Sarmila/GeoWiki-Features huggingface dataset:
The origins and early development of fixed male-only zones (&quot;nyonin kinsei&quot;; &quot;nyonin kekkai&quot;) remain a subject of debate, owing to a disjuncture between religious narratives, historical and material records, and present-day practices. Extant textual records indicate that communities of celibate male Buddhist practitioners at places like Mt. Hiei and Mt.

Geographic entities mentioned:
surface_form: hiei
instance_of: Mountain
countries: Japan
coordinates: lat: 35.066666666667
lon: 135.83833333333
Mount Ōmine. , is a sacred mountain in Nara, Japan, famous for its three tests of courage. Officially known as, it is more popularly known as Mount Ōmine due to its prominence in the Ōmine mountain range. It is located in Yoshino-Kumano National Park in the Kansai region, Honshū, Japan.

Geographic entities mentioned:
surface_form: mount ōmine
instance_of: Mountain
countries: Japan
coordinates: lat: 34.252777777778
lon: 135.94055555556
surface_form: ōmine
instance_of: Mountain
countries: Japan
coordinates: lat: 34.252777777778
lon: 135.94055555556
Mount Ōmine. , is a sacred mountain in Nara, Japan, famous for its three tests of courage. Officially known as, it is more popularly known as Mount Ōmine due to its prominence in the Ōmine mountain range. It is located in Yoshino-Kumano National Park in the Kansai region, Honshū, Japan.

Geographic entities mentioned:
surface_form: mount ōmine
instance_of: Mountain
countries: Japan
coordinates: lat: 34.252777777778
lon: 135.94055555556
surface_form: ōmine
instance_of: Mountain
countries: Japan
coordinates: lat: 34.252777777778
lon: 135.94055555556
surface_form: ōmine
instance_of: Mountain
countries: Japan
coordinates: lat: 34.252777777778
lon: 135.94055555556
History. The monastery at Mount Ōmine was founded in the 8th century by En no Gyōja, as a home for his new religion of Shugendō. Shugendo literally means &quot;the path of training and testing,&quot; and is based on the self-actualization of spiritual power in experiential form through challenging and rigorous ritualistic tests of courage and devotion known as &quot;shugyō&quot;.

Geographic entities mentioned:
surface_form: mount ōmine
instance_of: Mountain
countries: Japan
coordinates: lat: 34.252777777778
lon: 135.94055555556
surface_form: ōmine
instance_of: Mountain
countries: Japan
coordinates: lat: 34.252777777778
lon: 135.94055555556
During this time the mountain was closed, and any Shugendo practices were carried on in secret. However, in 1945 the Japanese Culture Act repealed these edicts, and the mountain was opened again. Shugendō practicers were quick to reclaim the mountain and restore the traditions. In 1964, Mountaineer/author Kyūya Fukada selected Mount Ōmine as number 91 of his 100 famous mountains in Japan.

Geographic entities mentioned:
surface_form: mount ōmine
instance_of: Mountain
countries: Japan
coordinates: lat: 34.252777777778
lon: 135.94055555556
surface_form: ōmine
instance_of: Mountain
countries: Japan
coordinates: lat: 34.252777777778
lon: 135.94055555556
Most territorial proscriptions dissolved in 1872 when the Meiji government granted women full access to mountain shrine and temple lands, but traces of gender-exclusive practices can be found at many mountains in Japan, especially those like Mount Ōmine which powerful Buddhist temples controlled.

Geographic entities mentioned:
surface_form: mount ōmine
instance_of: Mountain
countries: Japan
coordinates: lat: 34.252777777778
lon: 135.94055555556
surface_form: ōmine
instance_of: Mountain
countries: Japan
coordinates: lat: 34.252777777778
lon: 135.94055555556
Scholars debate the precise pathways through which temporary avoidances gave way to permanent bans, but they share a broad consensus that the phenomenon of women's exclusion derives at least in part—and in no small part—from Buddhist- and kami-related views of women's physiology as innately polluted.

Geographic entities mentioned:
surface_form: kami
instance_of: Mountain
countries: Japan
coordinates: lat: 35.233333333333334
lon: 139.02055555555555
Results. Despite being out-fundraised by Kulkarni, Olson won re-election in the district's closest race since he was first elected in 2008. District 23. The 23rd district stretches from rural Southwestern Texas, including Alpine, Del Rio, and Socorro, into the Greater San Antonio area, taking in Hondo and the outer areas of San Antonio. It is a prominently Hispanic-majority district.

Geographic entities mentioned:
surface_form: Southwestern Texas
instance_of: Valley
countries: United States
coordinates: lat: 30.56
lon: -103.79
2021 ICF Canoe Sprint World Championships – Men's VL1. The men's VL1 competition at the 2021 ICF Canoe Sprint World Championships in Copenhagen took place on Lake Bagsværd. Schedule. All times are Central European Summer Time (UTC+2)
Results. With fewer than ten competitors entered, this event was held as a direct final.

