Sarmila/GeoWiki-Features huggingface dataset:
They named this mountain after Sir David Rivett, Deputy Chairman and Chief Executive Officer of the Australian Council for Scientific and Industrial Research, 1927–45. See also. Lawson Aiguilles, a line of sharp peaks in the south part of Mount Rivett

Geographic entities mentioned:
surface_form: Lawson Aiguilles
instance_of: Mountain
coordinates: lat: -67.8333
lon: 66.25
surface_form: mount rivett
instance_of: Mountain
coordinates: lat: -67.8333
lon: 66.2333
surface_form: rivett
instance_of: Mountain
coordinates: lat: -67.8333
lon: 66.2333
Mount Rivett. Mount Rivett () is a bare rock mountain, the northeasternmost feature of the Gustav Bull Mountains in Mac. Robertson Land, Antarctica. On February 13, 1931, the British Australian New Zealand Antarctic Research Expedition (BANZARE) (1929–31) under Douglas Mawson made a landing on nearby Scullin Monolith.

Geographic entities mentioned:
surface_form: bull
instance_of: Mountain
coordinates: lat: -65.0833
lon: -60.3833
surface_form: mount rivett
instance_of: Mountain
coordinates: lat: -67.8333
lon: 66.2333
surface_form: rivett
instance_of: Mountain
coordinates: lat: -67.8333
lon: 66.2333
Mount Rivett. Mount Rivett () is a bare rock mountain, the northeasternmost feature of the Gustav Bull Mountains in Mac. Robertson Land, Antarctica. On February 13, 1931, the British Australian New Zealand Antarctic Research Expedition (BANZARE) (1929–31) under Douglas Mawson made a landing on nearby Scullin Monolith.

Geographic entities mentioned:
surface_form: mount rivett
instance_of: Mountain
coordinates: lat: -67.8333
lon: 66.2333
surface_form: rivett
instance_of: Mountain
coordinates: lat: -67.8333
lon: 66.2333
Robertson Land, Antarctica. On February 13, 1931, the British Australian New Zealand Antarctic Research Expedition (BANZARE) (1929–31) under Douglas Mawson made a landing on nearby Scullin Monolith. They named this mountain after Sir David Rivett, Deputy Chairman and Chief Executive Officer of the Australian Council for Scientific and Industrial Research, 1927–45. See also.

Geographic entities mentioned:
surface_form: rivett
instance_of: Mountain
coordinates: lat: -67.8333
lon: 66.2333
Whitewater Draw has its source at an elevation of 8,520 feet at in Rucker Canyon in the Chiricahua Mountains in the Coronado National Forest and flows generally westward, skirting the north end of the Swisshelm Mountains, then southwest and south through Sulphur Springs Valley into Mexico at Douglas, Arizona and Agua Prieta to, Sonora, Mexico.

Geographic entities mentioned:
surface_form: Rucker Canyon
instance_of: Valley
countries: United States
coordinates: lat: 31.7529
lon: -109.43
surface_form: Sulphur Springs Valley
instance_of: Valley
countries: United States
coordinates: lat: 32.4987
lon: -110.031
There it flows southward as Rio de Agua Prieta then southeast to join the Rio de San Bernardino at an elevation of, at La Junta de los Rios about 24.5 miles southeast of Douglas, Arizona. The San Bernardino River joins the Bavispe River at Morelos, Sonora at the northern end of the Sierra del Tigre.

Geographic entities mentioned:
surface_form: Sierra del Tigre
instance_of: Mountain
countries: Mexico
coordinates: lat: 30.59
lon: -109.19
Some channels lie near volcanic areas. When hot subsurface molten rock comes close to this ice, large amounts of liquid water and mud may be formed. Hrad Vallis in the Cebrenia quadrangle is close to Elysium Mons, a large volcano, which may have supplied water to create the channel. Hrad Vallis is pictured below. Galaxias region. The ground in Galaxias seems to have collapsed.

Geographic entities mentioned:
surface_form: Hrad Vallis
instance_of: Valley
coordinates: lat: 38.17
lon: 135.91
Tian Shan. The Tian Shan, also known as the Tengri Tagh or Tengir-Too, is a large system of mountain ranges in Central Asia. The highest peak is Jengish Chokusu at high and located in Kyrgyzstan. Its lowest point is at the Turpan Depression, which is below sea level. The Tian Shan is sacred in Tengrism.

Geographic entities mentioned:
surface_form: Jengish Chokusu
instance_of: Mountain
countries: Kyrgyzstan
People's Republic of China
coordinates: lat: 42.034662
lon: 80.128713
Its lowest point is at the Turpan Depression, which is below sea level. The Tian Shan is sacred in Tengrism. Its second-highest peak is known as Khan Tengri, which can be translated as &quot;Lord of the Spirits&quot;. At the 2013 Conference on World Heritage, the eastern portion of Tian Shan in western China's Xinjiang Region was listed as a World Heritage Site.

Geographic entities mentioned:
surface_form: Khan Tengri
instance_of: Mountain
countries: Kyrgyzstan
Kazakhstan
People's Republic of China
Russian Empire
Soviet Union
coordinates: lat: 42.210833333333
lon: 80.175
The range encompasses the Bogda Shan in the east, as defined by both Western and Chinese cartography. The Tian Shan's highest peak is Jengish Chokusu (also known as Victory Peak), shared by Kyrgyzstan and China. At high, it is the highest point in Kyrgyzstan.

