Sarmila/GeoWiki-Features huggingface dataset:
Blümcke Knoll. niqgnan8ddldbdrss09l6jyw0cy9w" xml:space="preserve">Blümcke Knoll () is a small steep-sided feature protruding through the ice of northern Adelaide Island, off the Antarctic Peninsula. It is about southwest of Mount Velain.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: blümcke knoll
instance_of: Mountain
coordinates: lat: -66.8333
lon: -68
Blümcke Knoll. niqgnan8ddldbdrss09l6jyw0cy9w" xml:space="preserve">Blümcke Knoll () is a small steep-sided feature protruding through the ice of northern Adelaide Island, off the Antarctic Peninsula. It is about southwest of Mount Velain.

Geographic entities mentioned:
surface_form: blümcke knoll
instance_of: Mountain
coordinates: lat: -66.8333
lon: -68
The species is native to eastern Australia. Etymology. The specific name, &quot;kosciuskoi&quot;, refers to Mount Kosciuszko, Australia's highest mountain, where the holotype was collected. Description. &quot;E. kosciuskoi&quot; may attain a snout-to-vent length (SVL) of. It has a narrow black vertebral stripe and yellow dorsolateral stripes. Geographic range. &quot;E.

Geographic entities mentioned:
surface_form: Mount Kosciuszko
instance_of: Mountain
countries: Australia
coordinates: lat: -36.4558303
lon: 148.2635105
Sanger moved to Jaffrey, New Hampshire, in Cheshire County, after his military service. He may have first worked there as a saddler. In 1777, he served on a committee of five to resist the annexation of a portion of Jaffrey by the neighboring Peterborough Slip. In 1782, he purchased a farm in Jaffrey near Gap Mountain. Alongside the farm, he operated a tavern and a small store on the property.

Geographic entities mentioned:
surface_form: Gap Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.8189
lon: -72.1378
Sanger himself farmed land in Sangerfield, as did relative William Cary Sanger much later in the century. Skaneateles. Sanger saw the potential of the area of Skaneateles Creek at the outlet of Skaneateles Lake and purchased large amounts of land there. He built a dam about 1796 or '97 and erected the first grist and sawmills there.

Geographic entities mentioned:
surface_form: Skaneateles Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.8625
lon: -76.372777777778
Federal Company. The Onondaga Salt Springs Reservation was a tract of land designated by the state legislature in 1797 around a natural salt spring for the commercialization of salt production in Salina on the shores of Onondaga Lake. Production began around 1789; salt was made by boiling the brine of the water.

Geographic entities mentioned:
surface_form: Onondaga Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.088888888889
lon: -76.208333333333
Mount Harmston. Mount Harmston is a mountain on Vancouver Island, British Columbia, Canada, located approximately southwest of Courtenay and north of The Red Pillar. Mount Harmston is part of the Vancouver Island Ranges which in turn form part of the Insular Mountains. History. Mount Harmston is named after the Harmston family, early settlers of the Comox Valley.

Geographic entities mentioned:
surface_form: The Red Pillar
instance_of: Mountain
countries: Canada
coordinates: lat: 49.5256
lon: -125.389
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount harmston
instance_of: Mountain
countries: Canada
coordinates: lat: 49.5489
lon: -125.398
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Harmston. Mount Harmston is a mountain on Vancouver Island, British Columbia, Canada, located approximately southwest of Courtenay and north of The Red Pillar. Mount Harmston is part of the Vancouver Island Ranges which in turn form part of the Insular Mountains. History. Mount Harmston is named after the Harmston family, early settlers of the Comox Valley.

Geographic entities mentioned:
surface_form: mount harmston
instance_of: Mountain
countries: Canada
coordinates: lat: 49.5489
lon: -125.398
Mount Harmston. Mount Harmston is a mountain on Vancouver Island, British Columbia, Canada, located approximately southwest of Courtenay and north of The Red Pillar. Mount Harmston is part of the Vancouver Island Ranges which in turn form part of the Insular Mountains. History. Mount Harmston is named after the Harmston family, early settlers of the Comox Valley.

Geographic entities mentioned:
surface_form: mount harmston
instance_of: Mountain
countries: Canada
coordinates: lat: 49.5489
lon: -125.398
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
Mount Harmston is part of the Vancouver Island Ranges which in turn form part of the Insular Mountains. History. Mount Harmston is named after the Harmston family, early settlers of the Comox Valley. They settled on a 200+ acre preemption in early December 1862, coming from Lincolnshire, England.

Geographic entities mentioned:
surface_form: mount harmston
instance_of: Mountain
countries: Canada
coordinates: lat: 49.5489
lon: -125.398
surface_form: comox valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.6798337
lon: -124.9694395
Multiple British squadrons were deployed into Russia as a part of the Allied intervention in the Russian Civil War. Between the Camel and the S.E.5, which were the two main types deployed to the Caspian Sea area to bomb Bolshevik bases and to provide aerial support to the Royal Navy warships present, Allied control of the Caspian region had been achieved by May 1919.

