Sarmila/GeoWiki-Features huggingface dataset:
The northbound exit ramp terminates at Southport Street, south of Vincent Street and Lake Monger Drive. The freeway then proceeds northwest for alongside Lake Monger's eastern edge, after which there is a half diamond interchange with Powis Street, with only a northbound exit ramp and a southbound entrance ramp.

Geographic entities mentioned:
surface_form: Lake Monger's
instance_of: Lake
countries: Australia
coordinates: lat: -31.9294
lon: 115.8265
Grey League. The Grey League (, or), sometimes called &quot;Oberbund&quot;, formed in 1395 in the &quot;Vorderrhein&quot; and &quot;Hinterrhein&quot; valleys, Raetia. The name Grey League is derived from the homespun grey clothes worn by the people. The league became part of the canton of Graubünden.

Geographic entities mentioned:
surface_form: Vorderrhein
instance_of: Watercourse
countries: Switzerland
coordinates: lat: 46.6325
lon: 8.6744444444444
Initially twelve judges were appointed, which was later expanded to fifteen. In 1424 the communities of the &quot;Hinterrhein&quot; valley, Heinzenberg-Thusis, Schams and Rheinwald, fully joined the League. With this expansion the League now controlled the strategic Spluegen and San Bernardino passes in addition to the Lukmanier Pass in the &quot;Vorderrhein&quot; valley.

Geographic entities mentioned:
surface_form: Schams
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.612
lon: 9.426
surface_form: Rheinwald
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.551778
lon: 9.319788
The Sardinians, for their part, were known to possess an ample amount of valuable obsidian from Monte Arci, a long-dormant volcano on the island. Among the most striking features of the Necropolis are the numerous carvings of long-horned bulls' heads, in and around at least three of the tombs.

Geographic entities mentioned:
surface_form: Monte Arci
instance_of: Mountain
countries: Italy
coordinates: lat: 39.777777777778
lon: 8.745
(His teacher was Zygmunt Batowski.)
From 1931 to 1939 he worked in the Department of Fine Arts of the Ministry of Religious Affairs and Public Education (Polish abbr.: WRiOP) and at the same time as the manager of Mobile Art Exhibition and organizer of the Summer Institutes of Folk Arts at Żabie on Hucul region — 1938 and in Zakopane on Podhale region — 1939.

Geographic entities mentioned:
surface_form: Podhale
instance_of: Valley
countries: Poland
coordinates: lat: 49.4793
lon: 20.0291
His feast day is observed on. Sisoës was a Copt by birth. Having withdrawn from the world since his youth, he retired to the desert of Sceté, and lived some time under the direction of his teacher, Abba Or. The desire of finding a retreat yet more unfrequented induced him to cross the Nile and hide himself in Mount Colzim where St. Anthony the Great had died some time before.

Geographic entities mentioned:
surface_form: Sceté
instance_of: Valley
countries: Egypt
coordinates: lat: 30.416666666667
lon: 30.333333333333
His feast day is observed on. Sisoës was a Copt by birth. Having withdrawn from the world since his youth, he retired to the desert of Sceté, and lived some time under the direction of his teacher, Abba Or. The desire of finding a retreat yet more unfrequented induced him to cross the Nile and hide himself in Mount Colzim where St. Anthony the Great had died some time before.

Geographic entities mentioned:
surface_form: Mount Colzim
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.9247117
lon: 32.3483919
Bhrigu had done several yajna (sacrifices) here. The temple ruins of Shiva, Shakti and Surya outskirt of the town confirms it antiquity. &quot;Brahmanotpattimartand&quot; mentions Brahmakhetak town in south of Mount Abu. It also mentions Hiranya river, confluence of two rivers and Brahma temple housing statues of Brahma and his two consorts.

Geographic entities mentioned:
surface_form: Mount Abu
instance_of: Mountain
countries: India
coordinates: lat: 24.5925
lon: 72.708333333333
Poncione di Ganna. Poncione di Ganna is a mountain of Lombardy, Italy. It has an elevation of 993 metres above sea level. It is part of the Varese Prealps subgroup of the Lugano Prealps.

Geographic entities mentioned:
surface_form: Varese Prealps
instance_of: Mountain
surface_form: varese
instance_of: Lake
countries: Italy
coordinates: lat: 45.816666666667
lon: 8.7333333333333
Poncione di Ganna. Poncione di Ganna is a mountain of Lombardy, Italy. It has an elevation of 993 metres above sea level. It is part of the Varese Prealps subgroup of the Lugano Prealps.

Geographic entities mentioned:
surface_form: poncione di ganna
instance_of: Mountain
countries: Italy
coordinates: lat: 45.89083333
lon: 8.84083333
Yoshida Bluff. qkyr4lsz0qrs6buq2c6rh3wpuify" xml:space="preserve">Yoshida Bluff () is a flat-topped bluff which rises to 2000 m at the north side of the head of Carlyon Glacier in Cook Mountains. The bluff is midway between Mill Mountain and Kanak Peak and is ice-covered except for rock cliffs at the south and west sides.

