Sarmila/GeoWiki-Features huggingface dataset:
Königssee. The Königssee () is a natural lake in the southeast Berchtesgadener Land district of the German state of Bavaria, near the Austrian border. Most of the lake is within the Berchtesgaden National Park. Description.

Geographic entities mentioned:
surface_form: königssee
instance_of: Lake
countries: Germany
coordinates: lat: 47.55
lon: 12.975
Located at a Jurassic rift, it was formed by glaciers during the last ice age. It stretches about in a north-south direction and is about across at its widest point. Except at its outlet, the Königsseer Ache at the village of Königssee, the lake is similar to a fjord, being surrounded by the steeply-rising flanks of mountains up to, including the Watzmann massif in the west.

Geographic entities mentioned:
surface_form: königssee
instance_of: Lake
countries: Germany
coordinates: lat: 47.55
lon: 12.975
The literal translation of the name, Königssee, appears to be &quot;king's lake&quot;; however while does indeed mean &quot;king&quot;, there had been no Bavarian kings since the days of Louis the German (d. 876) until Elector Maximilian I Joseph assumed the royal title in 1806.

Geographic entities mentioned:
surface_form: königssee
instance_of: Lake
countries: Germany
coordinates: lat: 47.55
lon: 12.975
The Königssee Railway (&quot;Königsseebahn&quot;) served the lake from 1909 until 1965. Its last tracks were dismantled during 1971, and the former station of the Königssee Railway in Berchtesgaden (Königsseer Bahnhof) was demolished in 2012. The only remaining element of the railway is the Königsee station, which is now a restaurant. The track route is mostly used as a walking path.

Geographic entities mentioned:
surface_form: königssee
instance_of: Lake
countries: Germany
coordinates: lat: 47.55
lon: 12.975
South of the Königssee, separated by the &quot;Salet&quot; moraine, is the smaller Obersee lake with the high Röthbach waterfall. Because there is no lakeside path on the steep shore of the Königssee, St. Bartholomä and the southern edge can only be reached by boat, or via hiking trails up the surrounding mountains, except during harsh winters when the lake freezes over.

Geographic entities mentioned:
surface_form: königssee
instance_of: Lake
countries: Germany
coordinates: lat: 47.55
lon: 12.975
Visits. Elizabeth was in Kenya at Treetops Hotel when her father, George VI, died on 6 February 1952 and she became queen. She had arrived in Nairobi on 1 February and had been staying at Sagana Lodge, near Mount Kenya. After the news of her accession, she returned immediately to the United Kingdom via Entebbe Airport.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
High Vinnalls. High Vinnalls is a hill in the English county of Herefordshire, though commonly considered a member of the Shropshire Hills. It is located in the parish of Pipe Aston, near the town of Ludlow, and is covered by Mortimer Forest (and ancient hunting forest). The Mortimer Trail runs for between Ludlow and Kington and passes over High Vinnalls.

Geographic entities mentioned:
surface_form: high vinnalls
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.347215
lon: -2.767824
It is located in the parish of Pipe Aston, near the town of Ludlow, and is covered by Mortimer Forest (and ancient hunting forest). The Mortimer Trail runs for between Ludlow and Kington and passes over High Vinnalls. Before the Norman Conquest of 1066, High Vinnalls marked the western edge of the manor of Richard's Castle.

Geographic entities mentioned:
surface_form: high vinnalls
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.347215
lon: -2.767824
The Mortimer Trail runs for between Ludlow and Kington and passes over High Vinnalls. Before the Norman Conquest of 1066, High Vinnalls marked the western edge of the manor of Richard's Castle. The Mortimer family were then the Norman lords of the region for around 300 years. The High Vinnals is home to the Ludlow parkrun, which held its first event on February 13, 2016.

Geographic entities mentioned:
surface_form: high vinnalls
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.347215
lon: -2.767824
It is in geographic Stewart Township and is part of the Great Lakes Basin. The lake flows west through a channel into Little Tomiko Lake; the Ontario Northland Railway line from North Bay to Cochrane crosses that channel. Little Tomiko Lake empties via the Little Tomiko River, the Tomiko River, the Sturgeon River, Lake Nipissing, and the French River to Georgian Bay on Lake Huron.

Geographic entities mentioned:
surface_form: Lake Nipissing
instance_of: Lake
countries: Canada
coordinates: lat: 46.283333333333
lon: -80
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: nipissing
instance_of: Lake
countries: Canada
coordinates: lat: 46.283333333333
lon: -80
surface_form: sturgeon river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.1167
lon: -62.5333
surface_form: sturgeon river
instance_of: Watercourse
countries: Canada
coordinates: lat: 53.2
lon: -105.867
Sturgeon Lake (Nipissing District). Sturgeon Lake is a lake located south of Tomiko and north-east of Highway 11 / Trans-Canada Highway in the Nipissing District of northeastern Ontario, Canada. It is in geographic Stewart Township and is part of the Great Lakes Basin.

