Sarmila/GeoWiki-Features huggingface dataset:
Chuckwalla Valley. The Chuckwalla Valley is a large valley in eastern Riverside County, California, named for a large lizard, the chuckwalla found in the arid Southwestern United States deserts. The region of the valley in southeast California, is the low elevation section of the Mojave Desert transitioning into the Colorado Desert, the northwest extension (in California) of the Sonoran Desert.

Geographic entities mentioned:
surface_form: chuckwalla valley
instance_of: Valley
countries: United States
coordinates: lat: 33.640856
lon: -115.0188589
Geography. The map of California showing the location of Ward Valley, also shows the &quot;low elevation green, low valleys&quot;, south of the 'map location point'. The northwest-by-southeast section, contains the three dry lake beds, from west to east: Bristol Lake, Cadiz Dry Lake, and Danby Lake.

Geographic entities mentioned:
surface_form: ward valley
instance_of: Valley
countries: United States
coordinates: lat: 34.50139
lon: -115.06275
Geographically, the entire region of Ward Valley is a transition from higher elevation bajadas and mountain ranges of the Mojave Desert, to lower elevation sections of Mojave Desert, and the northwest region of the Sonoran Desert in southeast California, called the Colorado Desert.

Geographic entities mentioned:
surface_form: ward valley
instance_of: Valley
countries: United States
coordinates: lat: 34.50139
lon: -115.06275
The region has mostly arid mountain ranges, bajadas, flatlands, sand dune fields (from prevailing, seasonal winds), and playas (salt-flats). The lengthy north section of Ward Valley is drained by one major wash, named Homer Wash. Its outfall end, due to scant rainfall, and distance from Danby Lake, ends about 5-mi from the north side of the lake (ground infiltration).

Geographic entities mentioned:
surface_form: ward valley
instance_of: Valley
countries: United States
coordinates: lat: 34.50139
lon: -115.06275
Chuckwalla Valley. The Chuckwalla Valley is a large valley in eastern Riverside County, California, named for a large lizard, the chuckwalla found in the arid Southwestern United States deserts. The region of the valley in southeast California, is the low elevation section of the Mojave Desert transitioning into the Colorado Desert, the northwest extension (in California) of the Sonoran Desert.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Chuckwalla Valley contains Ford Lake (Ford Dry Lake) in the east-southeast; Palen Lake (Palen Dry Lake) occurs in the center-northwest, at the south terminus of the smaller, north-south Palen Valley. The south end of the valley expands slightly northwest-by-southeast, and contains Danby Dry Lake, a 13-mi (21 km) long dry lake, or playa. Mountain ranges surround the valley on all sides.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The neighboring valleys eastward over the mountain ranges, Chemehuevi Valley, Vidal Valley, and Rice Valley are all western tributary valleys to the south-flowing Colorado River along the Lower Colorado River Valley corridor. The center of the valley is approximately just east of the &quot;Oro Plata Mine&quot; at the east of the Old Woman Mountains. Geography.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The region has mostly arid mountain ranges, bajadas, flatlands, sand dune fields (from prevailing, seasonal winds), and playas (salt-flats). The lengthy north section of Ward Valley is drained by one major wash, named Homer Wash. Its outfall end, due to scant rainfall, and distance from Danby Lake, ends about 5-mi from the north side of the lake (ground infiltration).

Geographic entities mentioned:
surface_form: danby lake
instance_of: Lake
countries: United States
coordinates: lat: 34.2397
lon: -115.148
There are only two of these types of sites in County Kildare (the other being Mouds Bog). The Ballynafagh Bog site is also a proposed National Heritage Area site or pNHA. Close to the Ballynafagh Bog SAC is the Ballynafagh Lake SAC, which is also a pNHA. Features. The Ballynafagh Bog site includes approximately 70 hectares of uncut high bog.

Geographic entities mentioned:
surface_form: Ballynafagh Lake
instance_of: Lake
countries: Ireland
coordinates: lat: 53.3038
lon: -6.7865
Birds. Protected bird species recorded at this site include merlin (&quot;Falco columbarius&quot;), snipe (&quot;Gallinago gallinago&quot;) and curlew (&quot;Numenius arquata&quot;). This Special Area of Conservation is adjacent to the Ballynafagh Lake wildfowl sanctuary and SAC, and likely to be used by the birds of that site. Conservation objectives.

Geographic entities mentioned:
surface_form: Ballynafagh Lake
instance_of: Lake
countries: Ireland
coordinates: lat: 53.3038
lon: -6.7865
Geyser Valley trail. The Geyser Valley trail in Olympic National Park is an area along the Elwha River between Rica Canyon and the Grand Canyon of the Elwha, where many homesteaders tried to eke out a living in the late 19th and early 20th centuries. Today, this trail allows hikers to visit several interesting sites, as well as, providing several loops of different lengths.