Geographic entities mentioned:
surface_form: Jengish Chokusu
instance_of: Mountain
countries: Kyrgyzstan
People's Republic of China
coordinates: lat: 42.034662
lon: 80.128713
The Tian Shan's highest peak is Jengish Chokusu (also known as Victory Peak), shared by Kyrgyzstan and China. At high, it is the highest point in Kyrgyzstan. The Tian Shan's second highest peak, Khan Tengri (King Heaven), straddles the Kazakhstan-Kyrgyzstan-China tripoint and at, is the highest point of Kazakhstan. Mountaineers class these as the two northernmost peaks surpassing in the world.

Geographic entities mentioned:
surface_form: Khan Tengri
instance_of: Mountain
countries: Kyrgyzstan
Kazakhstan
People's Republic of China
Russian Empire
Soviet Union
coordinates: lat: 42.210833333333
lon: 80.175
The Torugart Pass, at, marks the border between Kyrgyzstan and Xinjiang. The lower-altitude, forested Alatau ranges in the northern Tian Shan is home to Turkic-speaking pastoral tribes. The Tian Shan is separated from the Tibetan Plateau by the Taklimakan Desert and the Tarim Basin to the south. The Syr Darya, Ili River and Tarim River that originate in the Tian Shan.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
In Kyrgyzstan the mainline of the Tian Shan continues as Narat Range from the base of the Borohoros west to the point where China, Kazakhstan, and Kyrgyzstan meet. Here is the highest part of the range – the Central Tian Shan, with Peak Pobeda (Kakshaal Too range) and Khan Tengri. West of this, the Tian Shan split into an 'eye', with Issyk Kul Lake in its center.

Geographic entities mentioned:
surface_form: Khan Tengri
instance_of: Mountain
countries: Kyrgyzstan
Kazakhstan
People's Republic of China
Russian Empire
Soviet Union
coordinates: lat: 42.210833333333
lon: 80.175
At the east end of the Talas Alatau the Suusamyr Too range runs southeast enclosing the Suusamyr Valley or plateau. As for the area south of the Fergana Valley there is an group of mountains that curves west-southwest from south of Issyk Kul Lake separating the Tarim Basin from the Fergana Valley.

Geographic entities mentioned:
surface_form: Suusamyr Too
instance_of: Mountain
countries: Kyrgyzstan
coordinates: lat: 42.13
lon: 73.25
surface_form: Suusamyr Valley
instance_of: Valley
countries: Kyrgyzstan
coordinates: lat: 42.1941
lon: 73.5612
At the east end of the Talas Alatau the Suusamyr Too range runs southeast enclosing the Suusamyr Valley or plateau. As for the area south of the Fergana Valley there is an group of mountains that curves west-southwest from south of Issyk Kul Lake separating the Tarim Basin from the Fergana Valley.

Geographic entities mentioned:
surface_form: Fergana Valley
instance_of: Valley
countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
lon: 71.757777777778
surface_form: Fergana Valley
instance_of: Valley
countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
lon: 71.757777777778
Sima Qian, in the &quot;Records of the Grand Historian&quot;, mentioned &quot;Qilian&quot; in relation to the homeland of the Yuezhi, and the term is believed to refer to the Tian Shan rather than the range further east now known as the Qilian Mountains. The name of the Otgontenger in Mongolia has the same meaning.

Geographic entities mentioned:
surface_form: Otgontenger
instance_of: Mountain
countries: Mongolia
coordinates: lat: 47.636708333333
lon: 97.502288888889
Collections. There is a Fred Verity boiler in the National Trust's collection, at the Farmhouse & Outhouse, Brighouse Farm, Duddon Valley, Cumbria. This is a World Heritage Site: The English Lake District (1452615).

Geographic entities mentioned:
surface_form: Duddon Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.297688888889
lon: -3.2347888888889
Karoh Peak. Karoh Peak is a tall mountain peak in the Sivalik Hills range of greater Himalayas range located near Morni Hills area of Panchkula district, Haryana, India. It is the highest point in the state of Haryana.

Geographic entities mentioned:
surface_form: hills
instance_of: Mountain
countries: India
coordinates: lat: 23.166666666667
lon: 92.833333333333
surface_form: hills
instance_of: Mountain
countries: India
coordinates: lat: 23.166666666667
lon: 92.833333333333
surface_form: karoh peak
instance_of: Mountain
countries: India
coordinates: lat: 30.74361111
lon: 77.07694444
Karoh Peak. Karoh Peak is a tall mountain peak in the Sivalik Hills range of greater Himalayas range located near Morni Hills area of Panchkula district, Haryana, India. It is the highest point in the state of Haryana.

Geographic entities mentioned:
surface_form: karoh peak
instance_of: Mountain
countries: India
coordinates: lat: 30.74361111
lon: 77.07694444
Beartrap Hollow. Beartrap Hollow (also known as Bear Trap Hollow) is a tributary of White Deer Hole Creek in Lycoming County, Pennsylvania, in the United States. It is approximately long and flows through Washington Township. The watershed of the stream has an area of. The stream is not designated as an impaired waterbody.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Much of the stream's length is on South White Deer Ridge and it is near Tiadaghton State Forest. Course. Beartrap Hollow begins on South White Deer Ridge in Washington Township. It flows north down the ridge for several tenths of a mile before turning north-northwest. After several tenths of a mile, the stream reaches the bottom of the ridge and receives an unnamed tributary from the left.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: beartrap hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.11916
lon: -77.03053
Beartrap Hollow. Beartrap Hollow (also known as Bear Trap Hollow) is a tributary of White Deer Hole Creek in Lycoming County, Pennsylvania, in the United States. It is approximately long and flows through Washington Township. The watershed of the stream has an area of. The stream is not designated as an impaired waterbody.

