Sarmila/GeoWiki-Features huggingface dataset:
Mining on a smaller scale took place in Glenmalure. Ore from these mines was shipped to Ballycorus for processing. The last mine closed in 1957. In 1795, workers felling timber discovered gold near the Aughatinavought River, a tributary of the River Aughrim (since renamed the Goldmines River), that rises on the slopes of Croghan Kinsella mountain.

Geographic entities mentioned:
surface_form: Croghan Kinsella
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.8
lon: -6.3166666666667
P. O. on O'Connell Street and the Industry and Commerce building on Kildare Street in Dublin. Barnacullia, on the slopes of Three Rock Mountain, supplied paving stones to Dublin Corporation, and the quarry at Dalkey supplied granite for Dún Laoghaire Harbour and the Thames Embankment in London. Hydrology. The Wicklow Mountains are the source of several major river systems.

Geographic entities mentioned:
surface_form: Three Rock Mountain
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.245277777778
lon: -6.2391666666667
Since the thin blanket bog peats cannot hold great quantities of water, many of these rivers exhibit a flashy hydrography, filling rapidly after heavy rain. The River Liffey rises between the mountains of Kippure and Tonduff at Liffey Head Bog. One of the major tributaries of the Liffey, the River Dodder, rises nearby on slopes on Kippure.

Geographic entities mentioned:
surface_form: Kippure
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.169397
lon: -6.338322
The River Liffey rises between the mountains of Kippure and Tonduff at Liffey Head Bog. One of the major tributaries of the Liffey, the River Dodder, rises nearby on slopes on Kippure. The King's River rises on Mullaghcleevaun and joins the Liffey near Blessington. The River Vartry rises on the slopes of Djouce mountain.

Geographic entities mentioned:
surface_form: Kippure
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.169397
lon: -6.338322
The River Liffey rises between the mountains of Kippure and Tonduff at Liffey Head Bog. One of the major tributaries of the Liffey, the River Dodder, rises nearby on slopes on Kippure. The King's River rises on Mullaghcleevaun and joins the Liffey near Blessington. The River Vartry rises on the slopes of Djouce mountain.

Geographic entities mentioned:
surface_form: Mullaghcleevaun
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.103627777778
lon: -6.4067222222222
The Glenealo, Glendasan and Annamoe rivers meet to form the Avonmore near Laragh. The Annamoe rises near Sally Gap and is joined by Cloghoge Brook between Lough Tay and Lough Dan and by the River Inchavore in Lough Dan. The Avonbeg rises on Table Mountain and the Three Lakes.

Geographic entities mentioned:
surface_form: Lough Tay
instance_of: Lake
countries: Ireland
coordinates: lat: 53.106013888889
lon: -6.2667638888889
surface_form: Lough Dan
instance_of: Lake
countries: Ireland
coordinates: lat: 53.075436
lon: -6.285918
A second dam was added in 1924 to increase capacity. The River Dodder feeds the two Bohernabreena reservoirs in the northern foothills of the Wicklow Mountains at Glenasmole in County Dublin, which were constructed between 1883 and 1887 to supply water to the townland of Rathmines. The Poulaphouca Reservoir, on the River Liffey near Blessington, was constructed between 1938 and 1940.

Geographic entities mentioned:
surface_form: Glenasmole
instance_of: Valley
countries: Ireland
coordinates: lat: 53.23301
lon: -6.356268
There are also two hydroelectricity plants at Poulaphouca, constructed during the 1940s. A pumped-storage hydroelectricity plant was constructed at Turlough Hill between 1968 and 1974. Water is pumped up from Lough Nanahangan, a natural corrie lake, into an artificial reservoir on Tomaneena mountain and released at times of peak electricity demand. Climate.

Geographic entities mentioned:
surface_form: Turlough Hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.0242
lon: -6.41639
Climate. In common with the rest of Ireland, the Wicklow Mountains experience a temperate oceanic climate with mild, damp summers and cool, wet winters. Annual rainfall reaches on the highest mountains with the more westerly peaks getting the most rainfall (for example, Djouce mountain, in the east, receives approximately, whereas Duff Hill, in the west, receives approximately a year).

Geographic entities mentioned:
surface_form: Duff Hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.11666667
lon: -6.36666667
History. The earliest evidence of human activity in the interior of Wicklow dates to around 4,300 BCE. Passage tombs, from the Neolithic period, are the earliest and most prominent feature of prehistoric Irish civilisation in the Wicklow Mountains. These tombs sit on many of the western and northern summits between Saggart in Dublin and Baltinglass in Wicklow, such as at Seefin and Seefingan.

Geographic entities mentioned:
surface_form: Seefingan
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.192034
lon: -6.3749
Art O'Neill died from exposure during the journey and Red Hugh had several toes amputated due to frostbite. A cross and a plaque to the north of Conavalla mountain mark the place where Art O'Neill perished and an annual walk named the Art O'Neill Challenge is now held following in the two men's footsteps.

