Sarmila/GeoWiki-Features huggingface dataset:
With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted. Glacier Peak, a stratovolcano that is north of Kodak Peak, began forming in the mid-Pleistocene. Due to Glacier Peak's proximity to Kodak Peak, volcanic ash is common in the area and provides fertile soil for an abundance of wildflowers.

Geographic entities mentioned:
surface_form: Glacier Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: kodak peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.9875
lon: -121.12944444444
Kodak Peak. Kodak Peak is a summit on the border shared by Chelan and Snohomish counties in Washington, United States. Description. Kodak Peak is situated on the crest of the Cascade Range and is part of the North Cascades. It straddles the boundary shared by Glacier Peak Wilderness with Henry M.

Geographic entities mentioned:
surface_form: kodak peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.9875
lon: -121.12944444444
Kodak Peak. Kodak Peak is a summit on the border shared by Chelan and Snohomish counties in Washington, United States. Description. Kodak Peak is situated on the crest of the Cascade Range and is part of the North Cascades. It straddles the boundary shared by Glacier Peak Wilderness with Henry M.

Geographic entities mentioned:
surface_form: kodak peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.9875
lon: -121.12944444444
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
The Pacific Crest Trail traverses the south and east slopes of the peak. The summit is climbed via a 16-mile hike that gains 3,100 feet of elevation. The mountain's toponym has been officially adopted by the United States Board on Geographic Names as named by Albert Hale Sylvester. Kodak Peak was named for a Kodak camera lost there by Sylvester's assistant, Willett Ramsdell. Geology.

Geographic entities mentioned:
surface_form: kodak peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.9875
lon: -121.12944444444
With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted. Glacier Peak, a stratovolcano that is north of Kodak Peak, began forming in the mid-Pleistocene. Due to Glacier Peak's proximity to Kodak Peak, volcanic ash is common in the area and provides fertile soil for an abundance of wildflowers.

Geographic entities mentioned:
surface_form: kodak peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.9875
lon: -121.12944444444
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
Description. Kodak Peak is situated on the crest of the Cascade Range and is part of the North Cascades. It straddles the boundary shared by Glacier Peak Wilderness with Henry M. Jackson Wilderness, and is set on land managed by Mount Baker-Snoqualmie National Forest and Okanogan–Wenatchee National Forest.

Geographic entities mentioned:
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
Kunkush (Lima). Kunkush (Ancash Quechua for &quot;Puya raimondii&quot;, hispanicized spelling &quot;Cuncush&quot;) is a mountain in the Andes of Peru, about high. It is located in the Lima Region, Oyón Province, Oyón District.

Geographic entities mentioned:
surface_form: kunkush
instance_of: Mountain
countries: Peru
coordinates: lat: -10.64888889
lon: -76.72138889
Fay Peak. Fay Peak is a double-summit mountain located in Mount Rainier National Park, in Pierce County of Washington state. It is part of the Cascade Range, and lies northwest of the summit of Mount Rainier. The 6,492-foot elevation summit of Fay Peak lies a quarter-mile west of the highest point, East Fay Peak. Echo Rock is its nearest higher neighbor, to the southeast.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
The 6,492-foot elevation summit of Fay Peak lies a quarter-mile west of the highest point, East Fay Peak. Echo Rock is its nearest higher neighbor, to the southeast. Precipitation runoff from Fay Peak is drained by Cataract Creek on the east side of the mountain, and the west side drains into Mowich Lake and Mowich River. Climate.

Geographic entities mentioned:
surface_form: Mowich Lake
instance_of: Lake
countries: United States
coordinates: lat: 46.9382689
lon: -121.8620654
surface_form: fay peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.93233
lon: -121.84816
Fay Peak. Fay Peak is a double-summit mountain located in Mount Rainier National Park, in Pierce County of Washington state. It is part of the Cascade Range, and lies northwest of the summit of Mount Rainier. The 6,492-foot elevation summit of Fay Peak lies a quarter-mile west of the highest point, East Fay Peak. Echo Rock is its nearest higher neighbor, to the southeast.

Geographic entities mentioned:
surface_form: mount rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: fay peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.93233
lon: -121.84816
surface_form: summit mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.3539
lon: -113.37
surface_form: summit mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.996666666667
lon: -74.916666666667
The months of July through September offer the most favorable weather for viewing or climbing this peak. History. This mountain's name honors Fay Fuller (1869–1958), the first woman to stand atop the summit of Mount Rainier. Her first successful ascent occurred on August 10, 1890, and her second on July 27, 1897.

