Sarmila/GeoWiki-Features huggingface dataset:
Pennsylvania consumed about 1 million tons annually, cut on the state's lakes and rivers. Aside from Stillwater Lake, Pocono Mountain Ice Company harvested ice on Saylor's Lake, Trout Lake, Lake Naomi, Pocono Lake, Mountain Spring Lake, and the Lakes at Tobyhanna. It was reported that the Pocono Mountain Ice Company was harvesting ice for 6 cents per ton.

Geographic entities mentioned:
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 28.0381
lon: -81.7351
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 44.76083333
lon: -92.96277778
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 44.700833333333
lon: -93.473888888889
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 42.719669
lon: -83.392527
surface_form: trout lake
instance_of: Lake
countries: United States
coordinates: lat: 43.5377039
lon: -73.7045568
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 42.325555555556
lon: -74.964444444444
surface_form: trout lake
instance_of: Lake
countries: United States
coordinates: lat: 27.646944444444
lon: -81.5075
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 44.0111458
lon: -89.1607253
surface_form: trout lake
instance_of: Lake
countries: United States
coordinates: lat: 46.0431
lon: -89.6708
surface_form: trout lake
instance_of: Lake
countries: United States
coordinates: lat: 43.1625
lon: -74.3245
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 47.43638888888889
lon: -122.08888888888889
surface_form: stillwater lake
instance_of: Lake
countries: United States
coordinates: lat: 41.1215141
lon: -75.4143857
surface_form: trout lake
instance_of: Lake
countries: United States
coordinates: lat: 37.824444444444
lon: -107.885
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 45.3667276
lon: -88.9628259
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 42.6536
lon: -73.4215
surface_form: trout lake
instance_of: Lake
countries: United States
coordinates: lat: 47.266125
lon: -122.27959
surface_form: trout lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9006
lon: -110.131
Stillwater Lake (Pennsylvania). Stillwater Lake is a reservoir that covers approximately. The lake is located in Pocono Summit, Pennsylvania, at an elevation of. Fed by Dotter's Run, Hawkeye Run, Pocono Summit Creek, and several underground springs, the lake flows out to Lake Naomi via Tunkhannock Creek. There are several Tunkhannock Creeks in the Pocono Mountains in Northeastern Pennsylvania.

Geographic entities mentioned:
surface_form: stillwater lake (pennsylvania)
instance_of: Lake
countries: United States
coordinates: lat: 41.1215141
lon: -75.4143857
Stillwater Lake (Pennsylvania). Stillwater Lake is a reservoir that covers approximately. The lake is located in Pocono Summit, Pennsylvania, at an elevation of. Fed by Dotter's Run, Hawkeye Run, Pocono Summit Creek, and several underground springs, the lake flows out to Lake Naomi via Tunkhannock Creek. There are several Tunkhannock Creeks in the Pocono Mountains in Northeastern Pennsylvania.

Geographic entities mentioned:
surface_form: stillwater lake
instance_of: Lake
countries: United States
coordinates: lat: 41.1215141
lon: -75.4143857
Eventually, the ice companies folded, while still controlling large tracts of land. In 1949, Samuel Rubel and the Pocono Mountain Ice Company donated a majority of the land around Stillwater Lake to the Boy Scouts of America's Bethlehem Area Council (now Minsi Trails Council).

Geographic entities mentioned:
surface_form: stillwater lake
instance_of: Lake
countries: United States
coordinates: lat: 41.1215141
lon: -75.4143857
The remaining land was sold to developers and was marketed in the 1960s as Stillwater Lake Estates, a development of approximately 1,000 lots (typically about two-thirds of an acre each), with amenities presently including a beach, community center, playground, nature preserve, tennis courts and marina. 21st century.

Geographic entities mentioned:
surface_form: stillwater lake
instance_of: Lake
countries: United States
coordinates: lat: 41.1215141
lon: -75.4143857
21st century. In 2002, the Pennsylvania Department of Environmental Protection (DEP) reclassified the dam on Stillwater Lake as a B2 High Hazard Dam. Funding was approved in the 2006 Pennsylvania State R-CAP Budget to repair the dam, however the legislators were reluctant to release the already approved funds for the project.

Geographic entities mentioned:
surface_form: stillwater lake
instance_of: Lake
countries: United States
coordinates: lat: 41.1215141
lon: -75.4143857
It was formerly called Gombe Stream National Park. Overview. Established in 1968, it is one of the smallest national parks in Tanzania, with only of protected land along the hills of the eastern shore of Lake Tanganyika. The terrain is distinguished by steep valleys, and the vegetation ranges from grassland to woodland to tropical rainforest.

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
The Black Buttes, also known historically as the Sawtooth Rocks, make up an extinct stratovolcano in the Cascade Volcanic Arc in Whatcom County, Washington, United States. Glacially eroded remnants of this volcano rise above the Deming Glacier, part of the glacier system of the nearby volcano, Mount Baker. There are three major peaks — Colfax, Lincoln, and Seward — all of which can be climbed.

