Sarmila/GeoWiki-Features huggingface dataset:
As well as making the first ascent of some of the most significant unclimbed mountains in the Alps – the Grande Casse, Monte Viso, the Barre des Écrins and the Aiguille d'Argentière – he also made the first traverse of many previously uncrossed cols, including the col des Ecrins, the col du Sélé and the col du Glacier Blanc in the Massif des Écrins (all in 1862 with Francis Fox Tuckett, Peter Perren and Bartolomméo Peyrotte).

Geographic entities mentioned:
surface_form: Grande Casse
instance_of: Mountain
countries: France
coordinates: lat: 45.405278
lon: 6.8275
surface_form: Monte Viso
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6675
lon: 7.0916666666667
surface_form: Barre des Écrins
instance_of: Mountain
countries: France
coordinates: lat: 44.916666666667
lon: 6.3333333333333
surface_form: Aiguille d'Argentière
instance_of: Mountain
countries: Switzerland
France
coordinates: lat: 45.959761111111
lon: 7.0203194444444
In 1863, he climbed the Grandes Rousses with William Mathews, Thomas George Bonney and his brother Jean-Baptiste Croz, and in 1864 he made the first traverse of the brèche de la Meije and the first traverse of the col de la Pilatte (with Edward Whymper, Horace Walker, A. W. Moore and Saas-Fee guide Christian Almer). Of the latter expedition, Whymper was later to write,
Matterhorn accident.

Geographic entities mentioned:
surface_form: brèche de la Meije
instance_of: Mountain
countries: France
coordinates: lat: 45.004722222222
lon: 6.3086111111111
Of the latter expedition, Whymper was later to write,
Matterhorn accident. Following eight failed attempts on the Matterhorn starting from 1861, Whymper was recalled to London in the summer of 1864 and offered the services of Croz to his friend Adams-Reilly, advising him to make an attempt on the mountain (all three had been in a party that had made the first ascent of Mont Dolent that year).

Geographic entities mentioned:
surface_form: Mont Dolent
instance_of: Mountain
countries: Switzerland
Italy
France
coordinates: lat: 45.9225
lon: 7.0461111111111
This never came to anything, and the next year Croz was again employed by Whymper. Together with Christian Almer and Franz Biner they made the first ascent of the Grand Cornier, and the first ascent of &quot;Pointe Whymper&quot; on the Grandes Jorasses. On the Matterhorn, Croz and Whymper tried a route via a couloir on the south-east face but were unsuccessful.

Geographic entities mentioned:
surface_form: Grand Cornier
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.052222222222
lon: 7.6116666666667
surface_form: Grandes Jorasses
instance_of: Mountain
countries: Italy
France
coordinates: lat: 45.866666666667
lon: 6.9833333333333
S. Kennedy – they made the first ascent of the Moine ridge of the Aiguille Verte, whilst Whymper attempted to join forces with the Valtournenche guide Jean-Antoine Carrel. When this proved impossible (Carrel instead leading an Italian party on an attempt on the Italian ridge of the mountain), Whymper teamed up with Lord Francis Douglas and the two Zermatt guides, Peter Taugwalder father and son.

Geographic entities mentioned:
surface_form: Aiguille Verte
instance_of: Mountain
countries: France
coordinates: lat: 45.934722222222
lon: 6.97
&quot;Pointe Croz&quot; (4,110 m), a summit on the Grandes Jorasses, is named after him. It was first climbed in 1909, 'probably' by Eleonore Hasenclever, Wilhelm Klemm, Felix König and Richard Weitzenböck. The summit gives its name to the Croz Spur (), a major buttress on the north face of the mountain, one of the great north faces of the Alps.

Geographic entities mentioned:
surface_form: Grandes Jorasses
instance_of: Mountain
countries: Italy
France
coordinates: lat: 45.866666666667
lon: 6.9833333333333
He was missionary to the Māori in the western Waikato region. In 1839 he was sent to Kaitotehe, near Mount Taupiri, where he established the Kaitotehe Mission, with branch missions at Te Awamutu and Otawhao in the valley of the Waipā River. Early years. Ashwell was born on 26 May 1810 at Birmingham, England. His father was Benjamin Ashwell, a brassfounder.

Geographic entities mentioned:
surface_form: Mount Taupiri
instance_of: Mountain
countries: New Zealand
coordinates: lat: -37.603
lon: 175.186389
In 1838 the Revd. Robert Maunsell and Ashwell set up a mission station and a school at Port Waikato among the Ngāti Tāhinga. In 1839 he was sent to Kaitotehe, near Mount Taupiri, where he established the Kaitotehe Mission, with branch missions at Te Awamutu and Otawhao in the valley of the Waipā River. He remained at that mission into the 1840s.

Geographic entities mentioned:
surface_form: Mount Taupiri
instance_of: Mountain
countries: New Zealand
coordinates: lat: -37.603
lon: 175.186389
In Queensland it grows as far north as the Atherton Tableland, in the eastern half of New South Wales, the southern half of Victoria, the south-eastern corner of South Australia and in Tasmania, including King and Flinders Islands. It has also been found in New Zealand but is regarded as a vagrant there because the insect pollinator is not present in that country.

Geographic entities mentioned:
surface_form: Atherton Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
Regional officials in Tuscany are responsible for organizing a massive project, the purpose of which is to not only protect the area from future flooding but to maintain high water quality and effectively utilize water resources. Work commenced in 1984, with the construction of the Bilancino Dam, near Florence. The Sieve tributary and spillway at Pontedera are among other developments.

