Sarmila/GeoWiki-Features huggingface dataset:
About 2.5 kilometres north of the Zirler Berg rises the Rauenkopf (2,011 m), which leads to the Reither Spitze (2,374 m) north of that, and about 2.5 kilometres northeast is the Brunstkopf (1,719 m), all peaks within the Erlspitze Group. A tributary of the Inn, the Schlossbach, flows through the gorge of &quot;Schlossbachklamm&quot; to the east.

Geographic entities mentioned:
surface_form: Rauenkopf
instance_of: Mountain
countries: Austria
coordinates: lat: 47.30861111111111
lon: 11.228333333333333
surface_form: Reither Spitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.323
lon: 11.2361
surface_form: Brunstkopf
instance_of: Mountain
countries: Austria
coordinates: lat: 47.2947
lon: 11.2744
surface_form: erlspitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.32
lon: 11.2853
surface_form: brunstkopf
instance_of: Mountain
countries: Austria
coordinates: lat: 47.2947
lon: 11.2744
surface_form: reither spitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.323
lon: 11.2361
surface_form: zirler berg
instance_of: Mountain
countries: Austria
coordinates: lat: 47.2853
lon: 11.2247
surface_form: rauenkopf
instance_of: Mountain
countries: Austria
coordinates: lat: 47.30861111111111
lon: 11.228333333333333
The line runs from Innsbruck via Seefeld and Mittenwald to Garmisch-Partenkirchen and has several stations or halts including Reith, Seefeld and Scharnitz. East of the mountain the railway enters a wide curve over bridges and through tunnels on the south flank of the Rauenkopf and southwestern side of the Brunstkopf, crossing the Schlossbach.

Geographic entities mentioned:
surface_form: Rauenkopf
instance_of: Mountain
countries: Austria
coordinates: lat: 47.30861111111111
lon: 11.228333333333333
surface_form: Brunstkopf
instance_of: Mountain
countries: Austria
coordinates: lat: 47.2947
lon: 11.2744
surface_form: brunstkopf
instance_of: Mountain
countries: Austria
coordinates: lat: 47.2947
lon: 11.2744
Location. The Zirler Berg is on the southeastern extremity of the Seefeld Plateau, which is roughly 1,200 m above sea level and lies between the Wetterstein (north), Karwendel (east) and Mieminger Ranges (west) and drops away to the Inn valley to the south and 600 metres below.

Geographic entities mentioned:
surface_form: seefeld plateau
instance_of: Plateau
countries: Austria
coordinates: lat: 47.3286
lon: 11.1928
Zirler Berg. The Zirler Berg near Zirl in the Austrian federal state of Tyrol is a mountain, high, in the Karwendel Alps, a western part of the Northern Limestone Alps.

Geographic entities mentioned:
surface_form: zirler berg
instance_of: Mountain
countries: Austria
coordinates: lat: 47.2853
lon: 11.2247
&quot;Zirlerbergstraße&quot;. The southern section of the &quot;Seefelder Straße&quot; (B 177), runs up the southern slopes and across the eastern side of the Zirler Berg. This road section is also called the &quot;Zirlerbergstraße&quot;.

Geographic entities mentioned:
surface_form: zirler berg
instance_of: Mountain
countries: Austria
coordinates: lat: 47.2853
lon: 11.2247
The &quot;Seefelder Straße&quot; is oriented mainly in a south to north direction and climbs up the mountain from the Inn valley from Zirl (622 m) with a gradient of up to 16% heading for Leithen (1,010 m) and then continues through Reith, Auland and over the Seefeld Saddle (1,185 m) about 4 km (as the crow flies) northwest of the Zirler Berg to Seefeld.

Geographic entities mentioned:
surface_form: zirler berg
instance_of: Mountain
countries: Austria
coordinates: lat: 47.2853
lon: 11.2247
It is located in the Potosí Department, Tomás Frías Province, Potosí Municipality. It lies north of the plain called Jatun Molino Pampa and the Sip'uruni River. Jatun Q'asa lies near Q'illu Q'asa, Q'illu Urqu and Yuraq Yuraq.

Geographic entities mentioned:
surface_form: Yuraq Yuraq
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.6833
lon: -65.65
surface_form: yuraq yuraq
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.6833
lon: -65.65
Jatun Q'asa (Potosí). Jatun Q'asa (Quechua &quot;jatun, hatun&quot; big, great, &quot;q'asa&quot; mountain pass, &quot;great mountain pass&quot;, Hispanicized spelling &quot;Jatún Casa&quot;) is a mountain in the Khari Khari mountain range of the Bolivian Andes, about 5,023 m (16,480  ft) high. It is located in the Potosí Department, Tomás Frías Province, Potosí Municipality.

Geographic entities mentioned:
surface_form: jatun q'asa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.18611111
lon: -66.45
surface_form: jatun q'asa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.3903
lon: -65.6153
surface_form: jatun q'asa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.47694444
lon: -65.86277778
surface_form: jatun q'asa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.71666667
lon: -65.65
surface_form: jatun q'asa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.64055556
lon: -64.70277778
surface_form: jatun q'asa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.14856
lon: -65.363
surface_form: jatun q'asa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.85777778
lon: -64.61583333
Jatun Q'asa (Potosí). Jatun Q'asa (Quechua &quot;jatun, hatun&quot; big, great, &quot;q'asa&quot; mountain pass, &quot;great mountain pass&quot;, Hispanicized spelling &quot;Jatún Casa&quot;) is a mountain in the Khari Khari mountain range of the Bolivian Andes, about 5,023 m (16,480  ft) high. It is located in the Potosí Department, Tomás Frías Province, Potosí Municipality.