Geographic entities mentioned:
surface_form: Lake Bagsværd
instance_of: Lake
countries: Denmark
coordinates: lat: 55.772222222222
lon: 12.458333333333
It came into being with the creation of Nunavut on April 1, 1999. Geography. The four corners area is located between Kasba Lake to the north and Hasbala Lake to the south. It is located by an area of marginal taiga forest, which happens to be the only place in Nunavut which is not Arctic tundra or ice cap.

Geographic entities mentioned:
surface_form: Kasba Lake
instance_of: Lake
countries: Canada
coordinates: lat: 60.283333333333
lon: -102.00611111111
Kluskus Lakes. The Kluskus Lakes are a group of lakes on the northern perimeter of the Chilcotin District of the Central Interior of British Columbia, Canada. They are located east of Tsacha Lake and south of the Euchiniko Lakes and are part of the drainage of the West Road River (aka Blackwater River).

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: kluskus lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 53.0833
lon: -124.5
Kluskus Lakes. The Kluskus Lakes are a group of lakes on the northern perimeter of the Chilcotin District of the Central Interior of British Columbia, Canada. They are located east of Tsacha Lake and south of the Euchiniko Lakes and are part of the drainage of the West Road River (aka Blackwater River).

Geographic entities mentioned:
surface_form: kluskus lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 53.0833
lon: -124.5
Fort Kluskus was located in the vicinity, which today includes numerous Indian Reserves of the eponymous Kluskus First Nation. The Kluskus Hills are also located between the Kluskus Lakes and the Euchiniko Lakes. &quot;Kluskus&quot; is the English rendering of the Carrier language word lhoosk'uz, meaning &quot;the side of the fish is white&quot;.

Geographic entities mentioned:
surface_form: kluskus lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 53.0833
lon: -124.5
Grassberry Creek flows into the southern end of Limestone Lake. Limestone Lake Recreation Site. Limestone Lake Recreation Site () is a provincial recreation site at the northern end of Limestone Lake. There is free camping, a boat launch, and boat rentals. The site is associated with Northern Lights Lodge, which leases the nearby Deschambault Lake (South East Arm) Recreation Site. Fish species.

Geographic entities mentioned:
surface_form: deschambault lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.754756
lon: -103.515297
Limestone Lake (Saskatchewan). Limestone Lake is a lake in the Canadian province of Saskatchewan. It is in the Northern Saskatchewan Administration District and access is from Highway 106. The lake is at the northern limit of the Mid-boreal Lowland ecoregion within the Saskatchewan River watershed.

Geographic entities mentioned:
surface_form: limestone lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.6334
lon: -103.21708
surface_form: limestone lake
instance_of: Lake
countries: Canada
coordinates: lat: 56.5825
lon: -95.916666666667
surface_form: limestone lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.6833
lon: -125.617
It is in the Northern Saskatchewan Administration District and access is from Highway 106. The lake is at the northern limit of the Mid-boreal Lowland ecoregion within the Saskatchewan River watershed. Limestone Lake is along the course of Grassberry River, which flows south into Saskatchewan River Delta. Grassberry Creek flows into the southern end of Limestone Lake.

Geographic entities mentioned:
surface_form: limestone lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.6334
lon: -103.21708
surface_form: limestone lake
instance_of: Lake
countries: Canada
coordinates: lat: 56.5825
lon: -95.916666666667
surface_form: limestone lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.6833
lon: -125.617
The lake is at the northern limit of the Mid-boreal Lowland ecoregion within the Saskatchewan River watershed. Limestone Lake is along the course of Grassberry River, which flows south into Saskatchewan River Delta. Grassberry Creek flows into the southern end of Limestone Lake. Limestone Lake Recreation Site.

Geographic entities mentioned:
surface_form: limestone lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.6334
lon: -103.21708
surface_form: limestone lake
instance_of: Lake
countries: Canada
coordinates: lat: 56.5825
lon: -95.916666666667
surface_form: limestone lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.6833
lon: -125.617
Limestone Lake is along the course of Grassberry River, which flows south into Saskatchewan River Delta. Grassberry Creek flows into the southern end of Limestone Lake. Limestone Lake Recreation Site. Limestone Lake Recreation Site () is a provincial recreation site at the northern end of Limestone Lake. There is free camping, a boat launch, and boat rentals.

Geographic entities mentioned:
surface_form: limestone lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.6334
lon: -103.21708
surface_form: limestone lake
instance_of: Lake
countries: Canada
coordinates: lat: 56.5825
lon: -95.916666666667
surface_form: limestone lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.6833
lon: -125.617
Grassberry Creek flows into the southern end of Limestone Lake. Limestone Lake Recreation Site. Limestone Lake Recreation Site () is a provincial recreation site at the northern end of Limestone Lake. There is free camping, a boat launch, and boat rentals. The site is associated with Northern Lights Lodge, which leases the nearby Deschambault Lake (South East Arm) Recreation Site. Fish species.

