Sarmila/GeoWiki-Features huggingface dataset:
Bell Cow Lake (sometimes written as Bellcow) is a reservoir located within the city limits of Chandler, Oklahoma, in a section of the city located to the northwest of its central district, just off Interstate 44 and Oklahoma State Highway 18. The lake was constructed on Bell Cow Creek for flood control, water supply, recreation, and fish and wildlife purposes. The lake surface covers.

Geographic entities mentioned:
surface_form: cow creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.979722222222
lon: -97.84
Bicknell's thrush was first identified on its summit. Geography. Like most other Catskill peaks, Slide's summit is gentle and rounded, taking the form of a narrow ridge that rises to a wider bump on its eastern end. From there the mountain slopes down steeply to the col with neighboring Cornell Mountain.

Geographic entities mentioned:
surface_form: Cornell Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.001480555556
lon: -74.356816666667
From there the mountain slopes down steeply to the col with neighboring Cornell Mountain. At the western end, a broad slope, part of the Catskill Divide, leads down to the gap between Slide and Hemlock Mountain to the west and Winnisook Lake, the source of Esopus Creek, to the mountain's northwest.

Geographic entities mentioned:
surface_form: Hemlock Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0128698
lon: -74.4390407
surface_form: Winnisook Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.014444444444
lon: -74.4125
surface_form: hemlock
instance_of: Lake
countries: United States
coordinates: lat: 42.718611111111
lon: -77.608888888889
The Appalachians do not rise to that level again until West Virginia. Climate. These data are taken from the weather station at Winnisook Lake on the mountain's northwest slope. There is no weather station at the summit, but this climate table contains interpolated data for an area around the summit. Identification as highest Catskill peak.

Geographic entities mentioned:
surface_form: Winnisook Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.014444444444
lon: -74.4125
Seven years earlier, Princeton geology professor Arnold Henry Guyot had been staying at the Catskill Mountain House when he became interested in the surrounding mountains, and management's claim that nearby Kaaterskill High Peak () was the highest in all the Catskills despite growing doubt.

Geographic entities mentioned:
surface_form: Kaaterskill High Peak
instance_of: Mountain
countries: United States
coordinates: lat: 42.1620334
lon: -74.0801381
surface_form: high peak
instance_of: Mountain
countries: United States
coordinates: lat: 32.70166666666667
lon: -109.87138888888889
surface_form: high peak
instance_of: Mountain
countries: United States
coordinates: lat: 42.1620334
lon: -74.0801381
Two years later the Forest Preserve legislation was written into a new version of New York's constitution as Article 14. John Burroughs. Slide's fame was spread far and wide by Burroughs. He had often been able to see the peak's summit ridge from Old Clump Mountain near his boyhood home in Delaware County, likening it to seeing a horse grazing from behind.

Geographic entities mentioned:
surface_form: Old Clump Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.310833333333
lon: -74.635277777778
surface_form: old clump
instance_of: Mountain
countries: United States
coordinates: lat: 42.310833333333
lon: -74.635277777778
The most common route up Slide has always been from the pass between it and the mountains to the west, where the high elevation at the trailhead has greatly reduced the vertical ascent required. The move from Winnisook Lake to the new state trailhead has added to the climb slightly, but it is still less than that required to climb some of the lower Catskill High Peaks.

Geographic entities mentioned:
surface_form: Winnisook Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.014444444444
lon: -74.4125
surface_form: high peaks
instance_of: Mountain
countries: United States
coordinates: lat: 45
lon: -70.4
The most challenging route to the summit of Slide begins at the Burroughs Range Trail's eastern terminus, Woodland Valley State Campground south of Phoenicia. It takes in the whole range, going over Wittenberg and Cornell mountains for a, ascent. Wittenberg and Cornell are both challenging climbs in and of themselves, and the climax is the steep east slope of Slide.

Geographic entities mentioned:
surface_form: Wittenberg
instance_of: Mountain
countries: United States
coordinates: lat: 42.0081
lon: -74.3474
surface_form: Cornell
instance_of: Mountain
countries: United States
coordinates: lat: 42.001480555556
lon: -74.356816666667
Further upstream, as it passes the usual points of departure for Lone, Rocky, Balsam Cap and Friday mountains, the path gets increasingly disused and harder to follow. The challenge in hiking Slide this way is not so much the mountain itself as the routefinding when it begins to climb to the col. Deer Shanty Brook.

Geographic entities mentioned:
surface_form: Friday
instance_of: Mountain
countries: United States
coordinates: lat: 41.987591666667
lon: -74.362094444444
surface_form: balsam cap
instance_of: Mountain
countries: United States
coordinates: lat: 41.977036111111
lon: -74.357372222222
The neighboring high peaks to the east used to be able to be seen, and seemed like small hills and the Devil's Path and Blackhead Range in Greene County used to be visible to the north. In fact, it used to be possible to see, from various points along the summit ridge, all but one of the other 34 Catskill High Peaks (Thomas Cole may or may not have been hidden by Hunter).