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
Rat Portage 38A. Rat Portage 38A is a First Nations reserve on Lake of the Woods in northwestern Ontario. It is one of two reserves of the Obashkaandagaang Bay First Nation.

Geographic entities mentioned:
surface_form: Lake of the Woods
instance_of: Lake
countries: Canada
United States
coordinates: lat: 49.09027777777778
lon: -95.2388888888889
Within the walls, the buildings were arranged around one or more open courts surrounded by cloisters. The usual arrangement for monasteries of the Eastern world is exemplified in the plan of the convent of the Great Lavra at Mount Athos. With reference to the diagram, right, the convent of the Great Lavra is enclosed within a strong and lofty blank stone wall.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Adoption of the Roman villa plan. Monasticism in the West began with the activities of Benedict of Nursia (born 480 AD). Near Nursia, a town in Perugia, Italy, a first abbey was established at Monte Cassino (529 AD). Between 520 and 700 AD, monasteries were built which were spacious and splendid.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
In the central pavilion there is a special area where you could see the “super mineral pieces”, called the VIP area. Since 2007, there has been a new Alpine Area. Selected strahlers (mineral hunters) from Germany, Italy, Austria, Switzerland and France display their new finds made in the highest alpine mountains like Mont Blanc massif.

Geographic entities mentioned:
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
Hurvat Amudim. Hurvat Amudim or Sde Amudim was an ancient village, now an archaeological site, in Israel, located south-east of the Beit Netofa Valley, on the eastern side of Highway 65 between Golani Interchange and Kadarim Junction. History. The name derives from the columns that once supported the roof of the synagogue and that remained standing. G.

Geographic entities mentioned:
surface_form: Beit Netofa Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.80956667
lon: 35.33246111
Little Yosemite Valley. Little Yosemite Valley is a smaller glacial valley upstream in the Merced River drainage from the Yosemite Valley in Yosemite National Park. The Merced River meanders through the long flat valley, draining out over Nevada Fall and Vernal Fall before emptying into the main Yosemite Valley.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: yosemite valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: little yosemite valley
instance_of: Valley
countries: United States
coordinates: lat: 37.7328
lon: -119.52
The Merced River meanders through the long flat valley, draining out over Nevada Fall and Vernal Fall before emptying into the main Yosemite Valley. It can be reached by a day hike from the main valley, and is the most popular area in the Yosemite Wilderness. The Valley provides access to nearby destinations such as the back side of Half Dome, Clouds Rest and the High Sierra Camp at Merced Lake.

Geographic entities mentioned:
surface_form: Half Dome
instance_of: Mountain
countries: United States
coordinates: lat: 37.746
lon: -119.53316666667
surface_form: Clouds Rest
instance_of: Mountain
countries: United States
coordinates: lat: 37.767852777778
lon: -119.48922777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
It lies adjacent, to the north of Nevada Fall, on the John Muir Trail at. It rises feet from the base of Nevada Fall to a peak elevation of. A smaller, mesa-like dome called Mount Broderick stands immediately adjacent to Liberty Cap. Together, they form a barrier on the north side of the mouth of Little Yosemite Valley.

Geographic entities mentioned:
surface_form: Mount Broderick
instance_of: Mountain
countries: United States
coordinates: lat: 37.73354
lon: -119.53516
surface_form: mount broderick
instance_of: Mountain
countries: United States
coordinates: lat: 37.73354
lon: -119.53516
surface_form: liberty cap
instance_of: Mountain
countries: United States
coordinates: lat: 37.7285
lon: -119.533
Half Dome. Half Dome is a granite dome in Yosemite National Park located at the northwestern end of Little Yosemite Valley at
— possibly Yosemite's most familiar rock formation. The granite crest rises more than above the Yosemite Valley floor at Tenaya Canyon and above the floor of Little Yosemite Valley.

Geographic entities mentioned:
surface_form: Half Dome
instance_of: Mountain
countries: United States
coordinates: lat: 37.746
lon: -119.53316666667
surface_form: yosemite valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: granite dome
instance_of: Mountain
countries: United States
coordinates: lat: 38.21519
lon: -119.74601
surface_form: little yosemite valley
instance_of: Valley
countries: United States
coordinates: lat: 37.7328
lon: -119.52
Half Dome. Half Dome is a granite dome in Yosemite National Park located at the northwestern end of Little Yosemite Valley at
— possibly Yosemite's most familiar rock formation. The granite crest rises more than above the Yosemite Valley floor at Tenaya Canyon and above the floor of Little Yosemite Valley.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: yosemite valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: yosemite valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: little yosemite valley
instance_of: Valley
countries: United States
coordinates: lat: 37.7328
lon: -119.52
Moraine Dome is notable because the presence of lateral moraines from the Merced Glacier. It is likely that these moraines represent the highest level attained by glacial ice in Little Yosemite Valley. Although it is about as high as Sentinel Dome Moraine Dome is dwarfed to relative insignificance by its proximity to the bulk and elevation of Clouds Rest to the north.

