Sarmila/GeoWiki-Features huggingface dataset:
There is no detectable life living in Hodgson Lake. The lake extends eastward into George VI Sound and the George VI Ice Shelf making it adjacent to the sound. The northern side of this lake is bounded by the Saturn Glacier, which flows east into George VI Sound. The lake lies next to and southeast of Citadel Bastion, a pre-eminent mountain on Alexander Island.

Geographic entities mentioned:
surface_form: george
instance_of: Mountain
coordinates: lat: -67.71667
lon: 50
Bois Blanc Island (Michigan). Bois Blanc Island () is an island in Lake Huron within Bois Blanc Township, Mackinac County, Michigan. The island covers about and is about 12 miles (19 km) long, 6 miles (9.6 km) wide and has 6 lakes. It lies southeast of Mackinac Island and almost due north of the city of Cheboygan. &quot;Bois Blanc&quot; is French for &quot;white wood&quot;.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Adlersberg. The Adlersberg is a hill in the Harz mountains of central Germany that lies south of Sieber in the district of Göttingen in Lower Saxony. It is 593.2 m high and is situated west of the Aschentalshalbe. It also separates the valley of &quot;Breitental&quot; (&quot;wide valley&quot;) with its river, the Tiefenbeek, from the &quot;Langental&quot; (&quot;long valley&quot;).

Geographic entities mentioned:
surface_form: Aschentalshalbe
instance_of: Mountain
countries: Germany
coordinates: lat: 51.6863
lon: 10.4526
It also separates the valley of &quot;Breitental&quot; (&quot;wide valley&quot;) with its river, the Tiefenbeek, from the &quot;Langental&quot; (&quot;long valley&quot;). To the northwest the Adlersberg transitions to the Kloppstert and the Fissenkenkopf hills. Other nearby peaks are the Pagelsburg 1.2 km south, the Höxterberg 1.6 km southwest and the Großer Knollen 1.9 km southeast.

Geographic entities mentioned:
surface_form: Kloppstert
instance_of: Mountain
countries: Germany
coordinates: lat: 51.6856
lon: 10.4169
surface_form: Fissenkenkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 51.6853
lon: 10.4092
surface_form: fissenkenkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 51.6853
lon: 10.4092
surface_form: kloppstert
instance_of: Mountain
countries: Germany
coordinates: lat: 51.6856
lon: 10.4169
It also separates the valley of &quot;Breitental&quot; (&quot;wide valley&quot;) with its river, the Tiefenbeek, from the &quot;Langental&quot; (&quot;long valley&quot;). To the northwest the Adlersberg transitions to the Kloppstert and the Fissenkenkopf hills. Other nearby peaks are the Pagelsburg 1.2 km south, the Höxterberg 1.6 km southwest and the Großer Knollen 1.9 km southeast.

Geographic entities mentioned:
surface_form: Pagelsburg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.6723
lon: 10.4186
surface_form: Höxterberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.6723
lon: 10.4057
surface_form: Großer Knollen
instance_of: Mountain
countries: Germany
coordinates: lat: 51.667222222222
lon: 10.429722222222
surface_form: höxterberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.6723
lon: 10.4057
surface_form: großer knollen
instance_of: Mountain
countries: Germany
coordinates: lat: 51.667222222222
lon: 10.429722222222
Adlersberg. The Adlersberg is a hill in the Harz mountains of central Germany that lies south of Sieber in the district of Göttingen in Lower Saxony. It is 593.2 m high and is situated west of the Aschentalshalbe. It also separates the valley of &quot;Breitental&quot; (&quot;wide valley&quot;) with its river, the Tiefenbeek, from the &quot;Langental&quot; (&quot;long valley&quot;).

Geographic entities mentioned:
surface_form: adlersberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.6831
lon: 10.4197
Letnitsa Glacier. Letnitsa Glacier (,) is a long glacier on Smith Island in the South Shetland Islands, Antarctica draining the southeast slopes of Imeon Range east of Organa Peak and south of Riggs Peak. It is situated southwest of Gramada Glacier and northeast of Kremena Ice Piedmont, and flows southeastward into Hisarya Cove, Osmar Strait. Bulgarian early mapping in 2009.

Geographic entities mentioned:
surface_form: Organa Peak
instance_of: Mountain
coordinates: lat: -63.050555555556
lon: -62.629722222222
surface_form: Riggs Peak
instance_of: Mountain
coordinates: lat: -63.035555555556
lon: -62.613888888889
Narrative and historicity. According to Sawa oral history, Mbedi, the son of Mbongo, lived at Piti on the Dibamba River, northeast of present-day Douala. He was the father of Bojongo, Dibongo, Ewale, and several others. For reasons that vary with the tale, Mbedi's sons left him and migrated south to the coast.

