Sarmila/GeoWiki-Features huggingface dataset:
Bibbiena. Bibbiena () is a town and &quot;comune&quot; in the province of Arezzo, Tuscany (Italy), the largest town in the valley of Casentino. It is located from Florence, from Arezzo, from Siena, and from the Sanctuary of La Verna. There are approximately 11,833 inhabitants
The town is on top of a hill at an elevation of. Geography.

Geographic entities mentioned:
surface_form: Casentino
instance_of: Valley
countries: Italy
coordinates: lat: 43.7
lon: 11.816666666667
Bibbiena. Bibbiena () is a town and &quot;comune&quot; in the province of Arezzo, Tuscany (Italy), the largest town in the valley of Casentino. It is located from Florence, from Arezzo, from Siena, and from the Sanctuary of La Verna. There are approximately 11,833 inhabitants
The town is on top of a hill at an elevation of. Geography.

Geographic entities mentioned:
surface_form: La Verna
instance_of: Mountain
countries: Italy
coordinates: lat: 43.707
lon: 11.931
There are approximately 11,833 inhabitants
The town is on top of a hill at an elevation of. Geography. The municipality of Bibbiena is located in the heart of the Casentino, the valley in which the first stretch of the Arno river flows which, after having crossed the Valdarno (Upper, Middle and Lower), flows into the Tyrrhenian Sea near Pisa.

Geographic entities mentioned:
surface_form: Casentino
instance_of: Valley
countries: Italy
coordinates: lat: 43.7
lon: 11.816666666667
surface_form: Valdarno
instance_of: Valley
countries: Italy
coordinates: lat: 43.566666666667
lon: 11.533333333333
Events. The &quot;Sagra delle Sagre&quot; takes place every year in Bibbiena. In the historic center of the town many of the Casentino valley festivals gather for a day in June (Cetica, Chiusi della Verna, Corezzo, Faltona, Partina, Pratovecchio Stia, Premilcuore, Rimbocchi, San Piero in Frassino, Subbiano). Fractions.

Geographic entities mentioned:
surface_form: Casentino
instance_of: Valley
countries: Italy
coordinates: lat: 43.7
lon: 11.816666666667
Cali River. The Cali River is a river of western Colombia. It flows through the city of Cali and drains into the Cauca River. Its headwaters are in the Farallones de Cali of the Cordillera Occidental.

Geographic entities mentioned:
surface_form: Farallones de Cali
instance_of: Mountain
countries: Colombia
coordinates: lat: 3.34
lon: -76.695833333333
surface_form: cali
instance_of: Watercourse
countries: Colombia
coordinates: lat: 3.50567
lon: -76.49216
Cali River. The Cali River is a river of western Colombia. It flows through the city of Cali and drains into the Cauca River. Its headwaters are in the Farallones de Cali of the Cordillera Occidental.

Geographic entities mentioned:
surface_form: cali river
instance_of: Watercourse
countries: Colombia
coordinates: lat: 3.50567
lon: -76.49216
Cali River. The Cali River is a river of western Colombia. It flows through the city of Cali and drains into the Cauca River. Its headwaters are in the Farallones de Cali of the Cordillera Occidental.

Geographic entities mentioned:
surface_form: cali
instance_of: Watercourse
countries: Colombia
coordinates: lat: 3.50567
lon: -76.49216
Merume River. The Merume River is a river of Guyana, a tributary of the Kamarang River. Merume is also the name of a nearby mountain, which is 30 miles east of Mount Roraima. Director Creek is a tributary of Merume River. First Falls is a feature of the river which also limits travel by boat. Merumite was discovered in 1937 appearing as black grains among diamonds and gold in the river gravel.

Geographic entities mentioned:
surface_form: Mount Roraima
instance_of: Mountain
countries: Venezuela
Brazil
coordinates: lat: 5.141944444444444
lon: -60.76416666666667
Headquartered at JHQ Rheindahlen in West Germany and commanded by a General it consisted in peacetime of British I Corps and support troops. In the event of war with the Warsaw Pact the Commander-in-Chief of BAOR would have assumed command of NATO's Northern Army Group (NORTHAG), which was tasked with defending Northern Germany up to the river Elbe.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
On 27 November 1989 Peter Inge became the commander of NATO's Northern Army Group and Commander-in-Chief, British Army of the Rhine in Germany with the local rank of general; he succeeded General Brian Kenny. I British Corps. The area 1 BR Corps had to defend lay between Hanover to the North and Kassel to the South and extended from the Inner German Border to the Upper Weser Valley.

Geographic entities mentioned:
surface_form: Upper Weser Valley
instance_of: Valley
countries: Germany
coordinates: lat: 51.85
lon: 9.46667
Mondon. Mondon () is a commune in the Doubs department in the Bourgogne-Franche-Comté region in eastern France. Geography. Mondon lies south of Rougemont on a sunny slope. Above the village, there is a view toward the Vosges mountains and the Ballon de Servance.

