Sarmila/GeoWiki-Features huggingface dataset:
Eusebius makes mention of this twin site in his &quot;Onomasticon&quot;. The other ruin is situated on a hilltop overlooking the Elah Valley between Adullam and Azekah (), in the lower stratum of the Judaean foothills (grid position 147/121 PAL). Today it is a popular tourist attraction better known as Givat HaTurmusim.

Geographic entities mentioned:
surface_form: Elah Valley
instance_of: Valley
countries: Israel
coordinates: lat: 31.6806252
lon: 34.9891247
Antiquity. Although it is listed in as being a city in the plain, Socho is actually partly in the hill country and partly in the plain. The biblical account states that the Philistines encamped between Sokho and Azekah in the Valley of Elah before Goliath's historic encounter with David, the son of Jesse (). David slew the Philistine giant with a stone slung from a shepherd's sling.

Geographic entities mentioned:
surface_form: Valley of Elah
instance_of: Valley
countries: Israel
coordinates: lat: 31.6806252
lon: 34.9891247
Life and work. Gladkov was born in Kulbaki in Kursk Oblast where his father was a priest. He studied at Dmitriyev and worked in a local museum. In 1924 he went to the Aral Sea as a laboratory assistant of the Moscow Society of Naturalists. In 1926 he joined the physics and mathematics department of the Moscow State University and graduated in 1930.

Geographic entities mentioned:
surface_form: Aral Sea
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
It feeds on roots and tubers and lives underground in a burrow that it digs with its teeth. Distribution and habitat. The giant blind mole-rat is native to the North Caucasus, Chechnya, and southern Kalmykia located between the northern ends of the Caspian and Black Seas. It is restricted to a range of less than, and its distribution within that area is quite patchy.

Geographic entities mentioned:
surface_form: Caspian
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
After Ophir, the trail went southwest through the Kuskokwim Mountains to Iditarod. The trail went north from Iditarod through the now abandoned towns of Dikeman and Dishkaket and then northwest to the village of Kaltag. The trail then followed the long Kaltag Portage, an ancient native trading trail, to Unalakleet, on the Norton Sound.

Geographic entities mentioned:
surface_form: Norton Sound
instance_of: Landform
countries: United States
coordinates: lat: 63.849166666667
lon: -164.26888888889
Maláčová also campaigned at Metro stations giving out leaflets for the party. Free Bloc. The Free Bloc launched its campaign on 28 August 2021 with a meeting on Letná. Led by MP Lubomír Volný, it focused mainly on opposition to COVID-19 restrictions. Other prominent figures in their campaign were Jana Bobošíková and Hana Lipovská.

Geographic entities mentioned:
surface_form: Letná
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.0957
lon: 14.4165
There are two main seas in the North Indian Ocean – the Arabian Sea to the west of the Indian subcontinent, abbreviated &quot;ARB&quot; by the India Meteorological Department (IMD); and the Bay of Bengal to the east, abbreviated &quot;BOB&quot; by the IMD.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
El Paraíso, Peru. El Paraíso (, &quot;The Paradise&quot;) or Chuquitanta (Quechua &quot;chuqui&quot; lance or metal, &quot;tanta&quot; bread) are the moderns names of a Late Preceramic (3500–1800 BC) archaeological site located in the Chillón Valley on the central coast of Peru.

Geographic entities mentioned:
surface_form: Chillón
instance_of: Watercourse
countries: Peru
coordinates: lat: -11.938055555556
lon: -77.140277777778
Zgornji Tuhinj. Zgornji Tuhinj (;) is a village in the Tuhinj Valley in the Municipality of Kamnik in the Upper Carniola region of Slovenia. It lies above the central part of the upper Tuhinj Valley. Name. The settlement was first mentioned in documents dating 1213.

Geographic entities mentioned:
surface_form: Tuhinj Valley
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.221413888889
lon: 14.775925
The original road into the area was used for logging and mining. Years ago, they mined for gold, although that mine has been closed and dismantled. Active mining in the area is done around Bernic Lake by The Tanco Mining Company. The mine is an active producer of caesium, tantalum and spodumene.

