Sarmila/GeoWiki-Features huggingface dataset:
They figured they could sell the ranch together with some other ranches to the government for an Indian reservation. After the idea received the support of the Shoshone, the Bureau of Indian Affairs bought two ranches, and thus created the Indian reservation. At its creation, it had a size of, but the government has expanded it since by acquiring more ranch lands.

Geographic entities mentioned:
surface_form: shoshone
instance_of: Lake
countries: United States
coordinates: lat: 44.3722
lon: -110.713
Duckwater Valley. Duckwater Valley is a valley in Nye County, Nevada. It starts south of the northern border of Nye County, and runs south for a distance of approximately to Railroad Valley. The Duckwater Valley is enclosed by the Pancake Range in the west and by the Duckwater Hills in the east. The Duckwater Creek crosses the valley.

Geographic entities mentioned:
surface_form: duckwater valley
instance_of: Valley
countries: United States
coordinates: lat: 38.93604
lon: -115.72421
Duckwater Valley is a valley in Nye County, Nevada. It starts south of the northern border of Nye County, and runs south for a distance of approximately to Railroad Valley. The Duckwater Valley is enclosed by the Pancake Range in the west and by the Duckwater Hills in the east. The Duckwater Creek crosses the valley. State Route 379 goes partially through the Duckwater Valley as well.

Geographic entities mentioned:
surface_form: duckwater valley
instance_of: Valley
countries: United States
coordinates: lat: 38.93604
lon: -115.72421
The Duckwater Valley is enclosed by the Pancake Range in the west and by the Duckwater Hills in the east. The Duckwater Creek crosses the valley. State Route 379 goes partially through the Duckwater Valley as well. The only populated place in the valley is Duckwater. Part of the valley is occupied by the Duckwater Reservation. History.

Geographic entities mentioned:
surface_form: duckwater valley
instance_of: Valley
countries: United States
coordinates: lat: 38.93604
lon: -115.72421
Part of the valley is occupied by the Duckwater Reservation. History. The valley had been inhabited for a long time by Native Americans, when the first white Americans settled in the Duckwater Valley in the 1860s after silver ore was discovered in nearby Hamilton. Agriculture arose in the valley, and for years hay, grain, vegetables, and fruit were grown for the inhabitants of Hamilton.

Geographic entities mentioned:
surface_form: duckwater valley
instance_of: Valley
countries: United States
coordinates: lat: 38.93604
lon: -115.72421
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Agriculture arose in the valley, and for years hay, grain, vegetables, and fruit were grown for the inhabitants of Hamilton. Isaak &quot;Ike&quot; Irwin, who produced hay, was in 1868 the first person to settle in the present-day village Duckwater. When Hamilton was in decline, farmers in the Duckwater Valley started focussing on hay and grain, that they fed to their cattle.

Geographic entities mentioned:
surface_form: duckwater valley
instance_of: Valley
countries: United States
coordinates: lat: 38.93604
lon: -115.72421
That land was used for growing grain and vegetables. Back then, some fruit plants had been planted recently. Thereafter, the livestock sector gradually grew in the Duckwater Valley, and it became the biggest in the valley. Around 1910, the farmers reduced the size of their cattle, because their rangelands were damaged by flocks of wild sheep in the winter season.

Geographic entities mentioned:
surface_form: duckwater valley
instance_of: Valley
countries: United States
coordinates: lat: 38.93604
lon: -115.72421
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
In 1913, the &quot;Ely Record&quot; said the Duckwater Valley was &quot;one of the most extensive ranching and farming sections in Eastern Nevada.&quot; The newspaper wrote that there were a number of ranches, one of which with of land, of which were in cultivation. Those ranches grew hay, grain, alfalfa, and potatoes, and were grazed by herds of cattle.

Geographic entities mentioned:
surface_form: duckwater valley
instance_of: Valley
countries: United States
coordinates: lat: 38.93604
lon: -115.72421
Those ranches grew hay, grain, alfalfa, and potatoes, and were grazed by herds of cattle. The reservation of the Duckwater Shoshone Tribe, that is situated entirely in the Duckwater Valley, has a surface area of over, and was officially created in 1940.

