Sarmila/GeoWiki-Features huggingface dataset:
Astino Valley. The Astino Valley () is a valley in the Italian comune of Bergamo in Lombardy. It is relatively small in size and it is part of the Parco dei Colli di Bergamo system, west of Bergamo.

Geographic entities mentioned:
surface_form: astino valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.706
lon: 9.638
This strong performance came despite strong backing for his top opponent by the Civic Safety Commission. In March 1929, Meyering gave his support to the proposal of constructing a harbor at Lake Calumet. Meyering resigned from the City Council in late 1930 in order to assume the office of Cook County sheriff.

Geographic entities mentioned:
surface_form: Lake Calumet
instance_of: Lake
countries: United States
coordinates: lat: 41.68
lon: -87.59
Berneuse. The Berneuse (or &quot;la Berneuse&quot;) is a mountain of the western Bernese Alps, above Leysin in the canton of Vaud. It lies on the range east of the Rhone valley, culminating at the Tour d'Aï. Its summit (2,045 m) is a popular destination, hosting the &quot;Kuklos&quot;, a revolving restaurant accessible by cable cabin from town.

Geographic entities mentioned:
surface_form: Tour d'Aï
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.372111111111
lon: 7.002
surface_form: tour d'aï
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.372111111111
lon: 7.002
The Berneuse (or &quot;la Berneuse&quot;) is a mountain of the western Bernese Alps, above Leysin in the canton of Vaud. It lies on the range east of the Rhone valley, culminating at the Tour d'Aï. Its summit (2,045 m) is a popular destination, hosting the &quot;Kuklos&quot;, a revolving restaurant accessible by cable cabin from town. On a clear day, Lake Geneva is visible from this summit.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Berneuse. The Berneuse (or &quot;la Berneuse&quot;) is a mountain of the western Bernese Alps, above Leysin in the canton of Vaud. It lies on the range east of the Rhone valley, culminating at the Tour d'Aï. Its summit (2,045 m) is a popular destination, hosting the &quot;Kuklos&quot;, a revolving restaurant accessible by cable cabin from town.

Geographic entities mentioned:
surface_form: berneuse
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.359583333333
lon: 7.0021666666667
Berneuse. The Berneuse (or &quot;la Berneuse&quot;) is a mountain of the western Bernese Alps, above Leysin in the canton of Vaud. It lies on the range east of the Rhone valley, culminating at the Tour d'Aï. Its summit (2,045 m) is a popular destination, hosting the &quot;Kuklos&quot;, a revolving restaurant accessible by cable cabin from town.

Geographic entities mentioned:
surface_form: berneuse
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.359583333333
lon: 7.0021666666667
surface_form: berneuse
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.359583333333
lon: 7.0021666666667
State highway M-46 crosses the township, leading west to Muskegon, the county seat, and east to Kent City. According to the U.S. Census Bureau, the township has a total area of, of which are land and, or 2.21%, are water. Most of the township is drained by tributaries of Black Creek, which flows southwest to Mona Lake, an arm of Lake Michigan, in Norton Shores.

Geographic entities mentioned:
surface_form: Mona Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.16666667
lon: -86.25
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
The depth of the three ponds is an average of one meter. Crocodiles were introduced into one of the ponds that represent Lake Turkana (of northern Kenya) in the village theme. The other pond represents in the village theme, Lake Victoria, which is in western Kenya. Tilapia were introduced into this lake. Large flocks of birds nest on and feed on these wetlands.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Enonvesi. Enonvesi is a rather large lake in the Vuoksi main catchment area. It is located in the regions of Southern Savonia and Northern Savonia in Finland. It is a part of the Saimaa lake system.

Geographic entities mentioned:
surface_form: Saimaa
instance_of: Lake
countries: Finland
coordinates: lat: 61.25
lon: 28.25
Enonvesi. Enonvesi is a rather large lake in the Vuoksi main catchment area. It is located in the regions of Southern Savonia and Northern Savonia in Finland. It is a part of the Saimaa lake system.

Geographic entities mentioned:
surface_form: enonvesi
instance_of: Lake
countries: Finland
coordinates: lat: 62.061
lon: 29.003
surface_form: enonvesi
instance_of: Lake
countries: Finland
coordinates: lat: 62.116666666667
lon: 28.9
It aided the Allied offensive in Italy during May 1944, receiving a Distinguished Unit Citation for action from 12 to 14 May when the squadron bombed an enemy position on Monastery Hill 9 (Monte Cassino), attacked troops massing on the hill for counterattack, and hit a nearby stronghold to force the surrender of an enemy garrison.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
A unique setup, detached from Luke Air Force Base, 56th Fighter Wing, it is the second Block 42 F-16C formal training unit in the 54th Fighter Group at Holloman Air Force Base officially in 2015. On 25 November 2015, a 314th Fighter Squadron F-16 crashed near Salinas Peak near Truth or Consequences, New Mexico. The pilot was in good condition when he was found.