Geographic entities mentioned:
surface_form: sturgeon lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.4167
lon: -106.083
surface_form: sturgeon lake (nipissing district)
instance_of: Lake
countries: Canada
coordinates: lat: 46.5447
lon: -79.4181
surface_form: nipissing
instance_of: Lake
countries: Canada
coordinates: lat: 46.283333333333
lon: -80
surface_form: sturgeon lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.4667
lon: -78.7167
surface_form: sturgeon lake
instance_of: Lake
countries: Canada
coordinates: lat: 55.1044
lon: -117.569
surface_form: sturgeon lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.9744
lon: -90.7689
surface_form: sturgeon lake
instance_of: Lake
countries: Canada
coordinates: lat: 55.3967
lon: -90.9053
Sturgeon Lake (Nipissing District). Sturgeon Lake is a lake located south of Tomiko and north-east of Highway 11 / Trans-Canada Highway in the Nipissing District of northeastern Ontario, Canada. It is in geographic Stewart Township and is part of the Great Lakes Basin.

Geographic entities mentioned:
surface_form: sturgeon lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.4167
lon: -106.083
surface_form: sturgeon lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.5447
lon: -79.4181
surface_form: nipissing
instance_of: Lake
countries: Canada
coordinates: lat: 46.283333333333
lon: -80
surface_form: sturgeon lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.4667
lon: -78.7167
surface_form: sturgeon lake
instance_of: Lake
countries: Canada
coordinates: lat: 55.1044
lon: -117.569
surface_form: sturgeon lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.9744
lon: -90.7689
surface_form: sturgeon lake
instance_of: Lake
countries: Canada
coordinates: lat: 55.3967
lon: -90.9053
It can reach a length of SL. This species is seriously threatened by pollution and sedimentation due to human activities. It is potentially also threatened by large emissions of carbon dioxide (CO2) from the lake's bottom (compare Lake Nyos), although studies indicate that Barombo Mbo lacks excess amounts of this gas.

Geographic entities mentioned:
surface_form: Lake Nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889
The railroad bridge also crosses over Highway 70. The railroad Tobin Bridge is located on the Union Pacific Railroad's (originally Western Pacific Railroad's) Feather River Route through the Sierra Nevada in northeastern California, connecting the Sacramento Valley to Salt Lake City via the Feather River valley.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
Precipitation runoff and glacial meltwater from this mountain drains into tributaries of the Lillooet River. In-SHUCK-ch Mountain is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 2,186 metres (7,172 ft) above Little Lillooet Lake in. History.

Geographic entities mentioned:
surface_form: Little Lillooet Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.11083333
lon: -122.53444444
surface_form: lillooet lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.3333
lon: -122.417
surface_form: lillooet lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.25
lon: -122.5
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: in-shuck-ch mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1172
lon: -122.5941
In-SHUCK-ch Mountain. In-SHUCK-ch Mountain is a summit in British Columbia, Canada. Description. In-SHUCK-ch Mountain is located east of Whistler in Garibaldi Provincial Park and the Coast Mountains. Precipitation runoff and glacial meltwater from this mountain drains into tributaries of the Lillooet River.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: in-shuck-ch mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1172
lon: -122.5941
In-SHUCK-ch Mountain. In-SHUCK-ch Mountain is a summit in British Columbia, Canada. Description. In-SHUCK-ch Mountain is located east of Whistler in Garibaldi Provincial Park and the Coast Mountains. Precipitation runoff and glacial meltwater from this mountain drains into tributaries of the Lillooet River.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: in-shuck-ch mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1172
lon: -122.5941
In-SHUCK-ch Mountain. In-SHUCK-ch Mountain is a summit in British Columbia, Canada. Description. In-SHUCK-ch Mountain is located east of Whistler in Garibaldi Provincial Park and the Coast Mountains. Precipitation runoff and glacial meltwater from this mountain drains into tributaries of the Lillooet River.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
History. The mountain was officially named Gunsight Peak in 1978, but officially changed on August 13, 1992, by the Geographical Names Board of Canada. The name of the mountain is pronounced In-SHUCK-ch, meaning &quot;split like a crutch&quot;, which refers to the split gap of the summit area. The people of the In-SHUCK-ch Nation took their name from this sacred mountain.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The name of the mountain is pronounced In-SHUCK-ch, meaning &quot;split like a crutch&quot;, which refers to the split gap of the summit area. The people of the In-SHUCK-ch Nation took their name from this sacred mountain. In-SHUCK-ch Mountain is significant in the origin stories of the people, as the mountain provided a refuge from a great flood. Climate.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The name of the mountain is pronounced In-SHUCK-ch, meaning &quot;split like a crutch&quot;, which refers to the split gap of the summit area. The people of the In-SHUCK-ch Nation took their name from this sacred mountain. In-SHUCK-ch Mountain is significant in the origin stories of the people, as the mountain provided a refuge from a great flood. Climate.

