Sarmila/GeoWiki-Features huggingface dataset:
The mangroves along the low, alluvial coast that stretches over from Cabo Corrientes into Esmeraldas Province are the largest mangrove area in northwest South America, forming the tidal fringe of the coastal plain wide. There are large river deltas at the mouths of the Mataje, Mira, Patía, Sanquianga and Guapi rivers, and smaller deltas at the mouths of about 25 smaller rivers.

Geographic entities mentioned:
surface_form: Mataje
instance_of: Watercourse
countries: Ecuador
Colombia
coordinates: lat: 1.46958
lon: -78.8687
It is also one of the westernmost points in Europe after Iceland, and Azores. However, there are some exposed rocks further west: Tearaght Rocks, Tearaght Rocks West (10° 41.0'), and Foze Rocks (10° 41.3'). An Tiaracht is about a kilometre from east to west, and from north to south. The island is divided into two sections, a larger eastern part (high) and a western part that rises to.

Geographic entities mentioned:
surface_form: an tiaracht
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.075683333333
lon: -10.661283333333
Tearaght Island. Tearaght Island or Inishtearaght (, meaning 'the westerly') is an uninhabited steep rocky island west of the Dingle Peninsula in County Kerry, Ireland. Geography. At longitude 10° 39.7' Tearaght is the westernmost of the Blasket Islands, and thus the westernmost island of Ireland. It is also one of the westernmost points in Europe after Iceland, and Azores.

Geographic entities mentioned:
surface_form: inishtearaght
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.075683333333
lon: -10.661283333333
surface_form: tearaght
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.075683333333
lon: -10.661283333333
Leach's storm-petrels have also been found there (but not proved to be breeding) in recent years. The number of auks, especially puffins, has apparently fluctuated greatly, though early records are not always reliable. Inishtearaght Lighthouse. A lighthouse was established on the island in 1870, and automated in 1988.

Geographic entities mentioned:
surface_form: inishtearaght
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.075683333333
lon: -10.661283333333
Tearaght Island. Tearaght Island or Inishtearaght (, meaning 'the westerly') is an uninhabited steep rocky island west of the Dingle Peninsula in County Kerry, Ireland. Geography. At longitude 10° 39.7' Tearaght is the westernmost of the Blasket Islands, and thus the westernmost island of Ireland. It is also one of the westernmost points in Europe after Iceland, and Azores.

Geographic entities mentioned:
surface_form: tearaght
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.075683333333
lon: -10.661283333333
It is also one of the westernmost points in Europe after Iceland, and Azores. However, there are some exposed rocks further west: Tearaght Rocks, Tearaght Rocks West (10° 41.0'), and Foze Rocks (10° 41.3'). An Tiaracht is about a kilometre from east to west, and from north to south. The island is divided into two sections, a larger eastern part (high) and a western part that rises to.

Geographic entities mentioned:
surface_form: tearaght
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.075683333333
lon: -10.661283333333
surface_form: tearaght
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.075683333333
lon: -10.661283333333
Although private donations are a major source of support for trail maintenance, they are complemented by government and foundation grants. The Katy Trail is intended to provide an effective way of connecting the various Dallas city parks running from White Rock Lake to the Trinity River Project park system along the Trinity River.

Geographic entities mentioned:
surface_form: White Rock Lake
instance_of: Lake
countries: United States
coordinates: lat: 32.834166666667
lon: -96.722777777778
Ijebu East. Ijebu East is a Local Government Area in Ogun State, Nigeria bordering Lagos State and Lagos Lagoon in the south. Its headquarters are in the town of Ogbere on the A121 highwayat. Ijebu East is the largest LGA by area in Ogun State, with an area of 2,234 km and a population of 110,196 at the 2006 census.

Geographic entities mentioned:
surface_form: Lagos Lagoon
instance_of: Lake
countries: Nigeria
coordinates: lat: 6.5015814
lon: 3.5224915
Halgurd. Halgurd (Arabic: هالكورد, Halkurd) () is the second highest mountain in Iraq, after Cheekha Dar, and the tallest fully within Iraq. Located in Choman district in Northern Erbil Province, Kurdistan Region, Iraq, Halgurd has an elevation of 3,607 metres. Halgurd is surrounded by some high mountain lakes, including Bêrme Sard and Bêrmî Gewre.

Geographic entities mentioned:
surface_form: Cheekha Dar
instance_of: Mountain
countries: Iraq
Iran
coordinates: lat: 36.77528
lon: 44.91861
surface_form: halgurd
instance_of: Mountain
countries: Iraq
coordinates: lat: 36.73416667
lon: 44.8625
Halgurd. Halgurd (Arabic: هالكورد, Halkurd) () is the second highest mountain in Iraq, after Cheekha Dar, and the tallest fully within Iraq. Located in Choman district in Northern Erbil Province, Kurdistan Region, Iraq, Halgurd has an elevation of 3,607 metres. Halgurd is surrounded by some high mountain lakes, including Bêrme Sard and Bêrmî Gewre.

Geographic entities mentioned:
surface_form: halgurd
instance_of: Mountain
countries: Iraq
coordinates: lat: 36.73416667
lon: 44.8625
Located in Choman district in Northern Erbil Province, Kurdistan Region, Iraq, Halgurd has an elevation of 3,607 metres. Halgurd is surrounded by some high mountain lakes, including Bêrme Sard and Bêrmî Gewre. The valley below Halgurd peak and above Nawanda village serves as the summer pasture for nomadic Kurdish pastoralists (rewend).

