Sarmila/GeoWiki-Features huggingface dataset:
Saint Paul Peak. Saint Paul Peak is a mountain summit in Sanders County, Montana. Description. Saint Paul Peak is located south-southwest of Libby, Montana, in the Cabinet Mountains Wilderness, on land managed by Kaniksu National Forest. It is set west of the Continental Divide in the Cabinet Mountains which are a subrange of the Rocky Mountains.

Geographic entities mentioned:
surface_form: saint paul peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.079444444444
lon: -115.67638888889
It is set west of the Continental Divide in the Cabinet Mountains which are a subrange of the Rocky Mountains. Saint Paul Peak ranks as the fifth-highest summit in the Cabinet Mountains, and the eighth-highest in Sanders County. Precipitation runoff from the mountain drains into tributaries of the Clark Fork River.

Geographic entities mentioned:
surface_form: saint paul peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.079444444444
lon: -115.67638888889
Paul and Pacific Railroad. The mountain's toponym has been officially adopted by the U.S. Board on Geographic Names. Climate. Based on the Köppen climate classification, Saint Paul Peak is located in a subarctic climate zone characterized by long, usually very cold winters, and cool to mild summers. Winter temperatures can drop below −10 °F with wind chill factors below −30 °F.

Geographic entities mentioned:
surface_form: saint paul peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.079444444444
lon: -115.67638888889
It is located in the Moche District about 4 km south of the Historic Centre of Trujillo. Today it is a tourist area that presents recreational centers, agricultural areas and alongside this countryside. The Temples of the Sun and Moon is located in it. It is part of the Moche or Santa Catalina valley and was a place of development in the Moche culture. Description.

Geographic entities mentioned:
surface_form: Moche
instance_of: Valley
countries: Peru
&quot;D. stricticaulis&quot; is native to Australia, most commonly found near watercourses and granite outcrops in sandy clay or loam in Western Australia. &quot;D. stricticaulis&quot; has also been found in parts of South Australia, particularly the lower Eyre Peninsula and atop Dutchmans Stern in the southern Flinders Ranges. &quot;D.

Geographic entities mentioned:
surface_form: Dutchmans Stern
instance_of: Mountain
countries: Australia
coordinates: lat: -32.30613889
lon: 137.97078889
Maridalsvannet. Maridalsvannet () is a lake in Maridalen, Oslo, Norway. It is the largest lake in the municipality of Oslo, serving as its primary drinking water supply. The lake drains via the river Akerselva to the Oslofjord. The primary inflows are Skjærsjøelva and Dausjøelva. The Hammeren Hydroelectric Power Station exploits the fall from Skjærsjøen to Maridalsvannet.

Geographic entities mentioned:
surface_form: Maridalen
instance_of: Valley
countries: Norway
coordinates: lat: 59.99333333
lon: 10.77555556
surface_form: maridalsvannet
instance_of: Lake
countries: Norway
coordinates: lat: 59.98444444
lon: 10.77833333
The lake drains via the river Akerselva to the Oslofjord. The primary inflows are Skjærsjøelva and Dausjøelva. The Hammeren Hydroelectric Power Station exploits the fall from Skjærsjøen to Maridalsvannet. The shores of the lake and substantial areas of woods and fields around it are owned by the city of Oslo to protect the water supply.

Geographic entities mentioned:
surface_form: Skjærsjøen
instance_of: Lake
countries: Norway
coordinates: lat: 60.02208
lon: 10.70829
surface_form: maridalsvannet
instance_of: Lake
countries: Norway
coordinates: lat: 59.98444444
lon: 10.77833333
Maridalsvannet. Maridalsvannet () is a lake in Maridalen, Oslo, Norway. It is the largest lake in the municipality of Oslo, serving as its primary drinking water supply. The lake drains via the river Akerselva to the Oslofjord. The primary inflows are Skjærsjøelva and Dausjøelva. The Hammeren Hydroelectric Power Station exploits the fall from Skjærsjøen to Maridalsvannet.

Geographic entities mentioned:
surface_form: maridalsvannet
instance_of: Lake
countries: Norway
coordinates: lat: 59.98444444
lon: 10.77833333
Iuka, Mississippi. Iuka is a city in and the county seat of Tishomingo County, Mississippi, United States. Its population was 3,028 at the 2010 census. Woodall Mountain, the highest point in Mississippi, is located just south of Iuka. History. Iuka is built on the site of a Chickasaw village that is thought to have been subordinate to the settlement at Underwood Village.

Geographic entities mentioned:
surface_form: Woodall Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.787738888889
lon: -88.241627777778
The large summits and dry valleys of the TAM are some of the few places in Antarctica not covered by ice, the highest of which rise more than above sea level. The McMurdo Dry Valleys lie near McMurdo Sound and represent a special Antarctic phenomenon: landscapes that are snow and ice-free due to the extremely limited precipitation and ablation of ice in the valleys.

Geographic entities mentioned:
surface_form: McMurdo Dry Valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
The McMurdo Dry Valleys lie near McMurdo Sound and represent a special Antarctic phenomenon: landscapes that are snow and ice-free due to the extremely limited precipitation and ablation of ice in the valleys. The highest mountain of the TAM is the high Mount Kirkpatrick in the Queen Alexandra Range. Biology.