Geographic entities mentioned:
surface_form: Salinas Peak
instance_of: Mountain
countries: United States
coordinates: lat: 33.298055555556
lon: -106.53194444444
Joaquín Gomis Cornet. Joaquín Gomis Cornet (1869–1957) was a Spanish Catalan entrepreneur and politician. In business he is known mostly as co-owner and manager of numerous mid-size companies from the Catalan hydroelectricity sector, which controlled large part of the power grid based on the Llobregat and the Segre basins.

Geographic entities mentioned:
surface_form: Llobregat
instance_of: Watercourse
countries: Spain
coordinates: lat: 42.282412
lon: 2.012826
Productora y Distribuidora de Electricidad was intended more as a power distribution entity. The expansion anticipated consisted of launch of the Castillonroy dam on the Noguera Ribargorzana, part of the Segre system. After it went into operation, in the late 1940s the overall capacity of the Segre grid was 5-8m kWh per year.

Geographic entities mentioned:
surface_form: Noguera Ribargorzana
instance_of: Watercourse
countries: Spain
coordinates: lat: 42.6267
lon: 0.7058
Modřice. Modřice (;) is a town in Brno-Country District in the South Moravian Region of the Czech Republic. It has about 5,800 inhabitants. Geography. Modřice is located about south of Brno. It lies in the Dyje–Svratka Valley. It is situated on the right bank of the Svratka River. History. The first written mention of Modřice is from 1141. There used to be a castle owned by the Olomouc bishops.

Geographic entities mentioned:
surface_form: Dyje–Svratka Valley
instance_of: Valley
countries: Czech Republic
coordinates: lat: 49
lon: 16.5
Upper Two Medicine Lake is located in Glacier National Park, in the U. S. state of Montana. The lake is just east of the Continental Divide in the Two Medicine region of Glacier National Park. Upper Two Medicine Lake is in a cirque and surrounded by a number of peaks including Lone Walker Mountain, Mount Helen and Pumpelly Pillar. Upper Two Medicine Lake is a hike from the Two Medicine Store.

Geographic entities mentioned:
surface_form: Lone Walker Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.4533
lon: -113.479
surface_form: Pumpelly Pillar
instance_of: Mountain
countries: United States
coordinates: lat: 48.47472222
lon: -113.45055556
surface_form: mount helen
instance_of: Mountain
countries: United States
coordinates: lat: 43.1511
lon: -109.631
surface_form: mount helen
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: medicine lake
instance_of: Lake
countries: United States
coordinates: lat: 45.00644
lon: -93.41997
surface_form: mount helen
instance_of: Mountain
countries: United States
coordinates: lat: 48.4747
lon: -113.467
surface_form: two medicine lake
instance_of: Lake
countries: United States
coordinates: lat: 48.4769
lon: -113.387
surface_form: medicine lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9841655
lon: -97.3519987
surface_form: upper two medicine lake
instance_of: Lake
countries: United States
coordinates: lat: 48.4639
lon: -113.462
Upper Two Medicine Lake. Upper Two Medicine Lake is located in Glacier National Park, in the U. S. state of Montana. The lake is just east of the Continental Divide in the Two Medicine region of Glacier National Park. Upper Two Medicine Lake is in a cirque and surrounded by a number of peaks including Lone Walker Mountain, Mount Helen and Pumpelly Pillar.

Geographic entities mentioned:
surface_form: medicine lake
instance_of: Lake
countries: United States
coordinates: lat: 45.00644
lon: -93.41997
surface_form: two medicine lake
instance_of: Lake
countries: United States
coordinates: lat: 48.4769
lon: -113.387
surface_form: medicine lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9841655
lon: -97.3519987
surface_form: upper two medicine lake
instance_of: Lake
countries: United States
coordinates: lat: 48.4639
lon: -113.462
Upper Two Medicine Lake is located in Glacier National Park, in the U. S. state of Montana. The lake is just east of the Continental Divide in the Two Medicine region of Glacier National Park. Upper Two Medicine Lake is in a cirque and surrounded by a number of peaks including Lone Walker Mountain, Mount Helen and Pumpelly Pillar. Upper Two Medicine Lake is a hike from the Two Medicine Store.

Geographic entities mentioned:
surface_form: medicine lake
instance_of: Lake
countries: United States
coordinates: lat: 45.00644
lon: -93.41997
surface_form: two medicine lake
instance_of: Lake
countries: United States
coordinates: lat: 48.4769
lon: -113.387
surface_form: medicine lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9841655
lon: -97.3519987
surface_form: upper two medicine lake
instance_of: Lake
countries: United States
coordinates: lat: 48.4639
lon: -113.462
Chullunkhäni (Chuquisaca). Chullunkhäni (Aymara &quot;chullunkhä&quot; ('ä' stands for a long 'a') icicle, &quot;-ni&quot; a suffix, &quot;the one with icicles&quot;, also spelled &quot;Chulluncani&quot;) is a mountain in the Bolivian Andes. It is located in the Chuquisaca Department, Azurduy Province, Tarvita Municipality, and in the Jaime Zudáñez Province, Icla Municipality.