Geographic entities mentioned:
surface_form: duckwater valley
instance_of: Valley
countries: United States
coordinates: lat: 38.93604
lon: -115.72421
It starts south of the northern border of Nye County, and runs south for a distance of approximately to Railroad Valley. The Duckwater Valley is enclosed by the Pancake Range in the west and by the Duckwater Hills in the east. The Duckwater Creek crosses the valley. State Route 379 goes partially through the Duckwater Valley as well. The only populated place in the valley is Duckwater.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The Duckwater Valley is enclosed by the Pancake Range in the west and by the Duckwater Hills in the east. The Duckwater Creek crosses the valley. State Route 379 goes partially through the Duckwater Valley as well. The only populated place in the valley is Duckwater. Part of the valley is occupied by the Duckwater Reservation. History.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
State Route 379 goes partially through the Duckwater Valley as well. The only populated place in the valley is Duckwater. Part of the valley is occupied by the Duckwater Reservation. History. The valley had been inhabited for a long time by Native Americans, when the first white Americans settled in the Duckwater Valley in the 1860s after silver ore was discovered in nearby Hamilton.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Part of the valley is occupied by the Duckwater Reservation. History. The valley had been inhabited for a long time by Native Americans, when the first white Americans settled in the Duckwater Valley in the 1860s after silver ore was discovered in nearby Hamilton. Agriculture arose in the valley, and for years hay, grain, vegetables, and fruit were grown for the inhabitants of Hamilton.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
When Hamilton was in decline, farmers in the Duckwater Valley started focussing on hay and grain, that they fed to their cattle. According to the 1881 book &quot;History of Nevada&quot; by Thompson and West, the valley consisted almost entirely of meadows, of which was occupied by agricultural lands. That land was used for growing grain and vegetables.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
It was located on the Bishop Auckland and Weardale Railway line from to Blackhill between Wear Valley Junction and Tow Law. History. The station was opened by the Stockton & Darlington Railway in 1851 on their line between Bishop Auckland and Blackhill. It was located in a rural area of Weardale. The station closed to passengers in 1881 before closing to all traffic between Tow Law and Blackhill.

Geographic entities mentioned:
surface_form: Weardale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.716
lon: -1.925
Mesilla Valley AVA. The Mesilla Valley AVA is an American Viticultural Area located primarily in the state of New Mexico, with a small area in the state of Texas. Spanish explorer Don Juan de Oñate arrived in the area in 1598, and named a Native American village in the valley &quot;Trenquel de la Mesilla&quot;, from which the valley as a whole became known as Mesilla Valley.

Geographic entities mentioned:
surface_form: Mesilla Valley
instance_of: Valley
countries: United States
coordinates: lat: 31.7903
lon: -106.423
Deltaform Mountain. Deltaform Mountain is one of the mountains in the Valley of the Ten Peaks, located on the Continental Divide on the border of British Columbia and Alberta, and also on the border between Banff and Kootenay National Parks in Canada.

Geographic entities mentioned:
surface_form: Valley of the Ten Peaks
instance_of: Valley
countries: Canada
coordinates: lat: 51.3494444
lon: -116.1597222
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: deltaform mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.30166666666667
lon: -116.24527777777777
surface_form: kootenay
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Deltaform Mountain. Deltaform Mountain is one of the mountains in the Valley of the Ten Peaks, located on the Continental Divide on the border of British Columbia and Alberta, and also on the border between Banff and Kootenay National Parks in Canada.

Geographic entities mentioned:
surface_form: deltaform mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.30166666666667
lon: -116.24527777777777
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Deltaform was first climbed in 1903 by August Eggers and Herschel Clifford Parker who were guided by Christian and Hans Kaufmann. __NOTOC__
Geology. Deltaform Mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate.

Geographic entities mentioned:
surface_form: deltaform mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.30166666666667
lon: -116.24527777777777
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Deltaform Mountain is one of the mountains in the Valley of the Ten Peaks, located on the Continental Divide on the border of British Columbia and Alberta, and also on the border between Banff and Kootenay National Parks in Canada. The mountain was originally named Saknowa by Samuel Allen but Walter Wilcox named it to its official title in 1897 as it resembles the Greek letter delta.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Col-Glen Shinty Club. Col-Glen Shinty Club is a shinty club based in Clachan of Glendaruel, on the Cowal Peninsula, in Argyll and Bute, west of Scotland. History. The club was founded in 1920, and was originally called Colintraive and Glendaruel Shinty Club. The name reflects the two villages from which it has always drawn its players and support, Colintraive and Glendaruel.

Geographic entities mentioned:
surface_form: Clachan of Glendaruel
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.009126
lon: -5.214326
History. The club was founded in 1920, and was originally called Colintraive and Glendaruel Shinty Club. The name reflects the two villages from which it has always drawn its players and support, Colintraive and Glendaruel. The name was shortened to Col Glen some time in the 1930s.

Geographic entities mentioned:
surface_form: Glendaruel
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.009126
lon: -5.214326
Puka Mach'ay (Junín). Puka Mach'ay (Quechua &quot;puka&quot; red, &quot;mach'ay&quot; cave, &quot;red cave&quot;, also spelled &quot;Pucamachay&quot;) is a mountain in Peru which reaches a height of approximately. It is located in the Junín Region, Yauli Province, Morococha District.

