Sarmila/GeoWiki-Features huggingface dataset:
After the desolation of the Neutral tribe, the Iroquois Confederacy used the Grand River Valley as a hunting ground and trapping territory. Though the Six Nations (by then including the Tuscarora) held the territory by right of conquest, they did not settle it, apart from a limited presence on the northern and western shores of Lake Ontario.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Lake Muhazi. Lake Muhazi () is a long, thin shallow lake in the east of Rwanda. The bulk of the lake lies in the Eastern Province, with the western end forming the border between the Northern and Kigali Provinces. It is a flooded valley lake, lying predominantly in an east to west direction, but with numerous offshoots in a north to south direction, formerly the location of tributaries.

Geographic entities mentioned:
surface_form: kigali
instance_of: Mountain
countries: Rwanda
coordinates: lat: -1.95
lon: 30.06666667
The lake has a concrete dam at the western end, constructed in 1999 to replace an earth dam which had existed since time immemorial. The lake empties into the Nyabugogo River, which flows southwards to Kigali, where it meets the Nyabarongo River, part of the upper Nile. Description. Lake Muhazi is located in the eastern part of Rwanda, at coordinates.

Geographic entities mentioned:
surface_form: kigali
instance_of: Mountain
countries: Rwanda
coordinates: lat: -1.95
lon: 30.06666667
It is accessible from three of Rwanda's primary routes. The Kigali to Gatuna road passes close to the lake's western end, the Kigali to Kayonza road, which runs parallel to the lake to the south; finally, the Kayonza to Kagitumba road runs along the lakeshore for near Gahini, before passing over two of the ridges emanating from the lake and finally leaving the lake near Kawangire.

Geographic entities mentioned:
surface_form: kigali
instance_of: Mountain
countries: Rwanda
coordinates: lat: -1.95
lon: 30.06666667
surface_form: kigali
instance_of: Mountain
countries: Rwanda
coordinates: lat: -1.95
lon: 30.06666667
It is located in east-central Rwanda and has shoreline in three of the country's five provinces. The western third of the lake forms the border between Kigali Province (Gasabo District) to the south, and Northern Province (Gicumbi District) to the north.

Geographic entities mentioned:
surface_form: kigali
instance_of: Mountain
countries: Rwanda
coordinates: lat: -1.95
lon: 30.06666667
Eventually, in around 1830, Gisaka was annexed and the eastern borders of the state began to take their present form, with the lake fully under Rwandan control. Under German and Belgian colonial rule Lake Muhazi became an important east–west transport route, linking Kigali and the west of the country with the north–south and eastbound roads from Gahini.

Geographic entities mentioned:
surface_form: kigali
instance_of: Mountain
countries: Rwanda
coordinates: lat: -1.95
lon: 30.06666667
surface_form: lake muhazi
instance_of: Lake
countries: Rwanda
coordinates: lat: -1.85
lon: 30.4
Lake Muhazi, in common with the rest of Rwanda, has a temperate tropical highland climate, with lower temperatures than are typical for equatorial countries due to its high elevation. Temperature measurements in Kigali, which lies approximately south-west of the lake, show a typical daily temperature range between and, with little variation through the year.

Geographic entities mentioned:
surface_form: kigali
instance_of: Mountain
countries: Rwanda
coordinates: lat: -1.95
lon: 30.06666667
These are used both as stop off points for journeys to or from Akagera National Park, and as venues for lake tourism, offering boating, fishing and bird watching. There are also several resorts at Rwesero, on the north-eastern shore of the lake, including Rwesero Beach, offering camping accommodation and also popular with day-trippers from Kigali.

Geographic entities mentioned:
surface_form: kigali
instance_of: Mountain
countries: Rwanda
coordinates: lat: -1.95
lon: 30.06666667
Lake Muhazi. Lake Muhazi () is a long, thin shallow lake in the east of Rwanda. The bulk of the lake lies in the Eastern Province, with the western end forming the border between the Northern and Kigali Provinces. It is a flooded valley lake, lying predominantly in an east to west direction, but with numerous offshoots in a north to south direction, formerly the location of tributaries.

Geographic entities mentioned:
surface_form: lake muhazi
instance_of: Lake
countries: Rwanda
coordinates: lat: -1.85
lon: 30.4
The lake empties into the Nyabugogo River, which flows southwards to Kigali, where it meets the Nyabarongo River, part of the upper Nile. Description. Lake Muhazi is located in the eastern part of Rwanda, at coordinates. It is accessible from three of Rwanda's primary routes.

Geographic entities mentioned:
surface_form: lake muhazi
instance_of: Lake
countries: Rwanda
coordinates: lat: -1.85
lon: 30.4
and it is a research proposal of Mediatrice, Irene and Sandra
Lake Muhazi is 60 km long, in an east–west direction, but its width is less than 5 km. It is located in east-central Rwanda and has shoreline in three of the country's five provinces.