Geographic entities mentioned:
surface_form: beartrap hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.11916
lon: -77.03053
After several tenths of a mile, the stream reaches the bottom of the ridge and receives an unnamed tributary from the left. It then turns northeast for a short distance before reaching its confluence with White Deer Hole Creek. Beartrap Hollow joins White Deer Hole Creek upstream of its mouth. Tributaries. Beartrap Hollow has no named tributaries. However, it does have one unnamed tributary.

Geographic entities mentioned:
surface_form: beartrap hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.11916
lon: -77.03053
It then turns northeast for a short distance before reaching its confluence with White Deer Hole Creek. Beartrap Hollow joins White Deer Hole Creek upstream of its mouth. Tributaries. Beartrap Hollow has no named tributaries. However, it does have one unnamed tributary. This tributary is approximately long and starts lower on South White Deer Ridge than the main stem.

Geographic entities mentioned:
surface_form: beartrap hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.11916
lon: -77.03053
Beartrap Hollow has no named tributaries. However, it does have one unnamed tributary. This tributary is approximately long and starts lower on South White Deer Ridge than the main stem. It joins Beartrap Hollow in its lower reaches. Hydrology, geography, and geology. The elevation near the mouth of Beartrap Hollow is above sea level. The elevation near the stream's source is above sea level.

Geographic entities mentioned:
surface_form: beartrap hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.11916
lon: -77.03053
This tributary is approximately long and starts lower on South White Deer Ridge than the main stem. It joins Beartrap Hollow in its lower reaches. Hydrology, geography, and geology. The elevation near the mouth of Beartrap Hollow is above sea level. The elevation near the stream's source is above sea level. The headwaters of Beartrap Hollow are on a ridge known as South White Deer Ridge.

Geographic entities mentioned:
surface_form: beartrap hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.11916
lon: -77.03053
The elevation near the mouth of Beartrap Hollow is above sea level. The elevation near the stream's source is above sea level. The headwaters of Beartrap Hollow are on a ridge known as South White Deer Ridge. The ridge is relatively steep in the stream's upper reaches, but becomes less steep towards the lower reaches of the stream. It flows down into the broad valley of White Deer Hole Creek.

Geographic entities mentioned:
surface_form: beartrap hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.11916
lon: -77.03053
The ridge is relatively steep in the stream's upper reaches, but becomes less steep towards the lower reaches of the stream. It flows down into the broad valley of White Deer Hole Creek. Beartrap Hollow is in the Ridge and Valley Freestone region. Beartrap Hollow is not designated as an impaired waterbody. Watershed and biology. The watershed of Beartrap Hollow has an area of.

Geographic entities mentioned:
surface_form: beartrap hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.11916
lon: -77.03053
It flows down into the broad valley of White Deer Hole Creek. Beartrap Hollow is in the Ridge and Valley Freestone region. Beartrap Hollow is not designated as an impaired waterbody. Watershed and biology. The watershed of Beartrap Hollow has an area of. The stream is entirely within the United States Geological Survey quadrangle of Williamsport SE. Its mouth is located near Elmsport.

Geographic entities mentioned:
surface_form: beartrap hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.11916
lon: -77.03053
The stream is entirely within the United States Geological Survey quadrangle of Williamsport SE. Its mouth is located near Elmsport. Beartrap Hollow is being considered by the Pennsylvania Fish and Boat Commission for wild trout designation. History and recreation. The valley of Beartrap Hollow was entered into the Geographic Names Information System on August 2, 1979.

Geographic entities mentioned:
surface_form: beartrap hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.11916
lon: -77.03053
Its mouth is located near Elmsport. Beartrap Hollow is being considered by the Pennsylvania Fish and Boat Commission for wild trout designation. History and recreation. The valley of Beartrap Hollow was entered into the Geographic Names Information System on August 2, 1979. Its identifier in the Geographic Names Information System is 1168978.

Geographic entities mentioned:
surface_form: beartrap hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.11916
lon: -77.03053
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 stream does not have a name of its own, but instead takes its name from the valley through which it flows. It is also known as Bear Trap Hollow. Beartrap Hollow was surveyed by the Pennsylvania Fish and Boat Commission on June 14, 2013. It was listed on the Pennsylvania Fish and Boat Commission website as being considered for wild trout designation on January 20, 2015.

Geographic entities mentioned:
surface_form: beartrap hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.11916
lon: -77.03053
It is also known as Bear Trap Hollow. Beartrap Hollow was surveyed by the Pennsylvania Fish and Boat Commission on June 14, 2013. It was listed on the Pennsylvania Fish and Boat Commission website as being considered for wild trout designation on January 20, 2015. Beartrap Hollow is located near Tiadaghton State Forest.