Geographic entities mentioned:
surface_form: Ballon de Servance
instance_of: Mountain
countries: France
coordinates: lat: 47.83
lon: 6.79278
He was a pupil at Bedales School at its original location at Lindfield, West Sussex, and then from 1900 at its new site near Petersfield, Hampshire. He was head boy and left in 1901. He was then apprenticed to the family engineering firm, Hathorn Davey of Leeds. He erected pumping engines in the Lea Valley around 1903–4 and worked in Germany. Arts and Crafts.

Geographic entities mentioned:
surface_form: Lea Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69
lon: -0.01
Name. &quot;Named for U.S. Rep. David Skaggs who represented Colorado's 2nd Congressional District from 1987–99, the Skaggs Research Center was constructed at the base of the Flatirons rock formation in Boulder, Colorado on land already owned by the United States Department of Commerce (DOC).

Geographic entities mentioned:
surface_form: Flatirons
instance_of: Mountain
countries: United States
coordinates: lat: 39.9883
lon: -105.293
In 1855 he was also a member, representing the same province, of the. In his legislative work, he stood out for presenting reform projects for the army and for the defense of the Indians. He was also Mayor of Lima and in that role, he increased the waters of the Rímac River. On June 29, 1864, under the government of Juan Antonio Pezet, he was appointed prefect of the department of Cuzco.

Geographic entities mentioned:
surface_form: Rímac River
instance_of: Watercourse
countries: Peru
coordinates: lat: -12.032222222222
lon: -77.141111111111
Großer Segeberger See. Großer Segeberger See is a lake in Kreis Segeberg, Schleswig-Holstein, Germany.

Geographic entities mentioned:
surface_form: großer segeberger see
instance_of: Lake
countries: Germany
coordinates: lat: 53.948333333333
lon: 10.323055555556
He had to struggle with local bureaucracy, and at one pointed offered his resignation to the ministry, which was refused. The company was governed by the &quot;Cahier des charges&quot; agreement of 12 March 1925 which obliged it to provide service on a fixed timetable on the Congo and Kasai River, and on the navigable tributaries of these rivers.

Geographic entities mentioned:
surface_form: Kasai River
instance_of: Watercourse
countries: Angola
Democratic Republic of the Congo
coordinates: lat: -10.9603
lon: 19.3156
Sabkha Zamoul. Sabkha Zamoul is a salt lake situated in the northeastern region of Algeria, within the administrative boundaries of the Oum El Bouaghi Province and the Ouled Zouaï municipality. It has been partially exploited for salt extraction and represents the largest nesting area for flamingos in the Mediterranean.

Geographic entities mentioned:
surface_form: sabkha zamoul
instance_of: Lake
countries: Algeria
France
coordinates: lat: 35.875003
lon: 6.547165
This site was classified as a Ramsar site in 2004. The southern shore of the lake is situated at a distance of 200 meters from the municipality of Ouled Zouaï. The districts of Souk Naamane and Aïn Kechra District in Oum El Bouaghi assume administrative responsibility for Sabkha Zamoul. Climate.

Geographic entities mentioned:
surface_form: sabkha zamoul
instance_of: Lake
countries: Algeria
France
coordinates: lat: 35.875003
lon: 6.547165
Fan Changsheng. Fan Changsheng (Fàn Chángshēng) (died 318) was a Taoist priest and leader who was instrumental in the establishment of the Cheng-Han state during the Sixteen Kingdoms era in China. He led a Taoist community of over one thousand families on Mount Qingcheng, Sichuan. During a critical famine, Fan Changsheng provided Li Xiong's army with food from his community's bounty.

Geographic entities mentioned:
surface_form: Mount Qingcheng
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 31.002
lon: 103.605
After the elimination of the two downhills scheduled in November on the &quot;Gran Becca&quot; course on the Matterhorn from the 2025 schedule, the first race of the season in this discipline did not take place on 14 December in Beaver Creek, Colorado, United States.

Geographic entities mentioned:
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
Of the four major lake basins in Leon County - Lake Jackson, Lake Iamonia, Lake Miccosukee, and Lake Lafayette - the Lake Lafayette basin is the most intensively developed; it is also considered the most modified lake basin in all of northern Florida, since it is no longer functioning in a natural fashion due to human effects.

Geographic entities mentioned:
surface_form: Lake Iamonia
instance_of: Lake
countries: United States
coordinates: lat: 30.633119444444
lon: -84.177672222222
surface_form: Lake Miccosukee
instance_of: Lake
countries: United States
coordinates: lat: 30.5707
lon: -83.9791
He did not actually graduate until 1948 because he interrupted his studies to join the army. He served in the Second World War in the 20th Armored Division, landed in Europe in January 1945 and experienced bitter fighting in the Rhine valley. His division was involved with the Liberation of Dachau concentration camp on April 29, 1945. Foreign Service.

Geographic entities mentioned:
surface_form: Rhine valley
instance_of: Valley
In summer it is a relatively easy walk up to the summit from there. The Corral de la Veleta or Corral del Veleta glacier, at 37° N the southernmost glacier in Europe, disappeared in 1913. The IRAM 30m telescope is located on the slopes of Pico Veleta, at an elevation of 2920 m.