Geographic entities mentioned:
surface_form: limestone lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.6334
lon: -103.21708
surface_form: limestone lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.6334
lon: -103.21708
surface_form: limestone lake
instance_of: Lake
countries: Canada
coordinates: lat: 56.5825
lon: -95.916666666667
surface_form: limestone lake
instance_of: Lake
countries: Canada
coordinates: lat: 56.5825
lon: -95.916666666667
surface_form: limestone lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.6833
lon: -125.617
surface_form: limestone lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.6833
lon: -125.617
There is free camping, a boat launch, and boat rentals. The site is associated with Northern Lights Lodge, which leases the nearby Deschambault Lake (South East Arm) Recreation Site. Fish species. Fish commonly found in Limestone Lake include burbot, cisco, lake whitefish, northern pike, walleye, white sucker, and yellow perch.

Geographic entities mentioned:
surface_form: limestone lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.6334
lon: -103.21708
surface_form: limestone lake
instance_of: Lake
countries: Canada
coordinates: lat: 56.5825
lon: -95.916666666667
surface_form: limestone lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.6833
lon: -125.617
Isolated columns 5–5 meters in height stand adjacent to the coast between the north and south parts of the quarry; just to the north the sea wall exposes cross-sections of the columns 1-2.5 metres in diameter, resulting in a &quot;Giants Causeway&quot; appearance.

Geographic entities mentioned:
surface_form: Giants Causeway
instance_of: Landform
countries: United Kingdom
coordinates: lat: 55.240833333333
lon: -6.5116666666667
Bowyer was also active in the search for extraterrestrial intelligence, or SETI. In 1977, Bowyer started SERENDIP (the Search for Extraterrestrial Radio Emissions From Nearby Developed Intelligent Populations) using an 85-foot telescope at Hat Creek Radio Observatory near Lassen Peak in Northern California.

Geographic entities mentioned:
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
The specific name honors the late French paleontologist Albert-Félix de Lapparent, due to his contributions to dinosaur-related discoveries in the Sahara. In the same paper, several skull and vertebral fossils from the Tademaït of Algeria were attributed to a new species of &quot;Spinosaurus&quot; called &quot;S. maroccanus,&quot; which was described and compared to &quot;Cristatusaurus&quot;.

Geographic entities mentioned:
surface_form: Tademaït
instance_of: Plateau
countries: Algeria
coordinates: lat: 28.5
lon: 2.25
The museum displays some Saxon artefacts, including the Wareham Sword which is currently on loan from the Dorset Museum in Dorchester. The remains of this late 10th century sword were discovered in the mud of the River Frome in 1927 by workers constructing the new South Bridge at Wareham.

Geographic entities mentioned:
surface_form: River Frome
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 50.6958
lon: -1.98861
The highway is about long. Route description. Hwy 220 begins within Rowan's Ravine Provincial Park at a parking lot, just metres away from the shoreline of Last Mountain Lake. It heads east to pass through the main park gate, thereby leaving the park and travelling along the north side of Uhl's Bay, where it shares a short concurrency (overlap) with Hwy 731.

Geographic entities mentioned:
surface_form: Last Mountain Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.1667
lon: -105.25
Geology. The underlying rocks of the Vogler stem from the Bunter sandstone geological period. Places of interest. On the Ebersnacken (460.4 m) stands the Ebersnacken Tower, an observation tower, from which there is a good all-round view over the Vogler. Other such towers are the Bodo Tower (412 m) and the Königszinne (255,0 m).

Geographic entities mentioned:
surface_form: Ebersnacken
instance_of: Mountain
countries: Germany
coordinates: lat: 51.9292
lon: 9.56572
The port was opened in October 1896. The Merchant Seaport Authority was founded in 1903. The port was substantially reconstructed between 2000 and 2003. Passenger ferry service to the port of Baku, Azerbaijan as well as rail ferries to other ports on the Caspian Sea (Baku, Aktau) began in 1962. In recent years tanker transport of oil to the ports of Baku and Makhachkala has increased.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
1963 USAC Championship Car season. The 1963 USAC Championship Car season consisted of 12 races, beginning in Trenton, New Jersey on April 21 and concluding in Phoenix, Arizona on November 17. There was also one non-championship event at Pikes Peak, Colorado. The USAC National Champion was A. J. Foyt, and the Indianapolis 500 winner was Parnelli Jones.

Geographic entities mentioned:
surface_form: Pikes Peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.840555555556
lon: -105.04416666667
Leininger Peak. 23rmhtl04y5aktazgf7mrc7kldu" xml:space="preserve">#redirect Leininger Peak

Geographic entities mentioned:
surface_form: leininger peak
instance_of: Mountain
coordinates: lat: -70.5667
lon: -62.25
In 1957 he discovered the first stegondontid fossils reported from Ola Bula in Flores, along with Lower Palaeolithic stone blades and flakes. In 1965 he found a similar concurrence of stone tools with remains of Stegodon-dominated megafauna at nearby Mata Menge.

Geographic entities mentioned:
surface_form: Mata Menge
instance_of: Lake
countries: Indonesia
coordinates: lat: -8.704
lon: 121.1061
Vilobí d'Onyar. Vilobí d'Onyar () is a municipality in the &quot;comarca&quot; of the Selva in Catalonia, Spain. It is situated in the valley of the Onyar river, on the GE-533 road between Santa Coloma de Farners and Riudellots de la Selva. A substantial part of the northern portion of the municipality is taken up by Girona-Costa Brava Airport.