Geographic entities mentioned:
surface_form: halgurd
instance_of: Mountain
countries: Iraq
coordinates: lat: 36.73416667
lon: 44.8625
It is situated north of Kaslo, on the northern boundary of Purcell Wilderness Conservancy Provincial Park and Protected Area. The nearest higher peak is Mount Hamill, to the southeast. Other nearby peaks include Mount Macbeth, to the northwest, and Archduke Mountain, to the west. The first ascent of Truce Mountain was made August 9, 1916, by Conrad Kain, H. Otto Frind, Elise Hopkins, Albert H.

Geographic entities mentioned:
surface_form: Archduke Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.2999
lon: -116.76886
surface_form: mount macbeth
instance_of: Mountain
countries: Canada
coordinates: lat: 50.38944444444444
lon: -116.76416666666667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mount macbeth
instance_of: Mountain
countries: Canada
coordinates: lat: 50.03777777777778
lon: -122.79694444444445
Truce Mountain. Truce Mountain is a glaciated mountain summit located in the Purcell Mountains of British Columbia, Canada. It is situated north of Kaslo, on the northern boundary of Purcell Wilderness Conservancy Provincial Park and Protected Area. The nearest higher peak is Mount Hamill, to the southeast.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: truce mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.29992
lon: -116.68542
Truce Mountain. Truce Mountain is a glaciated mountain summit located in the Purcell Mountains of British Columbia, Canada. It is situated north of Kaslo, on the northern boundary of Purcell Wilderness Conservancy Provincial Park and Protected Area. The nearest higher peak is Mount Hamill, to the southeast.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: truce mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.29992
lon: -116.68542
The nearest higher peak is Mount Hamill, to the southeast. Other nearby peaks include Mount Macbeth, to the northwest, and Archduke Mountain, to the west. The first ascent of Truce Mountain was made August 9, 1916, by Conrad Kain, H. Otto Frind, Elise Hopkins, Albert H. MacCarthy, Elizabeth MacCarthy, Margaret Stone, Winthrop E. Stone, Mrs. George E. Vincent, and John Vincent.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: truce mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.29992
lon: -116.68542
Stone, Mrs. George E. Vincent, and John Vincent. The mountain's name was officially adopted June 9, 1960, when approved by the Geographical Names Board of Canada. __NOTOC__
Climate. Based on the Köppen climate classification, Truce Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors  below −30 °C.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Stone, Mrs. George E. Vincent, and John Vincent. The mountain's name was officially adopted June 9, 1960, when approved by the Geographical Names Board of Canada. __NOTOC__
Climate. Based on the Köppen climate classification, Truce Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors  below −30 °C.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: truce mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.29992
lon: -116.68542
__NOTOC__
Climate. Based on the Köppen climate classification, Truce Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors  below −30 °C. Precipitation runoff from the mountain and meltwater from its surrounding glaciers drains into tributaries of the Duncan River.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The major river within SJRWMD is the St. Johns River. The two major tributaries are the Econlockhatchee River and the Ocklawaha River. Other major waterways are the St. Marys River, which serves as the boundary between Florida and Georgia; and the Nassau, Ocklawaha, Matanzas, Halifax, and Indian rivers. SJRWMD contains 96 springs and more than 1,400 lakes.

Geographic entities mentioned:
surface_form: Matanzas
instance_of: Landform
countries: United States
coordinates: lat: 29.9138577
lon: -81.2836827
The list membership had grown to over 550, and with an average of 15 to 20 posts per day, the volume of email was large. In February 1995 responsibility for managing the list was taken on by Shoshana Edwards, owner of Books From Bree. The list was moved to SmartDOCS.com in the Santa Clarita Valley of Southern California, where it was run on an Oracle-based server.

Geographic entities mentioned:
surface_form: Santa Clarita Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.398
lon: -118.522
Thunderbolt Trail. The Thunderbolt Trail is a non-lift-served backcountry ski trail on Mt. Greylock, at 3491 feet, the highest point in Massachusetts. It runs from the summit down the east face of the mountain to the base via a trail that drops more than 2000 feet in 1.6 miles.

Geographic entities mentioned:
surface_form: Mt. Greylock
instance_of: Mountain
countries: United States
coordinates: lat: 42.6375
lon: -73.166666666667
Raichberg Transmitter. Raichberg transmitter is a broadcast facility for various FM radio and television programs operated by the Südwestrundfunk (SWR, &quot;Southwest Broadcasting&quot;) on the Raichberg mountain (elevation) in Albstadt, Baden-Württemberg, Germany. It uses a 137 meter (449 ft) guyed steel tube mast as the antenna tower.

Geographic entities mentioned:
surface_form: Raichberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.3056
lon: 8.99306
This province limits to the north with the Atlantic Ocean, to the south with the Caribbean Sea, to the east with the Mona channel and to the west with the provinces of La Romana and El Seibo. The most important river in the province is the Yuma, other rivers of consideration are in Duey, Maimon, Chavon, Anamuya, Sanate and Yonu.

Geographic entities mentioned:
surface_form: Chavon
instance_of: Watercourse
countries: Dominican Republic
coordinates: lat: 18.40007
lon: -68.89697
It is spoken mainly by Fula people, but is also used as a lingua franca by several populations of various origins, throughout Western Africa. One region where it is particularly important as a link language is the Adamawa Plateau of northern Cameroon, which, although largely populated by non-Fula people, was united and ruled by Fula conquerors prior to colonial rule.