Geographic entities mentioned:
surface_form: pico veleta
instance_of: Mountain
countries: Spain
coordinates: lat: 37.056027777778
lon: -3.3656888888889
surface_form: veleta
instance_of: Mountain
countries: Spain
coordinates: lat: 37.056027777778
lon: -3.3656888888889
Veleta (Sierra Nevada). Veleta (from the Arab word &quot;Balata&quot;, meaning cliff) or Pico del Veleta is the third highest peak of the Iberian Peninsula and the second highest of the Sierra Nevada. Its height is given variously as, and. The mountain can be seen from the city of Granada. Veleta's northern slopes are home to the Sierra Nevada Ski Station.

Geographic entities mentioned:
surface_form: pico del veleta
instance_of: Mountain
countries: Spain
coordinates: lat: 37.056027777778
lon: -3.3656888888889
surface_form: veleta
instance_of: Mountain
countries: Spain
coordinates: lat: 37.056027777778
lon: -3.3656888888889
surface_form: veleta
instance_of: Mountain
countries: Spain
coordinates: lat: 37.056027777778
lon: -3.3656888888889
Veleta (Sierra Nevada). Veleta (from the Arab word &quot;Balata&quot;, meaning cliff) or Pico del Veleta is the third highest peak of the Iberian Peninsula and the second highest of the Sierra Nevada. Its height is given variously as, and. The mountain can be seen from the city of Granada. Veleta's northern slopes are home to the Sierra Nevada Ski Station.

Geographic entities mentioned:
surface_form: veleta
instance_of: Mountain
countries: Spain
coordinates: lat: 37.056027777778
lon: -3.3656888888889
It has since been closed to general traffic beyond Hoya de la Mora, just above the ski station. However, the road is still used by ski station employees, national park rangers, observatory staff, cyclists and walkers, and by a microbus service which takes hikers up to Posiciones del Veleta, a viewpoint 3,100 metres above sea level.

Geographic entities mentioned:
surface_form: veleta
instance_of: Mountain
countries: Spain
coordinates: lat: 37.056027777778
lon: -3.3656888888889
In summer it is a relatively easy walk up to the summit from there. The Corral de la Veleta or Corral del Veleta glacier, at 37° N the southernmost glacier in Europe, disappeared in 1913. The IRAM 30m telescope is located on the slopes of Pico Veleta, at an elevation of 2920 m.

Geographic entities mentioned:
surface_form: veleta
instance_of: Mountain
countries: Spain
coordinates: lat: 37.056027777778
lon: -3.3656888888889
surface_form: veleta
instance_of: Mountain
countries: Spain
coordinates: lat: 37.056027777778
lon: -3.3656888888889
Franca Glacier. Franca Glacier () named after Fernando E. Franca, is a glacier in Antarctica, flowing northeast into the head of Solberg Inlet, Bowman Coast, to the south of Houser Peak. The glacier was photographed from the air by the United States Antarctic Service, 1940, and the U.S. Navy, 1966.

Geographic entities mentioned:
surface_form: Houser Peak
instance_of: Mountain
coordinates: lat: -68.3667
lon: -65.55
Course. Davis Hollow begins in a valley in Benton Township. It flows southwest for a short distance before turning west for several tenths of a mile, crossing Pied Piper Road. The stream then turns southwest for a few tenths of a mile, leaving the valley and entering a plain. It then turns southwest and crosses Pennsylvania Route 487 after several tenths of a mile.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
However, the surficial geology in the area mainly consists of bedrock made of sandstone and shale as well as a glacial or resedimented till known as Wisconsinan Till. Some Wisconsinan Lag is present at the top of the valley. The surficial geology near the lower reaches of the stream mainly consists of alluvium, bedrock, alluvial terrace, Illinoian Lag, and a small patch of Illinoian Flow-Till.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Some Wisconsinan Lag is present at the top of the valley. The surficial geology near the lower reaches of the stream mainly consists of alluvium, bedrock, alluvial terrace, Illinoian Lag, and a small patch of Illinoian Flow-Till. In the valley of Davis Hollow, the Wisconsinan glacial terminus descends over the course of (per mile). Watershed. The watershed of Davis Hollow has an area of.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: davis hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.1718
lon: -76.3849
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
However, its source is in the quadrangle of Stillwater. History and etymology. Davis Hollow was entered into the Geographic Names Information System on August 2, 1979. Its identifier in the Geographic Names Information System is 1172989. Davis Hollow is an unnamed stream that takes the name of the valley it flows through. The valley is in turn likely named after a local farmer or landowner.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: davis hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.1718
lon: -76.3849
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Davis Hollow is an unnamed stream that takes the name of the valley it flows through. The valley is in turn likely named after a local farmer or landowner. According to Walter Brasch's 1982 book &quot;Columbia County Place Names&quot;, some maps list the valley of Davis Hollow as being in Fishing Creek Township, while others list it as being near Rohrsburg.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Davis Hollow is an unnamed stream that takes the name of the valley it flows through. The valley is in turn likely named after a local farmer or landowner. According to Walter Brasch's 1982 book &quot;Columbia County Place Names&quot;, some maps list the valley of Davis Hollow as being in Fishing Creek Township, while others list it as being near Rohrsburg.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: davis hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.1718
lon: -76.3849
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Davis Hollow. Davis Hollow is a tributary of Fishing Creek in Columbia County, Pennsylvania, in the United States. It is approximately long and flows through Benton Township. The watershed of the stream has an area of. The surficial geology in its vicinity mainly consists of alluvium, alluvial terrace, Wisconsinan Till, Wisconsinan Lag, Illinoian Flow-Till, and Illinoian Lag. Course.