Geographic entities mentioned:
surface_form: Thomas Cole
instance_of: Mountain
countries: United States
coordinates: lat: 42.2708
lon: -74.1362
surface_form: high peaks
instance_of: Mountain
countries: United States
coordinates: lat: 45
lon: -70.4
Just above the signs indicating the camping and fire restrictions that NYSDEC has put in place for areas above in the Catskills to protect the montane forests, there are two viewpoints just off the trail. One takes in Table and Lone mountains; the other offers the only good glimpse of the lowest High Peak, remote and challenging Rocky Mountain.

Geographic entities mentioned:
surface_form: high peak
instance_of: Mountain
countries: United States
coordinates: lat: 32.70166666666667
lon: -109.87138888888889
surface_form: rocky mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9727
lon: -74.3732
surface_form: high peak
instance_of: Mountain
countries: United States
coordinates: lat: 42.1620334
lon: -74.0801381
surface_form: rocky mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.7955
lon: -79.1808
surface_form: rocky mountain
instance_of: Landform
countries: United States
coordinates: lat: 41.7958
lon: -71.055
surface_form: rocky mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0918
lon: -74.2151
One takes in Table and Lone mountains; the other offers the only good glimpse of the lowest High Peak, remote and challenging Rocky Mountain. It continues to the summit through long and fragrant stretches of balsam fir and soil muddy enough to require puncheon bridges in some areas. It is to the summit via this route.

Geographic entities mentioned:
surface_form: muddy
instance_of: Watercourse
countries: United States
coordinates: lat: 36.737500000000004
lon: -114.74416666666667
For many years, the first or so of the trail climbing Slide crossed the property of the nearby Winnisook Club. There was a metal gate across the Burroughs Range Trail marking the property line, below which nearly every tree had a No Trespassing sign on it. Because of the 1970s hiking boom, parking along the road at Winnisook Lake (there was no parking lot) had become a nightmare.

Geographic entities mentioned:
surface_form: winnisook
instance_of: Lake
countries: United States
coordinates: lat: 42.014444444444
lon: -74.4125
Because of the 1970s hiking boom, parking along the road at Winnisook Lake (there was no parking lot) had become a nightmare. In the late 1970s, the New York State Department of Environmental Conservation solved the problem by buying the land south of the ridgeline from the Winnisook Club, making all but the last stretch of trail to Winnisook Lake public land.

Geographic entities mentioned:
surface_form: winnisook
instance_of: Lake
countries: United States
coordinates: lat: 42.014444444444
lon: -74.4125
surface_form: winnisook
instance_of: Lake
countries: United States
coordinates: lat: 42.014444444444
lon: -74.4125
He had often been able to see the peak's summit ridge from Old Clump Mountain near his boyhood home in Delaware County, likening it to seeing a horse grazing from behind. &quot;Here the works of man dwindle,&quot; was put on a plaque near the summit by the Winnisook Club shortly after his death in 1921 and placed on a ledge near the summit that offers the best view from the mountain.

Geographic entities mentioned:
surface_form: winnisook
instance_of: Lake
countries: United States
coordinates: lat: 42.014444444444
lon: -74.4125
New regulations also ended abuse of the summit by campers. For many years, the first or so of the trail climbing Slide crossed the property of the nearby Winnisook Club. There was a metal gate across the Burroughs Range Trail marking the property line, below which nearly every tree had a No Trespassing sign on it.

Geographic entities mentioned:
surface_form: winnisook
instance_of: Lake
countries: United States
coordinates: lat: 42.014444444444
lon: -74.4125
After crossing the upper west branch of the Neversink at the trailhead, in elevation, the yellow-blazed P-EB trail works its way gently up slope and over some lesser streams to the old carriage road it originally followed through the Winnisook Club property.

Geographic entities mentioned:
surface_form: winnisook
instance_of: Lake
countries: United States
coordinates: lat: 42.014444444444
lon: -74.4125
surface_form: west branch
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
It is to the junction with the blue-blazed Fox Hollow Trail, which leads north to Giant Ledge and Panther Mountain. By striking out due south from this junction one will soon begin to climb the north ridge, reaching first a summit (on the private property of the Winnisook Club), then turning to the southeast through thickening boreal forest to the summit.

Geographic entities mentioned:
surface_form: winnisook
instance_of: Lake
countries: United States
coordinates: lat: 42.014444444444
lon: -74.4125
It can be used by starting from the Giant Ledge trailhead at a hairpin turn on County Road 42, about in elevation. It is to the junction with the blue-blazed Fox Hollow Trail, which leads north to Giant Ledge and Panther Mountain.