Geographic entities mentioned:
surface_form: lake muhazi
instance_of: Lake
countries: Rwanda
coordinates: lat: -1.85
lon: 30.4
1993). History. According to oral history the Kingdom of Rwanda was founded in the 14th century after disintegration of Kitara empire on the shores of Lake Muhazi in the Buganza area, close to the modern city of Rwamagana. At that time Rwanda was a small state in a loose confederation with larger and more powerful neighbours, Bugesera and Gisaka.

Geographic entities mentioned:
surface_form: lake muhazi
instance_of: Lake
countries: Rwanda
coordinates: lat: -1.85
lon: 30.4
In this expanded kingdom, the region around the lake became a powerful religious site, being synonymous with the earliest and most revered mwamis of the kingdom. In the late 16th or early 17th centuries, the kingdom of Rwanda was invaded by the Banyoro and the kings forced to flee westward, leaving Buganza and the Lake Muhazi area in the hands of Bugesera and Gisaka.

Geographic entities mentioned:
surface_form: lake muhazi
instance_of: Lake
countries: Rwanda
coordinates: lat: -1.85
lon: 30.4
Lake Muhazi became a border zone between Rwanda and the still independent Gisaka, a situation which remained in place for 200 years, despite several unsuccessful attempts by the Rwandan kings to subdue Gisaka. Eventually, in around 1830, Gisaka was annexed and the eastern borders of the state began to take their present form, with the lake fully under Rwandan control.

Geographic entities mentioned:
surface_form: lake muhazi
instance_of: Lake
countries: Rwanda
coordinates: lat: -1.85
lon: 30.4
This land was returned to Belgium in 1924 but the rulers allowed the CMS to continue its work, and a permanent mission and hospital was set up close to Lake Muhazi in Gahini village. In common with the rest of the country, Lake Muhazi was the scene of many killings during the 1994 Rwandan genocide.

Geographic entities mentioned:
surface_form: lake muhazi
instance_of: Lake
countries: Rwanda
coordinates: lat: -1.85
lon: 30.4
Large numbers of bodies were discarded in the lake by Interahamwe militias, while others drowned attempting to escape; witnesses described the water at the time as &quot;mixed with blood.&quot;
Geology and climate. The rocks underlying Lake Muhazi vary along its length. The western end, which is flanked by high hills has a schist base, while the soil at the eastern end is granite based.

Geographic entities mentioned:
surface_form: lake muhazi
instance_of: Lake
countries: Rwanda
coordinates: lat: -1.85
lon: 30.4
Rwanda housing authority (RHA) has recently completed the land control study and the elaboration of the town planning development project of the shores of lake Muhazi. The main objective of the study was to identify the sectors of the northern and eastern shores of lake Muhazi which are subjected to land pressure so as to establish protection belts and safeguard them.

Geographic entities mentioned:
surface_form: lake muhazi
instance_of: Lake
countries: Rwanda
coordinates: lat: -1.85
lon: 30.4
The region is sometimes referred to colloquially as &quot;the Elbtal&quot; (Elbe valley). The wine region covers, which makes it Germany's third smallest region, just ahead of Mittelrhein and Hessische Bergstraße in size. It is situated along the Elbe river from the Pillnitz section of Dresden to the village of Diesbar-Seußlitz located north of Meissen.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Lake Baikal) and southeast of Yenisei Kyrgyzes; the &quot;courageous and powerful&quot; Basmyls numbered 2,000 families, and had leaders but no princes (Tigin) Since 552, the Basmyls became a part of the First Turkic Khaganate, who might have recognized Basmyls' economic or political importance enough to appoint an Ashina yabghu over the Basmyls.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Shelikhov Gulf. Shelikhov Gulf () is a large gulf off the northwestern coast of Kamchatka, Russia. The gulf is named after Russian explorer Grigory Shelikhov. It is located in the northeastern corner of the Sea of Okhotsk and branches into two main arms, Gizhigin Bay to the west and Penzhina Bay to the east. Its southwest corner is formed by the P'yagin Peninsula, Yam Bay, and the Yamsky Islands.

Geographic entities mentioned:
surface_form: Yam Bay
instance_of: Body of water
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 59.71
lon: 154.428611
Kandidiana Ridge. Kandidiana Ridge (, ‘Rid Kandidiana’ \'rid kan-di-di-'a-na\) is the partly ice-free ridge extending 6 km and 1.1 km wide, rising to 1176 m on the west side of Elgar Uplands in northern Alexander Island, Antarctica. It is crescent-shaped facing north-northwest, and surmounts Nichols Snowfield to the northwest, Delius Glacier to the northeast and Bartók Glacier to the south.

Geographic entities mentioned:
surface_form: Elgar Uplands
instance_of: Landform
coordinates: lat: -69.65
lon: -70.7167
The feature is named after the ancient Roman fortress of Kandidiana in Northeastern Bulgaria. Location. The ridge is located at, which is 4.45 km west-northwest of Kozhuh Peak, 12.24 km north-northwest of Mount Pinafore, 18.67 km east of Mount Morley in Lassus Mountains, 15.26 km southeast of Shaw Nunatak and 9 km south of Tegra Nunatak.

