Sarmila/GeoWiki-Features huggingface dataset:
From 1944 to 1945, the German Navy continued to develop and successfully tested various short-range rockets that could be launched from submerged submarines at depths of up to at the naval testing station operated by the &quot;Torpedoversuch Anstalt Eckernförde&quot; at Lake Toplitz near Bad Aussee, Austria.

Geographic entities mentioned:
surface_form: Lake Toplitz
instance_of: Lake
countries: Austria
coordinates: lat: 47.641666666667
lon: 13.927777777778
Lower Klamath Lake. Lower Klamath Lake is a lake in Siskiyou County, California. At one time it was connected to Upper Klamath Lake. It currently is used to hold overflow water for Klamath Project irrigation uses. The lake is in Northern California, near the border with Oregon. The Lower Klamath National Wildlife Refuge (est.

Geographic entities mentioned:
surface_form: Upper Klamath Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.392222222222
lon: -121.88027777778
Lower Klamath Lake. Lower Klamath Lake is a lake in Siskiyou County, California. At one time it was connected to Upper Klamath Lake. It currently is used to hold overflow water for Klamath Project irrigation uses. The lake is in Northern California, near the border with Oregon. The Lower Klamath National Wildlife Refuge (est.

Geographic entities mentioned:
surface_form: lower klamath lake
instance_of: Lake
countries: United States
coordinates: lat: 41.99083983333333
lon: -121.74309983333333
El Poble-sec, Barcelona. (;) is a neighborhood in the Sants-Montjuïc district of Barcelona, Catalonia (Spain). The neighborhood is located between Montjuïc mountain and the Avinguda del Paral·lel. It covers around 70 hectares. The Poble Sec station of the Barcelona Metro is located in, and named after, this neighborhood.

Geographic entities mentioned:
surface_form: Montjuïc
instance_of: Mountain
countries: Spain
coordinates: lat: 41.364166666667
lon: 2.1580555555556
His interest in climbing was chiefly geographical and scientific and he was one of the first Alpine climbers to employ photography. In 1865 George and Sir George Young, with the guide Christian Almer, established the first direct route up the Jungfrau from the valley of Lauterbrunnen. They had to carry ladders with them in order to cross the many crevasses on the north flank.

Geographic entities mentioned:
surface_form: Jungfrau
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.536944444444
lon: 7.9625
They had to carry ladders with them in order to cross the many crevasses on the north flank. Having spent the night on the rocks of the Schneehorn () they gained next morning the Silberlücke, the depression between the Jungfrau and Silberhorn, and thence in little more than three hours reached the summit.

Geographic entities mentioned:
surface_form: Silberhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.542222222222
lon: 7.9488888888889
Rhondda Leader. The &quot;Rhondda Leader&quot; is a weekly newspaper distributed in the Rhondda Valleys, South Wales. The tabloid newspaper is published on a Wednesday by Media Wales which is owned by the UK's largest newspaper corporation, Trinity Mirror. Part of the Celtic Weekly Newspapers series, which publishes eight other titles in South Wales, the &quot;Leader&quot; was founded in 1899.

Geographic entities mentioned:
surface_form: Rhondda Valleys
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
The local authority modernised parts of the village in the late twentieth century. Nearby is Pye Hill and the bend in the Cromford Canal where it turns southward down the Erewash Valley and the junction with its extension to Pinxton. About a quarter of a mile north east is another transport landmark, Pye Bridge at the junction of the Erewash Valley railway line and the extension to Ambergate.

Geographic entities mentioned:
surface_form: Erewash Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.0045
lon: -1.3131
Mount Chittenden. Mount Chittenden, elevation, is a mountain peak in the Absaroka Range in Yellowstone National Park. The peak was named by Henry Gannett of the Hayden Geological Survey of 1878 for George B. Chittenden, a surveyor who had worked with Gannett, Hayden and others in surveys in Montana, Idaho and Wyoming. Chittenden never participated in any of the Yellowstone surveys.

Geographic entities mentioned:
surface_form: hayden
instance_of: Valley
countries: United States
coordinates: lat: 44.6439
lon: -110.456
Mount Chittenden. Mount Chittenden, elevation, is a mountain peak in the Absaroka Range in Yellowstone National Park. The peak was named by Henry Gannett of the Hayden Geological Survey of 1878 for George B. Chittenden, a surveyor who had worked with Gannett, Hayden and others in surveys in Montana, Idaho and Wyoming. Chittenden never participated in any of the Yellowstone surveys.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: yellowstone
instance_of: Lake
countries: United States
coordinates: lat: 44.466666666667
lon: -110.36666666667
surface_form: mount chittenden
instance_of: Mountain
countries: United States
coordinates: lat: 44.5466
lon: -110.171
The peak was named by Henry Gannett of the Hayden Geological Survey of 1878 for George B. Chittenden, a surveyor who had worked with Gannett, Hayden and others in surveys in Montana, Idaho and Wyoming. Chittenden never participated in any of the Yellowstone surveys. Mount Chittenden was not named for Major Hiram M. Chittenden, the U.S. Army Engineer famous for his road and bridge work in the park.

