Sarmila/GeoWiki-Features huggingface dataset:
Jochköpfl. The Jochköpfl is a mountain, on the &quot;Windach-Brunnenkogel-Kamm&quot;, a subgroup of the Stubai Alps in Austria. Name and location. The Jochköpfl is named after the col of Timmelsjoch and lies almost exactly on the border between the Austrian federal state of Tyrol and the autonomous Italian province of Bolzano-South Tyrol.

Geographic entities mentioned:
surface_form: jochköpfl
instance_of: Mountain
countries: Austria
coordinates: lat: 46.9275
lon: 11.1078
First ascent. The Jochköpfl was probably first ascended by chamois hunters and state survey staff during the 1850s. There are no records of ascents purely for pleasure dating to the 19th century. However, on 22 August 1890, Ludwig Purtscheller undertook a crossing of all the summits on the main chain of mountains including the one now called the Jochköpfl.

Geographic entities mentioned:
surface_form: jochköpfl
instance_of: Mountain
countries: Austria
coordinates: lat: 46.9275
lon: 11.1078
Vassbotna. Vassbotna is a village in the southern part of Høylandet Municipality in Trøndelag county, Norway. The village is located on an isthmus between the lakes Eidsvatnet and Grungstadvatnet, about southwest of the village of Høylandet and about northeast of the village of Skogmo (in neighboring Overhalla Municipality).

Geographic entities mentioned:
surface_form: Eidsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 64.5348
lon: 12.1143
surface_form: Grungstadvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 64.5919
lon: 12.2102
A yellow edge can be found on the anal fin of breeding males. Distribution and habitat. The fish is found in the Apalachicola River drainage. The fish is absent from the Chattahoochee River system north of Cedar Creek in Houston County, Alabama. The fish is common among sand-bottomed and silt-bottomed creeks and small rivers. It is often found among debris and undercut banks. Conservation status.

Geographic entities mentioned:
surface_form: Chattahoochee River system
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Lake Wallace. Lake Wallace is a lake in Edenhope, Victoria, Australia, featuring abundant bird life and located on the edge of the township. It is encircled by a track suitable for walking, running or bike riding, with plenty of shade and wildlife. Lake Wallace was named for William Wallace.

Geographic entities mentioned:
surface_form: lake wallace
instance_of: Lake
countries: Australia
coordinates: lat: -37.04888889
lon: 141.48861111
It is encircled by a track suitable for walking, running or bike riding, with plenty of shade and wildlife. Lake Wallace was named for William Wallace. Henley Park is located near the southern end of the lake, with a children's playground, shelters containing tables and barbecues, toilets and showers. Henley Park is home to many events, including Henley on Lake Wallace and Day of the Dackel.

Geographic entities mentioned:
surface_form: lake wallace
instance_of: Lake
countries: Australia
coordinates: lat: -37.04888889
lon: 141.48861111
Lake Wallace was named for William Wallace. Henley Park is located near the southern end of the lake, with a children's playground, shelters containing tables and barbecues, toilets and showers. Henley Park is home to many events, including Henley on Lake Wallace and Day of the Dackel. The water level in the lake can fluctuate over time, and the lake can dry up completely.

Geographic entities mentioned:
surface_form: lake wallace
instance_of: Lake
countries: Australia
coordinates: lat: -37.04888889
lon: 141.48861111
Callalli District. Callalli District is one of twenty districts of the Caylloma Province in Peru and is located within the geographical area of the Colca Canyon. Its capital, Callalli, lies on an ancient trade route for Obsidian that ran from Chivay to Lake Titicaca around 1800-200BC. The earliest findings in the region, carvings of camelids in the Mollupunko Cave, date around 8,000 years back.

Geographic entities mentioned:
surface_form: Colca Canyon
instance_of: Valley
countries: Peru
coordinates: lat: -15.5972
lon: -72.0559
Callalli District. Callalli District is one of twenty districts of the Caylloma Province in Peru and is located within the geographical area of the Colca Canyon. Its capital, Callalli, lies on an ancient trade route for Obsidian that ran from Chivay to Lake Titicaca around 1800-200BC. The earliest findings in the region, carvings of camelids in the Mollupunko Cave, date around 8,000 years back.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
The grape was created in 1952 at the Institut National de la Recherche Agronomique (INRA) center in Bordeaux. In the United States, Ederena is being cultivated by E & J Gallo Winery and the University of California, Davis in the San Joaquin Valley. There is also some plantings of the grape in Switzerland.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Barkol Tagh. The Barkol Tagh, also known as Barkol Shan (), forms together with the Qarlik Tagh the easternmost end of the Tian Shan mountain range. It is located along an active thrust fault in the Kumul prefecture in Xinjiang province. Barkol city and the hypersaline Lake Balikun (116 km2) are located at the northern flank of the mountain range.

