Sarmila/GeoWiki-Features huggingface dataset:
The storm forced the closure of Sir Seewoosagur Ramgoolam International Airport, along with schools and government offices. Wind gusts on Mauritius reached. Gerry dropped heavy rainfall, peaking at at Mare aux Vacoas, and it produced high waves along the northern coast. One person was killed who was electrocuted during the storm's passage. Tropical Cyclone Hape.

Geographic entities mentioned:
surface_form: Mare aux Vacoas
instance_of: Lake
countries: Mauritius
coordinates: lat: -20.366666666667
lon: 57.5
Malakand Agency. The Malakand Agency () was one of the agencies in the North West Frontier Province of British India and later of Pakistan until 2010. It included the princely states of Chitral, Dir and Swat, and an area around the Malakand Pass known as the Malakand Protected Area. The largest city in the area was Mingora, while the three state capitals were Chitral, Dir, and Saidu Sharif.

Geographic entities mentioned:
surface_form: Chitral
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.85111111111111
lon: 71.78888888888889
The main island, named Cuba, is long, constituting most of the nation's land area () and is the largest island in the Caribbean and 17th-largest island in the world by land area. The main island consists mostly of flat to rolling plains apart from the Sierra Maestra mountains in the southeast, whose highest point is Pico Turquino ().

Geographic entities mentioned:
surface_form: Pico Turquino
instance_of: Mountain
countries: Cuba
coordinates: lat: 19.989444444444
lon: -76.835833333333
The refuge was established (along with 3 other refuges in the Willamette Valley of Oregon) in 1965, in response to a need to establish vital winter habitat for wintering waterfowl with an emphasis on the dusky Canada goose whose nesting areas in Alaska were severely impacted by the violent earthquake of 1964.

Geographic entities mentioned:
surface_form: Willamette Valley of Oregon
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Natural attractions. The majestic valleys, rivers, springs, waterfalls, colorful vegetation, diversity of wildlife, thermal springs, summer quarters and rural settlements appeal to visitors. Mount Damavand, 5610 m, the highest point in the Middle East
Lar and Damavand Mountains. These mountains form the two branch ranges of the central Alborz Mountains, and are the highest sections of this range.

Geographic entities mentioned:
surface_form: Mount Damavand
instance_of: Mountain
countries: Iran
coordinates: lat: 35.955277777778
lon: 52.109166666667
Haraz River. The Haraz River's source is in the skirts of the Alborz Mountains in the region of Larijan. After flowing along the Haraz Road and Valley for about 100 km. it meanders in the midst of the city of Amol, from where it reaches the Caspian Sea. The fringes of this river are utilized as recreational areas as well as for fishing. Waterfall.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
The Sankenbach flows over the waterfalls, dropping a total of 40 metres. The falls drop down the headwall of the cirque of the Sankenbach Bowl (&quot;Sankenbachkessel&quot;) in the Eckscher Horizon (&quot;Eck’scher Horizont&quot;) of the Lower Bunter Sandstone. Shortly afterwards the Sankenbach feeds the Sankenbachsee.

Geographic entities mentioned:
surface_form: Sankenbachsee
instance_of: Lake
countries: Germany
coordinates: lat: 48.484
lon: 8.33844
It is a wetland of national significance. On the rare occasions when Lake Hindmarsh overflows, water runs, via Outlet Creek (Wergaia: &quot;Krumelak&quot;), to the deeper Lake Albacutya (Wergaia: &quot;Ngelbakutya&quot;), which has been recognised under the Ramsar Convention as a wetland of international importance. Flat and shallow, Lake Hindmarsh is subject to very high evaporation.

Geographic entities mentioned:
surface_form: Lake Albacutya
instance_of: Lake
countries: Australia
coordinates: lat: -35.75
lon: 141.967
surface_form: lake albacutya
instance_of: Lake
countries: Australia
coordinates: lat: -35.75
lon: 141.967
surface_form: lake hindmarsh
instance_of: Lake
countries: Australia
coordinates: lat: -36.0667
lon: 141.917
surface_form: lake hindmarsh
instance_of: Lake
countries: Australia
coordinates: lat: -36.0667
lon: 141.917
Lake Hindmarsh. Lake Hindmarsh, an ephemeral lake located in the Wimmera region of western Victoria, Australia, is the state's largest natural freshwater lake. The nearest towns are Jeparit to the south and Rainbow to the north. After more than a decade of drought, in early 2011 the lake filled as a result of flooding in the region.

Geographic entities mentioned:
surface_form: lake hindmarsh
instance_of: Lake
countries: Australia
coordinates: lat: -36.0667
lon: 141.917
The lake filled again in 1996, but then received no further water from the Wimmera River, and had dried up by 2000. It remained dry for almost a decade. In October 2009, water from the Wimmera River trickled into Lake Hindmarsh for the first time in thirteen years. The 2010 Victorian floods of September raised lake water levels higher and triggered a revival of birdlife.