Geographic entities mentioned:
surface_form: Mount Baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Mount Baker, a much younger volcano, sits on top of lava erupted from Black Buttes Volcano. Geography. The Black Buttes represent the remains of a large stratovolcano that was once located in the approximate location of its neighbor, Mount Baker. Black Buttes lies about from Mount Baker, between Baker and the middle fork of Nooksack River, in Whatcom County, Washington state.

Geographic entities mentioned:
surface_form: Mount Baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: black buttes
instance_of: Landform
countries: United States
coordinates: lat: 48.7693
lon: -121.853
The volcano reaches an elevation of, with a precision of 40 feet. Its peaks adjacent to Coleman Glacier, Thunder Glacier, and Deming Glacier. These peaks include the two principal summits, Colfax Peak (or East Butte), and Lincoln Peak (or West Butte), as well as the third major summit known as Seward Peak. Colfax Peak. First climbed by David Anderson, Clarence A.

Geographic entities mentioned:
surface_form: lincoln peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1273
lon: -72.9285
surface_form: east butte
instance_of: Mountain
countries: United States
coordinates: lat: 43.501388888889
lon: -112.6625
surface_form: lincoln peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.88273
lon: -114.29722
surface_form: lincoln peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.7683
lon: -121.859
The western side of the northern flank was first climbed by Paul Johanson and S. Reilly Moss in September, 1974, close to the 1958 route, and the trail takes approximately four hours. Lincoln Peak. Located west of Colfax Peak, Lincoln Peak, also known as West Butte, has an elevation of. It was first climbed by Fred Beckey, Wesley Grande, John Rupley, and Herb Staley on July 22, 1956.

Geographic entities mentioned:
surface_form: lincoln peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1273
lon: -72.9285
surface_form: lincoln peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.88273
lon: -114.29722
surface_form: lincoln peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.7683
lon: -121.859
The climb is technically demanding, taking about 9 hours, and it has significant rockfall hazards. The cirque can also be accessed from Middle Fork Nooksack River Road. The least accessible of the Black Buttes summits, Lincoln Peak has a northern face as well as a face to the east. To the west, Lincoln Peak drops into Thunder Glacier's cirque; its southern side features gullies and ridges.

Geographic entities mentioned:
surface_form: lincoln peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1273
lon: -72.9285
surface_form: lincoln peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.88273
lon: -114.29722
surface_form: lincoln peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.7683
lon: -121.859
surface_form: black buttes
instance_of: Landform
countries: United States
coordinates: lat: 48.7693
lon: -121.853
The least accessible of the Black Buttes summits, Lincoln Peak has a northern face as well as a face to the east. To the west, Lincoln Peak drops into Thunder Glacier's cirque; its southern side features gullies and ridges. It was rated as one of the ten most difficult peaks in the state of Washington by the climber Dallas Kloke
Seward Peak.

Geographic entities mentioned:
surface_form: lincoln peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1273
lon: -72.9285
surface_form: lincoln peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.88273
lon: -114.29722
surface_form: lincoln peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.7683
lon: -121.859
It was rated as one of the ten most difficult peaks in the state of Washington by the climber Dallas Kloke
Seward Peak. Seward Peak has an elevation of, and it lies to the west of Lincoln Peak. First ascended by Dallas Kloke and Bryce Simon on July 11, 1973, it does not require a technical climb.

Geographic entities mentioned:
surface_form: lincoln peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1273
lon: -72.9285
surface_form: lincoln peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.88273
lon: -114.29722
surface_form: lincoln peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.7683
lon: -121.859
First ascended by Dallas Kloke and Bryce Simon on July 11, 1973, it does not require a technical climb. Climbers are recommended to approach as though intending to climb Lincoln Peak, but instead to follow heather to the southwestern ridge before ascending a ridge to a false peak. After another of ascent, they should reach the summit of Seward Peak, the entire trip lasting about 4 hours. Geology.

Geographic entities mentioned:
surface_form: lincoln peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1273
lon: -72.9285
surface_form: lincoln peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.88273
lon: -114.29722
surface_form: lincoln peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.7683
lon: -121.859
Black Buttes. The Black Buttes, also known historically as the Sawtooth Rocks, make up an extinct stratovolcano in the Cascade Volcanic Arc in Whatcom County, Washington, United States. Glacially eroded remnants of this volcano rise above the Deming Glacier, part of the glacier system of the nearby volcano, Mount Baker.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: the sawtooth
instance_of: Mountain
countries: United States
coordinates: lat: 39.590833333333
lon: -105.66416666667
surface_form: black buttes
instance_of: Landform
countries: United States
coordinates: lat: 48.7693
lon: -121.853
Geography. The Black Buttes represent the remains of a large stratovolcano that was once located in the approximate location of its neighbor, Mount Baker. Black Buttes lies about from Mount Baker, between Baker and the middle fork of Nooksack River, in Whatcom County, Washington state. The volcano reaches an elevation of, with a precision of 40 feet.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: black buttes
instance_of: Landform
countries: United States
coordinates: lat: 48.7693
lon: -121.853
To the west, Lincoln Peak drops into Thunder Glacier's cirque; its southern side features gullies and ridges. It was rated as one of the ten most difficult peaks in the state of Washington by the climber Dallas Kloke
Seward Peak. Seward Peak has an elevation of, and it lies to the west of Lincoln Peak.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Colfax Peak. First climbed by David Anderson, Clarence A. Fisher, and Paul Hugdahl in 1921, Colfax Peak or East Butte, reaches an elevation of. It has a small ice cap on its eastern flank, along with a hanging ice cliff on its northern flank, and it consists of extremely steep rock walls.