Geographic entities mentioned:
surface_form: jatun q'asa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.18611111
lon: -66.45
surface_form: jatun q'asa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.3903
lon: -65.6153
surface_form: jatun q'asa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.47694444
lon: -65.86277778
surface_form: jatun q'asa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.71666667
lon: -65.65
surface_form: khari khari
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.58333333
lon: -65.66666667
surface_form: jatun q'asa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.64055556
lon: -64.70277778
surface_form: jatun q'asa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.14856
lon: -65.363
surface_form: jatun q'asa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.85777778
lon: -64.61583333
Kanem rose in the 8th century in the region to the north and east of Lake Chad. The Kanem empire went into decline, shrank, and in the 14th century was defeated by Bilala invaders from the Lake Fitri region. Around the 9th century AD, the central Sudanic Empire of Kanem, with its capital at Njimi, was founded by the Kanuri-speaking nomads. Kanem arose by engaging in the trans-Saharan trade.

Geographic entities mentioned:
surface_form: Lake Fitri
instance_of: Lake
countries: Chad
coordinates: lat: 12.809166666667
lon: 17.5025
In its place, the al-Kanemi dynasty of the &quot;shehu&quot; rose to power. Shilluk Kingdom. The Shilluk Kingdom was centered in South Sudan from the 15th century from along a strip of land along the western bank of the White Nile, from Lake No to about 12° north latitude. The capital and royal residence was in the town of Fashoda.

Geographic entities mentioned:
surface_form: Lake No
instance_of: Lake
countries: South Sudan
coordinates: lat: 9.4977777777778
lon: 30.465
Both were absorbed into the Sokoto Caliphate during the Fulani Jihad of 1805, which threatened Bornu itself. Luba Empire. Sometime between 1300 and 1400 AD, Kongolo Mwamba (Nkongolo) from the Balopwe clan unified the various Luba peoples, near Lake Kisale. He founded the Kongolo dynasty, which was later ousted by Kalala Ilunga. Kalala expanded the kingdom west of Lake Kisale.

Geographic entities mentioned:
surface_form: Lake Kisale
instance_of: Lake
countries: Democratic Republic of the Congo
coordinates: lat: -8.257701
lon: 26.50383
Sometime between 1300 and 1400 AD, Kongolo Mwamba (Nkongolo) from the Balopwe clan unified the various Luba peoples, near Lake Kisale. He founded the Kongolo dynasty, which was later ousted by Kalala Ilunga. Kalala expanded the kingdom west of Lake Kisale. A new centralized political system of spiritual kings () with a court council of head governors and sub-heads all the way to village heads.

Geographic entities mentioned:
surface_form: Lake Kisale
instance_of: Lake
countries: Democratic Republic of the Congo
coordinates: lat: -8.257701
lon: 26.50383
Kingdom of Kongo. By the 15th century AD, the farming Bakongo people (&quot;ba&quot; being the plural prefix) were unified as the Kingdom of Kongo under a ruler called the &quot;manikongo&quot;, residing in the fertile Pool Malebo area on the lower Congo River. The capital was M'banza-Kongo. With superior organization, they were able to conquer their neighbors and extract tribute.

Geographic entities mentioned:
surface_form: Pool Malebo
instance_of: Lake
countries: Republic of the Congo
Democratic Republic of the Congo
coordinates: lat: -4.2819444444444
lon: 15.488611111111
The maize and cassava would result in population growth in the region and other parts of Africa, replacing millet as a main staple. By the 16th century, the &quot;manikongo&quot; held authority from the Atlantic in the west to the Kwango River in the east. Each territory was assigned a &quot;mani-mpembe&quot; (provincial governor) by the &quot;manikongo&quot;.

Geographic entities mentioned:
surface_form: Kwango River
instance_of: Watercourse
countries: Angola
Democratic Republic of the Congo
coordinates: lat: -3.3713888888889
lon: 17.358055555556
The chief's power rested on cattle and his connection to the ancestor. This can be seen in the Toutswemogala Hill settlements with stone foundations and stone walls, north of the highveld and south of the Vaal River. Northwest of the Vaal River developed early Tswana states centered on towns of thousands of people.

Geographic entities mentioned:
surface_form: Toutswemogala Hill
instance_of: Mountain
countries: Botswana
coordinates: lat: -22.2325
lon: 27.1992
Urewe. The Urewe culture developed and spread in and around the Lake Victoria region of Africa during the African Iron Age. The culture's earliest dated artifacts are located in the Kagera Region of Tanzania, and it extended as far west as the Kivu region of the Democratic Republic of the Congo, as far east as the Nyanza and Western provinces of Kenya, and north into Uganda, Rwanda and Burundi.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
The Babito clan claim legitimacy by being descended from the Bachwezi clan, who were said to have ruled the Empire of Kitara. Buganda. The Buganda kingdom was founded by Kato Kimera around the 14th century AD. Kato Kintu may have migrated to the northwest of Lake Victoria as early as 1000 BC. Buganda was ruled by the &quot;kabaka&quot; with a &quot;bataka&quot; composed of the clan heads.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
However, by the early 20th century, Buganda became a province of the British Uganda Protectorate. Rwanda. Southeast of Bunyoro, near Lake Kivu at the bottom of the western rift, the Kingdom of Rwanda was founded, perhaps during the 17th century. Tutsi (BaTutsi) pastoralists formed the elite, with a king called the &quot;mwami&quot;. The Hutu (BaHutu) were farmers.