Geographic entities mentioned:
surface_form: Grand Canyon of the Elwha
instance_of: Valley
countries: United States
coordinates: lat: 47.9406
lon: -123.54
You can also see 100-year-old fruit trees in the pastures. Approximately 3/4 of a mile further, the trail climbs the eroding cliffs along the river and crosses Dodger point bridge at the mouth of the Grand Canyon of the Elwha. This marks the end of Geyser Valley, but the trail continues for 11 miles up to the summit of Dodger Point Mountain at over 5,700 ft.

Geographic entities mentioned:
surface_form: Grand Canyon of the Elwha
instance_of: Valley
countries: United States
coordinates: lat: 47.9406
lon: -123.54
Noble Peak. Noble Peak () is a peak in the Comer Range, 720 m, standing 1 nautical mile (1.9 km) southwest of Lockley Point and marking the northeast end of a prominent ridge on the northwest side of Wiencke Island, in the Palmer Archipelago. Discovered by the Belgian Antarctic Expedition, 1897–99, under Gerlache.

Geographic entities mentioned:
surface_form: noble
instance_of: Mountain
coordinates: lat: -60.65
lon: -45.2667
surface_form: noble peak
instance_of: Mountain
coordinates: lat: -64.8
lon: -63.4167
Discovered by the Belgian Antarctic Expedition, 1897–99, under Gerlache. The name appears on a chart based on a 1927 survey by DI personnel on the Discovery, but may reflect on earlier naming.

Geographic entities mentioned:
surface_form: discovery
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: discovery
instance_of: Body of water
coordinates: lat: -64.5167
lon: -63.0167
The report was published in the &quot;Bulletin of the Seismological Society of America&quot;, and described, in summary, that a &quot;shallow crustal earthquake close to the city would be most damaging.&quot;
Another publication by Allstadt that received secondary attention was a 2014 study on snow causing earthquakes at Mount Rainier.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
She has also presented at multiple society meetings, such as the 2021 EGU General Assembly and the 2023 SSA Annual Meeting. GeoGirls. Allstadt is the head coordinator and project leader of GeoGirls, a camp program intended to immerse and engage female students with women scientists and researchers with hand-on interaction at Mount St. Helens.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
Mount Strahan is a mountain located on the West Coast Range in the West Coast region of Tasmania, Australia. With an elevation of above sea level, the mountain is situated directly east of Macquarie Harbour and, like Mount Sorell, dominates the east side of the harbour near Sarah Island. The mountain was named by Thomas Bather Moore in honour of Sir George Strahan, a Governor of Tasmania.

Geographic entities mentioned:
surface_form: Mount Sorell
instance_of: Mountain
countries: Australia
coordinates: lat: -42.266666666667
lon: 145.53333333333
Mount Strahan is a mountain located on the West Coast Range in the West Coast region of Tasmania, Australia. With an elevation of above sea level, the mountain is situated directly east of Macquarie Harbour and, like Mount Sorell, dominates the east side of the harbour near Sarah Island. The mountain was named by Thomas Bather Moore in honour of Sir George Strahan, a Governor of Tasmania.

Geographic entities mentioned:
surface_form: george
instance_of: Lake
countries: Australia
coordinates: lat: -35.1667
lon: 149.417
Mount Strahan. Mount Strahan is a mountain located on the West Coast Range in the West Coast region of Tasmania, Australia. With an elevation of above sea level, the mountain is situated directly east of Macquarie Harbour and, like Mount Sorell, dominates the east side of the harbour near Sarah Island.

Geographic entities mentioned:
surface_form: mount strahan
instance_of: Mountain
countries: Australia
coordinates: lat: -42.23333333
lon: 145.51666667
Flatiron (volcano). The Flatiron is the name for an eroded volcanic outcrop in east-central British Columbia, Canada, located in Wells Gray Provincial Park. The Flatiron is high, long and generally about wide. It is flanked by Hemp Creek to the west and Trout Creek to the east. Geology.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: flatiron
instance_of: Mountain
countries: Canada
coordinates: lat: 51.88
lon: -120.05
The surface of the lake was the rim of the Hemp cliffs a few kilometres south of The Flatiron. The lake was created by a blockage downstream on the Clearwater River, but its actual location is unknown, and this could have been an ice dam, a landslide or a lava flow. The Flatiron erupted into this lake and was once much bigger than today. This action is called a ponded lava flow.

Geographic entities mentioned:
surface_form: clearwater river
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.7481
lon: -111.384
Flatiron (volcano). The Flatiron is the name for an eroded volcanic outcrop in east-central British Columbia, Canada, located in Wells Gray Provincial Park. The Flatiron is high, long and generally about wide. It is flanked by Hemp Creek to the west and Trout Creek to the east. Geology.

Geographic entities mentioned:
surface_form: flatiron (volcano)
instance_of: Mountain
countries: Canada
coordinates: lat: 51.88
lon: -120.05
Flatiron (volcano). The Flatiron is the name for an eroded volcanic outcrop in east-central British Columbia, Canada, located in Wells Gray Provincial Park. The Flatiron is high, long and generally about wide. It is flanked by Hemp Creek to the west and Trout Creek to the east. Geology.