Geographic entities mentioned:
surface_form: Conavalla
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.015277777778
lon: -6.4525
The Wicklow Military Road was constructed between 1800 and 1809 and runs from Rathfarnham, County Dublin to Aghavannagh, County Wicklow via Glencree, the Sally Gap and Laragh.

Geographic entities mentioned:
surface_form: Glencree
instance_of: Valley
countries: Ireland
coordinates: lat: 53.17
lon: -6.23
China's increasing levels of pollution have also weakened the soil, causing it to be unusable in many areas. Research of reforested areas of the Loess Plateau has found that the combination of exotic tree species and high-density planting could worsen water shortages. The forests increase the loss of soil moisture content when compared to farmland.

Geographic entities mentioned:
surface_form: Loess Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Geography. Sparta is located at (35.932335, -85.469837), approximately fifteen miles south of Cookeville. The city is situated on the Highland Rim, near the western base of the Cumberland Plateau. The Calfkiller River traverses Sparta north-to-south en route to its confluence with the Caney Fork several miles to the south.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
The power plant is associated with a planned tall concrete double-arch-gravity dam. According to the Georgian government-commissioned and the World Bank-supported study the construction of Namakhvani, Paravani and Khudoni hydro power plants are the most attractive scenarios for the development of Georgia's energy sector. History.

Geographic entities mentioned:
surface_form: Namakhvani
instance_of: Lake
countries: Georgia
coordinates: lat: 42.41972222222222
lon: 42.70277777777778
Bridal Veil Falls is separated from Horseshoe Falls by Goat Island and from American Falls by Luna Island, with both islands situated in New York. Formed by the Niagara River, which drains Lake Erie into Lake Ontario, the combined falls have the highest flow rate of any waterfall in North America that has a vertical drop of more than.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Niagara Falls is northwest of Buffalo, New York, and southeast of Toronto, between the twin cities of Niagara Falls, Ontario, and Niagara Falls, New York. Niagara Falls was formed when glaciers receded at the end of the Wisconsin glaciation (the last ice age), and water from the newly formed Great Lakes carved a path over and through the Niagara Escarpment en route to the Atlantic Ocean.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
The average annual flow rate is. Since the flow is a direct function of the Lake Erie water elevation, it typically peaks in late spring or early summer. During the summer months, at least of water traverse the falls, some 90% of which goes over Horseshoe Falls, while the balance is diverted to hydroelectric facilities and then on to American Falls and Bridal Veil Falls.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Scientists posit there is an old valley, St David's Buried Gorge, buried by glacial drift, at the approximate location of the present Welland Canal. When the ice melted, the upper Great Lakes emptied into the Niagara River, which followed the rearranged topography across the Niagara Escarpment. In time, the river cut a gorge through the north-facing cliff, or cuesta.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
Mount Hachimori (Yūbari). is a mountain of the Yūbari Mountains on the border of Minamifurano, Yūbari, Hokkaidō, Japan. It is the source of the Yūbari River.

Geographic entities mentioned:
surface_form: mount hachimori
instance_of: Mountain
countries: Japan
coordinates: lat: 36.086667
lon: 137.754722
surface_form: mount hachimori
instance_of: Mountain
countries: Japan
coordinates: lat: 43.19777778
lon: 142.28416667
The mountain is surrounded by several other notable mountains including Spiterhøi, Skauthøi, Leirhøi, and Veobreahesten to the northwest; Steinbukampen and Veopallan to the northeast; Veotinden to the east; Austre Memurutinden and Blåbreahøe to the southeast; Store Memurutinden to the south; and Nørdre Hellstugutinden, Midtre Hellstugutinden, Store Hellstugutinden, and Nestsøre Hellstugutinden to the southwest.

Geographic entities mentioned:
surface_form: Spiterhøi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.61277778
lon: 8.43861111
surface_form: Skauthøi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.6275
lon: 8.44888889
surface_form: Leirhøi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.591111111111
lon: 8.4669444444444
surface_form: Veobreahesten
instance_of: Mountain
countries: Norway
coordinates: lat: 61.5922
lon: 8.4727805555556
surface_form: Steinbukampen
instance_of: Mountain
countries: Norway
coordinates: lat: 61.6306
lon: 8.54944
surface_form: Veopallan
instance_of: Mountain
countries: Norway
coordinates: lat: 61.6025
lon: 8.54528
surface_form: Veotinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.571944444444
lon: 8.5327777777778
surface_form: Austre Memurutinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.56583333
lon: 8.50777778
surface_form: Blåbreahøe
instance_of: Mountain
countries: Norway
coordinates: lat: 61.5442
lon: 8.55639
surface_form: Store Memurutinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.5675
lon: 8.4880555555556
surface_form: Midtre Hellstugutinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.551388888889
lon: 8.4241666666667
surface_form: Store Hellstugutinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.551388888889
lon: 8.4241666666667
surface_form: nørdre hellstugutinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.56194444
lon: 8.42083333
surface_form: memurutinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.5675
lon: 8.4880555555556
surface_form: memurutinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.5675
lon: 8.4880555555556
surface_form: memurutinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.56583333
lon: 8.50777778
surface_form: memurutinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.56583333
lon: 8.50777778
surface_form: hellstugutinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.551388888889
lon: 8.4241666666667
surface_form: hellstugutinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.551388888889
lon: 8.4241666666667
surface_form: hellstugutinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.551388888889
lon: 8.4241666666667
surface_form: hellstugutinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.551388888889
lon: 8.4241666666667
surface_form: nestsøre hellstugutinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.538333055556
lon: 8.43
Veobretinden. Veobretinden is a mountain in Lom Municipality in Innlandet county, Norway. The tall mountain is located in the Jotunheimen mountains within Jotunheimen National Park. The mountain sits about south of the village of Fossbergom and about southwest of the village of Vågåmo.