Geographic entities mentioned:
surface_form: Lake Kivu
instance_of: Lake
countries: Democratic Republic of the Congo
Rwanda
coordinates: lat: -1.8530555555556
lon: 29.135277777778
Maravi. The Maravi claimed descent from Karonga (&quot;kalonga&quot;), who took that title as king. The Maravi connected Central Africa to the east coastal trade, with Swahili Kilwa. By the 17th century, the Maravi Empire encompassed all the area between Lake Malawi and the mouth of the Zambezi River. The &quot;karonga&quot; was Mzura, who did much to extend the empire.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
Mountains. Mount Meru, the second highest mountain in Tanzania after Mount Kilimanjaro, peaks at. Arusha Region has the highest number of craters and extinct volcanoes in Tanzania. Other prominent peaks and mountains include the Monduli Mountains, Mount Loolmalasin, Mount Lolkisale, Mount Longido, Gelai Volcano, and the Olduvai Gorge. Lakes.

Geographic entities mentioned:
surface_form: Mount Loolmalasin
instance_of: Mountain
countries: Tanzania
coordinates: lat: -3.05166667
lon: 35.81666667
surface_form: Mount Longido
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.68333333
lon: 36.7
surface_form: Gelai Volcano
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.61916667
lon: 36.10027778
Lakes. Arusha region is home to a number of lakes, the largest lake in the region being Lake Eyasi. Other prominent lakes in the region are Lake Duluti, Momela Lakes, Lake Manyara, Lake Masek, Lake Empakaai, Lake Magadi, Lake Ndutu and Lake Natron. Most of the lakes in the region are alkaline in nature. Districts.

Geographic entities mentioned:
surface_form: Lake Eyasi
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.66667
lon: 35.08333
Lakes. Arusha region is home to a number of lakes, the largest lake in the region being Lake Eyasi. Other prominent lakes in the region are Lake Duluti, Momela Lakes, Lake Manyara, Lake Masek, Lake Empakaai, Lake Magadi, Lake Ndutu and Lake Natron. Most of the lakes in the region are alkaline in nature. Districts.

Geographic entities mentioned:
surface_form: Momela Lakes
instance_of: Lake
countries: Tanzania
surface_form: Lake Manyara
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.5833333333333
lon: 35.833333333333
The A-104 also runs westward past Monduli to its junction at Makuyuni with the B-144 road that leads to Mto wa Mbu and the Ngorongoro Conservation Area. After that, the A-104 curves southward to the east of Lake Manyara and continues on to Babati and Dodoma. Most overland travel is done by bus from the city of Arusha.

Geographic entities mentioned:
surface_form: Lake Manyara
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.5833333333333
lon: 35.833333333333
Most overland travel is done by bus from the city of Arusha. Within the city and smaller towns, privately owned and operated &quot;dala-dalas&quot; (mini-buses) are used. The region is landlocked, and there are no navigable rivers. The larger lakes in the Rift Valley are not used for transportation. The region is home to Lake Eyasi, Lake Natron, Lake Duluti, Lake Empakaai, and the Momella lakes.

Geographic entities mentioned:
surface_form: Lake Eyasi
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.66667
lon: 35.08333
The group was assigned the flag and traditions of the 4th Heavy Field Artillery Regiment and named for the 5th Alpine Division &quot;Pusteria&quot;, which in turn had been named for the Puster Valley (). The group was assigned to the 4th Alpine Army Corps and consisted of a command, a command and services battery, and three batteries with FH70 155mm howitzers. Recent times.

Geographic entities mentioned:
surface_form: Puster Valley
instance_of: Valley
countries: Italy
Austria
coordinates: lat: 46.7405
lon: 12.369555555555555
Karlsborg Fortress. Karlsborg Fortress () is situated on the Vanäs peninsula in Karlsborg by lake Vättern, the province of Västergötland, Sweden. Construction on the fortress began 1819 to realize the so-called &quot;central defense idea&quot; adopted by the Swedish military after the Finnish and Napoleonic Wars.

Geographic entities mentioned:
surface_form: Vättern
instance_of: Lake
countries: Sweden
coordinates: lat: 58.4
lon: 14.6
Even the gold reserves of the central bank of Sweden were to be safeguarded in the fortress in times of trouble. The fortress is one of northern Europe's largest buildings and consists primarily of limestone from Omberg. History. Construction was begun in 1819 on 100 hectares (250 acres) of land. The fortress was to house a garrison of 6,000 enlisted men and an additional 8,000-10,000 people.

Geographic entities mentioned:
surface_form: Omberg
instance_of: Mountain
countries: Sweden
coordinates: lat: 58.30027778
lon: 14.6475
Torata. Torata is another ancient settlement in the Sierra mountains, where the local inhabitants moved from the Cerro Baul, after Incas had forced them to do so. The locale has large terrace systems and is also &quot;a complex of monumental architecture&quot;. There is an altiplano (not seen in the coastal belt) Chulpas. The altiplano has stone storehouses of the Inca deserted 500 years ago).

Geographic entities mentioned:
surface_form: altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Osmore River. Osmore River (also Moquegua, Ilo, or Tumilaca) system flows northeast to southwest in the Moquegua Region of southern coastal Peru. The river has its origin in the snow peaks of the Chuqi Ananta and Arundane mountains, at an elevation of above sea level.