Geographic entities mentioned:
surface_form: panther mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.672222222222
lon: -74.928333333333
surface_form: panther mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0564
lon: -74.395
surface_form: fox hollow
instance_of: Valley
countries: United States
coordinates: lat: 36.7889447
lon: -91.2729116
surface_form: fox hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.55476
lon: -76.10137
surface_form: fox hollow
instance_of: Valley
countries: United States
coordinates: lat: 42.83972222222222
lon: -73.375
surface_form: panther mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.770555555556
lon: -74.9975
Early 20th century. The trail built in 1892 had been meant to facilitate travel to the lookout towers that existed in some form or another on the mountain's summit. Recreational visitors found views from the summit severely limited without a stand to get above the trees; the state was interested in fire control.

Geographic entities mentioned:
surface_form: the lookout
instance_of: Mountain
countries: United States
coordinates: lat: 40.509444444444
lon: -75.346111111111
His findings were vehemently disputed by the hotelkeepers around North-South Lake until others confirmed his results. There was a movement, once its status had been confirmed, to give Slide a name believed to be more fitting for a highest peak. &quot;Mount Lincoln,&quot; after the late U.S. president, was considered for a while.

Geographic entities mentioned:
surface_form: mount lincoln
instance_of: Mountain
countries: United States
coordinates: lat: 44.149
lon: -71.6445
surface_form: mount lincoln
instance_of: Mountain
countries: United States
coordinates: lat: 47.55009
lon: -123.32822
surface_form: mount lincoln
instance_of: Mountain
countries: United States
coordinates: lat: 39.35138889
lon: -106.11083333
surface_form: mount lincoln
instance_of: Mountain
countries: United States
coordinates: lat: 39.28768
lon: -120.32798
surface_form: mount lincoln
instance_of: Mountain
countries: United States
coordinates: lat: 42.3639
lon: -72.4231
At the western end, a broad slope, part of the Catskill Divide, leads down to the gap between Slide and Hemlock Mountain to the west and Winnisook Lake, the source of Esopus Creek, to the mountain's northwest. Two more pronounced ridges lead off the mountain, one to the southwest and the col with Wildcat Mountain, the other to the north and Giant Ledge.

Geographic entities mentioned:
surface_form: wildcat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.7192
lon: -83.8394
surface_form: wildcat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9775
lon: -74.476111111111
surface_form: wildcat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.5681
lon: -90.7546
surface_form: wildcat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2589
lon: -71.2014
surface_form: wildcat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.478
lon: -113.2972
They had laid the trail out, and a small monument to them is located at the trail's southern end, where it leaves the Phoenicia-East Branch Trail south of the Burroughs Range Trail junction, in the col between Slide and neighboring Wildcat Mountain. The blue-blazed trail, long follows another ridge up to the junction with the Burroughs Range Trail on the summit ridge.

Geographic entities mentioned:
surface_form: wildcat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.7192
lon: -83.8394
surface_form: wildcat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9775
lon: -74.476111111111
surface_form: wildcat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.5681
lon: -90.7546
surface_form: wildcat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2589
lon: -71.2014
surface_form: wildcat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.478
lon: -113.2972
His survey, carried out on his own time and at his own expense, established that Slide, located some distance to the southwest, was far and away the highest peak in the range. His findings were vehemently disputed by the hotelkeepers around North-South Lake until others confirmed his results.

Geographic entities mentioned:
surface_form: south lake
instance_of: Lake
countries: United States
coordinates: lat: 43.5860057
lon: -74.6305866
surface_form: south lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3034
lon: -74.5238
There is no weather station at the summit, but this climate table contains interpolated data for an area around the summit. Identification as highest Catskill peak. For a mountain with so many superlatives, Slide actually took a long time to be discovered for what it was. The mountain received its name locally from a landslide in 1819 on its north face near the summit.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
Regardless, tourism soon shifted to the new highest peak, and a local woodsman, Jim Dutcher, who knew the mountain well from his days peeling hemlock bark for tanning, built a hotel and did a regular business escorting visitors to the summit up a trail he built in 1880.

Geographic entities mentioned:
surface_form: hemlock
instance_of: Lake
countries: United States
coordinates: lat: 42.718611111111
lon: -77.608888888889
This view is now completely overgrown. The neighboring high peaks to the east used to be able to be seen, and seemed like small hills and the Devil's Path and Blackhead Range in Greene County used to be visible to the north.

Geographic entities mentioned:
surface_form: blackhead
instance_of: Mountain
countries: United States
coordinates: lat: 42.2679
lon: -74.1046
The next year the state decided to use along the West Branch of the Neversink at the west slope of the mountain (south of the current trailhead) to reintroduce white-tailed deer, which had been seriously thinned in the area over the preceding century.