Geographic entities mentioned:
surface_form: Bernic Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.4173
lon: -95.4362
Booster Lake. Booster Lake is located in Nopiming Provincial Park in the province of Manitoba, Canada. It is located inside the Canadian Shield, at an elevation of, approximately northeast of Lac Du Bonnet and sits about west from the Ontario border. Highway 315 runs north of the lake.

Geographic entities mentioned:
surface_form: booster lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.44524
lon: -95.26746
36 billion. The interchanges at Dadabhai, Industrial Valley, Nooriabad, and Thana Bola Khan, were to enable Tharparkar, Jimphir, Keenjhar, and other areas to be connected as well. On 3 February 2017, Prime Minister Nawaz Sharif inaugurated a completed section of the motorway from Loni Kot to Lucky toll plaza.

Geographic entities mentioned:
surface_form: Keenjhar
instance_of: Lake
countries: Pakistan
coordinates: lat: 24.95
lon: 68.05
Piz Vatgira, or more precisely a lower 2,981 metre-high summit 350 metres south of the main summit, lies exactly above the Gotthard Base Tunnel, at its deepest point. The tunnel, the longest and deepest in the world, runs below the ground. Piz Vatgira is the highest of the three main peaks above the base tunnel, the other two being the Chrüzlistock and Pizzo dell'Uomo.

Geographic entities mentioned:
surface_form: Chrüzlistock
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.7145
lon: 8.7408
surface_form: Pizzo dell'Uomo
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.544583333333
lon: 8.7771111111111
surface_form: chrüzlistock
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.7145
lon: 8.7408
surface_form: pizzo dell'uomo
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.544583333333
lon: 8.7771111111111
Piz Vatgira. Piz Vatgira () is a mountain of the Lepontine Alps and part of the extended Saint-Gotthard Massif, located south of Sedrun in the canton of Graubünden. The mountain lies between the valleys of Nalps and Medel, about halfway between Lai da Nalps and Lai da Sontga Maria. On its east side is a small glacier ending in the lake named &quot;Lai Verd&quot; (2,702 m).

Geographic entities mentioned:
surface_form: piz vatgira
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.606111111111
lon: 8.7708333333333
Due to the valley's generally mild climate, it is used as a region to grow pears, and there are multiple vineyards. Medford has, on average, 175 sunny days per year, compared to 80 on average for the Willamette Valley, and 65 on average for the coast.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
surface_form: willamette valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
The mild climate and relative isolation have made the valley a popular retirement destination. The community of Ashland is famous for the Oregon Shakespeare Festival and Mount Ashland Ski Area. Interstate 5 follows the valley through Ashland, Medford and Grants Pass. History.

Geographic entities mentioned:
surface_form: mount ashland
instance_of: Mountain
countries: United States
coordinates: lat: 42.080555555556
lon: -122.71722222222
The largest communities in the Rogue Valley are Medford, Ashland, and Grants Pass. The most populated part of the Rogue Valley is not along the Rogue proper, but along the smaller Bear Creek tributary. The valley forms a relatively isolated enclave west of the Cascade Range along the north side of the Siskiyou Mountains.

Geographic entities mentioned:
surface_form: bear creek
instance_of: Watercourse
countries: United States
coordinates: lat: 39.8305929
lon: -92.2301817
surface_form: rogue valley
instance_of: Valley
countries: United States
coordinates: lat: 42.440122222222
lon: -122.92615277778
Rogue Valley. The Rogue Valley is a valley region in southwestern Oregon in the United States. Located along the middle Rogue River and its tributaries in Josephine and Jackson counties, the valley forms the cultural and economic heart of Southern Oregon near the California border. The largest communities in the Rogue Valley are Medford, Ashland, and Grants Pass.

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 most populated part of the Rogue Valley is not along the Rogue proper, but along the smaller Bear Creek tributary. The valley forms a relatively isolated enclave west of the Cascade Range along the north side of the Siskiyou Mountains. It is separated from the nearby coast by a high section of the Southern Oregon Coast Range.

