Sarmila/GeoWiki-Features huggingface dataset:
Mount Septimus. Mount Septimus is the western summit of a jagged mountain on Vancouver Island, British Columbia, Canada, located southeast of Gold River and south of Buttle Lake. It contains a huge glacier on the north flank. The highest peak on the massif is Mount Rosseau, located to the west. History.

Geographic entities mentioned:
surface_form: Mount Rosseau
instance_of: Mountain
countries: Canada
coordinates: lat: 49.4789
lon: -125.506
It contains a huge glacier on the north flank. The highest peak on the massif is Mount Rosseau, located to the west. History. &quot;By some, thought to be descriptive – Septimus being a mountain of seven peaks.&quot; (List of Place Names in Strathcona Park, compiled by Allan C.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Beaver.&quot; [note that this assumption is likely made because of the mountain's proximity to Price Creek and a mistaken assumption that Price Creek was named for Capt John Price, HMS Scout, under whom Septimus Evans was surgeon before joining the hired vessel Beaver under Captain Pender, 1868.]
Source: Canadian Geographical Names Database, Ottawa
Access.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Septimus. Mount Septimus is the western summit of a jagged mountain on Vancouver Island, British Columbia, Canada, located southeast of Gold River and south of Buttle Lake. It contains a huge glacier on the north flank. The highest peak on the massif is Mount Rosseau, located to the west. History.

Geographic entities mentioned:
surface_form: mount septimus
instance_of: Mountain
countries: Canada
coordinates: lat: 49.4806
lon: -125.514
Note: From Cream Lake, the south aspect can be accessed by ascending the wide couloir to the shoulder west of Mount Septimus' summit.

Geographic entities mentioned:
surface_form: mount septimus
instance_of: Mountain
countries: Canada
coordinates: lat: 49.4806
lon: -125.514
Zabolotye Lake. Zabolotye lake () is a freshwater lake in the Sergiyev Posad District of Moscow Oblast, Russia. The lake covers 3.2 km², though some sources instead report 1.96 km². The lake's catchment area is 355 km2, and reaches a maximum depth of 5m. One topographic map shows that the lake is predominantly swamp, and omits the name Zabolotye Lake. Geography.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: zabolotye lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 56.6855
lon: 38.0613
Zabolotye Lake. Zabolotye lake () is a freshwater lake in the Sergiyev Posad District of Moscow Oblast, Russia. The lake covers 3.2 km², though some sources instead report 1.96 km². The lake's catchment area is 355 km2, and reaches a maximum depth of 5m. One topographic map shows that the lake is predominantly swamp, and omits the name Zabolotye Lake. Geography.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: zabolotye lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 56.6855
lon: 38.0613
Zabolotye Lake. Zabolotye lake () is a freshwater lake in the Sergiyev Posad District of Moscow Oblast, Russia. The lake covers 3.2 km², though some sources instead report 1.96 km². The lake's catchment area is 355 km2, and reaches a maximum depth of 5m. One topographic map shows that the lake is predominantly swamp, and omits the name Zabolotye Lake. Geography.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The lake covers 3.2 km², though some sources instead report 1.96 km². The lake's catchment area is 355 km2, and reaches a maximum depth of 5m. One topographic map shows that the lake is predominantly swamp, and omits the name Zabolotye Lake. Geography. The lake is located 0.5 km from Zabolotye and 3 km from Verigino. Sulat River. a right tributary of Dubna River flows through the lake.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: zabolotye lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 56.6855
lon: 38.0613
The lake's catchment area is 355 km2, and reaches a maximum depth of 5m. One topographic map shows that the lake is predominantly swamp, and omits the name Zabolotye Lake. Geography. The lake is located 0.5 km from Zabolotye and 3 km from Verigino. Sulat River. a right tributary of Dubna River flows through the lake. The elevation is 127.8 m. History.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
One topographic map shows that the lake is predominantly swamp, and omits the name Zabolotye Lake. Geography. The lake is located 0.5 km from Zabolotye and 3 km from Verigino. Sulat River. a right tributary of Dubna River flows through the lake. The elevation is 127.8 m. History. The lake has a glacial origin, emerging 10,000 years ago.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The elevation is 127.8 m. History. The lake has a glacial origin, emerging 10,000 years ago. For millennia, silt deposits accumulated in the lake, which was once much larger than at present, leaving the Dubninsky and Ol'khovsko-Bat'kovskii boggy massifs, as well as meadows later overgrown with forest. The lake was and is a resting place for Muscovites.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The lake has a glacial origin, emerging 10,000 years ago. For millennia, silt deposits accumulated in the lake, which was once much larger than at present, leaving the Dubninsky and Ol'khovsko-Bat'kovskii boggy massifs, as well as meadows later overgrown with forest. The lake was and is a resting place for Muscovites. One source claims that Vladimir Ilich Lenin came to rest near Zabolotoye Lake.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The lake was and is a resting place for Muscovites. One source claims that Vladimir Ilich Lenin came to rest near Zabolotoye Lake. From the middle of the 20th century until the 1980s, water quality control measures were carried out and various reclamation projects were implemented. In the 1990s, large-scale activities on the lake ceased.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
From the middle of the 20th century until the 1980s, water quality control measures were carried out and various reclamation projects were implemented. In the 1990s, large-scale activities on the lake ceased. In 2011, the lake and its environs came under the state program of flooding of marshes, in connection with which the construction of a dam was planned. Flora and fauna.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
In the 1990s, large-scale activities on the lake ceased. In 2011, the lake and its environs came under the state program of flooding of marshes, in connection with which the construction of a dam was planned. Flora and fauna. The lake is inhabited by crucian, roach, pike, and perch. Until the 1960s, the relic seaweed of kladofora lived in the lake, but was eliminated during reclamation.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Lehigh Valley-area alumni who have appeared at the Civic Theatre of Allentown include Michaela Conlin (Fox's &quot;Bones&quot;), Dane DeHaan (&quot;In Treatment&quot;), Michael McDonald (Broadway revival of &quot;Hair)&quot;, Daniel Roebuck (&quot;The Late Shift&quot;), actress Amanda Seyfried (&quot;Mama Mia&quot;), and actress Christine Taylor (&quot;The Wedding Singer&quot;). Current status.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Sagrado. Sagrado (;;;) is a (municipality) in the Regional decentralization entity of Gorizia in the Italian region of Friuli-Venezia Giulia, located about northwest of Trieste and about southwest of Gorizia, on the left bank of the Isonzo River. Sagrado is nearby the Monte San Michele, the seat of fierce fightings between Italy and Austria-Hungary during World War I. Transport.