Geographic entities mentioned:
surface_form: Onyar
instance_of: Watercourse
countries: Spain
coordinates: lat: 41.970555555556
lon: 2.8394444444444
Geomagnetic excursions in the Matuyama, Gauss and Gilbert chrons are also reported, and new possible excursions are suggested for these chrons based on analysis of the deep drilling cores from Lake Baikal and their comparison with the oceanic core (ODP) and Chinese loess records. Possible causes. Scientific opinion is divided on what causes geomagnetic excursions.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Location. The monastery is located at 5 km south-east from the former village of Dolni Lozen (today the eastern part of Lozen), near Sofia, deep in the bowers of the Lozen Mountain under the Polovrak peak (1182 m), on a natural terrace with views of the Sofia Valley. Origins. The monastery was founded in the 13th century.

Geographic entities mentioned:
surface_form: Lozen Mountain
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.561
lon: 23.597
City water supply improvement. In 1845 Wightman was the chairman of a citizens committee that worked to improve water delivery into the City of Boston, this resulted in the development of the Cochituate Water Works. Boston public schools. From 1846 to 1855 Wightman served as a member of the Boston Primary School Committee.

Geographic entities mentioned:
surface_form: Cochituate Water Works
instance_of: Lake
countries: United States
coordinates: lat: 42.305555555556
lon: -71.372222222222
Subspecies. The Rhaetian Alps poppy (&quot;P. alpinum&quot; subsp. &quot;rhaeticum&quot;) has light yellow to orange petals and feathery foliage, and is found in the Central and Southern Alps. In Austria, it is scattered around Carinthia, Styria and Salzburg; in Switzerland, it has only been found in the Engadin. The Salzburg Alpine poppy (&quot;P. alpinum&quot; subsp.

Geographic entities mentioned:
surface_form: Engadin
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.5497
lon: 9.8959
Rench. The Rench is an eastern tributary of the Rhine in the Ortenau in Central Baden, Germany. It rises on the southern edge of the Northern Black Forest at Kniebis near Bad Griesbach im Schwarzwald. The source farthest from the mouth is that of the &quot;Schöngrundbächle&quot; which rises at a height of around in the parish of Zuflucht.

Geographic entities mentioned:
surface_form: Kniebis
instance_of: Mountain
countries: Germany
coordinates: lat: 48.476388888889
lon: 8.2938888888889
The only state that has allowed oil and gas drilling beneath the Great Lakes in recent years has been Michigan, and that only by directional drilling from onshore surface locations. All oil and gas drilling, either on or directionally beneath the Great Lakes, has been banned by federal law since 2002. The Canadian side of Lake Erie has 480 producing gas wells in the lake.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
A gas well to the Medina Group was drilled in 1958 in Pennsylvania state waters in Lake Erie. The only state that has current oil and gas production from beneath the Great Lakes is Michigan. Michigan has 13 oil and gas wells that produce from below Lake Michigan, all drilled directionally from surface locations on shore. Directional drilling beneath the Great Lakes is now banned.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Directional drilling beneath the Great Lakes is now banned. The US Geological Survey has estimated that of recoverable petroleum liquids and of recoverable natural gas underlie the US portion of the Great Lakes. Petroleum potential was given to all of the lakes except Lake Superior. The majority of the natural gas (3.0 TCF) is thought to underlie Lake Erie. State restrictions.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
He worked with fellow architect Philo Jacobson. He designed four houses with his wife, Sandra Miles, in Westwood, the Pacific Palisades, Carmel Valley and Sand City. Lomax participated in the 1976 LA12 exhibition at the Pacific Design Center He was a member of the Monterey Bay chapter of the American Institute of Architects based in Sand City, California. Personal life. He married Sandra E.

Geographic entities mentioned:
surface_form: Carmel Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.4748315
lon: -121.7205075
Years passed. New practice runs then occurred in Munich, probably in June 1873, and Brahms ventured south of the city to the small lakeside town of Tutzing for a summer respite. There, with the Würmsee (as Lake Starnberg was then called) and the Bavarian Prealps as backdrop, he put the finishing touches on the two quartets. He was 40 years old at the time of publication.

Geographic entities mentioned:
surface_form: Lake Starnberg
instance_of: Lake
countries: Germany
coordinates: lat: 47.903888888889
lon: 11.307222222222
The Twizel River originates from numerous streams which flow down the eastern flanks of the Ben Ohau Range, the longest being Gladstone Stream and Duncan Stream. The Twizel River flows south, veering slowly southeast close to the town of Twizel, and empties into the northern end of the artificial lake, Lake Benmore.

Geographic entities mentioned:
surface_form: Lake Benmore
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.415
lon: 170.22055555556
Loreto, Switzerland. Loreto is a quarter of the city of Lugano, in the Swiss canton of Ticino. It forms the part of the city which surrounds the shrine of Our Lady of Loreto to the south of the city center, and includes the Lake Lugano waterfront south of the city centre but north of Paradiso. In 2011, it had a population of 3,221.

