Sarmila/GeoWiki-Features huggingface dataset:
Boundary Bald Mountain. Boundary Bald Mountain is a mountain located in Somerset County, Maine, about southeast of the Canada–US border with Quebec. Boundary Bald Mountain is flanked to the east by Ironbound Mountain, and to the west by Sandy Bay Mountain.

Geographic entities mentioned:
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.655
lon: -114.409
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.8827026
lon: -88.0390147
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.8822
lon: -123.866
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6611024
lon: -107.4103338
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.4291
lon: -75.7503
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.6988
lon: -110.902
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.021388888889
lon: -75.190833333333
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.5344
lon: -119.115
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.423611111111
lon: -74.593888888889
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1209
lon: -74.2001
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.902777777778
lon: -74.724444444444
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.4439
lon: -105.969
surface_form: boundary bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.7668
lon: -70.2038
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7386
lon: -74.9129
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.294722222222
lon: -74.387777777778
Boundary Bald Mountain is flanked to the east by Ironbound Mountain, and to the west by Sandy Bay Mountain. The north side of Boundary Bald Mountain drains via Alder Brook, Fish Brook, and Hale Brook (east to west) into the South Branch of the Penobscot River, then into the West Branch, the main stem of the Penobscot, and into Penobscot Bay.

Geographic entities mentioned:
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.655
lon: -114.409
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.8827026
lon: -88.0390147
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.8822
lon: -123.866
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6611024
lon: -107.4103338
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.4291
lon: -75.7503
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.6988
lon: -110.902
surface_form: west branch
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.021388888889
lon: -75.190833333333
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.5344
lon: -119.115
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.423611111111
lon: -74.593888888889
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1209
lon: -74.2001
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.902777777778
lon: -74.724444444444
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.4439
lon: -105.969
surface_form: boundary bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.7668
lon: -70.2038
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7386
lon: -74.9129
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.294722222222
lon: -74.387777777778
The south side of Boundary Bald Mountain drains via Churchill Stream, Upper Churchill Stream, and Heald Stream (east to west) into the Moose River, then into the Kennebec River, and into the Gulf of Maine.

Geographic entities mentioned:
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.655
lon: -114.409
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.8827026
lon: -88.0390147
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.8822
lon: -123.866
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6611024
lon: -107.4103338
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.4291
lon: -75.7503
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.6988
lon: -110.902
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.021388888889
lon: -75.190833333333
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.5344
lon: -119.115
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.423611111111
lon: -74.593888888889
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1209
lon: -74.2001
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.902777777778
lon: -74.724444444444
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.4439
lon: -105.969
surface_form: boundary bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.7668
lon: -70.2038
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7386
lon: -74.9129
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.294722222222
lon: -74.387777777778
A number of minerals, including lithium, are dissolved in the lakes. Location. Pastos Grandes lies in the Sud Lipez Region of Bolivia. Geographically the area is part of the Altiplano, a high plateau bordered by the Cordillera Occidental and the Cordillera Oriental. The Altiplano contains two large salt pans, the Salar de Uyuni and Salar de Coipasa.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
but is apparently unrelated to the caldera. Cerro Chascon-Runtu Jarita is less than 100,000 years old according to argon-argon dating. This and ongoing geothermal manifestations suggest that volcanic activity may still occur at Pastos Grandes. Finally, Pastos Grandes and Cerro Guacha may be the heat source for the El Tatio geothermal field west of Pastos Grandes. Lake.

Geographic entities mentioned:
surface_form: Cerro Guacha
instance_of: Mountain
countries: Bolivia
coordinates: lat: -22.75
lon: -67.46666667
surface_form: El Tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
state of Missouri. The population was 61 at the 2020 census. The community is on US Route 169 four miles north of Trimble and approximately six miles west-southwest of Plattsburg. The Smithville Reservoir on the Little Platte River is about 3.5 miles to the east. History. Grayson was platted in 1871, and named after the maiden name of the wife of the original owner of the town site.

Geographic entities mentioned:
surface_form: Smithville Reservoir
instance_of: Lake
countries: United States
coordinates: lat: 39.402377777778
lon: -94.532888888889
In 2015 he set sights on the world record for highest elevation cycled. He chose Broad Peak as the place for this attempt as it provided flat enough terrain to ride the required 20m for the record. While he was hiking up the 12th highest mountain in the world he slipped on some ice and fell down the hill but was able to use his ice pick to stop himself.

Geographic entities mentioned:
surface_form: Broad Peak
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.810555555556
lon: 76.568055555556
The majority of its coastline is part of the Jurassic Coast World Heritage Site due to its geological and palaeontologic significance, and features notable landforms such as Lulworth Cove, the Isle of Portland, Chesil Beach and Durdle Door. The north of the county contains part of Cranborne Chase, a chalk downland. The highest point in Dorset is Lewesdon Hill (), in the southwest.