Geographic entities mentioned:
surface_form: flatiron
instance_of: Mountain
countries: Canada
coordinates: lat: 51.88
lon: -120.05
The lake bottom was about above the present bottom of the Hemp Creek Valley. The surface of the lake was the rim of the Hemp cliffs a few kilometres south of The Flatiron. The lake was created by a blockage downstream on the Clearwater River, but its actual location is unknown, and this could have been an ice dam, a landslide or a lava flow.

Geographic entities mentioned:
surface_form: flatiron
instance_of: Mountain
countries: Canada
coordinates: lat: 51.88
lon: -120.05
The surface of the lake was the rim of the Hemp cliffs a few kilometres south of The Flatiron. The lake was created by a blockage downstream on the Clearwater River, but its actual location is unknown, and this could have been an ice dam, a landslide or a lava flow. The Flatiron erupted into this lake and was once much bigger than today. This action is called a ponded lava flow.

Geographic entities mentioned:
surface_form: flatiron
instance_of: Mountain
countries: Canada
coordinates: lat: 51.88
lon: -120.05
The Flatiron erupted into this lake and was once much bigger than today. This action is called a ponded lava flow. The lava used to extend right across the Hemp Creek Valley, but floods from melting glaciers carried away the lava and left The Flatiron as a remnant. The water flow might have been 100 times the size of Hemp Creek today.

Geographic entities mentioned:
surface_form: flatiron
instance_of: Mountain
countries: Canada
coordinates: lat: 51.88
lon: -120.05
The water flow might have been 100 times the size of Hemp Creek today. The lava that is exposed today cooled very slowly and formed into columns, one of the park’s finest examples of columnar basalt. The columns that make up the Flatiron have been falling away regularly and piling up at the base, so the Flatiron keeps gets thinner. Access.

Geographic entities mentioned:
surface_form: flatiron
instance_of: Mountain
countries: Canada
coordinates: lat: 51.88
lon: -120.05
surface_form: flatiron
instance_of: Mountain
countries: Canada
coordinates: lat: 51.88
lon: -120.05
Access. A one-hour hike from Clearwater Valley Road (also called Wells Gray Park Road) leads to a viewpoint of the Hemp Canyonlands with the Flatiron in the distance. After another 30 minutes hiking, it is necessary to leave the trail and bushwhack to the base of the Flatiron. As the cliffs almost surround the Flatiron, the only access to the top is a scramble from the west side above Hemp Creek.

Geographic entities mentioned:
surface_form: flatiron
instance_of: Mountain
countries: Canada
coordinates: lat: 51.88
lon: -120.05
Weird Lake. Weird Lake is a natural lake in Cook County, Minnesota, United States. The lake has a surface area of and has a maximum depth of 6ft.

Geographic entities mentioned:
surface_form: weird lake
instance_of: Lake
countries: United States
coordinates: lat: 47.91333333
lon: -90.79027778
These representations are connected to pre-Columbian, European, and religious influences; beings that coexist in these spatiotemporal realms. A prominent example of this tendency is the figure of the Virgin of Legarda, the patroness of Quito, which frequently appears in his works, inspired by the statue atop the El Panecillo hill.

Geographic entities mentioned:
surface_form: El Panecillo hill
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.22861111111111
lon: -78.518611111111
Background. The vessel was named in honor of Frederick Lugard, 1st Baron Lugard, who served as Military Administrator of Uganda from 26 December 1890 to May 1892. During his time in Uganda, Lugard conducted extensive explorations around the Rwenzori Mountains, reaching Lake Edward and mapping significant portions of the territory.

Geographic entities mentioned:
surface_form: Lake Edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
The site chosen for the station was on the Mucomir Cut. Thomas Telford when constructing the Caledonian Canal was faced with a problem where the canal entered Loch Lochy. The only obvious route was that occupied by the River Lochy, and the solution adopted was to cut a new channel for the river between the loch and the River Spean, which joins the River Lochy a little further downstream.

Geographic entities mentioned:
surface_form: Loch Lochy
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.968611111111
lon: -4.9105555555556
Cult centers. The entire Faiyum region – the &quot;Land of the Lake&quot; in Egyptian (specifically referring to Lake Moeris) – served as a cult center of Sobek. Most Faiyum towns developed their own localized versions of the god, such as Soknebtunis at Tebtunis, Sokonnokonni at Bacchias, and Souxei at an unknown site in the area.

Geographic entities mentioned:
surface_form: Lake Moeris
instance_of: Lake
countries: Egypt
coordinates: lat: 29.472222222222
lon: 30.614166666667
The text also focuses heavily on Sobek's central role in creation as a manifestation of Ra, as he is said to have risen from the primal waters of Lake Moeris, not unlike the Ogdoad in the traditional creation myth of Hermopolis. Many varied copies of the book exist and many scholars feel that it was produced in large quantities as a &quot;best-seller&quot; in antiquity.

Geographic entities mentioned:
surface_form: Lake Moeris
instance_of: Lake
countries: Egypt
coordinates: lat: 29.472222222222
lon: 30.614166666667
Background. The song is about the Moors murders that took place on Saddleworth Moor, which overlooks Manchester, between 1963 and 1965. At the time of their deaths, many of the victims were only a few years older than Morrissey (born 1959), who wrote the lyrics of the song after reading a book about the murders, ' by Emlyn Williams.