Geographic entities mentioned:
surface_form: Monte San Michele
instance_of: Mountain
countries: Italy
coordinates: lat: 45.88
lon: 13.53
Course. It has its sources in Lake Usun-Kyuel and crosses the tundra roughly northeastwards. In its lower course it flows south of Lake Bolshoye Morskoye. Finally it flows into the Kolyma Gulf of the East Siberian Sea west of the mouths of the Kolyma. Owing to its extreme northerly location the Bolshaya Chukochya freezes up in early October and remains icebound until June.

Geographic entities mentioned:
surface_form: Lake Bolshoye Morskoye
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 70.066666666667
lon: 158.73333333333
Whiltilla Mountain. Whiltilla Mountain is a mountain on Vancouver Island, British Columbia, Canada, located east of Nimpkish.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: whiltilla mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.3664
lon: -126.706
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
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
Whiltilla Mountain. Whiltilla Mountain is a mountain on Vancouver Island, British Columbia, Canada, located east of Nimpkish.

Geographic entities mentioned:
surface_form: whiltilla mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.3664
lon: -126.706
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
South of Tecumseh, Missouri, the river becomes Norfork Lake, a reservoir created by Norfork Dam in Baxter County, Arkansas. A few miles below the dam, the North Fork River joins the White River near the town of Norfork, Arkansas. The part of the river below the Norfork Dam is called the Norfork Tailwater and is a trout fishing stream.

Geographic entities mentioned:
surface_form: Norfork Tailwater
instance_of: Lake
countries: United States
coordinates: lat: 36.246238888889
lon: -92.245480555556
Matawawaskweyau River. The Matawawaskweyau River is a tributary of the Pauschikushish Ewiwach River in Regional County Municipality (RCM) of Eeyou Istchee James Bay (municipality), in the administrative region of Nord-du-Québec, Canadian province of Quebec, in Canada.

Geographic entities mentioned:
surface_form: Pauschikushish Ewiwach River
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.736111111111
lon: -77.370555555556
surface_form: matawawaskweyau river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.690277777778
lon: -77.51
Geography. The &quot;Matawawaskweyau River&quot; flows on the north shore of the Pauschikushish Ewiwach River. From there, the current flows to the northeast and flows to the south shore of [Dana Lake (Eeyou Istchee James Bay)] which empties into a bay west of Evans Lake. Toponymy.

Geographic entities mentioned:
surface_form: Pauschikushish Ewiwach River
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.736111111111
lon: -77.370555555556
surface_form: pauschikushish ewiwach river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.736111111111
lon: -77.370555555556
surface_form: matawawaskweyau river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.690277777778
lon: -77.51
Geography. The &quot;Matawawaskweyau River&quot; flows on the north shore of the Pauschikushish Ewiwach River. From there, the current flows to the northeast and flows to the south shore of [Dana Lake (Eeyou Istchee James Bay)] which empties into a bay west of Evans Lake. Toponymy.

Geographic entities mentioned:
surface_form: evans lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.8167
lon: -123.167
surface_form: dana lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.8842
lon: -77.3375
The Matawawaskweyau River is a tributary of the Pauschikushish Ewiwach River in Regional County Municipality (RCM) of Eeyou Istchee James Bay (municipality), in the administrative region of Nord-du-Québec, Canadian province of Quebec, in Canada. The Matawawaskweyau River hydrographic slope is served by the Northern Highway from Matagami to west of the source of the Matawawaskweyau River.

