Sarmila/GeoWiki-Features huggingface dataset:
The Mourne Wall passes east–west over the mountaintop, and there is a small tower at the summit. There are also the remains of an ancient burial cairn on the mountaintop. Slieve Commedagh overlooks the Glen River to the east, and the Pot of Legawherry to the west. On its southern side are a group of granite tors known as 'the Castles'.

Geographic entities mentioned:
surface_form: slieve commedagh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.1889
lon: -5.93867
On its southern side are a group of granite tors known as 'the Castles'. This overlooks the Brandy Pad, a track used in the 18th century to smuggle commodities such as brandy and tobacco, mainly from Britain. The Slieve Commedagh massif also includes the lesser summits of Shan Slieve, Slievenamaddy and Slievenabrock (to the north).

Geographic entities mentioned:
surface_form: slieve commedagh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.1889
lon: -5.93867
Grand Rapids, Michigan. Grand Rapids is a city in and the county seat of Kent County, Michigan, United States. It is the second-most populous city in Michigan with a population of 198,917 at the 2020 census and estimated at 200,117 in 2024, while the Grand Rapids metropolitan area with over 1.18 million residents is the 49th-largest metropolitan area in the U.S.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
The terrain becomes more rolling hills away from the river. The countryside surrounding the metropolitan area consists of mixed forest and farmland, with large areas of orchards to the northwest. It is approximately east of Lake Michigan. The state capital of Lansing lies about to the east-by-southeast, and Kalamazoo is about to the south.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
With Michigan being the second most agriculturally diverse state in the nation, the Greater Grand Rapids region is well known for its fruit production. Due to its proximity to Lake Michigan, the climate is considered especially prime for apple, peach, and blueberry farming. Greater Grand Rapids produces 1/3 of Michigan's total agricultural sales. Arts and culture.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Henry Freeway running along the south side connecting I-96 and I-196
runs along Ironwood/Remembrance Road, Wilson Avenue, and 28th Street
is Fulton Street to the east
follows Alpine Avenue to the north, I-96, East Beltline Avenue and Broadmoor Avenue to the south
is East Beltline north of I-96
follows Lake Michigan Drive west toward Allendale and Lake Michigan
is Old US 131 south of 28th Street
Bus.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
He rode the train to Clearwater, then was driven to the end of the road at the park boundary where he stayed at the Helset Ranch. He travelled by horse to see Helmcken Falls, camped at The Horseshoe on the Clearwater River for two nights, then boated along Mahood Lake to stay at Mahood Lake Lodge overnight. Chess Lyons was appointed by Gray in 1940 to conduct the first survey of Wells Gray Park.

Geographic entities mentioned:
surface_form: Mahood Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.910443
lon: -120.399196
In the northern part of Skånland was the smaller village of Grov. Other villages were Renså, Tovik and Sandstrand. The largest lake was Skoddebergvatnet, and the highest mountain was Skittendalstinden at in the mountainous center of the peninsula. There were calcareous pine forests near Skoddebergvatnet. The lake Niingsvatnet was located on the border with Evenes Municipality.

Geographic entities mentioned:
surface_form: Skoddebergvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 68.5975
lon: 17.241389
state of Michigan. The river is located in the northwestern Lower Peninsula of the state, flowing into Lake Michigan at Frankfort. The river's course is mostly within Benzie County, (which takes its name from a variant pronunciation of the river), although the river rises in western Grand Traverse County and flows briefly through northern Manistee County.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
The river's course is mostly within Benzie County, (which takes its name from a variant pronunciation of the river), although the river rises in western Grand Traverse County and flows briefly through northern Manistee County. The river widens to form Betsie Lake before emptying into Lake Michigan between Frankfort and Elberta. The Betsie River is a part of Michigan's Natural Rivers Program.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Jackson Hollow. Jackson Hollow is a valley in Stone County in the U.S. state of Missouri. Jackson Hollow has the name of the local Jackson family.

Geographic entities mentioned:
surface_form: jackson hollow
instance_of: Valley
countries: United States
coordinates: lat: 36.6767291
lon: -93.4896334
Rowing at the 2014 Asian Games – Men's quadruple sculls. The men's quadruple sculls competition at the 2014 Asian Games in Chungju, South Korea was held from 20 September to 24 September at the Tangeum Lake International Rowing Center. Schedule. All times are Korea Standard Time ()

Geographic entities mentioned:
surface_form: Tangeum Lake
instance_of: Lake
countries: South Korea
coordinates: lat: 37.021944444444
lon: 127.86527777778
During the 2010 Winter Olympics in Vancouver, he finished 18th in the individual sprint event. His best World Cup competition finish was third at a sprint event in Rogla, Slovenia in December 2009. On 7 April 2016 his retirement from cross-country skiing was announced. Cross-country skiing results. All results are sourced from the International Ski Federation (FIS).