Geographic entities mentioned:
surface_form: Bilancino Dam
instance_of: Lake
countries: Italy
coordinates: lat: 43.977222222222
lon: 11.263333333333
Eaton collected insects 'whenever opportunity offered, which was not often.' The Eatons entered Norway via Christiana [<nowiki/>Oslo]. Travelling by rail, road and steamer ship, their travel itinerary had the stopping at Sandviken, Hønefoss, Heen, Sørum, through the Valdres District to Lærdalsøren, Gudvangen, Vossevangen, Eide and Bergen along with intermediate localities on route.

Geographic entities mentioned:
surface_form: Valdres
instance_of: Valley
countries: Norway
coordinates: lat: 60.916666666667
lon: 9.1666666666667
This was one of the first numbered state routes designated in Tennessee. This road followed the approximately location of the Road Prong Trail between Indian Gap and the Chimney Tops trailhead. In 1932, SR 71 was rerouted onto the present-day road between Newfound Gap and Gatlinburg.

Geographic entities mentioned:
surface_form: Chimney Tops
instance_of: Mountain
countries: United States
coordinates: lat: 35.629261111111
lon: -83.476272222222
The area is situated within the municipalities Oslo, Lørenskog, Rælingen, Ski and Enebakk. Østmarka is delimited to the west by populated areas of Oslo, to the north of communities of Skårer, Lørenskog and Rælingen and to the east by the lake Øyeren, to the south-east lies Enebakk and to the south-west Sørmarka, another forested area.

Geographic entities mentioned:
surface_form: Øyeren
instance_of: Lake
countries: Norway
coordinates: lat: 59.857222222222
lon: 11.163333333333
In Østmarka alone there were over 2,000 drivers and 4-5000 horses occupied with moving planks between Øyeren and Kristiania (today Oslo). It was too long to drive from Enebakk via Øyeren and Strømsveien to get to Kristiania. This is why the Plank Road was built.

Geographic entities mentioned:
surface_form: Øyeren
instance_of: Lake
countries: Norway
coordinates: lat: 59.857222222222
lon: 11.163333333333
This is why the Plank Road was built. The Plank Road starts at Eikeberg and Børter in Enebakk - it crosses the ice on Børtervann and moves up to Rausjø and turns up towards Vangen and Skjelbreia, further over Eriksvann, Søndre Skytten, Elvåga, across to Nøklevann, Rustadsaga, Østensjøvannet and down to the city. The Plank Road is today open and tagged as a ski track.

Geographic entities mentioned:
surface_form: Østensjøvannet
instance_of: Lake
countries: Norway
coordinates: lat: 59.888333333333
lon: 10.826944444444
Notable achievements. Founded in 1966 to stop the development of ski slopes on Massachusetts' highest peak, Mount Greylock, CLF has since expanded its advocacy to address both environmental and community issues in all six New England states. Traditional environmental advocacy.

Geographic entities mentioned:
surface_form: Mount Greylock
instance_of: Mountain
countries: United States
coordinates: lat: 42.6375
lon: -73.166666666667
Since that time, CLF's legal advocacy has focused on several natural resources cases, including the cleanup of Lake Champlain, the prevention of overfishing of groundfish – cod, haddock, and flounder – off the coast of New England (resulting in a settlement requiring the National Marine Fisheries Service to produce a management plan to eliminate overfishing), and the protection of the Vermont black bear habitat (by obtaining a federal court injunction halting destructive U.S.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Yaghnobi language. Yaghnobi is an Eastern Iranian language spoken in the upper valley of the Yaghnob River in the Zarafshan area of Tajikistan by the Yaghnobi people. It is considered to be a direct descendant of Sogdian and has sometimes been called Neo-Sogdian in academic literature. There are some 12,500 Yaghnobi speakers, divided into several communities.

Geographic entities mentioned:
surface_form: upper valley
instance_of: Valley
countries: Tajikistan
coordinates: lat: 39.2
lon: 69
Toe Jam Hill. Toe Jam Hill, 425 feet tall, is the high point on Bainbridge Island, Washington and one of the highest points in Kitsap County, Washington.

Geographic entities mentioned:
surface_form: toe jam hill
instance_of: Mountain
countries: United States
coordinates: lat: 47.5842
lon: -122.502
Toe Jam Hill. Toe Jam Hill, 425 feet tall, is the high point on Bainbridge Island, Washington and one of the highest points in Kitsap County, Washington.

Geographic entities mentioned:
surface_form: toe jam hill
instance_of: Mountain
countries: United States
coordinates: lat: 47.5842
lon: -122.502
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
The hill was once a &quot;villainous&quot; milestone for bicycle riders on the Chilly Hilly season opener sponsored by Seattle's Cascade Bicycle Club, and on the Bainbridge Island Half Marathon, formerly called Toe Jam Hill Half Marathon. The Bainbridge Island high point's location is reported variously at highpointing websites.

Geographic entities mentioned:
surface_form: toe jam hill
instance_of: Mountain
countries: United States
coordinates: lat: 47.5842
lon: -122.502
Listsofjohn.com gives Gazzam Lake Hill based on USGS topographic maps, which used photographic aerial surveys and stereoplotters. Peakbagger.com gives Toe Jam Hill at 15 feet higher or more, based on newer high-resolution LIDAR maps. LIDAR surveys in the 1990s also identified a geologic fault, now named the Toe Jam Hill Fault, north of the hill.

