Sarmila/GeoWiki-Features huggingface dataset:
He returned with three horses of his own, a saddle, and $200 in gold. Aged 17, while traveling to the Silver Lake-Summer Lake area of Oregon with a survey crew, William first saw the land that later became the Vandevert Ranch. It was a meadow on the Little Deschutes River, surrounded by pine forest, with a view of the Cascade Mountains, particularly Mount Bachelor.

Geographic entities mentioned:
surface_form: Mount Bachelor
instance_of: Mountain
countries: United States
coordinates: lat: 43.979166666667
lon: -121.68833333333
Mount Gurage. Mount Gurage or Zebidar terraria is a mountain located in central Ethiopia. It is the highest point in both the Gurage Zone and the entire Southern Nations, Nationalities, and Peoples' Region. The mountain has a latitude and longitude of and an elevation of 3900 meters above sea level.or 12,300 square feet
To the north is the village of Anige, while to the east is Bu'i.

Geographic entities mentioned:
surface_form: mount gurage
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 8.28333
lon: 38.3833
The mountain has a latitude and longitude of and an elevation of 3900 meters above sea level.or 12,300 square feet
To the north is the village of Anige, while to the east is Bu'i. Mount Gurage is described as part of an upwarped massif, which overlooks the Rift Valley. This massif is composed of layers of silicic lavas and tuffs, except for the summit line which is hidden by the Rift Valley tuffs.

Geographic entities mentioned:
surface_form: mount gurage
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 8.28333
lon: 38.3833
Andelfingen District. Andelfingen District is one of the twelve districts of the German-speaking canton of Zurich, Switzerland. It corresponds to the Zürcher Weinland, bounded by the Rhine to the north and west, by the canton of Thurgau to the east, by Winterthur to the south and by the Irchel to the southwest.

Geographic entities mentioned:
surface_form: Irchel
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.55
lon: 8.5833333333333
The journal &quot;Nature&quot; described Kröpelin as &quot;one of the most devoted Sahara explorers of our time.&quot; According to Siddiq Abd Algadir, president of the Sudanese Geologists' Union in Khartoum and a fellow student with Kröpelin in the 1980s, &quot;Much of what we now know about the geology, the environments and even the people in some of the most remote parts of the Sahara, we really owe to [Stefan Kröpelin] and the expeditions he has led.&quot;
Contrary to other evidence that the Sahara suddenly changed from a wet to dry climate 5,000 years ago, Kröpelin's core samples at Lake Yoa suggests the transition took longer, some 3,000 years from 5,600 to 2,700 BC.

Geographic entities mentioned:
surface_form: Lake Yoa
instance_of: Lake
countries: Chad
coordinates: lat: 19.05719
lon: 20.50634
Kröpelin was instrumental in fighting to have the Lakes of Ounianga in Chad listed as a UNESCO World Heritage Site in 2012. He was actively lobbying to have the Ennedi Plateau added as well that has been inscribed as Africa's 6th mixed Natural and Cultural World Heritage property in July 2016.

Geographic entities mentioned:
surface_form: Lakes of Ounianga
instance_of: Group of lakes
countries: Chad
coordinates: lat: 18.98333333
lon: 20.66666667
Kröpelin was instrumental in fighting to have the Lakes of Ounianga in Chad listed as a UNESCO World Heritage Site in 2012. He was actively lobbying to have the Ennedi Plateau added as well that has been inscribed as Africa's 6th mixed Natural and Cultural World Heritage property in July 2016.

Geographic entities mentioned:
surface_form: Ennedi Plateau
instance_of: Plateau
countries: Chad
coordinates: lat: 17
lon: 23
It is one of the NUTS-2 regions of Switzerland. The Lemanic Arc (French: &quot;Arc lémanique&quot;) is the region on the north side of Lake Léman, stretching out from Geneva to Lausanne and Montreux. Its parts are Geneva, La Côte, Lausanne, Lavaux, La Riviera and le Chablais. The cantons of Geneva and Vaud have a collaboration programme named &quot;Métropole lémanique&quot;.

Geographic entities mentioned:
surface_form: La Côte
instance_of: Plateau
countries: Switzerland
coordinates: lat: 46.46666666666667
lon: 6.333333333333333
Aaron, Malawi. Aaron is a village in the Nkhotakota District of Central Region, Malawi, located on the western shore of Lake Malawi. The town was named after the biblical prophet Aaron, by Christian missionaries.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
Frémont duly ignored the advice and directed the group westward. The Washoe were right in that they were not able to find food or game, and they ended up resorting to eating dogs, horses, and mules just to survive. On February 14, Frémont and his cartographer Charles Preuss made it up Red Lake Peak and became the first recorded white men to see Lake Tahoe in the distance.

Geographic entities mentioned:
surface_form: Red Lake Peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.7141
lon: -119.987
Reissend Nollen. The Reissend Nollen is a mountain peak of the Urner Alps, located on the border between the Swiss cantons of Obwalden and Bern. It lies on the range west of the Titlis, between Engelberg and Gadmen.