Geographic entities mentioned:
surface_form: Mill Mountain
instance_of: Mountain
coordinates: lat: -79.4333
lon: 157.867
surface_form: Kanak Peak
instance_of: Mountain
coordinates: lat: -79.2667
lon: 158.5
surface_form: mill
instance_of: Mountain
coordinates: lat: -65.25
lon: -64.05
The bluff is midway between Mill Mountain and Kanak Peak and is ice-covered except for rock cliffs at the south and west sides. Named after Yoshio Yoshida of the National Institute of Polar Research, Japan, geochemist with Japanese Antarctic Research Expedition (JARE) in four field seasons in the McMurdo Dry Valleys, 1963–64 to 1973–74.

Geographic entities mentioned:
surface_form: McMurdo Dry Valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
Yoshida Bluff. qkyr4lsz0qrs6buq2c6rh3wpuify" xml:space="preserve">Yoshida Bluff () is a flat-topped bluff which rises to 2000 m at the north side of the head of Carlyon Glacier in Cook Mountains. The bluff is midway between Mill Mountain and Kanak Peak and is ice-covered except for rock cliffs at the south and west sides.

Geographic entities mentioned:
surface_form: cook
instance_of: Mountain
coordinates: lat: -67.91667
lon: 56.46667
surface_form: yoshida bluff
instance_of: Mountain
coordinates: lat: -79.3333
lon: 158.2
Yoshida Bluff. qkyr4lsz0qrs6buq2c6rh3wpuify" xml:space="preserve">Yoshida Bluff () is a flat-topped bluff which rises to 2000 m at the north side of the head of Carlyon Glacier in Cook Mountains. The bluff is midway between Mill Mountain and Kanak Peak and is ice-covered except for rock cliffs at the south and west sides.

Geographic entities mentioned:
surface_form: yoshida bluff
instance_of: Mountain
coordinates: lat: -79.3333
lon: 158.2
Covering an area of approximately 40.5 square kilometers, Kalundu had an estimated population of 110,561 as of 2021. It is bordered by Kiliba-Kagando to the north, the Kambekulu River and Kigongo locality of the Bavira Chiefdom to the south, Lake Tanganyika to the east, and the Mitumba Mountains to the west.

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
These alluvial deposits are believed by geologists to have been formed during the glacial and pluvial phases of the Quaternary period. Lake-derived alluvium occurs in two forms: terrace-forming sediments and those lining the bed of Lake Tanganyika. The sandy texture of these lake sediments limits their agricultural productivity.

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
However, the claim conflicted with Spain's claim to sovereignty over the territory. Zebulon Pike led a U.S. Army reconnaissance expedition into the disputed region in 1806. Pike and his troops were arrested by Spanish cavalry in the San Luis Valley, taken to Chihuahua, then expelled from Mexico. Miguel Hidalgo y Costilla declared Mexico's independence from Spain on September 16, 1810.

Geographic entities mentioned:
surface_form: San Luis Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.2
lon: -105.42
On this occasion, he was granted the high Byzantine court title of &quot;kouropalates&quot;. Basil II also rewarded the valor of David's commander Tornikios by funding a Georgian Orthodox monastery on Mount Athos. Although populated now chiefly with Greek monks, it is to this day known as Iviron, &quot;of the Iberians (i.e. Georgians)&quot;.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Geography. The Pemadumcook chain of lakes forms the largest body of water in view as one gazes south from Mount Katahdin. If one takes a landscape picture from that summit, these lakes span the distance from the Piscataquis Mountains in the west to North Twin dam on Elbow Lake in the east.

Geographic entities mentioned:
surface_form: Mount Katahdin
instance_of: Mountain
countries: United States
coordinates: lat: 45.904355555556
lon: -68.921275
surface_form: katahdin
instance_of: Mountain
countries: United States
coordinates: lat: 45.904355555556
lon: -68.921275
surface_form: mount katahdin
instance_of: Mountain
countries: United States
coordinates: lat: 45.904355555556
lon: -68.921275
If one takes a landscape picture from that summit, these lakes span the distance from the Piscataquis Mountains in the west to North Twin dam on Elbow Lake in the east. It is the fifth-largest lake system in Maine, exceeded only by Moosehead Lake at, Sebago Lake at, Chesuncook Lake at, and Flagstaff Lake at. The Pemadumcook Chain of Lakes occupy.

Geographic entities mentioned:
surface_form: Moosehead Lake
instance_of: Lake
countries: United States
coordinates: lat: 45.633333333333
lon: -69.65
surface_form: Chesuncook Lake
instance_of: Lake
countries: United States
coordinates: lat: 45.987222222222
lon: -69.340833333333
surface_form: moosehead lake
instance_of: Lake
countries: United States
coordinates: lat: 45.633333333333
lon: -69.65
surface_form: flagstaff lake
instance_of: Lake
countries: United States
coordinates: lat: 42.5825
lon: -119.80027777778
surface_form: chesuncook lake
instance_of: Lake
countries: United States
coordinates: lat: 45.987222222222
lon: -69.340833333333
It is the fifth-largest lake system in Maine, exceeded only by Moosehead Lake at, Sebago Lake at, Chesuncook Lake at, and Flagstaff Lake at. The Pemadumcook Chain of Lakes occupy. Individually Mooselookmeguntic Lake is larger than Pemadumcook, but it is not larger than the chain. The series of lakes are named Ambajejus, Elbow, North Twin, Pemadumcook and South Twin Lake.