Geographic entities mentioned:
surface_form: ananta
instance_of: Mountain
countries: Peru
coordinates: lat: -13.81388889
lon: -70.62055556
surface_form: ananta
instance_of: Mountain
countries: Peru
coordinates: lat: -15.8128
lon: -71.6825
surface_form: ananta
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7678
lon: -70.8147
surface_form: chuqi ananta
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0814
lon: -70.4494
It has several tributaries which have their origin in the western cordillera. The river basin is bounded on the north by the Tambo River basin, which is a sub-basin of the Vizcachas River; on the east and south, with the Locumba River basin; and on the west by the Pacific Ocean and the region between Moquegua and Tambo, formed by a series of short and medium streams.

Geographic entities mentioned:
surface_form: vizcachas
instance_of: Mountain
countries: Peru
coordinates: lat: -16.9131
lon: -70.1744
Cerro Baul. The earliest historical record is of the Cerro Baul, an imposing mesa, or a rocky peak in the middle of the Moquegua Valley and which overlooks the valley. A city once existed on this peak, now ruined. Early on, Cerro Baul was a major center for the Wari culture; it flourished between AD 600 and 1000. This is where the Wari came in contact with the Tiwanaku empire of the same time.

Geographic entities mentioned:
surface_form: cerro baul
instance_of: Mountain
countries: Peru
coordinates: lat: -17.113845
lon: -70.862418
Although both cultures maintained defensible hilltop settlements, there is no indication that they were at war with each other. Around 600 AD, the Wari brought large numbers of settlers to Cerro Baul and region. On the other hand, the earlier Tiwanaku settlement here was mostly in the lower reaches of the Moquegua river valley. Later on, there was more cooperation between them.

Geographic entities mentioned:
surface_form: cerro baul
instance_of: Mountain
countries: Peru
coordinates: lat: -17.113845
lon: -70.862418
The Inca period. Later on, the Inca invaded the area. The local inhabitants took refuge on the rocky cliff as they could not fight the large army of the Incas. When emperor Mayta Capac of the Inca attacked the area he surrounded the hill as the local residents had moved to the safety of the Cerro Baul cliff, which could be approached by a tortuous route.

Geographic entities mentioned:
surface_form: cerro baul
instance_of: Mountain
countries: Peru
coordinates: lat: -17.113845
lon: -70.862418
This mine location is the origin of the Rio Moquegua. Now the &quot;citadel city of Cerro Baul&quot; (covering an area of) is witness to some ancient architecture with many ruins containing large cache of artifacts, designed textiles, and mummified human remains. Desolate untended agricultural terraces are seen on the slopes of the mountain with canals leading to the desert plains.

Geographic entities mentioned:
surface_form: cerro baul
instance_of: Mountain
countries: Peru
coordinates: lat: -17.113845
lon: -70.862418
One unanswered feature is the reason for the abandoned status of the terraces. Torata. Torata is another ancient settlement in the Sierra mountains, where the local inhabitants moved from the Cerro Baul, after Incas had forced them to do so. The locale has large terrace systems and is also &quot;a complex of monumental architecture&quot;.

Geographic entities mentioned:
surface_form: cerro baul
instance_of: Mountain
countries: Peru
coordinates: lat: -17.113845
lon: -70.862418
Around 600 AD, the Wari brought large numbers of settlers to Cerro Baul and region. On the other hand, the earlier Tiwanaku settlement here was mostly in the lower reaches of the Moquegua river valley. Later on, there was more cooperation between them. Cerro Mejia is another site adjacent to Cerro Baúl. It is surrounded by multiple walls.

Geographic entities mentioned:
surface_form: cerro baúl
instance_of: Mountain
countries: Peru
coordinates: lat: -17.113845
lon: -70.862418
In spite of water shortage in the coastal belt some olive groves are still farmed. Grapes from the valley are brewed to the well known brand of Pisco brandy. A major economic activity in the region the large porphyry copper Mining|mine known as the Toquepala mine, located the Tacna Province, Tacna Department, Peru.

Geographic entities mentioned:
surface_form: pisco
instance_of: Mountain
countries: Peru
coordinates: lat: -9.01183333
lon: -77.63113889
Osmore River. Osmore River (also Moquegua, Ilo, or Tumilaca) system flows northeast to southwest in the Moquegua Region of southern coastal Peru. The river has its origin in the snow peaks of the Chuqi Ananta and Arundane mountains, at an elevation of above sea level.

Geographic entities mentioned:
surface_form: osmore river
instance_of: Watercourse
countries: Peru
coordinates: lat: -17.62225
lon: -71.342582
However, at lower elevations rainfall is almost nil and hence considered as the &quot;world's driest desert, where decades can pass without even a shower.&quot;
In the upstream reaches of the valley, the Asana River is one of the four major tributaries of the Moquegua (Tumilaca) River, which becomes the Osmore River downstream. It is situated in the south central Andes mountains.

Geographic entities mentioned:
surface_form: osmore river
instance_of: Watercourse
countries: Peru
coordinates: lat: -17.62225
lon: -71.342582
Cerro Trapiche was another a Wari/Huaracane site in the middle valley near Tiwanaku settlements; it includes a walled hill peak with slingstone caches. After 1000, both Tiwanaku and Wari had abandoned their Moquegua settlements, and by 1100, the sister states had entirely collapsed. The Chiribaya culture persisted along the lower and middle sections of the Osmore River until about 1400 CE.