Geographic entities mentioned:
surface_form: Dibamba River
instance_of: Watercourse
countries: Cameroon
coordinates: lat: 3.948858
lon: 9.762726
Nyanza Province (;) was one of Kenya's eight administrative provinces before the formation of the 47 counties under the 2010 constitution. Six counties were organised in the area of the former province. The region is located in the southwestern part of Kenya around Lake Victoria. It includes part of the eastern edge of the lake and is inhabited predominantly by the Luo people and Kisii people.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
In 2013, the manufacturer Erbak-Uludağ İçecek A.Ş. achieved total sales of over 200 million U.S. dollars. Naming. The branded labels use the name of Mount Uludağ located in western Turkey. Previously, the drink was made exclusively from water sources of this mountain. Gazoz is a Turkish lemonade variety, and Uludağ Gazoz is the most well known.

Geographic entities mentioned:
surface_form: Uludağ
instance_of: Mountain
countries: Turkey
coordinates: lat: 40.0705295
lon: 29.222009805555555
Obernberger Seebach. The Obernberger Seebach, formerly called Obernberger Ache, is a river in Tyrol, Austria, a tributary of the Sill. The Obernberger Seebach originates south-west of the Brenner in the Stubai Alps and takes a north-east route to its mouth. On its course, it flows through Lake Obernberg. In the middle of the valley the river passes through the village of Obernberg am Brenner.

Geographic entities mentioned:
surface_form: Lake Obernberg
instance_of: Lake
countries: Austria
coordinates: lat: 46.991243
lon: 11.403759
Ski Ben Eoin. Ski Ben Eoin is a ski hill located in Ben Eoin, Nova Scotia, Canada, which is approximately 27 km from Sydney. The hill overlooks the East Bay of the Bras d'Or Lakes. The ski hill was founded in 1968. It features 11 runs, including a terrain park, and has two lifts, one a quad chair and the other a magic carpet. The longest run is 1300 m. The hill has a vertical drop of 153 m.

Geographic entities mentioned:
surface_form: Bras d'Or Lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.860277777778
lon: -60.778888888889
Ski jumping at the 2014 Winter Olympics – Men's large hill individual. The men's large hill individual ski jumping competition for the 2014 Winter Olympics in Sochi, Russia, was held on 14–15 February 2014 at RusSki Gorki Jumping Center in the Esto-Sadok village on the northern slope of Aibga Ridge in Krasnaya Polyana.

Geographic entities mentioned:
surface_form: Aibga Ridge
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 43.6278
lon: 40.2869
Pic de Nore transmitter. Pic de Nore transmitter is a facility for FM/TV transmission situated on the mountain of same name at 43°25'29&quot;N 2°27'47&quot;E, in the Montagne Noire, on the border of the Aude and Tarn departments, near to the Parc naturel régional du Haut-Languedoc in southern France. It uses a 102 metres tall concrete tower.

Geographic entities mentioned:
surface_form: mountain of same name
instance_of: Mountain
countries: France
coordinates: lat: 43.42416667
lon: 2.46277778
Capoeta razii. &quot;Capoeta razii&quot;, is a newly described species of freshwater cyprinid fish occurring mainly in the southern Caspian Sea basin, Iran. This species was mistakenly reported by many authors as &quot;Capoeta gracilis&quot; in northern Iranian regions. It was first reported to be different from &quot;C. gracilis&quot; by Levin et al. (2012).

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Of the water in the municipality, 0.8% is in lakes and 0.4% is in rivers and streams. The municipality is located in the Gruyère district, at the southern end of the Lake of Gruyère. It consists of the &quot;haufendorf&quot; village (an irregular, unplanned and quite closely packed village, built around a central square) of Morlon on the Bulle-Fribourg road. Coat of arms.

Geographic entities mentioned:
surface_form: Lake of Gruyère
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.65
lon: 7.1
Grant Peak (Murray Range). Grant Peak is a mountain in the Murray Range of the Hart Ranges in Northern British Columbia. Grant Peak is named for Royal Canadian Naval Volunteer Reserve Ordinary Seaman George William Grant from Prince George, BC; serving with HMMTB 460 when he died, 2 July 1944. O/S Grant is buried at Haslar Royal Naval Cemetery, Hampshire.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: grant peak
instance_of: Mountain
countries: Canada
coordinates: lat: 55.2175
lon: -122.2825
Grant Peak (Murray Range). Grant Peak is a mountain in the Murray Range of the Hart Ranges in Northern British Columbia. Grant Peak is named for Royal Canadian Naval Volunteer Reserve Ordinary Seaman George William Grant from Prince George, BC; serving with HMMTB 460 when he died, 2 July 1944. O/S Grant is buried at Haslar Royal Naval Cemetery, Hampshire.

Geographic entities mentioned:
surface_form: grant peak
instance_of: Mountain
countries: Canada
coordinates: lat: 55.2175
lon: -122.2825
Square Peak. Square Peak () is located in the Livingston Range, Glacier National Park in the U.S. state of Montana. Square Peak is SSW of Rainbow Peak.

Geographic entities mentioned:
surface_form: Rainbow Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.8792
lon: -114.097
surface_form: square peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.8667
lon: -114.104
Square Peak. Square Peak () is located in the Livingston Range, Glacier National Park in the U.S. state of Montana. Square Peak is SSW of Rainbow Peak.