Geographic entities mentioned:
surface_form: Lake Lugano
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46
lon: 9
Causey Pike. Causey Pike is a fell in the English Lake District. It is situated in the Newlands Valley, south-west of the town of Keswick. Even though it has a modest height of it is one of the most distinctive fells when viewed from the Derwent Water and Keswick area due to its distinguishing summit &quot;knobble&quot; which catches the eye.

Geographic entities mentioned:
surface_form: Newlands Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.573011111111
lon: -3.1848694444444
The central sector, rising between Whinlatter Pass and Newlands Pass, includes Causey Pike. The highest ground in the North Western Fells is an east–west ridge in this central sector, beginning with Grasmoor above Crummock Water and then gradually descending eastwards over Crag Hill, Sail, Scar Crags and Causey Pike.

Geographic entities mentioned:
surface_form: Grasmoor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.57115
lon: -3.2791805555556
surface_form: Crummock Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.55
lon: -3.3
surface_form: Crag Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.572
lon: -3.25
surface_form: Scar Crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.574388888889
lon: -3.2266805555556
surface_form: crummock water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.55
lon: -3.3
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.2445
lon: -2.47413
surface_form: sail
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.571
lon: -3.242
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.572
lon: -3.25
surface_form: scar crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.574388888889
lon: -3.2266805555556
surface_form: causey pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.576338888889
lon: -3.2112694444444
surface_form: causey pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.576338888889
lon: -3.2112694444444
surface_form: grasmoor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.57115
lon: -3.2791805555556
The highest ground in the North Western Fells is an east–west ridge in this central sector, beginning with Grasmoor above Crummock Water and then gradually descending eastwards over Crag Hill, Sail, Scar Crags and Causey Pike. Causey Pike is separated from Barrow and Outerside to the north by Stonycroft Gill. Southward across Rigg Beck is Ard Crags.

Geographic entities mentioned:
surface_form: Outerside
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5816
lon: -3.22226
surface_form: outerside
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5816
lon: -3.22226
surface_form: barrow
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5858
lon: -3.19703
Causey Pike is separated from Barrow and Outerside to the north by Stonycroft Gill. Southward across Rigg Beck is Ard Crags. Causey Pike has a long blunt-ended shoulder running eastward to the Newlands Valley, dropping steeply from its terminus at Rowling End. Geology. The entire hill is formed from Ordovician-age rocks assigned to the Skiddaw Group.

Geographic entities mentioned:
surface_form: Ard Crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5663
lon: -3.22953
surface_form: ard crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5663
lon: -3.22953
An easier and longer alternative from the same starting point goes by an old track which used to serve the cobalt mine on the slopes of Scar Crags, this approaches the fell &quot;from the back&quot; reaching Sail Pass and then crossing the summit of Scar Crags before attaining Causey Pike.

Geographic entities mentioned:
surface_form: Scar Crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.574388888889
lon: -3.2266805555556
surface_form: sail
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.571
lon: -3.242
surface_form: scar crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.574388888889
lon: -3.2266805555556
surface_form: scar crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.574388888889
lon: -3.2266805555556
surface_form: causey pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.576338888889
lon: -3.2112694444444
The fell is also part of the horseshoe walk known as the Coledale Round which is usually started at the village of Braithwaite just west of Keswick (but can also be started in the Newlands Valley) and includes the additional fells of Grisedale Pike, Hopegill Head, Grasmoor, Eel Crag, Sail and Scar Crags. It is a strenuous ridge walk with over of ascent. Summit.

Geographic entities mentioned:
surface_form: Grisedale Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.592
lon: -3.241
surface_form: Hopegill Head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5875
lon: -3.2626694444444
surface_form: Grasmoor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.57115
lon: -3.2791805555556
surface_form: Eel Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.572
lon: -3.25
surface_form: newlands valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.573011111111
lon: -3.1848694444444
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
surface_form: grisedale pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.592
lon: -3.241
surface_form: sail
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.571
lon: -3.242
surface_form: scar crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.574388888889
lon: -3.2266805555556
surface_form: grasmoor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.57115
lon: -3.2791805555556
surface_form: hopegill head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5875
lon: -3.2626694444444
surface_form: coledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.65
lon: -3.23333
The scree slopes around the summit have yielded some fossils: trilobites, trace fossils and graptolites are found on rare occasions. The view from the summit is extensive with Derwentwater, the Newlands valley, Skiddaw, Blencathra and the Helvellyn range seen very well. Protection. Causey Pike is within Buttermere Fells Site of Special Scientific Interest.

Geographic entities mentioned:
surface_form: Skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
surface_form: Blencathra
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.63985
lon: -3.0504611111111
surface_form: newlands valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.573011111111
lon: -3.1848694444444
surface_form: skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
surface_form: blencathra
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.63985
lon: -3.0504611111111
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
Causey Pike is separated from Barrow and Outerside to the north by Stonycroft Gill. Southward across Rigg Beck is Ard Crags. Causey Pike has a long blunt-ended shoulder running eastward to the Newlands Valley, dropping steeply from its terminus at Rowling End. Geology. The entire hill is formed from Ordovician-age rocks assigned to the Skiddaw Group.

