Sarmila/GeoWiki-Features huggingface dataset:
Course. Large river in southwestern Papua New Guinea. Its headwaters originate in the southern part of the Mount Bosavi. It flows through the seasonally flooded, rainforested, swampy &quot;Papua Lowlands&quot; and empties into the Gulf of Papua after more than 300 km. It is also called the &quot;Aworra River&quot; up to the mouth of the Wawoi. Its estuary is a tidal delta widened into a funnel.

Geographic entities mentioned:
surface_form: Mount Bosavi
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -6.6141666666667
lon: 142.82666666667
Sankuru District covered the upper part of the Lukenie River basin and a section of the Lubilash River, which originates further south in Lomami District. Colonial history. Between 1910 and 1912 Kasai District was divided into Sankuru District to the northeast and a smaller Kasai District to the southwest. As of 1926 both these districts were in the Congo-Kasaï province.

Geographic entities mentioned:
surface_form: Lukenie River
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: -2.73089
lon: 18.15563
An administrator checking rumors of the subversion was attacked from Ekombe, with several deaths and injuries on both sides. Buildings in Boliko, Ikali and Monjuku were destroyed. The rebellion spread among the Pongo and Batua people. The people of the Lomela River basin left their villages and gathered in a desert location, refusing to obey the Belgians.

Geographic entities mentioned:
surface_form: Lomela River
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: -2.3
lon: 23.28
River Lugg. The River Lugg () rises near Llangynllo in Powys, Wales. From its source, it flows through the border town of Presteigne and then into Herefordshire, England. It meets its main tributary, the River Arrow, to the south of Leominster, then flows into the River Wye downstream of Hereford at Mordiford, around from its source.

Geographic entities mentioned:
surface_form: river lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
At least four of the sites were recorded as having fulling mills subsequently, but none were recorded when a survey of the river was made in 1697. Between the 17th and 19th centuries, four acts of Parliament were passed which specifically named the River Lugg in their titles, but the middle two had the most effect on the river. The first, the Rivers Wye and Lugg Navigation Act 1726 (13 Geo. 1. c.