Geographic entities mentioned:
surface_form: square peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.8667
lon: -114.104
The Franco-British plan, as initially designed, proposed a defence of all of Scandinavia north of a line Stockholm–Gothenburg or Stockholm–Oslo (the British concept of &quot;the Lake Line&quot; following the lakes of Mälaren, Hjälmaren, and Vänern), which would provide a good natural defense some south of Narvik.

Geographic entities mentioned:
surface_form: Mälaren
instance_of: Lake
countries: Sweden
coordinates: lat: 59.5
lon: 17.2
surface_form: Hjälmaren
instance_of: Lake
countries: Sweden
coordinates: lat: 59.25
lon: 15.75
surface_form: Vänern
instance_of: Lake
countries: Sweden
coordinates: lat: 58.916666666667
lon: 13.5
The average location in Western Washington gets 168 days of measurable precipitation per year. The place that receives the most recorded precipitation is Lake Quinault on the Olympic Peninsula, with an average of per year. The Long Beach Experimental Station has the most days of measurable precipitation, averaging 215 each year. Population.

Geographic entities mentioned:
surface_form: Lake Quinault
instance_of: Lake
countries: United States
coordinates: lat: 47.476377777778
lon: -123.87016388889
The section between Battersby and Picton closed to passengers in 1954. From Battersby, goods trains also ran south to Ingleby where a cable pulley system raised wagons up a steep incline, and across the North York Moors to iron ore workings at Rosedale and Farndale.

Geographic entities mentioned:
surface_form: Rosedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.35
lon: -0.88333333333333
surface_form: Farndale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.3463
lon: -0.965
This is clad inside and out in Canadian materials where possible; the 10.5 million bricks were made by inmates of the Central Prison, and the Ontario sandstone—with a pink hue that has earned the building the colloquial name of &quot;The Pink Palace&quot;—comes from the Credit River valley and Orangeville, Ontario, and was given a rustic finish for most of the exterior, but dressed for trim around windows and other edges.

Geographic entities mentioned:
surface_form: Credit River
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.5478
lon: -79.5808
Round Lake (Bonner County, Idaho). Round Lake is a body of water located southwest of Sagle in Bonner County, Idaho. It is the prime feature of Round Lake State Park and has of shoreline. The maximum water depth is. The lakeshore and watershed are heavily forested and undeveloped. The shoreline is undeveloped except for the public swimming beach at the state park.

Geographic entities mentioned:
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9344286
lon: -96.9790408
surface_form: round lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.0648
lon: -75.1033
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 46.1508
lon: -86.7447
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.070277777778
lon: -74.584722222222
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 42.934604
lon: -73.7823057
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 27.9631
lon: -81.674
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 45.036388888889
lon: -97.773055555556
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 43.531388888889
lon: -75.180277777778
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.8685
lon: -93.4925
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 48.161666666667
lon: -116.63805555556
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 45.6020431
lon: -122.4032555
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 41.837095
lon: -86.418541
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.964444444444
lon: -96.827222222222
The maximum water depth is. The lakeshore and watershed are heavily forested and undeveloped. The shoreline is undeveloped except for the public swimming beach at the state park. Round Lake is eutrophic; its primary water source is Cocolalla Lake via Cocolalla Creek. The outflow is via the continuation of Cocolalla Creek. Most of the lake bottom is silt and detritus.

Geographic entities mentioned:
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9344286
lon: -96.9790408
surface_form: round lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.0648
lon: -75.1033
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 46.1508
lon: -86.7447
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.070277777778
lon: -74.584722222222
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 42.934604
lon: -73.7823057
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 27.9631
lon: -81.674
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 45.036388888889
lon: -97.773055555556
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 43.531388888889
lon: -75.180277777778
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.8685
lon: -93.4925
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 48.161666666667
lon: -116.63805555556
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 45.6020431
lon: -122.4032555
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 41.837095
lon: -86.418541
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.964444444444
lon: -96.827222222222
Exploration of the Southern Great Basin. By 1849, the Mormon pioneers were well established in the Salt Lake Valley, and their leader, Brigham Young, was anxious to branch out. At his request, the territorial legislature commissioned an exploring party to map the country to the south and identify areas that would make good settlements. Parley P. Pratt led the party that departed on Nov 23, 1849.

Geographic entities mentioned:
surface_form: Salt Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.6839
lon: -111.978
Livno. Livno () is a town and the administrative center of the Township of Livno and Canton 10 of the Federation of Bosnia and Herzegovina, an entity of Bosnia and Herzegovina. It is situated on the river Bistrica at the southeastern edge of the Livno Field at the foot of Kruzi plateau which is located beneath the Cincar mountain and rocky hill Crvenice.

Geographic entities mentioned:
surface_form: Cincar
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.90222222
lon: 17.06277778
Livno is also situated in the Livanjsko field which is the largest field in the entire country. The field is situated between the mountains Dinara and Kamešnica in the south, Tušnica in the east, Cincar in the north and Šator in the west. Livanjsko field is, making it almost half of the Livno municipality. Climate. Livno has a stable continental climate with cold winters and warm summers.

