Sarmila/GeoWiki-Features huggingface dataset:
Mount Parrish. Mount Parrish is a mountain summit located in Alberta, Canada. Description. Mount Parrish is situated eight kilometers southwest of the town of Coleman in the Crowsnest Pass area and can be seen from Highway 3, the Crowsnest Highway. It is part of the Flathead Range which is a subset of the Canadian Rockies.

Geographic entities mentioned:
surface_form: mount parrish
instance_of: Mountain
countries: Canada
coordinates: lat: 49.575
lon: -114.58805555555556
Chinook Peak is to the northwest of Mt. Parrish and the nearest higher neighbor is Andy Good Peak, to the south. History. Mount Parrish is named after Sherman Parrish, an early settler in the Crowsnest Pass area in 1898. He homesteaded at the foot of this mountain and raised cattle. The mountain's toponym was officially adopted March 15, 1962, by the Geographical Names Board of Canada.

Geographic entities mentioned:
surface_form: mount parrish
instance_of: Mountain
countries: Canada
coordinates: lat: 49.575
lon: -114.58805555555556
All seven crewmembers perished in the accident. Some wreckage of the aircraft is still present. Geology. Mount Parrish is composed of limestone which is a sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger Cretaceous period rock during the Laramide orogeny. Climate.

Geographic entities mentioned:
surface_form: mount parrish
instance_of: Mountain
countries: Canada
coordinates: lat: 49.575
lon: -114.58805555555556
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger Cretaceous period rock during the Laramide orogeny. Climate. Based on the Köppen climate classification, Mount Parrish has an alpine subarctic climate with cold, snowy winters, and mild summers. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: mount parrish
instance_of: Mountain
countries: Canada
coordinates: lat: 49.575
lon: -114.58805555555556
Joseph Hayward Bailey, who served as a Surgeon in the U.S. Army. Her Dutch ancestors were from the Hudson River Valley area and New England. Williams would serve as the commander of Fort Mackinac with the 4th Regiment of Artillery from 1852 to 1856. Williams was later assigned to posts in Florida and the Utah Territory.

Geographic entities mentioned:
surface_form: Hudson River Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Aard el Borj. Aard el Borj is a mountain of southern Lebanon. It has an elevation of 671 metres.

Geographic entities mentioned:
surface_form: aard el borj
instance_of: Mountain
countries: Lebanon
coordinates: lat: 33.22138889
lon: 35.41472222
Lake Tornow. Lake Tornow () is a lake in Ruppin Switzerland in Brandenburg, Germany. It is located east of Kunsterspring and south of Binenwalde and not far from the residential area of Tornow. It lies completely within the municipal boundaries of Neuruppin. The lake is a state waterway. It is wide and long, with an area of and a maximum depth of. Interpretation of the name.

Geographic entities mentioned:
surface_form: lake tornow
instance_of: Lake
countries: Germany
coordinates: lat: 53.0253
lon: 12.8031
Geography. The lake is part of the Ruppin Switzerland nature reserve and the Ruppin Switzerland waterway in a glacial channel formed by the Kalksee Lake to the north of the Lake Tornow, the Lake Tornow itself, and to the south of it the Lake Zermützelsee, Lake Tetzensee, Lake Molchowsee, and the Rhin. The chain of lakes stretches for around 40 kilometers south to the upper part of the Rhinluch.

Geographic entities mentioned:
surface_form: lake tornow
instance_of: Lake
countries: Germany
coordinates: lat: 53.0253
lon: 12.8031
surface_form: lake tornow
instance_of: Lake
countries: Germany
coordinates: lat: 53.0253
lon: 12.8031
It is known for the Milotice Castle, which is protected as a national cultural monument. Geography. Milotice is located about north of Hodonín and southeast of Brno. It lies in a flat landscape of the Lower Morava Valley. In the eastern part of the municipality is located the fishpond Písečný rybník, protected as a nature reserve. History. The first written mention of Milotice is from 1341.

Geographic entities mentioned:
surface_form: Lower Morava Valley
instance_of: Valley
countries: Czech Republic
coordinates: lat: 48.9430014
lon: 17.3295197
Tram Hollow (Ripley County, Missouri). Tram Hollow is a valley in Ripley County in the U.S. state of Missouri. Tram Hollow was so named on account of the tramway the valley once contained.

Geographic entities mentioned:
surface_form: tram hollow
instance_of: Valley
countries: United States
coordinates: lat: 36.804499
lon: -91.072074
surface_form: tram hollow
instance_of: Valley
countries: United States
coordinates: lat: 36.847555
lon: -91.319301
Tram Hollow (Ripley County, Missouri). Tram Hollow is a valley in Ripley County in the U.S. state of Missouri. Tram Hollow was so named on account of the tramway the valley once contained.