Geographic entities mentioned:
surface_form: Qarlik Tagh
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 43.05
lon: 94.25
surface_form: barkol tagh
instance_of: Mountain
coordinates: lat: 43.41219407
lon: 93.31597946
Barkol Tagh. The Barkol Tagh, also known as Barkol Shan (), forms together with the Qarlik Tagh the easternmost end of the Tian Shan mountain range. It is located along an active thrust fault in the Kumul prefecture in Xinjiang province. Barkol city and the hypersaline Lake Balikun (116 km2) are located at the northern flank of the mountain range.

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
Barkol Tagh. The Barkol Tagh, also known as Barkol Shan (), forms together with the Qarlik Tagh the easternmost end of the Tian Shan mountain range. It is located along an active thrust fault in the Kumul prefecture in Xinjiang province. Barkol city and the hypersaline Lake Balikun (116 km2) are located at the northern flank of the mountain range.

Geographic entities mentioned:
surface_form: barkol tagh
instance_of: Mountain
coordinates: lat: 43.41219407
lon: 93.31597946
Between Nabob and West Bend, WIS 144 follows WIS 33. While they run concurrently with each other, they meet US 45 at another diamond interchange. In Saukville, WIS 33 meets I-43/WIS 57 at a diamond interchange once again. Continuing east, it ends in downtown Port Washington at WIS 32 west of Lake Michigan. History.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Continuing east, it ends in downtown Port Washington at WIS 32 west of Lake Michigan. History. Prior to European settlement, the foot trail from Port Washington to Horicon was the most traveled of seven trails that met in Horicon Marsh. A road was constructed to provide access from Lake Michigan to the fertile hunting grounds of the marsh, to provide food for the crews of ships on the lake.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Hibbert Rock. jo2gd94ua4b9levxsdpywqdtbs77" xml:space="preserve">Hibbert Rock () is a &quot;drying rock&quot; lying SE of League Rock located in the Quest Channel off the Southern tip of Adelaide Island.

Geographic entities mentioned:
surface_form: Quest Channel
instance_of: Body of water
coordinates: lat: -67.8
lon: -69.0167
Chattooga River (Alabama–Georgia). The Chattooga River runs through northwest Georgia and northeast Alabama in the United States. The river begins in Walker County, Georgia, and flows southwest into Weiss Lake on the Coosa River in Alabama. This river is one of two rivers named Chattooga in the state of Georgia.

Geographic entities mentioned:
surface_form: Coosa River
instance_of: Watercourse
countries: United States
coordinates: lat: 32.4862464
lon: -86.2777475
Prehistoric and ancient times. One or possibly two megalithic dolmen have been found in Hejaz. The Hejaz includes both the &quot;Mahd adh-Dhahab&quot; (&quot;Cradle of the Gold&quot;) () and a water source, now dried out, that used to flow north east to the Persian Gulf via the Wādi Al-Rummah and Wādi Al-Bātin system.

Geographic entities mentioned:
surface_form: Wādi Al-Bātin
instance_of: Watercourse
countries: Saudi Arabia
Iraq
Kuwait
coordinates: lat: 29.10138889
lon: 46.55527778
The Hejazi dishes are known for their spice. Geography. The region is located along the Red Sea Rift. It is also known for its darker, more volcanic sand. Depending on the previous definition, the Hejaz includes some of the mountains of the Sarat range, which topographically separate the Najd from Tehamah. Bdellium plants are also abundant in the Hejaz.

Geographic entities mentioned:
surface_form: darker
instance_of: Mountain
countries: Saudi Arabia
coordinates: lat: 23.97646389
lon: 39.28213056
Archery at the 1996 Summer Olympics. Archery at the 1996 Summer Olympics in Atlanta consisted of four events, two for men and two for women. The events were held in neighboring Stone Mountain. All archery was done at a range of 70 metres. 64 archers competed in each the men's individual and women's individual competitions. They began with a 72-arrow ranking round.

Geographic entities mentioned:
surface_form: Stone Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.805944444444
lon: -84.145422222222
Nittany Valley. Nittany Valley is an eroded anticlinal valley located in Centre County, Pennsylvania. It is separated from the Bald Eagle Valley by Bald Eagle Mountain and from Penns Valley by Mount Nittany. The valley is closed to the north by a high plateau that joins these two mountain ridges, but is open to the south at the southern terminus of Mount Nittany.

Geographic entities mentioned:
surface_form: Bald Eagle Valley
instance_of: Valley
countries: United States
coordinates: lat: 41
lon: -77.75
surface_form: Bald Eagle Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.137222222222
lon: -77.327222222222
surface_form: Penns Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.85
lon: -77.61666667
surface_form: Mount Nittany
instance_of: Mountain
countries: United States
coordinates: lat: 40.8277
lon: -77.7731
surface_form: eagle valley
instance_of: Valley
countries: United States
coordinates: lat: 39.1652
lon: -119.757
surface_form: eagle valley
instance_of: Valley
countries: United States
surface_form: eagle valley
instance_of: Valley
countries: United States
coordinates: lat: 33.847500000000004
lon: -117.48055555555555
surface_form: eagle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0618
lon: -74.5093
surface_form: eagle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.8974
lon: -90.5601
surface_form: eagle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.15166667
lon: -115.15277778
The arch was an ancient Himalayan scale mountain towering above the valley. The oldest rock layers deep within the eroded mountain are now exposed on Sand Ridge in the middle of the valley. Younger rocks from the outer layers of the arch are exposed on the west side of the Bald Eagle Mountain ridge in the Bald Eagle Valley, with the youngest across that valley at the foot of the Allegheny Front.