Geographic entities mentioned:
surface_form: Rogla
instance_of: Mountain
countries: Slovenia
coordinates: lat: 46.4525
lon: 15.333611
Pfingstberg. Pfingstberg (Potsdam) is a hill in Brandenburg, Germany. The Belvedere auf dem Pfingstberg sits atop the hill.

Geographic entities mentioned:
surface_form: pfingstberg
instance_of: Mountain
countries: Germany
coordinates: lat: 52.4187
lon: 13.059
It has streaked greyish-brown upperparts and buff underparts, and is similar in appearance to other European pipits. There are two subspecies, of which the nominate is non-migratory, and the Fennoscandian one is migratory, wintering in shoreline habitats further west and south in Europe. The European rock pipit is territorial at least in the breeding season, and year-round where it is resident.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
European rock pipits in winter are readily distinguishable from water pipits, but very difficult to assign to subspecies by appearance or measurements. The western populations are known to be nearly sedentary, so east of the Elbe basin vagrant Eurasian rock pipits are presumably mostly &quot;littoralis&quot;. Ringing results show that &quot;A. p.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Gideon's farmhouse, now within the boundaries of Shorewood, Minnesota, is listed on the National Register of Historic Places. Gideon moved to Minnesota in 1853, near Lake Minnetonka, and experimented with planting pear, plum, cherry, peach, and apple seeds. After ten years of experimentation, the harsh Minnesota winters had killed off all of his trees except for one seedling crab apple tree.

Geographic entities mentioned:
surface_form: Lake Minnetonka
instance_of: Lake
countries: United States
coordinates: lat: 44.933333333333
lon: -93.566666666667
Mont Donon. Mont Donon is the highest peak in the northern Vosges. It is a Category 2 climb in the Tour de France. On Donon, there is an 80 metre tall lattice tower for TV transmission. Its TV transmission antennas are covered by a polymeric cylinder, which gives its structure a characteristic shape. An engraved block of sandstone near the summit commemorates the conception of Victor Hugo.

Geographic entities mentioned:
surface_form: mont donon
instance_of: Mountain
countries: France
coordinates: lat: 48.513333333333
lon: 7.165
surface_form: donon
instance_of: Mountain
countries: France
coordinates: lat: 48.513333333333
lon: 7.165
Mont Donon. Mont Donon is the highest peak in the northern Vosges. It is a Category 2 climb in the Tour de France. On Donon, there is an 80 metre tall lattice tower for TV transmission. Its TV transmission antennas are covered by a polymeric cylinder, which gives its structure a characteristic shape. An engraved block of sandstone near the summit commemorates the conception of Victor Hugo.

Geographic entities mentioned:
surface_form: donon
instance_of: Mountain
countries: France
coordinates: lat: 48.513333333333
lon: 7.165
Many archaeological remains of a Gallo-Roman sanctuary have been found on and around the top of the mountain. They are now displayed in the Musée archéologique de Strasbourg. World War I. During the earliest stages of World War I, Mount Donon was the site of heavy fighting between German and French troops between 14 August and 22 August 1914 and specially on 21 and 22 August.

Geographic entities mentioned:
surface_form: donon
instance_of: Mountain
countries: France
coordinates: lat: 48.513333333333
lon: 7.165
states of New York and Pennsylvania. It drains a rural dissected plateau of in the northern Allegheny Plateau, providing the northeasternmost drainage in the watershed of the Mississippi River. Its tributaries reach to within of Lake Erie in southwestern New York. Water from the Allegheny River eventually flows into the Gulf of Mexico via the Ohio and Mississippi rivers.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Ives Bank. Ives Bank () is a submarine bank with a least depth of in the Bellingshausen Sea. It is located in the southern approaches to Ryder Bay, Adelaide Island, Antarctica, south of the Mikkelsen Islands. It was named by the UK Antarctic Place-Names Committee after Lieutenant Commander David M. Ives, Royal Navy, who surveyed this bank from HMS &quot;Endurance&quot; in March 1981.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
surface_form: ryder
instance_of: Mountain
coordinates: lat: -66.95
lon: 52.25
Ives Bank. Ives Bank () is a submarine bank with a least depth of in the Bellingshausen Sea. It is located in the southern approaches to Ryder Bay, Adelaide Island, Antarctica, south of the Mikkelsen Islands. It was named by the UK Antarctic Place-Names Committee after Lieutenant Commander David M. Ives, Royal Navy, who surveyed this bank from HMS &quot;Endurance&quot; in March 1981.

Geographic entities mentioned:
surface_form: ives bank
instance_of: Landform
coordinates: lat: -67.6667
lon: -68.2
Ives Bank. Ives Bank () is a submarine bank with a least depth of in the Bellingshausen Sea. It is located in the southern approaches to Ryder Bay, Adelaide Island, Antarctica, south of the Mikkelsen Islands. It was named by the UK Antarctic Place-Names Committee after Lieutenant Commander David M. Ives, Royal Navy, who surveyed this bank from HMS &quot;Endurance&quot; in March 1981.

