooks Silver Cove, but is not particularly prominent.

Geographic entities mentioned:
surface_form: iron crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4951
lon: -3.35506
A narrow and steep sided col at provides Iron Crag with considerably more prominence than its parent, a small tarn lying on the northern slope. The rock face giving Iron Crag its name overlooks Silver Cove, but is not particularly prominent. From this top the ridge swings west again, the rough northern flanks running above the shore of Ennerdale Water.

Geographic entities mentioned:
surface_form: iron crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4951
lon: -3.35506
Geology. The north eastern flanks are overlain by drift deposits with the plagioclase-phyric andesite lavas of the Birker Fell Formation beneath. The rest of the fell exhibits rock of the Ennerdale Intrusion, granophyric granite. Iron Crag Mine operated below the crag of that name from around 1864 to 1896.

Geographic entities mentioned:
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
Caw Fell. Caw Fell is a fell in the English Lake District, standing between Haycock the Lank Rigg group. It occupies a wide upland area with Ennerdale to the north and Blengdale to the south. Caw Fell is distant from any point of access by Lakeland standards, but can be climbed from Blengdale or Bowness Knott car-parks. Topography.

Geographic entities mentioned:
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
The unnamed col connecting Caw Fell to Haycock is flat topped and carries the Ennerdale Fence, in this section a substantial dry stone wall. Tongue Gill, the principal headwater of the Bleng, flows from the southern side of the saddle while on the opposite side is the steep headwall of Silver Cove, a deeply enclosed side-valley running into Ennerdale.

Geographic entities mentioned:
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
surface_form: the saddle
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.162395
lon: -5.414721
The rock face giving Iron Crag its name overlooks Silver Cove, but is not particularly prominent. From this top the ridge swings west again, the rough northern flanks running above the shore of Ennerdale Water. The main features here are Mart Knott, Stair Knott and Boat How.

Geographic entities mentioned:
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
Monte Penice. Monte Penice is a mountain of Lombardy and Emilia-Romagna in Italy. It has an elevation of above sea level and belongs to the Ligurian Apennines.

Geographic entities mentioned:
surface_form: monte penice
instance_of: Mountain
countries: Italy
coordinates: lat: 44.78444444
lon: 9.31694444
The tephra was primarily composed of alkali carbonatite, making it the earliest well-documented example of premodern natrocarbonatite volcanism. The main carbonate mineral was nyerereite, which is also the major mineral in present natrocarbonatite lava flows from the neighboring volcano Oldoinyo Lengai.

Geographic entities mentioned:
surface_form: Oldoinyo Lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
Paphiopedilum dayanum. &quot;Paphiopedilum dayanum&quot; is a species of orchid endemic to Mount Kinabalu on Borneo. Taxonomy. It was named by John Lindley in &quot;Morph. Stud. Orchideenbl.:&quot; 11 in 1886.

Geographic entities mentioned:
surface_form: Mount Kinabalu
instance_of: Mountain
countries: Malaysia
coordinates: lat: 6.075
lon: 116.5586111111111
The school's presence was a major economic resource for the local people. There was a Subway restaurant on the school's campus, one of three on the island. The Picard River is a river in Dominica. It rises on the northern slopes of Morne Diablotins, flowing northwest to reach the Caribbean Sea at Prince Rupert Bay on the country's northwestern coast, close to the town of Portsmouth.

Geographic entities mentioned:
surface_form: Morne Diablotins
instance_of: Mountain
countries: Dominica
coordinates: lat: 15.503333333333
lon: -61.397222222222
Opheim Hills. The Opheim Hills, el., is a set of hills northwest of Opheim, Montana in Valley County, Montana, United States.

Geographic entities mentioned:
surface_form: opheim hills
instance_of: Landform
countries: United States
coordinates: lat: 48.8819
lon: -106.512
In the deal, two tracts of land owned by the State of Rhode Island&mdash;the &quot;Camp Pastore&quot; property in Charlestown (of along the northwest shoreline of Watchaug Pond) and the &quot;Stedman&quot; property (abutting the refuge in Kingstown&mdash;were added to the refuge grounds.

Geographic entities mentioned:
surface_form: Watchaug Pond
instance_of: Lake
countries: United States
coordinates: lat: 41.383433333333
lon: -71.689786111111
Sròn a' Choire Ghairbh. Sròn a’ Choire Ghairbh is a Scottish mountain situated on the northern side of Loch Lochy, 13 kilometres north of Spean Bridge in the Highland Council area. Overview. Sròn a’ Choire Ghairbh reaches a height of 937 metres (3074 feet) and is classified as both a Munro and a Marilyn.