Geographic entities mentioned:
surface_form: lake hindmarsh
instance_of: Lake
countries: Australia
coordinates: lat: -36.0667
lon: 141.917
Dalcheon. Dalcheon () is a river of South Korea. It is a river of the Han River system. A tributary of the Namhan River, it is one of the few Namhan tributaries that are navigable year round.

Geographic entities mentioned:
surface_form: dalcheon
instance_of: Watercourse
countries: South Korea
coordinates: lat: 36.9833
lon: 127.883
Mount Charles, Jamaica. Mount Charles is a high hill in St Elizabeth, Westmoreland Parish, Jamaica.

Geographic entities mentioned:
surface_form: mount charles, jamaica
instance_of: Mountain
countries: Jamaica
coordinates: lat: 18.18
lon: -78.03
Mount Charles, Jamaica. Mount Charles is a high hill in St Elizabeth, Westmoreland Parish, Jamaica.

Geographic entities mentioned:
surface_form: mount charles
instance_of: Mountain
countries: Jamaica
coordinates: lat: 18.18
lon: -78.03
Robinson (Lake District). Robinson is a fell in the English Lake District, its southern slopes descending to Buttermere, while its northern side is set in the Newlands Valley. Paths lead to the summit from the village of Buttermere, from the nearby summit Dale Head and from various locations in the valleys to the north. Name.

Geographic entities mentioned:
surface_form: Buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: Newlands Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.573011111111
lon: -3.1848694444444
surface_form: robinson
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.54
lon: -3.236
Robinson (Lake District). Robinson is a fell in the English Lake District, its southern slopes descending to Buttermere, while its northern side is set in the Newlands Valley. Paths lead to the summit from the village of Buttermere, from the nearby summit Dale Head and from various locations in the valleys to the north. Name.

Geographic entities mentioned:
surface_form: Buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: Dale Head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527
lon: -3.2020805555556
Two roads cross from east to west, dividing the fells into three convenient groups. Robinson stands in the southern sector. The principal ridge in this group of fells runs east from Buttermere, climbing over Robinson, Hindscarth and Dale Head. It then turns north, descending gradually toward Derwentwater, the main tops being High Spy, Maiden Moor and Catbells.

Geographic entities mentioned:
surface_form: Hindscarth
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.537661111111
lon: -3.2147611111111
surface_form: dale head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527
lon: -3.2020805555556
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: robinson
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.54
lon: -3.236
surface_form: hindscarth
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.537661111111
lon: -3.2147611111111
Robinson stands in the southern sector. The principal ridge in this group of fells runs east from Buttermere, climbing over Robinson, Hindscarth and Dale Head. It then turns north, descending gradually toward Derwentwater, the main tops being High Spy, Maiden Moor and Catbells. Robinson appears bland from Buttermere, smooth rounded slopes curving up from the valley floor.

Geographic entities mentioned:
surface_form: Derwentwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.583333333333
lon: -3.15
surface_form: High Spy
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.534
lon: -3.185
surface_form: Maiden Moor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5532
lon: -3.18275
surface_form: catbells
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5686
lon: -3.17083
surface_form: derwentwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.583333333333
lon: -3.15
surface_form: high spy
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.534
lon: -3.185
surface_form: maiden moor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5532
lon: -3.18275
There has been considerable mining activity in the vicinity, particularly at the Goldscope Mine, but this has all taken place beneath the slopes of neighbouring Hindscarth. The remains of a small reservoir can still be seen in Little Dale. Robinson itself has a pair of short levels driven for lead, near to the south east corner of Buttermere lake. They appear not to have progressed beyond trials.

Geographic entities mentioned:
surface_form: Buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
Access can also be gained from the Honister Pass road, from a point near the first bridge over the beck at about. From here a direct line northward will bring the walker to Littledale Edge. The north east ridge provides an excellent walk from the Newlands valley, rising up successive steps. Finally, a great deal of height can be gained by car, if the fell is climbed from Newlands Hause.

Geographic entities mentioned:
surface_form: newlands valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.573011111111
lon: -3.1848694444444
Littledale Edge marks the beheading of the original dale by the more vigorous Buttermere valley, fed by ice escaping through Honister Pass from Borrowdale. This geologically recent deep incision has destabilised the slope. Summit. The top is rounded and mainly of grass, but there are two low outcrops of rock with loose stones between. The more westerly of these is the summit and bears a cairn.