Geographic entities mentioned:
surface_form: ives bank
instance_of: Landform
coordinates: lat: -67.6667
lon: -68.2
surface_form: bellingshausen
instance_of: Mountain
coordinates: lat: -75.1167
lon: 162.1
Bishop Alemany High School. Bishop Alemany High School is a Roman Catholic secondary school located in the San Fernando Valley community of Mission Hills in Los Angeles, California. It is within the San Fernando Pastoral Region of the Archdiocese of Los Angeles. The school is accredited by the Western Association of Schools and Colleges.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
The Wiesental (,), named after the river Wiese, is a valley in the Southern Black Forest. The Wiese is a right-hand tributary of the Rhine which has its source in Feldberg and flows into the Rhine in Basel, Switzerland. The Wiesental was one of the first industrialized regions of the former grand dutchy of Baden and an important production location for the textile industry. Geography.

Geographic entities mentioned:
surface_form: feldberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.0739
lon: 7.91028
surface_form: feldberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.356
lon: 10.022
surface_form: feldberg
instance_of: Mountain
countries: Germany
coordinates: lat: 47.873611111111
lon: 8.0038888888889
surface_form: feldberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.4719
lon: 9.9509
The Wiesental was one of the first industrialized regions of the former grand dutchy of Baden and an important production location for the textile industry. Geography. With the exception of the two Swiss communes Riehen and Basel, as well as the Feldberg commune with the source of the Wiese (Landkreis Breisgau-Hochschwarzwald), the Wiesental belongs entirely to the district of Landkreis Lörrach.

Geographic entities mentioned:
surface_form: feldberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.0739
lon: 7.91028
surface_form: feldberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.356
lon: 10.022
surface_form: wiesental
instance_of: Valley
countries: Germany
surface_form: feldberg
instance_of: Mountain
countries: Germany
coordinates: lat: 47.873611111111
lon: 8.0038888888889
surface_form: feldberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.4719
lon: 9.9509
With the exception of the two Swiss communes Riehen and Basel, as well as the Feldberg commune with the source of the Wiese (Landkreis Breisgau-Hochschwarzwald), the Wiesental belongs entirely to the district of Landkreis Lörrach. The 55 km long river Wiese flows through the valley in a South-Western direction from the Feldberg (1200 meters above sea level) to Basel (244 meters above sea level).

Geographic entities mentioned:
surface_form: feldberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.0739
lon: 7.91028
surface_form: feldberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.356
lon: 10.022
surface_form: feldberg
instance_of: Mountain
countries: Germany
coordinates: lat: 47.873611111111
lon: 8.0038888888889
surface_form: feldberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.4719
lon: 9.9509
Blasien and the cloister of Säckingen. Several houses (von Waldeck, von Eichstetten, von Wehr-Wildenstein, von Grenchen and Höllstein) handed over the entire territory of Schönau and Todtnau to the cloister of St.Blasien during the 12th century. Furthermore, the cloister received Fröhnd from the Lords of Stein and Künaberg and owned a church in Weitenau in the centre of the Wiesental.

Geographic entities mentioned:
surface_form: stein
instance_of: Mountain
countries: Germany
coordinates: lat: 47.6336
lon: 11.3253
surface_form: wiesental
instance_of: Valley
countries: Germany
Blasien as well and the Wettingen cloister was given possessions from the Lords of Üsenberg. Thanks to the cloister's property, new noble families gained agency and tenure in the Wiesental. The Lords of Stein, who worked as stewards in Zell and Häg for the Damenstift Säckingen and handed down their duties to the family of Schönau, are one example.

Geographic entities mentioned:
surface_form: wiesental
instance_of: Valley
countries: Germany
Thanks to the cloister's property, new noble families gained agency and tenure in the Wiesental. The Lords of Stein, who worked as stewards in Zell and Häg for the Damenstift Säckingen and handed down their duties to the family of Schönau, are one example. The demesne Neuenstein was also given to them by the Lords of Stein, but was later sold to Rudolf III of Hachberg-Sausenberg in 1400.

Geographic entities mentioned:
surface_form: stein
instance_of: Mountain
countries: Germany
coordinates: lat: 47.6336
lon: 11.3253
Wiesental, Black Forest. The Wiesental (,), named after the river Wiese, is a valley in the Southern Black Forest. The Wiese is a right-hand tributary of the Rhine which has its source in Feldberg and flows into the Rhine in Basel, Switzerland.

Geographic entities mentioned:
surface_form: wiesental
instance_of: Valley
countries: Germany
The Wiesental (,), named after the river Wiese, is a valley in the Southern Black Forest. The Wiese is a right-hand tributary of the Rhine which has its source in Feldberg and flows into the Rhine in Basel, Switzerland. The Wiesental was one of the first industrialized regions of the former grand dutchy of Baden and an important production location for the textile industry. Geography.