Geographic entities mentioned:
surface_form: Titlis
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.771944444444
lon: 8.4377777777778
Reissend Nollen. The Reissend Nollen is a mountain peak of the Urner Alps, located on the border between the Swiss cantons of Obwalden and Bern. It lies on the range west of the Titlis, between Engelberg and Gadmen.

Geographic entities mentioned:
surface_form: reissend nollen
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.766536111111
lon: 8.4009222222222
Biography. Irma Luz Poma Canchumani is the daughter of Agustín Poma and Angélica Canchumani, promoters of the collective memory of the Mantaro Valley in Cochas Grande, a town located a few kilometers from Huancayo that has maintained the tradition of carved art since the beginning of the 20th century.

Geographic entities mentioned:
surface_form: Mantaro Valley
instance_of: Valley
countries: Peru
coordinates: lat: -11.91666667
lon: -75.33333333
In fact, they are more closely allied with the twelve-wired and standardwing birds-of-paradise. There are two agreeable subspecies, though races &quot;geisleri&quot; from the Huon Peninsula and &quot;inversus&quot; from the Weyland Mountains and nearby highlands require more detail to be considered valid subspecies or not. Description.

Geographic entities mentioned:
surface_form: Weyland Mountains
instance_of: Mountain
countries: Indonesia
coordinates: lat: -3.8586111111111
lon: 135.83888888889
New York State Route 90. New York State Route 90 (NY 90) is a north–south state highway in the Finger Lakes region of New York in the United States. All but five of the route's are located in Cayuga County, with the remaining situated in Cortland County. The southern terminus of the route is at an intersection with U.S. Route 11 (US 11) and NY 41 in the village of Homer.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
West of NY 34B, NY 90 crosses west through the residential edges of King Ferry before reaching a junction with Clearview Road (CR 31B), where it turns northwestward through the town of Genoa before leaving the community for the town of Ledyard. Crossing northwest through Ledyard, NY 90 passes numerous farms as it nears the eastern shores of Cayuga Lake. Ledyard to Montezuma.

Geographic entities mentioned:
surface_form: Cayuga Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.68805555555556
lon: -76.70222222222222
This junction marks as the northern terminus of NY 90, which continues north of NY 31 toward Fox Ridge. History. The earliest predecessor to NY 90 was the fifth segment of the Great Western Turnpike, chartered in 1814 to run from Homer to Cayuga Lake. At its western terminus, ferries took travellers to points opposite on the lake.

Geographic entities mentioned:
surface_form: Cayuga Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.68805555555556
lon: -76.70222222222222
NY 90 was assigned as part of the 1930 renumbering of state highways in New York. It originally began at US 11 in the hamlet of Messengerville and passed through Virgil, Cortland to King Ferry, where it ran along the eastern edge of Cayuga Lake to its terminus at NY 31 in Montezuma. In Cortland, NY 90 had an overlap with NY 13 along Tompkins Street from Owego Street to Main Street.

Geographic entities mentioned:
surface_form: Cayuga Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.68805555555556
lon: -76.70222222222222
History. The road alignment was first surveyed in 1890 by London-born engineer Robert Holmes, who later became the Engineer-in-Chief of the Public Works Department. Holmes initially preferred a route starting at Lake Wakatipu and running northwest, but the decision was instead made to start from Te Anau.

Geographic entities mentioned:
surface_form: Lake Wakatipu
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.085
lon: 168.561
Tourist traffic from Queenstown turn onto SH 94 here from. Beyond Mossburn, the road changes name to &quot;Te Anau Mossburn Highway&quot;, and runs underneath a terrace carved by the Ōreti River to the north before passing through more arable farmland and the turnoff to go to Mavora Lakes, one of the locations used in &quot;The Lord of the Rings&quot; film trilogy.

Geographic entities mentioned:
surface_form: Mavora Lakes
instance_of: Group of lakes
countries: New Zealand
coordinates: lat: -45.255555555556
lon: 168.16805555556
Once there, the road swings to the right and becomes &quot;Milford Road&quot;, once outside the town limits the road changes name to &quot;Te Anau Milford Highway&quot;. The road then hugs the shoreline of Lake Te Anau for about 29 km, skirting the edge of the Fiordland National Park until it reaches Te Anau Downs. From Te Anau Downs, the road veers right and joins the Eglinton Valley.

Geographic entities mentioned:
surface_form: Lake Te Anau
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.2
lon: 167.8
From Te Anau Downs, the road veers right and joins the Eglinton Valley. The road then enters the national park (45 km north of Te Anau) and runs parallel to the right side of the Eglinton River for 33 km while it passes through Knobs Flat. A car park at the Mirror Lakes on the northbound side is a popular stopping point for tour buses, as it is roughly halfway between Te Anau and Milford Sound.

Geographic entities mentioned:
surface_form: Mirror Lakes
instance_of: Group of lakes
countries: New Zealand
coordinates: lat: -45.028888888889
lon: 168.01083333333
A car park at the Mirror Lakes on the northbound side is a popular stopping point for tour buses, as it is roughly halfway between Te Anau and Milford Sound. At Cascade Creek, the closest camping ground to Milford Sound, the road emerges onto the shorelines of Lake Gunn and Lake Fergus.

