Sarmila/GeoWiki-Features huggingface dataset:
Specht was a founder member of the German Alpine Club. It is now a very popular destination due to it being the highest mountain of the Stubai Alps and because of the view from the summit, which takes in all the major peaks of the Stubai Alps, the Ötztal Alps, the Zillertal Alps and the Ortler Alps. The normal route is along the east ridge.

Geographic entities mentioned:
surface_form: zillertal
instance_of: Valley
countries: Austria
coordinates: lat: 47.333333333333
lon: 11.866666666667
surface_form: stubai
instance_of: Valley
countries: Austria
coordinates: lat: 47.1667
lon: 11.3167
surface_form: stubai
instance_of: Valley
countries: Austria
coordinates: lat: 47.1667
lon: 11.3167
surface_form: ötztal
instance_of: Valley
countries: Austria
coordinates: lat: 47.136944
lon: 10.927222
Zuckerhütl. The Zuckerhütl is a mountain in Tyrol, Austria. At 3,505 metres (11,499 feet), it is the highest peak of the Stubai Alps and lies at the southern end of the Stubaital Valley. It derives its name, the German for sugarloaf, from its conical shape. In nearby Italy it is known as &quot;Pan di Zùcchero&quot;, the Italian term for sugarloaf.

Geographic entities mentioned:
surface_form: zuckerhütl
instance_of: Mountain
countries: Austria
coordinates: lat: 46.964444444444
lon: 11.153611111111
In nearby Italy it is known as &quot;Pan di Zùcchero&quot;, the Italian term for sugarloaf. On the mountain's north face the huge &quot;Sulzenauferner&quot; glacier falls 1,000m from its summit, resembling an icefall which looks unclimbable without ladders. It is the views of this great glacier which give Zuckerhütl its name. On its south face a 500m high cliff drops down from the summit.

Geographic entities mentioned:
surface_form: zuckerhütl
instance_of: Mountain
countries: Austria
coordinates: lat: 46.964444444444
lon: 11.153611111111
It is the seat of Burabay District (form. Shchuchinsk District) in Akmola Region and is the centre of a large agricultural area. Geography. Shchuchinsk is located at the feet of the Kokshetau Massif, in the Kokshetau Hills, northern part of the Kazakh Uplands. Burabay spa town lies nearby to the northeast. History.

Geographic entities mentioned:
surface_form: Kokshetau Hills
instance_of: Mountain
countries: Kazakhstan
coordinates: lat: 53.080000000000005
lon: 70.18833333333333
Wachusett Potato Chip Company. Wachusett Potato Chip Company in Fitchburg, Massachusetts was founded in 1937, by Polish-American brothers Theofil and Stephen “Sam” Krysiak. The company takes its name from nearby Mount Wachusett. The company was originally founded in Clinton, Massachusetts and moved to Fitchburg in 1947 when it purchased a decommissioned Fitchburg County jail building and grounds.

Geographic entities mentioned:
surface_form: Mount Wachusett
instance_of: Mountain
countries: United States
coordinates: lat: 42.488888888889
lon: -71.8875
__NOTOC__
MD 903. Maryland Route 903 is the unsigned designation for a section of Mountain Road on the western slope of Sideling Hill in far western Washington County from the Exit 74 exit ramp from eastbound I-68 north to the Exit 74 entrance ramp to westbound I-68. MD 903 is not signed as such; rather, the northbound direction is signed as part of westbound US 40 Scenic. MD 904.

Geographic entities mentioned:
surface_form: Sideling Hill
instance_of: Mountain
countries: United States
coordinates: lat: 39.7192
lon: -78.2836
MD 942. Maryland Route 942 is the unsigned designation for the section of Bridge Street comprising the Blue Bridge, a steel through arch bridge across the North Branch Potomac River in Cumberland. The 1953 bridge connects Greene Street in Cumberland with the northern terminus of West Virginia Route 28 Alternate in Ridgeley. MD 943.

Geographic entities mentioned:
surface_form: North Branch Potomac River
instance_of: Watercourse
countries: United States
coordinates: lat: 39.5284255
lon: -78.5875141
MD 956. Maryland Route 956 is a state highway in Pinto in central Allegany County. Known as Patriot Parkway, the two-lane highway begins at US 220, crosses CSX's Mountain Subdivision, and reaches its eastern terminus at the West Virginia state line at the North Branch Potomac River, where the highway continues as West Virginia Route 956 (WV 956) through Rocket Center.

Geographic entities mentioned:
surface_form: North Branch Potomac River
instance_of: Watercourse
countries: United States
coordinates: lat: 39.5284255
lon: -78.5875141
The fan is the base layer of the Musashino Plateau, and is covered by the Kantō Loam Formation, which is 5 to 15 meters thick. The loam is primarily andesite or basaltic sandy mud formed from volcanic ash that the wind carried west from Mount Fuji. Two types of developed fluvial terraces (river terraces) are found on the plateau. One is formed by the flow of the Tama River on the south side.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
Musashino Plateau. The, also translated from Japanese as Musashino Platform and also named Musashino Region, is a large tableland that sits between the Arakawa and Tama rivers in the Kantō region of Honshu, Japan. The plateau consists of an alluvial fan formed by the ancient Tama River, covered by a layer of loam formed from volcanic ash. Location. The plateau is part of the Kantō Plain.

