Sarmila/GeoWiki-Features huggingface dataset:
The Patapsco valley was used as the route of the Baltimore and Ohio Railroad's original main line west constructed from 1829 onwards, and this route remains, though much altered. Many old railroad bridges were constructed in the valley, most notably the Thomas Viaduct and the Patterson Viaduct, of which ruins remain. Flour mills and a hydropower dam were formerly powered by the river.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
One of the good examples is at Bishapur, some of the floors were decorated with mosaics showing scenes of merrymaking as at a banquet; the Roman influence here is clear, and the mosaics may have been laid by Roman prisoners. Buildings were also decorated with wall paintings; particularly fine examples have been found on Mount Khajeh in Sistan.

Geographic entities mentioned:
surface_form: Mount Khajeh
instance_of: Mountain
countries: Iran
coordinates: lat: 30.94388888888889
lon: 61.24444444444445
The Cavallo Point conference center is in East Fort Baker on the eastern side of the peninsula. Other areas within Marin Headlands include Kirby Cove, Rodeo Lagoon, and Tennessee Cove. Various nonprofit organizations have facilities in Marin Headlands.

Geographic entities mentioned:
surface_form: Rodeo Lagoon
instance_of: Lake
countries: United States
coordinates: lat: 37.8308
lon: -122.531
surface_form: rodeo lagoon
instance_of: Lake
countries: United States
coordinates: lat: 37.8308
lon: -122.531
Hawk Hill. The centerpoint of the Marin Headlands skyline is the Hawk Hill, the lookout point for the largest known flight of diurnal raptors in the Pacific states. Each autumn, from August into December, tens of thousands of hawks, kites, falcons, eagles, vultures, osprey, and harriers are funneled by the peninsular shape of Marin County into the headlands.

Geographic entities mentioned:
surface_form: the lookout
instance_of: Mountain
countries: United States
coordinates: lat: 40.509444444444
lon: -75.346111111111
surface_form: hawk hill
instance_of: Landform
countries: United States
coordinates: lat: 37.8285
lon: -122.499
surface_form: marin headlands
instance_of: Landform
countries: United States
coordinates: lat: 37.827777777778
lon: -122.50611111111
Military sites. The Marin Headlands are the site of a number of historic military settlements and fortifications, including Fort Cronkhite, Fort Barry, a large number of bunkers and batteries, and the SF-88 Nike Missile silo. The Baker–Barry Tunnel connects the former military bases Fort Barry and Fort Baker in the Marin Headlands of Marin County, California.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: marin headlands
instance_of: Landform
countries: United States
coordinates: lat: 37.827777777778
lon: -122.50611111111
Conference center facilities are located in former military buildings maintained by the Point Bonita YMCA, NatureBridge, and the Headlands Center for the Arts. The Cavallo Point conference center is in East Fort Baker on the eastern side of the peninsula. Other areas within Marin Headlands include Kirby Cove, Rodeo Lagoon, and Tennessee Cove.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Summer days alternate between clear and warm intervals, giving way to foggy and cool periods. September and October bring the highest average temperatures of the year and the longest stretches of clear skies. Hawk Hill. The centerpoint of the Marin Headlands skyline is the Hawk Hill, the lookout point for the largest known flight of diurnal raptors in the Pacific states.

Geographic entities mentioned:
surface_form: hawk hill
instance_of: Landform
countries: United States
coordinates: lat: 37.8285
lon: -122.499
The batteries at Kirby Cove, above Black Sands Beach, south of Rodeo Beach, and at Battery Mendell are examples of fortifications from the pre–World War I period. During World War II, Batteries Wallace, Townsley, and 129 on Hawk Hill were built into the hills to protect them from aerial bombardment and the high-caliber shells that would be fired by Axis battleships.

Geographic entities mentioned:
surface_form: hawk hill
instance_of: Landform
countries: United States
coordinates: lat: 37.8285
lon: -122.499
surface_form: hawk hill
instance_of: Landform
countries: United States
coordinates: lat: 37.8285
lon: -122.499
The emplacements at the top of Hawk Hill were used for a radio station. During the Cold War, the gun batteries were decommissioned, but antiaircraft missile sites were built on the northern and southern sides of Rodeo Lagoon. Radar sites were placed atop Hawk Hill and Hill 88.

Geographic entities mentioned:
surface_form: rodeo lagoon
instance_of: Lake
countries: United States
coordinates: lat: 37.8308
lon: -122.531
On clear days, the site offers views of the bay, including the Farallon Islands, Angel Island, Alcatraz, the San Francisco–Oakland Bay Bridge, the Golden Gate Bridge and the East Bay. Where Conzelman Road runs along the southern shore of the Headlands and becomes one-way, a pedestrian path leads upwards to Hawk Hill.

Geographic entities mentioned:
surface_form: hawk hill
instance_of: Landform
countries: United States
coordinates: lat: 37.8285
lon: -122.499
Hiking/biking. There are many hiking and biking trails in the Headlands, several of which pass through coastal sage scrub, chaparral, and riparian areas. Birding. The raptor migration attracts birdwatchers to Hawk Hill, and waterfowl and seabirds can sometimes be seen on Rodeo Lagoon. Facilities and notable places.