Geographic entities mentioned:
surface_form: davis hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.1718
lon: -76.3849
The watershed of the stream has an area of. The surficial geology in its vicinity mainly consists of alluvium, alluvial terrace, Wisconsinan Till, Wisconsinan Lag, Illinoian Flow-Till, and Illinoian Lag. Course. Davis Hollow begins in a valley in Benton Township. It flows southwest for a short distance before turning west for several tenths of a mile, crossing Pied Piper Road.

Geographic entities mentioned:
surface_form: davis hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.1718
lon: -76.3849
It then turns southwest and crosses Pennsylvania Route 487 after several tenths of a mile. At this point, it turns south-southwest and reaches its confluence with Fishing Creek a short distance further downstream. Davis Hollow joins Fishing Creek upstream of its mouth. Geography and geology. The elevation near the mouth of Davis Hollow is above sea level.

Geographic entities mentioned:
surface_form: davis hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.1718
lon: -76.3849
Davis Hollow joins Fishing Creek upstream of its mouth. Geography and geology. The elevation near the mouth of Davis Hollow is above sea level. The elevation of the stream's source is between above sea level. There are two patches of alluvium, which contains stratified silt, sand, and gravel, near the upper reaches of Davis Hollow.

Geographic entities mentioned:
surface_form: davis hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.1718
lon: -76.3849
The elevation of the stream's source is between above sea level. There are two patches of alluvium, which contains stratified silt, sand, and gravel, near the upper reaches of Davis Hollow. However, the surficial geology in the area mainly consists of bedrock made of sandstone and shale as well as a glacial or resedimented till known as Wisconsinan Till.

Geographic entities mentioned:
surface_form: davis hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.1718
lon: -76.3849
In the valley of Davis Hollow, the Wisconsinan glacial terminus descends over the course of (per mile). Watershed. The watershed of Davis Hollow has an area of. The mouth of the stream is in the United States Geological Survey quadrangle of Benton. However, its source is in the quadrangle of Stillwater. History and etymology.

Geographic entities mentioned:
surface_form: davis hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.1718
lon: -76.3849
However, its source is in the quadrangle of Stillwater. History and etymology. Davis Hollow was entered into the Geographic Names Information System on August 2, 1979. Its identifier in the Geographic Names Information System is 1172989. Davis Hollow is an unnamed stream that takes the name of the valley it flows through. The valley is in turn likely named after a local farmer or landowner.

Geographic entities mentioned:
surface_form: davis hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.1718
lon: -76.3849
Drumcarban. Drumcarban () is a townland in County Cavan, Ireland, in the electoral division of the same name. The townland lies west of the R154 regional road. Neighbouring townlands are (clockwise, starting in the north): Cornamucklagh, Newtown, Drumbar, Coolnacarrick, Legaweel, Legaginny, Lackan Lower, and Drumcrow. On the boundary with the latter lies White Lough.

Geographic entities mentioned:
surface_form: White Lough
instance_of: Lake
countries: Ireland
coordinates: lat: 54.11333333
lon: -6.975
The importance of this day is all urban Pastusos, vented their repressed desires, since the cosmetic serves like a mask and at the same time to homogenize all social classes and ethnic groups as one great family settled on the slopes of Taita Urcunina.

Geographic entities mentioned:
surface_form: Taita Urcunina
instance_of: Mountain
countries: Colombia
coordinates: lat: 1.2166666666667
lon: -77.366666666667
Rural Culture & Cuy's Festival (7 January). This day is devoted to &quot;Remate&quot; (Finish) the Carnival with the celebration of &quot;Cuy's Day (Guinea Pig's Day)&quot; when locals and tourists delight the typical dish of the region, also many of them visit the near Guamuez Lake, and Obonuco and Catambuco rural fairs. The &quot;Artisans&quot; or &quot;Carnival Cultores&quot;.

Geographic entities mentioned:
surface_form: Guamuez Lake
instance_of: Lake
countries: Colombia
coordinates: lat: 1.1
lon: -77.152
He was one of the first correspondents to enter Paris after its liberation. MacVane continued to report from the Western Front until the fall of Berlin, and witnessed the meeting of American and Soviet forces at the Elbe near the end of the war. In 1946 MacVane convinced NBC to open up a bureau at the United Nations.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
However, the Samoa hotspot has features that resulted in enigma's for scientists. In the Samoa Islands, the easternmost island of Taʻū and the westernmost island of Savaiʻi have both erupted in the past 150 years. The most recent eruption on Savaiʻi occurred with Mount Matavanu (1905–1911) and on Taʻū in 1866.