Geographic entities mentioned:
surface_form: river lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
Navigation up to Leominster was for a time possible, although it was never hugely successful, and ceased in the 1860s, once railways had been built in the area. The river was a free navigation as a result of powers obtained in an act of Parliament, the Rivers Wye and Lugg Navigation Act 1695 (7 & 8 Will. 3. c.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
Course. The River Lugg rises at two locations on Pool Hill, to the north-west of Llangunllo, close to the contour, and is joined by several other streams as it descends rapidly. It is crossed by the Heart of Wales Line, between and stations, before passing under the first of four bridges that carry the B4356 road over it. Already it has dropped below the contour.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
It has been restored and on days when it is open to the public, it can be seen in operation. To the south of the mill is Lugg Bridge, consisting of three arches, two spanning the river and a third spanning the mill tailrace. The north face dates from 1771, when the bridge was built, while the south face dates from 1938, when it was widened.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
To the south of the mill is Lugg Bridge, consisting of three arches, two spanning the river and a third spanning the mill tailrace. The north face dates from 1771, when the bridge was built, while the south face dates from 1938, when it was widened. At Lugg Green, Kingsland is another Lugg Bridge, and after a series of weirs, the river arrives on the northern edge of Leominster.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
At Lugg Green, Kingsland is another Lugg Bridge, and after a series of weirs, the river arrives on the northern edge of Leominster. A leat to Crowards Mill, now disconnected from the main river, was formerly the main channel of the Lugg, with much of the flow passing over a weir into the Kenwater.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
The Lugg served Osborne Mill, Marsh Mill and a third corn mill, before rejoining the Kenwater within the town. Pinsley Brook ran through the town just to the south of Kenwater, to power Pinsley Mill, another corn mill just to the north of Leominster railway station and joined the Lugg below Eaton Bridge.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
Pinsley Brook ran through the town just to the south of Kenwater, to power Pinsley Mill, another corn mill just to the north of Leominster railway station and joined the Lugg below Eaton Bridge. There were once 19 bridges in Leominster, most of them crossing the Lugg, Kenwater or Pinsley Brook.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
The river system within the town was radically reworked in the 1960s, as part of a flood alleviation scheme. The Lugg continued southwards along the course of the Kenwater, to a new weir close to the former course of the Leominster and Kington Railway. The Kenwater passed over the weir, while a new channel was cut for the Lugg, following the course of the railway.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
The river forms the western and southern boundaries of the associated parkland and the building was remodelled and restored by Wyattville for Richard Arkwright at that time. The Humber Brook forms the eastern boundary of the estate, and joins the Lugg on its north bank. The river continues to the east and then turns to the south.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
It dates from the 16th or 17th century, but was altered in the mid-19th century. The bridge is to the east of the village of Moreton on Lugg. After Wergins Bridge, Morton Brook joins on the west bank, and the river is crossed by a railway bridge carrying the Cotswold Line. Lugg Bridge at Lugwardine dates from the 14th century, and was repaired in 1409 and 1464.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
It has three arches, and was widened in the 1960s, when the south side was largely rebuilt. The Little Lugg joins from the east near the bridge, which was the location of corn mills in 1903, when a structure spanned the river to the south of the bridge. A little further downstream is Lugwardine Bridge, consisting of three spans dating from the early 17th century.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
The bridge dates from the 14th century, and was widened in the 16th century. It consists of two main arches, through which the Lugg flows, with two flood arches and a causeway containing five more arches to the west of the main arches. The causeway was widened on the upstream side in the 20th century. To the west of the causeway are the remains of a pound lock.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
To the west of the causeway are the remains of a pound lock. The walls of the chamber survive, although they are in poor condition. The Pentaloe Brook joins the river on its east bank just below the bridge, and then the Lugg joins the River Wye. History. At the time of the Domesday Book, which recorded details of a survey of the land in 1086, the Lugg was an important river for milling.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
History. At the time of the Domesday Book, which recorded details of a survey of the land in 1086, the Lugg was an important river for milling. Some 80 mills were recorded in the county of Herefordshire, and of those, around one third were located in the valley of the Lugg, some on tributaries and others on the main river.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
Some 80 mills were recorded in the county of Herefordshire, and of those, around one third were located in the valley of the Lugg, some on tributaries and others on the main river. In addition, those on the Lugg were valued considerably higher than those elsewhere, with an average value of 15 shillings and 4 pence, compared to 6 shillings and 7 pence for mills on other rivers.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
In addition, those on the Lugg were valued considerably higher than those elsewhere, with an average value of 15 shillings and 4 pence, compared to 6 shillings and 7 pence for mills on other rivers. At that time, the hay meadows on the banks of the Lugg were the largest in the county, and the valley produced large crops of hay and corn.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
At least four of the sites were recorded as having fulling mills subsequently, but none were recorded when a survey of the river was made in 1697. Between the 17th and 19th centuries, four acts of Parliament were passed which specifically named the River Lugg in their titles, but the middle two had the most effect on the river. The first, the Rivers Wye and Lugg Navigation Act 1726 (13 Geo. 1. c.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
&quot;15&quot;), was passed on 19 May 1662, entitled &quot;An Act for the making navigable the Rivers Wye and Lugg, and the Rivers and Brooks running into the same, in the counties of Hereford, Gloucester and Monmouth.&quot; Sir William Sandys was appointed to carry out the work, which involved building weirs and flash locks to maintain water levels, but his previous experience on the Warwickshire Avon did not fit the Wye, which was a much steeper and faster-flowing river, and the work was abandoned by about 1668, before any work had been started on the Lugg.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
Therefore be it enacted that the rivers Wye and Lugg may be henceforth accounted, deemed and taken to be free and common rivers for all to make use of for carrying and conveying of all passenger goods, wares and commodities by boats, barges, lighters and other vessels whatsoever.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
The Rivers Wye and Lugg Navigation Act 1695 took a radical approach, allowing the weirs to be bought and demolished, with funding for the purchases to be raised by a rate on the county of Herefordshire. On the Wye, some of the weirs were associated with fishing, but on the Lugg, all of them were connected with milling.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
The survey listed ten mills between Lugg Bridge, Leominster and the junction with the Wye, but this was probably the number of wheels or pairs of millstones, rather than the number of buildings where milling occurred. The annual value of each mill was to be established, and the price to buy the mill and weir was then fixed at 16 times that value.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
Several bridges were altered, by breaking one of the arches and constructing a timber drawbridge or later a raised arch. Overall, the policy of removing the weirs was not a success, as it meant that water levels dropped significantly, and navigation was hindered by shoals, which prevented boats from passing. A third act of Parliament, the Rivers Wye and Lugg Navigation Act 1726 (13 Geo. 1. c.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
When the case was heard, he was only fined sixpence for each bridge and was not required to remove the locks. There are known to have been locks at twelve sites between Leominster and the Wye, at Volca Meadow, Ford Bridge, Hampton Court, Bodenham Mill, Kings Mill, Moreton Bridge, Wergins Bridge, Sherwick Mill, Lugg Bridge, Tidnor, Mordiford and the confluence.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
Some of these may have been half locks or flash locks, but some were definitely pound locks with two sets of gates, and of the three locks still in existence in 1906, both Tidnor and Mordiford were pound locks, but no clear evidence for a second set of gates at Lugg Bridge has been found. Barges on the river were hauled by teams of men.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
Barges on the river were hauled by teams of men. A fourth act of Parliament was obtained, the Wye and Lugg Navigation and Horse Towing-path Act 1809 (49 Geo. 3. c. lxxviii), to allow horse towing paths to be constructed on the Wye and the Lugg, but there is no evidence that such a path was ever started on the Lugg.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
3. c. lxxviii), to allow horse towing paths to be constructed on the Wye and the Lugg, but there is no evidence that such a path was ever started on the Lugg. The arrival of railways in the area in the 1850s led to the winding up of the Wye and Lugg Towing Path Company, and use of both the Lugg and the Wye for navigation ceased soon afterwards.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
The arrival of railways in the area in the 1850s led to the winding up of the Wye and Lugg Towing Path Company, and use of both the Lugg and the Wye for navigation ceased soon afterwards. Some traffic may have used the lower of the Lugg up to Lugg Bridge until about 1860.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
Some traffic may have used the lower of the Lugg up to Lugg Bridge until about 1860. As a result of the Rivers Wye and Lugg Navigation Act 1695, the Lugg was a free navigation, but in 1995 the National Rivers Authority sought to apply bylaws to both the Wye and the Lugg.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
Equivalent data for the Welsh section is not readily available. The water quality of the River Lugg system was as follows in 2019. Like most rivers in the UK, the chemical status changed from good to fail in 2019, due to the presence of polybrominated diphenyl ethers (PBDE), perfluorooctane sulphonate (PFOS) and mercury compounds, none of which had previously been included in the assessment.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
The survey also found that brown trout had benefitted from the improvements, as their numbers had also increased. Some of the work was funded by the Lugg and Arrow Fisheries Association. The Eaton Angling Club, which was established in 1877, manages the fishing rights on of the river near Eaton Hall.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
Research on similar rivers has shown that reducing the levels of restocking can have a disproportionate benefit for the native populations of both brown trout and grayling, and the club are monitoring catch data to see if this is the case on the Lugg.