Geographic entities mentioned:
surface_form: Mooselookmeguntic Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.905
lon: -70.808888888889
The channel between North and South Twin Lake between the western shore and these islands runs north and south and is called the Narrows. The islands in South Twin include the Rock Pile which marks the southwest corner of the archipelago of islands separating North and South Twin Lakes, Peanut Island, and the reef that runs between it and the Rock Pile to the north.

Geographic entities mentioned:
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 27.893888888889
lon: -81.594722222222
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 43.4834018
lon: -74.9490486
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 37.6181
lon: -119.008
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 44.8079
lon: -118.0867
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 40.7433
lon: -115.283
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.0183
lon: -73.3867
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 45.23888889
lon: -111.86472222
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 60.638888888889
lon: -153.86305555556
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 48.6494
lon: -113.718
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 45.7487796
lon: -84.4527626
surface_form: twin lakes
instance_of: Lake
countries: United States
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 44.6375
lon: -89.41583333333334
Geography. The Pemadumcook chain of lakes forms the largest body of water in view as one gazes south from Mount Katahdin. If one takes a landscape picture from that summit, these lakes span the distance from the Piscataquis Mountains in the west to North Twin dam on Elbow Lake in the east.

Geographic entities mentioned:
surface_form: elbow lake
instance_of: Lake
countries: United States
coordinates: lat: 46.8343363
lon: -122.4568674
surface_form: elbow lake
instance_of: Lake
countries: United States
coordinates: lat: 46.00833333
lon: -96.00833333
The Pemadumcook Chain of Lakes occupy. Individually Mooselookmeguntic Lake is larger than Pemadumcook, but it is not larger than the chain. The series of lakes are named Ambajejus, Elbow, North Twin, Pemadumcook and South Twin Lake. The lakes are part of the West Branch of the Penobscot River. The West Branch enters the northwest corner of Ambajejus, and the current flows south through that lake.

Geographic entities mentioned:
surface_form: south twin lake
instance_of: Lake
countries: United States
coordinates: lat: 45.620665
lon: -68.8605551
surface_form: south twin lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2731
lon: -90.4372
The Porus islands, while principally in Pemadumcook, do divide Pemadumcook to the west and south from Ambajejus to the north. The islands separating North Twin Lake from South Twin Lake are all south of Spring Island. The channel between North and South Twin Lake between the western shore and these islands runs north and south and is called the Narrows.

Geographic entities mentioned:
surface_form: south twin lake
instance_of: Lake
countries: United States
coordinates: lat: 45.620665
lon: -68.8605551
surface_form: south twin lake
instance_of: Lake
countries: United States
coordinates: lat: 45.620665
lon: -68.8605551
surface_form: south twin lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2731
lon: -90.4372
surface_form: south twin lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2731
lon: -90.4372
If the water is quite high one need not concern oneself about boulders in the middle of the lake. Exceptions include but are not restricted to a large reef at the west end of South Twin Lake that runs north and south and a large rock pile north-northwest of Partridge Cove which is usually marked. There are a couple of reefs in North Twin and a long reef about north of Indian Point Island.

Geographic entities mentioned:
surface_form: south twin lake
instance_of: Lake
countries: United States
coordinates: lat: 45.620665
lon: -68.8605551
surface_form: south twin lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2731
lon: -90.4372
Twitchell Brook enters the lake near a point where the Appalachian Trail provides a view of the lake, but there is no inlet. Road access to the lake is provided by Maine State Route 11 on the east side. This runs past Partridge Cove at the southeast corner of South Twin Lake and then serves the area up to Norcross. Millinocket is about east of Norcross on Maine Route 11.

Geographic entities mentioned:
surface_form: south twin lake
instance_of: Lake
countries: United States
coordinates: lat: 45.620665
lon: -68.8605551
surface_form: south twin lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2731
lon: -90.4372
Millinocket is about east of Norcross on Maine Route 11. The paved portion of the Millinocket–Baxter State Park road gives access to Spencer Cove at the northeast end of Ambajejus Lake about from Millinocket. A dike at Spencer Cove created by the Great Northern Paper Company prevents water from flowing from Ambajejus Lake, spillway elevation, into adjacent Millinocket Lake, elevation.

Geographic entities mentioned:
surface_form: millinocket lake
instance_of: Lake
countries: United States
coordinates: lat: 46.3
lon: -68.86666667
The Pemadumcook Chain of Lakes occupy. Individually Mooselookmeguntic Lake is larger than Pemadumcook, but it is not larger than the chain. The series of lakes are named Ambajejus, Elbow, North Twin, Pemadumcook and South Twin Lake. The lakes are part of the West Branch of the Penobscot River. The West Branch enters the northwest corner of Ambajejus, and the current flows south through that lake.