Geographic entities mentioned:
surface_form: east butte
instance_of: Mountain
countries: United States
coordinates: lat: 43.501388888889
lon: -112.6625
There are three major peaks — Colfax, Lincoln, and Seward — all of which can be climbed. The volcano was last active during the Middle Pleistocene from 495,000 to 288,000 years ago. Mount Baker, a much younger volcano, sits on top of lava erupted from Black Buttes Volcano. Geography.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: black buttes
instance_of: Landform
countries: United States
coordinates: lat: 48.7693
lon: -121.853
It has a small ice cap on its eastern flank, along with a hanging ice cliff on its northern flank, and it consists of extremely steep rock walls. The route up this summit traverses easy slopes, starting at the Mount Baker saddle from the Coleman Glacier Route, and running for about an hour along a lava ridge or snowslopes.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Lava flows made of andesite from 455,000 to 366,000 years ago were generated from a vent now buried under Mount Baker; at least two have subhorizontal columns indicating that they were settled adjacent to ice, likely from a glacier. Some of the lava flows also contain hypersthene basalt.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Some of the lava flows also contain hypersthene basalt. In addition to these eruptions traced to Black Buttes, there are five lava flows in the vicinity for which geologists have failed to pinpoint the source vent. These deposits were erupted after Black Buttes went extinct, but before Mount Baker became active. They consist of rhyodacite (dated to 199,000 years ago) and basaltic andesite.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: black buttes
instance_of: Landform
countries: United States
coordinates: lat: 48.7693
lon: -121.853
Human history. The Black Buttes were named by Edmund T. Coleman during his ascent of Mount Baker in 1868. He named Lincoln and Colfax Peaks, describing them on August 14 of that year as &quot;black, jagged, splintered precipices.&quot; Historian Charles Easton referred to the Black Buttes as a &quot;homogenous mass of black basalt&quot;, comparing them to &quot;a Chinese wall&quot;.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
He named Lincoln and Colfax Peaks, describing them on August 14 of that year as &quot;black, jagged, splintered precipices.&quot; Historian Charles Easton referred to the Black Buttes as a &quot;homogenous mass of black basalt&quot;, comparing them to &quot;a Chinese wall&quot;. Historically, the surveyor Thomas Gerdine called them the Sawtooth Rocks, a name which was used for a number of maps.

Geographic entities mentioned:
surface_form: the sawtooth
instance_of: Mountain
countries: United States
coordinates: lat: 39.590833333333
lon: -105.66416666667
Black Buttes. The Black Buttes, also known historically as the Sawtooth Rocks, make up an extinct stratovolcano in the Cascade Volcanic Arc in Whatcom County, Washington, United States. Glacially eroded remnants of this volcano rise above the Deming Glacier, part of the glacier system of the nearby volcano, Mount Baker.

Geographic entities mentioned:
surface_form: black buttes
instance_of: Landform
countries: United States
coordinates: lat: 48.7693
lon: -121.853
After another of ascent, they should reach the summit of Seward Peak, the entire trip lasting about 4 hours. Geology. Black Buttes is an extinct volcano with an amphitheater shape. It consists of jagged peaks that form an arc-shaped ridge, which were shaped and altered by glacial motion and erosion.

Geographic entities mentioned:
surface_form: black buttes
instance_of: Landform
countries: United States
coordinates: lat: 48.7693
lon: -121.853
Eruptive history. Black Buttes was active during the Middle Pleistocene from 495,000 to 288,000 years ago, producing viscous, andesitic lava flows with a steep dip (the steepest angle of descent of a tilted bed or feature relative to a horizontal plane) that reach thicknesses of up to, though they could actually be larger as they are covered by ice.

Geographic entities mentioned:
surface_form: black buttes
instance_of: Landform
countries: United States
coordinates: lat: 48.7693
lon: -121.853
Some of the lava flows also contain hypersthene basalt. In addition to these eruptions traced to Black Buttes, there are five lava flows in the vicinity for which geologists have failed to pinpoint the source vent. These deposits were erupted after Black Buttes went extinct, but before Mount Baker became active. They consist of rhyodacite (dated to 199,000 years ago) and basaltic andesite.