Geographic entities mentioned:
surface_form: junín
instance_of: Lake
countries: Peru
coordinates: lat: -11.0201
lon: -76.1075
surface_form: puka mach'ay
instance_of: Mountain
countries: Peru
coordinates: lat: -9.77167
lon: -77.2344
surface_form: puka mach'ay
instance_of: Mountain
countries: Peru
coordinates: lat: -10.64111111
lon: -76.61194444
surface_form: puka
instance_of: Mountain
countries: Peru
coordinates: lat: -12.6339
lon: -75.5692
surface_form: puka mach'ay
instance_of: Mountain
countries: Peru
coordinates: lat: -11.49888889
lon: -76.08666667
surface_form: mach'ay
instance_of: Mountain
countries: Peru
coordinates: lat: -9.63722222
lon: -76.40027778
Puka Mach'ay (Junín). Puka Mach'ay (Quechua &quot;puka&quot; red, &quot;mach'ay&quot; cave, &quot;red cave&quot;, also spelled &quot;Pucamachay&quot;) is a mountain in Peru which reaches a height of approximately. It is located in the Junín Region, Yauli Province, Morococha District.

Geographic entities mentioned:
surface_form: pucamachay
instance_of: Mountain
countries: Peru
coordinates: lat: -9.77167
lon: -77.2344
surface_form: puka mach'ay
instance_of: Mountain
countries: Peru
coordinates: lat: -9.77167
lon: -77.2344
surface_form: puka mach'ay
instance_of: Mountain
countries: Peru
coordinates: lat: -10.64111111
lon: -76.61194444
surface_form: puka
instance_of: Mountain
countries: Peru
coordinates: lat: -12.6339
lon: -75.5692
surface_form: puka
instance_of: Mountain
countries: Peru
coordinates: lat: -12.6339
lon: -75.5692
surface_form: puka mach'ay
instance_of: Mountain
countries: Peru
coordinates: lat: -11.49888889
lon: -76.08666667
surface_form: mach'ay
instance_of: Mountain
countries: Peru
coordinates: lat: -9.63722222
lon: -76.40027778
surface_form: mach'ay
instance_of: Mountain
countries: Peru
coordinates: lat: -9.63722222
lon: -76.40027778
Monson's Hoist Bay Resort. Monson's Hoist Bay Resort is a former summer resort on Namakan Lake in the U.S. state of Minnesota, in what is now Voyageurs National Park. Ted and Fern Monson established the resort in 1939 and operated it every summer until 1973, except for a three-year hiatus during World War II. The remote property was and remains accessible only by water.

Geographic entities mentioned:
surface_form: Namakan Lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 48.456693
lon: -92.585364
Paznaun. The Paznaun () is a valley in Tyrol, Austria, leading south-west from Pians (856 m) to the Bielerhöhe (2071 m), a mountain pass at the border of Vorarlberg and Tyrol. The Paznaun is watered by the Trisanna and surrounded by the Central Eastern Alps, specifically, the mountain ranges of Verwall in the north, Samnaun in the south-east and Silvretta in the south-west.

Geographic entities mentioned:
surface_form: paznaun
instance_of: Valley
countries: Austria
coordinates: lat: 47.05
lon: 10.333333333333
The Paznaun is watered by the Trisanna and surrounded by the Central Eastern Alps, specifically, the mountain ranges of Verwall in the north, Samnaun in the south-east and Silvretta in the south-west. The main villages in the Paznaun are See (1050m), Kappl (1226m), Ischgl (1377m) and Galtür (1586m). Today, the main economic activity in the valley is tourism, especially winter sports.

Geographic entities mentioned:
surface_form: paznaun
instance_of: Valley
countries: Austria
coordinates: lat: 47.05
lon: 10.333333333333
The population was 1,986 at the 2020 census. The city is partially surrounded by Munising Township, but the two are administered autonomously. Located on the southern shore of Lake Superior in the Upper Peninsula, it serves as the western gateway to Pictured Rocks National Lakeshore. History. The name for the city comes from the Ojibwe word &quot;minisiing&quot;, &quot;at the island&quot;.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Delos (mountain). Delos or Delos Mountain was the ancient name of a mountain located in Boeotia, Greece, above the city of Tegyra. The mountain was sacred to Apollo, to whom temples on its slopes were dedicated.

Geographic entities mentioned:
surface_form: delos mountain
instance_of: Mountain
countries: Greece
coordinates: lat: 38.52
lon: 23.047
Delos (mountain). Delos or Delos Mountain was the ancient name of a mountain located in Boeotia, Greece, above the city of Tegyra. The mountain was sacred to Apollo, to whom temples on its slopes were dedicated.

Geographic entities mentioned:
surface_form: delos (mountain)
instance_of: Mountain
countries: Greece
coordinates: lat: 38.52
lon: 23.047
Jualbup Lake. Lake Jualbup, formerly the Shenton Park Lake, is a freshwater lake located in Perth, Western Australia. Description. The lake is contained within Shenton Park, a parkland in the suburb of Shenton Park, bounded by Lake Avenue, Excelsior Street, Evans Street and Herbert Road.