Geographic entities mentioned:
surface_form: mount rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
Fay Peak. Fay Peak is a double-summit mountain located in Mount Rainier National Park, in Pierce County of Washington state. It is part of the Cascade Range, and lies northwest of the summit of Mount Rainier. The 6,492-foot elevation summit of Fay Peak lies a quarter-mile west of the highest point, East Fay Peak. Echo Rock is its nearest higher neighbor, to the southeast.

Geographic entities mentioned:
surface_form: fay peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.93233
lon: -121.84816
Fay Peak. Fay Peak is a double-summit mountain located in Mount Rainier National Park, in Pierce County of Washington state. It is part of the Cascade Range, and lies northwest of the summit of Mount Rainier. The 6,492-foot elevation summit of Fay Peak lies a quarter-mile west of the highest point, East Fay Peak. Echo Rock is its nearest higher neighbor, to the southeast.

Geographic entities mentioned:
surface_form: fay peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.93233
lon: -121.84816
surface_form: fay peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.93233
lon: -121.84816
Precipitation runoff from Fay Peak is drained by Cataract Creek on the east side of the mountain, and the west side drains into Mowich Lake and Mowich River. Climate. Fay Peak is located in the marine west coast climate zone of western North America. Most weather fronts originating in the Pacific Ocean travel northeast toward the Cascade Mountains.

Geographic entities mentioned:
surface_form: fay peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.93233
lon: -121.84816
History. This mountain's name honors Fay Fuller (1869–1958), the first woman to stand atop the summit of Mount Rainier. Her first successful ascent occurred on August 10, 1890, and her second on July 27, 1897. The name &quot;Fay Peak&quot; first appeared on a map of the mountain published in 1895. The toponym was officially adopted in 1913 by the United States Board on Geographic Names.

Geographic entities mentioned:
surface_form: fay peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.93233
lon: -121.84816
Great North Mountain. Great North Mountain is a long mountain ridge within the Ridge-and-Valley Appalachians in the U.S. states of Virginia and West Virginia. The ridge is located west of the Shenandoah Valley and Massanutten Mountain in Virginia, and it is east of the Allegheny Mountains and Cacapon River in West Virginia. Geography.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
surface_form: Massanutten Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.643
lon: -78.612
Local Sites of Interest. Part of Great North Mountain is within the George Washington National Forest, which offers many hiking and hunting trails, such as the Seven Springs trail, and those leading to an overlook on Big Schloss, a peak in the area.

Geographic entities mentioned:
surface_form: Big Schloss
instance_of: Mountain
countries: United States
coordinates: lat: 38.9406
lon: -78.6658
surface_form: big schloss
instance_of: Mountain
countries: United States
coordinates: lat: 38.9406
lon: -78.6658
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.4206
lon: -78.0889
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.2175
lon: -74.0492
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.31944444
lon: -76.55388889
Both of these name changes were made in order to differentiate the mountain from North Mountain to the north. In the colonial era, Great North Mountain was referred to by some on the frontier as &quot;The Devil's Backbone,&quot; an alias noted in the Fry-Jefferson map published in London in 1755. Local Sites of Interest.

Geographic entities mentioned:
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.4206
lon: -78.0889
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.2175
lon: -74.0492
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.31944444
lon: -76.55388889
surface_form: great north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.0356
lon: -78.5675
Geography. Great North Mountain is oriented along a northeast-southwest axis from its southern terminus along the North Fork Shenandoah River in Rockingham County, Virginia to its northern terminus at U.S. Route 522 in Frederick County, Virginia. In the south, the initial of the ridge is known as Church Mountain.

Geographic entities mentioned:
surface_form: church mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.926791
lon: -121.8820883
Geography. Great North Mountain is oriented along a northeast-southwest axis from its southern terminus along the North Fork Shenandoah River in Rockingham County, Virginia to its northern terminus at U.S. Route 522 in Frederick County, Virginia. In the south, the initial of the ridge is known as Church Mountain.

Geographic entities mentioned:
surface_form: shenandoah
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.4206
lon: -78.0889
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.2175
lon: -74.0492
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.31944444
lon: -76.55388889
surface_form: great north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.0356
lon: -78.5675
For much of its length, the mountain forms the border between Virginia and West Virginia, in two separate stretches; starting north of its southern terminus at the border of Hardy County, West Virginia, Rockingham County, Virginia and Shenandoah County, Virginia, for with a break where the border shifts east to Paddy Mountain around Wilson Cove, followed by an additional stretch to the north.

Geographic entities mentioned:
surface_form: shenandoah
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
The ridge reaches its greatest elevation, at the peak of Mill Mountain, on the border between Hardy County, West Virginia, and Shenandoah County, Virginia, in the George Washington National Forest. The mountain is crossed by U.S. Route 48 and West Virginia and Virginia routes 55 between Wardensville, West Virginia and Strasburg, Virginia. Variant names.