Geographic entities mentioned:
surface_form: black buttes
instance_of: Landform
countries: United States
coordinates: lat: 48.7693
lon: -121.853
These deposits were erupted after Black Buttes went extinct, but before Mount Baker became active. They consist of rhyodacite (dated to 199,000 years ago) and basaltic andesite. Human history. The Black Buttes were named by Edmund T. Coleman during his ascent of Mount Baker in 1868.

Geographic entities mentioned:
surface_form: black buttes
instance_of: Landform
countries: United States
coordinates: lat: 48.7693
lon: -121.853
Human history. The Black Buttes were named by Edmund T. Coleman during his ascent of Mount Baker in 1868. He named Lincoln and Colfax Peaks, describing them on August 14 of that year as &quot;black, jagged, splintered precipices.&quot; Historian Charles Easton referred to the Black Buttes as a &quot;homogenous mass of black basalt&quot;, comparing them to &quot;a Chinese wall&quot;.

Geographic entities mentioned:
surface_form: black buttes
instance_of: Landform
countries: United States
coordinates: lat: 48.7693
lon: -121.853
surface_form: chinese wall
instance_of: Mountain
countries: United States
coordinates: lat: 44.1285
lon: -114.619
On 5 May 1856, the company opened two new sections, Renens to Lausanne and the connecting curve from Morges to Bussigny. On 10 June 1857 a section from Villeneuve at the western end of Lake Geneva to Bex in the Rhone Valley opened. The link between Lausanne and Villeneuve was operated by boat until 1861.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Thus, the Miles Canyon Basalts are the reason for the establishment of the townsite of Closeleigh, eventually the City of Whitehorse. The lava flows and cinder cones in the Alligator Lake volcanic complex southwest of Whitehorse are the greatest accumulation of these rocks. The Miles Canyon Basalts were thought to be Pleistocene age.

Geographic entities mentioned:
surface_form: Alligator Lake volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 60.389722222222
lon: -135.42638888889
In February 1926 she reverted to her original name, and was broken up in late 1928 in Bruges, Belgium. &quot;Lalla Rookh&quot; (1881 ship). A schooner on Lake Michigan, 60.34 ton, built in Manitowoc, Wisconsin, by James Butler 2 February 1881, launched on 4 August 1881. Ran aground near Port Washington on 6 October 1887 and was stripped and abandoned. &quot;Lalla Rookh II&quot; (1956 ship).

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Sgor Gaibhre. Sgor Gaibhre (955 m) is a mountain in the Grampian Mountains of Scotland. It lies on the border of Highland and Perth and Kinross, near Loch Ossian. A remote mountain in the heart of the Grampians, it is usually climbed from either Rannoch Moor to the west or Corrour railway station.

Geographic entities mentioned:
surface_form: Loch Ossian
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.777707
lon: -4.627669
Sgor Gaibhre. Sgor Gaibhre (955 m) is a mountain in the Grampian Mountains of Scotland. It lies on the border of Highland and Perth and Kinross, near Loch Ossian. A remote mountain in the heart of the Grampians, it is usually climbed from either Rannoch Moor to the west or Corrour railway station.

Geographic entities mentioned:
surface_form: sgor gaibhre
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.772553
lon: -4.546498
After swerving to the east of Orono, Highway35/115 meets the eastern terminus of Highway407 East. It enters the Oak Ridges Moraine and passes through the eastern edge of the Ganaraska Forest at Enterprise Hill. Highway35 exits the divided highway—which continues as Highway115 east to Peterborough—at a trumpet interchange known as the 35/115 split, and proceeds north as a two lane road.

Geographic entities mentioned:
surface_form: Oak Ridges Moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
Highway 35 generally follows the former Bobcaygeon Colonization Road north of Minden, though several realignments over the years have led to its current winding route. At Carnarvon, it meets with Highway 118. The route then follows the east side of Boshkung Lake, passes through Buttermilk Falls, travels long the west side of Halls Lake, then arches northwest to cross the midpoint of Kushog Lake.

Geographic entities mentioned:
surface_form: Boshkung Lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.066111111111
lon: -78.729444444444
The speed limit for most of the length of the highway is, slowing to within built-up areas, and increasing to when it connects with Highway 115. History. Highway 35, like many highways that begin at Lake Ontario and eventually cross into the Canadian Shield, began as several trails connecting settlements. Most of the southern portion of the highway follows various sidelines and concessions.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Ocotlán District. Ocotlán District is located in the south of the Valles Centrales Region of the State of Oaxaca, Mexico.

Geographic entities mentioned:
surface_form: Valles Centrales Region
instance_of: Valley
countries: Mexico
coordinates: lat: 17.0833
lon: -96.75
Vly Creek. Vly Creek is a river in Delaware County and Greene County in New York. It flows into Bush Kill by Fleischmanns, New York. It flows through Lake Switzerland.

Geographic entities mentioned:
surface_form: Lake Switzerland
instance_of: Lake
countries: United States
coordinates: lat: 42.1604883
lon: -74.5205909
James Anderson (lawyer). James Anderson (5 August 1662 – 3 April 1728), Scottish antiquary and historian, was born in Edinburgh. His father was Patrick Anderson of Walston, a church minister, who was for some time imprisoned on the Bass Rock on the Firth of Forth in Haddingtonshire. Education and career.