Geographic entities mentioned:
surface_form: freshwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.6453
lon: -60.3967
surface_form: shenton park lake
instance_of: Lake
countries: Australia
coordinates: lat: -31.958888888889
lon: 115.81194444444
In the early days of European settlement, a timber miller named James Dyson worked in the area, and thus it became known as Dyson's Swamp. In 1877, James Dyson sold his swamp to George Shenton's son. Later it was renamed Shenton Park Lake, after the land developer and politician, George Shenton. The Aboriginal name &quot;Jualbup&quot; was restored to the lake in 1996.

Geographic entities mentioned:
surface_form: george
instance_of: Lake
countries: Australia
coordinates: lat: -35.1667
lon: 149.417
In the early days of European settlement, a timber miller named James Dyson worked in the area, and thus it became known as Dyson's Swamp. In 1877, James Dyson sold his swamp to George Shenton's son. Later it was renamed Shenton Park Lake, after the land developer and politician, George Shenton. The Aboriginal name &quot;Jualbup&quot; was restored to the lake in 1996.

Geographic entities mentioned:
surface_form: george
instance_of: Lake
countries: Australia
coordinates: lat: -35.1667
lon: 149.417
surface_form: shenton park lake
instance_of: Lake
countries: Australia
coordinates: lat: -31.958888888889
lon: 115.81194444444
Jualbup Lake. Lake Jualbup, formerly the Shenton Park Lake, is a freshwater lake located in Perth, Western Australia. Description. The lake is contained within Shenton Park, a parkland in the suburb of Shenton Park, bounded by Lake Avenue, Excelsior Street, Evans Street and Herbert Road.

Geographic entities mentioned:
surface_form: jualbup lake
instance_of: Lake
countries: Australia
coordinates: lat: -31.958888888889
lon: 115.81194444444
Unemployed professional women in New Jersey attended a specially created program. In Michigan, rented houses provided unemployed women instruction in housekeeping skills. In the Ozarks, women attended literacy classes. Details. The personal allowance for women was the same as that for men, $5 per month for personal needs in exchange for 56–70 hrs work per month on camp work projects.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
This detention in Ceylon enabled Marignolli to give a variety of curious particulars regarding Buddhist monasticism, the aboriginal races of Ceylon, and other marvels. The locals claimed that &quot;Seyllan&quot; (Adam's Peak) was 40 miles from Paradise, but he was unable to explore the area.

Geographic entities mentioned:
surface_form: Adam's Peak
instance_of: Mountain
countries: Sri Lanka
coordinates: lat: 6.809444444444445
lon: 80.49972222222222
Zonda Glacier. Zonda Glacier () is a glacier about 8 miles (13 km) long, flowing west-southwest between Fohn Bastion and Zonda Towers into George VI Sound. The glacier was included in surveys by Falkland Islands Dependencies Survey (FIDS), 1948, and British Antarctic Survey (BAS), 1971–72, and was photographed from the air by the U.S. Navy, 1966.

Geographic entities mentioned:
surface_form: Zonda Towers
instance_of: Mountain
coordinates: lat: -69.566
lon: -68.3
Upon her death in 2011, Dysart inherited her titles. Together with his son James, he is responsible for Rothiemurchus, in the Scottish Highlands, including part of Rothiemurchus Forest and Braeriach, which at 4252 ft (1296 m) is the third highest mountain in Britain. The 13th Earl's wife was killed following a collision with a coach in 2022. Marriage and issue.

Geographic entities mentioned:
surface_form: Braeriach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.078298
lon: -3.728389
Curacautín. Curacautín, which means &quot;Gathering Stone&quot; in Mapudungun, is a commune and city in the Chilean province of Malleco. Curacautín is located 90 kilometres northeast of Temuco, in a valley near the volcanoes Tolhuaca, Lonquimay and Llaima, all of which can be seen from the city.

Geographic entities mentioned:
surface_form: Llaima
instance_of: Mountain
countries: Chile
coordinates: lat: -38.697407
lon: -71.730445
In contrast to the sheartail, the woodstar usually flies with its tail cocked and seldom pumps its tail. Distribution and habitat. The Chilean woodstar is now (2022) known only from the Lluta, Azapa, and Vitor valleys of far northern Chile's Arica and Parinacota Region. There is an historical record further south in Antofagasta Province.

Geographic entities mentioned:
surface_form: Azapa
instance_of: Valley
countries: Chile
coordinates: lat: -18.51722222
lon: -70.19194444
Lužice () is a municipality and village in Hodonín District in the South Moravian Region of the Czech Republic. It has about 2,900 inhabitants. Geography. Lužice is located about west of Hodonín and southeast of Brno. It lies in a flat landscape of the Lower Morava Valley. The Kyjovka River flows through the municipality. History. The first written mention of Lužice is from 1250.

Geographic entities mentioned:
surface_form: Lower Morava Valley
instance_of: Valley
countries: Czech Republic
coordinates: lat: 48.9430014
lon: 17.3295197
Deadwood Draw. Deadwood Draw is part of the Sidney-Black Hills Trail near Sidney, Nebraska, which provided supplies for gold mining operations in the Black Hills from 1874 to 1881. The draw served as a staging area for freight wagons carrying supplies to the Black Hills and contains ruts caused by the wheels of the freight wagons and the animals that pulled them.

