Sarmila/GeoWiki-Features huggingface dataset:
Riffelhorn. The Riffelhorn (2,928 m) is a mountain in the Swiss section of the Pennine Alps, located south of Zermatt in the canton of Valais. The Riffelhorn forms part of the Gorner ridge and provides excellent rock climbing facilities having several routes of a different Climbing grades.

Geographic entities mentioned:
surface_form: Gorner ridge
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.983333333333
lon: 7.7836111111111
surface_form: riffelhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.981333333333
lon: 7.75825
It has been used a long time by the local Alpine guides to train rock climbing skills for climbers before ascending on higher mountains. It is also very popular view point being in the middle of one of the most famous valleys in the Alps, between the Matterhorn and Monte Rosa. Also the altitude of nearly 3,000 m gives a needed atmosphere of Alpine conditions.

Geographic entities mentioned:
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
It is also very popular view point being in the middle of one of the most famous valleys in the Alps, between the Matterhorn and Monte Rosa. Also the altitude of nearly 3,000 m gives a needed atmosphere of Alpine conditions. Nearest access is Rotenboden train station. Gornergratbahn continues from here up to summit of Gornergrat. On the northern side of the mountain lies the Riffelsee.

Geographic entities mentioned:
surface_form: Gornergrat
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.983333333333
lon: 7.7836111111111
It is also very popular view point being in the middle of one of the most famous valleys in the Alps, between the Matterhorn and Monte Rosa. Also the altitude of nearly 3,000 m gives a needed atmosphere of Alpine conditions. Nearest access is Rotenboden train station. Gornergratbahn continues from here up to summit of Gornergrat. On the northern side of the mountain lies the Riffelsee.

Geographic entities mentioned:
surface_form: Riffelsee
instance_of: Lake
countries: Switzerland
coordinates: lat: 45.983333
lon: 7.762222
Riffelhorn. The Riffelhorn (2,928 m) is a mountain in the Swiss section of the Pennine Alps, located south of Zermatt in the canton of Valais. The Riffelhorn forms part of the Gorner ridge and provides excellent rock climbing facilities having several routes of a different Climbing grades.

Geographic entities mentioned:
surface_form: riffelhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.981333333333
lon: 7.75825
Berchtesgadener Hochthron. The Berchtesgaden Hochthron is the highest peak of the Untersberg massif in the Berchtesgaden Alps in Berchtesgaden, Bavaria, Germany.

Geographic entities mentioned:
surface_form: berchtesgadener hochthron
instance_of: Mountain
countries: Germany
coordinates: lat: 47.694027777778
lon: 12.986111111111
Berchtesgadener Hochthron. The Berchtesgaden Hochthron is the highest peak of the Untersberg massif in the Berchtesgaden Alps in Berchtesgaden, Bavaria, Germany.

Geographic entities mentioned:
surface_form: berchtesgaden hochthron
instance_of: Mountain
countries: Germany
coordinates: lat: 47.694027777778
lon: 12.986111111111
The summit of the Berchtesgaden Hochthron offers one of the best views of the Berchtesgaden region, because it has an unobstructed view over the Berchtesgaden valley as well as all nine massifs of the Berchtesgaden Alps, the Chiemgau Alps, the Austrian mountains of the Salzkammergut and the Tennengebirge. Geography.

Geographic entities mentioned:
surface_form: berchtesgaden hochthron
instance_of: Mountain
countries: Germany
coordinates: lat: 47.694027777778
lon: 12.986111111111
Geography. The Berchtesgaden Hochthron rises around north of Berchtesgaden and about east-southeast from Bad Reichenhall. About west of the mountain summit is, managed by the German Alpine Club in the summer. At the foot of the steep falls of the summit lie the headwaters of the Almbach, which ends after flowing through the in Berchtesgadener Ache from the south. Climbing.

Geographic entities mentioned:
surface_form: berchtesgaden hochthron
instance_of: Mountain
countries: Germany
coordinates: lat: 47.694027777778
lon: 12.986111111111
It is also a popular destination for rock climbers. The Berchtesgaden Hochthron stops with massive, partly overhanging cliffs to the east and south. The numerous climbing routes of the south wall are among the most popular and historically significant climbs of the Berchtesgaden Alps. The most difficult climbs are usually attempted in November on the &quot;Old South Face&quot; (Level III +).

Geographic entities mentioned:
surface_form: berchtesgaden hochthron
instance_of: Mountain
countries: Germany
coordinates: lat: 47.694027777778
lon: 12.986111111111
Afon Crai. The Afon Crai is a river in Powys, Wales rising in the Fforest Fawr section of the Brecon Beacons National Park and flowing north into the River Usk. The headwaters known as Blaen-crai flow north from Bwlch Bryn-rhudd, a col between the Crai valley and the upper Swansea Valley for 2 km into the Cray Reservoir.

Geographic entities mentioned:
surface_form: Swansea Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.7593
lon: -3.7898
Conrad Mountains. The Conrad Mountains () are a narrow chain of mountains, long, located between the Gagarin Mountains and Mount Dallmann in Queen Maud Land, Antarctica. The Conrad Mountains are a subrange of the Orvin Mountains. With its summit at, the massive Sandeggtind Peak forms the highest point in the Conrad Mountains. Discovery and naming.