Geographic entities mentioned:
surface_form: Mount Kirkpatrick
instance_of: Mountain
coordinates: lat: -84.333333333333
lon: 166.41666666667
The following year, a party under expedition leader Robert Falcon Scott crossed into East Antarctica at a location now known as Ferrar Glacier, named after the geologist of the expedition. They explored part of Victoria Land on the Antarctic Plateau before returning via the same glacier. In 1908, Ernest Shackleton's party crossed the mountains through the Beardmore Glacier.

Geographic entities mentioned:
surface_form: Antarctic Plateau
instance_of: Plateau
coordinates: lat: -90
lon: 0
The motorway winds relatively steeply down past the site of New Zealand Refrigerating Company's former Burnside Freezing Works, and crosses the Main South Road/Kaikorai Valley Road interchange via an overbridge.Once on the flat of the Kaikorai Valley the motorway passes underneath the northbound on-ramp from Green Island before passing between the suburbs of Green Island and Abbotsford to the Green Island/Sunnyvale full diamond interchange.

Geographic entities mentioned:
surface_form: Kaikorai Valley
instance_of: Valley
countries: New Zealand
coordinates: lat: -45.8768
lon: 170.471
It is part of the larger Thale Noi Non-hunting Area. Thale Noi is the northernmost part of Songkhla Lake, separated from the main body of Thale Luang by a 0.5 m high natural sand bar, the waters are connected by a 2 km wide channel. While Thale Noi itself has only an area of 28 km2, it is surrounded by a swamp area of 459 km2. History. The district was established in 1896, then named Udon (อุดร).

Geographic entities mentioned:
surface_form: Songkhla Lake
instance_of: Lake
countries: Thailand
coordinates: lat: 7.2
lon: 100.46666666667
Metropolitana), Ecuador, Falklands, and Peru. It ranges from sea level in Tierra del Fuego to about 4000 m at the banks of Lake Titicaca. It grows in moist open grassland with other low herbs, on rill banks, snowmelt trickle and sometimes in brackish habitats.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
Lake Çavuşçu. Lake Çavuşçu (also known as Lake Ilgın) is a fresh water lake in Turkey
The lake is situated in Ilgın ilçe (district) of Konya Province at. Its elevation with respect to sea level is about. Its surface area is. The lake is fed by Battal and Çebişli creeks. Fauna.

Geographic entities mentioned:
surface_form: lake çavuşçu
instance_of: Lake
countries: Turkey
coordinates: lat: 38.3458
lon: 31.8768
Lake Çavuşçu. Lake Çavuşçu (also known as Lake Ilgın) is a fresh water lake in Turkey
The lake is situated in Ilgın ilçe (district) of Konya Province at. Its elevation with respect to sea level is about. Its surface area is. The lake is fed by Battal and Çebişli creeks. Fauna.

Geographic entities mentioned:
surface_form: lake çavuşçu
instance_of: Lake
countries: Turkey
coordinates: lat: 38.3458
lon: 31.8768
surface_form: lake ilgın
instance_of: Lake
countries: Turkey
coordinates: lat: 38.3458
lon: 31.8768
Geography. Huanglong County is located approximately from Yan'an's urban core, and from Xi'an's urban core. Located in the Loess Plateau, Huanglong County is hilly in elevation, ranging from to in height. A number of minor rivers run through the county. 87% of Huanglong County is forested, and the county is home to 1,012 species of plants and 225 species of animals. Climate.

Geographic entities mentioned:
surface_form: Loess Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Lake Shetek began forming as the climate started to warm 15,000 years ago. Water from the melting glaciers carved channels into the moraine. Where one channel—now occupied by Beaver Creek—intersected the channel now occupied by the Des Moines River, a buildup of sediment and slumping banks partially dammed the outflow, creating a large, shallow lake. Flora and fauna.

Geographic entities mentioned:
surface_form: shallow lake
instance_of: Lake
countries: United States
coordinates: lat: 43.49
lon: -74.444
The shoreline totals, about 85% of which is in private development. The watershed-to-lake ratio is 23:1, with much of that watershed under cultivation. Lake Shetek is by far the largest of Murray County's hundred or so lakes. The next largest is currently Lake Sarah just to the northwest. Great Oasis Lake at was once second-largest but was drained in the early 20th century for farmland.

Geographic entities mentioned:
surface_form: lake sarah
instance_of: Lake
countries: United States
coordinates: lat: 45.06583333
lon: -93.68111111
Lake Shetek. Lake Shetek is the largest lake in southwestern Minnesota, United States, and the headwaters of the Des Moines River. It is located in The Lakes, an unincorporated community in Murray County a few miles north-northwest of Currie. The name &quot;Shetek&quot; is derived from &quot;pelican&quot; in the Ojibwe language.

Geographic entities mentioned:
surface_form: lake shetek
instance_of: Lake
countries: United States
coordinates: lat: 44.12
lon: -95.69
The name &quot;Shetek&quot; is derived from &quot;pelican&quot; in the Ojibwe language. Since large lakes are rare in southwestern Minnesota and for some distance over the borders into Iowa and South Dakota, Lake Shetek is a significant regional draw for water recreation. Lake Shetek State Park lies on its eastern shore. Geography. Lake Shetek covers to a maximum depth of just.

Geographic entities mentioned:
surface_form: lake shetek
instance_of: Lake
countries: United States
coordinates: lat: 44.12
lon: -95.69
surface_form: lake shetek
instance_of: Lake
countries: United States
coordinates: lat: 44.12
lon: -95.69
The name &quot;Shetek&quot; is derived from &quot;pelican&quot; in the Ojibwe language. Since large lakes are rare in southwestern Minnesota and for some distance over the borders into Iowa and South Dakota, Lake Shetek is a significant regional draw for water recreation. Lake Shetek State Park lies on its eastern shore. Geography. Lake Shetek covers to a maximum depth of just.