Geographic entities mentioned:
surface_form: Saddleworth Moor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.543333333333
lon: -1.9558333333333
The morphology implies that a chamber of molten material drained and collapsed, forming a depression surrounded by concentric scarps spaced apart. The arc-shaped set of scarps, extending out to the north from the prominent ellipse, is evidence for a separate episode of withdrawal; the small lobe-shaped extension to the southwest may represent an additional event.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
Solidified lava flows long give the caldera its flower-like appearance. The flows are a lighter tone of gray in the radar data because the lava is blockier in texture and consequently returns more radar waves. Much of the lava, which was evacuated from the chamber, probably traveled to other locations underground, while some of it may have surfaced further south.

Geographic entities mentioned:
surface_form: gray
instance_of: Mountain
coordinates: lat: -65.1
lon: -60.0833
The arc-shaped set of scarps, extending out to the north from the prominent ellipse, is evidence for a separate episode of withdrawal; the small lobe-shaped extension to the southwest may represent an additional event. Solidified lava flows long give the caldera its flower-like appearance.

Geographic entities mentioned:
surface_form: flower
instance_of: Mountain
coordinates: lat: -70.2
lon: -67.8833
Mount Shizuhata. is a mountain located in Shizuoka Prefecture, Japan. It has a height of. The southern half of the mountain is called Mount Asama. It is said to be the origin of &quot;Shizu&quot; in &quot;Shizuoka&quot;.

Geographic entities mentioned:
surface_form: mount shizuhata
instance_of: Mountain
countries: Japan
coordinates: lat: 34.995
lon: 138.374944
surface_form: shizuhata
instance_of: Mountain
countries: Japan
coordinates: lat: 34.995
lon: 138.374944
Eskimo Hill. Eskimo Hill [el.] is summit in North Slope Borough, Alaska, United States. Eskimo Hill was named in 1924.

Geographic entities mentioned:
surface_form: eskimo hill
instance_of: Mountain
countries: United States
coordinates: lat: 69.36666667
lon: -159.76666667
Edgewater is a lakefront community area on the North Side of the city of Chicago, Illinois, north of the Loop. The most recently established of the city's 77 official community areas, Edgewater is bounded by Foster Avenue on the south, Devon Avenue on the north, Ravenswood Avenue on the west, and Lake Michigan on the east. Edgewater contains several beaches for residents to enjoy.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
It is the forty-second-highest mountain in the state. It rises from the head of Box Canyon (above Snow Lake), is part of the headwall of Thomas Canyon (with Mount Fitzgerald), and is a prominent part of the west wall of Lamoille Canyon above Lamoille and Dollar Lakes.

Geographic entities mentioned:
surface_form: Lamoille Canyon
instance_of: Valley
countries: United States
coordinates: lat: 40.6916
lon: -115.474
surface_form: mount fitzgerald
instance_of: Mountain
countries: United States
coordinates: lat: 40.6055
lon: -115.411
surface_form: snow lake
instance_of: Lake
countries: United States
coordinates: lat: 40.6017
lon: -115.4
surface_form: dollar lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 40.5917
lon: -115.385
surface_form: snow lake
instance_of: Lake
countries: United States
coordinates: lat: 46.7572
lon: -121.698
surface_form: snow lake
instance_of: Lake
countries: United States
coordinates: lat: 47.46694444
lon: -121.45555556
surface_form: snow lake
instance_of: Lake
countries: United States
coordinates: lat: 33.4226
lon: -108.496
Snow Lake Peak. Snow Lake Peak is the fifth-highest named mountain of the Ruby Mountains and the seventh highest in Elko County, in Nevada, United States. It is the forty-second-highest mountain in the state.

Geographic entities mentioned:
surface_form: snow lake
instance_of: Lake
countries: United States
coordinates: lat: 40.6017
lon: -115.4
surface_form: snow lake
instance_of: Lake
countries: United States
coordinates: lat: 46.7572
lon: -121.698
surface_form: snow lake peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.605483333333
lon: -115.39671944444
surface_form: snow lake
instance_of: Lake
countries: United States
coordinates: lat: 47.46694444
lon: -121.45555556
surface_form: snow lake
instance_of: Lake
countries: United States
coordinates: lat: 33.4226
lon: -108.496
surface_form: lake peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.563888888889
lon: -115.39388888889
Tenryū Hamanako Line. The, or for short, is a Japanese railway line in Shizuoka Prefecture, paralleling the north coast of Lake Hamana between Kakegawa Station in Kakegawa and Shinjohara Station in Kosai. This is the only railway line of. History.

Geographic entities mentioned:
surface_form: Lake Hamana
instance_of: Lake
countries: Japan
coordinates: lat: 34.741111111111
lon: 137.56972222222
History. The Japanese National Railways was built as an alternative route for the Tokaido Main Line and in particular as a backup for the bridge over Lake Hamana, which was considered potentially vulnerable to weather disruption. The Japanese military also supported the project as the new line would be less vulnerable to coastal attack than the existing section of the Tokaido Main Line.