Geographic entities mentioned:
surface_form: veobretinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.579722222222
lon: 8.4908333333333
&quot;On the 20th [October 1796] I rode to Messinurte; on the 21st preached here with
uncommon liberty, from Matthew 5 — v. 3. At candle light, I spoke at Br. Hiestand's, from Psalm 44-v. 15. The people here are rather hardened: may God have mercy on them.&quot; &quot;5th [August 1799]—After considerable enquiry and difficult search, I this day arrived at Br.

Geographic entities mentioned:
surface_form: Messinurte
instance_of: Mountain
countries: United States
coordinates: lat: 38.643
lon: -78.612
It is the only land-based accredited university program in the world. Activities. Dechinta is Indigenous-led, and serves Indigenous peoples in Canada at its location near Blachford Lake in Yellowknife, Canada. It is the only land-based accredited university program in the world and has been providing educational services for over ten years.

Geographic entities mentioned:
surface_form: Blachford Lake
instance_of: Lake
countries: Canada
coordinates: lat: 62.168
lon: -112.609
Oravasaari. Oravasaari is a district of Jyväskylä and a village in Central Finland. Before 2009, it was a part of Jyväskylän maalaiskunta. It is located in the southeastern part of Jyväskylä near Toivakka and between the major lakes Päijänne and Leppävesi. The direct distance to central Jyväskylä is about 12 km, while the distance to Vaajakoski is about 10 km. Geography.

Geographic entities mentioned:
surface_form: Leppävesi
instance_of: Lake
countries: Finland
coordinates: lat: 62.25
lon: 25.95
The direct distance to central Jyväskylä is about 12 km, while the distance to Vaajakoski is about 10 km. Geography. Oravasaari is located between the lakes Päijänne and Leppävesi. There is also an island called &quot;Oravasaari&quot; (also called &quot;Manunsaari&quot;) nearby in the Leppävesi, however it is a part of the Leppälahti district.

Geographic entities mentioned:
surface_form: Leppävesi
instance_of: Lake
countries: Finland
coordinates: lat: 62.25
lon: 25.95
The summit elevation is, making it the highest mountain in the Southern Uplands and southern Scotland. Line of sight. The view between Merrick and Snowdon is the longest line of sight in the British Isles. Although theoretically visible, looking from S-N, Merrick is almost entirely obscured by Lamachan Hill and as such, confirmed sightings are very rare. Granite boulders.

Geographic entities mentioned:
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
surface_form: snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
The summit elevation is, making it the highest mountain in the Southern Uplands and southern Scotland. Line of sight. The view between Merrick and Snowdon is the longest line of sight in the British Isles. Although theoretically visible, looking from S-N, Merrick is almost entirely obscured by Lamachan Hill and as such, confirmed sightings are very rare. Granite boulders.

Geographic entities mentioned:
surface_form: Lamachan Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.062747
lon: -4.451544
surface_form: merrick
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.139271
lon: -4.468411
Walking. The shortest route of ascent is from the car park in Glen Trool. The car park is located near &quot;Bruce's Stone&quot;, a monument commemorating the victory of Robert the Bruce over the English forces of Edward II at the Battle of Glen Trool in 1307. The Merrick is a relatively straightforward and easy hike from the car park near Bruce's Stone.

Geographic entities mentioned:
surface_form: Glen Trool
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.081
lon: -4.51
The Merrick is a relatively straightforward and easy hike from the car park near Bruce's Stone. The route climbs past the Culsharg bothy then up on to Benyellary. After dropping slightly the final climb to the summit trig-point is made. Be aware that if descending in poor visibility a very common mistake is to walk down the west ridge into remote terrain.

Geographic entities mentioned:
surface_form: Benyellary
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.1241
lon: -4.4874
Merrick (Galloway). The Merrick (from Gaelic &quot;meurag&quot;, &quot;fingered, knucked&quot;) is a mountain in the Range of the Awful Hand, a sub-range of the Galloway Hills range, part of the Southern Uplands of Scotland. The summit elevation is, making it the highest mountain in the Southern Uplands and southern Scotland. Line of sight.