Geographic entities mentioned:
surface_form: Cincar
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.90222222
lon: 17.06277778
surface_form: Šator
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 44.157330555556
lon: 16.5897
The Leinstermen broke the truce however, and Fergal retaliated by invading again. However in December of 722 Fergal and numerous nobles of the Ui Neill were slain at the Battle of Allen (County Kildare) by the Leinstermen led by Murchad.

Geographic entities mentioned:
surface_form: Battle of Allen
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.229497222222
lon: -6.8633111111111
Mount Silverthrone. Mount Silverthrone, officially named Silverthrone Mountain, is a mountain in the Pacific Ranges of the Coast Mountains of British Columbia, Canada, located over northwest of the city of Vancouver and about west of Mount Waddington, British Columbia, Canada.

Geographic entities mentioned:
surface_form: Mount Waddington
instance_of: Mountain
countries: Canada
coordinates: lat: 51.373611111111
lon: -125.26333333333
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount silverthrone
instance_of: Mountain
countries: Canada
coordinates: lat: 51.51777777777778
lon: -126.11333333333333
surface_form: silverthrone mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.51777777777778
lon: -126.11333333333333
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
It is the highest peak in the Ha-Iltzuk Icefield, which is the largest icefield in the Coast Mountains south of the Alaska Panhandle. Geology. Mount Silverthrone is an eroded lava dome on the northeast edge of a large caldera complex called the Silverthrone Caldera. It lies within the Coast Plutonic Complex, which is the single largest contiguous granite outcropping in the world.

Geographic entities mentioned:
surface_form: Silverthrone Caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
surface_form: mount silverthrone
instance_of: Mountain
countries: Canada
coordinates: lat: 51.51777777777778
lon: -126.11333333333333
The plutonic and metamorphic rocks extend approximately 1,800 kilometers on the coast of British Columbia, southwestern Yukon and southeastern Alaska. In addition, Garibaldi, Meager, Cayley and Silverthrone areas are of recent volcanic origin. The volcanic terrain in the Silverthrone area is very similar to the Mount Meager massif further south. However, there is much more ice.

Geographic entities mentioned:
surface_form: Garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
The extensive icefields around Mount Silverthrone are receding and are small compared to their former extent, but they are an impressive indication of how much of British Columbia looked 10,000 years or more ago. Silverthrone contains one of the few calderas buried beneath the ice caps of western Canada, another example being Mount Edziza in far northwestern British Columbia.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
It is skiable over, possibly over down to the Pacific Ocean. The easiest access to Mount Silverthrone is by air travel, starting from the rural community of Tatla Lake, landing on the major part of the Ha-Iltzuk Icefield. Air travels can also be made into logging camps at Owikeno Lake to the west or at the start of Knight Inlet to the southwest, followed by long hiking and skiing methods.

Geographic entities mentioned:
surface_form: Tatla Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.9667
lon: -124.417
surface_form: mount silverthrone
instance_of: Mountain
countries: Canada
coordinates: lat: 51.51777777777778
lon: -126.11333333333333
surface_form: tatla lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.9667
lon: -124.417
It is skiable over, possibly over down to the Pacific Ocean. The easiest access to Mount Silverthrone is by air travel, starting from the rural community of Tatla Lake, landing on the major part of the Ha-Iltzuk Icefield. Air travels can also be made into logging camps at Owikeno Lake to the west or at the start of Knight Inlet to the southwest, followed by long hiking and skiing methods.

Geographic entities mentioned:
surface_form: Owikeno Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.683333333333
lon: -126.91666666667
surface_form: owikeno lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.683333333333
lon: -126.91666666667
It lies within the Coast Plutonic Complex, which is the single largest contiguous granite outcropping in the world. The plutonic and metamorphic rocks extend approximately 1,800 kilometers on the coast of British Columbia, southwestern Yukon and southeastern Alaska. In addition, Garibaldi, Meager, Cayley and Silverthrone areas are of recent volcanic origin.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
The volcanic terrain in the Silverthrone area is very similar to the Mount Meager massif further south. However, there is much more ice. Mount Silverthrone is among the heavily glaciated peaks in southwestern British Columbia. It has a topographic prominence of approximately, greater than any other volcano in southwestern British Columbia.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount silverthrone
instance_of: Mountain
countries: Canada
coordinates: lat: 51.51777777777778
lon: -126.11333333333333
The volcanic terrain in the Silverthrone area is very similar to the Mount Meager massif further south. However, there is much more ice. Mount Silverthrone is among the heavily glaciated peaks in southwestern British Columbia. It has a topographic prominence of approximately, greater than any other volcano in southwestern British Columbia.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
It has a topographic prominence of approximately, greater than any other volcano in southwestern British Columbia. The extensive icefields around Mount Silverthrone are receding and are small compared to their former extent, but they are an impressive indication of how much of British Columbia looked 10,000 years or more ago.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount silverthrone
instance_of: Mountain
countries: Canada
coordinates: lat: 51.51777777777778
lon: -126.11333333333333
Mount Silverthrone. Mount Silverthrone, officially named Silverthrone Mountain, is a mountain in the Pacific Ranges of the Coast Mountains of British Columbia, Canada, located over northwest of the city of Vancouver and about west of Mount Waddington, British Columbia, Canada.