Geographic entities mentioned:
surface_form: Cranborne Chase
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 50.961419444444
lon: -2.0440888888889
The other two major settlements in the county are Dorchester, which has been the county town since at least 1305, and Weymouth, a major seaside resort since the 18th century. Blandford Forum, Sherborne, Gillingham, Shaftesbury and Sturminster Newton are historic market towns which serve the farms and villages of the Blackmore Vale in north Dorset.

Geographic entities mentioned:
surface_form: Blackmore Vale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 50.94
lon: -2.31
These limestone areas include a wide band of Cretaceous chalk which crosses the county as a range of hills from north-east to south-west, incorporating Cranborne Chase and the Dorset Downs, and a narrow band running from south-west to south-east, incorporating the Purbeck Hills. Between the chalk hills are large, wide vales and wide flood plains.

Geographic entities mentioned:
surface_form: Cranborne Chase
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 50.961419444444
lon: -2.0440888888889
Between the chalk hills are large, wide vales and wide flood plains. These vales are dotted with small villages, farms and coppices, and include the Blackmore Vale (Stour valley) and the Frome valley. The Blackmore Vale is composed of older Jurassic deposits, largely clays interspersed with limestones, and has traditionally been a centre for dairy agriculture.

Geographic entities mentioned:
surface_form: Frome valley
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 50.6958
lon: -1.98861
In the west this results in a hilly landscape of diverse character that resembles that of neighbouring county Devon. Marshwood Vale, a valley of Lower Lias clay at the western tip of the county, lies to the south of the two highest points in Dorset: Lewesdon Hill at and Pilsdon Pen at.

Geographic entities mentioned:
surface_form: Marshwood Vale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 50.78
lon: -2.83
Elbriot. Elbriot (&quot;Elbe riot&quot;) is an annual open air music festival in Hamburg, Germany, which features heavy metal and hardcore punk bands. It is organized by &quot;Hamburg Konzerte&quot; agency. History. The festival takes place on the compound of the Hamburg Wholesale Market. The first edition of the festival was sold out completely in a very short time with 14,000 tickets.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
He started working early where the activity he liked to do most was carry the bags of travelers arriving in the city, from the train station to the central hotel. In early adulthood he looked for better job opportunities in larger cities in the Paraíba Valley, such as Itajubá, Campos do Jordão, and São José dos Campos.

Geographic entities mentioned:
surface_form: Paraíba Valley
instance_of: Valley
countries: Brazil
coordinates: lat: -22.75
lon: -45.15
She married Robert McChesney in December 1949; they lived in the North Bay area. They moved to Sonoma Mountain in Sonoma County near Petaluma, California in 1952, after living in Mexico for a year, and lived and worked there through Robert McChesney's death in 2008, after which Mary remained there, continuing to work, until the late 2010s.

Geographic entities mentioned:
surface_form: Sonoma Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.3231
lon: -122.575
In 1881 Luschan and Otto Benndorf explored the ancient Lycian region of southern Anatolia, part of the Ottoman Empire, where they excavated the Heroon of Trysa near Myra, which is now on display at the Vienna Kunsthistorisches Museum. In February 1883 he accompanied Carl Humann on an expedition to Mount Nemrut in historic Commagene which was initiated by the Prussian Academy of Sciences.

Geographic entities mentioned:
surface_form: Mount Nemrut
instance_of: Mountain
countries: Turkey
coordinates: lat: 37.98073888888889
lon: 38.740830555555554
Arabia Mountain High School. Arabia Mountain High School Academy of Engineering Medicine and Environmental Studies is located on the edge of the Arabia Mountain green space in Stonecrest, Georgia, United States, with a Lithonia post office address. This public high school opened in August 2009.

Geographic entities mentioned:
surface_form: Arabia Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.665
lon: -84.1183
The Germans began to withdraw on 17–19 August, and the Allies linked up in Chambois. Gaps were forced in the Allied lines by German counter-attacks, the biggest being a corridor forced past the 1st Polish Armored Division on Hill 262, a commanding position at the mouth of the pocket. By the evening of 21 August, the pocket had been sealed, with c. 50,000 Germans trapped inside.

Geographic entities mentioned:
surface_form: Hill 262
instance_of: Mountain
countries: France
coordinates: lat: 48.84194444
lon: 0.15805556
Operation Dragoon. On 15 August 1944, the US 7th Army, spearheaded by the 3rd Infantry Division and 36th Infantry Division and other Allied forces landed in southern France between Cannes and Hyères. Their aim was to secure the southern half of France and in particular to capture Marseille as the main supply harbor for the Allies in France.

Geographic entities mentioned:
surface_form: Hyères
instance_of: Mountain
countries: France
coordinates: lat: 43.118888888889
lon: 6.1286111111111
Learning from the Battle of Saipan they prepared many fortified positions on the island, including pillboxes and tunnels. The Marines attack began on 19 February 1945. Initially the Japanese put up no resistance, letting the Americans mass, creating more targets before the Americans took intense fire from Mount Suribachi and fought throughout the night until the hill was surrounded.