Geographic entities mentioned:
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
Climate. Based on the Köppen climate classification, In-SHUCK-ch Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (orographic lift), causing them to drop their moisture in the form of rain or snowfall.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: in-shuck-ch mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1172
lon: -122.5941
As a result, the Coast Mountains experience high precipitation, especially during the winter months in the form of snowfall. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports an unnamed glacier on the north slope of the peak. The months of July and August offer the most favorable weather for climbing or viewing In-SHUCK-ch Mountain.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: in-shuck-ch mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1172
lon: -122.5941
As of December 2009, the town itself had a population of 3,586 inhabitants. It is situated on the Bulgarian Black Sea Coast in the vicinity of the salt-water Lake Shabla and Bulgaria's easternmost point, Cape Shabla. Shabla has an extensive white sand beach and was a popular destination for Eastern Bloc tourism until the fall of Communism.

Geographic entities mentioned:
surface_form: Lake Shabla
instance_of: Lake
countries: Bulgaria
coordinates: lat: 43.57305556
lon: 28.56555556
Commissioned by Charles Wood, 2nd Viscount Halifax, a former owner of Hickleton Hall, it was designed by Alfred Young Nutt in 1914. Nutt had been recently forcibly retired as Surveyor to the Dean and Canons of St George's Chapel, Windsor. Its strange Italian style is unique in this part of South Yorkshire and is distinctly odd for a Dearne Valley mining village.

Geographic entities mentioned:
surface_form: Dearne Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.5
lon: -1.2166666666667
Marc Birkigt married Eugénie Brachet in Geneva on November 23, 1901. From their union were born Louis in 1903 and Yvonne in 1905. He lived in Versoix Geneva, Switzerland, since 1930 in his sumptuous “Rive-bleu” residence on the shores of Lake Geneva facing the Mont-Blanc massif. He died on March 15, 1953, at the age of 75, after having filed more than 150 patents.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Tal Barahi Temple. Tal Barahi temple () also known as ‘Lake Temple’ or ‘Barahi Temple’ is a Hindu temple of the goddess Barahi. It is the most important religious monument in Pokhara, Nepal. This temple is located on a small island in the middle of Phewa Lake. As the temple is situated on a small island, the only way to visit it is by boat.

Geographic entities mentioned:
surface_form: Phewa Lake
instance_of: Lake
countries: Nepal
coordinates: lat: 28.214166666667
lon: 83.947222222222
Ibrahim Khan's courage under attack from Afghan, Oudh and Rohilla forces distinguishes him from others and makes him a memorable hero in folklore and songs in the Deccan region. His young son was freed by Hafiz Rahmat Khan Barech. Aftermath. The family and army of Ibrahim Khan Gardi kept on serving Peshwas as personal guards as well as musketeers until the end of the Peshwa rule in 1818.

Geographic entities mentioned:
surface_form: Deccan region
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Mont Ventoux Dénivelé Challenge. The Mont Ventoux Dénivelé Challenge is a professional cycle road race first held in 2019, which takes place between Vaison-la-Romaine and Mont Ventoux. The event was classified by the UCI as category 1.1 event on the UCI Europe Tour from 2019 to 2022. In 2023, the race joined the UCI ProSeries.

Geographic entities mentioned:
surface_form: Mont Ventoux
instance_of: Mountain
countries: France
coordinates: lat: 44.166666666667
lon: 5.2833333333333
After leaving Dartmouth, he studied law in Boston in the office of Robert Rantoul, Jr., and was admitted to the Massachusetts bar in 1845. Wisconsin. He moved to the Wisconsin Territory the following year and settled near Sheboygan, on the coast of Lake Michigan. He quickly became a prominent lawyer in the area and became involved in local politics as a member of the Democratic Party.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
In the Beit She'an area, several sites are named after him: &quot;Ein Kaftor&quot; and &quot;Ein Perach&quot; are two springs located between Tirat Zvi and Ein HaNatziv; near Beit She'an, there is &quot;Tel&quot; &quot;Ishtori&quot;, as well as a spring named &quot;Ma'ayan&quot; &quot;Ishtori&quot;.

Geographic entities mentioned:
surface_form: Beit She'an area
instance_of: Valley
countries: Israel
coordinates: lat: 32.4794
lon: 35.5058
It flows over the Muskox Rapids, takes in the left tributary Contwoyto River, and heads east through the Heywood Range. The Back River heads over the Malley Rapids, takes in the left tributary Siorak River and enters the long lake-expansion Lake Beechey in a southeast direction.

Geographic entities mentioned:
surface_form: Lake Beechey
instance_of: Lake
countries: Canada
coordinates: lat: 65.4167
lon: -106.833
The river turns northeast, takes in the left tributary Bullen River, and reaches Pelly Lake at an elevation of. It flows east through, in immediate succession: Upper Garry Lake, where it takes in the right tributary Morse River; Garry Lake; Lower Garry Lake; Buliard Lake; Upper MacDougall Lake; and Lower MacDougall Lake.

Geographic entities mentioned:
surface_form: Garry Lake
instance_of: Lake
countries: Canada
coordinates: lat: 65.966667
lon: -100.3
The river is long to the Muskox Lake outlet, though the river continues further upstream to its source. Like the Coppermine, Hood, Dubawnt or Kazan, which are other large rivers in this part of Canada, it is navigable only by experienced canoeists because of the numerous and challenging 83 rapids. The entire river is above the tree line. History.