Geographic entities mentioned:
surface_form: tram hollow
instance_of: Valley
countries: United States
coordinates: lat: 36.804499
lon: -91.072074
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: tram hollow
instance_of: Valley
countries: United States
coordinates: lat: 36.847555
lon: -91.319301
Mandarmani. Mandarmani is a seaside resort village in the state of West Bengal, India, and lies in East Midnapore district, at the northern end of the Bay of Bengal. It is one of the largest seaside resorts of West Bengal, fast-developing. Location. It is almost 200 km from Kolkata Airport on the old Delhi route. Red crabs crawling around the 13 km long beach is a special attraction of Mandarmani.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Sveshtnik. Svesthnik () is a 1,975 m peak in the Pirin mountain range, south-western Bulgaria, making it the second highest summit in South Pirin after Ushite (1,978 m). It rises on the main mountain ridge to the south of Popovi Livadi saddle and to the north-west of Ushite. Svesthnik is built up of granite and has a conical shape with rounded steep slopes.

Geographic entities mentioned:
surface_form: sveshtnik
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 41.5216
lon: 23.6291
Svesthnik is built up of granite and has a conical shape with rounded steep slopes. Its slopes are covered with forests of Scots pine (&quot;Pinus sylvestris&quot;) and Norway spruce (&quot;Picea abies&quot;), while the summit itself is bare, covered with subalpine herbaceous vegetation. Most sources have traditionally referred to Sveshtnik as the highest summit in the southern division of Pirin.

Geographic entities mentioned:
surface_form: sveshtnik
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 41.5216
lon: 23.6291
In 1996, he was elected the University of Illinois &quot;Man of the Year&quot;, in recognition of his sports and other accomplishments, and awarded the school's &quot;I&quot; Award for his achievements. In 2004, he was given the honor of lighting a torch at the 56th Israeli Independence Day ceremony on Mount Herzl. He and Maccabi Tel Aviv were the first non-U.S.

Geographic entities mentioned:
surface_form: Mount Herzl
instance_of: Mountain
countries: Israel
coordinates: lat: 31.774117
lon: 35.180567
A sampling of his shiurim on the Torah can be found in the &quot;sefer&quot; &quot;Ohr Gedalyahu&quot; (Light of Gedalyahu), a compendium of novel and lucid discourses on Jewish thought that he delivered in the last three years of his life. He died in Brooklyn, New York, on July 2, 1979 and was interred on the Har HaZeisim.

Geographic entities mentioned:
surface_form: Har HaZeisim
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
Morgan Lake (Oregon). Morgan Lake is a lake in the Umatilla National Forest in the heart of Union County in the U.S. state of Oregon. It is located west of La Grande, at an elevation of. In 1976 an earthen dam was constructed on the preexisting lake, long and high, for irrigation and electrical purposes. A U.S. Forest Service campground at the lake has 17 sites.

Geographic entities mentioned:
surface_form: morgan lake
instance_of: Lake
countries: United States
coordinates: lat: 45.300833333333
lon: -118.13583333333
First planted in 1679, Stellenbosch is located east of Cape Town. The region is surrounded by the Helderberg, Simonsberg and Stellenbosch Mountains and receives some climatic influences from nearby False Bay. The bay tempers the climate and keeps average temperatures during the summer growing season to around, just slightly warmer than Bordeaux.

Geographic entities mentioned:
surface_form: Simonsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 54.436666666667
lon: 8.9719444444444
The Ki language, &quot;Tuki&quot; (Baki, Oki), is a Southern Bantoid language of Cameroon. It is spoken by 26,000 people in the Central Province of Cameroon, in the Lekie division and in the Mbam and Kim division, along the Sanaga river. The dialects are Kombe (Tukombe), Cenga (Tocenga), Tsinga (Tutsingo), Bundum, Njo (Tonjo), Ngoro (Tu Ngoro), Mbere (Tumvele) and possibly Mengisa and Mbwasa.

Geographic entities mentioned:
surface_form: Sanaga river
instance_of: Watercourse
countries: Cameroon
coordinates: lat: 3.5593388888889
lon: 9.652175
In 1782, his family was killed during the Corbly Family massacre. The farm name of 'Slave Gallant' derived from Slieve Gallion in Ireland, which was nearby where John Corbley was born and raised before emigrating to Pennsylvania. It was listed on the National Register of Historic Places in 1984.

Geographic entities mentioned:
surface_form: Slieve Gallion
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.73
lon: -6.76
Three Mountains of Dewa. The refer to the three sacred mountains of Mount Haguro, Mount Gassan and Mount Yudono, which are clustered together in the ancient province of Dewa (modern-day Yamagata Prefecture). Holy to the Japanese Shinto religion and especially the mountain ascetic cult of Shugendo, Dewa Sanzan are a popular pilgrimage site visited by many, including famed haiku poet Matsuo Bashō.