Geographic entities mentioned:
surface_form: musashino plateau
instance_of: Plateau
countries: Japan
Musashino Plateau. The, also translated from Japanese as Musashino Platform and also named Musashino Region, is a large tableland that sits between the Arakawa and Tama rivers in the Kantō region of Honshu, Japan. The plateau consists of an alluvial fan formed by the ancient Tama River, covered by a layer of loam formed from volcanic ash. Location. The plateau is part of the Kantō Plain.

Geographic entities mentioned:
surface_form: musashino platform
instance_of: Plateau
countries: Japan
surface_form: musashino
instance_of: Plateau
countries: Japan
Origin. The Tama River carved the Okutama Mountains and deposited a large alluvial fan that spread out from Ōme. The fan is the base layer of the Musashino Plateau, and is covered by the Kantō Loam Formation, which is 5 to 15 meters thick. The loam is primarily andesite or basaltic sandy mud formed from volcanic ash that the wind carried west from Mount Fuji.

Geographic entities mentioned:
surface_form: musashino plateau
instance_of: Plateau
countries: Japan
Two types of developed fluvial terraces (river terraces) are found on the plateau. One is formed by the flow of the Tama River on the south side. The lowest terrace (low surface) is the Tachikawa terrace, and the terrace one step higher than that (high surface) is the Musashino terrace. The other is in the north and is thought to be a remnant of the former Tama River channel.

Geographic entities mentioned:
surface_form: musashino
instance_of: Plateau
countries: Japan
Also she twice won East Germany Women's Fast Chess Championships: in 1988 and in 1990. In 1990, Wagner-Michel participated in Women's World Chess Championship Interzonal Tournament in Genting Highlands where ranked 16th place. In 1975, she was awarded the FIDE Woman International Master (WIM) title.

Geographic entities mentioned:
surface_form: Genting Highlands
instance_of: Mountain
countries: Malaysia
coordinates: lat: 3.42368
lon: 101.79335
The Vltava swirls into the St John's Rapids; then it widens and flows toward Prague, past the Vyšehrad, and then majestically vanishes into the distance, ending at the Elbe. Vltava contains Smetana's most famous tune.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Blaník. Blaník was finished on 9 March 1879 and premiered on 4 January 1880. It is named for the mountain Blaník inside which a legend says that a huge army of knights led by St. Wenceslaus sleep. The knights will awake and help the country in its gravest hour (sometimes described as four hostile armies attacking from all cardinal directions).

Geographic entities mentioned:
surface_form: Blaník
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 49.642222222222
lon: 14.872777777778
Sgòr Gaoith. Sgòr Gaoith (, 'windy peak') is a mountain peak in the far western massif of the Cairngorms in the Scottish Highlands. It is high, and is the highest point on a long north-south ridge. The ridge is separated from the Braeriach massif to the east by Gleann Eanaich and Loch Eanaich. The name 'Sgòr Gaoith' also refers to the mountain as a whole.

Geographic entities mentioned:
surface_form: Braeriach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.078298
lon: -3.728389
surface_form: loch eanaich
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.069177
lon: -3.792183
Sgòr Gaoith. Sgòr Gaoith (, 'windy peak') is a mountain peak in the far western massif of the Cairngorms in the Scottish Highlands. It is high, and is the highest point on a long north-south ridge. The ridge is separated from the Braeriach massif to the east by Gleann Eanaich and Loch Eanaich. The name 'Sgòr Gaoith' also refers to the mountain as a whole.

Geographic entities mentioned:
surface_form: sgòr gaoith
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.068483333333
lon: -3.8100277777778
It is high, and is the highest point on a long north-south ridge. The ridge is separated from the Braeriach massif to the east by Gleann Eanaich and Loch Eanaich. The name 'Sgòr Gaoith' also refers to the mountain as a whole. The other summits of the mountain are Sgòran Dubh Mòr (1,111 m high) to the north, and Càrn Bàn Mòr (1052 m high) to the south.

Geographic entities mentioned:
surface_form: sgòr gaoith
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.068483333333
lon: -3.8100277777778
The other summits of the mountain are Sgòran Dubh Mòr (1,111 m high) to the north, and Càrn Bàn Mòr (1052 m high) to the south. The eastern side of Sgòr Gaoith is girded by steep cliffs which plunge down to Loch Eanaich; the western side is composed of heather slopes and a number of shallow corries. The two most commonly used routes up Sgòr Gaoith start from Glen Feshie to the west.

Geographic entities mentioned:
surface_form: sgòr gaoith
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.068483333333
lon: -3.8100277777778
surface_form: loch eanaich
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.069177
lon: -3.792183
The other summits of the mountain are Sgòran Dubh Mòr (1,111 m high) to the north, and Càrn Bàn Mòr (1052 m high) to the south. The eastern side of Sgòr Gaoith is girded by steep cliffs which plunge down to Loch Eanaich; the western side is composed of heather slopes and a number of shallow corries. The two most commonly used routes up Sgòr Gaoith start from Glen Feshie to the west.

Geographic entities mentioned:
surface_form: sgòr gaoith
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.068483333333
lon: -3.8100277777778
Dent de Burgin. Dent de Burgin is a mountain near the Meribel resort in Savoie, France. It lies in the Vanoise range. It has an altitude of 2739 meters above sea level.