Geographic entities mentioned:
surface_form: matagami
instance_of: Lake
countries: Canada
coordinates: lat: 49.8667
lon: -77.4464
surface_form: matawawaskweyau river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.690277777778
lon: -77.51
surface_form: matawawaskweyau river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.690277777778
lon: -77.51
Matawawaskweyau River. The Matawawaskweyau River is a tributary of the Pauschikushish Ewiwach River in Regional County Municipality (RCM) of Eeyou Istchee James Bay (municipality), in the administrative region of Nord-du-Québec, Canadian province of Quebec, in Canada.

Geographic entities mentioned:
surface_form: matawawaskweyau river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.690277777778
lon: -77.51
Toponymy. Of Cree origin, the toponym &quot;Matawawaskweyau River&quot; means: &quot;the river where we find rocks of many forms&quot;. The toponym &quot;rivière Matawawaskweyau&quot; was formalized on April 7, 1983 at the Commission de toponymie du Québec

Geographic entities mentioned:
surface_form: matawawaskweyau river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.690277777778
lon: -77.51
It was held on 28 November 2015 at Arena of Stars in Genting Highlands, Pahang, Malaysia, and was broadcast live through Malaysia's Astro Wah Lai Toi and Hong Kong's TVB Entertainment news channel. The awards ceremony was officially announced on 13 October 2015, and presented 13 nomination categories. Nominees were announced on 16 October through a mobile app for Android.

Geographic entities mentioned:
surface_form: Genting Highlands
instance_of: Mountain
countries: Malaysia
coordinates: lat: 3.42368
lon: 101.79335
It is a part of the municipality of Tynaarlo, and lies about 15 km southeast of Groningen. History. The village was first mentioned in 1285 as Growe, and means &quot;dug canal&quot; which refers to the Oostermoersche Vaart which is connected to the Zuidlaardermeer. The canal was dug by the monks of the Aduard Abbey to transport peat. The village used to be known as Midlaarderveen as well.

Geographic entities mentioned:
surface_form: Zuidlaardermeer
instance_of: Lake
countries: Netherlands
coordinates: lat: 53.120556
lon: 6.695556
Royal Menagerie of Versailles. The Ménagerie royale de Versailles (literal French for &quot;Royal Menagerie of Versailles&quot;) was Louis XIV's first major project at Versailles. It was built even before the creation of the Grand Canal. Its construction was entrusted to the architect Louis Le Vau, who began work in 1663.

Geographic entities mentioned:
surface_form: Grand Canal.
instance_of: Lake
countries: France
coordinates: lat: 48.81
lon: 2.10011
Under Louis XIV. Its construction was entrusted to the architect Louis Le Vau, who began work in 1663. The menagerie was built between 1662 and 1664, at the southern end of the future Grand Canal, along the road between Versailles and Saint-Cyr, but was not fully completed until 1668. It is centred around an octagonal building covered by a slate dome.

Geographic entities mentioned:
surface_form: Grand Canal
instance_of: Lake
countries: France
coordinates: lat: 48.81
lon: 2.10011
Alexander and Rebecca had two children, Manuela Fuller and Gabriel (Gabbi) Ezer, 6 grandchildren and 14 great-grandchildren. In 1973, Alexander died after a long battle with cancer. Alexander and Rebecca are buried in Israel's Har HaMenuchot Cemetery in Givat Shaul, Jerusalem. Promoting Industry. Alexander developed a vision of making Israel an industrial powerhouse.

Geographic entities mentioned:
surface_form: Har HaMenuchot
instance_of: Mountain
countries: Israel
coordinates: lat: 31.798133333333
lon: 35.177727777778
The population of Ridgecrest Heights was 380 in the 2020 census. Geography. Ridgecrest Heights is located 2.34 mi (3.76 km) southwest of Ridgecrest, California in the Indian Wells Valley at an elevation of 2,428 ft (740 m). Demographics. Ridgecrest Heights first appeared as a census designated place in the 2020 U.S. Census.

Geographic entities mentioned:
surface_form: Indian Wells Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.702777777778
lon: -117.68638888889
Here he joined Percy Bysshe and Mary Shelley, with his secretary John William Polidori on the shores of Lake Geneva, during the &quot;Year Without a Summer&quot;. Polidori's &quot;The Vampyre&quot; was published in 1819, creating the literary vampire genre. This short story was inspired by the life of Lord Byron and his poem &quot;The Giaour&quot; (1813).

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Birken, British Columbia. Birken is an unincorporated community on the north shore of Gates Lake in the Squamish-Lillooet region of southwestern British Columbia. On Pemberton Portage Road, the locality is by road about north of Vancouver and northeast of Whistler. Name origin. The Birkenhead River and the former name of the lake gave the community name. Trails and roads.