Geographic entities mentioned:
surface_form: shenandoah
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: mill mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.262777777778
lon: -74.734166666667
surface_form: mill mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.799722222222
lon: -74.2925
Great North Mountain. Great North Mountain is a long mountain ridge within the Ridge-and-Valley Appalachians in the U.S. states of Virginia and West Virginia. The ridge is located west of the Shenandoah Valley and Massanutten Mountain in Virginia, and it is east of the Allegheny Mountains and Cacapon River in West Virginia. Geography.

Geographic entities mentioned:
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.4206
lon: -78.0889
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.2175
lon: -74.0492
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.31944444
lon: -76.55388889
surface_form: great north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.0356
lon: -78.5675
Great North Mountain. Great North Mountain is a long mountain ridge within the Ridge-and-Valley Appalachians in the U.S. states of Virginia and West Virginia. The ridge is located west of the Shenandoah Valley and Massanutten Mountain in Virginia, and it is east of the Allegheny Mountains and Cacapon River in West Virginia. Geography.

Geographic entities mentioned:
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.4206
lon: -78.0889
surface_form: long mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.305
lon: -72.4831
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.2175
lon: -74.0492
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.31944444
lon: -76.55388889
surface_form: great north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.0356
lon: -78.5675
Variant names. The Board on Geographic Names handed down two official decisions concerning the mountain's name in the years 1941 and 1967. In 1941, the board decided upon the name Big North Mountain and in 1967, it chose Great North Mountain. Both of these name changes were made in order to differentiate the mountain from North Mountain to the north.

Geographic entities mentioned:
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.4206
lon: -78.0889
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.4206
lon: -78.0889
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.2175
lon: -74.0492
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.2175
lon: -74.0492
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.31944444
lon: -76.55388889
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.31944444
lon: -76.55388889
surface_form: great north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.0356
lon: -78.5675
Variant names. The Board on Geographic Names handed down two official decisions concerning the mountain's name in the years 1941 and 1967. In 1941, the board decided upon the name Big North Mountain and in 1967, it chose Great North Mountain. Both of these name changes were made in order to differentiate the mountain from North Mountain to the north.

Geographic entities mentioned:
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.4206
lon: -78.0889
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.2175
lon: -74.0492
surface_form: north mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.31944444
lon: -76.55388889
The retreat includes the Cathedral Shrine of the Transfiguration and The Virginia House (formerly known as the Orkney Springs Hotel). Nearby Basye boasts the four season Bryce Resort, which has golf, skiing, mountain biking, and Lake Laura.

Geographic entities mentioned:
surface_form: lake laura
instance_of: Lake
countries: United States
coordinates: lat: 47.3981
lon: -121.34343
Beside the small town of Orkney Springs, Virginia, at the foot of the mountain, is Shrine Mont, a retreat and conference center owned by the Episcopal Diocese of Virginia. The retreat includes the Cathedral Shrine of the Transfiguration and The Virginia House (formerly known as the Orkney Springs Hotel).

Geographic entities mentioned:
surface_form: the cathedral
instance_of: Mountain
countries: United States
coordinates: lat: 40.775833333333
lon: -110.71027777778
It is north of SP46. The town is a tourist destination. On the background of Valli, from right to left, are the Pasubio massif (whose highest peak is Cima Palon, also called Monte Pasubion), the Baffelan-Tre Apostoli-Cornetto (Group of Sengio Alto) group and finally, on the left, the Carega group: all are destinations for excursions and for climbing.

Geographic entities mentioned:
surface_form: Cima Palon
instance_of: Mountain
countries: Italy
coordinates: lat: 46.02694444
lon: 11.05861111
Mount Yudono. is one of the Three Mountains of Dewa in the ancient province of Dewa (modern-day Yamagata Prefecture). The Yudonosan Shrine, the most holy of the Dewa Sanzan shrines, is located on the mountain. Pilgrims have to enter the shrine itself barefoot, and photography is not allowed. Due to heavy winter snowfall, the mountain and shrine are inaccessible for long periods of the year.

Geographic entities mentioned:
surface_form: yudonosan
instance_of: Mountain
countries: Japan
coordinates: lat: 38.531111111111
lon: 139.985
Mount Yudono. is one of the Three Mountains of Dewa in the ancient province of Dewa (modern-day Yamagata Prefecture). The Yudonosan Shrine, the most holy of the Dewa Sanzan shrines, is located on the mountain. Pilgrims have to enter the shrine itself barefoot, and photography is not allowed. Due to heavy winter snowfall, the mountain and shrine are inaccessible for long periods of the year.