Geographic entities mentioned:
surface_form: Adamawa Plateau
instance_of: Plateau
countries: Cameroon
coordinates: lat: 9.8
lon: 14.08333333
Persian remains the lingua franca in Iran, Afghanistan and Tajikistan. Sadri. Sadri, also known as Nagpuri, is a Bihari-group language that functions as the lingua franca of the linguistically diverse Chota Nagpur plateau in India, mainly in the state of Jharkhand. It is frequently used between tribes who have different mother tongues. Some linguists e.g.

Geographic entities mentioned:
surface_form: Chota Nagpur plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
Kinnelon is home to Smoke Rise, a private gated community that describes itself as one of the oldest gated communities in the United States. It includes more than 900 unique homes located on in addition to Lake Kinnelon and Kitty Ann Mountain. In 2012, Forbes.com listed Kinnelon as 462nd in its listing of &quot;America's Most Expensive ZIP Codes&quot;, with a median home price of $630,414.

Geographic entities mentioned:
surface_form: Kitty Ann Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.008583333333334
lon: -74.41633333333334
Splitrock Reservoir is of wilderness, located on the borders of Kinnelon and Rockaway Township. The highest mountain in Kinnelon is Kitty Ann Mountain. Located in Smoke Rise, the mountain offers views of northern New Jersey at an elevation of from the Smoke Rise Tower.

Geographic entities mentioned:
surface_form: Kitty Ann Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.008583333333334
lon: -74.41633333333334
Smoke Rise. Smoke Rise is a private gated residential community established in 1946. It is one of the oldest gated communities in the United States, boasting over 900 unique homes located on in addition to Lake Kinnelon and Kitty Ann Mountain. Fayson Lakes. Fayson Lakes was founded in 1925 around three lakes located in the southeastern corner of the borough.

Geographic entities mentioned:
surface_form: Kitty Ann Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.008583333333334
lon: -74.41633333333334
Ferganastegos. &quot;Ferganastegos&quot; is a dubious genus of stegosaur from the Middle Jurassic (Callovian) Balabansai Formation of Fergana Valley, Kyrgyzstan. The holotype of &quot;Ferganastegos callovicus&quot;, IGB 001, consists of four posterior dorsal vertebrae. Although Averianov et al.

Geographic entities mentioned:
surface_form: Fergana Valley
instance_of: Valley
countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
lon: 71.757777777778
Osteoporosia. &quot;Osteoporosia gigantea&quot; is an informally named theropod, either belonging to Carcharodontosauridae or Megaraptora, from the Kem Kem Group of Morocco. It lacks the requirements to become a valid taxon, thus leaving it as a naked name.

Geographic entities mentioned:
surface_form: Kem Kem Group
instance_of: Mountain
countries: Morocco
coordinates: lat: 30.9
lon: -4
By the time of later French contact, the Five Nations of the &quot;Haudenosaunee&quot;: Mohawk, Onondaga, Oneida, Cayuga, and Seneca, were allied in the Iroquois Confederacy, based in present-day New York. Onondaga settlements extended up along the south shore of Lake Ontario. Both the Huron and Mohawk used the St. Lawrence Valley for hunting grounds and as a path for war parties.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Also carved are many mythical figures. Geography. Varaha Cave Temple is located on the hills of Mahabalipuram town, to the north of the main Mahabalipurm sites of rathas and Shore Temple, on the Coromandel Coast of the Bay of Bengal of the Indian Ocean. Now in the Kanchipuram district, it is approximately from Chennai city (previously Madras) and about from Chengalpattu. History.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Location. The Lowery Glacier flows north from Prince Andrew Plateau, Antarctica, along the east side of the Queen Elizabeth Range to enter Nimrod Glacier. To the north of Softbed Ridges it converges with Robb Glacier, but the two glaciers separate when they reach Taylor Hills. It was named by the New Zealand Geological and Topographical Survey Expedition (1959–60) for J.H.

Geographic entities mentioned:
surface_form: Prince Andrew Plateau
instance_of: Mountain
Location. The Lowery Glacier flows north from Prince Andrew Plateau, Antarctica, along the east side of the Queen Elizabeth Range to enter Nimrod Glacier. To the north of Softbed Ridges it converges with Robb Glacier, but the two glaciers separate when they reach Taylor Hills. It was named by the New Zealand Geological and Topographical Survey Expedition (1959–60) for J.H.

Geographic entities mentioned:
surface_form: Taylor Hills
instance_of: Landform
countries: United States
coordinates: lat: 45.65472
lon: -104.46301
Named by the Northern Party of NZGSAE (1961-62) after the English County and Dukedom of Cornwall. Dorrer Glacier. Glacier just south of Mount Heiser, flowing east into Lowery Glacier from the northeast slopes of the Queen Elizabeth Range. Mapped by the USGS from tellurometer surveys and Navy air photos, 1960-62.

Geographic entities mentioned:
surface_form: Mount Heiser
instance_of: Mountain
coordinates: lat: -82.6667
lon: 162.933
Named by US-ACAN for Egon Dorrer, USARP glaciologist on the Ross Ice Shelf 1962-63 and 1965-66. Heidemann Glacier. Glacier, long, originating close northwest of Mount Damm in the Queen Elizabeth Range and flowing east into Lowery Glacier. Mapped by the USGS from tellurometer surveys and Navy air photos, 1960-62. Named by US-ACAN for Richard P.