Geographic entities mentioned:
surface_form: Lake Hamana
instance_of: Lake
countries: Japan
coordinates: lat: 34.741111111111
lon: 137.56972222222
The GDP per employee was 74% of the EU average. Geography. The geography of the region varies considerably, comprising many land forms from lowlands to high mountains whose summits lie above the tree line. In the west lie the Hrubý Jeseník mountains, with the highest mountain of the region (and all Moravia), Praděd, rising.

Geographic entities mentioned:
surface_form: Praděd
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.083194444444445
lon: 17.23086111111111
The confluence of the Odra and Olza is the lowest point of the region, at 195 m. To the south-east, towards the Slovakian border, the landscape sharply rises into the Moravian-Silesian Beskids, with its highest mountain Lysá hora at, which is the place with the highest annual rainfall in the Czech Republic, a year.

Geographic entities mentioned:
surface_form: Lysá hora
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 49.545833333333
lon: 18.4475
The Walpole Island First Nation protects a population of eastern pondmussels residing in their tribal waters within the delta of Lake St. Clair. Like many Unionoid mussels, female eastern pondmussels display a lure to attract their fish hosts (see video, right).

Geographic entities mentioned:
surface_form: Lake St. Clair
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.450265
lon: -82.67572
S. Kennedy on an ascent of the Finsteraarhorn on 13 August 1857 (the fifth ascent of the mountain and the first British ascent). Ad hoc meetings at Mathews's house near Birmingham proceeded during November, and the meeting at which the Alpine Club was founded took place on 22 December 1857 at Ashley's Hotel in London, chaired by Kennedy.

Geographic entities mentioned:
surface_form: Finsteraarhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.537472222222
lon: 8.1260277777778
The Wilderness is managed by the United States Forest Service and is part of the National Wilderness Preservation System. The highest elevation in the Southern Nantahala Wilderness is the peak of Standing Indian Mountain in North Carolina and the lowest elevation is approximately. The Appalachian Trail passes through the Wilderness in both states.

Geographic entities mentioned:
surface_form: Standing Indian Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.035555555556
lon: -83.538055555556
In Georgia, the wilderness is divided into two sections by a corridor on either side of the Tallulah River. The western part of the Wilderness in Georgia includes the portion of the Appalachian Trail that begins at Blue Ridge Gap and climbs over Rocky Knob in Towns County before passing over the eastern flank of Rich Knob in Rabun County and entering North Carolina at Bly Gap.

Geographic entities mentioned:
surface_form: Rich Knob
instance_of: Mountain
countries: United States
coordinates: lat: 34.988888888889
lon: -83.601944444444
The landlocked Central Asian republics are conscious of the need to co-operate in order to maintain and develop their transport networks and energy, communication and irrigation systems. Only Kazakhstan and Turkmenistan border the Caspian Sea and none of the republics has direct access to an ocean, complicating the transportation of hydrocarbons, in particular, to world markets.

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
Lake Winneshiek. Lake Winneshiek is the name given to that portion of Navigation Pool 9 impounded by Lock and Dam No. 9 between the dam to 4 miles south of the city of Lansing, Iowa on the Upper Mississippi River, near Ferryville, Wisconsin. It encompasses about 6,000 acres (24 km2) and is part of the Upper Mississippi River National Wildlife and Fish Refuge.

Geographic entities mentioned:
surface_form: lake winneshiek
instance_of: Lake
countries: United States
coordinates: lat: 43.31
lon: -91.07
Apostle Islands Lighthouses. There are several historic lighthouses on Lake Superior on or near the Apostle Islands in Wisconsin. Six of these lighthouses, all in the Apostle Islands National Lakeshore, were listed as a group on the National Register of Historic Places in 1977 under the name Apostle Islands Lighthouses.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
In Luke 10 and Luke 20 it represents textual cluster 1167. History. The manuscript was written by John, a priest, in 1199. Formerly the manuscript was held at the monastery Vatopedi at Athos peninsula. It was brought to Moscow, in 1655, 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.

Geographic entities mentioned:
surface_form: Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
After a daylong battle, the Israelis had surrounded Ain Dara and were in a position to strike on the highway. In the east, Israeli forces advanced along four main routes towards Joub Jannine, along both sides of the Qaraoun reservoir. The Syrians resisted fiercely.

Geographic entities mentioned:
surface_form: Qaraoun reservoir
instance_of: Lake
countries: Lebanon
coordinates: lat: 33.5725
lon: 35.6975
His unpublished papers are collected in the library of the University of Dar es Salaam and, together with his publications, constitute an important ethnographic record of the history of Tanganyika. After 1950, Cory lived in Mwanza on Lake Victoria, and his last book was devoted to the history of the adjacent Bukoba district.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Ramon Airport. Ramon Airport (), named after Ilan and Assaf Ramon and unofficially also known as Eilat-Ramon Airport, is an international airport located in the Timna Valley in southern Israel. Ramon Airport is the second busiest in Israel (after Ben Gurion Airport) and has replaced the former Eilat Airport and Ovda Airport for civilian traffic.