Geographic entities mentioned:
surface_form: mount yudono
instance_of: Mountain
countries: Japan
coordinates: lat: 38.531111111111
lon: 139.985
Today only an obelisk commemorates this milestone in German railway history. History. Although the Leipzig–Dresden railway ran over the fairly flat terrain of northern Saxony, the northern slopes of the Dresden Basin meant that a tunnel was required because at that time it was believed that trains on major railways could not climb significant slopes.

Geographic entities mentioned:
surface_form: Dresden Basin
instance_of: Valley
countries: Germany
The railway had its station, Trondhjem Kalvskinnet Station, in Prinsens gate, crossed the Nidelva river on a newly constructed railroad bridge to Elgeseter, the Elgeseter Bridge. In 1877 the line was joined with the Røros Line, which went through the Østerdalen between Røros and Hamar.

Geographic entities mentioned:
surface_form: Østerdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.575916666666664
lon: 11.087111111111112
Traxel refers to a number of archeological findings by Frederick J. Pohl at Follins Pond, and connects these to the settlement of &quot;Hóp&quot;. He also reports that Robert Ellis Cahill found a Norse longhouse near Buzzard's Bay He also holds Pettaquamscutt River, Rhode Island as a candidate for the location of &quot;Hóp&quot;. Buzzards Bay.

Geographic entities mentioned:
surface_form: Follins Pond
instance_of: Lake
countries: United States
coordinates: lat: 41.704166666667
lon: -70.179166666667
In July 2006, &quot;Cassini&quot; saw the first proof of hydrocarbon lakes near Titan's north pole, which was confirmed in January 2007. In March 2007, additional images near Titan's north pole discovered hydrocarbon &quot;seas&quot;, the largest of which is almost the size of the Caspian Sea. In 2009, the probe discovered and confirmed four new satellites.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Bull Harbour. Bull Harbour is a settlement in British Columbia, Canada. Bull Harbour is a settlement on Hope Island, just north of northern Vancouver Island across Goletas Channel. It has an estimated population of 2-20 people. The name Bull Harbour has been in use since at least 1841. The name likely comes from the large and fierce sea lions that frequent the area. Climate.

Geographic entities mentioned:
surface_form: Goletas Channel
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.84004
lon: -127.72533
Alestopetersius taeniatus. &quot;Alestopetersius taeniatus&quot; is a species of freshwater ray-finned fish belonging to the family Alestidae, the African tetras. It is known only from the Sangha River in Cameroon. Description. &quot;Alestopetersius taeniatus&quot; reaches a standard length of.

Geographic entities mentioned:
surface_form: Sangha River
instance_of: Watercourse
countries: Cameroon
Central African Republic
Republic of the Congo
coordinates: lat: -1.2125
lon: 16.827777777778
Hipparchus is also credited with creating a celestial globe, although this object is not known to be extant. The catalog was lost to history, until parts of it were rediscovered in 2022 in the Codex Climaci Rescriptus, an ancient palimpsest found in Saint Catherine's Monastery on Mount Sinai. Rediscovery.

Geographic entities mentioned:
surface_form: Mount Sinai
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.5384
lon: 33.9752
It was nearly a month later when they arrived at what is now Stevensville, Montana, in the Bitterroot Valley, and began the foundations of the log mission. The missionaries worked at cutting the frozen earth with axes.

Geographic entities mentioned:
surface_form: Bitterroot Valley
instance_of: Valley
countries: United States
coordinates: lat: 46.247
lon: -114.16
Ozark hellbender. The Ozark hellbender (&quot;Cryptobranchus alleganiensis bishopi&quot;) is a subspecies of the hellbender (&quot;Cryptobranchus alleganiensis&quot;). The subspecies is strictly native to the mountain streams of the Ozark Plateau in southern Missouri and northern Arkansas. Its nicknames include lasagna lizard and snot otter.

Geographic entities mentioned:
surface_form: Ozark Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
He received a sound liberal arts education, possibly at the Benedictine monastery of Saint John the Baptist near Celano. His familiarity with monastic tradition suggests that he may have studied at Monte Cassino, Rome or Bologna. He joined the Franciscan order probably in 1215.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
Rudekšna. The Rudekšna is a river of Kėdainiai district municipality, Kaunas County, central Lithuania. It flows for and has a basin area of. It starts nearby the Gružai Forest, on the Ukmergė District Municipality and Panevėžys District Municipality limits. The Rudekšna flows southwards and meets the Obelis river (from the right side) nearby Runeikiai village.