Geographic entities mentioned:
surface_form: beartrap hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.11916
lon: -77.03053
History and recreation. The valley of Beartrap Hollow was entered into the Geographic Names Information System on August 2, 1979. Its identifier in the Geographic Names Information System is 1168978. The stream does not have a name of its own, but instead takes its name from the valley through which it flows. It is also known as Bear Trap Hollow.

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
On November 28, 1949, Žerjav married Carlo Abarth, the well-known Turin automobile industrialist. Abarth-Žerjav and Carlo Abarth met in 1944 at Lake Garda in Italy. They may have even met earlier, during the war in Ljubljana, because Abarth lived there for several years. He worked at Vok, a small local factory.

Geographic entities mentioned:
surface_form: Lake Garda
instance_of: Lake
countries: Italy
coordinates: lat: 45.633333333333
lon: 10.666666666667
Penck Glacier. Penck Glacier () is a small glacier flowing northward along the west side of Bertrab Nunatak to Vahsel Bay. Discovered by the German Antarctic Expedition, 1911–12, under Wilhelm Filchner, who named this feature for German geographer Albrecht Penck.

Geographic entities mentioned:
surface_form: Bertrab Nunatak
instance_of: Mountain
coordinates: lat: -77.9167
lon: -34.5333
There used to be a 70-metre-long tunnel on a curve near the former Gmundbrücke station at Tristram Gorge. Its profile was too restrictive to allow the introduction of 4-axle carriages, so in 1933/34 it was opened out to form a cutting. From 1909 to 1965 there was a connection at the end of the line at Berchtesgaden to the to the lake of Königssee.

Geographic entities mentioned:
surface_form: Königssee
instance_of: Lake
countries: Germany
coordinates: lat: 47.55
lon: 12.975
Mongolian language. Mongolian is the principal language of the Mongolic language family that originated in the Mongolian Plateau. It is spoken by ethnic Mongols and other closely related Mongolic peoples who are native to modern Mongolia and surrounding parts of East, Central and North Asia.

Geographic entities mentioned:
surface_form: Mongolian Plateau
instance_of: Plateau
countries: Mongolia
People's Republic of China
Russia
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 107
Together, these features formed the Gustav Line. Monte Cassino, a historic hilltop abbey founded in AD 529 by Benedict of Nursia, dominated the nearby town of Cassino and the entrances to the Liri and Rapido valleys. Lying in a protected historic zone, it had been left unoccupied by the Germans. They had defended some positions set into the steep slopes below the abbey's walls.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
The 2009 procession assembled on Bruntsfield Links and travelled along the following route: Bruntsfield Links – Whitehouse Loan – Bruntsfield Place – Glengyle Terrace – Leven Terrace – Melville Drive – Middle Meadow Walk crossing The Meadows (park) – Forest Road – George IV Bridge – The High Street AKA The Royal Mile – North Bridge – Waterloo Place – Regent Road – Calton Hill access road – to the summit of Calton Hill.

Geographic entities mentioned:
surface_form: Calton Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.955278
lon: -3.182222
Former MSP and MP Donald Gorrie, whose aunts Belle and Mary Gorrie played Mary Queen of Scots and Catherine Barlass in the original parade, also took part. Councillors joined the procession at this point and walked to Calton Hill where the Minister for Education, Fiona Hyslop MSP spoke on behalf of the Scottish Government.

Geographic entities mentioned:
surface_form: Calton Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.955278
lon: -3.182222
His elder brother sold tobacco while he studied and worked as a tutor. From 17141719, he taught the wealthy brothers Wang Hang (, &quot;Wāng Hàng&quot;, 17041784) and Wang Pu (). A poem by Wang Hang was later responsible for the naming of Yangzhou's Slender West Lake. In 1720 Li passed the imperial examination for the &quot;juren&quot; degree.

Geographic entities mentioned:
surface_form: Slender West Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 32.404051
lon: 119.420786
Pizzo Nero. Pizzo Nero (2,904 m) is a mountain of the Lepontine Alps, located on the border between the Swiss cantons of Valais and Ticino. Its summit is the tripoint between the valleys of Geretal, Gonerli (upper Rhone) and Bedretto (upper Ticino).

Geographic entities mentioned:
surface_form: pizzo nero
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.4925
lon: 8.41222222
The ancient North Siberians were once a people whose ancestors archaeological remains have been found at the Paleolithic Yana RHS (Rhinoceros Horn Site) on the Yana River delta in arctic northern Siberia that is dated 31,600 YBP, and at the Mal'ta site near Lake Baikal in southern Siberia just north of Mongolia that is dated 24,000 YBP.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Dogs and wolves living in the Himalayas and on the Tibetan plateau carry the EPAS1 allele that is associated with high-altitude oxygen adaptation, which has been contributed by a ghost population of an unknown wolf-like canid. This ghost population is deeply diverged from modern Holarctic wolves and dogs, and has contributed 39% to the Himalayan wolf's nuclear genome.

Geographic entities mentioned:
surface_form: Tibetan plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
The two 100 year old dogs were closely related with the Samoyed breed. Siberian Huskies show a genetic affinity with historical East Siberian dogs and ancient Lake Baikal dogs. Together, this indicates that the ancient arctic lineage lives on in some modern Siberian breeds.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
The Ōreti River flows through this ward. Geography. Southland District covers the majority of the land area of Southland Region, although the region also covers Gore District, Invercargill City and adjacent territorial waters. It has a land area of, excluding inland waters such as Lake Te Anau, Lake Manapouri, and Lake Hauroko.