Geographic entities mentioned:
surface_form: osmore river
instance_of: Watercourse
countries: Peru
coordinates: lat: -17.62225
lon: -71.342582
From the top of the Baul, Cuajone open pit copper mine is seen. This mine location is the origin of the Rio Moquegua. Now the &quot;citadel city of Cerro Baul&quot; (covering an area of) is witness to some ancient architecture with many ruins containing large cache of artifacts, designed textiles, and mummified human remains.

Geographic entities mentioned:
surface_form: rio moquegua
instance_of: Watercourse
countries: Peru
coordinates: lat: -17.62225
lon: -71.342582
The river has its origin in the snow peaks of the Chuqi Ananta and Arundane mountains, at an elevation of above sea level. It changes names as it descends from the Andes: From its origin it is called the Moquegua, then Osmore in the middle valley as Rio Coscori and Rio Tumilaca including where the river disappears into subterranean channels, and further down in the lower reaches as Rio Ilo.

Geographic entities mentioned:
surface_form: rio ilo
instance_of: Watercourse
countries: Peru
coordinates: lat: -17.62225
lon: -71.342582
Many springs in the lower valley (broad valley with flood plains developed for agriculture) were tapped for irrigation development and the river in the lower section in the coastal valley is known by the ancient name of Rio Ilo (Ilo River) with coast line occupied by villages of fishermen. The upper section of the Osmore contains several valleys.

Geographic entities mentioned:
surface_form: rio ilo
instance_of: Watercourse
countries: Peru
coordinates: lat: -17.62225
lon: -71.342582
It is situated in the south central Andes mountains. The main Asana has its primary source at an elevation of. This is within the pampas in the peripheral region of the high puna, defined as an area (&quot;Pampa Tinajones&quot; and Apachita Limani) above elevation. The river's run off source is seasonal precipitation including snow melt from the western cordillera of the Andes.

Geographic entities mentioned:
surface_form: apachita limani
instance_of: Mountain
countries: Peru
coordinates: lat: -17.015
lon: -70.4603
Ohlone Wilderness trail. The Ohlone Wilderness trail, a long distance footpath linking several East Bay regional parks, passes through the Sunol Regional Wilderness. It runs from Mission Peak Regional Preserve near Fremont to the Del Valle Regional Park near Livermore. Several backpack campgrounds exist along the way. Much of the routes land is owned by the San Francisco Water Department.

Geographic entities mentioned:
surface_form: Mission Peak Regional Preserve
instance_of: Mountain
countries: United States
coordinates: lat: 37.5124
lon: -121.881
Several backpack campgrounds exist along the way. Much of the routes land is owned by the San Francisco Water Department. Right to pass is subject to a permit, which is available at the Sunol Wilderness entrance gate. The terrain between Sunol Wilderness and Del Valle Park can be challenging. Rose Peak is the high point, only a bit lower than Mount Diablo in elevation.

Geographic entities mentioned:
surface_form: Mount Diablo
instance_of: Mountain
countries: United States
coordinates: lat: 37.881697781
lon: -121.914154997
The most common source of meat was the pig. Sheep and goats were apparently domesticated in the Loess Plateau area in the 4th millennium BC, found in western Henan by 2800 BC, and then spread across the middle and lower Yellow River area. Dogs were also eaten, particularly in Shandong, though cattle were less important.

Geographic entities mentioned:
surface_form: Loess Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Shandong Longshan. The center of Shandong is a mountainous area, including Mount Tai (1,545 m) and other several other peaks over 1000 m. Longshan settlements are found on the plains surrounding this massif. To the north are four evenly spaced walled centers, Chengziya, Dinggong, Tianwang and Bianxianwang (from west to east), with the largest, Chengziya, enclosing only 20 ha.

Geographic entities mentioned:
surface_form: Mount Tai
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 36.266666666667
lon: 117.1
However, in 194, before Cui Yan could even complete his first year of studies, the Yellow Turban rebels from Xu Province attacked Beihai Commandery, where Zheng Xuan conducted his classes, so Zheng and his students fled east to Mount Buqi (不其山; northwest of Mount Lao) to evade chaos.

Geographic entities mentioned:
surface_form: Mount Lao
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 36.191666666667
lon: 120.59166666667
After leaving Mount Buqi, Cui Yan could not return to Qinghe Commandery because rebel forces and bandits were rampant in the region and the roads leading west were blocked. He wandered around Qing, Xu, Yan and Yu provinces and visited several places, including Shouchun (壽春; present-day Shou County, Anhui), Lake Tai and the northern bank of the Yangtze River.

Geographic entities mentioned:
surface_form: Lake Tai
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 31.166666666667
lon: 120.15
Floods in Chad. Floods in Chad occur annually due to heavy seasonal rainfall between May and October. Rivers such as the Chari and Logone overflow, leading to surface runoff in low-lying areas. The country's drainage infrastructure and flat topography lead to flood risk, particularly in urban and agricultural regions.

Geographic entities mentioned:
surface_form: Logone
instance_of: Watercourse
countries: Cameroon
Central African Republic
Chad
coordinates: lat: 12.106111111111
lon: 15.035277777778
Helmsley. Helmsley is a market town and civil parish in North Yorkshire, England. Historically part of the North Riding of Yorkshire, the town is located at the point where Ryedale leaves the moorland and joins the flat Vale of Pickering. Helmsley is situated on the River Rye on the A170 road, east of Thirsk, west of Pickering and some due north of York.