Geographic entities mentioned:
surface_form: Mount Suribachi
instance_of: Mountain
countries: Japan
coordinates: lat: 24.749030555556
lon: 141.28778333333
In October 1534, a Muscovite army under the command of Prince Ovchina-Telepnev-Obolensky, Prince Nikita Obolensky, and Prince Vasily Shuisky invaded Lithuania, advancing as far as Vilnius and Naugardukas, and built a fortress on Lake Sebezh the following year, before being stopped.

Geographic entities mentioned:
surface_form: Lake Sebezh
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 56.266666666667
lon: 28.5
Most of the outdoor sequences were filmed at Aurahi Hingna, Araria district in Bihar and Bina, a town near Bhopal, Madhya Pradesh. A few scenes were filmed at Powai Lake and at Mohan Studios in Mumbai. A set of Gulababag fair's The Great Bharat &quot;nautanki&quot; (drama) company was created in Mumbai studio.

Geographic entities mentioned:
surface_form: Powai Lake
instance_of: Lake
countries: India
coordinates: lat: 19.13
lon: 72.91
Santa Giustina. Santa Giustina is a &quot;comune&quot; (municipality) in the province of Belluno in the Italian region of Veneto, located about northwest of Venice and about southwest of Belluno. Santa Giustina borders the following municipalities: Cesiomaggiore, Lentiai, Mel, San Gregorio nelle Alpi, Sedico, Sospirolo. Mount Pizzocco is located nearby.

Geographic entities mentioned:
surface_form: Pizzocco
instance_of: Mountain
countries: Italy
coordinates: lat: 46.11555556
lon: 12.03361111
History. The city is named after Huntsville, Alabama, the hometown of some early settlers. Huntsville incorporated as a town after the Civil War in 1877. The community was incorporated as a city on July 16, 1925. Geography. Huntsville is located north of the center of Madison County in the northwest part of the Arkansas Ozarks. Via U.S. Route 412 it is east of Springdale and west of Harrison.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
Port au Saumon River. The Port-au-Saumon River is a tributary of the northwest shore of the St. Lawrence River, flowing into the town of La Malbaie, into the Charlevoix-Est Regional County Municipality, in the Capitale-Nationale administrative region, Quebec, Canada. The course of this river flows into the St. Lawrence River in the hamlet of Port-au-Saumon, northeast of the town of La Malbaie.

Geographic entities mentioned:
surface_form: port au saumon river
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.755277777778
lon: -69.953611111111
The resort is developed around the northern appendage of the lake. The mouth of the lake is at the bottom of the eastern appendage. Upper part of the Port au Saumon River (segment of)
Lower part of the Port au Saumon River (segment of)
Toponymy. The French toponym &quot;Port-au-Saumon&quot; is linked to the bay, the hamlet, the river and the lake.

Geographic entities mentioned:
surface_form: port au saumon river
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.755277777778
lon: -69.953611111111
Lawrence River and by the road of the rang Sainte-Anne. The &quot;chemin des érables&quot; and Port-au-Saumon Lake Road serve the upper reaches of this stream. Forestry is the main economic activity of the sector; recreational and tourism activities (including vacationing around Lac au Saumon), second. The surface of this stream is generally frozen from mid-December to late-March.

Geographic entities mentioned:
surface_form: lac au saumon
instance_of: Lake
countries: Canada
coordinates: lat: 48.42
lon: -67.33
It is one of the driest places on Earth, though there are several anecdotal accounts of rainfall within the Dry Valleys. The region is one of the world's most extreme deserts, and includes many features including Lake Vida, a saline lake, and the Onyx River, a meltwater stream and Antarctica's longest river.

Geographic entities mentioned:
surface_form: Lake Vida
instance_of: Lake
coordinates: lat: -77.38888888888889
lon: 161.92777805555556
surface_form: vida
instance_of: Lake
coordinates: lat: -77.38888888888889
lon: 161.92777805555556
Geology. The McMurdo Oasis constitutes approximately of &quot;deglaciated mountainous desert&quot;, according to McKelvey, bounded by the coastline of south Victoria Land and the Polar Plateau. The Taylor and Wright Valleys are major ice-free valleys within the Transantarctic Mountains.

Geographic entities mentioned:
surface_form: Taylor
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
surface_form: Wright Valley
instance_of: Valley
coordinates: lat: -77.166666666667
lon: 161.83333333333
Irish and American researchers conducted a field expedition in 2013 to University Valley in order to examine the microbial population and to test a drill designed for sampling on Mars in the permafrost of the driest parts of the valleys, the areas most analogous to the Martian surface.

