Sarmila/GeoWiki-Features huggingface dataset:
It is an alluvial basin containing numerous lakes, remnants of a single lake that covered the valley floor up to deep during the Pleistocene epoch. Today, steep cliffs rise above a chain of endorheic lakes, such as Hart Lake, known collectively as the Warner Lakes. The valley has two regions commonly referred to as the South Warner Valley and the North Warner Valley.

Geographic entities mentioned:
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
surface_form: warner lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 42.4499
lon: -119.851
The deepest part of the lake is at its north end, while the south half is comparatively shallow. Hart Lake not only gets the overflow from Crump Lake, but also receives a steady flow of fresh water from Honey Creek. As a result, Hart Lake has the most stable water level within the Warner Lakes chain. Any outflow during high water drains into Anderson Lake, just north of Hart Lake.

Geographic entities mentioned:
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
surface_form: warner lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 42.4499
lon: -119.851
As a result, Hart Lake has the most stable water level within the Warner Lakes chain. Any outflow during high water drains into Anderson Lake, just north of Hart Lake. The water in Hart Lake is quite murky due to suspended particles stirred up from the shallow bottom by wave action. However, water clarity is not a good indicator of the lake's trophic state.

Geographic entities mentioned:
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
This is due to the reduced light level in the lake's cloudy waters, so overall, the lake is classified as eutrophic, with very high turbidity. Ecology. In addition to the lake's fish population, Hart Lake provides a unique habitat for plants and animals along the shore. The west-facing slope of Hart Mountain runs along the eastern shore of the lake.

Geographic entities mentioned:
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
In addition, willow, cottonwood, choke cherry, and wild roses are found near the lake. Local wildlife includes common high desert mammals, resident birds, and migrant waterfowl. Hart Lake's native fish species include the Warner sucker, tui chub, and Great Basin redband trout. The redband trout and small populations of the other species are also found in Honey Creek.

Geographic entities mentioned:
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
The redband trout and small populations of the other species are also found in Honey Creek. These stream-dwelling populations have likely been the source for re-colonizing Hart Lake after extended drought killed the lake populations. In addition to the native fish, rainbow trout, crappie, smallmouth bass, and bullhead catfish have been introduced into the lake.

Geographic entities mentioned:
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
These non-native species have put significant pressure on some of the native fish, which is why the Warner sucker is classified as &quot;threatened&quot; species. A 1996 fish survey estimated the total population of adult Warner suckers resident in Hart Lake at only 493 individuals.

Geographic entities mentioned:
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
To help preserve and restore the lake's threatened fish populations, the Fish and Wildlife Service developed a species recovery plan in 1998. There are 42 mammal species that live in the areas around Hart Lake. Mammals common in the Hart Lake shoreline and marshes include raccoons, striped skunks, and muskrats.

Geographic entities mentioned:
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
There are 42 mammal species that live in the areas around Hart Lake. Mammals common in the Hart Lake shoreline and marshes include raccoons, striped skunks, and muskrats. There are 264 species of birds that inhabit the area around Hart Lake or stop at the lake during migration.

Geographic entities mentioned:
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
Just north of Hart Lake, at the Warner Wetlands Interpretive Site, there are bird observation blinds maintained by the Bureau of Land Management where American bitterns, black-necked stilts, cinnamon teal, tundra swans, Brewer's blackbirds, western meadowlarks, nighthawks, and several swallow varieties are commonly observed.

Geographic entities mentioned:
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
In the meadows and marshes around Hart Lake, dusky flycatchers, yellow warblers, orange-crowned warblers, house wrens, and spotted towhees are common in the summer months. The larger birds common to the Hart Lake area include great horned owls, long-eared owls, turkey vultures, prairie falcons, red-tailed hawks, marsh hawks, golden eagles, and bald eagles. History.

Geographic entities mentioned:
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
History. Native Americans used the Warner Valley's lakes and wetlands for thousands of years before the first white explorers arrived. The natives made petroglyphs along the eastern shore of Hart Lake, some of which are dated to 12,000 years ago. The Greaser Petroglyph Site, approximately southeast of Hart Lake, is listed on the National Register of Historic Places.