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 is separated from the nearby coast by a high section of the Southern Oregon Coast Range. The valley is characterized by a mild climate that allows a long growing season, especially for many varieties of fruits, nuts and herbs. A regional manufacturing industry is centered in Medford, the most highly populated area of the valley.

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 valley is characterized by a mild climate that allows a long growing season, especially for many varieties of fruits, nuts and herbs. A regional manufacturing industry is centered in Medford, the most highly populated area of the valley. In recent years the valley has emerged as a wine-growing region and it is the location of the Rogue Valley AVA (American Viticultural Area).

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
A regional manufacturing industry is centered in Medford, the most highly populated area of the valley. In recent years the valley has emerged as a wine-growing region and it is the location of the Rogue Valley AVA (American Viticultural Area). The mild climate and relative isolation have made the valley a popular retirement destination.

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
surface_form: rogue valley
instance_of: Valley
countries: United States
coordinates: lat: 42.440122222222
lon: -122.92615277778
In recent years the valley has emerged as a wine-growing region and it is the location of the Rogue Valley AVA (American Viticultural Area). The mild climate and relative isolation have made the valley a popular retirement destination. The community of Ashland is famous for the Oregon Shakespeare Festival and Mount Ashland Ski Area.

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 mild climate and relative isolation have made the valley a popular retirement destination. The community of Ashland is famous for the Oregon Shakespeare Festival and Mount Ashland Ski Area. Interstate 5 follows the valley through Ashland, Medford and Grants Pass. 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
Interstate 5 follows the valley through Ashland, Medford and Grants Pass. History. In the early 19th century, the first European Americans began to pass through the valley, inhabited by the Shasta, Takelma, and Rogue River Athabaskan tribes of Native Americans. The early fur traders named this river the &quot;River of the Rogues&quot;.

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
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
The early fur traders named this river the &quot;River of the Rogues&quot;. White settlers began to arrive in the valley after the Donation Land Act, which allocated of land to each married couple. Between 1836 and 1856, the valley was the scene of a series of bloody conflicts between European Americans and the Rogue River tribes.

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
White settlers began to arrive in the valley after the Donation Land Act, which allocated of land to each married couple. Between 1836 and 1856, the valley was the scene of a series of bloody conflicts between European Americans and the Rogue River tribes. In 1850, gold was discovered on the Rogue River; the next year gold was discovered in the nearby mountains.

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
During the gold rush, some $70 million was extracted from the area. Climate. Unlike the rest of Western Oregon, because of the rain shadow effect resulting from the close range of the Cascades and Siskiyous, the Rogue Valley is relatively dry when compared to the coast and Portland. Most of the valley has a hot-summer Mediterranean climate.

Geographic entities mentioned:
surface_form: rogue valley
instance_of: Valley
countries: United States
coordinates: lat: 42.440122222222
lon: -122.92615277778
Summers are hot and sunny, but dry, with low humidity. Temperatures surpass on an average of 10–15 days during the summer. Because of the combination of heat and dry air, wildfires are a problem during the summer, and frequently, smoke will fill up the valley for weeks, reducing visibility and air quality. On average, the first frost occurs October 22, and the last on May 6.

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 Rogue Valley is in USDA plant hardiness zones 7–9. Sub-zero temperatures are extremely rare in the valley; the Rogue Valley International-Medford Airport has not recorded such extreme cold weather since December 21, 1990, when the temperature dropped to. Due to the valley's generally mild climate, it is used as a region to grow pears, and there are multiple vineyards.

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: 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: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: rogue valley
instance_of: Valley
countries: United States
coordinates: lat: 42.440122222222
lon: -122.92615277778
Rogue Valley. The Rogue Valley is a valley region in southwestern Oregon in the United States. Located along the middle Rogue River and its tributaries in Josephine and Jackson counties, the valley forms the cultural and economic heart of Southern Oregon near the California border. The largest communities in the Rogue Valley are Medford, Ashland, and Grants Pass.