Geographic entities mentioned:
surface_form: merrick (galloway)
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.139271
lon: -4.468411
Merrick (Galloway). The Merrick (from Gaelic &quot;meurag&quot;, &quot;fingered, knucked&quot;) is a mountain in the Range of the Awful Hand, a sub-range of the Galloway Hills range, part of the Southern Uplands of Scotland. The summit elevation is, making it the highest mountain in the Southern Uplands and southern Scotland. Line of sight.

Geographic entities mentioned:
surface_form: merrick
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.139271
lon: -4.468411
surface_form: the merrick
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.139271
lon: -4.468411
The total round-trip distance from Glen Trool to the summit and back is approximately. Climbing. Because of the nature of the rock, no good rock climbing has been recorded on the Merrick. However, in winter after a good freeze there are a number of good ice climbs of up to 200 m on the Black Gairy, which lies west of the summit.

Geographic entities mentioned:
surface_form: merrick
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.139271
lon: -4.468411
surface_form: the merrick
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.139271
lon: -4.468411
Ali Salalha. Ali Salalha (,; born 12 April 1952) is an Israeli Druze politician who served as a member of the Knesset for Meretz from 2021 to 2022. Early life and education. Salalha's hometown is Beit Jann, a Druze village on Mount Meron in northern Israel. Prior to entering politics, Salalha was the principal of Beit Jann Comprehensive High School. Political career.

Geographic entities mentioned:
surface_form: Mount Meron
instance_of: Mountain
countries: Mandatory Palestine
Israel
Ottoman Empire
coordinates: lat: 32.9975
lon: 35.41222222222222
While residing in the Cayman Islands, he attended Faulkner's Academy in Governor's Harbour and Grace Christian Academy (a school founded by his father) in West Bay, Grand Cayman. As a teen, he attended Los Angeles Baptist High School in the San Fernando Valley. He dropped out of high school in eleventh grade to pursue an acting career. However, he subsequently took college courses at UCLA.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Plot. Set primarily in Aokigahara, a forest at the base of Mount Fuji known as a common site for suicides, the film follows Sara Price, who receives news from Japanese authorities that her twin sister Jess is presumed dead after being seen entering the forest. Despite her fiancé Rob's concern, Sara travels to Japan and checks into the hotel where Jess was last staying.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
The valley passes through high mountains that are covered with snow in the winter season. Maidan is known for its lush green mountains and springs in the summer season. Kumber, being the main village of the Maidan valley, is a big trade centre comprising many commercial markets. People from various villages of the valley come to Kumbar Bazaar to fulfill their daily needs.

Geographic entities mentioned:
surface_form: maidan valley
instance_of: Valley
countries: Pakistan
surface_form: maidan
instance_of: Valley
countries: Pakistan
Maidan, Pakistan. Maidan is a valley in the Lower Dir District of the Khyber Pakhtunkhwa province of Pakistan. The inhabitants of Maidan are mostly Pashtuns. The most numerous tribe living in Maidan is Ismailzai or Samelzai. It is one of the four clans of Tarkani also called Tarkalani tribe.

Geographic entities mentioned:
surface_form: maidan, pakistan
instance_of: Valley
countries: Pakistan
surface_form: maidan
instance_of: Valley
countries: Pakistan
Maidan, Pakistan. Maidan is a valley in the Lower Dir District of the Khyber Pakhtunkhwa province of Pakistan. The inhabitants of Maidan are mostly Pashtuns. The most numerous tribe living in Maidan is Ismailzai or Samelzai. It is one of the four clans of Tarkani also called Tarkalani tribe.

Geographic entities mentioned:
surface_form: maidan
instance_of: Valley
countries: Pakistan
The most numerous tribe living in Maidan is Ismailzai or Samelzai. It is one of the four clans of Tarkani also called Tarkalani tribe. Maidan was not directly under the control of Pakistan government at the time of partition, the valley was governed by a Nawab named &quot;Nawab Shah Jehan&quot;. This region was part of the separate state named &quot;Royal State of the Dir&quot; till the 1960s.

Geographic entities mentioned:
surface_form: maidan
instance_of: Valley
countries: Pakistan
Most of the population of the valley go abroad for earning their livings. Tehsil Maidan has recently been declared a subdivision, which comprises five Union Councils: Lal Qilla, Kotkay, Bashigram, Zaimdara and Gal. There are two police stations in Maidan, namely Lal Qilla and Zaimdara. Religions, language and peoples. The peoples of Maidan are mostly Pashtuns and they speak the Pashto language.

Geographic entities mentioned:
surface_form: maidan
instance_of: Valley
countries: Pakistan
Religions, language and peoples. The peoples of Maidan are mostly Pashtuns and they speak the Pashto language. They are mostly Sunni Muslims. History. Early Maidan was under the Nawab rule. But after 1965, Maidan or Dir became a part of the Islamic Republic of Pakistan. Crops. Wheat, maize, rice and walnuts are common in the region. Politics.