Geographic entities mentioned:
surface_form: mount silverthrone
instance_of: Mountain
countries: Canada
coordinates: lat: 51.51777777777778
lon: -126.11333333333333
Skiing and recreation. The first mountaineering visit at Mount Silverthrone was in 1936 by the famous pioneering climbing couple Don and Phyllis Munday, accompanied by Henry Hall, by walking up the Klinaklini Glacier from the head of Knight Inlet. Because Silverthrone is heavily glaciated, Don Munday called the mountain &quot;home of the snows&quot;.

Geographic entities mentioned:
surface_form: mount silverthrone
instance_of: Mountain
countries: Canada
coordinates: lat: 51.51777777777778
lon: -126.11333333333333
Because Silverthrone is heavily glaciated, Don Munday called the mountain &quot;home of the snows&quot;. Skiing on Mount Silverthrone includes skiing on the largest ice field in the southern Coast Mountains, the Ha-Iltzuk Icefield. It is skiable over, possibly over down to the Pacific Ocean.

Geographic entities mentioned:
surface_form: mount silverthrone
instance_of: Mountain
countries: Canada
coordinates: lat: 51.51777777777778
lon: -126.11333333333333
The plutonic and metamorphic rocks extend approximately 1,800 kilometers on the coast of British Columbia, southwestern Yukon and southeastern Alaska. In addition, Garibaldi, Meager, Cayley and Silverthrone areas are of recent volcanic origin. The volcanic terrain in the Silverthrone area is very similar to the Mount Meager massif further south. However, there is much more ice.

Geographic entities mentioned:
surface_form: mount meager
instance_of: Mountain
countries: Canada
coordinates: lat: 50.63166667
lon: -123.50416667
Skiing and recreation. The first mountaineering visit at Mount Silverthrone was in 1936 by the famous pioneering climbing couple Don and Phyllis Munday, accompanied by Henry Hall, by walking up the Klinaklini Glacier from the head of Knight Inlet. Because Silverthrone is heavily glaciated, Don Munday called the mountain &quot;home of the snows&quot;.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
He was given command of, a British ship that had been captured on the Mississippi River, in 1779, but she was destroyed by a hurricane. He was then given another ship, also called, by Bernardo de Gálvez, the governor of Spanish Louisiana, to deal with British military shipping on Lake Pontchartrain. In September 1779 he captured a British ship.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
This process may have been the first use of so-called pyrotechnology by early mankind. In South Africa at Pinnacle Point researchers have determined that two types of silcrete tools were developed between 60,000 and 80,000 years ago and used the heat treatment technique. There is evidence to suggest the technique may have been known as early as 164,000 years ago.

Geographic entities mentioned:
surface_form: Pinnacle Point
instance_of: Mountain
countries: South Africa
coordinates: lat: -34.207863
lon: 22.089515
The peoples of the African Middle Stone Age (MSA) showed a preference for silcrete tools, sourcing the material from up to 200 km to use in place of more accessible quartz and quartzite. MSA quarries have recently been found in Botswana south of the Okavango Delta. Evidence was found that raw silcrete blanks and blocks were transported prior to heat treating during the MSA.

Geographic entities mentioned:
surface_form: Okavango
instance_of: Body of water
Watercourse
countries: Botswana
coordinates: lat: -19.4
lon: 22.9
Description. Bald Knob's elevation— only lower than the highest point in the Alleghenies, Spruce Knob)—gives it a unique hemiboreal ecosystem. While the lower and middle elevations of the mountain are populated by oak, hickory, birch, beech and maple, the summit dome was historically dominated by red spruce.

Geographic entities mentioned:
surface_form: Spruce Knob
instance_of: Mountain
countries: United States
coordinates: lat: 38.6999
lon: -79.5328
To the east of the main enclosure on a high terrace overlooking the site was a large W-shaped earthwork. This was once thought to be a snake effigy mound similar to the Great Serpent Mound in Adams County, Ohio; although archaeologists do not currently think this was the case. Timber circle.

Geographic entities mentioned:
surface_form: Serpent Mound
instance_of: Mountain
countries: United States
coordinates: lat: 39.025858
lon: -83.430444
Irvine. Irvine is a suburban Chinatown in Orange County that is growing as more Chinese people move into the San Gabriel Valley. Many Chinese business establishments are situated in the El Camino Real and Walnut neighborhoods. Cerritos. Cerritos is a majority Asian city located on the border of Orange County and Los Angeles County.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
In March 1801 Hunt set off on an Aegean voyage with Carlyle, looking further afield. A second visit to the Troad saw Hunt remove an inscription; Carlyle and Hunt also fell in with Edward Daniel Clarke there, but a scholarly disagreement over the site of Troy turned into something of a vendetta on Clarke's part. They also visited Mount Athos.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Lac Deschênes. Lac Deschênes () is a lake on the Ottawa River that runs from the Chats Falls Dam near Fitzroy Harbour in the west to the Deschênes Rapids at Britannia in the east. It is a little over wide at its widest point and little more than a few hundred metres at its narrowest.