Geographic entities mentioned:
surface_form: Mount Damm
instance_of: Mountain
coordinates: lat: -82.6
lon: 162.617
Named for Arthur S. Helm, former Secretary of the Ross Sea Committee, by the NZGSAE (1961-62). Kent Glacier. Glacier which drains the east side of Markham Plateau in the Queen Elizabeth Range and flows east for about to enter Lowery Glacier. Named by the northern party of the NZGSAE (1961-62) after the English county and the Dukedom of Kent. Linehan Glacier.

Geographic entities mentioned:
surface_form: Markham Plateau
instance_of: Landform
coordinates: lat: -82.9333
lon: 161.167
Named by the northern party of the NZGSAE (1961-62) after the English county and the Dukedom of Kent. Linehan Glacier. A glacier, long, flowing northeast from Prince Andrew Plateau along the north side of Turnabout Ridge to enter Lowery Glacier. Named by US-ACAN for French Daniel Linehan, who made seismic soundings of ice thickness from the USS Atka, 1954-55, and in the Ross Sea area, 1955-56.

Geographic entities mentioned:
surface_form: Prince Andrew Plateau
instance_of: Mountain
Named by US-ACAN for French Daniel Linehan, who made seismic soundings of ice thickness from the USS Atka, 1954-55, and in the Ross Sea area, 1955-56. Nottarp Glacier. Small glacier draining eastward into Lowery Glacier just south of Mount Damm in the Queen Elizabeth Range. Mapped by the USGS from tellurometer surveys and Navy air photos, 1960-62. Named by US-AC AN for Klemens J.

Geographic entities mentioned:
surface_form: Mount Damm
instance_of: Mountain
coordinates: lat: -82.6
lon: 162.617
Named by US-AC AN for Klemens J. Nottarp, USARP glaciologist on the Ross Ice Shelf, 1962-63 and 1965-66. Pavlak Glacier. A glacier that drains east from the Queen Elizabeth Range into Lowery Glacier close south of Mount Predoehl. Mapped by the USGS from tellurometer surveys and Navy air photos, 1960-62. Named by US-ACAN for Thomas L. Pavlak, USARP glaciologist at South Pole Station, 1962-63.

Geographic entities mentioned:
surface_form: Mount Predoehl
instance_of: Mountain
coordinates: lat: -82.93333
lon: 163.18333
Named by US-ACAN for Robert W. Rowland, USARP glaciologist at South Pole Station, 1962-63 and 1963-64. Oliver Glacier. Glacier draining the area west and south of Mount Christchurch and entering Lowery Glacier just north of the Taylor Hills. Mapped by the USGS from tellurometer surveys and Navy air photos, 1960-62. Named by US-ACAN for Edward J.

Geographic entities mentioned:
surface_form: Mount Christchurch
instance_of: Mountain
coordinates: lat: -82.4667
lon: 164.167
surface_form: Taylor Hills
instance_of: Landform
countries: United States
coordinates: lat: 45.65472
lon: -104.46301
Named by US-ACAN for Edward J. Oliver, USARP glaciologist at South Pole Station, 1961-62. Robb Glacier. A glacier about long, flowing from Clarkson Peak north along
the east side of Softbed Ridges to the Ross Ice Shelf at Cape Goldie. Named by the expedition after Murray Robb, leader of the NZGSAE (1959-60), who traversed this glacier to reach Lowery Glacier.

Geographic entities mentioned:
surface_form: Clarkson Peak
instance_of: Mountain
coordinates: lat: -83.3167
lon: 164.567
He was also a justice of the peace in later life. The family home was Anley (now a nursing home). Caving. His name is remembered for his involvement in some early explorations of some of the potholes of Ingleborough, especially Gaping Gill and Alum Pot, although the records are sparse.

Geographic entities mentioned:
surface_form: Ingleborough
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.165833333333
lon: -2.3975
It contains grassland, desert, wetland and rock habitats. Description. The Important Bird Area (IBA) has a complicated topography of sparsely vegetated mountain slopes and broad highland valleys containing the large freshwater lakes of Bulunkul, Yashilkul and other wetlands. Its altitude ranges from about 3200 m to 5700 m above sea level.

Geographic entities mentioned:
surface_form: Bulunkul
instance_of: Lake
countries: Tajikistan
coordinates: lat: 37.723055555556
lon: 72.96
surface_form: Yashilkul
instance_of: Lake
countries: Tajikistan
coordinates: lat: 37.75
lon: 72.883333333333
The first sheet is an astronomical calendar, the second sheet contains an unusual &quot;world map&quot;, the third, fourth and fifth sheets compose a typical 14th-century portolan chart (covering Europe, North Africa, the Mediterranean and Black Seas), the sixth, seventh and eighth sheets are specialized charts of the Aegean Sea, Adriatic Sea and Caspian Sea. World map.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Property. The Montrest property has been expanded over the years by the Healy family to straddling Lane Gate, a dirt road climbing into the hills of Philipstown above the village of Nelsonville. The land gently slopes downward, revealing views of the Hudson, Bull Hill and Storm King Mountain to the west. There are a number of buildings on the property.

Geographic entities mentioned:
surface_form: Bull Hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.4383
lon: -73.9556
Caribou Hide, British Columbia. Caribou Hide, also known as Metsantan, is a former community of the Sekani people in the Spatsizi Plateau region of the Stikine Country in northwestern British Columbia, Canada, just northwest of Metsantan Lake.