Geographic entities mentioned:
surface_form: maidan
instance_of: Valley
countries: Pakistan
There are other islands in North Dakota, however many are unnamed. Current Islands. List of named islands of North Dakota. Most islands are found in reservoirs including Lake Metigoshe and Lake Sakakawea, which was formed by damming the Missouri River. Former Islands. List of former islands of North Dakota. These islands are historical and do not exist anymore.

Geographic entities mentioned:
surface_form: Lake Metigoshe
instance_of: Lake
countries: United States
Canada
coordinates: lat: 48.9793433
lon: -100.3535643
2021 ICF Canoe Sprint World Championships – Men's C-2 500 metres. The men's C-2 500 metres 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)
Heats. The fastest three boats in each heat advanced directly to the final.

Geographic entities mentioned:
surface_form: Lake Bagsværd
instance_of: Lake
countries: Denmark
coordinates: lat: 55.772222222222
lon: 12.458333333333
The division would later repel a German counteroffensive at Mortain, and pursue the German Army across France, culminating in the Battles of Aachen and the Huertgen Forest. V Corps command. In January 1945 Huebner took command of the V Corps, which he directed from the Rhine to the Elbe, where his troops made first contact with the Red Army. He commanded V Corps until November 11, 1945.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
One was recovered by the US Army, but the other was left in the lake. In 2013, unsuccessful efforts were made to locate the remaining tank. Sources. This article incorporates material from the article 浜名湖 (&quot;Hamanako&quot;) in the Japanese Wikipedia, retrieved on December 11, 2007.

Geographic entities mentioned:
surface_form: hamanako
instance_of: Lake
countries: Japan
coordinates: lat: 34.741111111111
lon: 137.56972222222
Lake Hamana. is a brackish lagoon in Shizuoka Prefecture, Japan. Formerly a true lake, it is now connected to the Pacific Ocean by a channel. As an internal body of water, it is considered Japan's tenth-largest lake (by area). It spans the boundaries of the cities of Hamamatsu and Kosai. Data. The lake has an area of 65.0 km2 and holds 0.35 km3 of water. Its circumference is 114 km.

Geographic entities mentioned:
surface_form: lake hamana
instance_of: Lake
countries: Japan
coordinates: lat: 34.741111111111
lon: 137.56972222222
surface_form: hamana
instance_of: Lake
countries: Japan
coordinates: lat: 34.741111111111
lon: 137.56972222222
The lake has an area of 65.0 km2 and holds 0.35 km3 of water. Its circumference is 114 km. At its deepest point, the water is 16.6 m deep. The surface is at sea level. History. In ancient times, Lake Hamana was a freshwater lake. However, the 1498 Meiō Nankaidō earthquake altered the topography of the area and connected the lake to the ocean. As a result, the water in the lake is now brackish.

Geographic entities mentioned:
surface_form: lake hamana
instance_of: Lake
countries: Japan
coordinates: lat: 34.741111111111
lon: 137.56972222222
surface_form: hamana
instance_of: Lake
countries: Japan
coordinates: lat: 34.741111111111
lon: 137.56972222222
The pass at the head of the river, which connects to the head of the Little Toba River, is the prominence col for Mount Alfred, which lies just west of the river's mouth and is the highest summit between Jervis and Toba Inlets. Above the river's lower reaches, on the east flank of Mount Alfred, is Alfred Creek Falls, one of North America's highest.

Geographic entities mentioned:
surface_form: Mount Alfred
instance_of: Mountain
countries: Canada
coordinates: lat: 50.2061
lon: -124.077
This technique, appropriate for emotionally intense songs for which conventional video lip-syncing would seem especially false, was used by John Mellencamp in parts of the video for his 1985 song &quot;Rain on the Scarecrow&quot;, and by Springsteen himself in the video for his 1987 single &quot;Brilliant Disguise&quot;, singing the song directly into the camera as he sits on the edge of his chair on a Sandy Hook, New Jersey sound stage.

Geographic entities mentioned:
surface_form: Sandy Hook
instance_of: Landform
countries: United States
coordinates: lat: 40.452891
lon: -73.995237
Crn Kamen. Crn Kamen (&quot;Guri i Zi&quot; in Albanian) is a mountain found in Kosovo in the Šar Mountains in Gora next to North Macedonia and Albania. Crn Kamen reaches a top height of. The nearest peaks are Murga and Popova Sapka. The nearest town is Brod, and the nearest lake is Shutman Lake. It is one of the higher peaks in Kosovo.