Geographic entities mentioned:
surface_form: rogue valley
instance_of: Valley
countries: United States
coordinates: lat: 42.440122222222
lon: -122.92615277778
Located along the middle Rogue River and its tributaries in Josephine and Jackson counties, the valley forms the cultural and economic heart of Southern Oregon near the California border. The largest communities in the Rogue Valley are Medford, Ashland, and Grants Pass. The most populated part of the Rogue Valley is not along the Rogue proper, but along the smaller Bear Creek tributary.

Geographic entities mentioned:
surface_form: rogue valley
instance_of: Valley
countries: United States
coordinates: lat: 42.440122222222
lon: -122.92615277778
Jach'a Pata (Larecaja). Jach'a Pata (Aymara &quot;jach'a&quot; big, &quot;pata&quot; step, &quot;big step&quot;, Hispanicized spelling &quot;Jachcha Pata&quot;) is a mountain in the Cordillera Real in the Andes of Bolivia, about high. It is situated in the La Paz Department, Larecaja Province, in the south of the Guanay Municipality.

Geographic entities mentioned:
surface_form: jach'a pata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.1
lon: -68.2197
surface_form: jach'a pata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.0572
lon: -68.3419
It is situated in the La Paz Department, Larecaja Province, in the south of the Guanay Municipality. Jach'a Pata lies north-west of the mountain Janq'u K'ark'a and south of the lake Qutapata &quot;(Kkota Pata)&quot;.

Geographic entities mentioned:
surface_form: janq'u k'ark'a
instance_of: Mountain
countries: Bolivia
coordinates: lat: -15.9156
lon: -68.5486
surface_form: qutapata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.5353
lon: -67.8458
surface_form: janq'u k'ark'a
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.1114
lon: -68.2175
St. Martin in Passeier. St. Martin in Passeier (;) is a &quot;comune&quot; (municipality) and a village in the Passeier Valley in South Tyrol, northern Italian, located about northwest of Bolzano. Geography. As of 30 November 2010, it had a population of 3,137 and an area of.

Geographic entities mentioned:
surface_form: Passeier Valley
instance_of: Valley
countries: Italy
coordinates: lat: 46.766666666667
lon: 11.216666666667
Mount Finley. Mount Finley () is a prominent mountain, high, on the ridge which extends south from Mount Wade, located south-southwest of Mount Oliver in the Queen Maud Mountains. Mount Finley was named by Rear Admiral Byrd for John H. Finley, President of the American Geographical Society at the time of the Byrd Antarctic Expedition 1928-30. Nearby features.

Geographic entities mentioned:
surface_form: Mount Wade
instance_of: Mountain
coordinates: lat: -84.85
lon: -174.31666666667
surface_form: mount oliver
instance_of: Mountain
coordinates: lat: -84.93499667
lon: -173.73416333
surface_form: oliver
instance_of: Mountain
coordinates: lat: -84.93499667
lon: -173.73416333
surface_form: mount finley
instance_of: Mountain
coordinates: lat: -85.01000333
lon: -173.94000333
surface_form: finley
instance_of: Mountain
coordinates: lat: -85.01000333
lon: -173.94000333
Simplicity Hill. A small ice-free hill rising west of Crilly Hill, at the north side of McGregor Glacier. So named by the Texas Tech Shackleton Glacier Expedition (1964-65) because of the ease with which they were able to approach the feature, and because of the relative simplicity of its geologic nature. Crilly Hill.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
Crilly, medic with the U.S. Army Aviation Detachment which supported the expedition. Keel Hill. A small ice-free hill, standing at the north side of McGregor Glacier, about east of Crilly Hill, in the Queen Maud Mountains. Named by the Texas Tech Shackleton Glacier Expedition (1964-65) for Specialist 5th Class Elbert E. Keel, member of the U.S.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
Army Aviation Detachment which supported the expedition. Pendant Ridge. A ridge about long, extending southwest to the north side of the mouth of McGregor Glacier, northwest of Simplicity Hill. So named by the Texas Tech Shackleton Glacier Expedition (1964 65) because a pyramidal peak at its southern extremity appears to be dangling from the ridge as a pendant. Simplicity Hill.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
Nearby features. Mount Finley is in the northeast of a massif that is bounded by the Yeats Glacier to the north and the McGregor Glacier to the south, both tributaries of the Shackleton Glacier to the west. Other features of the massif, from west to east, are Lockhart Ridge, Pendant Ridge, Simplicity Hill, Crilly Hill, Keel Hill and Bynam Peak. Lockhart Ridge.