Geographic entities mentioned:
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
Native Americans used the Warner Valley's lakes and wetlands for thousands of years before the first white explorers arrived. The natives made petroglyphs along the eastern shore of Hart Lake, some of which are dated to 12,000 years ago. The Greaser Petroglyph Site, approximately southeast of Hart Lake, is listed on the National Register of Historic Places. In December 1843, Captain John C.

Geographic entities mentioned:
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
The Greaser Petroglyph Site, approximately southeast of Hart Lake, is listed on the National Register of Historic Places. In December 1843, Captain John C. Fremont led a party of explorers through the Warner Valley. Fremont and his party spent Christmas Day camped near Hart Lake. In honor of the date, Fremont named it &quot;Christmas Valley&quot; and the lake &quot;Christmas Lake&quot;.

Geographic entities mentioned:
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
Wilson and his son-in-law C.G. Alexander. Later in the 19th century, much of the private land near Hart Lake was acquired by physician Bernard Daly and became part of his &quot;7T Ranch&quot;. By 1916, the 7T Ranch encompassed more than north and west of Hart Lake. Beginning with the earliest pioneer ranchers, water from Honey Creek was diverted for irrigation.

Geographic entities mentioned:
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
By 1916, the 7T Ranch encompassed more than north and west of Hart Lake. Beginning with the earliest pioneer ranchers, water from Honey Creek was diverted for irrigation. By the 1930s, irrigation canals had significantly reduced the flow of water into Hart Lake. In most years, the diversions did not stop the flow into the lake.

Geographic entities mentioned:
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
By the 1930s, irrigation canals had significantly reduced the flow of water into Hart Lake. In most years, the diversions did not stop the flow into the lake. However, during periods of drought, the entire flow of fresh water was diverted, visibly lowering the water level in Hart Lake. The canal structures also impeded fish migration between the lake and Honey Creek's habitat.

Geographic entities mentioned:
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
The canal structures also impeded fish migration between the lake and Honey Creek's habitat. In 1950, a dike was constructed at the north end of the lake to increase its water holding capacity. In the late 1980s and early 1990s, the Warner Valley experienced an extended drought, reducing the water in Hart Lake to a dangerously low level. In 1992, the lake dried up completely.

Geographic entities mentioned:
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
Upon the end of the drought, the fish were reintroduced in the lake. In 1998, the FWS published a recovery plan for threatened fish species in the Warner Lakes system. Recreation. Most of the land to the south and east of Hart Lake is privately owned. However, the Bureau of Land Management administers the Warner Wetlands north of the lake.

Geographic entities mentioned:
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
These public lands offer numerous recreational opportunities such as hunting, fishing, bird watching, boating, and camping. However, some of these activities are dependent on the water levels of the Warner Lakes, which can fluctuate dramatically. Due to Hart Lake's stable water level, it is usually available for fishing and boating.

Geographic entities mentioned:
surface_form: warner lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 42.4499
lon: -119.851
Due to Hart Lake's stable water level, it is usually available for fishing and boating. There are no developed campgrounds near Hart Lake, although dispersed camping is allowed on BLM-administered lands adjacent to the lake. There is a day-use recreation site at the north end of Hart Lake at Hart Bar.

Geographic entities mentioned:
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
There are no developed campgrounds near Hart Lake, although dispersed camping is allowed on BLM-administered lands adjacent to the lake. There is a day-use recreation site at the north end of Hart Lake at Hart Bar. There are also public restrooms, sheltered picnic tables, and hiking trails at the Warner Wetlands Interpretive Site, north of Hart Lake.

Geographic entities mentioned:
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
Ecology. In addition to the lake's fish population, Hart Lake provides a unique habitat for plants and animals along the shore. The west-facing slope of Hart Mountain runs along the eastern shore of the lake. This area is typical high desert scrubland dominated by big sagebrush and desert grasses.

Geographic entities mentioned:
surface_form: hart mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.4597
lon: -119.741
However, the Bureau of Land Management administers the Warner Wetlands north of the lake. In addition, the land along the east shore is part of the Hart Mountain National Antelope Refuge, which is managed by the United States Fish and Wildlife Service. These public lands offer numerous recreational opportunities such as hunting, fishing, bird watching, boating, and camping.