Geographic entities mentioned:
surface_form: Bald Eagle Valley
instance_of: Valley
countries: United States
coordinates: lat: 41
lon: -77.75
surface_form: eagle valley
instance_of: Valley
countries: United States
coordinates: lat: 39.1652
lon: -119.757
surface_form: eagle valley
instance_of: Valley
countries: United States
surface_form: eagle valley
instance_of: Valley
countries: United States
coordinates: lat: 33.847500000000004
lon: -117.48055555555555
surface_form: bald eagle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.137222222222
lon: -77.327222222222
surface_form: eagle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0618
lon: -74.5093
surface_form: eagle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.8974
lon: -90.5601
surface_form: eagle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.15166667
lon: -115.15277778
surface_form: bald eagle valley
instance_of: Valley
countries: United States
coordinates: lat: 41
lon: -77.75
Nittany Valley. Nittany Valley is an eroded anticlinal valley located in Centre County, Pennsylvania. It is separated from the Bald Eagle Valley by Bald Eagle Mountain and from Penns Valley by Mount Nittany. The valley is closed to the north by a high plateau that joins these two mountain ridges, but is open to the south at the southern terminus of Mount Nittany.

Geographic entities mentioned:
surface_form: nittany valley
instance_of: Valley
countries: United States
coordinates: lat: 40.9
lon: -77.7
The valley drains to Bald Eagle Creek through water gaps in Bald Eagle Mountain formed by Spring Creek and Fishing Creek, along with smaller streams running through Curtain Gap and Howard Gap. The northwest side of the valley between the Bald Eagle Mountain ridge and the lower Sand Ridge is also known as the Little Nittany Valley.

Geographic entities mentioned:
surface_form: nittany valley
instance_of: Valley
countries: United States
coordinates: lat: 40.9
lon: -77.7
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: bald eagle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.137222222222
lon: -77.327222222222
surface_form: eagle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0618
lon: -74.5093
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: eagle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.8974
lon: -90.5601
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: eagle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.15166667
lon: -115.15277778
Transportation. The Keystone Shortway, now Interstate 80, runs diagonally across the Nittany Valley on a west to east line, from Curtin Gap east of Milesburg, Pennsylvania, to a natural gap in Mount Nittany and then via a deep rock cut along the Long Run stream.

Geographic entities mentioned:
surface_form: nittany valley
instance_of: Valley
countries: United States
coordinates: lat: 40.9
lon: -77.7
surface_form: mount nittany
instance_of: Mountain
countries: United States
coordinates: lat: 40.8277
lon: -77.7731
The Pennsylvania State Correctional Institution - Rockview, the Nittany Mall, the Pennsylvania Transportation Institute and University Park Airport are large facilities located in the valley. State College, Pennsylvania and the Pennsylvania State University main University Park campus lie at the southern end of the Nittany and Penns Valleys, and this area is also known as &quot;Happy Valley&quot;.

Geographic entities mentioned:
surface_form: happy valley
instance_of: Valley
countries: United States
coordinates: lat: -14.279722222222
lon: -170.69638888889
Nittany Valley. Nittany Valley is an eroded anticlinal valley located in Centre County, Pennsylvania. It is separated from the Bald Eagle Valley by Bald Eagle Mountain and from Penns Valley by Mount Nittany. The valley is closed to the north by a high plateau that joins these two mountain ridges, but is open to the south at the southern terminus of Mount Nittany.

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: mount nittany
instance_of: Mountain
countries: United States
coordinates: lat: 40.8277
lon: -77.7731
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The valley is closed to the north by a high plateau that joins these two mountain ridges, but is open to the south at the southern terminus of Mount Nittany. The valley drains to Bald Eagle Creek through water gaps in Bald Eagle Mountain formed by Spring Creek and Fishing Creek, along with smaller streams running through Curtain Gap and Howard Gap.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: bald eagle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.137222222222
lon: -77.327222222222
surface_form: eagle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0618
lon: -74.5093
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: eagle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.8974
lon: -90.5601
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: eagle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.15166667
lon: -115.15277778
The northwest side of the valley between the Bald Eagle Mountain ridge and the lower Sand Ridge is also known as the Little Nittany Valley. The valley has a mixture of farmland, woodlots, and several working and abandoned quarries. Bellefonte, the county seat of Centre County, is the largest municipality completely within the valley.

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
The valley has a mixture of farmland, woodlots, and several working and abandoned quarries. Bellefonte, the county seat of Centre County, is the largest municipality completely within the valley. The Pennsylvania State Correctional Institution - Rockview, the Nittany Mall, the Pennsylvania Transportation Institute and University Park Airport are large facilities located in the valley.