Geographic entities mentioned:
surface_form: west branch
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
This was the trailhead for a new section of the Phoenicia-East Branch Trail, which connected to the carriage road commonly used very near the base of the Burroughs Range Trail. This new section requires crossing the west branch of the Neversink right at the beginning. While it is normally not difficult to follow the stepping stones, the creek can be impassable and even fatal in high water.

Geographic entities mentioned:
surface_form: west branch
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
Legends have grown up over the years in the Catskills over this belated discovery of the range's highest peak. Some tell of a new owner of Hunter Mountain, the range's other 4,000-footer and second-highest peak, swinging a level around to ensure he had bought the highest peak until being stopped by Slide.

Geographic entities mentioned:
surface_form: hunter mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.1779
lon: -74.2304
While it is normally not difficult to follow the stepping stones, the creek can be impassable and even fatal in high water. In December 2000, Timothy O'Lear, a Boy Scout from Long Island drowned when he fell in and was caught under some nearby tree branches when returning after a weekend backpacking trip. He is memorialized with a small plaque on a bench at the beginning of the trail.

Geographic entities mentioned:
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
Slide Mountain (Ulster County, New York). Slide Mountain is the highest peak in the Catskill Mountains of the U.S. state of New York. It is located in the town of Shandaken in Ulster County. While the contour line on topographic maps is generally accepted as its height, the exact elevation of the summit has never been officially determined by the U.S.

Geographic entities mentioned:
surface_form: slide mountain (ulster county, new york)
instance_of: Mountain
countries: United States
coordinates: lat: 41.9986
lon: -74.3864
surface_form: slide mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.3127
lon: -119.884
Slide Mountain (Ulster County, New York). Slide Mountain is the highest peak in the Catskill Mountains of the U.S. state of New York. It is located in the town of Shandaken in Ulster County. While the contour line on topographic maps is generally accepted as its height, the exact elevation of the summit has never been officially determined by the U.S.

Geographic entities mentioned:
surface_form: slide mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9986
lon: -74.3864
surface_form: slide mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.3127
lon: -119.884
Slide would wind up lending its name to the state-designated Slide Mountain Wilderness Area, the largest in the Catskills at. New regulations also ended abuse of the summit by campers. For many years, the first or so of the trail climbing Slide crossed the property of the nearby Winnisook Club.

Geographic entities mentioned:
surface_form: slide mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9986
lon: -74.3864
surface_form: slide mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.3127
lon: -119.884
Steel for a more permanent tower was brought up to the summit in the early 1930s, but the tower itself was not built until wartime. It would be dismantled around 1965, and no replacement has been erected. In the late 1990s, when DEC updated the Slide Mountain Wilderness Area's Unit Management Plan, it considered rebuilding an observation tower at the summit to provide the long-absent views.

Geographic entities mentioned:
surface_form: slide mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9986
lon: -74.3864
surface_form: slide mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.3127
lon: -119.884
Catskill forest researcher Michael Kudish has found an anomalous grove of sugar maple at roughly in elevation just off the trail near the western end of the mountain's summit ridge. He has also noted that, in contrast to the boreal forests on other Catskill High Peaks, Slide's has no red spruce. He does not believe there ever has been any.

Geographic entities mentioned:
surface_form: high peaks
instance_of: Mountain
countries: United States
coordinates: lat: 45
lon: -70.4
Starting from the Denning trailhead, the P-EB Trail is followed to its junction with the blue-blazed Peekamoose-Table Trail, which drops down to the east into the river valley near the flood plain at the Deer Shanty Brook confluence and its many channels, some of them difficult to cross at high water.

Geographic entities mentioned:
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
Atsion, New Jersey. Atsion is an unincorporated community located within Shamong Township in Burlington County, in the U.S. state of New Jersey. The community is located next to Atsion Lake. The settlement is located within the Wharton State Forest, and a forest office, parking area and information kiosk are located at Atsion. History. Charles Read built a bog iron forge in 1766.

Geographic entities mentioned:
surface_form: Atsion Lake
instance_of: Lake
countries: United States
coordinates: lat: 39.741
lon: -74.7327
1600s–1800s: &quot;The Jewish Valley&quot;. By the early 17th century, Mountain Jews formed many small settlements throughout the mountain valleys of Dagestan. One valley, located 10 km south of Derbent, close to the shore of the Caspian Sea, was predominantly populated by Mountain Jews. Their Muslim neighbors called this area &quot;Jewish Valley&quot;.

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
Caridina sarasinorum. &quot;Caridina sarasinorum&quot; is a species of freshwater atyid shrimp. It is one of eight &quot;Caridina&quot; species endemic to Lake Poso. Eyes and antennular peduncle. &quot;Caridina sarasinorum&quot; has well-developed eyes that reach to around 80% of the length of the basal segment. The antennular peduncle, is as long as the body itself.