Geographic entities mentioned:
surface_form: lac deschênes
instance_of: Lake
countries: Canada
coordinates: lat: 45.383333333333
lon: -75.866666666667
As the Francophone population of the area increased, it became more commonly known as lac-Deschênes. It is now officially known by the French name only. Boating and sailing. Lac Deschênes is used for recreational boating and sailing. It is home to five sailing clubs and one commercial marina. Britannia Yacht Club is the oldest, established in 1887.

Geographic entities mentioned:
surface_form: lac deschênes
instance_of: Lake
countries: Canada
coordinates: lat: 45.383333333333
lon: -75.866666666667
It is located in Dick Bell Park on Carling Avenue in the former City of Nepean. The Lac Deschênes Sailing Club and the Kanata Sailing Club are the two smaller clubs consisting primarily of dinghy fleets. On the Quebec side of the lake is the Club de Voile Grande-Rivière located at the Aylmer Marina. Further upstream on the Ontario side is the Port of Call Marina.

Geographic entities mentioned:
surface_form: lac deschênes
instance_of: Lake
countries: Canada
coordinates: lat: 45.383333333333
lon: -75.866666666667
A small public dock exists at Pinhey's Point while the village of Quyon maintains much larger public dock facilities near the western end of the lake. Access between Ontario and Quebec across Lac Deschênes is provided by a ferry service between West Carleton and Quyon. Although a bridge has been proposed, it has not yet received approval.

Geographic entities mentioned:
surface_form: lac deschênes
instance_of: Lake
countries: Canada
coordinates: lat: 45.383333333333
lon: -75.866666666667
Although a bridge has been proposed, it has not yet received approval. Canadian Hydrographic Service Chart 1550 - Britannia Bay to Chats Falls covers the whole of Lac Deschênes. The Canadian Coast Guard maintains lights and buoys on the lake, however local emergency services in Ottawa and Gatineau are responsible for providing search and rescue services within their respective city boundaries.

Geographic entities mentioned:
surface_form: lac deschênes
instance_of: Lake
countries: Canada
coordinates: lat: 45.383333333333
lon: -75.866666666667
Chart datum is 57.9 metres above sea level. Current water levels can be found on the Ottawa River Levels website. Water levels fluctuate on Lac Deschênes approximately 0.9 m annually, with the high on average of
58.8 m occurring during the spring freshet and the low on average of 57.9 m occurring during September. Water levels are affected strictly by the flows being passed from upstream.

Geographic entities mentioned:
surface_form: lac deschênes
instance_of: Lake
countries: Canada
coordinates: lat: 45.383333333333
lon: -75.866666666667
Water levels are affected strictly by the flows being passed from upstream. Waters are slow flowing except immediately below the dam at Chats Falls and again at Britannia Rapids. Although much of Lac Deschênes is relatively shallow, generally less than 9.0 m, there is a deep trough between Twelve Mile Island and Aylmer Island that reaches depths of 49 m. Fishing.

Geographic entities mentioned:
surface_form: lac deschênes
instance_of: Lake
countries: Canada
coordinates: lat: 45.383333333333
lon: -75.866666666667
Although much of Lac Deschênes is relatively shallow, generally less than 9.0 m, there is a deep trough between Twelve Mile Island and Aylmer Island that reaches depths of 49 m. Fishing. Numerous species of sport fish can be found in Lac Deschênes including black crappie, pickerel (walleye), muskie, and pike. Catfish abound in many of the bays. Birds.

Geographic entities mentioned:
surface_form: lac deschênes
instance_of: Lake
countries: Canada
coordinates: lat: 45.383333333333
lon: -75.866666666667
He competed in the men's downhill at the 1952 Winter Olympics. Benavidez first began skiing after he and his brother, Emilio, saw a poster advertising a skiing competition at Cerro Otto. Although the two initially registered because of the promise of cake and chocolate at the finish line, Benavidez ultimately won the competition and was awarded a pair of skis.

Geographic entities mentioned:
surface_form: Cerro Otto
instance_of: Mountain
countries: Argentina
coordinates: lat: -41.1448
lon: -71.3758
Although the two initially registered because of the promise of cake and chocolate at the finish line, Benavidez ultimately won the competition and was awarded a pair of skis. After training at Cerro Otto, he later left to work as an instructor at Cerro Catedral. He was additionally an avid mountaineer, being apart of Club Andino Bariloche for over 70 years.

Geographic entities mentioned:
surface_form: Cerro Catedral
instance_of: Mountain
countries: Argentina
coordinates: lat: -41.183333333333
lon: -71.45
The largest cold desert is the Great Basin Desert, which encompasses much of the northern Basin and Range Province, north of the Mojave Desert. Other cold deserts lie within the Columbia Plateau/Columbia Basin, the Snake River Plain, and the Colorado Plateau regions. Western arid regions of North America.