Geographic entities mentioned:
surface_form: Spatsizi Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.8333
lon: -128.483
He specialised in the characterisation of binary stars using astrometry. Life. Wulff-Dieter Heintz was born in Würzburg, Germany on 3 June 1930. He earned his doctorate in astronomy from the University of Munich in 1953. He did research at the Southern Station on Mount Stromlo in Australia. Peter van de Kamp invited him to the Sproul Observatory to be a visiting professor in 1969.

Geographic entities mentioned:
surface_form: Mount Stromlo
instance_of: Mountain
countries: Australia
coordinates: lat: -35.316666666667
lon: 149.01666666667
Ligonier Valley, Pennsylvania. Ligonier Valley is a valley in Westmoreland County, Pennsylvania, United States. History. Around 1727 the first Native American settlement was made in the Ligonier Valley, near the confluence of Mill Creek and Loyalhanna Creek. The village was still relatively new when the first traders came in 1732.

Geographic entities mentioned:
surface_form: mill creek
instance_of: Watercourse
countries: United States
coordinates: lat: 44.4599675
lon: -89.6412311
surface_form: mill creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.871442
lon: -90.093448
The British troops, under Gen. Forbes and Col. Washington, pressed on after the Ligonier victory; when they arrived at Duquesne, they found the fort afire. The victory at Ligonier was the turning point for the British. They established their own fort, named it for Prime Minister William Pitt, thus giving birth to the city of Pittsburgh. Fort Ligonier functioned for a few more years.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
(Many of the Indians had returned home to prepare for the approaching winter.)
The French and Indians who attacked Fort Ligonier were under the command of DeVitri. They began firing at 11:00 am and the battle lasted until 3:00 pm After a spirited encounter, the French and Indians were beaten off with a heavy loss and they fled back to Duquesne. The British troops, under Gen. Forbes and Col.

Geographic entities mentioned:
surface_form: battle
instance_of: Watercourse
countries: United States
coordinates: lat: 44.9266
lon: -93.0291
Ligonier Valley, Pennsylvania. Ligonier Valley is a valley in Westmoreland County, Pennsylvania, United States. History. Around 1727 the first Native American settlement was made in the Ligonier Valley, near the confluence of Mill Creek and Loyalhanna Creek. The village was still relatively new when the first traders came in 1732.

Geographic entities mentioned:
surface_form: ligonier valley, pennsylvania
instance_of: Valley
countries: United States
coordinates: lat: 40.238
lon: -79.23
Am Faochagach. Am Faochagach (953 m) is a mountain in the Northwest Highlands of Scotland. It is located in Wester Ross, north of the main road to Ullapool. A rounded peak, it is surrounded by moorland and bogs, and a river crossing, which makes the approach to the mountain difficult from the road. However, the ascent itself is simpler.

Geographic entities mentioned:
surface_form: am faochagach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.771801
lon: -4.853899
Alton Bay, New Hampshire. Alton Bay is an unincorporated community in the town of Alton in Belknap County, New Hampshire, United States, and is located on Alton Bay, a cove of Lake Winnipesaukee which forms the southernmost point on the lake. The village is part of the Lakes Region, a popular resort area of the state.

Geographic entities mentioned:
surface_form: Lake Winnipesaukee
instance_of: Lake
countries: United States
coordinates: lat: 43.598888888889
lon: -71.323055555556
Buckingham Lake. Buckingham Lake, commonly referred to as Buckingham Pond or Rafts Pond, is a body of water located in a residential area of Albany, New York. It has a surface area of and a mean depth of three feet. The lake is adjacent to Buckingham Lake Park, a small recreation area with picnic tables and playground equipment.

Geographic entities mentioned:
surface_form: buckingham lake
instance_of: Lake
countries: United States
coordinates: lat: 42.6632
lon: -73.8063
It has a surface area of and a mean depth of three feet. The lake is adjacent to Buckingham Lake Park, a small recreation area with picnic tables and playground equipment. Three fountains help aerate water during the warmer months, while ice-skating often takes place on the lake's frozen surface during the winter. Wildlife at the lake includes ducks, Canada geese and red-winged blackbirds.

Geographic entities mentioned:
surface_form: buckingham lake
instance_of: Lake
countries: United States
coordinates: lat: 42.6632
lon: -73.8063
By the 1830s, traders and fur trappers were working in the region. The Astor family began supporting the latter during the next decade, and John C. Frémont led the first American expedition to the valley in 1843, returning two years later. Prospectors looking for gold in 1860 were disappointed, but named the Mount Sopris that dominates the valley after their leader.

Geographic entities mentioned:
surface_form: Mount Sopris
instance_of: Mountain
countries: United States
coordinates: lat: 39.2632
lon: -107.176
Novo River (Sono River tributary). The Novo River is a river of Tocantins state, Brazil. It is a headwater of the Do Sono River. The river forms to the south of the Jalapão State Park, a fully protected conservation unit created in 2001. It runs north along the west boundary of the park to the point where it meets the Soninho River from the left to form the Do Sono River.

Geographic entities mentioned:
surface_form: Soninho River
instance_of: Watercourse
countries: Brazil
coordinates: lat: -10.181875
lon: -46.935478
Novo River (Sono River tributary). The Novo River is a river of Tocantins state, Brazil. It is a headwater of the Do Sono River. The river forms to the south of the Jalapão State Park, a fully protected conservation unit created in 2001. It runs north along the west boundary of the park to the point where it meets the Soninho River from the left to form the Do Sono River.