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
The Nittany and Bald Eagle Railroad short line spur that enters the valley from Milesburg, then runs along Spring Creek to Bellefonte, splits, with a track going northeast to Pleasant Gap and another going southwest to Lemont and State College. The spur to Bellefonte follows Pennsylvania Route 144 and the line from Lemont to Pleasant Gap follows Pennsylvania Route 26.

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
The spur to Bellefonte follows Pennsylvania Route 144 and the line from Lemont to Pleasant Gap follows Pennsylvania Route 26. Route 26 is the primary north to south route through the valley, and the Interstate 99 extension will also run along its new alignment to I-80. Geology. Nittany Valley is in the western part of the Ridge and Valley province of the Appalachian Mountains.

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
Nittany Valley is in the western part of the Ridge and Valley province of the Appalachian Mountains. During the Appalachian orogeny, the sedimentary rock layers folded up into the Nittany Arch anticline. The arch was an ancient Himalayan scale mountain towering above the valley. The oldest rock layers deep within the eroded mountain are now exposed on Sand Ridge in the middle of the valley.

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
The arch was an ancient Himalayan scale mountain towering above the valley. The oldest rock layers deep within the eroded mountain are now exposed on Sand Ridge in the middle of the valley. Younger rocks from the outer layers of the arch are exposed on the west side of the Bald Eagle Mountain ridge in the Bald Eagle Valley, with the youngest across that valley at the foot of the Allegheny Front.

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
Augustine gives his birth date as October 12, 1774. Thomas Clarke had obtained by grant or purchase four tracts of land and three houses with their lots in St. Augustine. In 1770, Governor James Grant gave him title to 300 acres on the west side of the Matanzas River, four miles northwest of the Spanish fort at Matanzas Inlet, and about ten miles south of St. Augustine.

Geographic entities mentioned:
surface_form: Matanzas River
instance_of: Landform
countries: United States
coordinates: lat: 29.9138577
lon: -81.2836827
surface_form: Matanzas Inlet
instance_of: Landform
countries: United States
coordinates: lat: 29.7058
lon: -81.2283
WCZS-LD (as W07DP-D) was sold to Sonshine Family Television in 2018. In 2020, the station changed its city of license to Chambersburg and obtained a construction permit to move its transmitter to Clarks Knob, near its new city of license. The station signed on UHF analog channel 40 on August 29, 1986, as W40AF; and then began broadcasting on channel 35 on December 8, 2003, as W35BT.

Geographic entities mentioned:
surface_form: Clarks Knob
instance_of: Mountain
countries: United States
coordinates: lat: 40.047777777778
lon: -77.750555555556
Edwin Hansford. Edwin Arnold Hansford (December 1, 1895 &ndash; March 12, 1959) was a politician in Manitoba, Canada, and served as leader of that province's Co-operative Commonwealth Federation between 1948 and 1952. Hansford was born in the Annapolis Valley region of Nova Scotia. He served overseas in World War I for four-and-a-half years, and subsequently worked for Canadian National Railways.

Geographic entities mentioned:
surface_form: Annapolis Valley
instance_of: Valley
countries: Canada
coordinates: lat: 44.979166666666664
lon: -64.89222222222222
CSX Chef Menteur Pass Bridge. The CSX Chef Menteur Pass Bridge carries one track of CSX rail lines across the Chef Menteur Pass on the eastern side of Lake Pontchartrain in New Orleans by the Venetian Isles neighborhood.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
On that day the training area is opened to private vehicles; normally it is out-of-bounds. At the head of the valley is a small lake, the Mölssee.

Geographic entities mentioned:
surface_form: mölssee
instance_of: Lake
countries: Austria
coordinates: lat: 47.173333333333
lon: 11.609722222222
Wattental. The Wattental is a southern side valley of the Inn valley. The valley, through which the Wattenbach stream flows, is incised deeply into the quartz-phyllite rock of the Tux Prealps. The two dispersed settlements of Wattenberg and Vögelsberg (in the municipality of Wattens) sprawl across the outer part of the valley.

Geographic entities mentioned:
surface_form: wattental
instance_of: Valley
countries: Austria
coordinates: lat: 47.23
lon: 11.618611111111
The Wattentaler Lizum lies entirely on the territory of Wattenberg. The Wattental produces a high level of water power thanks to its large catchment area which is why internationally successful firms such as Swarovski, and Wattenspapier have been established in the village of Wattens by the River Inn.

Geographic entities mentioned:
surface_form: wattental
instance_of: Valley
countries: Austria
coordinates: lat: 47.23
lon: 11.618611111111
The Wattental was and is therefore the reason behind the economic boom of the market village of Wattens which has made it one of the wealthiest municipalities in Austria. The valley is a popular recreation area. The summits of the Rotwandspitze, Hirzer and Hahneburger have outstanding views and can be climbed from bases in the valley.