Geographic entities mentioned:
surface_form: newlands valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.573011111111
lon: -3.1848694444444
Ascents. The direct ascent of the fell is usually started from the Newlands valley at Stonycroft where there is some car parking space; this route is steep at the beginning and the end with an easier section in the middle, the final of ascent being a rocky scramble.

Geographic entities mentioned:
surface_form: newlands valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.573011111111
lon: -3.1848694444444
It lies at an height of around 400 metres and is 5.5 hectares (13.59 acres) in size. Fell race. There is an annual Causey Pike fell race which takes place in March; it starts and finishes at Stair in the Newlands Valley and has a distance of with of climbing.. It climbs the fell directly via Ellas Crag and returns via the mine track in Stonycroft Gill.

Geographic entities mentioned:
surface_form: newlands valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.573011111111
lon: -3.1848694444444
Geology. The entire hill is formed from Ordovician-age rocks assigned to the Skiddaw Group. The summit ridge and northern slopes are composed of the laminated mudstone and siltstone of the Kirkstile Formation, whilst the summit knobble and southern slopes are formed from the Buttermere Formation, an olistostrome of disrupted, sheared and folded mudstone, siltstone and sandstone.

Geographic entities mentioned:
surface_form: skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
Causey Pike. Causey Pike is a fell in the English Lake District. It is situated in the Newlands Valley, south-west of the town of Keswick. Even though it has a modest height of it is one of the most distinctive fells when viewed from the Derwent Water and Keswick area due to its distinguishing summit &quot;knobble&quot; which catches the eye.

Geographic entities mentioned:
surface_form: derwent water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.583333333333
lon: -3.15
Geology. The entire hill is formed from Ordovician-age rocks assigned to the Skiddaw Group. The summit ridge and northern slopes are composed of the laminated mudstone and siltstone of the Kirkstile Formation, whilst the summit knobble and southern slopes are formed from the Buttermere Formation, an olistostrome of disrupted, sheared and folded mudstone, siltstone and sandstone.

Geographic entities mentioned:
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
The eastern spur and Rowling End reveal the large olistoliths of greywacke sandstone of the Robinson Member, a sub-unit of the Buttermere Formation. Ascents.

Geographic entities mentioned:
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: robinson
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.54
lon: -3.236
Causey Pike. Causey Pike is a fell in the English Lake District. It is situated in the Newlands Valley, south-west of the town of Keswick. Even though it has a modest height of it is one of the most distinctive fells when viewed from the Derwent Water and Keswick area due to its distinguishing summit &quot;knobble&quot; which catches the eye.

Geographic entities mentioned:
surface_form: causey pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.576338888889
lon: -3.2112694444444
The fell is one of 214 fells described by Alfred Wainwright in his series of &quot;Pictorial Guides to the Lakeland Fells&quot;: Causey Pike features in Book Six, &quot;The North Western Fells&quot;. Topography. The North Western Fells occupy the area between the rivers Derwent and Cocker, a broadly oval swathe of hilly country, elongated on a north–south axis.

Geographic entities mentioned:
surface_form: causey pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.576338888889
lon: -3.2112694444444
Topography. The North Western Fells occupy the area between the rivers Derwent and Cocker, a broadly oval swathe of hilly country, elongated on a north–south axis. Two roads cross from east to west, dividing the fells into three convenient groups. The central sector, rising between Whinlatter Pass and Newlands Pass, includes Causey Pike.

Geographic entities mentioned:
surface_form: causey pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.576338888889
lon: -3.2112694444444
surface_form: whinlatter
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.614
lon: -3.252
The view from the summit is extensive with Derwentwater, the Newlands valley, Skiddaw, Blencathra and the Helvellyn range seen very well. Protection. Causey Pike is within Buttermere Fells Site of Special Scientific Interest. The land surface of Causey Pike mountain is owned by the National Trust. An area of unnamed woodland clings to the hillside on the southern (Rigg Beck) side of the hill.

Geographic entities mentioned:
surface_form: causey pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.576338888889
lon: -3.2112694444444
Lake Alexandrina (South Australia). Lake Alexandrina is a coastal freshwater lake located between the Fleurieu and Kangaroo Island and Murray and Mallee regions of South Australia, about south-east of Adelaide.

Geographic entities mentioned:
surface_form: freshwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.6453
lon: -60.3967
surface_form: alexandrina
instance_of: Lake
countries: Australia
coordinates: lat: -35.45
lon: 139.15
surface_form: lake alexandrina
instance_of: Lake
countries: Australia
coordinates: lat: -35.45
lon: 139.15
The lake adjoins the smaller Lake Albert (together known as the Lower Lakes) and a coastal lagoon called The Coorong to its southeast, before draining into the Great Australian Bight via a short, narrow opening known as Murray Mouth. Aboriginal naming.

Geographic entities mentioned:
surface_form: lake albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.61666667
lon: 139.3
surface_form: lake albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.167
lon: 147.373
surface_form: albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.167
lon: 147.373
Loveday Bay is an inlet located at the south-east of Lake Alexandrina, adjacent to Tauwitchere Channel. Lake Alexandrina is connected by a narrow channel to the smaller Lake Albert to the south-east. The lake empties into the Southern Ocean via a channel known as the Murray Mouth, south-east of the town of Goolwa, but when the river flow is low, the mouth is often blocked by a sand-bar.