Geographic entities mentioned:
surface_form: University Valley
instance_of: Valley
coordinates: lat: -77.8667
lon: 160.667
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
Part of the Valleys was designated an environmentally protected area in 2004. Valleys. From north to south, the three main valleys are
West of Victoria Valley are, from north to south,
Lakes. Some of the lakes of the Dry Valleys rank among the world's most saline lakes, with a higher salinity than Lake Assal or the Dead Sea. The most saline of all is small Don Juan Pond.

Geographic entities mentioned:
surface_form: Don Juan Pond
instance_of: Lake
countries: New Zealand
coordinates: lat: -77.562277777778
lon: 161.19116666667
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: pond
instance_of: Mountain
coordinates: lat: -62.95
lon: -60.55
This contributes to the low humidity of the area. For several weeks in the summer, the temperature increases enough to allow for glacial melt, which causes small freshwater streams to form. These streams feed the lakes at the base of the valleys, which do not have outflow to the sea, causing them to become highly saline. Geology.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
Part of the Valleys was designated an environmentally protected area in 2004. Valleys. From north to south, the three main valleys are
West of Victoria Valley are, from north to south,
Lakes. Some of the lakes of the Dry Valleys rank among the world's most saline lakes, with a higher salinity than Lake Assal or the Dead Sea. The most saline of all is small Don Juan Pond.

Geographic entities mentioned:
surface_form: victoria valley
instance_of: Valley
coordinates: lat: -77.383333333333
lon: 161.93333333333
They found no living organisms in the permafrost, the first location on the planet visited by humans with no active microbial life. In 2014, drones were used in the McMurdo Dry Valleys by a team of scientists from Auckland University of Technology (AUT) to create baseline maps of the vegetation.

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
Although no living organisms have been found in the permafrost here, endolithic photosynthetic bacteria have been found living in the relatively moist interior of rocks, and anaerobic bacteria, with a metabolism based on iron and sulfur, live under the Taylor Glacier. The valleys are located within the McMurdo Valleys Antarctic Specially Managed Area (ASMA-2). Climate.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
Geology. The McMurdo Oasis constitutes approximately of &quot;deglaciated mountainous desert&quot;, according to McKelvey, bounded by the coastline of south Victoria Land and the Polar Plateau. The Taylor and Wright Valleys are major ice-free valleys within the Transantarctic Mountains.

Geographic entities mentioned:
surface_form: polar plateau
instance_of: Plateau
coordinates: lat: -90
lon: 0
The basement complex is overlain by the Jurassic Beacon Supergroup, which is itself intruded by Ferrar Dolerite sheets and sills. The McMurdo Volcanic Group intrudes, or is interbedded with, the Taylor and Wright Valleys' moraines as basaltic cinder cones and lava flows. These basalts have ages between 2.1 and 4.4 Ma.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
These basalts have ages between 2.1 and 4.4 Ma. The Dry Valley Drilling Project (1971–75) determined the Pleistocene layer within the Taylor Valley was between 137 and 275 m thick, and composed of interbedded sandstones, pebble conglomerates, and laminated silty mudstones. This Pleistocene layer disconformably overlies Pliocene and Miocene diamictites. Life.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
Summer meltwater from the glaciers provides the primary source of soil nutrients. Scientists consider the Dry Valleys perhaps the closest of any terrestrial environment to the planet Mars, and thus an important source of insights into possible extraterrestrial life. Anaerobic bacteria whose metabolism is based on iron and sulfur live in sub-freezing temperatures under the Taylor Glacier.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
McMurdo Dry Valleys. The McMurdo Dry Valleys are a row of largely snow-free valleys in Antarctica, located within Victoria Land west of McMurdo Sound. The Dry Valleys experience extremely low humidity and surrounding mountains prevent the flow of ice from nearby glaciers. The rocks there are granites and gneisses, and glacial tills dot this bedrock landscape, with loose gravel covering the ground.

Geographic entities mentioned:
surface_form: dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
surface_form: mcmurdo dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
McMurdo Dry Valleys. The McMurdo Dry Valleys are a row of largely snow-free valleys in Antarctica, located within Victoria Land west of McMurdo Sound. The Dry Valleys experience extremely low humidity and surrounding mountains prevent the flow of ice from nearby glaciers. The rocks there are granites and gneisses, and glacial tills dot this bedrock landscape, with loose gravel covering the ground.

Geographic entities mentioned:
surface_form: dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
The Dry Valleys experience extremely low humidity and surrounding mountains prevent the flow of ice from nearby glaciers. The rocks there are granites and gneisses, and glacial tills dot this bedrock landscape, with loose gravel covering the ground. It is one of the driest places on Earth, though there are several anecdotal accounts of rainfall within the Dry Valleys.

Geographic entities mentioned:
surface_form: dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
The valleys are located within the McMurdo Valleys Antarctic Specially Managed Area (ASMA-2). Climate. The Dry Valleys are so named because of their extremely low humidity and lack of snow or ice cover. They are also dry because, in this location, the mountains are sufficiently high that they block seaward-flowing ice from the East Antarctic Ice Sheet from reaching the Ross Sea.