Geographic entities mentioned:
surface_form: Mount Matavanu
instance_of: Mountain
countries: Samoa
coordinates: lat: -13.53333333
lon: -172.4
Paul Bucher. Paul Bucher (1887 – 1966) was a 20th-century French egyptologist. He worked in the Valley of the Kings where he deciphered and published inscriptions on the walls of the tombs KV34 (Thutmose III) and KV35 (Amenhotep II).

Geographic entities mentioned:
surface_form: Valley of the Kings
instance_of: Valley
countries: Egypt
coordinates: lat: 25.74025
lon: 32.602358
Yeysky District. Geography. Yeysky District is home to Lake Khanskoye. Administrative and municipal status. Within the framework of administrative divisions, Yeysky District is one of the thirty-eight in the krai.

Geographic entities mentioned:
surface_form: Lake Khanskoye
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 46.25
lon: 38.366666666667
Its range extends from Lira southwards to Entebbe and the Bwindi Impenetrable Forest. It has also been reported from Katera in the southern foothills of Mount Kenya, but this record is disputed. Some toads found between 1909 and 1912 near Alexandria in Egypt were originally identified as this species but may have been misidentified.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
Setting. The Rocky Mountains range in latitude between the Liard River in British Columbia (at 59° N) and the Rio Grande in New Mexico (at 35° N), and in height up to the highest peak, Mount Elbert at, taking in great valleys such as the Rocky Mountain Trench and San Luis Valley. Precipitation ranges from per year in the southern valleys to per year locally in the northern peaks.

Geographic entities mentioned:
surface_form: Mount Elbert
instance_of: Mountain
countries: United States
coordinates: lat: 39.1175
lon: -106.44527777778
surface_form: Rocky Mountain Trench
instance_of: Landform
Valley
countries: Canada
United States
coordinates: lat: 54.5
lon: -122.5
surface_form: San Luis Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.2
lon: -105.42
They still survived in some isolated pockets, however, and these populations have been used to restore the cutthroats to many areas in their historic range. One of the largest strongholds was, and is, Trappers Lake in Colorado's Flat Top Mountains. However, in 1984, brook trout invaded because a flood washed them downstream from nearby Crescent Lake.

Geographic entities mentioned:
surface_form: Trappers Lake
instance_of: Lake
countries: United States
coordinates: lat: 39.986
lon: -107.231
Yellowstone cutthroat trout. Yellowstone Lake in Yellowstone National Park, Wyoming, is the site of the most recent catastrophic species invasion. The Washington Post reported that the nonindigenous lake trout, a native of the Great Lakes, had been insidiously introduced into one of the nation's premier fisheries.

Geographic entities mentioned:
surface_form: Yellowstone Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.466666666667
lon: -110.36666666667
It traverses the Lazio, Marche, and Abruzzo regions of Italy. The source of the Tronto is in the Monti della Laga mountain range in the province of Rieti. Monte Gorzano is north of the source of the river and Lake Campotosto is south of the source of the river. The source of the river is near the place where the provinces of Rieti, Teramo, and L'Aquila meet.

Geographic entities mentioned:
surface_form: Monte Gorzano
instance_of: Mountain
countries: Italy
coordinates: lat: 42.617777777778
lon: 13.396388888889
For example, Byron is the title character in Lady Caroline's Gothic novel &quot;Glenarvon&quot; (1816). Byron was also the host of the celebrated ghost-story competition involving himself, Percy Bysshe Shelley, Mary Shelley, and John William Polidori at the Villa Diodati on the banks of Lake Geneva in the summer of 1816.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Bound to protect and lead his men as they march through Italy, from Ortona to the Hitler Line near Monte Cassino, Adam finds himself struggling to maintain the composure fitting a commander, as an inner &quot;horror&quot; gnaws at his conscience (Adam's reflections occasionally resemble those of Marlow in Joseph Conrad's &quot;Heart of Darkness&quot;).

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
Hibbertia kaputarensis. &quot;Hibbertia kaputarensis&quot; is a species of flowering plant in the family Dilleniaceae, and is endemic to the Mount Kaputar area. It is a shrub with low-lying branches, oblong to lance-shaped leaves and yellow flowers with forty to about one hundred stamens arranged around three carpels. Description.

Geographic entities mentioned:
surface_form: Mount Kaputar
instance_of: Mountain
countries: Australia
coordinates: lat: -30.214722222222
lon: 150.14527777778
Lac de Roy. Lac de Roy is a lake in Haute-Savoie, France. It is located 2 km west of le Praz de Lys (Praz de Lys-Sommand?) ski resort, in the commune of Taninges.

Geographic entities mentioned:
surface_form: lac de roy
instance_of: Lake
countries: France
coordinates: lat: 46.143333333333
lon: 6.5736111111111
Christopher Lake diversion. In 1959, construction began on Spruce River Dam and the Emma Lake diversion project. The dam increased the size of Anglin Lake while the diversion drew water out of Anglin Lake and pumped it into Emma Lake. The construction of the dam was completed in 1960 and the first leg of the diversion channel was completed one year later in 1961.