Geographic entities mentioned:
surface_form: chullunkhäni
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.18
lon: -67.83138889
surface_form: chullunkhäni
instance_of: Mountain
countries: Bolivia
coordinates: lat: -21.5631
lon: -67.8556
surface_form: chullunkhäni
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.618
lon: -64.6892
Chullunkhäni (Chuquisaca). Chullunkhäni (Aymara &quot;chullunkhä&quot; ('ä' stands for a long 'a') icicle, &quot;-ni&quot; a suffix, &quot;the one with icicles&quot;, also spelled &quot;Chulluncani&quot;) is a mountain in the Bolivian Andes. It is located in the Chuquisaca Department, Azurduy Province, Tarvita Municipality, and in the Jaime Zudáñez Province, Icla Municipality.

Geographic entities mentioned:
surface_form: chullunkhäni
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.18
lon: -67.83138889
surface_form: chulluncani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -21.5631
lon: -67.8556
surface_form: chullunkhäni
instance_of: Mountain
countries: Bolivia
coordinates: lat: -21.5631
lon: -67.8556
surface_form: chullunkhäni
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.618
lon: -64.6892
Thakkarbapa visited forests in Assam, rural Bengal, drought affected areas of Orissa, Bhil belts in Gujarat and Harijan areas of Saurashtra, Mahar areas of Maharashtra, untouchables in Madras, hilly areas of Chhota Nagpur, desert of Tharparkar, foothills of Himalaya, coastal areas of Travancore to undertake his mission of empowering Harijans.

Geographic entities mentioned:
surface_form: Chhota Nagpur
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
Castle Rock (Chelan County). Castle Rock is an mountain summit located on the shared border of Glacier Peak Wilderness and Lake Chelan National Recreation Area in the North Cascades of Washington state. The mountain is situated above the western shore of Lake Chelan in Chelan County, on land managed by Wenatchee National Forest. The nearest higher peak is Flora Mountain, to the south.

Geographic entities mentioned:
surface_form: Lake Chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
surface_form: chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
surface_form: chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
The mountain is situated above the western shore of Lake Chelan in Chelan County, on land managed by Wenatchee National Forest. The nearest higher peak is Flora Mountain, to the south. Precipitation runoff from the peak drains into Lake Chelan via Castle Creek, Canyon Creek, and Bridal Veil Creek. Topographic relief is significant as the summit rises above the lake in 2.5 mile (4 km). Climate.

Geographic entities mentioned:
surface_form: Flora Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.2431
lon: -120.696
Castle Rock (Chelan County). Castle Rock is an mountain summit located on the shared border of Glacier Peak Wilderness and Lake Chelan National Recreation Area in the North Cascades of Washington state. The mountain is situated above the western shore of Lake Chelan in Chelan County, on land managed by Wenatchee National Forest. The nearest higher peak is Flora Mountain, to the south.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.14972222
lon: -109.84944444
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.155013
lon: -117.293429
surface_form: castle rock
instance_of: Mountain
countries: United States
coordinates: lat: 63.3664
lon: -150.274
surface_form: lake chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
surface_form: chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
surface_form: castle rock
instance_of: Mountain
countries: United States
coordinates: lat: 48.25764
lon: -120.69204
surface_form: castle rock
instance_of: Landform
countries: United States
coordinates: lat: 38.8611
lon: -100.17
surface_form: castle rock
instance_of: Mountain
countries: United States
coordinates: lat: 45.9106
lon: -84.7416
With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted. Glacier Peak, a stratovolcano that is southwest of Tupshin Peak, began forming in the mid-Pleistocene. In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago.

Geographic entities mentioned:
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.14972222
lon: -109.84944444
surface_form: tupshin peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.29708
lon: -120.75038
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.155013
lon: -117.293429
Castle Rock (Chelan County). Castle Rock is an mountain summit located on the shared border of Glacier Peak Wilderness and Lake Chelan National Recreation Area in the North Cascades of Washington state. The mountain is situated above the western shore of Lake Chelan in Chelan County, on land managed by Wenatchee National Forest. The nearest higher peak is Flora Mountain, to the south.

Geographic entities mentioned:
surface_form: castle rock
instance_of: Mountain
countries: United States
coordinates: lat: 63.3664
lon: -150.274
surface_form: chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
surface_form: castle rock
instance_of: Mountain
countries: United States
coordinates: lat: 48.25764
lon: -120.69204
surface_form: castle rock
instance_of: Landform
countries: United States
coordinates: lat: 38.8611
lon: -100.17
surface_form: castle rock
instance_of: Mountain
countries: United States
coordinates: lat: 45.9106
lon: -84.7416
The mountain is situated above the western shore of Lake Chelan in Chelan County, on land managed by Wenatchee National Forest. The nearest higher peak is Flora Mountain, to the south. Precipitation runoff from the peak drains into Lake Chelan via Castle Creek, Canyon Creek, and Bridal Veil Creek. Topographic relief is significant as the summit rises above the lake in 2.5 mile (4 km). Climate.