Geographic entities mentioned:
surface_form: dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
The valley floors are covered with loose gravel, in which ice wedge polygonal patterned ground may be observed. The unique conditions in the Dry Valleys are caused, in part, by katabatic winds; these occur when cold, dense air is pulled downhill by the force of gravity. The dry wind evaporates the snow rapidly and little melts into the soil. During the summer, this process can take only hours.

Geographic entities mentioned:
surface_form: dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
This Pleistocene layer disconformably overlies Pliocene and Miocene diamictites. Life. Endolithic bacteria have been found living in the Dry Valleys, sheltered from the dry air in the relatively moist interior of rocks. Summer meltwater from the glaciers provides the primary source of soil nutrients.

Geographic entities mentioned:
surface_form: dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
Summer meltwater from the glaciers provides the primary source of soil nutrients. Scientists consider the Dry Valleys perhaps the closest of any terrestrial environment to the planet Mars, and thus an important source of insights into possible extraterrestrial life. Anaerobic bacteria whose metabolism is based on iron and sulfur live in sub-freezing temperatures under the Taylor Glacier.

Geographic entities mentioned:
surface_form: dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
They found no living organisms in the permafrost, the first location on the planet visited by humans with no active microbial life. In 2014, drones were used in the McMurdo Dry Valleys by a team of scientists from Auckland University of Technology (AUT) to create baseline maps of the vegetation.

Geographic entities mentioned:
surface_form: dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
surface_form: mcmurdo dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
Part of the Valleys was designated an environmentally protected area in 2004. Valleys. From north to south, the three main valleys are
West of Victoria Valley are, from north to south,
Lakes. Some of the lakes of the Dry Valleys rank among the world's most saline lakes, with a higher salinity than Lake Assal or the Dead Sea. The most saline of all is small Don Juan Pond.

Geographic entities mentioned:
surface_form: dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
Halvfarhøe. Halvfarhøe is a mountain in Dovre Municipality in Innlandet county, Norway. The tall mountain is located in the Dovrefjell mountains and inside the Dovre National Park, about northeast of the village of Dombås. The mountain is surrounded by several other notable mountains including Gråhøe to the east, Falketind and Blåberget to the north, and Storhøe and Fokstuguhøe to the west.

Geographic entities mentioned:
surface_form: Dovrefjell
instance_of: Mountain
countries: Norway
coordinates: lat: 62.1
lon: 9.41666667
Halvfarhøe. Halvfarhøe is a mountain in Dovre Municipality in Innlandet county, Norway. The tall mountain is located in the Dovrefjell mountains and inside the Dovre National Park, about northeast of the village of Dombås. The mountain is surrounded by several other notable mountains including Gråhøe to the east, Falketind and Blåberget to the north, and Storhøe and Fokstuguhøe to the west.

Geographic entities mentioned:
surface_form: Blåberget
instance_of: Mountain
countries: Norway
coordinates: lat: 62.14055556
lon: 9.43722222
surface_form: gråhøe
instance_of: Mountain
countries: Norway
coordinates: lat: 62.07383
lon: 8.08391
surface_form: gråhøe
instance_of: Mountain
countries: Norway
coordinates: lat: 62.1231
lon: 9.5568
Halvfarhøe. Halvfarhøe is a mountain in Dovre Municipality in Innlandet county, Norway. The tall mountain is located in the Dovrefjell mountains and inside the Dovre National Park, about northeast of the village of Dombås. The mountain is surrounded by several other notable mountains including Gråhøe to the east, Falketind and Blåberget to the north, and Storhøe and Fokstuguhøe to the west.

Geographic entities mentioned:
surface_form: halvfarhøe
instance_of: Mountain
countries: Norway
coordinates: lat: 62.10222222
lon: 9.47416667
Mont Owl's Head. Mont Owl's Head is a mountain in Potton, Quebec, in the Eastern Townships of Quebec, Canada. The mountain has a height of. A ski area, with the same name, was developed on it by Fred Korman and opened in 1965 with 3 lifts (2 chairlifts and 1 t-bar) and 6 runs.

Geographic entities mentioned:
surface_form: owl's head
instance_of: Mountain
countries: Canada
coordinates: lat: 45.0742
lon: -72.2981
surface_form: mont owl's head
instance_of: Mountain
countries: Canada
coordinates: lat: 45.0742
lon: -72.2981
Mont Owl's Head. Mont Owl's Head is a mountain in Potton, Quebec, in the Eastern Townships of Quebec, Canada. The mountain has a height of. A ski area, with the same name, was developed on it by Fred Korman and opened in 1965 with 3 lifts (2 chairlifts and 1 t-bar) and 6 runs.