Geographic entities mentioned:
surface_form: Coppermine
instance_of: Watercourse
countries: Canada
coordinates: lat: 67.816666666667
lon: -115.06666666667
The river can also be travelled to its end, where a boat tow can be arranged to the Inuit community of Gjoa Haven, which has commercial air service back to Yellowknife. If planning a canoeing trip on the river, due to the weather, it is generally recommended to have navigated Garry Lake by August 8, the mark of the seasonal change to worse weather.

Geographic entities mentioned:
surface_form: Garry Lake
instance_of: Lake
countries: Canada
coordinates: lat: 65.966667
lon: -100.3
Gen. George Stoneman. In August, Wheeler's corps crossed the Chattahoochee River in an attempt to destroy the railroad Sherman was using to supply his force from Chattanooga. Wheeler's men captured the town of Dalton, but he was unable to defeat the Union garrison protected in a nearby fort. Wheeler then took his men into East Tennessee, crossing the Tennessee River above Knoxville.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Stones Peak. Stones Peak is a mountain summit located in Larimer County, Colorado. It is situated in Rocky Mountain National Park, one mile east of the Continental Divide and west of the community of Estes Park. Stones Peak is part of the Front Range which is a subrange of the Rocky Mountains. Precipitation runoff from the mountain drains into tributaries of the Big Thompson River.

Geographic entities mentioned:
surface_form: rocky mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9727
lon: -74.3732
surface_form: rocky mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.7955
lon: -79.1808
surface_form: rocky mountain
instance_of: Landform
countries: United States
coordinates: lat: 41.7958
lon: -71.055
surface_form: rocky mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0918
lon: -74.2151
Stones Peak. Stones Peak is a mountain summit located in Larimer County, Colorado. It is situated in Rocky Mountain National Park, one mile east of the Continental Divide and west of the community of Estes Park. Stones Peak is part of the Front Range which is a subrange of the Rocky Mountains. Precipitation runoff from the mountain drains into tributaries of the Big Thompson River.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: stones peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.35443
lon: -105.72056
Stones Peak. Stones Peak is a mountain summit located in Larimer County, Colorado. It is situated in Rocky Mountain National Park, one mile east of the Continental Divide and west of the community of Estes Park. Stones Peak is part of the Front Range which is a subrange of the Rocky Mountains. Precipitation runoff from the mountain drains into tributaries of the Big Thompson River.

Geographic entities mentioned:
surface_form: stones peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.35443
lon: -105.72056
Climate. According to the Köppen climate classification system, Stones Peak is located in an alpine subarctic climate zone with cold, snowy winters, and cool to warm summers. Due to its altitude, it receives precipitation all year, as snow in winter and as thunderstorms in summer, with a dry period in late spring. This climate supports the Sprague Glacier on the southwest aspect of Stones Peak.

Geographic entities mentioned:
surface_form: stones peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.35443
lon: -105.72056
Mount Howard (Washington). Mount Howard is a prominent mountain summit located west of Lake Wenatchee in Chelan County of Washington state. Mount Howard is the highest point of Nason Ridge, and is northeast of Rock Mountain, which is second-highest. This peak is set approximately midway between Stevens Pass and Lake Wenatchee, on land managed by the Okanogan–Wenatchee National Forest.

Geographic entities mentioned:
surface_form: Lake Wenatchee
instance_of: Lake
countries: United States
coordinates: lat: 47.82267
lon: -120.7772
surface_form: mount howard
instance_of: Mountain
countries: United States
coordinates: lat: 45.261
lon: -117.179
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
surface_form: mount howard
instance_of: Mountain
countries: United States
coordinates: lat: 47.813888888889
lon: -120.95472222222
Mount Howard is the highest point of Nason Ridge, and is northeast of Rock Mountain, which is second-highest. This peak is set approximately midway between Stevens Pass and Lake Wenatchee, on land managed by the Okanogan–Wenatchee National Forest. Precipitation runoff from the peak drains into tributaries of the Wenatchee River.

Geographic entities mentioned:
surface_form: Lake Wenatchee
instance_of: Lake
countries: United States
coordinates: lat: 47.82267
lon: -120.7772
The history of the formation of the Cascade Mountains dates back millions of years ago to the late Eocene Epoch. With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted. Glacier Peak, a stratovolcano that is north of Mt. Howard, began forming in the mid-Pleistocene.

Geographic entities mentioned:
surface_form: Glacier Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: mt. howard
instance_of: Mountain
countries: United States
coordinates: lat: 45.261
lon: -117.179
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.14972222
lon: -109.84944444
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.155013
lon: -117.293429
surface_form: mt. howard
instance_of: Mountain
countries: United States
coordinates: lat: 47.813888888889
lon: -120.95472222222
Mount Howard (Washington). Mount Howard is a prominent mountain summit located west of Lake Wenatchee in Chelan County of Washington state. Mount Howard is the highest point of Nason Ridge, and is northeast of Rock Mountain, which is second-highest. This peak is set approximately midway between Stevens Pass and Lake Wenatchee, on land managed by the Okanogan–Wenatchee National Forest.