Geographic entities mentioned:
surface_form: Loch Lochy
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.968611111111
lon: -4.9105555555556
surface_form: sròn a’ choire ghairbh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.00784
lon: -4.928747
Overview. Sròn a’ Choire Ghairbh reaches a height of 937 metres (3074 feet) and is classified as both a Munro and a Marilyn. It is highest of the Loch Lochy hills and is invariably climbed along with the neighbouring Munro of Meall na Teanga to which it is joined by the distinctive col of Càm Bhealach.

Geographic entities mentioned:
surface_form: Meall na Teanga
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.989012
lon: -4.930955
surface_form: loch lochy
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.968611111111
lon: -4.9105555555556
Another ridge called Meall a’ Choire Ghlais goes north and then north east along the other side of Coire Glas, it loses very little height for two kilometres before descending steeply and rockily to the Bealach Easain (548 metres) which connects it to the Corbett Ben Tee.

Geographic entities mentioned:
surface_form: Ben Tee
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.032511
lon: -4.899216
surface_form: ben tee
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.032511
lon: -4.899216
Càm Bhealach is seen as a distinct notch in the skyline between the two Munros whether viewed from the east or the west. To the north is the small Coire an Eich which drains north into Glen Garry to find its way to the sea at the east coast via Loch Oich and Loch Ness.

Geographic entities mentioned:
surface_form: Loch Oich
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.069478
lon: -4.770802
surface_form: Loch Ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
surface_form: ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
surface_form: loch ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
surface_form: loch oich
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.069478
lon: -4.770802
To the north is the small Coire an Eich which drains north into Glen Garry to find its way to the sea at the east coast via Loch Oich and Loch Ness. Sròn a’ Choire Ghairbh is on the main east-west watershed of Scotland with rainfall on all other parts of the hill going to the west coast via Loch Lochy and Loch Linnhe.

Geographic entities mentioned:
surface_form: Loch Lochy
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.968611111111
lon: -4.9105555555556
surface_form: loch lochy
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.968611111111
lon: -4.9105555555556
The mountain has a substantial prominence of 622 metres ensuring that the summit is a fine viewpoint for the surrounding mountains of Lochaber and beyond. Sròn a’ Choire Ghairbh is one of the few hills in Scotland that has a visitors book at its summit (Mam Sodhail being one of the others). The book is kept in a coffee jar inside a wooden box and is maintained by Richard Wood of Invergarry.

Geographic entities mentioned:
surface_form: Mam Sodhail
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.279801
lon: -5.120267
surface_form: mam sodhail
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.279801
lon: -5.120267
The book is kept in a coffee jar inside a wooden box and is maintained by Richard Wood of Invergarry. The two Loch Lochy Munros are sometimes climbed by travellers on the Great Glen Way between Fort William and Inverness, the two hills offering variety on what is a low level multi day walk.

Geographic entities mentioned:
surface_form: the great glen
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
surface_form: great glen
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
It is highest of the Loch Lochy hills and is invariably climbed along with the neighbouring Munro of Meall na Teanga to which it is joined by the distinctive col of Càm Bhealach. Both these hills which are often referred to as the Loch Lochy Munros are well seen from the A82 road on the opposite side of the loch, showing steep slopes which are forested below the 300 metre contour.

Geographic entities mentioned:
surface_form: loch lochy
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.968611111111
lon: -4.9105555555556
The mountain is horseshoe shaped and throws down two ridges on either side of the corrie, the lengthy east ridge is five kilometres long and goes over the two subsidiary tops of Sean Mheall (888 metres) and Meall nan Dearcag (693 metres) before descending to the Kilfinnan Burn at the north end of Loch Lochy.

Geographic entities mentioned:
surface_form: loch lochy
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.968611111111
lon: -4.9105555555556
Sròn a’ Choire Ghairbh is on the main east-west watershed of Scotland with rainfall on all other parts of the hill going to the west coast via Loch Lochy and Loch Linnhe. A 1.5 GW pumped-storage hydroelectricity project storing 24 hours of power is planned to connect Coire Glas with Loch Lochy. Ascents.

Geographic entities mentioned:
surface_form: loch lochy
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.968611111111
lon: -4.9105555555556
The southern approach starts at the car park at the Eas Cia-aig waterfall on the B8005 at grid reference, Gleann Cia-aig is ascended to its head where Càm Bhealach is clearly in view. The approach from the north east starts at the car park at Laggan Locks just off the A82 at grid reference and takes the rising track through the forest on Loch Lochy’s northern side to reach Càm Bhealach.