Geographic entities mentioned:
surface_form: hawk hill
instance_of: Landform
countries: United States
coordinates: lat: 37.8285
lon: -122.499
surface_form: rodeo lagoon
instance_of: Lake
countries: United States
coordinates: lat: 37.8308
lon: -122.531
Public restrooms are available in the Headlands at the visitor center parking lot, the parking lot near Rodeo Beach, and portable toilet facilities are available at the trailhead leading to the Point Bonita Lighthouse, along Conzelman Road near Black Sands Beach, at Battery Alexander dug into the hillside between Rodeo Beach and the Lighthouse, and at Battery 129 on Hawk Hill.

Geographic entities mentioned:
surface_form: hawk hill
instance_of: Landform
countries: United States
coordinates: lat: 37.8285
lon: -122.499
In 2003, there was a reported sighting of a black bear in the Headlands; the report was lent credence by a 2012 finding of bear scat on a hiking trail in the Kent Lake watershed, and another sighting on the Point Reyes National Seashore in 2011. River otters inhabit the freshwater lagoons and streams.

Geographic entities mentioned:
surface_form: kent lake
instance_of: Lake
countries: United States
coordinates: lat: 45.85916667
lon: -93.33083333
Marin Headlands. The Marin Headlands are a hilly peninsula at the southernmost end of Marin County, California, United States, located just north of San Francisco across the Golden Gate Bridge, which connects the two counties and peninsulas. The entire area is part of the Golden Gate National Recreation Area.

Geographic entities mentioned:
surface_form: marin headlands
instance_of: Landform
countries: United States
coordinates: lat: 37.827777777778
lon: -122.50611111111
Volunteers with the Golden Gate Raptor Observatory count and track this fall migration using bird-banding and radio-tracking techniques, all in cooperation with the National Park Service. Wildlife. The Marin Headlands are also home to black tail deer, mountain lions, bobcats, two types of foxes, coyotes, wild turkeys, hares, rabbits, raccoons, and skunks.

Geographic entities mentioned:
surface_form: marin headlands
instance_of: Landform
countries: United States
coordinates: lat: 37.827777777778
lon: -122.50611111111
visited San Francisco Bay in 1835 he wrote about vast elk (&quot;Cervus canadensis&quot;) herds on the Marin Headlands on December 27: &quot;...we came to anchor near the mouth of the bay, under a high and beautifully sloping hill, upon which herds of hundreds and hundreds of red deer [note: &quot;red deer&quot; is the European term for &quot;elk&quot;], and the stag, with his high branching antlers, were bounding about...&quot;
Geology.

Geographic entities mentioned:
surface_form: marin headlands
instance_of: Landform
countries: United States
coordinates: lat: 37.827777777778
lon: -122.50611111111
surface_form: marin headlands
instance_of: Landform
countries: United States
coordinates: lat: 37.827777777778
lon: -122.50611111111
The Marin Headlands are one of the featured field trips found in the Streetcar 2 Subduction online field trip guide series released in December 2019 by the American Geophysical Union. Native Americans. The Marin Headlands are home to the Coastal Miwok tribe.

Geographic entities mentioned:
surface_form: marin headlands
instance_of: Landform
countries: United States
coordinates: lat: 37.827777777778
lon: -122.50611111111
Development. In the 1960s, the government sold over of land in the Marin Headlands to a private developer who planned to build a city named Marincello. The development was to house 30,000 people in 50 apartment towers, vast tracts of single-family homes, a shopping center, and a hotel along the Headlands' pristine shoreline and hills.

Geographic entities mentioned:
surface_form: marin headlands
instance_of: Landform
countries: United States
coordinates: lat: 37.827777777778
lon: -122.50611111111
The Cavallo Point conference center is in East Fort Baker on the eastern side of the peninsula. Other areas within Marin Headlands include Kirby Cove, Rodeo Lagoon, and Tennessee Cove. Various nonprofit organizations have facilities in Marin Headlands.

Geographic entities mentioned:
surface_form: marin headlands
instance_of: Landform
countries: United States
coordinates: lat: 37.827777777778
lon: -122.50611111111
Various nonprofit organizations have facilities in Marin Headlands. These include the Marine Mammal Center, the Foundation for Deep Ecology, and the NatureBridge campus (formerly known as the Headlands Institute), all in Fort Cronkhite; the Headlands Center for the Arts and the at Fort Barry; and the Marin Headlands and Tennessee Valley Native Plant Nurseries.

Geographic entities mentioned:
surface_form: marin headlands
instance_of: Landform
countries: United States
coordinates: lat: 37.827777777778
lon: -122.50611111111
surface_form: tennessee valley
instance_of: Valley
countries: United States
coordinates: lat: 35.959166666667
lon: -83.850277777778
surface_form: tennessee valley
instance_of: Valley
countries: United States
coordinates: lat: 37.8611
lon: -122.534
Additional restrictions for heavy goods vehicles are applied on the section situated between Montjuïc–Morrot and Rambla de Prim near Sant Adrià de Besòs, whereby weight limits is posted 12 tonnes and all vehicles over 12 meters long are banned from that section. Exit list.