Geographic entities mentioned:
surface_form: wattental
instance_of: Valley
countries: Austria
coordinates: lat: 47.23
lon: 11.618611111111
Launched in 1930 as &quot;Stakesby&quot; for Rowland & Marwood Steamship Co. Operated under the management of Headlam & Son, Whitby. Torpedoed on 25 August 1940 by &quot;U-124&quot; north of Butt of Lewis, Hebrides. Beached on the west coast but slid off the beach and sank in deep water. she was salvaged sixteen months later and rebuilt. To MoWT in 1943 and renamed &quot;Empire Derwent&quot;.

Geographic entities mentioned:
surface_form: Butt of Lewis
instance_of: Landform
countries: United Kingdom
coordinates: lat: 58.5156
lon: -6.26119
This was followed by a second attempt on 3 March 1989 at a temple in Ganga Talao when armed with a razor blade and disguised as a Hindu pilgrim, Iqbal Ghani assaulted Prime Minister Jugnauth. Both attempts were believed to be the result of drug cartels, against whom Jugnauth was leading a crack-down. Personal life.

Geographic entities mentioned:
surface_form: Ganga Talao
instance_of: Lake
countries: Mauritius
coordinates: lat: -20.418055555556
lon: 57.491944444444
Łebsko Lake. Łebsko Lake (;) is a brackish coastal lake in the Pomeranian Voivodeship of Poland. It is connected to the Baltic Sea by the Łeba River, which causes saltwater intrusion. It is located within Słowiński National Park. The lake formed when sea winds pushed up a spit of sand that ultimately separated it from the Baltic sea. The town of Łeba sits where the Łeba river meets the sea.

Geographic entities mentioned:
surface_form: łebsko lake
instance_of: Lake
countries: Poland
coordinates: lat: 54.713611111111
lon: 17.408888888889
Nyssen's research in Belgium is also related to the consequences of human activities on geomorphic processes: the reintroduction of beavers, spoil tips of the derelict coal mining industry, and the age-old agriculture in the Pays de Herve region, which led to the occurrence of lynchets or cultivation terraces, by analogy to a common practice in current Ethiopia;
The beaver dams have drawn his attention because they contribute to conserving water in the rivers' headwaters.

Geographic entities mentioned:
surface_form: Pays de Herve
instance_of: Plateau
countries: Belgium
coordinates: lat: 50.65
lon: 5.83
Lac de Chambly. Lac de Chambly is a lake in the Jura department of France.

Geographic entities mentioned:
surface_form: lac de chambly
instance_of: Lake
countries: France
coordinates: lat: 46.644166666667
lon: 5.8044444444444
Distribution. This species is endemic to New Zealand and is found in both the North and South Islands. It has been observed in its type locality of Dunedin, at the head of Lake Wakatipu and also in the Gollan Valley of Wellington and Kaeo in Northland. This species has also been found in a site of ecological significance, at Decanter Bay in Canterbury, as set out in the Christchurch District Plan.

Geographic entities mentioned:
surface_form: Lake Wakatipu
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.085
lon: 168.561
Georgian Bay. The Georgian Bay () is a large bay of Lake Huron, in the Laurentia bioregion. It is located entirely within the borders of Ontario, Canada. The main body of the bay lies east of the Bruce Peninsula and Manitoulin Island. To its northwest is the North Channel.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Geography. The Georgian Bay is about long by wide. It covers approximately, making it nearly 80% the size of Lake Ontario. The eastern Georgian Bay is part of the southern edge of the Canadian Shield, granite bedrock exposed by the glaciers at the end of the last ice age, about 11,000 years ago.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
The granite rock formations and windswept eastern white pine are characteristic of the islands and much of the shoreline of the bay. The rugged beauty of the area inspired landscapes by artists of the Group of Seven. The western part of the bay, from Collingwood north, and including Manitoulin, Drummond, Cockburn and St. Joseph islands, borders the Niagara Escarpment.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
If the Georgian Bay were considered a lake in its own right, it would be the fourth largest lake located entirely within Canada (after Great Bear Lake, Great Slave Lake and Lake Winnipeg).

Geographic entities mentioned:
surface_form: Great Bear Lake
instance_of: Lake
countries: Canada
coordinates: lat: 66
lon: -121
surface_form: Great Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 61.666666666667
lon: -114
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Considered together with the Georgian Bay, Lake Huron is the second largest of the Great Lakes - if the Georgian Bay were excluded, Lake Huron would be the third largest (after Lake Superior and Lake Michigan, but still ahead of Lake Erie and Lake Ontario). There are tens of thousands of islands in the Georgian Bay.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Manitoulin Island, lying along the northern side of the bay, is the world's largest island in a freshwater lake. The Trent–Severn Waterway connects the Georgian Bay to Lake Ontario, running from Port Severn in the southeastern corner of the Georgian Bay through Lake Simcoe into Lake Ontario near Trenton. Further north, Lake Nipissing drains into the Georgian Bay through the French River.