Geographic entities mentioned:
surface_form: hart mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.4597
lon: -119.741
Geography and geology. Hart Lake is located in the Warner Valley in south-central Oregon. It is a natural lake that covers and is approximately long and wide. Annual precipitation in the Hart Lake basin averages from. The valley is approximately long and wide. Most of the valley is in Lake County; however, the north end extends about into Harney County.

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
Annual precipitation in the Hart Lake basin averages from. The valley is approximately long and wide. Most of the valley is in Lake County; however, the north end extends about into Harney County. It is an alluvial basin containing numerous lakes, remnants of a single lake that covered the valley floor up to deep during the Pleistocene epoch.

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
Most of the valley is in Lake County; however, the north end extends about into Harney County. It is an alluvial basin containing numerous lakes, remnants of a single lake that covered the valley floor up to deep during the Pleistocene epoch. Today, steep cliffs rise above a chain of endorheic lakes, such as Hart Lake, known collectively as the Warner Lakes.

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
In honor of the date, Fremont named it &quot;Christmas Valley&quot; and the lake &quot;Christmas Lake&quot;. However, early mapmakers mistakenly plotted Christmas Valley northwest of its actual location, leaving the valley and its lakes unnamed on early maps. In 1867, General George Crook decided to build a fort in the Warner Valley to prevent Indian raiding parties from passing through the area.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Before the lake water had disappeared, the Fish and Wildlife Service captured a number of Warner suckers for temporary relocation. Upon the end of the drought, the fish were reintroduced in the lake. In 1998, the FWS published a recovery plan for threatened fish species in the Warner Lakes system. Recreation. Most of the land to the south and east of Hart Lake is privately owned.

Geographic entities mentioned:
surface_form: warner lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 42.4499
lon: -119.851
Habitat. This is an uncommon bird at the edges and clearings of mountain forests, and in scrubby second growth, bamboo clumps, and bushy pastures from 1500 m altitude to the timberline. In the wet season it can descend to 1200 m altitude. Its numbers have reported to be high when the bamboo is flowering on favoured sites such as Cerro de la Muerte. Behaviour.

Geographic entities mentioned:
surface_form: Cerro de la Muerte
instance_of: Mountain
countries: Costa Rica
coordinates: lat: 9.56666667
lon: -83.75
Samzhubzê has a monsoon-influenced, alpine version of a humid continental climate (Köppen &quot;Dwb&quot;), with frosty, very dry winters and warm, wet summers. Temperatures are relatively moderate for the Tibetan Plateau, as the annual mean temperature is. Barely any precipitation falls from November to March, when the diurnal temperature variation can frequently exceed.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Soisberg. Soisberg is a mountain of Hesse, Germany.

Geographic entities mentioned:
surface_form: soisberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.7884
lon: 9.8832
The Bodélé Depression is a low region in the southern Sahara that is surrounded by basalt mountain ridges. Winds flow through this region and lift dust. The dust from this region supplies over half of the dust to Amazon rainforests. The only important rivers, the Logone and Chari, are located in the southwest and flow into Lake Chad. The lake doubles in size during the rainy season. Geology.

Geographic entities mentioned:
surface_form: Logone
instance_of: Watercourse
countries: Cameroon
Central African Republic
Chad
coordinates: lat: 12.106111111111
lon: 15.035277777778
Muzo territory. The Muzo were inhabiting the lower-elevation northwestern areas of the Cundinamarca department and western portion of the Boyacá Department, closer to the Magdalena River. Their northern neighbours were the Naura people, the Panche in the south, and to the southeast the Muisca inhabited the higher-elevation Altiplano Cundiboyacense. Their western neighbours were the Colima people.

Geographic entities mentioned:
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877
Their western neighbours were the Colima people. The Muzo people were considered the first inhabitants of Boyacá, originally from Saboyá. Their territory stretched from the thick forests surrounding the Carare River in the north at the border with Santander, the Río Negro in the south, in the east the Pacho River and the Ubaté-Chiquinquirá Valley, and the Magdalena River in the west.

Geographic entities mentioned:
surface_form: Carare River
instance_of: Watercourse
countries: Colombia
coordinates: lat: 6.8
lon: -74.1
Mount Pugh. Mount Pugh (or Pugh Mountain, or native name Da Klagwats) is a peak near the western edge of the North Cascades, in Washington state. It is located west of Glacier Peak, one of the Cascade stratovolcanoes. It rises out of the confluence of the White Chuck River (on the north) and the Sauk River (on the southwest), giving it very low footings.