Geographic entities mentioned:
surface_form: owl's head
instance_of: Mountain
countries: Canada
coordinates: lat: 45.0742
lon: -72.2981
surface_form: mont owl's head
instance_of: Mountain
countries: Canada
coordinates: lat: 45.0742
lon: -72.2981
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mont Owl's Head. Mont Owl's Head is a mountain in Potton, Quebec, in the Eastern Townships of Quebec, Canada. The mountain has a height of. A ski area, with the same name, was developed on it by Fred Korman and opened in 1965 with 3 lifts (2 chairlifts and 1 t-bar) and 6 runs.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
It flows northwest past Ouray, Ridgway, Montrose, and Olathe and joins the Gunnison at Confluence Park in Delta. The river forms Poughkeepsie Gulch and the Uncompahgre Gorge. The major tributaries are all creeks draining the northwest San Juan Mountains.

Geographic entities mentioned:
surface_form: Uncompahgre Gorge
instance_of: Landform
countries: United States
coordinates: lat: 38.0189
lon: -107.676
The major tributaries are all creeks draining the northwest San Juan Mountains. There are two dams on the Uncompahgre River, a small diversion dam in the Uncompahgre Gorge, and Ridgway Dam below the town of Ridgway which forms Ridgway Reservoir. The river is used for irrigation in the Uncompahgre Valley. Additionally, water from the Gunnison is diverted to the valley via the Gunnison Tunnel.

Geographic entities mentioned:
surface_form: Uncompahgre Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.46
lon: -107.89
Brighton and Dyke Railway. The Brighton and Dyke Railway was an independent railway company which built a branch line from Brighton in East Sussex to the Devil's Dyke, a popular beauty spot nearby in the South Downs, England. The line opened in 1887. The intermediary Golf Club Halt opened in 1891 and Rowan Halt opened in 1934. The line was not commercially successful and closed in 1939.

Geographic entities mentioned:
surface_form: Devil's Dyke
instance_of: Valley
countries: United Kingdom
coordinates: lat: 50.885
lon: -0.205
Kasan Wala. Kasan Wala Dera is a small village situated in the Soon Valley, Khushab District, Punjab, Pakistan. This village, or Dera, is part of Union Council Kund. The village has few houses, and is located near Dada Golra Mosque on the way to Naushehra from Khushab. It is located in the Soon valley, and Naushehra is just 20 kilometers away. Dera Kasan is about 35 kilometres from Khushab City.

Geographic entities mentioned:
surface_form: Soon Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 32.58
lon: 72.15
Kalanka. Kalanka (Hindi: कलंका) is a mountain of the Garhwal Himalayas in Uttarakhand, India. Kalanka stands at. It's the 20th highest located entirely within the Uttrakhand. Nanda Devi is the highest mountain in this category. Kalanka is the 48th highest peak in India and 319th highest peak in the world. Southern side of Kalanka falls under Nanda Devi National Park.

Geographic entities mentioned:
surface_form: Nanda Devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
Southern side of Kalanka falls under Nanda Devi National Park. Kalanka loosely translated means &quot;cockscomb&quot; in Hindi. Geography. Kalanka lies on the outer rim of the Nanda Devi sanctuary and in between Changabang and Saf Minal. The mountain is surrounded by glaciers on three sides: Changabang on the southern side, Uttari Rishi on the eastern side, and Bagini on the northern side.

Geographic entities mentioned:
surface_form: Changabang
instance_of: Mountain
countries: India
coordinates: lat: 30.483333333333
lon: 80.016666666667
surface_form: Saf Minal
instance_of: Mountain
countries: India
coordinates: lat: 30.528556
lon: 79.966702
surface_form: changabang
instance_of: Mountain
countries: India
coordinates: lat: 30.483333333333
lon: 80.016666666667
surface_form: nanda devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
surface_form: saf minal
instance_of: Mountain
countries: India
coordinates: lat: 30.528556
lon: 79.966702
Geography. Kalanka lies on the outer rim of the Nanda Devi sanctuary and in between Changabang and Saf Minal. The mountain is surrounded by glaciers on three sides: Changabang on the southern side, Uttari Rishi on the eastern side, and Bagini on the northern side. The river from the Bagini Glacier meets with the Dhauliganga River at Jumma.

Geographic entities mentioned:
surface_form: changabang
instance_of: Mountain
countries: India
coordinates: lat: 30.483333333333
lon: 80.016666666667
Climbing history. The first ascent was completed in 1975 by Ikuo Tanabe's four-member expedition from Japan. They followed the Rishi Ganga gorge and crossed over to Shipton's col to gain the col between Changabang and Kalanka and climbed the west ridge. The first summit was reached by Noriaki Ikeda, Tsuneo Kouma, Kazumasa Inoue and the leader Tanabe on 3 June 1975.