Geographic entities mentioned:
surface_form: Clouds Rest
instance_of: Mountain
countries: United States
coordinates: lat: 37.767852777778
lon: -119.48922777778
surface_form: clouds rest
instance_of: Mountain
countries: United States
coordinates: lat: 37.767852777778
lon: -119.48922777778
This cascade is often mistaken for Bunnell Cascade which is located between the Lost Valley and Echo Valley at. Bunnell Point. Bunnell Point is a granite dome summit in Mariposa County, California. Bunnell Point rises to AMSL. Bunnell Point is located at comprising the southeast margin of Little Yosemite Valley. Cascade Cliffs.

Geographic entities mentioned:
surface_form: Bunnell Point
instance_of: Mountain
countries: United States
coordinates: lat: 37.7391
lon: -119.467
surface_form: bunnell point
instance_of: Mountain
countries: United States
coordinates: lat: 37.7391
lon: -119.467
surface_form: granite dome
instance_of: Mountain
countries: United States
coordinates: lat: 38.21519
lon: -119.74601
Little Yosemite Valley. Little Yosemite Valley is a smaller glacial valley upstream in the Merced River drainage from the Yosemite Valley in Yosemite National Park. The Merced River meanders through the long flat valley, draining out over Nevada Fall and Vernal Fall before emptying into the main Yosemite Valley.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: little yosemite valley
instance_of: Valley
countries: United States
coordinates: lat: 37.7328
lon: -119.52
Little Yosemite Valley is a smaller glacial valley upstream in the Merced River drainage from the Yosemite Valley in Yosemite National Park. The Merced River meanders through the long flat valley, draining out over Nevada Fall and Vernal Fall before emptying into the main Yosemite Valley. It can be reached by a day hike from the main valley, and is the most popular area in the Yosemite Wilderness.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
The Valley provides access to nearby destinations such as the back side of Half Dome, Clouds Rest and the High Sierra Camp at Merced Lake. Little Yosemite Valley is a tread on the glacial stairway of the Merced River that runs from Yosemite Valley up to Mount Lyell, gaining some of vertical elevation over and is situated some in elevation above Yosemite Valley proper. Geology.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: mount lyell
instance_of: Mountain
countries: United States
coordinates: lat: 37.7394
lon: -119.272
surface_form: little yosemite valley
instance_of: Valley
countries: United States
coordinates: lat: 37.7328
lon: -119.52
The north wall in contrast, and similarly to the north wall of Yosemite Valley, has been subject to much less glacial planing and is much more differentiated and vegetated. Liberty Cap and Mount Broderick. Liberty Cap is a granite dome in Yosemite National Park, California, United States, which lies at the extreme northwestern margin of Little Yosemite Valley.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
Liberty Cap and Mount Broderick. Liberty Cap is a granite dome in Yosemite National Park, California, United States, which lies at the extreme northwestern margin of Little Yosemite Valley. It lies adjacent, to the north of Nevada Fall, on the John Muir Trail at. It rises feet from the base of Nevada Fall to a peak elevation of.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: granite dome
instance_of: Mountain
countries: United States
coordinates: lat: 38.21519
lon: -119.74601
surface_form: little yosemite valley
instance_of: Valley
countries: United States
coordinates: lat: 37.7328
lon: -119.52
It lies adjacent, to the north of Nevada Fall, on the John Muir Trail at. It rises feet from the base of Nevada Fall to a peak elevation of. A smaller, mesa-like dome called Mount Broderick stands immediately adjacent to Liberty Cap. Together, they form a barrier on the north side of the mouth of Little Yosemite Valley.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: little yosemite valley
instance_of: Valley
countries: United States
coordinates: lat: 37.7328
lon: -119.52
The granite crest rises more than above the Yosemite Valley floor at Tenaya Canyon and above the floor of Little Yosemite Valley. The trail to Half Dome branches to the north from the main Little Yosemite Valley trail near the ranger station, out houses and campground. Moraine Dome.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: half dome
instance_of: Mountain
countries: United States
coordinates: lat: 37.746
lon: -119.53316666667
surface_form: little yosemite valley
instance_of: Valley
countries: United States
coordinates: lat: 37.7328
lon: -119.52
Moraine Dome. Moraine Dome is a granite dome in Yosemite National Park along the northern margin of Little Yosemite Valley at which rises to an elevation of AMSL, above the Merced River. Moraine Dome is notable because the presence of lateral moraines from the Merced Glacier. It is likely that these moraines represent the highest level attained by glacial ice in Little Yosemite Valley.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: granite dome
instance_of: Mountain
countries: United States
coordinates: lat: 38.21519
lon: -119.74601
surface_form: little yosemite valley
instance_of: Valley
countries: United States
coordinates: lat: 37.7328
lon: -119.52
Moraine Dome is notable because the presence of lateral moraines from the Merced Glacier. It is likely that these moraines represent the highest level attained by glacial ice in Little Yosemite Valley. Although it is about as high as Sentinel Dome Moraine Dome is dwarfed to relative insignificance by its proximity to the bulk and elevation of Clouds Rest to the north.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: little yosemite valley
instance_of: Valley
countries: United States
coordinates: lat: 37.7328
lon: -119.52
Sugar Loaf. Sugar Loaf Dome is a granite dome in Yosemite National Park at the northeastern head of Little Yosemite Valley at which rises to AMSL. Although Sugar Loaf Dome has been repeatedly subject to glaciation, the core of this spur has resisted the icy onslaughts because what remains today is massive throughout except for one master joint, horizontal in character.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: granite dome
instance_of: Mountain
countries: United States
coordinates: lat: 38.21519
lon: -119.74601
surface_form: little yosemite valley