Geographic entities mentioned:
surface_form: toe jam hill
instance_of: Mountain
countries: United States
coordinates: lat: 47.5842
lon: -122.502
Peakbagger.com gives Toe Jam Hill at 15 feet higher or more, based on newer high-resolution LIDAR maps. LIDAR surveys in the 1990s also identified a geologic fault, now named the Toe Jam Hill Fault, north of the hill. It may intersect and may be secondary to the Seattle Fault. It was the first fault discovered by laser imagery.

Geographic entities mentioned:
surface_form: toe jam hill
instance_of: Mountain
countries: United States
coordinates: lat: 47.5842
lon: -122.502
LIDAR surveys in the 1990s also identified a geologic fault, now named the Toe Jam Hill Fault, north of the hill. It may intersect and may be secondary to the Seattle Fault. It was the first fault discovered by laser imagery. A city park, Nutes Pond Park (also spelled Nute's Pond), was created on Toe Jam Hill in 2011.

Geographic entities mentioned:
surface_form: toe jam hill
instance_of: Mountain
countries: United States
coordinates: lat: 47.5842
lon: -122.502
Little Wall Lake. Little Wall Lake is a natural lake in Hamilton County, Iowa, south of the town of Jewell. Said to be glacial in origin, in modern times it has required dredging to keep it from becoming marshland.

Geographic entities mentioned:
surface_form: little wall lake
instance_of: Lake
countries: United States
coordinates: lat: 42.27
lon: -93.6375
surface_form: wall lake
instance_of: Lake
countries: United States
coordinates: lat: 46.273055555556
lon: -95.964166666667
Said to be glacial in origin, in modern times it has required dredging to keep it from becoming marshland. On the northern end of the lake is Little Wall Lake Park, run by the county, which has camping facilities with full utility hook-ups, three cabins for rent, sixteen tent-only sites, a shower building, a boat ramp, a jetty, and kayak and canoe rentals.

Geographic entities mentioned:
surface_form: little wall lake
instance_of: Lake
countries: United States
coordinates: lat: 42.27
lon: -93.6375
surface_form: wall lake
instance_of: Lake
countries: United States
coordinates: lat: 46.273055555556
lon: -95.964166666667
On the northern end of the lake is Little Wall Lake Park, run by the county, which has camping facilities with full utility hook-ups, three cabins for rent, sixteen tent-only sites, a shower building, a boat ramp, a jetty, and kayak and canoe rentals. Big Wall Lake lies some to the north and is not hydrologically connected to Little Wall Lake.

Geographic entities mentioned:
surface_form: little wall lake
instance_of: Lake
countries: United States
coordinates: lat: 42.27
lon: -93.6375
surface_form: wall lake
instance_of: Lake
countries: United States
coordinates: lat: 46.273055555556
lon: -95.964166666667
surface_form: wall lake
instance_of: Lake
countries: United States
coordinates: lat: 46.273055555556
lon: -95.964166666667
Pool Malebo. The Pool Malebo, formerly Stanley Pool, also known as Mpumbu, Lake Nkunda or Lake Nkuna by local indigenous people in pre-colonial times, is a lake-like widening in the lower reaches of the Congo River. The river serves as the border between the Republic of the Congo to the north and the Democratic Republic of the Congo to the south.

Geographic entities mentioned:
surface_form: lake nkunda
instance_of: Lake
countries: Republic of the Congo
Democratic Republic of the Congo
coordinates: lat: -4.2819444444444
lon: 15.488611111111
surface_form: malebo
instance_of: Lake
countries: Republic of the Congo
Democratic Republic of the Congo
coordinates: lat: -4.2819444444444
lon: 15.488611111111
surface_form: nkunda
instance_of: Lake
countries: Republic of the Congo
Democratic Republic of the Congo
coordinates: lat: -4.2819444444444
lon: 15.488611111111
surface_form: stanley pool
instance_of: Lake
countries: Republic of the Congo
Democratic Republic of the Congo
coordinates: lat: -4.2819444444444
lon: 15.488611111111
surface_form: pool malebo
instance_of: Lake
countries: Republic of the Congo
Democratic Republic of the Congo
coordinates: lat: -4.2819444444444
lon: 15.488611111111
surface_form: nkuna
instance_of: Lake
countries: Republic of the Congo
Democratic Republic of the Congo
coordinates: lat: -4.2819444444444
lon: 15.488611111111
Pool Malebo. The Pool Malebo, formerly Stanley Pool, also known as Mpumbu, Lake Nkunda or Lake Nkuna by local indigenous people in pre-colonial times, is a lake-like widening in the lower reaches of the Congo River. The river serves as the border between the Republic of the Congo to the north and the Democratic Republic of the Congo to the south.

Geographic entities mentioned:
surface_form: malebo
instance_of: Lake
countries: Republic of the Congo
Democratic Republic of the Congo
coordinates: lat: -4.2819444444444
lon: 15.488611111111
surface_form: pool malebo
instance_of: Lake
countries: Republic of the Congo
Democratic Republic of the Congo
coordinates: lat: -4.2819444444444
lon: 15.488611111111
When a railway was constructed nearby, a plaque was installed at Palaba to commemorate the rail line connecting Matadi to Stanley Pool. Description. The Pool Malebo is about long, wide and in surface area. Its central part is occupied by M'Bamou or Bamu Island (), which is Republic of the Congo territory. The pool is shallow with depths of 3&ndash;10 m.