Geographic entities mentioned:
surface_form: Lake Gunn
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.88333333333333
lon: 168.08833333333334
surface_form: Lake Fergus
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.845
lon: 168.111
Following that pass, Milford Road emerges at the upper section of the Hollyford Valley and after turning west descends into that valley to the turn-off point to the Lower Hollyford Road, a gravel road leading north to the start of the Hollyford Track.

Geographic entities mentioned:
surface_form: Hollyford Valley
instance_of: Valley
countries: New Zealand
coordinates: lat: -44.727222222222
lon: 168.12927222222
The Milford Road section began in 1926 when a local Station Owner, started making his own road from Te Anau Downs Harbour south to the Te Anau Hotel, starting a project which turned into the most scenic highway in New Zealand including iconic landmarks the Mirror Lakes, the Avenue of Disappearing Mountain, Lake Gunn, the Key Summit, Mount Christina, Mount Talbot, the Homer Tunnel, The Chasm, Mount Tūtoko and Mitre Peak.

Geographic entities mentioned:
surface_form: Mirror Lakes
instance_of: Group of lakes
countries: New Zealand
coordinates: lat: -45.028888888889
lon: 168.01083333333
surface_form: Lake Gunn
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.88333333333333
lon: 168.08833333333334
surface_form: Mount Christina
instance_of: Mountain
countries: New Zealand
coordinates: lat: -44.793
lon: 168.048
surface_form: Mount Tūtoko
instance_of: Mountain
countries: New Zealand
coordinates: lat: -44.5925
lon: 168.0125
This route is part of the Te Waipounamu Wilderness Area. The Eglinton Mountains above Lake Gunn were used as a location in the Peter Jackson movie &quot;The Fellowship of the Ring&quot; where the actors walk along a mountain path with the Key Summit evident in the distance. The mountains here were also used in the Fellowship of the Ring introduction to represent the Misty Mountains.

Geographic entities mentioned:
surface_form: Lake Gunn
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.88333333333333
lon: 168.08833333333334
Berkatal. Berkatal is a municipality in the Werra-Meißner-Kreis in Hesse, Germany. Location. Berkatal lies in the Meißner-Kaufunger Wald Nature Park at the foot of the Hoher Meißner massif. The river Berka rises within community limits. Neighbouring communities.

Geographic entities mentioned:
surface_form: Hoher Meißner
instance_of: Mountain
countries: Germany
coordinates: lat: 51.207777777778
lon: 9.8472222222222
Awigna, California. Awigna (also, Awiz-na) is a former Tongva-Gabrieleño Native American settlement located at the site of modern-day La Puente High School, in the San Gabriel Valley in Los Angeles County, California.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
Ulendet Crevasses. Ulendet Crevasses is a crevasse field about 7 miles (11 km) long in the Jutulstraumen Glacier, about 15 miles (24 km) northeast of Neumayer Cliffs in Queen Maud Land.

Geographic entities mentioned:
surface_form: Jutulstraumen Glacier
instance_of: Landform
coordinates: lat: -71.5833
lon: -0.5
Refreshment Pavilion. The Refreshment Pavilion is a historic refreshment stand at Houghton's Pond in the Milton portion of Blue Hills Reservation, a Massachusetts state park. Built in 1920, it is one of a series of architect-designed structures built in the park by the Metropolitan District Commission. It was listed on the National Register of Historic Places in 1980. Description and history.

Geographic entities mentioned:
surface_form: Houghton's Pond
instance_of: Lake
countries: United States
coordinates: lat: 42.207222222222
lon: -71.096111111111
It was listed on the National Register of Historic Places in 1980. Description and history. The Refreshment Pavilion is located near the northern shore of Houghton's Pond, a body of water in the southwestern part of the Blue Hills Reservation. It is set south of Hillside Street, the access road for the pond's beach area, which is located east of the pavilion.

Geographic entities mentioned:
surface_form: Houghton's Pond
instance_of: Lake
countries: United States
coordinates: lat: 42.207222222222
lon: -71.096111111111
Neely Henry Lake. Neely Henry Lake is located on the Coosa River near Gadsden, Alabama. The lake was formed by the Neely Henry Dam (high), built in 1966 by Alabama Power Company for hydroelectric power and recreation. Completed on June 2, 1966, the dam and reservoir were named for H. Neely Henry, a senior executive vice-president of Alabama Power.

Geographic entities mentioned:
surface_form: Coosa River
instance_of: Watercourse
countries: United States
coordinates: lat: 32.4862464
lon: -86.2777475
Most are located in Johannesburg, with a smaller community in Cape Town. South Korean tourists generally choose Cape Town as their primary destination, due to the Table Mountain and other famous natural attractions. By 2011, the Korean population of South Africa had grown another 9% to 4,186.

