Sarmila/GeoWiki-Features huggingface dataset:
There are a number of intervening tops, in particular Smithy Fell and Sourfoot Fell, which Wainwright decided were satellites of Low Fell, based on the position of the lowest col. That convention is followed here. To the east of Fellbarrow is the Vale of Lorton, through which flows the River Cocker.

Geographic entities mentioned:
surface_form: low fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5912
lon: -3.33707
This gives access to the north east ridge above Broadmoor Hill, within easy reach of the summit. An alternative is to climb Low Fell via the drove road from Thackthwaite, either branching north at the ridge or climbing both tops. From the west there are no rights of way on the fell, although it is marked by OS as access land. An approach from the Mosser road is therefore a possibility.

Geographic entities mentioned:
surface_form: low fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5912
lon: -3.33707
Loweswater is unique amongst the major lakes of the District in emptying toward the centre of the National Park. Its waters flow out eastwards into Crummock Water before beginning their northward journey as the Cocker. Loweswater does not therefore represent any watershed between the fells on either side of its valley, as might be supposed from a quick glance at the map.

Geographic entities mentioned:
surface_form: loweswater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.5825
lon: -3.355277777777778
The fell is rounded and grassy almost throughout. Geology. The rocks beneath the summit are of the Loweswater Formation, composed of greywacke sandstone turbidities. Beneath this and occasionally outcropping on the eastern flanks are the laminated mudstone and siltstone of the Kirk Stile Formation. Summit.

Geographic entities mentioned:
surface_form: loweswater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.5825
lon: -3.355277777777778
To the east is a fine view of the North Western Fells across Lorton- the Whiteside - Grisedale Pike ridge perhaps the highlight- with Skiddaw and Blencathra popping up behind. Further round the view is crowded with fells, the northern wall of Ennerdale seen side on throughout its length and backed by Pillar and the Scafells. No lakes or tarns can be seen. Ascents.

Geographic entities mentioned:
surface_form: pillar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.497
lon: -3.282
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
To the west are a number of small streams including Mosser Beck and Cat Gill, which also flow northward and ultimately join the Cocker. This is rolling agricultural land on the very edge of the Lake District. North of Fellbarrow is the lower top of Hatteringill Head (1,263 ft), listed in some guidebooks before the ridge falls away over Whin Fell to a minor road known as Mirk Lane.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Fellbarrow. Fellbarrow is a low hill in the north west of the English Lake District. It is not far from the town of Cockermouth, near to Loweswater and can most easily be climbed from Low Lorton or Thackthwaite. From the summit there are views across the Lorton valley to Grasmoor and Whiteside. Topography.

Geographic entities mentioned:
surface_form: fellbarrow
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.605
lon: -3.342
Loweswater does not therefore represent any watershed between the fells on either side of its valley, as might be supposed from a quick glance at the map. A low ridge circuiting the western end of the lake joins Burnbank Fell to Low Fell and Fellbarrow, confirming them as the last outpost of the Western Fells. The two fells form a ridge 2 miles long with the lower Fellbarrow at the northern end.

Geographic entities mentioned:
surface_form: fellbarrow
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.605
lon: -3.342
That convention is followed here. To the east of Fellbarrow is the Vale of Lorton, through which flows the River Cocker. This is a wide cultivated valley with a number of small parcels of woodland, the settlement of Thackthwaite lying nearest to the fell. To the west are a number of small streams including Mosser Beck and Cat Gill, which also flow northward and ultimately join the Cocker.

Geographic entities mentioned:
surface_form: fellbarrow
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.605
lon: -3.342
This is rolling agricultural land on the very edge of the Lake District. North of Fellbarrow is the lower top of Hatteringill Head (1,263 ft), listed in some guidebooks before the ridge falls away over Whin Fell to a minor road known as Mirk Lane. Fellbarrow also sends out a short ridge north eastward over Broadmoor Hill towards Low Lorton village. The fell is rounded and grassy almost throughout.

Geographic entities mentioned:
surface_form: fellbarrow
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.605
lon: -3.342
Jahran, in the north-central part of the governorate, is its most extensive plain. A volcanic field, Harras of Dhamar, extends to the east of Dhamar town. The governorate's climate is temperate, although the central and eastern sections of the governorate tend to be cold during the winter, while the valleys and western slopes are warmer.

Geographic entities mentioned:
surface_form: Harras of Dhamar
instance_of: Mountain
countries: Yemen
coordinates: lat: 14.55
lon: 44.40166667
In the first year of his tenure, he captured the town of Gravina, which had risen in revolt, and took its leader, a certain Theophylact, prisoner. In December 999, and again on February 2, 1002, he reinstituted and confirmed the possessions of the abbey and monks of Monte Cassino in Ascoli. In 1004, he fortified and expanded the castle of Dragonara on the Fortore.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
This landform's toponym has been officially adopted by the U.S. Board on Geographic Names. Reverend John Roberts (1853–1949) was a missionary to the Shoshone and Arapahoe peoples of the Wind River Indian Reservation area and he was the first principal of the reservation's school. Climate.