Geographic entities mentioned:
surface_form: west branch
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
Watershed. The inlets to the lake are at Ragged Brook and Lincoln Brook on South Twin, the West Branch of the Penobscot at Ambajejus, Jo Mary Stream on the south side of Pemadumcook, and Nahmakanta Stream at the northwest corner of Pemadumcook. Twitchell Brook enters the lake near a point where the Appalachian Trail provides a view of the lake, but there is no inlet.

Geographic entities mentioned:
surface_form: west branch
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
Pemadumcook Chain of Lakes. The Pemadumcook Chain of Lakes are a set of large lakes in north-central Maine in the United States. Name. Thoreau's &quot;Pamadumcook&quot; or Joseph Chadwick's &quot;Bennedumcook&quot; is rendered by the United States Geographical Board in an 1897 decision as &quot;Pemadumcook Lake&quot;. Geography.

Geographic entities mentioned:
surface_form: pemadumcook chain of lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 45.7
lon: -68.95
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
end of the Piscataquis Mountains.&quot;
Henry David Thoreau crossed the lake in September 1846, writing in &quot;The Maine Woods&quot;: &quot;After poling up half a mile of river, or thoroughfare we rowed a mile across the foot of Pamadumcook Lake, which is the name given on the map to this whole chain of lakes, as if there was but one, though they are, in each instance distinctly separated by a reach of the river, with its narrow and rocky channel and its rapids.

Geographic entities mentioned:
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
The channel passes Deep Cove on the east and Porus Islands to the west. The river channel then passes east through the east end of Pemadumcook into the head of North Twin Lake at Indian Point. The channel then follows a southeasterly course across North Twin Lake, staying between Perrow Point and Spring Island, and then veering eastward past Snake Point in sight of the settlement of Norcross.

Geographic entities mentioned:
surface_form: north twin lake
instance_of: Lake
countries: United States
coordinates: lat: 46.049444444444
lon: -89.138333333333
The river channel then passes east through the east end of Pemadumcook into the head of North Twin Lake at Indian Point. The channel then follows a southeasterly course across North Twin Lake, staying between Perrow Point and Spring Island, and then veering eastward past Snake Point in sight of the settlement of Norcross. The channel then passes due east through the Elbow to North Twin dam.

Geographic entities mentioned:
surface_form: north twin lake
instance_of: Lake
countries: United States
coordinates: lat: 46.049444444444
lon: -89.138333333333
Hamlin wrote in 1881 in &quot;Appalachia&quot;, the journal of the Appalachian Mountain Club: &quot;After a short run through rapid water in the river, the way lies through Quakish Lake, two miles; thence one mile through furious rapids, that require all the strength and skill of practised boatmen to ascend them by poling, to North Twin Dam; thence a mile more of river, or — as a reach of running stream connecting two lakes is here termed — of
&quot;thoroughfare,&quot; leads into North Twin Lake, four miles long, from which another of a few rods only opens into Pemadumcook Lake, largest of the chain and ten miles in length.

Geographic entities mentioned:
surface_form: north twin lake
instance_of: Lake
countries: United States
coordinates: lat: 46.049444444444
lon: -89.138333333333
The last individual in the area was recorded in 1996. In 2005, leopard DNA was detected in the Hoggar Mountains of southern Algeria, in the central Sahara. In 2014, a leopard was killed in the Elba Protected Area in southeastern Egypt. This was the first sighting of a leopard in the country since the 1950s.

Geographic entities mentioned:
surface_form: Hoggar Mountains
instance_of: Plateau
countries: Algeria
France
coordinates: lat: 23.288611
lon: 5.534167
Northern Highlands. The Northern Highlands are a mountainous biogeographical region of northern Madagascar. The region includes the Tsaratanana Massif (with the highest mountain of Madagascar, Maromokotro) and smaller nearby massifs such as Marojejy, Anjanaharibe-Sud, and Manongarivo.

Geographic entities mentioned:
surface_form: Maromokotro
instance_of: Mountain
countries: Madagascar
coordinates: lat: -14.022777777778
lon: 48.965833333333
Occasionally the regions of the higher Swiss Plateau, especially the hills of the canton of Fribourg, the Napf region, the Töss region, the (lower) Toggenburg, and parts of the Appenzell region are considered to form the Swiss Alpine foreland in a narrow sense.

Geographic entities mentioned:
surface_form: Napf
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.004166666667
lon: 7.94
surface_form: Töss
instance_of: Valley
countries: Switzerland
coordinates: lat: 47.350277777778
lon: 8.935
surface_form: sense
instance_of: Watercourse
countries: Switzerland
coordinates: lat: 46.906
lon: 7.23389
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
However, if a division into the three main regions Jura Mountains, Swiss Plateau and Alps is considered, the Alpine foreland belongs clearly to the Swiss Plateau. In the southwest, the Swiss Plateau is confined by Lake Geneva, in the northeast, by Lake Constance and the Rhine. Geologically, the Swiss Plateau is part of a larger basin that extends beyond the border of Switzerland.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
The former alpine rivers built huge fans of sediment at the foot of the mountains. The most important examples are the Napf fan and the Hörnli fan; other sedimentary fans exist in the Rigi region, in the Schwarzenburg region and in the region between the eastern lake Geneva and the middle reaches of the Sarine. The eroded material has been sorted by grain size.