Geographic entities mentioned:
surface_form: yellowstone
instance_of: Lake
countries: United States
coordinates: lat: 44.466666666667
lon: -110.36666666667
Mount Chittenden. Mount Chittenden, elevation, is a mountain peak in the Absaroka Range in Yellowstone National Park. The peak was named by Henry Gannett of the Hayden Geological Survey of 1878 for George B. Chittenden, a surveyor who had worked with Gannett, Hayden and others in surveys in Montana, Idaho and Wyoming. Chittenden never participated in any of the Yellowstone surveys.

Geographic entities mentioned:
surface_form: mount chittenden
instance_of: Mountain
countries: United States
coordinates: lat: 44.5466
lon: -110.171
The peak was named by Henry Gannett of the Hayden Geological Survey of 1878 for George B. Chittenden, a surveyor who had worked with Gannett, Hayden and others in surveys in Montana, Idaho and Wyoming. Chittenden never participated in any of the Yellowstone surveys. Mount Chittenden was not named for Major Hiram M. Chittenden, the U.S. Army Engineer famous for his road and bridge work in the park.

Geographic entities mentioned:
surface_form: mount chittenden
instance_of: Mountain
countries: United States
coordinates: lat: 44.5466
lon: -110.171
Dove Elbe. The Dove Elbe () is a closed anabranch of the Unterelbe, the lower part of the river Elbe (near Hamburg, Germany). The inflow has been blocked by a dike since 1438. The lower end was shortened by a redirection of the Norderelbe in 1579. Before the Neuengammer &quot;Blaue Brücke&quot; (lit. Blue Bridge), there's the Neuengammer branch canal going off to the left.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Gallt y Daren. Gallt y Daren is a peak in the southern half of the Snowdonia National Park in Gwynedd, North Wales, and forms part of the Arenig mountain range. It is a top of Moel Llyfnant, and is twin peaked. It lies to the west of Moel Llyfnant. The summit itself is situated on a rocky outcrop offering extensive views of the Rhinogs and Snowdonia to the north.

Geographic entities mentioned:
surface_form: Moel Llyfnant
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.900833333333
lon: -3.7730555555556
Gallt y Daren is a peak in the southern half of the Snowdonia National Park in Gwynedd, North Wales, and forms part of the Arenig mountain range. It is a top of Moel Llyfnant, and is twin peaked. It lies to the west of Moel Llyfnant. The summit itself is situated on a rocky outcrop offering extensive views of the Rhinogs and Snowdonia to the north. The peak is often known as Foel Boeth.

Geographic entities mentioned:
surface_form: Moel Llyfnant
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.900833333333
lon: -3.7730555555556
It lies to the west of Moel Llyfnant. The summit itself is situated on a rocky outcrop offering extensive views of the Rhinogs and Snowdonia to the north. The peak is often known as Foel Boeth. However, the Nuttall list includes both the twin tops resulting in the higher top being called Gallt y Daren and the lower top being called Foel Boeth (616m). It lies to the west of Moel Llyfnant.

Geographic entities mentioned:
surface_form: Moel Llyfnant
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.900833333333
lon: -3.7730555555556
Gallt y Daren. Gallt y Daren is a peak in the southern half of the Snowdonia National Park in Gwynedd, North Wales, and forms part of the Arenig mountain range. It is a top of Moel Llyfnant, and is twin peaked. It lies to the west of Moel Llyfnant. The summit itself is situated on a rocky outcrop offering extensive views of the Rhinogs and Snowdonia to the north.

Geographic entities mentioned:
surface_form: gallt y daren
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.89375
lon: -3.81709
It lies to the west of Moel Llyfnant. The summit itself is situated on a rocky outcrop offering extensive views of the Rhinogs and Snowdonia to the north. The peak is often known as Foel Boeth. However, the Nuttall list includes both the twin tops resulting in the higher top being called Gallt y Daren and the lower top being called Foel Boeth (616m). It lies to the west of Moel Llyfnant.

Geographic entities mentioned:
surface_form: gallt y daren
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.89375
lon: -3.81709
Malcolm Carr Collier. Malcolm Carr Collier (née, Malcolm Carr; 1908–1983) was an American anthropologist remembered for her work with the Navajo. She did field work at Grand Coulee Dam in the U.S. state of Washington in 1936, studied the Navaho in the Pueblo Alto site with Katherine Spencer and Doriane Wooley in 1937, and in 1938, conducted research in the Navajo Mountain area.

Geographic entities mentioned:
surface_form: Navajo Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.034169444444
lon: -110.86888888889
Sumayar Valley boasts numerous tourist attractions, including snowy mountains such as Dumani on the northeast side of Diran, Silkiyang Peak, Silkiyang Glacier, Altusill and Menamgusham meadows, Baraimochay Farimuch, Hayano camping sites, Mamubar stream, and the gemstone mining area known as Chumar Bakur.