Geographic entities mentioned:
surface_form: lake shetek
instance_of: Lake
countries: United States
coordinates: lat: 44.12
lon: -95.69
Lake Shetek contains three main islands: Valhalla, Keeley, and Loon Islands. Causeways connect the first two to the western shore, and another connects the third to the eastern shore. Shetek also connects to Bloody Lake Fremont Lake and Armstrong Slough. Geology. Lake Shetek and the surrounding landscape of wetlands and rolling hills are the result of glaciation.

Geographic entities mentioned:
surface_form: fremont lake
instance_of: Lake
countries: United States
coordinates: lat: 44.14722222
lon: -95.68111111
surface_form: bloody lake
instance_of: Lake
countries: United States
coordinates: lat: 44.12972222
lon: -95.6675
Due to its shallowness, the entire basin constitutes the littoral zone, which harbors common invertebrates like snails and insect larvae. Five common species of waterfowl all breed on Lake Shetek: the American coot, gadwall, mallard, northern shoveler, and ruddy duck. White pelicans, the lake's namesake, are often seen during migration. History.

Geographic entities mentioned:
surface_form: lake shetek
instance_of: Lake
countries: United States
coordinates: lat: 44.12
lon: -95.69
White pelicans, the lake's namesake, are often seen during migration. History. The earliest humans around Lake Shetek were likely following the bison that came there to drink. Archaeologists identify the first permanent inhabitants as members of the Great Oasis culture. French explorer Joseph Nicollet camped beside the lake for three days in 1838.

Geographic entities mentioned:
surface_form: lake shetek
instance_of: Lake
countries: United States
coordinates: lat: 44.12
lon: -95.69
He noted that the region's Dakota people called the lake &quot;Rabechy&quot;, meaning &quot;place where pelicans nest.&quot; However his journals and maps opted for the Ojibwe language equivalent, which was already in use by voyageurs. Pioneers established a small settlement along the east shore of Lake Shetek in the late 1850s.

Geographic entities mentioned:
surface_form: lake shetek
instance_of: Lake
countries: United States
coordinates: lat: 44.12
lon: -95.69
To combat unemployment during the Depression, the federal government authorized several job creation programs to conduct public work projects. The Works Progress Administration (WPA) arrived in 1934 with an ambitious plan to build a road system across Lake Shetek and a state park on the wooded eastern shore.

Geographic entities mentioned:
surface_form: lake shetek
instance_of: Lake
countries: United States
coordinates: lat: 44.12
lon: -95.69
However the program was disbanded in 1940 with the sixth and final causeway incomplete. The Tepeeotah Resort closed in the 1960s just as housing subdivisions burgeoned around the shore of Lake Shetek. Although the shoreline was greatly developed, better runoff management practices throughout the watershed improved Shetek's water quality.

Geographic entities mentioned:
surface_form: lake shetek
instance_of: Lake
countries: United States
coordinates: lat: 44.12
lon: -95.69
A portion of the Casey Jones State Trail was constructed in the 1990s between the lake and nearby Currie. Issues. As a shallow lake with a fairly high watershed-to-basin ratio, Lake Shetek can be strongly affected by environmental issues. Maintaining the water level has been a local concern for decades. The lake was dammed in the 1920s, then raised another in the 1930s.

Geographic entities mentioned:
surface_form: lake shetek
instance_of: Lake
countries: United States
coordinates: lat: 44.12
lon: -95.69
Lake Shetek State Park lies on its eastern shore. Geography. Lake Shetek covers to a maximum depth of just. This modest depth is wholly typical for the Prairie Pothole Region. The shoreline totals, about 85% of which is in private development. The watershed-to-lake ratio is 23:1, with much of that watershed under cultivation.

Geographic entities mentioned:
surface_form: prairie pothole
instance_of: Lake
countries: United States
coordinates: lat: 47.129839
lon: -99.253147
Glencairn. Glencairn is an area based around the Ballygomartin Road, which runs off the Woodvale Road, as well the Forthriver Road. It is bordered by the Crumlin Road. As well as a large housing estate the area also includes Glencairn Park, a large woodland area at the bottom of Divis Mountain. Previously the estate of the Cunningham family the area was open to the public in 1962.

Geographic entities mentioned:
surface_form: Divis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6075
lon: -6.0094444444444
Penck Trough. Penck Trough () is a broad ice-filled valley trending southwest to northeast, for about between Borg Massif and the northeast part of Kirwan Escarpment, in Queen Maud Land. It was discovered by the Third German Antarctic Expedition (1938–1939), led by Capt. Alfred Ritscher, and named for German geographer Albrecht Penck.

Geographic entities mentioned:
surface_form: Kirwan Escarpment
instance_of: Landform
coordinates: lat: -73.4167
lon: -3.5
surface_form: penck trough
instance_of: Valley
coordinates: lat: -73
lon: -2.75
Maps of the German Antarctic Expedition incorrectly represent this feature with a north-south axis, but it was accurately mapped by the Norwegian-British-Swedish Antarctic Expedition (NBSAE) (1949–1952), led by John Schjelderup Giæver. Isbrynet Hill is a rock hill southwest of Penck Ledge, rising above the ice slopes at the west side of the head of Penck Trough.