Geographic entities mentioned:
surface_form: rudekšna
instance_of: Watercourse
countries: Lithuania
coordinates: lat: 55.322839
lon: 24.370174
It flows for and has a basin area of. It starts nearby the Gružai Forest, on the Ukmergė District Municipality and Panevėžys District Municipality limits. The Rudekšna flows southwards and meets the Obelis river (from the right side) nearby Runeikiai village. Pagiriai town stands by the Rudekšna. The name &quot;Rudekšna&quot; is derived from ('brown').

Geographic entities mentioned:
surface_form: rudekšna
instance_of: Watercourse
countries: Lithuania
coordinates: lat: 55.322839
lon: 24.370174
Topography. The Southern Fells include the highest ground in England, a horseshoe which begins with Scafell and Scafell Pike in the west and then curves around the north of Upper Eskdale to take in Great End, Esk Pike, Bow Fell and Crinkle Crags. As the name suggests, Esk Pike stands at the head of the valley, although it is not the highest of these fells.

Geographic entities mentioned:
surface_form: Scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
surface_form: Scafell Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454166666667
lon: -3.2115277777778
surface_form: Great End
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.464
lon: -3.194
surface_form: bow fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.447369444444
lon: -3.1658194444444
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.478
lon: -0.786
surface_form: esk pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456219444444
lon: -3.17995
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.189
lon: -3.068
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
To the north-west of Esk Pike is the depression of Esk Hause, a broad saddle carrying a number of important paths. The ‘true’ Esk Hause—so named by Alfred Wainwright in his influential &quot;Pictorial Guide to the Lakeland Fells&quot;—is the north–south route from Borrowdale to Eskdale. A lower path—the ‘false’ Hause—runs east–west from Langdale to Wasdale, passing a stone windshelter.

Geographic entities mentioned:
surface_form: Wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
surface_form: wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
A lower path—the ‘false’ Hause—runs east–west from Langdale to Wasdale, passing a stone windshelter. There are also paths climbing to the summits of Esk Pike and Allen Crags, together with the popular Calf Cove route to Scafell Pike, all contributing to make Esk Hause a confusing place in mist.

Geographic entities mentioned:
surface_form: Allen Crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4661
lon: -3.1802388888889
surface_form: esk pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456219444444
lon: -3.17995
surface_form: allen crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4661
lon: -3.1802388888889
surface_form: scafell pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454166666667
lon: -3.2115277777778
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
Allen Crags stands adrift from the main ridge, with the valleys of Langstrath and Grains Gill falling on either side. These combine some miles downstream to form the River Derwent, flowing through Borrowdale to Derwentwater and Keswick. South-east of the summit of Esk Pike is Ore Gap, the col separating it from Bow Fell.

Geographic entities mentioned:
surface_form: Derwentwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.583333333333
lon: -3.15
surface_form: derwentwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.583333333333
lon: -3.15
surface_form: borrowdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.42
lon: -2.665
A small cairn on the highest craggy outcrop marks the highest point. Esk Pike's central position above Eskdale gives it glorious views of the Scafells, with the Eastern and Northern Fells also forming a fine panorama. Derwentwater and a section of Windermere complete the scene. A little to the south, Pike de Bield provides an intimate view of the upper Esk. Ascents.

Geographic entities mentioned:
surface_form: Windermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.358333333333
lon: -2.9361111111111
surface_form: windermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.358333333333
lon: -2.9361111111111
Borrowdale gives a choice of starting points, either making for Esk Hause from Seathwaite, or Ore Gap from Stonethwaite. Access is also possible from Great Langdale, ascending Rossett Gill from the Old Hotel. Many walkers will reach the summit indirectly having climbed Bow Fell first via the Band, or perhaps climbed from Borrowdale over Glaramara and Allen Crags.

Geographic entities mentioned:
surface_form: Glaramara
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483319444444
lon: -3.1653
surface_form: bow fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.447369444444
lon: -3.1658194444444
surface_form: allen crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4661
lon: -3.1802388888889
surface_form: borrowdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.42
lon: -2.665
surface_form: glaramara
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483319444444
lon: -3.1653
Scar Lathing is particularly impressive, presenting sheer cliffs above a bend in the Esk. Although of minor significance Pianet Knott on the eastern side of the ridge also has a very striking appearance from lower down the valley. Geology.

Geographic entities mentioned:
surface_form: knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.686211111111
lon: -3.0935388888889
A series of steps rise up from Ore Gap whilst the approach from Esk Hause is rough and eroded. A small cairn on the highest craggy outcrop marks the highest point. Esk Pike's central position above Eskdale gives it glorious views of the Scafells, with the Eastern and Northern Fells also forming a fine panorama. Derwentwater and a section of Windermere complete the scene.