Geographic entities mentioned:
surface_form: dent de burgin
instance_of: Mountain
countries: France
coordinates: lat: 45.389
lon: 6.6062
It is situated north-northwest of Foreman Glacier, north of Wubbold Glacier and east of Lennon Glacier, flows northwards between Igralishte Peak on the west and Mount Newman on the east, leaves Havre Mountains and joins Bongrain Ice Piedmont. The feature is named after the Bulgarian composer Parashkev Hadzhiev (1912-1992). Location. Hadzhiev Glacier is centered at. British mapping in 1971.

Geographic entities mentioned:
surface_form: Mount Newman
instance_of: Mountain
coordinates: lat: -69.1833
lon: -71.4333
surface_form: Bongrain Ice Piedmont
instance_of: Landform
coordinates: lat: -69
lon: -71.5
Taxonomy. This species was described by Edward Meyrick in 1885 named &quot;Palaeomicra chrysargyra&quot; using a specimen collected in December at Lake Wakatipu at an altitude of 1100 ft. Meyrick went on to give a fuller description of the species published in 1886. In 1912 Meyrick placed this species within the &quot;Sabatinca&quot; genus. Gibbs, in 2014, synonymised &quot;S.

Geographic entities mentioned:
surface_form: Lake Wakatipu
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.085
lon: 168.561
Klawasi group. The Klawasi group is a cluster of three large mud volcanoes on the western flank of Mount Drum, a Pleistocene stratovolcano in the Wrangell Mountains of east-central Alaska in the United States. The cluster includes the Upper Klawasi, the Lower Klawasi and the Shrub.

Geographic entities mentioned:
surface_form: Mount Drum
instance_of: Mountain
countries: United States
coordinates: lat: 62.1161
lon: -144.638
A study of the diverse systems of the creation of the universe). Back in Colombia by 1871, he ran for president again but failed, although he was elected to the presidency of Cauca State until 1873. He was a senator again in 1876. He died October 7, 1878, in his farm Coconuco, in Puracé, close to Popayán. He was buried in the Panteón de los Próceres cemetery in Popayán.

Geographic entities mentioned:
surface_form: Puracé
instance_of: Mountain
countries: Colombia
coordinates: lat: 2.3141666666667
lon: -76.394166666667
He received the Medal of Honor for gallantry during the Battle of Cedar Creek fought near Middletown, Virginia on October 19, 1864. The battle was the decisive engagement of Major General Philip Sheridan's Valley Campaigns of 1864 and was the largest battle fought in the Shenandoah Valley. Medal of Honor citation.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
The Regalmspitze and its subpeak rise in the eastern part of the Kaisergebirge mountains, often referred to as the &quot;Ostkaiser&quot; or &quot;East Kaiser&quot;. They lie somewhat east of the Kleines Törl and west of the high and better-known Ackerlspitze. Seen from the south, from the area of Going, the &quot;Ostkaiser&quot; forms a famous mountain backdrop which includes the Regalmspitze.

Geographic entities mentioned:
surface_form: Ackerlspitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.55
lon: 12.333333333333
surface_form: ackerlspitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.55
lon: 12.333333333333
Another option is an approach from the north, i.e. from the &quot;Griesner Alm&quot; in the Kaiserbach valley via the Fritz Pflaum Hut and the Kleines Törl to the memorial plaque. Near the aforementioned memorial plaque, the signposted, but unsecured normal route branches off up to the Regalmspitze ab.

Geographic entities mentioned:
surface_form: Kaiserbach valley
instance_of: Valley
countries: Austria
coordinates: lat: 47.58166666666666
lon: 12.361666666666666
Regalmspitze. __NOTOC__
The Regalmspitze (or Regalpspitze) is a high, lesser known mountain in the Kaisergebirge in the Northern Limestone Alps in Austria. The name &quot;Regalmwand&quot; (or &quot;Regalpwand&quot;), refers to the high subpeak to the west of the Regalmspitze. Location.

Geographic entities mentioned:
surface_form: regalmspitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.556666666667
lon: 12.338888888889
Regalmspitze. __NOTOC__
The Regalmspitze (or Regalpspitze) is a high, lesser known mountain in the Kaisergebirge in the Northern Limestone Alps in Austria. The name &quot;Regalmwand&quot; (or &quot;Regalpwand&quot;), refers to the high subpeak to the west of the Regalmspitze. Location.

Geographic entities mentioned:
surface_form: regalmspitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.556666666667
lon: 12.338888888889
surface_form: regalpspitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.556666666667
lon: 12.338888888889
Regalmspitze. __NOTOC__
The Regalmspitze (or Regalpspitze) is a high, lesser known mountain in the Kaisergebirge in the Northern Limestone Alps in Austria. The name &quot;Regalmwand&quot; (or &quot;Regalpwand&quot;), refers to the high subpeak to the west of the Regalmspitze. Location.

Geographic entities mentioned:
surface_form: regalmspitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.556666666667
lon: 12.338888888889
surface_form: regalmspitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.556666666667
lon: 12.338888888889
They lie somewhat east of the Kleines Törl and west of the high and better-known Ackerlspitze. Seen from the south, from the area of Going, the &quot;Ostkaiser&quot; forms a famous mountain backdrop which includes the Regalmspitze. Routes. Because of its challenging approach route the Regalmspitze is one of the unknown and rarely climbed peaks on the Wilder Kaiser ridge.