Geographic entities mentioned:
surface_form: borrowdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.42
lon: -2.665
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
The mysterious Hackney Holes are now interpreted as the source of the largest 'rock slope failure' in the Lake District (1.3 km2), where most of the Buttermere-Gatesgarthdale trough wall has deformed and bulged downslope, leaving open trenches (the Holes) or, across the Little Dale col, a chevron pattern of short steep scarps; midslope, there are bold antiscarps (uphill-facing scarplets), a classic indicator.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
Name. According to influential guidebook author Alfred Wainwright, the name Robinson comes from a Richard Robinson who purchased estates in the Buttermere area many centuries ago. These included this unnamed hill which was then called &quot;Robinson's Fell&quot;, later shortened to Robinson. Topography.

Geographic entities mentioned:
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: robinson
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.54
lon: -3.236
surface_form: robinson
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.54
lon: -3.236
It then turns north, descending gradually toward Derwentwater, the main tops being High Spy, Maiden Moor and Catbells. Robinson appears bland from Buttermere, smooth rounded slopes curving up from the valley floor. Viewed from Keswick or Newlands to the north, its character is altogether different.

Geographic entities mentioned:
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
Viewed from Keswick or Newlands to the north, its character is altogether different. From here the wall of Robinson Crags drops from the summit of the fell, a great chunk of the hillside seemingly missing. The western flanks of the fell fall to Buttermere, the village itself standing on Robinson's territory.

Geographic entities mentioned:
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: robinson
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.54
lon: -3.236
The top and bottom sections are quite steep but the slope levels out at to accommodate Buttermere Moss, in Wainwright's words “ a wide marshy depression from which water cannot escape except by being carried away in the boots of pedestrians.” At the head of the lower slope is the subsidiary top of High Snockrigg (), a fine viewpoint for the Buttermere valley.

Geographic entities mentioned:
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
On the south western rim of the Moss is Goat Crag, overlooking Buttermere lake. To the south of Robinson are Gatesgarthdale Beck and the road up Honister Pass. This side of the fell presents a long and mainly featureless slope, although near the summit are the Hackney Holes, curious rocky depressions of uncertain origin (but see Geology section).

Geographic entities mentioned:
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
Beneath the nose of the ridge is the confluence of Scope Beck and Keskadale Beck. Keskadale forms the north western boundary of Robinson and is also the route of Newlands Pass, crossing the North Western Fells from Braithwaite to Buttermere. Its summit at Newlands Hause () lies beneath the northern edge of Buttermere Moss, from which the waterfall of Moss Force drops within easy reach of the road.

Geographic entities mentioned:
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: robinson
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.54
lon: -3.236
Keskadale forms the north western boundary of Robinson and is also the route of Newlands Pass, crossing the North Western Fells from Braithwaite to Buttermere. Its summit at Newlands Hause () lies beneath the northern edge of Buttermere Moss, from which the waterfall of Moss Force drops within easy reach of the road. Geology. Robinson's summit area is composed of rocks of the Buttermere Formation.

Geographic entities mentioned:
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
Its summit at Newlands Hause () lies beneath the northern edge of Buttermere Moss, from which the waterfall of Moss Force drops within easy reach of the road. Geology. Robinson's summit area is composed of rocks of the Buttermere Formation. This is an olistostrome of disrupted, sheared and folded mudstone, siltstone and sandstone.

Geographic entities mentioned:
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
There is another prominent cairn at the top of the north east ridge. From below this appears to be the summit, but disappointment awaits anyone so deceived by the convex slope. Fair paths run to Buttermere, Littledale Edge and the north east ridge, once the grass is reached. The view is robbed of foreground by the broad plateau of the summit, but serried ranks of fells appear in all directions.

Geographic entities mentioned:
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
Ascents. Buttermere Village provides a popular starting point, a good path leading up via High Snockrigg. Conditions deteriorate at the crossing of Buttermere Moss, followed by a stiff climb to the summit. Another route from Buttermere begins further south at Hassness, working around Goat Crag to join the main path above the moss.

Geographic entities mentioned:
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
Conditions deteriorate at the crossing of Buttermere Moss, followed by a stiff climb to the summit. Another route from Buttermere begins further south at Hassness, working around Goat Crag to join the main path above the moss. Access can also be gained from the Honister Pass road, from a point near the first bridge over the beck at about.

Geographic entities mentioned:
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
Robinson (Lake District). Robinson is a fell in the English Lake District, its southern slopes descending to Buttermere, while its northern side is set in the Newlands Valley. Paths lead to the summit from the village of Buttermere, from the nearby summit Dale Head and from various locations in the valleys to the north. Name.

Geographic entities mentioned:
surface_form: robinson
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.54
lon: -3.236
Name. According to influential guidebook author Alfred Wainwright, the name Robinson comes from a Richard Robinson who purchased estates in the Buttermere area many centuries ago. These included this unnamed hill which was then called &quot;Robinson's Fell&quot;, later shortened to Robinson. Topography.