Geographic entities mentioned:
surface_form: Mount Haguro
instance_of: Mountain
countries: Japan
coordinates: lat: 38.7008
lon: 139.9825
surface_form: Mount Gassan
instance_of: Mountain
countries: Japan
coordinates: lat: 38.548888888889
lon: 140.02694444444
surface_form: Mount Yudono
instance_of: Mountain
countries: Japan
coordinates: lat: 38.531111111111
lon: 139.985
These changes in religious association also altered the designation of the shrines located on the Dewa Sanzan. In the Empire of Japan, Hagurosan Shrine and Yudonosan Shrine were designated as kokuhei shosha, while Gassan Shrine on Mount Gassan was considered a kanpei taisha. Today all three are considered equal Beppyo shrines
Significance in Japanese religion.

Geographic entities mentioned:
surface_form: Mount Gassan
instance_of: Mountain
countries: Japan
coordinates: lat: 38.548888888889
lon: 140.02694444444
A battery from the 1074th artillery battalion of the 108th Motor Rifle Division used 240 mm mortars towed by MT-LB tractors against the Muhajeddin forces of Ahmed Shah Massoud in the Charikorskoy and Panjshir valley, including the first use of specialized laser-guided &quot;Daredevil&quot; rounds.

Geographic entities mentioned:
surface_form: Panjshir valley
instance_of: Valley
countries: Afghanistan
coordinates: lat: 35.266666666667
lon: 69.466666666667
The separation gives room for interstitial, eight-coordinated calcium between chains. History. Collinsite was discovered prior to 1927 near François Lake, British Columbia. In a, phosphorite nodules were discovered that consisted of a fragment of andesite enclosed by concentric layers of phosphate minerals coated in wurtzilite.

Geographic entities mentioned:
surface_form: François Lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05
lon: -125.75
He also won one world (1974) and two European titles (1971 and 1973). Schmied went to the 1978 World Rowing Championships on Lake Karapiro in New Zealand as a reserve but did not compete. It was at those championships that he got closer to one of the female rowers whom she later married; Bärbel Bendiks was also present as a reserve.

Geographic entities mentioned:
surface_form: Lake Karapiro
instance_of: Lake
countries: New Zealand
coordinates: lat: -37.943167
lon: 175.560833
M-183 (Michigan highway). M-183 is a north–south state trunkline highway in the Upper Peninsula of the US state of Michigan. It serves Fayette State Park as an access route from US Highway 2 (US 2). The highway runs through rural farmlands of the Garden Peninsula and next to Big Bay de Noc, a bay of Lake Michigan. The community at Fayette dates back to the 1860s.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Lake Keeri. Keeri is a lake of Estonia, Tartu County.

Geographic entities mentioned:
surface_form: lake keeri
instance_of: Lake
countries: Estonia
coordinates: lat: 58.3270499
lon: 26.4585014
It straddles the northward-flowing Chittenango Creek, which serves as the boundary between Onondaga County's town of Cicero on the west side of the creek and Madison County's town of Sullivan on the east side of the creek. The hamlet's namesake bridge spans the creek, which empties into Oneida Lake 2.25 linear miles approximately north of the bridge.

Geographic entities mentioned:
surface_form: Oneida Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.2
lon: -75.9
Agriculture. The Breisgau is known for its wine and used for fruit tree orchards and grain. Places in the Breisgau. The biggest city by far in the Breisgau region is Freiburg. Other notable cities and towns are Bad Krozingen, Breisach, Emmendingen, Endingen, Kenzingen, Neuenburg, Staufen and Waldkirch. A prominent mountain is the Schauinsland (1,284 m).

Geographic entities mentioned:
surface_form: Schauinsland
instance_of: Mountain
countries: Germany
coordinates: lat: 47.911111111111
lon: 7.8994444444444
Catoctin Valley. The Catoctin Valley is a small valley, geographically and culturally associated with the larger Loudoun Valley in Loudoun County, Virginia. Geography. The Catoctin Valley encompasses the northern part of the Loudoun Valley east of the Short Hill Mountain and west of Catoctin Mountain.

Geographic entities mentioned:
surface_form: Loudoun Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.2329
lon: -77.735
surface_form: catoctin valley
instance_of: Valley
countries: United States
coordinates: lat: 39.23
lon: -77.64
Geography. The Catoctin Valley encompasses the northern part of the Loudoun Valley east of the Short Hill Mountain and west of Catoctin Mountain. Its northern border is the Potomac River, while its southern border is an intangible line running from the southern terminus of the Short Hill to the base of Catoctin Mountain, located approximately two miles north of Virginia State Route 7.

Geographic entities mentioned:
surface_form: Short Hill Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.25
lon: -77.71
surface_form: Catoctin Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6478
lon: -77.4664
surface_form: loudoun valley
instance_of: Valley
countries: United States
coordinates: lat: 39.2329
lon: -77.735
surface_form: catoctin valley
instance_of: Valley
countries: United States
coordinates: lat: 39.23
lon: -77.64
Its northern border is the Potomac River, while its southern border is an intangible line running from the southern terminus of the Short Hill to the base of Catoctin Mountain, located approximately two miles north of Virginia State Route 7. Across the Potomac in Maryland, the valley continues on as the Middletown Valley, which historically has also been known as the Catoctin Valley.