Geographic entities mentioned:
surface_form: Vale of Pickering
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.2
lon: -0.7
Helmsley lies in a hollow in undulating open countryside, flanked by heather moor to the north and the rolling farmland of the Howardian Hills to the south. The flat lowland of the Vale of Pickering stretches eastwards from the town towards Malton. The River Rye runs by the town to the south where it is joined at Rye Bridge by the Borough Beck flowing southwards through the town from the moors.

Geographic entities mentioned:
surface_form: Vale of Pickering
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.2
lon: -0.7
Stratherrick. Stratherrick () is a strath situated above the south-eastern shore of Loch Ness, in the Scottish Highlands, Scotland. Much of the strath is covered by Loch Mhòr. This is a generally shallow loch, which acts as a reservoir for the Foyers hydro electricity schemes. The area has a number of small settlements, these include Whitebridge, Gorthleck, Aberchalder and Errogie.

Geographic entities mentioned:
surface_form: Loch Ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
surface_form: ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
surface_form: stratherrick
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.25
lon: -4.42
Stratherrick. Stratherrick () is a strath situated above the south-eastern shore of Loch Ness, in the Scottish Highlands, Scotland. Much of the strath is covered by Loch Mhòr. This is a generally shallow loch, which acts as a reservoir for the Foyers hydro electricity schemes. The area has a number of small settlements, these include Whitebridge, Gorthleck, Aberchalder and Errogie.

Geographic entities mentioned:
surface_form: Loch Mhòr
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.246
lon: -4.418
Stratherrick. Stratherrick () is a strath situated above the south-eastern shore of Loch Ness, in the Scottish Highlands, Scotland. Much of the strath is covered by Loch Mhòr. This is a generally shallow loch, which acts as a reservoir for the Foyers hydro electricity schemes. The area has a number of small settlements, these include Whitebridge, Gorthleck, Aberchalder and Errogie.

Geographic entities mentioned:
surface_form: stratherrick
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.25
lon: -4.42
Much of the strath is covered by Loch Mhòr. This is a generally shallow loch, which acts as a reservoir for the Foyers hydro electricity schemes. The area has a number of small settlements, these include Whitebridge, Gorthleck, Aberchalder and Errogie. Stratherrick Primary School is in Gorthleck. There is a Catholic church, Immaculate Conception Parish Church, Stratherrick near Whitebridge.

Geographic entities mentioned:
surface_form: stratherrick
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.25
lon: -4.42
Gohlig. Gohlig is a mountain of Saxony, southeastern Germany.

Geographic entities mentioned:
surface_form: gohlig
instance_of: Mountain
countries: Germany
coordinates: lat: 50.9828
lon: 13.7192
Central and Western Kenya is characterized by the Kenyan Rift Valley and central Province home to the highest mountain, Mount Kenya and Mount Elgon on the border between Kenya and Uganda. The Kakamega Forest in western Kenya is a relic of an East African rainforest. Much bigger is Mau Forest, the largest forest complex in East Africa. Geology.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
surface_form: Mount Elgon
instance_of: Mountain
countries: Uganda
Kenya
coordinates: lat: 1.1185
lon: 34.5265
Although Kenya is centred at the equator, it shares the seasons of the Southern Hemisphere: with the warmest summer months in December–March and the coolest winter months in June–August, again with differences in temperature varying by location within the country. On the high mountains, such as Mount Kenya, Mount Elgon and Kilimanjaro, the weather can become bitterly cold for most of the year.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
surface_form: Mount Elgon
instance_of: Mountain
countries: Uganda
Kenya
coordinates: lat: 1.1185
lon: 34.5265
Terrain. Kenya's terrain is composed of low plains that rise into central highlands that are, in turn, bisected by the Great Rift Valley. There is also a fertile plateau in the west of the country. Elevation extremes. The lowest point on Kenya is at sea level on the Indian Ocean. The highest point on Kenya is 5,199 meters above sea level at Mount Kenya. Rivers.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
The notable rivers in Kenya are the Athi-Galana-Sabaki River, which at a total length of about 390 kilometers while draining an area of about 70,000 square kilometers, is the second longest river in the country, the Tana River, the longest river in the country at a total length of just over 1000 kilometers, covering a catchment area of over 100,000 square kilometers, and the Nzoia River, which is a river, rising from Mount Elgon, which flows south.

Geographic entities mentioned:
surface_form: Mount Elgon
instance_of: Mountain
countries: Uganda
Kenya
coordinates: lat: 1.1185
lon: 34.5265
Current issues. Current issues that threaten the environment at the moment include water pollution from urban and industrial wastes; degradation of water quality from the increased use of pesticides and fertilisers; deforestation; water hyacinth infestation in Lake Victoria; soil erosion; desertification; and poaching. Extreme points.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Two years later, part of this land was separated from the Common, with the southwest portion used for public buildings—including a granary and jail—and the north portion dedicated to an almshouse (probably the first in the Thirteen Colonies). Boston Common took over from the gibbet outside the gate of Boston Neck as the town execution grounds and was used for public hangings until 1817.