Geographic entities mentioned:
surface_form: Mount Dallmann
instance_of: Mountain
coordinates: lat: -71.75
lon: 10.3
Conrad Mountains. The Conrad Mountains () are a narrow chain of mountains, long, located between the Gagarin Mountains and Mount Dallmann in Queen Maud Land, Antarctica. The Conrad Mountains are a subrange of the Orvin Mountains. With its summit at, the massive Sandeggtind Peak forms the highest point in the Conrad Mountains. Discovery and naming.

Geographic entities mentioned:
surface_form: Sandeggtind Peak
instance_of: Mountain
coordinates: lat: -71.866666666667
lon: 9.75
Patok Lagoon. Patok Lagoon () is a lagoon of the Adriatic Sea on the Mediterranean Sea in the central coast of Albania. Created during the Holocene period, this area was characterized by a geo-morphologic dynamism. Its development spanned four phases, which correspond to the formation of four lagoons, separated by littoral cordons. The fourth lagoon is the current one.

Geographic entities mentioned:
surface_form: patok lagoon
instance_of: Lake
countries: Albania
coordinates: lat: 41.629
lon: 19.591
The commission voted to invite Michigan to the project, and to extend a branch of the east route from Dayton north to Detroit via Toledo. It also studied a loop around Lake Michigan and a western route between Tallahassee and Miami. Within a week, Michigan agreed to construct a loop around the Lower Peninsula, passing via Toledo, Ohio; South Bend, Indiana; Mackinaw City, Michigan; and Detroit.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
The Wapack Trail traverses the mountain. The northern face includes the state-owned Temple Mountain Reservation Area, formerly Temple Mountain Ski Area. The mountain is long and has several summits; three of them are named: Burton Peak, Whitcomb Peak, and Holt Peak, the high point. Pack Monadnock Mountain is located directly to the north along the Wapack ridgeline; Kidder Mountain to the south.

Geographic entities mentioned:
surface_form: Pack Monadnock Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.862777777778
lon: -71.878611111111
surface_form: Kidder Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.784252777778
lon: -71.882297222222
surface_form: monadnock mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.860833333333
lon: -72.108055555556
surface_form: monadnock mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.8975
lon: -71.5444
Pack Monadnock Mountain is located directly to the north along the Wapack ridgeline; Kidder Mountain to the south. Scattered ledges along the ridgeline offer long vistas west to Mount Monadnock and south along the spine of the Wapack Range; the abandoned ski area on the north side of the mountain offers 270-degree views.

Geographic entities mentioned:
surface_form: Mount Monadnock
instance_of: Mountain
countries: United States
coordinates: lat: 42.860833333333
lon: -72.108055555556
Temple Mountain (New Hampshire). Temple Mountain is a mountain in the Wapack Range in Hillsborough County, New Hampshire, United States. The mountain lies within the towns of Sharon, Temple and Peterborough. The Wapack Trail traverses the mountain. The northern face includes the state-owned Temple Mountain Reservation Area, formerly Temple Mountain Ski Area.

Geographic entities mentioned:
surface_form: temple mountain (new hampshire)
instance_of: Mountain
countries: United States
coordinates: lat: 42.8275
lon: -71.885277777778
surface_form: temple mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.738888888889
lon: -116.72055555556
surface_form: temple mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.688611111111
lon: -110.68194444444
Temple Mountain (New Hampshire). Temple Mountain is a mountain in the Wapack Range in Hillsborough County, New Hampshire, United States. The mountain lies within the towns of Sharon, Temple and Peterborough. The Wapack Trail traverses the mountain. The northern face includes the state-owned Temple Mountain Reservation Area, formerly Temple Mountain Ski Area.

Geographic entities mentioned:
surface_form: temple mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.8275
lon: -71.885277777778
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: temple mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.738888888889
lon: -116.72055555556
surface_form: temple mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.688611111111
lon: -110.68194444444
The mountain lies within the towns of Sharon, Temple and Peterborough. The Wapack Trail traverses the mountain. The northern face includes the state-owned Temple Mountain Reservation Area, formerly Temple Mountain Ski Area. The mountain is long and has several summits; three of them are named: Burton Peak, Whitcomb Peak, and Holt Peak, the high point.

Geographic entities mentioned:
surface_form: temple mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.8275
lon: -71.885277777778
surface_form: temple mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.8275
lon: -71.885277777778
surface_form: temple mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.738888888889
lon: -116.72055555556
surface_form: temple mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.738888888889
lon: -116.72055555556
surface_form: temple mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.688611111111
lon: -110.68194444444
surface_form: temple mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.688611111111
lon: -110.68194444444
The Wapack Trail traverses the mountain. The northern face includes the state-owned Temple Mountain Reservation Area, formerly Temple Mountain Ski Area. The mountain is long and has several summits; three of them are named: Burton Peak, Whitcomb Peak, and Holt Peak, the high point. Pack Monadnock Mountain is located directly to the north along the Wapack ridgeline; Kidder Mountain to the south.