Geographic entities mentioned:
surface_form: Anglin Lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.6912
lon: -106.0074
surface_form: emma lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.6167
lon: -105.917
surface_form: anglin lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.6912
lon: -106.0074
The village of Christopher Lake is about from the south-eastern corner of the lake and Bell's Beach. Along much of the southern half of the lake are cabins, cottages, and summer homes. Description. Christopher Lake is in the Spruce River drainage basin, which is in the North Saskatchewan River watershed. There are no major creeks that flow into the lake as it has, at only, a small catchment area.

Geographic entities mentioned:
surface_form: spruce river
instance_of: Watercourse
countries: Canada
coordinates: lat: 53.21678
lon: -105.71771
surface_form: christopher lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.5656
lon: -105.8256
Christopher Creek flows out of the lake at the southern end near Bell's Beach and the village of Christopher Lake. Prior to the construction of the Emma and Christopher Lake diversions, neither lake connected directly to the Spruce River. Christopher Lake diversion. In 1959, construction began on Spruce River Dam and the Emma Lake diversion project.

Geographic entities mentioned:
surface_form: spruce river
instance_of: Watercourse
countries: Canada
coordinates: lat: 53.21678
lon: -105.71771
surface_form: christopher lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.5656
lon: -105.8256
Prior to the construction of the Emma and Christopher Lake diversions, neither lake connected directly to the Spruce River. Christopher Lake diversion. In 1959, construction began on Spruce River Dam and the Emma Lake diversion project. The dam increased the size of Anglin Lake while the diversion drew water out of Anglin Lake and pumped it into Emma Lake.

Geographic entities mentioned:
surface_form: spruce river
instance_of: Watercourse
countries: Canada
coordinates: lat: 53.21678
lon: -105.71771
surface_form: emma lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.6167
lon: -105.917
Christopher Creek is a partially natural run and partially constructed channel that flows out of Christopher Lake and heads south past Highway 263 towards the Little Red River Indian Reserve. It cuts through the eastern portion of the reserve and joins Spruce River just south of it. The Christopher Creek section of the Christopher Lake diversion project was completed in 1975. Parks and recreation.

Geographic entities mentioned:
surface_form: spruce river
instance_of: Watercourse
countries: Canada
coordinates: lat: 53.21678
lon: -105.71771
Christopher Lake (Saskatchewan). Christopher Lake is a recreational lake in the boreal forest ecozone in the Canadian province of Saskatchewan. It is south-east of Emma Lake and Great Blue Heron Provincial Park in the central part of the province in the District of Lakeland No. 521. Access to Christopher Lake is from Highways 953 and 263 and it is about north of the city of Prince Albert.

Geographic entities mentioned:
surface_form: blue
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.1
lon: -119.283
surface_form: emma lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.6167
lon: -105.917
This park has three hiking trails totalling about three kilometres for birdwatching and other wildlife viewing. In the winter, one of the trails is groomed for cross-country skiing and snowshoeing. The very northern tip of the lake is in Great Blue Heron Provincial Park, though there no facilities related to the park there. Fish species.

Geographic entities mentioned:
surface_form: blue
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.1
lon: -119.283
Christopher Lake (Saskatchewan). Christopher Lake is a recreational lake in the boreal forest ecozone in the Canadian province of Saskatchewan. It is south-east of Emma Lake and Great Blue Heron Provincial Park in the central part of the province in the District of Lakeland No. 521. Access to Christopher Lake is from Highways 953 and 263 and it is about north of the city of Prince Albert.

Geographic entities mentioned:
surface_form: christopher lake (saskatchewan)
instance_of: Lake
countries: Canada
coordinates: lat: 53.5656
lon: -105.8256
Christopher Lake (Saskatchewan). Christopher Lake is a recreational lake in the boreal forest ecozone in the Canadian province of Saskatchewan. It is south-east of Emma Lake and Great Blue Heron Provincial Park in the central part of the province in the District of Lakeland No. 521. Access to Christopher Lake is from Highways 953 and 263 and it is about north of the city of Prince Albert.

Geographic entities mentioned:
surface_form: christopher lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.5656
lon: -105.8256
It is south-east of Emma Lake and Great Blue Heron Provincial Park in the central part of the province in the District of Lakeland No. 521. Access to Christopher Lake is from Highways 953 and 263 and it is about north of the city of Prince Albert. The community of Bell's Beach is along the south-east corner of the lake and Clearsand Beach is along the western shore.

Geographic entities mentioned:
surface_form: christopher lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.5656
lon: -105.8256
The community of Bell's Beach is along the south-east corner of the lake and Clearsand Beach is along the western shore. The village of Christopher Lake is about from the south-eastern corner of the lake and Bell's Beach. Along much of the southern half of the lake are cabins, cottages, and summer homes. Description.

Geographic entities mentioned:
surface_form: christopher lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.5656
lon: -105.8256
There are no major creeks that flow into the lake as it has, at only, a small catchment area. The primary inflow for the lake is the man-made Christopher Lake diversion, which comes from neighbouring Emma Lake, and is part of the Emma Lake diversion project. Christopher Creek flows out of the lake at the southern end near Bell's Beach and the village of Christopher Lake.