Geographic entities mentioned:
surface_form: Columbia Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 45.999444444444
lon: -119.00138888889
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
This large arid region of includes: deserts, such as the Great Basin Desert and Sonoran Desert; and the non-desert arid region areas (with greater than annual precipitation) in the Great Basin arid region, Colorado Plateau, Mexican Plateau, and others.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
surface_form: Mexican Plateau
instance_of: Plateau
countries: Mexico
coordinates: lat: 24
lon: -103
Sakurab resembles a scallion having bulb at its base, a white stalk, and a fan of slender green leaves as well as an intense aroma and flavor reminiscent of shallots. It grows natively in the Lanao provinces of Mindanao in the Philippines, mostly commonly in cities and towns around Lake Lanao, and is sold by Maranao merchants in areas where it is desired but not commonly grown. Cuisine.

Geographic entities mentioned:
surface_form: Lake Lanao
instance_of: Lake
countries: Philippines
coordinates: lat: 7.88
lon: 124.2525
She did not publish the find until 1926. Ekman travelled to a number of places on to pursue her studies, including the island of Mäkisalo in Ladoga in 1914, the Austrian Alps in 1921, Greenland in 1923 and Ben Lawers in Scotland in 1930. She became a prominent researcher despite having no real academic background education or degree.

Geographic entities mentioned:
surface_form: Ben Lawers
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.544922
lon: -4.22086
King George burned the city of Oltisi to prevent it falling to the enemy and retreated to Kola. A bloody battle was fought near the village Shirimni at Lake Palakazio on 11 September; the emperor won a costly victory, forcing George I to retreat northwards into his kingdom. Basil plundered the country and withdrew for winter to Trebizond. Several attempts to negotiate the conflict failed.

Geographic entities mentioned:
surface_form: Lake Palakazio
instance_of: Lake
countries: Turkey
coordinates: lat: 41.0446
lon: 43.2556
HaMasrek Reserve is renowned and named for its prominent stand of Jerusalem pine trees, which are approximately 170 years old. It features several scenic viewpoints which offer panoramic views encompassing the coastal plain stretching from Netanya to Ashkelon, the Ayalon Valley, and the historic Burma Road.

Geographic entities mentioned:
surface_form: Ayalon Valley
instance_of: Valley
countries: Israel
coordinates: lat: 31.8675
lon: 34.959444444444
Abairegi. Abairegi (also Abhairege; Bairege) is one of the Kurya clans in the eastern part of Lake Nyanza (Victoria) in East Africa. They are east of the other Kurya in the Mara region of Tanzania and in Kenya west of the Nyanza Region.

Geographic entities mentioned:
surface_form: Lake Nyanza
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Japanese cruiser Haguro. &quot;Haguro&quot; (羽黒) was a heavy cruiser of the Imperial Japanese Navy, named after Mount Haguro in Yamagata Prefecture. Commissioned in 1929, &quot;Haguro&quot; saw significant service during World War II, participating in nine naval engagements between 1942 and 1945.

Geographic entities mentioned:
surface_form: Mount Haguro
instance_of: Mountain
countries: Japan
coordinates: lat: 38.7008
lon: 139.9825
Muisca mummification. The Muisca inhabited the Altiplano Cundiboyacense in the Colombian Andes before the arrival of the Spanish and were an advanced civilisation. They mummified the higher social class members of their society, mainly the &quot;zipas&quot;, &quot;zaques&quot;, &quot;caciques&quot;, priests and their families.

Geographic entities mentioned:
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877
In the 20th and 21st century Eliécer Silva Celis and Abel Fernando Martínez Martín have been analysing various Muisca mummies. Background. In the centuries before the Spanish conquest of the Muisca in 1537, the Altiplano Cundiboyacense, high plateau of the Eastern Ranges of the Colombian Andes, was inhabited by the Muisca people. They were an advanced civilisation of mainly farmers and traders.

Geographic entities mentioned:
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877
East-Central Kansas. East-Central Kansas is a region of Kansas. It is located between the Kansas City metropolitan area and Southeast Kansas, and on the border with Missouri. The region extends westward towards the Flint Hills to Lyon County. East-Central Kansas geographically features rolling hills and deep forested river valleys. The main crop of this predominantly agricultural region is corn.

Geographic entities mentioned:
surface_form: Flint Hills
instance_of: Landform
countries: United States
coordinates: lat: 37.2833
lon: -96.6753
Early graziers used the high country wilderness above Adaminaby as summer pastureland. The area was set aside as a National Chase in 1906 and later became the Kosciuszko National Park. Today the area is renowned for its historic huts and access to unique wilderness areas, including the Mount Jagungal Wilderness Area. Relocation of the original township.

Geographic entities mentioned:
surface_form: Mount Jagungal
instance_of: Mountain
countries: Australia
coordinates: lat: -36.13166666666667
lon: 148.3844444
It was photographed from the air by the U.S. Navy in 1967 and was surveyed by the British Antarctic Survey in the period 1968–71. In association with the names of geologists grouped in this area, it was named by the UK Antarctic Place-Names Committee in 1971 after Professor Arthur Holmes, after whom the Holmes Hills in Palmer Land were also named.