Geographic entities mentioned:
surface_form: Montjuïc
instance_of: Mountain
countries: Spain
coordinates: lat: 41.364166666667
lon: 2.1580555555556
Then, it flows southwest, crosses below the Panamericana, to the vicinity of the city of Talca to empty into the Maule River. In this last portion of its course, the river receives the waters of the tributary Lircay River. The invasive plant species &quot;Limnobium laevigatum&quot; is present in the river.

Geographic entities mentioned:
surface_form: Lircay River
instance_of: Watercourse
countries: Chile
coordinates: lat: -35.37929
lon: -71.64834
The sixth section comprises pictorial chronicles spanning the years 1195 to 1549, beginning with the migration from Chicomoztoc—the mythical place of origin of the Nahuatl-speaking peoples—and continuing with events in the Valley of Mexico. It includes representations of rulers, military campaigns, celestial phenomena, and other historical events (66v–94r).

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
Statistics show that most Indians in Italy tend to settle in the north of the country and work in agriculture. The Po Valley is similar in climate to the Punjab, where most of these Sikh workers are from. Their first jobs tend to be directly with the cows and buffalos, as many come from farming families, but some move on to become cheesemakers, which is better paying.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
San Lorenzo Valley Museum. The San Lorenzo Valley Museum is a pair of galleries and education centers created by the San Lorenzo Valley Historical Society &quot;to preserve and share the history of the San Lorenzo Valley&quot;. Founded in March 1976, it operates as a nonprofit educational institution. The Museum's original gallery is located in Boulder Creek.

Geographic entities mentioned:
surface_form: San Lorenzo Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.0967
lon: -122.0962
The dam was constructed originally to prevent flooding after the disastrous 1934 flood in Poland which took the lives of 55 people and caused damages estimated at 60 million interbellum zlotys; the biggest flood in the Second Polish Republic. The construction of the Rożnów Dam resulted in the creation of the Lake Rożnów which took two years to fill along the stretch of the Dunajec river.

Geographic entities mentioned:
surface_form: Lake Rożnów
instance_of: Lake
countries: Poland
coordinates: lat: 49.73222222
lon: 20.71444444
Sockeye that live and reproduce in lakes are commonly called &quot;kokanee&quot;, which is red-fish name in the Sinixt Interior Salish language and silver trout in the Okanagan language. They are much smaller than the anadromous variety and are rarely over long. In the Okanagan Lake and many others, there are two kinds of kokanee populations – one spawns in streams and the other near lake shores.

Geographic entities mentioned:
surface_form: Okanagan Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.920833333333
lon: -119.5
The largest spawning grounds in Asia are located on the Kamchatka Peninsula of the Russian Far East, especially on the Ozernaya River of the Kurile Lake, which accounts for nearly 90% of all Asian sockeye salmon production, and is recognized as the largest spawning ground outside of Alaska. Illegal fishing in Kamchatka is subject to environmental concern. Sockeye is almost never farmed.

Geographic entities mentioned:
surface_form: Kurile Lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 51.457222222222
lon: 157.09861111111
Phyllis Beatrice Munday (née James; 24 September 1894 &ndash; 11 April 1990) was a Canadian mountaineer, explorer, naturalist and humanitarian. She was famed for being the first woman to reach the summit of Mount Robson (with Annette Buck) in 1924, and with her husband Don for discovering Mount Waddington, and exploring the area around it via the Franklin River and the Homathko River.

Geographic entities mentioned:
surface_form: Mount Robson
instance_of: Mountain
countries: Canada
coordinates: lat: 53.11055555555556
lon: -119.15666666666667
surface_form: Mount Waddington
instance_of: Mountain
countries: Canada
coordinates: lat: 51.373611111111
lon: -125.26333333333
Munday was awarded the Order of Canada in 1972 for her work with the Girl Guides of Canada and St. John Ambulance, as well as for her mountaineering career. Mount Munday is named after Don and Phyllis Munday, and Baby Munday Peak is named for their daughter Edith. Early life. Phyllis Beatrice James was born on 24 September 1894 in Ceylon (now Sri Lanka).

Geographic entities mentioned:
surface_form: Mount Munday
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3286
lon: -125.216
surface_form: Baby Munday Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.166667
lon: -121.628334
Early life. Phyllis Beatrice James was born on 24 September 1894 in Ceylon (now Sri Lanka). Her parents, Frank and Beatrice James, were members of the upper class, as Frank managed tea plantations for the Lipton and Ridgways companies. The family departed Ceylon in 1901, and moved to England and Manitoba before settling on the western shore of Kootenay Lake in 1903.

Geographic entities mentioned:
surface_form: Kootenay Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
The family traveled Vancouver by steamship and train, intending to continue on to New Zealand, but they instead stayed in Vancouver. In 1912 she climbed Grouse Mountain with her Girl Guide company. In 1915, at 21, Phyllis joined the British Columbia Mountaineering Club and began going on club trips to such places as Mount Seymour, The Lions, Mount Tantalus and Mount Garibaldi. Meeting Don.