Geographic entities mentioned:
surface_form: Boston Neck
instance_of: Landform
countries: United States
coordinates: lat: 42.34394444
lon: -71.06597222
Biography. Pere was born in Ruatahuna in the Bay of Plenty on 25 July 1937. For her first seven years she lived with her maternal grandparents southeast of Waikaremoana. From 1944 she attended Kokako Native School. Between 1956 and 1957 she went to Wellington Teachers' College and obtained a New Zealand Teacher's Certificate.

Geographic entities mentioned:
surface_form: Waikaremoana
instance_of: Lake
countries: New Zealand
coordinates: lat: -38.766666666667
lon: 177.08333333333
McNutt also worked to settle a group of disbanded New England soldiers, which included Israel Perley, along the Saint John River. In 1764 he began negotiations with John Hughes of Philadelphia, an undertaking that culminated two years later with 60 Pennsylvania-German settlers establishing The Township of Monckton on the Petitcodiac River.

Geographic entities mentioned:
surface_form: Petitcodiac River
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.926944444444
lon: -65.188888888889
The Vesdre's total length is approximately. It is a right tributary to the river Ourthe. Its source lies in the High Fens (,), close to the border with Germany near Monschau. It flows through an artificial lake (Lake Eupen), and then through the towns of Eupen, Verviers, Pepinster and Chaudfontaine.

Geographic entities mentioned:
surface_form: High Fens
instance_of: Plateau
countries: Belgium
Germany
coordinates: lat: 50.521389
lon: 6.102778
Sgùrr a' Mhàim. is a mountain of the Mamores range in the Scottish Highlands. It is directly south of Ben Nevis, on the other side of Glen Nevis. With a height of 1,099 metres (3,605 feet), Sgùrr a' Mhàim is a Munro and the second-highest peak in the Mamores. Its cap of quartzite stones give it a light grey appearance which can be mistaken for a covering of snow. Landscape.

Geographic entities mentioned:
surface_form: Ben Nevis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.796891
lon: -5.003675
Landscape. Sgùrr a' Mhàim is the first or last peak of the 'Ring of Steall', a ridge walk taking in the other Munros of An Gearanach, Stob Coire a' Chàirn and Am Bodach. It is linked to the main spine of the Mamore group on its southern side by a feature called The Devil's Ridge, which is a one-kilometre undulating ridge with a few exposed sections which require care.

Geographic entities mentioned:
surface_form: An Gearanach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.759146
lon: -4.966211
surface_form: Stob Coire a' Chàirn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.750747
lon: -4.969017
surface_form: Am Bodach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.741729
lon: -4.983387
surface_form: sgùrr a' mhàim
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.75592
lon: -5.00369
Both these routes require some scrambling. A more circuitous ascent goes up to the head of Coire a' Mhusgain from Achriabhach to cross the ridge to the summit. The summit cairn is substantial being made up of light coloured quartzite stones and gives a view of the southern side of Ben Nevis, and also an aerial view down into Glen Nevis.

Geographic entities mentioned:
surface_form: Ben Nevis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.796891
lon: -5.003675
Sgùrr a' Mhàim. is a mountain of the Mamores range in the Scottish Highlands. It is directly south of Ben Nevis, on the other side of Glen Nevis. With a height of 1,099 metres (3,605 feet), Sgùrr a' Mhàim is a Munro and the second-highest peak in the Mamores. Its cap of quartzite stones give it a light grey appearance which can be mistaken for a covering of snow. Landscape.

Geographic entities mentioned:
surface_form: sgùrr a' mhàim
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.75592
lon: -5.00369
At the southern end of the ridge is Sgùrr an Iubhair ('peak of the yew'), a 1,001 m peak that briefly gained Munro status in 1981 only to lose it again in 1997. When viewed from the ridge, Sgùrr an Iubhair appears to be a separate mountain, but both the above peaks are listed as &quot;tops&quot; of Sgùrr a' Mhàim in the Munro Tables.

Geographic entities mentioned:
surface_form: sgùrr a' mhàim
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.75592
lon: -5.00369
surface_form: sgùrr a' mhàim
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.75592
lon: -5.00369
Lemuel Cushing. upnrlm64jkpf9v7q6rq20xovgy9qf" xml:space="preserve">Lemuel Cushing (April 29, 1806 &ndash; May 18, 1875) was a businessman and pioneer in the Ottawa valley. He was born in Trois-Rivières, Lower Canada, the son of Job Cushing, who came to the Eastern Townships from the United States. Cushing moved to Montreal with his parents at the age of eight.

Geographic entities mentioned:
surface_form: Ottawa valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
Pizzo Alzasca. Pizzo Alzasca is a mountain of the Swiss Lepontine Alps, overlooking Cevio in the canton of Ticino. On the south side lies the lake of Alzasca.

Geographic entities mentioned:
surface_form: lake of Alzasca
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.265974
lon: 8.584833
Pizzo Alzasca. Pizzo Alzasca is a mountain of the Swiss Lepontine Alps, overlooking Cevio in the canton of Ticino. On the south side lies the lake of Alzasca.

Geographic entities mentioned:
surface_form: pizzo alzasca
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.277444444444
lon: 8.5761111111111
The hills name translates from the Gaelic as &quot;Peak of the White Stone&quot;, this refers to an area of light coloured quartzite rocks near the summit. Geography. Sgùrr nan Clach Geala stands on a north-south ridge in the western part of the Fannichs along with two other Munros, Meall a' Chrasgaidh and Sgùrr nan Each.