Geographic entities mentioned:
surface_form: wiesental
instance_of: Valley
countries: Germany
The Wiese merges with its biggest tributary, the &quot;Little Wiese&quot;, approximately below Schopfheim. The Köhlgarten- and Belchenwiese merge to become the Little Wiese nearTegernau. Its valley is known as Kleines Wiesental (&quot;Little Wiesental&quot;). The biggest city in Wiesental is Lörrach with around 48 000 inhabitants, followed by Schopfheim with around 19 000 inhabitants. Geology.

Geographic entities mentioned:
surface_form: wiesental
instance_of: Valley
countries: Germany
surface_form: wiesental
instance_of: Valley
countries: Germany
The Köhlgarten- and Belchenwiese merge to become the Little Wiese nearTegernau. Its valley is known as Kleines Wiesental (&quot;Little Wiesental&quot;). The biggest city in Wiesental is Lörrach with around 48 000 inhabitants, followed by Schopfheim with around 19 000 inhabitants. Geology. The back part of the valley is mainly made of Gneiss and Granite.

Geographic entities mentioned:
surface_form: wiesental
instance_of: Valley
countries: Germany
Traffic. The 317 crosses the valley alongside the Wiese in a south-westerly direction. Near Schopfheim the 518 branches off in the direction of the Wehratal and Hochrhein. Additionally, near Lörrach the A98 crosses the valley on the Wiesental Bridge, resembling a viaduct. The Wiesentalbahn, which is operated by the Swiss SBB, runs parallel to the Wiese, connecting Zell and Basel SBB station.

Geographic entities mentioned:
surface_form: wiesental
instance_of: Valley
countries: Germany
First Settlement. Roman remains near Maulburg and Brombach provide evidence that the Wiesental was inhabited fairly early. The population of the valley increased greatly later; remains near Fahrnau and Schopfheim suggest that settlement of the central part of the Wiesental began around 700 AD, while the far end of the valley was most likely not populated until the 10th and 11th century.

Geographic entities mentioned:
surface_form: wiesental
instance_of: Valley
countries: Germany
The Wiesental's oldest town is Schopfheim (first documented in 807), which was also the first to gain market rights from the Lords of Rötteln around 1250. Land Tenure since the High Middle Ages. During the High Middle Ages the Wiesental was owned by numerous clerics and secular masters. Lörrach, Brombach and Rötteln were important locations for the Lords of Rötteln, who were reeves of the St.

Geographic entities mentioned:
surface_form: wiesental
instance_of: Valley
countries: Germany
Lörrach, Brombach and Rötteln were important locations for the Lords of Rötteln, who were reeves of the St. Alban cloister in Basel. Their castle sits above Lörrach. Additionally, the Röttler owned numerous parts of the centre of the Wiesental (e.g. Maulburg, Schopfheim) and the Little Wiesental. The Lords of Rotenburg, another Röttler line, owned a castle near Wieslet.

Geographic entities mentioned:
surface_form: wiesental
instance_of: Valley
countries: Germany
The Lords of Waldeck had tenure and rights in Fahrnau, Steinen, Hägelberg and Fröhnd, the noble family Kaltenbach ruled in the neighbouring Kandertal, and the Kienberg family owned land on the Dinkelberg, as well as in. Other families with large properties were the Klingens of Langenau and Gersbach, and the Wehrs from the upper Wiesental.

Geographic entities mentioned:
surface_form: wiesental
instance_of: Valley
countries: Germany
Other families with large properties were the Klingens of Langenau and Gersbach, and the Wehrs from the upper Wiesental. The noble family Wart held rights in Endenburg, Schlächtenaus and Weitenau, while the von Grenchens had theirs in Fröhnd, Schönau, Wembach and Höllstein. Moreover, numerous cloisters held rights and tenure in the Wiesental, namely St. Blasien and the cloister of Säckingen.

Geographic entities mentioned:
surface_form: wiesental
instance_of: Valley
countries: Germany
At the time of sale, the territory spanned the Wiesen- and Wehravallies including Gersbach, Schlechtbach, Raitbach, Kürnberg, Schweigmatt, as well as other farms, which nowadays are part of East Schopfheim. Furthermore, the Habsburger became important Lords in the Wiesental, particularly in the upper Wiesental, where they were reeves of the cloisters Säckingen (after 1181) and St.

Geographic entities mentioned:
surface_form: wiesental
instance_of: Valley
countries: Germany
surface_form: wiesental
instance_of: Valley
countries: Germany
The margraves of Hachberg had already started consolidating their dominion, and their successors continued with these policies. Therefore, the front part of the Wiesental is also part of the Markgräflerland. In the upper Wiesental the property of the cloisters Säckingen (priory Zell) and St. Blasien (priory Schönau and Todtnau) was under the rule of the Habsburger.