Geographic entities mentioned:
surface_form: shoshone
instance_of: Lake
countries: United States
coordinates: lat: 44.3722
lon: -110.713
Description. Roberts Mountain is located 2.5 miles east of the Continental Divide in the remote Wind River Range. It is the highest point in the Wind River Indian Reservation as well as the central portion of the range, and it ranks as the 55th-highest in Wyoming. Neighbors include Mount Lander, 2.54 miles to the south-southwest, and Pronghorn Peak 3.61 miles to the southwest.

Geographic entities mentioned:
surface_form: mount lander
instance_of: Mountain
countries: United States
coordinates: lat: 42.883888888889
lon: -109.32194444444
Roberts Mountain. Roberts Mountain is a summit in Fremont County, Wyoming, United States. Description. Roberts Mountain is located 2.5 miles east of the Continental Divide in the remote Wind River Range. It is the highest point in the Wind River Indian Reservation as well as the central portion of the range, and it ranks as the 55th-highest in Wyoming.

Geographic entities mentioned:
surface_form: roberts mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.91520555555556
lon: -109.29587222222223
Climate. According to the Köppen climate classification system, Roberts Mountain is located in an alpine subarctic climate zone with long, cold, snowy winters, and cool to warm summers. Due to its altitude, it receives precipitation all year, as snow in winter, and as thunderstorms in summer. Hazards. Encountering bears is a concern in the Wind River Range.

Geographic entities mentioned:
surface_form: roberts mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.91520555555556
lon: -109.29587222222223
Arkansas Highway 37 leads north to the Missouri line, where Missouri Route 37 continues north to Seligman and Cassville, Missouri. Gateway is on a plateau in the Ozarks at above sea level, overlooking the valley of the White River and Beaver Lake to the south. According to the United States Census Bureau, the town has a total area of, all land. Demographics.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
They paid US$1 million (about £300,000), or less than 25 cents per acre, between 1787 and 1788. At first Phelps and Gorham thought they would make the site of current-day Geneva their headquarters, but discovered that their survey had somehow left that site just east of their boundary. So they chose Canandaigua, New York, at the head of Canandaigua Lake, as the seat of the new Ontario County.

Geographic entities mentioned:
surface_form: Canandaigua Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.756666666667
lon: -77.317777777778
According to the shrine's legend, its foundation has strong connections with the Yamato Takeru mythology. According to the &quot;Kojiki&quot; and the &quot;Nihon Shoki&quot;, as the folk hero Yamato Takeru was returning home after his conquests in eastern Japan, he feel ill after blasphemy against the deity of Mount Ibuki and died in Ise Province.

Geographic entities mentioned:
surface_form: Mount Ibuki
instance_of: Mountain
countries: Japan
coordinates: lat: 35.417777777778
lon: 136.40611111111
Castle Craig Rock. Castle Craig Rock is a prominent geological feature to the south of Kawhia Harbour in the Waikato region of New Zealand. It is located from Marokopa, Waikato, New Zealand, above the valley of the Marokopa River. Castle Craig Rock is a type of flaggy Limestone (sandstone).

Geographic entities mentioned:
surface_form: castle craig rock
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.266716
lon: 174.808385
It is located from Marokopa, Waikato, New Zealand, above the valley of the Marokopa River. Castle Craig Rock is a type of flaggy Limestone (sandstone). It stands 610 feet (186m) above sea level and provides an expansive view of Castle Craig Farm, an organic beef farm, plus the little town of Awamarino.

Geographic entities mentioned:
surface_form: castle craig rock
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.266716
lon: 174.808385
It is located from Marokopa, Waikato, New Zealand, above the valley of the Marokopa River. Castle Craig Rock is a type of flaggy Limestone (sandstone). It stands 610 feet (186m) above sea level and provides an expansive view of Castle Craig Farm, an organic beef farm, plus the little town of Awamarino.

Geographic entities mentioned:
surface_form: castle craig
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.266716
lon: 174.808385
It stands 610 feet (186m) above sea level and provides an expansive view of Castle Craig Farm, an organic beef farm, plus the little town of Awamarino. In the 1920s the owner of Castle Craig Farm, which is where the rock is located, named it Castle Craig Rock because he thought it looked very similar to Castlecraig in Black Isle in northern Scotland.

Geographic entities mentioned:
surface_form: castle craig
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.266716
lon: 174.808385
surface_form: castle craig rock
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.266716
lon: 174.808385
Haynon Peak. Haynon Peak is a mountain summit located in British Columbia, Canada. Description. This remote peak is situated southwest of Lytton. It is part of the Lillooet Ranges of the Coast Mountains and the nearest higher neighbor is Kumkan Peak, to the southwest. Precipitation runoff from the peak's slopes drains into Chochiwa and Kwoiek creeks, thence the Fraser River.