Geographic entities mentioned:
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
surface_form: deadwood draw
instance_of: Valley
countries: United States
coordinates: lat: 41.1597
lon: -103.008
Deadwood Draw. Deadwood Draw is part of the Sidney-Black Hills Trail near Sidney, Nebraska, which provided supplies for gold mining operations in the Black Hills from 1874 to 1881. The draw served as a staging area for freight wagons carrying supplies to the Black Hills and contains ruts caused by the wheels of the freight wagons and the animals that pulled them.

Geographic entities mentioned:
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
The draw is listed on the National Register of Historic Places. Background. In 1868, the U.S. government signed the Fort Laramie Treaty, which promised the Lakota people that the Black Hills would be exempt from white settlement. However, in 1874, an expedition into the Black Hills led by George Armstrong Custer, found deposits of gold.

Geographic entities mentioned:
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
Background. In 1868, the U.S. government signed the Fort Laramie Treaty, which promised the Lakota people that the Black Hills would be exempt from white settlement. However, in 1874, an expedition into the Black Hills led by George Armstrong Custer, found deposits of gold. In 1876, Custer's discovery of gold led to the Black Hills Gold Rush. Initially, the U. S.

Geographic entities mentioned:
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
In 1876, Custer's discovery of gold led to the Black Hills Gold Rush. Initially, the U. S. government attempted to purchase or lease the Black Hills from the Lakota, but the government was unwilling to pay the price asked by the Lakota. When the talks broke down, the U. S. government ignored the Fort Laramie Treaty of 1868 and allowed the gold seekers to rush into the Black Hills.

Geographic entities mentioned:
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
When the talks broke down, the U. S. government ignored the Fort Laramie Treaty of 1868 and allowed the gold seekers to rush into the Black Hills. The Black Hills gold rush subsequently created a high demand for supplies by the gold seekers. In 1876, Sidney, Nebraska was a small town on the Union Pacific railroad.

Geographic entities mentioned:
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
In 1876, Sidney, Nebraska was a small town on the Union Pacific railroad. Sidney had two main advantages over other railroad towns in Nebraska as a staging point for supplying the gold rush in the Black Hills. First, there already was a trail from Sidney north to the Red Cloud Agency, which was protected by the military between Fort Sidney and Fort Robinson.

Geographic entities mentioned:
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
Second, the route was shorter than other possible supply points along the railroad and with the building of the Clarke Bridge toll bridge over the North Platte River by Henry T. Clarke, Sr., travel on Sidney-Black Hills Trail became easier for freight wagons.

Geographic entities mentioned:
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
Clarke, Sr., travel on Sidney-Black Hills Trail became easier for freight wagons. With the opening of the Clarke bridge, the Sidney-Black Hills trail began carrying larger quantities of freight to and from the Black Hills mining operations. During the summer of 1876, the Pony Express began operating along the trail, as did several stagecoach lines.

Geographic entities mentioned:
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
During the summer of 1876, the Pony Express began operating along the trail, as did several stagecoach lines. In 1876, there were an estimated 10,000 gold seekers in the Black Hills and their demand for supplies was so high that approximately 50 to 75 freight wagons left daily from Sidney, each wagon carrying of supplies.

Geographic entities mentioned:
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
In 1876, there were an estimated 10,000 gold seekers in the Black Hills and their demand for supplies was so high that approximately 50 to 75 freight wagons left daily from Sidney, each wagon carrying of supplies. In 1879, the Black Hills gold rush ended and so did the need for high passenger service along the trail.

Geographic entities mentioned:
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
By 1880, with the completion of the Chicago and Northwestern Railroad to Pierre, the transportation of freight along the trail dramatically dropped. It was quicker and cheaper to transport supplies along the new railroad than to use freight wagons along the Sidney-Black Hills trail. By the end of 1882, the trail was completely closed. Description.

Geographic entities mentioned:
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
Description. Deadwood Draw is located about northwest of Sidney, Nebraska, and close to the Union Pacific railroad from which supplies could be loaded onto freight wagons headed for the Black Hills via the Sidney-Black Hills trail. The draw is a wide, flat area that gently slopes up and out of Lodgepole Creek Valley and away from Union Pacific railroad and on to the Sidney-Black Hills trail.

Geographic entities mentioned:
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
surface_form: deadwood draw
instance_of: Valley
countries: United States
coordinates: lat: 41.1597
lon: -103.008
Description. Deadwood Draw is located about northwest of Sidney, Nebraska, and close to the Union Pacific railroad from which supplies could be loaded onto freight wagons headed for the Black Hills via the Sidney-Black Hills trail. The draw is a wide, flat area that gently slopes up and out of Lodgepole Creek Valley and away from Union Pacific railroad and on to the Sidney-Black Hills trail.