Geographic entities mentioned:
surface_form: Kozhuh Peak
instance_of: Mountain
coordinates: lat: -69.678333333333
lon: -70.921388888889
surface_form: Mount Pinafore
instance_of: Mountain
coordinates: lat: -69.7667
lon: -70.8667
surface_form: Mount Morley
instance_of: Mountain
coordinates: lat: -69.6667
lon: -71.4667
surface_form: Shaw Nunatak
instance_of: Mountain
coordinates: lat: -69.55
lon: -71.2
Fogo Island (Newfoundland and Labrador). Fogo Island (&quot;Fogo&quot;, Portuguese for &quot;Fire&quot;) is the largest of the offshore islands of Newfoundland and Labrador, Canada. It lies off the northeast coast of Newfoundland, northwest of Musgrave Harbour across Hamilton Sound, just east of the Change Islands. The island is about long and wide. The total area is.

Geographic entities mentioned:
surface_form: Hamilton Sound
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.55
lon: -54.11666666666667
It is part of the Logan, Utah-Idaho Metropolitan Statistical Area. History. The Bear River Massacre occurred in 1863 at a point a few miles northwest of Preston. The Bear River Massacre Site is a National Historic Landmark. In 1866, Latter-day Saint pioneers arrived in the northern end of the Cache Valley, stretching across southeastern Idaho and northeastern Utah.

Geographic entities mentioned:
surface_form: Cache Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.816666666667
lon: -111.93416666667
Course. Depot Creek begins at an unnamed lake Whatcom County, Washington State, United States, located in a cirque between Mount Redoubt and Mount Spickard. The creek exits the lake and flows northwest into a large, swamp-like area at the top of Depot Creek Falls. The creek then drops over the falls and reaches the bottom of the valley.

Geographic entities mentioned:
surface_form: Mount Spickard
instance_of: Mountain
countries: United States
coordinates: lat: 48.9697
lon: -121.241
The creek then drops over the falls and reaches the bottom of the valley. From here the creek flows northwest, passes into British Columbia, Canada, and reaches its mouth at Chilliwack Lake near the lake's south end. Chilliwack Lake flows via the Chilliwack River and the Fraser River to the Pacific Ocean.

Geographic entities mentioned:
surface_form: Chilliwack Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.05694444444445
lon: -121.41388888888889
The Cariboo Gold Rush was a gold rush in the Colony of British Columbia, which later became the Canadian province of British Columbia. The first gold discovery was made at Hills Bar in 1858, followed by more strikes in 1859 on the Horsefly River, and on Keithley Creek and Antler Creek in 1860. The actual rush did not begin until 1861, when these discoveries were widely publicized.

Geographic entities mentioned:
surface_form: Antler Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 53.25833333
lon: -121.41083333
360. In 1981, the tensions with Peru were rekindled by a military confrontation over the Cenepa River in the Cordillera del Cóndor. The conflict was centered in the Paquisha, Mayaycu and Manchinaza localities. By 1995 the conflict had reemerged, and in 1999 the signing of the Peace Agreement between Ecuador and Peru settled the contours of Zamora-Chinchipe's borders with its southern neighbor.

Geographic entities mentioned:
surface_form: Cordillera del Cóndor
instance_of: Mountain
countries: Ecuador
Peru
coordinates: lat: -4
lon: -78.5
Gretchen ultimately falls into a faint. Walpurgis Night and Walpurgis Night's Dream
A folk belief holds that during the Walpurgis Night (&quot;Walpurgisnacht&quot;) on the night of 30 April—the eve of the feast day of Saint Walpurga—witches gather on the Brocken mountain, the highest peak in the Harz Mountains, and hold revels with the Devil.

Geographic entities mentioned:
surface_form: Brocken
instance_of: Mountain
countries: Germany
Kingdom of Prussia
coordinates: lat: 51.800555555556
lon: 10.617222222222
West Hills, Los Angeles. West Hills is a neighborhood in the western San Fernando Valley region of the city of Los Angeles, California. It is bordered by mountain ranges to the west and the Los Angeles neighborhoods of Chatsworth to the north, Canoga Park to the east, and Woodland Hills to the south.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Water resources. Bell and Dayton creeks in West Hills are several of the headwaters of the Los Angeles River that originate in the Northwest San Fernando Valley. The Los Angeles River itself begins at the confluence of Arroyo Calabasas (Calabasas Creek) and Bell Creek in Canoga Park.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Bayan Har block. The Bayan Har block or Bayan Kola block is an elongate wedge-shaped block that forms part of the eastern Tibetan Plateau. It is bounded to the southeast by the Longmenshan Fault, a major thrust fault zone, which forms the active tectonic boundary between the plateau and the Sichuan Basin.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Ben Cleuch. Ben Cleuch is a hill in the Ochil Hills range, part of the Central Lowlands of Scotland. It is the highest point in the range, Clackmannanshire and the Central Belt of Scotland; the summit is marked by a trig point within a stone windshelter and a viewpoint indicator. Features.