Geographic entities mentioned:
surface_form: Kumkan Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.08301
lon: -121.93593
Haynon Peak. Haynon Peak is a mountain summit located in British Columbia, Canada. Description. This remote peak is situated southwest of Lytton. It is part of the Lillooet Ranges of the Coast Mountains and the nearest higher neighbor is Kumkan Peak, to the southwest. Precipitation runoff from the peak's slopes drains into Chochiwa and Kwoiek creeks, thence the Fraser River.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: haynon peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.09971
lon: -121.91933
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Topographic relief is significant as the summit rises 1,050 metres (3,445 ft) above Stukolait Lake in and 700 metres (2,297 ft) above Haynon Lake in. The first ascent of the summit was made in August 1958 by four members of the British Columbia Mountaineering Club: Dick Culbert, Art Dellow, Roy Mason, and Ralph Hutchinson. Etymology. The mountain is named in association with Haynon Lake.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Haynon Peak. Haynon Peak is a mountain summit located in British Columbia, Canada. Description. This remote peak is situated southwest of Lytton. It is part of the Lillooet Ranges of the Coast Mountains and the nearest higher neighbor is Kumkan Peak, to the southwest. Precipitation runoff from the peak's slopes drains into Chochiwa and Kwoiek creeks, thence the Fraser River.

Geographic entities mentioned:
surface_form: haynon peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.09971
lon: -121.91933
Climate. Based on the Köppen climate classification, Haynon Peak is located in a subarctic climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall.

Geographic entities mentioned:
surface_form: haynon peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.09971
lon: -121.91933
As a result, the Coast Mountains experience high precipitation, especially during the winter months in the form of snowfall. Winter temperatures can drop below −20°C with wind chill factors below −30°C. This climate supports the Kwoiek Glacier southwest of the peak. The months of July through September offer the most favorable weather for climbing Haynon Peak.

Geographic entities mentioned:
surface_form: haynon peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.09971
lon: -121.91933
The first ascent of the summit was made in August 1958 by four members of the British Columbia Mountaineering Club: Dick Culbert, Art Dellow, Roy Mason, and Ralph Hutchinson. Etymology. The mountain is named in association with Haynon Lake. &quot;Haynon&quot; is a Thompson Indian word meaning &quot;magpie&quot; which is common here.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Bristow Helicopters provide offshore support services to drill companies exploring offshore from Dongara. Local charter operations from Geraldton Airport providing fly-in fly-out services include Shine Aviation to Golden Grove Mine, Mount Magnet and Jack Hills. Virgin Australia operates to Boolgeeda Airport from Geraldton for Rio Tinto, using F100 and 737 aircraft.

Geographic entities mentioned:
surface_form: Jack Hills
instance_of: Mountain
countries: Australia
coordinates: lat: -26.1167
lon: 117.15
On 12 June 1812, Maret, in a correspondence with Kurakin, stated that France cannot accept Russian demands about French withdrawal behind the Elbe as a prerequisite to all peace negotiations and that France regards Kurakin's demand for passports as a declaration of war. On, Alexander I wrote to Saltykov: &quot;We expect to be attacked every hour.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Andrist. Family name. Andrist is a Swiss family name with proof of family vital records at least back to the 16th century. Places of origins (rights of citizenship) are known from Simmental, Canton of Bern. Andrist is a folksy version of &quot;Andreas&quot; (Andrew in English). There is also a branch of the family name that may originate from the Lombardy region named Andrista, Cevo, Italy.

Geographic entities mentioned:
surface_form: Simmental
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.55
lon: 7.36
There is also a branch of the family name that may originate from the Lombardy region named Andrista, Cevo, Italy. Mountains. There are two mountains called Andrist in Switzerland: &quot;Wild Andrist&quot; (means &quot;wild Andrist&quot;) has an altitude of 2849 m asl; &quot;Zahm Andrist&quot; (refers to &quot;tame Andrist&quot;) has an altitude of asl.

Geographic entities mentioned:
surface_form: Zahm Andrist
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.553416666667
lon: 7.7878055555556
She was slain by Regan after whom Tomregan is supposedly named. In ancient times the area that became known as Bréifne was said to be occupied by the Erdini, called in Irish 'Ernaigh', who possessed the entire country bordering Lough Erne. At the time of the Christianization of Ireland (c.

Geographic entities mentioned:
surface_form: Lough Erne
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.48262
lon: -7.80622
Cover art. The album cover features drawings by Giuliano Manfredini, Russo's son (who was 6 around that time), in textured paper. They depict the Sugar Loaf, the Maracanã Stadium, the Colosseum and the Tower of Pisa (spelled Tower of &quot;Pizza&quot;). The booklet came shaped as a small book per Russo's idea, containing initial letters inspired by 19th century typography.