Geographic entities mentioned:
surface_form: wiesental
instance_of: Valley
countries: Germany
surface_form: wiesental
instance_of: Valley
countries: Germany
The margraves of Hachberg had already started consolidating their dominion, and their successors continued with these policies. Therefore, the front part of the Wiesental is also part of the Markgräflerland. In the upper Wiesental the property of the cloisters Säckingen (priory Zell) and St. Blasien (priory Schönau and Todtnau) was under the rule of the Habsburger.

Geographic entities mentioned:
surface_form: wiesental
instance_of: Valley
countries: Germany
Industry. &quot;Im Wiesental Fabriken stehn,wie Schlösser klar und hell,Rauchfahnen aus Kaminen,von Lörrach bis nach Zell.&quot;
&quot;In the Wiesen valley there are factories,Bright and fair like castles,Trails of smoke are blown,From Lörrach up to Zell.&quot;
However, towards the end of the 20th century, the Textile industry withdrew more and more from the valley.

Geographic entities mentioned:
surface_form: wiesental
instance_of: Valley
countries: Germany
Nowadays textile factories remain in only a few cities. Today, the Wiesental's economy is based on mechanical engineering companies, a few of which are leaders on the global market. The center of the Wiesental for example is known for its vacuum pump industry. Dialects.

Geographic entities mentioned:
surface_form: wiesental
instance_of: Valley
countries: Germany
&quot;Er seit: &quot;O Muetter, lueg doch au,&quot;
&quot;so schön wie in di'm Himmelssaal!&quot;
&quot;‚He‘, seit sie, ‚drum isch's Wiesethal.‘&quot;
&quot;Er sagt: &quot;Oh Mutter, sieh doch auch&quot;
&quot;so schön wie in deinem Himmelssaal!&quot;
&quot;„Freilich“, sagt sie, „deswegen ist's das Wiesental“.&quot;
&quot;down there it shines in the morning dew&quot;
&quot;„Indeed“, she says, that is why it is the Wiesental“.&quot;
Landmarks.

Geographic entities mentioned:
surface_form: wiesental
instance_of: Valley
countries: Germany
surface_form: wiesental
instance_of: Valley
countries: Germany
North Fork Mountain is the driest high mountain in the Appalachians, and has vegetation and flora different from nearby, wetter high mountain areas immediately to the west such as Spruce Knob and Dolly Sods, with pines (&quot;Pinus&quot;) abundant on the mountain's ridgecrest, in contrast with the spruces (&quot;Picea&quot;) so characteristic of these comparably high summits across the North Fork Valley.

Geographic entities mentioned:
surface_form: Spruce Knob
instance_of: Mountain
countries: United States
coordinates: lat: 38.6999
lon: -79.5328
surface_form: high mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0887
lon: -74.2351
surface_form: high mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0887
lon: -74.2351
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
The mountain's strata (rock layers) are nearly flat, but the Tuscarora quartzite that forms the mountain's caprock is bent downwards (and now mostly eroded away) east and west of the ridge, becoming nearly vertical along the mountain's slopes, where the same quartzite stratum forms such dramatic outcrops as Seneca Rocks.

Geographic entities mentioned:
surface_form: Seneca Rocks
instance_of: Landform
countries: United States
coordinates: lat: 38.8347
lon: -79.3661
surface_form: seneca
instance_of: Lake
countries: United States
coordinates: lat: 42.655555555556
lon: -76.8975
surface_form: seneca rocks
instance_of: Landform
countries: United States
coordinates: lat: 38.8347
lon: -79.3661
There is no weather station, but this climate table contains interpolated data. Geology. North Fork Mountain is part of the Wills Mountain Anticline, a geological structure that extends from Pennsylvania through Maryland and West Virginia into Virginia. The same geologic ridge that forms North Fork Mountain is known as New Creek Mountain north of North Fork Gap.

Geographic entities mentioned:
surface_form: New Creek Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.228
lon: -79.1288
surface_form: new creek mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.228
lon: -79.1288
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
Immediately west of the mountain, the same quartzite formation is nearly vertical, along the western limb of the anticline, forming such dramatic outcrops as Seneca Rocks, Champe Rocks, Nelson Rocks, and Judy Rocks. This series of vertical outcrops is part of a formation known as the River Knobs or East Seneca Ridge.

Geographic entities mentioned:
surface_form: Seneca Rocks
instance_of: Landform
countries: United States
coordinates: lat: 38.8347
lon: -79.3661
surface_form: Champe Rocks
instance_of: Landform
countries: United States
coordinates: lat: 38.8914
lon: -79.3117
surface_form: champe rocks
instance_of: Landform
countries: United States
coordinates: lat: 38.8914
lon: -79.3117
surface_form: seneca
instance_of: Lake
countries: United States
coordinates: lat: 42.655555555556
lon: -76.8975
surface_form: seneca rocks
instance_of: Landform
countries: United States
coordinates: lat: 38.8347
lon: -79.3661
This series of vertical outcrops is part of a formation known as the River Knobs or East Seneca Ridge. The lower, western slopes of the mountain and the adjacent Germany Valley are underlain by the easily eroded Ordovician-aged New Market Limestone and are penetrated by numerous caves, such as the celebrated Hellhole. Shales occur on some of North Fork Mountain's slopes. History.