Geographic entities mentioned:
surface_form: Diran
instance_of: Mountain
countries: Pakistan
coordinates: lat: 36.116666666667
lon: 74.666666666667
surface_form: sumayar
instance_of: Valley
coordinates: lat: 36.30436
lon: 74.64848
The famous aquamarine mining area Chumar Bakhoor is also situated in the Sumayar Valley. Geography. The valley is located at the confluence of the Hunza and Nagar rivers. It is surrounded by Nagarkhas from the east, Askurdas from the west, Ganesh from the north, and mountain ridges including Diran from the south. Geomorphology.

Geographic entities mentioned:
surface_form: Diran
instance_of: Mountain
countries: Pakistan
coordinates: lat: 36.116666666667
lon: 74.666666666667
Geomorphology. The valley exhibits an elevation of 2,000 m (6,600 ft) at its northern entrance and rises to over 7,000 m as one moves towards the south, covering a distance of approximately 15 km (9.3 mi). The highest peak in this region, Diran, stands at an elevation of 7,257 m (23,809 ft) and is situated in the southern section of the valley.

Geographic entities mentioned:
surface_form: Diran
instance_of: Mountain
countries: Pakistan
coordinates: lat: 36.116666666667
lon: 74.666666666667
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
Sumayar. Sumayar (Burushaski, Urdu:) is a small valley situated within the Nagar District of the Gilgit Division of Gilgit-Baltistan. The valley is located at the confluence of the Hunza River and the Nagar River. It is bounded by an eroded landscape to the north-east and mountain ridges to the south.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: sumayar
instance_of: Valley
coordinates: lat: 36.30436
lon: 74.64848
It is bounded by an eroded landscape to the north-east and mountain ridges to the south. The valley is composed of nine small villages: Khai, Futhkhai, Yal, Boshat, Rashfari, Resman, Daltho, Thopkhan, and Jotorkhan. It is located approximately 100 km (62 mi) away from Gilgit city, and it takes about one and a half hours to reach this valley.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
Sumayar. Sumayar (Burushaski, Urdu:) is a small valley situated within the Nagar District of the Gilgit Division of Gilgit-Baltistan. The valley is located at the confluence of the Hunza River and the Nagar River. It is bounded by an eroded landscape to the north-east and mountain ridges to the south.

Geographic entities mentioned:
surface_form: sumayar
instance_of: Valley
coordinates: lat: 36.30436
lon: 74.64848
The valley is composed of nine small villages: Khai, Futhkhai, Yal, Boshat, Rashfari, Resman, Daltho, Thopkhan, and Jotorkhan. It is located approximately 100 km (62 mi) away from Gilgit city, and it takes about one and a half hours to reach this valley. The nearby areas of Sumayar include Askurdas and Shayar, and collectively, they are referred to as SAS Valley.

Geographic entities mentioned:
surface_form: sumayar
instance_of: Valley
coordinates: lat: 36.30436
lon: 74.64848
The valley contains the reserves of various gems and minerals such as Aquamarine, Fluorite, Apatite, Calcite, and Quartz. The famous aquamarine mining area Chumar Bakhoor is also situated in the Sumayar Valley. Geography. The valley is located at the confluence of the Hunza and Nagar rivers.

Geographic entities mentioned:
surface_form: sumayar
instance_of: Valley
coordinates: lat: 36.30436
lon: 74.64848
At places, it is occupied with avalanches and materials from lateral moraines. The Middle part: The middle region of the valley is a narrow canyon that is flanked by high precipices, probably due to outcrop rock of the Sumayar granite. This part of the valley is mostly covered by deep snow during the winter. The Lower part: The Lower part is comparatively wide and open.

Geographic entities mentioned:
surface_form: sumayar
instance_of: Valley
coordinates: lat: 36.30436
lon: 74.64848
The depth of the &quot;Mamuber&quot; stream increases and flows as a single channel. Chumar Bakhoor (Chumar Bakur). Chumar Bakhoor is located at an elevation of in the Sumayar Valley of Nagar District, Gilgit-Baltistan, Pakistan. Geographically it is also closer to the Nagarkhas. The Chumar Bakhoor pass links the Sumayar valley with the Nagar Khas.

Geographic entities mentioned:
surface_form: sumayar
instance_of: Valley
coordinates: lat: 36.30436
lon: 74.64848
Chumar Bakhoor is located at an elevation of in the Sumayar Valley of Nagar District, Gilgit-Baltistan, Pakistan. Geographically it is also closer to the Nagarkhas. The Chumar Bakhoor pass links the Sumayar valley with the Nagar Khas. Walking from central Sumayar, it takes around 4 to 5 hours to reach the pegmatites that crop out on the western side of the mountain above 4000 meters elevation.

Geographic entities mentioned:
surface_form: sumayar
instance_of: Valley
coordinates: lat: 36.30436
lon: 74.64848
Spinel-law twins have also been found here in incredible sizes. Octahedral fluorite from the pegmatites of Chumar Bakhoor of Sumayar valley, Nagar district has been known for quite some time. Green, white to pink fluorite associated with gemmy aquamarine, and pale pink to dark orange-pink fluorapatite on muscovite druses from the Chumar Bakhoor have been reaching the market since 1984.