Geographic entities mentioned:
surface_form: Lake Te Anau
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.2
lon: 167.8
surface_form: Lake Manapouri
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.514
lon: 167.508
surface_form: Lake Hauroko
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.958
lon: 167.305
Arthur Creek. Arthur Creek is a stream in the Texas County, Missouri. It is a tributary of the Big Piney River. The stream headwaters arise west of Missouri Route 137 between Yukon and Raymondville. It flows northwest under U. S. Route 63 northeast of Houston and on to its confluence with the Big Piney southwest of Prescott. The stream source is at and the confluence is at.

Geographic entities mentioned:
surface_form: arthur creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.42972222
lon: -91.94666667
It is a tributary of the Big Piney River. The stream headwaters arise west of Missouri Route 137 between Yukon and Raymondville. It flows northwest under U. S. Route 63 northeast of Houston and on to its confluence with the Big Piney southwest of Prescott. The stream source is at and the confluence is at. Arthur Creek has the name of George H. Arthur, a pioneer citizen.

Geographic entities mentioned:
surface_form: arthur creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.42972222
lon: -91.94666667
Unrest in Nyasaland. In the 1940s and early 1950s, the most pressing problem in Nyasaland was that of African access to land. Between 1892 and 1894, about 15% of the total land area of the Nyasaland, including over 350,000 hectares of the best land in the Shire Highlands, the most densely populated part of the country, had been turned into European-owned estates.

Geographic entities mentioned:
surface_form: Shire Highlands
instance_of: Plateau
countries: Malawi
coordinates: lat: -15.64684105
lon: 35.12557983
Birni, Giridih. Birni is a village in the Birni CD block in the Bagodar-Saria subdivision of the Giridih district in the Indian state of Jharkhand. Area overview. Giridih district is a part of the Chota Nagpur plateau, with rocky soil and extensive forests. Most of the rivers in the district flow from the west to east, except in the northern portion where the rivers flow north and north west.

Geographic entities mentioned:
surface_form: Chota Nagpur plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
Murrisk. Murrisk () is a village in County Mayo, Ireland, on the south side of Clew Bay, about 8 km west of Westport and 4 km east of Lecanvey. Murrisk lies at the foot of Croagh Patrick and is the starting-point for pilgrims who visit the mountain. Every year, on the last Sunday of July, thousands of people converge on the village to make the pilgrimage.

Geographic entities mentioned:
surface_form: Croagh Patrick
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.7595
lon: -9.6584
Flowering occurs from February to March and the fruit is a cylindric shaped cypsela long and tapering at the apex. Taxonomy and naming. This species was described in 1951 by Norman Wakefield based on a specimen collected in 1888 by Carl Walter at Mount Hotham and given the name &quot;Helichrysum alpinum&quot;. In 1991 Arne A.

Geographic entities mentioned:
surface_form: Mount Hotham
instance_of: Mountain
countries: Australia
coordinates: lat: -36.983333333333
lon: 147.13333333333
In 1991 Arne A. Anderberg gave it the name &quot;Ozothamnus alpinus&quot; and the description was published in &quot;Opera Botanica&quot;. Distribution and habitat. Alpine everlasting occurs from the Mount Kosciuszko area and southwards on the edge of wet alpine heath or in bogs.

Geographic entities mentioned:
surface_form: Mount Kosciuszko
instance_of: Mountain
countries: Australia
coordinates: lat: -36.4558303
lon: 148.2635105
Muslims form a majority of the population of the republics of Tatarstan and Bashkortostan in the Volga Federal District and predominate among the nationalities in the North Caucasian Federal District located between the Black Sea and the Caspian Sea: the Circassians, Balkars, Chechens, Ingush, Kabardin, Karachay, and numerous Dagestani peoples.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
The volcano is extinct. It is unknown when it last erupted. Its volcano number is 0205–01. Trou au Natron is located just south-east of Toussidé, the westernmost volcano of the Tibesti Mountains. Its edge cuts into the nearby Yirrigue caldera. Geology. The caldera sits at an elevation of. It has an irregular diameter of approximately and is up to deep.

Geographic entities mentioned:
surface_form: Toussidé
instance_of: Mountain
countries: Chad
coordinates: lat: 21.04083333333333
lon: 16.47361111111111
surface_form: toussidé
instance_of: Mountain
countries: Chad
coordinates: lat: 21.04083333333333
lon: 16.47361111111111
Trou au Natron. Trou au Natron (French: &quot;hole of natron&quot;) or (Teda: &quot;big hole&quot;) is a volcanic caldera of the Tibesti Massif in the nation of Chad in Northern Africa. The volcano is extinct. It is unknown when it last erupted. Its volcano number is 0205–01. Trou au Natron is located just south-east of Toussidé, the westernmost volcano of the Tibesti Mountains.

Geographic entities mentioned:
surface_form: trou au natron
instance_of: Mountain
countries: Chad
coordinates: lat: 20.975
lon: 16.5675
Umalila Mountains. The Umalila Mountains are a mountain range in southern Tanzania, on the border with Malawi. The Umalila Mountains are part of Tanzania's Southern Highlands. The mountains are named for the Malila people. Geography. The Umalila Mountains lie northwest of Lake Malawi, and trend roughly northwest-southeast. They form part of the western edge of the East African Rift.