Geographic entities mentioned:
surface_form: regalmspitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.556666666667
lon: 12.338888888889
Another option is an approach from the north, i.e. from the &quot;Griesner Alm&quot; in the Kaiserbach valley via the Fritz Pflaum Hut and the Kleines Törl to the memorial plaque. Near the aforementioned memorial plaque, the signposted, but unsecured normal route branches off up to the Regalmspitze ab.

Geographic entities mentioned:
surface_form: regalmspitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.556666666667
lon: 12.338888888889
Near the aforementioned memorial plaque, the signposted, but unsecured normal route branches off up to the Regalmspitze ab. It crosses steep slopes to a rocky gully, runs up the gully and then continues over very steep terrain and short steps to the wind gap between the Regalmwand and Regalmspitze.

Geographic entities mentioned:
surface_form: regalmspitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.556666666667
lon: 12.338888888889
This is where the main challenge, the vertical wall of the &quot;Wandl&quot; has to be overcome (UIAA climbing grade II). Once over that, the route continues without any difficulty over easy rocks up to the summit cross on the Regalmspitze.

Geographic entities mentioned:
surface_form: regalmspitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.556666666667
lon: 12.338888888889
Bělkovice-Lašťany is a municipality and village in Olomouc District in the Olomouc Region of the Czech Republic. It has about 2,300 inhabitants. Geography. Bělkovice-Lašťany is located about north of Olomouc. It lies on the border between the Upper Morava Valley and Nízký Jeseník range. The highest point is at above sea level. The stream Trusovický potok flows through the municipality. History.

Geographic entities mentioned:
surface_form: Upper Morava Valley
instance_of: Valley
countries: Czech Republic
coordinates: lat: 49.29417
lon: 17.45179
Tipula denali. &quot;Tipula denali&quot; is a crane fly species of the family Tipulidae. It is endemic to Alaska. The species holotype was collected from Muldrow Glacier in Denali National Park and Preserve. It is named after Denali. Description. The fly's length is about 16 millimeters, with wings about 14.5 mm and antennae about 4 mm.

Geographic entities mentioned:
surface_form: Denali
instance_of: Mountain
countries: United States
coordinates: lat: 63.06916666666667
lon: -151.0063888888889
It rises at a point 1289 feet (393 m) above sea level near the Three Shire Stone at the highest point of Wrynose Pass () in the Lake District. Its catchment area includes the northern flanks of Wetherlam, Great Carrs and others of the Furness Fells, as well as a substantial area of the Langdale Fells. It flows through Elter Water, marking the division between its upper and lower catchments.

Geographic entities mentioned:
surface_form: Wetherlam
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.401
lon: -3.098
surface_form: Great Carrs
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.3983
lon: -3.12438
Little Langdale Tarn is also replenished by the Greenburn Beck. The Brathay drains Little Langdale Tarn at its eastern side. It continues in an easterly direction, over Colwith Force where it falls 40 feet (12 m), before turning north and flowing into the tarn of Elter Water at an elevation of 187 feet (57 m) above sea level. Elter Water is also replenished by the Great Langdale Beck.

Geographic entities mentioned:
surface_form: Elter Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.427469444444
lon: -3.025875
Passing under the A593 road at Skelwith Bridge, and continues in an easterly direction, to the hamlet of
Clappersgate. After another quarter of a mile (400 m) it joins the
River Rothay close to Croft Lodge south-west of Ambleside before flowing into the northern end of Windermere. The stretches of the Brathay around Clappersgate and Skelwith Force are popular with canoeists. History.

Geographic entities mentioned:
surface_form: Windermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.358333333333
lon: -2.9361111111111
Since local government re-organisation in 1974 the Brathay has been within the administrative county of Cumbria. The river also gives its name to the Brathay estate where the Brathay Exploration Group is based, just south of its confluence with the River Rothay on the edge of Windermere, and is home to the Brathay Trust youth-development charity.

Geographic entities mentioned:
surface_form: Windermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.358333333333
lon: -2.9361111111111
Course. The Tundik has its sources near Akkora, on the slopes of the Keshubai and Konyrtemirshi mountains of the Kazakh Uplands. It heads roughly northwards, bending northeastwards by Mount Ku. After leaving the mountain to the west it flows northwards again. Shortly before reaching the 51st parallel north the Tundik bends northeastwards.

Geographic entities mentioned:
surface_form: Mount Ku
instance_of: Mountain
countries: Kazakhstan
coordinates: lat: 49.81666666666667
lon: 76.76666666666667
After leaving the mountain to the west it flows northwards again. Shortly before reaching the 51st parallel north the Tundik bends northeastwards. Finally it reaches salt lake Karasor and enters it from the western shore. The width of the river valley in the upper course is between and, in the middle stretch between and, and in the lower reaches of the river the valley widens, reaching to.

Geographic entities mentioned:
surface_form: Karasor
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 51.07944
lon: 77.51444
The riverbanks are mostly steep, between and. Tributaries. The main tributaries of the Tundik are the long Bala Tundik, with its sources in Mount Ku, on the left, and long Ashchyshiozek on the right. Other major tributaries are long Kyzylashchy, long Akzharyk, long Upper Karasu, long Lower Karasu, long Sarybulak, long Egindibulak, long Zharkayin and long Kundik.