Geographic entities mentioned:
surface_form: Middletown Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.43
lon: -77.53
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: catoctin valley
instance_of: Valley
countries: United States
coordinates: lat: 39.23
lon: -77.64
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
They established small self-sufficient farms centered on small mill villages. They brought with them and employed few if any slaves. This region of Loudoun stood in stark contrast to the southern Loudoun Valley and areas east of the Catoctin Mountain, where plantation-style farming was established by English settlers moving north out of Tidewater Virginia.

Geographic entities mentioned:
surface_form: loudoun valley
instance_of: Valley
countries: United States
coordinates: lat: 39.2329
lon: -77.735
surface_form: catoctin mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6478
lon: -77.4664
Geography. The Catoctin Valley encompasses the northern part of the Loudoun Valley east of the Short Hill Mountain and west of Catoctin Mountain. Its northern border is the Potomac River, while its southern border is an intangible line running from the southern terminus of the Short Hill to the base of Catoctin Mountain, located approximately two miles north of Virginia State Route 7.

Geographic entities mentioned:
surface_form: catoctin mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6478
lon: -77.4664
Across the Potomac in Maryland, the valley continues on as the Middletown Valley, which historically has also been known as the Catoctin Valley. The valley contains the communities of Waterford, Lovettsville, Wheatland, Morrisonville and Taylorstown. The valley is approximately wide east to west and long north to south. The valley is drained by the Catoctin Creek and its tributaries.

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 valley contains the communities of Waterford, Lovettsville, Wheatland, Morrisonville and Taylorstown. The valley is approximately wide east to west and long north to south. The valley is drained by the Catoctin Creek and its tributaries. Transportation.

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 valley is drained by the Catoctin Creek and its tributaries. Transportation. Virginia State Route 287, the Berlin Turnpike, is the major road through the valley, running north–south from the Potomac River to Virginia State Route 7. Virginia State Route 9 runs east–west across the very southern portion of the valley. History.

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
Transportation. Virginia State Route 287, the Berlin Turnpike, is the major road through the valley, running north–south from the Potomac River to Virginia State Route 7. Virginia State Route 9 runs east–west across the very southern portion of the valley. History. The valley was settled in the 1730s by German and Quaker immigrants who migrated south from southern Pennsylvania.

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
Virginia State Route 9 runs east–west across the very southern portion of the valley. History. The valley was settled in the 1730s by German and Quaker immigrants who migrated south from southern Pennsylvania. They established small self-sufficient farms centered on small mill villages. They brought with them and employed few if any slaves.

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
Catoctin Valley. The Catoctin Valley is a small valley, geographically and culturally associated with the larger Loudoun Valley in Loudoun County, Virginia. Geography. The Catoctin Valley encompasses the northern part of the Loudoun Valley east of the Short Hill Mountain and west of Catoctin Mountain.

Geographic entities mentioned:
surface_form: catoctin valley
instance_of: Valley
countries: United States
coordinates: lat: 39.23
lon: -77.64
According to the U.S. Census Bureau, the county has a total area of, of which is land and (16%) is water. The county is located in the state's Upper Peninsula on the shore of Lake Superior, at the southeast base of the Keweenaw Peninsula. The villages of Baraga and L'Anse are located at the base of Lake Superior's Keweenaw Bay. Point Abbaye projects north into the lake, enclosing Huron Bay.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
The villages of Baraga and L'Anse are located at the base of Lake Superior's Keweenaw Bay. Point Abbaye projects north into the lake, enclosing Huron Bay. The eastern two-thirds of the county includes much of the Huron Mountains, including Mount Arvon—the highest natural point in Michigan at. Demographics. The 2010 United States census indicated Baraga County had a population of 8,860.

Geographic entities mentioned:
surface_form: Mount Arvon
instance_of: Mountain
countries: United States
coordinates: lat: 46.755813888889
lon: -88.155433333333
Mount Bonifato. Mount Bonifato (825 metres high) is a mountain in north western Sicilly in the province of Trapani. It is famous for the pine forest and the Nature Reserve Bosco di Alcamo. On its slopes they have found a proto-historic necropolis and traces of an ancient settlement.

Geographic entities mentioned:
surface_form: mount bonifato
instance_of: Mountain
countries: Italy
coordinates: lat: 37.9608
lon: 12.9562
Territory. Mount Bonifato is located in the hinterland of Golfo di Castellammare, between the valley of Fiume Freddo (a river on the west) and Fiume Jato (a river on the east). It shows quite steep faces on the south, while the declivity is more gradual in the northern part of the mountain, in proximity of Alcamo.

Geographic entities mentioned:
surface_form: mount bonifato
instance_of: Mountain
countries: Italy
coordinates: lat: 37.9608
lon: 12.9562
Archeological research. Since the second half of the 16th century Mount Bonifato has already been explored by scholars who identified different archaeological sites on the mountain, such as the ruins of the old residential area, discovered by the scholar Tommaso Fazello.