Geographic entities mentioned:
surface_form: Central Lowlands
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.408
lon: -4.044
surface_form: ben cleuch
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.1858
lon: -3.7698
Features. On a clear day, the views are excellent, particularly those to the north looking towards the Southern Highlands. Ben Lomond, Ben Ledi, Stùc a' Chroin and Ben Vorlich are especially prominent. Looking to the south gives excellent views over the Forth Valley region, the Forth bridges and Edinburgh to the east, Glasgow to the west: almost a coast to coast view but not quite. Geodesy.

Geographic entities mentioned:
surface_form: Ben Lomond
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.190293
lon: -4.633009
surface_form: Ben Ledi
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.258659
lon: -4.322375
surface_form: Stùc a' Chroin
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.329315
lon: -4.237533
surface_form: Ben Vorlich
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.274021
lon: -4.755046
surface_form: ben vorlich
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.34268
lon: -4.219464
surface_form: lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
Ben Cleuch. Ben Cleuch is a hill in the Ochil Hills range, part of the Central Lowlands of Scotland. It is the highest point in the range, Clackmannanshire and the Central Belt of Scotland; the summit is marked by a trig point within a stone windshelter and a viewpoint indicator. Features.

Geographic entities mentioned:
surface_form: ben cleuch
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.1858
lon: -3.7698
Ben Lomond, Ben Ledi, Stùc a' Chroin and Ben Vorlich are especially prominent. Looking to the south gives excellent views over the Forth Valley region, the Forth bridges and Edinburgh to the east, Glasgow to the west: almost a coast to coast view but not quite. Geodesy. Ben Cleuch was the origin (meridian) of the six-inch and 1:2500 Ordnance Survey maps of the counties of Perth and Clackmannan.

Geographic entities mentioned:
surface_form: ben cleuch
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.1858
lon: -3.7698
&quot;Oshima&quot; is close to the shore and can also be crossed. The inspiration for the pond originates from West Lake in Hangzhou, and the rocks on the central island represent the mountains of West Lake. One corner of the pond includes a sandy beach area named &quot;Suhama&quot;, although swimming is not recommended.

Geographic entities mentioned:
surface_form: West Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 30.2375
lon: 120.14083333333
The rivers in the eastern areas of the district drain into the Pes River. Since the Pes belongs to the basin of the Volga, and the Syas, the Pchyovzha, and the Msta all belong to the basin of the Neva, the district is crossed by the divide between the basins of the Atlantic Ocean and the Caspian Sea.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Hanafjellet. Hanafjellet is the commonly used name for the small mountain located in the city of Sandnes in the western part of the large municipality of Sandnes in Rogaland county, Norway. &quot;Hanafjellet&quot; or &quot;Hana Hills&quot; lies in the northern part of the borough of Hana, separating Hana from the small village of Aspervika.

Geographic entities mentioned:
surface_form: hanafjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 64.133333333333
lon: 10.3
Kiboreia. j2hkq0mh0vjzte7i4r2aefnwbeyhv" xml:space="preserve">Kiboreia is a location that is known from a Greek inscription taken from a large temple at Deir El Aachayer on the northern slopes of Mount Hermon in Lebanon.

Geographic entities mentioned:
surface_form: Mount Hermon
instance_of: Mountain
countries: Lebanon
Israel
Syria
coordinates: lat: 33.4
lon: 35.85
Thankerton. Thankerton is a small village in South Lanarkshire, Scotland, United Kingdom. It is located between Biggar and Lanark, and situated between Quothquan Law and Tinto (two local hills). Thankerton's name derives from an early feudal lord called Thancard the Fleming, and means Thancard's enclosure.

Geographic entities mentioned:
surface_form: Tinto
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.591938888889
lon: -3.6628805555556
In Provence, probably between 9,000 and 7,000 years ago, it gave rise to the haplogroup subclade U5b3a1. This subclade U5b3a1 later came from Provence to the island of Sardinia by way of obsidian merchants, because it is estimated that 80% of the obsidian which is found in France comes from Monte Arci in Sardinia, reflecting the close relationship which once existed between these two regions.

Geographic entities mentioned:
surface_form: Monte Arci
instance_of: Mountain
countries: Italy
coordinates: lat: 39.777777777778
lon: 8.745
Karoro Pond. Karoro Pond () is a pond north-northeast of Mount J. J. Thomson on the rock divide separating Matterhorn Glacier and Rhone Glacier in Victoria Land. It was named by the New Zealand Geographic Board in 1998 after the New Zealand gull of that name.

Geographic entities mentioned:
surface_form: karoro pond
instance_of: Lake
coordinates: lat: -77.67472222
lon: 162.2675
Karoro Pond. Karoro Pond () is a pond north-northeast of Mount J. J. Thomson on the rock divide separating Matterhorn Glacier and Rhone Glacier in Victoria Land. It was named by the New Zealand Geographic Board in 1998 after the New Zealand gull of that name.

Geographic entities mentioned:
surface_form: gull
instance_of: Body of water
coordinates: lat: -68.1867
lon: -66.9872
Karoro Pond. Karoro Pond () is a pond north-northeast of Mount J. J. Thomson on the rock divide separating Matterhorn Glacier and Rhone Glacier in Victoria Land. It was named by the New Zealand Geographic Board in 1998 after the New Zealand gull of that name.