Geographic entities mentioned:
surface_form: changabang
instance_of: Mountain
countries: India
coordinates: lat: 30.483333333333
lon: 80.016666666667
surface_form: kalanka
instance_of: Mountain
countries: India
coordinates: lat: 30.50298119
lon: 79.94094086
The first ascent via the southeast face was completed by a Scottish team in 1978. After establishing base camp on September 20 at the junction of the Changabang and Uttar Rishi glaciers, Robert Barton and Allen Fyffe made a new route up the southeast face. They reached the summit on October 11.

Geographic entities mentioned:
surface_form: changabang
instance_of: Mountain
countries: India
coordinates: lat: 30.483333333333
lon: 80.016666666667
Kalanka. Kalanka (Hindi: कलंका) is a mountain of the Garhwal Himalayas in Uttarakhand, India. Kalanka stands at. It's the 20th highest located entirely within the Uttrakhand. Nanda Devi is the highest mountain in this category. Kalanka is the 48th highest peak in India and 319th highest peak in the world. Southern side of Kalanka falls under Nanda Devi National Park.

Geographic entities mentioned:
surface_form: कलंका
instance_of: Mountain
countries: India
coordinates: lat: 30.50298119
lon: 79.94094086
surface_form: kalanka
instance_of: Mountain
countries: India
coordinates: lat: 30.50298119
lon: 79.94094086
Kalanka. Kalanka (Hindi: कलंका) is a mountain of the Garhwal Himalayas in Uttarakhand, India. Kalanka stands at. It's the 20th highest located entirely within the Uttrakhand. Nanda Devi is the highest mountain in this category. Kalanka is the 48th highest peak in India and 319th highest peak in the world. Southern side of Kalanka falls under Nanda Devi National Park.

Geographic entities mentioned:
surface_form: kalanka
instance_of: Mountain
countries: India
coordinates: lat: 30.50298119
lon: 79.94094086
Kalanka stands at. It's the 20th highest located entirely within the Uttrakhand. Nanda Devi is the highest mountain in this category. Kalanka is the 48th highest peak in India and 319th highest peak in the world. Southern side of Kalanka falls under Nanda Devi National Park. Kalanka loosely translated means &quot;cockscomb&quot; in Hindi. Geography.

Geographic entities mentioned:
surface_form: kalanka
instance_of: Mountain
countries: India
coordinates: lat: 30.50298119
lon: 79.94094086
Kalanka stands at. It's the 20th highest located entirely within the Uttrakhand. Nanda Devi is the highest mountain in this category. Kalanka is the 48th highest peak in India and 319th highest peak in the world. Southern side of Kalanka falls under Nanda Devi National Park. Kalanka loosely translated means &quot;cockscomb&quot; in Hindi. Geography.

Geographic entities mentioned:
surface_form: kalanka
instance_of: Mountain
countries: India
coordinates: lat: 30.50298119
lon: 79.94094086
surface_form: nanda devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
Nanda Devi is the highest mountain in this category. Kalanka is the 48th highest peak in India and 319th highest peak in the world. Southern side of Kalanka falls under Nanda Devi National Park. Kalanka loosely translated means &quot;cockscomb&quot; in Hindi. Geography. Kalanka lies on the outer rim of the Nanda Devi sanctuary and in between Changabang and Saf Minal.

Geographic entities mentioned:
surface_form: kalanka
instance_of: Mountain
countries: India
coordinates: lat: 30.50298119
lon: 79.94094086
These two main rivers meet at Devpryag. The name Ganga starts from there. The entire surrounding area is protected within the Nanda Devi National Park or Nanda Devi Biosphere Reserve which is a World Heritage Site declared by UNESCO. The Nanda Devi National Park is home to several world-class treks. Climbing history.

Geographic entities mentioned:
surface_form: nanda devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
surface_form: nanda devi biosphere reserve
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
surface_form: nanda devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
The mountain is situated approximately north of Marblemount. Hagan Mountain is surrounded by other notable peaks in the North Cascades. Mount Blum, which is the nearest higher peak, lies to the north of Hagan Mountain. Bacon Peak is another prominent peak, located to the south. The mountain features the expansive Hagan Glacier, as well as the smaller Hidden Creek Glacier.

Geographic entities mentioned:
surface_form: Mount Blum
instance_of: Mountain
countries: United States
coordinates: lat: 48.7541
lon: -121.482
surface_form: hagan mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.72151
lon: -121.5018
The mountain is situated approximately north of Marblemount. Hagan Mountain is surrounded by other notable peaks in the North Cascades. Mount Blum, which is the nearest higher peak, lies to the north of Hagan Mountain. Bacon Peak is another prominent peak, located to the south. The mountain features the expansive Hagan Glacier, as well as the smaller Hidden Creek Glacier.