Geographic entities mentioned:
surface_form: lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
A little further downstream is Lugwardine Bridge, consisting of three spans dating from the early 17th century. It was widened in 1824 and altered in the 20th century. After the River Frome joins on the east bank, the final bridge connects Mordiford on the east bank to Hampton Bishop. The bridge dates from the 14th century, and was widened in the 16th century.

Geographic entities mentioned:
surface_form: river frome
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 50.6958
lon: -1.98861
surface_form: frome
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 50.6958
lon: -1.98861
The list also contained the highest mountains in Scotland, Wales, Ireland, and England. On 9 November 2019, Norfolk climber Liam Chase became the first person to complete all 120 P600s in a single calendar year, starting with Cross Fell on 1 January, and ending with Pen y Fan. Chase was also only the seventh person recorded to have climbed all P600s over any time period. P600 mountains by height.

Geographic entities mentioned:
surface_form: Cross Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.702777777778
lon: -2.4872222222222
surface_form: Pen y Fan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 51.884031
lon: -3.436765
Since 2006, one of Trengrove's Sub–Majors, Moel Siabod, was re–surveyed and shown to be a P600 &quot;Major&quot;. The list below is the October 2018 DoBIH list of the six mountains with a prominence between in the British Isles.

Geographic entities mentioned:
surface_form: Moel Siabod
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.073075
lon: -3.9324638888889
Distribution. It is native to southern California and northern Baja California, where it grows in scattered locations in vernal pool habitat. In 1993 it was known from fewer than 20 occurrences, including those at the Santa Rosa Plateau, a creek drainage near Hemet, Otay Mesa in San Diego County, and one spot in Woodland Hills.