Geographic entities mentioned:
surface_form: Lake Poso
instance_of: Lake
countries: Indonesia
coordinates: lat: -1.97955
lon: 120.6601
Eridania Lake is a theorized ancient lake with a surface area of roughly 1.1 million square kilometers. Its maximum depth is 2,400 meters and its volume is 562,000km. It was larger than the largest landlocked sea on Earth, the Caspian Sea and contained more water than all the other martian lakes together. The Eridania sea held more than 9 times as much water as all of America's Great Lakes.

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
Höllentalanger Hut. The Höllentalanger Hut (1,381 m) is a managed hut owned by the German Alpine Club in the Wetterstein Mountains of Bavaria, in the district of Garmisch-Partenkirchen. The hut lies in a narrow defile between the Höllental-Blassen and Waxenstein-Riffelwand crest and is open from the end of May to mid-October. It has more than 80 bedspaces.

Geographic entities mentioned:
surface_form: Waxenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 47.4475
lon: 11.022777777778
Cydia indivisa. &quot;Cydia indivisa&quot; is a species of moth of the family Tortricidae. It is found from Fennoscandia to France, Switzerland, Austria and Slovakia. In the east, the range extends to the Baltic region and northern Russia. The wingspan is 13–16 mm. Adults are on wing from May to July in one generation per year. The larvae feed on &quot;Picea abies&quot;.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Blatterle. Blatterle is a white Italian wine grape variety from the Alto-Adige of northeast Italy. The grape, which was historically grown around the commune of Bolzano in South Tyrol and the Eisacktal valley, gets its name from the term in the local Tyrolese dialect for &quot;little leaves&quot;.

Geographic entities mentioned:
surface_form: Eisacktal
instance_of: Valley
countries: Italy
coordinates: lat: 46.67
lon: 11.6
Anulocaulis annulatus. &quot;Anulocaulis annulatus&quot; is a species of flowering plant in the four o'clock family known by the common name valley ringstem. It is endemic to the Mojave Desert of California, especially in the vicinity of Death Valley. This is a perennial herb growing a number of thin, erect stems sometimes exceeding a meter in height from a thick caudex.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
A protest in October 2021 resulted in a 30-day military enforced 'state of siege' in the area, raids on local homes and media outlets, and several arrests. Background. The Fenix project encompasses 250,000 square kilometers near the town of El Estor and adjacent to Guatemala's largest freshwater lake: Lake Izabal. The lake is an important breeding ground for endangered manatees.

Geographic entities mentioned:
surface_form: Lake Izabal
instance_of: Lake
countries: Guatemala
coordinates: lat: 15.5
lon: -89.166666666667
The case is part of a years-long claim beginning in 2002, when area residents bought their land back from the Guatemalan government, but never received title. Lake Izabal pollution incident (2017). In May 2017, the water in Lake Izabal turned red for a period of weeks, and local fishermen began protesting the mine. At least one protester was shot and killed during these protests.

Geographic entities mentioned:
surface_form: Lake Izabal
instance_of: Lake
countries: Guatemala
coordinates: lat: 15.5
lon: -89.166666666667
Career as explorer. Jean-Louis Étienne got interested in medical matters and human psychology in extreme conditions. In order to further his research, he participated in several expeditions in Himalaya (Broad Peak and North of Mount Everest), Greenland and Patagonia. He was a teammate on the &quot;Pen Duick VI&quot; under Éric Tabarly for its race around the world in 1977–78.

Geographic entities mentioned:
surface_form: Broad Peak
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.810555555556
lon: 76.568055555556
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
The town became part of Lesser Poland Voivodeship after being part of Katowice Voivodeship (1975&ndash;1998). With population of 20,175 (Dec. 31, 2010), Trzebinia is an important industrial center. The town lies in the Kraków-Częstochowa Upland, above sea level. Trzebinia is a rail and road hub, and lies at a junction of the A4 Motorway and National Road Nr. 79.

Geographic entities mentioned:
surface_form: Kraków-Częstochowa Upland
instance_of: Plateau
countries: Poland
coordinates: lat: 50.2067
lon: 19.8292
Because of that, Klang Parade is struggling to get customers. Transport. However, due to the recent property developments at nearby areas such as Setia Alam (part of Shah Alam), Klang Sentral and Bandar Bukit Raja, Meru is all set to see a raise in traffic volume. Car. New Klang Valley Expressway
Jalan Meru
Rail. Jalan Meru LRT Station

Geographic entities mentioned:
surface_form: Klang Sentral
instance_of: Valley
countries: Malaysia
Horse Range (New Zealand). The Horse Range is a range of hills located inland from Oamaru in the South Island of New Zealand. The other side of the range is to the north east of the Shag River valley that contains the lower part of The Pigroot. The Horse Range transitions inland to the higher Kakanui Range. Geology.