Geographic entities mentioned:
surface_form: Penck Ledge
instance_of: Mountain
coordinates: lat: -73.05
lon: -4.3
surface_form: penck trough
instance_of: Valley
coordinates: lat: -73
lon: -2.75
It was discovered by the Third German Antarctic Expedition (1938–1939), led by Capt. Alfred Ritscher, and named for German geographer Albrecht Penck. Maps of the German Antarctic Expedition incorrectly represent this feature with a north-south axis, but it was accurately mapped by the Norwegian-British-Swedish Antarctic Expedition (NBSAE) (1949–1952), led by John Schjelderup Giæver.

Geographic entities mentioned:
surface_form: alfred
instance_of: Mountain
coordinates: lat: -70.31133
lon: -69.23369
Penck Trough. Penck Trough () is a broad ice-filled valley trending southwest to northeast, for about between Borg Massif and the northeast part of Kirwan Escarpment, in Queen Maud Land. It was discovered by the Third German Antarctic Expedition (1938–1939), led by Capt. Alfred Ritscher, and named for German geographer Albrecht Penck.

Geographic entities mentioned:
surface_form: penck trough
instance_of: Valley
coordinates: lat: -73
lon: -2.75
Teneguía. Teneguía () is a monogenetic cinder cone – a volcanic vent which has been active once (in 1971) and has had further seismic activity. It is situated on the island of La Palma, one of the Canary Islands, and is located at the southern end of the sub-aerial section of the Cumbre Vieja volcano, of which Teneguía is just one of several vents. 1971 eruption.

Geographic entities mentioned:
surface_form: Cumbre Vieja
instance_of: Mountain
countries: Spain
coordinates: lat: 28.566666666667
lon: -17.833333333333
surface_form: teneguía
instance_of: Mountain
countries: Spain
coordinates: lat: 28.47333333
lon: -17.85166667
Densely populated zones were not affected. The vent has since become an attraction for tourists and forms part of the &quot;Monumento Natural de Los Volcanes de Teneguía&quot;. Until the 2011–12 El Hierro eruption, this was the last volcanic eruption in Spain, and until the 2021 Cumbre Vieja volcanic eruption, the last volcanic eruption in Spain on land.

Geographic entities mentioned:
surface_form: cumbre vieja
instance_of: Mountain
countries: Spain
coordinates: lat: 28.566666666667
lon: -17.833333333333
Teneguía. Teneguía () is a monogenetic cinder cone – a volcanic vent which has been active once (in 1971) and has had further seismic activity. It is situated on the island of La Palma, one of the Canary Islands, and is located at the southern end of the sub-aerial section of the Cumbre Vieja volcano, of which Teneguía is just one of several vents. 1971 eruption.

Geographic entities mentioned:
surface_form: teneguía
instance_of: Mountain
countries: Spain
coordinates: lat: 28.47333333
lon: -17.85166667
Densely populated zones were not affected. The vent has since become an attraction for tourists and forms part of the &quot;Monumento Natural de Los Volcanes de Teneguía&quot;. Until the 2011–12 El Hierro eruption, this was the last volcanic eruption in Spain, and until the 2021 Cumbre Vieja volcanic eruption, the last volcanic eruption in Spain on land.

Geographic entities mentioned:
surface_form: teneguía
instance_of: Mountain
countries: Spain
coordinates: lat: 28.47333333
lon: -17.85166667
The First Emperor made five tours of his domain in the 3rd century BC and had Li Si make seven stone inscriptions commemorating and praising his work, of which fragments of two survive. One of the most famous mountain steles is the high stele at Mount Tai with the personal calligraphy of Emperor Xuanzong of Tang commemorating his imperial sacrifices there in 725.

Geographic entities mentioned:
surface_form: Mount Tai
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 36.266666666667
lon: 117.1
Gamlang Razi. Gamlang Razi () is possibly Southeast Asia's highest mountain, located in the northern Myanmar state of Kachin. It is in Hkakaborazi National Park. The mountain lies on the border of Myanmar and Tibet, 15 km from the border tri-point with India. The 5881-m high Hkakabo Razi is located 6.6 km ENE from Gamlang Razi. It has year-round snow and glaciers. Mt.

Geographic entities mentioned:
surface_form: Hkakabo Razi
instance_of: Mountain
countries: Myanmar
coordinates: lat: 28.333055555556
lon: 97.466666666667
surface_form: gamlang razi
instance_of: Mountain
countries: Myanmar
coordinates: lat: 28.3059
lon: 97.468
Possibly the highest peak in Southeast Asia. Gamlang Razi has been measured at 5,870 ±2 m (19,259 ft). It makes the highest mountain in Southeast Asia whose height has been measured exactly by GPS. Hkakabo Razi has not yet been measured via GPS. However, Hkakabo Razi may still be the highest peak according to a recent expedition to that peak.

Geographic entities mentioned:
surface_form: hkakabo razi
instance_of: Mountain
countries: Myanmar
coordinates: lat: 28.333055555556
lon: 97.466666666667
It makes the highest mountain in Southeast Asia whose height has been measured exactly by GPS. Hkakabo Razi has not yet been measured via GPS. However, Hkakabo Razi may still be the highest peak according to a recent expedition to that peak. Though the expedition team reached only 5742 m (18,840 ft), they estimated that Hkakabo Razi's summit to be another 240 m (800 ft) higher.