Geographic entities mentioned:
surface_form: Mount Ku
instance_of: Mountain
countries: Kazakhstan
coordinates: lat: 49.81666666666667
lon: 76.76666666666667
The municipality covers an area of 199.04 km2. It is part of the Zaachila District in the west of the Valles Centrales Region. As of 2005, the municipality had a total population of 4,303.

Geographic entities mentioned:
surface_form: Valles Centrales Region
instance_of: Valley
countries: Mexico
coordinates: lat: 17.0833
lon: -96.75
Mount James Walker. Mount James Walker is a mountain summit located in Kananaskis Country in the Canadian Rockies of Alberta, Canada. Mount James Walker is situated within Spray Valley Provincial Park, and its nearest higher peak is Mount Galatea, to the northwest. History.

Geographic entities mentioned:
surface_form: Mount Galatea
instance_of: Mountain
countries: Canada
coordinates: lat: 50.83972222222222
lon: -115.27388888888889
surface_form: mount james walker
instance_of: Mountain
countries: Canada
coordinates: lat: 50.805
lon: -115.22
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. The Lewis Overthrust extends over 450 km from Mount James Walker south to Steamboat Mountain, located west of Great Falls, Montana. Nearby Mount Kidd marks the northern end of the Lewis Thrust Fault. Climate.

Geographic entities mentioned:
surface_form: Mount Kidd
instance_of: Mountain
countries: Canada
coordinates: lat: 50.89361111111111
lon: -115.18972222222222
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. The Lewis Overthrust extends over 450 km from Mount James Walker south to Steamboat Mountain, located west of Great Falls, Montana. Nearby Mount Kidd marks the northern end of the Lewis Thrust Fault. Climate.

Geographic entities mentioned:
surface_form: mount james walker
instance_of: Mountain
countries: Canada
coordinates: lat: 50.805
lon: -115.22
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount James Walker. Mount James Walker is a mountain summit located in Kananaskis Country in the Canadian Rockies of Alberta, Canada. Mount James Walker is situated within Spray Valley Provincial Park, and its nearest higher peak is Mount Galatea, to the northwest. History.

Geographic entities mentioned:
surface_form: mount james walker
instance_of: Mountain
countries: Canada
coordinates: lat: 50.805
lon: -115.22
Mount James Walker. Mount James Walker is a mountain summit located in Kananaskis Country in the Canadian Rockies of Alberta, Canada. Mount James Walker is situated within Spray Valley Provincial Park, and its nearest higher peak is Mount Galatea, to the northwest. History.

Geographic entities mentioned:
surface_form: mount james walker
instance_of: Mountain
countries: Canada
coordinates: lat: 50.805
lon: -115.22
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Nearby Mount Kidd marks the northern end of the Lewis Thrust Fault. Climate. Based on the Köppen climate classification, Mount James Walker is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: mount james walker
instance_of: Mountain
countries: Canada
coordinates: lat: 50.805
lon: -115.22
Mount James Walker is situated within Spray Valley Provincial Park, and its nearest higher peak is Mount Galatea, to the northwest. History. The mountain was named in 1959 after Colonel James Walker (1846-1936), who was a Mountie, soldier, businessman, and postmaster of the Kananaskis Post Office. He was named Calgary's &quot;Citizen of the Century&quot; during the city's centennial year in 1975.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Climate. Based on the Köppen climate classification, Mount James Walker is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from the mountain drains into the Kananaskis River which is a tributary of the Bow River, and thence the Saskatchewan River.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
It is also called the &quot;all-front-sided&quot; keep because all sides look the same from all directions. It is believed that once Mount Fuji could be seen from this keep, hence the name. Since the main keep of Edo Castle was destroyed in 1657 and not reconstructed, the &quot;Fujimi-yagura&quot; took on its role and was an important building after being constructed in 1659 during the Edo period.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
Gladstone, California. Gladstone was a settlement established during the Southern California real estate boom of the 1880s, located in the San Gabriel Valley in or near the present-day cities of Azusa, Covina, and Glendora in Los Angeles County, California.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
Taxonomy and naming. &quot;Eucalyptus petraea&quot; was first formally described in 1983 by Denis and Stella Carr in the journal &quot;Nuytsia&quot; from material they collected near Gnarlbine Rock in 1980. The specific epithet (&quot;petraea&quot;) is from the Latin word &quot;petraueus&quot; meaning &quot;growing among rocks&quot;. Distribution and habitat.

Geographic entities mentioned:
surface_form: Gnarlbine Rock
instance_of: Mountain
countries: Australia
coordinates: lat: -31.15
lon: 120.95861111111
Marjing Polo Complex. The Marjing Polo Complex () is a sports complex dedicated to ancient Meitei deity Marjing, and Meitei horse (Manipuri pony), built in the hilltop of the Heingang Ching, the sacred abode of God Marjing, located in Heingang, Imphal East district. It houses Marjing Polo Statue, the world's tallest equestrian statue of a polo player.

Geographic entities mentioned:
surface_form: Heingang Ching
instance_of: Mountain
countries: India
coordinates: lat: 24.879
lon: 93.954
Act 5. &quot;The ruins of Amathus and the surrounding countryside&quot;
Diana has unleashed a terrible beast who is killing the people of Amanthus, much to the satisfaction of Mars. Cidippe implores him to intervene, but he refuses and ascends to Mount Olympus. Adonis meets Cidippe as he sets out to slay the monster.