Geographic entities mentioned:
surface_form: sumayar
instance_of: Valley
coordinates: lat: 36.30436
lon: 74.64848
Mamubar serves as the principal stream, and several tributaries contribute to it. Geographically, the valley can be divided into three distinct geomorphological units: the upper part, the middle part, and the lower part. The Upper part: The upper and southern part of the valley is usually covered with ice and a glacier.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
The company is based in Waasen, in Neumarkt an der Ybbs in Lower Austria. The company was operated by the brothers Wüster and was primarily active in the steel and metal manufacturing business. In 1897 they also set up an electric power station in Ybbs. Wüster became one of the leading producers in Austria for umbrella frames.

Geographic entities mentioned:
surface_form: Ybbs
instance_of: Watercourse
countries: Austria
coordinates: lat: 47.7603
lon: 15.2053
Jach'a Quta (Murillo). __NOTOC__
Jach'a Quta (Aymara &quot;jach'a&quot; big, great, &quot;quta&quot; lake, &quot;great lake&quot;, hispanicized spelling &quot;Jacha Kkota&quot;) is a lake in Bolivia located in the La Paz Department, Pedro Domingo Murillo Province, Achocalla Municipality. It is situated south of El Alto and La Paz near Achocalla.

Geographic entities mentioned:
surface_form: jach'a quta
instance_of: Lake
countries: Bolivia
coordinates: lat: -16.487222222222222
lon: -67.8561111111111
surface_form: jach'a quta
instance_of: Lake
countries: Bolivia
coordinates: lat: -16.89638888888889
lon: -68.09944444444444
surface_form: jach'a quta (murillo)
instance_of: Lake
countries: Bolivia
coordinates: lat: -16.56666667
lon: -68.15
Jach'a Quta (Murillo). __NOTOC__
Jach'a Quta (Aymara &quot;jach'a&quot; big, great, &quot;quta&quot; lake, &quot;great lake&quot;, hispanicized spelling &quot;Jacha Kkota&quot;) is a lake in Bolivia located in the La Paz Department, Pedro Domingo Murillo Province, Achocalla Municipality. It is situated south of El Alto and La Paz near Achocalla.

Geographic entities mentioned:
surface_form: jach'a quta
instance_of: Lake
countries: Bolivia
coordinates: lat: -16.487222222222222
lon: -67.8561111111111
surface_form: jach'a quta
instance_of: Lake
countries: Bolivia
coordinates: lat: -16.89638888888889
lon: -68.09944444444444
surface_form: jach'a quta
instance_of: Lake
countries: Bolivia
coordinates: lat: -16.56666667
lon: -68.15
Gauff Hill, Pennsylvania. Gauff Hill is an unincorporated community in the extreme eastern Salisbury Township in Lehigh County, Pennsylvania. It is part of the Lehigh Valley, which has a population of 861,899 and was the 68th-most populous metropolitan area in the U.S. as of the 2020 census.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Did you not know his conduct before, [and] so you sent him?&quot;
Donald Crummey notes that &quot;his fate, even the circumstances of his death, are mysterious.&quot; A contemporary account, the Church Missionary Society's &quot;Missionary Register for 1828&quot; writes that he is said to be living &quot;in Tigré: he is said to be in a state of perpetual intoxication.&quot; Mordechai Abir writes that &quot;Ras&quot; Yimam banished him to the monastery in Lake Tana, where Qerellos remained until his death, although Abir also notes alternative accounts of Qerellos' death exist: &quot;Another version...

Geographic entities mentioned:
surface_form: Lake Tana
instance_of: Lake
countries: Ethiopia
coordinates: lat: 12
lon: 37.25
104 of these are state forest inspectors. Geography. The total area of Karkaraly National Park is 90,323 hectares, of which, 40,341 hectares are forested. The park is divided into three sections: the mountain section, the Karkaraly Range section, and the Kent Range section.

Geographic entities mentioned:
surface_form: Kent Range
instance_of: Mountain
countries: Kazakhstan
coordinates: lat: 49.224444444444444
lon: 76.03944444444444
Carcluie Loch. Carcluie Loch (NS 34894 16186) is a small freshwater loch in the South Ayrshire Council Area, lying in a glacial Kettle Hole, Parish of Dalrymple, Scotland. The loch. Blaeu's map of circa 1654 taken from Timothy Pont's map of circa 1600 shows Loch Luy and nearby the dwelling of Kar Cluy. In 1821 the farm was recorded as Kirklewy, but no loch shown.

Geographic entities mentioned:
surface_form: carcluie loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.4118
lon: -4.60942
It is intersected by the Wollondilly River and the Mulwaree River, and the confluence of these two rivers is also located here. The Wollondilly then flows north-east, into Lake Burragorang (Warragamba Dam) and eventually into the Tasman Sea via the Hawkesbury River. The city is located within the Southern Tablelands Temperate Grassland. Climate.