Geographic entities mentioned:
surface_form: mount bonifato
instance_of: Mountain
countries: Italy
coordinates: lat: 37.9608
lon: 12.9562
The archaeological remains on Mount Bonifato were subjects of research by the historians Ignazio de Blasi (18th century) and Vincenzo di Giovanni (19th century). At the Regional Archeological Museum Antonio Salinas there are also some lanterns and stamps of bricks dating back to the Roman age, collected on Mount Bonifato by Pietro Maria Rocca during the 19th century.

Geographic entities mentioned:
surface_form: mount bonifato
instance_of: Mountain
countries: Italy
coordinates: lat: 37.9608
lon: 12.9562
Until the first decades of the 19th century the mountain was covered with an oak wood of ilex and downy oak. In the thirties they began a massive reforestation prevalently with Aleppo's pine that is the prevailing essence nowadays. The access to the mount and the Nature Reserve is provided by a town street: Via per monte Bonifato.

Geographic entities mentioned:
surface_form: monte bonifato
instance_of: Mountain
countries: Italy
coordinates: lat: 37.9608
lon: 12.9562
Chwarel Ddu quarry. Chwarel Ddu quarry was the earliest slate quarry in the Lledr Valley. It was working before 1810, and continued in sporadic operation until the late 1920s. It is about west of Dolwyddelan, just beneath Dolwyddelan Castle. History. The quarry is believed to have opened between 1800 and 1805.

Geographic entities mentioned:
surface_form: Lledr Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.06
lon: -3.87
Lake Aricoma. Lake Aricoma (possibly from Aymara for a variety of tuber &quot;(Smallanthus sonchifolius)&quot;,) is a lake in the Andes of Peru. It is situated in the Puno Region, Carabaya Province, Crucero District. The lake lies west of the mountains Aricoma and Jalahuana, and east of the lake Veluyoc Cocha.

Geographic entities mentioned:
surface_form: Aricoma
instance_of: Mountain
countries: Peru
coordinates: lat: -14.3119
lon: -69.7833
surface_form: Jalahuana
instance_of: Mountain
countries: Peru
coordinates: lat: -14.3347
lon: -69.7369
surface_form: lake veluyoc cocha
instance_of: Lake
countries: Peru
coordinates: lat: -14.31
lon: -69.831388888889
surface_form: veluyoc cocha
instance_of: Lake
countries: Peru
coordinates: lat: -14.31
lon: -69.831388888889
surface_form: jalahuana
instance_of: Mountain
countries: Peru
coordinates: lat: -14.3347
lon: -69.7369
surface_form: aricoma
instance_of: Mountain
countries: Peru
coordinates: lat: -14.3119
lon: -69.7833
Lake Aricoma. Lake Aricoma (possibly from Aymara for a variety of tuber &quot;(Smallanthus sonchifolius)&quot;,) is a lake in the Andes of Peru. It is situated in the Puno Region, Carabaya Province, Crucero District. The lake lies west of the mountains Aricoma and Jalahuana, and east of the lake Veluyoc Cocha.

Geographic entities mentioned:
surface_form: lake aricoma
instance_of: Lake
countries: Peru
coordinates: lat: -14.326388888889
lon: -69.812777777778
surface_form: aricoma
instance_of: Mountain
countries: Peru
coordinates: lat: -14.3119
lon: -69.7833
The Sisters (Alaska). The Sisters are mountain summits in Alaska, United States. Description. The Sisters are located on the west coast of Baranof Island, approximately northeast of Sitka. The highest peak reaches an elevation of. This mountain group is part of the Alexander Archipelago and is set on land managed by Tongass National Forest.

Geographic entities mentioned:
surface_form: the sisters (alaska)
instance_of: Mountain
coordinates: lat: 57.1004816
lon: -135.2199454
The Sisters (Alaska). The Sisters are mountain summits in Alaska, United States. Description. The Sisters are located on the west coast of Baranof Island, approximately northeast of Sitka. The highest peak reaches an elevation of. This mountain group is part of the Alexander Archipelago and is set on land managed by Tongass National Forest.

Geographic entities mentioned:
surface_form: the sisters
instance_of: Mountain
coordinates: lat: 57.1004816
lon: -135.2199454
Board on Geographic Names. Climate. Based on the Köppen climate classification, The Sisters is located in a subpolar oceanic climate zone with long, cold, snowy winters, and cool summers. Weather systems coming off the Gulf of Alaska are forced upwards by the mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall.

Geographic entities mentioned:
surface_form: the sisters
instance_of: Mountain
coordinates: lat: 57.1004816
lon: -135.2199454
Description. The Sisters are located on the west coast of Baranof Island, approximately northeast of Sitka. The highest peak reaches an elevation of. This mountain group is part of the Alexander Archipelago and is set on land managed by Tongass National Forest. Precipitation runoff from the mountain drains to the Indian River and Sitka Sound.