Geographic entities mentioned:
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
To prevent raids from limiting production, satellite factories near Belfast were operated at Aldergrove and Maghaberry, producing 232 Stirlings between them. A temporary Short's factory was established at White Cross Bay, Windermere, that produced 35 Sunderland Mark IIIs.

Geographic entities mentioned:
surface_form: Windermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.358333333333
lon: -2.9361111111111
His tenure lasted until 23 December that year when he was replaced by Gabriel Marie Joseph, comte d'Hédouville. In January 1797, his division covered the western side of Lake Garda during the fourth Austrian attempt to raise the Siege of Mantua. Summoned to the east by Bonaparte, some of his troops marched and others crossed the lake by boat to fight at the Battle of Rivoli on 14 January.

Geographic entities mentioned:
surface_form: Lake Garda
instance_of: Lake
countries: Italy
coordinates: lat: 45.633333333333
lon: 10.666666666667
Anfo. Anfo (Brescian:;) is a &quot;comune&quot; in the province of Brescia in northern Italy, roughly halfway between Milan and Venice. It is in the Lombardy region near Lake Idro and is bounded by other communes of Bagolino and Collio. Rocca d'Anfo, a fortress, is located in it.

Geographic entities mentioned:
surface_form: Lake Idro
instance_of: Lake
countries: Italy
coordinates: lat: 45.7745
lon: 10.511
It is situated in the John Muir Wilderness on land managed by Inyo National Forest. It is four miles north of Red and White Mountain, and approximately southeast of the community of Mammoth Lakes. The nearest higher neighbor is Red Slate Mountain, to the south-southwest. Baldwin ranks as the 257th highest summit in California.

Geographic entities mentioned:
surface_form: Red and White Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.479722222222
lon: -118.85722222222
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.94687
lon: -119.3096
It is situated in the John Muir Wilderness on land managed by Inyo National Forest. It is four miles north of Red and White Mountain, and approximately southeast of the community of Mammoth Lakes. The nearest higher neighbor is Red Slate Mountain, to the south-southwest. Baldwin ranks as the 257th highest summit in California.

Geographic entities mentioned:
surface_form: Red Slate Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.507555555556
lon: -118.86930555556
Most weather fronts originate in the Pacific Ocean, and travel east toward the Sierra Nevada mountains. As fronts approach, they are forced upward by the peaks, causing them to drop their moisture in the form of rain or snowfall onto the range (orographic lift). Precipitation runoff from the mountain drains east to Crowley Lake via McGee Creek, and west into Convict Creek, thence Convict Lake.

Geographic entities mentioned:
surface_form: Convict Lake
instance_of: Lake
countries: United States
coordinates: lat: 37.588611111111
lon: -118.85778055556
Mount Baldwin (California). Mount Baldwin is a mountain summit located in the Sierra Nevada mountain range in Mono County of northern California, United States. It is situated in the John Muir Wilderness on land managed by Inyo National Forest. It is four miles north of Red and White Mountain, and approximately southeast of the community of Mammoth Lakes.

Geographic entities mentioned:
surface_form: mount baldwin
instance_of: Mountain
countries: United States
coordinates: lat: 37.531944444444
lon: -118.85083333333
The first ascent of the summit was made July 2, 1928, by Norman Clyde, who is credited with 130 first ascents, most of which were in the Sierra Nevada. Climate. Mount Baldwin is located in an alpine climate zone. Most weather fronts originate in the Pacific Ocean, and travel east toward the Sierra Nevada mountains.

Geographic entities mentioned:
surface_form: mount baldwin
instance_of: Mountain
countries: United States
coordinates: lat: 37.531944444444
lon: -118.85083333333
Location. The ruins lie in the Hunsrück mountains between the Idar Forest to the north and the town of Idar-Oberstein to the south at a height of about 630 metres above sea level (NN) on the Wildenburger Kopf above the valley of the Idarbach. It was the highest castle in the Hunsrück. History.

Geographic entities mentioned:
surface_form: Wildenburger Kopf
instance_of: Mountain
countries: Germany
coordinates: lat: 49.7761
lon: 7.2568
Goat Hill (Larimer County, Colorado). Goat Hill—also called Bellvue Dome—is an anticline in Larimer County, Colorado near Bellvue. The dome has a gradual slope on its east side, but its west side is an almost-vertical cliff that hangs over the Cache la Poudre River that passes directly below. The mountain was formed as sedimentary rock was uplifted and folded during the Laramide orogeny. Access.

Geographic entities mentioned:
surface_form: goat hill
instance_of: Mountain
countries: United States
coordinates: lat: 40.6425
lon: -105.17
The mountain was formed as sedimentary rock was uplifted and folded during the Laramide orogeny. Access. The mountain itself is on property owned by the Bureau of Land Management, but it's surrounded by private land, so access is difficult or impossible without permission from the adjacent property owners. Goat Hill is prominently seen by motorists driving south on Highway 287.

Geographic entities mentioned:
surface_form: goat hill
instance_of: Mountain
countries: United States
coordinates: lat: 40.6425
lon: -105.17
Goat Hill (Larimer County, Colorado). Goat Hill—also called Bellvue Dome—is an anticline in Larimer County, Colorado near Bellvue. The dome has a gradual slope on its east side, but its west side is an almost-vertical cliff that hangs over the Cache la Poudre River that passes directly below. The mountain was formed as sedimentary rock was uplifted and folded during the Laramide orogeny. Access.