Geographic entities mentioned:
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.478
lon: -0.786
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.189
lon: -3.068
These combine some miles downstream to form the River Derwent, flowing through Borrowdale to Derwentwater and Keswick. South-east of the summit of Esk Pike is Ore Gap, the col separating it from Bow Fell. The soil here is red due to haematite, and climbing lore suggests that magnetic compasses cannot be trusted in this locality. North of the gap is Angle Tarn, a feeder of the Langstrath.

Geographic entities mentioned:
surface_form: bow fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.447369444444
lon: -3.1658194444444
surface_form: esk pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456219444444
lon: -3.17995
South-east of the summit of Esk Pike is Ore Gap, the col separating it from Bow Fell. The soil here is red due to haematite, and climbing lore suggests that magnetic compasses cannot be trusted in this locality. North of the gap is Angle Tarn, a feeder of the Langstrath. This round tarn occupies a corrie beneath Hanging Knotts, small trout lurking in its depths.

Geographic entities mentioned:
surface_form: angle tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.5197
lon: -2.90056
surface_form: angle tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.458638
lon: -3.167195
Esk Pike. Esk Pike is a fell in the English Lake District, one of the cirque of hills forming the head of Eskdale. Topography. The Southern Fells include the highest ground in England, a horseshoe which begins with Scafell and Scafell Pike in the west and then curves around the north of Upper Eskdale to take in Great End, Esk Pike, Bow Fell and Crinkle Crags.

Geographic entities mentioned:
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.478
lon: -0.786
surface_form: esk pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456219444444
lon: -3.17995
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.189
lon: -3.068
To the north-west of Esk Pike is the depression of Esk Hause, a broad saddle carrying a number of important paths. The ‘true’ Esk Hause—so named by Alfred Wainwright in his influential &quot;Pictorial Guide to the Lakeland Fells&quot;—is the north–south route from Borrowdale to Eskdale. A lower path—the ‘false’ Hause—runs east–west from Langdale to Wasdale, passing a stone windshelter.

Geographic entities mentioned:
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.478
lon: -0.786
surface_form: borrowdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.42
lon: -2.665
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.189
lon: -3.068
North of the gap is Angle Tarn, a feeder of the Langstrath. This round tarn occupies a corrie beneath Hanging Knotts, small trout lurking in its depths. Southward from the summit, Esk Pike throws out a long descending ridge into the uninhabited fastness of Upper Eskdale. This divides the Esk from its major upper tributary, Lingcove Beck, which has its beginnings at Ore Gap.

Geographic entities mentioned:
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.478
lon: -0.786
surface_form: esk pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456219444444
lon: -3.17995
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.189
lon: -3.068
Ascents. Being far from any roads, all ascents of Esk Pike involve considerable distance by Cumbrian standards. From Brotherilkeld on the Eskdale road the climber can choose between Ore Gap, Esk Hause and the south ridge, all of these options being around. Borrowdale gives a choice of starting points, either making for Esk Hause from Seathwaite, or Ore Gap from Stonethwaite.

Geographic entities mentioned:
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.478
lon: -0.786
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.189
lon: -3.068
Esk Pike. Esk Pike is a fell in the English Lake District, one of the cirque of hills forming the head of Eskdale. Topography. The Southern Fells include the highest ground in England, a horseshoe which begins with Scafell and Scafell Pike in the west and then curves around the north of Upper Eskdale to take in Great End, Esk Pike, Bow Fell and Crinkle Crags.

Geographic entities mentioned:
surface_form: esk pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456219444444
lon: -3.17995
Topography. The Southern Fells include the highest ground in England, a horseshoe which begins with Scafell and Scafell Pike in the west and then curves around the north of Upper Eskdale to take in Great End, Esk Pike, Bow Fell and Crinkle Crags. As the name suggests, Esk Pike stands at the head of the valley, although it is not the highest of these fells.

Geographic entities mentioned:
surface_form: esk pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456219444444
lon: -3.17995
As the name suggests, Esk Pike stands at the head of the valley, although it is not the highest of these fells. To the north-west of Esk Pike is the depression of Esk Hause, a broad saddle carrying a number of important paths. The ‘true’ Esk Hause—so named by Alfred Wainwright in his influential &quot;Pictorial Guide to the Lakeland Fells&quot;—is the north–south route from Borrowdale to Eskdale.

Geographic entities mentioned:
surface_form: esk pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456219444444
lon: -3.17995
Although of minor significance Pianet Knott on the eastern side of the ridge also has a very striking appearance from lower down the valley. Geology. Laminated volcaniclastic claystones and siltstones of the Esk Pike Formation form the upper reaches, crossed by an intrusion of andesite and hybridized andesite porphyry. Summit.