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
A wing at Dovercourt Cottage Hospital – which is now known as the Captain Fryatt Memorial Hospital. – was named in Fryatt's honour. A public house in nearby Parkeston is also named in Captain Fryatt's honour. In Canada, the high Mount Fryatt () was named in 1921 in honour of Captain Fryatt. The high Brussels Peak () was named in honour of his ship. Commemoration.

Geographic entities mentioned:
surface_form: Mount Fryatt
instance_of: Mountain
countries: Canada
coordinates: lat: 52.55
lon: -117.91027777777778
A public house in nearby Parkeston is also named in Captain Fryatt's honour. In Canada, the high Mount Fryatt () was named in 1921 in honour of Captain Fryatt. The high Brussels Peak () was named in honour of his ship. Commemoration. In 2016, an exhibition was held from 23 to 31 July at the Masonic Hall, Harwich, to commemorate the 100th anniversary of his execution.

Geographic entities mentioned:
surface_form: Brussels Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.51673
lon: -117.80232
Paleoenvironment. The Ciechocinek Formation represents a shallow brackish to freshwater embayment in the Polish Basin, with lagoonal, deltaic, and marine facies. It spanned the Eastern Bohemian Massif and southwestern Fennoscandian margin, with deltas at Parkoszowice and Brody-Lubienia. Climate was Tropical to subtropical, humid, with perennial rainfall driving kaolinite formation.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Mount Alpenglow is the highest peak alongside Turnagain Arm, and although modest in elevation, relief is significant since the northern aspect of the mountain rises nearly a vertical mile in only one mile from the sea-level shores. The summit of Penguin Peak offers another good view of Alpenglow directly across the arm.

Geographic entities mentioned:
surface_form: Penguin Peak
instance_of: Mountain
countries: United States
coordinates: lat: 60.96527777777778
lon: -149.3752777777778
Mount Alpenglow. Mount Alpenglow is a landmark mountain located in the Kenai Mountains, in the U.S. state of Alaska. The peak is situated in Chugach National Forest, southwest of Girdwood, Alaska, on the south shore of Turnagain Arm, opposite Bird Point from where it can be prominently seen from the Seward Highway and the Alaska Railroad.

Geographic entities mentioned:
surface_form: mount alpenglow
instance_of: Mountain
countries: United States
coordinates: lat: 60.8747
lon: -149.3344
Mount Alpenglow is the highest peak alongside Turnagain Arm, and although modest in elevation, relief is significant since the northern aspect of the mountain rises nearly a vertical mile in only one mile from the sea-level shores. The summit of Penguin Peak offers another good view of Alpenglow directly across the arm.

Geographic entities mentioned:
surface_form: mount alpenglow
instance_of: Mountain
countries: United States
coordinates: lat: 60.8747
lon: -149.3344
Climate. Based on the Köppen climate classification, Mount Alpenglow is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Weather systems coming off the Gulf of Alaska are forced upwards by the Kenai Mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall.

Geographic entities mentioned:
surface_form: mount alpenglow
instance_of: Mountain
countries: United States
coordinates: lat: 60.8747
lon: -149.3344
Wila Qullu is situated in the Sajama Province, in the west of the Curahuara de Carangas Municipality, west of the extinct Sajama volcano and north-east of the Paya Chata mountains. It lies south-west of the mountain Phaq'u Q'awa.

Geographic entities mentioned:
surface_form: Sajama
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.108055555556
lon: -68.883055555556
surface_form: Paya Chata
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -18.15
lon: -69.1333
surface_form: sajama
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.108055555556
lon: -68.883055555556
Wila Qullu (Curahuara de Carangas). Wila Qullu (Aymara &quot;wila&quot; red, blood, &quot;qullu&quot; mountain, &quot;red mountain&quot;, Hispanicized spelling &quot;Wila Kkollu&quot;) is a mountain in the Oruro Department in the Andes of Bolivia, about high.

Geographic entities mentioned:
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.3833
lon: -68.9667
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.51361111
lon: -66.96194444
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -20.3333
lon: -68.65
surface_form: wila qullu (curahuara de carangas)
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.11277778
lon: -69.08805556
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.37833333
lon: -66.68833333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.0833
lon: -66.3333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.9719
lon: -66.3703
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.12694444
lon: -68.27916667
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.7833
lon: -68.8333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -20.97472222
lon: -66.38083333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.67472222
lon: -68.625
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.2953
lon: -69.3989
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.065
lon: -66.3222
Wila Qullu (Curahuara de Carangas). Wila Qullu (Aymara &quot;wila&quot; red, blood, &quot;qullu&quot; mountain, &quot;red mountain&quot;, Hispanicized spelling &quot;Wila Kkollu&quot;) is a mountain in the Oruro Department in the Andes of Bolivia, about high.