Geographic entities mentioned:
surface_form: Santa Rosa Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 33.5434
lon: -117.27
Cherni Vrah. Cherni Vrah (, &quot;Black Peak&quot;) is the summit of Vitosha Mountain in Bulgaria. Rising to 2290 m, the peak is the fourth highest mountain summit in the country after Musala (2925 m, Rila Mountain), Vihren (2914 m, Pirin Mountain), and Botev Vrah (2376 m, Balkan Range).

Geographic entities mentioned:
surface_form: Vitosha Mountain
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.566666666667
lon: 23.283333333333
Cherni Vrah. Cherni Vrah (, &quot;Black Peak&quot;) is the summit of Vitosha Mountain in Bulgaria. Rising to 2290 m, the peak is the fourth highest mountain summit in the country after Musala (2925 m, Rila Mountain), Vihren (2914 m, Pirin Mountain), and Botev Vrah (2376 m, Balkan Range).

Geographic entities mentioned:
surface_form: Musala
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.179167
lon: 23.585278
Ski paths link Cherni Vrah to Aleko and Kumata areas in winter, and a ski run on the northern slope of the peak itself is served by a 600-m surface lift. With its annual average wind speed of 9.3 m/s Cherni Vrah is the second most windy peak in Bulgaria after Murgash Peak in the Balkan Range (10.3 m/s). The legend holds it that Cherni Vrah was climbed as early as 181 B.C.

Geographic entities mentioned:
surface_form: Murgash
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.833
lon: 23.669
Popularly, it is attributed to the black colour of the conspicuous rock formations dominating the peak's tip. Another belief holds it that the name derived from the darker appearance the peak presumably had in the past, when the Subalpine zone of Vitosha used to be overgrown by mountain pine (&quot;Pinus mugo&quot;) that was burnt in the Middle Ages to expand sheep pastures.

Geographic entities mentioned:
surface_form: Vitosha
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.566666666667
lon: 23.283333333333
Course. Río Bucaná originates in Cordillera Central at Monte Jayuya and runs in a winding fashion to the south receiving feeds from Rio Jauca, Rio Bayagan and Quebrada Guayo. Río Bucaná is channelized from the point it enters the city of Ponce and until it is fed by Rio Portugues (a river that is also channelized) in Barrio Bucaná at the southern tip of Julio Enrique Monagas Family Park.

Geographic entities mentioned:
surface_form: Monte Jayuya
instance_of: Mountain
countries: United States
coordinates: lat: 18.167777777778
lon: -66.574722222222
Red Mountain (Coconino County, Arizona). Red Mountain is a volcanic cinder cone located in the Coconino National Forest of northern Arizona, United States, 25 miles northwest of Flagstaff. It rises above the surroundings terrain and is shaped like the letter &quot;U&quot;, with its opening towards the west.

Geographic entities mentioned:
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.4867
lon: -86.8064
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.3918
lon: -121.145
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.60041
lon: -120.98678
surface_form: red mountain (coconino county, arizona)
instance_of: Mountain
countries: United States
coordinates: lat: 35.5231
lon: -111.876
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.415277777778
lon: -121.46694444444
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.45588
lon: -121.3891607
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.064444444444
lon: -117.24638888889
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.2979
lon: -119.441
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.26751
lon: -74.54952
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.5356
lon: -113.424
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.1122
lon: -105.181
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.9036
lon: -107.702
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.9783
lon: -110.872
Red Mountain (Coconino County, Arizona). Red Mountain is a volcanic cinder cone located in the Coconino National Forest of northern Arizona, United States, 25 miles northwest of Flagstaff. It rises above the surroundings terrain and is shaped like the letter &quot;U&quot;, with its opening towards the west.

Geographic entities mentioned:
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.4867
lon: -86.8064
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.3918
lon: -121.145
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.60041
lon: -120.98678
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.5231
lon: -111.876
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.415277777778
lon: -121.46694444444
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.45588
lon: -121.3891607
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.064444444444
lon: -117.24638888889
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.2979
lon: -119.441
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.26751
lon: -74.54952
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.5356
lon: -113.424
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.1122
lon: -105.181
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.9036
lon: -107.702
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.9783
lon: -110.872
It rises above the surroundings terrain and is shaped like the letter &quot;U&quot;, with its opening towards the west. Geological Survey (USGS) and Northern Arizona University scientists suggest that Red Mountain was formed in eruptions nearly 740,000 years ago. Geology.