Geographic entities mentioned:
surface_form: Lake Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
The Trent–Severn Waterway connects the Georgian Bay to Lake Ontario, running from Port Severn in the southeastern corner of the Georgian Bay through Lake Simcoe into Lake Ontario near Trenton. Further north, Lake Nipissing drains into the Georgian Bay through the French River. In October 2004, the Georgian Bay Littoral was declared a Biosphere Reserve by UNESCO. History.

Geographic entities mentioned:
surface_form: Lake Nipissing
instance_of: Lake
countries: Canada
coordinates: lat: 46.283333333333
lon: -80
Farther south there is the Patagonian Volcanic Gap in the Andean Volcanic Belt, which separates Hudson from the Austral Volcanic Zone and its first volcano, Lautaro. The next volcanoes to the north are Mate Grande and Macá and Cay from Hudson, then Mentolat and the Puyuhuapi volcanic field. The volcano is a ice-filled caldera that rises above the surrounding terrain.

Geographic entities mentioned:
surface_form: Macá
instance_of: Mountain
countries: Chile
coordinates: lat: -45.105833333333
lon: -73.169166666667
surface_form: Mentolat
instance_of: Mountain
countries: Chile
coordinates: lat: -44.696666666667
lon: -73.075833333333
surface_form: puyuhuapi
instance_of: Mountain
countries: Chile
coordinates: lat: -44.3334
lon: -72.5968
surface_form: mentolat
instance_of: Mountain
countries: Chile
coordinates: lat: -44.696666666667
lon: -73.075833333333
surface_form: macá
instance_of: Mountain
countries: Chile
coordinates: lat: -45.105833333333
lon: -73.169166666667
Tephra from its eruptions fell on the ice and was carried away by glaciers, ending up in their moraines. The deglaciation that began 17,900 years ago may have enhanced volcanic activity; the largest eruptions of Hudson, Llaima and Villarrica took place at that time.

Geographic entities mentioned:
surface_form: Llaima
instance_of: Mountain
countries: Chile
coordinates: lat: -38.697407
lon: -71.730445
surface_form: llaima
instance_of: Mountain
countries: Chile
coordinates: lat: -38.697407
lon: -71.730445
surface_form: villarrica
instance_of: Mountain
countries: Chile
coordinates: lat: -39.42
lon: -71.939166666667
surface_form: villarrica
instance_of: Lake
countries: Chile
coordinates: lat: -39.25
lon: -72.083333333333
Aircraft noted the ash cloud as far as Melbourne in Australia. Particles from Hudson have been found in ice at Mount Everest, Himalaya. The 1991 eruption of Hudson took place in the same year as the 1991 eruption of Mount Pinatubo. The Pinatubo aerosols had already spread worldwide when Hudson erupted. Unlike the Pinatubo eruption, Hudson mostly produced volcanic ash which fell out more quickly.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
The eruption may have been triggered by tectonic stress changes caused by the 1960 Valdivia earthquake. The eruption is the second-largest historic volcanic eruption in Chile, only behind the 1932 Quizapu eruption. With a volcanic explosivity index of 5, it is one of the largest volcanic eruptions of the 20th century. It formed a eruption column and pyroclastic flows within the caldera.

Geographic entities mentioned:
surface_form: quizapu
instance_of: Mountain
countries: Chile
coordinates: lat: -35.653333333333
lon: -70.760833333333
Hudson is the second-southernmost volcano of the SVZ, after Rio Murta; erroneously, it is often referred to as the southernmost. Farther south there is the Patagonian Volcanic Gap in the Andean Volcanic Belt, which separates Hudson from the Austral Volcanic Zone and its first volcano, Lautaro.

Geographic entities mentioned:
surface_form: lautaro
instance_of: Mountain
countries: Chile
coordinates: lat: -49.019
lon: -73.504
Hudson Volcano. Hudson Volcano (, or) is the most active volcano in the southern part of the Southern Volcanic Zone of the Andes Mountains in Chile, having erupted most recently in 2011. It was formed by the subduction of the oceanic Nazca Plate under the continental South American Plate.

Geographic entities mentioned:
surface_form: hudson volcano
instance_of: Mountain
countries: Chile
coordinates: lat: -45.92
lon: -72.95
A Holocene lava flow extends along the Huemules valley and is thick. The flow may be either 1,000 or 13,000 years old; it was possibly the product of multiple eruptions. The volcanic cones outside of the caldera are weathered and covered by vegetation; they are of Holocene age. Other geologic processes such as glacial erosion have modified the appearance of the Hudson volcano.

Geographic entities mentioned:
surface_form: hudson volcano
instance_of: Mountain
countries: Chile
coordinates: lat: -45.92
lon: -72.95
Noosgulch River. b12he6rul9shra6tqsevezhs8r6l" xml:space="preserve">The Noosgulch River is a river in the Bella Coola Valley of the Central Coast region of British Columbia, Canada, flowing southwest from the southernmost Kitimat Ranges to meet the Bella Coola River just north of Nusatsum Mountain.