Geographic entities mentioned:
surface_form: malebo
instance_of: Lake
countries: Republic of the Congo
Democratic Republic of the Congo
coordinates: lat: -4.2819444444444
lon: 15.488611111111
surface_form: pool malebo
instance_of: Lake
countries: Republic of the Congo
Democratic Republic of the Congo
coordinates: lat: -4.2819444444444
lon: 15.488611111111
The altitude here is an average of. Geography. The capitals of the Republic of the Congo and the Democratic Republic of the Congo &mdash;Brazzaville and Kinshasa, respectively&mdash; are located on opposite shores of the southern part of Pool Malebo. These two capital cities are the closest geographically of any in the world (other than the contiguous Rome, Italy and Vatican City).

Geographic entities mentioned:
surface_form: malebo
instance_of: Lake
countries: Republic of the Congo
Democratic Republic of the Congo
coordinates: lat: -4.2819444444444
lon: 15.488611111111
surface_form: pool malebo
instance_of: Lake
countries: Republic of the Congo
Democratic Republic of the Congo
coordinates: lat: -4.2819444444444
lon: 15.488611111111
History. In the late 19th century, British colonists named this natural feature Stanley Pool, after British explorer and journalist Henry Morton Stanley, who had mapped and reported on this region. When a railway was constructed nearby, a plaque was installed at Palaba to commemorate the rail line connecting Matadi to Stanley Pool. Description.

Geographic entities mentioned:
surface_form: stanley pool
instance_of: Lake
countries: Republic of the Congo
Democratic Republic of the Congo
coordinates: lat: -4.2819444444444
lon: 15.488611111111
Monte Rasu. Monte Rasu is a mountain in the Goceano's range, in the province of Sassari, central west Sardinia, Italy. Its summit, called &quot;sa Punta Manna&quot; (1,259 m), is the highest peak in the province of Sassari.

Geographic entities mentioned:
surface_form: monte rasu
instance_of: Mountain
countries: Italy
coordinates: lat: 40.422186111111
lon: 9.0066444444444
Horní Planá is situated in the Bohemian Forest on the southeastern rim of the Šumava National Park, in the Šumava Protected Landscape Area. The highest point of Horní Planá and of the entire Český Krumlov District is a point on the top of the mountain Smrčina with an altitude of. Horní Planá is located on the northern shore of the Lipno Reservoir, south of the Boletice Military Training Area.

Geographic entities mentioned:
surface_form: Smrčina
instance_of: Mountain
countries: Czech Republic
Austria
coordinates: lat: 48.736388888889
lon: 13.921111111111
The highest peak in the range is an unnamed summit with an elevation of. Tumacacori Highlands. A Santa Cruz county-border &quot;bootheel&quot; extends southwest; the bootheel contains &quot;Cobre Ridge&quot;, and it is connected northwest to a small range, the San Luis Mountains which are in the southeast of the Altar Valley, and borders the Buenos Aires National Wildlife Refuge.

Geographic entities mentioned:
surface_form: Altar Valley
instance_of: Valley
countries: United States
coordinates: lat: 31.82
lon: -111.4
River Muick. River Muick () is a river of the Grampian Mountains of Aberdeenshire, Scotland. A tributary of the River Dee, it flows for about from the southeastern hill area around Lochnagar into Loch Muick on Balmoral Estate. It has a catchment area of.

Geographic entities mentioned:
surface_form: Lochnagar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.959930555556
lon: -3.2447805555556
surface_form: Loch Muick
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.93333333333333
lon: -3.1666666666666665
Fairview Shores. Located on Lake Union in Seattle, Washington, Fairview Shores is a sustainable residential development comprising five contemporary residences. The project incorporates rooftop terraces, private elevators, and energy-efficient systems.

Geographic entities mentioned:
surface_form: Lake Union
instance_of: Lake
countries: United States
coordinates: lat: 47.6392
lon: -122.3337
Eğirdir marinka. The Eğirdir marinka (&quot;Schizothorax prophylax&quot;) is a species of cyprinid fish in the genus &quot;Schizothorax&quot;. It is endemic to Lake Eğirdir in Turkey.

Geographic entities mentioned:
surface_form: Lake Eğirdir
instance_of: Lake
countries: Turkey
coordinates: lat: 37.9936
lon: 30.8884
Morgan also attempted to damage Vanderbilt's investments and his business positions before they agreed to a truce in 1858. In the late 1850s, a lucrative business developed out of a segment of railroad running between New Orleans and Berwick Bay, Louisiana.

Geographic entities mentioned:
surface_form: Berwick Bay, Louisiana
instance_of: Landform
countries: United States
coordinates: lat: 29.7013
lon: -91.2172
High Knob (New York). High Knob is a mountain in Schoharie County, New York. It is located southwest of Livingstonville. Steenburg Mountain is located southeast and Scott Patent Hill is located east-northeast of High Knob.

Geographic entities mentioned:
surface_form: Steenburg Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.39453
lon: -74.27486
surface_form: Scott Patent Hill
instance_of: Mountain
countries: United States
coordinates: lat: 42.454444444444
lon: -74.2525
surface_form: high knob
instance_of: Mountain
countries: United States
coordinates: lat: 38.8833
lon: -78.1167
surface_form: high knob
instance_of: Mountain
countries: United States
coordinates: lat: 42.428333333333
lon: -74.312777777778
surface_form: high knob
instance_of: Mountain
countries: United States
coordinates: lat: 36.8926
lon: -82.6296
surface_form: high knob
instance_of: Mountain
countries: United States
coordinates: lat: 39.19916667
lon: -78.89916667
High Knob (New York). High Knob is a mountain in Schoharie County, New York. It is located southwest of Livingstonville. Steenburg Mountain is located southeast and Scott Patent Hill is located east-northeast of High Knob.