Geographic entities mentioned:
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.4867
lon: -86.8064
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.3918
lon: -121.145
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.60041
lon: -120.98678
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.5231
lon: -111.876
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.415277777778
lon: -121.46694444444
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.45588
lon: -121.3891607
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.064444444444
lon: -117.24638888889
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.2979
lon: -119.441
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.26751
lon: -74.54952
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.5356
lon: -113.424
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.1122
lon: -105.181
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.9036
lon: -107.702
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.9783
lon: -110.872
Geology. Red Mountain is a cinder cone in the San Francisco volcanic field that is noted for its red color and U shape when viewed from above. The cone was erupted from a volcanic vent that now sits under the intact material that comprises the U shape of the mountain.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
With 30 square miles of surface area, Lake Travis has the largest storage capacity of the seven reservoirs known as the Highland Lakes, and stretches 65 miles (105 km) upriver from western Travis County (near Lago Vista, Texas) in a highly serpentine course into southern Burnet County to Max Starcke Dam, southwest of the town of Marble Falls.

Geographic entities mentioned:
surface_form: Highland Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 30.5678
lon: -98.3827
Background. During his visit to the Italian lands in 1558–59, Jan Kochanowski encountered &quot;Scacchia Ludus&quot;, a poem by Marco Girolamo Vida, which describes a game of chess played on Mount Olympus between Apollo and Mercury. It is possible that Kochanowski also met Vida himself.

Geographic entities mentioned:
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
Memorial Union (University of Wisconsin–Madison). Memorial Union is located on the south shore of Lake Mendota on the campus of the University of Wisconsin–Madison. On the lakeshore to the north of the building is the Terrace, a popular outdoor space overlooking the lake. It has gained a reputation as one of the most beautiful student centers on a university campus. History.

Geographic entities mentioned:
surface_form: Lake Mendota
instance_of: Lake
countries: United States
coordinates: lat: 43.106666666667
lon: -89.424722222222
Much of the terrace reopened in May 2016 for graduation weekend, and the first floor/basement opened the following December. The remaining areas reopened in September 2017. Facility. Outside the main building is the Memorial Union Terrace, a stone outdoor dining and recreation area on the shore of Lake Mendota. The Terrace was designed by Peabody's daughter, Charlotte.

Geographic entities mentioned:
surface_form: Lake Mendota
instance_of: Lake
countries: United States
coordinates: lat: 43.106666666667
lon: -89.424722222222
Two moderate earthquakes in the Strait of Otranto in 1974 and 1976 hinted at a possible location for the 1743 earthquake. The introduction of a modern earthquake monitoring system indicated a northeast–southwest zone of concentrated earthquakes that extends from Salento to Altopiano delle Murge. The epicenter location of the event is still a debated topic among scientists.

Geographic entities mentioned:
surface_form: Altopiano delle Murge
instance_of: Plateau
countries: Italy
coordinates: lat: 40.976
lon: 16.406
Colonies of marimo balls are known to form in Japan and Iceland, but their population has been declining. Classification and name. Marimo were first described in the 1820s by Anton E. Sauter, found in Lake Zell, Austria. The genus &quot;Aegagropila&quot; was established by Friedrich T. Kützing (1843) with &quot;A.

Geographic entities mentioned:
surface_form: Lake Zell
instance_of: Lake
countries: Austria
coordinates: lat: 47.316666666667
lon: 12.8
They are sometimes sold in aquariums under the name &quot;Japanese moss balls&quot; although they are unrelated to moss. In Iceland the lake balls are called by the local fishermen at Lake Mývatn (meaning 'ball', meaning 'muck') where the &quot;muck&quot; is any weeds that get entangled in their fishing nets. The generic name &quot;Aegagropila&quot; is Greek for 'goat hair'. Ecology.

Geographic entities mentioned:
surface_form: Lake Mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
Size. The growth rate of marimo is about per year. In Lake Akan in Japan they grow particularly large, up to. Lake Mývatn, Iceland, had dense colonies of marimo that grow to about in diameter and formed well defined patches on the lake floor at depths ranging from. Shape. The round shape of the marimo is maintained by gentle wave action that occasionally turns it.

Geographic entities mentioned:
surface_form: Lake Akan
instance_of: Lake
countries: Japan
coordinates: lat: 43.451666666667
lon: 144.09861111111
Size. The growth rate of marimo is about per year. In Lake Akan in Japan they grow particularly large, up to. Lake Mývatn, Iceland, had dense colonies of marimo that grow to about in diameter and formed well defined patches on the lake floor at depths ranging from. Shape. The round shape of the marimo is maintained by gentle wave action that occasionally turns it.