Geographic entities mentioned:
surface_form: robinson
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.54
lon: -3.236
surface_form: robinson
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.54
lon: -3.236
Viewed from Keswick or Newlands to the north, its character is altogether different. From here the wall of Robinson Crags drops from the summit of the fell, a great chunk of the hillside seemingly missing. The western flanks of the fell fall to Buttermere, the village itself standing on Robinson's territory.

Geographic entities mentioned:
surface_form: robinson
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.54
lon: -3.236
On the south western rim of the Moss is Goat Crag, overlooking Buttermere lake. To the south of Robinson are Gatesgarthdale Beck and the road up Honister Pass. This side of the fell presents a long and mainly featureless slope, although near the summit are the Hackney Holes, curious rocky depressions of uncertain origin (but see Geology section).

Geographic entities mentioned:
surface_form: robinson
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.54
lon: -3.236
To the north of the Edge is a steady descent into the head of Little Dale, part of the Newlands catchment. This valley runs north east, flanked by parallel ridges descending from Robinson and Hindscarth, its stream being named Scope Beck. Robinson's north east ridge is rough and craggy towards the top before levelling out onto the grassy spur of High Snab Bank.

Geographic entities mentioned:
surface_form: robinson
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.54
lon: -3.236
surface_form: robinson
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.54
lon: -3.236
surface_form: hindscarth
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.537661111111
lon: -3.2147611111111
Geology. Robinson's summit area is composed of rocks of the Buttermere Formation. This is an olistostrome of disrupted, sheared and folded mudstone, siltstone and sandstone. West and north east of the summit are outcroppings of the Robinson Member. This comprises large olistoliths of greywacke sandstone, with interbedded mudstone and siltstone. The southern flanks are a large area of landslip.

Geographic entities mentioned:
surface_form: robinson
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.54
lon: -3.236
To the south of Robinson are Gatesgarthdale Beck and the road up Honister Pass. This side of the fell presents a long and mainly featureless slope, although near the summit are the Hackney Holes, curious rocky depressions of uncertain origin (but see Geology section). Running south east from the summit is Littledale Edge, an airy escarpment which connects to the neighbouring fell of Hindscarth.

Geographic entities mentioned:
surface_form: hindscarth
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.537661111111
lon: -3.2147611111111
This comprises large olistoliths of greywacke sandstone, with interbedded mudstone and siltstone. The southern flanks are a large area of landslip. There has been considerable mining activity in the vicinity, particularly at the Goldscope Mine, but this has all taken place beneath the slopes of neighbouring Hindscarth. The remains of a small reservoir can still be seen in Little Dale.

Geographic entities mentioned:
surface_form: hindscarth
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.537661111111
lon: -3.2147611111111
East Branch Moose River (Maine). The East Branch Moose River is a short tributary of the South Branch Moose River in Skinner (Maine Township 1, Range 7, WBKP), Maine. From its source () on Kibby Mountain, the river runs northwest to its confluence with the Moose River's South Branch.

Geographic entities mentioned:
surface_form: Kibby Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.4187
lon: -70.5443
Christensen retired as full professor in 1993 and moved to Mission, British Columbia. Electric power industries. Christensen was an active intervener in the National Energy Board (NEB) hearings which ultimately resulted in the rejection of the huge SE2 (Sumas Energy 2) coal-fired plant, one that would have emitted unacceptable pollution into the Fraser Valley funnel. Final years.

Geographic entities mentioned:
surface_form: Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
Lake Issyk. The Lake Issyk also known as Issyk Lake () is a lake in Kazakhstan fed by the Issyk River. History. It is estimated that the lake was formed about 8-10 millennia ago, as a result of a catastrophic earthquake that caused the collapse of the right slope of the gorge. After the collapse, debris blocked the gorge and created a dam about 300 meters tall.

Geographic entities mentioned:
surface_form: issyk
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 43.253055555556
lon: 77.484444444444
surface_form: lake issyk
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 43.253055555556
lon: 77.484444444444
Lake Issyk. The Lake Issyk also known as Issyk Lake () is a lake in Kazakhstan fed by the Issyk River. History. It is estimated that the lake was formed about 8-10 millennia ago, as a result of a catastrophic earthquake that caused the collapse of the right slope of the gorge. After the collapse, debris blocked the gorge and created a dam about 300 meters tall.

Geographic entities mentioned:
surface_form: issyk
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 43.253055555556
lon: 77.484444444444
surface_form: issyk
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 43.253055555556
lon: 77.484444444444
surface_form: issyk
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 43.253055555556
lon: 77.484444444444
surface_form: lake issyk
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 43.253055555556
lon: 77.484444444444
Beyond the lake rose a bold and steep jagged ridge of high squirrel... this mountain the guide called Issyk-bash.&quot;
The Caspian tiger was found in the Issyk gorge and around the lake at least at the beginning of the 1900s and is mentioned in the diaries of Pyotr Semyonov-Tyan-Shansky.