Geographic entities mentioned:
surface_form: high knob
instance_of: Mountain
countries: United States
coordinates: lat: 38.8833
lon: -78.1167
surface_form: high knob
instance_of: Mountain
countries: United States
coordinates: lat: 42.428333333333
lon: -74.312777777778
surface_form: high knob
instance_of: Mountain
countries: United States
coordinates: lat: 36.8926
lon: -82.6296
surface_form: high knob
instance_of: Mountain
countries: United States
coordinates: lat: 39.19916667
lon: -78.89916667
High Knob (New York). High Knob is a mountain in Schoharie County, New York. It is located southwest of Livingstonville. Steenburg Mountain is located southeast and Scott Patent Hill is located east-northeast of High Knob.

Geographic entities mentioned:
surface_form: high knob
instance_of: Mountain
countries: United States
coordinates: lat: 38.8833
lon: -78.1167
surface_form: high knob
instance_of: Mountain
countries: United States
coordinates: lat: 42.428333333333
lon: -74.312777777778
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: high knob
instance_of: Mountain
countries: United States
coordinates: lat: 36.8926
lon: -82.6296
surface_form: high knob
instance_of: Mountain
countries: United States
coordinates: lat: 39.19916667
lon: -78.89916667
Ceredigion, the northernmost part of Dyfed, has a narrow coastal strip and the Cambrian Mountains cover much of the east of the county. The highest point is Plynlimon at, on the slopes of which five rivers have their sources: the Severn, the Wye, the Dulas, the Llyfnant and the Rheidol, the first two of which flow eastwards into England and the last three of which flow westwards to the Irish Sea.

Geographic entities mentioned:
surface_form: Plynlimon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.4675
lon: -3.7828
Description. Navajo Church is part of the Zuñi Mountains. The landmark is located east-northeast of Gallup and north of the town of Church Rock, which is named after the landform. Topographic relief is modest as the summit rises above Red Rock State Park in 0.6 mile (1 km). A 2.2 mile (round-trip) hiking trail leads to, and around, the base of the spires.

Geographic entities mentioned:
surface_form: park
instance_of: Mountain
coordinates: lat: -67.2333
lon: 51
The spires rest atop a pedestal of the formation's Recapture Member. This then overlays Zuni Sandstone which displays spectacular eolian crossbedding on the south face. Successive layers below dropping south to Red Rock Park include Bluff Sandstone, Summerville Formation, and Entrada Sandstone. Climate.

Geographic entities mentioned:
surface_form: park
instance_of: Mountain
coordinates: lat: -67.2333
lon: 51
The landmark is located east-northeast of Gallup and north of the town of Church Rock, which is named after the landform. Topographic relief is modest as the summit rises above Red Rock State Park in 0.6 mile (1 km). A 2.2 mile (round-trip) hiking trail leads to, and around, the base of the spires. Precipitation runoff from the mountain drains to the Puerco River.

Geographic entities mentioned:
surface_form: trail
instance_of: Mountain
coordinates: lat: -67.2
lon: 50.85
Navajo Church. Navajo Church is a pillar in McKinley County, New Mexico, United States. Description. Navajo Church is part of the Zuñi Mountains. The landmark is located east-northeast of Gallup and north of the town of Church Rock, which is named after the landform. Topographic relief is modest as the summit rises above Red Rock State Park in 0.6 mile (1 km).

Geographic entities mentioned:
surface_form: navajo church
instance_of: Mountain
coordinates: lat: 35.557522
lon: -108.6014696
A 2.2 mile (round-trip) hiking trail leads to, and around, the base of the spires. Precipitation runoff from the mountain drains to the Puerco River. Navajo Church is a sacred place to the Navajo people. This landform's toponym has been officially adopted by the United States Board on Geographic Names. Geology.

Geographic entities mentioned:
surface_form: navajo church
instance_of: Mountain
coordinates: lat: 35.557522
lon: -108.6014696
Navajo Church is a sacred place to the Navajo people. This landform's toponym has been officially adopted by the United States Board on Geographic Names. Geology. The three spires of Navajo Church are composed of the Westwater Canyon Member of the Morrison Formation which dates to the Late Jurassic. The spires rest atop a pedestal of the formation's Recapture Member.

Geographic entities mentioned:
surface_form: navajo church
instance_of: Mountain
coordinates: lat: 35.557522
lon: -108.6014696
Successive layers below dropping south to Red Rock Park include Bluff Sandstone, Summerville Formation, and Entrada Sandstone. Climate. According to the Köppen climate classification system, Navajo Church is located in a cool semiarid climate zone (Köppen &quot;BSk&quot;). The summers are hot during the day, but the high altitude and low humidity mean that nights remain distinctly cool.

Geographic entities mentioned:
surface_form: navajo church
instance_of: Mountain
coordinates: lat: 35.557522
lon: -108.6014696
Öschbrig. Öschbrig (also known as Oetlisberg) with an elevation of, is a wooded mountain in Switzerland overlooking to the east Zürichsee (Lake Zürich). Geography. Öschbrig is a wooded mountain located to the east of the city of Zürich, between the Glatt river valley and Lake Zürich. Its highest point is about above the Lake Zürich.

Geographic entities mentioned:
surface_form: Glatt river valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 47.416666666667
lon: 8.5666666666667
surface_form: lake zürich
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2475
lon: 8.6775
surface_form: öschbrig
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.35833333
lon: 8.61388889
Its highest point is about above the Lake Zürich. The mountain is part of a chain of hills — among them Käferberg, Adlisberg and Pfannenstiel — between Greifensee (Lake Greifen) and Lake Zürich. On the western flanks of the Öschbrig is located part of the Zürich quarter of Witikon.