Geographic entities mentioned:
surface_form: lake chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
surface_form: chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
The belt has a lower metamorphic grade than the Omineca Belt and ranges from 400 million to 10,000 years old. Volcanic activity has been recorded as occurring in the past 10,000 years, including at Nazko Cone and in the Satah Mountain volcanic field. The Coast Belt is the single largest outpouring of granite and granodiorite in the Phanerozoic.

Geographic entities mentioned:
surface_form: Nazko Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 52.9272
lon: -123.734
It contains heavily metamorphosed fragments of both the terranes of the Insular Belt and the Intermontane Belt. In the southeast, there is a series of small terranes of both oceanic (Bridge River Vent and Chilliwack Batholith) and continental affinity (Jack Konat Mountain, Ladner). The hard-weathering granite is extensively rugged throughout the belt.

Geographic entities mentioned:
surface_form: Bridge River Vent
instance_of: Mountain
countries: Canada
coordinates: lat: 50.6563
lon: -123.502
Bahrey was also the author of Emperor Sarsa Dengel's chronicle, &quot;The History of King Sarsa Dengel.&quot;
Life. Bahrey was born and lived in the southernly region of Gamo near the shores of Lake Abaya until he was victimized by an earlier Oromo raid, as he later wrote that they &quot;devastated his country&quot; and &quot;looted all that he possessed&quot;.

Geographic entities mentioned:
surface_form: Lake Abaya
instance_of: Lake
countries: Ethiopia
coordinates: lat: 6.236
lon: 37.832
Had it not been for Daniel Burnham, head of the company's Board of Architects, the fair might never have been built. Burnham, whose favorite saying was, &quot;Make no little plans; they have no magic to stir men's blood&quot;, became the czar of the exposition's construction. An undeveloped site of on the shores of Lake Michigan was selected for the fairgrounds.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
A long period of rebuilding followed, ending with Jerusalem's second total destruction at the hands of the Romans in 70 CE. Josephus, the first-century CE historian who knew the city as it was before this second catastrophic event, identified Mount Zion as being the Western Hill, separated from the lower, Eastern Hill, by what he calls the &quot;Tyropoeon Valley&quot;.

Geographic entities mentioned:
surface_form: Tyropoeon Valley
instance_of: Valley
countries: State of Palestine
Israel
coordinates: lat: 31.776947222222
lon: 35.234238888889
The Needles (Arizona). The Needles are a distinctive group of rock pinnacles, mountain peaks adjacent to the Topock Gorge, and the Colorado River on the northwestern extreme of the Mojave Mountains within the Havasu National Wildlife Refuge in Mohave County, Arizona, United States. They range from 1207 to over 1600 feet in altitude.

Geographic entities mentioned:
surface_form: Topock Gorge
instance_of: Lake
countries: United States
coordinates: lat: 34.665263888889
lon: -114.448525
The southern part of the island has a desert climate, while the northeast and the higher elevations are semi-arid. Mountains. The tallest mountain is Tope de Coroa, reaching an elevation of 1,979 m. Other high mountains on the island are Monte Tomé (1,863 m), Gudo de Cavaleiro (1,810 m), Monte Moroços (1,767 m) and Pico da Cruz (1,584 m). Climate.

Geographic entities mentioned:
surface_form: Tope de Coroa
instance_of: Mountain
countries: Cape Verde
coordinates: lat: 17.033333333333
lon: -25.295833333333
The southern part of the island has a desert climate, while the northeast and the higher elevations are semi-arid. Mountains. The tallest mountain is Tope de Coroa, reaching an elevation of 1,979 m. Other high mountains on the island are Monte Tomé (1,863 m), Gudo de Cavaleiro (1,810 m), Monte Moroços (1,767 m) and Pico da Cruz (1,584 m). Climate.

Geographic entities mentioned:
surface_form: Gudo de Cavaleiro
instance_of: Mountain
countries: Cape Verde
coordinates: lat: 17.13333333
lon: -25.28333333
surface_form: Pico da Cruz
instance_of: Mountain
countries: Cape Verde
coordinates: lat: 17.1
lon: -25.029166666667
Fort du Portage / Fort Little Niagara. Fort Little Niagara, built above the Falls of Niagara by French traders and military men, was built as a satellite of Fort Niagara. Fort Niagara protected the mouth of the Niagara River at Lake Ontario and the Lower Landing. Fort Little Niagara anchored the Upper Landing (above the Falls). At the time, the Niagara Frontier was claimed part of New France.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Portage Master Johnathan Stedman succeeded Schlosser, and lived in a house which utilized the Chimney from 1763 until the end of the British era. The British made improvements to the Portage, including the construction of an incline tramway at the Niagara Escarpment and ox-pulled carts to relay cargo.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
Naltar Lakes. There are four major alpine lakes in Naltar Valley of Gilgit-Baltistan, Pakistan. They are known as Naltar Lakes () or &quot;Bashkiri&quot; Lakes at altitudes ranging from. The best time to visit the lakes is from May to October. During the winter, it becomes almost impossible to reach the lake by vehicle due to the heavy snowfall in Naltar Valley. Bashkiri Lake I or Satrangi Lake.