Geographic entities mentioned:
surface_form: horse range (new zealand)
instance_of: Mountain
Horse Range (New Zealand). The Horse Range is a range of hills located inland from Oamaru in the South Island of New Zealand. The other side of the range is to the north east of the Shag River valley that contains the lower part of The Pigroot. The Horse Range transitions inland to the higher Kakanui Range. Geology.

Geographic entities mentioned:
surface_form: horse range
instance_of: Mountain
Geology. The range is part of a fault scarp structure whose Waihemo fault strands extend from the Mackenzie Basin to the coast. The Horse Range Formation is a distinct Cretaceous sedimentary structure associated with the range and the south east portion of the scarp. It has become cemented with calcite, partially explained by later overlying marine sediments.

Geographic entities mentioned:
surface_form: horse range
instance_of: Mountain
It has become cemented with calcite, partially explained by later overlying marine sediments. The stratigraphy in the range passes from the highest marine sandstone Herbert Formation formed before about 75 million years ago to the Taratu Formation that overtops the most recent Horse Range Formation that is about 88 million years old.

Geographic entities mentioned:
surface_form: horse range
instance_of: Mountain
The stratigraphy in the range passes from the highest marine sandstone Herbert Formation formed before about 75 million years ago to the Taratu Formation that overtops the most recent Horse Range Formation that is about 88 million years old. A layer in some of the Horse Range Formation is a ignimbrite rhyolitic deposit from what must have been a surface eruption at about 112 million years ago.

Geographic entities mentioned:
surface_form: horse range
instance_of: Mountain
Underneath this is the basement of metamorphosed quartzofeldpathic semischist sedimentary rocks of the Rakaia Terrane. Between the coast at Shag Point and the Horse Range there are a range of hills called the Blue Mountains (there is another range called the Blue Mountains in Otago).

Geographic entities mentioned:
surface_form: horse range
instance_of: Mountain
The Blue mountains are associated with a marble layer about thick which extends about named the Blue Mountain Formation. This marble has also been mapped at Conical Hill in the middle of the Horse Range, to the north west of the main Blue Mountain Formation. Conical Peak. The highest point in the Horse Range is Conical Peak, at.

Geographic entities mentioned:
surface_form: horse range
instance_of: Mountain
Asia Ghee Mills. He represented Asia Ghee Mills in the departmental 2020 PFF Challenge Cup. SA Gardens. After the suspension of the Pakistan Football Federation by FIFA and the persistent inactivity of the Pakistan Premier League, Riaz participated in various local tournaments in Peshawar and Chitral and played for SA Gardens in 2021. International career.

Geographic entities mentioned:
surface_form: Chitral
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.85111111111111
lon: 71.78888888888889
Wichhu Qullu (Cochabamba). Wichhu Qullu (Aymara &quot;jichu, wichhu&quot; &quot;stipa ichu&quot;, &quot;qullu&quot; mountain, &quot;ichu&quot; mountain&quot;, also spelled &quot;Huichu Kkollu&quot;) is a mountain in the Bolivian Andes which reaches a height of approximately. It is located in the Cochabamba Department, Tapacari Province.

Geographic entities mentioned:
surface_form: wichhu qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.99888889
lon: -66.91166667
surface_form: wichhu qullu (cochabamba)
instance_of: Mountain
countries: Bolivia
coordinates: lat: -20.29629
lon: -68.58025
Wichhu Qullu (Cochabamba). Wichhu Qullu (Aymara &quot;jichu, wichhu&quot; &quot;stipa ichu&quot;, &quot;qullu&quot; mountain, &quot;ichu&quot; mountain&quot;, also spelled &quot;Huichu Kkollu&quot;) is a mountain in the Bolivian Andes which reaches a height of approximately. It is located in the Cochabamba Department, Tapacari Province.

Geographic entities mentioned:
surface_form: wichhu qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.99888889
lon: -66.91166667
surface_form: wichhu qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -20.29629
lon: -68.58025
It is located in the Cochabamba Department, Tapacari Province. Wichhu Qullu lies west of the Ch'iyar Jaqhi River and north of the village of Ch'iyar Jaqhi (&quot;black rock&quot;, also spelled &quot;Chiaraque&quot;).

Geographic entities mentioned:
surface_form: ch'iyar jaqhi
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.3267
lon: -69.3833
surface_form: ch'iyar jaqhi
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.17277778
lon: -68.31277778
surface_form: ch'iyar jaqhi
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.28333333
lon: -66.45
surface_form: ch'iyar jaqhi
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.35694444
lon: -69.01138889
surface_form: ch'iyar jaqhi
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.6611
lon: -66.4133
surface_form: ch'iyar jaqhi
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.1269
lon: -68.3864
No such force was in the District at the time. Topography. Souther Fell is the eastern extremity of Blencathra, a continuation of the arm that runs down from the summit over Doddick Fell and Scales Fell. A smooth slope falls eastward from Scales Fell to the col of Mousthwaite Comb at. The ridge then turns northeast for two miles along the summit of Souther Fell.