Geographic entities mentioned:
surface_form: mount howard
instance_of: Mountain
countries: United States
coordinates: lat: 45.261
lon: -117.179
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: mount howard (washington)
instance_of: Mountain
countries: United States
coordinates: lat: 47.813888888889
lon: -120.95472222222
Mount Howard (Washington). Mount Howard is a prominent mountain summit located west of Lake Wenatchee in Chelan County of Washington state. Mount Howard is the highest point of Nason Ridge, and is northeast of Rock Mountain, which is second-highest. This peak is set approximately midway between Stevens Pass and Lake Wenatchee, on land managed by the Okanogan–Wenatchee National Forest.

Geographic entities mentioned:
surface_form: mount howard
instance_of: Mountain
countries: United States
coordinates: lat: 45.261
lon: -117.179
surface_form: rock mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.799444444444
lon: -120.97444444444
surface_form: mount howard
instance_of: Mountain
countries: United States
coordinates: lat: 47.813888888889
lon: -120.95472222222
Howard, began forming in the mid-Pleistocene. In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago. Gneissic rock of the Nason Terrane is exposed on Mt. Howard. During the Pleistocene period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured and shaped the landscape.

Geographic entities mentioned:
surface_form: mt. howard
instance_of: Mountain
countries: United States
coordinates: lat: 45.261
lon: -117.179
surface_form: mt. howard
instance_of: Mountain
countries: United States
coordinates: lat: 47.813888888889
lon: -120.95472222222
Uplift and faulting in combination with glaciation have been the dominant processes which have created the tall peaks and deep valleys of the North Cascades area. Climate. Lying east of the Cascade crest, the area around Mt. Howard is a bit drier than areas to the west. Summers can bring warm temperatures and occasional thunderstorms.

Geographic entities mentioned:
surface_form: mt. howard
instance_of: Mountain
countries: United States
coordinates: lat: 45.261
lon: -117.179
surface_form: mt. howard
instance_of: Mountain
countries: United States
coordinates: lat: 47.813888888889
lon: -120.95472222222
74th (Y) Division was withdrawn into reserve at Biddu and there was another pause in operations while the EEF's engineers carried out a large amount of roadbuilding. Jericho was captured in late February and the EEF advanced to the escarpment overlooking the Jordan Valley. 74th (Y) Division was then brought up for the next operation, against Tell 'Asur.

Geographic entities mentioned:
surface_form: Jordan Valley
instance_of: Valley
countries: Jordan
coordinates: lat: 32.317222
lon: 35.57
It is significant in Egyptology as one of the two most important, and the most famous, autobiographical inscriptions of Old Kingdom officials. His name sometimes spelled as Herkhuf, Horkhuf, or Hirkhuf, all that is known of his life comes from the inscriptions in his tomb at Qubbet el-Hawa on the west bank of the Nile at Aswan, near the First Cataract of the Nile. He was a native of Elephantine.

Geographic entities mentioned:
surface_form: Qubbet el-Hawa
instance_of: Mountain
countries: Egypt
coordinates: lat: 24.1025
lon: 32.88888889
Harrow, Pennsylvania. Harrow is an unincorporated community in Nockamixon Township, Bucks County, Pennsylvania, United States. The community is located just northeast of Lake Nockamixon. It is drained by the Tohickon Creek into the Delaware River. It is served by Routes 412, 563, and 611.

Geographic entities mentioned:
surface_form: Lake Nockamixon
instance_of: Lake
countries: United States
coordinates: lat: 40.465488888889
lon: -75.220988888889
Supported by Vologases, Tiridates sent flying columns to raid the Romans far and wide in 58. Corbulo responded by using the same tactics. He also emboldened the Roman client-kings Antiochus IV of Commagene, Pharasmanes I, and the Moschi tribes to attack outlying areas of Armenia.

Geographic entities mentioned:
surface_form: Moschi
instance_of: Mountain
countries: Georgia
Armenia
The term &quot;Devil's Lake&quot; is a misinterpretation of the Ho-Chunk name Te Wakącąk or Te Wakącągara. Day-wa-kahn-chunk-gera, which better translates to &quot;Sacred Lake&quot; or &quot;Spirit Lake.&quot; Spirit Lake is highly significant in Ho-Chunk oral history, and voices of spirits were often claimed to be heard during the celebrations. History.

Geographic entities mentioned:
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 47.94
lon: -116.9
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 47.94
lon: -116.9
surface_form: spirit
instance_of: Lake
countries: United States
coordinates: lat: 46.273055555556
lon: -122.135
surface_form: spirit
instance_of: Lake
countries: United States
coordinates: lat: 46.273055555556
lon: -122.135
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4739
lon: -95.1018
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4739
lon: -95.1018
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 45.38055556
lon: -90.13694444
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 45.38055556
lon: -90.13694444
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 44.49305556
lon: -97.60861111
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 44.49305556
lon: -97.60861111
Many Native tribes throughout Wisconsin inhabited the lands. They called the lake various different names, such as &quot;Tewakakak&quot; or &quot;Minnewaukan&quot;, which translate to spirit lake in various Native American Languages. Devil's Lake was originally a gorge of the Wisconsin River prior to the last ice age.