Geographic entities mentioned:
surface_form: Naltar Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.16531026078764
lon: 74.17856522268198
It drains an area of the southern Sierra Nevada mountains northeast of Bakersfield. Fed by snowmelt near Mount Whitney, the river passes through scenic canyons in the mountains and is a popular destination for whitewater rafting and kayaking. It is the southernmost major river system in the Sierra Nevada, and is the only major river in the Sierra that drains in a southerly direction.

Geographic entities mentioned:
surface_form: Mount Whitney
instance_of: Mountain
countries: United States
coordinates: lat: 36.57861111111111
lon: -118.29194444444444
It is the southernmost major river system in the Sierra Nevada, and is the only major river in the Sierra that drains in a southerly direction. The Kern River formerly emptied into the now dry Buena Vista Lake and Kern Lake via the Kern River Slough, and Kern Lake in turn emptied into Buena Vista Lake via the Connecting Slough at the southern end of the Central Valley.

Geographic entities mentioned:
surface_form: Buena Vista Lake
instance_of: Lake
countries: United States
coordinates: lat: 35.1919
lon: -119.295
Its swift flow at low elevation makes the river below the reservoir a popular location for rafting. Course. The Kern begins in the Sierra Nevada in Sequoia National Park in northeastern Tulare County, near the border with Inyo County. The main branch of the river (sometimes called the North Fork Kern River) rises from several small lakes in a basin northwest of Mount Whitney.

Geographic entities mentioned:
surface_form: Mount Whitney
instance_of: Mountain
countries: United States
coordinates: lat: 36.57861111111111
lon: -118.29194444444444
The river channel continues about southwest to a point near the California Aqueduct on the western side of the San Joaquin Valley. A weir allows excess floodwaters from the Kern to drain into the California Aqueduct, while any remaining water continues south into the seasonal Buena Vista Lake, which once reached sizes of about in wet periods.

Geographic entities mentioned:
surface_form: Buena Vista Lake
instance_of: Lake
countries: United States
coordinates: lat: 35.1919
lon: -119.295
The Battle of Fort Frontenac took place on August 26–28, 1758 during the Seven Years' War (referred to as the French and Indian War in the United States) between France and Great Britain. The location of the battle was Fort Frontenac, a French fort and trading post which is located at the site of present-day Kingston, Ontario, at the eastern end of Lake Ontario where it drains into the St.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Following that failure, many of Abercrombie's underlings sought to distance themselves from any responsibility for the disaster. Lieutenant Colonel John Bradstreet renewed an earlier proposal to capture Fort Frontenac, a French fort and trading post on the northern shore of Lake Ontario near where it empties into the St. Lawrence River.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
According to Pénicaut,
From there [Manchacq] we went five leagues higher and found very high banks called &quot;écorts&quot; in that region, and in savage called &quot;Istrouma&quot; which means red stick [&quot;bâton rouge&quot;], as at this place there is a post painted red that the savages have sunk there to mark the land line between the two nations, namely: the land of the Bayagoulas which they were leaving and the land of another nation&mdash;thirty leagues upstream from the &quot;baton rouge&quot;&mdash;named the Oumas.

Geographic entities mentioned:
surface_form: Manchacq
instance_of: Landform
countries: United States
coordinates: lat: 30.3456
lon: -90.8919
Spanish officials renamed the site Fort San Carlos and took control of Baton Rouge. At the conclusion of the Revolutionary War, Great Britain turned West Florida over to Spain. 1779&ndash;1810: Spanish period. A colony of Pennsylvania German farmers migrated north from Bayou Manchac, after a series of floods in the 1780s, and settled to the south of Baton Rouge.

Geographic entities mentioned:
surface_form: Bayou Manchac
instance_of: Landform
countries: United States
coordinates: lat: 30.3456
lon: -90.8919
It stands above Kirkstone Pass on the road from Ullswater to Ambleside. Topography. High Hartsop Dodd is properly the north eastern ridge of Little Hart Crag, but was given the status of a separate fell by Alfred Wainwright in his &quot;Pictorial Guide to the Lakeland Fells&quot; and that convention is followed here.

Geographic entities mentioned:
surface_form: Little Hart Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.481630555556
lon: -2.9476194444444
surface_form: hartsop dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4981
lon: -2.9094
surface_form: high hartsop dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4889
lon: -2.93853
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493080555556
lon: -2.9772194444444
His decision was based on it having &quot;the appearance of an isolated mountain with a peaked summit and steep sides, a very shapely pyramid rising from the green fields.&quot;
There are three Dodds when viewed from Hartsop, the others being (Low) Hartsop Dodd and Middle Dodd. The names refer to their position in the valley rather than their height.