Geographic entities mentioned:
surface_form: Blencathra
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.63985
lon: -3.0504611111111
surface_form: blencathra
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.63985
lon: -3.0504611111111
A small cairn marks the top. This being the last of the Northern Fells in that direction, the view across to the Pennines is uninterrupted. The Lakeland view peeps around the looming presence of Blencathra, taking in Great Gable, the Scafells, the nearer Helvellyn range and a portion of the Far Eastern Fells. Ascents.

Geographic entities mentioned:
surface_form: Great Gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
surface_form: blencathra
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.63985
lon: -3.0504611111111
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
surface_form: great gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
A footbridge crosses the river just north of Mousthwaite Comb, the only reliable crossing between here and Mungrisdale village. Geology. In common with much of the Northern Fells, the Kirk Stile Formation of the Skiddaw Group predominates. This is composed of laminated mudstone and siltstone with greywacke sandstone and is of Ordovician age. The &quot;Spectral Army&quot; of Souther Fell.

Geographic entities mentioned:
surface_form: skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
Souther Fell. Souther Fell is a fell in the English Lake District. It stands to the south of Mungrisdale village in the Northern Fells. It is most famous for the appearance of a &quot;spectral army&quot;, said to have been seen marching along its crest on Midsummer's Day, 1745. No such force was in the District at the time. Topography.

Geographic entities mentioned:
surface_form: souther fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6538
lon: -3.00122
Topography. Souther Fell is the eastern extremity of Blencathra, a continuation of the arm that runs down from the summit over Doddick Fell and Scales Fell. A smooth slope falls eastward from Scales Fell to the col of Mousthwaite Comb at. The ridge then turns northeast for two miles along the summit of Souther Fell. Mousthwaite Comb is a geographical oddity.

Geographic entities mentioned:
surface_form: souther fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6538
lon: -3.00122
To the south of the col, flowing westward, is the same river. In the intervening time the Glenderamackin has run for six miles, surrounding Souther Fell on three sides like a moat. The Comb provides its only dryshod connection to other ground and even this is almost cut off by the tributary of Comb Beck on the southern slope.

Geographic entities mentioned:
surface_form: souther fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6538
lon: -3.00122
This is composed of laminated mudstone and siltstone with greywacke sandstone and is of Ordovician age. The &quot;Spectral Army&quot; of Souther Fell. On the evening of Midsummer's Day 1745, a line of marching troops, cavalry and even carriages was seen travelling along the summit ridge of Souther Fell.

Geographic entities mentioned:
surface_form: souther fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6538
lon: -3.00122
Rellim Farm. The Rellim Farm near Kearneysville, West Virginia is a farm and orchard complex which was once part of the nearby Traveller's Rest property. The upper Shenandoah Valley region supports a significant fruit industry, and Rellim Farm is a representative example of this form of agriculture, the oldest family-owned operation in Jefferson County. Beginning in the 1930s, Paul Miller Sr.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Goshute Valley. The Goshute Valley is an endorheic landform of the Great Basin in Elko County, Nevada, United States. Description. The towns of Oasis and Cobre are in the valley's north, and the central and north of the valley contains broken flatlands, with short washes draining from the surrounding mountain ranges.

Geographic entities mentioned:
surface_form: goshute valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7702
lon: -114.413
The southern of the valley turns southwest and includes the northeast-flowing Nelson Creek which drains into a flatland sink. Currie is in the Steptoe Valley to the southwest end of the Goshute Valley adjacent a drainage divide between the north flowing Nelson Creek and the south flowing drainage into the intermittent Goshute Lake near the ghost town of Goshute.

Geographic entities mentioned:
surface_form: goshute valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7702
lon: -114.413
The Goshute Canyon Wilderness lies to the southwest in White Pine County. Salt desert. The Goshute Valley includes the largest of the Nevada salt desert ecoregions.

Geographic entities mentioned:
surface_form: goshute valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7702
lon: -114.413
The Goshute Valley is an endorheic landform of the Great Basin in Elko County, Nevada, United States. Description. The towns of Oasis and Cobre are in the valley's north, and the central and north of the valley contains broken flatlands, with short washes draining from the surrounding mountain ranges. Interstate 80 crosses the valley and has a junction with State Route 233 at Oasis.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The Goshute Valley is an endorheic landform of the Great Basin in Elko County, Nevada, United States. Description. The towns of Oasis and Cobre are in the valley's north, and the central and north of the valley contains broken flatlands, with short washes draining from the surrounding mountain ranges. Interstate 80 crosses the valley and has a junction with State Route 233 at Oasis.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Interstate 80 crosses the valley and has a junction with State Route 233 at Oasis. The Nevada Northern Railway traverses the valley north from Ely and intersects the Western Pacific Railroad at Shafter and continues on north to a connection with the Southern Pacific Railroad at Cobre.