Geographic entities mentioned:
surface_form: Southern Highlands
instance_of: Mountain
countries: Tanzania
coordinates: lat: -9.1666666666667
lon: 34.516666666667
The Umalila Mountains lie northwest of Lake Malawi, and trend roughly northwest-southeast. They form part of the western edge of the East African Rift. The Kyela Plain lies to the east and northeast of the mountains in the rift valley. The volcanic Poroto Mountains and Mount Rungwe lie to the northeast across the Kiwira River. The town of Mbeya lies to the north, and plateaus to the west.

Geographic entities mentioned:
surface_form: Mount Rungwe
instance_of: Mountain
countries: Tanzania
coordinates: lat: -9.135
lon: 33.668055555556
Rainfall is mostly during the November through April wet season, although higher elevations experience mists and light rain during the May through August dry season. The highlands are cooler than the surrounding lowlands, with annual temperatures between 13°C and 19°C. The Umalila Mountains are drier than Mount Rungwe and the Poroto Mountains to the northeast. Ecology.

Geographic entities mentioned:
surface_form: Mount Rungwe
instance_of: Mountain
countries: Tanzania
coordinates: lat: -9.135
lon: 33.668055555556
The town of Biescas is located at 875 meters altitude on the banks of the Gállego river. The municipality extends along a small plain and includes the canyon to access to the Tena Valley. At 72 km north of the main city Huesca, Biescas is a communication hub between the regions of Jacetania and Sobrarbe.

Geographic entities mentioned:
surface_form: Tena Valley
instance_of: Valley
countries: Spain
coordinates: lat: 42.666666666667
lon: -0.31666666666667
Lobsang Spire. Lobsang Spire is a mountain in the Karakoram Range of the Gilgit-Baltistan region of Pakistan. It rises above the Baltoro Glacier near Broad Peak. First ascent. Lobsang Spire was first climbed on 13 June 1983 by an expedition led by Doug Scott, with Greg Child and Peter Thexton, via the South Pillar and in alpine style.

Geographic entities mentioned:
surface_form: Broad Peak
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.810555555556
lon: 76.568055555556
Lobsang Spire. Lobsang Spire is a mountain in the Karakoram Range of the Gilgit-Baltistan region of Pakistan. It rises above the Baltoro Glacier near Broad Peak. First ascent. Lobsang Spire was first climbed on 13 June 1983 by an expedition led by Doug Scott, with Greg Child and Peter Thexton, via the South Pillar and in alpine style.

Geographic entities mentioned:
surface_form: lobsang spire
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.769819
lon: 76.288006
It rises above the Baltoro Glacier near Broad Peak. First ascent. Lobsang Spire was first climbed on 13 June 1983 by an expedition led by Doug Scott, with Greg Child and Peter Thexton, via the South Pillar and in alpine style. They climbed from 10–13 June in one of the first routes to employ big wall aid climbing techniques, including portaledges, in the Karakoram.

Geographic entities mentioned:
surface_form: lobsang spire
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.769819
lon: 76.288006
The family contains a single genus, &quot;Finnlakevirus&quot;, which contains a single species, &quot;Finnlakevirus FLiP&quot;. This virus was isolated in 2010, with its gram-negative host &quot;Flavobacterium&quot;, from Lake Jyväsjärvi, a boreal freshwater habitat in Central Finland, and is the first described single-stranded DNA virus with an internal membrane.

Geographic entities mentioned:
surface_form: Lake Jyväsjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 62.23916667
lon: 25.7725
The storm, being a category 3 atmospheric river event, brought heavy rain and snowfall to the Western United States. Over of rain during the storm were recorded on Mount Tamalpais, a mountain in the San Francisco Bay Area, with San Francisco itself receiving around of rain from the event. Around of snow was recorded in Pinecrest, California.

Geographic entities mentioned:
surface_form: Mount Tamalpais
instance_of: Mountain
countries: United States
coordinates: lat: 37.9291
lon: -122.578
His house, in Summertown, a suburb of Oxford. was named Aorangi, a Māori name for Mount Cook, a favourite place visited on his travels. Walker's collections from the Pacific, Australia, New Zealand and the Mediterranean are shared by the Natural History Museum, London and the Oxford University Museum which also conserves his British Coleoptera.

Geographic entities mentioned:
surface_form: Mount Cook
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.595
lon: 170.14194444444445
At present, catches of bass and eels have dropped considerably, while those of mullet and American blue crab (a species introduced in the 1980s) have increased. During the 2024 October floods in the province of Valencia, the lagoon received water both from the Rambla del Poyo on the north and the paddies flooded by the Magro on the south.

Geographic entities mentioned:
surface_form: Rambla del Poyo
instance_of: Watercourse
countries: Spain
coordinates: lat: 39.378611111111
lon: -0.35638888888889
Amulree. Amulree (Scottish Gaelic: &quot;Àth Maol Ruibhe&quot;, 'Ford of [St.] Maelrubha') is a small hamlet in Perth and Kinross, Scotland. It lies in hilly country on the A822 road, east of Loch Freuchie in Strathbraan, west of Dunkeld and north of Crieff. It lies close to the geographical centre of Scotland.