Geographic entities mentioned:
surface_form: Lake Burragorang
instance_of: Lake
countries: Australia
coordinates: lat: -34
lon: 150.43333333333
The clinic has a mixture of general practitioners and specialists that provide comprehensive healthcare. Water supply. With a history of water shortages, an underground water supply pipeline was constructed to pump water from the Wingecarribee Reservoir in the Southern Highlands to Goulburn, opening in 2011. This pipeline has a capacity of 7.5 ML per day.

Geographic entities mentioned:
surface_form: Wingecarribee Reservoir
instance_of: Lake
countries: Australia
Herbold was inducted into the Mountain Bike Hall of Fame in 1996. __TOC__
Mountain biking career. Herbold was born in Denver, Colorado. He won the first dual slalom race at Mammoth Mountain in 1987. A year later, &quot;Over the 1989 Labor Day weekend, September 2–4, around 1,500 mountain bike aficionados united under a blazing sun at Big Bear Lakes, CA, home of the NORBA National Championships...

Geographic entities mentioned:
surface_form: Mammoth Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6306
lon: -119.033
Lake Bonney Riverland. Lake Bonney Riverland (alternative name: Barmera) is a freshwater lake located in the Riverland region of South Australia. The lake is fed and drained by the River Murray. The town of Barmera is located on its shores. History. The original inhabitants were the Barmerara Meru clan of the Ngawadj people.

Geographic entities mentioned:
surface_form: freshwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.6453
lon: -60.3967
surface_form: lake bonney riverland
instance_of: Lake
countries: Australia
coordinates: lat: -34.2333
lon: 140.45
surface_form: barmera
instance_of: Lake
countries: Australia
coordinates: lat: -34.2333
lon: 140.45
Lake Bonney Riverland. Lake Bonney Riverland (alternative name: Barmera) is a freshwater lake located in the Riverland region of South Australia. The lake is fed and drained by the River Murray. The town of Barmera is located on its shores. History. The original inhabitants were the Barmerara Meru clan of the Ngawadj people.

Geographic entities mentioned:
surface_form: lake bonney
instance_of: Lake
countries: Australia
coordinates: lat: -34.2333
lon: 140.45
In response to the request sent in 1981, the Geographical Names Board renamed both lakes as &quot;Lake Bonney, Riverland&quot; and &quot;Lake Bonney SE&quot; in order “to differentiate between the lakes.”
In 2014, the South Australian government declared the lake to have the dual names of &quot;Lake Bonney Riverland&quot; / &quot;Barmera&quot; in response to a request from a group known as the &quot;First Peoples of the River Murray and Mallee Region&quot;.

Geographic entities mentioned:
surface_form: lake bonney
instance_of: Lake
countries: Australia
coordinates: lat: -34.2333
lon: 140.45
surface_form: barmera
instance_of: Lake
countries: Australia
coordinates: lat: -34.2333
lon: 140.45
surface_form: lake bonney
instance_of: Lake
countries: Australia
coordinates: lat: -34.2333
lon: 140.45
surface_form: lake bonney
instance_of: Lake
countries: Australia
coordinates: lat: -34.2333
lon: 140.45
Lake Bonney Riverland. Lake Bonney Riverland (alternative name: Barmera) is a freshwater lake located in the Riverland region of South Australia. The lake is fed and drained by the River Murray. The town of Barmera is located on its shores. History. The original inhabitants were the Barmerara Meru clan of the Ngawadj people.

Geographic entities mentioned:
surface_form: barmera
instance_of: Lake
countries: Australia
coordinates: lat: -34.2333
lon: 140.45
Naming. The lake was named Lake Bonney by Joseph Hawdon after his friend, Charles Bonney in 1838. The name was changed to &quot;Lake Barmera, River Murray&quot; in 1908 and was changed back to &quot;Lake Bonney&quot; in 1913 &quot;for historic reasons&quot;. A subsequent proposal to rename the lake as &quot;Lake Barmera&quot; did not proceed.

Geographic entities mentioned:
surface_form: barmera
instance_of: Lake
countries: Australia
coordinates: lat: -34.2333
lon: 140.45
surface_form: lake bonney
instance_of: Lake
countries: Australia
coordinates: lat: -34.2333
lon: 140.45
Naming. The lake was named Lake Bonney by Joseph Hawdon after his friend, Charles Bonney in 1838. The name was changed to &quot;Lake Barmera, River Murray&quot; in 1908 and was changed back to &quot;Lake Bonney&quot; in 1913 &quot;for historic reasons&quot;. A subsequent proposal to rename the lake as &quot;Lake Barmera&quot; did not proceed.

Geographic entities mentioned:
surface_form: barmera
instance_of: Lake
countries: Australia
coordinates: lat: -34.2333
lon: 140.45
A subsequent proposal to rename the lake as &quot;Lake Barmera&quot; did not proceed. A lake located in the south east of the state near the continental coastline in what is now the gazetted locality of Canunda was also named as &quot;Lake Bonney&quot; after the same Charles Bonney in 1844 by George Grey, the then Governor of South Australia.