Geographic entities mentioned:
surface_form: Glacier Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.14972222
lon: -109.84944444
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.155013
lon: -117.293429
Mount Pugh. Mount Pugh (or Pugh Mountain, or native name Da Klagwats) is a peak near the western edge of the North Cascades, in Washington state. It is located west of Glacier Peak, one of the Cascade stratovolcanoes. It rises out of the confluence of the White Chuck River (on the north) and the Sauk River (on the southwest), giving it very low footings.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: mount pugh
instance_of: Mountain
countries: United States
coordinates: lat: 48.1431
lon: -121.374
It is located west of Glacier Peak, one of the Cascade stratovolcanoes. It rises out of the confluence of the White Chuck River (on the north) and the Sauk River (on the southwest), giving it very low footings. For example, it rises above the Sauk River Valley in just over; its rise over the White Chuck River is almost as dramatic. The mountain is named for John Pugh, who settled nearby, in 1891.

Geographic entities mentioned:
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
The trail to the summit is easily negotiable most of the way but the last is along a razorback ridge with significant exposure. This is the Northwest Ridge, Trail Number 644, which actually starts in the Sauk River Valley on the southwest side of the mountain. The total elevation gain is almost exactly one mile (). Climate.

Geographic entities mentioned:
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
Mount Pugh. Mount Pugh (or Pugh Mountain, or native name Da Klagwats) is a peak near the western edge of the North Cascades, in Washington state. It is located west of Glacier Peak, one of the Cascade stratovolcanoes. It rises out of the confluence of the White Chuck River (on the north) and the Sauk River (on the southwest), giving it very low footings.

Geographic entities mentioned:
surface_form: mount pugh
instance_of: Mountain
countries: United States
coordinates: lat: 48.1431
lon: -121.374
Cohen was born and lived in Wilkes-Barre, Pennsylvania until 2013. He attended Penn State University and Wilkes College between 1961 and 1965, and opened a commercial photo studio in 1966. The majority of the photography for which Cohen is known is shot in the Scranton/Wilkes-Barre metropolitan area (also known as the Wyoming Valley), a historic industrialized region of northeastern Pennsylvania.

Geographic entities mentioned:
surface_form: Wyoming Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
Lakpa Gelu. Lakpa Gelu () (born June 23, 1967), often spelled &quot;Lhakpa&quot;, is a Nepalese Sherpa climber born in Jubing - 1, KhariKhola, Solukhumbu, Nepal. He is known for holding a world record for the fastest climbing of Mount Everest (the world's tallest mountain at 8,848 meters, known to the Nepalese as &quot;Sagarmatha&quot;) in only 10 hours 56 minutes and 46 seconds.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
The ethnic Sherpa community in Nepal does not record exact birth dates, though, so it is impossible to know his precise birth date. Lhakpa Gelu comes from a family of climbers. His older brother died in 1991 while climbing Annapurna, and his youngest brother has also climbed Mount Everest. He is married to Fulli and has three children. In December 2006, Lhakpa Gelu moved to Utah.

Geographic entities mentioned:
surface_form: Annapurna
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.5958
lon: 83.82
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
In Utah, he had difficulty finding work as a mountain guide, so instead he had to work at a coffee house, installing signs, and delivering pizzas while searching for employment as an expedition guide. In 2008, Lhakpa began working as a guide for Alpine Ascents International, where he has guided expeditions up Mount Rainier and Aconcagua. Speed climb of Everest.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: Aconcagua
instance_of: Mountain
countries: Argentina
coordinates: lat: -32.653055555555554
lon: -70.01166666666667
Other ascents. In addition to over a dozen Everest summits, Lhakpa has also summitted Cho Oyu and Ama Dablam in the Himalayas. In 2007, Lhakpa climbed Everest to raise money for an elementary school in his hometown in Nepal and to increase public awareness of the contributions of the Sherpa people to Himalayan mountaineering.

Geographic entities mentioned:
surface_form: Cho Oyu
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 28.094166666667
lon: 86.660833333333
surface_form: Ama Dablam
instance_of: Mountain
countries: Nepal
coordinates: lat: 27.861111111111
lon: 86.861388888889
Geography. The Inn River runs through Zams, which is situated in the river's basin together with its neighbour town Landeck. The geographical location is. Here, the old roads coming from Vinschgau, Engadin, Bavaria, and Lake Constance cross. At the bridge over the Inn, tolls were demanded from trade wagons as early as the Middle Ages.