Geographic entities mentioned:
surface_form: matterhorn
instance_of: Mountain
coordinates: lat: -71.855
lon: 8.3297222222222
It is located in the Ancash Region, Bolognesi Province, Pacllon District, and in the Lima Region, Cajatambo Province, Copa District. Auxilio lies on the sub-range west of Yerupaja, south of Auxilio Lake and southwest of the mountain Huacrish.

Geographic entities mentioned:
surface_form: Huacrish
instance_of: Mountain
countries: Peru
coordinates: lat: -10.2986
lon: -76.9639
surface_form: huacrish
instance_of: Mountain
countries: Peru
coordinates: lat: -10.2986
lon: -76.9639
surface_form: auxilio
instance_of: Mountain
countries: Peru
coordinates: lat: -10.3056
lon: -76.9653
It is located in the Ancash Region, Bolognesi Province, Pacllon District, and in the Lima Region, Cajatambo Province, Copa District. Auxilio lies on the sub-range west of Yerupaja, south of Auxilio Lake and southwest of the mountain Huacrish.

Geographic entities mentioned:
surface_form: copa
instance_of: Mountain
countries: Peru
coordinates: lat: -9.2666666666667
lon: -77.516666666667
Auxilio. Auxilio (possibly from Quechua &quot;Awkillu&quot; word for apu (Andean mountain deity) or grandfather, old man, the Hispanicized spelling is the misleading word &quot;Auxilio&quot; which means &quot;assistance&quot; or &quot;support&quot;) is a mountain in the west of the Huayhuash mountain range in the Andes of Peru, about high.

Geographic entities mentioned:
surface_form: auxilio
instance_of: Mountain
countries: Peru
coordinates: lat: -10.3056
lon: -76.9653
Auxilio. Auxilio (possibly from Quechua &quot;Awkillu&quot; word for apu (Andean mountain deity) or grandfather, old man, the Hispanicized spelling is the misleading word &quot;Auxilio&quot; which means &quot;assistance&quot; or &quot;support&quot;) is a mountain in the west of the Huayhuash mountain range in the Andes of Peru, about high.

Geographic entities mentioned:
surface_form: auxilio
instance_of: Mountain
countries: Peru
coordinates: lat: -10.3056
lon: -76.9653
surface_form: auxilio
instance_of: Mountain
countries: Peru
coordinates: lat: -10.3056
lon: -76.9653
surface_form: awkillu
instance_of: Mountain
countries: Peru
coordinates: lat: -10.3056
lon: -76.9653
This formation is up to 140 metres thick. Formed in the middle Miocene, some 17 million to 14 million years ago. The remnants of this volcanic lava flow are confined to the higher altitudes in the western Blue Mountains. Such as Mount Hay, Mount Wilson, Mount Irvine, Mount Banks and Mount Tomah. The olivine basalt caps create red/brown soils, known as red podzolics or &quot;krasnozems&quot;.

Geographic entities mentioned:
surface_form: Mount Banks
instance_of: Mountain
countries: Australia
coordinates: lat: -33.5886
lon: 150.3712
Rasbora tawarensis. &quot;Rasbora tawarensis&quot;, locally known as depik, is a critically endangered species of cyprinid fish. It is endemic to Lake Laut Tawar in Indonesia, where its population is rapidly decreasing due to ecological disturbances, global warming, introduced species, unlawful fishing practices, and pollution. Description.

Geographic entities mentioned:
surface_form: Lake Laut Tawar
instance_of: Lake
countries: Indonesia
coordinates: lat: 4.6112
lon: 96.9267
1962: CP track dynamited and fire destroyed over 30 residences. Back-to-the-land movement. The back-to-the-land movement began during the late 1960s with new arrivals into the 1980s. The Slocan Valley was the focal point for BC. The various communes flourished 1968–1973. The New Family formed a commune on timbered land above Winlaw, buying in 1968 and the following spring.

Geographic entities mentioned:
surface_form: Slocan Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.6834
lon: -117.5024
Castle Lake (California). Castle Lake is a glacial lake (&quot;cirque&quot; lake or tarn) located in the Trinity Mountains, in Siskiyou County of northern California. It is west of Mount Shasta City and Mount Shasta peak. The outlet of the lake drains into Castle Lake Creek, and then into Lake Siskiyou reservoir, part of the headwaters of the Sacramento River.

Geographic entities mentioned:
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: mount shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: mount shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
About from the lake, along this road, are Ney Springs and Faery Falls. Ney Springs is the site of the historic Ney Springs Resort, a late 19th-century resort based on the mineral springs there; this resort was one of a number of such popular resorts in Siskiyou County, including Upper Soda Springs, and Shasta Springs.