Geographic entities mentioned:
surface_form: alexander
instance_of: Mountain
coordinates: lat: -63.3039
lon: -55.80564
Around a quarter of the common impala populations occur in protected areas, such as the Okavango Delta (Botswana); Masai Mara and Kajiado (Kenya); Kruger National Park (South Africa); the Ruaha and Serengeti National Parks and Selous Game Reserve (Tanzania); Luangwa Valley (Zambia); Hwange, Sebungwe and Zambezi Valley (Zimbabwe).

Geographic entities mentioned:
surface_form: Okavango Delta
instance_of: Body of water
Watercourse
countries: Botswana
coordinates: lat: -19.4
lon: 22.9
Its base is covered with scrub pine. The summit and below is overgrown with grass and shrubs. Approximately to the north is the Humboldt River and its valley. Eastward, there are hills and valleys. To the west is the Smoky Valley, Mount Hope, Bunker Hill, and other peaks of the Toiyabe Range. Mount Tenabo, east of and near the north end of the Toiyabe Range, is about south of Beowawe.

Geographic entities mentioned:
surface_form: Smoky Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.6644
lon: -117.171
surface_form: bunker hill
instance_of: Mountain
countries: United States
coordinates: lat: 39.2529
lon: -117.126
surface_form: bunker hill
instance_of: Mountain
countries: United States
coordinates: lat: 42.376361111111
lon: -71.060777777778
surface_form: mount hope
instance_of: Landform
countries: United States
coordinates: lat: 41.67388889
lon: -71.24
surface_form: mount hope
instance_of: Mountain
countries: United States
coordinates: lat: 39.0211
lon: -106.42
surface_form: mount hope
instance_of: Mountain
countries: United States
coordinates: lat: 39.795277777778
lon: -116.18833333333
Mount Tenabo. Mount Tenabo (Shoshoni: &quot;Lookout Mountain&quot;) is the principal peak in the Cortez Mountains. The mountain is of cultural and religious significance to the Western Shoshone people. Etymology. There are various theories as to the name's etymology.

Geographic entities mentioned:
surface_form: lookout mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.863713888889
lon: -85.392452777778
surface_form: lookout mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9473
lon: -74.6588
surface_form: lookout mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.553611111111
lon: -116.57388888889
surface_form: lookout mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.288888888889
lon: -118.49527777778
surface_form: lookout mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.248611111111
lon: -117.67611111111
surface_form: lookout mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.1168
lon: -96.0242
surface_form: lookout mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.55207
lon: -121.32929
surface_form: lookout mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.1927
lon: -114.759
surface_form: lookout mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.3422
lon: -121.524
surface_form: lookout mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.7658
lon: -105.239
surface_form: mount tenabo
instance_of: Mountain
countries: United States
coordinates: lat: 40.162977777778
lon: -116.58480555556
Mount Tenabo. Mount Tenabo (Shoshoni: &quot;Lookout Mountain&quot;) is the principal peak in the Cortez Mountains. The mountain is of cultural and religious significance to the Western Shoshone people. Etymology. There are various theories as to the name's etymology.

Geographic entities mentioned:
surface_form: shoshone
instance_of: Lake
countries: United States
coordinates: lat: 44.3722
lon: -110.713
Eastward, there are hills and valleys. To the west is the Smoky Valley, Mount Hope, Bunker Hill, and other peaks of the Toiyabe Range. Mount Tenabo, east of and near the north end of the Toiyabe Range, is about south of Beowawe. At an area approximately above the mountain's base, a vein of silver-bearing quartz cuts through obliquely, penetrating into the valley after for. Its width is.

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
Mount Tenabo. Mount Tenabo (Shoshoni: &quot;Lookout Mountain&quot;) is the principal peak in the Cortez Mountains. The mountain is of cultural and religious significance to the Western Shoshone people. Etymology. There are various theories as to the name's etymology.

Geographic entities mentioned:
surface_form: mount tenabo
instance_of: Mountain
countries: United States
coordinates: lat: 40.162977777778
lon: -116.58480555556
Etymology. There are various theories as to the name's etymology. The mountain may have been named by New Mexicans after an ancient pueblo, or Tenabo may be a Paiute word, meaning of &quot;dark colored water&quot;. Geography. The summit elevation of Mount Tenabo is, which is above the surrounding valleys. Its base is covered with scrub pine. The summit and below is overgrown with grass and shrubs.

Geographic entities mentioned:
surface_form: mount tenabo
instance_of: Mountain
countries: United States
coordinates: lat: 40.162977777778
lon: -116.58480555556
At an area approximately above the mountain's base, a vein of silver-bearing quartz cuts through obliquely, penetrating into the valley after for. Its width is. This vein (stratum) contains ore beds, and is encased in crystalline limestone. History. Silver ore was discovered at Mount Tenabo in 1862. By the later half of the 1860s, there were at least 20 working mills.