Geographic entities mentioned:
surface_form: Gates Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.4772
lon: -122.62618
Name origin. The Birkenhead River and the former name of the lake gave the community name. Trails and roads. The Pemberton Portage was that part of the Douglas Road between Lillooet Lake and Anderson Lake during the Fraser Canyon Gold Rush. By late 1858, this rough trail was completed. About midway on this section, Peter Dickenson built Halfway House in 1859.

Geographic entities mentioned:
surface_form: Lillooet Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.25
lon: -122.5
HTV Basket. Hyères-Toulon Var Basket, also referred to as simply Hyères-Toulon or HTV, is a basketball club based in Hyères and Toulon, France. Created by the merger of Omni Sport Hyerois and Club Sportif Toulonnais, the club shares its home games between the Espace 3000 in Hyères and the Palais des Sports in Toulon.

Geographic entities mentioned:
surface_form: Hyères
instance_of: Mountain
countries: France
coordinates: lat: 43.118888888889
lon: 6.1286111111111
Suusamyr Too. Suusamyr Too () is a mountain range in internal Tian Shan in Kyrgyzstan. It separates Suusamyr Valley and Toluk Saragat Valley. The length of the range is 126 km, and height up to 4048m. It is composed of granite, and schist of lower Paleozoic.

Geographic entities mentioned:
surface_form: Suusamyr Valley
instance_of: Valley
countries: Kyrgyzstan
coordinates: lat: 42.1941
lon: 73.5612
surface_form: suusamyr
instance_of: Mountain
countries: Kyrgyzstan
coordinates: lat: 42.13
lon: 73.25
Suusamyr Too. Suusamyr Too () is a mountain range in internal Tian Shan in Kyrgyzstan. It separates Suusamyr Valley and Toluk Saragat Valley. The length of the range is 126 km, and height up to 4048m. It is composed of granite, and schist of lower Paleozoic.

Geographic entities mentioned:
surface_form: suusamyr
instance_of: Mountain
countries: Kyrgyzstan
coordinates: lat: 42.13
lon: 73.25
The shire covered an area of, and existed from 1878 until 1994. History. Narracan was first incorporated as a shire on 20 September 1878. Due in part to its location at the crossroads of the Latrobe Valley region, many changes occurred to its boundaries, especially from the 1940s onwards, during the post-war industrial boom in the region.

Geographic entities mentioned:
surface_form: Latrobe Valley
instance_of: Valley
countries: Australia
coordinates: lat: -38.1806
lon: 146.278
Doris Lake is west-southwest of Blow Lake and Elk Lake in the Deschutes National Forest. Other nearby lakes include Senoj and Leech. Doris Lake lies slightly east of the Lane County border and the Mink Lake Basin. The lake is up to deep in a small basin carved by Pleistocene glaciers. No perennial streams enter or leave the lake, which is thought to gain and lose water through seepage. Recreation.

Geographic entities mentioned:
surface_form: mink lake
instance_of: Lake
countries: United States
coordinates: lat: 43.8106
lon: -110.846
surface_form: mink lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9303
lon: -121.924
surface_form: doris lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9508
lon: -121.842
Doris Lake. Doris Lake is a natural body of water in the Three Sisters Wilderness of the central Cascade Range in the U.S. state of Oregon. At above sea level, the lake is part of a volcanic landscape southwest of Bend and about by trail west of the Cascade Lakes Scenic Byway. Doris Lake is west-southwest of Blow Lake and Elk Lake in the Deschutes National Forest.

Geographic entities mentioned:
surface_form: three sisters
instance_of: Mountain
countries: United States
coordinates: lat: 34.5968
lon: -83.9444
surface_form: three sisters
instance_of: Landform
countries: United States
coordinates: lat: 41.7446
lon: -121.473
surface_form: doris lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9508
lon: -121.842
surface_form: three sisters
instance_of: Mountain
countries: United States
coordinates: lat: 33.8697
lon: -117.359
state of Oregon. At above sea level, the lake is part of a volcanic landscape southwest of Bend and about by trail west of the Cascade Lakes Scenic Byway. Doris Lake is west-southwest of Blow Lake and Elk Lake in the Deschutes National Forest. Other nearby lakes include Senoj and Leech. Doris Lake lies slightly east of the Lane County border and the Mink Lake Basin.

Geographic entities mentioned:
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9742
lon: -121.802
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 44.025277777778
lon: -115.07138888889
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 45.919166666667
lon: -95.521944444444
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 45.867222222222
lon: -95.804722222222
surface_form: doris lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9508
lon: -121.842
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 44.85
lon: -85.3833
Doris Lake. Doris Lake is a natural body of water in the Three Sisters Wilderness of the central Cascade Range in the U.S. state of Oregon. At above sea level, the lake is part of a volcanic landscape southwest of Bend and about by trail west of the Cascade Lakes Scenic Byway. Doris Lake is west-southwest of Blow Lake and Elk Lake in the Deschutes National Forest.