Geographic entities mentioned:
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.924722222222
lon: -74.288055555556
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.3209
lon: -74.6616
With a good eye and clear weather, the top of the mountain can be seen from the visitor center at Hurricane Ridge. The nearest higher peak is Mount Meany (6,695 ft), to the south. Due to heavy winter snowfalls, Mount Queets supports the Queets Glacier in a cirque on its north slope, despite its modest elevation.

Geographic entities mentioned:
surface_form: Mount Meany
instance_of: Mountain
countries: United States
coordinates: lat: 47.75064
lon: -123.59824
Mount Queets. Mount Queets is a mountain summit located deep within Olympic National Park in Jefferson County of Washington state, United States. With a good eye and clear weather, the top of the mountain can be seen from the visitor center at Hurricane Ridge. The nearest higher peak is Mount Meany (6,695 ft), to the south.

Geographic entities mentioned:
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount queets
instance_of: Mountain
countries: United States
coordinates: lat: 47.762335
lon: -123.595156
The name &quot;Queets&quot; first appeared on the Surveyor General's map of Washington Territory referring to the Queets River, then was later applied to the glacier on the mountain which is the primary source of the river. The word &quot;Queets&quot; is a derivation of the name of the &quot;Quai'tso&quot; (Queets) tribe.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Precipitation runoff from the mountain drains into the headwaters of both the Elwha River and Queets River. There are scrambling routes ranging from class YDS 2 via the North Ridge, class 3 via the ridge from Mt. Meany, and class 4 via the Queets Glacier. History. The present-day Mt. Meany - Mt. Queets area was referred to as Mt. Mesachie on the 1896 Gilman National Geographic Map.

Geographic entities mentioned:
surface_form: mt. queets
instance_of: Mountain
countries: United States
coordinates: lat: 47.762335
lon: -123.595156
surface_form: mt. meany
instance_of: Mountain
countries: United States
coordinates: lat: 47.75064
lon: -123.59824
Mount Queets. Mount Queets is a mountain summit located deep within Olympic National Park in Jefferson County of Washington state, United States. With a good eye and clear weather, the top of the mountain can be seen from the visitor center at Hurricane Ridge. The nearest higher peak is Mount Meany (6,695 ft), to the south.

Geographic entities mentioned:
surface_form: mount queets
instance_of: Mountain
countries: United States
coordinates: lat: 47.762335
lon: -123.595156
The nearest higher peak is Mount Meany (6,695 ft), to the south. Due to heavy winter snowfalls, Mount Queets supports the Queets Glacier in a cirque on its north slope, despite its modest elevation. Precipitation runoff from the mountain drains into the headwaters of both the Elwha River and Queets River.

Geographic entities mentioned:
surface_form: mount queets
instance_of: Mountain
countries: United States
coordinates: lat: 47.762335
lon: -123.595156
Meany - Mt. Queets area was referred to as Mt. Mesachie on the 1896 Gilman National Geographic Map. The word &quot;mesachie&quot; is from Chinook Jargon and means &quot;wicked&quot;. The mountain was dubbed &quot;Mt. Hearst&quot; during the 1889-90 Seattle Press Expedition to honor William Randolph Hearst, owner of the San Francisco Examiner, but Mount Queets is the officially accepted name today.

Geographic entities mentioned:
surface_form: mount queets
instance_of: Mountain
countries: United States
coordinates: lat: 47.762335
lon: -123.595156
Due to heavy winter snowfalls, Mount Queets supports the Queets Glacier in a cirque on its north slope, despite its modest elevation. Precipitation runoff from the mountain drains into the headwaters of both the Elwha River and Queets River. There are scrambling routes ranging from class YDS 2 via the North Ridge, class 3 via the ridge from Mt. Meany, and class 4 via the Queets Glacier. History.

Geographic entities mentioned:
surface_form: mt. meany
instance_of: Mountain
countries: United States
coordinates: lat: 47.75064
lon: -123.59824
Northeast Toulnustouc River. The Northeast Toulnustouc River () is a tributary of the Toulnustouc River in Lac-Walker, Sept-Rivières, Côte-Nord, Quebec, Canada. The Cartier Railway runs beside it for most of its length. Name. Toulnustouc is a term of Innu origin whose meaning is not known. According to the surveyor J.

Geographic entities mentioned:
surface_form: Toulnustouc River
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.59361111
lon: -68.39333333
surface_form: toulnustouc river
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.59361111
lon: -68.39333333
surface_form: northeast toulnustouc river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.90002
lon: -67.69893
It contains many water bodies, often small and round. A few streams run through the canton, connected to the Toulnustouc North-East River system, notably the Ruisseau Kaushkuepakau. The Northeast Toulnustouc River is fed by the Petit lac Manicouagan, and flows southeast and then south before turning west into Lac Caron, where it joins the Toulnustouc River.