Geographic entities mentioned:
surface_form: loch lochy
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.968611111111
lon: -4.9105555555556
In all other directions the mountain is steep and grassy, to the south lies Càm Bhealach, a mountain pass between Sròn a’ Choire Ghairbh and the Munro Meall na Teanga. Càm Bhealach is seen as a distinct notch in the skyline between the two Munros whether viewed from the east or the west.

Geographic entities mentioned:
surface_form: meall na teanga
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.989012
lon: -4.930955
surface_form: sròn a’ choire ghairbh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.00784
lon: -4.928747
Overview. Sròn a’ Choire Ghairbh reaches a height of 937 metres (3074 feet) and is classified as both a Munro and a Marilyn. It is highest of the Loch Lochy hills and is invariably climbed along with the neighbouring Munro of Meall na Teanga to which it is joined by the distinctive col of Càm Bhealach.

Geographic entities mentioned:
surface_form: sròn a’ choire ghairbh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.00784
lon: -4.928747
Sròn a' Choire Ghairbh. Sròn a’ Choire Ghairbh is a Scottish mountain situated on the northern side of Loch Lochy, 13 kilometres north of Spean Bridge in the Highland Council area. Overview. Sròn a’ Choire Ghairbh reaches a height of 937 metres (3074 feet) and is classified as both a Munro and a Marilyn.

Geographic entities mentioned:
surface_form: sròn a' choire ghairbh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.00784
lon: -4.928747
Enăchiuc claimed that the text had been written in the Dacian dialect of vulgar Latin, and the direction of writing is right-to-left, bottom-to-top. The alleged translation indicates that the text is an history of the Blaki (Vlachs) people in their fights against Hungarians and Pechenegs. Toponyms and hydronyms appear as Arad, Dridu, Olbia, Ineu, Rarău, Nistru (Dniester) and Tisa (Tisza).

Geographic entities mentioned:
surface_form: Rarău
instance_of: Mountain
countries: Romania
coordinates: lat: 47.452271
lon: 25.573878
Woronora Dam was completed in 1941 at a cost of about 13 million. The dam is the only one of Sydney's water supply dams which is not part of the Upper Nepean/Warragamba/Shoalhaven interconnected system. The dam was built with the objective of supplementing Sydney's water supply whilst the much larger Warragamba Dam was constructed.

Geographic entities mentioned:
surface_form: Shoalhaven
instance_of: Lake
countries: Australia
It is located in the Junín Region, Huancayo Province, Chongos Alto District. Wira Challwa lies west of Waqra Willka. The little lake named Wira Challwa lies northeast of the mountain at.

Geographic entities mentioned:
surface_form: Waqra Willka
instance_of: Mountain
countries: Peru
coordinates: lat: -12.4758
lon: -75.4017
surface_form: wira challwa
instance_of: Mountain
countries: Peru
coordinates: lat: -12.4819
lon: -75.4294
Wira Challwa. Wira Challwa (Quechua &quot;wira&quot; fat, &quot;challwa&quot; fish, &quot;fat fish&quot;, Hispanicized spelling &quot;Huirachaygua&quot;) is a mountain in the Andes of Peru and the name of a small lake near of the mountain. It is located in the Junín Region, Huancayo Province, Chongos Alto District. Wira Challwa lies west of Waqra Willka.

Geographic entities mentioned:
surface_form: wira challwa
instance_of: Mountain
countries: Peru
coordinates: lat: -12.4819
lon: -75.4294
Imagbon. Imagbon is a town located in Ogun State, Nigeria. It lies on the western frontiers of Ijebu-Ode, along a river tributary of the Lagos Lagoon. Imagbon War. The definitive Imagbon War, also referred to as the Anglo-ljebu War, occurred in 1892 in the town, between Ijebu forces and the Imperial British military.

Geographic entities mentioned:
surface_form: Lagos Lagoon
instance_of: Lake
countries: Nigeria
coordinates: lat: 6.5015814
lon: 3.5224915
It developed as a port around the 15th century AD. The port was used for the coastal trade between northern Odisha and Kolkata to the northeast, and continued to be used to a small extent after independence in 1947. During April, 1998, an agreement was signed to develop the Port of Dhamara, about seven kilometers away on the coast of the Bay of Bengal, as a deep water port. Roads.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Mabeskraal. Mabeskraal is a town in Bojanala District Municipality in the North West province of South Africa. Mabeskraal is approximately 72 km from the city of Rustenburg and near to the Pilanesberg and Sun City area.

Geographic entities mentioned:
surface_form: Pilanesberg
instance_of: Mountain
countries: South Africa
coordinates: lat: -25.240277777778
lon: 27.075833333333
These mountains are believed to have formed the southernmost part (southwards starting from the Mangalore region) of the Western Ghats, modern day Kerala, while the Northern part of the same was called the Sahya Mountains. The peaks of these Malaya mountains were said to be higher than those of the Sahya Mounta. Sangam Literature calls these mountains Pothigai.