Geographic entities mentioned:
surface_form: doris lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9508
lon: -121.842
No perennial streams enter or leave the lake, which is thought to gain and lose water through seepage. Recreation. The Six Lakes Trail, which runs by Doris Lake, connects the scenic byway to the east with the Pacific Crest Trail to the west. The trail offers opportunities for day hikes, backpacking, and horse riding. Brook trout, stocked annually in the lake, grow to here.

Geographic entities mentioned:
surface_form: doris lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9508
lon: -121.842
Both tops have small cairns set on grass. Gray Crag is located in the far eastern sector of the national park, five kilometres south east of the village of Patterdale, and is basically the narrow grassy northern ridge of the adjoining fell of Thornthwaite Crag.

Geographic entities mentioned:
surface_form: Thornthwaite Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.48305
lon: -2.8782
surface_form: gray crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4974
lon: -2.88622
Gray Crag is located in the far eastern sector of the national park, five kilometres south east of the village of Patterdale, and is basically the narrow grassy northern ridge of the adjoining fell of Thornthwaite Crag. It is characterised by very steep flanks with crags and gullies which fall away towards Hayeswater on the eastern side and Pasture Beck to the west.

Geographic entities mentioned:
surface_form: Hayeswater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.501388888889
lon: -2.88
It is characterised by very steep flanks with crags and gullies which fall away towards Hayeswater on the eastern side and Pasture Beck to the west. This fell should not be confused with Grey Crag, another Lakeland Fell located also in the far eastern sector above Longsleddale. Ascents.

Geographic entities mentioned:
surface_form: Grey Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.457680555556
lon: -2.7773888888889
An alternative from the same starting point is to follow Pasture Beck up to the head of the valley at Threshthwaite Mouth and then contour round onto Gray Crag. Alfred Wainwright gave this as his preferred route. Most walkers will continue their walk along the ridge south to Thornthwaite Crag which is away and return to Hartsop over Caudale Moor and Hartsop Dodd. View.

Geographic entities mentioned:
surface_form: Hartsop Dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4981
lon: -2.9094
surface_form: caudale moor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.481980555556
lon: -2.9013305555556
surface_form: thornthwaite crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.48305
lon: -2.8782
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
Alfred Wainwright gave this as his preferred route. Most walkers will continue their walk along the ridge south to Thornthwaite Crag which is away and return to Hartsop over Caudale Moor and Hartsop Dodd. View. The view from the top gives a good aspect of the Helvellyn range, with other views obtained by walking to the edges of the ridge and looking down into the valleys on either side.

Geographic entities mentioned:
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
Gray Crag. Gray Crag is a fell in the Lake District in Cumbria, England. Topography. The fell reaches a height of at the northern end of its summit ridge and this is the accepted highest point which gives the best views, although there is a spot height of less than a kilometre to the south. Both tops have small cairns set on grass.

Geographic entities mentioned:
surface_form: gray crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4974
lon: -2.88622
Gray Crag. Gray Crag is a fell in the Lake District in Cumbria, England. Topography. The fell reaches a height of at the northern end of its summit ridge and this is the accepted highest point which gives the best views, although there is a spot height of less than a kilometre to the south. Both tops have small cairns set on grass.

Geographic entities mentioned:
surface_form: gray crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4974
lon: -2.88622
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Ascents. Gray Crag is almost invariably ascended from the hamlet of Hartsop where there is a car park, Hayeswater Gill is followed for until the filter house just below Hayeswater is reached. The steep grassy northern ridge of Gray Crag is then ascended passing a rocky outcrop before reaching the flatter plateau and then the summit.

Geographic entities mentioned:
surface_form: gray crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4974
lon: -2.88622
surface_form: hayeswater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.501388888889
lon: -2.88
surface_form: hayeswater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.501388888889
lon: -2.88
Ascents. Gray Crag is almost invariably ascended from the hamlet of Hartsop where there is a car park, Hayeswater Gill is followed for until the filter house just below Hayeswater is reached. The steep grassy northern ridge of Gray Crag is then ascended passing a rocky outcrop before reaching the flatter plateau and then the summit.

Geographic entities mentioned:
surface_form: gray crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4974
lon: -2.88622
The steep grassy northern ridge of Gray Crag is then ascended passing a rocky outcrop before reaching the flatter plateau and then the summit. An alternative from the same starting point is to follow Pasture Beck up to the head of the valley at Threshthwaite Mouth and then contour round onto Gray Crag. Alfred Wainwright gave this as his preferred route.

Geographic entities mentioned:
surface_form: gray crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4974
lon: -2.88622
Chances Peak in the Soufrière Hills was the highest summit on Montserrat until the mid-1990s, but it has since been eclipsed by various rising and falling volcanic domes during the recent volcanic activity.

Geographic entities mentioned:
surface_form: Chances Peak
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 16.711111111111
lon: -62.177222222222
surface_form: soufrière
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 16.716666666667
lon: -62.183333333333
surface_form: chances
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 16.716666666667
lon: -62.183333333333
There are three main parts of the island: the central zone, subduction and exclusion. Name. Many volcanoes in the Caribbean are named Soufrière (French for 'sulphur outlet'). These include La Soufrière or Soufrière Saint Vincent on the island of Saint Vincent, and La Grande Soufrière on Guadeloupe. 1995–1999 eruption.