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 Nevada Northern Railway traverses the valley north from Ely and intersects the Western Pacific Railroad at Shafter and continues on north to a connection with the Southern Pacific Railroad at Cobre. The southern of the valley turns southwest and includes the northeast-flowing Nelson Creek which drains into a flatland sink.

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
, Jane Preston, Editor; Sandra Alcosser, Lee Briccetti, Dr. John Fraser, Dr. Dan Wharton, Executive Editors; Poets House, New York City, NY, 2013. (This project is made possible by a grant from the U.S. Institute of Museum and Library Services.)
Rogers worked with sculptor of Public Art Associates to create this bench along the in Green Mountain Falls, Colorado, at the base of Pikes Peak.

Geographic entities mentioned:
surface_form: Pikes Peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.840555555556
lon: -105.04416666667
He used to own one of the largest yachts in the world, with a length of. In 2015 he sold &quot;Serene&quot; to Saudi Crown Prince Mohammed bin Salman for a reported $550 million. In March 2017 he bought Tulchan Estate on Speyside, Scotland's most expensive sporting estate.

Geographic entities mentioned:
surface_form: Speyside
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.45
lon: -3.3
Grand Teton National Park. Grand Teton National Park is a national park of the United States in northwestern Wyoming. At approximately, the park includes the major peaks of the Teton Range as well as most of the northern sections of the valley known as Jackson Hole. Grand Teton National Park is south of Yellowstone National Park, to which it is connected by the John D. Rockefeller Jr.

Geographic entities mentioned:
surface_form: Jackson Hole
instance_of: Valley
countries: United States
coordinates: lat: 43.516666666667
lon: -110.83333333333
The monument was abolished in 1950 and most of the monument land was added to Grand Teton National Park. Grand Teton National Park is named for Grand Teton, the tallest mountain in the Teton Range. At, Grand Teton rises more than above Jackson Hole. The park has numerous lakes, including Jackson Lake as well as streams and the upper main stem of the Snake River.

Geographic entities mentioned:
surface_form: Grand Teton
instance_of: Mountain
countries: United States
coordinates: lat: 43.7412
lon: -110.802
Of the other major peaks on the Teton Range, all were climbed by the late 1930s including Mount Moran in 1922 and Mount Owen in 1930 by Fritiof Fryxell and others after numerous previous attempts had failed. Both Middle and South Teton were first climbed on the same day, August 29, 1923, by a group of climbers led by Albert R. Ellingwood.

Geographic entities mentioned:
surface_form: Middle
instance_of: Mountain
countries: United States
coordinates: lat: 43.73
lon: -110.811
surface_form: South Teton
instance_of: Mountain
countries: United States
coordinates: lat: 43.7186
lon: -110.819
Rock climbing and bouldering had become popular in the park by the mid 20th century. In the late 1950s, gymnast John Gill came to the park and started climbing large boulders near Jenny Lake. Gill approached climbing from a gymnastics perspective and while in the Tetons became the first known climber in history to use gymnastic chalk to improve handholds and to keep hands dry while climbing.

Geographic entities mentioned:
surface_form: Jenny Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.763888888889
lon: -110.73
In addition to Grand Teton, another nine peaks are over above sea level. Eight of these peaks between Avalanche and Cascade Canyons make up the often-photographed Cathedral Group. The most prominent peak north of Cascade Canyon is the monolithic Mount Moran () which rises above Jackson Lake. To the north of Mount Moran, the range eventually merges into the high altitude Yellowstone Plateau.

Geographic entities mentioned:
surface_form: Mount Moran
instance_of: Mountain
countries: United States
coordinates: lat: 43.835277777778
lon: -110.77638888889
Flowing from higher to lower elevations, the glaciers created more than a dozen U-shaped valleys throughout the range. Cascade Canyon is sandwiched between Mount Owen and Teewinot Mountain to the south and Symmetry Spire to the north and is situated immediately west of Jenny Lake. North to south, Webb, Moran, Paintbrush, Cascade, Death and Granite Canyons slice through Teton Range. Jackson Hole.

Geographic entities mentioned:
surface_form: Teewinot Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7472
lon: -110.78
surface_form: Symmetry Spire
instance_of: Mountain
countries: United States
coordinates: lat: 43.7736
lon: -110.766
Erosion of the range provided sediment in the valley so the topographic relief is only. Jackson Hole is comparatively flat, with only a modest increase in altitude south to north; however, a few isolated buttes such as Blacktail Butte and hills including Signal Mountain dot the valley floor. In addition to a few outcroppings, the Snake River has eroded terraces into Jackson Hole.

Geographic entities mentioned:
surface_form: Blacktail Butte
instance_of: Mountain
countries: United States
coordinates: lat: 43.6353
lon: -110.693