Geographic entities mentioned:
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 47.94
lon: -116.9
surface_form: spirit
instance_of: Lake
countries: United States
coordinates: lat: 46.273055555556
lon: -122.135
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4739
lon: -95.1018
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 45.38055556
lon: -90.13694444
surface_form: spirit lake
instance_of: Lake
countries: United States
coordinates: lat: 44.49305556
lon: -97.60861111
Devil's Lake (Wisconsin). Devil's Lake is a lake in Sauk County, Wisconsin, United States. It is part of the South Range of the Baraboo Range, about south of the city of Baraboo, Wisconsin. It has no surface outlets, so by some definitions, it is endorheic; however, it possibly drains by underground channels into the Baraboo River, which would make the lake cryptorheic.

Geographic entities mentioned:
surface_form: devil's lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4181
lon: -89.7319
It has no surface outlets, so by some definitions, it is endorheic; however, it possibly drains by underground channels into the Baraboo River, which would make the lake cryptorheic. The lake is one of the primary attractions of Devil's Lake State Park. It is also a popular recreation destination for watercraft, fishing, hiking, and climbing. Name.

Geographic entities mentioned:
surface_form: devil's lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4181
lon: -89.7319
It is also a popular recreation destination for watercraft, fishing, hiking, and climbing. Name. Devil's Lake was so named because it is situated in a deep chasm that was thought to have no visible inlet or outlet. However, the Koshawago Spring, originating from the Koshawago Creek, provides an inlet to the lake on the southwest side.

Geographic entities mentioned:
surface_form: devil's lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4181
lon: -89.7319
Name. Devil's Lake was so named because it is situated in a deep chasm that was thought to have no visible inlet or outlet. However, the Koshawago Spring, originating from the Koshawago Creek, provides an inlet to the lake on the southwest side. The term &quot;Devil's Lake&quot; is a misinterpretation of the Ho-Chunk name Te Wakącąk or Te Wakącągara.

Geographic entities mentioned:
surface_form: devil's lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4181
lon: -89.7319
Wildlife. Devil's Lake is home to a diverse selection of wildlife. Naturally occurring fish include bass and panfish, while walleye, northern pike, and trout are stocked by the Wisconsin DNR. Depending on the season, many types of birds can also be seen on the banks of Devil's Lake. Some of the more commonly seen birds include loons, herons, geese, and ducks.

Geographic entities mentioned:
surface_form: devil's lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4181
lon: -89.7319
Depending on the season, many types of birds can also be seen on the banks of Devil's Lake. Some of the more commonly seen birds include loons, herons, geese, and ducks. The northern water snake can also be spotted swimming around Devil's Lake. Although the snake is not venomous, it can be aggressive if it feels endangered. Water quality.

Geographic entities mentioned:
surface_form: devil's lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4181
lon: -89.7319
The northern water snake can also be spotted swimming around Devil's Lake. Although the snake is not venomous, it can be aggressive if it feels endangered. Water quality. Swimmer's itch (cercarial dermatitis) is a common problem at Devil's Lake, most apparent during the summer months. It is caused by a flatworm parasite hosted by snails.

Geographic entities mentioned:
surface_form: devil's lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4181
lon: -89.7319
At what is now the southern end of the lake, the river turned from a southerly direction to an easterly direction. During the ice age, a lobe of the glacier passed to the east of the Baraboo Hills and came up the river valley. It deposited materials and then melted, leaving a terminal moraine blocking the river, forming an earthen dam. Another moraine was deposited at the north end of the lake.

Geographic entities mentioned:
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
Geography. The municipality encompassed the Romsdalen valley (which follows the Rauma River) from the Oppland county border to the inner part of the Romsdal Fjord at Åndalsnes, as well as some smaller side valleys. The original municipality of Grytten was almost identical to the present-day Rauma Municipality, plus the southern part of Veøy Municipality (south of the Langfjorden).

Geographic entities mentioned:
surface_form: Romsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 62.447222222222
lon: 7.8333333333333
The original municipality of Grytten was almost identical to the present-day Rauma Municipality, plus the southern part of Veøy Municipality (south of the Langfjorden). The highest point in the municipality was the tall mountain Puttegga.

Geographic entities mentioned:
surface_form: Puttegga
instance_of: Mountain
countries: Norway
coordinates: lat: 62.214722222222
lon: 7.6913888888889
states of North Carolina and Virginia. In Person County, North Carolina the Hyco River is impounded by a dam, forming Hyco Lake. The main part of the river flows through Allensville, North Carolina (a township of Roxboro), on Gentry's Ridge and Mill Creek roads as it flows into Virginia townships such as Alton, Virginia, and Cluster Springs, Virginia, then combining with the Dan River.