Geographic entities mentioned:
surface_form: Napf
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.004166666667
lon: 7.94
surface_form: Hörnli
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.371
lon: 8.94175
surface_form: Rigi
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.05
lon: 8.4666666666667
Glacial landscapes. A look at a map still reveals the directions where the ice age glaciers ran. The furthest expansion of the Rhône Glacier to the northeast is indicated by way the western Swiss Plateau valleys trend: the valleys of the Broye and the Glâne as well as Lake Murten, Lake Neuchâtel, and Lake Biel all trend northeast, parallel to the Jura and to the Alps.

Geographic entities mentioned:
surface_form: Lake Neuchâtel
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.9
lon: 6.85
surface_form: Lake Biel
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.085555555556
lon: 7.1741666666667
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
The glaciers of the Reuss and the Limmat have carved the valleys of the central Swiss Plateau trend northwest (among others including the valleys of the Wigger, the Suhre, the Seetal, the Reuss and the Limmat). The Rhine Glacier has mostly left traces that trend west, such as the eastern Swiss Plateau of the Thur Valley and Lake Constance.

Geographic entities mentioned:
surface_form: Suhre
instance_of: Watercourse
countries: Switzerland
coordinates: lat: 47.4053
lon: 8.06583
surface_form: Seetal
instance_of: Valley
countries: Switzerland
coordinates: lat: 47.23166667
lon: 8.24361111
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
The Rhine Glacier has mostly left traces that trend west, such as the eastern Swiss Plateau of the Thur Valley and Lake Constance. In certain places, there are characteristic drumlins of the base moraine, often clustered, especially in the highlands of Zürich, in the Hirzel region, in the Lake Constance region and between the Reuss Valley and Lake Baldegg.

Geographic entities mentioned:
surface_form: Lake Baldegg
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.198611111111
lon: 8.2605555555556
The western plateau is stamped by the Gros-de-Vaud plateau (up to 600 meters AMSL) and the Jorat molasse hills (up to 900 meters AMSL) but is sometimes intersected by deep valleys. Near the Jura, there is an almost continuous dip consisting of the Venoge and the Orbe valleys which are separated by the Mormont hill, the main watershed between Rhône and Rhine, at only 500 m AMSL.

Geographic entities mentioned:
surface_form: Mormont
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.65514
lon: 6.53367
The central Swiss Plateau is characterised by a number of ranges and broad valleys, some of them with lakes, that run northwest. The last of them is the Albis range, which together with the Heitersberg range forms a bar from the Alps to the Jura. Major transportation routes cross it only in a few places, mostly via tunnels.

Geographic entities mentioned:
surface_form: Albis
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.283333333333
lon: 8.5
The last of them is the Albis range, which together with the Heitersberg range forms a bar from the Alps to the Jura. Major transportation routes cross it only in a few places, mostly via tunnels. The eastern Swiss Plateau is structured by the valleys of the Limmat (including Lake Zurich), the Glatt, the Töss, the Murg, the Thur, and the Sitter. Between them there are hill countries.

Geographic entities mentioned:
surface_form: Lake Zurich
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2475
lon: 8.6775
surface_form: lake zurich
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2475
lon: 8.6775
Between them there are hill countries. In the canton of Thurgau there are also the broad molasse ranges of Seerücken (lit.: 'back of the lake') and &quot;Ottenberg&quot; north of the Thur, and the hilly ranges between the Thur and the Murg. This area is colloquially also known as &quot;Mostindien&quot; (lit.: 'Cider India').

Geographic entities mentioned:
surface_form: Seerücken
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.6489
lon: 9.03333
This area is colloquially also known as &quot;Mostindien&quot; (lit.: 'Cider India'). Two hill countries are out of sync with the above-mentioned landscapes: the Napf region (with 1408 me AMSL the highest point of the Swiss Plateau) and the Töss region (up to 1300 meters AMSL); both are the remains of Tertiary conglomerate sediment fans.

Geographic entities mentioned:
surface_form: Napf
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.004166666667
lon: 7.94
surface_form: Töss
instance_of: Valley
countries: Switzerland
coordinates: lat: 47.350277777778
lon: 8.935
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
The most important cultures are wheat, barley, maize, sugar beet and potato; especially in the &quot;Seeland&quot;, vegetables are very important, too. Along the northern shores of the lakes of Geneva, Neuchâtel, Bienne, Morat, as well as in the Zürich Weinland and Klettgau, there is viticulture.

Geographic entities mentioned:
surface_form: Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
surface_form: Neuchâtel
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.9
lon: 6.85
surface_form: Morat
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.933333333333
lon: 7.075
The &quot;de facto&quot; capital of Switzerland, Bern, has only a small airport, Bern Belpmoos Airport. Härkingen respectively Niederbipp and Zürich are scheduled as one of the eight hubs of the proposed Cargo Sous Terrain, an underground cargo transport system those first phase of about is planned by the early 2030s. Tourism.