Geographic entities mentioned:
surface_form: Timna Valley
instance_of: Valley
countries: Israel
coordinates: lat: 29.78777778
lon: 34.98888889
Charles Alexander Stevenson. Charles Alexander Stevenson MICE MIEE FRSE (23 December 1855, – 9 May 1950) was a Scottish lighthouse engineer who built twenty-three lighthouses in and around Scotland. Life. He was born at 8 Forth Street in the east part of Edinburgh's New Town The family moved to 20 Royal Terrace on Calton Hill shortly after his birth.

Geographic entities mentioned:
surface_form: Calton Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.955278
lon: -3.182222
The water supply in the Philippines is threatened by climate change, as changes in rainfall patterns with heavy rainfall or drought make water harder to secure and flooding contaminates what would be safe drinking water. Changing weather patterns have led to trends of decreased inflow into major water reservoirs such as Lake Lanao, Pantabangan, Ambuklao, and Magat.

Geographic entities mentioned:
surface_form: Lake Lanao
instance_of: Lake
countries: Philippines
coordinates: lat: 7.88
lon: 124.2525
Despite temperatures of three degrees Celsius and persistent snowmelt, the event succeeded due to significant efforts, including snow transported by the NVA from the Frauenwald region and the area around the 983-meter-high Beerberg.

Geographic entities mentioned:
surface_form: Beerberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.659444444444
lon: 10.746111111111
History. Giovanni da Verrazzano explored the area known today as Highlands in 1525. During the next two centuries, the Highlands area would welcome English and Dutch settlers. Even by the 20th Century, many immigrants saw the hills of the Highlands of Navesink which were almost above sea level.

Geographic entities mentioned:
surface_form: Navesink
instance_of: Mountain
countries: United States
coordinates: lat: 40.3996
lon: -74.0365
The northeastern third of the Wilderness is dominated by volcanic ridges and peaks; the remaining areas consist of many sparsely vegetated, granitic ridges interspersed with numerous lakes and meadows. Elevations range from below near Cherry Reservoir to at Leavitt Peak, but the elevation range of most of the popular areas is. Precipitation averages annually, 80% of it in the form of snow.

Geographic entities mentioned:
surface_form: Leavitt Peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.2862
lon: -119.651
Tectonic setting. The active plate convergence between the Indian and Eurasian plates along the Main Himalayan Thrust results in widespread intracontinental deformation within Central Asia. As the Indian plate collides with the Eurasian plate, part of the Eurasian plate is uplifted and deformed, resulting in the formation of the Tibetan Plateau.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
This group consisted of 300 celibate Seon practitioners. One result of this split was that the ritual masters all remained with what became the Taego Order. Today, the Taego Order preserves the full ritual tradition of Korean Buddhism, including the Yeongsanjae, which is a reenactment of the Buddha's preaching of the &quot;Lotus Sutra&quot; on Vulture Peak.

Geographic entities mentioned:
surface_form: Vulture Peak
instance_of: Mountain
countries: India
coordinates: lat: 25.001666666666665
lon: 85.44638888888889
The tall mountain is located in the Breheimen mountains and inside the Breheimen National Park, about southwest of the village of Bismo. The mountain is surrounded by several other notable mountains including Gjuvkampen to the north, Lomseggi to the east, Moldulhøi and Sandgrovhøi to the southeast, Hesthøi to the south, Hestdalshøgdi to the southwest, and Grjothøi.

Geographic entities mentioned:
surface_form: Gjuvkampen
instance_of: Mountain
countries: Norway
coordinates: lat: 61.86003
lon: 8.13025
surface_form: Lomseggi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.81666667
lon: 8.36666667
surface_form: Moldulhøi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.80861111
lon: 8.26833333
surface_form: Sandgrovhøi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.78472222
lon: 8.23027778
surface_form: Hesthøi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.678055555556
lon: 8.1922222222222
surface_form: Hestdalshøgdi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.80083333
lon: 8.03638889
surface_form: Grjothøi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.83617
lon: 8.07277
Tverrfjellet (Skjåk). Tverrfjellet is a mountain in Skjåk Municipality in Innlandet county, Norway. The tall mountain is located in the Breheimen mountains and inside the Breheimen National Park, about southwest of the village of Bismo.

Geographic entities mentioned:
surface_form: tverrfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 62.2258
lon: 9.49222
surface_form: tverrfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 62.413333333333
lon: 6.1655555555556
surface_form: tverrfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 61.10337
lon: 8.35782
surface_form: tverrfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 61.8424
lon: 8.1109
Other commercial enterprises in Belmont included clay mining and waste management. The reclamation of a large dump and quarry off Concord Avenue into sites for the Belmont High School and the Clay Pit Pond is a lasting example of environmental planning. With the introduction of automobiles and highways, Belmont continued its transition to a commuter-based suburb throughout the 20th century.