Geographic entities mentioned:
surface_form: Lake Mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
An excess of nutrients (due to agriculture and fish farming), along with mud deposition from human activity are thought to be the main causes for its disappearance from many lakes. The species still exists in Lake Zell in Austria (where it was first discovered in the 1820s) but the lake ball growth form has not been found there since around 1910.

Geographic entities mentioned:
surface_form: Lake Zell
instance_of: Lake
countries: Austria
coordinates: lat: 47.316666666667
lon: 12.8
The same has happened in most locations in England and Scotland, where mainly the attached form can be found. Dense colonies of marimo were discovered in Lake Mývatn in Iceland in 1978, but they have shrunk considerably since then. By 2014 the marimo had almost completely disappeared from the lake due to an excess of nutrients.

Geographic entities mentioned:
surface_form: Lake Mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
Thanneermukkom Bund. The Thanneermukkom Bund (Thannermukkom Salt Water Barrier) was constructed as a part of the Kuttanad Development Scheme to prevent tidal action and intrusion of salt water into the Kuttanad low-lands across Vembanad Lake between Thannermukkom on west and Vechur on east. Thanneermukkom Bund was constructed in 1974 and is functional since 1976.

Geographic entities mentioned:
surface_form: Vembanad
instance_of: Lake
countries: India
coordinates: lat: 9.85
lon: 76.35
In the period 2007–2014, however, no significant retreat was observed. The glacier may be accessed from below up a &quot;klettersteig&quot;, and from above quite easily via the Kellerwand rock face. Remains of defensive positions witness to the mountain war of 1915-1918.

Geographic entities mentioned:
surface_form: Kellerwand
instance_of: Mountain
countries: Austria
Italy
coordinates: lat: 46.6092
lon: 12.9
The area is traditionally divided into comarques, of which five (French Cerdagne, Capcir, Conflent, Roussillon and Vallespir) are historically Catalan-speaking and one (Fenouillèdes) is historically Occitan-speaking. The five Catalan-speaking comarques were historically part of the Kingdom of Majorca. Administration.

Geographic entities mentioned:
surface_form: Capcir
instance_of: Valley
countries: France
coordinates: lat: 42.6
lon: 2.1166666666667
Karimala Gopuram. Karimala Gopuram (കരിമല ഗോപുരം) is the highest peak in the Thrissur district of Kerala. It is located at southern boundary of Parambikulam Wildlife Sanctuary. It lies in the border of Chalakudy taluk of Thrissur district and Chittur taluk of Palakkad district of Kerala. It is about 1,439m above sea level in the Western Ghats.

Geographic entities mentioned:
surface_form: karimala gopuram
instance_of: Mountain
countries: India
coordinates: lat: 10.366241666666665
lon: 76.7467861111111
Vernik. Vernik (,, &quot;Vrbnik&quot;) is a village in the former Qendër Bilisht Municipality of the Korçë County in Albania, on the border with Krystallopigi in Greece. At the 2015 local government reform it became part of the municipality Devoll. It is situated south of the Small Prespa Lake and is the easternmost settlement of Albania. History.

Geographic entities mentioned:
surface_form: Small Prespa Lake
instance_of: Lake
countries: Albania
Greece
coordinates: lat: 40.766111111111
lon: 21.1
The sale converted the station in a H&I owned-and-operated station, though the possibility of Weigel's other networks being contained to it is also possible. It was Weigel's first station purchase outside of a state along Lake Michigan, as all of its properties were in Illinois, Indiana and Wisconsin. This sale closed December 5, 2017.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Dead Stream is the main outlet from Torsey Pond to Maranacook Lake's west. Annabessacook Lake is the main outlet, but the lake also feeds Cobbosseecontee Lake and Cobbosseecontee Stream, as well as the Kennebec River. Recreation. A popular and historic recreation area and tourist attraction, Maranacook is heavily developed with many summer homes, rental cabins, and year-round residences.

Geographic entities mentioned:
surface_form: Annabessacook Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.26833333333333
lon: -69.98102777777778
surface_form: Cobbosseecontee Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.25
lon: -69.933333333333
Maranacook Lake. Maranacook Lake is a lake in Kennebec County, Maine located in the towns of Readfield and Winthrop. The lake covers with a maximum depth of and a mean depth of. It is one of the major bodies of water in the Winthrop Lakes Region. Water supply. Maranacook Lake serves as the secondary drinking water supply for Winthrop, Maine.