Geographic entities mentioned:
surface_form: Toulnustouc River
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.59361111
lon: -68.39333333
surface_form: toulnustouc river
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.59361111
lon: -68.39333333
The members of the Uashat Mak Mani-Utenam band of Innu people make use of parts of the Toulnustouc River basin, including Fortin Lake, Caron Lake, and the Northeast Toulnustouc River. Lake Arthur in the Réserve faunique de Port-Cartier–Sept-Îles flows west into Grand lac Caotibi, which drains north into Petit lac Caotibi, a tributary of Rivière Toulnustouc Nord-Est. Environment.

Geographic entities mentioned:
surface_form: rivière toulnustouc
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.59361111
lon: -68.39333333
surface_form: toulnustouc
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.59361111
lon: -68.39333333
surface_form: grand lac
instance_of: Lake
countries: Canada
coordinates: lat: 48.866666666667
lon: -57.433333333333
surface_form: grand lac
instance_of: Lake
countries: Canada
coordinates: lat: 45.933611111111
lon: -66.032777777778
surface_form: grand lac caotibi
instance_of: Lake
countries: Canada
coordinates: lat: 50.733055555556
lon: -67.553888888889
surface_form: rivière toulnustouc nord-est
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.90002
lon: -67.69893
surface_form: petit lac caotibi
instance_of: Lake
countries: Canada
coordinates: lat: 50.86583
lon: -67.54167
Northeast Toulnustouc River. The Northeast Toulnustouc River () is a tributary of the Toulnustouc River in Lac-Walker, Sept-Rivières, Côte-Nord, Quebec, Canada. The Cartier Railway runs beside it for most of its length. Name. Toulnustouc is a term of Innu origin whose meaning is not known. According to the surveyor J.

Geographic entities mentioned:
surface_form: toulnustouc
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.59361111
lon: -68.39333333
surface_form: northeast toulnustouc river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.90002
lon: -67.69893
It contains many water bodies, often small and round. A few streams run through the canton, connected to the Toulnustouc North-East River system, notably the Ruisseau Kaushkuepakau. The Northeast Toulnustouc River is fed by the Petit lac Manicouagan, and flows southeast and then south before turning west into Lac Caron, where it joins the Toulnustouc River.

Geographic entities mentioned:
surface_form: toulnustouc
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.59361111
lon: -68.39333333
surface_form: toulnustouc
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.59361111
lon: -68.39333333
surface_form: east river
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.5529
lon: -62.3032
The Northeast Toulnustouc River is fed by the Petit lac Manicouagan, and flows southeast and then south before turning west into Lac Caron, where it joins the Toulnustouc River. The members of the Uashat Mak Mani-Utenam band of Innu people make use of parts of the Toulnustouc River basin, including Fortin Lake, Caron Lake, and the Northeast Toulnustouc River.

Geographic entities mentioned:
surface_form: toulnustouc
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.59361111
lon: -68.39333333
surface_form: toulnustouc
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.59361111
lon: -68.39333333
surface_form: northeast toulnustouc river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.90002
lon: -67.69893
The Cartier Railway runs beside it for most of its length. Name. Toulnustouc is a term of Innu origin whose meaning is not known. According to the surveyor J. Bignell, the term means &quot;elbow river&quot; or &quot;angled river&quot; which matches the old name of Rivière du Coude (Elbow River).

Geographic entities mentioned:
surface_form: toulnustouc
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.59361111
lon: -68.39333333
EverestMax. qz43iit6n8x3dt80bq1ey0z9j90ke" xml:space="preserve">EverestMax was the first expedition to successfully travel from the lowest point on land, the Dead Sea, to the highest point, Mount Everest, by unpowered means. Led by Dominic Faulkner, a former UK SAS soldier, the six-person cycling team set out on 21 December 2005.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Yaeda Valley. The Yaeda Valley, or Yaida Valley, is a swampy valley located in Mbulu District of Manyara Region, Tanzania. The Valley is situated south of Lake Eyasi. The valley forms an endorheic basin with no drainage outlet. A low ridge running northeast–southwest separates the valley from the basin of Lake Eyasi.

Geographic entities mentioned:
surface_form: Lake Eyasi
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.66667
lon: 35.08333
surface_form: eyasi
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.66667
lon: 35.08333
The Valley is situated south of Lake Eyasi. The valley forms an endorheic basin with no drainage outlet. A low ridge running northeast–southwest separates the valley from the basin of Lake Eyasi. The Yaeda Swamp is fed from the northeast by the Yaeda River, which originates in the Mbulu Highlands to the east.

Geographic entities mentioned:
surface_form: Mbulu Highlands
instance_of: Plateau
countries: Tanzania
coordinates: lat: -3.8556
lon: 35.5444
Yaeda Valley. The Yaeda Valley, or Yaida Valley, is a swampy valley located in Mbulu District of Manyara Region, Tanzania. The Valley is situated south of Lake Eyasi. The valley forms an endorheic basin with no drainage outlet. A low ridge running northeast–southwest separates the valley from the basin of Lake Eyasi.

Geographic entities mentioned:
surface_form: manyara
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.5833333333333
lon: 35.833333333333
surface_form: yaeda valley
instance_of: Valley
countries: Tanzania
coordinates: lat: -4.0003083333333
lon: 34.999916666667
The Valley is situated south of Lake Eyasi. The valley forms an endorheic basin with no drainage outlet. A low ridge running northeast–southwest separates the valley from the basin of Lake Eyasi. The Yaeda Swamp is fed from the northeast by the Yaeda River, which originates in the Mbulu Highlands to the east.