Geographic entities mentioned:
surface_form: christopher lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.5656
lon: -105.8256
surface_form: emma lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.6167
lon: -105.917
surface_form: emma lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.6167
lon: -105.917
There are no major creeks that flow into the lake as it has, at only, a small catchment area. The primary inflow for the lake is the man-made Christopher Lake diversion, which comes from neighbouring Emma Lake, and is part of the Emma Lake diversion project. Christopher Creek flows out of the lake at the southern end near Bell's Beach and the village of Christopher Lake.

Geographic entities mentioned:
surface_form: christopher lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.5656
lon: -105.8256
Christopher Creek flows out of the lake at the southern end near Bell's Beach and the village of Christopher Lake. Prior to the construction of the Emma and Christopher Lake diversions, neither lake connected directly to the Spruce River. Christopher Lake diversion. In 1959, construction began on Spruce River Dam and the Emma Lake diversion project.

Geographic entities mentioned:
surface_form: christopher lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.5656
lon: -105.8256
From a pumphouse about one kilometre north-east of the dam, about are pumped annually into Emma Lake. The first part of the Christopher Lake diversion, which was completed in 1965, is a short channel that connects Emma Lake to Christopher Lake near Clearsand Beach. Within a few years, the inflow from the diversion had increased water levels in the lake by 2.2 metres compared to 1960 levels.

Geographic entities mentioned:
surface_form: christopher lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.5656
lon: -105.8256
surface_form: christopher lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.5656
lon: -105.8256
surface_form: emma lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.6167
lon: -105.917
Within a few years, the inflow from the diversion had increased water levels in the lake by 2.2 metres compared to 1960 levels. Controlling the inflow to Christopher Lake is a high grated culvert control structure through Highway 953. The outflow from Christopher Lake is via Christopher Creek and is controlled by a two-bay log-stop structure which controls flow into two high culverts.

Geographic entities mentioned:
surface_form: christopher lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.5656
lon: -105.8256
Controlling the inflow to Christopher Lake is a high grated culvert control structure through Highway 953. The outflow from Christopher Lake is via Christopher Creek and is controlled by a two-bay log-stop structure which controls flow into two high culverts. The structure allows drawdown of both Emma and Christopher Lakes simultaneously.

Geographic entities mentioned:
surface_form: christopher lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.5656
lon: -105.8256
The structure allows drawdown of both Emma and Christopher Lakes simultaneously. Christopher Creek is a partially natural run and partially constructed channel that flows out of Christopher Lake and heads south past Highway 263 towards the Little Red River Indian Reserve. It cuts through the eastern portion of the reserve and joins Spruce River just south of it.

Geographic entities mentioned:
surface_form: christopher lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.5656
lon: -105.8256
Christopher Creek is a partially natural run and partially constructed channel that flows out of Christopher Lake and heads south past Highway 263 towards the Little Red River Indian Reserve. It cuts through the eastern portion of the reserve and joins Spruce River just south of it. The Christopher Creek section of the Christopher Lake diversion project was completed in 1975. Parks and recreation.

Geographic entities mentioned:
surface_form: christopher lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.5656
lon: -105.8256
The Christopher Creek section of the Christopher Lake diversion project was completed in 1975. Parks and recreation. Christopher Lake is a recreational lake with parks, campgrounds, Christian camps, marinas, swimming, boating, and fishing. The two marinas are located at the southern end of the lake – one at Bell's Beach the other at Slottens Bay.

Geographic entities mentioned:
surface_form: christopher lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.5656
lon: -105.8256
The two marinas are located at the southern end of the lake – one at Bell's Beach the other at Slottens Bay. Kinasao Lutheran Bible Camp is located on the eastern shore while the other three Bible camps, Quest at Christopher Lake, Camp Kadesh, and Camp Christopher, are on the western shore. At the south-eastern corner of the lake at Slottens Bay is the Christopher Lake Nature Area.

Geographic entities mentioned:
surface_form: christopher lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.5656
lon: -105.8256
Kinasao Lutheran Bible Camp is located on the eastern shore while the other three Bible camps, Quest at Christopher Lake, Camp Kadesh, and Camp Christopher, are on the western shore. At the south-eastern corner of the lake at Slottens Bay is the Christopher Lake Nature Area. This park has three hiking trails totalling about three kilometres for birdwatching and other wildlife viewing.

Geographic entities mentioned:
surface_form: christopher lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.5656
lon: -105.8256
In the winter, one of the trails is groomed for cross-country skiing and snowshoeing. The very northern tip of the lake is in Great Blue Heron Provincial Park, though there no facilities related to the park there. Fish species. Fish commonly found in the Christopher Lake include walleye and northern pike.

Geographic entities mentioned:
surface_form: christopher lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.5656
lon: -105.8256
The construction of the dam was completed in 1960 and the first leg of the diversion channel was completed one year later in 1961. From a pumphouse about one kilometre north-east of the dam, about are pumped annually into Emma Lake. The first part of the Christopher Lake diversion, which was completed in 1965, is a short channel that connects Emma Lake to Christopher Lake near Clearsand Beach.