Geographic entities mentioned:
surface_form: hkakabo razi
instance_of: Mountain
countries: Myanmar
coordinates: lat: 28.333055555556
lon: 97.466666666667
Gamlang Razi. Gamlang Razi () is possibly Southeast Asia's highest mountain, located in the northern Myanmar state of Kachin. It is in Hkakaborazi National Park. The mountain lies on the border of Myanmar and Tibet, 15 km from the border tri-point with India. The 5881-m high Hkakabo Razi is located 6.6 km ENE from Gamlang Razi. It has year-round snow and glaciers. Mt.

Geographic entities mentioned:
surface_form: gamlang razi
instance_of: Mountain
countries: Myanmar
coordinates: lat: 28.3059
lon: 97.468
The mountain lies on the border of Myanmar and Tibet, 15 km from the border tri-point with India. The 5881-m high Hkakabo Razi is located 6.6 km ENE from Gamlang Razi. It has year-round snow and glaciers. Mt. Gamlang Razi rock type is granite, according to the Department of Geological Survey of Myanmar. Climbing history. Andy Tyson (1968–2015) led the first ascent in 2013.

Geographic entities mentioned:
surface_form: gamlang razi
instance_of: Mountain
countries: Myanmar
coordinates: lat: 28.3059
lon: 97.468
In favorable weather, it typically takes about two weeks to reach the base camp. Possibly the highest peak in Southeast Asia. Gamlang Razi has been measured at 5,870 ±2 m (19,259 ft). It makes the highest mountain in Southeast Asia whose height has been measured exactly by GPS. Hkakabo Razi has not yet been measured via GPS.

Geographic entities mentioned:
surface_form: gamlang razi
instance_of: Mountain
countries: Myanmar
coordinates: lat: 28.3059
lon: 97.468
Their exploits included the destruction or capture of several Danish and Dutch ships on the Elbe. In early January, Colonel Sydau, with about 400 dragoons and 400 infantrymen, led another Swedish expedition to Elbe in Kehdingen against about 500 entrenched Münster soldiers under Lieutenant Colonel Lamsdorff.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
It is the second-largest marshalling yard in Germany after the Maschen Marshalling Yard. Geography. The station stretches along the Mannheim-Basel railroad line on an area of over 200 hectares between the Mannheim districts of Neckarau in the southwest, Neuhermsheim in the northwest, Pfingstberg in the southeast and Hochstätt in the northeast.

Geographic entities mentioned:
surface_form: Pfingstberg
instance_of: Mountain
countries: Germany
coordinates: lat: 52.4187
lon: 13.059
He named Burnaby Lake after his secretary Robert Burnaby, and he named Port Coquitlam's 400-foot 'Mary Hill' after his wife Mary Hawks. Moody designed the first Coat of arms of British Columbia.

Geographic entities mentioned:
surface_form: Burnaby Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.24306
lon: -122.94611
Below is a list of many ethnic enclaves present in the Los Angeles metropolitan area. Historical demographics. Los Angeles has a history of Jewish residents, and they used to have neighborhoods on the East side of Los Angeles in the early 20th century. Nowadays, Jews in Los Angeles tend to live in the West side and the San Fernando Valley.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Mount Russell (Alaska). Mount Russell is one of the major peaks of the central Alaska Range, approximately southwest of Denali. Though much lower than Denali or its neighbor Mount Foraker, Russell is a steep, dramatic peak and a significant mountaineering challenge in its own right.

Geographic entities mentioned:
surface_form: Denali
instance_of: Mountain
countries: United States
coordinates: lat: 63.06916666666667
lon: -151.0063888888889
surface_form: mount russell
instance_of: Mountain
countries: United States
coordinates: lat: 36.59
lon: -118.29083333333334
surface_form: mount russell
instance_of: Mountain
countries: United States
coordinates: lat: 62.7989
lon: -151.882
Mount Russell (Alaska). Mount Russell is one of the major peaks of the central Alaska Range, approximately southwest of Denali. Though much lower than Denali or its neighbor Mount Foraker, Russell is a steep, dramatic peak and a significant mountaineering challenge in its own right.

Geographic entities mentioned:
surface_form: Mount Foraker
instance_of: Mountain
countries: United States
coordinates: lat: 62.9608
lon: -151.398
surface_form: denali
instance_of: Mountain
countries: United States
coordinates: lat: 63.06916666666667
lon: -151.0063888888889
Mount Russell (Alaska). Mount Russell is one of the major peaks of the central Alaska Range, approximately southwest of Denali. Though much lower than Denali or its neighbor Mount Foraker, Russell is a steep, dramatic peak and a significant mountaineering challenge in its own right.

Geographic entities mentioned:
surface_form: mount russell
instance_of: Mountain
countries: United States
coordinates: lat: 36.59
lon: -118.29083333333334
surface_form: mount russell (alaska)
instance_of: Mountain
countries: United States
coordinates: lat: 62.7989
lon: -151.882
To give a sense of its size and steepness, note that its summit rises over the Chedotlothna Glacier to the northwest in only, and almost above the lower Yentna Glacier to the south in only. Mount Russell is the highest point in the Kuskokwim River watershed. The first ascent of Mount Russell was made on May 28, 1962, by a party led by Hellmut Raithel.