Geographic entities mentioned:
surface_form: lake eyasi
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.66667
lon: 35.08333
surface_form: eyasi
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.66667
lon: 35.08333
Yaeda Valley. The Yaeda Valley, or Yaida Valley, is a swampy valley located in Mbulu District of Manyara Region, Tanzania. The Valley is situated south of Lake Eyasi. The valley forms an endorheic basin with no drainage outlet. A low ridge running northeast–southwest separates the valley from the basin of Lake Eyasi.

Geographic entities mentioned:
surface_form: yaeda valley
instance_of: Valley
countries: Tanzania
coordinates: lat: -4.0003083333333
lon: 34.999916666667
Marys, Tiffin, Upper Sandusky, Van Wert, Wapakoneta, Wauseon, Willard, and Woodville. Other areas served include the Lake Erie Islands north of Port Clinton and west of Sandusky.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Rocky Top (Georgia). Rocky Top is a summit in the U.S. state of Georgia. The elevation is. Rocky Top was so named on account of its appearance.

Geographic entities mentioned:
surface_form: rocky top
instance_of: Mountain
countries: United States
coordinates: lat: 34.982222222222
lon: -84.003611111111
Tunis, the capital city of Tunisia, lies at the south-western edge of the Gulf, as have a series of settled places over the last three millennia. Djebel Ressas rises to around south of the southern edge of the Gulf. The central part of the gulf, corresponding to the city of Tunis, is favorable to the implementation of a commercial port due to its location of being a well protected area.

Geographic entities mentioned:
surface_form: Djebel Ressas
instance_of: Mountain
countries: Tunisia
coordinates: lat: 36.6
lon: 10.33333333
Chilata lake. dhkistqod7j8lbn7936ikhmzvje3" xml:space="preserve">#REDIRECT Chilata Lake

Geographic entities mentioned:
surface_form: chilata lake
instance_of: Lake
countries: Bolivia
coordinates: lat: -15.68
lon: -68.6
Course. The Wateree River is a continuation of the Catawba River, which flows from the Blue Ridge Mountains in North Carolina; this river had the different names of Catawba and Wateree assigned to different sections by different groups of settlers. Today the name change is marked at the point where Wateree Creek empties into Lake Wateree.

Geographic entities mentioned:
surface_form: Lake Wateree
instance_of: Lake
countries: United States
coordinates: lat: 34.411111111111
lon: -80.792222222222
Blastobasis elgonae. &quot;Blastobasis elgonae&quot; is a moth in the family Blastobasidae. It is found in Kenya, where it is known from Mount Elgon in the western highlands. The length of the forewings is 6.8 mm.

Geographic entities mentioned:
surface_form: Mount Elgon
instance_of: Mountain
countries: Uganda
Kenya
coordinates: lat: 1.1185
lon: 34.5265
It is generally accepted by the art historical community that Sassetta's San Francesco altarpiece was one of the largest and most expensive of the Quattrocento. The fact that it was produced by a Sienese artist in Siena, and shipped to the Tiber Valley town in late spring 1444 also speaks to Sassetta's fame in his time period.

Geographic entities mentioned:
surface_form: Tiber Valley
instance_of: Valley
countries: Italy
coordinates: lat: 42.133333333333
lon: 12.583333333333
The Mutimbuzi River watershed is north of the city of Bujumbura between 3°12’00&quot; and 3°24’30&quot; South latitude and 29°19’00&quot; and 29°34’00&quot; East longitude. Although the Mutimbuzi River is a tributary of Lake Tanganyika, it drains part of the Ruzizi plain. The watershed includes parts of three ecoclimatic regions: the Imbo plain, the Mumirwa foothills and the Congo-Nile ridge.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
The Mutimbuzi flows through the Commune of Mutimbuzi, along the east side of the Melchior Ndadaye International Airport and under the RN4 coastal highway before emptying into Lake Tanganyika. About from the Rusizi the Mpanda River, a tributary of the Ruzizi, crosses an enormous expanse of marshes that connects to the Mutimbuzi River basin.

Geographic entities mentioned:
surface_form: Mpanda River
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.31944
lon: 29.27917
surface_form: mutimbuzi
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.3586111111111
lon: 29.328055555556
surface_form: mutimbuzi
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.3586111111111
lon: 29.328055555556
In 2020 Burundian Office of Urban Planning, Housing and Construction (OBUHA) banned commercial dredging of the Muha, Kanyosha, Ntahangwa, Mutimbuzi and other rivers of Bujumbura, since only OBUHA had the proper equipment for mechanical dredging, and manual dredging could not handle large rocks in the river bed.