Geographic entities mentioned:
surface_form: issyk
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 43.253055555556
lon: 77.484444444444
surface_form: issyk
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 43.253055555556
lon: 77.484444444444
Threat to the lake due to the construction of a hydropower plant. In 2005, &quot;BTA Bank&quot; and a private company LLP &quot;EnergoAlem&quot; proposed a project to build more than four private hydroelectric power plants (HPPs) along the river below the Issyk Lake mudflow protection dam.

Geographic entities mentioned:
surface_form: issyk
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 43.253055555556
lon: 77.484444444444
In 2005, &quot;BTA Bank&quot; and a private company LLP &quot;EnergoAlem&quot; proposed a project to build more than four private hydroelectric power plants (HPPs) along the river below the Issyk Lake mudflow protection dam. The peculiarity of these HPPs is that their operation is possible only by regulating the flow in the river by discharging from the reservoir of Lake Issyk.

Geographic entities mentioned:
surface_form: issyk
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 43.253055555556
lon: 77.484444444444
surface_form: lake issyk
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 43.253055555556
lon: 77.484444444444
KChS responded to the appeal that &quot;KazSeleZashchita&quot; State Institution conducted a survey of the territory near the mudflow protection dam, which found that drilling and blasting operations were carried out behind the dam on Lake Issyk (downstream the Yesik River at a distance of about 250–300 meters).

Geographic entities mentioned:
surface_form: issyk
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 43.253055555556
lon: 77.484444444444
surface_form: lake issyk
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 43.253055555556
lon: 77.484444444444
The branch of the State Institution Kazselezaschita of the Ministry of Internal Affairs and the Department of Emergency Situations of Almaty Oblast were not notified of these works. The branch of GU Kazselezaschita KChS MIA initiates the issue of informing the prosecutor's office of Almaty region regarding the threat of violation of the integrity of the Issyk Lake mudflow retaining dam&quot;.

Geographic entities mentioned:
surface_form: issyk
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 43.253055555556
lon: 77.484444444444
860–880 Lake Shore Drive. 860–880 Lake Shore Drive is a twin pair of glass-and-steel apartment towers on N. Lake Shore Drive along Lake Michigan in the Streeterville neighborhood of Chicago, Illinois. Construction began in 1949 and the project was completed in 1951.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Cutthroat Lake. Cutthroat Lake is a lake in the Uinta Mountains in south‑central Summit County, Utah, United States. The lake is located within the Uinta-Wasatch-Cache National Forest and was so named on account of the lake being stocked with cutthroat trout.

Geographic entities mentioned:
surface_form: cutthroat lake
instance_of: Lake
countries: United States
coordinates: lat: 40.68138889
lon: -110.01
In addition, goldeneyes, mallards, goosanders, wigeons, teals, tufted ducks and great crested grebes can also be seen. History. During the nineteenth century, a drainage channel was dug, connecting Loch of Craiglush with Lowes, causing the water levels of the two lochs to equalise. The Lunan Burn now flows through this channel.

Geographic entities mentioned:
surface_form: Loch of Craiglush
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.581
lon: -3.5587
Geography. Loch of the Lowes forms part of a chain of lochs known as the Lunan Lochs. The Lunan Lochs are Lochs Craiglush, Lowes, Butterstone, Clunie and Marlee, and are connected by the Lunan Burn, which drains into the River Isla, itself a tributary of the River Tay.

Geographic entities mentioned:
surface_form: Craiglush
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.581
lon: -3.5587
surface_form: Butterstone
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.587
lon: -3.5335
surface_form: Clunie
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.583333333333
lon: -3.4333333333333
surface_form: Marlee
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.566666666667
lon: -3.4
Loch of the Lowes. Loch of the Lowes is a loch near Dunkeld in Perth and Kinross, Scotland. The loch and the surrounding area are designated as a wildlife reserve, run by the Scottish Wildlife Trust. The loch is also a designated Site of Special Scientific Interest (SSSI), as well as forming part of a Special Area of Conservation.

Geographic entities mentioned:
surface_form: loch of the lowes
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.577
lon: -3.5491
Geography. Loch of the Lowes forms part of a chain of lochs known as the Lunan Lochs. The Lunan Lochs are Lochs Craiglush, Lowes, Butterstone, Clunie and Marlee, and are connected by the Lunan Burn, which drains into the River Isla, itself a tributary of the River Tay.