Geographic entities mentioned:
surface_form: mount russell
instance_of: Mountain
countries: United States
coordinates: lat: 36.59
lon: -118.29083333333334
surface_form: mount russell
instance_of: Mountain
countries: United States
coordinates: lat: 62.7989
lon: -151.882
Mount Russell is the highest point in the Kuskokwim River watershed. The first ascent of Mount Russell was made on May 28, 1962, by a party led by Hellmut Raithel. The summit party comprised Klaus Ekkerlein, Robert Goodwin, and Peter Hennig. They ascended the West Face from the Chedotlothna Glacier.

Geographic entities mentioned:
surface_form: mount russell
instance_of: Mountain
countries: United States
coordinates: lat: 36.59
lon: -118.29083333333334
surface_form: mount russell
instance_of: Mountain
countries: United States
coordinates: lat: 62.7989
lon: -151.882
This route is rated at Alaska Grade 2+, and is made much shorter by the feasibility of landing at around 8,000 feet in the basin, just outside the wilderness portion of the park. Overshadowed as it is by its larger neighbors, Mount Russell had seen only six recorded ascents by 2001. However guided climbs of the peak are available.

Geographic entities mentioned:
surface_form: mount russell
instance_of: Mountain
countries: United States
coordinates: lat: 36.59
lon: -118.29083333333334
surface_form: mount russell
instance_of: Mountain
countries: United States
coordinates: lat: 62.7989
lon: -151.882
Mount Sago. Sago (also known as Malintang) is a mountain in West Sumatra, Indonesia. It is near the city of Payakumbuh and the town of Batusangkar. Mount Sago (Indonesian: Gunung Sago) is an imposing stratovolcano. It is one of the many mountains that form part of the Bukit Barisan Range, which runs along the western side of Sumatra island.

Geographic entities mentioned:
surface_form: sago
instance_of: Mountain
countries: Indonesia
coordinates: lat: -0.32694444444444
lon: 100.67055555556
surface_form: mount sago
instance_of: Mountain
countries: Indonesia
coordinates: lat: -0.32694444444444
lon: 100.67055555556
Mount Sago. Sago (also known as Malintang) is a mountain in West Sumatra, Indonesia. It is near the city of Payakumbuh and the town of Batusangkar. Mount Sago (Indonesian: Gunung Sago) is an imposing stratovolcano. It is one of the many mountains that form part of the Bukit Barisan Range, which runs along the western side of Sumatra island.

Geographic entities mentioned:
surface_form: sago
instance_of: Mountain
countries: Indonesia
coordinates: lat: -0.32694444444444
lon: 100.67055555556
Mount Sago. Sago (also known as Malintang) is a mountain in West Sumatra, Indonesia. It is near the city of Payakumbuh and the town of Batusangkar. Mount Sago (Indonesian: Gunung Sago) is an imposing stratovolcano. It is one of the many mountains that form part of the Bukit Barisan Range, which runs along the western side of Sumatra island.

Geographic entities mentioned:
surface_form: sago
instance_of: Mountain
countries: Indonesia
coordinates: lat: -0.32694444444444
lon: 100.67055555556
surface_form: sago
instance_of: Mountain
countries: Indonesia
coordinates: lat: -0.32694444444444
lon: 100.67055555556
surface_form: mount sago
instance_of: Mountain
countries: Indonesia
coordinates: lat: -0.32694444444444
lon: 100.67055555556
surface_form: gunung sago
instance_of: Mountain
countries: Indonesia
coordinates: lat: -0.32694444444444
lon: 100.67055555556
Mount Sago (Indonesian: Gunung Sago) is an imposing stratovolcano. It is one of the many mountains that form part of the Bukit Barisan Range, which runs along the western side of Sumatra island. With an elevation of approximately 2,261 meters (7,451 feet) above sea level, Mount Sago stands as a prominent feature in the region’s landscape.

Geographic entities mentioned:
surface_form: sago
instance_of: Mountain
countries: Indonesia
coordinates: lat: -0.32694444444444
lon: 100.67055555556
surface_form: mount sago
instance_of: Mountain
countries: Indonesia
coordinates: lat: -0.32694444444444
lon: 100.67055555556
The route west from Montreal has been called the 'first Trans-Canada Highway'. It ran from near Montreal, up the Ottawa River, west up the Mattawa River to Trout Lake and over the 7 mile La Vase portage at what is now North Bay on Lake Nipissing and down the French River to Georgian Bay of Lake Huron. This route was first used by Étienne Brûlé in 1610 and later by Champlain.

Geographic entities mentioned:
surface_form: Lake Nipissing
instance_of: Lake
countries: Canada
coordinates: lat: 46.283333333333
lon: -80
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Lawrence at Trois-Rivières. Routes ran from the French River south to the Jesuit Huron missions at the southern end of Georgian Bay (1626–1640), west through the Strait of Mackinac to Lake Michigan, or west north of Manitoulin Island and up the St Marys River (26 feet difference in elevation) to Lake Superior.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
On Lake Superior voyageurs would normally hug the northern shore because of the danger of frequent squalls that could overturn their boats. The route up the St. Lawrence to Lake Ontario, Niagara Falls, Lake Erie, Detroit River, Lake St. Clair, St. Clair River and lower Lake Huron developed later (Adrien Jolliet in 1669 was probably the first) and was never the main westward route. North of the St.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
North of the St. Lawrence were many complex lakes and rivers that were sometimes used to go as far as James Bay. The Toronto Carrying-Place Trail was a major portage route in the St. Lawrence basin, linking Lake Ontario with Lake Simcoe and the northern Great Lakes. Nelson River basin. The Canada–United States border meets Lake Superior near Grand Portage, Minnesota.