Geographic entities mentioned:
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
The rut pairs range in width from to. Historical significance. Deadwood Draw was a staging area for freight wagons using the Sidney-Black Hills trail. As of 1992, when it was placed on the National Register of Historic Places, it had well-preserved ruts caused by freight wagons, stage coaches, and the animals that pulled them from 1874 to 1881.

Geographic entities mentioned:
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
surface_form: deadwood draw
instance_of: Valley
countries: United States
coordinates: lat: 41.1597
lon: -103.008
Clarke, Sr., travel on Sidney-Black Hills Trail became easier for freight wagons. With the opening of the Clarke bridge, the Sidney-Black Hills trail began carrying larger quantities of freight to and from the Black Hills mining operations. During the summer of 1876, the Pony Express began operating along the trail, as did several stagecoach lines.

Geographic entities mentioned:
surface_form: stagecoach
instance_of: Mountain
countries: United States
coordinates: lat: 37.036111111111
lon: -110.0725
Deadwood Draw. Deadwood Draw is part of the Sidney-Black Hills Trail near Sidney, Nebraska, which provided supplies for gold mining operations in the Black Hills from 1874 to 1881. The draw served as a staging area for freight wagons carrying supplies to the Black Hills and contains ruts caused by the wheels of the freight wagons and the animals that pulled them.

Geographic entities mentioned:
surface_form: deadwood draw
instance_of: Valley
countries: United States
coordinates: lat: 41.1597
lon: -103.008
Russell Nunatak. 2hx2njrn1s3266cbdfk7luy5854b" xml:space="preserve">Russell Nunatak () is a solitary rounded nunatak 10 nautical miles (18 km) east of the Masson Range and 7 nautical miles (13 km) southeast of Mount Henderson. Discovered in December 1954 by an ANARE (Australian National Antarctic Research Expeditions) party led by R.

Geographic entities mentioned:
surface_form: mount henderson
instance_of: Mountain
coordinates: lat: -67.7
lon: 63.0667
surface_form: russell nunatak
instance_of: Mountain
coordinates: lat: -67.7833
lon: 63.3167
Russell Nunatak. 2hx2njrn1s3266cbdfk7luy5854b" xml:space="preserve">Russell Nunatak () is a solitary rounded nunatak 10 nautical miles (18 km) east of the Masson Range and 7 nautical miles (13 km) southeast of Mount Henderson. Discovered in December 1954 by an ANARE (Australian National Antarctic Research Expeditions) party led by R.

Geographic entities mentioned:
surface_form: russell nunatak
instance_of: Mountain
coordinates: lat: -67.7833
lon: 63.3167
The city, harbour and the Remutaka and Tararua Ranges can be seen from the summit. On a clear day Mount Tapuae-o-Uenuku and the Kaikōura Ranges in the South Island may be seen, whilst northwest is the Porirua Basin and the Tasman Sea. Name. The hill's original name &quot;Tarikākā&quot; means 'where the parrots rested' and is shared with the nearby settlement in Ngaio at the base of the mountain.

Geographic entities mentioned:
surface_form: Tapuae-o-Uenuku
instance_of: Mountain
countries: New Zealand
coordinates: lat: -41.995833333333
lon: 173.6625
Mount Kaukau. Mount Kaukau () is a large hill in the northern suburbs of Wellington, New Zealand near Johnsonville, Khandallah and Ngaio. The summit is above sea level and is the most visible high point in the Wellington landscape further accentuated by Wellington's main television transmitter mast, which stands from the summit.

Geographic entities mentioned:
surface_form: kaukau
instance_of: Mountain
countries: New Zealand
coordinates: lat: -41.231472
lon: 174.777806
surface_form: mount kaukau
instance_of: Mountain
countries: New Zealand
coordinates: lat: -41.231472
lon: 174.777806
Before the clearing of the native tōtara forest on the slopes and general area, the native parrot kākā was common through the city. Over a hundred years later today, the population of kākā has begun to regenerate thanks mostly to the efforts at Zealandia, and are becoming a more regular sight throughout the city and in the rejuvenating native forest on the slopes of Mount Kaukau.

Geographic entities mentioned:
surface_form: kaukau
instance_of: Mountain
countries: New Zealand
coordinates: lat: -41.231472
lon: 174.777806
surface_form: mount kaukau
instance_of: Mountain
countries: New Zealand
coordinates: lat: -41.231472
lon: 174.777806
Slopes and surrounding area. Much of the eastern 'city side' slopes of Mount Kaukau make up Khandallah Park, which is one of the oldest parks in New Zealand, established in 1888 and then registered as a domain in 1909. Khandallah Park has more than 60 hectares of native forest. Native birds such as the kererū, tūī and New Zealand fantail are common sights when walking through the native forest.