Geographic entities mentioned:
surface_form: Hyco Lake
instance_of: Lake
countries: United States
coordinates: lat: 36.512777777778
lon: -79.046944444444
Breidvågnipa Peak. Breidvågnipa Peak () is a peak, high, rising southeast of Mount Hiroe on the coast of Queen Maud Land, Antarctica. It was mapped by Norwegian cartographers from air photos taken by the Lars Christensen Expedition, 1936–37, and named &quot;Breidvågnipa&quot; (the &quot;broad bay peak&quot;) in association with nearby Breidvåg Bight.

Geographic entities mentioned:
surface_form: Mount Hiroe
instance_of: Mountain
coordinates: lat: -69.35
lon: 39.7833
surface_form: breidvågnipa peak
instance_of: Mountain
coordinates: lat: -69.35
lon: 39.8
Breidvågnipa Peak. Breidvågnipa Peak () is a peak, high, rising southeast of Mount Hiroe on the coast of Queen Maud Land, Antarctica. It was mapped by Norwegian cartographers from air photos taken by the Lars Christensen Expedition, 1936–37, and named &quot;Breidvågnipa&quot; (the &quot;broad bay peak&quot;) in association with nearby Breidvåg Bight.

Geographic entities mentioned:
surface_form: breidvågnipa
instance_of: Mountain
coordinates: lat: -69.35
lon: 39.8
Dark Mountain. Dark Mountain, formerly also known as Black Mountain, is a mountain in the Tanzilla Plateau of the Northern Interior of British Columbia, Canada, located northeast of the settlement of Dease Lake, near Cry Lake. Before 1937 Dark Mountain was known as Black Mountain.

Geographic entities mentioned:
surface_form: Tanzilla Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.3667
lon: -130.367
surface_form: dark mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 58.635305555556
lon: -129.43919444444
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Dark Mountain. Dark Mountain, formerly also known as Black Mountain, is a mountain in the Tanzilla Plateau of the Northern Interior of British Columbia, Canada, located northeast of the settlement of Dease Lake, near Cry Lake. Before 1937 Dark Mountain was known as Black Mountain.

Geographic entities mentioned:
surface_form: dark mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 58.635305555556
lon: -129.43919444444
Juma people. The Júma are an Indigenous people of Brazil, who live in the Terra Indígena Juma in the Amazonas, along the Mucuim River, a tributary of Rio Açuã. Name. The Júma are also known as Kagwahibm, Kagwahiph, Kagwahiv, Kavahiva, Kawahip, Kawaib, and Yumá people. Population. In the 18th century, the Juma numbered between 12,000–15,000 people. The Juma numbered 300 in 1940.

Geographic entities mentioned:
surface_form: Mucuim River
instance_of: Watercourse
countries: Brazil
coordinates: lat: -6.56009
lon: -64.30631
After the war, Kiepenheuer benefited from his close connections with researchers all over Europe and managed to slowly establish a scientific network for solar observations. Together with the solar telescopes at the Schauinsland, Kiepenheuer established the Fraunhofer Institute near Freiburg in 1943. He was able to keep the solar telescopes in Schauinsland after the Second World War.

Geographic entities mentioned:
surface_form: Schauinsland
instance_of: Mountain
countries: Germany
coordinates: lat: 47.911111111111
lon: 7.8994444444444
Career. When he returned from Germany, he was employed by Norwegian Water Resources and Energy Directorate (&quot;Kanalvæsenet&quot;), where he researched the possibility of a canal in Tyrifjorden. Blix also periodically maintained a private practice as an architect and designed several villas and hotels.

Geographic entities mentioned:
surface_form: Tyrifjorden
instance_of: Lake
countries: Norway
coordinates: lat: 60.033333333333
lon: 10.133333333333
Severe thunderstorms also formed in Western North Texas before impacting the western and central parts of Oklahoma. Strong winds overturned two trailers and caused heavy sand damage to cars in Coachella Valley in California. Multiple hailstorms caused major damage in Sullivan County, New Hampshire.

Geographic entities mentioned:
surface_form: Coachella Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.72
lon: -116.2
In 2017, Perrier oversaw Amundi's acquisition of Pioneer Investments, a subsidiary of Unicredit. Early life and education. Yves Perrier was born in 1954 to a family from the Arve Valley in the Haute-Savoie region of France. His father is a craftsman who works in the field of bar turning, an activity that has a long history in the region.

Geographic entities mentioned:
surface_form: Arve Valley
instance_of: Valley
countries: France
coordinates: lat: 46.067
lon: 6.5
Gian Carlo Grassi. Gian Carlo Grassi (Condove, October 14, 1946 - Monte Bove, April 1, 1991) was an Italian mountaineer and mountain guide. He was a pioneer of ice climbing in Italy in the 1980s, making many first ascents among waterfalls and in high mountains. Biography.

Geographic entities mentioned:
surface_form: Monte Bove
instance_of: Mountain
countries: Italy
coordinates: lat: 42.936
lon: 13.1903
Biography. Originally from Val di Susa, in the 1970s he was part of the “New Morning” movement, where he associated with, among others, and Danilo Galante. These were the years of climbing routes in Orco Valley, on the Caporal and the Sergent, and bouldering on erratic blocks in the lower Val di Susa.