Geographic entities mentioned:
surface_form: Bella Coola Valley
instance_of: Valley
countries: Canada
surface_form: Nusatsum Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.39722222
lon: -126.3783333
Jaskinia Wielka Śnieżna. 1vcy3b0u3f1l58wv7q07bnzdzim70" xml:space="preserve">Jaskinia Wielka Śnieżna (&quot;great snowy cave&quot;) is a limestone cave system in Mount Małołączniak in the Western Tatra Mountains, of the Carpathian Mountains System, in southern Poland. The cave is within Tatra National Park.

Geographic entities mentioned:
surface_form: Małołączniak
instance_of: Mountain
countries: Slovakia
Poland
coordinates: lat: 49.235805555556
lon: 19.919305555556
Suri (Peru). Suri (Aymara and Quechua for rhea) is a mountain in the Andes of southern Peru, about high. It is situated in the Puno Region, El Collao Province, Santa Rosa District. Suri lies northeast of the lake Wilaquta and the mountain Chinchillani.

Geographic entities mentioned:
surface_form: suri (peru)
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0686
lon: -69.9925
Suri (Peru). Suri (Aymara and Quechua for rhea) is a mountain in the Andes of southern Peru, about high. It is situated in the Puno Region, El Collao Province, Santa Rosa District. Suri lies northeast of the lake Wilaquta and the mountain Chinchillani.

Geographic entities mentioned:
surface_form: suri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0686
lon: -69.9925
Suri (Peru). Suri (Aymara and Quechua for rhea) is a mountain in the Andes of southern Peru, about high. It is situated in the Puno Region, El Collao Province, Santa Rosa District. Suri lies northeast of the lake Wilaquta and the mountain Chinchillani.

Geographic entities mentioned:
surface_form: suri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0686
lon: -69.9925
surface_form: chinchillani
instance_of: Mountain
countries: Peru
coordinates: lat: -17.11666679
lon: -70.5
surface_form: wilaquta
instance_of: Mountain
countries: Peru
coordinates: lat: -14.0294
lon: -70.2753
surface_form: wilaquta
instance_of: Mountain
countries: Peru
coordinates: lat: -16.6156
lon: -70.1561
Suri (Peru). Suri (Aymara and Quechua for rhea) is a mountain in the Andes of southern Peru, about high. It is situated in the Puno Region, El Collao Province, Santa Rosa District. Suri lies northeast of the lake Wilaquta and the mountain Chinchillani.

Geographic entities mentioned:
surface_form: santa rosa
instance_of: Mountain
countries: Peru
coordinates: lat: -10.48540278
lon: -76.72636111
Gestione Governativa Navigazione Laghi. (), commonly known as, is an Italian public body responsible for providing scheduled public boat transport services on Lake Maggiore (), Lake Garda (), and Lake Como (), mostly in Italy but also in Switzerland. It operates under the supervision of the Ministry of Infrastructure and Transport. Its headquarters are located in Milan. History.

Geographic entities mentioned:
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
surface_form: Lake Garda
instance_of: Lake
countries: Italy
coordinates: lat: 45.633333333333
lon: 10.666666666667
History. Regular steamship services on the major Italian lakes began in the early 19th century, typically operated by private companies, sometimes with government subsidies. After periods of disruption and varying management structures, particularly following World War II, the Italian government moved to consolidate and directly manage these essential services.

Geographic entities mentioned:
surface_form: Italian lakes
instance_of: Group of lakes
countries: Italy
Switzerland
It is situated in the Cusco Region, Canchis Province, Pitumarca District and in the Quispicanchi Province, Ocongate District. Yanajaja lies south of the peak of Q'ampa, southwest of Callangate, west of the river Chillcamayu, and east of Ausangate, close to Chilinita (Santa Catalina).

Geographic entities mentioned:
surface_form: Callangate
instance_of: Mountain
countries: Peru
coordinates: lat: -13.74319783
lon: -71.137118
surface_form: Ausangate
instance_of: Mountain
countries: Peru
coordinates: lat: -13.788611111111
lon: -71.231111111111
surface_form: callangate
instance_of: Mountain
countries: Peru
coordinates: lat: -13.74319783
lon: -71.137118
surface_form: ausangate
instance_of: Mountain
countries: Peru
coordinates: lat: -13.788611111111
lon: -71.231111111111
Yanajaja. Yanajaja (possibly from Quechua &quot;yana&quot; black, &quot;qaqa&quot;, rock) is a mountain in the Vilcanota mountain range in the Andes of Peru, about high. It is situated in the Cusco Region, Canchis Province, Pitumarca District and in the Quispicanchi Province, Ocongate District.

Geographic entities mentioned:
surface_form: yanajaja
instance_of: Mountain
countries: Peru
coordinates: lat: -13.79194444
lon: -71.11527778
surface_form: yanajaja
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7914
lon: -71.1158
Rocky Comfort Creek (Florida). Rocky Comfort Creek is a stream near Florida's capital city of Tallahassee. It now feeds into Lake Talquin which was formed by a dam on the Ochlockonee River. David Ochiltree who served as mayor of Tallahassee in 1827 resided in a home by the creek and died there in 1834. He moved to Florida from Fayetteville, North Carolina.