Geographic entities mentioned:
surface_form: Grouse Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.38611111
lon: -123.07638889
The family traveled Vancouver by steamship and train, intending to continue on to New Zealand, but they instead stayed in Vancouver. In 1912 she climbed Grouse Mountain with her Girl Guide company. In 1915, at 21, Phyllis joined the British Columbia Mountaineering Club and began going on club trips to such places as Mount Seymour, The Lions, Mount Tantalus and Mount Garibaldi. Meeting Don.

Geographic entities mentioned:
surface_form: Mount Seymour
instance_of: Mountain
countries: Canada
coordinates: lat: 49.393333333333
lon: -122.94444444444
surface_form: Mount Tantalus
instance_of: Mountain
countries: Canada
coordinates: lat: 49.818111111111
lon: -123.32938888889
surface_form: Mount Garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Their daughter, Edith was born in 1921, and at 11 weeks she was carried to the top of Crown Mountain. From 1923 to 1926 the Mundays lived in a tent, and then a cabin on Grouse Mountain where Don worked cutting a trail from Lonsdale Avenue in North Vancouver, British Columbia to the summit, while Phyllis ran the Alpine Lodge, serving hot drinks and meals to hikers.

Geographic entities mentioned:
surface_form: Grouse Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.38611111
lon: -123.07638889
Exploration of the Waddington Range. In 1925, while on a trip to Mount Arrowsmith, Vancouver Island, Don and Phyllis Munday spotted what they believed to be a peak taller than Mount Robson, the then accepted tallest peak entirely within British Columbia.

Geographic entities mentioned:
surface_form: Mount Arrowsmith
instance_of: Mountain
countries: Canada
coordinates: lat: 49.12
lon: -124.29
surface_form: Mount Robson
instance_of: Mountain
countries: Canada
coordinates: lat: 53.11055555555556
lon: -119.15666666666667
On April 11, 2016, West traveled to the Isle of Skye in Scotland to film a music video for &quot;Waves&quot;, flying there from a performance in the Philippines that included the song. The shoot spanned a few days and Hype Williams served as director, with Lealt Falls and the Storr reported as locations.

Geographic entities mentioned:
surface_form: the Storr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.507106
lon: -6.183079
Espot. Espot () is a town and municipality in Pallars Sobirà county in Catalonia. It has a population of. It is located in the Espot Valley, west of the river Noguera Pallaresa. The municipality is one of the entrances to the Aigüestortes i Estany de Sant Maurici National Park. Espot has been mentioned in documents dating back to the year 839. Economy.

Geographic entities mentioned:
surface_form: Noguera Pallaresa
instance_of: Watercourse
countries: Spain
coordinates: lat: 41.9064
lon: 0.8901
Sea Lion Tarn. Sea Lion Tarn (,) is a freshwater tarn with an area of located between Sea Lion Glacier and the north-western slopes of Atlantic Club Ridge on Hurd Peninsula in eastern Livingston Island in the South Shetland Islands, Antarctica. The lake drains westward through a 100 m creek into South Bay. The feature takes its name from the adjacent Sea Lion Glacier. Location.

Geographic entities mentioned:
surface_form: sea lion tarn
instance_of: Lake
coordinates: lat: -62.646666666667
lon: -60.370555555556
Sea Lion Tarn. Sea Lion Tarn (,) is a freshwater tarn with an area of located between Sea Lion Glacier and the north-western slopes of Atlantic Club Ridge on Hurd Peninsula in eastern Livingston Island in the South Shetland Islands, Antarctica. The lake drains westward through a 100 m creek into South Bay. The feature takes its name from the adjacent Sea Lion Glacier. Location.

Geographic entities mentioned:
surface_form: sea lion tarn
instance_of: Lake
coordinates: lat: -62.646666666667
lon: -60.370555555556
surface_form: hurd
instance_of: Landform
coordinates: lat: -62.68341667
lon: -60.36841667
He served as King Magnus IV's lendmann (governor) for the Oplands. Ivar Gjesling, allied himself with the Birchlegs (Birkebeinerne) — who chose Sverre as their King at the Øreting in 1177. King Sverre granted him the valley of Heidal as a reward. Sigrid Undset's fictional Lady Ragnfrid, wife of Lavrans, was created a Gjesling from Sandbu.

Geographic entities mentioned:
surface_form: Heidal
instance_of: Valley
countries: Norway
coordinates: lat: 61.71789
lon: 9.4512
Jaeyaksan. Jaeyaksan () is a mountain of South Korea. It has an elevation of 1,108 metres. It is part of the Yeongnam Alps mountain range.

Geographic entities mentioned:
surface_form: jaeyaksan
instance_of: Mountain
countries: South Korea
coordinates: lat: 35.54666667
lon: 128.98055556
Basket Lake Wildlife Management Area. Basket Lake Wildlife Management Area (WMA) is a provincially designated protected area in Manitoba. It is located north of Lake Manitoba and west of Hwy 6. It was designated under the Manitoba Wildlife Act by the Government of Manitoba in 1974. It is in size.

Geographic entities mentioned:
surface_form: Lake Manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
Tai Mun Shan. Tai Mun Shan (大蚊山; daaih mān shāan) lies to the west of Tai Long Wan near Chek King on the Sai Kung Peninsula in Hong Kong. The hill comprises a rounded peak, which rises to a height 370 metres (1,210 feet). The name translates as the &quot;Big Hill of the Mosquitoes&quot;.