Geographic entities mentioned:
surface_form: Clay Pit Pond
instance_of: Lake
countries: United States
coordinates: lat: 42.3939
lon: -71.165
Consistent and adequate precipitation in the surrounding basins usually ensures that nearby water basins feeding the Aburrá Medellín River basin and subsequently the MAM can store approximately 178 BCM of water for the Metropolitan Area of the Aburrá Valley. Adequate supply and good resource management has allowed nearly 100% of MAM citizens across ten municipalities to receive piped water.

Geographic entities mentioned:
surface_form: Medellín River
instance_of: Watercourse
countries: Colombia
coordinates: lat: 6.09
lon: -75.638055555556
With a mean depth of, it is the third-deepest loch of Scotland. Geography. Located southwest of Loch Ness along the Great Glen, the loch is over long with an average width of about. The River Lochy flows from its southwestern end while the Caledonian Canal links its northeastern extent to Loch Oich. Loch Lochy should not be confused with Loch Loch, which lies to the east of Beinn a' Ghlò. History.

Geographic entities mentioned:
surface_form: Loch Ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
surface_form: the great glen
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
surface_form: great glen
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
surface_form: ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
With a mean depth of, it is the third-deepest loch of Scotland. Geography. Located southwest of Loch Ness along the Great Glen, the loch is over long with an average width of about. The River Lochy flows from its southwestern end while the Caledonian Canal links its northeastern extent to Loch Oich. Loch Lochy should not be confused with Loch Loch, which lies to the east of Beinn a' Ghlò. History.

Geographic entities mentioned:
surface_form: Loch Oich
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.069478
lon: -4.770802
With a mean depth of, it is the third-deepest loch of Scotland. Geography. Located southwest of Loch Ness along the Great Glen, the loch is over long with an average width of about. The River Lochy flows from its southwestern end while the Caledonian Canal links its northeastern extent to Loch Oich. Loch Lochy should not be confused with Loch Loch, which lies to the east of Beinn a' Ghlò. History.

Geographic entities mentioned:
surface_form: Loch Loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.85
lon: -3.6666666666667
surface_form: Beinn a' Ghlò
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.833333333333
lon: -3.7166666666667
surface_form: loch lochy
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.968611111111
lon: -4.9105555555556
The Stand-off at the Fords of Arkaig in September 1665 ended a 360-year feud between the Camerons and the Chattan Confederation. It took place at Achnacarry, on the isthmus between Loch Lochy and Loch Arkaig. Folklore tales mention a supernatural being called the River Horse which was said to emerge from the lake and assume a horse's shape before feeding on the loch's banks.

Geographic entities mentioned:
surface_form: Loch Arkaig
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.971989
lon: -5.158376
surface_form: loch lochy
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.968611111111
lon: -4.9105555555556
Loch Lochy. Loch Lochy () is a large freshwater loch in Lochaber, Highland, Scotland. With a mean depth of, it is the third-deepest loch of Scotland. Geography. Located southwest of Loch Ness along the Great Glen, the loch is over long with an average width of about. The River Lochy flows from its southwestern end while the Caledonian Canal links its northeastern extent to Loch Oich.

Geographic entities mentioned:
surface_form: loch lochy
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.968611111111
lon: -4.9105555555556
It took place at Achnacarry, on the isthmus between Loch Lochy and Loch Arkaig. Folklore tales mention a supernatural being called the River Horse which was said to emerge from the lake and assume a horse's shape before feeding on the loch's banks. The River Horse was also known as the Lord of the Lake and the Water King and would overturn boats and &quot;entice mares from their pastures&quot;.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
The River Horse was also known as the Lord of the Lake and the Water King and would overturn boats and &quot;entice mares from their pastures&quot;. Another tradition was that of the River Bull, &quot;a gentle, harmless creature&quot;, who would &quot;emerge from the lake into the pasture of cows&quot;.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
From the fell's 1,148-ft (350-m) summit, views are afforded of Preston to the south-west; the Fylde Coast to the west; the Vale of Chipping and the fells of the Forest of Bowland to the north and west (including Parlick, Fair Snape Fell and Beacon Fell); the Yorkshire Dales to the north-east (including, most notably, Pen-y-ghent); Clitheroe, Pendle Hill and Whalley, to the east and south-east; and Winter Hill and the West Pennine Moors and the BAE Systems factory at Samlesbury Aerodrome.

Geographic entities mentioned:
surface_form: Parlick
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.8998
lon: -2.6167
surface_form: Fair Snape Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.919361111111
lon: -2.6150888888889
surface_form: Pen-y-ghent
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.155277777778
lon: -2.2497222222222
surface_form: Pendle Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.869
lon: -2.3
surface_form: winter hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.63
lon: -2.515
surface_form: beacon fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.3069
lon: -3.11
On clear days, the Lake District and sometimes the Isle of Man can be seen to the north-west, and the Snowdonia mountain range to the south-west. The River Hodder and its tributary, the River Loud, flow eastward along the north side of the fell, before turning south at the end of the fell to join the River Ribble, which runs westward along the south of the fell.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Longridge Fell. Longridge Fell is the most southerly fell in England, near the town of Longridge, Lancashire. It lies at the southern end of the Forest of Bowland Area of Outstanding Natural Beauty. As its name suggests, it takes the form of a long ridge which rises in a north-easterly direction from within the town of Longridge to its summit 4.5 miles distant.