Geographic entities mentioned:
surface_form: maranacook lake
instance_of: Lake
countries: United States
coordinates: lat: 44.343
lon: -69.951
The lake covers with a maximum depth of and a mean depth of. It is one of the major bodies of water in the Winthrop Lakes Region. Water supply. Maranacook Lake serves as the secondary drinking water supply for Winthrop, Maine. The area around Maranacook Lake that is not developed is mainly forest and fairly level ground used for agriculture.

Geographic entities mentioned:
surface_form: maranacook lake
instance_of: Lake
countries: United States
coordinates: lat: 44.343
lon: -69.951
Maranacook Lake serves as the secondary drinking water supply for Winthrop, Maine. The area around Maranacook Lake that is not developed is mainly forest and fairly level ground used for agriculture. Maranacook Lake is fed primarily by four perennial streams: Tingley Brook from the northeast, Beaver Brook from the east, Roseanne Brook from the west, and Dead Stream from the northwest.

Geographic entities mentioned:
surface_form: maranacook lake
instance_of: Lake
countries: United States
coordinates: lat: 44.343
lon: -69.951
The area around Maranacook Lake that is not developed is mainly forest and fairly level ground used for agriculture. Maranacook Lake is fed primarily by four perennial streams: Tingley Brook from the northeast, Beaver Brook from the east, Roseanne Brook from the west, and Dead Stream from the northwest. Dead Stream is the main outlet from Torsey Pond to Maranacook Lake's west.

Geographic entities mentioned:
surface_form: maranacook lake
instance_of: Lake
countries: United States
coordinates: lat: 44.343
lon: -69.951
A popular and historic recreation area and tourist attraction, Maranacook is heavily developed with many summer homes, rental cabins, and year-round residences. Known as one of the cleanest bodies of water in Maine, the lake belongs to the Cobbossee Watershed, and is monitored by the Maranacook Lake Association. The North Basin in Readfield is roughly and shallow, with a homothermous quality.

Geographic entities mentioned:
surface_form: maranacook lake
instance_of: Lake
countries: United States
coordinates: lat: 44.343
lon: -69.951
The North Basin in Readfield is roughly and shallow, with a homothermous quality. The roughly South Basin in Winthrop is deeper and colder. Maranacook Lake Upper Dam is a recent addition to the area. Constructed in 1995, the concrete dam is found at the southeastern tail of the lake in Winthrop.

Geographic entities mentioned:
surface_form: maranacook lake
instance_of: Lake
countries: United States
coordinates: lat: 44.343
lon: -69.951
Stalin feared a Turkish invasion and he saw Kurds as unreliable, even though many Kurds served in the Soviet military. Many of them died during the deportations. After the Osh riots and the riots in Fergana Valley between Kyrgyzs and Uzbeks, many Kurds moved to Kazakhstan.

Geographic entities mentioned:
surface_form: Fergana Valley
instance_of: Valley
countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
lon: 71.757777777778
Route description. Highway 108 is a highway in Algoma District that serves to connect the Trans-Canada Highway with the mines in the Elliot Lake and Quirke Lake area. Elliot Lake is the only community on the highway and is located approximately two-thirds of the distance between Highway 17 and Highway 546. The route begins at Highway 17, east of Spragge and west of Serpent River.

Geographic entities mentioned:
surface_form: Quirke Lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.49
lon: -82.55222
Specimens of this plant were collected in the 1820s and 1830s by Ecklon in the Winterberg which is an extension of the Amathole range, and by Drège at Katberg near the western end of the Amatola range, Table Mountain in the Queenstown district, the Bamboesberge in the Tarkastad district, the Witteberg above Lady Grey and other high mountainous areas in the Cape Colony, such as the Prentjiesberg north of Ugie.

Geographic entities mentioned:
surface_form: Prentjiesberg
instance_of: Mountain
countries: South Africa
coordinates: lat: -31.15
lon: 28.18333333
Eiskögele. The Eiskögele is a mountain in the Glockner Group in the western part of the main Tauern chain, a range of the Austrian Central Alps. It lies right on the border between the Austrian states of Salzburg, Carinthia and East Tyrol and thus forms a tripoint.

Geographic entities mentioned:
surface_form: eiskögele
instance_of: Mountain
countries: Austria
coordinates: lat: 47.099868
lon: 12.655731
Eiskögele. The Eiskögele is a mountain in the Glockner Group in the western part of the main Tauern chain, a range of the Austrian Central Alps. It lies right on the border between the Austrian states of Salzburg, Carinthia and East Tyrol and thus forms a tripoint.