Geographic entities mentioned:
surface_form: Orco Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.417
lon: 7.467
During these years, he met and together they accomplished a series of significant ascents in the Mont Blanc massif. In 1978, they opened a new goulotte on the north face of the Aiguille Verte and the &quot;Ypercouloir&quot; on the south face of the Grandes Jorasses.

Geographic entities mentioned:
surface_form: Aiguille Verte
instance_of: Mountain
countries: France
coordinates: lat: 45.934722222222
lon: 6.97
surface_form: Grandes Jorasses
instance_of: Mountain
countries: Italy
France
coordinates: lat: 45.866666666667
lon: 6.9833333333333
He also climbed abroad: in California, Canada, the Andes, Patagonia, and the Himalayas. In 1984, with Renato Casarotto and Guido Ghigo, he climbed &quot;Pomme d’Or&quot; in Quebec (180 meters of stalactite), &quot;Polar Circus&quot;, and &quot;Slipstream&quot; (a 900-meter icefall) in the Canadian Rockies. In 1985, with Mauro Rossi, he repeated the &quot;Supercanaleta&quot; route on Fitz Roy.

Geographic entities mentioned:
surface_form: Fitz Roy
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -49.271388888889
lon: -73.043333333333
Small green utaka. The small green utaka (&quot;Nyassachromis leuciscus&quot;) is a species of cichlid endemic to Lake Malawi where it prefers areas with a sandy substrate. This species can reach a length of TL. It can also be found in the aquarium trade.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
The company received a 37% discount to charges in its first year of operation, decreasing to 16% and 8% in the second and third years. The initial service was criticised for the lack of a stop in the Susa Valley, in the Italian Alps. Among those campaigning for a stop were Alberto Cirio, the Piedmontese president, and Marco Gabusi, the regional councillor for infrastructure and transport.

Geographic entities mentioned:
surface_form: Susa Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.133333333333
lon: 7.05
It flows northwards into the Kolyuchinskaya Bay, Chukchi Sea. It is long, and has a drainage basin of. Mount Ioni and Ioni lake are located close to it to the east in mid course. This river and its basin belong to the Chukotka Autonomous Okrug administrative region of Russia.

Geographic entities mentioned:
surface_form: Ioni
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 65.9
lon: -173.65
The underparts are pale buffy to whitish, and the throat and cheeks are whitish. The tail is brown, often with a black tip, and the feet/hands are blackish. Melanistic individuals are known from the Kaghan Valley in Pakistan. The white-bellied giant flying squirrel is medium-large in size, with measurements in the mid to upper range of those reported for the red giant flying squirrel.

Geographic entities mentioned:
surface_form: Kaghan Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 34.833333
lon: 73.516667
The metre gauge Lugano–Ponte Tresa Railway (FLP) has a separate station at Lugano FLP railway station across the station forecourt from the main line station. The station is situated on a hillside to the west of the city centre, overlooking the city and Lake Lugano, and the funicular provides a direct link from the station to the city centre below.

Geographic entities mentioned:
surface_form: Lake Lugano
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46
lon: 9
It was judged there were above a thousand people; to whom I declared God's everlasting truth and Word of life freely and largely for about the space of three hours. Because of Fox's preaching there, the site is sometimes called &quot;Fox's Pulpit.&quot; A plaque on the rock there commemorates the event, which is sometimes considered the beginning of the Friends movement.

Geographic entities mentioned:
surface_form: fox's pulpit
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.3391
lon: -2.60442
Firbank Fell. Firbank Fell is a hill in Cumbria between the towns of Kendal and Sedbergh that is renowned as a place where George Fox, the founder of the Religious Society of Friends (Quakers), preached. While others were gone to dinner, I went to a brook, got a little water, and then came and sat down on the top of a rock hard by the chapel.

Geographic entities mentioned:
surface_form: firbank fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.3391
lon: -2.60442
Seewlisee. __NOTOC__
Seewlisee (or &quot;Seewli&quot;) is a lake in Uri, Switzerland at an elevation of 2028 m. Its surface area is. The lake lies at the foot of the Gross Windgällen. The lake can be reached by foot in 2–3 hours from the cable car Silenen-Chilcherbergen.

Geographic entities mentioned:
surface_form: Gross Windgällen
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.807222222222
lon: 8.7322222222222
surface_form: gross windgällen
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.807222222222
lon: 8.7322222222222
Seewlisee. __NOTOC__
Seewlisee (or &quot;Seewli&quot;) is a lake in Uri, Switzerland at an elevation of 2028 m. Its surface area is. The lake lies at the foot of the Gross Windgällen. The lake can be reached by foot in 2–3 hours from the cable car Silenen-Chilcherbergen.

Geographic entities mentioned:
surface_form: seewli
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.811111111111
lon: 8.7144444444444
surface_form: seewlisee
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.811111111111
lon: 8.7144444444444