Geographic entities mentioned:
surface_form: longridge fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.8643
lon: -2.5193
Its total land area consisted of 3,737 dunums prior to 1962. According to the Israeli Central Bureau of Statistics, in it had a population of. Location. Nein lies a short distance from Mount Tabor. A hill known in Arabic as Tell el-Ajul lay on the path that ran between Nein and nearby Indur, an Arab village destroyed in the 1948 Arab-Israeli war.

Geographic entities mentioned:
surface_form: Mount Tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
A hill known in Arabic as Tell el-Ajul lay on the path that ran between Nein and nearby Indur, an Arab village destroyed in the 1948 Arab-Israeli war. Biblical archaeologist Edward Robinson describes Nein as lying on the northern slope of a hill called &quot;the little Hermon&quot;, and it is described in biblical guidebooks as lying at the foot of the Hill of Moreh. Antiquity.

Geographic entities mentioned:
surface_form: Hill of Moreh
instance_of: Mountain
countries: Israel
coordinates: lat: 32.615833333333
lon: 35.363611111111
Saddle Mountain (Alberta). Saddle Mountain is a summit in Alberta, Canada. Description. Saddle Mountain is located in the Bow Valley within Banff National Park, and it is part of the Bow Range of the Canadian Rockies. Lake Louise townsite is situated to the northeast and the Continental Divide is to the west. The nearest higher neighbor is Fairview Mountain, to the northwest.

Geographic entities mentioned:
surface_form: Bow Valley
instance_of: Valley
countries: Canada
coordinates: lat: 51.1671
lon: -115.48
surface_form: saddle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.393055555555556
lon: -116.20861111111111
Saddle Mountain (Alberta). Saddle Mountain is a summit in Alberta, Canada. Description. Saddle Mountain is located in the Bow Valley within Banff National Park, and it is part of the Bow Range of the Canadian Rockies. Lake Louise townsite is situated to the northeast and the Continental Divide is to the west. The nearest higher neighbor is Fairview Mountain, to the northwest.

Geographic entities mentioned:
surface_form: saddle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.393055555555556
lon: -116.20861111111111
The nearest higher neighbor is Fairview Mountain, to the northwest. Precipitation runoff from Saddle Mountain drains into tributaries of the Bow River. Topographic relief is modest as the summit rises over 600 meters (1,968 ft) above Paradise Creek in one kilometer (0.6 mile) and nearly 900 meters (2,953 ft) above Bow River in.

Geographic entities mentioned:
surface_form: saddle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.393055555555556
lon: -116.20861111111111
Access. The Paradise Valley Trail leads from Lake Louise to Saddleback Pass, and from the pass an off-trail scramble leads to the top of Saddle Mountain. The summit offers one of the finest views of the area, including the Bow Valley and a close view of the impressive north face of Mount Temple. History. The mountain's descriptive name was applied in 1894 by Samuel E.S. Allen.

Geographic entities mentioned:
surface_form: saddle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.393055555555556
lon: -116.20861111111111
Allen. The mountain's toponym was officially adopted on April 3, 1952, by the Geographical Names Board of Canada. Geology. Like other mountains in Banff Park, Saddle Mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate.

Geographic entities mentioned:
surface_form: saddle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.393055555555556
lon: -116.20861111111111
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate. Based on the Köppen climate classification, Saddle Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below -20 °C with wind chill factors below -30 °C.

Geographic entities mentioned:
surface_form: saddle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.393055555555556
lon: -116.20861111111111
The ship was sold to a Swedish firm and reflagged 1947. Merchant service. &quot;Cabell&quot; was sold to the Swedish shipping firm of Rederlaktiebolaget Bris, 28 May 1947, after they refused her sister ship. She was renamed &quot;Sommen&quot; after the lake Sommen in Sweden. In 1963, &quot;Sommen&quot; was reflagged again as the Greek ship MV &quot;Donald&quot;.

Geographic entities mentioned:
surface_form: Sommen
instance_of: Lake
countries: Sweden
coordinates: lat: 58.015833333333
lon: 15.176944444444
Dundee. Dundee (;; or,) is the fourth-largest city in Scotland. The mid-year population estimate for the locality was. It lies within the eastern central Lowlands on the north bank of the Firth of Tay, which feeds into the North Sea. Under the name of Dundee City, it forms one of the 32 council areas used for local government in Scotland.

Geographic entities mentioned:
surface_form: central Lowlands
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.408
lon: -4.044
The built-up area occupies a roughly rectangular shape long by wide, aligned in an east to west direction and occupies an area of. The town is bisected by a line of hills stretching from Balgay Hill (elevation of 143 m) in the west end of the city, through the Dundee Law (174 m) which occupies the centre of the built up area, to Gallow Hill (83 m), between Baxter Park and the Eastern Cemetery.

Geographic entities mentioned:
surface_form: Dundee Law
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.47017
lon: -2.989399