Geographic entities mentioned:
surface_form: Germany Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.765
lon: -79.39
surface_form: germany valley
instance_of: Valley
countries: United States
coordinates: lat: 38.765
lon: -79.39
The contrast is also great between North Fork Mountain's quartzite-outcrop vegetation and the superficially similar vegetation of the rocky sandstone-conglomerate openings of Spruce Knob, Dolly Sods, and similar sites just west of North Fork Mountain. While North Fork Mountain's lesser rainfall is a substantial factor in this difference, another consideration is the nature of the bedrock itself.

Geographic entities mentioned:
surface_form: Spruce Knob
instance_of: Mountain
countries: United States
coordinates: lat: 38.6999
lon: -79.5328
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
Scenery and recreation. Views westward overlooking the North Fork River abound from many of North Fork Mountain's rocky outcrops. Places visible to the west from points on the ridgetop may include the River Knobs (including Seneca Rocks and Champe Rocks), the Germany Valley, the Fore Knobs, Hopeville Gorge, Spruce Mountain and Spruce Knob, and the Allegheny Front.

Geographic entities mentioned:
surface_form: Seneca Rocks
instance_of: Landform
countries: United States
coordinates: lat: 38.8347
lon: -79.3661
surface_form: Champe Rocks
instance_of: Landform
countries: United States
coordinates: lat: 38.8914
lon: -79.3117
surface_form: Germany Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.765
lon: -79.39
surface_form: Spruce Knob
instance_of: Mountain
countries: United States
coordinates: lat: 38.6999
lon: -79.5328
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.405555555556
lon: -74.198888888889
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.75
lon: -79.48
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0175
lon: -74.45
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.5521
lon: -114.822
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.33007
lon: -74.1154089
North Fork Mountain and the River Knobs feature prominently in views from the mountaintops immediately west of the North Fork Valley, including Spruce Knob and Dolly Sods. Nelson Sods on North Fork Mountain has views of the Roaring Plains, Spruce Mountain, and the North Fork Valley, as well as Shenandoah Mountain to the east. Similar views are also offered by other open summits on the mountain.

Geographic entities mentioned:
surface_form: Shenandoah Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.5097
lon: -79.1842
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.405555555556
lon: -74.198888888889
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.75
lon: -79.48
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0175
lon: -74.45
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.5521
lon: -114.822
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.33007
lon: -74.1154089
The oak-and-pine vegetation of North Fork Mountain contrasts strongly with the more diverse vegetation of the nearby mountains just west of the North Fork River, such as Spruce Mountain and the Allegheny Front, which receive considerably more rainfall.

Geographic entities mentioned:
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.405555555556
lon: -74.198888888889
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.75
lon: -79.48
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0175
lon: -74.45
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.5521
lon: -114.822
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.33007
lon: -74.1154089
Similar views are also offered by other open summits on the mountain. State Route 28 follows the North Fork River from North Fork Gap south to Cherry Grove, offering diverse views of the River Knobs and North Fork Mountain to the east and the Fore Knobs, Allegheny Front, and Spruce Mountain to the west. The Germany Valley Overlook on U.S.

Geographic entities mentioned:
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.405555555556
lon: -74.198888888889
surface_form: river knobs
instance_of: Mountain
countries: United States
coordinates: lat: 38.7369
lon: -79.4347
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.75
lon: -79.48
surface_form: fore
instance_of: Landform
countries: United States
coordinates: lat: 43.661694444444
lon: -70.307833333333
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0175
lon: -74.45
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.5521
lon: -114.822
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.33007
lon: -74.1154089
The same geologic ridge that forms North Fork Mountain is known as New Creek Mountain north of North Fork Gap. At North Fork's southern end, the ridge fragments into Devils Backbone, Brushy Mountain, and Monterey Mountain, with Snowy Mountain being a minor continuation into Virginia.

Geographic entities mentioned:
surface_form: snowy mountain
instance_of: Mountain
countries: United States
coordinates: lat: 58.336
lon: -154.682
surface_form: snowy mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7003
lon: -74.386
Similar views are also offered by other open summits on the mountain. State Route 28 follows the North Fork River from North Fork Gap south to Cherry Grove, offering diverse views of the River Knobs and North Fork Mountain to the east and the Fore Knobs, Allegheny Front, and Spruce Mountain to the west. The Germany Valley Overlook on U.S.

Geographic entities mentioned:
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
Immediately west of the mountain, the same quartzite formation is nearly vertical, along the western limb of the anticline, forming such dramatic outcrops as Seneca Rocks, Champe Rocks, Nelson Rocks, and Judy Rocks. This series of vertical outcrops is part of a formation known as the River Knobs or East Seneca Ridge.