Geographic entities mentioned:
surface_form: kaukau
instance_of: Mountain
countries: New Zealand
coordinates: lat: -41.231472
lon: 174.777806
surface_form: mount kaukau
instance_of: Mountain
countries: New Zealand
coordinates: lat: -41.231472
lon: 174.777806
Stumps of the old totara trees can also be seen walking through the first lower parts of the forest. In mid 2017 an old bunker off Woodmancote Road, at the base of Mount Kaukau, was rediscovered after it had been sealed off and forgotten many years previously. The bunker in an 'H' shape, had been built for Royal New Zealand Signals Corps in 1942.

Geographic entities mentioned:
surface_form: kaukau
instance_of: Mountain
countries: New Zealand
coordinates: lat: -41.231472
lon: 174.777806
surface_form: mount kaukau
instance_of: Mountain
countries: New Zealand
coordinates: lat: -41.231472
lon: 174.777806
Due to poor construction the bunker was very leaky and was never used. Mount Kaukau forms part of the Northern Skyline track from Johnsonville to Karori and Makara. Recreation. Khandallah Park has 9 kilometres of walking tracks allowing access to the peak of Mt Kaukau from Khandallah, Johnsonville, Ngaio and Crofton Downs. Some tracks are also open to mountain biking and e-biking. Transmitter.

Geographic entities mentioned:
surface_form: kaukau
instance_of: Mountain
countries: New Zealand
coordinates: lat: -41.231472
lon: 174.777806
Some tracks are also open to mountain biking and e-biking. Transmitter. The Mount Kaukau television transmitter was approved for construction in February 1965, at a cost of £410,000. It incorporated 100 kW television transmitter and a 122-metre transmission tower to transmit television channel WNTV1 (now part of TVNZ 1).

Geographic entities mentioned:
surface_form: kaukau
instance_of: Mountain
countries: New Zealand
coordinates: lat: -41.231472
lon: 174.777806
The UHF TV antennas are located 93 metres up the tower, while the FM radio antennas are located 65 metres up the tower. Former analogue television frequencies. The following frequencies were used until 29 September 2013, when Kaukau switched off analogue broadcasts (see Digital changeover dates in New Zealand). Kaukau Challenge.

Geographic entities mentioned:
surface_form: kaukau
instance_of: Mountain
countries: New Zealand
coordinates: lat: -41.231472
lon: 174.777806
surface_form: kaukau
instance_of: Mountain
countries: New Zealand
coordinates: lat: -41.231472
lon: 174.777806
Kaukau Challenge. Every year Khandallah School, which is at the base of Mount Kaukau, organises a fun walk / fun run from the school to the summit and back, called the Kaukau Challenge. The Kaukau Challenge has been an annual event since 2006 with about 500 people taking part each year. Snowfall of 2011.

Geographic entities mentioned:
surface_form: kaukau
instance_of: Mountain
countries: New Zealand
coordinates: lat: -41.231472
lon: 174.777806
surface_form: kaukau
instance_of: Mountain
countries: New Zealand
coordinates: lat: -41.231472
lon: 174.777806
surface_form: kaukau
instance_of: Mountain
countries: New Zealand
coordinates: lat: -41.231472
lon: 174.777806
surface_form: mount kaukau
instance_of: Mountain
countries: New Zealand
coordinates: lat: -41.231472
lon: 174.777806
Snowfall of 2011. In mid-August 2011, two Wellington men, Nick Fone and Daniel McFadyen claimed to be the first people to ski and snowboard down Mount Kaukau when they took advantage of the unusual weather pattern delivering snow to most parts of the North Island. As Wellington has a temperate climate, snow down to near sea level is extremely rare, happening less often than once every 15 years.

Geographic entities mentioned:
surface_form: kaukau
instance_of: Mountain
countries: New Zealand
coordinates: lat: -41.231472
lon: 174.777806
surface_form: mount kaukau
instance_of: Mountain
countries: New Zealand
coordinates: lat: -41.231472
lon: 174.777806
A survey of bryophytes on peatlands across Alberta's Mackenzie River basin found optimal ribbed bog moss growth occurred on sites with annual temperatures ranging from. In interior arctic, subarctic, and boreal zones, climate is strongly continental in the west, becoming more humid to the east. Climate shift from continental to humid generally occurs near Hudson Bay and Lake Superior.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
This land, the deed of which was confirmed by Governor Benjamin Fletcher, was on the eastern side of the Hudson, north of Albany, and was seventy miles in length and twelve in breadth. Dellius also obtained a large tract of land in the valley of the Mohawk, fifty miles by four. In an interview, the Indians told Bellomont the details of how the deed was conveyed.

Geographic entities mentioned:
surface_form: valley of the Mohawk
instance_of: Valley
countries: United States
Early in her career, the crane was used throughout the entire harbour, but the barge's poor seakeeping ability made it dangerous to tow the crane across Sydney Heads, and she was later banned from operating north and east of Bradleys Head. A modernisation of &quot;Titan&quot; began in the late 1960s.