Geographic entities mentioned:
surface_form: mount tenabo
instance_of: Mountain
countries: United States
coordinates: lat: 40.162977777778
lon: -116.58480555556
History. Silver ore was discovered at Mount Tenabo in 1862. By the later half of the 1860s, there were at least 20 working mills. In 2008, the Te-Moak tribe, the Timbisha tribe and others sought an emergency injunction that would have halted further development of Barrick Gold's Cortez Hills mining operation which includes facilities on the slopes of Mount Tenabo.

Geographic entities mentioned:
surface_form: mount tenabo
instance_of: Mountain
countries: United States
coordinates: lat: 40.162977777778
lon: -116.58480555556
Topography. The fell stands on the ridge running south east from Fairfield to Dove Crag, at the point where a long subsidiary spur sweeps off to the north east. This is Hartsop above How and, although in reality part of Hart Crag, was treated as a separate fell by Alfred Wainwright in his &quot;Pictorial Guide to the Lakeland Fells&quot;. That convention is also followed here.

Geographic entities mentioned:
surface_form: Dove Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.485061111111
lon: -2.9677694444444
surface_form: fairfield
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4969
lon: -2.99059
Topography. The fell stands on the ridge running south east from Fairfield to Dove Crag, at the point where a long subsidiary spur sweeps off to the north east. This is Hartsop above How and, although in reality part of Hart Crag, was treated as a separate fell by Alfred Wainwright in his &quot;Pictorial Guide to the Lakeland Fells&quot;. That convention is also followed here.

Geographic entities mentioned:
surface_form: Hartsop above How
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4995
lon: -2.95421
surface_form: hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493080555556
lon: -2.9772194444444
This is a hanging valley, discharging via waterfalls into upper Deepdale. Deepdale Beck in turn runs north east to join other streams bound for Ullswater. The main faces of Hart Crag lie on this side, presenting a fine prospect from St Sunday Crag and other fells to the north. Dovedale is the third valley, running broadly eastward and separated from Deepdale by the Hartsop Above How ridge.

Geographic entities mentioned:
surface_form: St Sunday Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.512861111111
lon: -2.97615
surface_form: st sunday crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.512861111111
lon: -2.97615
surface_form: hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493080555556
lon: -2.9772194444444
This is the geographical link between Rydale and Link Cove, but there is no practicable walkers' route from one to the other. Beyond here the ridge mounts a rocky step (the end of Scrubby Crag) and then turns westward onto the widening grassy top of Fairfield. Dove Crag to the south-east is reached across the unnamed col between Houndshope Cove and Rydale.

Geographic entities mentioned:
surface_form: fairfield
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4969
lon: -2.99059
Two cairns mark the ends of a short ridge running along the top, with other cairns giving guidance to the viewpoints for Deepdale and Dovedale. The highest point is at the south-eastern end of the summit area, a little to the west of the main path. The view is good westward to the Scafells and also toward the Far Eastern Fells, but Fairfield and Dove Crag obscure much of the District. Ascents.

Geographic entities mentioned:
surface_form: dove crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.485061111111
lon: -2.9677694444444
surface_form: fairfield
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4969
lon: -2.99059
Hart Crag. Hart Crag is a fell in the English Lake District, being one of the Fairfield group of hills in the Eastern Fells. Topography. The fell stands on the ridge running south east from Fairfield to Dove Crag, at the point where a long subsidiary spur sweeps off to the north east.

Geographic entities mentioned:
surface_form: fairfield
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4969
lon: -2.99059
surface_form: hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493080555556
lon: -2.9772194444444
Immediately below Hart Crag is Houndshope Cove, a high level corrie in upper Dovedale. The ridge to Fairfield starts north-westward as far as the saddle of Link Hause (). This is the geographical link between Rydale and Link Cove, but there is no practicable walkers' route from one to the other.

Geographic entities mentioned:
surface_form: fairfield
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4969
lon: -2.99059
surface_form: the saddle
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.162395
lon: -5.414721
The view is good westward to the Scafells and also toward the Far Eastern Fells, but Fairfield and Dove Crag obscure much of the District. Ascents. Hart Crag is most commonly climbed as part of the Fairfield horseshoe. This popular fellwalk makes a circuit of Rydale, claiming 8 Wainwrights over a distance of. Starting at Bridgend, Hartsop Above How provides another means of indirect access.

Geographic entities mentioned:
surface_form: fairfield
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4969
lon: -2.99059
The main faces of Hart Crag lie on this side, presenting a fine prospect from St Sunday Crag and other fells to the north. Dovedale is the third valley, running broadly eastward and separated from Deepdale by the Hartsop Above How ridge. Immediately below Hart Crag is Houndshope Cove, a high level corrie in upper Dovedale.