Geographic entities mentioned:
surface_form: tai mun shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.4156
lon: 114.365
Crimson Hill. Crimson Hill () is a prominent, ice-free hill, high, on the south side of Pendulum Cove, Deception Island, in the South Shetland Islands. It was so named in 1829 by the British expedition under Foster, because there was a prominent stratum of brickstone in the hill.

Geographic entities mentioned:
surface_form: foster
instance_of: Mountain
coordinates: lat: -62.996666666667
lon: -62.548611111111
Crimson Hill. Crimson Hill () is a prominent, ice-free hill, high, on the south side of Pendulum Cove, Deception Island, in the South Shetland Islands. It was so named in 1829 by the British expedition under Foster, because there was a prominent stratum of brickstone in the hill.

Geographic entities mentioned:
surface_form: crimson hill
instance_of: Mountain
coordinates: lat: -62.95
lon: -60.6
Punnappuzha is also known as Pandiyar when it flows through Tamil Nadu. One branch of this river originate from northern slopes of Mukurthi National Park and another branch from Gudalur, in Nilagiri district of Tamil Nadu. These two branches join together 5 km south-west of Gudalur town. When it reaches Edakkara, the river Maruthappuzha joins with it.

Geographic entities mentioned:
surface_form: Mukurthi
instance_of: Mountain
countries: India
coordinates: lat: 11.3715
lon: 76.5177
state of Michigan. Incorporated in 1879, the -long railroad began operations in 1881. It was intended to help the economic development of a region of frontier timberland along the shores of Lake Michigan and Lake Superior. Its successor line was the Duluth, South Shore and Atlantic Railway. History.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Colonel Samuel Smith Park is an urban park in the Etobicoke district of Toronto, Ontario, Canada and a former weekend get-away destination for Victorian Torontonians. The park has a variety of attractions, including a children's playground located only steps from Lake Ontario. The park is named for Lieutenant Colonel Samuel Smith and lands were part of his property in the 1800s.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Wetherlam. Wetherlam (763 m) is a mountain in the English Lake District. It is the most northerly of the Coniston Fells, the range of fells to the north-west of Coniston village; its north-east slopes descend to Little Langdale. Topography. Wetherlam stands apart from the main north–south spine of the Coniston Fells, the connection being via the long east ridge of Swirl How.

Geographic entities mentioned:
surface_form: Little Langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.419557
lon: -3.073825
Topography. Wetherlam stands apart from the main north–south spine of the Coniston Fells, the connection being via the long east ridge of Swirl How. Midway along this ridge is Black Sails, an intermediate top usually considered to be part of Wetherlam, and listed as a Hewitt in its own right.

Geographic entities mentioned:
surface_form: Swirl How
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.395661111111
lon: -3.1212305555556
surface_form: wetherlam
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.401
lon: -3.098
Black Sails has a descending southern spur which steps down over High and Low Wether Crags. Between this and the main Coniston range is the valley of Swirl Hawse Beck and Levers Water. This tarn has been raised by damming to a depth of, originally to supply water to the Coniston Copper Mines.

Geographic entities mentioned:
surface_form: Levers Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.384134
lon: -3.11098
A natural waterbody was dammed in the early 18th century to provide water for the Greenburn Mine. The barrage has now been breached to leave a collection of pools and bogs. Greenburn is bounded to the north by the curve of Wet Side Edge, falling from Great Carrs. Summit. The summit is a gentle dome with a cairn marking the highest point.

Geographic entities mentioned:
surface_form: Great Carrs
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.3983
lon: -3.12438
The principal copper mining areas were to the south of Wetherlam, in what is now Coppermines Valley. Much of the activity took place on the slopes of Brim Fell to the south, but Red Dell and the ridges on either side hold many shafts, and there are workings below the bed of Levers Water. These mines were at their most productive in the 1850s, closing in 1915.

Geographic entities mentioned:
surface_form: Brim Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.3777
lon: -3.12381
surface_form: brim fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.3777
lon: -3.12381
surface_form: levers water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.384134
lon: -3.11098
It is then a steep ascent (around 200 metres in half a kilometre – 40%) up the latter ridge to reach the summit. Wetherlam is often climbed as part of the &quot;Coniston Round&quot;, a circuit of the skyline of the Coppermines Valley that takes in Swirl How, Brim Fell, the Old Man of Coniston and optionally Dow Crag.

Geographic entities mentioned:
surface_form: Dow Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.369438888889
lon: -3.1374388888889
surface_form: dow crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.369438888889
lon: -3.1374388888889
surface_form: swirl how
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.395661111111
lon: -3.1212305555556
surface_form: brim fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.3777
lon: -3.12381
Midway along this ridge is Black Sails, an intermediate top usually considered to be part of Wetherlam, and listed as a Hewitt in its own right. From Swirl How the east ridge drops steeply down Prison Band to Swirl Hawse, before rising again to the summit of Black Sails. Black Sails has a descending southern spur which steps down over High and Low Wether Crags.