Geographic entities mentioned:
surface_form: Sugar Loaf
instance_of: Mountain
countries: Brazil
coordinates: lat: -22.949444444444445
lon: -43.156666666666666
Lake Umayo. Lake Umayo (Spanish: Laguna Umayo) is a lake in Atuncolla District of the Puno Region of Peru. The Sillustani burial ground is near the shores of the lake. The lake is located at an elevation of and is about long and wide.

Geographic entities mentioned:
surface_form: umayo
instance_of: Lake
countries: Peru
coordinates: lat: -15.742777777778
lon: -70.189722222222
surface_form: lake umayo
instance_of: Lake
countries: Peru
coordinates: lat: -15.742777777778
lon: -70.189722222222
Lake Umayo. Lake Umayo (Spanish: Laguna Umayo) is a lake in Atuncolla District of the Puno Region of Peru. The Sillustani burial ground is near the shores of the lake. The lake is located at an elevation of and is about long and wide.

Geographic entities mentioned:
surface_form: umayo
instance_of: Lake
countries: Peru
coordinates: lat: -15.742777777778
lon: -70.189722222222
surface_form: umayo
instance_of: Lake
countries: Peru
coordinates: lat: -15.742777777778
lon: -70.189722222222
surface_form: lake umayo
instance_of: Lake
countries: Peru
coordinates: lat: -15.742777777778
lon: -70.189722222222
Tyrrhena Terra is typical of the southern Martian terrae, with heavily cratered highlands and other rugged terrain. It contains the large volcano Tyrrhena Patera, one of the oldest volcanoes on Mars. Its largest crater is Herschel. Licus Vallis and the Ausonia Montes are other major features in the region. Some channels and dunes are visible in Tyrrhena Terra, as shown in the images below. Dunes.

Geographic entities mentioned:
surface_form: Licus Vallis
instance_of: Valley
coordinates: lat: -3.05
lon: 126.35
Landing site. The Lander/Ascender landed on the Moon on 1 December 2020, at 15:11 UTC. The Chang'e 5 landing site is at 43.1°N (in latitude), 51.8°W (in longitude) in the Northern Oceanus Procellarum near a huge volcanic complex, Mons Rümker, located in the northwest lunar near side. The area is mapped as 'Eratosthenian Mare' by the USGS.

Geographic entities mentioned:
surface_form: Mons Rümker
instance_of: Mountain
coordinates: lat: 40.76
lon: -58.38
He was defeated when he ran for re-election in 1945. He also ran unsuccessfully for the Kamloops federal seat in 1935. Stirling later owned a ranch on Shuswap Lake. He died November 7, 1966, in Victoria at the age of 89.

Geographic entities mentioned:
surface_form: Shuswap Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.000693
lon: -119.01263
Agumba people. adeq40t4pvx166evquj23smxpq3mu5" xml:space="preserve">The Agumba (also Gumba) people were an ethnic group who inhabited the forests of Mount Kenya, but are now either extinct or assimilated. Sources. The Agumba people are known of only through the oral tradition of the Kikuyu, Embu, and Meru peoples. language.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
Championnet accompanied a column of 8,000–9,000 men that crossed the Col de Montgenèvre and moved southeast to Fossano via Pinerolo. The southernmost column marched over the Maddalena Pass (Col de l'Argentière) into the Valle Stura di Demonte in the direction of Cuneo.

Geographic entities mentioned:
surface_form: Valle Stura di Demonte
instance_of: Valley
countries: Italy
coordinates: lat: 44.31
lon: 7.17
Wadi al-Qura. Wadi al-Qura () is a wadi north of Medina in Saudi Arabia, mentioned in early Islamic sources. It was located on the main trade road between the Hejaz and Syria. The wadi is tentatively identified with the modern Wadi al-'Ula region. The meaning of the name, &quot;Valley of Villages&quot;, suggests the area contained several villages.

Geographic entities mentioned:
surface_form: wadi al-qura
instance_of: Valley
countries: Saudi Arabia
coordinates: lat: 26.5
lon: 37.5
The 9th-century historian Ibn al-Kalbi described it as highly fertile and dotted with villages throughout. Recent discoveries of Geonic &quot;responsa&quot; have shown that there was a Jewish presence in Wadi al-Qura as late as the 11th century CE, and that they maintained correspondence with Rabbi Sherira Gaon and Rabbi Hai Gaon.

Geographic entities mentioned:
surface_form: wadi al-qura
instance_of: Valley
countries: Saudi Arabia
coordinates: lat: 26.5
lon: 37.5
Cornone di Blumone. Cornone di Blumone is a mountain of Lombardy, Italy, It has an elevation of 2,843 metres.