Geographic entities mentioned:
surface_form: arthur
instance_of: Mountain
coordinates: lat: -67.65
lon: 49.86667
surface_form: holmes
instance_of: Mountain
coordinates: lat: -66.78333333
lon: -64.26666667
surface_form: holmes
instance_of: Mountain
coordinates: lat: -66.78333333
lon: -64.26666667
Holmes Summit. Holmes Summit is a peak rising to, the highest elevation in the Read Mountains of the Shackleton Range in Antarctica. It was photographed from the air by the U.S. Navy in 1967 and was surveyed by the British Antarctic Survey in the period 1968–71.

Geographic entities mentioned:
surface_form: holmes
instance_of: Mountain
coordinates: lat: -66.78333333
lon: -64.26666667
surface_form: holmes summit
instance_of: Mountain
coordinates: lat: -80.6667
lon: -24.6667
Holmes Summit. Holmes Summit is a peak rising to, the highest elevation in the Read Mountains of the Shackleton Range in Antarctica. It was photographed from the air by the U.S. Navy in 1967 and was surveyed by the British Antarctic Survey in the period 1968–71.

Geographic entities mentioned:
surface_form: holmes
instance_of: Mountain
coordinates: lat: -66.78333333
lon: -64.26666667
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
surface_form: holmes summit
instance_of: Mountain
coordinates: lat: -80.6667
lon: -24.6667
Today, Baratuciat is found almost exclusively in the province of Turin, particularly in the Susa Valley, where it is found in the villages of Almese, Buttigliera Alta, Rosta, Rubiana and Villar Dora. History.

Geographic entities mentioned:
surface_form: Susa Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.133333333333
lon: 7.05
It is soft (not higher than 2.5 on the Mohs scale) and water-soluble. Optical properties are variable; the purest form is transparent and colorless, but opaque gray or yellow deposits are also known. It occurs in fumaroles, as at Mount Vesuvius and associated with coal seam fires. It was named for Italian anatomist Paolo Mascagni (1752–1815) who first described the mineral.

Geographic entities mentioned:
surface_form: Mount Vesuvius
instance_of: Mountain
countries: Italy
coordinates: lat: 40.821388888889
lon: 14.425555555556
Mount Longdon. Mount Longdon is a hill located in the east of East Falkland island forming part of the Falkland Islands Archipelago. It has an elevation of 186 metres (610 ft) above sea level. It is the highest land in any direction for 2 kilometres (1.2 miles). It is known as the site of the Battle of Mount Longdon, and overlooks Stanley, the capital of the Falkland Islands. Geography.

Geographic entities mentioned:
surface_form: mount longdon
instance_of: Mountain
countries: Falkland Islands
coordinates: lat: -51.666666666667
lon: -57.966666666667
It has an elevation of 186 metres (610 ft) above sea level. It is the highest land in any direction for 2 kilometres (1.2 miles). It is known as the site of the Battle of Mount Longdon, and overlooks Stanley, the capital of the Falkland Islands. Geography. Mount Longdon forms part of a hilly area in the East of the East Falkland Island. Geology.

Geographic entities mentioned:
surface_form: mount longdon
instance_of: Mountain
countries: Falkland Islands
coordinates: lat: -51.666666666667
lon: -57.966666666667
It is known as the site of the Battle of Mount Longdon, and overlooks Stanley, the capital of the Falkland Islands. Geography. Mount Longdon forms part of a hilly area in the East of the East Falkland Island. Geology. Mount Longdon and the surrounding area primarily consists of sedimentary rocks with formations of sandstones, quartzites, and shales, which date back to the Paleozoic era. Climate.

Geographic entities mentioned:
surface_form: mount longdon
instance_of: Mountain
countries: Falkland Islands
coordinates: lat: -51.666666666667
lon: -57.966666666667
Geography. Mount Longdon forms part of a hilly area in the East of the East Falkland Island. Geology. Mount Longdon and the surrounding area primarily consists of sedimentary rocks with formations of sandstones, quartzites, and shales, which date back to the Paleozoic era. Climate. The Climate for Mount Longdon is extremely similar to Stanley and RAF Mount Pleasant due to its proximity.

Geographic entities mentioned:
surface_form: mount longdon
instance_of: Mountain
countries: Falkland Islands
coordinates: lat: -51.666666666667
lon: -57.966666666667
Geology. Mount Longdon and the surrounding area primarily consists of sedimentary rocks with formations of sandstones, quartzites, and shales, which date back to the Paleozoic era. Climate. The Climate for Mount Longdon is extremely similar to Stanley and RAF Mount Pleasant due to its proximity. Mount Longdon has a maritime climate in the polar, tundra zones, Köppen classification &quot;ET&quot;.

Geographic entities mentioned:
surface_form: mount longdon
instance_of: Mountain
countries: Falkland Islands
coordinates: lat: -51.666666666667
lon: -57.966666666667
Climate. The Climate for Mount Longdon is extremely similar to Stanley and RAF Mount Pleasant due to its proximity. Mount Longdon has a maritime climate in the polar, tundra zones, Köppen classification &quot;ET&quot;. The climate is very much influenced by the cool South Atlantic ocean and its northerly Patagonian current.

Geographic entities mentioned:
surface_form: mount longdon
instance_of: Mountain
countries: Falkland Islands
coordinates: lat: -51.666666666667
lon: -57.966666666667