Geographic entities mentioned:
surface_form: swirl how
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.395661111111
lon: -3.1212305555556
Wetherlam. Wetherlam (763 m) is a mountain in the English Lake District. It is the most northerly of the Coniston Fells, the range of fells to the north-west of Coniston village; its north-east slopes descend to Little Langdale. Topography. Wetherlam stands apart from the main north–south spine of the Coniston Fells, the connection being via the long east ridge of Swirl How.

Geographic entities mentioned:
surface_form: wetherlam
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.401
lon: -3.098
Topography. Wetherlam stands apart from the main north–south spine of the Coniston Fells, the connection being via the long east ridge of Swirl How. Midway along this ridge is Black Sails, an intermediate top usually considered to be part of Wetherlam, and listed as a Hewitt in its own right.

Geographic entities mentioned:
surface_form: wetherlam
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.401
lon: -3.098
Following the decline of mining a water treatment plant was built, and since the 1970s the tarn has supplied drinking water for Coniston and other local villages as far east as Sawrey. The main ridge continues east from Black Sails across the depression of Red Dell Head to the summit of Wetherlam. A second southward spur, paralleling that from Black Sails, descends from the main summit.

Geographic entities mentioned:
surface_form: wetherlam
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.401
lon: -3.098
A second southward spur, paralleling that from Black Sails, descends from the main summit. This is Lad Stones ridge and the valley contained between the two is Red Dell. Wetherlam has a further ridge which descends steeply north eastward along Wetherlam Edge. This leads via Birk Fell to an attractive upland plateau between Tilberthwaite and Little Langdale.

Geographic entities mentioned:
surface_form: wetherlam
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.401
lon: -3.098
surface_form: wetherlam
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.401
lon: -3.098
This leads via Birk Fell to an attractive upland plateau between Tilberthwaite and Little Langdale. Many rocky knolls characterise the area, the most prominent being Blake Rigg and Great Intake. To the south east of Wetherlam is a further upland area, named Yewdale Fells on Ordnance Survey maps. This displays less bare rock, but is fringed by a wall of crag above the Coniston - Ambleside road.

Geographic entities mentioned:
surface_form: wetherlam
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.401
lon: -3.098
To the south east of Wetherlam is a further upland area, named Yewdale Fells on Ordnance Survey maps. This displays less bare rock, but is fringed by a wall of crag above the Coniston - Ambleside road. To the north of Wetherlam is the Greenburn Valley, a feeder of Little Langdale. A steep sided, rather marshy valley, Greenburn's waters join the River Brathay at Little Langdale Tarn.

Geographic entities mentioned:
surface_form: wetherlam
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.401
lon: -3.098
surface_form: little langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.419557
lon: -3.073825
Little Langdale is perhaps the finest aspect. Mining. In the past Wetherlam was extensively exploited for its mineral resources. The slopes on all sides are pitted with disused copper mines and slate quarries, making it the most industrialised of the Lake District fells. The workings are on a small scale, however, and, according to Alfred Wainwright, unobtrusive: &quot;this fine hill...

Geographic entities mentioned:
surface_form: wetherlam
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.401
lon: -3.098
is too vast and sturdy to be disfigured and weakened by man's feeble scratchings of its surface&quot;. The principal copper mining areas were to the south of Wetherlam, in what is now Coppermines Valley. Much of the activity took place on the slopes of Brim Fell to the south, but Red Dell and the ridges on either side hold many shafts, and there are workings below the bed of Levers Water.

Geographic entities mentioned:
surface_form: wetherlam
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.401
lon: -3.098
Ascents. There are three natural starting points for an ascent of Wetherlam: the village of Coniston to the south, and the valleys of Tilberthwaite to the east and Little Langdale to the north-east. From Coniston a path and an unsurfaced road lead into the Coppermines Valley, the site of a number of disused mines; this is also the start of a popular path up the Old Man of Coniston.

Geographic entities mentioned:
surface_form: wetherlam
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.401
lon: -3.098
surface_form: little langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.419557
lon: -3.073825
From Coniston a path and an unsurfaced road lead into the Coppermines Valley, the site of a number of disused mines; this is also the start of a popular path up the Old Man of Coniston. There are two possible routes to Wetherlam's summit from the Coppermines: either up the south ridge, called Lad Stones, or up the Red Dell valley to the west of the ridge.

Geographic entities mentioned:
surface_form: wetherlam
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.401
lon: -3.098
There are two possible routes to Wetherlam's summit from the Coppermines: either up the south ridge, called Lad Stones, or up the Red Dell valley to the west of the ridge. Walkers approaching from Little Langdale or Tilberthwaite can take any of a number of paths to Birk Fell Hawse, a small col to the north-east of the summit at the foot of the ridge of Wetherlam Edge.

Geographic entities mentioned:
surface_form: wetherlam
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.401
lon: -3.098
surface_form: little langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.419557
lon: -3.073825
Little Langdale is perhaps the finest aspect. Mining. In the past Wetherlam was extensively exploited for its mineral resources. The slopes on all sides are pitted with disused copper mines and slate quarries, making it the most industrialised of the Lake District fells. The workings are on a small scale, however, and, according to Alfred Wainwright, unobtrusive: &quot;this fine hill...