Geographic entities mentioned:
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.3833
lon: -68.9667
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.3833
lon: -68.9667
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.51361111
lon: -66.96194444
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.51361111
lon: -66.96194444
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -20.3333
lon: -68.65
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -20.3333
lon: -68.65
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.37833333
lon: -66.68833333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.37833333
lon: -66.68833333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.0833
lon: -66.3333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.0833
lon: -66.3333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.9719
lon: -66.3703
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.9719
lon: -66.3703
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.12694444
lon: -68.27916667
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.12694444
lon: -68.27916667
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.7833
lon: -68.8333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.7833
lon: -68.8333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -20.97472222
lon: -66.38083333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -20.97472222
lon: -66.38083333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.67472222
lon: -68.625
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.67472222
lon: -68.625
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.2953
lon: -69.3989
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.2953
lon: -69.3989
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.065
lon: -66.3222
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.065
lon: -66.3222
Mount Zefachot Trail. This trail ascends Mount Zefachot, where there are several forks leading back down. Nahal Amud Trail. Beginning from Mount Meron, this trail parallels the Israel National Trail and passes pools and ancient flour mills. This trail is a national park with an entry fee, and takes approximately 5 hours to complete. Upper Nahal Yehudiah Trail.

Geographic entities mentioned:
surface_form: Mount Meron
instance_of: Mountain
countries: Mandatory Palestine
Israel
Ottoman Empire
coordinates: lat: 32.9975
lon: 35.41222222222222
This trail loops and is 42 km (26 mi) long and takes approximately two days to complete. Jesus Trail. This trail begins in Nazareth and passes tourist sites related to the life and ministry of Jesus, including Tzippori, the Sea of Galilee, the Horns of Hattin, and several other sites. The trail is a 60 km (40 mi) long and takes approximately 4 days to complete. Israel National Trail.

Geographic entities mentioned:
surface_form: Horns of Hattin
instance_of: Mountain
countries: Israel
coordinates: lat: 32.799722222222
lon: 35.459722222222
Greenwoodochromis christyi. &quot;Greenwoodochromis christyi&quot; is a species of fish in the family Cichlidae. It is endemic to the deeper water of southern Lake Tanganyika. Etymology. The specific name of this fish honours the explorer and naturalist Cuthbert Christy (1863-1932).

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
Rowan's Ravine Provincial Park. Rowan's Ravine Provincial Park is a provincial park in the Canadian province of Saskatchewan. It is on the eastern shore of Last Mountain Lake near a coulee named Rowan's Ravine () in the RM of McKillop No. 220. Highway 220 provides access to the park and the town of Strasbourg is about away. The hamlet of Uhl's Bay is less than a mile away just off of Highway 220.

Geographic entities mentioned:
surface_form: Last Mountain Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.1667
lon: -105.25
The distance to the summit is and will take the average hill climber just under five hours to reach. This makes Seana Bhràigh one of the two most inaccessible Scottish hills, along with A' Mhaighdean, north of Kinlochewe. A ski approach is possible in winter, providing a &quot;superb&quot; run from the summit to Strath Mulzie. Geography and geology.

Geographic entities mentioned:
surface_form: A' Mhaighdean
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.719653
lon: -5.346721
surface_form: seana bhràigh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.84733
lon: -4.89662
Seana Bhràigh. Seana Bhràigh is a mountain east of Ullapool, in the Highlands of Scotland. Ascent. The main approach is from the A835 road through the Lael Forest then over the Coire an Lochain Sgeirich ridge at the head of Gleann a' Mhadaidh. The base of the hill is then reached across pathless boggy terrain, keeping the cliffs of Cadha Dearg to the north.

Geographic entities mentioned:
surface_form: seana bhràigh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.84733
lon: -4.89662
Lake Algonquin was a prehistoric proglacial lake that existed in east-central North America at the time of the last ice age. Parts of the former lake are now Lake Huron, Georgian Bay, Lake Superior, Lake Michigan, Lake Nipigon, and Lake Nipissing. The lake varied in size, but it was at its biggest during the post-glacial period and gradually shrank to the current Lake Huron and Georgian Bay.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: Lake Nipissing
instance_of: Lake
countries: Canada
coordinates: lat: 46.283333333333
lon: -80
Lake Algonquin was a prehistoric proglacial lake that existed in east-central North America at the time of the last ice age. Parts of the former lake are now Lake Huron, Georgian Bay, Lake Superior, Lake Michigan, Lake Nipigon, and Lake Nipissing. The lake varied in size, but it was at its biggest during the post-glacial period and gradually shrank to the current Lake Huron and Georgian Bay.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Physiography. About 11,000 years before present, the Laurentian Glacier had retreated northward, forming a boundary across the northern edges of Lake Superior and Lake Huron. The water level was at above sea level, creating a single body of water in the three basins of Lake Michigan, Lake Huron and Lake Superior. The lake drained through three outlets, the Chicago Outlet River, the St.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Physiography. About 11,000 years before present, the Laurentian Glacier had retreated northward, forming a boundary across the northern edges of Lake Superior and Lake Huron. The water level was at above sea level, creating a single body of water in the three basins of Lake Michigan, Lake Huron and Lake Superior. The lake drained through three outlets, the Chicago Outlet River, the St.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Early Lake Algonquin. The Early Lake Algonquin covered only part of Lake Huron. It included Saginaw Bay, but did not include Georgian Bay or any of the Lake Michigan or Lake Superior basins. Lake Chicago was in the southern portion of Lake Michigan and Lake Duluth was in the western tip of the Lake Superior basin. Lake water drained through the Port Huron outlet and down the St.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Geography. Graham is near the eastern end of the range beginning at Barkaboom Mountain in Delaware County in the west and centered around the lengthy Mill Brook Ridge. A ridge with two summits known unofficially as East and West Schoolhouse mountains connects Graham with Balsam Lake Mountain, the westernmost High Peak.