Geographic entities mentioned:
surface_form: Lake Talquin
instance_of: Lake
countries: United States
coordinates: lat: 30.388611111111
lon: -84.646666666667
The same cycle repeated for a total of seven times. On the seventh time, Meng Huo surrendered and told Zhuge Liang, &quot;My lord, against Heaven's might the people of the south will never again rebel.&quot; Zhuge Liang then led his forces towards Dian Lake in triumph. The Nanzhong region was basically pacified by the autumn of 225.

Geographic entities mentioned:
surface_form: Dian Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 24.800555555556
lon: 102.67138888889
Before his death, Zhuge Liang said that he wanted to be buried as simply as possible in Mount Dingjun (in present-day Mian County, Hanzhong, Shaanxi): his tomb should be just large enough for his coffin to fit in; he was to be dressed in the clothes he wore when he died; he did not need to be buried with any decorative objects or ornaments.

Geographic entities mentioned:
surface_form: Mount Dingjun
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 33.1125
lon: 106.66194444444
Disposal. In 2011, after a period of lay-up, &quot;Kathryn Spirit&quot; was sold to the Groupe St-Pierre for scrapping. The company decided that they would carry out the demolition at Beauharnois in the Greater Montreal Area, Quebec, on the shores of Lake Saint-Louis.

Geographic entities mentioned:
surface_form: Lake Saint-Louis
instance_of: Lake
countries: Canada
coordinates: lat: 45.401388888889
lon: -73.814166666667
History. The Fâstâci Monastery was founded by the Palade landowners during the 17th century. In 1711, it was dedicated to the Frumoasa Monastery from Iaşi (Jassy), a branch of the &quot;Saint Ecaterina&quot; Monastery on Mount Sinai (in present-day Egypt). It was rebuilt by Lord Mihai Racoviţă Cehan during the 18th century. It was extended and suffered transformations during the 19th century.

Geographic entities mentioned:
surface_form: Mount Sinai
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.5384
lon: 33.9752
The region is within the Vale do Ribeira, the poorest part of São Paulo. The population grew by 27.18% from 1960 to 1980, but fell by 2.17% between 1980 and 1989. As of 1994 the human population was 153,164 inhabitants. To the north the complex is bordered by the Juréia Massif and the Serra da Canavieira. In the south, Paranaguá Bay extends about inland, and has depths up to.

Geographic entities mentioned:
surface_form: juréia massif
instance_of: Mountain
countries: Brazil
coordinates: lat: -24.527563
lon: -47.255395
Iguape-Cananéia-Paranaguá estuary lagoon complex. The Iguape-Cananéia-Paranaguá estuary lagoon complex () is a stretch of interconnected coastal estuaries and lagoons that extends southwest from Iguape in the south of São Paulo past Cananéia, São Paulo to Paranaguá, Paraná. It includes the Mar Pequeno in São Paulo, between Ilha Comprida and the mainland, and Paranaguá Bay in Paraná. Location.

Geographic entities mentioned:
surface_form: iguape-cananéia-paranaguá estuary lagoon complex
instance_of: Body of water
countries: Brazil
It includes the Mar Pequeno in São Paulo, between Ilha Comprida and the mainland, and Paranaguá Bay in Paraná. Location. The Iguape-Cananéia-Paranaguá estuary lagoon complex lies between (Barra do Una, SP) and (Morretes, PR) along the southeast São Paulo coast and the north Paraná coast. The complex covers an area of. The region is within the Vale do Ribeira, the poorest part of São Paulo.

Geographic entities mentioned:
surface_form: iguape-cananéia-paranaguá estuary lagoon complex
instance_of: Body of water
countries: Brazil
Molteno Dam. Molteno Dam is a small but historic dam, on the lower slopes of Table Mountain in Western Cape, South Africa. Still in service, it was established in 1877 and is now located in the suburb of Oranjezicht, Cape Town. Background and construction.

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
Still in service, it was established in 1877 and is now located in the suburb of Oranjezicht, Cape Town. Background and construction. In earlier days, the infant settlement of Cape Town had been supplied with water from Table Mountain by way of canals or &quot;grachts&quot; (such as Buitengracht, Kaizergracht and Heerengracht - now major streets).

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
The route continues north through the northern suburbs of Philadelphia and serves Jenkintown, Willow Grove, and Doylestown, the latter of which it bypasses on a freeway. North of Doylestown, PA 611 heads through rural areas and runs along the west bank of the Delaware River to Easton in the Lehigh Valley.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Northampton County. PA 611 leaves Riegelsville for Williams Township in Northampton County, which is in the Lehigh Valley region, and becomes South Delaware Drive, heading north-northwest through forested areas immediately to the west of the Delaware Canal and the Delaware River. The road bends east and runs through a mix of woods, fields, and homes, curving to the north again.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5