Geographic entities mentioned:
surface_form: loch of the lowes
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.577
lon: -3.5491
Loch of the Lowes, along with Loch Craiglush and Loch Butterstone is situated just north of the Highland Boundary Fault, and are mesotrophic lochs, and are characterised by a relatively low nutrient level, as their catchment areas are mostly acidic uplands. By comparison, Lochs Clunie and Marlee are situated south of the Highland Boundary Fault, and have a higher nutrient level.

Geographic entities mentioned:
surface_form: loch of the lowes
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.577
lon: -3.5491
Cortez Mountains. The Cortez Mountains are located in north central Nevada in the United States. The range lies in a southwest-northeasterly direction between Crescent Valley and Pine Valley. Mount Tenabo is the principal peak of the range, at 9,153 feet above sea level.

Geographic entities mentioned:
surface_form: Mount Tenabo
instance_of: Mountain
countries: United States
coordinates: lat: 40.162977777778
lon: -116.58480555556
Shaver Lake, California. Shaver Lake (formerly Musick Creek and Musick Creek Heights) is a census-designated place (CDP) in Fresno County, California, United States. The population was 580 at the 2020 census, down from 634 at the 2010 census. Shaver Lake is on the southwest end of the lake of the same name, east of New Auberry, at an elevation of. The name honors C.B.

Geographic entities mentioned:
surface_form: lake of the same name
instance_of: Lake
countries: United States
coordinates: lat: 37.125969444444
lon: -119.29075
The eponymous Lake Pihlajavesi is located within the municipality, and connects via Lake Tarjanne to the Kokemäenjoki basin, which drains into the Bothnian Sea. History. Pihlajavesi has existed at least since the early 17th century. Its name is derived from the nearby lake's name, which literally means &quot;rowan water&quot;.

Geographic entities mentioned:
surface_form: Tarjanne
instance_of: Lake
countries: Finland
coordinates: lat: 62.11384
lon: 24.076824
It went through various changes in extent, but roughly corresponded to the modern Mai-Ndombe Province. Location. The district takes its name from Lac Léopold II, today called Lake Mai-Ndombe, which drains to the west along the Fimi River to the Kasai River, a major left tributary of the Congo River. The district seat was the town of Inongo, on the northeast shore of the lake.

Geographic entities mentioned:
surface_form: Lake Mai-Ndombe
instance_of: Lake
countries: Democratic Republic of the Congo
coordinates: lat: -2
lon: 18.33
surface_form: Fimi River
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: -3.013472222222222
lon: 16.954305555555557
surface_form: Kasai River
instance_of: Watercourse
countries: Angola
Democratic Republic of the Congo
coordinates: lat: -10.9603
lon: 19.3156
The district seat was the town of Inongo, on the northeast shore of the lake. At its greatest extent between 1914 and 1933 the district extended west from the lake to the Congo River. To the east it extended along the whole length of the Lokoro River in the north, and along most of the Lukenie River in the south up to the border of the present Sankuru province. History.

Geographic entities mentioned:
surface_form: Lukenie River
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: -2.73089
lon: 18.15563
Mount Daisengen. Mount Daisengen (大千軒岳, &quot;Daisengen-dake&quot;) is a mountain located on the Oshima Peninsula of Hokkaidō, Japan. Mount Daisengen is the tallest mountain in the southern region of the peninsula.

Geographic entities mentioned:
surface_form: 大千軒岳
instance_of: Mountain
countries: Japan
coordinates: lat: 41.579319
lon: 140.160818
surface_form: daisengen-dake
instance_of: Mountain
countries: Japan
coordinates: lat: 41.579319
lon: 140.160818
surface_form: mount daisengen
instance_of: Mountain
countries: Japan
coordinates: lat: 41.579319
lon: 140.160818
surface_form: mount daisengen
instance_of: Mountain
countries: Japan
coordinates: lat: 41.579319
lon: 140.160818
Mount Daisengen. Mount Daisengen (大千軒岳, &quot;Daisengen-dake&quot;) is a mountain located on the Oshima Peninsula of Hokkaidō, Japan. Mount Daisengen is the tallest mountain in the southern region of the peninsula.

Geographic entities mentioned:
surface_form: mount daisengen
instance_of: Mountain
countries: Japan
coordinates: lat: 41.579319
lon: 140.160818
History. By about 1612, some Japanese Christians began to flee to the less populated Tōhoku and Ezo (modern-day Hokkaido) regions of Japan in order to escape religious persecution by the Tokugawa shogunate. Some of these Japanese Christians took up residence working at the gold mine near Mount Daisengen.