Geographic entities mentioned:
surface_form: Shutman Lake
instance_of: Lake
countries: Kosovo
coordinates: lat: 41.92027777777778
lon: 20.734166666666667
surface_form: shutman lake
instance_of: Lake
countries: Kosovo
coordinates: lat: 41.92027777777778
lon: 20.734166666666667
Crn Kamen. Crn Kamen (&quot;Guri i Zi&quot; in Albanian) is a mountain found in Kosovo in the Šar Mountains in Gora next to North Macedonia and Albania. Crn Kamen reaches a top height of. The nearest peaks are Murga and Popova Sapka. The nearest town is Brod, and the nearest lake is Shutman Lake. It is one of the higher peaks in Kosovo.

Geographic entities mentioned:
surface_form: murga
instance_of: Mountain
countries: Kosovo
coordinates: lat: 41.937778
lon: 20.618333
Crn Kamen. Crn Kamen (&quot;Guri i Zi&quot; in Albanian) is a mountain found in Kosovo in the Šar Mountains in Gora next to North Macedonia and Albania. Crn Kamen reaches a top height of. The nearest peaks are Murga and Popova Sapka. The nearest town is Brod, and the nearest lake is Shutman Lake. It is one of the higher peaks in Kosovo.

Geographic entities mentioned:
surface_form: crn kamen
instance_of: Mountain
countries: Kosovo
coordinates: lat: 41.891666666666666
lon: 20.689166666666665
Crn Kamen. Crn Kamen (&quot;Guri i Zi&quot; in Albanian) is a mountain found in Kosovo in the Šar Mountains in Gora next to North Macedonia and Albania. Crn Kamen reaches a top height of. The nearest peaks are Murga and Popova Sapka. The nearest town is Brod, and the nearest lake is Shutman Lake. It is one of the higher peaks in Kosovo.

Geographic entities mentioned:
surface_form: crn kamen
instance_of: Mountain
countries: Kosovo
coordinates: lat: 41.891666666666666
lon: 20.689166666666665
surface_form: crn kamen
instance_of: Mountain
countries: Kosovo
coordinates: lat: 41.891666666666666
lon: 20.689166666666665
surface_form: guri i zi
instance_of: Mountain
countries: Kosovo
coordinates: lat: 42.120105
lon: 20.8011297
Dizang of Mount Jiuhua. The Dizang of Mount Jiuhua is a high (including pedestal, and including staff) statue of a standing bodhisattva Kṣitigarbha located in Qingyang County, Chizhou, Anhui Province, China on Mount Jiuhua. It is located in the Huashan Dayuan Cultural Park. As of 2025, it is the fifteenth-tallest statue in the world. History. The statue's construction was completed in 2012.

Geographic entities mentioned:
surface_form: Mount Jiuhua
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 30.482222
lon: 117.804444
It is named after the River Mersey in Liverpool, England. The river proper flows from the eastern end of Eleven Mile Lake in Annapolis County southward to Kejimkujik Lake in Kejimkujik National Park, then through Lake Rossignol to empty into the Atlantic Ocean at the town of Liverpool, Nova Scotia.

Geographic entities mentioned:
surface_form: Kejimkujik Lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.383333333333
lon: -65.25
surface_form: Lake Rossignol
instance_of: Lake
countries: Canada
coordinates: lat: 44.1797
lon: -65.1258
South Park (Park County, Colorado). South Park is a grassland flat within the basin formed by the Rocky Mountains' Mosquito and Rampart Mountain Ranges within central Colorado. This high valley ranges in elevation from approximately 9,000 to 10,000 ft (3,000 m).

Geographic entities mentioned:
surface_form: south park (park county, colorado)
instance_of: Valley
countries: United States
coordinates: lat: 38.96794
lon: -106.04517
South Park (Park County, Colorado). South Park is a grassland flat within the basin formed by the Rocky Mountains' Mosquito and Rampart Mountain Ranges within central Colorado. This high valley ranges in elevation from approximately 9,000 to 10,000 ft (3,000 m).

Geographic entities mentioned:
surface_form: south park
instance_of: Valley
countries: United States
coordinates: lat: 38.96794
lon: -106.04517
Red Hill runs through the center of the valley as a hogback ridge of tilted Cretaceous and Jurassic sedimentary rocks. Gold. Gold mining in South Park began in 1859. Extensive placer deposits were mined along the west side of the park, and lode deposits were mined in the Mosquito Range. The extensive gravel ridges east of Fairplay are the result of dredging for gold.

Geographic entities mentioned:
surface_form: south park
instance_of: Valley
countries: United States
coordinates: lat: 38.96794
lon: -106.04517
(&quot;see Gold mining in Colorado&quot;). Petroleum. Although South Park contains some of the same geologic formations that yield oil and gas in the Denver Basin further east, efforts to find commercial oil and gas in South Park have so far proven unsuccessful. Uranium. A minor amount of uranium has been mined from sandstone in South Park (&quot;see Uranium mining in Colorado&quot;).

Geographic entities mentioned:
surface_form: south park
instance_of: Valley
countries: United States
coordinates: lat: 38.96794
lon: -106.04517
Petroleum. Although South Park contains some of the same geologic formations that yield oil and gas in the Denver Basin further east, efforts to find commercial oil and gas in South Park have so far proven unsuccessful. Uranium. A minor amount of uranium has been mined from sandstone in South Park (&quot;see Uranium mining in Colorado&quot;). Transportation.