Geographic entities mentioned:
surface_form: cornone di blumone
instance_of: Mountain
countries: Italy
coordinates: lat: 45.95
lon: 10.46666667
Santomeri. Santomeri (Greek: Σαντομέρι) is a village and a community in the municipal unit of Olenia, Achaea, Greece. It is located on the northern end of Mount Skollis, 5 km north of Portes, 18 km south of Kato Achaia and 32 km southwest of Patras. The community includes the villages Ampelakia and Polylofo. History.

Geographic entities mentioned:
surface_form: Skollis
instance_of: Mountain
countries: Greece
coordinates: lat: 37.968
lon: 21.577
It is located on the northern end of Mount Skollis, 5 km north of Portes, 18 km south of Kato Achaia and 32 km southwest of Patras. The community includes the villages Ampelakia and Polylofo. History. Santomeri is named after Nicholas III of Saint Omer, a French baron of Thebes who gave his name to the castle Santameri and the nearby mountain, now known as Skollis. Venetians called it Edrolcamo?.

Geographic entities mentioned:
surface_form: Skollis
instance_of: Mountain
countries: Greece
coordinates: lat: 37.968
lon: 21.577
View Ridge, Seattle. View Ridge is a neighborhood in north Seattle, Washington. As with all Seattle neighborhoods, its boundaries are not fixed, but can be thought of as NE 65th Street in the south, 40th and 45th Avenues NE in the west, the Sand Point Country Club in the north, and Sand Point Way NE in the east. Many homes offer views of Lake Washington, Mount Rainier, and the Cascade Range.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
Geography. Altybaysor is an endorheic lake of the northern end of the Kazakh Uplands at an elevation of. The Irtysh flows to the east of the eastern shores of the lake. There are a number of smaller lakes in its vicinity, such as Zhamantuz (Aksu City Administration) to the northwest, Zhamantuz (May District) to the SSE, Batyrsha to the west and Bozshasor to the south. Alkamergen lies to the south.

Geographic entities mentioned:
surface_form: Zhamantuz
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 51.1355
lon: 76.9153
Altybaysor. Altybaysor () is a salt lake in the Aksu City Administration, Pavlodar Region, Kazakhstan. The lake lies to the SSW of Aksu city. The area surrounding the lake is used for livestock grazing. Geography. Altybaysor is an endorheic lake of the northern end of the Kazakh Uplands at an elevation of. The Irtysh flows to the east of the eastern shores of the lake.

Geographic entities mentioned:
surface_form: altybaysor
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 51.57722
lon: 76.60528
It is in the Indus River watershed basin. Origin and route. Kunhar is the main river in the Naran Valley. It originates from the Lulusar Lake, near the Babusar Pass at the elevation of 3455m, in the
Kaghan Valley. Melting snow and natural tributaries are the main source of water for the Kunhar river. It joins Jhelum river at Pattan.

Geographic entities mentioned:
surface_form: Kaghan Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 34.833333
lon: 73.516667
Little Hart Crag. Little Hart Crag is a fell in the Lake District area of England. It stands at the head of Scandale, north of Ambleside, at a height of. It is an eastern outlier of Dove Crag in the Eastern Fells, although it does have of prominence from that fell making it both a Hewitt and a Nuttall fell.

Geographic entities mentioned:
surface_form: Dove Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.485061111111
lon: -2.9677694444444
It is an eastern outlier of Dove Crag in the Eastern Fells, although it does have of prominence from that fell making it both a Hewitt and a Nuttall fell. It is frequently climbed as part of the Dovedale horseshoe, an walk over the neighbouring fells of Hartsop above How, Hart Crag, Dove Crag and High Hartsop Dodd, starting and finishing at Brothers Water. Topography.

Geographic entities mentioned:
surface_form: Hartsop above How
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4995
lon: -2.95421
surface_form: Hart Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493080555556
lon: -2.9772194444444
surface_form: High Hartsop Dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4889
lon: -2.93853
surface_form: Brothers Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.505555555556
lon: -2.925
surface_form: dove crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.485061111111
lon: -2.9677694444444
surface_form: hartsop dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4981
lon: -2.9094
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
The western top is the higher and is marked by a cairn, while the eastern one is more shapely but a few metres lower and has quartzite set into its rocks. The view from the top of the fell is restricted by higher fells, but it does give the opportunity of studying the crags of Dove Crag and Red Screes in detail. Ascents.

Geographic entities mentioned:
surface_form: Red Screes
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.470061111111
lon: -2.9334694444444
surface_form: dove crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.485061111111
lon: -2.9677694444444
To the east it drops steeply into Caiston Glen. On its west side it is connected to Dove Crag by the boggy hollow of Bakestone Moss and to the north east a ridge falls away towards Patterdale going over High Hartsop Dodd before dropping steeply to the valley. The fell is craggy on its northern side as the crags of Black Brow fall into Dovedale. Geology.