Geographic entities mentioned:
surface_form: hartsop above how
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4995
lon: -2.95421
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.264
lon: -2.432
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.54
lon: -1.99
Hart Crag is most commonly climbed as part of the Fairfield horseshoe. This popular fellwalk makes a circuit of Rydale, claiming 8 Wainwrights over a distance of. Starting at Bridgend, Hartsop Above How provides another means of indirect access. A number of direct ascents are also possible. Rydale can be followed to its head from where the steep climb out of the valley leads to the summit.

Geographic entities mentioned:
surface_form: hartsop above how
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4995
lon: -2.95421
A number of direct ascents are also possible. Rydale can be followed to its head from where the steep climb out of the valley leads to the summit. Alternatively an approach can be made along Deepdale, skirting the worst of the bogs, and climbing onto the Hartsop Above How ridge from the lower part of Link Cove. Dovedale and Houndshope Cove provide a third possibility.

Geographic entities mentioned:
surface_form: hartsop above how
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4995
lon: -2.95421
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.264
lon: -2.432
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.54
lon: -1.99
This flows almost due south for, finally emptying into the River Rothay at Rydal village. The slopes of Rydal Head below Hart Crag are steep, but reasonably free of outcropping rock. To the north of Hart Crag is Link Cove. This is a hanging valley, discharging via waterfalls into upper Deepdale. Deepdale Beck in turn runs north east to join other streams bound for Ullswater.

Geographic entities mentioned:
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.264
lon: -2.432
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.264
lon: -2.432
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.54
lon: -1.99
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.54
lon: -1.99
Summit. The summit of Hart Crag has a covering of rock with rich turf showing through. Two cairns mark the ends of a short ridge running along the top, with other cairns giving guidance to the viewpoints for Deepdale and Dovedale. The highest point is at the south-eastern end of the summit area, a little to the west of the main path.

Geographic entities mentioned:
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.264
lon: -2.432
surface_form: dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.54
lon: -1.99
Hart Crag. Hart Crag is a fell in the English Lake District, being one of the Fairfield group of hills in the Eastern Fells. Topography. The fell stands on the ridge running south east from Fairfield to Dove Crag, at the point where a long subsidiary spur sweeps off to the north east.

Geographic entities mentioned:
surface_form: hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493080555556
lon: -2.9772194444444
That convention is also followed here. Being at the meeting point of three ridges, Hart Crag also has a share in three valleys. Despite forming a part of the headwall in each case, the fell is not the true head of any of them. West of the summit runs the long and unfrequented valley of Rydal Beck. This flows almost due south for, finally emptying into the River Rothay at Rydal village.

Geographic entities mentioned:
surface_form: hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493080555556
lon: -2.9772194444444
West of the summit runs the long and unfrequented valley of Rydal Beck. This flows almost due south for, finally emptying into the River Rothay at Rydal village. The slopes of Rydal Head below Hart Crag are steep, but reasonably free of outcropping rock. To the north of Hart Crag is Link Cove. This is a hanging valley, discharging via waterfalls into upper Deepdale.

Geographic entities mentioned:
surface_form: hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493080555556
lon: -2.9772194444444
This flows almost due south for, finally emptying into the River Rothay at Rydal village. The slopes of Rydal Head below Hart Crag are steep, but reasonably free of outcropping rock. To the north of Hart Crag is Link Cove. This is a hanging valley, discharging via waterfalls into upper Deepdale. Deepdale Beck in turn runs north east to join other streams bound for Ullswater.

Geographic entities mentioned:
surface_form: hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493080555556
lon: -2.9772194444444
Dovedale is the third valley, running broadly eastward and separated from Deepdale by the Hartsop Above How ridge. Immediately below Hart Crag is Houndshope Cove, a high level corrie in upper Dovedale. The ridge to Fairfield starts north-westward as far as the saddle of Link Hause ().

Geographic entities mentioned:
surface_form: hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493080555556
lon: -2.9772194444444
surface_form: dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
Dove Crag to the south-east is reached across the unnamed col between Houndshope Cove and Rydale. A stone wall runs along the majority of the ridge, providing an aid to route-finding in poor conditions. The Hartsop Above How ridge starts indistinctly from the summit of Hart Crag, a descent across a wide area of rough ground being made before a discernible ridgeline materialises. Summit.

Geographic entities mentioned:
surface_form: hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493080555556
lon: -2.9772194444444
Summit. The summit of Hart Crag has a covering of rock with rich turf showing through. Two cairns mark the ends of a short ridge running along the top, with other cairns giving guidance to the viewpoints for Deepdale and Dovedale. The highest point is at the south-eastern end of the summit area, a little to the west of the main path.

Geographic entities mentioned:
surface_form: hart crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493080555556
lon: -2.9772194444444
Sundarbans. The largest mangrove forest in the world is in the Sundarbans. The Sundarban forest lies in the vast delta on the Bay of Bengal formed by the super confluence of the Brahmaputra and Meghna rivers with distributaries of the Ganges. The seasonally flooded Sundarbans freshwater swamp forests lie inland from the mangrove forests on the coastal fringe.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88