Geographic entities mentioned:
surface_form: novo river (sono river tributary)
instance_of: Watercourse
countries: Brazil
coordinates: lat: -10.182454
lon: -46.93558
Novo River (Sono River tributary). The Novo River is a river of Tocantins state, Brazil. It is a headwater of the Do Sono River. The river forms to the south of the Jalapão State Park, a fully protected conservation unit created in 2001. It runs north along the west boundary of the park to the point where it meets the Soninho River from the left to form the Do Sono River.

Geographic entities mentioned:
surface_form: novo river
instance_of: Watercourse
countries: Brazil
coordinates: lat: -10.182454
lon: -46.93558
The park receives around of rain per year, mostly from October to May. At the end of the state road is a lookout onto the Kalalau Valley, once home to thousands of native Hawaiians. The valley was the backdrop for Jack London's short story &quot;Koolau the Leper&quot;. In October it is the home of a festival honoring Queen Emma of Hawaii.

Geographic entities mentioned:
surface_form: Kalalau Valley
instance_of: Valley
countries: United States
coordinates: lat: 22.18
lon: -159.65361111
Ludic language. Ludic, Ludian, or Ludic Karelian (or), is a Finnic language in the Uralic language family or a Karelian dialect. It is transitional between the Olonets Karelian language and the Veps language. It is spoken by 300 Karelians in the Republic of Karelia in Russia, near the southwestern shore of Lake Onega, including a few children. Classification.

Geographic entities mentioned:
surface_form: Lake Onega
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
Kowalewka. Kowalewka is a river of Poland. It flows into the Pasiecka Struga, which terminates in Lake Drużno. Drużno is drained by the Elbląg.

Geographic entities mentioned:
surface_form: Drużno
instance_of: Lake
countries: Poland
coordinates: lat: 54.105
lon: 19.461666666667
Milbrodale, New South Wales. Milbrodale is a village in the Hunter Region of New South Wales, Australia. It is in the local government area of Singleton Council. Description. Milbrodale is set in a rural area 23 kilometres south of Singleton. To the north of Milbrodale is Darkey Creek, while to the east is Wollombi Brook.

Geographic entities mentioned:
surface_form: Hunter Region
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Mount Churchill. Mount Churchill is a dormant volcano in the Saint Elias Mountains and the Wrangell Volcanic Field (WVF) of eastern Alaska. Churchill and its neighbor Mount Bona are both ice-covered volcanoes with Churchill having a caldera just east of its summit. There are sparse outcrops of lava flows and tephra, mostly dacite.

Geographic entities mentioned:
surface_form: Mount Bona
instance_of: Mountain
countries: United States
coordinates: lat: 61.3856
lon: -141.749
Elias Mountains. The Wrangell volcanic field features numerous large shield volcanoes, which are among the largest arc volcanoes on Earth. Mount Drum and other volcanoes in the WVF during the middle Pleistocene had eruptions even larger than the White River Ash eruptions. Mount Churchill and Mount Wrangell are the only volcanoes in the WVF with Holocene eruptions.

Geographic entities mentioned:
surface_form: Mount Drum
instance_of: Mountain
countries: United States
coordinates: lat: 62.1161
lon: -144.638
Elias Mountains. The Wrangell volcanic field features numerous large shield volcanoes, which are among the largest arc volcanoes on Earth. Mount Drum and other volcanoes in the WVF during the middle Pleistocene had eruptions even larger than the White River Ash eruptions. Mount Churchill and Mount Wrangell are the only volcanoes in the WVF with Holocene eruptions.

Geographic entities mentioned:
surface_form: Mount Wrangell
instance_of: Mountain
countries: United States
coordinates: lat: 62.006944444444
lon: -144.01583333333
surface_form: mount churchill
instance_of: Mountain
countries: United States
coordinates: lat: 61.41916666666667
lon: -141.71527777777777
surface_form: wrangell
instance_of: Mountain
countries: United States
coordinates: lat: 62.006944444444
lon: -144.01583333333
An ice core taken in 2002 from the col between Mount Churchill and Mount Bona is the longest non-polar ice core, being long. The ice cores record evidence of volcanic eruptions, including of Katmai, Krakatau, Laki and Tambora, and of climate variations like the Medieval Warm Period and the Little Ice Age.

Geographic entities mentioned:
surface_form: Tambora
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.2452777777778
lon: 117.99277777778
Both were very violent Plinian eruptions with a volcanic explosivity index of 6. Deposits from the eruption were first discovered in 1883 along the upper Yukon River. After Mount Wrangell had been ruled out as its source in 1892, Mount Natazhat was proposed instead as the source vent and in 1965 Mount Bona. Only in 1984 and 1995 was Mount Churchill identified as the source.

Geographic entities mentioned:
surface_form: Mount Natazhat
instance_of: Mountain
countries: United States
coordinates: lat: 61.5219
lon: -141.101
surface_form: mount bona
instance_of: Mountain
countries: United States
coordinates: lat: 61.3856
lon: -141.749
Eastern White River Ash. The eastern White River Ash is better studied and covers a wider area. Its intensity was intermediate between the Mount Mazama eruption and the 1883 eruption of Krakatau. It was more than twice the size of the 1912 Novarupta/Katmai eruption and was ten times larger than the 1991 eruption of Mount Pinatubo.