Geographic entities mentioned:
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.50486111
lon: 7.64305556
Swiss Plateau. The Swiss Plateau or Central Plateau is one of the three major landscapes in Switzerland, lying between the Jura Mountains and the Swiss Alps. It covers about 30% of the Swiss surface area, and is partly flat but mostly hilly. The average height is between and AMSL. It is by far the most densely populated region of Switzerland, the center of economy and important transportation.

Geographic entities mentioned:
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
Swiss Plateau. The Swiss Plateau or Central Plateau is one of the three major landscapes in Switzerland, lying between the Jura Mountains and the Swiss Alps. It covers about 30% of the Swiss surface area, and is partly flat but mostly hilly. The average height is between and AMSL. It is by far the most densely populated region of Switzerland, the center of economy and important transportation.

Geographic entities mentioned:
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
surface_form: central plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
The average height is between and AMSL. It is by far the most densely populated region of Switzerland, the center of economy and important transportation. Geography. In the north and northwest, the Swiss Plateau is sharply delimited geographically and geologically by the Jura Mountains. In the south, there is no clear border with the Alps.

Geographic entities mentioned:
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
However, if a division into the three main regions Jura Mountains, Swiss Plateau and Alps is considered, the Alpine foreland belongs clearly to the Swiss Plateau. In the southwest, the Swiss Plateau is confined by Lake Geneva, in the northeast, by Lake Constance and the Rhine. Geologically, the Swiss Plateau is part of a larger basin that extends beyond the border of Switzerland.

Geographic entities mentioned:
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
In the southwest, the Swiss Plateau is confined by Lake Geneva, in the northeast, by Lake Constance and the Rhine. Geologically, the Swiss Plateau is part of a larger basin that extends beyond the border of Switzerland. At its southwestern end, in France, the plateau, in the Genevois, ends at Chambéry where Jura and Alps meet.

Geographic entities mentioned:
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
On the other side of Lake Constance, the plateau continues in the German and Austrian Pre-Alps. Within Switzerland, the Swiss Plateau has a length of about, and its width increases from the west to the east: In the Geneva region, it is about, at Bern about and in eastern Switzerland about. Many cantons of Switzerland include a part in the Swiss Plateau.

Geographic entities mentioned:
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
Many cantons of Switzerland include a part in the Swiss Plateau. Entirely situated within the Swiss Plateau are the cantons of Zürich, Thurgau and Geneva; mostly situated within the Swiss Plateau are the cantons of Lucerne, Aargau, Solothurn, Bern, Fribourg and Vaud; small portions of the Swiss Plateau are situated in the cantons of Neuchâtel, Zug, Schwyz, St. Gallen and Schaffhausen.

Geographic entities mentioned:
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
Gallen and Schaffhausen. Geological layers. The geological layers of the Swiss Plateau are relatively well known. The base level is crystalline basement which outcrops in the central crystalline Alps as well as in the Black Forest and the Vosges mountain range but forms a deep geosyncline in the Swiss Plateau and in the Jura (see also Jurassic).

Geographic entities mentioned:
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
The uppermost layer consists of gravel and glacial sediments that have been transported by the glaciers of the ice ages. Geologically the most important layer of the Swiss Plateau is the thick molasse sequence that accumulated at the border of the Alps due to the rapid erosion of the concurrently uplifted mountains.

Geographic entities mentioned:
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
In the middle of the plateau, there are finer sandstones and near the Jura, clays and marl. During the Tertiary orogenic uplift, around 60 – 40 million years ago, the area of today's Swiss Plateau was a Karst plateau somewhat inclined to the south. Through processes of rising and lowering that were brought by the folding of the Alps, the area was twice flooded by a sea.

Geographic entities mentioned:
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
Ice ages. The contemporary landscape of the Swiss Plateau has been shaped by the ice age glaciers. During all the known alpine glaciations (Günz glaciation, Mindel glaciation, Riss glaciation and Würm glaciation), huge glaciers penetrated the Swiss Plateau.

Geographic entities mentioned:
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
The contemporary landscape of the Swiss Plateau has been shaped by the ice age glaciers. During all the known alpine glaciations (Günz glaciation, Mindel glaciation, Riss glaciation and Würm glaciation), huge glaciers penetrated the Swiss Plateau. During the warm interglacials, the glaciers receded to the high alps (sometimes more than today) and subtropical vegetation spread in the plateau.

Geographic entities mentioned:
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
During the warm interglacials, the glaciers receded to the high alps (sometimes more than today) and subtropical vegetation spread in the plateau. During the ice ages, the Rhône glacier split into two branches when leaving the Alps, covering the whole western Swiss Plateau and reaching today's regions of Solothurn and Aarau. In the region of Bern, it merged with the Aar Glacier.

Geographic entities mentioned:
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
Traces of the older Günz and Mindel glaciation are only left in a few places because most have been removed or transferred by the later glaciations. The greatest extent was reached by the glaciers of the Riss glaciation, when the entire Swiss Plateau was covered with ice except for the Napf and Töss regions. Most notable are the traces of the Würm glaciation about 15 000 years ago.