Geographic entities mentioned:
surface_form: Loch Freuchie
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.516666666667
lon: -3.8333333333333
Cultural beliefs. Surrounded by great grasslands, the Tikar people developed a unique understanding of nature and performed planting rituals to bless seeds and work implements. Other ethnic groups in the region were known to offer animal sacrifices when it was time to plant. The Tikar also had their own cultural beliefs regarding birthing.

Geographic entities mentioned:
surface_form: grasslands
instance_of: Plateau
countries: Cameroon
coordinates: lat: 6.5
lon: 10.5
Arndt Lake. Arndt Lake is a lake in Yosemite National Park, in California. Arndt Lake was named for Alvin Arndt, of the U.S. Army.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: arndt lake
instance_of: Lake
countries: United States
coordinates: lat: 38.0757
lon: -119.504
Arndt Lake. Arndt Lake is a lake in Yosemite National Park, in California. Arndt Lake was named for Alvin Arndt, of the U.S. Army.

Geographic entities mentioned:
surface_form: arndt lake
instance_of: Lake
countries: United States
coordinates: lat: 38.0757
lon: -119.504
Gervais Lake. Gervais Lake is a lake in Ramsey County, in the U.S. state of Minnesota. Gervais Lake was named after Benjamin Gervais, a pioneer who settled at the lake in 1844.

Geographic entities mentioned:
surface_form: gervais lake
instance_of: Lake
countries: United States
coordinates: lat: 45.02
lon: -93.07055556
Dinosaurs of Tendaguru (original title: Dinosaria wa Tendaguru) is a story for young readers that combines both fiction and natural history, focussing on the discovery and subsequent excavations of dinosaur fossils at Tendaguru hill in Lindi Region of South Eastern Tanzania.

Geographic entities mentioned:
surface_form: Tendaguru
instance_of: Mountain
countries: Tanzania
coordinates: lat: -10.05
lon: 39.11666667
From 2018 to 2022, Byrne served as the New York State chair of the American Legislative Exchange Council (ALEC). Life and career. Byrne was born and raised in the Hudson Valley and attended Carmel High School before enrolling at the University of Scranton. As a high school student, he earned the rank of Eagle Scout.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Catchment Area. The water catchment area of the Campo Moro dams comes from the Fellaria and Scersen glaciers in the Bernina range, the largest glacial mountain range in Italy, located east of the Gotthard Pass (Switzerland). The range includes summits such as Mount Cevedale (3779 meters a.s.l.), Mount Adamello (3539 meters a.s.l.), and Piz Bernina (4049 meters a.s.l.).

Geographic entities mentioned:
surface_form: Mount Cevedale
instance_of: Mountain
countries: Italy
coordinates: lat: 46.448055555556
lon: 10.620833333333
surface_form: Mount Adamello
instance_of: Mountain
countries: Italy
coordinates: lat: 46.156
lon: 10.496388888889
surface_form: Piz Bernina
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.382388888889
lon: 9.9081111111111
Her hull was reinforced for light icebreaking. She was initially stationed at Mobile, Alabama, with cruising grounds to Lake Pontchartrain, Louisiana, and Fowey Rocks, Florida. During World War I she escorted convoys out of Halifax, Nova Scotia. After the war she served with the Bering Sea Patrol before returning to Savannah, Georgia, before World War II.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
Piz Forun. Piz Forun is a mountain of the Albula Alps, located east of Bergün in the canton of Graubünden.

Geographic entities mentioned:
surface_form: piz forun
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.655333333333
lon: 9.8649722222222
It is set on land administered by the Bureau of Land Management as the Red Rock Canyon National Conservation Area, part of the Rainbow Mountain Wilderness Area. The peak is immediately north of Mount Wilson. Precipitation runoff from the mountain's slopes drains north into Red Rock Wash and south into Oak Creek.

Geographic entities mentioned:
surface_form: mount wilson
instance_of: Mountain
countries: United States
coordinates: lat: 34.2238
lon: -118.062
surface_form: mount wilson
instance_of: Mountain
countries: United States
coordinates: lat: 37.8392
lon: -107.991
surface_form: mount wilson
instance_of: Mountain
countries: United States
coordinates: lat: 36.0936
lon: -115.484
surface_form: mount wilson
instance_of: Mountain
countries: United States
coordinates: lat: 38.85047
lon: -119.21988
surface_form: mount wilson
instance_of: Mountain
countries: United States
coordinates: lat: 44.0048
lon: -72.9259
surface_form: mount wilson
instance_of: Mountain
countries: United States
coordinates: lat: 35.99658541
lon: -114.61187301
Rainbow Mountain (Clark County, Nevada). Rainbow Mountain is a mountain summit in Clark County, Nevada, United States. Description. Rainbow Mountain is located west of downtown Las Vegas in the Spring Mountains which are a subrange of the Great Basin Ranges.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: rainbow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 63.3090952
lon: -145.6326361
surface_form: rainbow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.73473611111111
lon: -86.72911666666667
surface_form: rainbow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.1080241
lon: -115.4902857
Rainbow Mountain (Clark County, Nevada). Rainbow Mountain is a mountain summit in Clark County, Nevada, United States. Description. Rainbow Mountain is located west of downtown Las Vegas in the Spring Mountains which are a subrange of the Great Basin Ranges.