Geographic entities mentioned:
surface_form: Käferberg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.405330555556
lon: 8.5202111111111
surface_form: Adlisberg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.370555555555555
lon: 8.591944444444444
surface_form: lake zürich
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2475
lon: 8.6775
surface_form: pfannenstiel
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.2922
lon: 8.67083
surface_form: lake greifen
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.35
lon: 8.6833333333333
surface_form: greifensee
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.35
lon: 8.6833333333333
Öschbrig. Öschbrig (also known as Oetlisberg) with an elevation of, is a wooded mountain in Switzerland overlooking to the east Zürichsee (Lake Zürich). Geography. Öschbrig is a wooded mountain located to the east of the city of Zürich, between the Glatt river valley and Lake Zürich. Its highest point is about above the Lake Zürich.

Geographic entities mentioned:
surface_form: zürichsee
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2475
lon: 8.6775
surface_form: lake zürich
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2475
lon: 8.6775
surface_form: öschbrig
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.35833333
lon: 8.61388889
surface_form: oetlisberg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.35833333
lon: 8.61388889
Geography. Öschbrig is a wooded mountain located to the east of the city of Zürich, between the Glatt river valley and Lake Zürich. Its highest point is about above the Lake Zürich. The mountain is part of a chain of hills — among them Käferberg, Adlisberg and Pfannenstiel — between Greifensee (Lake Greifen) and Lake Zürich.

Geographic entities mentioned:
surface_form: lake zürich
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2475
lon: 8.6775
On the western flanks of the Öschbrig is located part of the Zürich quarter of Witikon. On the slope between the north side of the mountain and the southeast side of the Adlisberg is situated the hamlet of &quot;Pfaffhausen&quot;, belonging to the &quot;gemeinde&quot; of Fällanden. Origin of the name.

Geographic entities mentioned:
surface_form: adlisberg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.370555555555555
lon: 8.591944444444444
Öschbrig. Öschbrig (also known as Oetlisberg) with an elevation of, is a wooded mountain in Switzerland overlooking to the east Zürichsee (Lake Zürich). Geography. Öschbrig is a wooded mountain located to the east of the city of Zürich, between the Glatt river valley and Lake Zürich. Its highest point is about above the Lake Zürich.

Geographic entities mentioned:
surface_form: öschbrig
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.35833333
lon: 8.61388889
Its highest point is about above the Lake Zürich. The mountain is part of a chain of hills — among them Käferberg, Adlisberg and Pfannenstiel — between Greifensee (Lake Greifen) and Lake Zürich. On the western flanks of the Öschbrig is located part of the Zürich quarter of Witikon.

Geographic entities mentioned:
surface_form: öschbrig
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.35833333
lon: 8.61388889
Origin of the name. Öschbrig is the Swiss German form of &quot;Oetlisberg&quot;, which is the name given to the forest lying on the mountain. &quot;Oetli&quot; could be a family name or could derive from the alemannic male names &quot;Otmar&quot; or &quot;Otfrid&quot;. The name Öschbrig is first attested in 1492. Nature.

Geographic entities mentioned:
surface_form: oetlisberg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.35833333
lon: 8.61388889
It acquired its name from the McGowan or McGown family who kept a tavern near there from 1756 through the Revolutionary period, and owned the surrounding property until the 1840s. The area was incorporated into Central Park after 1860, when the park's boundaries were extended north from the line of 106th Street to 110th Street, and the Harlem Meer was built in the park's northeast corner.

Geographic entities mentioned:
surface_form: Harlem Meer
instance_of: Lake
countries: United States
coordinates: lat: 40.7966
lon: -73.9517
Vincent's. When Central Park was being built, a lake called Harlem Meer was constructed from a natural waterway north of McGowan's Pass. A new section of East Drive was made to veer sharply to the west and south and again to the north, bypassing the Meer. Tavern. A refreshment house, known as Mount St. Vincent's Hotel, opened at McGowan's Pass in 1883–1884. Its proprietor until 1890 was Patrick H.

Geographic entities mentioned:
surface_form: Harlem Meer
instance_of: Lake
countries: United States
coordinates: lat: 40.7966
lon: -73.9517
Duplje. Duplje () is a settlement in the Vipava Valley in the Municipality of Vipava in the Littoral region of Slovenia.

Geographic entities mentioned:
surface_form: Vipava Valley
instance_of: Valley
countries: Slovenia
coordinates: lat: 45.876147222222
lon: 13.907319444444
Much of the northern half of Wood Mountain Hills is in the Wood River watershed while the southern half flows south into the United States and the drainage basin of the Milk River — a tributary of the Missouri River. This part of the drainage divide is known as the Missouri Coteau.

Geographic entities mentioned:
surface_form: Missouri Coteau
instance_of: Plateau
countries: Canada
United States
coordinates: lat: 50.8
lon: -109.2
Near the small community of Summercove, the river turns north-east and begins to head out of the hills where it is joined by several tributaries. Along the route, south of Gravelbourg, a dam was built that created Thomson Lake. On the eastern shore of the lake is Thomson Lake Regional Park, the oldest regional park in Saskatchewan.