Geographic entities mentioned:
surface_form: mount daisengen
instance_of: Mountain
countries: Japan
coordinates: lat: 41.579319
lon: 140.160818
First offered in 1946 in the Sandusky area and later expanded to serve Erie, Huron, Lorain, and Ottawa counties, extension programs established a foundation for BGSU Firelands, the university's regional campus. The college was established at a site located near Lake Erie in Huron, Ohio, when the first building (now Foundation Hall) was opened.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
The BGSU Center for Sustainability and the Environment conducts research on renewable energy such as solar energy and wind generation on Lake Erie, energy conversion, and using algae to generate biofuel. Research in conjunction with the University of Toledo created new ways to effectively determine appropriate Ohio windmill sites.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Set up by George Washington's Continental Army, the &quot;Blue Hills Beacons&quot; were used by both sides and played an important role in many key battles and campaigns, including the Battle of Long Island and the Siege of Boston. The area was the site of the Pompton Mutiny, an insurrection of American soldiers in the winter of 1781.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: battle
instance_of: Watercourse
countries: United States
coordinates: lat: 44.9266
lon: -93.0291
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
Producing crushed stone and other materials for construction, it has been an important source of jobs and economic activity in the region for over 100 years. Stone from the quarry on Federal Hill has provided rock for the entrance steps and atriums of several national landmarks in Washington, D.C.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: federal hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.004166666667
lon: -74.307777777778
The area is part of the Passaic River watershed, which collects water from a number of NJ highlands streams and lakes in the region. The Pompton River, which flows northward from the Ramapo Mountains, passes through the valley to the east of Federal Hill and provided water power for mills and other industries in the area.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: federal hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.004166666667
lon: -74.307777777778
Federal Hill (Bloomingdale, New Jersey). Federal Hill is a ridge nestled in the foothills of the New Jersey Highlands. It is located in the town of Bloomingdale in Passaic County, in the U.S. state of New Jersey. Geography. The hill is in the northern part of the state, in the New Jersey Highlands region, which is known for its rugged terrain, forests, and lakes.

Geographic entities mentioned:
surface_form: federal hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.004166666667
lon: -74.307777777778
The ridgeline rises approximately above sea level, and is surrounded by other rugged hills and ridges, including Pompton Mountain and the Ramapo Mountains to the west. Following a generally northeastern course, Federal Hill and the NJ Highlands area are part of the same orogen as the Appalachian Mountains further west in the state.

Geographic entities mentioned:
surface_form: federal hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.004166666667
lon: -74.307777777778
Caused by a number of grievances, including lack of pay, poor living conditions, and a lack of provisions, the soldiers, who were mostly from New Jersey and Pennsylvania, mutinied against their officers and demanded better treatment and payment. The mutiny was later solved through negotiations, however some perpetrators were later prosecuted and punished for their actions on Federal Hill.

Geographic entities mentioned:
surface_form: federal hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.004166666667
lon: -74.307777777778
Contemporary history. In the twentieth century, the Amerika-Deutscher Volksbund, or German-American Bund as it is commonly referred to, constructed a youth camp on Federal Hill called Camp Bergwald. The camp was active during the interwar period, amidst a resurgence in German nationalism in the United States due to Adolf Hitler's ascent to power in Germany in 1934.

Geographic entities mentioned:
surface_form: federal hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.004166666667
lon: -74.307777777778
Trångsund. Trångsund () is a part of Huddinge to the south of Stockholm located between the two lakes Magelungen and Drevviken. Trångsund had 9,114 inhabitants in 2019. Trångsund is 17 minutes away from Stockholm City Station by train on the Bålsta-Nynäshamn line of the Stockholm commuter rail.

Geographic entities mentioned:
surface_form: Magelungen
instance_of: Lake
countries: Sweden
coordinates: lat: 59.228055555556
lon: 18.104722222222
surface_form: Drevviken
instance_of: Lake
countries: Sweden
coordinates: lat: 59.233333333333
lon: 18.175
Females of this species differ from their western counterparts in being overall colder-colored and duller. Ecology. It is found breeding in the eastern Mediterranean, Southeast Europe to the Caspian Sea and Iran and migrates to winter quarters in the Sudan. Prefers open habitats with scattered trees, such as savanna, rocky slopes, and barren pastures.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Piz Picuogl. Piz Picuogl is a mountain of the Albula Alps, located between Mulegns and the Val Bever, in Graubünden. On its northern side lies the glacier &quot;Vadret da Calderas&quot;. On the same ridge is located the lower summit Tschima da Flix.

Geographic entities mentioned:
surface_form: Tschima da Flix
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.521666666667
lon: 9.69975
surface_form: tschima da flix
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.521666666667
lon: 9.69975
Piz Picuogl. Piz Picuogl is a mountain of the Albula Alps, located between Mulegns and the Val Bever, in Graubünden. On its northern side lies the glacier &quot;Vadret da Calderas&quot;. On the same ridge is located the lower summit Tschima da Flix.