Geographic entities mentioned:
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
surface_form: mount finley
instance_of: Mountain
coordinates: lat: -85.01000333
lon: -173.94000333
surface_form: finley
instance_of: Mountain
coordinates: lat: -85.01000333
lon: -173.94000333
Other features of the massif, from west to east, are Lockhart Ridge, Pendant Ridge, Simplicity Hill, Crilly Hill, Keel Hill and Bynam Peak. Lockhart Ridge. A conspicuous ridge about long, extending west along the south side of Yeats Glacier and terminating at Shackleton Glacier. Named by the Texas Tech Shackleton Glacier Expedition (1964-65) for CWO James J. Lockhart, pilot with the U.S.

Geographic entities mentioned:
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
Lockhart Ridge. A conspicuous ridge about long, extending west along the south side of Yeats Glacier and terminating at Shackleton Glacier. Named by the Texas Tech Shackleton Glacier Expedition (1964-65) for CWO James J. Lockhart, pilot with the U.S. Army Aviation Detachment which supported the expedition. Pendant Ridge.

Geographic entities mentioned:
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
Simplicity Hill. A small ice-free hill rising west of Crilly Hill, at the north side of McGregor Glacier. So named by the Texas Tech Shackleton Glacier Expedition (1964-65) because of the ease with which they were able to approach the feature, and because of the relative simplicity of its geologic nature. Crilly Hill.

Geographic entities mentioned:
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
Crilly Hill. The central of three ice-free hills at the north side of McGregor Glacier, south-southwest of Mount Finley. Named by the Texas Tech Shackleton Glacier Expedition (1964-65) for Specialist 6th Class Clifford L. Crilly, medic with the U.S. Army Aviation Detachment which supported the expedition. Keel Hill.

Geographic entities mentioned:
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
Army Aviation Detachment which supported the expedition. Keel Hill. A small ice-free hill, standing at the north side of McGregor Glacier, about east of Crilly Hill, in the Queen Maud Mountains. Named by the Texas Tech Shackleton Glacier Expedition (1964-65) for Specialist 5th Class Elbert E. Keel, member of the U.S. Army Aviation Detachment which supported the expedition. Bynum Peak.

Geographic entities mentioned:
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
Mount Finley. Mount Finley () is a prominent mountain, high, on the ridge which extends south from Mount Wade, located south-southwest of Mount Oliver in the Queen Maud Mountains. Mount Finley was named by Rear Admiral Byrd for John H. Finley, President of the American Geographical Society at the time of the Byrd Antarctic Expedition 1928-30. Nearby features.

Geographic entities mentioned:
surface_form: mount finley
instance_of: Mountain
coordinates: lat: -85.01000333
lon: -173.94000333
surface_form: finley
instance_of: Mountain
coordinates: lat: -85.01000333
lon: -173.94000333
Crilly Hill. The central of three ice-free hills at the north side of McGregor Glacier, south-southwest of Mount Finley. Named by the Texas Tech Shackleton Glacier Expedition (1964-65) for Specialist 6th Class Clifford L. Crilly, medic with the U.S. Army Aviation Detachment which supported the expedition. Keel Hill.

Geographic entities mentioned:
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Keel, member of the U.S. Army Aviation Detachment which supported the expedition. Bynum Peak. A rock peak southeast of Mount Finley, overlooking the north side of McGregor Glacier in the Queen Maud Mountains. Named by US-ACAN for Gaither D. Bynum, USARP satellite geodesist at McMurdo Station, winter 1965.

Geographic entities mentioned:
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Mount Finley. Mount Finley () is a prominent mountain, high, on the ridge which extends south from Mount Wade, located south-southwest of Mount Oliver in the Queen Maud Mountains. Mount Finley was named by Rear Admiral Byrd for John H. Finley, President of the American Geographical Society at the time of the Byrd Antarctic Expedition 1928-30. Nearby features.