Geographic entities mentioned:
surface_form: esk pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456219444444
lon: -3.17995
Derwentwater and a section of Windermere complete the scene. A little to the south, Pike de Bield provides an intimate view of the upper Esk. Ascents. Being far from any roads, all ascents of Esk Pike involve considerable distance by Cumbrian standards. From Brotherilkeld on the Eskdale road the climber can choose between Ore Gap, Esk Hause and the south ridge, all of these options being around.

Geographic entities mentioned:
surface_form: esk pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456219444444
lon: -3.17995
Borrowdale gives a choice of starting points, either making for Esk Hause from Seathwaite, or Ore Gap from Stonethwaite. Access is also possible from Great Langdale, ascending Rossett Gill from the Old Hotel. Many walkers will reach the summit indirectly having climbed Bow Fell first via the Band, or perhaps climbed from Borrowdale over Glaramara and Allen Crags.

Geographic entities mentioned:
surface_form: great langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.449119444444
lon: -3.0733305555556
Jerisjärvi. Jerisjärvi is a medium-sized lake of Finland in Muonio and Kittilä. It belongs to Tornionjoki main catchment area in Lapland. in the southern side of the Pallas-Yllästunturi National Park. The best season to visit and kayak or canoe is between.

Geographic entities mentioned:
surface_form: jerisjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 67.9032375
lon: 24.1574561
Jerisjärvi. Jerisjärvi is a medium-sized lake of Finland in Muonio and Kittilä. It belongs to Tornionjoki main catchment area in Lapland. in the southern side of the Pallas-Yllästunturi National Park. The best season to visit and kayak or canoe is between.

Geographic entities mentioned:
surface_form: pallas
instance_of: Mountain
countries: Finland
coordinates: lat: 68.0747
lon: 24.0539
&quot;A Dying Cub Fan's Last Request&quot; contains several references to the city of Chicago and to the Chicago Cubs. The song's opening lines (&quot;By the shores of old Lake Michigan / Where the hawk wind blows so cold&quot;) refer to a colloquial term for the wind in Chicago. The man in the song compares his crushed hopes to popcorn being eaten by pigeons beneath the &quot;L&quot; tracks.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Kawaikini is a shield volcano on the Hawaiian Island of Kauai and in Kauai County and measures in elevation. It is the summit of the island's inactive central shield volcano, Mount Waialeale. Other peaks on Kauai include: Waialeale (5,148 feet), Namolokama Mountain (4,421 feet), Kalalau Lookout (4,120 feet), Keanapuka Mountain (4,120 feet), Haupu (2,297 feet) and Nounou (1,241 feet). Description.

Geographic entities mentioned:
surface_form: Keanapuka Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 22.16
lon: -159.61
surface_form: waialeale
instance_of: Mountain
countries: United States
coordinates: lat: 22.073888888889
lon: -159.49861111111
Kawaikini. Kawaikini is a shield volcano on the Hawaiian Island of Kauai and in Kauai County and measures in elevation. It is the summit of the island's inactive central shield volcano, Mount Waialeale. Other peaks on Kauai include: Waialeale (5,148 feet), Namolokama Mountain (4,421 feet), Kalalau Lookout (4,120 feet), Keanapuka Mountain (4,120 feet), Haupu (2,297 feet) and Nounou (1,241 feet).

Geographic entities mentioned:
surface_form: waialeale
instance_of: Mountain
countries: United States
coordinates: lat: 22.073888888889
lon: -159.49861111111
surface_form: mount waialeale
instance_of: Mountain
countries: United States
coordinates: lat: 22.073888888889
lon: -159.49861111111
Description. A rain gauge placed on the nearby Waialeale lake records daily rainfall and regularly lands Kauai's peaks on the National Climatic Data Center's list of places averaging the highest annual rainfall. This high rainfall makes reaching the summit difficult on most days. The rain is not the only barrier to reaching Kawaikini.

Geographic entities mentioned:
surface_form: waialeale
instance_of: Mountain
countries: United States
coordinates: lat: 22.073888888889
lon: -159.49861111111
The Alakai Wilderness Preserve is located to the west and its miles of dense, swampy forest limit access to the summit. To the north, east, and south, Kawaikini is protected by steep, wet cliffs. Etymology. &quot;Ka wai kini&quot; literally translates to &quot;the multitudinous water&quot; in the Hawaiian language, referring to the island's high rainfall.

Geographic entities mentioned:
surface_form: ka wai kini
instance_of: Mountain
countries: United States
coordinates: lat: 22.0675
lon: -159.49277778
Kawaikini. Kawaikini is a shield volcano on the Hawaiian Island of Kauai and in Kauai County and measures in elevation. It is the summit of the island's inactive central shield volcano, Mount Waialeale. Other peaks on Kauai include: Waialeale (5,148 feet), Namolokama Mountain (4,421 feet), Kalalau Lookout (4,120 feet), Keanapuka Mountain (4,120 feet), Haupu (2,297 feet) and Nounou (1,241 feet).