Geographic entities mentioned:
surface_form: Bass Rock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.08
lon: -2.64
The highest point in Harstad Municipality is Sætertinden, which is above sea level. It is located near the village of Sandtorg in southern Harstad. The tall mountain, Nupen, is located in the northwestern part of the municipality on the border with Kvæfjord. Climate and light.

Geographic entities mentioned:
surface_form: Nupen
instance_of: Mountain
countries: Norway
coordinates: lat: 68.85194444
lon: 16.24833333
Gore Mtn. is flanked to the northeast by Black Mountain, and to the northwest by Middle Mountain. The north and northwest sides of Gore Mountain drain via several short brooks into the Coaticook River, thence into the Massawippi River, Saint-François River, and Saint Lawrence River in Quebec, and thence into the Gulf of Saint Lawrence. The southwest side of Gore Mtn.

Geographic entities mentioned:
surface_form: black mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.304444444444
lon: -120.40333333333
surface_form: black mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.03881
lon: -119.27877
surface_form: middle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.9566
lon: -120.181
Gore Mountain (Vermont). Gore Mountain is a mountain located in the uninhabited Avery's Gore in Essex County, Vermont, about 6 miles (10 km) south of the Canada–US border with Quebec. In Vermont, gores and grants are unincorporated portions of a county which are not part of any town and have limited self-government (if any, as many are uninhabited). Gore Mtn.

Geographic entities mentioned:
surface_form: gore mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.9198
lon: -71.794
Gore Mtn. is flanked to the northeast by Black Mountain, and to the northwest by Middle Mountain. The north and northwest sides of Gore Mountain drain via several short brooks into the Coaticook River, thence into the Massawippi River, Saint-François River, and Saint Lawrence River in Quebec, and thence into the Gulf of Saint Lawrence. The southwest side of Gore Mtn.

Geographic entities mentioned:
surface_form: gore mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.9198
lon: -71.794
They are classified either as part of Bavarian Prealps or the larger chain of Northern Limestone Alps. The range stretches for about 15 kilometres. From the west it is bordered by the valley of the river Loisach and from the east by Walchensee lake and the valley of the river Isar. With its highest peak being Krottenkopf (2,086 m), the highest part of the range just exceeds 2,000 m.

Geographic entities mentioned:
surface_form: Walchensee
instance_of: Lake
countries: Germany
coordinates: lat: 47.593888888889
lon: 11.346111111111
The range stretches for about 15 kilometres. From the west it is bordered by the valley of the river Loisach and from the east by Walchensee lake and the valley of the river Isar. With its highest peak being Krottenkopf (2,086 m), the highest part of the range just exceeds 2,000 m. The range is of composed of limestone. The treeline is around 1,700 m. Etymology.

Geographic entities mentioned:
surface_form: Krottenkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 47.545280555556
lon: 11.192780555556
basque &quot;Ezterenzubi&quot;, occitan &quot;Esterel&quot;). Most important summits. The most important summits in the Ester range are the Krottenkopf (2,086 m), the Bischof (2,033 m), the Hohe Kisten (1,922 m), the Hoher Fricken (1,940 m) and the Simetsberg (1,836 m). The climbs both from the Loisach valley as well as from Krün or Wallgau in the southeast are relatively long.

Geographic entities mentioned:
surface_form: Krottenkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 47.545280555556
lon: 11.192780555556
surface_form: Hohe Kisten
instance_of: Mountain
countries: Germany
coordinates: lat: 47.561944444444
lon: 11.209166666667
surface_form: Hoher Fricken
instance_of: Mountain
countries: Germany
coordinates: lat: 47.532777777778
lon: 11.155277777778
As a result the Ester Mountains are relatively quiet with the exception of the Wank mountain (1,780 m) which is accessible by cable car (the Wankbahn). Most tourists and mountaineers are attracted to the nearby higher ranges Wetterstein, Karwendel and to the highest peak of Germany, the Zugspitze. Activities.

Geographic entities mentioned:
surface_form: Zugspitze
instance_of: Mountain
countries: Germany
Austria
coordinates: lat: 47.421217
lon: 10.986314
He initially set out on a Hajj, the obligatory Pilgrimage to Mecca. Departing on 5 March 1046, Khusraw took a less than direct route, heading north toward the Caspian Sea. Throughout his travels he kept a minutely detailed journal which clearly describes many facets of life in the Islamic world of the 11th Century.

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
Crary Mountains. Crary Mountains () are a group of ice-covered volcanoes in Marie Byrd Land, Antarctica. They consist of two or three shield volcanoes, named Mount Rees, Mount Steere and Mount Frakes, which developed during the course of the Miocene and Pliocene and last erupted about 30,000-40,000 years ago.