Geographic entities mentioned:
surface_form: Meall a' Chrasgaidh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.712866
lon: -5.048742
surface_form: Sgùrr nan Each
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.680833333333
lon: -5.0466666666667
surface_form: meall a' chrasgaidh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.712866
lon: -5.048742
surface_form: sgùrr nan each
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.680833333333
lon: -5.0466666666667
Drainage from the mountain reaches both coasts of Scotland, rainfall on the west and northern slopes go via the River Broom and Loch Broom to reach the west coast at Ullapool. Drainage from the south and east flank goes south to Loch Fannich to eventually reach the east coast at the Cromarty Firth. Ascents and summit.

Geographic entities mentioned:
surface_form: Loch Fannich
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.6417
lon: -5.0032
surface_form: loch fannich
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.6417
lon: -5.0032
The eastern cliffs fall precipitously into Coire Mòr directly from the summit. The view takes in all but one of the Fannichs and is an excellent place to study the geography of the group. There is an excellent view of An Teallach 18 kilometres away to the north west, while the valley of the Allt a‘ Choire Mhoir looks impressive to the south as it flows down to Loch Fannich.

Geographic entities mentioned:
surface_form: An Teallach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.806530555556
lon: -5.2516611111111
surface_form: an teallach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.806530555556
lon: -5.2516611111111
surface_form: loch fannich
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.6417
lon: -5.0032
These Schist cliffs have attracted winter ice climbers with 20 named routes available, the best known being Skyscraper Buttress and Gamma Gully. Drainage from the mountain reaches both coasts of Scotland, rainfall on the west and northern slopes go via the River Broom and Loch Broom to reach the west coast at Ullapool.

Geographic entities mentioned:
surface_form: loch broom
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.7
lon: -3.6166666666667
Most walkers will continue south from the summit to take in Sgùrr nan Each before returning to the starting point via the Allt Breabaig. The summit of the mountain has the remains of a trig point, it has been vandalised and seems to have been attacked with a sledgehammer, leaving only a quarter of the pillar remaining. The eastern cliffs fall precipitously into Coire Mòr directly from the summit.

Geographic entities mentioned:
surface_form: pillar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.497
lon: -3.282
Overview. With a height of 1093 metres (3586 feet) Sgùrr nan Clach Geala is the second highest of the Fannaichs behind Sgùrr Mòr and is regarded by many as the best peak of the group with its fine east facing corrie and pointed buttresses. The hill is not easily seen from any public road being situated in the centre of the group some eight kilometres from the A832 road to the south.

Geographic entities mentioned:
surface_form: best peak
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -54.1167
lon: -36.8167
surface_form: sgùrr nan clach geala
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.696944444444
lon: -5.0480555555556
surface_form: sgùrr mòr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.700133
lon: -5.016765
surface_form: sgùrr mòr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.028446
lon: -5.354189
Sgùrr nan Clach Geala. Sgùrr nan Clach Geala is a mountain in Wester Ross in the Northwest Highlands of Scotland, south of Ullapool. With a height of, it is one of ten Munros in the group of hills known as the Fannichs. Overview.

Geographic entities mentioned:
surface_form: sgùrr nan clach geala
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.696944444444
lon: -5.0480555555556
Ascents and summit. The most usual route of ascent approaches from the north starting at a parking spot on the A832 at grid reference and climbs the adjoining Munro of Meall a' Chrasgaidh before climbing Sgùrr nan Clach Geala. Most walkers will continue south from the summit to take in Sgùrr nan Each before returning to the starting point via the Allt Breabaig.

Geographic entities mentioned:
surface_form: sgùrr nan clach geala
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.696944444444
lon: -5.0480555555556
surface_form: meall a' chrasgaidh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.712866
lon: -5.048742
The hill is not easily seen from any public road being situated in the centre of the group some eight kilometres from the A832 road to the south. The best views are from nearby mountains with the eastern cliffs being seen to best effect from Sgùrr Mòr across Coire Mòr.

Geographic entities mentioned:
surface_form: sgùrr mòr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.700133
lon: -5.016765
surface_form: sgùrr mòr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.028446
lon: -5.354189
This northern ridge drops down to a col with a height of 819 metres called Am Biachdaich (The Feeding Place), named because of the col's rich pastures where deer often feed. From the col the Munros of Meall a' Chrasgaidh and Sgùrr Mòr can be climbed, a small lochan lies on the col.

Geographic entities mentioned:
surface_form: sgùrr mòr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.700133
lon: -5.016765
surface_form: meall a' chrasgaidh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.712866
lon: -5.048742
surface_form: sgùrr mòr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.028446
lon: -5.354189
From the col the Munros of Meall a' Chrasgaidh and Sgùrr Mòr can be climbed, a small lochan lies on the col. The southern ridge of the mountain connects to the Munro of Sgùrr nan Each, which lies just under two kilometres away across a col with a height of 815 metres. The mountains western slopes are mostly grassy with a few rocky outcrops as they drop down to the valley of the Allt Breabaig.

Geographic entities mentioned:
surface_form: sgùrr nan each
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.680833333333
lon: -5.0466666666667
Ascents and summit. The most usual route of ascent approaches from the north starting at a parking spot on the A832 at grid reference and climbs the adjoining Munro of Meall a' Chrasgaidh before climbing Sgùrr nan Clach Geala. Most walkers will continue south from the summit to take in Sgùrr nan Each before returning to the starting point via the Allt Breabaig.

Geographic entities mentioned:
surface_form: sgùrr nan each
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.680833333333
lon: -5.0466666666667