Geographic entities mentioned:
surface_form: Lake Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
It continues down the Loon River to Lake Namakan and north over either of two portages to Rainy Lake (a depot was established here to shorten the voyage of the Athabasca brigade) and down the Rainy River to Lake of the Woods west-northwest of Grand Portage. Leaving the US border, northwest down the Winnipeg River with 26 portages to Lake Winnipeg, a poor lake for small craft.

Geographic entities mentioned:
surface_form: Rainy Lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 48.636944444444
lon: -93.031388888889
surface_form: Lake of the Woods
instance_of: Lake
countries: Canada
United States
coordinates: lat: 49.09027777777778
lon: -95.2388888888889
It continues down the Loon River to Lake Namakan and north over either of two portages to Rainy Lake (a depot was established here to shorten the voyage of the Athabasca brigade) and down the Rainy River to Lake of the Woods west-northwest of Grand Portage. Leaving the US border, northwest down the Winnipeg River with 26 portages to Lake Winnipeg, a poor lake for small craft.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
For the two routes from Lake Superior see Grand Portage National Monument and Kaministiquia River. A minor route ran from Duluth, Minnesota west and north up the St. Louis River and Embarrass River over another Height of Land Portage and north down the Pike River (Minnesota) and Vermilion River (Minnesota) to Rainy Lake on the Grand Portage route.

Geographic entities mentioned:
surface_form: Rainy Lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 48.636944444444
lon: -93.031388888889
Around these rapids to Cedar Lake. (Cedar Lake is one of the chain of lakes that look like a single lake west of Lake Winnipeg.) Although it was not much used, a route ran from Cedar Lake south over the Mossy portage to Lake Winnipegosis and then the mile-and-a-half Meadow Portage to Lake Manitoba and then at least of Portage la Prairie to the Assiniboine River.

Geographic entities mentioned:
surface_form: Lake Winnipegosis
instance_of: Lake
countries: Canada
coordinates: lat: 52.5
lon: -100
surface_form: Lake Manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
From the depot at Cumberland House, Saskatchewan on the lower Saskatchewan River, this route runs north up the Sturgeon-Weir River, across Frog Portage to the east-flowing Churchill River which is mostly a chain of lakes, west up the Churchill past the depot on Lac Île-à-la-Crosse, through Peter Pond Lake to Lac La Loche and over the 12 mile Methye Portage to the Clearwater River whose waters reach the Arctic.

Geographic entities mentioned:
surface_form: Lac Île-à-la-Crosse
instance_of: Lake
countries: Canada
coordinates: lat: 55.4444
lon: -107.849
surface_form: Peter Pond Lake
instance_of: Lake
countries: Canada
coordinates: lat: 56.00918
lon: -108.86918
surface_form: Lac La Loche
instance_of: Lake
countries: Canada
coordinates: lat: 56.5128
lon: -109.587
The Methye Portage, which was first reached by Peter Pond in 1778 ranks with Grand Portage as the most difficult of the major portages. The route continues west down the Clearwater River to the Athabasca River at Fort McMurray and north down the Athabasca to the Peace-Athabasca Delta and the depot at Fort Chipewyan, Alberta, at the west end of Lake Athabasca.

Geographic entities mentioned:
surface_form: Lake Athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
This was about as far as canoes could reach and return in one season and was the gathering place for furs from the rich Athabasca region and further west. One could continue into poorer country north down the Slave River to the Great Slave Lake and thence northwest down the Mackenzie River to the Arctic Ocean. Pacific coast.

Geographic entities mentioned:
surface_form: Great Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 61.666666666667
lon: -114
From there it went at least 400 miles south-southeast up the Yukon River and Pelly River, then the Findlayson and Campbell Rivers and a portage to Frances Lake, down the Frances River to the Liard River and east to Fort Simpson on the Mackenzie about 275 miles east of Frances Lake. There was some transport on the Liard, but the Liard river canyon made this difficult. Mississippi basin.

Geographic entities mentioned:
surface_form: Frances Lake
instance_of: Lake
countries: Canada
coordinates: lat: 61.3478
lon: -129.572
Another route was the Chicago River and across the Chicago Portage to the Des Plaines River and south to the Illinois. Alternatively, from the northwest side of Lake Michigan, at the head of Green Bay, up the Fox River, past serious rapids to Lake Winnebago, up the Fox and over a short portage to the Wisconsin River and southwest to the Mississippi.

Geographic entities mentioned:
surface_form: Lake Winnebago
instance_of: Lake
countries: United States
coordinates: lat: 44.0169756
lon: -88.4095327
Lake-Champlain-Hudson River. This was the main axis of British-French and British-US military conflict late in the period. From Quebec upriver about a third of the way to Montreal, up the Richelieu River to Lake Champlain, portage west parallel to the La Chute River (230 feet drop in miles) to Lake George, overland to the Hudson River and downstream to New York. Upper Ohio River basin.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Johannes Philippus de Lignamine. Johannes Philippus de Lignamine (1420 &ndash; ??) was a Sicilian printer/publisher and tax collector from Messina active at Monte Cassino near Rome and a courtier to Pope Sixtus IV. He is best known for his publication of &quot;Herbarium Apuleii Platonici&quot; in 1481.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
Fissile Peak. Fissile Peak, formerly known as Red Mountain, is a mountain peak located on the eastern side of Cheakamus Lake southeast of Whistler in Garibaldi Provincial Park of British Columbia, Canada. The mountain is composed of red slate which is easily divided into thin sheets of uniform thickness; in geological terms this feature is known as fissility. __NOTOC__
Climate.