Geographic entities mentioned:
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Its core territory was the fertile land along the lower Zarafshon river, and its urban centres were the ancient cities of Samarqand and the emirate's capital, Bukhara. It was contemporaneous with the Khanate of Khiva to the west, in Khwarazm, and the Khanate of Kokand to the east, in Fergana. In 1920, it ceased to exist with the establishment of the Bukharan People's Soviet Republic.

Geographic entities mentioned:
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countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
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There are two major dams along the river. The first one is Moose Mountain Dam and the second is Grant Devine Dam, both of which created large reservoirs along the course. Both reservoirs have parks; Lost Horse Hills is on Moose Mountain Lake and Moose Creek Regional Park is on Grant Devine Reservoir. Course. The Chapleau Lakes are a chain of two lakes that run diagonally in a valley north to east.

Geographic entities mentioned:
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From the outflow of that lake near Highway 48 and Highway 606, the river travels in a south-easterly direction until passes through the Saint Clair National Wildlife Area and Highway 711. From there, it empties into Moose Mountain Lake, which is a man-made reservoir. Moose Mountain Dam, which was built in 1937, is at the south-east corner of the lake, near Lost Horse Hill.

Geographic entities mentioned:
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Moose Mountain Creek. Moose Mountain Creek is a river in the Canadian province of Saskatchewan. Its source is the Chapleau Lakes near Montmartre and it is a tributary of the Souris River, which, in turn, is a tributary of the Assiniboine River.

Geographic entities mentioned:
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Saint Clair National Wildlife Area () is one of 27 Prairie National Wildlife Areas in Saskatchewan. The park is at the northern end of Moose Mountain Lake, on the north side of Highway 711, about three miles west of the Highway 47 and 711 intersection. Moose Mountain Creek cuts through the park from the north-east to the south-west corner at which point it goes under Highway 711 and into the lake.

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Moose Mountain Creek. Moose Mountain Creek is a river in the Canadian province of Saskatchewan. Its source is the Chapleau Lakes near Montmartre and it is a tributary of the Souris River, which, in turn, is a tributary of the Assiniboine River.

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states. It is also within Palliser's Triangle and the Great Plains ecoregion. The entirety of Moose Mountain Creek is in Census Division No. 1. The river passes through two Indian reserves, Ocean Man and Pheasant Rump, and eight rural municipalities: Montmartre, Chester, Golden West, Tecumseh, Brock, Moose Mountain, Moose Creek, and Enniskillen.

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1. The river passes through two Indian reserves, Ocean Man and Pheasant Rump, and eight rural municipalities: Montmartre, Chester, Golden West, Tecumseh, Brock, Moose Mountain, Moose Creek, and Enniskillen. While there are no communities along the banks of the river, there are four within two kilometres of its banks: Montmartre, Kisbey, Alameda, and Oxbow.

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While there are no communities along the banks of the river, there are four within two kilometres of its banks: Montmartre, Kisbey, Alameda, and Oxbow. The original location of Carlyle, NW 26-07-03 W2, was located near confluence of Moose Mountain, Swift, and Morrison Creeks.

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The original location of Carlyle, NW 26-07-03 W2, was located near confluence of Moose Mountain, Swift, and Morrison Creeks. Moose Mountain Creek flows generally in a south-easterly direction, starting north-west of Moose Mountain Upland and ending up at the Souris River near Oxbow.

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Moose Mountain Creek flows generally in a south-easterly direction, starting north-west of Moose Mountain Upland and ending up at the Souris River near Oxbow. The western and southern regions of Moose Mountain fall within the river's watershed, which is part of the Upper Souris watershed.

Geographic entities mentioned:
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coordinates: lat: 51.4677778
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The western and southern regions of Moose Mountain fall within the river's watershed, which is part of the Upper Souris watershed. The northern most point of Moose Mountain Creek's watershed is near McLean, which is only away from Saskatchewan's capital, Regina. There are two major dams along the river.