instance_of: Valley
countries: United States
coordinates: lat: 37.7328
lon: -119.52
Cascade Fall. Cascade Fall at, elevation AMSL tumbles via a water wheel over the glacially polished granite saddle between Sugar Loaf and Bunnell Point into a delightful pool at the eastern head of Little Yosemite Valley. This cascade is often mistaken for Bunnell Cascade which is located between the Lost Valley and Echo Valley at. Bunnell Point.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: sugar loaf
instance_of: Landform
countries: United States
coordinates: lat: 44.028342
lon: -91.626792
surface_form: bunnell point
instance_of: Mountain
countries: United States
coordinates: lat: 37.7391
lon: -119.467
surface_form: little yosemite valley
instance_of: Valley
countries: United States
coordinates: lat: 37.7328
lon: -119.52
This cascade is often mistaken for Bunnell Cascade which is located between the Lost Valley and Echo Valley at. Bunnell Point. Bunnell Point is a granite dome summit in Mariposa County, California. Bunnell Point rises to AMSL. Bunnell Point is located at comprising the southeast margin of Little Yosemite Valley. Cascade Cliffs.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: little yosemite valley
instance_of: Valley
countries: United States
coordinates: lat: 37.7328
lon: -119.52
Cascade Cliffs. Cascade Cliffs is a wall of unjointed granite that rises to AMSL, above the Merced River and make up the southern wall of Little Yosemite Valley at, southwest of Bunnell Point and northeast of Mount Starr King, of which Cascade Cliffs comprises the northern flank. In few other places in the Yosemite region is the granite more continuously massive than in the Cascade Cliffs.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: mount starr king
instance_of: Mountain
countries: United States
coordinates: lat: 44.4347
lon: -71.433
surface_form: bunnell point
instance_of: Mountain
countries: United States
coordinates: lat: 37.7391
lon: -119.467
surface_form: mount starr
instance_of: Mountain
countries: United States
coordinates: lat: 37.429166666667
lon: -118.765
surface_form: mount starr king
instance_of: Mountain
countries: United States
coordinates: lat: 37.7027
lon: -119.518
surface_form: little yosemite valley
instance_of: Valley
countries: United States
coordinates: lat: 37.7328
lon: -119.52
They comprise two domes, West Quarter Dome and East Quarter Dome. The higher of the two is East Quarter Dome, at; West Quarter Dome stands at. Trail. The Merced River enters Little Yosemite Valley at at the pool at the base of the cascade and leaves the valley at for a total elevation difference of over a trail length of.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: little yosemite valley
instance_of: Valley
countries: United States
coordinates: lat: 37.7328
lon: -119.52
Campground. The hike-in campground here is a little under 4 miles (6.5 km) from the trailhead in Yosemite Valley and about 3.5 miles (5.5 km) from the summit of Half Dome at. Fires are allowed in the two communal campfire rings just outside the campground. Potable (drinking) water is not available at the campground. River water is available nearby, at the Merced River.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: half dome
instance_of: Mountain
countries: United States
coordinates: lat: 37.746
lon: -119.53316666667
The Merced River meanders through the long flat valley, draining out over Nevada Fall and Vernal Fall before emptying into the main Yosemite Valley. It can be reached by a day hike from the main valley, and is the most popular area in the Yosemite Wilderness. The Valley provides access to nearby destinations such as the back side of Half Dome, Clouds Rest and the High Sierra Camp at Merced Lake.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
Geology. The north wall of Little Yosemite has not been subject to the same kinds of glacial planing as the south wall because the granite rocks of Moraine Dome and Sugar Bowl Dome are tougher and more resistant.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
This is remarkable considering that it is likely that Little Yosemite was not only scoured repeatedly by glaciers that were wholly contained by the canyon, but also overrun by glaciers that overflowed the Merced canyon and spread widely into surrounding uplands with occasional surges of ice contributed over the pass from the overflowing Tuolumne River basin.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
The west end and south wall of the canyon are &quot;exceptionally massive, few cliffs anywhere in the Yosemite region exhibit a more complete absence of fractures.&quot; This also leads to an almost complete absence of vegetation as well, as there are few opportunities for roothold.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
Post-glaciation, Sugar Loaf Dome retains a 1,300 feet rise over, and its shoulder perturbs the course of the Merced River and provides the relief over which the river descends into Little Yosemite via Cascade Fall. Cascade Fall.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: sugar loaf
instance_of: Landform
countries: United States
coordinates: lat: 44.028342
lon: -91.626792
Cascade Cliffs. Cascade Cliffs is a wall of unjointed granite that rises to AMSL, above the Merced River and make up the southern wall of Little Yosemite Valley at, southwest of Bunnell Point and northeast of Mount Starr King, of which Cascade Cliffs comprises the northern flank. In few other places in the Yosemite region is the granite more continuously massive than in the Cascade Cliffs.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
The river is the only water source for the area. Little Yosemite Valley Ranger Station is staffed during summer. A composting toilet is available for use near the campground
The Park Service provides communal food lockers at the campground in which to store food, toiletries, and trash safe from abundant hungry black bears that frequent Little Yosemite.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
The north wall in contrast, and similarly to the north wall of Yosemite Valley, has been subject to much less glacial planing and is much more differentiated and vegetated. Liberty Cap and Mount Broderick. Liberty Cap is a granite dome in Yosemite National Park, California, United States, which lies at the extreme northwestern margin of Little Yosemite Valley.