Geographic entities mentioned:
surface_form: dove crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.485061111111
lon: -2.9677694444444
surface_form: hartsop dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4981
lon: -2.9094
surface_form: high hartsop dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4889
lon: -2.93853
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
The most direct route from Patterdale starts at Brothers Water and firstly ascends High Hartsop Dodd before continuing to the summit of Little Hart Crag. Also from Patterdale the fell can also be climbed in conjunction with Red Screes or Dove Crag and even Fairfield.

Geographic entities mentioned:
surface_form: dove crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.485061111111
lon: -2.9677694444444
surface_form: fairfield
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4969
lon: -2.99059
surface_form: red screes
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.470061111111
lon: -2.9334694444444
Ascents. Little Hart Crag is nearly always climbed in conjunction with other adjacent fells, there being no feasible direct ascent although it can be climbed from Patterdale via the top of the Scandale Pass. The most direct route from Patterdale starts at Brothers Water and firstly ascends High Hartsop Dodd before continuing to the summit of Little Hart Crag.

Geographic entities mentioned:
surface_form: hartsop dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4981
lon: -2.9094
surface_form: high hartsop dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4889
lon: -2.93853
surface_form: little hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.481630555556
lon: -2.9476194444444
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: brothers water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.505555555556
lon: -2.925
surface_form: hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493080555556
lon: -2.9772194444444
Little Hart Crag. Little Hart Crag is a fell in the Lake District area of England. It stands at the head of Scandale, north of Ambleside, at a height of. It is an eastern outlier of Dove Crag in the Eastern Fells, although it does have of prominence from that fell making it both a Hewitt and a Nuttall fell.

Geographic entities mentioned:
surface_form: little hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.481630555556
lon: -2.9476194444444
surface_form: hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493080555556
lon: -2.9772194444444
Little Hart Crag. Little Hart Crag is a fell in the Lake District area of England. It stands at the head of Scandale, north of Ambleside, at a height of. It is an eastern outlier of Dove Crag in the Eastern Fells, although it does have of prominence from that fell making it both a Hewitt and a Nuttall fell.

Geographic entities mentioned:
surface_form: little hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.481630555556
lon: -2.9476194444444
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493080555556
lon: -2.9772194444444
Topography. Little Hart Crag is composed of grassy slopes on its eastern slopes above the Scandale Pass, with the tiny Scandale Tarn tucked in a hollow in the hill. To the east it drops steeply into Caiston Glen.

Geographic entities mentioned:
surface_form: little hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.481630555556
lon: -2.9476194444444
surface_form: hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493080555556
lon: -2.9772194444444
Ascents. Little Hart Crag is nearly always climbed in conjunction with other adjacent fells, there being no feasible direct ascent although it can be climbed from Patterdale via the top of the Scandale Pass. The most direct route from Patterdale starts at Brothers Water and firstly ascends High Hartsop Dodd before continuing to the summit of Little Hart Crag.

Geographic entities mentioned:
surface_form: little hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.481630555556
lon: -2.9476194444444
surface_form: hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493080555556
lon: -2.9772194444444
The fell is craggy on its northern side as the crags of Black Brow fall into Dovedale. Geology. The summit is an outcrop of Middle Dodd Dacite, the underlying rock being volcaniclastic sandstone. Summit. The summit is of interest, there being two distinct tops about apart, both of whom are rocky.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: middle dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4781
lon: -2.93211
To the east it drops steeply into Caiston Glen. On its west side it is connected to Dove Crag by the boggy hollow of Bakestone Moss and to the north east a ridge falls away towards Patterdale going over High Hartsop Dodd before dropping steeply to the valley. The fell is craggy on its northern side as the crags of Black Brow fall into Dovedale. Geology.

Geographic entities mentioned:
surface_form: dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
Toledo Division. The Toledo Division was the southern half of the Pere Marquette Railway's main line, which ran from Ludington, Michigan (on the coast of Lake Michigan) to Toledo, Ohio (on the coast of Lake Erie). The Toledo Division encompassed the portion which ran from Toledo north to Saginaw, Michigan, where it met the Ludington Division.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Sirudavoor Lake. Sirudavoor Lake is an inland lake with wetlands in the Kanchipuram district of Tamil Nadu state, in eastern South India. This lake is on the Coromandel Coast, near the Bay of Bengal. It lies approximately south of Chennai city. The lake is home to a number of bird species. During winter, several migratory species can be spotted. Ecology.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
The Bünzau is a sandy lowland stream. Important tributaries are the Höllenau and Bredenbek. The river's discharge is fed by various pipes and ditch systems. History. The Bünzau was navigable for the barges used until around 1870. From the Bünzau harbor, wood was transported from Aukrug south to the Stör and further to the Elbe.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
'Dick' Southby arrived on 21 March to take over command (Maj Fyfffe was promoted to command a battalion of the Royal West Kent Regiment in May). on 7 April the battalion was sent up to hold a piece of the line opposite San Angelo, south of Monte Cassino, under 2nd Parachute Bde. It acted in a purely infantry role, actively patrolling at night, returning to Piedimonte d'Alife after 10 days.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
That night it took Monte Morrone (overlooking the bridge) without opposition. The division now advanced up the Tiber Valley along Route 4, meeting a rearguard at Mentana, which 10th RB and B Sqn Derbyshire Yeomanry were ordered to outflank. The main problems were minefields covered by mortars and machine guns. Next day 61st Bde was given a rest and left behind the advance.