Geographic entities mentioned:
surface_form: Pothigai
instance_of: Mountain
countries: India
coordinates: lat: 8.6166916666667
lon: 77.24625
New TTC routes since the 1940s have generally been operated by other modes of transportation, and the less busy streetcar routes have also been converted. Streetcar routes are now focused on the downtown area, although two run farther from the core: one being on St. Clair Avenue, from Lake Ontario on average, served by the 512 St.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Songgwangsa. Songgwangsa (; translation: Spreading Pine Temple; alternates: Songgwang-sa, or Songgwang Sa, or Songkwangsa; also known as: Piney Expanse Monastery; originally: Gilsangsa), one of the three jewels of Seon Buddhism, is located in South Jeolla Province on Mount Jogye on the Korean Peninsula. Situated approximately away from the sea, it is within the Jogyesan Provincial Park.

Geographic entities mentioned:
surface_form: Jogyesan
instance_of: Mountain
countries: South Korea
coordinates: lat: 35.0025
lon: 127.31361111
Geography. Songgwangsa is located on the west side of Jogyesan in Songgwang-myeon, Suncheon, South Jeolla Province, South Korea. Seonamsa, a quieter hermitage dating to 529, lies on the eastern side of Janggunbong Mountain at, also within the Jogyesan Provincial Park. Songgwangsa, located between Chongju and Maisan, is accessible via Chonju city bus or taxi.

Geographic entities mentioned:
surface_form: Jogyesan
instance_of: Mountain
countries: South Korea
coordinates: lat: 35.0025
lon: 127.31361111
His record as of December 2017 was 10–3–2. He went on to help at risk youth, joining Ring of Hope Boxing. Early life. Zachary Wohlman was Jewish, and was born in the San Fernando Valley of Los Angeles to David Wohlman and his wife, a beautician. He lived in Northridge, Reseda, and Woodland Hills, California.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
The Treaty of Paris in 1783 freed Umfreville and he arrived in London. Disputes between him and the HBC ended his tenure there and he left for Quebec. By May 1784, he was employed by the North West Company to search for an alternate canoe route from Lake Superior to Lake Winnipeg, since the usual route along the Grand Portage and Pigeon River had come under American control.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
In 2013, along with the Fort Caswell Rifle Range constructed during WWI, it was designated as a National Historic District. In the early 1800s, in recognition of the dangers to navigation caused by Frying Pan Shoals, Jay Bird Shoals, and Bald Head Shoals, which lay south and southeast of the island, construction of a series of lighthouses and life saving stations in the area began.

Geographic entities mentioned:
surface_form: Frying Pan Shoals
instance_of: Landform
countries: United States
coordinates: lat: 33.80111111
lon: -77.94694444
Walton in Gordano. Walton in Gordano is a village and civil parish in the North Somerset district, in the ceremonial county of Somerset, England. It is situated in a small valley at the side of the south-western end of the Gordano Valley, about a mile from Clevedon. In 2011 the parish had a population of 273. History. The parish of Walton was part of the Portbury Hundred. Governance.

Geographic entities mentioned:
surface_form: Gordano Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.45315
lon: -2.8145111111111
Junker describes coastal polities of Tondo and Maynila's size as &quot;administrative and commercial centers functioning as important nodes in networks of external and internal trade.&quot; While the basic model for the movement of trade goods in early Philippine history saw coastal settlements at the mouth of large rivers (in this case, the Pasig river delta) controlling the flow of goods to and from settlements further upriver (in this case, the upland lakeside barangays of Laguna de Bay), Tondo and Maynila had trade arrangements which allowed them to control trade throughout the rest of the archipelago.

Geographic entities mentioned:
surface_form: Laguna de Bay
instance_of: Lake
countries: Philippines
coordinates: lat: 14.508888888889
lon: 121.11888888889
Isolation. &quot;T. celer&quot; was discovered by Dr. Wolfram Zillig in 1983. The organism was isolated on the beaches of Vulcano, Italy, from a sulfur-rich shallow volcanic crater. Original samples were isolated from the depths of the marine holes and inoculated into 10-ml anaerobic tubes. The tubes contained 100 mg of elemental sulfur and a solution of 95% N2 and 5% H2S.