Geographic entities mentioned:
surface_form: Thomson Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.75003
lon: -106.60061
After Gravelbourg, the river continues north-east, passes by Shamrock Regional Park, and flows into the western end of Old Wives Lake. Old Wives Lake is part of an Important Bird Area (IBA) of Canada and, along with Reed and Chaplin Lakes, were designated part of the Western Hemisphere Shorebird Reserve Network (WHSRN). Lakes and reservoirs.

Geographic entities mentioned:
surface_form: Reed
instance_of: Lake
countries: Canada
coordinates: lat: 50.40003
lon: -107.08397
surface_form: Chaplin Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.4016
lon: -106.6004
Eason's Grove site. Eason's Grove () was an unofficial recreation site that had no level of formal government organisation. From about 1907, local residents began using the area as a picnic spot and gathering site due to the natural grassy field, groves of trees, and access to Woody River. Eventually ball diamonds were constructed on the south side of the property and pick-up games were played.

Geographic entities mentioned:
surface_form: woody river
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.1583
lon: -101.60919
Wood River (Saskatchewan). Wood River is a river in the Canadian province of Saskatchewan. It has its source in the Wood Mountain Hills of south-western Saskatchewan and flows in a north-easterly direction to its mouth at Old Wives Lake. Old Wives Lake is a salt water lake with no outflow. As a result, the drainage basin of Wood River is an endorheic one.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The song is considered by many to be the quintessential Saskatchewan song. Course and description. Wood River begins in south-western Saskatchewan at the height of the Wood Mountain Hills in semi-arid grasslands within a large region called Palliser's Triangle.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: wood river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.13336
lon: -106.21789
Wood River begins in south-western Saskatchewan at the height of the Wood Mountain Hills in semi-arid grasslands within a large region called Palliser's Triangle. Much of the northern half of Wood Mountain Hills is in the Wood River watershed while the southern half flows south into the United States and the drainage basin of the Milk River — a tributary of the Missouri River.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: wood river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.13336
lon: -106.21789
Along the route, south of Gravelbourg, a dam was built that created Thomson Lake. On the eastern shore of the lake is Thomson Lake Regional Park, the oldest regional park in Saskatchewan. Gravelbourg, the largest town along the river's course, is about downstream from the dam.

Geographic entities mentioned:
surface_form: thomson lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.75003
lon: -106.60061
Wood River (Saskatchewan). Wood River is a river in the Canadian province of Saskatchewan. It has its source in the Wood Mountain Hills of south-western Saskatchewan and flows in a north-easterly direction to its mouth at Old Wives Lake. Old Wives Lake is a salt water lake with no outflow. As a result, the drainage basin of Wood River is an endorheic one.

Geographic entities mentioned:
surface_form: wood river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.13336
lon: -106.21789
It has its source in the Wood Mountain Hills of south-western Saskatchewan and flows in a north-easterly direction to its mouth at Old Wives Lake. Old Wives Lake is a salt water lake with no outflow. As a result, the drainage basin of Wood River is an endorheic one. Along the course of the river, there are several parks, historical sites, and small towns.

Geographic entities mentioned:
surface_form: wood river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.13336
lon: -106.21789
As a result, the drainage basin of Wood River is an endorheic one. Along the course of the river, there are several parks, historical sites, and small towns. Wood River was the inspiration for the famous Canadian folk song by the same name written by Connie Kaldor and sung nationwide by Canadian choirs. The song is considered by many to be the quintessential Saskatchewan song.

Geographic entities mentioned:
surface_form: wood river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.13336
lon: -106.21789
This part of the drainage divide is known as the Missouri Coteau. Beginning at Pinto Butte at over in elevation, Wood River flows eastward through grasslands, rolling hills, and valleys that were carved by glacial meltwaters. Near the small community of Summercove, the river turns north-east and begins to head out of the hills where it is joined by several tributaries.

Geographic entities mentioned:
surface_form: wood river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.13336
lon: -106.21789
Lakes and reservoirs. There are several notable lakes and reservoirs within the Wood River watershed. Due to the semi-arid conditions in the region of Palliser's Triangle, several reservoirs were built to retain water for irrigation and consumption. Shamrock Regional Park. Shamrock Regional Park () is a regional park in the RM of Shamrock No. 134 along the course of Wood River.

Geographic entities mentioned:
surface_form: wood river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.13336
lon: -106.21789
Due to the semi-arid conditions in the region of Palliser's Triangle, several reservoirs were built to retain water for irrigation and consumption. Shamrock Regional Park. Shamrock Regional Park () is a regional park in the RM of Shamrock No. 134 along the course of Wood River. Founded in 1961, it is one of the oldest regional parks in Saskatchewan.

Geographic entities mentioned:
surface_form: wood river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.13336
lon: -106.21789
Historical sites. Along the course of the river, there are three Saskatchewan historical sites on the Canadian Register of Historic Places. A fourth site, Eason's Grove, is located on a small bluff north of Gravelbourg in the Wood River Valley that overlooks Wood River. All four sites are within the RM of Gravelbourg No. 104. Cripple Creek Crossing site.

Geographic entities mentioned:
surface_form: wood river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.13336
lon: -106.21789
surface_form: wood river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.13336
lon: -106.21789
All four sites are within the RM of Gravelbourg No. 104. Cripple Creek Crossing site. Cripple Creek Crossing (), located at the point where Cripple Creek meets Wood River just south of Old Wives Lake, is the site of a North-West Mounted Police camp during their March West in 1874. By mid-August, the rigours of the difficult trek west left some men in poor health.