Geographic entities mentioned:
surface_form: mount broderick
instance_of: Mountain
countries: United States
coordinates: lat: 37.73354
lon: -119.53516
surface_form: liberty cap
instance_of: Mountain
countries: United States
coordinates: lat: 37.7285
lon: -119.533
Together, they form a barrier on the north side of the mouth of Little Yosemite Valley. Both Liberty Cap and Mount Broderick are roches moutonnées, features that protruded above or resisting being overridden by successive Merced River glaciers because they are made of massive unjointed granite sufficiently resistant to glacial erosive power, leaving them prominent in the post-glacial landscape.

Geographic entities mentioned:
surface_form: mount broderick
instance_of: Mountain
countries: United States
coordinates: lat: 37.73354
lon: -119.53516
There are two wide, relatively short yet quite deep arches at the bottom of the cliff. The Quarter Domes. The Quarter Domes are granodiorite domes rising between Half Dome and Clouds Rest. They comprise two domes, West Quarter Dome and East Quarter Dome. The higher of the two is East Quarter Dome, at; West Quarter Dome stands at. Trail.

Geographic entities mentioned:
surface_form: clouds rest
instance_of: Mountain
countries: United States
coordinates: lat: 37.767852777778
lon: -119.48922777778
surface_form: half dome
instance_of: Mountain
countries: United States
coordinates: lat: 37.746
lon: -119.53316666667
Both features are glacially polished on their glacier-facing side and ragged on their leeward side. Half Dome. Half Dome is a granite dome in Yosemite National Park located at the northwestern end of Little Yosemite Valley at
— possibly Yosemite's most familiar rock formation.

Geographic entities mentioned:
surface_form: half dome
instance_of: Mountain
countries: United States
coordinates: lat: 37.746
lon: -119.53316666667
Although it is about as high as Sentinel Dome Moraine Dome is dwarfed to relative insignificance by its proximity to the bulk and elevation of Clouds Rest to the north. The south western margin of Moraine Dome is wrapped by a broad, striped granite apron with an approximately 40° slope that appears to rise some from the valley floor. Sugar Loaf.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The south western margin of Moraine Dome is wrapped by a broad, striped granite apron with an approximately 40° slope that appears to rise some from the valley floor. Sugar Loaf. Sugar Loaf Dome is a granite dome in Yosemite National Park at the northeastern head of Little Yosemite Valley at which rises to AMSL.

Geographic entities mentioned:
surface_form: sugar loaf
instance_of: Landform
countries: United States
coordinates: lat: 44.028342
lon: -91.626792
Cascade Fall. Cascade Fall at, elevation AMSL tumbles via a water wheel over the glacially polished granite saddle between Sugar Loaf and Bunnell Point into a delightful pool at the eastern head of Little Yosemite Valley. This cascade is often mistaken for Bunnell Cascade which is located between the Lost Valley and Echo Valley at. Bunnell Point.