Geographic entities mentioned:
surface_form: Barkaboom Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.07176
lon: -74.72016
Geography. Graham is near the eastern end of the range beginning at Barkaboom Mountain in Delaware County in the west and centered around the lengthy Mill Brook Ridge. A ridge with two summits known unofficially as East and West Schoolhouse mountains connects Graham with Balsam Lake Mountain, the westernmost High Peak.

Geographic entities mentioned:
surface_form: Balsam Lake Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0457
lon: -74.5945
surface_form: high peak
instance_of: Mountain
countries: United States
coordinates: lat: 32.70166666666667
lon: -109.87138888888889
surface_form: balsam lake
instance_of: Lake
countries: United States
coordinates: lat: 45.465
lon: -92.4369
surface_form: high peak
instance_of: Mountain
countries: United States
coordinates: lat: 42.1620334
lon: -74.0801381
surface_form: balsam lake
instance_of: Lake
countries: United States
coordinates: lat: 47.53
lon: -93.414166666667
An informal poll of 3500 Club members has found Graham ranks with nearby Eagle as their least favorite summit among the Catskill High Peaks. There are open views west to Balsam Lake Mountain.

Geographic entities mentioned:
surface_form: Balsam Lake Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0457
lon: -74.5945
surface_form: balsam lake
instance_of: Lake
countries: United States
coordinates: lat: 45.465
lon: -92.4369
surface_form: balsam lake
instance_of: Lake
countries: United States
coordinates: lat: 47.53
lon: -93.414166666667
Graham Mountain (New York). Graham Mountain is the seventh highest of the Catskill High Peaks and the highest privately owned mountain in the range. It is located in the town of Hardenburgh, New York, United States.

Geographic entities mentioned:
surface_form: graham mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.70166666666667
lon: -109.87138888888889
surface_form: graham mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0393
lon: -74.5496
Graham Mountain (New York). Graham Mountain is the seventh highest of the Catskill High Peaks and the highest privately owned mountain in the range. It is located in the town of Hardenburgh, New York, United States.

Geographic entities mentioned:
surface_form: graham mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.70166666666667
lon: -109.87138888888889
surface_form: graham mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0393
lon: -74.5496
surface_form: high peaks
instance_of: Mountain
countries: United States
coordinates: lat: 45
lon: -70.4
The summit itself is covered with a pygmy forest, unique in the Catskills, with its black cherry and mountain ashes barely taller than average human height. Balsam fir, which dominates the summits of both Doubletop and Balsam Lake mountains to either side of Graham, is found in small stands on the slopes below the summit of Graham.

Geographic entities mentioned:
surface_form: balsam lake
instance_of: Lake
countries: United States
coordinates: lat: 45.465
lon: -92.4369
surface_form: balsam lake
instance_of: Lake
countries: United States
coordinates: lat: 47.53
lon: -93.414166666667
Access. The most frequent route to the summit follows the Dry Brook Ridge Trail from the Mill Brook Road crossing, the highest trailhead in the Catskills at. Hikers follow the blue-blazed trail, the old jeep road to the Balsam Lake Mountain fire tower, to where the unblazed Old Tappan Road, a relocated stretch of the Turner Hollow Road, forks off to the left at an elevation of.

Geographic entities mentioned:
surface_form: balsam lake
instance_of: Lake
countries: United States
coordinates: lat: 45.465
lon: -92.4369
surface_form: balsam lake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0457
lon: -74.5945
surface_form: balsam lake
instance_of: Lake
countries: United States
coordinates: lat: 47.53
lon: -93.414166666667
Other access routes include a bushwhack approach from the Seager-Big Indian Trail along Dry Brook; this usually is combined with an ascent of Doubletop. It also has been hiked in combination with Balsam Lake, for which the hike sometimes begins from the south, at the end of Beaverkill Road north of Quaker Clearing. A direct off-trail hike from there is also possible.

Geographic entities mentioned:
surface_form: balsam lake
instance_of: Lake
countries: United States
coordinates: lat: 45.465
lon: -92.4369
surface_form: balsam lake
instance_of: Lake
countries: United States
coordinates: lat: 47.53
lon: -93.414166666667
Known as Furlow Lodge, it still is owned by the Gould descendants and serves as a family retreat. The south slopes, up to almost on the summit ridge's southwest spur, are publicly owned Forest Preserve in the Big Indian-Beaverkill Range Wilderness Area. Flora and fauna. Most of Graham's slopes, given their high base elevation, are covered in northern hardwood forest of beech, birch and maple.