Geographic entities mentioned:
surface_form: (Low) Hartsop Dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4981
lon: -2.9094
surface_form: Middle Dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4781
lon: -2.93211
surface_form: hartsop dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4981
lon: -2.9094
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: middle dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4781
lon: -2.93211
The fell is bounded on either side by valleys of the Ullswater catchment. To the east is the narrow defile of Caiston Glen, falling from the summit of Scandale Pass. This separates the fell from Middle Dodd and its parent Red Screes. On the west is Hogget Gill, a sidestream of picturesque Dovedale. Across here is Stangs, a subsidiary top of Dove Crag.

Geographic entities mentioned:
surface_form: Red Screes
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.470061111111
lon: -2.9334694444444
surface_form: red screes
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.470061111111
lon: -2.9334694444444
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: middle dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4781
lon: -2.93211
To the east is the narrow defile of Caiston Glen, falling from the summit of Scandale Pass. This separates the fell from Middle Dodd and its parent Red Screes. On the west is Hogget Gill, a sidestream of picturesque Dovedale. Across here is Stangs, a subsidiary top of Dove Crag. Dovedale and Caiston Glen are both tributaries of Kirkstone Beck, the main feeder of Brothers Water. Geology.

Geographic entities mentioned:
surface_form: Dove Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.485061111111
lon: -2.9677694444444
surface_form: dove crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.485061111111
lon: -2.9677694444444
On the west is Hogget Gill, a sidestream of picturesque Dovedale. Across here is Stangs, a subsidiary top of Dove Crag. Dovedale and Caiston Glen are both tributaries of Kirkstone Beck, the main feeder of Brothers Water. Geology. Middle Dodd dacite forms the crest of the ridge with the volcaniclastic sandstone of the Esk Pike Formation beneath.

Geographic entities mentioned:
surface_form: Brothers Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.505555555556
lon: -2.925
surface_form: brothers water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.505555555556
lon: -2.925
Summit. The summit of High Hartsop Dodd bears a small cairn at the point where the ridge briefly levels out. The view is not extensive given the high ring of surrounding fells, but many of these are seen in close detail, particularly Dove Crag. Ascents. High Hartsop Dodd is rarely climbed for its own sake, being merely a stop on the road to Little Hart Crag and Dove Crag.

Geographic entities mentioned:
surface_form: dove crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.485061111111
lon: -2.9677694444444
The view is not extensive given the high ring of surrounding fells, but many of these are seen in close detail, particularly Dove Crag. Ascents. High Hartsop Dodd is rarely climbed for its own sake, being merely a stop on the road to Little Hart Crag and Dove Crag. From here either Caiston Glen or Dovedale can be circumnavigated along fine high level ridges.

Geographic entities mentioned:
surface_form: dove crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.485061111111
lon: -2.9677694444444
surface_form: little hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.481630555556
lon: -2.9476194444444
surface_form: hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493080555556
lon: -2.9772194444444
High Hartsop Dodd. High Hartsop Dodd is a fell in the English Lake District, an outlier of the Fairfield group in the Eastern Fells. It stands above Kirkstone Pass on the road from Ullswater to Ambleside. Topography.

Geographic entities mentioned:
surface_form: hartsop dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4981
lon: -2.9094
surface_form: high hartsop dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4889
lon: -2.93853
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
High Hartsop Dodd. High Hartsop Dodd is a fell in the English Lake District, an outlier of the Fairfield group in the Eastern Fells. It stands above Kirkstone Pass on the road from Ullswater to Ambleside. Topography.

Geographic entities mentioned:
surface_form: hartsop dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4981
lon: -2.9094
surface_form: fairfield
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4969
lon: -2.99059
surface_form: high hartsop dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4889
lon: -2.93853
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
This was an unsuccessful trial for lead and extends about 80 ft into the fellside. There is a further small working nearby. According to Wainwright High Hartsop Dodd was briefly in the news in 1948 owing to efforts to save two terriers trapped in a hole on the Caiston flank. Summit. The summit of High Hartsop Dodd bears a small cairn at the point where the ridge briefly levels out.

Geographic entities mentioned:
surface_form: hartsop dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4981
lon: -2.9094
surface_form: high hartsop dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4889
lon: -2.93853
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
All three present an imposing pyramidal profile when seen from below, totally obscuring their parent fells. Similarly, all three appear entirely derivative when viewed from other angles. From the rocky summit of Little Hart Crag a narrowing ridge descends north eastward on grass. The ground is quite wet and there are areas of peat and sedge.

Geographic entities mentioned:
surface_form: little hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.481630555556
lon: -2.9476194444444
surface_form: hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493080555556
lon: -2.9772194444444
Across here is Stangs, a subsidiary top of Dove Crag. Dovedale and Caiston Glen are both tributaries of Kirkstone Beck, the main feeder of Brothers Water. Geology. Middle Dodd dacite forms the crest of the ridge with the volcaniclastic sandstone of the Esk Pike Formation beneath. There is evidence of mining in Caiston Glen, with the mouth of a level opening about halfway up the beck.