Geographic entities mentioned:
surface_form: Vinschgau
instance_of: Valley
countries: Italy
coordinates: lat: 46.615
lon: 10.705
surface_form: Engadin
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.5497
lon: 9.8959
Through his mother, Haselton was a descendant of John Eliot, a missionary in the Massachusetts Bay Colony who was famed as the &quot;Apostle to the Indians&quot;. Legacy. In 1909, the University of Vermont conferred on Haselton the honorary degree of LL.D. The Green Mountain Club's Haselton Trail is a hiking route from Smugglers Notch to the summit of Mount Mansfield.

Geographic entities mentioned:
surface_form: Mount Mansfield
instance_of: Mountain
countries: United States
coordinates: lat: 44.543611111111
lon: -72.814166666667
It and another Selig release, &quot;The Way of the Eskimo&quot;, were produced at the same time in the same location in the United States, in Escanaba, Michigan. Both &quot;Arctic&quot; stories were filmed there in less than two weeks during the early winter months of 1911, staged along the frozen shoreline of Little Bay de Noc that connects to Lake Michigan.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
It was instead one of two films shot on location at the same time in the United States, in Escanaba, Michigan, located approximately 300 miles north of Chicago. Situated next to the Little Bay de Noc linked to Lake Michigan, Escanaba offered a winter environment that on screen proved to be a convincing alternative to Canada's northern frontier.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Taxonomy. The rare Tobusch fishhook cactus was federally listed as endangered species, but has been moved to threatened species since the discovery of many more plants. It was known from about 200 to about 500 individual specimens on the eastern part of the Edwards Plateau. New plant discoveries have augmented that number to over 3000.

Geographic entities mentioned:
surface_form: Edwards Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 30.3
lon: -99.6
Englefield, East Maitland. Englefield is a heritage-listed former inn and now residence at 49 Newcastle Street, East Maitland, in the Hunter region of New South Wales, Australia. It was built in 1837. It operated as the Black Horse Inn from 1845 to 1878. It was added to the New South Wales State Heritage Register on 30 April 2008. History.

Geographic entities mentioned:
surface_form: Hunter region
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Shawaq. Shawaq (Quechua &quot;shawa&quot; &quot;Sambucus peruviana&quot;, &quot;-q&quot; a suffix, hispanicized spelling &quot;Shahuac&quot;) is a mountain in the Andes of Peru, about high. It is located in the Junín Region, Yauli Province, Morococha District, north of a lake named Waqraqucha.

Geographic entities mentioned:
surface_form: waqraqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -11.71333333
lon: -75.70083333
surface_form: waqraqucha
instance_of: Lake
countries: Peru
coordinates: lat: -11.593888888889
lon: -76.161388888889
surface_form: waqraqucha
instance_of: Lake
countries: Peru
coordinates: lat: -11.8542
lon: -75.9189
surface_form: waqraqucha
instance_of: Lake
countries: Peru
coordinates: lat: -11.27638889
lon: -76.16141667
Shawaq. Shawaq (Quechua &quot;shawa&quot; &quot;Sambucus peruviana&quot;, &quot;-q&quot; a suffix, hispanicized spelling &quot;Shahuac&quot;) is a mountain in the Andes of Peru, about high. It is located in the Junín Region, Yauli Province, Morococha District, north of a lake named Waqraqucha.

Geographic entities mentioned:
surface_form: shawaq
instance_of: Mountain
countries: Peru
coordinates: lat: -11.56305556
lon: -76.165
The station's transmitter is located atop Mount Seymour in the district municipality of North Vancouver. CIVT went on the air in 1997 as the first new Vancouver TV station in 21 years after the Canadian Radio-television and Telecommunications Commission selected the application of Baton Broadcasting from among five bids.

Geographic entities mentioned:
surface_form: Mount Seymour
instance_of: Mountain
countries: Canada
coordinates: lat: 49.393333333333
lon: -122.94444444444
Langbo Kangri. Langbo Kangri (also known as &quot;Langpo Kangri&quot;) is a mountain peak in the Himalayas on the border of Nepal and Tibet Autonomous Region of China. Location. The peak's location is shared between Nepal's Gandaki Province and China's Ngari Prefecture at above sea level. The prominence is at.