Geographic entities mentioned:
surface_form: big indian
instance_of: Mountain
countries: United States
coordinates: lat: 37.020833333333
lon: -110.09222222222
There are open views west to Balsam Lake Mountain. Rough use paths lead along the ridge through the pygmy forest to views over the Dry Brook valley and Big Indian, Eagle and Fir mountains to the northwest, and Doubletop and the Beaver Kill's headlands to the southeast.

Geographic entities mentioned:
surface_form: big indian
instance_of: Mountain
countries: United States
coordinates: lat: 37.020833333333
lon: -110.09222222222
Rough use paths lead along the ridge through the pygmy forest to views over the Dry Brook valley and Big Indian, Eagle and Fir mountains to the northwest, and Doubletop and the Beaver Kill's headlands to the southeast. Other access routes include a bushwhack approach from the Seager-Big Indian Trail along Dry Brook; this usually is combined with an ascent of Doubletop.

Geographic entities mentioned:
surface_form: big indian
instance_of: Mountain
countries: United States
coordinates: lat: 37.020833333333
lon: -110.09222222222
The old relay station, a one-story cinderblock structure with no remaining roof and the three steel supports that can be seen from various viewpoints in the area near the mountain, is at the center of a large clearing. An informal poll of 3500 Club members has found Graham ranks with nearby Eagle as their least favorite summit among the Catskill High Peaks.

Geographic entities mentioned:
surface_form: high peaks
instance_of: Mountain
countries: United States
coordinates: lat: 45
lon: -70.4
Dobongsan. Dobongsan () is a mountain in Bukhansan National Park, South Korea. It extends across Seoul, the national capital, and the cities of Yangju and Uijeongbu, in the province of Gyeonggi Province. It has an elevation of. Nearby Dobongsan Station is named after it. It is known for the magnificent rock formations of the Manjangbong, Seoninbong, Jubong, Obong and Uiambong Peaks.

Geographic entities mentioned:
surface_form: bukhansan
instance_of: Mountain
countries: South Korea
coordinates: lat: 37.660833333333
lon: 126.99333333333
surface_form: dobongsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 37.700555555556
lon: 127.01555555556
Dobongsan. Dobongsan () is a mountain in Bukhansan National Park, South Korea. It extends across Seoul, the national capital, and the cities of Yangju and Uijeongbu, in the province of Gyeonggi Province. It has an elevation of. Nearby Dobongsan Station is named after it. It is known for the magnificent rock formations of the Manjangbong, Seoninbong, Jubong, Obong and Uiambong Peaks.

Geographic entities mentioned:
surface_form: dobongsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 37.700555555556
lon: 127.01555555556
In 1983, HMAS &quot;Moresby&quot;, a Royal Australian Navy survey ship, surveyed the area where &quot;Muirfield&quot; was damaged, and charted in detail a previously unsuspected hazard to navigation, the Muirfield Seamount.

Geographic entities mentioned:
surface_form: Muirfield Seamount
instance_of: Mountain
coordinates: lat: -13.225
lon: 96.125
Aland placed it in Category V. It was not examined by the Claremont Profile Method. History. Formerly the manuscript was held in the Iberian monastery at Athos peninsula. It was brought to Moscow, by the monk Arsenius, on the suggestion of the Patriarch Nikon, in the reign of Alexei Mikhailovich Romanov (1645-1676). The manuscript was collated by C. F. Matthaei.

Geographic entities mentioned:
surface_form: Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
During the preceding Last Glacial Maximum, the Sahara contained extensive dune fields and was mostly uninhabited. It was much larger than today, and its lakes and rivers such as Lake Victoria and the White Nile were either dry or at low levels. The humid period began about 14,600–14,500 years ago at the end of Heinrich event 1, simultaneously to the Bølling–Allerød warming.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Research history. In 1850 the researcher Heinrich Barth discussed the possibility of past climate change leading to increased wetness in the Sahara after discovering petroglyphs in the Murzuq Desert, as did Ahmed Hassanein following his 1923 exploration of the Libyan Desert when he saw depictions of savanna animals at Gabal El Uweinat.

Geographic entities mentioned:
surface_form: Gabal El Uweinat
instance_of: Mountain
countries: Libya
Egypt
Sudan
coordinates: lat: 21.919444444444
lon: 24.922222222222
Exceptional dry phases are linked to Heinrich events when there are a large number of icebergs in the North Atlantic; the discharge of large amounts of such icebergs between 11,500 and 21,000 years before present coincided with droughts in the subtropics. Before the onset of the AHP, it is thought that Lake Victoria, Lake Albert, Lake Edward, Lake Turkana and the Sudd swamps had dried out.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
surface_form: Lake Edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
The Nile Delta was partially dry, with sandy plains extending between ephemeral channels and exposed seafloor, and it became a source of sand for ergs farther east. Other lakes across Africa, such as Lake Chad and Lake Tanganyika, also had shrunk during this time, and both the Niger River and Senegal River were stunted. Early humidity increases.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
In southern and central Africa earlier starts 17,000 and 17,500 years ago, respectively, may be linked to Antarctic warming, while Lake Malawi appears to have been low until about 10,000 years ago.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
The terrestrial system (e.g groundwater bodies) took time to respond to changed conditions. Lake Victoria reappeared and overflowed; Lake Albert also overflowed into the White Nile 15,000–14,500 years ago and so did Lake Tana, into the Blue Nile. The White Nile flooded part of its valley and reconnected to the main Nile.