Geographic entities mentioned:
surface_form: south park
instance_of: Valley
countries: United States
coordinates: lat: 38.96794
lon: -106.04517
To the west, the extremely high Mosquito Pass crosses the Mosquito Range to Leadville. (Mosquito Pass is no longer a practical transportation route, but is now a historical and recreation site.) On its southwestern side, at the southern end of the Mosquito Range, it is connected by Trout Creek Pass to the upper valley of the Arkansas River near Buena Vista. U.S.

Geographic entities mentioned:
surface_form: south park
instance_of: Valley
countries: United States
coordinates: lat: 38.96794
lon: -106.04517
U.S. Highway 24 enters South Park from the east at Wilkerson Pass, where the highway provides vehicle access to Colorado Springs. To the very south, CO Route 9 crosses Currant Creek Pass, which marks the southern edge of the South Park region. History.

Geographic entities mentioned:
surface_form: south park
instance_of: Valley
countries: United States
coordinates: lat: 38.96794
lon: -106.04517
South Park City, an open-air museum outside Fairplay, provides a historical recreation of the gold rush days. The basin was connected to Denver by railroad with the extension of the Denver, South Park and Pacific Railroad over Kenosha Pass in 1879. In popular culture. Since the late 1990s, South Park has been best-known as the eponymous setting of the animated series &quot;South Park&quot;.

Geographic entities mentioned:
surface_form: south park
instance_of: Valley
countries: United States
coordinates: lat: 38.96794
lon: -106.04517
In popular culture. Since the late 1990s, South Park has been best-known as the eponymous setting of the animated series &quot;South Park&quot;. Trey Parker, one of the creators of the &quot;South Park&quot; series, grew up in Conifer, about 40 miles (65 km) east of Fairplay.

Geographic entities mentioned:
surface_form: south park
instance_of: Valley
countries: United States
coordinates: lat: 38.96794
lon: -106.04517
surface_form: south park
instance_of: Valley
countries: United States
coordinates: lat: 38.96794
lon: -106.04517
It encompasses approximately 1,000 square miles (2,590 km2 or 640,000 acres) around the headwaters of the South Platte River in Park County approximately 60 mi (100 km) southwest of Denver. It is the largest and southernmost of three similarly named high elevation basins in the Front Range of Colorado, the others being North Park and Middle Park.

Geographic entities mentioned:
surface_form: north park
instance_of: Landform
countries: United States
coordinates: lat: 40.81
lon: -106.3
The highway crosses Red Hill at Red Hill Pass. On its northern side, the valley is connected by several high mountain passes to the valley of the North Fork of the South Platte River (a tributary of the South Platte). It is also connected by CO Route 9 via Hoosier Pass to the valley to the Blue River near Breckenridge.

Geographic entities mentioned:
surface_form: high mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0887
lon: -74.2351
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The largest town in the basin is Fairplay, with a population of 724. Geology. Geologically, the valley is a wide faulted syncline of sedimentary rocks, sitting between the predominantly Precambrian igneous rocks of the Front Range to the east and the Sawatch Uplift to the west. The Mosquito Range forms a high barrier along the western side of the valley.

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
Geology. Geologically, the valley is a wide faulted syncline of sedimentary rocks, sitting between the predominantly Precambrian igneous rocks of the Front Range to the east and the Sawatch Uplift to the west. The Mosquito Range forms a high barrier along the western side of the valley. The long-extinct Thirty-Nine Mile volcanic field is located just to the southeast.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The Mosquito Range forms a high barrier along the western side of the valley. The long-extinct Thirty-Nine Mile volcanic field is located just to the southeast. The valley is mostly underlain by Paleozoic and Mesozoic sedimentary rocks concealed by a thin layer of gravel laid down by glaciation during Pleistocene time. The underlying rocks are dipping slightly to the east.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The underlying rocks are dipping slightly to the east. The eastern (and newer) side of the valley is underlain primarily by Pierre Shale laid down during Cretaceous time. The western (and older) side of the valley, on the west side of Red Hill, is underlain primarily by Permian and Pennsylvanian rocks.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The eastern (and newer) side of the valley is underlain primarily by Pierre Shale laid down during Cretaceous time. The western (and older) side of the valley, on the west side of Red Hill, is underlain primarily by Permian and Pennsylvanian rocks. Red Hill runs through the center of the valley as a hogback ridge of tilted Cretaceous and Jurassic sedimentary rocks. Gold.

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: red hill
instance_of: Mountain
countries: United States
coordinates: lat: 37.1252501
lon: -121.194283
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: red hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.924166666667
lon: -74.517777777778
The eastern (and newer) side of the valley is underlain primarily by Pierre Shale laid down during Cretaceous time. The western (and older) side of the valley, on the west side of Red Hill, is underlain primarily by Permian and Pennsylvanian rocks. Red Hill runs through the center of the valley as a hogback ridge of tilted Cretaceous and Jurassic sedimentary rocks. Gold.