Geographic entities mentioned:
surface_form: piz picuogl
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.524083333333
lon: 9.7079166666667
Taxonomy. American mycologists Howard E. Bigelow and Alexander H. Smith first described the species officially in 1963, from specimens collected in June, 1954, near Payette Lake, Idaho. The species name refers to mycelial cords (rhizomorphs), which extend from the base. Description. The cap measures, and is initially convex before flattening and becoming funnel-shaped.

Geographic entities mentioned:
surface_form: Payette Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.95
lon: -116.085
The Barbee chain of lakes was formed by retreating glaciers during the Pleistocene era as were most of northeast Indiana's lakes. Location. The greater Barbee lakes are located just west of Indiana State Road 13, approximately south-southeast of Tippecanoe Lake and southwest of Webster Lake. Inflow and outflow. Inflow via Grassy Creek feeds Barbee (Big Barbee), Little Barbee, Irish, and Sawmill.

Geographic entities mentioned:
surface_form: Tippecanoe Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.327777777778
lon: -85.759722222222
surface_form: webster lake
instance_of: Lake
countries: United States
coordinates: lat: 42.0425
lon: -71.843333333333
surface_form: webster lake
instance_of: Lake
countries: United States
coordinates: lat: 41.907018
lon: -86.301546
surface_form: webster lake
instance_of: Lake
countries: United States
coordinates: lat: 41.3247
lon: -85.6819
surface_form: webster lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4694
lon: -71.6864
Shoe Lake flows into Banning Lake while Heron Lake flows into Kuhn Lake. Banning and Kuhn Lakes have the best water quality in the chain because their small watersheds contribute fewer nutrients. Water leaving the Barbee chain heads north and feeds Tippecanoe Lake. Some 75% of the watershed is agricultural. Residential.

Geographic entities mentioned:
surface_form: Tippecanoe Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.327777777778
lon: -85.759722222222
Inflow and outflow. Inflow via Grassy Creek feeds Barbee (Big Barbee), Little Barbee, Irish, and Sawmill. Shoe Lake flows into Banning Lake while Heron Lake flows into Kuhn Lake. Banning and Kuhn Lakes have the best water quality in the chain because their small watersheds contribute fewer nutrients. Water leaving the Barbee chain heads north and feeds Tippecanoe Lake.

Geographic entities mentioned:
surface_form: shoe lake
instance_of: Lake
countries: United States
coordinates: lat: 41.3075
lon: -85.7497
surface_form: heron lake
instance_of: Lake
countries: United States
coordinates: lat: 43.77416667
lon: -95.26916667
Barbee Lake. Barbee Lake is a fresh water lake located in Warsaw, Indiana, United States. The Barbee chain of lakes was formed by retreating glaciers during the Pleistocene era as were most of northeast Indiana's lakes. Location. The greater Barbee lakes are located just west of Indiana State Road 13, approximately south-southeast of Tippecanoe Lake and southwest of Webster Lake.

Geographic entities mentioned:
surface_form: barbee lake
instance_of: Lake
countries: United States
coordinates: lat: 41.283611111111
lon: -85.705
Some 75% of the watershed is agricultural. Residential. The chain of Barbee lakes has approximately 2,300 residences spread throughout the lakes with the highest concentration near Barbee's north end, Sechrist, and Little Barbee Lake. Recreation. All of the lakes support bluegill, largemouth bass, yellow perch, catfish, and crappie.

Geographic entities mentioned:
surface_form: barbee lake
instance_of: Lake
countries: United States
coordinates: lat: 41.283611111111
lon: -85.705
Barbee Lake. Barbee Lake is a fresh water lake located in Warsaw, Indiana, United States. The Barbee chain of lakes was formed by retreating glaciers during the Pleistocene era as were most of northeast Indiana's lakes. Location. The greater Barbee lakes are located just west of Indiana State Road 13, approximately south-southeast of Tippecanoe Lake and southwest of Webster Lake.

Geographic entities mentioned:
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
It may be confused with &quot;Lobostemon trichotomus&quot;, but the hairs on the mericarpids (nutlets) of &quot;Lobostemon glaber&quot; are diagnostic. Distribution and habitat. This species is found growing from the Koue Bokkeveld to the Cape Peninsula and Witteberg. It is found growing on shale soils and rocky slopes. Ecology. This species is popularly visited by bees.

Geographic entities mentioned:
surface_form: Koue Bokkeveld
instance_of: Plateau
countries: South Africa
coordinates: lat: -32.2
lon: 19.4167
While this strike was unsuccessful, it marked the beginning of organizing cannery workers. Cannery work in the 1920s. The California Santa Clara Valley, south of San Francisco, was the largest fruit growing and processing center in the world during the 1920s. Moreover, during this time, food processing was the largest United States industry in both labor size and product value.

Geographic entities mentioned:
surface_form: Santa Clara Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.366944444444
lon: -121.98388888889