Geographic entities mentioned:
surface_form: Muha
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.3952777777778
lon: 29.348888888889
surface_form: Kanyosha
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.4208333333333
lon: 29.342222222222
surface_form: Ntahangwa
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.3719444444444
lon: 29.338333333333
surface_form: ntahangwa
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.3719444444444
lon: 29.338333333333
surface_form: kanyosha
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.4208333333333
lon: 29.342222222222
surface_form: muha
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.3952777777778
lon: 29.348888888889
surface_form: mutimbuzi
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.3586111111111
lon: 29.328055555556
Course. The Mutimbuzi River rises in the Kavya &quot;colline&quot; in the Commune of Muramvya, Muramvya Province. Its three main tributaries are the Muzazi, Murago and Gikoma. The Mutimbuzi flows through the Commune of Mutimbuzi, along the east side of the Melchior Ndadaye International Airport and under the RN4 coastal highway before emptying into Lake Tanganyika.

Geographic entities mentioned:
surface_form: mutimbuzi
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.3586111111111
lon: 29.328055555556
Mutimbuzi River. The Mutimbuzi River () is a river in Bujumbura Rural Province, Burundi. Watershed. The Mutimbuzi River watershed is north of the city of Bujumbura between 3°12’00&quot; and 3°24’30&quot; South latitude and 29°19’00&quot; and 29°34’00&quot; East longitude. Although the Mutimbuzi River is a tributary of Lake Tanganyika, it drains part of the Ruzizi plain.

Geographic entities mentioned:
surface_form: mutimbuzi river
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.3586111111111
lon: 29.328055555556
Mutimbuzi River. The Mutimbuzi River () is a river in Bujumbura Rural Province, Burundi. Watershed. The Mutimbuzi River watershed is north of the city of Bujumbura between 3°12’00&quot; and 3°24’30&quot; South latitude and 29°19’00&quot; and 29°34’00&quot; East longitude. Although the Mutimbuzi River is a tributary of Lake Tanganyika, it drains part of the Ruzizi plain.

Geographic entities mentioned:
surface_form: mutimbuzi river
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.3586111111111
lon: 29.328055555556
surface_form: mutimbuzi river
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.3586111111111
lon: 29.328055555556
About from the Rusizi the Mpanda River, a tributary of the Ruzizi, crosses an enormous expanse of marshes that connects to the Mutimbuzi River basin. The Mutimbuzi's mouth on Lake Tanganyika is about from that of the Ruzizi. Flooding. The Mutimbuzi has a very changeable course, and feeds many ponds during the rainy season.

Geographic entities mentioned:
surface_form: mutimbuzi
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.3586111111111
lon: 29.328055555556
In April 2018 the Mutimbuzi River in the Buterere area, which had been diverted from its bed, had destroyed over 300 houses, flooded others and devastated many fields. In October 2018 the Burundi Civil Aviation Authority began dredging the Mutimbuzi River to prevent it from flooding into the airport. Drains would also be installed to prevent flooding.

Geographic entities mentioned:
surface_form: mutimbuzi river
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.3586111111111
lon: 29.328055555556
If the summit of one closed contour line is greater than the summit over the tangent closed contour line, the greater summit is the parent, or encirclement parent, of the other. Thus Olenos is the parent peak of Granitis. To find a parent of Olenos in the Peloponnesos, however, one must travel all the way to Mount Kyllini in Korinthia, to the east, which has an elevation of. The key col is ESE.

Geographic entities mentioned:
surface_form: Mount Kyllini
instance_of: Mountain
countries: Greece
coordinates: lat: 37.939166666667
lon: 22.396666666667
surface_form: mount kyllini
instance_of: Mountain
countries: Greece
coordinates: lat: 37.939166666667
lon: 22.396666666667
surface_form: kyllini
instance_of: Mountain
countries: Greece
coordinates: lat: 37.939166666667
lon: 22.396666666667
The river has great recreational value, including white-water rafting, but there is a growing danger of pollution from farm run-off and unprocessed waste water. Region. Mount Skollis is to the west, and many smaller mountains are to the north. Stretching east and southeast is Chelmos, also known as Aroania, which is the name of both a mountain and a village.

Geographic entities mentioned:
surface_form: Skollis
instance_of: Mountain
countries: Greece
coordinates: lat: 37.968
lon: 21.577
Stretching east and southeast is Chelmos, also known as Aroania, which is the name of both a mountain and a village. Chelmos, which can be seen from the mountain, is located to the east, but stretches to the south. The villages of south area of Panachaiko and Omplos are located in an agriculturally rich valley between the peaks of Erymanthos. Description.

Geographic entities mentioned:
surface_form: Panachaiko
instance_of: Mountain
countries: Greece
coordinates: lat: 38.2025
lon: 21.868888888889
surface_form: Omplos
instance_of: Mountain
countries: Greece
coordinates: lat: 38.166
lon: 21.781
surface_form: erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
surface_form: erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
The perimeter is about. A representative NE-SW distance is. A representative NW-SE distance is; that is to say, the mountainous terrain is approximately ovoid with the long axis NW-SW. The protected area is extended to the SW in GR2320002, Oropedio Folois, &quot;Plain of Foloi,&quot; comprising Foloi Forest, protected for its birds. It is not part of the mountain.