Geographic entities mentioned:
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
The glaciers of the Reuss and the Limmat have carved the valleys of the central Swiss Plateau trend northwest (among others including the valleys of the Wigger, the Suhre, the Seetal, the Reuss and the Limmat). The Rhine Glacier has mostly left traces that trend west, such as the eastern Swiss Plateau of the Thur Valley and Lake Constance.

Geographic entities mentioned:
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
In certain places, there are characteristic drumlins of the base moraine, often clustered, especially in the highlands of Zürich, in the Hirzel region, in the Lake Constance region and between the Reuss Valley and Lake Baldegg. Another reminder of the glaciation are glacial erratics which are found all over the Swiss Plateau.

Geographic entities mentioned:
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
Sometimes, there is also gravel from older glaciations. Topography. Even though the Swiss Plateau forms a basin, it is by no means a flat territory, but depending on the region, it has a manifold structure. Important elements are the two big lakes, Lake Geneva and Lake Constance that delimit the Swiss Plateau in the southwest and the northeast.

Geographic entities mentioned:
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
Near the Jura, there is an almost continuous dip consisting of the Venoge and the Orbe valleys which are separated by the Mormont hill, the main watershed between Rhône and Rhine, at only 500 m AMSL. The Seeland ('lake land'), characterized by the Murten, Neuchâtel and Biel lakes, represents the largest plain of the Swiss Plateau, though it is also interrupted by isolated molasse ranges.

Geographic entities mentioned:
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
In July, the mean temperature of Geneva is 20 °C, alongside the southern edge of the Jura it is 18 – 20 °C, and in higher regions 16 – 18 °C. With regard to mean sunshine duration, the Lake Geneva region is again advantaged with more than 1900 hours, whereas in the rest of the Swiss Plateau, it is between 1600 (especially in the east) and 1900 hours.

Geographic entities mentioned:
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
In the warmest regions at Lakes Geneva and Neuchâtel, there are less than 20 days with snow cover, whereas, in the rest of the plateau, it is between 20 and 40, depending on elevation. In the winter half-year, the air on the Swiss Plateau can stay still, with little exchange with the rest of the atmosphere, building a lake of cold air on the plateau and often a ceiling of high fog.

Geographic entities mentioned:
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
Major oppida were built after the Celts appeared in the 3rd century BC. Urban settlements with stone houses were built during the Roman Empire. The Swiss Plateau became a part of the Roman Empire in 15 BC when the Romans occupied the land of the Helvetii under the reign of Augustus, and it remained Roman until the end of the 3rd century.

Geographic entities mentioned:
surface_form: swiss plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
A point on the coast just south of this peak was first charted and the name Lagrange applied by the Belgian Antarctic Expedition under Gerlache, 1897–99. On one of the photos published by the expedition, the name is applied to the southern tip of the island. To avoid confusion, the generic term has been altered and the name applied to this peak.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
Lagrange Peak. Lagrange Peak () is a conspicuous peak, high, standing northeast of Strath Point on the southeast coast of Brabant Island, in the Palmer Archipelago, Antarctica. A point on the coast just south of this peak was first charted and the name Lagrange applied by the Belgian Antarctic Expedition under Gerlache, 1897–99.

Geographic entities mentioned:
surface_form: lagrange peak
instance_of: Mountain
coordinates: lat: -64.4667
lon: -62.4333
Håkås. Håkås (; from Old Norse &quot;Haukáss&quot;, &quot;hawk hill&quot;), formerly spelled &quot;Haagaas&quot; and &quot;Haakaas&quot;, is a hill and an area near the lake Øyeren in Båstad in Trøgstad, Østfold, Norway, 25 kilometres southeast of Oslo. It is also the name of three neighbouring farms in the immediate vicinity of the hill.

Geographic entities mentioned:
surface_form: Øyeren
instance_of: Lake
countries: Norway
coordinates: lat: 59.857222222222
lon: 11.163333333333
It is also the name of three neighbouring farms in the immediate vicinity of the hill. In 2016 the Håkås nature reserve was established by the King-in-Council; consisting of the Håkås forests near Øyeren, it was fully protected due to its importance to biodiversity. History.

Geographic entities mentioned:
surface_form: Øyeren
instance_of: Lake
countries: Norway
coordinates: lat: 59.857222222222
lon: 11.163333333333
Two main rivers run south through the reserve, the Chamby River and the Hushmy River. The river valleys are generally waterlogged when not frozen. Lake Cheko, a round, picturesque thermokarst lake is on the northern border of the site; it has been suggested as a possible impact site of the 1908 meteorite fall. Climate and ecoregion.

Geographic entities mentioned:
surface_form: Lake Cheko
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.963888888889
lon: 101.86027777778
Lake Bogoria. Lake Bogoria (formerly Lake Hannington) is a saline, alkaline lake that lies in a volcanic region in a half-graben basin south of Lake Baringo, Kenya, a little north of the equator.