Geographic entities mentioned:
surface_form: lake albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.61666667
lon: 139.3
surface_form: lake albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.167
lon: 147.373
surface_form: albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.167
lon: 147.373
It was handed back to the Ngarrindjeri people in 1974, and renamed Raukkan in 1982. Inventor and author David Unaipon is from Raukkan. In 2008, water levels in Lake Alexandrina and Lake Albert became so low that there was a high risk of large quantities of acid sulphate soils forming. The soils on the lake beds are naturally rich in iron sulphides.

Geographic entities mentioned:
surface_form: lake albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.61666667
lon: 139.3
surface_form: lake albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.167
lon: 147.373
surface_form: albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.167
lon: 147.373
Freshwater fish inhabit the lake, including the introduced European carp. The soils around the lake are relatively low in organic carbon, although good barley and vegetable crops may be produced. Non-wetting soils are present along the south eastern bounds of Lake Albert and in areas around Lake Alexandrina. Birds.

Geographic entities mentioned:
surface_form: lake albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.61666667
lon: 139.3
surface_form: alexandrina
instance_of: Lake
countries: Australia
coordinates: lat: -35.45
lon: 139.15
surface_form: lake alexandrina
instance_of: Lake
countries: Australia
coordinates: lat: -35.45
lon: 139.15
surface_form: lake albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.167
lon: 147.373
surface_form: albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.167
lon: 147.373
Supplied almost entirely by the Murray, the whole lake retains the muddy tinge of which I have spoken, and this sadly detracts from the otherwise beautiful appearances of this magnificent sheet of water.&quot;
The Point McLeay mission was established by George Taplin on the shore of the lake in 1859 and became an Aboriginal reserve in 1916.

Geographic entities mentioned:
surface_form: george
instance_of: Lake
countries: Australia
coordinates: lat: -35.1667
lon: 149.417
Lake Alexandrina (South Australia). Lake Alexandrina is a coastal freshwater lake located between the Fleurieu and Kangaroo Island and Murray and Mallee regions of South Australia, about south-east of Adelaide.

Geographic entities mentioned:
surface_form: alexandrina
instance_of: Lake
countries: Australia
coordinates: lat: -35.45
lon: 139.15
surface_form: lake alexandrina
instance_of: Lake
countries: Australia
coordinates: lat: -35.45
lon: 139.15
Aboriginal naming. Aboriginal people having an association with the lake were reported as knowing it by such names as &quot;Mungkuli,&quot; &quot;Parnka&quot; and &quot;Kayinga.&quot;
European naming. English settlers named the lake after Princess Alexandrina, niece and successor of King William IV of Great Britain and Ireland.

Geographic entities mentioned:
surface_form: alexandrina
instance_of: Lake
countries: Australia
coordinates: lat: -35.45
lon: 139.15
English settlers named the lake after Princess Alexandrina, niece and successor of King William IV of Great Britain and Ireland. When the princess ascended the throne and took the name Queen Victoria, there was some talk of changing the name of the lake to Lake Victoria, but the idea was dropped. Description.

Geographic entities mentioned:
surface_form: lake victoria
instance_of: Lake
countries: Australia
coordinates: lat: -38.2667
lon: 144.6
Description. Lake Alexandrina is located north of Encounter Bay and east of Fleurieu Peninsula within what are now the two following South Australian government regions: Fleurieu and Kangaroo Island region, and the Murray Mallee region. The Murray River is the major river to flow into Lake Alexandrina.

Geographic entities mentioned:
surface_form: alexandrina
instance_of: Lake
countries: Australia
coordinates: lat: -35.45
lon: 139.15
surface_form: lake alexandrina
instance_of: Lake
countries: Australia
coordinates: lat: -35.45
lon: 139.15
Others include the Bremer, Angas, and Finniss rivers, all from the eastern side of the southern Mount Lofty Ranges. The lake is shallow and contains a number of islands near the southern end. Loveday Bay is an inlet located at the south-east of Lake Alexandrina, adjacent to Tauwitchere Channel. Lake Alexandrina is connected by a narrow channel to the smaller Lake Albert to the south-east.

Geographic entities mentioned:
surface_form: alexandrina
instance_of: Lake
countries: Australia
coordinates: lat: -35.45
lon: 139.15
surface_form: alexandrina
instance_of: Lake
countries: Australia
coordinates: lat: -35.45
lon: 139.15
surface_form: lake alexandrina
instance_of: Lake
countries: Australia
coordinates: lat: -35.45
lon: 139.15
surface_form: lake alexandrina
instance_of: Lake
countries: Australia
coordinates: lat: -35.45
lon: 139.15
History. Edward Wilson, visiting the lake in the 1850s described it as follows: &quot;Lake Alexandrina is the finest sheet of fresh water I ever saw. Indeed so formidable did it look, with a stiff wind blowing up quite a sufficient swell to make one seasick, that I could scarcely believe it to be fresh. Such is the fact however.