Geographic entities mentioned:
surface_form: echo valley
instance_of: Valley
countries: United States
coordinates: lat: 37.743888888889
lon: -119.43444444444
This cascade is often mistaken for Bunnell Cascade which is located between the Lost Valley and Echo Valley at. Bunnell Point. Bunnell Point is a granite dome summit in Mariposa County, California. Bunnell Point rises to AMSL. Bunnell Point is located at comprising the southeast margin of Little Yosemite Valley. Cascade Cliffs.

Geographic entities mentioned:
surface_form: bunnell point
instance_of: Mountain
countries: United States
coordinates: lat: 37.7391
lon: -119.467
These rocks were thus subject to tremendous gravitational and flow forces yet retain a remarkable degree of integrity, eroding almost exclusively and superficially along exfoliation joints. The south wall of the valley has been subject to extensive glacial planing, with all jointed granite completely smoothed away, leaving a stark, featureless unjointed sheer cliff face, as is apparent in.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
It is located at the southern edge of the district's area, along the border with the district of Sigmaringen. Allmannsweiler is physically located in the basin of the Federsee. Elevation above sea level in the municipal area ranges from a high of Normalnull (NN) to a low of NN. Culture. The architecture of Allmannsweiler is primarily made up of Baroque farmhouses and half-timber buildings.

Geographic entities mentioned:
surface_form: Federsee
instance_of: Lake
countries: Germany
coordinates: lat: 48.083333333333
lon: 9.6333333333333
The ruler Tupac Inca Yupanqui (1471-1493) is credited with the conquest of the south extending their domains Tahuantisuyo in Diaguita territory. The expedition was prepared under the leadership of General Sinchiruca, with over ten thousand soldiers who fought for six years between Copiapo and Aconcagua. Some argue that the Inca domination lasted 50 to 75 years until the arrival of the Spaniards.

Geographic entities mentioned:
surface_form: Aconcagua
instance_of: Mountain
countries: Argentina
coordinates: lat: -32.653055555555554
lon: -70.01166666666667
Kawdy Mountain. Kawdy Mountain is a subglacial mound on the Kawdy Plateau, the northernmost sub-plateau of the Stikine Plateau in northwestern British Columbia, Canada. It consists of nearly horizontal beds of basaltic lava, capping outward dipping beds of fragmental volcanic rocks and last erupted in Pleistocene.

Geographic entities mentioned:
surface_form: Kawdy Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 59.24948
lon: -131.50356
surface_form: Stikine Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: kawdy mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 58.88
lon: -131.23
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Kawdy Mountain. Kawdy Mountain is a subglacial mound on the Kawdy Plateau, the northernmost sub-plateau of the Stikine Plateau in northwestern British Columbia, Canada. It consists of nearly horizontal beds of basaltic lava, capping outward dipping beds of fragmental volcanic rocks and last erupted in Pleistocene.

Geographic entities mentioned:
surface_form: kawdy mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 58.88
lon: -131.23
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
It consists of nearly horizontal beds of basaltic lava, capping outward dipping beds of fragmental volcanic rocks and last erupted in Pleistocene. Kawdy Mountain is one of many basaltic volcanic features of the Stikine Volcanic Belt, which is forming because the North American tectonic plate is stretching slightly as it moves to the west.

Geographic entities mentioned:
surface_form: kawdy mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 58.88
lon: -131.23
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
It is located in the Lima Region, Cajatambo Province, Cajatambo District. Waylla Hirka lies at the Pumarinri valley south of the Waywash mountain range, southwest of Pukaqaqa and north of Millpu. The lakes Quyllurqucha, Warmiqucha (Quechua for &quot;woman lake&quot;, &quot;Huarmicocha&quot;) and Challwaqucha (&quot;fish lake&quot;, &quot;Challhuacocha&quot;) lie northeast of Waylla Hirka.

Geographic entities mentioned:
surface_form: huarmicocha
instance_of: Lake
countries: Peru
coordinates: lat: -12.7089
lon: -75.5269
surface_form: waylla hirka
instance_of: Mountain
countries: Peru
coordinates: lat: -10.53305556
lon: -76.85694444
surface_form: waylla hirka
instance_of: Mountain
countries: Peru
coordinates: lat: -10.455
lon: -76.8658
surface_form: challhuacocha
instance_of: Lake
countries: Peru
coordinates: lat: -13.371325
lon: -71.85291111
surface_form: challwaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -11.0425
lon: -76.5556
surface_form: challwaqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -11.5119
lon: -76.1358
surface_form: challwaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -12.649444444444
lon: -75.716388888889
It is located in the Lima Region, Cajatambo Province, Cajatambo District. Waylla Hirka lies at the Pumarinri valley south of the Waywash mountain range, southwest of Pukaqaqa and north of Millpu. The lakes Quyllurqucha, Warmiqucha (Quechua for &quot;woman lake&quot;, &quot;Huarmicocha&quot;) and Challwaqucha (&quot;fish lake&quot;, &quot;Challhuacocha&quot;) lie northeast of Waylla Hirka.