Geographic entities mentioned:
surface_form: lake bonney
instance_of: Lake
countries: Australia
coordinates: lat: -34.2333
lon: 140.45
When Charles Sturt passed by in 1844 on his expedition into the interior of Australia, he surveyed Lake Bonney for the first time, as well as the creek connecting it to the River Murray. James Collins Hawker, then residing at Moorundie, assisted Sturt’s surveyor Poole.

Geographic entities mentioned:
surface_form: lake bonney
instance_of: Lake
countries: Australia
coordinates: lat: -34.2333
lon: 140.45
The regulator was removed in December 2010 and this, with wet summer and winter rains restored it to normal levels by April 2011. Naming. The lake was named Lake Bonney by Joseph Hawdon after his friend, Charles Bonney in 1838. The name was changed to &quot;Lake Barmera, River Murray&quot; in 1908 and was changed back to &quot;Lake Bonney&quot; in 1913 &quot;for historic reasons&quot;.

Geographic entities mentioned:
surface_form: lake bonney
instance_of: Lake
countries: Australia
coordinates: lat: -34.2333
lon: 140.45
Castellini Baldissera. The Castellini Baldissera are an Italian family, originating from Milan and Brescia. History. The Castellini Baldissera family's ancestral seat is the 18th-century Villa Castellini or Villa Grande, on Lago Maggiore, and the 14th-century Casa Atellani in Milan. The family is still active in banking, real estate, and textile production in Italy.

Geographic entities mentioned:
surface_form: Lago Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
Around the same time she began studying the Langdale axe industry in Cumbria, the project for which she is perhaps best remembered. She was not the first person to notice that Neolithic axes had been produced in Great Langdale, but she was able to demonstrate the scale of the activity there, and used the word &quot;factory&quot; to describe it.

Geographic entities mentioned:
surface_form: Great Langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.449119444444
lon: -3.0733305555556
Location. The town is situated along the Kampala–Masaka Road, approximately, southwest of Kampala, Uganda's capital and largest city. This location is approximately, north of Lake Victoria, at the point where River Katonga, exits the lake to begin its journey west to Lake George. The coordinates of Nkozi town are:00 00 36N, 32 00 00E (Latitude:0.0100; Longitude:32.0000). Population.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
He contemplated making a hit-and-run attack across the frozen Lake Erie against the British position at Amherstburg in Upper Canada and moved to the mouth of the Maumee, but found that the ice on the frozen lake was already breaking up and returned to the half-finished fort. He found the officer he had left in charge, Joel B.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Lake Michigan–Huron. Lake Michigan–Huron (also Huron–Michigan) is the body of water combining Lake Michigan and Lake Huron, which are joined through the, open-water Straits of Mackinac. Huron and Michigan are hydrologically a single lake because the flow of water through the straits keeps their water levels in overall equilibrium.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: michigan–huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 45.813888888889
lon: -84.753888888889
surface_form: lake michigan–huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 45.813888888889
lon: -84.753888888889
Although the flow is generally eastward, the water moves in either direction depending on local conditions. Combined, Lake Michigan–Huron is the largest freshwater lake by area in the world. Lake Superior is larger than either individually, so it is counted as the largest of the Great Lakes when Lake Michigan and Lake Huron are considered separately. Geologic history.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
surface_form: huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: lake huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Clair River were cut off around 4,000 years ago. The current configuration of the lakes reflects the latest step in a long history of their post-glacial evolution. Bathymetry and hydrology. The connection between Lake Michigan and Lake Huron through the Straits of Mackinac is wide and deep. This depth compares with the maximum depths of in Lake Huron and in Lake Michigan.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Because of the link through the Straits, Lakes Michigan and Huron have the same mean water level (in June 2015 it was). The largest inflow to the system is the St. Mary's River from Lake Superior, and the main outflow is the St. Clair River toward Lake Erie; both lie in the Lake Huron basin.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
surface_form: erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
surface_form: huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: lake huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
surface_form: st. clair
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.450265
lon: -82.67572
Lake Michigan–Huron. Lake Michigan–Huron (also Huron–Michigan) is the body of water combining Lake Michigan and Lake Huron, which are joined through the, open-water Straits of Mackinac. Huron and Michigan are hydrologically a single lake because the flow of water through the straits keeps their water levels in overall equilibrium.

Geographic entities mentioned:
surface_form: huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: michigan–huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 45.813888888889
lon: -84.753888888889
surface_form: lake michigan–huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 45.813888888889
lon: -84.753888888889
Lake Michigan–Huron. Lake Michigan–Huron (also Huron–Michigan) is the body of water combining Lake Michigan and Lake Huron, which are joined through the, open-water Straits of Mackinac. Huron and Michigan are hydrologically a single lake because the flow of water through the straits keeps their water levels in overall equilibrium.

Geographic entities mentioned:
surface_form: huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Although the flow is generally eastward, the water moves in either direction depending on local conditions. Combined, Lake Michigan–Huron is the largest freshwater lake by area in the world. Lake Superior is larger than either individually, so it is counted as the largest of the Great Lakes when Lake Michigan and Lake Huron are considered separately. Geologic history.