Geographic entities mentioned:
surface_form: esk pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456219444444
lon: -3.17995
From the rocky summit of Little Hart Crag a narrowing ridge descends north eastward on grass. The ground is quite wet and there are areas of peat and sedge. After half a mile of steady fall, the ridge throws up the barely perceptible summit of High Harsop Dodd. Beyond this the character of the fell changes completely and a steep slope plunges straight down to the valley floor.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
According to Wainwright High Hartsop Dodd was briefly in the news in 1948 owing to efforts to save two terriers trapped in a hole on the Caiston flank. Summit. The summit of High Hartsop Dodd bears a small cairn at the point where the ridge briefly levels out. The view is not extensive given the high ring of surrounding fells, but many of these are seen in close detail, particularly Dove Crag.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
To the east is the narrow defile of Caiston Glen, falling from the summit of Scandale Pass. This separates the fell from Middle Dodd and its parent Red Screes. On the west is Hogget Gill, a sidestream of picturesque Dovedale. Across here is Stangs, a subsidiary top of Dove Crag. Dovedale and Caiston Glen are both tributaries of Kirkstone Beck, the main feeder of Brothers Water. Geology.

Geographic entities mentioned:
surface_form: dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
Ascents. High Hartsop Dodd is rarely climbed for its own sake, being merely a stop on the road to Little Hart Crag and Dove Crag. From here either Caiston Glen or Dovedale can be circumnavigated along fine high level ridges. The nose of the fell provides the only practicable route, starting from either Kirkstonefoot or Cow Bridge. This is grassy and rather steep.

Geographic entities mentioned:
surface_form: dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
Lake Augusta (Washington). Lake Augusta is a freshwater lake located on the southwest skirt of Big Jim Mountain, East of Icicle Ridge, in Chelan County, Washington. Because of its close proximity to Icicle Ridge Trail, the lake is a popular area for hiking, swimming, and fishing cutthroat trout.

Geographic entities mentioned:
surface_form: Big Jim Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.6629
lon: -120.8329
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
surface_form: lake augusta
instance_of: Lake
countries: United States
coordinates: lat: 47.653611111111
lon: -120.83527777778
Because of its close proximity to Icicle Ridge Trail, the lake is a popular area for hiking, swimming, and fishing cutthroat trout. Smaller Lake Ida is a short distance on the opposite side of Icicle Ridge and Big Jim Mountain Lakes or on the northeast slope of the mountain. Lake Augusta is located approximately 15 miles west of the city of Leavenworth.

Geographic entities mentioned:
surface_form: Big Jim Mountain Lakes
instance_of: Group of lakes
Body of water
countries: United States
coordinates: lat: 47.6662365
lon: -120.8233391
surface_form: big jim mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.6629
lon: -120.8329
surface_form: lake ida
instance_of: Lake
countries: United States
coordinates: lat: 45.990277777778
lon: -95.418055555556
surface_form: lake ida
instance_of: Lake
countries: United States
coordinates: lat: 47.635555555556
lon: -120.85944444444
surface_form: lake ida
instance_of: Lake
countries: United States
coordinates: lat: 27.762222222222
lon: -81.521111111111
Geography. Lake Augusta sits on the south skirt of Big Jim Mountain, consisting of rocky soils of intrusive rock geology. The bedrock is about 3 feet from the surface and mapped as quartz-dolerite and exposed rock that tends to be granodiorite with influence from the intrusions originated from the Mount Stuart Batholith which underlies the Stuart Range and the nearby Wenatchee Mountains.

Geographic entities mentioned:
surface_form: Big Jim Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.6629
lon: -120.8329
surface_form: lake augusta
instance_of: Lake
countries: United States
coordinates: lat: 47.653611111111
lon: -120.83527777778
Chatter Creek Trail #1580 is approximately 5.5 miles long and travels fairly closely to the course of Chatter Creek. The trail leads past Lake Sylvester and Lake Alice reaching and joining Icicle Ridge Trail #1580 on the north skirt of Grindstone mountain. Access to Lake Augusta is off Icicle Ridge Trail to the right (east) of its junction with Chatter Creek Trail.