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: red hill
instance_of: Mountain
countries: United States
coordinates: lat: 37.1252501
lon: -121.194283
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: hogback
instance_of: Mountain
countries: United States
coordinates: lat: 42.706388888889
lon: -74.465
surface_form: red hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.924166666667
lon: -74.517777777778
Uranium. A minor amount of uranium has been mined from sandstone in South Park (&quot;see Uranium mining in Colorado&quot;). Transportation. The valley is traversed by several highways, including U.S. Highway 285, which enters the valley from the eastern side over the Front Range at Kenosha Pass, providing a vehicle link to Denver. The highway crosses Red Hill at Red Hill Pass.

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
On its northern side, the valley is connected by several high mountain passes to the valley of the North Fork of the South Platte River (a tributary of the South Platte). It is also connected by CO Route 9 via Hoosier Pass to the valley to the Blue River near Breckenridge. To the west, the extremely high Mosquito Pass crosses the Mosquito Range to Leadville.

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
Highway 24 enters South Park from the east at Wilkerson Pass, where the highway provides vehicle access to Colorado Springs. To the very south, CO Route 9 crosses Currant Creek Pass, which marks the southern edge of the South Park region. History. Like much of the mountainous areas of Colorado, the valley was inhabited by Utes before the arrival of European settlers in the middle 19th century.

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
It was explored by John C. Fremont during his second expedition in 1844, at which time it was referred to as &quot;Bayou Salade&quot;, a corruption of Spanish &quot;Valle Salado&quot;, meaning salty valley. In 1859, the discovery of placer gold in the streams of the valley during the Colorado Gold Rush led to an influx of prospectors and miners.

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
Highway 285, which enters the valley from the eastern side over the Front Range at Kenosha Pass, providing a vehicle link to Denver. The highway crosses Red Hill at Red Hill Pass. On its northern side, the valley is connected by several high mountain passes to the valley of the North Fork of the South Platte River (a tributary of the South Platte).

Geographic entities mentioned:
surface_form: red hill
instance_of: Mountain
countries: United States
coordinates: lat: 37.1252501
lon: -121.194283
surface_form: red hill
instance_of: Mountain
countries: United States
coordinates: lat: 37.1252501
lon: -121.194283
surface_form: red hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.924166666667
lon: -74.517777777778
surface_form: red hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.924166666667
lon: -74.517777777778
Farlowella taphorni. &quot;Farlowella taphorni&quot; is a species of armored catfish endemic to Venezuela where it is found in the Torondoy River basin in the Lake Maracaibo drainage. This species grows to a length of SL.

Geographic entities mentioned:
surface_form: Lake Maracaibo
instance_of: Lake
countries: Venezuela
coordinates: lat: 9.8158333333333
lon: -71.556666666667
From the Art Deco period, Montreal offers a handful of notable examples: Ernest Cormier's Université de Montréal main building located on the northern side of Mount Royal and the Aldred Building at Place d'Armes, an historic square in Old Montreal.

Geographic entities mentioned:
surface_form: Mount Royal
instance_of: Mountain
countries: Canada
coordinates: lat: 45.506388888889
lon: -73.588888888889
M. Pei's landmark cruciform Place Ville-Marie, the CIBC Building and CIL House. Its tallest buildings, the 51-storey 1000 de La Gauchetière and the 47-storey 1250 René-Lévesque, were both completed in 1992. Montreal places height-limits on skyscrapers so that they do not exceed 200m in height nor the summit of Mount Royal. Only the St.

Geographic entities mentioned:
surface_form: Mount Royal
instance_of: Mountain
countries: Canada
coordinates: lat: 45.506388888889
lon: -73.588888888889
An old Roman road ran through Bocchetta Pass from Genua (modern Genoa) to Dertona (modern Tortona). The Bocchetta Pass is located about north of Genoa. From the south, the SP5 (Provincial) highway follows the Polcevera valley north from the town of Campomorone. From the north, the SP160 highway approaches the pass along the Lemme valley via the towns of Gavi and Voltaggio.

Geographic entities mentioned:
surface_form: Polcevera valley
instance_of: Valley
countries: Italy
coordinates: lat: 44.44
lon: 8.89
Decapolis. The Decapolis (Greek:) was a group of ten Greek Hellenistic cities on the eastern frontier of the Greek and late Roman Empire in the Southern Levant in the first centuries BC and AD. Most of the cities were located to the east of the Jordan Rift Valley, between Judaea, Iturea, Nabataea, and Syria.

Geographic entities mentioned:
surface_form: Jordan Rift Valley
instance_of: Valley
countries: Jordan
Lebanon
Israel
Syria
State of Palestine
coordinates: lat: 32.317222222222
lon: 35.57