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
This is Lad Stones ridge and the valley contained between the two is Red Dell. Wetherlam has a further ridge which descends steeply north eastward along Wetherlam Edge. This leads via Birk Fell to an attractive upland plateau between Tilberthwaite and Little Langdale. Many rocky knolls characterise the area, the most prominent being Blake Rigg and Great Intake.

Geographic entities mentioned:
surface_form: little langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.419557
lon: -3.073825
This displays less bare rock, but is fringed by a wall of crag above the Coniston - Ambleside road. To the north of Wetherlam is the Greenburn Valley, a feeder of Little Langdale. A steep sided, rather marshy valley, Greenburn's waters join the River Brathay at Little Langdale Tarn. Greenburn itself bears a tarn, or more correctly the remains of a reservoir.

Geographic entities mentioned:
surface_form: little langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.419557
lon: -3.073825
Greenburn is bounded to the north by the curve of Wet Side Edge, falling from Great Carrs. Summit. The summit is a gentle dome with a cairn marking the highest point. The vista is wide with the majority of the Southern, Central and Eastern Fells in view. Little Langdale is perhaps the finest aspect. Mining. In the past Wetherlam was extensively exploited for its mineral resources.

Geographic entities mentioned:
surface_form: little langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.419557
lon: -3.073825
This includes a discussion of belief in gods and how those religious views were shaped by the existence of gravity and its prevalence on living beings and all matter. The topics of Mount Olympus and stories among Aboriginal cultures in Australia are discussed in how the sky is believed to be separate from the earth and creates a separation between humans and the divine.

Geographic entities mentioned:
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
Rowing at the 1992 Summer Olympics – Women's coxless pair. The women's coxless pair competition at the 1992 Summer Olympics took place at took place at Lake of Banyoles, Spain. Competition format. The competition consisted of three main rounds (heats, semifinals, and finals) as well as a repechage. The 13 boats were divided into three heats for the first round, with 4 or 5 boats in each heat.

Geographic entities mentioned:
surface_form: Lake of Banyoles
instance_of: Lake
countries: Spain
coordinates: lat: 42.125277777778
lon: 2.7552777777778
Wawel Hill (Antarctica). aj8d5vx0pml5yj5xvl4lueetxxhx" xml:space="preserve">Wawel Hill is a hill rising to 290 m north of Point Hennequin, on the east side of Admiralty Bay, King George Island. Named &quot;Gora Wawel&quot; in 1980 by the Polish Antarctic Expedition after a hill by this name in Kraków, historic site of the castle of the Polish kings.

Geographic entities mentioned:
surface_form: wawel hill
instance_of: Mountain
coordinates: lat: -62.1167
lon: -58.4
Wawel Hill (Antarctica). aj8d5vx0pml5yj5xvl4lueetxxhx" xml:space="preserve">Wawel Hill is a hill rising to 290 m north of Point Hennequin, on the east side of Admiralty Bay, King George Island. Named &quot;Gora Wawel&quot; in 1980 by the Polish Antarctic Expedition after a hill by this name in Kraków, historic site of the castle of the Polish kings.

Geographic entities mentioned:
surface_form: wawel hill
instance_of: Mountain
coordinates: lat: -62.1167
lon: -58.4
surface_form: george
instance_of: Mountain
coordinates: lat: -67.71667
lon: 50
Flattop Peak is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 1,660 meters (5,446 ft) above East Creek in. The nearest higher neighbor is line parent Howser Peak, to the southeast. History.

Geographic entities mentioned:
surface_form: Howser Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.813889
lon: -116.681111
Flattop Peak. Flattop Peak is a summit in British Columbia, Canada. Description. Flattop is located in The Bugaboos, west of the Bugaboo Glacier along the southern boundary of Bugaboo Provincial Park. Precipitation runoff from Flattop Peak drains east into Bugaboo Creek which is a tributary of the Columbia River; as well as west to Duncan River via East Creek.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: flattop peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.7166
lon: -116.80218
The nearest higher neighbor is line parent Howser Peak, to the southeast. History. The peak's descriptive name was applied by Eaton Cromwell, who made the first ascent of the summit with Peter Kaufmann on August 10, 1930. The mountain's toponym was officially adopted on June 9, 1960, by the Geographical Names Board of Canada. Climate.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Flattop Peak. Flattop Peak is a summit in British Columbia, Canada. Description. Flattop is located in The Bugaboos, west of the Bugaboo Glacier along the southern boundary of Bugaboo Provincial Park. Precipitation runoff from Flattop Peak drains east into Bugaboo Creek which is a tributary of the Columbia River; as well as west to Duncan River via East Creek.

Geographic entities mentioned:
surface_form: flattop peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.7166
lon: -116.80218
Precipitation runoff from Flattop Peak drains east into Bugaboo Creek which is a tributary of the Columbia River; as well as west to Duncan River via East Creek. Flattop Peak is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 1,660 meters (5,446 ft) above East Creek in.

Geographic entities mentioned:
surface_form: flattop peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.7166
lon: -116.80218
The mountain's toponym was officially adopted on June 9, 1960, by the Geographical Names Board of Canada. Climate. Based on the Köppen climate classification, Flattop Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: flattop peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.7166
lon: -116.80218
Sand River, Nova Scotia. Sand River is a community in the Canadian province of Nova Scotia, located in Cumberland County.