Geographic entities mentioned:
surface_form: Upper Soda Springs
instance_of: Landform
countries: United States
coordinates: lat: 41.2219
lon: -122.277
surface_form: upper soda springs
instance_of: Landform
countries: United States
coordinates: lat: 41.2219
lon: -122.277
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
The Pacific Crest National Scenic Trail stretches from Mexico to Canada, following the highest portion of the Sierra Nevada, Klamath Mountains, and Cascade Range and paralleling the Pacific Ocean by. The Little Castle Lake Trail continues on to Mt. Bradley, a locally prominent mountain with views of Mount Shasta, overlooking Dunsmuir, California and the canyon of the Upper Sacramento River.

Geographic entities mentioned:
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: mt. bradley
instance_of: Mountain
countries: United States
coordinates: lat: 62.92472222222222
lon: -150.7263888888889
surface_form: mt. bradley
instance_of: Mountain
countries: United States
coordinates: lat: 48.1687464
lon: -113.4593874
surface_form: mt. bradley
instance_of: Mountain
countries: United States
coordinates: lat: 41.22184755
lon: -122.3089186
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: mount shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: mt. bradley
instance_of: Mountain
countries: United States
coordinates: lat: 58.2478
lon: -134.4142
History. Castle Lake was within the range of the Okwanuchu tribe, one of a number of small Shastan-speaking tribes of Native Americans who were closely related to the adjacent larger Shasta tribe. The Okwanuchu occupied territory near Mount Shasta, including the nearby present-day cities of Mount Shasta and Dunsmuir, California, and the upper Sacramento River canyon (among other areas).

Geographic entities mentioned:
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: mount shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
Along the way, the trail joins with a network of connections leading into Castle Crags State Park. Formation. The lake's origins date to the Pleistocene Era (more than 10,000 years ago) when a glacier carved a basin in the location of the current lake. During that era, much of North America was glaciated.

Geographic entities mentioned:
surface_form: current lake
instance_of: Lake
countries: United States
coordinates: lat: 44.164444444444
lon: -95.946388888889
The first non-Native Americans to pass through the area of Castle Lake were hunters and trappers of the Hudson's Bay Company, who began to come down the Siskiyou Trail from present-day Washington into Mexican-controlled California, in the late 1820s and early 1830s, in search of beaver and other pelt-bearing animals.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Nearly all of the lake's are within the Shasta-Trinity National Forest. Trails lead from Castle Lake into the adjacent Castle Crags Wilderness area, and on to Castle Crags State Park, including trails to Little Castle Lake and Heart Lake. Fishing, camping, and hiking are also available at or near the lake. Natural history.

Geographic entities mentioned:
surface_form: heart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.259
lon: -95.3051
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 41.227039
lon: -122.383789
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 41.227039
lon: -122.383789
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5683
lon: -115.398
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5683
lon: -115.398
surface_form: heart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.577
lon: -121.318
surface_form: heart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.137777777778
lon: -112.65111111111
surface_form: heart lake
instance_of: Lake
countries: United States
coordinates: lat: 44.2678
lon: -110.489
surface_form: heart lake
instance_of: Lake
countries: United States
coordinates: lat: 44.892403
lon: -84.692776
Castle Lake (California). Castle Lake is a glacial lake (&quot;cirque&quot; lake or tarn) located in the Trinity Mountains, in Siskiyou County of northern California. It is west of Mount Shasta City and Mount Shasta peak. The outlet of the lake drains into Castle Lake Creek, and then into Lake Siskiyou reservoir, part of the headwaters of the Sacramento River.

Geographic entities mentioned:
surface_form: castle lake (california)
instance_of: Lake
countries: United States
coordinates: lat: 41.227039
lon: -122.383789
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5683
lon: -115.398
Castle Lake (California). Castle Lake is a glacial lake (&quot;cirque&quot; lake or tarn) located in the Trinity Mountains, in Siskiyou County of northern California. It is west of Mount Shasta City and Mount Shasta peak. The outlet of the lake drains into Castle Lake Creek, and then into Lake Siskiyou reservoir, part of the headwaters of the Sacramento River.

Geographic entities mentioned:
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 41.227039
lon: -122.383789
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5683
lon: -115.398
It is west of Mount Shasta City and Mount Shasta peak. The outlet of the lake drains into Castle Lake Creek, and then into Lake Siskiyou reservoir, part of the headwaters of the Sacramento River. Nearly all of the lake's are within the Shasta-Trinity National Forest.

Geographic entities mentioned:
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 41.227039
lon: -122.383789
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5683
lon: -115.398
Natural history. Castle Lake and the surrounding area contain a wide variety of animals and plants including trout, bears, deer, otters, frogs, and osprey. The area is also well-known for early summer displays of flowers, including red Columbine (&quot;Aquilegia truncata&quot;), fawn lily (&quot;Erythronium sp.&quot;), and Shasta pentstemon (&quot;Pentstemon laetus&quot;).

Geographic entities mentioned:
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
A short hiking trail leads to nearby Faery Falls, where Ney Springs Creek falls nearly down a granite cliff face, forming a clear pool at the bottom. About one-quarter mile (400 m) north of Castle Lake is a campground with 6 first-come, first-served campsites. At the lake itself, fishing and picnicking, as well as viewing the local plant life, wildlife and scenery, are common activities.