Geographic entities mentioned:
surface_form: wood river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.13336
lon: -106.21789
Today, the historical site consists of of fields and pasture land. Trapper's Cabin site. Trapper's Cabin (), located near Gravelbourg, is the only surviving trapper's cabin in the area from the fur trade. The 32-hectare site has the remains of a small dugout shelter on the banks of Wood River that was built in the 1930s by Norman Poulin, a local Métis farmer and trapper.

Geographic entities mentioned:
surface_form: wood river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.13336
lon: -106.21789
Photographed from the air by the U.S. Navy, 1967, and surveyed by British Antarctic Survey (BAS), 1968–71. In association with the names of geologists grouped in this area, named by the United Kingdom Antarctic Place-Names Committee (UK-APC) after Sir Arthur E.

Geographic entities mentioned:
surface_form: arthur
instance_of: Mountain
coordinates: lat: -67.65
lon: 49.86667
Trueman Terraces. Trueman Terraces () are ice-free terraces rising to 1,520 m on the east side of Goldschmidt Cirque, near the east end of Read Mountains, Shackleton Range. Photographed from the air by the U.S. Navy, 1967, and surveyed by British Antarctic Survey (BAS), 1968–71.

Geographic entities mentioned:
surface_form: trueman terraces
instance_of: Landform
coordinates: lat: -80.7167
lon: -22.6833
Trueman Terraces. Trueman Terraces () are ice-free terraces rising to 1,520 m on the east side of Goldschmidt Cirque, near the east end of Read Mountains, Shackleton Range. Photographed from the air by the U.S. Navy, 1967, and surveyed by British Antarctic Survey (BAS), 1968–71.

Geographic entities mentioned:
surface_form: trueman terraces
instance_of: Landform
coordinates: lat: -80.7167
lon: -22.6833
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
Trueman (1895–1956), British geologist, who worked on the coal measures and their correlation by marine bands, and on the introduction of statistical methods into paleontology; Professor of Geology, Glasgow University, 1937–46; President, Geological Society of London, 1945–47.

Geographic entities mentioned:
surface_form: coal
instance_of: Mountain
coordinates: lat: -72.1167
lon: -68.5333
Background. Han Xizai was born in 902, late in the Tang dynasty. He was said to be from Beihai (北海, in modern Weifang, Shandong) (and, based on subsequent events, appeared to have been born there). In his youth, he lived as a hermit on Mount Song.

Geographic entities mentioned:
surface_form: Mount Song
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 34.484722222222
lon: 112.96027777778
The St. Croix River (; Maliseet-Passamaquoddy: &quot;Skutik&quot;) is a river in northeastern North America, in length, that forms part of the Canada–United States border between Maine (U.S.) and New Brunswick (Canada). The river rises in the Chiputneticook Lakes and flows south and southeast, between Calais and St. Stephen. It discharges into Passamaquoddy Bay, in the Bay of Fundy. Geography.

Geographic entities mentioned:
surface_form: Chiputneticook Lakes
instance_of: Group of lakes
countries: Canada
United States
coordinates: lat: 45.666666666667
lon: -67.75
surface_form: chiputneticook lakes
instance_of: Group of lakes
countries: Canada
United States
coordinates: lat: 45.666666666667
lon: -67.75
The river rises in the Chiputneticook Lakes and flows south and southeast, between Calais and St. Stephen. It discharges into Passamaquoddy Bay, in the Bay of Fundy. Geography. The river forms from the Chiputneticook Lakes (North Lake, East Grand Lake, Mud Lake, and Spednic Lake) along the Canadian–U.S. border. U.S. Geological Survey topographic maps show the St.

Geographic entities mentioned:
surface_form: Spednic Lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 45.6051
lon: -67.6278
surface_form: chiputneticook lakes
instance_of: Group of lakes
countries: Canada
United States
coordinates: lat: 45.666666666667
lon: -67.75
surface_form: spednic lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 45.6051
lon: -67.6278
The river rises in the Chiputneticook Lakes and flows south and southeast, between Calais and St. Stephen. It discharges into Passamaquoddy Bay, in the Bay of Fundy. Geography. The river forms from the Chiputneticook Lakes (North Lake, East Grand Lake, Mud Lake, and Spednic Lake) along the Canadian–U.S. border. U.S. Geological Survey topographic maps show the St.

Geographic entities mentioned:
surface_form: spednic lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 45.6051
lon: -67.6278
surface_form: st. croix river
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.8231
lon: -67.7558
With or without a permit, lumbermen were in a race to cut the best timber from the land while it was under dispute. Although it was illegal to cut trees with no permit, the Saint John River enabled this activity because it increased business at the local mills, shipyards and timber ponds in New Brunswick so the officials were slow to halt the ongoing illegal activity.

Geographic entities mentioned:
surface_form: saint john river
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.266667
lon: -66.066667
The geography of the river was not charted clearly until the Jay Treaty (1794) provided provisions for surveying the boundary. The boundary between Maine and New Brunswick north of the headwaters of the Saint Croix took another four decades to establish. Following the War of 1812 there was a push to settle this disputed territory north of the St. Croix on the St.

Geographic entities mentioned:
surface_form: st. john
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.266667
lon: -66.066667
St. Croix River (Maine–New Brunswick). The St. Croix River (; Maliseet-Passamaquoddy: &quot;Skutik&quot;) is a river in northeastern North America, in length, that forms part of the Canada–United States border between Maine (U.S.) and New Brunswick (Canada). The river rises in the Chiputneticook Lakes and flows south and southeast, between Calais and St. Stephen.

Geographic entities mentioned:
surface_form: st. croix river (maine–new brunswick)
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.8231
lon: -67.7558