Geographic entities mentioned:
surface_form: Cheakamus Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.0081
lon: -122.92
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: red mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
surface_form: red mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.2036
lon: -122.549
surface_form: fissile peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0186
lon: -122.849
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: red mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.0919
lon: -117.821
Fissile Peak. Fissile Peak, formerly known as Red Mountain, is a mountain peak located on the eastern side of Cheakamus Lake southeast of Whistler in Garibaldi Provincial Park of British Columbia, Canada. The mountain is composed of red slate which is easily divided into thin sheets of uniform thickness; in geological terms this feature is known as fissility. __NOTOC__
Climate.

Geographic entities mentioned:
surface_form: fissile peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0186
lon: -122.849
__NOTOC__
Climate. Based on the Köppen climate classification, Fissile Peak is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall.

Geographic entities mentioned:
surface_form: fissile peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0186
lon: -122.849
As a result, the Coast Mountains experience high precipitation, especially during the winter months in the form of snowfall. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. The months July through September offer the most favorable weather for climbing Fissile Peak.

Geographic entities mentioned:
surface_form: fissile peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0186
lon: -122.849
Fissile Peak. Fissile Peak, formerly known as Red Mountain, is a mountain peak located on the eastern side of Cheakamus Lake southeast of Whistler in Garibaldi Provincial Park of British Columbia, Canada. The mountain is composed of red slate which is easily divided into thin sheets of uniform thickness; in geological terms this feature is known as fissility. __NOTOC__
Climate.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Cotopaxi. Cotopaxi () is an active stratovolcano in the Andes Mountains, located near Latacunga city of Cotopaxi Province, about south of Quito, and northeast of the city of Latacunga, Ecuador. It is the second highest summit in Ecuador (after Chimborazo), reaching a height of. Cotopaxi is among the highest active volcanoes in the world.

Geographic entities mentioned:
surface_form: Chimborazo
instance_of: Mountain
countries: Ecuador
coordinates: lat: -1.4691666666667
lon: -78.8175
The volcano &quot;remains in a very abnormal situation. In August, 2,100 earthquakes were recorded and emission rates of sulfur dioxide reach approximately. The government estimates some 300,000 people are at risk from the volcano in the provinces of Cotopaxi, Tungurahua, Napo and Pichincha. Climbing.

Geographic entities mentioned:
surface_form: tungurahua
instance_of: Mountain
countries: Ecuador
coordinates: lat: -1.4669444444444
lon: -78.441666666667
surface_form: cotopaxi
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.68055555555556
lon: -78.437777777778
surface_form: pichincha
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.17722222222222
lon: -78.598888888889
Cotopaxi. Cotopaxi () is an active stratovolcano in the Andes Mountains, located near Latacunga city of Cotopaxi Province, about south of Quito, and northeast of the city of Latacunga, Ecuador. It is the second highest summit in Ecuador (after Chimborazo), reaching a height of. Cotopaxi is among the highest active volcanoes in the world.

Geographic entities mentioned:
surface_form: cotopaxi
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.68055555555556
lon: -78.437777777778
Cotopaxi. Cotopaxi () is an active stratovolcano in the Andes Mountains, located near Latacunga city of Cotopaxi Province, about south of Quito, and northeast of the city of Latacunga, Ecuador. It is the second highest summit in Ecuador (after Chimborazo), reaching a height of. Cotopaxi is among the highest active volcanoes in the world.

Geographic entities mentioned:
surface_form: cotopaxi
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.68055555555556
lon: -78.437777777778
surface_form: cotopaxi
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.68055555555556
lon: -78.437777777778
It is the second highest summit in Ecuador (after Chimborazo), reaching a height of. Cotopaxi is among the highest active volcanoes in the world. Cotopaxi is known to have erupted 87 times, resulting in the creation of numerous valleys formed by lahars (mudflows) around the volcano. An ongoing eruption began on 21 October 2022.

Geographic entities mentioned:
surface_form: cotopaxi
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.68055555555556
lon: -78.437777777778
Cotopaxi is known to have erupted 87 times, resulting in the creation of numerous valleys formed by lahars (mudflows) around the volcano. An ongoing eruption began on 21 October 2022. At the end of February 2023, the Geophysical Institute of Ecuador reported that Cotopaxi had produced around 8,000 earthquakes since October 21, 2022, amounting to 1,600 events per month. Description.

Geographic entities mentioned:
surface_form: cotopaxi
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.68055555555556
lon: -78.437777777778
At the end of February 2023, the Geophysical Institute of Ecuador reported that Cotopaxi had produced around 8,000 earthquakes since October 21, 2022, amounting to 1,600 events per month. Description. On a clear day, Cotopaxi is clearly visible on the skyline from Latacunga and Quito. It is part of the chain of volcanoes around the Pacific Plate known as the Pacific Ring of Fire.

Geographic entities mentioned:
surface_form: cotopaxi
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.68055555555556
lon: -78.437777777778
It has an almost symmetrical cone that rises from a highland plain of about, with a width at its base of about. It has one of the few equatorial glaciers in the world, which starts at the height of. At its summit, Cotopaxi has an wide crater which is deep. The crater consists of two concentric crater rims, the outer one being partly free of snow and irregular in shape.

Geographic entities mentioned:
surface_form: cotopaxi
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.68055555555556
lon: -78.437777777778