Geographic entities mentioned:
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 41.227039
lon: -122.383789
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5683
lon: -115.398
Along the way, hikers will pass the Castle Lake Limnological Research Station. Following the eastern shore, the Little Castle Lake Trail leaves the parking area, and then climbs the adjoining ridge; about along this trail is Little Castle Lake, a small glacial tarn reached by passing through meadows of wild flowers in the early summer. Little Castle Lake is within the Castle Crags Wilderness Area.

Geographic entities mentioned:
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 41.227039
lon: -122.383789
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 41.227039
lon: -122.383789
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 41.227039
lon: -122.383789
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5683
lon: -115.398
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5683
lon: -115.398
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5683
lon: -115.398
Little Castle Lake is within the Castle Crags Wilderness Area. Heart Lake, another small tarn, located above the headwall of Castle Lake, may also be reached via an informal cut-off from the Little Castle Lake Trail. At this point, the well-known Pacific Crest National Scenic Trail is one-half mile (1 km) away, just over the Trinity Divide.

Geographic entities mentioned:
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 41.227039
lon: -122.383789
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 41.227039
lon: -122.383789
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5683
lon: -115.398
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5683
lon: -115.398
The bowl shape extended to its northeast edge, where there was a terminal moraine of smaller rocks and debris which had been deposited by the glacier. When the bowl-shaped crater filled with water, this terminal moraine acted as a natural dam, helping to contain the water in the newly formed cirque lake. History.

Geographic entities mentioned:
surface_form: cirque lake
instance_of: Lake
countries: United States
coordinates: lat: 43.8297
lon: -110.836
However, members of a tribe of the Penutian-speaking family of languages, the Wintu, who arrived in central Northern California about 1200 years ago, were out-competing their Hokan-language family neighbors, and were expanding Wintu territory. It is unclear at the time of first contact with non-Native Americans in the 1820s which tribe was living nearest to Castle Lake.

Geographic entities mentioned:
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 41.227039
lon: -122.383789
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5683
lon: -115.398
It is unclear at the time of first contact with non-Native Americans in the 1820s which tribe was living nearest to Castle Lake. Little or no information is available about Native American use or beliefs regarding Castle Lake; for example, Castle Lake is not mentioned in a published collection of Wintu tales and legends.

Geographic entities mentioned:
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 41.227039
lon: -122.383789
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 41.227039
lon: -122.383789
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 41.227039
lon: -122.383789
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5683
lon: -115.398
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5683
lon: -115.398
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5683
lon: -115.398
At about this same time, Ewing Young led the first group of Americans up the Siskiyou Trail, passing near Castle Lake. In 1841, an overland party of the United States Exploring Expedition, the first cartographers and scientists came through the area.

Geographic entities mentioned:
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 41.227039
lon: -122.383789
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5683
lon: -115.398
In 1841, an overland party of the United States Exploring Expedition, the first cartographers and scientists came through the area. Following the annexation of California by the United States in 1848 as a result of the Mexican–American War, Castle Lake came under the control of the U.S. Federal Government as public land.

Geographic entities mentioned:
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 41.227039
lon: -122.383789
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 41.227039
lon: -122.383789
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5683
lon: -115.398
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5683
lon: -115.398
This battle was reportedly the last battle between Native Americans and settlers in which the Native Americans fought exclusively with bow and arrow. With the development, first, of the U.S. &quot;Forest Reserve&quot; system in the late 19th century, and then the organization of the U.S. National Forests in the early 20th century, Castle Lake came under the stewardship of the U.S. Forest Service.

Geographic entities mentioned:
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 41.227039
lon: -122.383789
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 41.227039
lon: -122.383789
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5683
lon: -115.398
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5683
lon: -115.398
Federal Government as public land. In 1855, an area near Castle Lake, now known as Battle Rock, was the site of a battle between Native Americans and California Gold Rush-era settlers. The poet Joaquin Miller wrote a first-hand account of this battle, &quot;The Battle of Castle Crags,&quot; in which Miller took part in the fight, and received an arrow wound through the cheek and jaw.

Geographic entities mentioned:
surface_form: battle
instance_of: Watercourse
countries: United States
coordinates: lat: 44.9266
lon: -93.0291
surface_form: battle
instance_of: Watercourse
countries: United States
coordinates: lat: 44.9266
lon: -93.0291
The outlet of the lake drains into Castle Lake Creek, and then into Lake Siskiyou reservoir, part of the headwaters of the Sacramento River. Nearly all of the lake's are within the Shasta-Trinity National Forest. Trails lead from Castle Lake into the adjacent Castle Crags Wilderness area, and on to Castle Crags State Park, including trails to Little Castle Lake and Heart Lake.

Geographic entities mentioned:
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
History. Castle Lake was within the range of the Okwanuchu tribe, one of a number of small Shastan-speaking tribes of Native Americans who were closely related to the adjacent larger Shasta tribe. The Okwanuchu occupied territory near Mount Shasta, including the nearby present-day cities of Mount Shasta and Dunsmuir, California, and the upper Sacramento River canyon (among other areas).