Geographic entities mentioned:
surface_form: La Grande Soufrière
instance_of: Mountain
countries: France
coordinates: lat: 16.0438
lon: -61.6634
surface_form: soufrière
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 16.716666666667
lon: -62.183333333333
surface_form: soufrière
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 16.716666666667
lon: -62.183333333333
surface_form: soufrière
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 16.716666666667
lon: -62.183333333333
The first phreatic explosion in this new period of activity occurred on 21 August 1995, and such activity lasted for 18 weeks until it caused an andesitic lava dome formation. This was initially confined by a sector-collapse scar, first identified in the 1930's and called English's Crater.

Geographic entities mentioned:
surface_form: English's Crater
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 16.711111111111
lon: -62.177222222222
Soufrière Hills. The Soufrière Hills () is an active, complex stratovolcano with many lava domes forming its summit on the Caribbean island of Montserrat. After a long period of dormancy, the Soufrière Hills volcano became active in 1995 and continued to erupt through 2010. Its last eruption was in 2013.

Geographic entities mentioned:
surface_form: soufrière hills
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 16.716666666667
lon: -62.183333333333
On 3 April 1996, after pyroclastic flows and mudflows began occurring regularly, southern Montserrat, including the capital, Plymouth, was permanently evacuated. Earthquakes continued to occur in three epicentre zones: beneath the Soufrière Hills volcano, in the ridge running to the northeast, and beneath St George's Hill, about to the northwest.

Geographic entities mentioned:
surface_form: soufrière hills
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 16.716666666667
lon: -62.183333333333
There are three main parts of the island: the central zone, subduction and exclusion. Name. Many volcanoes in the Caribbean are named Soufrière (French for 'sulphur outlet'). These include La Soufrière or Soufrière Saint Vincent on the island of Saint Vincent, and La Grande Soufrière on Guadeloupe. 1995–1999 eruption.

Geographic entities mentioned:
surface_form: soufrière
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 16.716666666667
lon: -62.183333333333
He established the factory Kverneland Fabrikk in 1879 in the village of Kvernaland in Time. The factory was located at Frøyland near the lake of Frøylandsvatnet, and utilized waterfalls from Frøylandsåna. The main products from the factory were scythes, sickles and ploughs.

Geographic entities mentioned:
surface_form: Frøylandsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 58.749722222222
lon: 5.6758333333333
They had outside bar frames, Belpaire fireboxes and Walschaerts valve gear. Service. The locomotives were erected at the Uitenhage workshops and placed in service on the Avontuur Railway between Port Elizabeth and Avontuur in the Langkloof, where they spent most of their working lives. For much of that time they worked out of Loerie, either assisting up the bank or on the Patensie branch.

Geographic entities mentioned:
surface_form: Langkloof
instance_of: Valley
countries: South Africa
coordinates: lat: -33.825
lon: 23.857777777778
Barbodes tumba. &quot;Barbodes tumba&quot; is a species of cyprinid fish endemic to Mindanao, Philippines where it is found in Lake Lanao and associated water systems. This species can reach a length of SL.

Geographic entities mentioned:
surface_form: Lake Lanao
instance_of: Lake
countries: Philippines
coordinates: lat: 7.88
lon: 124.2525
Both are still in operation; the Lowell Observatory in Flagstaff, established in 1894 by Percival Lowell, and the Steward Observatory, built in 1916 by the University of Arizona at Tucson. Since that time, several other observatories have been built and maintained in Arizona. Among these are; the Northern Arizona University and U.S.

Geographic entities mentioned:
surface_form: Kitt Peak
instance_of: Mountain
countries: United States
coordinates: lat: 31.963966666667
lon: -111.59983611111
This fish is endemic to Venezuela. Habitat. Habits mainly in black or acidic waters in Amazonas State of Venezuela (High Orinoco). The type locality is a lagoon near San Fernando de Atabapo in the confluence of the Atabapo and Orinoco rivers in Venezuela. Description. This is a beautiful fish. Body discoid with the anterodorsal profile slightly curved in a &quot;S&quot; shape.

Geographic entities mentioned:
surface_form: Atabapo
instance_of: Watercourse
countries: Venezuela
Colombia
coordinates: lat: 4.04111
lon: -67.70306
In 1808 he was commissioned as a lieutenant in the Danish Army; he took part in the Battle of Sehested (Schleswig-Holstein) during the Napoleonic Wars. After the Denmark-Norway union ended in 1814, Stockfleth joined the Norwegian Army as an officer posted to Valdres. He resigned from the army in 1823 to study theology, graduating in 1824.

Geographic entities mentioned:
surface_form: Valdres
instance_of: Valley
countries: Norway
coordinates: lat: 60.916666666667
lon: 9.1666666666667
Isku (disambiguation). Isku is a mountain in the Andes of Peru.