Geographic entities mentioned:
surface_form: kawaikini
instance_of: Mountain
countries: United States
coordinates: lat: 22.0675
lon: -159.49277778
This high rainfall makes reaching the summit difficult on most days. The rain is not the only barrier to reaching Kawaikini. The Alakai Wilderness Preserve is located to the west and its miles of dense, swampy forest limit access to the summit. To the north, east, and south, Kawaikini is protected by steep, wet cliffs. Etymology.

Geographic entities mentioned:
surface_form: kawaikini
instance_of: Mountain
countries: United States
coordinates: lat: 22.0675
lon: -159.49277778
Gabriel served in the sultan's court for four years. Monastic life. In 1828, during the Greek War of Independence, he left Constantinople and took a boat to Gregoriou Monastery at Mount Athos. He was tonsured there as a monk and then moved to Kafsokalyvia, where he became a disciple of Father Neophytos Karamanlis.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Kopa Kondracka. Kopa Kondracka () is a mountain in the Western Tatras mountain range, situated on the main ridge of the Tatras east of Małołączniak, on the border between Poland and Slovakia. It's the easternmost of the four summits making up the Czerwone Wierchy massif, as well as the lowest, with an elevation of 2005 meters.

Geographic entities mentioned:
surface_form: Małołączniak
instance_of: Mountain
countries: Slovakia
Poland
coordinates: lat: 49.235805555556
lon: 19.919305555556
surface_form: kopa kondracka
instance_of: Mountain
countries: Slovakia
Poland
coordinates: lat: 49.2365
lon: 19.932222222222
Kopa Kondracka. Kopa Kondracka () is a mountain in the Western Tatras mountain range, situated on the main ridge of the Tatras east of Małołączniak, on the border between Poland and Slovakia. It's the easternmost of the four summits making up the Czerwone Wierchy massif, as well as the lowest, with an elevation of 2005 meters.

Geographic entities mentioned:
surface_form: kopa kondracka
instance_of: Mountain
countries: Slovakia
Poland
coordinates: lat: 49.2365
lon: 19.932222222222
Description. This species is similar in appearance to &quot;Pasiphila dryas&quot; but it lacks the pink-brown shade of the latter species. Distribution. This species is endemic to New Zealand and has been observed on Mount Taranaki and Mount Ruapehu in the North Island and on Ben Lomond, Bold Peak and around Lake Wakatipu, all in Otago in the South Island. &quot;P.

Geographic entities mentioned:
surface_form: Lake Wakatipu
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.085
lon: 168.561
Lava spine. A lava spine (or lava spire) is a vertical growth of solid lava that is forced from a volcanic vent. A lava spine can either be formed by viscous lava slowly being pushed out of the vent, or by magma that has solidified within the vent before being pushed out. In February 1983, the dome activity of Mount St.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
In November 2005, a new spine, called &quot;the slab&quot; grew continuously until late 2006, though it continually collapsed under its own weight; the growth finally stopped in January 2008, when Mount St. Helens' eruption ended. Another example is a spine that appeared on the lava dome of the Soufrière Hills Volcano in Montserrat prior to the volcano's eruption in 1997.

Geographic entities mentioned:
surface_form: Soufrière Hills
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 16.716666666667
lon: -62.183333333333
Anders Sandvig. Anders Sandvig (11 May 1862 &ndash; 11 February 1950) was a Norwegian dentist most noted for having founded Maihaugen, an innovative regional ethnological and architectural museum in Lillehammer, documenting the vernacular architecture of Gudbrandsdalen. Biography. Sandvig was born at Bud in Møre og Romsdal, Norway. He was the son of Sjur Sandvig and Maren Knudsdotter Hustad.

Geographic entities mentioned:
surface_form: Gudbrandsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.1333
lon: 10.35
During his stay in Germany, he was diagnosed with tuberculosis. In 1885, he moved to Lillehammer to start a dentist practice and promote his recovery. At this time he was the only dentist in Gudbrandsdalen. On a travel to Skjåk in 1894, he came to the realization that Norwegian farmers had not yet begun to appreciate their cultural heritage.

Geographic entities mentioned:
surface_form: Gudbrandsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.1333
lon: 10.35
The union was poised to launch its next major campaign in the lettuce fields in 1970 when a deal between the International Brotherhood of Teamsters and the growers nearly destroyed it. Initially, the Teamsters signed contracts with lettuce growers in the Salinas Valley, who wanted to avoid recognizing the UFW.

Geographic entities mentioned:
surface_form: Salinas Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.7654
lon: -121.7918