Geographic entities mentioned:
surface_form: oropedio
instance_of: Plateau
countries: Greece
coordinates: lat: 35.181175
lon: 25.466394
surface_form: foloi
instance_of: Plateau
countries: Greece
coordinates: lat: 37.75
lon: 21.75
surface_form: foloi
instance_of: Plateau
countries: Greece
coordinates: lat: 37.75
lon: 21.75
Mount Erymanthos. Mount Erymanthos (, Latin: &quot;Erymanthus&quot;) overall is an irregular massif of peaks connected by ridges embedded in the mountains located in the north of the Peloponnese, Greece. Erymanthos is on the west side.

Geographic entities mentioned:
surface_form: erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
surface_form: mount erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
Mount Erymanthos. Mount Erymanthos (, Latin: &quot;Erymanthus&quot;) overall is an irregular massif of peaks connected by ridges embedded in the mountains located in the north of the Peloponnese, Greece. Erymanthos is on the west side.

Geographic entities mentioned:
surface_form: erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
surface_form: erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
surface_form: mount erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
Erymanthos is on the west side. Its highest peak, Olenos or Olonos (Ωλενός or Ωλονός), Olenos original and preferred, elevation, is often called Mount Erymanthus, and conversely, Mount Olenos can be used for the entire range, although the customary usage is Erymanthos for the range and Olenos for the peak. Olenos is not a single peak.

Geographic entities mentioned:
surface_form: erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
The key col is ESE. There is a 3rd peak, which is not the highest of the range, nor is it traditionally Erymanthos, and yet it has inherited the name, Erymanthos, perhaps because it hangs over and is an essential part of the Erymanthos River watershed. Location is, elevation, prominence.

Geographic entities mentioned:
surface_form: erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
surface_form: erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
surface_form: erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
Location is, elevation, prominence. This Mount Erymanthos is visible from below at on the left side of the road in the village of Platanitsa, Achaea. The ridge of Olenos is visible above Erymanthos to the right, and the upper Erymanthos river, here a trickle in an otherwise dry Canyon, can be seen on the right. The village has a lot of plane trees but is on the edge of the tree line.

Geographic entities mentioned:
surface_form: erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
Location is, elevation, prominence. This Mount Erymanthos is visible from below at on the left side of the road in the village of Platanitsa, Achaea. The ridge of Olenos is visible above Erymanthos to the right, and the upper Erymanthos river, here a trickle in an otherwise dry Canyon, can be seen on the right. The village has a lot of plane trees but is on the edge of the tree line.

Geographic entities mentioned:
surface_form: erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
surface_form: erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
Olenos is the fourth-tallest peak in the Peloponnese peninsula. The summit is on the boundary of Achaea and Elis. Historically, Mount Erymanthos was part of northwestern Arcadia, where it was the second-tallest mountain range. The northern portion belonged to the historic Achaea. The name, Erymanthos, is a legacy from prehistoric times; that is, the Bronze Age, and possibly before.

Geographic entities mentioned:
surface_form: erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
surface_form: mount erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
Historically, Mount Erymanthos was part of northwestern Arcadia, where it was the second-tallest mountain range. The northern portion belonged to the historic Achaea. The name, Erymanthos, is a legacy from prehistoric times; that is, the Bronze Age, and possibly before. It does appear as an implied region in Linear B, the script of the Late Bronze Age.

Geographic entities mentioned:
surface_form: erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
It is not Greek. Olenos, on the other hand, is Greek for ulna, &quot;forearm,&quot; although the reason for the name has been lost (some sort of bend has been suggested). In contrast to most of the other mountain ranges of Eurasia, Erymanthos seems to have no discernible geometric pattern, which leads to certain difficulties in discerning which peaks are in it and which not.

Geographic entities mentioned:
surface_form: erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
Some sources erroneously refer to the southern slopes alone as GR2320012. The stage was thus set for the popular distinction &quot;Erymanthos in Achaea&quot; versus &quot;Erymanthos in Elis.&quot; The government, however, manages them both under the same agency in the same way, as Federal distinctions supersede regional and municipal. Management of Oros Enymanthos.

Geographic entities mentioned:
surface_form: erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
Drainage to the east is pre-empted by the higher mountains of Arcadia, which also drain to the west into the Alfeios. Erymanthos river. Overall the Erymanthos River flows directly south from the col between Psele Tourla and Lepidas a distance of about to intersect the Alfeios as a right-bank tributary. The lower half of the river is well-channeled through the Erymanthos ravine.

Geographic entities mentioned:
surface_form: erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
The mountain is the source of the Pineios river to the southwest, Selinountas to the east, Erymanthos to the south, and Peiros and Parapeiros to the southeast. It is part of the Oleni-Pindos geological zone. Panorama. The view from the summit of Erymanthos includes most of the western and northwestern Peloponnese, northern Arcadia, and the hills of eastern Ilia.

Geographic entities mentioned:
surface_form: erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
It is not part of the mountain. GR2320008 as a legal entity did not vanish away, which it could not do without a change in law. When GR2320012 became a &quot;Special Protection Area (SPA)&quot; in 2010 (for its birds, same as Foloi Forest), it incorporated GR2320008, which now had a double status, a SAC as 0008, and an SPA as 0012.