Geographic entities mentioned:
surface_form: Vulcano
instance_of: Mountain
countries: Italy
coordinates: lat: 38.4042
lon: 14.9658
History. In 1925, Carl Laemmle purchased land on the northwest corner of Hollywood and Vine from George Hoover for $350,000. Laemmle, then president of Universal Pictures Corporation, owned a successful movie studio in the San Fernando Valley and planned to build a 900-seat theatre and office tower on this property, but the Great Depression thwarted his plan.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
The Cariboo Plateau is a volcanic plateau in south-central British Columbia, Canada. It is part of the Fraser Plateau which is a northward extension of the North American Plateau. The southern limit of the plateau is the Bonaparte River although some definitions include the Bonaparte Plateau between that river and the Thompson, but it properly is a subdivision of the Thompson Plateau.

Geographic entities mentioned:
surface_form: Fraser Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 52
lon: -123
The Cariboo Plateau is a volcanic plateau in south-central British Columbia, Canada. It is part of the Fraser Plateau which is a northward extension of the North American Plateau. The southern limit of the plateau is the Bonaparte River although some definitions include the Bonaparte Plateau between that river and the Thompson, but it properly is a subdivision of the Thompson Plateau.

Geographic entities mentioned:
surface_form: Bonaparte Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 51.15
lon: -121.283
surface_form: Thompson Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 50.25
lon: -120.5
The portion of the Fraser Plateau west of the Fraser River is properly known as the Chilcotin Plateau but is often mistakenly considered to be part of the Cariboo Plateau, which is east of the Fraser.

Geographic entities mentioned:
surface_form: Chilcotin Plateau
instance_of: Mountain
countries: Canada
coordinates: lat: 52.166666666666664
lon: -123.41666666666667
surface_form: cariboo plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 50.81652
lon: -118.81904
The Cariboo region is generally considered to reach as far southeast as the city of Kamloops and to include the Cache Creek and Lillooet areas in the south. The region west of the Fraser River north of Lillooet, the Chilcotin, is often considered to be a part of the Cariboo; the country south of it immediately west of Lillooet is sometimes referred to as the West Cariboo.

Geographic entities mentioned:
surface_form: Chilcotin
instance_of: Mountain
countries: Canada
coordinates: lat: 52.166666666666664
lon: -123.41666666666667
The region west of the Fraser River north of Lillooet, the Chilcotin, is often considered to be a part of the Cariboo; the country south of it immediately west of Lillooet is sometimes referred to as the West Cariboo. The Cariboo Plateau is made of Late Miocene flood basalt lavas of the Chilcotin Group, a group of related volcanic rocks that is nearly parallel with the Fraser Plateau.

Geographic entities mentioned:
surface_form: Fraser Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 52
lon: -123
The Cariboo Plateau is made of Late Miocene flood basalt lavas of the Chilcotin Group, a group of related volcanic rocks that is nearly parallel with the Fraser Plateau. It extends along the adjacent Garibaldi Volcanic Belt in the Coast Mountains. Volcanism of the Cariboo Plateau is considered to be a result of extension of the crust behind the coastal Cascadia subduction zone.

Geographic entities mentioned:
surface_form: Garibaldi Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5283
lon: -126.113
Volcanism of the Cariboo Plateau is considered to be a result of extension of the crust behind the coastal Cascadia subduction zone. The Last Chance Lake and the Goodenough Lake beside it in the Bonaparte Plateau, as well as the Probe Lake and the Deer Lake in the Cariboo Plateau, are soda lakes. &quot;The Cariboo Trail&quot; is a 1950 film about the gold rush era of the 1890s in the area.

Geographic entities mentioned:
surface_form: Bonaparte Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 51.15
lon: -121.283
surface_form: cariboo plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 50.81652
lon: -118.81904
surface_form: bonaparte plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 51.15
lon: -121.283
Cariboo Plateau. The Cariboo Plateau is a volcanic plateau in south-central British Columbia, Canada. It is part of the Fraser Plateau which is a northward extension of the North American Plateau.

Geographic entities mentioned:
surface_form: cariboo plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 50.81652
lon: -118.81904
Cariboo Plateau. The Cariboo Plateau is a volcanic plateau in south-central British Columbia, Canada. It is part of the Fraser Plateau which is a northward extension of the North American Plateau.

Geographic entities mentioned:
surface_form: cariboo plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 50.81652
lon: -118.81904
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
It extends along the adjacent Garibaldi Volcanic Belt in the Coast Mountains. Volcanism of the Cariboo Plateau is considered to be a result of extension of the crust behind the coastal Cascadia subduction zone. The Last Chance Lake and the Goodenough Lake beside it in the Bonaparte Plateau, as well as the Probe Lake and the Deer Lake in the Cariboo Plateau, are soda lakes.

Geographic entities mentioned:
surface_form: cariboo plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 50.81652
lon: -118.81904