Geographic entities mentioned:
surface_form: the dome
instance_of: Mountain
countries: United States
coordinates: lat: 46.307777777778
lon: -122.1575
Watershed. The Corte Madera (aka Ross Valley) Watershed ranges in elevation from sea level to at the East Peak of Mount Tamalpais. The watershed covers in the southeastern quarter of Marin County and encompasses the towns of Larkspur, Corte Madera, Kentfield, Ross, San Anselmo, and Fairfax.

Geographic entities mentioned:
surface_form: Mount Tamalpais
instance_of: Mountain
countries: United States
coordinates: lat: 37.9291
lon: -122.578
By 1948, she was logging an average of almost per year. On the night of 3 June 1950, &quot;Penguin&quot; was moored at the FWS dock in Lake Union at Seattle when a fire destroyed her superstructure and cabins.

Geographic entities mentioned:
surface_form: Lake Union
instance_of: Lake
countries: United States
coordinates: lat: 47.6392
lon: -122.3337
As a metropolitan area, it is known as the Scranton–Wilkes-Barre metropolitan area, after its principal cities, Scranton and Wilkes-Barre. With a population of 567,559 as of the 2020 United States census, it is the fifth-largest metropolitan area in Pennsylvania, after the Delaware Valley, Greater Pittsburgh, the Lehigh Valley, and the Harrisburg–Carlisle metropolitan statistical areas.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
surface_form: carlisle
instance_of: Mountain
countries: United States
coordinates: lat: 52.8939
lon: -170.054
Wyoming Valley. The Wyoming Valley is a historic industrialized region of Northeastern Pennsylvania. The region is historically notable for its influence in helping fuel the American Industrial Revolution with its many anthracite coal mines. As a metropolitan area, it is known as the Scranton–Wilkes-Barre metropolitan area, after its principal cities, Scranton and Wilkes-Barre.

Geographic entities mentioned:
surface_form: wyoming valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
With a population of 567,559 as of the 2020 United States census, it is the fifth-largest metropolitan area in Pennsylvania, after the Delaware Valley, Greater Pittsburgh, the Lehigh Valley, and the Harrisburg–Carlisle metropolitan statistical areas. Within the geology of Pennsylvania the Wyoming Valley makes up its own unique physiographic province, the Anthracite Valley.

Geographic entities mentioned:
surface_form: wyoming valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
The Pocono Mountains, a ridgeline away, are often visible from higher elevations to the east and to the southeast of the Wyoming Valley. Early history.

Geographic entities mentioned:
surface_form: wyoming valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
Early history. The name Wyoming derives from the Lenape Munsee name, meaning &quot;at the big river flat.&quot;
According to &quot;The Jesuit Relations&quot; in 1635, the Wyoming Valley was inhabited by the Scahentoarrhonon people, an Iroquoian-speaking group; it was then known as the Scahentowanen Valley.

Geographic entities mentioned:
surface_form: wyoming valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
The counties of Bradford, Lackawanna, Susquehanna, and Wyoming were all formed from parts of Luzerne County. Metropolitan statistical area. The Scranton–Wilkes-Barre–Hazleton, PA Metropolitan Statistical Area, also known as the Wyoming Valley, covers Lackawanna, Luzerne, and Wyoming counties. It had a combined population of 558,166 in 2015.

Geographic entities mentioned:
surface_form: wyoming valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
Physical valley. The physical Wyoming Valley, also referred to as the Anthracite Valley Section, is different from the Wyoming Valley metropolitan statistical area. The physical Wyoming Valley is a canoe-shaped valley, about long, which extends from the counties of Susquehanna and Wayne (in the north) to Columbia County (in the south).

Geographic entities mentioned:
surface_form: wyoming valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
surface_form: wyoming valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
The physical Wyoming Valley is a canoe-shaped valley, about long, which extends from the counties of Susquehanna and Wayne (in the north) to Columbia County (in the south). It includes the cities of Carbondale, Scranton, Pittston, Wilkes-Barre, and Nanticoke. Even though Wyoming County is part of the Wyoming Valley Metropolitan Statistical Area, it is not part of the physical valley. Culture.

Geographic entities mentioned:
surface_form: wyoming valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
It includes the cities of Carbondale, Scranton, Pittston, Wilkes-Barre, and Nanticoke. Even though Wyoming County is part of the Wyoming Valley Metropolitan Statistical Area, it is not part of the physical valley. Culture. Scranton is the cultural center of the Wyoming Valley, being the largest city by population in the metropolitan area. Sports.

Geographic entities mentioned:
surface_form: wyoming valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
Local attractions include the Mohegan Sun Arena at Casey Plaza in Wilkes-Barre, the Pocono Raceway in Long Pond, PNC Field in Moosic, Mohegan Pennsylvania in Plains, the Toyota Pavilion in Scranton, the Wyoming Valley Mall in Wilkes-Barre, the Shoppes at Montage in Moosic, the Steamtown Mall in Scranton, the Viewmont Mall in Scranton/Dickson City, Pennsylvania, and the Ski Resort in Scranton.