Geographic entities mentioned:
surface_form: huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: michigan–huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 45.813888888889
lon: -84.753888888889
surface_form: lake michigan–huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 45.813888888889
lon: -84.753888888889
Numerous proglacial lakes formed in various places and configurations as the ice sheet advanced and retreated. At various times, what is now Michigan–Huron was clearly separated into two or more lakes, and at other times was part of a single, deeper lake.

Geographic entities mentioned:
surface_form: huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: michigan–huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 45.813888888889
lon: -84.753888888889
At various times, what is now Michigan–Huron was clearly separated into two or more lakes, and at other times was part of a single, deeper lake. Around 9,000 years BC, as the ice sheet retreated, the modern Lakes Huron, Michigan, and much of Superior, were a single lake known to geologists as Lake Algonquin. Ice sheets dammed Lake Algonquin to the northeast.

Geographic entities mentioned:
surface_form: huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Lake Algonquin and Lake Chicago both drained south into the Mississippi River watershed. Around 9,500 years ago, new pathways draining the system to the east were opened by the retreat of the ice, and proglacial Lake Stanley (precursor of Lake Huron) was separated from proglacial Lake Chippewa (precursor of Lake Michigan), with Lake Chippewa at a slightly higher level.

Geographic entities mentioned:
surface_form: huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: lake huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
They were connected by the now-submerged Mackinac Channel, which discharged into Lake Stanley over Mackinac Falls. Ongoing warping of the land by post-glacial rebound due to the retreat of the glacial ice continued to modify the drainage structure of the region, allowing the reunification of all three basins (Superior, Michigan, and Huron) as the Nipissing Great Lakes.

Geographic entities mentioned:
surface_form: huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Clair River were cut off around 4,000 years ago. The current configuration of the lakes reflects the latest step in a long history of their post-glacial evolution. Bathymetry and hydrology. The connection between Lake Michigan and Lake Huron through the Straits of Mackinac is wide and deep. This depth compares with the maximum depths of in Lake Huron and in Lake Michigan.

Geographic entities mentioned:
surface_form: huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: lake huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Although the Straits create a pronounced bottleneck in the contours of the shoreline and a major constriction in the local bathymetry, defining two distinct basins, they are still deep and wide enough to allow the free exchange of water between the two sides. Because of the link through the Straits, Lakes Michigan and Huron have the same mean water level (in June 2015 it was).

Geographic entities mentioned:
surface_form: huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Constituent lakes. Compared to the water basins it connects, the wide and deep Straits of Mackinac appear relatively small. Thus by historical naming convention, Lake Michigan and Lake Huron are usually considered distinct, e.g. in lists of the largest lakes in the world by area and volume. In the context of hydrology, however, the two are one body of water.

Geographic entities mentioned:
surface_form: huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: lake huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
In the context of hydrology, however, the two are one body of water. Because of the hydrologic connectivity through the Straits, some sources consider the total area and volume of Lake Michigan–Huron when placing this system in a global or regional context. When Lake Michigan–Huron is treated as a single entity, it is the largest freshwater lake by surface area in the world.

Geographic entities mentioned:
surface_form: huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: michigan–huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 45.813888888889
lon: -84.753888888889
surface_form: lake michigan–huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 45.813888888889
lon: -84.753888888889
However, the long-term average flow through the Straits is eastwards at, toward the outlet of the St. Clair River. Flows into the system from Lake Superior are controlled by the bi-national Lake Superior Board of Control through the operation of locks and canals. Constituent lakes. Compared to the water basins it connects, the wide and deep Straits of Mackinac appear relatively small.

Geographic entities mentioned:
surface_form: superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
surface_form: superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
surface_form: lake superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
surface_form: lake superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Ongoing warping of the land by post-glacial rebound due to the retreat of the glacial ice continued to modify the drainage structure of the region, allowing the reunification of all three basins (Superior, Michigan, and Huron) as the Nipissing Great Lakes. This arrangement was probably stable for more than 1,000 years, ending only when lake outlets other than the St.

Geographic entities mentioned:
surface_form: st. clair
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.450265
lon: -82.67572
However, the long-term average flow through the Straits is eastwards at, toward the outlet of the St. Clair River. Flows into the system from Lake Superior are controlled by the bi-national Lake Superior Board of Control through the operation of locks and canals. Constituent lakes. Compared to the water basins it connects, the wide and deep Straits of Mackinac appear relatively small.

Geographic entities mentioned:
surface_form: st. clair
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.450265
lon: -82.67572
New Gisborne. New Gisborne is a suburb of Gisborne in Victoria, Australia, in the foothills of Mount Macedon in the Shire of Macedon Ranges. The Gisborne railway station on the Bendigo line is located in New Gisborne, and a bus service connects residents of the two towns between the railway station and the Gisborne town centre. At the 2011 census, New Gisborne had a population of 2,380.