Geographic entities mentioned:
surface_form: millpu
instance_of: Mountain
countries: Peru
coordinates: lat: -9.30888889
lon: -76.8375
surface_form: millpu
instance_of: Mountain
countries: Peru
coordinates: lat: -11.635
lon: -76.3017
surface_form: pukaqaqa
instance_of: Mountain
countries: Peru
coordinates: lat: -10.4347
lon: -76.8561
surface_form: millpu
instance_of: Mountain
countries: Peru
coordinates: lat: -10.4628
lon: -76.8536
Waylla Hirka (Cajatambo). Waylla Hirka (Quechua &quot;waylla&quot; meadow, Ancash Quechua &quot;hirka&quot; mountain, &quot;meadow mountain&quot;, Hispanicized spelling &quot;Huayllajirca&quot;) is a mountain in the Andes of Peru, about high. It is located in the Lima Region, Cajatambo Province, Cajatambo District.

Geographic entities mentioned:
surface_form: waylla hirka
instance_of: Mountain
countries: Peru
coordinates: lat: -10.53305556
lon: -76.85694444
surface_form: waylla hirka (cajatambo)
instance_of: Mountain
countries: Peru
coordinates: lat: -10.455
lon: -76.8658
Waylla Hirka (Cajatambo). Waylla Hirka (Quechua &quot;waylla&quot; meadow, Ancash Quechua &quot;hirka&quot; mountain, &quot;meadow mountain&quot;, Hispanicized spelling &quot;Huayllajirca&quot;) is a mountain in the Andes of Peru, about high. It is located in the Lima Region, Cajatambo Province, Cajatambo District.

Geographic entities mentioned:
surface_form: waylla hirka
instance_of: Mountain
countries: Peru
coordinates: lat: -10.53305556
lon: -76.85694444
surface_form: huayllajirca
instance_of: Mountain
countries: Peru
coordinates: lat: -10.53305556
lon: -76.85694444
surface_form: waylla hirka
instance_of: Mountain
countries: Peru
coordinates: lat: -10.455
lon: -76.8658
Mount Rosenthal. Mount Rosenthal () is a prominent mountain, 1,840 m, at the north end of Liberty Hills, in the Heritage Range, Ellsworth Mountains. Named by Advisory Committee on Antarctic Names (US-ACAN) for Lieutenant Commander Ronald Rosenthal, U.S. Navy, navigator on LC-47 aircraft, who perished in a crash on the Ross Ice Shelf, February 2, 1966.

Geographic entities mentioned:
surface_form: rosenthal
instance_of: Mountain
coordinates: lat: -80.05
lon: -83.25
surface_form: mount rosenthal
instance_of: Mountain
coordinates: lat: -80.05
lon: -83.25
Mount Rosenthal. Mount Rosenthal () is a prominent mountain, 1,840 m, at the north end of Liberty Hills, in the Heritage Range, Ellsworth Mountains. Named by Advisory Committee on Antarctic Names (US-ACAN) for Lieutenant Commander Ronald Rosenthal, U.S. Navy, navigator on LC-47 aircraft, who perished in a crash on the Ross Ice Shelf, February 2, 1966.

Geographic entities mentioned:
surface_form: rosenthal
instance_of: Mountain
coordinates: lat: -80.05
lon: -83.25
Cow Myers (wetland). Cow Myers is a Site of Special Scientific Interest (SSSI) located in the Nidderdale Area of Outstanding Natural Beauty (AONB), near Ripon, North Yorkshire, England. The site was designated in 1984 for its fen and alder carr habitat, which supports a diversity of wetland plant life.

Geographic entities mentioned:
surface_form: Nidderdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.0867
lon: -1.75773
Its level and marshy land surrounds Kex Beck, where it flows between Ellington Banks and the hamlet of Cow Myers, north west of Ripon, North Yorkshire. It is part of the Nidderdale Area of Outstanding Natural Beauty (AONB), and it is also a Site of Importance for Nature Conservation (SINC). The site is fed by springs, and is surrounded by alder carr.

Geographic entities mentioned:
surface_form: Nidderdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.0867
lon: -1.75773
Mount Manunggal. Mount Manunggal is the third-highest peak in the island of Cebu after Osmena Peak and Lugsangan Peak. It is located in Barangay Magsaysay in Balamban, Cebu province, rising above sea level. It is the site of the crash of the presidential plane &quot;Mt. Pinatubo&quot; that killed President Ramon Magsaysay and 24 others on March 17, 1957. History.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
History. Mount Manunggal is within the Central Cebu Protected Landscape and is protected by &quot;Republic Act 9486&quot;, otherwise known as the “Central Cebu Protected Landscape Act”; which also covers the Mananga-Kotkot-Lusaran river system, the Sudlon National Park and the watersheds of Buhisan, Mananga and Lusaran. It is the site of the crash of the presidential plane &quot;Mt.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Mount Manunggal. Mount Manunggal is the third-highest peak in the island of Cebu after Osmena Peak and Lugsangan Peak. It is located in Barangay Magsaysay in Balamban, Cebu province, rising above sea level. It is the site of the crash of the presidential plane &quot;Mt. Pinatubo&quot; that killed President Ramon Magsaysay and 24 others on March 17, 1957. History.