Geographic entities mentioned:
surface_form: Mount Steere
instance_of: Mountain
coordinates: lat: -76.7
lon: -117.8
surface_form: Mount Frakes
instance_of: Mountain
coordinates: lat: -76.8
lon: -117.7
The Crary Mountains form a drainage divide for the West Antarctic Ice Sheet; they dam it, which is thus higher on the southwestern side of the range. Debris stripes have been observed on the ice near the foot of the mountains. The northeasternmost volcano is Mount Rees, which reaches a summit height of at Tasch Peak. Volcanic rocks crop out at Trabucco Cliff on its northeastern flank.

Geographic entities mentioned:
surface_form: Tasch Peak
instance_of: Mountain
coordinates: lat: -76.6667
lon: -118.05
Outcrops consist of breccia and lavas, which in one case are intruded by a dike. In the middle of the chain lies Mount Steere with a summit elevation of and a rectangular summit caldera. Lie Cliff is a volcanic outcrop on the northeastern flank.

Geographic entities mentioned:
surface_form: Mount Steere
instance_of: Mountain
coordinates: lat: -76.7
lon: -117.8
Outcrops feature breccias and lava with numerous intruded dikes. South of Mount Steere is Mount Frakes, with it is the highest peak in the range and the least eroded of the Crary Mountains. It has a wide circular summit caldera and unlike Mount Rees and Mount Steere it bears no evidence of subglacial eruptions, probably due to lack of erosion that could have exposed them.

Geographic entities mentioned:
surface_form: Mount Frakes
instance_of: Mountain
coordinates: lat: -76.8
lon: -117.7
It has a wide circular summit caldera and unlike Mount Rees and Mount Steere it bears no evidence of subglacial eruptions, probably due to lack of erosion that could have exposed them. Volcanic rocks crop out both on the southern and western flank, at Morrison Rocks and English Rock respectively. These outcrops are cinder cones that formed on the slopes of Mount Frakes.

Geographic entities mentioned:
surface_form: English Rock
instance_of: Mountain
coordinates: lat: -76.8167
lon: -118
Volcanic and nonvolcanic boulders on the slopes of Mount Frakes may either be xenoliths or glacial erratics. Boyd Ridge is smaller than the other three volcanoes and located southeast of Mount Frakes and reaches an elevation of. Runyon Rock crops out to its east and is the only area of Boyd Ridge not covered by ice. Cinders and a cliff of hyaloclastite are found there.

Geographic entities mentioned:
surface_form: Runyon Rock
instance_of: Mountain
coordinates: lat: -76.9333
lon: -116.55
It is directed away from the centre of the Marie Byrd Land volcanic province and may reflect the propagation of a fracture in the crust. West Antarctica has been subject to glaciation since the Oligocene, where a perhaps local ice cap or snow deposit existed at Mount Petras.

Geographic entities mentioned:
surface_form: Mount Petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
Meigh. Meigh () is a small village and townland near Slieve Gullion in County Armagh, Northern Ireland. It had a population of 444 people in the 2001 Census. It lies within the Newry, Mourne and Down District Council area. Geography. Meigh lies within the Ring of Gullion area of natural beauty, about 7 km southwest of Newry. Nearby villages include Camlough, Dromintee and Jonesborough.

Geographic entities mentioned:
surface_form: Slieve Gullion
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.133333333333
lon: -6.4333333333333
Helmet of Iron Gates. The Helmet of Iron Gates () is a Geto-Dacian silver helmet dating from the 4th century BC, housed in the Detroit Institute of Arts, United States. It probably comes from Iron Gates area, in the Mehedinți County, Romania. Formerly it was in the collection of Franz Tau, Vienna.

Geographic entities mentioned:
surface_form: Iron Gates
instance_of: Valley
countries: Serbia
Romania
coordinates: lat: 44.671111111111
lon: 22.529722222222
Early life and education. Bray grew up in California's San Fernando Valley. Bray's interest in comic book art started in the 1950s when he was 9 years old, and he saw Basil Wolverton's art in &quot;Mad&quot; magazine. As a teen, Bray started working in his family’s hardware store and began collecting comics, original art, toys and posters. Career and comic art collection.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
It lies just 3 km east of the state capital city of Oaxaca, within the Oaxaca metropolitan area. It is part of the Centro District in the Valles Centrales region. The city of Santa Lucía del Camino had a 2005 census population of 42,570 and serves as the municipal seat of the municipality of Santa Lucía del Camino, which has an area of 9.437 km2 (2.95 sq mi) and a population of 45,752.

Geographic entities mentioned:
surface_form: Valles Centrales region
instance_of: Valley
countries: Mexico
coordinates: lat: 17.0833
lon: -96.75
Geologically, the region is sandy, with sandy-loam and sandy-clay covering most of the village, making it one of the most fertile lands in Uvira Territory. The northwest basin of Lake Tanganyika, which encompasses Uvira Territory, is characterized by outcrops of very ancient (Precambrian) and very recent (Quaternary) rocks.