Geographic entities mentioned:
surface_form: foloi
instance_of: Plateau
countries: Greece
coordinates: lat: 37.75
lon: 21.75
Majeerteen Sultanates. The Majeerteen Sultanate was founded in the 15-16th century and came to prominence in the 19th century, under the reign of the resourceful King (&quot;Boqor&quot;) Osman Mahamuud. His Sultanate controlled Bari Karkaar, Nugaal and also central Somalia in the 19th and early 20th centuries.

Geographic entities mentioned:
surface_form: Nugaal
instance_of: Valley
countries: Somalia
coordinates: lat: 8.46178056
lon: 48.0542
Plot summary. The story concerns a mountain climber named James Abram Robbons who is the first man to reach the summit of Mount Everest, after having been dropped there by airplane. Robbons is picked up again two weeks later, and he reports that the summit of Everest is the location of a Martian outpost, and that the yeti are actually Martians.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
History. The locality name &quot;Goolman&quot; comes from nearby Mount Goolman, which in turn derives its name from &quot;stone axe&quot; in the Yuggera language. Residents in the Fassifern Valley petitioned the Queensland Government to build a railway line to their district, and the first section of the Dugandan railway line was opened on 10 July 1882 as far as Harrisville.

Geographic entities mentioned:
surface_form: Fassifern Valley
instance_of: Valley
countries: Australia
coordinates: lat: -27.810944444444
lon: 152.66505555556
Lake James State Park. Lake James State Park is a North Carolina state park in Burke and McDowell counties, North Carolina in the United States. Located near Nebo, North Carolina, it covers and borders Lake James. History. Started in 1987, Lake James State Park had 471,566 visitors in 2014.

Geographic entities mentioned:
surface_form: Lake James
instance_of: Lake
countries: United States
coordinates: lat: 35.7478
lon: -81.8785
Michael that passed through Unalakleet. Geography and climate. Unalakleet is located at (63.878907, −160.789680). Unalakleet is located on the Norton Sound of the Bering Sea at the mouth of the Unalakleet River, southeast of Nome and northwest of Anchorage. Unalakleet has a subarctic climate (Koppen: &quot;Dfc&quot;) with considerable maritime influences. Winters are cold and dry.

Geographic entities mentioned:
surface_form: Norton Sound
instance_of: Landform
countries: United States
coordinates: lat: 63.849166666667
lon: -164.26888888889
Topographic relief is significant as it rises in two miles on its north side above the Virgin River which drains precipitation runoff from this mountain. Its nearest higher neighbor is Lower Mountain, to the south, Shunesburg Mountain is four miles to the northeast, and Smithsonian Butte is four miles to the west-southwest.

Geographic entities mentioned:
surface_form: Shunesburg Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.1561453
lon: -112.9567568
surface_form: Smithsonian Butte
instance_of: Mountain
countries: United States
coordinates: lat: 37.113888888889
lon: -113.07972222222
Access is via the 2.8 mile Eagle Crags Trail which passes through pinyon–juniper woodland, sagebrush, blackbrush, yucca, and cacti as it gains 900 feet of elevation to the base of the sandstone pinnacles, spires, and crags. Views from the trail include Mount Kinesava, Johnson Mountain, and other landmarks within Zion National Park.

Geographic entities mentioned:
surface_form: Mount Kinesava
instance_of: Mountain
countries: United States
coordinates: lat: 37.19804
lon: -113.0305
Owned and operated by NBCUniversal's Telemundo Station Group, the station maintains studios are located on South Redwood Road in the northwestern section of Salt Lake City, and its transmitter is located on Farnsworth Peak in the Oquirrh Mountains, southwest of Salt Lake City.

Geographic entities mentioned:
surface_form: Farnsworth Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.659783333333
lon: -112.20234722222
The lake is located about south of the town of Odda. The village of Røldal is located at the northern tip of the lake and the village of Botnen is located at the southern end. The European route E134 highway runs along the northern end of the lake, and the Norwegian National Road 13 runs along the western shore of the lake.

Geographic entities mentioned:
surface_form: botnen
instance_of: Lake
countries: Norway
coordinates: lat: 63.5749
lon: 9.9646
Røldalsvatnet. Røldalsvatnet is a lake in Ullensvang Municipality in Vestland county, Norway. The lake is located about south of the town of Odda. The village of Røldal is located at the northern tip of the lake and the village of Botnen is located at the southern end.

Geographic entities mentioned:
surface_form: røldalsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 59.795
lon: 6.7752777777778
Baikal seals. The only exclusively freshwater seal species is the Baikal seal, locally named (). The Baikal seal has inhabited Lake Baikal for roughly two million years, the closest relative to it being the Arctic ringed seal whence it has likely descended.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Two subspecies of ringed seals live solely in freshwater lakes. The Ladoga seal inhabits Lake Ladoga in the Leningrad Oblast and Republic of Karelia. The seals became isolated in Lake Ladoga from the Baltic ringed seal (&quot;Pusa hispida botnica)&quot; as early as 8,800 BP due to the gradual isostatic rebound of the region following the end of the Weichselian Glaciation.

Geographic entities mentioned:
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222