Geographic entities mentioned:
surface_form: manunggal
instance_of: Mountain
countries: Philippines
coordinates: lat: 10.453055555555556
lon: 123.815
surface_form: mount manunggal
instance_of: Mountain
countries: Philippines
coordinates: lat: 10.453055555555556
lon: 123.815
Accessibility. The trail to Mount Manunggal from the jump-off point at the river that separates Cebu City from Balamban is quite steep and takes between 2 and 7 hours to traverse. The trail to Mount Manunggal from Tagba-o is absent of forest canopies and wildlife, and traverses through many upland farms planted with onions, tomatoes, ginger, garlic, eggplants, cabbage, carrots, etc.

Geographic entities mentioned:
surface_form: manunggal
instance_of: Mountain
countries: Philippines
coordinates: lat: 10.453055555555556
lon: 123.815
surface_form: mount manunggal
instance_of: Mountain
countries: Philippines
coordinates: lat: 10.453055555555556
lon: 123.815
Monument. At the campsite, the monument to President Magsaysay and the cylinder block of one of the &quot;Pinatubos engines remind visitors of the historical value of Manunggal in Philippine history. A chapel, erected nearby during the height of a communist insurgency in the 1980s, guides the local inhabitants' spiritual yearning.

Geographic entities mentioned:
surface_form: manunggal
instance_of: Mountain
countries: Philippines
coordinates: lat: 10.453055555555556
lon: 123.815
Nikon of Karoulia. Hieromonk Nikon of Karoulia (also known as Nikon Karulskiy,; born Nikolai Nikolaevich (von) Strandtman,; also known as Nikon N. Strandtman; 4 September 1875, Grodno, Belarus – 20 September 1963, Mount Athos, Greece) was a Russian military officer and Orthodox monk. During his later years, he was known as a hesychast hermit and starets in Karoulia, Mount Athos.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Hieromonk Nikon of Karoulia (also known as Nikon Karulskiy,; born Nikolai Nikolaevich (von) Strandtman,; also known as Nikon N. Strandtman; 4 September 1875, Grodno, Belarus – 20 September 1963, Mount Athos, Greece) was a Russian military officer and Orthodox monk. During his later years, he was known as a hesychast hermit and starets in Karoulia, Mount Athos. Early life and military career.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
He was also a member of the Indian branch of the Theosophical Society in St. Petersburg but later quit, saying that the society had told him that &quot;love was a degradation and that the mind was the highest thing.&quot;
Monastic life. He moved to Mount Athos in 1935 or 1936 and became a hieromonk in the cell of St. John the Chrysostom of Hilandar Monastery at Mount Athos.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Traditionally, they were predominantly distributed in the districts of Durg, Raipur, Bastar, Nagpur and Bhandara. History. Raut may have been a tribal militia in Chhota Nagpur, originating from the Kawar
Culture. Traditionally, the Rauts were involved in herding and milking cattle. Traditionlly, their main business was sale of milk and milk products.

Geographic entities mentioned:
surface_form: Chhota Nagpur
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
Quebrada Limas. Quebrada Limas is a small river of Bogotá that originates in the path of Quiba, in the rural part of the Ciudad Bolívar and therefore, it is a tributary of the Tunjuelo River. General characteristics.

Geographic entities mentioned:
surface_form: Tunjuelo River
instance_of: Watercourse
countries: Colombia
coordinates: lat: 4.30708333
lon: -74.13061111
The eastern part of Harvard is on a large ridgeline. In 1931 Harvard College established the Oak Ridge Observatory at an elevation of 609 feet on Pinnacle Rd, the highest point between Mount Wachusett and the ocean. Harvard is largely wooded with rolling hills, fields, and wetlands.

Geographic entities mentioned:
surface_form: Mount Wachusett
instance_of: Mountain
countries: United States
coordinates: lat: 42.488888888889
lon: -71.8875
The island has a rectangular outline and is the remnant of three mostly eroded volcanoes. The highest point of the island, Quadrant Peak, directly overlies the coast. Inland Vindication Island features a rich vegetation, consisting of lichens and mosses, while various bird and penguin species breed along the coasts. There is no evidence of recent volcanic activity. History and toponymy.

Geographic entities mentioned:
surface_form: Quadrant Peak
instance_of: Mountain
countries: South Georgia and the South Sandwich Islands
United Kingdom
coordinates: lat: -57.1
lon: -26.78333333