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There are two major dams along the river. The first one is Moose Mountain Dam and the second is Grant Devine Dam, both of which created large reservoirs along the course. Both reservoirs have parks; Lost Horse Hills is on Moose Mountain Lake and Moose Creek Regional Park is on Grant Devine Reservoir. Course. The Chapleau Lakes are a chain of two lakes that run diagonally in a valley north to east.

Geographic entities mentioned:
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coordinates: lat: 51.4677778
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Course. The Chapleau Lakes are a chain of two lakes that run diagonally in a valley north to east. The northern most of the two lakes is the source of Moose Mountain Creek. From the outflow of that lake near Highway 48 and Highway 606, the river travels in a south-easterly direction until passes through the Saint Clair National Wildlife Area and Highway 711.

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From the outflow of that lake near Highway 48 and Highway 606, the river travels in a south-easterly direction until passes through the Saint Clair National Wildlife Area and Highway 711. From there, it empties into Moose Mountain Lake, which is a man-made reservoir. Moose Mountain Dam, which was built in 1937, is at the south-east corner of the lake, near Lost Horse Hill.

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Dykes and culverts were built south of Kisbey to protect the village and control the river's flow. South of Forget, there were also culverts and other flood control measures built to control surface water before it reaches the river. From south of Kisbey, the river roughly parallels Highway 13 towards Arcola where it leaves the floodplain and flows into a valley, the Moose Mountain Creek Spillway.

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It continues east until it crosses Highway 9, at which point it takes a more southerly route and flows into a Grant Devine Reservoir. In 1994, the Alameda Dam was built along Moose Mountain Creek's course, near the point where it meets the Souris River, creating a large reservoir called Alameda Reservoir.

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In 2017, the name of the reservoir and dam were changed to Grant Devine Dam and Grant Devine Reservoir, in honour of the premier of Saskatchewan who was responsible for its construction, Grant Devine. Moose Mountain Creek is the primary inflow and outflow of the reservoir and meets the Souris River about three miles south of the dam in the Souris River Valley, near the town of Oxbow.

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Moose Mountain Creek is the primary inflow and outflow of the reservoir and meets the Souris River about three miles south of the dam in the Souris River Valley, near the town of Oxbow. Moose Mountain Creek Spillway.

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Moose Mountain Creek Spillway. Moose Mountain Creek Spillway is a valley that was formed during the last ice age as the path taken by melting glacial waters between two glacial lobes, the Weyburn Lobe and the Moose Mountain Lobe, en route to the Souris Spillway.

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On the southern side of Moose Mountain Upland, in the interlobate area, a short lived glacial lake named Lake Arcola formed along the current path of Moose Mountain Creek. Glacial moraines can be found throughout the area. Saint Clair National Wildlife Area. Saint Clair National Wildlife Area () is one of 27 Prairie National Wildlife Areas in Saskatchewan.

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Saint Clair National Wildlife Area () is one of 27 Prairie National Wildlife Areas in Saskatchewan. The park is at the northern end of Moose Mountain Lake, on the north side of Highway 711, about three miles west of the Highway 47 and 711 intersection. Moose Mountain Creek cuts through the park from the north-east to the south-west corner at which point it goes under Highway 711 and into the lake.

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Moose Mountain Creek cuts through the park from the north-east to the south-west corner at which point it goes under Highway 711 and into the lake. It is about one square mile in size and sits in the valley at the confluence of Moose Mountain and an unnamed creek that comes in from the west.

Geographic entities mentioned:
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Weber is the former Artistic Director for the Jean Will Presents concert series at the California Center for the Arts, Escondido, California. As a classical pianist Weber has performed internationally as well as in the U.S.

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coordinates: lat: 34.155833333333334
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Mount McBride is one of two peaks in British Columbia named for BC Premier Sir Richard McBride. The other is Mount Sir Richard. There is a second Mount McBride—named for Captain Kenneth Gilbert McBride of The Seaforth Highlanders of Canada, a Canadian officer killed in action during the Second World War—elsewhere in BC and yet another in the Yukon.

Geographic entities mentioned:
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coordinates: lat: 49.9639
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