Geographic entities mentioned:
surface_form: wyoming valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
surface_form: long pond
instance_of: Lake
countries: United States
coordinates: lat: 44.329722222222
lon: -68.363611111111
This area is celebrated in Lydia Sigourney's poem Vale of Wyoming published in her Scenes in my Native Land, 1845, with accompanying descriptive text. In the science-fiction story Armageddon 2419 A.D. by Philip Francis Nowlan, American Radioactive Gas Corporation employee Anthony &quot;Buck&quot; Rogers is investigating an abandoned coal mine in the Wyoming Valley when a cave-in traps him.

Geographic entities mentioned:
surface_form: wyoming valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
A gas which fills the mine shaft places him in suspended animation for nearly 500 years. He awakens to find that the United States has been destroyed by a Chinese invasion, and he joins a &quot;gang&quot; of Americans who survive by hiding in the forests of the Wyoming Valley area.

Geographic entities mentioned:
surface_form: wyoming valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
History. During the British Raj, Bhuntar had a bazaar and a branch office for post and telegraphs. In 1905, Duff Dunbar, a British forest officer posted in Kullu, got a suspension bridge constructed at Bhuntar over the Beas River. The bridge connected the Kullu valley to the Parvati valley. The bridge was rendered unserviceable by heavy floods in September 1947.

Geographic entities mentioned:
surface_form: Kullu valley
instance_of: Valley
countries: India
coordinates: lat: 31.957777777778
lon: 77.109444444444
surface_form: Parvati valley
instance_of: Valley
countries: India
coordinates: lat: 31.992352777778
lon: 77.481766666667
Geography. Bhuntar is located on the right bank of the Beas River. Directly opposite Bhuntar, near the left bank of the Beas River, there is the confluence of the Parvati River with the River Beas. The Parvati Valley begins at this confluence and runs eastward, through a steep-sided valley towards Kasol and Manikaran. The next major settlement after Bhuntar, in the direction of Kullu, is Shamshi.

Geographic entities mentioned:
surface_form: Parvati Valley
instance_of: Valley
countries: India
coordinates: lat: 31.992352777778
lon: 77.481766666667
Bhuntar lies on the National Highway 3, which till 2010 was the National Highway 21. The airport at Bhuntar connects the Kullu valley to a few major north Indian cities like Delhi and Amritsar. Bhuntar is a centre within the Kullu valley for accessing places in the Kullu valley such as Shamshi, Kullu, and Manali, and for places in the Parvati valley such as Manikaran, Kasol, and Tosh. Demography.

Geographic entities mentioned:
surface_form: Kullu valley
instance_of: Valley
countries: India
coordinates: lat: 31.957777777778
lon: 77.109444444444
Bhuntar lies on the National Highway 3, which till 2010 was the National Highway 21. The airport at Bhuntar connects the Kullu valley to a few major north Indian cities like Delhi and Amritsar. Bhuntar is a centre within the Kullu valley for accessing places in the Kullu valley such as Shamshi, Kullu, and Manali, and for places in the Parvati valley such as Manikaran, Kasol, and Tosh. Demography.

Geographic entities mentioned:
surface_form: Parvati valley
instance_of: Valley
countries: India
coordinates: lat: 31.992352777778
lon: 77.481766666667
Nevado El Cisne. The Nevado El Cisne or Nevado del Cisne (), also known as Paramillo el Cisne or Paramillo del Cisne (), is a volcano in the Central Ranges of the Andes in Colombia. Its summit is at an altitude of approximately. The mountain belongs to the Cisne-Morro Negro lava dome, a small volcanic complex near Nevado del Ruiz.

Geographic entities mentioned:
surface_form: nevado el cisne
instance_of: Mountain
countries: Colombia
coordinates: lat: 4.8430555555556
lon: -75.352222222222
Five emission centers have been identified as generators of lava flows. The lava flows are andesitic and present notably smaller volumes compared to those observed in neighbouring volcanic complexes (Ruiz and Santa Isabel). The volcano is located over the Palestina Fault, that crosscuts the underlying El Bosque Batholith of Eocene age, dated at 49.1 ± 1.7 Ma.

Geographic entities mentioned:
surface_form: santa isabel
instance_of: Mountain
countries: Colombia
coordinates: lat: 4.81666667
lon: -75.36666667
Dollar Lake (Independence Township, Michigan). Dollar Lake is a lake along the main branch of the Clinton River. The lake lies within Independence Township in Oakland County, Michigan. Dollar Lake connects upstream with Middle Lake to the north and downstream (under a bridge over Dixie Highway) with Greens Lake to the west. Name.

Geographic entities mentioned:
surface_form: dollar lake
instance_of: Lake
countries: United States
coordinates: lat: 45.1899
lon: -117.1877
surface_form: dollar lake (independence township, michigan)
instance_of: Lake
countries: United States
coordinates: lat: 42.724409
lon: -83.423268
surface_form: michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: dollar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.6882
lon: -114.419
Dollar Lake (Independence Township, Michigan). Dollar Lake is a lake along the main branch of the Clinton River. The lake lies within Independence Township in Oakland County, Michigan. Dollar Lake connects upstream with Middle Lake to the north and downstream (under a bridge over Dixie Highway) with Greens Lake to the west. Name.

Geographic entities mentioned:
surface_form: dollar lake
instance_of: Lake
countries: United States
coordinates: lat: 45.1899
lon: -117.1877
surface_form: dollar lake
instance_of: Lake
countries: United States
coordinates: lat: 42.724409
lon: -83.423268
surface_form: dollar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.6882
lon: -114.419