Geographic entities mentioned:
surface_form: seneca
instance_of: Lake
countries: United States
coordinates: lat: 42.655555555556
lon: -76.8975
surface_form: river knobs
instance_of: Mountain
countries: United States
coordinates: lat: 38.7369
lon: -79.4347
Golden eagles are also known there. Various locally abundant but globally rare species of bats that roost in nearby limestone caverns are also often seen foraging over North Fork Mountain's western slopes. The pink-edged sulphur butterfly is known from Panther Knob, Its caterpillars feed on the blueberries that thrive atop this knob after fires. Scenery and recreation.

Geographic entities mentioned:
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
North Fork Mountain and the River Knobs feature prominently in views from the mountaintops immediately west of the North Fork Valley, including Spruce Knob and Dolly Sods. Nelson Sods on North Fork Mountain has views of the Roaring Plains, Spruce Mountain, and the North Fork Valley, as well as Shenandoah Mountain to the east. Similar views are also offered by other open summits on the mountain.

Geographic entities mentioned:
surface_form: river knobs
instance_of: Mountain
countries: United States
coordinates: lat: 38.7369
lon: -79.4347
North Fork Mountain is structurally an anticline mountain and a major component of the Wills Mountain Anticline system.

Geographic entities mentioned:
surface_form: wills mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.845555555556
lon: -78.681666666667
There is no weather station, but this climate table contains interpolated data. Geology. North Fork Mountain is part of the Wills Mountain Anticline, a geological structure that extends from Pennsylvania through Maryland and West Virginia into Virginia. The same geologic ridge that forms North Fork Mountain is known as New Creek Mountain north of North Fork Gap.

Geographic entities mentioned:
surface_form: wills mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.845555555556
lon: -78.681666666667
North Fork Mountain. North Fork Mountain is a quartzite-capped mountain ridge in the Ridge and Valley physiographic province of the Allegheny Mountains, also known as the High Alleghenies or Potomac Highlands, of eastern West Virginia. Kile Knob, at 4,588 feet (1,398 m), is the mountain's highest point, and Panther Knob and Pike Knob are nearly as high.

Geographic entities mentioned:
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
Much of the mountain is within the Monongahela National Forest, and a large portion of the mountain has been proposed for federal wilderness designation or inclusion within a new unit of U.S. National Park System. The Nature Conservancy's Panther Knob and Pike Knob preserves are also located on North Fork Mountain. The scenic North Fork Mountain Trail follows much of the ridge crest, and U.S.

Geographic entities mentioned:
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
National Park System. The Nature Conservancy's Panther Knob and Pike Knob preserves are also located on North Fork Mountain. The scenic North Fork Mountain Trail follows much of the ridge crest, and U.S. Route 33 is the only road that crosses the steep, rugged ridge. Geography. North Fork Mountain runs roughly northeast to southwest for throughout Grant and Pendleton Counties in West Virginia.

Geographic entities mentioned:
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
Future Generations Graduate School's main campus is located at the top of the ridgeline near U.S. Route 33, the only major road that crosses the mountain. Climate. Kile Knob (West Virginia), the highest point of North Fork Mountain, has a humid continental climate (Köppen &quot;Dfb&quot;). There is no weather station, but this climate table contains interpolated data. Geology.

Geographic entities mentioned:
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
Tuscarora quartzite (or sandstone), a layer of erosion-resistant Silurian rock only about thick, the major ridge-forming stratum in eastern West Virginia, caps most of North Fork Mountain, often as a broad, slightly eastward-tilted slab, forming numerous west-facing cliffs and various larger outcrops such as Chimney Top and Harmon Rocks.

Geographic entities mentioned:
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
Shales occur on some of North Fork Mountain's slopes. History. Scattered family homesteads existed on the east slope of North Fork Mountain throughout the 19th and 20th centuries. These few early settlers were of English, German or Dutch stock and constituted a community known as &quot;Smoke Hole&quot;, named for the gorge to the east of the Mountain.

Geographic entities mentioned:
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
(It was listed on the National Register of Historic Places in 1993.) The steeper western slopes have, with few exceptions, always been uninhabited. Most of the forests on the North Fork Mountain were cut for timber in the late 19th and early 20th centuries. Much of North Fork Mountain has been included in the Monongahela National Forest, established in 1911.

Geographic entities mentioned:
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
Most of the forests on the North Fork Mountain were cut for timber in the late 19th and early 20th centuries. Much of North Fork Mountain has been included in the Monongahela National Forest, established in 1911. Panther Knob, near the south end of North Fork Mountain, was first explored botanically by P.A. Rydberg of the New York Botanical Garden in 1926.

Geographic entities mentioned:
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
However, his findings were doubted until the mountaintop was revised by a group of botanists in the 1950s. Beginning in the early 1980s, The Nature Conservancy has become increasingly involved in habitat conservation on North Fork Mountain, working cooperatively with the Forest Service and with various private landowners, as well as establishing preserves on Panther Knob and on Pike Knob. Flora.