Geographic entities mentioned:
surface_form: langbo kangri
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 28.49838
lon: 85.1564
Location. The peak's location is shared between Nepal's Gandaki Province and China's Ngari Prefecture at above sea level. The prominence is at. The peak is located 12.17 km north-northeast of Yangra Kangri (&quot;Ganesh I&quot;), to which a ridge connects it. The gap height is 1474 m. At 3.88 km further north rises the Pashuwo at. Climbing history. There are no documented ascents of Langbo Kangri.

Geographic entities mentioned:
surface_form: langbo kangri
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 28.49838
lon: 85.1564
Location. The peak's location is shared between Nepal's Gandaki Province and China's Ngari Prefecture at above sea level. The prominence is at. The peak is located 12.17 km north-northeast of Yangra Kangri (&quot;Ganesh I&quot;), to which a ridge connects it. The gap height is 1474 m. At 3.88 km further north rises the Pashuwo at. Climbing history. There are no documented ascents of Langbo Kangri.

Geographic entities mentioned:
surface_form: yangra
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 28.391666666667
lon: 85.127222222222
surface_form: ganesh i
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 28.391666666667
lon: 85.127222222222
Lake Waubesa. Lake Waubesa is one of the four major lakes in Dane County, Wisconsin that surround the city of Madison. The lake has a surface area of and a max depth of. This lake is fed via the Yahara River Watershed and 9 Springs Wastewater Effluent. In 2013, the Wisconsin state record Yellow bass was caught in Lake Waubesa. It was long and weighed.

Geographic entities mentioned:
surface_form: lake waubesa
instance_of: Lake
countries: United States
coordinates: lat: 43.013055555556
lon: -89.324444444444
I never changed my profession.” In 2000, he created the first permanent wax chamber in Roc del Maure in the Pyrenees mountains near Perpignan. Other wax chambers followed near his studio in southern Germany, in the lower Engadin in Switzerland, in the Phillips Collection in Washington, D.C., and a 50-meter-long corridor for Anselm Kiefer in Barjac, southern France, realized in 2014.

Geographic entities mentioned:
surface_form: Engadin
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.5497
lon: 9.8959
Its administrative center is the town of Ostrov. Population: 36,685 (2002 Census); The population of Ostrov accounts for 69.7% of the district's total population. Geography. The entire district lies in the basin of the Velikaya River, a major tributary of Lake Peipus. The Velikaya crosses the district from southeast to northwest; the town of Ostrov is located on its banks.

Geographic entities mentioned:
surface_form: Lake Peipus
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
It is 26 km from Cochin International Airport and 4.5 km from Cherai Beach. It is covered by Ayyambilly Post Office with PIN 682 501. The east border is Veeranpuzha, the northern extension of Vembanad Lake and the Arabian Sea is the western border. Places of interest. The village contains the Pallathamkulangara Bhagavathi Temple, Sree Balakrishna Swami Temple, St.

Geographic entities mentioned:
surface_form: Veeranpuzha
instance_of: Lake
countries: India
coordinates: lat: 10.07
lon: 76.24
US 6 rejoins I-70 east of Grand Junction; US 50 departs on a course toward Pueblo. I-70 exits the valley through De Beque Canyon, a path carved by the Colorado River that separates the Book Cliffs from Battlement Mesa. The river and its tributaries provide the course for the ascent up the Rocky Mountains.

Geographic entities mentioned:
surface_form: Battlement Mesa
instance_of: Mountain
countries: United States
coordinates: lat: 39.358611111111
lon: -107.91472222222
In 1836, the Ngāti Tama chief Te Pūoho led a 100-person war party, armed with muskets, down the West Coast and over the Haast Pass. He ambushed a Ngāi Tahu encampment between Lake Wānaka and Lake Hāwea, then went south past Lake Wakatipu. His raid ended in Southland where he was killed and his war party destroyed by the southern Ngāi Tahu leader Tūhawaiki.