Geographic entities mentioned:
surface_form: lake alice
instance_of: Lake
countries: United States
coordinates: lat: 29.6417
lon: -82.3567
surface_form: lake alice
instance_of: Lake
countries: United States
coordinates: lat: 44.8779156
lon: -96.6338965
surface_form: grindstone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.6978
lon: -115.905
surface_form: lake alice
instance_of: Lake
countries: United States
coordinates: lat: 47.22277778
lon: -95.08277778
surface_form: lake alice
instance_of: Lake
countries: United States
coordinates: lat: 47.6474147
lon: -120.917581
surface_form: grindstone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.6373
lon: -120.9134
surface_form: lake sylvester
instance_of: Lake
countries: United States
coordinates: lat: 47.6340416
lon: -120.9247133
Lake Augusta (Washington). Lake Augusta is a freshwater lake located on the southwest skirt of Big Jim Mountain, East of Icicle Ridge, in Chelan County, Washington. Because of its close proximity to Icicle Ridge Trail, the lake is a popular area for hiking, swimming, and fishing cutthroat trout.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: lake augusta (washington)
instance_of: Lake
countries: United States
coordinates: lat: 47.653611111111
lon: -120.83527777778
Icicle Ridge is also intersected by Hatchery Creek Trail #1577 a short distance from Lake Augusta coming from the north. The Hatchery Creek Trailhead is approximately 6 miles from the Icicle Ridge Junction and is located West of Tumwater Campground as Highway 2 crosses over Wenatchee River, south of Chiwaukum, Washington.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Lake Augusta is located approximately 15 miles west of the city of Leavenworth. Self-issued Alpine Lake Wilderness permit required for transit within the Lake Augusta area. Along with neighboring lakes, Lake Augusta was given its name by Albert Hale Sylvester, a topographer for the United States Geological Survey working throughout the North Cascades National Park Complex in the 1900s. Geography.

Geographic entities mentioned:
surface_form: alpine lake
instance_of: Lake
countries: United States
coordinates: lat: 37.9622
lon: -119.304
surface_form: lake augusta
instance_of: Lake
countries: United States
coordinates: lat: 47.653611111111
lon: -120.83527777778
surface_form: lake wilderness
instance_of: Lake
countries: United States
coordinates: lat: 47.3746
lon: -122.036
Several campsite are also located around the shore of Lake Augusta. Self-issued Alpine Lake Wilderness permit required for transit within the Grindstone Mountain area and can be obtained at the Chatter Creek Trailhead and the Campground past the Guard station. Alternate routes.

Geographic entities mentioned:
surface_form: alpine lake
instance_of: Lake
countries: United States
coordinates: lat: 37.9622
lon: -119.304
surface_form: grindstone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.6978
lon: -115.905
surface_form: grindstone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.6373
lon: -120.9134
surface_form: lake wilderness
instance_of: Lake
countries: United States
coordinates: lat: 47.3746
lon: -122.036
The trail to the lake consists of sandy loam the first half and boulders added in the second half of the trajectory. The west hills of Big Jim Mountain surrounding Lake Augusta grow tonalite and granodiorite corona-bearing dikes. The East hill grew pyroxenites, gabbro amphibolites and other diorites.

Geographic entities mentioned:
surface_form: big jim mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.6629
lon: -120.8329
surface_form: lake augusta
instance_of: Lake
countries: United States
coordinates: lat: 47.653611111111
lon: -120.83527777778
The East hill grew pyroxenites, gabbro amphibolites and other diorites. Mineral boundaries are sharp along Big Jim Mountain except between these two matrix subdomains, which are not immediately distinguishable. Coronas found in dikes along Lake Augusta show evidence of strain, deformed into elongate ellipsoids with long axes that lie parallel to the dike boundaries.

Geographic entities mentioned:
surface_form: big jim mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.6629
lon: -120.8329
The trail leads past Lake Sylvester and Lake Alice reaching and joining Icicle Ridge Trail #1580 on the north skirt of Grindstone mountain. Access to Lake Augusta is off Icicle Ridge Trail to the right (east) of its junction with Chatter Creek Trail. Icicle Ridge Trail shortly afterwards will follow the ridge to Lake Ida on the right and Lake Augusta over the east slope of Big Jim Mountain.

Geographic entities mentioned:
surface_form: big jim mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.6629
lon: -120.8329
surface_form: lake augusta
instance_of: Lake
countries: United States
coordinates: lat: 47.653611111111
lon: -120.83527777778
surface_form: lake ida
instance_of: Lake
countries: United States
coordinates: lat: 45.990277777778
lon: -95.418055555556
surface_form: lake ida
instance_of: Lake
countries: United States
coordinates: lat: 47.635555555556
lon: -120.85944444444
surface_form: lake ida
instance_of: Lake
countries: United States
coordinates: lat: 27.762222222222
lon: -81.521111111111
Smaller Lake Ida is a short distance on the opposite side of Icicle Ridge and Big Jim Mountain Lakes or on the northeast slope of the mountain. Lake Augusta is located approximately 15 miles west of the city of Leavenworth. Self-issued Alpine Lake Wilderness permit required for transit within the Lake Augusta area.

Geographic entities mentioned:
surface_form: lake augusta
instance_of: Lake
countries: United States
coordinates: lat: 47.653611111111
lon: -120.83527777778
Lake Augusta is located approximately 15 miles west of the city of Leavenworth. Self-issued Alpine Lake Wilderness permit required for transit within the Lake Augusta area. Along with neighboring lakes, Lake Augusta was given its name by Albert Hale Sylvester, a topographer for the United States Geological Survey working throughout the North Cascades National Park Complex in the 1900s. Geography.

Geographic entities mentioned:
surface_form: lake augusta
instance_of: Lake
countries: United States
coordinates: lat: 47.653611111111
lon: -120.83527777778