Geographic entities mentioned:
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
Other rocky summits, including the summit of Pike Knob, are blanketed by red pine (&quot;Pinus resinosa&quot;) forests, here at their southernmost natural occurrences. The Monongahela National Forest has designated of old growth red pine forest on the mountain as the North Fork Mountain Red Pine Botanical Area.

Geographic entities mentioned:
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
The Monongahela National Forest has designated of old growth red pine forest on the mountain as the North Fork Mountain Red Pine Botanical Area. Another unusual vegetation type on North Fork Mountain is an elfin forest dominated by yellow birch (&quot;Betula alleghaniensis&quot;), mountain ash (&quot;Sorbus americana&quot;), and mountain holly.

Geographic entities mentioned:
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
While North Fork Mountain's lesser rainfall is a substantial factor in this difference, another consideration is the nature of the bedrock itself. North Fork Mountain's fine-grained Tuscarora quartzite erodes into sand, which either quickly disperses or persists in cracks and crevices, sometimes even forming tiny dunelets on wide, nearly flat open outcrops, as on Panther Knob.

Geographic entities mentioned:
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
Fauna. Wildlife on North Fork Mountain includes whitetail deer, wild turkey, black bear, Coyotes, bobcats, gray foxes, timber rattlesnakes, eastern newts, and a variety of other bird, mammal, reptile, and amphibian species. Two U.S. Fish and Wildlife Service Species of Concern are found on North Fork Mountain, the peregrine falcon and the Allegheny woodrat. Golden eagles are also known there.

Geographic entities mentioned:
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
Panther Knob is easily viewed from the west from Snowy Mountain Road south of Cherry Grove. Other views of Seneca Rocks and North Fork Mountain are offered by U.S. 33 as it descends the Allegheny Front approaching Seneca Rocks, and by SR 28 approaching Cherry Grove from the southwest.

Geographic entities mentioned:
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
Kungsholmen. Kungsholmen is an island in Lake Mälaren in Sweden, part of central Stockholm, Sweden. It is situated north of Riddarfjärden and considered part of the historical province Uppland. Its area is with a perimeter of. The highest point is at Stadshagsplan at. The total population is 71,542 (December 31, 2020).

Geographic entities mentioned:
surface_form: Lake Mälaren
instance_of: Lake
countries: Sweden
coordinates: lat: 59.5
lon: 17.2
Miquel Carbonell Selva. Miquel Carbonell i Selva (23 July 1854, Molins de Rei – 14 May 1896, Barcelona) was a Catalan painter, muralist and poet. He is especially known for his realistic portraits and landscapes of the area around the Llobregat River. Biography.

Geographic entities mentioned:
surface_form: Llobregat River
instance_of: Watercourse
countries: Spain
coordinates: lat: 42.282412
lon: 2.012826
His works, which included many hymns and paraphrases of the psalms, and a book called &quot;Without Faith, without God&quot;, were edited by J. Thomson and D. Macmillan, with a memoir (1852). In 1784 he was living in a house in Calton village on Calton Hill. The houses still exist but it is unclear which house he lived in. He continued to live on Calton Hill until his death.

Geographic entities mentioned:
surface_form: Calton Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.955278
lon: -3.182222
Brooks School. Brooks School is a private, co-educational, college-preparatory boarding school in North Andover, Massachusetts, United States, on the shores of Lake Cochichewick. History. Brooks School was founded in 1926 by Endicott Peabody, who had previously established Groton School in 1884.

Geographic entities mentioned:
surface_form: Lake Cochichewick
instance_of: Lake
countries: United States
coordinates: lat: 42.703888888889
lon: -71.097222222222
Brooks School has had just one head of school in over 80 years. The school started admitting day students in the early 1950s and became co-educational in 1979. In the 21st century, Brooks has focused on renovating the campus. New buildings include the arts center, the science center, the admissions building, and a crew boathouse on Lake Cochichewick. Student body.

Geographic entities mentioned:
surface_form: Lake Cochichewick
instance_of: Lake
countries: United States
coordinates: lat: 42.703888888889
lon: -71.097222222222
Lake Emma is within the Hakatere Conservation Park, and is part of the Ashburton Lakes (&quot;Ōtūwharekai&quot;), an area of cultural importance to the iwi Ngāi Tahu because the lakes were a significant food-gathering area and also on a main route for travel between the east and west coasts of the South Island (&quot;Te Waipounamu&quot;).

Geographic entities mentioned:
surface_form: Ashburton Lakes
instance_of: Group of lakes
countries: New Zealand
coordinates: lat: -43.572929
lon: 171.160126
surface_form: ōtūwharekai
instance_of: Group of lakes
countries: New Zealand
coordinates: lat: -43.571666666666665
lon: 171.17555555555555
surface_form: lake emma
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.636
lon: 171.106
surface_form: ashburton lakes
instance_of: Group of lakes
countries: New Zealand
coordinates: lat: -43.572929
lon: 171.160126