Geographic entities mentioned:
surface_form: Lake Wānaka
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.5
lon: 169.13333333333
surface_form: Lake Hāwea
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.5
lon: 169.28333333333
surface_form: Lake Wakatipu
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.085
lon: 168.561
The visitor centre offers a wide range of information about the surrounding area. Lake Moeraki is to the northeast, and the Haast Pass is to the southeast by road. The settlement of Okuru is located on the coast south-west of Haast. The small settlement of Haast Beach is on the coast of the Tasman Sea, approximately west southwest of Haast Junction, on the road to Jackson Bay. Climate.

Geographic entities mentioned:
surface_form: Lake Moeraki
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.73333333
lon: 169.28333333
Geography. Unlike much of Indiana with its low rolling hills, the terrain of Brown County is rugged and hilly, with the drainage areas filled with brush, undergrowth, or trees. The county's highest point (ASL) is Weed Patch Hill, the third-highest prominence in the state. According to the 2010 census, the county has a total area of, of which (or 98.53%) is land and (or 1.47%) is water.

Geographic entities mentioned:
surface_form: Weed Patch Hill
instance_of: Mountain
countries: United States
coordinates: lat: 39.1669
lon: -86.2175
The ridge runs northeast–southwest for about departing from South Mountain near Emmitsburg, Maryland, and running south past Leesburg, Virginia, where it disappears into the Piedmont in a series of low-lying hills near New Baltimore, Virginia. The ridge forms the eastern rampart of the Loudoun and Middletown valleys. Geography.

Geographic entities mentioned:
surface_form: Loudoun
instance_of: Valley
countries: United States
coordinates: lat: 39.2329
lon: -77.735
surface_form: Middletown
instance_of: Valley
countries: United States
coordinates: lat: 39.43
lon: -77.53
Due to its proximity to Washington, D.C., and its beautiful mountain scenery, Camp David has proven to be a popular weekend &quot;getaway&quot; for many United States presidents, and approximately one-third of Catoctin Mountain Park can be closed to the public on short notice.

Geographic entities mentioned:
surface_form: beautiful mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.488888888889
lon: -108.98916666667
surface_form: catoctin mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6478
lon: -77.4664
The ridge runs northeast–southwest for about departing from South Mountain near Emmitsburg, Maryland, and running south past Leesburg, Virginia, where it disappears into the Piedmont in a series of low-lying hills near New Baltimore, Virginia. The ridge forms the eastern rampart of the Loudoun and Middletown valleys. Geography.

Geographic entities mentioned:
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.182222222222
lon: -74.477777777778
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.949166666667
lon: -74.293333333333
surface_form: piedmont
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -80
surface_form: south mountain
instance_of: Landform
countries: United States
coordinates: lat: 40.33
lon: -76.2
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5544
lon: -72.8236
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.40111111
lon: -109.26111111
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.189166666667
lon: -74.051666666667
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.361944444444
lon: -74.285277777778
From its northern terminus in Maryland headed south, the range is composed mainly of a single north–south running ridge with periodic low-lying gaps, though it does contain several spur ridges, most notably near its intersection with South Mountain at its northern terminus.

Geographic entities mentioned:
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.182222222222
lon: -74.477777777778
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.949166666667
lon: -74.293333333333
surface_form: south mountain
instance_of: Landform
countries: United States
coordinates: lat: 40.33
lon: -76.2
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5544
lon: -72.8236
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.40111111
lon: -109.26111111
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.189166666667
lon: -74.051666666667
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.361944444444
lon: -74.285277777778
However, the ridge clearly has two prominent segments, one south of the Potomac River in Virginia and one north of it in Maryland. According to the USGS, variant names of Catoctin Mountain have included Kittochiny Mountains, Kittockton Mountain, Kittocton Mountain, and South Mountain. However, in Maryland, South Mountain and Catoctin Mountain are separate, roughly parallel, mountains.

Geographic entities mentioned:
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.182222222222
lon: -74.477777777778
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.949166666667
lon: -74.293333333333
surface_form: catoctin mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6478
lon: -77.4664
surface_form: south mountain
instance_of: Landform
countries: United States
coordinates: lat: 40.33
lon: -76.2
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5544
lon: -72.8236
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.40111111
lon: -109.26111111
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.189166666667
lon: -74.051666666667
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.361944444444
lon: -74.285277777778
(The GNIS does, however, recognize the community of Braddock Heights, which is located there.)
Geology. The mountain, like much of the Blue Ridge/South Mountain in the immediate area, consists of Proterozoic Catoctin metabasaltic greenstone interspersed by metasedimentary white quartz and other phyllites and Precambrian basalt flows.