Geographic entities mentioned:
surface_form: Tiber Valley
instance_of: Valley
countries: Italy
coordinates: lat: 42.133333333333
lon: 12.583333333333
The battalion was now operating as pure infantry, supplied by pack mules. On the dark night of 20/21 September 2nd and 10th RB captured Monte Erbolini, then D Company passed through and established itself at the top of the Muraglione Pass between the Sieve Valley and the Po Valley.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
Mount Hardisty. Mount Hardisty is a mountain summit located in the Athabasca River valley of Jasper National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Kerkeslin, to the south. Both mountains are part of the Maligne Range and are visible from the Icefields Parkway. __NOTOC__
History.

Geographic entities mentioned:
surface_form: Mount Kerkeslin
instance_of: Mountain
countries: Canada
coordinates: lat: 52.64861111111111
lon: -117.82666666666667
Mount Hardisty. Mount Hardisty is a mountain summit located in the Athabasca River valley of Jasper National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Kerkeslin, to the south. Both mountains are part of the Maligne Range and are visible from the Icefields Parkway. __NOTOC__
History.

Geographic entities mentioned:
surface_form: athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
surface_form: athabasca
instance_of: Mountain
countries: Canada
coordinates: lat: 52.18055555555556
lon: -117.20166666666667
surface_form: mount hardisty
instance_of: Mountain
countries: Canada
coordinates: lat: 52.70472222222222
lon: -117.82444444444444
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Climate. Based on the Köppen climate classification, Mount Hardisty is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Mount Hardisty drains into the Athabasca River.

Geographic entities mentioned:
surface_form: athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
surface_form: athabasca
instance_of: Mountain
countries: Canada
coordinates: lat: 52.18055555555556
lon: -117.20166666666667
surface_form: mount hardisty
instance_of: Mountain
countries: Canada
coordinates: lat: 52.70472222222222
lon: -117.82444444444444
Mount Hardisty. Mount Hardisty is a mountain summit located in the Athabasca River valley of Jasper National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Kerkeslin, to the south. Both mountains are part of the Maligne Range and are visible from the Icefields Parkway. __NOTOC__
History.

Geographic entities mentioned:
surface_form: mount hardisty
instance_of: Mountain
countries: Canada
coordinates: lat: 52.70472222222222
lon: -117.82444444444444
The mountain's name was officially adopted in 1912 by the Geographical Names Board of Canada. Geology. Mount Hardisty is composed of sedimentary rock laid down during the Cambrian period and pushed east and over the top of younger rock during the Laramide orogeny. Climate.

Geographic entities mentioned:
surface_form: mount hardisty
instance_of: Mountain
countries: Canada
coordinates: lat: 52.70472222222222
lon: -117.82444444444444
Geology. Mount Hardisty is composed of sedimentary rock laid down during the Cambrian period and pushed east and over the top of younger rock during the Laramide orogeny. Climate. Based on the Köppen climate classification, Mount Hardisty is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.

Geographic entities mentioned:
surface_form: mount hardisty
instance_of: Mountain
countries: Canada
coordinates: lat: 52.70472222222222
lon: -117.82444444444444
Both mountains are part of the Maligne Range and are visible from the Icefields Parkway. __NOTOC__
History. The mountain was named by James Hector in 1859 for Richard Hardisty (1831–1889), Chief factor at Rocky Mountain House, and later the first Metis Senator in Canada. The mountain's name was officially adopted in 1912 by the Geographical Names Board of Canada. Geology.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Both mountains are part of the Maligne Range and are visible from the Icefields Parkway. __NOTOC__
History. The mountain was named by James Hector in 1859 for Richard Hardisty (1831–1889), Chief factor at Rocky Mountain House, and later the first Metis Senator in Canada. The mountain's name was officially adopted in 1912 by the Geographical Names Board of Canada. Geology.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
However, during Barak's term as prime minister she changed her opinions about him. Death. Leah Rabin was diagnosed with lung cancer and died in Rabin Medical Center in Petah Tikva in 2000 at the age of 72 and was buried in Mount Herzl in Jerusalem beside her husband Yitzhak Rabin, a few days after the fifth anniversary of her husband's assassination. Family.