Geographic entities mentioned:
surface_form: Sydney Heads
instance_of: Landform
countries: Australia
coordinates: lat: -33.8368
lon: 151.281
Samson or Sampson's Rock is a glacial erratic boulder in Madison in New Haven County, Connecticut that, according to Algonquin legend, was formed by Odziozo the giant. The legend says that Odziozo created it after he flung some land out to sea, creating Tuxis Island. The hole filled up to become Tuxis Pond. One rock fell from his hand and became Samson Rock. While leaving, he stepped on the rock.

Geographic entities mentioned:
surface_form: Tuxis Pond
instance_of: Lake
countries: United States
coordinates: lat: 41.28091667
lon: -72.59722222
Elbow Pond (Plymouth, Massachusetts). Elbow Pond is a pond in the Cedarville section of Plymouth, Massachusetts. The pond is located south of Island Pond and west of Great Herring Pond.

Geographic entities mentioned:
surface_form: Great Herring Pond
instance_of: Lake
countries: United States
coordinates: lat: 41.8075
lon: -70.564722222222
surface_form: island pond
instance_of: Lake
countries: United States
coordinates: lat: 43.0667
lon: -72.0842
surface_form: island pond
instance_of: Lake
countries: United States
coordinates: lat: 43.6837248
lon: -73.6567523
surface_form: island pond
instance_of: Lake
countries: United States
coordinates: lat: 42.8675
lon: -71.2133
surface_form: island pond
instance_of: Lake
countries: United States
coordinates: lat: 41.9
lon: -70.6411
surface_form: island pond
instance_of: Lake
countries: United States
coordinates: lat: 41.884722222222
lon: -70.573055555556
Elbow Pond (Plymouth, Massachusetts). Elbow Pond is a pond in the Cedarville section of Plymouth, Massachusetts. The pond is located south of Island Pond and west of Great Herring Pond.

Geographic entities mentioned:
surface_form: elbow pond (plymouth, massachusetts)
instance_of: Lake
countries: United States
coordinates: lat: 41.805
lon: -70.58
surface_form: elbow pond
instance_of: Lake
countries: United States
coordinates: lat: 43.9700635
lon: -74.916294
Elbow Pond (Plymouth, Massachusetts). Elbow Pond is a pond in the Cedarville section of Plymouth, Massachusetts. The pond is located south of Island Pond and west of Great Herring Pond.

Geographic entities mentioned:
surface_form: elbow pond
instance_of: Lake
countries: United States
coordinates: lat: 41.805
lon: -70.58
surface_form: elbow pond
instance_of: Lake
countries: United States
coordinates: lat: 43.9700635
lon: -74.916294
Lyall Glacier. Lyall Glacier is within the Wenatchee National Forest in Chelan County, Washington, United States, and is just southeast of Frisco Mountain. It occupies the north cirque on Rainy Peak. Melt from Lyall Glacier contributes to waterfalls which tumble into Rainy Lake. Lyall Glacier is now said to have disappeared.

Geographic entities mentioned:
surface_form: Frisco Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.48902
lon: -120.75649
Lyall Glacier. Lyall Glacier is within the Wenatchee National Forest in Chelan County, Washington, United States, and is just southeast of Frisco Mountain. It occupies the north cirque on Rainy Peak. Melt from Lyall Glacier contributes to waterfalls which tumble into Rainy Lake. Lyall Glacier is now said to have disappeared.

Geographic entities mentioned:
surface_form: Rainy Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.48527778
lon: -120.74638889
Ardennes. The Ardennes lie in Belgium, with foothills in France and Luxembourg. Eifel. The Eifel lies in Germany with foothills in Belgium and Luxembourg. → &quot;main article: List of mountains and hills of the Eifel&quot;
High Fens. The High Fens lie in Belgium with foothills in Germany. Hunsrück. The Hunsrück lies in Rhineland-Palatinate with foothills in the Saarland. Kellerwald.

Geographic entities mentioned:
surface_form: High Fens
instance_of: Plateau
countries: Belgium
Germany
coordinates: lat: 50.521389
lon: 6.102778
Tom Creek. Tom Creek is a creek located in the Omineca Country region of British Columbia. The creek flows into Kenny Creek. Tom Creek was discovered in 1869 by the Byrnes Party. The creek yielded gold for more than one hundred years. This creek has been mined for silver and gold. The creek has been mined using wing-damming and hand-mining by Europeans and Chinese miners.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: tom creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 55.61653
lon: -125.63668
Tom Creek. Tom Creek is a creek located in the Omineca Country region of British Columbia. The creek flows into Kenny Creek. Tom Creek was discovered in 1869 by the Byrnes Party. The creek yielded gold for more than one hundred years. This creek has been mined for silver and gold. The creek has been mined using wing-damming and hand-mining by Europeans and Chinese miners.

Geographic entities mentioned:
surface_form: tom creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 55.61653
lon: -125.63668