Geographic entities mentioned:
surface_form: Lake Baringo
instance_of: Lake
countries: Kenya
coordinates: lat: 0.63333333333333
lon: 36.083333333333
surface_form: kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
surface_form: baringo
instance_of: Lake
countries: Kenya
coordinates: lat: 0.63333333333333
lon: 36.083333333333
surface_form: lake bogoria
instance_of: Lake
countries: Kenya
coordinates: lat: 0.25
lon: 36.1
surface_form: bogoria
instance_of: Lake
countries: Kenya
coordinates: lat: 0.25
lon: 36.1
Lake Bogoria (formerly Lake Hannington) is a saline, alkaline lake that lies in a volcanic region in a half-graben basin south of Lake Baringo, Kenya, a little north of the equator. Lake Bogoria, like Lake Nakuru, Lake Elementeita, and Lake Magadi further south in the Rift Valley, and Lake Logipi to the north, is periodically home to one of the world's largest populations of lesser flamingos.

Geographic entities mentioned:
surface_form: Lake Magadi
instance_of: Lake
countries: Kenya
coordinates: lat: -1.8666666666667
lon: 36.266666666667
surface_form: Lake Logipi
instance_of: Lake
countries: Kenya
coordinates: lat: 2.2333333333333
lon: 36.566666666667
surface_form: magadi
instance_of: Lake
countries: Kenya
coordinates: lat: -1.8666666666667
lon: 36.266666666667
surface_form: lake bogoria
instance_of: Lake
countries: Kenya
coordinates: lat: 0.25
lon: 36.1
surface_form: bogoria
instance_of: Lake
countries: Kenya
coordinates: lat: 0.25
lon: 36.1
Lake Bogoria is located in Baringo County, about 120 km north of Nakuru city and 240 km north of Nairobi. It is in the Gregorian Rift Valley. It was once part of a larger freshwater lake, joined with the current Lake Baringo. As shown on the satellite picture at the top of this page, it is divided in three lobes: a large center one and two smaller ones at the north and south extremities.

Geographic entities mentioned:
surface_form: Lake Baringo
instance_of: Lake
countries: Kenya
coordinates: lat: 0.63333333333333
lon: 36.083333333333
surface_form: baringo
instance_of: Lake
countries: Kenya
coordinates: lat: 0.63333333333333
lon: 36.083333333333
The drainage basin is. The lowest point of the drainage divide is at 999 m near Loboi village; when the level of the lake reaches that altitude, its waters flow northward in lake Baringo drainage basin. In 1978 its maximum depth was recorded as or, and precise that this was in the largest sub-basin or lobe; and that the two smaller parts at the north and south extremities were deep at that time.

Geographic entities mentioned:
surface_form: lake Baringo
instance_of: Lake
countries: Kenya
coordinates: lat: 0.63333333333333
lon: 36.083333333333
surface_form: baringo
instance_of: Lake
countries: Kenya
coordinates: lat: 0.63333333333333
lon: 36.083333333333
surface_form: lake baringo
instance_of: Lake
countries: Kenya
coordinates: lat: 0.63333333333333
lon: 36.083333333333
For example, in 2020 its area increased to about: 2020 was one of the hottest years on record, but despite depressed rainfall in the short-rains season (October to December, or OND) it also saw a wetter than normal January and February because of the strong positive Indian Ocean Dipole index during that period, and enhanced rainfall during the long-rains season (March to May, or MAM) (that year, Lake Victoria rose to a new record level).

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Wetlands areas. The marshes to the north of the lake do not feed any river outlet. They are linked to both Lake Bogoria and adjacent Lake Baringo; both lakes are fed by the Waseges river (or Sandai river), the latter bringing a small permanent flow of the diverted Loboi river. These wetlands are fed by ephemeral or perennial streams, and by springs.

Geographic entities mentioned:
surface_form: Lake Baringo
instance_of: Lake
countries: Kenya
coordinates: lat: 0.63333333333333
lon: 36.083333333333
surface_form: baringo
instance_of: Lake
countries: Kenya
coordinates: lat: 0.63333333333333
lon: 36.083333333333
surface_form: lake baringo
instance_of: Lake
countries: Kenya
coordinates: lat: 0.63333333333333
lon: 36.083333333333
surface_form: lake bogoria
instance_of: Lake
countries: Kenya
coordinates: lat: 0.25
lon: 36.1
surface_form: bogoria
instance_of: Lake
countries: Kenya
coordinates: lat: 0.25
lon: 36.1
In 2003 its maximum depth is just over in an area of. This is relatively shallow, but nevertheless deeper — and therefore hydrologically more stable — than the other endorheic lakes in Kenya. The Rift Valley lakes undergo regular (and cyclic) changes in water levels mostly in response to precipitation, which is unreliable and unpredictable.

Geographic entities mentioned:
surface_form: kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
Wetlands. Although the lake is in a semi-arid part of Kenya Rift Valley, it is surrounded by numerous and varied wetlands along its shorelines, along faults where hot, warm and cold springs have developed, and along rivers that run across the rift floor. Types of wetlands. the graminoid vegetation is interspersed with cyanobacterial and algal mats.

Geographic entities mentioned:
surface_form: kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2