Geographic entities mentioned:
surface_form: emma lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.6167
lon: -105.917
The excavations at the Federsee, for example, involved the natural sciences at an early stage (pollen analysis (Palynology), moor geology and geomorphology, dendrochronology, radiocarbon dating, archaeozoology and archaeobotany, paleoclimatology, material research, etc.).

Geographic entities mentioned:
surface_form: Federsee
instance_of: Lake
countries: Germany
coordinates: lat: 48.083333333333
lon: 9.6333333333333
It is included in the Calumet, Northwest Indiana, and Great Lakes regions. It is located on the southern shore of Lake Michigan, about southeast of Chicago. It stretches from the famous Indiana Dunes on its northern border, south to the Valparaiso Moraine, a ridge of rolling hills left by the last glacier to pass through the area. As of the 2010 census, its population was 19,396. Towns.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Nixon announced a relaxation of the 20 year old trade embargo with China, allowing the export of non-strategic goods. Elements of the ARVN 1st Division commanded by Brigadier General Vũ Văn Giai and a battalion from the U.S. 101st Airborne Division (Airmobile) began Operation Lam Son 720 against PAVN bases in the A Sầu Valley meeting minimal resistance.

Geographic entities mentioned:
surface_form: A Sầu Valley
instance_of: Valley
countries: Vietnam
coordinates: lat: 16.259305555556
lon: 107.2125
Five U.S. soldiers from the Americal Division were killed when their armored personnel carrier hit a landmine from Da Nang. The PAVN fired two SA-2 missiles at a USAF AC-130 gunship operating west of the Ban Karai Pass, both missed. The PAVN captured Paksong, the last RLA held position on the Bolaven Plateau. The PAVN captured Don Hene, Laos after destroying much of the town in a rocket barrage.

Geographic entities mentioned:
surface_form: Bolaven Plateau
instance_of: Mountain
countries: Laos
coordinates: lat: 15.11
lon: 106.44
François Lake. François Lake in British Columbia is about south of Burns Lake and west of Fraser Lake. The lake is long, making it the second longest natural lake entirely within British Columbia after Babine Lake. Nadina River is the inflow of the lake at the west and Stellako River is the outflow of the lake. The lake is popularly fished for its rainbow trout and char.

Geographic entities mentioned:
surface_form: Babine Lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.75
lon: -126
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
François Lake. François Lake in British Columbia is about south of Burns Lake and west of Fraser Lake. The lake is long, making it the second longest natural lake entirely within British Columbia after Babine Lake. Nadina River is the inflow of the lake at the west and Stellako River is the outflow of the lake. The lake is popularly fished for its rainbow trout and char.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: françois lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05
lon: -125.75
François Lake. François Lake in British Columbia is about south of Burns Lake and west of Fraser Lake. The lake is long, making it the second longest natural lake entirely within British Columbia after Babine Lake. Nadina River is the inflow of the lake at the west and Stellako River is the outflow of the lake. The lake is popularly fished for its rainbow trout and char.

Geographic entities mentioned:
surface_form: françois lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05
lon: -125.75
The name Français later was altered to François and is pronounced locally as Francis. Climate. Equity Silver is a weather station roughly 20 km (12.4 miles) north of François Lake, at an elevation of 1280 m (4199 ft). Equity Silver has a subarctic climate (Köppen &quot;Dfc&quot;), bordering on a tundra climate (Köppen &quot;ET&quot;).

Geographic entities mentioned:
surface_form: françois lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05
lon: -125.75
The peak can be accessed from Cascade Pass via the Ptarmigan Traverse. Geography and climate. Mount Formidable is located on a spur ridge about half a mile west of the Cascade crest, between Cascade Pass and Dome Peak, and about a mile west of Spider Mountain. It is within the Marine west coast climatic zone, and experiences heavy snowfall as a result.

Geographic entities mentioned:
surface_form: Dome Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.3034
lon: -121.03
surface_form: Spider Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.40929
lon: -121.03622
surface_form: mount formidable
instance_of: Mountain
countries: United States
coordinates: lat: 48.4164
lon: -121.067
Mount Formidable itself is likely composed of originally igneous rocks that formed in the Triassic and were metamorphorphized in the Late Cretaceous. Climbing. Mount Formidable can be accessed via the Ptarmigan Traverse, which begins at Cascade Pass. Climbers access the higher elevations of the Middle Fork Cascade River basin via Cache Col and proceed to the summit via the Middle Cascade Glacier.

Geographic entities mentioned:
surface_form: Cache Col
instance_of: Mountain
countries: United States
coordinates: lat: 48.4484594
lon: -121.0528892
Mount Formidable. Mount Formidable is a mountain in the North Cascades of Skagit County, in Washington state. Its first ascent was undertaken by members of the original Ptarmigan Traverse. It was named by early mountaineer Herman Ulrichs in 1935 because of the rugged appearance of its north face. The peak can be accessed from Cascade Pass via the Ptarmigan Traverse. Geography and climate.

Geographic entities mentioned:
surface_form: mount formidable
instance_of: Mountain
countries: United States
coordinates: lat: 48.4164
lon: -121.067