Geographic entities mentioned:
surface_form: eiskögele
instance_of: Mountain
countries: Austria
coordinates: lat: 47.099868
lon: 12.655731
surface_form: glockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.074528
lon: 12.69385
Gert produced significant coastal flooding on moving ashore near Bluefields and Tasbapauni, prompting about 1,000 residents and hundreds of indigenous Miskito villagers to evacuate. Farther inland, prolonged heavy rain caused numerous rivers to overflow, which led to disastrous freshwater flooding, especially in departments around Lake Nicaragua.

Geographic entities mentioned:
surface_form: Lake Nicaragua
instance_of: Lake
countries: Nicaragua
coordinates: lat: 11.5742
lon: -85.3563
As many as 123,000 people were affected throughout the country, and there were 37 confirmed fatalities. The impact on the ecology was profound: rivers, estuaries, and mangroves in and around lakes Nicaragua and Managua, as well as the inhabiting fauna, suffered from severe erosion and siltation.

Geographic entities mentioned:
surface_form: Managua
instance_of: Lake
countries: Nicaragua
coordinates: lat: 12.333333333333
lon: -86.416666666667
The additional flooding from Gert affected 24,000 people in the region and made communication with surrounding areas nearly impossible. Elsewhere, the rain filled several major rivers, including the Ulúa; many rivers across the Sula Valley had their banks destroyed, flooding much of San Pedro Sula&mdash;the country's second-largest city&mdash;and adjacent municipalities in the Cortés Department.

Geographic entities mentioned:
surface_form: Sula Valley
instance_of: Valley
countries: Honduras
coordinates: lat: 15.45
lon: -87.85
The Calabozo River eventually topped its banks, cutting the village of Platón Sánchez off from the outside world. By far the most devastating, however, was the overflow of the Pánuco River on September 24, which runs from the Valley of Mexico through the municipality of Pánuco and empties in the gulf.

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
As of 2017, an estimated 90,000 vehicles a day pass through the island. Routes. The junction serves the following routes, some of which terminate at the island;
Future proposals. Proposals have been put forward by Highways England to build a new link road through Rimrose Valley to ease congestion on the A5036 route for traffic heading towards the motorways via Switch Island.

Geographic entities mentioned:
surface_form: Rimrose Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.473
lon: -3.01
Not long after, a newly constructed road for regular transport was opened. After World War II, the silted up areas south of the dam were poldered with a second and a third Sloedam. When the Veerse Gat estuary was closed off by the Veerse Gatdam in 1961, the Sloedam lost it function as a primary defense against the sea. World War II.

Geographic entities mentioned:
surface_form: Veerse Gat
instance_of: Lake
countries: Netherlands
coordinates: lat: 51.547
lon: 3.675
Flint is not natural to the area, indicating it came along trade routes from the south. The first humans in the deep forests of Våler lived mainly by hunting and fishing. Even though the people around the nearby lake Mjøsa already kept livestock and grew crops, some time passed before the people in Våler settled as farmers. Pre-Christian times.

Geographic entities mentioned:
surface_form: Mjøsa
instance_of: Lake
countries: Norway
coordinates: lat: 60.666666666667
lon: 11
From 1948 to 1952, he was a vice-principal. He retired in 1952. A Fellow of the Royal Society of Canada, he was its president from 1950 to 1951. He was a founder, governor, and board chairman of the Arctic Institute of North America. In 1999 a new mineral from Mont Saint-Hilaire was named &quot;oneillite&quot; in his honour. He died in Ottawa in 1966.

Geographic entities mentioned:
surface_form: Mont Saint-Hilaire
instance_of: Mountain
countries: Canada
coordinates: lat: 45.552222222222
lon: -73.163888888889
Having left St. Nazaire on 3 February 1942, as part of Operation &quot;Drumbeat&quot;, (U-boat operations off the eastern seaboard of the United States), &quot;U-578&quot; hit R.P. Resor on the 27th with a torpedo east of Manasquan Inlet, New Jersey. The tug attempted to take the ship in tow, but she capsized and sank 48 hours after the initial attack east of Barnegat, also New Jersey.

Geographic entities mentioned:
surface_form: Manasquan Inlet
instance_of: Landform
countries: United States
coordinates: lat: 40.1025
lon: -74.035