Geographic entities mentioned:
surface_form: Lake Tana
instance_of: Lake
countries: Ethiopia
coordinates: lat: 12
lon: 37.25
Even earlier, 17,000–16,800 years ago, meltwater from glaciers in Ethiopia – which were retreating at that time – may have begun to increase the flow of water and sediment in the Nile. In the East African Rift water levels in lakes began to rise by about 15,500/15,000-12,000 years ago; Lake Kivu began overflowing into Lake Tanganyika by about 10,500 years ago.

Geographic entities mentioned:
surface_form: Lake Kivu
instance_of: Lake
countries: Democratic Republic of the Congo
Rwanda
coordinates: lat: -1.8530555555556
lon: 29.135277777778
An early Holocene monsoonal episode extended as far as the Mojave Desert in North America. In contrast, a drier episode is recorded from much of South America where Lake Titicaca, Lake Junin, the discharge of the Amazon River and water availability in the Atacama were lower. The discharge of the Congo, Niger, Nile, Ntem, Rufiji, and Sanaga rivers increased.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
surface_form: Lake Junin
instance_of: Lake
countries: Peru
coordinates: lat: -11.0201
lon: -76.1075
In contrast, a drier episode is recorded from much of South America where Lake Titicaca, Lake Junin, the discharge of the Amazon River and water availability in the Atacama were lower. The discharge of the Congo, Niger, Nile, Ntem, Rufiji, and Sanaga rivers increased. Runoff from Algeria, equatorial Africa, northeastern Africa and the western Sahara was also larger.

Geographic entities mentioned:
surface_form: Sanaga
instance_of: Watercourse
countries: Cameroon
coordinates: lat: 3.5593388888889
lon: 9.652175
It influenced the climate itself; for example rainfall would have been reduced at the centre of the lake and increased at its margins. Lake Chad was possibly fed from the north by rivers draining the Hoggar (Taffassasset drainage) and Tibesti Mountains, from the Ennedi Mountains in the east through the &quot;Eastern palaeorivers&quot; and from the south by the Chari-Logone and Komadugu Rivers.

Geographic entities mentioned:
surface_form: Ennedi Mountains
instance_of: Plateau
countries: Chad
coordinates: lat: 17
lon: 23
surface_form: Logone
instance_of: Watercourse
countries: Cameroon
Central African Republic
Chad
coordinates: lat: 12.106111111111
lon: 15.035277777778
Skeletons of elephants, hippos and hominins have been found in the Angamma delta, which is the dominant shoreline feature of northern Lake Chad. The lake overflowed into the Niger River during highstand through the Mayo Kebbi and the Benue River, eventually reaching the Gulf of Guinea. Older dune systems were submerged by Lake Chad.

Geographic entities mentioned:
surface_form: Benue River
instance_of: Watercourse
countries: Cameroon
Nigeria
coordinates: lat: 7.783333
lon: 6.766667
The lake overflowed into the Niger River during highstand through the Mayo Kebbi and the Benue River, eventually reaching the Gulf of Guinea. Older dune systems were submerged by Lake Chad. Among the large lakes which may have formed in the Sahara are Lake Megafezzan in Libya and Lake Ptolemy in Sudan.

Geographic entities mentioned:
surface_form: Lake Ptolemy
instance_of: Lake
countries: Sudan
coordinates: lat: 19.5
lon: 26
Other lakes are known from Adrar Bous in Niger, Era Kohor and Trou au Natron in the Tibesti Mountains, I-n-Atei in the Hoggar, at Ine Sakane and in Taoudenni in Mali, the Garat Ouda and Takarkori Lakes in the Acacus Mountains, Chemchane in Mauretania, at Guern El Louläilet in the Great Western Erg and Sebkha Mellala close to Ouargla, both in Algeria, at Wadi Shati and elsewhere in the Fezzan in Libya, at Bilma, Dibella, Fachi and Gobero in the Ténéré, in Niger and at &quot;Eight Ridges&quot;, El Atrun, Lake Gureinat, Merga, &quot;Ridge&quot;, Sidigh, Wadi Mansurab, Selima and Oyo in Sudan.

Geographic entities mentioned:
surface_form: Adrar Bous
instance_of: Mountain
countries: Niger
coordinates: lat: 20.37083333
lon: 9.025
surface_form: Trou au Natron
instance_of: Mountain
countries: Chad
coordinates: lat: 20.975
lon: 16.5675
The lakes of Ounianga merged into two large lakes and overflowed, either above surface or underground. Mosaics of small lakes developed in some regions, such as the Grand Erg Occidental. Wetlands also expanded during the AHP, but both their expansion and subsequent retreat were slower than that of lakes.

Geographic entities mentioned:
surface_form: lakes of Ounianga
instance_of: Group of lakes
countries: Chad
coordinates: lat: 18.98333333
lon: 20.66666667