Geographic entities mentioned:
surface_form: Bacon Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.6627
lon: -121.521
Hagan Mountain. Hagan Mountain is a multi-peak mountain located in Whatcom County, Washington state, within North Cascades National Park. It has an elevation of 7,080-feet (2,160-metres). The mountain is situated approximately north of Marblemount. Hagan Mountain is surrounded by other notable peaks in the North Cascades.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: hagan mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.72151
lon: -121.5018
surface_form: peak mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.970277777778
lon: -72.74
surface_form: peak mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.1308
lon: -81.8336
Hagan Mountain. Hagan Mountain is a multi-peak mountain located in Whatcom County, Washington state, within North Cascades National Park. It has an elevation of 7,080-feet (2,160-metres). The mountain is situated approximately north of Marblemount. Hagan Mountain is surrounded by other notable peaks in the North Cascades.

Geographic entities mentioned:
surface_form: hagan mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.72151
lon: -121.5018
It has an elevation of 7,080-feet (2,160-metres). The mountain is situated approximately north of Marblemount. Hagan Mountain is surrounded by other notable peaks in the North Cascades. Mount Blum, which is the nearest higher peak, lies to the north of Hagan Mountain. Bacon Peak is another prominent peak, located to the south.

Geographic entities mentioned:
surface_form: hagan mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.72151
lon: -121.5018
Precipitation runoff and meltwater from these glaciers flow into tributaries of the Skagit River, contributing to the water supply in the region. Climate. Hagan Mountain is situated in the marine west coast climate zone of western North America. In this region, weather fronts typically originate in the Pacific Ocean and move northeast towards the Cascade Mountains.

Geographic entities mentioned:
surface_form: hagan mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.72151
lon: -121.5018
This upward motion causes the moisture within the fronts to be released as precipitation in the form of rain or snowfall, a phenomenon known as Orographic lift. The west side of the North Cascades, including Hagan Mountain, receives significant precipitation, particularly during the winter months when snowfall is common.

Geographic entities mentioned:
surface_form: hagan mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.72151
lon: -121.5018
Saddle Peak (Andaman Islands). Saddle Peak or Saddle Hill is located on North Andaman Island in India's Andaman and Nicobar Islands. At 732 m, it is the highest point of the archipelago in the Bay of Bengal. Asper Geologists & Volcanists it is a Dormant Volcano with last eruption in 50-100 BC. The peak is located close to the east coast. It is surrounded by Saddle Peak National Park.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Saddle Peak (Andaman Islands). Saddle Peak or Saddle Hill is located on North Andaman Island in India's Andaman and Nicobar Islands. At 732 m, it is the highest point of the archipelago in the Bay of Bengal. Asper Geologists & Volcanists it is a Dormant Volcano with last eruption in 50-100 BC. The peak is located close to the east coast. It is surrounded by Saddle Peak National Park.

Geographic entities mentioned:
surface_form: saddle peak
instance_of: Mountain
countries: India
coordinates: lat: 13.158388
lon: 93.006134
At 732 m, it is the highest point of the archipelago in the Bay of Bengal. Asper Geologists & Volcanists it is a Dormant Volcano with last eruption in 50-100 BC. The peak is located close to the east coast. It is surrounded by Saddle Peak National Park. It is located to the south of Diglipur and to the southwest of Kalipur Beach.

Geographic entities mentioned:
surface_form: saddle peak
instance_of: Mountain
countries: India
coordinates: lat: 13.158388
lon: 93.006134
The anchor stores are two Dillard's stores and JCPenney. There are two vacant anchor stores that were once Gordmans,Conn's and Macy's. The first mall to be opened in College Station, Post Oak is the largest mall within the Brazos Valley area. At its opening, it became the city's largest employer, and nearly doubled its city sales tax revenues.

Geographic entities mentioned:
surface_form: Brazos Valley
instance_of: Valley
countries: United States
coordinates: lat: 30.66
lon: -96.3
It was quickly replaced by the Brazos Valley seventh Sonic Drive-In location, the only in the area with neither a drive-in nor drive-through option. The Sonic closed in late 2012. Economic impact. Post Oak Mall was the first mall in the city of College Station, and as of 2008, it is the largest mall in the Brazos Valley.

Geographic entities mentioned:
surface_form: Brazos Valley
instance_of: Valley
countries: United States
coordinates: lat: 30.66
lon: -96.3
Especially horse milk was widely used and consumed as horses were also held for transportation purposes. Many of the practices of this nomadic diet can still be observed in the descendants of Uyghurs who immigrated from the Mongolian Plateau to the Gansu Province. After the Uyghurs accepted Islam as their state religion in the 1060s, many adopted a halal diet.

Geographic entities mentioned:
surface_form: Mongolian Plateau
instance_of: Plateau
countries: Mongolia
People's Republic of China
Russia
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 107
Jordan Lake (Nova Scotia). Jordan Lake, Nova Scotia is a lake that is located mostly in Shelburne District, in Nova Scotia, Canada. Its northeastern portion crosses into Region of Queens Municipality. The lake lies southwest of the much larger Lake Rossignol.

Geographic entities mentioned:
surface_form: Lake Rossignol
instance_of: Lake
countries: Canada
coordinates: lat: 44.1797
lon: -65.1258