Geographic entities mentioned:
surface_form: Isku
instance_of: Mountain
countries: Peru
coordinates: lat: -10.61444444
lon: -76.70722222
Early life and education. Todd was born in Hamilton, Ontario, Canada in 1939 and grew up near Hamilton Bay on Lake Ontario. The area near his home included marshes and streams which were being badly damaged by pollution. The writings of Louis Bromfield offered Todd a &quot;marvelous tale of hope&quot; about the possibility of land restoration. Todd earned his B.Sc.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
As of late 2024, the tower was deemed unsafe, according to the state forest's web site (see ref#2). Initially constructed in 1928 on Alander Mountain in Massachusetts, the tower was moved to Washburn Mountain in Columbia County in 1933, and finally to Beebe Hill in 1964. It remained in operation until 1987.

Geographic entities mentioned:
surface_form: Alander Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.088055555556
lon: -73.504444444444
Suez inscriptions of Darius the Great. The Suez inscriptions of Darius the Great were texts written in Old Persian, Elamite, Babylonian and Egyptian on five monuments erected in Wadi Tumilat, commemorating the opening of the &quot;Canal of the Pharaohs&quot; between the Nile and the Bitter Lakes.

Geographic entities mentioned:
surface_form: Bitter Lakes
instance_of: Group of lakes
countries: Egypt
coordinates: lat: 30.268611111111
lon: 32.447222222222
The monument, also known as the &quot;Chalouf stele&quot; (alt. Shaluf Stele), records the construction of a forerunner of the modern Suez Canal by the Persians, a canal through Wadi Tumilat, connecting the easternmost, Bubastite, branch of the Nile with Lake Timsah, which was connected to the Red Sea by natural waterways.

Geographic entities mentioned:
surface_form: Lake Timsah
instance_of: Lake
countries: Egypt
coordinates: lat: 30.577777777778
lon: 32.288888888889
Raven Rocks (rock formation). Raven Rocks is a spur of Blue Ridge Mountain in Jefferson County, West Virginia. The peak is located just north of Jefferson County's border with Clarke County, Virginia and west of its border with Loudoun County, Virginia.

Geographic entities mentioned:
surface_form: Blue Ridge Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.08166667
lon: -77.86222222
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: blue ridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.275833333333
lon: -74.403888888889
surface_form: raven rocks
instance_of: Mountain
countries: United States
coordinates: lat: 39.1401
lon: -77.8347
surface_form: blue ridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.60777778
lon: -76.09305556
Raven Rocks (rock formation). Raven Rocks is a spur of Blue Ridge Mountain in Jefferson County, West Virginia. The peak is located just north of Jefferson County's border with Clarke County, Virginia and west of its border with Loudoun County, Virginia.

Geographic entities mentioned:
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
Raven Rocks is formed by the drainage gorges of Rocky Branch Creek to the north and Raven Rocks Creek to the south (both direct tributaries of the Shenandoah River) on the mountains western watershed. Raven Rocks is the northernmost spur in a series spurs and hollows that occur along the western slope of Blue Ridge Mountain south to Ashby Gap.

Geographic entities mentioned:
surface_form: blue ridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.275833333333
lon: -74.403888888889
surface_form: raven rocks
instance_of: Mountain
countries: United States
coordinates: lat: 39.1401
lon: -77.8347
surface_form: blue ridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.08166667
lon: -77.86222222
surface_form: blue ridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.60777778
lon: -76.09305556
The peak is located just north of Jefferson County's border with Clarke County, Virginia and west of its border with Loudoun County, Virginia. Raven Rocks is formed by the drainage gorges of Rocky Branch Creek to the north and Raven Rocks Creek to the south (both direct tributaries of the Shenandoah River) on the mountains western watershed.

Geographic entities mentioned:
surface_form: shenandoah
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
surface_form: raven rocks
instance_of: Mountain
countries: United States
coordinates: lat: 39.1401
lon: -77.8347
surface_form: raven rocks
instance_of: Mountain
countries: United States
coordinates: lat: 39.1401
lon: -77.8347
surface_form: rocky branch
instance_of: Watercourse
countries: United States
coordinates: lat: 38.601957
lon: -94.144666
Raven Rocks (rock formation). Raven Rocks is a spur of Blue Ridge Mountain in Jefferson County, West Virginia. The peak is located just north of Jefferson County's border with Clarke County, Virginia and west of its border with Loudoun County, Virginia.

Geographic entities mentioned:
surface_form: raven rocks
instance_of: Mountain
countries: United States
coordinates: lat: 39.1401
lon: -77.8347
The first historical mention of the site with this meaning, from 1364, used the phrase &quot;die von Obriede&quot; (&quot;those from the &quot;Ried&quot; area&quot;). Geography. Oberried am Brienzersee is located in the Bernese Oberland at the north shore of Lake Brienz. The highest mountain in the municipality is the Tannhorn ().