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
Goldfield Hills. The Goldfield Hills is a mountain range in Esmeralda County, Nevada, south of the mining district and town of Goldfield, in the Great Basin.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: goldfield hills
instance_of: Landform
countries: United States
coordinates: lat: 37.6088
lon: -117.248
Goldfield Hills. The Goldfield Hills is a mountain range in Esmeralda County, Nevada, south of the mining district and town of Goldfield, in the Great Basin.

Geographic entities mentioned:
surface_form: goldfield hills
instance_of: Landform
countries: United States
coordinates: lat: 37.6088
lon: -117.248
It is located in the western part of the municipality along the river Glomma, about east of the town of Hamar. The town is the regional centre for commerce and industry for the middle Østerdalen valley and the northern part of Solør. The old village of Elverum has grown over the years and in 1996, the municipal council of Elverum Municipality granted the urban village of Elverum town status.

Geographic entities mentioned:
surface_form: Østerdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.575916666666664
lon: 11.087111111111112
Military ties. During the Nordic Seven Years' War (1563–1570), Swedish troops invaded Norway in a number of locations, including a number of incursions into Østerdalen. In 1563, Norwegian troops stopped the Swedish advance at Elverum, which provided a strategic point since it lay on both north-south and east–west trade and travel routes.

Geographic entities mentioned:
surface_form: Østerdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.575916666666664
lon: 11.087111111111112
They are managed as one unit. Terry Andrae State Park, established in 1927, and John Michael Kohler State Park, established in 1966, total. The parks contain over two miles (3 km) of beaches and sand dunes along the shore of Lake Michigan, with woods and wetlands away from the water. The Black River flows through the parks. History.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Directly north of the state park, the Kohler company has proposed to clear as much as 200 acres of forest, which may affect as much as 80 acres of protected wetlands, in order to construct an 18-hole golf course along the shore of Lake Michigan.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Challenges from state residents and environmental activists have caused the proposal to be delayed and modified because of concerns over the fragility of the neighboring ecosystems. Amenities. Activities related to Lake Michigan include fishing, boating, and swimming. There are no boat launching ramps or docks at the park. The lake contains dozens of species of fish including trout and salmon.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Rossbodenstock. Rossbodenstock is a mountain peak of the Saint-Gotthard Massif and part of the Lepontine Alps south of the Oberalp Pass. It is high; its peak is located on the border between the cantons of Uri and Graubünden, which follows the ridge from north to south. The source of the Rein da Tuma, the source of the Rhine is on the eastern flank of the mountain.

Geographic entities mentioned:
surface_form: rossbodenstock
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.635216666667
lon: 8.6509527777778
Kirkkosaari. (Church Island) is a small island in Finland. It is surrounded by lake Pielavesi and is part of the municipality of Pielavesi. It was the former parish center, and was originally called Lammassalo. There is a bridge connecting Kirkkosaari to the mainland via the northern Tenhusaari.

Geographic entities mentioned:
surface_form: lake Pielavesi
instance_of: Lake
countries: Finland
coordinates: lat: 63.3
lon: 26.58333333
On February 11, 2021, the USGS officially recognized Mt. Borah as Idaho's only active glacier. Description. The mountain was nameless until it was discovered to be higher than Hyndman Peak, previously regarded as the state's highest point. In February 1934, the U.S. Geological Survey named it for William Borah, the prominent senior U.S.

Geographic entities mentioned:
surface_form: Hyndman Peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.7494
lon: -114.131
Borah Peak. Borah Peak, also known as Mount Borah or Beauty Peak, is a mountain in the western United States and the highest summit in Idaho. One of the most prominent peaks in the contiguous United States, it is located in the central section of the Lost River Range, within the Challis National Forest in eastern Custer County. On February 11, 2021, the USGS officially recognized Mt.

Geographic entities mentioned:
surface_form: borah peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1373891
lon: -113.78110123
1983 earthquake. The 1983 Borah Peak earthquake occurred on Friday, October 28, at <abbr>8:06:09 MDT</abbr> in the Lost River Range at Borah Peak in central Idaho, United States, measuring 6.9 on the moment magnitude scale. Mount Borah rose about and the Lost River Valley in that vicinity dropped about. The peak was scarred on the western side, and the mark is still visible.

Geographic entities mentioned:
surface_form: borah peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1373891
lon: -113.78110123
The face features a number of Grade II class 5 routes on mixed terrain. Three climbers are known to have died on Borah Peak: two climbers, Vaughn Howard and Guy Campbell, ascended the northwest ridge on November 24, 1977 and were killed in an avalanche. The bodies were not recovered for nine months, until August 26, 1978. On June 13, 1987, another climber, Dave Probst, died on a glissade.

Geographic entities mentioned:
surface_form: borah peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1373891
lon: -113.78110123
Pristimantis supernatis. &quot;Pristimantis supernatis&quot; is a species of frog in the family Strabomantidae. It is found in the Cordillera Central, Colombia, from Nevado del Huila southward to the Colombian Massif and the Carchi Province in northern Ecuador. Some sources report records from further north (Antioquia), but others attribute these to &quot;Pristimantis permixtus&quot;.