Geographic entities mentioned:
surface_form: sand river, nova scotia
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.532222222222224
lon: -64.67861111111111
Sand River, Nova Scotia. Sand River is a community in the Canadian province of Nova Scotia, located in Cumberland County.

Geographic entities mentioned:
surface_form: sand river
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.532222222222224
lon: -64.67861111111111
A second procession was held in Varna at the entrance of the Sea Garden while in Samokov, the public gathered at Zahari Zograf Square. Burundi. In Bujumbura, 35 activists cleared rubbish on the shores of Lake Tanganyika. Canada. Strikes began on 20 September, with &quot;die-in&quot; demonstrations staged in Vancouver and many other cities across the country.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
Provenance, education and training. Eva Backofen was born in Meissen (a short distance down-river of Dresden. When she was not quite three the family moved to Berlin where she grew up and attended primary and middle schools, between 1956 and 1968 in Berlin-Köpenick.

Geographic entities mentioned:
surface_form: river
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
In September 2021, $400,000 of emergency work was approved on the southern bank stopbank. Another proposal for the future of Franz Josef is to relocate the entire town away from the flood danger and the alpine fault to the shore of Lake Mapourika, 10 km north of the town. The estimated cost for this is $300–$600 million, or as high as $1 billion. Demographics.

Geographic entities mentioned:
surface_form: Lake Mapourika
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.316666666667
lon: 170.2
From 1951 through 1961 he directed the Institut Biblique, a pastoral training institute of the Communauté Mennonite au Congo (then Congo Inland Mission) in the Democratic Republic of Congo (then Belgian Congo). The Institute Biblique is also known as the Kalonda Bible Institute and is located at Kalonda Station, just north of Tshikapa on the east bank of the Kasai River.

Geographic entities mentioned:
surface_form: Kasai River
instance_of: Watercourse
countries: Angola
Democratic Republic of the Congo
coordinates: lat: -10.9603
lon: 19.3156
See Döpe. See Döpe is a lake in the Nordwestmecklenburg district in Mecklenburg-Vorpommern, Germany. At an elevation of 38 m, its surface area is 0.77 km2.

Geographic entities mentioned:
surface_form: see döpe
instance_of: Lake
countries: Germany
coordinates: lat: 53.777222222222
lon: 11.530833333333
surface_form: döpe
instance_of: Lake
countries: Germany
coordinates: lat: 53.777222222222
lon: 11.530833333333
The dedicatory inscription in the fresco by Melozzo da Forlì in the Vatican Palace records: &quot;You gave your city temples, streets, squares, fortifications, bridges and restored the Acqua Vergine as far as the Trevi...&quot;
In addition to restoring the aqueduct that provided Rome an alternative to the river water, which had made the city famously unhealthy, he restored or rebuilt over 30 of Rome's dilapidated churches such as San Vitale (1475) and Santa Maria del Popolo, and he added seven new ones.

Geographic entities mentioned:
surface_form: Acqua Vergine
instance_of: Watercourse
countries: Italy
All places marked in the map are linked in the larger full screen map. Overview. The region shown in the map is a part of the undulating uplands bustling with coalmines. The Damodar River, the most important river of the Chota Nagpur Plateau, flows along the southern border. The area beyond the Damodar was once a part of Dhanbad district but was transferred to Bokaro district in 2001.

Geographic entities mentioned:
surface_form: Chota Nagpur Plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
The Dexaroi were the northernmost tribe that belonged to the Chaonian group, one of the three major North-Western Greek-speaking tribes of Epirus. Mount Amyron has been identified by some modern scholars with Mount Tomorr, in present-day Albania. The mountain was probably located in a region that in Roman times was called Dassaretis.

Geographic entities mentioned:
surface_form: Tomorr
instance_of: Mountain
countries: Albania
coordinates: lat: 40.709088888889
lon: 20.141802777778
Geography. The Dexaroi are mentioned as dwelling under mount Amyron, near the Enchelei. The mountain has been identified by some modern scholars with Mount Tomorr, in present-day Albania. The mountain was probably located in a region that in Roman times was called Dassaretis. However, all these hypothetical connections remain uncertain. N. G. L.

Geographic entities mentioned:
surface_form: Tomorr
instance_of: Mountain
countries: Albania
coordinates: lat: 40.709088888889
lon: 20.141802777778
N. G. L. Hammond reconstructed for the period from the 6th century BC a vast northern dominion of the Chaonians in an area which expanded form the Bay of Vlorë in the south to the Korçë Plain in the north and the lakeland area in the east. In particular Hammond located the Dexaroi in a region that stretched from mount Amyron (Tomorr) up to the southern coast of lake Lychnitis (Lake Ohrid).

Geographic entities mentioned:
surface_form: Tomorr
instance_of: Mountain
countries: Albania
coordinates: lat: 40.709088888889
lon: 20.141802777778
surface_form: Lake Ohrid
instance_of: Lake
countries: North Macedonia
Albania
coordinates: lat: 41.03333333333333
lon: 20.716666666666665