Geographic entities mentioned:
surface_form: Mount Herzl
instance_of: Mountain
countries: Israel
coordinates: lat: 31.774117
lon: 35.180567
Cìr Mhòr. Cìr Mhòr (Scottish Gaelic, usually with definite article, &quot;A' Chìr Mhòr&quot;) is a Corbett known as the Matterhorn of Arran. Its name means the &quot;big comb&quot;, referring its resemblance to a cockscomb. It is separated from the island's highest peak, Goat Fell, by a col called &quot;The Saddle&quot;.

Geographic entities mentioned:
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
surface_form: cìr mhòr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.639538888889
lon: -5.2218777777778
surface_form: a' chìr mhòr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.639538888889
lon: -5.2218777777778
Cìr Mhòr. Cìr Mhòr (Scottish Gaelic, usually with definite article, &quot;A' Chìr Mhòr&quot;) is a Corbett known as the Matterhorn of Arran. Its name means the &quot;big comb&quot;, referring its resemblance to a cockscomb. It is separated from the island's highest peak, Goat Fell, by a col called &quot;The Saddle&quot;.

Geographic entities mentioned:
surface_form: Goat Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.626111111111
lon: -5.1905555555556
surface_form: goat fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.626111111111
lon: -5.1905555555556
surface_form: the saddle
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.162395
lon: -5.414721
Cìr Mhòr. Cìr Mhòr (Scottish Gaelic, usually with definite article, &quot;A' Chìr Mhòr&quot;) is a Corbett known as the Matterhorn of Arran. Its name means the &quot;big comb&quot;, referring its resemblance to a cockscomb. It is separated from the island's highest peak, Goat Fell, by a col called &quot;The Saddle&quot;.

Geographic entities mentioned:
surface_form: cìr mhòr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.639538888889
lon: -5.2218777777778
Tropical Storm Two. August 31-September 10. A tropical storm spotted near Dominica on August 31 moved west-northwest to Jamaica before moving northward to the Grand Banks by September 10. Hurricane Three. A strong hurricane devastated Orotava Valley, Tenerife, and the rest of the Canary Islands off north Africa in November. About 500 – 1,000 dead from the hurricane. Hurricane One.

Geographic entities mentioned:
surface_form: Orotava Valley
instance_of: Valley
countries: Spain
coordinates: lat: 28.387469444444
lon: -16.545411111111
It lies about to the east of the left bank of the Ishim. The Akkanburlyk, a tributary of the Ishim, flows to the north of the northern end. The lake has a roughly triangular shape. Ulykol lake is located to the northwest in the same district. Lake Zhaksy-Zhalgyztau lies to the northeast. Flora. The vegetation in the area of the lake is steppe.

Geographic entities mentioned:
surface_form: Ulykol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.950833333333335
lon: 66.845
It lies about to the east of the left bank of the Ishim. The Akkanburlyk, a tributary of the Ishim, flows to the north of the northern end. The lake has a roughly triangular shape. Ulykol lake is located to the northwest in the same district. Lake Zhaksy-Zhalgyztau lies to the northeast. Flora. The vegetation in the area of the lake is steppe.

Geographic entities mentioned:
surface_form: zhaksy-zhalgyztau
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.61666667
lon: 68.175
Kalmakkol. Kalmakkol (), is a salt lake in Gabit Musirepov District, North Kazakhstan Region, and Zhaksy District, Akmola Region, Kazakhstan. Novoishim town, the administrative center of the district, is located approximately to the NNW of the lake. The border with Akmola Region runs close to the southwestern shore of the lake and a small sector lies within Zhaksy District. Geography.

Geographic entities mentioned:
surface_form: kalmakkol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.456
lon: 67.53236
The border with Akmola Region runs close to the southwestern shore of the lake and a small sector lies within Zhaksy District. Geography. Kalmakkol occupies a tectonic depression at the southern end of the West Siberian Plain. It lies about to the east of the left bank of the Ishim. The Akkanburlyk, a tributary of the Ishim, flows to the north of the northern end.

Geographic entities mentioned:
surface_form: kalmakkol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.456
lon: 67.53236
Levitical priests or &quot;kohanim&quot; are traditionally believed and halakhically required to be of direct patrilineal descent from Aaron. According to the Book of Numbers, Aaron died at 123 years of age, on Mount Hor, in the fortieth year after the Israelites had come out of the land of Egypt. Deuteronomy, however, places these events at Moseroth.

Geographic entities mentioned:
surface_form: Mount Hor
instance_of: Mountain
countries: Jordan
coordinates: lat: 30.31677704842186
lon: 35.40653791009069
In May, Van Garderen won the first major stage race of his career, the Tour of California. He performed well in all the key stages, coming in second at stage two's hilltop finish, then winning the individual time trial on stage 6. He topped it off by defending the lead on stage 7, a mountaintop finish to Mount Diablo. He somewhat lacked form at the Tour de France, finishing in 45th position.

Geographic entities mentioned:
surface_form: Mount Diablo
instance_of: Mountain
countries: United States
coordinates: lat: 37.881697781
lon: -121.914154997