Geographic entities mentioned:
surface_form: alexandrina
instance_of: Lake
countries: Australia
coordinates: lat: -35.45
lon: 139.15
surface_form: lake alexandrina
instance_of: Lake
countries: Australia
coordinates: lat: -35.45
lon: 139.15
Australian government. Lake Alexandrina is part of the wetland complex known as the Coorong and Lakes Alexandrina and Albert Wetland which is listed as a Ramsar site. The wetland is also appears in the non-statutory list known as &quot;A Directory of Important Wetlands in Australia&quot;. South Australian government.

Geographic entities mentioned:
surface_form: alexandrina
instance_of: Lake
countries: Australia
coordinates: lat: -35.45
lon: 139.15
surface_form: albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.167
lon: 147.373
South Australian government. Lake Alexandrina includes the following protected areas declared under the &quot;National Parks and Wildlife Act 1972&quot; - Currency Creek Game Reserve, Mud Islands Game Reserve, Salt Lagoon Islands Conservation Park and Tolderol Game Reserve. Non-statutory arrangements.

Geographic entities mentioned:
surface_form: alexandrina
instance_of: Lake
countries: Australia
coordinates: lat: -35.45
lon: 139.15
surface_form: lake alexandrina
instance_of: Lake
countries: Australia
coordinates: lat: -35.45
lon: 139.15
Non-statutory arrangements. Lake Alexandrina is included within the boundary of the Lakes Alexandrina and Albert Important Bird Area which is an area considered by BirdLife International to be a place of ‘international significance for the conservation of birds and other biodiversity.’

Geographic entities mentioned:
surface_form: alexandrina
instance_of: Lake
countries: Australia
coordinates: lat: -35.45
lon: 139.15
surface_form: albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.167
lon: 147.373
The Murray River is the major river to flow into Lake Alexandrina. Others include the Bremer, Angas, and Finniss rivers, all from the eastern side of the southern Mount Lofty Ranges. The lake is shallow and contains a number of islands near the southern end. Loveday Bay is an inlet located at the south-east of Lake Alexandrina, adjacent to Tauwitchere Channel.

Geographic entities mentioned:
surface_form: mount lofty
instance_of: Mountain
countries: Australia
coordinates: lat: -34.966666666667
lon: 138.7
In the same year, he married Barbara Chizzoli, an heiress whose dowry allowed him to devote himself to literary-historical studies. Mazzucchelli's father bought the Moggi's sixteenth-century family house, located between Brescia and Lake Garda, in 1722, and added the central building and the west wing some time later.

Geographic entities mentioned:
surface_form: Lake Garda
instance_of: Lake
countries: Italy
coordinates: lat: 45.633333333333
lon: 10.666666666667
Savage Junction and Mt. Savage, and discontinued use of the tunnel under Frostburg, due to the tunnel's low clearances. Some branch lines to local mines were also eliminated. Coal traffic south of Frostburg was routed along the WM's Georges Creek Branch to the WM junction at Westernport, Maryland (directly across the North Branch Potomac River from Piedmont). Extant facilities.

Geographic entities mentioned:
surface_form: North Branch Potomac River
instance_of: Watercourse
countries: United States
coordinates: lat: 39.5284255
lon: -78.5875141
Hnilec (river). The Hnilec (),) is a river in Slovakia. Its source is located below the Kráľova hoľa mountain, Low Tatras. It flows into the Hornád river near Margecany. The Palcmanská Maša dam is located on the river near Dobšiná. Places of interest along the river include Dobšiná Ice Cave and the Slovak Paradise. It is long and its basin size is.

Geographic entities mentioned:
surface_form: Kráľova hoľa
instance_of: Mountain
countries: Slovakia
coordinates: lat: 48.882961111111
lon: 20.139111111111
A $4,400 Model E-8-75 floatplane became the Navy's first aircraft when ordered by Captain Washington Irving Chambers on 8 May 1911 and received the designation A-1, as well as the nickname &quot;Triad&quot; hydroaeroplane since it could operate from land and sea and in the air. Theodore Ellyson became the Navy's first pilot when he took off from Keuka Lake near Hammondsport, New York on 30 June.

Geographic entities mentioned:
surface_form: Keuka Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.496388888889
lon: -77.146111111111
It is the second most important north-south link through the Swiss Alps after the Gotthard railway. Together with the Simplon Tunnel and the Italian part of the Simplon line, it also connects the Swiss Plateau to Northern Italy. The more recent Lötschberg Base Tunnel replaces most of the open-air section of the mountain line and allows faster travel between Bern and Brig.

Geographic entities mentioned:
surface_form: Swiss Plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
After the Kander viaduct, the mountain line continues towards Kandergrund and Mitholz. The line turns northward after the loop at Mitholz and climbs out of the valley on the western flanks of the Ärmighorn. A spiral tunnel turns the line southward again, before it reaches Kandersteg, the last station on the northern approach.

Geographic entities mentioned:
surface_form: Ärmighorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.541694444444
lon: 7.7137777777778