Geographic entities mentioned:
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.182222222222
lon: -74.477777777778
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.949166666667
lon: -74.293333333333
surface_form: south mountain
instance_of: Landform
countries: United States
coordinates: lat: 40.33
lon: -76.2
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5544
lon: -72.8236
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.40111111
lon: -109.26111111
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.189166666667
lon: -74.051666666667
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.361944444444
lon: -74.285277777778
The name &quot;Catoctin&quot; probably derives from the Kittoctons, an American Indian tribe or clan which once lived between the mountain and the Potomac River; a local tradition asserts that &quot;Catoctin&quot; means &quot;place of many deer&quot; in an Indian language. Catoctin Mountain is perhaps best known as the site of Camp David, a mountain retreat for presidents of the United States.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
The mountain is much lower in elevation in Virginia, reaching its highest peak just south of the Potomac at Furnace Mountain (891 feet/271 m) and with only one peak above south of Leesburg.

Geographic entities mentioned:
surface_form: furnace mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.27
lon: -77.55
Catoctin Mountain. Catoctin Mountain, along with the geologically associated Bull Run Mountains, forms the easternmost mountain ridge of the Blue Ridge Mountains, which are in turn a part of the Appalachian Mountains range.

Geographic entities mentioned:
surface_form: catoctin mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6478
lon: -77.4664
Catoctin Mountain. Catoctin Mountain, along with the geologically associated Bull Run Mountains, forms the easternmost mountain ridge of the Blue Ridge Mountains, which are in turn a part of the Appalachian Mountains range.

Geographic entities mentioned:
surface_form: catoctin mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6478
lon: -77.4664
surface_form: bull
instance_of: Watercourse
countries: United States
coordinates: lat: 49.46663
lon: -115.45205
The ridge forms the eastern rampart of the Loudoun and Middletown valleys. Geography. Catoctin Mountain traverses Frederick County, Maryland and extends into northern Loudoun County, Virginia.

Geographic entities mentioned:
surface_form: catoctin mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6478
lon: -77.4664
Recreation. A number of federal, state, local, and private protected lands are located on Catoctin Mountain including the Emmitsburg Reservoir, Catoctin Mountain Park, Cunningham Falls State Park, the Frederick Municipal Forest, Gambrill State Park, the Chesapeake and Ohio Canal National Historical Park, all in Maryland, and the Morven Park estate in Virginia.

Geographic entities mentioned:
surface_form: catoctin mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6478
lon: -77.4664
surface_form: catoctin mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6478
lon: -77.4664
The 27-mile (43 km) long Catoctin Trail traverses the northern half of the range. The trail, which is maintained by the Potomac Appalachian Trail Club, starts at Gambrill State Park, which also contains several shorter hiking and mountain biking trails as well as picnic pavilions, and continues north through the Frederick Municipal Forest to Cunningham Falls State Park and Catoctin Mountain Park.

Geographic entities mentioned:
surface_form: catoctin mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6478
lon: -77.4664
Names. The name of Catoctin Mountain follows the convention of referring to an entire mountainous ridge as a single &quot;mountain&quot; in situations where there is no single prominent peak. However, the ridge clearly has two prominent segments, one south of the Potomac River in Virginia and one north of it in Maryland.

Geographic entities mentioned:
surface_form: catoctin mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6478
lon: -77.4664
There is also a declining population of native orchids that have been monitored and surveyed since the 1960s. Amphibians. There are 22 known species of amphibians living on Catoctin Mountain. The salamanders that live in the region fall into three groups: mole salamanders, newts, and lungless salamanders.

Geographic entities mentioned:
surface_form: catoctin mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6478
lon: -77.4664
Arthropods. One survey of aquatic insects in Big Hunting Creek found 20 species of stoneflies, the most prevalent being the winter stonefly. Birds. Since 2007, the National Capital Region Network (NCRN) Inventory & Monitoring program has monitored birds across 385 forested plots throughout the Catoctin Mountain region.

Geographic entities mentioned:
surface_form: catoctin mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6478
lon: -77.4664