Geographic entities mentioned:
surface_form: Nevado del Huila
instance_of: Mountain
countries: Colombia
coordinates: lat: 2.9333333333333
lon: -76.033333333333
Several bus routes also depart from the ground-level station. Future plans. Zürich Zoo, situated on the Zürichberg mountain above the tunnel, has plans to construct a cable car to link the zoo and station, a distance of about. the cable car is expected to open in 2028.

Geographic entities mentioned:
surface_form: Zürichberg mountain
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.3856
lon: 8.56694
Lake Ossiach. Lake Ossiach (,) is a lake in the Austrian state of Carinthia. It is the state's third largest lake after Lake Wörth () and Lake Millstatt (). Geography. Lake Ossiach is located in the southern Nock Mountains range of the Gurktal Alps along the road from Villach to Feldkirchen. The lake is above sea level. Its average depth is 19.6 m (64.30 ft) with a maximum depth of.

Geographic entities mentioned:
surface_form: Lake Wörth
instance_of: Lake
countries: Austria
coordinates: lat: 46.625
lon: 14.15
surface_form: Lake Millstatt
instance_of: Lake
countries: Austria
coordinates: lat: 46.795
lon: 13.579722222222
Lake Ossiach. Lake Ossiach (,) is a lake in the Austrian state of Carinthia. It is the state's third largest lake after Lake Wörth () and Lake Millstatt (). Geography. Lake Ossiach is located in the southern Nock Mountains range of the Gurktal Alps along the road from Villach to Feldkirchen. The lake is above sea level. Its average depth is 19.6 m (64.30 ft) with a maximum depth of.

Geographic entities mentioned:
surface_form: lake ossiach
instance_of: Lake
countries: Austria
coordinates: lat: 46.666666666667
lon: 13.966666666667
surface_form: ossiach
instance_of: Lake
countries: Austria
coordinates: lat: 46.666666666667
lon: 13.966666666667
Lake Ossiach. Lake Ossiach (,) is a lake in the Austrian state of Carinthia. It is the state's third largest lake after Lake Wörth () and Lake Millstatt (). Geography. Lake Ossiach is located in the southern Nock Mountains range of the Gurktal Alps along the road from Villach to Feldkirchen. The lake is above sea level. Its average depth is 19.6 m (64.30 ft) with a maximum depth of.

Geographic entities mentioned:
surface_form: lake ossiach
instance_of: Lake
countries: Austria
coordinates: lat: 46.666666666667
lon: 13.966666666667
surface_form: ossiach
instance_of: Lake
countries: Austria
coordinates: lat: 46.666666666667
lon: 13.966666666667
surface_form: gurktal
instance_of: Watercourse
countries: Austria
coordinates: lat: 46.909922
lon: 13.949844
The lake is above sea level. Its average depth is 19.6 m (64.30 ft) with a maximum depth of. The total surface area is approximately. Lake Ossiach is a dimictic lake with mixing periods in spring and in late autumn. In summer the waters reach 28 °C at the surface. Several uninhabited parts of the shore are protected as natural reserves.

Geographic entities mentioned:
surface_form: lake ossiach
instance_of: Lake
countries: Austria
coordinates: lat: 46.666666666667
lon: 13.966666666667
surface_form: ossiach
instance_of: Lake
countries: Austria
coordinates: lat: 46.666666666667
lon: 13.966666666667
The lake empties via Seebach Creek into the Drava () River. Primary villages on the lake are Annenheim at the western end, Sattendorf and Bodensdorf on the northern shore, Steindorf at the eastern end, and Ossiach on the southern shore. Sattendorf and Annenheim belong to the municipality () of Treffen. Bodensdorf and Steindorf belong to the municipality of Feldkirchen.

Geographic entities mentioned:
surface_form: ossiach
instance_of: Lake
countries: Austria
coordinates: lat: 46.666666666667
lon: 13.966666666667
Sattendorf and Annenheim belong to the municipality () of Treffen. Bodensdorf and Steindorf belong to the municipality of Feldkirchen. The lake is named after Ossiach Abbey. Mount Gerlitzen rises over the northern side of the lake, reaching at its summit. From Annenheim, the Kanzelhöhe subpeak of Mount Gerlitzen can be reached by a cable car built in 1928 by the Bleichert engineering company.

Geographic entities mentioned:
surface_form: ossiach
instance_of: Lake
countries: Austria
coordinates: lat: 46.666666666667
lon: 13.966666666667
Immediate action is required for restoring these habitats and conserving the water birds in Bangladesh. The key breeding and staging areas of Bangladesh include Haor areas such as the Meghna estuary, Tanguar haor and Hail-Hakaluki haors, Chalan Beel, the Sundarbans and other coastal mangroves including Hatia and Nijhum Dweep, and haor areas of the north west and off shore islands.

Geographic entities mentioned:
surface_form: Chalan Beel
instance_of: Lake
countries: Bangladesh
coordinates: lat: 24.52
lon: 89.01