Geographic entities mentioned:
surface_form: Mount Macedon
instance_of: Mountain
countries: Australia
coordinates: lat: -37.38291
lon: 144.57625
The Lippisch Ente (meaning “duck” in German), the world's first rocket-powered glider and piloted for its first flight on June 11, 1928, by Fritz Stamer at Wasserkuppe, was bought and operated by Opel in context of the Opel RAK program but is not formally designated an Opel RAK series number.

Geographic entities mentioned:
surface_form: Wasserkuppe
instance_of: Mountain
countries: Germany
coordinates: lat: 50.498055555556
lon: 9.9377777777778
Opel RAK rocket planes. After testing at Wasserkuppe, in June 1928, Fritz von Opel had purchased an Alexander Lippisch-designed sailplane, the Ente, and fitted it with rockets. Fritz Stamer was the pilot during the OPEL RAK experimentations with Lippisch's design. Opel did not get the chance to fly it, however, as the aircraft was destroyed by an engine explosion on its second test flight.

Geographic entities mentioned:
surface_form: Wasserkuppe
instance_of: Mountain
countries: Germany
coordinates: lat: 50.498055555556
lon: 9.9377777777778
Mont Glacier. Mont Glacier is a mountain in the Graian Alps, in the Aosta Valley, north-western Italy, approximately 30 km / 19 miles for the border with Switzerland. It has an elevation of 3,185 m. Part of the Gran Paradiso massif, it commands the valleys and the communes of Champorcher and Champdepraz.

Geographic entities mentioned:
surface_form: mont glacier
instance_of: Mountain
countries: Italy
coordinates: lat: 45.63166667
lon: 7.53944444
Before it was dried and turned into a thoroughfare, as many other canals and rivers in Mexico City, the Canal de San Juan (San Juan Channel) connected Texcoco and Xochimilco. Because of this, the pictogram for the station depicts the bow of an Aztec canoe travelling through a canal, commonly associated to the way the Aztecs used to travel along the canals in the Valley of Mexico.

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
Transport. Lying in the Great Glen, Spean Bridge has road links north towards Inverness and south to Fort William, provided by the A82, and the A86 heads east to join the A9 at Kingussie. The village is served also served by Spean Bridge railway station providing links to Glasgow, London, and Mallaig. Between 1903 and 1933 it offered a branch line service to Fort Augustus. Sport.

Geographic entities mentioned:
surface_form: Great Glen
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
Acantilados de Los Gigantes. Acantilados de Los Gigantes (&quot;Cliffs of the Giants&quot;) are vertical cliffs along the western coast of Tenerife. They are vertical walls reaching heights of 500 metres in some places. They are a basaltic geological feature. In times of the Guanches they were known as the &quot;Wall of Hell&quot; (Muralla del Infierno). Tourism.

Geographic entities mentioned:
surface_form: acantilados de los gigantes
instance_of: Mountain
countries: Spain
coordinates: lat: 28.296521
lon: -16.855774
Beldore Hollow, Virginia. Beldore Hollow, Virginia (also referred to as &quot;Beldor&quot; and spelled &quot;Beldor Hollow&quot;) is an extinct unincorporated community in Rockingham County, Virginia. The Beldore Hollow community included homesteads, farms, cemeteries, a one-room school, and a village in the mountains of the Shenandoah Valley.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Moncton. Moncton (;) is the most populous city in the Canadian province of New Brunswick. Situated in the Petitcodiac River Valley, it lies at the geographic centre of the Maritime Provinces. The city has earned the nickname &quot;Hub City&quot; because of its central inland location in the region and its history as a railway and land transportation hub for the Maritimes.

Geographic entities mentioned:
surface_form: Petitcodiac River
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.926944444444
lon: -65.188888888889
History. Acadians settled the head of the Bay of Fundy in the 1670s. The first reference to the &quot;Petcoucoyer River&quot; was on the De Meulles map of 1686. Settlement of the Petitcodiac and Memramcook river valleys began about 1700, gradually extending inland and reaching the site of present-day Moncton in 1733.

Geographic entities mentioned:
surface_form: Petitcodiac
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.926944444444
lon: -65.188888888889
In the late 17th century the mountains were scouted by Spanish explorers who gave it its modern name. They translated the native Apache and Yavapai terms for the mountains as &quot;Pinal&quot; or Pine Mountains. Later still, in the mid-19th century, the U.S. Army scouted the mountains, and used Signal Peak as a heliograph station, which is how that peak got its name.

Geographic entities mentioned:
surface_form: signal peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.3197
lon: -113.492
surface_form: signal peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.3338
lon: -123.554
surface_form: signal peak
instance_of: Mountain
countries: United States
coordinates: lat: 33.6061
lon: -117.812
Pinal Peak. Pinal Peak, located in southern Gila County, Arizona, is the highest point in the Pinal Mountains, with an elevation of. It is the highest point of land located in between the Salt and Gila rivers in Arizona before they merge, making it visible from miles away on a clear day.

Geographic entities mentioned:
surface_form: pinal peak
instance_of: Mountain
countries: United States
coordinates: lat: 33.28235661
lon: -110.82123282