Geographic entities mentioned:
surface_form: rainbow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 63.3090952
lon: -145.6326361
surface_form: rainbow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.73473611111111
lon: -86.72911666666667
surface_form: rainbow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.1080241
lon: -115.4902857
Rainbow Mountain is a mountain summit in Clark County, Nevada, United States. Description. Rainbow Mountain is located west of downtown Las Vegas in the Spring Mountains which are a subrange of the Great Basin Ranges. It is set on land administered by the Bureau of Land Management as the Red Rock Canyon National Conservation Area, part of the Rainbow Mountain Wilderness Area.

Geographic entities mentioned:
surface_form: rainbow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 63.3090952
lon: -145.6326361
surface_form: rainbow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.73473611111111
lon: -86.72911666666667
surface_form: rainbow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.1080241
lon: -115.4902857
Description. Rainbow Mountain is located west of downtown Las Vegas in the Spring Mountains which are a subrange of the Great Basin Ranges. It is set on land administered by the Bureau of Land Management as the Red Rock Canyon National Conservation Area, part of the Rainbow Mountain Wilderness Area. The peak is immediately north of Mount Wilson.

Geographic entities mentioned:
surface_form: rainbow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 63.3090952
lon: -145.6326361
surface_form: rainbow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.73473611111111
lon: -86.72911666666667
surface_form: rainbow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.1080241
lon: -115.4902857
Board on Geographic Names. Climate. Rainbow Mountain is set within the Mojave Desert which has hot summers and cold winters. The desert is an example of a cold desert climate as the desert's elevation makes temperatures cooler than lower elevation deserts. Due to the high elevation and aridity, temperatures drop sharply after sunset. Summer nights are comfortably cool.

Geographic entities mentioned:
surface_form: rainbow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 63.3090952
lon: -145.6326361
surface_form: rainbow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.73473611111111
lon: -86.72911666666667
surface_form: rainbow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.1080241
lon: -115.4902857
Geology. Rainbow Mountain is composed of Aztec Sandstone which formed about 180–190 million years ago as lithified sand dunes in a desert during the Early Jurassic. The red, orange, and brown coloring of the sandstone is caused by the presence of iron oxide or hematite. Red spots in the buff sandstone are iron oxide concretions called &quot;Moqui marbles.&quot;

Geographic entities mentioned:
surface_form: rainbow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 63.3090952
lon: -145.6326361
surface_form: rainbow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.73473611111111
lon: -86.72911666666667
surface_form: rainbow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.1080241
lon: -115.4902857
The peak is immediately north of Mount Wilson. Precipitation runoff from the mountain's slopes drains north into Red Rock Wash and south into Oak Creek. Topographic relief is significant as the summit rises above Oak Creek Canyon in less than one-half mile (0.8 km). This mountain's descriptive toponym has been officially adopted by the U.S. Board on Geographic Names. Climate.

Geographic entities mentioned:
surface_form: oak creek canyon
instance_of: Landform
countries: United States
coordinates: lat: 34.9125
lon: -111.727
The municipality covers an area of 479.1 km2. It is the primary production region of the &quot;equipal&quot;-style wood and pigskin furniture. As of 2005, the municipality had a total population of 30,528. Geography. The municipality covers an area of 479.1 km2. To the east lies the largest lake in Mexico, Lake Chapala.

Geographic entities mentioned:
surface_form: Lake Chapala
instance_of: Lake
countries: Mexico
coordinates: lat: 20.333333333333
lon: -103
The North Fork of the St. Lucie River flows south from St. Lucie County into Martin County where it joins the north-flowing South Fork, which was once called the Halpatiokee River, just south of the old Roosevelt Bridge (Old Dixie Highway) in Stuart to form the main St. Lucie River. It then passes under the Florida East Coast Railway drawbridge and the new high-level Roosevelt Bridge (U.S.

Geographic entities mentioned:
surface_form: Indian River Lagoon
instance_of: Body of water
countries: United States
coordinates: lat: 28.05527778
lon: -80.57611111
Lucie Inlet which goes into the Atlantic Ocean. The entire river is accessible to Lake Okeechobee by the Okeechobee Waterway. The main river passes through Sewall's Point, Port Salerno, Stuart, and Jensen Beach. The South Fork passes through Palm City. Although brackish for most of its length, the salt content of the South Fork diminishes considerably south of the Kanner Highway bridge.

Geographic entities mentioned:
surface_form: Lake Okeechobee
instance_of: Lake
countries: United States
coordinates: lat: 26.933333333333
lon: -80.8
The headwaters of the North Fork are in the farmlands of St. Lucie County near Interstate 95 at an elevation of above sea level. Discharges. In 2016, 237 billion gallons of water was discharged into the St. Lucie River from Lake Okeechobee by the U.S. Army Corps of Engineers between January and November. In 2013, the U.S. Army Corps of Engineers dumped 137 billion gallons of water into the St.

Geographic entities mentioned:
surface_form: Lake Okeechobee
instance_of: Lake
countries: United States
coordinates: lat: 26.933333333333
lon: -80.8
Lucie County near Interstate 95 at an elevation of above sea level. Discharges. In 2016, 237 billion gallons of water was discharged into the St. Lucie River from Lake Okeechobee by the U.S. Army Corps of Engineers between January and November. In 2013, the U.S. Army Corps of Engineers dumped 137 billion gallons of water into the St. Lucie River from Lake Okeechobee.

Geographic entities mentioned:
surface_form: Lake Okeechobee
instance_of: Lake
countries: United States
coordinates: lat: 26.933333333333
lon: -80.8