Geographic entities mentioned:
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
These can include wood rose (&quot;Rosa gymnocarpa&quot;), Shasta lupine (&quot;Lupinus albicaulis&quot;), scarlet columbine (&quot;Aquilegia formosa&quot;), tiger lily (&quot;Lilium pardalinum&quot;), fawn lily (&quot;Erythronium sp.&quot;), pine-drops (&quot;Pterospora andromedea&quot;), douglas spiraea (&quot;Spiraea douglasii&quot;), scarlet paintbrush (&quot;Castilleja pinetorum&quot;), alpine paintbrush (&quot;Castilleja arachnoidea&quot;), dwarf paintbrush (&quot;Castilleja miniata&quot;), alpine saxifrage (&quot;Saxifraga nidifica&quot;), Shasta penstemon (&quot;Penstemon laetus&quot;), alpine buckwheat (&quot;Eriogonum pyrolifolium&quot;), and Tofield's swamp lily (&quot;Tofieldia occidentalis&quot;).

Geographic entities mentioned:
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
Gilgit was once a major centre for Buddhism; it was an important stop on the ancient Silk Road, and today serves as a major junction along the Karakoram Highway with road connections to China as well as the Pakistani cities of Skardu, Chitral, Peshawar, and Islamabad. The city's economic activity is mainly focused on agriculture, with wheat, maize, and barley as the main crops. Etymology.

Geographic entities mentioned:
surface_form: Chitral
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.85111111111111
lon: 71.78888888888889
Gilgit was ruled for centuries by the local Trakhàn Dynasty, which ended about 1810 with the death of Raja Abas, the last Trakhàn Raja. The rulers of Hunza and Nager also claim origin with the Trakhàn dynasty. They claim descent from a heroic Kayani Prince of Persia, &quot;Azur Jamshid&quot; (also known as &quot;Shamsher&quot;), who secretly married the daughter of the king &quot;Shri Badat&quot;.

Geographic entities mentioned:
surface_form: Hunza
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.31666667
lon: 74.65
surface_form: Nager
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.4
lon: 73.8
1800s. The area had been a flourishing tract but prosperity was destroyed by warfare over the next fifty years, and by the great flood of 1841 in which the river Indus was blocked by a landslip below the Hatu Pir and the valley was turned into a lake. After the death of Abas, Sulaiman Shah, Raja of Yasin, conquered Gilgit.

Geographic entities mentioned:
surface_form: Yasin
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.367777777777775
lon: 73.33777777777777
After the death of Abas, Sulaiman Shah, Raja of Yasin, conquered Gilgit. Then, Azad Khan, Raja of Punial, killed Sulaiman Shah, taking Gilgit; then Tahir Shah, Raja of Buroshall (Nagar), took Gilgit and killed Azad Khan. Tair Shah's son Shah Sakandar inherited, only to be killed by Gohar Aman, ethnic Kho Raja of Yasin of the Khushwakhte Dynasty when he took Gilgit.

Geographic entities mentioned:
surface_form: Punial
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.0852
lon: 74.041
surface_form: Nagar
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.4
lon: 73.8
Gilgit is connected to Karimabad (Hunza) and Sust in the north, with further connections to the Chinese cities of Tashkurgan, Upal and Kashgar in Xinjiang. Gilgit is also linked to Chitral in the west, and Skardu to the east. The road to Skardu will be upgraded to a 4-lane road at a cost of $475 million.

Geographic entities mentioned:
surface_form: Chitral
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.85111111111111
lon: 71.78888888888889
The road to Skardu will be upgraded to a 4-lane road at a cost of $475 million. Transport companies such as the Silk Route Transport Pvt, Masherbrum Transport Pvt and Northern Areas Transport Corporation (), offer passenger road transport between Islamabad, Gilgit, Sust, and Kashgar and Tashkurgan in China. The Astore-Burzil Pass Road, linking Gilgit to Srinagar was closed in 1978. Rail.

Geographic entities mentioned:
surface_form: Masherbrum
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.6425
lon: 76.310833333333
Walnut Hill Lane runs directly through the neighborhood. About. Alexander's Village is about 4 miles (6.43 km) from White Rock Lake, which is accessible via Fair Oaks Park bike trail along White Rock Creek that directly connects the neighborhood, the lake, and other park facilities along White Rock Creek. Education.

Geographic entities mentioned:
surface_form: White Rock Lake
instance_of: Lake
countries: United States
coordinates: lat: 32.834166666667
lon: -96.722777777778
Bois Noirs (Livradois). The Bois Noirs (,) Forest is the highest point of the Livradois mountains, at an altitude of 1,215 meters. The absolute summit of the massif is also called Signal de Mons. Located in the Livradois-Forez Regional Natural Park and in the Puy-de-Dôme department, its summit, in the heart of a coniferous forest, does not allow for a panoramic view of the regional natural park.

Geographic entities mentioned:
surface_form: bois noirs
instance_of: Mountain
countries: France
coordinates: lat: 45.531667
lon: 3.635833