Geographic entities mentioned:
surface_form: Mount Mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
Eastern White River Ash. The eastern White River Ash is better studied and covers a wider area. Its intensity was intermediate between the Mount Mazama eruption and the 1883 eruption of Krakatau. It was more than twice the size of the 1912 Novarupta/Katmai eruption and was ten times larger than the 1991 eruption of Mount Pinatubo.

Geographic entities mentioned:
surface_form: Novarupta
instance_of: Mountain
countries: United States
coordinates: lat: 58.266666666667
lon: -155.15666666667
Strong westerly winds carried the ash cloud eastward, where it may have mixed with snow as it fell out. The eastern lobe of the White River Ash is thick at distance from Mount Churchill, extending to the Great Slave and Great Bear Lakes. The eastern White River Ash has a color ranging from white to beige.

Geographic entities mentioned:
surface_form: Great Slave
instance_of: Lake
countries: Canada
coordinates: lat: 61.666666666667
lon: -114
surface_form: Great Bear Lake
instance_of: Lake
countries: Canada
coordinates: lat: 66
lon: -121
surface_form: bear lakes
instance_of: Lake
countries: United States
coordinates: lat: 47.64798
lon: -121.485943
Mount Churchill and Mount Bona consist of andesitic lava flows. University Peak is a 8.4 million years old volcanic intrusion, now exposed through erosion. The basement under Mount Bona is formed by a plateau consisting of Permian to Pennsylvanian-age rocks and Tertiary granites; most of Mount Bona may be formed by these nonvolcanic rocks.

Geographic entities mentioned:
surface_form: university peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.3272
lon: -141.785
surface_form: university peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.748
lon: -118.361
Potassium-argon dating has yielded an age of 119,000±17,000 years for a dacite lava close to the summit. The 190,000 years old Sheep Creek tephra sub-unit &quot;F&quot; in Canada and Alaska may have originated at Mount Churchill, but more likely at Mount Drum. The appearance and height of Mount Churchill (and neighbouring Bona) imply that they were constructed in recent time.

Geographic entities mentioned:
surface_form: mount drum
instance_of: Mountain
countries: United States
coordinates: lat: 62.1161
lon: -144.638
surface_form: mount churchill
instance_of: Mountain
countries: United States
coordinates: lat: 61.41916666666667
lon: -141.71527777777777
The collision with the Yakutat Block caused the cessation of subduction, with plate motion now occurring along strike-slip faults like the Denali and Totschunda Faults while subduction continues farther west in the Aleutian megathrust. The intersection of the Totschunda Fault with the Connector and Duke River fault(s) may be the point where magma ascends into Mount Churchill.

Geographic entities mentioned:
surface_form: denali
instance_of: Mountain
countries: United States
coordinates: lat: 63.06916666666667
lon: -151.0063888888889
Gates and J. Lindberg and named in 1965 after the English politician Winston Churchill and is also known as Klutlan Glacier, Churchill-Bona, or White River volcano. Various measurements have yielded summit heights of, or. It is a mountain in a glaciated, rugged mountain massif that rises sharply above the surrounding land. It is the tenth-highest peak in the United States.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
Mount Churchill. Mount Churchill is a dormant volcano in the Saint Elias Mountains and the Wrangell Volcanic Field (WVF) of eastern Alaska. Churchill and its neighbor Mount Bona are both ice-covered volcanoes with Churchill having a caldera just east of its summit. There are sparse outcrops of lava flows and tephra, mostly dacite.

Geographic entities mentioned:
surface_form: mount churchill
instance_of: Mountain
countries: United States
coordinates: lat: 61.41916666666667
lon: -141.71527777777777
Mount Churchill. Mount Churchill is a dormant volcano in the Saint Elias Mountains and the Wrangell Volcanic Field (WVF) of eastern Alaska. Churchill and its neighbor Mount Bona are both ice-covered volcanoes with Churchill having a caldera just east of its summit. There are sparse outcrops of lava flows and tephra, mostly dacite.

Geographic entities mentioned:
surface_form: mount churchill
instance_of: Mountain
countries: United States
coordinates: lat: 61.41916666666667
lon: -141.71527777777777
surface_form: wrangell
instance_of: Mountain
countries: United States
coordinates: lat: 62.006944444444
lon: -144.01583333333
It is the tenth-highest peak in the United States. The mountain is mostly covered by ice hundreds of meters thick, but lava flows with columnar jointing and tephra deposits form outcrops, indicating that Mount Churchill may be a stratovolcano. East of Mount Churchill, below the summit, is a caldera, which forms a flat amphitheater open to the northeast.

Geographic entities mentioned:
surface_form: mount churchill
instance_of: Mountain
countries: United States
coordinates: lat: 61.41916666666667
lon: -141.71527777777777
Alternatively, they could have deposited during floods over the ice, perhaps after an eruption or the breach of a pumice-dammed lake. A pumice mound on the other side of the glacier, from Mount Churchill, was formed by tephra building up on a bedrock bench. It was once considered the vent of the White River Ash. In some places, volcanic ash covers the pumice.

Geographic entities mentioned:
surface_form: mount churchill
instance_of: Mountain
countries: United States
coordinates: lat: 61.41916666666667
lon: -141.71527777777777
It was once considered the vent of the White River Ash. In some places, volcanic ash covers the pumice. The older Mount Bona is southwest of Mount Churchill. With a summit height of above sea level, it is the highest mountain in the Wrangell Mountains and the highest volcano in the Wrangell volcanic field and the United States in general.