Geographic entities mentioned:
surface_form: Lake Brienz
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.716667
lon: 7.95
Geography. Oberried am Brienzersee is located in the Bernese Oberland at the north shore of Lake Brienz. The highest mountain in the municipality is the Tannhorn (). It includes the sections of Dörfli, Mehrendorf and Ebligen on the shore of the lake and then rises into the alps.

Geographic entities mentioned:
surface_form: Tannhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.774833333333
lon: 7.9843888888889
The highest mountain in the municipality is the Tannhorn (). It includes the sections of Dörfli, Mehrendorf and Ebligen on the shore of the lake and then rises into the alps. In addition to the Tannhorn, the Augstmatthorn and Riederengrat as well as peaks around the Riederengrat are part of the municipality. The municipality has an area of.

Geographic entities mentioned:
surface_form: Augstmatthorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.742277777778
lon: 7.9286944444444
Kangerluluk Range. The Kangerluluk Range () is a mountain range in the King Frederick VI Coast, southeastern Greenland. Administratively this range is part of the Kujalleq municipality. This mountain group was named after Kangerluluk, the fjord flanking the range on the southern side. The area of the range is uninhabited. Geography.

Geographic entities mentioned:
surface_form: Kangerluluk
instance_of: Body of water
countries: Greenland
coordinates: lat: 61.1
lon: -43.08333333
The Kangerluluk Mountains are craggy and steep nunataks, relatively little glaciated in the eastern side and progressively rising less and less above the glaciers further inland until being engulfed by the Greenland ice sheet. The range runs roughly from east to west from Cape Olfert Fischer in the Irminger Sea coast, between Kangerluluk fjord in the south and Igutsaat Fjord in the north. Peaks.

Geographic entities mentioned:
surface_form: Kangerluluk
instance_of: Body of water
countries: Greenland
coordinates: lat: 61.1
lon: -43.08333333
In 1881 the Northern Pacific Railway included a stop in what is now Townsend. Geography. According to the United States Census Bureau, the county has a total area of, of which is land and (3.7%) is water. The boundaries of the county are roughly formed by the Big Belt Mountains to the east and north, the Elkhorn Mountains to the west, and the Horseshoe Hills to the south.

Geographic entities mentioned:
surface_form: Horseshoe Hills
instance_of: Landform
countries: United States
coordinates: lat: 46.0236
lon: -111.272
The specific epithet (&quot;uniflora&quot;) refers to the usually single-flowered inflorescence. Distribution and habitat. This species grows in mallee scrub and coastal heath on limestone and is endemic to the Mount Lofty and Port Lincoln areas and Kangaroo Island in south-eastern South Australia.

Geographic entities mentioned:
surface_form: Mount Lofty
instance_of: Mountain
countries: Australia
coordinates: lat: -34.966666666667
lon: 138.7
He previously served as the United States attorney for the same district. Early life and education. Michael Mosman was born in the Willamette Valley of Oregon in 1956 in the city of Eugene. He grew up in Lewiston, Idaho, the son of an attorney and judge with an older sister and three younger brothers. He attended Ricks College in Idaho, which is now Brigham Young University–Idaho.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
There they fixed bayonets and &quot;with bright weapons glittering, colours flying and drums beating, they marched up Church Street and back to Town Plot, where the barracks stood.&quot; This show of force brought the locals back in line. Bayard took an interest in the Annapolis Valley, and after the war he took up a grant of 4,730 acres at Wilmot Mountain.

Geographic entities mentioned:
surface_form: Annapolis Valley
instance_of: Valley
countries: Canada
coordinates: lat: 44.979166666666664
lon: -64.89222222222222
Ulaangom. Ulaangom (;;) is the capital of Uvs Province in Mongolia. It is located on the slopes of the Kharkhiraa mountain, southwest from Uvs Lake shore and south from the Russian border. Description. The city has a population of 37,754 (2022 census), 26,319 (2000 census), 23,000 (2006 est.), 22,300 (end of 2008 est.) or 37.8% of the total population of Uvs aimag.

Geographic entities mentioned:
surface_form: Kharkhiraa mountain
instance_of: Mountain
countries: Mongolia
coordinates: lat: 49.56972222
lon: 91.38527778
That same day, she captured the blockade runner &quot;P. C. Wallis&quot;. In April, she bombarded Confederate-held Fort Jackson and Fort St. Philip. Next month, &quot;John P. Jackson&quot; participated in a scout of Lake Pontchartrain. After moving up the Mississippi River towards Vicksburg, Mississippi, &quot;John P. Jackson&quot; was damaged by Confederate fire on June 28.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
The rescue was instead performed by &quot;Sachem&quot;. On 9 May, &quot;Sachem&quot;, &quot;John P. Jackson&quot;, &quot;Clifton&quot;, and &quot;Westfield&quot; were ordered to scout the Pearl River and Lake Pontchartrain. The vessels entered Lake Pontchartrain on 13 May and entered the Tchefuncte River that evening. The next day, &quot;John P.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889