Geographic entities mentioned:
surface_form: mount churchill
instance_of: Mountain
countries: United States
coordinates: lat: 61.41916666666667
lon: -141.71527777777777
surface_form: mount bona
instance_of: Mountain
countries: United States
coordinates: lat: 61.3856
lon: -141.749
A snow-covered col at elevation separates the two mountains. Both mountains are covered with about of ice. The Russell and Klutlan Glaciers run along the northern-western and eastern-southern side of Mount Churchill, respectively. The Klutlan Glacier is flanked by moraines and talus deposits. Both glaciers eventually discharge into the White River.

Geographic entities mentioned:
surface_form: mount churchill
instance_of: Mountain
countries: United States
coordinates: lat: 61.41916666666667
lon: -141.71527777777777
The Klutlan Glacier is flanked by moraines and talus deposits. Both glaciers eventually discharge into the White River. Glaciers on the southern flank of Mount Bona discharge into the Chitina River. Ice on Mount Churchill is up to 800, and possibly 1500, years old. Geology. The more than Wrangell volcanic field (WVF) has been active for the past 30 million years in the Wrangell and St.

Geographic entities mentioned:
surface_form: mount churchill
instance_of: Mountain
countries: United States
coordinates: lat: 61.41916666666667
lon: -141.71527777777777
Mount Churchill and Mount Wrangell are the only volcanoes in the WVF with Holocene eruptions. With the exception of Mount Churchill, volcanism in the Wrangell volcanic field has migrated northwestwards and declined as plate configuration changed about 200,000 years ago and subduction ceased. Mount Churchill and Mount Bona consist of andesitic lava flows.

Geographic entities mentioned:
surface_form: mount churchill
instance_of: Mountain
countries: United States
coordinates: lat: 61.41916666666667
lon: -141.71527777777777
surface_form: wrangell
instance_of: Mountain
countries: United States
coordinates: lat: 62.006944444444
lon: -144.01583333333
With the exception of Mount Churchill, volcanism in the Wrangell volcanic field has migrated northwestwards and declined as plate configuration changed about 200,000 years ago and subduction ceased. Mount Churchill and Mount Bona consist of andesitic lava flows. University Peak is a 8.4 million years old volcanic intrusion, now exposed through erosion.

Geographic entities mentioned:
surface_form: mount churchill
instance_of: Mountain
countries: United States
coordinates: lat: 61.41916666666667
lon: -141.71527777777777
surface_form: mount bona
instance_of: Mountain
countries: United States
coordinates: lat: 61.3856
lon: -141.749
The collision with the Yakutat Block caused the cessation of subduction, with plate motion now occurring along strike-slip faults like the Denali and Totschunda Faults while subduction continues farther west in the Aleutian megathrust. The intersection of the Totschunda Fault with the Connector and Duke River fault(s) may be the point where magma ascends into Mount Churchill.

Geographic entities mentioned:
surface_form: mount churchill
instance_of: Mountain
countries: United States
coordinates: lat: 61.41916666666667
lon: -141.71527777777777
Several different rock chemistries contribute to each of the White River Ash lobes, which are otherwise very similar to each other and thus difficult to distinguish. The particles in the eastern lobe are coarser than in the northern and show evidence of two separate chemical trends; the deposits on Mount Churchill match the composition of the eastern lobe.

Geographic entities mentioned:
surface_form: mount churchill
instance_of: Mountain
countries: United States
coordinates: lat: 61.41916666666667
lon: -141.71527777777777
The Wrangell slab left over from the subduction may have stalled in the mantle, and was heated by asthenosphere flowing through a slab window until it melted and gave rise to the Mount Churchill magmas, which thus have an adakitic composition typical for melts derived from subducted basalts at high temperatures.

Geographic entities mentioned:
surface_form: mount churchill
instance_of: Mountain
countries: United States
coordinates: lat: 61.41916666666667
lon: -141.71527777777777
surface_form: wrangell
instance_of: Mountain
countries: United States
coordinates: lat: 62.006944444444
lon: -144.01583333333
Ice cores and climate. Several ice cores have been taken from the Bona-Churchill massif and are an important source of information on the climate of the Pacific Northwest. An ice core taken in 2002 from the col between Mount Churchill and Mount Bona is the longest non-polar ice core, being long.

Geographic entities mentioned:
surface_form: mount churchill
instance_of: Mountain
countries: United States
coordinates: lat: 61.41916666666667
lon: -141.71527777777777
surface_form: mount bona
instance_of: Mountain
countries: United States
coordinates: lat: 61.3856
lon: -141.749
Shallow ice and snow has been used to reconstruct dust composition at the St. Elias Mountains. The Chugach Mountains block the maritime airmasses, leading to a continental climate in the region. Mean annual temperature on Mount Churchill is about. Annually, about of snow water equivalent falls on Mount Churchill. Eruption history.

Geographic entities mentioned:
surface_form: mount churchill
instance_of: Mountain
countries: United States
coordinates: lat: 61.41916666666667
lon: -141.71527777777777
Elias Mountains. The Chugach Mountains block the maritime airmasses, leading to a continental climate in the region. Mean annual temperature on Mount Churchill is about. Annually, about of snow water equivalent falls on Mount Churchill. Eruption history. The age of the Churchill-Bona massif is unknown but Mount Churchill began erupting during the late Pleistocene.

Geographic entities mentioned:
surface_form: mount churchill
instance_of: Mountain
countries: United States
coordinates: lat: 61.41916666666667
lon: -141.71527777777777